801 UC-NRLF C 5 ^75 bS3 >*>* u DESCRIPTION or SOUK NEW FOSSIL SHELLS, FROM THE TERTIARY OF PETERSBURG, VA. Read before the American Philosophical Society, May 29, 1813, !*, .' ' BY HENRY C. LEA. PHILADELPHIA: PRINTED FOR THE AUTHOR. MATTHEW UMAftY . *.. ' ' . * * % ARTICLE IX. Description of some new Fossil Shells, from the Tertiary of Petersburg, Virginia. By Henry C. Lea, Philadelphia. Read May 29, 1843. IN the United States, the various Supercretaceous, or Tertiary, formations, are widely extended and beautifully developed. They have been traced from the St. Lawrence to the Gulf of Mexico, and from the Atlantic far into the western territory. For the sake of convenience, geologists have divided them into two groups, according to their geogra- phical position, namely, the Atlantic and the Western Tertiary. Of the latter it is not, at present, my intention to speak, but little, comparatively, is known of it, and it presents a rich field to any enterprising geologist who may undertake its investigation. The northern extremity of the Atlantic Tertiary, as far as it has been discovered, is on the St. Lawrence and around Lake Champlain. From thence to Maryland, its course may be traced by a few small patches in New Jersey, and, from Maryland to the Gulf of Mexico, it exists in a broad sheet. It is to be expected that, extending as it does over so wide a space, it should present very different characters in different localities. Accordingly, we find that much confu- sion has existed in its classification. Mr. McClure, the first who attempted to syste- matize American geology, considered it all as alluvial, but subsequent geologists soon corrected this error. Mr. Conrad, in the first number of his " Fossil Shells of the Tertiary of North America," divided it into the Upper Marine, Middle Tertiary, and Lower Tertiary. In this arrangement, the Upper Marine corresponds very nearly with Mr. Lyell's Pliocene, the Middle Tertiary comprises the Miocene and Eocene of the same author, and the Lower Tertiary consists of sand and gravel containing Lignite and a few shells. Mr. Conrad has, more recently, adopted the classification of Lyell, which is perhaps best, as the beds comprising his Lower Tertiary are hardly of sufficient importance to constitute a separate formation. The latest, and probably, most correct views upon this subject are, however, those which Mr. Conrad advances in the second number of the Bulletin of the National Institution. He there supposes that we possess the Eocene, Miocene, and Post-Plio- cene, as nearly as the parallel can be drawn between our strata and those of Europe. Several links of the chain, however, appear to be wanting, as but one or two species are common to the Eocene and Miocene, and only recent shells have been found exist- ing in both the Miocene and Post-Pliocene. The Eocene does not possess a single NEW FOSSIL SHELLS species at present existing; in the Miocene the proportion is small; \vhile, in the Post- Pliocene all are recent. According to Mr. Conrad, the per centage of still existing shells in the Miocene is about seventeen, but I am inclined to think that it will prove, on further in vestigajioji, to: be smaller. It, however, cannot be relied on as a certain criterion, bemg exttiefeiefy-variable in different localities. Petersburg, Virginia, may be taken a,ai an.-dflStjaiJCfejofciie extreme: the following is a list of the fossils which have been fou'nd'tMreJ 'exclusive of those herein described. Dentaliuin thallus, . . " atlenuatura, . Serpula granifera, Balanus sp. ? Pholas ovalis, Panopaea reflexa, . , Mactra congesta, . , Crassatella undulata, " melina, . , Corbula cuneata, . . " inaequalis, . , Tcllina aequistriata, . . Lucina speciosa, . . " contracta, . , " edentula, " divaricata, . , Astarte undulata, " arata, . . " concentrica, Clathrodon Grayi, . , Cytherea reposta, . " convexa, . Artemis acetabulum, Con. Con. Say. " dillbrmis, Say. " Cardium sub-lineatum, . . Con. " laqueatura, Say. Cardita granulata, . . . Say. M Cypricardia arata, . . . M Con. Area centenaria,. U Say. Con. " incile, Say. Pectunculus subovatus, . . H 4( " quinquerugatus, Con. H " pulvinatus,* . Lamk. H Nucula la?vis Say. " obliqua, .... " Lamk. Chama congregata, . . . Con. Say. " corticosa, . . . u, Con. Pecten eboreus " " Madisonius, . . Say. 14 Plicatula marginata, u ,1 H Say. Ostrea Virginiana? var. . Gmel. Con. Capulus lugubris, Con. Fissurella redimicula, . Say. Crepidula fornicata, . . " " costata, . . Morton. Dispotpca ramosa, . . Con. Natica dnplieata, . . Say. " heros? ... " Acteon Wetherilli, . . Lea. Rotella nana, ... " Trochus philanthropus, Con. Turritella variabilis, . " " indenta, . . " " plebeia, . . Say. Pleurotoma pyrenoides, Con. Fasciolaria mutabilis, . " Pyrula cariCa, . . . Say. " canaliculata, . " Fusus cinereus, ... " " exilis, .... Con. Murex quadricoetatus, . Say. Buccinum laqueatura, . Con. " porcinum, . " Marginella perpusilla, . " " limatula, . " We have here sixty-eight species, in addition to one hundred and five which I shall describe in this paper, and which I consider as hitherto unknown, or in all, one hundred and seventy-three. Now, of these, but nine can be identified with existing shells, namely,. Lucina divaricata, Artemis acetabulum, Ostrea Virginiana? Crepidula fornicata, Natica heros? " duplicata, Pyrula carica, " canaliculata, Fusus cinereus. and of these, two appear to me doubtful, namely, Natica heros, and Ostrea Virginiana. Considering them, however, as the recent species, this gives us about five per cent, of still existing shells. It appears almost absurd to compare this with the Miocene of Dax, the best characterized in Europe, which, by the tables of Dr. Grateloup, con- * In the first number of the "Fossil Shells of the Tertiary of North America," Mr. Conrad has described and figured a shell as the Feet, pulvinatus, Lam. But, after comparing it with a number of specimens of that species, and with Deshayes' figures, I am forced to consider it as specifically distinct. I, therefore, propose to name it P. ELEPHANTOPUS. FROM THE TERTIARY OF VIRGINIA. 