t '•.■»•-
JANUARY, 1973
THE
NAUTILUS
Vol. 87
No. 1
A quarterly
devoted to
malacology and
the interests of
conchologists
ifcgical L?.^or5itory
JAN 2 61973
J
Founded 1889 by Henry A. Pilsbry. Continued by H. Burrington Baker.
Editors; R. Tucker Abbott and Charles B. Wurtz
EDITORIAL COMMITTEE
CONSULTING EDITORS
Dr. Arthur H. Clarke, Jr.
Department of Mollusks
National Museum of Canada
Ottawa, Ontario, Canada K1A-0M8
Dr. William J. Clench
Curator Emeritus
Museum of Comparative Zoology
Cambridge, Mass. 02138
Dr. William K. Emerson
Department of Living Invertebrates
The American Museum of Natural History
New York, New York 10024
Mr. Morris K. Jacobson
Department of Living Invertebrates
The American Museum of Natural History
New York, New York 1 0024
Dr. Aurele La Rocque
Department of Geology
The Ohio State University
Columbus, Ohio 43210
Dr. James H. McLean
Los Angeles County Museum of Natural History
900 Exposition Boulevard
Los Angeles, California 90007
Dr. Arthur S. Merrill
Biological Laboratory
National Marine Fisheries Service
Oxford, Maryland 21654
Dr. Donald R. Moore
Division of Marine Geology
School of Marine and Atmospheric Science
1 0 Rickenbacker Causeway
Miami, Florida 33149
Dr. Joseph Rosewater
Division of Mollusks
U. S. National Museum
Washington, D.C. 20560
Dr. G. Alan Solem
Department of Invertebrates
Field Museum of Natural History
Chicago, Illinois 60605
Dr. David H. Stansbery
Museum of Zoology
The Ohio State University
Columbus, Ohio 43210
Dr. Ruth D. Turner
Department of Mollusks
Museum of Comparative Zoology
Cambridge, Mass. 02138
Dr. Gilbert L. Voss
Division of Biology
School of Marine and Atmospheric Science
10 Rickenbacker Causeway
Miami, Florida 33149
EDITORS
Dr. R. Tucker Abbott
Delaware Museum of Natural History
Box 3937, GreenvQle, Delaware 19807
Dr. Charles B. Wurtz
3220 Penn Street
Philadelphia, Pennsylvania 19129
Mrs. Horace B. Baker
Business and Subscription Manager
1 1 Chelten Road
Havertown, Pennsylvania 19083
OFFICE OF PUBLICATION
Delaware Museum of Natural History
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Box 3937, Greenville, Delaware 19807
Second Class Postage paid at Wilmington, Delaware
Subscription Price: $7.00 (see inside back cover)
■^jft^!^P>\ THE
,, / ' NAUTILUS
(^ '■-■'-'.'' ,
io- \ Volume 87, number 1 --January 1973
CONTENTS '^
David L. West
Notes on the Development ofColus stimpsoni {Prosohr^nchia: Buccinidae) 1
T. S. Katsigianis and W. N. Harman
Variation in the Radular Teeth of Helisoma anceps(Menke) 5
Branley A. Branson
Significant Pelecypod Records from Oklahoma 8
James B. Sickel
A New Record of Corbicula manilensis (Philipp'i) in the Southern Atlantic Slope Region of Georgia ..11
David Bickel
Non-marine Mollusks and Two New Species of Pisidium from the Tongue River Formation
(Paleocene), North Dakota 13
John W. Ropes and Arthur S. Merrill
To What Extent Do Surf Clams Move? 19
William K. Emerson
LeoGeorgeHertlein(1898-1972), AnObituaryandFinalBibliography 22
John W. Clark, Jr.
The Problem of the Land Snail Genus Rabdotus in Texas Archeological Sites 24
Lothar Forcart
Noteson Veronicellidae and Athoracophoridae in the Field Museum of Natural History, Chicago ... .25
SHORT PAPERS
James L. Murphy
Cerion from an Archeological Site in Northern Ohio 28
J. P. E. Morrison
New Name for a Texas Hvdrobia 28
Dorothy E. Beetle
Phvsa acuta in Virginia 28
R. Tucker Abbott
Spread of Melanoides tuberculata (Thiaridae) 29
Dorothy E. Beetle
Fresh-water MoUusks from Coastal Virginia 29
Book Reviews
(oOPat Halliday,4; A. Feininger and W. K. Emerson, 12;S. and L.Goodman, 22; K.J. Boss, 29.
Obituary and News 27, 30
i
STATEMENT OF OWNERSHIP. MANAGEMENT AND CIR-
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1. Title of publication: THE NAUTILUS.
2. Date of filing, September 25, 1972.
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19807.
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6. Names and addresses of publisher, editor, and managing edi-
tor: Publisher, Mrs. Horace Burrington Baker, 11 Chelten
Rd., Havertown, Pa. 19083. Editor, R. Tucker Abbott, Dela-
ware Museum of Natural History, Box 3937, Greenville, De.
19807. Managingeditor, none.
7. Owner: Mrs. Horace Burrington Baker, 11 Chelten Rd.,
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Vol. 87(1)
THE NAUTILUS
NOTES ON THE DEVELOPMENT OF COLUS STIMPSONl
(PROSOBRANCHIA: BUCCINIDAE)'
David L. West
Marine Science Institute
Northeastern University
Nahant, Mass. 01908
ABSTRACT
The buccinid whelk of New England, Colus stimpsoni (March), feeds on the snails,
Littorina littorea (Linnej and Polinices heros (Say), and occasionally on damaged bi-
valves. In the laboratory, C. stimpsoni lays single capsules on rocks, each containing 4,000
■ 5,500 eggs, but with only 1 to 8 eventually developing into young snails. During five
years of observations, capsule-laying occurred from February to May. Development to a
shell length of 5 to 8 mm takes 5 to 6 months.
Colus stimpsoni (Morch, 1 867) ranges from Maine
to North Carolina along the Atlantic coast, and oc-
curs intertidally in its nortliernmost range. For the
past 5 years, a population of C. stimpsoni has been
maintained at the Marine Science Institute. The orig-
inal population and subsequent additions were col-
lected intertidally at Cobscook Bay State Park,
Edmunds, Maine and at Eastport, Maine. A few ob-
servations on the larval development are herein de-
scribed.
Littorina littorea (L.) serves as a food item in the
field and is used to maintain C. stimpsoni in the
laboratory as recorded by Riser (1969). However, it
will feed as well on Polinices heros (Say). The be-
havior of Colus wliile feeding on P. heros is the same
as for L. littorea (for description see Riser, 1969).
However, there is one important additional condition.
When P. heros is moving about and has its metapo-
dium extended, Colus cannot attack. The predator
cannot gain purchase when the prey's metapodium is
extended over the sheU. C. stimpsoni has also been
observed to feed on damaged bivalves and, on one oc-
casion, upon a molting hermit crab. Smaller snails
(less than 7 cm.) have also been observed to feed on
dead, gaping Mercenaria mercenaria (L.) In the labo-
ratory the smaller snails will feed also on the de-
posited egg capsules of its own species. Crowded con-
ditions in the aquaria may lend to this behavior.
Thorson (1935) suggested that the capsules of Colus
(=Sipho) curtus (Jeffreys) were attacked by various
Natica in East Greenland. However, it is possible that
'Contribution number 18 from the Marine Science
Institute.
the capsules were preyed upon by small Colus.
In the laboratory, C. stimpsoni deposits egg cap-
sules throughout the year with increased deposition
from February to May. Capsule-laying can be stimu-
lated by periods of starvation followed by abundant
food (similarly reported for Thais by D'Asaro, 1966).
Capsules are laid singly and attached to rocks, the
sides of aquaria, and occasionally on the shells of liv-
ing C stimpsoni. Each capsule contains approxi-
mately 4,000 to 5,500 eggs.
In surface view, the capsules (Fig. 1 ) are circular to
oval (10 - 16 mm. diameter) and, in side view, are
subhemispherical (4 - 8 mm. in height). The capsule
operculum (exit hole) is fusiform and measures 4-5
mm. in long axis and 3-4 mm. in short axis. When the
capsule is viewed from the side, the operculum is situ-
ated 1/3 - 2/3 the distance from the base to the apex.
Capsules are whitish hyaline in appearance with a yel-
low central portion containing the eggs. The capsule
surface is slightly undulated with irregular striations.
These egg capsules appear very similar to those of
Colus (=Sipho) islandicus (Gmelin) figured by
Thorson (1935: 14, Fig. 5). In cross section the cap-
sule wall is composed of 3 differentially staining lay-
ers and appears similar to the capsule wall of Ur-
osalpinx cinerea (Say) described by Tamarin and Car-
riker(1968).
Individual eggs measure 1 80-1 90 /n in diameter and
are densely packed with large yolk granules.
The number of young snails which develop in a
capsule varies from 1 to 8 (occasionally none) with an
average of 4. The remaining eggs serve as food for the
developing young. There is apparently no relation be-
tween the size of the capsule and the number of snails
THE NAUTILUS
January 1973
Vol. 87(1)
which develop. The largest capsules do not always
contain the largest numbers of developing young.
The first indication of embryos (which are young
veligers) within a capsule still attached to the sub-
strate is what appears to be an enlarged egg, 15-20
days after capsule deposition. The early veliger (figs.
2 & 3), after washing free from the surrounding eggs
and albumin, measure 700-800 /i in length and
400-500 11 across the head vesicle and foot. The
velum is small with the larval kidneys situated slightly
ventral and near the junction of the velum and
visceral mass.
As the veliger continues to ingest the nurse eggs,
the visceral mass increases in size at a rapid rate. The
head vesicle and foot enlarge slightly, and the velum
expands laterally (figs. 4 & 5).
Development is usually delayed at this stage until
all nurse eggs are ingested. However, this is variable
depending on the number of larvae per capsule and
the size of the capsule. In a large capsule with 4
veligers, development will continue before all nurse
eggs are consumed; whereas, in a small capsule with 4
veligers, all nurse eggs will be consumed before devel-
opment proceeds. The veligers may remain in this
Fig. 1. Egg capsule (i]Xo\ti%%\.\m^%on\.
Fig. 2. Early veliger. ventral view.
Fig. 3. Early veliger, lateral view.
Fig. 4. Late veliger, lateral view.
Vol. 87(1)
THE NAUTILUS
stage for 3 to 5 weeks, depending upon temperature
and the relative number of nurse eggs.
As development continues, whether all nurse eggs
are ingested or not, the velum and head vesicle en-
large, and the teloconch is laid down. The body be-
gins to coil, and the mantle cavity enlarges (figs. 6 &
7). The foot is relatively small, and there is no ap-
parent operculum at this stage. The digestive gland
also begins to differentiate at this stage. The ingested
nurse eggs can be seen through the shell.
As tlie foot develops and the operculum is laid
down, the velum enlarges laterally (fig. 8). The head
vesicle does not increase and appears relatively small.
The tentacles appear as small buds at the junction of
the velum and head esicle and the body cannot be
retracted into the shell at this stage.
Development is completed when 2'/i • 3 whorls are
formed. The protoconch is cast off just before or
shortly after the velum disappears. The apex of the
shell has a slight indentation where the protoconch
was (see fig. 10). All nurse eggs are consumed before
development is completed.
Fig. 5. Late veliger, ventral view.
Fig. 6. Early pediveliger, lateral view.
Fig. 7. Early pediveliger, ventral view.
Fig. 8. Pediveliger, ventral view.
THE NAUTILUS
January 1973
Vol. 87(1)
The young snails remain within the capsule until
the capsule operculum ruptures. In cases where this
has been observed, the snails aid in removing the
operculum by bumping against it as they wander
about within the capsule. Apparently the capsule
operculum is softened by external factors such as bac-
teria and fungi. Young snaOs exit when they discover
the hole in the capsule.
The shell of the emerging snail (figs. 9 & 10) is 5-8
mm. in height and 3-4 mm. wide. The aperture has an
undulating margin and about the first ^h of the body
whorl has fine spiral striae.
Total development time, from capsule deposition
to emergence, takes 5 to 6 months in the laboratory.
Development time apparently depends on temper-
ature as well as the number of young and the number
of nurse eggs available to the embryos. In all cases, all
nurse eggs were ingested before emergence. Usually
Figs. 9 & 10. Shell of emerging young Coins
stimp soni.
the young are of different sizes during development
and at emergence. Tlie development of C. stimpsoni is
similar to that of Buccinum undatum (L.) described
by Portmann (1925). Both C. stimpsoni and B. un-
datum emerge with about 3 whorls. However, the em-
bryos of C. stimpsoni are of unequal size whereas
Portmann (1925) indicates that the young of B. un-
datum are of equal size througliout development and
emergence.
LITERATURE CITED
D'Asaro, C. N. 1966. The egg capsules, embryo-
genesis, and early organogenesis of a common oys-
ter predator. Thais haemastoma floridana (Gastro-
poda: Prosobranchia). Bull Mar. Sci. 16: 884-914.
Morch, O. A. L. 1867. Faunula molluscorum Insu-
larum Faeoroensium. Beretning om de hidtil fra
Faeroerne bekjendte Bloddyr. Vidensk. medd. fra
Naturh. Forn. Kjb. 1867 No. 4-7: 67-111.
Portmann, A. 1925. Der Einfiuss der Nahreier auf die
Larvenentwicklung von Buccinum und Purpura. Z.
Morph. Okol. Tiere 3: 526-541.
Riser, N. W. 1969. Feeding behavior of some New
England marine gastropods. The Nautilus 82:
112-113.
Tamarin, A. and M. R. Carriker. 1968. The egg cap-
sule of the muricid gastropod Urosalpinx cinerea:
an integrated study of the wall by ordinary light,
polarized light, and electron microscrope. Jour. Ul-
trastr. Res. 21: 26-40.
Thorson, G. 1935. Studies on the egg-capsules and de-
velopment of Arctic marine prosobranchs. Medd.
Greenland. 10(K5): 1-71.
BOOK REVIEW
SNAILY VERSE by Pat Halliday. 48 pp., numerous
pen drawings; paperback. 1972. Volturna Press,
Wellington House, Peterhead, Aberdeenshire AB4
7JH, Scotland. 30 pence (about 90c U. S.).
This charming booklet of malacological rhymes
and limericks is the funniest to be published in a
century, and contains a remarkable amount of zoolo-
gical information, as well as several parodies of
English poets laureate. The numerous teleological
etchings add to the humor of the 39 conchological
poems.
Otala, Otala, 0, snail of Morocco!
Please answer me tliis, if you will -
Do you suffer a lot during summer sirocco?
Do you wish that the air was more chill?
etc . . .
R. Tucker Abbott
Delaware Museum of Natural History
Vol. 87(1)
THE NAUTILUS
VARIATION IN THE RADULAR TEETH
OF IIEUSOMA ANCEPS (Menke)
T. S. Katsigianis' and W. N. Harnian^
' Graduate student in Malacology, Biology Dept.,SUNY,Oneonta, New York 13820
^ Assoc. Prof., Aquatic Biology, Biology Dept.,SUNY,Oneonta, New York 13820
ABSTRACT
Variation in the structure of the radular teeth in several populations of Helisoma an-
ceps ( Menke j ( Pulmonata: Planorbidae) have been studied in central New York State.
A ratio was calculated, utilizing measurements obtained from a series of the first later-
al radular teeth from individuals in each population. The data show that interpopulation
variation is greater than intrapopulation variation, and that individual variation is less
than intrapopulation variation.
Interpopulation differences in the number and size of the cusps of the radular teeth of
H. anceps were observed. Two populations studied possess first lateral teeth with simple
entocones, mesocones and ectocones; another exhibits an accessory cusp on the distal
portion of the entocone, while a second shows accessory cusps both distal and proximal
on the entocone.
INTRODUCTION
The existence of intraspecific variation within spe-
cies is an important aspect in the study of freshwater
mollusks. Morphological differences of an ecopheno-
typic or genetic nature often are apparent. Since
populations of freshwater animals are normally sepa-
rated in isolated environments, it is relatively easy for
genetic differences to arise. This phenomenon is fur-
ther enhanced by the hermaphroditic characteristic of
pulmonale gastropods, which makes it possible for an
entire population to be founded by a single individual
having only a fraction of the genetic potential of the
parent population. However, due to the relatively
short duration of most freshwater biotopes, tliis gene-
tic variation does not usually proceed to the species
level (Hubendick, 1962).
It has often been logically assumed that the
morphology of the radulae of the omnivorous fresh-
water pulmonates is not subject to severe selection
pressures in the relatively homogeneous microhabitats
in which these organisms live. Therefore, the radular
teeth of these mollusks have long been considered
conservative characters and have always been an im-
portant part of the descriptions of these species [e.g.,
figure 1 illustrates the first lateral tooth of Helisoma
antrosa (=anceps) (Menke) from Baker's (1928)
description of the species] .
A comparative study of the radular teeth of
Lymnaea peregra (MuUer) (Pulmonata: Lymnaeidae)
(Berrie, 1959) showed that although the structure of
the teeth on the same radula, and within the same
population exhibited variation, this was greatly ex-
ceeded by interpopulation differences. In fact, there
was often statistically significant differences between
populations.
This work was initiated to determine if differences
could be observed between the structure of the radu-
lar teeth in four populations of Helisoma anceps
(Menke) (Pulmonata; Planorbidae) occurring within a
20 mile radius of Oneonta, Otsego Co., New York,
U.S.A.
METHODS
Samples were taken at; 1. WUber Reservoir,
Oneonta, Otsego Co., Susquehanna watershed; 2.
Susquehanna River, Oneonta, Otsego Co., Susque-
hanna watershed; 3. Moe Pond, SUNY at Oneonta Bi-
ological Field Station, Cooperstown, Otsego Co.,
Susquehanna watershed; 4. Delaware River, Walton,
Delaware Co., Delaware watershed (figure 2).
Upon collection, snails of approximately the same
size were preserved in 70% ethanol. The radula of
each snail was removed from the buccal mass by heat-
ing it in a concentrated potassium hydroxide solu-
tion. Each radula was then rinsed in water foUowed
by 90% ethanol and mounted unstained in euparol.
An eyepiece micrometer was used to make measure-
ments of individual teeth. All measurements were tak-
en at 970X with an oil immersion lens on a phase
contrast microscope.
THE NAUTILUS
January 1973
Vol. 87(1)
FIGURE I. First lateral tooth of H. anceps showing measurements.
Ec = ectocone. Me = mesocone. En = entocone (modified from
Baker. 19281.
FIGURE II. A portion of New York State showing the location of
each population ■ Wilber Reservoir, ♦ Susquehanna River, • Moe
Pond, A Delaware River.
We calculated the B/E ratio as shown in figure 1,
where B is the distance between the tips of the ecto-
cone and the entocone, and E is the height of the me-
socone from its junction with the ectocone to its tip.
These measurements were taken on the first lateral
teeth of one transverse row of teeth. Teeth from
three rows, five rows apart, were studied on each
radula. Six individuals were chosen from each popula-
tion, therefore, a total of 36 teeth were studied from
each. AH teeth measured were from the central por-
tion of the radulae. It is in this region that the teeth
are fully developed, yet not severely eroded.
These are the same methods utilized by Berrie
(1959). He calculated the B/E and F/E ratios (figure
1) on the first and sixth lateral teeth of each snail but
concluded that the calculafion of the F/E ratio and
the analysis of measurements on the sixth tooth were
not necessary. The F/E ratio varied independently
from the B/E ratio as did the data collected from the
first and sixth lateral teeth.
Figure III. First lateral radular teeth of H. anceps (drawn to scale,
1940x). A = Delware River, B = Moe Pond.
RESULTS
The means, standard errors, and standard devia-
tions of the calculated B/E ratio are given in Table I.
By adopfing the method used by Berrie (1959),
the interpopulation differences have been estimated.
Tliis analysis utilizes the following ratio.
Mean - Mean
Standard Error + Standard Error
1 2
A value of more than two for this ratio indicates a
significant interpopulation difference while a value of
three or more indicates that the populations are ob-
viously different. Table II summarizes these results.
In all cases a significant difference exists between
each population. Althougli the Delaware River popu-
lation is from an entirely different watershed than the
other groups considered, it is extremely different
only from the Wilber Reservoir population. There is
no correlation between the proximity of each popula-
tion and the degree of interpopulation variation.
Tlie Moe Pond population was selected to examine
the intrapopulation variation and the differences that
\'ol. S-( 1 )
THE NAUTILUS
occur bcivvcoii the iccth on the sumo r;idula. To ac-
comphsh this, the stiiiulaid deviation lor the entire
population was compaiei.1 to the standard deviation
ot" tiie teeth on one ladula of one snail trom that
population (Table 3). The standard deviation is much
greater between the teeth from several members of
the population than from the teeth of one individual,
which parallels Berrie's results with /,. peregra. This
indicates less variation between the radular teeth of
each individual than between the radular teeth of the
members of the population.
DISCUSSION
Althougli there were not as many populations con-
sidered in this work as were studied by Berrie ( 1959).
and although the populations are geographically
much closer together, the results obtained are similar.
The data show that interpopulation variation in the
B/E ratio of the first lateral radular teeth of local
populations of H. anceps is greater than intrapopu-
1; tion variation, and that individual variation is less
than intrapopulation variation.
Interesting interpopulation differences in the num-
ber and size of cusps of the first lateral teeth of //.
anceps have been observed. Figure 3 illustrates teeth
from snails in two of the four populations studied.
Each tooth was drawn with the aid of a Whipple
micrometer in a phase contrast microscope at 1940X.
All teeth are drawn to scale. They should be com-
pared with figure I, showing Baker's ( 1928) typical
//. anceps. Note the three cusps on the entocone of
the tooth representing the Moe Pond population. This
is the only population studied which had teeth that
exhibited this morphology. The size of the marginal
cusps on the entocone vary considerably. In some
cases all three cusps are of equal size, in others the
accessory cusps are much smaller. Other variations
within this population include teeth which entirely
lack the marginal cusps on the entocone and others
which have a small cusp between the mesocone and
ectocone. All of these variations may appear on the
same radula. The population from the Delaware River
exhibits teeth with one marginal cusp on the ento-
cone. However, some individuals in that population
show teeth having only the simple ectocone. inesti-
cone. and entocone more typical of the Wilber Reser-
voir and Susquehanna River populations. The latter
populations never exhibited accessory cusps on the
first lateral teeth of their radulae and were essentially
the same as the tooth illustrated in figure I.
LITERATURE CITED
Baker, F. C. 1928. The freshwater mollusca of Wis-
consin, Pt. I. Gastropoda. Wisconsin Gcol. Nat.
Hist. Suiv. Bui. 70(1): I -.507, pi. 1-28.
Berrie. A D. 1959. Variation in the radula of the
freshwater snail Lyninaca peregra (Mliller) from
northwestern Europe. Arkiv. for Zool. 12(27):
391-404.
Hiibeiidick, B. 1962. Aspects on the diversity of the
fresh-water fauna. Oikos.l3(2): 251-261.
Table I. Means, standard errors and standard deviations of
the B/E ratio for the first lateral tooth.
Table II. Differences between the means of the first
lateral teeth for the calculated B/E ratio.
Table III. The variation between the teeth of the six
Moe Pond specimens as compared to one specimen from
Moe Pond. Means, standard errors and standard deviations
are given.
THE NAUTILUS
January 1973
Vol. 87(1)
SIGNIFICANT PELECYPOD RECORDS FROM OKLAHOMA
Branley A. Branson
Eastern Kentucky University
Richmond. Kentuci<y 40475'
ABSTRACT
34 species of Unionidae and one Sphaerium are reported from the Ouachita Mountai:i
river drainages of southeastern Oklahonw, and all show a relationship with the fauna of
the lower Mississippi Valley, rather than the Ozarkian Assemblage. Construction plans for
the Arkansas River threaten these species.
In a previous paper ( 1966), I indicated that the en-
tire moUuscan fauna of the Oklahoma Ozarks (as well
as that of adjacent Kansas) belonged to van der
Schalie's (1950) so-called Ozarkian assemblage, and
that the fauna was probably most closely related to
that of the Cumberland region. However, there is at
least a small segment of this assemblage which reflects
a lower Mississippi Valley relationship (Branson,
1963; 1970).
The fauna of Ouachita Mountain streams, and of
those tlowing through the Gulf Coastal Plains south
of them, in extreme southeastern Oklahoma is an-
other matter. The relationship here is not Ozarkian.
but is primarily with the lower Mississippi Valley, the
southeastern U. S., and, of course, Texas and Louisi-
ana. Isely (1925) indicated some of this in reporting
Ptychobranchus clintuncnsis. P. phaseolus (merely a
southern form of P. fasciolarc, in my opinion) and
Lampsilis hydiana from several Red River tributaries.
Hubricht (1965) and I (1963) reported Eupera
singleyi from southeastern Oklahoma, a species occur-
ring mainly in northern Florida and adjacent Georgia,
and southern Louisiana and Texas.
Over the years, several interesting pelecypod
records have accumulated in the author's files, rec-
ords which lend some weiglit to the comments made
above. Most of these records resulted from collections
secured while I was on the staff of the University of
Oklahoma Biological Station, Willis, Oklahoma, to
which I am indebted for laboratory facilities and vehi-
cles. I am also grateful to Drs. J P. E. Morrison and
Joseph Rosewater, Division of Mollusks, U. S. Nation-
al Museum, for verifications and identifications. The
entire collection (plus many others) herein discussed
' ConI libulion from Fisheries Management.
Department of Biological Sciences.
reside under accession number 23470 at the U. S. Na-
tional Museum. Records for 20 genera and 34 unionid
species, and one sphaeriid species are presented
below.
COLLECTING STATIONS
In the annotations the following form is used:
3(A), 2(B), etc. The Arabic numeral indicates the
number secured, and the letter in parentheses refers
to the station number as listed below: (A) 17 April
1959, Machire Creek, State Hwy 31 crossing, Haskell
Co.. Oklahoma; (B) 3 May 1959, Illinois River, 5 M
east of TahlequalT, Cherokee Co., Oklahoma: (C) 16
May 1960, Grand Lake (Lake O" the Cherokees),
Delaware Co.. Oklahoma; (D) 11 June 1960, Slate
ford. Poteau River, Leflore Co., Oklalioma; (E) 17
April 1959, Mountain Fork River, just above mouth,
McCurtain Co.. Oklahoma; (F) 22 April 1959. Moun-
tain Fork River, T75, R6E. SIO, McCurtain Co.. Ok-
lahoma; (G) 6 July 1952. Little River, between
Broken Bow and Idabel, U. S. 70 crossing. McCurtain
Co., Oklahoma; (H) 24 April 1955, Kiamichi River,
State Hway 2 crossing, McCurtain Co., Oklahoma; (1)
2 September 1955, Lost Creek, near Wyandotte, Ot-
tawa Co., Oklahoma; (J) 16 March 1955, Lake Carl
Blackwell, Payne Co.. Oklahoma; (K) 7 May 1960,
Honey Creek, Camp Classen. Arbuckle Mountains,
Murray Co., Oklahoma; (L) 6 May 1958, Water fall
Creek, just east of Idabel. State Hwy 21, McCurtain
Co., Oklahoma; (M) 28 June I960, Blue River, at
Connoi-ville, Johnston Co., Oklahoma; (N) 6 June
1960, Muddy Boggy Creek, 1 M north of Jessie
Pontotoc Co., Oklahoma; (O) 28 June I960, Moun-
tain Fork River, 6 M southwest of Smithville, State
Hway 21. McCurtain Co., Oklahoma; (P) 24 July
I960. Yashau Creek, 3 M south of Broken Bow, U. S.
70, McCurtain Co., Oklahoma; (Q) II June 1959,
Pennington Creek, 5 M north of Tishamingo,
Johnston Co.. Oklahoma.
Vol. S7(l)
THE NAUTILUS
UNIONIDAE
1. Strophiius uihhilatus Say. Collections: 1 1(B). A
common species througliout the Ozarks, in lowland,
mudbottomed streams with a relatively low profile.
2. Aiiodonta imbecilis Say. Collections: 4(L). Very
dark, chlorophyll-green with indistinct, broad rays;
locally abundant in vegetated backwaters.
3. Anodonta grandis Say. Collections: 1(C); 1(0).
4. Lasmigona complaiiata Barnes. Collections;
1(1). This species, nowhere exceptionally abundant,
gives way in numbers to the next species in southeast-
ern Oklahoma.
5. Lasmigona costata Rafinesque. Collections:
1(0).
6. Throgoiiia verrucosa Rafinesque. Collections;
3(A); 1(E); 1(F); 4(H). A common species through-
out the watersheds of eastern Oklahoma, but absent
in the far west.
7. Fusconaia ccrina (Conrad). Collections: 25(B);
1(M). The distribution of this interesting little
unionid demands more intensive study. The species
was. and probably still is. abundant in the Little Red
River of Arkansas (Call, 1895), southern Louisiana
and Mississippi (Meek, 1896). and clear streams of
east Texas (Murray and Ray, l%8). In most of the
streams of Oklahoma, F. flava outnumbers F. ceriua,
but the latter is quite abundant in the Illinois River
(Ozarks) and common in Blue River (Red River
System). Probably should be synonomized with F.
Jlava. Blue River is a typical stream with regard to
most of the other drainages in its vicinity. It is clear
and spring-fed. and has several relicts of fishes, such
as Etheostoma microperca, Etheostoma radiosum,
Notropis chrysocephahis, and others. The clam fauna,
several representatives of which are listed here, may
likewise be considered in part to be relict.
8. Quadnda pustulosa Lea. Collections: 3(B); 2(F);
3(0).
9. Quadnda cylindrica Say. Collections: 4(F);
l(M). Another relict form and locally common in
Blue River. The next sizable populations of this clam
are found in Mountain Fork and Little Rivers of
McCurtain County.
10. Quadnila melaneiira ( Rafinesque). Collections;
1(H).
11. Plectomerus trapezoides (Lea). Collections:
1(F). This specimen, representing several collected,
was diagnosed as P. dombeyaiiits by the U. S. Nation-
al Museum, a form relegated to synonomy by Murray
and Ray (1968), whom I follow. Strecker (1931)
found this species to be higlily variable in east Texas,
and the same is surely true of adjacent populations in
Oklahoma. P. intcrniptus (Say) is a synonym.
1 2. Amblema perplicata (Conrad). Collections:
2(F). Merely a "washboard" variation of A. costata.
13. Aiid^lcnw costata (Rafinesque). Collections:
1(E); 1(F); 1(H); 1(0). Very common at all locaHfies
(riffles).
14. Plcurobciiia cordatum (Rafinesque). Col-
lections: 1(F); 2(0), but very common. These spec-
imens are of the P. c. catilus (Conrad) form, but I
consider this, as well as P. coccineitm (Conrad), P.
pyramidatum (Lea) and P. c. solidum (Conrad) to be
ecotypes rather than races or spepies.
I 5. Pleurobema aiitillus (Conrad). Collections:
1(F). Merely a southern variety of P. cordatum
16. Elliptio dilatatus (Rafinesque). Collections:
1(D).
1 7. Uniomems tetralasmus (Say). Collections:
3(F); 12(J). In most lakes and ponds of central and
western Oklahoma.
18. Ptychobranchus clintonensis (Simpson). Col-
lections: 5(F) (Common). Simpson (1914) delimited
the range of this southern form as the Little Red
River of Arkansas and, questionably, west to Okla-
homa. It is probably P. phaseolus (HUdreth).
19. Proptera alata (Say). Collections: 1(B); 1(C).
20. Proptera (Leptodeaj ohiensis (Rafinesque).
Collections: 6(C). Questionably distinct from P.
laevissima ( Lea ).
21. Proptera (Leptodeaj fragilis (Rafinesque). Col-
lections: 1(F) (Common).
22. Proptera (Leptodeaj amphichaema (Frierson).
Collections: 1(F). An interesting species, common in
Texas (Murray and Ray, 1968; Strecker, 1931).
23. Proptera ( Proptera j purpcrata (Lamarck). Col-
lections: 7(E); 5(F).
24. Tntncilla pcriniculata (Rafinesque). Collec-
tions; 2(F). I cannot believe this form is distinct from
T. donaciformis ( Lea ).
25. Caninculina pan'a (Barnes). Collections: 1(H);
4(J); 2(L). Common in small creeks and ponds. See
remarks below.
26. Caninculina rc.Yffs«;5/s ( Lea). Collections: l(P)
(but common). Altliougli Murray and Ray (1968)
consider this form a subspecies of C. pan'a, and
Strecker (1931) opinioned that typical L. pan'a was
not known from Texas, I have found both forms to-
gether in northeastern Texas, and Meek (1896) re-
10
THE NAUTILUS
January 1973
Vol. 87 (i:
ported C texasensis to dominate the Caninculina
populations in portions of the abandoned channel of
the St. Francis River near Greenway, Arkansas; both
species were present.
27. Lampsilis anodontoides Lea. Collections: 3(A).
28. Lampsilis liiteola Lamarck. Collections: 2(C);
1(E); 2(K); 6(M); 1(0) (very common).
29. Lampsilis hydianus (Lea). Collections: 2(E);
3(F) (common); 1(0). Tliis species, still common in
the St. Francis and Saline Rivers of Arkansas (Call,
1895), Texas tributaries of the Red River (Strecker,
1931), is characteristic of the lower Mississippi Drain-
age (Louisiana, Texas, Arkansas and neigliboring
states) (Coker, 1919).
30. Lampsilis (Villosa) lienosa (Conrad). Collec-
tions: 2(E); 4(F) (common). This species, with a type
locality in southern Alabama (Clench and Turner,
1956), has a rather wide distribution in the Ohio and
Mississippi basins of Kentucky, Red and Saline rivers
of Texas (Strecker, 1931) (higlily variable), southern
Arkansas (Meek, 1896), and Oklahoma. The habitat is
invariably in mud.
31. Lampsilis cardiiim satuma (Lea). Collections:
1(F) (common). Probably a synonym of Lampsilis
ventricosa (Barnes).
32. Ligumia subrostrata (Say). Collections: 4(F);
1(H).
33. Obovaria jacksoniana Frierson. Collections:
5(F); 1(0) (common in both localities). A species
characteristic of the Pearl and Yalabusha rivers of
Mississippi.
34. Actinonais carinata (Barnes). Collections:
1(C); 4(E); 1(G); 1(0). Specimens from southeastern
Oklahoma are almost invariably referred to A. c.
gibba (Simpson).
SPHAERIIDAE
35. Sphaerium partumeium (Say). Collections:
4(K); 26(M); 2(N); 3(Q). Generally distributed in the
eastern two-thirds of the state.
Discussion
As Meek (18%) indicated in his appraisal of some
pelecypod faunules in southern Arkansas, many of
the species listed herein have a decidedly southern re-
lationship when compared with populations in north-
eastern Oklahoma. Regardless of their systematic dis-
tinctness as full-species, the following nominate forms
indicate southern affinity: Pleurobema antillus,
Ptychobranchus clintonense, Proptera amphichaema.
Proptera purpitrata, Carnnculina texasensis, Lampsilis
hydianus, L. (villosa) lienosa, Actinonais carinata
gibba, and Obovaria jacksoniana.
In view of the extensive habitat modification such
as dam constructions and the opening of the seaway
in the main Arkansas River, it is imperative that much
field work be accomplished in the Ouachita drainages,
particularly in the Poteau, Mountain Fork and Little
Rivers, before it is too late.
LITERATURE CITED
Branson, B. A. 1963. New Mollusk records from Ok-
lahoma and their Zoogeographical Significance.
Trans. Kansas Acad. Sci. 66: 501-512.
Branson, B. A. 1966. A partial Biological Survey of
the Spring River Drainage in Kansas, Oklahoma
and Missouri. Part I, Collecting sites, basic limnolo-
gical data, and mollusks. Proc. Kansas Acad. Sci.
69: 242-293.
Branson, B. A. 1970. Glebula in Oklahoma. Sterkiana
36:25.
Call, R. E. 1895. A study of the Unionidae of Arkan-
sas, with Incidental Reference to their Distribution
in the Mississippi Valley, trans. Acad. Sci. St.
Louis 8: 1-65.
Clench. W. J. and R. D. Turner. 1956. Freshwater
Mollusks of Alabama, Georgia and Florida, from
the Escambia to the Suwannee River. Bull. Fla.
State Mus. 1:97-239.
Coker, R. E. 1919. Freshwater Mussel Industries of
the United States. Bull. Bur. Fish. 36:1 1-89.
Hubricht, L. 1965. Eupera singlegi in Oklahoma.
Nautilus 78:106.
Isely, F. B. 1925. The Freshwater Mussel Fauna of
Eastern Oklahoma. Proc. Okla. Acac. Sci.
4:43-118.
Meek, S. E. 1 896. A List of Fishes and Mollusks Col-
lected in Arkansas and Indian Territory in 1894.
Bull. U. S. Fish. Comm. 1895:341-349.
Murray, H. D. and E. C. Ray. 1968. Checklist of
Freshwater and Land Mollusks of Texas. Sterkiana
30:25-42.
Simpson, C. T. 1914. A Descriptive Catalogue of the
Naiades or Peariy Freshwater Mussels. Bryant
Walker, Detroit, Mich. 1 540 p.
Strecker, J. K. 1931. The Distribution of the Naiades,
or pearly Freshwater Mussels, of Texas. Baylor
Univ. Mus. Sp. Bull. 2:1-71.
Van der Schalie, H. and A. 1950. The Mussels of the
Mississippi River. Amer. Midi. Nat. 44: 448-466.
Vol. .S7(l)
THE NAUTILUS
II
A NEW RECORD OF CORlilCULA MANILENSIS (PHILIPPI) IN THE
SOUTHERN ATLANTIC SLOPE REGION OF GEORGIA
James B. Sickel
Emory University
Department of Biology
Atlanta, Georgia 30322
ABSTRACT
Basal (III previous extensive surveys, it appears that the freshwater clam, Corbicula
manilensis (Philippi), was introduced into the Altamaha River system of Georgia in 1968,
initially into the Ocmulgec River from which it has spread downstream into the Altamaha
River, being found there for the first time in the summer of 1971. This is a first record of
this Asian species occurring in the Southern Atlantic Slope region.
The range of Corbicula manilensis (Philippi) con-
tinues to expand and has finally reached the Southern
Atlantic Slope region, an extension of its range from
the Gulf of Mexico drainage. As of last year, Sinclair
(1971) excluded the Atlantic Slope region from the
known range of Corbicula. In 1968 the author
(Sickel, 1969) made extensive collections of bivalves
in all habitat types from the Altamaha River, Appling
County, Georgia, between River Mile 113 and 118.
Ten species of unionids were found but no Corbicula.
Recent collections have shown Corbicula is now in
the Altamaha River system, both in the Ocmulgee
River and the Altamaha River itself.
On October 15, 1971, while collecting in the Alta-
maha system, the author found one Corbicula mani-
lensis shell on a sandbar in the Ocmulgee River three
miles from its confluence with the Oconee River at
which point the Altamaha begins. Shell annual rings
are not absolute determinants of age since they are
frequently indistinct, but based on what appear to be
annual rings, i.e., variations in the width of concentric
ridges, and the size, 10.0 x 8.6 x 6.3 mm., the shell is
estimated to be two years old and to have died in the
spring of 1971.
While collecting in the Flint River, Crawford
County, on November 4, 1971, the author found an
abundance of Corbicula manilensis. The Flint River is
a part of the Apalachicola River system in the Gulf
drainage and is not connected with the Altamaha
system, but tributaries of each reach within a mile of
the other. The Flint River population was in coarse
sand along the upstream end of most sandbars where
the sandy bottom was relatively stable. Using a view-
ing box in shallow water and viewing a 1 sq. ft. area.
10 to 15 adult Corbicula could be seen in any square
foot area chosen within the favorable habitat. Along
the middle and downstream reaches of the sandbars
fewer Corbicula were found, and scattered among
them were the following unionids: Lampsilis ano-
dontoides floridensis (Lea), Lampsilis binominatus
(Simp.), and Quincuncina infucata {Comad). Wliere the
Corbicula were most dense there were no unionids,
even though the habitat appeared suitable. This indi-
cates some form of competition, and it is unlikely to
be simply spatial competition since the size of Cor-
bicula and its density did not appear to be great
enougli to exclude the much larger unionids.
The adult Corbicula in the Flint River were still
expelling veliger larvae on the date collected. This ex-
tended breeding season is probably common in south-
ern rivers and means that control measures taken by
industry will have to be extended correspondingly.
In the Altamaha River, Appling County, at one of
the same sites where the author collected unionids in
1968, five juvenile Corbicula were found on Decem-
ber 15, 1971. Using a modified Peterson dredge, sam-
ples were taken on sandy and muddy bottom. The
Corbicula were found only in coarse sand near the
bank where the sand grades into mud. Six grab sam-
ples taken at one site produced five Corbicula which
ranged in length from 6.0 mm. to 7.8 mm. Each still
retained a byssal thread and had the characteristic
purple rays of the juveniles. They were obviously in
their first year of development.
The first report of Corbicula in the Altamaha came
from Drs. Donald C. Scott and James Schindler, Uni-
versity of Georgia (personal communication), who
found several young specimens while sampling in
i:
THE NAUTILUS
January 1 973
Vol. 87(1)
August, 1971, near the same area where the author
collected.
Corbicula nianileiisis is not yet abundant in the
Altamalia River. No adults over 2 years old have been
found. Many sites have been examined in the Alta-
maha and lower Ocmulgee in which Corbicula has not
been found.
The author proposes that Corbicula was intro-
duced into the Ocmulgee River by overland transfer
from the Flint River in 1968 or 1969. This transfer
could have occurred by fishermen who frequent both
rivers and use mussels for bait or accidentally in the
sand dumped into boats, possibly from anchors or
nets. One fertile adult could produce enougli off-
spring to establish a breeding population from which
veligers would be carried downstream to populate the
entire Altamalia to the Atlantic. It will be only a mat-
ter of time before Corbicula moves northward to in-
habit the remainder of the Southern Atlantic Slope
region.
Appreciation is expressed to John G. Adams and
the Georgia Power Company for the boat, collecting
equipment, and facilities so graciously provided for
the Altamaha River collections.
LITERATURE CITED
Sickcl, J. B. 1969. A survey of the mussel populations
(Unionidae) and Protozoa of the Altamaha River
with reference to their use in monitoring environ-
mental changes. MS Thesis. Emory University,
Atlanta.
Sinclair, R. M. l^?!. Annotated bibliography on the
exotic bivalve Corbicula in North America,
1900-1971. Sterkiana 43:11-18.
BOOK REVIEW
SHELLS. Photography by Andreas Feininger, text by
William K. Emerson. A Studio Book, the Vikmg
Press, New York. 295 pp. (including the plates),
175 pis. (including 32 in color), 7 numbered and
194 unnumbered figs. 1972. $27.50.
This is a large format (12 3/8" x 10") book of
photographs of marine moUusk shells, chosen by a
distinguished photographer "not from the point of
view of the scientist but from that of the engineer in-
trigued by structure and the interdependence of func-
tion and form, and from the point of view of the
artist who is fascinated by shape and design." It is
said to be "a shell-appreciation book" differing from
other shell books which "are too much preoccupied
with facts."
Most of the photographs are indeed spectacular.
They are grouped around chapters with the following
lieadings: Forms of the Sea; an Infinite Variety of
Shapes; Carrier Shells; the Structure of Sliells; the
Spiral; the Color of Shells; the Surface Texture of
Shells; Knobs and Spines, and Ornamental Design.
Magnifications vary greatly, and the shells are orient-
ed in all sorts of positions, resting im sand, gravel,
boulders, or glass bespattered with water, sometimes
with a background of sky or cloud. Not a single shell
is shown alive or in its natural habitat.
There is an elementary Introduction to malacology
and the text following it parallels fairly well the se-
quence of photographs, diverting in places to such
subjects as fluorescence. There is no first-hand in-
formation about the biology of mollusks. The plate
captions consist solely of the scientific name and a
reference number relating it to the systematically ar-
ranged catalog at the end. Only by referring to the
latter would the novice learn that the Haliotis shells
shown on pis. 1 19 and 1 20 are polished. Most of the
shells in the catalog are refigured at natural size and
in more conventional orientations. There are also a
glossary, bibliography and index.
The Foreward unwisely states that the text is
"scientifically accurate down to the last detail." The
phyletic successions of marine bivalves and snails
(figs. 2 and 3) are grossly misleading. Two entirely
different species on pi. 101 each are identified as
Comis maldivus Hwass. Various scientific names are
misattributed to authors, and various adjectival speci-
fic names disagree in gender with the generic names.
Vermicularia is wrongly included in the Vernietidae.
How well does this book achieve its objective of
being "a complement to all other kinds of shell
books"? It differs little in inieiii from The Shell; Five
Hundred Million Years of Inspired Design by Stix.
Stix and Abbott (l')68). Both of these are modern
photographic counterparts of the type of shell book
begun by Buonanni in 1084: Rccrcario Mentis et
Oculi. Thus there is nothing unique about the
Feininger-Emcrson book; the photographs are its
iiKist redeeming feature.
Robert Robertson
Academy of Natural Sciences of Philadelphia
Vol. 87(1)
THE NAUTILUS
13
NON-MARINE MOLLUSKS AND TWO NEW SPECIES OF PISIDIUM FROM THE TONGUE
RIVER FORMATION (PALEOCENE), NORTH DAKOTA.
David Bickel
Science Division
Minot State College
Minot, North Dakota 58701
ABSTRACT
Fifteen taxa of Paleocene freshwater Mollusca were recovered from relatively soft
carbonate sediments of the Tongue River Fommtion (Paleocene: Fort Union Group). The
beds, exposed at two sites in southern Ward County, North Dakota, apparently accumu-
lated in a small hard-water lake. The faunule is discussed and illustrated. Unlike the few
previously described species of Pisidium from early Tertiary rocks, preservation of Pisi-
dium wardensis and Pisidium russelli n. spp. is good enough to permit detailed description
of their hinge morphology.
INTRODUCTION
The Late Cretaceous and early Tertiary deposits in
the North Dakota portion of the Williston Basin
record a conformable transition from marine to
brackish water to non-marine sediments. The Fort
Union Group includes Paleocene rocks in North
Dakota and occurs in the western half of the state
and on an outlier in northeastern North Dakota.
These strata in North Dakota include from base to
top the Tullock. Ludlow, Cannonball, Tongue River,
and Sentinel Butte Formations. All are of alluvial
origin except for the Cannonball Formation which
apparently accumulated in an early Tertiary relic or
rejuvenation of the Cretaceous seaway that crossed
the midcontinent region. The Tongue River Forma-
tion was deposited over Tullock, Ludlow, and Can-
nonball sediments by a system of streams flowing
from a western source with low gradients and veloci-
ties (Royce, 1970). Tongue River sediments are most-
ly poorly consolidated yellowish sUts and clays with
lesser amounts of sand, lignite coal, and limestone.
Thick units that formed in backswamp and floodplain
environments characterize the formation. Thick
deposits of glacial drift cover pre-Pleistocene rocks
east and north of the Missouri River and bedrock out-
crops are small and generally limited to the larger
stream valleys, shallow road cuts, and strip mines.
Royce (1970) summarizes the sedimentary history of
the Tongue River and Sentinel Butte Formations.
A higlily fossiliferous exposure of the Tongue
River Formation (Paleocene) was brought to my at-
tention in January, 1971, by Mr. Fred Ballentyne of
Unit Paleocene: Tongue River Formation
4 Buff to light gray limestone, friable, blocky;
lower half coarse grained near base, finer
textured toward top; mollusks abundant in
Umonitic band near middle.
3 Dark gray calcareous shale, soft, strongly fissOe
2 Light gray to buff limestone, blocky; moderately
hard at base; moderately friable above.
1 Brown to gray lignitic clay, weakly calcareous;
base not exposed.
Thickness (Feet)
11.3
1.0
6.2
0.3
TOTAL 18.8 ft.
THE NAUTILUS
Jamuirv I'^V.^
Vol. 87(1)
Sawyer, North Dakota. Most of the fossils were col-
lected that month. The faunule from this locality is
notable for the number of ta.xa present and the occur-
rence of new species of Pisidiiim. The outcrop is
located about 8 miles south of Sawyer. Ward County.
North Dakota m NW'/a. sec. 10, T15:N. R81W. The
exposure is an isolated man-made cut on the west
wall of a shallow coulee at about 1 800 ft. above sea
level. A stratigraphic section is described below:
Bedrock is completely covered on both sides ot
the outcrop; however, more typical Tongue River
clastic sediments are exposed at the same elevation in
an abandoned strip mine about 100 yds. to the west.
Carbonate sediments with similar lithology and strati-
graphy are poorly exposed at the same elevation
about 1 mi. to the east in SW'/i, NWii. sec. 20 of the
same township, but any lateral transition of this se-
quence into silt-clay facies that outcrop nearby is also
covered.
The stratigraphic position of these beds in the
Tongue River Formation cannot be accurately fixed
at present. Lemke (1960. p. 30, 3'i) places the
Tongue River-Cannonball contact at an elevation of
1540 ft. along the Souris River 8 to 9 mi. to the
northeast. Allowing for a sliglit northeast dip in this
area, these exposures are probably 200-250 t~t. above
the base of the Tongue River Formation.
The deposit apparently accumulated in a shallow
tloodplain depression or series of depressions that
held a permanent hard water lake. The lake formed
over clastic and organic backswamp sediments and
maintained a permanent water level long enougli for
diverse moUuscan and ostracode assemblages to be-
come established. Pisidiwn, small amnicolids, and
ostracodes suggest a lacustrine environment. Vivi-
parids are prominent elements in the Fort Union
fauna and these snails probably inhabited slower mov-
ing streams as well as standing water in backswamp
areas.
SYSTEMATIC PALEONTOLOGY
Family Uniunidae
Plesielliptio priscus (Meek and Hayden, 1 856)
Fig. 16
Uiiio priscus Meek and Hayden, 1856, Proc. Acad.
Nat. Sci. Philadelphia 8; 117.
Unionid mussels are common and generally occur
with both valves connected, aligned, and closed. Pres-
ervation in place is often excellent except for frac-
tures induced by compaction, but specimens crumble
and exfoliate during extraction even v<.'ith careful field
and laboratory techniques. One specimen is intact
enough to show both the double looped beak sculp-
ture o\' PIcsiclllptli) and the proportions off. priscus.
Its measurements are: length 78.0 mm., heiglit 45.0
mm., width 21 mm. Three valve fragments have the
concentric looped ornamentation o\ Plcsiclliprid but
are too incomplete for specific determination. About
30 other large fragments of exfoliated hinge areas
cannot be identified to genus.
Family Corbulidae
Bicorbula niuctriturniis (Meek and Hayden. 1856)
Fig. 1 5
Corhula niactritcnuis Meek and Hayden. 1856. Proc.
