See
70 Nee,
t
ea
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vi
THE ANNALS
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MAGAZINE OF NATURAL HISTORY,
INCLUDING
ZOOLOGY, BOTANY, ann GEOLOGY.
(BEING A CONTINUATION OF THE ‘ANNALS’ COMBINED WITH LOUDON AND
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CONDUCTED BY
ALBERT C. L. G. GUNTHER, M.A., M.D., Ph.D., F.R.S.,
WILLIAM S. DALLAS, F.LS.,
WILLIAM CARRUTHERS, F.R.S., F.LS., F.G.S.,
AND
WILLIAM FRANCIS, Ph.D., F.LS.
VOL. XIII.—FIFTH SERIES,
aniigalR —~vnsonian Insti. :
fj, a8 oy way
,
\\ & A az (os
Ne?
Sonal Musev
ake ———_
\
LONDON:
PRINTED AND PUBLISHED BY TAYLOR AND FRANCIS,
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MACLACHLAN AND STEWART, EDINBURGH :
HODGES, FOSTER, AND CO., DUBLIN: AND ASHER, BERLIN,
1884.
“ Omnes res create sunt divine sapientiz et potentis testes, divitia felicitatis
humane :—ex harum usu Jonitas Creatoris; ex pulchritudine sapzentia Domini;
ex ceconomia in conservatione, proportione, renoyatione, potentia majestatis
elucet. Earum itaque indagatio ab hominibus sibi relictis semper estimata;
4 veré eruditis et sapientibus semper exculta; malé doctis et barbaris semper
inimica fuit.”—Linnzus.
“Quel que soit le principe de la vie animale, il ne faut qu’ouvrir les yeux pour
voir qu’elle est le chef-d’ceuvre de la Toute-puissance, et le but auquel se rappor-
tent toutes ses opérations.”—Bruckyur, Théorie du Systéme Animal, Leyden,
1767.
so yo hie oe The sylvan powers
Obey our summons; from their deepest dells
The Dryads come, and throw their garlands wild
And odorous branches at our feet; the Nymphs
That press with nimble step the mountain-thyme
And purple heath-flower come not empty-handed,
But scatter round ten thousand forms minute.
Of velvet moss or lichen, torn from rock
Or rifted oak or cavern deep: the Naiads too
Quit their loved native stream, from whose smooth face
They crop the lily, and each sedge and rush
That drinks the rippling tide: the frozen poles,
Where peril waits the bold adventurer’s tread,
The burning sands of Borneo and Cayenne,
All, all to us unlock their secret stores
And pay their cheerful tribute.
J. Taytor, Norwich, 1818,
CONTENTS OF VOL. XIII.
[FIFTH SERIES. ]
NUMBER LXXIII.
Page
I, On the Fertilization of the Floridee. By Prof. F, Scummpr. ‘
ebseestle SOZC EL Win hon vet tc sinhas os 2) ot ofl reisivi sy 3y 00m: 016k «a, ees snip? Olbyataete te
II. Note on the Structure of the Skeleton in the Genera Corallium,
Tubipora, and Syringopora. By H. AtLEyNE Nicuoxson, M.D.,
D.Sc., Regius Professor of Natural History in the University of Aber-
URI MIE S. ASS ac ccs tiatetes | ehd Teed /a dea's's: Gale Marine ante a atene
II. On the Mantis metallica of Westwood. By J. Woop-Mason 84
IV. Notes on the Genus Gyracanthus, Agassiz. By Dr. R. H.
PereeMEDER elEngr Se LUC. os teh soos sais ole e's we ae's ble w tu Vale aabemale ee
V. Report on the Polyzoa of the Queen Charlotte Islands. By
the Rev. THomas Hincxs, B.A., F.R.S. (Plates ITI. & 1V.) ....: 49
Vi; Lepidoptera from the Island of Nias. By Artuur G.
ere MEE Le GOT Gs wis cles 6 ea tymec es eevee whee +9 wemee
Proceedings of the Geological Society ...........cc cece eeeee
37
New Books:—Farm Insects: being the Natural History and Eco-
nomy of the Insects injurious to the Field-crops of Great Britain
and Ireland, and also those which infest Barns and Granaries.
By Joun Curtis, F.L.S.— Monograph of the British Aphides.
By George BowviER Buckron. Vol. IV.,..........00- 63,
On the Development of Balanoglossa, by William Bateson ; On the
Development of the Branchia in the Cephalopoda, by M. L.
Joubin ; Injury sustained by the Eye of a Trilobite at the Time
of the Moulting of the Shell, by Charles D. Walcott; The
Pelagic and Deep Faunas of the two Lakes of Savoy (the Lac
du Bourget and Lac d’Annecy), by Dr. O. E. Imhof; An In-
stance of Sexual Colour-variation in Crustacea, by H. W. Conn ;
On the Influence of Physico-Chemical Agencies upon the Deve-
lopment of the Tadpoles of Rana esculenta, by M. Emile Y ma as
op
1V CONTENTS.
NUMBER LXXIV.
Page
VII. On a Specimen of Pecopteris (? polymorpha, Brongn.) in
Circinate Vernation, with Remarks on the Genera Spiropterts and
Rhizomopteris of Schimper. By Roserr Kipsron, F.G.S. (Plate V. oe
Bier, i.) vas ce seis e Weare ee He aielele sw nels 6 > 010 0 oe wire aici cae
VIII. On a new Species of Schutzia from the Calciferous Sand-
stones of Scotland. By Rospgrr Kinston, F.G.S. (Plate V. fig. 2.) 77
IX. On the Fertilization of the Floridee. By Prof. F. Scumipr. 80
X. Contribution to the Knowledge of the Freshwater Sponges.
By Dr. F. Vespovsky, of Prague. With Remaris by H. J. Carrsr,
PF Rp. &e- (Llate V1.) 0 5b: une: Mane ee cee +. 96
XI. A Reply to the Remarks of Prof. Duncan on a Paper entitled
‘¢ Contributions to the Actinology of the Atlantic Ocean.” By Prof.
G., LENDSTROMG |. o:ii..ccantwupleeomic am npeeryier= nie ecit: ite «kam 102
XII. On the Species of Pseudoboletia. By Prof. F. Jnerrrey Brxt,
INUSAS, ciaicie hace siee fo ceils eat ates siete t/t inate athe Sette anette etek eee 108
XIII. On new Stylasteride, with Remarks on some recently
described Forms. By J. J. Quricu, B.Sc. Lond., Assistant, Zoolo-
gical Department, British Museum .........-..0eeeesesnectesee Ill
XIV. Contributions to Micro-Paleontology.—Notes on some
Species of Monticuliporoid Corals from the Upper Silurian Rocks of
Britain. By H. Arteyne Nicyozson, M.D., D.Se., Regius Pro-
' fessor of Natural History in the University of Aberdeen. (Plate VII.) 117
XV. Description of a new Genus and Species of Longicorn Coleo-
ptera from the Philippine Islands. By Cuartes O. WATERHOUSE 128
XVI. Generic Characters of the Sponges described in Mr. Carter’s
“Contributions to our Knowledge of the Spongida ” (‘ Annals,’ 1883,
vol. xil.-p.,308).,! By thm AUTHOR, AUid.s aioeaba wn pele 129
XVII. On some Histeride new to the Japanese Fauna, and Notes
of others. . By Groner Luwis, Figs. (a Ek Wabi let open 131
Proceedings of the Dublin Microscopical Club .............. 140—145
Proceedings of the Geological Society ...........-eceeeees 145—146 _
On the so-called Dimorphism in the Genus Cambarus, by Walter
Faxon; On Visual Organs in Solen, by Dr. B. Sharpe; On a
Nematode Parasitic on the Common Onion, by M. Joannes
Chatin ; Evidence of a Protozoéa Stage in Crab Development,
bys, WConn |... .. ccs cee ee ee ...L47—152
CONTENTS.
NUMBER LXXV.
XVII. On Grantia ciliata, var. spinispiculum, Crtr. By H. J.
CaAmrmanmbenics race ag rlete WED). vic ay lea caddie de ok
XIX. Some Preliminary Remarks on the Gemmules of the Fresh-
water Sponges. By Dr. WittiAM MARSHALL ..............000-
XX. On a new Genus of Butterflies from New Zealand. By
mC uri, Wshis. PAS Ge. iP ach.. il aed aeeeue
XXI. N ote on some Parasites of Fishes from Madras determined
by Dr. Orley. By Prof. F: Jnreray Bern, MiA...... 600.0505 dee
XXII. The Ephyre of Cotylorhiza and Rhizostoma, and their
Development into Kight-armed Meduse. By C. CLaus ..........
XXIII. The Lepidoptera collected during the recent Expedition
of H.M.S. ‘Challenger.’—Part II. By Artuur G. Butter, F.L.S.,
F.Z.S., Assistant Keeper, Zoological Department, British Museum
Dy Sie eeEEIS AVL ticle) anes aAn.s lew nie 4+ she noi t SRr acs ehh aire
XXIV. Report on the Polyzoa of the Queen Charlotte Islands.
By the Rev. Tomas Hincxs, B.A., F.R.S. (Plate IX.) ........
XXV. On Schizoporella Ridleyi, MacG., and Schizoporella simplex,
D’Orbigny and Johnston. By J. J. QuEtcH, B.Sc. Lond., Zoolo-
gical Department, British’ Museum... 2... 2. .00. 400s stva newswoman
XXVI. On new Stylasteride. By Brycr WriGHT............
New Book:—Catalogue of the Fossil Sponges in the Geological
Department of the British Museum (Natural History) ; with
Descriptions of new and little-known Species. By Grorer
PRAEGER ORUUN DE FoR, Wsy EGS... as, here oie.e's «Vevayel Secret Shetare gray
Preliminary Report on the Expedition of the ‘Talisman’ in the
Atlantic Ocean, by M. A. Milne-Edwards; New Aphidological
Discoveries, by M. Lichtenstein; Note on two new Californian
Spiders and their Nests, by the Rev. Dr. McCook; On an Aerial
Alga inhabiting the Bark of the Vine, by M. J. B. Schnetzler.
223—-
NUMBER LXXVI.
XXVII. On the Modern Philosophical Conceptions of Life. By
J. J. Woopwarp, President of the Philosophical Society of Wash-
MINEO al Shares sen) ass i ay epaie HRlerv ae 81h0 8 hee ced Hele E eam mE
XXVIII. Note on Professor G.Seguenza’s List of Tertiary Polyzoa
from Reggio (Calabria). By the Rev. Taomas Hr1ncxs, B.A.,
FE.RS.
iW ashe) Real w © w sie) 0 ele) © 0) 6 ¢ © 64s a we 6 6 Ula 06. 4 6 Bs 86 Be HS 6 6.68 Oe F aS
ee crdvelehdieasamnsoteds Sto
Page
153
163
171
215
218
219
232
267
vi CONTENTS.
Page
XXX. The Branched and Unbranched Forms of the Freshwater
Sponges considered generally. By H.J. Carrer, F.R.S. &e....... 269
XXXI. Descriptions of five new Species of Heterocerous Lepido-
ptera from Yesso. By Artuur G, Burter, F.LS., F.Z8., &..... 273
XXXII. Coleoptera collected during the Expedition fof H.MS.
‘Challenger.’ By CHARLES O. WATERHOUSE ....seseeeeeeeeeee 276
XXXIII. On the Classificatory Value of Growth and Budding in
the Madreporide, and on a new Genus illustrating this point. By
Sruart O. Ripiey, M.A., F.L.S., &., Assistant in the British
Museum (Natural History). (Plate XL.) ...........eeeeeeeees: 284
XXXIV. Preliminary Notice of new Genera and Species of ‘ Chal-
lenger’ Reef-Corals.—Part I. By J. J. Quetcu, B.Sc. (Lond.) .. 292
Proceedings of the Geological Society ..........seseeeenee 297—299
New Books:—Notes on Natural Selection and the Origin of Species.
By Francis P. Pascon, F.L.S.—Phytogeogenesis. The Pri-
meval Development of the Crust of the Earth and of Plants.
sketched cut iby Dr. Orro KUNTak .2 2%... eos + omens 500—802
On the Operculum of the Gasteropoda, by M. Houssay; A Fungus
infesting Flies, by Prof. Leidy ; On the Occurrence of Colobus
Kirkii, by Sir J. Kirk; Polythalamia from Inland Salt Water in
Hungary, by Dr. Eugen von Daday ; On the Sexual Differences
of Corebus bifasciatus, and on its supposed Ova, by M. A. La-
boulbéne; New Contributions to the Knowledge of the Rota-
toria, by Dr. Kugen von Daday; On the Development of the
Gamatule, bby Mi Perron. } 0 siccs0.cs eda conven one 304—310
NUMBER LXXVII.
XXXV. The Classification of the Animal Kingdom, with refe-
rence to the newer Zoological Systems. By Dr.'T. Mar@o........ 313
XXXVI. Description of a new Species of Ptycholepis from the Lias
of Lyme Regis. By Jamrs W. Davis, F.G.S. &. (Plate X.) .. 885
XXXVII. On three new Species of Monticuliporoid Corals. By
Artuur H. Foorp, F.G.S., late Assistant Palecontologist to the
Geological and Natural History Survey of Canada, (Plate XII.) .. 338
XXXVI. A Collection of Butterflies from the Fiji Islands. By
crit Go DU ULEMR PLS 4 dE Zi. Sse WGc 8 (ities ace niet SiG mate cet ate 343
XXXIX. A Contribution to the Knowledge of the Marine Fauna
of Kurraehee., By J.jA5 Munna i) i vias jfeas come e aitio ene & 348
XL. Note on the assumed Relationship of Parkeria to Stromato-
pora,and on a Microscopic Section of Stromatopora mamilluta, Fy.
Sehmidt... By dw, wCartaR, ERS. Ret: cas iodine called aS
CONTENTS. Vil
Page
XLI. Contributions towards a General History of the Marine
Polyzoa. By the Rey. Tuomas Hincxs, B.A., F.R.S. (Plates
BBW ACEV <)i <5 cla cos 5 api hela otti, Seer Bie cr ence Sate tie 356
XLII. New Coleoptera in the British Museum. By Cuartzs 0.
MR EMEREA TN I rcs N86. F ogals tel oo. dros © 0 aun as0,n ale coke: dadmmapetiecdar als aid & 370
XLII. Remarks on the Gastrea-Theory. By G. Birscutrt.
(Usd: )o. 2 en chats A ReAe cof Par te ace a Naet vate crc. Ree
XLIYV. On Mesozoic Dicotyledons, By Lester F. Warp,..... 383
XLV. Descriptions of new Species of Reptiles and Batrachians in
the British Museum.—Part II. By G, A. BouLencer
XLVI. On the Genus Megascolecr of Templeton. By F. E.
Bapp anny, MA HRS. Be ost oe Bi ahclvivetarateietr ease erate tie Statete 398
XLVII. On the Hymenoptera collected during the recent Expe-
dition of H.M.S. ‘Challenger.’ By W. F. Kirsy, Assistant in Zoolo-
gical Department, British Museum ..... sea NED Ble ahean! ges reteue ple 402
New Books :—Annual Report and Proceedings of the Belfast Natu-
ralists’ Field Club, 1882-83. Ser. 2, vol. ii. part 3.—Transac-
tions of the Cumberland Association for the Advancement of
Literature and Science. No. VIII. 1882-85, Edited by J. G.
Ie ERET Dy cperetater Web S''e\ o aNer ihe = Wale. warp sails alot Crate Pasar ibd © oR EENG 413
On the Structure of the Otocysts of Arenicola Grubii, Clap., by M.
E. Jourdan; On Prof. Lindstrém’s Remarks on Prof. Martin
Duncan’s Criticisms, by Prof. P. Martin Duncan, F.R.S. &e. ;
Reproduction in Amphileptus fasciola, by Andrew S. Parker,
M.D., Ph.D.; On the Anatomy of Peachia hastata, by M.
Faurot; On a Cilio-flagellate Infusorian recently observed in
Baltimore Drinking-Water, by C.S. Dolley ; How a Carpenter-
Ant Queen founds a Formicary, by the Rey. Dr. McCook ; On
some new and imperfectly-known Exotic Simple Ascidia, by Dr.
ihe VOTED Ea NOt Mane « Giire veaia cow rigs kN yeas Spe 415—424
NUMBER LXXVIII.
XLVIII. On the Origin of the Fauna and Flora of New Zealand.
Pee NW ELUIDDON 2 oleic citja:a.srat ne. Rite agli eae WR 9 Oe Sela ua 425
XLIX. Description of a new Genus of Fossil Fishes from the Lias.
By James W. Davis, F.G.S. &e. (Plate XVI.)
L. On the Neuroptera collected during the recent Expedition of
H.M.S. ‘ Challenger” By W. F. Kirpy, Assistant in Zoological
Department, British Museum ...........-.sccessceesesceseees 453
LI. On the Diptera collected during the recent Expedition of
H.M.S. ‘ Challenger.’ By W. F, Kirpy, Assistant in the Zoological
Department, British Museum ...ceseeesecesecrernccenceeeeees 456
LII. Coral-soundings in the Solomon Islands. By H, B. Guppy,
M.B:, Surgeon H.MLS. ‘Lark’ 1... 20... eee ete e pe neeseeseves 460
LIII. On the Relation of the Pali of Corals to the Tentacles. By
Pe MAnTIN DUNCAN, EB: GC. sc ecs sven ate fet basnimten 466
viii CONTENTS.
Page
LIV. On some Hydrocorallinse from Alaska and California. By
PN cel bete ASAT Ge Yh ae RM abs se Wicwele 8 ADAM MURS See ckyntls 467
LV. Descriptions of Paleeozoic Corals in the Collections of the
British Museum (Nat. Hist.)—No.I. By Roserr ErHeripeGs,
Jun., and ArrHur H. Foorp, F.G.S. (Plate XVIL.)............ 472
LVI. On the Orthoptera collected during the recent Expedition of
HLM.S. ‘ Challenger.” By W. F. Kirsy, Assistant in Zoological
Department, British Marsewmil 9.65, <jsieiale:¢/a: «sa feo crmtedam ate ean een 476
LVIL. Description of an African Species of the Coleopterous Genus
Helota, MacLeay. . By As: SIDNEY QUULLEF J ¢.\5 shbe ss 0 a/c le sete ae 479
Proceedings of the Geological Society ......ccceeeseeerees 48] —484
New Book:—Geological and Natural-History Survey of Canada:
Catalogue of Canadian Plants.—Part I. Polypetale. By JoHn
Macoun, MRA; EELS: Wnne i, Aes eR re aisle chee 484
Freshwater Sponges as Improbable Causes of the Pollution of River-
water, by EK. Potts; On the Brain of Eunice Harassit and its
Relations with the Hypodermis, by M. E. Jourdan; On Mana-
yunkia, by Prof. Leidy ; On a Mediterranean Species of Lingu-
dnopsts, by ‘Drs 1,-G; Bornemann, Jun; oes ce sss 486—490
Indexes Ss SR at Oe Se Lid es a mae aren Ree eta tee eee ~. 401
. PLATES IN VOL. XIII.
git Fertilization of the Floridez.
Til. New Polyzoa.
IV.
V. Spiropteris——Schutzia Bennieana.
VI. Freshwater Sponges.
VII. Monticuliporoid Corals.
VIII. Grantia ciliata,
IX. New Polyzoa.
X. Ptycholepis gracilis.
XI. Anacropora Forbesi,
XI. Monticuliporoid Corals.
se }N ew Martine Polyzoa.
XIV.
XV. fllustrating the Gastrea-theory.
XVI. Lissolepis serratus.
XVII. Paleozoic Corals.
THE ANNALS
AND
MAGAZINE OF NATURAL HISTORY.
[FIFTH SERIES.]
ser aNoategexv avarice per litora spargite muscum,
Naiades, et circim vitreos considite fontes:
Pollice virgineo teneros hic carpite flores:
Floribus et pictum, dive, replete canistrum.
At vos, o Nymphe Craterides, ite sub undas;
Ite, recurvato variata corallia trunco
Vellite muscosis e rupibus, et mihi conchas
Ferte, Dew pelagi, et pingui conchylia succo.”
N. Parthenii Giannettasii Eel, 1,
No. 73. JANUARY 1884.
1.—On the Fertilization of the Floridez.
By Prof. F. Scumirz*.
[Plates I. & IL]
RECENT botanical investigations have proved, in more and
more numerous cases, that in sexual fertilization a direct union
of two sexually differentiated cells takes place, the product of
which, as a fertilized ovicell, becomes developed into the germ
of a new plant. At the same time it appeared that the most
essential point in this union of the two sexual cells was the
union of the nucleus of the male cell, which sometimes con-
stitutes almost the entire mass of this male cell, with the
nucleus of the female cell, in precisely the same way as also
occurs in the fertilizing processes of animalst. Nevertheless
several processes of fertilization not satisfactorily explained
have hitherto stood in the way of a generalization of these
* Translated by W. S. Dallas, F.L.S., from the ‘Sitzungsberichte der
kon. pr. Akademie der Wissenschaften zu Berlin, 1883, p. 215.
+ See also Strasburger, “‘ Ueber den Befruchtungsvorgang,” Sitzungsb.
niederrhein. Gesellsch. fiir Nat.- und Heilkunde zu Bonn, 4th December,
1882.
Ann. & Mag. N. Hist. Ser. 5. Vol. xiii. 1
2 Prof, F. Schmitz on the
results. The Floridez, especially, in which the union of the
two sexual cells usually has as its consequence the further
development of a third more or less distinct cell, present great
difficulties to a general theory of sexuality.
My own observations upon the development of the Squa-
marie had led me to the discovery of peculiar processes in
the formation of the fruit in that group of Floridee, which
joined on to the previous observations of Thuret and Bornet
on the fructification of Dudresnaya and Polyides. This in-
duced me to extend my investigations further, and to attempt
the general solution of the question of the mode of sexual
fertilization and fructification in the Floridee. The solution
of this problem was rendered remarkably difficult by the cir-
cumstance that in my dwelling-place (situated far inland) the
procuring of the requisite material for mvestigation was at-
tended with the greatest difficulty. Hence I feel it to be my
duty to offer my special thanks to the Royal Academy of
Sciences in Berlin, for having enabled me to make a long
sojourn on the sea-coast in the autumn of 1881. And I also
express my most grateful thanks to Dr. Bornet of Paris for
his liberal and always ready assistance with material for in-
vestigation.
This difficulty of procuring suitable material for examina-
tion, in order to complete and conclude the studies that I had
commenced, may also justify me in bringing together in what
followst the results obtained, as a report upon my investiga-
tions up to this time, without at present going much into
detail. I propose still further to continue this investigation of
the Floridez, and, if possible, to complete it by the exami-
nation of all the types of the Huropean seas.
I.
The thallus of the Floridee is generally composed of
branched cellular filaments. ‘These individual branched cel-
lular filaments are sometimes free (Chantransia, Callitham-
nion), sometimes held together by a more or less dense jelly
(Batrachospermum, Crouania, Nemalion), sometimes so firmly
and closely involved by a very dense and tenacious intercel-
lular substance as to represent a parenchymatous cellular
* Sitzungsb. niederrhein. Gesellsch. fiir Nat.- und Heilkunde zu Bonn,
4th August, 1879, pp. 876, 377.
+ The numerous statements in literature which are opposed to various
individual points in the following statement cannot here be entered upon
in detail. This must remain for a future special elaboration of the diffe-
rent groups of the Floridez.
Fertilization of the F loridee. 3
body*. Sometimes in this case the main branch of a system
of ramification projects particularly in the midst of its nume-
rous lateral branches (Batrachospermum) ; sometimes, by rapid
growth of the lateral branches which arrange themselves be-
side it in equal development and strength, it becomes con-
cealed and unrecognizable.
The individual filaments increase in length by apical growth
with acropetally advancing division of the terminal cell, which
sometimes exceeds the rest in size, and is then easily distin-
guished as the apical cell, and sometimes does not differ from
the other cells. Hence the individual branches of the thallus
are sometimes seen to be provided with a distinct apical cell
at the apex of the main branch of the whole system of ramifi-
cations, and sometimes, if neither the main shoot of the system
of ramifications nor the terminal cells of the individual branches
stand out distinctly, they grow in length apparently with an
apical surface, while in all cases the same mode of apical
growth takes place.
The apical growth of the cellular filament is generally fol-
lowed by a frequently very abundant intercalary growth by
extension of the individual cells. In this case, however, no
(orthogonal or oblique) transverse division of the individual
joint-cells ever takes place, any more than a longitudinal
division, with a divisional wall occupying the organic longi-
tudinal axis of the cellf. ‘The only divisions which break
* From this dissimilar structure of the thallus the differences in habit
of the different forms of thallus appear much greater than the differences
of the general mode of growth really are. These essentially consist in a
different behaviour of the older lamelle of the mother-cell membranes.
Thus if these older lamella of the mother-cell membranes are perforated
locally during the outgrowth of a branch-cell, the branch-cell grows
into a free filamentous branch. On the other hand, if these lamelle are
only stretched and lifted up by the growing branch-cell, the branch-cell
remains united with the neighbouring cells in a more or less closely packed
so-called parenchymatous cell-union, and held together by a common ex-
ternal membrane. If these common cell-membranes then swell up gela-
tinously the thallus assumes the form of a system of branched cellular
filaments, which are enclosed and enveloped by a more or less dense
jelly.
: This heterogeneous development of the thallus consequently never pre-
cludes a near relationship of two Floridean genera, however different they
may be in habit at the first glance.
For the same reason, however, a near relationship of two genera can-
not any more be excluded because the spore-forming mass of tissue, the
so-called nucleus of the cystocarp, forms, in the one case, a closed cellu-
lar body, and in the other a branching tuft of filaments (compare, for
example, Helminthora and Nemalion, Callithamnvon and Setrospora,
Cruoria and Cruoriopsis, Chylocladia and Lomentaria, c.). ;
+ For the establishment of this fact, in many cases, very wearisome
and troublesome investigations are necessary, So that it res easily be
4 Prof. F. Schmitz on the
up the individual filament cells, rather cut portions of the
margins off*, which then become developed into longer or
shorter lateral branches.
These marginal cells are formed on the individual joint-cells,
sometimes singly, sometimes in plurality, sometimes simulta-
neously, sometimes one after the other, and, according to their
number and their earlier or later development, they produce a
very heterogeneous habit of the cell-division and of the ramifica-
tion of the individual filaments. A very widely spread mode
is that at the upper end of a newly produced joint-cell a
branch-cell is at once separated off which extends itself by the
side of the terminal cell of the filament almost as rapidly and
strongly as the latter itself, and thus readily produces the
appearance of a regular dichotomous branching; in what
follows this mode of ramification is characterized as subdicho-
tomous as by Bornet.
At each division of a Floridean cell a peculiar pit is formed
in the organic central point of the dissepiment formed ; this
maintains the two sister cells in communication so long as
they remain alivef.
overlooked. In literature therefore there are many contradictory state-
ments (by Nageli, Kny, Reinke, &c.). In all cases, however, that I have
hitherto been able to investigate I have been unable to confirm these
statements ; and now, after very numerous investigations, I believe I am
justified in establishing the above propositions as generally applicable to
the Florideee. Should exceptions really occur here and there, they cer-
tainly take place extremely seldom.
* Upon the circumstance that in the Floridez a joint-cell is never
divided by a transverse wall, or by an (organically) median longitudinal
wall, but that rather lateral marginal cells only are cut off from such
joint-cells, depends also the fact that the cellular tissue of the Floridean
thallus is always to be referred back to a system of branched cellular fila-
ments, even when the thallus is solid and the individual cells are held
together without gaps. Every cell-body constructed under this condi-
tion must show the same behaviour; and it is due only to the cessation
of this condition that the roots, stems, leaves, &c. of the Archegoniata
and Phanerogamia also cannot be referred back to a system of simple
branched cell-filaments.
The Ascomycetes, however, show an exactly similar behaviour to the
Floridese ; in the great majority of them a transverse division of the indi-
vidual joint-cells of vegetative cell-filaments takes place but rarely. In
consequence of this the construction of the thallus out of branched cell-
filaments usually appears just as distinctly in these Ascomycetes also as in
the Floridez ; and the occasional occurrence of parenchymatous cell-bodies
(e. g. in the foundation of the perithecia of Pleospora herbarum (cf. Bauke
in feet ee maa NG pp. 315 et segg.]) is probably due,
ust as in the Floridez, only to a close firm conglobatio 7 -
Tyne branched eelleainiienia Be Ts ee
+ Such a pit consequently occurs both in the lower and in the upper
septum of each joint-cell. Between the two pits of these two transverse
Fertilization of the F loridee. 5
In any subsequent division of the cell, by which, as already
mentioned, marginal cells alone are always separated, this
pit never occurs in any such marginal cell, but is always pre-
served in the joint-cell itself. The same thing is repeated at
each cutting off of a marginal cell, so that from the number
and distribution of these pits, even in the quite unequally
extended cells of full-grown branches of the thallus, the
genetic connexion of the individual cells with the whole of
their neighbour-cells may be recognized, at all events so long
as the occurrence of secondary pits does not produce difficul-
ties. Such secondary pits, however, frequently occur, especi-
ally in species with a small-celled thallus, developed in such
a manner that the individual thallus-cells are placed in con-
nexion with all the neighbouring cells by subsequent develop-
ment of one or more pits in the separating septa, indifferently
whether they are or are not separated by these septa from
sister-cells. Nay, even the cells of the secondary rhizoidiform
medullary-filaments of the thicker Floridean stems are some-
times brought into close connexion with individual cells of the
tissue through which they grow, by such secondary pits.
These pits (which are generally circular) are closed by ex-
tremely thin membranous lamellz. But on each side of these
closing membranes there always lies a thick lamina of a very
dense substance (very easily and intensely coloured* by heema-
toxyline and analogous staining materials), and this so closely
and firmly that it can rarely be separated, and only by swel-
ling up of the closing membraneyt. ‘The two plates are
walls runs the organic longitudinal axis of the joint-cell. As already
stated, no transverse division nor any (organically) median longitudinal
division ever occurs in a joint-cell, and consequently no dissepiment is
ever formed in the joint-cells which either cuts their organic longitudinal
axis or includes it; hence it follows that the joint-cell must always retain
the two original pits in the two end-surfaces, as indeed is the case.
* With regard to this behaviour with colouring agents the substance of
these closing plates of the pits shows a very close analogy with the so-
called mucilage of the sieve-tubes,’which, however, I think, onthe ground
of repeated investigations (on Cucurbitacez), must be regarded quite
otherwise than is now commonly the case.
Thus, while this mucilage is generally regarded as lifeless, and supposed
to travel in the sieve-tubes from cell to cell, I am quite unable to find
in the facts any support for such a migration of the mucilage. In my
judgment this “ mucilage ” rather remains In a definite form (which, how-
ever, is exceedingly easily destroyed in preparation) in the individual cells
in which it was produced. In the more complicated cases (¢. g. 1m the
Cucurbitacez) the formed mucilage-masses (closing plates of the sieve-
plates and uniting hollow cylindrical cords) of the individual joints of the
sieve-tubes (cells) all remain in connexion with each other, and thus
form in the plant a connected system of peculiar cords.
+ I succeeded in effecting this in a very instructive manner In speci-
6 Prof. F. Schmitz on the
directly connected by numerous cords, which principally
(sometimes apparently exclusively) perforate the closing
membrane at the periphery of the pit, and here often coalesce
laterally into hollow cylindrical bands*.
On the other hand, however, these plates are directly and
firmly coherent with the parietal protoplasm of the cell, and
apparently form only the completion of the parietal proto-
plasmic sac T along the surfaces of the pits; in reality, how-
ever, they are probably, at least towards the lumen of the
cell, coated with a very thin layer of protoplasm. In dead
material, the cell-walls of which usually swell up more or
less in a gelatinous form, the pairs of lami remain united,
and in accordance with this we see the contracted plasma-
body of all the individual cells more or less drawn out into
cord-like processes towards the neighbouring cells, connected
together by means of these pairs of lamine.
Thus by means of the cords which traverse the closing
membranes of the pits and unite the two lamine of the diffe-
rent pairs, a direct connexion of the neighbouring cells with
one another is established, and thereby a direct union of all
the cells of the thallus is attained}, enabling these thallus-
cells, notwithstanding their extraordinarily great number, by
unitary cooperation to form a single whole, a single indivi-
dual plant §.
mens of Griffithsia Schousbwt, J. Ag., and Pterothamnion plumula, Nag.,
which had been hardened with picric acid.
* How far analogous closing-plates also belong to the pits of other
Algw (Fucacez, Dictyotacee, Volvocacez, &c.) can only be decided by
further investigation. The fact that, on the contraction of the plasma,
plasma-cords remain pretty regularly attached to these pits, leads one to
expect similar conditions in the structure of these pits. But the small
size of most of these structures greatly increases the difficulty of deciding
the question with certainty.
+ Whether these lamin are produced by local differentiation (chemi-
cal transformation) of the parietal protoplasm, may for the present remain
an open question. I regard this, however, as not improbable.
{ The direct connexion of all the cells of the thallus by means of these
pits has already been indicated by Bornet (‘Etudes Phycologiques,’
p- 100), who, however, regards these pits as perfectly open canals. He
even endeavoured, through this direct connexion of all the thallus-cells, to
explain how, from the fecundated female cell, the fertilizing influence
propagates itself to that cell which grows into the spore-fruit.
§ In my opinion these connecting cords between the two closing plates
of the pit serve essentially for the transference of dynamic influences from
cell to cell; the corresponding pores of the cell-membrane, however, at
the same time render possible a readier exchange of dissolved substances
between the two neighbouring cells. A migration of protoplasm itself
from one cell to another by means of these open communications I regard
as inadmissible.
Various facts indeed seem to me to favour our regarding the two
Fertilization of the Floridex. 7
An open communication, so that an interchange of formed
protoplasmic portions, cell-nuclei, or chromatophores could take
place between the two neighbouring thallus-cells, is, how-
ever, not established by these pits. Such an open communi-
cation is indeed formed only in a few cases (Corallinee*) by
the development of large open pores which are produced sub-
sequently in the common dissepiment of neighbouring thallus-
cells, analogous to the widely diffused H-shaped connexions
of the hyphe of Ascomycetes and Basidiomycetes.
II.
On this thallus the sexual cells originate by the differenti-
ation of certain terminal cells of the entire system of branched
cell-filaments.
The male cells are usually formed in great numbers toge-
ther. Close to the generally small terminal cell of a shorter
or longer branch-filament (one or) several small branch- cells
are formed by the uppermost joint-cells, and these, like the
terminal cell itself, become developed into male cells. The
same thing is repeated in the second and often in the third
joint-cell (sometimes also in the following joint-cells), or
short, one- or more-celled lateral branchlets issue from these
joint-cells, the terminal cells of which, as well as the
branch-cells of the superior joint-cells, become converted
into male cells. Hence the male cells are placed several
together at the apex of the uppermost cell and at the upper
endof the next following joint-cells of a simple or ramified
branch-filament. Such branches are distributed sometimes
singly, sometimes united in groups on the thallus of the
different species of Floridez, and thus form so-called anthe-
ridia of very multifariously variable structure.
Such antheridia sometimes present the form of separate
larger or smaller tufts of filaments (Callithamnion, Scinaia,
&c.) ; but generally a greater or less number of such tufts
closing plates of the pits as those organs of the individual cells which
receive and use up the stimuli transmitted from neighbouring cells. And
likewise, for various reasons, I would regard it as not impossible that the
above-mentioned “mucilaginous masses” of the sieve-tubes (which,
in my opinion, agree in substance with the closing plates) possess a func-
tion perfectly analogous to that of these closing plates and their connecting
cords, namely, essentially the using up and cones of CUA Me
fluences, so that Hanstein’s idea (‘ Protoplasma,’ p. 172), that possibly
the sieve-tubes of plants are comparable to the nerves of animals, would
firmed. ce :
ne . ie Bebra in ‘Sitzungsb. niederrh. Gesellsch, fiir Natur- und Heil-
kunde,’ 1880, p. 122.
8 Prof. F. Schmitz on the
are collected into groups covering larger or smaller portions of
the surface of the thallus (Nitophyllum, Peyssonelia, Polyides,
Ceramium, &c.). Sometimes these groups are immersed and
line depressions of the surface of the thallus, or these depres-
sions may even be converted into pitcher-like receptacles,
which, in their development, present the greatest resemblance
to the spermogonia of the Lichens and Ascidiomycetes (Grace-
laria, Gialaxaura, and many Corallinee). In all cases, how-
ever, the male cells originate exclusively (I have never ob-
served an exception) from the terminal cells of longer or
shorter branches of the thallus-filaments, never from their
joint-cells*. ‘ae
In all exactly investigated cases the individual male cell
appeared colourless from its first origin onwards; formed
chromatophores were never to be recognized in it. On the
other hand, a pretty large nucleus was everywhere to be de-
tected in the protoplasm, which usually contained some small
shining granules. At the complete maturity of the male cell
its membrane ruptures at the apex and the plasma-body issues
forth as a solid spherical or elongated body, which is some-
times drawn out into a tail-like point at the inferior extremity
(Cruoria purpurea, Corallina, Amphiroa). In the interior of
this escaped spermatium, however, a tolerably dense proto-
plasm with some small shining granules always encloses a
pretty large cell-nucleus, which is sometimes central, some-
times rather excentrically placed.
The development and emission of the individual spermatia
of an antheridium takes place gradually. Very frequently,
however, after the evacuation of a spermatium-mother-cell, its
supporting cell grows through it and develops, within the
empty envelope of the spermatium-mother-cell, a new male
cell (Batrachospermum, Chantransia), until the contained
masses of the supporting cell are used up.
The individual escaped spermatia represent small mem-
braneless cells, which, according to the prevailing opinion,
are destitute of any spontaneous mobility. My own observa-
* Some few contradictory statements in literature (on the formation of
the spermatia of Melobesia deformans, in Solm’s ‘Corallinenalgen des
Golfes von Neapel,’ p. 53, and of Hildenbrandtia rivularis, in Borzi
‘Rivista Scientifica, i. no. 1, Messina, 15 May, 1880) I must leave out
of consideration for the present, as I have not myself been able to inves-
tigate the cases referred to. But as I have found the above-given rule
confirmed in all carefully investigated Florideee, even when the first
glance at the antheridia gave one the impression of a quite different mode
of development, I must regard it as not improbable that on more exact
investigation the above-mentioned exceptional cases may also be referred
to the same rule.
Fertilization of the Floridex. 9
tions have also hitherto failed in detecting, with certainty, in
these cells either any locomotive organs, or, indeed, a striking
spontaneous mobility of any kind. But one series of observa-
tions* leads me to think that the prevalent supposition, ac-
cording to which the spermatia only reach the female cells
passively by the movement of the surrounding water, by no
means entirely exhausts the facts; and I would therefore
prefer, for my own part, to leave the question of the mobility
of the isolated spermatia still undecided.
Hr.
The female sexual cells of the Floridez originate without
exception from the terminal cells of longer or shorter lateral
branches of the whole system of ramification of the filaments
of the thallus. These branches are frequently formed only
as secondary lateral branches after the formation of all the
other ramifications. Sometimes they are confined to a very
small number of cells (two or three, rarely one), sometimes they
attain a greater length; and while sometimes they do not
differ in structure from the other neighbouring sterile branches,
in most cases they may easily be distinguished by their formt,
the size of their cells, or the different branching of their joint-
cells. In all cases, however, their terminal. cell finally be-
* For example, when observing living spermatia of Polysiphonia elon-
gata, Grev. (at Heligoland), I quite distinctly saw a single spermatium
travel slowly through the field of the microscope, while the other sper-
matia lay quite still.
Several times I also saw spermatia of the same Polysiphonia attached
in such a manner that the globular spermatium stood off from the sup-
porting surface about twice the length of the diameter of its body,
although still firmly adhering to it, as it accompanied all (even the
smallest) movements of the supporting body with pendulum-like oscil-
lations. It was natural to see in the filamentous connecting cord which,
from what has been said, it must be assumed attached the spermatium
to the supporting body, the cilium of the spermatium which has hitherto
been sought in vain. But, unfortunately, notwithstanding all my endea-
vours, I was unable clearly to detect this supposed cilium, often as I
thought I could discern it.
A further indication of spontaneous mobility in the spermatia of the
Florides is to be found in the fact that in Batrachospermum the spermatia
must penetrate through the gelatinous envelope of the branches of the
thallus in order to reach the apex of the completely immersed carpogonia,
They can hardly be capable of such penetration without some proper
(perhaps amceboid ?) mobility.
+ These branches appear to be particularly noteworthy on account of
their similarity to the “ procarpia’’ of the Collemacee, as in Batrachosper-
mum Julianum, Aycangeli, according to the description of Arcangeli
(Nuov. Giorn. Bot. Ital. xiv. 1882, pp. 160 et seqg. tav. v. figs. 1-8), in
which species the female cell occupies the apex of a short-jointed spirally-
contorted branch.
10 Prof. F. Schmitz on the
comes converted into the female sexual cell by allowing a _
diverticulum to issue from its apex, which elongates into a
longer or shorter hair-like or clavate process, the trachogyne,
which has sometimes one or more spiral contortions (figs. 17,
23) or is bulbously dilated (fig. 33) at the base. ‘This temale
cell may be here described as the carpogonium * (by analogy »
with the oogonium of the Chlorophycez).
At the period of fertilizable maturity the carpogonium con-
tains, in its usually ovate ventral portion, a very abundant
protoplasm with a large distinct cell-nucleus, Sometimes
also well-developed more or less intensely coloured chromato-
phores are contained in this protoplasm (Nemalion, Helmin-
thocladia, Batrachospermum); but in other cases the proto-
plasm of the carpogonium is perfectly hyaline. The tricho-
gyne into which this bellied part of the carpogonium is
continued by means of a short neck-like constriction, is filled
with colourless protoplasm, which is usually free from
vacuoles in the apex itself, but pervaded by more or less
numerous vacuoles in other parts, and also contains some
larger or smaller shining granules of variable number and
distribution (fig. 8), which behave towards staining agents like
the chromatine granules of the cell-nucleus.
At this time the cells of the carpogonial branch (@. e. of that
branch the apical cell of which becomes converted into the
carpogonium) present a very different development in the
different genera and species. In many instances (Batracho-
spermum, Lemanea sp., Naccaria, Chondria, &c.) they are
furnished with more or less numerous lateral branches, while
in other cases they are unbranched. Sometimes the whole of
these cells are somewhat enlarged, and filled with more or less
numerous plasma-masses ; in other cases only certain joint-
cells of the carpogonial branch are enlarged and abundantly
furnished with contents (Calosiphonia) ; but the uppermost of
these joint-cells, the hypogynal cell, is particularly often
distinguished from the other cells by its stronger develop-
ment (Gleosiphonia, figs. 8-10, Scinata, Kc.).
These fertilizably mature carpogonia then in most cases
extend the apex of their trichogyne beyond the surface of the
thallus and into the surrounding water. In certain cases,
* The terminology of the organs of fructification of the Floridez is at
present rather uncertain, The expressions “carpogonium,” “ procar-
pium,” “carpogenous cell,” “ trichogyne,” “trichophore,” “ fructifying
tube,” &c. are used by different authors in very different ways. I have
therefore found myself for my present purpose compelled to settle this
terminology, which, moreover, frequently was not suited to modern con-
ceptions, quite independently, although still, as far as possible, employing
previously established terms.
Fertilization of the Floridee. 11
however, the apex of the trichogyne remains concealed in the
interior of the thallus, that is to say, enclosed within its gela-
tinous envelope (Batrachospermum). But in both cases the
isolated spermatia (by spontaneous movement ?) reach the apex
of the trichogyne and attach themselves to it, at the same
time (hardly previously) surrounding themselves with a mem-
brane. ‘T’hen the membrane of the spermatium and apex of
the trichogyne is resorbed at the point of adhesion, and
through this opening the two masses of contents are placed
freely in connexion. In this way the plasma-bodies of the
carpogonium and spermatium unite to form a single coherent
cell, which at first still contains two different cell-nuclei.
In the next developmental stage the cell-nucleus of the
spermatium has disappeared from its previous place and is
nowhere to be discovered in the interior of the conjugation-cell,
but in the bellied part of the carpogonium there is, as before,
a single cell-nucleus. A fusion of the two original cell-nuclei
to form this latter cell-nucleus could nowhere be directly per-
ceived. Nevertheless, from the analogy of other cases, it may
with the greatest probability be assumed that the cell-nucleus
of the spermatium travels through the trichogyne into the
bellied part of the carpogonium, and here amalgamates with
the cell-nucleus of the carpogonium.
The cell-wall then thickens in the neck of the trichogyne
and narrows the central opening more and more until finally
this is completely closed in the middle (figs. 1, 2-4, 6, 7, 10,
16, 23, 35). In this way the connexion between the bellied
part of the carpogonium and the trichogyne with the sper-
matium is interrupted by means of a more or less thick mem-
branous plug, and the whole conjugation-cell divided into two
independent cells.
These two division-cells, however, are of quite different
value, inasmuch as only the lower cell possesses a cell-
nucleus and now commences a rapid further development ; the
upper one, on the contrary, is quite destitute of a formed cell-
nucleus, and remains inactive until its earlier or later disap-
pearance. The former represents the fecundated female cell,
the fertilized ovicell; the latter, on the contrary, forms a
useless part of the conjugation-product of the two sexual cells,
which is now divided off and thrown aside, while the fertilized
ovicell prepares for further development.
In the interior of the separated trichogyne-cell there are
frequently, varying in number and form, larger or smaller
granules which behave towards colouring-agents like the
chromatine corpuscles of cell-nuclei, but never belonged to
formed cell-nuclei (fig. 1). I have not been able to ascertain
12 Prof. F. Schmitz on the
whether these granules, which are already present within
the trichogyne in the fertilizably mature carpogonium, are
given off by the cell-nucleus of the carpogonium ; but it seems
not improbable that they really originate from the chromatine
corpuscles of that cell-nucleus. The described process of
fecundation would then have to be explained as follows :—
that in the female cell, the carpogonium, the separation of the
directive body (¢. e. a portion of protoplasm with the separated
useless portions of the cell-nucleus) does not take place until
after the union of the male cell with the female cell, and the
fusion of the male cell-nucleus with the nucleus of the female
cell. I have no hesitation* in fact about interpreting the
processes described in this manner f.
Fecundation is effected in the manner just described in all
the Floridez hitherto exactly investigated by me, however
different the form of the trichogyne may be in the individual
cases. Everywhere this trichogyne, after fecundation had
taken place, was divided off as a non-nucleated cell from the
fecundated ovicell by the closure of the short neck of the tri-
chogyne, and abandoned to destruction. The fecundated ovi-
cell, however, then immediately commenced a very active new
growth.
nV:
In this recommencing growth the fertilized ovicell by no
means separates from its previous tissue-connexions (as in
the oogonia of the green Alg or the archegonia of the Arche-
goniata), but rather remains afterwards as before in unaltered
connexion with the neighbouring hypogynous cell and retains
the old cell-membrane of the carpogonium as its own cell-
membrane, extending and strengthening it as required. Nay,
* In most instances, certainly, in plants (as in animals), the directive
corpuscle is separated before the fecundation of the female cell (see Stras-
burger, ‘ Befruchtung und Zelltheilung,’ pp. 79, 80), as, for example,
among the Algze in Utdogonium, Coleochete, and Vaucheria (in the last-
named alga the directive corpuscle contains numerous small fragments of
nucleus which have been separated off from the numerous cell-nuclei of
the young oogonium). But an expulsion of the directive corpuscle
only after fecundation has taken place cannot be regarded as at all incon-
ceivable if we consider that in the expulsion of the directive body only an
evidently useless part of the cell-nucleus with some protoplasm is sepa-
rated and thrown off from the female cell, but that such a rejection of
the separated part of the cell-nucleus may just as well take place before
as after the conjugation of the two sexual cells.
+ The portion of the female cell destined to be expelled as a directive
body was consequently employed before its separation as an extended
trichogyne to intercept the spermatium, and thus to facilitate the access
of the male cell-nucleus to the nucleus of the female cell.
Fertilization of the Floridez. 13
even the pit which united the carpogonium-cell with the
hypogynous cell also continues its function, and places the
fertilized ovicell in direct connexion with the hypogynous cell,
and through this with the general cellular tissue of the parent
plant. Hence the requisite nutritive materials can be trans-
mitted to the growing ovicell in the simplest and most con-
venient manner. Nay, this connexion of the fertilized ovicell
with the tissue of the thallus of the parent plant is so com-
plete, that this fertilized ovicell easily produces exactly the
impression of an ordinary thallus-cell, from which, in fact, it
can sometimes be distinguished almost solely by its perfectly
peculiar further development (Chantransia corymbifera, Thur.,
figs. 2, 3, 4).
This further development of the ovicell is, however, very
different in the individual cases.
1. Helminthocladice.
In the simplest case the ovicell pushes forth one after the
other numerous offshoots, ooblastemas as they may here be
called (fig. 1), which grow into short-jointed cell-filaments of
greater or less length, and abundantly subdichotomously
branched. ‘The number of these ooblastema-filaments is,
however, very variable; sometimes they are produced in
great numbers on the whole periphery of the ovicell except
the basal surface and the vertex (Batrachospermum); sometimes
their development on the ovicell is only one-sided (Chan-
transia, figs. 2-4, Scinaza, fig. 7) ; sometimes the ramifica-
tions of these ooblastema-filaments are perfectly free (Batra-
chospermum, Chantransia, Helminthocladia, Nemalion, Sci-
naia), and sometimes they are united by a common gelati-
nous envelope into a nearly globular closed cell-body (Hel-
minthora, according to Bornet*). Sometimes also the
fertilized ovicell first of all arches upwards and cuts off a large
upper daughter-cell, and the ooblastema-filaments then push
forth from the whole free surface of this daughter-cell
(Nemalion multifidum).
In the genus Lemanea several ooblastema-filaments grow
forth from the fertilized ovicell at the apex of a carpogonial
branch, which may be unramified (LZ. fluviatilis and ciliata,
according to Sirodot’s figures f) or furnished with short lateral
branches (L. torulosa, and, according to Sirodot’s figures, also
L. catenata and parvula}), and these filaments growing ob-
* Thuret-Bornet, ‘ Etudes phycologiques,’ p. 64,
+ Ann. des Sci. Nat. sér. 5, tome xvi. pl. iii,
¢ Ibid. pls. iv. and v.
14 Prof. F. Schmitz on the
liquely downwards extend into the cavity of the tubular
thallus, and here become abundantly ramified.
In all these cases, however, by ramification of the ooblas-
tema-filaments a more or less abundantly and closely com-
pressed tuft of threads is formed, and this sometimes remains
naked (Chantransta, Lemanea), but in most cases is furnished
with a more or less dense envelope of cell-filaments proceed-
ing from the carpogonial branch or the neighbouring filaments
of the thallus (Batrachospermum, Nemalion, Helminthocladia),
which sometimes even close together to form a_ solid
fruit-wall (Scinaia). Sometimes also certain of these sterile
envelope-filaments grow through the ramification of the fertile
tuft of filaments, and become interwoven, as sterile para-
physes, among the branched ooblastema-filaments (Batracho-
spermum).
In certain cases (Batrachospermum, Chantransia, Nemalion,
Helminthocladia) these ooblastema-filaments finally develop
single carpospores from the terminal cells of their ramifications.
These terminal cells swell up and become filled with an
abundance of contents. At last the membrane at the apex of
the cell bursts, and the whole plasma-body escapes as a
single naked spore. ‘These spores are successively evacuated
from the different terminal cells of the same tuft of filaments ;
but after the evacuation of the individual terminal cell its
supporting cell grows through it and produces within the
evacuated membrane a new spore-forming terminal cell, until
finally all the nutritive substances of the whole tuft of fila-
ments are used up. In other cases, besides the terminal cells
of the ramifications of the tuft of ooblastema-filaments, the
upper joint-cells also develop single carpospores in greater or
less number, so that these become developed into longer or
shorter, simple or branched chains (Scinaia, Lemanea).
In all these instances, however, the developed fruit, the
cystocarp, constitutes a more or less richly branched tuft of
filaments, sometimes naked, sometimes covered with envelop-
ing filaments, sometimes surrounded by a closed fruit-wall,
and either immersed in the thallus or attached externally.
2. Gelidiee.
In the cases hitherto referred to, the spore-forming ooblas-
tema-filaments are nourished during their development from
the thallus-tissue of the pareit plant by the intermediation of
the ovicell, which remains persistent (usually as the central
cell of the whole tuft of filaments). This, however, is no
moe the case in a group of genera which come nearest to
these.
Fertilization of the Floridez. 15
In these forms the fertilized ovicell usually develops only a
single ooblastema-filament (Caulacanthus, fig. 39, Pterocladia),
which, ramifying abundantly, turns towards the middle of the
branch of the thallus to which it belongs, and with its rami-
fications clings round the central cord of cells, the so-called
central axis of the branch, which at this part is frequently
(Pterocladia, Wrangelia pectinata, Ag.) enveloped by a
special small-celled tissue with abundant contents. Through
the cell-masses of this tissue the ramifications of the ooblas-
tema-filament twist about and frequently attach themselves
firmly to individual very full cells of this tissue (Pterocladia),
or, when it is deficient, to the cells of the central cord itself
(Caulacanthus, fig. 39), here and there also entering into
direct connexion with them by the development of pits
(Wrangelia). Bemg abundantly nourished through the
agency of this tissue, the branches of the ooblastema-tilament
then ramify very considerably, and develop from each of the
clavate and erected terminal branch-cells either a single spore
(Caulacanthus) or short chains of two (or more) spores, in the
same way as in the Helminthocladiez already described.
Thus by the abundant ramification of the ooblostema-
filament there is produced a tuft of spore-forming filaments,
which spread out in the interior of the branch of the thallus,
and give rise to a local enlargement of it. This enlargement
increases more and more until the maturity of the spores,
and becomes constantly more and more distinctly marked off
from the remaining sterile part of the thallus-branch. This
dilated part then finally constitutes the fruit, the cystocarp, of
these Floridean genera, the peripheral tissue of the thallus
becoming developed into the fruit-wall, in which an aperture
of egress is produced by local separation of the cells, while in
the interior the mass of the spores is produced around the
central cell-cord from the ramifications of the ooblastema-
filament. :
In some of these forms (Naccaria Wigghit, Endl., and
hypnoides, J. Ag.) a further complication of the course of
development of the fruit occurs. Here the carpogonial branch
in very different states of development is beset with several
short lateral branchlets, and in this way forms a pluricellular
complex of larger and smaller cells (figs. 24 and 26 *), gene-
rally with abundant contents. ‘The sprouting ovicell now
enters into open connexion with one or another of these
neighbouring larger cells, with complete amalgamation of the
two plasma-bodies (fig. 27), and only then does the ooblastema-
* See the explanation of the figures.
16 Prof. F. Schmitz on the
filament shoot forth from the conjugation-cell and become
developed in the manner above described. In detail this
conjugation of the growing ovicell with neighbouring cells
rich in contents (auxiliary cells, as they may be called in the
sequel) takes place in very different ways according to the
species. In general, however, the only object of this borrowing
from neighbouring cells rich in contents in connexion with
the development of the ooblastema-filament is evidently to
strengthen the latter, which originates from the very small
fertilized ovicell, and enable it to develop more luxuriantly.
3. Cryptonemiece and Squamariee.
In some of the last-mentioned forms, as stated, the cells of
the creeping spore-producing filaments enter into close con-
nexion with the cells of the central axis or of its enveloping
tissue by the formation of pits, evidently for the facilitation of
nutrition. This goes still further in a series of other forms
which follow these most closely (Dudresnaya, Polyides, Du-
montia, Calostphonia, Gleosiphonia*, Petrocelis, Cruriopsis,
and other Squamariea).
In these one or several ooblastema-filaments shoot forth
from the fertilized ovicell, and these either become immedi-
ately diffused in the surrounding thallus-tissue (Dumontia,
Gleosiphonia, fig. 10, Calosiphonia, fig. 23), or first of all
become connected by pit-formation with neighbouring auxiliary
cells (generally cells of the carpogonial branch itself), and
then grow further (Petrocelis Ruprechti, Hauck), or, lastly,
enter into a conjugation with these auxiliary cells, when the
ooblastema-threads issue from the conjugation-cell singly or in
plurality (Dudresnaya, fig. 17, Polyides). In all cases, how-
ever, the ooblastema-threads, branching abundantly, creep
about as thin long-jointed cell-filaments in the interior of the
thallus-tissue.
While thus creeping about the apices of these cell-filaments
attach themselves to certain cells rich in contents, which are
developed in greater or less number in the vicinity of the
carpogonial branches within the branch of the thallus. Some-
times these cells are simple joint-cells of the ordinary sterile
branches of the thallus-filaments, scarcely distinguished by
their size from the other cells of the filament (Calosiphonia) ;
* Berthold has also observed processes similar to those occurring in the
above-mentioned genera in other Cryptonemiacez (species of Halymenia,
Nemastoma, and Grateloupia), but has hitherto published no detailed
account of them (see Falkenberg, in Schenk’s ‘ Handbuch der Botanik,’
Ba. ii. p. 184). My own attention was called by Berthold to the occur-
rence of such processes in Calostphonia.
Fertilization of the Floridez., 27
in other cases these cells are easily distinguished by their
remarkable size (Petrocelis, Polyides) ; in other cases, again,
they become developed into peculiarly-formed thallus-fila-
ments, and are thus easy to detect in the midst of the sterile
tissue (Dudresnaya, figs. 18, 20, Dumontia). To these cells,
which from their subsequent behaviour are also to be called
auxiliary cells, the ooblastema-threads attach and unite them-
selves.
Sometimes (Petrocelis Ruprecht’, Hauck) the apex of the
ooblastema-thread grows directly to the auxiliary cell and
attaches itself firmly thereto. By resorption of the separating
membranes the apical cell itself enters into a conjugation with
the auxiliary cell. In the majority of cases, however, the
apex of the ooblastema-thread grows close by the auxiliary
cell, not unfrequently clinging to it (fig. 18), and then sepa-
rates as a growing terminal cell (fig. 20). But the newly
formed joint-cell, which is now applied more or less closely to
the auxiliary cell, enters into open connexion therewith by the
development of a shorter or longer conjugation-process. In
both cases, after the resorption of the separating membranes,
the plasma-bodies of the auxiliary cell and the ooblastema-
cell unite to form a single cell-body.
The further development of this conjugation-cell is, how-
ever, very different in the various individual cases. In many
instances (Polyides, Petrocelis, Dudresnaya) the amalgama-
tion of the two conjugating cells is limited to the union of
the two protoplasm-bodies into’a single cell-body, while the
cell-nuclei of the two conjugating cells remain separated, and
are still to be found within the two halves of the conjugation-
cell. In these cases a process issues laterally from that half
of the conjugation-cell which represents the ooblastema-cell,
and its apex becomes segmented off as a separate cell (fig. 19),
and then, by further growth, gives origin to a distinct spore-
complex*. Lastly, in other cases (Gleosiphonia) the two
conjugating cells fuse together completely, and from the
ooblastema-cell the whole of the protoplasm, with the cell-
nucleus, gradually passes over into the auxiliary cell until
only the external membrane remains (figs. 11,12). Then
the auxiliary cell becomes separated off as an independent
* In Dudresnaya coccinea, Crouan, the terminal cell of this process
does not grow into a spore-complex (as in D. purpurifera, J. Ag.), but it
develops into a long-jointed cell-filament, which, as a side-branch of the
ooblastema-thread, diffuses itself in the surrounding tissue. But besides
this process of the former ooblastema-cell (one or) two ae
issue from the same cell (fig. 21), which apply themselves laterally to the
former auxiliary cell, grow and close around it, and then produce a single,
sometimes indistinctly bilobed spore-complex.
Ann. & Mag. N. Hist. Ser. 5. Vol. Xlil. ,.
18 Prof. F. Schmitz on the ‘
cell from the emptied ooblastema-cell and shoots forth late-
rally (fig. 13). This outgrowth, however, becomes separated
off as an independent cell (fig. 14), and then, as the central
cell, gives origin to a single spore-complex (fig. 15).
Thus, in the first case, the individual joint-cell of the
ooblastema-thread (after prelimimary conjugation with an
auxiliary cell) produces a lateral branch-cell which leads to
spore-formation, just as in the Gelidiez, previously described,
only that here this cell does not give origin to a single spore,
but (just in consequence of the conjugation with an auxiliary
cell) to a whole complex of spores, which appears to be indi-
vidualized as a single fruit or cystocarp. Here the ooblas-
tema-cell is evidently strengthened by the conjugation with
the auxiliary cell, and rendered capable of the production of
more numerous spore-mother-cells (Polyides, Dudresnaya).
In the latter case, however, this calling in aid of the auxiliary
cell passes into a complete amalgamation and union of the
ooblastema-cell with the auxiliary cell, after which the re-
sulting conjugation-cell becomes further developed in the same
way as the ooblastema-cell assisted by the auxiliary cell in
the former case,
Thus, in both cases, either a lateral offshoot becomes sepa-
rated off as an individual cell and then commences a very
rapid growth, or, more rarely, this rapid new growth proceeds
from the conjugation-cell representing the ooblastema-cell.
More or less numerous marginal cells are separated off from
this outgrowing cell as the central cell of the cystocarp, and
grow into short-jointed abundantly-branched cell-filaments.
By this means is produced a more or less highly-developed
tuft of filaments, the filaments of which either remain indivi-
dually free (Peyssonelia, Cruoriopsis*), or are held together
* With regard to Cruortopsis 1 have formerly stated (Sitzungsb. d.
niederrh. Gesellsch. ftir Natur- und Heilkunde zu Bonn, 1879, p. 877)
that after the conjugation of the “ fertilization-tube” of a “ procarp”
without a trichogyne, the other cells of the latter become directly con-
verted into spores. I must now correct this statement in this respect,
that after the conjugation of the ooblastema-cell with an auxiliary cell
(the above-mentioned cell of the trichogyneless “ procarp”’), the former
cell sprouts as the central cell of the cystocarp, and gives origin to one or
two short lateral branches of from one to three cells. These lateral
branches take a direction parallel to the erect thallus-filament, so that of
two lateral branches, the one regularly grows upwards and the other
downwards. Both together then precisely present the aspect of a tri-
chogyneless “procarp,’ with the middle ceil of which the “ fertiliza-
tion-tube” has conjugated, just as I formerly interpreted the observed
facts. After I had found the key to the processes in the fructification of
the Florideze by the comparative investigation of numerous individual
forms, it became comparatively easy to fathom and establish as above the
development of Cruortopsis, the complete elucidation of which in detail,
for a time, presented many difficulties.
Fertilization of the Florides. 19
as a closed cell-body by a common dense and tenacious gela-
tinous envelope (Cruoria, Polyides, Dudresnaya, Dumontia,
Gleosiphonia, Calosiphonia). The individual sections of this
tuft of filaments reach maturity sometimes simultaneously,
sometimes at different times; but all the filaments of these
sections develop their superior cells, or even almost the whole
of their individual cells, into spores, which, in the latter
case, directly envelop the central cell, which alone remains
sterile (Dumontia), but in the former case are separated from
this central cell by a more or less abundant mass of sterile
cells, the so-called placenta of systematic authors (Glwosipho-
nia, Dudresnaya).
Here, then, the conjugation of an ooblastema-cell with an
auxiliary cell leads finally to the development of a complex
of spores, which, as an independently individualized cell-body,
is sometimes surrounded with a special envelope by the sur-
rounding thallus-tissue, sometimes enclosed in the thallus-
tissue without any such envelope. Such a cell-body shows
exactly the habit of a distinct independent spore-fruit, and is
accordingly regarded as a distinct independent cystocarp.
But, in accordance with what has been stated, the origin of
such a cystocarp is quite different from that of the individual
cystocarp of the Helminthocladiesw and Gelidiee. In the
latter the fertilized ovicell develops into an individual spore-
fruit (cystocarp), as in the Mosses; but in the present case
the ovicell grows into a branched system of offshoots, which
develops numerous individual cystocarps on its branches,
analogous to the numerous spore-fruits of the branched ferns.
These individual cystocarps in the Squamariee frequently
come so near together that they can hardly be distinguished
from each other as independent fruit-bodies. ‘Thus in Cruri-
opsis cructata, Duf., numerous cystocarpia, in the form of short
chains of spores, which are generally interrupted in the middle
by the sterile central cell, lie close together among the erect
filaments of the thallus. “In Peyssonelva the individual closely
approximated cystocarps form tufts of branched filaments, the
branches of which arrange themselves among the erect parallel
filaments of the nemathecia, and develop into separate chains
of spores; so that here also, at the commencement of the
maturity of the spores, numerous chains of spores are lodged
close to each other among the erect sterile fibres. These
chains of spores consequently appear as the essential, inde-
pendently individualized fruit-bodies, just as in Cruortopsis,
and accordingly, just as in Cruortopsis, they have been de-
scribed as the true cystocarps, and distinguished, under the
name of cystidia, as a special form of cystocarpia. “
~
20 Prof. F. Schmitz on the
4. Corallinee. *
In the Squamariez parallel thallus-fibres with carpogonial
branches and auxiliary cells also often stand in great num-
bers close together (Petrocelis, Cruoriopsis). This is the case
to a far greater degree in the Corallinese, which moreover, in
other respects, closely approach the Squamariez.
In these Corallinee the formation of the fruit begins with
the development of a closed stratum of long parallel thallus-
fibres. The penultimate cell of these threads becomes en-
larged, and develops (usually in a characteristic manner) one
or several unicellular lateral branches, which place themselves
beside the terminal cell. But in a larger or smaller number
of these parallel cell-fibres bicellular side branches are also
developed on this penultimate cell, while the terminal cell
becomes developed into the carpogonium and puts forth a
long trichogyne. The penultimate cells of all these parallel
cell-fibres, however, become auxiliary cells.
Of the numerous carpogonial branches which are in this
way placed close together only a small number attain com-
plete development and fertilizable maturity, the majority being
aborted (and this is observed in the same manner also among
the Squamariez, e. g. in Petrocelis Ruprechti, Hauck). But
on the fertilization of a perfectly developed carpogonium the
fertilized ovicell enters (at least as I think I may assume,
from the analogy of the other Floride*) into a conjugation
with the nearest auxiliary cell; the conjugation-cell thus
formed then puts forth several processes, which immediately
conjugate with the auxiliary cells in their immediate neigh-
bourhood ; and this process of conjugation is then further
continued laterally to the following auxiliary cells until a
tolerably extended layer of auxiliary cells is amalgamated into
a distinct large discitorm conjugation-cell. At the margin of
this disk several offshoots are then pushed forth ; these be-
come divided by a transverse dissepiment, and thus give
origin to so many separate spore-complexes.
* This point in the development of the fruits of the Corallines (the
exact investigation of which, as is well known, is rendered remarkably
difficult by the small size of their cells) I have hitherto been unable to
establish directly.
Moreover, not only in the Corallinese, but also in many other Floridese
with small-celled, closely packed cellular tissue, there are special diffi-
culties opposed to the exact ascertainment of the fate of the fertilized
ovicell, which render these investigations eavtremely troublesome and
tedious, and greatly hinder any certain decision. From this also are to
be explained the numerous divergent statements which occur in literature,
and which differ essentially from the present explanation precisely in this
point.
Fertilization of the F loridez. 21
In detail this process shows many and various peculiar
variations in the different forms of the Corallinez ; but in gene-
ral its course is that the ooblastema-fibres of the fertilized ovi-
cell conjugate successively with several approximated auxiliary
cells, until, but only after the last conjugation, a sprouting forth
of the conjugation-cell is set up, which develops a complex of
spores (here usually a single chain of spores). The close
union of the whole of the thallus-fibres, which bear auxiliary
cells and carpogonial branches, has, however, as its conse-
quence, that the whole of the spore-complexes which originate
in consequence of the above repeated conjugations are placed
very close together and form a connected group, which rises
as a single whole upon the thallus, and therefore is to be
regarded as an individual cystocarp. But according to its
development this individual cystocarp is essentially different
from the individual cystocarp of the Helminthocladies and
Gelidiez, and rather approaches more nearly to the group of
isolated cystocarps which, in the Cryptonemiexw and Squama-
rie, proceed from the ooblastema-threads of a single fertilized
carpogonium.
5. Ceramiece, Rhodomelee, Spherococcee, Rhodymeniee,
and Gigartinee.
Among the Cryptonemiee already referred to, Gleosiphonia
presents the peculiarity that a single, short branch-filament
of the thallus-tissue develops its penultimate cell into an
auxiliary cell, whilst the lowest cell of this branch develops
laterally a short, three-celled carpogonial branch. ‘The carpo-
gonium and auxiliary cell are thus in this case formed as a
pair, and close together*, so that it is the simplest thing
possible for the ooblastema-fibres of the fertilized carpogonium
to meet with the auxiliary cell belonging to it, in order to
unite with the latter. In fact, in Gleosiphonia the single
sparingly branched ooblastema-thread usually grows directly
to its auxiliary cell and conjugates with it, unless the ooblas-
tema-thread of a neighbouring earlier fertilized carpogonium
has already preoccupied it.
Such a condition must, however, be greatly facilitated when
the auxiliary cell is brought still nearer, or into the close
vicinity of the carpogonium. The ooblastema-thread may
then be reduced to a very small length or completely sup-
pressed, as the fertilized ovicell can enter into direct union
with the contiguous auxiliary cell.
* Such groups of carpogonial branches and auxiliary cells, which arise
as independent wholes me the thallus of the parent plant, are indicated
in the sequel as fruit-rudiments or procarpia.
22 Prof. F. Schmitz on the
This is really the case in a very great number of Floridex,
nay, I believe I may assert that in the majority of the Flori-
dew in general (in the numerous families of the Ceramiez,
Wrangelies, and Rhodomelez, the Chylocladieex, Rhodyme-
niew, and Spherococcee, and lastly, the Gigartinez) the
further development of the fertilized ovicell is effected in this
manner.
A short, frequently three- or four-celled carpogonial branch
is attached laterally to a thallus-fibre, and is at the same time
curved in such a manner that the carpogonial cell is directly
applied against the neighbouring auxiliary cell, or, at least,
can conveniently reach it by means of a short lateral process.
Not unfrequently, also, the direct contact of these two cells is
brought about by the auxiliary cell itself extending towards
and closely applying to the carpogonial cell a lateral diverti-
culum or conjugation-process (figs. 31, 35, 38). In other
respects, however, the position of the carpogonial branch and
the auxiliary cell in the tissue of the thallus may be very
variable.
1. These organs are most easily observed in many Cera-
mie and Wrangeliee.
Thus in Pterothamnion plumula, Nag. (fig. 35), for example,
one of the terminated (begrenzte) lateral branches of the thallus
bears, inserted at one side of its basal cell, a four-celled, short-
jointed carpogonial branch, which bends its apex towards the
upper surface of the branch, while, on the opposite side of this
basal cell, a unicellular branch develops into the auxiliary cell,
which also curves its apex towards the upper surface of the whole
branch of the thallus, and thus comes into direct contact with
the carpogonial cell. In other cases a shorter or longer
terminated cell-filament bears near the apex on a joint-cell a
short (usually three- or four-celled) carpogonial branch, while
from the same joint-cell several other, one- or more-celled
lateral branchlets issue (fig. 34). Sometimes this joint-cell
itself becomes the auxiliary cell (Lejolisia mediterranea, Born.,
according to Bornet) ; in other cases one of the unicellular
lateral branchlets which issue, besides the carpogonial branch,
from the joint-cell develops its cell into the auxiliary cell
(Ptilothamnion pluma, Thur., and Spondylothamnion multifi-
dum, Niig., according to Bornet) ; or an auxiliary cell origi-
nates on each side from the unicellular lateral branchlets
(Spermothamnion, certain species of Callithamnion, fig. 34).
In many species of Callithamnion the cell-filament which
bears the carpogonial branch and the two auxiliary cells
on one of its joint-cells is not terminated, but grows on at the
apex without alteration fora longer or shorter time (C. corym-
Fertilization of the Floridez. 23
bosum, Lyngb., &c.). In Griffithsia the penultimate joint-
cell of a terminated small-celled branch-filament bears laterally
two short two-celled branchlets, the lower cell of which produces
lateraliy a four-celled carpogonial branch, and then itself
becomes developed into the auxiliary cell. In Ceramium, on
the other hand, the joint-cell of a still-growing branch develops
laterally a two-celled branch, the lower cell of which becomes
the rather large auxiliary cell, but also develops laterally not
only one but two four-celled carpogonial branches.
2. The arrangement of these parts in the multicellular off-
shoots of the Rhodomelee is still more complicated and ditti-
cult of recognition.
In Polystphonia, as is well known, the individual joint-cell
first of all develops a whorl of branch-cells, which, closing
together firmly at the sides, surround the central cell with a
closed rind, which, by the continued division and branching
of its cells, becomes more or less thickened according to the
species. Here the carpogonia are now usually formed on special,
terminated, lateral offshoots. On one of the superior joint-cells
of such an offshoot one of the “ marginal cells,” and indeed
the last-formed unpaired marginal cell, grows into the four- or
five-celled carpogonial branch. Its lowest cell becomes the
auxiliary cell, but the small-celled apex of the branch bends
upwards, so that the carpogonial cell touches the auxiliary
cell with the lower angle (figs. 36, 28) ; while, in the simplest
cases, from the auxiliary cell itself a unicellular, sterile,
lateral branchlet proceeds downwards. At the same time the
other “ marginal cells” of the above joint-cell divide and
branch repeatedly, and thus produce a small cell-body, which
encloses the carpogonial branch together with the auxiliary
cell, and, as it rises as a whole distinctly on the thallus, may
appropriately be characterized as a procarpium.
In other species of Polysiphonia and other genera of the
Rhodomelez this procarpium appears still more complicated,
because, besides the terminal carpogonial branch, one or two
lateral branchlets issue from the auxiliary cell, and these
sometimes branch abundantly and give origin to a many-celled
cell-complex, which in the fertilizable procarpia conceals the
auxiliary cell, and may easily be interpreted (as, indeed, has
hitherto been generally the case) as a ‘ group of carpogenous
cells” (Chondria tenuissima, Ag.). Perhaps, also, in some
of these forms a plurality of auxiliary cells may be formed in
the individual procarpium ; but I have hitherto never been
able to demonstrate such a case with certainty.
3. Among the Chylocladiew the carpogonial branches in
Chylocladia kaliformis, Hook., are usually very early formed
24 Prof. F, Schmitz on the
near the still-growing apex (fig. 29). On one of the large
cells composing the wall of the tubular thallus-joints a four-
celled branch is developed upon the cuter side, and this curves
in a characteristic fashion and develops its apical cell into
the carpogonium (figs. 30, 33). But over this carpogonial
cell larger covering cells curve from both sides (more rarely
from one side, fig. 31), which are segmented off from the two
bordering cells of the thallus-wall, and bend over in such a
manner that they are applied to the carpogonium by their
extended margin, the conjugation-process (fig. 32). These
two cells represent the auxiliary cells, of which, however,
after the fertilization of the carpogonium, only a single one, as
a rule, arrives at further development.
4, As the clearest example of the structure of the female
sexual organs in Spheerococcese the genus Nitophyllum may
here be cited. In the species of this genus (e. g. N. venu-
losum, Zan.) the formation of the sexual organs proceeds from
a single cell of the originally always one-layered thallus.
This separates off towards the under surface of the flat thallus
‘several branch-cells, which further branch in various ways ;
but superiorly it regularly forms two branch-cells, one of
which develops a short sterile pluricellular branch, while the
other, besides a terminal sometimes divided cell, develops a
three- or four-celled small-celled branch, the terminal cell of
which becomes the carpogonium. ‘This branch bends from
its point of insertion in such a manner along the supporting
cell, that its terminal cell is applied to the opposite end of
the supporting cell, and then from the apex of this terminal
cell the short trichogyne is extended outside through a fissure
between the neighbouring cells. ‘This supporting-cell becomes
the auxiliary cell.
5. Among the Rhodymeniee, for example in Plocamium
eoceineum, Lyngb., a short three-celled lateral branch, the
terminal cell of which becomes the carpogonium, is formed
supplementarily upon one of the larger cells within the locall
enlarging small-celled external cortical layer (fig. 37). This
short branch bends along the simultaneously enlarging sup-
porting cell and then extends the trichogyne externally from
the apex of the terminal cell through the overlying cellular
tissue. ‘This mother-cell of the carpogonial branch, however,
develops at its upper end a lateral diverticulum, a conjuga-
tion-process, until it comes in contact with the carpogonial
cell, and forms for its part the auxiliary cell (fig. 38).
6. Finally, of the Gigartiner, Gigartina Teedii, Lmx.,
and Chondrus crispus, Stackh., likewise present, within the
small-celled external cortical layer of the thallus, small secon-
Fertilization of the Floridee. 25
dary lateral branchlets, formed upon certain cells of the vege-
tative cell-filament, and these curve in a characteristic manner
so that their terminal cell approaches very closely with one of
its corners to the supporting-cell, which at the same time also
greatly increases. This terminal cell becomes the carpogo-
nium, the trichogyne of which is much enlarged, but in a
variable manner, at its base *, before it extends itself exte-
riorly as a thin capillary process through the small-celled
cortical tissue; but the supporting-cell of the whole carpo-
gonial branch becomes the auxiliary cell.
Different as the arrangement of the carpogonia and auxiliary
cells may be in all these individual cases, the forms in question
nevertheless agree in the mode of further development of these
organs after the fertilization of the carpogonium has taken
lace.
First of all the ventral part of the carpogonium becomes
segmented off as the ovicell. In the next stage of develop-
ment this ovicell appears emptied of protoplasm, except a
very small residue (it was but seldom that I found more
abundant plasma-masses retained in the ovicell, e.g. in Calli-
thamnion plumula, Nig.), but the closely approximated
auxiliary cell appears very full of contents and at once com-
mences a new and rapid growth.
That in this case the protoplasm (with the cell-nucleus) of
the fertilized ovicell (or at least a part of this protoplasm with
the cell-nucleus) migrates into the auxiliary cell can hardly
be doubted, as the ovicell empties itself to a greater or less
extent; but the mode of this transference I have hitherto
been unable to ascertain with certainty in its details.
In Gleosiphonia open conjugation takes place between the
ooblastema-cell and the auxiliary cell; but after the migration
of the protoplasm of the former cell, the latter cell completely
closes the aperture of conjugation by the new formation of a
portion of membrane, so that after the conjugation has been
effected scarcely any trace of it is to be detected (fig. 12). If
in this case the protoplasm of the ooblastema-cell passed very
rapidly over into the auxiliary cell, it would depend entirely
upon chance whether one could succeed in fixing the two cells
during the conjugation, and so bring the latter to demonstra-
tion; but with the slower course that the process really follows
it is not very difficult to find such stages of conjugation in
fixed material.
In the forms now under consideration I believe we must
* Such enlargements of the base above the neck of the trichogyne
also occur among many other Floridee with densely packed cellular
tissue (see figs. 33 and 38).
26 Prof. F. Schmitz on the
assume that the process of conjugation takes place in exactly
the same way as in Gleosiphonia, but that it is effected much
more rapidly than in that genus, so that direct observation of
the conjugation-stages is perfectly a matter of chance. Not-
withstanding all my endeavours, however, chance has not
hitherto been favourable to me in the present forms (which
are also difficult of investigation in other respects). Never-
theless at present I would not doubt of the occurrence of a
true conjugation of these two cells.
It is true that it is quite possible that there may be a
migration of the protoplasm (with the cell-nucleus) of the ovi-
cell into the auxiliary cell wrthout complete conjugation of
the two cells (as in the fertilization of the Phanerogamia *, of
many Peronosporee [ Phytophthora, Peronosporat], Krysiphex,
&c.) through the separating membranes }, that is fine pores
(not micellar interstices) of these membranes. But the analogy
of the nearly allied Floridean genera, which distinctly show a
complete conjugation of these two cells, appears to me still
too weighty to allow me to decide in favour of this latter
assumption so long as we have no certain demonstration upon
a readily accessible object of the non-occurrence of conjuga-
tion §.
After this migration of the protoplasm (that is, of the cell-
nucleus) of the fertilized ovicell into the auxiliary cell, the
latter commences a very rapid new growth, which leads to the
development of a fruit-body. This growth, however, takes
place in the above-mentioned individual groups in very diffe-
rent manners, and the consequence of this is the very different
structure and habit of the different forms of fruits ||.
* Strasburger, ‘Befruchtung und Zelltheilung,’ p, 58 ; ‘ Bau und Wachs-
thum der Zellhiute,’ p. 247; Sitzungsber. d. Ges. f. Nat.- und Heilk. zu
Bonn, December 4, 1882.
+ De Bary, ‘ Beitrage zur Morphologie und Physiologie der Pilze,’ 4te
Reihe, pp. 72, 73.
t See also Pringsheim’s description of the passage of amceboidal plasma-
masses through the membrane of the antheridial tube of Achlya colorata
(Sitzungsb. Akad. Wiss. Berlin, 1882, p. 870).
§ The fact that I have myself for a long time endeavoured in vain to
demonstrate such a conjugation in the easily accessible species of Calli-
thamnion, Spermothamnion, and G'riffithsia, would certainly seem to lend
support to the notion that here there is really no conjugation of the cells
in question.
|| To enter in more detail into the further development of the cysto-
carp in the various genera of Floridez would lead us too far. But one
of these forms of fruit needs special mention, as it has been affirmed to
have a parthenogenetic origin.
Thus while in the majority of the species of Callithamnion the spore-
complex into which the single auxiliary cell grows constitutes a dense and
close tuft of filaments, a close cell-body (favella), this spore-complex in
Fertilization of the Floridee. 27
It is, however, a very common phenomenon that the deve-
loping auxiliary cell first of all puts forth a rather large diver-
ticulum, and then separates it off as an independent cell.
From this cell, as the central cell of the entire fruit-body,
numerous side-branches then sprout forth, which ramify more
or less, and finally produce, from single or numerous cells of
their whole system of ramifications, individual naked carpo-
spores. The mother-cell of this central cell, the former
auxiliary cell, however, sometimes remains undivided, some-
times develops only a few side-branches, which spread out
laterally and attach the developing spore-fruit to the branch
of the thallus (Callithamnion corymbosum, Lyngb. &e.), and
sometimes branches more abundantly, and forms with its
Callithamnion versicolor, Draparnauld (according to Bornet, ‘ Etudes phy-
cologiques,’ p. 70, note 4, identical with C. seirospermum, Harv. [ =Sei-
rospora Griffithsiana, Harv.|, C. stipitatum, Nig., and C. hormocarpum,
Holmes), forms a loosely branched tuft of filaments, exactly like the
tufts of Seirospora, which in this species originate by metamorphosis of
the apices of the branches. These “seirosporiform favelle,” according
to Falkenberg (‘‘ Meeresalgen des Golfes von Neapel,” in Mitth. der Zool.
Station zu Neapel, i. p. 255), originate by parthenogenetic development
of the auxiliary cells, the carpogonia being either early aborted or not
developed at all, while the auxiliary cells belonging to them continue their
development notwithstanding. From my own observation, however, I
cannot agree with this interpretation of the facts. Certainly in C. verst-
color, Drap. (as in many other Floridez), there are often aborted carpo-
gonia, the auxiliary cells belonging to which persist. But these auxili-
ary cells do not grow into parthenogenetic spore-fruits, but simply become
small sterile thallus-cells in the same way as in other species of Calli-
thamnion; and these “ seirosporiform favellz” originate from auxiliary
cells, the carpogonial branch belonging to which develops a normal car-
pogonium with a well-developed trichogyne. Evidently such carpo-
gonia were accidentally no longer persistent in the specimens of the plant
investigated by Falkenberg.
Moreover Falkenberg ((oc. cit.) cites the present plant not as C. vers?-
color, Drap., but as C. corymbosum, J. Ag., var. ? sevrosporum, and Ber-
thold (“ theirs der Algen im Golf von Neapel,’ in Mitth. d. Zool.
Stat. iii. p. 515) has quite recently united the same plant with C. corym-
bosum, Lyngby (J. Ag. Sp. Alg. iii. p. 40). From this latter species, cer-
tainly very similar in habit, in which seirospore are entirely wanting (and
which, moreover, occurs with C. versicolor in the Bay of Naples), C. ver-
sicolur, Drap., is distinguished not only by the form of the cystocarps and
antheridia (to which attention has already been called by Bornet, /oc. cit.),
but also by the structure of the individual thallus-cells. In C. versicolor,
Drap., the sterile thallus-cells are always uninucleate, while in C. corym-
bosum, Lyngby (with the exception of the youngest cells) they are always
multinucleate (see my statements in the Sitzungsb. d. niederrh. Ges. f.
Nat.- u. Heilk. zu Bonn, June 7, 1880, p. 125 [p. 4 of the separate im-
pressions ]). baer «Stet
So far as I know, a parthenogenetic, ¢. e, apogamic, origin of the spore-
fruits has never been described in any other Floridee.
28 On the Fertilization of the Florideee.
ramified lateral branches, in conjunction with the neighbouring
thallus-tissue, a very variously formed envelope around the
developing spore-tuft.
Sometimes, indeed, the auxiliary cell enters upon a per-
fectly different course of development; as, for example, in
Chondria tenuissima, Ag. In this species, namely, the
auxiliary cell at the period of fertilizable maturity bears, be-
sides the terminal carpogonial branch, two very richly rami-
fied lateral branchlets, which coalesce closely, to form an
elongated cell-complex, which pushes the carpogonial branch
somewhat to one side. After fertilization the auxiliary cell
then increases in size, and, conjugating with the nearest cells
of that cell-complex, becomes developed into a large, branched,
multinucleate cell, which bears, attached to its outer surface,
numerous two- or three-celled sterile cell-filaments, the final
ramifications of the cell-filaments of that cell-complex. Then
at the superior free extremity of this conjugation-cell, which
(so far as I could make out) is not here segmented off as an
independent cell, several lateral branches sprout forth, one
after the other, and these, ramifying abundantly, form a short
stumpy tuft of sporigerous filaments. I have no doubt that
similar processes will be observable in other Rhodomelee.
Lastly, the Gigartinee (Gigartina, Chondrus) call for
special notice. In these forms the single auxiliary cell be-
comes itself the central cell of the spore-fruit. From its whole
surface cell-filaments shoot forth in all directions like the rays
of a star, and diffuse themselves, branching abundantly, in
the surrounding thallus-tissue*.
In Gigartina these branched filaments finally develop single
naked carpospores from the individual cells of the filaments.
In Chondrus, on the other hand, numerous cells of these fila-
ments enter into close connexion with individual neighbouring
cells of the sterile thallus-tissue by the formation of a pit, and
then, from individual cells of these filaments by repeated divi-
sion, there originate complexes, each consisting of four cells,
which, for their part, give origin each to a naked carpospore.
Consequently, even within so natural a group as the Gigar-
* Hence the offshoots of the auxiliary cell in the present series of
forms, the Ceramieze, Rhodomelez, Spherococceee, Rhodymeniex, Gigar-
tine, and § V. appear perfectly analogous to the offshoots of the
fertilized carpogonial cell, which are indicated in the preceding as ooblas-
temas. It may therefore be advisable to contrast them as secondary
ooblastemas or meta-ooblastemas with those primary ooblastemas. This
appears to be particularly indicated if we regard (as I believe we are
bound to do, see under § V.) the action of the fertilized carpogonial cell
(7. e. the ooblastema-cell in Glwostphonia and other similar species) upon
the auxiliary cell as a second act of fertilization, and interpret the fer-
tilized auxiliary cell therefore also as a fertilized ovicell.
On the Skeleton in Corallium, Tubipora, and Syringopora. 29
tineze, there is a repetition of the same phenomenon which has
been previously described in the series of forms of the Gelidiex
and Cryptonemiez, namely, that in certain forms the ramified
ooblastema-filaments produce spores directly from their cells ;
whilst in others these individual cells enter into connexion
with the cells of the surrounding sterile thallus-tissue, and thus
the formation of multicellular complexes of spores is super-
induced*.
[To be continued. ]
Il.—wNote on the Structure of the Skeleton in the Genera
Corallium, Tubipora, and Syringopora. By H. ALLEYNE
Nicuotson, M.D., D.Sc., Regius Professor of Natural
History in the University of Aberdeen.
SoME time ago I published a short paper on the structure of
the skeleton in Tubzpora, with special reference to the rela-
tions of this genus to the Paleozoic Syringopora (Proc. Roy.
Soc. Edinb. 1880-81, p. 219). The general conclusion to
which I was led by a comparison between these two types
was that, though undoubtedly similar in aspect, they were not
really related to one another. The grounds upon which I
based this conclusion were the following :—
(1) ‘In the first place, there is the very important and
remarkable difference in the minute structure of the calcareous
skeleton in the two types in question. In Tubipora the
corallum is made up of fused calcareous spicules, which are
so disposed as to give rise to a universally distributed system
of minute canaliculi or tubuli, which open on both the outer
and inner surfaces of the skeleton by well-marked apertures.
The size of these tubuli is comparatively so great that it is
quite impossible that their presence could be overlooked in
thin sections of Syringopora, if they really existed in this
genus. Qn the other hand, the skeleton of Syringopora, as
* I have hitherto found among the Gigartines nothing analogous to
the third case, namely, that the cells of the ooblastema-filaments conju-
gate with individual cells of the thallus, and then these thallus-cells de-
velop into multicellular spore-complexes.
+ Mr. Hickson has rightly pointed out that the term “ fused” as applied
to the spicules of Tubipora might lead to some misconception, as actual
amalgamation of the spicules does not take place. The spicules, on the
other hand, are united with one another closely by their sides or projecting
points, and it was to indicate this union only that I employed the term
“ fused ” in my former paper.
30 Prof. H. A. Nicholson on the
regards its minute structure, is quite compact, and shows no
signs whatever either of being penetrated by a system of
tubuli or of being formed by the fusion of ectodermal spicules.”
(2) Secondly, I was not able to recognize in Tubipora any
thing which appeared to me to be truly of the nature of
“tabule;’ nor did [ regard the “ axial tube” of Tubipora
as truly homologous with the funnel-shaped tabule of Syrin-
gopora.
(3) I pointed out that the corallites in Syringopora are
provided with a well-developed system of septal spines, which
are extremely similar to the septal spines of various species of
Favosites and Porites, whereas I had been unable to detect
similar septal spines in the corallites of Tubipora.
Recently an elaborate paper has been published by Mr.
Sydney J. Hickson “On the Structure and Relations of
Tubipora” (Quart. Journ. Micr. Sci., Oct. 1883). In this
memoir Mr. Hickson comes to the conclusion that the genus
Tubipora is, after all, closely allied to Syringopora, and that
the latter is really an Alcyonarian, the Favositide also being
referable to the Alcyonaria. In formulating this conclusion,
Mr. Hickson passes in review the three points mentioned above
which had led me to believe that Syringopora and Tubipora
were not really related to one another; and I should wish,
therefore, to make one or two remarks on each of these points.
In the first place, as to the wide difference in the minute
structure of the corallum in these two genera, Mr. Hickson
remarks that “it is difficult to see why this difference should
be considered of any great morphological importance. The
size of the pores or ‘ tubuli,’ as Prof. Nicholson calls them,
varies considerably in the different regions of the corallite,
being at the younger ends much larger than they are at the
older ends, so that it is evident that as the corallite grows
older the tubuli have a tendency to be filled up, and a still
further continuation of this process would make the wall of
the corallite quite aporous. I have no evidence to prove that
the complete filling-up of these perforations in the walls ever
does occur in Zubipora; but should an example be found in
which this has occurred, I should certainly not consider it
sufficient reason for the formation of a new genus or even a
new species. ‘That the skeleton of Syringopora ‘ shows no
signs of being formed by the fusion of ectodermal spicules’
is not to be wondered at, as we possess no means of studyin
either the development or the growth of the skeleton of this
form, since the delicate growing ends would be broken down
and destroyed ; and even in recent genera (such as Corallium,
Lacaze-Duthiers), in which the skeleton is known by an
Skeleton in Corallium, Tubipora, and Syringopora. 31
examination of its growth to be composed of fused spicules,
no evidence of them can be seen in thin transverse section
through the hard parts.”
With regard to Mr. Hickson’s statement that it is “ difficult
to see’? why the difference between the spicular skeleton of
Tubipora and the compact skeleton of Syringopora “ should
be considered to be of any great morphological importance,” I
can merely say that this is clearly a matter of opinion. For
my own part I find it difficult to see why this distinction as to
the minute structure of tle corallum should not be considered
as of great morphological importance; and some investiga-
tions that I have recently been carrying out have very much
confirmed me in this opinion. The hypothesis, on the other
hand, that possibly an aporous form of Tubzpora may be in
future discovered, would not lead me to disregard the known
structure of the actual form of Yubipora. Moreover it is not
only that the skeleton of Syringopora does not show “ signs
of being formed by the fusion of ectodermal spicules,” but that
it does show signs of having a structure very similar to that of
various undoubted recent Zoantharians, and quite unlike that
of any known recent Alcyonarian. Again, it is not the case
that ‘ we possess no means of studying either the develop-
ment or the growth of the skeleton” of Syringopora, “ since
the delicate growing ends would be broken down and de-
stroyed.” On the contrary, as regards the growth of the
skeleton, any good collection of Paleozoic corals contains
perfect colonies of Syringopora, in which the growing extre-
mities of the tubes are as well preserved as we have any
ground for supposing that they would be were the coral a recent
one; and an examination of these growing ends shows that
they do not differ in minute structure from what is found in
the older parts of the tubes.
Lastly, as regards the structure of the skeleton in Corallium,
Mr. Hickson has fallen into error, and his argument, in reality,
points in the opposite direction. He argues, namely, as I
understand him, that Syringopora may have really had a
spicular skeleton, because in the recent genus Coralliwm,
though we know from an examination of its growth that the
skeleton is really composed of fused spicules, “ no evidence of
them can be seen in thin transverse section through the hard
parts.” As a matter of fact, however, such spicules were
shown to exist in sections of the skeleton of Corallium by La-
caze-Duthiers, and were both described and figured by Kolliker
(‘Die Bindesubstanz der Ceelenteraten,’ p. 146, Taf. xvi.
fig. 9). It is not necessary, however, to quote authorities on
such a point, as I have never had any difficulty in demon-
32 Prof. H. A. Nicholson on the
strating the presence of the component spicules in any thin
section of the skeleton of Corallium that I have prepared.
The annexed sketch of part of a longitudinal section of a
branch of Corallium will show that the skeleton is made up
of spicules of the ordinary type of these structures amongst
the Alcyonarians, the outline of the spicules being sometimes
indistinct, and the interspaces between them being occupied
by a peculiar crystalline tissue. Essentially similar pheno-
mena are seen in transverse sections of the skeleton of Coral-
lium. I may add that [ have also always found it possible
to recognize the presence of the component spicules of the
corallum even in the genus Js?s, though the fusion of the
spicules is here much more complete than it is in Corallium.
In fact, the spicules in Corallium are not, strictly speaking,
fused,” any more than they are in T’ubipora.
Part of a longitudinal section of Corallium rubrum, magnified 180 times,
showing the spicules of the skeleton united by a crystalline or fibrous
matrix, produced by the calcification of the soft interspicular tissues.
In the second place, Mr. Hickson has made a series of very
interesting investigations as to the endothecal structures of
Tubipora, in which he shows that there is a much closer
apparent resemblance between the axial tube of this genus
and the infundibuliform tabule of Syringopora than I had
been led to believe was the case by examining the specimens
of the former genus at my disposal. He also shows that flat
tabule, sometimes complete and sometimes incomplete, are
{
}
Skeleton in Corallium, Tubipora, and Syringopora. 33
present in Zubipora. These latter structures, which are evi-
dently very variable, I have not succeeded in detecting, but I
do not doubt their existence. I cannot, however, admit that
the presence of flat tabule in Zwubipora affords any strong
argument for concluding that this genus is nearly related
either to Syringopora or to any of the Favositide. Nor,
indeed, can I admit that tabule, in themselves, are any guide
whatever to the zoological position of any calcareous skeleton,
whether recent or extinct, since these structures are known to
occur in Zoantharians (Pocillopora &e.), Alcyonarians (Helio-
pora), Hydrozoa (Millepora), and Polyzoa (Heteropora). I
cannot, further, allow Mr. Hickson’s statement (loc. ct. p. 21),
that “tabule are quite unknown amongst the Poritide,”’ to
pass without pointing out that, in making it, he has fallen
into error. Thus Dana, long ago, showed that “ tabule,”
essentially similar to the tabule of Favosites, occur in the
genus Alveopora, and figures of these were given by this dis-
\"
Part of a longitudinal section of the corallites of Porites clavaria, Lam.
(Recent), enlarged eleven times. ¢, tabula; ss, septal spines, cut across near
their bases; p, septal spine, projecting into the visceral chamber; ™,
mural pore.
tinguished observer in support of his statement. It is, more-
over, easy to demonstrate by means of thin sections that
“ tabula,” in all essential points quite like those of the l’avo-
Ann. & Mag. N. Hist. Ser. 5. Vol. xiii. 3
34 Mr. J. Wood-Mason on Mantis metallica.
sitida, occur in species of the genus Porttes itself. Thus, I
find them to be well developed in Porites clavaria, Lam., and
to be even more numerously developed in Porttes astreoides,
Lam. I annex asketch of a thin longitudinal section of some
of the corallites of Porites clavaria, to show the tabula (fig. 2).
As I purpose, however, to return to this subject at greater
length, I shall say nothing further about it here, merely add-
ing that a comparison between the accompanying section of
Porites clavaria, Lam., and a corresponding section of such a
species of Havosites as I". hemispherica, Yand. & Shum., will
show how striking is the structural agreement between the
two.
Finally, as regards the existence of septa, Mr. Hickson
has described in 7ubipora certain septiform structures which
he finds occasionally to unite the axial tube to the theca; and
he also mentions that ‘ occasionally individual spicules will
project out radially into the cavity of the corallite in a manner
exactly similar to the so-called ‘septa’ of Syringopora.”
JT regret that I cannot accept either of these structures (both
of which I have seen) as being at all of the nature of true
septal spines, or as being in any way properly comparable
with the vertically arranged spiniform septa of Syringopora.
The septal spines of Syringopora are, on the other hand,
properly comparable, in my opinion, with the septal spines of
such Zoantharians as Porites and Alveopora.
T need hardly add, finally, that I find myself compelled to
dissent entirely from Mr. Hickson’s conclusion, that “ the
evidence at our command tends to prove that the Favositide
are really Alcyonarians, and that Syringopora is also an
Alcyonarian allied to Tubipora.” On the contrary, | think
the evidence at our command is sufficient to prove that the
Favositide are Zoantharians closely allied to the Poritide,
and that Syrinyopora, instead of being an Alcyonarian and
allied to Tubipora, is a Zoantharian and allied to Havosites.
On this last point I hope shortly to publish some interesting
additional evidence that I have recently obtained.
III.— On the Mantis metallica of Westwood.
By J. Woop- Mason.
THE beautiful species of the Orthopterous family Mantodea,
which was described and figured nearly forty years ago by
Prof. Westwood in his ‘ Arcana Entomologica,’ under the
name of Mantis metallica, would appear still to be unique, or at
Mr. J. Wood-Mason on Mantis metallica. 35
any rate very rare, in Kuropean collections, no specimens of it
having been seen either by De Saussure or by Stal, the latter
of whom makes not the slightest allusion to it in his ‘ Sys-
tema Mantodeorum,’ while the former is able to do no more
than place it next ‘after his Odontomantis javana, one of the
two species to which it turns out to be most nearly affined,
A second specimen has at last been obtained in the district
adjoining that from which the first was received. It was
captured in September 1881, on Nemotha, a peak of the
North Cachar hills, which rises to the height of 3336 feet,
by my native collector, by whom it was forwarded alive to
Silchar, where I happened at the time to be stationed.
The species belongs to the subfamily Harpagide of Stal’s
system, and is very closely allied to Odontomantis javana,
Saussure, and to Antissa pulchra, Fabry. It differs from the
former, but not from the latter, in the discoidal vein of the
wings being branched ; from the latter, but not from the for-
mer, in the transverse ridge of the clypeus being angulated ;
and from both of these species in its greater robustness, in its
more firmly chitinized integument, and especially in the form
of the prothorax ; on which last account | propose for its re-
ception a new subgenus, which may be thus named and cha-
racterized :—
NEMOTHA, subgen. nov.
Pronotum robust and tolerably broad, strongly constricted
posteriorly ; the portion of it in front of the constriction oval ;
the disk of its posterior lobe slightly inflated on each side ot
the median ridge at the anterior end. Clypeus transversely
elevated into a strongly angulated ridge. Frontal shield
obtuse-angular at base, with the angle but slightly projecting ;
its disk furnished with two short and widely separated ridges.
Discoidal vein of the wings branched.
Nemotha metallica.
Mantis metallica, Westwood, Arcana Entomol. ii. p.54, pl. 62. fig. 3, 2.
?. Head, legs, margins of the pronotum as far back as
the constriction and a band running from the margins across
the supracoxal groove, and the under surface shining black,
with blue reflections like the blue-black paper used to cover
pill-boxes, with all the articular membranes, two streaks on
each eye, the middle two fourths of the first joint of the
fore tarsi (this paler and greenish), a thick bracket-shaped
mark at the posterior end of the second, third, fourth, fifth,
and sixth abdominal sterna, all the soft and membranous
3%
36 Mr. J. Wood-Mason on Mantis metallica.
parts of the thoracic sterna, and a short streak on the extre-
mity of the dorsal crest of the four posterior femora pale
turquoise-blue; head between juxtocular bosses from vertex-
line to ocelli, and the disk of both lobes of the pronotum yellow,
of the shade of autumn leaves; tegmina yellow-green, clouded
with reddish fuscous, and narrowly edged in front with jet-
black, their anal area red at the very base, beyond which the
veins are red and the meshes smoky ; wings with base and an-
terior area rather opaque, red, passing into yellow at extremity,
as to the rest black-smoky with purple reflections ; abdomen
above dark steel-blue, tipped with yellow.
Head thicker than in A. pulchra; forehead marked by five
longitudinal grooves ; facial shield a little longer, its obtuse-
angled basal margin projecting very slightly in the middle
line, its disk furnished on each side with a transversely elon-
gated tubercle, representing the ridges present in A. pulchra ;
clypeus transversely elevated into a prominent angulated
ridge, from the middle of which a strong longitudinal ridge
runs. forward to the anterior margin of the part; labrum
convex. ;
Pronotum robust, only about twice as long as broad, tra-
versed along the middle from about the commencement of the
posterior fourth of the anterior up to the pair of smooth eleva-
tions near the hinder end of the posterior lobe by a coarse
ridge; strongly constricted posteriorly; the portion of it
lying in front of the constriction having an oval outline, which
is slightly broken on each side antero-laterally by a faint
flattening or oblique truncation of the edge; the prominent
heart-shaped disk of its anterior lobe having two conspicuous
oval wrinkled elevations, placed obliquely on each side of the
posterior end; its posterior lobe having the muscular impres-
sions at the anterior end large and deep, and the part of the
disk between these impressions and the constriction somewhat
inflated on each side, so that the groove in which, in the
allied species, the ridge is throughout lodged is, in this part
of its length, effaced ; its finely-denticulate lateral margins a
little lamellar.
Organs of flight extending by about one sixth of their
length beyond the apex of the abdomen, of the same structure
and texture as in A. pulchra; the discoidal vein of the wings
3-branched, with one of the branches on one side bifurcate.
Legs longer and slenderer.
Abdomen oval, about 1} times as long as broad.
Total length of body 28 millim.; length of pronotum 8,
breadth of pronotum at dilatation 4°5; length of abdomen 12,
On the Genus Gyracanthus, Agassiz. 37
breadth of abdomen 8 ; length of tegmina 22, breadth of teg-
mina 6; breadth of marginal field 1°5.
_ The above description was drawn up from the living
insect.
Hab. Sylhet and North Cachar hills, Assam.
The specimen has since been compared with the mutilated
type in the Oxford Museum by Professor Westwood and
myself, and found to agree perfectly therewith. The discre-
pancy between Westwood’s figure and the above description
as to the structure of the discoidal vein of the wings is ex-
plained by the bad state of preservation of the typical specimen.
1V.—WNotes on the Genus Gyracanthus, Agassiz.
By Dr. R. H. Traquair, F.R.S.*
1, Did Gyracanthus possess dorsal spines?
Although Agassiz himself pointed out that the spines of
Gyracanthus were not bilaterally symmetrical, inasmuch as
one side was more rounded than the other, he nevertheless
regarded them as dorsal, and so did people in general, until
in 1863 Messrs. Kirkby and Atthey pointed out the probable
pectoral nature of some at least of these appendages, the
grounds for this conclusion being the conspicuous lateral cur-
vature shown by such specimens, along with the wearing
away of the apices, as if they had been subject to habitual
attrition at the bottom of the water in which their possessors
lived. In 1868 Messrs. Hancock and Atthey returned to
the subject t, and, reviewing the extensive series of specimens
in the collection of the last-named gentleman, divided them
into two categories—first, those with lateral curvature and
worn apices, and second, those in which apparently there was
* Read before the Royal Physical Society of Edinburgh, December 19,
1883.
+ Ann. & Mag. Nat. Hist. (4) 1868, vol. i. p. 3868. In a footnote
Messrs. Hancock and Atthey refer to a paper by Messrs. Atthey and
Kirkby, entitled “ Fish-remains in the Coal-measures of Durham and
Northumberland,” as having been read before the British Association at
Newcastle in 1863, and as containing the first suggestion of the paired
nature of these spines. I cannot find this paper in the British Associa-
tion’s ‘Proceedings’ for that year; and although a paper of the same
title is found in the ‘ Proceedings of the Tyneside Naturalists’ Field Club,’
it contains no reference to Gyracanthus. These original remarks would
therefore seem not to have been published.
38 Dr. R. H. Traquair on the
only an antero-posterior curvature and in which the apex was
entire and pointed. The former set, which could also be
arranged in pairs, they regarded as pectoral, the latter as
dorsal*.,
The occurrence of numerous spines of this genus in the
Blackband Ironstone of Borough Lee, near Edinburgh, having
lately induced me to inquire into the whole subject of Gyra-
canthus, I was surprised to find that, among the numerous
specimens which came under my observation from that and
other localities in Seotland, there was not one which was
bilaterally symmetrical, and which consequently could be
assigned to a median position. On this subject I published
a few remarks in the ‘Geological Magazine’ for December
1882. To pursue the subject further it was, however, abso-
lutely necessary to reexamine the specimens in the Atthey
collection, now in the museum at Newcastle-on-Tyne. And
having recently visited that city, I must here express my
cordial thanks to my friends Mr. W. Dinning, Secretary of
the Newcastle Natural-History Society, Mr. R. Howse,
Curator of the Museum, and Mr. J. Hancock, member of com-
mittee, for the kind and liberal manner in which they afforded
me every facility for examining the specimens in that remark-
able collection of Coal-measure vertebrate remains.
Although I have not seen the original type of Agassiz’s
Gyracanthus tuberculatus, 1 have no hesitation in referring to
it the great majority of the specimens from Newsham in the
Atthey collection, and they form, indeed, a most beautiful and
instructive series. And as no systematic description has been
given of this form since the time of Agassiz, who had only a
drawing of a mere fragment to go upon, it will not be out of
place to enter somewhat into detail as to the configuration of
these spines.
Proceeding first to the consideration of those labelled
“ pectoral” in the Atthey collection, one very fine example is
153 inches in length by 2} in diameter at its widest part near
the base; its distal extremity is obliquely truncated or worn
off on the anterior aspect, and the whole spine, when looked
* In a paper on Z)istychius, published in the Ann. & Mag. Nat. Hist.
for September 1883, My. T, Stock states, with regard to Messrs. Hancock
and Atthey’s views as to the pectoral ‘nature of certain Gyracanthus-
spines, that he has “been able to confirm their conclusions by the finding
of an interesting specimen containing well-preserved remains of the
pectoral arch,” and refers to a paper on the subject, read by himself to the
Edinburgh Naturalists’ Field Club. However, on consulting the paper,
now published (Trans. Kdinh. Nat. Field Club, vol. i. pt. 2, pp. 50-61),
it turns out that the ‘“ pectoral arch,” in this case, is Messrs, Hancock
and Atthey’s “ carpal bone,” of which more anon.
Genus Gyracauthus, Agassiz. 39
at from the front, displays a well-marked lateral curvature or
bend, which enables us to distinguish a convex and a concave
side. It will also be observed that the lateral surface is more
gibbous or rounded on the convex aspect of the spine, flatter
on the opposite, so that for purposes of description we may
distinguish the two sides as ‘ gibbous’”’ and ‘ subgibbous ”’ re-
spectively. Still regarding it from the front, it will be seen
that the sculptured surface ends proximally in an acute angle ;
but the apparent middle line on which the tuberculated or
“ ovrating ” ridges meet does not bisect this angle, but divides
it so that the sculptured part is larger on the gibbous side.
Now, turning the spine over so as to look at it from behind,
we observe that the longitudinal cleft or sulcus leading into
the central cavity is not in the middle of the non-sculptured
inserted part, but is placed more towards the subgibbous side,
so that we have here from the very beginning a marked
deviation from bilateral symmetry, one side, the convex or
gibbous one, being larger than the other. We next observe
that, from the distal closure of the sulcus, the lip on its sub-
gibbous side is continued onwards towards the apex as a
blunt keel or margin, having on the gibbous side a shallow
longitudinal depression or groove. Thus the spine has now
become keeled or marginated posteriorly, and from this mar-
gin round to the line of convergence of the gyrating ridges
in front the surface on the subgibbous side is narrower and
flatter, while on the opposite or gibbous aspect it is more ex-
tensive, more rounded, and provided with the aforesaid longi-
tudinal groove. I have already, on a previous occasion*,
ointed out that the groove is obviously equivalent to the pos-
terior flattened area in such median spines as Ctenacanthus, but
here turned awry and looking to one side, while the posterior
marginal ridge represents one of the denticulated margins in the
last-named genus; the other is to be looked for in the opposite
or feebly-marked edge of the groove on the gibbous side in
Gyracanthus. The sculptured or gyrating ridges are on the
whole pretty straight and parallel in their course, though they
show a slight tendency to a sigmoidal direction, curving a
little towards the apex in front, towards the base behind, as
well as increasing progressively in obliquity from the base
onwards. They are closely tuberculated along their whole
extent, and are continued as lines of tubercles over the lips of
the posterior groove, in the bottom of which they converge
and meet. In the above described specimen the groove is
filled with tubercles as far as the spine reaches ; but in others
the groove becomes bare of tubercles at a variable distance
* Geol. Mag. dec, ii, vol. ix. (1882), p. 542.
40 Dr. R. H. Traquair on the
from the closure of the sulcus, and only marked by delicate
longitudinal strie, while in one I find it devoid of tubercles
along its whole extent. In some too, before the truncation of
the apex occurs, the gyrating ridges tend to lose their close
tuberculation, at least posteriorly, and to become only distantly
nodulose or even quite plain.
Putting the wearing of the tips altogether aside as a secon-
dary question, the striking want of bilateral symmetry in
these spines, together with their occurrence in “rights and
lefts,” amply justifies the opinion of Messrs. Kirkby, Atthey,
and Hancock that they were pectoral or at least paired appen-
dages. Which are the right and which the left spines it is,
however, at present not very easy to determine. Accepting
the suleated aspect as posterior, it would be necessary to
ascertain whether the flat or the gibbous side was superior in
order to indicate to which side of the fish it belonged.
Now, turning. to the spines labelled ‘‘ dorsal” in the same
collection, we find that they are smaller in size, varying in
length from 44 to 10} inches, and almost all lying laterally
compressed on pieces of shale. In this way the lateral cur-
vature is obscured, though in one, also marked “ dorsal,”
which happens to be only obliquely placed on its matrix, this
curvature is quite obvious. Furthermore, all of them show
in other respects the same want of lateral symmetry which
I have just described in those acknowledged to be pectoral,
namely the possession of a flat and of an inflated and grooved
side ; in fact they are rendered still more asymmetrical than
the large truncated spines by the much greater prominence
and sharpness of the posterior marginal keel, which we have
seen is morphologically a lateral structure in the general plan
of the spines. This keel is also furnished with a row of small
closely-set recurved denticles. The gyrating ridges become
very oblique towards the point, and tend to become plain or
only distantly nodulose, except perhaps on the front of the
spine. On the flat side a space bare of ridges runs down from
the point along the posterior margin for about 14 inch, and
an analogous appearance is also observable on the grooved
side. The groove itself is smooth and marked with delicate
longitudinal striz ; and, as Messrs. Hancock and Atthey have
already noted, the point is much compressed laterally*.
If we next compare the proximal or basal end of one of the
* These young spines of G. tuberculatus bear an extreme resemblance
to the figure of G. denticulatus, Davis, in Ann. & Mag. Nat. Hist. (5) vi.
1880, p. 373, being similar in shape, in the characters of the gyrating
ridges, and the denticulation of the posterior margin, while the same bare
space runs down fora little distance from the point. Myr. Davis, how-
ever, states that his spine has ¢wo rows of denticles posteriorly.
a
Genus Gyracanthus, Agassiz. 41
largest of these supposed dorsal spines with the distal extre-
mity of one of the least worn of those labelled “ pectoral,” we
find a mutual approximation in character; and, further, if
we compare both with an allied species, G. nobilis, Traq.,
from the Edinburgh district, pretty large specimens of which
sometimes occur with the points very slightly worn indeed,
the whole matter is cleared up. I have now no longer any
doubt that the spmes of Gyracanthus tuberculatus, sup-
posed by Messrs. Hancock and Atthey to be “ dorsal,” are
simply young specimens of the very same spines classed by
them as ‘pectoral,’ and represent the distal portions or
extremities, which in the adult spines have been lost by
attrition. ‘These spines increased by progressive growth at
the base, and as they grew, progressive differences in sculpture,
amount of lateral compression, and so on manifested them-
selves; so that the young spine is not a miniature of the old
one, but represents only a distally situated portion of it,
greater or less as the case may be. And in the case of the
Newsham specimens of Gyracanthus tuberculatus, I ma
mention, as a final and convincing proof, that, although
Messrs. Hancock and Atthey state that in the spines supposed
by them to be dorsal the pointed extremities “ are all perfect,
not being in the least worn,” I find in one so labelled, a speci-
men 11 inches in length, very distinct wearing already in
progress just in front of the tip.
Although Messrs. Hancock and Atthey’s dorsal spines of
Gyracanthus are certainly not so, and although, since my
attention was directed to the subject, I have not been able to
find in any collection, public or private, spines of this genus
to which I could assign a median position, and am conse-
quently inclined to doubt the presence of dorsal spines alto-
gether, Ido not mean to affirm that the subject is thereby
closed. Further investigation is necessary into the Irish
Lower Carboniferous G. obliguus of M‘Coy*, and into two
American species named G. compressust and G, Allenit by
Prof. Newberry, the published figures of which do not indicate
a want of lateral symmetry. M‘Coy gives an outline of the
transverse section of G. obliquus from a position considerably
proximal to the point, in which the two sides with the posterior
area seem as symmetrical as in a Ctenacanthus. In such a
spine it would be well to examine the extreme point. There
is in the collection of the Geological Survey of Scotland a
rather young spine from the Liddesdale beds, which I am
* Paleozoic Fossils, p. 629, pl. iii. &, figs. 13, 14.
t Pal. Ohio, vol. i. p. 330, pl. xxxvii. figs. 1, 2.
t Jb. p. 831, pl. xxxvii. fig. 3.
42 Dr. R. H. Traquair on the
inclined to refer to G. obliqguus, and in it, near the tip, the
transverse section has a form much resembling in general
characters that in M‘Coy’s figure; but one margin of the
groove is nevertheless a little more prominent than the other.
It is to be hoped that American paleichthyologists will care-
fully examine the spines of Gyracanthus occurring in their
country with special reference to the present question.
2. The supposed Carpal Bones of Gyracanthus.
Of constant occurrence in the same beds with G'yracanthus
spines, and often found closely associated with them on the
same slabs of stone, are certain peculiar bones, first noticed by
Messrs. Hancock and Atthey, and by them interpreted as
“carpal”? bones. These occur of two forms or shapes, the
first of which was described by the above-named authors in
1868*. It is a flat triangular bone, with a thick apex oppo-
site to a thin base; and two other sides, one of which, the
longer, is slightly convex, the other, or shorter, being straight
or slightly concave : of the two surfaces one is slightly convex,
the other slightly concave in general contour. Of. these
Messrs. Hancock and Atthey say, “Their structure is very
open; and as they are seldom well preserved, they are pro-
bably only imperfectly ossified; the bony fibre radiates from
the apex to the expanded base. ‘There can be little doubt that
these are carpal bones similar to those in connexion with the
pectoral fins in sharks and dog-fishes.”
The second form is briefly noticed by the same authors in
another communication published four years later, and its form
is described as follows :—‘‘'T'his second form is probably the
inner carpal; it is a broad flat bone irregularly bilobed or
somewhat reniform, with one of the lobes produced and the
external margin straightened ; the convex border is a little
flattened, angulated, and thickened, thence the bony fibres
radiate to the opposite or lobed margin... .. The texture
of the bone is quite similar to that of the large triangular
carpal, namely, it is of a semicartilaginous appearance, with
coarse radiating fibres extending from margin to margin ”’T,
In other passages Messrs. Hancock and Atthey clearly
indicate that they considered the thin margin, in both forms,
to be distal, and the apex, or point from which the “ bony
fibres ” radiate, to be proximal in original position.
Before making any critical remarks on the above determi-
nation of the bones in question, it is necessary to fix accu-
* Ann. & Mag. Nat. Hist. ser. 4, 1868, vol. i. p. 369.
+ Ann. & Mag. Nat. Hist. ser. 4, 1872, vol. ix. pp. 260, 261.
Genus Gyracauthus, Agassiz. 43
rately to what elements of the Selachian skeleton Messrs.
Hancock and Atthey compare them.
The term “carpal” is not used by anatomists of the
modern school to denote any part of the skeleton of the fore
limb in fishes; but on turning to Prof. Owen’s ‘ Compara-
tive Anatomy of the Vertebrata,’ vol. 1. p. 168, fig. 104, we
find the three basal cartilages of the pectoral fin of the picked
dogfish so designated. ‘Two of these, the mesopterygium and
metapterygium of Gegenbaur, are triangular, with their apices
directed towards the shoulder-girdle, while the third or pro-
pterygium has an oblong shape, faintly reminding us of the
second form of so-called carpal of Gyracanthus. There can
thus be no doubt that these basal cartilages, which, in the
skeleton of the recent shark, intervene between the shoulder-
girdle and the radial cartilages, or cartilaginous fin-rays, are
the elements which Messrs. Hancock and Atthey meant by
the term carpal. And the question is simply this, Is it likely
that the process of calcification in such cartilages would give
rise to bodies like the peculiar bones so often -found associ-
ated with the spines of Gyracanthus? Or can any better ex-
planation of their nature be suggested ?
One point in their external configuration was not noticed
by Messrs. Hancock and Atthey, namely, that these bodies
were hollow, and that their extreme flatness is due to the
crushing together of the thin walls of the internal cavity. If
we take first one of the triangular series, it may easily be seen
that the two walls, or laminz of which the bone is composed,
are united at the apex and along the two thick sides which
meet at the apex, but that they are separate at the thin base,
at which accordingly the cavity was open. It may also be
seen that the edges of the basal opening do not coincide, as
careful development of these edges shows that the one on the
convex side of the bone is indented by a large angular notch
or sinus, which runs up for some distance in the direction of
the apex; this appearance I have seen in every case in which
I have looked for it. The internal cavity is at once distin-
guishable, filled with matrix, when a specimen is broken or
cut across. I have equally assured myself of the hollow
character of the bones of the second series.
If we now look at the texture of these bodies we shall be
at a loss to explain the expressions “ imperfectly ossified ”
and “ semicartilaginous,”’ used by Messrs. Hancock and
Atthey, in the passages already quoted. On examining the
surface with a lens its apparent fibrous aspect is seen to be
due to its being closely covered with minute grooves inter-
spersed with small openings, these markings being clearly
44 Dr. R. H. Traquair on the
vascular ins their nature and of the same essential character
as those on the inserted portion of a Selachian spine, only not
so regularly parallel as is usually the case in the latter. On
making microscopic sections, transverse and longitudinal,
through the substance of the supposed “carpal bone,” it is
found to be completely traversed by a close network of
vascular or Haversian canals, the canals in some parts en-
larging so as to give a rather more open character to the
tissue than is found in the internal part of a Gyracanthus-
spine itself, while the ground-substance, hard and calcareous,
is permeated by minute branching and anastomosing tubules,
which are frequently seen to radiate from the vascular canals.
This is not, however, the structure which Selachian cartilage
assumes when calcified or “ ossified’’* ; on the contrary, if
the tissue be not vascular dentine, it is certainly very like it.
I am therefore of opinion, that the bodies in question have
nothing to do with “ carpal bones,”’ or with the endoskeleton
of a shark at all, but that they were, on the other hand,
dermal appendages, which may probably enough have been
situated in the neighbourhood of the pectoral fin, the thin or
open side being proximal and the apex distal. The want of
enamel, or of sculpture on any part of the surface, shows
that they must have been covered with a thin layer of skin.
Their frequent occurrence in close relation to the spines of
Gyracanthus yenders it, indeed, highly probable that they
belong to the same fish.
I hope, on a future occasion, to enter more minutely into
the microscopic structure, both of these bodies, and of the
Gyracanthus-spines themselves.
3. On two new Species of Gyracanthus.
In the ‘ Geological Magazine’ for last month (Nov. 1883)
I have given brief diagnoses of two new species of this genus
from the Carboniferous Limestone series of Scotland, concern-
ing which I propose, in the present communication, to enter a
little more into detail.
Gyracanthus nobilis, Traquair.
Gyracanthus tuberculatus, Traq. Geol. Mag. dec, ii. vol. viii, 1881,
p. 34.
Gyracanthus nobilis, Traq. ibid. dec. ii. vol. x. 1883, p. 542.
The spines which I have named Gyracanthus nobilis are of
* For an account of the structure of calcified Selachian cartilage, see
Williamson on the “Structure and Development of the Scales and Bones
of Fishes,” Phil. Trans. 1851.
Genus Gyracanthus, Agassiz. 45
common occurrence in the ironstone worked at Borough Lee,
near Edinburgh, belonging to the Middle Carboniferous Lime-
stone series of Central Scotland; and I have also seen a frag-
ment from a similar horizon at Cowdenbeath, in Fifeshire. At
first I confounded them with G. tuberculatus, Ag., but the
accession of more extensive material, along with a closer in-
vestigation of the subject, soon convinced me of their specific
distinctness.
Gyracanthus nobilis attains a large size. One spine in my
own collection, wanting a small portion of the base, but having
its extreme point preserved, measures 21 inches ; had it been
entire its length could not have been less than 2 feet. Another,
wanting the point, must have been about the same size; and
fragments are not uncommon which indicate still greater
dimensions. The general form is elongated and slender, the
breadth increasing more rapidly towards the base in adult
specimens. ‘Théy are very variable in respect of curvature :
in some both antero-posterior and lateral curves are well
marked ; in others the lateral bend is only slight or hardly
perceptible ; and I have one which appears almost perfectly
straight in both directions. Every one of them, without ex-
ception, is nevertheless asymmetrical as regards those special
points of configuration upon which I have dwelt in connexion
with G. tuberculatus, and, as in that species, they may be
arranged in pairs.
In the form of the non-sculptured inserted part, with its pos-
terior sulcus, and in the general configuration of the spine as
seen in transverse sections, G. nobilis closely resembles CG.
tuberculatus. The posterior marginal keel is in its distal
portion strongly denticulated ; in one specimen the denticles
may be traced, from the point, a distance of 10 inches in the
direction of the base. ‘The posterior groove varies much in
its degree of sharpness ; in some it is very shallow and slightly
marked till towards the point, while in others it is very well
defined along its whole extent. In adult specimens continu-
ations of the gyrating ridges usually encroach upon it at its
commencement; but the salient point in this species lies in
the disposition and mode of tuberculation of these ridges.
At the proximal end of the spine, in adult examples, they
are disposed much as in G. tuberculatus, meet each other
anteriorly at much the same angle, and are closely tubercu-
lated along their whole extent. But near the closure of the
sulcus this close tuberculation becomes limited to the anterior
aspect, each ridge as it arises and advances forward showing
first a comparatively distant tuberculation, then a smooth
space (sometimes very minutely crenulated) on the side of the
46 Dr. R. H. Traquair on the
spine, and finally becoming thick and coarsely tuberculated
as it turns round to the front. Where this feature of the
ridges commences they also become excessively oblique and very
delicate, and in some specimens they also occasionally bifur-
cate along the sides of the spine; but in front, where the
tuberculation appears, they become coarse and curve a little
JSorward, so as to become less oblique, and in many cases they
turn slightly again towards the point just before meeting those
of the opposite side. ‘Towards the extremity the ridges become
entirely smooth on the sides of the spine, their slight curva-
ture also ceases, and the tuberculation of the anterior aspect
gives way to simple undulation. ‘The point, even where it is
not positively truncated by attrition, looks smooth and
rubbed.
Gyracanthus nobilis may easily be distinguished from both
G. formosus and G. tuberculatus (probably only varieties of one
common species) by the direction of the gyrating ridges. In
the latter forms these ridges are disposed in a pretty straight
and parallel fashion over the sides of the spine, although they
do increase in obliquity towards the apex. Here, however,
their excessive obliquity and delicacy along the sides, after the
closure of the sulcus, give the sculpture a peculiar aspect
which cannot be mistaken. The tuberculation of the ridges
is in general coarser than in G. tuberculatus, and, in the
latter, it is only pretty well towards the apex that the ridges
tend proximately to become plain, or only distantly nodulose.
Of course, as regards the disposition of tuberculation, this new
species differs still more from G. formosus, in which the ridges,
from the very base, tend to be plain in front.
Adult specimens of G, tuberculatus show invariably, so far
as I have observed, a strongly-marked lateral curvature ; in
G. nobilis, as we have seen, its presence and amount is very
variable.
The course of the ridges, the disposition of the tubercula-
tion, and the form of the transverse section equally distinguish
it from G. obliquus of M‘Coy, and it is certainly not G. den-
ticulatus of Davis. Nor can it be shown to be identifiable
with any of the North-American species named by Prof.
Newberry and Dr. Dawson.
There only remains the G. alnwicensis of Agassiz, which
is recorded trom a somewhat similar horizon, viz. the Car-
boniferous Limestone series of Alnwick, in Northumberland.
This is very briefly mentioned by Agassiz as being slender in
form, with very oblique and entirely smooth or non-tubereu-
lated ridges, which ridges also bifurcate, and even trifureate,
in a very remarkable manner, as shown in the figure. If this,
Genus Gyracanthus, Agassiz. 47
description is correct *, G. nobilis is even more distinct from
G. alnwicensis than from any other.
One remarkable feature in these spines as occurring at
Borough Lee is the small amount of apical wearing to which
they have for the most part been subjected. Hven the extreme
point, only a little blunted and polished, is sometimes present
in large specimens, and in many others comparatively little of
the extremity has been lost by that process which has reduced
some of the large Gyracanthus-spines from Northumberland
and Staffordshire to mere stumps. It has been noted that
this wearing process has obliquely truncated the Northumbrian
specimens in their anterior aspect ; but in those from Borough
Lee evidence of wearing is sometimes found on the posterior
aspect as well. These circumstances would lead us to infer
some difference either in the habitat or the habits of the species
in question.
Gyracanthus Youngit, Traq.
Gyracanthus Youngit, Traq. Geol. Mag. dee. ii, vol. x. 1885, p, 543.
Occurring also at Borough Lee, but found likewise in many
other localities on the horizon of the Scottish ‘ Edge”? Coal
or Middle Carboniferous Limestone series, is a remarkably
distinct species of Gyracanthus, to which T have given the
name C. Youngii, in honour of my friend Mr. John Young,
of the Hunterian Museum, Glasgow, who has done so much
for the elucidation of the paleontology of the west of Scotland.
The finest specimens I have seen are in the collection of Mr.
R. Craig, Beith, Ayrshire, and are from the shale overlying
the Clay-band Ironstone at Barkip, Dalry. I have also seen
specimens from Bo’ness in Linlithgowshire (collection of
Mr. H. M. Cadell), Possil in Lanarkshire (collection of Mr.
John Young), Cowdenbeath in Fife, and Maryhill near
Glasgow.
These are large spines, some of ‘which must have attained
a length of over 2 feet, had not their apices been worn off.
They always show some amount of lateral curvature ; but the
degree to which they are antero-posteriorly bent is very
* Possibly it is not, as Agassiz never saw the specimen, but drew up
his description from a drawing sent to him by Messrs. Buckland and De
la Beche. As reproduced in the plate in the ‘ Poissons fossiles,’ this
drawing looks like a very hurriedly executed pen-and-ink sketch, from
which it is quite impossible to identify any thing. Under these cireum-
stances doubt whether the term “ alzwicensis” has any more value than
a mere manuscript name.
48 On the Genus Gyracanthus, Agassiz.
variable; some are indeed in that direction nearly quite
straight.
The first salient point which strikes the eye is the great
size of the inserted or non-sculptured portion, which is not
only broader and more expanded, but extends further beyond
the sculptured part proximally than in any other species. ‘The
anterior middle line on which the gyrating ridges meet does
not cut equally the very acute angle formed proximally by
the sculptured part; but in this case the larger division is
found on the subgibbous side, this being due to the encroach-
ment of the non-sculptured part on the gibbous side. It is
next to be noticed that the shaft of the spine after the closure
of the sulcus is more cylindrical than in other species; still
the want of bilateral symmetry is very obvious, and a gibbous
and subgibbous side may be distinguished. ‘The posterior
groove is sometimes not apparent for some distance after the
closure of the sulcus, or, though indicated, it may be filled
with tubercles ; sooner or later it becomes well marked, and
the lip on the subgibbous side becomes more prominent than
the other, but does not form so marked a feature in the con-
figuration of the spine as the corresponding posterior marginal
keel in such species as G. tuberculatus and nobilis ; it is in fact
only towards the extremity, that the spine takes on a keeled
appearance. A well-marked row of recurved denticles occurs
along the aforesaid lip or ridge of the posterior groove on the
subgibbous side, and on that of the opposite side denticles are
also seen in some examples. ‘The last remarkable feature in
this species is the slight obliquity of the gyrating ridges, which
meet each other on the front of the spine at angles greater
than right angles almost as far as the very apex. These
ridges are also rather less oblique on the subgibbous than on
the gibbous side ; on the former they are in fact sometimes
nearly transverse; a certain amount of sigmoidal curvature
is assumed after the middle of the spine, the anterior extre-
mities of the ridge turning slightly towards the apex, their
posterior extremities towards the base. Only towards the apex
have the ridges any marked obliquity in their middle portions,
and there they often also become wavy. ‘The gyrating ridges
are closely tuberculated over their whole extent, except to-
wards the apex, where the tuberculation tends to become
irregular. ‘The amount of apical wearing is very variable.
On the Polyzoa of Queen Charlotte Islands. | 49
V.—Report on the Polyzoa of the Queen Charlotte Islands.
By the Rev. Tuomas Hincxs, B.A., F.R.S.
[Continued from vol. xi. p. 451.]
[Plates III. & IV.]
~ LEPRALIA (part.), Johnston.
Lepralia bilabiata, n. sp. (Pl. ILL. fig. 1.)
Zoecia quincuncially arranged, short, very slightly convex,
the sutures little more than incised lines, rounded above
(where the cell-wall forms a distinct border round the orifice),
widening out at each side, and narrowing off towards the
base, which is subtruncate or pointed; surface dense, smooth,
of a somewhat waxy appearance and a dark brown colour;
orifice large, occupying nearly half of the front surface, rounded
above, slightly contracted a short distance above the lower
margin, which is arched outwards; peristome unarmed, not
elevated; operculum smooth, of a deep black colour, with a
slight rim round the edge, the inner surface attached to a bi-
labiate tubular passage (Pl. IIL. fig. 1), through which the
polypide issues. Avicularia none. Ocwcium a subtriangular
extension of -the cell above the orifice, very little raised, a
great part of its front surface occupied by a large foramen,
closed in by membrano-chitinous material (Pl. ILI. fig. 1 a).
Zoarium of a very dark brown colour (almost black).
Houston-Stewart Channel, on shells.
When the zocecium is open, the orifice is occupied in great
part by the entrance to a tubular passage, through which the
polypide issues; this entrance is bilabiate, the lower lip con-
sisting of a semicircular chitinous rim, as it were soldered
to the inner surface of the operculum ; the upper or opposed
lip, also chitinous, is movable, and closes upon the opercular
lip when the polypide retreats.
The structure of the ovicell in this species is peculiar; it
consists of a short extension of the cell upwards, the front
wall of which is much depressed, and bears a large foramen,
with a chitinous lid or covering. The ocecial chamber is
small, and the entrance to it is closed by the operculum of
the cell. This is a very distinct modification of the ordinary
form of ocecium. i
L. bilabiata is luxuriant in growth, and forms very large
spreading crusts.
Ann. & Mag. N. Hist. Ser. 5, Vol, xiii. 4
BO... Rev. T'. Hincks on the
Lepralia claviculata, n. sp. (PI. III. fig. 2.)
Zoecia ovate or lozenge-shaped (sometimes irregular in
shape and size), regularly quincuncial, depressed; surface
glossy, thickly covered with minute circular punctures, which
give it a pretty speckled appearance ; orifice arched and ex-
panded above, more or less narrowed downwards, contracted
by a small acute projection on each side just above the lower
margin, which is distinctly curved; peristome not raised.
Avicularia keyhole-shaped, placed on a distinct area, very
much smaller than that of the cell, sometimes immediately
above a zoceclum, more commonly in the angle between two
zocecia ; mandible directed upwards. Occium (fig. 2 a) very
large, higher than broad, depressed towards the opening, and
often grooved longitudinally above the oral arch, rising above
into a kind of central knob (but on the whole not much ele-
vated), white, glossy, thickly punctured.
Zoarium forming large, spreading, whitish crusts.
Houston-Stewart Channel; Cumshewa, 20 fms.
Cases occur in which the avicularium is situated on an area
almost as large as that of the cells, just below the upper
extremity, occupying, in fact, the position of the oral aperture.
Occasionally two of these appendages occur together, either
placed one above the other or side by side.
PoRELLA, Gray.
Porella concinna, Busk.
Cumshewa, on shell.
[ Britain, Adriatic, Finmark, Norway, Spitzbergen, Franz-
Josef Land (fdley), Greenland, Gulf of St. Lawrence,
Bass’s Straits. |
A beautiful variety occurs in which the whole surface of
the cell, except the umbo below the orifice, is covered with
rather large punctures; the orifice is ample, and its characteristic
features are very distinctly marked. The zoarium is white,
and delicate in texture.
Porella marsupium, MacGillivray, form porifera.
(PI. IV. fig. 4.)
This species, which is a common Australian form, occurs
abundantly amongst the dredgings. The specimens from the
Queen Charlotte Islands differ from those which I have exa-
mined from Bass’s Straits in one or two points, but they are
quite unimportant. On the front of the suboral swellin
which supports the avicularium, are two (or occasionally three)
Polyzoa of Queen Charlotte Islands. 51
rather large circular pores, placed side by side. They give
a somewhat peculiar appearance to the cell, but do not seem to
have any special significance. Frequently too there is a
small raised oval avicularium on the front of the cell, besides
the oral avicularium, which I have not noticed on Australian
specimens. ‘The cell-wall is smooth and entire ; the ocecium
is traversed by delicate radiating lines.
Extremely common, on shells &c.
[Victoria (MacGillivray) ; Bass’s Straits (Capt. Cawne
Warren).|
The species described by Mr. Ridley from the Straits of
Magellan (Proc. Zool. Soc. Jan. 4, 1881) as Schi'zoporella
marsupium, and identified by him with MacGillivray’s Le-
pralia marsupium, is, I have no doubt, the Hscharina simplex
of D’Orbigny (‘ Voyage dans Amérique Mérid.’), obtained
from “les Iles Malouines.” MacGillivray, who has found this
species in Victoria, has named it Schizoporella Ridleyi (Proc.
Roy. Soc. Victoria, Oct. 12, 1882).
We have no alternative, however, but to revert to the earlier
designation, and it must stand as Schizoporella simplex,
D’Orb.
Porella major, n. sp. (PI. IV. fig. 5.)
Zoecia ovate or (sometimes) hexagonal, somewhat elongate,
quincuncial, rather depressed, sutures shallow, often with a
line of punctures round the margin; surface smooth or slightly
roughened, glossy ; orifice arched above, lower margin curved
inwards, so as almost to appear dentate ; peristome thin, un-
armed, elevated (in the adult cell), especially above, immedi-
ately below the orifice a narrow avicularian swelling, stretching
across the front of the cell and bearing in the centre a small
oval avicularium, mandible directed downwards. Oactum
rounded, moderately prominent, surface minutely roughened,
the peristome forming a raised rim round the oral arch.
Zoarium of a very light brownish colour.
Cumshewa ; Houston-Stewart Channel, common on shells.
SmirtiA, Hincks.
Smittia trispinosa, Johnston.
Houston-Stewart Channel; off Cumshewa; Virago Sound :
abundant. J
[Britain, Norway, Arctic regions, St. Lawrence, Mingan
Islands, Florida, Mazatlan, Cape Horn, Aden, Adriatic,
East Indies (Dr. Anderson), Bass’s Straits.]
Several varieties occur. As a rule, the avicularian appen-
dages are present in great profusion and of unusual size.
4#
52 Rev. T’. Hincks on the
Smittia plicata, Smitt.
Houston-Stewart Channel ; off Cumshewa, 20 fms. : not un-
common.
[Spitzbergen, Greenland, 100 fms., Godhavn Harbour,
Disco.
The form which I refer to Smitt’s Cellepora plicata differs
slightly from the description and figures given by that author ;
but in essential particulars, I believe, it agrees with them.
In the specimens from the Queen Charlotte Islands the avicu-
larium is well within the peristome, and there is little if any
trace of the umbo, on which, according to Smitt, it is placed
in his OC. plicata. This, however, may be due to the greater
development of the peristome, by which the umbo may have
been to a large extent concealed. The cells are often in-
vested by a membranous epitheca.
Smittia spathulifera, n. sp. (Pl. IV. fig. 3.)
Zoecia large, ovate, quincuncially arranged, very mode-
rately convex, bordered by delicate raised lines; surface
covered with rather large round punctures, which, however,
are in great measure concealed by the stout epitheca that
clothes the zoarium; orifice arched above, lower margin
straight and within it a large bifid tooth; peristome much
raised (especially above) forming an elongate secondary orifice,
produced below into a spout-like sinus, which is occupied by
a spatulate aviculartum; mandible directed downwards.
Ocecium large, immersed, closely united to the cell above ;
surface roughened, punctured round the edge. Zoarium
forming a brownish crust.
Houston-Stewart Channel.
Muvcrone.ia, Hincks.
Mucronella ventricosa, Hassall.
Virago Sound, in about 20 fms., on shells.
[Britain, France (S.W.), Mediterranean, New Zealand,
Bergen, Greenland, Nova Zembla, Kara Sea. ]
Mucronella pavonella, Alder.
Virago Sound. ;
[St. Lawrence, Greenland, Nova Zembla, Spitzbergen, Fin-
mark, off Jutland, Britain (north-east) .]
Mucronella prelucida, n. sp. (Pl. IV. fig. 1.)
Zeocia large, ovate, quincuncial, slightly convex, separated
Polyzoa of Queen Charlotte Islands. 53
by raised lines; surface thickly covered with roundish pune-
tures, lustrous; orifice arched above, lower margin straight
(without denticles), peristome raised, especially at the back
and in front, where it rises in the centre into a blunt mucronate
projection, which bends slightly inwards; the surface of the
peristome smooth, entire, and very glossy. Avicularia
none. Occium (?).
Houston-Stewart Channel, not uncommon on shells.
Mucronella prelonga,n. sp. (PI. IV. fig. 2.)
Zoecia long and (usually) slender, quincuncially disposed,
somewhat wider above than at the base (elongate-ovate, some-
times appearing almost subtubular), convex, depressed below,
rising towards the oral extremity; surface thickly covered
with minute punctures, shining (the glistening appearance
due to the presence of an epitheca) ; orifice suborbicular, peri-
stome elevated round it, carried out in front into a very pro-
minent process, often much thrown back and greatly elon-
gated, sometimes simply pointed, sometimes bi- or trimucro-
nate, on the inner side of it near the base a single, small,
sharply-pointed denticle ; the upper margin produced in the
centre into a tall spinous process, broad at the base, attenu-
ated and membrano-calcareous above. Avicularia none.
Oecium (?). Zoarium forming a whitish subcircular crust.
Houston-Stewart Channel, on shell.
A very picturesque form, distinguished by the remarkable
processes on the upper and inferior margins of the peristome.
The mucro in front is sometimes very greatly elongated, and,
in such cases, the upper portion seems to be formed of very
delicate membrano-calcareous material. ‘The spinous exten-
sion of the peristome on the upper margin, which is much
attenuated above, is also made up, to a great extent, of similar
material. The subtubular character of the zocecia is a striking
feature, though occasionally, and especially near the growing
edge of the colony, they assume a more distinctly ovate form.
Mucronella spinosissima, Hincks, form major.
(Pl. IIL. fig. 3.)