5 tains between thirty and forty per cent, of recent shells. Yet the Miocene of Peters- burg has not a single species which can be identified with any of the Claiborne Eocene fossils, while it abounds in shells which are found, at other localities, in company with more than twenty per cent, of recent species. These few facts will sufficiently exem- plify the fallacy of attempting to classify our Tertiary by the rules which regulate that of Europe. It may, perhaps, be deemed not irrelevant to this subject, to introduce here the fol- lowing table of the number of the species in each genus, hitherto described from the Tertiary of the United States. Unfortunately great confusion exists in their synonymy, and he who would review the descriptions of them, with an impartial and unsparing hand, would confer a great benefit on all interested in American geology. To this part of the subject, I have not pretended to pay any attention, and therefore the number of species is, in reality, smaller than that given here, many of them being repeated under the same or different genera. I, however, have not felt inclined, at present, to undertake the Augean task of clearing away the synonymes, but I hope that, as far as I pretend to go, I shall be found correct; that is, as far as the mere numbers are concerned.* List of the Fossil Shells found in the Tertiary Seels of the United States. Genera. Acteon, . Aligena, Amphidesma, Anatina, Ancillaria, Anolax, Anomia, . Area, . Artemis, . Astarte, Avicula, . Balanus, Bissomya, Bonellia, Buccinum, Bulla, . Bullina, . Calyptrea, . Cancellaria, Capulus, Cardita, . Cardium, . Cassis, . No. of species. Genera. . 23 Cemoria, . . 2 Cerithium, . 12 Chama, . . . 3 Chiton, . 7 Conus, . . . 2 Corbis, 1 Corbula, . . . 14 Crassatella, . . 2 Crepidula, . . 20 Cryptostoma, . 4 Cucullaea, Cypraea, . . 4 Cumingia, 1 Cypricardia, . . 2 Cyrena, . . 20 Cytherea, . . . 5 . 1 Delphinula, Dentalium, . . . 4 Diplodonta, . 17 Dispotsea, . . . 1 Donax, . 6 . . 7 Egeria, . 1 Emarginula, No. of species. Genera. 1 Erycina, . . 10 . 3 Fasciolaria, . . 1 Fissurella, . . 5 Fistulana, . . 3 Fulgur, . 11 Fusus, . . . 8 Gastrochama, . 12 Gnathodon, . . 1 Grateloupia, 4 . . 1 Gryphsa, . 1 Hiatella, . . . 1 Hippagus, . 1 Hipponix, . . . 26 Infundibulum, . 12 Isocardia, . . . 5 Lepton ? . 1 Lima, . . . 6 Littorina, . 1 Lucina, Lutraria, . . . 10 1 Mactra, No. of species. . . 2 5 . . 7 1 . . 7 . 51 . . 1 . 3 . . 1 . 1 . . 1 . 1 6 2 1 2 1 27 2 18 * I regret that I have not been able to obtain the names of the species figured by M. Lesueur from the Eocene of Walnut Hill, Mississippi. I have seen the plates, but I do not know whether the descriptions were ever pub- lished. It may be seen that I have included in this catalogue the species described in the following pages. NEW FOSSIL SHELLS Genera. No. of species. Genera. No. of species. Genera. No. of species. Marginella, . . 16 Patella, . 1 Serpula, . . 5 Melongena, . 3 Pecten, . . . . 22 Sigaretus, . . . 5 Mitra, . . 13 Pectunculus, . . . 22 Siliquaria, . 2 Modiola, . 2 Perna, . . 2 Solarium, . . . 18 Monodonta, . . 1 Petaloconchus, . . 1 Solen, . 2 Monoceros, . 5 Petricola, . . . 3 Solecurtis, . . . 2 Monoptygma, Murex, . . . 2 . 6 Pholadomya, . Pholas, . 2 . . 5 Spirorbis, . Stalagmium, . 1 . . 1 Mya, . . . 3 Placuna, . . . . 1 Strigilla, . . 1 Myoparo, Mysia, Mytilus, . . 1 . . 2 . 2 Plagiostoma, Planaria, Pleurotoma, . . 1 . 1 . . 32 Tellina, Terebra, Tprprln . . 9 . 8 Nassa, . . . 5 Plicatula, Proto, . . 4 . . 1 A t i ' t < i ' j Thracia, . . 1 Natica, . . 23 Psammobia, . . 2 Triton, . . 1 Nautilus, . . . 1 Psammocola, . . 2 Trochus, . . 16 Nucula, . . Nummulites, . 31 . . 1 Pyramidella, . . Pyrula, . 3 .' . 7 Tuba, . Turbinella, Turritella, . . . 3 . 5 . . 20 Oliva, '. . 16 Typhis, . . 2 Orbicula, . . . 1 Ranella, . 1 Orbis, . . 1 Rostellaria, . . . 4 Venericardia, . . 7 Ostrea, . . 18 Kotella, . . 5 Venerupis, . 1 Venus, . . 11 Pandora," . 2 Saxicava, . . . 2 Vermetus, . 1 Panopxa, . . . 4 Sanguinolaria, . 2 Voluta, . . 12 Pasithea, . 21 Scalaria, . . 16 Volvaria, . . 1 It is to the kindness of Mr. Tuomey, of Petersburg, that I owe the following shells, as well as those in the list a few pages back. Most of the smaller species herein described, I met with by carefully examining the sand scraped from the cavities of larger shells, as well as a small portion of the marl of the vicinity, with which Mr. Tuomey was kind enough to favor me. I mention this merely to show the importance of thoroughly searching the strata of the various localities before we conclude that we have all the species existing there. Attracted by the beauty of the larger shells, conchologists have very much neglected the more minute ones, which require a closer examination, and thus our knowledge of our fossil conchology is still limited. I may as well observe here, that I found the species met with in the sand from the cavities of the larger shells, in general, different from those in the loose marl. It is difficult to give a reason for this, unless there were species which usually inhabited the interior of dead shells, like the recent Valvata tricarinata, Say. In looking over these shells, I have been struck with the general resemblance which obtains between them and those of a corresponding age from Dax. This is peculiarly observable in the genera Acteon, Pasithea, &c. which are very numerous in both localities. Their connexion is so close that in some cases they are scarce specifically distinct. FROM THE TERTIARY OF VIRGINIA. FAMILY SERPULID^E. GENUS SERPULA. S. CONVOLUTA, PL. 34. FIG. 1. S. testa in spiram discoiddem contortd, tenni, plerumque cancellatd, apud apicem rcgulariter valuta; apertura rotunda. Shell twisted into a discoidal spire, thin, usually cancellate, regularly whorled near the apex; mouth round. Diam. .10 of an inch. Remarks. This shell is generally twisted into a regular disc. The sculpture is very variable, sometimes seeming like longitudinal moniliferous costee, and, at others, regu- larly cancellate. The apex is singularly formed, being smooth and perfectly voluted, like a young Turbo. This is, I suppose, the form it has when excluded from the egg. S. ANGUINA, PL. 34. FIG. 2. 