NEPHRONAIAS. This genus has for its type the _Unio plicatulu

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THE

NAUTILUS

A QUARTERLY

DEVOTED TO THE INTERESTS

OF CONCHOLOGISTS

EDITORS AND PUBLISHERS:

H. A. PILSBRY, Special Curator of the Department of Mollusca, Academy

of Natural Sciences, Philadelphia.

C. W. JOHNSON, Curator of the Boston Society of Natural History.

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Vol. XXXI. OCTOBER, 1917. No. 2

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CONTENTS:

Notes on the variation of Ischnochiton conspicuus. By _E. P. Chace_ 37

Lampsilis ventricosa cohongoronta in the Potomac River. By _Wm. A.

Marshall_ 40

Collecting about Guantanamo Bay, Cuba. By _John B. Henderson_ 41

Amnicolidæ from Oneida Lake, N. Y. By _H. A. Pilsbry_ 44

New Genera and Species of Central American Naiades. By _L. S.

Frierson_ 47

On the rate of growth of pond Unios. By _L. S. Frierson_ 49

A new South African Nesopupa. By _H. A. Pilsbry_ 50

A new Gundlachia from Guatemala. By _Bryant Walker_ 51

A list of shells from the East Coast of Florida. By _Bryant Walker_ 53

Collecting in Digby, Nova Scotia. By _Lilian Dyer Thompson_ 57

A new type of the naiad-genus Fusconaia. By _A. E. Ortmann_ 58

The Relation of snail fauna to floods. By _A. Richards_ 64

William Bullock Clark 68

Publications received 69

Notes 71

═══════════════════════════════════════════════════════════════════════

C. W. JOHNSON, Business Manager,

Boston Society of Natural History,

Berkeley Street,

Boston, Mass.

Entered as Second-Class matter at the Boston Post-Office.

The Cruise of the “Tomas Barrera”

By JOHN B. HENDERSON

32 full-page illustrations in black and white. 5 color plates. 5 maps.

Octavo. $2.50 net.

This is the narrative of a scientific expedition to Western Cuba and the

Colorados Reefs, with observations on the Geology, Fauna, and Flora of

the region, undertaken in May and June, 1914, under the joint auspices

of the Smithsonian Institution and the Cuban Government.

“A genuine feast for the reader. It is a narrative replete with

interest concerning the roads, mountains, trees, dwellings, the

inland lakes and ponds (alive with queer fish), many species of

mollusca, found along the coast; the land crabs and their curious

habits,” etc.—_Louisville Courier Journal._

ALL BOOKSELLERS

NEW YORK =G. P. PUTNAM’S SONS= LONDON

2 West 45th St. 24 Bedford St.

NEW SHELL LISTS FREE.

A new list of Philippine Land Shells covering many of the most beautiful

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priced at 5 to 10 cents per species. Two lists of the finer cabinet

shells, the more aristocratic forms. List of American Land Shells.

Illustrated list of Philippine Shells. Further lists in preparation. I

desire correspondence with collectors who wish to build up large and

extensive cabinets. I have in stock over three times as many species as

are covered by my lists. Collections of a strictly scientific nature

purchased for cash.

WALTER F. WEBB,

202 Westminster Road,

ROCHESTER, N. Y.

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FOR EXCHANGE: Marine shells from various parts of the world, for others.

Send lists.

J. R. LEB. TOMLIN, 120 Hamilton Road, Reading, England.

[Illustration:

WASHINGTON MEETING, 1914

Bryant Walker

Geo. H. Clapp

T. H. Aldrich

John B. Henderson

H. A. Pilsbry

Wm. H. Dall

Paul Bartsch

]

THE NAUTILUS.

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VOL. XXXI. OCTOBER, 1917. NO. 2

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NOTES ON THE VARIATION OF ISCHNOCHITON CONSPICUUS CPR.

BY E. P. CHACE.

To the naturalist the study of variation and environment and their

relation to each other is always interesting and to the conchologist who

studies his shells in their natural surroundings as well as in the

cabinet many things are revealed. It is not, often, however, that

variation in form may be so easily traced to qualities of environment as

in the following instance.

_Ischnochiton conspicuus_, Cpr. is common at San Pedro and is usually

found on the under side of rocks in sandy tidepools. In this situation

they grow quite regularly, showing but slight variation in form. They

are active fellows and evidently sensitive to light; for if the rocks to

which they are clinging are turned over, they soon glide away, always

taking the shortest route to the under side of the rock.

While cleaning a lot of this species taken at San Pedro last fall two

specimens were noticed which differed so widely from the others that

they might easily have been mistaken for another species. They were much

wider and lower-arched than the typical form and the posterior corners

of the valves were rounded off, making the lateral areas very narrow.

Hoping to find more specimens of this odd form, a trip to Point Firmen

was devoted wholly to the collection of chitons, with interesting

results. The usual species were found in the tidepools including

numerous specimens of _Ischnochiton conspicuus_ of the ordinary form.

Ledges of soft rock beyond the tidepools contained many old pholad holes

and in these were found the form for which I was searching. Twenty

specimens of various sizes were collected from as many pholad holes. In

the larger specimens the foot had become so greatly enlarged to fit the

concave bottoms of the holes that it was impossible for them to curl up

in the usual manner. Some of these specimens were so badly eroded by the

sand and gravel which wash in and out of the holes that the anterior

valve was reduced to two thirds of its normal height.

In color pattern, sculpture, and mantle characters these specimens were

identical with those from the tidepools, and, as will be seen by

referring to the table of measurements, the smaller specimens approach

quite closely to the proportions of the typical or tidepool forms.

TYPICAL OR TIDEPOOL FORMS. ║ SPECIMENS FROM PHOLAD HOLES.