Zoecia broad-ovate, short, arranged in quincunx, very
convex, sutures deep, surface smooth, subhyaline in the
younger cells, opake in the older, a number of slender tubules
immersed in the cell-wall immediately beneath the surface,
and radiating from the margin towards the centre, the
aperture opening out apparently on the surface, but closed ie
a calcareous diaphragm ; the oral extremity of the cell muc
54 Rev. T. Hincks on the
raised, contracted, suberect, forming a neck which bears the
orifice ; orifice suborbicular, a small mucronate projection in
the centre of the lower margin, the rest of the peristome occu-
pied by 6-10 tubular spinous processes, a denticle within the
peristome on the lower primary margin. Avicularia none.
Owcium (fig. 36) rounded, developed behind the neck-like peri-
stome (the orifice, with its full armature of spines, rising before
it), sometimes traversed by a number of the immersed tubules.
Primary cell (fig. 3 a) small, ovate; aperture occupying about
two thirds of the front surface, surrounded by a raised border,
which bears about 8-10 spines; the orifice nearly semicircular,
occupying the upper portion of the aperture, the lower part
closed in by a delicate membrano-calcareous covering; por-
tion of the cell below the aperture smooth and solid.
Zoartum forming very large cream-coloured crusts on shells.
Extremely abundant; probably the commonest species
amongst Dr. Dawson’s dredgings.
[Bass’s Straits (Capt. Cawne Warren).]
I have ranked this interesting form as a variety of MW.
spinosissima, a species which I have described and figured in
my report on the Polyzoa of Bass’s Straits (‘ Annals ’ for Aug.
1881). In all the principal elements of structure there is an
exact correspondence between the two; but there are also one or
two differences, which materially affect the general appearance,
and, at the first glance, few probably would be likely to iden-
tify them. In the present variety the cells are very much
larger than those of the Australianform. The latter are small
and delicate, while those of the variety major are ample,
broadly ovate, massive, and strongly built. But the chief
difference between them lies in the system of tubules, more
or less immersed in the cell-wall and showing as white striz
on the glossy surface, which gives so distinctive a character
to the North-Pacific form. Of this tubular structure I have
been unable to detect any trace in the Australian specimens
which I have examined. Possibly the condition of the stony
crust may be such as to conceal it; but this hardly seems
probable, as in the finest colony which has come under my
notice calcification has evidently not proceeded far. It may
also be noted that the cells of the Australian variety have a
well-marked row of punctures round the margin.
At present, looking to the close structural agreement be-
tween the two forms, and in the absence of any precise know-
ledge as to the development and function of the tubules, I
prefer to include them in one specific group.
The tubules appear as delicate white lines through the
subhyaline crust, radiating from the circumference towards
Polyzoa of Queen Charlotte Islands. 55
the centre of the zocecium. They vary much in length, some
being almost rudimentary, and others extending nearly or
quite to the centre of the cell. Not unfrequently short tubes
alternate with the longer ones; and commonly the latter seem
to be composed of several short tubules, which originate one
from the other, a little below and behind the orifice. In the
younger zocecia the tubules are, I believe, on the surface; but
they are soon overgrown by the calcareous crust, and in older
states they are completely concealed by it. In highly calci-
fied colonies this feature disappears, and the cells present a
uniform opake surface. The tubules traverse the neck-like
portion of the cell, and the numerous oral spines seem to be
nothing more or less than their free extremities projecting be-
yond the margin of the peristome.
It is difficult to form a conjecture as to the precise import
of the tubular system, and the more so as there has been no
opportunity thus far of tracing the growth of the cell-wall and
the mode in which the tubules originate.
The primary cell of Mucronella spinosissima closely resembles
that of M. Peachit.
RetTepora, Imperato.
Rtetepora Wallichiana, Hincks.
Houston-Stewart Channel, 15-20 fms.
[Spitzbergen, 20-80 fms., Finmark, Godhaab, 150 fms. ]
This form was first described by Smitt * as a variety of R.
notopachys, Busk, a Crag fossil. Some years later the exa-
mination of specimens obtained by Dr. Wallich in Davis
Straits convinced me that it was a distinct species, and it was
accordingly described as such (‘ Annals’ for Jan. 1877,
p. 107), with the name which Mr. Busk had already assigned
to it in MS.
R. Wallichiana, when fully developed, forms intricate
convoluted and chambered masses of considerable size. It is
one of the many arctic species which have migrated to the
Queen Charlotte Islands.
Family Celleporide.
CELLEPORA (part.), Fabricius.
Cellepora incrassata, Lamarck.
Houston-Stewart Channel; Virago Sound, incrusting the
stems of Hydrozoa.
* “Kritisk forteckn, Ofver Skandinavien’s Hafs-Bryozoer,” Q#fvers.
Kongl. Vetensk. Akad, Forhandl. 1867, Bihang.
56 Rev. T. Hincks on the
Finmark, Spitzbergen, Greenland, Banks of Newfound-
fend. » &P gen, ?
and. ]-
Cellepora, ? sp.
Zoartum inecrusting, of a rather dark browncolour. Zowcia
(towards the centre of the colony) erect, crowded, barrel-
shaped, some elevated, some immersed ; surface smooth, more .
or less punctured round the margin; orifice arched above,
lower margin slightly curved outwards (suborbicular), and
having in the centre a small notch, rounded below and con-
tracted at the opening by two minute denticular projections ;
operculum arched above, straight and entire below; peristome
raised in front, embracing a short and stout rostrum, placed
immediately below the oral notch, and bearing an avicula-
rium on one side close to the top, with rounded mandible
directed upwards ; two very tall articulated marginal spines,
placed one on each side of the orifice above. Large avicularia
scattered amongst the cells with a broad subspatulate man-
dible, the beak elevated at the extremity into a hood-like
projection, not denticulate. Occium (?).
Incrusting Retepora and shells.
I cannot identify this form with any of the described species
known to me; but I am by no means prepared at present to
say that it is new to science. It does not appear (so far as I
can judge in the absence of the figures) to be included amongst
the ‘Challenger’ Cellepore characterized by Busk (Journ.
Linn. Soc. vol. xv. 1881, p. 841, &e.). If it should prove to
be (as I suspect) undescribed, I should propose for it the name
of Cellepora brunnea.
ADDITIONAL.
Family Porinide.
LaGenipora, Hincks.
This genus, as originally constituted *, was formed for a
Porinidan species in which the cells are more or less im-
mersed in a calcareous crust. But I am now convinced that
this character cannot properly be made the foundation of a
generic group, and I propose to apply the name to such forms
as possess a lageniform cell with a free orbicular orifice and
are destitute of a special pore. The original type of the genus,
L. socialis mihi, will hold a place in the reconstituted group,
* ¢ Annals’ for September 1877 ; ‘ Hist. Brit. Marine Polyzoa,’ vol. i.
p. 236.
—$$ $$$ ————————_—~
ri
Polyzoa of Queen Charlotte Islands. 57
along with Phylactella lucida mihi, a Madeiran species (see
‘Annals’ for July 1880), and a kindred form from the Queen
Charlotte Islands, which I shall now describe.
Lagenipora spinulosa, n. sp. (Pl. III. fig. 4.)
Zowcia lageniform, rather irregularly disposed, the lower
portion adherent, ovate, thickly covered with punctures (some-
times almost obliterated, when the surface appears roughened
or subgranulous) ; the oral extremity free, tubular, much pro-
duced, suberect, the surface perfectly smooth and subhyaline,
slightly expanded upwards ; orifice terminal, suborbicular, the
front margin plain or trimucronate, and more or less elevated
above the rest, somewhat everted, on each side a raised process
bearing a small avicularium of the Scrupocellaria type, with
minute pointed mandible directed outwards, on the upper (or
hinder) margin several spinous processes. Occium small,
rounded, smooth, placed far down at the back of the tubular
portion of the cell.
Zoartum forming small lobate patches.
On Tubulipora (especially) and shells ; not uncommon.
This form is nearly related to Z. lucida, mihi, but is, I have
no doubt, distinct. ‘There is a marked difference between the
avicularia of the two species. In JZ. spinulosa there are
two, one on each side of the orifice, resembling very closely
the form which is characteristic of the genus Scrupocellaria.
In L. lucida there is only a single minute, oval avicularium,
which is borne on a stout process, in the centre of the lower
margin. JL. spinulosa is altogether stouter in habit than the
Madeiran species, and in the normal state the adherent portion
of the cell is thickly punctured, whereas it is entire and smooth
and subhyaline in the latter. It differs from Z. lucida in
another point. On each side of the free tubular portion of the
cell there is a very distinct line, running the whole length of
it, which seems'to mark the junction between the front piece
and the rest of the tube. The strongly marked groove at the
base of the neck-like extension in L. /ucida is wanting in the
present form, which is also characterized by a peculiar habit
of growth. ‘
Microporella Malusi’, Audouin.
A variety of this species occurs, in which there is a very
prominent umbo below the pore.
Schizoporella biaperta, Michelin.
In a variety of this widely distributed species from the
58 Mr. A. G. Butler on Lepidoptera from
Queen Charlotte Islands the lateral avicularia have a pointed
mandible instead of the normal rounded one. Smitt has
noticed the same thing in Floridan specimens.
EXPLANATION OF THE PLATES.
Puate III.
Fig. 1, Lepralia bilabiata, n. sp. 1a. A zocecium with ovicell. 10. Zocs-
cium with the operculum thrown back, showing the entrance to
the tubular passage.
Fig. 2. Lepralia claviculata, n. sp. 2. a. Ocecium.
Fig. 3. Mucronella spinosissima, Hincks, form major; group of cells,
showing the tubules in the front wall. 3a. Primary cell. 36.
Zocecium, showing the position of the ovicell behind the tubular
orifice.
Fig. 4. Lagenipora spinulosa, n. sp.
Puate lV.
1. Mucronella prelucida, n. sp.
2. Mucronella prelonga, n. sp.
Fig. 3. Smittia spathulifera, u. sp.
4, Porella marsunm, MacGillivray, form porifera.
5. Porella major, n. sp.
VI.—Lepidoptera from the Island of Nias.
By Arruur G. Butter, F.L.S., F.Z.8., &e.
THE following species from the Island of Nias have recently
been added to the collection of the British Museum :—
HurLainz.
Caduga funeralis, sp. n.
Nearly ailied to C. Banksii, Moore (frorfi Sumatra), but
differing much as Purantica eryx does from P. agleoides, the
wings being of a narrower and more elegant form, with the
whole of the greenish-white markings much narrower; the
abdomen a little browner. Expanse of wings 86 millim.
Salatura eurydice, sp. n.
Primaries above most like S. nubila of Gilolo, but the
reddish area of the primaries of a lurid mahogany-red colour,
more restricted, divided into three well-marked areoles by the
median vein and its first branch, which are very broadly
black-bordered, and bounded on costa and inner margin by
the Island of Nias. 59
broad black borders; the white spots on the black apical area
also differ a little, the fifth in the subapical series being longer
and wider, so that it becomes the largest of the series; below
this series are two moderate-sized spots, as in S. nubila, and
below the inner one (within the first median interspace) is a
slightly larger spot; below the outer one and in the same
interspace with it is a white dot, there are also four white
submarginal dots, one at apex and three near the centre of
outer margin; the secondaries are quite unlike those of 8.
nubila and allies, being of a smoky-brown colour, with white-
spotted fringe, with nine white dots in a double series towards
anal angle, and two placed obliquely near apex; these wings
are therefore most like those of S. ferruginea. LExpanse of
wings 81 millim.
AT.
NYMPHALINZ.
Doleschallia niasica, sp. n.
9. Nearest to D. pratipa; primaries with the basal two
fifths and inner border smoky fulvous, the apex and external
border broadly black, and the intermediate area creamy white ;
a transverse black patch at the end of the cell, and three un-
equal decreasing white dots placed obliquely near apex ; se-
condaries smoky fulvous, the costal area broadly smoky grey ;
two slightly undulated blackish submarginal stripes and the
two usual black spots on the disk ; abdominal border whitish
towards the base ; body dark olivaceous. Under surface with
the pattern of D. pratipa, but the wings altogether paler than
in any specimens known to me of that species. Expanse of
wings 72 millim.
Symphedra perdix, sp. n.
@. Allied to S. wetes of Menado, Celebes; blackish
piceous, with white and tawny spots, arranged much as in
S. dirtea, though differing in colour; the chief differences
between the two females are as follows:—In S. perdizv the
two series of spots which cross the disk are considerably
larger, those on the median interspaces being also confluent,
so as to produce (with those which are confluent in S. e@etes 2
of Hewitson) a broad white angular belt, interrupted by
black nervures, and throwing off three decreasing white spots
from its angle to the costa; the submarginal spots are more
regular, larger towards external angle, where they are
whitish, but decreasing to a mere point towards apex ; the
two series of spots across the basal half of secondaries are
60 On Lepidoptera from the Island of Nias.
larger and paler towards costa, the inner series terminating in
a white subcostal spot; a second white subcostal spot is placed
nearer to the base at the extremity of a fulvous stripe which
borders the basal portion of the subcostal vein and its first
branch ; the tawny borders of the ocelloid discal series of spots
are more isolated, the inner series less lunate; the body is
black above, the autenne tipped with fulvous, the thorax with
two spots of ochreous behind the collar; two lateral white
spots in the middle and two behind; the abdomen is spotted
in front and narrowly banded behind with ochreous. The
coloration and general pattern below are most like those of
S. dirtea of Java, but differ im the decidedly more tawny
ground-tint, excepting towards the abdominal border of
secondaries (the area around which is, as usual, pale bluish),
in the broad white belt on the disk of primaries, and the black
edges of the discoidal and supradiscoidal spots of secondaries.
Expanse of wings 102 millim.
This is one of the most handsome species in the genus; it
approaches nearest to two females in Hewitson’s collection
regarded as my S. canescens, but decidedly larger than the
type of that species ; the latter, however, may vary, though
certainly not sufficiently to include the Macassar female asso-
ciated with it by Hewitson, and which is nothing more than
the more prevalent variety of the insect described by Hewit-
son as the female of his 8. wetes of Menado.
The true female of S. wetes is in Hewitson’s collection from
Tondano ; and, excepting that it is larger, differs in no respect
from the male. ‘The female of the Macassar species, however,
is larger still, and has the general character of markings of S,
dirtea, excepting that the spots of the discal series, including
the spots of the inner series of the furca, are larger, and thus
form an angular band broken up into well-separated spots
below the median vein, but only interrupted by the black
nervures above it; the entire furca is occasionally composed
of white spots, as in the type of Hewitson’s description. The
male differs chiefly from that sex of S. wetes in the larger
white spots of the inner series of the furea on the primaries
and in the narrow inner border of the ocelloid spots on the
secondaries, so that there is no well-defined grey band across
these wings as in S. eetes. I propose that this species should
take the name of S. phasiana: so far as I know it occurs only
at Macassar, the pair in our collection being taken in that
locality, as well as one of Hewitson’s females; a pair in his
collection, however, is only labelled ‘‘ Celebes,” but was pro-
bably obtained from the same source as our examples. .
Te,
Geological Society. 61
PROCEEDINGS OF LEARNED SOCIETIES.
GEOLOGICAL SOCIETY.
November 21, 1883.—J. W. Hulke, Esq., F.R.S.,
President, in the Chair.
The following communications were read :—
1, “ On the Skull and Dentition of a Triassic Mammal (7’ritylodon
longevus, Ow.) from South Africa.” By Prof. Owen, C.B., F.R.S.,
F.G.S.
The specimen described in this paper formed part of a collection con-
taining remains of some of the known South-African Triassic Reptilian
genera, and agreed with them in its mode of fossilization. It was
submitted to the author by Dr. Exton, of Bloemfontein. The spe-
cimen is a nearly entire skull, wanting only the hinder part, and it
measures about 3? inches in length, from the broken end of the
parietal crest to the point of the united premaxillaries. The upper
surface shows the anchylosed calvarial portions of the parietals,
and the frontal bones divided by a suture ; the contiguous angles of
these four bones are cut off, so as to leave an aperture, occupied by
matrix, which may be a fontanelle, or a pineal or parietal foramen.
The frontals form the upper borders of the orbits, which are bounded
in front by the lacrymal and malar bones, and were not completed
behind by bone. ach frontal is narrowed to a point at the
suture between the nasal and maxillary. The nasals are narrow,
but widen in front to form the upper border of the exterior nostril,
which is terminal, and is completed by the premaxillaries. The
maxillaries are widened posteriorly, then constricted, and again
widened before their junction with the intermaxillaries.
The teeth include a pair of large round incisors, broken off close
to the sockets, and showing a large pulp-cavity, surrounded by
a complete ring of dentine, which is covered by a thin coat of
enamel on the front and sides. At 2 millim. behind each of these teeth
is the socket of a smaller premaxillary tooth; this tooth apparently
had a thin wall and a pulp-cavity relatively larger than in the
anterior tooth. It is separated by a ridged diastema from the
series of six molar teeth on each side, the first of which has a sub-
triangular crown with the base applied to the second tooth. The
latter and the four following teeth are nearly similar, subquadrate
in form, with the crowns “impressed by a pair of antero-posterior
grooves, dividing the grinding-surface into three similarly disposed
ridges, and each ridge is subdivided by cross notches into tubercles.
Of these there are, in the second to the fourth molar inclusive, four
tubercles on the mid ridge, three on the inner ridge, and two on the
outer ridge.”
The author discussed the relations of this new form of mammal,
62 Geological Society.
especially as indicated by the structure of the teeth, which he
showed to resemble those of Microlestes, from the Keuper of Wiirt-
temberg and the Rheetic of Somersetshire, and those of the Oolitic
genus Stereognathus, the former having on each tooth two multitu-
berculate ridges, and the latter three ridges, but with only two
tubercles on each. ‘The fossil presents no characters to show
definitely whether the animal it represents was a placental or a non-
placental mammal.
2. “ Cranial and Vertebral Characters of the Crocodilian Genus
Plesiosuchus, Owen.” By Prof. R. Owen, C.B., F.R.S., F.GS.
In this paper the author, with the view of showing that the
Kimmeridgian Stenecosaurus Manselii, Hulke, really forms the type
of a distinct genus, discussed the characters by which Cuvier divided
the fossils referred by him to the Crocodiles into three principal
groups, to which Geoffroy St.-Hilaire gave generic names, and those
by which the latter author afterwards distinguished his genus
Steneosaurus, including Oolitic forms, from the Liassic genus T’cleo-
saurus. From his exposition of these characters the author con-
cluded that the above-named species does not belong to Steneosaurus,
Geoff., and he proposed to make it the type of a new genus, Plesio-
suchus, characterized by the convergence of the frontal bones to a
point nearer the apex of the skull than in Steneosawrus, by the ex-
tension of the gradually attenuated nasal bones into a point pene-
trating the hind border of the nostril, and by other peculiarities of
the skull, teeth, and vertebre. The author pointed out that this
form, like Stencosaurus, helped to bridge over the space between the
Liassic Teleosaurs and the Tertiary and recent Crocodiles, even ap-
proaching nearer to the latter than the older Oolitic type.
3. **On some Tracks of Terrestrial and Freshwater Animals.”
By Prof. T. M*Kenny Hughes, M.A., F.G.S.
The author’s observations have been made on certain pits in
the district about Cambridge which are filled with the fine mud
produced in washing out the phosphatic nodules from the “Cam-
bridge Greensand ’—a seam at the base of the Chalk Marl. As the
water gradually dries up, a surface of extremely fine calcareous mud
is exposed. ‘This deposit is often very finely laminated, and occa-
sionally among the lamine old surfaces can be discovered, which,
after having been exposed for some time to the air, had been covered
up by a fresh inflow of watery mud into the pit. The author de-
scribed the character of the cracks made in the process of drying,
and the results produced when these were filled up. He also de-
scribed the tracks made by various insects, indicating how these
were modified by the degree of softness of the mud, and pointed out
the differences in the tracks produced by insects with legs and elytra,
and by Annelids, such as earthworms. ‘The marks made by various
worms and larve which burrow in the mud were also described.
Bibliographical Notices. 63
Marks resembling those called Nerettes and Myrianites are produced
by a variety of animals. The groups of ice-spicules which are
formed during a frosty night also leave their impress on the mud.
The author concluded by expressing the opinion that Cruziana,
Nereites, Crossopodia, and Palcochorda were mere tracks, not marine
vegetation, as has been suggested in the case of the first, or, in the
second, the impression of the actual body of ciliated worms.
BIBLIOGRAPHICAL NOTICES.
Farm Insects: being the Natural History and Economy of the Insects
injurious to the Field-crops of Great Britain and Ireland, and also
those which infest Barns and Granaries. By Joun Curtis, F.L.S.
Illustrated with numerous Engravings. 8vo. London: Van
Voorst, 1883.
Tue value of the work of the late John Curtis on Farm Insects is
so generally recognized that we need do little more than call atten-
tion to this reissue of it in its original form. No doubt economic
entomology has made considerable progress since the first publica-
tion of the book in its complete form in 1859; but while we may
admit that this progress would enable us to correct some statements
and to fill up gaps in the history of certain species which the author
was compelled to leave, it is astonishing to notice how little the
broad treatment of the subjects would need to be modified. The
work of the great English entomologist was in fact so thoroughly
done according to the lights of his day, that later writers have
practically added but little to it, and we may say that the agricul-
turist need wish for no better guide to the history of those minute
and often hidden enemies whose attacks are frequently so fatal to
his interests; while to the entomologist, at any rate, this reprint of
a classical, work which has been long unprocurable will prove ex-
ceedingly welcome, and he will hardly be inclined to regret that
the contents of the book have not been meddled with. The plates
alone, executed in the author’s happiest manner, are a delight to the
entomological eye, quite apart from their practical usefulness ; they
are, as the publisher says in his ‘ Advertisement,” *“* so excellent
and so full of detail” that their reissue to the public, with the ac-
companying text, not only needs no apology, but entitles him to the
thanks of all interested in entomology.
John Curtis, as we all know, was so careful and conscientious a
worker, that it is no great wonder if his labours in the department
of agricultural entomology carried him so far in advance that even
now we have little to add to his account of the natural history of
the farmer’s insect foes, and that all subsequent writers on the sub-
ject have been compelled to borrow largely from his pages. It is
64 Bibliographical Notices.
not difficult, in fact, to recognize the direction that an editor’s
labours would have to take should it ever be decided to produce a
new edition of this book; his researches would have to be devoted
chiefly to collecting the records of cases in which particular species
had proved specially injurious, and the details of the application of
new remedies, of which many, as may be seen from Miss Ormerod’s
useful little book, have been proposed with varying success, often
involving the use of materials comparatively unknown when Curtis
wrote. This new information might easily be worked up into the
form of appendices or supplementary notes without interfering
seriously with the original text, and changes of nomenclature, of
which there are many, could be indicated in a similar manner.
Monograph of the British Aphides. By Grorer Bowpier Bucrton.
Vol. IV. 8vo. London: Ray Society, 1883.
In this fourth volume Mr. Buckton concludes his monograph of
the British Aphides, and supplements the descriptive portion with
some general remarks, which will serve to direct the attention of
students to the very interesting questions connected with the history
of that remarkable group of insects. .
The species here described are the British members of the tribes
Pemphiginz, Chermesine, and Rhizobiine ; they are treated in the
same fashion as in the preceding volumes, and several of them are
of special interest in connexion with M. Lichtenstein’s theory as to
the reproduction of Aphides. The views of that entomologist,
which appear to be gaining ground, are quoted by the author in
several places, notably in connexion with the genus Phyllowera,
under which we find the translation of an excellent summary of his
opinions furnished by Lichtenstein himself to Mr. Buckton (p. 63),
which will be of great service to English readers,
As already stated, Mr. Buckton has appended to the systematic
part of his work a discussion of various interesting questions con-
nected with the natural history of Aphides in general, commencing
with some remarks on the relation between Aphides and Ants—a
subject upon which much has been written, often in a somewhat
hyperbolical strain. Mr. Buckton apparently does not regard the
extant evidence as sufficient to establish anything like a necessary
relation between the Aphides and the Ants in whose nests they are
sometimes found; and certainly those writers who maintain that
certain ants obtain nearly the whole of their sustenance from plant-
lice are manifestly in the wrong. At the same time the existence
of this curious relationship between insects of such different types is
proved by the testimony of so many good observers, that we cannot
deny it some considerable importance in the economy of the ants.
Mr. Buckton’s remarks are eminently suggestive.
The most important section of his supplementary matter, how-
ever, is that in which he deals with the reproduction of Aphides ;
and in the preparation of this he appears not only to have carefully
Miscellaneous. 65
gone through all the contributions of previous writers, but also to
have entered personally upon a most elaborate investigaion of the
anatomy of the reproductive organs in the different forms of these
insects. This portion of Mr. Buckton’s work is particularly valuable.
The succeeding section, relating properly to fossil Aphides, is
rather discursive, and strikes us as perhaps hardly in place in con-
nexion with a Monograph of British Aphides. The author here
enters more or less into a discussion of the occurrence of fossil
insects in sedimentary rocks and in amber, and finally describes and
figures the Aphides occurring in the latter, those determined by
Heer from the Tertiary deposits of Giningen and Radoboj, and
finally the species obtained by Mr. Scudder from the Tertiary basin
of Florissant, in the Colorado region. ‘The last-mentioned forms
have been determined and named by Mr. Buckton from Mr. Scudder’s
drawings.
The volume concludes with some practical remarks on natural
and artificial checks to the increase of Aphides, and on preserving
and dissecting these minute and delicate insects, which will prove
of great service to intending students of the group, whose number
we hope may be greatly increased by the facilities which Mr. Buck-
ton’s labours have offered to them in his present work. His care-
fully prepared descriptions and figures place in the hands of students
a ready means of working out whatever is already known of the
British forms of one of the most interesting and curious groups of
insects, a group many members of which, from their wonderful
fecundity, are among the most formidable foes of the farmer and the
gardener, and which thus has as it were a double claim to our
notice. In conclusion, we would heartily congratulate Mr. Buckton
upon the completion of his work, which, although we know it to
have been a labour of love, must nevertheless have tasked his
energies severely.
MISCELLANEOUS.
On the Development of Balanoglossus. By Witrt1am Bateson,
Cambridge, England*.
Aw unlimited quantity of this remarkable form was easily to be
obtained at half-tide all along the shores in the neighbourhood of
Hampton, Virginia. The difficulties attending the investigation
were far less than those that have been previously met with at other
localities. Since the time during which I have been able to remain
in America was exceedingly limited, I thought it best to confine my
work at Hampton to the study of fresh specimens of the animal,
and to the task of collecting and preserving them for subsequent
* Note from the ‘Chesapeake Zoological Laboratory,’ 1883.
Ann. & Mag. N. Hist. Ser. 5. Vol. xiii. 5
66 Miscellaneous.
examination by means of sections. My observations are therefore
very meagre and inadequate, especially as regards the organogeny
of the form, owing to the extreme scarcity of the larvee. These im-
portant deficiencies I hope subsequently to supply when I shall have
been able to examine my material by sectional methods. The
general appearance of the Hampton form presents many points of
slight divergence from the species common at Naples (B. minutus),
so that at first sight the two animals seem very different; but
whether the anatomy of this form is essentially different, I could
not decide by examination of fresh specimens alone. The principal
result of my work has been to show that the form common on the
Chesapeake coast does not pass through the Tornaria stage, which
has been described by previous observers as the larva of Balanoglossus,
The eggs of this animal are opaque, yellowish-grey bodies, enclosed
in a thin tough egg-shell which is quite transparent. Segmentation
is begun by the appearance of a median furrow which divides the
ege into two equal halves. This is followed by another median
furrow at right angles to the first, forming four segments. In the
next stage that I have been able to observe segmentation was com-
plete, having probably proceeded in a regular manner, though
this I have not been able to determine. One edge of the blasto-
derm is next flattened and gradually depressed, causing the embryo
to take the shape of a concavo-convex disk. The concavity be-
comes gradually reduced in size as its edges grow together to form
the blastopore, appearing at the same time to become thickened.
This process is continued until the blastopore becomes exceedingly
small; whether it subsequently disappears or not I cannot say until
I have cut sections of it. I believe, however, that it becomes the
anus, which at all events is found in the same position. As this
gastrula becomes shut off it resumes the spherical shape and begins
to rotate about the axis which eventually becomes the long axis of
the animal, at the top of which the blastopore is placed. This
rotatory movement is caused by a uniform covering of fine cilia,
After rotating in this way for some few hours, the body elongates
and aring of large cilia appears surrounding the posterior end.
The animal then swims round the egg, rotating at the same time on
its long axis. A nearly median transverse constriction next occurs,
which is followed by another one anterior to it, giving the body the
appearance of being composed of three segments. The anterior seg-
ment becomes the proboscis, the middle one forms the collar, and
from the posterior portion the rest of the body is developed. With-
in the anterior constriction the mouth is subsequently formed. At
the anterior end of the proboscis a tuft of fine long cilia grows
out as in the larvee of many Cheetopoda, &c. A pair of depressions
are at the same time formed posteriorly to the collar in a dorsal
position. These depressions form the first pair of gill-slits. In
this condition the larva is generally hatched, though I have found
individuals already free before the appearance of the transverse con-
striction. On hatching these larve are still quite opaque, and live
buried in the muddy sand which the adults inhabit. In this con-
Miscellaneous. 67
dition the animal remains for some time, increasing in size, until it
is about an eighth of an inch long, the proboscis being about half
the total length of the body. The tip of the proboscis is used by
the larve to attach themselves by suction to foreign bodies, though
apparently no special suctorial organ exists. As the body grows, the
posterior band of cilia becomes wider and the cilia themselves longer
and coarser, while the direction of the band alters slightly. From
the appearance of fresh specimens in this stage, treated with acetic acid,
I believe that several pouches arise from the gut which probably are
destined to form the other gill-slits; but this is quite uncertain,
though of course sections will at once decide this question. I have
been unable to procure any specimens older than these, and of the
changes by which this larva becomes converted into Balanoglossus
I can therefore say nothing. Possibly the animal remains in this
condition during the winter and awaits the spring for its final de-
velopment. I hope to be able to observe the subsequent stages at
some future season.—Johns Hopkins University Circulars, Noy. 1883.
On the Development of the Branchia in the Cephalopoda.
By M. L. Jounin.
The investigations of Kolliker upon the development of the Cepha-
lopoda, while throwing much light upon the embryogeny of those
animals, have nevertheless left in obscurity the origin of the organ
of respiration. I have set myself, in the laboratories of M. de
Lacaze-Duthiers, to fill up this gap by studying principally the
Sepia officinalis, the eggs of which are easily procured.
The branchiz of the embryo make their appearance at the begin-
ning of the development in the form of two small buds, situated
symmetrically with relation to the antero-posterior plane upon the
middle of what will eventually become the posterior wall of the
palleal cavity. The bud, produced by a pushing forth of the epi-
thelial layer by the cells of the subjacent layer, soon elongates and
forms a small well-differentiated eminence, rounded at the apex
and attached by a broad base. I found it impossible, even in the
youngest embryos that I could obtain, to ascertain the presence of
vibratile cilia upon the branchia, although the palleal cavity is lined
with them. ‘The bud afterwards flattens so as to present two sur-
faces—a posterior one, applied against the visceral mass, and an
anterior one, which is subsequently covered by the mantle which
bounds the respiratory cavity superiorly.
Upon this little lamina, which is about 1 millim. in length, a first
horizontal fold appears towards the middle, then a second nearer to
the point, then a third still nearer to the free extremity, and so on.
These folds form depressions upon one of the surfaces correspon-
ding with elevations upon the other surface ; the branchial bud has
therefore become an undulated lamina; gradually other folds appear,
always towards the point, while the whole organ at the same time
increases in dimensions, so that a length of 13 millim. corresponds
with a dozen folds. But the latter do not oceupy the whole surface
68 Miscellaneous.
of the young branchia; a space is reserved along its two margins
(the external and the internal), in one of which will be formed the
efferent vessel, and in the other the special gland of the branchia.
One of these undulations, considered in its totality, may be re-
garded as a semicircle formed by three parallel curves of cells, a
middle one enclosed between an external convex and an internal
concave one. Supposing the two extremities of this arc fixed in the
same plane, if growth took place with equal rapidity in the three
layers of cells, we should soon have a large cul-de-sac, no longer a
semicircle, but more or less conical and deep; but things go on
otherwise—the cells of the middle layer increase in number, and
push before them the epithelium forming the convex surface, while
that which forms the concave layer is not modified. By advancing
more and more by means of a terminal focus of cell-division, the
median layer gives rise to a lamina clothed on its two faces by the
convex epithelium. The cells of this lamina, which are at first con-
tiguous, soon separate from each other, so as to form lacunee, and, at
certain points, vessels, From this it results that, as this process
is repeated alternately to the right and left of the primary undulated
lamina, we obtain sections of the branchia composed of a slightly
undulated axis, from which issue, to the right and left alternately,
lamine which become longer and longer the further we go from the
extremity of the branchia. A little later we easily distinguish a
small muscular band, which follows the inferior margin of each of
the laminze composing the branchia and fixes it.
Each of the laminw formed as I have just stated produces in its
turn a series of undulations by becoming folded in the direction of
its width. But in this case the undulations are much hollowed,
and correspond with strong eminences on the other side; no new
productions are formed at the expense of the median layer, which
remains even throughout and preserves its two epithelia. These
undulations start from the point of attachment of the lamina, to
run, gradually diminishing, to the point where is the focus of in-
crease and where the new folds are formed.
Lastly, in the adult we observe a third system of undulations,
consequently of the third order, situated perpendicularly to the point
of inflexion of the laminz, the formation of which I have just
described. These series of new folds only appear very late in the
embryo; at the moment when, being on the point of quitting the
egg, it measures about 15 millim. in length, we only see scarcely
perceptible traces of them, but they become quite distinct when in-
jections of the branchia are made, which, however, is a very delicate
operation.
As regards the vessels of the branchia, the one which conveys the
blood to it appears early at the commencement of the formation of
the laminz ; it occupies nearly the centre of the organ, and is com-
prised within the base of the lamine and the gland of the branchia,
which is also distinctly marked at this period. The efferent vessel
is formed upon the crest of the branchia and on the outer border of
the lamine ; it is undulated, like the parts which bear it, and issues
Miscellaneous. 69
from the branchia at the base, to be continued by the auricle of the
heart.— Comptes Rendus, November 12, 1883, p. 1076.
Injury sustained by the Eye of a Trilobite at the Time of the
Moulting of the Shell.. By Cuartes D. Waxcorr.
Mr. William P. Rust, of Trenton Falls, N. Y., called my atten-
tion some time since to the eyes of a small but very perfect speci-
men of Jllenus crassicauda, from the Trenton Limestone, that he has
in his beautiful collection of Trenton fossils.
The left eye is perfect: the visual surface is clearly defined, and
in the sunlight almost translucent between the darker base and the
curve of the facial suture above. The right eye at first sight ap-
pears to have been broken in working away the matrix ; but aclose
examination shows, as Mr. Rust expressed it, that the eye had
been put out while the animal was living. This is shown by the
peculiar growth of the shell about the aperture formerly occupied by
the visual surface of the eye. The margins are turned in, rounded,
and contracted, and the size of the palpebral lobe materially lessened.
An injury to the visual surface would scarcely produce this effect if
the shell was hard. If slightly injured before the moulting of the
shell the separation would be imperfect and the visual surface carried
away with the old shell would leave a cavity around which the new
shell would form, as in the eye before us. If injured before the new
shell had hardened, that effect might be produced; but the proba-
bilities are, that the loss of the visual surface occurred at the time
of the moulting of the old shell.
Among the thousands of trilobites that have passed through my
hands in which the eyes were preserved I have never noticed any
distortion or injury that occurred during the life of the animal.
In a few instances the shell of the pygidium of Asaphus platyce-
phalus has shown evidence of local fracture that appears to have
occurred during the life of the animal, but these were very unsatis-
factory. To Mr. Rust’s skill in working out the specimen described,
and also in detecting the character of the injured eye, we are in-
debted for some positive information of an injury sustained during
the moulting of the shell of a trilobite —<Amer. Journ. Science, Oct.
1883, p. 302.
The Pelagic and Deep Faunas of the two Lakes of Savoy (the Lae
du Bourget and Lac d’ Annecy). By Dr. O. E, Imnor.,
The Lac du Bourget is 17 kilom. long and about 5 kilom. broad,
and its depth is stated at 80-100 metres. The Lac d’Annecy mea-
sures 14 kilom. in length, and its greatest breadth is 33 kilom. ; its
greatest depth is estimated at 62 metres.
In the Lac du Bourget on the 5th October the author obtained at
20 metres Daphnella brachyura, Liev., Leptodora hyalina, Lillj., a
70 Miscellaneous.
Bosmina, a Cyclops, and a Diaptomus. From 50 metres he got two
more Cladocera, Sida crystallina, Miull., and Daphnia hyalina,
Leyd. Of the Rotatoria his two new species, Asplanchna helvetica
and Anurca longispina, were pretty abundant. Of Protozoa a
Ceratium and a new Dinobryon (D. cylindricum, which also occurs
in the lake of Neuchatel) occurred. ‘The Copepoda and Daphnella
brachyura were most numerous in individuals, while the Bosmina
occurred rarely. Bythotrephes appeared to be absent.
The pelagic flora consisted of numerous tufts of Anabena circinalis,
Pleurococcus angulosus, Giallionelle, and Fragillarie, The Anabena
bore numerous Vorticelle, which never occurred on the Pleurococcus, a
condition also obseryed by Forel in the lake of Geneva and by the
author in the lake of Zug.
The bottom, at about 100 metres, between Petit Port and the
Chateau de Bourdeau, furnished but few forms. A specimen of the
blind Asellus Foreli, Blanc, bore many Vorticelle. There was also
a perfectly transparent Cypris. A rather large, fusiform, rather
thick, pale reddish Rhabdoccelous Turbellarian formed a rather deep
furrow in the mud when moving forward. Of Protozoa there were
a Oothurnia with a yellow, sessile, beaker-shaped carapace, and a
Rhizopod of the family Euglyphina, a Cyphoderia, Schlumb. (mar-
garitacea ?).
The pelagic fauna of the Lac d’Annecy included :—Cladocera :
Daphnella brachyura, Liey., Daphnia hyalina, Leyd. (the most
numerous of the Cladocera); a Bosmina (rare here also); and
Leptodora hyalina, Lill}.
Copepoda: a species of Cyclops and one of Diaptomus. Bytho-
trephes appears to be wanting here also.
Corethra-larvee in considerable numbers.
Rotatoria: three species, Asplanchna helvetica (extraordinarily
abundant), Anurewa spinosa (rare), and Anurea longispina (less
rare).
Eis : a species of Dinobryon and one of Ceratium.
The deep fauna at the same place, at 80 metres, was richer than
in the Lac du Bourget. Colonies of redericella bore many exam-
ples of the Rotatorian Floscularia proboscidea, Khr., together with
four species of Infusoria, namely Stentor ceeruleus, Khr. (pretty abun-
dant), two species of Vorticelle (in considerable quantity), and
Epistylis (Opercularia) nutans, Ehr. Other Protozoa met with were
Carchesium polypinum, Ehr. (not uncommon), an Ameba, and the
same Cyphoderia as in the Lac du Bourget.
Besides these, the author dredged up a species of Pisidium and
Asellus Foreli; of the Cladocera, Sumocephalus veiulus, O. F. Mill.,
and Lynceus affinis, Leyd.; of the Ostracoda, a species af Cyprid ;
of the Copepoda, a Canthocamptus, probably undescribed. A dingy
white Hydra also occurred.—Zool. Anzeiger, vi. no. 155, Dec. 10,
1883, p. 655.
MD
Miscellaneous. 71
An Instance of Sexual Colour-variation in Crustacea.
By H. W. Conn*.
Differences in the colour of the two sexes among Crustacea are of
very rare occurrence. Darwin in ‘The Descent of Man,’ chap. ix.,
refers to this fact and says he is acquainted with but two instances
of this peculiarity. One in the case of Squilla stylifera, and a
second in a species of Gelasimus, or fiddler crab, described by Fritz
Miiller as occurring in Brazil. A third and very striking instance
is found in Callinectes (Neptunus) hastata, the common edible crab
of our southern coast. There are a number of differences in the shape
of the two sexes, but besides these they present a marked difference in
colour. This colour-variation is confined to the first pair of thoracic
appendages, the pair bearing the large chele. These appendages are
of a yellowish brown on the upper surface, a whitish yellow on the
outside, and of a brilliant blue on the inside and particularly at those
parts which are protected from the light when the appendage is
folded. It would seem therefore that this blue coloration was en-
hanced by not being exposed to light. The colour of different
individuals is tolerably constant and uniform,
Between the colours of the male and female appendages considerable
differences are discernible. The most noticeable difference is that
the male appendage appears remarkably blue when compared with
the female. ‘This is due partly to the fact that the amount of blue
surface in the male is much greater than in the female, and partly
to the fact that the blue colour is of a much more brilliant hue. The
blue colour in the male extends nearly to the tips of the two fingers
of the chele, both the finger-like process of the propodite and the
dactylopodite being largely coloured blue. The very tips are, how-
eyer, of a brilliant purple. In the female these parts are of an
orange hue, with not a trace of blue about them. ‘The tips are
also coloured purple, but not so brilliant a purple as is found in the
male. In the male the blue colour extends partly upon the outer
surface. In the female it is confined to the inner surface and only
extends to the base of the dactylopodite. The outer surface of the
dactylopodite and of the finger-like process of the propodite are in
the male white, while in the female they are reddish orange. Upon
the male appendage there is no orange colour as a rule.
These differences in colour are in all cases very marked, and will
always serve to distinguish a male from a female appendage. No
colour-differences are seen in any part of the crab except upon the
first pair of appendages ; and it is interesting to note that this sexual
difference does not make its appearance till the crab reaches ma-
turity. The chele of immature males and females cannot be dis-
tinguished from each other. Fritz Miiller says that the same is
true of the Gelasimus observed by him. On the other hand, con-
sidering the habits of Crustacea, these sexual differences can hardly
be considered as the results of sexual selection.—Johns Hopkins
University Circulars, Noy. 1883.
* Note from the ‘ Chesapeake Zoological Laboratory,’ 1883.
‘42 Miscellancous.
On the Influence of Physico-Chemical Agencies upon the Development
of the Tadpoles of Rana esculenta. By M. Emite Youne.
The author subjected tadpoles just hatched to the action of saline
solutions of various strengths. The salts employed were obtained
by the evaporation of the water of the Mediterranean, and the larve
were placed in solutions of 1, 3,5, 7, and 9 per 1000, which were
renewed at the same time in all the vessels, and the whole were in
other respects placed under precisely the same conditions. Asa
general result, M. Yung states that the tadpoles are developed the
more slowly the more considerable the degree of saltness of the water.
In the solution of 2,5 no transformation took place, though some
tadpoles lived long enough to acquire hind limbs. In a solution of
71%, very young tadpoles die in a few hours; older ones survive
for a few days.
The author remarks upon the importance of placing equal num-
bers of individuals in each vessel in experiments of this kind. On
placing 4, 8, 12, 16, &c. tadpoles of the same age and the same
brood in a series of vessels, and keeping them under precisely the
same conditions, their development is found to be slower in proportion
to the number living together, which confirms the results obtained by
Semper for the Limnee.
Finally, M. Yung subjected young tadpoles, which normally live
in quiet water, to continuous agitation in a vessel containing two
litres of water regularly renewed and suitable food. The agitation
of the liquid was felt to the bottom of the vessel, but reached its
maximum at the surface, where the tadpoles, on coming up to the air,
had to struggle against strong waves. Under these conditions the
eggs developed well; but the newly hatched tadpoles, being too
feeble to seize their prey in so disturbed a medium, died of hunger,
unless care was taken to give them daily a few moments of repose
to take their food. The mortality was always greatest in the first
few days ; it diminished immediately the first transformations were
effected. Of twenty individuals placed in the vessel in April, eight
have furnished little frogs, and on the Ist August only one had not
completed its metamorphoses.
If these agitated tadpoles be compared, at different periods, with
others of the same brood developing in quiet water, it is found that
the development of the former is slower (the test-tadpoles were all
transformed on the 15th July), that they are less pigmented, which
indicates bad nutrition (the tadpoles which do not eat much are
always pale) ; and, lastly, that their tails are relatively more de-
veloped, especially in width, which is explained by the greater use
they are obliged to make of these organs in struggling against the
waves.— Bibl. Univ., Arch. des Sciences, pér. 3, tome x. p. 347,
October 15, 1883.
THE ANNALS
AND
MAGAZINE OF NATURAL HISTORY.
[FIFTH SERIES.]
No. 74. FEBRUARY 1884.
VII.—On a Specimen of Pecopteris (? polymorpha, Brongn.)
tn Cuircinate Vernation, with Remarks on the Genera
Spiropteris and Rhizomopteris of Schimper. By Ropert
Kipston, F.G.8.*
[Plate V. fig. 1.]
ALTHOUGH the beautiful specimen which forms the subject of
this communication does not throw any additional light on
the growth of fossil ferns, yet as none of the figures of cir-
cinate vernation with which I am acquainted surpass this
example, I have ventured to give a short description and a
figure of it.
The fossil is about 3 inches long; but if we measure the
full length of the circinately rolled-up portion as if it were
straightened out, it is fully 6 inches inlength. The specimen
is, however, incomplete at its lower extremity ; so its original
size cannot now be ascertained.
_ The rachis is thick and still shows slight traces of the little
scales with which its surface was once covered. ‘he inner side
of the rachis bears about thirty-three circinately rolled-up pinne.
* Read before the Royal Physical Society of Edinburgh, December 19,
3
Ann. & Mag. N. Hist. Ser. 5. Vol. xiii. 6
Pe AS ee 1
74 Mr. R. Kidston on Pecopteris (? polymorpha,
These show nothing further than the midribs of the pinnules,
which appear as strongly defined ridges. There is no evi-
dence in the specimen itself to indicate the species to which
it belongs ; but from the occurrence of fragments of Pecopteris
polymorpha, Brongn., on the same slab *, it probably belongs
to that fern.
The specimen is in the collection of the Geological Survey
of Great Britain, to whom it was presented by Mrs. Stock-
house Acton.
My thanks are due to Dr. A. Geikie, F.R.S., Director-
General of the Geological Survey of Great Britain, for per-
mission to describe this interesting fossil.
Position and Locality. From the Coal-measures, Leebot-
wood, about nine miles from Shrewsbury.
As a means of giving a definite place in the classification of
fossil plants to such fossils as that just described, Schimper
has proposed the genus Spiropteris t, in which he places
those specimens of ferns that do not afford sufficient characters
for the determination of the species to which they belong.
For fossils of this nature the genus is very useful, as it gives
a fixed, though provisional, position to many interesting speci-
mens which cannot be specifically associated with the fully-
developed frond.
Several very interesting examples of Spdropter’s have been
already described.
In 1828 Brongniartf figured a Spzropteris-condition of Pec.
Miltont, Artis (=Pec. polymorpha, Brongn.), which shows a
few of the pinne spirally coiled.
Goppert gives a figure of circinate vernation of Pec.
Jdgert§. It exhibits a very young condition of probably a
whole frond. He also gives another specimen of Spzropteris
on his plate xxxvi. fig. 8.
Probably the most interesting figures of Spiropterts are
those given by Germar ||, which he named Selaginites Erd-
mannt. ‘These, as Schimper has pointed out, are not Lyco-
pods, but young ferns {], and referable to Sprropteris.
Though the specimens are of considerable size, they show
merely the early condition of a large frond. The dense cover-
* Not shown in the figure.
+ Traité d. Paléont. Végét. vol. i, p. 688, pl. xlix. (1869).
{ Hist. d. Végét. Foss. p. 334, pl. exiv. fig. 1.
§ Die fossilen Farrnkrauter, p. 368, pl. xxii. fig. 6 a (1836).
| Die Verst. d. Stemkoblengebirges y. Wettin u. Lobejun, p. 61,
pl. xxvi. (1844).
q Schimper, Traité d. Pal. Vég. vol. i. p. 689,
Brongn.) in Ciretnate Vernation. 735
ing of scales with which they are bedecked, gave rise to the
mistaken opinion that the fossils were Lycopods and the
scales their leaves.
A small specimen of Pec. arborescens, Schl. sp., in circinate
vernation has been figured by Geinitz in his ‘ Verst. d. Stein-
kohlenform. in Sachsen’ *.
Sir C.J. F. Bunbury described a very curious fossil fern
from the Sydney Coal-field, Cape Breton f, which showed por-
tions of a frond in circination.
This specimen beautifully exhibits numerous long scales
on the rachis. Some of the lateral pinne are fully expanded ;
but these, unfortunately, are not sutiiciently well preserved to
enable one to determine the species to which the fern belongs.
Bunbury regarded it asa Fecopteris standing in the neigh~
bourhood of P. plumosa, Brongn.
From the scales on the rachis Mr. R. Brown, who found
the specimen, “ supposed it to belong to a peculiar species of
Lepidodendron”’ t; but there can remain no doubt as to the
fossil being a fern referable to Spdropteris.
The same writer in 1857 § figured and described a specimen
of Neuropteris (probably, as suspected by the author, Neur.
gigantea, Sternb.) circinately coiled, from Glodwick Colliery,
near Oldham, Lancashire.
Examples of Neuropterts in this condition are even more
rare than those of Pecopteris.
The figure which accompanies his paper shows a very per-
fect example with the usual accompanying scales on the
rachis.
Mr. T. Stock has shown me a small circinate specimen of
Neuropteris from the Coal-measures near Dysart, Fife ; but
this one probably belongs to N. Loshii, Brongn., as it was
associated with that fern.
In the ‘Illustrations of Fossil Plants,’ which consists of a
reproduction of a number of unissued plates prepared by
Lindley and Hutton for their ‘Fossil Flora,’ three good figures
of Spiropteris are given ||.
- Plates xlv. and xlvii. are referable to Neuropteris, but of
that on pl. xlvi. the genus is uncertain{.
* p. 24, pl. xxviii. f. 10 (1855).
+ Diliat. Journ. Geol. Soc. vol. viii. p. 31, pl. i. (1852).
t Ibid. vol. viii. p. 82.
§ Bunbury, “On a remarkable Specimen of Newropteris, with Remarks
on the Genus,’ Quart. Journ. Geol. Soc. vol. xiv. p. 243.
| Edited by G. A. Lebour, Newcastle-on-Tyne, 1877.
q See Crépin, Révision de quelques espéces figurées dans l’ouvrage
_ intitulé “Illustrations of Fossil Plants,’ Soc, roy. de botanique de Bel-
_ gique, vol. xx. part ii. p. 25 (1881). .
3 6
76 Ona Specimen of Pecopteris (? polymorpha, Brongn.).
In a paper on Sphenopteris afiinis, L. & H.*, Mr. C. W.
Peach gives some good figures of the young state of this
fern. His figures 6 and 7 show very clearly the character-
istic dichotomy of the rachis of this species.
The above is a list of the chief Paleozoic examples of Sp7-
ropteris which have been figured and described ; and it is re-
markable, that though ferns are our most common class of
fossil plants in the Carboniferous formation, specimens show-
ing their early stages of development are so seldom met with.
There is another group of fossils which, though very similar
in general appearance to Spiropterts, are most probably quite
different in nature. For these Schimper has proposed the
name Rhizomopteris T.
In this genus Schimper places the specimens which Geinitz
has figured} as Selaginites Erdmanni, believing them to be
fern-rhizomes; and certainly the fossils in question have a
great resemblance to such structures.
There can be no doubt as to Geinitz’s plants being quite
distinct from those originally described under the same name
by Germar §.
Schimper also places in his Rhizomopteris the Selaginites
uncinnatus, Lesqx. ||.
Lesquereux, though he says the specimen cannot posi-
tively be referred to the Lycopodiacez, still keeps it separate
from Rhizomopteris, and includes it in Lycopodites (L. un-
cinnatus) 4.
I am inclined to regard this fossil as the rhizome of a fern ;
and the spiral terminations of several of the branches, which
appear to be the chief character that prevents Lesquereux from
regarding his plant as a rhizome, are most probably spirally-
coiled young fronds springing from the points of the branchlets
of the rhizome.
From the nature of the fossil and the state of its preserva-
tion, there is, however, room for difference of opinion as to its
true nature.
* Quart. Journ. Geol. Soc. vol. xxxiv. p. 131, pl. viii. figs, 5-7.
+ Schimper, /. c. vol. i. p. 699 (1869).
t Geinitz, /.c. pl.i. figs. 5 and 6.
§ Geinitz figures in his ‘ Flora der Kohlenform. v. Hainichen-Ebersdorf
u. Fliher-Guckelsberg,’ p. 56, pl. xiv. fig. 20, a plant which he also names’
S. Erdmanni. This appears to be only a badly-preserved Lepidodendron.
|| Geol. Survey of Illin. vol. ii. p. 446, pl. xli. fig. 3 (1866).
q ‘ Coal-Flora of Pennsylvania,’ p. 359 (1880).
+5
Mr. R. Kidston on a new Species of Schutzia. va
VIII.—On a new Species of Schutzia from the Calczferous
Sandstones of Scotland. By Roserr Kipsron, F.G.8.*
[Plate V. fig. 2.]
Schutzia Bennieana, n. s., Kidst.
Specific character.—F ruit campanulate, composed of linear
lanceolate bracts; pedicels of fruits short and placed spirally
on the axis.
Remarks.—The specimen on which the above description is
based, shows the upper portion of a fructification, but its
lower part is broken over, so that its original length cannot
now be determined. ‘The part which has been preserved is
3,3, inches long.
Only three fruits are attached to the stem, the terminal one
and two immediately beneath it.
Below these are seen the scars from which four others have
fallen. The spiral arrangement of the fruits is clearly shown
by the position of those which still remain, that on the right
being placed at about a third of the circumference of the
stem distant from the one to the left hand.
The bracts of the little cones are about half an inch long,
narrow, and terminating in a sharp point, and they appear to
have had a central keel. From the compressed state of the
fossil it is impossible to make out their arrangement clearly,
but they were probably placed in a few spirals.
The stalks to which they are attached are short, being
barely, in the longest and lowest example, the fifth of an inch
long. ‘The main axis is irregularly striated longitudinally.
A ffinities—This plant is closely related to Schutzia ano-
mala, Geinitz t, from the Rothliegenden of Ottendorf, near
Braunau, Bohemia}; but the differences between the Permian
and the Scotch plant are such as to necessitate a specific
designation.
* Read before the Royal Physical Society of Edinburgh, December 19,
1883.
+ Geinitz, Neues Jahrbuch, 1863, “‘ Ueber zwei neue dyadische Pflan-
zen,” p. 526, pl. vi. figs. 1, 2, 3.
{ Goppert also notes the occurrence of this plant at Neurode, Silesia,
see ‘ Die foss. Flora der permischen Formation,’ pl. xxiii. figs. 1-6, pl. xxiv.
figs. 1, 2, 3, 5 (1864-5). The plates for this work were prepared before
the publication of the paper by Geinitz, though not issued till after ; hence
the name which Géppert had proposed for this plant (Anthodopsis
Beinertina) appears on his plates; Schutzia anomala, Gein., is used in his
text. See also Géppert, Fos. Flora d. Uebergangsgebirges, p. 214,
(1852).
78 Mr. R. Kidston on a new Spectres of Schutzia.
They agree in the spiral arrangement of the little cones, in
their being short-stalked, and in the furrowed stem, as also in
the angle made by the pedicels and the stem.
The form of the fruit is, however, essentially distinct.
In Schutzia anomala they are globular, and consist of
numerous and much shorter keeled scales, which are similarly
arranged in a few short rows. ‘These often appear blunt, but
Geinitz thinks this bluntness may arise through a bending of
their apices.
Schutzia Bennieana teaches nothing as regards internal
structure; but in S. anomala, Geinitz thought he could dis-
cover, “at the base of the inner side of the fruit-scales, the
appearance on each side of a longitudinal depression, which
corresponded to the two seeds in the fruit-scales of Coniferee.”
In addition to the plates of Schutzia given by Géppert,
he also figured another fossil, which he named Dictyothala-
mus Schrollianus *.
This he thought might belong to Schutzia anomala, the
latter being the female, the former the male plant. These
occurred together and often on the same slab.
The central part of Dictyothalamus is composed of small
elongated roundish bodies, which Géppert thought were the
seeds.
He believed these fossils might belong to the Neggerathie,
but Geinitz regarded them as coniferous.
As there occurred with the specimens Neggerathia (Cor-
dattes) and Coniferse of different genera, as Walchia pini-
formis, Schl., sp., and Ulimannia, no light is thrown on the
affinities of Schutzia by the vegetable remains with which it
was associated.
But that it does not belong to Walchia or Ullmannia is
pretty certain, as the fruits of both these plants are now well
knownt.
Schimper unites Dictyothalamus Schrollianus, Gopp., with
Schutzia anomala, Geimitz}, and regards the Schutzia as
the female, and the Dictyothalamus as the male plant. The
* Goppert, Die fos. Flora d. perm. Formation, p. 164, pl. xxiv. figs, 4 &
6, pl. xxv. figs. 1-4. f
+ Goppert figures and describes what he believes to be the fruit and
male flowers of Walchia piniformis, in Die fos. Flora d. perm. Form,
p- 239, pl. xlix.—the cones, figs. 1-10; the male flowers, figs. 11-14. See
also Weiss, Flora d. jiing. Stk. u. d. Rothl. p. 179, pl. xvii. fig. 1. The
fruit of Ulimaniia was described as far back as 1828 by H. Bronn, in
Leonhard’s Zeitschrift fiir Mineral. Band ii. p. 509, pl. iv., under the name
of Cupressus Ullmanni. _Goppert also figures, in his Permian Flora
similar cone-like fruits (pl. xlv. figs. 24, 25). }
{ Schimper, Traité d, Paléont, Végét. vol. ii. p, 368,
yt Wh ver
Mr. R. Kidston on a new Species of Schutzia. 79
structure in the latter which Géppert believed to be seeds,
Schimper thinks are stamens, and this view I am inclined to
adopt. These remarks show thatthe real affinities of Schutzia
are very obscure.
Schimper regarded these fossils as belonging to a “ coni-
ferous plant, which was altogether paradoxical and without
any analogy, either fossil or recent ”’*.
Although this is not a very satisfactory manner of dispo-
sing of Schutzia, the conclusions arrived at by Schimper
may possibly be correct, though we have little positive
evidence to support this opinion.
Large coniferous stems, with their internal structure beauti-
fully preserved, are of frequent occurrence in various parts of
the Calciferous Sandstones of Scotland. The remains of
coniferous trees also occur in rocks of similar age in different
parts of the globe; but notwithstanding their wide geo-
graphical distribution and frequency of occurrence, there is
nothing definitely known regarding their fruit or foliage.
Prof. Dawson has described and figured a small coniferous-
like branch from Tatamagouche (Carboniferous formation),
which he has named Araucarites gracilist. ‘This, he thinks,
may possibly belong to his Dadoxylon materiarum }f.
Some botanists regard the Trigonocarpons as the fruit of
Conifers, but this opinion is not universally accepted§.
The absence, however, of conclusive evidence as to the
fruit and foliage of Paleozoic Coniferee is not so surprising
when we consider that the ancient pines most probably occa-
pied the uplands of the then existing continents, and only the
stems and larger branches would be able to resist the abrasion
and decay of their long journey from the uplands to the flats,
where mud or sand was being deposited ; and as proof of this,
many of the stems of these trees are found imbedded in sand-
stone quarries, where they have been drifted.
The undoubted occurrence of the genus Schutzia so low
down in the geological scale is of considerable importance ;
the discovery in the Calciferous Sandstones of a plant so
closely related to a Permian species, is alinost without parallel.
* Loc. cit. p. 358.
+ Dawson, ‘ Acadian Geology,’ 2nd edit. p. 474, fig. 159 a (1868).
t Dawson, /. c. p. 424. ale,
Stur also gives, in his ‘Culm Flora’ (p. 81, pl. xiv. fig. 4), a small
figure and description of a fossil he has named Pinites antecedens. The
specimen is small, and its union with the Conifers appears a little un-
certain.
§ Since writing the above, Prof. Williamson, in his Address at the
British Association, has given aréswmé of this subject (‘ Nature,’ Sept. 20,
1883).
80 Prof. F. Schmitz on the
The small fossils which I previously described and placed
in the genus Schutzia are different from the present example,
and their real claim to this genus may perhaps be open to
question*.
Schutzia Bennieana comes so near the Permian species,
that it is only after very careful consideration I have given
it a specific designation f.
It gives me pleasure to name this plant after Mr. J. Bennie,
to whom I owe so much for kind assistance in many points
connected with my study of fossil botany.
Position and Locality.—In bituminous shale, water of
Leith, opposite Kate’s Mill, Midlothian ; Calciferous Sandstone
series. Collected by Mr. James Bennie.
1X.—On the Fertilization of the Floride.
By Prof. F. Scumirz.
[Concluded from page 29.] _
V.
THE preceding description has by no means exhausted all
the modifications presented by the process of fertilization and
fructification in the Floridez, as is shown by the fact that
in almost every fresh genus that I investigated I detected
new modifications of the previously observed processes. It is
also sufficiently demonstrated by Bornet’s statements with
regard to Spyridia, Callymenia, Crouania, and other genera
which I have hitherto been unable to examine. But the
most important modifications of these processes have probably
been shown in the foregoing in the described genera, which
belong to the most different families of the Floridez.
From this description it appears, however, that throughout,
in the fertilization of the Flovidez a material connexion exists
between the male cell, the spermatium, and the cell which is
developed into the sporigenous tissue of the cystocarp (the
“nucleus” of systematic botany). A fertilizing influence of.
1867, p. 288, pl. iil. fig. 4), is an analogous fruit, but specifically distinct
(Traité d. Paléont. Végét, vol. 11. p. 358).
Fertilization of the Floridee. St
the union of spermatium and carpogonium upon a third, dis-
tant cell is never to be observed *.
The general result of the above description may, however,
be briefly summarized as follows :—In all Floridew a single
male cell (spermatiwm) unites by open conjugation with the
apex of the trichogyne of the female cell (the carpogontium) ;
the cell-nucleus of the spermatium passes into the carpogo-
nium and unites (apparently) with the cell-nucleus of the
carpogonium. Then the ventral part of the carpogonium
separates as a fertilized ovicell from the trichogyne. The
fertilized ovicell, however, now becomes further developed in
many different ways. It either grows directly into a bundle
of branched ooblastema-threads, which finally produce the
carpospores directly from their cells; or these threads enter
into union with neighbouring cells of the sterile thallus-tissue
for the obtentation of more abundant nourishment, and then
produce the spores from their cells ; or the individual cells of
these threads enter into conjugation with cells of the thallus-
tissue rich in contents, and afterwards produce pluricellular
complexes of spores; or the cells of these ooblastema-threads
evacuate the whole of their plasmatic contents, or a portion of
* Asis well known the great accordance in the development of the
fruit in Ascomycetes and Floridez has already been repeatedly indicated
in literature. This agreement appears particularly great since Stahl has
succeeded in the Collemacez in tracing back the development of the
apothecium to a “ procarpium ” of which the trichogyne is fertilized by
spermatia. The preceding investigations on the fructification of the
Florideze haye shown that a material connexion always exists between
the two sexual cells, which concur in the act of fertilization, and the
cell which in consequence thereof develops into the spore-fruit. The
question now arises whether analogous conditions do not prevail also
among the Collemacez and other similar Ascomycetes (and Ascidiomy-
cetes ?) ; whether in these also the fertilized “ trichogynal cell” does not
develop into an ooblastema-thread, and then one of the ooblastema-cells
does not unite with one or more neighbouring auxiliary cells for the
development of the tuft of filaments of the ‘“‘ascogenous hypha.” Various
things seem to me to be in favour of this supposition, especially the great
morphological agreement which exists in so many points between the
Floridez and Ascomycetes. But nothing certain for the decision of this
question can be derived from the results of the extant investigations (of
Stahl, Borzi, and Fisch), as these investigations started from quite diffe-
rent points of view, and therefore have not gone sufficiently in detail into
the points which here essentially come under consideration. My own
observations upon the development of the Collemaceze have not as yet
been sufficiently detailed and complete to render any decision of this ques-
tion possible. f j
Further investigations will have to decide whether really (as it appears)
perfectly analogous processes occur in the fructification of the Ascomy-
cetes (and Ascidiomycetes?) and in that of the Floridez, or whether in these
groups of Thallophytes, notwithstanding external resemblance, essential
differences prevail in the processes in detail.
82 Prof. F. Schmitz on the
them, under open conjugation, into analogous auxiliary cells,
and these then produce pluricellular complexes of spores ; or,
finally, the fertilized ovicell itself empties the whole or a part
of its contents, without any formation of branched ooblastema-
threads, into the auxiliary cells immediately bordering it, and
thereby causes these to produce pluricellular complexes of
spores, or branched sporigenous filaments.
However, this last mode seems essentially to be confined
to Florideee with very dense and firmly closed cell-tissue
(Gigartiner, Rhodymeniex, Spharococceex, and Rhodomelez) ;
but the development of widely spreading ooblastema-threads
is chiefly proper to the Cryptonemiez, Gelidiez, and Squa-
mariez, in which either the whole thallus, or the fructifying
part of it, displays a gelatinous, soft or loose tissue. The
fertilized ovicell becomes developed directly into simple
bundles of sporigenous threads generally in such forms, the
moneecious individuals of which develop numerous carpo-
gonia and spermatia in close proximity, and make sure of the
fertilization of numerous carpogonia by the quantity of these
spermatia, so that it is not necessary, as in the preceding
cases, in which the fertilizations of the carpogonia only take
place singly, to use these up, and make them available in as
many ways as possible.
In all these different cases, however, it comes finally to the
formation of a sporigenous tissue-body of very variable size
and form. ‘This is sometimes seated upon the exterior of the
thallus of the parent plant, or is enclosed, without any special
envelope, in the tissue of the thallus ; but generally this tissue-
body forms a fruit-nucleus (‘ nucleus”’), and is surrounded
by a very variously formed envelope called the ‘ pericarp ”
or “involucre.” Both these forms are indicated in deserip-
tive algology indifferently as “ cystocarpia ;” but such cysto-
carpia (as, indeed, appears from the foregoing description) are
of very different origin in the different groups of the Floridez,
so that, for example, the cystocarpia of Nemalion, Naccaria,
Dudresnaya, Gleosiphonia, Chilocladia, Nitophyllum, Peys-
sonelia, Corallina, and Chondrus are by no means equivalent
in respect of their origin. Nevertheless the circumstance
that in all these cases the sporigenous mass of tissue, whether
naked or furnished with a wall, rises on the thallus of
the parent plant as an independent fruit-body, sufficiently
justifies the uniform designation of all these different forms of
fruit.
If we compare the different process-details of the fructifica-
tion with one another, it appears that, in the simplest cases,
the ooblastema-cells directly and immediately produce the
Fertilization of the Floridee. 83
carpospores. In other cases these ooblastema-threads, for the
purpose of readier and more abundant nourishment, first of
all enter into union with the cells of the sterile thallus-tissue.
In a later stage of fuller differentiation, special thallus-cells,
the auxiliary cells, are already previously prepared for this
purpose and abundantly furnished with contents; but the
ooblastema-cells enter mto a closer and closer union with
them, which may advance to complete conjugation. Finally,
the ooblastema-cell unites completely with the auxiliary cell to
form a single cell, which now, for its part, takes on the func-
tion of the ooblastema-cell and carries it to completion; and
at length there is no longer any development of pluricellular
ooblastema-threads, but the ovicell itself (or a part of it) unites
with the auxiliary cell. Thus, as the development of a simple
process of nutrition, there results a process which, in its whole
course, agrees perfectly with those processes which are desig-
nated as sexual processes of fecundation.
If in order to proceed quite securely we limit the discussion
to the processes of fructification in Gleosiphonia which are
comparatively easy to ascertain, the union of ooblastema-cell
and auxiliary cell here shows ail the characters of a sexual
fertilization. ‘The conjugation of the two cells and the trans-
fer of the protoplasm of the ooblastema-cell take place in
exactly the same way as in recognized processes of fecunda-
tion, for example in the fertilization of Pythium* and Anci-
listes T ; nay, 1t may even be ascertained that the cell-nucleus
of the ooblastema-cell unites with the cell-nucleus of the
auxiliary cell, as finally, after the evacuation of the ooblas-
tema-cell into the auxiliary cell, only a single cell-nucleus is
present. ‘The consequence of this union of the two cells is,
however, a new and very rapid growth of the auxiliary cell
quite different from its previous growth, a growth which
never occurs without a union of the auxiliary cell with the
ooblastema-cell. ‘Thus therefore a// the conditions f are ful-
filled that can be required of a process which is to be regarded
as a process of sexual fecundation ; and certainly no one would
* De Bary, Beitr. zur Morphol. und Physiol. der Pilze. 4te Reihe.
+ Pfitzer in Monatsh. Akad. Wiss. Berl. 1872, pp. 393, 394.
} If we leave out of consideration all inconceivable, mysterious, meta-
physical qualities of sexuality only the following remain as common
characters of all vegetable processes which have hitherto been by com-
mon consent recognized as sexual :—union of two (similar or diflerently
developed) cells with fusion of the cell-nuclei, and a new and peculiar
mode of growth of the conjugation-cell, which, without this conjugation,
does not take place. In other respects the generally recognized processes
of fecundation (to say nothing of the disputed ones) display the most
multifarious differences.
84 Prof. F. Schmitz on the
hesitate to interpret this process in Gl@osiphonia as a sexual
act, if it were not that in the developmental cycle of this
species there was already another process which must be
regarded as a process of sexual fecundation. To assume a
double act of fecundation in the developmental cycle of a
single species is, however, in complete opposition to botanical
conceptions,—that contradicts all tradition *.
But before the power of facts tradition must always give
way. As a matter of fact the state of the case is that in
Gleosiphonia the above-mentioned processes possess all the
characters which have elsewhere been reckoned requisite for
a sexual act. There is therefore nothing for it but either to
embrace as a character in the definition of a sexual act, that it
can occur only a single time in the developmental cycle of a
species, and that of two processes, both of which possess
the other requisite characters of an act of fecundation, only
one is to pass as a sexual act; or to admit that in the de-
velopmental cycle of Glaosiphonia (and all analogous Flori-
dew) a sexual act is twice intercalated, a fecundation of the
auxiliary cell following after the fecundation of the carpogo-
nium.
But if this amalgamation of ooblastema-cell and auxiliary
cell must be recognized as a sexual act, there is thus thrown
avery peculiar light upon sexuality in general. For here,
among the Floridee, the comparison of the different genera
shows distinctly that the process which in Gleosiphonia dis-
plays all the characters of a sexual act, is to be referred, as it
is distinctly observed in variously nearly allied Floridez, to a
simple act of nutrition, and has evidently originated from such
a simple act of nutrition. In this way then sexual fecunda-
tion is tacked on to the simple vegetative nutrition of one cell
* Certainly Pringsheim (Jahrb. f. wiss. Bot. xi. pp. 18 e¢ segg.) has
already distinguished, in the fecundation of the Thallophyta (and espe-
cially of the Floridez), two distinct acts, which he indicates as “ con-
jugation” and “connubium.” But this distinction simply divides the
individual sexual act into two steps, while in the present case we have
actually to do with two separate sexual acts.
+ At the same time it appears from the preceding description that the
actual course of the second process of fecundation is somewhat different
in different cases. In some instances (Gleosiphonia) this process takes on
the form of a complete union of two cells; in other cases (Ceramieze &e.)
it would almost appear, as has already been pointed out, that in place of
such an open conjugation the protoplasm (or the cell-nucleus) of one cell
migrates through the separating membrane into the other cell. In this
case the process of fecundation would display exactly the same differences
which haye been recently demonstrated by De Bary (Beitr. zur Morphol.
und Physiol, der Pilze: 4te Reihe) in the fecundation of the Perono-
sporese (Pythium, Phytophthora, Peronospora).
Fertilization of the Floridee. 85
by another *, and appears merely to be a peculiar further
development of this process, which is so widely diffused in
vegetable life, while otherwise sexual fecundation stands
rather isolated among the processes of organic life.
But whether we regard this second act of conjugation in
Glaosiphonia and other Floridez as a sexual act or not, in
any case this process has only been originated within the
roup itself; in the simplest forms it is entirely wanting.
In these (Nemalion &c.) the course of development of the
individual species proceeds as follows :—the vegetative plant
proceeds from the germinating carpospore and develops sexual
cells, after which the fecundated female cell grows upon the
* That by this I by no means wish to assert that the fertilization of
a (female) cell by another (male) cell consists simply in the accession of
fresh nutritive material (as indeed has been formerly asserted) needs no
express declaration. In all cases the male cell, as also the female cell, is
a formed dwng cell-body and not a “ lump” of /ifeless nutritive material.
+ Just as this second sexual act has made its original appearance within
the group Floridez, so, evidently, may it also disappear again in the course
of the development of this group, or instead of it the original first sexual act
may be eliminated. In the first case the course of development of the
species implicated will simply revert to the original form, and such forms
might be hardly distinguishable from the primary simplest forms. On
the other hand, if the first original sexual act disappears, the course of
development of the species must thereby acquire a completely different
aspect. For in this case the formation of spermatia must have entirely
ceased; but, in exchange, either the individual spermatium mother-cells
would develop directly into (simple or branched) male cell-filaments,
which would fecundate the auxiliary cells, while the carpogonia entirely
disappear, or no spermatium mother-cells at all would be formed, but
instead of them the carpogonia would grow out directly into male cell-
filaments (of course without preliminary development of a trichogyne).
The final result, however, would be the same in both cases, namely the
fertilization of auxiliary cells (produced sometimes from terminal cells,
sometimes from joint-cells of the thallus-filaments) by the cells of shorter
or longer, simple or branched cell-filaments.
This elimination of the first sexual act has, however, never been actu-
ally traced in the domain of the Floridez so far as our present observa-
tions extend. It appears, however, to be realized among the Aseo-
mycetes. Here, as already pointed out (p. 81, note), the Collemacez
present such great analogies with the Floridez that one may well assume
that the formation of the fruit is in them brought about in the same
manner as, for example, in the Cryptonemiez. But in other Ascomy-
cetes the above elimination of the first act of fertilization seems actually
to have taken place in the course of development of the species, so that
in these the second sexual act of the Floridez has alone persisted as the
sole sexual act; the mother-cell of the ascogenous hyphz therefore repre-
sents a Floridean auxiliary cell (Ascobolus &c.). Nay (if, indeed, the
extant descriptions really exhaust the actual processes), this second sexual
act appears to have also frequently disappeared, so that the auxiliary cell,
whether distinguished or not by its peculiar form from the other cells of
the hypha, becomes developed apogamically into the spore-fruit.
86 Prof. F. Schmitz on the
parent plant itself into a spore-fruit, which, by the develop-.
ment of carpospores, brings back the whole developmental
cycle again to the starting-point. This is exactly the same
course that is displayed by the development of the Liverworts
and Mosses,—the same sequence of alternating generations as
in those cases. Thus it becomes easy in the course of deve-
lopment of these simplest Florides to recognize the alternation
of generations of the Archegoniata, which, as is well known,
we have accustomed ourselves to regard as the typical mode
of vegetable development, so much so, indeed, that only the
recognition of this alternation of generations in the individual
case explains and renders intelligible the course of develop-
ment in the group of plants in question *,
But these simplest Floridee are approached most closely
and distinctly, as has been shown above, by the other forms
with more complicated fructification, and precisely by this
distinct approximation enable us also to recognize clearly and
distinctly in their development the above alternation of genera-
tions, although it has been here somewhat complicated by the
intercalation of the second sexual act +.
But, independently of this complication, the above typical
alternation of generations makes its appearance quite undis-
turbed and distinctly recognizable in the course of develop-
ment of many Floridee. In many other forms, however,
still further complications of it occur, the vegetative generation
dividing, as in the true mosses, into prothallium and leafy
plant (Batrachospermum &c.). In numerous other forms,
moreover, the tetraspores or bud-formations of various kinds
are developed in the vegetative generation as accessory organs
of increase, whether they are produced upon the sexual indi-
viduals themselves (Cruortopsis cruciata, Duf., Petrocelis Ru-
prechti, Hauck, &c.) or confined to special neutral individuals
(as in most Floridee).
Lastly, in many Floridez there seems to be associated with
the above typical alternation of generations (corresponding to
* That in such an explanation of the course of development of a group
of plants we have to do with a perfectly analogous process, as in the
explanation of the more complicated forms of flowers of Phanerogamia,
which are explained and made intelligible (see Schmitz, ‘ Die Familien-
iagramme der Rhéadinen’) by comparison with other previously known
flowers, will not be hard to see upon consideration.
+ In these forms of the Floridese (Gleosiphonia &c.) we can if we like
distinguish series of three generations, as here the female sexual cell of
the simpler Florideze (Nemalion &c.) is replaced by two cells, the carpo-
gonium and the auxiliary cell, and between these a new third generation
is intercalated.
Fertilization of the Floridee. 87
the alternation of generations of the Archegoniata) * a still
further complication, a regular alternation of sexual indivi-
duals and (single or numerous successive) tetraspore-indivi-
duals being developed. ‘This at least seems to be indicated
with great probability by the fact that, of many short-lived
Floridez, sexual plants are to be met with only at particular
seasons, while neutral plants are to be found either throughout
the year or, at any rate, for a considerable time. Certainly,
however, no instance of such a regular alternation of neutral
individuals and sexual individuals (which in itself might be
regarded as a particular kind of alternation of generations) has
hitherto been demonstrated with certainty by observation.
eT.
The whole process of development of the simplest Floridez
approximates them, as has repeatedly been pointed out in
literature, very nearly to the Chlorophycean group of the
Coleochetez.
In both groups of Alge the entire body of the plant is
composed of ramified cell-filaments with apical growth, and
the joints of which are never transversely divided, and these
are more or less closely pressed together laterally. In both
groups of Algz the sexual cells originate from terminal cells
of these cell-filamentst. Small terminal cells develop from
their entire protoplasm single naked male cells; individual
larger terminal cells become inflated into female cells, and
extend from their apex a longer or shorter thin trichogyne.
But in the Coleochzetez these trichogynes open at the joint;
the protoplasm of the female cell, even before fecundation,
cuts off an unserviceable portion as a directive body, and
evacuates this through the open apex of the trichogyne ;
further, in the Coleocheetez the naked male cells are sponta-
neously motile by means of two cilia; and, lastly, in the
Coleochetez the fertilized ovicell first of all passes into a
resting state, and only after this period of rest develops a cell-
body, which leads to the formation of motile “ carpospores.”
All these last-mentioned points, to which may be added, as
less important matters, the difference of the assimilation
* Pringsheim some time since (Jahrb. fiir wiss. Bot. Bd. xi. p. 6) ex-
pressed an essentially different view of the sexual alternation of genera-
tions of the Floridez. But it would lead us too far to enter here in any
detail into the differences of the two conceptions.
+ In the position of the sexual cells, according to the extant statements
(Pringsheim, in Jahrb. fiir wiss. Bot. Bd. ii.), some species certainly show
a different character, inasmuch as they develop their sexual cells from
joint cells of the thallus-filaments.
88 Prof. F. Schmitz on the
colouring-matters and of the solid assimilation-products, are
of sufficient weight to make an ¢mmediate annexation of the
Florideew to the Coleocheetez impossible; but, on the other
hand, the agreement pointed out between the two forms is so
great that, in the natural system of the Thallophyta, the
simplest Floridezee may be arranged next to the Coleocheetee,
and consequently the whole of the Floridese or Rhodophycez
next to the Green Algee or Chlorophycez *.
On the other hand, I can by no means regard another rela-
tionship of the Floridex, so often dwelt upon of late, the
relationship to the Bangiacez, as so close as is supposed.
This group of Alge which we have lately been accustomed
simply to arrange among the Floridez, on the ground of
Berthold’s observations J, must, in my opinion f, be quite sepa-
rated from the Floridez, and for this reason no reference has
been made to it in the above description. or the establish-
ment of this opinion the most important points in the deve-
lopment of the Bangiaceze which distinguish them from the
Florideze may therefore be briefly indicated here.
In the first place, the construction of the thallus of the
Bangiacee is essentially different from that of the Floridee.
In the Bangiacee transverse division of the joint-cells takes
place in an unlimited degree, and numerous longitudinal divi-
sions of the cells are produced by partitions which occupy the
organic middle line of the cells, neither of which ever happens
in the Floridew. In consequence of this also the thallus of
the Bangiacez, so long as it does not actually represent a
simple cell-filament, can never be reduced to a mere system
of branched fibres. Further, the vegetative thallus-tissue of
the Bangiacez is also always quite destitute of the remarkably
characteristic primary pits of the Florideze, which are formed
in unity in the organic centre of each newly formed dissepi-
ment.
Further, the sexual cells of the Bangiacez are formed from
any cells of the thallus, while in the Floridez they are formed
exclusively from terminal cells of longer or shorter cell-fila-
ments. For the formation of the spermatia, in most Bangi-
acee (Bangia, Porphyra), the individual thallus-cell breaks
up by repeated division by means of dissepiments perpendi-
cular to each other into a pluricellular complex of small cells,
* An opposite opinion has been recently expressed by Falkenberg
(Schenk, Handb. der Bot. Bd. ii. pp. 252, 253) and Berthold (‘ Fauna und
Flora des Golfes von Neapel, VIII. Bangiacez,’ p. 22).
+ Mittheil. aus der zool. Station zu Neapel, ii. pp. 78 e¢ segg., and
Fauna und Flora des Golfes von Neapel, Bd. viii.
¢{ See Schmitz, Chromatophoren der Algen, p. 3, note 1.
Fertilization of the F loridex. &9
which are all alike, and each of which gives origin to a single
spermatium * ; in the Floridex the spermatia always originate
only from superficial cells, terminal cells, or branch-cells of
the cell-filaments of the thallust. In the Bangiacex the in-
dividual thallus-cells, without distinction, become converted
into female cells, extending a short diverticulum on the outer
surface of the thallus, which usually hardly even distantly
resembles the trichogyne of the always terminal carpogonia of
the Floridee}. In the act of fecundation in the Bangiacez,
moreover, the whole protoplasm of the spermatium, except a
very small residue §, passes over into the female cell, which then
retracts the above conjugation-process, and becomes converted
into the fertilized ovicell, without separating off the directive
body which is so characteristic of the Floridee. Lastly,
in the Bangiacew, this fecundated ovicell either becomes
directly the spore (Hrythrotrichia, according to Berthold, @. c.
p. 17), or breaks up by repeated division into a complex of
more or less numerous cells, all of which give origin to single
naked spores; a sporigenous tuft of threads with a sterile
central cell, as in the cystocarp of the Floridez, is here never
produced.
In my judgment, all these peculiarities distinguish the
angiacez very essentially from the Florides||, which, with
all their other differences of construction, display a complete
agreement in the points mentioned. Consequently the Ban-
* In Erythrotrichia, however, according to Berthold (Bangiacez, p. 13)
the spermatia are formed from marginal cells of the individual joint-
cells of the thallus.
+ I would lay less stress upon the further fact that, as Berthold states
(J. c. pp. 12, 18), in the Bangiacee the spermatia always contain formed
chromatophores with pyrenoids | see Schmitz,‘ Die Chromatophoren,’ Xe. ],
while in the Floridez, the spermatia, so far as my present observations
extend, are always destitute of chromatophores.
In passing it may be here once more (see Schmitz, ‘ Chromatophoren
der Algen, p. 39, note 1) indicated that Berthold everywhere confounds
the pyrenoids of the chromatophores with the celi-nuclei, but has over-
looked the true cell-nuclei in the cells of the Bangiaceee. I took up the
investigation of this question again after the appearance of Berthold’s
‘recent memoir, in which his previous statements are simply repeated ;
but this time also I find my above-cited statements about the cell-nuclei
and pyrenoids of the Bangiacez completely confirmed.
t Compare figs. 2, 4, 12, 15, 25, and 24 in Berthold, /. e.
§ See also Berthold’s statements, /.¢. pp. 14 ef seqq.
|| Berthold (Bangiaces, p. 21) thinks, on the contrary, that the charac-
ters of structure and growth of the thallus, with reference to which the
Bangiaces stand quite isolated among the Floridew, but correspond with
the Fe ficiees and Ulotriches (/. c. p. 1), are of no importance with re-
_ gard to the systematic position of the Bangiacez.
_ Ann. & Mag. N. Hist. Ser. 5. Vol. xii. 7
sy
90 Prof. F. Schmitz on the
giacex must at least be separated as a distinct group from the
very coherent group of the Floridea*.
But it seems to me that this peculiar group of the Bangiacez
cannot be placed close to the Floridee as the most nearly
allied group in the natural system. The agreement of the
Bangiaceew with the Floridee depends fundamentally only
upon a few subordinate points. In both groups of Alge the
chromatophores are generally not chlorophyll-green, but
coloured with various shades of red or brown ; in both groups
of Alge the male cells are not motile (so far as is at present
ascertained t); in both groups of Alge the fertilized ovicell
produces, without a period of rest, usually a considerable
number of asexual spores. Nearly all these individual cha-
racters also occur in other groups of Algae (e.g. even the
Dictyotacese likewise possess motionless male cells, for which
reason they have also sometimes been regarded as Floridez) ;
but, in my judgment, they do not of themselves alone establish
an immediate relationship between the Bangiacez and Floridez.
I rather believe, as I have already stated briefly elsewhere f,
that, in the natural system of the Thallophyta, the Bangiacez
are to be placed alongside of the Chlorophycean group of the
Schizogones (Prasiola, Schizomeris, Schizogonium, Palmoglea,
Porphyridium) ; while the Floridee certainly attach them-
selves through the Coleochetex to the main stem of the Alga,
the Chlorophycex §, but are separated by a_ sufficiently
wide gap from these Chlorophycez, and represent a group
sufficiently large, numerous in forms, and peculiarly developed
to be judiciously distinguished as a special, independent section
of the Alge, the Rhodophycee.
The results of the extant investigations upon the fructifi-
* Even the conception of the Bangiaceze as a peculiar branch of the
Floridez, which has branched off from the very base of this great Algal
stem, cannot prevent the otherwise so perfectly harmonious ramification
of ae Algal stem from being seriously interfered with by this very
branch.
+ Hitherto the faculty of free locomotion is ascribed only to the sper-
matia of Erythrotrichia by Berthold (/. c. p. 13). But at present we are
quite without any statements in what manner this locomotion is effected.
Compare herewith the above statements (p. 9, note *) upon the spon-
taneous mobility of the spermatia of the Florideze. :
¢ Schmitz, ‘Chromatophoren der Algen,’ p. 3, note 1.
§ By this arrangement the relationship of the Floridee with the
Bangiaceee, so far as this actually exists, is also expressed, in my judg-
ment, in a perfectly satisfactory manner; for by the approximation of
the Floridez to the Coleochatez the former also join on to the other
groups of the Chlorophyceze, and thereby also to the Bangiacese. Never-
theless the Bangiacew and Floridee are certainly here torn more widely
asunder than has usually been the case of late.
Fertilization of the Floridex. ot
cation of the Floridez furnish also some contributions to the
classification of this section of the Alga.
At present, as is well known, we have only the commence-
ment of a natural system of the Floridee. Our present know-
ledge of the group, which includes such an abundance of
forms, is still too imperfect for it to be possible as yet to esta-
blish a natural system of these Alga. For the present we
must make artificial systems answer our purpose, and these
are now founded entirely upon the structure of the mature
cystocarp (J. Agardh), a preponderant consideration of the
growth of the thallus (Nigeli) having proved to be unsuitable.
A consistent carrying through of this principle of division,
however, frequently tears the nearest allies wide apart (e. g.
Delesseria and Hydrolapathum, Chylocladia and Lomentaria,
Griffithsia and Bornetia, &c.).
For the advancement of the natural system of the Floridee
an exact investigation of the processes in the fructification of
the different individual forms is, in my opinion, essentially
necessary. It would, however, lead me too far to enumerate
here in detail the results which I think I can deduce from my
investigations towards the natural system of the Floridez.
The more general results of this kind have already had ex-
pression given to them in the above statement in the arrange-
ment of the groups. A more thorough-going representation
of them will only be indicated when we have been able to
investigate exactly a far greater number of forms than at
present with regard to their fructification.
EXPLANATION OF THE PLATES.
PEATE L
Fig. 1. Batrachospermum moniliforme, Roth.
(Picric-acid-Hematoxyline preparation.)
Apex of the carpogonial branch with the carpogonium already fertilized ;
trichogyne separated off from the ventral part of the carpogonium,
and the latter sprouting forth laterally, The hypogynal cell
develops beside the older ramified side-branch a new lateral
sprout as the foundation of a new sterile enveloping branch. In
the ovicell, the hypogynal cell, and the branch-cells of both sides
the nucleoli of the cell-nuclei are intensely coloured; within
the trichogyne the protoplasm encloses a number of intensely
coloured granules (derivatives of the cell-nucleus of the female
eell?). x 800 diam.
Figs. 2-4. Chantransia corymbifera, Thur.
(Spirit-material, relaxed in water and coloured with heemateine-
ammonia. )
_ Fig. 2. In the fertilized carpogonium the trichogyne is separated off by
5 means of the membranous stopper within the neck of the tri-
7*
92 Prof. F. Schmitz on the
chogyne. The fecundated ovicell forms an offshoot upwards,
which has already been separated off by a transverse wall.
x 800.
Fig. 3. Next stage of development. Besides the terminal offshoot a
second offshoot is commenced laterally. x 800.
Fig. 4. Further stage of development. x 800.
Figs. 5-7. Scinaia furcellata, By.
(Spirit-specimen.)
Fig. 5. Young carpogonial branch. In the terminal carpogonium the
formation of the trichogyne has just commenced. The hypo-
gynous cell has already formed a marginal cell for the pro-
duction of the hypogynous disk. On the lowest cell of the
carpogonial branch has commenced the sprouting forth of the
enveloping filaments, which subsequently close together to
form the fruit-wall. x 800.
Fig. 6. Four-celled hypogynous disk, with the separated ventral part of
the just fecundated carpogonium. X 800.
Fig. 7. The fertilized ovicell (still furnished at the apex with the closed
neck of the trichogyne) has projected at one side, and developed
an abundantly ramified tuft of ooblastema-threads (the forma-
tion of which by no means proceeds from the cells of the hypo-
gynous disk, as has hitherto been supposed). xX 800.
Figs, 8-15. Gileosiphonia capillaris, Carm.
(Spirit-material.)
Fig. 8. Young procarpium from the side. 6, basal cell of the whole pro-
carpial branch, the penultimate cell (a) of which (the terminal
cell is bent laterally and in the figure concealed by the cell a)
becomes the auxiliary cell. This basal cell bears, as a side-
branch, the three-celled carpogonial branch, the terminal cell
of which has already developed a long trichogyne, while the
hypogynous cell has projected very much on one side (A) and
become abundantly filled with protoplasm. The second cell of
the procarpial branch bears laterally a sterile side-branch.
x 800.
Fig. 9. Young procarpium from below. 4, basal cell of the entire pro-
carpial branch, the joint-cells of which are separated by diffe-
rently inclined transverse walls, and have nearly all formed
sterile lateral branches, while the penultimate cell (a) becomes
the auxiliary cell. The basal cell bears as a side-branch the
three-celled carpogonial branch, the hypogynous cell (h) of
which has here remained much smaller than in fig. 8. x 800.
Fig. 10. Carpogonial branch. In the fertilized carpogonium the ventral
part is separated and has grown out into a single ooblastema-
thread (c), which, near its base, has developed a side-branch (c’).
The ventral part of the carpogonium is completely emptied; the
hypogynous cell (2) has still abundant contents. x 800.
Fig. 11. Auxiliary cell (a) at the apex of the procarpial branch (seen
from below) in open conjugation with the ooblastema-cell (e).
x 800.
Fig. 12. Procarpial branch seen from below. The basal cell (6) and the
neighbouring joint-cell each bear laterally a carpogonial branch,
of which in the figure only the lowest cell (d) is shown. The
auxiliary cell (a) had entered into conjugation with the ooblas-
tema-cell (e), and, after the transference of the whole of the
Wess
Fertilization of the Floridez. 93
a
protoplasm from e, has again closed up as an independent cell
with abundant contents. x 800.
Fig. 13, Apex of the procarpial branch witk the fertilized auxiliary cell a,
from the side. x 800.
Fig. 14. The same. The fertilized auxiliary cell (a) has separated off
outwards the central cell of the spore-complex. x 800.
Fig. 15, The same, further stage of development. The central cell
separates off successive marginal cells. x 800.
Figs. 16-19, Dudresnaya purpurifera, J. Ag.
(Spirit-material.)
Fig. 16. Carpogonial branch, with the apex bent inwards. From the
ventral part of the fertilized carpogonium, which is already
separated off, an ooblastema-thread grows out, and takes a direc-
tion towards the auxiliary cells, which are formed by the ter-
minal cells of short side-branches of the carpogonial branch.
x 800.
Fig. 17. The same. From the ventral part of the fertilized carpogonium
two short ooblastema-threads have grown out and have conju-
gated with certain (one or two) auxiliary cells. One of these
short filaments pushes out a side-branch (c), which grows out
into the neighbouring thallus-tissue. x 800.
Fig. 18. The apex of an ooblastema-thread growing close past an auxi-
liary cell, which here forms the terminal cell of a special branch,
x 800.
Fig. 19. Later stage of development of fig. 18. The growing apex of the
ooblastema-thread has cut off a joint-cell, and this has entered
into conjugation with the auxiliary cell. Afterwards the ooblas-
tema-cell has formed a diverticulum outwards, and separated
this off as an independent cell for the formation of the spore-
complex. x 800.
Figs. 20 and 21. Dudresnaya coccinea, Crouan.
(Spirit-material.)
Fig. 20. The apex of an ooblastema-thread has grown close past an auxi-
liary cell, which here forms a joint-cell in a special branch; the
separated joint-cell of the ooblastema-thread enters into conju-
gation with this auxiliary cell, the two neighbouring cells of
which are also richly filled with protoplasm,
Fig. 21. A further stage of development. The joint-cell of the ooblas-
i tema-thread (ec) has formed outwardly an offshoot (c’), which
fe grows into a side-branch of the ooblastema-thread, and also two
lateral offshoots (¢,e), which apply themselves to the auxiliary
cell externally, and grow round it, to give origin afterwards to
the spore-complex of the cystocarp. x 800.
Fig. 22. Dumontia filiformis, Grev.
(Spirit-material.)
Carpogonial branch, bent into a hook. The formation of the trichogyne
+ has already commenc:d on the terminal carpogonium. X 800.
Puate Li.
* Fig. 23. Calosiphonia finisterre, Crouan.
a (Treated with picric acid and hematoxylin. )
Three-celled carpogonial branch. The lowest cell is much enlarged, like
94
Fig. 24.
Fig. 25.
Fig. 28.
Fig. 27.
Fig. 28.
Fig. 29.
Prof. F. Schmitz on the
an auxiliary cell, but does not function as such. From the
separated ventral part of the fertilized carpogonium three ooblas-
tema-threads grow forth and diffuse themselves into the neigh-
bouring thallus-tissue. x 800.
Figs. 24-27. Naecaria hypnoides, J. Ag.
(Material in spirit. )
Young carpogonial branch (0, d, e) with incurved apex. Its
basal eell (6) bears laterally two branch-cells (a), which subse-
quently develop into auxiliary cells. x 800.
Later stage of development. The cell d of fig. 24 has formed
laterally a branch-cell, 7; the cell e has divided itself by an
oblique transverse wall into the terminal cell g and the joint-cell
e,so that now the cells bdeg form the uncinately incurved
carpogonial branch. x 800.
Further stage of development. The cells d, e, and f have
repeatedly branched and formed a small-celled hypogynous cell-
complex. The cell g has become developed into the carpo-
gonium, and upon this, after fertilization, the trichogyne has
become separated off from the ventral part. x 800.
A still later developmental stage. The ventral part of the fertilized
carpogonium has entered into conjugation with the basal cell (8)
of the carpogonial branch, and now puts forth an ooblastema-
thread (c). ¢, remains of the trichogyne, which is here very
transitory. (The fertilized ovicell also enters into conjugation
with the auxiliary cells @ in fig. 24 through short processes in a
very variable manner, after which fresh ooblastema-threads
originate from the conjugation-cell; these processes, however,
have been omitted from the figure for the sake of distinctness.)
x 800.
Diagram of the cell-division in the procarpium (median longi-
tudinal section) of Chondria, Polysiphonia, and other Rhodo-
mele.
b, cell of the central axis of the procarpial branch; a, un-
paired marginal cell of this, from which in the first place the
curved carpogonial branch, e ee c, grows forth as a terminal
growth, while laterally one or more branch-cells, d, are produced ;
these sometimes (as in Chondria tenwissima) vamify very abun-
dantly, and form a complex of short, closely adpressed, sterile
cell-filaments. ‘The cell aitself subsequently becomes the auxi-
lary cell, and, after the fertilization of the carpogonium (e), is
fertilized by the separated ventral part of this carpogonium,
with which it is in contact at the time of fertilizable maturity.
From the cell @ the sporigenous filaments then shoot forth,
while the cell-series e ¢ e, as well as the sterile tuft of filaments
of the cell d, disappears.
Figs. 29-83. Chylecladia kalifermis, Hook.
(Material in spirit.)
One of the short-jointed cell-filaments, which, meeting at the
apex, constitute the growing vertex of the branches of the
thallus. The joint-cells of this cell-filament branch outwards |
to form the large-celled layer of the wall of the hollow joints
of the thallus. From the branch-cell of the sixth joint-cell there
Fertilization of the Floridee. 95
shoots forth laterally an uncinately curved carpogonial branch.
Drawn without the camera,
Fig. 30. The sixth joint-cell of fig. 29, with the adherent carpogonial
branch, more highly magnified and drawn with the camera.
The newly-formed trichogyne of the carpogonium strongly in-
flated at its base on one side. 6, supporting cell of the carpo-
gonial branch. x 800.
Fig. 31. Young rudiment of a cystocarp seen from the outside of the
thallus. The shaded cells represent the carpogonial branch : ¢,
the ventral part of the carpogonium, the trichogyne of which
was segmented off after fertilization and has perished; the
dotted cell, b, the supporting cell of the carpogonial branch. a,
the auxiliary cell, which bends towards the fertilized ovicell (c)
with a broad conjugation-process ; m, one of the large cells of
the wall of the¢hallus-joint, which has separated off the auxi-
liary cel) (a) externally as a daughter-cell. This entire cell-
group is covered by numerous small marginal cells, which the
neighbouring cells have separated off, and which form the first
rudiment of the future wall of the cystocarp. x 3800.
Fig. 82. An auxiliary cell with a broad curved conjugation-process, seen
from the side. x 800.
Fig. 33. Carpogonial branch with fully-developed carpogonium, A sper-
matium has conjugated with the apex of the trichogyne. x
800.
Fig. 34. Callithamnion gracillimum, Hary.
(Material in spirit.)
Procarpium. On one of the uppermost joint-cells of a completed branch
of the thallus there stand in a whorl the sterile branch-cells (6),
the two auxiliary cells (a), one of which has also segmented off
a cell (d) on its outer side, and the three-celled carpogonial
branch (ee c). x 800.
Fig. 35. Pterothamnoon plumula, Nig.
(Osmic acid and hzmatoxylin preparation.)
Procarpium. The basal cell (6) of a frond-pinna bears upon one side the
curved four-celled carpogonial branch, and on the other side the
auxiliary cell (a). The latter has curved over towards the upper
surface of the basal cell, and so comes in contact with the
ventral part of the carpogonium, which has already separated
from the trichogyne, as the fertilized ovicell, by means of a very
short and dense closing-plate (p). x 800.
Fig. 36. Polysiphonia atrorubescens, Grev.
(Picric acid and hematoxylin preparation.)
Young procarpium in median optical longitudinal section. On the joint-
cell 6 of the central axis the unpaired marginal cell @ has seg-
mented off a terminal offshoot, which already consists of two
cells, and by the development of further transverse walls in the
terminal cell will grow into the curved carpogonial branch of
the fertilizably mature procarpium (fig. 28). x 800,
96 Dr, F. Vejdovsky’s Contributions to the
Figs. 87 and 38. Plocamium coccineum, Lyngb.
(Spirit-material.)
Fig. 37. Young fruit-rudiment at the period of fertilizable maturity. A
spermatium has conjugated with the extended trichogyne.
x 150.
Fig. 88. Longitudinal section through a still younger fruit-rudiment, the
apex of the trichogyne of which has not yet got free, An in-
ternal tissue-cell (a) has developed, as a secondary side-branch,
a three-celled carpogonial branch (e ec), and itself become de-
veloped into the auxiliary cell, extending a conjugation-process
towards the ventral part of the carpogonium. The trichogyne
is much inflated in aclavate form above the neck before, breaking
through the surface of the thallus with its dense cuticle, it pro-
trudes as a long thin hair. xX 400. *
Fig. 39. Caulacanthus ustulatus, Kiitz.
(Spirit-material.)
Longitudinal section through a young fruit-branch ; mm, central axis.
A side-branch of this central axis bears laterally on a joint-cell
(d) the carpogonial branch (e@ ec). The lowest cell of this
grows into a sterile rhizoidiform thread. The uppermost cell
has developed into the carpogonium ; its ventral part has be-
come segmented off after fertilization, and has grown out
into a single ooblastema-thread, which, branching abundantly,
coils itself about the central axis. At X originated another
ramified side-branch of the ooblastema-thread, which spread
out upon the under surface of the central axis, but has been
omitted in the figure for the sake of distinctness. x 400,
X.—Contributions to the Knowledge of the Freshwater
Sponges. By Dr. F. Vrspovsky, of Prague. With Re-
marks by H. J. Carter, F.R.S. &e.
[Plate VI.]
THE above is a translation of the Title of a memoir commu-
nicated by Dr. F. Vejdovsky to the Society of Science in
Prague, on the 12th October last, and since printed in the
Bohemian language, with the following Résumé in German :—
RESUME*,
In my monograph of the freshwater sponges of Bohemiat
I left two questions, among others, open, to be answered by
subsequent investigations.
The first question relates to the multiform ‘ Ephydatia
* Translated from a separate impression of the Memoir sent by the
author to Mr. H. J. Carter, F.R.S.
+ “ Revisio Faunze Bohemice. Pars I. Die Susswasserschwamme Boh-
mens.” Von Dr, Franz Vejdovsky in Prag (mit 3 lithographirten Tafeln).
Abhandl., d. k. Bohm. Gesellsch, der Wiss. Folge 6, Band xii.
Knowledge of the Freshwater Sponges. 97
Miillert,” of which I distinguished ‘ Forma A,” “ Forma B,”
and ‘‘ var. astrodiscus.” From observations made recently
from fresh materials on ‘‘ Forma B,” this must be recognized
as a distinct ‘ good” species, for which I propose the name
of Ephydatia amphizona.
The other question relates to the external parenchymatous
envelope of the gemmules. I had previously found this in
most of the indigenous species—Luspongilla lacustris, E. jor-
danensis, and Ephydatia fluviatilis. It remained still unde-
cided whether corresponding envelopes were present on the
gemmules in “ Hphydatia Miilleri” and Trochospongilla
erinaceus. r
Having been able during the last vacation to investigate
the above-mentioned forms in the fresh state, I can now fur-
nish satisfactory information upon this question also.
I. Ephydatia amphizona (syn. H. Miillerit, Forma B) was
obtained from the Juvorka brook near Sobeic (Ostromer),
with the same characters that I have described in my mono-
graph. Nevertheless the structure of the gemmules is quite
different, and divergent from all allied forms. Fig. 2 shows
anearly median longitudinal section through a gemmule. In
this we see the following layers :—
1. Externally, an outer layer of amphidisci (a), which pro-
ject with their columns and distal terminal disks freely from
the parenchymatous layer (6), while the proximal terminal
disks are inserted into the upper parenchyma.
2. A tolerably thick parenchymatous layer (6) contains in
its base the other layer of amphidisci (c), which is closely
applied to
3. The brown chitinous membrane (d).
4, The inner space of the gemmule contains the germinal
corpuscles (e@).
Consequently Eph. amphizona is especially distinguished
by the double layer of amphidisci in the parenchymatous en-
velope of the gemmules from Eph. Miillert, var. astrodiscus,
which, as I have recently convinced myself, possesses only a
single layer of amphidisci in a feeble parenchymatous layer.
As this latter form is also characterized by the form and habit
of the exclusively hispid skeleton-spicules, it may be indicated
by Lieberkiihn’s original name, Ephydatia Miiller’*.
Whether the form indicated in my monograph as “ Eph.
Miillert, Forma A,” and as characterized by the peculiarly
formed amphidisci, is to be regarded as a variety of the above-
* [M. mirabilis, Retzer, presents ‘a oe armature of amphidisci,”’
according to Marshall, in a paper of which a translation will appear in
our next number.—Ep. |
98 Dr. F. Vejdovsky’s Contributions to the
mentioned species, or as a distinct species, I cannot at present
decide with certainty.
II. Trochospongilla erinaceus was found in cushion-like
stocks in a deep side-water of the Elbe, near Neratovic. The
inferior layers of the lamelle contain extraordinarily nume-
rous gemmules, seated close together, as shown in fig. 8. The
longitudinal section through a gemmule (fig. 5) presents the
following interesting characters :—
1. The inner chitinous membrane is very thick and layered
(fig. 5, c).
2. The very depressed amphidisci (+) are in direct con-
nexion with the chitinous membrane.
3. The layer representing the parenchymatous envelope of
the other Spongillidzs is peculiarly modified in T'rochospon-
gilla. When the surface of the gemmule is examined it
appears to be composed of five- or six-sided prismatic spaces
(fig. 4). Longitudinal sections, however, show that this
layer consists of tall hollow columns (fig. 6), which are divided
by transverse walls into a number of air-chambers. The
walls are firm, not very flexible, shining, and probably com-
posed of a chitinous substance. ‘The interior space becomes
filled with air.
The whole of this outer envelope evidently forms an aero-
static apparatus as a means of the more ready transportation
of the gemmule, and perfectly corresponds to the natatory
rings of the statoblasts of the freshwater Bryozoa.
Whether the North-American species with smooth-edged
amphidisci, Meyenia Leidii and MM. gregaria, possess corre-
sponding envelopes, must be ascertained from fresh material.
I cannot detect the air-chamber layer in the dry Meyenia
Leidii transmitted to me for comparison by the kindness of
Mr. H. J. Carter.
Ul. Ephydatia fluviatilis, aut., I have also obtained from
the neighbourhood of Sobeic (Ostromér), out of stagnant
water, and found that it agrees perfectly in its characters with
the sponges of the same species that I have described in my
monograph.
By the kindness of Mr. H. J. Carter also, [have been enabled
to compare the English specimens of this species with our
indigenous ones, and from this comparison it appears that the
English “ Meyenia fluviatilis, Carter,” is identical with my
Ephydatia fluviatilis.
EXPLANATION OF PLATE VI.
Fig. 1. Ephydatia amphizona, n. sp.; gemmule very slightly magnified.
Fig. 2. The same species. A nearly median longitudinal section (magn.
Knowledge of the Freshwater Sponges. 99
Zeiss V. oc. 2, obj. C). a. External amphidiscus-layer; 0.
Granular parenchymatous layer; c. Inner amphidiscus-layer ;
d. Chitinous membrane ; e, Germinal corpuscles.
Figs, 3-6. Trochespongilla erinaceus, Ehy.
Fig. 3, Arrangement of the gemmules in the intermediate layers of the
lamelle. a, Air-chamber layer, representing the natatory ring
of the statoblasts of the freshwater Bryozoa; 6. Chitinous cap-
sule ; c. Aperture of the gemmule.
Fig. 4. Structure of the air-chamber layer on the surface.
Fig, 5. Median longitudinal section through a gemmule (magn. Zeiss V.
oc. 2, obj. C). 0. Aperture; a. Air-chamber layer; 6. Amphi-
discus-layer; ¢. Chitinous capsule ; d. Germinal corpuscles.
Fig. 6, Longitudinal section of the air-chamber layer (magn. Zeiss, oc. 2,
obj. EK). a. Air-chambers; 6. Amphidiscus-layer.
Remarks by H. J. Carrer, F.R.S. &e.
The foregoing translation of a “Résumé” in German,
which is appended by Dr. Franz Vejdovsky to his “ Contribu-
tions to the Knowledge of the Freshwater Sponges,” read at
the Society of Sciences in Prague on the 12th of October last,
and subsequently published in the Bohemian language, is
of much interest, because it points out additional instances of
what has been seen in other treshwater sponges, viz. Parmula
Batesii, Spongilla nitens, and S. alba (‘ Annals,’ 1881,
vol. vii. pp. 99, 89, and 88, pl. v. figs. 1 and 3, respec-
tively), together with a new variety in structure. ‘Thus, in
his Ephydatia amphizona (syn. Eph. Miillert, forma B) we
have an illustration (Pl. VI. fig. 2) of what occurs in the sta-
toblasts of the two former, viz. a layer of statoblast-spicules
on each side of the “ crust” ( Annals,’ 7. c. p. 83), here com-
posed of the “ microcell-structure” (¢b. 7b. pl. v. fig. 2, a) ;
while in his Trochospongilla erinaceus (Spongilla erinaceus,
Ehr.) is another example of what occurs in Spongilla alba
(‘ Annals,’ 2. c. p. 88), viz. a mixture of spicules with the
“ microcell-structure,” but in a new form,, that is, instead of
the crust being composed of microcell-structure charged with
statoblast-spicules only, as in Spongzlla alba, it is made up of
comparatively large cells, like that in Spongilla nitens, &c.,
(‘ Annals,’ Z. c. pl. v. fig. 3, ¢), arranged in a columnar form,
but traversed by full-sized skeleton-spicules of the species, and
finally united to a layer of birotulates which are fixed to the
“ chitinous coat” (Pl. VI. figs. 5 and 6), yet so tenderly
that, whether on account of this or the intermingling of the
ends of the skeletal spicules which project beyond the cell-
structure with the rest of the sponge, it very often happens
that, in endeavouring to extricate the whole statoblast, the
cellular crust &c. remains, while the chitinous coat and its
layer of birotulates (amphidiscs) come away without it.
100 Mr. H. J. Carter on Freshwater Sponges.
At least this is the result of my examination of several of
the statoblasts taken from specimens of this sponge which
Dr. Vejdovsky kindly sent me; but of course I am aware
that in his illustration (PI.VI. fig. 5) the s¢mple fact of the
arrangement of the parenchyma around the statoblast in hexa-
gonal columns perpendicularly to the layer of birotulates on
the chitinous coat alone is represented.
As yet I have been able to see this arrangement in frag-
ments only, partly from the cell-structure being so intricately
traversed by the skeletal spicules of the species and partly
from its diffuse extension here and there beyond the surtace of
the capsule, recalling to mind that which is seen in Spongilla
fragilis, Leidy=S Lordii, Bk., to which Mr. Potts of Phila-
delphia directed my attention in the slide of this species which
he kindly sent me in 1881.
Being better informed now on the subject than I was when
I stated that Spongilla erinaceus, Khr., of central Kurope was
‘identical’ with Meyenia Leidii, Bk., of Pennsylvania in
North America (‘ Annals,’ 1883, vol. xi. p. 3831), T am now
able to point out that they are different, viz. that whereas the
crust in Meyenia Letdit is composed of microcell-structure
enveloping the layer of birotulates which is fixed to the chiti-
nous coat and separately surrounded by a capsule of smaller-
sized spicules than those of the skeleton, although of the same
form, viz. more or less spined and abruptly pointed, that of
‘rochospongilla erinaceus is surrounded by the comparatively
large-cell structure first pointed out by Dr. Vejdovsky (/. ¢.),
traversed by the long, fusiform, spined, sharp-pointed skeletal
spicules of the species, as above described. Jn the American
variety (for we can hardly call the differences specific, although
it should be considered distinct and still retain its original
name) the crust is sharply defined and separated from the sur-
rounding spicular layer, while, as we have seen, in Trocho-
spongilla erinaceus it is traversed by the skeletal spicules of
the species which, with their outer points and diffuse cellular
parenchyma here and there, intermingle with the surrounding
tissue of the sponge. As I have before stated, however
(‘ Annals,’ . c. p. 331), the first specimen of Meyenia Letdit
from the Schuylkill river, kindly sent me on a slide by my
friend Mr. Potts, bears, in addition to the smaller spicules
around the statoblast above mentioned, others, viz. skeletal
ones, almost identical with those of T’rochospongilla erinaceus,
thus still keeping up the almost endless variety in character
of the Spongida generally. Other peculiarities of Trocho-
sponyilla erinaceus are the grey instead of the usual yelk-like
colour and substance of the germinal contents of the statoblast ;
Mr. H. J. Carter on Freshwater Sponges. 101
the larger size of the “spherical cells” containing the germs, and
their comparative tenacity, so that even in the broken section
after desiccation these contents present a granular appearance
instead of the usual homogeneity, from the unruptured state
of these cells.
Through the great kindness of Dr. Vejdovsky I am in
possession not only of a copy of his publications on the Fresh-
water Sponges of Bohemia, but of specimens mounted and
unmounted of Ephydatia amphizona and Lrochospongilla eri-
naceus, so that I am able to confirm the interesting facts
which he has stated and illustrated respecting these sponges.
While on this subject, I would add that on the 29th of
November last I received for examination some specimens of
the bottom-sediment of some lakes near Pictou, in Nova
Scotia, from Mr. A. H. McKay, B.A., B.Sc., Principal of the
Pictou Academy ; and in that of “ Karltown Lakes” I found,
besides spined skeletal spicules, birotulates identical with
those of Meyenia Leidii, together with others like those of
the North-American form of Spongilla lacustris and those of
the statoblasts &c. of Mr. Potts’s ? Meyenta cratertformis, so
that, in a geographical point of view, the freshwater species
of Pennsylvania are in all probability to be found also in
Nova Scotia.
P.S.—Since the above was written I have also received from
Mr. Henry Mills, of Buffalo, N. Y., a letter dated 25th De-
cember last, in which he states the same fact of some of the
North-American freshwater sponges as that from Bohemia,
described and illustrated above by Dr. Vejdovsky under the
name of Ephydatia amphizona. Mr. Mills’s letter is accom-
panied by two specimens, viz. one from Ischua Creek, Catta-
rangus Co., N. Y., and the other from Bear Creek, Iowa, in
which I have been able to confirm what he has stated. He
also notices a third locality, viz. the Calumet Creek, sixteen
miles south of Chicago, adding that “ all these have the bi-
serial arrangement of the birotules in the outer coat of the
statoblast.”’
Of what specific value the bi- and triserial rows of biro-
tulates may be I am not prepared to say, as I find them also in
the statoblasts of Meyenia fluviatilis of Bombay, wherein the
crust of those that are fully developed is very thick, and often
shows three birotulates end to end, although not so numerous, so
regular, or so uniform in arrangement as in the innermost row ;
indeed [ should say the outer ones were scattered, particularly
those of the outermost row—recalling very much to mind the
102 Prof. G. Lindstrém on the
enormously long birotulates of Mr. Potts’s Heteromeyenia angy-
rosperma (‘ American Naturalist,’ Dec. 1883, p. 1296, fig. 13,
e, f), in which one set are very long indeed and the other
comparatively short; thus the former project much beyond the
latter on the statoblast, which renders its surface correspond-
ingly irregular. Nor is the size alone of the cells of the par-
enchymatous structure of any use specifically, as I find from
a variety of Spongilla fragilis just (12th January) received
from Mr. Potts, in which there are all sizes mixed together
like the bubbles in froth.
XIL—A Reply to the Remarks of Prof. Duncan on a Paper
entitled ‘* Contributions to the Actinology of the Atlantic
Ocean.” By G. LINDSTROM.
Tn the ‘ Annals and Magazine of Natural History’ for De-
cember 1883, Prof. Duncan has thought proper to criticise
a paper of mine which was published in 1877. Prof. Duncan,
who during the interval of seven years “ felt no disposition ”
to “reply” to me, now finds it necessary not only to “re-
consider’’ my paper, but to use language by no means con-
sistent with the quiet tone that ought to prevail in scientific
discussions.
Prof. Duncan seems to think* that I, convinced of my
errors, especially through his writings, ought to have re-
canted my statements long ago, and admitted that they were
erroneous. I have not done so—first, because I am not con-
vinced that I am wrong to the extent Prof. Duncan supposes ;
secondly, because I could not admit facts solely upon the
dictum even of Prof. Duncan himself; thirdly, because I have
not had occasion to revert to this matter specially until now,
when I am compelled by Prof. Duncan’s uncalled-for attack,
much against my will, to turn from more urgent occupations.
Premising that a great part of his criticism consists of a
recapitulation of remarks already made by Pourtalés and
Moseley, and with which zoophytologists have been long
conversant, I shall now try to reply to the points put forward as
Prof. Duncan’s own animadversions.
Caryophyllia Pourialesii, Duncan.—I was led to give this
* “JT hoped that time would bring some remarks from him..... .
These researches [of Duncan, Pourtalés, and Moseley] might have
modified Prof, Lindstrém’s views; but as theydo not appear to have done
so,” &e, (Ann. & Mag. Nat. Hist. Dec. 1883, pp. 361, 362).
Actinology of the Atlantic Ocean. 103
name to my specimens, which are in a fine state of preserva-
tion, on account of the description, and especially the fig. 10,
pl. xlii., in Prof. Duncan’s first ‘ Porcupine’ memoir. Though
not quite so clear as might be desirable, this figure is far more
instructive than those given later; and I may ask any one
who chooses to compare my figure in ‘ Actinol. Atl. Ocean,’
pl. i. fig. 4, with that above mentioned, whether I was not
justified in referring the North-Atlantic coral to this species.
As to the pali, Prof. Duncan seems himself to admit their
partial deficiency. After speaking (Ann. & Mag. Nat. Hist.
Dec. 1883, p. 362) of “the irregular pali,” he says, “ they
are especially visible when the columella is small.” This
seems to imply that the columella varies in size, and that
when the columella is large the pali are not so visible. But
I cannot make out whether this means that they are deficient
or that they are hidden from view. ‘The former is probably
the case, as it is stated in Duncan’s second ‘ Porcupine’
memoir, p. 238, that “the pali.... are well developed
when the columella has only one twist, and are less so when
this structure is more complicated.” The accompanying
figures 4 and 7 on pl. xlii. do not show any distinct pall.
Moreover it may be questioned whether what have been called
pali in several of the Caryophylliw and others are really
structures corresponding to the first definition given by Milne-
Edwards in Ann. d. Sciences Nat. 1848, vol. ix. p. 80. If
we take for granted that they are to be found “ entre les
cloisons et la columelle”’ and independent of either, as is
shown in pl. iv. fig. 1 (Caryophyllia cyathus) of Milne-
Edwards’s memoir, those occurring in Caryophyllia Smithii
are not pali, as they are in direct continuation of the septal
«lamina and formed by a deep vertical incision near the interior
border of the latter, being in fact nothing but the innermost
part of the septa*. It may be that such false pali occur
now and then in specimens of Caryophyllia Pourtalesti; and
one of my specimens shows an irregular indentation at the
interior end of only one septum. Now, if Caryophyllia
cyathus is provided with real pali, and other species, such as
C. Smithii and C. Pourtalesii, have only false pali, I
think this is a sufficient reason for separating them into
different genera. I have never regarded C. Pourtalesii
as a doubtful species, but I have only questioned the pro-
* Unfortunately Milne-Edwards, in the continuation of his description,
also unites with the independent structures, which alone are true pali,
those lobes or “ dentelures” which so often occur on the axial end of the
septa and are an integral part of them. But in reality a distinction
must be made between the two.
104 Prof. G. Lindstrém on the
priety of placing it in the genus Caryophyllia; and Prof.
Duncan himself seems also now to be vacillating on this
point, as he (Ann. & Mag. Nat. Hist. Dec. 1883, p. 363)
says that it is a member of the Caryophyllia “ group”
which of course is something different from the “ genus”
Caryophyllia.
Paracyathus thulensis I did not implicitly propose as a
synonym, but with a doubt, as plainly shown by the mark of
interrogation. J admit, however, that it might have been
better not to have mentioned it at all.
Leptocyathus Stimpsont, Pourtalés.—There cannot be the
slightest doubt that my specimens are identical with those of
Pourtalés, who kindly sent me typical specimens for compa-
rison. J have mentioned this in my paper. Moreover,
Pourtalés, in the‘ Blake’ Report for 1878, p. 201, confirms my
determination, and says, “In the Florida Straits .....
quite a number were dredged of the more elongated shape,
which Mr. Lindstrém has tound to be the prevalent form in
the Eastern Atlantic.”’ I then failed, and I still fail, to detect
any pali, or any thing at all deserving that name, in them ; and
Pourtalés also says that those of a higher order are not very
distinguishable from columellar processes. He, moreover,
admits that the pali may be wanting in smaller specimens,
when he says that he found them “ quite distinct in large
specimens in front of the tertiaries.”” It seems, then, that if
pali exist at all they are highly variable, and occur in some
specimens, while they are deficient in others. Nor are the
pali at all clearly indicated in the figure given by Pourtalés
in ‘ Deep-sea Corals,’ pl. iii. fig. 2.
Leptocyathus? halianthus, Lindstrém.—Prof. Duncan says
that either the description or the figure is wrong, as they con- ~
tradict each other. Both are correct, though I admit that the
former might have been more complete, and that there might
have been one figure more. The case stands as follows :—
There are in the Swedish State Museum two specimens
dredged up alive, during the expedition of H. Swed. M. ship
‘Eugenie,’ off Cape Frio, both broadly attached to the valves
of a Pecten. One of them is the original of the figure 9 of
pl. i. in my paper, and there only the tertiary septa coalesce
with the secondary ones. But in the other specimen those
of the fourth and the fifth orders are united to those of the
third in one moiety of the coral, while in the opposite
moiety they are straight and do not coalesce at all. This,
taken together with the former specimen, shows what a highly
variable character this coalescence of the septa is. ‘There are
no pali. The coste are large and prominent where they are
)
it
1
e
iy
J
YT een
E
Actinology of the Atlantic Ocean. 105
not covered by a thin epitheca. It is true that the coral
approaches very nearly to what I regarded as a variety of
Deltocyathus Agassizii, pl. i. fig. 16.
Deltoeyathus Agassizii, Pourt.—Seeing the many different
forms which have been lately grouped under this species, and
comparing the figures of Milne-Kdwards as well as original
specimens from Monte Gibbio of D. déalicus, I find that it
is by no means finally settled whether D. Agassizii is to be
merged into D. dtalicus or not.
I think Prof. Duncan makes too much of my having
dared to hint at the possibility that his Sabénotrochus apertus
might be a variety of D. Agassiz’. ‘ We do not want con-
jectures,”’ he exclaims; and yet everybody who has consulted
his writings must have noticed how freely he indulges in con-
jectures himself. Thus, for instance, Pourtalés remonstrates
(Bull. Mus. Cambr. vol. vi. no. 4, p. 110) :-—‘ Prof. Duncan’s
supposition that the office of the pali is to support an extra
circle of tentacles is not borne out in this species, nor in any
other paliferous coral of which I have had the opportunity of
examining the polyp.” Further on Professor Duncan says,
“Certainly the coste and pali of Trochocyathus Rawsoni
remove it entirely from Deltocyathus. . . . After seeing Lind-
strém’s criticism Pourtalés still retained the form in the genus
Trochocyathus ;” but Prof. Duncan omits quoting the follow-
ing statement of Pourtalés (Bull. vol. v. no. 9, p. 199) :—
“There is no possibility of identity of this species with D.
Agassiziz, as supposed by Lindstrém, though there is very
little doubt that the two genera can scarcely be kept separate.”
In fact the numerous small, discoid, Fungia-like corals yet
await a final arrangement by somebody who shall have access
to all species described and to large numbers of specimens.
This is evident when we see such zoophytologists as Pour-
talés and Duncan give such conflicting opinions.
Flabellum laciniatum, Philippi.—Considering the many
different forms of Deltocyathus which have been comprised
under one and the same species, I find it less unreasonable to
unite such forms as Flabellum alabastrum and LI, laciniatum.
My specimen, dredged up from 200-300 fathoms off the
Azores, from its deeper coloration and the nearly straight
edges of the septa, may be regarded as a variety of the
North-Atlantic species. Prof. Moseley also says, ‘ I cannot,
however, tell what amount of variation a long series of speci-
mens might show.”
Schizocyathus jissilis, Pourt.—On comparing the figures
given by Pourtalés and myself, there can be little doubt that
we have described the same species. ‘The presumed discre-
Ann. & Mag. N. Hist. Ser. 5. Vol, xiii. 8
106 Prof. G. Lindstrém on the
pancies may be reconciled in the following manner. We have
given different values to the septal orders, viz. :—
The primary septa of Pourtalés are my tertvary septa.
The secondary _,, 4 o primary 5,
The tertiary iy, 55 3 secondary 4,
Those large septa which are enclosed by a pair of other
septa I regarded as the primaries. I was led to this by what
I had learnt from Balanophyllia Goésti (Actin. Atl. Ocean,
pl. iii. figs. 40-42), in which it is evident that the primaries
are enclosed within two of the next succeeding order, that is
the secondary, so that there are two secondaries for each of
the primaries, or in all twelve, as seen on plate ii. fig. 41, in
Actin. Atl. Ocean. On comparing smaller and larger speci-
mens of Schizocyathus I cannot but think that I was right in
arranging the septa as I had done. The primaries of Pour-
talés are easily recognizable by their position inside the distinct
line which is so clearly visible on the wall outside, and along
which the coral splits. Now in the smallest specimens,
scarcely 1 millimetre in length, what I have called primaries
are the largest septa developed, and the primaries of Pour-
talés, my tertiaries, are just beginning to appear.
Prof. Duncan further says (p. 367), ‘that there are no septa
in Lindstrém’s figure (pl. 1. fig. 27) in the position of the
primaries of Pourtalés.’”’ It is true that they are not visible
in the specimen figured, because their growth has ceased or is
retarded, as is shown on the same plate (fig. 26). But I have
other specimens, in which these septa, though short, are as
plainly seen on a level with the others in the calicle as in the
original specimen of Pourtalés.
As to my remark on the composition of the septum of three
distinct strata or lamine, one central enclosed within two
lateral ones, Prof. Duncan makes a quasi-quotation from my
paper, from which it might be implied that I have contradicted
myself or partially admitted the truth of the old opinion.
After briefly stating my views he adds that, ‘ He [Lindstrém] —
candidly admits that the two lamin are to be seen in some
fossils”” (Ann. & Mag. Nat. Hist. Dec. 1883, p. 367).
I said, consistently with my view of there being three
structural elements in the septum, that old and weathered
specimens look just as if they had septa consisting only of
two lamine; but this is only owing to the central or original
lamina having been removed by solution and its place left
empty (Actin. Atl. Ocean, p. 17). It is just this structure of
the septum which is one of the chief points that link the
Actinology of the Atlantic Ocean. 107
Recent and Mesozoic corals with the Paleozoic forms, in
which the same structure is often retained and easily enough
distinguished.
Stenocyathus vermiformis, Pourtalés.—Prof. Duncan con-
tends “ that it is hardly conceivable that they [Pourtalés and
Lindstrém] are treating of the same species.” I have now,
when I write this, and had also when I described the species,
three specimens of S. vermiformis, sent from Pourtalés him-
self, named in his own handwriting Canocyathus? vermi-
Sormis, which was the first denomination given to the species.
I cannot but see, even now on renewed examination, that his
specimens and mine belong to the same species. Prof. Dun-
ean, who must have seen so many specimens of living and
tossil corals, ought certainly to be aware of their great varia-
bility—how some specimens take the shape of a regular cone,
while others of the same species are crooked and vermiform ;
and consequently he ought not to be so much astonished, as he
seems to have been, that I have placed turbinate and vermi-
form corals together. It is indeed more easy to reconcile my
specimens with those of Pourtalés and with the fig. 12, pl. i11.,
in his ‘ Deep-sea Corals,’ than to identify the figures 1 and 2,
pl. i., in the same memoir with those given on pl. in. figs. 11
and 12. Judging from these it really seems as if there had
been two different species, one of which tallies with those
described by me and with the specimens sent from Pourtaleés.
The latter author, in ‘ Deep-sea Corals,’ p. 92, explanation of
figures, says also that the calicle of fig. 12, pl. ill., is more
common than that of pl. i. fig. 2. Moreover, I have now made
a section near the wall of one of the specimens sent by
Pourtalés, and it does not in any way differ from fig. 9,
p. 20, in my paper. It depends, of course, much on the state
of preservation of the coral whether this dissepimental trellis-
work is left or not, as in the lower and older parts of the
coral, where it may have disappeared through solution or
other changes.
At present my time and the materials at hand do not admit
of my entering further into the questions raised by Prof.
Duncan’s criticism, or attempting to settle finally some of the
moot points, which would require more figures and more re-
search than I can now bestow upon them. I have only
defended my statements and views against him, and now
leave to the unbiassed reader to decide on which side the
“very hasty criticism ”’ lies.
S*
108 Prof. F. J. Bell on the
XII.—On the Species of Pseudoboletia.
By Prof. F. Jerrrey Bex, M.A.
M. pre Lorton has just added another to the many services he
has rendered to the students of Echinoderms by the publica-
tion of the first part of a ‘ Catalogue raisonné des Echino-
dermes recueillis par M. V. de Robillard 4 Vile Maurice ” *, in
which the Echinoidea are discussed. Among the forms
found was the species of Pseudoboletia long since described by
Michelin as Toxopneustes indianus ; of this a full and elabo-
rate description is opportunely given, and the concluding
paragraph of discussion ends with the sentence—‘‘ M. Bell
(loc. cit.) a pris, je crois, le Pseud. indiana pour le Ps. granu-
lata et vice versa; le Ps. granulata n’a jamais encore été
envoyé de Maurice, 4 ma connaissance du moins.”
It is perfectly true that M. de Loriol’s description of P.
indiana applies to specimens which have been labelled by
me P. granulata.
The first question which arises, on this matter of fact being
settled, is what kind of proof can one or the other adduce in
favour of the view which he holds; as M. de Loriol says he
has a specimen from Réunion which “ correspond trés exacte-
ment 4 la description de Vindividu type de Michelin, qui pro-
vient également de la Réunion, et il est identique aux exem-
plaires de Maurice,” it is clear that M. de Loriol is right, and
that I am wrong.
I should not trouble the readers of this Journal with a
demonstration of M. de Loriol’s exactness (which has been
proved by works too numerous to stand in need of any testi-
monial from me), or have thought it necessary to expose in
such detail the steps by which I convinced myself of having
been in error, were it not that, on examination of the whole
question, I found that the more important matters on which
1 have now to enter could be best introduced in the manner
here adopted.
There can be no manner of doubt that there are two species
now in existence which belong to the genus Pseuwdoboletia ;
one of these is exactly known from the description and
figures just published by M. de Loriol—P. indiana. Of this
species specimens were presented to the British Museum in
1842, by Lady Frances Cole; and forty years later a speci-
men, covered with spines, was purchased by the Trustees
from M. de Robillard; these specimens have been hitherto
* Mém,. Soe. Phys. Hist. Nat. Genéve, xxviii. no. 8.
=y.
Species of Pseudoboletia. 109
labelled “ P. granulata,” but this shall be changed to P.
indiana.
The other species was first described by Mr. Alexander
Agassiz in 1863 as Boletia granulata, and was thus defined :—
“Remarkable for its comparatively long spines. 'Tubercles
uniform in size, very closely crowded together. Sandwich
Islands.” Ten years later a rather more detailed description
was published in the ‘Revision of the Echini’ (p. 455),
which agrees very well with the specimens which, in the
British Museum, have been hitherto labelled P. granulata,
save that I should not say of them that “the test is depressed,
quite flattened both above and below, slightly conical, regu-
larly arched in profile,” as Mr. Agassiz’s type specimens from
’ the Sandwich Islands appear to be. As the description given
by the author of the species Boletia granulata corresponds, so
far as it goes, with that given by M. de Loriol of Yozxo-
pneustes (Pseudoboletia) indiana of Michelin, granulata and
indiana would appear to be synonymous specific terms.
To come to the second species: that there is such a second
species the collection of the British Museum is sufficient to
bear witness, and we have specimens which go some way
towards indicating the area of its distribution, from the
Philippines and from Torres Straits. With regard to this
species there should be less chance of error than with the
other : firstly, because the student will not here be dependent
on the poor services of one who still has much to learn *, but
will have a specimen named for him by one whose services
were solicited by a great nation containing not a few com-
petent zoologists, and who, as is well known, is the greatest
living authority on the Echinoidea—well, the specimen
named by Mr. Agassiz for the ‘ Challenger’ collection is
called P. ndiana ; secondly, this species is not one that can be
easily mistaken, on account of the curious dark brown patclies
on its test and on its spines. The species with patches is
identical with the P. ¢ndiana from the ‘ Challenger,’ and the
description given in the ‘ Revision’ of P. indiana applies to the
specimens so labelled by me in the British Museum.
_ Lhave, I trust, made it clear that, in the absence of Michelin’s
or of Agassiz’s type specimens of the two species, I had (a)
the next best thing—a specimen named by Mr. Agassiz, the
namer of one of the two recognized species; (@) that I had
only the incomplete definitions of Michelin or Agassiz, in addi-
tion to the information given in the ‘ Revision’ itself; or, in
other words, I was, I submit, justified in taking the ‘ Re-
vision’ as my guide.
* Cf. P.Z. 5. 1880, p. 36.
110 On the Species of Pseudoboletia.
The only possible fault then that can, here at any rate, be
found with me (and I am sure no one will call it a fault) is
that I put my trust in Mr. Agassiz’s ‘ Revision of the Kehini.’
To him therefore what blame is due must be transferred.
Two questions now remain: the first is, what name shall
be given to the species which has been till now labelled in
the British Museum PL. indiana? In the year 1869 that
eminent zoologist the late Professor Trosehel described in the
‘ Sitzungsberichte ’ (not ‘ Verhandl.,’ as stated by Mr. Agassiz,
op. cit. p. 153) two species of Pseudoboletia—P. stenostoma
and P. maculata: the former appears to be a synonym of
P. indiana (Mich.) ; the latter is in all probability the species
which now is found to be without a name, but has been
labelled P. indiana.
The “ synonymy ”’ of the species will then stand thus :—
Pseudoboletia indiana.
Toxopneustes indianus, Michelin, in Maillard’s ‘ Réunion,’ ed. 2, annex.
A, p. 5.
Spheriechinus indianus, Liitken, Bidrag, p. 76 (144).
Pseudoboletia stenostoma, Troschel, Sitzb. nat. Ver. preuss. Rheinl, 1869,
p96.
Pseudoboletia granulata, Agassiz, Rev. Ech. pp. 155 and 455; Bell,
P, Z. 8. 1881, p. 482.
Pseudoboletia indiana, de Loriol, Cat. raisonné Ech. Maurice (1883),
p- 28.
Pseudoboletia maculata.
Pseudoboletia maculata, 'Troschel, Sitzb. nat. Ver. preuss. Rheinl.
p- 96.
Pseudoboletia indiana, Agassiz, Rev. Ech. p. 456, pl. v. a, figs. 8 and 9;
Bell, P. Z. S. 1881, p. 483; Agassiz, Chall. Rep. Ech. p. 107.
The second question that remains for consideration is the
geographical distribution of the species, in which again there
is some confusion, owing to the statements made by Mr. Agas-
siz. In the Rev. Ech. p. 158, the only locality given for
“P. granulata” is Sandwich Islands, while “P. tndiana” is
said to come from Masbate, Philippines, Mauritius, Bombay
and Bourbon. Specimens from the first three of these locali-
ties are said to be in the British Museum; it is now clear
that those from the first two are examples of P. maculata.
For P. indiana Mauritius and the neighbouring islands are
authentic localities, while, like Tripneustes variegatus, it
appears too to be found at no less distant a locality than the
Sandwich Islands. In conclusion it may be added that Mr,
Agassiz incorrectly ) refixed the sign ® to his “P. indiana”
Mr. J. J. Quelch on new Stylasteride. 111
of the ‘Challenger’ Report (p. 269), inasmuch as that sign
means that the species was “ previously known, but found in
the district for the first time by the ‘Challenger’; ” and, on
his own showing, he had seen in the British Museum, some
ten years previously, specimens from Masbate and the Philip-
pine Islands.
The preceding remarks show into what confusion the species
of this genus, with a literature more scanty than most, have
been allowed to fall, and the thanks of systematic naturalists
are due to M. de Loriol for directing attention to its con-
dition.
XIUI.—On new Stylasteridee, with Remarks on some recently
described Forms. By J. J. Quetcu, B.Sc. Lond., Assis-
tant, Zoological Department, British Museum.
THE four species herein described as new are founded on speci-
mens in the collection of the British Museum. Special interest
is attached to D. breviserialis, owing to the very great obli-
teration of the lateral furrows of cyclosystems, except at the
distal parts of the ccenosteum ; and also to Adlopora ochracea,
in which the number of the dactylozooids in each cyclosystem
is very limited, being usually only three or four. ‘The locality
of Stylaster pulcher is specially interesting among the Hydro-
coralline. In describing the colours of the specimens I have
had reference to Werner’s ‘ Nomenclature of Colours.’
Allopora ochracea, un. sp.
Ccenosteum of a reddish-orange ochre colour, branched,
compact, irregularly flabellate; branches thick, spreading,
slightly flattened and obtuse at the ends; surface nearly
smooth or finely granulated ; cyclosystems closely placed on
all parts, often in irregular series, being about *d millim, to 2
millim. apart, of very variable structure, but not raised above
the general surface of the coenosteum ; dactylopores very few
in each system, variable in number, from 1 to 5, generally 3
or 4, very rarely absent, small, subcircular, placed irregularly
around the gastropore, with cavities always distinctly separa-
ted, and occupied by a relatively large hirsute style ; gastro-
_ pores about ‘4 millim. in diameter, circular, rather deep, with
a thick, rather short, hirsute style; ampulle large, about 14
millim. in diameter, vesicular.
112 Mr. J. J. Quelch on new Stylasteride.
Hab. Unrecorded. B.M.
The specimen to which this specific name has been given
consists of a small broken portion of a rather massive struc-
ture—a short branch with four short chief branchlets, on
different parts of which there are indications of still smaller
branchlets. In the sum of its characters it differs altogether
from all other known species, though in many points its close
affinities with A. californica, V., A. venusta, V., A. miniata,
Powt., and A. nobilis, K., ave clearly seen. Its thick and
massive structure, its cyelosystems placed on all sides of its
branches and not raised above the surface, its few dactylo-
pores in each system (generally 3 or 4), its rather short thick
style in the gastropore, and its reddish-orange ochre colour
are its essential characters, and will serve to mark the species
with certainty. As the specimen is simply a broken branch,
the details of the form of the entire cceenosteum must await
description from a more perfect specimen ; but it is probable
that it will be found to agree very closely with A. nobilis, K.
Stylaster pulcher, n. sp.
Coenosteum of a yellowish vermilion or bright tile-red
colour, much branched, somewhat flabelliform but very irre-
gularly so, branches not coalescing, surface very finely marked
with whitish striations, especially on the basal parts; main
trunk and branches rather thick, rounded or very slightly
compressed, regularly diminishing and giving off many short
branchlets, but these are not very small or delicate ; cyclo-
systems arranged in two rows on opposite sides of the branches,
but this is often disturbed, and many are found scattered over
the surface of the ccenosteum, very few towards the basal
_ parts of the main trunk, many having given rise to branchlets,
very variable in size and structure, subcircular or elongate,
prominent but never pedicellate, about *75 millim. in diameter,
often much smaller, about 1:25 millim. apart in the same row ;
dactylopores generally about 8 to 10, frequently less, very
rarely 11 or 12, small, with minute styles, often unequally
placed around the gastropore so as to give a varying thickness
to the pseudosepta; gastropores very deep, rather wide, with
a distinct short brush-like style; ampulle forming circular
swellings, rather paler than the axis in colour, about 1 millim.
in Giameter, placed on all sides of the branchlets, and giving
them a rough swollen appearance ; many small pores, avout
the size of the dactylopores, occur scattered over the surface
of the coenosteum.
Hab. Enoshima Island, Japan. B.M. (presented by Dr.
F. J. Burge).
aes tial
Mr. J. J. Quelch on new Stylasteride. 113
This species is closely related to S. elegans, V., S. tenuis,
V., and less so to S. obliquus, Stud., but its differences are
well marked and easily separate it. The larger of two speci-
mens in the collection is about 5:5 centim. high, its base being
about 6 millim. thick and its branchlets about 1:5 millim.
thick close to their extremities. Many large swollen ampulla
occur on this specimen, being quite absent on the smaller.
On this smaller specimen, however, there occur on the branch-
lets many small, raised, white porous masses, which are very
rarely present on the larger specimen, and which, when scraped
away, reveal circular cavities in the coenosteum. ‘These are
markedly different from the large, coloured, non-porous
ampullee.
Distichopora breviserialis, n. sp.
Coenosteum of a rather deep flesh-red or pale aurora-red
colour, branched, very compact, irregularly flabellate, with
the surface granulated, roughened, and minutely canaliculated ;
branches often coalescent, rather short, thick, uneven, often
twisted, almost round above, but much compressed, at the base
especially, where three or four branches arise together in the
same plane; branchlets very short, thick, and obtuse, of a
deeper colour than the rest of the ccenosteum; cyclosystems
almost entirely absent from the main branches and the basal
parts of the longer branchlets, primarily developed on opposite
sides of the branched ccenosteum in well-marked furrows, as
indicated on the extremities of the branchlets, but becoming
obliterated by growth, except where incipient branchlets are
present on the main stem and branches and at the extremities
of the long branchlets; at these extremities the dactylopores,
which are very small, are generally situated on raised lateral
ridges on each side of the furrow, with many smaller pores on
the face of the branchlets, but these gradually disappear by
overgrowth; the gastropores are very irregularly shaped,
large and small often alternating at a distance apart about
equal to their diameter, with deep, long, and thin styles,
finely plumose ; large, swollen, distinct vesicular ampulle are
absent, but on many parts of the branches and branchlets occur
rough masses of small irregular cells, often open, which seem
to be ampulle.