5, testa minima, irrcgulariter contortd, striatd, crassd; striis irregularibus transversis; apertura rotunda. Shell very small, irregularly twisted, striate, thick; striae irregular, transverse; mouth round. Diam. .04 of an inch. Remarks. This is a very minute species, and is, I believe, the only one of our fossil Serpulse that has no longitudinal lines on the surface. This character will readily dis- tinguish it from others. The apex has the same voluted character as the last, although not as well developed. GENUS PETALOCONCHUS,* (Nosis.) Testa tubularis, solida, irrcgulariter contorta, laminis longitudinalibus duabus internis. Shell tubular, solid, irregularly twisted, with two internal longitudinal plates. Remarks. -The singular shell, on which I propose to found the above genus, differs from all the known tubular shells that I have met with, in the two internal longitudinal plates. It may possibly belong to the family Scalaridse, and, if so, presents a link be- tween them and the Plicacidse. P. SCULPTURATUS, PL. 34. FIG. 3. P. testa vel contorta vel turritd, crassd, costulis longitudinalibus noduliferis; laminis internis politis, Icevibus, ad aper- turam obsoletis; apertura rotundd. Shell sometimes twisted, sometimes turrited, thick, with small longitudinal noduliferous ribs; internal laminiE smooth, polished, obsolete at the mouth; mouth round. Diam. .20 of an inch. Remarks. The longitudinal costa? are generally nodulous, but they occasionally seem rather to be cancellated by transverse sulci, which, in other specimens, appear to usurp their place. The two internal lamina? are placed at about one-sixth of the circumference apart. They are generally directed towards the centre, and sometimes nearly meet. In some specimens they are much smaller than in others. They rarely or never seem to be continued to the aperture. This is a very variable shell, both as to the sculpture and internal plates. I at first * A tt'fttojw, lamina, et vyxs> concha. 8 NEW FOSSIL SHELLS thought that there were two or three distinct species, but the varieties glide impercepti- bly into each other. It appears to be by no means an uncommon shell at Petersburg. The form figured is a very usual one. I have but few specimens which do not exhibit a decided tendency to form regular revolutions, and in some, the axis is so straight that a pin may be thrust through the umbilicus from the apex to the base. The second figure is a specimen fractured to exhibit the appearance of the laminae. V. ^ FAMILY TUBICOLID.E. GENUS TEREDO. T. CALAMUS, PL. 34. FIG. 4. T. testa incognita; tubo parvo, rotunda, tenui, rugoso, striis irregularibus trantversis. Shell unknown; tube small, round, thin, rugose, with irregular transverse strise- Diam. .08 of an inch. Remarks. I found several specimens of this little species of Teredo, on breaking open a mass of Madrepore which they had pierced. It differs from the following shell, prin- cipally, in being much smaller, thinner, and more rugose. T. FISTULA, PL. 34. FIG. 5. T. testa incognita; tubo rotunda, tereti, crassissimo, turn recto turn curvato; striis irregularibus transversis raris. Shell unknown; tube round, terete, very thick, sometimes straight and sometimes curved; with a few irregular transverse strise. Diam. .50 of an inch. Remarks. The transverse lines of growth vary exceedingly both in size and direction. The substance of the shell is very thick, the outer diameter being frequently .50, while that of the aperture is about .28 of an inch. I have them, however, even thicker. GENUS GASTROCH.ENA. G. LIGULA, PL. 34. FlG. 6. G. Uibo incognito; testa transversd, oblanceolatd, valde inaquilatcraii, posiice' rotundatd, antice actiminatd, inflatd, con- cenlrice striatd; striis parvis, irregularibus; antice hiatu maxima, valde obliquo; margine basali tortuoso; margine dorsali recto; margine antico brevissimo; natibus sub-prominulis, Tube unknown; shell transverse, oblanceolate, very inequilateral, rounded posteriorly, acuminate anteriorly, in- flated, concentrically striate; strise small, irregular; anteriorly gaping widely and very obliquely; basal margin tor- tuose; dorsal margin straight; anterior margin very short; beaks somewhat prominent. Diam. .15 of an inch. Length .28. Breadth .12. Remarks. The opening at the anterior extremity commences near the dorsal margin, and extends to about the middle of the base. The beaks are placed very near the ante- rior end of the shell. As in most Gastroch?ena3, there is a small interior cuneiform pro- cess immediately under them. In procuring several specimens of this shell from a piece of madrepore which they had pierced, I unfortunately broke the tubes, and am therefore unable to describe them. This species is not unlike the G. truncata, Sowerby, a recent shell from Panama, but may be distinguished by its smaller size, rounded extremity, and longer opening. It is, FROM THE TERTIARY OF VIRGINIA. * I believe, the first species of the genus as yet discovered in a fossil state in this country. Mr. Conrad mentions having found the Fistulana elongata, Lam. at Claiborne, but, upon comparison with M. Deshayes' figure of that shell, I do not think that it can be identical with the present species. It is larger, more twisted, and has a different sculpture on the anterior part. The genus Gastrochaana, as formed by Lamarck, was placed among the Pholadidae, and considered to have no tube. M. Deshayes, however, includes it in the genus Fis- tulana, as it inhabits a tube and has no teeth. Mr. Sowerby, again, considers as Gas- trochasnse those species which