(Lot 1) ║ (Lot 2)

_Lon._ _Lat._ _Index._ _Div._ ║ _Lon._ _Lat._ _Index._ _Div._

99 35 2.52 130°║ 65 33 1.97 135°

83 33 2.51 130°║ 63 32 1.97 155°

83 30 2.76 125°║ 62 27 2.29 140°

62 22 2.80 125°║ 60 30 2.00 130°

59 23 2.56 130°║ 56 29 1.93 130°

38 14 2.71 130°║ 42 17 2.47 130°

In brief, Lot 1 shows an angle of divergence constant at 125° to 130°,

where Lot 2 shows an angle varying from 130° to 155°, and a proportion

of length to width 2.51 to 2.80 as against a proportion ranging from

2.47 to 1.93.

The noticeable differences to the eye are first, the narrow and sharply

raised lateral areas, and second, the shape of the posterior edge of the

median valves. In the tidepool specimens the posterior or exposed edge

of each valve is a straight line, while in specimens from the pholad

holes this line becomes a double convex curve, the most posterior

portion of the valves being about midway between the beaks and the

girdle.

These differences seem to be explained by the following facts. In

collecting, the tidepool specimens are usually found on the under side

of large rocks and well back from the edge. This situs protects them

from the light which they evidently find objectionable, but it makes

necessary a nightly journey of about two feet to the nearest growth of

algae on which they feed. This activity stretches the girdle downward

from the edges of the valves and permits a free play of all the valves

so that the mantle deposits its shelly secretions according to the

normal habit of the species. The specimens living in the pholad holes,

however, apparently never leave them as they are frequently found

feeding on the fucus which overhangs them. It protects them from the

light, so they have no occasion to move about, and the sand which is

washed down into these burrows would make re-entrance almost impossible.

A series of these specimens shows a gradual change of form. The young

specimens are very similar to young specimens from the tidepools, but as

they increase in size they become crowded so that the valves press

against each other, especially at the posterior end where the valves are

bent back across the bottom of the hole. This crowding of the valves

upon each other and the crowding of the girdle against the outer edges

of the valves so displaces portions of the mantle as to cause the

changes noted above.

Several specimens from each situs were disjointed and a study of the

individual valves showed that those from pholad-hole specimens were

thicker and had shorter sutural plates and a wider sinus, this last

being especially noticeable in the valves from the posterior end.

Apparently this change in the sinus is the result of the broadening of

the connecting ligaments due to compression by the crowding valves.

A count of the insertion plates of these disjointed specimens was made

and considerable variation noticed. So much, in fact, that more

specimens were pulled apart for the express purpose of counting these

plates. Representative counts were as follows: 9 slits on the anterior

valve, 2‒3 on the median valves, and 10 on the posterior. Others show

12, 2‒3, 8; 11, 2‒3; 14, 3‒4, 11. Absolutely no difference in this

character could be found between specimens from the tidepools and those

from the pholad holes.

On page 64 of vol. xiv of the Manual of Conchology, Dr. Pilsbry says,

“Carpenter has given a varietal name to a broad, worn specimen which he

thus describes:

“Var. _solidus_. Very solid, wide, ashen; inside whitish, the posterior

valve with 10, central valve 2‒3, anterior valve 12 slits. Length 72,

breadth 40, divergence 130°. Carpenteria, near Sta. Barbara, Cal. This

is scarcely more than an individual variation. The mantle (girdle) is

normal. The sculpture is worn away except at the edge. It has evidently

lived in a very exposed situation.”

From this description and the figure which he gives of the valves it

would seem that this is the same form as my specimens from the pholad

holes. I fully agree with Dr. Pilsbry that it is hardly worthy of

varietal rank. It is, however, too distinct in appearance to be labeled

simply _Ischnochiton conspicuus_, Cpr., and I have therefore marked

these specimens from the pholad holes _I. conspicuus_, Cpr., _form

solida_, Cpr., using the term _form_ as advocated by Dr. Cockerell, “to

designate variations plainly due to environment.”[1]

LAMPSILIS VENTRICOSA COHONGORONTA IN THE POTOMAC RIVER.

BY WILLIAM A. MARSHALL.

In 1912 Dr. A. E. Ortmann recorded[2] finding in the Potomac River a

variety of _Lampsilis ventricosa_[3] to which he gave the name

_cohongoronta_. His records were:

September 4, 1909. Potomac River, Hancock, Washington, Co., Md. (about

two dozen).

May 9, 1911. South Branch, Potomac River, Southbranch, Hampshire Co.,

W. Va. (about a dozen).

August 16, 1911. Shenandoah River, Harper’s Ferry, Jefferson Co., W.

Va. (a single male, below medium size).

May 6, 1912. South Branch, Potomac River, Romney, Hampshire Co., W.

Va. (about a dozen).

Dr. Ortmann remarked “It is probable that this species will turn up

elsewhere in the Potomac. The localities known at present are all to the

west of the Blue Ridge Mountain, that is to say, within the Great

Alleghany Valley and the Alleghany Mountains.”

Perhaps the above prediction has been realized in a specimen found at

Great Falls, Md., by Mr. Manly D. Barber of Knoxville, Tennessee, in

Sept. 1915. At that time Mr. Barber brought to the National Museum a

basketful of naiades which he had collected the same day at Great Falls,

about 18 miles above Washington. Among the shells, which were mostly

dead ones, was a specimen of _cohongoronta_, dead, but in a fine state

of preservation and with the periostracum nearly unblemished except for

the usual erosion at the beaks. Its appearance indicated that it had

been recently alive and that its home had been in the immediate vicinity

of the place in which it was found. Had it been washed down from

Harper’s Ferry, some 50 or more miles above Great Falls it probably

would have shown ill effects from so long a journey.

When found the two valves were separated, but so accurately do they fit

together that it is evident they belong to the same individual. The fact

that the valves were separated and yet were found near each other is

additional (though not conclusive) evidence that they had not been

transported any great distance by currents. At any rate this is the

first recorded finding of the species in the Potomac River so far south

as Great Falls.