Acad. Nat. Sci. Philadelphia 8; 117.
Bicorbula mactriforniis is the most common bi-
valve encountered. The numerous specimens ex-
amined range in length from a few millimeters to a
maximum of 23 mm. Outlines vary from sub-ovate to
sub-trigonal with most valves appearing somewhat tri-
angular. Sub-trigonal valves seem to have greater
heights in proportion to length than do ovate speci-
mens. The genus is inequivalved. Dentition is well pre-
served and all intact specimens are easily distin-
guished from other bivalves.
Family Pisidiidae
Hinge tooth terminology in the following descrip-
tions is that of Herrington (1962. p. 1 1 ) with addi-
tion of the abbreviations RV and LV for right and
left valves.
PisiJiuni wardcnsis new species
Figs. 9. 10
Dcscriptidn: Shell small, inflated, oulline ovate;
w;ills moderately thick; beaks prominent, sliglitly to
distinctly raised, sub-central toward posterior; pos-
terior margin rounded to slightly truncate; anterior
margin rounded, narrower than posterior margin; dor-
sal margin broadly angular at umbo, forms slight
rounded angle with posterior margin, smoothly
curved into anterior margin; ventral margin convex;
striae fine, evenly-spaced; growth pauses shallow in-
dentations or steps; hinge narrow; lateral teeth long,
covering about four-fifths of shell length; inner ante-
rior lateral tooth Al (RV) pointed, triangular; outer
anterior lateral AlII (K\) linear, narrow, near distal
hinge margin; anterior lateral All (LV) straight, tri-
angular, cusp distal; posterit)r lateral teeth PI. PIM.
(RV) with short cusps; posterior lateral tooth PIl
(LV) toward proximal hinge margin, cusp prominent;
\ol. 87(1)
THE NAUTILUS
15
FIG. 1. Lioplacodes nebrascensis 'pxo&\KVA(White)X I: FIG. 2. Lioplacodcs mariana YeiiX I:FIG. 3. Lioplacodes
limnaeformis (Meek ami Haydenj, a slender specimen X 1.5: FIG. 4. Vivipaius raynoldsanus Meek and Hayden,
specimen slightly compressed into plane oj illustration X I: FIG. 5. Campeloma nebiasceiisis whitei Russell XI;
FIG. 6. Campeloma nebrascensis (Meek and Harden) X I: FIG. 7. Vivipaius peculiaris (Meek and Haydenj X I:
FIG. 8. Gyraulus cf. G. militaris (White) X 10: FIG. 9. Pisidium wardensis /). sp. interior of Holotype (USNM
180367) X 10: FIG. 10. Pisidium wardensis n. sp., exterior of Holotype X 10: FIG. 11. Pisidium russelli «. sp..
interior of Holotype (USNM 180370) X 10: FIG. 12. Pisidium russelii n. sp.. exterior ofHohitypc X 10: FIG. 13.
Hydrobia warrenana (Meek and Hayden) X 4: FIG. 14. Hydrobia anthonyi (Meek and Hayden) X 4: FIG. 15.
Bicorbula mactriformis (Meek and Harden), interior view X 2: FIG. 16. Plesielliptio priscus (Meek and Hayden) X
'A.
16
THE NAUTILUS
January 1973
Vol. 87(1)
cardinal tooth C3 (RV) distinctly curved, enlarged
posteriorally; cardinal teeth C2, C4 (LV) slender,
rouglily parallel; C2 curved, shorter than C4; C4
slightly curved or distinctly curved on anterior half.
Tvpes and measurements: Types are deposited in
the United States National Museum of Natural His-
tory. Holotype (USNM 180367) length 2.0 mm.,
height 1.8 mm.; Paratype (USNM 180368) length 1.9
mm., heiglit 1.8 mm.; Paratype (USNM 180369)
length 1.6 mm., heiglit 1.5 mm.
Type locality: About 8 mi. south of Sawyer.
North Dakota, NW'/j, NW>/4, sec. 19, T152N, R81W.
Paleocene; Tongue I^ver Formation. Collected Jan.
1971.
Remarks: The 40 specimens examined vary in out-
line and the degree to wliich beaks project above the
hinge line. Smaller specimens tend to appear quite in-
flated. Pisklium wardensis is distinguished from other
Late Cretaceous and early Tertiary pisidid clams by
its inflated ovate shell, broad and rather prominent
beaks, and small size. The species is named for Ward
County, North Dakota.
Pisidium russelli new species
Figs. 11, 12
Description: Shell moderately small, moderately
inflated, outline ovate; beaks prominent, raised above
hinge, situated about one third of shell length from
posterior edge; anterior and posterior valve margins
rounded; dorsal margin sliglitly convex, rounded pos-
teriorally, forms rounded angle with anterior margin;
ventral margin convex; striae fine, evenly spaced;
hinge narrow; lateral teeth long, covering about
three-fourths of sheU length; anterior inner lateral
tooth Al (RV) long, cusp toward distal end; anterior
outer lateral AIII generally parallel to AL prominent;
anterior lateral All (LV) on inner margin of hinge,
straight, cusp rounded and distal; posterior lateral
teeth PL PHI (RV) slender, low, parallel, depression
for opposing tooth long, narrow; posterior lateral
tooth PU (LV) slender, low cusp rounded; cardinal
tooth C3 (RV) distinctly curved, enlarged poster-
iorally; cardinal teeth C2, C4, (LV) parallel, very
sliglitly curved, C2 sliglitly shorter than C4.
Types and measurements: Types are deposited in
the United States National Museum of Natural His-
tory. Holotype (USNM 180370) length 2.85 mm.,
heiglit 2.4 mm.; Paratype (USNM 180371) length
1.75 mm., height 1.55 mm.; Paratype (180372)
length 1.8 mm., height 1.5 mm.
Type locality: About 8 mi. south of Sawyer, Ward
County, North Dakota, NW'/*, NWi4, sec. 19. T152N.
R81W. Paleocene: Tongue River Formation. Col-
lected Jan. 1971.
Remarks: Pisidium russelli resembles P. wardensis
in outline and hinge structure. It is distinguished from
that species by its less inflated shell, sliglitly angular
dorsal-anterior margin, more posteriorally situated
beaks, and parallel cardinal teeth on the left valve.
The name honors Dr. Loris S. Russell.
Family Viviparidae
Vivipanis peculiaris (Meek and Hayden. 1856)
Fig. 7
Paludina peculiaris Meek and Hayden. 1856, Proc.
Acad. Nat. Sci. Philadelphia 8: 122.
The species is characterized by having a thin
trocliiform shell, about 5Vi flattened and slightly con-
vex whoris, fine growth Hues, and very indistinct spi-
ral ridges. The body wliori is angular at its base and
the aperture is ovate to sub-quadrate. Three incom-
plete specimens were found at this site. Two speci-
mens measure: heiglit 18.6 mm. (juvenile whods miss-
ing) and 18.2 mm.; width 16.5 mm. and 13.4 mm.;
aperture heiglit 1 1 mm. and 10 mm.
Vivipanis planolatcrc Russell from the Paleocene
of Alberta seems to be a junior synonym of V. peculi-
aris. The relarionship of V. peculiaris to the similar
Cretaceous species. V. ro/irat// (Meek and Hayden). is
uncertain, and the name V. conradi, has priority if
the two shells are conspecific.
Vivipanis raynoldsanus Meek and Hayden. 1861
Fig. 4
Meek and Hayden, 1861, Proc. Acad. Nat. Sci. Piula-
delphia 13: 446.
Large adult specimens are crushed but several
body whorl fragments suggest maximum shell widths
of over 25 mm. The largest intact shells have heiglits
of about 30 mm. and widths of about 20 mm. Four
of eleven specimens have somewhat flattened whorls,
a rounded angle where the side and base of the body
whori meet, and whods with sliglit shoulders. Such
specimens have an almost turbonate appearance.
Meek (1876, p. 584) mentions specimens of V. ray-
noldsanus with slightly flattened and shouldered
whorls.
On the basis of crushed and fragmcntaiy speci-
mens of V. peculiaris and V. raynoldsanus. 1 incor-
rectly reported V. trochiformis (Meek and Hayden)
and V. retusus (Meek and Hayden) from this locality
in an abstract (Bickel and Hall, 1971).
Vol. 87(1)
THE NAUTILUS
17
Canipdoina iicbrasccnsis (Meek and Hayden, 1 856)
Fig. 6
Buliimis ncbrascensis Meek and Hayden. I 856. Proc.
Acad. Nat. Sci. Philadelphia 8: 118.
Two specimens from this site have the convex
whorls, intlated body whorl, slight shoulder, and
raised spiral lines of the typical form of C. ncbrascen-
sis. Meek (1876. p. 586) states that on some speci-
mens "the lower whorl shows faint traces of an ob-
scure revolving ridge just below the suture." This
characteristic occurs commonly on specimens 1 have
seen from other localities in the Williston Basin and
Delimata (1969, p. 29) notes it on material from the
Little Missouri Badlands. Shoulders, when present,
are less prominent than on C. ncbrascensis whitci
Russell. The two specimens measure: heiglit 27.0
mm. and 16.6 mm.; width 18.0 mm. and 12.8 mm.;
aperture heiglit 13.3 mm. and 9.0 mm.
Campcloma ncbrascensis whitci Russell, 1931
Fig. 5
RusseU, 1931, Trans. Roy. Soc. Canada, ser. 3, 25
(sec. 4): 12, pL 2, fig. 1.
This shell is the most common of the larger vivi-
parids encountered with 17 fairly intact specimens
being recovered. Many shells are crushed by sediment
compaction and others were destroyed during col-
lection. Campcloma ncbrascensis whitci differs from
typical C. ncbrascensis in having a prominent
shoulder at the top of the penultimate and body
whorl and a broad, shallow depression or sinus just
below the shoulder. Five specimens lack raised spiral
ornamentation. This form occurs with typical C.
nebrascensis and is easily distinguished from it, sug-
gesting that C. ncbrascensis whitci may be a distinct
species.
Lioplacodes Umnaeformis (Meek and Hayden, 1856)
Fig. 3
Bulimus Umnaeformis Meek and Hayden. 1856, Proc.
Acad. Nat. Sci. Philadelphia 8: 118.
Specimens are fairly common at the exposure and
generally well preserved. Most specimens have a
slightly convex spire but occasionally sheUs (4 of 50
specimens) have relatively straight-sided spires. Three
specimens have the following measurements; heiglit
17.0 mra, 15.5 mm., 12.2 mm.; width 7.9 mm., 7.5
mm., 5.5 mm.; aperture height 7.2 mm., 6.8 mm., 5.8
mm.
Lioplacodes mariana Yen, 1946
Fig. 2
Yen, 1946, Anier. Jour. Sci.. 244: 44-45, pi. 1, figs.
5a- 5c.
Five specimens are referred to this species which is
distinguished from L. nebrascensis by having a slender
spire, less intlated body whorl, more loosely coiled
whorls, and a smaller aperture. The upper two-thirds
of each whorl is sliglitly convex and the lower third is
strongly convex where it meets the lower suture. Two
specimens measure: height 27.5 mm. and 26.5 mm.;
width 14.0 mm. and 12.7 mm.; aperture height 11.0
mm. and 1 0.0 mm.
Lioplacodes nebrascensis producta ( Wliite, 1 883)
Fig. 1
Campcloma producta White, 1883, U. S. Natl. Mus.
Proc, 3: 97, pi. 3, figs. 7-9.
Over 100 specimens were examined and they vary
in spire heiglit, convexity of whorls, and degree of
ornamentation. The original description of L. nc-
brascensis (Meek and Hayden, 1856, p. 124) depicts
the variability of this species, and Russell (1931) con-
siders L. ncbrascensis producta and typical L. ne-
brascensis end members in the range of variation in
one species. The trinomial is used here as a form
name. Many of the specimens are ornamented with
fine spiral raised lines that are occasionally developed
enough to make juvenile and intermediate whorls ap-
pear liglitly carinate. Liglitly carinate shells resemble
L. tenuicarinata (Meek and Hayden) but lack the
strongly keeled and convex whorls of that species.
About one-fifth of the material has the tall, slender
spire and whorl morphology of L. mariana but retains
the fuUer body whorl and larger aperture of L. nc-
brascensis producta.
Family Planorbidae
Gyraulus cf. G. militaris (White, 1 880)
Fig. 8
Planorbis militaris White. 1880, Proc. U. S. Natl. Mus.
3: 159.
Two specimens of small planorbids, both crushed
along the axis of coiling, resemble G. militaris. The
illustrated specimen shows the proportions of G. mili-
taris and has the deep umbilicus of that species. Shell
widths of the two specimens are 1.9 mm. and 1.8
mm.
THE NAUTILUS
January 1973
Vol. 87 ( 1 )
Family Amnicolidae
Hydrobia anthonyi (Meek and Hayden, 1 856 )
Fig. 14
Melania anthonyi Meek and Hayden, 1856, Proc.
Acad. Nat. Sci. Philadelphia 8: 124.
On large specimens, penultimate and body whorls
are somewhat more convex than the immature
whorls. Intermediate sized shells tend to have sliglitly
convex whorls and well impressed sutures. Smaller
specimens generally have subrounded apertures, while
apertures on larger individuals tend to be more elon-
gate. Persistant and very fine spiral striae are present
on adult whorls but are absent or extremely fine on
juvenile whorls. Fifty-seven specimens were exam-
ined. One large and one intermediate-sized specimen
measure: heiglit 6.3 mm., 3.4 mm.; width 33 mm.,
1.8 mm.; aperture heiglrt 2.8 mm., I.l mm.
Hydrobia warrenana (Meek and Hayden, 1 857)
Fig. 13
Melania warrenana Meek and Hayden. 1857, Proc.
Acad. Nat. Sci. Philadelpliia 9: 137.
Hydrobia warrenana is distinguished by its conical
spire, 6 to 7 sliglitly convex whorls, and a body whorl
that forms a rounded angle with the base. This angle
tends to be sharply defined on immature shells but
more rounded on large specimens. The aperture is
subquadrate. Two large specimens measure; length
5.6 mm., 4.8 mm.; width 2.6 mm., 2.2 mm.; aperture
heiglit 2.0 mm., 1.7 mm. Most of the 30 specimens
have lengths of less than 3.0 mm.
Family Physidae
Pliysa sp.
One fragmented and apparently immature speci-
men of this genus was found. The apex and aperture
periphery are missing and specimen length is 7.0 mm.
LITERATURE CITED
Bickel, D., and Hall, D. H. 1971. Paleocenc fresh-
water Mollusca from southern Ward County,
North Dakota (abstr.). North Dakota Acad. Sci
Proc.pt. 1,25: 3.
Delimata, J. J. 1969. Fort Union (Paleocenc) mol-
lusks from southern Golden Valley and south-
eastern Billings Counties, North Dakota. MS
Thesis. Univ. North Dakota. 73 p.. 6 pis. (unpubl..
typewritten).
Herrington, H. B. 1962. A revision of the Sphaeriidae
of North America (Mollusca: Pelecypoda). Mus.
Zool. Univ. Michigan Misc. Publ. 118, 74 p., 7 pis.
Lemke. R. W. 1960. Geology of the Souris River area.
North Dakota. U. S. Geol. Surv. Prof. Pap. 325,
138 p.
Meek. F. B. 1876. A report on the invertebrate Creta-
ceous and Tertiary fossils of the Upper Missouri
country. U. S. Geol. Geogr. Surv. Terr. (Hayden
Survey) 9: 629 p., 45 pis.
Meek, F. B. and Hayden, F. V. 1856. Descriptions of
new species of Acephala and Gastropoda . . . Proc.
Acad. Nat. Sci. Philadelphia 8: 11 1-125.
Meek, F. B., and Hayden, F. V. 1857. Description of
new species and genera of fossils, collected by Dr.
F. V. Hayden in Nebraska Territory . . . Proc.
Acad. Nat. Sci. Philadelphia 9: 117-148.
Meek, F. B., and Hayden. F. V. 1861. Descriptions of
new Lower Silurian (Primordial). Jurassic. Creta-
ceous, and Tertiary fossils, collected in Nebraska .
. . Proc. Acad. Nat. Sci. Philadelphia 13: 415-447.
Royce, C. F., Jr. 1970. A sedinicntologic analysis of
the Tongue River-Sentinel Butte intei-val (Paleo-
cenc) of the Williston Basin, western North
Dakota. Sedimentary Geol. 4: 19-80.
Russell, L. S. 1931. Mollusca from the Upper Creta-
ceous and Lower Tertiary of Alberta. Roy. Soc.
Canada Trans. Ser. 3, 25 (sec. 4): 9-19, 2 pis.
White, C. A. 1880. Descriptions of new invertebrate
fossils from the Mesozoic and Cenozoic rocks of
Arkansas. Wyoming, Colorado, and Utali. Proc. U.
S.Natl. Mus. 3: 157-162.
Wliite, C. A. 1883. New molluscan forms from the
Laramie and Green River Groups, with discussion
of some associated forms heretofore known. Proc.
U. S. Natl. Mus. 5: 94-99, pi. 3-4.
Yen. T.-C. 1946. Paleocenc freshwater molhisks from
Sheridan County. Wyoming. Amer. Jour. Sci. 244:
41-48. 1 pi.
Vol. 87(1)
THE NAUTILUS
19
TO WHAT EXTENT DO SURF CLAMS MOVE?
John W. Ropes and Arthur S. Merrill
National Marine Fisheries Service
Middle Atlantic Coastal Fisheries Center
Oxford, Maryland 21654
ABSTRACT
Locomotion by surf clams, Spisula solidissima, includes rapid burrowing, crawling, and
leaping from the bottom. Observations of these activities led to the suspicion that some
movement over the sea floor may occur. We found that the usual response of surf clams
removed from a burrow is rapid re-entry into the substrate. Occasional leaping, when
seen, was usually by recently disturbed, small and very young specimens. They propelled
themselves very short distances and immediately burrowed upon landing. Unusual circum-
stances seemed necessary to elicit the leaping response and it was considered a relatively
ineffective means of locomotion
Surf clams {Spisula solidissima (Dillwyn)), like
many other bivalves, are considered to be benthic, in-
faunal, and sedentary. They are normally found
buried and expose only their siphon tips at the sea
bottom. In an account of a trip in the deep sub-
mersible Alvin. Edwards and Emery (1968) made a
brief statement about seeing a 6-inch surf clam "leap-
ing" across the bottom. Leaping, a behavior that
seems to contradict the usual sluggish reactions of
surf clams, may be a hitherto unsuspected means of
escaping hazards which threaten survival. It may also
be an exceptional behavior to which an observer
miglit attach too great a significance. The purpose of
this paper is to review the literature on the movement
of surf clams and report on our observations of its
activities.
Three general locomotor activities have been re-
ported for surf clams: gliding, crawling, and burrow-
ing (Belding, 1910; Ropes and Merrill, 1966; Ropes,
1967). Gliding, the result of a clam forcefully pushing
itself off of a substrate by a sudden straiglitening of
the bent, extended foot, is termed "leaping" by
Ansell (1969). The clam glides with the posterior part
of its shell directed like a keel (Fig. 1). Muscular acti-
vities of the foot or adductor muscles that miglit be
used for swimming movements have not been seen
during the gliding act. After a leap, a surf clam glides
for only a few seconds and then falls to the bottom
because of negative buoyancy.
Our observations of gliding surf clams were inci-
dental to other experiments. The action was very in-
frequent. For example, more than 30,000 small
clams, hand dug between 1964 and 1967 from the
beach at Wallops Island, Virginia, immediately rebur-
rowed if left on the sand surface. This action hap-
pened whether the clams were in or out of the water.
Only two small ones, 25 to 30 mm. in length, were
seen gliding in the water. Upon landing on the sand
surface, they began to reborrow.
Stimuli for the gliding or leaping response in Mac-
tra corallina, a close relative of S. solidissima in the
family Mactridae, have been reported by Ansell
(1969) to be: (1) close proximity or contact with a
predator, (2) failure of the foot to penetrate the sub-
stratum, and (3) exposure to air. He considered the
latter two stimuli to be of minimal ecological signi-
ficance and explained that, to increase the chance of
contact and obtain a reaction from predators, the
clams were confined in small aquaria. No mention
FIG. 1. A small (about 25 mm. long) surf clam leap-
ing.
20
THE NAUTILUS
January 1973
Vol. 87(1)
was made of the possibility of a clam closing its shells
or burrowing deeper in the substratum to avoid
predator contact. This latter activity was described by
Pratt and Campbell ( 1956) as a behavior of northern
quahogs IMercenaria mcrccnaria) confined in boxes
with predaceous starfish.
Surf clams have adaptations for living in a burrow
and divers have always found them there. Burial may
be well below the sand surface, because the siphons
can be extended nearly equal to the length of the
shell. Numerous papillae fringing the siphonal open-
ings (Morse. 1919) may be adaptations to prevent
sand from being drawn into the body cavity by the
respiratory and food-gathering water currents. The
clean shells of most clams taken by dredges or thrown
onto beaches by storms indicate that they had been
covered completely. A report by Ropes and Merrill
(1966) on SCUBA observation of a bed of surf clams
near Cape Cod. Massachusetts, stated that the clams
were completely buried in the bottom. Visible siphon
holes were the only evidence that surf clams were
present in the bottom. Another SCUBA diver (Bul-
loch. 1965) described a surf clam bed about 4 miles
offshore from Point Pleasant, New Jersey. He saw
surf clams with the posterior portion of their shells
protruding from the sandy bottom. All seemed to be
oriented in the direction of a strong current flow
which had apparently removed sand from around the
shells. In spite of this, no clams were seen on the
surface or moving about on the surface. On rare occa-
sions, we have seen quantities of commercially cauglit
clams with algae growing on a portion of the shell
nearest the siphon. The localized growth of algae im-
plies that these clams have been embedded for some
time in the bottom with the posterior end slightly
above the surface. It is important to note that none
of the divers reported surf clams out of the bottom.
The diver who reported on the surf clams near Cape
Cod dislodged some and they promptly reburied
themselves (Ropes and Merrill, 1966). A clam of com-
mercial si/e ( 1 25 mm. long) took about 2 minutes to
burrow into the bottom. Subsequent to these obser-
vations, the diver has collected surf clams for us at
monthly intervals during 2 years. Althougli we have
asked him to observe and photograph movements, he
has been unable to obtain any evidence of crawling,
gliding, or leaping.
The movement of surf clams out of their burrows
has not been clearly demonstrated as a usual loco-
motor activity. Surf clams have been observed to ele-
FIG. 2. Surf clams raised our uj the cxpascJ inur-
tidal substratum at Wallops Island. Virginia.
vate themselves out of the bottom substratum on ex-
posed beaches during periods of low tide (Ropes.
1967) (Fig. 2). Exposure of the drained bar to solar
heat may have initiated the clam movement out of
the bottom. Apparently the effort to dig deeper in
the more compact, drier substrate moved the clam
upward. However, our attempts to cause surf clams to
exhume in laboratory experiments, by draining water
from the bottom of the aquarium and exposing the
surface of the sand to radiated heat, were unsuccess-
ful.
Storms appear to be very effective in moving surf
clams from an area; large numbers of surf clams are
found washed upon the beach after severe winter
storms (Yancey and Welch, 1968). Bottom currents,
produced during storms, dislodge clams from the bot-
tom and many are unable to burrow quickly enough
to avoid being thrown further up on the beach. That
many do reburrow is evident, since the surf zone at
low tide is one of the best areas to collect small surf
clams.
Armstrong (1965) studied the burrowing limita-
tions of 10 species of clams. He found that the clams
showed no movement other than rotational or bur-
rowing, and that none were able to exhume or elevate
in their burrows under their own power. Clams
planted 4 to 7 inches below the tips of their extended
siphons died. Our experiments with the juvenile and
adult surf clams produced similar results.
We have conducted several other experiments to
determine burrowing movements of surf clams. Bur-
rowing ability was considered essential to survival of
clams marked and replanted for growth studies
Vol. 87(1)
THE NAUTILUS
21
(Rt)pes and Mcnill. 1^70). Clams. 50 to 75 mm. long.
placed in an aquarium, dug into the bottom soon
after initiating burrowing. Descriptions and photo-
graphs of this action were reported by Ropes and
Merrill (1966). However, small clams averaging 25
mra also showed some gliding movements, suggesting
that small surf clams may be more active than larger
ones. Gliding by these small clams was apparently
caused by the disturbance of other clams burrowing
nearby. The clams burrowed upon landing on the
sand surface. Burrowing was the only consistent re-
sponse obser\'ed.
Clams we marked and planted off Wildwood, New
Jersey, were recovered in the same area one year
later. Several hundred clams were recovered up to
two years after being marked and planted in shallow
water near Chincoteague Inlet, Virginia (Ropes and
Merrill, 1970). Recovery of clams was always within
the release area, indicating a lack of movement.
Heavy, hydraulic jet dredges used by commercial fish-
ermen are not sufficiently disturbing to cause clams
actively to "flee" an area, because the fishermen re-
peatedly dredge througli a dense patch or "hot spot"
for periods of several days or sometimes months and
still take clams in commercial numbers. The staff of
the BCF Exploratory Fishing and Gear Research
Base, Gloucester, Massachusetts, have obsei-ved surf
clam beds and the action of a commercial-type hy-
draulic jet dredge ' by underwater television and
cinematography. At no time were surf clams seen on
the surface of the sand bottom, nor were any seen
gliding through the water in escape movements' . The
many field and laboratory observations demonstrate
that surf clams rarely move other than to reburrow
when disturbed or removed from their burrows.
' Personal communication by Phillip S. Parker,
Fishery Biologist, formerly with the BCF Explora-
tory Fishing and Gear Research Base, Gloucester,
Massachusetts.
We wish to stress that, from our observations, the
movement of surf clams can be considered to be in-
frequent and exceptional. All of the movements we
have observed have occurred after the clams were dis-
turbed by removal from the substratum, and the
clams invariably reburrowed. Voluntary movements
of surf clams out of the bottom have never been re-
ported nor have we been able to induce this activity
in laboratory experiments. The abihty of most pele-
cypod mollusks to move througli the water is so rare
that notes are published reporting such unusual
phenomena (Baker and Merrill, 1965). Surf clams,
especially the larger adults of commercial size, are,
for all intents and purposes, sedentary bottom dwel-
lers.
The above observations were used to prepare a
justification for adding the surf clam to the List of
Creatures of the Continental Shelf An amended
regulation to the law included surf clams and was
published in the Federal Register on June 23, 1971.
LITERATURE CITED
Ansell. Alan D. 1969. Leaping movements in the
Bivalvia. Proc. Malacol. Soc. Lond. 38: 387-399.
Armstrong. Lee R. 1965. Burrowing limitations in
Pelecypoda. The Veliger 7 (3): 195-200.
Baker, Emmett B. and Arthur S. Merrill. 1965. An
observation of Laevicardium mortoni actually
swimming. The NautUus 78 (3): 104.
Belding, David L. 1910. The growth and habits of the
sea clam (Mactra solidissima). Rep. Comm. Fish.
Game Mass. 1909, Publ. Doc. 25: 26-41.
Bulloch, David K. 1965. Field observations - 1964.
Underwater Natur. 3 (1): 27-28.
Edwards. R. L. and K. 0. Emery. 1968. The view
from a storied sub - the Alvin off Norfolk, Va.
Commer. Fish. Rev. 30 (8-9): 48-55.
Morse, Edward S. 1919. Observations on living
lamellibranchs of New England. Proc. Boston Soc.
Natur. Hist. 35: 139-196.
Pratt, David M. and Donald A. Campbell. 1956.
Environmental factors affecting growth in Venus
mercenaria. Limnol. Oceanogr. 1: 2-17.
Ropes, John W. 1967. The locomotion and behavior
of surf clams, Spisula solidissima. Proc. Nat. Shell-
fish. Ass. 57: 4. (Abstract).
Ropes, John W. and Arthur S. Merrill. 1966. The bur-
rowing activities of the surf clam. Underwater
Natur. 3(4): 11-17.
Ropes. John W. and Arthur S. Merrill. 1970. Marking
surf dams. Proc. Nat. Shellfish. Ass. 60: 99-106.
Yancey, Robert M. and Walter R. Welch. 1968. The
Atlantic coast surf clam - with a partial biblio-
graphy. U. S. Fish WUdl. Serv. Circ. 288, 14 pp.
THE NAUTILUS
Januarv I 973
Vol. 87(1)
LEO GEORGE HERTLEIN (1898 1972). AN
OBITUARY AM) FINAL HII5LI0GR APHY
William K. Emerson
Department of Living Invertebrates
The American Museum of Natural History
Central Park West at 79th. N. Y.. N. Y. 10024
Dr. Leo George Hertlein. Curator Emeritus of
Invertebrate Paleontology, California Aeadeiny of
Seiences. San Francisco, died on January 15, 1972
after a brief illness. His deatli came as a shock to his
many friends, for he appeared to be enjoying robust
health and looked much younger than his years. He
was actively working on several research projects at
the Academy until the time of his illness. He liad
noted on his 1971 Christmas card that he was enjoy-
ing his retirement and was now able to devote most
of his time tt) the completion of a long-term study on
the geology and paleontology of the marine Pliocene
of San Diego, California. The third part of this
treatise, a monograph on the pelecypods of the San
Diego formation, was in press at the time of his death
and has now been published (see review. The
Nautilus. 86 (2-4), This major contribution, together
with more than 150 scientific publications, testifies
to his ability and devotion as a scientist who held the
universal esteem of his colleagues.
On the occasion of his retirement, the October,
1970. number of The Nautilus was subtitled the "Leo
George Hertlein Honor Issue" by his friends who con-
tributed a biographic profile, a list of taxa proposed
in his honor, a bibliography of his works, a list of
names proposed b\ him. and original papers on
MoIIusca dedicated to him.
A gentleman and a scholar. Leo was a quiet,
friendly man who was always willing to assist others,
be they amateurs, students, or professional col-
leagues. He will be remembered by his many friends
as a kind man who combined characters of high moral
and ethical strength with a gentleness and warmth of
aftection thai wa^ uiuque. Leo Hertlein was trul> a
Prince of a Man,
I have appended l)i. ilerlleni's bibliography and a
list ol new laxa pro|iosed by him, fi)r the period of
1970 to 1972.
Bibliography of Leo G. Hertlein
for the period of 1970-1972
Papers preceded b\ an asterisk (*) contain new
taxa.
1970a, *A new species of fossil Kclktia (Mollusca:
Gastropoda) Irom the Loniita Marl, late Cenozoic
of San Pedro, California, Contributions in Science.
Los Angeles Co. Mus.. no. 190, p. 1-8, fig, 1-3,
1970b. Review of Carrington, A, J. and B. F.
Kensley. 1969. Pleistocene Mollusks from the
Namaqualand Coast. Veliger, 12: 381.
1970c. Review of Figueiras. Alfredo and Omar E.
Sicardi, 1968, Catalogo de los Moluscos Marinhos
del Uruguay. Veliger, 12: 381-382.
1970d. Review of Work, Robert C, 1969. System-
atics. Ecology, and Distribution of the Mollusks of
Los Roques, Venezuela. Veliger, 12: 382.
1970e. Review of Barnard. K. H.. 1969. Contri-
butions to the knowledge of South African Mol-
lusca. Part IV: Veliger, 12: 382.
1970f, Review of Ludbrook, Nellie H., 1969, The
genus Miltha in the Australian Cainozoic: Veliger,
13: 114.
1970g. Review of Kensley, Brian and Mary-Louise
Penrith. 1970, New records of Mytilidae from the
northern South West African coast: Veliger, 13:
205.
1970h, (v\'ith Victor A. Zullo) Catalogue of specimens
in the type collection of the Department of Geo-
logy, California Academy of Sciences. Cephalo-
pi)da: Occ. Papers Calil'ornia Acad, Sci.. no. 82,
130 pp.
1 97 la. Review of Kosuge. Sadao. 19(i9, Fossil Mol-
lusks of Oaliu. Hawaiian Islands: Veliger. 13: 301.
1971b. Review of Fischer-Piette. L,, M. Kempf, and
A. M. Testud, 1969, Nouvelles donnees sur les
Veneridae (mollusques, lamellibranches) du Bresil:
Veliger, 13: 302,
1971c. Review of Darragh. Thomas A., l970,Cata-
logue of Australian Tertiary Mollusca (except
chitons): Veliger, 13: 302.
197 Id. The researcher and the library: Spec. Libr.
Assoc, San Francisco Bay Reg, Chap, Bull.. 41
(4): 7-8,
|97 1e. Review of Osorio, Cecelia and Nibaldo
Bahamonde, 1970. Lista preliminar de lameli-
branquios ile Chile; Veliger, 13: 373.
1 97 If. Review of Ageitos de Castellanos, Zulma J.,
1970, Catalogo de los moluscos marinos
Bonaerenses: Veliger, 13: 374.
Vol. 87 ( 1 )
THE NAUTILUS
23
1972a. *Description of a New Species oi Chlamys
(Mollusca: Pelecypoda) From the Galapagos Is-
lands; Proc. California Acad. Sci., ser. 4, 39 (1):
1-6, 5 figs.
1972b. (with Victor A. ZuUo): Catalog of Specimens
in the Type Collection of the Department of Geo-
logy, California Academy of Sciences. Echino-
dermata: Occ. Papers California Acad. Sci., no. 91,
26 pp.
1972c. *Pliocene fossils from Baltra (South Seymour
Island), Galapagos Islands: Proc. California Acad.
Sci., ser. 4, 39 (3): 25-46, 39 figs.
1972d. *(and Grant, U. S., IV). The geology and
paleontology of the marine Pliocene of San Diego,
California, Pt. 2b, Paleontology (Pelecypoda): San
Diego Soc. Nat. Hist. Mem., 2: 135-411, text figs.
7-13, pis. 25-57.
Names Proposed by Leo G. Hertlein
From 1970 To 1972
The format follows that used in the previous list-
ing for the period of 1925 to 1970 (Nautilus 84 (2):
pp. 52-69). All the new taxa in the present list are
mollusks and are referable to the class Bivalvia
(Pelecypoda), except Kelletia kanakoffi, which is a
gastropod.
abbotti Hertlein & Grant, Chlamys abieds 1972d: p.
196, pi. 34, fig. 5;pl. 36, figs. 1,6.
allisoni Hertlein & Grant, Chione (Chione) 1972d: p.
273, pL 51, figs. 11-16.
ashleyi Hertlein & Grant, Semele 1972d: p. 299, pi.
48, figs. 3, 4, 6, 9, 10.
axinola Hertlein & Grant, 1972d: p. 159. Type spe-
cies by original designation: Axinaea (? septentri-
onalis, war.) siibobsoleta Carpenter, 1864.
balboana Hertlein & Grant, Nucula (Ennucula)
1972d: p. 145, pi. 27, figs. 1-4.
baltrana Hertlein, Diplodonta subquadrata 1972c: p.
33, figs. 8, 11.
diegoana Hertlein & Grant, Aligena 1972d: p. 235, pi.
44. figs. l,6;pL45, figs. 6, 7, 10, 11, 13.
diegoana Hertlein & Grant, Dosina (Dosina) pon-
derosa 1972d: p. 265, pi. 47, figs. 2, 3, 6, 8, 10;
pi. 49, fig. 8, pL 51, fig. 14.
ellisi Hertlein & Grant, Chlamys (Chlamys) hastata
1972d: p. 190, pi. 31, figs. 2, 3; pi. 34, fig. 6.
frankiana Hertlein & Grant, Borina (Temblorinaj
1972d: p. 238, text fig. 11.
incantata Hertlein, Chlamys (Chlamys) 1972a: p. 2,
figs. 1-5.
imsella Hertlein & Grant 1972d: p. 279. Type species
by original designation: Venus lamellifera Conrad,
1837.
kanakoffi Hertlein & Grant, Chione (Securella)
1972d: p. 274, pL 49, figs. 1, 3, 4-6; pL 51. figs.
4-7, 10.
kanakoffi Hertlein, Kelletia 1970a: p. 1, figs. 1-3.
kanakoffi Hertlein & Grant, Thracia 1972d: p. 338,
pi. 42, figs. 11, 13-15.
orcutti Hertlein & Grant, Lima (Limaria) 1972d: p.
215, pi. 35, fig. 11; pL 36, figs. 2-5; pi. 57, fig. 10.
stephensae Hertlein & Grant, Psephidia 1972d: p.
280, pL44, figs. 21,22, 24, 26.
stembergi Hertlein & Grant, Mytilus (Crenomytilus)
coalingensis 1972d: p. 163, pL 41, figs. 10, 14.
BOOK REVIEW
ART FROM SHELLS. By Stuart and Leni Goodman.
210 pp., 393 photographs, 21 in color. Crown
Publ. Inc., 419 Park Ave. South, N. Y., N. Y.
10016. Paperback, S3.95; cloth, hardback, $7.95.
This is probably the most extensive and most prac-
tical book on the subject of using shells in jewelry,
shell pictures, collages, figurines, and shell sculptures.
It is profusely illustrated with simple pictorial steps
on how to clean, mount and use shells in various art
forms. There are short sections on collecting and
cleaning shells, as well as a current list of supphers.
R. Tucker Abbott
Delaware Museum of Natural History
24
THE NAUTILUS
January 1973
Vol. 87(1)
THE PROBLEM OF THE LAND SNAIL GENUS
RABDOTUS IN TEXAS ARCHEOLOGICAL SITES
John W. Clark, Jr.
Balcones Research Center
Rt. 4, Box 189, Austin, Texas 78756
Vast numbers of land snaUs, principally Rabdotus
dealbatus (Say) in central Texas and R. schiedeanus
(Pfr.) in south and southwest Texas (Pratt 1969:
47-48), are found in prehistoric archeological sites.
These snails often occur in lenses of thousands of
adult shells associated with cultural debris in burned
rock middens in central Texas and in rockshelters in
southwest Texas.
The area in central Texas in which this pheno-
menon occurs lies within the Edwards Plateau region,
especially to the east and south edges of the Balcones
Escarpment where limestone forms the bedrock and
numerous streams dissect the plateau. This area falls
within the Balconian Biotic Province described by
Blair (1950; 12-13).
In southwest Texas, the area of snail-archeological
association is quite restricted. It is centered on the
Rio Grande River in the vicinity of the mouths of the
Pecos and Devil's Rivers. This area falls on the bound-
aries of Blair's Chihuahuan and Balconian Biotic Pro-
vinces (Blair 1950: 105-108). It is characterized by a
limestone plateau dissected by deep canyons. Both
areas are within the Great Plains Province which is
characterized by decreasing annual rainfall from east
to west (Carr 1967: 3-4) so that the central Texas
area receives between 22 and 30 inches of rain per
year while the southwest area receives between 13
and 16 inches per year. Rabdotus shells are also
found in some archeological sites in south Texas as-
sociated with Blair's (1950: 102-105) Tamaulipan
Biotic Province.
The vast numbers of these snails in central Texas
burned rock middens was noted as early as 1932
(Pearce) and 1933 in southwest Texas (Martin).
Numerous hypotheses have been formulated since
then attempting to explain this phenomenon. The
four principal hypotheses are:
(1) These snails were intentionally collected as a
source of protein in the diet (Martin 1933 and Suhm
1957),
(2) They represent a natural population of snails
attracted by decomposing midden refuse,
(3) They were carried to the sites inadvertently on
vegetation collected by the Indians, and
(4) They were collected for their shells which were
used as adornment (Martin 1933). Rabdotus shells
appear to have accumulated or been collected in the
two regions over quite a long period of time, from
about 8,000 B.C. at Arenosa Shelter at the mouth of
the Pecos River to about 1.000 B.C. in central Texas.
Unfortunately, much of the speculation has been
based on little empirical evidence. There is no good
ethnographic account of Indians in either region eat-
ing snails and the evidence for the use of shells for
decoration is scant. No empirical evidence for the
remaining hypotheses has been obtained through
archeological techniques. One of the principal prob-
lems concerning the presence of Rabdotus is
whether they were principally collected as a food
source. Providing they are preserved, the presence of
radulae of these snails in coprolites (dessicated human
feces) could be a major factor in assigning hypothesis
number one as the principal cause of the snaO lenses
in the sites. Coprolites are present in a collection
from a rockshelter in southwest Texas. Analysis of
coprolites from occupation lenses in which numerous
snail shells were found should provide some im-
portant data on the snail collection at this site and,
by extension, at other sites.
Tliis short paper is principally a plea for informa-
tion concerning the validity of the hypotheses pre-
sented herein and an appeal for co-operation of
malacologists in the analysis of coproUte samples for
snail radulae.
LITERATURE CITED
Blair, Frank W. 1950. The Biotic Provinces of Texas.
The Texas Journal of Science. 2(1).
Carr, John T., Jr. 1967. The Climate and Physio-
graphy of Texas. Texas Water Development Board,
Report, 53.
Martin, George C. 1933. Archaeological Exploration
of the ShuirJa Caves. Tlie Witte Memorial Muse-
um, Bulletin 3.
Pearce, J. E. 1932. The Present Status of Texas
Archeology. Bulletin of the Texas Archeological
and Paleontological Society 4.
Pratt, William D. 1969. Jiabdotus in Texas, Prelimi-
nary Revision of the Land Snail Genus. The
American Malacological Union, Inc., Annual
Reports for 1969: 47-48.
Suhm, Dee Ann. 1957. Excavations at the Smith
Rockshelter, Travis County, Texas. The Texas
Journal of Science, 9(1).
Vol. 87(1)
THE NAUTILUS
25
NOTES ON VERONICELLIDAE AND ATHORACOPHORIDAE
IN FIELD MUSEUM OF NATURAL HISTORY, CHICAGO.
Lothar Forcart
Naturhistorisches Museum, Basel
Switzerland
Dr. A. Solem entrusted me with the identification
of slugs in the collections of Field Museum of Natural
History, Chicago. These materials expand our know-
ledge on the distribution and taxonomy of several
veronicellid and athoracophorid species. The follow-
ing abbreviations indicate the repository of cited
materials:
FMNH - Field Museum of Natural History, Chicago.
MG - Zoologisches Institut und Museum, Gottingen.
NMB - Naturhistorisches Museum, Basel.
ZMB - Zoologisches Museum, Berlin.
VERONICELLIDAE
Laevicaulis alte (Ferussac, 1821)
Material examined: New Caledonia, E. coast 5 km.
N. of Theim (2 spec, FMNH 144278, coU. Jan. 1962
by A. & B. Solem); W. coast 8 km. W. Bourail (6
spec, FMNH 159224, 159237, coU. Oct. 1967 by L.
Price).
Remarks: Grimpe & Hoffman (1925, p. 366) pre-
viously recorded L. alte from New Caledonia. A sum-
mary of its complex synonymy is given in Forcart
(1969, pp. 148-149).
Veronicella (Tenacipesj tenax Baker, 1931
Veronicella (Tenacipesj tenax Baker, 1931,
Nautilus, 44(3): 131, pL 8, figs. 3-5. (Ensenada
de San Vicente, Pinar del Rio, Cuba).
Material examined: West Indies: Puerto Rico, foot
of stone cliff (2 spec, FMNH 157272, coU. Feb.
1968 by M. Moran). Dominica (5 spec, FMNH
157135, coll. Feb. 1968).
Remarks: All specimens are juvenile, the largest
being only 46.5 mm. long, as compared to the 96-105
mm. holotype and paratypes described by Baker.
They agree with the original description in the notum
having small papillae, in the sole being considerably
shorter than the notum and completely surrounded
by the hyponota, the posterior end being rounded
and crossed by numerous fine, transverse grooves.
The anus is as in the subgenus Leidyula, only partly
covered by the foot. The vagina is without accessory
bursa. The penis and the stimulatory organ
(dart-gland in Baker 1931) are as figured by Baker
(1931, pi. 8, figs. 4, 5) for the holotype.
All these specimens differ from the types in lack-
ing whitish spots on the notum. The three specimens
from Dominica have dark lateral bands on the notum.
?Vaginulus (Latipesj occidentalis (GuUding, 1825)
Onchidium occidentale Guilding, 1825, Trans.
Linn. Soc, London, 14: 323, pi. 9, figs. 9-10.
(St. Vincent, Windward Islands).
Vaginulus (Latipesj occidentalis (Guilding), Baker
1925, Proc Acad. Nat. Sci. PhUadelpliia, 77:
174-177, pi. 5, figs. 18-20.'
Material examined: Almirante, Bocas del Toro,
Panama. (5 spec, FMNH 86536, coU. Mar. 1959 by
H. S. Dybas).
Remarks: The examined specimens agree with
those Baker (1925) described from Panama. No
type-specimens of V. occidentalis exist, and 1 have
not been able to examine specimens from St.
Vincent. Onchidium occidentale is a nomen dubium
and it is doubtful whether the specimens from
Panama are the same species. Proposal of a new name
for the Panama specimens should wait until the iden-
tity of the St. Vincent specimens has been deter-
mined.
Vaginulus (Angustipesj buergeri (Simroth, 1914)
Vaginula burgeri Simroth, 1914, Mem. neu-
chateloise Sci. nat., 5: 328, pi. 14, figs.
124-126. - Santo Domingo. Lectotype and 2
lectoparatypes MG (see Thome, 1970: 73-76,
figs. 1-7).
Cylindrocaulis occidentalis Hoffmann 1925, Jena.
Z. Naturw., 61 ('/-): 144-147 pardm, pi. 5, fig.
45, 2, d, F.
Material examined: Salilia, Dominica. (3 spec,
FMNH 157147).
Remarks: The detailed redescription of V. buergeri
by Thome (1970, pp. 73-76, figs. 1-7) makes it evi-
dent that Baker (1925, 180-182, pi. 6, figs. 28-30)
described another species under this name.
The bursa of the receptaculum seminis is elongate,
sessile (Thome, 1970, p. 88, fig. 5), and has no dif-
ferenfiated stalk as described by Baker (1925, p. 181,
pi. 6, fig. 28). The stimulatory organ has only 9
tubules, of wluch some are bifurcated (Thome, 1970,
p. 175), and not 26, as menfioned by Baker (1925, p.
26
THE NAUTILUS
January 1973
Vol. 87(1)
181). The verge is short, lanceolate, as figured by
Hoffman (1925, pi. 5, fig. 45, d, 2, F) and Thome
(1970, p. 87, fig. 7), and has no spiral ridges, as des-
cribed by Baker (1925, p. 1 81, pi. 6, figs. 29, 30).
Vaginulus (Sarasinulaj plebeius Fischer, 1 868
Material examined: Saint Martin, Leeward islands
(1 spec, FMNH 173062, coll. Oct. 1947 by Oden
Meeker); Saba Island (1 spec, FMNH 157155, coll.
Jan. 1968).
New Caledonia, 19 km north of Boulouparis (2
spec, FMNH 159240, coll. Oct. 1967 by L. Price)
and 8 km west of Bourail, on pierced rock (3 spec,
FMNH 159224, coll. Oct. 1967 by L. Price).
Marianas, Saipan (1 spec, FMNH 173065, coll.
Feb. 1945); Guam, Ritidian Point (1 spec, FMNH
173063, coU Aug. 1945 by H. S. Dybas).
Philippine Islands, Leyte, San Jose (1 spec, FMNH
173064, coll. Dec. 1944 by E. Ray).
Moluccas, Ambon, Wasi (25 spec, FMNH 172984,
172986, 172991, 172992, 172993, coll. 1964, Sept.
1965 by A. M. Wegner).
Remarks: Except for New Caledonia, V. plebeius
was not reported previously from these islands. It is
probably of West Indian origin, and has been acci-
dently introduced to Pacific and Mascarene Islands
(Baker, 1931, p. 135). A full synonymy is given by
Forcart(1969: 150).
Sempenda sclmeideri (Simroth, 1895)
Vagimda sclmeideri Simroth, 1895, SB. Naturf.
Ges. Leipzig, 19/21: 7. - Tandjong, Kuba, East
Sumatra.
Material examined: Tebing Tingii, Pedis, Malaya ( 1
juv. spec, FMNH 156725, colL Feb. 1966 by A.
Berry) under moist leaves at foot of hill.
Sempenda celebensis Hoffmann, 1941
Vaginula melotomus, Bollinger 1918, Rev. Suisse
Zool., 26 (9): 319, not Vagimda melotomus?.
Sarasin & F. Sarasin, 1899.
Semperula idae, Grimpe & Hoffmann 1925, Z.
wiss. Zool., 124 (1): 33-36 partim, fig. 14 (p.
14); Hoffman 1925 Jena Z.Naturw., 61 ('/.):
186-189, 255-256 partim, pL 6, fig. 45, k, 2.
Not Vaginula idae Semper, 1 885.
Vaginula (Semperula) idae, Forcart 1935, Verh.
Naturf. Ges. Basel, 46, p. 54, not Vaginula idae
Semper, 1885.
Semperula wallacei var. celebensis Hoffmann,
1941, Zool. Anz., 136(11/12); 234. New name
for Vaginula melotomus Bollinger, 1918, not P.
Sarasin & F. Sarasin. 1899. Type locality (re-
stricted): South Celebes, Lamontjong. Lecto-
type NMB 2419-b, coll. P. & F. Sarasin
1902/03. 5 lectoparatypes, NMB 2419-a from
Central Celebes, Gimpu, coll. P. & F. Sarasin
1902/03.
Material examined: Western Samoa, Upolu,
Solaua-Sauniato road junction, coconut-cocoa planta-
tion (1 spec, FMNH 152677, coll. Nov. 1965, by A.
Solem & L. Price). Moluccas, Ambon, Wasi (5 spec,
FMNH 172987, 172988, 172991. coll. 1964 by A.M.
Wegner).
On the Veronicellidae from Ambon
Van Benthcm Jutting (1953. p. 300) listed from
the Moluccan Island of Ambon Laevicaulis alte
(Ferussac), Filicaulis bleekeri (Keferstein), and
Sempenda maculata (Templeton). These citations are
erroneous. Martens (1867. p. 176) described the first
Veronicellid known from Ambon as Vaginulus has-
selti. mentioning it (p. 68) from Bangkok, Thailand,
and (pp. 176-177) from Sumatra, Borneo, Ambon,
and Banda. Hoffmann (1925: 136-137), revising
syntypes of V. liasselti (ZMB). found those from
Bangkok and Sumatra identical with Filicaulis
bleekeri (Keferstein. 1865), but those from Ambon
and Banda with Sempenda maculata (Templeton,
1858).
Vagimda bocagei Simroth. 1893 was described as
from Ternate, Ambon, and from Banda. Grimpe &
Hoffmann (1925: 29-30), revising 14 specimens in
the ZMB labeled V. bocagei. probably the syntypes of
V. bocagei, stated that 9 specimens from Ambon are
identical with Sempenda maculata, and 5 specimens
from Banda with Laevicaulis alte (Fer.). Laevicaulis
alte is consequently not known from Ambon, and the
citafions of Ambon as locality of I. alte in Grimpe &
Hoffmann (1925, p. 28) and Hoffmann (1925: 227)
are erroneous.