have a bent tube and an oval shell. According to this arrangement, the present species would, most probably, come under this genus, and as such I have placed it. There are two Gastrocheense among the fossils of Great Britain, one from the Oolite, the other from the London Clay. Deshayes describes five from the Paris Basin. FAMILY PHOLADID.E. GENUS PHOLAS. P. RHOMBOIDEA, PL. 34. FlG. 7. P. testa transverse!, oblique rhomboidea. valdl incequilatcrali, postice rotundato-angulatti, antice rostratd, injlatii, tenui, media divisd lined impressdj area posticri striis lavibus conccntricis; area anticd striis acutis flcxuosis concentricis; margine basali curto; margine dorsali recto, volde rcflexo; palmuld parvu, reeurva, tenui: lineis internis duabus clevatis loneitudi- nalibus. iSholl transverse, obliquely rhomboidal, very inequilateral, rounded-angular posteriorly, rostrate anteriorly, inflated, thin, divided in the middle by an impressed line; posterior area with smooth concentric striae; anterior area with acute, flexuose, concentric striae; basal margin short; dorsal margin straight, very much reflected; palmule small, recurved, thin; two longitudinal internal, elevated lines. Diam. .20 of an inch. Length .28. Breadth .18. Remarks. The stria? on the anterior part of the shell are sometimes wrinkled so regularly that they give it the appearance of being cancellate, although there are no radiating lines. The posterior part of the shell is nearly smooth, from the dividing line to the umbonial slope, where there are numerous regular lines of growth. There is a kind of second dentiform process, immediately below the beaks, formed by the recurving of the upper termination of the posterior margin. The two internal stria? extend from the beaks to the base. The posterior one is situated immediately under the umbonial slope. The anterior one is caused by the impressed dividing line. It extends, in a point, a little beyond the basal margin. This shell is very similar to a specimen of the P. ovalis, Say, without the tube, and with the thin anterior basal portion removed, but I believe it to be a perfect shell, as I obtained it myself from the hole which it had formed, and in which it appeared to have remained undisturbed. It was surrounded by a little indurated mud which preserved it entire. It seemed to be entirely destitute of a tube, which character separates it from the P. ovalis. It also differs in the shape and size of the palmule, and in the two in- ternal lines. 10 NEW FOSSIL SHELLS FAMILY SOLENID.E. GENUS SOLEN. S. MAGNODENTATDS, PL. 34. FlG. 8. S. testa antict truncatd, et valde hiante, Itevi, politd, crassd; natibiis compressis; dente laterali uno; dcnte cardinali uno, longo, acuto. Shell truncate, and gaping very much anteriorly, smooth, polished, thick ; beaks compressed ; with one lateral, ami one long, acute, cardinal tooth. Diam. . Length . Breadth Remarks. Although I possess but a small fragment of this shell, yet it differs so essentially in the teeth from all of our Solenes, that I have no hesitation in pronouncing it distinct. I believe that it is the only extinct fossil species as yet found in our Tertiary. GENUS PANOP^EA. P. DUBIA, PL. 34. FIG. 9. P. testa quadrato-ellipticd, transversd, iruequilaterali, posticS truncatd, anticl rotundatd, sub-infatd, crassiusculii, strintii; ttriis cancentricis, regularibus ; margine basali recto; margine dorsali recto ; nymphis magnis, exsertis, longissimis; cardine cochlea parvd. Shell quadrately elliptical, transverse, inequilateral, posteriorly truncate, anteriorly rounded, somewhat inflated, ra- ther thick, striate; striae concentric, regular; basal margin straight; dorsal margin straight; beaks prominent; nymph large, exserted, very long; hinge with a small fosset. Diam. .10 of an inch. Length .08. Breadth Remarks. The nymphae are unusually large, much exserted, and very long, extending the whole length of the dorsal margin. Near the beak, they are suddenly depressed and twisted round, and terminate in a small, shallow, internal fosset, or spoon-shaped tooth. It is not without some hesitation that I have placed this shell among the Panopffice, as it has a spoon-shaped tooth in place of an erect, pointed one, but there is no genus to which it can be said positively to belong, and I do not consider its peculiar characters sufficient to authorize the erection of a new one for its reception. It seems to connect the Glycymeris with the Anatina, having the nymphae of the one, and the spoon-shaped tooth of the other. FAMILY MYID.E. GENUS MY A. M. REFLEXA, PL. 34. FIG. 10. M. testa quadrilaterali, sub-inaquilaterali, postice rotundatd, antice truncatd et valdl apertd, inflatd, striatd; striis conccn- tricis, irregularibus; clivo umboniali elevato, rotundato; margine basali curvato; margine dorsali arcualo; natibus prominen- tibus, incurvis. Shell quadrilateral, somewhat inequilateral, rounded posteriorly, truncate and very open anteriorly, inflated, striate; stria; concentric, irregular; umbonial slope elevated, rounded; basal margin curved; dorsal margin arcuate; beaks prominent, incurved. Diam. .18 of an inch. Length .22. Breadth .29. Remarks. The opening at the anterior portion of the shell is remarkably large, and the margin there appears to be somewhat reflected. The stria3 are more numerous and better characterized at the extremities, than in the central portion of the shell. FROM THE TERTIARY OF VIRGINIA. 