The specimen is rather a small one. It measures, length 71 mm.; height

47 mm.; diameter 28 mm. It is in the collection of the U. S. National

Museum, catalogue number 273834.

COLLECTING DAYS ABOUT THE NAVAL STATION, GUANTANAMO BAY, CUBA.

BY JOHN B. HENDERSON.

In March last, while waiting for a boat to take us to Haiti, Dr. Bartsch

and I spent nearly three weeks at the U. S. Naval Station at the

entrance to Guantanamo Bay. We employed our time in exploring the

country about and subjecting it to a high degree of intensive

collecting. In this eastern corner of Cuba the coastal strip of some ten

miles in width is a semi-arid region with a complex of mountains that

are either quite bare of trees or, at most, covered with a scrub forest

and low-growing spiny shrubs, with, here and there, a wealth of cacti

that almost suggests Lower California. The rock foundation of all this

region,—barring some shore strips of very recently elevated coral, is

everywhere composed of about everything in the line of rocks except

limestone. This is a condition that in the Antilles usually spells

disappointment and failure to the snail hunter. North of the big bay and

then across several miles of low flat country, just where the foothills

of the sierras begin, lies the city of Guantanamo, interesting to us as

the home of Charles Ramsden, the naturalist. Just north of Guantanamo is

a great rampart of high limestone mountains which beckon most alluringly

to the collector. Sections of this rampart, somewhat arbitrarily marked

off, are the “Monte Verde,” the “Monte Toro” and the “Monte Libano” of

classic fame in Cuban Natural History.

In company with Ramsden we spent a wonderful day on nearby Monte Libano

but a revolution that was then devastating the province and filling the

land with incendiaries and bandits drove us out of this richer field and

obliged us to confine our attentions thereafter to the arid country

lying within the safer limits of the Naval Station,—some fifty square

miles upon which Uncle Sam holds a long lease.

It seems to be a natural law that arid or desert lands support but few

species of snails, but that these few species exist in great numbers and

that they take on a very considerable range of variation. All this is

perfectly true of this region. We were constantly amazed by the great

number of specimens to be found; and each day of exploration in some new

valley or over some range of hills added even greater figures of

abundance to our already astonishing records.

The “prevailing” snail of this region is _Cepolis ovumreguli_ Lea. Its

shell is very suggestive of the true helix of Spain or Algeria of the

_lactea_ group. The variation is exceedingly great in color, size and

shape, and it would make a dozen excellent species if the intermediates

were left out of account. Those living near the coast and among the

cacti of the most arid parts of the district are of whiter and more dull

color, are more banded and show a decided tendency to abnormalities,

especially about the apertures. Specimens from further inland are more

polished and shining, even as though varnished, and are much more given

to a dotted or fly-specked type of ornamentation than to bands. A

fence-post or a dead tree-limb with a hundred specimens closely

assembled in aestivation was no unusual sight. We learned finally to pay

no attention to them. Upon the low bushes in certain localities the

lovely little _Cepolis lucipeta_ Poey cling like berries. These are the

largest and finest of the species I have ever seen. The range of color

variation in this delightful little snail is also very great, but the

colors never blaze out in the vivid flash of the Polymitas. The blues

and purples and chestnut browns are subdued but very rich and splendid.

One very noticeable color form is the subsp. _velasqueziana_ of Poey

where the many broken bands of the type coalesce into two broad

bluish-black zones of solid color.

As nearly all the vegetation of this dry region bears thorns we did not

at first discover that many of these thorns were in reality Macrocerami.

When we did find this out we could see nothing else. Bartsch and I

finally agreed, and shook hands upon it, that we would gather no more of

them, and a stiff penalty was placed upon any violation of the compact.

Two hundred and more from one bush is an earlier record before we really

got started. This is the _Macroceramus festus_ (Gundl.) Pfr., blue and

yellow and buff in color. Another arboreal snail of this section is

_Polymita versicolor_ Born and it is probably very abundant in places

although we never saw more than fifteen or twenty on any one tree. This

is to me the least attractive species of that wonderful genus of richly

painted snails. The brilliant yellow and pink are too primitive and the

two colors do not seem to harmonize very well. It always impresses me as

an experimental species that was laid aside in nature’s laboratory as

not wholly a success.

There were some ground snails too, but to secure living ones required

much grubbing up of tufts of tall grass and shaking out their roots,

like digging up miniature potatoes. These are the _Annularia putris_

(Gundl.) Pfr. and the _Chondropoma marginalbum_ (Gundl.) Pfr., the

latter apparently quite rare. There are no minute things beyond some few

_Thysanophora inaguensis_ Weinland.

Some days we spent gathering marines on the little pebbly beaches hidden

far down under the lofty cliffs that mark this rugged shore line, and we

obtained some unusual species washed up from the exceedingly narrow

island-shelf; blue water is but a few hundred yards out. Among these are

some _Conus cedonulli_ Lam. Beach collecting is, however, an

aggravation; and too much of it becomes a misdemeanor in the collector’s

ethical code, for it obliges an acceptance of something short of the

best.

AMNICOLIDÆ FROM ONEIDA LAKE, N. Y.

BY HENRY A. PILSBRY.

The New York College of Forestry, under the direction of Professor Hugh

P. Baker, is carrying on a biological survey of Oneida Lake and has

issued an interesting bulletin[4] upon the relations of mollusks to

fish, by Frank C. Baker. Some _Amnicolidæ_ obtained during this work,

and subsequent to the preparation of the bulletin were submitted to the

writer. The collection proves to be of considerable interest, including

some species not before noticed.

AMNICOLA BAKERIANA, n. sp.

The shell is umbilicate, turrited-conic, thin, whitish-corneous,

somewhat translucent, with unevenly developed striation, distinct, and

close in places, weaker and sparse elsewhere. The summit is decidedly

obtuse, as in _A. limosa_, the first whorl being nearly planorboid;

subsequent whorls are evenly, strongly convex. The aperture is very

shortly ovate, almost round, its length contained almost 2½ times in

that of the shell. Peristome thin, in contrast with the preceding whorl

for a short distance.