Hab. guM.
The specimen of this species consists of a ccenosteum about
7 centim. high, with six main branches, the thickness of
which is about 7 millim. at base, being much wider in the
plane of the flabellum. Many of the branchlets are broken off
114 Mr. J. J. Quelch on new Stylasteride.
and others were dead when the specimen was taken. ‘The
species has many points of affinity with D. rosea, Kent, but
differs strikingly in the structure and position of its cyclo-
systems and its colour, J). rosea being almost of a deep
peach-blossom red, with well-marked furrows throughout the
coenosteum, although these are often irregularly interrupted,
and with large elongated dactylopores. It seems probable
that Tenison- Woods, who himself was doubtful of the identi-
fication, has mistaken this form for D. rosea, K., since the
additional characters which he has given belong to this
species and not to D. rosea.
Distichopora Milesii, n. sp.
Coenosteum of a dull lake-red colour, branched, flabellate,
compact, very slender, with an uneven granulated surface,
irregularly canaliculated ; branches very small, even at their
base, rounded ; branchlets short, small, obtuse, slightly com-
pressed at the tips, and somewhat smaller than the branches ;
cyclosystems arranged evenly on opposite sides in very dis~
tinct, deep, continuous lateral furrows; dactylopores small,
placed in a line on the edges of the furrows, very elongated in
a direction at right angles to this line; gastropores often un-
equal, placed very close to each other, with but a narrow par-
tition between them, having long, deep, thin, and finely
hirsute styles; ampulle in raised crowded masses in which
cells are almost undistinguishable, giving a warty appearance
to the coenosteum.
British Museum : received in exchange from the Brighton
Museum, through the kindness of Dr. Miles of Brighton,
after whom, in acknowledgment, the species has been named.
Hab. South Sea Islands. The exact locality is unknown ;
but as the specimen was growing on the same piece of rock
as a very fine Stylaster stellulatus (Stewart), a species which
has hitherto been recorded only from the Society and Paumotu
Islands, it is probable that it was obtained in this region.
The specimen of this species is about 3 centim. high, the
branches and branchlets being about 24 and 14 millim. thick
respectively. The only species to which it seems to be closely
related is D. fragilis, Dana; but the description of this is
so short, and its details so few, that its identification be-
comes somewhat uncertain. Judging, however, by the figures
of D. fragilis in the ‘ Atlas,’ which do not seem to me to re-
present one species, D. Milesii can be easily distinguished
by its dull lake-red colour and its rounded branches. Although
agreeing somewhat in colour with D. cecetnea, Gray, yet
its much more delicate and rounded form, and the structure of
Mr. J. J. Quelch on new Stylasteride. 115
its cyclosystems separate it widely, even from small speci-
mens of that species.
Distichopora livida, 'Venison- Woods.
‘This species was first described by the Rev. J. E. Tenison-
Woods, in the Proc. Linn. Soc. New South Wales, vol. iv.
1879; and in his valuable monograph of the genus (Journ.
Roy. Soc. N. S. Wales, 1879) that author gives further
details of its structure. It is to be regretted, however, that a
more definite term than ‘ livid” was not given in the de-
scription of the colour of the main portion of the coenosteum,
since this furnishes such a valuable help in the determination
of the species. Judging by specimens in the British-Museum
collection, which seem to belong to this species and of which
the locality is unknown, the colour varies considerably from
dull or pale purplish red to dull reddish or brownish orange,
having the extremities, as given in the description of the
species, white, yellow, or orange, and the lateral furrows and
incipient branchlets bright red or orange. If this identifica-
tion is correct, it will be seen how closely this species is re-
lated to, if indeed it is distinct from (which may fairly be
doubted), D. nitéda, Verrill, which comes from the same
locality, and the description of which Tenison- Woods had had
no opportunity of consulting. If, however, the strict meaning
of lividus was intended, ¢. e. bluish or black and blue, then this
species presents a most remarkable variation in colour, and
certainly would seem to be distinct from any yet described ;
and although stated to be very common in collections made
in the neighbourhood of the Solomon and Marshall Islands,
it is absent from the large and very fine collection of Stylas-
teridz in the British Museum.
Distichopora nitida, Verrill.
Distichopora nitida, Verrill.
Distichopora Brasseyi, Bryce Wright.
Distichopora Allnutti, Bryce Wright.
It seems advisable to state here, in order to prevent mis-
understanding and further complication in the synonymy of
the species, a few facts concerning the characters and distribu-
tion of D. nitida, V., which must have been known to any
one who had read the description of the species.
The specimens of D. nitida described by Verrill in the
Bull. Mus. Comp. Zool. vol. i. no. 3, published in 1864, were
collected by A. Garrett, at Ebon Island (Marshall Islands),
and although described in the old terminology before the
brilliant researches of Prof. Moseley revealed the true nature
116 Mr. J. J. Quelch on new Stylasteride.
of the Stylasteride, yet the main characters as given in the
old description are sufficiently striking.
The following are selected from it:—“Corallum flabelli-
form, branching dichotomously in a plane; branches round
or flattened transversely ; branchlets obtuse, often compressed
at the tips; surface very minutely granular, appearing almost
smooth, with scattered patches of rounded verruce; three
rows of minute pits arranged closely in regular series along
the edges of the branches, those of the central larger row cir-
cular, often having a slender columella in the centre; lateral
ones much smaller, generally irregular in form ; colour bright
red, tips of the branches yellowish white ; other specimens are
light orange.”
From this it will be seen that even in the specimens de-
scribed by Verrill the variations of colour were remarkable,
ranging from bright red to light orange.
In the Ann. & Mag. Nat. Hist. 5th ser. vol. ix. (1882),
p- 74, in a paper “On some new Species of Corals,” in
which this species was redescribed as D. Brasseyt and D.
Allnutti, it is stated that the habitat of D. nitida, with the
many species described by Pourtalés, is the Gulfstream and
in and about the West-India Islands and Florida; while its
colour is indicated as being of a whitish tint, and is contrasted
with the vivid colours of the Pacific species, from the list of
which D. fragilis, D., and D. livida, Tenison-Woods, are
omitted !
It is scarcely to be wondered at that, having so little
knowledge of the characters and distribution of the species,
the author of this paper should have redescribed it under two
new specific terms.
Where the colour in the same species, and more especially
in the same specimen, varies so extremely, it is confessedly a
difficult matter to name the combination in such a way as to
convey exactly to another what is intended; but the speci-
mens of D. ntida which have so lately been described as D.
Brasseyt and D. Allnutti seem to present unusual difficulty ;
for in one place they are given as being “ of a fuscous or
deep foxy-red orange and of a pinkish orange respectively,”
while in another they are ‘ fuscous orange-red in colour,
paling towards the extremities,” and “deep red, tinted or
slightly mottled with orange at the extremities of the stems
and adult branches, paling off into white and pale orange-
yellow.”
The specimens collected by Lady Brassey were from the
Gilbert Islands, a group in the immediate vicinity, and south
ot Ebon Island; and though they certainly are unique and
ba
Contributions to Micro-Paleontology. 117
most interesting in point of size, no sufficient character has
yet been given which would separate them into different
species. ~ Indeed the very characters most insisted upon are
those which seem most certainly to point to their identity with
D. nitida, Verrill.
Distichopora coccinea, Gray.
In his monograph of the genus, the Rev. J. E. Tenison-
Woods has given a figure of this species, and states that he
does not think the species has yet been figured. It may be
pointed out that when the species was described by Dr. Gray
it was also figured (Proc. Zool. Soc. 1860).
XIV.—Contributions to Micro-Paleontology.—Notes on some
Species of Monticuliporoid Corals from the Upper Silurian
Rocks of Britain. By H. ALteyNe Nicuorson, M.D.,
D.Se., Regius Professor of Natural History in the Uni-
versity of Aberdeen.
[Plate VII.]
Ir has long been my intention to give a. detailed account of
the microscopic structure of the Monticuliporoid Corals of
the Wenlock Limestone of Britain, so far as known to me.
I have found, however, that the accomplishment of this would
demand more time than is at present at my disposal; and I
therefore, in the meanwhile, publish the following notes on
the minute structure of some of the commoner Wenlock
Morticuliporoids*, in the hope that they may prove useful to
other workers in the same field. From the brief descriptions
and accompanying figures of structure, it will, I think, be
found easy to recognize the types which I have had under
observation, and this is the special object which I have had in
view. On the other hand, I have found great difficulties as
to the nomenclature of the forms here described, and I have
not been able to clear up these difficulties to any extent. The
earlier observers of these fossils, as, for example, Mr. Lons-
dale, necessarily founded their names upon macroscopic cha-
* Besides certain ramose Monticuliporoids which I have as yet imper-
fectly examined, the Wenlock Limestone contains various incrusting
forms (such, for example, as the curious type figured by Milne-Edwards
and Haime under the name of Monticulipora papillata), which require for
their elucidation a more detailed investigation than I have hitherto been
able to undertake.
118 Prof. H. A. Nicholson’s Contributions
racters principally, the method of investigation by means of
thin sections being of recent origin; and they also gave, as a
rule, extremely brief descriptions. Hence it is exeeedingly
difficult, in many cases, among the Monticuliporoids, to be
certain as to the precise forms to which the older names should
be attached. In the following notes, therefore, I have not
employed any of the older specific names, except in cases
where [ can do so with tolerable certainty of being correct in
so doing. Those forms which I cannot satisfactorily identify
with previously described species I have provisionally desig-
nated by new titles, though it is quite possible that some of
these will also prove to be referable to species to which
names have been attached at some earlier date.
1. Fistulipora crassa, Lonsd. sp. (PI. VII. figs. 1, 1 a, 2, 2a.)
Heteropora crassa, Lonsdale, Sil. Syst. pl. xv. figs. 14, 14 @ (1889).
The corallum in this species is ramose, the branches being
rounded or somewhat compressed, mostly solid, and varying
in diameter from about one line up to half an inch. The sur-
face appears to be smooth, and devoid of either monticules or
macule, so far as I have seen. ‘The tube-mouths are usually
distinctly, though slightly, elevated above the general surface,
and are surrounded by a distinct ring, though in some ex-
ceedingly well-preserved specimens these features are not
observable. The interstitial tubules may or may not be super-
ficially recognizable. In thin tangential sections (Pl. VII.
figs. 1 & 2) the corallites are seen to be oval or circular, not
markedly pinched in or indented at any point, and varying in
size in different specimens, being mostly between z}o and
zy inch in diameter (generally nearer the latter). In one
section I have examined (fig. 2) two of the corallites are
seen to be connected by a lateral tube of communication. ‘The
interspaces between the corallites are rarely more than 74> inch
in diameter, and they are occupied by interstitial tubuli, which
are polygonal or angular in shape, with imperfect walls.
Mostly only a single row of such tubuli separates any pair of
contiguous corallites, but two rows are also often seen in places.
In long sections (Pl. VII. figs. 1 a and 2 a) the corallites are
seen to be crossed by a few complete and approximately hori-
zontal tabule; while the interspaces between them are occupied
by vesicular tissue formed by the anastomosis of the tabulee of
the interstitial tubules. No ‘ spiniform corallites”’ appear
to be present.
It is, perhaps, open to question whether Lonsdale’s figure
and description of Leteropora crassa really apply to this
to Micro-Paleontology. 119
form, and not rather to the very similar /. dudensis, which
I shall describe immediately.
If, however, Lonsdale’s title is to be retained, it is best to
keep it for the form which has been usually regarded by
observers as Heteropora crassa. ‘There is no doubt as to the
propriety of the reference of this form to Fistulipora, M‘Coy,
as shown by the in general complete isolation of the corallites,
and the fact that the walls of the interstitial tubules are so
imperfect as to allow of a confluence of their tabule, and the
consequent production of an intermediate vesicular tissue.
Fistulipora crassa is most nearly allied to &. ludensis, Nich.,
from which it is distinguished by its not forming thin crusts,
by the generally projecting mouths of the corallites and their
larger size, by the larger size and smaller number of the
interstitial tubuli, as well as by their incomplete walls, and,
lastly, by the want of “ spiniform tubuli.”
Formation and Locality. Wenlock Limestone, Dudley,
Benthall Edge, Dormington.
2. Fistulipora ludensis, Nich. (Pl. VII. figs. 3-3 0.)
The corallum in this species forms thin crusts, from half a
line to three quarters of a line in thickness, growing upon
foreign objects. ‘The surface is smooth, without definite
macule or monticules, and exhibits the circular openings of
the ordinary corallites, surrounded by very numerous minute
interstitial pores. As seen in tangential sections (Pl. VII.
fig. 3), the corallites are seen to be circular or oval, often
indented at one point, or at two points, and about 4; inch
in diameter. ‘The corallites are in general completely isolated,
and are separated by one, two, or three rows of very minute
interstitial tubuli, which are subpolygonal in shape, and have
tolerably complete walls. As just mentioned, the wall of the
visceral chambers of the corallites is often bent inwards on
one side or at more than one point, and at such points “ spini-
form tubuli” are usually developed (Pl. VIL. fig. 3a). Simi-
lar spiniform tubuli may also be sparingly developed among
the ordinary interstitial tubuli, As seen in long sections
(Pl. VII. fig. 36), the corallum is seen to be built up of suc-
cessively superimposed thin strata of tubes. The proper
corallites are crossed by a few remote, complete, horizontal
tabule ; while the interstitial tubules have more closely set
tabule, which are so disposed as to give rise in the longitudi-
nal section to a sort of vesicular interstitial tissue.
The present species is in many respects very similar to
Fistulipora crassa, Lonsd., sp.; and it is quite possible that
Mr. Lonsdale may have had this form, at any rate partly, in
120 Prof. H. A. Nicholson’s Contributions
view in describing his Heteropora crassa. As regards its
general characters, it is distinguished from F’. crassa by its
habit of growth, and also by the much greater development of
the interstitial tubuli, which give to the surface of well-pre-
served specimens a minutely porous appearance. Moreover,
the mouths of the corallites are not surrounded by prominent
rims. As regards internal structure, the chief features which
distinguish F. ludensis from F. crassa are the greater number
of the interstitial tubes and their more complete walls, the
smaller size of the ordinary corallites and their more com-
plete isolation, and the presence of well-marked “ spiniform
tubuli.””
Formation and Locality. Wenlock Limestone, Dudley.
The best preserved specimen I have seen forms a thin crust
growing upon a specimen of Monticulipora pulchella, K. & H.,
which it entirely envelops.
3. Callopora nana, Nich. (Pl. VII. figs. 4-4 d.)
The corallum in this species is in the form of minute,
cylindrical, or bulbous masses, generally two or three lines
in length, and about a line or a line and a half in dia-
meter. The surface is free from monticules or macule, but
exhibits the openings of the large circular or oval coral-
lites, largely or wholly separated by regular, often oblong
interstitial pores. In tangential sections (Pl. VII. fig. 4 a)
the corallites are seen to be oval or subcircular, averaging
about = inch in their long diameter, which corresponds
in direction with the long axis of the corallum. They are
separated by intervals occupied by the interstitial tubes, which
have quite complete walls, and are mostly long-oval or irre-
gularly oblong in shape. The long diameters of the intersti-
tial tubes correspond with the long axis of the corallum, and
vary from 74, inch to #5 inch, their shorter diameters being
from +35 to 74, inch. Hence the intervals separating con-
tiguous corallites are much greater in the direction of the long
axis of the coral than when measured transversely to the
corallum.
In long sections (Pl. VII. fig. 4 6) the corallum is seen to
be composed of tubes which are vertical in the axis of the
colony, and then gradually bend outwards to open on the
surface. They are similar in internal structure through-
out their entire extent, complete horizontal tabule bemg
largely developed both in the axial region .and the peripheral
region, while their walls have a nearly uniform thickness
throughout. As they bend outwards, however, towards the
42
to Micro-Palcontology. 121
surface, the corallites become separated by the development
of the interstitial tubes, which entirely resemble the proper
corallites in structure, except in the fact that they possess a
much larger number of tabule, these structures, however,
being still horizontal and complete, and not assuming a vesi-
cular character.
As regards the generic position of this species, I find it
necessary to make a few remarks, as I have elsewhere (Pal.
Tab. Cor. p. 304) expressed the opinion that Callopora,
Hall, should be regarded as a synonym of Pistulipora, M‘Coy.
I arrived at this view from a study of the description and
figures given by Prof. Hall of Callopora, from an examination
of M‘Coy’s type species of F’studipora, and from an investi-
gation of various corals which appeared to be precisely similar
to various forms included by Prof. Hall under Callopora.
That Callopora, Hall, has been made by its original
founder, as well as by other paleontologists, to include a
large number of heterogeneous forms, and that some of these
are truly referable to /istulipora, M‘Coy, are points which
appear to me to be free from doubt, and it was therefore not
unnatural ‘that I should ave concluded that the two genera
were identical.
Recently, however, this question has been attacked in a
more satisfactory manner by Mr. Ulrich (Journ. Cincinn.
Soc. Nat. Hist. 1882), who has had the opportunity of
examining by means of thin sections authentic specimens of
Callopora elegantula, Hall, which is the type species of the
genus Callopora, Hall. Mr. Ulrich has shown that this
species differs in its structure from the majority of the nume-
rous forms referred by Prof. Hall to Callopora, and that it
exhibits characters entirely similar to those of various Monti-
culiporoids which I included under the name of Heterotrypa,
and certainly quite unlike those of Sistulipora, M‘Coy.
While 1 am not prepared to admit the justice of all the re-
marks which Mr. Ulrich has seen fit to make upon this
subject, I am quite ready to recognize the new light which
he has thus thrown upon the structure and affinities of Callo-
pora, Hall. I also quite recognize that Heterotrypa, as origi-
nally defined by me, is a wide group which may be ad-
vantageously subdivided. For these reasons, therefore, I
shall accept the genus Callopora, Hall, as defined by Mr.
Ulrich, as including Monticuliporoids of the type of the
present species, with numerous interstitial tubes, which re-
semble the normal corallites in all except their size and their
possession of more numerous tabule. The corallites, more-
over, are always rounded, and their walls are amalgamated.
Ann. & Mag. N. Hist. Ser. 5. Vol. xiii. 9
137g Prof. H. A. Nicholson’s Contributions
The nearest allies of Callopora nana, so far as I know at
present, are C. (Heterotrypa) O’ Nealli, James, and C. (Hetero-
trypa) nodulata, Nich., both of which are found in the Cin-
cinnati group of North America. From both of these forms,
however, the present species is distinguished by well-marked
external and internal peculiarities, its distinguishing features
being its small dimensions, the proportionately large size of
the corallites, and the peculiar elongated form of the inter-
stitial tubes, while a marked internal feature is the very ex-
tensive development of the tabule in not only the peripheral
but also the axial region of the corallites.
Formation and Locality. Wenlock Limestone, Benthall
Edge; Wenlock Shales, Buildwas.
4. Callopora Fletcheri, EK. & H. (PI. VII. figs. 5-5 6.)
Monticulipora Fletcheri, Edwards & Haime, Brit. Foss. Corals, p. 267,
pl. Ixii, figs. 3, 3 a,
Corallum ramose, of cylindrical branches, which have a dia-
meter of from a line anda half to two lines and a half. There
are no proper monticules or macule; but the surface shows
the approximately circular apertures of the ordinary corallites,
the diameter of which is about 7, mch. ‘The corallites are
separated by interspaces of from y+, to yz5 mch in diameter,
and in badly-preserved specimens these interspaces either
appear as solid or show only here and there a minute poly-
gonal opening. On the other hand, in well-preserved ex-
amples the intervals between the ordinary corallites are seen
to be wholly occupied by the openings of interstitial tubuli.
In tangential sections (Pl. VII. fig. 5 a) the corallites are seen
to be thick-walled and circular, with a well-defined internal
boundary, though not showing the peculiar dark marginal
ring which is so characteristic of many species of Callopora.
Occasionally minute tooth-like processes, which look like
septa, project into the visceral chamber, though I have never
seen more than two or three of these in a single corallite.
The walls of the corallites are amalgamated with those of the
interstitial tubes, and there is rarely more than a single row
of the latter, while in places the corallites are actually in con-
tact. The interstitial tubes are rounded or polygonal, and
only rarely have an elongated form. In long sections (Pl. VIL.
fig. 56) the ordinary corallites are seen to be provided abun-
dantly with complete horizontal tabulze, both in the axial and
the peripheral region of the corallum. As they proceed out-
wards from the centre to the circumference of the branches,
they bend at a considerable angle, and their walls become at
the same time considerably thickened. The interstitial
to Micro-Palceontology. 123
tubules altogether resemble the normal corallites in structure,
except that they are provided with much more numerous
tabulz. Moreover, in old examples the interstitial tubules
become largely filled up with secondary deposit, so that their
cavities become largely or wholly obliterated.
I feel very doubtful as to whether or not I am correct in
identifying the present species with the Monticulipora Fletcheri
of Edwards and Haime. After an examination, however, of
avery large number of specimens I have come to the conclusion
that these observers probably founded the above-mentioned
Species upon an example of the form which I have just de-
scribed, in which the surface was not sufficiently well preserved
to show more than a few of the larger interstitial tubes. At
any rate, if this conclusion be incorrect, [ know of no other
similarly shaped and sized coral in the Wenlock Limestone
which would show the same circular calices separated by well-
marked interspaces.
In various structural features Callopora Fletchert shows a
reseinblance to C. nana, Nich. ; but it is distinguished by its
generally much larger dimensions, the circular shape and
thick walls of the corallites, and the polygonal form and small
size of the interstitial tubules. Internally the present species
is at once distinguished by the thickening of the walls of the
tubes, which in old specimens is sometimes carried so far as
to almost entirely fill up and obliterate the interstitial tubes.
Formation and Locality. Not uncommon in the Wenlock
Limestone of Benthall Edge and Dormington.
5. Callopora? glans, Nich. (Fig. land Pl. VII. fig. 6.)
The corallum in this species is of small size, generally
about four or five lines in greatest height and width, and
mostly subspherical, hemispherical, or pyriform in shape.
Sometimes a basal epitheca is developed; but at other times
the corallum is apparently destitute of this structure, its under
surface, except the peduncle of attachment, being covered by
the calices. ‘The surface shows no monticules or macule,
and is covered witn the large circular openings of the coral-
lites, with the well-marked apertures of the minute interstitial
tubes between them. As seen in tangential sections (fig. 1,
A) the corallites are provided with very thin and delicate walls,
and have a diameter of about =45 inch. ‘They are approxi-
mately circular, but their wall is generally bent inwards at
one or more points into a kind of pseudo-septal fold, giving
the visceral chamber a heart-shaped form. In other cases
there axe two of these infoldings of the wall, generally placed
Qs
124 Prof. H. A. Nicholson’s Contributions
opposite each other. The corallites often touch at points, but
they are mostly separated by narrow interspaces occupied by
a single row of large, angular, imperfectly walled interstitial
tubes. Asscen in long sections (fig. 1, B) the ordinary coral-
lites are crossed by a few remote and complete tabule, and
the interstitial tubes are provided with numerous horizontal
tabule, which at times anastomose and become subvesicular.
Fig. 1.
A
Callopora ? glans, Nich. A, tangential section, enlarged twenty times ;
B, longitudinal section, similarly enlarged.
I am indebted for specimens of this curious species to the
kindness of Mr. Madeley, of Dudley. It is of interest as
forming in some respects a transition between the proper
Fistulipore and the typical species of Callopora. This is
shown both in the infolding of the walls of the corallites,
which is such a characteristic feature of the species, and also
in the fact that the walls of the interstitial tubes are so im-
perfect as commonly to allow of a confluence of their tabule,
giving rise to a partially vesicular interstitial tissue. Callo-
pora? glans has some resemblances to one of the numerous
Russian Monticuliporoids which have the general form of
Monticulipora petropolitana; but I know of no form with
which it could be confounded.
Formation and Locality. Lower Ludlow shales, Sedgeley.
6. Monotrypa crenulata, Nich. (Fig. 2.)
The corallum in this species is hemispherical or subglobu-
to Micro-Paleontoloqy. 125
lar, ordinary examples having a height of an inch or an inch
and a half, anda diameter of about the same at the base. The
base is flat or concave, and is covered by a striated epitheca ;
and the corallites radiate from the base to open over the whole
convex upper surface of the colony. The corallites are pris-
matic, mostly pentagonal, thin-walled, and not firmly united
with one another, their walls being regularly and uniformly
crenulated in such a manner that contiguous tubes are accu-
rately dovetailed together. The corallites vary in size from
about -'5 inch up to 3; inch, there being occasionally definitely
defined groups of the larger tubes. No spiniform tubuli are
developed. ‘The surface is apparently smooth and devoid of
Fig. 2.
c
Monotrypa crenulata, Nich. A, outline of a specimen, of the natural
size; B, part of a few tubes, enlarged; C, longitudinal section, enlarged
twenty times; D, tangential section, similarly enlarged.
monticules. As seen in long sections the tubes are found to be
crossed at considerable intervals (s'5 to 75 inch) by a few
horizontal tabule, which are not uniformly placed at corre-
sponding levels in contiguous corallites.
126 Prof. H. A. Nicholson’s Contributions
I think it tolerably certain that this form corresponds with
part of the Favosites jibrosa of Mr. Lonsdale (Sil. Syst.
pl. xv. dis, figs. 6-6 d); and I should very willingly have
retained the specific name of fibrosa if this had seemed at all
advisable. The name of Favosites fibrosa has, however, been
given by different authors to very different corals *, and the
specific name can only be retained for the form to which Gold-
fuss originally applied this title, whatever that may really be.
The widest differences also have existed among British pale-
optologists in their descriptions of the characters and structure
of the forms to which this name has been given. Thus Mr.
Lonsdale both figures and describes mural pores in some of
the forms which he placed under Favosites fibrosa, whereas
M‘Coy expresses his conviction that mural pores are wanting,
and places the forms which he considers Lonsdale to have
had in view under Stenopora, retaining for them the specific
name of Goldfuss. Again, it seems certain that Milne-
Edwards and Haime, in their great work on the British
Fossil Corals, included two quite distinct types, one from the
Devonian and the other from the Silurian, under the name of
Favosites fibrosa. Upon the whole, therefore, it has appeared
to me to be safest to give a new name to the forms now
under consideration, even though they should prove to be
what Lonsdale regarded as Havosites fibrosa, Goldf.
As to the generic position of this type, I have failed to
convince myself that it possesses mural pores. ‘The shape of
the tubes reminds one of what one sees in some species of
Favosites, such as I. aspera, D’Orb., and £. mullochensis,
Nich. and Eth., and one naturally expects to find foramina
on the crenulated angles of the corallites. Moreover, I have
occasionally seen phenomena which I should have regarded as
probably indicating the presence of mural pores, had I been
able to look only at rough fractures of the coral with a com-
paratively low magnifying-power. If mural pores really
* If we take the description of Favosies fibrosa, Goldf., given by Milne-
Edwards & Haime (Pol. Foss. p. 244) we tind at once that it cannot
possibly be the same as the form here under consideration, since (quite
apart from the question of the presence or absence of mural pores) the
tabulee are stated to be very close-set (five or six in the space of a milli-
metre). Similarly the close-set tabulz, as well as the want of crenulated
corallites, will show that the form figured by these same authors from
the Devonian of Devonshire as F. fibrosa, Goldf. (Brit. Foss. Cor. pl. xlviii.
figs. 3-36), cannot be identical with the present type. On the other
hand, the coral figured by Milne-Edwards and Haime under the same
name from the Upper Silurian of Britain (Brit. Foss. Cor. pl. lxi. figs. 5,
5a) does really seem to be identical with the form which I have here
described.
ee
to Micro-Paleontology. 127
existed, however, at the angles of the tubes (where alone in
this form they could exist), they would certainly be detected
in thin sections; and I have not seen any traces of such
openings in either tangential or longitudinal slices. In the
absence of mural pores the species must be referred to the
genus Monotrypa, Nich., and it is, indeed, in many respects
closely allied to the Monotrypa undulata, Nich., of the Tren-
ton Limestone and Hudson-River formation of Canada. The
‘principal characters, in fact, which would distinguish JZ.
crenulata from the globular forms of MZ. undulata, Nich., are
that the corallites of the former are, on the whole, decidedly
larger than they are in the latter, that there are none of the
smaller angular corallites which are found among the larger
tubes in the latter species, that the thickened nodes at the
angles of the larger corallites (“spiniform tubuli” ?) in JZ.
undulata are wholly absent in M. crenulata, and that the
walls of the corallites in the English species are decidedly
more strongly crenulated than in the Canadian type.
Formation and Locality. Wenlock Limestone, Dudley.
Lower Ludlow Shale, Sedgeley (coll. Mr. Madeley).
7. Monotrypa pulchella, EK. & H.
I have already described and figured this species (‘ The
Genus Monticulipora,’ p. 188, figs. 38, 39), and have nothing
special to add, except that I find the species to be a more
abundant one than I had previously supposed, fragments
being not uncommon both at Benthall Edge and Dormington.
EXPLANATION OF PLATE VIL.
Fig. 1. Tangential section of Fstulipora crassa, Lonsd., sp., enlarged
twenty times.
Fig. 1 a. Longitudinal seetion of the same, similarly enlarged.
Fy. 2. Tangential section of another example of F. crassa, in which the
corallites are of smaller size. Two of the corallites are united
by a lateral connecting-tube. Enlarged twenty times,
Fig. 2a. Longitudinal section of the preceding, similarly enlarged.
fig. 3. Tangential section of Fistulipora ludensis, Nich., enlarged twenty
times.
Fig. 3a. Part of the same, enlarged fifty times, showing “ spiniform
tubuli.”
Fig. 3b. Longitudinal section of the preceding, enlarged twenty times.
Fig. 4, Outline of a specimen of Callopora nana, Nich., of the natural
size,
Fig. 4a, Tangential section of the same, enlarged twenty times.
Fig. 4b, Longitudinal section of the same, similarly enlarged.
Fig. 5, Outline of a fragment of Callopora Fletcheri, HW. & H., of the
natural size.
Figs. 5a & 5b, Tangential and longitudinal sections of the same, en-
larged twenty times.
Fig. 6. Outline of a specimen of Callopora? glans, Nich., of the natural
size,
128 Mr. C. O. Waterhouse on new Longicorn Coleoptera.
XV.—Description of a new Genus and Species of Longicorn
Coleoptera from the Philippine Islands. By CHARLES O.
WATERHOUSE.
Lamiide.
APOMECYNINA:. ’
DIAXENES, n. gen.
General characters of Apomecyna, but a little less parallel
in outline, the elytra being more narrowed towards the anex.
Antennal tubercles a little more prominent and more approxi-
mate; face equilateral, very gently convex. LHEyes coarsely
granular, not quite so deeply emarginate. Antenne reaching
two thirds of the length of the elytra, moderately stout,
finely ciliate below ; the basal joint three times as long as
broad, only very slightly narrowed at the base; third a little
longer than the first and second taken together, slightly bent,
and distinctly narrower at the base than at the apex; fourth
joint three quarters the length of the third; the fifth a little
more than half the length of the fourth ; the following joints
gradually but only slightly diminishing in length and thick-
ness. ‘Thorax a little broader than long, subcylindric, a little
narrowed in front. Scutellum transverse. Hlytra at the base
one quarter broader than the thorax, not quite fourtimes as long,
moderately narrowed towards the apex, flattened at the suture;
at the base, gradually declivous from just behind the middle
the apex ot each elytron obliquely truncate. Legs short and
stout; the femora considerably inflated. Intermediate tibiee
with an incision on the outer edge at the apex. ‘T'arsi short ;
claws diverging. Prosternal process sloping down posteriorly.
Mesosternal process rather broader than the prosternal,
sloping down in front.
The species on which I propose to found this genus very
much resembles some of the smaller species of Hathliodes. It
differs from Apomecyna chiefly in the proportions of the an-
tennal joints (which also diminish in thickness and are ciliate)
?
the even surface of the thorax, and less parallel form.
Diaxenes Taylori, un. sp.
Pube pallide flavo-grisea dense vestitus ; antennarum dimidio api-
cali fusco, articulis griseo annulatis; thorace ad basin gutta alba
notato ; scutello fusco, gutta mediana lateribusque albis ; elytris
ante medium prope suturam gutta fusca ; abdomine fusco-vittato,
of ee he
Mr. H. J. Carter’s Generic Characters of Sponges. 129
guttis albis utrinque ornato; femorum basi, tibiarum apice tar-
sisque nigris.
Long. 5} lin.
The general colour is a pale sandy, with a slightly darker
shade at the base and apex of the elytra. Scattered more or
less all over the body, including the basal joint of the antennze
and the legs, there are erect white sete. There are a few
distinct punctures on the head between the antenna. The
fourth to the apical joints of the antenne are blackish brown,
with the base of each joint pale. The thorax is very slightly
broader than long, moderately narrowed in front of the
middle, with a very slight constriction at the base, the sides
very gently arcuate; near the base there are a few very distinct
punctures; on the basal margin on each side there is a very
small fuscous spot. The elytra have the shoulders rounded ;
some punctuation is visible through the pubescence, there are
some small black punctures here and there, and near the scu-
tellum there are numerous larger dark punctures. There is a
brown patch on each side of each abdominal segment, and in
each patch a small white spot. The legs are nearly white,
with the base of the femora dark; the apex of the tibie and
the tarsi nearly black.
Hab. Philippine Islands? Brit. Mus.
The specimen from which the above description is taken
was found alive in the Royal Nursery, Chelsea, on a species
of Orchis (Phalenopsis) from Manilla; it was gnawing off
the stems of the plant.
British Museum,
Cromwell Road, 8. W.
~XVI.—Generic Characters of the Sponges described in Mr.
Carter’s “Contributions to our Knowledge of the Spongida”
(‘ Annals,’ 1883, vol. xii, p. 308). By tHe AurHor.
Order III. PSAMMONEMATA.
Family 1. Surface even, not polygonally divided.
Genus CoscrINoDERMA, Crtr.
Char. Sieve-like incrustation, composed of foreign bodies,
130 Mr. H. J. Carter’s Generic Characters of Sponges.
uniformly foraminated and continuously spread over the sur-
face, whose evenness is not disturbed by the usual polygonal
projection of the subdermal fibre. Fibre fine, woolly.—Species
Coscinoderma lanuginosum.
Order V. ECHINONEMATA.
Family 1. Echinated with proper spicules on the fibre.
Genus Ectyon, Gray.
Char. Sponge massive, reticulated, composed of cylindrical
horny fibre, with single scattered or groups of diverging spi-
cules. Spicules acuate, verticillately spined. (Hmended from
Proc. Zool. Soc. 1867, p. 515.)—Species Hetyon sparsus, &e.
Genus Eoryonopsis, Crtr.
Char. Branched, with solid axis. Spicules with spines
generally distributed, 7. e. not arranged in verticils. Spicules
of the interior of the fibre cylindrical, obtusely ended; those
on the exterior of the fibre acuate, in groups of two or more,
echinating the surface.—Species Hetyonopsis ramosa.
Family 2. Echinated with proper spicules projecting from
the ¢nterior of the fibre.
Genus Puycopsts, Crtr.
Char. Fueus-like, branched. Stem hard, woody ; covered
hirsutely with filamentous processes more or less expanded
and divided at the free ends. Spicule acerate.—Species Phy-
copsis hirsuta.
Genus PTILOCAULIS, Crtr.
Char. Long, cylindrical branches with solid axis, passing
outwardly into more or less spatuliform processes, like the
barbs of a feather, more or less divided at the free ends.
Spicule acerate or subacuate.—Species Piclocaulis gracilis Ke.
Genus LEucOPHL@US, Crtr.
Char. Pyramidal, erect, in groups, or massive, or flabel-
late. Surface snow-white when dry. Interior light amber-
yellow. Surface incrusted by coalescent tufts of proper
spicules. Spicule acerate or acuate.—Species Leucophleus
massalis &c. °
~
S,
«
Mr. G. Lewis on new Japanese Histeride. 131
XVII.—On some Histeride new to the Japanese Fauna, and
Notes of others. By Grorer Lewis.
In 1879, twenty-six species of Histeride were recorded from
Japan, and the present paper treats of twenty-three more.
Besides these, there are fourteen species of Paromalus and seven
of Saprinus to be determined, which will bring the Japanese
species up to about seventy, when all those contained in my col-
lection are recorded ; and itis hardly likely that this list will be
much augmented at present, as the rarer Histeride are very
local, and those which associate with Formicide are difficult to
find. The eight species marked with an asterisk are such as
have allies in the tropical parts of Hastern Asia; the others
agree with the Histeride of Europe and Northern Asia. The
species of Tiryponceus are worthy of notice, because one of
them occurs as far north as latitude 43°, and hitherto Mexico
has been the most northern country from which any species
has been recorded.
I failed to find Teretrius in Japan; but it is the only
genus likely to be found in the archipelago which is not as
yet represented in the list. ister quinquestriatus, Motsch.,
given in my ‘Catalogue’ as no. 663, I now consider =duo-
decimstriatus, Schrank, and Onthophilus striatus, F. (? var.
Harold), no. 676,=flavicornis, Lewis.
In the Histeridz, as in other families, some of the species
from Japan are closely allied to European forms, and I think
we cannot refuse to admit the probability of a common origin
for both at no very remote period; so that a close compari-
son and careful study of such insects as Hololepta plana and
depressa, Hister unicolor and concolor, or Hetwrius gratus and
ferrugineus, will perhaps show the direction that modification
may assume in like forms when isolation is fairly complete,
as in Japan, and the conditions realized within the area
are sufficiently potent to produce a visible effect. It may
be said that it is only incidentally that Hister concolor and
Hololepta depressa can be distinguished from their European
congeners by a densely punctured pygidium : but the incident
does not lie simply in their having it; it lies in the fact that
both from their habits have been subjected to certain conditions
which cause such sculpture.
The most essential differences between any part of Europe
and Japan are shown in the climate and other physical con-
ditions, which in the latter country nourish great forests of
magnificent timber even at fairly high altitudes, while in
132 Mr. G. Lewis on new Japanese Histeride.
Europe forests relatively occupy an insignificant area, and
such trees as grow in favourable situations never attain to the
vigour and consequent stature of those in the Kast.
List of Species, arranged generically.
Hololepta depressa, n. sp.
parallela, n. sp.*
amurensis, Jevtter.
Platysoma pini, n. sp.*
Lewisti, Marseul *.
-——- yagans, N. sp.
rasile, n. sp.
celatum, n. sp.
lineicolle, Marsev.
Hister japonicus, Marseul.
12-striatus, Sch.
punctulatus, Wied.*
aino, 0. sp.
Jekeli, Marseul.
concolor, n. sp.
— Pirithous, Marseul.
— cadaverinus, Hoffm.
—— boleti, n. sp.
—— agnatus, N. sp.
—— sutus, n. sp.
—— navus, Marseul.
depistor, Marseul.
—— japanus, Motsch.
margine-punctatus, Lewss.
simplicisternum, Lereis.
The new species are :-—
Carcinops 14-striata, Steph.
Epierus lucts, n. sp.
Paromalus musculus, Marseul.
Notodoma fungorum, n. sp.*
Hetzerius gratus, n. sp.
optatus, n. sp.
Dendrophilus Xavieri, Marseul.
Triballus semen, n. sp.
Saprinus speciosus, Zr.
pecunius, Marseul.
nitidus, Payh.
sine, Marseul.
Gnathoncus rotundatus, Z7/.
Tryponzeus fagi, n. sp.*
venator, n. sp.*
Plegaderus Marseuli, Reitter.
Onthophilus flavicornis, n. sp.
ostreatus, Lewis.
silvee, n. sp.
arboreus, n. sp.*
Abreeus bonzicus, Marseul.
Bacanius niponicus, Lewis.
Acritus Komai, Lewis.
Myrmidius ovalis, Beck.
Hololepta depressa, n. sp.
H., plane proxime affinis, nigra, nitida; pronoto stria marginali
tenuissima ; elytris striis 2 dorsalibus abbreviatis ; pygidio dense
punctato. L. 63 mill.
Exceedinely like the European 1. plana ; the head and pro-
sternum are both narrower, and the pygidium thickly and
rather coarsely punctured.
Distributed sparingly from the Kumagawa in Higo to the
Ishikari river in Yezo. All the specimens taken were resting
under bark, and generally on the lateral branches 12 or 14
feet from the ground.
Hololepta parallela, n. sp.
H. elongate proxime affinis, parallela, valde plana, nigra, levissima ;
fronte non tuberculata; elytris stria subhumerali brevissima ;
Mr. G. Lewis on new Japanese Histeride. 133
abdomine subtus plano; propygidio utrinque sulcato, pygidio
impunctato. L.7 ad 8 mill.
This species is like H. elongata, but it has no tuberele on the
head, nor is there an arched sulcus in the third (the broadest)
segment of the abdomen beneath. The sides of the thorax
are more rotundate, and each elytron has one short stria at
the base. These characters, joined to the broader outline and
facies generally, are of good specific value.
I obtained a series of twenty specimens in the moist forests
of Higo in May, chiefly at Konose and Yuyama; it is the
most tropical form of the genus in Japan, and is found under
the bark of both the hard-wooded evergreens and the deciduous
trees.
Hlololepta amurensis, Reitter.
Hololepta amurensis, Reitter, Deutsche ent. Z. xxiii. (1879) p. 218.
The male of this species has a deep thoracic fossa. It was
described by Herr K. Reitter from Amurland, as the trivial
name indicates, and I found it commonly in all the forests of
Japan of moderate elevation. I have beaten it in plenty near
the Junsai lake in August, off the branches of Salix infested
with Cossus.
Note.—Some of the Histerids of the Hololepta group with
simple mandibles are not strictly entomophagous in the imago
state; and this is particularly the case with H. amurensis, which,
I believe, feeds exclusively on exuding sap. Hololepta elon-
gata, which I have taken plentifully in Ceylon and other
places, is probably (with H. parallela) wholly dependent on
smal] soft-bodied larva for food, and I have never seen H.
depressa at sap.
Platysoma pint, n. sp.
Ovale, subconvexum, nigrum, nitidum, leve; fronte clypeoque con-
cavis, stria transversa integra; pronoto stria non interrupta ; elytris
striis 1-4 integris, 5 breviori, 6 nulla; propygidio biimpresso,
pygidio margine elevato, grosse punctatis; antennis pedibusque
brunneis. L. 5 mill.
Closely allied to H. odiosum (Marseul’, Cand.), but smaller ;
with a different system of dorsal striation.
Occurs under pme-bark in the warmer parts of Japan; Higo
and Isei are the chief localities for it.
Platysoma vagans, n. sp.
Oblongum, parallelum, subconvexum, nigro-piceum ; fronte sub-
concayva, stria recta; pronoto punctulato, stria integra; elytris
134 Mr. G. Lewis on new Japanese Histeride.
striis 1-3 integris, 4-5 abbreviatis, 6 nulla; propygidio pygidioque
grosse punctatis et immarginatis ; pedibus rufis. L. 4} mill.
This species comes near to P. Lewist7; it is less convex, more
parallel, with the fourth and fifth striz shortened from the
middle; the pygidium is emarginate and convex.
I obtained it from an oak near Bibi, in South Yezo,
August 16, 1880.
Platysoma rasile, n. sp.
Oblongum, subparallelum, depressum, nigrum, nitidum, leve ; fronte
concava, stria integra; pronoto lateribus sparse punctatis, stria
pone oculos utrinque angulata ; elytris striis 1-3 dorsalibus in-
tegris, 4-5 abbreviatis ; propygidio pygidioque fortiter punctatis.
L. 32 mill.
This species is very close to P. Leconted; it is more parallel
and less quadrate, but the general sculpture above is almost
identical. Beneath, the segments of the abdomen are of equal
breadth, not contracted in the middle, as in P. Lecontec ; and in
this particular there is a like modification to that hereafter
noticed between HHister Arias¢ and Hister aino. :
I took a few examples at Kumamoto and Konose in Higo.
p) 4 a
Platysoma celatum, n. sp.
Oblongo-ovatum, nigrum, nitidum ; fronte subconcava, stria recta ;
pronoto antice rufo, lateribus punctulatis, stria transversa inter-
rupta; elytris striis 1-4 integris, 5abbreviatis; propygidio pygidio-
que punctatis ; antennis pedibusque rufo-brunneis. L. 3 mill.
This species is allied to the preceding (P. rast/e), but the
striation is different and also the coloration.
Occurs in the vicinity of Yokohama in “ fir-stools”’ early
in spring.
Hister aino, nu. sp.
Ovalis, convexus, niger, nitidus; pronoto lateribus late punctatis,
stria integra, margine angusto, elevato ; elytris striis 1—4 dorsalibus
integris, quinto et suturali abbreviatis ; propygidio sparse punc-
tato, utrinque subfoveolato, in medio linea longitudinali distincta ;
pygidio dense et grosse punctato. L. 8 mill.
This insect in its general sculpture agrees with the rare
European H. Arzasz, but it has not the subparallel outline of
that species. This shortness or more ovate form as compared
with H. Arias? arises from the structure of the abdominal seg-
ments. In H. Arvas?, the segments of the abdomen beneath
are of equal breadth ; in H. aino, the three median segments
are narrow and only clearly visible at the sides, for in the
Mr. G. Lewis on new Japanese Histeride. 135
middle they are soldered together, and a few punctures alone
remain to indicate their limits. The broad lateral band of
punctures on the thorax separates it from all the other Histerids
in Japan ; but it may be placed in the catalogue near H. Jekel?.
This peculiar Hister has been found in the district of the
Ishikari river in Yezo.
flister concolor, un. sp.
Ovalis, subconvexus, niger, nitidus; fronte stria integra; pronoto
stria laterali externa valde, interna vix abbreviatis ; elytris striis
1-3 integris, 4-6 brevibus ; propygidio subfoveolato pygidioque
dense et grosse punctatis. L. 8 mill.
H. concolor is sculptured like H. unicolor, except on the two
abdominal segments seen from above, which are strongly and
closely punctured. In its general facies itis like H. 4-notatus,
being wider and less convex than H. unicolor, and the interstice
between the inner thoracic stria and the outer margin is wider
and the short stria is more in the centre of this interstice.
This is also from the vicinity of the Ishikari river.
Note.—I found three specimens of Hister japanus, Motsch.,
on the beach at Yokohama; it comes near H. 4-notatus, Scriba.
Hister boleti, n. sp.
Ovalis, convexus, niger, nitidus; fronte plana, stria integra pro-
funde impressa; pronoto striis punctatis, stria pone oculos utrin-
que deflexa ; elytris striis crenatis, 1-3 dorsalibus integris, 4, 5, et
suturali brevibus ; propygidio subfoveolato pygidioque punctatis ;
mesosterno leviter sinuato. L. 7 mill.
This species is the size of H. caduverinus, but in general
sculpture comes nearest to the rare Huropean JH. distinctus.
From the latter, the longer mandibles, the remarkable deflexure
in the thoracic stria behind the eyes, the fourth dorsal stria
not reaching the middle, and the sinuate mesosternum (as in
H. cadaverinus) are good distinguishing characters.
It oceurs commonly at Chiuzenjiin an arboreal fungus, and
I also obtained it at Kashiwagi in the Kii peninsula.
Hister agnatus, n. sp.
Ovalis, subconvexus, niger, nitidus ; pronoto striis lateralibus inte-
gris, postice approximatis; elytris striis 4 dorsalibus integris,
5 et 6 abbreviatis; prosterno impunctato. L. 5 mill.
This species is almost identical with //. cadaverinus as re-
gards sculpture, but it is much less convex. It is not larger
than H. foedatus, which it resembles in the structural plan of its
136 Mr. G. Lewis on new Japanese Histeride.
abdominal segments and also in its outline. Lister faedatus
and marginicollis, with H. aino and agratus, have segments 2-4
of the abdomen much contracted in the middle ; and the result
of this is that the pygidium is reflexed by being drawn up
towards the sternum.
I obtained my specimens from a dead fowl, set as a trap
for necrophagous insects, at Nikko, in the forest behind the
temples, in June 1880.
Hister sutus, n. sp.
Suborbicularis, convexiusculus, niger, nitidus; stria frontali sub-
transversa ; pronoto subtiliter et parce punctulato; elytris striis
1-3 integris, 4 ante basin abbreviata, 5 et 6 ante medium ter-
minatis; prosterno basi bistriata; mesosterno sinuato, margine
punctato-striato. L. 4 mill.
This species is of the same stature as /. ruficornis, and pos-
sesses some of its characters, but the two thoracic strie bring
it into the H. cadaverinus group.
It is apparently rare. 1 obtained only four specimens from
the elevated forest above Kiga, near Miyanoshita, in May
1880.
Epierus lucés, n. sp.
Ovalis, parum convexus, niger, nitidus; antennis rufis, pedibus
piceis ; pronoto punctulato; elytris striis 5 dorsalibus et suturali
integris ; propygidio pygidioque dense punctatis. L. 23 mill.
Larger and more ovate than EL. comptus ; the head is very
finely punctured, with a transverse stria between the eyes. The
thorax is clearly punctate, and rather thickly so at the base,
in front of the scutellum ; the interstices of the elytral strize
are all finely punctured.
The type of this species came from a rotten tree in the
grounds of the Kasuga no Miya, at Nara, June 1881, and I
believe all the species of this genus are of arboreal habits.
I have only one specimen.
6 f
Notodoma fungorum, n. sp.
Globosum, rufo-castaneum, nitidum, punctatum ; elytris punctato-
striatis, 1, 2 et 4 integris, 4 antice cum suturali arcuatim juncta ;
tibiis multispinosis. L. 33 mill.
When in Paris, I carefully compared this species with Mar-
seul’s type of NV. globatum from India, and found it distinct, but
closely allied. ‘Ihe size is larger and the punctuation more
coarse, and there is a slight difference in the form of the striz.
On the humeral angle, and in the space between the second
Mr. G. Lewis on new Japanese Histeride. 137
and fourth stria at the base of each stria, there is a large
cream-coloured blotch; this, with the prevailing red colour of
the species, is a very remarkable feature for the family.
It is not uncommon in all the islands, infesting fungi on
trees, which it visits in the first stage of decomposition, ‘when
there is an abundance of other insects, on the larve of some
of which it doubtless feeds.
Heterius gratus, n. sp.
Subquadratus, rufo-brunneus, fulvo-hispidus; fronte lateribus
striatis ; pronoto utrinque bisulcato; elytris striis 3 distinctis,
3 brevi; pygidio parce punctato, tenuissime impresso. L.
13 mill.
This species is very closely allied to H. ferrugineus ; it is
darker in colour, half as large again, with legs relatively
much longer and tibia much more dilated. The elytral
strie are three in number, two complete, and the third only as
long as two thirds of the elytra.
I took this species with a fuscous-coloured ant, midway be-
tween Shimonosuwa and the Wada-toge, August 1, 1881.
Heteerius optatus, n. sp.
Oblongo-ovatus, nigro-piceus, sparse fuscescenti-hirtus, punctulatus ;
pronoto lateribus subrotundatis, margine latissimo, medio bi-
striato; elytris striis 1-3 et suturali integris ; pedibus rufis, tibiis
modice latioribus. L. 2 mill.
I have only a single example of this curious Heterius,
which differs in colour and outline from all the hitherto re-
corded species. ‘The whole insect is piceous black, save the
anterior angles of the thorax and the legs, which arered. The
thorax has the lateral margin very wide, with two short fine
striz in the centre; these lines are not, as may at first appear,
the limit of the thoracic margin. The thorax, especially in
the anterior portion, is much more coarsely punctured than
the elytra.
I received this species from the vicinity of the Ishikari
river, in Yezo, and with it came specimens of a genus of
Synteliidee (not yet enunciated) , which corresponds with Oylistix
in the Histeridz, and it is probable that they all came from
the same tree. I think, therefore, that H. optatus has been
taken in association with an arboreal ant; and this idea seems
confirmed by the colour of the species, which agrees somewhat
with Dendrophilus punctatus or a dark-coloured Hretmotes.
Triballus semen, n. sp.
Ovalis, parum convexus, dense punctatus, nigro-piceus, parum
Ann. & Mag. N. Hist. Ser. 5. Vol. xii. 10
138 Mr. G. Lewis on new Japanese Histeride.
nitidus ; fronte post oculos subtuberculata ; elytris striis dorsali-
bus 2 abbreviatis, obsoletis. L. 2 mill.
Allied to 7. americanus, but more convex, with the forehead
behind the eyes more elevated, the elytra strigose-punctate at
the sides, and the margin simple, not reflexed.
I have only one specimen; it was taken in an old tree at
Kiga, near Miyanoshita, May 1880.
Tryponeus fagi, n. sp.
Cylindricus, niger, nitidus, undique punctatus; antennis pedibusque
rufo-piceis. L. 4 mill.
do. Frontis lateribus basisque margine elevatis; proncto antice
retuso, medio subelevato.
9. Fronte plana, in medio depressa ; pronoto antice convexo.
T. kalemantenus is rather shorter and broader than this
species, but the two are nearly allied. The prosternum in
7. fagt has no lateral stria, and the thoracic marginal line con-
tinues well round the basal angles.
The perfect insects of Tryponceus prey on those of Platypus,
and it is useless seeking for the former in trees not infested
by the latter, which go 6 or 8 inches into the trees and are
followed by the Histerids. It is impossible to say from ob-
servation whether the spines or processes on the apices of
the elytra of the wood-borers protect them in any way from
their enemies, but I think they do not, and that they have other
uses. Zryponeus cannot turn round in the trees, but can
move backwards or forwards in the narrow galleries with
almost equal facility. It can only be caught, as a rule, when
traversing the distance between two holes ; but I have beaten
stray specimens in summer,
Tryponeus venator, n. sp.
Niger, nitidus, filiformis, parum dense punctatus; antennis pedibus-
que piceis; prothorace stria laterali integra, prosterno utrinque
striato. L. 33 mill.
3. Rostro apice modice reflexo, thorace antice linea in medio yix
elevata.
@. Fronte excavata.”
This species is more filiform than any other I know from
Asia, and is remarkable for its cylindricity, because the eastern
forms of the genus are usnally much more robust than the
American species. 7. venator teeds on a much smaller Platypus
than 7. fagi; each species preys, in fact, on an insect of its
own girth. ‘The male has the thorax a little longer than the
female and slightly compressed at the sides.
Mr. G. Lewis on new Japanese Histeride. 139
Found only in South Japan, at Yuyama and Konose, but
it is not rare where it occurs.
Onthophilus flavicornis, n. sp.
Breviter ovalis, niger, subnitid us ; antennis brunneis, clava flava ;
fronte in medio unicostata; pronoto dense strigoso, margine an-
gusto, subelevato ; propygidio tricarinato. L. 2 mill.
The sculpture is very similar in every respect to that of
the European O. striatus; the distinguishing characters are
the colour of the antenne, and the sides of the thorax being
only very narrowly margined, and not elevated at the base.
There is a slight difference also of outline, and some of my
remarks on Hester concolor will apply to this species.
Taken from a fungus at Bukenji, near Yokohama, early in
March 1880.
Onthophilus ostreatus, Lewis.
Onthophilus ostreatus, Lewis, Ent. Mo. Mag. xvi. 1879, p. 76.
This species, which is the largest yet known in the genus,
was formerly only recorded from China. In the autumn of
1880 Mr. Pryer obtained a fair series near his bungalow at
Yokohama, from refuse in a turnip field, and I am indebted
to him for four examples.
Onthophilus silve, n. sp.
Suborbicularis, niger, opacus; fronte triangulariter carinata; pronoto
parce tenuissime punctato, costis octo validis, duabus tantum ab-
breviatis; elytris sutura, margine laterali costisque duodecim,
elevatioribus. L. 23 mill.
The outline of this species in the head and thorax resembles
that of the American O. alternatus, but the insect is a little
smaller. The thorax has eight costa, six complete, two (the
third from the margin on each side) very short, with the punc-
tuation of the intervening spaces very scattered and shallow.
The elytrahave twelve costes complete and equally elevated, the
suture and margin corresponding with them ; the interstices
have at intervals a transverse line-like puncture, but none of
the longitudinal punctures which are so general in this genus.
Found under dead leaves at the Akinomiya, near the Suwa
lake, July 31, 1881.
Onthophilus arboreus, n. sp.
Orbicularis, niger, hispidus, opacus; antennis clava ferruginea. 0.
hispido proxime affinis, sed minor. L. 13 mill.
This insect has the dorsal punctures much less deep than in
10?
140 Dublin Microscopical Club.
O. hispidus ; it must, however, be observed that the species of
this section of Onthophilus are very difficult to define, as,
when in good condition, they are covered with minute
spines and mud-like scales, and it is impossible to see the
sculpture. As in the genus Dastarcus, the specific differ-
ences are very slight. All the hispid species are arboreal
in habit; the specimens I have from Japan were residing
in galleries of wood-borers, probably Tomicus, and were
8 or 10 inches from any orifice by which they could
emerge. In Ceylon, I found O. hispidus in the same way, ob-
taining a large number in one tree; and M. Raffray, under
similar conditions, found O. cost/pennis (also a hispid species)
in the island of Zanzibar.
The locality for O. arboreus is the forest behind the large
temple at Nara, in Hawatchi, where I took it in June 1881.
PROCEEDINGS OF LEARNED SOCIETIES.
DUBLIN MICROSCOPICAL CLUB.
February 15, 1883.
Magnetic Iron-Sand.—-Dr. Frazer showed a specimen of magnetic
iron-sand, of which the crystals were of brilliant adamantine lustre,
and showed several modifications of the primary form; these dis-
played marked polarity when acted on by an artificial magnet,
arranging themselves in bead-like strings.
Starch-granules (?) remaining in the Ash of Platinotupe Photo-
graphic Paper—Mr. Greenwood Pim showed a preparation of the
ash of platinotype photographic paper after treatment with potass
oxalate developer. Imbedded in the fibre of the paper were bright
blue semitransparent bodies, somewhat rounded, and which dissolved
in hot nitric and hydrochloric acids ; but cold acid did not appear to
produce much effect. They were considered to be a peculiar form
of starch-granule in the sizing of the paper.
Nauplius-stage of Astacus.—Prof. Haddon showed the Nauplius-
stage of Astacus fluviatilis, also the similar stage of a Cirripede for
comparison.
Penium rufopellitum, Roy, from Connemara, exhibited, to show
the Eaufoliation of the external reddish Cortical Coating.—Mr. Archer
showed examples from Connemara of Penium rufopellitum, Roy, a
remarkable, if not very striking, Desmid. It is curious, as would
seem, that this species has not been found out of the United King-
Dublin Microscopical Club. 141
dom, one station being in Scotland, near Aberdeen, originally found
by Mr. Roy ; the other being at Connemara, and found by Mr. Archer.
It probably most resembled Penium cylindrus (of which Mr. Archer
now showed an example); but it is very distinct indeed. This
form, P. rufopellitum, is of a brownish-red colour, due to an external
roughish bark-like coating, which is occasionally shed from a por-
tion of the superficies, the bare portion of the wall being then seen
to be colourless. There does not seem to be any other species with
this curious characteristic ; the reddish colour and roughish granular
superficies belonging to Penium cylindrus do not appear to be due to
an outward coating capable of exfoliation.
March 15, 1888.
Vaucheria sessilis showing septation.—Dr. E. Perceval Wright
exhibited some specimens, which had been some years mounted, of
Vaucheria sessilis, showing the septation of this form, which was
to be met with in the winter or early spring months. His object
in doing so was to direct attention to Dr. M. C. Cooke’s ‘* Notes on
Vaucheria” in the current (March) number of ‘ Grevillea,’ in which
he describes and figures septation of the filaments in a Vaucheria,
stating that such had not been previously recognized. In a foot-
note Dr. Cooke remarks that the septation which he figures differs
materially from that detailed by Stahl (Bot. Zeit. xxxvii. p. 129);
but is this so? for the species described are not the same. Le this
as it may, Hanstein, in 1872, has noticed the appearance of parti-
tion-walls in Vaucheria; and Schaarschmidt, judging from a short
analysis of his paper, written in Hungarian in November 1882
(‘ Biologisches Centralblatt’), had also done the same. ‘The speci-
mens exhibited had been observed by Dr. Wright in 1879.
Echinobotryum atrum, Corda.—Mr. Greenwood Pim showed
Echinobotryum atrum, Corda. This curious fungus is found parasitic
on the stems of certain moulds, usually in this case Stysanus or
Pachnocybe. It consists of groups of pear-shaped nearly black
spores, resembling perithecia. It is referred to the Torulacei by
Cooke, but its affinities with that group seem very doubtful. Some-
thing like mycelium was noticed in one or two instances. Possibly
culture may reveal something more of its history. The present
example appeared in abundance on the cut surface of an elm-branch
at Monkstown.
Haliphysema Tumanowiezii new to Ireland.—Prof. Haddon
showed Haliphysema Tumanowiczii from Dalkey Island, taken in
1882, the first recorded Irish example.
Cosmarium plicatum, Reinsch, forma majus, from damp walls
in a warm House at Glasnevin Botanic Garden.—Prof. M‘Nab
showed some gelatinous stuff from the walls of one of the warm
houses at Glasnevin Botanic Garden, formed by the confluent mucous
142 Dublin Microscopical Club.
envelopes of Phycochromaceous Alge, as frequently occurs on damp
rocks in subalpine spots, but here rather unexpectedly showing
imbedded certain Cosmaria. Prominent amongst these was the
large and on the whole decidedly rare rock-form Cosmarium plica-
ium, Reinsch, forma majus. Doubtless under the name Cosmarium
plicatum, Reinsch had in view two very distinct things, both indeed
rare, although the smaller one is somewhat more frequently met
with and usually in somewhat greater numbers than the “ forma
majus.” This, the present one, occurs both in Ireland and Scotland,
specimens from those wide-apart sources being absolutely identical.
Cosmarium acanthophorum, Nordstedt, exhibited to show that the
form appertains rather to Xanthidium.—Mr. Archer showed the so-
called Cosmarium acanthophorum, Nordstedt, also Xanthidium Nord-
stedti, Reinsch, showing how closely they approached one another,
and expressing some wonder that Nordstedt should relegate such a
form to Cosmarium at all, his name seeming to involve what might
be almost regarded as a contradiction in terms as is expressed in the
designation ‘‘ spine-bearing Cosmarium.”
Ammodiscus Scharmanni new to Ireland.—Mr. Balkwill, amongst
many beautifully mounted Foraminifera, showed Ammodiscus
Scharmannt, new to the Dublin fauna.
Air-bubbles in Water-cavities of Quartz—Prof. Hartley showed
some good and striking examples of air-bubbles in water-cayities of
quartz.
April 19, 1883.
Specimens of Torrubia (Cordyceps) exhibited—Mr. Pim showed
one of the strange group of Spheriaceous Fungi parasitic on insects,
formerly called Cordyceps, now referred to Torrubia. The speci-
mens were from the herbarium of Trinity College, and were identi-
fied by the Rev. M. J. Berkeley as Torrubia (Cordyceps) Gunme,
natives of Van Diemen’s Land, whence they had been sent to the
late Professor Harvey. The sections showed very long slender
sporidia having a seemingly chain-like structure, or like a number
of dumb-bells ranged end to end. Further maceration in caustic
potash resolved them into a series of transverse ridges across each
sporidium, with small globules between each pair of ridges. The
sporidia, though long, are extremely slender, so that it is very diffi-
cult to make out their structure. Specimens of Zorrubia Robertsit
from New Zealand were shown for comparison.
Microthamnion Kitzingianum exhibited—Mr. Crowe showed
examples of that minute arborescent Alga Microthamnion Kutzingi-
anum, somewhat widely distributed, but always scantily represented
and fitful in appearance. It forms an elegant very tiny little bushy
tuft of bright green colour.
Dublin Microscopical Club. 143
Budding in Polyzoa.—Prof. Haddon showed budding state of
Polyzoa, illustrating late union of the lophophore with the stomach,
and the origin of part of a bud from the endocyst and part from the
funiculus.
Augite Crystal_—Prof. V. Ball exhibited a transverse section of
an augite crystal from the Vesuvian lava of 1794. Under polarized
light this is a very beautiful object, and exhibits striae which mark
the position of a plane of twinning. A photograph of it, magnified
about 25 diameters, taken by Prof. G. F. Fitzgerald, represents this
character, some included cells, and the structure of the matrix with
admirable definition. The photograph was taken by electric light.
Foraminifera from the Vienna Basin.—Mr. Eleock showed a fine
series of mounted (fossil) Foraminifera from the Vienna basin, re-
marking that many were identical with those from oceanic collections
made during the expedition of H.M.S. ‘ Challenger,’ in fact in no way
distinguishable.
Alliospora sapugaye, Pim, further phases—Mr. Pim drew atten-
tion to the fungus shown by him last year, and provisionally named
Alliospora sapugaye. The description in the Club Minutes, though
correct in so far as it went, proved on further investigation imperfect,
inasmuch as the spore-bearing hyphe do not originate, as was thought,
directly from the globose columella, but from a layer of somewhat
wedge-shaped closely packed cells forming an outer coat, whose
thickness is twice or thrice the diameter of the columella, The
sporiferous hyphe, moreover, are frequently branched articulately
at the tip, where spores are formed, as in the genus Penicillium.
May 24, 1883.
Pileolaria tercbinthi exhibited-—Mr. Pim showed Pileolaria tere-
binthi, a native of Genoa, from specimens in the herbarium at Trinity
College, Dublin. This curious rust is technically a Uromyces, but
the lenticular spores with extremely long slender pedicels are abun-
dantly distinct from any ordinary form of that genus.
Section of Stem of Lycopodium.—Prof. M‘Nab exhibited a trans-
verse section of the stem of a species of Lycopodium, probably Lyco-
podium ilictfolium, from a plant growing in the stove at Glasnevin,
The central fibro-vascular cylinder presented a peculiar complicated
appearance on account of its construction, the xylem and phloem
being partly concentric, partly radial, according to the types of
DeBary. The centre was concentric, whilst the periphery of the
axile cylinder consisted of alternating radial bundles of xylem and
phloem.
A problematic Organism.—Dr. E. P. Wright showed a mounted
specimen of a peculiar and problematic organism which he had
found in some quantity, quite incrusting the root-like portions
144 Dublin Microscopical Club.
of one or two deep-sea aleyonarians. The specimens shown,
though mounted dry, had been quite lately in strong spirit, into
which they had, without doubt, been plunged on coming out
of the sea. The organism, which was found in the form of thin,
creeping, chain-like masses, consisted of a stoloniferous portion,
from which arose a forest of trichome-like bodies all about the
same length, and all terminating in a star of from five to six
rays. These bodies, like the stoloniferous body-mass, were all
formed of calcic carbonate, which, in spirit-specimens, seemed to
be invested with a thin homogeneous plasmodic layer of a protoplas-
mic nature. While inclined to ascribe to this form Rhizopodal affini-
ties, Dr. Wright found it quite impossible to do this with any cer-
tainty. With the crystal bodies in some Ascidians (in which these
bodies form separate entities, and not, as here, part of a common
mass) he fancied the exhibited specimens had nothing in common.
The few remains of siliceous spicules entangled in the trichome-like
bodies had obviously nothing to do with the strange but beautiful
organism.
Spirotenia acuta, Hilse, not strictly appertaining to the genus,
though of similar habit—Mr. Archer showed some examples of a
not uncommon, though local, unicellular Alga, doubtless that usually
regarded as Spirotenia acuta, Hilse, but in whieh, in fact, he never
could distinguish any trace whatever of a spiral arrangement of the
chlorophyll-mass, so characteristic in Spirotenia condensata, Sp.
closteridea, Sp. truncata, and Sp. parvula. No doubt the plant has the
habit and the same kind of occurrence as those named, the young
just- divided individuals hanging together in the same way in pairs
in the sharply defined common investing mucous matrix. This
plant, then, like Spirotenia obscura, so-called, he could hardly think
was truly a Spirotenia at all, but approached more to Peniwm, the
central axile (not parietal) mass of contents being only somewhat
twisted.
June 22, 1883.
Fruit of Cliftonia —Dr. E. Perceval Wright exhibited some moun-
ted fragments of Cliftonia pectinata, Harv., which he had quiterecently
received from Baron F. von Miller, and which had been dredged by
Prof. Bracebridge Wilson outside Port Phillip Head. These specimens
showed ovate ceramidia, which were developed from the points of
emergence of the pectinate ramelli of the frond. Harvey had never
seen the species in fruit, but hazarded the conjecture that the cera-
midia would prove to be, as in Claudia, formed out of contracted
phyllodia ; but it will be seen that the actual phenomenon is diffe-
rent from this, and adds one more to the characteristics of the genus
Cliftonia. So far the tetrapores of this species remain undescribed.
Section of Ailsa Crag Rock.—Prof. Hull, F.R.S., exhibited a thin
section of the rock of which Ailsa Crag, at the entrance to the Firth
of Clyde, is formed. It is a grey felsitic rock, composed of crystals
Geological Society. 145
of orthoclase, grains of quartz, a few needle-like crystals of horn-
blende, and a little chlorite, all of which are set in a felsite paste.
With a high power the grains of quartz are seen to contain nume-
rous gas-cavities, remarkable for their angular and crystalline forms ;
others contain a fluid, and show a small bubble. Prof. Hull ex-
plained. the supposed origin of this remarkable rock, as having
been the consolidated core of an ancient volcano, from which the
loose materials, originally forming the sides of the voleanic cone,
had been stripped off by denudation, thus leaving the solid core
standing alone,
Staurastrum mesoleium, n. s., evhibited —Mr. Archer drew atten-
tion to a Staurastrum form, which, though not quite peculiar to
Callery Bog, seems to have its headquarters there. He had once or
twice seen it from Connemara, and he suspected it may probably be the
same as aform mentioned by Mr. Roy as having been found at Scor-
ston Moor, near Aberdeen ; but Mr. Archer had never seen examples
from there. Mr. Roy had suspected his form, at any rate, to come
near to Staurastrum oligacanthwm, non Bréb., but as once under-
stood by Herr Nordstedt; but the latter, as he since acknowledged,
is wholly a different thing from St. oligacanthum, Bréb. (rare enough
in Ireland), and he had proposed to name the Swedish form Stawr-
astrum medioleve. But the Callery form (and possibly, as men-
tioned, the Aberdeen form too) seems to be, indeed, altogether
different from the Swedish form, now to be known as St. medioleve,
Nordstedt. The Callery form is a pretty one, about medium-sized,
triangular in end view, in front view the angles a little produced,
slightly spinulose. From its resemblance (albeit distant) to, and its
association, for the time being, in our ideas, with the Swedish form
(although neither name appears very appropriate), Mr. Archer
would propose to designate the present form by the (companion)
name Staurastrum mesoleium.
GEOLOGICAL SOCIETY.
December 19, 1883.—J. W. Hulke, Esq., F.R.S.,
President, in the Chair.
The following communication was read :—
““On some Remains of Fossil Fishes from the Yoredale Series
at Leyburn in Wensleydale.” By James W. Davis, Esq., F.G.S.
After describing the nature and succession of beds among the
rocks which yielded the fossils under consideration, the author dis-
cussed the conditions under which they were deposited. He pointed
out that the Fish-fauna of the Yoredale series was distinguished by
some important peculiarities from that of the Mountain Limestone
below, as also from that of the Coal-measures. Some of the Car-
146 Geological Society.
boniferous-Limestone types are represented only by very small
specimens in the Yoredale series; certain Coal-measure fish make
their first appearance in these Yoredale beds; but a large propor-
tion of the species in the latter are peculiar to the formation.
Of the thirty-four species cited twenty are identified with known
Carboniferous-Limestone forms, namely :—Cladacanthus paradoxus,
Ag.; Physonemus hamatus, Ag.; Cladodus mucronatus and Hornet,
Davis, and C. striatus, Ag.; Pristicladodus dentatus, McC., and con-
einnus, Davis; Glyphanodus tenuis, Davis ; Petalodopsis tripartitus,
Davis ; Polyrjizodus Colei, Davis ; Diclitodus scitulus, Davis; Peta-
lodus acuminatus, Ag.; Pleurodus Woodi, Davis ; Pacilodus corru-
gatus, Davis ; Lophodus reticulatus, serratus, and bifurcatus, Davis ;
Psammodus rugosus, Ag. ; Copodus cornutus, Ag. ; and Ctenopetalus
erenatus, Davis. The Coal-measure species, Megalichthys Hibberti,
is also cited. The remaining thirteen species are described as new ;
they are :—Chomatodus lamelliformis, Sandalodus minor, Lophodus
conicus and angularis, Deltoptychius plicatus, and the following,
which are regarded as the types of new genera: Gomphacanthus
acutus, Hemicladodus unicuspidatus, Astrabodus eapansus, Cyrto-
nodus gibbus, Echinodus paradoxus, Diplacodus bulboides, Mycetodus
verrucosus, and Cercidognathus canaliculatus.
In conclusion the author noticed the occurrence, associated with
the above, of some very fragmentary remains, apparently belonging
to a Labyrinthodont, a portion of which have already been described
by Prof. Miall in the ‘ Quarterly Journal’ (vol. xxx. p. 775).
These remains consist of parts of the head and of one hind limb.
January 9, 1884.—J. W. Hulke, Esq., F.R.S.,
President, in the Chair.
The following communication was read :—
“On further Discoveries of Vertebrate Remains in the Triassic
Strata of the South Coast of Devonshire, between Budleigh Salterton
and Sidmouth.” By A. T. Metcalfe, Esq., F.G.S.
The author gave a brief stratigraphical account of the Triassic
rocks of the coast. He then described some vertebrate remains,
consisting chiefly of portions of jaw-bones with teeth in line, pro-
bably of Labyrinthodonts, found in the Upper Sandstones ( Ussher’s
classification) at High Peake Hill, near Sidmouth, by H. J. Carter,
Esq., F.R.S. At numerous places between Budleigh Salterton and
Sidmouth Mr. Carter and the author had found a large number of
isolated bone fragments. Such fragments had been submitted to a
microscopical examination by Mr. Carter. In some specimens the
bone structure was visible throughout; in some the bony portion
had been partially removed and replaced by an infiltration of
mineral matter; in others the removal of the bony portion was
complete. From these facts the author drew the conclusion that a
comparative abundance of vertebrate life was maintained during the
Miscellaneous. 147
Triassic period ; and that the rareness of Triassic fossils was due not
so much to the paucity of animal life during that period as to the
fact that Triassic strata afforded no suitable conditions for the pre-
servation of organic remains.
MISCELLANEOUS.
On the so-called Dimorphism in the Genus Cambarus.
By Watrter Faxon.
Tue existence of two forms of the adult male in all the species
of the genus Cumbarus was discovered by Louis Agassiz and Henry
James Clark. The differences between the two forms affect more
especially the first pair of abdominal appendages, organs concerned
in the act of coition, but also extend to the general form and sculp-
ture of the body. In one form (unhappily called by Dr. Hagen the
“second form’’), the first pair of abdominal appendages have a
structure nearly like that seen in all young males. The hooks on
the third joint of the third (in some species of the third and fourth)
pair of legs are small, and in the sculpture of the shell and shape of
the claws this form approaches the female. In the other form
(Hagen’s “ first form”), the articulation near the base of the first
pair of abdominal appendages is gone, and the whole member is
much more highly specialized, the terminal hooks being horny, more
widely separated, and in every way more highly developed; in
those species with bifid tips to these appendages the branches are
longer, slenderer, more widely separated, and stiffer; the hooks on
the thoracic legs are longer and more perfectly finished ; the sculp-
ture of the whole body is more pronounced, and the claws are larger
and more powerful. No intermediate conditions are found, and
there is no relation between these forms and the size of the indivi-
dual, the ‘‘ second form ” being large and the “first form” small,
or vice versd. Hence we are forbidden to interpret the two forms
as stages in ordinary development. Dr. Hagen has shown that in
individuals of the “second form” the internal generative organs are
smaller than in the “first form,” but having only alcoholic material
he was unable to determine any thing concerning the presence or
absence of spermatozoa. He interprets the facts asa case of dimor-
phism, and surmises that the “second form” males are sterile
individuals.
In the autumn of 1875 I received a lot of living Cambarus rusti-
eus, Girard, from Kentucky, males of the “ first form” and females,
which bred freely in confinement. After pairing, three of the males
moulted, and were thrown, while in the soft-shelled state, into
alcohol, together with their exuvie. An examination of these
Specimens now reveals the fact that the soft-shelled specimens are
148 Miscellaneous.
all of the “ second form,” their exuvice of the “first form”! After
attaining the “first form” and after pairing the same individual
has reverted to the “second form.” It is now clear that we are
not dealing with a case of true dimorphism, such as is well known
among insects and plants, but it appears probable that the two
forms of the crayfish are alternating periods in the life of the indi-
vidual, the “first form” being assumed during the pairing-season,
the ‘second form ” during the intervals between the pairing-seasons,
It is to be inferred that before the animal is again capable of repro-
duction another moult will bring it again into the “ first form.”
The fact that large collections, made at one time and place, often
contain only one or a great preponderance of one form of the male
is now explained.
I have also before me a male specimen of Cambarus propinquus,
Girard, from Wisconsin, belonging to the Peabody Museum of Yale
College, which was taken in the act of moulting. The old shell is
‘first form,” the soft shell emerging from it is ‘ second form.”
It is remarkable that two forms of the male have not been
detected in any other genus of crayfishes.
Fritz Miller (‘ Fiir Darwin’) has pointed out the existence of two
forms of the male in the genera Yanais and Orchestia, which he
considers as truly dimorphic forms. It is possible that these are to
be explained in the same way as the two forms of the male Cam-
barus.
Such a change as this connected with the reproductive period is
unparalleled, so far as I know, among the Invertebrata, and even
among the Vertebrata ; the cases of partial atrophy of the genera-
tive organs or shedding of antlers (as in the stag) after the rut is
over are hardly comparable.
At the time I had the specimens alive my attention had not been
drawn to the questions relating to the two forms of the males, so
that I failed to make anatomical examination, and the specimens
have now lain too long in alcohol to be serviceable for internal
dissection. I hope, however, that naturalists who are more
favourably situated will be able to throw more light on this subject.
I will add that the males of extraordinary size which I have seen
are all of the “ first form.” Do these very old individuals cease to
moult? Do they become permanently capable of reproduction ?—
Amer. Journ. Sci., January 1884, p. 42.
Museum of Comparative Zoology,
Cambridge, Mass.,
Noy. 12, 1883.
On Visual Organs in Solen. By Dr. B. SHarpe.
Dr. Benjamin Sharpe called attention to a remarkably primitive
form of visual organ that he had discovered in the siphon of Solen
ensis and S. vagina (the common “ razor-shell ”’).
His attention was directed to the probable possession of visual
Miscellaneous. : 149
organs by observing a number of these animals which were ex-
posed in large basins for sale at Naples. A shadow cast by his
hand caused the extended siphons of the specimens on which the
shadow fell, instantly to retract, while those not in the shadow re-
mained extended. Repeating this experiment at the Zoological
Station at Naples, and being fully convinced that the retraction
was due to the shadow and not to a slight jar which might have been
the cause, he was led to examine the siphon more closely, and he
also made a series of vertical sections for the purpose of very minute
study.
When the siphon of a large Solen is cut open and examined, a
number of fine blackish-brown lines or fine grooves are seen. These
are situated between and at the base of the short tentacular pro-
cesses of the external edge of the siphon. As many as fifty of these
little grooves were found to be present in some specimens, and some
of them were from | to 1°5 millim. in length.
When a vertical section is examined these pigmented grooves are
distinctly seen, and the cells of which they are composed are very
different from the ordinary epithelial cells which cover the more
pigmented parts. These latter cells are ordinary columnar epithelial
cells with a large nucleus which is situated near the tunica on which
it rests. The pigmented cells are from one third to one half longer
than those just described, and consist of three distinct parts. The
upper part, or that part furthest from the tunica, appears perfectly
transparent and takes up about one ninth or one tenth of the total
length of the cell; this part is not at all affected with the colouring-
matter used in colouring the whole. The second part of the
cell is deeply pigmented and consequently opaque; it is filled
with a dark brown or almost black granulated pigment; this takes
up about one half of the length of the cell. Below this is the third
part of this cell, consisting of a clear mass, which takes a slight tinge
when coloured ; this is probably the most active part of the cell; in
this is imbedded the large oval nucleus. This nucleus is sharply
demarcated and is filled with a granulated matter, which takes a
dark colour in borax carmine, as do, indeed, the nuclei of all the
epidermal cells.
These retinal cells, if they may be so called, are similar to those
described by P. Fraisse in 1881 (Zeitschr. f. wiss. Zool., Bd. xxyv.), in
the very primitive eye of Patella cwrulea, the principal difference
being that in Patella the transparent part at the top of the cell
seems to be a little more extensive. This eye of Patella is open,
being merely an invaginated part of the epidermis, and has no lens,
In Haliotis tuberculata we find an open eye also, but with the addi-
tion of a very primitive lens. The next higher grade of eye seems
to be that of Fisswrella rosea, in which the eye is closed and pos-
sesses also a lens; now in these two latter forms, where we find a
lens present, the retinal cells do not possess the transparent ends
we find in Patel/a and Solen, but the pigment fills the upper part
of the cell quite to the top. This would indicate, he thinks, that the
transparent part took the place of a lens,
150 Miscellaneous.
No special nerve-fibres could be detected passing to these pig-
mented grooves. Nerves passing to the eye of Patella were also
wanting; while, on the other hand, distinct veins were found
passing to the eye of Haliotis and Fissurella.
He further stated that this power of distinguishing a shadow
would be of great use to the animal in the struggle for existence.
The Solen lies buried perpendicularly in the sand, and allows the
siphon to project a little above the surface. This projecting part
would, probably, frequently be bitten off by fishes, were it not for
the fact that the shadow of the enemy would give warning, so that
the siphon could be withdrawn in time to save it from destruction.
—Proc. Acad. Nat. Sci. Philad., Nov. 6, 1883, p. 248.
On a Nematode Parasitic on the Conmon Onion.
By M. Joannus Cuatin.
It is well known that the parasitism of the Nematoda is exerted
not only at the expense of animals, a certain number of these worms
attacking various plants, in which they give rise to more or less
serious alterations. The Anguillula of mildewed wheat has been very
long known ; an allied species, parasitic on the coffee-tree, has been
studied by M. C. Jobert ; and other worms belonging to the same
group are observed in Dipsacez, Mosses, &c., as [ took occasion to
state in a communication dating some years back.
The worm which forms the subject of the present note lives as a
parasite in the common onion (Alliwm Cepa, Linn.), and becomes in
it the cause of a disease of which I have been able to trace the
different phases, thanks to the extreme kindness of M. Pasteur, who
sent me, in May 1881, a portion of a bulb infested by these Nema-
todes. I have been compelled to defer the publication of the results
of my researches on account of the time necessary for tracing the
development and the mode of propagation of the worm, apprecia-
ting exactly its vital resistance &. Even now I shall confine
myself to a summary of the principal points of its history ; the ana-
tomical and embryogenic details &¢. must find a place in a more
extended work.
By its general characters and especially the construction of its
digestive tube, as also by the organization of its reproductive ap-
paratus, the Anguillula of the onion must be classed in the great
genus Z'ylenchus, and every thing authorizes our thinking that it
represents a species distinct from those which have hitherto been
described.
It is in the larval state that the worm penetrates into the bulb,
which it attacks at the level of the “ fundamental axis;” then it
spreads into the roots and to the base of the flowering stem, gene-
rally respecting the external tissues, but completely disorganizing
the central tissue, even getting into the fibro-vascular bundles and
reducing them to a brownish pultaceous mass, in which nothing but
a few fragments of spiral vessels is soon to be observed.
Miscellaneous. 151
The Anguillula then attains its full development, the sexual
organs, sketched out in the larva, rapidly complete their formation ;
fecundation takes place ; and from the ova issue the young clayi-
form larvee, which are speedily set free by the disaggregation of the
bulb. They creep about in the surrounding soil, that is, if the
latter is sufficiently damp ; in the contrary case they remain dried
up and in a state of latent vitality, until the moment when favour-
able conditions permit them to revert to active life. On arriving in
the neighbourhood of a normally developed Alliwm they penetrate
into it, as above stated, and the cycle recommences.
In this way is explained how the same bulb contains at the same
time adults, ova, and larvee, and also how the parasite can be trans-
mitted with the greatest facility from one plant to another, and how
itis rapidly propagated through a whole plantation. As to the propa-
gation through the floral organs &c., this is rare, the Anguillula only
attaining them with difficulty, and this, indeed, precisely on account
of the initial injuries which it causes in the bulb, and the effect of
which is to arrest the development of the flowering-stem or to dry
it up quickly.
The larvze present a faculty of revivification analogous to that ob-
served in the larve of the Anguillula of mildewed wheat; but it
would seem that here this faculty is less powerful. I have, how-
ever, been able to ascertain it in larve preserved for twenty-six
months in a dry well-corked bottle; beyond this period I have only
obtained negative results. The adult Anguillulee, subjected to desic-
eation, perish quickly, as is also the case when they are exposed to
a cold of —10° (=14° F.), which has no action on the larve.
Acidulated water and dilute alcohol instantly kill the adults, while
the Jarvee retain their vitality in them for some time.
These facts are obviously comparable to those observed in the case
of the Anguillula of mildewed wheat, but the onion-parasite con-
stantly manifests a smaller vital resistance. There is only one
exception to be made in this particular:—M. Davaine has shown
that the Anguillula of the mildewed wheat when introduced into
the digestive canal of fishes, batrachians, and reptiles remains intact,
whereas if the experiment be repeated with birds or Mammalia the
worm is soon digested. Now the Anguillula of the onion does not
undergo any alteration in this same medium, and is to be met with
again, distinctly characterized, either in the dejections or in the con-
tents of the intestine, if the animal has been killed shortly after the
ingestion of portions of the plants containing the worms. One
might thus be exposed to the error of regarding them as true para-
sites of the host into which they have been accidentally introduced,
and in which they cannot acquire any development or undergo any
encystation, as I have clearly ascertained.
The agents employed against the Anguillula of mildewed wheat
may be used against the parasite of the onion ; but the most effica-
cious process consists in pulling up the diseased plants and burning
them.—Comptes Rendus, December 24, 1883, p. 1503.
152 Miscellaneous.
Evidence of a Protozoéa Stage in Crab Development.
By H. W. Conn*.
There is great interest attached to speculations as to the probable
ancestry of the Decapods, owing to the value which the conclusions
have in enabling us to interpret paleontological facts. There have
been quite a number of theories advanced as to the original stem
from which the Decapods have been derived, two of which claim
especial attention. One is the theory of Miller, who finds such a
stem-form in the zoéa. Another, suggested by Glaus, or in a diffe-
rent form by Brooks, considers the protozoéa as the ancestral stem.
It is of great importance in understanding the Crustacea to decide
between these two views, inasmuch as by the first view Crustacea
are supposed to have descended from a form without a thorax, while
according to the second, the thorax was present in the original
Decapod stem. Some work done at Hampton during the last summer
upon the larval cuticle of crabs indicates conclusively that the latter
view is the correct one, or that at least Fritz Miiller’s view is in-
correct. The larval skin, particularly the telson, of a large number
of crab zoéas was studied with the following results :—The larval
skin is not in different crabs alike, nor is it in any case exactly
similar to the enclosed zoéa. There is always an indication, more or
less complete, of some previously existing stage. There has been
shown in the various forms studied a gradation from the larval skin,
with little difference from the zoéa enclosed, to a larval skin which
is utterly unlike the zoéa, but which possesses a forked tail with
fourteen long feathered spines. This gradation is complete, and a
study of the different embryonic telsons shows that all have been
derived from the form shown by Panopeus, which has a forked tail
with fourteen spines. Now such a larval skin is to be considered
simply as the cast-off skin of some stage immediately preceding the
zoéa. It has been shown by Paul Meyer that the study of the larval
skin of Macrura leads to a similar result; that a forked tail with
fourteen spines is also seen in the early history of this group. If
therefore a form can be found which shows these peculiarities, we
have reason for accepting it as the stem-form of the higher Crus-
tacea. Now a study of the different. protozoéa-forms which occur in
the ontogeny of various Macrura shows that we have in this form
a stage which fulfils the conditions. It has the forked tail with
fourteen spines, and has large swimming antenne, another pecu-
liar characteristic of the crab larval cuticle. If the various larval
skins of crabs and Macrura be compared with each other, it will be
seen that they are all to be ccnsidered as modifications of a tail
much like that present in the larval skin of Panopeus; and if this
tail be compared with the protozoéa-tail of Peneus, the likeness will
be seen to be very striking. We have therefore, in the comparative
study of the larval cuticle of crabs, good reason for accepting as the
stem-form of the Decapods a form which had resemblance to a pro-
tozoéa.—Johns Hopkins University Circulars, Jan. 1884, p. 41.
* Abstract of a communication to the University Scientific Association,
November 7, 1888.
THE ANNALS
AND
MAGAZINE OF NATURAL HISTORY.
[FIFTH SERIES.]
No. 75. MARCH 1884.
XVIII.— On Grantia ciliata, var. spinispiculum, Crer.
By H. J. Carter, F.R.S. &e.
[Plate VIII. ]
HAvInG lately (September 1883) had occasion to collect a few
of the Calcispongiz which grow upon the rocks and seaweed
about this place (Budleigh-Salterton, South Devon), I found
it necessary to refer to Dr. Bowerbank’s ‘ Monograph of the
British Spongiade’ to ascertain if I had among them any
specimens of the Granta ciliata illustrated in his third vol.
(pl. 11. figs. 1-15), which appears to me to be typically that
described and illustrated by Dr. Johnston in his ‘ History of
British Sponges’ (p. 176, pl. xx. fig. 4, and pl. xxi. figs. 6
and 7). Of this the type specimen is in the Johnstonian
collection in the British Museum (no. 30, registered 47. 9. 7.
79), evidencing Montagu’s remark respecting this sponge,
which Johnston has quoted, viz. “ that the specific character
of being ‘ surrounded at top by a crown of spines’ is rarely
identified” (op. et loc. cit.). This is also shown in Dr.
Bowerbank’s illustration (op. et loc. cit. pl. ii. figs. 1 and 3) ;
but in his description of this species (op. c7t. vol. ii. p. 24)
he refers for further particulars to his first paper on “‘ The
Organization of Grantia ciliata,” viz. that in the ‘'Transac-
Ann. & Mag. N. Hist. Ser. 5. Vol. xiii. 11
154 Mr. H. J. Carter on Grantia ciliata,
tions of the Microscopical Society’ (vol. vii. p. 79, pl. v.),
where the illustrations of the entire sponge (figs. 1 and 2) are
quite different from those in the third volume of his ‘ Mono-
graph.’
These differences were observed by Hiickel in 1870, when
he made two species of them under the name of Sycandra
ciliata for the former and S. coronata for the latter (‘ Die
Kalkschwamme,’ vol. ii. pp. 296 and 304, and ‘ Atlas,’ Taf.
li. and lviii. and Taf. li. and 1x.). But it does not seem to have
influenced Dy Bowerbank in 1874, although the Rev. A. M.
Norman, who edited the posthumous volume of his work (vol.
iv., 1882), adopts the separation (p. 230).
However, after carefully reading and comparing Hiickel’s
description of Syeandra (Grantia) ciliata, S. coronata, and S.
rapnanus respectively (vol. ii. p. 296 et seqg.), together with
the specimens of the two former found here, it appears to me
_that they run into each other in such a way that, although
there may be grounds for making a separate species of the
latter, I, with the late Dr. Bowerbank, see none for separating
specifically the two former. The differences that exist be-
tween Sycandra ciliata and 8S. coronata appear to me to arise
chiefly from the circumstances under which they have grown,
viz. whether this has taken place in strong currents or com-
paratively still water, which, on account of the extreme
brittleness and delicacy of the finer and longer spicules on the
surface ot the body, leads to their being more or less broken
off. If these spicules have been, retained entire, they are
generally so matted together in the dried specimen as to ob-
scure the conuli from which they proceed and thus give the
surface of the body a shaggy (‘ zottig,’’ H.) character; while
those of the peristome or mouth may be more or less worn
away, thus corresponding with Johnston’s type specimen, Dr.
Bowerbank’s illustrations (vol. ii. 7. c.), and my own expe-
rience here ; but if, on the other hand, the finer and longer
spicules of the conuli have been broken off, while the shorter
and stouter ones which succeed them inwards remain, which is
generally the case, then the conuli will of course be exposed,
and the peristome remaining intact, we shall get a specimen
like that represented by Dr. Bowerbank in the ‘ Transactions
of the Microscopical Society’ (/. c.), the former being Hiickel’s
_ Sycandra ciliata and the latter his S. coronata. As to spe-
cific differences being deduced from themeasurements of spicules
and even the entire forms themselves of sponges, these are go
variable generally that it is only here and there that they
afford any trustworthy evidence.
But there is a difference in structure between Sycandra
var. spinispiculum, Ctr, 155
etliata and SS. coronata on the one hand and S. raphanus on
the other, which may, if constant, claim specific distinction
for the latter; I allude to the prismatic form of the radial
chambers in S. raphanus, whose transverse section made lon-
gitudinally to the body, midway between the surface of the
cloaca and the conuli, presents a hexagonal arrangement with
triangular spaces between the hexagons, first noticed by
Hickel in his synoptical table of these sponges (op. e7t. vol. il.
p- 294), while in Sycandra ciliata and 8S. coronata a similar
section shows the chambers to be c¢rcular or cylindrical. How
far this is sufficiently persistent to justify specific separation
I am not prepared to state.
Carefully comparing Hiickel’s description of Sycandra ra-
phanus with the species that prevails here, which in all re-
spects agrees with that from the north of Shetland which I
have named “Grantia ciliata, var. spinispiculum ” (“ Sponges
dredged on board H.M.S. ‘ Porcupine,’”’ ‘ Annals,’ 1876,
vol. xviii. p. 468, pl. xii. figs. 6 and 7), I can see no differ-
ence between the two except in the presence of the spiniferous
spicules in the latter, to which I shall presently allude, but
which Hiickel does not notice at a// either in his descriptions
or illustrations, although F. E. Schulze a few years later
illustrated and described them particularly in Sycandra ra-
phanus (Zeitschrift f. wiss. Zoologie, 1875, Bd. xxv. 3es
Suppl. pp. 254 and 255, Taf. xix. fig. 1, a-d).
Now the fact of such spinous spicules having been found in
Sycandra raphanus compared with their presence here in
Grantia spinispiculum, whose structure otherwise corre-
sponds exactly with Hiickel’s description of the former,
leads me to infer that Grantia spinispiculum and Sycandra
raphanus are the same, while the prismatic form of their
radial chambers (and, perhaps, the spiniferous spicules) alone
distinguishes them from Sycandru ciliata and S. coronata.
It is the identity or not of the two former which I wish to be
confirmed, as | de not possess a type specimen of Sycandra
raphanus from the Adriatic for comparison ; and therefore shall
give hereafter an illustrated description of Grantia ciliata, var.
spinispiculum, in all its principal detail, not only for this pur-
pose, but to illustrate the variety itself, which hitherto has not
been done.
In alluding to the acerate spicules which form the outer
layer of the “collar-ring ” noticed by Lieberkiihn in “Grantia
ciliata sive Sycon ciliatum” (Archiv f. Anat. u. Physiologie,
July 1859, Heft iii. p. 373), and subsequently by Bower-
bank (Trans. Microscop. Soc. J. c. p. 82), Hiickel observes
(op. cit. vol. ii. p. 308) that they are not to be ny Grantia
156 Mr. H. J. Carter on Grantia ciliata,
ciliata (“bei S. celiata feilen ”’), which I fancy must be a mis-
take,asfrom microscopical examination of specimens now before
me | must agree with Lieberkiihn and Bowerbank in affirm-
ing that the collar-ring (“ Halsring,”’ H.) in all three (that
is including S. raphanus) commences where the conuli on the
surface outsede, and therefore the oscules of the radial cham-
bers on the surface of the cloaca cnside, cease and ends where
the corona proper or circle of long, straight, setaceous, simple
spicules commences (PI. VIII. fig. 2, 4), and that this layer of
comparatively thick acerate spicules externally may be more or
less present, according to the wear and tear above noticed to
which the specimens may have been subjected. How far we
may be justified in identifying with Sycandra raphanus the
specimens of Grantia ciliata, var. spinispiculum, which I have
lately found here, the following illustrated description, as above
suggested, may determine.
Granita ciliata, var. spinispiculum. (PI. VILE. figs. 1-8.)
Pyriform elongated, fixed by the small end to the object on
which it may be growing, terminated at the large or free end
by an asbestine glistening pencil of long straight spicules ;
conulated over the surface, which is also ciliated with fine
long spicules, inclined forwards and often presenting an asbes-
tine sheen, like that of the pencil of spicules at the free end ;
more or less inflated and bent upon itself, often dividing
into two heads, that is bigeminate (Pl. VIII. figs. 1 and 2).
Colourless or transparent white. Consistence fragile. Sur-
face uniformly covered with conical processes in juxtaposition
(fig. 2, aaa), whose framework is composed of triradiate spi-
cules, terminating towards the point of the cone in a slightly
extended ray, which, intermingling with a bunch of linear
spicules consisting of fifty or more of variable length, alto-
gether forms the ciliary covering of the body just mentioned.
“ Bunch of linear spicules’? composed of six forms, viz. :—1,
extremely slender, almost immeasurably thin, straight,
smooth, almost imperceptibly -tapering outwards from an
equally slight enlargement of the proximal end, in shape
something like knitting-needies (‘“ Stricknadeln,” H.), in
bundles scantily dispersed among the larger acerates, variable
in length, averaging perhaps about 1-85th inch long, but
seldom found entire from their delicacy. 2, short, fusiform,
shghtly curved and spined over one or both sides of the distal
portion, which is terminated by a short smooth spur turned in
the opposite direction, varying in length about 1-461st of an
inch, which is that of the shortest observed (fig. 3, ¢). 3,
var. spinispiculum, Crér. 157
short straight acerates, minutely spined or serrated also over
their distal portion, sharp-pointed, or terminated by a pin-like
inflation at. the distal end; shortest form seen about 1-300th
of an inch (fig. 4, ¢ and d). 4, long, straight, smooth,
slightly tapering from a more or less slightly enlarged lanceo-
late or simply pointed proximal end to a curved free extre-
mity, about 1-300th inch in length, serrated over the convexity
and ending in a sharp smooth spineless point, which is turned
in the opposite direction ; serratures more or less distinct and in
many instances evidently directed outwards, diminishing in
size towards either extremity, the whole spicule varying
in length from 1-461st of an inch, which is that of the
smallest above mentioned, to 1-6th inch, which may be the
maximum length of the longest (fig. 3). 5, like the last
in form, but straight throughout, terminating in a very fine
point, serrated on one side only, in two approximated broken
lines, for about the same length as the foregoing, but with the
teeth much larger and directed ¢nwards, diminishing in size to
the distal extremity as they increase in size in the opposite
direction; length variable, viz. from about 1-300th of an inch,
which is that of no. 3 above mentioned, to 1-25rd inch, which
is the maximum of that observed (fig. 4). 6, gently curved
once or twice, variable in length, but much shorter than the
foregoing ; smooth and pointed in the imner or proximal por-
tion, serrated and abruptly or capitately terminated at the
other; teeth as in the foregoing, on one side only, recurved
and arranged in two approximated broken lines extending
backwards for about 1-3338rd inch from a slightly inflated head
with 0-3 spines, directed backwards like the anchoring-spicule
of Euplectella ; length of longest observed about 1-36th inch
(fig. 5). All these forms in jront of the stem are directed
forwards, and in all not only is the length very variable, as
may be seen from the measurements above given, but the ser-
ration or spination and general form also are much modified,
especially in the smaller kinds (nos, 2 and 3), while in the
larger and longer (nos. 4 and 5) they are more persistent ; and
while no. 4 prevails towards the larger end of the body, the
more distinctly spined or toothed spicules, nos. 5 and 6, to-
gether with 2 and 3, prevail towards the root. Peristome,
vent, or mouth, as it has unfortunately been termed, composed
of two portions, viz. a “neck ” or “ collar” (fig. 2, 2) and a
“crown” (fig. 2, g), the “collar” consisting of a contracted
portion of the body about 1-G60th inch in longitudinal dia-
meter, naked or uncovered by the conuli, which do not extend
further forward than this point, and thus the distinction is
clearly defined ; composed outside of a layer of stout, smooth,
158 Mr. H. J. Carter on Grantia ciliata,
slightly curved, fusiform, sharp-pointed acerates, about as
long as the collar is broad (fig. 2, 2), arranged longitudinally
side by side, with their convexities inwards, and supported
inside by a layer of tri- and quadriradiate spicules con-
tinuous with that of the surface of the cloaca, and equally
armed by the projecting spur of the quadriradiate, although
of course deficient in the holes of the radial chambers, which
cease at the commencement of the structure externally and
internally. ‘ Crown” consisting of a circular row of long,
straight, smooth, almost cylindrical spicules, about 1-18th inch
in length, arranged longitudinally side by side, tapering
slightly towards their free extremities from an equally slightly
enlarged and pointed end which penetrates for some distance
the distal margin of the collar, and on issuing thus forms a
fringe or pencil of setaceous spicules that, when together, pre-
sent the asbestine sheen above noticed, and, finally, may beex- |
panded or approximated as required. Internal or body-
structure (fig. 2, ee) composed of radiating prismatic chambers
in juxtaposition, which extend transversely from the conuli that
form their extremities on the surface to that of the plane of the
cloaca internally (fig. 2, £7), supported throughout by the inter-
lacing of tri- and quadriradiate spicules, which are so disposed
in their courseas to present a hexagonal form separated by small
triangular interspaces externally (fig. 2,dd), and on the surface
of the cloaca, so as to leave a number of holes corresponding in
regularity to the chambers of the body (fig. 2, m), each of which
is provided with a sphinctral diaphragm of sarcode just inside
the margin (fig. 6,). Stem (fig. 2, 7) very variable in length,
often obsolete, composed of a solid cylindrical mass of the
tri-, quadriradiate, and linear spicules above mentioned, ex-
tending from the bottom ofthe cloaca to the object on which
the sponge may be growing, and, of course, as destitute of
the conuli and the radial chambers as the collar of the peri-
stome. Root (fig. 2, 4) presenting a group of tri- and quadri-
radiate spicules, from each of which an arm of variable length,
below 1-60th of an inch, is considerably extended backwards
and longitudinally, tapering at first and then ending in a more
or less inflated lanciform extremity ; surrounded by a fringe
of short and long spiniferous or toothed spicules recurved or
directed backwards, such as have been described under nos. 3,
5, and 6, most of which, but especially the latter (whose
proximal ends are more or less lanceolately inflated, their
length greater, and their teeth larger than those about the
body), have their extremities fixed in their own or the indu-
rated sarcode of some other neighbouring organism, which ad-
heres to the rock (fig. 8) and thus forms the ‘‘ root” or final
var. spinispiculum, Crtr. 159
bond of attachment. Pores in the spaces between the conuli
on the surface (fig. 7,4). Hxcretory canal-system consisting of
the radial chambers, which have been described before as open-
ing into the cloaca through sphinctered apertures (fig. 6, ad),
and the cloaca itself, which, occupying the centre of the body,
consists of a cylindrical cavity corresponding in shape with the
specimen, that is, narrow behind and wide in front, commen-
cing in a blind point close to the stem, and ending in a wide
mouth at the collar (fig. 2, 7/1); surfaced uniformly with circular
holes, which are the oscular vents of the radial chambers
above mentioned, arranged with corresponding regularity
(fig. 2,m), and would be in juxtaposition but for the inter-
vention of the spicular structure of the body, from which pro-
jects the fourth arm of the cloacal quadriradiates that are curved
and directed forwards (fig. 2,) ; limited in front by a sarcodic
. sphincter which separates the collar from the cavity of the
cloaca. Size of specimen variable according to age and situa-
tion ; average of that above described, which grows a little
below high-water mark on the rocks here (fig. 1), about
4-12ths inch long by 1-12th inch in its broadest part, not in-
cluding the lateral spicules, which, as above stated, vary under
1-6th inch in length.
Hab. Marine. On Fuct near low-water mark, or abun-
dant on the under surface of New Red Sandstone rocks a little
below high-water mark. In company with an equal abun-
dance of the following Calcispongix, viz. Grantia clathrus,
G. compressa, Leuconia Johnstonit, L. fistulosa, and Leucogyp-
sia Gosset, together with the common littoral siliceous sponges
Halichondria panicea and H. sanguinea.
Loc. Budleigh-Salterton, south coast of Devon.
Obs. It is evident that a longitudinal section of the body
across the radial chambers of this variety shows, as Hiickel
has stated respecting Sycandra raphanus (op. et loc. cit.), that
its chambers are ‘‘ hexagonal”’ in contradistinction to those
of Grantia (Sycandra) ciliata and G. (S.) coronata, which are
circular; but, as before stated, what these differences may
amount to from a specific point of view, as they may easily
graduate into each other under the circumstances, | am not
prepared to say ; nor am I able to state how far the longer
spicules with spinous extremities may be absent in these two
forms, as Hiickel does not mention any, and my own speci-
mens, which are all dry, fail to show them ; for they are either
broken off or so inextricably clotted together by hardened
sarcode as to defy all attempts at disassociation; but the
spines certainly do not appear on the shorter linear ones of the
cone specimens which remain in these, while they do so on
160 Mr. H. J. Carter on Grantia ciliata,
most of the shorter linear ones of Grantia spinispiculum,
although even here there may be an admixture of both kinds.
At the same time long, stout, terminally curved spicules of a
similar form, but smooth throughout (that is, without spines
and not so much bent at the ends), may be more or less plenti-
ful in the conular “ bunches” of Grantia ciliata and G’. coro-
nata; wherein the chief differences between these and those of
the variety G. spinispiculum appear to me to consist.
The capability of entirely closing the cloaca, which is essen-
tially the “rectum” or termination of the excretory canal-
systems in a// hollow sponges, whether calcareous or siliceous,
by the extension of a sarcodic, sphinctral diaphragm across
the mouth at the junction of the body with the collar-ring,
first noticed by Bowerbank in Grantia ciliata (Trans. Micros.
Soc. 1859, vol. vil. p. 83), although not so plainly seen as
that provided for the opening of each radial chamber into the
cloaca, together with the relationship of the ends of the cones,
which, although closed in the dried state by a kind of spiral twist
of the linear spicules (“ monoceles,’’ H.) around their apices,
respectively, would appear to have an opening here in the
living one, is a mechanism which I cannot understand, seeing
that the inhalent channels which lead to the chambers are on
their outer side, as distinctly indicated by the pores themselves
in the triangular interspaces between the conuli on the surface
(Pl. VIL. fig. 7). That the single tubular vent projected
from the young Spongilla when grown from the statoblast
does close up for a time after a surfeit of carmine, I have long
since witnessed and described (‘ Annals,’ 1857, vol. xx. p. 30,
pl. i. fig. 1); and if the sphinctral membrane at the base of
the collar-ring acts in connexion with the conuli and sphinc-
tral diaphragms of the radial chambers in Grantia ciliata
and its varieties, they being all parts of the excretory canal-
system, then the same kind of general closure may take
place as in the young Spongilla under similar or other cir-
cumstances.
To attempt to describe all the varieties of form in the
spicules of the sponge would be vain, from their great number,
hence they can be only learned by a practical examination.
To assign the use of the spined spicules too would appear to
be wholly conjectural from their almost general distribution
over the whole surface of the body, had we not a parallel case
in the young spherical G'eodia &c., wherein the anchoring-
spicules (“‘ anchors” and “ forks”) are developed over the
whole of the surface, but for the most part only retained in a
projected state where the Geodia is nearest to the object to
which it may be attached, when they come into use for
var. spinispiculum, Ort. 161
‘ anchoring-purposes, while those in the more exposed parts
are more or less broken off. Such appears to be the case in
Grantia ciliata, var. spinispiculum, 'Vhe capitate spiniferous
or denticulated spicules (Pl. VIII. fig. 5) would appear to
be particularly adapted for this purpose; but they are by no
means so numerous as the pointed ones (fig. 4), neither are
they a bit more confined to the root, while the capitate portion
itself appears to arise from a modification of the end of the
spiniferous portion of fig. 4, in which the substance of the
latter becomes retracted into an inflation, which may be simply
round (‘ Annals,’ 1876, vol. xvii. pl. xu. fig. 8), or provided
with two or three recurved spines like that of the anchoring-
spicule of Huplectella, as above stated. Hence I cannot agree
with Schulze (Zeitschrift f. wiss. Zool. Bd. xxv. 3es Suppl.
. 255) in deriving this from a quadriradiate spicule.
The hardy nature of the Calcispongiz, which are so much
more fragile and delicate in structure than the siliceous sponges,
is very remarkable here, where the roof of the cavern in the
New Red Sandstone rock at “ Straight Point” is just now
absolutely covered with a mixture of all the species above
mentioned, together with the siliceous species, viz. Halichon-
dria panicea and H, sanguinea, Johnst., although it is only a
few feet below high-water mark, and must be wholly uncovered
by the sea for several hours twice a day, during which, of
course, the sponges are kept wet by the dripping from the
rock of the sea-water, which has also twice a day been ab-
sorbed during the time that it has been under water. Thus,
high-water mark is not less characterized by the well-known
littoral siliceous species with linear, than calcareous sponges
with triradiate spicules.
I would here remark that to examine satisfactorily Grantia
ciliata, var. spinispiculum, great delicacy of manipulation is
required, otherwise most of the long spicules will inevitably
be broken off, if they have not already suffered much in this
way by the waves in their natural element. Thus it will be
found advisable to bring away a.portion of the rock on which
they are growing and place it in spirit then or afterwards, to
examine this carefully under water at home, to raise the root
with a spatuliform needle most carefully, and to transfer to a
slide for microscopical examination or subsequent mounting in
balsam (N.B. which does not show an acid reaction with test-
paper) the parts that are required, by means of capillary attrac-
tion, through a pipette. In this way the spiculation may be
seen in situ; but when the entire spicules of different parts
are required, then such portions of the body as might yield
them are to be boiled separately, in liguor potasse, until they
162 On Grantia ciliata, var. spinispiculum, Cr¢r.
become disintegrated ; the liquor poured off and the residuum
in the watch-glass washed twice only with pure water, most
carefully draining throughout, lest the minute spicules be
carried away by the edulcoration ; then the last drop containing
the spicules should be transferred to a glass slide and drained
again, but not to perfect dryness ; now add one or two drops
ot glycerine, and secure the whole under a large glass cover,
finally adding a little balsam at the cardinal points to keep it
from slipping. ‘This process has the advantage of preserving
all the spicules, small and great, and, from their not having
been reduced to absolute dryness, of preventing that crystal-
lization of the remaining potash around them which otherwise
would inevitably obscure their forms, while it yields a prepa-
ration which can be recurred to for deliberate examination as
long as it may be required.
P.S.—A delicate spiniferous spicule, to which attention has
not hitherto been directed, exists all over the surface of Leuco-
gypsia Gosset, often fringing the mouth too in the manner of a
peristome. It is fusiform, slightly curved, and spined proxi-
mally, chiefly over one side only, while the free extremity is
armed, bayonet-like, with a short, delicate, smooth, slightly
curved spur.
EXPLANATION OF PLATE VIII.
Note.—The representations in this Plate must (with the exception of
fig. 1, which is of the natural size) be regarded as diagrams drawn to
scale, that the reader may be able to realize as far as possible the relative
proportions of the different parts of which fig. 1 is composed. Thus fig. 2
has been drawn to the scale of about 1-96th to 1-180U0th inch, and even
here the scale is not sufficiently large to show the spines on the spicules ;
so these, viz. 3, 4, and 5, have been drawn to the scale of 1-24th to
1-6000th inch; while for perspicuity also figs. 6 and 7 are magnified to
double the size of the same parts in fig. 2,
Fig.1. Grantia ciliata, var. spinispiculum, Crtr., single and double.
Natural size.
Fig. 2. The same. aaa, body; 6, peristome and collar; c, stem and
root; dd, cones on the surface, direct view; ee, the same,
lateral view, showing their connexion with ff, the radial cham-
bers; g, peristome; A, collar; 2, stem ; k, root; ///, dotted line
showing the form of the internal cavity or cloaca; m, openings
of the radialchambers into the cloaca ; », projection of the fourth
ray of the quadriradiates of the cloaca into that cavity.
Fig. 8. The same. Spined spicule of the cone with curved free extremity,
about 1-13th inch long. a, inflated, smooth, or proximal end ;
b, curved, serrated or distal end; c, shortest form seen, about
1-461st of aninch. Teeth directed outwards.
Fig. 4. The same. Spined spicule of the cone and root, with a straight
free extremity, about 1-28rd inch long. a, inflated, smooth, or
proximal end; 4, straight, toothed, or distal end; c, shortest
On the Gemmules of Freshwater Sponges. 163
straight specimen seen; and d, shortest capitate specimen seen,
each about 1-300th inch long. Teeth directed inwards.
Fig. 5, The same. Capitate spined spicule of the cone and root, about
1-36th inch long. a, smooth, sharp-pointed, or proximal end ;
b, spined and capitate or distal end. ‘Teeth recurved.
Fig. 6. The same. Diagram of four radial-chamber vents, to show the
sarcodic sphincters in them respectively. a, vent; 6, sarcodic
sphincter.
Fig. 7. The same. Diagram of seven cones, to show the position of the
pores in the triangular spaces between them. a, cone; 8, pore.
Fig. 8, Sand-grains of the rock on which the variety has grown.
XIX .—Some Preliminary Remarks on the Gemmules of the
Freshwater Sponges. By Dr. WitttAM MARSHALL *.
Tue gemmules of the freshwater sponges, as is well known,
present in the constitution of their envelopes a series of very
remarkable peculiarities, which are very different according
to the species, and which, as adaptations, must have very
special causes and significations.
Each germ possesses, according to the species, a round or
oval, sometimes convexo-concave shell, furnished with one
opening, or (in Spongilla multiforis, Cart.) with one prin-
cipal and several subordinate apertures, through which the
mature contents issue at the proper time. The innermost
layer of this shell is a firm structureless membrane, which
Carter t describes as chitinous (‘‘ chiténous coat”), by which,
no doubt, is meant only that it is “ horny,” without reference
to its chemical constitution.
In some few kinds of gemmules this innermost simple thin
layer is alone present; in others the wall is thicker, and
appears sometimes very peculiarly modified. Thus in Spon-
gilla nitens (according to Carter’s { and my own observations)
and in 8. Cartert (according to Carter) we see that the thick
capsule is not homogeneous, nor does it show that constitution
which Carter calls “ granular cell-structure.” Under a low
power it appears in section to be finely striated radially, and
its surface, like that of the eye of an insect, appears divided
up into elegant convex equilateral hexagons ; by the employ-
ment of higher powers we discover that the lines of striation
are not the expression of hexagonal corneous pyramids di-
* Translated by W. S. Dallas, F.L.S., from the ‘ Zoologischer Anzeiger,’
1883, pp. 630-634 and 648-652.
+ Ann. & Mag. Nat. Hist. ser, 5, vol. vii. p. 85.
t Loe. cit,
164 Dr. W. Marshall on the
minishing centripetally, but that they appear zigzagged and
always so that in two neighbouring lines the opposite angles
of the zigzag have their apices either turned towards or away
from each other; and at the same time it is observed that the
angles of two horny lamellae which are turned towards one
another are united by transverse floors; in other words the
entire capsule of the gemmule consists of a system of little com-
partments inserted into each other in accordance with the three
dimensions of space, and gradually diminishing in the thick-
ness of their walls and in their dimensions from without in-
wards. ‘The superficial compartments are hollow, and in the
dry state, which alone we have here to take into consideration,
filled with air; the innermost are solid; their form is that of
a hexagonal prism terminated at each end with six faces, the
longitudinal diameter of which lies tangentially to the sphere of
the contents of the gemmule. These compartments are certainly
not modified cells, but, like the innermost independent horny
layer of the whole capsule, a cuticular formation. Their sub-
stance is structureless and very strongly refractive; it resists
calcination remarkably, becomes brown without shrivelling,
and during this process only the angle-lines stand forth
strongly, especially of the angles of the compartments in which
several walls meet together from different sides. Hydrofluorie
acid has a peculiar effect upon this substance ; by treatment
therewith it loses its strong refractive power and also some-
what of its yellowish colour, and especially its brittleness, for
which reason in gemmules treated with hydrofluoric acid we see
the radial lines of contact of the compartment-columns brought
much closer together, and the compartments, often enlarged
in aradial direction, in general, but especially in the peripheral
layers, much more irregular in form. Henceit seems to me
not improbable that a strong percentage of silica is proper to
this substance. Externally and internally the compartment-
layer of the capsule is surrounded by a system of tangentially-
placed but otherwise irregularly-arranged siliceous spicules,
beset at both ends, even as far as the middle, with fine spi-
nules curved inwards. ‘The spicules adhere more firmly to the
inner surface of the compartment-layer than to the outer surface
of the firmer horny layer in immediate contact with the
germ, which exhibits a fine concentric striation, and on the
outside fine irregularly-placed pits, the impressions of the
spinules of the inner tangential spicules. ‘This is easily seen
in sections through the gemmules, in which the inner layer
readily separates from the compartment-layer.
‘Lhe aperture of exit for the germ when awakened to life
is round, and passes through both layers of the wall; but it
Gemmules of Freshwater Sponges. 165
is furnished with a remarkable closing-apparatus, as Carter
figures it in a gemmule of S. Carter?, Bow. The envelope
immediately surrounding the inner germ separates at one spot
in such a manner as to form a globular hollow space, the outer
wall of which projects somewhat beyond the outer surface of
the compartment-layer, in the thickness of which the cavity is
situated ; therefore this alone is penetrated. If the dry gem-
mules be thrown into water they float with this capsule up-
wards, so that its surface remains out of the water. It is
only after from eight to ten days that they begin to sink; and
if, as is probable, this is the case also with the living gemmules,
the germs will only then awaken. This closing-vesicle seems
to me to be a hydrostatic apparatus ; and that it maintains the
gemmules so long at the surface of the water is perhaps not
without significance, for if they are carried by the wind into
shallow pools, which the power of the sun would soon dry up,
their contents will not issue forth before the evaporation
occurs, and will thus, by the delay that takes place, escape
destruction.
The formation of the germ-capsule will very probably take
place as follows :—the portion of the parent animal separated as
a germ first of all itself secretes on its surface a horny covering
in layers (whence the concentric striation) as a cuticular for-
mation; to this is then applied from without a system of tan-
gential spicules; and upon this again, as a cuticular formation
of the parent organism, the compartment-layer, which is finally
coated by the external system of tangential spicules. The
germ, which, as in all Spongille, consists in the dry state for
by far the greater part of starch-corpuscles (probably reserve
nutritive material), as already described and figured by Carter,
is in this way admirably protected, but at the same time also
in other respects most advantageously endowed.
The gemmules in S. nitens are remarkably small (as also
in S. Carterd), and therefore light, and all the lighter because
the comparatively thick enveloping capsule contains such
numerous cavities. ‘The importance of this remarkable archi-
tecture of the capsule in my opinion lies in this, that by it the
gemmules will find the widest possible distribution under the
circumstances in which the stock or parent Spongilla appears
to exist—the light capsule enclosing air-spaces acts as an
aerostatic apparatus !
The Spongille in question which break up into such gem-
mules are inhabitants of hot countries; they will frequently
be liable, under the influence of the glowing sun, to be laid
dry : most of them when this happens will die away ; but they
live on in the parts of themselves in the protected gemmules,
166 Dr. W. Marshall on the
which precisely in these species escape very easily from the
dead Spongilla, with which they are not in the least united.
The wind will take them up, scatter them here and there over
the great plains of Africa &c., and deposit them in dried-up
watercourses, in which they will be found by the vivifying
element at the commencement of the rainy season. This is
not contradicted by the fact that others come to rest in peren-
nial fresh waters and develop there; many will be carried
far away to islands and from land to land, many will get into
the sea and never fulfil their destiny ; but if, out of their great
number, the greater because they are so small, only a very
small percentage arrives at development, the preservation of
the species is thereby abundantly assured.
What a means of transport for organic substances the wind
is we may learn from the works of the honoured master
Ehrenberg ; out of the 1200 figures which he gives of organ-
isms obtained from samples of dust carried by the trade-
winds, no fewer than 285, or, in round numbers, 24 per cent.,
are evidently remains of sponges ; and of these 46, or, in round
numbers, 4 per cent. of the whole, or nearly 16 per cent. of
the sponge-fragments, are fractured or entire amphidisci of
various species of Spongille.
By far the greater part of the organic remains figured by
Ehrenberg are derived from fresh water: we find among them
Diatomee still with green contents rich in chlorophyll; the
marine objects, Polythalamia, sponge-spicules (some of which
are of deep-water forms, such as Geodiew and Hexactinellide),
are probably not, as Ehrenberg supposed, recent, but originate
from the Tertiary deposits of North-west Africa (Oran), which
contain such an abundance of fossils. ‘That among this dust,
which therefore originates from Africa, and not, as Ehren-
berg supposed, from South America, to be thrown down in
Europe, there are no such large specimens as the gemmules
of Spongilla nitens for example, proves scarcely any thing.
The further the particles of dust are carried from the regions
in which they were taken up, the finer will they be, and vice
versa. According to the weight of the objects transported a
sort of sifting of the atmosphere will gradually take place!
I have experimented, certainly with the roughest apparatus,
in the following manner :—a number of gemmules from speci-
mens of Spongilla lacustris and S. nitens {from the White
Nile, in the Leipzig Museum), which had already been pre-
served dry for many years, were further dried at a moderate
heat under the same conditions for eight days; then fifty of
each kind were taken and mixed together, and then placed in
a little heap at one end of a perfectly flat newly polished
Gemmules of Freshwater Sponges. 167
table. ‘Towards this little heap a very moderate horizontal
current of air (the force of which, however, I had no means
of measuring) was then directed by means of a pair of small
hand-bellows, and this immediately caused its dispersal. This
proceeding was repeated six times, and each time after the
dispersion of the gemmules a pair of compasses was set in the
middle of the spot where the little heap had been ; its legs
were gradually opened at intervals of 1 centimetre, and curves
were drawn upon the table. In this way were obtained ten
curved regions each of 1 centimetre broad, and in these the
gemmules were counted; then the mean of the six observed
cases was taken and multiplied by two, in oxder to bring it to
a percentage for each kind of gemmule. The following was
the result :—
| 10
Regions of =
1 centim. broad. 10h ea e l ie a a Mi = woe Total.
Gemmules of | ee
Sp. lacustris. { kg il iY Gl ei Mgt lel dal a 100
Gemmules of 4 is
Sp. nitens. 2 |} .. | 9 | 15 | 22 | 27 | 13 | 9 4 100
These experiments, I readily admit, are very rough, but
they do not seem to me to be absolutely valueless: this much,
at any rate, may be learned from them, that the moving power
of the wind acts more powerfully upon the gemmules of
Spongilla nitens than upon those of S. lacustris; and to ascer-
tain this was the purpose of the experiments.
The gemmules of the other freshwater sponges* usually
differ considerably from those of Spongilla nitens and Cartert.
In no freshwater sponge known to me is the connexion of the
gemmules with the rest of the body so intimate as in Par-
mula Brownit, Bow., of which I have been able to examine
three specimens from the Rio Negro, most kindly presented
to the Leipzig Museum by Dr. Carl Miiller-Halle. Each
gemmule, with its shell, is surrounded by a special capsule,
which is never provided with an aperture, and which contains
a very small quantity of horny substance, but is formed chiefly
of naviculiform spicules, lying close together, like cobble-
* IT have been unable to compare those of the genus 7wbella, Carter,
and of the remarkable new North-American forms,
168 . Dr. W. Marshall on the
stones, in such a manner that their convex sides are directed
outwards. These spicules are not quite irregularly arranged ;
they have a tendency to radiate from certain points in a stellate
arrangement, and, on close examination, for example in sec-
tions, we observe that at these points the inner surface of the
capsule is in contact with the true envelope of the gemmule.
The latter, in fact, is not uniformly smooth, but furnished
with numerous, irregularly distributed, conical prominences,
which pass to the inner surface of the exterior capsule, but
are only loosely connected therewith. If the gemmules are
allowed to swell up in warm water within the capsules, which
is a rather long operation, it is seen that in course of time the
exterior capsules are first ruptured at these points of contact.
This may also occur normally when the capsule with its still
living contents has again got under water; as the capsule has
not, like the true gemmule-envelope, a special aperture of
issue, the germ, newly awakened into life, could hardly other-
wise be set free.
The true envelope of the gemmule is not thick, shows a
simple granular structure, and is only covered superficially
with round siliceous shields, which, on the outside, rise into
short spiniform knobs and are slightly hollowed within,
These shields lie so closely over the whole surface that their
margins overlap; only the conical prominences are quite free
from them. ‘Their margins are imbedded in the base-sub-
stance of the envelope, while their little points are exposed.
The round exit-aperture for the germ is here furnished with a
closing apparatus.
The significance of this complicated investiture of the gem-
mules of Parmula is not hard to understand. The exterior
capsule, as Carter has already pointed out, is composed of
true skeletal elements specially modified. These naviculiform
spicules exactly resemble those with which the stronger trains
of spicules of the framework of the sponge are coated; the
capsules usually pass into this coating, and are continuously
connected with it; frequently also two or more capsules are
intimately united by bridges of such spicules, as Bowerbank
has already shown in his figures. It is clear that in this way
the gemmules are very firmly attached to the rest of the
framework ; and it often happens that, when one wishes to
separate such a gemmule-capsule from the dried sponge with
the forceps, a portion of the adhering spicule-train of the
skeleton is broken away with it. This intimate union is
certainly of some importance to the gemmule, and I believe
that we come upon the track of it if we consider the mode of
lite of the species of Tarmula. Bates mentions that Spongilla
eh oth
Gemmules of Freshwater Sponges. * 169
Batesti occurs upon the twigs and stems of trees which
are under water during the months of the rainy season; and
Carl Miiller* states, from the reports of the traveller Gustav
Wallis, who also met with this sponge, called in its native
country “ Canixi”’ (pron. Canisch1), that the sponge appears
especially to be produced where air can act upon it—that is,
upon stones which are alternately wet and dry during the
rising and sinking of the stream. By means of the spicular
capsules the gemmules are firmly affixed to the dried sponge,
so that they cannot fall out and perish on the dry ground ; but
when, in the rainy season, the rising water again reaches the
sponges of the previous year, the capsules are ruptured (as
may be artificially shown), and the true gemmules are set
free and can become developed in the water. The armature
of siliceous shields seems to prevent too great a collapse
of the delicate gemmule-envelopes during desiccation; as
their margins overlap the conditions are similar to those of a
coat of scale-armour, which also is only compressible to a
certain extent. When I removed the siliceous structures by
hydrofluoric acid the envelopes became very flexible. The
amphidisci of the gemmule-envelopes of the Meyenie seem
to have a similar function, but a double disk would not be
necessary for this purpose; this, as we shall see immediately,
has been produced by another adaptation.
The gemmules of the series of forms to which Spongilla
lacustris belongs have homogeneous membranous walls pro-
vided at the surface with projecting, often spinose, tangential
or radiating spicules; hence they are certainly heavier than
the gemmules of the nitens series, but at the same time always
light enough to be able to swim in and upon the water. The
superficial spicules, like the uncinate processes of many stato-
blasts of Bryozoa, will act as adherent organs, by which the
gemmules may on occasion be anchored. ‘This constitution
of the gemmules is certainly advantageous to forms of Spon-
gille which live in stagnant or slowly flowing water, but
would be of doubtful advantage to those dwelling in brooks
and rivers with strong currents; here, being continually
rolled and driven along, they would have few chances of
coming to rest, and a large percentage would be lost. To
prevent this the gemmule would have to adopt, as it were,
a check in the form of a heavier shell; and this is effected by
the introduction of special siliceous elements, the amphidisci,
which at the same time form a shield against the occasional
‘shocks and contusions which are inevitable in running water,
* See ‘Die Natur,’ Bd. xxiii. (1870), p. 181.
Ann. & Mag. N. Hist. Ser. 5. Vol. xiii. 12
170 ‘On the Gemmules of Freshwater Sponges.
especially with a stony bottom. The gemmules of the fluvia-
tilis-series are heavier than those of the lacustris-series, as
one may easily convince one’s self by scattering the two upon
water; the fuviatilis-gemmules sink much sooner than those
of lacustris. By moving water they will be rolled along
slowly, and especially at the bottom.
It would appear that the Meyenie are chiefly distributed
in running waters, while the true Spongille are rather inhabi-
tants of still water. This, of course, does not mean that the two
forms are sharply separated in this respect; on the contrary,
Meyenie will easily be found in stagnant water, although true
Spongille are not so readily met with in strongly running
water.
A form of Meyenia, M. mirabilis, from the Ohlau, near
Breslau, lately made known by Dr. Wilhelm Retzer*, is
interesting in more than one respect ; but especially on account
of its gemmules, which have a triple armature of amphi-
disci one above the other. Ido not know the character of
the Ohlau (not Ohle) and its subsidiary waters, but probably
its system includes many rapid brooks, so that the gemmules
of the sponges occurring in it have had to adapt themselves
in this direction.
I find it not inconceivable that, in the lapse of time, Spon-
gillee (Euspongilla, Vejd.) may become converted into Meyenie
(Ephydatia, Lamx., Gray) by long residence in running
water, ¢. e. that their skeletal elements, and especially their
gemmule-envelopes, may become modified in this direction ;
and that, on the other hand, by a long undisturbed sojourn in
standing water, Meyenie may revert to true Spongille, by the
gradual loss of the amphidisci &c. From this point of view
the ELuspongilla jordanensis, var. drulieformis, recently de-
scribed by VejdovskyT, acquires a heightened interest. In it
we have perhaps before us a J/eyenia in process of reversion.
In the siliceous elements of the shell of the gemmule drawn by
Vejdovsky, in his pl. ii. fig. 19, we have before us a series of
transitions from the amphidisci (c) to the simple disk (e).
Moreover, these structures are much more sparingly scattered
in the membrane of the gemmule (see pl. 11. fig. 14) than in
the true Meyenie. I should not be at all surprised if, in
course of time, in the quiet water of the pool of the Jordan,
this siliceous armature were entirely to disappear—that is,
supposing that no “ new blood” was introduced from with-
* W. Retzer, ‘Die deutschen Siisswasserschwamme,” Inaug. Diss,
Tiibingen, 1483, p. 25, pl. il. fig. 18.
+ Abhandl. d. kén, bohm. Gesellsch. d. Wiss. 6 Folge, Bd. xii. p. 22,
Taf, ii. figs, 14-19.
Mr. A. G. Butler on a new Butterfly. 171
out, producing intercrossings by sexual reproduction. That
the gemmules of the new form are considerably smaller than
is usual in Spongilla has little or nothing to do with the
matter; the gemmules of S. lacustris vary very considerably
in size in different localities, perhaps according to the size of
the piece of water inhabited by the sponges, or that of the
parent animal, but I can say nothing positive as to the cause
of this phenomenon.
From what is above stated, we find the gemmules of the
freshwater sponges adapted in the following manners :—
1. Passively locomotive with aerostatic apparatus, the flying
form (of the dry season), nitens series ; 2. Passively locomo-
tive swimming form, with anchoring apparatus, for propulsion
at the surface before the wind, /acustris series; 3. Swimming
form, with check-apparatus for slow locomotion in running
water, fluviatilis series; 4. Secured from desiccation by a
double enclosure, adhering firmly to the body of the parent,
and only arriving at development when the water, during
the wet season, rises again to the level, genus Parmula, Cart.
Besides these there also exist freshwater sponges without
gemmules :—Lubomirskia from Lake Baikal; the forms col-
lected in the Congo by Dr. Pechuél-Lésche, forming a new
genus, Potamolepis, a description of which, by myself, has
lately appeared in the ‘Jenaische Zeitschrift’*, and the subter-
ranean Spongilla stygia, Joseph, from the Cave of Gurk, in
Carniolia.
In conclusion, I repeat my previous request to all my
fellow-labourers to be kind enough to aid me with material,
accompanied by the most exact account of the localities (the
nature of the water, whether moving or quiet, whether
large or small, brook, river, old river-course, pool or lake; the
nature of occasional aftluences, whether exposed to desiccation,
&c. It is necessary to know everything!). A great many
gentlemen have most kindly complied with my former prayer,
but for the solution of certain questions the material can
hardly be large enough !
XX.—On a new Genus of Butterfly from New Zealand.
By Artuur G. BuTLeER, F.L.S., F.Z.8., &e.
AT a meeting of the Philosophical Institute of Canterbury,
New Zealand, held on the 30th November, 1883, Mr. R. W.
Fereday read the “‘ Description of a Species of Butterfly new
* See Ann. & Mag. Nat. Hist. ser. 5, vol. xii. p. 391, Beene 1833.
12
172 Mr. A. G. Butler on a new Butterfly.
to New Zealand and probably to Science,” to which he gave
the name of Genus? helms?; this species he referred to the
Nymphalide, but did not venture to assign it to any group
in that family.
As Mr. John D. Enys, who is now in England, has brought
over the type specimen of this butterfly for my examination,
with the request that I will determine its position and name
the genus, | have great pleasure in doing so. The genus
being a new one and greatly resembling the genus Dodona of
Hewitson both in form and general coloration, I propose to
call it
DoDONIDIA, gen. nov.
This genus, as indicated by Mr. Fereday, belongs to the
great family Nymphalide (subfamily Satyrine), and although
it corresponds most nearly in form with Oorades (a New-
World genus), it appears to me to be more closely related to
the Australian genera Argynnina and (rectoneura, from the
former of which (apart from its different form) it chiefly differs
in the shape of the discoidal cell of the secondaries, which is
acutely pointed instead of truncated, owing to the length and
obliquity of the discocellular veinlets. ‘The body, inclusive of
palpi and antenne, corresponds closely with that of Argynnina;
the style of coloration of the wings is most like that of A.
lathoniella: the primaries are triangular, but with the apex
and external angle obtusely rounded off; the costal margin is
nearly straight, slightly incurved before the middle, and very
slightly convex from apical third; the outer margin is nearly
straight, rather oblique, slightly convex at apex, and incurved
at external angle to meet the inner margin, which is also
nearly straight ; costal vein extending to apical third; sub-
costal five-branched, the first branch only emitted before the
end of the-cell, the second, third, and fourth at about equal
distances beyond the cell, the fourth and fifth forming an
Prof. F. J. Bell on some Parasites of Fishes. 173
almost equal fork to apex and outer margin; upper radial
emitted from anterior angle of the cell, lower radial near to
upper, so that the upper discocellular (which is inangled) is
of about one third the length of the lower discocellular ; the
latter is slightly arched and oblique; median nervules about
equidistant ; submedian vein running rather near to inner
margin: secondaries elongate triangular, subcaudate, and evi-
dently internally lobed at anal angle (these wings are, how-
ever, much injured); costal margin strongly lobate close to
base, so as to commence with almost a rectangle, nearly
straight from the angle to the apex; outer margin slightly
convex and sinuous and very oblique; abdominal margin
sinuous or elongate-sigmoidal to the extremity of submedian
vein, where it appears to form an obtuse angle to first median
branch (but unfortunately this part of the wing is chipped
away) ; costal vein arched, with well-defined precostal veinlet
projecting into the lobate subbasal angle; subcostal branches
and radial emitted at equal distances, their points of emission
forming an unbroken oblique line with the lower discocellular
veinlet, which is about four times the length of the upper;
second and third median branches emitted slightly nearer
together than the first and second. Type D. Helmsii,
Fereday.
Dodonidia Helmsii.
Genus? helmsit, Fereday, Trans. N.-Zeal. Inst. 1883.
Paporoa Range, near Greymouth, South Island, about
1200-1500 feet (&. Helms). ‘Type in Canterbury Museum.
XXI.—Note on some Parasites of Fishes from Madras deter-
mined by Dr. Orley. By Prof. F. Jerrrey Bext, M.A.
BRIGADE-SURGEON Brpigz, in charge of the Government
Central Museum at Madras, lately forwarded to Dr. Giinther
some specimens of Entozoa found parasitic in some of the
bony fishes of Madras, where their prevalence, or alleged
prevalence, had given rise to one of those epidemics of dis-
quiet which are best allayed by scientific knowledge and
investigation.
When the specimens in question were handed over to me I
suggested, and Dr. Giinther was kind enough to accede to the
suggestion, that their exact determination should be entrusted
j74 Prof. F. J. Bell on some Parasites of Fishes.
to my friend Dr. Orley, of the National Museum of Buda-
Pest, whose contributions to and accurate knowledge of hel-
minthological subjects is so well known.
In the present condition of fishery problems it will be well,
I think, to publish Dr. Orley’s list, (a) as it is the first contri-
bution to our knowledge of the parasites of Indian fishes, (8)
as a stimulus to collectors to search for Entozoic forms, and
(y) as a possible source of comfort to those who are anxious
as to the effects of eating fishes infested with such parasites as
these.
At the foot of his list Dr. Orley says that all the parasites
that were sent to him were in the cystic stage of unknown
species of tapeworms; the history, however, of Anthocephalus
hippoglosst and A. elongatus has been traced by no less an
authority than Von Siebold, who has shown* that they are the
cystic stages of Tetrarhynchus corollatus. Now this Cestode,
when adult, lives only in the digestive tracts of rays and dog-
fishes ; and as we know, therefore, its two hosts we may feel
confident that man may eat fishes such as Carane or Arius
without any danger of being infested with Anthocephalus.
So far as we are justified in arguing from the known to the
unknown, we may expect that the parasites whose cystic stages
are here recorded, but whose tapeworm condition has not yet
been traced, will be found, likewise, to have their other host
in some animal with whom the bony fishes have come for a
longer time, and still come, into more frequent contact than
they do with man; some shark or dogfish is, almost certainly,
the second host.
On this matter, however, we must wait for the definite
knowledge which is dependent on experimental investigation.
This exposition of our present ignorance brings us, in the
next place, to observe that, of the eight species represented
in the collection, two are new to science, though Dr. Orley
very properly abstains from giving a name to an imma-
ture form. <A percentage of twenty-five unknown forms in a
collection shows that much remains to be done before we can
be said to have any thing like a fair knowledge of the Hel-
minthology of the Indian seas. Definite knowledge of the
parasites of fishes, though by no means the first, is a most
important factor in the solution of those problems which
are of interest and importance not only to the zoologist, but to
those that catch and sell and those that buy and live on fish.
The following gives, in the third column, Dr. Orley’s de-
terminations :—
* Zeitschr. f. wiss. Zool. ii. p. 241.
On the Ephyre of Cotylorhiza and Rhizostoma. 175
Name of fish. Region of body. Name of parasite.
Anthocephalus giganteus, Dies.
1. Caranx, sp. ...... Abdomen. hippoglossi vulgaris,
( Bellgh.
De MAD ete Av <4 (Esophagus. —— yiganteus, Dies.
3. Arius thalassinus .. do. —— elongatus, Rud.
4, Equula caballa .... do. Pterobothrium macrourum,
Dies.
5. Cybium guttatum .. do. —— heteracanthum, Dies.
6. Synagris luteus .... do. erassicolle, Dies.
7. Trichiurus savala .. do. —— crassicolle, Dies.
IDES so nics un Abdomen. Anthocephalus, n. sp.
9. Stromateus niger .. (Esophagus. Pterobothrium heteracanthum,
Dies.
10. Sctena, sp... 10... do. , 0. sp.
11 SDE ayn aatins Intestine. —— crassicolle, Dies.
12. Drepane punctata.. Cisophagus. ©—— heteracanthum, Dies.
XXII.— The Ephyre of Cotylorhiza and Rhizostoma, and their
Development into Hight-armed Meduse. By C. Ciaus *.
Durine several decades various naturalists have already
endeavoured to trace the development of the Mediterranean
Cotylorhiza tuberculata (Cephea Wagner, Cassiopea borbonica)
from the egg to the Ephyra, but unfortunately with only im-
perfect results. Most of them} did not even get beyond the
eight-armed Scyphostoma-stage. Gegenbaur}{ alone suc-
ceeded in rearing the sixteen-armed Scyphostoma-stage,
without, however, being able to bring it to strobilation and the
throwing off of Ephyre. So much, however, could be deduced
with certainty from these observations, that Cotylorhiza does
not undergo a direct development after the fashion of Pelagia,
but passes through a Strobila-stage, the peculiarities of which
were still to be ascertained. For although the known Strobile
of Aurelia, Cyanea, and Chrysaora so closely repeat the same
form that, without careful investigation of the tissues, we can
hardly distinguish them, it is & prior? by no means demon-
* Translated by W.S. Dallas, F.L.S., from the ‘ Arbeiten aus dem
zoologischen Institute der Universitat Wien,’ &c., Bd. v. Heft ii.
+ See Ecker, “ Ueber die Entwicklung einer Schreibenqualle ( Cephea
Wagneri),” in ‘ Bericht iiber die Verhandlungen der naturf. Gesellsch. in
Basel,’ Bd. viii. 1849; W. Busch, ‘ Beobachtungen iiber Anatomie und
Entwicklung einiger wirbellosen Thiere,’ Berlin, 1851; A. von Frantzius,
“Ueber die Jungen der Cephea,” in Zeitschy. fiir wiss. Zool. Bd. iv. 1853.