Tlie revisions of the specimens from Ambon pub-
lished as Vaginulus liasselti and Vaginula bocagei re-
sulted that these determinations arc misinterpreta-
fions for Sempenda maculata, hitherto the sole spe-
cies known from Ambon. Semperula celebensis
Hoffmann and Vaginulus (Sarasinulaj plebeius
Fischer are added to the fauna of Ambon by the new
material.
Vol. 87(1)
THE NAUTILUS
27
ATHORACOPHORIDAE
Aneita (Aiicita) simrothi Grimpe & Hoffmann, 1925
Aiicira simrothi Grimpe & Hoffmann, 1925, in
Sarasin & Roux, Nova Caledonia, 3 (3): 421,
figs. 15e, 16g, 17d, 18e, 20, pi. 5, figs. 5 a, b,
14 a. b. Type locality: New Caledonia, Mt.
Ignambi near Oubatche, 700-1300 m alt.
Syntypes NMB 3448 a, b, coll. April & May,
1911 by F. Sarasin & J. Roux.
Material examined: 6.4 km East of Ouegou, North-
east New Caledonia, at ± 130 m alt. (6 spec, FMNH
159245, coll. Oct. 1967 by L. Price). The biggest
specimen has a length of only 53.8 mm. as compared
with the 85 mm. length of the largest syntype.
LITERATURE CITED
Baker, H. Burrington. 1925. North American Veroni-
ceilidae. Proc. Acad. Nat. Sci. Philadelphia, 77:
157-184, pis. 3-6.
Baker, H. Burrington. 1931. Notes on West Indian
Veronicellidae. Nautilus: 44(4): 131-137, pl. 8.
Benthem Jutting, W. S. S. van. 1953. Annotedlist of
the non-marine Mollusca of the Moluccan Islands
Ambon, Haruku, Saparua and Nusu Laut. Treubia,
22(2): 275-318.
Bollinger, G. 1918. Land-Mollusken von Celebes. Rev.
Suisse ZooL, 26 (9): 309-340, pl. 1 1.
Forcart, L. 1935. Revision der Vaginuliden aus
Celebes in der Sammlung des Easier Natur-
historischen Museums. Verb. Naturf. Ges. Basel,
46: 50-55.
Forcart, L. 1969. Veronicellid land slugs from the
New Hebrides, with description of Semperula
solemi new species. Fieldiana Zool., 51 (12):
147-156.
Grimpe, G. & Hoffmann, H. 1925; Versuch einer Re-
vision der indischen, indo- und polynesischen
Vaginuliden. Z. wiss. ZooL, 124(1): 1-50.
Grimpe, G. & Hoffmann, H. 1925a. Die Nackt-
schnecken von Neu-Caledonien, den
Loyalty-lnseln und den Neuen Hebriden. Sarasin,
F. & Roux, J., Nova Caledonia, A. Zool., 3 (3):
339-476, pis. 5-6.
Hoffmann, H. 1925. Die Vaginuliden. Jena. Z.
Naturw., 61(1/2): 1-374, pis. 1-11.
Hoffmann, H. 1941. Ueber einige Vaginuliden auf
Grund bisher fur verschollen gehaltener
Typstucke. Zool. Anz., 136(1/2): 229-242.
Martens, Ed. 1867. Die Landschnecken. Die Preus-
sische Expedition nach Ost-Asien, Zool., 2: 1-Xll,
1-447, pis. 1-22.
Thome, J. W. 1970. Redescricao dos tipos de Veroni-
cellidae neotropicais: III. Especies depostadas no
"11. Zoologisches Institut und Museum der Univer-
sitiit" de Gbttingen, Alemania. Iheringia Zool., 38:
73-88.
OBITUARY
Gilbert Ranson (1899-1972)
Gilbert Ranson, distinguished French zoologist
and oyster expert died in Paris August 19, 1972, at
the age of 72. He received the equivalent of B. S. in
natural sciences at the Sorbonne in 1923, and was a
student of Louis Joubin. He received his Ph. D. in
1927. his thesis being on the physiology of aquatic
animals. He published well over 200 articles on dia-
toms, medusae and especially the taxonomy of
oysters. In 1951, he authored the book, Les
Huitres—biologie--culture. Dr. Ranson became
sub-director of the Malacological Laboratory of the
National Natural History Museum in Paris in 1938.
He was born in France on September 4, 1899.
St. Croix Shell Booklet
A revised edition of "A Supplementary Listing of
New Shells (Illustrated) to be added to the Check List
of the Marine Shells of St. Croix" by G. W.
Nowell-Usticke was published on Dec. 20, 1971. It is
privately printed and distributed by the author, 1
North St., Christiansted, St. Croix, Virgin Islands
00820, and is available for $3.69 post fiee, or S4.00
by airmail. It has 32 pp., an index, 6 pis., many new
species and subspecies, many of which are synonyms
and/or homonyms.
THE NAUTILUS
January 1973
Vol. 87(1)
SHORT PAPERS
NEW NAME FOR A TEXAN HYDROBIA
J. P. E. Morrison
Division of Mollusks
National Museum of Natural History
Washington. D. C. 20560
CERION FROM AN ARCHEOLOGICAL SITE
IN NORTHERN OHIO
James L. Murphy
Sears Library
Case Western Reserve University
Cleveland, Ohio 44106
A single fragmentary specimen of the terrestial gas-
tropod Cerion incanum (Binney) has been found in
collections from a Late Woodland or Late Prehistoric
village site in Lorain County, Ohio. The Eiden Site
hes on a bluff top in the vUlage of Sheffield, near the
confluence of French Creek and the Black River, two
mOes south of Lake Erie. The collections were made
by A. A. Bungart over ten years ago and are now
being analyzed for the Lorain County Park Board by
Dr. D. H. McKenzie and Dr. J. E. Blank, Cleveland
State University, Dr. 0. C. Shane, Kent State Univer-
sity, and the author.
McKenzie and Blank estimate that the major occu-
pation of the site lasted for approximately 50 years,
sometime between 1300 and 1450 A.D. Minor Early
Woodland and Late Prehistoric components also
occur at the site, however. Nonetheless, the over-
whelming majority of the materials recovered from
the site appear to represent a Late Woodland com-
ponent, and it is very probable that the Cerion shell
found in the general midden represents the Late
Woodland component.
Other shell artifacts associated with the Late
Woodland component include marine shell disc beads,
conch columella beads, and Marginella beads. The
occurrence of such a variety of worked marine shell
in a Late Woodland component is unusual and in it-
self lends support to the contention that the Cerion
shell belongs to the Late Woodland occupation of the
Eiden Site and is a Late Woodland trade item from
the Florida Keys.
Dr. R. Tucker Abbott kindly identified tlie Eiden
shell for me. The rather prominent vertical riblets of
the two last whorls suggest the form saccharimeta,
which Pilsbry (1946: 164) has found to intergrade
with typical C. incanum
The species named Odostomia barret ti Morrison
(Proc. Biol. Soc. Wash. 78: 220, fig. 4, 1965) is pre-
occupied by Odostomia barreti L. Morlet (Journ. de
Conchyl. 33: 314, 1885), as James X. Corgan of
Austin Peay State University, Tennessee, has so kind-
ly pointed out.
On July 25, 1968, with the guidance and helpful
assistance of Mrs. Hollis Q. Boone of Houston, Texas,
a considerable number of these tiny snails were col-
lected from a narrow stretch of intertidal sand on the
west side of Galveston Bay. Examination of the strik-
ingly pink, living animals proved them to belong to
the genus Hydrobia, as reported {in litt.) by Dr.
Robert Robertson of the Academy of Natural
Sciences of Philadelphia.
I wish to rename this brackish water species
Hydrobia booneae in honor of Mrs. Boone, who first
discovered them in numbers in Texas waters. At
present Hydrobia booneae is known to be Uving in
waters of reduced salinity between the northeast
corner of Heron Bay, Mississippi (the southwest
corner of that state) and the west side of Galveston
Bay, Texas.
•
PHYSA ACUTA IN VIRGINIA
Dorothy E. Beetle
Peninsula Nature and Science Center
Newport News, Virginia 23601
Physa acuta Draparnaud, an introduced European
fresh water snail, has been found at several localities
in coastal Virginia. It is well-established at two locali-
ties in the City of Hampton: along the shores of Big
Bethel Reservoir and in a small pond receiving water
pumped out of Rice's Fossil Pit, a well-known marine
Miocene deposit. In the City of Newport News, /%^sa
acuta occurs in Lake Maury. It is in York County at
Wormley Pond in the Colonial National Historical
Park. Another locality is on the North Carolina bor-
der of the City of Virginia Beach, Rt. 165, in a small
pond behind the beach at Currituck Sound.
Pond bottoms consist of sandy silt, and the snaUs
were Ibund along the shore in dead leaves. Specimens
were kindly identified by Dr. Wilham J. Clench.
Vol. 87(1)
THE NAUTILUS
29
SPREAD 0¥ MELANOIDES TUBERCULATA
R. Tucker Abbott
Delaware Museum of Natural History
Greenville, Del. 19803
The freshwater Asian thiarid, Melanoides tuber-
culata (Miiller) is now spreading rapidly southward
from United States into Central America. Mrs. Dot
Myhre, of Stuart, Florida, has sent us specimens col-
lected in the vicinity of Vera Cruz, Mexico, where the
shells are sold by the bagful for making novelties. Dr.
Byron N. Chaniotis, of the Walter Reed Army Insti-
tute of Research, Canal Zone, collected live speci-
mens in Panama in 1971. The snaU, an intermediate
host in China for the bile fluke, Clonorchis sinensis,
arrived in Texas and Florida prior to 1963, and soon
thereafter in Puerto Rico. A distributional map show-
ing the range of the species from North Africa to the
East Indies prior to 1927 was published by Pilsbry
and Bequaert, 1927, BuU. Amer. Mus. Nat. Hist., vol.
53. p. 253.
FRESH-WATER MOLLUSKS FROM
COASTAL VIRGINIA
Dorothy E. Beetle
Peninsula Nature and Science Center
Newport News, Virginia 23601
The following moUusks were collected from small
fresh water creeks and ponds in the independent
Cities of Hampton, Newport News and Virginia Beach
and York County: Anodonta cataracta Say, Pisidium
casertanum Poll, Sphaerium occidentale Prime, S.
partumeium Say, Campeloma decisa Say, Littorid-
inops tenuipes Cooper, Amnicola limosa Say , Pomati-
opsis lapidaria Say, Physa acuta Draparnaud, P.
heterostropha Say, Fossaria humilis Say, F. obrussa
exigua Lea, Pseudosuccinea columella Say, Helisotna
anceps Menke, H. trivolvis Say, Planorbula armigera
Say, P. wheatleyi Lea, Gyraulus parvus Say, Menetus
brogniartianus Lea, M. dilatatus Gould, M. dilatatus
buchanensis Lea, Laevepex fuscus C. B. Adams. Mate-
rial is in the collection of the author.
MONOGRAPH REVIEW
THE GENUS SEMELE IN THE WESTERN
ATLANTIC (Semelidae; Bivalvia) by Kenneth J.
Boss. Johnsonia, Harvard University, Cambridge,
Mass., Vol. 5, no. 49, pp. 1-32. May 25, 1972.
The taxonomic treatment of the six known hying
species of Western Atlantic Semelidae is sufficiently
good to enable workers to identify their unknown
material. The illustrations, descriptions, remarks and
locality records are up to the usual standard of pre-
vious Johnsonia numbers.
Tliere are, however, a startling number of typo-
grapliical errors, spelling mistakes, examples of incor-
rect grammar, and mis-uses of words - at least 97 in
only 32 pages. Part of this can be excused because of
an improved format of the journal, and a change in
printer. Readers should note, however, that the cor-
rect spelling for the common semele is Semele bel-
lastriata (Conrad), not bellestriata, and that the
gender of Semele is feminine (lenticularis, not len-
ticulare, and solida, not solidum). The geological
terms, particularly those such as Group and Forma-
tion, seem not to be employed correctly in several
places. Some biological terms are mis-used, such as
allometric, when allopatric was meant. Scientific
names have been hyphenized, contrary to the
"Rules", such as media-americana on page 11. How-
ever, in the synonymy, they should have been re-
tained, instead of eliminated, as on page 9. The
author, and editor, of this monograph has the sym-
pathy of fellow editors and malacologjsts, but we
shall all look forward to a more painstaking effort in
future numbers. As Dr. Boss recently stated himself
in reviewing another bivalve paper (see Jour. Paleon-
tology, Vol. 45, no. 3, p. 558), "In the final analysis,
the editorial offices ... are responsible for publishing
a manuscript which was never critically reviewed in a
format which was never carefully proofed, and the
short-comings are now the affliction of science ~ to
the embarrassment of all."
R. Tucker Abbott
du Pont Chair of Malacology
Delaware Museum of Natural History
30
THE NAUTILUS
January 1973
Vol. 87(1)
A. M. U. Meeting
INDEX TO THE NAUTILUS
The Thirty-Eighth Annual Meeting of The Amer-
ican Malacologjcal Union will be held in Newark and
Greenville, Delaware, from June 25 through 28,
1973. Lodging and the main meetings will be held on
the campus of the University of Delaware. Early regis-
tration will be possible on Sunday, June 24. One day
of meetings will be held at the Delaware Museum of
Natural History, near Greenville, about 6 miles from
Newark. The current President is Dr. Dee Dundee,
Dept. Biology, Louisiana State Univ., New Orleans,
La. 70150. Further details will be published in the
AMU Newsletter and the April issue of The Nautilus.
Tlie extensive 279-page Author Index to The
Nautilus, vols. 1-75, compiled and published by
Aurele La Rocque in 1963 is still available (unbound)
for the extremely low price of $2.00 postpaid. A con-
tinuation, covering vols. 76-85, was recently pub-
lished in no. 49 of Sterkiana, 1972. Reprints of tliis
very useful addition are also avaUable for 25 cents.
Wlien ordering both of these indispensable indices, we
suggest an additional 50 cents be added to cover
postage. Write: Dr. Aurele La Rocque, 125 South
Oval Dr., Ohio State Univ., Columbus, Ohio 43210.
The first truly comprehensive
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MORE THAN 250 MAGNIFICENT ILLUSTRATIONS, 100 IN FULL COLOR
In this one colorful volume the entire
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guidance takes the reader from
man's early use of shells to today's
fascinating pursuit of oceanic
treasures. Written by one of the
world's leading authorities, it
provides a wealth of information and
lore about shells (their biology;
their influence on art, medicine,
religion, and archeology; their
importance in commerce), a complete
guide for the collector, and much
more. The brilliant photographs, more
than 100 of them in full color, make
this important and useful book a
delight to the eye as well as
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APRIL, 1973
THE
NAUTILUS
Vol. 87
No. 2
A quarterly
devoted to
malacology and
the interests of
conchologists
V
Founded 1889 by Henry A. Pilsbry. Continued by H. Burrington Baker.
Editors: R. Tucker Abbott and Charles B. Wurtz
EDITORIAL COMMITTEE
CONSULTING EDITORS
Dr. Arthur H. Clarke, Jr.
Department of Mollusks
National Museum of Canada
Ottawa, Ontario, Canada KIA-0M8
Dr. William J. Clench
Curator Emeritus
Museum of Comparative Zoology
Cambridge, Mass. 02138
Dr. William K. Emerson
Department of Living Invertebrates
The American Museum of Natural History
New York, New York 10024
Mr. Morris K. Jacobson
Department of Living Invertebrates
The American Museum of Natural History
New York, New York 1 0024
Dr. Aurele La Rocque
Department of Geology
The Ohio State University
Columbus, Ohio 43210
Dr. James H. McLean
Los Angeles County Museum of Natural History
900 Exposition Boulevard
Los Angeles, Cahfornia 90007
Dr. Arthur S. Merrill
Biological Laboratory
National Marine Fisheries Service
Oxford, Maryland 21654
Dr. Donald R. Moore
Division of Marine Geology
School of Marine and Atmospheric Science
10 Rickenbacker Causeway
Miami, Florida 33149
Dr. Joseph Rosewater
Division of Mollusks
U. S. National Museum
Washington, D.C. 20560
Dr. G. Alan Solem
Department of Invertebrates
Field Museum of Natural History
Chicago, Illinois 60605
Dr. David H. Stansbery
Museum of Zoology
The Ohio State University
Columbus, Ohio 43210
Dr. Ruth D. Turner
Department of Mollusks
Museum of Comparative Zoology
Cambridge, Mass. 02138
Dr. Gilbert L. Voss
Division of Biology
School of Marine and Atmospheric Science
10 Rickenbacker Causeway
Miami, Florida 33149
EDITORS
Dr. R. Tucker Abbott
Delaware Museum of Natural History
Box 3937, Greenville, Delaware 19807
Dr. Charles B. Wurtz
3220 Penn Street
PhUadelphia, Pennsylvania 19129
Mrs. Horace B. Baker
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THE
NAUTILUS
Volume 87, number 2 -- April 1973
CONTENTS
Thomas R. Waller
The Habits and Habitats of Some Bermudian Marine MoUusks 31
Richard Edward Young
Evidence for Spawning by Gonatus sp. (Cephalopoda: Teuthoidea) in the High Arctic Ocean 53
S. L. H. Fuller and C. E. Powell, Jr.
Range Extensions of Corbicula maiiilensis (Philippi) in the Atlantic Drainage of the United States . .59
Margaret C. Teskey
Emarginula dentigera Heilprin, 1 889, a Littoral Mollusk 60
Book Reviews
(of) S. Peter Dance, 52; A. Myra Keen, 58
News; AMU Meeting in June 1973 59, 60
The first truly comprehensive
and authoritative survey of shells
MORE THAN 250 MAGNIFICENT ILLUSTRATIONS, 100 IN FULL COLOR
In this one colorful volume the entire
field of shells is covered. Expert
guidance takes the reader from
man's early use of shells to today's
fascinating pursuit of oceanic
treasures Written by one of the
world's leadmg authorities, it
provides a wealth of information and
lore about shells (their biology:
their influence on art. medicine,
religion, and archeology: their
importance in commerce), a complete
guide for the collector, and much
more The brilliant photographs, more
than 100 of them in full color, make
this important and useful book a
delight to the eye as well as
informative and engrossing reading
8%" X 11 'A", A Rutledge Book,
KINGDOM OF
THE SEASHELL
$14 95, now at your bookstore Of
ogy, CROWN PUBLiSHERS
al History 419 Park Ave Soutri, New York, N Y 10016
Ul
. »»»»»»\»»»»»w%%»»»»»»»»*»*»*v»»»»»»»»»»w»»*v»\»»»w»»»»*»»*^
ii^ne ibneu Lamnet
Successor to:
Richard E. Petit
and
John Q. Burch
OLIVE SHELLS
OF
THE WORLD
SPECIMEN SHELLS
NATURAL HISTORY
BOOKS
ROWLAND f ZEIGLER
HUMBERT CPORRECA
International Directory of Conchologists - $3.00
A current worldwide list of 2,000 people interested
in mollusks and in exchanging shells. Gives addresses
and interests. Available only from The Shell Cabinet.
Olive Shells of the World by Zeigler and Porreca -
$12.95
13 full-page color plates illustrating over 150 species
and named varieties. The only current treatment of
the popular family. Clothbound. Available from your
book store or directly from us.
Other Recently Published Shell Books Available
Post Office Box 29, Falls Church. Virginia 22046
Sea Shells of
Tropical West America
Marine Mollusks from Baja California to Peru
Second Edition. A. Myra Keen with the assistance of James H.
McLean. This revised and expanded classic now treats all molluscan
species recorded from the Panamic province and is illustrated with
over 4,000 halftones and 85 color photographs. The geographic range
has been extended to northwestern Peru. The coverage now extends to
microscopic and deepwater species and to the shell-less mollusks.
For most of the 3,325 species there are detailed descriptions,
synonymies, range data, notes, and one or more illustrations. Included
are anatomical drawings, identifying keys, introduction and
systematics, rejected species, maps and place-name list, glossary,
bibliography, and index. 1,120 pages. $29.50
Stanford University Press
Vol. 87 (2)
THE NAUTILUS
31
THE HABITS AND HABITATS OF SOME BERMUDIAN MARINE MOLLUSKS'
Thomas R. Waller
Department of Paleobiology
Smithsonian Institution
Washington, D. C. 20560
ABSTRACT
During a Jiving sun'ey of the living habits of scallops ( Pectinidae j in bermudian
waters, 160 species of shelled mollusks were collected at 40 diving stations. The
shallow-water bias in previous bermudian collecting is indicated by the fact that 17 of
these species have not previously been reported from Bermuda and 15 of these new
records are from depths greater than 30 m. Among the new records are five species of
the bivalve family Pectinidae, including Argopecten noronliensis (E. A. Smith),
previously known only from off Brazil but now known to be widely but sparsely
distributed in the tropical western Atlantic from Brazil to Bermuda.
Habitat preferences and living habits are described for several species, including a
discussion of species in Harrington Sound relative to the ecological zones described by
Neumann (1965). Twenty-one species inadequately figured in the literature are
illustrated using optical photographs and scanning electron micrographs.
INTRODUCTION
Despite the fact that Bermuda has been a haven
for malacologists since Angelo Heilprin and A. E.
Verrill first visited the islands in the late 1800's, the
habitats of Bermudian moUuscs are still poorly
known. Many of the older collections, althougli rich
in numbers of taxa, are poor in habitat data and
commonly list only "Bermuda" as the sole record
of occurrence for a species. The purpose of tliis
paper is to provide data on the habits and habitats
of species collected through diving and to illustrate
certain poorly known or previously unillustrated
species.^
During a period of two weeks in late May, 1971,
marine moUuscan communities were surveyed by
the author and two diving assistants using SCUBA
equipment. Althougli the primary purpose of the
survey was to gather data on the living habits and
habitats of scallops known from Bermudian waters,
collections of other shelled mollusks were made at
most of the diving stations. At most stations col-
lecting was by visual spotting and hand picking. In
the interest of conservation, many living individuals
were examined underwater and returned to their
habitat, with later identification assisted by dead
shells of the same species found at the site. At the
stations deeper than 30 m (Stations 21, 24, and
39), in the deepest portions of Harrington Sound
(Stations 1 and 6), and on the bottom of Wal-
singham Pond (Station 11), short non-decom-
pression time limits or turbid conditions prevented
visual collecting, and sediment samples in both net
and plastic bags were taken instead. These sediment
samples were retained in running salt water and
later examined in the laboratory for living material.
The resulting coUections contain about 160
species of shelled mollusks (Table 1) distributed
among 40 diving stations (Figs. 1, 2, and Table 2).
Surprisingly, 17 of these species have not been
previously recorded from Bermudian waters.^ Be-
cause all but two of these new records are from the
three diving stations deeper than 30 m (Stations 21,
24, and 39), it is clear that much of our present
'Contribution No. 546, Bermuda Biological Station
for Research, St. George's West, Bermuda.
^With regard to new records, 1 am indebted to Mr.
Russell Jenson, Assistant Curator, Department of
Mollusks, Delaware Museum of Natural History. It
is through his help and his extensive records,
compiled through a painstaking search of the liter-
ature on Bermuda, that I can with reasonable
confidence refer to species as having been
previously unreported.
32 THE NAUTILUS
April 1973
Vol. 87 (2)
knowledge of the Bermudian marine fauna is based
on shore and shallow-water coUections. Although
the West Indian character of the fauna has long
been known, it is probable that more intensive
collecting by means of diving (deeper than 45 m)
and other methods not avaUable to early collectors
will continue to turn up a wealth of species pre-
viously thougjit to be restricted to the West Indies
proper or to the Atlantic coast of South America.
The stations listed below are plotted in Figures 1
and 2. Groupings of stations according to general
environment or ecological zone are shown in Table
2.
Station 1. DevO's Hole, Harrington Sound.
Depth, 25 m; bottom temperature, about 20° C;
barren mud bottom with mounds, trails, fine ex-
crement, and small shells. May 19, 1971.
Station 2. Devil's Hole, Harrington Sound, on a
line extending southeastward from Station 1. Depth,
17 to 9 m; fine sand bottom with abundant
Oculina, Area, and Pododesmus. May 19, 1971.
Station 3. Devil's Hole, Harrington Sound, on a
line extending southeastward from Station 1. Depth,
9 to 6 m; coarse sandy bottom with little vegetation
and abundant Area zebra. May 19, 1971.
Station 4. Rocky shore on east side of Devil's
Hole, Harrington Sound. Depth, 0 to 3 m. May 19,
1971.
Station 5. Between Trunk Island and Small Is-
land, Harrington Sound. Depth, 3 to 4 m; sandy
FIG. I . Map of the Bermuda Islands showing loeations of diving stations.
Vol. 87 (2)
THE NAUTILUS
33
bottom with scattered patches of grass. May 19,
1971.
Station 6. Shark Hole, Harrington Sound, along
traverse extending north northwestward from a
depth of 21 m. Depth, 21 to 18 m; bottom
temperature, 19° C; barren mud bottom witli
mounds, trails, scattered shells, and Oculina frag-
ments. May 20, 1971.
Station 7. At 32° 20.2' N, 64° 42.5' W, near
Shark Hole, Harrington Sound. Depth, 18 to 11 m;
fine sand bottom with abundant Oculina. May 20,
1971.
Station 8. Near Station 7, Harrington Sound.
Depth, 8 to 1 1 m. May 20, 1971. No collection was
made at this station.
Station 9. Midway between Abbot's Cliff and
Trunk Island, Harrington Sound. Shoal area with
large areas of barren, sandy bottom covered with
the shells of Area. May 20, 1971. No collection
made.
Station 10. Southwest side of Trunk Island,
Harrington Sound. Depth, 3 to 6 m; sandy bottom
with patches of grass. May 20, 1971.
Station 11. Walsingham Pond, Bermuda Island.
Depth, 1.5 to 6 m; barren, dark, soupy mud bottom
with film of organic matter and small shells. May
21, 1971.
Station 12. Seaward side of rocks at mouth of
Whalebone Bay, western end of St. George's Island.
Depth, 4.5 m; water temperature, 22°C; coarse sand
bottom with abundant hard coral and Gorgonacea.
May 22, 1971.
Station 13. Western end of Church Bay, Har-
rington Sound. Depth 3 to 6 m. May 22, 1971.
Station 14. Hungry Bay, on south shore of
Bermuda Island. Depth, 1 m; coarse sand bottom
FIG. 2. Map of Harrington Sound, Bermuda, showing locations of diving stations with respect to the zonation
of Neumann (1965).
34 THE NAUTILUS
April 1973
Vol. 87 (2)
with broad-bladed marine grass and the alga, Pedina.
May 24, 1971.
Station 15. Outside mouth of Hungry Bay, on
south shore of Bermuda Island. Depth, 4.5 to 8 m;
water temperature, 22° C; bottom of coarse sand
and bare rock with potholes. May 24, 1971.
Station 16. Off small bay between Tobacco Bay
and Coot Pond, northern St. George's Island. Depth,
6 to 8 m; water temperature 22 to 23° C; coarse
sand bottom with large and small coral-covered
rocks. May 24, 1971.
Station 17. Buildings Bay, near eastern tip of St.
George's Island. Depth, 0.5 to 3.5 m; very coarse,
ripple-marked sand bottom with some large rocks
and abundant green to lavender leafy algae. May 24,
1971.
Station 18. At 32° 22.4' N, 64° 39.2' W, off
mouth of pass between Paget Island and St. Davids
Island. Depth, 6 to 7 m; water temperature, 21.5°
C; coarse, ripple-marked sand with patches of coral
and leafy algae. May 25, 1971.
Station 19. Near Station 18, but further from
shore. Depth, about 6 m. May 25, 1971. No
collection.
Station 20. Higgs Cut, between Higgs Island and
Paget Island at eastern end of St. George's Harbor.
Depth, 0.5 to 4.5 m (within small boat channel and
surrounding area) and 6 m (deep hole at western
end of cut); bottom fine sand and grassy in shallow
water, barren sand at bottom of channel. May 25,
1971.
Station 21. At 32° 30.6' N, 64° 38.2' W, north-
east of "North East" marker buoy. Depth, 37 m;
bottom water temperature, 20.5° C; small coral
knolls rising a few feet from the bottom and
separated by patches of very coarse, ripple-marked
sand. May 26, I97I.
AH specimens recorded from this station were
picked from bulk samples taken from the sand
patches.
Station 22. Anchor chain of "North East"
marker buoy, 32° 30.2' N, 64° 38.5' W. Depth, 6
m. May 26, 1971. No collection.
Station 23. Top of large patch reef between St.
George's Island and "North East" marker buoy
(Station 22). Exact position not plotted. Depth, 18
m. May 26, 1 97 1.
Station 24. At 32° 18.2' N, 64° 40.8' W, off
south shore of Tucker's Town. Depth, 34 m; bot-
tom temperature, 20.5° C; higli coral patches with
scattered small areas of coarse sand. May 27, 1971.
Station 25. At 32° 19.6' N, 64° 41.4" W, inside
breaker zone off south shore of Tucker's Town.
Depth, 6 to 8 m; patch reefs surrounded by coarse,
ripple-marked sand. May 27, 1971.
Station 26. At 32° 22.6' N, 64° 39.0' W. off
entrance to St. George's Harbor. Depth, 6 to 18 m;
coral platform rising 12 m above a medium to fine
sand bottom May 27, 1971.
Station 27. At 32° 23.9' N, 64° 40.9' W, north
northeast of St. Catherines Point, St. George's Is-
land. Depth. 14 m; water temperature, 22° C: silty
mud bottom with large colonies of Ociilina. May
28, 1971.
Station 28. At 32° 24.8' N. 64° 41.2' W, north-
east of St. Catherines Point, St. George's Island.
Depth, 4.5 to 8 m; patch reef with prolific, diverse
coral. May 28, 1971.
Station 29. South side of Ferry Point, western
tip of St. George's Island, from rocky shore to a
depth of 4.5 m in the channel between Ferry Point
and Coney Island. May 29. 1971.
Station 30. At 32° 21.6' N, 64° 42.7' W, in
shallow area in mouth of Ferry Reach southwest of
Ferry Point. Depth, 1.5 to 3.5 m; Ociilina patch
reef and adjacent sandy bottom. May 29, 1971.
Station 31. North half of Ely's Harbor, Somerset
Island. Depth, 1.5 to 6 m. May 30, 1971.
Station 32. Off mouth of Ely's Harbor, Somerset
Island. Depth, 2.5 m; patch reef on sandy bottom.
May 30, 1971. No collection.
Station 33. South half of Ely's Harbor, Somerset
Island. Depth, 1.5 to 6 m. May 30, 1971.
Station 34a. In channel between Wilsons Island
and Bermuda Island, Port Royal Bay. Depth, 1.5 to
4 m; fine silty bottom with mounds, worm tubes,
and few holothurians. May 30, 1971. No collection.
Station 34b. East side of Wilsons Island, Port
Royal Bay. Depth. I to 4.5 m; sandy, trash-covered
bottom at base of steep, rocky drop-off. May 30,
1971.
Station 35. North end of Grace Island, Great
Sound. Depth, 4.5 m; barren, fine sand bottom at
base of rocky drop-off. May 30. 1 97 1. No
collection.
Station 36. Between Hunts Island and Perots
Island, Port Royal Bay. Depth, 3.5 to 5.5 m; firm,
clean sand bottom with grass in shallow areas. May
30, 1971. No collection.
Vol. 87 (2)
THE NAUTILUS
35
Station 37. Transect across channel between Burt
Island and Darrell Island, Great Sound. Depth, 1 to
4 m; firm, fine sand with patches of grass. May 30,
1971.
Station 38. Channel between Coney Island and
Bermuda Island at northeastern tip of Bermuda
Island. Depth, 0.5 to 4.5 m. May 31, 1971.
Station 39. At 32° 18.1' N, 64° 40.2' W, off
south shore of Tucker's Town. Depth, 51 m;
rubbly, coarse, foraminiferal sand with abundant
dark red algal nodules. June 1, 1971.
NOTES ON HABITATS
Harrington Sound
Siibthermocline Zone. Neumann (1965) has pro-
vided an excellent account of the bathymetry,
hydrography, and ecological zonation of Harrington
Sound. As described by Neumann (p. 1003), the
SubthermocUne Zone (Fig. 2) has an abrupt upper
boundary at a depth of 17 m (55 feet), at which
the extensive, essentially barren mud bottom of this
zone meets an area of abundant branching, bushy
coral (Oculinaj, characterized by Neumann as the
Oculina Zone. This zonal boundary is the result of
seasonal water stratification and coincides with the
deepest position of a thermocline in summer.
During the summer there is little mixing of water
beneath the thermocline, resulting in cooler, ox-
ygen-poor water below. Neumann described the
subthermocline bottom as a smooth and barren
surface marked only by the scattered holes of
burrowing organisms, possibly crustaceans, and
having patches of a thin purplish algal or bacterial
mat. He reported the valves of the small bivalve
Transennella conradina (but see below) as common
on the mud surface, with a few live specimens, and
added that this species is the only significant cal-
careous form.
Our observations confirm Neumann's. At Station
1, near Devil's Hole, we found the upper boundary
of the Subthermochne Zone to be sharp and to he
precisely at 17 m. Although underwater visibility
was less than 1 m, we observed that the mud
bottom was marked with numerous mounds, traUs,
small dead moUusk shells, and a Utter of fine
excrement. The dominant bivalve is Gouldia cerina
(see Notes on Taxa), not Transennella as reported
by Neumann, and all specimens were dead. In
addition we recovered a single valve of a young
Pitar fulminata as well as numerous dead specimens
of a tiny diastomid gastropod (Fig. 26), Finella
dubia (Orbigny).
The traverse comprising Station 6 (Fig. 2) ap-
proached the upper boundary of Neumann's Sub-
thermocline Zone, which here is within a depth
interval of 17 to 18 m. We observed that the actual
thermocline was very close to this boundary, with
water temperature rising from 19° C below the
thermocline to 21 above. The more varied fauna
than that collected from the same zone at Station 1
is most hkely due to the fact that we were near the
upper boundary of the Subthermocline Zone at
Station 6. Most of the shells collected are rather
old, the exceptions being the abundant Gouldia and
less abundant Pitar, the same bivalves represented at
Station 1. The valves of Argopecten gibbus collected
here are of particular interest and are discussed
under Notes on Taxa.
As pointed out by Stanley (1970, p. 83), suspen-
sion feeders (such as Gouldia and Pitar) living on
soupy muds face the problem of being clogged by
loose, fine-grained sediment as they sink into the
substrate. Most inhabitants of this type of bottom
remain small, thus keeping their surface-volume
ratio large and maximizing support from the sub-
stratum per unit of animal weight. Gouldia appears
to be an opportunistic species that colonizes the
Subthermocline Zone at times when conditions are
most favorable, probably during the time of max-
imum water mixing in the winter. The species then
flourishes until conditions become lethal, probably
during maximum summer stagnation.
Oculina Zone. Stations 2 and 7 in Harrington
Sound are within the Oculina Zone of Neumann
(1965, p. 1001), an area between 9 and 17 m (30
and 55 feet) in depth characterized by a fine sand
bottom and abundant growth of the branching
coral, Oculina valenciennesi. As described by Neu-
mann, the coral supports itself on the soft mud by
forming bush-like growths on its own debris or on
clusters of Area zebra. Area zebra is by far the most
common mollusk in this zone and lives byssally
attached in clusters on or near the bottom. Other
common bivalves (Table 1) are Pododesmus rudis
(attached to Oculina), Chama congregata (attached
to any hard object), and Lithophaga bisculcata
(boring into Oculina). Neumann described
Vermicularia as abundant in the Oculina Zone, and
Gould (1969, p. 432) has also noted the common
association of Vermicularia and Oculina. Neumann's
36 THE NAUTILUS
April 1973
ol. 87 (2)
report of Anomia simplex as common in this zone
could not be confirmed, and it is probable that he
was referring to Pododesmus, which was absent
from his list.
Shallow Sandy Zone. Stations 3, 5, 8-10, and 13
lie within the Shallow Sandy Zone of Neumann
(1965, p. 1001), an area extending in depth from 9
m to the surface (Fig. 2). As described by Neu-
mann, the sandy floor is covered by marine grasses,
sponges, and algae in the well-lit regions down to
about 4.5 m. Below 4.5 m grass is less abundant
and there are more open sandy areas, frequently
with large clusters oi Area zebra.
The western end of Church Bay, Harrington
Sound (Station 13, Fig. 2), within the harbor of a
private estate, has a silty sand bottom with little
vegetation, common Cassiopeia (the bottom-dwelling
jellyfish), and common Anadara notabilis. About 30
m. out from shore the bottom is more typical of
the Shallow, Sandy Zone, with patches of marine
grass, coarser, barren sand, abundant Area zebra,
and many living Argopecten gibbus, Pecten ziczac,
and Macrocallista maculata. Over sandy bottoms
near the rocky shore of Church Bay, both Pinctada
and Anomia are common on the abundant bottles
and other trash that litter the bottom.
Walsingham Pond
Twenty years ago De Laubenfels (1950, p. 194),
in his colorful style, described the rock walls of
Walsingham Pond as a sponge metropolis and noted
that the bottom is largely mud-covered, but so deep
that the water is clear. A more detailed summary of
conditions in the pond was provided by Walton
(1969), who studied the bathymelr), sediments, and
water chemistry. Tlie maximum depth is about 6 m
and the bottom througliout the deeper portions of
the pond consists of soupy, pelleted mud covered
by a mat of organic matter 5 to 10 cm. thick. The
most abundant moUusks in this soupy, mud layer
are, according to Walton (op. cit., p. 44), Batillaria,
Vermicularia, and Gouldia.^ Beneath this layer is a
thicker layer of brown pelleted mud with more
abundant shells interpreted by V.alton to represent a
time when the pond was less restricted than at
present. Gould (1968) studied the moUuscan fauna
of Walsingham Pond, listing 9 species of bivalves
and 15 species of gastropods. Although he did not
distinguish living from dead or fossil material, he
stressed the similarity of the overall assemblage to
other mangrove-mud environments in Bermuda.
Our collecting concentrated on the mud bottom
of the southwest arm of the pond. Contrary to the
pristine quality of water implied by De Laubenfels'
description, liglit penetration to the bottom of the
pond is now very low, and it was necessary to use
liglits in order to see small objects on the bottom.
Underwater visibility was poor and would rapidly
drop to zero if we allowed our trail of disturbed
mud to overtake us. As noted by Gould (1968), the
bottom harbors a profusion of the bottom-dweUing
jeUyfish, Cassiopeia. Below the organic tllm and
soupy layer is an accumulation of small shells.
^I infer that Walton's "Batillaria minima" is actually
Cerithium variabile and his Gouldia is actually
small Ctena orbiculata.
FIGS. 3-15. Bermuda Marine MoUusks. All specimens in optical photographs are coated with ammonium
chloride and those in scanning electron micrographs coated with gold unless indicated otherwise.
FIGS. 3, 4. Matching left and right valves of Aequipecten acanthodes (Dallj, syntype, USNM 333637, Santa
Lucia, Cuba, height 31.5 mm,
FIGS. 5-7. Right valve uncoated, matching left valve coated, and sculptural detail of left valve f.x 9),
Argopecten noronhensis (E. A. Smith), USNM 501857, Barbados, height 15.0 mm.
FIG. 8. Fragment of left valve of Argopecten noronhensis (E. A. Smith), USNM 708130, Bermuda Sta. 39,
height of fragment 8.0 mm
FIGS. 9-11. Chlamys multisquamata (Danker), matching left and right valves of specimen from off Palm
Beach, Florida, in collection of F. M. Bayer, height 46.8 mm, and fragment of valve, USNM 708131, Bermuda
Sta. 39, height of fragtnent 7.0 mm.
FIGS. 12, 13. Structural detail of outer surface (x 17) and inner surface of right valve of Neopycnodonte
cochlear (PoH), USNM 708132, Bermuda Sta. 39, height 12.5 mm.
FIGS. 14, 15. Matching left and right valves of Limaria hyalina (Verrill and Bush), USNM 708133, Bermuda
Sta. 39, height 4.1 mm.
Vol. 87 (2)
THE NAUTILUS
37
,|ii'
% m
A
r4'.uW,
14
Bermuda Marine Mollusks
(explanation on opposite page)
38 THE NAUTILUS
April 1973
Vol. 87 (2)
primarily Vermicularia, Cerithium, and Ctena
(Table 1). Live individuals of these species were
brought up in samples, but their living positions in
the substrate were not observed. Seven species of
bivalves and 26 species of gastropods were re-
covered, with the most abundant species essentially
the same as those hsted by Gould (op. cit., p. 3).
However, our samples, obtained by visual collecting
and digging in the muddy bottom by hand, con-
tained no Gouldia cerina, listed as "very common"
by Gould, and numerous Anachis catenata, not
recovered by Gould. Many of the less common
species in the pond (see Table 1, Station 11)
undoubtedly come from the fossil shelly layer men-
tioned above.
Although many of the species Usted may have
dropped off the rock walls of the pond, many also
probably hve on the organic debris and algae coat-
ing the muddy bottom, as suggested by a com-
parison of the list of these species with the Ust of
molluscan-algal associations of Warmke and
Almodovar (1963). The abundance of Ctena
orbiculata in the pond may reflect stress conditions.
Jackson (1970, p. 586) found that lucinids are
tolerant of stagnant conditions involving the pres-
ence of hydrogen sulfide and, unlike most other
bivalves, are able to feed on microbial populations
present on plant detritus.
Other Localities
Hungry Bay. Hungry Bay (Station 14), on the
south shore of Bermuda Island, is very shallow, less
than 1 m. deep at low tide, with a bottom of coarse
sand vvdth broad-bladed marine grass and coral frag-
ments. The small alga, Pedina, is also abundant, and
it is in this shallow area that we found many small
(5 mm) Chione. At the entrance to the bay and out
to a depth of about 8 m (Station 15), the max-
imum depth of this dive, the bottom is rock with a
thin algal covering broken here and there by the
tootli marks of large parrot fish. Pot holes up to 1
m. deep and some deep channels have been scoured
out of the rock, and the turbulence of the area has
left few rocks small enough to overturn. Under the
few that could be overturned, Barbatia domingensis
was common. Malleus candeanus was seen far be-
FIGS. 16, 17. Right valve and hinge (x 15) of Erycina sp. aff. E. linella Dall, USNM 708134. Bermuda Sta.
24, length 6.2 mm
FIG. 18. Right valve of Carditopsis smitlii (Dall), scanning electron micrograph, USNM 708135, Bermuda Sta.
11, height 1.7 mm.
FIG. 19. Prodissoconch o/ Carditopsis smithi (Dall), scanning electron micrograph, USNM 708136, Bermuda
Sta. 11, length 0.39 mm.
FIG. 20. Alvania didyma (Watson), scanning electron micrograph, USNM 708137, Bermuda Sta. 21, height 2.1
mm
FIG. 21. Alvania platycephala Dautzenberg and Fischer, scanning electron micrograph, USNM 708138,
Bermuda Sta. 11, height 2.4 mm,
FIG. 22. Caecum delicatulum Verrill and Bush, scanning electron micrograph, USNM 708139, Bermuda Sta.
11, height 2.9 mm
FIG. 23. Cerithiopsis cyntliia? Bartsch, USNM 708140, Bermuda Sta. 24, height 5.0 mm.
FIG. 24. Triphora mirabilis (C. B. Adams), USNM 708141, Bermuda Sta. 24, height 9.0 mm.
FIG. 25. Pusia variata? (Reeve), USNM 708142, Bermuda Sta. 21, height 18 mm.
FIG. 26. Finella dubia (Orbigny), USNM 708143, Bermuda Sta. 1, height 3.3 mm.
FIG. 27. Aesopus stearnsi Tryon, USNM 708144, Bermuda Sta. 21, height 4.9 mm.
FIG. 28. Thala foveata (Sowerby), USNM 708145, Bermuda Sta. 24, height 4.4 mm.
FIG. 29. Pyrgocythara candidissima (C. B. Adams), USNM 708146, Bermuda Sta. 39, height 4. 7 mm.
FIG. 30. Odostomia didyma Verrill and Bush, scanning electron micrograph, USNM 708147, Bermuda Sta. 11,
height 1. 8 mm.
FIG. 31. Mitrolumna bipUcata (Dall), USNM 708148, Bermuda Sta. 39, height 3.9 mm.
FIG. 32. Odostomia nioba Dall and Bartsch, scanning electron micrograph, USNM 708149, Bermuda Sta, 21,
height 2.5 mm.
FIG. 33. Turbonilla heilprini Bush, scanning electron micrograph, USNM 708150, Bermuda Sta. 11, height 2.8
mm
Vol. 87 (2)
THE NAUTILUS
39
16
17
^^^i''^^ 18
^*5
iiv
Bermuda Marine Mollusks
(explanation on opposite page)
40 THE NAUTILUS
April 1973
Vol. 87 (2)
neath the overhangs of pot holes and channels,
whereas Chama was common atop the bare rock
surface.
Ely's Harbor. Almost the entire area of Ely's
Harbor was surveyed for the presence of scallops by
towing divers behind the boat, but no living spec-
imens were found. In the north half of the harbor
(Station 31), the bottom in the center is soft,
barren mud or silt with some coral-covered rocks.
Peripheral areas are sandy and grassy with scattered
clusters oi Area zebra.
North Lagoon. The bottom features and fauna at
Station 27, north of St. George's Island, are very
similar to those in the Oculina Zone of Harrington
Sound (Neumann, 1965; see preceding notes) with
the dominant mollusks being Area zebra, Po-
dodesmus rudis, Vermieularia, Spondylus, and
Chania. Many dead Chlamys imbricata, not found in
Harrington Sound, were present at this station, but
no living individuals could be found after an in-
tensive search.
Outer Platfonru The deepest areas sampled lie
well outside of the breaker zone: Station 21 (depth,
37 m). Station 24 (depth, 34 m) and Station 39
(depth, 51 m). The bottom at these stations consists
of patches of barren coarse carbonate sand, gen-
erally ripple marked, with intervening patches of
coral and algae. Tlie sand at Station 39 consists
almost entirely of the tests of the foraniinifer,
Amphistegiim gibbosa. and the bottom is strewn
with maroon algal nodules. Bulk samples of the
sand yielded a profusion of small shells, particularly
gastropods such as Euchelus giittarosea, Zebina
browniana, various cerithiopsids, Triphora mirabilis.
Trivia quadripimctata. various columbellids and
margineUids, and Williamia krcbsiL Small bivalves
are also common, particularly Area imbrieata,
Barbatia domingensis. fragmented Comptopallium
antillanim, Spondylus, Lima lima, Chama sarda,
Trigonioeardia media, and Gouldia eerina. The
bivalve Ventrieolaria rugatina, previously unknown
from Bermuda, increases in both size and abundance
from Station 24 to the deepest station (Station 39).
In addition to the small mollusks, the tiny
brachiopod, Argyrotheea benmidana (Dall, 1911), is
common in the sand at Stations 24 and 39. Pre-
sumably these specimens, like the many byssate and
cemented bivalves that are also found in the sed-
iment, have become detached from living sites
among and beneath small corals.
The fact that 1 5 out of 1 7 new records listed in
Table 1 are from the three outer-platform stations is
a striking indication of how httle is known about
the Bermudian molluscan fauna from these depths.
TABLE L List of speeies of shell-bearing Mollusca eollected in Bermuda, with references to
illustrations and eollecting stations. The order of families follows that of Moore (1969) for the
bivalves and Taylor and Sohl (1962) for the gastropods. Taxa are alphabetically arranged within
each family. Station numbers in bold-face type indicate living specimens; other specimens are
represented by shells only. Species not previously known from Bermuda are preceded by an
asterisk (*). Specimens that document the list are deposited in the collections of the
Department of Invertebrate Zoology, National Museum of Natural History, Smithsonian
Institution, Washington, D. C.
Species
BIVALVIA
Anadara notabilis (Roding, 1798)
Area imbricata Bruguiere, 1789
Area Zebra (Swainson, 1 833)
Barbatia (Area) domingensis (Lamarck, 1819)
*Barhatia (Fugleria) tenera? C. B. Adams, 1845
Barbatia sp.
Arcopsis adamsi (E. A. Smith, 1888)
Brachidontes sp.
Lithophaga bisulcata (Orbigny, 1 842)
Illustration
Stations
Warmke and Abbott 3, 5, 10, 13
Warmke and Abbott 12, 18, 21, 24, 27, 39
Warmke and Abbott 2, 3, 5, 6, 7, 9, 10, 13, 27
29, 31,33, 34b, 35, 39
Warmke and Abbott 11, 12, 15, 18, 21, 24, 27, 39
Warmke and Abbott 39
24
Warmke and Abbott 6, 24
Warmke and Abbott 2, 7
Vol. 87 (2)
THE NAUTILUS
41
Species
Modiolus amcricamis Leach, 1815
Musculus lateralis (Say, 1822)
Pinna carnea Gnielin, 1791
Pinctada imhricata Roding, 1 798
Pteria colymbus (Roding, 1798)
Isognomon radiatus (Anton, 1839)
Isognomon sp.
Malleus (Malvufundus) candeanus (Orbigny, 1842)
Aequipecten acanthodes (Dall, 1925)
Argopecten gibbus (Linndiews,, 1758)
*Argopecten noronhensis (E. A. Smith, 1885)
*Chlamys benedicti Verrill and Bush, 1897
Chlamys imbricata (Gmelin. 1791 )
*Chlamys multisquamata (Dunker, 1864)
*Comptopallium antillanim (Recluz, 1 853)
*Pecten chazaliei Dautzenberg, 1900
Pecten ziczac (Linnaeus, 1758)
Spondylus americanus Hermann, 1781
Anomia simplex Orbigny, 1842
Pododesmus rudis (Broderip, 1834)
L/ma L(wa (Linnaeus, 1758)
*Limaria hyalina (Verrill and Bush, 1 898)
*Neopycnodonte cochlear (Poli, 1795)
Lop/;a /o //a (Linnaeus, 1758)
Anodontia schrammi (Crosse, 1876)
Codakia orbicularis (Linnaeus, 1758)
Ctena orbiculata (Montagu, 1808)
Parvilucina costata (Orbigny, 1842)
Erycina sp. aff. E. linella Dall, 1 899
Lasaea adansoni (GmtWn, 1791)
Carditopsis smithi (DaW, 1896)
Charna congregata Conrad, 1833
Chama macerophylla Gmelin, 1791
*Chama sarda Reeve, 1 847
Chama sp.
Pseudochama radians (Lamarck, 1819)
Crassinella lunulata (Conrad, 1 834)
Laevicardium laevigatum (Linnaeus, 1758)
Laevicardium sp.