Length 4.3, diam. 2.7 mm.; 5 whorls (type).

Length 3.75, diam. 2.3, length of aperture 1.35 mm.; 4⅔ whorls.

Length 4.1, diam. 2.75, length of aperture 1.65 mm.; 4⅔ whorls.

Oneida Lake; off Short Point in 8½ ft., mud bottom. Lower South Bay, in

18 ft., on mud bottom.

This species resembles _A. limosa_ in the conspicuously obtuse apex, but

differs by the more elevated, turrited spire and the smaller calibre of

the whorls, hence smaller aperture. It is also a weaker shell, with more

whorls in specimens of the same length.

There is also an abundant smaller form, resembling the typical form in

texture, apex and shape of the whorls, varying in form, but relatively

broader than the type. There are some intermediate examples, but as Mr.

Baker considers it desirable to have a designation for this form, it may

be called _A. bakeriana_ form _nimia_. The type measures: length 3,

diam. 2.5, length of aperture 1.4 mm.; 4 whorls.

AMNICOLA CLARKEI, n. sp.

The shell is narrowly umbilicate, conic, a little obtuse at the apex,

corneous, nearly smooth. The whorls are very convex, separated by a deep

suture, the last whorl tubular. The aperture is distinctly oblique,

almost circular, the upper end rounded, but a trifle more narrowly so

than the base. It projects but little beyond the preceding whorl

laterally. The peristome is thin, continuous, scarcely or barely in

contact with the preceding whorl above.

Length 3.1, diam. 1.9, length aperture 1.1 mm.; 5 whorls (type).

Length 2.8, diam. 1.6, length aperture 0.85 mm.

Operculum having the spiral rather large, the nucleus being above the

lower third.

This little species resembles _Lyogyrus_ by its tubular whorls of small

calibre. The whorls are more convex and increase less rapidly than in

_Amnicola walkeriana_, which is also less slender. _A. schrockingeri_

Ffld. has less deeply convex whorls, and the apex is more acute. _A.

bakeriana_ is much larger, with a more obtuse apex.

Found in Short Point Bay, Oneida Lake, near shore, in 3 feet of water,

bottom of sand with algae; also in Lower South Bay, etc. Collected by

Mr. F. C. Baker.

It is named for Dr. John M. Clarke, the distinguished Director of the

Museum of the State of New York.

AMNICOLA ONEIDA, n. sp.

The shell is typically more slender than _A. lustrica_, turrited-conic,

narrowly umbilicate, corneous, minutely striate. The apex is slightly

obtuse, but the first whorl projects visibly, as in _lustrica_, whorls

_very convex_, parted by a _deep suture_. The aperture is ovate, small,

its length contained more than 3 times in that of the shell; upper

extremity narrowly rounded. The peristome is continuous, thin, very

briefly in contact with the preceding whorl above.

Length 4, diam. 2, length of aperture 1.25 mm.; 6 whorls.

Lower South Bay, Oneida Lake, N. Y., collected by F. C. Baker, 1916.

This species is typically narrower than _A. lustrica_ Pils., with a

smaller aperture and shorter whorls; but it is chiefly distinguished by

the more convex whorls (deeper suture), and the rounded instead of

angular posterior end of the aperture. In _Paludestrina nickliniana_ the

last whorl is much longer. Possibly it may be a subspecies of

_lustrica_, yet it has so distinct an appearance that a special name

seems desirable. There are also wider examples, which still differ from

_lustrica_ by the deeper suture and aperture.

NEW GENERA AND SPECIES OF CENTRAL AMERICAN NAIADES.

BY L. S. FRIERSON.

In 1893 Messrs Crosse and Fischer divided the Mexican Naiades into quite

a number of sections, to which they assigned names. Almost

simultaneously (in 1900) von Martens and C. T. Simpson, in treating the

Central American Naiades, accepted some of these sections of Crosse and

Fischer, raising them to generic or subgeneric rank. Because of paucity

of material, considerable diversity of opinion concerning the specific

identity of several species may be noted in the works of these authors.

Furthermore, their work of classification being done independently and

from different points of view, the same species was sometimes placed by

them in different genera.

Thanks to the arduous labors of A. A. Hinkley, who has again and again

enriched our cabinets with material and data from these tropical

countries, we are enabled to offer the following suggestions concerning

some of the genera of these shells, and also the description of an

unpublished species.

NEPHRONAIAS. This genus has for its type the _Unio plicatulus_, Küster,

a species identified by von Martens as belonging to the Lampsiline

shells, as _aztecorum_. Mr. Simpson however believed it to be nearly

allied to the _persulcatus_, a markedly Unioid shell. In this the writer

follows Mr. Simpson.

The genus _Nephronaias_ as constituted by Mr. Simpson embraces two quite

distinct groups, divisible as follows.

_Nephronaias_ (_s. s._) embraces _plicatulus_, _persulcatus_, _melleus_,

_dysoni_, _ortmanni_, _ravistellus_, etc. Ample material of these two

latter species show that they are anatomically very closely allied to

_Elliptio_. There is no sexual difference of shape, and the gill is

gravid in its whole length. _Nephronaias_ differs from _Elliptio_ in its

sulcated disc, in its beak sculpturing, etc.

Included in _Nephronaias_ by Simpson are, however, shells of a totally

different type, such as _medellinus_, _gundlachi_, _sapotalensis_, etc.

These latter are sexually dimorphic, smoother, more generally rayed, and

the gravid uterus is of Lampsiline type.

The position of the dorsal scars within the beak cavities is different,

in the examples of the pseudo _Nephronaias_ seen by the writer.