11 As but one valve of this shell, and that the left one, is -before me, I cannot determine the shape of the tooth. The pit to receive it is small and almost horizontal. This is, I believe, the only extinct species of Mya as yet found in our Tertiary. GENUS THRACIA, (LEACH.) T. TRANSVERSA, PL. 34. FIG. 11. T. testa sub-ellipticii, valde inaequilaterali, postice acuminato-rotundatd, antice truncatd, sub-compressd, tenui, media Icevi, postice el antice concentricc striatii; clivo umboniali rotundato; margins basali curvato; margins dorsali media angulato, postice convexo, antice concavo; natibus sub-aculis; callo nymphali parvo, obliquo. Shell sub-elliptical, very inequilateral, acuminately rounded posteriorly, truncate anteriorly, sub-compressed, thin, smooth centrally, striate posteriorly and anteriorly; umbonial slope rounded; basal margin curved; dorsal margin angular in the middle, posteriorly convex, anteriorly concave; beaks somewhat acute; nymphal callosity small, oblique. Diam. .10. Length .18. Breadth .28 of an inch. Remarks. From the shape of the anterior margin, I conclude that the shell must have gaped considerably there, but as I have no pair of valves, I cannot be certain. The sinus of the palleal impression is deep, and near the anterior cicatrix. In this character, it differs from the rest of the genus. This is, I believe, the first Thracia found in our Tertiary deposites. Deshayes, in his tables, gives four as the number of European Tertiary species. The present one is the smallest of the genus. GENUS ANATINA. A. TELLINOIDES, PL. 34. FIG. 12. A. testa ovato-triangulari, transversd, postice angulatd, antice rolundatd, compressd, postice undulatd, tenui, con- centrice striatd; striis crebris minutis; margins basali sub-Jlexuoso; natibus compressis, prominentibus ; dentibus lateralibus magnis; cockled obliqud, ovato-acuminatd, minime profundd; cicatricibus magnis. Shell ovate-triangular, transverse, angular posteriorly, rounded anteriorly, compressed, posteriorly undulate, thin, concentrically striate; stria? numerous, minute; basal margin slightly flexuose; beaks compressed, prominent; lateral teeth large; fosset oblique, ovate-acuminate, shallow; cicatrices large. Diam. .25. Length .45. Breadth of an inch. Remarks. Of the lateral teeth, the posterior one is much the longer. The fosset is small, quite oblique, acute above and rounded below. The broad undulation on the pos- terior part of the shell gives it very much the appearance of a Tellina, when viewed externally. The lines of growth are small, very numerous and irregular. This species is quite thin and fragile. Out of some half a dozen specimens, I have but one perfect valve, and that is a very young one. I am therefore unable to give all the dimensions. Judging from description, this shell is not unlike the A. antiqua, Conrad, but the dif- ference in size and sculpture, and the posterior undulation distinguish them at once. 12 NEW FOSSIL SHELLS FAMILY MACTRID.E. GENUS ALIGENA, (Noais.) Testa aquivdvisf subaquilateralis, posticS et antice clausa; cardo dente cardinali uno, sulco sub natibus longo, minime profundo. Shell equivalve? sub-equilateral, closed posteriorly and anteriorly; hinge with one cardinal tooth, and a long shal- low sulcation under the beaks. Remarks. The cardinal tooth is, in general, rather small. The sulcus appears to have received the ligament. It commences at the beak, and runs obliquely past the dorsal margin into the cavity under the beak. As I possess only odd valves of both the following species, I am unable to determine whether the shell is equivalve or not. I have in vain endeavoured to find some genus, already described, which might receive these little shells, but their peculiar characters in having one cardinal tooth, and a liga- mentiferous sulcation, descending into the shell, distinguish them from other genera. Their place in the systems is, most probably, in the family Mactrida?, between Erycina and Ungulina. I have called the genus, Aligena, one of the surnames of Venus, from its resemblance to Erycina, also an appellation of that goddess. A. STRIATA, PL. 34. FIG. 13. A. testa transversd, sub-cllipticd, postice et antice rotundatd, inflatd, tcnui, striatd; striis concentricis, propc marginem basakm maximis; clivo umboniali elevato, sub-angulato; margine basali curvato; margint dorsali media angulato, postice et antice curvato; natibus promijientibus, incurvis, sub-lavibus; dente cardinali minima; sulco longo. pene transverse: margine interno integro. Shell transverse, sub-elliptical, rounded anteriorly and posteriorly, inflated, thin, striate; stria; concentric, very large near the basal margin; umbonial slope elevated, somewhat angulate; basal margin curved; dorsal margin angu- lar in the middle, curved posteriorly and anteriorly; beaks prominent, incurved, nearly smooth; cardinal tooth very small; sulcation long, nearly transverse; margin entire within. Diam. .10. Length .19. Breadth .21 of an inch. Remarks. The concentric striaa are irregular in size and number, but there is a general increase from the beaks to the base. Those near the base, indeed, almost merit the name of costee. The cardinal tooth is extremely small. A. L.EVIS, PL. 34. FIG. 14. A. testa transversd, sul-quadrilaterali, postice rotundatd, antice subtruncatd, convexd, inflatd, leevi; margine basali recto; margine dorsali media angulato, postice et antice curvato; natibus sub-prominulis, incurvis; dente cardinali longo; sulco lato, curto, penu transverso; margine interno integro. Shell transverse, sub-quadrilateral, posteriorly rounded, anteriorly sub-truncate, convex, inflated, smooth; basal margin straight, dorsal margin angular in the middle, curved anteriorly and posteriorly; beaks somewhat prominent, incurved; cardinal tooth long; sulcation wide, short, nearly transvefse; margin entire within. Diam. .14. Length .18. Breadth .22 of an inch. Remarks. There are a few, almost imperceptible lines of growth over the surface of the shell, which, under a powerful microscope, give it a somewhat roughened appearance. The cardinal tooth is very long, and the sulcus is shallow, so that the hinge, at first glance, is not unlike that of the genus Thracia. FROM THE TERTIARY OF VIRGINIA. 