Papyridea semisulcata (Gray, 1 825)
Trigoniocardia media (Linnaeus, 1758)
Ervilia concentrica (Holmes, 1 860)
Florimetis intastriata (Say, 1 826)
Macoma tenta Say, 1834
42 THE NAUTILUS
April 1973
Vol. 87 (2)
Species
Strigilla mirabilis (Philippi, 1841)
Tellina (Acon'his) guitldii Hanley. 1846
Tellina (Aiignlus) paramera Boss, 1964
Tellina (Laciolina) laevigata Linnaeus. 1758
Tellina (Laciolina) magna Spengler, 1 798
Tellina (Scissulaj similis Sowerby, 1 806
Tellina (Tellina) radiata Linnaeus, 1758
Tellina (Tellinella) listen Roding. 1798
Semelina proficua (Pulteney. 1799)
Tagelus divisus (Spengler, 1794)
Coralliophaga coralliophaga (Ginelin, 1791)
Macrocallista maculata (Linnaeus. 1758)
Chione cancellata (Linnaeus, 1767)
Gouldia cerina (C. B. Adams, 1845)
Pitar fulminata {Menke, 1828)
*Ventricolaria ntgatina (Heilprin. 1887)
*Corbula (varicorbula) sp.
Gastrochaena Mans (Gmelin, 1791)
GASTROPODA
Diodora dysoni (Reeve. 1850)
Diodora sp.
Emarginula pwnila (A. Adams 1851)
Acmaea pustulata (Helbling, 1779)
Lepeta? sp.
Euchelus giittarosea Dall. 1 889
Synaptocochlea picta (Orbigny, 1 842)
Astraea phoebia Roding, 1798
Truncatella caribaeensis Reeve, 1 842
Alvania didyma (Watson, 1886)
Alvania platycephala Dautz. and Fischer. 1896
Cingiila? sp.
*Micwdochiis jloridanus Rehder, 1943
Rissoina biyerea (Montagu. 1803)
Rissoina sp. aff. /?. /jn'e/rfl (Montagu. 1803)
Rissoina cancellata Philippi. 1 847
Rissoina fischeri Desjardin, 1949
Zebina bwwniana (Orbigny. 1842)
Vitrinella species A
Vitrinella species B
Vitrinella species C
*Spirolaxis exquisita (Dall and Simpson. 1901)
Vermicularia knorrii (Deshayes, 1843)
Vermicularia spirata Philippi, 1 836
Siliquaria sqiwmata Blainville, 1827
Caecum delicatulwn Verrill and Bush, 1900
Caecum plicatum Carpenter. 1 858
Caecum sp.
Modulus modulus (Linnaeus. 1758)
Illustration
Boss (1969)
Boss (1966)
Boss (1968)
Warmke and Abbott
Boss (1966)
Warmke and Abbott
Warmke and Abbott
Warmke and Abbott
Warmke and Abbott
Warmke and Abbott
Warmke and Abbott
Warmke and Abbott
Warmke and Abbott
Warmke and Abbott
Warmke and Abbott
Abbott
Warmke and Abbott
Warmke and Abbott
Warmke and Abbott
Warmke and Abbott
Warmke and Abbott
Warmke and Abbott
Warmke and Abbott
Our Fig. 20
Our Fig. 21
Warmke and Abbott
Warmke and Abbott
Warmke and Abbott
Warmke and Abbott
Warmke and Abbott
Warmke and Abbott
Warmke and Abbott
Gould (1969)
Gould (1966)
Our Fig. 22
Warmke and Abbott
Warmke and Abbott
Stations
26
16. 24
24
5. 10. 24. 25
10. 37
24
25
10, 37. 38
16
11
24
3
27
5, 13
11. 14
1. 2. 6. 16,
1. 6. 16
21. 24, 39
39
M. 24, 39
Warmke and Abbott 24
17
5
24
24. 39
24
21, 24. 39
24
24. 39
11
21. 24
11
24
11
24
39
11
11. 24
21, 24. 39
11
24. 39
39
24
24. 27, 39
11
24
II
11, 24.39
11
11, 16, 39
Vol. 87 (2)
Species
Finella dubia (Orbigny, 1 842)
Alaba incerta (Orbigny, 1842)
Cerithium litteratum (Born, 1778)
Cerithium variabile (C. B. Adams, 1845)
Cerithiopsis ara Dall and Bartsch, 1911
Cerithiopsis cynthia? Bartsch, 1911
Cerithiopsis nigiilosum (C. B. Adams, 1 850)
Cerithiopsis vicola Dall and Bartsch, 1911
Cerithiopsis species B
Cerithiopsis species C
Cerithiopsis species D
Triphora mirabilis (C. B. Adams, 1850)
Triphora species B
Triphora species C
Triphora species D
Triphora species E
Bemiudaclis bermudensis (Dall and Bartsch, 1911)
Strombus costatus Gmelin, 1791
Trivia quadripunctata (Gray, 1 827)
Cypraea cinerea Gmelin, 1791
*Cypraea spurca acicularis Gmelin, 1791
Cypraea sp. (Bulla stage)
Natica sp.
*Aspella elizabethae McGinty, 1940
Murex (Favartia) cellulosus Conrad, 1 846
*Pusia variata? (Reeve, 1845)
Aesopus stearnsi Tryon, 1 883
Anachis catenata (Sowerby, 1 844)
Columbella mercatoria (Linnaeus, 1758)
Mitrella lunata (Say, 1 826)
*Nassarina monilifera (Sowerby, 1844)
Colubraria swifti {Tryon, 1881)
Colubraria testacea Morch, 1877
Nassarius albus (Say, 1 826)
Thala foveata (Sowerby, 1 874)
Latirus brevicaudatus (Reeve, 1847)
Hyalina avena (Kiener, 1 834)
Hyalina lactea (Kiener, 1841)
Persicula lavalleeana (Orbigny, 1 842)
Persicula? species A
Persicula? species B
Mitra nodulosa (Gmelin, 1791)
Glyphoturris quadrata rugirima (Dall, 1889)
Mitrolumna biplicata (Dall, 1 889)
Pyrgocythara candidissima (C. B. Adams, 1 845)
Conus bermudensis Clench, 1942
Odostomia didyma Verrill and Bush, 1900
Odostomia nioba Dall and Bartsch, 1911
Turbonilla heilprini Bush, 1 899
43
44 THE NAUTILUS
April 1973
Vol. 87 (2)
Species
Turbonilla pupoides (Orbigny, 1842)
Bulla striata (Bruguiere, 1792)
Atys sp.
Hammoea succinea (Conrad, 1846)
Haminoea sp.
Retitsa candei Orbigny, 1841
WilliamJa krehsii (Morch, 1 877)
Laemodonta cubensis (Pfeiffer, 1854)
Pedipes mirabilis (Mulilfeldt, 1816)
Pleurobranclnts sp.
SCAPHOPODA
Cadulus qiiadridentatus {Dan, 1881)
POLYPLACOPHORA
Radsiella mgidata (Sowerby, 1832)
Clench (1964)
39
Warmke and Abbott 24
Keen
39
NOTES ON TAXA AND THEIR HABITS
Bivalvia
Arcidae
The similarity of living habits of Area imbricata
and Area zebra have been emphasized by Stanley
(1970, p. 122), who also stated that both prefer
shallow subtidal habitats. Our collections indicate,
however, that in Bermuda Area imbricata is more
common in open marine situations than in pro-
tected sounds (see Table 1). Tlie only co-occurrence
of living specimens was in the North Lagoon at
Station 27, where conditions similar to those in the
Oeuliiia Zone of Harrington Sound exist on the
open platform.
Area zebra is perhaps the most conspicuous
mollusk in the shallow inshore waters of Bermuda.
It is especially abundant in Harrington Sound,
where it can be found at depths from about 1.5 m
to 17 m within the Shallow Sandy Zone and
Oculina Zone of Neumann (1965). Secreting a
strong, pedestal-like byssus. Area zebra attaches to
the top or sides of any hard object, most commonly
to shells, rocks, or other debris on the sandy
botton^ Subsequently, other individuals attach to
one another, resulting in clusters or knots which
themselves form a substrate for epifauna. Each
individual Area raises itself on its byssus while
filtering but quickly lowers itself when sensing a
passing shadow. Area zebra does not colonize the
rocky shore, nor does the species attach to corals
far above the bottom. At Station 29, Area zebra
clusters have formed on the old concrete pilings of
the abandoned causeway, but these clusters are
subtidal and close to the bottom.
In contrast to its inshore abundance, the paucity
or absence of Area zebra from the outer shallow
waters of Bermuda is striking. It is usually un-
common in smaU bays with free access to the open
sea and is not common in the shallow waters within
the breaker zone of the south shore. The only
outside area at which Area zebra was found in
abundance is Station 27 in an area of abundant
Oeidina on a silty mud bottom, very similar to the
Oeiilina Zone of Harrington Sound.
In a study of Barbatia dommgensis on the Ber-
muda Platform, Bretsky (1967) found that this
species is most abundant in turbulent environments
and least abundant in protected bays and sounds.
Its most common site of byssal attachment is
beneath corals, less commonly beneath rocks. The
strong representation of B. domingensis in our col-
lections from the open platform confirms Bretsky's
observations, and in view of these habitat pre-
ferences only the occurrence of the species in
Walsingham Pond (Station 1 1 ) is unexpected. Tlie
pond specimens are all immature and possibly in-
dicate that larvae forced into the pond through
crevices are unable to reach maturity.
Vol. 87 (2)
THE NAUTILUS
45
Pteriidae, Isognomonidae, and Malleidac
Among the Pteriacean bivalves (Pteria, Pinctada,
Isognomon. and Malleus), only Pteria colymbits lives
off the bottom, attached by a strong, clasping
byssus to the tlexible, waving arms of gorgonaceans.
At all stations where living individuals were ob-
served Pinctada radiata attaches to shells or rocks
on the sandy bottom, generally with the plane of
commissure nearly horizontal or somewhat inclined
to the substrate. Wliereas Pteria was obsei-ved only
in open-marine areas, Pinctada is common in bays
and sounds.
Isognomon radiatus was observed living only at
two open-marine stations (Stations 1 5 and 25),
where individuals were byssally attached between
large rocks. According to Stanley (1970, p. 136),
nestling beneath or between rocks with weak byssal
attachment is the usual living habit of the species.
Orientation relative to the attachment surface is
variable, although generally the distal portions of
the shell are erect and project into the water rather
than lie flat against the attachment surface.
Malleus candeanus is a rare species throughout
the West Indies and Florida but occurs in abun-
dance at Bermuda. The taxonomy, distribution and
living habits of the species have been described by
Boss and Moore (1967), and Yonge (1968) has
given a detailed account of the functional morph-
ology of the very similar Pacific species, M. regula.
Although Boss and Moore did not observe living
specimens, they concluded that Malleus candeanus
lives attached to hard substrates, particularly in the
crevices of coral or coralline rock. Our underwater
observations confirm this habit. At all localities
observed, specimens were found tightly byssally
attached to the sides and undersurfaces of large
rocks, particularly where there are large crevices or
small caves between rocks, or beneath overhanging
ledges of coral. At Station 26, Malleus was par-
ticularly common on the high; steep side of a large
patch reef. All localities were in open marine areas
generally deeper than 6 meters and with con-
siderable current or surge flowing between the
rocks.
The elongate, distal portion of the shell of
Malleus projects from the attachment surface. This
portion of the shell is thin and composed entirely
of fragile prismatic calcite. Although it is frequently
fractured during attacks by nibbling predators,
Yonge (1968, p. 387) has pointed out that
prismatic calcite can be rapidly regenerated by the
highly letractible mantle, which remains uninjured.
Pectinidae
Both Comptopallium antillarum (Recluz, 1853)
and Pecten cbazaliei Dautzenberg, 1900, have not
been previously reported from Bermuda. Shells and
fragments of both were recovered from sediment
samples taken on dives deeper than 30 m. (Stations
24 and 39). Comptopallium antillarum is a common
species in the Caribbean and tropical Western At-
lantic, where hving specimens have been found at
depths ranging from 3 m. to 70 m. and where, in
shallow waters, they are commonly attached among
Halimeda algae. The previously known geographic
range of the species extends from off Colon, Pan-
ama and Barbados northward to Great Abaco, Ba-
hamas. Pecten chazaliei is known to live at depths
ranging from 18 to 230 m. in an area ranging from
off Brazil, through the Caribbean and eastern Gulf
of Mexico, and up the North American coast as far
north as Cape Fear, North Carolina (depth, 73 m.).
Aequipecten acanthodes (Dall, 1925) was orig-
inally described as being "less inflated, wider, and
with less prominent spines" than Aequipecten
muscosus (Wood, 1828) [= Pecten exasperatus
Sowerby, 1843]. Althougli the type locality of
Dall's species was never given, the syntypes (USNM
333367) are from "Santa Lucia, northwest Cuba,
depth 2 to 4 fathoms". Tlie Bermuda specimens
listed in Table 1 bear a closer resemblance to the
Cuban forms than to A muscosus from the Florida
coast. The larger of the two syntypes of A.
acanthodes is illustrated in Figures 3 and 4.
The occurrence of Argopecten gibbus within a
neady land-locked sound is unusual. Along the
North American coast, the species is found only in
open marine waters generally within a depth range
of 9 to 365 meters (Waller, 1969, p. 37), whereas
bays and sounds harbor populations of Argopecten
irradians and Argopecten nucleus.
As observed by Neuman (1965, pp. 999, 987),
Harrington Sound "does not exhibit extremes in
either dilution or evaporation", and regardless of
the almost complete isolation of the sound, "tidal
exchange througli the narrow inlet is sufficient to
maintain near-normal oceanic temperature and sa-
linity." In addition there is some exchange of water
througli caves and the porous limestone surrounding
the sound. As emphasized by De Laubenfels (1950.
46 THE NAUTILUS
AprU 1973
Vol. 87 (2)
p. 1 59), the small amount of land area surrounding
Harrington Sound in comparison to the large size of
the sound itself, coupled with the porous bedrock,
permits httle land runoff and allows for greater
constancy of oceanic conditions. In contrast, sounds
located along the North American coast commonly
exhibit extremes of both salinity and temperature,
favoring species adapted to variation of these con-
ditions.
In Harrington Sound, Argopecten gibbus rests on
the bottom with its right valve on or sliglitly within
the sediment. Tlie majority of the largest individuals
lie free, without byssal attachment, although many
mature individuals attach a weak byssus to dead
sheOs and coral fragments. The species is sluggish
and rarely begins to swim when approached by a
diver or when handled. Wlien swimming begins, it is
an irregular motion with rapid adductions of the
valves and short flights of no more than a meter.
Like all free-living scallops, A. gibbus has an over-
turning reaction when placed with its left valve
downward. Generally the animal rests motionless for
a time varying from a half minute to three minutes.
Then the valves gape broadly, the vela become rigid,
and with one or two claps the scallop rotates on
either its liinge axis (10 out of 18 trials) or on an
axis perpendicular to the liinge and parallel to the
plane of commissure. Generally the smaller in-
dividuals (those of about 25 or 30 mm in height in
our test sample) begin the righting reaction sooner
than larger individuals (those 50 to 60 mm in
height).
Two valves and numerous fragments of
Argopecten gibbus were found in the Sub-
thermochne Zone near Shark Hole, Harrington
Sound (Station 6, Fig. 2). Tlie larger of the two
nearly complete valves is a typical representative of
the species, with a thick shell and moderate con-
vexity. It is indistinguishable from individuals living
in the Shallow Sandy Zone, and because its auricles
are chipped as thougli bitten, the shell may have
been dropped or dragged into this zone by a
predator.
Tlie smaller of the two valves is strikingly dif-
ferent from any of the specimens found elsewhere
around the Bermuda Islands. Its shell is exceedingly
thin with very low curvature and radial plicae of
low amplitude. Its disk flanks are very low and, on
the posterior side, there is no sharp demarcation
between the disk flank and posterior auricle, which
lacks radial costae. Dark, brownish red pigment
produces mottling on the valve exterior and a more
uniform dark hue on the interior of the valve in
areas outside of the pallial Une. Sculptural details,
such as the fine, concentric lamellae on the exterior
and ridged cardinal crura on the interior, and the
aragonitic myostraca are well-enough preserved to
suggest that the thinness of the shell is not entirely
due to solution. Most of the fragments recovered
exhibit the same thinness and pigmentation as the
smaller of the two whole valves, and according to
G. R. Clark, II (personal communication) such
specimens are common from drill cores of sediments
within the Subthermocline Zone. The thin shells are
within the range of variation exliibited by
Argopecten gibbus and most closely resemble fossil
specimens from early Pleistocene deposits in
southern Florida (see Waller, 1969, pp. 65, 66).
The thin specimens may be the offspring of
shallow-water populations which have entered the
Subthermocline Zone as larvae during maximum
overturn of the water. Subsequent grov^^h may then
have been modified by the unusual conditions pre-
sent in the subthermocline environment. Al-
ternatively, the subthermocline Argopecten may in
fact be fossils introduced into Harrington Sound
some thousands of years ago at a time when
populations throughout the Sound were of this
morphology. These hypotheses can be tested, the
former through culturing of Argopecten gibbus
within the Subthermocline Zone, the latter through
radiocarbon dating of shells and observation of
Bermuda fossils both from within and outside of
Harrington Sound.
Argopecten noronhensis (E. A. Smith, 1885) was
originally described from the coast of Brazil, where
it was dredged by the H. M. S. Challenger from a
depth of 46 m off Fernando Noronlia. Since
Smith's original description, there have apparently
been no further reports on the occurrence of the
species outside of Brazilian waters. However, col-
lections in the U. S. National Museum contain
numerous specimens from Barbados (depths, 46 to
1 83 m ), Antigua (220 m ), the Virgin Islands and
Puerto Rico (73 to 256 m ), and Cat Cay, Baliamas
(550 m ). All of these specimens were found dead
with only the shells remaining on bottoms of coarse
sand or coral rubble. Living specimens have been
taken by the R/V Oregon off St. Lucia (66 to 75
m), south of Saba Banks (91 to 110 m), and off
Vol. 87 (2)
THE NAUTILUS
47
Tortola. Virgin Islands (49 m). Argopecten
noronlicnsis is not known to occur in the western
Caribbean or in the Gulf of Mexico. In Bermuda
fragments of A. noronhemis were recovered from
sediment samples taken on our deepest dive, at a
depth of 51 m (Station 39). The species is il-
lustrated in Figures 5-8.
Althougli not well-known because of its small
size (generally less than 1 5 mm), Chlamys benedicti
VerrUl and Bush, 1897, is the most widespread and
numerous Chlamys in the Western Atlantic region.
According to data with specimens examined thus
far, the species ranges from the coast of South
America off Surinam northward to a point south-
east of George's Bank and is also widespread in the
northern and eastern Gulf of Mexico. Shells of C.
benedicti have been found from beach level down
to 2,480 in, but living specimens are known only
from about 2 to 806 m. Out of 86 records of
living specimens, 75% are within the 46 to 90 m
range. At many localities the species is associated
with coral debris and sponges, and preserved spec-
imens indicate that, like all Chlamys, C. benedicti is
byssally attached. At Bermuda, fragments and one
small valve of Chlamys benedicti were recovered
from sediment samples taken at Stations 24 (34 m)
and 39 (51 m).
Despite an intensive search for living Chlamys
imbricata, only one live individual only 17 mm in
height was found (Station 18). It was byssally
attached with its riglit valve upward against the
undersurface of a hemispherical head of dead coral
at a depth of 7 m. The scallop voluntarily released
its byssal attachment when the coral was overturned
and, by clapping its valves, slid along the coral
surface.
In a bucket on the boat, the specimen quickly
attached itself with a new byssus to a clump of
coral. However, after a few hours in a laboratory
aquarium, the specimen detached itself from the
same clump of coral, moved up and out of a small
glass bowl in the bottom of the aquarium, and
reattached to the lower umbo of an Argopecten
gibbus on the bottom of the same aquarium. On the
basis of only a few trials with this one immature
specimen, C. imbricata seems to have only a weak
overturning reaction, generally not beginning to
right itself for several minutes after being over-
turned and then rigliting with a single clap and
rotation about the hinge line. Tlie specimen was
observed to swim with its commissure inclined and
left valve uppermost, taking off from the bottom at
a steep angle with very rapid valve adductions.
Bermuda is the northernmost occurrence of this
species, which on the North American coast occurs
no further north than Miaini. In the south, C
imbricata is known only from the Caribbean,where
it has been found as far south as Payardi Island,
Panama.
Chlamys multisquamata (Dunker, 1864) is the
rarest of the Western Atlantic Chlamys. Originally
described from Havana Bay, Cuba, the species was
subsequently redescribed as Pecten effluens by DaU
(1886) on the basis of two immature valves dredged
from 230 m. off Havana. Since this time, additional
specimens have been found at Barbados (USNM, 46
to 110 ni); Dominica (Nat. Marine Fish. Service,
Lab. at Pascagoula, Miss., 62 to 110 m); Puerto
Rico (USNM. 73 to 91 m); Cuba (USNM, 550 m);
Bahamas (USNM, 90 to 550 m): off Palm Beach,
Florida (F. M. Bayer Collection, 24 to 30 m); and
Bonaine, Dutch West Indies (S. D. Abbott ,17 m.
in crevice, on coral heads). At Bermuda, un-
mistakable fragments of the species were recovered
from sediment samples taken on the deepest dive
(Station 29, 51 m). According to data accom-
panying the Palm Beach specimen, the species was
living among rocks and between the shells of
Spondylus. Morphologically, Chlamys multisquamata
resembles several Indo-Pacific species that live in
coral crevices (see Waller, 1972). The Western At-
lantic species is illustrated in Figures 9-11.
Living Pecten ziczac was found only in the
Shallow Sandy Zone of Harrington Sound, althougli
shells of the species are common in other bays such
as Ely's Harbor and inner Port Royal Bay. The
living habits of F. ziczac are as described by Stanley
(1970, p. 140). The scallops live with their riglit
valve buried in the sediment to the level of the
commissure; a thin layer of sediment covers the
upper flat valve; and the only portion visible from
above is the ring of extended tentacles.
Pecten ziczac is more adept at swimming and
does so more readily than Argopecten gibbus. Al-
thougli the latter would not swim when sensing the
approach of a diver, Pecten would occasionally do
so. Other specimens would begin swimming when
lifted from the sediment. The animal takes off at a
steep angle and then levels out in flights of about 5
seconds duration or longer. Adduction frequency is
48 THE NAUTILUS
April 1973
Vol. 87 (2)
fairly rapid, generally about two claps per second,
and flight distances average slightly more than 1 in.
Like Argopecten, P. ziczac has a distinct rigliting
reaction but because of the flatness of its left valve,
righting is accomplished with great difficulty.
Studies of three specimens in an aquarium indicated
that rigliting begins one or two minutes after over-
turning. Rotation is about an axis parallel to the
hinge line, generally requiring three or four claps of
the valves during rotation.
Tlie ability of Pecten ziczac and many other
scallops to excavate a shaOow depression in the
sediment has been described by Waller (1969, p. 17)
and Stanley (1970, P- 140).
Anomiidae
Collections of Anomia simplex and Pododesmus
nulls from Harrington Sound suggest differences in
habitat between the two species. Anomia is most
abundant in the Shallow Sandy Zone where it
attaches to shells and other debris on the sandy
substrate. Pododesmus, on the otlier hand, is most
abundant in the Oculina Zone, where it attaches to
Ocullna and avoids contact with the bottom. In
areas on the North American coast, Stanley (1970,
p. 144) has observed that A. simplex generally
occurs attached to pebbles and debris on a firm
substrate where there is a moderate current flow.
Limidae
Lima lima attaches with a strong byssus beneath
rocks in open marine areas and avoids bays and
sounds.
Gryphaeidae and Ostreidae
The listing of Neopycnodonte cochlear is based
on a single, eroded riglit valve from the deepest
station (Station 39, 51 n^; Figs. 12, 13). The
specimen is roughly circular in form, measures 13
mm in diameter, and clearly displays the vesicular
shell structure and outer prismatic layer (Fig. 12)
that Stenzel (1971, p. 1105) considers to be char-
acteristic of the genus. According to Stenzel there is
only one living species in the genus, which has a
worldwide distribution in tropical and subtropical
oceanic waters ranging in depth from 27 to 1,500
m.
The familiar Ostrea frons of the West Indian
region has been relegated to the genus Lopha and to
the synonymy of Ostrea folium Linnaeus by Stenzel
(1971, pp. 1024, 1158). Tlie elongate, clasping form
associated with Ostrea frons is one of two
ecomorphic end members within the species. Al-
thougli commonly attributed to growth while at-
tached to mangrove roots (Warmke and Abbott,
1954, p. 173), this ecomorph is generally the result
of attachment to gorgonacean corals in subtidal
habitats. In Harrington Sound (Station 13), the
species also cements itself to shells lying on the
bottom, in which case it secretes clasps only where
the oyster shell overlaps the edge of the shell to
which it is attached. As with all oysters, the shape
of the attachment surface profoundly affects the
shape of the oyster, and those attached to shells are
less crenulated and less elongate than those found
on gorgonaceans.
Condylocardiidae
Viviparity is conmion in the superfamily
Carditacea (Dall, 1902, p. 696), and Cardltopsls
smlthl is no exception. One of the dead but tiglitly
closed specimens from Walsingham Pond yielded
three articulated prodissoconchs, one of which is
illustrated in Figure 19. Large, sculptured,
saucer-shaped prodissoconchs, of this type are gen-
erally associated with viviparity in several taxonomic
groups, as in the genera Condylocardla (Bernard,
1 897, p. 1 70) and Philobrya (Bernard, 1 896, p. 9).
Chamidae
Certain species of Bermudian chamids are sepa-
rated in open marine and partially enclosed en-
vironments. Pseudochama radians lives in abundance
in the Shallow Sandy Zone of Harrington Sound
and also occurs in the Ocullna bed at Station 27 in
association with well-developed Chama
maccrophylla. Another common chamid in Har-
rington Sound is Chama congregata, which is most
abundant in the Ocullna Zone. Chama sarda was
found only well off-shore, where it was abundant at
the three stations deeper than 30 m.
The shells of Chama maccrophylla found on the
bottom of Walsingliam Pond have extremely heavy
and deep left valves and resemble the Chama ber-
mudensls described by Heilprin (1889, p. 141) from
Harrington Sound. Because these have crenulated
inner margins and lack an exterior sulcus, they
cannot be considered a subspecies of Chama slnuosa
Broderip as in Bayer (1943, p. 122).
Vol. 87 (2)
THE NAUTILUS
49
In Table 1 the Chainidae have been placed near
the Carditidae rather than near the Lucinidae fol-
lowing the convincing evidence of relationships pre-
sented by Kennedy, Morris, and Taylor (1970).
Crassatellidae
FoUovk'iiig the study of Harry (1966), both
Crassinella parva (C. B. Adams, 1845) and C. guad-
ahipensis (d'Orbigny, 1846) are considered to be
junior synonyms of C. Iwndata (Conrad, 1 834).
Veneridae
The Western Atlantic species of Gouldia are
higlily variable and inadequately described. It is
curious that G. ceriiia (C. B. Adams, 1845), G.
bermudemis (E. A. Smith, 1885), G. imularis (Dall
and Simpson, 1901), and G. foresti Fischer-Piette
and Testud, 1967, were all described without ade-
quate published comparison to other known species.
Tliere is no adequate basis for separating G. cerina,
G. benmidensis, and G. foresti without an extensive
quantitative study of geographical variation; Gouldia
insularis appears somewhat more distinct, character-
ized by its rounded form and high degree of
inflation.
None of the numerous Gouldia from the Sub-
thermocline Zone of Harrington Sound were alive
when collected. All show some deterioration of
their aragonitic shells and lack preserved ligaments,
although some have traces of pigment remaining
(see Notes on Habitats).
Gastropoda
Rissoidae
Alvania platycephala was first described and il-
lustrated by Dautzenberg and Fischer (1896, p. 63,
plate 19, figs. 12, 13) on the basis of specimens
taken from a depth of 1,385 meters in the Azores.
The first Bermudian record is that of Verrill and
Bush (1900, p. 539), who identified the species
from "shell sand" taken from waters less than 15
m deep. Tlieir identification was apparently based
on Dautzenberg and Fischer's illustration, and the
specimens themselves were evidently not compared.
The species was subsequently reported by Piele
(1926, p. 77) from an unknown site and by Gould
(1968, p. 4) from Walsingliam Pond. These spec-
imens, shown here in Figure 21, bear an even closer
resemblance to the illustration of Dautzenberg and
Fischer than the rather poor line drawing of Verrill
and Bush would indicate. Tlie species was found by.
us only in Walsingliam Pond (Station 1 1 ), where it
is abundant.
A second species of Alvania, also reported by
Piele (1926, p. 77), is A. pagodula (Bucquoy,
Dautzenberg, and Dollfus, 1884), originally des-
cribed from the Mediterranean and Adriatic. Piele's
specimens were more likely Alvania didyma (Wat-
son, 1886), which in the present study was taken at
depths exceeding 30 m. (Stations 21 and 24, Fig.
20).
Turritellidae
Gould (1968, p. 4) recognized Vermicularia
spirata Philippi, 1836, as the most common moUusk
in Walsingham Pond and later (Gould, 1969) studied
the ecology and functional significance of uncoiling
in the species. In Bermudian waters V. spirata
cements itself to a variety of hard substrates but is
particularly common in association with the branch-
ing coral, Oculina. In Walsingliam Pond there is no
development of Oculina, and, as noted by Gould,
fewer than 1 percent of the largest Vermicularia
present show uncoiling. Instead, individuals live in
burrows with their apertures projecting sliglitly
above the mud.
Specimens of Vermicularia from stations on the
open Bermuda Platform have all been identified
here with V. knorri (Deshayes, 1843) only because
their early whorls are white, rather than tan or
brown as in V. spirata. This is a character that some
workers believe is genetically significant. However,
there are no differences in whorl profile or sculp-
ture other than those imposed by differing rates of
uncoiling, a process shown by Gould to be en-
vironmentally controlled, and it is possible that
further study will place V. knorri in the synonymy
of K spirata.
Caecidae
Caecum plicatum Carpenter, 1858, is a senior
synonym of Caecum termes Heilprin, 1 889, re-
ported by Piele (1926, p. 78) to be the most
common Caecum in Bermuda and by Gould (1968,
p. 4) to be the most common in Walsingham Pond.
Buccinidae
All living Colubraria swifti observed in Bermuda
(Table 1) were beneath rocks in open marine areas,
commonly associated with Barbatia domingensis.
50 THE NAUTILUS
ApiU 1973
Vol. 87 (2)
TABLE 2. Collecting stations grouped according to general environment or ecological zone. Ecological zones in
Harrington Sound follow Neunwnn ( 1 965).
Description
Harrington Sound. Shallow Sandy Zone
Harrington Sound and North Lagoon,
Oculina Zone
Harrington Sound, Subthermocline Zone
Walsingham Pond, muddy bottom
Bays and sounds other than Harrington
Sound
Open platform, sand pockets and
patch reefs, 5 to 18 m
Open platform, sand pockets, 34 to 51 m
Stations
3. 5, 9, 10, 13
2, 7, 27
1, 6
11
14, 17, 20, 29, 30, 31
33, 34b, 35, 36, 37, 38
12, 15, 16, 18, 23,25,
26, 28
21, 24, 39
Polyplacophora
Isclmochitonidae
Radsiella nigulata (Sowerby, 1832) is a senior
synonym of Ischnochiton boogii Haddon, 1886
(Keen, 1971, p. 869), which in turn is a senior
synonym of Ischnochiton bermudensis Dall and
Bartsch, 1911.
ACKNOWLEDGMENTS
Tlie field portion of this study was carried out at
the Bermuda Biological Station for Research, St.
George's West. I am grateful to the staff of the
Station, particularly Dr. Wolfgang Starrer, Director,
and Mr. Brunell Spurling, skipper of the Micmac.
Dr. Porter M. Kier, Chairman of the Department of
Paleobiology, Smithsonian Institution, kindly per-
mitted his assistant, Mr. Tliomas F. Phelan, to
accompany me as a companion diver. Both Mr.
Phelan and Miss Ellen P. Broudy, my research
assistant, ably assisted in the field study. Additional
help in Bermuda was received from Dr. J. D.
Herkes, Dr. David Pawson, and Mr. Arthur Guest.
Assistance in identification was received from Mr.
Russell Jensen and Dr. R. T. Abbott, Delaware
Natural History Museum; Dr. D. R. Moore, Uni-
versity of Miami; Dr. K. J. Boss, Harvard Uni-
versity; Dr. Ruth Todd, U. S. Geological Survey,
and Drs. J. P. E. Morrison, H. A. Rehder, J.
Rosewater, and G. A. Cooper, Smithsonian In-
stitution, and Mr. W. G. Lyons, Florida Department
of Natural Resources, St. Petersburg. I am grateful
to Dr. F. M. Bayer, University of Miami, for the
loan of a specimen of Chlamys nndtisquamata, and
to Mr. H. R. Bullis, Jr., National Marine Fisheries
Service, for permission to study his collections in
Pascagoula, Mississippi. Dr. D. R. Moore, Dr. R. T.
Abbott, and Mr. R. Jensen read the manuscript and
gave many helpful suggestions. Mr. Larry Isham,
artist for the Department of Paleobiology, drafted
the maps.
Funding for travel and field study was through
the Department of Paleobiology, Smithsonian Insti-
tution, and funding for all other aspects of the
work was througli grants to the author from the
Smithsonian Research Foundation.
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Boss, Kenneth J. 1968. The subfamily Tellininae in
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143-163.
Vol. 87 (2)
THE NAUTILUS
51
Boss, Kenneth J. 1969. The subfamily Tellininae in
the Western Atlantic. The genus Strigilla. Ibid. 4
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Bretsky, Sara S. 1967. Environmental factors in-
fluencing the distribution of Barbatia do-
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tables.
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Western Atlantic. Johnsonia 1 (6): 40 p., 15 pis.
Clench, William J. 1964. The genera Pedipes and
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4, no. 42, p. 117-127, pis. 76-79.
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Dall, William Healey. 1 889. A preliminary catalogue
of the shell-bearing marine ■ mollusks and
brachiopods of the southeastern coast of the
United States, with illustrations of many of the
species. Bull. U. S. Natl. Mus., no. 37, 232 p., 95
pis.
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Carditacea and of the American species: Proc.
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clature of some of our east American species of
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Dall, William Healey and Paul Bartsch. 1911. New
species of shells from Bermuda. Proc. U. S. Natl.
Mus. 40 (1820): 277-288, pi. 35.
Dall, William Healey and Charles Torrey Simpson.
1901. The Mollusca of Puerto Rico. U. S. Fish
Commission Bull. 1: 351-524, pis. 53-58.
Dautzenberg, P., and H. Fischer, 1896. Compagnes
scientifiques de S. A. le Prince Albert 1 de
Monaco. Dragages effectives par VHirondelle et
par \a Princess- Alice , 1885-1895. Mem. de la Soc.
Zool. de France 9: 1-104, pis. 15-22.
Davis, J. D., 1967. Ervilia concentrica and Meso-
desma concentrica. Clarification of synonymy.
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De Laubenfels, M. W. 1950. An ecological dis-
cussion of the sponges of Bermuda. Trans. Zool.
Soc. London 27: 155-201, 4 figs.
Fischer-Piette, E. and A.-M. Testud. 1967.
MoUusques Lamellibranches: Veneridae. Resultats
scientifiques de campagnes de la "Calypso", Fas-
cicule 8, no. 13, p. 205-220, 4 pis.
Gould, Stephen Jay. 1966. Notes on shell mor-
phology and classification of the Siliquariidae
(Gastropoda). The protoconch and slit of
Siliquaria squamata Blainville: Amer. Mus.
Novitates, no. 2263, 13 p., 7 figs., 2 tables.
Gould, Stephen Jay. 1968. The moUuscan fauna of
an unusual Bermudianpond: A natural experiment
in form and composition: Breviora, no. 308, 13
p., 2 figs., 2 tables.
Gould, Stephen Jay. 1969. Ecology and functional
significance of uncoiling in Vermicularia spirata:
An essay on gastropod form. Bull. Marine Sci. 19
(2): 432-445, 3 figs., 1 table.
Harry, Harold W. 1966. Studies on bivalve molluscs
of the genus Crassinella in the Northwestern Gulf
of Mexico: Anatomy, Ecology and Systematics.
Publ. Inst. Marine Sci., Texas 11: 65-89, 17 figs.
Heilprin, Angelo. 1889. On some new species of
Mollusca from the Bermuda Islands. Proc. Acad.
Nat. Sci. Philadelphia for 1889, p. 141, 142, pi.
8.
Jackson, Jeremy B. C. 1970. The ecology and
paleoecology of near shore tropical Lucinacea
(Bivalvia). Geol. Soc. America Abstracts, 2 (7):
586-587.
Keen, Angeline Myra. 1971. Sea shells of tropical
west America, 2nd Edition. Stanford, California,
Stanford Univ. Press., 1,064 p., 22 pis.
Kennedy, William James, N. J. Morris and John D,
Taylor. 1970. The shell structure, mineralogy and
relationships of the Chamacea (Bivalvia).
Palaeontology 13, part 3, p. 379-413, 6 figs.,
pis. 70 - 77.
McGinty, Thomas L. 1940. New land and marine
Tertiary shells from southern Florida. The Nauti-
lus 53 (3): 81-84, pi. 10.
52 THE NAUTILUS
April 1973
Vol. 87 (2)
Moore, Raymond C. (Editor). 1969. Treatise on
invertebrate paleontology, Part N, vols. 1 and 2,
moUusca 6, bivalvia: Univ. of Kansas and Geol.
Soc. Amer., 951 p., illustr.
Neumann, A. Conrad. 1965. Processes of recent
carbonate sedimentation in Harrington Sound,
Bermuda. Bull. Marine Sci. 15: 987-1035, 8 figs.,
1 table.
Piele, A. J. 1926. The MoUusca of Bermuda. Proc.
Malac. Soc. London 17 (2 and 3): 71-98.
Smith, Edgar A. 1885. Report on the
LameDibranchiata. Report on the scientific re-
sults of tlie voyage of the H. M. S. Challenger
during the years 1873-76, Zoology 13 (35); 341
p., 25 pis.
Stanley, Steven M. 1970. Relation of shell form to
life habits in the Bivalvia (MoUusca). Geol. Soc.
Amer. Mem. 125. xiii -i- 296 p., 48 figs., 40 pis.
Stenzel, H. B. 1971. Oysters: in Raymond C. Moore
(Editor), Treatise on invertebrate paleontology,
Part N, vol. 3, MoUusca 6, Bivalvia, p. 953-1224,
1 53 figs.
Taylor, Dwiglit W. and Norman F. Sohl. 1962. An
outline of gastropod classification. Malacologia 1
(1): 7-32, 2 figs.
Verrill, A. E. and Katherine J. Bush. 1900. Addi-
tions to the marine MoUusca of the Bermudas.
Trans. Connecticut Acad. Sci. 10; 513-544, pis.
63-65.
Waller, Tliomas Richard. 1969. Tlie evolution of the
Argopecten gibbus stock (MoUusca: Bivalvia),
with emphasis on the Tertiary and Quaternary
species of eastern North America. Paleont. Soc.
Mem. 3 (Jour. Paleont. 43 (5), suppl.), 125 p.,
13 figs., 7 pis., 43 tables.
WaUer, Thomas Richard. 1972. The Pectinidae (Mol-
lusca: Bivalvia) of Eniwetok Atoll, Marshall Is-
lands. Veliger 14(3); 221-264, 22 figs., 8 pis., 13
tables.
Walton, Anthony W. 1969. Walsingham Pond: A brief
study of its sediments and water chemistry. Re-
ports of Research, 1968 Seminar on organism-sedi-
ment interrelationships, Bermuda Biol. Sta. for Re-
search, Special Publ. no. 2: 41-50, 3 figs.
Warmke, Germaine L. and R. Tucker Abbott. 1961.
Caribbean seashells. Narberth, Pennsylvania, Liv-
ingston Publ. Co., 346 p., 44 pis., 34 text-figs.
Warmke, Germaine L. and Luis R. Almodovar.
1963. Some associations of marine moUusks and
algae in Puerto Rico: Malacologia 1 (2): 163-177,
1 fig., 10 tables.
Yonge, C. M. 1968. Form and habit in species of
Malleus (including the "hammer oysters") with
comparative observations on Isognomon isogno-
mon Biol. BuH. 135 (2): 378-405, 13 figs.. 1
table.
BOOK REVIEW
SHELLS AND SHELL COLLECTING. By S. Peter
Dance. 128 pp., 110 photos, 30 in color. Index.
HamlynPubl, London, N. Y., Toronto. $4.95.
This is one of the more attractive of the recent
rash of popular books on conchology. It is
well-written, accurate and Ulustrated by excellent
photographs. It is an interesting introduction to the
major groups of moHusks. shell shapes and colors,
the history of shell collecting, rare shells, and man's
use of moUusks as food, money and objects of art.
Peter Dance has included several accounts new to
the popular literature, and has illustrated a number
of land and marine shells that previously had not
been published in books for the layman. Missing
from tills otherwise excellent book on sheU col-
lecting are instructions on how to coUect shells and
how to clean and preserve them. The art director
has reversed the negative on the first double-page
spread, thus creating sinistral Nucella dogwinkles.
For its low price, this book is a worthwhile pur-
chase.
R. Tucker Abbott
Delaware Museum of Natural History
I
Vol. 87 (2)
THE NAUTILUS
53
EVIDENCE FOR SPAWNING BY GONATUS SP. (CEPHALOPODA: TEUTHOIDEA)
IN THE HIGH ARCTIC OCEAN
Richard Edward Young
Department of Oceanography
University of Hawaii, Honolulu, Hawaii 96822
ABSTRACT
A specimen of the squid, Gonatus sp., was captured through an ice hole at 79° 58'
N. lat., 170° 23' E. long, (about 500 miles north of Wrangel Island, Siberia) whose
condition suggests it had spawned just before its capture on March 30, 1962. The
emaciated condition is described in specimens of other Califomian female Gonatus that
presumably had spawned just before capture, and a brief review is given of the records
of the degeneration and fatal effects from spawning by females in other genera of
squid and octopods.
The cephalopod fauna of the high Arctic Ocean
is poorly known; pelagic cephalopods have been
reported only on a few occasions. Berry (1925)
described from seal stomachs a small collection of
cephalopod beaks, one of which taken at
70°13'N, 140°50'W, probably belongs to a squid.
MacGinity (1955) recorded a juvenile and adult
Cirroteuthis sp. (finned octopods) that were
dip-netted near shore and 3 specimens of Gonatus
"fabricii" (72, 63, 59 mm mantle length) that had
washed ashore at Pt. Barrow, Alaska. Voss (1967),
in a footnote, mentioned the capture of Cir-
rothauma (finned octopod) in the high Arctic. The
locality of this capture is 86°N, 173°E (Roper and
Brundage, 1972). Nesis (1971a) found 2 specimens
of Gonatus "fabricii" (175 and 87 mm Mantle
Length) in an ice hole at §7°24.2'N, 132°01.5'E
and one specimen of G. "fabricii" (130 mm ML) in
an ice hole at 80°13.3'N and 143°01'E. He further
reports that Gonatus is abundant at the border of
the Arctic Basin and the Greenland Sea, particularly
young specimens ranging from 30-71 mm ML. The
only pelagic cephalopods known from the high
Arctic Ocean, therefore, are members of the squid
family Gonatidae and two species of finned oc-
topods.
The squid reported here was captured from ice
island Arlis II (Arctic Research Laboratory Ice
Station No. 2) in the high Arctic Ocean on March
30, 1962. The squid, alive at the time of capture,
was found floating head downward in a hole cut
through the ice for hydrographic and plankton
studies.
DESCRIPTION
Since the identity of this specimen is of con-
siderable importance but impossible to determine to
species at present due to the condition of the
animal, a brief description is presented (Fig. 1 & 2).
The pen is 210 mm in length. The manfle and fins
are gelatinous and flaccid. A well-developed conical
"tail" is present posterior to the conus of the pen.
In preservation in 70% ethanol the fins measure 102
mm in total length and 145 mm in total width. The
fins extend posteriorly along the "tail."
The funnel is large and reaches to the level of
the midpoint of the eyes. The funnel locking-carti-
lages bear simple straight grooves (Fig. 2, F). The
dorsal pad of the funnel organ has an inverted
V-shape, the anterior half of each limb has low
ridges along the lateral margin (Fig. 2, G). A small
anterior papilla is present. The ventral pads are
smaU and nearly teardrop-shaped with the blunt end
anterior. A large funnel valve is present.
The head is short and bears large eyes with a
distinct sinus on the anterior margin of each eyelid.
A nuchal crest with three indistinct pairs of nuchal
folds occurs on the head. "Olfactory" lobes lie on
the second pair from the funnel on each side. The
nuchal cartilage, which is long and sliglitly rounded
at either end, bears a median ridge containing a
central groove.
The arms are gelatinous and relatively short (Arm
I = 73 mm. III - 97 mm, IV = 98 mm). A weakly
developed aboral keel is present on each arm III and
large lateral keels are present on each arm IV. All
arms bear very broad, thick, gelatinous trabeculae
that are joined by thick, poorly defined protective
membranes which converge and conceal the hooks
in the distal portion of the arms. The arm tips are
not attenuate. The armature of arms I-III consists of
two alternating rows of small hooks (Arm I = 42
54 THE NAUTILUS
April 1973
Vol. 87 (2)
hooks, II = 41 hooks, III = 44 hooks). The marginal
and terminal rows of suckers are absent and only
small grooves indicate their former presence. Suckers
are absent from arms IV (Fig. 2, B). The tenta -
cles have been lost except for rounded stubs.
The specimen is a female. Oviducal and
nidamental glands are slightly swollen (lengths: 28
mm and 14 mm respectively). The ovary is rather
small but still contains many elongate immature ova
and a few scattered, larger sperical ova of various
sizes, the largest of which measures about 1.5 mm
in diameter.
The radula (Fig. 2, C) contains only five teeth in
a transverse series. The rachidian tooth has a short
central cusp and two small lateral cusps. The first
lateral teeth are absent. The second laterals have
broad bases each with a rather blunt medial cusp.
Marginal plates are absent. The beaks (Fig. 2, D) are
heavily pigmented. The lower mandible shows a
faint ridge on the lamella. Many sperm reservoirs are
attached to the inner wall of the buccal membrane.
Although the generic boundaries in the family
Gonatidae appear to be somewhat indistinct
(Okiyama, 1969; Fields & Gauley, 1971; Nesis,
1971b), this specimen clearly belongs within the
genus Gonatus sensu stricto as indicated by the
presence of a tail extending beyond the gladius,
tentacle stubs and a radula with only five teeth.
DISCUSSION
The following evidence suggests that the spec-
imen has recently spawned:
1. The specimen had mated as indicated by the
presence of sperm reservoirs (discharged
spermatophores) embedded in the buccal
membrane.
2. The nidamental and oviducal glands are of
intermediate size (i. e. these glands are larger
than would be expected in immature specimen
but much smaller than would be expected in a
gravid specimen.
3. The ovary is almost totally depleted of mature
ova.
4. The specimen has undergone degeneration as
indicated by the gelatinous nature of the
muscular tissues and the loss of suckers from
all arms, as well as the loss of the tentacles.
The features which typify spent females are not
well-known. In order to confirm the above list as
characteristic of spent females of the family
Gonatidae, I have examined the extensive col-
lections of cephalopods at the University of South-
em California for females that appear to have
recently spawned. Four species of Gonatus are
found in the waters off southern California; females
of three species were found which appear to have
spawned.
Gonatus pyros Young, 1972. Two specimens,
135 mm pen length (P. L.) and 130 mm pen length,
easUy identified by the presence of a large oval
photophore on the ventral surface of each eye,
showed extreme signs of degeneration. In con-
sistency they are flaccid and gelatinous which con-
trast strongly wdth the muscular condition of im-
mature specimens. Tentacles are absent except for
small stubs. All arm suckers are absent; small poc-
kets or shght puckerings of the skin on the gela-
tinous trabeculae mark the spots where the suckers
had once been. The nidamental glands in both
specimens are considerably larger ( 30 and 25
mm) than one would expect to find in a large
immature specimen. The oviducal glands are fairly
large (22 and 16 mm). In both cases the ovary is
small and filled with small, deteriorated eggs. In one
specimen a mature egg which was presumably dis-
lodged from the oviducal gland during dissection
was found in the mantle cavity. No other eggs were
found in the oviducal glands or oviducts. The
mature egg, oval in shape, measures 3 mm long by
1.7 mm at the widest point. The deteriorating eggs
are sliglitly more than .5 mm in length. A number
of sperm reservoirs were found attached to the
buccal membrane. Clusters of small oval vesicles also
were found in the buccal membrane; broad
funnel-shaped ducts connected the clusters to the
oral surface of the buccal membrane (one funnel
per cluster). Presumably these are organs for storing
sperm. All of the vesicles examined appear to be
empty.
Gonatus berryi Naef. 1923. A single female (185
mm P. L), tentatively identified as this species on
the basis of the massive size of the arms, showed
evidence of having spawned. In most respects the
features of this specimen are the same as in G.
pyros. Tlie consistency is gelatinous; suckers are
absent; the ventral arms are completely bare and the
tentacles are absent. Tlie buccal membrane lacks
sperm reservoirs but most of the membrane is
Vol. 87 (2)
THE NAUTILUS
55
missing. Nidamental and oviducal glands are some-
what enlarged (35 mm and 25 mm respectively).
(For comparison, nidamental and oviducal glands of
an immature specimen (103 mm P. L.) measured 5
and 4 mm respectively). The ovary is small but has
a large number of small, elongate immature ova.
Interspersed among these cells are a number of
spherical, pale orange ova in various stages of ma-
turity, the largest of which is about 3.5 mm in
diameter.
Gcmatus onyx Young, 1972. One presumably
spent female has tentatively been identified to this
species, primarily on the basis of body proportions.
This specimen is somewhat different than the
others; the tissues are much firmer and more mus-
cular but still not as muscular as in an immature
specimen of this species. Both tentacles are missing
and suckers are absent from the dorsal three pairs
of arms. The ventral arms are bare except for a few
suckers at the arm bases. The nidamental and
/
..-'ft;®;'/'.'/'- ■'■■ ' ■
•V,.';
FIG. 1. Gonatus sp. from the Arctic Ocean. A, Ventral view; B, Dorsal view.