_Nephronaias_ (_s. s._) possesses an (accessory?) adductor scar attached

to the frontal portion of the cardinal teeth, which is either absent or

obsoletely marked in the second assemblage. For this latter group the

writer, therefore, proposes to use the generic term of _Actinonaias_

Crosse and Fischer, 1893, type _U. sapotalensis_ Lea. The female of this

species has been described by Dr. Ortmann (1912). _Actinonaias_

embraces, besides the type, _medellinus_, _gundlachi_, (accepting

Simpson’s interpretation of this latter species), and others.

PSORONAIAS, Crosse and Fischer (1893). This group of remarkable shells,

embracing _crocodilarum_, _psoricus_, _semigranosus_, etc., was

provisionally treated by Simpson as a group of _Elliptio_, but their

remarkable sculpturing, and the deep beak cavities of some of their

species, led him to observe that it was possible that the group should,

after all, be placed in _Quadrula_.

I follow von Martens, in giving generic rank as above to the group. The

type is _Unio psoricus_. To this genus we are enabled to add a species

hitherto undescribed, under the name of

PSORONAIAS KUXENSIS, n. sp., PI. VII, figs. 1, 2.

Shell small, compressed, rough, brown, biangular. Length 50, height 30,

diam. 17 mm.

Shell hyperbolically rounded before, the extreme frontal point below the

centre. Dorsum slightly arched, descending behind the ligament to the

widely biangular posterior; the upper angle of which is midway the

height, the lower angle very little above the base, which is nearly

straight. The beaks are small, low, acute, approximate; and

_apparently_, concentrically ridged. Epidermis dark brown (olivaceous

and obsoletely rayed in the young), rough, the lines of growth numerous

and well impressed. The discs are covered with fine pustulations, more

pustular in front, biradially linear behind. The post ridge is low, but

distinctly double, making the shell biangulate behind. The teeth are

double in the left valve, single in the right. The cardinals are deeply

sulcate and stout. Laterals slightly curved or nearly straight,

separated by an interdentum. Nacre purple, beak cavities rather deep.

Dorsal scars numerous, extending in a row from above the centre of the

cavity down and forward upon the base of the cardinal teeth. Three well

impressed muscle scars in front, two behind, the latter almost

confluent. Habitat, Kux Creek, Chama, Guatemala. Collected by Mr. A. A.

Hinkley, Feb. 6, 1917. A few dead specimens were obtained on the bank of

the Isaibha River (Chama) of which the Kux Creek is a tributary. Type in

Academy Natural Sciences. Cotypes in collection of A. A. Hinkley, the

author and U. S. N. Museum.

I place this species in _Psoronaias_ Crosse and Fischer, type _U.

psoricus_, because of its evident relationship to _crocodilarum_, and

_distinctus_, differing mainly from the latter in size and degree of

inflation, being much inferior in both respects to _distinctus_.

ON THE RATE OF GROWTH OF POND UNIOS.

BY L. S. FRIERSON.

During the latter part of March 1916, the writer, for the purpose of

constructing a fish pond, excavated a barrow-pit near the bank of a

small creek, about ten feet wide, and at the time nearly dry. The

barrow-pit was perhaps one hundred feet long, fifty feet wide and three

feet deep. Early in April, 1916, the pit became full of water,

overflowing from the adjacent creek, and together with two subsequent

overflows, supplemented with seepage from the newly constructed fish

pond, the pit remained more or less full of water, until May 25, 1917,

when it was drained by a ditch into the nearby creek. From the dried

bottom of this pit some thirty Unios were picked up by the writer. Ten

of these were _Unio tetralasmus_ Say, and the rest were _T. texasensis_

Lea. All the specimens were of remarkably uniform size and appearance.

The _texasensis_ being about one and a half inches, and the

_tetralasmus_ two and a half inches long. Exact dimensions of a

_texasensis_: length 43, height 24, diam. 16 mm.; of _tetralasmus_ 75,

40, and 25 mm.

Both of these species had attained puberty. A female _texasensis_ had

its gills fairly full of young glochidia. A _tetralasmus_ had several

(three or four) ovisacs with a few (remaining) glochidia. In assigning

an age to these shells it is quite sure that the _tetralasmus_

discharges its glochidia in March and early April, so that when picked

up on May 25, these shells were just about fourteen months old, from the

date of discharge from their mother’s gills.

In the case of the _texasensis_ (which spawns somewhat later) it is

possible that these were dropped by fish of which, at least six species

obtained access to the pit on May 7, 1916 (on which date an overflow

occurred), thus making about thirteen months. At any rate the maximum

age of either species is fourteen months from their mother’s ovisacs.

One of the _U. tetralasmus_ is shown of natural size in Pl. VII, fig. 4.

Another observation concerning pond mussels might here prove of

interest. A large pond was cut into two by a railroad embankment, a

culvert preserving the level and providing communication between the

two. In the lower and larger pond a half-bushel of Yonkapin (_Nelumbium

luteum_) seed was sown. It was six years before these seeds germinated.

These plants, during the summer, cover the entire surface of the pond

with their broad peltate leaves. In this pond the writer planted a

colony of a dozen _Anodonta grandis_. Several years after, taking

advantage of extreme low water, the writer made a careful survey of

these twin ponds, with the result that hundreds of Anodons could be

found in the upper pond, but not a single one was found in the lower

pond. Either the shade killed the young shells, or else the

glochidia-laden fish avoided the shade of the lotus plants and

congregated in the upper pond (there are no Nelumbii in the upper pond).

Is not this avoidance of shade a reason for the paucity of unios in the

tropics?

A NEW SOUTH AFRICAN NESOPUPA.

BY H. A. PILSBRY.

NESOPUPA FARQUHARI, n. sp.