13 This shell is closely allied to the preceding, but the differences in outline, hinge and sculpture separate them. FAMILY LITHOPHAGDXE. GENUS PETRICOLA. P. COMPRESSA, PL. 34. FIG. 15. P. testa valdc transversd, valdc in&quilaterali, sub-ellipticd, compressd, postice sub-truncatd. antice rotundatd, tenui, striatd postice et antice; striis minimis, concentricis; margins basalt recto; margine dorsali recto; natibus sub-acutis, prominenlibus; dentibus duobus, parvis, divergentibus. Shell very transverse, very inequilateral, sub-elliptical, compressed, posteriorly sub-truncate, anteriorly rounded, thin, striate posteriorly and anteriorly; stria; very small, concentric; basal margin straight; dorsal margin straight; beaks somewhat acute, prominent; teeth two, small, divergent. Diam. .10. Length .12. Breadth .25 of an inch. Remarks. The concentric lines of growth are very small. They are visible on the anterior and posterior portions of the shell. On the central part they are obsolete, leaving it smooth. The teeth are small and unusually divergent for a Petricola. This shell is smaller and more compressed than any of our described species. In form it much resembles Saxicava vaginoides, Desh., but it is more transverse and differs in the hinge. FAMILY NYMPHID.E. GENUS PSAMMOCOLA, (BLAINVILLE.) P. LUCINOIDES, PL. 34. FIG. 16. P. testa sub-orbiculari, pene cequilaterali, postice et antice rotundatd, convexd, tenui, striatd; striis concentricis, minimis; natibus prominentibus, sub-rectis; valvd sinislrd dentibus duobus cardinalibus, quorum unus bijidus, late- raiibus nullis. Shell suborbicular, almost equilateral, rounded anteriorly and posteriorly, convex, thin, striate; striae concentric, very small; beaks prominent, nearly straight; left valve with two cardinal teeth, one of which is bifid, and no late- ral ones. Diam. .15. Length .31. Breadth .35 of an infth. Remarks. This shell is unusually lenticular for a Psamnoocola. The concentric striae are numerous and extremely small. There are, however, three or four larger ones, nearly equidistant, over the surface of the shell. The general resemblance which this shell bears to some species of the genus Lucina, will readily distinguish it from its congeners. I have adopted this genus on the authority of Sowerby, who says that in it Blainville unites the Psammobia and Psammoteea of Lamarck, considering the difference between these genera as artificial and accidental. P. REGIA, PL. 34. FIG. 17. P. testa transversa, ovato-quadratd, inaequilalerali, postice hiante, antice et postice subtruncatd, valde inflata, crassissimd, sulcatd; sulcis radiantibus, crebris, aqualibus, latis; margine basali pene recto; margine dorsali sub-cur- 14 NEW FOSSIL SHELLS tato; natibut valde elevatis, acuminatis; in valvi utraque dentibus cardinalibus duolus, lateralibus nvllit; nymphis rurtis. crassis; lunula parvfi, cordata; cicatricibus maximis; cicatrice palleali valde situtalu. Shell transverse, ovately quadrate, inequilateral, gaping posteriorly, subtruncate anteriorly and posteriorly, very much inflated, very thick, sulcate ; sulci radiating, numerous, equal, wide; basal margin almost straight; dorsal margin slightly curved; beaks much elevated, acuminate; hinge in each valve with two cardinal and no lateral teeth; nym- phffi short, thick; lunule small, cordate; cicatrices very large; palleal impression much sinuated. Diam. 1.25. Length 1.56. Breadth 2.30 inches. Remarks. The radiating sulci are largest and deepest on the posterior extremity of the shell; they are interrupted by occasional lines of growth. The palleal impression becomes very broad as it approaches the anterior cicatrix. It is very rugose, and lias a large, semi-elliptical sinus posteriorly. In the right valve, one of the teeth is bifid, but, as in all my specimens the hinge of the left valve is fractured, I am unable to say whether this be the case in it or not. The outline of the shell is very variable. I have one specimen which is nearly oblong, with a sinuated basal margin and almost central beaks. In this form its external appearance approaches closely that of the Area centenaria of Say. Judging from description^ this shell must resemble the Petricola centenaria, Conrad, but its nymphae, teeth and sinuated palleal impression, exclude it from that genus. It is larger and more beautiful than any of its congeners* GENUS LUCINA. L. PUNCTULATA, PL. 34. FIG. 18. L. testa rotunda, lenticular!. sub- sinistrorsum deflecto, lavi; foramine elliptico; aperturd quadratd, oblongd. * A SXOIJH&OC, navigiolum. 22 NEW FOSSIL SHELLS Shell conical, somewhat elevated, thin, diaphanous, costate; costs longitudinal, noduliferous, alternate; apex produced, incurved, with one whorl, deflected to the left; foramen elliptical; aperture quadrate, oblong. Height .04. Length .07. Breadth .05 of an inch. Remarks. The nodules on the ribs are placed in regular series, giving the effect of cancellating transverse striae. The ribs are alternately large and small, which, I believe, is the case with all our fossil species of these shells. The foramen is widely elliptical, approaching to circular, and placed at some distance posterior to the apex. The apex is large, bent to the left, and twisted into rather more than one whorl. The shell is not much elevated. But two species of this interesting little genus have been hitherto described. One, the C. noachina, Leach, is from the coast of Great Britain, the other, C. princeps, Mighels and Adams, from that of New England. The one now before us is, I believe, the first fossil species. It differs from the others principally in its minute size, the absence of an internal plate, and the circular form of the foramen. GENUS CALYPTR^EA. C. PILEOLUS, PL. 35. FIG. 38. C. testa irregulariter conic/I, crassd, sulcatd; sulci s radiantibus, magnis, irregularibus ; strlis concentricis, par- vis; apice laevi, contorto anfractibus duobus; aperturd sub-rotunda; cyatho magno, lato, angulato. Shell irregularly conical, thick, sulcate; sulci radiating, large, irregular; concentric striae minute, small; apex smooth, twisted into two whorls; aperture sub-rotund; cyathus large, wide, angular. Diam. .80. Height .40 of an