C. Gegenbaur, *‘ Zur Lehre des Generationswechsels und der Fort-
pflanzung der Medusen und Polypen,’ Wiirzburg, 1854.
176 Dr. C. Claus on the Ephyre of
strated that Strobile differently constructed from them do not
exist, especially as, in the remarkable Stephanoscyphus mira-
bilis, we know of a polyp which is comparable with the Scy-
phostoma, and which, in consideration of the four gastral
pads, might actually be judged to be an Acalephan nurse.
It is no better with our knowledge of the development of
Rhizostoma, with regard to which the statements given by
Noshin * and A. Kowalevsky t have not even settled the
question whether or not a process of strobilation occurs.
Under these circumstances I was much interested in a
statement in the zoological ‘ Jahresberichte,’ according to
which G. Du Plessis} had recently succeeded in demon-
strating in Cotylorhiza the occurrence of the alternation of
generations characteristic of most Acalephs. However, IL
learned from the statement of Du Plessis just referred to, that
this observer also had really not got beyond the rearing of the
Scyphostomes, and that the supposed proof rests only upon
very doubtful considerations. In point of fact, Du Plessis has
not traced the process of strobilation, but has rather referred
to Cotylorhiza, without satisfactory reasons, Strobile met with
in the aquaria of the zoological station (at Naples). Moreover,
they were neither fully described nor figured ; and the Kphyree
thrown off by them were so insufficiently described that the
existing gap is to be regarded as still unfilled. From the
agreement which the Ephyra shows in coloration with the
adult Cotylorhiza (Cassiopea) we can evidently not derive any
data for the determination of their mutual relation any more
than a general resemblance of the Ephyra to the adult Cassio-
pea can be made available for the same purpose. Such a
resemblance moreover does not exist, or it is so distant that
the same must apply to any other Ephyra. Should the Ephyra
described by Du Plessis § really belong to Cotylorhiza, the
description given by that author is, as we shall see, a very
superticial one, for no intermediate vessels are spoken of, nor
is there any mention at all of the charging of the entoderm
* N. Noshin, Bull. Acad. Imp. St. Pétersb. tome viii. (1866).
+ A. Kowalevsky, “ Untersuchungen iiber die Entwicklung der Ceelen-
teraten” (with eight plates), in Nachr, der Gesellsch. der Freunde der
Naturerkenntniss, &c., Moscow, 1875 (in Russian).
t G. Du Plessis, “ Remarques sur les métamorphoses de la Cassiopée
borbonniére (Cassiopea borbonica, Dell. Ch.) faites a la Station Zoologique
de Naples,” Bull. Soc. Vaud. Sci. Nat. tome xvii. no. 86,
§ Du Plessis, dc. p. 638 :—“ Du reste, ces jeunes Méduses ressemblent
déja beaucoup a la Cassiopée adulte. Elles en diflérent seulement par
une bouche quadrangulée, quatre bras simples (au lieu de huit trés rami-
fiés) et sans sugoirs, et les bords de l’ombrelle beaucoup plus échanerés
par des profondes découpures,’
Cotylorhiza and Rhizostoma. 177
with zoochlorelle, a peculiarity which immediately catches the
eye as influencing the coloration and marking.
As for a long time | could not sueceed, notwithstanding
many endeavours, in obtaining sexually mature Cotylorhize
at the period of egg-laying, and consequently in rearing
Ephyre, I attempted to get possession of them in another way,
namely by pelagic fishing. For several years larve of Rhizo-
stoma and Cotylorhiza were regularly captured, especially in
August, which, being already in stages of more or less ad-
vanced development, could be easily determined as belonging
to those two genera. I was therefore enabled some time since
to publish a tolerably detailed account of the metamorphosis of
these larve—which were already provided with intermediate
marginal lobes, bifurcate buccal arms, and traces of the vas-
cular net—into the perfect Lhizostoma- and Cotylorhiza-form*.
The Ephyre, however, were not to be obtained, and conse-
quently an important part of the transformation, namely that
of the Ephyre into the four-armed, and of the latter into the
eight-armed form, remained unknown. ‘The circumstances
through which the important peculiarity of rhizostomism is
brought about and conditioned consequently were still to be
ascertained. It was only in the summer of the present year
that our zealous and able seaman Kossel chanced to fall in, on
the 14th, 17th, and 18th July, with great swarms of Cotylo-
rhiza-larve, in which were included all those young states
which had hitherto been sought in vain.
The swarms, as Dr. E. Graetfe informs me, were driven
together with masses of Zostera and of Sargassum covered
with Hydroid polyparies, in the middle of the Gulf of Trieste
between Barcola and the lighthouse, and must probably have
been brought up by strong currents from the southern parts
of the Adriatic.
Now it appeared that the same Ephyra had already once
before been observed singly by me, and determined quite cor-
rectly from the nature of the entoderm, which was filled with
algal cells, as probably belonging to Cotylorhizat. Of course
absolute certainty could only be arrived at by the demonstra-
tion of the intermediate steps to the undoubted Cotylorhiza,
which was now furnished by the discovery of this swarm in
all stages of transition. The circumstance that the entoder-
mal coat of the gastral cavity and vascular canals was filled,
although imperfectly, with zoochlorelle, might probably indi-
* ©. Claus, ‘Untersuchungen tiber Organisation und Entwicklung der
Medusen’ (with twenty plates), Prague and Leipzig, pp. 44-06,
+ C. Claus, /. ce, p. 54.
178 Dr. C. Claus on the Ephyree of
cate that the older Scyphostomes, as well as the Strobila-stages,
contain these vegetable cells in abundance, and grow large in
definite localities which are particularly favourable to the
access of those organisms. Perhaps in this we may also find
the reason why no one has hitherto succeeded in bringing the
bred Scyphostomes to strobilation.
The youngest Ephyra of the Mediterranean and Adriatic
Cotylorhiza 1s a comparatively large form of about 14 to
2 millim. diameter, with eight long slender lobes, the cleft
pieces or ocular lobes of which appear rounded off rather than
pointed. In form and internal structure it possesses all the
peculiarities of the known Ephyree of the Semaostomean Me-
duse with the exception of the Ephyropside, the Kphyree of
which, as I have recently proved, exhibit important deviations
both in the constitution of the gastral space and in the form
of the umbrella (see Claus, d.c. Taf. vii. fig. 48). In
its appearance our form stands between the well-described
Ephyre of Aurelia and Chrysaora, but is distinguished from
both by several peculiarities which are wanting in them, and
which enable it to be at once recognized and determined.
The most striking of these are the numerous yellowish-brown
algal cells, which partly float freely in the gastral space and
partly in the radial canals, already taken up by the entoderm,
giving rise to the peculiar coloration, and by their accumulation,
especially at the lateral confines of the radial canals, producing
two streaks in each of the main lobes. Among hundreds of
Ephyre I have not met with a specimen in which this charac-
ter did not strikingly occur, and I therefore believe that these
vegetable intruders perform a great, perhaps a necessary, part
in the life of the Cotylorhiza. 1 will hereafter revert
more particularly to these vegetable cells. Another less
striking character, only observable by careful examination,
consists in the presence of numerous spindle-shaped crystals
in the terminal division of the ocular lobes. ‘These crystals
remind one of the chrome-yellow crystals in the ectoderm of
Nausithoé; but they are colourless and do not border the whole
margin of the lobe, but lie collected together at the surface of
the lobe. ‘They likewise originate singly in ectodermal cells.
In the vascular apparatus the size of the radial intermediate
vessels is remarkable, which, indeed, are entirely covered by
the radial muscle, but the limits of which are still easily recog-
nized on account of the colour of the contents. In the Ephyra
of Aurelia these vessels scarcely appear as diverticula; while
in that of Chrysaora they show the same considerable deve-
lopment. Nevertheless the latter larva cannot be confounded
with ours, for it is at ouce recognizable by the external and
Cotylorhiza and Rhizostoma. 179
internal circlets of large exumbral urticating pads, and by the
rudiments of the four primary gastral filaments, which, in our
larvee, have already attained a very considerable size. The
buccal tube is already characterized by the strength of its
wall and the thickness of its jelly, and it is still destitute of
the four arms, so that the Ephyra of Cotylorhiza would have
to be described as “‘ cannostomous”’ in Hickel’s sense.
During the gradual growth the umbrellar disk of the larva
constantly acquires a greater extension in comparison with
the eight lobes; in other words, the distal extension of the
interradii advances more rapidly than that of the radii. In
Ephyre which only slightly exceed the diameter of 2 millim.
the proportion between the length of the lobe-stems and the
radius of the umbrellar disk already appears distinctly altered
in favour of the latter. While in the youngest Ephyre it
represented 13:1, the semidiameter of the disk has already
attained the length of the eight lobe-stems. We may regard
this larval form as asecond Ephyra-stage, because on the oral
part of the buccal tube new structures have made their appear-
ance which seem to be of very great importance in the deve-
lopment of rhizostomism, and in combination with the strength
of the wall already indicated, pave the way towards the very
divergent structure of the buccal arms. Thus on the free
border of the buccal tube short tentacles have grown forth,
even before there could be any reference to the presence of
buccal tentacles. ‘The number of filaments is now doubled.
In the vascular apparatus no essential alteration is yet per-
ceptible, although lateral diverticula already appear on the
radial canals, tending towards a union with the intermediate
canals to form the annular canal.
The larvee of about 24-3 millim. diameter show an essen-
tially altered form, short pointed velar lobes making their
appearance in the interradi, which already considerably ex-
ceed half the length of the radii. ‘These stages already possess
a closed annular canal, for the formation of which the diver-
ticula of the radial vessels have united with the intermediate
canals ; and also four well-marked buccal arms beset with ten-
tacles. ‘They represent the floresca-stage. Moreover the
buccal arms, independently of the tentacular fringe on their
elongated distal margin, already show a complication pre-
aring the way for the future pairs of arms, in the shape of
two lateral folds diverging in a fork distally. The number of
filaments has advanced to 3-4 in each radius, and the
occupation of the entoderm by vegetable cells is denser
in comparison with the younger larve. In connexion with
the appearance of the marginal corpuscles the cord-like con-
180 Dr. C. Claus on the Ephyre of
striction of the vascular canal and the dorsal dilatation above
the otolith-sac seem worthy of notice.
With advancing growth the velar lobes, which are at first
small and narrow, gradually increase in dimensions, while at
the same time the periphery of the intermediate areas grows
out at the expense of the lobes, which are transferred to the sub-
stance of the disk, and the velar lobules seem to advance more
and more into the zone of the alternating ocular lobes. Under
these changes the larva gradually loses the character of the
Ephyra in favour of the young Acalephan form distinguished
by a circlet of marginal lobes.
The sixteen areas of the vascular lamella become at the
same time divided by vascular processes, which unite with
each other into a great number of islets. First of all there is
produced regularly between the radial canal and intermediate
vessel a narrow pararadial vessel parallel to the latter, so that
now thirty-two elongate ovate areas are present. ‘These are
then somewhat irregularly interrupted by transverse vascular
diverticula, and even in larve 4 millim. in diameter the
rapidly advancing development of irregular radial series of
areas is commenced, ‘The filaments are now already increased
into small coil-like groups; and the buccal arms, by the en-
largement of their processes, which are already contiguous,
and by new formation of tentacles on their divergent terminal
halves, have acquired a form in which the foundation of the
pairs of arms unmistakably appears. Now also the comph-
cation of the vascular network makes rapid progress. Larvee
of 44-5 millim. diameter, already furnished with four pairs of
arms cleft at the extremity, represent the stage which I lately
described and figured as the youngest Cotylorhiza-larva
known to me*, ‘The annular vessel, which was well marked
at an earlier age, already appears indistinct and effaced to such
a degree, that without a knowledge of the younger larva one
might regard it as altcgether suppressed, and come to the con-
clusion that the narrow-meshed vascular net of Cotylorhiza
has a mode of formation quite different from that applying
to Rhizostoma and the Aureliide. In larve of 7 millim. dia-
meter, the areolation of the entodermal lamina already appears
so narrow and close, and the frequently notched margin of the
vascular network so far advanced peripheraily, that the generic
and family characters are recognizable. ‘The further meta-
morphosis of the larva in connexion with the general form of
the disk, the marginal lobes, and the structure of the brachial
* C. Claus, l. c. p. 52, figs. 106, 107. ‘The average size is here, by an
oversight, stated as too small; it amounts not to 3 millim, but to
5 millim,
Cotylorhiza and Rhizostoma. 181
apparatus has been fully described by me in the work above
cited ; and here I venture only to call attention particularly to
the development of the nematophores, which also stand in
an important relation to the establishment of points of amalga-
mation in the progress of the buccal arms, which are greatly
enlarging and forming secondary infundibuliform folds.
In general therefore it appears (and the same may also
recur in Rhizostoma and all Rhizostomez) that the early ap-
pearance of the buccal tentacles in the Cannostomous stage ¢s
the primary process superinducing rhizostomism, then fol-
lowed by the pecuiiar form of the four arms with their ex-
tended distal margin, and then paired foldings of the brachial
processes. Krom these stages onwards the development of
rhizostomism depends essentially upon the continued folding
of the surfaces of the arms, and their margins beset with ten-
tacles, as I have already described in detail (C. Claus, Z. c.
p: 52 &e.).
As regards the yellowish-brown corpuscles which occur in
great quantity in the entoderm of the larve of Cotylorhiza,
they belong undoubtedly to the category of the plant-cells
which vegetate symbiotically in so many of the lower organ-
isms, first recognized as such by Cienkowski*, and_subse-
quently distinguished by R. Brandt} as zoochlorelle and
zooxanthelle. In Cotylorhiza they were detected some years
ago by Hamannf, but erroneously interpreted as unicellular
glands with a difficultly recognizable aperture, until soon
afterwards Patrick Geddes§ first demonstrated their true
nature.
These chlorophyll corpuscles lie here and there singly, but
generally in groups, in the cells of the entoderm, and project
as globular or racemose balls into the jelly. Probably they
have originated as products of continued division from a single
cell; and, in point of fact, one meets with all transitions down
to the bisection of the cell. I have never seen the zoo-
xanthelle completely separated from their union with the ento-
derm, although it is not improbable in itself that they might
be transferred in‘o the jelly by entodermal cells which have
* Cienkowski, “ Ueber Schwirmerbildung bei Radiolarien,” in Archiv
fiir mikr. Anat. 1871.
+ K. Brandt, “ Ueber das Zusammenleben von Algen und Thieren,” in
Biolog. Centralbl. 1881, no. 17; and also Geza Entz, did. 1882,
no, 21.
{ O. Hamann, “ Die Mundarme der Rhizostomen,” in Jenaische naturw.
Zeitschr. Bd. xy. 1851. This author has lately recognized the error of
his interpretation and retracted it.
§ Patrick Geddes, “On the Nature and Functions of the ‘ Yellow Cells’
of Radiolarians and Ceelenterates,” in Proc. Roy, Soc. Edinb, 1882.
182 On the Ephyre of Cotylorhiza and Rhizostoma.
wandered into the latter. Perhaps also by means of this sup-
position we may explain the free occurrence of the globular
ageregations of yellowish-brown cells which C. Keller* has
recently described in the jelly of his Casstopea polypoides, and
has interpreted, certainly erroneously, as a peculiar cell-form
of the mesoderm.
The mode in which the chlorophyll-bearing algal cells,
which also float very numerously free in the gastrovascular
space, get into the entoderm, may be explained withont diffi-
culty by means of the faculty of amceboid movement now
demonstrated in the case of the entodermal cells of the Meduse.
One might indeed imagine an active immigration on the part
of the algal cells, which also have been known in the state of
swarming; but the well-marked amceboid movements of the
entoderm, which are so important for the inception of corpus-
cular elements, fully suffice to explain their introduction.
Perhaps we may even succeed in obtaining this demonstration
by direct observation ; and for this purpose the Hphyra-stages
may be particularly well fitted, as their gastral lining is not
yet overcharged with zooxanthelle., At a later age the filling
up of the epithelium, especially in the close vascular ramifi-
cations, is so complete that one must take a good deal of
trouble to find a free entodermal cell, at least in this section
of the gastrovascular apparatus. ‘The arms and funnel-frills
also, as well as the central stomach and the filaments, contain
the foreign guests so densely packed, that one is led to ask
the question, whether there is any independent animal nourish-
ment, and whether the superfluous assimilation-products of
the zooxanthelle, brought to the entoderm, do not suffice for the
support of the Medusee. With regard to this question, young
Cotylorhize, which may be very well kept for months in the
aquarium, would certainly be favourable objects of experi-
ment, and would probably in essential .points confirm the
results obtained by K. Brandt} by experiments with Anthea
cereus.
Hitherto I have not been so fortunate as to find the youngest
Ephyre of Rhizostoma, which have been sought after for years.
However, I succeeded in obtaining a young form, 34 millim.
in diameter, which is notably inferior to the known and de-
scribed stage, and by the small development of the velar lobes,
which are already cleft, shows that the latter do not grow
* ©. Keller, “ Untersuchungen tiber neue Medusen aus dem rothen
Meere,”’ in Zeitschr, fiir wiss. Zool. Bd. xxxviii. 1883.
+ K. Brandt, “Ueber die morphologische und physiologische Bedeu-
tung des Chlorophylls bei Thieren,” in Mittheil. aus der zool. Station zu
Neapel, Bd. iv. Heft 2 (1883).
we
a)
On the ‘Challenger ’ Lepidoptera. 183
forth, as in Cotylorhiza and Aurelia, as unpaired tongue-
shaped lobules, but in pairs as in Discomedusa. The annular
vessel is already completely closed, but the buccal arms,
abundantly beset with tentacles, are still simple and undivided.
Probably the preceding Ephyre, which have not yet been
observed, agree with those of Cotylorhiza.
XXIT1.— The Lepidoptera collected during the recent Expedi-
tion of H.M.S. ‘ Challenger.—Part I]. By Artaur
G. Butter, F.L.S., F.Z.8., Assistant Keeper, Zoological
Department, British Museum (Natural History).
THE first part of the Lepidoptera (which at the time I sup-
posed to be the complete collection) obtained by the natura-
lists of H.M.S ‘Challenger’ appeared in the ‘ Annals’ for
June 1883, pp. 402-428 ; since the publication of that account,
which embraced the species obtained in the Philippine, Aru,
Admiralty, Fiji, and Friendly Islands, series have been re-
ceived which were collected in the islands of St. Thomas,
Bermuda, Rat Island, Ké Dulan, Ternate, and Amboina,
amounting in all to one hundred and two species, which have
yet to be recorded *,
The collections from St. Thomas and Bermuda being from
the New World, are here treated separately from those of the
other islands. ‘They are as follows :—
Ru OPALOCERA,
Nymphalida.
Evrr@12.
1. Anosia leucogyne, sp. n.
This is the West-Indian form of A. pleatippus of North
America, from which it chiefly differs in the external black
border of the secondaries of the male being either unspotted
or very imperfectly spotted with white; the female also is
usually (though not invariably) paler, and has the outer border
* In an envelope were numerous specimens of Pyrameis carye, Hiibn.,
two damaged specimens of Leucania decolorata, Blanch., and two unrecog-
_ nizable Micro-Lepidoptera from Juan Fernandez, taken on the 14th and
15th November 1875; these I have not entered in this List.
184 Mr. A. G. Butler on the
of the secondaries less distinctly spotted with white than in
the northern form. The expanse of wings varies from 76-106
millim., the females being not unfrequently dwarfed.
St. Thomas, March 1878.
The northern form, A. pleaippus, is the type found in the
Australian region.
NYMPHALINZ.
2. Dione vanille.
Papilio vanille, Linneus, Mus. Lud. Ulz. p. 806 (1764).
St. Thomas, March 1878.
The North-American species, which has hitherto stood as
a synonym of this butterfly, being perfectly distinct both in
size, form, pattern, and colour, must henceforth stand as
Dione passiflore (under which name it was figured by Abbot).
3. Junonia cenia.
Junonia cenia, Hiibner, Samim. exot. Schmett. (1816-24).
St. Thomas, March 1878; Bermuda, in April.
Hrzriconin#.
4, Fleliconius charithonia.
Papilio charithonia, Linnteus, Syst. Nat. i. p. 757 (1767) ; Cramer,
Pap. Exot. ii. pl. exci. F (1779).
St. Thomas, March 1878.
The examples from St. Thomas are typical, and therefore
distinct from those of Mexico and St. Domingo; the latter
represent a larger longer-winged insect, with much narrower
yellow bands; why it should not have been considered dis-
tinct by lepidopterists generally it would be hard to say.
Lycenide.
5. Tmolus columella.
Hesperia columella, Fabricius, Ent. Syst. iii. 1, p. 282. n. 83 (1798).
g. St. Thomas, March 1878.
Papilionide.
PrerinZ.
6. Appias Poeyt ?
Appias Poeyi, Butler, Proc. Zool. Soc. 1872, p. 49.
3d. St. Thomas, March 1878.
‘Challenger’ Lepidoptera. 185
The specimen before me is slightly shorter in the wing than
those which we have from St. Domingo and Honduras ; but
without seeing more specimens it would be rash to regard it as
distinct.
7. Ganoris cleomes.
Pieris cleomes, Boisduval & Leconte, Lép. Am. Sept. p. 43, pl. xvi.
(1833).
3. St. Thomas, March 1878.
8. Callidryas senne.
Papilio senne, Linneeus, Syst. Nat. i. p. 764. n. 103 (1766).
3 2. St. Thomas, March 1878.
9. Terias euterpe.
Colias euterpe, Ménétriés, Bull. Mosc. 1832, p. 299; Nouv. Mém.
Mose. iii. p. 121, pl. xi. fig. 4 (1834).
3. St. Thomas, March 1878.
PapiLionin2.
10. Papilio polydamas.
Papilio polydamas, Linnzeus, Mus. Lud. Ulr. p. 192 (1764); Drury, Dl.
Ex. Ent, i. pl. xvii. figs. 1,2 (1773).
@. St. Thomas, March 1878.
Hesperiida.
11. Goniuris proteus.
Papilio proteus, Linnzeus, Mus. Lud. Ulr. p. 333 (1764); Clerck, Icones,
pl. xlii. fig. 1 (1764).
St. Thomas, March 1878.
12. Gonturis dorantes.
Papilio dorantes, Stoll, Supp]. Cramer, pl. xxxix. fig. 9 (1790).
St. Thomas, March 1878.
13. Proteides amyntas.
Papilio amyntas, Fabricius, Syst. Ent. p. 533 (1775).
St. Thomas, March 1878.
14. Pamphila pustula.
Thymelicus pustula, Hiibner, Zutr. exot. Schmett. figs. 625, 626 (1832).
6 ?. St. Thomas, March 1878.
: Ann. & Mag. N. Hist. Ser. 5. Vol. xiii. 13
186 Mr. A. G. Butler on the
15. Pyrgus syrichtus.
Papilio syrichtus, Fabricius, Syst. Ent. p. 534 (1775).
St. Thomas, March 1878.
HETEROCGERA.
Sphingide.
16. Cherocampa tersa.
Sphinx tersa, Drury, Ill. Exot. Ent. i. p. 61, pl. xxviit. fig. 3.
Bermuda.
Arctiidae.
17. Composia sybaris.
Phalena (Bombyx) sybaris, Cramer, Pap. Exot. i. p. 112, pl. lxxi. fig. B
(1779).
St. Thomas, March 1878.
Lithosiide.
18. Detopeia ornatrix.
Noctua ornatrix, Linneeus, Syst. Nat. i. p. 839 (1766).
St. Thomas, March 1878.
Leucaniide.
19. Leucania antica.
Leucania antica, Walker, Cat. Lep. Het. ix. p. 100 (1856).
Bermuda, in April. |
This species was evidently the commonest moth met with
at Bermuda.
Xylophasiidex.
20. Laphygma macra.
Laphygma macra, Guénée, Noct. i. p. 157. n, 251 (1852),
Bermuda, in April.
21. Perigea subaurea.
Perigea subaurea, Guénée, Noct. i, p. 227. n. 862 (1852).
Bermuda, in April.
‘Challenger’ Lepidoptera. 187
Ihave little doubt that I have rightly identified this species,
although Guénée’s description of the secondaries is hardly
satisfactory ; they are not “ clear ochreous,” but pearl-whitish
with golden reflections; here, as in the primaries, Guénée
seems to have described the shot tints rather than the true
colour of the wing.
¥
Plusiide.
22. Plusia ou.
Plusia ov, Guénée, Noct. ii. p. 96 (1852),
Bermuda, April 1873.
Remigiide.
23. Remigia marcida.
Remigia marcida, Guénée, Noct. iii. p. 317 (1852).
Bermuda, April 1873.
Thermesiidz.
24. Thermesia monstratura.
Thermesia monstratura, Walker, Cat. Lep. Het. xv. p. 1564 (1858).
Bermuda, April 1873.
Margarodide.
25. Margaronia jairusalis.
Margarona jairusalis, Walker, Cat. Lep. Het. xviii. p. 524 (1859).
Bermuda, in April.
26. Margaronia flegia.
Phalena-Pyralis flegia, Cramer, Pap. Exot. ii. p. 66, pl. exl. fig, D
(1779).
St. Thomas.
Botydidez.
27. Botys? onophasalis.
Botys onophasalis, Walker, Cat. Lep. Het. xviii. p. 735. n, 826 (1859).
Botys thisoalis, Walker, J, c. p. 737. n, 329 (1859),
St. Thomas.
Without going into the whole history of the genus I will
not follow the example of one of our rising lepidopterists and
13
188 Mr. A. G. Butler on the
assert dogmatically that the above species either is or is not a
true Botys; but one thing is certain, that the two names above
associated were given to two specimens registered consecu-
tively from the same collection. It is also certain that the
species is nearly allied to Walker’s “Megaphysa?” serenalis,
which (in common with the other species referred by Walker
to Megaphysa) has no affinity whatever to M. Guénée’s genus.
Botys simmialis of Walker is also allied to B. serenalis.
Scopariide.
28. Stenopteryx hybridalis.
Pyralis hybridalis, Hiibner, Pyral. p. 29, pl. xvii. fig. 114.
Bermuda, April 1873.
A few species were obtained at Teneriffe; but as they are
well-known forms, it will be sufficient to enumerate them :—
Pararge meone, Esper; Synchloe daplidice, Linn.; Ganoris
rape, Linn.; a small moth, the body of which is too much
injured to allow of its identification (in size and form of wings
it corresponds with Sterrha sacrarva, but the neuration differs
not a little) ; and an imperfect specimen of Hypena obacerralis,
Walk.,—five species in all, three of which are butterflies and
two moths, all taken on the 14th February, 1873.
The remaining collections are distributed as follows :—
Z E i |
& 1s ) =
a =) * ot
ley, Moelle
© De ae 5
FS 2) H <
Radena meganira, Godt. ........ | 2 Pi
Limnas cratippus, Felder ........ ie isle aN ee .
Salatura philene, Cramer ........ te ae sit x
DAMASIO a scleig pte niein ain ae %
Ravadeba cleona, Cramer ........ ik + a *
Hamadryas niveipicta, Butler ....| .. %
Vadebra Zinckenti, We/der ........! ‘ie Ma Mie me
| Monrraiyd, UHer ed aoe p28 4.4 ave i 5 sf 2
| Chirosa eurypon, Hewits. ........ ee x
| Hirdapa fraterna, Felder .......... A *
| Salpinx pasithea, Felder .......... ee Peed es S|
‘Challenger’ Lepidoptera. 189
|
\
|
rs : ost
Ee ee) leet
a = 5 TA eer
up A I 2
= x) B =
mS <a H <q |
| Melanitis taitensis, Felder ..%..,., |
SOMATA Neel COnUC sales ese dielo'; gis Gils «%e : # |
| constantia, Cramer........+. Si ids |
Wbetherarete: CrQmer iwc cide eee eol|, ye AK we
| Calysisme justina, Cramer.....++.| +. Ae oe #%
Mydosama remulia, Cramer .,.,..| «+ >i a %
SSOP, LELCITLE 5.3.0. doi 5 Sabie ae x |
SIMIC DH LOT-UG TC ates et cseyee eg oles ‘af a *
Ypthima norma, MWestw...... eine eae e os a *
Doleschallia australis, Lelder......) 0.3 *
Messaras Crameri, Felder ...,,...| «- at fe *
Cethosia insulata, Butler........ Tals ee * |
eydippe, Lenneus ns secssee|. ve oe he *
| Hypolimnas nerina, Fubric. ......| «. a *
Tee ssa ss CEOIMEM am cy tecars vis, o] ocns Sis id +#
Precis hedonia, Zinn. ......... Tah oie Sr ee *%
timorensis, Wallace ........| «. *%
Gerydus Boisduvalii, Butler ......) .. of x *
stygianus, Butler ...... Pec) Wee sh *%
Tarucus plinius, Fabric... 2... <5. Fe we es *
Catochrysops trifracta, Butler ....) x
Lampides elianus, Fabric. ........ in *
pnerialig. MAGER > J uln bine mace las *
aratus, Cramer ..... b opeessaye il bub bers Se *% *
Lycena erinus?, Fabrie........... an ce *
Delias plexaris, Donovan... ... Lit SoD aaa JE ss *
Terias photophila, Butler ........| .. *
biformis, Butler ....... et ao hohe 50 ae *
DD OULU oar a was chad Se betas a x
tera, Felder oA s ou iA a oe *
Ornithoptera criton, Felder........| .. ae *
Papilio deiphontes, Felder ........ oe ri *
mucumor, Peder wae cew es i ie es *
Severus, Cramer .isceceseses| os us a *
—— Thomsonii, Butler ..........) 6. *
—— ulysses, Zinn. .......... Aros peny’ < RF *
polyphontes, Botsd...........) «. or *
Hesperia celeenus, Cramer ........| .. Be - *
Pamphila Moseleyi, Budler..... cael werd %
—— phineus, Cramer............] ++ of ws *
prusias, Felder....... Py eg Sl il oe re *
Padraona sunias?, Felder ........| «. *
Tagiades japetus, Cramer ........| .. a #2 *
Protoparce cingulata, Fabric.......) .. — *
Ophthalmis lincea, Cramer........) .. *
Cocytia Durvillei, Bowsd....... Ss Borvlis te « *
Euchromia ganymede, Doubl. ....) .. | x
1 Dyphlebia liboria, Cramer ........|) «. PN ate *
Hypsa heliconia, Limn....0....eees| os ane Fie * |
190 Mr. A. G. Butler on the
Rat Island.
Ké Dulan.
| Ternate.
Amboina.
——- ——
Hypsa lanceolata, Walker ........
Cleis evander, Cramer .........005
Artaxa simulans, Butler ..........
tUpNOtie, BP. . cee ec cae nsseaad
Pegella ichorina, Butler ..........
Bursada perdica, Cramer..........
Craspedosis ernestina, Cramer ....
Alcidis orontes, Zinn. ........-... a Sgt
Eumelea rosalia, Cramer.......... a *
ludovicata, Guénée.......... ae a
Xanthodes transversa, Guénée ....| .. *
Spiramia funestis, Butler..........
Ophiusa simillima, Guénée........
Glyphodes Ledereri, Butler ......
xe KKK HK
*
*
* *
A series of Lepidoptera from Queensland was in such poor
condition, and the species were so well known as common
North-Australian forms, that I have not thought it worth
while to record them ; the most abundant species was Orni-
thoptera richmondia, Gray.
The following is a catalogue of the insular species :—
Nymphalide.
EUrL@in.
1. Kadena meganira.
Danais meganira, Godart, Enc. Méth. ix. p. 192 (1819).
& ¢. Amboina.
2. Limnas cratippus.
Danais cratippus, Felder, Sitzb, Acad. Wiss. Wien, math.-nat, Cl, x1.
p- 449 (1860).
é. Ternate.
3. Salatura philene.
Papilio philene, Cramer, Pap. Exot. iv. pl. ccelxxy. A, B (1782),
& 3. Amboina.
4. Salatura affinis.
Papilio affinis, Fabricius, Syst. Ent. p. 511 (1775).
&. Ké Dulan, 25th September, 1874.
7.
‘Challenger’ Lepidoptera. 191
5. Ravadeba cleona.
Papilio cleona, Cramer, Pap. Exot. iy. pl. ceelxxvii, F (1782).
&. Amboina.
Up to the present time this species has been incorrectly
identified in British collections, as evidenced by the locality
given in Moore’s recent Monograph— Celebes.”” Cramer’s
species is of a pale (almost greenish) sulphur-yellow colour,
not unlike the ground-tint of R&R. lutescens, but with the
markings smaller and more restricted; on the other hand, the
Celebes form (which may be called 2. luctplena) is of a deep
gamboge-yellow colour, especially in the male sex.
6. Hamadryas niveipicta, sp. n.
Closely allied to H. nats from Aru, but smaller; the spots
on the primaries pure white (not greyish), sharply defined; a
white longitudinal line from the base to the middle of the
cell above, as well as below; the outer border of the secon-
daries narrower towards the anal angle than in H. nais.
Expanse of wings 46 millim.
Ké Dulan, 25th September, 1874.
We also have a specimen in the Museum from N. Ceram.
7. Vadebra Zinckenit.
Eupleea Zinckeni, Felder, Reise der Noy. Lep. ii. p. 335.
& ?. Amboina.
This is the Amboinese representative of V. sepulchralis of
Java, specimens of which were evidently confounded with it
by Felder.
8. Vadebra Murrayt, sp. n.
&. Primaries above rich piceous brown (similar to V.
melina), the external border and a diffused subapical band
continuous with it slightly paler, and therefore redder in ap-
pearance: secondaries dark olivaceous brown, with white
costal border; a diffused black nebula covering the lower
half of the cell at the bases of the interno-median and median
interspaces ; external area, with the exception of the apical
border, paler than the ground-colour: body dark piceous ;
head and collar black ; the usual white dots on the collar.
Wings below rufous-brown ; primaries with the costal, sub-
apical, and interno-median areas paler, the latter with two
well-separated cinereous longitudinal streaks, the lower of
which rests on the submedian vein; internal border white ;
192 Mr. A. G. Butler on the
an oval bluish-white spot within the cell, a second lilacine
white spot beyond it upon the second median interspace, and
a large oval spot of the same colour below the latter on the
first median interspace: secondaries with a bluish-white spot
within the cell, and an arched series of six spots beyond it;
three subapical white dots nearly parallel to the outer margin ;
the two usual white basal dots: body below much as in JV.
melina and allies. Hxpanse of wings 80 millim.
Amboina.
Decidedly smaller and of a different form from V. melina.
9. Chirosa eurypon.
Euplea eurypon, Hewitson, Exot. Butt. ii. Hupl. pl. i. fig. 3 (1858).
3 ¢@. Ké Dulan, 25th September, 1874.
10. Hirdapa fraterna.
Euplea fraterna, Felder, Reise der Noy. Lep. ii. p. 321.
6. Ké Dulan, 25th September, 1874.
11. Salpinx pasithea.
Euplea pasithea, Felder, Reise der Noy. Lep. ii. p. 318,
& ?. Amboina.
SATYRINE.
12. Melanitis tattensis.
Cyllo leda, var. taitensis, Felder, Verh. zool.-bot. Ges, Wien, xii.
p. 493 (1862),
3g. Amboina.
13. Melanitis solandra.
Papilio solandra, Fabricius, Syst. Ent. p. 600 (1775).
3. Ternate.
14. Melanitis constantia.
Papilio constantia, Cramer, Pap. Exot. ii. pl. exxxiii. A, B (1779).
9. Amboina.
15. Lethe arete.
Papilio arete, Cramer, Pap. Exot. iv. pl. ecexiii. E, F (1782).
3 9. Amboina.
16. Calysisme justina.
Papilio justina, Cramer, Pap. Exot. iv. pl. ceexxvi. C (1782).
dg ?. Amboina.
‘Challenger’ Lepidoptera. 193
17. Mydosama remulia.
Papilio remulia, Cramer, Pap. Exot. iii. pl. cexxxvii. F, G (1782).
&6 ¢. Amboina.
18. Mydosama asophis.
Mycalesis asophis, Hewitson, Exot. Butt. 11. Mye. pl. iv. figs. 20, 21
(1862).
9. Ternate.
19. Mydosama sirius.
Papilio sirius, Fabricius, Syst. Ent. p. 488 (1775).
¢. Amboina.
20. Ypthima norma.
Ypthima norma, Westwood, Gen. Diurn. Lep. pl. lxvii. fig. 1 (1851).
¢. Amboina.
NYMPHALINE.
21. Doleschallia australis.
Doleschailia australis, Felder, Reise der Noy. Lep. iii. p. 405, pl. li.
figs. 1, 2 (1867).
Ké Dulan, 25th September, 1874.
22. Messaras Crameri.
Messaras Crameri, Felder, Sitz. Akad. Wiss. Wien, math -nat. Cl. xL
p- 449 (1860),
Amboina,
23. Cethosta insulata.
Cethosia insulata, Butler, Cist. Ent. i. p. 165 (1878),
Ké Dulan, 25th September, 1874.
24, Cethosia cydippe.
Papilo cydippe, Linnzeus, Syst, Nat. i. p. 776 (1766).
&. Amboina.
25. Hypolimnas nerina.
Papilio nerina, Fabricius, Syst. Ent, p. 509 (1775).
6 2. Ternate.
26. Hypolimnas lasinassa.
Papilio lasinassa, Cramer, Pap. Exot, ii. pl. cey. A, B (1779).
¢. Amboina.
194 * Mr. A. G. Butler on the
27. Precis hedonia.
Papilio hedonia, Linneeus, Mus. Lud. Uly. p. 279 (1764).
Amboina.
28. Precis timorensis.
Junonia timorensis, Wallace, Trans. Ent. Soc. 1869, p. 346.
Ké Dulan, 25th September, 1874.
Lycenide.
29. Gerydus Boisduvalit, sp. n.
Symethus pandu, Boisduval (nee Horsfield), Voy. de l’Astrolabe, p. 73.
n. 2 (1882).
g¢ ¢. Amboina.
‘This species is considerably larger than that from Java, and,
curiously enough, the colouring of the sexes is reversed, the
male of the Amboinese species having the basal three fifths of
the primaries white clouded with grey at the base, and the
female with a narrow angulated white band, nearly as in G.
leos.
30. Gerydus stygianus, sp. n.
Allied to G. learchus; above fuliginous brown with bronze
reflections; a whitish fusiform spot at base of third median
branch: wings below greyer than in Felder’s figure of G.
learchus, with a faint lilac tint, the markings rather narrower
and the band across the disk of primaries uninterrupted. HEx-
panse of wings 37 millim.
Ternate.
Unfortunately only one somewhat damaged example was
obtained of this interesting species.
31. Tarucus plinius.
Hesperia plinius, Fabricius, Ent. Syst. iii, 1, p. 284 (1793).
¢. Amboina.
32. Catochrysops trifracta, sp. nov.
g. Deep lilac, the thorax above blue-black ; head white ;
palpi with the terminal joint and a dorsal line black ; abdo-
men blackish grey: wings below much as in C. engjus, but
differing noticeably in the fact that the series of spots across
the disk of the primaries, instead of forming one slightly irre-
gular stripe, are broken into three parallel oblique bifid white-
edged brown dashes, one below the other; the secondaries
also have only one subanal black spot with pale yellow zone,
‘Challenger’ Lepidoptera. 195
and barely perceptibly touched with metallic scales, [Ex-
panse of wings 23-28 millim.
(Two damaged examples.)
Rat Island, Straits of Malacca, Ist September, 1873.
33. Lampides elianus.
Hesperia elianus, Fabricius, Ent. Syst. iii. 1, p. 280 (1798).
3 ¢. Ké Dulan, 25th September, 1874.
34. Lampides etherialis, sp. n.
3. Pale silvery blue above ; primaries with a narrow grey
external border and blackish fringe : secondaries with a sub-
marginal series of seven blackish spots, the fifth largest, the
sixth and seventh confluent; a black marginal line; costal
and abdominal borders pearl-white: body bluish white ; head
and collar brown. Wings below brownish grey, with white
and black markings, arranged as in L. aratus, except that the
orange zones of the ocelloid spots of secondaries are narrower.
Expanse of wings 31 millim.
2. Smaller, whiter above, the grey border of primaries
broader. Expanse of wings 29 millim.
Ké Dulan, 25th September, 1874.
The male of this species is of a beautiful silvery-blue colour,
most nearly approached in Lalmenus evagoras of Australia,
but of a purer (less green) shade. The female is more like
L. aratus.
35. Lampides aratus.
Papilio aratus, Cramer, Pap. Exot. iv. pl. ceclxy. A, B (1782).
3 ¢. Amboina, Ternate.
56. Lycena ertnus ?
Hesperia erinus, Fabricius, Syst. Ent. p. 525 (1775).
Ternate.
The examples are so much rubbed that it is impossible to
be sure of this identification.
Papilionide.
PIERIN:.
37. Delias plexaris.
Papilio plexaris, Donovan, Ins. New Holl. pl. xviii. fig. 2 (1805),
& ¢. Amboina,
196 Mr. A. G. Butler on the
38. Tertas photophita, sp. n.
3. Gamboge-yellow, with black borders, as in 7. hecabe,
from which, however, it differs in being considerably smaller,
in its pale colour, and narrower primaries; below lemon-
yellow, the borders visible through the wings; the usual
markings, with the exception of the black marginal dots, ill
defined. Expanse of wings 32 millim.
Ké Dulan, 25th September, 1874.
Nearest in size, form, and pattern of primaries to 7’. variata,
but deeper in colour ; with well-defined border to the secon-
daries, and no subapical brown patch on the under surface of
the primaries.
39. Terias biformis, sp. n.
Allied to 7. eumide and T. hecabe, the male differing from
the latter in its bright lemon-yellow (instead of deep gamboge)
colour, the external border obliquely cut off at external angle
and continued as a narrow squamose streak along the internal
margin ; the border of the secondaries narrower, more deeply
sinuated, and terminating in a few brown scales at the first
median branch, beyond which are only the usual black mar-
ginal dots; the female creamy white, with broad brown borders,
formed as in the male of 7. sarz. Expanse of wings 438
millim.
& 9. Amboina.
This is the first recorded instance of a species in this section
of the genus having a white female. It is a most interesting
form, being one of the links between the 7. rahel and T.
hecabe groups of species.
40. Tertas puella.
Xanthidia puella, Boisduyal, Voy. de l’'Astrolabe, Lép. p. 60, pl. ii. fig. 8
(1882).
g. Ternate.
41. Terias lerna.
Terias lerna, Felder, Sitzb. Ak. Wiss. Wien, math,-nat. Cl. xl. p. 448
(1860).
Amboina.
PaPimLionInaél.
42. Ornithoptera criton.
Ornithoptera criton, Felder, Wien. ent. Monatschr. iy. p. 225 (1860) ;
Reise der Nov. Lep. i: p. 12, pl. iv. a-c (1865).
od ?. Ternate.
‘Challenger’ Lepidoptera. 197
Unfortunately, like all the specimens collected at Ternate,
the pair obtained is much broken,
43. Papilio deiphontes.
Papilio deiphontes, Felder, Reise der Noy. Lep. i. p. 126 (1865).
o. Ternate.
44, Papilio nicanor.
Papilio nicanor, Felder, Reise der Noy. Lep, i. p. 102, pl. x. ¢, d (1865).
Ternate.
45. Papilio severus.
Papilio severus, Cramer, Pap. Exot. iii. pl. eelxxvii. A, B (1782).
6 ?. Amboina.
46. Papilio Thomsonit, sp. n.
&. Black-brown, primaries with paler scales sprinkled over
the basal area, a costal and four discoidal divergent longitu-
dinal lines of pale scales; costa, apex, and external border
fuliginous brown; traces of an oblique, subapical, creamy
whitish bar sometimes present; a broad irregular creamy-
white belt or patch (somewhat as in P. severus, but wider and
tapering to abdominal border, where it is squamose) across the
extremity of the discoidal cell and the disk of secondaries ;
sinuations of the external border with narrow cream-white
fringe: body as usual. Primaries below smoky brown, the
cell and the disk from the upper radial, with the exception of
the veins and a broad external border, blackish ; sometimes
three squamose oval creamy whitish spots placed obliquely
beyond the cell; the divergent lines of scales as above: secon-
daries black-brown, smoky brown upon the basi-abdominal
area, which is also sprinkled with white scales ; no trace of
the broad white belt of the upper surface ; seven large black
spots enclosing orange lunate spots parallel to outer margin ;
sinuations of outer margin white. Hxpanse of wings 113-
120 millim.
3. Ké Dulan, 25th September, 1874.
47. Papilio ulysses.
Papilio ulysses, Linneus, Mus. Lud. Ulr. p. 201 (1764).
9. Amboina.
48, Papilio polyphontes.
Papilio polyphontes, Boisduval, Sp. Gén. Lép. i. p. 268 (1836),
9. Ternate.
198 Mr. A. G. Butler on the
The single damaged example before me differs slightly from
the Celebesian type, the white areas on the primaries being
interrupted by a rather broad and very oblique band of the
ground-colour ; this may, however, prove to be an individual
variation.
Hesperiide.
49. Hesperia celenus.
Papilio celenus, Cramer, Pap. Exot. iy. pl. eeexevi. A, B (1782).
&. Amboina.
50. Pamphila Moseleyt, sp. n.
&. Upper surface similar to P. phineus, but larger, blacker,
the base not streaked with fulvous, the angular discal band of
the primaries narrower and that of the secondaries nearly twice
as broad ; below these bands are decidedly yellow ; the apical
area of the primaries and the whole ground-colour of the
secondaries are pale olivaceous instead of ochraceous or clay-
coloured, and there is a large patch of black near the anal
angle of the latter wings. LExpanse of wings 47 millim.
Ké Dulan, 25th September, 1874.
51. Pamphila phineus.
Papilio phineus, Cramer, Pap. Exot. ii, pl. elxxvi. E (1779).
¢. Amboina.
Cramer’s locality ‘‘ Surinam ”’ is here, as in other instances,
erroneous ; it is evident that some of the insects received by
him from the two localities got confounded either through his
own carelessness or that of those from whom he received
them.
52. Pamphila prusias.
Pamphila prusias, Felder, Sitzb. Ak. Wiss. Wien, math.-nat. Cl. xliii.
p- 44 (1861).
Amboina.
53. Padraona sunias ?
Pamphila sunias, Felder, Sitzb. Ak, Wiss. Wien, math.-nat. Cl. xl.
p. 462 (1860).
Ké Dulan, 25th September, 1874.
The single example before me is rather aberrant; it is,
however, somewhat broken, and may be only individually
separable from the Amboinese form.
‘Challenger’ Lepidoptera. 199
54. Tagiades japetus.
Papilio japetus, Cramer, Pap. Exot. iv. pl. eeelxv. E (1782).
Amboina.
This species is also in the British Museum from Ké Island.
Sphingide.
55. Protoparce cingulata.
Sphinx cingulata, Fabricius, Syst. Ent. p. 545 (1775).
d. Ternate.
The appearance of this New-World species at Ternate is
very surprising; it is probably only an accidental immigrant.
The specimen was much worn and shattered, and may have
been long on the wing. Some of the Sphingidz have been taken
at an almost incredible distance from land, showing that their
flight is not only extremely rapid, but capable of being sus-
tained for a considerable time.
Agaristide.
56. Ophthalmis lincea.
Phalena lincea, Cramer, Pap. Exot. iii. p. 61, pl. cexxviii. B (1782).
Ké Dulan, 25th September, 1874.
Originally described from an Amboinese example supposed
by Cramer to have come from Surinam ; the species is found
(and is probably common) at Ceram and New Ireland ; an
allied species, O. bambucina, takes its place in the Philippines.
Cocytiide.
57. Cocytia Durvillet.
Cocytia Durvillei, Boisduval, Mon. Zyg. p. 22, pl. i. fig. 1 (1829).
Ké Dulan, 25th September, 1874.
Not rare in New Guinea, though doubtless a rapid flier.
Zygenida.
58. Euchromia ganymede.
Glaucopis ganymede, Doubleday, Lort’s Discov. Austral., Append. i,
p. 519, pl. iii. fig. 3,
&. Ké Dulan, 25th September, 1874.
200 Mr. A. G. Butler on the
Lithosiide.
59. Dyphlebia liboria.
Phalena liboria, Cramer, Pap. Exot. iv. p. 106, pl. eeexlv. D (1782).
9. Amboina.
60. Hypsa heliconia,
Phalena (Noctua) heliconia, Linnzeus, Syst. Nat. i. p. 839 (1766).
& 2. Amboina.
61. Hypsa lanceolata.
Hypsa lanceolata, Walker, Cat. Lep. Het. vii. p. 1675 (1856),
9. Amboina.
Originally described from a female obtained at Celebes.
We have a male in the Museum probably from the same col-
lection.
62. Clets evander.
Papilio evander, Cramer, Pap. Exot. iv. pl. eeexxxi. F, G (1782).
& ¢. Amboina.
Liparida.
63. Artaxa simulans, sp. n.
A remarkable copy of Ophthalmis lincea from the same
locality. Primaries black-brown, densely irrorated with black
scales ; a large ochreous spot at apex: secondaries with the
basi-abdominal half black and the externo-apical half bright
orange, the line of demarcation between the two areas being
elbowed outwardly at the inferior angle of the cell: head,
antenne, collar, tegule, and prothorax ochreous ; remainder
of thorax and abdomen black; anal tuft pale testaceous.
Wings below as above. Expanse of wings 47 millim.
Amboina.
This is one of those instances of mimetic assimilation so
perfect as to catch the eye at the first glance. That the Aga-
ristid is the species copied cannot be questioned, since it is
not only a common form, but it belongs to a group which, like
the allied Zygenide, is evidently distasteful to insect enemies.
64. Stilpnotia, sp.
A white species, too much injured to be described, but
interesting as representing the genus in a locality where it
would not have been supposed to occur.
¢. Amboina.
“Challenger? Lepidoptera. 201
65. Pegella ichorina, sp. n.
?. Allied to P. curvifera. Primaries above white, crossed
by three nearly equidistant golden-brown stripes—the first
interrupted, angulated, just before the basal fourth of the wing,
the second rather broad, oblique, crossing the middle of the
wing, and confluent with an angular discocellular fasciole of
the same colour, the third narrow, oblique, crossing the disk
halfway between the central stripe and the outer margin ; two
or three basal spots, the veins, a spot in the cell, and a mar-
ginal series of spots golden brown: secondaries rose-pink,
becoming gradually white towards outer margin, where there
is a series of little brown dashes: body above sordid whitish ;
antenne black. Wings below white, showing traces of the
markings of the upper surface; costal borders and veins sor-
did; marginal spots or dashes as above ; interno-median area
of primaries slightly tinted with pink ; secondaries with the
basal two thirds tinted with pink; abdominal area washed
with rose-pink: body sordid whitish; anterior legs blackish.
Eixpanse of wings 100 milim.
Amboina.
Euschemide.
66. Bursada perdica.
Phalena perdica, Cramer, Pap. Exot. ii. p. 126, pl. clxxviii. E (1779).
Var. Bursada truncata, Walker, Cat. Lep. Het. Suppl. p. 191 (1864).
So ¢- Amboina.
Of this species an instructive series was obtained, completely
linking the two forms associated above.
67. Craspedosis ernestina.
Phalena Geometra ernestina, Cramer, Pap. Exot. iv. p. 156,
pl. ecclxix. F (1782).
Celerena sobria, Walker, Cat. Lep. Het. Suppl. p. 164 (1864),
& ¢. Amboina.
In his ‘Catalogue’ Walker states that C. sobria is the
type of his genus Celerena; the latter genus, however, had
been already described by him in the ‘ Transactions of the
Entomological Society’ for 1862, pp. 71, 72, with C. divisa
as type. The two species are not congeneric.
3 . :
me}
Uraniide.
68. Alcidis orontes.
Papilio orontes, Linneeus, Amcen, Acad. vi. p. 402.
g. Amboina.
Ann. & Mag. N. Hist. Ser. 5. Vol. xii. 14
—s Ae Ee a
jee. ans
202 On the ‘Challenger ’ Lepidoptera.
Palyade.
69. Humelea rosalia.
Phalena Geometra rosalia, Cramer, Pap. Exot.iv. p. 152, pl. ceclxviii.
F (1782).
Ké Dulan, 25th September, 1874.
70. Humelea ludovicata.
Eumelea ludovicata, Guénée, Phal. i. p. 393.
Amboina.
Acontiide.
71. Xanthodes transversa.
Xanthodes transversa, Guénée, Noct. ii. p. 211 (1852).
Xanthodes intercepta, Walker (nec Guénée), Cat. Lep. Het. xii. p. 778
(1857).
Ké Dulan, 25th September, 1874.
Walker transposed X. transversa and intercepta in his
‘ Catalogue.’
Hypopyride.
72. Spiramia funestis, sp. n.
¢. Nearest to 8S. spiralis; velvety fuliginous brown,
paler beyond the middle and at the base of the primaries, the
pale area being bounded by an elbowed black stripe; two
ill-defined blackish diffused discal stripes, the inner one sepa-
rating the dark and pale areas, sinuous on the primaries and
regularly undulated but straight and central on the secon-
daries, the outer one bounding the external area, terminating
before the apex of the primaries in an oblique angle and
barely visible upon the secondaries ; the usual spiral ocelloid
marking with the spot unusually small and less black than
usual; external area slightly greyish, fringe whitish: prima-
ries with a submarginal series of black dots: thorax as usual,
brown varied with black ; abdomen velvety black, with the
two terminal segments vermilion. Wings below smoky brown
with pale fringe; the primaries crossed beyond the middle
and the secondaries in the middle by two parallel dusky stripes,
slightly inangled towards the costal margin of primaries and
arched on the secondaries: body below vermilion ; tibiz and
tarsi brown; anus pale ochreous. Expanse of wings 71
millim.
3g. Amboina.
On the Polyzoa of Queen Charlotte Islanits. 203
Ophiuside.
73. Ophiusa simillima.
Ophiusa simdlima, Guénée, Noct. iii. p. 266 (1852).
Amboina.
Margarodide.
74. Glyphodes? Ledereri, sp. n.
Glyphodes actorionalis, Lederer (nec Walker), Wien. ent. Monatschr.
vii. pl. xiv. fig. 4 (1863).
Amboina.
Walker’s species comes nearer to Lederer’s G. Zeller?’ J
am not satisfied that G. Ledereri is a true Glyphodes.
XXIV.—Report on the Polyzoa of the Queen Charlotte Islands.
By the Rev. THomas Hincxs, B.A., F.R.S.
[Concluded from page 58. }
[Plate IX.]
Suborder CyCLOSTOMATA.
Family Crisiide.
CRISIA (part.), Lamouroux.
Crista cornuta, Linneus.
Houston-Stewart Channel; Virago Sound; common,
[Norway, Britain, Brittany, Mediterranean. |
Crista eburnea.
Virago Sound.
[North and Arctic Seas, St. Lawrence, Labrador, St.
George’s Banks, California, Fiji Islands, New Zealand and
Australia, Madeira, Mediterranean, Britain. }
Crista denticulata, Lamarck.
Houston-Stewart Channel.
[Kara Sea, Norway, Spitzbergen, Grand Manan, Britain,
Adriatic, Madeira, South Africa. ]
14*
204 Rev. T. Hincks on the
Family Tubuliporide.
Sromatopora, Bronn.
Stomatopora major, Johnston.
On shell, rare.
(Bergen, Britain, Brittany.]
Stomatopora diastoporides, Norman.
On shell.
[Entrance of Baffin’s Bay, Gulf of St. Lawrence, Britain.]
Stomatopora tncrassata, Smitt.
A specimen occurs exhibiting the anastomosing habit
which is characteristic of British examples of this species.
Cumshewa; Houston-Stewart Channel.
[Spitzbergen, Nova Zembla, Kara Sea, Britain. ]
TuBULIPORA, Lamarck.
Tubulipora lobulata, Hassall.
Houston-Stewart Channel, on shell.
{Scandinavian coasts, Britain. |
Tubulipora perfragtlis, n. sp.
Zoarium adnate, white, and composed of very delicate ma-
terial, consisting of a short stem, widening upwards, which
divides dichotomously into two principal branches, these again
subdividing dichotomously, the lower segments curving down-
wails so as almost to surround the point of origin and the
stem: and giving to the whole colony a flabellate form ;
brandhes slender at the base, expanding upwards, thickly
covered with the cells, occasionally a second expansion origi-
natimg from the summit of the first, to which it is connected
by @ narrow base. Zowcia crowded on the branches, radi-
ately disposed, very slender, with a speckled surface, a large
porti6ii of the length Sec uid crbhorizental, sometimes con-
nate and in companies of 2-4, sometimes single and detached ;
orifice orbicular, unarmed. Gonocyst an irregular inflation of
the surface of the branch, minutely punctate.
On shell.
This form has some points of resemblance to Tubulipora
capitata, mihi (‘ Annals’ for August 1881, “ Contributions
Polyzoa of Queen Charlotte Islands. 205
towards a General History of the Marine Polyzoa”’), an Aus-
tralian species; but there are differences in the habit of
growth and in some of the details of structure which probably
entitle it to a distinct name. ‘The present species is exceed-
ingly delicate and of most graceful form. ‘The branches seem
to be slightly attached and are commonly free towards the
extremities; the tubes are remarkably slender, and the free
portions are horizontally inclined rather than erect. 7’. per-
fragilis bears much resemblance to D’Orbigny’s figure of his
Idmonea cenomana (Pal. Frang., Terr. Crétacés, vol. v. Atlas,
pl. 633. fig. 2).
Tubulipora Dawsoni, n. sp. (Pl. LX. fig. 5.)
Zoarium forming a spreading, irregularly shaped, intricate,
coral-like mass, composed of many branches, much divided
and subdivided dichotomously, which radiate from the point
of origin and anastomose freely ; branches massive, of consi-
derable width, somewhat compressed, flattened in front, ex-
panding upwards, bifid or trifid at the extremities, which are
cellular, recumbent or suberect, never adnate, but attached by
numerous calcareous -offsets from the dorsal surface to the shell
or stone on which the colony grows. Zowcia arranged (in
part) in transverse rows (two to five in each), which slant
slightly downwards, connate, with a large suborbicular orifice,
increasing in height from the inner side outwards, so as to
give a serrated appearance to the edge of the branch ; the rows
sometimes extending to the centre of the branch, but not sepa-
rated by any distinct mesial line, sometimes (and more com-
monly) ranging along the sides, the centre being occupied
by many detached cells irregularly distributed, with a sube~-
bicular orifice, which is usually scarcely raised above tl
surface ; walls thickly and minutely punctate; the dorsal sur
face rounded, lineated longitudinally, punctate, often. with
transverse furrows.
Common amongsi the dredgings; on shells and stones.
In this fine species the disposition of the cells connately in
transverse rows is very much confined to the sides of the
branch, and a striking characteristic is the crowd of scattered
cells which very commonly fills the centre. The latter are
generally very slightly raised above the surface of the zoarium.
‘The rows vary in length and occasionally extend to the centre
of the branch; but usually the condition is as I have de-
scribed it. The zocecia composing them increase in height
trom within outwards, and the tallest form a conspicuous line
along the margin of the branch. The branches are for the
206 Rev. T. Hincks on the
most part broad and compressed, and inosculation takes place
freely. A peculiarity which at once arrests attention is the
large development of dorsal appendages for the purpose of
attachment: these are short, cylindrical, calcareous processes,
which are given off in great number from the under surface
of the branches, and become firmly soldered to the body on
which the polyzoon grows (Pl. IX. fig. 5a).
I have great pleasure in naming this form, which is a very
characteristic member of the Polyzoan fauna of the Queen
Charlotte Islands, after Dr. G. M. Dawson.
Tubulipora fasciculifera, n. sp.- (Pl. IX. fig. 6.)
Zoarium flat, thin, closely adnate, flabellate. Zowcia free
and erect above, depressed below, the free extremities dis-
posed in short, disconnected, more or less divergent series, which
range in radiate fashion (but somewhat irregularly) towards
the margin, the series sometimes composed of a single line of
connate tubes, sometimes of two lines placed side by side,
sometimes of clusters (or fascicles) of tubes ; orifice orbicular,
unarmed ; surface thickly speckled. Gonocyst an inflation of
the zoarium, usually placed near the margin, involving a num-
ber of the zocecial tubes ; surface covered with minute disks
closely packed together.
On shell.
The fasciculate arrangement of the zocecia is the most dis-
tinctive character of the present species, but many single lines
of cells mingle with the composite series. It grows in flabel-
late patches, which sometimes give off long linear or subclavate
lobes. The free portion of the cell is much elevated and more
than suberect.
/ So far as the character and arrangement of the zocecial
erles are concerned, the Cretaceous Multifascigera Campit-
~ cheana, D’Orbigny, curiously resembles the present form (see
Paléont. Frang. vol. v., Atlas, pl. 762. fig. 8).
Drasropora (part,), ’Lamouroux.
Diastopora patina, Lamarck.
Cumshewa, on Tubulipora and Myriozoum.
[North and Arctic Seas, South Labrador, Britain, France
(S.W.), Adriatic. ]
Diastopora sarniensis, Norman,
Off Cumshewa, 20 fms.
[English coasts (south-west and south-east), Mediterranean
(probably). ]
Oe
Polyzoa of Queen Charlotte Islands. 207
Diastopora suborbicularis (?), Hincks.
[=D. simplex, Busk.]
On shell.
_[Greenland, Finmark, Britain, Naples. ]
A single specimen occurs, imperfectly developed, which
seems to have the characters of this species. A larger portion
of the cell is free than is usual in D. suborbicularis ; but there
is always much diversity in this respect, due to difference of
habitat. The margin of the zoarium is slightly lobate, but
this may be owing to the immature condition of the specimen.
Family Lichenoporide.
LicHENOPORA, Defrance.
Lichenopora hispida, Fleming.
On shell.
[Norway, Finmark, Greenland, South Labrador, Britain,
France (S.W.), Naples. ]
Lichenopora verrucaria, Fabricius.
Virago Sound, on Sertularella.
[Norway, Arctic Seas, Bay of Fundy, St. George’s Banks,
Britain (North and West).]
Suborder CTENOSTOMATA.
Family Alcyonidiide.
ALcYONIDIUM, Lamouroux.
Alcyonidium gelatinosum, Linneeus.
Virago Sound.
[North and Arctic Seas, North America, Britain, Natal.]
Family Vesiculariide.
BoOWERBANKIA, Farre.
A member of this genus occurs on Sertularians from Virago
Sound, which is probably referable to B. imbricata, Adams,
form densa, Farre.
[White Sea, Caspian Sea, Britain. ]
208 Rev. T. Hincks on the
Family Buskiide.
Busta, Alder.
Buskia nitens, Alder.
Virago Sound, ona Sertularian ; also creeping over Cellaria.
[Davis Straits, White Sea, Barents Sea, Britain. ]
Family Cylindreciide.
CyLinpracium, Hincks.
Cylindracium giganteum, Busk.
Jn the specimens which I refer to this species, the cell is
of more slender habit than in British examples and the ecto-
cyst less opaque ; but these differences are of slight moment,
and I have little doubt that the Pacific form is specifically
identical with our own.
[ Britain. ]
[Group ENTOPROCTA. }
Order PEDICELLINEA.
Family Pedicellinide.
PEDICELLINA, Sars.
Pedicellina gracilis, Sars.
Virago Sound.
(Norway, Spitzbergen, White Sea, Britain.]
APPENDIX.
Family Cellulariide.
Menipea ternata, Ellis & Solander.
The form occurs in which the two lower cells in the triplet are
much elongated and attenuated, and the habit in consequence
is much more slender and graceful than in the normal condi-
tion. Smitt has recorded this variety from the north.
Menipea compacta, n. sp., form triplex.
(Pl. TX.dig: 8.)
[Described in ‘ Annals’ for December 1862, p. 461.]
Only a small and imperfectly developed example of this
species occurs amongst Dr. Dawson’s dredgings; but very
Polyzoa of Queen Charlotte Islands. 209
fine specimens from California (where it seems to be ex-
tremely abundant) and Vancouver Island enable me to cor-
rect my description of it in one or two particulars.
I find that on the same colony internodes composed of three
cells are mingled with others bearing five or six, so that it is
incorrect to designate the triple condition as a distinct form.
We have a similar variation in Menipea ternata. 'The oper-
culum is not ‘acicular,” as described, in its fully developed
state, though always very moderate in size. It is usually, in
its perfect condition, clavate, expanding slightly above.
M. compacta grows in luxuriant bushy tufts, which bristle
with spines.
Family Cellariide.
Cellaria mandibulata, n. sp. (Pl. IX. fig. 7.)
[ Described in ‘ Annals’ for December 1882, p. 463. ]
The figures represent the avicularium, which exhibits pro-
bably the least specialized form of the appendage in the Cel-
larian series, and a shoot of the natural size, in which there
is a curious departure from the usual dichotomous ramifica-
tion. The branches are given off from the stem at intervals
on each side, instead of forming a fork at the joints. This
peculiarity, however, does not appear to be characteristic of
the species.
Family Membraniporidz.
Membranipora velata, Hincks.
This Californian species occurs on shells dredged off Cum-
shewa ; but the specimens from the Queen Charlotte Islands
are destitute of the large avicularia. (See ‘ Annals’ for
August 1881, p. 130.)
Membranipora acifera, MacGillivray, form multispinata.
[‘ Annals’ for December 1882, p. 465, pl. xix. fig. 4. ]
In a previous portion of this Report I have referred a
Membranipora from the Queen Charlotte Islands to the JZ.
acifera ot MacGillivray*, of which it seemed to me to be a
variety. But in a paper read before the Royal Society of
Victoria, October 12, 1882, MacGillivray states that further
examination has led him to identify this species with his JZem-
branipora serrata, which is certainly quite distinct from the
North-Pacific form. I shall therefore characterize the latter as
* Described and figured in a paper read before the Royal Society of
Victoria, December 9, 1881.
210 Rev. T. Hincks on the
Membranipora pallida, n. sp.
Zoecia elongate-oval, front wall wholly membranous, quin-
cuncially disposed, margin thin, smooth, usually slightly
elevated at the top ; an erect spine on each side above and from
six to eight slender pointed spines down each side, which in-
cline inward; generally at the bottom of the cell, on a small
quadrate area, an aviculartum with an expanded base (occu-
pying the area) and a very long, slender, tapering beak,
which stretches upward along the margin; mandible trian-
gular below, above setiform. Occium (?).
Zoarium whitish, texture delicate.
Virago Sound; spreading luxuriantly over shell.
Membranipora exilis, n. sp.
[ Described in ‘ Annals’ for December 1882, p. 466. ]
On further examination of this species I find that it agrees
with MW. radic¢fera, Hincks, in being attached (in some cases
at least) by radical tubes given off from the dorsal surface.
It is not closely adnate to the surface on which it grows, as
most of the Membranipore are, but is furnished with special
organs of attachment. ‘The first specimen which came under
my notice (and on which my description was based) is grow-
ing on Celiaria borealis, the stem of which 7 loosely invests ;
in this case I have not been able to detect any of the dorsal
appendages. But on a colony which spreads over a Tubuli-
pora they are present in great numbers, and there can be no
doubt that it is anchored by the radical tubes and not adhesive.
In both cases the dorsal surface of the cells is convex and
rounded, and clearly unfitted for direct attachment. Probably
the presence or otherwise of the appendages is dependent on
the nature of the habitat.
I have already (‘ Annals’ for July 1881, p. 5, under Mem-
branipora radicifera) drawn attention to certain links con-
necting the Membraniporidan series with such forms as
Bugula and Diachoris. We have another such link in the
present species. A Membranipora which, from the nature of
its habitat, had ceased to be adherent and had developed
radical fibres as a means of attachment, would have made a
very decided advance towards the Bugulan type.
Family Porinide.
Lagenipora spinulosa, n. sp.
| Described in ‘Annals’ for January 1884, p. 57. |
When I first described this species I had only met with
Polyzoa of Queen Charlotte Islands. 211
small incrusting colonies, and was under the impression that
they represented the mature and perfect form. I now find,
however, that this is by no means the case. When fully
erown the zoarium of Lagenipora spinulosa is erect and ra-
mose (Pl. IX. fig. 4), consisting of a cylindrical stem, which
divides and subdivides dichotomously, the branches termina-
ting above in short bifid segments. The zowcva are arranged
longitudinally in six lines along the stem and branches, those
in neighbouring lines alternating; the oral (or neck-like)
portion free and projecting, the lower immersed. 'The surface
of the cell is covered with very large foramina, which are
closed in by membrane. Primary orifice elliptical, slightly
narrowed below. The surface of the owcitwm is smooth, and
entire behind ; a raised line arches across it towards the front,
and the portion in advance of this line is covered with minute
disks closely packed together.
In its pertect condition this species bears a close resemblance,
so far as habit and general appearance are concerned, to an
Entalophora.
The wall of the cell is built up of tubes placed longitudi-
nally and closely appressed to one another; this curious
structure may be best observed in the erect neck-like portion
of the zocecium. The superficial foramina are probably the
openings of the tubes.
The lateral avicularia are supported on a tubular structure,
which may be traced stretching down the inner wall of the
oral cylinder (neck) and tapering off finely below. Lagent-
pora spinulosa would seem to be abundant where it occurs ;
it must be accounted one of the most interesting forms which
Dr. Dawson’s dredgings have yielded.
Family Myriozoide (part.).
Schizoporella cruenta, Norman.
This species must be added to the list of North-Pacifie
forms. ‘The single specimen which occurs is in fine condition,
and has the oral sinus much more strongly marked than the
British examples which I have examined. The deep-red
colour of the zoarium when fresh has given place toa uniform
black.
[Nova Zembla, Greenland, Britain, from Shetland to the
Channel Islands. |
Schizoporella biaperta, Michelin.
A specimen has occurred in which the oral avicularia as-
pb Rev. T. Hincks on the
sume both the round and spatulate form, as is commonly the
case In the allied Schizoporella armata, mihi.
Schizoporella Dawsont.
[Described in ‘ Annals’ for June 1883, p. 449. ]
The species described under the above name I have now no
doubt is identical with LEscharina torguata of D’Orbigny
(‘ Voyage dans Amérique méridionale,’ tome v. 4° partie,
p- 11, =flustra torquata, Lamouroux). Schizoporella tor-
guata must therefore take the place of S. Dawsoni in the
Report. I have, however, much pleasure in dedicating a fine
species of Yubulipora (which I trust will prove to be unde-
scribed) to the able investigator to whom we are indebted for
our knowledge of the marine fauna of the Queen Charlotte
Islands.
Schizoporella torquata (D’Orbigny), Lamx.
(PIA tig. 2: )
Virago Sound, on shell.
[Bay of Rio, on dead shells. |
Schizoporella linearis, Hassall, form ¢narmata.
The only specimens amongst the dredgings which are refer-
able to this species are totally destitute of avicularia. In
other respects they agree with the typical form, and must be
regarded as an unarmed variety.
[Seandinavia, South Labrador, Mediterranean, Britain,
France (S.W.). ]
Family Escharide (part.), Smitt.
Lepralia cletdostoma, Smitt, var.
A variety of this species occurs which is destitute of avicu-
laria. ‘There is frequently a small knob on each side of the
orifice, and always a stout mucro immediately below it. The
ocecia do not exhibit the strie which Smitt describes, but are
smooth and polished. ‘The only specimen, however, which I
have examined is strongly calcified and has a highly varnished
surface, and in this condition the striae may be obliterated.
An Australian variety has already been described with circular
instead of pointed avicularia (‘ Annals’ for August 1881,
p. 122).
? Porella argentea, n. sp. (Pl. LX. fig. 1.)
Zoecia ovate, quincuncial, rather depressed (sutures shal-
Polyzoa of Queen Charlotte Islands. 213
low), surrounded by raised lines, surface thickly covered with
punctures ; orifice expanded above and well arched, contracted
below ; peristome slightly raised, especially above, a very
prominent hinge-denticle on each side a little above the lower
margin ; immediately below it an umbonate swelling, bearing
on its inner aspect an aviculardum, with rounded mandible,
directed upwards. Occiwm rounded, not prominent, surface
somewhat roughened, usually a circular pore on the front.
Zoartum white and silvery.
Houston-Stewart Channel, on shell.
Mucronella spinosissima, Hincks.
On further examination I find that in the younger cells there
are two or three lines of pores forming a belt round the mar-
gin; and it seems probable that the curious tubular system
which I have described (‘ Annals’ for January 1884, p. 53)
owes its origin tothese. Atleast I can only explain it by sup-
posing that, as calcification proceeds, it is arrested by the
pores, and only extends round them and not over them ; so
that they continue open, and form at last tubular shafts piercing
the stony crust which has been piled up about them.
Retepora Wallichiana, Hincks.
This species has been obtained in Vancouver Island.
General Remarks.
The number of species recorded in the present Report from
the Queen Charlotte Islands is 96, of which 36 appear to
have been hitherto undescribed. Of the 60 species known to
science more than a third (24 at least) seem to be distinctively
Arctic forms, and of these 17 occur in the British seas *.
Migration has taken place on the side of Davis Straits and
Behring Straits: on the one the circumpolar species have
distributed themselves along the North-American coasts and
more or less widely along those of the British Islands; on
the other they have colonized the nearer portions at least of
the North Pacific. In the comparatively warm waters which
* The seven Arctic species which occur in the Queen Charlotte Islands
but not in Britain are Cellaria borealis, Flustra membranaceo-truncata,
Membranipora S phie, Smittia plicata, Retepora Wallichiana, Cellepora
incrassata, and Myriozoum coarctatum. The whole number of species
common to the Islands and Britain is forty-three. .
214 On the Polyzoa of Queen Charlotte Islands.
bathe the shores of the Queen Charlotte Islands they evi-
dently find a congenial home and are finely developed.
There is nothing to show that they are unfavourably affected
by the change of climate. Of these northern forms only one
seems to reach the Mediterranean ; a few are widely distributed
in the British seas, while the rest are pretty much confined to
Shetland and the north-east and north-west coasts. In Prof.
Verrill’s ‘Check-List of the Marine Invertebrata of the
Atlantic coast, from Cape Cod to the Gulf of St. Lawrence’
(1879) thirty-one species are included which occur in the
(Jueen Charlotte Islands, and of these nineteen are Arctic; so
that the results of the northern migration have been much the
same on both sides of the continent.
The remaining species obtained by Dr. Dawson constitute
a somewhat miscellaneous company. They include a small
group of cosmopolitan forms which occur in almost all lati-
tudes, and are expected, as a matter of course, to be present
wherever Polyzoa are found. Such are Microporella ciliata
(perhaps the most widely distributed species in the class),
Schizoporella hyalina (which almost equals it in this respect),
Smittia trispinosa, and perhaps Hippothoa distans. A few
species occur which have been found as far up the Pacific
coast of America as California and Vancouver Island, but
which are not known as Arctic forms. These are no doubt
southern species which have travelled so far northwards.
Indeed the Queen Charlotte Islands are, in a remarkable
degree, the meeting-ground of northern and southern forms.
Membranipora Rosselii, M. tenutrostris, Cribrilina radiata,
Schizoporella Cecilit, S. sanguinea, S. torquata, and Diastopora
suborbicularis are essentially southern.
Seventeen species are common to the Islands and Australia,
and of these thirteen are also Kuropean: nine of them occur
in the Arctic seas. ‘Two have only been found, so far, in
Avstralia and the Queen Charlotte Islands (Porella marsupium
and Mucronella spinosissima). Lepralia cleidostoma has oc-
curred in these two localities and off the coast of Florida.
It may be noted here that of the whole number of Queen
Charlotte Islands species only nine are not also European.
Some of the ascertained facts respecting the distribution of
the Polyzoa are sufficiently perplexing, and we must wait for
a larger accumulation of data before we may hope to explain
them satisfactorily. ‘The way in which certain species are
strewn, as it were, at haphazard over the surface of the globe
is a difficulty of which the solution is not apparent. We must,
I think (as I have suggested before), make large allowance
for the agency of man, and of currents, floating weed and
On Schizoporella Ridleyi and §. simplex. 215
timber, &c., in the diffusion of the species, apart from the
general laws which preside over the distribution of life.
Further light will no doubt be thrown on the relations of
the Polyzoan fauna of the Islands when we know more of the
history of the group of new forms recorded in this Report.
We may venture, I think, to say, that they are not to any
large extent Arctic. Are they southern coast-line emigrants,
or do they occupy their original home ?
EXPLANATION OF PLATE IX.
Fig. 1. ? Porella argentea, n. sp.
Fig. 2. Schizoporella torquata (D’Orbigny), Lamx.
Fig. 3. Cellepora? n.sp. (brunnea); a cluster of zocecia, showing one of
the marginal decumbent cells.
Fig. 4. Lagenipora spinulosa, n. sp.; erect form, nat. size.
Fig. 5. Tubulipora Dawsoni, n. sp., nat. size. 5a. Portions of the stem
showing the offsets from the dorsal surface, by which the zoa-
rium is attached. 66. Portion of a branch, showing the dispo-
sition of the zocecia. 5c¢. The extremity of a branch, showing
the cellular capitulum and several of the scattered central
zocecia.
Fig. 6. Tubulipora fasciculifera, n. sp.; portion of the zoarium, showing
the arrangement of the zocecia. 6a. A colony, nat. size.
1g. 7. Cellaria mandibulata, n. sp.; avicularian cell. 7a. Nat. size,
showing a peculiarity in the ramification.
Fig. 8. Menipea compacta, n. sp.; front view of an internode. 8a,
Dorsal surface.
XXV.—On Schizoporella Ridleyi, MacG., and Schizopo-
rella simplex, D’ Orbigny and Johnston. By J. J. QuELCH,
B.Se. Lond., Zoological Department, British Museum.
THE Schizoporella Ridleyi, MacGillivray, was orignally de-
scribed as S. marsuptum by Mr. Ridley, who identified it
with Lepralia marsupium, MacG., having been misled by the
short and incomplete description of this species, which was,
moreover, as stated since by Mr. MacGillivray, drawn up
from a bad specimen. And certainly, if excuse were needed
for such an identification, | may state that the agreement
between the type specimen of the ‘ Alert’ collection described
by Mr. Ridley, and the description and figures of L. marsu-
ptum given by Mr. MacGillivray in the Prodr. Zool. Vict.
decade iv., seems to me much closer than is the agreement
between the figures given since by Mr. MacGillivray (Roy.
Soc. Vict. 1882) for Porella (Lepralia) marsupium and his
previous description and figures of the same species.
The ‘ Alert’ species, being found by Mr. MacGillivray to
216 Mr. J. J. Quelch on Schizoporella Ridleyi, MacG..,
be distinct from his Porella marsupium, was named by him
after Mr. Ridley; and as some misconception of the real
characters of the species exists, I have deemed it advisable,
after examining the type specimen, to give a more detailed
description than has been given of a few of its leading features,
in order to point out its specific distinctness from Schizoporella
(Escharina) simplex, D’Orbigny, to which species Mr. Hincks
has recently assigned it (Ann. & Mag. Nat. Hist. January
1884, p. 51).
The most striking feature of Schtzoporella Ridleyt is the
infraoral, bluntly-pointed projection on which the avicularian
pore is situated. This is not merely a swelling of the
common wall of the zocecium, for where the projection has
been broken away a delicate membranous wall still remains
beneath it in continuity with the zocecial wall. It seems
rather to be the basal portion of the avicularian cell itself,
which entirely occupies the large circumscribed area below
the mouth of the cell, as originally pointed out by Mr.
Ridley.
A clearer idea of this projection will be formed by viewing
it from the side, so that 1t may be seen in profile, as it would
be if a median longitudinal section of it were made. It will
then be seen to arise, at its inferior part, somewhat above the
middle of the zocecium, as a slightly convex line forming an
angle of at least 45° with the surface-wall of the zocecium,
continuing outwards and forwards until it is joined by a line
drawn from the sinus in the lower lip of the mouth at right
angles to the zocecial wall. The length of this perpendicular
line gives the height of the projection above the zocecium ;
and this corresponds very nearly with the length of the cell-
mouth, except in the youngest zocecia at the edges of the
colony, where the projection is smaller, but still quite distinet
and prominent. ‘This raised portion, seen from the front, is
nearly semicircular in outline, the curved portion terminating
at the lateral angles of the mouth, while the straight, flat,
superior portion forms a platform, so to speak, immediately
below the mouth. At the outermost pointed limit of this
platform is the avicularian opening, which can only be dis-
tinctly seen by looking down from the top of the zocecium, as
it were.
The lower lip of the aperture of the zocecium in this species
is straight, with a shallow median rectangular sinus; there is
no sinus in the edge of the infraoral projection, that shown
apparently in such a position in figures of the species being
really in the lower lip of the aperture of the cell, supposed to
be seen above the projection; the surface is glistening and
and Schizoporella simplex, D’Orbigny and Johnston. 217
more or less hyaline, almost smooth or very finely and sparsely
punctated; the zocecia are convex, nearly as broad as long,
separated by rather deep depressions, the sutures being thin
lines often slightly raised. In the type specimen I can find
no distinct areolations, such as those mentioned by Mr. Mac-
Gillivray, around the margins of the old cells, but there are
often faintly marked radiating lines ; two short lateral spines
are almost constantly present on the aperture, three or four
longer ones being on the young zocecia.
On comparing this more complete description of the species
with the description and figures of Escharina simplex, D’Orb.,
I think it must be considered that the two species are
quite distinct. In this Schizoporella (Escharina) simplex,
D’Orb., attention must be called to the rounded lateral angles
of the mouth producing an oval shape transversely, to the
rather deep rounded sinus of the lower lip, to the complete
absence of spines, to the numerous and distinct punctures on
the surface of the zocecium, and more especially to the nature
of the ‘ tubercule’”’ below the mouth on which the pore is
situated—this “ tubercule”’ being present as a rounded pro-
tuberance of the wall, seen, in the lateral view that D’Orbigny
gives in fig. 8, as being scarcely raised above the general sur-
face of the zocecial wall, whereas in Schizoporella Ridleyt,
MacG., this projection forms a comparatively immense
rostrum.
Even making allowance for the probable incompleteness of
D’Orbigny’s description and figure, and for a possibly great
variability in the species, it does not seem to me that differ-
ences such as those mentioned taken together can be safely
regarded as being within the limits of specitic variation ; and
hence it seems that the two species must be considered
distinct.
In any case, however, Schizoporella (Escharina) simplex,
D’Orb., seems to be sufficiently diagnosed to be recognized ;
and as, I believe, it claims priority over Schizoporella sim-
plex, Johnston, this latter name must give way. D’Or-
bigny’s species bears the date 1839 against it, and is printed
in Part 4, vol. v. of the ‘ Voy. dans Amér. Mérid.,’ which bears
the date of publication 1839-46. Dr. Johnston’s species was
published in the second edition of the ‘ Zoophytes’ in 1847.
For this form described by Dr. Johnston, which is thus
destitute of a name, I propose that of the distinguished author,
so that the species may be known as Schizoporella (Lepralia)
Johnston.
Ann. & Mag. N. Hist. Ser. 5. Vol. xiii. 15
218 Mr. Bryce Wright on new Stylasteride.
XXVI.—On new Stylasteride.
To the Editors of the Annals and Magazine of Natural History.
GENTLEMEN,—In the current February number of the Ann.
& Mag. Nat. Hist. I notice that Mr. Quelch (Brit. Mus. Zoo-
logical Department), in describing some new forms of the
above group, has criticized a paper of mine published in vol. ix.
(1882), in which I described. two new forms of Disticho-
pora; and I crave to be allowed space for a few lines in reply,
the more so as his remarks are slightly inexact or misleading.
I did not profess to give a complete list of the Distichopores
either of the Pacific or any other region, but only so far as
suited the object [had inview. Ofthe twospecies referred to as
absent, D. livida, Tenison-W oods, was published in New South
Wales (1879-80), and D. fragilis, D., I do not know. Does
Mr. Quelch mean D. gracilis, Dana? 1 do not find either
species mentioned in the list of “all the species known,” as
given by Mr. Moseley in the ‘Challenger’ Reports, vol. i.
(1880 and 1881), so that if I have sinned at all I did so in
good company. J did not say D. nitida, Verrill, was of a
whitish tint, but that most of the West-Indian &c. species
were; and this is correct (see ‘ Pourtalés,” &c.). I find,
however, on looking at the original references, I have inad-
vertently transposed the species; but this does not affect the
question in any way.
With regard to D. Brasseyi and D. Allnutti, opinions will
always vary as to the limits and definition of a species ; yet
it wants but a fair examination of the beautiful and accurately
coloured lithographic plates of the two forms (reduced to scale)
and the figure of the life-sized fronds, with a careful reference
to the description of each, to see that two species, let them be
called as they may, are sufficiently indicated. Prof. Verrill
gives no figures, and in a critical examination of a group of
organisms more or less closely allied a simple diagnosis
does not always suffice. If it did, having Verrill’s and
‘Tenison-Wood’s descriptions (and a figure of the latter) of
their respective species to direct him, why has Mr. Quelch
appended a query (?) to the names of the examples assigned
by him to these species in the cases under his charge in the
British Museum? Having compared the above as now exhi-
bited with the species described by myself, I see no reason to
reverse my opinion as to their distinctness. Had I seen Mr.
Tenison-Wood’s paper and figure earlier I might have hesi-
tated before describing D. Al/nutti as a new species; but as
Bibliographical Notice. 219
it is, in the absence of authentic examples, and there being
some features in which the descriptions of the two species do
not quite harmonize, I feel justified in retaining my opinion
as to their difference. D. nit¢éda of Verrill, as judged by the
Museum examples, it certainly is not. The latter is probably
the same as the unnamed fragments I mentioned in my paper
as being in the Museum collection. I have not as yet seen a
second example of D. Brasseyi; but in Lady Brassey’s col-
lection are several specimens of D. Allnutt’, some fronds
being very large, much more so than is given by Mr. Tenison-
Woods.
I am, Gentlemen,
Yours obediently,
204 Regent Street, W. Bryce WRIGHT.
Feb. 18, 1884.
BIBLIOGRAPHICAL NOTICE.
fatalogue of the Fossil Sponges in the Geological Department of the
British Museum (Natural History); with Descriptions of new and
little-known Species. By Guorer Jennrnes Hrypz, Ph.D., F.G.S.
4to. London: printed by order of the Trustees. 1883.
Terex is certainly no group of organisms that has presented so
many difficulties to naturalists as the Sponges. The very kingdom
of nature to which they belonged was long a matter of dispute;
indeed, not much more than thirty years ago so good a naturalist as
Carl Vogt, after briefly discussing their peculiarities, decided that
they were at least quite as much plants as animals, and showed that
he thought they were less animals than plants by leaving them out
of his ‘ Zoologische Briefe.’ Even since their recognition as members
of the animal series they have been subjected to vicissitudes such as
have fallen to the lot of no other group: after passing for a time
as undoubted Protozoa, they were raised by Leuckart and Hiickel
on embryological grounds to the rank of Metazoa, and finally ranked
by Saville Kent as Flagellate Infusoria, while Balfour was inclined
to regard them as forming a group in some respects intermediate
between Protozoa and Metazoa.
With organisms as to the absolute nature of which such divergent
t\ opinions prevailed, with such complete uncertainty with regard even
\
\to what constitutes the individual ‘“ persona,” it is no great matter of
wonder that the views of zoologists upon their classification and as
\ were irreconcilably diverse, and that for many years spongologists
y were occupied chiefly with investigations which could only be re-
Yt, 15*
\
\\
)
‘ the characters which ought to be employed to distinguish them
220 Bibliographical Notice.
garded as tentative. Gradually, however, some order began to be
evolved out of the chaos. Bowerbank, Gray, and Carter in this
country, Oscar Schmidt and others in Germany, proposed systems of
classification, in which, although they could not be maintained in
their entirety, certain well-marked groups were indicated ; and the
recognition of these, coupled with the great mass of information
accumulated by these authors, paved the way towards an intelligible
systematic treatment of the class of Sponges.
If there was all this difficulty in dealing with the recent forms,
it is not surprising that the fossil sponges were treated after a very
conventional fashion. The characters derived from the constitution
of the skeleton, upon which it was shown more and more that we
must chiefly rely in determining the nature and affinities of these
organisms, were often lost or rendered exceedingly difficult of recog-
nition by the process of fossilization, and paleontologists until quite
recently founded their genera and species almost wholly upon the
general form and other surface-characters of the fossils. By this
means in some instances allied forms were roughly brought together
in a manner which might suffice for stratigraphical purposes ; but
in ali other respects our knowledge of the fossil sponges was most
unsatisfactory. A few species and genera had been described by
various authors with reference to their skeletal and other structural
characters, but no respectable attempt to construct a classification
of fossil sponges was made until the publication of Prof. Zittel’s
admirable ‘* Studien iiber fossile Spongien” in the Memoirs of the
Bavarian Academy for 1877 and 1878. That author having taken
up the study of the fossil sponges as far as possible on the same
principles as are applied to the recent forms, with a view to the
preparation of his ‘ Handbuch der Paliiontologie,’ a portion of which
has made its appearance, was led to the establishment of a remarkably
broad and simple classification, which at once took its place as the
certain foundation for all future work in this department of palzeon-
tology.
Some three years ago Dr. G. J. Hinde was applied to by the
Keeper of the Geological Department of the British Museum to
undertake the preparation of a Catalogue of the Fossil Sponges in
the national collection. Already well known as a careful worker
in several branches of what Ehrenberg denominated ‘ Micro-
geology,” Dr. Hinde had been attracted to Munich by the publication
of Prof. Zittel’s memoirs above referred to, and had remained at
Munich for a considerable time, availing himself of the instructions
of Prof. Zittel and of the magnificent series of preparations of
sponges, recent and fossil, which that gentleman had collected during ©
the progress of his own researches. Dr. Hinde’s qualifications for
the task offered to him, both natural and acquired, were therefore of the
highest order ; and we are not surprised to learn that under these
circumstances the original rather scanty design was in course of '
time expanded into the much more satisfactory form of which the
present volume is the result. The first idea was that of arranging
the fossil sponges in the Museum systematically, “ and preparing a
=
ee
Bibliographical Notice. 221
simple catalogue of their specific names and references ;” but
examination of the collection soon showed that ‘‘ numerous speci-
mens, more particularly those from British strata, were either quite
new to science or had been described and figured in such an imper-
fect manner that their real characters were unknown.” Accordingly
“with the consent of the Trustees, it was decided to enlarge the
plan and embrace in the Catalogue condensed descriptions of all the
species from British strata and of the now species from foreign
localities, with figures of all the new forms as well as of those
which had been either inadequately figured previously, or of which
it was desirable to illustrate the minute structure.” Looking at the
result, we think that all parties are to be congratulated upon the
course that was pursued in this ease,—the Trustees for the enlight-
ened liberality which led them to accede to the increased expenditure
required, the Keeper of the Geological Department for the valuable
work done in the collection under his charge, and the credit attach-
ing to his department through the production of a most valuable
contribution to paleontological literature, and the author upon the
satisfactory conclu-ion of his three years’ labour and the magnificent
style in which his work has been brought out. Nor must we omit
to congratulate the working paleontologist upon the acquisition of
such a valuable help to the study of perhaps the most difficult group
of fossil organisms.
In his treatment of the systematic part of his work, the catalogue
proper, the author, as might be expected, follows implicitly the
classification of Prof. Zittel, which, as he says, is “the only one, in
fact, which is at all applicable.” The sponges are referred to the
same orders and the same families, and for the most part to the same
genera, as by Zittel; but, especially among the British forms, the
author has met with many which he was unable to place in any
extant genera, and for these new generic groups are proposed.
That he has not exercised this power of genus-making recklessly,
however, is shown by the fact that out of 139 genera cited only 18
are characterized as new, a degree of reticence which is truly praise-
worthy in an author who has had through his hands a mass of speci-
mens referred to over 400 species of organisms so obscure and
difficult of investigation that few will have the courage or even the
opportunity of criticizing his work. To save space the genera of
former writers are not characterized, except in those few cases in
| which Dr. Hinde has departed more or less from Prof. Zittel’s
views, so that, so far as the characters of the genera are concerned,
the student will have to supplement this catalogue with Zittel’s
‘Studien’ (a translation of which appeared in this journal at the
time of their appearance *), or with the abridgment of that work in
the ‘ Neues Jahrbuch,’ reprinted and issued separately in 1879 under
the title of ‘ Beitriige zur Systematik der fossilen Spongien.’ It is,
we think, to be regretted that the short characters of orders, sub-
orders, families, and genera contained in the last-mentioned work
were not translated or abridged and given under the respective
* Ser. 4, vol. xx., and ser. 5, vols, iil. and iil. (1877-79),
a,
222 Bibhographical Notice.
groups; twenty more pages would have sufficed for this, and the
usefulness of the book to students would have been immensely in-
creased.
Out of the 248 pages of which this volume is composed, the actual
catalogue of species, including the descriptions, occupies 193; the
remainder is devoted to a brief introductory chapter, a tabular and
a stratigraphiecal list of species, a bibliography, and a copious index.
The introduction treats very briefly of a few general matters con-
nected with fossil sponges and their mode of occurrence, and deals
especially with those curious phenomena of fossilization involving
the replacement of silica by carbonate of lime and vice versd, about
which there has been considerable discussion of late years. This
introductory portion concludes with a few remarks upon the geolo-
gical distribution of sponges, and on the classification of the fossil
forms, with a classified list of the orders, families, and genera re-
ferred to in the body of the work. The tabular list of species, in
which those occurring in Britain are specially indicated by an
appended asterisk, shows in vertical columns the distribution of the
species in the broader divisions of geological time ; while the strati-
graphical list displays the same series of facts arranged from a geo-
logical point of view. This latter list brings into promimence a
remarkable point, namely, that the earliest sponges of all, the
Cambrian Protospongia fenestrata and the three species recorded
from Dr. Hicks’s Ordovian strata, all belong to the Hexactinellidee,
which have commonly been regarded as the most complex of sponges.
Further it would appear that while the Cretaceous deposits swarm
with the remains of these organisms, they are represented far more
scantily in the Tertiary deposits. The British Museum collection
possesses only some forms of Cliona from the Tertiaries.
We trust that it will be very clearly seen from this short notice
that Dr. Hinde, in this Catalogue, has furnished his confréres with
a most valuable treatise ; in fact, with this work and those of Prof.
Zittel already referred to, the Sponges, from a literary point of
view, may be regarded as perhaps the most favoured group of fossil
organisms. But we have yet to say a few words about the plates
with which the volume is illustrated, as these contribute in no small
degree to its usefulness and importance. There are no fewer than
thirty-eight of these plates, and they are for the most part beauti-
fully executed, showing in a most characteristic fashion the external
appearance of the fossils, with many of which one is tolerably
familiar, and also the spicular and other structural characters known
chiefly to students of the group. ‘These illustrations, which by their
beauty and number admirably illustrate the text and help to render |
this the finest paleeontological treatise that has issued from the {
English press for many years, reflect the highest credit upon the
artists concerned in their production—a credit, however, which they |
must be content to share with the author, as in such a case as this
we may be pretty sure that without the most careful superinter
dence on his part, such excellent results as we here meet with cout °
not have been attained. ¥
Miscellaneous. 223
MISCELLANEOUS.
Preliminary Report on the Expedition of the ‘Talisman’ in the
Atlantic Ocean. By M. A. Mitye-Epwarps.
At the public meeting of the five Academies on the 25th October,
1882, I had the honour of giving an account of the explorations of
the ‘ Travailleur,’ and I announced that this year a new scientific
campaign would take place in the Atlantic. In fact, the Minister
of Marine, in reply to a desire expressed by his colleague the Minister
of Public Instruction and by the Academy, had given the necessary
orders that a despatch-ship, the ‘ Talisman,’ should be fitted out for
that purpose.
The ‘Talisman’ is an excellent screw-steamer, provided with
powerful sails, sufficient without the help of its machinery to give
it a rapid motion. During several months, in the dockyards of the
arsenal at Rochefort, it was placed in the hands of the Marine en-
gineers, who undertook to adapt it to the service which it was to
fulfil. The old hempen ropes intended to raise the dredges were
replaced by a steel cable of extreme firmness and flexibility, able to
support, without breaking, a weight of nearly 4500 kilogrammes,
and presented to the Admiralty by the Minister of Public Instruction*.
Two steam-engines secured its action: one of them set in motion
the enormous reel on which it was coiled; the other, which was
more powerful, drew up the dredging-apparatus. Some large nets
or trawls of 2 or 3 metres across the mouth replaced with advan-
tage the heavy dredge which we formerly employed. ‘The soundings
were made by means of an apparatus perfected by M. Thibandier,
marine engineer, and arranged in such a manner that the move-
ments of the vessel should have no influence on the tension of the
steel rope ; an automatic brake arrested the unwinding directly the
sounding-apparatus touched the bottom. In order to measure the
temperatures of the deep strata of the water I had caused to be
constructed an apparatus enabling a thermometerwith a broken
column of mercury to turn over at a given moment. The same
movement caused the breakage of the capillary extremity of glass
tubes in which a vacuum had been produced, and into which the
sea-water then rushed, furnishing samples of perfect purity, which
could be indefinitely preserved after hermetically sealing the tubes.
Our confrére, Colonel Perrier, was kind enough to lend me a
Gramme machine, which furnished electricity to some Edison lamps,
so placed as to illumine our apparatus, or, at need, to descend into
the sea to a depth not exceeding 35 metres. At my request the
command of the vessel was confided to Captain Parfait, who, the
preceding year, occupied the same post on board the ‘ Travailleur’f.
* The weight of a metre was 344 grammes, and the price about 0 fr. 62.
+ The staff was composed of M. Antoine and M. Jacquet, lieutenants,
of MM. Gibory and Bourget, ensigns, of M. Vincent, doctor, and M. Huas,
assistant doctor, and of M. Plas, purser.
224 ‘Miscellaneous.
I may here be permitted to express to the officers of the ‘ Talisman ’
all the gratitude with which their courtesy has inspired us. They
interested themselves in our work with an ardour which never
flagged, and if we have completely succeeded in our mission it is to
them that we owe our success.
On the 30th of May the scientific commission met at Rochefort *,
and on June Ist the ‘ Talisman’ quitted port.
The expedition of 1883 may be subdivided into several distinct
sections :—we had in the first place as our object to study the coast
of Africa as far as the Senegal; then to explore the neighbourhood
of the Cape-Verd Islands, the Canaries, and the Azores, volcanic
lands which could not fail to furnish us with some interesting facts ;
lastly, we hoped to pay some attention to:the Sargasso Sea, from the
point of view of its fauna and the nature of its bed.
The depths which extend to the west of Morocco and the Sahara
are of yery great regularity ; one no longer finds there that dis-
turbed relief which, on the coasts of Spain, had rendered our opera-
tions so difficult. On the contrary, the slope is gradual, and by
travelling further from or nearer to the land one can find, almost
certainly, the depth that one expected. On these bottoms we
used the dredge about 120 times, and at the end of some days we
knew the bathymetric distribution of the animals of this region well
enough to be able to indicate from the contents of our nets what
had been the depth explored.
At 500 or 600 metres live numerous fishes, such as Macrurus,
Malacocephalus, Hoplostethus, and Pleuronectes, as well as some
shrimps of the genus Pandalus and of a new species with a rostrum
pointed like a sword, species of Peneus and Pasiphaé, some small
crabs (Oxyrhynchi, Portunidee, and Ebalids), some rose-coloured
Holothurians, some rare specimens of Calveria, that soft sea-urchin
discovered in our seas by the naturalists of the ‘ Porcupine,’ and
known previously in the fossil state, and many sponges of great
size, such as Askonema and Lurrea.
At a greater depth, about 1000 or 1500 metres, fishes abound f.
Often they constituted the greater part of our booty. Their colours
are, in general, dull, their flesh is gelatinous, their skin is indued
with a thick coat of mucus; many bear phosphorescent plates,
intended to light them in the darkness where they live.
The Pandali have given place to the new genus Heterocarpus,
Peneide in which the last two pairs of legs are long and articulated
like antenne ; and to enormous shrimps of a blood-red colour and
* The commission was composed of M. A. Milne-Edwards, of the
Institute, president, of MM. de Folin, Vaillant, Perrier, Marion, Filhol,
and Fischer, to whom had been added, as assistants, MM. Brongniart and
Poirault. Detained at the last moment by his university duties, M.
Marion was unable to embark.
+ There are still Macruri, to which are to be added the following
genera :—Bathynectes, Coryphenotdes, Malacocephalus, Bathygadus, Argy-
ropelecus, Chauhodus, Bathypterois, Stomias, Malacosteus, Alepocephalus.
ee
Miscellaneous. 225.
with excessively long antennz, which were not known, and which
ought to be placed in the genus Aristeus. Nephropses appear at
this level ; these are blind Crustaceans, of a coral-colour ; their geo-
graphical distribution seems to be very extended, for they have been
found on the other side of the Atlantic, in the Caribbean Sea, and a
very nearly allied species has been taken at a great depth in the neigh-
bourhood of the Andaman Islands. The blind Polycheles, which
replace in existing nature the Jurassic Hryons, hide themselves in
the mud, and only allow their long hooked claws, destined to seize
their prey in passing, to protrude.
Some other crabs oceur ; some Maiide (Scyramathia, Lispognathus);
Homolides of a new species; and some species of Lithodes, a genus
which was thought to be peculiar to the northern and southern
seas, Numerous species of the group of the Galatheidw were ob-
served, of which several have the eyes transformed into spines. The
sponges are extremely common ; the greater number havea siliceous
skeleton. We have taken a profusion of Rosselle and Holtenice of
several species, of which the fibres, like snow-white crystal, are
buried in the mud, while the sponge alone emerges; and some
Aphrocalliste, of which the solid framework assumes the most ele-
gant forms. The Calverie become more numerous; Holothurians
(Letmogone and others) crawl on the ground in the midst of Aste-
rians, Ophiurans, and Brisinge. Our nets often came up charged
with such riches that the day did not suffice to classify them.
Passing Cape Ghir and Cape Nun, at about 120 miles from the coast,
the ‘ Talisman,’ during several days, explored a very regular bank, of
which the depth is about 2000-2300 metres. It was upon this
same bank that, on August 2, 188%, the ‘ Travailleur’ captured the
singular fish described by M. Vaillant under the name of Eury-
pharynx pelecanoides, and of which two examples have been taken
this year. Our dredgings were once more of great value. Superb
sponges, allied to those which have been described under the name
of Huplectella suberea, occurred, mixed with great violet Holothu-
rians of the genus Benthodytes and with other species of the same
kind, remarkable for their dorsal appendages. A Calveria distinct
from those of lesser depths, Brisinge, corals of rare beauty (/label-
lum, Stephanotrochus), a Democrinus, and a Bathycrinus not yet
described, very numerous Crustaceans, nearly all new to us and
belonging to the group of Galatheidee (Galathodes, Galcantha, Elas-
monvtus), completed the invertebrate fauna. The fishes were very
varied, and their study will furnish new facts of the greatest in-
terest. Amongst the most remarkable I will mention Melanocetus
Johnsoni, some Bathytroclites, a Stomias with phosphorescent plates,
and several Malacostet.
Between the Senegal and the Cape-Verd Islands our nets at-
tained a depth of 3200 and 3€55 metres, and brought up the greater
part of the preceding species as well as many others (crustaceans,
mollusks, zoophytes, sponges) which had not been met with else-
where.
These last dredgings terminated the first part of our expedition,
226 Miscellaneous.
and on the 20th July, after fifty-one days’ sailing, we cast anchor
in the Bay of Praia, at Santiago, in the Cape-Verd Islands.
These volcanic islands detained us some days, and while zoclogical,
botanical, and geological excursions were made on land, the ‘ Talis-
man’ investigated the irregular littoral regions in search of marine
animals, and, in particular, the red coral which has been for some
years the object of an active commerce on these shores. I shall
not dwell upon these littoral researches any more than upon the
exploration of the islet of Branco, where we studied, in their home,
the great lizards (Macroscincus Coctec), which seem to be confined
to this isolated rock. All these details find their place in the report
which I have addressed to the Ministry, and of which the publi-
cation will take place shortly.
In the depths of these seas off Cape Verd, life has an astonishing
vigour. Our nets came up filled to the brim; at one cast we have
taken more than 1000 fishes, belonging for the most part to the
genus Melanocephalus, more than 1000 Pandali, 500 shrimps of a
new species with enormously long legs (Nematocarcinus), as well
as many other species.
On the 30th July, the ‘ Talisman’ started to the north-west and
sailed towards the Sargasso Sea. I will not enlarge upon this part
of our journey; it will be sufficient for me to say that in no part
have we met with those floating meadows of which the older navi-
gators speak. The Sargassos appeared in isolated bundles floating,
in definitely oriented lines, in the direction of the winds or of the
currents, and sheltering a whole pelagic population of which the
colours harmonized admirably with those of the seaweeds which
serve them as a refuge; the naturalists on board made a careful
study of them.
The soundings of the ‘ Talisman’ in this part of the Atlantic
show in a general way that, starting from the Cape-Verd Islands,
the bottom deepens regularly to about the 25th parallel, where it
reaches 6267 metres, then it gradually rises again towards the
Azores, and under the 35th parallel it is no longer more than 3000
metres. These results are far from agreeing with the curves
indicated on the most recent bathymetric charts. The bed of the
Sargasso Sea seems to be formed of a thick layer of very fine mud
of a pumiceous nature, containing fragments of pumice-stone and of
volcanic rocks.
It seems that there may be here, at more than a league below
the surface of the water, an immense voleanic chain parallel to the
coast of Africa, and of which the Cape-Verd Islands, the Canaries,
Madeira, and the Azores would be the only emergent points.
The submarine fauna is poor; it is composed of a few fishes, of
some Crustaceans, such as Paguri, lodged in colonies of Epizoanthi,
shrimps of the genus Nematocarcinus, and species of Pasiphaé, and
of a few Mollusca (Fusus, Plewrotoma, and Leda), which scarcely
sufficed to compensate us for the time which dredgings so deep as
these occupied.
It was not until about the northern limit of the Sargasso Sea,
Miscellaneous. 227
where the bottom is raised to 3000, 2500, and 1500 metres, that our
captures again became abundant ; it was here that we took the giant
of the family of the Schizopodes, a Gnathophausia of a blood-red
colour, measuring almost 0-25 metre in length. <A short stay of
the ‘Talisman’ at Fayal and afterwards at St. Michael, in the
Azores, enabled us to compare the still active volcanic phenomena
with those which we had just studied at the summit of the Peak of
Teneriffe.
The analogy of the rocks, of the gaseous products, and of the de-
posits of sulphur is striking, and, from what takes place at the
surface of the ground, one can form an idea of the submarine con-
vulsions which have covered the bed of the Sargasso Sea with pumice
and igneous rocks.
Our voyage from the Azores to France was made under excellent
conditions, and every day a dredging was made at depths of from 4000
to 5000 metres. These difficult operations, very skilfully conducted
by Captain Parfait, brought to us harvests of extreme importance.
Under this crushing pressure, in a dark medium and without
traces of vegetation, the animals are numerous and of a very perfect
organization.
Great fishes of the genus Macrurus, as well as Scopeli and Melano-
ceti, seem not to be rarethere. Some Hermit Crabs and Galatheide
of anew form, a gigantic Nymphonid of the genus Colossendeis, some
unknown Lthene, some Amphipodes, and some Cirripedes represent
the Crustaceans. But this abyssal fauna owes its physiognomy
especially to the number, variety, and size of the Holétiutinns
which dwell there.
The sea-bottom is carpeted in all that region with a thick white
mud, almost entirely formed of Globigerine, and covering pumice and
fragments of rocks of different natures, of which some bear the im-
pressions of fossils, and, among others, of Trilobites ; but what
surprised us most was to find, at a distance of more than 700 miles
from the coast of Europe, pebbles polished and striated by ice
The distinctness of these strix does not allow us to suppose that they
were transported by currents. The presence of these pebbles is
probably due to the action of floating masses of ice which, at the
quaternary epoch, advanced further towards the south iliah at the
present day, and which, melting in that part of the Atlantie com-
prised between the Azores and France, let fall on the bottom
stones which they had previously carried along torn from the bed
of the glaciers.
On the 30th August we dragged our nets for the last time on
the rapid declivity which unites the abysses of the ocean with the
depths of the Bay of Biscay, and our captures added to the fauna of
the French seas a great number of new or interesting species. It
was time to return to Rochefort: our casks and jars were full
our alcohol was exhausted. This expedition has furnished us with
incomparable materials for study; it remains now to set to work
upon them. The Minister of Public Instruction recognizes the im-
portance of this, and he has been kind enough to furnish mo with
228 Miscellaneous.
the means of commencing the publication of the results. Finally I
intend to place before the public in a special exhibition, which will
take place at the Museum about the end of the month, the collec-
tions gathered during the expeditions of the ‘Travailleur’ and the
‘Talisman.’—Comptes Rendus, December 17, 1883, p. 389.
New Aphidological Discoveries. By M. Licurensrer.
Thanks to the assistance of several foreign entomologists, among
whom M. Howath of Budapest and M. Kessler of Cassel occupy
the first place, I have been able to ascertain absolutely the fact of
the migration of the Aphides of the elm to the roots of grasses, and
their return to the trunks of the trees in autumn.
Tetraneura ulmi of authors, the commonest of the Aphides of the
elm, upon the leaves of which it forms little smooth, green galls the
size of a large pea or a hazel-nut, lives, during its subterranean
budding phase, on the roots of maize in Austria and Hungary, and
here on the roots of the dog’s-tooth grass (Cynodon dactylon). Pas-
serini and many others had made of this subterranean Aphis a dis-
tinct species under the name of Pemphigus Boyeri, Pass.,=radicum,
Boyer, = Zee maidis, Low & Duf., &c. &c. As there are very pro-
bably many species which live upon the roots of plants in summer
(in my own opinion nearly all the gallicolous species have their
corresponding subterranean form), the characters of these insects
vary much according to authors; but the Tetrancura ulmi seems to
me to be very well characterized and easily recognized by the fifth
joint of the antenne being as long as the third.
I have conveyed winged insects taken from the roots of the dog’s-
tooth grass upon a strip of brown paper, fixed round a young smooth-
barked elm, with the view of giving them an artificial shelter be-
tween the paper and the bark. They did not attempt to fly away ;
on the contrary, they set to work at once to deposit sexual pupe,
which soon opened and furnished males and females, destitute of
rostra, as in most Pemphigine. What is more, the next day all
the winged Aphides of the roots in the neighbourhood seemed to
have appointed to meet on my strip of paper, which swarmed with
insects, drawn together probably by the inexplicable instinct of the
lowest forms of animals. :
At the same time I was able to ascertain the arrival upon the
same tree of a second species, Tetraneura rubra, Licht., which
forms small red, curled, and villous galls upon the leaves. After
pulling up some hundreds of different plants I also found the sub-
terranean habitat of this species; it is the Panicum sanguinale. In
this species the apterous form is reddish, while it is quite white in
Tetraneura ulmi. The winged forms have the fifth joint of the
antenn shorter than the third.
I still (10th December) find wingless Aphides alive upon the
roots, which would prove that, as in the Phyllowera, side by side
with the winged pupiferous form which gives origin to the sexual re-
producers, there is, parallel with this reproduction, an uninterrupted
sequence of subterranean agamic reproduction, so that, should any
Miscellaneous. 229
circumstance happen to destroy the winter-egg, there is always a
subterranean provision of reproduction ready to replace the sexual
generation which has not prospered.
Moreover, in the case before us, the winter-egg, that is to say the
fecundated egg of the Tetraneura, besides being well sunk into the
fissures of the bark, is further protected by the dried skin of the
mother, for she does not expel it, but keeps it encysted within her,
as do the Aphides of the galls of the Lentiscus observed by Prof.
Derbes. Thus protected the egg braves the attacks of mites, Heme-
robil, Thrips, and other small enemies.
In indicating the two species of grasses upon which I have found
the subterranean forms of Tetranewra, I do not wish to imply that
they do not attack others; on the contrary, I know very well that
Passerini, for example, cites eleven species of grasses upon which he
has found his Pemphiqus Boyeri, which now becomes synonymous
with Tetrancura ulmi; and as the latter is everywhere very com-
mon, it is very probable that in countries where maize or the dog’s-
tooth grass are wanting, it contrives to find other grasses to its
taste. I believe this species is polyphagous.
But if it is polyphagous in its subterranean phase, it appears to
be very faithful to the elm and even to Ulmus campestris in forming
its gall. In fact I have, side by side with Ulmus campestris, two
or three plants of Ulmus effusa, a tree very nearly allied to the
former species, which the botanists can hardly distinguish except
by the form of the flowers. Now at this present moment the elms
have neither leaves nor flowers, and I put the same strip of paper
upon Ulmus effusa as upon Ulmus campestris; nevertheless the
insect makes no mistake, and I never find a Tetraneura upon the
Ulmus effusa. On the other hand there is upon the latter tree a
peculiar gall of a species of Aphis very nearly allied to Vetraneura,
namely Schizonewra compressa, Koch. This arrives in numbers upon
the species of elm that it prefers. I do not yet know whence it
comes. Here, therefore, we have Aphides which, cleverer than the
botanists, can recognize in the winter trees which the naturalist can
only distinguish in summer by their flowers and fruits. Of course
I make no attempt to explain such phenomena as these; I do not set
up hypotheses, and confine myself to indicating exact facts, which I
observe with the greatest possible attention. The problem of the
biological evolution of the Aphides of the elm was enunciated more
than a century ago; it is now solved.—Comptes Ltendus, December
31, 1883, p. 1572.
Note on two New California Spiders and their Nests.
The Rey. Dr. McCook presented a small collection of spiders re-
ceived from Mr. W. G. Wright, San Bernardino, Cal., mailed
November 18. One of these came within a nest, and is a Saltigrade
spider, probably an <Attus. The nest is a rare one, and was so
happily placed, by the builder, on a branch of sagebrush (Ephedra
antisyphilitica) that it was preserved intact. It is the only one
230 Miscellaneous.
which Mr. Wright had seen in site. Another nest, which he had no
doubt was the same, he had observed torn from its place by some
bird, as material for the construction of a bird’s-nest.
Nests somewhat similar are habitually made by Pennsylvania
Saltigrades upon or among leaves, which shrink up as they die and
tear the spinning-work so as to destroy the specimen. The one
exhibited was in perfect condition. It is the tent and egg-nest of
the species which was alive within it, and the speaker thought to
be new. It is a large example, five-eighths inch in body-length,
stout, the legs of moderate thickness, the whole animal covered
closely with greyish-white hairs, the skin beneath being black.
Dr. McCook named the species, provisionally, Attus opifea, with a
double reference to the discoverer (Mr. Wright) and the admirable
housewright qualities of the aranead herself. The nest is externally
an ege-shaped mass of white spinning-work, three inches long by
two and one-half inches wide. ‘The outer part consists of a mass
of fine silken lines crossing in all directions and lashed to the twigs
within which it is enclosed. ‘This maze surrounds a sac or cell of
thickly-woven sheeted silk, irregularly oval in shape, two inches long
by one inch wide, and also attached to the surrounding twigs. At
the bottom this cell or tent is pierced by a circular opening, which
serves the spider as the door of her domicile. It is the habit of her
genus to live and hibernate within such a silken nest. Against one
side of the tent within is spun a lenticular cocoon (double convex)
of thick white silk, within which the eggs were placed. The young
spiders when received had escaped from the cocoon, and occupied
the package-box. They are about one-eighth inch long, resembling
the mother, but less heavily coated with grey.
This collection also contained three specimens (?) of the genus
Pucetia, as defined by Thorell*. This genus belongs to the family
Oxyopide of the Citigrade spiders, to which it is doubtless properly
relegated in spite of certain analogies with the Attoide (Saltigrades)
on the one hand, and the Philodromine (Laterigrades) on the other.
Mr. Wright calls them “jumping spiders.” Hentz, who describes
several species of Owyopes, says that O. salticus leaps with more
force and vivacity than an Attust. Of O. viridans he thinks it
possible that the mother carries its young like Lycosa, This family
of spiders is arboreal in habit, is found on plants, with their legs
extended, thus disguising themselves after the manner known as
“‘ mimicry,” and springing upon their prey. The cocoon is usually
conical, surrounded with points, placed in a tent made between
leaves drawn together and lashed, and is sometimes of a pale greenish
colour. 0. viridans will make a cocoon suspended in mid-air by
threads attached to the external prominences, which she will watch
constantly from a neighbouring site. Dr. McCook believed the
species presented to be new; the body-length is fourteen milli-
metres; legs long, tapering, with many long spines. The body is
yellow and pale yellow ; the cephalothorax striped longitudinally with
* See “ On European Spiders,’ Nova Acta Reg. Soci. Sci. Upsalensis,
3rd ser. vol. vi. p. 196.
+ ‘Spiders of the United States,’ p. 48.
Miscellaneous. 231
bright red streaks; the abdomen marked above with red bell-
shaped and angular patterns, and beneath with red streaks ; the
sternum red, the legs yellow with réd rings at the joints. The
species was named Pucetia aurora, because of the bright red streaks
upon the yellow background, suggesting “the daughter of the
dawn.”
According to some field-notes forwarded by Mr. Wright since
the above was in print, Pucetia aurora is rather abundant in a
limited locality. The nests are uniformly upon bushes of Hrio-
gonum corymbosum, and several specimens of them were sent. The
nest is hung from three to four feet from the ground, and, being
upon the topmost twigs, is easily seen from a distance. The cocoon
is a straw-coloured sphere or ovoid, five-eighths of an inch in diameter.
It is covered externally with various pointed rugosities, from which
numerous lines extend to the adjoining foliage, and into the maze of
right lines which extends below the corymb of the plant upon which
all the specimens sent are attached. ‘This retitelarian snare doubt-
less serves as a temporary home for the young spiders. The cocoon
has no suture, the spiderlings escaping by cutting the case, which is
thick and closely woven. No floss padding was found inside of the
case.
Upon approaching the nest, the mother is usually seen hovering
over the young spiders, or guarding a new sack of eggs. She lays
two and sometimes three broods on one twig. Sometimes the young
ones will be still in the old nest, while the mother is guarding a
new bundle of eggs immediately adjoining the old one. In no case
were any young ones seen on the mother’s back. The mother stays
close by her nest. If the spiderlings be hatched, she will, perhaps,
drop down a foot or so, if a first effort to capture her be not successful ;
but will not drop to the ground, unless forced todo so. If guarding
her eggs, she must be forcibly separated from the cocoon. The
young ones take alarm sooner than their mother; they drop down
a few inches—or, at times, two feet—every one on its tiny thread,
forming a pretty, swaying fringe. In a few moments, if all is still,
they climb up again; but if frightened, will drop to the ground
and run. The little ones in such case do not jump.
It is a further interesting fact in so-called “ mimicry” that of
several examples of P. aurora seen by Mr. Wright, one found on
a green bush was in colour almost wholly green, with scarcely a
trace of red; while two found on a hoary-white bush had simulated
the white colour of their habitat. The specimens, as described
above by Dr. McCook, approach in coloration the prevailing hue
of the Hriogonum on which they were nested, and he was inclined to
think that this is the normal colour of the adult, which is taken on as
the animal matures; indeed, as the green and whitish specimens
were not sent to him, he would be inclined to think (awaiting further
evidence) that those colours may have been due to immature age.
At least the tendency to such colours is strong in young spiders.
However, the fact of mimicry is not improbable, as Dr. McCook
had observed it in our native Laterigrades.
From the same gentleman and locality, Dr. McCook had received
IZ, Miscellaneous.
a specimen of Argiope fasccata, which is thus located upon the
Pacific coast, giving this beautiful and interesting spider a conti-
nental distribution.—Proc. Acad, Nat. Sci. Philad. 1883, Noy. 27,
p. 276.
On an Aerial Alga inhabiting the Bark of the Vine.
By M. J. B. Scunerztzr.
In the month of April of the present year (1883) there was
observed upon numerous vines between Pully and Belmont (Canton
de Vaud) a pulverulent matter of a brownish-red colour, which
penetrated into the fissures of the periderm. This pulverulent
matter is formed by an aerial alga, Chroolepus umbrinum, Ktz., or
Trentepohlia umbrina (Kg.), Born., which is met with upon the
bark of various trees, but has not hitherto been mentioned upon that
of the vine. This alga contains a very refractive red oil, which
diffuses a faint odour of violets; it does not appear to injure the
vine, upon which occurs a complete cryptogamic vegetation formed
by species of Oscillaria, Nostoc, and Pleurococcus, Confervee, Mosses,
and Lichens (Physcia ciliaris, Pyrenula, &c.). Chroolepus umbrinum
is composed of small spherical cells of about 30 y, forming small
curved chains.
When the bark of the vine reddened by Chroolepus umbrinum is
moistened with water, this same alga is seen very distinctly in the
thallus of one of the lichens of the genus Pyrenula. It must be re-
marked, however, that the cells of the alga which occur in the
thallus are smaller than those which exist in the air; they form in
it very distinct little chains. We observe, moreover, all the transi-
tions between the cells which exist out of the thallus and those which
occur more or less deeply buried in it. Around the chaplets and
free cells of the Chroolepus we sometimes find the filaments of the
mycelium of a fungus, which surround them and bind them into
small colonies.
The cells of Chroolepus umbrinum, which occur either in the free
state or immersed in the thallus of Pyrenula, often present a green
coloration. One can find all the transitions between entirely red
cells and others partially or entirely green. This green coloration
is met with especially when vine-bark reddened by the free Chroo-
lepus is plunged into water. In this latter case we see issuing from
some of these cells, which are still red, small ovoid bodies which
swim briskly in the water (zoogonidia of Wille *),
In avery interesting memoir by M. A. B. Frank f we find some
observations precisely analogous to the preceding. It results from
them, as we have likewise ascertained, that Chroolepus umbrinum
may lead a completely free and independent existence, while the
same alga occurs with smaller dimensions in the thallus of crusta-
ceous lichens ; but when, in consequence of the disaggregation of this
thallus, the alga is set free, it multiplies and by degrees resumes
its typical form and its normal dimensions.—Bulletin de la Société
Vaudoise des Sciences Naturelles, sér. 2, vol. xix. no. 89, p. 53.
* Just, Bot. Jahresber. 1878, p. 390.
+ “Ueber die biologischen Verhaltnisse des Thallus einiger Krusten-
flechten,” in Just, Bot. Jahresber. 1876, p.70.
THE ANNALS
AND
MAGAZINE OF NATURAL HISTORY.
[FIFTH SERIES.]
No. 76. APRIL 1884.
XXVII.—On the Modern Philosophical Conceptions of Life.
By J. J. Woopwarp, President of the Philosophical
Society of Washington *.
I PROPOSE to invite your attention this evening to some thoughts
on the Modern Philosophical Conceptions of Life. The theme
is so large that it would be idle to attempt its systematic
treatment in the course of a single evening ; nor do [ pretend
to be in possession of any satisfactory solution of this ancient
question, of which I might offer you an abstract or outline,
pending the fuller presentation of my results elsewhere. Yet
I have ventured to hope that a discussion of some of the con-
siderations involved, and a brief statement of certain views
that I have been led to entertain, would not be without in-
terest, and perhaps might prove of actual service, especially
to those of you who are engaged in biological pursuits.
Undoubtedly the conception of life most popular at the
present time is that which assumes all the phenomena of
living beings to be the necessary results of the chemical and
physical forces of the universe, and claims or intimates that
wherever this has not yet been proven to be the case the evi-
rence will hereafter be forthcoming. ‘This doctrine, which
* From the ‘ Bulletin of the Philosophical Society, Washington,’ 1883.
Ann. & Mag. N. Hist. Ser. 5. Vol. xu. 16
234 Mr. J. J. Woodward on the Modern
may conveniently be designated the chemico-physical hypo-
thesis of life, has readily found its way from the speculative
writings of philosophers to the rostrums of some of our teachers
of chemistry and physics, who boldly declare, in their class-
lectures and public addresses, that the forces at work in the
inorganic world are fully adequate to explain all the pheno-
mena of living beings, and prophesy that the time is soon
coming “when the last vestige of the vital principle as an
independent entity shall disappear from the terminology of
science’ =.
Now most of these gentlemen are not embarrassed by any
very definite or detailed knowledge of the physiological and
pathological phenomena which a tenable theory of lite must
be competent to explain, while they do know, or at least
ought to know, a great deal of chemistry and physics; the
confidence with which they maintain their creed is therefore
readily understood. Much more surprising is it to find the
same doctrine embraced by numerous zoologists, physiolo-
gists, nay, even pathologists, among them men who cannot
for a moment be supposed to be unacquainted with the pheno-
mena to be explained, and of whose abilities and reasoning
powers it is impossible for me to think or speak otherwise
than respectfully. Yet I cannot but believe that they have
adopted the chemico-physical hypothesis, not so much because
they are really satisfied with it as a scientific explanation of *
all the phenomena, as because they are unduly biassed in its
favour by the utterances of the great philosopher who has
done, as [ think we will all agree, such good service to bio-
logical science by elaborating and popularizing the doctrine
of evolution.
It is only natural that such a bias should exist. The dis-
cussion of the nature of life, in the case of man at least, has
always, and not unreasonably, been conjoined with the dis-
cussion of the nature of the soul; and the philosophers who
have won higher repute in the latter discussion have always
been willing enough to offer solutions of the life-problem, and
have never had any difficulty in finding followers even among
those whose special lines of investigation might be supposed
to impose upon them the duty of independent inquiry into the
meaning of life.
Just as it was in the old time with regard to this matter, so
itis now. When Galen undertakes to discuss the complex
* George F. Barker, “Some Modern Aspects of the Life Questicn”
(Address as President of the Amer. Assoc. for the Advancement of
Science, Boston meeting, August 1880; ‘ Proceedings,’ vol. xxix. part i.
p. 23).
Philosophical Conceptions of Life. 235
phenomena of the Psyche, as manifested by the human species,
he openly and continually confesses the extent to which he
relies upon the authority of Plato; and when the dicta of the
master are such as to require a special effort of faith on the
part of the disciple, he honestly exclaims, ‘‘ Plato indeed
appears to be persuaded of this; as for me, whether it be so or
not, I am unable to dispute the question with him” *.
In like manner, did they venture to be as frank as Galen
was, most of the modern biologists who have adopted the
chemico-physical theory of life would, I presume, confess,
“* As to this matter our opinions are derived from Mr. Herbert
Spencer’s ‘ Principles of Biology;’ what are we that we should
venture to dispute as to questions like these with him?”
Nevertheless in striking contrast to this chemico-physical
hypothesis of life, which is to be regarded as the fashionable
faith of the hour, there still survives in many quarters, and
especially among physicians, a disposition to regard indis-
criminately almost all the phenomena of living beings as
peculiar manifestations of a vital principle. So strong, indeed,
is the faith of some of these modern vitalists, that they seem
to shut their eyes to the evidence already in our possession
as to the actual participation of known chemical and physical
forces in the operations going on within living bodies, and
appear almost to resent the willing aid that chemistry and
ea afford to the physiological investigator of the present
ay.
Nay, further than this, in the inevitable reaction that is
beginning to make itself felt against the avowed revival of
the materialism of Epicurus and Lucretius—for we all know
now that the chemico-physical hypothesis of life is not a new
induction of modern science, but an ancient Greek speculation
reappearing in modern petticoats—that other Greek specula-
tion of the threefold Psyche, the doctrine taught by Plato and
Aristotle, and which Galen accepted on their authority, the
doctrine of a vegetable, an animal, and a rational soul, a
human trinity coexisting in every human being, is once more
rehabilitated and finding followers—likely, indeed, as I think,
to obtain more followers than perhaps any of you yet suppose.
And these followers are by no means confined to metaphysi-
cians or churchmen; they can be found also already among
the biologists. It is an English biologist of good repute and
of no mean abilities who takes occasion, in a technical biolo-
gical work published this very year, to express his belief that
* Galen, ‘Quod animi mores corporis temperamenta sequantur,’ cap. 3
(Kiihn’s edit. t. iv. p. 772).
16*
236 Mr. J. J. Woodward on the Modern
the Greek conception of the threefold Psyche ‘ appears to be
justified by the light of the science of our own day” *.
For myself I must confess at once that I am quite unable
to join either of these opposing camps as a partisan. I cannot
accept the more strictly vitalistic views, because I am com-
pelled continually to recognize the operation of purely che-
mical and physical forces in living beings. On the other
hand, there are whole groups of phenomena characteristic of
living beings and peculiar to them of which the chemico-
physical hypothesis offers no intelligible explanation.
From this point of view the various processes and functions
of living beings may indeed be divided into two classes, of
which the first may be regarded with more or less certainty
as the special results, under special conditions, of the very
same forces that operate in the inorganic world; while the
second, to which alone I would apply the term vital, are not
merely in every respect peculiar to living beings, and hitherto
utterly inexplicable by the laws of chemistry and physics, but
are so different in character from the phenomena of the inor-
ganic world, that it does not seem rational to attempt to
explain them by these laws.
Let me refer briefly to the processes and functions belonging
to the first class. Here I place all those more strictly chemical
processes by which, within the very substance of vegetable
protoplasm, inorganic elements are combined into organic
matter, as well as those which produce all the various subse-
quent transformations, whether in plants or animals, of the
organic matter thus prepared. This general conception in-
cludes of course, in the case of the higher animals, all the
chemical phases of the processes of digestion, assimilation,
and tissue-metamorphosis or metabolism, including secretion
and excretion; in the case of the lower animals and plants,
so much of these several functions as belongs to each species.
Now please to understand that when I say I recognize all
the chemical phases of these processes to be the results of the
ordinary chemical laws, I do not entertain any mental reserva-
tion with regard to the unrestricted application of these laws.
I cannot for a moment agree with those physiologists who
have imagined the vital principle to thwart or interfere with
or counteract these laws in any way. I know indeed that we
are far from being as thoroughly acquainted as we may by and
by hope to be with the chemical phenomena of living beings ;
that many of the questions are very difficult, so that as yet,
with all our labour, we have obtained but partial or even con-
tradictory results; but I find in this only a reason for further
* St. George Mivart, ‘The Cat’ (London, 1881), p. 387,
Philosophical Conceptions of Life. 237
investigation—no logical difficulty of a radical kind. In a
general way I recognize that the matter of which living beings
are composed is built up of elementary substances belonging
to the inorganic world, and that it consists of atoms possessed
of the very same properties and obedient to the very same
laws as like atoms in inorganic bodies. Yet 1 confess I find
in all this no reason for denying the existence of a vital prin-
ciple; only I do not figure this principle in my mind as a
hostile power interfering in any way with the chemical ten-
dencies of the atoms present; I liken its operations rather to
those of the chemist in his laboratory who obtains the results
he needs only on the condition of most rigid obedience to
chemical laws.
Intimately associated with some of the chemical processes
just enumerated are those chemical processes of respiration in
which the chemical affinities of the oxygen of the atmosphere
are directly or indirectly the means of promoting tissue meta-
morphosis, as well as of reducing at once to simpler forms
some portion of the various complex substances derived from
the food. These chemical processes are undoubtedly the chief
original sources of the heat and mechanical power manifested
by animals. Of course they receive heat also from without
by conduction and radiation; but this is a small matter to the
heat generated within them ; of course, too, mechanical power
is continually transformed into heat within the body of ani-
mals; but this neither increases nor diminishes the total
amount of energy liberated.
I yield my hearty assent to that modern scientific induc-
tion * which sees in the potential energy of the complex
chemical compounds supplied to animals by their food the
essential source of all the actual energy of the body, whether
manifested in the form of heat or work. In a general way
the reduction of these complex chemical compounds by oxida-
tion into the much simpler ones, urea, carbon dioxide, and
water, is the means by which potential is converted into actual
energy. In the case of plants, too, the source of any little
heat that may be developed under special conditions, and of
such sluggish motions as actually occur, is doubtless to be
found in the reduction to simpler combinations by oxidation
of a part of the organic matter already formed. ‘The chief
function of the vegetable world, however, is to build up, by
means of the solar energy, those complex and unstable
* First taught by J. R. Mayer, ‘Die organische Bewegung in ihrem
Zusammenhange mit dem Stoffwechsel: Kin Beitrag zur Naturkunde '
(Heilbronn, 1845).
238 Mr. J. J. Woodward on the Modern
organic compounds that supply the animal world with food.
Nevertheless, while I yield my hearty assent to this generali-
zation, and freely admit that it is more than a mere deduction
from the general doctrine of the conservation of energy—that,
in fact, it affords the most satisfactory explanation yet suggested
for a large number of observed phenomena—it is my duty to
caution you against the erroneous supposition that any one
has ever yet succeeded in affording a rigorous demonstration
of the truth of the generalization by an adequate series of
actual experiments.
Various attempts have indeed been made of late years to
determine experimentally both for animals and for man the
potential energy contained in the food of a given period, and
the actual energy liberated during the same time in the form
of heat and work. I think, however, that all practical physi-
ologists who have looked into the question will agree with me
that the numerical results hitherto obtained must be received
with the utmost caution *. Difficulties exist on both sides of
the problem. It is comparatively easy no doubt to obtain a
close approximation to the quantity and composition of the
food; but to represent numerically what becomes of it in the
body, to deduct correctly what passes through unchanged,
and ascertain with reasonable accuracy the amount of carbon
dioxide, water, and urea into which the rest is transformed,
these are questions which have taxed the utmost resources of
investigators, and as to which our knowledge is yet in its
infancy.
On the other hand, the direct measurement of the resulting
heat and work has hitherto proved still less satisfactory. It
would seem to be a very simple thing to place an animal in
a calorimeter and measure the heat-units evolved in a given
time, as Lavoisier and Laplace attempted to do in the latter part
of the last century ; and we have been told that “ Lavoisier’s
guinea-pig placed in the calorimeter gave as accurate a return
for the energy it had absorbed in its food as any thermic
engine would have done” 7. But this assertion is not sup-
ported by the results of actual experiment. We know now
that many precautions, unknown to Lavoisier, must be taken
to secure any approach to accuracy in calorimetric experiments
with animals ; and just as the method is being brought to
something like perfection, by arranging for the respiratory
process and its influence on the results, and by other neces-
* See, for example, M. Foster, ‘Text-book of Physiology’ (2nd edit.
London, 1878, p. 355).
+ Barker, op. cit. supra
Philosophical Conceptions of Life. 23°
sary modifications of the primitive rude attempts*, doubts
are beginning to arise as to whether after all the conditions in
which the animal is placed in the calorimeter are not so far
abnormal as seriously to vitiate the results + ; so that, in fact,
the most approved numerical expressions of the heat-produc-
tion of the body to be found in the books are based rather
upon calculation of the amount that ought to be produced by
the oxidation of an estimated quantity of food than upon
actual calorimetric observations.
Nor do we find it any easier when we attempt the actual
measurement of the amount of work produced by an animal
from a given amount of food. Indeed, in attempting to for-
mulate an equation between the potential energy of the food
and the actual amount of heat and work in any given case, we
are met with the special difficulty that the animal does not
evolve less heat because it is doing work than it does when it
is at rest; on the contrary, it actually evolves more heat,
consuming for the purpose more food than usual, or, if this is
not forthcoming, consuming a part of its own reserve of adi-
pose tissue; so that from this source fresh complications of the
problem arise.
The labour and ingenuity with which all these difficulties
have been encountered is certainly worthy of the highest
praise, and I willingly admit the probably approximate truth
of the figures generally in use, say 2} to 2? million gramme-
degrees as the daily average heat-production of an adult man,
and 150,000 to 200,000 metre-kilogrammes as his capacity
for daily mechanical work f. Nevertheless, these figures are
after all only probable approximations, and there still exists,
with regard to these questions, a large and inviting field for
the application of chemical and physical methods to physio-
logical research.
All the mechanical work done by living beings is effected
by means of certain contractions of their soft tissues. The
movements of the Amoeba, so often described of late years,
may be taken as the type of the simplest form of these con-
tractions. Similar movements occur, with more or less
activity, in the protoplasm of all young cells, and in the
higher animals are strikingly illustrated by the movements
ot the white corpuscles of the blood and the wandering cells
of the connective tissue. In the lowest animal forms-these
* See H. Senator, ‘‘ Unters. iiber die Warmebildung und den Stoff-
wechsel,” Archiv fur Anat. Phys. und wiss. Med. 1872, 8. 1.
+ Foster, p. 368, op. ct. supra.
} L. Landois, Lehrb. der Phys. des Menschen (Vienna, 1879), 8. 402.
240 Mr. J. J. Woodward on the Modern
simple amceboid movements of the protoplasm are the only
movements; but in the higher forms, besides these, certain
special contractile tissues make their appearance, by which
the chief part of the mechanical work done is effected; these
are the striated aud unstriated muscular fibres.
On account of the extreme minuteness of the little proto-
plasmic bodies in which the amceboid movements are mani-
fested, the investigation of the mechanical means by which
these movements are effected has not as yet been attempted,
although a great mass of details have been accumulated by
actual observation with regard to the phenomena themselves
and the conditions under which they occur. Very little more
has been done with regard to the contractions of the unstriated
muscular fibres. The striated muscles, however, have been
made the subject of a host of researches; and I suppose the
conclusions to which we may ultimately be led by these can
be regarded, with but little reservation, as applicable to the
function of the unstriated muscles, and also to the simpler
amceboid protoplasmic contractions.
Yet, notwithstanding the vast amount of experimental
labour and speculative ingenuity that has been lavished since
the time of Haller upon the question of the contraction of the
striated muscle, it must be confessed, in the honest language
of Hermann *, that the problem still mocks our best endea-
vours. Tor myself, I am unwilling to believe that the
phenomena of muscular contraction, or, indeed, of any of the
varieties of protoplasmic contraction by which animals effect
mechanical work, will not by and by be fully and satisfac-
torily explained on chemico-physical principles. I cannot for
a moment give my adherence to the dogmatism of those
modern vitalists who insist that the contractions of a muscle
or of an Ameeba are essentially vital phenomena; for this
would be to claim that life can create force. But it would be
folly to shut our eyes to the circumstance that no chemico-
physical explanation of muscular contraction yet offered has
been so convincingly supported by facts as to command the
universal assent of competent physiologists.
Of the various hypotheses devised to explain muscular
contraction, those which regard the phenomena as in some
way resulting from electrical disturbances have long enjoyed
great popularity. Such of these hypotheses as still survive
are based upon the electrical manifestations actually observed
in living muscles. It has been pretty generally accepted im
accordance with the observations of Du Bois-Reymond, whose
* 1. Hermann, Handb. der Phys. Bd. i. Th, 1, S. 242.
Philosophical Conceptions of Life. 241
brilliant series of experiments in animal electricity * is de-
servedly renowned, that even quiescent living muscles are in
a state of electrical tension. If, for example, a muscle com-
posed of parallel longitudinal fibres be exposed with suitable
precautions, and divided near each extremity by a transverse
incision, the surface of the muscle will be found to be positive
to the cut ends, and if one of a pair of non-polarizable elec-
trodes, connected with a suitable galvanometer, is placed in
contact with the surface of the muscle and the other in con-
tact with one of the cut ends, the existence of a current is
made manifest. The conditions are, moreover, such that while
the maximum effect is produced when the equator of the sur-
face is connected with the centre of one of the cut ends, more
or less current will also be manifested whenever any two
points of the surface are thus connected with the galvano-
meter, provided they are not equidistant from the equator.
In such cases the point most distant from the equator is always
negative. he electromotive force of this natural current of
the quiescent muscle varies greatly, but has been found by
Du Bois-Reymond to amount sometimes to as much as ‘08
Daniell in one of the thigh-muscles of the frog f. In muscles
of different form or cut differently from what has just been
described the currents are somewhat differently arranged ; but
the example just given must suffice for my present purpose.
In accordance with the observations of the same investi-
gator, it is claimed that during a muscular contraction the
electrical tension diminishes, the normal muscle-current expe-
riences a negative variation, and this occurs in such a way that,
as the wave of actual contraction moves along the muscle,
which it does, according to the observations of Bernstein
and Hermann f, with a velocity of about 3 metres per second,
it is preceded by a wave of negative variation. ‘This negative
variation is indeed so trifling if the muscle contracts but
once, that it is difficult to observe it; but when the contrac-
tions succeed each other with great rapidity, as in artificially
roduced tetanus, it may become sufficient to neutralize com-
pletely the deflection of the galvanometer due to the current of
the quiescent muscle.
But the belief that the electrical currents shown to exist in the
* Emil Du Bois-Reymond, ‘ Unters. iiber thierische Elektricitat ’
(Berlin, 1848-60), and ‘Gesammelte Abhandl. zur allgemeinen Muskel-
und Nervenphysik’ (Leipsic, 1875-77).
+ Du Bois-Reymond, Ges. Abhandl. Bd. ii. 8. 243.
t Bernstein, ‘ Unters. iiber den Erregungsvorgang im Nerven- und Mus-
kelsysteme’ (Heidelberg, 1871); also Du Bois-Reymond’s ‘ Archiv,’
1875, S. 526; Hermann, in Pfliiger’s ‘ Archiv, Bd. x. 1876, S. 48.