Among Pupillidae sent by Mr. J. Farquhar there is a new species from

Grahamstown which may be defined by comparison with _Nesopupa

griqualandica_ (Melv. and Pons.).[5] The new form is ovate, of about the

size of the other species, which it resembles in sculpture and in the

lamellae of the parietal wall and columella. The two palatal plicae are

subequal, the upper emerging to the lip, the lower one also long,

reaching to the inner edge of the peristome. There is a very small

nodule on the base of the columella. In _griqualandica_ the lower

palatal plica is short and very deeply immersed and there is a distinct

though small basal plica within the base, in front of the lower palatal

plica. In _griqualandica_ there is a deep sulcus outside, over the upper

palatal plica, and a flattening or short groove over the lower palatal;

but in _farquhari_ the sulcus is far less impressed except quite close

to the lip. The color is reddish brown. Length 1.65, diam. 0.9 mm.

Mr. Burnup’s figure 9, in Melvill and Ponsonby’s Revision,[6] may

perhaps represent this species, while their description in the same

paper appears to comprise both _griqualandica_ and _farquhari_, though

chiefly relating to the former. Their pl. I, figs. 8 and 10 represent

_griqualandica_. The new form is named in honor of one of the most

successful South-African collectors. It will be figured in the Manual of

Conchology.

A NEW GUNDLACHIA FROM GUATEMALA.

BY BRYANT WALKER.

GUNDLACHIA HINKLEYI, n. sp., Pl. I, figs. 10‒16; Pl. III, fig. 1.

Shell subovate, being much wider posteriorly, the anterior margin rather

shortly rounded, the right margin nearly rectilinear, but somewhat

diverging anteriorly, the left margin obliquely expanded and broadly

rounded, anterior margin wider and much more curved than the posterior;

apex very excentric, depressed and decidedly turned toward the right

side, bluntly rounded, smooth except for a few concentric wrinkles;

color a very pale corneous, nearly pure white; lines of growth rather

strong and irregular; anterior slope with strong radial striæ

originating below the septate growth and extending to the anterior

margin, similar striæ appear on the left lateral slope, but are

scarcely, if at all, visible on the right slope; the septate portion of

the shell is small in comparison with the adult expansion, it is narrow

and the posterior portion covered by the septum is free from and

projects over, but scarcely beyond, the posterior margin of the adult

aperture; the first growth of the shell from the septate form is

continued on the sides in a nearly direct continuation of the lateral

slopes of the septate shell for some little distance, the anterior slope

of this stage is also a continuation of the anterior slope of the

septate stage but owing to the oblique position assumed by the septate

shell is at first somewhat convex, as viewed laterally, later as the

side slopes begin to expand, the anterior slope is continued in a nearly

straight line to the margin; the left lateral slope of the adult shell

below the secondary constriction is concave at first, becoming nearly

straight toward the margin; the right lateral slope is less concave

above and straighter and more oblique than the left; owing to the small

size of the septum and consequent large aperture of the septate shell

and the narrow first growth of the adult shell there is no distinct

aperture to the septate portion visible in the adult shell from below,

the whole interior of the adult shell appears to pass, practically

unconstricted, directly into the septate portion; the posterior margin

of the adult shell narrow and somewhat abruptly expanded and reflected.

Length 5.5; width 3.75; alt. 1.75 mm.

The septate shell is oblong, the sides being nearly parallel, but

slightly expanding anteriorly, the right slightly convex and the left

slightly concave; the posterior margin is regularly rounded; the

anterior more broadly rounded; the apex depressed, bluntly rounded,

excentric, reaching nearly to the right margin, smooth except for slight

concentric wrinkles, lines of growth fine and regular; the anterior

slope is slightly convex; the very short posterior slope below the

projecting apex to the line of the septum is straight and oblique; the

right lateral slope is steep and nearly straight, the left slope very

convex; the septum is very short, being less than half of the length of

the septate shell, convex on its lower surface, the margin is very

short, being less than half of the length of the septate shell, convex

on its lower surface, the margin is very concave and on the right side,

extends further forward than it does on left, there does not seem to be

the distinct thickening of the margin so noticeable in other species;

aperture much larger than in any other species yet described.

Length 2; width 1.5; alt. .75 mm.

Type (43455 Coll. Walker) from the Maya Farm, Quirigua, Guatemala,

collected by A. A. Hinkley. Cotypes in the collection of Mr. Hinkley.

This fine species is the first from either Central or South America, of

which both the septate and adult forms are known.

It differs from all other described species except _crepidulina_ Guppy

in the small size of the septum and the consequent difference in the

position of the aperture of the septate stage in the adult shell. The

septum in the specimen figured appears very like the incomplete septum

in the North American species, but as the three adult specimens before

me are exactly alike in the position of the septate shell, this would

seem to be the normal condition in this species. The specimen figured,

which is 3.25 mm. in length, has apparently slightly passed the septate

stage and begun the growth of the constricted portion of the adult shell

and shows the beginnings of the radial striæ.

With the Gundlachias was associated a species of _Lævapex_, very like

the _excentricus_ Morelet. Whether it has any closer relations with the

_Gundlachia_ remains to be determined as the radula has not yet been

examined. While the general aspect of the two species, if such they be,

is very similar, the _Lævapex_ has a very much more acute apex than the

_Gundlachia_.

As shown by the figure, the radula of this species is quite typical of

the genus.

A LIST OF SHELLS FROM THE EAST COAST OF FLORIDA.

BY BRYANT WALKER.

The late Dr. Charles A. Davis, the well known peat-expert of the U. S.

Bureau of Mines, in addition to his special acquirements in geology and

botany, was a good all-round zoologist and had a lively and unaffected

interest in the work that any of his friends might be carrying on in

that department. It was his kindly habit in his travels about the

country to preserve any specimens that he came across that seemed to him

likely to be of interest to any of his zoological friends. It will be

remembered that the conchologists owe to him the rediscovery of the long

lost _Planorbis multivolvis_ Case, (NAUT., XXI, p. 16), and also the

little _Lymnæa davisi_ Walker, (NAUT. XXII, p. 17), which bears his

name.