56 THE NAUTILUS
April 1973
Vol. 87 (2)
oviducal glands are somewhat enlarged (34 mm and
22 mm respectively). A small portion of the buccal
membrane is missing; the remaining portion is
strewn with sperm reservoirs and some of these are
attached to the bases of the arms. The ovary is
somewhat larger than in the other species and is
packed with long (about 1 mm in length), slender
immature eggs with a few larger orange, sperical,
partically mature eggs (1 mm diam.) interspersed.
Apparently a larger percentage of the eggs of this
specimen failed to mature completely before spawn-
ing.
These three species of Gonatus correspond rather
closely in their appearance with the specimen from
the Arctic Ocean. All show similar signs of degen-
eration, and comparable conditions of the ovary,
oviducal and nidamental glands; and several have
sperm reservoirs stOl attached to the buccal mem-
brane. The evidence strongly suggests that all of
these specimens are spent females.
Relatively little information is in the hterature
regarding the degeneration effects related to spawn-
ing in squids. Fields (1965) showed that the mantle
of spent females of Loligo opalescens decreased
greatly in thickness and girth and he concluded that
the mantle is the chief site for storing food reserves
consumed during the spawning period. He also
noted that oviducal and nidamental glands decreased
greatly in size after spawning but were still rela-
tively larger than these glands in immature females.
In an immature female (ML 87 mm) he found that
the nidamental gland was 0.6% of the total body
weiglit. In a mature female (ML 151 mm) the
nidamental gjand was 22.8% of the body weiglit
while in a spent female (ML 151 mm) the figure
was 5%.
McGowan (1954) observed a mass mortality of
the squid Loligo opalescens following copulation
and spawning. He noted that in the dead and dying
squid that the mantles were thin and limp. Sasaki,
1913 (according to Hamabe, 1963) found that in
the squid, Watasenia scintillam, males die after
mating in off-shore waters while females die after
spawning in coastal waters. Hamabe (1963) noted
that the cuttlefish Sepia esculenta apparently dies
after spawning. For Todarodes pacificus, Hamabe
(1963) found that in females with a reduced num-
ber of eggs in the ovary the mantle was thin and
flabby, the liver was reduced in size and firmness
and the stomach walls were thin and flabby. These
animals had large numbers of eggs in the oviducts
and Hamabe assumed that they had not yet
spawned but were about to do so.
It has been thought for many years that Octopus
dies after brooding its eggs (Nixon, 1969). Recently
W. Van Heukelem (in press) has noted rather rapid
degenerative changes occurring in the muscles of
female octopods in aquaria upon completion of the
brooding period and just prior to death.
The evidence suggests that degeneration and
death foUowing spawning by female squid is a
common if not universal phenomenon, and that the
same situation occurs in octopods although delayed
to the end of the brooding period (See also dis-
cussion in Arnold, in press).
Presumably the Arctic specimen had spawned
and was about to die when captured. Spawning
therefore probably occurred near March 30 and
about 79°58' N lat. and 170°23'E long., the time
and place of capture. This point is over water 2655
m deep in the Hyperborean Basin of the Arctic
Ocean. No information is available on the amount
of time which passes from spawning to hatching in
any gonatid. It is also not known whether gonatids
lay pelagic or benthic egg masses. Nesis (1971a)
estimates that the young specimens of Gonatus
from the northern Norwegian Sea hatched in April
or May.
ACKNOWLEDGMENTS
I thank the following people for reading and
commenting on the manuscript: J. Arnold, Pacific
Biomedical Research Center; M. Nixon, University
College London; M. Okiyama, Japan Sea Reg. Fish-
eries Res. Lab. Niigata; W. VanHeukelem and J.
McMahon, University of Hawaii. Tlie squid was
collected througli a program supported by NONR
228(19), NR 307-270 Office of Naval Research
contract with the University of Southern California
- work being pursured now under Dr. Hector Fer-
nandez: contract NOOO14-67-A-0269-0013 NR
307-270. I also thank Mrs. Constance McSweeny for
preparing the illustrations.
LITERATURE CITED
Arnold, J. M. 1972. Cephalopoda, Decapoda. In:
Reproduction of Marine Invertebrates. Giese, A.
and J. Pierce, edit.. Academic Press, In press.
Berry, S. S, 1925. The Cephalopoda collected by
the Canadian Arctic Expedition, 1913-18. Rept.
Can. Artie Exped. 1913-18, 8(B): 3-8.
Vol. 87 (2)
THE NAUTILUS
57
Fields, G. 1965. The structure, development, food
relations, reproduction, and life history of the
squid Loligo opaleseens Berry. Fish Bull. 131,
1-108.
Fields, W. G. and V. A. Gauley. 1971. Preliminary
description of an unusual gonatid squid
(Cephalopoda: Oegopsida) from the North Pa-
cific. Jour. Fish. Res. Bd. Canada 28(11):
1796-1801.
FIG. 2. Gonatus sp. from the Arctic Ocean. A, Left third arm; B, Left ventral arm; C, Radula; D, Beaks; E,
Large arm hook; F, Funnel-locking cartilage; G, Funnel organ.
58 THE NAUTILUS
April 1973
Vol. 87 (2)
Hamabe, M. 1963. Exhaustion process of the genital
organs of common squid, Ommastrephes sloani
pacificus. Bull. Japan Sea Reg. Fish. Res. Lab.
11: 1-11 [in Japanese] .
MacGinitie, G. E. 1955. Distribution and ecology of
the marine invertebrates of Point Barrow, Alaska.
Smithsonian Misc. Coll. 128(9): 1-201.
McGowan, J. A. 1954. Observations on the sexual
behavior and spawning of the squid Loligo
opalescens at La Jolla, California. Calif. Fish
Game 40: 47-54.
Naef, A. 1923. Die Cephalopoden. Systematik.
Fauna u. Flora Neapel, Monogr. 35, 1(1):
149-863.
Nesis, K. N. 1971a. The squid Gonatiis fabricii at
the center of the Arctic Basin. Hydrobio. Jour.
7(1); 93-96 [in Russian].
Nesis, K. N. 1971b. The family Gonatidae - abund-
ant squids of the North Pacific (their dis-
tribution, ecology, system and phylogeny).
Fourth Meeting of Investigation of Molluscs,
Academy of Sciences, U. S. S. R., Zoological
Institute, pp. 63-65 [in Russian].
Nixon, M. 1969. The hfespan of Octopus vulgaris
Lamarck. Proc. Malac. Soc. London 38: 529-540.
Okiyama, M. 1969. A new species of Gonatopsis
from the Japan Sea, with the record of a spec-
imen referable to Gonatopsis sp. Okutani, 1967
(Cephalopoda: Oegopsida, Gonatidae). Pub. Seto
Mar. BioL Lab. 17(1): 19-32.
Roper, C. F. E. and W. L. Brundage, Jr. 1972.
Cirrate octopods with associated deep-sea or-
ganisms: new biological data based on deep
benthic photographs. Smithson. Contr. Zool. No.
121: 1-46.
Sasaki, N. 1913. Ecology of hotaru-ika (Watasenia
scintillans (Berry)). Zool. Mag. 30(302): 581-590.
Van Heukelem, W. 1972. Life span of Octopus
cyanea Gray. Jour. Zool. (London), in press.
Voss, G. L. 1967. The biology and bathymetric
distribution of deep-sea cephalopods. Studies in
Tropical Oceanography, Miami 5: 511-535.
Young, R. E. 1972. The systematics and areal
distribution of the cephalopods from the seas off
southern California. Smithson. Contr. Zool., No.
97: 1-159.
BOOK REVIEW
SEA SHELLS OF TROPICAL WEST AMERICA.
Marine Mollusks from Baja California to Peru.
Second Edition. By A. Myra Keen; with assis-
tance by James H. McLean, xvi + 1064 pp., 4000
illus., 22 pages in color. Index. Stanford Uni-
versity Press, Stanford, Calif. 1971. $29.50.
It seems almost superfluous to recommend this
classic compendium to both professional and
amateur students of the tropical West American
marine mollusk fauna. The second and greatly en-
larged edition is the labor of love of A. Myra Keen
and a number of her able associates, such as James
H. McLean who undertook the herculean task of
organizing the section on the Turridae and most of
the Archaeogastropoda. Twila Bratcher and Robert
Burch contributed the revision of the Terebridae;
Eugene Coan and Barry Roth, the Marginellidae;
and Spencer Thorpe, the chitons.
Over 3,325 species are included, most of which
are well-illustrated and accompanied by succinct
descriptions, ranges, and synonyms. The updated
bibliography is one of the most complete ever
assembled for the mollusks of a major marine
province. The index, a measure of the magnitude of
the book, contains over 7,000 scientific entries. A
bonus comes to the users of the book in the form
of a good glossary, a geographical guide to and a
series of maps of the area, and tables for fath-
om-meter-feet conversion.
A very welcome addition is a fairly full treat-
ment of the known nudibranchs, thanks to the
efforts of Jame Lance. This rapidly growing subfield
of malacology has been greatly stimulated by the
inclusion of these shell-less orphans of conchology.
Twelve new plates of stunning color photographs
of 72 living mollusks add to the beauty and use-
fulness of this remarkable faunal guide.
In the face of such a huge, meticulous and
detailed documentation, one cannot resist repeating
Dr. Keen's quote from another woman writer,
George Eliot; "Why, you might take up some light
study - conchology now; I always thought that must
be a liglit study."
R. Tucker Abbott
Delaware Museum of Natural History
Vol. 87 (2)
THE NAUTILUS
59
SHORT PAPERS
RANGE EXTENSIONS OF CORBICULA
MANILENSIS (PHILIPPI) IN THE ATLANTIC
DRAINAGE OF THE UNITED STATES
Samuel L. H. Fuller
and
Charles E. Powell, Jr.
Academy of Natural Sciences of Philadelphia
Philadelphia, Pennsylvania 19103, U. S. A.
ABSTRACT
Corbicula manilensis (Philippi) is newly recorded
from the Savannah, Pee Dee, and Delaware river
systems in the Atlantic drainage of the United
States.
In a recent issue of this journal, Sickel (1973,
The Nautilus, 87 (1); 11-12) discussed the appear-
ance of Corbicula manilensis (Philippi) in the
Altamaha river system of Georgia, where this Asian
species was first detected in 1971. According to the
age of Sickel's oldest material, establishment of
Corbicula in this system had probably occurred as
early as 1968. "It will be only a matter of time
[Sickel concluded] before Corbicula moves north-
ward to inhabit the remainder of the Southern
Atlantic Slope region." To the probable detriment
of the native Atlantic drainage benthos, that time is
come.
Several living Corbicula were taken 20 September
1972 by Dr. Selwyn S. Roback and one of us
(SLHF) from the Savannah River, about 9 miles
northeast of Milhaven, Screven County, Georgia.
The specimens lived in shifting sand on a bar at the
mouth of an enormous slough; none was found at
depths greater than about 1 foot of water. Visits to
this locality in 1971 had failed to produce
Corbicula, but this material falls into at least two
size classes, and, at 20.0 mm in length, the largest
individual may have been in its second year of life.
During the previous week (12 September), Mr. C.
Kirkland Dunlap, Jr., and one of us (SLHF) had
found one living Corbicula and several "gapers" in
the Pee Dee River, about 3 miles southeast of
Society Hill, Darlington County, South Carohna. At
this point the Pee Dee floor is chiefly of hard clay,
with pockets of sand, which drifts in from springs
along the river margin. The living specimen was
found on bare clay in a few inches of water. The
largest individual (a gaper) measures 28.5 mm in
length, shows extensive erosion at the beaks, and
appears to have reached at least two years of age.
During September and October, 1972, one of us
(CEP) found Corbicula at numerous localities in the
Delaware River between Philadelphia, Pennsylvania,
and Trenton, New Jersey. The species was common
in no more than 1 8 inches of water on a variety of
substrates, primarily muds and fine gravels. The
largest individual collected is 16.5 mm in length and
appears to have been in its second year.
Thus Corbicula has now invaded the Savannah,
Pee Dee, and Delaware river systems, in each case
probably as eariy as 1971. Sickle argued per-
suasively that the species reached the Altamaha
system from the Apalachicola river system of the
eastern Gulf of Mexico drainage by means of man's
inadvertent carriage overland. We, on the other
hand, have no evidence which would incriminate
any given vehicle in the rapid and far-reaching
dispersal of Corbicula recorded here.
•
STREAM POLLUTION
REPORTED 104 YEARS AGO
"In the Erie Canal, Anodonta Lewisii Lea, for-
merly very abundant, is now quite scarce, prob-
ably on account of chemical contamination from
the gas works and armory at Uion, a mile and a
half west from Mohawk" [N.Y.] . - James Lewis,
M.D., Amer. Jour. Conch., vol. 4, p. 245, 1869.
•
JUNE A. M. U. MEETING
PLANS COMPLETE
Delaware will be the site of the 39th Annual
Meeting of the American Malacologjcal Union from
Monday, June 25, through Thursday, June 28,
1973. The main meetings will be held at the new
air-conditioned conference center on the campus of
the University of Delaware, Newark, Del. On Tues-
day there will be a guided tour of the Delaware
Museum of Natural History, with special films and
additional A. M. U. papers being given there. Pro-
spective new A. M. U. members are also welcome,
and are asked to send their annual dues ($4.00 per
person and $1.00 for an additional family member)
to obtain registration and dormitory reservation
forms from Mrs. Marian S. Hubbard 3957 Marlow
Court, Seaford, New York 11783.
60 THE NAUTILUS
April 1973
Vol. 87 (2)
EMARGINULA DENTIGERA HEILPRIN, 1889,
A LITTORAL MOLLUSK
Margaret C. Teskey
P. 0. Box 273
Big Pine Key, Florida 33043
From more than sixty shallow water stations in
the Florida Keys, both reef and shore, no specimen of
Emarginula was collected until a colony was dis-
covered in 1972 at the north (GulQ end of Big Pine
Key. Here the live mollusks cUng to slab limestone
rubble that was pushed into the water to form a nar-
row, sloping shore when a bordering road was con-
structed two years ago. They occur occasionally at
tide line but are most abundant at the two-foot
depth. Density of population may be judged by the
fact that on about fifty feet of shore, one hundred
specimens were taken by one collector in less than an
hour. Only Aaiiaea pustulata (Helbling) is more
numerous at the site.
Identification was made by Dr. R. Tucker Abbott
who remarked ( in litt.) that althougli Emarginula
dentigera has been considered an ecological form of
E. pumila A. Adams (Farfante, 1947), he is inclined
to recognize it as a valid species. E. pumila is reported
as extremely variable in size and shape; The Big Pine
Key shells are remarkably uniform, high-spired and
somewhat narrow. Adults vary little from a length of
6 to 7 mm,, width 4 mm., height 3 mm. The apical
whorls form a definite hook at about 2/3 of the
posterior length of the shell; color chalky-white or
FIGS. Emarginula dentigera /ye(7pn», 1889, from Big
Pine Key, Monroe Co., Florida. X5.
stained green; interior glossy; sculpture of 18 to 26
radial ribs of varying size and of numerous, smaller
concentric threads, giving a slightly cancellate appear-
ance.
Emarginula dentigera Heilprin, 1 889, was original-
ly described from Bermuda, as was its synonym, E.
pileum Heilprin, 1 889.
LITERATURE CITED
Farfante, Isabel Perez, 1947. Johnsonia, 2, (24):
107-109.
Heilprin, A. 1889. On Some New Species of Mollusca
from the Bermuda Islands, Proc. Acad. Nat. Sci.
Phila. for 1889: 141-142, pL 8, figs. 6 and 7.
•
New Council of Systematic Malacologists
On November 17, 1972, a group of 11 American
malacologjcal systematists, representing some of the
leading moUusk collections in the country, gathered
at the Academy of Natural Sciences of Philadelphia
to form a "CouncU of Systematic Malacologists." The
purposes of this organization are 1 ) to prepare recom-
mendations concerning standards and techniques of
collection management for malacological resources;
and 2) to define the goals and priorities of malaco-
logy. Working subgroups were appointed to prepare
recommendations concerning:
1) Compatible EDP (electronic data processing)
and curatorial programs for use by malacologists in
collection management and research;
2) Articulation of national goals for malacological
research;
3) Coordination of specimen acquisition policies
for malacological collections;
4) Preparation of position papers outlining priority
programs for malacology.
Membership to the Council is open to all profes-
sional persons in the Americas who use or manage
systematic malacological resources. Further informa-
tion may be obtained from the Chairman of the
Steering Committee, Dr. Alan Solem, Dept. of
Zoology, Field Museum of Natural History, Chicago,
111. 60605. It is hoped that other institutions and
their managerial malacologists will be added to the
initial participants: Acad. Nat. Sci. Phila.; Delaware
Mus. Nat. Hist.; Field Mus. Nat. Hist. (Chicago); Los
Angeles Co. Mus. Nat. Hist.; Mus. Comp. Zool. at
Harvard; National Mus. Canada (Ottawa); Nat. Mus.
Nat. Hist. (Wash., D.C.); Ohio State Univ. Mus.; Nat.
Hist. Mus. San Diego; Mus. Zool., Univ. Mich.
INFORMATION FOR SUBSCRIBERS
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mestic or foreign). Subscriptions may be commenced
in January when a new volume begins. Send check or
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Advertising rates may be obtained from the
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CONTRIBUTORS
Manuscripts: Authors are requested to follow the
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Journals, which may be purchased from the American
Institute of Biological Sciences, 2000 "P" Street,
N.W. Washington, D.C. 20036. Manuscripts should be
typewritten and doublespaced; original and one copy
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in arable, should be on separate pages, with the title
at the top. Legends to photographs should be typed
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within a drawing should be neatly printed, or they
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the printer may set them in 8 pt. type. There is a
charge of 50 cents per word for this extra service. All
authors or their institutions will be charged 50 cents
per line of tabular material and taxonomic keys. The
publishers reserve the right, seldom exercised, to
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An abstract should accompany each paper.
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They are obtained from the Economy Printing Co.,
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JULY, 1973
THE
NAUTILUS
;ie=B!-J
Vol. 87
No. 3
A quarterly
devoted to
malacology and
the interests of
conchologists
Founded 1889 by Henry A. Pilsbry. Continued by H. Burrington Baker.
Editors: R. Tucker Abbott and Charles B. Wurtz
O
EDITORIAL COMMITTEE
CONSULTING EDITORS
Dr. Arthur H. Clarke, Jr.
Department of Mollusks
National Museum of Canada
Ottawa, Ontario, Canada K1A-0M8
Dr. WUliam J. Clench
Curator Emeritus
Museum of Comparative Zoology
Cambridge, Mass. €2 138
Dr. William K. Emerson
Department of Living Invertebrates
The American Museum of Natural History
New York, New York 10024
Mr. Morris K. Jacobson
Department of Living Invertebrates
The American Museum of Natural History
New York, New York 1 0024
Dr. Aurele La Rocque
Department of Geology
The Ohio State University
Columbus, Ohio 43210
Dr. James H. McLean
Los Angeles County Museum of Natural History
900 Exposition Boulevard
Los Angeles, California 90007
Dr. Arthur S. Merrill
Biological Laboratory
National Marine Fisheries Service
Oxford, Maryland 21654
Dr. Donald R. Moore
Division of Marine Geology
School of Marine and Atmospheric Science
1 0 Rickenbacker Causeway
Miami, Florida 33149
Dr. Joseph Rosewater
Division of Mollusks
U. S. National Museum
Washington, D.C. 20560
Dr. G. Alan Solem
Department of Invertebrates
Field Museum of Natural History
Chicago, Illinois 60605
Dr. David H. Stansbery
Museum of Zoology
The Ohio State University
Columbus, Ohio 43210
Dr. Ruth D. Turner
Department of Mollusks
Museum of Comparative Zoology
Cambridge, Mass. 02138
Dr. Gilbert L. Voss
Division of Biology
School of Marine and Atmospheric Science
10 Rickenbacker Causeway
Miami, Florida 33149
EDITORS
Dr. R. Tucker Abbott
Delaware Museum of Natural History
Box 3937, Greenville, Delaware 19807
Dr. Charles B. Wurtz
3220 Penn Street
Philadelphia, Pennsylvania 19129
Mrs. Horace B. Baker
Business and Subscription Manager
1 1 Chelten Road
Havertown, Pennsylvania 19083
OFFICE OF PUBLICATION
Delaware Museum of Natural History
Kennett Pike, Route 52
Box 3937, GreenvUle, Delaware 19807
Second Class Postage paid at Wilmington, Delaware
Subscription Price: $7.00 (see Inside back cover)
THE
NAUTILUS
Volume 87, number 3 - July 1973
CONTENTS
Ronald P. Thomas and Lee Opresko
Observations on Ocropus joiibim: Four Laboratory Reared Generations 61
Dorothea S. Franzen
Oxyloma dcprimida, a New Species of Succineidae (Pulmonata) 66
David Nicol and Graig D. Shaak
Late Eocene Distribution of the Pelecypod Exputens in Southeastern United States 72
John N. Kraeuter
Notes gn Mollusics Ostrea and Siphonaria from Georgia (U.S.A.) 75
Maria Luiza S. Mello and Marlene T. Ueta
Observations by Polarized Liglit on the Radula of Aplexa marmorata 79
Alan K. Craig
A New Record for Liginis: The Boynton Beach Colony 83
Stuart A. Harris
PisiJium heiisluwanwu (Sheppard) in Western Canada 86
James T. Carlton
Corbicula in San Francisco, California 87
Robert Robertson
Cyclostremella: A Planispiral Pyramidellid 88
Donald R. Shasky
Obituary of G. Bruce Campbell, M.D 89
Frank Perron and Thomas Probert
Vivipanis malleatus in New Hampshire 90
Book Reviews
(of) Tom Rice, 77; J. C. Bequaert and W. B. Miller, 78; Recent Publications, 74.
J.ne iJneU Cabinet
Successor to :
Richard E. Petit
and
John Q. Burch
OLIVE SHELLS
OF
THE WORLD
SPECIMEN SHELLS
NATURAL HISTORY
BOOKS
ROWLAND F. ZEIGLEK
HUMBERT a PORRECA
International Directory of Conchologists - $3.00
A current worldwide list of 2,000 people interested
in mollusks and in exchanging shells. Gives addresses
and interests. Available only from The Shell Cabinet.
Olive Shells of the World bv Zeigler and Porreca -
$12.95
13 full-page color plates illustrating over 150 species
and named varieties. The only current treatment of
the popular family. Clothbound. Available from your
book store or directly from us.
} Other Recently Published Shell Books Available
I Post Office Box 29. Falls Church, Virginia 22046
A Rare Callectar^s I town .
now available at a startlingly low price!
Now only $n.7'> (formerly $30.00)
The few remaining copies of this unusual facsimile have
been purchased by the Delaware Museum of Natural History
and are now made available practically at cost to all libraries,
scientists and amateur conchologists. 48 beautiful, colored
plates, representing a faithful reproduction of Swainson's
1834 and 1841 classic, together with the original text and a
modern analysis by R. Tucker Abbott and Nora NfcMillan.
Handsomely bound, gilt-edged on 3 sides and in full 9x12
inch page size. A useful and rare work belonging in the
library of every lover of mollusks. Both available from your
favorite book dealer or directly from the
Delaware Museum of Natural History
Box 3937, Greenville, Delaware 19807, U.S.A.
INDO-PACIFIC
MOLLUSCA
MONOGRAPHS OF THE MARINE MOLLUSKS OF
THE WORLD WITH EMPHASIS ON THOSE OF
THE TROPICAL WESTERN PACIFIC
AND INDIAN OCEANS
The most technical and most beautifully illustrated
journal now being published on Recent and Tertiary
marine mollusks. Over 20 professional malacologists are
currently contributing. Edited by R. Tucker Abbott.
Among the groups treated are Strombidae, Cassidae,
Tridacnidae, Turridae, Littorinidae. Phasianelhdae, and,
soon to come. Patellidae, Harpidae and Mitridae.
Issued to date in looseleaf form with three sturdy,
permanent binders — 1100 pages, 810 plates (31 in full
color). Limited number of complete .sets left, $91.90 U.S.
(foreign: $94.00), postage paid. Any number of extra
binders available at $6.00.
Published by
The Delaware Museum of Natural History, Box 3937, Greenville, Delaware 19807 U.S.A.
VI
Vol. 87 (3)
THE NAUTILUS
61
OBSERVATIONS ON OCTOPUS JOUBINI: FOUR LABORATORY
REARED GENERATIONS'
Ronald F. Thomas and Lee Opresko
University of Miami, Rosenstiel School of Marine and
Atmospheric Science, Miami, Florida 33149
ABSTRACT
Four consecutive generations of Octopus joubini Robson were reared in the
laboratory. Spawning occurred at 4-5 months after hatching. At 27-29° C,
development of the eggs was completed in 34-42 days. Fiddler crabs /'Uca spp.j were
used almost exclusively for food, although other animals were also presented to the
octopods. Results indicate that there are probably two generations of 0. joubini per
year in the field.
INTRODUCTION
Few laboratory studies have been carried out
on the life history of octopods. Discussion of
hatching and rearing of the fry of sepioid squids
were presented by Choe and Oshima (1963), Choe
(1966). Schroder (1969a, b) and Boletzky et al.
(1971). The loliginid squids Sepioteuthis sepioidea
and Doryteuthis plei were discussed by LaRoe
(1971). Wolterding (1971) reared Octopus briareus
from egg to maturity and Arnold et al. (1972)
have reared Euprymna scolopes.
Owing to their accessibility and relative hardi-
ness in aquaria, some shallow water octopods, and
particularly species of Octopus, have been studied.
Octopus vulgaris was used extensively by J.Z.
Young in his classic series of experiments on
learning and behavior. Nixon (1969) studied the
rate of growth of O. vulgaris kept in the
laboratory. Boletzky (1969) studied the early
development of O. vulgaris, O. joubini and O.
briareus. In the same year Boletzky and Boletzky
reported on the first success in raising O. joubini
to maturity in the laboratory. From one brood of
about 50 eggs collected in the field, one female
survived to maturity and spawned about S^A.
months after hatching.
'Contribution No. 1592 from the University of
Miami, Rosenstiel School of Marine and Atmos-
pheric Science. This work was supported in part
by National Science Foundation grant
GB-24994X.
Octopus joubini is a species of small octopus
which is found in shallow waters along the west
coast of Florida and the northwestern Caribbean.
Its small size (about 10 cm. in total length at
maturity) makes it well-suited for laboratory
culture. The present paper reports on four genera-
tions of 0. joubini reared in laboratory. Observa-
tions on culture, feeding, brooding and life span
are given.
METHODS AND MATERIALS
This study was begun in February 1971 and is
still in progress. The octopods were maintained in
aquaria of 5-, 10-, and 20-gallon capacities and
FIG. 1. Adult male Octopus joubini //; aquarium.
Natural size. Photo by Dennis Opresko.
62 THE NAUTILUS
July 30, 1973
Vol. 87 (3)
FIG. 2. Eggs being brooded by female 0. joubini
on inside of empty flower pot. x I'A. Photo by
Dennis Opresko.
supplied with running sea water piped from
Biscayne Bay. The bay water was first passed
through settling tanks and was then filtered
througlr a series of gravity-fed compound filters
containing layers of CaCO pebbles and sand and
glass wool. With this system, adequate water
quality and aeration for the survival of the
octopods was maintained. Additional aeration was
provided by means of a mechanical pump as a
safeguard against water stagnation due to possible
blockage of the filters and subsequent loss of
water flow.
The initial brood and female were obtained
from inside a bottle found in shallow water of
about 1-2 meters at Key Biscayne, Miami, Florida.
The newly-hatched animals were supplied refuge
by astro turf floating on the water-surface. After 4
weeks, flower pots, rocks and shells were provided
for the animals. Mature females would readily
deposit eggs in the flower pots. Octopus joubini
attaches each egg individually to the substrate.
After hatching, the attachment point of the egg
on the substrate can be seen as a dark spot; this
permitted the estimation of the size of the brood.
For the first several days after hatching, the
octopods were still receiving nourishment from the
internal yolk sac and would not feed. During the
following 2 to 3 weeks, the juveniles would not
accept live ilea as food and were individually fed
daily. A segment of a Uca appendage placed in
contact with the octopus was usually seized and
eaten. After several weeks, the young animals
accepted live Uca of appropriate size.
The water level was kept several inches below
the tops of the aquaria to discourage animals from
crawling out of the tanks. This method was found
to be successful for this species.
OBSERVATIONS
At an early age O. joubini selected a home site,
either in a flower pot or in a rock crevice. Seven
adult octopods, each provided with a suitable
refuge and placed together in a 20-gallon aquari-
um, did not display any territorial aggressive
behavior. Under these conditions no deaths in any
aquaria were considered to be caused by other
octopuses.
The animals consumed a considerable amount
of food (Uca). The young octopods successfully
attacked crabs equal to or larger than themselves.
They were strongly nocturnal, remaining in crev-
ices during the day and searching for food at
night. If a liglit were turned on at niglit while an
octopus was feeding, it would drop the partially
consumed crab and return to its den. It would
later attack another Uca rather than continue to
feed on the dead, half-eaten crab.
In table 1. temperatures in the aquaria are
given. Small fluctuations of aquarium temperatures
(from 1-2 C) tended to reflect those of the room
rather than those of the field, but in general,
aquarium temperatures were comparable to those
in the field.
Fj GENERATION
The F generation hatched on 13 February
1971. The newly hatched animals grew slowly,
probably because of an inadequate supply of food.
The most critical stage in rearing O. joubini occurs
between 2 and 21 days of age, since the animals
would not attack live food. Consequently this is
the time during which the higliest mortality
occurred. Later mortalities usually occurred when
the sea water system became blocked and addi-
tional aeration was not used. As the water in the
tank began to foul, the animals responded by
leaving their dens and moving to the water
surface.
Three F females laid eggs 4'/i months after
hatching, all within several days of each other.
Vol. 87 (3)
THE NAUTILUS
63
Thus the maturation ot~ laboratory-raised O. joii-
bini was sutTiciently rapid to allow two genera-
tions to be completed within a year.
One female laid about 40 eggs. The length of
these eggs (7.6 mm.) did not differ significantly
from measurements reported in the literature
(8.0-8.5 mm.) by Boletzky (1969).
Once the eggs were laid, the female remained
with them until they hatched. Her arms continu-
ously swept over the eggs to remove detritus that
settled on them. She would not leave the eggs to
feed. If a crab entered the octopus' den while she
was brooding eggs, she would generally attack and
consume it. Due to the higli density of crabs in
each tank, females were able to feed while
brooding. Although it is generally believed that the
female octopus dies soon after the eggs hatch, this
did not always occur in the laboratory, probably
due to the availabihty of food during brooding.
At 27-30°C, hatching occurred within 34-42
days, usually at niglit. Near the time of hatching,
mechanical stimulation caused by examining the
eggs resulted in premature hatching of some eggs.
Although these octopods hatched prematurely,
they were still able to survive.
The females did not lay a second brood of
eggs. After the eggs hatched both males and
females showed a reduction in feeding intensity
(the animals now fed sporadically rather than
regularly). At about 6 months of age the F males
and females began to die. The mortality rate
steadily increased so that by 8 months of age
about 50% adult mortality was attained. Old,
dying O. joubini typically stopped feeding and
abandoned their dens. They often sat on the floor
or sides of the aquarium, slowly coiling and
uncoiling their arms in an uncoordinated manner.
F^ GENERATION
Eggs were laid by F females on 23 June 1971.
The F generation hatched between 34 and 42
days later. Growth of these animals was similar to
that stated for the F generation. Egg laying by
F^ females began at the end of November,
indicating that this generation reached maturity in
about 4 months. The water temperature in the
aquaria during the development of the F genera-
tion was 27-29°C, about 1-3°C higher than the
temperature during the development of the first
generation.
TABLE 1. Temperature values (°Cj measured in the
aquaria.
Date
21 July 1971
28 July
3 August
10 August
16 August
24 August
31 August
7 September
1 1 September
20 September
24 September
30 September
Temp (°C)
28.9
28.2
29.0
27.8
27.1
29.0
27.8
26.7
27.0
27.0
27.0
27.0
FIG. 3. Young O. joubini in typical posture, x 2.
Photo by M. Wolterding.
64 THE NAUTILUS
July 30, 1973
Vol. 87 (3)
TABLE 2. Dates of hatching o/ Octopus joubini eggs
laid 23 June 1971. Water temperatures: 27-29° C.
Fj GENERATION
Approximately 95 eggs were laid by one of the
F females. Hatching of these eggs began on 26
December 1971. At the end of six weeks. 52
young were still alive. This generation was raised
very successfully, and about 42 animals reached
maturity, with 1 5 females laying broods of eggs.
The size of the F animals was quite small
(average mantle length of 5 males: 26.7 mm.; of 5
females: 21.9 mm.). We feel that stunting occurred
as a result of crowded conditions in the aquaria.
Inadequate food may have been a contributing
factor during the early growth period. Egg-laying
began at AVi months (15 May 1972) even in the
small females, althougli the number of eggs per
brood was low. It is interesting to note that O.
joubini in Biscayne Bay, Florida, were also
observed to have eggs at the same time as the F^
females (James Espy, personal communication).
F GENERATION
4
These octopuses began to hatch on 20 June
1972 and hatching continued to the middle of
July. A culture of brine shrimp (Artemia salina)
was established and maintained in an attempt to
replace the individual feeding of each juvenile
octopus. For this experiment, octopuses between 1
and 7 days old were supplied with brine shrimp of
various sizes, excluding newly hatched brine
shrimp. The brine shrimp were placed in the tank
with the octopus at 4:00 PM daily and the
running water was turned off. The Artemia were
observed to swim slowly around the tank, during
which time they often came in contact with an
octopus. Many times brine shrimp were seen to
crawl under the octopus. Instead of seizing the
brine shrimp, the octopus blanched, inked and
swam away. Brine shrimp held with forceps and
presented to the octopus were rejected. One
octopus, presented with brine shrimp in this
manner, accepted the food after many trials and
was later observed to capture live Artemia. This
procedure unfortunately met with little success
and it became necessary to resume the hand
feeding.
The number of F juveniles that hatched could
not be accurately estimated because many were
able to hide in the rocks that were provided for
the adults. About 70 were isolated and placed in
separate aquaria of 3- to 5-gallon capacity. One
month after the initial hatching occurred 15 of
the largest F O. joubini were placed in a single
20-gallon aquarium and were fed exclusively with
live Uca spp. The small individuals which remained
in the 3- to 5-gallon aquaria were fed pieces of
Uca appendages and were also provided with
suitably-sized live Uca.
DISCUSSION
Boletzky & Boletzky (1969) were able to raise
one female Octopus joubini to maturity. This
animal laid eggs 5'/i months after hatching. The
present study confirms the rapid development of
this species of octopus. Mangold- Wirz (1963)
found that females of Eledone cirrosa, E. mos-
chata. Octopus vulgaris and Pteroctopus tetracir-
rhus reached sexual maturity at about 18-24
months, while Bathypolypus sponsalis matured at
8-17 months.
According to Boletzky (1969), at 24-25°C the
eggs of O. vulgaris hatch in 25 days, O. joubini in
30 days, and O. briareus in 50 days. In this study,
hatching of O. joubini began at about 34 days,
thus agreeing with Boletzky's findings.
As is typical with most octopods, the female of
O. joubini diligently cares for the eggs until they
hatch. Brooding behavior weakens the female and
she generally dies soon after the eggs hatch, but
death appears to be delayed if she is able to feed
during brooding.
The rapid maturation of O. joubini in the
laboratory suggests that there are two generations
Vol. 87 (3)
THE NAUTILUS
65
annually. Thus in certain parts of the range it is
likely that there is both a summer and a winter
population of tiiis species. This species of small
octopus with its short life span provides an
opportunity to study development in the labora-
tory and to establish techniques for cephalopod
maintainance. An important problem, water qual-
ity, can be minimized by a running sea-water
system with filtering equipment. With running
sea-water, additional aeration is unnecessary but is
advisable in the event that the water flow is
temporarily blocked.
Feeding presents the other major problem in
the culture of benthonic octopods. At the present
time, suitable live food for the young juveniles has
not been found. Gammarid and caprellid amphi-
pods and various other amphipods as well as
numerous isopods were offered to the juveniles
but were rejected by them. This was found to be
the case for Artemia salina, except with one O.
joubini The largest and probably oldest (7 days
old) F juvenile which was offered brine shrimp
did finaUy attack Artemia. Even though the
octopus accepted them as food, the fact that the
smaller O. joubini would not eat brine shrimp
prevents this method from being used on newly
hatched O. joubini Artemia seems to be more
suitable for octopods with planktonic larvae and
has been used in rearing O. vulgaris (Boletzky,
personal communication).
The method of feeding with Uca described here
is time consuming and inefficient, contributing to
most of the mortalities at this stage of growth. In
areas where Uca is abundant, it provides a
satisfactory and easily obtainable source of live
food for the larger animals.
ACKNOWLEDGMENTS
We wish to thank Mr. Dennis Opresko and Mrs.
Irene Thomas for their help in maintaining the
animals and for their assistance in the preparation
of the manuscript. We also wish to thank Mr. D.
Opresko for photographing the animals. Dr. Won
Tack Yang provided helpful suggestions in the
culture of marine organisms and also provided the
stock of live Artemia. We especially wish to thank
Dr. Gilbert L. Voss for his support and encour-
agement during this study and for his critical
reading of the manuscript.
LITERATURE CITED
Arnold, J.M., C. T. Singley and L. D. Wil-
liams-Arnold 1972. Embryonic development and
post-hatclring survival of the Sepiolod squid
Euprymna scolopes under laboratory conditions.
The VeHger 14(4); 361-364.
Boletzky, S. von 1969. Zum Vergleich der Onto-
genesen von Octopus vulgaris, O. joubini. und
O. briareus. Rev. Suisse Zool. 76: 716-726.
Boletzky, S. von • & M. V. von Boletzky 1969.
First results in rearing Octopus joubini Robson,
1929. Verh. naturf. Ges. Basel 80: 56-61.
Boletzky, S. von, M. V. von Boletzky, D. Frosch,
& V. Gatzi 1971. Laboratory rearing of Sepio-
linae (Mollusca; Cephalopoda). Mar. Biol. 8:
82-87.
Choe, S. 1966. On the eggs, rearing, habits of the
fry, and growth of some Cephalopoda. Bull.
Mar. Sci. 16: 330-348.
Choe, S. & Y. Oshima 1963. Rearing of cuttle-
fishes and squids. Nature 197: 307.
LaRoe, E. T. 1971. The culture and maintainance
of the loliginid squids Sepioteuthis sepioidea
and Doryteuthis plei Mar. Biol. 9: 9-25.
Mangold- Wirz, K. 1963. Biologie des Cephalopodes
benthiques de la Mer Catalane. Vie et Milieu
(Suppl.) 13: 1-285.
Nixon, M. 1969. The lifespan of Octopus vulgaris
Lamarck. Proc. malac. Soc. London 38:
529-540.
Schroder, W. 1969a. Observations made during the
breeding of cuttlefish {Sepia officinalis L.).
Drum and Croaker 69: 9-15.
Schroder, W. 1969b. Notes concernant Cepha-
lopoda et la reproduction de la seich commune.
Zool. Anvers. 34th year (3).
Wolterding, M. 1971. The rearing and maintainance
of Octopus briareus in the laboratory with
aspects of their behavior and biology. M.S.
thesis, Univ. of Miami, 120 pp.
66 THE NAUTILUS
July 30, 1973
Vol. 87 (3)
OXYLOMA DEPRIMIDA, A NEW SPECIES OF SUCCINEIDAE (PULMONATA)
Dorothea S. Franzen
Ulinois Wesleyan University
Bloomington, Illinois 61701
ABSTRACT
Oxyloma deprimida, a new species of Succineidae (Piilmonataj is described from
Utica, LaSalle County, lilinoiSj (type locality) and near Canton Lake, NE of Canton,
Fulton County, Illinois. The nuclear whorl of the shell is depressed, hence, the species
name deprimida. The habitat of O. deprimida is on cattails generally 3 to 5 ft. above
the wet ground or v^ater level The snails mature in the fall and not in the summer as
does O. retusa, a sympatric species. Anatomical features include a broadly based penial
appendix and an albumengland which is smaller than the prostate gland.
The search for succineas in the state of Illinois
has resulted in the recognition of a hitherto
undescribed species, Oxyloma deprimida, new spe-
cies.
Description of Holotype: The amber-colored,
ovate, imperforate shell, composed of three inflated
whorls, is thin, fragile, shiny, and marked only by
tme striae. The nuclear whorl is depressed (Fig. 1,
upper riglit), rough and pitted (Fig. 1, lower left).
The whorls increase rapidly in size from the nuclear
to the body whorl. The suture is sharply incised
resulting in a sliglit shouldering along the upper
border of the whorl. The peristome of the ovate
aperture is sharp and continuous over the surface of
the body whori in the form of a thin, white callus
(Fig. 2, left). The narrow, white columella follows
the inner border of the peristome (Fig. 2, left). The
dimensions of the shell are: heiglit, 12.45 mm.;
width, J. 6 mm.; height of aperture, 9.85 mm.;
width of aperture, 5.7 mm. Tlie ratios of the several
dimensions are shown in Table I.
The surface of the head and the body wall are
cream-colored and coarsely and irregularly tuber-
culate. The pigmentation of the anterior dorsal
portion of the head consists of black blotches
arranged in five, indistinctly defined, longitudinal
bands that form a shield-shaped pattern (Fig. 2,
riglit). Tliey converge medially between the pos-
terior tentacles and then spread apart continuing as
two bands towards the mantle. The shield pattern is
Hanked on either side by a pigmented band, narrow
anterioriy, but broadening at the base of the pos-
terior tentacles as it continues to the mantle. On
FIG. 1 . Upper left. Chromosomes of an ovotestis
smear of Oxyloma deprimida from the type
locality. Enlarged. Upper right, Scanning-elec-
tron-photomicrograph showing the nuclear whorl of
Oxyloma deprimida of a shell from the f}'pe locality.
Enlarged. Lower left, Scanning-electron photo-
micrograph of the nuclear whorl of Oxyloma
deprimida of a shell from the type locality, showing
surface detail. Enlarged. Lower right. Scanning-elec-
tron-photomicrograph of the nuclear whorl of a shell
of Succinea luteola, showing surface detaiL Enlarged.
Vol. 87 (3)
THE NAUTILUS
67
FIG. 2. Drawings of the holotype of Oxyloma
deprimida. Left, shell drawn to scale as indicated.
Right, head and anterior portion of mantle.
Enlarged.
the lateral body wall flecks of light pigmentation
form a broad band that tapers and diminishes
posteriorly. Tlie manfle collar is lightly pigmented
on the upper and outer surface and more heavily
pigmented on the anterior and inferior surface. The
pigmentation of the anterior portion of the mantle
occurs as widely-spaced blotches (Fig. 2, riglit). The
anterior border of the nephridium is outlined by a
narrow, broken, black band whereas the posterior
border is outlined by a broader, darker band.
Sparse, scattered patches of pigment occur on the
remainder of the body. The genital aperture, cres-
cent-shaped, 2 mm. in length, surrounded by a white,
tumid lip, is situated on the anterior right-hand side
of the body. A pedal groove, continuous from the
labial palp to the posterior tip of the body, sep-
arates the foot from the lateral body wall; the pedal
groove is paralleled dorsally by a less-pronounced,
suprapedal groove. Shallow, vertical grooves incise
the pedal and suprapedal grooves and the broad,
pigmented band. These vertical grooves produce a
series of shallow scallops along the margin of the
pedal groove especially when the animal is in a
somewhat contracted state.
Holotype: catalogue no. FMNH 176002; para-
types nos. FMNH 176003, FMNH 176004, and
FMNH 176005, Molluscan CoUection, Field Museum
of Natural History, Chicago, Illinois. Additional
paratypes are in the private collection of the author.
The author has examined shells of succineas of
the collection in the Natural History Museum, Uni-
versity of Illinois. A shell identified by Frank
Collins Baker (1939) as Succinea retusa peoriensis
Wolf and which Pilsbry (1948) identified as Oxy-
loma decampi peoriensis (Walker), as indicated be-
low, is herein identified as Oxyloma deprimida, new
species.
Synonymy —
Succinea retusa peoriensis Wolf. Frank Collins
Baker, 1939. Fieldbook of Illinois Land Snails,
Manual 2, Natural History Survey Division, p. 126,
Fig. E, left-hand figure only.
Oxyloma decampi peoriensis (Walker), Henry A.
Pilsbry, 1948. Land Mollusca of North America,
Vol. II, Ft. 2, p. 785, Fig. 420, b, left-hand figure
only.
Known geographic distribution and habitat: I.
Type locality: Field No. D.S.F. 350; NEVa SWA S 9,
Twp. 33 N, R 2 E, Utica (N. Utica), LaSaUe
County, Illinois, about Vz mile east of the crossing
of Illinois Highway 178 over the Rock Island and
Pacific railroad tracks, between the Rock Island and
Pacific railroad tracks and Clark Run Creek. The
habitat is the shore of a water-filled pit on the
northern edge of Clark Run Creek that supports
cattails (Typha sp.), goldenrod (Solidago sp.), and
willow (Salix sp.). Oxyloma deprimida lives on the
cattails several feet (2 to 5) above the wet ground
and/or above the water level.
An earher unpublished record of the species
taken from "Utica, Illinois" is in the Molluscan
Collection of the Field Museum of Natural History,
Chicago, Illinois. The shells, catalogue no. 58198,
were identified as Succinea (Oxyloma) decampi
Bryant Walker. They were formerly in the James H.
Ferriss collection and identified as Succinea retusa
peoriensis Wolf
Locality: 2. Field No. D.S.F. 194; NEy4 SEV*
NW54 S 19, Twp. 7 N, R 5 E; 3 miles NE of the
town square in Canton, Fulton County, Illinois. The
habitat is a lowland adjacent to a northeastern arm
of Canton Lake where moist ground supports a
stand of cattails and willows. Oxyloma deprimida
lives on this vegetation 3 to 5 feet above the
ground, and is not found on the ground where lives
O. retusa (Lea), a sympatric species. This association
does not, however, occur at the Utica locality.
Anatomy of paratypes: The large, coiled, heavily
pigmented hermaphroditic duct, coming from the
ovotestis, enters the fertilization sac which is con-
nected with the seminal vesicles. The relatively
large, twinned, unequal seminal vesicles are coarsely
peppered with black pigmentation whereas the in-
68
THE NAUTILUS
July 30, 1973
Vol. 87 (3)
flated fertilization sac is lightly pigmented. The
prostate gland is situated immediately anterior to
the albumen gland. The acinar prostate gland is
covered by a thin, lightly pigmented sheath, and is
larger than the albumen gland. The albumen gland,
about two-thirds the length of the prostate, is
composed of acini which are smaller than those of
the prostate gland. Tlie single duct leading from the
fertilization sac divides to form two ducts, one
leading into the prostate gland and the other form-
ing the oviduct (Fig. 3, F).
The vagina is straight, slightly pigmented, equal
to about seven-eighths of the length of the penis,
and opens along with the penis into the genital
antruiTL The oviduct is higlily convoluted, slightly
pigmented, and enters the distal end of the vagina
as does the spermathecal duct. The spermathecal
duct loops over the oviduct just prior to its entry
into the vagina.
The retractor muscle of the right posterior tent-
acle passes between the penis and the vagina. The
penis is enclosed in a thin, translucent sheath pep-
pered with black pigment in the middle or towards
its distal end. The vas deferens may or may not be
lightly stippled. As the vas deferens approaches the
distal end of the penial sheath it loops ventrally
under the penial retractor muscle and enters the
penial sheath terminaOy; then known as the
epiphallus, it coils, increases in caliber as it ap-
proaches the penis and becomes enlarged just before
it merges with the penis subterminally (Fig. 3, A).
The penial appendix, because of its broad base,
appears to be a terminal extension of the penis
rather than an appendix separated from the body of
the penis by a constriction. The size and shape of
the penial appendix is variable (Fig. 3, A - E).
The ovotestis ot many individuals of Oxyloma
deprimida, from both localities, were squashed and
l-R-L
2-R-M 4-R-M 21-R-M
FIG. 4. Representative teeth of a radula of a snail
taken from near Canton Lake; 3 mi. NE Canton,
Illinois. C, central tooth: l-R-L, 1st right lateral;
2-R-M, 2nd right marginal; 4-R-M. 4th right
marginal; 21-R-M, 21st right marginal.
stained with orcein. Examinations of the stained
chromosomes in metaphase revealed the haploid
number of nineteen to be characteristic of this
species (Fig. 1, upper left). This is the same number
found in O. retusa (Lea), O. haydeni (W. G. Binney)
and O. salleana (Pfeiffer), (Franzen, 1966, p. 67).
The radula (Fig. 4) is composed of many rows of
teeth and numerous teeth to a row. The number of
rows in 6 radulae examined, ranged from 90 to 116.
The numbers of marginals and laterals of re-
presentative rows of 5 radulae are to be noted in
Table II. The ratios of marginals to laterals ap-
proaches 1:3 and 1:4. Tliis compares with what has
been reported for Oxyloma ren<xa, (Franzen, 1963,
Table II, p. 89) and for O. haydeni, (Franzen, 1964,
Table II, p. 78).
The structural details of the individual teeth
resemble those of the genus in general (Fig. 4). The
central tooth has a broad basal plate which has a
lateral basal pointed projection on either side. The
pointed mesocone, somewhat variable in length,
does not usually extend to the lower margm of the
basal plate. A shorter, pointed ectocone flanks the
mesocone on either side. The laterals have a large,
pointed mesocone which, like tliat of the central
tooth, is usually not as long as the basal plate: the
single ectocone, sometimes divided into
two — especially of the more lateral teeth — is
pointed; a short, pointed endocone may be present.
The marginals, smaller than the laterals, have a long,
slender basal plate which is characteristic of the
genus Oxyloma (Quick, 1933:296, Fig. 1, Oxyloma
(Succineaj pfeifferi Rossm.). Of the cusps of the
marginals, the mesocone is the largest, the endocone
is small and pointed. The ectocone of about the six
medial-most marginals is divided into two unequal
cusps of which the lateral-most is the largest, and
curved. The ectocone of the more lateral marginals
is divided into three cusps of which the outermost
is the largest. The ectocone of the marginals nearest
the outer side of the radula may be divided into
four cusps of which the outermost is short and
pointed. The features of the amber-colored jaw are
typical of the genus. A prominent median fold
projects anteriorly and is flanked on either side by a
broadly rounded fold.
The surfaces of the bodies of the paratypes are,
as in the holotype, creanvcolored and coarsely and
irregularly tuberculate. The pattern of pigmentation
of the head and body is like that of the holotype
Vol. 87 (3)
THE NAUTILUS
69
althougli tlie intensity of pigmentation is variable.