242 Mr. J. J. Woodward on the Modern
quiescent muscles in these experiments exist also in uninjured
animals hasnot remained unchallenged. Since 1867 it has been
attacked especially by Hermann*, who has endeavoured to show
that these currents are produced only under the special conditions
of the experiments, and that there are in reality no natural
muscle-currents at all. It was well known that the currents
observed in the experiments varied greatly under different
circumstances, and it seemed a significant fact that they should
be most intense when the muscle was removed from the body
and had both ends cut off. If the muscle was removed with
its tendinous extremities still attached, the current was usually
found to be very feeble or entirely absent, until the ends were
well washed in salt and water or dipped in acid. Du Bois-
Reymond had explained this by supposing the natural ends
of the muscle to be protected by what he called a parelectro-
nomic layer of positive elements that must be removed before
the natural current could be made manifest. On the other
hand, Hermann has endeavoured to show that the parts in-
jured by the knife or acted on by the salt or acid enter at once
into the well-known condition of rigor mortis, and only be-
come negative to the still living portions of the muscle in
consequence of this change. ‘That electrical disturbances
actually occur in contracting muscles he admits, but endea-
vours to show that they are due simply to the fact that the
changes preceding contraction make the affected part of the
muscle negative to every part less modified or wholly unal-
tered. Hence if an uninjured muscle be caused, under proper
precautions, to contract simultaneously in all its parts, it will
be found that the contraction is wholly unaccompanied by any
muscle-current f.
Observations that appear to support these views of Her-
mann have been brought forward by Engelmann f. On the
other hand, Du Bois-Reymond has defended his views with
vigour, and sharply criticized, of course, the labours and logic
of his assailant §. I need not at present express any opinion
as to the merits of this voluminous controversy. It is enough
for my purpose to indicate the questions at issue as sufficiently
important and uncertain to be well worthy of independent
experimental criticism.
Suppose, however, this criticism should result in showing
* L. Hermann, ‘ Weitere Unters. zur Phys. der Muskeln und Nerven’
(Berlin, 1867) ; also Handb. der Phys. Bd. i. Th. 1 (Leipsic, 1879), 8, 192
et seq.
+ Hermann, Handb. der Phys. Bd. i. Th. 1, S. 216.
} Engelmann, Pfliiger’s ‘ Archiv, Bd. xv. (1877), S. 116 e¢ seg.
§ Du Bois-Reymond, Ges. Abhandl. Bd. ii. 8. 319 et seg.
_— .
Philosophical Conceptions of Life. 243
that Hermann is wholly in the wrong and that the muscle-
currents observed by Du Bois-Reymond really exist in
healthy muscles. How then shall these currents explain the
phenomena of muscular contraction? I presume that no
physiologist of the present day is misled by the superficial
comparison which Mayer and Amici were led by their micro-
scopical studies of the muscles of insects to make between
the striated muscular fibre and a voltaic pile *. But the
molecular theory by which Du Bois-Reymond has endea-
voured to explain his natural muscle-currents and their
negative variation would appear to open up an inexhaustible
mine of speculative possibilities for those who are inclined to
speculate.
Yet the old experiment of Schwann f has always been a
stumbling-block in the way of any theory that would explain
muscular contraction by the action of a force which must
increase inversely as the square of the distance between the
molecules, for the force of the contraction, as it actually
occurs, diminishes as the muscle shortens; and hence we find
so good a physiologist as Radcliffe { reviving in a modified
form the old hypothesis of Matteucci §, in accordance with
which the electrical tension of the fibre in the state of rest
causes a mutual repulsion of the molecules, and so elongates
the muscle, while the contraction is merely the effect of the
elasticity of the tissue, which asserts itself so soon as the
repulsive force is diminished by the negative variation that
precedes contraction.
In consequence of these and other difficulties many physio-
logists are beginning to regard the electrical phenomena as
subordinate accidents of the chemical processes that go on in
muscle, and endeavour to explain muscular contraction as
resulting directly from these chemical processes themselves.
Arthur Gamgee || has adopted as most probable the chemical
hypothesis of Hermann {]. This assumes the contraction to
result from the decomposition of a complex nitrogenous com-
pound supposed to be contained in the muscular tissue, and
* Mayer, Miiller’s ‘ Archiv,’ 1854, 8.214; Amici (1858), translation in
Virchow’s ‘ Archiv,’ Bd. xvi. 1859, S. 414.
+ Schwann, in Miiller’s Handb. der Phys. 1837, Bd. ii. S. 59.
¢ C. B. Radcliffe, ‘ Dynamics of Nerve and Muscle’ (London, 1871).
§ Matteucci, ‘ Lectures on the Physical Phenomena of Living Beings’
(translated by J. Pereira), London, 1847, p. 333.
|| Arthur Gamgee, ‘A Text-Book of the Physical Chemistry of the
Animal Body,’ vol. i. (London, 1881), p. 418.
s pe Hermann, ‘Grundriss der Phys. des Menschen,’ 5te Aufl. 1874,
244 Mr. J. J. Woodward on the Modern
named inogen. During contraction inogen breaks down into
carbon dioxide, lactic acid (Fleischmilchsiiure), and gelati-
nous myosin. The rearrangement of molecules necessary to
produce the latter body determines the contraction. Subse-
quently the gelatinous myosin combines with the necessary
materials furnished by the blood, and becomes inogen again.
This decomposition and recomposition goes on also while the ~
muscle is at rest; but as then the gelatinous myosin is re-
converted into inogen as rapidly as it is formed, no con-
traction results.
Du Bois-Reymond declares all this to be merely unsup-
ported hypothesis *. Gamgee himself admits that it is after
all not very clear why the gelatinous myosin should contract.
Michael Foster ¢, who wholly rejects this particular chemical
hypothesis, nevertheless seems quite sure that the true expla-
nation will be found to be a chemical one. He insists that
muscular contraction is essentially a translocation of molecules,
and declares that whatever the exact way in which this trans-
location is effected may be, it is fundamentally the result of
a chemical change, or, as he describes it, ‘an explosive de-
composition of certain parts of the muscle-substance.”’
The purpose I have in view does not require, fortunately,
that I should attempt to decide whether these more purely
chemical theories of muscular contraction or the more purely
electrical theories are best entitled to confidence. My object
has been effected if I have impressed you with the fact that
wide differences of opinion still exist as to the nature of the
process, and that further investigation is indispensable for the
settlement of existing controversies.
The subject thus briefly discussed brings us naturally to
the consideration of the nature of the action of the motor
nerves, by which, in all animals possessed of a muscular and
nervous system, the contraction of the muscles is regulated
and determined.
The hypothesis which identifies the nervous currents with
electricity was propounded in the posthumous work of Hausen}
in 1748, and, notwithstanding all the difficulties and objec-
tions it has encountered, still survives in a modified form in
many contemporaneous minds. Those who hold to this view
appeal in its support to the electrical phenomena actually
observed in nerves in accordance with the investigations of
* Du Bois-Reymond, Ges. Abh. Bd. ii. 8. 820,
+ Foster, op. cit. p. 79 et seq.
C. A. Hausen, ‘Novi profectus in historia electricitatis’ (Leipsic,
1743). I cite from Du Bois-Reymond, ‘ Unters. ber thierische Elek-
tricitat,’ Bd. ii. (Berlin, 1849), Th. i. 5. 211.
-_ oo,”
Philosophical Conceptions of Life. 245
Du Bois-Reymond. These observations have long been
widely accepted as conclusive proof that natural currents exist
in the quiescent nerve of the same general character as those
attributed to the quiescent muscle, which I outlined a few
minutes ago. ‘The electromotive force of this current was
found by Du Bois-Reymond * to be equal to ‘022 Daniell in
the sciatic nerve of the frog. When a nervous impulse passes
along the nerve, the natural current is diminished; it expe-
riences a negative variation, which, according to Bernstein ft,
when the impulse results from a very potent stimulation,
may more than neutralize the natural current. The same
physiologist has shown that this negative variation moves
along the nerves of the frog at the rate of 28 metres per
second, that is, at the same rate as the nervous impulse itself,
as determined without reference to the electrical phenomena.
As in the case of the muscle-currents, these phenomena
have been differently interpreted by Hermann {, who denies
the existence of any natural nerve-current in uninjured nerves,
and ascribes those observed in the experiments to the circum-
stance that the parts of the nerve dead or dying, in conse-
quence of the section, become negative to the living nerve.
The negative variation produced by the stimulation of a
nerve he explains by assuming that the stimulated part of the
nerve becomes, in consequence of the changes resulting from
the stimulation, negative to the unstimulated parts. I will
not attempt to enter to-night into the merits of the contro-
versy still in progress with regard to this question, nor will
I pause to discuss the exceedingly curious and interesting
phenomena of electrotonus §, concerning which I will only say
that the question has even been raised by Radcliffe as to how
far these phenomena are peculiar to nerves, and how far they
may be regarded as mere phenomena of the electrical currents
employed, which would be equally manifested under similar
circumstances if a wet string or other bad conductor should
be substituted for the nerve ||.
However these disputes may be ultimately decided, what-
ever the actual facts with regard to the electrical manifesta-
tions In nerves at rest or in action may ultimately prove to
* Du Bois-Reymond, Ges. Abh. Bd. ii. S. 250.
+ Bernstein, op. cit. supra.
¢ Hermann, loc. cit. supra, note *, p. 242; also Handb. der Phys. Bd. ii.
Th. 1 (Leipsic, 1879), 8. 144 e¢ seq.
§ See especially Du Bois-Reymond, ‘ Unters. Bd. ii. Th. 1, 8. 289, and
Pfliiger, ‘ Unters. tber die Physiologie des Electrotonus’ (Berlin, 1859).
An excellent summary of the observations (with the literature) is given
by Hermann, ‘ Handb. der Physiologie, Bd. ii. Th. 1, 8. 157 e¢ seg.
|| Radcliffe, p. 74 et seqg., op. cit. supra,
246 Mr. J. J. Woodward on the Modern
be, there is a group of easily repeated elementary experiments
which seem to show pretty distinctly that whatever the ner-
vous impulse may be itis not merely an electrical current.
It was known already when Haller wrote * that a string
tied tightly around a nerve, although it in no wise interferes
with the passage of electrical currents, puts a speedy end to
the transmission of nervous impulses. With this old experi-
mental difficulty uncontradicted, it seems strange that any one
should declare at the present time that “the main objection
raised to the electrical character of nerve energy is based upon
its slow propagation” f. In fact this latter objection is alto-
gether a subordinate difficulty which may perhaps be entirely
explained away; the main experimental objection does not
relate to the velocity, but to the conditions of the propagation
of the nervous impulse. If instead of tying a string around
it the nerve be merely pinched or bruised well with a pair
of forceps, so as to destroy its delicate organic texture, if it
be compressed tightly by a tiny, metallic clamp, if it be
divided by a sharp knife, and the cut ends brought nicely into
contact, or brought into contact with the extremities of a piece
of copper wire, it will still conduct electrical currents as well
as ever, but can no longer transmit the nervous impulse. So,
too, there are certain poisons, such as the woorara, which
completely destroy the capacity of the nerve for transmitting
nervous impulses without in the least diminishing its conduc-
tivity for electricity {.
In view of these and other practical difficulties, the best
instructed modern physiologists no longer attempt to identify
the nervous impulse with the electrical phenomena by which it
is accompanied. Du Bois-Reymond himself has suggested that
the nervous agent “ in all probability is some internal motion,
perhaps even some chemical change, of the substance itself con-
tained in thenerve-tubes, spreading along the tubes” §. Herbert
Spencer came to the conclusion that “ nervous stimulations and
discharges consist of waves of molecular change” || flowing
* A, von Haller, ‘Klementa Physiologiz,’ lib. x. sect. viii. § 15, t. iv.
(Lausanne, 1762), p. 880. He cites as authority the essay of Le Cat,
crowned by the Berlin Academy in 1753. [We have in the S. G. O.
Library the Berlin edition of 1765, ‘Traité de lexistence &c. du fluide
des nerfs,’ &c. |
+ Barker, p. 8, op. cit. supra.
{ Claude Bernard, ‘ Legons sur la Phys. et la Path. du Systéme ner-
veux’ (Paris, 1858), t. i. pp. 157 and 224.
§ Translation of a lecture given by E. Du Bois-Reymond at the Royal
Institution, London, in Appendix no. 1 of H. Bence Jones’s ‘Croonian
Lectures on Matter and Force’ (London, 1868), p. 180.
| Herbert Spencer, ‘The Principles of Psychology,’ vol. i. (New York,
1871), p. 95. Compare also his ‘ Principles of Biology,’ vol. ii. (New
York, 1867), p. 346 et seq.
Philosophical Conceptions of Life. 247
through the nerve-fibres ; and I suppose that most physiologists
at the present time think of the nervous current in some such
way as this. Even those who attach most importance to the
electrical phenomena will, I take it, agree with Michael
Foster that these “ are in reality tokens of molecular changes
in the tissue much more complex than those necessary for the
propagation of a mere electrical current ” *,
We do not, however, as yet possess any sufficient founda-
tion of facts on which to build a reasonable hypothesis as to
the nature of the molecular disturbances that accompany a
nervous impulse. The labours of the physiological chemists
have taught us nothing with regard to the changes that go on,
except that the axis-cylinder, which in the inactive living
nerve is alkaline, becomes acid after long-continued activity
or after death +. We can measure the velocity with which
the impulse travels, we can study the conditions under which
it arises, we can believe, as I certainly do, that it will ulti-
mately receive a chemico-physical explanation; but its real
nature we do not yet know.
So far as we can ascertain, the phenomena of the conduc-
tion of nervous impulses by the sensitive nerves are so similar
to those of the conduction of motor impulses that any explana-
tion ultimately adopted for the one will probably apply to the
other also. When, however, we ascend to the study of the
nervous centres, by which sensitive and motor nerves are con-
nected together, and attempt the interpretation of the complex
functions of nerve-cell, ganglion, spinal cord, and brain, we
find that none of the hypotheses hitherto brought forward to
explain the observed phenomena repose on any defensible
chemico-physical basis.
I cannot of course undertake to give to-night even the most
meagre outline of the wondrous mechanism which physiolo-
gical experiments show must exist. That reflex actions,
co-ordinated muscular movements, and all the complex phe-
nomena of this class do depend upon a wonderfully complex
mechanism, and occur in strict accordance with the ordinary
chemical and physical laws, I do not for a moment doubt, and
I cordially invite the cooperation of the chemists and physicists
to aid the physiologists in the explanation of this mechanism,
for we stand only upon the threshold as yet.
If now we turn from the more general discussion of mus-
cular contraction and nervous action to the consideration of
the several functions carried on in animals by means of
special arrangements of the muscular and nervous systems,
* Foster, p. 79, op. cit. supra.
+ A Gamgee, p. 447, op. cit, supra.
248 Mr. J. J. Woodward on the Modern
we continually encounter the preponderating influence of
purely physical laws. ‘The introduction of air into the lungs
of breathing animals and its expulsion thence is effected in a
purely mechanical way, while the exchange of the carbon
dioxide of the blood with the oxygen of the inspired air occurs
in strict obedience to the laws of the diffusion of gases.
The ordinary laws of hydraulics govern the circulation of
the blood and lymph, and all the complex visible motions of
the body are executed in accordance with the ordinary laws
of mechanics ; nor is it at all necessary for me to insist upon
the purely physical nature of the operations of the organs of
the special senses, conspicuously the eye and the ear. For
example, so far as concerns the means by which images of
external objects are formed sharply upon the retina, the eye
is as purely a physical instrument as the telescope or the
microscope. But I need not dwell upon this group of pheno-
mena, because the importance of the réle of the ordinary
physical laws in this domain is conceded, I suppose, by the
extremest of the vitalists of the present day.
We see, therefore, that, with regard to a large part of the
phenomena of living beings, there are grounds for affirming
either that they have already been satisfactorily explained by
a reference to established chemical and physical laws, or at
least that they are of such a character that it is reasonable to
hope they may be thus explained at some future time. Is it
possible, then, to return, as some have done of late years, to
the old speculation of Des Cartes, and look upon living beings
as mere machines? ‘To do so it will not suftice to image to
yourselves ordinary machines in which fuel yields force. To
satisfy the chemico-physical hypothesis of lite you must sup-
pose machines that build themselves, repair themselves, and
direct from time to time new applications of their energy in
accordance with changes in the environment—nay, more,
machines that accouple themselves together, breeding little
machines of the same kind, that grow. by and by to resemble
their parents, and all this self-directed, without any engineer,
But even Des Cartes required an engineer—the soul—to run
his man-machine ; and the logic which compelled him to this
view applies just as forcibly to all the modern machine-con-
ceptions of living beings.
I have already asserted that there are whole groups of
phenomena characteristic of living beings, and peculiar to
them, which cannot be intelligently explained as the mere
resultants of the operation of the chemical and physical forces
of the universe. ‘Lhese phenomena I reter—I avow it without
hesitation—to the operations of a vital principle, in the
Philosophical Conceptions of Life. 249
existence of which I believe as firmly as I believe in the
existence of force, although I do not know its nature any
more than I know the nature of force. If, for convenience,
at any time [ compare the living body to a machine, I must
compare the vital principle to the engineer ; it is the director,
the manager if you will, but it does not supply the force that
does any part of the work. Let us consider, then, in the
remainder of this discourse the phenomena which indicate the
guidance of the vital principle.
The first group of phenomena belonging to this second
class are those forced upon our attention whenever we attempt
to study the question of the origin of life. It has seemed to
some of our contemporaries that, in accordance with the doc-
trine of evolution, as deduced by Mr. Herbert Spencer from
the great truth of the persistence of force, life ought always
to arise spontaneously out of inorganic matter whenever the
necessary materials and other conditions of life are brought
together. Indeed, if there be nothing more or other in life
than force, I confess I do not understand how this conclusion
can be logically escaped; and yet when we come to interrogate
nature we find that, in point of fact, things do not happen so.
The sun may stream all the enormous energy of his rays
upon the slime of the Nile, but he generates no monsters ;
nay, not even a bacterium, except in the presence and under
the direction of pre-existing life. Our biological knowledge has
so far advanced that it is easy for us to get together mixtures
of matter, for the most part derived from pre-existing living
beings, which are peculiarly well fitted to supply the materials
needed for the building up of a variety of low forms of
life ; and the extent of our present knowledge of the conditions
favourable to the development of these low forms of life is
shown by the rapidity with which they do develop from a
few individuals to countless millions, if only a few indivi-
duals are introduced as parents into our flasks and brood-
ovens. ‘The species to which the countless progeny belongs,
depends always upon the species of the parents we introduced
by design or accident ; and if parents of several species are
introduced we may imitate on a tiny scale the great struggle
for existence, and witness the survival of the fittest. Never,
however, has the spontaneous generation, out of inorganic
matter, of a single living form been yet observed. —
Speculative considerations have, indeed, from time to time
led certain enthusiasts to desire earnestly that it might be
observed; and when we consider, on the one hand, the influ-
ence of pre-existing bias, and, on the other, the intricacy of
some of the experimental processes in question, it is by no
Ann. & Mag. N. Hist. Ser. 5. Vol. xiii. 17
250 Mr. J. J. Woodward on the Modern
means necessary to charge dishonesty upon those who, from
time to time, have actually fancied that their desires have been
realized to the extent of the spontaneous generation of bac-
teria at least. When we consider the immense development
of the trade in canned food, which could not exist for a single
summer’s day if these experimenters were not mistaken, it
will be seen how little need there was for renewed scientific
experiment to refute their conclusions ; but it is a noteworthy
fact that among those who have contributed most by exact
research to recent scientific demonstrations of the truth that
life never arises except from pre-existing life, are to be found
some of the most earnest and eloquent advocates not merely
of the doctrines of evolution, but of its supposed corollary, the
chemico-physical hypothesis of life.
I sympathize heartily with those who, recognizing that the
supposition of the spontaneous origin of life on our globe is
flatly contradicted by the facts of science, have endeavoured
to escape the difficulty by imagining the earliest parent living
forms to have been brought to our earth on the surface of
meteoric stones or other cosmical bodies. This hypothesis,
put forward originally on purely theoretical grounds, has re-
cently acquired a certain degree of support from the published
observations of Hahn and Weinland*, who believe they have
recognized the remains of humble coralline forms in thin sec-
tions of meteoric stones collected in Hungary. Yet these
observations, if indeed they should prove to be correct, would
rather afford indications of the existence of life in other worlds
than ours, than show that living forms could survive the high
temperature to which such cosmical masses must be exposed
during their transit through our atmosphere; and even should
we find reasons for ultimately adopting this hypothesis, we
should not have solved the problem of the origin of life, but
only removed it entirely beyond the domain of further scientific
investigation.
If, however, we reject this view, and still mean to support
the chemico-physical hypothesis of life, we shall have to
resort to a still more improbable supposition. We shall have
to suppose that although in the present order of things life
can only arise out of pre-existing life, the order of things was
at some past time so far different that life could then arise
out of inorganic matter—a supposition which implies an insta-
bility in the course of nature that is contradicted by all the
teachings of science.
* O, Hahn, ‘Die Meteorite und ihre Organismen,’ Tibingen, 1881.
I cite the Journ, of the Royal Microsc. Soc. October 1881, p. 723,
Philosophical Conceptions of Life. 251
I willingly admit that, in view of our present scientific
notions of the cosmogony, it is impossible to believe that life
always existed upon this planet. I willingly admit that life
on the earth must have had a beginning in time. But we do
not know how it began. Let us honestly confess our igno-
rance. I declare to you I think the old Hebrew belief, that
life began by a creative act of the Universal Mind, has quite
as good claims to be regarded as a scientific hypothesis as the
speculation that inorganic matter ever became living by
virtue of its own forces merely.
If we turn now to the consideration of the processes of
growth, we shall find additional reasons for believing in the
existence of a vital principle. Let us consider first, in the
most general way, the conditions under which those strictly
chemical processes occur, to which I have already alluded,
and by which the inorganic atoms are combined into organic
matter. I repeat it, I do not for a moment question that the
actual force by which these processes are compelled exists in
the solar rays, and that it is, after all, the solar energy thus
stored up in the vegetable protoplasm and its products that
supplies, by its subsequent liberation, all the force manifested
by living beings. Yet, let me beg you to observe that in all
the myriads of years during which the solar energy has
streamed upon the earth, that energy has never, on any occa-
sion that we know of, determined the combination of inorganic
atoms into organic matter, except within the substance of
already living protoplasm. The water and carbon dioxide
and ammonia in the atmosphere and in the soil come into
contact with each other, within thesubstance of porous inorganic
clods on the surface of the soil, much as they do in the sub-
stance of protoplasm, and the equal sun warms both alike ;
but in the clod they remain water, carbon dioxide, and ammo-
nia; in the protoplasm, provided only that it is living proto-
plasm, they combine into starch or oil, or even into protoplasm
itself. The essential condition, then, of this storing up of
the solar energy for the subsequent use of living beings is
the presence of life, and in these fundamental operations
the mighty force of the sun acts, in the fullest sense of the
words, the part of the servant of lite.
The view thus suggested, that we have here to do with
something more than the mere operation of the inorganic
forces, is still further strengthened when we come to consider
more in detail the phenomena of the growth of living beings,
whether plants or animals. The better we become acquainted
with these phenomena the more fully we become convinced
> 17*
252 Mr. J. J. Woodward on the Modern
that we have to do with processes for which the inorganic
world affords no parallel.
Linneeus, indeed, declared, “ lapides crescunt,” using the
very same phrase which he applied also to plants and animals*.
But it is impossible to maintain this assertion without adopt-
ing the most superficial view of the growth of living beings,
and defining the process to consist merely in increase of size.
That this should have appeared reasonable in the time of
Linneus need excite no surprise ; but it seems strange to find
so astute a thinker as Mr. Herbert Spencer repeating the old
fallacy in the first chapter of his ‘ Inductions of Biology,’ and
declaring, “ Crystals grow, and often far more rapidly than
living bodies’}. ‘Then, after instancing the formation of
geological strata by the deposit of detritus from water, as well
as the formation of crystals in solutions, as examples of growth
in the inorganic world, he asks: “Is not the growth of an
organism a substantially similar process ?” and adds, ‘f Around
a plant there exist certain elements that are like the elements
which form its substance, and its increase in size is effected
by continually integrating these surrounding like elements
with itself; nor does the animal fundamentally differ in this
respect from the plant or the crystal.”
Now, as opposed to this, I must express my belief that the
more we know of the actual details of the process of growth
in plants and animals the more clearly will it be seen that this
process does differ so fundamentally from that by which a
crystal is formed and increases in size, or from any increase
in size of inorganic bodies, that the same scientific term can-
not with any propriety be applied to both, however long
popular usage may have given to both a common name.
When inorganic bodies increase in size the additional atoms
are deposited on their external surfaces ; or, if a fluid, after
penetrating the interstices of some porous body, deposits there
any material held in solution, the mass, indeed, is increased
thereby, but not the size. When, however, vegetable proto-
plasm grows, it does not merely integrate with itself certain
elements around it like the elements which form its substance ;
the needed elements exist in compounds quite unlike itself,
and it combines them together into protoplasm in all parts
* “ Lapides crescunt, Vegetabilia crescunt et vivunt, Animalia crescunt,
vivunt et sentiunt.” This phrase occurs in the first edition of the ‘ Sys-
tema Nature,’ Leyden, 1735. I cite the reprint of Fée, Paris, 1830,
p. 3, as well as the second Stockholm edition, 1740, p. 76. The expression
is replaced in the later editions by more guarded language.
+ Herbert Spencer, ‘The Principles of Biology,’ vol. i. New York,
1866, p. 107.
Philosophical Conceptions of Life. 253
of its mass, so that it grows by a process of intussusception
wholly unlike anything that occurs in the inorganic world.
In the case of animal protoplasm, the mode of growth by
intussusception is the same, but the capability of combining
together mere inorganic elements into its own substance is
lost; and, besides these, a certain amount of pre-existing
vegetable or animal protoplasm must be present in the food,
or growth will not go on.
In both cases, when the growth has proceeded to a certain
extent—within certain definite limits—a new characteristic
phenomenon occurs in a growing mass of vegetable or animal
protoplasm ; it multiplies by division, its whole mass partici-
pating in the act, in accordance with one or other of a few
definite methods. This process is repeated again and again.
The progeny may separate, without modification, as inde-
pendent forms, or, as in the case of the more complex organ-
isms, they may cohere together, and the process culminates
by groups of them undergoing certain definite and peculiar
transformations, after which further multiplication becomes
rare or ceases altogether, and the growth of the complex
organism is thus limited.
I cannot, of course, attempt this evening to describe all the
known details of the progress of growth which I have thus
hastily sketched; to give you a really satisfactory account of
them would require a series of lectures. But I do not hesitate
to say that the more fully you know these details the more
unscientific you will think the attempt to class them as in any
way similar to the circumstance that inorganic crystalline com-
pounds seem “ each to havea size that is not usually exceeded
without a tendency arising to form new crystals, rather than
to increase the old.” It is, at the best, a waste of words to
attempt to explain complex phenomena by comparing them to
simpler ones which are fundamentally unlike them.
I have but now referred to a process by which, in the growth
of the more complex living beings, the small primitive proto-
plasmic mass, out of which each individual arises, subdivides
and produces a numerous brood of protoplasmic masses, at first
closely resembling the parent mass, but after a time differing
from it more and more, and finally undergoing transforma-
tions into definite and peculiar forms. ‘This process, which
does not take place in any disorderly manner, but in a very
characteristic and definite way in each individual form, is
designated by the term development. In point of fact, so
far as it consists in the mere growth and multiplication of
the individual elements that compose the organism, and the
- imerease in size of the organism itself on account of these
254 Mr. J. J. Woodward on the Modern
processes, it is properly designated by the term growth. In so
far, however, as the individual elements are differentiated,
and the wonderful architecture of the living being, with its
organs and systems, is completed thereby, it is properly de-
signated by the term development.
Nothing like the process of development as thus defined
exists in the inorganic world, and in all the attempts at such
a comparison that it has been my fortune to meet with, the most
fundamental facts of the development of living beings have
been persistently ignored. Among these fundamental facts I
invite your attention especially to the circumstance that there
is something in the microscopic mass of protoplasm, out of
which, even in the case of the highest and most complex
living beings, each individual arises, that goes even further
in determining the direction: in which the individual shall
develop than the pabulum, or environment, or all the mighty
chemical and physical forces that are brought into play as the
process goes on. In a word, the individual develops after
the pattern of its parent, or not even all the solar energy can
compel it to develop it at all.
We are thus brought face to face with the facts of sexual
generation, and especially of heredity, with all their wide
bearings on the great biological questions of natural selection
and the origin of species. Into the details of these large ques-
tions the limits of the hour will not permit me to enter.
Could I take time to do so, I am satisfied that at every step I
should be able to collect for you additional evidence of the
existence of a vital principle. Still, I regret this the less
because most of you, | think, are so familiar with the modern
literature of these subjects, and especially with the admirable
writings of Mr. Darwin, that I feel sure, if I can succeed in
giving you a clear outline of ‘my views, much that I should
say, had | time, will suggest itself to your own minds. In a
general way, however, when we study, in the history of life
upon this globe, the double phenomena of long-continued per-
sistence of type, and of slow variation continually occurring,
we shall find that almost all biologists, whatever their theory
of life, explain these phenomena on the one hand by heredity,
on the other by the sensibility of the organism to the influence
of the environment.
Both heredity and the influence of the environment may be
very conveniently studied in those simplest organisms in which
each individual consists of a single minute mass of naked
protoplasm, as in certain rhizopods, for example, the Amoeba.
‘These tiny creatures produce a progeny which preserves the
parental type as closely as is done by the offspring of the ~
Philosophical Conceptions of Life. 250
higher animals. Their sensibility to the influence of the
environment is manifested in several ways. They grow, that
is they appropriate materials from the environment, in the
way I have already specified ; they manifest automatic move-
ments, that is, on encountering food, obstacles, or other dis-
turbing external circumstances, movements result the direction
and energy of which are in no wise determined by the cha-
racter or force of the external influences, or, as they may be
conveniently termed, the stimuli by which these movements
are provoked; and finally, simultaneously with the process
of growth, a certain metamorphosis, or metabolism, of the
protoplasm is continually going on, resulting in the formation ~
of excrementitious substances which are continually being
excreted.
The processes of growth and metabolism exhibit different
degrees of intensity in accordance with variations of the envi-
ronment ; and whatever physical theory of the mode in which
the protoplasmic motions are produced we may adopt, the
mechanical force manifested can only be supposed to proceed
from the decomposition of a part of the protoplasm itself into
simpler compounds, that is, from a particular kind of meta-
bolism. Hence you will, I think, be quite prepared to hear
me speak of all the circumstances in the environment that so
act upon living protoplasm as to increase its growth or meta-
bolism as stimuli, and of the property of living protoplasm
by which all its responses to stimuli are guided as irrita-
bility, instead of limiting these terms to the phenomena of
automatic movement only, as was formerly done. This irri-
tability of living protoplasm determines the direction in which
its internal forces shall be manifested. Speaking of it as I
do, perhaps you would wish me to call it sensibility rather
than irritability ; and I do not know that I should object very
strenuously to any one who wished to do this. But however
you mayname it, it is this vital property of all living protoplasm
that produces the sensibility to changes in the environment,
which has been the main factor in the gradual evolution, durmg
the ages, of the highest and most complex from the simplest
and lowest living forms.
Against this view it has been urged with much ingenuity
that protoplasm is the material substratum of life, and life
merely a property of protoplasm; that is, if the words have
any meaning at all, that life is the resultant only of the forces
inherent in the inorganic atoms of which the protoplasm is
built up. Now, in the first place, no one has ever yet been
able to show, by any conceivable synthesis, how the forces
known to belong to the several kinds of inorganic atoms, of
256 Mr. J. J. Woodward on the Modern
which protoplasm is composed, could by their combination,
produce the characteristic phenomena of living protoplasm,
namely, the phenomena of irritability, as I have just described
them. But, in the second place, this speculation appears to
be pretty flatly contradicted by the circumstance that, although
protoplasm can only be formed within the substance of previ-
ously existing living protoplasm, it can continue to exist, it
does continue to exist as protoplasm after it has ceased to live.
Not merely can it persist for a time without chemical change
as dead protoplasm, it can subsequently serve as food and be
reconverted into living protoplasm once more. Bear in mind,
however, that this change can only be effected within the sub-
stance of the living protoplasm of the animal that assimilates
this food. It is not effected by the chemistry of digestion ;
that merely makes peptone of the protoplasm—merely makes
it soluble enough to pass into the substance of the protoplasmic
masses that are to appropriate it. ‘These considerations, then,
would seem to show that the material, protoplasm, cannot be
rightly believed to be of itself the cause and essence of life.
If I should pause here, it seems to me that I should have
brought forward adequate reasons for believing in the existence
of a vital principle. But I cannot pause here. Beyond and
above all this there is another great group of phenomena
peculiar to living beings—a group of phenomena concerning
which, in my own individuality, | have knowledge at least as
positive as any I possess of the existence of force, and which
I am led, by a logic quite as convincing as that by which any
general proposition with regard to the external world is proven,
to believe exists in like kind and degree in the case of my
fellow-man. I refer to the phenomena of the perceiving,
emotional, will-full, reasoning human mind. Into the argu-
ment that makes it highly probable that a similar but less
and less perfect mind exists in the animal world, and iden-
tifies with mind the sensibility of the lowest animal forms,
and even that of vegetable protoplasm, I will not attempt to
enter to-night. Mr. Herbert Spencer himself has presented
this view with so much ingenuity, that, without committing
myself to an approval of all his details, I must content my-
self by referring you to his writings for one of the best discus-
sions of this matter. It will be sufficient for my present
purpose to close this discourse by the presentation of a few
considerations in relation to mind as it exists in man.
For myself I know mind only as a manifestation of life, if,
indeed, it is not the essence of life. But the old doctrine of
Epicurus, handed down to us in the poem of Lucretius, that
in some way or fashion mind is produced by the clashing
Philosophical Conceptions of Life. 257
together of the atoms, has been boldly revived of late years,
and transmuted into a form more plausible to modern thought,
although just as unsupported by any actual knowledge of
facts.
No one has done this more boldly or more cleverly than
Mr. Herbert Spencer has done in his ‘ First Principles,’ and
of course you are all familiar with the ingenious argument,
in favour of this view, which runs through that masterly
work. It would be, from many points of view, profitable,
but it would be a very laborious task, to attempt the critical
discussion of his argument. It must suffice, for my present
purpose, to point out that two of the fundamental assumptions
upon which that argument is based are wholly undemonstrated.
The first assumption is, that mind is itself a force*; the
second, that mind cannot be conscious of itself, but only of
the external worldT.
If I could bring myself to believe that mind is, in any
proper sense of the word, a force, and that such popular meta-
phorical expressions as mental force or mental energy accu-
rately described the phenomena, I should certainly expect to
find at least some shadow of proof for Mr. Herbert Spencer’s
assertion that mental operations fall within the great gene-
ralization of the correlation and equivalence of the forces.
On the contrary, however, you will find, on reading his lucid
periods, that his whole argument relates to those physical
conditions in the organs of sense and in the muscular and
nervous systems which are the antecedents of perception—
which are, in fact, the things really perceived—and in no
sense constitute the perceiving mind. Between strictly
mental phenomena and the physical forces no one has as yet
even attempted to establish a numerical equivalent; nay, more,
the correlation of thought with the physical forces is not
only undemonstrated, it is utterly unthinkable. You can con-
ceive several different ways, it matters not whether true or
false, in which the motions we know as heat might be con-
verted into those we know as light, and so on with the other
physical forces; but you cannot represent mentally any
intelligible scheme by which any of the physical forces can
be converted into the simplest or most elementary thought.
As to the question of self-consciousness, it seems as if the
great philosopher were reasoning in a circle. He first assumes
that the fundamental condition of all consciousness is the
antithesis between subject and object,—which is true only
* Herbert Spencer, ‘ First Principles,’ Amer. Ud. New York, 1864,
p. 274.
+ Id. op, cit. p. 65 et seg.
258 Mr. J. J. Woodward on the Modern
with regard to consciousness of perception, the form of con-
sciousness by which we become acquainted with the non ego,
—and then he concludes that there can be no consciousness of
the ego because it cannot fulfil these conditions. That is, in
a word, he denies consciousness of the ego, because it is not
consciousness of the non ego. Really it appears to me that,
as against such a philosophy as this it is not amiss to appeal
to “the unsophisticated sense of mankind,” of which Mr.
Mansel speaks*. But there is fortunately a better philosophy
than this—a philosophy which recognizes the validity of the
mind’s self-consciousness as at least fully equal to the validity
of its consciousness of the conditions of the body by which it
obtains a knowledge of the external world. By this self-
consciousness [ know, with a certainty which no doubt can
ever disturb, that [ have a mind ; and by rightly applying my
reasoning powers to the data of my self-consciousness, 1 can
learn much that will be useful to me with regard to my mental
processes and the methods of employing them. But here I
have to stop. I can learn nothing, whether by consciousness
or by reasoning, with regard to the real nature of my con-
scious mind, and however much it may long for immortality,
neither philosophy nor science affords any foundation of proof
upon which it might build its hopes.
I have already said that I know mind only as a manifesta-
tion of life. Its operations are intimately connected with the
chemical and physical phenomena of living beings, and it
exercises over them a certain directing influence, the nature
of which we do not understand. The obedience of our volun-
tary muscular actions to the mandates of the guiding will is
a tamiliar illustration of this directing influence. On the
other hand, all the knowledge of the external world on which
the mind exerts its reasoning power reaches it through the
organs of sense and the nervous system. Indeed, our studies
of the phenomena of sensation compel us to conclude that
what our mind really perceives, when it takes cognizance of
the external world, is merely the ever-changing panorama of
our own cerebral states. It should be anticipated therefore
that disturbed or morbid conditions of the brain would lead to
irregular or disorderly mental operations; and the circum-
stance that this really happens affords no better proof of the
materiality of thought than is afforded by the circumstances of
our ordinary normal thought.
So, too, since the cerebral changes, which the mind per-
ceives, are themselves of a purely chemico-physical nature, it
should be anticipated that, like the metabolic processes in
* Ascited by Mr. Herbert Spencer, /oc. cit. last note.
Philosophical Conceptions of Life. 259
other tissues, they would be accompanied by an increased ex-
cretion of characteristic waste-products, by evolution of heat
and by afflux of blood. Experimental investigation has been
directed to each of these points, and some important observa-
tions have no doubt been made; but much of the testimony
is conflicting, and our knowledge is still so incomplete that
further inquiry in each direction is greatly to be desired.
This is particularly the case with regard to the chemical
questions connected with the metabolism of the brain. In
the first place, our knowledge of the chemical composition of
brain-substance is still in its infancy. The view that its
characteristic ingredient is the phosphorized nitrogenous body
described in 1865 by Liebreich under the name of protagon
has been strongly controverted by Diaconow, Hoppe-Seyler,
and Thudicum, while recently it has been reaffirmed by
Gamgee and Blakenhorn*. But even should this view turn out
to be well founded, we have yet every thing to learn with regard
to the transformations protagon undergoes during functional
activity, and the nature of the resulting waste products.
Long before Liebreich announced the existence of protagon,
however, the attention of the physiological chemists had been
directed to the prominence of phosphorus as an element in
the composition of the cerebral substance, and it had been
suggested that a part of the phosphoric acid excreted in the
urine might be derived from the metabolism of the brain. As
early as 1846 Bence Jones} had observed an excess of phos-
phatic salts in the urine during certain brain-diseases, notably
acute inflammations ; and an observation published in 1853
by Mosler} appeared to indicate that a similar excess followed
intellectual activity.
Byasson [1868] in his essay on the relation between cere-
bral activity and the composition of the urime§, reports a
number of urinary analyses which support the view that the
excretion of alkaline phosphates by the kidneys is habitually
increased during mental work. ‘This opinion has also received
a certain degree of support from the more recent papers of
Ziilzer || and Stribling{[; nevertheless it is impossible to
* Gamgee, p. 425 et seg. op. cit. supra.
+ Henry Bence Jones, “ On the Variations in the Alkaline and Harthy
Phosphates in Disease,” Phil. Trans. for 1846, p. 449.
t Mosler, “ Beitrige zur Kenntniss der Urinabsonderung,” &c., Inaug.
Diss., cited in Canstatt’s Jahresbericht, 1853, Bd. i. 8. 154.
§ H. Byasson, “Essai sur la relation qui existe a l'état physiologique
entre activité cérébrale et la composition des urines,” Paris, 1868.
|| W. Ziilzer, “ Ueber das Verhiiltniss der Phosphorsiure zum Stick-
stoff im Urin,” Virchow’s Archiy, Bd. lxvi. 1876, 8. 228.
{| Striibling, “ Ueber die Phosphorsiiure im Urin,’ Archiv fur exp,
Path. und Pharm., Bd. vi. 1876-77, 8. 266.
260 Mr. J. J. Woodward on the Modern
study the detailed observations upon which it is based without
feeling how meagre and unsatisfactory the evidence relied
upon really is. It is, at best, only sufficient to indicate the
importance of further inquiry, and to suggest the necessity of
avoiding certain obvious errors of method which complicate
and obscure the results of the investigations hitherto made.
The opinion that mental effort is accompanied by an in-
crease in the temperature of the brain was first propounded
by Lombard in 1867. Using a delicate thermo-electric
apparatus of his own contrivance, he observed during mental
effort a rise of the surface temperature of the head, which
sometimes amounted to as much as one-twentieth of a degree
centigrade*. Subsequent and more elaborate investigations
confirmed him in this conclusion, which has also been supported
by observations made with thermo-piles by Schiff and Bert, as
well as by the use of surface thermometers in the hands of Broca
and L. C. Gray of Brooklynt. Gray claimed to have observed
a maximum rise of as much as two and a half degrees Fahren-
heit. These physicians and some others have also investigated
the relative temperature of the two sides of the head, of diffe-
rent regions on each side, the variations produced in certain
regions by voluntary muscular movements, and those resulting
from localized brain-diseases f.
T'o attempt any discussion of these interesting studies and
their conflicting results would lead me altogether beyond my
prescribed limits. It is enough for my present purpose to
* J.S. Lombard, “ Experiments on the Relation of Heat to Mental
Work,” The New York Medical Journal, vol. v. 1867, p. 199.
+ J.S. Lombard, “ Experimental Researches on the Tdinpardeits of the
Head,” Proc. of the Royal Society of London, vol. xxvii. 1878, p. 166;
Idem, “The Regional Temperature of the Head,” London, 1879; Idem,
“ Experimental Researches on the Temperature of the Head,” London,
1881. Moritz Schiff, “ Recherches sur l’échauffement des nerfs et les
centres nerveux & la suite des irritations sensorielles et sensibles,”
Achives de Physiol. norm. et path. t. iii. 1870, p. 5 et sey. Bert, Com-
munication to the Société de Biologie, read Jan. 18, 1879, in ‘ Gazette
Hebdomadaire,’ Jan. 24, 1879, p. 63. Broca, Communication to the
French Association for the Advancement of the Sciences, at the Havre
meeting of 1877, in Gaz. Hebd., Sept. 7, 1877, p. 577; also Gaz. Méd. de
Paris, 1877, p. 457 ; Idem, in London Med. Record, Jan. 15, 1880. L.C.
Gray, “Cerebral Thermometry,” The New York Med. Journ. vol. xxviii.
1878, p. 31; also ‘Chicago Journ. of Nervous and Mental Diseases,’
yol. vi. 1879, p. 65.
t See, besides the papers cited in the last note, C. K. Mills, in the
New York Med. Record, vol. xiv. 1878, p. 477, and vol. xvi. 1879, p. 130;
Maragliano and Seppelli, ‘ Studies on Cerebral Thermometry in the In-
sane,” translated by J. Workman, ‘The Alienist and Neurologist,’ St.
Louis, Jan. 1880, p. 44 et seg.; R. W. Amidon, “ The Effect of willed
Muscular Movements on the Temperature of the Head,” ‘ Archives of
Medicine,’ April 1880, p. 117.
Philosophical Conceptions of Life. 261
point out that the recent investigations of Francois Frank *
would seem to indicate that the variations of temperature
actually observed are chiefly due to changes in the eerebral cir-
culation. Plunging suitable sounds, connected with a thermo-
electric apparatus, into the brains of animals to different
depths, Frank found that the deeper parts of the brain are
always warmer than its superficial layers. The superficial
layers are continually cooled by radiation, and their tempera-
ture is a degree, or more than a degree, centigrade lower than
that of the deeper parts. Even these, however, are from 1°
to 2° centigrade cooler than the blood in the thoracic aorta ; and
it will therefore readily be understood that a relaxation in the
‘muscular coats of the cerebral vessels, permitting the more
rapid circulation of a larger quantity of blood, would be
promptly followed by an increase in the temperature of the
superficial parts of the brain. None of the observers I have
cited have reported a surface temperature of the head during
mental effort that is too high to be accounted for in this way ;
and if, as I willingly concede is probable, there is really an in-
creased heat-production in the brain itself, it is wholly masked
by the more considerable change due to afflux of blood. |
Now a consideration of the phenomena of blushing, and
certain well-known sensations in the head, might lead us to
expect that emotional and mental conditions would prove to
be attended by increased activity in the circulation of the
blood in the brain; yet many difficulties have hitherto been
encountered in the attempt to demonstrate experimentally that
this is true. Mosso of Turin supposed that he had succeeded
in doing this with his plethysmographt. The instrument is
essentially a cylinder of water, into which the arm is intro-
duced and so fastened in place by a caoutchoue membrane
that the slightest increase or diminution in the volume of the
arm will cause the rise or fall of the water, through a tube
connected at one end with the interior of the cylinder and at
the other with a suitable recording apparatus. The pen or
pencil of this apparatus inscribes a curve that rises or falls
with the fluid in the tube. Among the curious observations
made with this instrument, Mosso reports that the mental
operations and emotions of the persons he experimented on
* Francois Frank, Communication to the Société de Biologie, May 29,
1880, in Gaz. Hebd., June 11, 1880, p. 392.
t+ Angelo Mosso, ‘ Sopra un nuoyo metodo per scrivere i movimenti
dei vasi sanguini nell’ uomo,” Atti della Reale Accademia delle Scienze
di Torino, t. xi., Nov. 14, 1875. Ihave not obtained access to the ori-
ginal, but find an abstract inthe Archives de Phys. norm, et path. 1876,
p- 175. See also Barker, p. 12, op. cit. supra.
262 Mr. J. J. Woodward on the Modern
were accompanied by a fall of the curve, which he regarded
as proof that more blood goes to the brain and less to the arm
during emotion, or mental action, than at other times. But
the following year these observations were repeated with great
care, and with an improved plethysmograph, by Basch, of
Vienna*, who failed to verify them. Most of the phlegmatic
Germans on whom he experimented did sums in their heads,
and otherwise exerted their minds, without producing the
slightest modification of the curve; and none of them appear
to have been as emotional as Dr. Pagliani, of whom Mosso
relates that, his arm being in the plethysmograph, when the
revered Prof. Ludwig entered the room the curve fell as if he
had received an electric shock. Basch has cautiously investi-
gated the causes of the varying quantity of blood in the arm
in these experiments, and has clearly shown how many
general and local conditions concur in producing the result.
Hspecially has he emphasized the effect of variations in the
abdominal circulation, which appear to exercise a much more
considerable influence upon the size of the arm than any
changes that occur in the brain.
In subsequent works Mosso has stated that during mental
effort, such, for example, as is required to multiply small
numbers in the head, the radial pulse, as recorded by the
sphygmograph, is shown to become somewhat more frequent,
and the recerding lever does not rise so high as at other
times}. Thanhoffer, who has pointed out that in these ob-
servations the influence of respiration on the pulse was neg-
lected, concluded, nevertheless, from his own sphygmographie
observations, that after due allowance is made for this com-
plicating influence, it must be conceded that cerebral activity
does exercise a certain effect upon the pulse, and in the direc-
tion statedt{. Kugéne Gley, in a recently published essay,
claims to have obtained similar results, and states that at the
same time the sphygmographic trace of the carotid artery
shows a higher upstroke of the recording lever, and other
indications of dilatation of the vessel§. While these observa-
* Basch, “ Die volumetrische Bestimmung des Blutdrucks am Men-
schen,” Stricker’s Med. Jahrb. 1876, 8. 431. See also Rollet, in Her-
mann’s Handb. der Phys. Bd. iv. Th. 1 (Leipsic, 1880), 8. 306.
+ Mosso, ‘‘ Die Diagnostic des Pulses in Bezug auf die localen Verin-
derungen desselben,” Leipsic, 1879; also by the same, “Sulla circola-
zione del sangue nel cervello dell’ uomo,” Rome, 1880.
{ Thanhofter, ‘“ Der Einfluss der Gehirnthatigkeit auf den Puls,” Pfii-
ger’s Archiv, Bd. xix. 1879, S. 254.
§ Eugéne Gley, “ Essai critique sur les conditions physiologiques de la
pensée. Etat du pouls carotidien pendant le travail intellectuel,’ Ar-
chives de Phys. norm. et path., Sept.-Oct. 1881, p. 741.
Philosophical Conceptions of Life. 263
tions are not sufficiently numerous, or free from objections,
to be accepted without question as proof that an increased
supply of blood to the brain invariably accompanies mental
effort, they are certainly sufficient to encourage further labour
in this interesting field.
But if the arguments in favour of the purely material nature
of our mental operations that have been based upon the im-
perfect results of the three lines of investigation I have just
referred to must be rejected as utterly fallacious, what shall
we say of the logic that attempts to draw a similar conclusion
from the results of those inquiries into the phenomena of
personal equation which aim at determining the time that
must be allowed for the mental operation involved? * Do we,
then, indeed need the beautiful experiments of Hirsch and
Donderst to prove that thought occupies time? Whence,
indeed, do we derive our primitive conceptions of time save
from our consciousness of the succession of thought? And
how could even the shortest time be occupied by even an
infinite number of thoughts if each thought did not occupy at
least some time, however brief ?
I have thus, gentlemen, attempted to show that we are
logically compelled to invoke the existence of a vital principle
in order to account for certain important groups of phenomena
occurring in living beings which cannot possibly be explained
by the chemical and physical forces of the universe. ‘These
phenomena form a series, at one end of which we find the mere
irritability or sensibility of the humblest mass of living pro-
toplasm ; at the other the reasoning faculty of the human
mind. From the one extreme of this series to the other I
recognize the manifestations of the vital principle. I wil-
lingly confess that I know nothing of the ultimate nature of
this principle, except that it must be very different from the
chemical and physical forces whose operations I have learned
to recognize in the organic as well as in the inorganic world ;
nevertheless I am compelled by my study of the phenomena
to conclude that it exists. I know that Mr, Huxley, only
last summer, declared in the International Medical Congress
at London, that the doctrine of a vital principle is the ‘‘ asylum
ignorantie of physiologists ”’{; but this ancient sarcasm has
now been applied to so many things that it has long since lost
whatever sting it may once have possessed, when it was fresh
* Barker, p. 11, op. cit. supra.
+ Hirsch, “ Détermination télégraphique de la différence de longitude
entre les observatoires de Genéve et de Neuchatel,” Genéve et Bale, 1864.
Donders, in Reichert and Du Bois-Reymond’s Archiv, 1868, p. 657.
} T. H. Huxley, “The Connexion of the Biological Sciences with Medi-
cine,” ‘ The Popular Science Monthly,’ October 1881, p. 800,
264 On Modern Philosophical Conceptions of Life.
and new. And [ also know that one of the chief character-
istics of true science is the sharpness with which it enables us
to discriminate between that which we have proven and really
know and that which we have not proven and do not know.
Better far is it, and a thousand times more in accord with the
simple honesty of science, to acknowledge frankly the truth,
that phenomena occur in living beings which the inorganic
forces do not explain, than to mistake our wishes for disco-
veries, to convert conjectures into dogmas, or, worst of all, to
transform an undemonstrated hypothesis into a superstitious,
ageressive, and intolerant creed.
Nor will the soundness of the conclusions at which the
present generation shall arrive as to this matter, be without
its practical effect upon methods of biological research, and
the consequent future progress of biological science. It is
not a mere metaphysical subtlety, but a subject of practical
importance, that I have asked you to consider to-night. For
if the chemico-physical hypothesis of life be true, the only
road of progress in biology lies through the chemical and
physical laboratories. Now, I have already this evening
more than once indicated how highly I esteem the class of
biological work that has already been done in these labora-
tories, and I have endeavoured to show how large is the un-
explored biological field that can be explored only in this
manner. But in addition to all that we can ever hope to do
in this direction—and I insist upon its importance—l insist
also upon the importance of other lines of work: I insist upon
the importance of the systematic study of the phenomena of
growth and development, of generation and heredity, of sen-
sibility and mind. All that can thus be learned we need to
know, and not merely for its own sake. ‘This knowledge is
indispensable to the right interpretation of the succession of
life upon the globe in the past, and the successful direction of
the interference of the human will with the future succession of
life upon the globe in accordance with human necessities.
We shall make slow progress in this direction if we confine
our efforts to the application of chemistry and physics to those
phenomena of living beings that can be thus explained. The
other phenomena, not thus explicable, must also be studied
in detail, arranged into orderly groups, and made the basis of
such inductions as our knowledge of them may warrant. It
is only by pursuing this method that we can hope ultimately
to acquire, with regard to the phenomena of living beings,
that power to predict, which is the criterion of true science,
and that power to control, which we so sorely need.
On Prof. G. Sequenza’s List of Tertiary Polyzoa. 265
XXVITI.—Note on Professor G. Sequenza’s List of Tertiary
Polyzoa from Reggio (Calabria) *. By the Rev. THomas
Hincks, B.A., F.R.S.
WE are indebted to Professor G. Seguenza for a very able
report on the Tertiary formations of Reggio, which includes
a list of the Polyzoa found in the various beds of the district.
Many species supposed to be new are described and illustrated
by excellent figures. Amongst these are a number of forms
that seem to me to have been raised to specific rank on very
insufficient grounds ; and as the maintenance of false species
is clearly an injury to science, I venture to submit this portion
of Prof. Seguenza’s work to some critical revision.
Lepralia elegantissima, Seguenza (p. 83, pl. vii. fig. 11).
This is undoubtedly referable to Cribrilina radiata, Moll,
form ¢nnominata, Couch. The species is a variable one; but
Seguenza’s Miocene form does not depart in any essential point
from the type. It agrees very closely with the Pliocene Lepralia
innominata of Manzoni (Sitz. d. K. Akad. d. Wiss. in Wien, lix.
Bd. i. Abth. Jiin.-Heft, 1869, pl. ii. fig. 13), The characters
relied upon by Seguenza as distinctive (absence of avicularia,
free development of ocecia, &c.) are quite insignificant. He
remarks that L. e/egantissima is most nearly allied to L. radi-
ata and L. figularis, and more especially to the Floridan form
of the latter . This form, however, is not the true jigularis,
but merely a variety of radiata to which I have no doubt
elegantissima also must be referred.
Lepralia radiato-foveolata, Seguenza (p. 129, pl. xii. fig. 20).
Identical with Microporella violacea, Johnston. There is
perfect agreement with the latter species in all the essential
characters, and even the superficial sculpture has a very exact
parallel in the Crag form of JZ. violacea, which I have de-
scribed in my ‘ History of British Marine Polyzoa’ (p. 218,
pl. xxx. fig. 4) f.
Cumulipora porosa, Seguenza (p. 130, pl. xu. fig. 21).
Not distinguishable from the well-known Smittia trispinosa,
* Contained in his valuable work entitled “ Le formazioni terziarie nella
provincia di Reggio (Calabria).” Memoria del Prof. G. Seguenza, ‘ Atti
della R. Accademia dei Lincei,’ 1879-80, serie terza, vol. vi. (physical
science class), 1880,
+ Smitt, ‘Floridan Bryozoa, pt. 2, pl. v. fig. 112.
t See also woodcut, fig. 12, on p. 219 of the same work,
Ann. & Mag. N. Hist. Ser. 5. Vol. xii. 18
266 On Prof. G. Sequenza’s List of Tertiary Polyzoa.
Johnston. The oval and pointed avicularia, which are so
characteristic of the species, are noted, and the pore, which is
usually present on the front of the ocecium, is represented in
the figure. The granulose condition of the surface is often
met with in old specimens.
Lepralia radiato-porosa, Seguenza (p. 129, pl. xii. fig. 19).
A mere variety of Schizoporella unicornis, Johnston (in-
cluding ZL. ansata, Johnston). ‘The only characters noticed as
distinctive are a larger number of radiating lines of pores than
usual and a more prominent central umbo. Such slight super-
ficial differences are without any special significance amongst
the Polyzoa. ‘The size of the umbo is one of the most vari-
able characters.
Lepralia eximia, Seguenza (p. 203, pl. xiv. fig. 238).
There can be little doubt, I think, that this is identical with
Membraniporella nitida, Johnston. So far as I know, the
species has not previously been recorded asa fossil. Its range
in time is now extended to the Pliocene period.
Lepralia Calabra, Seguenza (p. 201, pl. xv. fig. 6).
Undoubtedly a form of the protean Aicroporella ciliata,
Pallas. In this species there is the greatest possible diversity
in the size of the cells; the present seems to be a somewhat
diminutive variety. Altogether this Phocene form exhibits a
very small amount of divergence from the type as compared
with many of the known varieties; the specific facies is
strongly marked in it. J/. ciliata is as variable as it is cos-
mopolitan.
Lepralia mitrata, Seguenza (p. 203, pl. xv. fig. 8).
Referable to Cribrilina radiata, Moll, form c¢nnominata.
The large size of the cells, the small number of prominent
radiating ridges, the depth of the dividing furrows, giving a
strongly crenate appearance to the margin, the papillose
oceciuin, ail these are well known as occasional conditions
amongst the many varieties of this variable form. They
have none of them any specific value, as the study of any
large series of specimens will abundantly show.
Lepralia coronata, Seguenza (p. 295, pl. xvii. fig. 6).
A variety of Microporella Malusti, Audouin, chiefly re-
markable for the curiously furrowed surface of the ocecium,
Mr. J.J. Quelch on some Stylasteride. 267
a peculiarity of the superficial calcification which has no special
significance. ‘The shape and basal areolation of the ovicell
as well as all the characters of the cell in the Pliocene speci-
men are thoroughly typical.
Lepralia thiara, Seguenza (p. 370, pl. xvii. fig. 57).
= Cribrilina punctata, of very normal character. Pliocene
and Quaternary.
Salicornaria mammillata, Seguenza (p. 294, pl. xvii. fig. 5).
Probably a species of Myrtozouwm; it is certainly not refer-
able to Salicornaria (Cellaria).
Professor Séguenza’s work is of such sterling character and
will deservedly have so much weight with the student that it
seems peculiarly desirable to prevent these spurious species,
if possible, from sheltering themselves under its authority.
| XXIX.— On some Stylasteride. By Joun J. QUELCH. <
To the Editors of the Annals and Magazine of Natural History.
GENTLEMEN,—In reply to the letter of Mr. Bryce Wright, I
must first point out that one ef the species of Déstichopora
to which | referred as having been omitted from his list was
the D. gracilis, Dana, the only species of D¢stichopora that
bears Dana’s name. ‘This was accidentally referred to in my
paper as D. fragilis. of
Mr. Wright states that he did not say that D. nitida, V.,
was of a whitish tint: I might reply, using his mode of ex-
pression, that I did not say that he sazd so; Isaid he cndicated
it; and to justify my statement I quote the following from Mr,
Wright’s original paper :—“ the habitats of the living species
being the Gulf-stream and in and about the West-India
Islands and Florida, for D. nitida, Verrill, and D. cervina,
D. foliacea, D. sulcata, D. barbadiensis, and D. contorta ot
Pourtales. Most of these species are of a whitish tint, with
the exception of D. foliacea, which is a pale pink-orange,
whereas those inhabiting the Pacific are much more vivid in
their colours.” I leave it to the judgment of any competent
impartial person to decide whether I have misinterpreted Mr,
Wright’s words or not.
S 18*
268 Mr. J. J. Quelch on some Stylasteride.
Believing, as Mr. Wright did, that D. nitida, V., was
of a whitish tint, and that it was found in the West-Indian
fauna, he could im all good faith describe Lady Brassey’s very
large and beautiful specimen as new ; but as it happens that
D. nitida has the same coloration as this specimen, varying
from a bright red to light orange, agrees with it in its other essen-
tial features, and comes from very nearly the same locality in
the Pacific, the specific name he has proposed cannot stand.
The specimen is decidedly a typical example of Verrill’s
species.
Mr. Wright says, “D. nitida of Verrill, as judged by the
Museum examples, it certainly is not.” It 1s strange that
Mr. Wright should have taken as his standard of comparison
specimens doubtfully referable to Verrill’s spectes—specimens
which, as he himself remarks in his letter, have a query (?)
appended to their names. His method of identification,
which thus neglects the description itself of the species, is
certainly peculiar.
I may point out again that the variation in the colours of
different specimens of D, nitida, as described by Verrill, is
remarkable; and the fine examples collected by Lady Brassey,
as shown in the description and plates that have been given
f them, are wanting in characters by which to separate them
ee rs . than those of the very variable differences in the shades
st “ ey AVS, saan ih ac os
therences Ww aTU 135-SUCn.-as one
a
an oy
described by
Hnet from one another
remarks on ‘Tenison-Woods’ species.
In reply to Mr. Wright’s note of exclamation, Imay say that
it really does not seem necessary to explain why, in appending
a query to the names of specimens which, in the present state
of knowledge, seem to be divergent and, perhaps, even doubtful
forms of the species, I regard such a course as preferable to
publishing them as new, or to labelling them definitely with
ihe name of a species of which they cannot be regarded as
typical examples, and from which, on further knowledge,
they may have to be separated.
Lastly, 1 must say that I regret extremely to have to seem
lacking in courtesy to the distinguished lady after whom one
The Branched and Unbranched Freshwater Sponges. 269
of the species was named by pointing out that the species can-
not stand ; but all true workers in natural history, who know
the extreme difficulty of a complicated synonymy, will recog-
nize the absolute necessity of preventing such complication in
all cases where it is possible.
I am, Gentlemen,
Yours obediently,
JOHN J. QUELCH.
XXX.—The Branched and Unbranched Forms of the
Freshwater. Sponges considered generally. By H. J.
Carter, F.R.S. &e.
ACCORDING to my own actual experience as well as that of
others, there are two distinct forms assumed by the freshwater
sponges of England, viz. one stipitate, long-branched, and of
a brown colour, and the other sessile, spreading, unbranched,
and of a light fawn-colour when dry. The former has been
called “ Spongilla lacustris,” and the latter “ Spongilla flu-
viatilis ;” but as they both grow in still as well as running
water (that is, in lakes and docks as well as rivers) they
were more or less confounded, until Lieberkiihn definitively
settled the differences between them, by pointing out that the
former was characterized by the presence of a little, spined,
curved acerate; and the latter by an amphidisk or birotulate
spicule.
That the branched species was recognized as such by the
earliest authority on Spongilla, viz. Plukenet, in 1696, is
known by his having used the term “ ramosissima”’ in his
description (‘ Almagestum Botanicum,’ p. 356); while Lamarck,
in 1816 (An. sans Vertébres, t. 11. p. 100), changed this to
“amosa,”’ instancing at the same time Plukenet’s represen-
tation “ t. 112. fig. 3,” and Hsper’s “t. 234” as illustra-
tions of the species. Hsper’s “ tab. 23” represents undoubt-
edly, under the name of ‘‘ Spongia lacustris,” the branched
form of the freshwater sponge which we call ‘ Spongilla
lacustris” at the present day. .
It is true that Lamouroux, in 1816 (‘ Hist. des Polypiers
flexibles,’ Engl. transl. 1824, p. 147), introduced the name
“ Ephydatia” (épvddtios, of the water) for the freshwater
sponges; but as Lamarck used that of ‘‘ Spongilla” about
the same time for the same organisms in his ‘ Hist. des An,
sans Vertébres,’ without any allusion to Lamouroux’s term,
270 Mr. H. J. Carter on the Branched and
it may fairly be assumed that when the second volume of this
great work was priuted (viz. in the month of March 1816),
Lamouroux’s appellation had not been generally accepted, if,
indeed, known or published.
Clear, however, as all this would appear to be, the confu-
sion to which I have alluded extends down to 1842, when
Johnston published his work on the ‘ British Sponges,’
wherein he not only puts Esper’s representation under his
“ Spongilla fluviatilis” (p. 159), but in his diagnosis of .
Spongilla lacustris never mentions any thing about branching ;
while the printed report of the “ Joint Standing Committee
on the Impurity of the Boston Water-supply”’ (Document
143—1881) contains an excellent illustration of the branched
freshwater sponge of North America (viz. Spongilla lacus-
trioides, Potts), under which is the name “ Spongilla fluvia-
telis.”” How far this may be owing to Johnston’s mistake,
which obtains in Ads illustration (pl. xviii.), as well as in his
description, I am not able to say.
So much for the branched forms of the freshwater sponges
ot Kurope and the United States. We have now to add
Uruguaya coraltioides from South America, and Lubomirskia
baicalensis from Lake Baikal, in Central Asia, all the rest
being, so far as I know, unbranched, sessile, spreading, plane, -
lobate, or rendered irregular on the surface by more or less
projecting processes, but not all fawn-colour.
As regards Spongilla lacusiris, Dr. W. Dybowski (Mém.
de l’Acad. Imp. d. Sc. St. Pétersbourg, 1882, t. xxx. no. 10,
pp. 6, 7) not only enumerates seventeen places in Russia
where it has been found, but includes among them the ‘‘ Pacha-
bicha-See,” at the S.W. extremity of Lake Baikal, from
whence his brother brought back a branched (‘ baumférmige’’)
specimen charged with statoblasts (“‘ gemmule ”’); at the same
time that he brought back the branched specimen of Spongia
baicalensis, Pallas, which Dr. Dybowski has described, repre-
sented, and made the type of a new genus under the name of
“ Lubomirskia,” calling the species “ L. baicalensis”’ (op. cit.
1880, t. xxvu. p. 11, Taf. 1. fig. 1), in which he found no
statoblasts (“ Gemmule habe ich niemals gefunden,” p. 16),
any more than in any of his sessile species of this genus and
their varieties (op. et loc. cit.).
It is worthy of remark, however, that where the specimen
of Spongilla lacustris was found, another species, which he
has described, illustrated, and named “ Spongilla sibirica”
(op. cit. t.xxx. no. 10, p. 10), was obtained bearing statoblasts,
‘seeing that it is identical with that obtained from the Schuyl-
kill River, in Pennsylvania, by Prof. Leidy, and named by
Unbranched Forms of the Freshwater Sponges. 271
him “ Spongilla fragilis ;” as also by the late Mr. J. K. Lord at
Lake Osogoos, in the Cascade Mountains of British Columbia,
but hitherto in no other part of the world. That Spongilla
sibirica is Spongilla fragilis, Leidy, is not only shown by the
description, but confirmed by the characteristic, polygonal cell-
structure among the statoblast spicules represented in the illus-
trations (Taf. i. figs. 12 @ and 12 5).
Then as regards Uruguaya corallioides, 1 have before
stated that, under the most careful examination of several
large specimens not a trace of a statoblast has as yet been
found, so that (also as before stated) it becomes questionable
whether it is ever propagated by statoblasts or not, seeing
that the sexual as well as the statoblast means may take place
in Spongilla, as pointed out by Lieberkiihn in his Spongilla
erinaceus, so far back as 1856 (Archiv f. Anat. Physiologie
&e. Heft iv. p. 405, Taf. xv.).
Unfortunately, I have nothing but dried specimens of Uru-
guaya corallioides in my possession, so have been obliged to
have recourse to an indirect method of examining the sarcodic
parts under the microscope, which, however, has yielded much
more than might have been expected ; for by softening minute
fragments of the interior of a branch from two different speci-
mens, through placing them for a few hours in liquor potasse,
and then, after they have been washed, examining them under
a microscope, the sarcode is found to be abundantly charged
with spherical cells of a light brown colour, which are granu-
liferous and nucleated, together with others that are less
round. ‘These, when the fragments have been stained with
magenta-dye (red ink), become much more deeply coloured
than the other parts of the sarcode, and after having been
washed in water and mounted in glycerine, afford a prepara-
tion which can be deliberately examined at any time.
The granulifero-nucleated cells in their sharply delineated
spherical form are from 3- to 4-6000ths inch in diameter,
which being much larger than the spongozoa (“Geisselzellen”’),
and much smaller than the ampullaceous sacs (“Geisselkam-
mern”), both of which are also present for comparison, shows
that the former are spermatic cells or young ova, or both
mixed together ; but here the analysis ends for want of a wet-
preserved specimen or more matured ova, if there be any
present.
It is not improbable that hereafter Uruguaya corallioides
may be found to propagate itself by ova alone ; but then this
can only be determined by inference, since Lieberkiihn, as just
mentioned, has shown that the freshwater sponges may be
propagated by ova or statoblasts.
272 The Branched and Unbranched Freshwater Sponges.
Lastly, there is the inference that these granuliferous cells
(for the granules are very large, spherical, and sharply de-
fined) may be spermatic alone, and that Uruguaya corallioides
may be nothing more than the male of a dicecious sponge ;
while it then becomes questionable whether a male form pro-
duces any statoblasts.
Miklucho-Maclay has long since given a series of illus-
trations (Mém. de l’Acad. Imp. de Se. St. Pétersbourg, 1870,
t. xv. no. 3, p. 1, Taf. 1), in which we find Pallas’s Spongia
baicalensis again represented (fig. 5); but here under the
name of “ Veluspa polymorpha, var. baicalensis” (p. 8), as
derived from the marine form Spongia oculata, Pallas,
of 1766,= Chalina oculata, Bk., of 1866, and the typical ex-
ample of my order Rhaphidonemata ; but although the least
like of the branched freshwater sponges to Chalina oculata
is Spongilla lacustris, it comes nearest in the form of its
spicule, which is acerate, smooth, curved, fusiform, and sharp-
pointed in both ; while in Lubomirskia baicalensis it is spined,
and in Uruguaya corallictdes not only microspined but much
curved, cylindrical, and round at the ends. On the other
hand, in the general form of the sponges themselves it is
almost impossible to be more like Chalina oculata than are
Uruguaya corallioides and Lubomirskia baicalensis.
Still it is not what a sponge may have been, but what it
as, that the student should chiefly concern himself about, and
then it will be found inconvenient to put sponges bearing
statoblasts with those which have none; hence my family
Potamospongida is provisionally placed by itself at the
end of my order Holorhaphidota, to which in texture Spon-
gilla otherwise belongs. The typical form of the spicule
in the Rhaphidonemata, just described, is identical with
that of the Renierida, which is the first family of my
Holorhaphidota ; but the main support of the fibre in the
former is the horny investment, while in the latter it is the
axial core of spicules; thus the Rhaphidonemata are resilient
and the Holorhaphidota may be crushed.
P.S.—Since the above was written, I have received (15th
March) a packet from Dr. W. Dybowski (Niankow, near
Novogrodek, in Minsk), in which he has kindly sent me
copies respectively of his paper on the freshwater sponges of
Russia, in the thirty-ninth vol. of the Imp. Acad. of Sc. above
mentioned ; of a notice of others sent to him by Prof. P. T.
Stephanow, of the University of Kharkow, which he communi-
cated to the Natural History Society of Dorpat in February
1883, among which is a new species from a little lake called
Mr. A. G. Butler on new Lepidoptera. 273
“ Wielikce,” in the district of Lebeden, near Kharkow, for
which he proposes the name of ‘“Dostlia Stephanowti ;” and,
lastly, an illustrated copy of a description in Russian of this
species &e., printed at Kharkow in 1884.
From the spicular illustrations of Dosilia Stephanowii in
the latter (t. vil. fig. 1, a—-d, which are neatly executed) it is
evident that this species is closely allied to the mounted speci-
men of Heteromeyenia repens, Potts, which the latter kindly
sent me, as the only exceptions are that the teeth of the disks
in the birotules are not so claw-like or recurved, and the
long spines of the flesh-spicules not inflated at the extremities,
as in /T. repens; but there are the same sparsely-spined
skeletal spicules to be seen in both instances.
Thus another species of freshwater sponge analogous to
Meyenia plumosa of Bombay and Heteromeyenia repens of
Pennsylvania, if not to M/. Bazleyt also, has been found in
Europe (¢. e. in Southern Russia). As the skeletal spicule
of M. Baileyi is not stated by Dr. Bowerbank to be spined,
and the illustration is smooth (Proc. Zool. Soc. Nov. 1863,
p- 13, pl. xxxvin. fig. 6, a), I cannot confidently affirm
that in this respect also ¢# accorded with that of Dosilia
Stephanowtt. In Mr. Potts’s mounted specimen of Hetero-
meyenia repens (? Meyenia Baileyi) there are smooth as well
as sparsely spined skeletal spicules present. Unfortunately
there only exist the slides (three) of MZ. Bacley? in the British
Museum for comparison ; but this object has just (20th March,
1884) been kindly effected for me by Mr. 8. O. Ridley, F.L.S.,
of the British Museum, who concludes his statement as fol-
lows, viz.: —‘‘ The specimens are nearly related, but, at the
same time, it is not difficult to separate them under the micro-
scope ;’’ while I gather from the rest of his letter that the
differences are hardly sufficient to constitute even a variety ;
hence it may be considered that Mr. Potts’s and my conjec-
tures respecung the identity of Meyenia (Spongilla, Bk.)
Baileyt and Heteroneyenia repens are correct.
XXXI.—Deseriptions of five new Species of Heterocerous
Lepidoptera from Yesso. By ArruurG. Butter, F.L.S.,
¥.Z.8., &e.
Tne following species were recently selected from a collection
sent home by Mr. Henry Pryer :—
274 Mr. A. G. Butler on new
Lithosiide.
1. Nola gigas, sp. nov.
Belongs to the N.-strigula group, but is more nearly allied
to N. fumosa; smoky grey, the primaries paler than the
secondaries, but densely irrorated with grey scales, and glossy ;
the lines much less distinct than in N. strigula, the spots on
the fringe less defined; the embossed spots on the discoidal
area strongly marked ; base of costal area blackish. Expanse
of wings 34 millim.
Yesso.
Possibly allied to N. gigantula of Staudinger from Asia
Minor ; but the description of that species states that the lines
across the primaries are more distinct than in N. sérigula,
the reverse being the case in the present species.
Acontiide.
2. Chasmina atrata, sp. nov.
Nearest to C. nervosa, of the same size, but the wings dark
bronze-brown, with the base of primaries, excepting at costa,
and the interno-basal area of secondaries snow-white, slightly
opaline ; fringe with the basal half grey and the external half
white: body snow-white, antenne dark brown. Wings below
nearly as above, but the basal half of primaries irrorated with
white in continuation of the white basal area of the upper
surface ; the basal half of costal border of secondaries white,
and the centre of the wing irrorated with white scales: body
below white; under surface of antennee and proboscis casta-
neous. Expanse of wings 27 millim.
Yesso.
This species can be at once identified by its coloration, all
the forms hitherto recorded being snow-white, C. nervosa only
having the veins brownish.
Hypogrammide.
3. Gerbatha pseudodyops, sp. nov.
Nearly resembles the New-World Dyops ocellata in general
coloration ; agrees in the position and outline of its markings
with Xylophasia scolopacina, with which I should have con-
sidered it congeneric but for its more slender body and smaller
palpi; the general coloration of the primaries is slaty grey,
) lei
Lepidoptera from Yesso. 275
spotted here and there with rust-red, the external area with
cupreous reflections; the ordinary lines black, with white
margins, better defined in some specimens than in others ;
ordinary discoidal spots edged with ash-grey or white and
black; costal area irrorated with ash-grey scales; a pale
irregularly undulated submarginal stripe, bounded internally
near the costa and interrupted in the middle by sagittate black
spots; a marginal series of depressed black spots; fringe
brown, traversed by a darker stripe: secondaries fuliginous
brown, with faint golden reflections; fringe whity brown,
traversed by a blackish line: thorax brown, black-speckled ; —
abdomen greyish brown, sericeous ; anal tuft whity brown,
with two black patches above. Primaries below greyish
brown, glossed with cupreous, paler towards the external and
internal borders; two parallel diffused irregular dusky discal
stripes: secondaries whitish, with the apical half densely
irrorated with rosy brown; a dark brown discocellular spot,
an angulated discal stripe, and an abbreviated dash beyond
the latter towards apex: body below whitish; legs brown-
et tarsi barred with black. Expanse of wings 36
millim.
& @. Yesso.
Boarmiide.
4. Tephrosia excellens, sp. nov.
Nearly allied to 7. crepuscularia, but about one third larger
in every respect, less yellow in tint; the male greyer, with
less strongly ciliated antenne. Expanse of wings, ¢ 51
millim., 2 58 millim.
Yesso.
Larentiide.
5. Scotosia corrugata, sp. nov.
Most like 8. wndulata; whity brown or sordid white ; the
primaries crossed by eleven to thirteen undulated parallel
grey-brown stripes, two of which are darker, to indicate the
central belt; a pale greyish submarginal band ; basal half of
secondaries crossed by four parallel grey-brown bands, fol-
lowed by three parallel undulated stripes; a pale greyish
submarginal band: markings below very indistinct, only indi-
cated here and there. Expanse of wings, ¢ 32, ¢ 34
miilim.
Yesso,
276 Mr. C. O. Waterhouse on
Although I have referred this species to Scotosta, this action
is but tentative; like nearly all the large genera of moths,
Scotosia will have to be subdivided, and the form of the wings
(especially of the primaries *) in the male of this species will
then probably entitle it to rank as a distinct genus.
XXXII. — Coleoptera collected during the EHapedition of
H.M.S. ‘ Challenger.’ By CHARLES O. WATERHOUSE.
THE present paper has reference only to the Coleoptera col-
lected at Tristan d’Acunha, Ki Dulan, Aru Islands, and
Tahiti.
TRISTAN D’ACUNHA.
Carmichael, in his “ Description of Tristan da Cunha”
(Tr. Linn. Soe. xii. pp. 497-8), says, “‘ The only insects I ob-
served are three small species of Curculio, four Phalena, one
Hippobosca, two of Musca, one of Tipula.”
Probably the Curculionide referred to may be those de-
scribed below as Palechthus and Pentarthrum.
Lancetes varius, Faby.
Hab. Inaccessible Island.
The eight specimens received are a trifle longer and nar-
rower than the Chilian specimens; they have the anterior
margin of the thorax pitchy, and the fuscous spot at the base
extends beyond the middle of the thorax. The sterna and
posterior coxe are pale. All the Chilian specimens in the
Museum collection have the sterna and coxe blackish, and
the fuscous marks on the thorax, when present at all, are
very small. The Fabrician type from Patagonia has the
thorax entirely yellow as well as the sterna and _ posterior
coxe. Babington’s types, described as Colymbetes nigro-
rematus, from Port Famine and Port Desire, have scarcely
any trace of the spots on the thorax, but have the sterna and
coxee black. Mr. Sharpe, in his monograph of the Dytiscide
(Sci. Tr. R. Dublin Soc. 1. 1880-2, p. 604), under Lancetes
premorsus (the name he adopts for the species) gives Bolivia
and Monte Video as additional localities,
Cercyon littorale, Gyll.
Hab. Ynaccessible Island.
Two examples agreeing with Kuropean specimens.
* The male primaries are formed as in the genus Chesvas,
‘ Challenger’ Coleoptera. 277
Quedius fulgidus, Fabr.
Hab. Nightingale Island.
Numerous specimens agreeing perfectly with Huropean
examples. This species has occurred in very remote parts of
the world.
PALACHTHUS, n. gen.
General characters of Hrirrhinus, but with the third joint
of the tarsi scarcely broader than the preceding, &c. Rostrum
about the length of the thorax, rather stout, slightly curved, a
little narrowed to the apex; the antennal scrobe commencing
near the apex, extending to the eye, deep, bounded above by
a ridge. Antenne long, moderately slender; scape a little
enlarged towards the apex; first joint of the funiculus about
twice as long as broad; the second joint a little longer, the
third to seventh subglobose ; club ovate, the first joint smooth
and shining. LKyes not large, not prominent, transversely
ovate, a little simuate anteriorly for the antennal scrobe,
Thorax a little longer than broad, subparallel, a little nar-
rowed at the base, rather more so in front, moderately flat-
tened, with surface even; anterior margin slightly sinuate
behind the eye; the anterior margin of the prosternum emar-
ginate. Scutellum very small, elongate. Llytra at the base
a little broader than the thorax, narrowed at the apex, arched
posteriorly, the sides nearly perpendicularly ; punctate-striate,
the surface even, setose. Legs moderate. Anterior cox
very prominent, contiguous; intermediate coxe globular,
prominent, separated by a narrow process; posterior cox
transversely ovate. Femora moderately enlarged in the
middle. ‘Tibi bisinuate on the inner side; the outer apical
angle obliquely rounded ; the mucro distinct, especially to the
anterior tibia. ‘T'arsi moderately long and narrow, densely
pilose below, the first, second, and third joints subequal in
length ; the third scarcely wider than the preceding, scarcely
bilobed, with only a narrow incision at the apex visible from
below ; claws free. Metasternum very short, impressed pos-
teriorly ; parapleura extremely narrow. Abdomen with the
divisions between the basal segments effaced (except close to
the side), these segments concave; the intermediate segments
very short, separated by very deep incisions.
The general form of the larger of the two species for which
I propose this genus is somewhat that of Hrirrhinus macu-
latus, but with a longer thorax, not narrowed at its base.
The smaller species is rather more depressed.
278 Mr. C. O. Waterhouse on
Palechthus glabratus, 0. sp.
Elongatus, fusiformis, convexus, glaber, piceus; capite rostroque
erebre subtiliter punctulatis ; thorace latitudine paulo longiori,
nitido, crebre evidenter punctato, basi medio impressa ; elytris
thorace paulo latioribus post medium gradatim arcuatim angus-
tatis, nitidis, striatis, striis punctatis, interstitiis perparum con-
vexis, subtiliter coriaceis, dimidio apicali fulvo-hirto; metasterno
subtiliter (latera versus obsolete) punctulato, parapleuris angus-
tissimis; pedibus punctatis, fulvo-pubescentibus, tibiis sat as-
peratis.
Long. (rostr. excl.) 12 millim., lat. 43 millim.
The rostrum has a fine, smooth, raised line, commencing at
around fovea which is between the eyes and extending to
the apex. ‘The eyes are distinctly narrowed below. ‘The
thorax is scarcely arcuate at the sides, shghtly narrowed from
near the base to the front, and also at the extreme base.
The elytra have the shoulders obliquely rounded off with a
slight impression above; the strie are distinct posteriorly,
but at the base are only represented by lines of fine punc-
tures. he pubescence is stiff and dense at the apical decli-
vity, particularly on the suture, and forms a slight tuft at the
apex of the fourth stria.
Hab. Nightingale Island (Oct. 17, 1873).
Three examples. Probably the pubescence would be found
in fresh examples to exist, to a small extent, on the thorax
and base of the elytra.
Palachthus cossonoides, n. sp.
Elongatus, subparallelus, depressiusculus, pallide piceus, parce flavo-
setosus ; thorace fere parallelo, ad apicem ipsum angustato, crebre
evidenter punctato, depresso ; elytris ad apicem arcuatim angus-
tatis, leviter striato-punctatis, interstitiis parum nitidis, punctis
parvis setigeris sat discretis seriatim dispositis.
Long. (rostr. excl.) 73 millim., lat. 24 millim.
Much more depressed than the foregoing species, and more
parallel in outline. The rostrum is relatively a little shorter
(a little shorter than the thorax), only very slightly arched,
the punctuation obscure and confused, the fovea between the
eyes almost wanting. The thorax is more parallel, only nar-
rowed just before the apex and at the extreme base; with no
dorsal impression. ‘The elytra are more depressed, and conse-
quently the posterior declivity is more gradual; the strie are
represented by lines of fine (generally elongate) punctures ;
the pubescence is more sparse and more equally distributed.
Hab. Nightingale Island. A single example.
Vs Vitibe st.
‘Challenger’ Coleoptera. 279
Pentarthrum Carmichaeli, un. sp.
Statura fere P, Huttoni, minus nitidum, pallide piceum, aureo-pubes-
cens; rostro paulo longiori, thorace lateribus postice magis rotun-
datis, creberrime punctato ; elytris fortiter striatis, striis confertim
evidenter punctatis, interstitiis convexis, seriatim punctatis.
Long. (rostr. excl.) 33 millim., lat. 1 millim.
The rostrum a little longer than in P. Huttoni, nearly
parallel, rather dull, finely and rather closely punctured at the
base, the punctuation beyond the middle excessively fine and
longitudinally confluent. Eyes moderately prominent. An-
tenn rather short and stout, beset with long hairs; funiculus
5-jointed, the first joint a trifle longer than broad, narrowed
at the base, the second as long as the first; the third, fourth,
and fifth shorter, subequal; the club elongate-ovate, pilose.
Thorax moderately flattened, the surface finely coriaceous,
very thickly and moderately strongly punctured, broadest at
one third from the base, narrowed in front and at the base,
the sides distinctly rounded. Scutellum small and rounded.
Elytra at the base not quite so broad as the broadest part of
the thorax, somewhat flattened, parallel, arcuately narrowed
at the apex, strongly striated, the strie closely and mode-
rately strongly punctured, the punctures rather transverse ;
the interstices convex, each with a single irregular line of
small punctures; all the punctures bear golden hairs, which
have a slight greenish tint in some lights. Tarsi short and
stout; the third joint broad and excavated nearly as in P.
Huttoni, not bilobed.
Hab. Inaccessible Island. Several examples.
KI DULAN.
Leptochirus samoensis, Blanch.
A single example, which appears to be referable to this
species.
Aceraius Germari, Kaup.
Many examples. ‘The specimens in the Museum collection
are from Ki Island and Aru Island.
Pelops * gularis, n. sp.
Niger, nitidissimus; elytris punctato-striatis; interstitiis parum
convexis; gula parum nitida; processu prosternali postice sat
* Kaup, Berlin. ent. Zeit. xv. (Mon, Passalidz), p. 37.
280 Mr. C. O. Waterhouse on
convexo, opaco; metasterni lateribus late confertim ruguloso-
punctatis, basi utrinque punctis nonnullis impressa.
Long. 21 lin.
This species is very close to P. Salamonis, Kaup (Berl. ent.
Zeit. xv. p. 389), but a little smaller. Labrum beset with
reddish hairs, sparingly and strongly punctured, deepl
emarginate, the left lobe a little the longer. Middle of the
epistoma considerably produced forwards, with a deep quad-
rangular emargination. ‘Thorax moderately convex, smooth,
with scarcely any trace of the middle line; the later al i impres-
sion is oblique and not very deep, smooth; at the anterior
angles there are a few punctures. Llytra with the striz
rather deeply impressed ; the punctures in the sutural stria
are scarcely visible, but in each stria the punctures are
more distinct as the sides are approached; the © punc-
tures in the lateral striz are deep, very close together, and
transverse; in P. Salamonis these punctures are scarcely
transverse, and are more distinctly separated from each other.
The middle portion of the gula is smooth, semicircular in
outline, gently convex, slightly opaque on each side, not im-
pressed on each side of the base, as it is in P, Salamonis.
The prosternal process is somewhat dull posteriorly, sub-
parallel, moderately convex, and not flattened at the apex, as
it is in P. Salamonis. The sides of the metasternum are
densely and finely rugulose and opaque, and on each side of
the base there are some rather strong punctures as in P
Salamonis.
A single example.
Pecilopharis truncatipennis, Ritsema.
A single specimen. ‘This species is described (Notes
Leyden Mus. 11. 1881, p. 1) trom a male from the Aru
Islands.
The following more or less widely distributed species were
also met with :—Hupholus Linnei, Th. (1); nee granu-
latus, Fabr. (2) ; Sphenophorus obscurus, Boisd. (1) ; Chloro-
phanus annularis, Fabr. (1) 5 Aulacophora rubrozonata, Boisd.
(1). Alsoa single specimen of the genus Praonetha which I
am unable to determine.
ARU ISLANDS (Wokam, Dobbo, and Wanumbar).
The following is a list of the species met with in these
islands :—
Therates labiatus, Fabr.; Tricondyla aptera, Oliv.; Rho-
pea aruensis, Lansb. ; Anomala aenetventris, Fairm. ; ; Cautires
‘Challenger’ Coleoptera. 281
amabilis, n. sp. ; Metriorrhynchus cinctus, Waterh.; Trichalus
flavicans, Waterh.; Spherarthrum (n. gen.) preeustum, Guérin ;
Lagria pulchelia, Guérm ; Eupholus Linnei, Th.; Oeleuthes
cinerascens, Blanch. ; Isomerinthus tessellatus, Bl. ; Aleédes
albolituratus, Bl.; Paipalesomus dealbatus, Boisd.; Acalles
pallens, Bl. ; Miolispa suturalis, Pascoe; Ithystenus frontalis,
Pascoe ; Tmesisternus marmoratus, Guérin ; Rhiparida nigro-
cenea, Baly ; Stethotes lateralis, Baly; Hsernia magnifica,
Baly ; Galleruca, sp.; Aspidomorpha punctum, Fabr.
The following is a description of the new species of Lycides
mentioned above as Cautires amabilis :—
Cautires amabilis, n. sp.
Niger; thorace elytrisque ochraceis, his apice nigris. 6,
Long. 6 lin., lat. 14 lin,
Eyes large and prominent. Antenne moderately long;
the first joint rather large, the second small and partially
hidden by the first, the third about ? millimetre long, with
a rather narrow branch 3 millimetres long arising from the
extreme base of the joint, the branch pilose; the fourth to
eleventh joints each a trifle longer than the preceding, the
branch proportionally longer, the apical joint long, flat, a
little narrowed at the apex. Thorax rather broad, quadrangu-
lar, clothed with yellowish-red silky pile, the middle of the
anterior margin somewhat produced, reflexed, and thickened ;
the sides reflexed ; the discoidal areolet moderately broad in
front of the middle, extending to the basal margin, united to
the anterior incrassate margin by a short costa; there is a
slight costa on each side, arismg from the median areolet
rather in front of the middle, and extended to the side of the
thorax ; the two anterior median areolets are but faintly indi-
cated. Scutellum oblong, emarginate at the apex. Llytra
long, parallel, each with nine coste, the second, fourth, and
sixth distinctly stronger than the others; the intervals with
lines of strong, generally slightly transverse punctures; the
apical fifth blackish.
This species has much the appearance of some species of
Metriorrhynchus trom Australia (e. g. MZ. abdominalis, W.).
The following is the description of the new genus of
Telephoridee mentioned above :—
SPHARARTHRUM, nh. gen.
I propose this name tor a small ‘l’elephorid which appears
to be common in the islands visited by Mr. Wallace. It is
parallel in form, with the segments shining, and in appear-
Ann. & Mag. N. Hist. Ser. 5. Vol. xi. 19
282 Mr. C. O. Waterhouse on
ance somewhat resembles Telephorus rujicollis, but with ex-
cessively fine punctuation on the elytra. The male has the
basal joint of the antenne large, inflated, somewhat globular,
and shining; the second joint is rather short, linear; the third
is nearly twice as long as the second; the following joints
longer and more slender, slightly diminishing in thickness to
the apex. The female has the antenne similarly constructed,
except that the basal joint is normal. The anterior claw to
all the tarsi is bifid at the apex in the male, simple in the
female.
I think this genus should be placed near Anisotelus, with
which it agrees in having a large basal joint to the an-
tenne (although of a different form), but from which it
differs in, form and in not having the antenne enlarged
at the apex, and widely separated at the base. In the
Munich Catalogue Anisotelus, Hope* (Royle’s ‘ Himalaya,’
p. 55), is placed as a synonym of Zylocerus, a genus founded
on a West-Indian insect. I think the two genera should be
kept distinct, the males having the anterior claw to all the
tarsi bifid in Andsotelus, and only the anterior claw of the
front tarsi in Tylocerus.
Spherarthrum preustum.
1 believe that it is the female of the species in question
which Guérin has described (Voy. Coquille, p. 75) under the
name of Telephorus preustus, from New Guinea. ‘There are
numerous specimens in the British-Museum collection from
Dorey, Aru Islands, Batchian, Amboyna, and Mysol.
The antenne are generally blackish, with the basal joint
either black, reddish, or yellow. The head (except in one of
the specimens from Batchian) is yellow. ‘The thorax is
always yellow. ‘The elytra are yellow, with a little black at
the apex, half black, or nearly all black, or blackish with the
suture and margin yellow. The legs are yellow, with the
tarsi dusky, except the female specimen from Batchian with
the black head ; this has the legs black. The male example
from Batchian has the head yellow (with a little dusky mark
on the forehead), the elytra broadly margined at the suture
and sides with yellow, and the legs yellow.
A single female example.
* It may be well to point out that the following species mentioned in
afew words by Hope in Gray’s Zool. Miscell. p. 26, are omitted (perhaps
purposely) from the Munich Catalogue :— Telephorus rubricollis, cyanurus,
trimaculatus, unipunctatus, purpurascens, assimilis; Anisotelus lividus
bispilotus.
‘Challenger’ Coleoptera. 283
Miolispa suturalis, Pascoe.
The specimen brought is entirely black, except a yellow
stripe on each elytron. It does not, however, appear to differ
in any other respect from the usual red examples with black
head.
TAHITI (Lake Wathiria).
Anchomenus anachoreta, eremita, and monticola, Fairm.
The three species brought by the Expedition from Lake
Waihiria appear to correspond with the three described by M.
Fairmaire (Rev. Zool. 1849, p. 283) from the same locality.
If this be the case, however, his descriptions are not strictly
accurate.
He states that A. anachoreta and A. eremita have the strize
of the elytra impunctate. This can only apply to the dorsal
strie, as the lateral ones are distinctly punctured, and even
the dorsal striz are seen to have punctures if the insect is
viewed obliquely. The punctures are more obscure in A. ere-
mita than in A. anachoreta. The sculpture of the interstices
of the striz of the elytra is so excessively fine and delicate
in A. eremita that it can only be seen with a strong magni-
fying power, and the interstices consequently appear highly
polished. In A. anachoreta the sculpture is still very fine,
but’ is seen much more easily, whilst in A. monticola it is
visible with a weak magnifying-glass and renders the surface
slightly opaque.
It appears to me from description that Dyscolus castaneus,
Bohem. (‘ Kugenies Resa,’ p. 16) is the same as A. monticola.
These species are correctly placed under the genus Colpodes
in the Munich Catalogue.
Colymbetes pacificus, Boisd.
Two examples.
Sphenophorus obscurus, Boisd.
Two examples.
British Museum, South Kensington,
March 15, 1884,
19*
284 Mr. 8. O. Ridley on Growth and Budding
XXXII.—Onthe Classificatory Value of Growth and Budding
in the Madreporide, and on a new Genus illustrating this
point. By Stuart O. Ripiey, M.A., F.L.S., &., As-
sistant in the British Museum (Natural History).
[Plate XI.]
THE manner in which growth is effected in the corallum has
long been considered a character of very great importance for
the systematic division of the Madreporaria.
Thus MM. Milne-Edwards and Haime (Hist. Nat. Corall.)
appeal constantly to the characters gemmiparity and _fissi-
parity, and the various modifications of gemmiparity, in the
formation of their genera, and (e.g. Astrangiaceee, Oculinide)
sometimes in the distinction of larger groups; they point out
at the same time that gemmiparity may occur in a group
(‘Turbinoliidee) whose members are not normally compound.
In the genus Madrepora the characteristic form of increase
has been held by the highest authorities to be that of lateral
extracalicinal gemmation from a primary zooid. ‘Thus
Ehrenberg (Cor. roth. Meer. p. 108) defines that section of
his family Madreporina which he calls Heteropora, but which
is now termed Madrepora, as follows :—“ Stella ramulorum
qualibet solitaria, gemmipara, seepe maiore (gubernatrice),
reliquis raro gemmiparis, minoribus (frutices erectos, ramo-
sissimos, prostratosve formant).”
Dana’s generic diagnosis of Madrepora (U.S. Expl. Exp.
Zooph. p. 431) 1s :—* Patrio-ramose ; arborescent, ceespitose,
or, through coalescence, reticulate or foliaceous. Coralla with
the branches terete (very rarely compressed) ; calicles regular.”
He says further, “The genus J/adrepora includes species
which bud from a parent-polyp, with which each branch ter-
minates. . . . But two or three species are known in which
the apical polyp cannot be distinguished; and these form a
conuecting-link between this genus and the following ” (the
following genus is Manopora, Dana,=Montipora, De Blain-
ville). The three species mentioned by Dana as not having
an apical polyp are J. cuneata, labrosa, securis.
Milne-Edwards and Haime (Hist. Nat. des Coralliaires,
p. 152) define Madrepora thus :—‘ Polypiérites réunis en
masses ramifiées, fasciculées ou lobées. Calices saillants, au
moins dans le jeune Age, & ouverture petite ou médiocre et 4
bords assez €épais. Cloisons non débordantes. Columelle
nulle;’’ and continue, pointing out that budding is usually
circular and that “ le polypiérite souche de chaque pousse est
in the Madreporide. 285
presque toujours plus développé que ceux dont il est entouré et
constitue 4 l’extrémité de chaque branche ou ramuscule, mn
calice dit apical, qui est plus grand et plus proéminent que les
calices latéraux.”
Verrill (“* Review of the Corals and Polypes of the West
Coast of America,” Trans. Connecticut Acad. 1. (1869) p. 501)
says of Madreporaand Montipora, ‘ The resemblance between
certain species of these two genera, both in appearance and
structure, is very close, the chief difference being that in
Madrepora there is usually a terminal or leading polyp at the
end of each branch, which is not the case in Montipora.”
Klunzinger (Korallenthiere des rothen Meeres, 1. p. 2) com-
mences his account of Madrepora by stating that ‘“ the colony
bears branches which are usually more or less round, and the
terminal calicle of which is always distinguished by size or
shape from the numerous lateral calicles which lic as lateral
buds around the median calicle.”’ Studer (Monatsbericht
Akad. wiss. Berlin, 1878, p. 535) does not define Madrepora ;
but at the end of his account of those species of the genus col-
lected by the ‘ Gazelle’ establishes a new subgenus, which he
calls Zsopora, and definesas ‘‘Cormus foliar or lobate, the calicles
projecting equally, distributed evenly over the whole colony,
no specially differentiated apical calicle,’ placing under it
Madrepora securis and labrosa of Dana. [In view of the
unwieldiness of the large genus Madrepora, it is perhaps
desirable that it should be thus subdivided for working pur-
poses in this way into minor groups or subgenera, and perhaps
WMV. elegans might advantageously be similarly set aside from
the rest of the genus, as suggested by Milne-Edwards and
Haime (/. c.).] Subsequently (see below, ad jin.) Studer
suggests fission or marginal gemmation as the mode of growth
in Jadrepora.
Now it seems to me that while these various accounts of the
distinctive characters of Madrepora as opposed to Montipora
lay sufficient weight on the external facts of this distinction,
they do not, as a rule, bring forward the underlying law of
which these facts (¢. e. the terminality or non-terminality of
the distal calicles) are merely an expression, viz. the character
of the budding, which is essentially and fundamentaily diverse
in the two cases.
To how great an extent this essential difference has been
overlooked seems to be strikingly shown by Dana’s remark
above quoted, to the effect that the species of Madrepora
without an apical calicle “ form the connecting-link between
this genus” (Madrepora) “and the following” (Monti-
pora). This assertion does not even find support in the
286 My. 8. O. Ridley on Growth and Budding
evidence he adduces, viz. the growth of these species in
erect or incrusting plates, and the absence of an apical
polype, for the simple fact is, that, though in the species re-
ferred to there is no one apical polype, there are instead
several. I have examined two of these species, labrosa and
cuneata, and find that the ends of the branches are well
covered by large calicles, at the sides (and in cuneata, at any
rate, from the sides) of which originate young calicles. The
fact that there is no one apical calicle appears to be due to the
fact that on the broad ends of the lobes all calicles are equally
circumstanced, whereas in the pointed-ended Madrepore the
terminal calicles stand alone in position and circumstances.
In point of fact the most essential distinction between
Madrepora and. Montipora is thus overlooked by Dana. In
Madrepora (as may be seen at once by examining the ends of
branches of any species except labrosa, securis, cuneata) one
or more calicles take the lead in the growth, and others origi-
nate below them, constituting a centrifugal method of budding ;
in Montipora an undifferentiated apex of coenenchyma takes
the lead in the growth (as may be well seen in both the widely
different species J/. foliosa, Pallas, and digitata, Dana), and
new calices originate in this coonenchyma above the already
formed calicles; in other words, the budding is centripetal.
This distinction lies so deeply rooted in the structure and
physiology of these corals that it is difficult to see how a
directly ‘ connecting-link”’ between the two types can be
found. Ishould rather expect to find the connecting-point far
back in some common form in remote geological time.
The distinetion is the same as that denoted in flowering
plants by the terms “determinate” and ‘indeterminate in-
florescence.”’ In a determinate inflorescence growth is centri-
fugal, the first flower being formed at the apex; in an inde-
terminate inflorescence the first flowers are formed at the sides
and they successively approach the centre or apex of the spike,
The distinction appears to me to furnish a good character
by which to divide the Madreporme from the Montiporine
(sufficiently closely allied to each other and removed from the
Poritide, as it seems to me, by the possession of a spongy
coenenchyma, of a well-developed and deep calicle, devoid of
columella and pali) ; hence I would classify Madreporide as
follows :—
Subfam. 1. Madreporine.—Gemmation centrifugal, from
the sides of terminal calicles.
Subfam. 2. Montiporine.—Gemmation centripetal, from
a terminal coenenchymal mass.
A new genus, which I describe below under the name Ana-
in the Madreporide. 287
cropora, referable, from the character of its budding, to the
subfamily Montiporinee, fully bears out these views as to the
nature and importance of the mode of gemmation occurring in
that subfamily.
ANACROPORA *, n. gen.
Madreporide of ramose habit. Axis and apex of branches
formed by a spongy ccenenchyma. New calicles formed cen-
tripetally, 7. e. from the base towards the apex; no calicle
of any kind at the apex. Calicles equally distributed all
round stem and branches, with a tendency to an arrangement
in longitudinal series. Septal system well developed, com-
prising two cycles of six septa each, two (approximately upper
and lower) primaries being larger than the four lateral pri-
maries.
Obs.—Anacropora is based on the new species A. Forbesi,
described below, and on some forms which occur in the ‘ Chal-
lenger’ collection of reef-corals, to be hereafter described by
Mr. J. J. Quelch, of the Natural-History Museum; I have
had the advantage of Prof. Duncan’s and Mr. Quelch’s opinions
on this important form, opinions which have been freely and
kindly given. The general growth and other characters given
above are essentially the same in all the species. In all the
growth is low, the branches tending to form inosculations
between each other; the stem and branches are cylindrical,
and no distinct tubular calicles are formed.
From Madrepora this genus differs markedly in the
centripetal production of the calicles, by which the youngest
cealicles are always the uppermost. From the subgenus Jso-
pora, Studer (see above), it differs in the same point, as well
as in its slender dendroid growth; but the first distinction is
not so marked at first sight, since the peculiar growth of Jso-
pora almost necessitates the absence of a distinct apical calicle,
but (as stated above) the mode of gemmation is centrifugal in
Isopora, as in Madrepora s. str. Other points distinguishing
Anacropora from most species of Madrepora are the formation
of the axis of the branches by a spongy coenenchyma, whereas
in many (if not all) Madrepore this, in accordance with the
centrifugal habit of budding, is occupied to a greater or less
distance from the ends of the branches by the downward pro-
longations of the septa and the interseptal spaces of the apical
calicle. The rudimentary condition of the external part of
the calicle distinguishes <Anacropora; for although it is
* From ay, privative particle, adkpos, summit, répos, passage or pore ; in
allusion to the absence of pores from the ends of the branches.
288 Mr. 8. O. Ridley on Growth and Budding
commonly found (I refer to the sunk calicles occurring in so
many species between the prolonged tubular or nariform ones)
in some, it is never, so far as my knowledge extends, found
in all the calicles in any Madrepora.
Although in its general appearance it differs remarkably
from even the branched species of Montipora, yet the struc-
tural differences which separate Anacropora from this genus
are very far less distinctive than those which separate it from
Madrepora. In the first place, in spite of its external resem-
blance to Madrepora, it has the same system of calicular bud-
ding (viz. centripetal, from the distal coenenchyma) which we
find well developed in the ramose Montipora; the trabecular
structure and the two-cycled arrangement of the septa is the
same in both genera. On the other hand, whereas in Anacro-
pora there is always an undifferentiated coenenchymal apex, de-
void of calicles, to the branches, in Montipora this apex appears
always to bear at least one calicle on its surface. In Anacro-
pora the calicles are always rather distant and tend to form
lines, and are slightly raised above the surface, forming low
hill-like eminences, whereas in the ramose Montipore (e. g.
digitata, Dana, divaricata and superficialis, Briiggeman),
which on the whole most closely approach Anacropora, the
ealicles open flush with the surface, are crowded indiscrimi-
nately, and no linear arrangement is apparent. In Montipora
foliosa, it is true, the calicles, especially on the posterior aspect
of the corallum, are elevated in a similar manner; but the
foliate growth and the monticular cnter-calicular eminences
of the upper surface seem to remove this species far from the
ramose Montipore. It seems to me not improbable that, for
the reasons I have indicated, these ramose forms may have to
be separated from the foliate and massive species of Montipora.
The relations of Anacropora may be thus shortly stated :—
Anacropora has the general growth of Madrepora, but the
manner of budding of Montipora.
The following is a description of the single species referable
to this genus which I am able to describe; owing to the
interest attaching to the type, I have allowed myself to give
its characters at full length :—
Anacropora Forbest, n. sp. (Pl. XL.)
Corallum branching frequently, dichotomously, occasionally
subtrichotomously ; branches given off in succession in a sub-
spiral manner, the planes of successive bifurcations varying
from about 30° to 100° with regard to each other; angle be-
tween branches composing bifurcation 80° to 100°. Stem
and branches slightly curved, the apical branches more strongly
in the Madreporide. 289
so, cylindrical, except the terminal branches, which tend to
curve outwards and taper gradually to points ; diameter, main
axes 6-7 millim., intermediate and terminal branches about
4 millim., greatest length between bifurcations of main
branches about 30 millim., terminal twigs 25 millim. long.
Calicles arranged more or less definitely, for the most part
in series which follow approximately the longitudinal axis
of the stem and branches, the calicles of one series alterna-
ting with those of the adjacent series ; series about 2 millim.
apart, calicles about 2 to 2°5 millim. apart in the series.
Calicles forming, everywhere but on the tips of the branches,
low rounded elevations, by the gradual rising of the surface
towards their inferior margins to a height of :25 to -7 millim.,
and occasionally by the similar but very slight elevation of
their superior margins. Calicles orbicular, looking upwards ;
orifice of adult calicles 5 to *7 millim. in diameter ; on the
tips of the branches they open on the level of the surface of
the corallum, are more or less imperfectly defined from the
surrounding loose coenenchyma, and measure about 25 to
‘4 millim. in diameter. Septa trabecular, consisting of ver-
tical series of horizontal pointed projections from the wall
of the calicle, beginning just below its margin, distinct.
Primaries about *25 millim. in length in full-grown calicles,
comprising two main, opposite ones, variously placed (7. e.
from parallel to the long axis to at an angle of 45° with the
same), which converge towards the bottom of the calicle,
where they meet and form a vertical plate ; the other prima-
ries are slightly smaller and do not meet below. Secondaries
varying from about half the diameter of primaries to mere
points on the side of the calicle ; the secondary septum between
the two lateral primaries is sometimes wanting.
Corallum slightly vermiculate, always covered by minute
points at surface (at apex looser, very porous) ; the outer one-
quarter of diameter (except at apex, see fig. 5), formed of
a denser tissue, in which the calcareous trabeculae exceed in
diameter the spaces between them ; the central one-half of the
diameter (viz. usually about 2 millim.), consisting of a loose
tissue, in which the calcareous bars are only about half the
diameter of the intervening spaces; the meshes of this tissue
(as seen in transverse section of a branch) elongate towards
margin, smaller and relatively shorter at centre. Apices of
branches, to a distance of from 2-8 millim. from the ends (see
fig. 5), formed of the looser axial coenenchyma, and carrying
more or less rudimentary calicles, which are at least 1 millim,
from all other calicles in the same longitudinal series.
Hab. Keeling Islands, Indian Ocean ; deeper water inside
reef.
290 Mr. 8. O. Ridley on Growth and Budding
Represented by a single colony (fig. 1) and a detached
branch, which has lived independently after its fracture from
the parent specimen. They were collected and presented to the
British Museum by Mr. H. O. Forbes, F.Z.S. &e., who has
already (Proc. Roy. Geogr. Soc., Dec. 1879) described these
islands, and with whose name I have much pleasure in asso-
ciating this new type. The chief colony measures 83 millim.
(34 inches) in height, 100 millim. (4 inches) in greatest
breadth, and 55 millim. (24 inches) from front to back; the
detached branch, which bifurcates three times, was about
60 millim. long when alive. Parts of the corallum, owing
either to an evanescent pigment or to traces of animal matter,
have a most delicate pink tint.
Some interesting points are brought out by the detached
branch ; this occurs unrooted, but obviously had been broken
off from the colony while yet alive (see fig. 4) and lived sub-
sequently free. As commonly happens in such cases, the
fractured surface has healed over; but in this case the new
material is not a continuation of the superficial coenenchyma
of the adjacent side over the stump, but the prolongation out-
wards ot the loose central coenenchyma which has developed
on itself five or six young calicles. Here also the law of
centripetal gemmation asserts itself, these calicles occurring
on the sides of a central cone of loose coenenchyma, of which
the apex, 1 millim. long, is undifferentiated and bears no cali-
cles. The same law is followed in the process of repair
exhibited by a broken stump of a branch on the larger speci-
men. The wide angle of bifurcation of the branches causes the
colony to assume a low decumbent form, and bringing, as it does,
neighbouring branches into juxtaposition, gives rise to ana-
stomoses; the branching in various planes gives it a broad top.
Bilateral Symmetry in the Madreporide.—In Madrepora
elegans we have a decided bilaterality in the arrangement of
the calicles on the corallum, a circumstance which has induced
MM. Milne-Edwards and Haime to entertain the idea that
this form might be generically distinct from Madrepora. No
other Madreporidee exhibit this, so far as I am aware; bilatera-
lity in the arrangement of the parts of the calicle is, how-
ever, a prominent feature of a number of Madrepore, taking
the form of a superior development of the upper and lower
(distal and proximal) primary septa, sometimes carried to the
extent of their union in the middle line at no great distance
below their upper margins. In Montipora also. (at any rate, in
digitata, Dana) the primaries are thus distinguished ; but here
they are not always strictly upper and lower in relation to the
long axis of the branches. This form of calicular bilaterality
in the Madreporide. 291
is well marked also in Anacropora, although I have not ob-
served it to extend to the union near the summit of the calicle
of the two leading septa; in this genus also these two septa
are sometimes placed diagonally with relation to the axes of the
branch (see fig. 2). Klunzinger (Kor. roth. Meer. 11. p. 2)
states that in Madrepora one of these two (which he calls
“Hauptsepta’’) has its corresponding tentacle longer than the
other eleven tentacles.
In Seriatopora these two septa are represented ¢n position by
the long plate which extends from the proximal to the distal
wall of the calicle, ¢. e. in the direction of its (here) longer
axis; but the fact that, as Prof. Moseley has shown (Quart.
Journ. Microsc. Sci. n. s. xxil. p. 392), six primary septa
are present without counting this, seems to favour Milne-
Edwards and Haime’s view, that this plate is columellar,
not septal, in origin—in which case Sertatopora would
differ from the Madreporide in having its primary septa
wholly distributed to the right and left of a dorso-ventral line.
Budding or Fission in Madrepora ?—Prof. Studer, in his
paper on Budding and Fission in the Madreporaria (Mitth.
naturf. Ges. Bern, 1880, p..3), surmises (p. 14) from ap-
pearances that in the Madreporide (he evidently refers only
to Madrepora, as Montipora has no apical calicle) the new
ealicles are really formed by fission or lateral gemmation from
the margin of the apical calicle, which he thinks sends out
curved bulges from its margin. All the evidence I have
gathered myself from Madrepora is rather in favour of the old
view that the buds are formed from the sides of the wall
of the apical calicle in this genus.
EXPLANATION OF PLATE XI.
Fig. 1. Anacropora Forbest, the chief specimen, seen somewhat from
above. Natural size.
Fig. 2, Ditto, part of a main branch of the same specimen, showing cha-
racters of adult calicles and of the exterior of the ccenenchyma,
x 6 diameters.
(Note that one calicle has the main primary septa dorso-
ventral, the other diagonal in position.)
Fig. 3, Ditto, vertical section of main branch of the same specimen,
showing :—a, axial; 6, superficial cenenchyma; and e, longitu-
dinal section of a calicle. X 6 diameters. .
Fig. 4. Ditto, basal end of detached branch, showing the renovation of
the stump by the emergence of the loose axial coenenchyma and
the formation in this coenenchyma of young calicles. Xx 8 dia-
meters.
Fig. 5, Ditto, apex of branch of chief specimen, showing the loose texture
of the ccenenchyma at this point and the formation (as in
fig. 4) of young calicles from this loose ceenenchyma. The view
selected shows an unusually regular longitudinal series of young
calicles, x 3 diameters,
292 Mr. J. J. Quelch on new Genera and
XXXIV.—Preliminary Notice of new Genera and Species
of ‘Challenger’ Reef-Corals. By J. J. Quetcu, B.Sc.
(Lond.).
Part I.
THE present paper contains short descriptions of five new
genera and their typical species in the collection made during
the voyage of H.M.S. ‘ Challenger.’ More complete descrip-
tions, with figures, will be given hereafter in the ‘ Challenger’
series, when also their affinities with fossil and recent forms
will be discussed. It is sufficient in this notice to point out
that Physogyra is to be classed with Plerogyra, Napopora
close to Synarrhaa and Stephanaria, Sandalolitha to Halo-
mitra and, perhaps, to Zoopilus ; while Tichoseris and Mose-
leya may be mentioned as presenting special interest. T%cho-
seris takes a very clearly transitional place between the
Lophoserine and the Astreide ; while Moseleya, which I have
had the pleasure of naming in honour of Prof. Moseley, seems
to necessitate the establishing of a new subfamily of the
Astreide to receive it—subfamily Moseleyine, characterized
by the abundant endotheca with the dissepiments in more or
less concentric circles, forming nearly complete tabule at the
centre. The approach which it makes to the Rugosa seems
tome to point to the very probable dismemberment of that
group.
MOSELEYA, nov. gen.
Corallum compound, flattened, or slightly and broadly con-
vex. Young calicles developing by calicinal marginal budding
around a very large median calicle, which has very numerous
septal orders, the calicles becoming polygonal and deep at
the centre. Epitheca very slight; wall very thin and almost
rudimentary, but developed so as to give a distinct simple line
of separation to the calicles on the surface, often interrupted,
seen in section in a very rudimentary state separating the
calicinal centres. Coste very distinct, thin, and finely den-
ticulate. Septa often confluent and continuous from centre to
centre in the line of union between adjoining calicles; very
thin and close, finely toothed above, and having the teeth
subequal or slightly larger near the centre. Endothecal
dissepiments vesicular, very abundantly developed, leaving
but a very small portion of the septa free exteriorly, seen in
transverse section forming nearly concentric lines, and more
or less complete tabule at the centre. A false columella
~
Species of ‘Challenger’ Reef- Corals. 293
present, seen exteriorly to be formed by the trabeculate and
vermiform nature of the innermost upper part of the septa,
entirely or almost absent in transverse section, where the
septa are seen to meet almost at a point.
Moseleya latistellata, n. sp.
Calicles very large, the median calicle attaining a width of
6 centim., and attached by a very broad base to the surface
on which it grew. Epitheca and wall very thin, the wall
often rudimentary between the confluent septa of adjacent
ealicles. Coste very distinct and finely denticulate above,
continuing as well-marked lines to the very base. Septal
system containing orders of seven cycles, but the last two
cycles are incompletely developed, there being about two
hundred septa in the largest calicle ; the septa are very thin,
finely cut into subequal sharp teeth nearly 1 millim. in
length, laterally granulated and thickened chiefly in the direc- ©
tion of the teeth, free above only for a short portion, owing to
the great development of endotheca, but at the centre the
endotheca is much less developed, and consequently the
calicles become much deeper and the septa more prominent.
The septa of the first two or three orders are about equal and
run quite to the centre; those of the higher orders become
smaller and shorter, while rudiments of the highest orders
are present only at the extreme edge of the calicles ; with the
exception of these last, the septa are regularly placed and
equally raised, giving a very even appearance to the calicles,
especially to the older ones. Pali and true columella absent,
but the finely trabeculate edges of the septa give the appear-
ance of a small columella.
Locality. Wednesday Island, Torres Straits, 8 fathoms.
PHYSOGYRA, nov. gen.
Corallum compound, form massive, of very light structure,
having the calicles in long, sinuous, more or less meandroid
series, with their walls fused throughout so as to form a
simple very thin line of separation between the series. Cali-
cinal centres generally distinct, indicated by the curving of
the septa. Coste almost entirely absent. Hpitheca very
slightly developed. Septa thin, fragile, very prominent, dis-
tant, edge entire. Columella absent. Lndotheca well deve-
loped, vesicular; the dissepiments continuous between the
septa from the centre of the calicle to the wall, very convex
above, rather far apart above each other, thus forming wide
interseptal chambers. Owing to this great development of
94 Mr. J. J. Quelch on new Genera and
vesiculate endotheca the series of calicinal centres are sepa-
rated by wide ridges, formed entirely by the thin wall and
by the convex dissepiments which stretch from the centre to
this thin wall.
This genus will include, besides the following new species,
the Plerogyra Lichtensteiné of Milne-Edwards and Haime ;
the genus Plerogyra being limited to those forms in which
the walls are not fused together so as to form a thin lamina,
but in which the series remain distinct with their walls sepa-
rated, except occasionally when two free-growing ends meet
and grow together.
Physogyra aperta, n. sp.
Corallum convex above; wall very thin, simple, sometimes
almost rudimentary. Coste very slightly developed, and then
only at the margin of the series. The series of the calicinal
‘centres open and shallow, in no part deep and narrow ; the
centres are often difficult to distinguish, owing to the uniform
development of dissepiments along the series. Width of
series about 16 millim., but at times more than 20 millim.
The septa are 2-4 millim. apart, very thin and very projecting,
subequal, except at the ends of series where some are very
small, easily broken away, leaving the vesicular dissepimental
ridges almost bare. ‘The dissepiments are thin, convex above,
easily broken away, about 3 millim. apart from these above
or below at the wall, closer at their inner terminations,
forming simple, curved, wide interseptal chambers.
Locality. Banda.
SANDALOLITHA, nov. gen.
Corallum compound, flattened, free, much elongated and
very thin. Wall sparsely porous and extremely reduced;
distinct coste, closely granulated or very finely and bluntly
echinulate, curving towards the short axis. Calicles few, in
the long diameter of the corallum; parent calicle very large,
occupying the centre, forming almost the entire corallum, with
very numerous septa, there being about seven complete cycles,
a much larger number of cycles being developed in the long
axis of the corallum ; smaller calicles very few, distinctly
radiate, developing in the course of and interrupting the
larger septa in the long axis of the parent calicle. ‘The septa
are crowded and very long, curving towards the short axis,
and of more or less equal vertical extent, very low, giving an
even laminate appearance to the corallum. Synapticula well
developed and forming strong connexions at the basal parts of
the septa. Columella rudimentary and trabecular.
Specres of ‘Challenger’ Reef-Corals. 295
Sandalolitha dentata, n. sp.
Corallum almost flat, irregularly sandal-shaped, fragile,
translucent, being about 6 millim. thick except immediately
around the mouth of the central calicle where the septa are
somewhat elevated and thickened. The parent calicle attains
a large size (nearly 15 centim. in length) before the smaller
calicles begin to develop. Wall very thin, pierced with
numerous small pores ; costa unequal, with very small granu-
lated blunt spines, distinct, curving in radiating lines towards
the short axis of the corallum except at the centre where the
costal spines become crowded over a thickened circular space
that seems to have been a former base of attachment. Septa
of the central calicle of seven complete cycles, but incomplete
orders are developed at the extremities of the long axis of as
many as sixteen cycles; those of the first three cycles sub-
equal, slightly thickened and prominent at the centre; and,
with the exception of the very small ones, all the septa are
nearly equally raised over the general surface, cut into
strong long and narrow teeth, very granulated, especially at
the apex of the teeth, which are divided into little points
forming a blunt or pointed end. The septa of the higher
orders unite one on each side with one of a lower order at
that part of it from which they originate.
Locality. ‘Tahiti.
TICHOSERIS, nov. gen.
Corallum compound, massive, columnar or lobate, with
neither transverse calicinal ridges nor longitudinal crests,
astreiform. Calicles with distinct solid walls, which are thin
at their edges, but thick at their basal parts ; calicinal centres
arranged either singly within their own wall, or united in more
or less irregular and sinuous groups of two or more incom-
pletely separated from each other and surrounded by the
common wall of the calicle from which they are developed.
New calicles arise either by direct fission of a single calicle
forming two separate ones with distinctly raised walls, or by
the upgrowth of the synapticula at different parts of the calicle
to form new walls, the resulting centres often forming mean-
droid series, until the development of their own wall isolates
them. Septa not at all confluent, entire, those of adjoining
calicles quite separated by the raised walls. Columella ab-
sent or forming a very small styliform projection at the point
of coalescence of the septa. Synapticula distant, very un-
equally and irregularly developed, being generally rather
thick interseptal outgrowths of the wall.
296. On new ‘Challenger’ Reef- Corals.
Tichoseris obtusata, n. sp.
Corallum consisting of blunt, elongated, lobate masses of
very dense structure throughout. Calicles small, often sepa-
rate, subcircular or elongated and polygonal, about 8-5 millim,
in diameter, rather deep, but almost filled up by the closely
packed septa ; more generally two to six or more calicles are
grouped together, with their walls incompletely developed, so
that they give the appearance of many centres surrounded by
one raised wall, which is of very irregular shape and size,
being long, sinuous, and narrow, or rounded and wide, often
5-14 millim. in diameter. Wall very solid, thin-edged above,
but thick below. Septa not exsert, very numerous, in the
separate calicles there are as many as five cycles, but the fifth
is very incomplete ; those of the first two cycles are subequal,
those of the fourth and fifth very small; but all are entire,
very thin above, extremely granulated or finely echinulate on
their sides, with their inner edges nearly vertical. Columella
very rudimentary.
Locality. Reets, Fiji Islands.
NAPOPORA, nov. gen.
Corallum compound, porous. Gemmation intracalicinal, the
developing buds with distinct centres almost destitute of dis-
tinct walls, at first united in groups of two to six, and sur-
rounded by the common wall of the parent calicle; but as
development proceeds they are separated off by a narrow,
raised, distinct wall. Calicinal depressions very variable in
size and shape, according to the number, position, and degree
of development of the buds. Walls of the older calicles porous,
distinctly raised, angular. Septa generally of two cycles,
rudimentary. Pali six, sometimes one smaller than the others
or absent, generally well developed, and distinctly marking
the position of the calicinal centres. Columella rudimentary,
represented by small papilliform projections, often absent.
Napopora trregularis, 1. sp.
Corallum ramose ; branches rather short, moderately thick,
obtuse, and slightly or not at all compressed. Calicles very
variable, seen in all stages of development, with many
granular points or flattened projections; the single calicles
with distinct walls, subcircular, about 2 millim. in diameter ;
the larger ones with many distinct centres in the same cavity,
with a common wall, raised, angular, and of irregular shape,
with a diameter of about 4-9 millim. Many of the develop-
Geological Society. 297
ing centres present no trace of a wall, others possess walls
more or less incomplete; but the centres are easily distin-
guished by the position of the pali. The septa of two or
three cycles, generally twelve, sometimes fewer, rudimentary,
sometimes rather distinct at their inner ends and united two
by two where the pali are placed. The pali are six, promi-
nent, sometimes one very small or absent. Columella incon-
spicuous.
Locality. 'Vahiti.
PROCEEDINGS OF LEARNED SOCIETIES.
GEOLOGICAL SOCIETY.
February 20, 1884.—Prof. T. G. Bonney, D.Sc., F.R.S.,
President, in the Chair.
The following communications were read :—
1. **On a recent Exposure of the Shelly Patches in the Boulder-
clay at Bridlington.” By G. W. Lamplugh, Esy. Communicated
by Dr. J. Gwyn Jeffreys, F.R.S., F.G.S.
During some long-continued windy weather in the early part of
the winter of 1882-83, the Boulder-clay, usually hidden by sand
and shingle, was laid bare on the foreshore at Bridlington Quay.
The beds thus exposed belong to the lowest recognized part of the
glacial series of Yorkshire, the ‘‘ Basement Boulder-clay.” Over
this, parted occasionally by a little sand or gravel, comes the Purple
Boulder-clay, the Laminated Clay being wholly absent. The Base-
ment Clay thus exposed contained angular and subangular boulders,
with rounded pebbles occasionally scratched, besides many crushed
masses of sand, sandy gravel, and clay, forming nearly a third of the
whole mass. The last, which generally contained marine remains,
were very variable in shape and in lithological character. Tho
fauna of the masses varied greatly, both in abundance and in species,
those common in one mass being rare or absent in another. The
shells were commonly much crushed, though whole specimens oc-
curred occasionally. The author considered that these shell-bearing
patches had once formed a part of the bed of a glacial sea, which
had been invaded and ploughed up by ice, which had transported
them to their present locality. He gave reasons for thinking that
they have not come from the immediate neighbourhood, but pro-
bably from the north-east, having been floated by icebergs to their
present places.
Ann. & Mag. N. Hist. Ser. 5. Vol. xiii. 20
298 Geological Society :—
The paper concluded with lists of the fossils discovered (obtained,
for the most part, by washing parts of the included masses). The
result has been that the number of the Mollusca (examined by Dr. J.
Gwyn Jeffreys) has been raised from 67 to 101, five of the additions
being new to science. Four species of Balanus and one of Verruca
have been identified. More than eleven species of fish have been
identified with more or less certainty. These, Mr. E. T. Newton
remarks, seem to be either Norwich-Crag, Red-Crag, or London-clay
forms; and all nay have been derived from the last-named deposit.
The Ostracoda and Foraminifera, which are numerous, were described
by Dr. Crosskey in an appendix.
2. “On the so-called Spongia paradoxica, 8. Woodward, from
the Red and White Chalk of Hunstanton.” By Prof. T. M°Kenny
Hughes, M.A., F.G.S.
The author described a branched structure found in the Red and
White Chalk of Hunstanton, which was named Spongia paradoaica
by 8S. Woodward, and has since generally been known as Spongza or
Siphonia paradowica. The beds in which this supposed sponge
occurs, contain fragments of various organisms, including sponge-
spicules, but no trace of structure can be found in sections of the
Spongia paradoxia. The fragmentary state of the urdoubted
organic remains would indicate that they were drifted into their
present position, and therefore a state of things quite unfitted for
the growth of a slender branching sponge; the so-called sponge
commonly occurs in layers along the bedding-planes, but frequently
rises through the whole thickness of one bed and extends up into
the overlying layers. It does not seem likely that it was the root
of a Siphonia or some similar organism. Another body which has
been also called Spongia paradowica consists of masses of more
erystalline texture, exhibiting upon weathered surfaces a network of
small ridges enclosing cup-like depressions. These appearances were
compared by the author to the weathered surfaces often seen in
certain beds of the Mountain Limestone and in gypsum ; the masses
show no traces of internal structure.
The author stated that sections of these bodies show exactly
the same characters as the containing rock, except that the material
is more compactly crystalline ; it contains the same fragments of
shell, &c., and the same sand and pebbles. He regarded them as of
concretionary origin, and explained their symmetry of form and
regularity of arrangement by their being formed at the intersections
of joints with the bedding-planes or with one another. Phosphatic
nodules occur in the lower parts of the White Chalk, and had these
bodies been sponges they would probably have been phosphatized ;
but analyses have shown no marked difference in this respect be-
tween their substance and that of the surrounding rock.
On the Structure and Formation of Coal. 299
March 5, 1884.—Prof. T. G. Bonney, D.Sc., F.R.S.,
President, in the Chair.
The following communication was read :—
1. “On the Structure and Formation of Coal.” By E. Wethered,
ists, Hrs, EC.0.
The author, having referred to the work of previous investigators,
pointed out that seams of coal do not always occur in one bed, but
are divided by distinct partings, some of which, as in the case of the
Durham main seam, contain Stigmarie. It was important to
notice this feature for several reasons, but especially as the beds of
coal, defined by the partings, showed differences both in quality and
structure. In the case of the shallow seam of Cannock Chase they
had at the top a bed of coal 1 foot LO inches thick, the brown layers
of which were made up of macrospores and microspores. The
bright layers were of similar construction, except that wood-tissue
sometimes appeared, also a brown structureless material, which the
author looked upon as bitumen. He, however, objected to that
term, and thought that hydrocarbonaceous substance would be
preferable. What this hydrocarbonaceous material originated from
was a question for investigation. In the lower bed of the Welsh
* Four Feet” seam wood-tissue undoubtedly contributed to it;
whether spores did was uncertain; it was true they could be
detected in it. In the second bed of the shallow seam they had a
very different coal from the upper one. It was made up almost as
a whole of hydrocarbonaceous material. Very few spores could be
detected. It was possible that the scarcity of these objects might be
due to decomposition ; but the author’s investigations seemed to show
that spores resisted decomposing influences more effectually than
wood-tissue, which seemed to account for the fact that where they
occur they stand out in bold relief againstthe other material composing
the coal. Below the central bed of the shallow seam came the main
division. In it the author detected a large accumulation of spores,
but hydrocarbon formed a fair proportion of the mass. The author
referred to other seams of coal from various parts of England, and
pointed out the structure of each bed composing them. The con-
clusions on the evidence elicited from his investigations were (1)
that some coals were practically made up of spores, others were not,
these variations often occurring in the beds of the same seam ; (2)
that the so-called bituminous coals were largely made up of the sub-
stance which the author termed hydrocarbon, to which wood-tissue”*
undoubtedly contributed.
An appendix to the paper, written by Prof. Harker, Professor of
Botany and Geology at the Royal Agricultural College, Cirencester,
dealt with the determination of the spores seen in Mr. Wethered’s
microscopic sections. ‘Taking the macrospores, the resemblance to
those of Jsoétes could not fail to strike the botanist. He had
procured some herbarium specimens of Jsoétes lacustris in fruit, and
20*
300 Bibliographical Notices.
compared the spores with those from the coal. When gently crushed,
the identity of the appearance presented by these forms from the
coal was very striking. The triradiate markings of the latter were
almost exactly like the flattened three radiating lines which mark
the upper hemisphere of the macrospores of Jsoétes lacustris. The
writer therefore concluded that the forms in the coal were from a
group of plants having affinities with the modern genus Jsoétes, and
from this Isoétoid character he suggested for them the generic title
of Isoétovdes pending further investigation.
BIBLIOGRAPHICAL NOTICES.
Notes on Natural Selection and the Origin of Species. By Francis
P. Pascoz, F.L.S. London, 1884. Taylor and Francis.
Mr. Darwin having outlived the unreasoning rancour of his early
critics, his works are likely for some time to come to form the text
for much useful, thoughtful, and no doubt, in many cases, well-
founded criticism truly so called. Mr. Pascoe’s ‘ Notes’ belong to
this latter category. He admits that ‘“‘ no naturalist in these days
doubts that species have arisen by modifications through descent ;”
and he offers no suggestion as to the fixation of specific characters
by any means except natural selection. His object is simply to
point out various classes of difficulties in the way of the acceptance
of this, which is after all the Darwinian theory, and, in addition to
apparently endorsing many of Mr. Mivart’s criticisms, to insist on
the view that all the characters which serve to differentiate species
are ‘“‘ unimportant except as incipient structures, to which, as yet,
no advantage can be attached.” This difficulty, and it is a weighty
one, is, in the present writer’s opinion, partly owing to the unfor-
tunate prominence given to the indefinite, subjective term “ species ”
in the title of Mr. Darwin’s great work. It is apparently forgotten
that a “species” is not so much a series of forms similar iu their
main positive characters as a series isolated from other series by
negative characters—in the language of logicians, “ genus et diffe-
yentia.’” Hence the problem of the origin of species is not one of the
acquisition of positive characters, but deals with the isolation of
groups of variations by the extermination of forms intermediate
between the variations of one geological age and those of another.
‘It is not the origin of specific characters, but of specific divergence
or difference. Hence, admitting, as one undoubtedly must, that
the positive diagnostic characters of species are very generally indif-
ferent from the point of view of utility, they may yet have well
become characteristic by the extermination of intermediate stages
which may very probably have been harmful to the organism.
No one can deny the existence of a keen struggle for existence,
and surely it is no “‘assumption ” to state that in this struggle the
Bibliographical Notices. 301
weakest must succumb. Incipient structures being small, make but
small demands upon nutrition, and may well therefore be indifferent.
More advanced intermediate stages will make greater demands, and,
being less perfect, will, in competition with more completely special-
ized structures, be actually harmful.
Nevertheless it may be admitted that whilst Mr. Darwin never
professed to explain variability by the theory of natural selection,
he may not have sufficiently recognized the universality of indiffe-
rent variations. Heredity, towards the explanation of which Mr.
Darwin merely threw out the hypothesis of pangenesis, would, of
course, perpetuate these indifferent characters, as it does useful and
harmful ones. On the Darwinian theory, the persistence of lowly
organized types, of useless or even harmful structures, and of imper-
fect adaptations, is perfectly explicable, as is also the existence of a
variety of structures to serve one purpose, or conversely that of one
organ serving divers purposes. These, together with the varied
forms of Radiolaria or Foraminifera on which Mr. Mivart insists,
are simply cases of the absence of a struggle or of its slowness in
producing extermination. Such persistent forms as Nautilus and
Lingula, to which Mr. Pascoe alludes, and to which we might pro-
bably add the soft-bodied Peripatus and Amphiowus, are after all
but few in proportion to the immense number of extinct species, and
their existence is but a lingering one, “far from the madding
crowd ;” and whilst no doubt, if looked at as worms, the two latter
may be termed “ extremely specialized,” considered as Arthropods or
Vertebrates they are certainly not so.
These cases of persistence suggest what appears to be some answer
to Mr. Mivart’s hypothesis, “ that specific differences may be deve-
loped suddenly instead of gradually.” External conditions do not,
as a rule, change rapidly. The rise and fall of land, changes in
climate, or in the characters of aqueous sediments, are in the main
gradual, A sudden variation will be of the nature of a monstrosity
and but little likely to occur similarly and simultaneously in many
individuals. The chances are also apparently against its being so
well adapted to its surroundings as its slowly adapted congeners.
The case adduced by Mr. Mivart of the change of Siredon into
Amblystoma is not the origin of a new but the reversion to an old
form ; and possibly the Ancon sheep would not have been perpetua-
ted in a wild state. The latter is an illustration of the increased
variability of forms when domesticated, a result that might well be
anticipated from the unnatural suddenness of man’s changes in their
surroundings inducing a condition of unstable physiological equi-
librium. It was with reference to such views as to sudden changes
that Mr. Darwin wrote, “Slight individual differences, however,
suffice for the work, and are probably the sole differences which are
effective in the production of new species.’ This sentence Mr,
Pascoe apparently misunderstands as representing natural selection
as the sole cause of the origin of new specics.
It is in many cases difficult to gather how far Mr. Pascoe endorses
Mr. Mivart’s objections, and space only permits a brief reference to
302 Bibliographical Notices.
three of these, viz. highly specialized structures, the absence of
‘‘infinitely numerous fine transitional forms,” living or extinct, and
the ‘ polyphyletic hypothesis.” The first of these was fully dealt
with by Mr. Darwin, who showed for example that even the human
eye is an imperfect instrument, and that among the lower animals
we have a very large series of transitional forms of eye, from a mere
nerve-ending epithelium cell to the eye of a Nautilus, of a lobster, or
of aman. So, too, we must join issue with Mr. Mivart as to the
absence of extinct transitional forms. The progress of geology
even since Mr. Darwin wrote has added enormously to our know-
ledge of such forms, whilst it has also shown that it is difficult to
overstate the imperfection of the geological record. In the face of
such cases as those of the Ammonites described by Wiirtenberger
and of Planorbis multiformis in the Steinheim Limestone, described
by Hilgendorf, it is difficult to say that “the mass of palontolo-
gical evidence is indeed overwhelmingly against minute and gradual
modification.” Of course these evidences have often, as Hickel
has shown, been evaded by arguing in a circle as to wide specific
limits and limited variability; but this only demonstrates the
meaninglessness of the term “ species.”
To imagine that the characters of two sets of organisms can so
have varied as to produce in distant regions the same result is surely
a greater violence to the ordinary laws of causation than to suppose
that an organism now found in two such regions has previously
existed in the area intervening between them. Like causes may
produce like effects; but in the complexity of organic life and its
surroundings can causes ever be sufficiently like for this polyphy-
lesis ?
Mr. Pascoe’s pamphlet suggests many other topics of interest in
matters of detail, as, for instance, why man’s action should be ex-
cepted in discussing the recent extermination of species ; but per-
haps its chief merit is in the frank statement of difficulties and of
arguments pro and con without any attempt to set up any agency
as an alternative to natural selection. ‘A tendency to be wingless ”
or any other “‘ tendency ” is, it must be remembered, only a state-
ment, and not even an approach to an explanation.
G. S. Bounerr. -
Phytogeogenesis. The Primeval Development of the Crust of the
Earth and of Plants. Sketched out by Dr. Orro Kunrzz.
Pp. 213. 8vo. Leipsic: 1884. [Phytogeogenesis. Die vorwelt-
liche Entwickelung der Erdkruste und der Pflanzen in Grundziigen
dargestellt von Dr. Orro Kuntze. |
Tue special objects of consideration in this treatise are the formation
of the primeval rocks from gasogenous glowing crystals, the gradual
salinity of the ocean, and the marine development of the coal-plants,
Having laid down his principles for the reconstruction of primeval
conditions and his hypothesis on the origin of the first beings, indi-
Bibliographical Notices. 303
eating that fecundation is an originally morbid phenomenon, and
treating of the probable origin of the first organic cells, the author
proceeds to the consideration of the characteristics of the successive
geological periods :—I. Inorganic, beingless, lifeless, or hidden-life
(cryptobiotic) periods. No fossils; volcanic products withut steam-
cavities and glassless, and eruptions not dependent on water. 1.
First, anhydrate, waterless, or sealess period (Primeval Gneiss) :
+1000°-300° C. Sedimentary spheroidal formations (volcanic
bombs, granite nodules) by glowing crystallized precipitates from
the atmosphere, and their coagulation into primeval rocks destitute
of hydrated minerals. 2. Second, thermohydrate or hot-sea period
(Huronian): +3800°-130° C. Hot calciferous seas and aqueous
cementation of the minerals left unconsolidated after the first period.
3. Third, unfossiliferous and early-being, or eryptobiotic (hidden-
life) period (Clay-slate): -++150°-140° C. Origin of the first animate
existences, which were not, however, preserved fossil. Rock-forma-
tion scanty, microcrystalline.
II. Visible-life (pheenobiotic) or fossiliferous periods. Fossils
present ; volcanic products dependent on water, with the hardness
of the earth’s crust greater, the ocean’s saltness decreasing, and
steam-cavities and glass-inclusions increasing. A. Azonal or zone-
less-sea periods. No climatal zones nor continental climate. Flora
and fauna confined quite or almost to the tranquil sea, which is full,
since the still warm earth-crust absorbs but little water. The clastic
sediments quickly conveyed from the naked and relatively small
continents to the sea, and but slightly broken. ‘The absence of
atmospheric carbonic acid permits of only a marine flora, 4. Fourth,
or algo-marine period (Silurian): +40°-30° C., 4 per cent. of saline
contents in the sea. Luxuriant marine algal flora, with a rich
marine fauna, especially of calcareous animals. 5. F ifth, is prato-
marine (sea-meadow ) period (Devonian): +380°-25° C., 4 per cent.
of salt in the sea. Luxuriant, meadow-like, floating marine flora.
Fishes, but of a freshwater character, plentiful. Borne or growing
up above the water, the marine alge become by this supermarine
habit vascular-cryptogamic, and also more suitable for the formation
of coal. 6. Sixth, or sylvo-marine (sea-forest) period (Carboniferous,
in part): +25°-15° C., as much as 1 per cent. of salt in the sea.
The supermarine flora is more developed and woody ; with the first
plants haying aerial fructification. The rootless Lepidosigillarie
simply float. On the shore a woody, rooted, shallow-water flora is
developed, with at last the first land-plants. Coal-beds are formed
abundantly by the sinking of the decaying supermarine plant-
remains to the bottom, if clay-beds lie upon and tend to preserve
them; or there remains the Coal-Limestone separated by the sea-
plants. By the exhalation of the supermarine forest the air becomes
charged with carbonic acid, and thence the possibility of a ter-
restrial flora. 7. Seventh, or sea-shore (marine littoral) period
(Dyas or Permian): +15° C., up to 13 per cent. of salt in the sea,
‘the supermarine flora nearly dies out ; the littoral flora increases.
Angiosperms in the 6th and 7th periods.
304 Miscellaneous.
B. Land-zonal periods. Zones of climate, continental climate,
and unquict shallow seas. Plants and animals are developed on the
increasing land; but in the sea they are changed or destroyed by its
saltness, calcareousness, cooling, and restless surface. The continually
increasing land-flora causes permanent rivers, hinders the passage
of the clastic products considerably, favours their decomposition, and
consequently the increase of salt and lime in the sea. With the
development of terrestrial fauna and flora the proportion of carbonie
acid in the air is raised, and land-plants increase. 8. Eighth, or
dizonal-littoral (two-zoned littoral) period (Mesozoic). Broad mid-
zone tropical; polar zones subtropical : 13-2 per cent. of salt in the
sea. Flora and fauna more limited to the shore and neighbourhood
of inland waters. 9. Ninth, or dizonal-continental period (Tertiary).