In the spring of 1911 Dr. Davis’ professional duties took him to Florida

and while there he collected quite a number of samples of “drift,” which

in due time came into my possession. Several of the localities

represented in the collection, such as Miami and St. Augustine, have

already been reported upon by previous collectors and there seems to be

no occasion to duplicate their work, but quite a number of the places

visited by Dr. Davis have not been covered by any of the previous

collectors in Florida and a record of the species found by him seems

worthy of publication as a contribution to the distribution of the

Mollusca along the east coast of the state.

I am indebted to Dr. George H. Clapp for the identification of the

Gastrocoptas and Vertigos.

The list of localities and species represented in the collection is as

follows:

MARSHES NEAR CHESTER SHOALS.

_Euglandina rosea_ Fér.

_Polygyra cereolus carpenteriana_ Bld.

_Zonitoides minuscula_ (Binn.).

_Zonitoides minuscula alachuana_ (Dall).

_Vitrea dalliana_ (‘Simpson’ Pils.).

_Pupoides modicus_ (Pfr.).

_Gastrocopta rupicola_ (Say).

_Gastrocopta pellucida hordeacella_ (Pils.).

_Gastrocopta tappaniana_ (C. B. Ads.)?

_Gastrocopta pentodon_ (Say).

_Vertigo milium_ (Gld.).

_Melampus coffeus_ (L.).

_Detracia bulloides_ (Mont.).

_Chrondropoma dentatum_ (Say).

_Plecotrema cubense_ (Pfr.).

_Blauneria heteroclita_ (Mont.).

_Microtralia minuscula_ (Dall).

_Truncatella clathrus_ Lowe.

_Truncatella caribæensis pulchella_ Pfr.

_Truncatella bilabiata_ Pfr.

_Littoridina monroensis_ (Ffld.).

_Paludestrina?_ sp.? A single specimen that I can not approximate to any

of the described species.

This is the first record, I believe, for _Plecotrema cubense_ from the

mainland of Florida. Originally described from Cuba, it was listed from

the Bermudas by Dr. Pilsbry in 1900, (Trans. Conn. Acad., X, p. 504, pl.

lxii, fig. 11), and there figured by him for the first time. Both he and

Mr. John B. Henderson inform me that they have collected it on several

of the Keys and I am indebted to both of them for the opportunity of

comparing my specimen with theirs.

CHESTER SHOALS REFUGE STATION.

_Euglandina rosea_ (Fer.).

_Polygyra auriculata_ (Pfr.).

_Polygyra uvulifera_ (Shutt.).

_Polygyra cereolus_ (Mühlf.).

_Polygyra cereolus carpenteriana_ (Bld.).

_Polygyra cereolus septemvolva_ Say.

_Polygyra cereolus volvoxis_ (Pfr.).

_Praticolella jejuna_ (Say.).

_Melampus coffeus_ (L.).

_Detracia bulloides_ (Mont.)

_Lymnaea humilis_ Say.

_Physa cubensis_ Pfr.

_Planorbis tumidus_ Pfr.

_Planorbis alabamensis_ Pils.

_Chrondropoma dentatum_ (Say).

_Truncatella bilabiata_ Pfr.

_Truncatella clathrus_ Lowe.

_Littoridina monroensis_ (Ffld.).

BETWEEN CHESTER SHOALS AND CAPE CANAVERAL.

_Polygyra cereolus_ (Muhlf.).

_Polygyra cereolus carpenteriana_ (Bld.).

_Polygyra cereolus volvoxis_ (Pfr.).

_Polygyra uvulifera_ (Shutt.).

_Zonitoides minuscula_ (Binn.).

_Pupoides modicus_ (Pfr.).

_Gastrocopta pentodon_ (Say).

_Gastrocopta pellucida hordeacella_ (Pils.).

_Gastrocopta rupicola_ (Say).

_Melampus coffeus_ (L.).

_Detracia bulloides_ (Mont.).

_Blauneria heteroclita_ (Mont.).

_Chrondropoma dentatum_ (Say).

_Truncatella bilabiata_ Pfr.

_Truncatella clathrus_ Lowe.

_Truncatella caribæensis pulchella_ Pfr.

_Amnicola._ sp.? A single immature specimen.

CANAVERAL P. O.

_Euglandina rosea_ (Fer.).

_Polygyra cereolus septemvolva_ Say.

_Polygyra cereolus volvoxis_ (Pfr.).

_Polygyra cereolus carpenteriana_ (Bld.).

_Pupoides modicus_ (Pfr.).

_Helicina orbiculata_ Say.

EAU GALLIE.

_Polygyra cereolus septemvolva_ Say.

_Polygyra cereolus volvoxis_ (Pfr.).

_Polygyra uvulifera_ (Shutt.).

_Physa cubensis_ Pfr.

_Helicina orbiculata_ Say var.

ISLAND OF EAU GALLIE.

_Polygyra uvulifera_ (Shutt.).

_Praticolella jejuna_ (Say).

_Lymnaea humilis_ Say.

_Physa cubensis_ Pfr.

PALM BEACH.

_Euglandina rosea_ (Fer.).

_Polygyra auriculata_ Say.

_Polygyra cereolus carpenteriana_ (Bid.).

_Strobilops floridana_ Pils.

_Strobilops hubbardi_ (Brown).

_Pupoides modicus_ (Pfr.).

_Gastrocopta contracta_ (Say).

_Gastrocopta rupicola_ Say.

_Gastrocopta pellucida hordeacella_ (Pils.).

_Gastrocopta pentodon_ (Say).

_Vertigo milium_ (Gld.).

_Vitrea dalliana_ (‘Simp.’ Pils.).

_Vitrea indentata_ (Say).

_Zonitoides arborea_ (Say).

_Zonitoides minuscula_ (Binn.).

_Zonitoides minuscula alachuana_ (Dall).

_Guppya gundlachi_ (Pfr.).

_Thysanophora granum_ (Streb.).

_Physa cubensis_ Pfr.