The sole of the foot may be lightly or not at all
speckled. The most striking variation of pig-
mentation is that of the mantle. The pattern of the
anterior portion may be in the form of black,
widely-spaced blotches, as in the holotype, or
heavier blotches arranged in indistinctly defined
rows connected by less intense stripes of pigment,
or the blotches may merge, resulting in an irregular
pattern. The amount of pigmentation anterior to
the nephridium varies from light to heavy, the latter
in the form of a dark area interspersed by
fine-lined, light streaks. The intensity of the pig-
mentation outlining the nephridium is light in some
individuals and more intense in others. The pigmen-
tation of the area posterior to the nephridium varies
from a few scattered blotches to many patches
merging to form a more overall pattern extending to
the posterior tip of the animal.
Shell of paratypes: The shell of the mature snail,
attaining a height of almost 13.5 mm., is comprised
of 2^/2. to 3 inflated whorls. The surface of the
nuclear whorl is rougli and pitted (Fig. 1, lower
left) but not distinctly malleated as in Succinea
lutenla Gould (Fig. 1, lower riglU), S.
vaginacontorta Lee, and S. campestris Say.
Dimensions of the three largest shells, number of
shells measured, and the median of each series
measured, are recorded in Table L The range of the
greatest height of the series of shells included in this
study is from 9.8 inm. to 13.46 mm.; and the range
of the greatest width is from 6.7 mm. to 8.4 mm.
The greatest heiglit of shells obtained from the
Canton Lake locality is 11.8 mm.; the greatest
diameter is 8.4 mm. (October, 1960): the com-
parable dimensions of shells of the Utica locality
are, greatest height, 13.46 mm., greatest diameter,
8.04 mm. (September, 1967).
Distinctive characteristics of Oxyloma deprimida:
The name of the species, deprimida, denotes the
depressed position of the nuclear whorl (Fig. 1,
upper riglit) as contrasted with the prominent,
knoblike nucleus which is characteristic of other
known species of the genus. The tip of the nuclear
whorl appears to be somewhat "tucked in"" under
the penultimate whorl.
The epiphallus enters the penis subterminally
which produces a terminal extension of the penis,
the penial appendix. In O. deprimida the base of
the penial appendix is broad which makes it appear
to be a terminal extension of the penis rather than
an appendix distinctly separated from the body of
the penis by a constriction as in, for example, O.
haydeni, (Franzen, 1964, Fig. 1). The epiphallus
enlarges as it approaches the penis and merges
imperceptibly with it.
The albumen gland is smaller than the prostate
gland and is located posterioriy to it. The acini of
the albumen gland are distinctly smaller than are
those of the prostate.
Oxyloma deprimida lives on cattails and willows
generally 3 to 5 feet above the ground and/or the
water level, not on the ground nor on objects
floating on the water. The last time the type
locality was visited (September 28, 1971) the water
had receded to the level of the small stream as a
PENIAL RETRACTOR
MUSCLE
PENIAL SHEATH
FIG. 3. Drawings of genital organs of Oxyloma
deprimida: A - E, penis, penial appendix and
epiphallus shown inside of penis sheath cut open.
The figures are of snails from the following
localities: A, near Canton Lake, 3 mi. NE Canton,
Illinois: B, Utica. Illinois: C, Utica, Illinois: D,
Utica. Illinois: E, near Canton Lake. S mi. NE
Canton. Illinois. F. prostate gland and albumen
gland of a snail from the Utica, Illinois, locality:
PG, prostate gland: AG, albumen gland: FS,
fertilization sac: SV, seminal vesicles: HD, herma-
phroditic duct.
70 THE NAUTILUS
July 30, 1973
Vol. 87 (3)
TABLE 1. Dimensions of the shells o/Oxyloma depressa. The measurements are of the 3 largest shells of each
of the 9 series as indicated. In the 4th column of measurements are listed the ratios of the width of the shell
over its height. In the last 3 columns are listed the ratios of the height of the aperture over the height of the
shell, width of aperture oner width of shell, width of aperture over height of aperture.
result of a period of about a year of low pre-
cipitation. The ground of the usually submerged
area was wet though not muddy. Even under such
conditions O. deprimida was not found on the
ground. Many of the snails were aestivating on the
cattails 2 feet above the ground.
Oxyloma deprimida differs from other species of
the genus, at least in the Mississippi Valley, as to
the time of year in which it reaches maturity. The
mature, fully grown, sexually active adults are to be
found from the latter part of September to the
early part of October. This is several months later
Vol. 87 (3)
THE NAUTILUS
71
TABLE 2. Formulae of representative rows of teeth o/Oxyloma deprimida new species.
No. of Rows
TABLE 3. Comparisons of the medians of ratios of several dimensions o/Oxyloma deprimida with
several other species of Oxyloma as previously reported (Franzen, 1969, Table III).
Species
O. deprimida
O. retusa
O. haydeni
O. salleana
0. sanibelensis
W. of Shell/
H. of Shell
59.7%.- 71.0%
52.0%
49.0%
56.3%
47.8%
H. Aperture/
H. Shell
73.7% - 78.0%
74.4%
73.0%
78.6%
60.7%
W. Aperture/
W. Shell
67.9% - 76.8%
80.5%
85.3%
79.2%
68.8%
W. Aperture/
H. Aperture
59.4% - 64.5%
57.1%
57.6%
57.6%
55.2%
than the maturation time of O. retusa, O. haydeni,
and O. salleana whose mature adults disappear in
the latter part of June or in early July.
ACKNOWLEDGMENTS
National Science Foundation Grants-in-Aid No's.
NSF G18000 and NSF GB2715 provided laboratory
equipment and supported, in part, the field studies.
The author is grateful to Dr. B. V. Hall, Director,
Center for Electron Microscopy, Univ. of Illinois,
Urbana, and to Dr. James Anderson for the scan-
ning-electron-photomicrographs. Dr. Alan Solem,
Field Museum of Natural History, Chicago, Illinois,
and Dr. Donald F. Hoffmeister, Natural History
Musuem, Univ. of Illinois, Urbana, graciously lent
shells of the respective museum collections. Dr. A.
Byron Leonard read the manuscript and offered
helpful suggestions.
LITERATURE CITED
Baker, Frank Collins. 1939. Fieldbook of Illinois
Land Snails, Natural History Survey Division,
Manual 2, State of Illinois: 3-166.
Franzen, Dorothea S. 1963. Variations in the Anat-
omy of the Succineid Gastropod Oxyloma retusa.
The Nautilus 76 (3); 82-95, Tables I-II, Figs. 1-4.
Franzen, Dorothea S. 1964. Anatomy of the
Succineid Gastropod Oxyloma haydeni. The
NautUus 77(3): 73-81, Tables I-II, Fig. 1.
Franzen, Dorothea S. 1966. Anatomy of the
Succineid Gastropod Oxyloma salleana (Pfeiffer).
The Nautilus 80(2): 59-69, Tables I-II, Figs. 1-3.
Franzen, Dorothea S. 1969. Structural Character-
istics of Succineid Gastropod Oxyloma
sanibelensis. The Nautilus 82(3): 77-83, Tables
I-III, Figs. 1-2.
Pilsbry, Henry A. 1948. Land MoUusca of North
America (North of Mexico). Acad. Nat. Sci.
Philadelphia Mon. No. 3, Vol. 11, Pt. 2: xlvii -^
521-1113, 585 figs.
Quick, H. E. 1933. The Anatomy of British
Succineae. Proc. Mala. Soc. London 20(VI,
Nov.): 295-318 PI. 23-25, Figs. 1-18, Tables
1-V.
THE NAUTILUS
July 30. 1973
Vol. 87 (3)
LATE EOCENE DISTRIBUTION OF THE PELECYPOD KXPlTEys
IN SOUTHEASTERN UNITED STATES
David Nicol
Box 14376, University Station.
Gainesville, Florida 32601
and
Graig D. Shaak
The Florida State Museum
University of Florida
Gainesville, Florida 32601
ABSTRACT
The pelecypod Exputens (Malleidae) was confined To the Tethyan marine province
during the Middle and Late Eocene. In Peninsular Horida Exputens ocalensis
(MacNeil) is found in the two lowest zones of the Crystal River Limestone, which is
Late Eocene in age. Exputens has also been found in the Ocala Limestone of
southwestern Georgia and the Castle Hayne Marl in North Carolina, which shows
that at least one Tethyan mollusc lived farther north during the Late Eocene than
had previously been supposed.
Tlie presence of the pelecypod Exputens in
strata of Late Eocene age in Peninsular Florida has
been reported by Palmer, 1957. p. 70; 1967, pp.
189-190; and Palmer and Brann, 1965. p. 143.
However, Exputens was not mentioned as occur-
ring in Florida by Hertlein and Cox, 1969, in the
Treatise on Invertebrate Paleontology. Moreover,
the type species, Exputens llajasensis Clark, 1934,
was stated as fixed by original designation. In his
original description of Exputens, Clark described
two new species, E. llajasensis and E. alexi, but he
selected neither species as the type of Exputens.
The type species was subsequently designated by
Yokes, 1939, p. 51, as E. llajasensis Clark from
Middle Eocene beds from Simi Valley, California.
Palmer, 1957. 1967. has particularly emphasized
the fact that Exputens was confined to the
Tethyan marine province, and it has been reported
from Jamaica and southern California as well as
Florida. The stratigraphic range of the genus
appears to be Middle and Upper Eocene.
MacNeil described Vulsella ocalensis in 1934
from specimens collected at the Sumter Rock
Quarry about two miles northeast of Sumterville.
Sumter County. Florida. Also in the type lot was
a specimen collected from a limestone quarry
about a mile south of Newberry. Alachua County.
Florida. V. ocalensis was later allocated to the genus.
Exputens, and the outline of the valves is similar
to the type species, E. llajasensis. In his original
description, MacNeil mentioned the fact that the
shell of V. ocalensis could be composed of
lamellar calcite. In every specimen of V. ocalensis
we have seen, much of the original shell is
preserved, and tliis leads us to the conclusion that
TABLE 1. The stratigraphic range of Exputens
ocalensis in the Crystal River Formation of
Florida.
CLASSIFICATION OF THE CRYSTAL RIVER
FORMATION IN FLORIDA
{adopled from Puri,I957)
Vol. S7 (3)
THE NAUTILUS
73
the shell was composed nuiiiily of calcite. Except
for the Ostieidae and Pectinidae. almost all of the
other molluscs are preserved only as internal and
external molds and casts in the Crystal River
Limestone. The correct orientation of the valves is
questionable, but we are assuming that the beaks
and the small wing-like projection on the dorsal
border are located anteriorly. The location of the
beaks varies from nearly a central position to near
the anterior end of the dorsal border.
There are more than 40 specimens of Exputens
ocalensis in the collections at The Florida State
Museum, indicating that this species is not rare.
On one small piece of limestone, there are seven
right valves and some embedded double valves. At
some localities the riglit valve is much more
common; at others the reverse is true. This fact
indicates selective sorting by currents and wave
action.
Exputens ocalensis is most abundant in the
lowest zone in which it appears, Puri's (1957)
FIGS. 1, 2, 3. Exputens ocalensis (MacNeil). The
porous material showing around the shells is the
limestone matrix. Locality: Limestone quarry west
of old U. S. 441 at south edge of Kendrick,
Marion County, Florida, N. W. !4 Sec. 25, T. 14
S., R. 21 E.
FIG. 1. Left valve exterior, hypotype Florida State
Museum 3481, length 28.1 mm, height 16.6 mm.
FIG. 2. Left valve interior, hypotype Florida State
Museum 3482, length 27.4 mm, height 14.1 mm,
FIG. 3. Right valve exterior, hypotype Florida
State Museum 3483, length 25.0 mm, height 14.7
mm.
Spiroloculina newberryensis faunizone of the
Crystal River Limestone. It apparently is found
less frequently in the zone above, the Lepido-
cyclina-Pseudophragmina faunizone. It is doubtful
that E. ocalensis is found in any of the higher
zones of the Crystal River (see Table 1). The
Tethyan gastropod Gisortia harrisi Palmer seems to
have about the same stratigraphic distribution as
E. ocalensis because G. harrisi has been found at
nearly aU localities where E. ocalensis has been
reported. Thus, some Tethyan molluscs appeared
in Florida during the time that the lower part of
the Crystal River Limestone was being deposited
and after the Avon Park, Inglis, and Williston
Formations were laid down.
Exputens ocalensis has been found in the
following counties in surface outcrops in Penin-
sular Florida: Columbia, Suwannee, Dixie, Gil-
christ, Alachua, Levy, Marion, Citrus, and Sumter.
Exputens has been collected by U. S. Geological
Survey geologists in Mitchell and Dougherty Coun-
ties in southwestern Georgia in the Ocala Lime-
stone. More surprisingly, they have also collected
Exputens from the Castle Hayne Mad in Pender
and Wayne Counties, which are in southeastern
and east-central North Carolina. A specimen from
Wayne County is considerably larger than any
specimens of Exputens ocalensis from Florida and
may be a different species. At least one Tethyan
mollusc, Exputens, lived farther north during the
Late Eocene than had previously been supposed.
ACKNOWLEDGMENTS
We are particularly indebted to Mr. Druid
Wilson of the U. S. Geological Survey, who
showed the senior author specimens of Exputens
from Georgia and North Carolina. Dr. Katherine
V.W. Palmer of the Paleontologjcal Research
Institution sent the senior author a list of
localities in Florida where Exputens has been
collected.
LITERATURE CITED
Clark, B. L. 1934. A new genus and two new
species of Lamellibranchiata from the Middle
Eocene of California. Jour. Paleo. 8 (3):
270-272.
Hertlein, L. G. and L. R. Cox. 1969. Family
Malleidae. in Treatise on Invertebrate Paleon-
74 THE NAUTILUS
July 30, 1973
Vol. 87 (3)
tology (R. C. Moore, editor). Part N, Vol. I,
Mollusca 6, Bivalvia. N326-N332.
MacNeil, F. S. 1934. The pelecypod genus Vulsella
in the Ocala Limestone of Florida and its
bearing on correlation. Jour. Wasliington Acad.
Sci. 24 (10): 428-431.
Palmer, K. V.W. 1957. A new Gisorda from the
Crystal River Formation, Ocala Group, of
Florida, with explanatory notes on the Tethyan
influence in the Floridian Middle and Upper
Eocene. Jour. Palaeo. Soc. India, Lucknow. D.
N. Wadia Jubilee Number. 2: 69-72.
Palmer, K. V.W. 1967. A comparison of certain
Eocene molluscs of the Americas with those of
the western Tethys. Systematics Assoc. Pub.
No. 7. Aspects of Tethyan biogeography.
183-193.
Palmer, K. V.W. and D. C. Brann. 1965. Catalogue
of the Paleocene and Eocene Mollusca of the
southern and eastern United States. Part I.
Pelecypoda, Amphineura, Pteropoda, Scapho-
poda, and Cephalopoda. Bull. Am. Paleo. 48
(218): 1-466.
Puri, H. S. 1957. Stratigraphy and zonation of the
Ocala Group. Florida Geol. Survey. Geol. Bull.
38: 1-248.
Vokes, H. E. 1939. Molluscan faunas of the
Domengine and Arroyo Hondo Formations of
the California Eocene. Ann. New York Acad.
Sci. 38: 1-246.
RECENT PUBLICATIONS
Cheatuin, E. P. and R. W. FuUington. 1971. The
Aquatic and Land MoUusca of Texas. Pt. 1.
The Recent and Pleistocene Members of the
Gastropod Family Polygyridae in Texas ($2.50).
Pt. 2 — Pupillidae and Urocoptidae (Gastropoda)
in Texas ($4.50). Bull. 1 Dallas Museum of
Natural History, P. O. Box 26193, DaUas,
Texas, 75226. Illustrated and Useful.
Ladd, Harry S. 1972. Cenozoic Fossil MoUusks
from Western Pacific Islands; Gastropods (Turri-
teUidae Through Strombidae). U. S. Geol.
Survey Professional Paper 532, 79 pp., 20 pis.
Descriptions or citations of 174 species of 18
gastropod families from seven island groups.
Excellent.
Britton, J. C. Jr. 1972. Two New Species and a
New Subgenus of Lucinidae (Mollusca: Bivalvia),
with Notes on Certain Aspects of Lucinid
Phylogeny. Smithsonian Contributions to Zoo-
logy, no. 129, 19 pp. Liicina hendersoni n. sp.
from Antigua; Pannluciua rehderi n. sp. from
Brazil, and Radiolucina n. subgenus (type:
amiantus Dull, 1901).
Sandved,K. B. and R. Tucker Abbott. 1973. Shells
in Color. 101 pis. in color. 48 pp. accompany-
ing text; bibUography; index. Viking Press, Inc.,
625 Madison Ave., N. Y., N. Y., 10022.
$12.95. A pretty book, but over-priced.
Wriglit, C. A. 1971. Flukes and Snails. Science of
Biology Series no. 4. 168 pp. George Allen and
Unwin, Ltd., London. Hardback, about $7.50.
Biology of schistosomes and planorbid and
bulinid molluscan hosts, mainly in Africa.
Saul, Louella R. 1973. Evidence for the Origin ot
the Mactridae (Bivalvia) in the Cretaceous. Univ.
Calif. Publications in Geol. Sci., vol. 97, 51 pp.,
3 pis. $4.00.
Parenzan, Pietro. 1970. Carta d'identita delle
conchiglie del Mediterraneo. Vol. 1, Gastropodi,
283 pp., 53 pis. Bio Taras Editrice, paperback
$11.00. Useful guide, but many of the 1000
ink drawings are inadequate for identification.
Kensley, Brian. 1973. Sea-Shells of Southern
Africa - Gastropods. 236 pp., 910 species illus.,
some in color. Maskew Miller, Ltd., Cape Town.
About $17.00. Contains misidentifications,
many out-of-date genera, some wrong author
names, non-binomial names, incorrect numbers
under the illustrations and a pasted-in errata
sheet containing two obsolete names. Recom-
mend waiting for second printing.
Ocean Management, Vol. 1, no. 1. A new
international, multi-disciplinary journal dealing
with the economics and exploration of oceans.
About 500 pp. per year; quarterly. Annual U.
S. subscription, $31.00. Elsevier Scientific Jour-
nals, P. O. Box 211, Amsterdam, Netherlands.
Vol. 87 (3)
THE NAUTILUS
75
NOTES ON MOLLUSKS OSTREA AND SIPHONARIA FROM GEORGIA (U. S. A.)
John N. Kraeuter
University of Georgia Marine Institute'
Sapelo Island, Georgia 31327
ABSTRACT
The sponge-dwelling oyster Ostrea permoUis Sowerby, is now known to occur off
Georgia at 20 meters depth; and the pulmonate limpet, Siphonaria pectinata (Linne)
has been found laying eggs on tree stumps on Cabretta Island, Georgia.
Recent systematic studies have illustrated how
much is still to be learned about the marine fauna
of Georgia. Darby (1965) described 13 new species
from the 24 species of podocopid ostracods he
collected. Menzies and Frankenberg (1966) des-
cribed 1 1 new species and one new genus of
isopods among the 30 species represented in the
University of Georgia Marine Institute collections.
Malacologjsts have also reported high numbers of
new species in this area. Marcus and Marcus
(1967) described three new species and a new
subspecies from the 12 opistobranch species pre-
sent in the above collections. Merrill (1963) and
Frankenberg (1966) have reported on smaD col-
lections of moDusks off Georgia. Merrill and Petit
(1965, 1969) compiled 26 and 19 range records
for moUusks from South Carolina. They reported a
ratio of one range extension for each six species
previously reported from the area. Similar ratios
are beUeved to be found in Georgia.
Range modifications for two recently studied
species are presented: one, Ostrea permollis,
Sowerby creates a continuum where a disjunct
distribution has been suggested; the other. Siphon-
aria pectinata (Linne), extends the range of this
common intertidal pulmonate beyond its northern
Umit. This paper is preliminary to a more
thorough study of the molluscan fauna of Georgia
and is intended to alert malacologjsts to the
opportunities available through the study of the
Georgia fauna.
After examination of published records and
museum specimens, Forbes (1964) concluded that
the distribution of the oyster Ostrea permollis
Sowerby was disjunct between Molasses Reef,
Florida (25° r N, 80°23' W), in 154 m, and Cape
Fear, North Carolina (33°50' N, 78°02'40" W), in
15 ra He Beheves that the absence of its host
sponge Stelletta grubii (?) Schmidt from the
continental shelf in the South CaroUna-Florida area
has isolated O. permollis populations since at least
the Sangamon Interglacial.
The discovery of O. permollis and its host
sponge Stelletta grubii (?) in Georgia emphasizes a
continuum between the Keys (Molasses ReeO and
Cape Fear. The station locations provided by
Forbes (1964) are plotted and the two collections
from Georgia are included (Fig. 1). The Georgia
specimens of O. permollis were from 31°22'55" N,
80°52.2' W, Sta. 44 & 45, M. Gray coU., 20 m,
3/7/61, 8 live individuals, and 31°24'15" N,
80°52'35" W, J. Kraeuter, coU., 20 m, 5/23/71, 2
live individuals. These lots are on deposit in the
^^;"t-^
'Contribution No. 267 from the University of
Georgia Marine Institute.
FIG. 1. Distribution of Ostrea permollis after
Forbes (1964) with Georgia data added.
76 THE NAUTILUS
July 30, 1973
Vol. 87 (3)
collections of the University of Georgia Marine
Institute, Sapelo Island. In both cases spiculation
on the sponge fragments from the shells typify
spicules figured by de Laubenfels (1953). The
spicules measured (terminology from de Lauben-
fels, 1953):
1. Oxeas 350 - 437 ju x 10 - 21 m
2. Hagiotriane 392 - 432 m x 11.7 - 40 ^
(across head)
3. Anatriaene 392 - 422 m x 11.7 - 38 fi
(across head)
4. Eutylaster 6 - 8 /i across
5. Oxyeuaster 5 - 8 /.i across
The eutylasters were much more numerous than
the oxyeuasters and the former did not seem to
have as rough a termination as illustrated by de
Laubenfels (1953).
The presence of the host sponge and the
commensal oyster in Georgia indicates that the
lack of populations between Molasses Reef and
Cape Fear is not due to disjunct distributions, but
is due to either (1) lack of collections in offshore
waters or (2) lack of substrate for the sponge, or
(3) a combination of these factors.
The extreme narrowness of the continental shelf
near Miami obviously limits the number of
possible sites; however, submerged reefs or out-
crops have been found in North Carolina (Menzies
et al. 1966) and tliis reef is similar to those of
the Gulf of Mexico (Parker, 1956). A reef off
Georgia has been described by Hunt, Woolsey and
Henry (1971), and other reefs or "live bottom
habitats" have been listed by Struhsaker (1969)
for South Carolina, Georgia, northeast Florida and
central Rorida. It seems probable that as these
areas are sampled more extensively, fewer gaps will
exist in offshore distribution patterns.
Siphonaria pectinata, an intertidal pulmonale
limpet, has its reported northern range as eastern
Florida (Abbott, 1954) or Fernandina. Florida
(Voss, 1959). Dr. Erik Rasmussen has found it
with egg masses on tree stumps in the surf of
Cabretta Island, Georgia, adjacent to Sapelo Island.
He has been kind enougli to let me record its
northern limit and breeding during January 1972.
Tlus reproductive time is very close to that found
for the same species in south Florida by Nancy
Voss (1959). She correlated the northern limit of
S. pectinata with the 55°F isochryme on a
worldwide basis. Sapelo Island is not much beyond
the previous record of Fernandina. but the
presence here of S. pectinata suggests the northern
distributional limit may be controlled by lack of
suitable substrate on the exposed sandy shores of
the mid-Atlantic region. The large numbers and
breeding individuals found at Cabretia seem to
indicate that S. pectinata could survive even
farther north.
Historically. Dall (1927) has provided the most
conspicuous source of moUuscan daia for the
north Georgia to Florida area. In this one paper
he listed 332 species of which he considered 213
to be new. Thus, the area between 30 44" N.
79°26' W (948 m) and 30°58" N, 79°38' W (678
m) provided data which seems to be primarily
responsible for the major faunal separation at the
Georgia-north Florida boundary found by Fischer
(1961) in his analysis of diversity gradients of the
U. S. East coast. The magnitude of Dall's paper
can best be appreciated by comparing Fischer's
pelecypod and gastropod distributions. Fischer
(1961) was not able to demonstrate a clear, faunal
discontinuity of pelecypods in the north
Florida-Georgia area. It appears from his data,
however, that perhaps ten species have their
northern latitudinal limits at this point. Converse-
ly, the gastropods have approximately 160 species
reaching their northern latitudinal limits at the
Georgia-Florida boundary - a clear faunal break.
DalFs paper listed only 41 pelecypods, four new
species, but he catalogued 277 gastropod species
of which 200 were new. It appears that the
gradual loss of species with latitude as described
by Fischer (1961) for the lamellibranchs may
come closer to distributional reality than that of
the sharp zoogeographic boundary illustrated by
the Gastropoda.
The obvious influence of one major work such
as Dall's and the records of Ostrea permollis and
Siphonaria pectinata demonstrate the need for
more thorougli ecologjc and systematic work in
the Georgia-north Florida area. The importance of
hard substrates as limiting factors in marine
distributional patterns along the East coast of the
United States is also emphasized.
The critical reading and suggestions given by
Drs. Dirk Frankenberg and William Shaw are
gratefully acknowledged.
Vol. 87 (3)
THE NAUTILUS
77
LITERATURE CITED
Abbott, R. T. 1954. American Seashells. D. Van
Nostiand Co., Inc., New York, 541 pp.
Dall, W. H. 1927. Small shells from dredgings off
the southeast coast of the United States by the
United States fisheries steamer "Albatross" in
1885 and 1886. Proc. U. S. Nat. Mus. 74(18);
1-134.
de Laubenfels, M. W. 1953. Sponges from the
Gulf of Mexico. Bull. Mar. Sci. Gulf and
Caribbean 2(3): 511-557.
Darby, D. G. 1965. Ecology and taxonomy of
Ostracoda in the vicinity of Sapelo Island,
Georgia. National Science Foundation project
GB-26. Report No. 2, 59 pp. University of
Michigan.
Fischer. A. G. 1961. Latitudinal variations in
organic diversity. Amer. Sci. 49: 50-75.
Forbes, M. L. 1964. Distribution of the commen-
sal oyster, Ostrea pennollis, and its host sponge.
Bull. Mar. Sci. Gulf and Caribbean 14(3):
453-464.
Frankenberg, D. 1966. Southern limit oi Nassariits
trivittatus. The Nautilus 79(3): 89-90.'
Hunt. J. L, Jr., J. R. Woolsey. Jr. and V. J.
Henry, Jr. 1971. Geological investigation of a
submerged reef off Sapelo Island, Georgia.
Abstract Volume, Second National Coastal and
Shallow Water Research Conference, 268 pp.
Marcus, E. and E. Marcus. 1967. Some opistho-
branchs from Sapelo Island, Georgia, U. S. A.
Malacologia 6(1-2): 199-222.
Menzies, R. J. and D. Frankenberg. 1966. Hand-
book on the common marine isopod Crustacea
of Georgia. University of Georgia Press, 93 pp.
Menzies, R. T., O. H. Pilkey, B. W. Blackwelder,
D. Dexter, P. Huling and L. McCloskey. 1966.
A submerged reef off North Carolina. Int. Rev.
ges. Hydrobiol. 51(3): 393-431.
Merrill, A, S. 1963. Mollusks from a buoy off
-Georgia. The NautUus 77(2): 68-70.
Merrill, A. S. and R. E. Petit. 1965. Mollusks new
to South Carohna. The Nautilus 79(2): 58-66.
Merrill, A. S.' and R. E. Petit. 1969. Mollusks new
to South Carohna: II. The Nautilus 82(4):
117-122.
Parker, R. H. and 1. R. Curray. 1956. Fauna and
bathymetry of banks on the continental shelf,
northwest Gulf of Mexico. Bull. Amer. Assoc.
Petrol. Geol. 40: 2428-2439.
Struhsaker, P. 1969. Demersal fish resources:
Composition, distribution, and commercial
potential of the continental shelf stocks off
southeastern United States. Fishery Industrial
Res. 4(7): 261-300.
Voss, N. A. 1959. Studies on the pulmonate
gastropod Siphonaria pectinata (Linnaeus) from
the southeast coast of Florida. Bull. Mar. Sci.
Gulf and Caribbean 9(1): 84-99.
BOOK REVIEW
A SMELLER'S DIRECTORY of Clubs, Books,
Periodicals, and Dealers. By Ton} Rice. Third
Edition, 1 9 72. 64 pp. , paperback. Of Sea and
Shore Publications, P. O. Box 33, Port Gamble,
Wash. 98364. $L00.
There is no handier guide to shell dealers, shell
clubs and popular literature than this greatly im-
proved and neatly printed booklet. 88 shell clubs
are listed, including some new ones, such as the
Whitsunday SheU Club (of Queensland) and the
Wilmington Shell Club of Delaware. There is an
imposing list of shell and book dealers, and a useful
and complete list of periodicals dealing with mol-
lusks.
R. Tucker Abbott
Delaware Museum of Natural History
78 THE NAUTILUS
July 30, 1973
Vol. 87 (3)
BOOK REVIEW
THE MOLLUSKS OF THE ARID SOUTHWEST
WITH AN ARIZONA CHECK LIST. By Joseph
C. Bequaert and Walter B. Miller. Tucson:
University of Arizona Press, pp. 271, maps.
$8.00.
A seasoned veteran wise in the ways of
traditional systematics and a younger well-versed in
newer techniques of study have combined to
summarize the mollusks of an important faunal
area where both have had extensive field experi-
ence. The result is a massive, but somewhat
disappointing, compilation of literature citations
and locality records. This book will be a fun-
damental information source for all who are
interested in the molluscan fauna of the arid
southwestern United States. Wlien combined with
the descriptions and illustrations in Pilsbry's
1939-1948 "Land Mollusca of North America",
the student of this region now has better
bibliograpliic and identification tools than for any
equivalent area of the United States.
The book presents first a general zoogeographic
analysis, then a species by species analysis of
distribution for the terrestrial species, and con-
cludes with an annotated check list of the Arizona
land and fresh water moUusks. The last two
sections contain very extensive duplication of data
and could have been condensed to good effect.
The locality lists give no clear indication in most
cases as to whether the cited record is based on
literature compilation or previously unreported
material.
Throughout the book there are many changes
proposed in synonymy and species limits. The
changes in Sonorella are taken from Miller's
unpublished thesis, while those proposed in other
genera generally are not documented. It is quite
useful to know the opinion of the authors
concerning the rank and relationships of the many
named forms in such genera as Ashmunella,
Holospira, Gastrocopta, Oiaenaxis and Vertigo, but
presentation of their evidence for changes would
have been preferable.
In the systematic portion of this work there
seems to be only a few errors and omissions.
Work in Europe indicafing the presence of sibling
species or species complexes in such groups as
Cionella, Pupilla, Columella and Vertigo, has not
been alluded to in their discussions. This is an
important omission, since "circumpolar" represen-
tatives of these genera occur in Arizona. The
section on foreign desert dwellers (pp. 98-102) is
cursory. The genus Sculptaria is misclassified in
the Endodontidae rather than the Corillidae. More
important, the Australian bulimulid Bothriembryon
is called a desert genus, while in reality it is
characteristic of the at least seasonally moist
forested areas of Southwest Australia.
The most disappointing portion of the book is
the discussion on zoogeography. It is concerned
with the classic and rather sterile problem of
delimiting faunal area boundaries (pp. 7-10) and
descriptive spatial accounts of each species (pp.
14-98). It accepts as axiomatic the now generally
discredited idea that the center of diversity for a
genus represents its center of origin (p. 20).
Dynamic aspects of biogeography are virtually
ignored, with a discussion of Sonorella (p. 21)
talking of "genetic drift" and "invasion of new
territory", whereas the area involved apparently
still is undergoing progressive drying. Consequent
restriction of ranges and increased colony isolation
is a more probably recent history. Despite the
advances in theoretical and experimental biogeog-
raphy in recent years, questions of species diver-
sity and species-area relationships are not dis-
cussed, although the mollusk-inhabited mountains
of Arizona form ideal "islands" in a zoogeograpltic
sense.
In summary, the authors are to be congrat-
ulated on producing an encyclopaedic work of
great usefulness. I shall make continual reference
to it. Unfortunately, it is not the significant work
in terms of new ideas or syntlieses that could have
been hoped for from the niixing of diverse talents.
That it is a mix and not a blend can be inferred
from divergent views of shell versus anatomy. On
page 1 5, the absence of generic or specific shell
characters is called exceptional, while on page 100
the shell is called untrustworthy for generic or
even family placement. Given the difficulties of
mollusk collecting in Arizona and the massive data
gathering needed to produce the present volume, it
is perhaps unfair of me to want something more
than usefulness.
Alan Solem, Curator of Invertebrates
Field Museum of Natural History
Chicago, Illinois 60605
Vol. 87 (3)
THE NAUTILUS
79
OBSERVATIONS BY POLARIZED LIGHT ON THE RADULA OF
APLEXA MARMORATA
Maria Luiza S. Mello and Mariene T. Ueta
Institute de Biologia, Universidade Estadual de Campinas,
13100 Campinas, Sao Paula, Brazil
INTRODUCTION
Many ultrastructural aspects of mollusc radulae
have been recently pointed out by scanning
electron microscope studies (Runliam, 1969;
Thomas, 1971; Kohn et al., 1972). However,
nothing concerned with the organizational state of
the macromolecules which make up the radula
teeth has been ytt estabhshed.
In the present paper observations with polarized
light were performed in radulae subjected to some
special histochemical procedures as an approach to
the discovery of the molecular arrangement of the
structure.
MATERIAL AND METHODS
Specimens of Aplexa marmorata (Guilding,
1828) (Pulmonata, Physidae) were collected in a
small artificial tank of a country house in
Campinas, Sab Paulo, BrazU. The animals were
killed in hot water (nearly 70°C), removed from
their shells, fixed in 70% ethanol and dissected.
After being extracted from their bulbs, some
radulae were treated with a 10% KOH aqueous
solution for 24 hours. They were washed, stained,
dehydrated in ethanol and mounted in Canada
balsam.
The following staining solutions were used: 1.
Congo Red saturated solution in 96% ethanol
(Barth, 1958); 2. Orange G saturated solution in
70% ethanol (Barth, 1958); 3. Xylidine-Ponceau at
pH 1.7 (Vidal, 1972); 4. Toluidine Blue at pH 4.0
(Uson, 1960).
At least five radulae were subjected to each
staining procedure.
The investigation of anisotropic properties was
carried out with a Zeiss Pol-photomicroscope
equipped with a MPM photometer and an EMI
6256 photomultipher. Histophotometric readings
were performed in different regions of the teeth
of the 1st and 2nd distal rows, oriented paraUel
(d||) and perpendicular (djj to the plane of
polarized light. A Plan 40/0.65 objective, 2.0
optovar, lOx projection lens and 2mm measuring
diaphragm were used; the area of the specimen
measured corresponds to a 2.5 /n diameter. Differ-
ent wavelengths were provided by a Zeiss mono-
chromator ruler.
The wavelength of the absorption peak was
determined for each set of measurements at the
visible spectrum. Maxima of linear dichroism (=Ad
= d|| - dj) and diochroic ratios (d||/dj) were also
calculated.
The dispersion of the birefringence (DB) was
investigated in the same material by determining
the optical path differences at several wavelengths
with a rotatory analyser and a X/4 compensator,
according to Senarmont's methods.
RESULTS
The teeth stained strongly with Congo Red and
Xylidine-Ponceau and slightly with Orange G and
Toluidine Blue.
Anisotropic phenomena are found after staining
on the basal portion of the teeth (prop and region
A) and on the denticular region (B) (Fig. 2, 3, 6,
7 and 8; Table I). Some aspects of the linear
dichroism (selective absorption of the polarized
hght) and birefringence are shown in Figures 1 to
10. The absorption values are larger when the
different regions analysed are placed parallel to the
plane of polarized light (positive dichroism), ex-
cept when the radula is stained with Toluidine
Blue (negative dichroism). When Orange G is used
as staining solution the dichroism (Ad) is very
weak and only found at the region B (Table I).
The anisotropical properties are usually less
evident at the prop region (Fig. 3 and 7).
Tlie dichroism is stronger in teeth stained with
Congo Red (Fig. 2, 3, 4 and 5; Table I) and in
this case the radicular membrane also stains red
and displays birefringence.
DB curves were determined but they did not
show inflection points within the X range used
under present experimental conditions. However,
when the radula is stained with Xylidine-Ponceau
the compensated image remains unchanged in
80 THE NAUTILUS
July 30, 1973
Vol. 87 (3)
directions NE-SO and NO-SE at wavelengths lower
than 520nm (Fig. 1 1 - dotted line).
The dichroism and birefringence values are
slightly decreased in KOH-untreated radulae.
DISCUSSION
Optical properties such as those observed in the
present work (dichroism and birefringence) indicate
that there are oriented macromolecules in the
teeth of Aplexa mannorata suitable to bind the
dyes (Congo Red. Xylidine-Ponceau and Toluidine
Blue) in a preferential way and that this level of
molecular orientation can be measured. However,
from the fact that a precise inflection point has
not been found in the DB curves, it can be
considered that there is a very complex organiza-
tion of the stained molecules in the teeth, yeilding
inner compensations and a background effect
which would also account for the low dichroism
values. Mollusc radulae have been reported by
FIG. I. A radula stained with Congo Red (5Wnmj. x 48
FIG. 2 and 3. Details from Fig. 1. The tooth region A is oriented parallel (Fig.
3) to the plane of polarized light, x 480
FIGS. 4 and 5. Idem Fig. 2 and 3 (5l0nmj. x 185
1j and perpendicular (Fig.
Vol. 87 (3)
THE NAUTILUS
81
many authors as being composed of cliitin;
however other components are probably found in
the teeth because they stain with Xyhdine-Ponceau
at pH 1.7 and Orange G which usually attach to
protein radicals and also with Toluidine Blue
wliich generally shows dichroism when bound to
oriented polyanion substrates. Congo Red also
binds to mucins (Conn, 1967). These data suggest
that the stained substrate is probably a muco-
protein.
The staining sliglitly increases after the KOH
treatment indicating that it functions as a definite
saponification, liberating the anionic groups of the
polyanion and allowing them to become reactive.
This treatment, in addition, does not remove these
groups from their structural complex.
Present data can be considered as a starting
point for further demonstration of differences as a
function of several physiological states in the
teeth. Preliminary observations point out differ-
ences of birefringence intensity and dichroism
between the apical and basal zones of the radula,
which would mean decreasing orientation of the
macromolecules as the teeth become older and
worn.
FIG. 6. KOH-untreated radula stained with Orange G and observed with crossed polarizer and analyser, x
480
FIG. 7. The analyser was turned for compensation of region B. x 480 P = prop
FIG. 8. Compensation of the region A and of the denticles (arrow), x 480
FIG. 9. Congo Red-stained radula as seen with crossed analyser and polarizer, x 500. d = denticles
FIG. 10. Idem Fig. 9. Arrow indicates birefringence at the prop region, x 250
THE NAUTILUS
July 30, 1973
Vol. 87 (3)
TABLE 1. Polarized light extinction values and dichroism data at the wavelengths of the peaks of the absorption
curves (number of measurements = 5).
ACKNOWLEDGM ENTS
Authors are indebted to Dr. J. L. Moreira Leme
(Museu de Zoologia, Univ. S. Paulo) for the
identification of the specimens.
LITERATURE CITED
Barth, R. 1958. Metodos usados em micro-
anatomiae histologia entomologjca. Mem. Inst.
Oswaldo Cruz 56: 453-471.
Conn, H. J. 1967. Stains and staining. In Mc-
Clung's Handbook of Microscopical Technique.
Hafner Publ. Co., N. Y., pp. 72-111.
Kohn, A. J., J. W. Nybakken and J.-J. Van Mol.
1972. Radula Tooth Structure of the Gastropod
Conus imperialis Elucidated by Scanning Elec-
tron Microscopy. Science 176: 49-51.
Lison, L. 1960. Histochimie et Cytochimie Ani-
males. Paris, Gauthier-Villars.
Runhani, N. W. 1969. The use of the scanning
electron microscope in the study of the gastro-
pod radula: the radulae of Agriolimax reticu-
latus and Nucella lapillus. Malacologia 9:
179-185.
Tliomas, R. F. 1971. A scanning electron micro-
scope study of the marginal teeth of Nerita
peloronta Linnaeus. Tlie Nautilus 84: 118-119.
Vidal, B. C. 1970. Dichroism in Collagen Bundles
Stained with Xylidine-Ponceau 2R. Ann. His-
toch. 15: 289-296.
FIG. 1 1 . Curves of the dispersion of the birefringence.
P = optical path differences (nm)
Vol. 87 (3)
THE NAUTILUS
83
A NEW RECORD FOR LIGUUS: THE BOYNTON BEACH COLONY
Alan K. Craig
Department of Geography
Florida Atlantic University
Boca Raton. Florida 33432
ABSTRACT
A new and disjunct northern range limit for Liguus fasciatus has been found at
Boynton Beach, Florida. Coloration indicates affinity with extinct adjacent
populations extending southward to Ft. Lauderdale. The relict beach ridge hammock
habitat is highly restricted and destined to be destroyed.
A surprising occurrence of Liguus fasciatus in a
remnant of beach ridge hammock was noted by
university personnel in 1970 in conjuction with
routine botanical studies at Boynton Beach, Flor-
ida. Subsequent investigation by the writer has
confirmed the presence of a small colony existing
at the northernmost limit of range under some
interesting conditions not previously reported by
earlier contributors such as Moore (1921), Pilsbry
(1912. 1946). Rhoads (1899). Simpson (1921.
1922), and Young (1960).
From historic accounts (Pierce: 1970) we know
tropical hammock vegetation formerly extended in
a narrow, almost unbroken band along the crest of
beach ridges formed between Ft. Lauderdale and
Lake Worth. Further northward hammock vegeta-
tion was displaced by a more xeric dune cover
consisting of Caribbean pine and palmetto. This
habitat effectively precluded any diffusion of
Liguus in that direction. Mangrove forests and the
sawgrass environment of the Everglades created an
impassable western boundary for these arboreal
snails.
Intense real estate development has destroyed
almost every vestige of beach ridge hammock in
southeast Florida. The only example remaining
survives in an inconspicuous strip (400 x 50 yds.)
crowded between U. S. Highway AlA and the
Atlantic Ocean (Fig. 1). Thousands of residents
and tourists daily pass by this relict habitat as
they travel the busy highway or visit the public
beach.
The Boynton Beach hammock has developed a
canopy 30-40 feet in height dominated by mature
gumbo limbo, ficus, and seagrape. Many trees
show marked wind shear in response to the
prevailing southeast tradevwnd. In addition, a
survey by Austin (1972) has shown the presehce
of the plants indicated in Table 1. Trees from this
group are commonly encountered in a very mature
state, with many signs of storm damage and
general senility. The hollow trunks, cavities and
other damaged areas provide abundant estivation
sites for the Liguus colony. Shading by the upper
storey effectively precludes the growth of most
under storey plants althougli a rather conspicuous
layer of leaf mould and litter has accumulated
over much of the hammock floor.
A careful analysis of the vegetation indicates
that it has been moderately to severely disturbed
in the southern half of the hammock so that
conditions approaching a natural equilibrium state
are restricted largely to the northern half -
amounting to little more than 10.000 sq. yds.
total area. The Liguus population is further
concentrated in a protected microhabitat situated
to the leeward of the seagrape stand that occupies
the beach ridge crest.
On penetrating the hammock the abundance of
empty shells of the carnivorous Euglandina rosea is
FIG. 1. Interior of the Boynton Beach Hammock.
84 THE NAUTILUS July 30, 1973
TABLE 1. Important botanical components of the Boynton Beach Hammock.
Vol. 87 (3)
Cenchnis tribuloides
Sabal palmetto
Serenoa repens
Smilax bona-nox
Coccoloba uvifera
Yucca aloifolia
Agave decipiens
Hymenocalis latifolia
Salix caroliniana
Ficus aiirea
Nectandra coriacea
Capparis cynophallophora
Capparis flexuosa
*Forestiem segregata
Chiococca alba
Chrysobalaniis icaco
Caesalpinia bonduc
* - trees frequented by Ligiius
Source: Austin and Weise (1972)
Dalbergia ecastophyllum
Pithecellobium keyense
*Zanthoxylum fagara
Simarouba glauca
*Bursera simaruba
Cnidoscolus stimulosus
Croton punctatus
*Metopium toxiferum
Schinus terebinthifolius
Toxicodendron radicans
Knigiodendron ferreum
Eugenia axillaris
Eugenia myrtoides
Ardisia escallonioides
*Mastichodendron foetidissium
Psvchotria nen'osa
immediately noticeable. This strictly terrestrial
snail is the control predator for the arboreal
Ligiais. One has the impression that any Liguus
unfortunate enough to be blown from a tree
branch probably has little chance of returning to
safety if it should fall more than a few feet from
a tree trunk. A thorough search of the Boynton
hammock has not revealed other terrestrial snails
of substantial size that would provide suitable prey
for E. rosea so I conclude that it subsists almost
exclusively upon Liguus. Both animals are basically
nocturnal and predation has not been witnessed by
the writer although it has been reported elsewhere.
It is possible that land crabs constitute another
significant predator. Their burrows are present in
low areas of the hammock and some Z./,gwi/x shells
have been noted with damage suggestive of
pincers.
Specimens of Liguus from the Boynton Beach
hammock have certain physical characteristics that
may be especially significant. Adults are often
quite elongate (40 mm x 15 mm), exceptionally
thin-shcUed, and higlily porcellaneous on both
interior and exterior surfaces. Adult coloration
consists of two or more broad golden bands with
narrow orange borders on a white background.
These colors usually disappear beyond the penul-
timate whorl. Many specimens disclose an affinity
with the variety L. fasciatus septentrionalis (Pils.),
having three or four fine olivaceous lines super-
imposed on the gold bands. Althougli coloration as
described is not duplicated by Liguus from other
locations, we can reasonably assume that a
gradation toward olive on white formerly existed
in what was once a continuous population extend-
ing southward to Ft. Lauderdale. However, the
majority of dead shells collected from the ground
are weathered to a dull white and often much
broken.
Juveniles of a different type appear frequently.
These specimens are relatively robust and
thick-shelled. Coloration is largely brownish fiames
similar to L. marmoratus but no adults with this
coloration have been seen. If L. marmoratus does
prove to exist in the hammock together with L.
fasciatus a problem in distribution exists since the
former subspecies was never found in hummocks
to the south at Yamato, Pompano, and Ft.
Lauderdale according to Pilsbry (1946:102). Con-
sequently its disjunct presence at the extreme
northern limit of the range under natural circum-
stances seems quite unlikely. However, artificial
Vol. 87 (3)
THE NAUTILUS
85
implantation of this relatively common variety by
some well-meaning conservationist in the past is a
likely explanation. The possibility of aboriginal
involvement must not be excluded as there is
some indirect evidence of Indian presence in the
hammock.
Having found Ligiius in the densely populated
locale of Boynton Beach, further efforts were
made to seek it in some of the previously known
localities listed above by Pilsbry and indicated on
his earlier (1912) map. In every case the former
hammock habitat was completely destroyed. The
search was extended to the inland oak-palmetto
hammocks but these likewise proved barren.
Survival of Liguus in the Boynton hammock is
not by mere accident (that is, beyond preservation
of the hammock itself). Nearness to the sea with
its ameliorating effect on winter temperatures is an
obvious advantage to these cold-sensitive animals.
Higli relative humidity fosters the growth of
epiphytic algae and fungi providing abundant
forage for tree snails (see Craig 1972 for details).
Beach ridge substrate material along this part of
the southeastern Florida coast is surprisingly
siliceous (Craig et al: 1969), whereas Liguus are
known to prefer habitats having a rocky, calca-
reous substrate. In fact, the survival of a Liguus
colony in an area not having a well-indurated
substrate is difficult to demonstrate (with the
possible exception of the Cape Sable area).
Initially this lack of a rocky floor appeared to be
an anomaly of the Boynton Beach site but in the
course of investigation an outcrop of calcareous
beach ridge rock was found along part of the
western side of the hammock. Case-hardening
(secondary cementation) of this strata may have a
subtle effect on plant food intake of the vegeta-
tion and thus be reflected in the shell structure of
the tree snails.
At the time this account was being written
(Dec, 1971) the Boynton Beach hammock was
still intact. It is, however, an extremely valuable
tract from the real estate viewpoint and privately
owned. Preservation of this unique site to date
apparently is due to temporary lack of develop-
ment funds as construction of a large multi-storied
residential building was announced several years
ago.
It is unfortunate indeed that no organized
effort has been made to save this last remnant of
the primeval landscape for the benefit of future
generations who can never know the splendid
beauty of this forest once it is gone forever.
LITERATURE CITED
Austin, D. F. and J. G. Weise 1972. Annotated
checklist of the Boynton Beach Hammock.
Jour. Florida Acad. Sci. 35.
Craig, A. K. 1972. Observations on the arboreal
snail Orthalicus floridemis. Jour. Florida Acad.
Sci. 35(1): 15-20.
Craig, A. K., S. Dobkin, R. B. Grimm and J. B.
Davidson 1969. The gastropod Siphonaria pecti-
nata: a factor in destruction of beach rock.
Amer. Zool. 9(3, ed. 2): 895-901.
Moore, C. B. 1921. Liguus at Marco, Florida. The
NautUus 34: 139-140.
Pierce, C. W. 1970. Pioneer life in Southeast
Florida. Univ. Miami Press, Coral Gables, Flor-
ida. 1-264.
Pilsbry, H. A. 1912. A study of the variation and
zoogeography of Liguus in Florida. Jour. Acad.
Nat. Sci. Philadelphia 15: 429-471.
Pilsbry, H. A. 1946. Land mollusca of North
America (north of Mexico) Acad. Nat. Sci.
Phil., PhOadelphia, Pennsylvania. 2(1): 1-520.
Rlioads, S. N. 1899. Annotated list of land and
fresh-water shells recently coUected in the
vicinity of Miami, Florida. The Nautilus 13:
43-47.
Simpson, C. T. 1921. Florida West Coast Liguus.
The Nautilus 35: 66-73.
Simpson, C. T. 1922. A Search for Liguus. The
Nautilus 35: 66-73.
Simpson, C. T. 1929. The Florida Tree snails of
the genus Liguus * Proc. U. S. Nat. Mus.
73(Art.30): 1-44.
Young, F. N. 1960. Color pattern variations
among snails of the genus Liguus on the
Florida Keys. Bull. Fla. St. Mus. 5: 259-266.