Tropical mid-zone and temperate polar zones: up to 3 per cent. of
salt in the sea. Flora and fauna more continental. The shiftings
or derangements in the crust of the earth reach their maximum.
The greater cooling causes great variability in plants. The origin
of man, at first black only, dates from this 9th period. 10. Tenth,
or three-zoned (trizonal) period (Quaternary). Hot, temperate, and
cold zones. Development of the existing conditions.
The main principles and very much of the details on which the
foregoing classification of the geological periods and orders of nature
has been founded by the author are treated of in Chapters ]V.—X1I,
Thus :—the climatic interpolations of the geological periods, the pro-
gressive salinity of the ocean, the absence of salt or muriatic acid in
the inclusions of the last-formed primary quartz, the passing of
fish from fresh to saline water, the sea containing in early times
some phosphate of lime and more of lime than soda, the salinity of
fresh water, geological time, the Caspian anciently freshwater, the
gradual decrease of lime in the sea, carbonic acid in the economy of
nature past and present, hypotheses of the developmental condition
of early marine beings, the relationship of the oldest recognizable
land-plants to sea-weeds, the genealogy.of the vegetable kingdom
(table, p. 140), the differences between Monocotyledons and Dico-
tyledons explained by their developmental history, carbonaceous
sediments in the sea, proofs of the oceanic life-habits of all coal-
making plants, and refutations of erroneous hypotheses of the for-
mation of coal. This last subject is very fully treated in Chap. XI.
under more than forty headings. Arguing throughout on premises
of his own making, the author satisfactorily arrives at his own
conclusions, which are far from being in accordance with the views
of geologists and botanists of the present day.
MISCELLANEOUS.
On the Operculum of the Gasteropoda. By M. Hovssay.
In 1825 Blainville wrote, in his ‘Manuel de Malacologie,’ as
follows :—
**The operculum is evidently the production of the skin which
Miscellaneous. 305
covers the foot. ... But how does a flat oval or circular surface
produce a material which rolls into a spiral, often in a very regular
manner, and sometimes forming a great number of turns? It is
a question which it really seems to me very difficult to answer,
perhaps especially because it has not been sufficiently studied.”
In 1829 Dugés endeavoured to fill up this gap, but, considering
only opercula detached from the animals, he arrived at the false
conclusion that the operculum is a production of the mantle. The
authors who have followed him have scarcely attempted to do more
than try to find ont with what part of the Acephala the operculum
was homologous ; but, as they had no basis for their argumentation,
they arrived at the most contradictory results, some regarding it as
the homologue of the second valve of the Lamellibranchs, others,
like Lowén, comparing it with the byssus.
The foot alone is implicated in the formation of the operculum,
and I have set myself to determine precisely what parts of this
organ excrete the material, and how the growth of the operculum
takes place. Contrary to what is generally supposed, I have
ascertained that the whole surface of the foot does not take part in
the production, but only a very clearly defined small portion.
I shall give the name of the columellar margin of the operculum
to that which lies on the side of the columella when the animal is
withdrawn into its shell, and that of parietal margin to the opposite
part. The operculum presents an internal and an external surface;
it is necessary to distinguish them, as they have not the same mode
of formation.
Let us first of all see to the external part. It presents on its
surface strie of variable form according to the genera under
examination. On examining carefully a Littorina, a Murex, or a
Purpura, we observe, quite close to the columellar margin of the
operculum, a small transverse fissure which penetrates about
1 millim. into the thickness of the columellar muscle, and which
occupies the whole length of the foot. The walls of this pedal fis-
sure are lined with a peculiar epithelium, folded, or rather goffered,
so as somewhat to resemble the polypary of a Meandrina. We
see within it a very delicate and very flexible transparent lamella.
With a fine needle this lamella may be taken out, when after
remaining for some time in the air, it dries and acquires a horny
appearance.
By making sections we find that the epithelial cells of the fissure
excrete a structureless material, of a yellowish colour, and strongly
refractive, which, by ag elomeration, constitutes the hyaline lamella.
The latter issues from. the pedal fissure and adds itself to the old
operculum.
The newly formed parts apply themselves to the epithelium
situated between the fissure and the parts of the operculum which
are already fixed. At this poiut the epithelial cells are but feebly
adherent to each other, and only by their basal part, a remarkable
exception among epithelia, From this it results that the still
plastic opercular material invests these cells, and even diffuses itself
306 Miscellaneous.
somewhat among the elements of the subjacent tissues (muscular
fibres and conneccive cells). It is thus that, by successive
appositions of new parts issuing from the pedal fissure, the striz
are formed, of which only the most salient are visible to the naked
eye or the lens.
On the other surface of the operculum we must distinguish two
regions, the surface of insertion of the columellar muscle, and the
free internal surface. It is very easy to see that the free inner
surface and the outer surface of the operculum have not the same
constitution. The inner surface is covered with a homogeneous layer
which forms, as it were, a varnish without any strie perceptible to
the eye. This coating may even be so thick that we cannot see
through it the striz of the other surface (Murex). In other cases
it is delicate enovgh not to hide them (Littorina, Trochus). This
difference of constitution arises from a difference of origin. In front
of the surface of insertion the metapodinm forms an anterior expan-
sion or lip, which, during the life of the animal, is constantly applied
against the inner unattached part of the operculum. The epithelial
cells of this anterior lip produce the varnish.
It still remains to ascertain why the opercular material is rolled
into a spiral. To elucidate this point we must study the muscular
impression. As the operculum grows, the surface of insertion of
the operculum is displaced with a slight movement of rotation,
since during the same time the shell grows in a spiral. The
muscle attaches itself to the newly formed parts, abandoning the
old parts on the side of the parietal margin. These stages of the
columellar muscle are marked by strixw independent of those of the
superior surface. We observe them when preparing an operculum
after removing all traces of muscle. By studying these lines we can
even understand why there are opercula of which the form always
remains the same, while there are others of which the form varies
with the age of the animal. The latter are said to have a nucleus
of formation. The posterior secreting portion of the foot always
retains the same form in tlfe first case, whereas in the second we
see it from nearly circular become almost straight.
Thus we see that the operculum is a production of a definite
portion of the epithelium of the foot, and appears to be very
different from the byssus of the Acephala, which is produced by a
highly developed gland occupying a good part of the volume of the
foot. It is still more different from the second valve of a shell.—
Comptes Rendus, January 28, 1884, p. 236.
A Fungus infesting Flies.
Prof. Leidy directed attention to a vial filled with flies adherent
to fragments of leaves. He stated that on the Ist of August, the
last summer, he had noticed that from the swarm of flies that
were attracted by the ripe fruit of a black mulberry, Morus nigra,
many settled on the underside of the leaves, and there became fixed
and died from the invasion of a fungus, in the same manner as the
Mi'scelianeous. 307
house-fly often becomes attached to walls and window-panes, in the
autumn, through the agency of the fungus known as the Sporendo-
nema. The infested flies on the mulberry-tree were so numerous,
that perhaps a fourth of the foliage of the lower boughs had from
one to half a dozen of the flies adherent to each leaf. The fly,
though a familiar one, is unknown by name to him. It resembles
the house-ily, but is larger and has a black abdomen, with lateral
whitish spots. The fungus, of a fuscous hue, is especially evident
in the extended intervals of the segments of the abdomen, along the
sides of the thorax, and at the neck. Though extending to and
attaching the flies to the leaves, the specimens no not exhibit the
zone of spores on the leaf, as commonly seen in those of infested
house-flies. Microscopic examination exhibited a similar structure
of the fungus to that of the Sporendonema or Empusa musce. It
mainly consists of translucent cylindrical, straight or somewhat
tortuous rods or tubes of yariable length with rounded ends, and
containing homogeneous liquid with rows of oil-like globules.
Mingled with the tubes are numerous oval, ovoid, and pyriform
spore-like bodies, usually each with two oil-like globules. The
spore-like bodies measure 0-028 to 0-036 millim. long by 0-016
millim. thick. The longer tubes measure usually up to 0:16 millim.
long by 0°012 millim. thick.—Proc, Acad. Nat. Sci. Philad., Dec.
1883, p. 302.
On the Occurrence of Colobus Kirkii.
We have received the following communication from Sir J. Kirk
regarding this monkey ; it is dated from Zanzibar, Feb. 16th :—
‘In the Proe. Zool. Soc. Feb. 1868, p. 27, Dr. Gray described a
new Colobus, and named it after me. That monkey then was rare,
but still to be had in many of the wooded districts of this island.
I am not aware that it has been found in Pemba Island or on the
mainland; and now I discover that, if not extinct, it has become so
rare as not to be procurable, even when I sent the hunters over the
islaud. I have a report that it exists still in one spot which they
could not reach. I think two specimens were sent to Germany some
time ago; but it looks as if the animal will be lost. This is due to
the destruction of forest and jungle over the island.”
Polythalanua from Inland Salt Water in Hungary.
By Dr. Even von Danay.
The author has found, in a mass collected from a salt pool near
Déva, in Transylvania, examples of Polythalamia, the shells of which
show no traces of calcification, but consist of a yellowish chitinous
substance, on the surface of which numerous little plates of quartz
adhere. Probably the Polythalamia found near Déva are the repre-
sentatives of a living continental species ; but the author leaves this
to be settled by further investigation Math. naturwiss. Berichte
aus Ungarn, Bd. i. p. 357.
308 Miscellaneous.
On the Sexual Differences of Corcebus bifasciatus, and on its
supposed Ova. By M. A. Lapoursine.
The Buprestid, Corwbus bifasciatus, which is exceedingly inju-
rious to the evergreen oak in the south of France, has been reported
upon by MM. Régimbeau * and De Trégomain 7. The author finds
that the organ described by these writers as an ovipositor is in
reality the male organ! The female Corabus has a simple oviduct.
M. Régimbeau describes certain bodies as ova, most of which the
author regards as fecal masses; while M. de Trégomain notices the
occasional presence in the galleries in which the beetles undergo
their metamorphoses of great quantities of eggs, “some nearly
spherical, others somewhat oval, about 0-07 millim. in diameter, of
a yellow colour, and slightly translucent.” In some cases these
eges presented “ whitish lineaments.” M. de Trégomain thinks
that if they are the ova of Corwbus they must be unfecundated, as
the insect is always alone in its gallery.
The author confirms the description and figures given by M. de
Trégomain, and adds that he has found upon pup which died before
completing their metamorphosis oviform bodies, varying in size from
+ millim. to 0-82 millim. They were of an amber colour, and some
of them presented whitish lines and even spots. These, he thought,
could not be true ova, and rather believed that they were vesicular
Ascomycetous Fungi developed upon the dead insects; and the
microscope showed a few filaments of mycelium.
He goes on to say :—‘‘ On observing these oviform bodies with
the microscope, I constantly found with them some Acarina perfectly
recognizable by their rostrum, legs, &c. Further, these oviform
hedies. when crushed or subjected to the action of various reagents
(prolonged maceration in glycerine, staining in carmine), showed
in their interior true ova in various stages of development. The
smallest of these ova were rounded; the largest had acquired an
elliptical form; their average size was in the greatest diameter
0-10 millim. and in the other 0-075.
‘Carefully examining the position of the mite relatively to the
oviform bodies, I ascertained many times (with M. Rémy, chief of
the Laboratory of La Charité) that the posterior part of the body of
the mite was prolonged into a globular abdomen, and was attached
to it by chitinous rods. The oviform body was in reality only the
abdomen more or less vesicularly dilated, strengthened by chitinous
threads, three on each side, and filled with the ova of a mite,
attached to the pupa of the Corebus.
«The conclusion that forces itself upon one is as follows :— A mite
(the species of which will be hereafter determined, and which is
allicd to Tyroglyphus) occurs in the galleries upon dead pupe of
Corebus bifasciatus. This mite is remarkable because its abdomen
becomes dilated into a large vesicle and filled with ova. ‘The abdo-
* “Le Corebus bifasciatus, ou Bupreste ravageur du Chéne vert’ (1876).
+ ‘Les Insectes du Chéne vert’ (1876).
Miscellaneous. 309
minal development, which is peculiar to this Acarine, and has not
previously been indicated in the Arachnida of this group, resembles
that occurring in the female termites, and especially in the females
of the Chigoe (Dermatophilus or Pulex penetrans) of the tropics.” —
Comptes Rendus, February 25, 1884, p. 539.
New Contributions to the Knowledge of the Rotutoria.
By Dr. Evern von Dapay.
After devoting several years to the study of the Hungarian Roti-
fera, especially those of Transylvania, the author in 1882 visited the
group of pools in the Mezéséy, and found in the Mezé-Zdher pool
several new species, one of them representing a new genus. ‘The
following are the characters of these new forms :—
Genus Bracutonus, Ehr.
Brachionus Margot, n. sp.
Testula levi, oblongo-ovata; frontis dorso processibus quatuor,
mediis longioribus, basi inflatis, acutis; lateralibus brevioribus,
arcuatis ; ventri margine undulata, medio excisa; postice utrin-
que latere processu longo, acuminato ac valde arcuato; apertura
pedis bidentata. Long. corp. 0°5—-0°8 mill.
Collected on the frothy surface of the large pool near Mezé-Zah,
where it occurred pretty abundantly with small Crustacea and the
following Rotifera. It most nearly approaches Brachionus amphi-
ceros, especially as regards the processes of its carapace; but in
that species the processes are all of equal length, while they differ
in length in the new one. The essential distinction between the
two species is to be sought in the rotatory organ, the musculature,
the jaws, and salivary glands. The new form is named in honour of
Prof. T. von Margo.
Genus ScH1zocERca, n. gen.
Novum genus e Brachionorum familia; testa levi; oculis duobus
conjunctis sessilibus; pede longo, cylindrico, apice magnopere
fisso, furcam longam efficto, ramis apice dentibus duobus in-
zequalibus instructis.
Schizocerca diversicornis, 0. sp.
Species unica, charactere generis. Corpore elongato, fronte latius-
culo, postice parum attenuato; testa levi, frontis processibus
quatuor, mediis parvis, basi inflatis, marginalibus elongatis, acutis,
arcuatis ; ventri margine medio excisa ; mucronibus duobus posti-
cis ineequalibus, dextro multo longiore, acutiore inflexoque, sinistro
breviore, latiore. Long. corp. 0°15—0-2 mill.
Occurs frequently in the pool of Mezé-Zih. Resembles Brachi-
310 . -Miscellaneous.
onus in internal organization, but differs so much from the Brachi-
onea, and, indeed, from all Rotatoria, in the structure of its foot,
that the author regards it as the type of a new genus.
Genus ASPLANCHNA, Gosse.
Asplanchna triophthalma, un. sp.
Corpus truncato-ovatum ; ocellis tribus, duobus marginalibus, uno
majore collari; organo rotatorio simplice, parum undulato; fronte
organis tentaculatis; pede anoque caret. Long. corp. 0°8-1:2
mill.
This is also found abundantly in the froth of the surface of the
great pool near Mezo-Zah. It is one of the largest of Rotifera, and
very similar to Asplanchna Sieboldii (Notommata Siboldii, Leyd.) in
the form of the body, the digestive apparatus, and the ovary. But
the nervous system, the aquiferous vessels, and the construction of
the rotatory organ show such considerable differences that the author
has no hesitation about separating the two species, and he gives the
new one the name of Asplanchna triophthalma, because besides the
frontal eye, seated upon the cesophageal ganglion, it possesses two
other smaller eyes placed at a distance from the ganglion and pro-
vided with visual nerves. The male of Asplanchna Sieboldii pos-
sesses on each side of its body a triangular process; but no such
appendages occur in the male of the new species.—Math. naturwiss.
Berichte aus Ungarn, Bd, i. p. 261,
On the Develoz ment of the Comatule. By M. E. Prrrirr.
To arrive at a strict determination of the different parts which
constitute an adult Comaiula we have endeavoured to ascertain, by
means of materials kindly furnished to us by Dr. Viguier, of Algiers,
what is the organization of the animal at the three phases:—1, of
Cystidean ; 2, of Pentacrinus; 3, of free Comatula, but not yet
adult.
1, At the close of the Cystidean phase the young Comatula still
possesses only buceal tentacles and no arms. Its digestive tube forms
a half spiral, and presents an anus situated upon the side of the
body. Around the mouth there is an annular canal into which the
buccal tentacles open. A short tube, bent into a V, starts from the
annular canal, traverses the wall of the body, at the same time
slightly changing its structure, and becoming united with the sur-
rounding tissues, and then opens exteriorly by a pore situated upon
the wall of the body. This tube has been compared with the hydro-
phorous canal of the Holothuriz, which is itself regarded as homo-
logous with what is called the sand-canal in the Sea-urchins,
Starfishes, and Ophiurans. It serves indubitably to introduce water
into the tentacular apparatus ; but we must make the most express
Miscellaneous. 311
reservations as to its homology with the sand-canal of the other
Echinodermata.
The peduncle of the young animal contains six cellular cords—
one central and five forming around the central cord the edges of a
pentagonal prism, the axis of which it would occupy. The central
cord is prolonged into the inflated part of the body, in such a way
as to occupy the axis of the spiral formed by the digestive tube,
and its cellular walls become thickened so as to form an ovoid body,
the large cells of which, in sections, are always arranged in two
contiguous series, so that the ovoid body is filled up. This body is
surrounded by a fibrous envelope, and becomes united at its upper
part with the wall of the pharynx. It occupies exactly the same
position, relatively to the digestive tube, as the sand-canal of the
Sea-urchins.
The five cords which surround the axial canal are slightly in-
flated at their entrance into the body properly so called; a cavity
makes its appearance in their inflated region; from this results the
formation of five chambers, which constitute the first trace of the
chambered organ. Cellular buds, starting from the apex of these
chambers, soon arrive, by creeping along the walls of the body, at the
cireumbuccal canal ; the latter forms a bud at the point of meeting ;
the two buds then bear towards the exterior; the wall of the body
forms a sort of cap for them, and all these parts, increasing in size
together, finally constitute an arm. The five arms do not make
their appearance simultaneously, but successively, and still continue
to show great difference of size during nearly the whole duration
of the following phase. Their growth is executed from the com-
mencement as indicated in our communication of the 16th July.
2. The Pentacrinoid phase extends from the appearance of the
arms to the complete-formation of the cirri. At this moment, in
consequence of the development of the arms, the oral surface of the
larva, which was at first entirely occupied by the tentacular ring,
has become considerably enlarged, and the anus has been shifted
into it; it opens henceforward at the apex of a special tube. This
surface is cut up into five sectors by the tentacular canals, which
run towards the anus. Upon each of these sectors there is seen a
hydrophorous orifice, resembling the single orifice of the preceding
phase, and to each of these five orifices there corresponds a hydro-
phorous tube. In sections these five tubes appear to terminate by
a free extremity in the general cavity ; but we have reason to think
that these tubes are normally in continuity with tho five canals
which traverse the wall of the body to terminate at the five hydro-
phorous orifices.
The ovoid body which traversed the axis of the general cavity has
now the aspect of a double canal, the two parts of which seem to open
into the pharynx, a point, however, which still needs further investi-
gation. The chambered organ has acquired very nearly its definitive
form. At its level, in those individuals of which the arms are not
yet much developed, we see originate from the central peduncular
ale Miscellaneous.
cord clavate buds alternating with those of the arms. These buds,
taking a direction downwards and outwards, soon reach the integu-
ments. The latter become inflated and elongated over them, and
then these various parts, growing together, finally constitute a cirrus.
The cirri consequently have no true homology with the arms; they
originate from the central cord of the peduncle, and the arms from
the five peripheral cords. At this age there is no trace of a vascular
apparatus, and the axial organ retains very nearly the histological
structure of the ovoid organ of the preceding phase.
3. At the moment when the young Comatula becomes detached
the digestive tube has formed new folds around the axial organ.
The hydrophorous tubes have considerably increased in number ;_ but
we observe the same relations between them and the canals which
traverse the wall of the body to open externally. The axial organ
has still the exclusively cellular structure which it has constantly
presented up to this point; but its walls bend inwards into rolled
lamelle which pretty closely remind one of the arrangement of the
sand-canal of the starfishes. This organ terminates below in a
conical tube, which, constantly narrowing, penetrates into the axis
of the chambered organ.
The trabecule of connective tissue of the general cavity are very
numerous, and some of. them which are attached to the envelope of
the axial organ might be taken for vessels, but there exists nothing
that can be designated by that name. Through the vacant spaces
which exist between these trabecule there run a few solid cellular
cords which indirectly pass to the arms. The cellular tissue which
envelopes the chambered organ is extremely thick and has quite
the aspect of a tissue engaged in rapid multiplication. This tissue
is produced into the centre of the calcareous axis of the arms,
and already presents all those connexions which we have formerly
described with the muscular tissue and the connective tissue of the
arms.
To sum up, at this age the pores which place the general cavity
in communication with the exterior may be regarded as the orifices
of hydrophorous tubes, with which they are connected at once by
their number and position; these tubes, perhaps homologous with
those of the Holothurians, by no means correspond to the sand-canal
of the other Echinodermata ; this sand-canal, on the contrary, seems
to be represented by the axial organ of the Comatule, which pos-
sesses at once the structure of the sand-canal of the starfishes and
the position of the organ of the same name in the sea-urchins.
This organ is evidently in relation with the nutrition of the cirri,
the origin and nature of which are very different from those of the
arms.—Oomptes Rendus, February 18, 1884, p. 444.
THE ANNALS
AND
MAGAZINE OF NATURAL HISTORY.
(FIFTH SERIES.]
No. 77. MAY 1884.
— ————
XXXV.—The Classification of the Animal Kingdom, with
reference to the newer Zoological Systems. By Dr. T.
Marco *,
THE sum of our knowledge of the anatomical and histological
structure as well as the development of different animals
has advanced of late years with wonderful rapidity. In
accordance with this the views of zoologists as to the classi-
fication of the animal kingdom have also changed continually.
It is therefore no wonder that with such frequent alterations
of the system younger naturalists, who may be inclined to
regard the system as the foundation of the science, find them-
selves at first in no small difficulty, until, subsequently, after
they have penetrated more deeply into the interior of nature,
and recognized the essence of zoology more accurately, they
arrive at the right view, that in reality classification or taxo-
nomy is by no means the foundation of the science, but
rather only the roofing-in of the structure raised upon the
foundation of morphology and embryology.
As the main cause of the vacillations nowadays apparently
occurring in classification we must undoubtedly regard only
* Translated by W. 8S. Dallas, F.L.S., from the ‘Mathematische und
naturwissenschaitliche Berichte aus Ungarn,’ Band 1. pp. 234-260 (1883),
Ann. & Mag. N. Hist. Ser. 5. Vol. xii. 21
314 Dr. T. Margé on the Classification
the enormous advance lately observable in the domain of mor-
phology and embryology, an advance which from year to
year becomes more and more evident by the discovery and
exact observation and demonstration of new facts of great im-
portance to science, which naturally lead to changes, modi-
fications, and rectifications of opinion. From this it is easily
understood why we meet with different systems in the different
treatises and manuals of zoology, and how, even with the
same naturalist, the system may change essentially from time
to time.
Thus, for example, Huxley’s system of the year 1875 is
essentially different from that followed by him at a later
period (1878) ; for while this naturalist formerly adopted the
formation of the embryonal nutritive cavities, the mouth, and
cceloma as the foundation for a phylogenetic grouping of
animals, and accordingly divided the Metazoa into Archeo-
stomata and Deuterostomata, and the latter again, in accord-
ance with the mode of formation of the coeloma, into Kntero-
coela, Schizoccela, and Epiccela, and consequently the whole
animal kingdom into twenty-six stems or phyla*, the same
author, some years later, leaving the phylogenetic point of
view and the descent of animals entirely out of consider-
ation, divided the whole animal kingdom, exclusively from
morphological types, into eight large typical groups. We
find similar alterations also more or less in the classifications
of Gegenbaur, Ray Lankester, Claus, &c.
Further vacillations of many kinds may also be produced
in the system by the circumstance that the individual views
of the different naturalists as to the value and usefulness of
the facts ascertained by observation sometimes do not exactly
agree, by which means the combinations and deductions from
those facts may often lead to quite different final results.
But if we consider not so much these combinations, but rather
the already ascertained facts which constitute the proper sub-
ject, the true foundation of classification, we come without
much difficulty to see that the systems, however different
they may be, nevertheless contain many generally admissible
truths, which are raised beyond the least doubt.
We may consider animals like all other natural objects—
treat them systematically or group them from different points
of view, and combine them at pleasure into a system. very
zoological system, if it be objective and founded upon already
demonstrated facts, has its justification, and when considered
from a certain standpoint may have its value and use. ‘Thus,
* Huxley, “On the Classification of the Animal Kingdom,” in Quart.
Journ. Micr. Sci., January 1875,
of the Animal Kingdom. 315
as is well known, there are Natural-history systems, such, for
example, as the systems of the old school, which were chiefly
founded upon the external form and vital relations of the
animals. There are systems chiefly founded upon anatomical
facts, such as the system proposed at the beginning of the
present century by Cuvier, who divided the whole animal
world into four principal types (Vertebrata, Mollusca, Articu-
lata, Radiata) ; and there are also systems established upon
embryological facts, such as that of C. Semper, who, as is well
known, has quite recently attempted to determine accurately
the relationships of animals according to the embryonal prim1-
tive kidneys or segmental organs, and to classify the Metazoa
phylogenetically upon this exclusively embryological basis *.
The discovery of segmental organs (primitive kidneys) in
the embryos of sharks, for which we are indebted to Professor
C. Semper, and in part also to the English embryologist F.
Balfour, is doubtless so far of great importance to the trans-
formation-theory, that it furnishes a fresh proof of the fact
that the Vertebrata and Evertebrata, namely the Vermes,
possess in common organs which are homologous from a
morphological point of view.
It is, however, questionable whether it is permissible to
ascribe to the above-mentioned organs so great an importance,
and to found upon them exclusively a classification of the
entire animal kingdom. I would ask, is the relationship
between the other Vertebrata and the Annelida really greater
than between the other Vertebrata and Amphioaus, or between
this latter and the Ascidia?
Many zoologists believe that they can give science a new
direction by selecting according to their judgment one of
the embryonal organs, or any phenomenon of the embryonal
organism, in order to found upon it a phylogenetic classifica-
tion, in the hope of being able in this way to establish a
natural relationship of the groups of animals. We may
readily admit that embryonal characters are of greater value
in taxonomy than characters of the fully developed animals
derived from anatomy or biology, as in the latter the characters
may much more easily suffer change by adaptation and change
of function; but we think we may assert with certainty that
embryonal characters taken by themselves (even if they relate
to the most important organ of the embryo) are far from being
sufficient for the sure establishment of the descent of one of
the smaller groups of animals, and still more of the whole
animal kingdom.
* ©. Semper, ‘Die Verwandtschafts-Bezichungen der gegliederten
+ Thiere’ (Hamburg, 1876), 2 vols. 918
316 Dr. T. Margé on the Classification
We think that we must speak in the same way of the
system made known by M. A. Giard*. This zealous and
otherwise distinguished zoologist, as is well known, took as
the basis of his new classification of the animal kingdom the
amnion, that is the embryonal envelope originating from the
ectoderm, and so, according as the embryos possess or are
destitute of such an envelope, divided the Metazoa into two
great groups (Hymenotoca and Gymnotoca). But that the
presence or absence of an embryonal envelope can by no means
serve as a proof for or against genealogical relationship, and
therefore cannot suffice for the establishment of a grouping of
the animal kingdom resting upon natural affinity, will be at
once seen by any one who will compare with each other all
the different groups of animals, such as the Vertebrata, ‘Tuni-
cata, Arthropoda, Echinodermata, Acanthocephala, ‘Trema-
toda, Cestoda, Turbellaria, and Nemertina, which Guard
united in the group of the Hymenotoca on account of the
embryonal envelope observed upon their embryos, although in
every other respect many of them stand very far apart. Obser-
vation shows us, moreover, that even groups of animals, e. g.
fishes, amphibia, reptiles, birds, and mammals, which demon-
strably belong to one and the same natural stem, differ from
each other in this respect, that while some of them (mammals,
birds, and reptiles) during their embryonal existence are in
possession of an amnion, others, on the contrary (Amphibia
and fishes), are quite destitute of any thing of the kind.
From this, however, we may evidently conclude that the
amnion, or the embryonal envelope, where it is actually
present, is to be regarded as originally not an inherited cha-
racter, but one acquired by adaptation. As such it might
originate, under the action of exactly similar conditions in
quite divergent animals, even belonging to different stems,
and quite independently of each other. It would therefore
be very precipitate to conclude at once as to the true relation-
ships of animals, in all cases, from the presence or non-presence
of such a character.
We must therefore regard all the different endeavours of
systematists to group animals exclusively in accordance with
one character, whether morphological, embryological, or bio-
logical, external or internal, as mere experiments,—such a
grouping or classification of animals can never be the true
expression of their natural affinities.
It was an error on the part of L. Agassiz to attempt to
group the fishes according to the form and structure of their
scales into cycloid, ctenoid, ganoid, and placoid fishes, or
* ‘ Revue scientifique de la France et de l’étranger ’ (1876), no. 38,
of the Animal Kingdom. 317
when the same naturalist referred the Vorticelle to the group
Bryozoa merely from their external similarity, without at all
taking into account the important differences in their structure
and development; and the classifications of the Medusz at-
tempted by Gegenbaur according to the presence or absence
of a velum (Craspedota and Acraspeda), by Forbes * with
exclusive reference to the marginal corpuscles (Steganoph-
thalmata and Gymnophthalmata), and by Eschscholtz fT ac-
cording to the position of the generative organs (Phanero-
carpe and Cryptocarpe) are equally unsatisfactory.
There is consequently no doubt that for the foundation of
a truly natural or so-called phylogenetic classification the
knowledge and consideration of the individual peculiarities is
not sufficient, however important these peculiarities may be,
or however early a period of development they may pertain to.
The distinguished naturalist Fritz Miller, in his exceedingly
valuable little work ‘ Fiir Darwin,’ has given us a perfectly
new systematic grouping of the Crustacea according to one of
the earliest embryonal characters, namely the segmentation
and the mode of curvature of the embryo within the egg
(Holoschista and Hemischista, Gasterotropa and Nototropa) ;
but he thereby furnished a proof that the groups proposed by
him were any thing rather than natural groups {.
Among all properties of animals the biological conditions
especially offer the least certainty in their classification, as
even animals of admittedly different origin frequently live
under exactly similar conditions, and in accordance with this
not unfrequently also exhibit the same peculiarities. Thus,
for example, the Cetacea and fishes live under exactly similar
conditions, and therefore we find, in consequence of adapta-
tion, not only the external form, but also the organs of motion,
similarly formed, although, in fact, they are by no means
nearly allied to one another. But even among the great
marine Mammalia, according to recent investigations, the
Sirenia prove to be essentially different from the true whales
or Cetacea; and yet both forms of animals are externally so
similar as to be confounded together, and they live under
exactly the same conditions.
* Forbes, ‘Monograph of the British Naked-eyed Medusee’ (London,
1848).
ji Hechecholta, ‘System der Acalephen’ (Berlin, 1829).
{ [Leipzig, 1864. English translation under the title of ‘Facts and
Arguments for Darwin’ (London, 1869). The classification here cited
is given by Fritz Miller ironically, to show to what results the yin 3
tion of certain authoritative dogmas would lead in the case of the Crus-
tacea— TRANSL. ]
318 Dr. T. Marg6 on the Classification
Tn order to avoid as far as possible these and similar errors
all earnest and prominent systematists seek the true character
of a group of animals (species, genus, family, &c.) not in its
individual peculiarities, but in a certain combination of all
characteristic peculiarities ; that is to say, they found the cha-
racter of the group upon a correctly combined summing-up of
all its peculiarities, and, indeed, so that in each individual
case the combined sum of the peculiarities always represents
a definite animal-form, although the latter must not necessarily
be assumed to be so unchangeable as was usual with the
systematists of the old school.
Nowadays, therefore, it could not occur to any thorough
naturalist or earnest systematist to classify any group of
animals in accordance with any exclusively external or inter-
nal peculiarity observed either in an embryo, or in a larva, or
in fully developed animals, with any one organic or biological
condition.
If we now put the question, how 7s a correct and really
scientific classification of the animal kingdom to be created?
we may be permitted, in connexion with this, to assume as a
principle that a classification which, being based upon mor-
phological and embryological facts, also takes sufficiently into
account the paleontological and biological data, and carefully
follows these facts step by step, must in any case lead with most
certainty to the final aim of science. ‘This final aim is, how-
ever, nothing else than the knowledge of the law in accordance
with which, by means of inheritance and adaptation, animals
have originated from each other. If this be correct (as to
which, in the light of Darwin’s law of development, we cannot
doubt for a moment), then such a classification of the animal
kingdom, such a system, can alone be accepted as perfectly natu-
ral, objective, and strictly scientific, which is capable of repre-
senting, in the formof a genealogical tree, the origin and gradual
development of the world of animals.
Another question is, whether this ideal goal of our science
will some day be really attainable, even after the labour of many
generations. Among the younger zoologists there may per-
haps be some who esteem it possible to attain to such a goal ;
but if we seriously consider the many difficulties of this
gigantic task and the insurmountable obstacles presented to
it In certain directions, we must perhaps give up the hope
that man, who in so many respects is able to govern nature,
will really ever be in a position to construct a perfectly ob-
of the Animal Kingdom. 319
jective and truly phylogenetic system of nature. For the
present, however, we may be content with the result if we
succeed in approaching this final aim as nearly as possible,
and in course of time at least in constructing such a system
as will represent in part, although not perfectly, the true
genealogical tree of the animal kingdom.
We will here at once look somewhat closely into those
difficulties and obstacles which may not unfrequently confront
the naturalist in his zealous endeavours to determine accu-
rately the relationships of animals, and which readily give
rise to errors.
1. Sometimes the difficulty may consist in this, that in the
case of organisms with accordant structures one may not un-
frequently be inclined to conclude, from the similarity of
structure, that they are true blood relations, and further that
this affinity must be closer the greater their similarity of
structure is found to be. The cautious naturalist, however,
will soon perceive that this principle, if very generally applied,
easily leads to errors, for in judging of a true blood-relationship
that resemblance only can be of value which is produced origi-
nally by inheritance, but not that in which the agreement in
structure has merely resulted from adaptation to similar vital
conditions.
The judgment of these circumstances may sometimes appear
very difficult, in many cases even impossible. This, then, is
a difficulty which may easily lead the Zoologist astray by
uniting in one and the same branch of the genealogical tree
animals which are bound together by no close family tie, and
this merely because they show an accordant structure, or
because their larvee or embryos prove to be more or less alike.
In phylogenetic classification therefore the zoologist must
above all be able to distinguish well and accurately the homo-
logy originating by inheritance, or the so-called homogeny,
from a similarity produced by adaptation or homoplasy*.
Observation shows that by the action of similar conditions
of life, and therefore merely by adaptation, similar and some-
times almost exactly identical organs may often be developed
in animals which belong to perfectly distinct types or natural
groups. As examples of this we may cite the chele occurring
on the legs of crabs, and the palpi and chelicera of scorpions,
as well as the pedicellariz of the Echinodermata, all of which
show a wonderful agreement both in structure and function,
although no one would venture to assert that they have actu-
ally originated from each other by inheritance. In homo-
* Ray Lankester, ‘On the use of the Term ‘ Homology,’ in Modern
Zoology,” Ann. & Mag. Nat. Hist., 1870.
320 Dr. T. Margé on the Classification
plasy or adaptive homology we also find the explanation of
the formation of segments which occurs in many Platyel-
mintha, which therefore, as a simple phenomenon of adaptation,
ean by no means be equivalent to the metamere-formation of
the Annelida. As a homoplasy of the same kind we also
regard the resemblance between Rotatoria and Crustacea,
which is erroneously interpreted by some authors, as well as
that between the bills of birds and the maxillary horny
sheaths of the Chelonia, and many others. Many erroneous
views in this respect have already been refuted by more
accurate investigations.
2. In consequence of Darwin’s researches it is generally
recognized as the law of development in the organic world,
that all organisms, animals as well as plants, are in a state
of constant, although very slow, change and progressive deve-
lopment, so that, in general, the effort to attain greater perfec-
tion ts predominant in the organic world. Fyrom this con-
stantly advancing progressive movement of phylogenesis
many have erroneously concluded that all the simpler organ-
isms living at the present day are only the representatives of
similar animals which have continued in existence from an
earlier period, and that consequently those natural groups to
which they belong have never been at a higher stage of
organization than that upon which they now stand.
In accordance with this principle many were at first of
opinion that the whole animal kingdom, as well as its larger
and smaller groups, might be quite simply embraced in several
ascending series, just as these, in consequence of constant
and unceasing advance towards perfection, had gradually
become developed from the lowest to the highest stage of
animal organization. It was soon found to be impossible,
however, to establish the true genealogical tree of the animal
kingdom upon this principle without falling into faults and
errors. For Darwin’s law of development, which in its final
results is certainly progressive, by no means eacludes a retro-
grade movement or retrogression in certain stages of develop-
ment, as life presents not only progressive but also retrograde
phenomena of movement, and absolute rest or unchangeability
(Stabelismus) is an impossibility in Nature as in social life.
In accordance with this law, by the action of unfavourable
conditions of existence, and by means of natural selection,
perfectly organized higher organisms may originate much
simpler forms, which are, so to speak, degenerated by retro-
gression, although for this very reason better fitted for and
corresponding to the new conditions of existence.
Of late the parasitic animals have been regarded as such
of the Animal Kingdom. 321
animal forms, as well as those which live under ground, in
mud, in dark caverns, and at great depths in the sea, or which,
firmly adhering to other bodies, are incapable of any locomo-
tion. We may refer here only to the Trematoda and Cestoda
among the Platyelmintha, which evidently are nothing but
the direct descendants of Turbellaria once leading a free
existence, but gradually retrograded in consequence of a para-
sitic mode of life. The Cirripedia and Rhizocephala among
Crustaceans, and the Linguatulides among the Arachnida, are
nowadays justly regarded as such animal forms produced by
retrograde metamorphosis, as alsothe Bryozoa, Brachiopoda, &e.
It may, however, not always be easy to recognize with
certainty the cases of retrograde phylogenesis, or degeneration,
and probably many forms which at present are ascribed to
retrograde metamorphosis may in course of time prove to be
progressive animal forms.
As in all other things, so also in science, man is inclined to
overstep the bounds of sober reason, and to assume or assert
& priort more than what facts directly prove. This applies
so much to the theory of retrogression or degeneration, so widely
diffused at the present day, that a natural philosopher has even
ventured to set up the proposition that all animal forms are
direct descendants of man, gradually degenerated by retro-
gressive metamorphosis !
Another view, which I believe to be erroneous, is also
entertained by some savants, namely, the opinion that the
formation of body-segments (metameres), or the repetition of
similar parts of the body, always leads towards the perfection
of the organism. In accordance with this assumption many
naturalists are inclined to derive the unsegmented animal-
forms, or those destitute of metameres, from supposititiously
more perfect and allied animals, in which the body was once
composed of numerous segments or metameres, and therefore
originally segmented. Prof. Semper, of Wiirzburg, as is well
known, has lately promulgated a similar opinion*,. namely,
that the Mollusca are to be regarded as the direct descendants
of the Annelida, and consequently that the unsegmented
Molluscan form has gradually been developed by retrograde
metamorphosis from the Annelidan form. While it is pos-
sible, or even probable, that in many cases the formation of
metameres, or the frequent repetition of equivalent parts, may
lead towards perfection, observation often seems to prove the
contrary. Thus, for example, among the Mollusca, we find
generally in the Cephalopoda and Gasteropoda not the smallest
trace of metamere formation (with the exception of the ex-
* Op. cit, supra, p. 315, note.
322 Dr. T. Margé on the Classification
tremely anomalous form of the Placophora or Chitonacea,
whose segmentation, moreover, is only external, imperfect,
and apparent), and yet these stand upon an indubitably higher
stage of organization than the Annelida composed of innume-
rable metameres. No one certainly will nowadays regard
the Myriopoda as higher or more perfect animals than the
Insecta or Arachnida, although in the latter it is the amalga-
mation of metameres that leads to greater concentration of
the organization and individual perfection. The same is
proved by the Vertebrata, the lower and less perfect forms of
which are in general characterized by a greater number of
metameres than the higher Vertebrata, the Amniota, which
have been gradually developed from them by means of pro-
gressive phylogenesis.
In organic nature, as in human society, the law seems
generally to prevail that, by the fusion of similarly con-
structed equivalent parts into larger complexes, an indivi-
dually higher potentiality and perfection of the general
organism always results. This is most strikingly shown to
us in the formation of the head out of a certain number of
metameres by the fusion of the anterior segments in the
Arthropoda and Vertebrata; while, on the other hand, a
frequent repetition of the more or less independent homolo-
gous parts or organs seems usually, in most organisms, to
indicate an organic inferiority.
For these reasons many, especially among the American
zoologists (A. Agassiz among others), justly regard the
greater concentration of the organism, the so-called ‘ cepha-
lization,” as the indication of a higher potentialization of the
organization, a higher degree of perfection ; and “ metame-
rization,”’ on the contrary, generally as the character of greater
inferiority in the organism ; so that the cephalized organisms,
as it were, represent centralized states, and the metamerized
mere federations.
All these considerations appear to be important and sig-
nificant when we have to do with determining the natural
position of an organism on the genealogical tree, and to state
exactly to what branch or twig it belongs, in accordance
with its affinities and derivations, and at which end (the upper
or the lower) of the twig it is to be placed.
We see this best in the case of the Tunicata. The most
esteemed and authoritative zoologists of the present day (Ge-
genbaur, Huxley, Ray Lankester, Giard, &c.) regard the near
affinity of these animals with the lowest Vertebrata, espe-
cially with Amphioxus, as completely demonstrated, and this
not alone because as regards their structure and development
of the Animal Kingdom. 323
the above mentioned animals are surprisingly similar, and
agree in most of their characters, but, above all, for the special
and important reason that there seems to be evidence that the
chorda which occurs in nearly all Ascidia in the larval period
(with the sole exception of the Molgulide) can by no means
be regarded as an organ acquired by adaptation during the
larval period, but as one which they have obtained originally
by inheritance from their formerly more perfectly organized
ancestors. We may therefore, from the transitory presence
of the chorda, and its, in most cases, complete retrogression at
a later period, draw the correct conclusion that the Tunicata
were not produced by progressive phylogenesis, but that they
must have originated by retrogression or degeneration from
other more highly organized ancestors, similar, but provided
with a fully developed chorda.
If we now suppose the case that of the known Tunicata
the Appendicularie and all those numerous Ascidia which
possess a chorda in the larval period had by chance disap-
peared without leaving any traces, we may ask, what proof
should we then have of the retrograde metamorphosis of the
Tunicata? It might then easily happen that we should place
them at the topmost stage of some lower but progressive series
of animals, and therefore classify them incorrectly in the
system.
It will be seen from this that for correct classification caution
and sober reason are above all necessary, especially in those
cases where we have to do with the accurate determination of
the relationships of an isolated group, with the development
and other essential peculiarities of which we are only imper-
fectly acquainted.
When we take all this into consideration it appears clearly
that side by side with progressive phylogenetic serves there are
also retrogressive series and groups, which, in spite of fre-
quently very divergent structure, may nevertheless not unfre-
quently be very nearly allied.
Darwin’s law of development justifies the assumption that
among the many partly progressive, partly retrogressive
series there must certainly exist one progressive develop-
mental series, which commences below with a perfectly simple
plastid and terminates above in man; but to decide which of
the numerous branches and twigs of the genealogical tree of
animals are truly progressive, or which of them owe their
existence to a retrogressive phylogenesis, can only become
possible in course of time, and then with any certainty, or at
any rate with probability, only upon the foundation of embryo-
logical and morphological investigations. So long, however,
324 Dr. T. Margé on the Classification
as we have no indubitable grounds or facts which directly
indicate the retrogression or degeneration of a given animal-
form or group, we shall proceed most securely in judging of
its derivation if we for the time assume it to have been pro-
gressive.
Nevertheless there are animals with regard to which we
may assume, if not with certainty at least with much proba-
bility, that they have originated by retrograde development
from other more perfect animals. Thus, among others, it
seems very probable that the Dicyemide, which EK. van
Beneden regards as an independent progressive animal-form
standing between Protozoa and Metazoa, and refers to the
group Mesozoa, which he has established, are really only
forms of some Platyelminth, degenerate in consequence of a
parasitic mode of life; just as the Myzostoma are Chetopod
worms degenerated by retrograde metamorphosis. It is, more-
over, probable, although not certain, that among the Protozoa
forms occur which possibly owe their existence to a retrograde
metamorphosis and have originated from Metazoa. Nay, the
possibility does not seem to be excluded that even the Polyps
and Corals belong to the retrogressive animal-forms, and per-
haps are nothing else than the peculiarly modified and dege-
nerated descendants of some originally free-swimming bilateral
form of worm. Even in the great group of the Vertebrata
it is a highly interesting question whether Amphioxus and
the Cyclostomt are not the descendants of some more highly
organized craniate Protovertebrate, constructed after the type
of the Monorhina, which has become in course of time entorely
extinct, and in which both the jaws and the paired limbs were
still wanting.
3. Besides the difficulties here mentioned which come in
our way in the classification of the animal kingdon, but which
seem to be superable sooner or later by further investigation
and unwearied labour, we must consider one obstacle, the
power of which the human mind will never be able completely
to overcome.
Thus, for a truly genealogical and phylogenetic classification
of the animal kingdom we need not only an accurate knowledge
of the existing forms, but also of those which have long since
been extinct, and, further, a comparison of these forms with
each other, for paleontological facts, as is well known, are of
no less value than the knowledge of the embryological and
morphological characters of living animals.
According to Darwin’s developmental law, we may con-
clude that very numerous ¢éransitional forms between the
different groups of animals must formerly have existed; this
of the Animal Kingdom. g2o
is the necessary condition, the natural result of the theory of
evolution. Matters are quite different, however, when we con-
sider existing nature. We see that existing animals are all
separated into larger or smaller groups, more or less removed
from each other. The individual members of these groups
frequently stand in very close relationship to one another, but
the groups themselves are generally separated by smaller or
larger intervals or gaps, and these gaps are now usually not
occupied by intermediate forms. Every isolated group in the
system, many families, orders, and classes furnish plenty of
examples of what has just been said. ,
It would be a great mistake if any one were to conclude at
once, from the total absence of intermediate forms, that such
had never existed in nature. As experience shows, it is only
in very rare cases and under favourable conditions that the
fossil forms remain quite unaltered, leaving out of considera-
tion the fact that a great number of them, such as the Ceelen-
terata, Tunicata, and Protovertebrata, as well as the greater
part of the Vermes, owing to their softer texture, could not,
even under the most favourable circumstances, leave any trace
behind them.
What great value attaches to the knowledge of paleonto-
logical facts, and how important it is for the determination of
the phylogenetic relationships between the different groups, as
well as for a correct classification, is best proved by the most
recent position of our system. ‘Thus the character or defini-
tion of the class of Birds appears something quite different, if
we take into consideration exclusively the existing forms, or
if we include the extinct Archwopteryx and the fossil Odont-
ornithes (toothed birds), lately discovered by Prof. Marsh in
North America, such as Hesperornis regalis and Ichthyornis
dispar. Not only in this class, however, but in nearly every
more or less isolated group, forms occur, the natural position
of which in the system can only be correctly determined by
comparison with the known paleontological types. If we
consider thegreat number of extinct forms the traces of which
are still unknown to us, we must regard the establishment
of a complete genealogical and phylogenetic system as still
impossible, considering the imperfection of our present pale-
ontological knowledge. Finally, if we think of those delicate
and soft animal forms whose traces are entirely lost, and which
therefore will for ever remain unknown to the naturalist, it
becomes more than probable that we shall really never be in a
position to establish and completely construct an absolutely
perfect genealogical tree of the whole animal kingdom.
For the present, however, we must content ourselves with
326 Dr. T. Margé on the Classtfication
the best attainable, and we may be satisfied with the result of
our labour if, supported on the morphological and embryolo-
gical facts already collected and ascertained, and considering
the known paleontological forms, we endeavour with our full
knowledge and conscientiously, by a systematic grouping of
the animal kingdom, to express, to the best of our power, the
relations existing between the different animals, as well as
the natural position of the groups and their individual
members.
Now that we have discussed in detail the general principles
of classification, as well as the precautions necessary for a
natural grouping of animals, I may be permitted, as a small
contribution towards the construction of a phylogenetic
system, to expound my views as to the relationships of the
different groups, although only tentatively, in the form of a
genealogical tree (see p. 334). In the grouping of the dif-
ferent stems, as well as in their relations to one another, this
agrees in many respects with others, but nevertheless, as
regards certain ramifications and groups of the genealogical
tree, it differs, not unessentially, from other similar attempts.
The following remarks may serve to explain and elucidate
our subject.
First of all I must notice particularly that, although the
denominations “ Protozoa’ and ‘ Metazoa’’ are almost uni-
versally employed in modern zoology for the two principal
groups of the animal kingdom, I think it would be better to
call the former “ Protoplastica,” as a word which expresses
more accurately and better the nature of these lowest animals ;
and the latter “ Blastodermica.”’ In these latter the body
never consists of one or more homogeneous protoplasmic cells,
but is always composed of heterogeneous cells and tissues,
which tissues are originally produced from two different
blastodermic cell- or germ-layers, namely, from the primitive
ectoderm and. entoderm.
The animals which are developed with such a blastoderm
(Blastodermica) divide, from a phylogenetic point of view,
into two main branches.
The smaller main branch is represented by those blasto-
dermic animals which, remaining at a low stage of develop-
ment, possess only a simple primitive nutritive cavity, formed
by the ectcderm alone, without any trace of a cceloma. ‘These
lower Metazoa (Blastodermica), which are nourished by
a primitive nutritive cavity (archenteron), we therefore name
“ Archentera.”
of the Animal Kingdom. 327
To the Archentera there belong, according to our views,
as separate ramifications or phyla, the Pordfera (Sponges)
and the Celenterata.
With regard to the Porifera or Sponges, I by no means
share in the opinion of those naturalists who regard these
animals somewhat as aborted or degenerated Anthozoa, and
who, partly for this reason and partly on account of the simi-
larity in structure and development, refer them to the stem
of the Ccelenterata. It is possible that they only form a
transition between the Protozoa and Metazoa, and perhaps
are nothing else than colonies or cell-stocks composed of
different kinds of cell-individuals, so that a part of the cells
have the duty of alimentation and reproduction, while the
other cells perform the functions of respiration and movement.
It is well known that Clark, referring to the presence of the
peculiar collared cells or flagellate cells which have hitherto
been found in no other blastodermic animals, has brought the
Sponges into direct connexion with the Flagellata, described
by him under the names of Salpingeca and Codosiga (= Cyl-
comastiges, Biitschli), and explained them as resembling
the colonies composed of Flagellata. This view may certainly
be very well brought into agreement with the still free-
swimming larve of the Sponges, but it most decidedly
contradicts the further developmental characters of the Sponges,
especially taking into consideration the recently acquired
embryological facts, according to which the Porifera differ in
no small degree from the other Metazoa both in the formation
and in the function of the germ-lamelle. If this be really
the case, we must regard them logically as a group of animals
equivalent to the Metazoa, but differing from them.
So long, however, as the developmental history of these
animals is not accurately and thoroughly known, I regard it
as more logical to refer them for the present to the Metazoa,
and to regard them as a special type or ramification of the
Archenterate main-branch, diverging from the Ccelenterata.
Another, far stronger, main branch of the blastodermic
animals combines all those animal-stems which, with the
exception of some Platyelmintha (Turbellaria, Trematoda,
and Cestoda), are all provided with a secondary alimentary
canal (metenteron), composed of two layers, namely, the
entodermal layer and the inner mesodermal lamina (splanch-
nopleura), and enclosed by a cceloma. As the cceloma
generally, as is well known, originates by constriction from
the archenteron, and indeed from the parenteric processes or
diverticula of the latter, we characterize all those blastodermic
animals or Metazoa which possess a perfect secondary alimen-
328 Dr. T. Margé on the Classification
tary canal, modified in the way just mentioned, with the name
of Metentera.
To the great main-branch of the Metentera belong, above
all, in our opinion, the vermiform animals or Helminthozoa.
According to all extant investigations, these animals form one
of the oldest of the great stems or phyla of the whole genea-
logical tree, most important from a phylogenetic point of
view, and most interesting anatomically and embryologically.
The group Helminthozoa embraces very many different
forms, which, as regards both their structure and their mode
of development, differ so much from each other that it can
hardly be regarded as too bold an assertion to say that, in the
whole animal kingdom, there is hardly another stem that
would embrace such different and sometimes widely divergent
modifications or classes. For this reason, also, it seems
scarcely permissible to regard the Vermes as forming an
equally unitary animal-type, as, for example, the Arthropoda,
Echinodermata, Coelenterata, and other great groups. Thus,
among other things, the Platyelmintha (with the sole ex-
ception of the Nemertina) are distinguished not only by
greater simplicity of organization, but also essentially by the
absence of a true coeloma, from all other Vermes, and even
from all Metentera. Nay, from this last-mentioned nega-
tive character (the absence of a cceloma) they might quite
logically be regarded as a special group of the Archentera.
We must not forget, however, that the Platyelmintha which
are destitute of a ceeloma (Turbellaria, Trematoda, and Ces-
toda) are, on the other hand, nearly related to the Nemer-
tina, and through these to the other groups of the same stem,
all of which are furnished with a cceloma; also that the other
groups of the Vermes deviate from one another in many
respects, and sometimes considerably, especially when we
take into account the segmentation of the ovum and the
mode of formation of the cceloma. Chiefly for this reason we
hold it necessary for the present still to regard the Platyel-
mintha as united with the other groups of Vermesinthe common
stem of the Helminthozoa, although, by many naturalists,
attempts have already been made to divide this stem into
several subordinate stems or subphyla. But if we consider
how imperfect the knowledge still 1s that we possess as to the
structure and development of the Vermes, we must regard all
such attempts at the present day as premature.
The results of the numerous investigations hitherto made
seem only to prove one thing, namely, that the stem Vermes
is perhaps very well divisible mto two or several divergent
branches—the group of the Scolecida (Platyelmintha with the
of the Animal Kingdom. 329
exception of the Nemertina) and the group of the Annelida.
Of these latter, however, the Polychaeta differ essentially in
their mode of development from the Oligocheta, and, more-
over, as is well known, there are many other forms, such as
the Nematoda, Acanthocephala, Gephyrea, Cheetopoda, Entero-
pneusta, and Rotatoria, which differ not inconsiderably, in
many respects, not only from the above-mentioned Annelida
and Scolecida, but also from one another.
From the consideration of all these facts, from the stand-
point of phylogenesis, in accordance with the present state of
science, only one thing can be accepted as established, namely,
that the Helminthozoa form on the genealogical tree of the
animal kingdom, a knot, which ts at present not quite untiable,
from which probably all the other higher stems have branched
off (see the Table, p. 534); and, consequently, there is no
doubt that the main stem of the Helminthozoa was of the
greatest importance in the origin and descendence of the
higher types.
From the results of recent. embryological investigations it
is sufficiently clear that the embryos, as well as the free-
swimming ciliated larvee, of different Vermes more or less
resemble the larvee of the Echinodermata, Bryozoa, Brachio-
poda, many Mollusca, and the Provertebrata (‘T'unicata and
Leptocardii). From the remarkable similarity of the con-
ditions of development of these animals it is further to be
assumed that these might all have originated by the process
of natural selection from one or more simple, vermitorm,
primitive forms. Nevertheless we must freely admit that the
known facts of embryology, as well as all the hypotheses
built upon these facts, by no means suffice for the final deci-
sion of the question, From what special primitive form have
the Mollusca, Bryozoa, and Brachiopoda, the Arthropoda and
the Provertebrata been phylogenetically developed? Both
in amount and in importance the facts at present known are
only capable of proving this much: that the great stem of
the Helminthozoa very probably forms the starting-point for
the higher animal-stems of the Echinodermata, Arthropoda,
Malacozoa, and Chordovertebrata.
Further, as regards the opinion of Prof. Semper and other
zoologists, according to which the Annelida are specially
adopted as the ancestors of the Vertebrata, I may here be
permitted only to remark that the facts cited for the esta-
blishment of this opinion (the segmental organs or primitive
kidneys) do not, in my estimation, suffice to demonstra‘e in-
dubitably that the Annelida are in reality more nearly allied
Ann. & Mag. N. Hist. Ser. 5. Vol. xii. 22
330 Dr. T. Margé on the Classification
to the Vertebrata than these latter to Amphioxus and the Tuni-
cata. Nay, it even seems very probable that the resemblance
founded upon the segmental organs does not owe its existence
originally to heredity, but that it has originated only in conse-
quence of adaptation to similar conditions of existence, and
consequently is to be referred to a so-called homoplasy, which,
as has already been explained in detail, is not sufficient for
the demonstration of a true blood-relationship. In my
opinion, that other hypothesis is much more acceptable, ac-
cording to which both the Annelida and the Provertebrata
have originally been produced from worms whose body as yet
exhibited no segmentation at all, such as we may still see
among the Turbellaria, Nemertina, Chetognatha, Hntero-
pneusta, and Nematoda.
With regard to the Bryozoa and Brachiopoda, my tendency
is towards the opinion that these animals belong to the great
stem of the Malacozoa. It appears exceedingly probable that
they branched off very early from the true Mollusca, as is
sufficiently proved by a careful comparison of their structure
and conditions of development, and especially the similarity
of their larvee (modified trochospheres). ‘This view finds
further support in the interesting form Rhabdopleura, (a diver-
gent form of the Phylactolemata), which becomes of the more
importance because, in its external form and internal struc-
ture, it is very similar not only to the Brachiopoda, but also
(according to Ray Lankester’s investigations) to the embryos
of a Lamellibranchiate, namely Pisedium. All this may
serve as evidence that the Bryozoa, as also the Brachiopoda,
have originated with the true Mollusca from one and the same
main stem, and, indeed, very probably by their having, at a
very early geological period, gradually adapted themselves to
a sedentary mode of lite, differimg from that of the remaining
progressive Malacozoa.
Upon these facts and considerations we have thought that
we could best represent the true relationships of the Bryozoa
and Brachiopoda to each other and to the true Mollusca by
dividing the main stem of the Malacozoa into two branches or
subphyla, of which the larger branch embraces the so-called
Mollusca, ¢. e. all the more or less progressive forms of this
stem (Lamellibranchiata, Scaphopoda, Placophora, Gastro-
poda, Pteropoda, and Cephalopoda, as distinct classes), while
the other branch, namely the subphylum of the Molluscoidea,
includes the Brachiopoda and Bryozoa, originating by means
of retrogressive phylogenesis.
With regard to the groups belonging to the stem of the
Arthropoda, we must remark that, as is well known, the
of the Animal Kingdom. 331
number of Arthropoda breathing by trachez has lately, since
the structure and development of Per‘patus have been more
accurately known, been increased by a new class, namely that
of the Protracheata (of Balfour and others). Since Moseley
succeeded in proving that these animals, which for a long
time were referred to the Vermes under the name of Onycho-
phora, really respire by trachese, and were also distinguished
from the other Arthropoda by the possession of quite diver-
gent, primitively constructed, and foot-like buccal organs *,
I regard it as perfectly right to unite this small but interesting
group, after the example of recent naturalists, with the stem
of the Arthropoda as a separate branch of the Tracheata.
In like manner I have regarded it as more judicious and
more in accordance with nature to establish in the class Crus-
tacea, besides the chief groups hitherto adopted (Thoraco-
straca, Arthrostraca, and Entomostraca), a fourth group,
namely that of the Paleostraca. This section of the Crus-
tacea, which includes the Trilobita and the Xiphosura, as
well as the fossil Merostomata first described by H. Wood-
ward, is distinguished from all others by the fact that the
mouth-organs of the forms belonging to it are very different
from those of the other Crustacea, and either foot-like or rudi-
mentary, or sometimes even entirely wanting (Trilobita).
Finally, as regards the Chordo- Vertebrata, I find myself
led in some points to adopt views somewhat diverging from
those of other naturalists. Thus I agree perfectly with
Balfour, Ray Lankester, &c., that we must unite the Uro-
chorda (Tunicata) as well as the Cephalochorda (Leptocardii)
with the stem of the Vertebrata; but with respect to the
Cyclostomi or Monorhina I by no means share the opinion of
those savants. ‘The Cyclostomi are in fact distinguished by
a great number of partly positive, partly negative, characters
of importance, which never occur elsewhere in other fishes
(Selachii, Ganoidei, Dipnoi, and Teleostei), or, indeed, in any
true Vertebrata even during the embryonal period; and by
these peculiarities they evidently, on the other hand, nearly
approach the Leptocardii and Tunicata. These characters
are :—
a. The absence of the mandible.
b. The absence of paired extremities.
c. The absence of the nervus sympathicus.
d. The originally simple and unpaired nasal cavity
(olfactory cavity) with a simple external dorsal
olfactory aperture,
* Phil. Trans. vol. clxiv. (1874).
22*
332 Dr. T. Margé on the Classification
e. The composition of all the nerves of exclusively white
elements.
f. The direct course of the nerve? optici to the two eyes
without any crossing.
g- A remarkably large and wide stomadeum, or the
remarkable size of the anterior portion of the ali-
mentary canal representing the stomadeeum.
h. The occurrence of a hypopharyngeal groove, always
developed at least during the larval period.
7. The smoothness and softness of the integuments, as
well as the absence of any formation of scales.
k. Absence of the lateral organs which are developed
elsewhere in all fishes and Amphibia (in the latter
in the larval period).
If the Cyclostomi be compared with Amphiorus and the
Tunicata, we find, further, that of all these the Cyclostomi
alone are possessed of a primitive cartilaginous skull, in which
a prechordal part is already developed. If, however, we
examine this Cyclostome skull more closely, we arrive at
once at the conviction that, as regards its external form and
internal structure, it presents essential differences from the
cartilaginous skull of fishes (Selachii, Dipnoi, Ganoidei).
The blood is red, like that of other fishes, but the blood-
corpuscles are of a circular and not of an elliptical form.
The segmentation of the ovum, as shown by recent investi-
gations, is not regular, as in Amphiowus and the Tunicata,
but irregular and amphiblastic (as in Acipenser and the Batra-
chia). But if we consider that the mode of segmentation
may sometimes be quite different even in nearly allied ani-
mals, and that, moreover, the conditions of existence of the
animal may exert a great influence, if not directly, yet in-
directly, upon the process of segmentation, we must regard
the different mode of segmentation as by no means a safe
criterion in judging of the relationships of the Cyclostomi.
On the other hand, it seems to us to be of much greater im-
portance that the earhest larval form of Petromyzon is very
like Amphioxus, and then subsequently becomes transformed
first into the Ammocetes-torm, and finally into the definitive
form.
If, then, we take all these peculiarities into consideration,
and weigh them all carefully, it appears clearly that the
number of bonds which unite the Cyclostomi with Amphiowus
and the Tunicata is greater than the number of characters
which those animals have in common with the Selachii and
the other fishes.
of the Animal Kingdom. 333
I think, therefore, that the relationships between the diffe-
rent classes of the Chordo-Vertebrata may be expressed by a
more natural grouping, if I divide their main stem into two
divergent branches or subphyla, one of which, the subphylum
of the Provertebrata, or .Primitive Vertebrata, includes the
more or less reduced or retrogressive forms of simpler struc-
ture, furnished with a wide stomadeum, a hypopharyngeal
groove, and an unpaired median olfactory organ, but destitute
of a mandible and of paired limbs, as well as of a nervus
sympathicus and of true lateral organs, to which belong, as
distinct classes, the Tunicata, Leptocardii, and Monorhina.
The other, larger branch, the subphylum of the Metavertebrata,
or true Vertebrates, would then embrace the true fishes or
Ichthyozoa (Selachii, Ganoidei, Dipnoi, and Teleostei), ori-
ginating by progressive phylogenesis the Amphibia, Reptilia,
Birds, and Mammalia, all of which are furnished with man-
dibles, paired extremities, paired nasal cavities, and a nervus
sympathicus (see Table, p. 334).
As regards the forms of the Provertebrata living in the
present geological period, ¢¢ appears very probable that they
are the descendants of the more perfect free primitive Verte-
brates which existed in Paleozoic times, even before the first
appearance of the Selachti, of which, however, a great part has
gradually died out and disappeared entirely in consequence of
the occurrence of unfavourable conditions of existence in course
of time.
And if we consider, in conclusion, that the still existing
forms of the Provertebrata are for the most part characterized
by a semi-parasitic or sedentary mode of life, it may be as-
sumed with some probability that they are indebted for their
preservation to this their peculiar mode of life. Thus, while
some of their formerly free-living ancestors had the good for-
tune to become transformed by natural selection in the way of
progressive phylogenesis into Metavertebrata, or true Verte-
brates, and others, on the contrary, in course of time have
gradually died out, the rest were able, in consequence of
retrogressive metamorphosis, to maintain their existence,
although with a reduced structure of body, under the allotted
conditions of existence, uninjured to the present day, in the
form of Tunicata, Leptocardii, or Monorhina.
334 On the Classification of the Animal Kingdom.
Mammalia
(Dicoridylia) Aves
Repiilla
Monocondylia
Amphibia
Ichthyozoa
Pp gactyla Holochorda (Cephalochorda) Gastropoda
)
lydact es
Placophora
Pteropoda Scaphopoda
Insecta
Arachnoidea PROVERTHEBRATA
Lamellibranchiata
Myriopoda
MOLLUSCA
ati heat
Sat nae Brachiopoda
Protracheata Bryozoa
CHORDO.WERTEBRATA
Crustacea
(Branchiata)
ARTHROPOD MOLLUSCOIDEA
By ange Ctenophora
MALACQZOA
Holothurioidea COELENTERA Anthozoa
(93
Ecbinoidea HELIMINTHOZOA
r RCHENTERA
ECHINODERMA ARCHENT PORIFERA
METENTERA
Asteroidea
. . (6)
Crinoidea BLASTODERMICA (Metazoa)
PROTOPEASTICA (Protozoa)
ANIMALIA
Typokiching Ca.sc.
Mr. J. W. Davis on a new Species of Ptycholepis. 330
XXX VI.—Deseription of a new Species of Ptycholepis from
the Lias of Lyme Regis. By James W. Davis, F.G.S. &c.
[Plate X.]
Genus PrycHOLEPIs, Agassiz.
Scales thick, elongated, plicated transversely on the base,
and deeply turrowed longitudinally ; under surface smooth
and devoid of rib; pectoral fins pointed; dorsal fin opposite
the ventral fin; anal fins remote. (Zgerton.)
Ptycholepis gracilis, sp. nov.
A well-preserved specimen of Ptycholepis recently came
into my possession, which differs in several respects from the
species of this genus which have been described by Prof.
Agassiz and Sir Philip Egerton. Its form is more attenu-
ated than that of either of the previously figured species.
The first representative of the genus, Ptycholepis bollensis*,
Agassiz, from the Lias at Whitby, was a tolerably large
specimen about 10°5 inches in length, of which length the
head occupies more than one fourth. Sir Philip -gerton
described two species, P. minor T aud P. curtus t; the former,
from the Lias of Barrow-on-Soar, is a small and elegant fish,
now in the Enniskillen-Egerton collection at the Natural-
History Museum, South Kensington. Ptyocholepis curtus is
a much shorter and thicker fish ; it is 4°75 inches in length,
the head being 1°75 inch, or more than one third the entire
length of the fish. The depth of the body at the dorsal fin
is 1:7 inch. The specimen now before me is 7 inches in
length from the snout to the termination of the tail; of this
length the head occupies 1‘5inch, and the depth of the body
at the dorsal fin is 1°5 inch. In proportion to the size of the
whole fish the head is much smaller than in any of the species
before mentioned, and the form of the body is slender and
graceful as compared with either P. bollensis, Ag., or P.
curtus, Kg. ‘The anterior portion of the dorsal outline of the
specimen is slightly broken, the ventral and caudal margins
are intact, and the lateral surface of the body and head is
beautifully preserved.
The head is small, more or less triangular, with a bluntly-
rounded snout; the posterior outline of the operculum is_
* “Poissons Fossiles,’ vol. ii. part 2, p. 108, pl. lix. 4, figs. 1-3 (1883-43).
+ ‘Memoirs of the Geological Survey,’ dec. vi. pl. vii.
t Ibid. dec. viii. pl. viii. (1853).
336 Mr. J. W. Davis on a new Species of Ptycholepis.
convex; the mouth is large, apparently extending far towards
the anterior extremity of the operculum; the snout projects a
short distance beyond the mouth ; the orbit is well developed,
occupying an area one fifth the length of the head and about
its own diameter distant from the end of the snout. The
bones of the head are well preserved, and are ornamented with
the enamelled ridges characteristic of the genus. The opercu-
jJum—unlike that of P. bollensts, which is smooth, or P. curtus,
which is anteriorly ornamented by widely separated ridges,
whilst on the posterior portion they are nearly obsolete—in this
specimen is deeply channelled, the shining ridges standing i
high relief over the whole surface, but without any apparently
definite arrangement. Along the inner or basal margin of
the operculum there is a narrow strip, separated by a deep
groove, which is perfectly smooth. The suboperculum is
comparatively small; it is similarly decorated and possesses
a smooth strip along the margin next the operculum. The
bones of the cranium, as well as those of the jaws, are orna-~
mented with a series of more or less parallel ridges, which
anteriorly bend with a sinuous curvature so as to encircle the
nasal extremity.
The scales on the body are larger anteriorly than those
nearer the tail; they are arranged in symmetrical parallel
rows, each about ‘1 inch in length and extending more or
less diagonally from the dorsal towards the ventral surface.
The scales of the dorsal part of the body are wider than those
of the ventral. The enlarged figure (Pl. X. fig. 1 a) repre-
sents a scale midway across the body and *5 inch behind the
operculum ; fig. 1¢ is taken from the ventral surface at °S
inch behind the pectoral fin, and 16 is from the surface
near the tail. The posterior margin of all the scales is deeply
serrated ; the number of serrations varies with the width of the
scales, and corresponding to them are depressions of the sur-
face or grooves, deepest at the anterior margin and extending
towards, but rarely attaining, the posterior one. The base of
each scale has a number of transverse imbrications, delicately
marked and only distinguishable when highly magnified.
The dorsal jin is indicated by a faint impression of some of
the fin-rays. It appears to be situated slightly in advance of
the ventral fins, but not so much so as in Ptycholepis curtus,
Eeert. The pectoral fins are situated immediately behind
the head; they are well developed, nearly an inch in length,
consisting of about twenty rays. ‘The rays are grooved near
the base, but afterwards dichotomizing towards the margin ;
the transverse articulations are clearly discernible at about
half an inch from the base of the fin, and may be distinguished
——EE————
Mr. J. W. Davis on a new Species of Ptycholepis. 337
to the outer extremity of the rays. A series of minute fulcral
scales extends along the margin of the anterior ray of the fin.
The ventral jin is smaller than the pectoral and is equidistant
between the pectoral fin and the tail; in this specimen the
fin may not be quite perfect; it is °7 inch in length. The
basal part of the rays is grooved longitudinally, as in the
pectoral fin, and their extremities are divided into two or
more parts. The anal fin is not well defined. The tazd is
supported by a base *7 inch across; it is forked, the distal
extremities of the two lobes being 2 inches apart. The base
of each lobe is somewhat hidden by a covering of iron pyrites ;
the extremities are composed of fine rays divided and sub-
divided from those nearer the base; each is composed of
numerous small joints attached by transverse articulations.
A number of triangular scales thickly coated with black
enamel encircle the dorsal aspect of the base of the tail and
extend along the margin of the upper lobe of the tail in an
oblique imbricating series, decreasing in size as they approach
the extremity. The lower lobe is devoid of fulcra. The
vertebral column is extended towards or partially into the
upper lobe of the tail. The lower lobe, though the rays are
finer, is considerably larger than the upper one.
This species is characterized by its slim and graceful form
and the small size of the head in proportion to that of the
body. It may also be distinguished by the ornamentation of
the head-plates and scales, the difference between the latter
and the corresponding scales of the species described by Prof.
Agassiz and Sir Philip Egerton being sufficiently character-
istic. Sir Philip Egerton, ina supplement to the eighth decade
of the ‘ Memoirs of the Geological Survey,’ gives some details
of a second specimen of Ptycholepis curtus found at Lyme
Regis ; the length of the fish is 5} inches and that of the
head two inches, showing a similar disproportion as compared
with the example now described. The ventral fins are placed
nearer to the pectoral than the anal fins in P. curtus; whereas
in this species the anal fin cannot be more than half as far
from the ventral as the latter from the pectoral.
I propose to designate this species Ptycholepis gracilis,
Locality. Lias, Lyme Regis.
EXPLANATION OF PLATE X.
Fig. 1. Ptycholepis gracilis, Davis. Natural size.
Fig. 1a. Scale midway across the body, about half an inch behind the
operculum, X15,
Fig. 16. Scale near the caudal extremity. x 15.
Fig. 1c. Scale from the ventral surface. x 15.
338 Mr. A. H. Foord on
XXXVIL—On three new Species of Monticuliporoid Corals.
By Artuur H. Foorp, F.G.S., late Assistant Palaon-
tologist to the Geological and Natural History Survey of
Canada.
[Plate XII.]
1. Monotrypa macropora, Foord. (Pl. XII. figs. 1-1 d.)
Corallum discoid, concavo-convex, with expanding and
gradually tapering margins; attached by the base to some
foreign body, such as a shell or trilobite. Base covered with
a thin and concentrically wrinkled epitheca. Cells opening
upon the upper surface of the corallum. Calicinal surface
almost smooth, with very slightly raised areas about 5 milli-
metres apart, occupied by groups of cells a little larger than
the average. Of the larger cells about one to one and a half
fill the space of 1 millimetre ; of the smaller about two are
comprised within the same limits. The largest specimen
known to the writer measures about 7 centimetres in its
greatest diameter and about 25 millimetres in thickness, from
the centre of the surface to the base, measured vertically.
Microscopic characters.—In sections taken as near to the .
surface as possible the corallites are observed to be polygonal,
mostly six-sided, with comparatively thin but remarkably
clearly outlined walls, the original divisions of which may be
faintly discerned under a moderately high power. Clusters
of the larger cells are seen grouped together amongst those of
the average size, while at rare intervals a few much smaller
ones are intercalated with the former (fig. 10); but these
are not of the nature of interstitial tubes, their tabulation not
differing in any respect from that of the other corallites. Sec-
tions cut longitudinally to the axis of the corallites show that
these are furnished with complete horizontal or slightly curved
and very delicate tabule, which vary from about one half to
two tube-diameters apart.
This species may be readily distinguished from the only one
of the genus hitherto described from British rocks, viz. Mono-
trypa crenulata, Nicholson *, by its discoidal habit of growth,
the large size of its corallites, its more abundant tabulex, the
total absence of crenulations in the tube-walls, and lastly by
the presence of small angular corallites.
The writer is indebted to the kindness of Mr. George Maw,
* Ann. & Mag. Nat. Hist. ser. 5, vol. xiii. p. 124, fig. 2 (1884).
oe
new Species of Monticuliporoid Corals. 339
F.G.8., for a fine example of this species, from which the
section figured on Pl. XII. fig. 1 6 was prepared. The species
appears to be not rare in the Buildwas beds (Wenlock shales),
where they crop out on the east bank of the Severn near
Buildwas Abbey. It is associated in these beds with a rich
Brachiopodous fauna, which has been worked out by Messrs.
Davidson and Maw *.
The two following species are contained in the collections
of the British Museum (South Kensington), and the author
has obtained Dr. Woodward’s kind permission to describe
them.
2. Amplewopora T microstoma, Foord.
Corallum lobato-palmate, with a tendency to become ra-
mose in some places. Surface with irregular swellings.
Corallites prismatic, extremely slender, nearly straight in the
axial region, but bending slightly towards the surface. No
monticules are present, but the surface shows under a hand-
lens small clusters of cells somewhat larger than, the average.
Of these about three occupy the space of 1 millimetre, and
about five of the smaller ones, so that the latter do not exceed
zis inch in diameter. In rough fractures the walls of the
cells are seen quite distinctly to be minutely crenulate, a cha-
racter which occurs in so many species of the Monticuliporide f
that its value for purposes of classification appears very ques-
tionable.
Microscopic characters.—Tangential sections show that the
corallites are thin-walled, polygonal in outline, and very
variable in size. The spiniform corallites are numerous and
are observed at the angles of junction of the cell-walls, and
frequently also in the substance of the walls between those
angles. In this latter situation they give rise to an inflation
of the walls of the cells. In longitudinal sections the tubes
are seen to have thin walls, which are very slightly thickened
* Vide Geol. Mag. new series, decade ii. vol. viii. p. 100 (Feb. 1881).
+ This genus is defined by E, O. Ulrich (Journ. Cincinnati Soc. Nat.
Hist. vol. v. p. 154, 1882) for the reception of such forms of the Monticu-
liporid as possess the following characters :—a ramose, free, or incrust-
ing corallum, composed of cells of one kind only, the walls as seen in
microscopic sections being thin in the axial but thicker in the peripheral
region, and being provided with straight tabule. Spiniform corallites are
developed more or less abundantly in different species, to such an extent
in some as to completely surround the cell-mouths. The geological range
of the genus in the United States extends from the Cincinnati group
(Caradoc) to the “ Sub-” Carboniferous (Mountain Limestone).
t Crenulate walls are found in Monotrypa undulata, Nich., M. crenu-
lata, Nich., Heterotrypa Dawsoni, Nich., and in the present species.
340 Mr. A: H. Foord on
as they approach ina gentle eurve the surface of the corallum.
Very few tabule are developed in the axial region of the -
corallum, and it is not until the surface is nearly attained that
they occur in greater numbers. Here they are placed at
irregular distances apart, and are often sharply curved either
upwards or downwards. The minute crenulations of the walls
are seen in these sections (see woodcut, fig. D). The minute-
D
Amplexopora microstoma, Foord,—A. Corallum of this species of the
natural size. 1b. Tangential section, enlarged about 30 diameters. C. Part
of the same section, enlarged about 50 diameters. D, Longitudinal section,
showing at @ one of the spiniform corallites, enlarged about 15 diameters,
ness of the corallites separates this species from all others of
the same genus known to the writer.
formation and Locality. Wenlock Limestone, Dudley.
new Species of Monticuliporoid Corals. 341
3. Dekayella* robusta, Foord. (PI. XII. figs. 2-2 d.)
Corallum ramose, frequently branching. Branches thick,
usually cylindrical or subcylindrical, sometimes compressed.
Surface covered with small but tolerably conspicuous mon-
ticules, situated about 3 millimetres apart, and bearing cells
of a somewhat larger size than those in the intermediate
spaces. ‘The apertures of the corallites are polygonal in out-
line, and in places where the surface is well preserved some of
the larger of the spiniform corallites may be seen with a hand-
lens. Of the larger corallites about four occupy the space of
1 millimetre, of the smaller about five.
Microscopic characters,—Tangential sections reveal clearly
the dimorphic character of the corallum, which is provided
with two kinds of tubes, large and small; both are of poly-
gonal form, and their outline is inflated in many places by
the occurrence of numerous spiniform corallites. ‘l'hese also
are of two kinds: the larger are usually situated at the angles
formed by the junction of four or five cells,’and fill a space
quite as great as that occupied by some of the interstitial
cells; the smaller are generally found to be in the substance
of the cell-walls, about midway between two angles. The
spiniform corallites form a very conspicuous feature in tan-
gential sections of this species, and give to such sections a
highly characteristic appearance. Under a moderately high
power traces of the original walls of the corallites may be
discerned in tangential sections; but as a rule this structure
appears to have been destroyed in the process of fossilization.
In longitudinal sections the two sets of tubes are clearly
brought into view. In the larger ones there are numerous
horizontal, sometimes slightly oblique, tabula, situated at
from one half to one tube-diameter apart ; they begin in the
axial region of the corallum, and are about equally developed
in their course from thence to the peripheral region. ‘he
smaller tubes do not differ in the character of their tabulation
from the larger ones, except that the tabule in the former are
a little more frequent than they are in the latter. There is a
feature worthy of note in the structure of the walls of this
species, and that is a periodic inflation, which reminds the
* Mr. E. O. Ulrich (“ American Paleozoic Bryozoa,” Journ. Cincinnati
Soc. Nat. Hist. vol. v. p. 155, 1882) constituted this genus for the recep-
tion of forms “ more nearly allied to Dekayia, Edwards and Haime, than
to any other genus of the Monticuliporide,” but differing therefrom “ in
having the tube-walls in the mature region of the zoarium thicker, in
having numerous interstitial tubes, and, instead of one, two distinct sets of
spiniform tubuli” |=‘ spiniform corallites” of Nicholson}. This last is
stated by Mr. Ulrich to be the most important character of the genus.
342 On new Species of Monticuliporoid Corals.
observer of a similar structure characteristic of the genus
Stenopora (Lonsdale). Mr. Ulrich draws attention to a like
feature in his description of a Cincinnati-group species of
Dekayella—D, obscura, Ulrich (Journ. Cincinnati Soc. Nat.
Hist. vol. vi. p. 150).
On leaving the axial region the tubes rapidly thicken
towards the surface, the spiniform corallites being seen at
frequent intervals piercing the corallum and intermingling
with the ordinary corallites. The spiniform corallites appear
to originate in the axial region of the corallum, as they may
be seen in sections cut as deeply as it is possible to make them
without destroying the walls of the tubes.
It may be well here to enumerate the chief characters which
separate this species from the only two known to the writer,
viz. Dekayella Ulrichii, Nicholson *, and D. obscura, Ulrich—
both from the Cincinnati Group of Ohio. From the former
of these the present type may be distinguished as follows :—
by its much more robust habit of growth, by the possession
of monticules, and by the much greater number of its tabule
and spiniform corallites. The exceedingly small and delicate
corallum of D. obscura, Ulrich, would be sufficient alone to
differentiate it from D. robusta, and added to this the great
development of the tabule and spiniform corallites in the
latter make the distinction between the two forms sufficiently
clear.
Formation and Locality. Cincinnati Group, Cincinnati,
Ohio.
* EXPLANATION OF PLATE XII.
ig. 1. Monotrypa macropora, Foord: upper surface of corallum. Nat.
size.
Fig. 1 a. Side view of the same specimen.
Fig. 1b. Tangential section of this species, enlarged about 20 diameters.
Fig. 1c. A few cells, enlarged about 50 diameters.
Fig. 1d. Longitudinal section, enlarged about 15 diameters.
Fig. 2, Dekayella robusta, Foord: corallum, showing monticules. Nat.
size,
Fig. 2a. Tangential section of this species, showing the two series of
spiniform corallites a, a. Enlarged about 30 diameters,
Fig. 2b. Two cells, enlarged about 50 diameters.
Fig. 2c. Longitudinal section, showing at @ one of the spiniform coral-
lites. Enlarged about 20 diameters.
Fig. 2d. Portion of the same, showing more clearly the periodic inflation
of the walls of the tubes. Enlarged about 50 diameters.
Fi
>
* =Monticulipora (Heterotrypa) Ulrichti, Nicholson (‘The Genus
Monticulipora,’ Nicholson, p. 181, fig. 22, 1881).
On Butterflies from the Fiji Islands. 843
XXXVIII.—A Collection of Butterflies from the Fiji Islands.
By Artuur G. Butter, F.L.S., F.Z.S., &e.
THE collection of which the present is an account is one of
unusual interest, from the great care with which it has been
made, a record of the locality and date of capture being given
upon each envelope. Of some of the species no examples
have previously (so far as I know) reached this country,
whilst of others we have only known single examples or a
air.
This series was collected by C. M. Woodford, Esq., and
presented to the British Museum.
Nymphalidae.
Evrrie@in#.
Much discussion has arisen respecting Mr. Moore’s revision
of this group of butterflies, and there is no doubt that by the
introduction into this otherwise most laboriously constructed
paper, of unquestionably incomplete “ tables of the genera,”
its author has laid himself open to criticism. Whether the
groups regarded by Mr. Moore as genera are allowed to retain
that rank or are regarded as sections, there can be no doubt
that many of them are sufficiently distinct to exhibit series of
parallel species, such as are recognized as existing between
the universally admitted New-World genera Ceratinia, Me-
chanitis, Melina, and Heliconius. So far as I am personally
concerned, [ think a generic boundary separating such parallel
series (even though it be only indicated by a slight constant
modification in the wing-structure) is profitable to the student,
in that it calls his attention to the existence of parallelism in
the subfamily ; and I think it convenient to admit the greater
part of Moore’s genera (in the present paper I admit all with
which I have to deal), though in the case of Andasena and
Nipara, I believe the latter name will not stand.
1. Tirumala moderata.
Danais moderata, Butler, P. Z.S. 1874, p. 275,
Tairuni, September 1882.
2. Andasena eleutho.
Danais eleutho, Quoy & Gaimard in Freye, Voy. p. 554, pl. Ixxxiii.
fig. 2 (1815).
Mango, 20th July, 1882.
344 Mr. A. G. Butler on Butterflies
3. Nipara intermedia.
Nipara intermedia, Moore, P. Z.S. 1883, p. 258. n. 3.
3 ?. Mango, 13th and 18th July.
4. Salpine Greffiana.
Euplea Greffiana, Herrich-Schaffer, Stett. ent. Zeit. 1869, p. 70, pl. ii.
fig. 5.
9. Mango, 18th July, 1882.
5. Vadebra mangoensis, n. sp.
Dark piceous, primaries becoming almost black towards the
end and around the end of the cell, but with the veins paler ;
a diffused submarginal paler band curving inwards to costa at
apex, and bearing eight whity-brown spots, the four first of
which form an oblique subapical series and are very small
and almost white; the remainder increasing gradually in
size to the seventh, the eighth considerably larger than the
latter ; external border smoky dark grey-brown : secondaries
paler than the primaries, with an olivaceous tinge, the sub-
marginal band wider and much paler than that of the prima-
ries, bearing seven white spots near its inner edge, two of which
are subapical and very sharply defined; four minute sub-
marginal dots : body blackish. Wings below paler than above,
olivaceous brown: primaries with the costal area pale, form-
ing a continuous belt with the submarginal one; all the
spots in the submarginal belt small, especially the fourth and
fifth ; a blue point near the extremity of the discoidal cell,
and three forming an obtuse angle above the three median
branches; an elongated white interno-median longitudinal
streak ; internal border dull white: secondaries with the sub-
marginal belt very pale, especially towards the anal angle, so
that only the first two of the white spots along its inner border
are well defined; the four submarginal spots decidedly larger
and more conspicuous than above; costal border, excepting
at base, clear whity-brown; a blue spot in the cell and an
angulated series of seven blue spots round the outer half of
the cell between the veins, the last of these being distinctly
linear; pectus and base of secondaries black spotted with
white; venter dark brown, with a few central white points.
Expanse of wings 52 millim.
Mango, 15th July, 1882.
Nearest to V. sepulchralis of Java and V. Zinckenii of
Amboina; but readily distinguished from both by the discal
series of spots on both surfaces and other less important cha-
racters.
Srom the Fit Islands. 345
6. Calliplea Forstert.
Euplea Forstert, Felder, Reise der Nov. Lep. ii, p. 822 (1867).
Mango, 15th July.
NyupHaLine.
7. Hypolimnas formosa.
Diadema formosa, Herrich-Schaffer, Aussereur, Schmett, fig. 119 (1869).
Mango, 16th July.
8. Hypolimnas lutescens.
Diadema lutescens, Butler, P. Z.S. 1874, p. 283, n. 49, pl. xliv. fig. 3,
?. Mango, 16th July.
A dark form of this species was taken at the same time,
which is interesting, inasmuch as it approaches H. antilope
of Amboina. It is probably a female with male colouring.
9. Hypolimnas pallescens.
Diadema pallescens, Butler, P. Z. 8, 1874, p. 282. n. 47,
Nine females. Mango, 18th July.
The series collected by Mr. Woodford shows a series of
gradations, commencing with the extremely pale form figured
in Brenchley’s ‘Voyage,’ through a series of gradually
darkening forms near to H. antigone of Batavia, to a smoky
brown form in which the markings, excepting the discal series
of white spots on the primaries, are much obscured; the
general character of H. pallescens, apart from the ground-
tint, is nevertheless retained throughout the series.
10. Hypolimnas porphyria?
Papilio porphyria, Cramer, Pap. Exot. iii. pl. eclvy, E, F (1782).
9. Tairuni, 16th September.
Cramev’s figure is taken from an Amboinese example in
which the submarginal series of spots appear to be decidedly
whiter than in the Fijian form; this, however, may be an
error in colouring.
11. Hypolimnas Moseleyi.
Hypolimnas Moseley, Butler, Ann. & Mag. Nat, Hist. ser. 5, vol, xi.
p. 414. n. 43 (1883).
?. Mango, 18th July.
It is a singular thing that the only male Hypolimnas in
this collection is the specimen of H. formosa.
Ann. & Mag. N. Hist. Ser. 5. Vol. xiii. 23
346 Mr. A. G. Butler on Butterflies
12. Junonia villida.
Papilio villida, Fabricius, Mant, Ins, ii. p, 35. n, 866 (1787).
Mango, 20th July.
AcrDINE.
13. Acrea andromacha.
Papilio andromacha, Fabricius, Syst. Ent. p. 466, n, 102 (1775),
18th and 20th July, 1882.
Lycenide.
14. Catochrysops patala.
Lycena patala, Kollar, in Hiigel’s Kashmir, iv. 2, p, 419 (1848).
3. Mango, 13th July, 1882.
15. Jamides Woodfordii, sp. nov.
3. Brilliant glossy ultramarine-blue, with narrow external ~
black border to the primaries about two thirds the width of
that in J. candrena (14 millim. in the middle, slightly wider
at apex) ; costal margin very narrowly blackish : secondaries
with a more or less well-developed submarginal series of oval
black spots, bounded externally by a bluish-white line, those
nearest to anal angle also with an internal bluish-white bor-
der; an interrupted black marginal line ; abdominal border
smoky grey, whitish at base: body blackish, with bluish and
grey hairs on the thorax. Under surface rich golden brown,
with the usual slender white lines; ocelli towards and at
anal angle with reddish-orange internal lunate borders. Hx-
panse of wings 29 millim.
?. Paler than’ the male on both surfaces, the primaries
above with costal and external blackish borders almost as wide
as in J. plato 9: secondaries with a complete marginal series
of blind black ocelli, with pale blue irides and black zones.
Expanse of wings 31 millim.
3 3. Mango, 13th July.
We also have a male in the Museum from Vanua Levu.
16. Jamides campanulata, sp. nov.
Smaller than the preceding species, deep glossy sky-blue
with hlac reflections; similar in pattern to the preceding
species, but the submarginal line bounding the submarginal
spots of the male and forming the irides of the ocelli of the
Jrom the Fiji Islands. 347
female pure white. Under surface distinctly paler than in
J. Woodfordit, of a stone-greyish colour ; the lunules bounding
the ocelli of secondaries golden-orange. Hxpanse of wings,
3 25, 2 27 millim.
3 2. Mango, 13th July.
We also possess a male taken at Vanua Levu on the 3rd
July, and a second from Viti Levu received in 1874 as a sup-
posed variety of the far more beautiful J. candrena.
17. Jamides lobelia, sp. n.
3. The smallest species of the group: bright Morpho-
blue; primaries with a rather narrow black external border
(just over 1 millim, in the middle, slightly wider at costa) :
secondaries with black submarginal spots much as in J.
Woodfordit, but less oval. Under surface grey, the white
lines indistinct, the ocelli of secondaries with pale stramineous
internal lunate border. Expanse of wings 16 millim.
3. Mango, 13th July *.
18. Lycena mangoensis, sp. 0.
3. Violet-blue, rather dull; with narrow dull dust-grey
external border, slightly wider at costa than at external angle ;
* Before passing on to another genus I think it best to name two other
forms which have for some time past stood in the Museum collection as
supposed varieties of J. candrena, but which I now am sure are distinct.
Jamides pulcherrima, sp. n.
3. Colour of J. candrena ; intense glistening ultramarine-blue ; pri-
maries with the costal margin and a rather broad external border black,
the width of this border gradually increased from 13 millim. at external
angle to 6 millim. on the costal margin, so that it is decidedly wider than
in J. candrena, but narrower than in J. plato: secondaries also with a regu-
lar black border nearly 2 millim. in width, enclosing a series of blue
erescents; abdominal border brown. Wings below stone-grey; white
lines inconspicuous: ocelli of secondaries rather small, the larger one over
the tail Fae with a greenish silver spangle at each end and, like the
smaller one, with a narrow reddish-orange half-zone. Kxpanse of wings
26 millim,
Tanna, New Hebrides, 23rd Apvril.
Jamides morphoides, sp. 0.
3. Brilliant Morpho-blue, with black borders as in the preceding
species, that of secondaries enclosing three oval spots outlined in lilac.
nder surface silver-grey, with a very faint golden shot, only visible in-
certain lights; the white lines on the primaries very indistinct ; ocelli on
the secondaries with ochreous inner borders. Expanse of wings 30
millim.
Montague Island, New Hebrides.
Nearest to J. Goodenoviti, though entirely differing in the colour of both
surfaces.
23%
348 Mr. J. A. Murray on the Marine
basal half of costa of primaries and abdominal border of
secondaries chalky white: body bluish. Under surface
greyish white ; a narrow discocellular stone-grey stria with
white edges at the end of each discoidal cell; a marginal
series of grey-centred and grey-zoned white ocelli: primaries
with a series of white-edged grey lunate spots near to outer
margin: secondaries with two spots near the base and an
irregularly angulated series of white-edged stone-grey spots
beyond the middle. Expanse of wings 25-27 millim.
Mango, 20th July, 1882.
Not very nearly allied to any thing known to me.
Papilionide.
Prerinaz,
19. Belenois teutonia?
Papilio teutonia, Fabricius, Syst. Ent. p. 474 (1775).
Mango, 20th July.
Not perfectly typical ; but only one example was obtained.
20. Belenots clarissa.
Belenois clarissa, Butler, Ann. & Mag. Nat. Hist. ser. 5, vol. xii. p. 590
(1878).°
Mango, 13th July.
Two males were obtained.
PAPILIONINA.
21. Papilio Schmeltzt.
Papilio Schmeltzi, Herrich-Schiffer, Stett. ent. Zeit. 1869, pl. i. fig. 1.
Levuka, 29th June; Mango, 15th July.
No species of Hesperides were obtained.
XXXIX.—A Contribution to the Knowledge of the Marine
Fauna of Kurrachee. By J. A. Murray.
THE marine fauna of Kurrachee and the Sind coast generally
has not hitherto received quite the attention it deserves, and
it is evident, from the results of collections made during the
last five years, that there are many undescribed forms, not
—_
Fauna of Kurrachee. 349
only of mammals, but also of fish, Crustacea, and the lower
organisms, as Hichini, Polyzoa, Zoophytes, &c.
In this paper I shall describe two new species—one a
Shark of the genus Zamna, and the other a Cetacean of the
family Delphinide, and of the genus Neomeris.
Taking the Shark first, it is necessary to make mention of
a species from the Kurrachee harbour, which Dr. Giinther, of
the British Museum, described in the ‘Annals and Magazine
of Natural History’ for February 1883, under the name of
Carcharias Murrayt. It is quite possible that this species
would be found to occur on the Mekran, Kutch, and Bombay
coasts also; but at present I am not aware of its distribution
east or west. ‘T’he several imperfect jaws in the Kurrachee
Museum from Kutch lead me to believe that the species
occurs on that coast also.
The new species of the genus Lamna requires but little
preface. According to Dr. Giinther (Cat. Fish, Brit. Mus.
vol. viii.) the genus contains only three species, viz. L. cor-
nubica, L. Spallanzani, and L. glauca. Of these L. Spallan-
zant is mentioned by Mr. Day as occurring in the Indian
Ocean, and a figure of the species is given by him on plate 186
of his work on the Fishes of India, taken from a drawing by
Sir Walter Elliot of an example captured at Madras,
The present species is not LZ. Spallanzani nor any of the
other described forms, from all of which it differs very mate-
rially, first in having a greater number of teeth, next in the
position and shape of the fins, also in the position and short-
ness of the keel on the sides of the tail ; and, lastly, in having
a very prominent lateral line or ridge extending from the
lateral keel of the tail forwards along the entire length of the
body, rising upwards above the gill-openings and terminating
immediately behind the eye.
The species now needs a name, and I venture to associate
with it that of our veteran ichthyologist, and describe it as
Lamna Ginthert, sp. nov.
Its measurements as taken in the flesh are as under :—
feet. inches,
Length from tip of snout to root of caudal.. 7
From root of caudal to tip of upper caudal
[OLED 6 Stet Raine Rede ee oe ae 1
From root of caudal to tip of lower caudal
Mee riety olvidar act eeiwvenné. hie. sie.ec0 0 1 03
Distance between tips of upper and lower
SHUI LOE rite Nisin viuitettlg. 80.0.8 0 ft 36
Length of pectoral fin ....s.ccsisssscses 1 4
Width of pectoral fin at base..........+.0. O 83
350 Mr. J. A. Murray on the Marine
feet. mches.
Height of dorsal fins avwee arene oes ee 9
Width of dorsal sim. vnc pane head Seis sere 0 9
Distance of dorsal from base of pectoral fin.. 0 3
Distance of pectoral from base of ventral.... 1 103
Height ofanaltiia')) AU LOS. CRAKS ofa) 0 21
Height of second dorsal ...........00000 0% 0 21
Girth round body at third gill-opening 3. 10
Teeth 22,
The snout is much produced and subtriangular; from the
front of the eye to the tip of the snout it measures 64 inches, and
the space between the eyes is 6inches. From the front of the
eye to the tip of the snout on each side is a band, 4 inch wide,
of a series of irregularly arranged minute pores, and there isa
similar patch on the cheeks and below the snout, but extend-
ing only to within 2 inches of the gums. The nostrils are
conspicuous, open, and placed nearer the eye than the tip of
the snout; the greatest diameter of each is 0°37 inch. The
angle of the mouth is midway between the nostril and first
gill-opening. Gzill-openings five, all of equal width. Teeth
$3, their edges sharp and smooth, no basal cusps. The first
set of three in the lower jaw is longest, and measures from
1:25 to 1°37 inch in length, curved inwards, rather flattened
on the outer side and convex or rounded on the inner. The
third tooth on each side of the symphysis of the upper jaw is
smaller than the rest.
The first dorsal fin is placed nearer the pectoral than the
ventral fin, and about its own length behind the hinder base
of the pectoral; pectoral fin narrowing falcately from the
base to the tip; anal fin situated about its own length poste-
riorly to the second dorsal. A pit at the root of the caudal fin.
The keel on the sides of the tail begins from in line with the
origin of the anal fin; a strongly ridged lateral line is con-
tinued from it, extending along the entire length of the body,
rising upwards above the gill-openings, and terminating im-
mediately behind the eye. Upper caudal lobe falcate, termi-
nating in a point and not in a triangular lobe, as shown in
the figure of L. Spallanzani in Mr. Day’s work. Colour
dark plumbeous on the upper half, greyish on the lower half;
underside of snout yellowish. Skin smooth.
The synopsis below will show at a glance how this species -
differs from the other described forms :—
LL, Giinthert, sp. nov. | 22 on each side, | Gill-openings all! Origin of dorsal| Prominen
Fauna of Kurrachee. 851
Teeth. Gill-openings. Dorsal fin. Lateral 1:
28 of equal width, | fin nearer pecto-
No basal cusps. ral than ventral,
13—16
Ti, COFNUDCA 6.5% s pat Width of first gill-| Above the root of
A small basalcusp| pening nearly) pectoral.
on each side. equal to its dis-
tance from the
last.
LL Spallanzant ...... i Rather more than} Short _—_ distance
its distance from} from base of pec-
the last. torals. Second)
dorsal and anal
opposite one an-
other.
BB
No basal cusps.
APE 13° Ditto. Ditto.
No basal cusps.
‘The next is a Cetacean of the family Delphinide, which I
shall describe under the name
Neomeris kurrachiensis.
The characters of the genus are :—Dorsal fin none. Nose
of skull short, rounded in front, flat and shelving above.
Teeth numerous, compressed, nicked, acute, extending nearl
the whole length of the jaw (Gray, ‘Seals and Whales,’ &c.).
Neomeris phocenoides is the only species of the genus, and
its dentition is given as +§ (Delphinus melas) or 7§ on each
side.
The species under notice has {$ teeth on each side, and
there are besides a set of 3, which were scarcely visible through
the gums, and situated out of the line of the other teeth in
front of the jaws. In shape these 3 teeth are quite unlike the
rest, being conical instead of flattened or compressed.
The measurements of the animal taken in the flesh are as
under :—
inches.
Length along curves from tip of snout to
notch between caudal flukes .......... 52
PRA MMRURING co's ctete' ew Fon Wiest sree + 0.0.0 5 6 6 45
Tip of snout to pectoral fin .............. 10
EM NGS wie o occ eo aialew ce wise ¢ e ¥ oe esti s 9x3
Distance of blowhole from tip of snout along
CULE OF te Br ae eee eee 65
Ditto from angle of mouth to eye.......... 1:62
Vent from root of caudal fin ........... Fae
302 On the Marine Fauna of Kurrachee.
Snout rounded; head very convex, rising posteriorly high
to the dorsal surface. Blowhole semilunar. Back with a
longitudinal band of spinous tubercles on the vertebral area,
beginning nearly opposite the root of the pectoral, widening
to 1°5 inch about the middle, and again contracting and ending
narrowly opposite or in line with the vent. No dorsal fin.
Pectoral subtaleate. Teeth 3. Colour shining black through-
out, except a purplish-red patch in front of the snout (on the
upper lip) and on the throat. Intestines 31 feet in length.
Contents of stomach Crustacea (species of Pencus).
Skull.
inches.
Length of skull over curves to upper edge of
fOTHINEN MAGNUM) 4.6 Lee he tees wake 10
Ditto, straight from below ................ 8
Height of skull (vertex of superoccipital) .... 4°25
Tip of snout to blowhole .....)............. 4:25
Ditto to anterparictaly. W. .), ees. voce ee eee 6:25
Interparietal to upper edge of foramen magnum 3°75
Across MBXMIATION 5... vce phe Caden ne eee 4:75
Aeross blowhicles (UA). Vian he themes 15
Hoength on mmal ar |. sjesavs wesc ORM eb eis Ln, Sine 2°0
ADIGtO AOL PLAINCa VIL. 16's chet a eere wes tne Siete oes 4:0
eNCLOSS ‘PATOCCIPltals yee cm .abesmeceee ree eee 3°37
Greatest space between occipital condyles
(UP Per) yrs tee Mi pre, Eee busta ttn te Ste aeahe 15
Smallest space between occipital condyles at
LGwersthind src gah oe. oh kane Acted mete 1:0
Vertical diameter of foramen magnum ...... 175
Breadth across last teeth on each side (upper
BBY) LoeidP Al Ah ME OR, Babe Coa eam 2'5
Ditto, ditto!Gower jaw) 0%) oth). he sdebeeee « 25
Teeth-line in upper and lower jaw .......... 2°5
Length of lower jaw to coronoid process .... 5°62
Greatest vertical depth of ramus............ 2°62
Palabe fs COE Ses al hed bali aoe ae eee 4:0
The superoccipital is subglobular and very convex above.
Rostrum short, rounded in front. Foramen magnum vertically
oval, with the occipital condyles vertically elongated and
convex, wider at their lower third. ‘Teeth small, flattened, or
compressed, with a sharp subcrescentic crown, faintly nicked,
and with the middle of their outer and inner sides slightly
swelled ; they are rather obliquely arranged in line, about
one fifth of each succeeding hinder one overlapping its fellow,
but not in contact.
The assumed Relationship of Parkeria to Stromatopora. 353
XL.—WNote on the assumed Relationship of Parkeria to
Stromatopora, and on a Microscopic Section of Stromatopora
mamillata, fr. Schmidt. By H. J. Carter, F.R.S. &e.
In 1877 (‘ Annals,’ vol. xix. p. 55 et seg.) I made it plain
(at all events to myself) that Parkerta was neither a species
of Foraminifera nor one of Spongida; and at p. 61 (¢b.) began
to compare the structure of Parkerta with that of Stromato-
pora, meaning that stromatoporoid organism of the Devonian
Limestone called by Phillips “‘ Cawnopora placenta,” which
was originally described by Lonsdale under the name of
“ Coscinopora placenta.” But subsequently, that is in 1879
(‘ Annals,’ vol. iv. p. 101 et seqg.), I found that Caunopora
must be considered as an instance of “ symbiosis,” in which
the vertical tubes belonged to one organism and the stromato-
poroid mass in which they are imbedded to another, probably
both allied to the Hydroida; thus my comparison of the
“ vertical tubes”? of Caunopora with those of Parkeria be-
came inadmissible, and the nature of the animal of Parkeria
was still left open for conjecture.
To assume that Parkeria was not a Hydroid because the
skeletal structure of the former was probably calcareous and
not chitinous would be equally inadmissible, because Hydrac-
tinia calearea affords a living instance to the contrary, to say
nothing of the fossil species, viz. H. pliocena (‘ Annals,’
1877, vol. xix. p. 50) and H. Kingw (db. 1878, vol. 1.
p- 301), both of which are of considerable thickness. Thus,
prevalent as the chitinous skeleton is among the Hydroida,
there are instances of calcareous ones in which the structure
mutatis mutandis is the same; but to this I shall presently
recur more particularly.
Meanwhile fossil specimens of massive Polyzoa from the
Coralline Crag of Suffolk have been presented to me to show
how much their general form, structure, and mode of growth
resembles that of Parkeria; that is, they are hemispherical
masses with nodular segmented surface, radiating structure,
and concentric lines of intervals or chambers (analogous to
the “ chamberlets’”’ in Parkeria), all growing from a central
point and furnished with an epithecalinvestment. But, while
the segments are composed of little groups or masses of parallel
tubes in juxtaposition, which groups are separated in the direc-
tion of the radiation by the intervening of the ‘ chambers,”
and each mass is based upon an epithecal layer of amorphous
substance which extends more or less up the sides, thus form-
ing the ceiling of the empty “ chamber,” whose floor, on the
354. = Mr. H. J. Carter on the assumed Relationship
other hand, consists of the open mouths of the tubes in juxta-
position, as seen on the surface of the fossil, the whole of the
structure of Parkeria is elaborated out of tissue composed of
anastomosing, reticulated and vermiculated, solid, calcareous
thread in which there is no epithecal or other differentiation
whatever beyond form ; that is to say, that although this tissue
is traversed by distinct tubes which radiate in broken lines
from the centre to the circumference (passing through the
chambers in an isolated manner, that is, separated for some
distance from each other without any intervening substance,
which chambers, as before stated, are empty in the fossil
Polyzoa from the Coralline Crag), the tubes themselves of
Parkeria are composed of the same reticulated tissue as the
rest of the fossil. In both instances, of course, these calca-
reous structures respectively represent the skeletal or hard
parts, while the intervals were occupied by the soft parts of
the animal.
Again, the embryo or commencement of Parkeria seems to
have settled, for development, on a loose or rolling fragment
of foreign material, whence the future growth became more
or less spherical, often including in its progress small Fora-
minifera and other particles of foreign matter, as may be seen
by the vertical sections.
Thus the resemblance of the fossilized Polyzoa of the Crag
to Parkeria is reduced to the general structure, while the ele-
mentary structure is totally different.
Where Parkeria looks most like the fossilized forms of the
Polyzoa from the Crag is in the solidified specimens, that is,
where the cavities originally occupied by the flesh or soft
parts have been filled up with calcite; but this is not the
condition in which the comparison should be made, seeing
that, in many instances when the Parkeria is broken with a
hammer, more or less of the interior comes out in a large
spherical form or nucleus, like a nut from its shell, wherein
the whole of the calcite, which in the solidified specimens fills
the intervals originally occupied by the soft parts, is absent,
and therefore nothing but the tissue formed of the anastomo-
sing, reticulated, skeletal thread, now incrusted with minute
crystals of calcite through fossilization, remains, which nucleus,
on being picked to pieces as much as may be required, can
be most satisfactorily studied, and then it is that the great
difference which exists between it and the fossilized Polyzoa
of the Coralline Crag can be fully realized. Indeed, in this
condition, the skeletal part can be more satisfactorily studied
even than in the living animal, when the whole of the skeleton
was probably imbedded in flesh.
of Parkeria to Stromatopora. B55
But whether the reticulated tissue of anastomosing, vermi-
culated thread be infiltrated or not, the distinction between the
tubes and this tissue is equally manifest, from the small size
of the meshes of the latter contrasted with the much larger
size and scattered position of the former, either on the surface
of the fossil or in the vertical section, as they traverse the
chamber ; at the same time if the surface alone be examined,
then it does resemble that of the Polyzoa called “ Heteropora”
(large and small tubes together) ; but this impression is soon
corrected by an examination of the wninfiltrated or wnconsoli-
dated specimen, when the “tubes,” which on the surface
look like Heteropora, are seen to be separated by an inter-
vening structure that, to my knowledge, hitherto has, in
no shape, ever been found to occur with the cells of the
Polyzoa.
What, then, was the form of the animal that inhabited these
tubes in the midst of the elementary structure of Parkeria,
which is so totally different from that of the fossilized
Polyzoa of the Coralline Crag, to which I might add those of
the Coral Rag and the recent species of branched coralliform
polyzoon, called “ Heteropora,” from New Zealand ?
This question throws us back again upon the Hydroida, to
which I have before alluded as presenting in the calcareous
form the only kind of reticulated tissue mixed with large tubes
(the calicles) for the use of the polyps or hydranths which
have any direct resemblance to the structure of Parkerta (see
‘ Annals,’ 1877, vol. xix. p. 50, pl. vii. fig. 5, &c.).
If we assume that Parkeria was a polyzoon, then it must
be entirely upon general resemblance and form, but not at all
upon the elementary structure ; hence the assumption must
be so far simply conjectural; while if we assume that it was
a Hydroid, then we have in addition an almost identity in
elementary structure to go upon for our assumption, and this
being, under the circumstances, of the more consequence of the
two, must be considered the more tenable. Besides, we have
the instance of Chitina ericopsis (‘ Annals,’ 1873, vol. xi.
p- 13), which, although dendritic in general form, is iden-
tical in tissue with Parkeria, that is, the whole is elabo-
rated out of a mass of continuous, anastomosing, reticulated,
and vermiculated thread, without differentiation in any part
beyond mere form; and although there are no ‘“ chambers ”
here to be traversed by the “ tubes,” as in Parkeria, their
analogues are to be seen in the form of hollow cylindrical
processes or hydrothece at the ends of the branches, which
tubes are composed of the same tissue and originally contained
the polyps or hydranths. Now, were this “ thread” calca-
356 Rev. T. Hincks’s Contributions towards a
reous instead of chitinous, as it 7s in Hydractinia calcarea,
then the identity in structure with Parkeria would be so far
complete.
Thus, although Parkerta cannot be identified with Cauno-
pora, there is still no reason whatever why it should not be
indirectly connected through Hydractinia with Stromatopora
by being a Hydroid, if I am right in assuming that the animal
of the latter was of this nature (‘ Annals,’ 1878, vol. ii.
p- 304 &c.).
With reference to the examination of the microscopic
section of Stromatopora mamillata, Fr. Schmidt (Rosen,
‘Ueber die Stromatoporen,” p. 71 &c., Taf. viii.), I have
only to repeat what Nicholson and Murie, in their excellent
memoir, have already stated, viz. that the skeleton of Stroma-
topora is ‘composed of non-spicular, granular, calcareous
matter” (Linn. Soc. Journ. Zool. 1878, vol. xiv. p. 241).
Selecting a rolled portion, from the ‘ Parson and Clerk”
rocks at Teignmouth, of the species above mentioned, in which
the so-called ‘ hexactinellid structure’’ is sharply defined, I
thought, as I had lately been successful in bringing out the
spicules of the fossilized Calcispongie of the Coral Rag from
Faringdon, that I might be equally successful in doing so
with Stromatopora under similar circumstances, if there were
any present; but although the slice was reduced almost to
transparency, the skeletal fibre of the Stromatopora through-
out never presented any thing but a granular composition,
the minute grains of which contrasted strongly with the clear
rhomboid crystalline calespar of the intervening spaces,
without the most remote trace of any kind of sponge-spicule
in any part.
XLI.— Contributions towards a General History of the Marine
Polyzoa. By the Rev. THomas Hincxs, B.A., F.R.S.
[Continued from vol. xi. p. 202. ]
[Plates XIII. & XIV. ]
XII. POLYZOA FROM INDIA (coast of Burmah).
A small gathering of Polyzoa from an island in the Mergui
Archipelago, off the coast of Burmah, obtained by Dr. J.
Anderson, F.R.S., Superintendent of the Indian Museum,
Calcutta, has been placed in my hands for examination by
General History of the Marine Polyzoa. 357
my friend Mr. H. J. Carter. It consists of fourteen species,
of which four are probably undescribed ; the rest are well-
known forms, but they have a definite interest as coming
from a new locality, and one which has hitherto, so far as I
know, been little explored.
The following is the list of species :—
Suborder CHEILOSTOMATA.
Family Cellulariide.
SCRUPOCELLARIA, Van Beneden.
Scrupocellaria diadema, Busk.
Range. Queensland.
_ Family Bicellariide.
BEANIA, Johnston.
Beania mirabilis, Johnston.
On shell.
Range. Scandinavia, Great Britain, Adriatic.
Family Membraniporide.
MEmMBRANIPORA, De Blainville.
Membranipora favus, n.sp. (Pl. XIII. fig. 2.)
Zoecia oval, or hexagonal, or suborbicular (presenting
many irregularities both in form and arrangement), of con-
siderable depth, closely packed together, surrounded by a
narrow brown line, which forms a kind of keel on the top of
the cell-wall; inner surface of the margin granular; area
occupying the whole front of the cell, closed in by a delicate
membrane; numerous small cells of various shapes (some-
times quadrate, with an orbicular area) interspersed amongst
the larger ones. Avicularia none.
Zoaritum forming a rather thick crust, and (especially in
the absence of the membranous front wall) closely resembling
a honeycomb.
The species is without striking features. “The dwarf cells,
which are present in large numbers, are, perhaps, the most
notable peculiarity.
358 Rey. T. Hincks’s Contributions towards a
Membranipora marginella, n. sp. (Pl. XIII. fig. 1.)
Zowcta rather small, quincuncially arranged, ovate or pyri-
form, sometimes pointed below, with a rather thick, unarmed,
minutely granular margin; aperture occupying about two
thirds of the front and closed in by membrane, contracted above
and expanded and rounded below ; a small oval avicularium,
elevated above and sloping downwards, borne on the margin of
the zocecia, usually placed on the side, near the top. Occa-
sionally cells with a very large oral operculum of a dark horn-
colour, occupying nearly half the area, and enclosed by a
thin raised border (? avicularian or reproductive).
Family Steganoporellide.
STEGANOPORELLA, Smitt.
Steganoporella magnilabris, Busk.
Range. Abrolhos Islet (south tropical Atlantic), Algoa
Bay, Bass’s Straits, Florida.
Smitt places this genus amongst the Microporide, and I
have given it the same position in my ‘ History of the
British Marine Polyzoa.’ But I am now imclined to agree
with Dr. J. Jullien * so far as to regard the dithalamic con-
dition of the zocecium which distinguishes it as entitling it to
rank in a separate family group. It is only right, however,
that the name of this group should be taken from Smitt’s
genus Steganoporella, which is founded on the division of the
zocecium into an upper and lower chamber by the interposition
of a calcareous lamina beneath the membranous front wall.
I am unable to follow Dr. Jullien in his proposed distribu-
tion of the Cheilostomata into two principal groups, charac-
terized by the presence or absence of this ‘‘ double ectocyst.”
It seems to me that he assigns a significance to this struc-
tural peculiarity to which it is by no means entitled. There
is room, however, for a fuller investigation of its history and
meaning.
SMITTIPORA, J. Jullien.
Smittipora abyssicola, Smitt.
Range. Cuba, Florida, Singapore or Philippines.
es
* See his interesting paper entitled “ Note sur une nouvelle division
des Bryozoaires Cheilostomiens,” Bull. de la Soc. Zool. de France, t. vi.
(1881).
General History of the Marine Polyzoa. 359
There seem to be two generic types at least* included in
the group of the Steganoporellide, one of them represented by
S. magnilabris and the forms which agree with it in the
structure of the zocecium, the other by such forms as the
present. For the latter 1 have adopted (provisionally) Jul-
lien’s name Smittipora, though I am not prepared to accept
his diagnosis of the genus in all points, and should be dis-
posed to make it much more comprehensive than he has done.
The genus Steganoporella (as I propose to limit it) is distin-
guished by the tubular passage leading from the inner
chamber towards the external orifice and the corresponding
modification of the internal orifice (‘ opesta”’ of Jullien),
which is a simple opening in the calcareous lamina communi-
cating directly with the inner chamber in Smittipora and
kindred forms f.
I at one time referred the present species to Setosel/a, mihi,
but the British species (S. vulnerata) for which this genus
was founded does not possess the dithalamic cell.
The specimens of S. abyssicola from Burmah are crusta-
ceous in habit.
Family Microporellide.
MIcroPoRELLA, Hincks.
Microporella violacea, Johnston, form plagiopora, Busk.
(Pl. XIII. fig. 3.)
Range. Off Tortugas, Florida; France (south-west): Eng-
lish Coralline and Red Crag, Italian Pliocene.
Zoecia large, ovate, very regularly placed, punctured or
areolated round the margin; orifice (primary) arched above,
lower margin straight ; peristome often much raised, giving
a tubular character to the orifice; pore subcentral, simple,
round ; aviculartum originating a little below the orifice, bent
towards one side of it, and extending obliquely to the margin ;
mandible slender and finely pointed, curved at the extremity.
The Burmese specimens agree in all essential particulars
with Busk’s Crag species. The only peculiarities are the very
irregular arrangement of the zocecia and the elevated tubular
peristome which occurs on many of the cells. I see no
reason for regarding WM. plagiopora as any thing more than a
slightly modified form of MW. violacea.
* There are probably more, but I confine my attention at present to the
two noted above.
+ See ‘Annals’ for Feb. 1882, “ Contributions towards a General His-
tory of the Marine Polyzoa.”—IX., pl. v. figs. 8, 9.
360 Rey. T. Hincks’s Contributions towards a
Microporella Fuegensis, Busk.
Range. Tierra del Fuego.
A small erect and branched specimen of this species occurs.
The suboral pore presents some peculiarities. It is placed
immediately below the rim of the orifice in front, and is only
found in the adult cell. In the marginal zocecia the orifice is
suborbicular and the peristome not elevated; but in a more
advanced stage the peristome rises considerably round the
back and sides of the orifice, but not in front, the result being
that a sinus is formed here. In a still more advanced stage
the margin of the side walls of the peristome is extended
across the upper part of this sinus, forming a narrow rim, and
converting the open fissure into a circular pore, which com-
municates directly with the interior of the tubular peristome.
It is evident that this is a very different structure from the
ordinary pore of the Microporelle, as it occurs in MV. ciliata
and M. Malus’, where it opens into the interior of the cell
itself, and must be placed in a very different category.
Family Myriozoide (part), Smitt.
SCHIZOPORELLA, Hincks.
Schizoporella biaperta, Michelin.
The single specimen which occurs is crustaceous in habit
and referable to the form divergens of Smitt. It is furnished
with large spatulate avicularia as well as the small circular
form so characteristic of the species; the walls of the cell are
smooth and white. The ocecium is very unlike that figured
by Smitt for his Hippothoa (Schizoporella) braperta ; and this
dissimilarity, in conjunction with the difference in the shape
of the orifice, may prove that he was right in regarding the
form divergens as a species. The ovicell in Dr. Anderson’s
specimen (which is a very typical example of Smitt’s S. di-
vergens) is small, rounded, and thickly covered with raised
punctures ; the opening is closed by the oral operculum of the
cell.
Family Escharide (part), Smitt.
LEpPRALIA, Johnston (part).
Lepralia robusta, n. sp. (Pl. XIII. fig. 4.)
Zowcia very large, ovate, quincuncial, flattish, separated by
arather deep furrow, which is occupied by a line of large
General History of the Marine Polyzoa. 361
punctures ; surface uneven, rather coarsely granulose, usually
a small depression (? pore) in the centre; orifice large, much
taller than wide, arched and expanded above, somewhat con-
tracted below, constricted a short distance above the inferior
margin, which curves outwards; on each side of the orifice
(or sometimes on one side only) a much elongated subspatulate
avicularium, which originates some way below the orifice and
slants obliquely upwards to a little above the top of it; man-
dible long, blunt and slightly expanded at the extremity, and
directed upwards. Owciwm rounded, somewhat prominent,
moderate in size, surface roughened.
A fine characteristic member of the genus, of which the size
of the cells and the elongate avicularium are the striking
features.
PoRELLA, Gray.
Porella malleolus, n. sp. (Pl. XIII. fig. 5.)
Zowcia rectangular, disposed in linear series, depressed,
separated by delicate raised lines; surface covered with small
punctures and nodulous ridges; a line of larger foramina
round the sides; orifice arched and expanded above, much
contracted below, the margin about the centre projecting
inward on each side, lower lip slightly curved (nearly
straight); within it an avicularium with a hammer-shaped
mandible. Occasionally an avicularium at one side, which
takes its origin some way down the cell and slopes upward to
the top of the orifice; mandible elongate, slightly expanded
at the base, slender above it, and pointed at the extremity,
directed upwards. Ocectum (?).
Zoarium incrusting, whitish, of very delicate material.
The hammer-shaped mandible of the avicularium is a
curious peculiarity, and, when ‘elevated and standing erect
within the lower hp, a very conspicuous one,
SmitriA, Hincks.
Smittia trispinosa, Johnston, vars.
Range. Norway and Arctic seas, St. Lawrence, Mazatlan,
North Pacific (Queen Charlotte Islands), Florida, Cape Horn,
Aden, Adriatic, Britain, Bass’s Straits.
Of this cosmopolitan species several varieties occur.
i. Peristome usually not elevated, and the marginal den-
ticle very prominent (as in the Arctic form); sometimes the
usual triangular avicularium present, but in some of the cells
Ann. & Mag. N. Hist. Ser. 5. Vol. xiii. 24
362 Rev. T. Hincks’s Contributions towards a
replaced by an elongate form, originating below the orifice,
and stretching up alongside it, with a long slender mandible
(occasionally subspatulate) directed upwards. Zowcia very
irregularly placed and turned in all directions (Pl. XIII.
figs. 7, (a).
ii. Zowcia very regularly disposed in lines. Owctwm thickly
punctured, and with a penthouse-like projection in front; a
triangular avicularium below the orifice. .
ii. Form bimucronata (Pl. XIII. fig. 6). Zowcia ovate,
moderately convex, in linear series, radiating regularly from
the central primary cell, separated by raised lines, punctured
round the margin; surtace reticulated, silvery ; orifice subor-
bicular, with a denticle on the lower lip; peristome (in the
older cells) much elevated, thin, rising on each side into a
prominent mucronate process, more or less produced in front,
two spines on the upper lip; frequently on one side a gigantic
aviculartum, which originates alongside the peristome (near
the top of the orifice), and extends straight downwards to
the base of the cell; beak deeply channelled, broad at the
base, and narrowing gradually towards the rounded extremity ;
an elongate subtriangular opening on the upper half of it ;
mandible long, very slender above the expanded basal por-
tion, formed of very delicate membrane, directed downwards.
This variety also occurs in Australia (J. B. Wélson).
This has much the appearance of a distinct species ; but it
is connected by intermediate varieties with the typical form.
We might expect the most widely distributed forms to be
the most lable to variation; and this is certainly so in the
case of the present species and Microporella ciliata, which
are both eminently cosmopolitan.
Family Celleporide.
CELLEPORA, Fabricius (part).
Cellepora, ?n. sp.
A Cellepora occurs amongst Dr. Anderson’s specimens
which is identical with that described in my “ Report on the
Polyzoa of Queen Charlotte Islands’ under the provisional
name of C. brunnea.
Suborder CYCLOSTOMATA,
Family Lichenoporide.
LicHenopora, Defrance.
Lichenopora Nove-Zealandic, Busk.
Range. New Zealand.
General History of the Marine Polyzoa. 363
XIII. POLYZOA FROM VICTORIA AND
WESTERN AUSTRALIA.
Under the present heading I shall continue the account of
the Polyzoa dredged by Mr. J. Bracebridge Wilson off Port
Phillip Heads, Victoria*. The collection which he has
placed in my hands for examination is large and interesting,
and I propose to give a complete list of the species contained
in it which are not included in MacGillivray’s ‘ Decades,’ as
well as descriptions of the new forms.
Group Lwroprocra.
Family Pedicellinide.
PEDICELLINOPSIS, n. gen.
Generic character.—Polypides cup-shaped, supported on
chitinous tubes with a much enlarged base (consisting of an
opaque white core, probably muscular, enveloped in a chiti-
nous covering), by which they are attached to an erect tubular
stem. Zoarium adherent by means of tubular root-fibres.
This is a truly arboresent Pedtcellina, in which the soft
parts, with the exception of the polypide itself, are clothed
with a well-developed chitinous ccencecium. ‘The prolonga-
tion of the common flesh from which the polypide buds is
protected by a chitinous tube, which is open above, and at the
base is attached to a stem (also invested with a solid periderm).
The root-fibres by which the colony is fixed in its place are
sheathed in chitine. The polypide resembles closely that of
such a form as Pedicellina cernua, and, so far as I can judge
from an examination of spirit-specimens, presents no special
peculiarities ; it is not elevated above the orifice of the tube,
but rests immediately upon it. The base of the tube is
modified for the reception of a special structure ; and if we may
judge from the analogy of such a species as Pedicellina gracilis,
Sars t, it must be muscular in character, and probably much
more powerful and highly organized, as it is much larger
than the kindred structure which occurs in the latter. If it be
muscular it must secure free mobility to the polypide in con-
junction with the protection afforded by the solid covering, and
* See ‘Annals’ for August 1882.
+ In this form the mobility resides in the enlarged cylindrical base, the
stem merely bending from the bottom, and the upper portions being chiti-
nous and rigid,
24*
364 Rev. T. Hincks’s Contributions towards a
a colony of Pedicellinopsis in health and vigour must present a
strange scene of unrest and lively movement. We may hope
that Mr. Wilson may yet have an opportunity of examining
the species alive and studying its habits.
This localization of the muscular power seems to me to be
fairly accounted a generic character ; and I should be disposed
to separate Pedicellina gracilis from the species in which it
is diffused and in which there are no chitinous elements. At
the same time it must be remembered that Leidy has described
an American form very closely resembling P. gracilis, in
which the basal expansion is present, while at the same time
the whole stem is highly flexible and often becomes “ more or
less revolute’? *. ‘This is certainly a transition form. The
distinctive characteristics of Pedicellinopsis are the arborescent
form (which is by no means comparable with the mere
ordinary variations in habit amongst the calcareous Cheilo-
stomata), the specialized muscular structure, and (primarily)
the highly developed periderm. In the localization of the
muscular power this genus agrees with Pedicellina gracilis and
with the remarkable Arctic genus Barentsia, mihi. In the
possession of the first of the characters named it stands alone
amongst the tribe; the last it shares (though with an im-
portant difference) with Urnatella, Leidy, a very interesting
and beautiful form from the American fresh waters.
Pedicellinopsis fruticosa, n. sp. (Pl. XIV. figs. 3-3.)
Zoarium erect, consisting of a number of stout chitinous
stems rising from a mat of tubular root-fibres, and sending
off branches sparingly and irregularly, the whole forming a
bushy shrub-like growth. olypides borne on the summit of
tall chitinous tubes, obliquely truncate at the top, and pro-
duced at the upper side into a sharp spinous projection,
terminating below in large turbinate expansions with an
opaque-white core and chitinous envelope, annulated through-
out, which are attached to the stem by the inner side towards
the base, and are thickly crowded upon it; body of the poly-
pide cup-shaped, whitish, ventricose on one side and almost
straight on the other ; tentacles (probably) about twenty ; the
tubes traversed by four double lines, the spaces between them
being occupied by a row of minute disks, which project from
the surface. Height of the zoarium about one inch.
Loc. Port Phillip Heads (J. B. Wilson).
The tubes are densely crowded on the stems, which they
* See his paper entitled “ Urnatella gracilis, a Freshwater Polyzoan,”
Journ. Ac. Nat. Sci. Philad. vol. ix.
General History of the Marine Polyzoa. 365
clothe throughout their whole length; they are disposed
somewhat irregularly in whorls. The basal enlargements are
closely packed together, and almost conceal the surface of the
stem. ‘There is little branching; near the base the stem
divides into two principal shoots, which give off laterals occa-
sionally, but there is no definiteness in the plan of the
ramification. ‘lhe whole surface of the tubes is finely lineated
longitudinally. A very marked character of the species is
the obliquely truncate extremity of the tube, which is pro-
duced on one side into a strong spike-like projection. To-
wards the base the stem gives off a large number of chitinous
fibres, which torm a kind of adherent disk.
The whole structure recalls very forcibly one of the Tubu-
larian Hydroids.
Group Heroprocra.
Suborder CTENOSTOMATA.
Family Flustrellide.
FLUSTRELLA, Gray.
Flustrella hispida, Fabricius, form cylindrica.
(Pl XUV. figssd; Lat)
Zoarium erect, much branched; stem and branches cylin-
drical, composed of rather firm chitinous material. Zowcta
disposed round the cylinder in six linear series, those of the
neighbouring series alternating, large, regularly ovate, convex
in front; surface smooth, round the margin a large number
(15-18) of tapering acuminate spines, with an enlarged base,
which bend inward over the front wall, but without meeting ;
orifice close to the upper extremity of the cell, bordered above
and below by a *' 1 horny rib; immediately above it a few
(usually three) erect spinules; numerous large spines,
springing from a kind of boss, scattered over the interspaces
between the cells.
Loc. Port Phillip Heads (J B. Wilson).
Lange. Northern and Arctic seas, Britain, France (S.W.).
This is a very remarkable form, and for some time I was
quite disposed to regard it as a distinct species ; but a careful
examination of the cell has convinced me that in this essential
element of the structure there are no characters to separate it
from the common /. hispida of our English coasts. ‘The
difference in habit and external appearance, striking as it is,
has a parallel in many other cases, and is merely varietal.
366 Rey. T. Hincks’s Contributions towards a
Similar diversities in the mode of growth are of frequent
occurrence within the limits of a species amongst the Cheilo-
stomata, and in the Ctenostomatous group Alcyonidium hir-
sutum is found as a gelatinous crust and as an erect palmate
expansion with many lobate branches. In the present case
the zoarium seems to be firmer and less fleshy than in the
crustaceous condition, and is of a rather dark horn-colouy.
The branching is irregular; in the largest specimen I have
seen the stem divides dichotomously near the base, the secon-
dary shoots dividing into tall flexuous branches, which bear
numerous short branchlets. The branches are slightly
attenuated and smooth at the base. There is always much
variability in the number of the spines, and in English speci-
mens they are often very much confined to the oral region, but
they are also found surrounding the cell. In the Australian
variety they are few in number and small above the orifice,
but form a regular line round the margin of the cell, and bend
in over the front of it.
Flustrella dichotoma, v. Suhr (sp.).
(PI. XIV. figs. 2 a, 2d.)
Verrucularia dichotoma, vy. Suhr, Ratisbon Flora (1854), p. 725, tab. i.
fig. 9, a, a.
Puinceinaree dichotoma, Busk, Quart. Journ. Microscop. Sc., ‘ Zoo-
phytology.”
Zoartum erect, much branched di- and trichotomously,
the terminal branchlets generally trifid; stem and branches
slender, cylindrical, composed of a transparent membranous
material; attainsa height of about 2 inches. Zowcia arranged
in six series, those of neighbouring series alternating, very
regularly ovate, bounded by a strongly marked dark line,
very convex ; surface smooth, destitute of spines, prolonged
below into a kind of peduncle ; orifice placed a little way
below the top of the cell, bilabiate, with a dark chitinous
border. Between the rows of cells a narrow smooth inter-
space divided at intervals by transverse dark lines (? septa).
Loc. Port Phillip, Australia (Kirchenpauer); Port Phillip
Heads (J. B. Wilson).
This form, originally described by v. Suhr as a Pucus, was
referred by Busk to his family Farciminariide, and placed in
the genus Farciminaria. Owing probably to the dried con-
dition of his specimens the latter writer has overlooked the
Ctenostomatous structure of the ovifice, which agrees in all
respects with that of Flustrella. In the characters of the
zocecium and the general habit this species approaches the
General History of the Marine Polyzoa. 367
cylindrical form of Flustrella hispida just described, and must
rank in the same genus.
The cells in the same longitudinal series are not in imme-
diate contact, but are connected one with the other by a
peduncular extension, which is bounded like the cell itself by
a dark reddish-brown line. Nor are the cells in neighbouring
rows united laterally, a narrow interspace lying between the
series and extending throughout the length of the branch.
In the isolation of the cells this species differs from FP. his-
pida. ‘There is no true joint at the origin of the branches,
but merely a constriction, and the zocecia run on continuously.
This form and the preceding illustrate a very different
phase of the genus Llustrel/a trom that to which we have
been accustomed, and show that it has a wide geographical
range.
Suborder CHEILOSTOMATA.
Family Cellulariide.
Buauta, Oken.
Bugula uniserialis, n. sp. (Pl. XIII. fig. 8.)
Zourium minute, composed of geniculate, slightly branched
shoots of transparent texture and a delicate horn-colour ;
branches given off sparingly from about the middle of the
dorsal surtace of a cell. Zoawcia uniserial; bent alternately to
opposite sides, so as to present a zigzagged appearance, each
cell originating on the dorsal surtace of the one beneath it,
immediately below the top and directed obliquely outwards,
boat-shaped, of equal width in the upper portion, slightly
contracted below ; aperture occupying the whole front, and
closed by a transparent membrane ; margin thin, running out
above at each side into a sharp spinous projection; at the top
of each cell a very minute articulated avicularium, placed
just below the upper margin and usually about the middle of
it, well rounded behind, with a rather long back sloping
down to a well-developed beak, mounted on a rather promi-
nent peduncle. Oaciwm helmet-shaped, smooth and shining,
placed on the side of the cell close to the top, and overhanging
the orifice more or less.
Loc. Western Australia, on weed (Miss E. Gore).
This species is probably the minutest of its tribe (so far
as known), and is very scantily branched and simple in habit.
Though the uniserial and geniculate character of the cells
368 Rey. T. Hincks’s Contributions towards a
confers upon it a marked individuality, it is really a very
typical Bugula, so far as all the essential elements of structure
are concerned.
Family Cellariide.
CELLARIA (part.), Lamouroux.
Cellaria jistulosa, var. australis, MacGillivray.
(Pl. XIV. figs. 4, 4a, 42.)
Zoartum much and irregularly branched, consisting of
stout, unjointed, cylindrical stems (made up of as many as ten
rows of cells), often of considerable length, tapering slightly
downwards, from which similar shoots are given off without.
regularity on all sides, originating in a horny base, which
rises in all cases from the centre of a zocecium; the whole
rooted by a mass of tubular fibres. Zoweia very regularly
six-sided, usually truncate above and below, contiguous in the
same line; of considerable depth, the walls sloping inward
and minutely pitted, slightly crenate at the top; area very
small, occupying the lower half of the cell; orifice central,
arched above, the lower lip carried up into a very prominent
mucronate projection, rounded at the top, a small denticle on
each side of it; above the orifice a large circular ocecial
opening. Aviculartwm in the line of the cells, placed on a
transversely oblong area, suberect; mandible very wide and
shallow, arched above and straight below, directed upward.
Loc. Victoria (MacGillivray) ; Port Philip Heads (J. B.
Wilson).
This form is described by MacGillivray as C. fistulosa, var.
australis ; but the differences between it and the normal C,
fistulosa are such as to raise a doubt whether it would not
more properly be ranked as a distinct species.
J am unable to say whether the peculiar habit of growth
which characterizes all the specimens I have seen is con-
stant; but if so, it is a point of considerable importance.
The jointing of the stem, by which it is divided into definite
segments (or internodes) in the ordinary forms of Cellaria,
has disappeared, and with it the regular dichotomous ramifi-
cation. ‘The shoots are continuous throughout, and the
branches are given off irregularly, each of them originating
from the centre of one of the zocecia, to which it is attached .
by a chitinous base (Pl. XIV. tig. 4a).
The large size of the cylinders is also a distinctive point,
for though there is considerable variability in this respect in
.
General History of the Marine Polyzoa. 369
CO. fistulosa, it never, I believe, makes any approach to the
size and stoutness of habit which we find in the present form.
But the most important differences are found in the cell. The
orifice is placed very low down, about the centre of it; the
space above it is occupied by the opening to the ocecium,
which is very large and circular in form. Round the upper
part of the orifice there is a kind of border, which seems to
pass downward behind it.
The lower margin is elevated into a mucronate process,
which more or less conceals a considerable portion of the
opening, and in each corner, between it and the side walls of
the orifice, is a conspicuous white denticle. The mucronate
extension of the peristome is very conspicuous when the cell
is viewed in profile. In C. fistulosa the lower margin is all
but straight, and the denticles are (so far as my experience goes)
wanting. The avicularium resembles in general character that
of C. fistulosa, but it is very much wider and almost erect and
has an extremely shallow mandible; the area on which it is
placed is also of a different shape.
In spirit-specimens a delicate membrane is present, which
covers the whole of the front of the cell (including the ovarian
opening), with the exception of the oral operculum.
EXPLANATION OF THE PLATES.
Prate XIII.
Fig. 1. Membranipora marginella, 0. sp.
Fig. 2, Membranipora favus, n. sp.
Fig. 3. Microporella violacea, Johuston, form plagiopora, Busk,
Fig. 4. Lepralia robusta, n. sp.
Fig. 5. Porella malleolus, n. sp.
Fig. 6. Smittia trispinosa, Johnston, form biémucronata, n.
Figs. 7, 7 a. Smittia trispinosa, Johnston, var. 1.
PLATE XIV.
Fig. 1. Flustrella hispida, Fabr., form eylindrica,n. 1a, Nat. size.
Figs. 2,2 a. Flustrella dichotoma, v. Suhr (sp.): zocecia, magnified. 2 6,
Nat. size.
Fig. 3. Pedicellinopsis fruticosa, n. gen. and sp.: group of polypides. 3a.
Nat. size (about). 36, Two polypides. 3c. Portion of tube.
Fig. 4. Cellaria fistulosa, var. australis, MacGillivray : zocecia, magnified.
4a. A single cell, showing the origin of a branch. 46. Nat.
size, Showing the peculiar mode of branching.
370 Mr. C. O. Waterhouse on new Coleoptera,
XLII.—New Coleoptera in the British Museum.
By CuHar_es O. WATERHOUSE.
Dynastide.
Fleteronychus simplex, n. sp.
Niger, bene convexus, nitidus, subtus piceus; thoracis lateribus laxe
subtiliter punctulatis ; elytris sat fortiter punctato-striatis, apice
crebre punctato ; pygidio sat fortiter punctato, medio apiceque fere
leevibus ; pedibus nigro-piceis, tarsis piceis, tibiarum corona apicali
spinis circiter quinque instructa.
Long. 6-7 lin.
Very similar to 1. arator, Fabr., but with fewer spines at
the apex of the posterior’ tibia. Head finely rugulose.
Thorax one third broader than long, parallel at the sides,
arcuately narrowed in front; punctuation very fine, not very
close (often obscure); the punctures at the posterior angles
distinct, and at the anterior angles rather strong. Scutellum
smooth. Elytra with the sutural stria strongly marked,
closely punctured. Hach elytron with eight lines of distinct
punctures ; the intervals between them nearly equal; the first
line is entire; the second does not quite reach the apex; the
third and fourth terminate at one quarter from the apex; the
fifth and sixth lose themselves in the apical punctuation; the
seventh and eighth are composed of distinct punctures near
the shoulder, but posteriorly the punctures are extremely fine
and the line is apt to be broken. ‘There are generally a few
punctures on the first interstice. The apex is moderately,
closely, and strongly punctured. The two lines which form
the stridulating-organ on the propygidium are very distinct,
nearly parallel, and a little less than one millimetre apart.
At the apex of the posterior tibie there are the usual two
strong spines at the lower angle, and two long, very slender
spines at the upper angle; on the outer margin there are five
not very long, stout, lanceolate spines.
Hab. China (J. C. Bowring, Esq.).
Cetoniide.
Pecilopharis uniformis, n. sp.
Allied to P. emilia, White, but relatively a little broader.
Entirely of an olivaceous-green colour, immaculate. Head
finely punctured ; the clypeus not impressed in the middle of
the front margin, which is nearly straight. Thorax a trifle
Mr. C. O. Waterhouse on new Coleoptera. 371
broader in front, impunctate, as well as the scutellum. Elytra
with five or six lines of shallow punctures (which are open
posteriorly), the lines not reaching the apex; the sides of the
elytra are posteriorly marked with transverse stria, as in
P. emilia. The pygidium more closely striolate than in
P. emilia, Anterior tibiz with three acute teeth at the apex,
placed close together, parallel to one another, and at right
angles to the tibia. Length 10 lines.