_Helicina orbiculata_ Say.

LONG KEY.

_Euglandina rosea_ (Fer.).

_Polygyra cereolus_ (Mühlf.).

_Polygyra cereolus carpenteriana_ (Bid.).

_Strophia incanum_ (Binn.).

_Pupoides modicus_ (Pfr.).

_Gastrocopta pentodon_ (Say).

_Gastrocopta rupicola_ (Say)?

_Gastrocopta pellucida hordeacella_ (Pils.).

_Gastrocopta pellucida hordeacella_ (Pils.) var. Small form.

_Thysanophora incrustata_ (Gld.).

_Thysanophora granum_ (Streb.).

_Thysanophora dioscoricola_ (Guppy).

_Guppya gundlachi_ (Pfr.).

_Varicella gracillima floridana_ Pils.

_Succinea campestris_ Say?

_Melampus coffeus_ (L.).

_Detracia bulloides_ (Mont.).

_Microtralia minuscula_ (Ball).

_Lymnæa columella_ Say.

_Physa cubensis_ Pfr.

_Helicina tantilla_ Pils.

_Chrondropoma dentatum_ (Say).

_Truncatella caribæensis_ Sby.; Rve.

_Truncatella caribæensis pulchella_ Pfr.

_Truncatella clathrus_ Lowe.

_Truncatella bilabiata_ Pfr.

_Littoridina monroensis_ (Ffld.).

_Amnicola. sp?_ A single specimen of a very small, globose form that

may be an n. sp. Alt. 1 mm.

COLLECTING IN DIGBY, NOVA SCOTIA.

BY LILLIAN DYER THOMPSON.

While traveling through Nova Scotia and New Brunswick last summer, we

stayed for about six weeks at Digby, N. S. Digby is about 200 miles

northeast of Boston, and is situated near the Bay of Fundy, opposite St.

John, N. B. The town is located on the southeast shore of the Annapolis

Basin,—a sheet of water about twenty miles long and ten miles wide. This

basin is connected with the Bay of Fundy by a channel about

three-fourths of a mile wide at its greatest width. This channel, known

as Digby Gap, is noted for its rapid tides,—the rate of flow through the

Gap being about eight miles an hour. The tide fall at Digby is thirty

feet. The shores of the Basin are sandy, with the exception of the two

rocky promontories on each side of the Gap; the one which is nearest to

Digby being Point Prim. The town is on a small peninsula on either side

of which are two inlets of the Annapolis Basin, known as the Racquet, on

the west, and the Jacquet, on the east of Digby proper. On the ebb tide

these are almost dry, exposing long mud flats.

There is one island in the Basin, about opposite the Gap and at the

mouth of Bear River, called Bear Island. From this a long bar extends,

called Bear Island Bar, which is covered to a depth of about six feet at

low water, and is covered with eelgrass.

Near the Yacht Club pier were found many _Polinices heros_, and their

red-brown “sand-collars.” In the Jacquet were many _Litorina littorea_

and _Litorina rudis_. On the exposed beach, nearer the town, we found

_Mytilus edulis_. On the rocks, in the Racquet, we found _Thais

lapillus_ and a host of _Acmaea testudinalis_ ranging in size from

one-eighth of an inch to about an inch in diameter. In the mud, at the

base of the rocks, were a multitude of _Buccinum undatum_, _Neptunea

decemcostata_, ranging in size from one-eighth of an inch to about an

inch in diameter. In the mud, at the base of the rocks, were a multitude

of _Buccinum undatum_, _Neptunea decemcostata_, and _Colus stimpsoni_,

all alive and half-buried. Some dead specimens of _Aporrhais

occidentalis_ were also found, five of them being full-grown.

On the suggestion of Capt. Danforth, we constructed a dredge, and

endeavored to dredge Bear Island Bar from his motor-boat. Here we found

quantities of _Lacuna vincta_, _Alectrion obsoleta_, _Cylichna alba_,

and two _Polinices triseriata_.

There were some soldiers encamped at Digby, and they used to gather

_Litorina littorea_ and steam and eat them, without any flavoring. They

sometimes ate _Thais lapillus_ also. One day, after a rain, we found two

_Helix hortensis_ crawling along the road.

A NEW TYPE OF THE NAYAD-GENUS FUSCONAIA. GROUP OF F. BARNESIANA LEA.

BY A. E. ORTMANN.

During the study of the nayad-fauna of the upper Tennessee, the present

writer found that there exists, in this region, a peculiar type of

shells, belonging to the genus _Fusconaia_, the various forms of which

have been described previously under a great number of specific names,

which, however, seem to belong all to one species. In addition, among

material received from L. S. Frierson from the Ozark Mountains, a form

was discovered which presented the same structure.

The oldest name for the upper Tennessee form is _Unio barnesianus_ Lea.

A more detailed account of its various phases is to be given elsewhere,

and it suffices here to mention only those forms which belong here.

According to obesity, I distinguish three local, or ecological races:

1. FUSCONAIA BARNESIANA (Lea) 1838.

_U. barnesianus_ Lea, ’38. _U. meredithi_ Lea, ’58. _U. pudicus_ Lea,

’60. _U. Lyoni_ Lea, ’65. _U. tellicoensis_ Lea, ’72. _U. lenticularis_

Lea, ’72.

As the normal (most abundant) forms we may regard _U. meredithi_,

_pudicus_ and _lenticularis_, which differ from each other only in the

development of the rays (topotypes examined). _U. barnesianus_ is a

slightly more elongated individual, with poorly developed rays. _U.

tellicoensis_ (topotypes examined) is a _lenticularis_ slightly more

swollen; and _U. Lyoni_ forms the transition toward var. _tumescens_,

having a little more elevated beaks, greater obesity, and rather

distinct rays.

The Nautilus. Vol. XXXI, No. 2, October 1917 A Quarterly Journal Devoted to the Interests of Conchologists · 第 1 / 3 段