inch. Remarks. This species varies very much both in outline and height, some specimens being nearly flat, while in others the perpendicular distance from the apex to the base is nearly as great as the diameter. The cyathus is large, bent at a right angle, and fast- ened to the sides of the shell by the two edges. The sulci vary very much in different specimens, both as to number and size. In general outline, this shell is not unlike the Dispotsea costata, Say, but the form of the cyathus separates it from the Dispota3se, and it also differs in proportionate height. Young specimens are not unlike, in external appearance, the Infundibulum concentri- cum, herein described, as nearly the upper half of the shell is smooth. The peculiar voluted form of the apex, which may also be observed in the Dispotsea costata, Say, and D. ramosa, Con., would almost seem to entitle them to a separate division, were it not that in this family the form of the shells is by no means a criterion for that of the animal, and therefore, until the latter has been examined, no separations should be made. M. Lesson and Mr. Owen, who have dissected the inhabitants of these shells, both say that the difference between the animal of Calyptrsea and Crepidula is by no means sufficient to establish a generic distinction. Mr. Owen, in a paper read before the Zoological Society, observes, " The soft parts of Crepidula are the same with those of Calyptraa, in all essential points of structure, differing only in the proportionate extent of the anterior part of the foot, and dorsal groove of the mantle." M. Lesson,* as quoted * Zoologie de la Coquille, Tom. II. p. 388. FROM THE TERTIARY OF VIRGINIA. 23 by Mr. Broderip, says, " L'animal des Calyptrees et des Crepidules nous parait ne dif- ferer en rien d'essentiel ; et quant a la cloison du test, soit que cette cloison soit trans- versale, soit qu 'elle ne consiste qu 'en lamelles anexees au fond de la coquille, elle pre- sente des passages de ces deux etats, et ne peut servir qu 'a etablir des simples sous- genres, au grand genre Calyptrsea ou Crepidula comme on voudrait 1'appeler." I have therefore put the following shells as merely in sub-genera. SUB-GENUS INFUNDIBULUM (D E MONTFORT.) I. CONCENTRICUM, PL. 35. FIG. 39. 1, testa patdliformi, deprcsso-ccmicd, tenui, simplici; lineis minutis concentricis; apice centrali, anfractu parvo uno; aper- turd sub-rotunda; cyatho recto, varice marginato. Shell patclliforra, depressed-conical, thin, simple; with minute concentric lines; apex central, with one small whorl; aperture sub-rotund; cyathus straight, margined with a varix. Diam. .22. Height .09 of an inch. Remarks. This shell is entirely simple and patelliform, with the exception of one small whorl at the apex. The cyathus is flat and straight, extending from the centre to the margin, with a thick varix at its outer edge. The only Infundibulum, to which this is allied, is the I. centrale, Con., but that species is described as ovate, while this is conical, or even slightly concave. This is one of the shells that show the gradual passage from the Infundibulum to the Crepidula, and the propriety of uniting these genera. Its want of whorls, and the con- centric lines of growth, seem to place it in the Calyptrseee, while the cyathus constitutes it an Infundibulum. SUB-GENUS CREPIDULA. C. PONDEROSA, PL. 35. FIG. 40. C. testa sub-globosd, crassissimd, ponderosd, convolutd, rugosd; sulco prope suturam lato, minime prof undo; suturd parvd; apice vohtto, rotundato, anfractibus sesqui; aperturd arctato ellipticd; cyatho crassissimo, undulato, acie Jlexuosd, vix aperturte dimidiam aquante. Shell sub-globose, very thick, ponderous, whorled, rugose; with a wide, shallow sulcation near the suture; suture small; apex voluted, rounded, with a whorl and a half; mouth narrow-elliptical; cyathus very thick, undulate, with a flexuose edge; scarcely half the length of the mouth. Height 1.15. Length 1.90. Breadth 1.50 inches. Remarks. There are occasional irregular lines of growth over the surface. The sul- cation near the suture is sometimes scarcely perceptible. It usually continues for about one third of a whorl from the aperture, and then becomes obsolete. The mouth is some- times very small and nearly round. The cyathus is extremely solid with two depres- sions on its surface and a waved edge. It is deeply set in the shell, and disappears gradually into the sides, so that its margin cannot be traced. The apex is more voluted than in any species of Crepidula that I have met with. This fine shell has, most probably, been heretofore confounded with the C. costata, Morton, as it is too common and too conspicuous to have escaped observation, and as there are specimens of both under that name in the collection of the Academy of Natural F 24 NEW FOSSIL SHELLS Sciences; but our shell is much larger, more ponderous, with the apex more twisted, and without the spines of the C. costata. I have a number of specimens of each now before me, and I find that these characters obtain at all ages. C. CORNUCOPIA, PL. 35. FIG. 41. C. testa valde tlevatd et convexa, Itevi, polild, crastd; apice termmali. valde producto, votuto, superne sub-angulato, tinislrorsum deflexo; aperturd parvd, ovatd; cyatho profundo, piano, acie curvo. Shell much elevated, very convex, smooth, polished, thick; apex terminal, very much produced, whorled, some- what angular above, turned to the left; aperture small, ovate; cyathus deep, flat, with the margin curved. Height .16. Length .30. Breadth .18 of an inch. Remarks. The apex is very far removed from the margin of the mouth; it is slightly turned to the left, and has about half a volution. The aperture is ovate, approaching to elliptical. The cyathus is situated deep in the shell, so that there is a large cavity under the apex. It is perfectly flat, and its outer margin has a gentle and regular incised curve. I at first considered this curious little shell as identical with