This last character will at once distinguish it from its allies.
Hab. Santa Anna, Solomon Islands (H. B. Guppy).
Pecilopharis Curtisit, n. sp.
Allied to the preceding; and, like it, of a uniform colour,
except that there is a slight coppery tint in certain lights.
The clypeus has a slight impression in the middle of the front
margin, which is very slightly emarginate; the punctuation
is closer and stronger than in P. emilia, and there is a mix-
ture of extremely fine punctuation. ‘Thorax with some exces-
sively fine punctures above, and a few larger ones at the sides.
Elytra very smooth, much flattened at the apex, with no lines
of punctures, but a few excessively fine punctures may be
traced here and there ; the apical half of the lateral margin
is transversely striolate. The pygidium is rather more
strongly and decidedly more closely striolate than in P. emilia.
The anterior tibie have three apical teeth, two approximate
at the apex, the third slightly removed from the others.
Length 10 lines.
Hab. Batchian (C. Curtis).
This species has the elytra less suddenly declivous at the
apex than its allies.
Buprestide.
Chalcotenia leta, n. sp.
Valde elongata, nitida, cyanea; thorace rugoso, pallide pollinogo ;
elytris viridi-cyaneis, quadricostatis, interstitiis flavo-pollinosis.
Long. 21 lin., lat. 73 lin.
Allied to C. gigas, but a little broader, the thorax relatively
broader posteriorly. Light sky-blue above, the raised parts
on the thorax darker; the whole underside very dark blue,
almost black in parts. ‘The thorax has numerous, irregular,
raised smooth spots above, the intervals finely punctured.
The coste of the elytra are as in C. gigas, but the third one
is shorter. ‘The apex of each elytron has four or five acute
teeth, but the sutural angle is scarcely more produced than
the other teeth. ‘lhe underside is shining, with very numerous
372 Dr. G. Biitschli on the Gastrea- Theory.
small (generally elongate) marks, which are finely punc-
tured, and generally filled with yellow pollen. The under
flanks of the prothorax, the sides of the metasternum, the
metathoracic epipleura, and the sides of the basal segment of
the abdomen are not densely and finely punctured as they are
in C. gigas.
Hab. Queensland.
Erotylide.
Aulacochilus humeralis, n. sp.
Ovate, very convex, shining, black. Hach elytron with
two large yellow spots, the basal one occupying all the
shoulder, nearly touching the scutellum, but leaving the
narrow reflexed lateral margin black; the spot is oblique on
its inner margin and trisinuate posteriorly. The second spot
is behind the middle, transverse, lunate. ‘The head is very
distinctly and moderately thickly punctured. The thorax is
narrowed in front, finely but distinctly and moderately closely
punctured. ‘The sides are rather straight (as compared with
allied species), the margins strongly incrassate ; the incrassate
margin much wider at the anterior angles; the anterior angles
rather prominent. The elytra are very delicately striate-
punctate, the intervals obscurely punctured. Length 44 lines.
Hab. Pasamanca, Philippine Islands (‘ Challenger’ Haped.).
This species is allied to A. guadrisignatus ; but is quite
black, more convex, the thorax straighter at the sides, with
more incrassate lateral margins, and the humeral spot of the
elytra does not leave a black spot on the callus.
British Museum, South Kensington.
XLUI.—Remarks on the Gastrea- Theory.
By G. BurscuHi *.
[Plate XV. ]
In the sphere of speculation on the Metazoa as regards their
developmental history and phylogenesis the explanation of the
probable origin of the primitive bilamellar form has hitherto
formed a principal difficulty. Hence, of course, the concep-
tion which one must form of the general morphology of this
first bilamellar Metazoan form has also varied.
* Translated by W. 8. Dallas, F.L.S., from the ‘ Morphologisches
Jahrbuch’ (1884), Band ix. pp. 415 427,
Dr. G. Biitschli on the Gastreea- Theory. 373
The most usual view, which, as is well known, Hickel first
endeavoured to establish, holds this primitive form to be the
so-called gastrula, or, translated into phylogenetic language, the
gastrea. ‘The conception of the phylogenetic origin of this
gastrea is also conformable to this view ; it was produced, as
indeed may so frequently be observed ontogenetically, by the
invagination of a one-layered blastula or blastosphere. The
deviations from this primitive course of development of the
gastrula which occur in the ontogeny of numerous Metazoa
may then be explained by the assumption of secondary
deviations, changes of the original course of development.
In opposition to this view different ideas were put forward,
especially by Ray Lankester * and Metschnikoff +, who, not-
withstanding certain differences, agreed in this, that they dis-
puted the originality of the production of a bilamellar form by
invagination, and thus endeavoured to deprive the so-called
invagination-gastrula of its significance as a primitive form.
In the place of this latter bilamellar form they sought to set
one which also sometimes occurs in ontogeny, namely the
so-called planula-form, which is destitute of a primitive
mouth. Ray Lankester thought that we might regard as the
most primitive that form of the planula which is furnished
from the first with a central cavity; while Metschnikoff
expressed himself in favour of the view that those planula-
forms are the most primitive which are originally (¢. e. after
bilamellarity has been preduced) solid, and only subsequently
acquire an intestinal cavity by the separation of the central
entodermal cell-mass. ‘he difference in the views of the
two naturalists is chiefly caused by differences in their specu-
lative opinions as to the processes of nutrition which led to
the production of a special nutritive entodermal cell-layer.
But upon this point we shall hereafter have to enter more
into detail.
Considering these contradictory views and the small pro-
spect that is nowadays offered to us of attaining with our
speculations to any thing really elucidatory, it might perhaps
seem desirable to suppress a third view, to some extent inter-
mediate between those above referred to._ If I nevertheless
venture to develop it here briefly, 1 may plead that it pre-
sented itself to me very unexpectedly in the course of other
investigations, and that, after I had long pursued it, it
* KE, Ray Lankester, “Notes on Embryology and Classification,”
Quart. Journ. Mier. Sci. n. s. vol. xvii.
+ E. Metschnikoff, “ Spongiologische Studien,” Zeitschr. fiir wiss,
Zool. Bd. xxxii., and also “ Vergleich, embryol, Studien,”’ 2¢d, Bd. xxxyi,
and XXXVil.
374 Dr. G. Biitschli on the Gastrwa- Theory.
received a sort of confirmation by a discovery which came
from quite another side.
When the business is to ascertain, in a speculative fashion,
the course of a phylogenetic process, it seems to me that in
general a discussion of the primitiveness of the ontogenetic
process is very difficult, and has little prospect of result. It
appears to me, on the other hand, to be much more important
that for certain stages of the assumed phylogenetic course of
development there are at the present day, or have been for-
merly, representatives which demonstrate the possibility of
the existence of these stages. Finally, it seems to me very
important that the changes of the assumed forms should be
readily intelligible, and occur gradually, not suddenly, and
also should be really advantageous. In the last respect espe-
cially I think that the new view now to be developed possesses
some advantages over its predecessors.
The starting-point of my observations was formed by the
colonies of the Flagellata, for, as has already frequently been
urged by myself and others, we must undoubtedly connect
the derivation of the Metazoa with some such forms. I[
believe that in connexion with this, moreover, it is of com-
paratively little consequence whether the Flagellata that
we adduce for comparison possess either a more animal or
a more vegetable mode of nutrition, as the physiology of
nutrition varies much, without reference to the morphology,
in the section Flagellata. Now we certainly find among the
colonies of the Flagellata not a few which in their structure
represent a so-called blastula-form, as among the Volvocinese
the genera Volvox and Hudorina, and, further, especially the
genus Uroglena, and approximately some others.
Nevertheless the difficulty of deriving a bilamellar form
from such colonies appears to me to be very considerable, and
so, indeed, according to either of the hypotheses previously
mentioned. ‘The assumption of the invagination of such a
blastula-stage presupposes the differentiation of one half, or, at
any rate, of a section of the cell-sphere. ‘The one half would
become nutritory, and therefore the entoderm, while the
other would remain essentially locomotory. Liven this differ-
entiation will be difficult to bring into harmony with the
presupposed spherical formation. Such a cell-vesicle, in
connexion with its general uniformly rotating movement,
will present little chance of the occurrence of a differentiation
into two different half-spheres. Should a differentiation of
two kinds of cells occur, it would certainly be much more
advantageous to such an organism if the different kinds of
Dr. G. Biitschli on the Gustrea- Theory. 375
cells were uniformly distributed intermixed over the surface
of the sphere.
To this may be added further, as indeed has already been
pointed out by Metschnikoff and others, that the advantages
of a commencing invagination of one half into the other are
not very intelligible; and in this view I also entirely agree.
Perhaps, therefore, it would be better to allow the bilamellar
form to originate from the blastula-stage referred to by a
process of so-called delamination, therefore in the way which
Metschnikoff and Lankester regard as the more primitive.
But even this view seems to present very serious difficulties.
The hypothesis put forward by Lankester seems to be quite
inadmissible, namely that the inner ends of the cells of the
unilamellar blastula were particularly entrusted with the assimi-
lation of the nutriment, and finally even split themselves off
as independent entodermal cells. It is difficult to recognize
in this an advantage to the collective body. We might say
that the separated entodermal cell is deprived of its better
half, 7. e. the ectodermal part, which brought it nourishment ;
nay, one might really say with justice, it is deposed from its
function. But to make up for this, according to Lankester’s
conception, a further change now occurs, that is to say, the
reception of nourishment becomes concentrated upon one spot
of the surface of the sphere, and the nourishment penetrates
here into the intestinal cavity, at first without the existence of
any mouth-opening. In the first place, this localization of
the reception of nutriment would certainly be a disadvantage,
and not an advantage ; and further, this profound change of the
whole process of reception of nourishment is supposed to take
place without any visible cause, and, moreover, quite suddenly.
I think, theretore, that we cannot accept as satisfactory
Lankester’s hypothesis as to the origin of the bilamellar
embryonal form. Metschnikoff’s idea also seems to me to
suffer under inherent improbabilities, in many respects corre-
sponding with those which have been brought forward against
Lankester’s hypothesis. Metschnikoff supposes that indi-
vidual cells out of the unilamellar cell-wall of a blastuloid
primitive form wandered into the interior of the vesicle, and,
indeed, especially such cells as had received nourishment
particularly abundantly. This immigration, which was
originally only occasional, gave rise finally to a constant accu-
mulation, a central mass of cells, ¢. e. to the formation of an
entoderm, which originally neither enclosed a central primitive
intestinal cavity nor was accessible through a mouth-opening.
As, however, the formation of an entoderm is inconceivable
376 Dr. G. Biitschli on the Gastrea- Theory.
unless real advantages in nutrition thereby occur, with which,
indeed, the differentiation of this germinal layer seems to be
causally connected, the question is, Can we really demonstrate
actual advantages for the process of nutrition, which render
the immigration of the entodermal cells admissible? It seems
to me, however, that the immigration of the entodermal cells,
to which the reception of nourishment-is confided, cannot be
regarded as an advantage. Without the simultaneous for-
mation of a mouth-opening, which, as in Lankester’s hypo-
thesis, is unintelligible and destitute of motive, the immigration
of the entodermal cells would, in my opinion, have been only
disadvantageous, because, if we may so speak, they would
thereby have bolted themselves in.
These and similar considerations, but especially the endea-
vour to establish a plausible connexion between invagination
and delamination, led me to the idea that probably the
spherical blastula might not have been after all the starting
form of the first bilamellar stages; and I believe that both
ontogenetically and among fully-developed organisms stages
are presented which form more satisfactory starting-points
than the blastula for the bilamellar stage.
Among the colonies of the Flagellata there is a genus of
Volvocinee which is constructed upon the type of the uni-
lamellar cell-plate, namely Gontum, and a very nearly allied
one which occurs in the form of a unilamellar ring. When
once the notion had occurred to me that bilamellarity might
well have commenced in the stage of such a cell-plate, the
conception seemed to me to offer the most favourable condi-
tions for arriving at a satisfactory idea of the phylogenesis of
the gastrula formation.
Accordingly it appears to me to be assumable that the bi-
lamellar stage first occurred in a Protozoan colony, the cells
of which were arranged side by side in the same plane, so as
to form a one-layered plate. ‘Then, all the cells dividing
parallel to the surtaces of the plate, there was next produced
a two-layered plate, of which the two layers of cells perhaps
still showed no differentiation. or the sake of intelligibility,
and because this has since been kept similar, we shall give
his stage of the bilamellar plate the name of placula.
Moreover, it is easily conceivable that the two sides of a
unilameliar plate might develop different functions—that the
one might adapt itself chiefly for locomotion and the other for
nutrition, and that, finally, in the passage into the two-layered
state, these two functions may have been localized upon the
two cell-layers *.
* Many reasons derivable from the structure of the Flagellata and their
4
Dr. G. Biitschli on the Gastrea-Theory. 377
We therefore take such a two-layered plate as the starting-
point, and will see, in the first place, how a gastrula-like form
could be developed from it. Clearly by the simple incurvation
of such a placula towards the entodermal surface, and final
conglobation until the formation of a blastopore. But, one
naturally asks, what advantage will such an incurvation of
the plate possess ? Upon this point various statements may
be made. The incurvation of the plate, and particularly of
its entodermal layer, which is at first but slight, will enable
large nutritive masses to be attacked simultaneously by a
number of neighbouring cells, and at the same time the cavity
of the underside will serve as a sort of trap in which prey
may be captured and held fast, if the curved plate lowers
itself over a prey resting upon some support. Both advan-
tages will become more and more marked the more the curva-
ture makes itself felt; and the disadvantage which consists
in the fact that the invagination-aperture gradually diminishes
in size, may be compensated by the increased security of the
prey when captured, of which it is the cause.
The next question, however, is whether a course of deve-
lopment such as we have constructed hypothetically is any-
where ontogenetically represented, and this is actually the case.
It occurs mostly in certain Nematoda, such as Cucullanus
according to Butschh*, and in the main also in Rhabdonema,
according to Géttet. In these cases the result of the process
of segmentation is a two-layered cell-plate, a true placula
consisting of ectoderm and entoderm, which afterwards be-
comes incurved as above described, and passes into the
gastrula-stage. Indications of the same course of develop-
ment are also frequently to be seen, although usually the
plate-form does not appear in such purity, seeing that between
the two layers there occurs a small accumulation of fluid, 7. e.
a segmentation-cavity has been developed, which was entirely
wanting in the first-mentioned cases. I will here cite a few
examples which distinctly show such a plate-form :—Lumbri-
cus according to Kowalevsky, Paludina, Chiton, according to
Kowalevsky’s investigations ; further, Sag¢tta, in which the
segmentation-cavity is very slightly developed; and, finally,
colonies make me regard the first-mentioned view as the more probable.
Unfortunately, however, I am unable to cite any plausible advantages for
the commencement of the bilamellarity of the plate, although this may
perhaps have occurred simply by special conditions of growth, and at any
*rate one cannot see that any disadvantage could accompany the com-
mencement of bilamellarity.
* * Zeitschr. f. wiss. Zool. Band xxvi. p. 103.
+ Abhandlungen zur Entwicklungsgeschichte der Thiere, Leipzig, 1882,
Ann. & Mag. N. Hist. Ser. 5, Vol. xiii. 25
378 Dr. G. Biitschli on the Gastrea- Theory.
Phoronis and Ascidia mentula, according to Metschnikoff. Of
course we here leave out of consideration all those cases in
which the original conditions appear to be obscured by an
abundant development of nutritive vitellus.
Our conception, therefore, requires that, in opposition to the
ordinary pre-existing notions, we should regard the so-called
blastula-stages not as palingenetic developmental forms. In
this we partly agree with Lankester and Metschnikoff, both
of whom regard the so-called invagination-blastula, 7. e. the
blastula which becomes converted into the bilamellar gastrula
by invagination, as a ccenogenetic form.
My conception, however, also brings the so-called delami-
nation-gastrula into the series of coenogenetic forms; and this
consequence, in general, need not be regarded as contradictory,
although the important differences of the two kinds of blasto-
spheres are just as marked from my point of view as from
those of the two above-mentioned naturalists.
The production of the so-called invagination-gastrula from
the bilamellar placula, which we have assumed as the primary
stage, is not difficult to understand. It took place simply by ac-
cumulation of fluid between the two cell-layers, by which these
were gradually more and more separated from each other and
finally inflated into a spherical form, so that one half of the
wall of the sphere was formed by the ectoderm and the other
by the entoderm. The right to conceive of the formation of
the invagination-gastrula in this fashion may be based upon
the fact that all possible degrees of transition between the
simple bilamellar plate and its more or less considerable sphe-
rical inflation by the development of a segmentation-cavity,
occur in the ontogeny of different Metazoa.
At any rate, it is for the present just as permissible and
justifiable to endeavour to derive the invagination-blastula
from the bilamellar plate in the manner here indicated, as, on
the contrary, to adopt the opposite course, which has hitherto
been usually followed, and to regard the plate as a coenogenetic
product of metamorphosis of an original blastula. In accord-
ance with our view, however, we must again, in this place,
put the question, Could the transformation of the so-called
placula into the blastula-form confer upon the developing
embryo certain advantages which are of a nature to give pro-
bability to the occurrence of such a ccenogenetic process ?
To this I have but little to answer, and hence it appears to
me that here lies a weak point of the hypothesis. How-
ever, it may be noted that the production of the spherical
form may have given rise to an increased mobility of
the incipient stages of development, of course under the
Dr. G. Biitschli on the Gastrea- Theory. 379
supposition that a very early issue of the embryo from the
ege-envelopes has been the rule, which, considering the
process of development of the simplest living Metazoa,
appears not very improbable. On the other hand, an advan-
tage might be found in the circumstance that a blastuliform
metamorphosis of the plate is favourable to any eventual
nourishment of the embryo by fluid aliment introduced from
without, the receptive surface being increased by the inflation
into the spherical form. That such a process does occur may
perhaps be indicated by the accumulation of fluid which so
frequently leads to the formation of a segmentation-cavity,
and which, at any rate, points to an imbibition of the cells
from without.
I might here bring forward another point, namely, that the
developmental history of the blastula, which we see perma-
nently preserved in certain Volvocinex, is by no means the
same as that which we observe in the so-called invagination-
blastula. Thus the blastula of the Volvocinez does not origi-
nate by the central separation of the cells of a cell-aggregate,
but by the gradual incurvation of a unilamellar cell-plate,
during which, therefore, the cavity of the blastula, which only
becomes closed by degrees, remains open by a sort of blasto-
pore until the last moment of the incurvation.
I now come to say a few words of the delamination-
gastrula, which, as already shown, must also, in accordance
with our hypothesis, not be an original form. As a matter
of course the original process which produces the bilamel-
larity of our placula is a process of delamination, and we have
therefore at any rate to regard the delaminative production of
the entoderm as original, and we may do this the more be-
cause the invaginated entoderm of the invagination-gastrula
originally also separated itself from the ectodermal cells by a
division (delamination). Whether this separation of the
elements of the ectoderm and entoderm takes place earlier or
later seems to be a matter of indifference, as indeed Ray
Lankester has already sufficiently pointed out, as it is easy to
understand how a separation of the two kinds of elements
would occur constantly earlier and earlier, until finally even
the first segmentation permanently separated the ectodermal
and entodermal elements, and indeed we see this actually
carried out in the interesting example of Lhabdonema
(according to Gétte). While in this way an acceleration
of the separation of the two kinds of elements proves
to be favourable, it certainly appears conceivable also that
under certain circumstances a retardation might occur,
aud this might satisfactorily explain the phenomenon of
25*
380 Dr. G. Biitschli on the Gastrea-Theory.
the delamination-gastrula. In this case, just as we see in
the Volvox-blastula at the present day *, a contraction of the
still unilamellar cell-plate occurred betore the formation of
the entoderm, and the formation of the entoderm took place
only subsequently within the closed blastula. The advan-
tages of such an anticipatory sphere-formation would be the
same that have been already urged in regard to the develop-
ment of the invagination-blastula. But, should this concep-
tion of the delamination-gastrula prove to be correct, an
essential difference from the invagination-blastula must have
shown itself in the history of its production, or been able to
show itself, as it is conceivable that this difference may be
cancelled by secondary variations. While the invagination-
blastula is formed by the separation or divergence of the
segmentation-cells (Pl. XV. figs. 2a, 3a, 3b), the delami-
nation-blastula must, on the contrary, have originated by a
process of incurvation like that which leads to the formation
of the blastula of Volvow (Pl. XV. figs. la-1d). The mate-
rials at my command upon the history of the formation of the
delamination-blastula furnish no certain data for the settlement
of this question, but at the same time they are not adverse to
our conception. From the representation that Fol T gives of
the production of the delamination-gastrula of the Geryonida,
our conception may perhaps obtain some support; at least, in
his fig. 5 Fol represents a 16-celled stage, which closely agrees
with the corresponding stage of Volvox. Although the figure
does not show this quite certainly, it nevertheless seems to be
pretty well indicated that the four cells of the inferior sur-
face do not close together, and therefore the already existent
blastula-cavity still communicates through an inferior aperture
with the outer world, just as in Volvox. In general, however,
little attention has hitherto been paid to this not unimportant
question in the formation of the blastula.
Asa matter of detail we have still the question, which state
of the delamination-gastrula are we to regard as the more
primitive, that with an original primitive intestinal cavity or
that with a solid entodermal mass, the so-called “ parenchy-
mula” of Metschnikoff? In accordance with the hypothesis
to which we have hitherto adhered, we must, with Lankester,
* On the development cf this see Goroshankin, “Genesis im Typus der
palmellenartigen Algen,” in Mitth. d. k. k. russ. Ges, naturf. Freunde zu
Moskau, Bd. xvi. (in Russian ),and Kirchner, “ZurEntwicklungsgeschichte
von Volvox minor” in Cohn’s Beitr. zur Biologie der Pflanzen, Bd. iii.
A connected exposition of the reproduction and developmental phenomena
of the Volvocinez and their allies will be found in the next section, on
the Flagellata, in my Protozoa.
+ Jenaische Zeitschrift, Bd. vii. p. 471, Taf. xxiv.
Dr. G. Biitschli on the Gastreea- Theory. 381
although upon other grounds, decide in favour of the primi-
tiveness of the first form. We come to this decision the more
readily because we have already indicated that the so-called
parenchymula appears to us, as a primitive form, to offer great
difficulties as regards its explanation.
We must not close this discussion without pointing out
that, in considering these circumstances, we have purposely laid
no stress upon the ontogeny of the Sponges. In this respect
my ideas are directly the reverse of those of Metschnikoff, to
whom the ontogeny of the Sponges appears to be especially
favourable to his parenchymula theory. As [ am of opinion
that the group of the Sponges is completely shut off from
the rest of the Metazoa, proceeding quite independently from
the section Choanoflagellata (Savile Kent), it appears to me
incorrect to bring this group into consideration in the expla-
nation of the phylogenesis of the other Metazoa.
Finally there still remains for discussion one circumstance
which may perhaps give essential support to our hypothesis,
namely, the quite recent discovery of an organism which in
many respects fulfils the requirements which we must lay
upon the hypothetical, tabulitorm, bilamellar primitive stage,
our placula.
This organism is the singular marine Trichoplax adherens
lately described by F. E. Schulze*. Although the life-
history and especially the reproduction of this form are not
thoroughly elucidated, it nevertheless appears certain to me,
as well as to Schulze, that it is a mature, fully-developed form,
and not a larva. This Zrichoplax, then, would in every re-
spect form a representative of our placula, if it had not already
made an advance towards a higher development, inasmuch as
it forms, not a bilamellar, but a trilamellar plate. Between
the entoderm, occupying the lower surface, which resembles
a cylinder-epithelium, and the thin flat-celled ectoderm cover-
ing the upper surface, there is interposed a connective-like
layer, no doubt proceeding from the entoderm, and which is
comparable to amesoderm. For my part, I regard the com-
parability of the tissue-layers of this Zrichoplax with the
germinal layers of the Metazoa, already indicated by F. E.
Schulze, as exceedingly probable, except as regards a direct
homology of the intermediate so-called mesoderm, which is
rather to be esteemed an independent analogous formation.
However, I regard it as very probable that Zrichoplax
adherens forms one of those transitional forms towards the
higher Metazoa, constructed in accordance with the gastrula-
* Zool. Anzeiger, Jahrg. vi. no. 132 (1883), p. 92,
~
382 Dr. G. Biitschli on the Gastreea- Theory.
plan, such as we might expect to meet with upon the above-
stated hypothesis.
As I had formulated the outlines of the hypothesis before
the publication of Schulze’s discovery, I was surprised to find
in the latter, in a certain degree, such unexpected confirma-
tion of purely speculative considerations. Although, there-
fore, the present hypothesis is not based upon the interesting
Trichoplax, nevertheless the latter has furnished the induce-
ment to publish the speculation. Jam, indeed, not convinced
that our science will derive any direct gain from the pursuit of
such speculative endeavours, but perhaps they may furnish
some incitement to a more accurate investigation of the onto-
genetic history of the formation of the blastule and gastrule,
by means of which the most probable hypothesis, 7¢.e. the
one which is at once freest from contradictions and most ex-
planatory, will finally obtain the victory.
EXPLANATION OF PLATE XV.
On the accompanying Plate I have endeavoured, by means of a few
diagrams, to elucidate the ideas developed in the preceding pages as to
the reference of tle different forms of blastulee and gastrule to a common
starting-point. That process which I regard as the most primitive is
represented in figs. la-2a-d. Fig. 1, binary division; fig. 2a, eight-
celled stage: by an equatoreal segmentation the (tinted) entodermal
elements haye separated from the (white) ectodermal elements. Of
course, under certain circumstances this separation may take place either
earlier or later. Fig. 2b, section. The ectodermal and entodermal cells
have increased and now form a very distinct placula. In fig, 2 this
commences its curyature towards the entodermal surface; and this leads,
finally, as in fig. 2d, to complete invagination of the entoderm,
Figs. 1 a, 2a, 3a-8c show the development of the so-called invagina-
tion-blastula. The further development of the stage fig. 2a
is altered in this way: the severed ecto- and entodermal cells
are separated from each other by the development of a seg-
mentation-cayity (fig. 3a), and finally lead to the blastula.
This, of course, consists of two different parts—an ectodermal
and an entodermal section. Itis particularly to be noted, how-
ever, that the relative size of these two sections appears to be
very different in the different invagination-blastule, which
may be referred to an earlier or later severance of the ecto-
and entodermal elements, as well as to the relative quantities of
these two elements. The stage fig. 3d passes finally, in the
well-known manner, by invagination (fig. 3c) into the gastrula-
stage.
Figs. 1a-1 e represent the delamination-blastula. Fig. 1 a, binary divi-
sion. Fig. 10, eight-celled stage, but with only four cells drawn
in side view. ven in the four-celled stage the tendency to-
wards incurvation will be expressed, leading to a change of
position in the cells, so that these now direct their entodermal
parts axially. At the same time it may happen that the groove
which effects the transition from the four- to the eight-celled
Mr. L. F. Ward on Mesozoic Dicotyledons. 383
stage runs nearly or quite equatoreally, namely, if a change of
position of the first four segmentation-spheres round a right
angle has occurred. By further divisions, all of which really
run parallel to one another and appear to be radially directed
towards the centre of the embryo only in consequence of the
continued incurvation, the stage fig. le (section) is produced ;
this already shows a distinct cavity, which, however, is still open
at the inferior surface. Finally, this stage passes, in an easily
intelligible manner, by further increase of cells and final closure,
into the blastula, which, according to our view, originates in
accordance with the blastula of the Volvocineze. All the cells
of this blastula are still composed of the two elements, the
ecto- and entodermal parts, which are now severed by an equa-
toreal groove dividing each cell into an external and internal
portion (fig. le). The cutting off of the entodermal portions of
the delamination-blastula appears not always to proceed so
uniformly as is here represented in accordance with the process
demonstrated in the Geryonida by Fol and Metschnikoff. At
least the representation that Kowalevsky gives of the delamina-
tion in Encope seems to indicate that the division sometimes
takes place successively, and thus the central cavity of the
blastula is gradually filled with the entodermal cell-material.
That here perfectly solid entodermal contents are first of all
produced, in which an archenteric cavity only subsequently
makes its appearance, may certainly be regarded as a secon-
dary variation. The Siphonopora, however, present another
variation of the delamination-blastula, as in them the develop-
ment of a blastula-cavity is suppressed, and an archenteric
cavity is only subsequently developed in the entodermal cell-
mass. The reference of this modification to the mode in the
Geryonida, which I regard as the original mode, appears to
present no particular difficulties.
XLIV.—On Mesozoic Dicotyledons. By Lester F. Warp*.
In the following remarks on Mesozoic Dicotyledons, I con-
fine the term Dicotyledons to that subclass of the vegetable
kingdom which is embraced under the term Angiosperms in
most modern text-books of botany. This is the usage of
most vegetable paleontologists T, and the reasons of adopting
it have been frequently statedf.
The Dicotyledons occupy somewhat the same position in
the history and development of plants that the Mammalia
occupy with respect to animals. They constitute the domi-
nant type, and in their rapid march have now so completely
* From the ‘ American Journal of Science,’ April 1884, pp. 292-803.
+ Goppert, Geinitz, and one or two others conform to the Jussizan
system.
t See the ‘ American Naturalist,’ yol. xii. (June 1878), pp. 359-878.
384 Mr. L. F. Ward on Mesozoic Dicotyledons.
gained the ascendant as to dwarf all other forms into relative
insignificance. ‘They include nearly all the deciduous forest
trees, the shrubby undergrowth, the leafy herbage, and the
weeds of all temperate regions.
But this has not always been the case. In fact the reign
of the Dicotyledons, geologically considered, has been very
brief. Although there is evidence that the earth has been
covered with vegetation since the beginning of the Carboni-
ferous age at least, still there is nothing to warrant us in
saying that a single dicotyledonous plant existed prior to the
close of the Jurassic. Indeed, we do not know from the
actual discovery of specimens that this type appeared earlier
than the second recognized group of the Cretaceous—the
Urgonian. Until quite recently the presence of these plants
in formations lower than the Miocene was so rare that it was
with the Tertiary rather than with the Cretaceous that the
existing dominant vegetation of the globe was assumed to
have originated.
Notwithstanding this, some of the earliest, if not the very
earliest, discoveries of these forms were in Cretaceous strata.
In the stone-quarries of the Harz Mountains near Blanken-
burg, were found, near the beginning of the eighteenth cen-
tury, prints of large leaves which the workmen believed to
be those of the grape-vine, and which were mentioned by
Scheuchzer, Briickmann, and Walch, but without any attempt
at their scientific determination.
A brief historical review of the discovery, identification,
and publication of dicotyledonous species in Cretaceous strata
of Europe and America, including the arctic regions, will
show the importance which this subject is assuming among
alzontologists.
In 1833 Zenker* took up in earnest the study of the Blank-
enburg leaf-prints, and described, figured, and named five
species belonging to two genera. One of these genera he
rightly concluded to have no living representatives, and he
therefore named it Credneria, after his friend Prof. Credner,
who collected the specimens.
In 1841 Goppertt figured a number of dicotyledonous leaves
from the Quadersandstein of Silesia, but did not venture to
give names to them.
* ¢Beitrige zur Naturgeschichte der Urwelt,’ von Jonathan Carl Zenker,
Jena, 1833.
+ ‘ Ueber die fossile Flora der Quadersandsteinformation in Schlesien,’
c.,in Nova Acta Acad. Nature Curiosorum, vol. xix. Taf. xlvii., li., liii.
Mr. L. F. Ward on Mesozote Dicotyledons. 385
The next year Geinitz* identified three species in the lower
Quader of Saxony at Niederschéna, the fossil flora of which
lace was so well worked up by Ettingshausen in 1867.
In 1845 Cordat figured some dozen leaves from Trziblitz,
Luschitz, Perutz, and Weberschan, in Bohemia, some of
which localities he placed in the Gault, but they are probably
all in the Lower Quadersandstein, or Cenomanian. He made
no attempt to refer these forms to genera and species.
Unger’s ‘ Synopsis’ { appeared the same year, in which
sixteen species of Cretaceous Dicotyledons are recognized
down to that date. Gdéppert$, however, admitted only thirteen
species in his table published in Bronn’s ‘ Naturgeschichte,’
which also appeared in 1845.
Debey||, in 1848, enumerates sixteen species as previously
published, and adds to these twenty-seven others from the
neighbourhood of Aix-la-Chapelle, most of which, however, he
contents himself with calling Phylites ; and as no figures were
made, it is possible that some of these were not Dicotyledons.
He also gives four Carpolithes which he identifies with dico-
tyledonous orders.
The same year Géppert{] published a supplement to his
Flora of the Quadersandstein, in which a number of Dicotyle-
dons are recognized.
In Ettingshausen’s ‘ Proteaceen der Vorwelt,’ 1851**, four
Cretaceous species are enumerated, and Von Ottotf in his
‘ Additamente,’ 1852-54, also described Proteaceze from the
Quader of Saxony ; while Miquelff, in 1853, described a few
Dicotyledons trom the Upper Cretaceous of Limburg.
* “Characteristik der Schichten und Petrefacten des sachsisch-boh-
mischen Kreidegebirges,’ von Dr. Hans Bruno Geinitz. Heft 3, Dresden and
Leipzig, 1842, p. 97.
+ In: ‘Die Versteinerungen der béhmischen Kreideformation,’ yon
Aug. "im. Reuss. Stuttgart, 1845-46, Taf. 1., li.
. t ‘Synopsis plantarum fossilium’ autore Fr. Unger, M.Dr., Lipsiz,
845
§ ‘ Naturgeschichte der drei Reiche,’ vol. xv. 2 (‘Handbuch einer
Geschichte der Natur,’ iii. 2), von Heinrich G. Bronn. Stuttgart, 1849,
pp. 44-57, 66. ‘
\| ‘ Uebersicht der urweltlichen Pflanzen des Kreidegebirges tiberhaupt
und der Aachener Kreideschichten insbesondere,’ von Dr. M. Debey, in
‘Verhandlungen des naturhistorischen Vereines der preussischen Rhein-
lande,’ 5. Jahrgang, 1848, p. 113.
4 ‘Zur Flora des Quadersandsteins,’ in Nova Acta Acad. Nat. Cur.
xxii. 1, p. 365,
** ‘Sitzungsberichte der mathem.-naturw. Classe der kaiserlichen
Academie der Wissenschaften, Wien,’ Bd. vii. Heft iv. 1851, p. 711.
t+ ‘Additamente zur Flora des Quadergebirges in Sachsen,’ von Ernst
yon Otto, Heft ii. Leipzig, 1854, p. 44.
tt ‘De fossile planten van het Krijt in het hertogdom Limburg,,
Srlem, 1863; Verhandl. Geol. Kaart Nederl. i, pp. 83-56,
386 Mr. L. F. Ward on Mesozoic Dicotyledons.
In 1856 Dunker* described and figured in the ‘ Paleonto-
graphica’ four species from Blankenburg in addition to those
of Zenker, and one cluster of fruit which he believed to belong
to Credneria, and to indicate strongly that those ancient plants
belonged to the Polygonacee. Zenker had divined that they
might be amarantaceous.
One year later Stiehlert reviewed in the ‘ Palesontographica’
the whole subject of the Cretaceous flora of the Harz Moun-
tains, and added to all previous results the discoveries made
by Hampe, a druggist of Blankenburg, in the marls near that
place. Out of the numerous forms of Credneria he carves a
new genus which he calls Httingshausenia, and of which he
makes eight species. He admits seven species of Credneria,
and figures several others which he calls new species, but
without assigning specific names to them.
Thus far America had contributed nothing to the flora of
the Cretaceous, but in 1858 Heer described, in the proceedings
of the Academy of Natural Sciences of Philadelphiat, eight
species of Dicotyledons which had been collected by Dr.
Hayden in Kansas and Nebraska. ‘These, however, he erro-
neously believed to be Miocene.
The next year Mr. Lesquereux § contributed a paper to this
Journal, in which a number of fossil plants from Nanaimo,
Vancouver’s Island, and from Bellingham Bay were described
as Miocene. It is now known that Nanaimo is Cretaceous,
and his paper enumerates six species of Dicotyledons from
that locality.
Nothing further appears to have been done until 1863,
when Dr. Newberry || reported, in the ‘ Boston Journal of
Natural History,’ upon certain fossil plants from Orcas
Island, British Columbia, collected by the North-west Boun-
dary Commission. He declared the horizon Cretaceous, and
among the plants described were four Dicotyledons,
* “ Ueber mehrere Pflanzenreste aus dem Quadersandsteine von Blank-
enburg,” von Wilhelm Dunker. Palzeontographica, iv. 1856, pp. 179-185,
tab. Xxxli.-xxxy.
+ “ Beitrige zur Kenntniss der vorweltlichen Flora des Kreidegebirges
im Harze,” von August Wilhelm Stiehler. Paleeontographica, v. pp. 45-
80, Taf. ix.-xv.
} “Fossil Plants of the Lower Cretaceous beds of Kansasand Nebraska,”
by Oswald Heer, Proc. Acad, Nat. Sci. Phil, 1858, pp. 265, 266.
§ “On some Fossil Plants of recent Formations,” by L. Lesquereux,
Amer. Journ. Sci. 2, xxvii. 1859, pp. 359-366.
|| “ Descriptions of Fossil Plants collected by Mr. George Gibbs, Geo-
logist to the U.S. North-west Boundary Commission under Mr. Archibald
Campbell, U.S. Commissioner,” by J. 8. Newberry, Boston Journ, Nat.
Hist. vii. 1863, pp. 506-524,
Mr. L. F. Ward on Mesozoic Dicotyledons. 387
In 1866 appeared the somewhat famous “ Phyllites créta-
cées du Nebraska” of Capelliniand Heer*, the latter of whom
determined the fossil plants which the former had himself
helped to collect at Blackbird Hill, Nebraska, in the now
well-known Dakota group. The Cretaceous character of these
fossils was here rather grudgingly conceded, and has never
since been seriously doubted.
While America had been thus coming forward Europe had
remained in the background for about ten years, or since
Stiehler’s monograph of the Harz in 1857. It was not till
1867 that Ettingshausen ft published in the ‘ Sitzungsberichte’
of the Vienna Academy his valuable paper on the fossil flora
of Niederschéna in Saxony. The horizon of this place is con-
siderably lower than that of Blankenburg, and belongs at the
base of the Quadersandstein formation of Germany. Never-
theless, the species nearly all belong to living genera
Quercus, Fagus, Ficus, Laurus, Protea, &c. ‘Twenty-eight
species are enumerated.
In the same volume Unger f{ described and figured four
Dicotyledons, thus far unknown, from the Gosau (Upper
Senonian) of Austria, at St. Wolfgang and Neue Welt.
Though contenting himself with calling them all Phyllites, he
yet ventured to assign two of them to the Magnoliacez and two
to the Proteacez.
Returning to America, we find in 1868 the two most
important contributions yet made in this country to the Cre-
taceous flora of the west. ‘These were Dr. Newberry’s “ Notes
on the later extinct floras of North America,’ published in
the ‘ Annals of the New York Lyceum of Natural History’
(April) §, and Mr. Lesquereux’s paper in this Journal || for
July of the same year. Though prepared quite independently
of each other, these two papers followed the same method and:
reached the same results. Both authors give lists of the
American Cretaceous species known up to that date, Dr. New-
berry enumerating 20 and Mr. Lesquereux 21 Dicotyledons.
* Verhandl. d. schweiz. Gesellsch. d. Naturf. Ziirich, 1866.
+ “Die Kzeideflora von Niederschéna in Sachsen, ein Beitrag zur
Kenntniss der altesten Dicotyledonengewichse,” yon Const. Freih. y.
Ettingshausen. Sitzb. lv. Abth. 1, pp. 285-264, Taf. i—iii.
{ “ Kreidepflanzen aus Oesterreich,” yon Dr. F, Unger, . ec. pp. 642-
654, Taf. i,, ii.
§ The figures corresponding in the main to the species here described
were published in separate form by the U.S. G. and G. Survey of the
Territories, F. V. Hayden, Geologist-in-charge, under the title “ Illus-
trations of Cretaceous and Tertiary Plants of the Western Territories of
the United States,” which did not appear until 1878.
\| “On some Cretaceous Fossil Plants from Nebraska,” by L. Lesque-
reux. Am. Journ. Sci. 2, xlvi. 1868, pp. 91-105.
388 Mr. L. F. Ward on Mesozoic Dicotyledons.
The number of species described by Dr. Newberry as new
was 45, and the number by Mr. Lesquereux was 47. Nine
species from Fort Ellsworth, Kansas, included in Mr. Lesque-
reux’s list, the descriptions of which did not appear until the
following year *, do not enter into the figures above given.
It will thus be seen that about 75 species of Dicotyledons had
been described from the Dakota Group and other American
Cretaceous strata down to the year 1869.
Far less could be said for Europe at this date. Hosius f,
in 1869, was able to enumerate in his ‘Geognosie West-
falens’ twenty-five characteristic species of the Quadersand-
stein, which had been described and figured either by Von der
Marck ¢ or by himself §. In this year, too, Heer || published
his ‘ Fossil Flora of Moletein in Moravia,’ which belongs to
the Lower Quadersandstein, or base of the Cenomanian.
Twelve species are described and carefully figured.
In Hayden’s annual reports of the geological survey of the
Territories for 1870 and 18714], Lesquereux continues to
enlarge the list of American species; and in 1872, Heer **,
in his “‘ Fossil Flora of Quedlinburg,” makes further additions
to that of Europe.
We are thus brought down to the year 1874, which is
marked by three very important publications.
Schimper’s ‘'Traité de Paléontologie Végétale’ was com-
pleted in that year, and in its fourth volume {ft 109 species
of Cretaceous Dicotyledons are recognized. Of these 46
are American, which shows that the author was far behind
in the literature of the subject. He also expresses serious
doubts as to the Cretaceous age of these plants, although this
had been long settled here beyond a peradventure.
Next should be mentioned Heer’s “ Kreideflora der are-
* “On Fossil Leaves from Fort Ellsworth, Nebraska,” Transactions of
the American Philosophical Society, Philadelphia, vol. xiii. new series,
pp: 430-483, pl. xxiil.
+ “Die in der westfalischen Kreideformation vorkommenden Pflan=
zenreste ” (Beitrige zur Geognosie Westfalens), von A. Hosius. Miinster,
1869.
t “Fossile.... Pflanzen aus dem Plattenkalk yon Sendenhorst,’’
Palezontographica, xi. 1865.
§ “Ueber einige Dicotyledonen der westfilischen Kreideformation,”
Paleontographica, xvii. 2, pp. 9-104, Taf. xii.-xvii.
|| Beitrage zur Kreideflora. I. Flora von Moletein in Mihren, Zurich,
1869,
q “On the Fossil Plants of the Cretaceous and Tertiary Formations of
Kansas and Nebraska,” Ann. Rep. 1870, p. 870.“ Fossil Flora, Creta-
ceous Strata, Kansas,” Ann. Rep. 1871, p. 301.
** Beitrige zur Kreideflora. II. Zur Kreideflora von Quedlinburg.
tt Pp. 677-679.
Mr. L. F. Ward on Mesozoic Dicotyledons. 389
tischen Zone,” which appeared in 1874 in volume iii. of his
‘Flora Fossilis Arctica.’ In this work he describes one
solitary dicotyledonous species (Populus primeva) in the
schists of Kome—Urgonian—by far the most ancient form
thus far met with, and 33 species in the higher strata of Atane,
which are now generally believed to correspon() with the
Cenomanian of Europe. These researches of Heir appeared
too late to be embodied in Schimper’s great work.
Finally, as crowning this fruitful year’s labour, appeared
Mr. Lesquereux’s important quarto volume on the Cretaceous
Flora of the Western Territories *, reviewing the results of -
all previous researches in this country, and describing and
illustrating 107 species of American Cretaceous Dicotyledons.
In Hayden’s annual report for the same year f 26 species are
described and some figured, but most of these were also more
fully treated in the ‘ Cretaceous Flora.’
During the succeeding six years little activity was mani-
fested in this field, the attention of paleeobotanists being prin-
cipally directed to the floras of later formations ; but in 1880
Hosius and Von der Marck published, in the ‘ Paleonto-
graphica’ f, their “ Flora der westfalischen Kreideformation,”
an important work reviewing the entire Cretaceous flora of
Westphalia. Although fossil plants have been found through-
out almost the entire Cretaceous series as there represented,
still it was only in the Senonian that any Dicotyledons were
detected. At two quite distinct horizons within the Senonian
such plants were found, 37 species being credited to the Upper
and 24 to the Lower Senonian, or 61 species.
Quite an important paper by Dr. Debey appeared in 1881 §,
describing certain very interesting querciform leaves from the
sands of Aix-la-Chapelle. Fifteen species are described and
well illustrated, all of which are referred to Dryophyllum, a
genus founded long ago by Debey on unpublished material,
aud to which Saporta refers four of the forms from the traver-
tines of Sézanne. It had been announced || that Debey had
collected in the vicinity of Aix-la-Chapelle no less than two
* “Contributions to the Fossil Flora of the Western Territories,
Part 1. The Cretaceous Flora.” By L. Lesquereux, being Report of
the U. 8. Geological Survey of the Territories, F. V. Hayden, Geologist-
in-charge, vol. vi. Washington, 1874.
+ Pp. 271-565, pls. i—viil.
¢ Vol. xxvi. 1880.
§ “Sur les feuilles querciformes des sables d’Aix-la-Chapelle,” par
M. Debey. Bruxelles, 1881. (Compte rendu du Congrés de botanique
et @horticulture, 1880.)
|| Schimper, ‘ Traité de Paléontologie Végétale’ (Paris, 1869-1874),
tome iii. pp. 671, 675.
390 Mr. L. F. Ward on Mesozoic Dicotyledons.
hundred species of dicotyledonous plants ; and it is to be hoped
that this paper may form a beginning, at least, of the much-
needed work of acquainting vegetable paleontologists with the
nature of this remarkable flora.
The sixth volume of Heer’s ‘ Flora Fossilis Arctica’ ap-
peared in 1882. In this the Cretaceous flora of Kome and
Atane are reviewed with fresh materials. While unable to
find any companions for the solitary Populus of Kome, he adds
largely to the dicotyledonous flora of Atane. From 33 species.
in 1874 this flora now rises to 95. In the seventh volume
of the same work, which unfortunately must now be the last,
a new Cretaceous flora is announced, that of Patoot, also in
Greenland, which is regarded as extreme Upper Cretaceous.
Dicotyledons here abound; and no less than 74 species are
made known in Heer’s work.
Within the past few months an important paper has been
contributed to the Royal Society of Canada by Principal
Dawson *, in which 30 species, mostly new, from two distinct
horizons of the Cretaceous of British Columbia, are described
and figured.
Lastly, I am able to add to this enumeration one of the
most important works that has ever been produced on vege-
table paleontology, but which is still unpublished, though
now ready for the press. I refer to Mr. Lesquereux’s ‘ Cre-
taceous and Tertiary Floras,’ which is to form the eighth
volume of the series of quartos of the U.S. Geological Survey
of the Territories in charge of Dr. F. V. Hayden. In this
work the author again exhaustively reviews the entire subject
of the American Cretaceous flora, and we find the number of
Dicotyledons thus far yielded by the Dakota Group to have
reached 167. In his table of distribution he attempts to
embrace the flora of the entire Cenomanian Formation, to
which he doubtless rightly believes our Dakota Group to
belong. The total number of Dicotyledons thus marshalled
is 812. Large as these figures seem, there is much reason to
believe that they fall in both cases considerably below the
actual state of science at the present time, as will be seen by
the tabular statement given below.
If we now turn from this strictly chronological enumeration
to a consideration of the stratigraphical position in which
these plants have been found, as indicating their relative age,
we shall find the results no less interesting than is the history
of their discovery.
The various countries of the globe where geology is studied
* ‘Transactions, pp. 15-34, pls. 1.—viii.
Mr. L. F. Ward on Mesozoic Dicotyledons. 391
have adopted divisions for their geological formations corre-
sponding to the character of the rocks in each country. These
divisions cannot be made to harmonize with exactness when it
is sought to compare widely separated regions. The attempt
here made to correlate the subdivisions of the Huropean,
Arctic, and North-American Cretaceous can therefore at best
only lay claim to approximate accuracy.
The Quadersandstein of Germany, in which the greater
part of the Huropean fossil plants have been found, is an ex-
tensive formation, reaching in Saxony and Bohemia from the
Lower Cenomanian to the White Chalk, or Upper Senonian.
Its middle portion is occupied by the Pliner sandstone and
Pliner marls, which extend downward into the Upper Ceno-
manian and upward to the base of the Senonian. The some-
. what local character and indefinite boundaries of the Quader
formations have rendered it customary on the Continent, even
with German geologists, to adopt the system of D’Orbigny as
now modified, and to speak of the Cenomanian, Turonian, and
Senonian instead of Lower Quader, Pliner, and Upper Quader;
and it is also now common to apply these terms to formations
in other parts of the world which are supposed to occupy the
same stratigraphical positions.
The leading European localities from which Cretaceous
Dicotyledons have been collected are—Saxony (Niederschéna),
Moravia (Moletein), Bohemia (Trziblitz, Perutz), Silesia
(Oppeln, Tiefenfurth), the Harz district (Blankenburg, Qued-
linburg), Westphalia (Legden, Sendenhorst), and the vicinity
of Aix-la-Chapelle. The first four of these localities belong
to the Lower Quadersandstein, or Cenomanian, that of Nieder-
schéna lying near its base. The Cretaceous of the Harz
district is probably Lower Senonian. In Westphalia, Hosius
and Von der Marck find fossil Dicotyledons at two different
horizons, both of which, however, they place in the Senonian.
The region about Legden, Ahaus, Haltern, &c. is regarded
as Lower Senonian, while Sendenhorst, Haldem, &c. dre
said to be Upper Senonian. The iron-sand near Aix-la-
Chapelle is probably still higher, and occupies the extreme
Upper Senonian.
The next greatest source, outside of the United States, of
the class of fossils under consideration is Greenland. The
Kome beds, as already remarked, are distinctly fixed in the
Urgonian, which is Lower Cretaceous, and lies between the
Neocomian and the Gault. The discovery of a dicotyle-
donous plant at this horizon is one of the most interesting
facts of paleontological science. The beds of Atane, where
the greater part of the species were found, although called
392 Mr. L. F. Ward on Mesozoic Dicotyledons.
Upper Cretaceous by Heer, are admitted by him to exhibit in
their fossil remains so close a relationship with the American
Dakota Group as to render it probable that they are of the
same age. Patoot, on the other hand, is set down as extreme
Upper Cretaceous; and Heer says that its invertebrate fauna
indicates its identity with the Fox Hills of our Western Terri-
tories.
The localities in British Columbia from which Cretaceous
Dicotyledons have come are all regarded by the Canadian
geologists as Upper Cretaceous. The inland portions, situated
on the Pine and Peace rivers, are said by Dr. Dawson to cor-
respond to the Niobrara of the north-western United States,
which he also correlates with the Lower Senonian of Kurope.
Vancouver’s Island and the localities on the Pacific coast are
higher, and are placed in the Upper Senonian, though he .
does not correlate them with any of the groups of American
geologists. Fossil plants were found on the Bow and Belly
river, which is said to agree with the Pierre Group; but the
dicotyledonous remains appear to have been indistinct and
undeterminable.
With the exception of the Dakota Group, which is com-
monly regarded as Cenomanian, and in which such a profu-
sion of dicotyledonous vegetation is imbedded, no fossil plants
have thus far been described from the Cretaceous of the
Western Territories. Nevertheless, I have myself collected and
brought to Washington during the past season some dicotyle-
donous leaves from a locality on the Upper Missouri river
some seven miles below Coal Banks, whose position is fixed
with certainty in the Fort Pierre Group, No. 4 of Meek and
Hayden, which Dr. C. A. White regards as merely forming
the lower portion of the Fox Hills. The material thus ob-
tained, though meagre and fragmentary, is sufficient to render
it quite certain that we here have forms nearly allied to Pla-
tanus latiloba of Newberry (Sassafras mirabile, Lesqx.), and
perhaps connecting this with Platanus nobilis, Newb., from
the Laramie strata that overlie these beds, as well as forms
resembling Quercus salicifolia, Newb., and other Cretaceous
genera and species. here is therefore ground for hoping
that when this and other similar localities are thoroughly
studied a new Cretaceous flora may come to light in the
North-west.
J have in this paper intentionally omitted all consideration
of the great Laramie Group, although this is regarded by
many as Cretaceous. This 1s because it seems at least to be
more recent than any of the Huropean, Arctic, or British-
American plant-bearing beds, while its abundant flora con-
Mr. L. F. Ward on Mesozoic Dicotyledons. 393
sists in large part of types represented in the Miocene of
Europe.
It thus appears that throughout both hemispheres the con- .
ditions required for the preservation of vegetable remains in
Cretaceous time have existed in a marked degree during two
epochs only, the Cenomanian and the Senonian, separated
from each other by a period, perhaps equal to either, during
which marine forms of animal life are chiefly found. <A few
Dicotyledons only occur in the Turonian of Europe, as e. g.
Magnolia telonnensis from Toulon, while the Colorado Group
(Fort Benton, Niobrara) of our Western Territories has thus
far proved destitute of plant life.
If now we take up the several subdivisions of the Creta-
ceous formation in their stratigraphical order, beginning with
the lowest, we shall see that in the Neocomian, or lowest
member, no plant-remains of the subclass we have been
studying have as yet ever been detected *.
Inthe Urgonian, or next higher group, one species, Populus
primeva, Heer, has been collected at Pattorfik, in Greenland.
In volume vi. of his ‘ Flora Fossilis Arctica,’ which appeared
in 1882 (or eight years subsequent to the original description
of this plant), Heer continued to adhere to this species as well
as to its anomalous stratigraphical position.
The Gault, like the Neocomian, has thus far furnished no
Dicotyledons, though not always destitute of plant-remains f.
It is with the Cenomanian that there seems to have burst
in upon the world a great and luxuriant dicotyledonous
vegetation. Itis found alike in Saxony, Bohemia, Silesia,
in Greenland, and in the western United States. Upwards
of three hundred and fifty species, representing all three of
the divisions of the subclass (Apetale, Polypetale, Gamo-
petal), and consisting chiefly of living genera, have been
described.
It was formerly supposed that the beds at Blankenburg
occupied a much lower position than that to which I have
assigned them, and such as would place them in the Turonian
at least, if not in the Cenomanian; and Mr. Lesquereux, in
the large and important work which is about to appear f,
* The supposed Neocomian Dicotyledons of Russia (Eichwald, ‘ Lethea
Ressica,’ ii. pp. 58 e¢ seg.) are shown by Heer (Fl. Ross. Arct. iii. Theil 2,
S. 26) to come from the Lower Senonian corresponding to the Harz
district.
+ Heer assigns the plant-beds of Spitzbergen to the Gault (7. c. S. 24),
and Coemans finds nine new species of fossil plants in the Cretaceous of
Hainaut (Mém. de lAcad. Royale de Belgique, xxxvi., 1867), which
Briart and Cornet (J. c. xxxiii. p. 46) placed in the Gault.
{ “ Cretaceous and Tertiary Floras,” Report of the U.S. Geol. Survey
of the Territories, vol. viii. (Washington, 1883.
Ann. & Mag. N. Hist. Ser. 5. Vol. xiii. 26
394. Mr. L. F. Ward on Mesozoic Dicotyledons.
includes the species of Heer’s Quedlinburg flora in his table
of distribution of the Cenomanian. It is now quite certain,
however, that the Cretaceous of the Harz district is much
higher, and authorities seem to agree in placing it in the Lower
Senonian. On the other hand, the upper boundaries of the
Cenomanian in France and elsewhere are somewhat imper-
fectly established. For this and other reasons I have felt
justified in relegating the few species that have been classed as
Turonian to the Cenomanian, of which great group they seem
to be but straggling outliers.
In the Senonian, both in Europe and in British Columbia,
two quite distinct horizons for fossil plants seem to occur,
separated from each other by a considerable interval. In
view of this I have attempted to divide this group into two
horizons, and am thus able to show the Lower and Upper
Senonian separately. From the Lower Senonian we have
about eighty species and from the Upper about one hundred
and eighty.
The following Table exhibits the number of dicotyledo-
nous species thus far recognized in each of the groups of the
Cretaceous for the four principal geographical areas within
which they have been collected :—
Cretaceous Dicotyledons.
SS
F -: 5 E
Geological Position. A FI < 2)
ay | a 3 ;
z 3 = = 3
5 = cee Ss
ss & ea 5 a
Upper Senonian .... 81 74. 24 179
Lower Senonian .... 67 14 81
AORN Gono boo aos 5 pd Ee ie
Cenomanian ati 53 114 ae
Dakota Group : & 184 =
(alice ee ero eres fe in or a ae
Wivanran® 6. 645.4 65 eh 1 Ag i: 1
INeocomisn, ....)..6.6. bb 6
Mota 201 189 38 184 612
As all the plants with which we are here concerned are
found in the Cretaceous, some may be surprised that this
paper should have been entitled Jesozoic rather than Creta-
Mr. L. F. Ward on Mesozoic Dicotyledons. 395
ceous Dicotyledons. ‘The reason for the title chosen is simply
that it may tend somewhat to enlarge the view of the true
history and age of this great type of vegetation. When we
see that more than three hundred and fifty species of fully
developed Dicotyledons, implying the existence of many more,
were flourishing in all their present luxuriance in the Middle
Cretaceous, and that even in the Lower Cretaceous one species
is known to have existed belonging to a genus that still sur-
vives, we cannot, if we would, repress the thought that the
ancestors of these forms must have come down through older
periods of the Mesozoic.
That we shall ever discover the true progenitors of the
known Dicotyledons it is, of course, impossible to say ; but
that they had progenitors science no more hesitates to assume
than any one would hesitate to assume that a foundling child
must have had parents. Moreover, such is the slow and
secular character of the development of living forms on the
globe, that no one would suppose it possible for so prominent
a group of plants as were the Dicotyledons in the Cenomanian
age to have attained that condition in any thing short of a
vast geologic period.
It is to be hoped that we are at last approaching the be-
ginning at least of a solution of this truly great problem of
the origin of the Dicctyledons. I have myself seen at least
one slight, it may be, but very interesting sign of possible
progress in this direction. Certain very defective, but very
instructive, specimens collected in the Upper Jurassic of Vir-
ginia by Professor Wm. M. Fontaine, and which he kindly
brought to Washington for my inspection, certainly possess
all the essential elements of dicotyledonous leaves, although
at the same time bearing a certain recognizable stamp of the
cryptogamic and gymnospermous vegetation that characterizes
that earlier age. What is to be the final verdict of science
upon these forms cannot now be told; but it is to be hoped
that the Mesozoic strata, not only in Virginia, but in all parts
of the world, may be diligently searched and the materials
carefully studied, with a view to discovering these certainly
merely ‘missing links” of a chain that can but have been
once complete.
It is iemarkable that in both its flora and its fauna the life
of this continent has been thus abruptly truncated. The
sudden irruption of a perfectly developed mammalian fauna
at the beginning of the Tertiary is not less astonishing than
the appearance unannounced of many hundreds of species
of highly organized dicotyledonous plants in the Middle
Cretaceous. ‘I'he advocates of special creation, and likewise
26*
396 Mr. G. A. Boulenger on new
the hunters after a lost Atlantis, were they informed upon
the facts which science itself so plainly teaches, could ask no
stronger argument for either of their positions. But such
persons are usually not so informed, and it seems almost im-
possible for them to become so and still hold such views, for,
fortunately, knowledge is a poison that contains its own
antidote, and the very possession of the facts suffices to pre-
clude a perverse use of them.
XLV.— Descriptions of new Species of Reptilesand Batrachians
in the British Museum.—Part Il. By G. A. BouLENGER.
Blanus Bedriage, sp. un.
In a recent paper *, Dr. J. v. Bedriaga has established the
specific distinctness of two forms of Amphisbeenas which have
hitherto been confounded under the name of Blanus cinereus,
Vandelli, viz. a Western form, inhabiting the Spanish penin-
sula, Morocco, and Algiers, for which the name Bb. cinereus
must be retained, and an Eastern form, occurring in Asia
Minor, which he named Amphisbena Strauchi. My attention
being drawn to this question, I have reviewed the series of
Blanus in the British Museum; and the result has not only
confirmed Dr. v. Bedriaga’s conclusions, but brought to light
a third form, represented by several specimens from the river
Xanthus, Asia Minor, and which must likewise be regarded
as a species, which I will name B. Bedriage ; its characters
are as follows :—
Intermaxillary teeth seven, maxillaries three on each side,
mandibulars seven on each side. Snout prominent. Three
lower labials, the first and second large, the third small; the
suture between the frontal and the second labial nearly as
long as that between the latter and the ocular. No cervical
fold separating the head from the body. Annuli 101 to 114
on the body, 19 to 21 on the tail; an annulus contains 16 to
18 dorsal and 18 to 20 ventral segments. Preanal pores ten.
The other Oriental specimens of Blanus in the collection,
and which bear the localities Constantinople and valley of
the Meinder, agree in every respect with B. Straucht, of which
a specimen from Smyrna has been obtained from Dr. v. Be-
driaga.
Stenostoma affine, sp. n.
Allied to S. albifrons, but distinguished by the much larger
* Arch. f. Naturg. 1884, p. 23, pl. iv.
Reptiles and Batrachians. 397
anterior labial shield, which is broader than either the naso-
labial or the oculo-labial. Supraocular separated from the
anterior labial. 7 longitudinal and 215 transverse series of
scales. Brown above, brownish white beneath ; the centre of
the scales darker, but not forming such conspicuous markings
asin S. albifrons. Total length 205 millim. ; tail 16 millim. ;
diameter of body 4 millim.
One specimen from the province of Tachira, Venezuela.
Rana Masonii, sp. n.
Vomerine teeth in two slightly oblique series between the
choane. Head moderate; snout rounded, slightly longer than
the diameter of the orbit, with strong canthus rostralis ; loreal
region deeply concave ; interorbital space a little broader than
the upper eyelid; tympanum very distinct, half the size of
the eye. Fingers rather slender, first extending slightly
beyond second; toes moderate, nearly entirely webbed, tips
of fingers and toes dilated into small disks; subarticular
tubercles strong ; inner metatarsal tubercle small, oval; no
outer metatarsal tubercle. Hind limb very long; if carried
forward, the femoro-tibial articulation reaches the axilla, and the
tibio-tarsal articulation far beyond the tip of the snout. Skin
smooth ; a well-marked glandular lateral fold. Brown above ;
a blackish streak under the canthus rostralis and a large
blackish temporal spot; tympanum light, dark in the centre ;
limbs with dark cross bars. Lower surfaces whitish, brown-
mottled on the throat and breast. From snout to vent 68
millim.
Near Rana jerboa, Gthr., but well distinguished by the
shorter hind limb.
A single female specimen, from near Batavia, was presented
by G. EH. Mason, Esq.
Microhyla fissipes, sp. n.
Habit slender. Snout truncate, slightly longer than the
orbital diameter ; interorbital space broader than the upper
eyelid. Fingers slender, first much shorter than second ; toes
long and slender, free, with a slight lateral fringe; tips of
fingers and toes not swollen; subarticular tubercles distinct ;
two rather small, obtuse, metatarsal tubercles. The hind
limb being carried forward along the body, the tibio-tarsal
articulation reaches the eye. Skin nearly smooth above, with
small warts on the sides. Olive-brown above, the small warts
tinged with red; a darker lateral band from the tip of the
snout, passing through the eye down to the middle of the side ;
an elongate X-shaped darker marking commencing between the
398 Mr. F. E. Beddard on the
eyes, and another, A-shaped, on sacral region; limbs with
dark cross bars. From snout to vent 26 millim.
One specimen from Taiwanfoo, S. Formosa.
Cecilia Buckley?, sp. n.
Maxillary teeth rather large, about 10 on each side; vomero-
palatines 8 on each side ; inner mandibulars small, few ; outer
mandibulars large, especially the most anterior, 9 on each’side.
Snout broad, rounded, not very prominent, shorter than the
distance between the eyes; latter very distinct; tentacle below
the nostril. Body short for the genus, cylindrical; 175
circular folds, all complete. ‘Tail indistinct, rounded. Olive
above, lighter beneath and round the lower jaw ; throat olive.
Total length 160 millim.; diameter of body 4 millim.
A single specimen, probably young, collected at Intac,
Keuador, by Mr. Buckley.
XLVI.—On the Genus Megascolex of Templeton.
By F. E. Bepparp, M.A., F.R.S.E.
In a recent paper by Dr. Horst* of Leyden, the author, in
describing a collection of earthworms belonging to the genus
Pericheta of Schmarda, takes occasion to point out the iden-
tity of this genus with another genus established fifteen years —
previously by T'empleton, viz. Megascoler. Having recently
had an opportunity, through the kindness of Dr. Traquair and
Prof. F. Jeffrey Bell, of examining several specimens preserved
in the British Museum and the Edinburgh Museum of Science
and Art, which are undoubtedly Templeton’s Megascolex ceru-
leus, I think it worth while to point out that these two genera,
Megascolex and Pericheta, are by no meansidentical, but present
numerous and important differences. In the paper already
mentioned Dr. Horst recapitulates the main points in Tem-
pleton’s original description of Megascolea ceruleus, and calls
attention to the misinterpretations of this description intro-
duced by subsequent writers; there is no doubt that these
misinterpretations, for which Schmarda is mainly responsible,
in reality caused Perrierf and Vaillant} to separate the genera
Megascolex and Pericheta in their tables of classification, since
there is nothing in Templeton’s description itself which would
* Notes from the Leyden Museum, vol. v. no. xvii.
t+ Nouv. Arch. du Mus. t. viii. (1872).
¢ Ann. Sci. Nat. sér. 5, x. (1868).
Genus Megascolex of Templeton. 399
serve to clearly differentiate the two. Templeton’s original
notice of Megascolex ceruleus is contained in a letter read
before the Zoological Society of London in 1845* ; but the
facts given chiefly relate to certain external characters and
are not at all sufficient to determine the systematic position of
the earthworm. The sete are stated to be arranged in a con-
tinuous ring round each segment, except in the mesial line
of the back, where they are altogether wanting, while the
generative organs occupy segments 16, 17, 18. The latter part
of the description is too vague to be of any use, since it is not
clear what is meant by “ generative organs,” whether the
testes and ovaries, their external apertures, or, finally, the seg-
ments upon which the clitellum is developed. Schmardat
distinguished his genus Pericheta mainly by the arrangement
of its sete; his generic definition is as follows :—“‘ Sete
totam segmentorum circumferentiam in forma annuli cin-
gentes.”” He mentions Templeton’s genus MJegascolex as
having the setee developed only upon the back, and, in fact,
entirely reverses the account of the arrangement of the sete
given by Templeton; the “ generative organs” of ‘Temple-
ton’s description Schmarda interprets as the clitellum. In
1869} Baird examined the type specimens of Megascolex ceru-
eus in the British Museum, and came to the conclusion that
there was no difference of importance (indeed no difference
at all, except size) between that genus and Pericheta, The
only structures, however, which he seems to have compared
with any care in the two forms are the sete; and these are
precisely the very worst characters that could have been chosen
to determine such a question. Itis impossible to arrive at pny
corrée. notion about the systematic position of an earth’. orm
without an examination of its internal structure and the rela-
tions of the male generative apertures to the clitellum. Vail-
lant §, and afterwards Perrier||, more fully demonstrated the
importance of the latter character; and Perrier has suffi-
ciently shown how earthworms, similar in external characters,
may differ most widely in their anatomy; moreover Baird’s
figures of the sete ot Megascolex caruleus and Pericheta
diffringens do show some slight differences, quite enough to
distinguish them if it were at all possible to make use of such
a trifling external character. Baird makes no statements at
all about the clitellum and generative pores in Megascolex.
* P.Z.S. 1845, p. 89.
+ Neue wirbellose Thiere (Leipsic, 1861), Bd, i. 2.
t P.Z.S. 1869, p. 40.
§ Ann. Sci. Nat. loc. cit.
|| Nouv. Arch. &e. doe. cit.
400 Mr. F. E. Beddard on the
Dr. Horst, in the paper already quoted, entirely agrees with
Baird’s identification of Megascolex with Pericheta, and
naturally points out that the latter name must be cancelled,
since Megascolex has a priority of fifteen years. Although the
last-named author does not state his own reasons for this
identification, but relies chiefly upon Baird’s authority, any one
reading ‘empleton’s description would naturally think that
the earthworm presented no points of generic difference from
Pericheta; the distribution of the sete is not sufficiently
peculiar to mark off the genus Megascolex from Pericheta,
inasmuch as we know that a continuous ring of sete is not
always found in species which would unhesitatingly be as-
signed to the genus Perichwta. ‘The only other point in
Templeton’s description, the account of the generative organs,
might well be referred to the apertures of the male generative
ducts upon the 18th segment and to genital papille, such as
are frequently found in Pertcheta.
None of the specimens in the British Museum nor the single
specimen in the Edinburgh Museum had the clitellam fully
developed, though in one specimen segments 13-19 showed a
slightly different colour from the rest of the body, which is
doubtless a trace of a clitellum in a condition of development
or degeneration. The specimen in the Edinburgh Museum,
which presents an interesting peculiarity to be described
shortly, Dr. Traquair kindly allowed me to open, and I at once
ascertained that it was identical with an earthworm recently
described by myself* as new, under the name of Pleurocheta ;
I was able to verify my description and to add some details
as well as to make one or two corrections. ‘The specimen in
the Oxford Museum had a fully developed clitellum, extending
from the 13th to about the 20th segment, and therefore beyond
the apertures of the male generative duct, which are in seg-
ment 18. ‘This fact alone is amply sufficient to show that
there can be no possibility of confounding this earthworm
with Pericheta, seeing that in this latter genus, as is well
known, the clitellum occupies certain segments anterior to the
openings of the male generative ducts, which only agree with
those of JMegascolex (as also of other genera, e. g. Ponto-
drilus) in being situated upon the 18th segment and in being
provided with a prostate gland. The absence of a fully deve-
loped clitellum in the specimens of Megascolex contained in
the national collection renders it, of course, more difficult to
distinguish this genus from Pericheta, though a careful ex-
amination even of these specimens, and with regard to exter-
nal characters only, reveals at once certain points of difference.
* Trans. Roy. Soc. Edinb. vol. xxx. pt. ii.
la i i
Genus Megascolex of Templeton. 401
In all the specimens, with one exception, the ventral surfaces
of the 17th, 18th, and 19th segments are traversed by two
thick glandular folds (the remnant of the clitellum), differing
by a yellowish colour from the surrounding integument,
and separated from each other by a space of about 7 inch:
in the groove on the inner side of each of these folds are
situated the male generative apertures and two papille; the
former lie in the middle of the 18th segment, just in
front of the row of sete which traverses it, whilst the latter
are upon the boundary-line between segments 17-18 and
18-19 respectively ; the rows of setes upon segments 17, 18,
and 19 stop short at the outer edge of the glandular fold.
Although it is well known that many species of Pericheta
possess genital papille in the neighbourhood of the male
genital apertures, an inspection of Perrier’s figures of these
structures at once shows that they are not quite the same
as those of Megascolex ; instead of being upon the boundary-
line between two segments, they are quite in the middle
of a segment in the region occupied by the row of sete. In
one of the five specimens of Megascolex that are in the na-
tional collection the male genital apertures and the papille,
instead of being hidden away at the bottom of a deepish groove,
are situated upon the upper surface of an oval longitudinal
swelling which extends over exactly the same number of
segments as the longitudinal fold. Upon the 13th segment
are two apertures, which are most probably the external open-
ings of the oviducts; like the male generative apertures they
are placed just in front of the row of sete. The specimen
in the Edinburgh Museum, which in other respects showed a
perfect agreement with the five of Megascolex in the British
Museum, has only a single oviducal aperture situated upon
the middle of the ventral surface of the same segment and
surrounded by a circular area differing somewhat in colour
and appearance from the rest of the integument.
With regard to the internal structure of Megascolex I have
nothing to add to my former description, where the numerous
differences between Megascolex aud Pericheta are indicated.
I append a definition of the two genera.
Pericu&TA, Schmarda.
Pericheta, Schmarda, Neue wirbellose Thiere, 1861, Bd. i. 2.
Megascolea, Baird, P. Z.S. 1869, p. 40.
Pericheta, E. Perrier, Nouv. Arch. du Mus. 1872.
Megascolex, Horst, Notes Leyden Museum, vol. y., note xvii. p. 182,
Sete generally arranged in a continuous row round the
middle of each segment; clitellum occupying 2, 3, or 4 seg-
402 Mr. W. I. Kirby on the
ments (14-17). Male generative apertures paired, and situ-
ated upon 18th segment of body, which is always behind the
clitellum ; genital papillee occasionally developed in neigh-
bouring segments. Female generative aperture single, and
within the clitellum upon the 14th segment. ‘Iwo pairs of
testes, more or less solid and compact, in segments 11 and 12;
terminal portion of vas deferens on either side connected with
the duct of a large prostate gland. Copulatory pouches
varying in number from two to four pairs, and provided each
with a variously shaped supplementary pouch or pouches.
Intestine with a cecum on either side in 20th segment*.
Mecascotex, Templeton.
Megascolex, Templeton, P. Z.S. 1845, p. 89.
Pleurocheta, ¥, 4. B., Trans. Roy. Soc. Edinb, vol, xxx. pt. ii.
Setee arranged in nearly a continuous row round each seg-
ment, only failing for a short space in the dorsal and ventral
median lines; clitellum occupying segments 138-20, but not
developed upon the area which separates the male genital aper-
tures and papille of one side from those of the other. Male
genital apertures paired and situated upon 18thsegment of body,
which is within the area over which the clitellum extends ;
genital papille two pairs, developed upon boundary-line
between 17th-18th and 18th-19th segments respectively.
Female generative pore single or double, upon 14th segment.
A single pair of testes, branched and racemose, in 12th seg-
ment; a large prostate gland on either side in 18th segment.
Copulatory pouches simple and unprovided with any supple-
mentary pouches; two pairs situated in segments 8 and 9.
Intestine with no cecum, but with a series of large compact
glands arranged in fifteen or sixteen pairs, commencing at
about segment 106.
XLVII.—On the Hymenoptera collected during the recent
Expedition of H.M.S. ‘Challenger. By W. F. Kirsy,
Assistant in Zoological Department, British Museum. -
THE series of Hymenoptera collected during the voyage of
H.M.S. ‘Challenger’ is interesting not only on account of
several apparently new species having been obtained, but because
* Intwo species, P. Sieboldi and P. musicus, Horst (‘ Notes Leyden
Museum,’ &c. pp. 192 & 194) describes six of these czeca on each side;
but in the latter species, at least, they do not seem to be at all regular
in their presence.
‘Challenger’ Hymenoptera. 403
most of the specimens were obtained from localities which have
been but little worked; and consequently the greater part
were brought from countries which they were not previously
known to inhabit. A list is given below.
HYMENOPTERA TEREBRANTIA.
SERRIFERA.
Tenthredinide.
Preryq@oPHORINz.
1. Pterygophorus analis.
Pterygophorus analis, Costa, Aun. Mus. Nap. ii. p. 66 (1864).
Sydney, May 1874.
ENTOMOPHAGA.
SPICULIFERA.
Chalcidide.
EHucHarine.
2. Schizaspidia Murray?.
Long. corp. 14 lin.
Male.—Closely allied to S. naswa, Walk., from the Philip-
pines. Head and thorax green, granulated, with a slight
coppery reflection ; antenne yellowish brown; scape yellow
beneath ; flagellum with seven long rami before the extremity,
which divides into two equal rami, shorter than the others;
scutellum sloping upwards, more shortly constricted than in
S. nasua, and terminating in a blunt fork, about as long as
the first portion ; abdomen subpetiolated, vertical, smooth and
shining, blackish green on the sides, and with a broad yellowish
stripe above, continued round backwards to the extremity ;
legs yellowish. Wings hyaline; subcostal nervure rather tick.
blackish ; stigma short, blackish, well defined. ;
- Tongatabu, July 1874.
Evaniide.
3. Hvania levigata.
Evania levigata, Latr, Gen. Crust. et Ins. iii. p. 251 (1807).
Honolulu.
404 Mr. W. F. Kirby on the
Braconide.
4. Bracon trisignatus.
Female.—Exp. al. 103 lin.
Head, thorax, legs, first and base of second segment of
abdomen pale luteous ; abdomen whitish beneath ; antenna,
vertex as far as the antenne, three spots on thorax, the
greater part of the abdomen above, hind tibiz except at base,
and hind tarsi black; ovipositor red, sheaths black ; wings
yellow nearly to the middle, and smoky black beyond; stigma
not coloured.
Zamboanga, Philippines, Oct. 18, 1874.
5. Bracon stigmaticus.
Female.—Exp. al. 12 lin.
Luteous; head pale yellow; antenne black, the scape
luteous beneath; wings yellowish hyaline for two fifths of
their length, the remaining three fifths beg smoky brown ;
stigma ivory-white; abdomen with the first three segments
luteous above, but paler than the thorax, the remainder of the
abdomen black above, the last two segments narrowly edged
behind with white ; abdomen white beneath, except the valves
of the ovipositor, which are black; ovipositor red, sheaths
black ; legs red, hind tarsi black.
Ki Dulan, Sept. 25, 1874.
HYMENOPTERA ACULEATA.
PRAD ONES.
HETEROGYNA.
Formicide.
FORMICINA.
6. Lormica nigra.
Formica nigra, Linn. Syst. Nat. ed. x. vol. i, p. 580 (1758).
Bermuda, April 1873. ;
Perhaps introduced. The specimens do not appear to differ
from the ordinary European species.
7. Camponotus maculatus.
Formica maculata, Fabr. Spec. Ins. i. p. 491 (1781).
San Jago, Cape Verdes, Aug. 11, 1873; Cape of Good
Hope, Nov. 1873.
‘Challenger’ Hymenoptera. 405
A common species throughout tropical and subtropical
Africa.
8. Camponotus intrepidus.
Formica intrepida, Kirby, Trans. Linn. Soc. Lond. xii. p. 477 (1818).
Sydney, May 1874.
9. Polyrhachis bihamata.
Formica bihamata, Drury, Tl. Ex, Ent. ii. pl. xxxviii. figs. 7,8 (1773).
Zamboanga, Philippines, Feb. 1875.
10. Polyrhachis sculpturata.
Polyrhachis sculpturatus, Smith, Journ. Linn. Soc. Lond., Zool. v. p. 70
(1861).
Zamboanga, Philippines, Feb. 1875.
Previously recorded from Celebes, Salawatty, Timor, and
Siam, but not from the Philippines.
11. Polyrhachis phyllophila.
Polyrhachis phyllophilus, Smith, Journ. Linn. Soc. Lond., Zool. v. p. 69
(1861).
Zamboanga, Philippines, Feb. 1875.
Previously recorded from Sumatra and Celebes.
12. Polyrhachis latifrons.
Polyrhachis latifrons, Roger, Berl. ent. Zeitschr. vii. p. 155 (1863).
Amboina, Oct. 1874; Cape York, Torres Straits.
Originally described from Java.
13. Polyrhachis neptunus.
Polyrhachis neptunus, Smith, Journ. Linn, Soc. Lond., Zool. viii. p. 69,
pl. iv. fig. 2 (1865).
Amboina, Oct. 1874.
This species was originally described from New Guinea.
In many of the specimens the antenne and legs are more
ferruginous than in the typical form.
ODONTOMACHINE.
14. Odontomachus hematodes.
Formica hematoda, Linn, Syst. Nat. ed. x. vol. i, p. 582. n. 16 (1758).
Ki Dulan, Sept. 25, 1874.
406 Mr. W. F. Kirby on the
PoneERINae..
15. Lobopelta diminuta.
Ponera diminuta, Smith, Cat. Hym. Ins. B. M. vi. p. 89 (1858).
Zamboanga, Philippines, Feb. 1875.
Widely distributed in the Eastern Archipelago, but not
previously recorded from the Philippines.
16. Paraponera clavata.
Formica clavata, Fabr. Syst. Ent. p. 394 (1775).
Bahia, Sept. 1873.
17. Typhlopone punctata.
Typhlopone punctata, Smith, Cat. Hym. Ins. B, M. vi. p. 112 (1858).
Cape of Good Hope.
Mvyrurcinz.
18. Aphenogaster hostilis.
Atta hostilis, Smith, Cat. Hym. Ins. B. M. vi. p. 165 (1858).
Simon’s Bay, Cape of Good Hope, Dec. 1873.
Smith describes the female and the worker minor. The
pair in the ‘ Challenger’ collection agree with a series from
Natal, which I take to belong to the worker major. ‘They
are much darker than the small specimens; but the workers
of this genus differ very much in colour.
19. Atta abdominalis.
Gcodoma abdominalis, Smith, Cat. Hym. Ins. B. M. vi. p. 184 (1858).
Bahia, Sept. 1873.
FOSsSORES.
Mutillide.
20. Mutilla diadema.
Mutiilla diadema, Fabr. Mant. Ins. i. p. 811 (1787).
Bahia, Oct. 1873.
Scoliide.
21. Dielis Wallacet.
Male.—Exp. al. 12 lin.
Black ; abdomen with a steel-blue lustre, the greater part
‘ Challenger’ Hymenoptera. 407
of the body more or less clothed with short grey hair, which is
especially dense upon the metathorax ; clypeus narrowly bor-
dered below with yellow, and the mouth-parts, above the closed
mandibles, of the same colour ; mandibles black, the extreme
tips red; abdomen with the first two dorsal segments bor-
dered with yellow behind, the border on the second interrupted
in the middle; the third segment is marked with a faint spot
of the same colour on each side, on its hinder edge; wings
violaceous hyaline, with chestnut-brown nervures; tegule
chestnut-brown.
Ki Dulan, Sept. 2, 1874.
Allied to D. agilis, Smith, from Celebes, but quite distinct.
22. Dielis extranea.
Exp. al. 11 lin.
Male——Black ; clypeus incised, yellow below; labrum
yellow, with a black spot in the angle formed by the clypeus ;
thorax clothed with greyish pubescence ; prothorax and tegule
yellow, a black stripe, narrowly edged below with yellow,
running towards the tegule, and bounding the yellow colour
on each side; scutellum and postscutellum and the sides of
the metathorax behind yellow; the lateral sutures of the
mesothorax may also be yellow, but this is much obscured
by the villous covering; abdomen with the first three seg-
ments broadly bordered with yellow behind, and most broadly
at the sides; on the under surface the second and third seg-
ments are bordered with yellow behind, this colour being
interrupted in the middle; wings yellowish hyaline, with
chestnut nervures; front legs yellow, front femora black
above ; middle legs yellow above, the femora with a black
basal stripe above and beneath; the tibie and tarsi and a
small spot at the tip of the femora black beneath; hind legs
black ; the femora and a short line on the outside of the tibize
ellow.
Wild Island (Admiralty Islands). ;
Allied to D. aurulenta, Smith, a Philippine species.
Bembicide.
23. Monedula signata.
Vespa signata, Linn, Syst. Nat. ed. x. vol. i, p. 574 (1758),
Bahia, Sept. 1873.
408 Mr. W. F. Kirby on the
Larride.
24. Tachytes pompiliformis (?).
Larra pompiliformis, Panz, Faun. Germ. Heft 89, pl. xiii. (1805).
St. Vincent, Cape Verdes, July 1873.
25. Sphex maura.
Sphex maura, Smith, Cat. Hym. Ins. B, M. iv. p. 255 (1856).
Zamboanga, Philippines, Feb. 1875.
Originally described from Celebes.
26. Sphew sericea.
Pepsis sericea, Faby. Syst. Piez. p. 211 (1804).
Amboina, Oct. 1874.
27. Pelopeus chalybeus.
Pelopeus chalybeus, Smith, Cat. Hym. Ins. B. M. iv. p. 229 (1856).
Cape of Good Hope, Nov. 1873.
Pompilide.
28. Priocnemis atlanticus.
Long. corp. 6 lin.
Male.—Black, orbits (exceptonthe vertex) and mouth-parts
red; antenne straw-coloured, scape of a redder shade; lateral
angles of the prothorax prominent, and, as well asthe tegule,
red, shining ; abdomen with a coppery-green lustre ; legs (espe-
cially the front ones) more or less shading into ferruginous ;
wings with a strong greenish-purple iridescence.
The female differs from the male in having the greater part
of the head red; the green lustre of the abdomen is much less
distinct, and the wings are of a violet-purple rather than
of a greenish lustre.
St. Vincent, Cape Verdes, 1875.
Allied to P. exasperatus, Smith, from Natal, but differs
in the colour of the head.
29. Pepsis collaris.
Female.—Long. corp. 11 lin. Black, with dull bluish-green
tints. Face greenish ; antenne: scape black ; 2nd, 3rd, and
apical joints black above and grey below, the intermediate
joints yellow. Prothorax black, the sides varied with green
and bordered behind with grey pubescence, indistinct above,
: Challenger ” Hymenoptera. 409
but very conspicuous below the black tegulz, and on the sides.
Mesothorax velvety black or silky green, according to the light.
Metathorax inky black, with a double longitudinal carina,
and transversely striated; abdomen black, tinted with verdigris-
blue on the upper side; legs black, violet-blue above; wings
violaceous, an indistinct transverse yellowish crescent near
the end of the radial cell; face, thorax, and tip of abdomen
clothed with rather long divergent hairs.
Bahia, Sept. 1873.
Allied to P. mutabilis, St.-Farg.
30. Pepsis cerulea.
Sphex cerulea, Linn. Syst, Nat. ed, x. vol. i. p. 571 (1758).
St. Thomas, March 1873; Bahia, Sept. 1873.
31. Pepsis stellata.
Sphex stellata, Faby. Ent. Syst. ii. p. 217 (1798).
St. Thomas, March 1873.
32. Pepsis xanthocera.
Pepsis xanthocera, Dahlb. Hym. Eur. i. p. 120 (1845).
San Jago, Cape Verdes, Aug. 10, 1873.
DIPLOPTERA.
Eumenide.
33. Humenes colona.
Eumenes colona, Sauss. Guépes Solit. p. 70 (1852).
St. Thomas, March 1873.
34. Odynerus atlanticus.
Long. corp. 4 lin.
Female.—Black, closely punctured ; clypeus convex, biden-
tate at the apex ; sides and lower surface of clypeus, a dot
between the antenne, their lower surface, especially the
scape beneath and towards the tip, prothorax above, and
the sides in front, tegule, and legs red; mesothorax with
a shallow and inconspicuous channel above, on each side;
abdomen: first segment red, with a black spot in front ;
second segment black above, with the sides, hinder edge,
and under surface red ; wings smoky hyaline, with blackish
nervures.
St. Vincent, Cape Verdes, July 1873.
Differs from most other black species with red markings
by the black scutellum.
Ann. & Mag. N. Hist. Ser, 5. Vol, xiii. 27
410 Mr. W. F. Kirby on the
Vespide.
35. Belenogaster bidentatus.
Exp. al. 12 lin.
Female.—Black, mouth-parts pale testaceous ; clypeus with
the sides emarginate beneath; mandibles reddish, avery narrow
reddish line behind the upper part of the eyes ; antenne ending
in a sharp point; this, the two preceding joints, and the base
beneath are testaceous; thorax thickly punctured; the pro-
thorax, a large lateral spot below and rather in front of the
black tegule, two large spots on the scutellum, contiguous,
but not united, the hinder part of the postscutellum, and the
sides of the metathorax above (the middle is black and
channelled) red; legs red, coxee black; abdomen black and
shining, the petiole rather wide at its extremity, where
it is slightly marked with reddish beneath and on the
lateral angles; on the under surface the median line of
the petiole is first carinated and then channelled rather beyond
the middle ; on the under surface is a small projecting tooth
on each side.
Pandana, Fiji, Aug. 1874.
36. Polistes perplexus.
Polistes perplexus, Cress. Trans. Amer. Ent. Soc. iv. p. 245 (1872).
Bermuda, April and June 1873.
Originally described from Texas.
37. Polistes aurdfer.
Polistes aurifer, Sauss. Mon. Guépes Soe. p. 78 (1858).
Honolulu, Aug. 1875.
38. Polistes rubiginosus.
Polistes rubiginosus, St.-Farg. Hym. i. p. 524 (1836),
San Jago, Cape Verdes, Aug. 10, 1873.
39. Polistes fortunatus.
Long. corp. 73 lines.
Female.—Ferruginous-tawny, with more or less extended
black markings, and clothed with a slight golden pile. Ver-
tex black, the colour sometimes extending as far ag the
antenne, and sending off a branch behind to the occiput; in
any case the furrows below the antenne are always more or
less marked with black. Clypeus subconvex, sparingly pune-
—_—o--:- °° °° °°» —
‘Challenger ’ Hymenoptera. 411
tured, and more or less yellowish beneath. Antenne, except
the base of the scape, blackish above. Prothorax ferruginous-
tawny, narrowly edged behind with yellow ; mesothorax black,
with or without a U-shaped pale mark in the middle, often
accompanied by a small one on each side; pectus mostly
black, except some pale spots on the pleura; scutellum and
postscutellum ferruginous-tawny ; metathorax either of the
same colour or black, but always with a wide black groove in
the centre. When the mesothorax is black there is always a
reddish stripe on each side of the groove, beyond which is
sometimes another red mark. Abdomen and legs yellowish
tawny, the first segment of the abdomen and often some of
the succeeding segments narrowly edged behind with yellow;
the first segment sometimes marked with black at the base,
the second nearly always with a triangular black spot at the
base, and occasionally the succeeding segments are also marked
with black at the base. The black markings are always more
extended on the under surface than on the upper. Wings
subhyaline, iridescent.
Described from eight specimens taken at San Jago, Cape
Verdes, on the 10th August, 1873. Not closely allied to any
known species.
40. Polistes Madoct.
Long. corp. 6 lin.
Female.—Black ; face ferruginous. Clypeus hairy. An-
tenn ferruginous, black above in the middle of the flagellum,
the apical portion more yellow; cheeks yellow, with an
indistinct dusky spot on the lower part. Prothorax yellow
above, with a large black streak running upwards on
the sides; mesothorax black, unmarked; tegule, scutellum,
postscutellum, two stripes on the back of the metathorax,
and two narrower ones on the sides, back of the metathorax,
knees, tibie, and tarsi yellow; coxe, femora, and hind
tibies black; abdomen black, the first four segments bor-
dered with yellow behind, both above and below, except
on the first segment, on which it is hardly continued below,
but it is continued forwards on the sides of all four segments ;
hinder segments yellow, tinted with ferruginous. Wings
yellowish hyaline.
St. Thomas, March 1873.
Apparently allied to P. modestus, Smith, and navajod,
Cresson.
41. Polistes carnifex.
Vespa carnifex, Fabr. Syst. Ent. p. 865 (1775).
Honolulu, May 1875.
412 On the ‘Challenger’ Hymenoptera.
42. Polistes elegans.
Polistes elegans, Smith, Journ. Linn. Soc. Lond., Zool. iv. p. 169 (1860).
Ki Dulan, Sept. 25, 1875.
43. Polistes diabolicus.
Polistes diabolicus, Sauss. Mon. Guépes Soe. p. 68, pl. vi. fig. 7 (1858).
Ki Dulan, Sept. 25, 1875.
’ 44. Polybia occidentalis.
Vespa occidentalis, Oliv. Enc. Méth. vi. p. 675 (1791).
Small nest and numerous specimens from Bahia. The
species does not appear to vary.
ANTHOPHILA.
Apide.
DenvparZ.
45. Crocisa scutellaris.
Nomada scutellaris, Faby. Spec. Ins. 1. p. 487 (1781).
St. Vincent, Cape Verdes, July 1873.
46. Crocisa nitidula.
Melecta nitidula, Fabry. Syst. Piez. p. 386 (1804).
Ki Dulan, Sept. 25, 1874.
ScoPuLIPEDES.
47, Xylocopa circumvolans.
Xylocopa cireumvolans, Smith, Trans, Ent. Soc. Lond. 1873, p. 205.
Eucosca Dock, Japan, May 1875.
48. Xylocopa eneipennis.
Apis eneipennis, De Geer, Mem. iii. p. 573, pl. xxviii. fig. 8 (1773).
St. Thomas, March 1873 ; Honolulu, Aug. 1875.
49. Xylocopa bryorum.
Ams bryorum, Fabr. Syst. Ent. p. 381 (1775).
Wokan, Dobbo, Aru.
Bibliographical Notices. 413
S OCIALES.
50. Trigona ruficrus.
Apis ruficrus, Latr. Ann. Mus. Hist. Nat. v. p. 176 (1804).
Bahia, Sept. 1873.
Sl. Apis mellifica.
Apis mellifica, Linn. Syst. Nat. ed. x. vol. i. p. 576 (1758).
Bermuda, April 1873; Sydney, May 1874.
BIBLIOGRAPHICAL NOTICES.
Annual Report and Proceedings of the Belfast Naturalists’ Field
Club, 1882-83. Ser. 2, vol. ii. part 3. 8vo. 1884,
Tux Report for the year ending 3lst March, 1883, completes the
history of the twentieth year of the Society’s existence and work.
Besides the reports of the several excursions, in which scientific
research and healthy pleasure appear to have been well combined,
and of the conversazione and annual meeting, this part contains
notices of several interesting papers:—on the crannogs at Lough
Mourne, near Carrickfergus (with an illustrative plate); on the
stone monuments of Carrowmore, near Sligo; and on Fungi, their
properties and uses. Mr. Joseph Wright, in occasional notes, men-
tions some Foraminifera new to.the British fauna, namely Milio-
lina triangularis, Haplophragmium agqylutinans, and Lagena castren-
sis, the last hitherto known only on the Australian coast. These
were dredged by him off Dublin. Also Rhabdogonium tricarinatum
and Pullenia quinquelola, dredged by Messrs. J. Wright and F. P.
Blakwill, the first off Lambay Island, in 50 fathoms water, and
the second at 45 fathoms about 20 miles off Dublin. A Meteoro-
logical Summary for 1883, and the Appendix vii., consisting of a
Supplement to a List of Mosses of the North-east of Ireland, by Mr.
8. A. Stewart, complete this Report.
Transactions of the Cumberlund Association for the Advancement of
Literature and Science. No. VII. 1882-83. Edited by J. G.
Goopcuitp. 8vo. Carlisle: G. and T. Coward. 1883.
Ir must be a question difficult to settle in the minds of many
working naturalists how far they should feel grateful to the swarm
of small local societies and field-clubs in all” parts of the country
which bring out their Transactions and Proccedings as separate
and independent publications. In the districts to which the activity
of these bodies is devoted such publications are doubtless of great
interest, and the societies gain much credit by their production ;
but it is rather hard upon the student to have to keep himself up to
the contents of so many comparatively obscure periodicals on the
chance of the appearance in their pages, among a mass of material
414 Bibliographical Notices.
of purely local interest, of some paper containing important results
in connexion with the subject of his special studies.
This difficulty would be certainly not altogether got over, but to
a considerable extent diminished, if the members of all our smaller
local societies and field-clubs would adopt the same plan as the
Cumberland Association, which owes its origin, we believe, to the
efforts of the late Rev. J. Clifton Ward. This Association consti-
tutes a central body to which all the local associations in Cumber-
land are affiliated ; it holds one meeting annually, and its meetings
are movable feasts, after the fashion of those of the British Associ-
ation, or, more accurately, the annual meetings of the Tyneside and
Berwickshire Field-Clubs ; but the Cumberland Association prints
in its ‘Transactions’ not only the papers read at the annual
meeting, but also a selection of the more valuable communications
made during the year to its affiliated local societies. It is this
plan, if it can be carried out without producing heartburnings, that
gives a special value to the publications of the Association ; the
ambition which prompts the secretaries of small local societies to
seat themselves in the editorial chair is crushed back by the weight
of the Association, and thus the chaff is to a great extent winnowed
from the wheat.
Thus in the present number, which contains 215 pages besides
the preliminary official matter, we have only twelve articles, two of
which, namely the Address of the President, Mr. Robert Ferguson,
M.P., and a paper by the Rev. T. Ellwood, relate to the ethnology
of the district, treated from a linguistic point of view, while a third,
by the Rev. H. D. Rawnsley, deals with the formation of a Lake-
District Permanent Defence Society, which we hope may meet with
full success in its endeavours ; and a fourth, by Mr. Fisher Cros-
thwaite, gives some curious particulars with regard to an immigration
of German miners to Keswick in the sixteenth century. All the
rest are of more or less interest. to naturalists. For the botanist we
have a “Contribution towards a list of Cumberland Mosses,” by the
Rev. R. Wood, recording the occurrence of 183 species, chiefly in a
limited locality, embracing the parishes of Westward and Caldbeck ;
additions by the same author to the list of Flowering-plants growing
in Cumberland ; and a note on the Botany of the Calder valley, by Mr.
William Hodgson ; andthe entomologist will find a catalogue of the
Lepidoptera of West Cumberland, by Mr. G. Mawson; all of interest
in connexion with the geographical distribution of species. An
important paleontological article is contributed by Mr. J. Postle-
thwaite, on the Graptolites of the Skiddaw Slates, in which the
author notices all the forms of those curious organisms which have oc-
curred in the formation, and supplements it witha note of the localities
where Graptolites have been found in the Skiddaw Slates, and a list of
published works relating to the subject. Mr. T. V. Holmes has a short
paper on the Geology of the Carlisle basin in connexion with water-
supply ; and the editor, Mr. J. G. Goodchild, furnishes a contribution
towards a list of minerals occurring in Cumberland and Westmore-
land, besides a long and exceedingly interesting memoir of the late
Miscellaneous. 415
Prof. Harkness, whose connexion with the Lake-district and its
geology renders such a commemoration on the part of the Cumber-
land Association peculiarly graceful aud appropriate. Mr. Good-
child has had access to many letters addressed to Prof. Harkness by
distinguished geologists at home and abroad; and his long extracts
from these give additional value to his memoir.
Besides the formal papers above mentioned, the part contains a
set of “ Local Scientific Notes and Memoranda,” relating chiefly to
various: minor matters of natural history, some of which may have
interest for students outside the district. Not content with having
written the longest article in the book, the Editor is the principal con-
tributor of these short notes, and, indeed, throughout he seems to
have performed his duties in an energetic and conscientious manner,
which has naturally led to the production of a most respectable and
valuable volume.
MISCELLANEOUS.
On the Structure of the Otocysts of Arenicola Grubii, Clap.
By M. E. Jourpan.
Tne author’s investigations were made upon the small Arenicole
of the coast of Marseilles and in the laboratory of that place.
By sectioning the cephalic segment of an <Arenicola previously
fixed by the injection of a solution of osmic acid of 0°50 per cent.,
the auditory capsules were shown in some sections and easily
recognized by their little calcareous corpuscles. The otocysts are
situated in the thickness of the integuments far from the hypodermis
and in the midst of muscular bundles; they are fixed by the con-
nective envelope of these bundles, which surrounds them. They are
not in direct contact with the cesophageal commissures, but connected
with them by several nerves. They are placed towards the dorsal
surface.
The nerve-fibres composing the commissure and the brain are
very fine and striated longitudinally. Nerve-cells exist throughout
the length of the commissure, some in its interior, but a much
greater number between the commissure and the hypodermis, often
intimately connecting these two parts.
The otocysts are spherical. The diameter of their cavity is ;)),
millim. and that of the sphere formed by the outer capsule ;22, mil-
lim. The thick walls consist of a layer of fusiform cells, a network
of fibrille arranged in a dense plexus, and a connective envelope.
The cells form the greater part of its thickness ; they are very deli-
cate, spindle-shaped, slightly inflated towards the middle, where the
nucleus is situated; they also increase in thickness towards their
inner extremity, where they are surmounted by a thick plate. The
plates of all the cells are closely soldered together, forming a cuticle,
which, in sections, is often detached from the cells which produced
416 Miscellaneous.
it. No layer of vibratile cilia was to be seen distinctly, but indi-
cations of them seemed to exist upon portions which had been long
in osmic acid. The cells taper at their base and at the same time
bend in different directions; and these basal prolongations anastomose
and form a very delicate network of fibrille, which, by their union,
constitute at the base of the epithelial layer a regular little zone,
intermediate between the nerve-fibres and the foot of the cells; a
few nuclei are distinguishable in it. This plexus rests against the
connective envelope, which is formed by a thin and dense mem-
brane, presenting perforations, through which the basilar plexus
enters into relations with the nerve-fibres.— Comptes Rendus, March
24, 1884, p. 757.
On Prof. Lindstréim’s Remarks on Prof. Martin Duncan’s
Criticisms.
To the Editors of the Annals and Magazine of Natural History.
GENTLEMEN,— With reference to Prof. Lindstrém’s communication
to the Ann. & Mag. Nat. Hist. for March 1884, p. 162, I wish to
inform you that, having sought the opinion of some naturalists well
qualified to judge between Prof. Lindstrom and myself, I find that
the language I used was not of a kind to merit the condem-
nation of being ‘* by no means consistent with the quiet tone that
ought to prevail in scientific discussions.” It appears to them and
to me that Prof. Lindstrom took unnecessary offence and that his
tone was very uncourteous.
I can assure you that nothing was further from my thoughts
than to give him personal offence; but he must remember that
his communication which I wrote upon was eminently critical, and
was bound sooner or later to provoke discussion. I gave the reasons
for not having sooner attempted a reply. Probably when some time
has elapsed Prof. Lindstrém will read my essay with more charitable
and kindlier feelings; and itmay happen that we may criticize one
another as Pourtalés and I did, with advantage to ourselves and
with the establishment of a sincere friendship.
Yours truly,
April 10, 1884, P. Martin Doncay.
Reproduction in Amphileptus fasciola.
By Anprew 8. Parker, M.D., Ph.D.
Several years ago, while examining some Infusoria, I noticed a
specimen of Amphileptus fasciola undergoing some curious changes,
the nature of which, at that time, I did not fully appreciate, sup-
posing them to be due to the dissolution of the animal. Recently
I observed the same series of phenomena occurring in another indi-
vidual, and on tracing them out more fully I found that they were
due, not to the death of the Infusorian, but to what I believe is a
method of reproduction not hitherto observed, or at least not de-
scribed, in this group. My attention, in both instances, was at-
tracted by a peculiar oscillating movement, the Amphileptus rocking
from side to side, the animal remaining stationary, although its
Miscellaneous. 417
cilia were in active motion. In other respects the animal appeared
normal, no changes being observed in its nucleus, protoplasmic
contents, or contractile vesicle. Shortly after I had noticed this
peculiar rocking movement | found that the elongated extremity was
breaking up into small masses of protoplasm; these gradually
separated from the parent body, and each of them exhibited distinct
amceboid movements. Although the cilia seemed to break off with
the small masses, I could not detect any signs of their presence
after separation. For about five minutes small protoplasmic masses,
exhibiting distinct and independent amceboid movements, continued
to be shed.
The rocking movement still continued, but now began to show
signs of being converted into a movement of rotation. Finally
a rotary motion was established, and the animal began to change
its position. At the same time I noticed a distinct elongation
occurring at the end where the changes described above had
taken place, a rounded projection appearing, which gradually elon-
gated, until finally, in the course of about two hours, the individual
had assumed its original shape and activity, although apparently
somewhat diminished in bulk. Cilia covered the new growth, but
they did not seem to be a new formation, but were produced by a
simple elongation of the ectosare, this being carried forward by
the growing endosarc. As regards the protoplasmic masses that
were shed or discharged, I observed them for about four hours, at
which time they were still active and the parent mass still in
active motion. On the following day I was unable to detect them,
and as to their subsequent history I know nothing.
To characterize the phenomena as described above, I propose the
term ‘“ Reproduction by Partial Dissociation.” Reproduction by
fission, gemmation, conjugation, and encystation have all been
observed in the ciliated Infusoria; and some of the older writers,
such as Ehrenberg and others, have described a mode of increase, in
which the substance of the body breaks up into a number of frag-
ments, each of which is capable of becoming a distinct individual.
This process they called diffluence ; but Stein and other more recent
observers Lave denied the existence of this process, claiming that it
was merely a form of increase from encysted forms. The pheno-
mena as exhibited by Amphileptus fasciola seem to be quite different
from those described as occurring in diffluence, and it certainly
was not a case of encystation.. I have been unable to find any ac-
count of reproduction in the Infusoria resembling that described
above, and I therefore place the facts on record, in order that the
attention of other observers may be directed towards the verifica-
tion of the phenomena and views expressed above.—Proc, Acad.
Nat. Sci. Philad. 1883, p. 313.
On the Anatomy of Peachia hastata. By M. Favror.
The Actinia discovered by Gosse (in 1855), and named by him
Peachia hastata, is known only by its external characters. Hitherto
any exact observation of its internal organization has been impos-
4i8 Miscellaneous.
sible, owing to the ruptures which take place in its mesenteroid
folds. The insensibility produced by water charged with carbonic
acid enables chromic acid to act fatally upon the animal without
causing contractions and lesions. When thus: treated its internal
organization differs considerably from that of all known Zoantharia,
including Cerzanthus, which hitherto presented the most exceptional
structure.
Twelve perforated mesenteroid folds at the level of the cesophagus,
Two of these folds, close together, instead of detaching themselves
from the lower margin of the cesophagus, and floating freely in the
general cavity, attach themselves to a gutter-like organ, the two
margins of which are approximated. This gutter commences on one
of the sides of the peristome, appearing externally as a papilliform
lip, and terminates in the general cavity not far from an orifice,
analogous to that of Cerianthus, which the animal possesses at its
lower extremity. Hight longitudinal muscular cords project upon
the inner wall, These are arranged in pairs, so that only four
chambers out of the twelve possess them. These four chambers
are placed unsymmetrically, one on each side of the organ above
described, the other two opposite one another upon an axis perpen-
dicular to that which would pass through the papilliform lp and
the inferior orifice.—Comptes Rendus, March 24, 1884, p. 756.
On a Cilio-flagelate Infusorian recently observed in Baltimore
Drinking- Water. By C. 8. Dottey*.
Having had my attention called to the presence of large numbers
of a peculiar minute green organism in the water-supply of the
Biological Laboratory, I became interested in identifying the same,
and find it to be a species of Peridinium. So far as I have been
able to ascertain, the only member of the family Peridiniide hitherto
described as occurring in America is a salt-water species from the
coast of South Carolina. After examining the specimens found
here, very carefully, and comparing them with the specific descrip-
tions given by Kent, I find that while they agree in most respects
with Peridinium tabulatum, they also have many points in common
with Peridiniwm apiculatum, though differing in several particulars
from both. They would therefore seem to constitute an interme-
diate species, or variety, if, in accordance with Stein, P. apiculatum
be regarded as only a variety or older phase of P. tabulatum. The
characters of our Baltimore specimen are as follows :—Body ovate
or subglobose, as seen in dorsal or ventral aspect, with a convex
dorsal and concave ventral surface as seen in lateral aspect ; cuirass
composed of numerous polygonal facets, which in the row next to
the equatorial furrow are separated by a clear space; the edges of
these spaces as well as of the longitudinal and equatorial furrows
are finely hispid. The remaining facets are closely united; all the
facets have a very marked reticulate structure, with the exception
* Abstract of some remarks before the University Scientific Association,
February 6, 1884.
Miscellaneous. 419
of the narrow linear ones in the equatorial furrow. There is a
deep notch or sulcus in the extremity of the posterior segment con-
tinuous with the longitudinal furrow of the ventral surface. The
equatorial groove does not remain in the same plane in passing
around the body; but upon the ventral surface, where it is joined
by the longitudinal furrow, it exhibits a fault, being in fact one
turn of a spiral. The margins of the equatorial groove are everted
and present laterally the appearance of tooth-like processes. The
flagellum is very delicate, and inserted at or near the posterior
sulcus in the longitudinal furrow. I was only able to detect it
in specimens killed with osmic acid, I could detect cilia only at
the posterior sulcus, on each side of which they present a tuft-like
appearance.
The eye-like pigment-spots are rather unfrequently present, and
vary from one to three or four in an individual, being located at
one side of the longitudinal fissure. The colour of the Infusorian
is a yellowish green, and its diameter =, inch. It moves with a
rolling motion about.its dorso-ventral axis, and was mistaken at
first for a Volvow or zoospore. It is attracted by light, moves
about freely on the slide, but ceases its motion if the slide be jarred
or struck. Many of the specimens which had been kept in a large
dish seemed to have taken on a resting-stage, the endoplasm
being retracted from the walls of the cuirass, and containing nume-
rous oil-globules. I was not able to find any of the “ lunate encyst-
ments” mentioned by Kent, nor could I make out the existence of
an endoplast.
The observations of Mr. Carter of Bombay indicate that the gre-
garious habit of Peridinium may at times render it a potent factor
in the contamination of drinking-water, and the peculiar taste of
Baltimore water at times may be due in part to large numbers of
Peridinia dying and decaying in the pipes.—Johns Hopkins Univ.
Circulars, March 1884, p. 60.
How a Carpenter-Ant Queen founds a Formicary.
Rev. Dr. McCook presented three specimens of fertile queens of
the Pennsylvania carpenter-ant, Camponotus pennsylvanicus. These
had been given him by Dr. Joseph Leidy, who had taken them
during the last summer at Wallingford, Delaware Co., Pa. The
circumstances under which they were captured afforded a good
demonstration of the manner in which a new colony of this and
other species is begun, confirming the speaker’s own observations
and published statements. One specimen was taken, August 9, in
a chestnut log; the others, August 14, in the stump of a chestnut-
tree. ‘They were enclosed within small cavities about an inch in
diameter, and, curiously, the queens had sealed themselves within
their nests by closing up the original opening by which they had
entered, and from which, as a nucleus, they must have cut out their
resident-room and nursery. If, therefore, they sallied forth to
obtain food, as they may have done (for Dr. McCook had at various
420 Miscellaneous.
times observed queens wandering solitary), they must have removed
the plug or “door,” and restored it to its place again upon re-entrance.
However, he believed it to be guite within the bounds of proba-
bility that a well-fed queen could live without additional food for
several weeks—a period long enough to rear a small brood, and also
feed the larvee from the contents of her crop, which might serve as a
storehouse of food, as was explained by illustrations of the anatomy
of the alimentary canal.
In the same receptacle with the queens were found:—(1) the
white oval or cylindrical eggs of the species; (2) larvae of various
sizes, from those just escaped out of the egg (2:3 millim. long) to
full-grown (about 10 millim.); (3) the cocoons, or enclosed pupe ;
and in one case (4) a callow antling, which had evidently just
escaped from its case. This antling was, as indeed all the larvee
and cocoons appeared to be, of the dwarf caste. There are three
castes in a formicary of Camponotus: the worker-major, the worker-
minor, and the minim or dwarf. We may infer that the latter caste
is the one which is first produced in rearing a family.
In response to a remark and suggestion made, that the imperfect
nurture given to the larvee, under the peculiar circumstances, might
account for the appearance of small workers first in order, Dr.
McCook stated that, whatever one might conjecture to have been
the fact in the remote origin of these castes among ants, it is certain
that when the formicary has been fully peopled with workers, and
the food-supply is unlimited, the several castes still continue to
appear. Minims, minors, and majors not only abound among the
mature insects, but are found among the larvae and cocoons. These
distinctions are a permanent feature of the ant economy ; and while
it is perhaps not permitted one to say that they are not caused by
differences in amount or character of the nurture given in the larval
state, yet this did not seem at all probable to the speaker. Tke
fact that, in some genera, the workers have also remarkable diffe-
rences in structure (as of the head, for example, in Phetdole and
Pogonomyrmex crudelis) goes to show that differentiation into castes
is regulated by something other than the food-supply.
The above observations are valuable as proving that the females
of Camponotus, when fertilized, go solitary, and after dispossessing
themselves of their wings, begin the work of founding a new family.
This work they carry on until enough workers are reared to
attend to the active duties of the formicary, as tending and feeding
the young, enlarging the domicile, &«. After that, the queens
generally limit their duty to the laying of eggs, and, as the speaker
had elsewhere fully described*, are continually guarded and re-
stricted in their movements by a circle of attendant workers, or
“court.”
The above facts are further illustrated and enlarged by a series
of observations made by Mr. Edward Potts, in accordance with the
* Proceed. Acad. Nat. Sci. 1879, p. 140; ‘ Agricultural Ants of Texas,’
p- 144; ‘ Honey and Occident Ants,’ p. 41.
Miscellaneous. 421
speaker’s suggestions and directions. On or about June 16, Mr.
Potts captured a queen of C. pennsylvanicus running across his
parlour floor, late at night. He placed it in a bottle, but forgot to
examine it until five days later (21st and 22nd June), when he was
surprised to find that the ant was alive, and had laid six or eight
eggs in the otherwise empty bottle; which eggs, in their various
stages of development, she continued to attend for about fifty days.
He fed the ant by dropping into her bottle a pinch of white sugar,
which he moistened every evening with a drop or two of water; at
which timesshe quitted her otherwise unremitting watch over the egos
and the larvze, to press her labium for a moment into the sweet fluid,
her labial and maxillary palps meanwhile rapidly vibrating with plea-
sure. The egg-laying was, from the first, very deliberate ; one or two
eggs were added to the original stock from time to time, until about
the 15th August, making the highest number counted, of all ages,
nineteen.
He did not observe the date of the first hatching, but these larvae,
at first no larger than the eggs, and only distinguishable upon close
observation by the slight grooves between the body-segments and the
ill-defined head, grew gradually at first, and afterwards more rapidly,
and reached finally a length of about 7 inch and began to spin their
cocoons. On the morning of July 20, the first was surrounded by a
single layer of web, but could still be seen working inside it. By
evening the cocoon was too opaque to be seen through. On the
morning of the 21st the second larva was covered in like manner,
and the third by the evening of the 22nd. For some days he was
able to detect the dark form of the young ant in one of these
cocoons, and on the evening of August 11 a worker was running
about the bottle and already essaying its administrations upon the
undeveloped eggs and the next series of larvae, quite as big as and
much heavier than itself. We have, then, the period from, say
June 20 to July 20 (thirty days), occupied in the development of
the first eggs and the fulfilment of the larval stage; from J uly 20
to August 11, say twenty-two days, were spent in the pupa state.
The manner of the young worker was very nervous and far from
soothing, especially to the well-grown larvae, who evidently much
prefer a mother’s care to that of an elder sister. He did not observe
this antling feeding from the sugar, but upon one or two occasions
saw osculatory advances towards its mother, which seemed to
indicate that it was not above receiving its nutriment from the
maternal fount to which it became accustomed during its wriggling
youth. It constantly climbed over the eggs and larvee, apparently
nipping them with its mandibles, but not moving them to any pur-
pose. He saw no well-defined attempt at feeding them on its part ;
though, after patient observation, upon several occasions, he observed
this act performed by the parent ant. She would caress the larva
by sundry pats with her antenne upon each side of the face, when,
if hungry, it would lift up its head under her mandibles, placing its
labium against hers, at which time a flow of liquid down the larval
throat was seen.
422 Miscellaneous.
As the queen’s labours increased, she was less given to moving
her charges from place to place, though they were not allowed to
remain long quiescent. While nervously anxious about them, Mr.
Potts thought that she showed little evidence of tenderness in her
treatment, trampling on them with her feet or dragging them
around under her heavy abdomen, as if they were really the putty
they looked like.
The moisture necessary for the cleansing and growth of the larvee
was apparently supplied from the tongue of the caretaker, who
examined them one after another, moistening the dry places and
keeping the egg and larval skins flexible. ‘The queen was very
careful of the eggs, standing nearly all the time with her head over
the little heap, occasionally picking them up to move them a quarter
of an inch or more to one side. She was thrown into a great
excitement of solicitude when a fly, attracted by the crumbs, in-
truded within her domicile. She sprang fiercely at the fly and
raged around her narrow compartment, seizing a group of eggs as if
to escape with them from a threatened danger, then replacing them
as though recognizing the impossibility of getting away. Her de-
meanour on this occasion indicated strong maternal solicitude.
Mr. Potts made some attempt to follow the embryonic changes,
and made a few drawings of the different phases. When first
seen the egg is full of fluid, uniform in appearance throughout.
When next observed segmentation had taken place and advanced
to the morula stage, showing everywhere small granular cells of
uniform size. Afterward a hy aline spot appears at one end of the
egg, which there seems empty or filled with a homogeneous fluid ; ~
next to which are large cells, containing smaller ones of various
sizes. Later both ends become transparent, the large cells
bounding the small-celled body-cavity and forming the well-known
gastrula condition. He was not able to trace the formation of
the various internal or external organs. ‘The cyclosis of pulsation
of the larval heart was counted in two instances at forty-five and
fifty per minute.
The manner of ovipositing (August 13) the nineteenth egg is
thus described :—When first observed the queen stood up high upon
all three pairs of legs, the abdomen thrown forward between them
and the head bent back almost to meet it. The egg was then about
half protruded. Considerable muscular action was visible throughout
the abdomen, and when presently the egg was posited she straight-
ened herself out with a visible air of relief, but forgot all about the
ege, which was left lying under her for several minutes while she
attended to other matters, until at last, accidentally touching it with
one antenna, she picked it up and carried it to the family apart-
ments, where, presently, the worker found it and placed it in the
group of the older eggs. An evident intent at classifying the eggs
and larvae was remarked, these (within the narrow limitations of
the chosen space) having ‘been kept to a good degree separate.
August 13, another worker was released from its cocoon. Mr. Potts
did not see the act, but believed that the female assisted, as she was
Miscellaneous. 423
seen standing over the neophyte, who seemed to be weak, its femora
bent forward, the tarsi and tibize still nearly reaching the end of the
abdomen, indicating the manner in which the legs were folded in
the cocoon. Immediately after release the mother gave the young
imago nourishment in the manner above described.
At this date there were in the formicary, beside the mature ants,
two full-grown larve, very fat, two about half-grown, and several
smaller ones, with the eggs in different stages of development. The
two oldest were then evidently about ready to spin, but what chance
they could have, with the mature ants continually trampling over
them, standing them up on end or hauling them cff to a distance,
Mr. Potts was at a loss to imagine. From the mouth of one he
observed a strand of silk protruding, but the workers came, appa-
rently trying to grasp it, and left him in doubt whether their object
was to help or hinder the weaving process.
August 14, one of the two full-grown larve was found wrapped
in its winding sheet. The web was very thin and the motion of
the larva readily seen through it. The other larva seemed almost
totally quiescent, but careful examination with a Coddington lens
showed some muscular action in the posterior segments of the body.
Their state of comparative torpor was thought to immediately pre-
cede the act of spinning. At this date the workers had become less
nervous in their motions, and the female seemed to have resigned
most of her labours to them, resting much of the time quietly in one
place.
August 16, the third worker had emerged and was found quite at
home in attending to its duties. The second grown larva was then
still uncovered and quiescent. Very close observation was required
to show that it still breathed, and it made no other visible motion.
These observations of Mr. Potts establish or confirm the following
points :—(1) The manner of depositing the eggs, which, as well as
the larvee, are cared for by the queen until the workers are matured ;
(2) the stages in the development of the egg and larva are partially
noted; (3) the time required for the change from larval to pupal
state is about thirty days; (4) about the same period is spent in
the pupa state, the entire period of transformation being about sixty
days; (5) the work of rearing the first broods of Camponotus
begins in the latter part of June or early in July ; (6) about twenty-
four hours are spent by larve in spinning up into cocoon; (7) the
ant-queen probably assists the callow antling to emerge from its
case; (8) not only the larvee, but occasionally also the antlings, are
fed by the queen; (9) the young workers, shortly after emerging,
begin the duty of nurses, caring for the eggs and tending the larvee.
Some of these points thus abstracted and formulated by him Dr.
McCook was subsequently able to confirm from observations upon
the same queen. His thanks were due to Mr. Potts for the intel-
ligent and successful manner in which his suggestions had been
carried out.—Proc. Acad. Nat. Sci. Philad., Dec. 1883, p. 303.
424 Miscellaneous.
On some new and imperfectly-known Exotic Simple Ascidia.
By Dr. R. von Drascur,
The author has submitted the exotic simple Ascidians of the Zoolo-
gical Museum of Vienna to a revision, the results of which are as
follows:—Of the eighteen species described by him ten are new.
Of the others some have been very imperfectly described, or at least
there was room for remarks and observations tending to complete
our knowledge of them. Of the new species the following appear
to be particularly interesting on account of their remarkably formed
hypophysial tubercles — Microcosmus Herdmanii and Cynthia
Roretzii. In both tne tubercle consists of two cones inclined to-
wards each other at an obtuse angle, upon which the ciliated
groove is spirally twisted. In Oynthia Roretzir the ciliated canal
bears teeth, which fit into opposite spaces. A similar tubercle is
figured in Cynthia preputialis, Heller. A transition from the
usual arrangement of the ciliated canals of the tubercles in the same
plane towards that above described is shown by Polycarpa rugosa,
sp. un. The tubercle of Polycarpa sulcata, Herdm., has a remarkable
form ; in it there occur numerous crateriform apertures of the hypo-
physial canal, reminding one of similar conditious in Ascidia mamil-
lata. In Chelyosoma productum, Stimpson, a species remarkable
for the abundance of its musculature, all the peculiarities of the
hypophysial organ described by Julin were again met with.
The new species Microcosmus Julinii and Cynthia mauritiana
are distinguished by spicules both in the test and the mantle. The
latter species is closely allied to Cynthia pallida, Herdm. - Cynthia
sacciformis, sp. n., contains peculiar spicules, resembling those of
Culeolus, Herdm. Spicules were also detected in Boltenia pachy-
dermatica, Herdm.
A new Cynthia (C. mirabilis) is particularly interesting. Its
branchial and cloacal apertures are placed at the opposite ends of
the ovate body. The remarkable distribution of the musculature
aud the peculiar position of the digestive and generative organs
caused by the abnormal position of the apertures seem to the author
to furnish characters which, in the event of the discovery of other
similar species, may justify the establishment of a new genus.
Cynthia nodulosa, sp. n., is distinguished by an enormous annular
muscle situated at the base of the siphons, as also by the spinosity
of the ring-membrane. Cynthia castaneiformis, sp. n., which in
external aspect resembles C. echinata, is remarkable for a branchial
sac, the inner longitudinal vessels of which only embrace between
them three large circular stigmata. Corella novare, sp. n., very
closely approaches C. ewmyota, Traustedt, from which species it is
distinguished by its differently formed hypophysial tubercle and the
great number of tentacles—Anzeiger der k. k. Akad. der Wiss. in
Wien, March 20, 1884, pp. 66, 67.
THE ANNALS
AND
MAGAZINE OF NATURAL HISTORY.
[FIFTH SERIES.]
No. 78. JUNE 1884.
XLVIII.—On the Origin of the Fauna and Flora of New
Zealand. By Captain F. W. Hutton *.
I. THe AUSTRALIAN AND SouTH-AMERICAN ELEMENTS.
Eleven years have elapsed since I read a paper to the
Wellington Philosophical Society on the ‘ Geographical
Relations of the New-Zealand Fauna” t. During that time
the data on which the discussion of this question rests have
very much increased, and the literature of the subject has
been enriched by the valuable works of Mr. A. R. Wallace
on the distribution of animals, works which embody the
results of much patient research and acute reasoning. Under
these circumstances I wish, in this address, to return to my
theme once more. I wish to explain how far I now think my
own ideas of 1872 to be erroneous; how far I am able to
agree with Mr. Wallace in his view of the origin of our fauna
and flora, published in 1880 in ‘ Island Life ;’ and how far,
* Presidential Address to the Philosophical Institute of Canterbury,
Ist November, 1885. Reprinted from a separate impression from the
‘New Zealand Journal of Science’ for January 1884. Communicated by
the Author.
+ Trans. N. Z, Inst. vol. v, (1872), p. 227; and Ann. & Mag. Nat,
Hist. ser. 4, vol. xii. p. 25.
Ann, & Mag. N. Hist. Ser. 5. Vol. xiii. 28
426 Capt. F. W. Hutton on the Origin of the
as it appears to me, Mr. Wallace’s theory fails to explain the
whole of the facts. I also wish to suggest the alterations and
additions that seem to be necessary in order to get a good
working hypothesis. It will be advisable, however, not to
limit ourselves to New Zealand, but to take first a wider view
of the subject; for the faunas and floras of Australia and
Polynesia are so intimately connected with those of New
Zealand, that the origin of the latter cannot well be considered
until a general knowledge of the biological and geological
history of the Pacific area has been obtained.
Fossil plants have been found in many places in New
Zealand, often abundantly and in good preservation, and they
belong to several different geological periods. These plants
have not yet been described, but they have been examined by
Dr. Hector, who has published an abstract of the results of his
examination in the ‘ Proceedings of the New-Zealand Insti-
tute,’ vol. xi. (1878), p. 536, and in the ‘ Handbook of New
Zealand’ (1880). The earliest traces of plants are very
obscure, but the Triassic rocks contain ferns (lossopteris),
horse-tails (Schizoneura), cycads (Zamites), and wood of a
kauri (Dammara). The oldest known extensive flora is of
Jurassic age; it consists chiefly of ferns and cycads, which
are closely allied to those which inhabited India at the same
period, as exemplified by the fossils of the Rajmahal hills, In
the Cretaceous rocks numerous dicotyledonous plants occur,
forty different species having been distinguished. ‘These, as
well as some conifers, belong to species closely allied to those
at present living in the country, although some, such as
Araucaria, have become extinct in New Zealand. In the
lower beds of the system these plants are associated with
ferns that are also found in the Jurassic strata. The flora of
the Tertiary era ‘‘is badly preserved, and the collections are
scanty; but, as far as yet studied, it bears a very close affinity
to the recent flora of the country.” It thus appears that the
main features of the present New-Zealand flora are very old, ©
dating from the Cretaceous period, with a mixture of still
older forms among the ferns and conifers.
Let us now turn to Australia. No fossil plants, so far as
I know, have as yet been found in Western Australia, but in
Eastern Australia they occur in several places. The Paleo-
zoic rocks of Victoria, New South Wales, and Queensland
contain Calamites, Lepidodendron, and ferns, in some cases
identical with plants of the same era in EKurope and America.
In the Triassic and Jurassic beds cycads and conifers are
found, together with the same ferns which occur in New
Zealand and in India in equivalent systems. No plants are
Fauna and Flora of New Zealand. 427
known of Cretaceous age, but in the Eocene vegetable remains
have been found in New South Wales which, according to
Baron von Miller and Baron von Ettingshausen, are all
extinct forms but little allied to the present Australian flora ;
for with Pittosporum, Knightia, and tour kinds of Eucalyptus
there occur birches, alders, oaks, and beeches; while in Vic-
toria extinct tropical trees are found which resemble those of
Asia. The fossil plants mentioned by Mr. Darwin at Geil-
ston Bay, near Hobart, in a freshwater limestone of probably
Miocene age, are also very different from those now living in
Tasmania. They belong, as Mr. Darwin says, to a lost vege-
tation *. They represent willows, birches, alders, oaks, and
beeches, along with Coprosma, Araucaria, and others. They
are more characteristic of Australia than are the Eocene
plants; but still both are much nearer to the Tertiary floras of
Europe, Asia, and North America than to the recent Austra-
lian flora. In beds of newer Pliocene age plant-remains have
been found both in New South Wales and in Victoria, and
these, according to Baron von Miiller, are allied to the present
flora of Eastern Australia. What a contrast to New Zealand
is here! The present flora of Eastern Australia does not date
beyond the Phocene period, previous to which the country
was covered by a lost vegetation allied to the Tertiary floras
of Europe and Asia; while in New Zealand, as we have just
seen, the present flora dates from the Cretaceous period.
Mr. Wallace has given a very simple explanation of these
curious facts. The Australian flora, he says, consists of two
large divisions :—(1) the characteristic Australian flora, which
is chiefly temperate and hardly represented in New Zealand ;
and (2) a tropical flora, which is less in number than the first,
is closely allied to the floras of India and Malaya, and has
many representatives in New Zealand and in South America.
Western Australia has no European, Antarctic, or South-
American types, but it is far richer than Eastern Australia
in true Australian forms, many of which are only found there.
He also points out that a submarine ridge, nowhere more than
1000 fathoms below the present sea surface, runs from New
Zealand to Northern Queensland, and that the distribution of
the Cretaceous rocks in Australia proves that at that period
the sea flowed over the centre portion of the continent,
dividing the east from the west. rom these facts Mr. Wal-
lace infers (1) that the submarine ridge between New Zealand
and North-eastern Australia was elevated above the ocean at
the same time that Central Australia was submerged; and
* Volcanic Islands,’ p. 140. :
28
428 Capt. F. W. Hutton on the Origin of the
(2) that South-western Australia is the remnant of an extensive
isolated continent which received the ancestral forms of its
fauna and flora at a very early, probably Jurassic date, by a
temporary union with the Asiatic continent over what is now
the Java sea; and it was on this continent that the charac-
teristic Australian flora and mammalian fauna were developed*.
He supposes that during the Cretaceous period Eastern
Australia, separated from Western Australia by a wide arm
of the sea, supported a flora that was principally tropical and
of Polynesian type, derived from the north through New
Guinea; but, in addition, there were fragments of the typical
Australian vegetation which had reached it as stragglers from
Western Australia, and also a few south-temperate forms from
antarctic lands, which had arrived from ‘lasmania. New
Zealand, which at this time is supposed to have been joined
to North-eastern Australia, was open to the immigration of
the Polynesian flora and of such Australian types as had
reached the tropical portions of Eastern Australia. At the
close of the Cretaceous period the northern prolongation of
land between New Zealand and Queensland sank; New
Zealand was separated from Australia, and has ever since
remained isolated with its flora. Eastern Australia remained
separated from the west until late in the Tertiary era, when
Central Australia was elevated. The flora of Western Aus-
tralia then invaded the east, and exterminated to a large
extent the older tropical vegetation and completely changed
the character of the flora.
Such is Mr. Wallace’s hypothesis, which, except in some
details, is so far gatisfactory, the only obvious objections
being (1) that the origin of the Australian flora is attributed
to a period when no Dicotyledons are known to have existed,
and (2) that the majority of the characteristic Australian
mammals belong to Eastern and not to Western Australia.
These are difficulties, however, which further knowledge may
dispel ; but the hypothesis cannot be considered as a complete
solution of the problem, because one large class of facts is not
satisfactorily explained. I allude to the South-American
types found in Eastern Australia and New Zealand, many of
which belong to tropical and subtropical genera. Mr. Wal-
lace’s explanation of the presence of these forms is that a
migration took place through New Zealand, South Victoria
Land, South Shetland Islands, and Tierra del Fuego over a
* This had been indicated by the Rey. J. Tenison- Woods in the Proc.
Roy. Soc. Tasmania, 1875, p. 20, and previously by Prof. Jukes in his
‘Physical Structure of Australia,’ quoted by Hooker, ‘Flora Tasmania,”
Intr. p. ci.
Fauna and Flora of New Zealand. 429
greater extension of southern lands during a warm Miocene
period. Now Dr. P. Martin Duncan is certainly of opinion that
the sea in this portion of the southern hemisphere was much
warmer in the Miocene period than at present, and he has
suggested that this was due to an extension of the Antarctic
Continent up to 50°8.*; but, on the other hand, Mr. Darwin
considered the Eocene sea of Chili to have been no warmer
than at present, and Mr. Tenison-Woods says that “the whole
evidence of the [Tertiary] fossil corals shows a climate and
isolation in the New-Zealand fauna not very different from
the conditions which exist now,” and that the Tertiary fauna
of New Zealand generally “is not that of a warm sea, nor like
what we should find on the warmer extra-tropical portions of
the Australian coast” +. The Miocene Mollusca appear to
me to indicate a rather warmer sea; but, as several of the
species still live as far south as Foveaux Straits t, no eleva-
tion of temperature sufficient to take tropical and subtropical
plants and animals to 50° 8. is probable; and, in addition to
other difficulties presently to be mentioned, I shall, I think,
be able to show that the South-American connexion is of a
far older date than the Miocene. Before doing so, however,
it will be necessary to give a short review of the fauna of the
Australian region.
In Mr. Wallace’s opinion the deep oceans, 7. e. the Pacific,
Atlantic, and Indian Oceans, have been in existence from the
earliest geological times. All the principal groups of land
animals, he thinks, have originated in the northern hemi-
sphere, and have gradually migrated southwards through the
continental extensions’ of America, Africa, and Australia
(including the Indian archipelago), comparatively few having
subsequently spread east and west by means of antarctic islands
now submerged. If this be true, it is evident that the fauna
of Australia ought to be more nearly allied to that of South
Africa than to that of South America, because the connexion
with the former by way of India is so much closer than the
connexion with the latter by Kamschatka and Alaska. Let us
see if this is so.
The Australian Mammalia are very peculiar, and are more
closely allied to the Jurassic mammals of Kurope and America
than to any now living. The marsupials of America are
related to the Hocene marsupials of Kurope, and are evidently
* Quart. Journ. Geol. Soc. 1876, p. 345.
+ ‘ Paleontology of New Zealand,’ part iv. p. 4 (1880).
} Such as Voluta pacifica, Triton Spenglert, Parmophorus unguis, Chione
Stutchburyi, Tapes intermedia, Pectunculus laticostatus, Waldheimia lenti-
cularts, and others.
430 Capt. F. W. Hutton on the Origin of the
a younger branch of the family from which the Australian
mammals had been separated long previously. Consequently
the relationship between the American and Australian marsu-
pials does not militate against Mr. Wallace’s theory. ‘The
distribution of the birds is decidedly favourable to it. The
flycatchers, sun-birds, hornbills, bee-eaters, king-crows, king-
fishers, nightjars, swifts, bustards, and other Australian
birds are all related to Old-World forms, exceptions perhaps
being found in the Megapodes, or mound-builders, which are
probably allied to the curassows of Brazil, and also in the
brush-tongued parrots, which have their nearest allies in the
parrots of South America.
Most of the families of lizards follow the same rule of dis-
tribution as the birds; but the Gymnophthalmide are not
known in North America, although found in Timor, New
Guinea, Polynesia, and South America ; and of the Iguanidz
(a characteristic South-American family) a very distinct
species is found in Fiji, and another is supposed to occur in
Australia. With the snakes the case is different. Out of the
fourteen families of land-snakes inhabiting the Australian
region, no less than four are found in India, Africa, and South
America, but not in North America; and another family, the
Amblycephalidee, is found in India, in South America, and
doubtfully in New Caledonia, but not in North America,
although all, according to Mr. Wallace, must have passed
through North America. The freshwater tortoises are found
only in Africa, Australia, and South America. The principal
genus, however, occurs both in Australia and in South
America, but notin Africa. Here, therefore, the distribution
is not in accordance with theory.
The affinity between the faunas of Australia and South
America is still better shown in the frogs, whose distribution
is quite at variance with that of the birds. One family (Pelo-
dryadze) is confined to these two regions; two others have the
same distribution as the families of snakes just mentioned,
being absent from North America, while closely allied forms
are found in Australia and South America; and a family of
tree-frogs, although widely spread and occurring in North
America, has the South-American species more closely related
to those of Australia than to those of North America.
The marine and most of the freshwater fishes (except
Osteoglossum, which is found only in Borneo, Queensland, and
Brazil), as well as some groups of insects, such as most of the
butterflies and stag-beetles, follow the same rule in distribu-
tion as the birds; while other groups of insects, such as the
Buprestide, Longicorn beetles, and the family of Castniude
among moths, follow the distribution of the frogs.
Fauna and Flora of New Zealand. 431
The distribution of the marine Mollusca of Australia and
Polynesia is favourable to Mr. Wallace’s theory; but’ the
terrestrial Mollusca, although most nearly allied to those of
the Indian archipelago, have strong affinities with the Mol-
lusca of South America, and show no connexion with those of
Africa. This is seen in Trochomorpha, Tornatellina, Cyclo-
tus, Cyclophorus, and Helicina, which are found in Polynesia,
Australia, and South America ; Macrocyclis, in Australia and
South America; Partula (a characteristic Polynesian genus)
is found also in South America; Placostylus is allied to Ortha-
licus of Chili, Peru, and the Solomon Islands; and Vaginulus,
a marine pulmonate, occurs in India, the Philippines, and in
South America. This remarkable distribution is very instruc-
tive; for as the marine shells of the Indo-Pacific province
have been unable during the whole of the Tertiary era to cross
from Polynesia to America, it follows that when the ancestors
of these land-shells crossed, the physical geography of the
region must have been very different trom what it is now, for
there is no trace of their having passed into South America
from the north.
We see, then, that the Australian fauna consists of three
elements. The first is typified by the mammals, and is cha-
racteristically Australian. The second is typified by the birds,
and is more nearly related to African than to American forms.
The third is typified by the frogs, and is more nearly related
to South America than to any other partof the globe. There
is also a fourth element—the antarctic—which I pass over for
the present.
Now it is very difficult, or even impossible, to believe that
all the groups of semitropical plants and animals which con-
nect Australia, Polynesia, and even the Sandwich Islands
with South America have travelled down from the north by
the present land-routes, for then we should have to suppose
that all had become extinct in North America, and certainly
we should expect to find the connexion between Australia
and Africa at least as close as it is between Australia and
South America, which is not the case. But even if we got
over this difficulty, we should still be unable to explain the
facts. If, for example, the frogs had passed into South
America by the same route as the birds, both would have
shown a similarity in their distribution. The assumption
that the present frogs are mere relics of a formerly more
extended distribution, and that allied groups have become
discontinuous through extermination, will not help us; for if
all birds were now to become extinct north of the equator, we
should still find the avifauna of Australia more nearly related
to that of Africa than to that of South America; and it is
432 Capt. F. W. Hutton on the Origin of the
impossible, by assuming any reasonable amount of extermina-
tion, to make the distribution of birds accord with that of the
frogs. The lines of migration of frogs must therefore have
been different from those of birds. Again, Mr. Wallace
himself allows that salt water is almost a complete barrier to
the dispersal of frogs * ; consequently where frogs could pass
birds could pass also; and as the former have passed between
Australia and South America, but not the latter, it follows
that the two could not have spread together, but each must
have pursued a different route at a different time. And as
the present shape of the land accounts for the distribution of
the birds, the distribution of the frogs must have taken place
before the present groups of birds were in existence. But
birds of many kinds were abundant in Europe and in
America in Eocene times; and as we know that penguins
inhabited New Zealand at the same period, it is probable
that birds then existed in Australia also. Consequently
the South-American migration must have taken place be-
fore the Hocene, and cannot be referred to a warm Miocene
period. Evidently, therefore, the existence of the South-
American element ‘in the Australian fauna and flora requires
some explanation which Mr. Wallace’s hypothesis does not
supply.
It was these considerations, together with the fact that the
earthquake-wave of 1868 had proved that the average depth
of the South Pacific Ocean was not great, which led me in
1872 to propose the hypothesis that in the Lower Cretaceous
period an antarctic continent extended northwards into Poly-
nesia, connecting Australia with South America and, perhaps,
with South Africa. I introduced the African connexion
solely to account for the distribution of the Struthious birds ;
but I am now satisfied that Mr. Wallace’s explanation of
the spread of these birds from the north is more correct; and
no reason therefore remains for supposing that Australia was
ever connected with Africa. But the evidence of a connexion
with South America is stronger than ever. Nevertheless I
now abandon the idea of an extensive antarctic continent,
because the soundings that have been lately taken in the
Pacific Ocean have shown that such a supposition is highly
improbable. At the same time these soundings have made it
clear how the connexion really took place.
The surveys of the ‘Tuscarora,’ the ‘Gazelle,’ and the
‘Challenger’ have proved that a vast submarine plateau,
nowhere more than 2000 fathoms below the sea-level, runs
* ‘Geographical Distribution of Animals,’ i. p, 416,
Fauna and Flora of New Zealand. 433
from New Guinea and North Australia in an easterly direc-
tion through the Fiji and Tonga Islands to Samoa, spreading
south to New Zealand and north to the Ellice, Gilbert, Mar-
shal, Caroline, and Pelew Islands. This plateau is split into
two portions by a deep narrow channel, which runs between
New Zealand and the Kermadec Islands and between New
Caledonia and the New Hebrides until it almost reaches
Torres Straits. Another submarine plateau, also never more
than 2000 fathoms below the sea-level, extends from Chili in
a north-west direction to the Society Islands and Cook’s
Islands, including Juan Fernandez, Kaster Island, the Pau-
motus, and the Marquesas Islands. Between Cook’s Islands
and the Samoa Islands there is a deep channel, but whether
this is continued into the deep sea north of Samoa or whether
the two plateaux are continuous is uncertain. Mr. Wild, of
the ‘ Challenger’ Expedition, says, ‘ It seems as if an almost
uninterrupted area of elevation crossed the whole basin of
the Pacific in a north-westerly direction from Patagonia to
Japan” *, probably about 1500 fathoms from the surface.
North of this plateau the ocean averages 3000 fathoms in
depth. ‘To the south it ranges from 2900 to 2600 fathoms,
getting gradually shallower towards the south-east. The
shallowest part of the plateau is the ridge, already mentioned,
between New Zealand and North Australia, which is nowhere
more than 1000 fathoms below the surface.
Here we have probably the remains of an ancient conti-
nental area, which bridged the South Pacific and allowed the
passage of frogs, land-shells, insects, and plants between New
Guinea and South America, but which became submerged
before the present groups of birds had come into existence.