86
THE NAUTILUS
July 30, 1973
Vol. 87 (3)
PISIDIUM HENSLOWANUM (SHEPPARD) IN WESTERN CANADA
Stuart A. Harris
Department of Geography
The University of Calgary, 2920 24 Ave., N.W.
Calgary, Alberta, Canada T2N1N4
ABSTRACT
New localities of Pisidium henslowanum (Sheppardj are recorded for Alberta,
British Columbia, the North-West Territories and Ontario. This species is found in
snwll numbers in boreal North America where there are alkaline oligotrophic to
somewhat entrophic waters of low to moderate salinity. Since it also occurs in
post-glacial alluvial deposits over 7000 years old, it does not appear to be
introduced species.
Collections of freshwater mollusca by the writer
from Western Canada between 1970 and 1972
have frequently yielded valves identical to Pisidium
henslowanum (Sheppard) as described by Herring-
ton (1962). Although it has been found in the
Upper Pliocene and Early Pleistocene of Idaho (U.
S. Geological Survey in Herrington, 1962, p. 41),
Herrington (loc. cit.) has concluded that "this
species appears to be introduced." Accordingly, it
would seem appropriate to list the new occur-
rences, and re-examine this conclusion. The mate-
rial is in the collection of the author and a
sampling in the Delaware Museum of Natural
History, Greenville, Delaware.
NEW LOCALITIES
Alberta
Cardinal Lake, near Peace River; ponds between
Cochrane and Calgary; Crimson Lake, near Rocky
Mountain House; Elkwater Lake, 26 iniles
south-east of Medicine Hat; Gull Lake, 10 iniles
north of Red Deer; beaver pond on Lusk creek
along the Kananaskis road, 3 miles south of Seebe;
Ma-me-o beach. Pigeon Lake, 40 miles south of
Edmonton; Vermilion Lakes at Banff; pond,
one-quarter mile inside Waterton National Park;
Lake Winnegami, near Peace River (also form
supiuum).
It is also known from the post-glacial alluvial
deposits of the area around the Porcupine Hille
(Harris and Pip. 1973).
British Columbia
Altrude Lake, Vermilion Pass, Kootenay Nation-
al Park; Lake Columbia at Canal Flats; Dog Lake,
Kootenay National Park; Kootenay Lake.
Manitoba
Lynch 's Pt., Lake Manitoba.
North West Territories:
Great Slave Lake at Hay River; latitude 63°9'
N., and longitude 122° 14' W. in terrace deposits
above the MacKenzie River. The last two samples
were collected by A. N. Boydell.
Ontario
Lake Bancroft, at Bancroft; Lake Ontario at
Hamilton.
GEOGRAPHICAL RANGE
Wlien these localities are added to those listed
by Herrington (loc. cit.), and Sterki (1916), it is
clear the Pisidium henslowanum is a fairly wide-
spread boreal species ranging from the north-east
United States almost to the Arctic Circle. It is
never very abundant since it composed 3-13% of
the valves collected at any particular site. Unless a
large collection, say, 100 valves is made, it could
easily be missed.
HABITAT AND ECOLOGY
Contrary to the statements in Herrington, this
species occurs in ponds (e.g. at Waterton), in
creeks (e.g. Lusk Creek, Kananaskis) and in small
lakes (e.g., Altrude Lake, Lake Bancroft, Cardinal
Lake and Dog Lake) in North America. The fact
that it occurs in post-glacial, alluvium beneath
Vol. 87 (3)
THE NAUTILUS
87
Mazamash (7000 years B.P.) agrees willi this
interpretation and suggests that it was hving in tire
area long before Emopean man set foot on this
continent.
The range of water quality noted so far is pH
7.2-9.4; 91-142 alkalinity (CaCO^ mg/litre): total
hardness 101-179 (CaCO^ mg/htre) 138-797 ppm.
dissolved salts; dissolved oxygen 7.7-13.4 ppm;
bicarbonate 1.97-11.06 meq. /litres; chloride
0.02-3.00 meq./litre; nitrate 0.09-0.24 meq./litre;
sulphate 0.02-1.25 meq./litre; phosphate 0.004-0.07
meq./litre; potassium 0.01-0.51 meq./litre; mag-
nesium 0.58-14.17 meq./litre; calcium 0.50-2.87
meq./litre; and sodium 0.08-8.70 meq./litre. Thus
it favors alkaline waters of low-moderate salinity
in zones of calcareous soil and rock. The water
may be oligotrophic to somewhat entrophic and
is normally characterized by dominance of the
bicarbonate anion. Since it occurs in Lake Mani-
toba, it may also survive where sulphate ions are
fairly abundant.
Presumably, this explains why it has not been
reported from the extremely low salinity waters of
central British Columbia and parts of the shield of
Northern Ontario. It has yet to be found in the
waters with higlier salinities in the south-central
Prairie Provinces.
LITERATURE CITED
Harris, S. A., and Pip, E., 1973. MoUusca as a
means of determining late and post-glacial
climatic history in Alberta. Can. Jour. Zool. in
press.
Herrington, H. B., 1962. A revision of the
Sphaeriidae of North America (Mollusca: Pelecy-
poda). Museum of Zool; Univ. of Michigan
Misc. Paper No. 118, 74 pp.
Sterki, V., 1916. A preliminary catalogue of the
North American Sphaeriidae. Ann, Carnegie
Mus., 10 {%). pp. 429-74.
CORBICULA IN SAN FRANCISCO, CALIFORNIA
James T. Carlton
California Academy of Sciences
San Francisco, California 94118
Living specimens of the introduced Asiatic
Clam, Corbicula manilensis (Philippi, 1 844) (the
same as C. fluminea of authors), were collected on
February 24, 1973, from Stow Lake, a small,
shallow, artificial body of water in Golden Gate
Park, San Francisco, California. While Corbicula is
well-known from the Sacramento-San Joaquin Del-
ta of central California (and especially in the
Delta-Mendota Canal), as well as from the South
Bay Aqueduct, this is the first record of this
exotic clam on the San Francisco Peninsula. Only
two living specimens were found (measuring ap-
proximately 17.2 mm and 17.6 mm in length.
indicating an age of perhaps one and a half years),
but several dead and smaller valves (the smallest
8.5 mm in length) collected at the same time
suggest the presence of a reproducing population.
The largest dead valve measures approximately
21.7 mm in length. Tlie clams were found in
about 12 inches of water on a muddy substrate,
along the southeastern shore of the lake. The
presence in large numbers of the native mussel,
Anodonta wahlamctensis Lea, 1838, in Stow Lake
may provide an opportunity for students to study
the effects of the introduction of Corbicula on the
mussel population.
THE NAUTILUS
July 30, 1973
Vol. 87 (3)
CYCLOSTREMELLA. A PLANISPIRAL
PYRAMIDELLID
Robert Robertson
Academy of Natural Sciences
Philadelphia, Pennsylvania 19103
The genus Cyclostremella Bush (1897) was
originally placed in the family Vitrinellidae. Tliiele
(1929) ranked it as a doubtful subgenus of
Daronia A. Adams in the subfamily Skeneinae
(family Trochidae). Defining it conchologically.
Donald R. Moore (1966) has proposed the family
Cyclostremellidae. One character setting it apart
from vitrinellids, trochaceans and most other proso-
branchs (except mathildids and architectonicids) is
its hyperstrophic protoconch.
The type-species of Cyclostremella (by original
designation) is C. humilis Bush (1897) which is
probably the most abundant minute gastropod on
the Texas coast, although rarely collected alive
(Ode, 1966-1968; Boone, 1969). Mrs. Constance
(Mollis Q.) Boone of Houston has kindly sent me
two living specimens which she found among
polychaete tubes washed ashore at Bryan Beach,
Freeport, Texas, on November 26, 1972.
Tlie external body morphology closely resem-
bles that of the five species of east American
odostomias (sensu late) with which I am familiar;
the resemblance to Odostomia dianthophila Wells
& Wells is particularly close. The pair of purplish
black eyes is posteromedian to the base of the
fairly short tentacles. (Bush also observed that
"two large black eyes [are] close together on the
top of the head"). The tentacles are ciliated and
concave ventrolaterally; the cilia near the tip are
longer than the others. A narrow mentum is
present and this can extend beyond the anterior
end of the foot, which is slightly cleft medially.
The operculum is as described and illustrated by
Bush and Moore. Behind the head there is some
grey speckling. A shallow anal sinus is present
both on the shell and the mantle edge. The
pigmented mantle organ ('? hypobranchial gland) is
greenish white anteriorly and briglit yellow and
brown to the posterior and right. All these
characters are in accord with the European
pyraniidellids studied by Fretter and Graham
(1949).
For final proofs of the pyramidellid nature of
Cyclostremella I squashed each animal under a
cover slip. No radula is present (Bush had been
unable to find one either). Instead there is an
elongate buccal stylet together with an oral sucker
at the tip of a long acrembolic proboscis (deeply
inverted in the specimens studied). C humilis is
hermaphroditic: both oocytes and spermatozoa
were observed in the gonad of one of the
specimens. The spermatozoa are long-tailed and
have corkscrew-shaped heads that are like those of
the pyramidellid described and figured by Franzen
(1955, fig. 84). Such spermatozoa are unknown
among prosobranchs (ibid., pp. 449-450).
No other known pyramidellid approaches Cyclo-
stremella in shell shape. Thus spire height per se
is not a good familial character. With its low spire,
Cyclostremella is convergent with the Architec-
tonicidae which have, however, much larger proto-
conchs (those of C humilis are only 0.28 mm in
diameter) and differ conchologically in other ways
too.
LITERATURE CITED
Boone, C. 1969. Bring 'em back alive. Texas
Conchologist 5(8): 85.
Bush, K. J. 1897. Revision of the marine
gastropods referred to Cyclostrema, Adeorbis,
Vitrinella. and related genera; with descriptions
of some new genera and species belonging to
the Atlantic fauna of America. Trans. Con-
necticut Acad. Sci. 10(3): 97-144. 10 figs., pis.
22-23.
Franzen, A. 1955. Comparative morphological
investigations into the spermiogenesis among
Mollusca. Zoologjska Bidrag fran Uppsala 30:
399-456. 146 figs., 2 pis., 2 tables.
Fretter, V. and A. Graham. 1949. The structure
and mode of life of the Pyramidellidae, para-
sitic opisthobranchs. Jour. Mar. Biol. Assoc.
United Kingdom [ser. 2] 28: 493-532. 12 figs.
Moore, D. R. 1966. The Cyclostremellidae, a new
family of prosobranch moUusks. Bull. Mar. Sci.
16(3): 480-484. 6 figs.
Ode, H. 1966. Relative abundance of shells at
Galveston. Texas Conchologist 2 (6): [8].
Ode, H. 1967. Some Galveston records of new and
unusual shells. Texas Conchologist 3(9): [6-8]
Ode, H, 1968. Cyclostremella humilis Bush 1897.
Texas Conchologist 5(4): 38-39, 1 fig.
Thiele, J. 1929. Handbuch der systematischen-
Wcichtierkunde. Jena: Fischer 1(1): 1-376, 470
figs.
Vol. 87 (3)
THE NAUTILUS
89
OBITUARY
G. Bruce Campbell, M.D.
(1934-1973)
G. Bruce Campbell was born October 14, 1934,
at Wichita, Kansas, and died suddenly, February
28, 1973, at Victorville, California. He graduated
from the school of medicine, Loma Linda Univer-
sity, in 1959, at the top of his class, and interned
at the Glendale Adventist Hospital. After one year
of residency in neurosurgery at the White Memor-
ial Hospital in Los Angeles, he transfered to a
dermatology residency at the same hospital. Since
1970, he had practiced dermatology at Victorville,
California. He married Anita Martin in 1955.
Besides his widow, he leaves three children.
As a boy. Dr. Campbell was an ardent butterfly
collector, and assembled a fine collection from the
United States and Cuba. He was also interested in
orchid culture and in raising cats for show. While
a medical student, he developed a deep interest in
marine shells of West Mexico. He made many
shore collecting, diving, and dredging trips to Baja
California, Guaymas, and Mazatlan. He was the
president of the Conchologjcal Club of Southern
California in 1962, and the vice-chairman of the
American Malacological Union-Pacific Division in
1968. For the past few years, due to health
problems, he was inactive with his collection.
However, he had recently renewed his interest, and
was planning a collecting trip to Panama at the
time of his death. He was especially interested in
the fossO and recent Typhinae and was compiling
data for a monograph of the family. He will be
deeply missed by liis many friends and especially
the writer, since we shared many collecting trips
and also shared our professional office. Trigono-
stoma campbelli Shasky, 1964, was named in his
honor.
Bibliography of G. Bruce Campbell
1961a. Range extension for Terebra ornata Gray,
1834. The Veliger, 3(4): 112.
1961b. Colubrariidae (Gastropoda) of tropical West
America, with a new species. The Nautilus,
74(4): 136-142, pi. 10.
1961c. Four new Panamic gastropods. The Veliger,
4(1): 25-28, pL 5.
1961d. Range extension of Anatina cyprinus
(Wood 1828). ibid, 4(2): 115, 3 text figure.
1962. A new deep-water Anadara from the Gulf
of California, ibid, 4(3): 152-154, pi. 37, 1 text
figures.
1963a. Rediscovery of Terebra formosa Deshayes,
1857. ibid. 5(3): 122.
1963b. A new marine research station at Guaymas,
Mexico, ibid, 5(3): 122.
1963c. (With Burch, J. Q.) Four new Olivella from
the Gulf of California. The Nautilus, 76(4):
120-126, pis. 6, 7.
1963d. (With Burch, J. Q.) A new genus for
deep-water California naticid. Proc. Malac. Soc.
London, 35: 221-225, pi. 5.
1963e. (With Burch, J. Q.) Shaskyus, new genus
of Pacific Coast Muricidae (Gastropoda). Jour.
de Conchyl. 103(4): 201-206, pL 6.
1964a. New terebrid species from the Eastern
Pacific (Mollusca: Gastropoda). The Veliger,
6(3): 132-138, pi. 17.
1964b. (With Keen, A. M.) Ten new species of
Typhinae, (Gastropoda; Muricidae). ibid, 7(1):
46-57, pis. 8-11, 3 text figures.
1964c. (With Shasky, D. R.) New and otherwise
interesting species of mollusks from Guaymas,
90 THE NAUTILUS
July 30, 1973
Vol. 87 (3)
Sonora, Mexico, ibid, 7(2); 114-120, pis. 21,
22, 1 text figure, 1 map.
Names Proposed by G. Bruce Campbell
adairensis Campbell, Terebra (Strioterebnim). 1964
altatae Burch and Campbell, Olivella (Olivellaj,
1963
anitae Campbell, Nassarina (Zanassarina). 1961
berry'i Campbell. Terebra (Strioterebnim). 1961
Calinaticina Burch and Campbell, 1963
churea Campbell, Terebra (Strioterebnim). 1964
clarki Keen and Campbell, Typhis (Typhinopsis),
1964
cortezi Shasky and Campbell. Crassispira (Stri-
ospira). 1964
crebriforma Shasky and Campbell. Clathurella (Li-
oglyphostoma). 1 964
Distichotyphis Keen and Campbell, 1964
diishanae Campbell. Terebra (Strioterebnim). 1964
eri'tlirostigma Keen and Campbell. Siphonochelus
(Sipfionochelus), 1964
fayae Keen and Campbell. Pterotyphis (Tripter-
otyphis). 1964
hyphalopilema Campbell, Amdora(Scapharca), 1962
imperialis Keen and Campbell. Typhis (Typhina).
1964
ludbrookae Keen and Campbell. Laevityphis (Laevi-
typhis). 1964
mcleani Shasky and Campbell. Calliostoma, 1964
myrae Campbell, Trivia (Piisula). 1961
ninfae Campbell. Terebra (Strioterebnim). 1961
nipponensis Keen and Campbell. Sipiionochcliis
(Siphonochelus). 1 964
precursor Keen and Campbell, Tvphis (Talitvphis).
1964
schencki* Keen and Campbell, Laevityphis (Laev-
ityphis). 1964
Shaskyus Burch and Campbell. 1963
sphoni Burch and Campbell. Olivella (Olivella).
1963
steveni Burch and Campbell. Olivella (Olivella).
1963
steveni campbelli Burch and Campbell, Olivella
(Olivella). 1963
teramachii Keen and Campbell, Typhis (Tyhpina).
1964
vemae Keen and Campbell. Distichotyphis, 1964
xavieri Campbell, Columbraria. 1961
by Donald R. Shaskv, 229 Cajon Street
Redlands. California 92373
VI VIP A R US MA L LEA TUS
IN NEW HAMPSHIRE
Frank Perron and Thomas Probert
Box 2146, Babcock Hall
University of New Hampshire
Durham, N. H. 03824
A large population of Vivipanis malleatus
(Reeve) was found on May 25, 1972, in the
Cocheco River in the town of Rochester. New
Hampshire. William J. Clench kindly verified the
identification, and we believe that this is the first
record of V. malleatus in this state. Specimens
were deposited in The Ohio State Museum,
Columbus. Ohio.
The snaUs occupy an extensive area of slack
water backed up above the Rochester town dam.
The substrate is quite sandy, but is covered with a
thick layer of algae. It has been noted that the
snail population is densest near a large trailer park
where concrete septic tanks have been built very
close to the river. Finally, these snails share the
substrate with Elliptio complanatus. Alasmidonta
undulata. Amnicola limosa, and Helisoma anceps.
Heretofore, this species has been recorded by
Abbott (1950) from San Francisco (1891); San
Jose, California (1900); Muddy River, Boston
Massachusetts. W. J. Clench (1914); Lake Quin-
sigamond, Worcester. Massachusetts (1917); Fair-
mount Park, Philadelphia, Pennsylvania (1925); St.
Petersburg. Florida (1950); near Niagara Falls, New
York (1942). The Delaware Museum of Natural
History (R. T. Abbott, in lift.) has specimens from
Putnam Pond, Fitchburg. Massachusetts, K. and R.
Wriglit, January 1973; Roosevelt Common Pond.
Tenafly, New Jersey, Alice D. Barlow. October
1968; Pine Tree Brook, Milton, Massachusetts,
Clench and R. D. Turner, May 1957; Central Park,
New York City, 1970; Sawntill Lake, Higlt Point
Park. N. J., Dorothy Fackert, 1971.
LITERATURE CITED
Abbott, R. Tucker. 1950. Snail Invaders. Natural
History 59(2): 80-85.
INFORMATION FOR SUBSCRIBERS
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MOLLUSK VOUCHER SPECIMENS
It is becoming increasingly important for future
research purposes that an identified sampling of
species mentioned in pubUcations be deposited in
a permanent, accessible museum specializing in
mollusks. This is particularly true of mollusks used
in physiological, medical, parasitological, ecological,
and experimental projects.
The Delaware Museum of Natural History has
extensive, modern facilities and equipment for the
housing and curating of voucher specimens. Mater-
ial should be accompanied by the identification,
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is no charge for this permanent curating service,
and catalog numbers, if desired, will be sent to
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OCTOBER 1973
THE
NAUTILUS
Vol. 87
No. 4
A quarterly
devoted to
malacology and
the interests of
conchologists
Founded 1889 by Henry A. Pilsbry. Continued by H. Burrington Baker.
Editors: R. Tucker Abbott and Charles B. Wurtz
EDITORIAL COMMITTEE
CONSULTING EDITORS
Dr. Arthur H. Clarke, Jr.
Department of Mollusks
National Museum of Canada
Ottawa, Ontario, Canada K1A-0M8
Dr. William J. Clench
Curator Emeritus
Museum of Comparative Zoology
Cambridge, Mass. 02 138
Dr. William K. Emerson
Department of Living Invertebrates
The American Museum of Natural History
New York, New York 1 0024
Mr. Morris K. Jacobson
Department of Living Invertebrates
The American Museum of Natural History
New York, New York 10024
Dr. Aurele La Rocque
Department of Geology
The Ohio State University
Columbus, Ohio 43210
Dr. James H. McLean
Los Angeles County Museum of Natural History
900 Exposition Boulevard
Los Angeles, California 90007
Dr. Arthur S. Merrill
Biological Laboratory
National Marine Fisheries Service
Oxford, Maryland 21654
Dr. Donald R. Moore
Division of Marine Geology
School of Marine and Atmospheric Science
10 Rickenbacker Causeway
Miami, Florida 33149
Dr. Joseph Rosewater
Division of Mollusks
U. S. National Museum
Washington, D.C. 20560
Dr. G. Alan Solem
Department of Invertebrates
Field Museum of Natural History
Chicago, Illinois 60605
Dr. David H. Stansbery
Museum of Zoology
The Ohio State University
Columbus, Ohio 43210
Dr. Ruth D. Turner
Department of Mollusks
Museum of Comparative Zoology
Cambridge, Mass. 02138
Dr. Gilbert L. Voss
Division of Biology
School of Marine and Atmospheric Science
1 0 Rickenbacker Causeway
Miami, Florida 33149
EDITORS
Dr. R. Tucker Abbott
Delaware Museum of Natural History
Box 3937, Greenville, Delaware 19807
Dr. Charles B. Wurtz
3220 Penn Street
Philadelphia, Pennsylvania 19129
Mrs. Horace B. Baker
Business and Subscription Manager
1 1 Chelten Road
Havertown, Pennsylvania 1 9083
OFFICE OF PUBLICATION
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Kennett Pike, Route 52
Box 3937, Greenville, Delaware 19807
Second Class Postage paid at Wilmington, Delaware
Subscription Price: $7.00 (see inside back cover)
THE
NAUTILUS
Volume 87, number 4 - October 1973
CONTENTS
R. Tucker Abbott
Acteon eloiseae, a New Opisthobranch from Arabia 91
Michael A. Rex and Kenneth J. Boss
Systematics and Distribution of the Deep-sea Gastropod, Epitonium ( Eccliseogyraj nitidum 93
Francisco J. Palacio
On the Double Hectocotylization of Octopods 99
William A. Sodeman, Jr.
The Influence of Light on Biomphalaria glabrata 1 03
Morris K. Jacobson
On the Identity of Helicina granulum Pfeiffer (Prosobranchia) 1 07
Wayne D. Cable
The Valvular Membrane in Young Mactrid Clams, Spisula solidissima 110
Kenneth W. Turgeon and Richard A. Fralick
Size and Sex Ratio Differences in Urosalpinx cinerea (Say) (Muricidae)
from Great Bay, New Hampshire 112
Willard N. Harman
The Mollusca of Canadarago Lake and a New Record for Lasmigona compressa (Lea) 114
Richard W. FuUington
Obituary of Elmer P. Cheatum (1901-1973) 115
Book Reviews
(of) Percy A. Morris, 102; Edwin A. Joyce, Jr 114
INDEX TO THE NAUTILUS
The extensive 279-page Author Index to The
Nautilus, vols. 1-75, compiled and published by
Aurele La Rocque in 1963 is still available
(unbound) for the extremely low price of $2.00
postpaid. A continuation, covering vols. 76-85, was
recently published in no. 49 of Sterkiana, 1972.
Reprints of this very useful addition are also
available for 25 cents. When ordering both of
these indispensable indices, we suggest an addi-
tional 50 cents be added to cover postage. Write:
Dr. AurSle La Rocque, 125 South Oval Dr., Ohio
State Univ., Columbus, Ohio 43210.
vu
american malacologists
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Here are the facts about each biog-
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pation, educational record, protessional
career, present position, malacological
and civic memberstiips, writings (in-
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and books), current mollusk research
activities, extent of shell collection,
expeditions, sources of additional bio-
graphical information, marital status,
current address — all in a clear and
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Also contains Three Major Cross-
Indexings with over 1,000 biographees
arranged (1) geographically by states
and cities, (2) by current research ac-
tivities, and (3) by occupations.
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I I for institutional libraries (20% discount) $10.00
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and are now made available practically at cost to all libraries,
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Handsomely bound, gilt-edged on 3 sides and in full 9x12
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VIU
Vol. 87 (4)
THE NAUTILUS
91
ACTEON ELOISEAE, A NEW OPISTHOBRANCH FROM ARABIA
R. Tucker Abbott
Delaware Museum of Natural History
Greenville, Delaware 19807
In 1970, Dr. Donald Bosch of the American
Mission Hospital in the Muscat obtained eight
specimens of an undescribed species of Acteon.
Unfortunately, soft parts were not preserved,
although one shell contained a dried operculum.
When the radulae are known it may be possible to
place properiy this species which closely resembles
members of the genus or subgenus Maxacteon
Rudman, 1971. I take great pleasure in naming
this species after the discoverer's wife, Eloise
Bosch.
Acteon eloiseae new species, Abbott
Figs. 1-4
Diapiosis—kA\Ai shell 30 to 35 mm, stoutly
ovate, solid, spirally and closely grooved, with
about 7 whorls and a low spire. Color white with
3 spiral rows of large rose-colored, crescent-shaped,
irregular splotches, each of which is bordered by a
strong black Une. Columella white, with one spiral
cord. It is most similar to Acteon flammeus
(Gmelin) but the latter is smaller, less obese, with
more numerous axial flames of color which are
lacking the black borders.
Description—ShtW 30 to 35 mm in length (1
3/8 inches), stoutly ovate, soUd, with a deep but
minute umbilicus; whorls 7 to 8; nuclear whorls 2,
smooth, white. Postnuclear whorls in the spire
with 5 to 7 deep, narrow spiral grooves which are
crossed by regular, microscopic axial threads giving
a pitted appearance. Between the grooves there are
raised, slightly rounded cords crossed by numerous
weak growth threads. Last whorl with about 30
grooves. Suture slightly channeled. Aperture ovate,
narrow above white within. Spire slightly eleVated
and about 1/3 to 1/4 the length of the shell.
Outer lip thin and sharp. Parietal callus thick and
translucent white. Columella thick, glistening white
and bearing a single, smooth, large, spiral cord
which runs back into the aperture. Umbilicus very
narrow and deep, well-grooved. Periostracum thin,
translucent tan, but thicker in the umbilical
region. Color of shell white, with 3 spiral bands of
irregular, crescent-shaped, rose to crimson blotches
which are bordered by a narrow black line. The
latter is usually wider on the adapertural side.
There are 6 to 7 blotches on the top and bottom
rows and about 11 in the middle row. Operculum
thin, chitinous, translucent amber, elongate, 14
nun in length, 6 mm in width (from a shell 31
mm in length). Nucleus indistinct and at the
broader thick end. It resembles the operculum of
Acteon tomatilis (Linn^) in shape.
FIGS. 1-3. Acteon eloiseae Abbott, new species,
Figs. 1, 2. holotype, Delaware Museum Natural
History, no. 27213. 31 mm in length. Fig. 3.
Exterior of chitinous operculum 14 mm in length.
92 THE NAUTILUS
Vol. 87 (4)
no. whorls
7.0 holotype
8.0 paratype
8.0 paratype
8.0 paratype
7.0 paratype
Types— The type locality: Al Masirali Island,
Oman Protectorate, southeast Arabia. Collected by
fishermen in shallow water near shore, 1970.
Holotype in the Delaware Museum of Natural
History, no. 27213. Paratypes in Delaware Museum
of Natural History, no. 67746, and in the
collection of Dr. Donald Bosch.
Remarks- Acteon eloiseae is a very colorful and
attractive species of unusual large size, and is
characterized by the three rows of large,
black-bordered, rose-colored blotches. Its nearest
relative, found in the Indian and southwest Pacific
Oceans, A. flammeus (GmeUn), differs in having
twice as many, narrower, pinkish rose, axial flames
of color wliich lack the black borders. Other
curious marine moUusks inhabiting the waters of
this island include Cypraea teuleri Cazenavette,
1846, and Cymatium boschi Abbott and Lewis,
1970.
american malacologists
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FIG. 4. Acteon eloiseae Abbott, new species.
Paratype, details of sculpture and color pattern
X6. FIG. 5. Details of sculpture and color pattern
of Acteon flammeus (Gmelin, 1791) from Praia de
Chocas, Mozambique. X6. Photos by the author
American Malacologists
6314 Watprway Drive
Falls Church,
Va. 22044
Vol. 87 (4)
THE NAUTILUS
93
SYSTEMATICS AND DISTRIBUTION OF THE DEEP SEA
GASTROPOD EPITONIUM (ECCLISEOGYRA) NITIDUM
Michael A. Rex
Department of Biology, University of Massachusetts
Boston, Massachusetts 02116
and
Kenneth J. Boss
Museum of Comparative Zoology, Harvard University
Cambridge, Massachusetts 02138
ABSTRACT
Recent deep sea dredging in the western North Atlantic and South Atlantic
Oceans has yielded new specimens of the rare, open-coiled gastropod Epitonium
nitidum (Verrill and Smith). It is the type-species of the subgenus Eccliseogyra Dall,
1892, which is now removed from the subfamily Liotiinae (family Turbinidaej and
placed in the genus Epitonium (family Epitoniidaej. The synonymy and Pan-Atlantic
distribution of this species are discussed.
INTRODUCTION
In 1 885, Verrill described a fragment of an
open-coiled gastropod shell dredged by the Alba-
tross as Delphinula nitida and provisionally re-
ferred the unusual species to the prosobranch
family Trochidae. Subsequently, Dall (1889a)
assigned nitida to Laxispira Gabb, a subgenus of
Liotia Gray in the Delphinulidae. But later, after
discovering that Gabb's taxon was based on a
fossil cast or mold of Siliquaria, Dall (1892)
proposed the subgenus Eccliseogyra for nitida. A
very similar, but intact, specimen was described
from the Challenger material by Watson (1886) as
vermetiformis and placed in the genus Scalaria
Lamarck, now a synonym of Epitonium Roding
(Clench and Turner, 1951). Locard (1897 a, b)
named two additional specimens collected during
the Travailleur and Talisman expeditions as
Scalaria dissoluta, distinguishing them from S.
vermetiformis Watson on the basis of minor
differences in shell size, shape and sculpture. Bayer
(1971) first suggested that, except for the relative
height of the spire, Verrill's and Watson's species
were "close ... if not identical."
Recent deep sea dredging operations on vessels
of the Woods Hole Oceanographic Institution
(Sanders, Hessler, and Hampson, 1965) have yield-
ed numerous additional specimens of nitida (Table
1 and Figure 1). This new material was compared
with the holotype of vermetiformis Watson, the
FIG. 1. Typical specimen of E. nitidum (Verrill
and Smith) from the western North Atlantic
(Chain station 103, see Table 1). Height 6.3 mm.
94 THE NAUTILUS
October 1973
Vol. 87 (4)
paratype of dissohita Locard, additional fragments
identified by Verrill as nitida (USNM 78566), but
evidently never reported on, and Bayer's excellent
photograph (1971: Figure 11, D). It is concluded
that all belong to the same species and that
previously noted small differences between speci-
mens are aspects of intraspecific character
variation.
Keen (1960) considered Eccliseogyra Dall a
genus and placed it in the family Turbinidae of
the superfamily Trochacea. On the basis of
morphological features of its type species, Ec-
cliseogyra is here considered a subgenus of Epi-
tonium and is transferred to the Epitoniidae.
SYSTEMATICS
The following synonymy summarizes the
nomenclatorial history of this species.
Genus Epitonium Roding 1798
Subgenus Eccliseogyra Dall 1892
Eccliseogyra Dall 1892, Trans. Wag. Free Inst. Sci.
3: 307 (type species: Delphinula nitida Verrill
and Smith 1885, by monotypy).
Solutiscala de Boury 1909, Bull. Mus. Hist. Nat.,
Paris 15: 482 (type species: Scalaria
[=Epitonium] dissoluta Locard, original
designation).
Epitonium (Eccliseogyra) nitidum
(Verrill and Smith 1885)
Figs. 1-4; Table 1
Delphinula nitida Verrill and Smith 1885 [in]
Verrill, Trans. Conn. Acad. Arts Sci. 6 (2):
424-425, pi. 44, fig. 11. (Albatross Sta. 2229,
off Chesapeake Bay, 37°38'40" N; 73°16'30"W,
1423 fathoms [= 2602 meters] ; holotype in the
USNM destroyed); paratype, USNM 78566,
Albatross Sta. 2714, SW of Nantucket,
38°22'N; 70°17'30"W, 1825 fathoms [= 3338
meters] .
Scalaria vermetifonnis Watson 1886, Challenger
Repts., Zool. 15: 142, pi. 9, fig. 6. (Challenger
Sta. 122, off Pemambuco (Recife], Brazil,
09°5'S; 34°50'W, 350 fathoms [= 640 meters] ;
holotype in BMNH).
Liotia (Laxispira) nitida (Verrill [sic] ). Dall 1 889,
Bull. Mus. Comp. Zool. 18: 386 [generic and
subgeneric affinities of nitida discussed] ; Dall
1889, Bull. U. S. Nat. Mus., 37: 166, pi. 46,
fig. 1 1 [Verrill and Smith's figure of nitida
reproduced] .
Liotia (Eccliseogyra) nitida (Verrill [sic]). Dall
1892, Trans. Wag. Free Inst. Sci. 3 (2): 307
[nitida assigned to a new subgenus] .
Scalaria dissoluta (P. Fischer MS) Locard 1897.
L'Echange, Revue Linneenne, 145, p. 3; Locard
1897. Exped. Sci. Travailleur et Talisman,
MoUusques Testaces 1: 407-408, pi. 19, figs.
1-3 (Talisman Sta. 113, off Cape Verde Islands,
495-618 meters [corrected to 80-110 meters by
Smith, 1 888] ; location of figured holotype
unknown; paratype, here figured, Travailleur
Sta. 3 [1881, Atlantic Series], W of Portugal,
39°47'50"N; 9°51'45"W, 3307 meters).
Solutiscala (Solutiscala) vermetiformis (Watson).
Clench and Turner 1952, Johnsonia 2: 347, pi.
170, figs. 1-2.
Epitonium (Solutiscala,) vermetiforme (Watson).
Bayer 1971, BuU. Mar. Sci. 21: 133, fig. 11 d
(Gerda Sta. G-966, Straits of Florida SW of
Marquesas Keys, 24°10'N; 82°22'W, 544-549
meters).
REMARKS
A specimen from the new material dredged in
the western North Atlantic (Table 1) is shown in
Figure 1 . For comparison, the paratype of Scalaria
dissoluta Locard and the holotype of Scalaria
vermetiformis Watson are illustrated in Figures 2
and 3 respectively. The protoconch was described
by Watson (1886, p. 142, pi. 9, fig. 6; see also
Figure 3 this paper). It is brown in color, has four
connected whorls and is sculptured with closely
placed axial ribs. The postlarval shell was
described by Verrill (1885). It is delicate and
whitish gray in color. Whorls are circular in
cross-section and are completely disconnected.
Sculpture consists of many closely placed spiral
ribs crossed by delicate axial lamellae which
completely circumscribe the whorls. As Verrill
(1885) pointed out, the lamellae are more elevated
on the upper, inner and lower surface of the
whorls (see, e.g.. Figure 1). This fact, along with
the broken appearance of the lamellae, suggests
that they are normally more extended, but have
been damaged during dredging.
Vol. 87 (4)
THE NAUTILUS
95
Except for the relative height of the spire,
there is Httle variation among the specimens that
we have examined. The width to height ratio at
the end of the fourth whorl ranges from 0.68
(specimen in Figure 1) to 0.48 (specimen in
Figure 2).
From its general appearance, nitidum is refer-
able to Epitonium and we concur with Clench and
Turner (1952) who placed it in the subgenus
Solutiscala which deBoury (1909) estabUshed for
the uncoiled species. However, deBoury's taxon, is
a junior subjective synonym of Eccliseogyra Dall
1892 and, thus, the proper nomen for the species
is Epitonium (Eccliseogyra) nitidum.
Unfortunately, both Verrill's surviving fragment
and specimens in the new material are missing the
distinctive protoconch illustrated by Watson (1886,
pi. 9, fig. 6). Several specimens in the new
material show remains of broken eroded apices
which are smooth and lack periostracum. However,
the similarities both in the sculpture and in the
FIG. 2. Paratype of Scalaria dissoluta Locard
f'Travailleur staHon 3, off Portugal, MNHP 642).
Specimen decollated, height 5.5 mm, coated with
magnesium oxide for photography.
FIG. 3. Holotype of Scalaria vermetiformis Watson
/■Challenger station 122, off Pemambuco [Recife],
Brazil, BMNH 87.2.9.500. Specimen complete with
protoconch, height 4.8 mm, coated with
magnesium oxide for photography.
form of postlarval whorls are sufficient to justify
the synonymy of vermetiformis and dissoluta with
nitidum
Epitonium revolutum (Hedley, 1899), reported
from shallow water in Funafuti Atoll, is reminis-
cent of E. nitidum because of its open-coiled shell,
and was included in Solutiscala by deBoury
(1909). However, it can be clearly distinguished by
its less numerous and more pronounced varices.
Ladd (1972) recently noted this species from the
Late Miocene of Palau.
An unusual feature of E. nitidum is its
open-coiled or alloiostrophic (Simroth 1896-1907)
FIG. 4. The distribution of Epitonium nitidum
(Verrill and Smith, 1885) in the Atlantic Ocean.
Solid stars indicate individual records, and the
open star in the western North Atlantic represents
a composite of the first nine new records
presented in Table 1 and two previous records
from Verrill discussed in the text.
96 THE NAUTILUS
October 1973
Vol. 87 (4)
condition. Coiling in snails was described by Raup
(1966) in terms of four geometric parameters:
whorl shape (S), rate of whori expansion (W),
distance of whorls from the coiling axis (D), and
translation rate along the coiling axis (T). Yochel-
son (1971) pointed out that "open coiling may
occur if any of these components is large enough
to prevent contact of the whoris." In isostrophic
(planispiral) shells it obtains when either D > - or
W >-(Raup, 1967; Yochelson, 1971). In ortho-
D
strophic (downward spiraling) forms such as E.
nitidum it is generally achieved by having an
exceptionally high translation rate. Alloiostrophy
occurred in numerous hneages of fossU gastropods
(cf Wenz, 1938) and is widespread in Recent
fresh-water and marine prosobranchs as well as in
terrestrial and fresh-water pulmonates (Boss and
Rex in prep.). In the Vermetidae, open coOing
provides increased surface area for cementation
(Gould, 1966), but the adaptive significance of
open coiling in other cases is not clear. In
sedentary deposit, or suspension feeding forms it
might function to maintain position in the
substratum.
DISTRIBUTION
New locality records for E. nitidum are present-
ed in Table 1, and all known localities are plotted
in Fig. 4.
The horizontal distribution pattern depicted in
Fig. 4 is largely an artifact of where extensive
dredging has taken place. It is evident, however,
that the geographic range of the species includes
both the eastern and western North Atlantic, and
a Pan-Atlantic distribution appears Ukely. Un-
fortunately, there is some confusion about the
location and depth of Talisman station 113.
Locard (1897 b) variously cited this station as
being located either in the Azores or the Cape
Verde Islands at depths ranging from 495 to 1983
meters. We have followed Smith (1888) in placing
Talisman station 113 in the Cape Verde Islands at
depths of 80-110 meters (Fig. 4).
Though a comparatively rare species', nitidum
exhibits nearly the same broad geographic range as
dominant deep sea gastropod species such as
Cithna tenella Jeffreys, Adeorbis umbilicatus
Jeffreys, Mangelia bandella Dall, and Lacuna
cossmanni Locard (Rex, 1972). Madsen (1961) and
Knudsen (1970) have shown that
macro-topographic relief of the ocean floor, such
as the Mid-Atlantic Ridge, does not exert an
important influence on the distribution of many
deep sea benthic invertebrate groups. This appears
to be true of some gastropods, including E.
nitidum
In the northwestern Atlantic, E. nitidum has
been collected only between the depths of 2022
and 4693 meters (Table 1) despite extensive
dredging both above and below these depths.
However, in more equatorial regions the species'
bathymetric range extends into much shallower
waters including the upper continental slope off
Brazil {Challenger Sta. 122, 640 meters), off
Florida {Gerda Sta. G-966, 544-549 meters), and
the continental shelf in the Cape Verde Islands
{Talisman Sta. 113, 80-110 meters according to
Smith 1888). Thus nitidum has a vertical distribu-
tion ranging from the continental shelf to the
abyssal plain. Deep sea benthic invertebrate species
with wide horizontal distribution are typically
eurybathic (Vinogradova 1959), but this tendency
has not previously been reported for gastropods
because of inadequate material. It should be noted
that this type of distribution is not universal
among deep sea gastropods and that its frequency
remains to be determined.
ACKNOWLEDGMENTS
We thank W. D. Hartman (PMNH), J.
Rosewater (USNM), J. Taylor (BMNH), and M.
Testud (MNHP), for the loan of specimens from;
these institutions. This research received support
from NSF Grant GB- 19922 to Harvard University
(R. C. Rollins, principal investigator). We especially
wish to thank H. L. Sanders who kindly provided
the new material presented in Table 1 which was
collected by WHOI under NSF Grants GB-563 and
GB-15638. The manuscript was read by R. D.
Turner, R. Bullock and R. Tucker Abbott.
' Eight live specimens collected between the depths
of 2022 to 3834 meters off North America
(Table 1) comprised less than 0.7% of the
number of live gastropods dredged between these
depths during the WHOI Gay Head-Bermuda deep
sea dredging project.
Vol. 87 (4)
THE NAUTILUS
97
ABBREVIATIONS
USNM United States National Museum, Washing-
ton, D. C.
PMNH Peabody Museum of Natural History, Yale
University
WHOI Woods Hole Oceanograpluc Institution
BMNH British Museum of Natural History
MNHP Museum of Natural History, Paris
LITERATURE CITED
Bayer, F. M. 1971. New and unusual mollusks
collected by R/V John ElUott Pillsbury and
R/V Gerda in the tropical western Atlantic.
BuU. Mar. Sci. 21: 111-236.
Boss, K. J. and M. A. Rex. In prep. Alloiostrophy
in Tertiary and Recent Gastropods.
deBoury, E. 1909. Observations sur les Scalidae
des Expeditions scientifiques du Tmvailleur et
du Talisman. Bull. Mus. Natl. Hist. Nat., Paris
15: 478-484.
Clench, W. J. and R. D. Turner. 1951. The genus
Epitonium in the western Atlantic. Johnsonia 2:
249-288.
Qench, W. J. and R. D. Turner. 1952. The genera
Epitonium (Part II), Depressiscala, Cylindriscala,
Nystiella and Solutiscala in the western
Atlantic. Johnsonia 2: 289-356.
Dall, W. H. 1889a. Report on the MoUusca, Part
II Gastropoda and Scaphopoda. Reports on the
results of dredging ... in the Gulf of Mexico
(1877-78) and in the Caribbean Sea (1879-80),
by the U. S. Coast Survey steamer "Blake" . . .
Bull. Mus. Comp. Zool. 18: 492 p.
Dall, W. H. 1 889b. A preUminary catalogue of the
shell-bearing marine mollusks . . . Bull. U. S.
Nat. Mus. 37: 1-221.
Dall, W. H. 1892. Contributions to the Tertiary
fauna of Florida, with special reference to the
Miocene Silexbeds of Tampa and the Pliocene
beds of the Caloosahatchee River. Part. II.
Streptodont and other gastropods, concluded.
Trans. Wagner Free Inst. Sci. (Philadelphia) 3:
201-473.
Gould, S. J. 1966. Notes on shell morphology and
classification of the Siliquariidae (Gastropoda).
The protoconch and slit of Siliquaria squamata
Blainville. Amer. Mus. Novitates 2263: 1-13.
Hedley, C. 1 899. The Mollusca of Funafuti. Part 1
Gastropoda. Australian Mus. Mem. 3: 395-488.
Keen, M. 1960. In Moore, R. C. [ed.] Treatise on
Invertebrate Paleontology. Part I, Mollusca 1,
Univ. Kansas, Lawrence, Kansas, 351 p.
Knudsen, J. 1970. The systemarics and biology of
abyssal and hadal Bivalvia. Galathea Rept. 11:
1-241.
Ladd, H. S. 1972. Cenozoic fossil mollusks from
western Pacific islands; Gastropods (Turritellidae
through Strombidae). Geol. Surv. Prof Pap.
532: 1-79.
Locard, A. 1897a.. Notices conchyliologiques.
XLII. Scalaridae nouveaux. L'Echange, Revue
Unneenne 145: 2-3.
Locard, A. 1897b. Expeditions scientifiques du
Travailleur et du Talisman. Mollusques Testaces
1: 1-516.
Madsen, F. J. 1961. On the zoogeography and
origin of the abyssal fauna, in view of the
knowledge of the Porcellanasteridae. Galathea
Rept. 4: 177-218.
Raup, D. M. 1966. Geometric analysis of shell
coiling: general problems. Jour. Paleontology
40: 1178-1190.
Raup, D. M. 1967. Geometric analysis of shell
coiling: coiling in ammonoids. Jour. Paleon-
tology 41: 43-65.
Rex, M. A. 1972. Species diversity and character
variation in some western North Atlantic deep
sea gastropods. Unpublished Ph.D. Thesis, Har-
vard University, 178 pp.
Sanders, H. L., R R. Hessler and G. R. Hampson.
1965. An introduction to the study of deep-sea
benthic faunal assemblages along the Gay
Head-Bermuda Transect. Deep-Sea Res. 12:
845-867.
Simroth, H. 1896-1907. Mollusca. In H. G. Bronn
[ed.]. Klassen undOrdnungen des Tier-Reichs 3:
1506 p. C. T. Winter'sche Verlagshandlung,
Leipzig.
Smith, S. 1888. Lists of the dredging stations of
the U. S. Fish Commission . . . Ann. Rept. U.
S. Comm. Fish and Fisheries, for 1886:
837-1017.
Verrill, A. E. 1885. Third catalogue of Mollusca
recently added to the fauna of the New
England Coast . . . Trans. Conn. Acad. Arts.
Sci. 6: 395-452.
Vinogradova, N. G. 1959. The zoogeographical
distribution of the deep-water bottom fauna in
the abyssal zone of the ocean. Deep-Sea Res. 5:
205-208.
98 THE NAUTILUS
October 1973
Vol. 87 (4)
TABLE 1. New Records o/ Epitonium (Eccliseogyra) nitidum (Verrill and Smith, 1885) in the Atlantic
Ocean.
Cruise
Depth
in
Station Meters
Locality
Date
Number of Specimens
Watson, R. B. 1886. Report on the Scaphopoda
and Gastropoda collected by the H.M.S. "Chal-
lenger" during the years 1873-1876. Challenger
Repts., Zool. 15: 1-756.
Wenz, W. 1938. Gastropoda, Teil 1: Allgemeiner
Teil und Prosobranchia. In O. H. Schindewolf
[ed.], Handbuch der Palaozoologie 6; 1-948,
Gebriider Borntraeger, Berlin.
Yochelson, E. L. 1971. A new Late Devonian
gastropod and its bearing on problems of open
coiling and septation. In J. T. Dutro, Jr. [ed.] .
Paleozoic perspectives: A paleontological tribute
to G. Arthur Cooper: Smithsonian Contr.
Paleobiology 3: 231-241.
BOOK REVIEW
A PARTIAL BIBLIOGRAPHY OF OYSTERS,
WITH ANNOTATIONS. By Edwin A. Joyce.,
Jr. State of Florida Department of Natural
Resources, Special Scientific Report No. 34,
June 1972. Paperback, 846 pp.
Among the many useful scientific works on
marine mollusks emanating from the Marine Re-
search Laboratory in St. Petersburg, Florida, this
enormous compilation leads this year's contribu-
tions in popularity and usefulness. Joyce's biblio-
graphy now replaces the famous, but hard to
obtain, oyster reference book that J. L. Baughman
issued in 1948.
Although the emphasis is naturally on papers
dealing with commercial oysters, there is excellent
coverage in other research areas, such as on the
venerid clams, the freshwater Corbicula and
unionid mussels, scallops and gastropod predators.
Of the 4,117 references listed 45% are annotated,
a feature invaluable to those without an extensive
hbrary. The key to the Uterature appears in a
Subject Index that lists all papers dealing with one
of 55 various categories, such as Age and
Longevity; Embryology; Mariculture; Pearls; Pollu-
tion and Taxonomy. Edwin Joyce and his Florida
associates are to be congratulated and thanked for
producing this much-needed compendium.
R. Tucker Abbott
Delaware Museum of Natural History
Vol. 87 (4)
THE NAUTILUS
99
ON THE DOUBLE HECTOCOTYLIZATION OF OCTOPODS
Francisco J. Palacio'
University of Miami
Rosenstiel School of Marine and Atmospheric Science
Miami, Rorida 33149
ABSTRACT
Two cases of double unilateral hectocotylization in Incirrate octopods are
reported for the first time. The supernumerary hectocotylized arms have smaller
ligulas, calami and seminal canals, and the last few rows of suckers are reduced in
size. The extra modified arms are believed to be sexually functional Double
hectocotylization is not accompanied by modifications of the genitalia. The extra
hectocotylization is possibly caused by a sex-linked mutatiQn, and it is manifested in
a uniform proportionality.
Most male octopods have the third right arm
modified for insemination; the tip of the arm is
transformed into a spoon-shaped or flat hgula
which may bear small transverse ridges; and a velar
membrane, converted into a seminal groove, fringes
the margin of the arm terminating distally into a
conical "cheeked" calamus. In shallow water
Octpodinae the ligula is small, usually not exceed-
ing 15% of the arm length. In deeper water forms
the modified portion may attain 60 or 70% of the
arm length.
Only three monotypic genera have the third left
arm hectocotyUzed: Scaeurgus unicurrhus
d'Orbigny of worldwide distribution, Euaxoctopus
panamensis, from the Gulf of Panama (Voss,
1971), and Pteroctopus tetracirrhus (delle Chiaje)
occurring in the Atlantic Ocean (a doubtful
species, Pteroctopus witjazi was described from off
the Kamchatka Peninsula (Akimsuhkin, 1963).
In the past only two cases of double bilateral
hectocotyUzation phenomena have been reported.
One case was in Eledone cirrosa from the
Mediterranean and North Sea (Appelof, 1892),
with the third left arm also modified. An idea of
the rarity of the case was given by Morales (1958)
who examined 1,538 specimens of this common
species without finding a single example. The
other case was in Octopus briareus, from Curacao
'Contribution No. 1640 from the Rosenstiel
School of Marine and Atmospheric Science,
University of Miami.
and the West Indies, which had the second left
arm also modified (Robson, 1929).
In the course of a study of the cephalopod
fauna of Brazil, I encountered a double unilateral
hectocotylization in Octopus vulgaris from off Rio
de Janeiro, in which the fourth right arm is also
hectocotyUzed. Another double, unilateral hecto-
cotylizafion was observed by Mr. Martin Wolter-
ding during morphometric measurements of Octo-
pus selene from the Gulf of Panama, in which the
second right arm is also modified.