the C. convexa, Say, but the differences in the apex and cyathus render the separation necessary. C. LAMINA, PL. 35. FIG. 42. C. testa, discoidale, planissima, tenui. leevi; apice elevato, polilo, sinistrorsum deflexo, anfractibus sesqui; aperturd magnd, subrolundd; cyatho parvo, tenui, convexo. Shell discoidal, very flat, thin, smooth; apex elevated, polished, deflected to the left, with a whorl and a half; aperture large, subrotund; cyathus small, thin, convex. Height .03. Length .18. Breadth .15 of an inch. Remarks. The most peculiar character in the species now before us, is in the shape of the apex. This is perfectly smooth and polished, rising suddenly from the flat back of the shell, and twisted into about a whorl and a half. The margin of the mouth projects anteriorly beyond it, so that it is invisible on a front view. There are small concentric lines of growth aver the surface of the shell. The cyathus is slightly and regularly convex. When very young, this species, from the peculiar formation of the apex, has a striking resemblance to a small Natica, and I have been for some time in doubt as to what genus a specimen of that age belonged. This shell is closely allied to the C. plana, Say, but the peculiar apex and nearly flat cyathus at once distinguish it. FAMILY BULL^ID^E. GENUS BULLA. B. CYLINDRUS, PL. 35. FTG. 43. B. testd lub-ellipticd, superne et inferne acuminatd, crassd, politd, itriata; spird umbilicatd; anfractu ultimo ad basim et apicem ttriato; aperturd falcatd, inferne laid; columellii refiecla. Shell subelliptical, acuminate above and below, thick, polished, striate; spire umbilicate; last whorl etriate at the base and apex; mouth falcate, wide below; columella reflected. FROM THE TERTIARY OF VIRGINIA. 25 Length .21. Breadth .10 of an inch. Remarks. Although this shell has no very peculiar characters, yet I cannot refer it to any described species. One or two species, the B. St. Hillairii and Dekayi, from Claiborne, are somewhat allied to it, but they are not identical. FAMILY MELANID.E. GENUS PASITHEA, (LEA.) P. EXARATA, PL. 35. FIG. 44. P. testa subulatd, acuminatd, crassd, imperforatd, nitente, costata; spird valde atlenuala, mamillata, ad apicem letvi: suturis profundis, excavatis; anfractibus quindecim, planulatis, costis oblique longitudinalibus crebris planis; an- fraclu ultimo angulato; bast laoi, politd; aperturd parvd, sub-quadratd, sub-effusa. Shell subulate, acuminate, thick, imperforate, shining, costate; spire very attenuate, mamillate, smooth at the apex, sutures deep, excavated; whorls fifteen, flattened, with numerous fiat obliquely longitudinal ribs; last whorl angulate; base smooth, polished; mouth small, sub-quadrate, somewhat effuse. Length .35. Breadth .07 of an inch. Remarks. The ribs are slightly oblique. They disappear at both sutures, which are triangular, smooth and deep. They extend, on the last whorl no farther than the angle, leaving the base perfectly smooth. The mouth is ovately quadrate, with sharp angles where the columella and outer lip join the preceding whorls. This shell appears to resemble the Turritella laqueata, Con., but its larger size, mami- late apex, and angular mouth serve to distinguish it from that species. P. STJBULA, PL. 35. FIG. 45. P. testa subulata, crassd, imperforatd, costata, striata; spird attenuatd, obtusd, mamillata, ad apicem polita; suturis profundis; anfractibus oclo, contexts; costis longitudinalibus magnis, crebris, prope basim obsoletis, planulatis, Ics- vibus; striis transversis, parvis, crebris, interruptis; ultimo anfractu rotundato; basi lisversis, quatuor, noduliferis; anfractu ultimo acute angulato, carinato; basi crebre et profunde striatd; perforatione parvd; aperturd quadrangulari. Shell conical, acuminate, thick, polished, perforate, crenulately costate; spire somewhat conical, rather depressed; obtuse; sutures small; whorls four, nearly flat; costce transverse, four, noduliferous; last whorl acutely angular, cari- oate; base closely and profoundly striate; perforation small; mouth quadrangular. Length .13. Breadth .12 of an inch. Remarks. The carina on the periphery of the last whorl is round and polished. There are three large, and one small nodulose costse, the small one being next to the one nearest the upper suture. This much resembles the T. armillus, herein described, but may be readily distin- guished from that shell by its umbilicus, more ovate shape, arid more striate base. T. ARATDS, PL. 37. FIG. 85. T. testa, ovato-conicd, crassd. politd, imperforatd, costatd; spird depressd, sub-ovatd, obtusd, ad apicem lavi; siituris pari'is, linearibus; anfractibus tribus, sub-convcxis ; costis transversis, tribus, magnis, sub-noduliferis; anfractu ultimo aii -a 3 Petafoconchus 4 T&vdtf 5 fistula 6 frasf rocht&fia 7 f*hofas rhomhoidea, 8 Solen // ThraeitL /2 J3 14- J6 77 78 /& 20 compresses fut re& 2? 22 23 24 25 2 27 28 29 a- eievat**. sphceric ascia. lancea. krtevlata. T. Sinclair* m iiina^' ^^. Mod i oia Qpiniqera. 31 Avicula mulfastyula. 32, 'Pecten -rrticrofjlfurci- 33 . tennis 34 Plicaiuia, rizdts 35 Chxteri franjenrLft 36 fhtellas acina.ces J7. Cerrmria, ollonja- 33 Calrptrcea, piltoliu 3.9 J^nfandiiu-lufn, cencenfnMm 4:0 Creft^fulcL- ponder osa. 41 , coriw-copiae 4.2 , lamina 43 Bulta- ayltnd7-us 44 fasilJtcn cJrnjflta. '4-6 - subula 46 eturnea 48 49 50 turkinapsts del TSuulmr's x .;. 4,.,. M .... Q :<3 , & CO o 51 y&tL 52 53 crasstlafrrum. $4 /Ictceort. ^7 #(? ; n.1- H. C. Lea,, d*L. 67 62 63 64- 6$ 66 f>7- 68 69 D&tphinxiia, c0stuia+-(t, 70 77 72 73 74 7$ 76 77 78 79 80 Delphi nulcL /ipara. 0$liqu&-stria sf trochi/orrnis sizJjconica- cai-inatct lertticultuis T.Sutclatr's < //> f u /* Pf too SI Trorhns 82 2wui parvuia. 9f fusus 97 Succiruun 98 ,i fri 1O4 14 DAY USE RETURN TO DESK FROM WHICH BORROWED EARTH SCIENCES LIBRARY This book is due on the last date stamped below, or on the date to which renewed. Renewed books are subject to immediate recall. TT>9i sn., A '