The date of this South-Pacific continent must have been
anterior to the marine Indo-Pacific fauna, because hardly any
of the fishes, Crustacea, and shells of Polynesia have crossed.
over to America; and it must have been posterior to the
appearance of dicotyledonous plants. Now of the genera of
marine shells characteristic of the Indo-Pacific fauna and not
found on the American coast, Turbinella, Ricinula, Tridacna,
and Aspergillum are Miocene; Rimella, Rostellaria, Seraphs,
Dolium, Ancillaria, Cardilia, Pythina, and Glaucomya are
Eocene; while Vulsel/a is found in the Upper Cretaceous
rocks. A few others, such as Nauttlus, Stomatia, and Nerit-
opsis, are old forms apparently dying out. The genus Mono-
ceros is also found in the Kocene rocks of Chili, but is not
known in the Indo-Pacific province. We cannot therefore
* ‘Thalassa,’ p. 22.
434 Capt. F. W. Hutton on the Origin of the
put the South-Pacific continent later than the Cretaceous
period. On the other hand, though fossil plants belonging to
the Jurassic period are known from many parts of the world,
not a single Dicotyledon has as yet been found among them, the
oldest known form being a poplar from the Lower Cretaceous
beds: of Greenland. In the Upper Cretaceous epoch dico-
tyledonous plants were abundant in Europe, North America,
and in tropical Africa, and each of the three classes Mono-
chlamydez, Polypetale, and Gamopetale were represented.
The South-Pacific continent must therefore have existed after
the Jurassic, and must have been submerged before the
Eocene period.
Let us now see what light the geology of the surrounding
countries throws on the subject. ‘To commence with Chill:
from Mr. Darwin’s ‘ Observations on the Geology of South
America’ we learn that the fundamental rock-system of Chili
and Western Tierra del Fuego consists of an irregular plateau
of mica-schist and gneiss. On this floor immense masses of
volcanic rocks, chiefly andesites and diorites, have been poured
out from submarine volcanoes, forming the ranges of moun-
tains called the Andes. ‘These mountains are highest in the
north, and get lower and lower southwards ; but portions of
volcanic rocks are found all through to Tierra del Fuego.
High up among the volcanic rocks of the Andes in Chili a
sedimentary gypseous system occurs, containing fossils of the
Lower Cretaceous or perhaps Upper Jurassic period. Fossils
of the same age are also found in a clay-slate system forming
the eastern side of Tierra del Fuego and stretching far up the
eastern flanks of the Andes. These Lower Cretaceous rocks
go toa height of 14,000 or 15,000 feet above the sea. On
the Atlantic side enormous plains of gravel and silt slope
from the sea to an elevation of 8000 feet or more at the
base of the mountains. On the Pacific side horizontal strata
of probably Eocene age lie on the older rocks, and_ these
are covered in places by gravel-beds, which go to a height of
1300 feet.
From these facts Mr. Darwin infers that during the Juras-
sic period this part of South America was a deep sea, on the
bed of which volcanic eruptions took place. In the Lower
Cretaceous it was shallow sea, with land in the neighbourhood,
but the bottom was sinking, and it was further depressed for
7000 or 8000 feet, although the volcanic ejections continued
to maintain land above the surface of the ocean. In the
Upper Cretaceous period upheaval commenced, and, although
interrupted by many oscillations, this upheaval has been
going on ever since, until the elevation has been as much as
Fauna and Flora of New Zealand. 435
14,000 or 15,000 feet, that is 2500 fathoms. Now it is fair
to suppose that when the immense mass of Chili, part of Peru,
La Plata, and Patagonia was depressed 2500 fathoms below
its present level, a compensating elevation may have occurred
in the South Pacific Ocean, and that as South America rose
the bed of the Pacific sank. If this were the case, the South-
Pacific continent must have been in existence in the Jurassic
and Lower Cretaceous periods, and begun to subside in
the Upper Cretaceous. The lowest portion, that between
Samoa and the Society Islands, would have been submerged
first, and the connexion between New Guinea and South
America may have been severed before the close of the Cre-
taceous period. This conclusion agrees very well with that
drawn, quite independently, from a study of the Australian
fauna and flora.
On the western side of the South Pacific the oscillations of
the land appear to have been much less. Of the geology of
New Guinea it is known that Jurassic rocks are largely deve-
loped both in the north and in the south, which indicates that
the land then stood at a lower level. No Cretaceous rocks
are known from any part, and at this period therefore it may
have been upheaved. ‘Tertiary clays and limestones occur at
Hall’s Sound and at Yule Island; but as, according to Mr.
Tenison-Woods, the fossils have nothing in common with
those of Australia, their age remains at present doubtful *.
New Caledonia consists principally of two rock-systems,
one of older Paleozoic, the other of older Mesozoic age. Ac-
cording to M. Garnier, Lower Cretaceous rocks are also found
there; but the evidence appears to consist of a single fossil
(Pinna) only.
In Eastern Australia and Tasmania the main range of
mountains is formed of contorted schists and slates of Lower
Paleozoic age. In New South Wales the denuded surface of
these rocks is covered by enormous masses of shales and sand-
stones of Upper Paleozoic and Lower Mesozoic age, lying in
a nearly horizontal position and forming the upper portions
of the Blue Mountains. Further to the north, in Queensland,
this system is overlain in places by rocks of Jurassic and Cre-
taceous age. Jurassic rocks are also found in Tasmania,
Victoria, and in Western Australia; consequently we must
suppose that during this period Australia was more depressed
than at present, although not altogether submerged. During
* Mr. C.S. Wilkinson believes them to be of Lower Miocene age (Proc.
Linn. Soc. N. S. Wales, vol. i. p. 114). For Mr, Tenison-Woods’s
opinion see the same publication, vol. vii. p. 882. Formerly he con-
sidered them as probably older Pliocene (/. c. vol. ii. p. 127).
436 Capt. F. W. Hutton on the Origin of the
the whole of the Cretaceous period all Central Australia and
the whole of Queensland appear to have been under the ocean,
the Rev. J. Tenison-Woods having found Upper Cretaceous
rocks on the very summit of the dividing range inland from
Brisbane. But Western Australia, New South Wales, Hast-
ern Victoria, and ‘Tasmania remained above water. There
are no Tertiary marine rocks on the east coast of Australia,
and we must therefore assume that in the Eocene period
Queensland was elevated, and from that time neither it nor
New South Wales has ever stood much lower than at present.
It also appears probable that the centre of the continent re-
mained submerged until the close of the Miocene period or
even later. But the geological evidence on this point is at
present uncertain, for the ‘“ Desert Sandstone,” so largely
developed in the interior, and which lies unconformably on
the Cretaceous system, is thought by Daintree and Clarke to
be marine, by Etheridge to be lacustrine, and by Tenison-
Woods to be of eolian origin and of different ages. Marine
Miocene rocks are found at an elevation of 800 feet above the
sea * ; butas the central plateau of Australia rises to more than
1000 feet in the north, it would not necessarily be altogether
submerged, especially as the northern parts of Australia
appear to have been subsiding for a long time. On the other
hand, Professor Duncan is of opinion that the Miocene sea
of South Australia and Tasmania was of so high a tempera-
ture that it must have been open to the influx of warm currents
from the north. Be this as it may, it is evident (1) that
during the Jurassic and Cretaceous periods Australia stood at
a lower level than at present, and (2) that it could not have
been joined to New Guinea during the Cretaceous period, as
supposed by Mr. Wallace, although this may very probably
have occurred during the Kocene period.
Western Australia appears to have been more stable than
any other part of the continent. The Darling range consists
of granite, capped by sedimentary rocks of Upper Paleozoic
age. On the east these ranges end abruptly in cliffs from
200 to 500 feet high, overlooking plains and salt~marshes
composed of the ‘‘ Desert Sandstone.” ‘Towards the sea, on
the west, the granite disappears, and its place is taken by
Upper Paleozoic’ rocks, which are overlain in places by
another system of undoubtedly Jurassic age; and these are
again overlain near the coast by eolian rocks of a recent
date. Western Australia, therefore, appears to have been a
* C, 8. Wilkinson, ‘ Notes on the Geology of New South Wales,’ 1882,
p. 57.
Fauna and Flora of New Zealand. 437
land-surface during the whole of the Tertiary and Cretaceous
periods, and perhaps it may date back to Triassic times.
The oscillations of land were on a much smaller scale in
Australia than in South America, but they were somewhat
similar. During the Jurassic and Lower Cretaceous periods
both seem to have undergone subsidence ; but while in South
America elevation commenced in the Upper Cretaceous, in
Australia it did not commence until the Hocene. This there-
fore agrees with, or at any rate in no way contradicts, the
conclusion already arrived at, that the South-Pacific continent
existed in the Jurassic and Cretaceous periods; but New
Guinea, perhaps, was not connected until the Lower Cre-
taceous.
In the Pacific area itself all we know is that a sedimentary
rock containing fossils occurs in the centre of Levuka, one of
the Fiji Islands; and, according to Mr. Tenison-Woods, the
fossils are of Tertiary, possibly early Tertiary, age, and show
a tropical climate*, This is interesting to us as indicating
that the South-Pacifie continent was broken up in early
Tertiary times.
Having thus got some idea of what has probably been
going on in the South Pacific, we will now turn our attention
to our own country, New Zealand. Sir Joseph Hooker, in
the well-known introduction to his ‘ Flora Nove Zealandiz,’
published in 1853, divides our flora into five elements :—(1)
Australian, (2) 8. American, (3) North Temperate, (4) Ant-
arctic, and (5) Polynesian; and he thinks that a land com-
munication, not necessarily continuous, is required to account
for the presence of each of these elements, although the diffe-
rent communications may not have been at the same epoch.
I do not mean on the present occasion to touch the North
Temperate and Antarctic elements further than to show that,
on the whole, they are of later origin than the other three, all
of which, with few exceptions, are more or less subtropical
in character. In my remarks [ shall take all my data from
Hooker’s ‘ Handbook to the Flora of New Zealand’ (1867),
because, although many new species have been added since
its publication, almost all are endemic and belong to genera
already known from New Zealand ; and as they are divided
in nearly equal proportions between the Australian, South-
American, and North Temperate elements, with a few Ant-
arctic forms, their omission will not change in any appreciable
degree the relative proportions of the flora of the ‘ Handbook.’
* Proc. Linn. Soe. of N. S. Wales, vol. iv. p. 358,
438 Capt. F. W. Hutton on the Origin of the
Indeed, as Mr. G. M. Thomson has pointed out in his inter-
esting address to the Otago Institute last year, “the general
conclusions arrived at in the ‘ Flora Nove Zealandie’ have
not been materially altered by recent discoveries”? *. For the
local distribution of Australian plants, I have Baron von
Miiller’s valuable ‘ Systematic Census’ (1882).
There are in New Zealand 35 subtropical or warm-
temperate genera of flowering plants, which are also found in
South America, and which probably did not pass from one
country to the other by an Antarctic routet, and of these
31 occur also in Australia. These 35 genera contain 74
species, of which 89 per cent. are peculiar to New Zealand.
If now we take the subtropical, or warm-temperate, genera,
which do nof occur in South America, we find that there are
33 of them¢{, of which 31 are also found in Australia. These
genera contain 96 species, of which 93 per cent. are endemic.
There are thus 68 genera which appear to have been intro-
duced from the north, and to these we must add the greater
part, at any rate, of the 41 genera which are confined to
Australia and New Zealand, for 90 per cent. of the New-
Zealand species belonging to these genera are endemic. Mr.
Wallace gives a list of 16 of these genera, which, not occur-
ring in tropical Australia, he supposes must have migrated to
or from New Zealand across the sea; and he says that nearly
all these genera have in their seeds special facilities for trans-
mission. But just as good reasons could be found for showing
that many of his tropical genera have equal facilities for
transmission ; and as 87 per cent. of the New-Zealand species
belonging to these 16 genera are endemic, while of the 33
genera named by Mr. Wallace as having come from the
north, only 72 per cent. of the species are endemic, we must
conclude that the 16 temperate genera have been in New
Zealand as long as the 33 subtropical genera. As a matter
of fact, 15 out of the 16 are found in Queensland; and it is
* Trans. N. Z. Institute, vol. xiv. p. 486.
+ They are Drimys, Aristotelia, Discartia, Dodonea, Sophora, Wein-
mannia, Gunnera, Eugenia, Fuchsia, Passiflora, Sicyos, Eryngium, Oreo-
myrrlis, Griselinia, Loranthus, Viscum, Lagenophora, Pratia, Myrsine,
Sapota, Sebea, Calceqlaria, Grratiola, Vitex, Pisonia, Cassytha, Athero-
sperma, Peperomia, Piper, Libocedrus, Podocarpus, Libertia, Asteha, Cor-
dyline, and Cyperus. Grasses omitted.
t They are Pittosporum, Melicope, Leptospermum, Metrosideros, Meryta,
Coprosma, Stylidium, Cyathodes, Parsonsia, Mitrasacme, Geniostoma,
Mazus, Tetranthera, Knightia, Exocarpus, Santalum, Epicarpurus, Elato-
stemma, Ascarina, Dammara, Dacrydium, Dendrobium, Bolbophyllum,
Sarcochilus, Gastrodia, Corysanthes, Microtis, Lyperanthus, Thelymitra,
Freycinetia, Dianella, Areca, and Gahnia.
Fauna and Flora of New Zealand. 439
more reasonable to suppose that some of the tropical species
have died out in Australia than that all the 16 genera have
crossed the sea, an opinion not shared in by Sir J. Hooker,
or by Mr. T. Kirk*.
Passing on now to the probably antarctic genera, that is
southern genera which have spread east and west in south-
temperate latitudes, we find that they number 20, containing
76 species, of which only 60 per cent. are endemic. Nineteen
of the species are also found in Australia or T’asmania, and
11 or 12 in South America. There are also 56 genera of
north-temperate plants, which probably spread with the
antarctic forms, containing 199 species, of which 67 per
cent. are peculiar to New Zealand. ‘The remaining 87
genera I am unable to place. Most of them belong to two
or more geographical elements, but others—such as Fagus
—are doubtful.
Statistical results like these are always open to the objection
that the data on which they rest are incomplete and more or
less erroneous (for example, Corzaria and Gunnera may
belong to the antarctic element, and Drosera to the South-
American). They also assume that the rate of variation is
equable, which of course cannot be strictly accurate. But
this method of investigation has been used with great success
in geology, and it can, I think, be trusted here for establishing
the two following conclusions:—First, that the northern
immigration, taken as a whole, was anterior to the southern
immigration, also taken as a whole; and second, that the im-
migration of the subtropical South-American genera belongs
to the first period and not to the last. The first conclusion is
similar to that of Mr. Wallace, but arrived at in a different
way. ‘The second is opposed to Mr. Wallace’s idea that the
South-American plants passed through New Zealand and
antarctic lands during a warm Miocene period, which is also
opposed by the fact that a number of Australian genera are
found in South America but not in New Zealand. The fact
that very few of our South-American genera are absent from
Australia, while a large number of our Australian genera are
absent from South America, makes it probable that there have
been at least two migrations into New Zealand from the
north, and that the South-American element belongs to the
first of these only. This is borne out by the distribution of
* See Trans. N. Z. Institute, vol. xi. p. 546.
+ Itake the following as typical :—Colobanthus, Oxalis, Acena, Donatia,
Tillea, Drosera, Apium, Nertera, Abrotanella, Cotula, Forstera, Pernet-
tya, Ourisia, Drapetes, Callixene, Rostkovia, Gaimardia, Carpha, Oreobolus,
and Uneimia.
440 Capt. F. W. Hutton on the Origin of the
some of the groups. ‘The best example perhaps is the Orchids,
of which 18 genera occur in New Zealand. Of these 2 are
endemic, and the other 16 are all found in Australia. Two
occur also in New Caledonia, three in Polynesia, four in the
Indian archipelago, and three in India, while one consists of
a single species widely spread over Asia and Australia. None
of them are found in South America. The path of the Orchids
into New Zealand, by the Indian archipelago and New Cale-
donia, is thus plainly mapped out, and as none have passed
into South America the migration probably took place after
the South-Pacific continent had disappeared. The number
of New-Zealand species of this order 1s 38, of which 32 (or
84 per cent.) are endemic, so that the immigration must have
been an early one. Other examples are found in Pittosporee,
Rutacex, and Santalacee. Hxamples of the earlier South-
American migration are seen in the Monimiacez and Chlor-
anthacez, while examples of the antarctic migration are the
Caryophyllex, the Geraniacee, and the Rutacez. It may be
objected that the percentage of endemic species is greater in
the Australian than in the South-American element, and
therefore that the first must be the older. But the objection
is not fatal, because, in the first place, we must remember that
the American genera would continue to live in Polynesia,
and would migrate into New Zealand again with the Austra-
lian forms, thus making the percentage nearly the same in
each case; and, in the second place, one or two genera may
be included in the South-American element which are really
antarctic, and this would at once bring down-the percentage
of endemic species. ‘This is a mistake which could not be
made with the Australian genera.
The Kermadec Islands occupy a very important position
for furnishing evidence of migrations into New Zealand from
the north, but unfortunately very little is known of their flora.
What is known shows a remarkable affinity to the flora of
New Zealand. Of the 21 species of flowering plants
collected by Dr. Macgillivray, only three (14 per cent.) are
endemic, 17 are found in New Zealand (one of which is
supposed to have been introduced into both places), and the
other (Metrosideros polymorpha) inhabits Polynesia and New
Caledonia. From this we must infer that at a comparatively
late period New Zealand extended further to the north-east
than at present; for if it had not done so the Kermadec
plants would have been far more differentiated from those of
New Zealand than they are. At the same time, as but few
subtropical species are common to New Zealand and Aus-
tralia, this land could not have extended far to the north-
Fauna and Flora of New Zealand. 441
west; but we may perhaps refer to this period the introduc-
tion of several of those tropical species, such as Avicennia
officinalis and Sicyos angularis, which are also found in
Australia.
It would thus appear that there have been three migra-
tions of plants from the north into New Zealand: two of
very ancient date; the third comparatively recent and com-
paratively unimportant. ‘The supposition that New Zealand
was at one time connected with a South-Pacific continent,
from which plants spread into South America and into New
Guinea, and that, at a subsequent period, Hastern Australia
was attached to New Guinea, and received from thence frag-
ments of this Polynesian flora, together with plants of the
Indian archipelago, will explain, I think, why some Poly-
nesian and South-American genera are found in New Zealand
but not in Australia, and why some occur in Australia but
not in New Zealand.
Passing on now to a consideration of our fauna, we find it
composed of the same elements that we recognized in the
flora, viz.—(1) Australian, (2) Polynesian, (3) 5. American,
(4) Antarctic, and (5) North Temperate. The South-Ame-
rican element seems to be the weakest, but until the distri-
bution of our insects, land-mollusca, and land-worms is better
known we cannot speak with any confidence on this point.
One of our two bats was formerly thought to belong to an
American family; but this has been shown to be a mistake,
and it now seems that both are of Old-World extraction.
This removes a difficulty, for bats are certainly not a more
ancient group than birds, and it would have been very
puzzling if their distribution had coincided with that of the
frogs instead of with that of the birds.
Our birds show only three elements :—(1) an Antarctic,
which comprises the penguins, the petrels, three out of five
gulls, and four out of nine cormorants; (2) a Polynesian,
consisting of the paroquets, Aplonis, and the long-tailed
cuckoo; and (3) an Australian, which includes all the rest,
except a few which are cosmopolitan. Of a South-American
element we see no trace except it be in Nestor, which may be
distantly related to the macaws, although still more nearly to
the brush-tongued parrots of Australia and Polynesia. ‘The
Merganser of the Auckland Islands may represent the North-
Temperate element. The affinities of Zurnagra are still
doubtful. I pointed out in 1872* that our land-birds had
been derived from the north, and Mr. Wallace has subse-
* Trans. N. Z. Institute, vel. v. pp. 251, 252.
Ann. & Mag. N. Hist. Ser. 5. Vol. xiii. 29
442 Capt. F. W. Hutton on the Origin of the
quently, but quite independently, arrived at the same conclu-
sion. While, however, Mr. Wallace thinks that the birds
migrated along a land-communication with Northern Australia
in the Cretaceous period, I was, and still am, of opinion that
the fragmentary nature of our avifauna shows that the land
was not continuous, but was interrupted by an arm of the
sea between New Caledonia and the mainland, and further,
that this communication took place in the Eocene and not in
the Cretaceous period. The remarkable fact that both our
cuckoos migrate annually to New Zealand from Australia or
Polynesia indicates, as I explained in my former paper, a
much more recent northern extension of New Zealand, and
this agrees with the evidence given by the flora of the Ker-
madeec Islands. Mr. Wallace refuses to believe that these
birds migrate, and thinks that they retire to some unexplored
parts of the islands in the winter, but unfortunately he gives
no hint as to where these unexplored parts are situated.
Our lizards show an Australian element in Mocoa and
Hinulia; but the genus Nauléinus is endemic and belongs to a
group of geckos found in Abyssinia, India, the Indian arehi-
pelago, Australia, and Chih. Sphenodon belongs to New
Zealand only. Our single species of frog has decided South-
American affinities.
Of the freshwater fishes Hleotris is an Indian-archipelago
and Australian genus, but as it is also found in Mexico and
the West Indies it may possibly indicate a South-American
element ; Galaxias, Chetmarrichthys (an endemic genus allied
to Aphrites), Prototroctes, and the lampreys are Antarctic ;
while the eels are Australian or Polynesian. The marine
fishes are a southward extension of the Indo-Pacific fauna,
with a strong Antarctic element in Bovichthys, Notothenia,
Thersites, Gonorhynchus, Callorhynchus,and perhaps in Geny-
pterus and others.
The land molluscan fauna appears to consist of Australian,
Polynesian, and South-American elements, the latter being
marked by Zornatellina, Amphidoxa, Cyclotus, and perhaps
Strobila.. There is no Antarctic element. In my paper on
the ‘“ Geographical Relations of the New-Zealand Fauna” I
stated that the freshwater shells showed a Polynesian affinity
distinct from the Australian; but in this I was mistaken,
owing to my want of knowledge of the Australian fauna. It
now appears that most of the genera are also Australian ; but
Melanopsis is Polynesian, and Potamopyrgus is said to occur
in South America, The affinities of our freshwater limpet
(Latia) are not known. The marine Mollusca are, like the
Fauna and Flora of New Zealand. 443
marine fishes, a southward extension of the Indo-Pacific fauna
with a well-marked Antarctic element, the South-American
element being but slightly developed. The main point of
interest is the difference exhibited between them and the
marine Mollusca of temperate Australia and Tasmania, shown
chiefly in the absence trom our seas of many common sub-
tropical forms. Tasmania, for example, possesses several
species of Conus, Cyprea, Fasciolaria, and Oliva, of which
we have no representatives. We have but one species each
of the genera Mitra, Columbella, and Nassa; while Tasmania
has respectively 14, 10, and 5 species. We have only 3
species of Voluia and 2 of Marginella, while Tasmania has
7 of the former and 8 of the latter. This great difference is
probably accounted for by the warm south-east current that
flows down the coast of Australia, and the cold south-west
current that sweeps the shores of New Zealand. If, however,
New Zealand was joined to Northern Australia or New
Guinea all this would be changed; the warm current would
pass down its east coast, while the cold current would be
deflected from the west coast of New Zealand to the east coast
of Australia. But the difference in the shells was nearly as
well marked in Tertiary times as now; consequently we must
suppose that New Zealand has been isolated, and that the
warm current has passed down the east coast of Australia
ever since these genera inhabited the districts. Now Voluta,
Mitra, Conus, Fasciolaria, and Cyprea date from the Upper
Cretaceous, the others from the Eocene, and the conclusion
seems plain that New Zealand has not been connected with
Australia since the Cretaceous period, which agrees well with
the inference derived from the fragmentary nature of our
avifauna.
The geographical relations of our insects and spiders are not
yet known, but as the families of insects in many cases date
back to the Jurassic, and several genera to the Cretaceous
period, we may expect to find a marked South-American
element among them; indeed, Mr. Meyrick has, in papers
read to our society, already pointed out that in the Crambidee
the New-Zealand species of Diptychophora are more closely
related to South-American than to the single Australian
species; and that among the Geometrina the genera Azelina,
Drepanodes, and Siculoides are South American, while Tato-
soma is found in Europe, Ceylon, Borneo, Australia, and
South America, the New-Zealand species being nearest to
those of South America. Peripatus is no doubt a very old
form; it is found in South Africa, Chili, Central America,
and the West Indies, and consequently cannot be considered
29%
444 Capt. F. W. Hutton on the Origin of the
as representing an Antarctic element, but must be referred to
the South-American migration.
It is very remarkable that our crayfishes should belong to
the same genus as the species found in Fiji, while those of
Australia and South America are generically distinct, although
all belonging to the same subfamily. This, I think, proves
incontestably that Fiji and New Zealand have had direct
land-communication ; for Prof. Huxley has pointed out that
freshwater crayfishes are very ill adapted for crossmg even a
narrow arm of the sea. Mr. Wallace thinks that this con-
nexion with Fiji “is hardly probable, or we should find
more community between the productions ” of the two coun-
tries ; but when we remember the difference of climate we
cannot expect a greater community than actually exists.
The marine Crustacea agree with the marine fishes and shells
in having well marked Australian and Antarctic elements, but
perhaps it 1s not yet possible to distinguish South-American
from Antarctic forms. It will not be necessary to pass in re-
view the lower classes of animals; but little is as yet known
of them, and at present they throw no new light on the origin
of our fauna.
I will now recapitulate the results we have arrived at about
the New-Zealand flora and fauna. The South-American
element in the fauna and flora, as shown by the plants, frog,
Jand-mollusca, and insects, proves that New Zealand was
closely connected with the South-Pacific continent which pro-
bably existed in Jurassic and Lower Cretaceous times, while
the distribution of the freshwater crayfishes proves that Fiji
and New Zealand have had a continuous land-communication.
The distribution of the marine Mollusca shows that New
Zealand has been separated from all northern lands ever since
the Cretaceous period, and this explains the fragmentary
nature of the avifauna. At the same time, the fact that many
birds, land-shells, and plants, showing no South-American
relations, have passed to New Zealand from the north-west,
proves that these islands, although not actually connected,
must have extended much further north and approached much
more nearly to Queensland and New Guinea at some period
in the Tertiary era than they do now, and that that period
was an early one is shown by the amount of change that has
since taken place in both plants and animals. The flora of the
Kermadec Islands, and the remarkable phenomenon of our
migratory cuckoos, give evidence of a third north-easterly
extension of New Zealand at a much later date; but the
absence of many common types of Australian birds, and the
small number of northern plants and animals specifically
Fauna and Flora of New Zealand. 445
identical with those of Australia, prove that this extension
was much less than the other two, and perhaps did not last
long. It is now necessary to examine the geology of New
Zealand, and see how it bears on the subject.
New Zealand is a mountainous country, partly covered
with forests, and difficult to explore geologically, and the
fossils, although largely collected, have as yet been but little
studied. It is not therefore surprising that many points in
its geology remain uncertain, especially as to the ages to be
assigned to the several rock-systems of which it is composed,
and which, being commonly discontinuous, require the aid of
paleontology for their elucidation more than in most coun-
tries. Nevertheless, thanks to the energy and skill with
which the Geological Survey department has during the last
twenty-two years attacked the problem, I think [ am safe in
saying that the main structure of thé country is tolerably well
known, especially in those points which alone concern us
here, and which [ will briefly mention.
The main range forming the New-Zealand Alps in the
South Island, and the mountains stretching from Wellington
towards the East Cape in the North Island, is composed of
highly-inclined sedimentary rocks belonging to four, or per-
haps five, distinct systems. The first is probably Archean or
Cambrian. According to Dr. Hector the second is Ordovi-
cian, the third Silurian and Lower Devonian, the fourth Upper
Devonian and Lower Carboniferous, while the fifth ranges
from Permian to Jurassic. ‘This last system contains fossils
related to those from the Gondwana system of India and the
newer Carbonaceous system of Hastern Australia. According
to Mr. 8. H. Cox, it is about 21,000 feet in thickness, and is
entirely a littoral formation, plant-remains being found all
through it; thus implying a subsidence of 3500 fathoms in
early Mesozoic times. ‘The axis of the geanticlinal, however,
is not in the centre of the range, but lies along its western
base, the whole western portion of the elevated mass having
been removed by denudation, except in the west part of
Nelson and the north part of Auckland. Of the rest, all that
remains is the submarine plateau which stretches out towards
Australia.
The next system of rocks is of Cretaceous, probably Upper
Cretaceous, age*. Along the eastern base of the main range
it lies quite unconformably on the Jurassic and older rocks,
and, according to Dr. Hector and Dr. von Haast, it is also
* Dr. Hector considers the oldest beds to be the equivalent of the Lower
Greensand of England.
446 Capt. F. W. Hutton on the Origin of the
found in a similar position on the west coast of the South
Island: thus lying at a low level on the geanticlinal axis.
In the North Island the geanticlinal axis is covered by thick
masses of Tertiary sedimentary and volcanic rocks, which
hide the Cretaceous system if it exists there. Evidently a
great upheaval, followed by enormous denudation, must have
taken place immediately before the deposition of this last
rock-system, that is at the close of the Jurassic and com-
mencement of the Cretaceous periods. There may be some
doubt as to the exact time of this upheaval, but that the New-
Zealand Alps were principally formed during the periods
mentioned is unquestionable.
The Cretaceous, or according to Dr. Hector the Cretaceo-
Tertiary, system has also been much disturbed in places, and
is everywhere denuded, and generally overlain unconform-
ably by beds of Oligocene and Miocene age. This proves
that a second elevation, probably of less extent than the first,
took place in the Eocene period, and was followed by a second
depression in the Oligocene. The Oligocene and Miocene
marine rocks are largely developed, and extend to a height of
2500 feet above the sea*, proving conclusively that during
this period New Zealand was represented by a cluster of
twenty or more islands, on which, as I pointed out in 1872,
the various species of moa were probably developed+. Since
that time a third elevation has taken place, the proofs of which
I must defer to another opportunity. ‘These three elevations
agree quite with the conclusions already arrived at by a study
of the fauna and flora; and we must suppose that it was”
during the Upper Jurassic or Lower Cretaceous period that
New Zealand was joined to the South-Pacitie continent,
while during part of the Hocene it extended towards New
Caledonia, and again in the Pliocene towards the Kermadec
Islands.
Our general results, then, are that in early Mesozoic times
New Zealand, Eastern Australia, and India formed one biolo-
gical region, land probably extending continuously from New
Zealand to New South Wales and Tasmania. At the close
of the Jurassic period the New-Zealand Alps were upheaved,
and the geosynclinal trough between New Zealand and Aus-
* According to Dr. von Haast they ascend to 5000 feet above the sea,
but is localities are given (‘Geol. of Canterbury and Westland,’ 1879,
_ 805).
+t Mr. Wallace agrees with this opinion, but in his ‘Island Life’ says
that it is a pure hypothesis, of which we have no independent proof; he
not, as I suppose, being aware of the distribution of our Miocene rocks,
although I mentioned it in my paper (see Trans. N. Z. Inst. vol. vy.
p. 253).
Fauna and Flora of New Zealand. 447
tralia was formed. During the Lower Cretaceous period a
large Pacific continent extended from New Guinea to Chili,
sending south from the neighbourhood of Fiji a peninsula
that included New Zealand. Nearly all the southern part
of America was submerged. Western Australia and Eastern
Australia formed two large islands lying at some distance
from the continent. This continent supported dicotyledonous
and other plants, insects, land shells, frogs, a few lizards, and
perhaps snakes and a few birds, but no mammals. In the
Upper Cretaceous period New Zealand became separated and
reduced to two small islands; the South-Pacific continent
divided in the middle between Samoa and the Society Islands,
and (the eastern portion being elevated while the centre sank)
it ultimately became what we know now as Chili, La Plata,
and Patagonia. In the Hocene period elevation commenced
in our district; Eastern Australia was joined to New Guinea,
which stretched through New Britain to the Solomon Islands,
New Zealand was also upheaved and extended towards New
Caledonia, but the two lands were divided by an arm of the
sea. ‘The mainland of ‘New Guinea had by this time been
invaded from the north by a large number of plants, birds,
lizards, snakes, &c., which migrated south into Eastern Aus-
tralia, and a few passed over the New-Caledonia channel and
reached New Zealand. Butstill nomammals. In the Oligo-
cene period New Zealand again gradually sank, carrying with
it the sparse flora and fauna it had received, and in Miocene
times was reduced to a cluster of islands, Eastern Australia
all this time receiving constant additions to its fauna and
flora through New Guinea. Jn the Pliocene period elevation
once more took place; New Zealand extended towards the
Kermadec Islands, and the continent of Australia was formed ;
after which subsidence again occurred in the New-Zealand
area.
These conclusions are more precise, but are much the same
as those at which I arrived in 1872, with the exception
that I now substitute a South-Pacific continent from which
Australia was isolated, for the Lower Cretaceous Antarctic
continent of my former paper. Mr. Wallace’s hypothesis of
an isolated West-Australian continent on which the charac-
teristic Australian flora and mammalian fauna were developed
is fairly satisfactory, but I presume that the Australian birds
are not supposed to belong to the West-Australian fauna. A
few, such as the ancestors of the honey-suckers and the brush-
tongued parrots, may have crossed over the sea from New
Guinea to Western Australia, but the mass of the birds are
supposed to be Kast-Australian, to have passed into West
448 My. J. W. Davis on a new
Australia by the north while the continent was being upheaved
and its climate still humid, and to have become differentiated
since the entire drying up of the interior sea so desiccated the
country as once more to isolate West Australia almost as
effectually as if it were surrounded by water. But Mr.
Wallace does not make this sufficiently clear. When, how-
ever, we come to that part of Mr. Wallace’s hypothesis which
deals with the connexion between Australia and New Zealand
we find it to be not so satisfactory. In the first place, the
facts of geology are against any connexion having taken
place between the two countries at the time supposed. In
the second place, the South-American element in the fauna
and flora is not separated from the Antarcticelement. In the
third place, the hypothesis fails to expla the South-A merican
element, except on the supposition of large extensions of land
during the warm Miocene period, for which there is no suffi-
cient evidence, and which if it had oecurred would have
allowed birds as well as frogs and land-shells to pass. And
in the fourth place, it ignores altogether the special relation
which exists between New Zealand and some of the islands
in the Pacific. The hypothesis here proposed is no doubt
incomplete, and will be much improved when the paleon-
tology of New Zealand is better known; but it does, [ think,
give a fairly satisfactory account of the origin of the South-
American, Australian, and Polynesian elements in our fauna
and flora. The Antarctic and North-Temperate elements still
remain for consideration; but so wide a subject cannot be
entered upon at the end of an address, and I must postpone
all discussions to some future occasion.
XLIX.—Deseription of a new Genus of Fossil Fishes from
the Lias. By James W. Davis, F.G.S. &e.
[Plate XVI]
Genus LissoLepis, Davis.
Class Pisces. Subclass PaLarcuTuyrs. Order GANorDeEt.
Suborder ACIPENSEROIDEL Family Patzoniscip zm.
Body fusiform; head large; gape wide; jaws elongated,
furnished with closely-set uniform enamel-tipped teeth ; scales
of medium size, rhomboidal, mostly with smooth surface, a few
anterior ones with slight furrows, posterior margin serrated ;
Genus of Fossil Fishes from the Lias. 449
pectoral fins large and broad; ventral fin smaller; anal fin
largest; caudal fin equilobate heterocereal. Notochord
persistent.
Lissolepis serratus, Davis.
The specimen of fossil fish which forms the subject of the
observations following, presents several peculiar features which
render it worthy of careful study. For the most part it is
beautifully preserved, the only part wanting being the pos-
terior portion of the dorsal margin of the body along with the
dorsal fin. The bones of the head to a large extent, the
scales, the pectoral, ventral, anal, and caudal fins remain un-
disturbed. The entire length between the snout and the
extremity of the caudal fin is 8-2 inches; of this length the
head occupies 2°6 inches, or about one third the entire length,
The greatest depth is between the ventral fin and the dorsal
surface, where it is 2°2 inches. ‘The cranial bones are strong,
covered with enamel, the surface of which is ornamented
with numerous pustulations, somewhat irregular in form.
The superior portion of the orbit is well defined and pro-
minent. ‘The orbit is comparatively small, placed about
equidistant between the upper jaw and the roof of the cranium,
and ‘7 inch behind the snout. The jaws are large, capable
of wide expansion, and armed with closely-set, sharp, conical
teeth, curved slightly inwards, their points capped with
enamel. The mandible is 1°6 inch in length; it is slightly
expanded in front near the symphysis ; its median portion is
somewhat attenuated, whilst posteriorly the bone becomes
deeper and stronger. ‘The maxilla is large; its posterior
portion has been slightly displaced and damaged, and is
consequently obscure ; but it appears to have had a tolerably
wide expansion towards the orbit. ‘Che premaxillary bone
is ‘3 inch in length, and has attached to it a number of teeth
similar to those on the maxilla and mandible. The operculum
is more or less rounded, except on the anterior margin,
which presents a concave outline ; attached to its lower surface
there is an interopercular bone; it is about one half the size
of the operculum, and probably extends to form a connexion
with the branchiostegal rays, of which there are some indica-
tions below the mandible. A series of clavicular bones extend
posteriorly behind the opercula. The lower portion of the
external covering of the head is removed, and the scapula,
contiguous to the pectoral fin, is exhibited. ‘The operculum is
enamelled and covered with punctures; tiie interoperculum
presents similar characters. The frontal and ethmoid bones
do not project beyond the premaxillaries ; they are strongly
450 Mr. J. W. Davis on a new
coated with ganoine, their surface ornamented with vermi-
culate ridges.
The surface of the body is covered with thickly-enamelled
rhomboidal scales ; the scales along the lateral line are larger
than those above or below, and largest near the head, where the
height of each scale is double the breadth; nearer the tail the
scales are more nearly equilateral. They are arranged in
rows, with a slightly sigmoidal curvature backwards from the
dorsal towards the ventral surface of the fish. The number
of scales in each row varies from twenty-eight in the deepest
part of the fish to fourteen near the caudal extremity. Along
the flank, on each side of the lateral line, the scales are also
arranged in rows antero-posteriorly ; but this does not hold
good for more than four or five rows, the arrangement towards
both the dorsal and the ventral aspect being more or less
indeterminate. Dorsally the scales are smaller, but in front
of the dorsal fin they are higher than broad; on the ventral
portion they are broader than the median ones, the height
being only about one third the breadth. The posterior mar-
gin of each scale is finely serrated, as represented in Pl. XVI.
fig. la. The surface in the large majority is smooth; a
few scales nearest the head are slightly striated with minute
furrows. The posterior margin of the scales becomes gradually
less serrated towards the caudal extremity, and those behind
the anal fin are devoid of serrations and quite smooth. ‘The
body-scales extend 1 inch beyond the fork of the tail over its
upper lobe; they are irregular in form; those in contact
with the fin-rays are much elongated.
The dorsal jin is absent, and there is nothing to indicate
its exact position. ‘The pectoral jins are both preserved in
this specimen ; they are large, a little more than 1:2 inch
in length. There are twenty rays in each, which for a
distance of 5 inch remain simple and unarticulated ; beyond
that distance the rays bifureate, and in several instances, if
not in all, the bifurcations dichotomize towards the outer
margin of the fin. The bifurcated rays are composed of
numerous joints, divided by transverse articulations. ‘The
anterior rays of the fin are the longest and the strongest ;
there is no appearance of fulcral rays. The ventral fins are
situated 1°7 inch behind the pectoral fins. In this speei-
men the fin is folded and extends along the side of the
fish; it is ‘9 inch in length. The anterior rays are very
strong, and at the base a number of large black enamelled
fulcra are situated. The anal fin is situated 1°5 inch in
front of the tail; it is larger than the pectoral or ventral fins,
being 1°3 inch in length. The anterior rays are the longest
Genus of Fossil Fishes from the Lias. 451
in this fin as in the others, and along the front of the anterior
ray there is a number of strong fulcral scales. The basal
portion of each ray is grooved and smooth for about a quarter
of an inch, beyond which the rays are articulated at short
intervals and dichotomize freely. The caudal fin is large,
bifurcated, heterocercal, and equally lobed. The vertebral
column extends at least an inch beyond the termination of
the body into the upper lobe of the tail, and the surface is
covered with enamelled scales to an equal distance; from the
osterior margin spring sixteen rays, which are articulated
and freely dichotomize. ‘The ventral surface of the body
from the anal fin to the root of the tail is protected by a series
of large enamelled plates, which assume a fulcral aspect near
the commencement of the lower lobe. The rays of the lower
portion of the fin are stronger than those above, and are 1°6
inch in length. They are articulated at short intervals, and
each ray dichotomizes ; the external ones begin to divide
at about 1 inch from the base, and only divide once, whilst
those shorter and nearer the centre of the lobe divide into
four, and, in a few cases, into six fine-jointed rays. The
margin of the lobe is bordered by a row of small obliquely
arranged slender fulcra.
This ichthyolite, as already described, possesses many
strongly marked characters, the most prominent being the
extremely long jaws and wide gape, the sculptured surface-
enamelled plates for the protection of the head, the anteriorly
situated orbit, and the well-developed clavicles. The rhombic
scales beautifully imbricating, with serrated posterior margins
and smooth surface ; wide along the lateral line, very narrow
ventrally. Pectoral and ventral fins paired, the former very
large, composed of frequently- -dichotomizing closely-set rays.
Single and large anal fin. Heterocercal tail with vertebral
prolongation into the upper lobe ; the lower lobe, as well as
the anal and ventral fins, having a series of fulcral scales
along the anterior margin. ‘These characters indicate its
relationsbip to the family Paleoniscide, as defined by Dr.
Traquair*. Of the twenty-two genera included in this
family by that author four have been obtained from the Lias,
the remainder occurring in the older strata of the Permian
and Carboniferous rocks. The four genera from the Lias are
Centrolepis, Egerton; Oxygnathus, Egerton; Cosmolepis,
Agassiz; and Thrissonotus, Agassiz.
The genus Thrissonotus was instituted by Agassiz T for the
accommodation of a fossil fish intermediate between Sauropsis
* Paleontographical Society, vol. xxxi. (1877),
+ Rech. sur les Poissons fossiles, vol. ii. pt. 2, p. 128.
452 Ona new Genus of Fossil Fishes from the Lias.
and Thrissops, having the dorsal fin situated in the middle of
the back and the anal fin extended backwards, as in the latter
genus. The specimen was in the collection of Lord Ennis-
killen, and is now at the museum in Cromwell Road. It is
from the Lias at Lyme Regis, and was named 7. Colet.
The specimen has since been figured and fully described by
Sir P. Egerton in the ‘ Decades’ of the Geological Survey
(decade ix. pl. u.).. The dorsal fin corresponds in position to
those of Oxygnathus. ‘The scales are comparatively small,
more or less rhomboidal in form, ornamented by raised ridges,
and with a smooth posterior outline, in this respect differing
from the specimen now under description. The anal fin is
remarkably extended, measuring 1°75 inch along the base
and containing fifty or sixty rays.
The genus Cosmolepis was established by Agassiz in MS.
for a single specimen in Lord Enniskillen’s collection from the
Lias of Barrow-on-Soar. ‘The scales resemble those of Thris-
sonotus, except that they are smaller in proportion to the size
of the fish, there being about sixty in a dorso-ventral row,
and their surface is more thickly ornamented by raised lines
of the enamel. The anal fin is extended, though not so far as
in Thrissonotus. ‘The fin-rays are divided transversely into
numerous ossicles. ‘The genus is fully described by Egerton
in decade 1x. pl.i. of the Geological Survey. -
The third genus of the Paleoniscide of ‘Traquair occurring
in the Liassic formation is Oxygnathus, described and illus-
trated by Sir P. Egerton in the eighth decade of the Geolo-
gical Survey, pl. ix. Itis a long and gracefully slender fish,
with numerous small scales ornamented with oblique ridges
similar to those of the two genera previously mentioned.
The jaws are furnished with numerous small incurved teeth
intermixed with larger ones. ‘The most characteristic feature
rests in the form of the tail, which is deeply cleft into two
lobes, the upper one measuring 3°5 inches in length, the lower
one only 2°5, the fish measuring 11 inches from the snout to
the fork of the tail. The upper lobe ‘has a scaly invest-
ment from the base to the extremity, below which issues a
fringe of innumerable fine rays, with frequent transverse
articulations and longitudinal bifurcations: the lower lobe
contains about twenty-four rays ; of these the strongest occupy
the middle of the lobe, those of the upper and lower margins
becoming gradually finer as they recede from the centre” (see
supplement to decade vui.). The teeth of the genus Centro-
lepis, EXxgerton (decade ix. pl. v.) are similar to those of Oxy-
gnathus. 'The scales are very thick, their exposed surface
covered with coarse rug, arranged, not as in the other genera
mentioned, in a longitudinal direction, but transversely.
On the ‘Challenger’ Neuroptera. 453
The specimen now described, whilst it agrees in family
characteristics with the genera mentioned above, differs consi-
derably in those less important peculiarities which constitute
their generic features. In each instance the size and orna-
mentation of the scales is distinct from this one, and the speci-
men now described is also more especially divergent from
Thrissonotus and Cosmolepis in the non-extension of the anal
fins. There are no intermediate small teeth, as in Centrolepis
and others; and the deeply forked caudal fin, with its long
upper lobe invested to its extremity with scales, is a cha-
racter which readily distinguishes Oxygnathus, and separates
this specimen from that genus. Hence there appears to be
no alternative but to form a new genus under the title Ldsso-
lepis, with the specific designation serratus.
Locality. Lias, Lyme Regis.
EXPLANATION OF PLATE XVI.
Fig. 1. Lissolepis serratus, Davis. Natural size.
Fig. 1 a. Scales, enlarged.
L.—On the Neuroptera collected during the recent Expe-
dition of H.M.S. ‘Challenger.’ By W. F. Kirpy, Assis-
tant in Zoological Department, British Museum.
TuE Neuroptera collected during the voyage of the ‘Chal-
lenger’ were not very numerous, but included several inter-
esting species. | With the exception, however, of a small
series from the Philippines, which were sent home in papers,
the greater number were destroyed by having been placed in
_ spirit—a means of preserving insects which is just as ill
adapted for large-winged insects, like dragonflies, as it is for
soft-bodied or hairy insects, which should always be preserved
dry.
I have only ventured to describe one new species from
Tongatabu.
NEUROPTERA.
ISOPTERA.
Termitide.
1. Termes fatalis (?).
Termes ae Kon, Schrift. Berl. nat. Freunde, iv. p. 1, pl. i. figs. 1-9
ANE
oe fatalis, Hag. Linn, Ent. xii. p, 143 (1858),
Philippines.
A54 Mr. W. F. Kirby on the
The head is darker and more deeply impressed in front than
in other specimens of 7. fatalis in the British Museum.
2. Hutermes fumipennis.
Termes fumipennis, Walker, List Neur. B, M. iii. p. 6525 (1853).
Wellington, New Zealand.
A well-known Australian species.
ODONATA.
Libellulide.
DIBELLULINA.
3. Pantala flavescens.,
Libellula flavescens, Fabr. Ent. Syst. Suppl. p. 285 (1798).
Malamani, Philippines, Feb. 1875; Tongatabu, July 1874;
Queensland.
An almost cosmopolitan species out of Kurope, although
its claims to be considered European rest solely upon a
single reputed British specimen of very doubtful origin (cf.
M‘Lachlan, Ent. Monthly Mag. xx. p. 256, April 1884).
4. Neurothemis palliata.
Polyneura palliata, Ramb. Névr. p. 129 (1842).
Amboina, Oct. 1874; Pasananca, near Zamboanga, Philip-
pines, Feb. 1875.
5. Neurothemis apicalis.
Libellula apicalis, Guér. Voy. Coq., Zool. (2) 11. p. 194 (1830),
Polyneura apicalis, Ramb. Névr. p. 127 (1842),
Ayu.
6. Neurothemis elegans.
Libellula elegans, Guér, Voy. Coq., Zool. (2) ii. p. 194, pl. x. fig. 8
(1830).
Philippines; also Ki Dulan, Sept. 25, 1874.
One specimen from the Philippines exactly agrees with N.
elegans. A second is reddish brown, nearly to the pterostigma,
which is reddish, the tips of the wings and the whole border
of the hind wings being hyaline.
The best authorities regard the three forms of Neurothemis
here mentioned as hardly entitled to the rank of distinct
species.
7. Agrionoptera pectoralis.
Lnbellula pectoralis, Brauer, Verh. zool.-bot. Ges. Wien, xvii, p. 19
(1867).
Philippines.
‘Challenger’ Neuroptera. 455
Agrees very fairly with the description, except that Brauer
gives 17-19 antecubital and 12 postcubital nervures. This
specimen has only 14 antecubitals on both fore wings, and 11
posteubitals on the right fore wing and 12 on the left.
8. Lepthemis sabina.
Lrbellula sabina, Drury, I. Ex. Ent. i. pl. xlviii. fig. 4 (1773).
Philippines.
A rather small specimen.
9. Diplax pacificus.
Male.—Exp. al. 1 unc. 10 lin.; long. corp. 1 une. 1§ lin.
Wings hyaline, rounded; fore wings rather narrow ; hind
wings slightly stained with yellow at the base, and consider-
ably expanded between the base and the nodus. Nervures
black, pterostigma yellowish brown. Fore wings with 8
antecubital nervures of the costal series and only 7 of the
subcostal series, and 7 postcubital nervures of the costal
series and 4 of the subcostal before the pterostigma; hind
wings with 6 antecubital and 7 posteubital nervures; in the
second series only the last 4 of the latter; triangles ordinary,
that of the fore wings with the basal side rather shorter than
the outer; the dividing line slightly oblique. Body testa-
ceous yellow. Head: middle ocellus red, placed in a deep
depression ; epicranium emarginate above, vertex convex ;
clypeus (which is semicircular and with two indentations in
front), labrum, and sides of epicranium paler yellow than the
rest of the head ; prothorax quadrifid, the frontal lobes trans-
verse, each marked with a large black spot, the hinder ones
contiguous, being less distinctly separated ; mesothorax rather
long, with two large black spots in front, almost concealed by
the junction with the prothorax ; a deep longitudinal depression,
with a narrow keel in the middle; the lateral sutures slightly
marked with black at two or three points. Abdomen with a
longitudinal keel on the back, which is reddish brown beyond
the second segment, and marked somewhat irregularly with a
series of square spots, chiefly towards the ends of the seg-
ments ; there is also a dark line on the ventral surface, and a
series of 4 or 5 irregular long and partly connected reddish-
brown spots on the sides of the middle segments. Legs
yellowish, the four hinder ones black above; spines strong ;
claws very large and slightly bifid.
Anal appendages as long as the two preceding segments,
pointed ; lower appendages broad and a little shorter.
Tongatabu, July 1874.
456 Mr. W. F. Kirby on the
Agrionida.
A GRIONINZE.
10. Ischnura aurora.
Ayrion (Ischnura) aurora, Brauer, Verh. zool.-bot. Ges. Wien, xv.
p- 510 (1865).
Waihiri, Tahiti, Sept. 1875.
CALOPTERYGINA.
11. Vestalis melania.
Vestalis melania, De Selys, Bull. Acad. Belg. (2) xxxv. p. 474 (1873),
(2) xlvii. p. 360 (1879).
Philippines.
The brilliant blue of the male (sometimes shading into
greenish, especially towards the base) and the rich purplish
violet of the more highly coloured females render this species,
which was not previously in the British-Museum collection,
one of the most beautiful of the Odonata.
PLANIPENNIA.
Myrmeleontide.
12. Myrmeleon variegatus.
Myrmeleon variegatus, Klug, Symb. Phys. pl. xxxv. tig. 4 (1834).
Common in July and August at St. Vincent and St. Jago,
Cape Verdes, along with its larva from the former locality.
It was previously known from 8. France and Arabia.
LI.—On the Diptera collected during the recent Expedition of
H.M.S. ‘Challenger. By W. F. Kirpy, Assistant in the
Zoological Department, British Museum.
THE collection of Diptera formed was not very extensive, but
contained several interesting species, three of which are here
described as new. The capture of a species of Tachininaw,
originally described from the Red Sea, in the Cape-Verde
Islands is very remarkable.
‘Challenger’ Diptera. 457
Stratiomyide.
SArGIna.
1. Sargus spinigera.
Xylophagus spiniger, Wied.
Beris Servillet, Macq. Dipt. Exot. i. (1) p. 172, pl. xxi. fig, 1 (1838).
Sydney, May 1874.
Tabanide.
TABANINE.
2. Tabanus fulvipes, var. (?).
Tabanus fulvipes, var.?, Phil. Verh. zool.-bot, Ges. Wien, xv. p. 723
(1865).
Messier Channel, Patagonia, January 1876.
Four female examples of a species allied to T. magellanicus
and fulvipes, Phil. 7. fulvipes, with which (judging from
the description) they may possibly be identical, is a Chilian
species.
Panqoninz.
3. Chrysops aterrimus.
Long. corp. 5 lin.
Female.—Inky black, very shining ; head, thorax, and the
basal half of the antenne clothed with short black hair; eyes
dull black ; wings hyaline, but more or less broadly brown
along the costa. The brown shade covers the whole costal
portion of the wing, from the base as far as the point where
the third longitudinal vein branches; it is then continued
narrowly along the costa to just beyond the third vein, being
distinctly thickened on the second and third veins. The
discoidal cell is almost clear, but the fourth submarginal
cell is clouded. From the extremity of the discoidal cell,
and below the third longitudinal vein, from a point just before
the fork, the brown coloration extends around and above the
whole of the discoidal cell, almost as far as the posterior
intercalary vein, just before which it ceases, although it runs
along the anterior intercalary vein almost to the hind margin.
Eucosca Dock, Japan, May 1875.
Allied to various North-Ainerican species, such as C. niger,
Macq., sepulchralis, Fabr., carbonarius, Walk., &c., from
which it is easily distinguished by the different pattern of
the wings. ‘The single specimen from Kucosca Dock being
Ann, & Mag. N. Hist. Ser. 5. Vol. xin. 30
458 My. W. F. Kirby on the
damaged, I have described the species from two perfect speci-
mens from Yokohama, collected by Mr. Jonas.
Bombyliide.
ANTHRACINE:.
4. Anthrax Tantalus.
Anthrax Tantalus, Faby. Ent. Syst. iv. p. 260 (1794).
Amboina.
A small specimen, with a brilliant violet iridescence. It
most resembles a specimen from Celebes in the British-
Museum collection.
5. Anthrax bombyliformis.
Anthrax bombyliformis, Macl. King’s Surv, Coasts Austr. ii, p. 468
(1827).
Cape York.
Asilide.
DaAsvPoGonInz.
6. Dasypogon diversipes.
Length 53-74 lines; expanse 10 lines.
Black ; thorax dusted with yellowish white on the borders,
with three slightly raised reddish longitudinal lines near the
middle, the interspaces being entirely black. Beyond this the
front half of the mesothorax is yellowish white (the inner-
most part being very bristly, which gives it a dusky appear-
ance), but the hinder part is only of this colour on the borders
and along a transverse median line. Head yellowish; pro-
boscis, antenne, and a line on the vertex black ; scutellum
and halteres yellow, a yellowish spot on each side of the back
of the metathorax ; under surface of thorax clothed with
yellowish hair. Abdomen rather long, black, with con-
spicuous pale yellow spots, diminishing in size, on the sides of
all the segments except the two last near the extremity ;
under surface clothed with yellowish hair, but less densely
than the thorax ; coxe reddish, densely clothed with yellowish-
grey hair; femora red, trochanters and tips of knees black ;
tibie yellow, with black bristles, tip broadly black above ;
tarsi black above and testaceous beneath; basal half of first
joint yellow. Wings brownish hyaline, with chestnut-
coloured nervures.
Sydney, May 1874.
‘Challenger’ Diptera. 459
LAPHRIIN”,
7. Laphria consobrina.
Laphria consobrina, Walk. Journ, Linn. Soc., Zool. iv. p, 84 (1860).
Aru.
Muscide Calyptere.
T'acurninZ.
8. Echinomyia Micado.
Length 6 inches.
Male.—Superficially resembles H. fera, Linn. Head dull
yellow ; eyes and ocelli red, the latter on a black prominence
near the occiput, bounded by the branches of a reddish Y-
shaped depression, between which and each eye is a long
black oval stripe ; antenne red, club black, spatulate; thorax
blue-black above and dull black below; the shoulders and a
narrow space at the base of the wings reddish; scutellum
more distinctly red. Abdomen reddish, with yellowish shades
towards the sides; a blue-black stripe, narrowing behind, on
the middle of each segment, but ceasing about the middle of
the fourth segment; abdomen beneath dull black in the
middle, with each segment edged behind with a yellowish
line. Wings dull hyaline, tinged with yellow at the base,
the veins yellow except towards the tip, where they are
blackish; alule ivory-white. Legs reddish; femora black
nearly to the tip, especially above; all the bristles black,
except the hair on the cheeks, which is partly yellowish;
proboscis reddish, partly black in the middle.
Kobé, Japan.
9. Gonia (?) guttata.
Gonia (?) guttata, Walk. Entomologist, v. p. 341 (1871).
St. Vincent, Cape Verdes, July 1873.
Originally described from ‘Tajora (Straits of Bab-el-Man-
deb!). The specimen from St. Vincent does not appear to
differ from the type.
10. Masicera prominens (?).
? Masicera prominens, Walk. Journ. Linn. Soc., Zool. v. p, 155 (1861).
Aru.
30*
460 Mr. H. B. Guppy on Coral-soundings
Muscide Acalyptere.
Micropezina.
11. Calycopteryx Moseleyt.
Calycopteryx Moseleyi, Eaton, Ent. Month. Mag. xii. p, 59 (1875);
Verrall, Phil. Trans. clxviii. p. 259, pl. xiv. figs. 1 a-e (1879).
Royal Sound, Graves Island, Kerguelen, Jan. 19, 1874 ;
Heard Island, Feb. 6, 1874.
Epryprina.
12. Amalopteryx maritima.
Amalopteryx maritima, Eaton, Ent. Month. Mag. xii. p. 58 (1875) ;
Verrall, Phil. Trans, clxviii. p. 241, pl. xiv. fig. 2 (1879).
Heard Island, Feb. 6, 1874.
BorzBorina.
13. Anatalanta aptera.
Anatalanta aptera, Eaton, Ent. Month. Mag. xii. p. 59 (1875) ; Verrall,
Phil. Trans, clxviii, Pp: D44, pl. xiv. fig. 4 (1879),
Heard Island, Feb. 6, 1874 ; Betsy Cove, Kerguelen Land,
Jan. 10, 1874.
Bibionide.
14. Libio Maret, var.
Tipula Maret, Linn. Syst. Nat. ed. x. vol. i. p. 588 (1758),
Eucosea Dock, Japan, May 1875.
The wings appear to be darker and the thorax duller than
in European specimens; but I will not venture to separate
the Japanese form as a distinct species.
15. Plecia fulvicollis.
Penthetria fulvicollis, Wied. Dipt. Exot. p. 31 (1821).
Aru.
LII.— Coral-soundings in the Solomon Islands.
By H. B. Guppy, M.B., Surgeon H.M.S. ‘ Lark.’
Tue following observations were made in different localities
of the Solomon group during 1882 and 1883.
1. Selwyn Bay, on the west side of Ugi Island.—The
in the Solomon Islands. 461
shore-reefs which fringe this island attain their greatest
width on the weather or east side, where they receive the
brunt of the trade-swell. On the lee side, however, around
the shores of Selwyn Bay, corals thrive in considerable pro-
fusion ; and here my soundings were taken. Out of fourteen
casts in depths less than 25 fathoms and more than 5 fathoms,
sand was only brought up on the arming on two occasions;
whilst out of fifteen casts in depths beyond 25 fathoms and
extending to 50 fathoms, there was only one instance, viz.
a cast of 26 fathoms, in which sand or gravel was not found
on the arming. On examining the results of the four lines
of soundings which I took, I am inclined to place the limit
of depth at which coral thrives in this bay at between 20 and
25 fathoms. The branching Madrepores and corals of the
genus Serdatopora appeared from the broken fragments
brought up in the arming to have a vertical range extending
through the whole zone of coral-growth; the Madrepores,
however, apparently lived under more favourable conditions
in the shallower water; whilst the Sertatopore* seemed
to prefer the lower limits of the zone. This accords with
Mr. Darwin’s experience on the leeward coast of Mauritius
(‘Coral Reefs,’ 1842, p. 81).
2. Port Mary, on the west side of Santa-Anna Island.—
This small island, which les off the eastern extremity of
St. Christoval, is an upraised coral-atoll, about 450 feet in
height, and completely girt by shore-reefs which on the west
side of the island almost enclose a large circular lagoon known
as Port Mary. My soundings were taken off the outer edge
of the reef enclosing this harbour. ‘They extended to depths
of between 70 and 80 fathoms, and included sixty-three casts.
The conclusions to be deduced from the indications given by
the arming of the lead may be briefly stated. The most
favourable conditions for the growth of coral existed in depths
less than 12 fathoms. Down to 20 fathoms living coral
flourished, but in less profusion. Beyond that depth sand
and gravel were more frequently brought up on the arming,
and a depth varying between 20 and 30 fathoms represented
the lower limit of the coral-zone. From the absence of
branching corals, no fragment of living coral was brought up
during the soundings. In only one cast was I able to recog-
nize the nature of the coral from the form of the impression,
when, from a depth of 17 fathoms, the arming preserved the
prints of the large cells of one of the Astreide. From ex-
perimental observation I have found that in the majority of
soundings the unavoidable swaying of the lead renders the
* Probably a new species.
462 Mr. H. B. Guppy on Coral-soundings
impression difficult to recognize. In section 1, I have shown,
drawn on the true scale, the seaward slope of that part of the
reef at which the soundings were taken. For the first 100 to
150 yards from the edge of the reef the submarine slope was
somewhat gradual until a depth of about 16 fathoms was
reached, when, within a distance of two boats’ length, the
Sections showing the Seaward Slopes of Reefs in the Solomon group.
(Drawn on a true scale to the 100-fathom line, 5 inch=100 feet.)
Section 1.—Port-Mary Reef, Santa Anna.
Sea-level,
MQ WY :
Section 2.—Reef of Onua Islet, Shortland Islands.
Sea-level.
Section 3.—Barrier-reef of Choiseul Bay.
WM
soundings suddenly increased in depth by about 100 feet,
or another 16 fathoms. rom the foot of this declivity there
was an easy descent for about 450 yards, with a fall of some
50 or 60 feet, terminating in a precipitous slope where
there was a drop of about 25 fathoms or 150 feet. The
submarine slope beyond descended at a moderate angle to
considerable depths. Ihave, however, terminated this section
Sea-level.
in the Solomon Islands. 463
at the 100-fathom line, having no reliable information of the
greater depths. Santa Anna, [ should add, rises out of deep
water, where 200 fathoms of line have failed to reach the
bottom.
3. The Reef of Onua Islet—This islet is one of a group of
islets and small islands situated on a broken line of barrier-
reef which skirts the weather or south-east border of the
Shortland Islands. My soundings were taken off the weather
edge of this reef in a ‘Rob Roy’ canoe, and considerable
caution had to be exercised in the shallower depths on account
of the uncertain behaviour of the rollers. From a series of
soundings between the depths of 6 and 33 fathoms, it would
appear that the lower limit at which coral thrives on the sea-
ward slope of this reef is about 20 fathoms. Beyond that
depth the arming was thickly coated with sand and gravel,
Section 2 shows on a true scale the submarine contour of this
reef where the soundings were taken. Tor the first 100 yards
from the edge of the reef-flat there was a gradual descent
until a depth of 5 or 6 fathoms was reached, when there was
a rapid fall of from 10 to 15 fathoms, followed by a moderate
slope to the 100-fathom line.
4, The Harbour of Treasury Island.—In this harbour,
which has a maximum depth reaching down to 46 fathoms, I
found the living coral restricted, on account of the rapid
descent of the submarine slope, to a narrow zone limited by
a depth of from 12 to 15 fathoms. In the more open part of
the harbour a calcareous mud, often foraminiferous and occa-
sionally loamy, and derived from the material brought down
by the streams, formed the bottom beyond the coral zone;
but among the islets in the more sheltered south side of the
harbour I found that calcareous gravel derived from the débris
of corals and shells occurred in the deeper water.
5. North-west Coast of Baldlai Island, Bougainville Straits.
—This low island is of raised coral formation and fringed by
shore-reefs. My soundings (over sixty in number) were
taken off the north-west coast, which is the lee side of the
island during the greater portion of the year. A depth of
15 fathoms apparently represented the lowest limit of the
zone of corals. Beyond that depth the arming, in the great
majority of the casts, came up thickly coated with calcareous
sand and gravel. My soundings showed that extensive
thickets of a branching Porites (Porites lavis, Dana) oc-
curred in the shallower depths of from 2 to 8 fathoms, living
fragments frequently breaking off inthe arming. ‘This species
of coral apparently occupied the region that is usually usurped
464 Mr. H. B. Guppy on Coral-soundings
on the protected sides of islands by the arborescent Madrepores.
The branching coral most frequent in the greater depths was
a slender Madrepore, fragments of which, bearing the living
polyps, came up in the arming from depths of 93, 10,
and 13 fathoms. I should add that a portion of an Alcyo-
narian (Anthelia), was brought up from 13} fathoms.
6. The Barrier-reef of Choiseul Bay.—This bay lies within
a broken line of barrier-reef which skirts the western extremity
of the large island of Choiseul, at a distance of from one half
to three quarters of a mile from the shore. Basing his obser-
vation on Bougainville’s chart of this bay, Mr. Darwin inferred
(‘ Coral Reefs,’ p. 167, edit. 1842) that part of the shores is
fringed by coral-reefs. In reality the reefs have the charac-
ters of the barrier class, although associated with shore-reefs
to the northward and southward of the bay ; and the capacious
anchorage with adepth of from 13 to18 fathoms, which Choiseul
Bay affords, owes its existence to the fact of its lying within
a line of barrier-reef. ‘The intention of the French navigator
to anchor in this harbour was frustrated by an attack made
by the natives on his boats whilst employed in searching for
an anchorage. For this reason his plan of the harbour was
imperfect, and may be viewed as merely a preliminary sketch.
My soundings off this barrier-reef gave results somewhat at
variance with my previous experiences. I was surprised to
find that in fifteen casts between the depths of 3 and 20
fathoms sand or gravel was brought up on the arming on
seven occasions, and that six out of fourteen casts in depths
between 20 and 40 fathoms gave a similar indication of the
bottom. A living fragment of Madrepore was brought up
from 13 fathoms. Ina cast of 23 fathoms the arming pre-
served the impression of the cells of one of the Astreide, and
in another of 31 fathoms there was a rounded impression of
the size of a billiard-ball, the inner surface of which retained
the prints of small cells as if of a Porites. The conclusion
at which J arrived after extending my soundings to 40 fathoms,
at a distance of about 600 yards from the shore, was that I
had not reached the lower limit of the coral-zone. An exami-
nation of the configuration of the bottom, as shown in section 3,
may throw some light on this unusual experience. With the
eye assisted by the lead I could observe that the submarine
portion of the reef at first sloped gradually to a depth of 4 or
5 fathoms. There was then a sudden drop of another 9 or
10 fathoms, forming a steep declivity, at the foot of which
began a broad platform with a gentle slope down to 25 fathoms,
and terminating in another somewhat gradual slope. An
inspection of this diagram would lead one to expect that an
in the Solomon Islands. 465
accumulation of detritus would be found in depths of from 15
to 20 fathoms at the foot of the declivity, and that in the more
level region beyond, from the absence of such accumulations,
there would be more favourable conditions for the growth of
coral. My soundings afford evidence that such is the dispo-
sition of the detritus on the outer slope of this reef. Hight
out of twelve casts in depths between 15 and 20 fathoms
brought up sand or gravel on the arming; whilst out of
eleven casts in depths between 23 and 40 fathoms, seven
showed a perfectly clean indentation, in two of which the
nature of the coral was shown. ‘There would thus appear in
this reef to be a belt of sand and gravel separating the zone
of coral into two parts, and situated in those depths in which
corals are stated to cease to flourish. I was on the point
of concluding that I had found in this band of sand and gravel
the lower limit of the corals; but a subsequent extension of
my line of soundings seaward prevented my falling into this
error.
The question then arises, whether in other reefs there may
not be a belt of detritus dividing the coral-zone into two por-
tions. In reefs of which the submarine slope is rapid, or which
are exposed to the whole strength of the trade-swell on the
weather side of the island, it would be a difficult matter to
ascertain the existence of such a belt, as in the former case
an accumulation of detritus of small horizontal extent would
reach downwards to a great depth; whilst the violence of the
surf in the second instance would distribute the sand and
gravel over a considerable area. In the somewhat gradual
slope of the reef of Choiseul Bay there are more suitable con-
ditions for the formation of such a belt of detritus*.
My observations on the outer slopes of reefs in this group
point to the conclusion that the corals grew in greatest
profusion in depths under 10 fathoms. Beyond this depth
the sloping surface of the reef usually presented the character
of extensive tracts of bare coral-rock, studded here and there
with bosses of living massive corals, and marked at intervals
by small patches of calcareous sand and gravel. In some
isolated reefs, sunken some 6 to 8 fathoms below the surface,
and only indicated to the navigator by the “ rips”’ produced
by the powerful tidal currents of these regions, I was much
surprised by their comparatively barren aspect. Lark Shoal,
an isolated reef exposed to the full force of the trade-swell in
the eastern portion of the Solomon group, is covered by from
* Itis worthy of note that in the cases of the soundings off the reefs of
Santa Anna and Onua Islet, the lower limit of the coral-zone corresponds
with the base of the declivities shown in the sections.
466 Prof. P. M. Duncan on the Pali of Corals.
7 to 9 fathoms of water, and offers an instance of this nature.
Here I expected to find the corals in luxuriance; but the
appearance of its surface from the ship’s side and the character
of the soundings showed that the greater portion of its area
consisted of dead coral-rock dotted with bosses of massive corals
here and there. Such was the condition of another shoal in
Bougainville Straits, which was covered by from 5 to 6
fathoms of water. Here the eye could discern an occasional
dark-coloured boss of coral in a field of a pale grey hue,
which was shown by the nature of the crushed material
adhering to a heavy lead to be dead coral-rock.
A word with reference to the general character of the reefs
in the Solomon group may not be out of place in concluding
this paper. From the works of Krusenstern, Surville, Bou-
gainville, and Labillardiére, Mr. Darwin presumed that these
islands were fringed (‘Coral Reefs,’ p. 167, edit. 1842).
There are, however, numerous reefs in this archipelago which
belong to the class of barrier-reefs. A barrier-reef of exten-
sive nature is situated on the west side of Bougainville
Straits, where it follows the edge of a wide submarine plat-
form, which may be viewed as the submerged continuation
of Bougainville Island. A smaller barrier-reef, previously
referred to in the instance of Choiseul Bay, skirts the western
extremity of the island of Choiseul on the opposite side of
these straits. Similar lines of dangerous reefs le off portions
of the coasts of Guadalcanar, Malayta, and other islands. I
hope on some future occasion to enter more fully into this
subject, this reference to which must for the present suffice,
LIII.— On the Relation of the Pali of Corals to the Tentacles.
By Prof. P. Martin Duncan, F.R.S. &e.
Pror. Linpstr6mM has brought under my notice that my
late friend M. de Pourtalés differed from me in reference to
the relation of pali to the tentacles of Corals. In noticing a
very interesting form from the Caribbean Sea which has a
Miocene ancestry, M. de Pourtalés considered the question of
pali. He wrote, “ Prof. Duncan’s supposition that the office
of the pali is to support an extra circle of tentacles is not
borne out in this species, nor in any other paliferous coral of
which I have had the opportunity of examining the polyp.”
We had a conversation on this point, and M. de Pourtalés
told me that he had not had opportunities of seeing man
living forms with pali with the soft parts extended, but that
On Hydrocoralline from Alaska and California. 467
those he had seen had the soft disk supported by the pali. He
was then made aware that the supposition did not come within
the scope of the word conjecture, and there was no remon-
strance whatever on his part, as Prof. Lindstrém thinks. The
so-called supposition was not mine, but that of a man whose
admirable and extensive original researches led him beyond
the troubles of criticism. Jules Haime’s essay on the soft
parts of Cladocora cespitosa* is one of the most interesting
and important of his works, and is of great value because he
described the soft structures in their natural condition and not
after altering them by reagents. It was necessary that I
should abstract this essay in my introduction to the ‘ Sup-
plement to the British Fossil Corals,” Paleontographical
Society, 1866. ‘The translation of the part of the sentence,
“coincide avec la présence des palis situés au dessous et en
dedans de ces tentacules,”’ although placed between inverted
commas, was mistaken by my friend as my own opinion and
the result of my own work.
There was no supposition, but a definite statement of a fact
by a naturalist who was as well able to judge the truth as
any subsequent investigators.
Whilst I was preparing the monograph just alluded to, Mr.
Peach was good enough to watch and draw some specimens
of Caryophyllia clavus, var. borealis, and to send me his
finished delineations and descriptions. The lithographs on
plate ii. Monogr. Brit. Foss. Corals, pt. 1. 1866, figs. 9-20,
are correct reproductions of nature. He was convinced, as I
was and still am, that the inner row of tentacles of figs. 9 and
11 relate to the pali in ‘the manner seen by Jules Haime in
Cladocora.
May 1884.
LIV.—On some Hydrocoralline from Alaska and California.
By W. H. Dattf.
TuE descriptions herewith, with one exception, are of species
from an area from which none have hitherto been described f.
* Hist. Nat. des Corall. vol. ii. p. 591.
+ From a separate impression from the ‘ Proceedings of the Biological
Society of Washington,’ vol. ii. 1883-84. Communicated by the Author,
having been read March 22, 1884.
t A Stylaster rosso-americanus, Brandt, has been mentioned (Z. wiss.
Zool. xxii. p. 292), but has never been described or figured. It may be
an additional species.
468 Prof. W. H. Dall on Hydrocoralline from
They are closely allied to species found in the Oregonian and
Californian province described by Prof. Verrill, but have
been, by his kind assistance, compared with his types, and
appear to him and to myself to be distinct species, differing
not only in habit and form, as well as relative size of the
calyces, but especially in the sculpture and texture of the
surface of the corallum. It is quite probable that the other
species may hereafter be found in South-eastern Alaska, in
which case the fauna would comprise :—
Allopora venusta, Verrill; Allopora Verrillit, Dall; Allo-
pora californica, Verrill ; Allopora Moseleyt, Dall; Allopora
paptllosa, Dall.
To complete the list of Alaskan coralloid animals, Calli-
gorgia compressa of Verrill may be added, as found in the
Aleutian Islands, the only representative of the sea-fans yet
known from the region, which is, however, extremely rich in
Sertularian Hydroids.
Allopora Verrillii, n. s.
Coenosteum thin, reptate, whitish to pale rose-pink, solid,
incrusting ; with a smoothish irregularly lumpy surface, pretty
regularly dotted with sporadic calyces, composed of circular
gastropores, each surrounded by a circle of from five to nine
dactylopores, with occasional sac-shaped ampulla, which are
most abundant on the most elevated projections of the surface
and almost entirely absent from depressed parts. Diameter of
the dactyloporic circle about 1:0 millim., of the central gas-
tropore about 0'37 millim. ; the distance from centre to centre
of the calyces varies from 1°5 to 2°5 millim.
Gastropores cup-shaped, shallow (0:25-0°50 millim.),
smooth inside, with the tip of a white spiculose nipple-shaped
or roundly conical style in the bottom of each, projecting about
its own diameter or less into the cup through the aperture of
a long, nearly vertical, conical tube, which it occupies and
closely fills. The length of this style, which resembles a
fox’s brush, is nearly equal to the thickness of the ccenosteum.
The margin of the cup in fully developed gastropores is
simple and entire, and depressed slightly below (or in no case
elevated above) the general surface. In immature calyces
there is frequently a shallow groove running from the inner-
most point of each dactylopore toward or into the gastropore.
Dactylopores variable in number, eight seeming to be the
normal, but seven the most common number, never sporadic,
in well-developed calyces entirely separated from the cavity of
the gastropore throughout their extent; in immature ones
Alaska and California. 469
joined to it by a shallow superficial groove. ‘Transverse sec-
tion a little ovoid, the wider arch away from the gastropore,
and marked by a vertical, narrow, spongy lamina forming the
style. The exterior margin simple, not elevated above the
general surface, but rather slightly depressed below it.
Neither sort of pore shows tabule. Ampulle simple, sac-
shaped cavities as large as or larger than the calyces, not pro-
truding above the general surface, but more numerous on the
prominences of the crust.
General surface between the above-described openings
impervious, nearly smooth, with the vermicular fine reticula-
tions of the coenosteum structure showing through the trans-
lucent substance, and giving the surface a granular look, a
vertical section of the crust looking much the same. Soft
parts unknown. Crust growing several inches in diameter,
and rarely more than three-eighths of an inch in thickness,
generally found on dead shells of MJodzola or pieces of Nulli-
pore from deep water.
Habitat. Thrown up on beach of Chika Islands, Akutan
Pass, Aleutian Islands, near Unalashka. Five specimens
collected May 1872 by W. H. Dall. Catalogue number,
U.S. Nat. Museum, 4193.
Allopora Moseley?, n. 8.
Coenosteum thick, nodulous, or indistinctly branched, rosy
pink, solid, with an irregular vesicular surface with sporadically
distributed protuberant calyces, consisting of subcircular gas-
tropores, deeply vertically grooved near their margins by from
seven to twelve dactylopores, whose cavities are continuous
with the cavity of the gastropore. Ampulle not observed.
Diameter of the dactyloporic circle about 1°5 millim. ; of the
gastropore proper 0°75 millim. Gastropores rather deeply
(0°50-0°75 millim.) cup-shaped, with the inner surface spicu-
lose; style as in the preceding; margin of the pore deeply
indented by the dactylopores, which are usually nine in
number, but appear to be normally twelve ; the whole calyx
projecting, nipple-like, about 0°5-0°6 millim. from the general
surtace ; recalling, in form, a small contracted Zoanthus. A
spiculose lamellar style appears in the depth of each dactylo-
poric groove oncareful search. The grooves appear to remain
always open.
General surface impervious, covered between the raised
calyces by small irregular sparse vesicular projections of the
ccenosteum, otherwise in appearance and compactness much
as in the previously mentioned form. Soft parts unknown,
470 Prof. W. H. Dall on Hydrocorallince Srom
Habitat. Kyska Harbour, Kyska Island, in the Western
Aleutians; one specimen on the beach growing in a cavity
between the layers of a mass of Nullipore, collected July 1873,
by W. H. Dall. Museum number 6851.
Allopora papillosa, n. s.
Coenosteum very thin, incrusting, livid madder-pink or
brown, with a regularly papillose surface, with close-set
sporadic calyces composed of deep cylindrical gastropores
vertically grooved for from three to six dactylopores, which are
wholly continuous with the cavity of the gastropore. Am-
pulle not noticed. Diameter of the calyx about 0-5 millim.,
of the gastropore proper about 0°35 millim. ; average distance
between the calyces 0°7-1°3 millim.
Gastropores deep, cylindrical, with a short, hardly percep-
tible style, which comes into the bottom of the gastropore ;
but, as a vertical section shows, not vertically but obliquely
from one side. Inner surface nearly smooth, a narrow ele~-
vated ridge bounding the margin of the combined gastropores
and dactylopores.
Dactyloporic grooves rather shallow, long, each with an
evanescent trace of a style on the outer wall ; six seems to be
the normal number to each calyx.
General surface spiculose or finely granulated with small,
pointed granules, with regularly-shaped, elevated, uniform
papille: standing in the spaces between the pore-margins, and
rising to about the same height, but absent on the immature
growing margin of the colony.
Coenosteum less vesicular than in the previously described
forms. Soft parts unknown.
Habitat. On the outside of a living Mytilus californianus,
from 6 fathoms, Coal Harbour, Unga Island, Shumagin
Islands; collected October 1874, by W. H. Dall. Museum
number 6852.
Errina Pourtalesii, n. s.
Ccenosteum of a saccharine structure, rising in stout, sub-
cylindrical, rather round-pointed, occasionally branching stems
10 to 50 millim. high (possibly much larger at times), and
8 or more in diameter; colour, when fresh, deep rose-red,
bleaching to white or grey in dead specimens ; surface loosely
granular, becoming lighter coloured and more compact inward
toward the central axis; gastropores disposed in irregular
lines, which, in the specimen in hand, have a tendency to run
from the base spirally to the left, around the column, but are
Alaska and California. 471
so crowded that little of the surface is free from the nariform
hoods of the attendant dactylopores ; the gastropores average
0°25 millim. apart, but are rather irregular and occasionally
sporadic; a rounded, rather smooth-topped style fills the pore
nearly to the brim; the dactylopores are arranged alternately
on opposite sides of the row of gastropores opposite the
intervals between the latter, though sometimes crowded out of
regularity ; they are furnished with subtubular projections,
squarely truncated at the top and open toward the gastro-
pores, rising above the general surface to about 0:5 millim.
or more; when perfect the styles rise nearly to the summit of
the enclosing hood, slender, pointed, and rather feathery ;
two thirds of their length, in general, is above the -surface,
and the depth of the gastropores is seldom greater (as a rule
less) than that of the submerged portion of the others. Am-
pulle on the surface, barely covered by a network of ccenosteal
granules, which are often broken away, leaving shallow
open cups between the projecting hoods ; there are no scales,
and the circular margin of the gastropores is smooth and
simple.
Soft parts unknown. |
Habitat. In 50-100 fathoms about the Farallones Islands,
off the coast of California, on stones which are frequently
brought up on the fishermen’s hooks entangled in the corals.
A large stone with several specimens upon it was obtained
by Count Pourtalés in 1873, and is now in the Museum of
Comparative Zoology at Cambridge, from which the speci-
men described was selected; other specimens are in the col-
lection of the California Academy of Sciences. This coral,
as well as Allopora venusta and A. californica, Verrili, meet
with a ready sale in San Francisco, owing to their beautiful
colour, which, however, is not lasting if the specimens be
much exposed to the light. ‘The present species seems to do
a good deal toward bridging the gap between Hrrina and
Distichopora, as defined by Moseley. Museum number 6853.
I may add, in conclusion, that through the kind co-opera-
tion of Prof. G. O. Sars and Miss Birgithe Esmark, I have
been enabled to compare the Alaskan and Norwegian Allo-
poras, which, however, do not present any very marked points
of resemblance outside of the generic characters. }
472 Messrs. R. Etheridge, Jun., and A. H. Foord on
LV.— Descriptions of Paleozoic Corals in the Collections of
the British Museum (Nat. Hist.).—No. I. By Rosert
ETHERIDGE, Jun., and ArTHuR H. Foorp, F.G.S.
[Plate XVII.
FAVOSITELLA, gen. nov.
Gen. char. Corallum of irregular form, concavo-convex,
thin ; attached to some foreign body ; composed of minute
rounded or subpolygonal contiguous corallites, which are of
two kinds, large and small; the latter distributed over the
surface in clusters, raised slightly above the general level.
Walls lamellar, distinct. Tabulee in the larger cells some-
what remote, horizontal, slightly curved, with the convexity
downwards ; more numerous in the smaller ones. Mural
pores few in number, large, irregularly distributed. Base
covered with a concentrically striated epitheca.
Obs. In all its external characters this form bears a marked
resemblance to some of the genera of the Monticuliporide,
and until microscopical sections of it had been examined it
was unhesitatingly referred to that group. The presence of
mural pores, however, points clearly to its I’avositoid affinities,
while from all the known genera of the Favositide it is dis-
tinguished by the monticulose character of its surface and the
dimorphic structure of its tubes. As regards the perforation
of the walls in Favosztella, a character which excludes it from
the Monticuliporide, it is true that Mr. EK. O. Ulrich * (who
has given much attention to that group) states that he has
detected mural pores in a ‘ single specimen of an undoubted
Monticuliporoid species,” viz. Homotrypa curvata, Ulrich; but,
granting that they do occur in this one species, it may be
confidently affirmed that out of hundreds of sections of Mon-
ticuliporoid species which have been examined by Dr.
Nicholson, Mr. Ulrich, and one of the writers of this paper,
no such structures have been seen in any other form, If
Homotrypa curvata does possess mural pores, then the proper
course is to remove it from the Monticuliporide and place it
in the Favositide, where also Stenopora finds its appropriate
position, and not in the Monticuliporide, according to Mr.
Ulrich’s amended classification of that group}. In_ brief,
Favositella differs from all other genera of the Favositide in
* Journ. Cincinnati Soc. Nat. Hist., “ American Paleeozoic Bryozoa,”
vol. v. p. 124 (1882).
+ Loe, cit. p. 158.
Patwozotc Corals in the British Museum. 473
the minuteness and dual character of its corallites and in its
monticulose surface. From the Monticuliporide it is separated
by the possession of mural pores.
We are acquainted at present with only one species. ‘This
has been quite inadequately described, though well figured, by
Quenstedt (whose specimens came from Dudley) under the
name of Kavosites tnterpunctus.
Favositella interpuncta, Quenst. sp. (Pl. XVII. figs. 1-1 f.)
Favosites interpunctus, Quenstedt, Petref. Deutsch]. 1881, Abth.i. p. 10,
t. 148. f. 9.
Sp. char. Corallum of medium size, the largest measuring
about 7 centim. in its greatest diameter and about 10 millim.
in its greatest thickness, usually elongate, sometimes nearly
circular, concavo-convex, rising above into irregularly rounded
or lobate elevations, with thin slightly expanded margins.
Base shallowly concave, covered with a concentrically
wrinkled epitheca; usually attached to a shell or other
foreign body, which seems, at least in some cases, to have
governed the form assumed by the corallum. ‘The thin
margins of the latter are sometimes contracted or folded
inwards towards the object of attachment, so that their out-
line exhibits an irregularly sinuous appearance. The tubes
which compose the corallum are so minute as to be barely
distinguishable, excepting in well-preserved specimens, with-
out the aid of a lens; they open upon the upper surface,
the small tubes forming groups about 5 millim. apart, ele-
vated a little above the general level of the surface, so as
to constitute faintly defined monticules. ‘The corallites, as
seen in tangential sections, are irregularly rounded or sub-
polygonal in outline, with thick walls. The smaller ones are
intercalated at the angles of junction of those of larger size.
The latter measure about one half, the former from about one
tenth to one fifth of a millimetre in diameter. Longitudinal
sections exhibit great irregularity in the walls of the corallites ;
these are crinkled, with here and there a minute septum-like
projection of the wall. The tabula of the larger tubes are
very delicate, horizontal, or a little oblique, and slightly
curved, and placed at from one to two tube-diameters apart.
In the smaller cells the tabule are more numerous and are
thickened with a fibrous layer of sclerenchyma. Mural pores
of a large size, remote and irregularly disposed, are seen in
these sections.
Obs. The species above described occurs abundantly in the
Wenlock Shales at Dudley, Worcestershire, associated with
Ann. & May. N. Hist. Ser, 5. Vol, xii. dl
474 Messrs. R. Etheridge, Jun., and A. H. Foord on
the characteristic fossils of that formation. In some speci-
mens the mural pores have been filled with chalcedony of a
concentric structure. It may be noted that the pores are so
large as to be seen on a polished surface with a hand-lens.
Locality and Horizon. Dudley, Wenlock Limestone.
Collection. British Museum (Natural History), and A. H.
Foord.
Genus CH&TETES, Fischer, 1837.
Cheetetes Lonsdalet, Eth. & Foord. (Pl. XVII. figs. 2-2 ¢.)
Sp. char. Corallum incrusting in the young state, pro-
bably forming large masses in a more advanced stage of
growth, of undeterminable dimensions, composed of minute
closely contiguous corallites, of which three or four, according
as they are measured in conformity with their longer or shorter
diameter, occupy the space of 1 millim. Calices polygonal,
very irregular in outline, with from one to four tooth-like
projections characteristic of Chetetes. 'Tabule numerous,
complete, horizontal, or slightly arched, usually about one
tube-diameter apart.
Obs. So far as we are’ aware, no species of Chetetes has
been described hitherto from the Devonian rocks of Devon-
shire, as the Chwtetes tumidus mentioned by Mr. T. M. Hall
from the Pilton beds of Braunton (Quart. Journ. Geol. Soe.
1861, xxii. p. 376), if correctly determined, is now known to
be a Monticuliporid. We have the present species in the
young state incrusting a Cyathophylloid coral, and there is
evidence to show that at a more advanced age it became
massive and probably lobate. The largest specimen, which
is a polished fragment, measures 83 centim. in its greatest,
by about 6 centim. in its smallest diameter. This species is
distinguished from all others known to the writers, except
C. depressa, Fleming, sp., by the minuteness of its corallites,
and from the latter by the numerous septum-like projections of
its calices and the greater irregularity of the corallites. The
so-called “septal teeth”? in Chetetes are now known to be
due, as originally pointed out by Lonsdale, to “ fission taking
place in the older corallites”? (wide Journ. Linn. Soe. vol.
xiil., Nich. & Eth., jun., “On the Genus Alveolites,” &c.
p- 853, 1877). It becomes therefore a question whether such
a character can be used as a means of specific separation,
unless, indeed, the degree of fissiparity differs in various species.
Under the circumstances it will be better to say that the
form now before us differs from its nearest ally CU. depressa,
Flem., sp., in the greater irregularity of its corallites.
Paleozoic Corals in the British Museum. 475
Many Devonian Corals have been referred to the genus
Chetetes, but in most cases these have been shown to belong
to other genera. In concluding his notice of Chetetes Prof.
H. A. Nicholson remarked, “The species. . . . are not known
to occur out of the Carboniferous (and possibly the Devonian)
rocks” (‘Tabulate Corals,’ 1879, p. 266). There are,
however, a few forms which should be referred to in passing ;
for instance, in 1851, Messrs. Edwards and Haime described
their C. Trigert (Mon. Polyp. Foss. Terr. Pal. p. 269,
t. xvil. fig. 6), which from the description appears to belong
perhaps to the genus. Mr. A. Winchell has likewise described
(Report Geol. & Industrial Resources of the Peninsula of
Michigan, 1866, pp. 89, 90) two species under the names of
C. hamiltonensis and C. microscopicus. In the first, the septa
are said to be “ complete,” and we should therefore doubt its
reference to the present genus at all; whilst the description
of the second is, lacking a figure, too brief for identification.
The Devonian rocks of Muscatine, Iowa, have yielded to
the researches of Dr. C. A. White an exceedingly fine form,
C. muscatinensis, White, of which we have examined
specimens; and although in many respects resembling a
Jheetetes, we do not feel justified in at once pronouncing it
to belong to that genus. Lastly, Prof. F. von Rémer has
recently described (Lethea Geogn. 1883, i. Th. p. 459) a
coral from the Devonian rocks of the Hifel, as C. stromato-
poroides. This is clearly distinct from our species, and, in
fact, the author appears to doubt its reference to Chetetes
at all.
We have much pleasure in associating with this coral the
name of the late Mr. W. Lonsdale, who may be said to have
laid the foundation for the study of British Devonian Corals,
and for that of the genus Chetetes in particular.
Loc. and Horizon. Bishop’s Teignton, near Torquay, and
Torquay, S. Devon.
Collection. British Museum (Natural History), presented
by Messrs. A. Rogers and HE. B. Luxmore.
EXPLANATION OF PLATE.
Fig. 1. Favositella interpuncta, Quenst., sp. Specimen showing lobate
form of the corallum. About 2 natural size. Coli. Foord.
Fig. 1a. Another specimen, drawn to the same scale. Coll. Brit. Mus,
(Nat. Hist.) J :
Fig. 16. Under surface of the preceding, showing the wrinkled epitheca.
Attached to a Bellerophon? :
Fig. 1c. Tangential section of this species. Enlarged about 15 diameters.
Fig. 1d. A single cell, enlarged about 50 diameters. .
Fig. le. Longitudinal section, showing pores. Enlarged about 15
diameters,
ale
476 Mr. W. F. Kirby on the
Fig. 1f. Portion of a longitudinal section, showing one of the small tubes
between two larger ones. Enlarged about 15 diameters.
Fig. 2. Chetetes Lonsdalei, Eth. & Foord. Small polished specimen,
showing this species incrusting a Cyathophylloid Coral. Nat.
size. Coll. Brit. Mus. (Nat. Hist.).
Fig. 2. a, Tangential section, showing septum-like teeth. Enlarged about
15 diameters.
Fig. 2b. A few cells, enlarged about 50 diameters. In this figure the
walls of the corallites are represented with somewhat too regular
and curved an outline. Their true character is best seen in
fig. 2a.
Fig. 2c. Longitudinal section, enlarged about 15 diameters.
LVI.—On the Orthoptera collected during the recent Hape-
dition of H.M.S. ‘ Challenger.’ By W. F. Kirsy, Assistant
in the Zoological Department, British Museum.
THE present paper includes only the families Blattide, Man-
tide, Phasmide, and Gryllide. One species of Phasmidz is
here described as new.
CURSORIA.
Blattide.
1. Panchlora indica.
- Blatta indica, Fabr. Syst. Ent. p. 272 (1775).
San Jago, Cape Verdes, Aug. 10, 1873.
2. Panchlora viridis.
Blatia viridis, Fabr. Syst. Ent. p. 272 (1775).
Bahia, Sept. 1873.
3. Panchlora madere.
Blatta madere, Faby. Spec. Ins. i. p. 341 (1781).
St. Vincent, Cape Verdes, July 1873.
4, Kpilampra laticollis.
Epilampra laticols, Walk. Cat. Blatt. B. M. p. 203 (1868).
Queensland (three specimens).
‘Ihe type is from Richmond River. The species is allied
to £. notabilis, Walk., but is larger and paler. The latter
species 1s probably synonymous with Z. inquinata, Stal.
‘Challenger’ Orthoptera. AT7
5. Polyzosteria ligata.
Polyzosteria hgata, Watt. Syst. Blatt. p. 220 (1865).
Somerset, Torres Straits, Sept. 1874.
GRESSORIA.
Mantide.
6. Mantis hybrida.
Mantis hybrida, Burm. Handb. Ent. ii. p. 536 (1839).
Ki Dulan, Sept. 25, 1874.
Agrees with a specimen from Borneo in the British
Museum.
Phasmidz.
7. Lopaphus cocophages.
Alopus cocophages, Newp. Phil. Trans. 1844, p. 288, pl. xiv. fig. 4.
Tongatabu.
Common in the Pacific Islands, and very destructive to
cocoanut-trees.
8. Cyphocrania gigas.
Gryllus gigas, Linn. Syst. Nat. ed. x. vol. i, p. 425 (1758).
Amboina, October.
9. Cyphocrania maculata.
Mantis maculata, Oliv. Enc. Méth. vii. pp. 626 & 636 (1791).
Amboina, October.
The male was not previously in the British-Museum col-
lection.
10. Necroscia moderata.
Long. corp. 3 une. 2 lin.; exp. al. 3 une. 5 lin.
Male.—Straw-coloured (perhaps greenish during life) ;
wings transparent, with yellow nervures; body moderately stout,
of nearly uniform thickness. Head large, oblong, smooth,
with a slight indentation on the median line behind; antennz
moderately long and darkening into reddish brown towards
the tip; ocelli obsolete. Head and prothorax rather wider
than the front of the mesothorax; prothorax unarmed, but
478 On the ‘Challenger’ Orthoptera.
with channels on the back, as shown in the woodcut; meso-
thorax four times as long as the prothorax, expanded behind and
with a double row of short spines on the back, five or “six on
each side, but unsymmetrically, those on the right side being
aT
nalvaan 2
Nery era eaaeae
> =
Za
A
= res
>. e Sa SWE eS
SSC ae
SS =
SS
ral
4
q
generally placed more forward than on the left; metathorax
moderately short and broad; tegmina oval, concolorous with
the costal area of the wings, the abdomen, the legs, and
thorax being rather darker. Wings broad, moderately long ;
legs mostly unarmed ; femora with three small serrated ridges,
the teeth on the front pair being nearly obsolete.
Mr. A. 8. Olliff on the Genus Helota, MacLeay, 479
_ This species appears to differ from any previously known
in the armature of the thorax.
Amboina.
SALTATORIA,
Gryllide.
11. Gryllus capensis.
Acheta capensis, Fabr. Syst. Ent. p. 281 (1775).
St. Vincent, Cape Verdes, July 1873; Green Mountain,
Ascension, April 1876.
12. Anastostoma australasice.
Anastostoma australusie, Gray, Mag. Nat. Hist. (2) i. p. 143, fig. 16
(1837).
Somerset, Torres Straits, Sept. 1874.
A single immature specimen.
LVII.—Description of an African Species of the Coleopterous
Genus Helota, MacLeay. By A. SrpNeY OLLIFF.
THE species I am about to describe was collected by the
late Dr. Welwitsch at Angola, and was recently received by
Mr. Martin Jacoby in a box, containing chiefly Phytophagous
Coleoptera, from Signor Paulino d’Oliveira, of Coimbra, in
Portugal. I have elsewhere pointed out (Cist. Ent. iii,
p- 49) that all the previously known species of the genus
Helota ave found in Eastern Asia, and therefore the species
here described is of special interest, as showing that the genus
is of far wider range than could have been anticipated. Lord
Walsingham informs me that he has received from Bathurst,
West Africa, a new species of Dewterocopus, Zeller (belonging
to the Lepidopterous family Pterophoride), a genus which,
up to the present time, has only been known from Java.
This appears to be a somewhat similar and equally unex-
pected case of geographical distribution.
Helota africana, sp. n.
Elongate, depressed, narrowed both in front and behind,
pale fulvous, shining; the head, disk of the prothorax, a spot
near the base, and the apical half of each elytron black.
480 Mr. A. 8. OIliff on the Genus Helota, MacLeay.
The head rather broad, slightly convex, strongly and not
very closely punctured in the middle, the punctures much
finer and closer near the sides; epistoma rounded in front,
finely and closely punctured; mandibles black and very finely
punctured. Antenne reddish testaceous, the club pitchy
black and covered with fine grey pubescence. Prothorax
considerably narrowed towards the apex, moderately convex ;
the disk black, highly polished, strongly and sparingly
punctured ; the sides fulvous and finely punctured; the large
punctures are arranged in two longitudinal irregular patches
extending throughout the whole length of the prothorax, one
on each side of the middle; anterior margin bisinuate, the
angles very slightly produced; sides oblique; posterior
margin very strongly bisinuate, the angles acute. Scu-
tellum transverse, black and impunctate. Hlytra about
half as long agam as the head and prothorax together, as
broad at the base as the prothorax, slightly narrowed pos-
teriorly, moderately strongly punctate-striate, the seventh
interstice somewhat raised, the others rather broad, flat, and
impunctate; each elytron with an elongate spot near the
base between the third and fourth striz and the apical half black,
the latter with a slight tinge of greenish bronze; humeral
angles notvery prominent. Underside fulvous and impunctate;
head black, finely and closely punctured behind the eyes ; the
mentum very sparingly punctured; prosternum with an obscure
black patch on each side extending from just behind the
anterior margin to the middle. Legs fulvous; the coxe,
knees, tips of the tibie, and the tarsi pitchy black. Length
13 millim., greatest width 4 millim.
Angola, West Africa (Welwitsch). Type in Lisbon
Museum.
This pretty species is one of the most distinct of all the
described species of the genus. In form it appears to approach
Helota Serville’, Hope, but differs not only in the absence of
the flavous callosities so conspicuous in that species, but also
in having the prothorax comparatively shorter and the elytra
less produced at the apex. In coloration it is quite unlike
any species with which I am acquainted, but, on account of
the absence of the flavous callosities and the apical half of the
elytra being black tinged with green, it bears some slight
resemblance to H. semifulva, Rits., with which species in other
respects it has little in common.
Mr. C. O. Waterhouse proposes to figure H. africana and
H. semzfulva in an early number of his ‘ Aid to the Identifi-
cation of Insects.’
Geological Society. 481
PROCEEDINGS OF LEARNED SOCIETIES.
GEOLOGICAL SOCIETY.
March 22, 1884.—Prof. T. G. Bonney, D.Sc., F.R.S.,
President, in the Chair.
The following communications were read :—
1. “ On Rhytidosteus capensis, Owen, a Labyrinthodont Amphibian
from the Trias of the Cape of Good Hope.” By Sir Richard Owen,
eC 5: EE... B.G.S.
The author first noticed the discovery of certain forms of Am-
phibia belonging to the genera Labyrinthodon, Brachyops, Petrophryne,
and Lhinosaurus, and called attention to certain typical peculiarities
in the structure of the teeth, the form of the bony palate, and the
double occipital condyle.
An imperfect cranium of the species now described as Rhytid-
osteus capensis was procured by Heer Swanepoel from the Trias on
his farm of Beersheba, in the Orange Free State, and deposited by
him in the Bloemfontein Museum.
This specimen, which was brought to England and submitted to
the author by Dr. Exton, consists of the anterior portion of the
skull with part of the mandible attached. The general form is
batrachoid, and one of the hinder palato-vomerine teeth, on being
examined microscopically, exhibited the characteristic labyrinthodont
structure.
The surface of the skull, and the characters of the premaxillary,
nasal, frontal, and prefrontal bones were described. ‘The parietals
and postfrontals are imperfect, the hinder part being lost. The
rami of the mandible are also imperfect behind, but a broken frag-
ment shows the articular surface. The vomerine bones were also
described, with the posterior nostril and the teeth before and behind
this opening. The breadth of the bony palate at its hinder frac-
tured border is 5 inches ; the length of the part preserved 43 inches ;
the mandible, when perfect, was probably from 11 inches to a foot
in length. The author also gave an account of the dentition wielded
by the premaxillary, maxillary, vomerine, palatine, and mandibular
bones.
The author pointed out that the type of air-breathing vertebrates
to which the present genus belongs reached its highest development
in the Triassic period in Britain, Russia, North America, Hindostan,
and South Africa. The only known antecedent form from which
the labyrinthodont structure of tooth might have been derived is a
genus of fishes named Dendrodus, in the Old Red Sandstone. The
Liassic Ichthyosaurs also show some similarity in tooth-structure ;
but in them there is far greater simplicity.
482 Geoloyical Society.
2. “On the Occurrence of Antelope-remains in Newer Pliocene
Beds in Britain, with the Description of a new Species, Gazella
anglica.” By E. Tulley Newton, Ksq., F.G.S..
Part of the skull and horn-core of a small cavicorn Ruminant,
which had been obtained by Mr. H. B. Woodward from the Norwich
Crag of Thorpe, was described, the chief points noticed being the
almost erect position of the horn-core upon the frontal bone, its
oval section and enlargement just above the pedicle, the presence
of a deep pit on the outer side of the pedicle, and of a well-marked
frontal fossa, from which a large foramen passed directly into the
orbit. ‘The frontal suture being well preserved, the precise direc-
tion of the horn-cores could be ascertained.
The presence of a frontal fossa with a foramen passing directly
into the orbit, was held to indicate an affinity with the Antelopes ;
and after comparison with the available recent specimens in the
British Museum and Royal College of Surgeons, it was regarded as
most near to the Gazelles,—G'azella dorcas, G. subgqutturosa, Gi. picti-
cauda, and G. Bennettit being most like the fossil, and agreeing
with it in having the skulls more or less compressed in the frontal
region, nearly upright horns, and a well-marked frontal fossa and
foramen, but differing in the form of the fossa and in the position
of the pit on the pedicle. On the whole G. Bennettia was regarded
as nearest to the fossil.
The perfect condition of the frontal bone allowed a cast of the
interior to be taken, which reproduced the form of the frontal lobe
of the brain, and it became possible therefore to compare this part
of the fossil with the brains of recent forms, which was then done,
special reference being made to the casts taken from Gazella picti-
cauda and G. Bennettii. In the form of the convolutions of the
frontal lobe, G. Bennett?i was again found to be the most like the
fossil.
Among the known fossil forms only a few were thought suffi-
ciently near to render a comparison with them necessary ; the fol-
lowing, however, were mentioned, and attention called to the points
in which they differed from the Norwich specimen, namely Antilope
deperdita, A. brevicornis, A. porrecticorms, Tragoceros Valenciennes,
and Paleoryx parvidens. Seeing that all the important characters
of this fossil are found among the recent Gazelles, it is referred to
that genus; but as it differs in certain points from each of them, it
is necessary to give it a new specific name; the author therefore
called it Gazella anglhea.
Fortunately this interesting discovery is corroborated by two
other similar examples of horn-cores with frontals from the same
locality and horizon. One of them is in the British Museum, and
the other in the possession of Dr. Arthur King, of Norwich.
A short appendix, by Mr. H. B. Woodward, on the horizon from
which these fossil Gazelles were obtained was also read.
Geological Socvety. 483
3. ‘A Comparative and Critical Revision of the Madreporaria of
the White Lias of the Middle and Western Counties of England,
and of those of the Conglomerate at the Base of the South-Wales
Lias.” By Robert I’. Tomes, Esq., F.G.S.
After referring to previous memoirs on the subject by MM.
Tawney, C. Moore, Tate, and Bristow, and to the conflicting con-
clusions arrived at by those geologists, the author insisted that the
Madreporaria are not necessarily contemporaneous with the beds in
which they are found imbedded. He took exception to some of
the identifications of these forms by Dr. Duncan, and suggested that
their nearest analogues are to be found in the St. Cassian beds.
The few and imperfect corals of the White Lias of Warwickshire,
the author believes to have resemblances with the coral fauna of the
Sutton Stone on the one hand, and the St. Cassian beds on the other.
The Mollusca found in the same beds, however, are those of the
zone of Ammonites angulatus.
While the Brocastle Conglomerate is, according to the author, a
local deposit with uncertain relations, the Sutton Stone is a much
more regular stratum, and is quite distinct from the conglomerate
which immediately overlies it, and which is seen at Southerndown.
He regarded the Sutton Stone as the equivalent of the White Lias,
and of Rheetic, not Liassic age.
The revised list of corals found in the St. Cassian beds, the White
Lias, the Sutton Stone, and the Brocastle Conglomerate respectively,
shows, according to the author, that nearly all the White-Lias forms
occur at St. Cassian; that a certain number of the corals of those
two formations occur also in the Sutton Stone, but that none of
them occur at Brocastle ; and, furthermore, that the coral faunas of
Sutton are quite distinct.
In conclusion, the author contested the views of the late Mr. C.
Moore concerning the existence of a series of conglomerates below
the base of the Sutton Stone, and insisted that the presence of a
Hettangian molluscan fauna in these beds and the White Lias is not
sufficient to counterbalance the evidence of Rheetic affinities afforded
by the corals. The Brocastle Conglomerate, however, contains corals
with Liassic affinities.
Detailed descriptions of the new species of corals formed the
conclusion of the paper.
April 2, 1884.—Prof. T. G. Bonney, D.Sc., F.R.S.,
President, in the Chair.
The following communication was read:—
“On a new specimen of Megalichthys from the Yorkshire Coal-
field.” By Prof. L. C. Miall, F.G.S.
A large and unusually complete example of this fish was recently
found in the roof of the Halifax Hard bed, at Mr. 8S. B. Ellison’s
Firebrick works, Idle, near Leeds. The fossil is in good preserva-
484 © Bibliographical Notice.
tion, the ventral surface is uppermost, the pectoral, ventral, anal,
caudal fins can be more or less satisfactorily made out; the dorsal
surface is absent. The length is 3 feet 83 inches, of which the head
measures about 10 inches, and the tail (from the end of which 5 or
6 inches may be wanting) about a foot. Judging by the large skull
figured by Agassiz and preserved in the Leeds Museum, Megalich-
thys may have attained a length of from 4 to 5 feet.
The skull shows the mandible and mandibular teeth, the end of
the snout, the opercula, and the jugular plates. The pectoral fins
show the obtuse lobate character, previously suspected by Huxley to
obtain in this genus. Large basal scales lie on each side of each
pectoral fin.
The ventral fins are abdominal. The right, which is best pre-
served, exhibits the arrangement of the scales which is described,
and which gives a clue to the disposition of the underlying bones or
cartilages. This must have closely resembled that in some Elasmo-
branchs. The same type of fin may be traced, though with important
modifications, in Polypterus, Polyodon, and Acipenser, whilst in other
recent Ganoids and in Teleostei the arrangement is widely different.
Between the ventral fins are three large scales, one median and
two lateral. On the left side of the median scale lies what appears
to be the anus. A similar arrangement seems to occur in Plerich-
thys. This region is rarely exposed in fossils.
The anal fin has also its pair of large basal scales. The caudal
fin cannot be well made out. There are indications of the under-
lying skeleton, but nothing can be distinctly made out.
All the features of the present fossil confirm the opinion long ago
expressed by Pander and Huxley as to the near affinity of Megal-
ichthys to Osteolepis and Diplopterus.
BIBLIOGRAPHICAL NOTICE.
Geological and Natural-History Survey of Canada: Catalogue of
Canadian Plants.—Part I. Polypetale. By Joun Macovn, M.A.,
F.L.S., F.R.S.C. Montreal, 1883.
Mosr of our colonial governments have recognized in an enlight-
ened manner the great importance, even from a merely commercial
stand-point, of a complete stock-taking of their natural productions.
Mineral wealth has no doubt generally been looked to first ; and the
necessity for the conservation of forests and of animals yielding
food and clothing has not always been recognized so readily as the
immediate profit to be obtained from them; but the value of the
knowledge of what plants and animals the country contains has led
to the frequent conjunction of Natural History departments with
State Geological Surveys. This healthy sign of wise counsels is
seen in the work before us—the first part of a catalogue of Canadian
Bibliographical Notice. 485
plants, issued by the “ Geological and Natural-History Survey” of
the Dominion ; and the colony is to be congratulated on the business-
like manner in which Mr. John Macoun has begun his task. The
form, paper, and printing of the work are admirable, the type being
especially clear ; and beyond the dropping of a letter here and there,
as in the generic initial of the fourth species mentioned, the appear-
ance of Alianthus for Ailanthus, and one or two slips of the
kind, no fault can be found under this head. In a short preface the
Author summarizes the brief literature of his subject and the history
of botanical exploration in the country, enumerating also the collec-
tions examined for the purposes of the work. From this it appears
that the Survey-staff have been collecting for the last ten years, but
that the examination of the Rocky-Mountain region and of British
Columbia is still very imperfect. When we remember that the area
of the Dominion is estimated at over three and a half million square
miles, or little less than that of Europe, we cannot expect it to be as
yet at all completely known to the botanist, as is perhaps evident
from Mr. Macoun’s Catalogue, which enumerates 907 species of
Polypetale under 243 genera, as against 616 species in the 193
genera of the same group in our British flora, according to the
‘ London Catalogue.’ One useful detail in Mr. Macoun’s work is that
both the genera and the species are numbered continuously through-
out, thus facilitating the above comparison, which gives the possibly
significant result of an average of 3°73 species to every genus in the
continental, as against 3°18 in the insular flora. It must, however,
be noticed that Mr. Macoun has included in his numbering not only
“introduced plants,” ‘“‘ garden escapes,” and those ‘* spontaneous
in gardens,” but also planted trees, such as the horse-chestnut and
Tilia europea, and even species “likely to be found”! ‘There are
at least a hundred of these in the present part, and their inclusion
without typographical distinction seems perfectly unjustifiable,
though the indication of the western migration of such plants as
Papaver somniferum and P. Rheas, Chelidonium, Armoracia, Cap-
sella, Thlaspi arvense, and the Brassicas is undoubtedly of interest.
It is remarkable that the list includes so many migrants from the
east and but very few from the south. There are, of course, many
names and authorities for names that might be called in question
according to the law of priority; but this is no new fault in
recent systematic works; blemishes perhaps of a more practical
bearing and more readily remediable, however, are, first, that no
apparent distinction is made between bond fide local names, as
May-flower, Yellow Puccoon, and White Cohosh, and mere “ book-”
names, such as Virgin’s-Bower, Awl-wort, or Thyme-leaved Pin-
weed; and, secondly, that the localities are stated continuously, with
no obvious grouping under provinces or natural divisions. In a
catalogue it may have been inevitable to insert under the genus:
Astragalus two unnamed species without descriptions, which can
only be referred to by their numbers or localities ; but it is a course
open to considerable objection. When all is said, however, these
are but slight faults in a generally excellent piece of work, and the
486 Miscellaneous.
continuation of Mr. Macoun’s list will be looked forward to with
interest. The apparent occurrence of natural hybrids of Wuphar (a
characteristic, as appears from Mr. Thomas Meehan’s publications,
of the allied genus Sarracenia) is one among many points of interest
in the work, and the flora with which it deals is characterized by
possessing 37 species of Astragalus, 2 of Potentilla, 27 of Ranun-
culus, 26 of Sawifraga, 22 of Viola, 17 of Ribes, 16 of Arenaria, 14
of Lupinus and of Anemone, 13 of Stellaria, 12 of Cornus, 10 each
of Geum, Gnothera, Desmodium, and Claytonia, 8 of Acer, 7 of Rhus,
and 5 of Paurnassia. Such a catalogue makes a botanist hope that
it may be speedily followed by such a descriptive flora as shall be a
credit to the largest of our colonies.
G. 8S. Bovterr.
MISCELLANEOUS.
Freshwater Sponges as Improbable Causes of the Pollution of
Tiver-water.
Mr. Porrs reported that on the 9th of February he had visited
and partially examined the forebay at Fairmount Waterworks, on
the Schuylkill River, from which the water had been temporarily
withdrawn, with a view to discover the winter condition of the
freshwater sponges and the other inhabitants of that locality. He
found by far the larger part of the wall-surface below the water-line
inaccessible on account of a thick deposit of mud upon the bottom
and much water remaining in the forebay. Wherever reached,
however, and so far as the eye could detect in other places, 1t was
covered by a mud-coloured incrustation of considerable thickness,
which a more minute examination showed to be composed almost
wholly of the statoblasts and spicules of the sponge Meyenia Leidyt.
Some few fragments of Meyenia fluviatilis and Spongilla fragilis
were seen, but the first-named was clearly the prevailing species.
A sluiceway which formerly supplied the last of the old “ breast
wheels” used in pumping into the reservoir, but from which the
water had been for many months excluded, was entered and ex-
amined. Here the remaining incrustation (much having doubtless
crumbled and fallen away) was from one fourth to one half an inch
thick, of the appearance of crumbling plaster, and, as in the other
cases, it consisted of the sponge before named, with but a small
proportion of intruded material.
While considering the effect of the presence of so large a sponge-
growth at the very inlet to the supply-pumps, Mr. Potts stated that
this particular species was conspicuous among the known North-
American sponges by its great relative density and the small propor-
tion of its sarcode or flesh. Its decay, therefore, at the termination
Miscellaneous. 487
of its period of summer growth would be a less cause of pollution to
the water-supply than that of any other sponge.
Moreover, from recent investigations into the life-history of these
low organisms, he was inclined to believe that decay was not the
normal or necessary result of the close of each season’s growth.
The fragile branches of some species inhabiting exposed situations
may, of course, be broken off and destroyed while the sarcode still
covers them ; but in the sessile portions, and in all when sufficiently
protected, the cells of the sarcode at the period of full maturity, for-
saking their places along the lines of the skeleton framework, gather
together by simultaneous amceboid movements into dense groups,
where they are soon covered by a tough chitinous “ coat,” which, in
time, generally becomes surrounded by a “ crust ” of minute granular
cells, and armour-plated by a series of protective spicules. These
groups are now recognized as the statoblasts, gemmules, or winter-
eggs of the sponge—eggs only in appearance—in reality the resting-
spores or protected germs which conserve the life of the individual
through the cold and storms of winter, and awake very early in the
springtime into new life—yet a continuance only of the same exis-
tence which was seen a few months before nestling into this winter’s
sleep.
If this is the ordinary course with these organisms there seems
no reason to regard them as serious causes of the pollution of our
streams, though violent freshets before this resting-period is reached
may tear them to pieces, and their decay may give a temporary
taint to the water.
Continuing the narrative of his exploration, Mr. Potts described
the iron pipes which had lain for many years upon the bottom of the
forebay, as covered, in some places to the depth of an inch or more,
with a crust richly coloured by iron oxide, but principally composed,
as were the others, of the spicules and statoblasts of MZ. Leidyi.
Upon the surface of this crust in places he found the remains of
large colonies of Urnatella gracilis, Leidy. In the absence of any
positive knowledge of the winter condition of this curious polyzoan,
Mr. Potts had examined with much interest a novel form of statoblast,
which was frequent upon the same pieces of sponge; but he was
unsuccessful in associating it with the polyzoan. It is most pro-
bable that the life is continued, as suggested by Dr. Leidy, within
the urn-like joints of this creature, and that they put out buds and
anew growthinthe spring. To discover if this were the case, he had
placed some fragments in water, and while awaiting results he had
been surprised at the appearance within a few days amongst the
fragments of Urnatella of numbers of the recently described cheeto-
branch worm, Manayunkia speciosa of Leidy, as well as several
living cells of a species of Paludicella, probably P. elongata, of the
sameauthor. ‘The persistence and tenacity of life in these apparently
delicate creatures, overcoming not only the severity of a hard winter,
but an exposure of several days in the open air, were further com-
mented upon.—Proc. Acad. Nat. Sci. Philad., Feb. 12, 1884, p. 28.
488 Miscellaneous.
On the Brain of Kunice Harassii and its Relations with the
Hypodermis. By M. E. Jourpay.
Quatrefages and Claparéde were the first to indicate the relations
that exist between the hypodermic cellular layer and the nervous
centres in some Annelides. More recently Ehlers, with reference
to the brain of the species which is the subject of the present note,
and Spengel, in his memoir upon a EKunician, Oligognathus Bonel-
liv, have pointed out the difficulty of separating the brain from the
hypodermis in the cephalic lobe of these worms. These notions, so
contrary to the classical data and figures relating to the brain of most
Annelides, seemed to us to need confirmation. With this view we
have made sections of the whole of the cephalic lobe, including both
the brain and the integuments of the species under consideration.
The observations that we have been able to make by this method
have not only allowed us to demonstrate the correctness of the
opinion of Ehlers and Spengel, but have also revealed some new
facts.
The brain of Hunice Harassii, upon the external form of which
we shall say nothing, seeing that this apparatus is very imper-
fectly limited, consists essentially of a central mass of punctate
substance, surmounted by a thick layer of nervous cells, designated
by Ehlers the nuclear layer.
Above this nuclear zone, and immediately beneath the cuticle,
we see epithelial elements in the form of cones, with their apices
directed towards the deeper surface of the integuments. The feet
of these hypodermic cells, instead of terminating upon a basal, as in
the case of the integuments of the rest of the body, become trans-
formed and prolonged into so many rigid threads, which penetrate
into the nuclear layer, grouping themselves together in larger or
smaller numbers, to form a sort of pillar passing from the cuticle
to the mass of punctate substance. The protoplasm of these hypo-
dermic cells is much reduced in quantity ; their nuclei have a cha-
racteristic fusiform aspect. The basal prolongations appear as rigid
threads with a vitreous aspect and with a clean fracture. United
into bundles, these hypodermic fibres are not stained readily by
carmine or by hematoxyline; but under the influence of hemat-
oxylic eosine they acquire the pearl-grey coloration characteristic
of the cuticle and basals of the hypodermis of Annelides. It is
impossible to trace one of these filaments from the hypodermic cell
to which it belongs to the punctate substance ; they lose themselves
in the nuclear layer, where they become intimately confounded with
other fibrille presenting similar histological characters, but haying ~
a different origin.
The nuclear layer is justly regarded by Ehlers and Spengel as of
neryous nature, but it is composed of elements of varied aspect.
In a section this layer appears as a delicate network filling up the
space between the pillars of which we have just spoken, and the
meshes of which are occupied each by a spherical nucleus. It is
Miscellaneous. 489
very difficult, in the sections, to know whether this network is con-
stituted by sections of cell-membranes soldered together by means
of a cement or by very delicate fibres. Dissociations enable us
easily to answer this question; they show that the nuclear layer
consists of nerve-cells each possessing a large nucleus, a protoplasm
so reduced that they seem to be destitute of it, and a fine enveloping
membrane. We notice also that from each of these cells there start
most frequently one, but sometimes two processes. These filaments
are very delicate, and, when examined with an objective giving an
enlargement of 400 or 500 diameters, comparable to the appearance
presented by a spider’s thread seen with the naked eye. By several
of them becoming grouped and soldered together, these filaments
constitute the cross-lines of the meshes of the network which are
observed in the sections. Among these cells reduced to their nucleus,
which form nearly the whole of the nuclear layer, we observe
a certain number distinguished by their larger dimensions; they
possess a nucleus and a finely granular protoplasm, which is
coloured yellow by picrocarmine ; from their peduncle starts a pro-
cess which mingles with those of the small nerve-cells, and likewise
penetrates into the punctate substance.
By examining the boundaries of the nuclear layer and punctate
substance we easily distinguish a great number of fibrille which
emanate from the nerve-cells and become connected with the punc-
tate substance. It is impossible to say what the fibrille of the
hypodermic cells become at this level, or to know whether they
penetrate into the punctate substance or lose themselves at its sur-
face. These fibres, of which the origin and no doubt the functions
are so different, in fact present such similar histological characters
in Hunice Harassvi that itis impossible to distinguish them. The
punctate substance itself consists essentially of a mass of interlaced
fibrille forming a network which is more or less close in different
regions. The spaces left vacant by the meshes of this fibrillar net-
work are filled up by a finely granular protoplasm, which acquires a
lilac-rose colour with hematoxylic eosine, and is perhaps comparable
with the granular substance of the neuroglia of Vertebrates.
The principal facts resulting from the preceding observations, and
which seem to us to be of some interest in general anatomy, are as
follows :—In the first place, the intimate mixture of the hypodermic
epithelial cells and of their basilar processes with the cells of the
nerve-fibres, from which results the difficulty of defining the brain
in a clear and certain manner; and the absence of any histological
character enabling us to distinguish the basilar fibrillee of the hypo-
dermic cells from the nervous fibres. It seems to us to be inter-
esting to point out these anatomical peculiarities, which remind us
of the condition of the nervous system in the larvee of Annelides*.—
Comptes Rendus, May 19, 1884, p. 1292.
* Kleinenberg, “ Origine du systéme nerveux central des Annelides,” in
Archives Italiennes de Biologie, tome i. p. 67.
Ann. & Mag. N. Hist. Ser. 5. Vol. xiii. 32
490 Miscellaneous.
On Manayunkia.
Prof. Leidy made some remarks on a specimen of Manayunkia,
of which he exhibited a drawing, and which had been recently
obtained by Mr, Edward Potts, from the mill-pond of Absecom
Creek, at Absecom, N. J. It was of especial interest as appa-
rently confirming the freshwater habit of a cephalobranch annelide.
The worm was contained in a tube attached to the midrib of a
decayed leaf, to which there were attached several similar but
empty tubes about 1 line long. The worm, 1°5 millim. long,
appears to be an immature form of Manayunkia speciosa. The
body consists of ten setigerous segments succeeding the head.
The latter supports two lophophores, each with ten tentacles, of
which none are conspicuously larger than the others. A pair of
eyes occupy the head, but no pigment spots exist along the base of
the tentacles. The podal sete are from two to four, but mostly
three, on each side of the segments. The podal hooks, but one on
each side of the setigerous segments, except the first of the latter,
which has none; and the last two, which have rows of six comb-
like hooks on each side. The worm is translucent white, and the
blood very pale green.
Ordinarily, Absecom pond is purely fresh water, and contains in
abundance the usual plants and animals characteristic of fresh
waters. Mr. Stuart Wood stated that in occasional extreme high
tides of Absecom Creek, the pond had been subjected to the overflow
of salt water—Proc. Acad. Nat. Sci. Philad., Dec. 1883, p. 302.
On a Mediterranean Species of Lingulinopsis. By Dr. L. G.
BornEMANN, Jun.
In 1860 Reuss established the genus Lingulinopsis for a Forami-
niferan intermediate between the families Rhabdoidex, Glanduli-
nid, and Cristellaroidee. He referred to this genus the form
previously described by him under the name of Lingulina bohemica
from the Pliner near Teplitz. Subsequently Schwager united with
it Amphistegina striata, Reuss, from the Neocomian of Westphalia.
The author now records the occurrence off Carloforte (in the island
of San Pietro, Sardinia) of a recent species of the genus, for which
he proposes the name of Lingulinopsis carlofortensis. It is a rather
large species, over 5 millim. long, and lives in great abundance on
the beds of coral in the above locality — Att: della Soc. Toscana di
Sci. Nat., Mem. vol. vi. p. 26.
491
INDEX to VOL. XIII.
ActinoLoey of the Atlantic Ocean,
remarks on the, 102, 416.
Allopora, new species of, 111, 468.
Amphileptus fasciola, on reproduc-
tion in, 416,
Amplexopora, new species of, 539.
Anacropora, description of the new
genus, 287.
Animal kingdom, on the classifica-
tion of the, 518.
Anosia, new species of, 185.
Aphides of the Elm, on the biolo-
gical evolution of the, 228.
Archer, Mr., on a new species of
Staurastrum, 145.
Arenicola Grubii, on the structure
of the otocysts of, 415,
Artaxa, new species of, 200.
Ascidia, on some new exotic simple,
424,
Asplanchna, new species of, 310.
Aulacochilus, new species of, 372.
Balanoglossus, on the development
of, 65,
Bateson, W., on the development of
Balanoglossus, 65,
Batrachians, new, 396.
Batrachospermum, on the fertiliza-
tion of, 15.
Beddard, F. E., on the genus Mega-
scolex, 398.
Belenogaster, new species of, 410.
Bell, Prof. F. J., on the species of
Pseudoboletia, 108; on some para-
sites of fishes from Madras, 173,
Blanus, new species of, 396,
Books, new :—Curtis’s Farm Insects,
63; Buckton’s British Aphides,
64; Hinde’s Fossil Sponges, 219 ;
Pascoe’s Notes on Natural Selec-
tion, 500; Kuntze’s Phytogeo-
genesis, 302; Proceedings of the
Belfast Naturalists’ Field Club,
413; Transactions of the Cumber-
land Association for the Advance-
ment of Literature and Science,
415; Macoun’s Catalogue of Cana-
dian Plants, 484.
Bornemann, L. G., on a Mediter-
ranean species of Lingulinopsis,
490,
Boulenger, G. A., on new species of
Reptiles and Batrachians, 396,
Brachionus, new species of, 309.
Bracon, new species of, 404,
Biitschli, Dr. G., on the Castreea-
theory, 372.
Bugula, new species of, 367.
Butler, A. G., on new Lepidoptera,
58, 171, 183, 278, 343.
Caduga, new species of, 58,
Cecilia, new species of, 398,
Callithamnion, on the fertilization of,
22.
Callopora, new species of, 120,
Calosiphonia, on the fertilization of,16,
Cambarus, on the so-called dimor-
phism in the genus, 147.
Camponotus pennsylyanicus, on the
habits of, 419.
Carter, H. J., remarks on some fresh-
water Sponges, 99; on the generic
characters of some new Sponges,
129; on Grantia ciliata, var. spini-
spiculum, 158; on the branched
and unbranched forms of the fresh-
492
water Sponges, 269; on the as-
sumed relationship of Parkeria to
Stromatopora, 553.
Catochrysops, new species of, 194.
Caulacanthus, on the fertilization of,
15.
Cautires, new species of, 281.
Cellepora, new species of, 56,
Cephalopoda, on the development of
the branchia in the, 67.
Cheetetes, new species of, 474.
Chalcotzenia, new species of, 371.
Chantrausia, on the fertilization of,
13.
Chasmina, new species of, 274.
Chatin, J., on a Nematode parasitic
on the common onion, 150.
Chroolepus umbrinwm, observations
on, 252.
Chrysops, new species of, 457.
Chylocladia, on the fertilization of,
23
Claus, C., on the ephyree of Cotylo-
rhiza and Rhizostoma, 175.
Coal, on the structure and formation
of, 299.
Coleoptera,
370, 479.
Colobus Kirkii, on the occurrence of,
307.
Comatula, on the development of
the, 510,
Conn, H. W., on sexual colour-
variation in Crustacea, 71; on a
Protozoéa stage in crab develop-
ment, 152.
Corallium, on the structure of the
skeleton in, 29.
Corals, new, 111, 117, 284, 292,
38.
Corals, on the relation of the pali of,
to the tentacles, 466 ; new Palzo-
zoic, 472.
Coral-soundings in the
Islands, on, 460.
Coreebus bifasciatus, on the sexual
differences of, 508.
Coscinoderma, characters of the ge-
nus, 129,
Cotylorhiza, on the development of
the ephyre of the, 175.
Crab development, on a Protozoéa
stage in, 152.
Crustacea, on sexual colour-variation
an, 74:
Daday, Dr. E. von, on Polythalamia
new, 128, 181, 276,
Solomon
IN DEX.
from inland salt water in Hungary,
307; on new forms of Rotatoria,
309.
Dall, Prof. W. H., on some Hydro-
corallinee from Alaska and Cali-
fornia, 467.
Dasypogon, new species of, 458.
Davis, J. W., on some fossil fishes,
145; on a new species of Ptycho-
lepis, 335; on a new genus of
fossil fishes from the Lias, 448.
Deep-sea dredging, results of, 225,
Dekayella, new species of, 341.
Delphinide, on a new genus of, 351.
Diaxenes, description of the new
genus, 128,
Dicotyledons, on Mesozoic, 383.
Dielis, new species of, 407.
Diplax, new species of, 455.
Diptera, on the ‘Challenger’ collec-
tion of, 456.
Distichopora, new species of, 113.
Dodonidia, description of the new
genus, 172.
Doleschallia, new species of, 59.
Dolley, C. S., on a cilio-flagellate
Infusorian recently observed in
drinking-water, 418.
Drasche, Dr. R. von, on some new
simple Ascidia, 424.
Dublin Microscopical Club, proceed-
ings of the, 140.
Dudresnaya, on the fertilization of,
16
Dumontia, on the fertilization of,
16.
Duncan, Prof. P. M., on Atlantic
Actinology, 416; on the relation
of the pali of corals to the tentacles,
466.
Echinomyia, new species of, 459.
Ketyon, emended characters of the
genus, 150,
Beiyanapt characters of the genus,
OU,
Epierus, new species of, 136.
Errina, new species of, 470.
Etheridge, R., jun., on some Paleeo-
zoic corals, 472.
Eunice Harassii, on the brain of, 488.
Fauna of New Zealand, on the origin
of the, 425.
Faunas, on the pelagic and deep, of
the lakes of Savoy, 69.
Faurot, M., on the anatomy of
Peachia hastata, 417.
INDEX.
Favositella, description of the new
genus, 472.
Faxon, W., on the so-called dimor-
phism in the genus Cambarus, 147.
Fishes, on some parasites of, 173;
new, 349; new fossil, 145, 335,
448,
Fistulipora, new species of, 119.
Flies, on a fungus infesting, 306.
Flora of New Zealand, on the origin
of the, 425.
Floridez, on the fertilization of the,
1, 80.
Foord, A. H., on new species of
Monticuliporoid Corals, 338; on
some Paleozoic Corals, 472.
Fungus, on a new species of, infest-
ing flies, 506.
Gasteropoda, on the operculum of
the, 304.
Gastreea-theory, remarks
372.
Gazella anglica, description of, 482.
Geological Society, proceedings of
the, 61, 145, 297, 481.
Gerbatha, new species of, 274.
Gerydus, new species of, 194.
Gleeosiphonia, on the fertilization of,
16.
Grantia ciliata, var. spinispiculum,
observations on, 153.
Guppy, H. B., on coral-soundings in
the Solomon Islands, 460.
Gyracanthus, notes on the genus, 37 ;
new species of, 44.
Hamadryas, new species of, 191.
Helota, new species of, 479.
Hetzerius, new species of, 157,
Heteronychus, new species of, 370.
Hincls, Rey. T., on the Polyzoa of
the Queen Charlotte Islands, 49,
203; on Prof, Seguenza’s list of
Tertiary Polyzoa, 265; on marine
Polyzoa, 356.
Hister, new species of, 154.
Histeride, new Japanese, 151.
Hololepta, new species of, 152.
Houssay, M., on the operculum of
the Gasteropoda, 304.
Hughes, Prof. T. M‘Kenny, on some
tracks of terrestrial and freshwater
animals, 62; on the so-called
Spongia paradoxica, 298.
Hutton, Capt. F. W., on the origin
of the Fauna and Flora of New
Zealand, 425.
on the,
493
Hydrocoralline from Alaska and
California, on some, 467.
Hymenoptera of the ‘ Challenger’
expedition, on the, 402.
Imhof, Dr. O. E., on the pelagic
and deep Faunas of the Lakes of
Savoy, 69.
Jamides, new species of, 346,
Joubin, L., on the development of
the branchia in the Cephalopoda,
67.
Jourdan, E., on the structure of the
otocysts of Arenicola Grubii, 415;
on the brain of Eunice Harassii
and its relations with the hypo-
dermis, 488,
Kidston, R., on a specimen of Peco-
pteris in circinate vernation, with
remarks on the genera Spiropteris
and Rhizomopteris, 75; on a
new species of Schutzia, 77.
Kirby, W. F., on the ‘ Challenger’
Hymenoptera, 402; on the ‘ Chal-
lenger’ Neuroptera, 453; on the
‘Challenger’ Diptera, 456; onthe
‘Chailenger’ Orthoptera, 476.
Kirk, Sir J., on the occurrence of
Colobus Kirkii, 307.
Laboulbéne, A., on the sexual diffe-
rences of Corcebus_bifasciatus,
308.
ee new species of, 657,
210.
Lamna, new species of, 349.
Lampides, new species of, 195.
Lancetes, new species of, 276.
Leidy, Prof., on a fungus infesting
flies, 306; on Manayunkia, 490.
Lepidoptera, new, 58, 171, 183, 273,
343.
Lepralia, new species of, 49, 360.
Leucophlceus, characters of the genus,
130.
Lewis, G., on new Japanese Histe-
ride, 131.
Lichtenstein, M., on new aphidio-
logical discoveries, 228.
Life, on the modern philosophical
conceptions of, 233.
Lindstrom, Prof. G., on the actino-
logy of the Atlantic Ocean, 102,
416,
Lingulinopsis, on a Mediterranean
species of, 490.
Lissolepis, description of the new
genus, 448.
494
Lycvena, new species of, 347,
McCook, Rev. Dr., on two new Cali-
fornian spiders and their nests,
229; on the mode in which a car-
penter-ant queen founds a formi-
cary, 419.
Madreporide, on the classificatory
value of growth and budding in
the, 284.
Manayunkia, on a specimen of,
490.
Mantis metallica, observations on,
34.
Margé, Dr. T., on the classification
of the animal kingdom, 313.
Marshall, Dr. W., on the gemmules
of the freshwater sponges, 163.
Megalichthys, on the affinities of,
483.
Megascolex, observations
genus, 398.
Membranipora, new species of, 210,
307.
Menipea, new species of, 208.
Metcalfe, A. T., on some vertebrate
remains from the Trias of Devon-
shire, 146.
Miall, Prof. L. C., on a specimen of
Megalichthys from the Yorkshire
Coal-field, 483.
Microhyla, new species of, 397,
Milne-Edwards, M., on some results
of the expedition of the ‘ Talis-
man,’ 223.
Monotrypa, new species of, 124,
338.
Moseleya, characters of the new
genus, 292.
Mucronella, new species of, 52.
Murray, J. A.,on the marine fauna
of Kurrachee, 348.
Naccaria, on the fertilization of, 15.
Napopora, characters of the new
genus, 296,
Necroscia, new species of, 477.
Nemotha, description of the new
genus, 35,
Neomeris, description of the new
genus, 351.
Neuroptera, on the ‘ Challenger’ col-
lection of, 455,
Newton, E. T., on the occurrence of
a new species of Gazella in the
Norwich Crag, 482.
Nicholson, Prof. H. A., on the
structure of the skeleton in the
on the
INDEX.
genera Corallium, Tubipora, and
Syringopora, 29; on some Monti-
euliporoid corals from the Upper
Silurian rocks, 117.
Nola, new species of, 274.
Notodoma, new species of, 156.
Odynerus, new species of, 409.
Olliff, A. S., on an African species of
Helota, 479.
Onion, on a Nematode parasitic on
the common, 150.
Onthophilus, new species of, 159.
Orley, Dr., on some parasites of fishes
from Madras, 178.
Orthoptera, on the ‘Challenger,’
476.
Owen, Sir R., on the skull and den-
tition of Tritylodon longzevus, 61 ;
on the cranial and vertebral cha-
racters of Plesiosuchus, 62; on
Rhytidosteus capensis, 481.
Palechthus, characters of the new
genus, 277.
Pamphila, new species of, 198.
Papilio, new species of, 197.
Parker, Dr. A. 8., on reproduction in
Amphileptus fasciola, 416.
Parkeria, on the assumed relationship
of, to Stromatopora, 353.
Peachia hastata, on the anatomy of,
417.
Pecopteris, on a specimen of, in cir-
cinate vernation, 73.
Pedicellinopsis, description of the
new genus, 363.
Pegella, new species of, 201.
Pelops, new species of, 279,
Pentarthrum, new species of, 279.
Pepsis, new species of, 408.
Peridinium, on a new species of,
418.
Perrier, E., on the development of
the Comatule, 310.
ee ies characters of the genus,
130.
Physogyra, characters of the new
genus, 293
Platysoma, new species of, 133.
Plesiosuchus, on the cranial and yer-
tebral characters of, 62.
Plocamium, on the fertilization of,
Peecilopharis, new species of, 370.
Polistes, new species of, 410.
Polysiphonia, on the fertilization of,
23
ae
INDEX.
Polythalamia from inland salt water
in Hungary, on, 307.
Polyzoa of the Queen Charlotte
Islands, on the, 49, 203; on Prof.
Seguenza’s list of Tertiary, 265 ;
on new marine, 356,
Porella, new species of, 51, 212,
361.
Potts, E., on freshwater Sponges as
improbable causes of the pollution
of river-water, 486.
Priocnemis, new species of, 408.
Pseudoboletia, on the species of,
108.
Pterothamnion, on the fertilization
of, 22.
Ptilocaulis, characters of the genus,
130.
Ptycholepis, new species of, 835,
Quelch, J. J., on new Stylasteride,
with remarks on some reéently
described forms, 111, 267; on
Schizoporella Ridleyi and S. sim-
plex, 215; on new genera and
species of reef-corals, 292.
Rana, new species of, 397.
Rana esculenta, on the influence of
physico-chemical agencies upon
the development of the tadpoles of,
2
Reptiles, new, 596,
Rhizomopteris, remarks on the genus,
76.
Rhizostoma, on the development of
the ephyre of, 175.
Rhytidosteus capensis, observations
on, 481.
Ridley, 8. O., on growth and budding
in the Madreporide, and on a new
genus, 284.
Rotatoria, new genera and species of,
309.
Salatura, new species of, 58.
Sandalolitha, characters of the new
genus, 294,
Schizaspidia, new species of, 403.
Schizocerca, characters of the new
genus, 309.
Schizoporella Ridleyi and S. simplex,
observations on, 215.
Schmitz, Prof. F., on the fertilization
of the Floridez, 1, 80.
Schnetzler, J. B., on an aerial Alga
inhabiting the bark of the vine,
232.
495
Schutzia, new species of, 77.
Scinaia, on the fertilization of, 13.
Scotosia, new species of, 275.
Seguenza’s, Prof. G., list of Tertiary
Polyzoa from Reggio, observations
on, 265,
Sharpe, Dr. B., on visual organs in
Solen, 148.
Smittia, new species of, 52.
Solen, on visual organs in, 148,
Spheerarthrum, characters of the new
genus, 281.
Spiders, on two new Californian,
229,
Spiramia, new species of, 202.
Spiropteris, remarks on the genus,
74.
Sponges, on some freshwater, 96;
characters of new genera of, 129 ;
on the gemmules of the freshwater,
163; on the branched and un-
branched forms of the freshwater,
269; notes on some freshwater,
486.
Spongia paradoxica, on the so-called,
298.
Staurastrum, new species of, 146.
Stenostoma, new species of, 596.
Stromatopora, on the assumed rela-
tionship of Parkeria to, 553.
Stylaster, new species of, 112.
Stylasteride, on new, with remarks
on some recently described forms,
111, 218, 267.
Sympheedra, new species of, 59.
Syringopora, on the structure of the
skeleton in, 29.
Tadpoles, on the influence of physico-
chemical agencies upon the deve-
lopment of, 72.
Tephrosia, new species of, 275.
Terias, new species of, 196.
Tichoseris, characters of the new
genus, 295.
Tomes, R. F., on the Madreporaria
of the White Lias, 483.
Traquair, Dr. R. H., on the genus
Gyracanthus, 87.
Triballus, new species of, 137.
Trichoplax adherens, observations
on, 381.
Trilobite, on the injured eye of a, 69.
Tritylodon longevus, on the skull
and dentition of, 61.
Tryponzus, new species of, 138.
496
Tubipora, on the structure of the
skeleton in, 29.
Tubulipora, new species of, 204.
Tylenchus, new species of, 150.
Vadebra, new species of, 191, 544.
Vejdovsky, Dr. F., on some fresh-
water sponges, 96.
Walcott, C. D., on the injured eye of
a Trilobite, 69.
Ward, L. F., on Mesozoic Dicoty-
ledons, 383.
Waterhouse, C. O., on new genera
and species of Coleoptera, 128,
276, 370,
LN DE xX.
Wethered, E., on the structure and
formation of coal, 299.
Wood-Mason, J., on the Mantis me-
tallica, 34.
Woodward, J. J., on the modern
philosophical conceptions of life,
Wright, B., on new Stylasteride,
218
Yung, E., on the influence of physico-
chemical agencies upon the deve-
lopment of the tadpoles of Rana
esculenta, 72.
END OF THE THIRTEENTH VOLUME.
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