From my observations and the previous records,
it appears that when this unique phenomenon
occurs, the double hectocotyUzafion is manifested
in a similar pattern. Fig. 1 illustrates the modifica-
tion of the tips of the arms of Octopus selene and
vulgaris the present observations indicate a regular
pattern of proporfional modificafion of the extra
hectocotylized arm to the normally hectocotylized
arm.
The normal third hectocotylized arm is usually
shorter and thinner than the other arms. The extra
hectocotylized arm is not diminished in length,
and maintains its normal relative proportionality in
being 1.06-1.21 times longer and 1.05-1.25 times
wider than the normal arm. The ligula of the
extra hectocotyUzed arm is reduced by 71-83% of
the normal hectocotyUzed arm; the extra calamus
is more variable, being between 48.0-91.6% of the
normal arm. The Ugula/arm proportion of the
extra to the normal hectocotyUzed arms is fairly
uniform (63.0-72.0%), and the calamus/Ugula pro-
portion of the extra to the normal arm ranges
100 THE NAUTILUS
October 1973
Vol. 87 (4)
from 57.5-128.0%. The extra hectocotylized arm
has about 1.16-1.27 times as many sucker rows
than the normal arm; however, the last 19.0 -
28.0% of the suckers of the extra hectocotylized
arm are conspicuously reduced in size.
As was noted in the double hectocotylized
Eledone cirrosa and Octopus briareus, there are no
structural differences in the genitalia of Octopus
selene and O. vulgaris. Nevertheless, the seminal
canal in the extra modified arm is smaller than
that of the normal hectocotylized arm, although
the length and width of the extra hectocotyhzed
arm are larger.
The comparative development of the hecto-
cotylus and the associated organogenesis has not
been studied, but the structural modification of
the arm takes place prior to the onset of
spermatogenesis. Because of the general morpho-
logy, I beheve the additional hectocotyhzed arm is
sexually functional.
The genetic control of hectocotyhzation has not
been studied, but I assume that it is governed by
sex-linked genes, and that mutations at these loci
are possibly responsible for the double hecto-
cotyUzations reported here.
ACKNOWLEDGMENTS
I am grateful to Dr. Gilbert L. Voss, Chairman,
FIG. 1. A-B, Octopus selene, C?. A, tip of second right extra hectocotylized arm; B, tip of third normal
hectocotylized arm. C-D, Octopus vulgaris, Cf ' C, tip of third right normal hectocotylized arm; D, tip of
fourth right extra hectocotylized arm. Notice the reduction in size of the distal suckers of the extra
modified arm.
Vol. 87 (4)
THE NAUTILUS
101
Division of Biology. Rosenstiel School of Marine
and Atmospheric Science. University of Miami, for
making the specimen of Octopus selene available
to me and for the use of his laboratory and
library. Special gratitude is due to Dr. P. E.
Vanzolini. Museu de Zoologia, Universidade de Sao
Paulo, Brazil, for making the Brazilian cephalopod
collections available for study. I am indebted to
Drs. G. L. Voss and Frederick M. Bayer for
reviewing the manuscript and to Miss Susan
Stevens for the illustrations.
TABLE 1. Measurements and proportions of the normal and supernumerary hectocotylized arms fin mm.).
TABLE 2. Sizes and percentages of extra to normal hectocotylized arms (in mm.).
102 THE NAUTILUS
October 1973
Vol. 87 (4)
LITERATURE CITED
Akimishki, I. I. 1963. Cephalopods of the U.S.S.R.
Acad. Sci. U.S.S.R, Institute of Oceanology.
U.S. Dept. Commerce (translation), 233 pp., 60
text-figs.
Appellof, A. 1892. Teuthologische Beitrage IV.
Uber einem Fall von doppelseitiger Hecto-
kotylisation bei Eledone cirrosa (Lam.) d'Orb.
Bergens Mus. Aarbog, :14-15.
Morales, E. 1958. Notas sobre la morfologja del
aparato genital en Eledone aldrovandi (Raf.) =
E. cirrosa (Lamarck). Rap. Proces-Verbaux
Reunios, 14: 389-394.
Robson, G. C. 1929. On a case of bilateral
hectocotylization in Octopus rugosus. Proc.
Zool. See. for 1929: 95-97, 1 text-fig.
Voss, G. L. 1971. Biological results of the
University of Miami Deep- Sea Expeditions. 76.
Cephalopods collected by the R/V JOHN
ELLIOTT PILLSBURY in the Gulf of Panama
in 1967. BuU. Mar. Sci. 21(1): 1-34, 6 figs., 12
tbls.
BOOK REVIEW
A FIELD GUIDE TO SHELLS OF THE ATLAN-
TIC AND GULF COASTS AND THE WEST
INDIES. By Percy A. Morris. Tlnrd Edition,
edited by William J. Clench 330 pp., 8 color
pis., 68 black-and-white pis. Houghton Mifflin
Co., 2 Park St., Boston, Mass. 02107. Hard-
back, $7.95. Paperback. $4.95.
For almost three decades, Percy Morris's field
guides to shells have been a constant companion
for legions of beginning conchologists. For clarity,
compactness and inexpensiveness, his books have
led the field and have been responsible for
encouraging and serving two generations of
American shelling enthusiasts. And now a
much-improved and enlarged edition, with eight
exquisite colored plates and 68 black-and-white
plates, has been issued under the technical direc-
tion of Dr. William J. Clench. The entire format
of the book is refreshingly different and affords
much easier consulting. The nomenclature, and
especially the use of technical and popular names,
has been put on a sounder basis.
In the expanded introduction, the new class,
Monoplacophora, is included, and many valuable
classificatory explanations for the beginner are
introduced. A list of shell clubs and an infor-
mative glossary are added. With the inclusion of
several dozens of West Indian sheUs, tliis field
guide now covers just over a thousand kinds of
Western Atlantic shells.
It is a happy note that a close friend of the
late Percy Morris and a competent malacologist,
Dr. WUliam J. Clench, should shepherd this book
through the rigors of publication. Dr. Clench spent
many tedious hours in bringing the finer points of
nomenclature up to date. Curiously, he did the
very same forty years ago for his deceased mentor,
Charles W. Johnson, in 1933, when he revised and
corrected the manuscript of the now historical
"List of Marine MoUusca of the Atlantic Coast
from Labrador to Texas." Were it not for Dr.
Clench, this last monument to Mr. Morris's many
Uterary contributions would not have attained the
perfection and credit that it riglitfully deserves.
For a handy S7.95 field guide to eastern
American shells, members of the shell public will
not go wrong in adding this book to their
conchological libraries.
R. Tucker Abbott
Delaware Museum of Natural History
Vol. 87 (4) THE NAUTILUS
THE INFLUENCE OF LIGHT ON BIOMPHALARIA GLABRATA'
William A. Sodeman, Jr.
University of Arkansas, School of Medicine
Department of Internal Medicine
4301 West Markham
Little Rock, Arkansas 72201
ABSTRACT
The effect of changes in incident light intensity on the activity of albino
Biomphalaria glabrata was studied utilizing a treadmill apparatus to measure crawling
rate of the snail. The study showed that B. glabrata have a threshold for light
perception which is at least as low as 8 foot candles. When this low intensity light
is turned off the snails respond with a transient pause in crawling activity. This
response was reproducible from trial to trial and was observed with all snails tested.
With sustained activity in the absence of food snails tire. The maximum crawling
rate observed for B. glabrata was 90 cm per hour.
103
Successful maintenance of the cycle of schisto-
somiasis in a natural environment depends upon
vector snails being sited to both receive infection
from and discharge it to suitable definitive hosts.
It is not clear whether the evolution of the
host-vector-parasite relationship depends in part
upon the presence of a critical density of snails,
thus permitting fortuitous snail parasite contact, or
whether other environmental factors cue the snail's
activity resulting in favorable positioning for both
receipt and discharge of the parasite. Isolation of
environmental factors that may cue behavior is
difficult under field conditions. There have been
substantial observations on the effect of environ-
mental variables on physiologic responses of snails,
such as growth, metabolic rates, reproductive
capacity and longevity, both in the field and in
the laboratory. Behavioral responses to environ-
mental variables, particularly in a controlled
laboratory setting, have received only minimal
attention. This paper reports changes in the
activity of Biomphalaria glabrata in relation to
fiuctuations in the intensity of incident light.
MATERIALS AND METHODS
The snails employed were Biomphalaria glabrata
of the albino mutant M-line. Stocks were obtained
'This work was supported by a grant from the
National Institutes of Allergy & Infectious
Disease. AI 10292-02.
in October, 1970 from the University of Michigan
Museum of Zoology, and have been maintained by
random breeding in 40-liter glass aquaria. Four, 10
mm-diameter snails were selected and individually
isolated in 6-liter glass tanks. Snails were fed 3
times weekly with boOed dried lettuce and
commercial tropical fish food (Bio-rell, Sternco,
Harrison, New Jersey). The four test snails were
Photocell
Treadmill
E^^disc
FIG. 1. Cross section of treadmill appartus (right)
and the treadmill in % view (left). The lower disc
and lower 'A of the vertical axle were submerged.
The remainder of the unit was above the water
level. The upper disc and the light and photocell
were encased in an opaque shield to prevent
artifact caused by extraneous light.
104 THE NAUTILUS
October
maintained under cool, white fluorescent liglit for
a 12-hour light, 12-hour dark cycle. Liglit intensity
at the tank surface measured 1.400 lux (130 foot
candles). Tanks were continuously aerated through
a charcoal and glass-wool filter.
Snail activity was monitored by a treadmill
illustrated in figure 1. A horizontally oriented
plastic disc, 1 cm thick and 16 cm in circum-
ference, was balanced on a needle bearing and
connected by an axle extending above the water
surface to a second disc. The circumference of the
upper disc was marked with two wedge-shaped
masks. A beam of liglit was directed througli the
edge of the upper disc to a sensitive photo cell on
the opposite side of the disc. Rotation of the disc
in either direction resulted in a change in the liglit
passing througli the wedge-shaped mask and falling
on the photo cell. The photo cell output was
measured on a strip chart recorder (Beckman,
Fullerton, Calif.). Calibration permitted monitoring
of both direction and rate of rotation of the unit.
Snails were held in a plastic clip with the shell
aperture 3 mm away from and facing the
circumference of the submerged lower disc. On
emerging from its shell the snail's foot fell on to
the disc rim. All snails were able to crawl easily in
either direction with the shell rigidly held and
such crawling resulted in rotation of the treadmill
unit. All observations were carried out in a
photographic darkroom. Tlie snails were clamped
in the unit and then followed for a 3-hour
observation interval. With the room liglits turned
off there was no incident light in the test area.
With a single incandescent bulb turned on the
light intensity at the treadmill level was 88 lux (8
foot candles). Four ligliting patterns were tested as
follows: 3 hours of continuous liglit (L), 3 hours
of continuous dark (D), liglit on for ninety
minutes, dark for ninety minutes (L-D) and liglit
off for ninety minutes then turned on for ninety
minutes (D-L). The initial 30 minutes were
considered as a stabilization period and were
discarded for the purpose of observation. Crawling
rates in cm per hour were calculated for the 30 to
90 minutes (interval 1), 90 to 120 minutes
(interval 2), and 120 to 180 minutes (interval 3).
Each snail was observed througli 7 trials of each
light pattern. Light intensities were measured with
a Gossen Luna-Pro Cadmium sulfide type light
meter (Woodside, N. Y.).
1973
60
50
40
30
u20
Vol. 87 (4)
10
D^rk
Light
Dark Lighl Lighl D.uk
FIG. 2. Crawling rates observed during the three
periods of each lighting pattern. Dotted lines
represent the means of 7 trials for each snail. The
heavy lines represent the overall means for the
four snails.
RESULTS
Results are summarized in figure 2. Mean
crawling rates are plotted for periods 1, 2 and 3
of each ligliting pattern for each of the four snails
and an overall mean is indicated by the heavy
line. Analysis of the pattern yields the following
results. Mean rates during period 1 were higher
than the following periods. Mean rates during
period 2 were usually equal to or higlier than
those of period 3 except for the L-D lighting.
Wlien the light was turned off there was a pause
in activity expressed as a lower mean rate for
period 2 of the L-D trial. The maximum crawling
rate for Biomphalaria glabrata. 1 cm in diameter,
measured over a 10 minute intei"val was 90 cm an
hour and the maximum distance traveled during a
1 hour period of observation was 89 cm.
DISCUSSION
Three characteristics of light may be of signifi-
cance in affecting snail behavior. These are
intensity, duration and wave length, or color. A
number of investigators have commented on the
effects of the light intensity on snail behavior.
Deschiens (1957) described withdrawal of B. glab-
rata into its shell on exposure to intense liglit. A
withdrawal response on exposure to intense light
has been documented for the marine mollusk.
Vol. 87 (4)
THE NAUTILUS
105
Pleurobranchaea califomica (Davis and Mpitsos,
1971). Harry and Aldridge (1958) could not
confirm a difference in distribution of B. glabrata
between light and shade sections of the environ-
ment. Deschiensand Bijan (1956) described normal
behavior and normal fertility, fecundity and devel-
opment in B. glabrata maintained in darkness of
periods of up to 90 days. Joy (1971, a, b) studied
growth and oviposition of B. glabrata in changing
patterns of light and dark. A prevalence of
nighttime oviposition was demonstrated though the
differences between oviposition rates in the dark
and in the light narrowed as the dark interval was
shortened. When a greater portion of the light
energy was delivered in the infrared spectrum,
oviposition in the dark interval was favored.
Changes in the day length of plus or minus 2
hours did not affect the growth. Nocturnal
oviposition has been documented for other species
of gastropods, including Planorbarius conieus and
Helisoma trivolvis (Cole, 1925), Gyraulus parvus
(Krull, 1931) and Oncomelania quadrasi (Pesigan,
et al., 1958) and for the limpet Ancylus fuscus
(Clapp, 1921).
Four points are clear from the current study.
First, the threshold for Ught perception in B.
glabrata is at least as low as 88 lux (8 foot
candles). Second, B. glabrata may respond to
changes in light intensity as small as 88 lux (8
foot candles) with a change in activity. Third,
with sustained activity B. glabrata will tire.
Finally, the maximum rate of travel for B.
glabrata based on a 10 minute measurement is 90
cm per hour and the maximum observed distance
traveled on a one hour period was 89 cm.
The low levels of Hght intensity were selected
for this study to represent a better simulation of
changes in intensity in natural environments. A
number of investigators (Abbott, 1948; Kawanoto,
1952; Komiya, et al, 1959; Deschiens, 1957;
Moose and Williams, 1961-62) have documented
withdrawal reactions, or correlated behavior, of a
variety of snails when exposed to intense Ught.
While abrupt transition from deep shade to
brightly sunlit water could approach the levels
used by most of these investigators, it is more
frequent to find environmental changes of a
smaller magnitude. The fact that this snail does
respond to such low light intensities as 88 lux (8
foot candles) sets the physiologic limit of its
perception at an even lower level. Several investiga-
tors (Joy, 1971, a, b; van der Schalie and Davis,
1968; Yasuraoka, 1955; Pesigan, et al, 1958;
Clapp, 1921; Cole, 1925; KruU, 1931) reported an
effect of hght on oviposition by a variety of
molluscan species.
This study would add locomotive activity to
the Ust of behavioral alterations affected by
changes in ambient light. Several questions are
suggested by these observations, particularly the
effect of changes in light intensity when they
occur against a background level of ambient light
rather than the light to dark changes utilized here.
Also, the response to changes in Ught wave-length
would also be of interest. Such studies were
beyond the scope of the present investigation and
would entail such prolonged periods of observation
that another protocol permitting simultaneous
observation of multiple snails would probably be
necessary. In any event, changes of ambient
illumination of 88 lux (8 foot candles) to darkness
do result in measurable transient decrease in
activity of Biomphalaria glabrata. Oviposition on
the treadmill was never noted.
Snails were not fed during the trial. In the
absence of substrate, continued activity is marked
by a decrease in the rate of activity. Whether this
is a result of fatigue or whether the faUing activity
is a result of a substrate deficiency is not clear.
The cliche that our research proceeded at a snail's
pace rapidly lost favor in the laboratory; however,
it is the limiting factor in any behavioral study.
When the snail must choose among several environ-
ments, the speed with which the snail can sample
the environments controls the observation time.
Mixing times in tanks 1 meter long must be weU
in excess of 1 hour to permit vaUd observations of
B. glabrata the size with which we experimented.
Critical observation of snail activity should be an
integral part of the planning of any behavioral
study that depends upon snail migration.
LITERATURE CITED
Abbott, R. T. 1948. Handbook of medicaUy
important moUusks of the Orient and the
Western Pacific. BuU. Mus. Comp. Zool. Har-
vard. 100: 245-328.
Clapp, W. F. 1921. Eggs and young of the river
Umpet, Ancylus fuscus C. B. Adams. Boston
Soc. Nat. Hist. Occ. Papers. 5: 5-10.
106 THE NAUTILUS
October 1973
Vol. 87 (4)
Cole, W. H. 1925. Egg-laying in two species of
Planorbis. Am. Nat. 59: 284-286.
Davis, W. J. and G. J. Mpitsos. 1971. Behavioral
Choice and Habituation in the Marine Mollusk
Pleurobranchaea califomica MacFarland (Gastro-
poda, Opisthobranchia). z. vergl. Physio. 75:
207-232.
Deschiens, R. 1957. Sur la perpetuation des
elevages des mollusques vecteurs des bilharzioses
a Tobscurite. Bull. Soc. Path. Exot. 50:
229-233.
Deschiens, R. and H. Bijan. 1956. Comportement
d'elevages de mollusques vecteurs des bilhar-
zioses a I'obscurite. Bull. Soc. Path. Exot. 49:
658-661.
Harry, H. W. and D. V. Aldrich. 1958. The
ecology of Australorbis glabratus in Puerto
Rico. BuU. WHO. 18: 819-832.
Joy, J. E. 1971. The Influence of Light Condi-
tions upon the Egg-Laying of the Planorbid
Snail, Biomphalaria glabrata. The Nautilus 85:
43-49.
Joy, J. E. 1971. Tlie influence of day length upon
the egg-laying of Biomphalaria glabrata, Ann.
Trop. Med. and Parasit. 65: 573-578.
Kawanoto, S. 1952. On the photophobotaxis of
Oncomelania nosophora. Med. Biol. 23: 76-79.
Komiya, Y., K. Kuniko, and C. koyama. 1959. A
simple breeding method for Oncomelania using
a Petri dish. Jap. Jour. Parasitol. 8: 721-724.
KruU, W. H. 1931. Importance of laboratory-raised
snails in helminthology with life history notes
on Gyraulus parvus. Mich. Univ. Mus. Zool.
Occ. Papers. 10(226): 1-10.
Moose, J. W. and J. E. WiUiams. 1961-62. Medical
General Laboratory (406), U, S. Army Medical
Command, Japan, Professional Reports.
Pesigan, T. P., N. G. Hariston, J. J. Jauregui, E.
G. Garcia, A. T. Santos, B. C. Santos, and A.
A. Gesa. 1958. Studies on Schistosoma japon-
icum infections in the Phillippines. 2. The
moUuscan host. Bull. WHO. 18: 481-578.
van der Schalie, H. and G. M. Davis. 1968.
Culturing Oncomelania snails (Prosobranchia:
Hydrobiidae) for studies of Oriental schisto-
somiasis. Malacologia 6: 321-367.
Yasuraoka, K. 1955. The behavior of Oncomelania
nosophora, the intermediate host of Schisto-
soma japonicum, to light in water. Jap. Jour.
Med. Sci. Biol. 8: 323.
INDO-PACIFIC
MOLLUSCA
MONOGRAPHS OF THE MARINE MOLLUSKS OF
THE WORLD WITH EMPHASIS ON THOSE OF
THE TROPICAL WESTERN PACIFIC
AND INDIAN OCEANS
The most technical and most beautifully illustrated
journal now being published on Recent and Tertiary
marine moUusks. Over 20 professional malacologists are
currently contributing. Edited by R. Tucker Abbott.
Among the groups treated are Strombidae, Cassidae,
Tridacnidae, Turridae, Littorinidae, Phasianellidae, and,
soon to come, Patellidae, Harpidae and Mitridae.
Issued to date in looseleaf form with three sturdy,
permanent binders — 1100 pages, 810 plates (31 in full
color). Limited number of complete sets left, $91.90 U.S.
(foreign: $94.00), postage paid. Any number of extra
binders available at $6.00.
Published by
The Delaware Museum of Natural History, Box 3937, Greenville, Delaware 19807 U.S.A.
Vol. 87 (4)
THE NAUTILUS
107
ON THE IDENTITY OF HELICINA GRANULUM PFEIFFER
(PROSOBRANCHIA)
Morris K. Jacobson
American Museum of Natural History
Central Park West at 79th Street
New York, N. Y. 10024
ABSTRACT
Helicina granulum Pfeiffer, 1864 is shown to be a valid species, differing in
important morphological respects from H. tantilla Pilsbry, 1902. The former taxon
has been taken in several localities in the south central part of Oriente Province,
Cuba. The use of subgenus Poenia Adams & Adams, 1856 for H. granulum is shown
to be erroneous.
The taxon Helicina granulum Pfeiffer (ex MS,
Gundlach), 1864, has not been clearly understood
in the Uterature. Pfeiffer described the species on
the basis of a single specimen sent him from
Monte Toro, Guantanamo, Oriente Province, Cuba,
by Gundlach. He was moved to do this by the
unusually small size of the shell, smaller than any
known helicinid at that time. The original Latin
description and my English translation follow:
Helicina granulum Pfeiffer (1864, Malak. Blatt.
11: 161): "T. minuta, depressa, tenuiscula, laevi-
gata, translucida, succinea; spira parum conoi-
deo-elevata; anfr. fere 4 convexiusculi, ultimus
depresso-rotundatus, subtus medio subexcavatus,
levissime callosus; columella brevissima, verticahs;
apertura obhqua, late semiovalis; perist, breviter
expansum, margine basali arcuatin in columellam
transuente -- Operc? -- Diam maj. 2 2/3, alt. vix 1
mill. Habitat Monte Toro in districto Guanta-
namensi insulae Cubae."
"Shell minute, depressed, quite thin, smooth,
translucent, amber-colored; spire little conic-ele-
vated; whorls almost 4, rather convex, the last one
depressed rounded, subexcavated centrally below,
Ughtly callused; columella exceedingly short, verti-
cal; aperture oblique, widely semi-oval; peristome
briefly expanded, basal margin inserting arc-like
into the columella. Operculum? Major diameter 2
2/3 mm, altitude barely 1 mm."
It might be noted that Pfeiffer did not mention
the presence of axial sculpture, but this omamert-
tation could have been overlooked in a single dead,
minute specimen. However, as wall be seen later,
the references to an expanded peristome and an
arched basal insertion clearly point to granulum,
Pfeiffer's holotypic specimen was never figured
and was destroyed during World War II (Clench &
Jacobson, 1971a: 101). There are few subsequent
references to the species in the hterature: Pfeiffer
(1865: 233) reprinted his original description
verbatim and later (1876: 271) merely listed the
name. Sowerby (1866: 296) listed it as an
unidentified species, and Reeve (1874) and Wagner
(1910) omitted it entirely; nor did Fulton (1915)
FIG. 1. Lucidella granulum (Pfeiffer) between
Nimfitas and La Victoria, Monte Toro, Guanta-
nomo, Oriente Province, Cuba; Ramsden, leg. 1914,
ANSP 110769, 10 X.
108 THE NAUTILUS
October 1973
Vol. 87 (4)
mention it among the names omitted by Wagner
in his extensive monograph of the Helicinidae.
Arango (1879), Crosse (1890), and Aguayo &
Jaume (1948) repeated only the locaUty cited
originally by Pfeiffer, thus leading to the supposi-
tion that Pfeiffer's record is the only one known,
and that the species had not been collected again.
Clench & Jacobson (1971b) tentatively included it
in the genus Troschelviana, although Pfeiffer had
made no reference to a mucronate protoconch, a
diagnostic feature of the helicinine tribe Vianini in
which the genus Troschelviana belongs. There is no
reason to doubt that granulum belongs to the
genus Lucidella Swainson, 1840, as was noted by
Aguayo & Jaume (1948). However, their sub-
generic placement in Poenia H. & A. Adams,
1856, is erroneous. As the type-species of Poenia
they cited the subsequent designation by Fischer,
1885 of H. unidentata Pfeiffer. But since Fischer
did not use the word "type" in his citation, this
must be regarded as an example and is not a valid
designation. Pilsbry (1911, p. 585) vahdly desig-
nated Helicina depressa Gray, 1825, as the type.
Furthermore, Poenia has been regarded as a
synonym of Lucidella by both Thiele (1929: 88)
and Wenz (1938: 445). Because of the axial
sculpture, granulum belongs in the subgenus
Poeniella H. B. Baker, 1923, type species Helicina
plicatula christophori Pilsbry, 1897, by original
designation.
The vagueness regarding the identity of granu-
lum increased when it was confused with another
species, Helicina tantilla Pilsbry, 1902. This species
was described on the basis of a single specimen
taken near Palm Beach, Florida in 1899 together
with other small land shells in a forest about
one-quarter mile from the beach. Pilsbry wrote
that the new species was distinct from any other
Antillean helicinid. He did not compare it with
the description of granulum, which it closely
resembles, nor, as we have seen, were any
typological specimens of that species available for
study. Thus when Ramsden in 1914 sent him
some small shells from Monte Toro, Pilsbry
identified them as H. tantilla, overlooking the fact
that Monte Toro is the type locality of H.
granulum I have been able to examine these
specimens in the ANSP and they clearly differ
from tantilla and are undoubtedly topotypes of H.
granulum The specimen here illustrated is, there-
fore, a potential neotype.
Tlie differences between tantilla and granulum
are the following: the peristome of tantilla is
rounded and faintly thickened, but barely expand-
ed and not reflected, and the basal angle of
insertion in the body whorl is barely perceptible.
In granulum the hp is well expanded and slightly
reflected and the angle at the point of insertion is
quite distinct. In addition, the spire of granulum is
somewhat higher and the suture deeper.
Ramsden reported that he found the shell "in
dirt at the root of trees." Ramsden's description
of the supposed "tantilla" (1914: 50) clearly
refers to granulum since reference is made to an
expanded and reflected Up and a shallow notch at
the basal insertion.
There are several lots of granulum in the
Ramsden Collection labelled as Lucidella rugosa
Pfeiffer and coming from the following locahties:
Florida Blanca, Alto Songo; Km. 54, Sierra Canas-
ta, Santiago de Cuba; La Cueva, Diego Cobas,
Majaguabo, all from Oriente Province. In addition
the USNM has one lot from Guaso River, Monte
Libano, Guantanamo, and both the USNM and
ANSP have one lot each from the type-locality,
Monte Toro, Guantanamo.
Lucidella tantilla has also been reported from
Cuba in Cayo GuUlermo, northern Camagiiey
Province (Aguayo & Jaume, 1948) and from Cayo
Las Brujas, Caibarien, Las Villas Province (Clench
1959: 35). In addition. Clench records it from
Mores, Great Abaco, Bimini, and Great and Little
Inagua Islands in the Bahamas, and Pilsbry (1948:
1085) reports it from several localities in the
Florida Keys, as well as erroneously from Monte
Toro.
It is thus clear that Lucidella granulum is
confined to south central Oriente Province, while
L. tantilla occurs in the more western provinces' of
Camagiiey and Las Villas. From here tantilla
appears to have dispersed to the Bahamas and the
Florida Keys, since Pilsbry was most likely correct
when he wrote that the Florida specimen was
"probably a hurricane-borne waif from Cuba"
(1948).
I wish to express my gratitude to Dr. William
K. Emerson of the American Museum of Natural
History who discussed the problem with me and
critically read the manuscript. Dr. Robert Robert-
son of the Academy of Natural Sciences and Dr.
Vol. 87 (4)
THE NAUTILUS
109
Joseph Rosewater of the National Museum of
Natural History, Smithsonian Institution, most
generously permitted me to examine material in
their respective collections. I am indebted to the
kindness of Dr. Kenneth J. Boss for the photo-
graphs. The abbreviations ANSP and USNM stand
for the Academy of Natural Sciences of Philadel-
phia and the National Museum of Natural History,
Smithsonian Institution (formerly the United
States National Museum) respectively.
LITERATURE CITED
Aguayo, C. G. and M. L. Jaume, 1948. Cat&logo
molluscos de Cuba, HeUcinidae, no. 495, 1 p.
mimeo.
Arango, R., 1879. Contribucion a la fauna mala-
col6gica cubana, Helicinidae, Havana, pp. 41-57.
Baker, H. B., 1923. The Mollusca collected by the
University of Michigan - Williamson Expedition
in Venezuela. Occ. Papers Mus. Zool. Univ. of
Michigan, no. 137, 58 pp., 5 pis., 21 figs.
Qench, W. J., 1959. Land and freshwater mollusks
of Great and Little Inagua, Bahama Islands.
Bull. Mus. Comp. Zool., Cambridge, Mass.,
121(2): 29-54, 1 pi.
Clench, W. J. and M. K. Jacobson, 1971a. Mono-
graph of the Cuban genera Emoda and Glyp-
temoda. Bull. Mus. Comp. Zool. 141(3):
99-130, 7 pis.
Clench, W. J. and M. K. Jacobson, 1971b. A
monograph of the genera Calidviana, Ustronia,
Troschelviana, and Semitrochatella in Cuba.
ibid., 141(7): 402-463, 8 pis., 1 text fig.
Crosse, H., 1890. Faune malacologique terrestre et
fluviatile de I'ile de Cuba. Jour. Conchyl. 38:
173-335, pis. 4-6.
Fischer, P., 1885. Manuel de Conchyliologie, Paris,
pp. 794-797, figs. 554-556 (Helicinidae).
Fulton, H. C, 1915. On Dr. Anton Wagner's
monograph of Helicinidae in the Conchy-
lien-Cabinet. Proc. Mai. Soc. London, 11:
237-241; 324-326.
Pfeiffer, L., 1864. Zur Molluskenfauna von Cuba.
Malak. Blatt. 11: 157-161.
Pfeiffer, L., 1865. Monographia Pneumono-
pomorum Viventium, suppl. 2, 284 pp.
Pfeiffer, L., 1876. ibid., suppl. 3, 10 + 479 pp.
Pilsbry, H. A., 1902. A new Floridian Helcina,
Nautilus 19: 53.
Pilsbry, H. A., 1948. Land Mollusca of North
America. Monograph 3, Acad. Nat. Sci. Phila-
delphia 2(2): 1078-1090, figs. 576-581 (HeUcini-
dae).
Pilsbry, H. A. and A. P. Brown, 1911. The Land
Mollusca of Montego Bay, Jamaica; with Notes
of the Land Mollusca of the Kingston Region.
Proc. Acad. Nat. Sci. Phila. for 1911, p. 585.
Ramsden, C. T., 1914. Notes on some land shells
of eastern Cuba. The NautUus 28: 49-51, pi. 2,
Reeve, L., 1874. Conchologia Iconica, 19: 34 pis.
-H text (Helicinidae).
Sowerby, G. B. II, 1866. Thesaurus Conchyliorum,
3: 277-302, pis. 266-278 (Helicinidae).
Thiele, J., 1929. Handbuch der systematischen
Weichtierkunde, Jena, 1: 80-91, figs. 57-67
(Helicinidae).
Wenz, W., 1938. Gastropoda [in] Handbuch der
Palaozoologie, BerUn, pp. 435-448, figs.
1061-1118 (Helicinidae).
Wagner, A. J., 1910. [in] Martini and Chemnitz,
Conchylien-Cabinet (2) 1: sect. 18, pt. 2, pp.
337-351, pis. 67-69. (Lucidella)
110 THE NAUTILUS
October 1973
Vol. 87 (4)
THE VALVULAR MEMBRANE IN YOUNG
MACTRID CLAMS, SPISULA SOLIDISSIMA
Wayne D. Cable
National Marine Fisheries Service
Middle Atlantic Coastal Fisheries Center
Milford Laboratory
Milford, Connecticut 06460
ABSTRACT
Juvenile surf clams, Spisula solidissima, were reared from fertilized eggs in the
laboratory. Observations were made of the appearance and activity of the valvular
membrane (primary exhalant siphon), which has not previously been reported in
recently-metamorphosed animals.
The siphonal system of the bivalve mollusks has
been considerably studied. Aspects of mantle
fusion in the Lamellibranchia and the subsequent
formation of siphons from the mantle folds were
described in detail by Yonge (1957). Development
of siphons in the evolution of the lamellibranchs
enabled this group of animals to live in the shelter
of a substrate while obtaining food and oxygen
from the water above the substrate (Yonge, 1957).
In discussing the types of siphon systems,
FIG. 1. Juvenile Spisula solidissima with the
valvular membrane, or exhalant siphon, (on the
left) fully extended to a length of 1.5 mm.
FIG. 2. Juvenile Spisula solidissima, valvular mem-
brane (on the right) collapsed but not inverted
within shell.
Vol. 87 (4)
THE NAUTILUS
111
Yonge ascribes to the Mactridae what he terms a
"type C" siphon system. In this type the opening
of the definitive exhalant siphon is usually bound-
ed by a valvular membrane (a narrow flange just
inside the ring of tentacles) which, when open,
controls and directs the flow of water from the
exhalant siphon. However, he does not illustrate
this structure in any of the Mactridae, nor does he
show how this structure is formed in the young of
the Mactridae. Prior to development of the
definitive siphonal system in many recently meta-
morphosed Lamellibranchia a precursor of the
definitive exhalant siphon, a valvular membrane or
primary exhalant siphon is formed (Quayle, 1952;
Carriker, 1961).
The presence of the valvular membrane in
newly metamorphosed Spisula solidissima has been
recenfly observed by the author. There was no
question as to the identity of these young surf
clams since they were reared from fertilized eggs
spawned in the laboratory. The presence of this
structure and its appearance may serve as an aid
to identification of young juvenile surf clams
gathered in the field.
Photographs were made approximately one
month after metamorphosis; the size range of the
young clams then ranged from 0.5 mm to 3.0
mm. Photograph #1 shows the siphons of a young
clam 1.5 mm long. Here the valvular membrane is
fully extended. Photograph #2 shows the valvular
membrane in a state of collapse and dangling
externally; this clam is also 1.5 mm long.
One should notice that the state illustrated in
these photographs is an advanced one, in that
juvenile Spisula solidissima of this size have
already developed the inhalant siphon with its ring
of tentacles, and the tentacles of the exhalant
siphon have also begun to form. These structures
are formed subsequent to the development of the
valvular membrane.
The valvular membrane was observed to be an
extremely flexible and active structure. It was
rapidly extended when the young clam was
pumping water through the mantle cavity, and
rapidly withdrawn or inverted within the mantle
cavity when the clam was disturbed.
The presence of such a "filmy membrane" on
the excurrent siphon on young clams, which
moved in and out with a folding motion and was
held out as a hose to direct flow of water from
the exhalant opening, was described in Mercenaria
mercenaria by Belding (1912). Carriker (1961) has
subsequently described in some detail the develop-
ment of this membrane in young Mercenaria
mercenaria ranging from 210 to 300 ^.
The valvular membrane of recently meta-
morphosed bivalve moUusks appears to function to
deflect the excurrent and incurrent streams during
the period of definitive siphon formation. The
same function would be served in later life by the
shght offset of the tips of the siphons and the
smaller exhalant siphon orifice (Carriker, 1961). In
describing a similar membrane in young Mya
arenaria and Venerupis pullastra, Quayle (1952)
reported the function of this structure to be one
of keeping the mantle and gills free of feces by
directing them away from the vicinity of the
young animal.
Since siphon formation takes place considerably
after metamorphosis and the loss of the velum,
there is a sedentary phase prior to the time when
the siphons are formed and the animal is able to
enter the substrate (Carriker calls this the byssal
plantigrade). He believes it probable that young
byssal plantigrade Mercenaria mercenaria cannot
burrow until the ring of tentacles is available on
the inhalant siphon to exclude sedimentary grains.
This is most likely true for other lamellibranchs
that also live in soft substrates, including the
Spisula solidissima described here.
LITERATURE CITED
Belding, D. L. 1912. Report on the Quahaug and
Oyster Fisheries of Massachusetts, Common-
wealth of Massachusetts, Boston.
Carriker, M. R. 1961. Interreladon of Functional
Morphology, Behavior, and Autecology in Early
States of the Bivalve Mercenaria mercenaria.
Journal of the Elisha Mitchell Scientific Society
77 (2): 168-241.
Quayle, D. B. 1952. Structure and Biology of the
Larva and Spat of Venerupis pullastra (Mon-
tagu). Trans. Roy. Soc. Edinburgh 62 (8);
255-297.
Yonge, C. M. 1957. Manfle Fusion in the
Lamellibranchia. Pubbl. Staz. Zool. NapoU 26:
151-171.
112 THE NAUTILUS
October 1973
Vol. 87 (4)
SIZE AND SEX RATIO DIFFERENCES IN UROSALPINX CINEREA
(SAY) (MURICIDAE) FROM GREAT BAY, NEW HAMPSHIRE'
Kenneth W. Turgeon
and
Richard A. Fralick
Jackson Estuarine Laboratory, University of New Hampshire
Adams Point, Durham, New Hampshire 03824
ABSTRACT
Three hundred and ninety-seven Urosalpinx cinerea from Great Bay, New
Hampshire, were sexed and measured for total shell length. Statistical comparison of
the mean shell lengths and chi-square analysis of sex ratios for several size classes
show that females are significantly larger than males. Hypotheses to account for this
sexual dirmorphism are presented.
INTRODUCTION
Previous investigators have noted in several
populations of the common oyster drill, Uro-
salpinx cinerea (Say), that females attain a greater
maximum shell length than males (Federighi,
1931a, 1931b; Cole, 1942; Hargis and MacKenzie,
1961). However, none of these workers demon-
strated statistically significant differences in mean
shell lengths between the sexes. Griffith and
Castagna (1962), working with Urosalpinx cinerea
folly ensis (Baker, 1951) from Chincoteague Bay,
Maryland, showed that females, in addition to
having a greater maximum shell length, had a
mean shell length significantly greater than males.
Our paper reports the results of a similar study
conducted on U. cinerea from Great Bay, New
Hampshire.
Great Bay is a shallow, highly turbid estuary
with a mud-silt bottom. Yearly salinities range
from approximately seven ppt during the spring
freshet to 30 ppt in late summer in the mid and
lower reaches of the Bay. The drills are limited in
their distribution to the few, remaining oyster
reefs and are present in very low abundance. Drill
density is approximately one to two individuals
per square meter of oyster reef. However, they are
often distributed in widely separated clusters of
four to seven individuals.
METHODS
Approximately 500 oyster drills were
hand-collected during the summer of 1972 by
'Jackson Estuarine Laboratory Scientific Contri-
bution No. 1.
scuba divers. The collection site was an oyster reef
located in the mid-portion of Great Bay encom-
passing an area of about 30,000 square meters.
The divers collected all drills sighted. Trapping
techniques were not employed since bias for a
particular size or sex might have resulted. Griffith
and Castagna (1962) found that male:female ratios
differed between trap-collected and hand-collected
drills. The low population density of the Great
Bay drills and the Irigh turbidity of the water
necessitated numerous dives in order to collect
sufficient numbers for statistical analyses. Only
individuals greater than 10 mm in length and
exhibiting a complete lack of a penis (females) or
presence of a well-defined, C-shaped penis (males)
were used. Smaller individuals were not used since
they are extremely difficult to sex and quite often
have not reached sexual maturity. Sexing was done
by the live method of Hargis (1957) using 5 X
and 10 X hand magnifiers. Shell length was
measured to the nearest 0.1 mm with vernier
calipers. Drills, after being sexed and measured,
were assigned to one of four, pre-determined size
classes: >\0 & < 15 mm (class 1), > 15 & < 20
mm (class 2), > 20 & < 25 mm (class 3) and >
25 mm (class 4). These size classes were arbitrarily
chosen and do not represent natural breaks in size
distribution. Statistical comparison of female and
male mean shell lengths was by Cochran's approxi-
mation of the Behrans-Fisher test (Snedecor,
1956). Chi-square analysis was used to determine
significant deviations from 50-50 sex ratios for the
individual size classes and the total sample. All
statistical analyses were evaluated at the 99
percent confidence level.
Vol. 87 (4)
THE NAUTILUS
113
RESULTS
The results of this study are presented in
figures 1 and 2. Females had a maximum shell
length of 38.3 mm and a mean shell length of
20.2 mm. The respective values for males were
30.0 mm and 17.8 mm. Statistical analysis showed
that the mean shell lengths were significantly
different. Two hundred and thirty-three drills
(58.69%) were females and 164 (41.31%) were
males. This is a female: male ratio of 1.42:1 and
represents a significant deviation from a 50-50 sex
ratio. Significant deviations in sex ratios occurred
in size classes 3 and 4, the female: male ratios
being 1.73:1 and 18:1 respectively. The sex ratios
for size classes 1 and 2 showed no significant
deviation from a 50-50 sex ratio (0.95: 1 and
1.09:1). One hundred females (42.9%) and 39
males (23.7%) were 20 mm or more in length,
while 36 females (15.4%) and only 2 males (1.2%)
were 25 mm or more in length. Eleven females
(4.7%) were greater than 30 mm in length.
DISCUSSION
The results of our study clearly indicate that
sexual dimorphism exists in oyster drills from
Great Bay, New Hampshire. In addition, our work
suggests that this dimorphism is due to the
significantly greater number of females than males
in the larger size classes. This preponderance of
large females was sufficient to yield a significant
deviation from a 50-50 sex ratio.
The sexual dimorphism in Great Bay drills may
be attributable to the following reasons: females
have a faster rate of growth than males, females
? 20-
LENGTH IN MM
FIG. 1. Length-frequency and size distribution of
Urosalpinx cinerea from Great Bay, New Hamp-
shire. Upper figure represents range, mean and ±
one standard deviation.
live longer than males and thus have a longer
period of growth, or both. Another possibility is
that sexually mature males undergo a sex trans-
formation into females. The occurrence of female
U. cinerea with structures resembling vestigal penises
suggests that this deserves investigation.
LITERATURE CITED
Baker, Bemadine B. 1951. Interesting shells from
the Delmarva Peninsula. Nautilus 64 (3): 73-77.
Cole, H. A. 1942. The American whelk tingle,
Urosalpinx cinerea (Say), on British oyster beds.
J. Mar. Biol. Assoc. U. K. 25: 477-508.
Federighi, H. '1931a. Further observafions on the
size of Urosalpinx cinerea Say. J. Conchol. 19:
171-176.
Federighi, H. 1931b. Studies on the oyster drill
{Urosalpinx cinerea Say). Bull. U. S. Bur. Fish.
47 (4): 83-115.
Griffith, G. W. and M. Castagna. 1962. Sexual
dimorphism in oyster drills of Chincoteague
Bay, Maryland-Virginia. Chesapeake Sci. 3(3):
215-217.
Hargis, W. J., Jr. 1957. A rapid live-sexing
technique for Urosalpinx cinerea and Eupleura
caudata with notes on previous methods. Lim-
nol. Oceanogr. 2: 41-42.
Hargis, W. J., Jr. and C. MacKenzie. 1961. Sexual
behavior of the oyster drills: Eupleura caudata
and Urosalpinx cinerea. Nautilus 75 (1): 7-16.
n?
80-
\-
z
Ld
^ 60H
u
Q.
40-
3 4
SIZE CLASSES
FIG. 2. Percent distribution of female and male
Urosalpinx cinerea from Great Bay, New Hamp-
shire in each size class. * = Significant deviation
from a 50-50 sex ratio.
1 14 THE NAUTILUS
October 1973
Vol. 87 (4)
THE MOLLUSCA OF CANADARAGO LAKE
AND A NEW RECORD FOR
LASMIGONA COMFRESSA (LEA)
Willard N. Harman
New York State University College at Oneonta
Oneonta, N. Y. 13820
Canadarago Lake is located in Otsego County,
New York (42°50'N, 75°00'W). The lake is 3
miles long, averages 1 mile in width and has a
surface area of 761 hectares. It is shallow and
turbid with the greatest depth being only a little
over 12 meters and secchi transparencies averaging
less than 2 meters. Summer epilimnion tempera-
tures attain 25°C. Oxygen is absent from the
hypolimnion during these periods and varies near
saturation at the surface. Hydrogen ion concentra-
tion is extremely erratic, varying from about 4.5
to 10 in both surface and profundal waters (Fuhs,
1972). Canadarago would be expected to be a
moderately eutrophic lake in its natural state but
is now highly eutrophic as a result of sewage
input from the village of Richfield Springs and
from summer camps. Blue-green algal blooms are
common and the undersides of cobbles are covered
with fungi and bacteria. Turbid waters prevent the
extensive growth of rooted macrophytes, although
Myriophyllum is abundant in the shallows. Com-
mon emergent plants are Scirpus, Nuphar,
Nymphaea, Pontederia, Typha, and Sparganium. A
eutrophication study of the lake was begun in
1968 by the New York State Department of
Health and the New York State Department of
Environmental Conservation. As a result, a tertiary
sewage treatment plant was installed at Richfield
Springs and was activated in February 1973.
This survey of the moUuscan fauna was under-
taken for the acquisition of base hne data that
can be used for comparison with studies in future
years to indicate possible improvements in water
quality. Samples were made at 9 stations in both
deep waters and Uttoral areas. It appears that
Canadarago once supported dense populations of
mollusks that are now severely depleted. We found
an abundance of empty shells of Lymnaea humilis,
L. palustris, Gyraulus parvus, Helisoma anceps,
Ferrissia parallela, Physa spp., Viviparus georgianus,
Amnicola limosa, A. Integra, Valvata tricarinata,
Lampsilis radiata, and Pisidium spp. Only a few
hving specimens of L. humilis, G. parvus, F.
parallela, Physa sp. and Pisidium spp. were col-
lected. All Physa, empty shells and living speci-
mens, were so small as to prevent confident
determination to the species level. One living
specimen of Lasmigona compressa (Lea) (Union-
idae) was found at the entrance of Herkimer
Creek into the lake. This is the first record of this
species in the Susquehaima River watershed.
After noting the condition of the molluscan
fauna in the Lake we made collections along 5
miles of Oaks Creek, the outlet of Canadarago, to
ascertain if water quality improved downstream
from the lake. The only snail found was an
immature Physa sp. A few living specimens of the
bivalves Lampsilis radiata, Elliptio complanatus and
Strophitus undulatus were found. Empty shells of
all the mollusks found in Canadarago Lake were
collected.
LITERATURE CITED
Fuhs, W. 1972. Canadarago Lake eutrophication
study. Lake and tributary surveys 1963-1970.
Methodology and Data. N.Y.S. Dept. of En-
viron. Cons., Research and Development Unit.
292 pp.
Vol. 87 (4)
THE NAUTILUS
115
OBITUARY
Elmer P. Cheatum
(1901-1973)
On May 1, 1973, science and education lost
one of their most notable contributors with the
death of Dr. Elmer P. Cheatum. Throughout his
48 years of service at Southern Methodist Uni-
versity he remained a leader of Southwestern
scientific investigation and educational inspiration.
Elmer Phillip Cheatum was born in Langdon,
Kansas, July 19, 1901. He grew up in rural
surroundings assisting in his father's general store.
As a young man, he washed dishes in a hotel near
Southwestern College where he earned his B.A. in
biology (1921-1924). He was also a good athlete,
setting the Kansas record for the sprint race that
stood for some time. Later, he earned his M.S. in
zoology at Kansas State College (1924-1925). At
this time, he married Edith Deck and left alone
two days later to assume a job as instructor at
Southern Methodist University. Five weeks later he
had earned enough money to bring his bride to
Dallas. During summers and for two winters he
and Edith traveled to the University of Michigan
where he gained his Ph.D. in aquatic biology
under such people as Dr. Paul Welch (1931-1933).
As a scientist and educator. Dr. Cheatum
worked in several fields, parasitology, entomology,
malacology and Umnology. Although he continued
to teach in these fields and in comparative anatomy,
his main research interest gravitated to the Mol-
lusca. He pubUshed over 30 scientific articles,
some in The Nautilus (1934-1972). Most were
concerned with the area he loved most, Texas.
His academic affiliations were numerous. He
was a member of Sigma XI, a fellow in the
A.A.A.S., a member of the American Microscopical
Society, a fellow and past President (1941-1942)
of the Texas Journal of Science, a member of the
Texas Ornithological Society and the Limnologjcal
Society of America. In Dallas, he belonged to the
S.M.U. Men's Faculty Club, Town & Gown Qub,
and he was a director of the Junior Leader
Training, Circle Ten Council, Boy Scouts of
America. For his leadership in Boy Scout work, he
was given the Silver Beaver Award.
Although Dr. Cheatum was a moving force in
the scientific worid, I think his true greatness lay
in his teaching. He had the unique ability to
inspire student thought and activity far beyond
the classroom. He led students to almost every
type of environment that Texas had to offer.
These field trips with Dr. Cheatum were truly
experiences that few students ever forget. Dr.
Cheatum's life work and collections have been
transferred to the Dallas Museum of Natural
History.
by Richard W. Fkllington
Dallas Museum of Natural History
P. O. Box 26193, Fair Park Sta., Texas 75226
JUST PUBLISHED
Third Edition, enlarged and
completely rewritten,
now includes shells
of the West Indies,
This enlarged edition of the Atlantic Coast
shell guide takes its place as an up-to-date
counterpart of the author's Field Guide to
Shells of the Pacific Coast and Hawaii.
More species and new material on individual
shells have been included, and information in
earlier editions has been brought up to date
throughout. Redesigned and entirely reset, the
new edition covers 1035 shells, 1033 of which
are illustrated with photographs. All the plates
are new, and there are 31 additional plates.
Changes in typography and arrangement en-
hance the ease of use. Boldfaced subheadings
point up facts about range, habitat, and physi-
cal characteristics. Illustrations are conven-
iently located in the center of the book for
quick reference. And the area of coverage has
been expanded to include the more common
shells of the West Indies— a boon to those who
visit the Caribbean.
Introductory sections contain all the help and
advice a beginner needs to start him on a fasci-
nating hobby. For the experienced collector
there exists no equally satisfactory one-volume
guide to identification.
A Field Guide to Shells
OF THE ATLANTIC AND GULF
COASTS AND THE WEST INDIES
By Percy A. Morris
EDITED BY WILLiAM J. CLENCH
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MOLLUSK VOUCHER SPECIMENS
It is becoming increasingly important for future
research purposes that an identified sampling of
species mentioned in pubHcations be deposited in
a permanent, accessible museum speciahzing in
mollusks. This is particularly true of mollusks used
in physiological, medical, parasitologjcal, ecological,
and experimental projects.
The Delaware Museum of Natural History has
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MBl. WHOI I IHKARY
liJH 17XV Z