Return to LIBRARY OF MARINE BIOLOGICAL LABORATORY WOODS HOLE, MASS. Loaned by American Museum of Natural History ■ J7 i P\HK, PROCEEDINGS kJty> (i (UB ACADEMY OF NATURAL SCIENCES t K PHILADELPHIA 1865. PHIL A DELPHI A : PRINTED FOR THE ACADKMT 1865. LIST OF CONTRIBUTORS, With references to the several Articles contributed by each. Allen, Dr. Harrison. On a New Genus of Vespertilionidae 173 Carpenter, P. P. Diagnoses Specierum et Varietatum novarum Molusco- rum, prope Sinum Pugetianum a Kennerlio Doctore, nuper decesso, collectorum 54 Cassin, John. Notes on some new and little known Rapacious Birds 2 An examination of the Birds of the Genus Chrysomitris, in the Museum of the Academy of Natural Sciences of Philadelphia.... 89 On some Conirostral Birds from Costa Rica, in the Collection of the Smithsonian Institution 169 Conrad, T. A. Observations on the Eocene Lignite Formation of the United States 70 Catalogue of the Eocene Annulata, Foraminifera, Echinodermata and Cirripedia of the United States 73 Descriptions of new species of Echinidae 75 Observation on American Fossils, with descriptions of new species 184 Cooper, Dr. J. G. On a new Cormorant from the Farallone Islands, California 5 Cope, E. D. Partial Catalogue of Cold-blooded Vertebrata of Michigan. Part 2 78 Oa Amphibamus grandiceps, a new Batrachian from the Coal Measures 134 Note on a species of Whale caught in the River Delaware 168 Note on a species of Hunchback Whale 178 Third Contribution to the Herpetology of Tropical America 185 Contribution to a knowledge of the Delphinidas 198 Second Contribution to a History of the Delphinidae 278 Gill, Theo. Synopsis of the Genus Pornoxy's, Raf. 6& On the Genus Caulolatilus 66 On the Cranial Characteristics of Gadus proximus, Grd., 69 Note on several Genera of Cyprinoids 69 On a new Genus of Serraniate 104 On a new Generic Type of Sharks 177 On two new species of Delphinidse, from California, in the Smithsonian Institution 177 IV. LIST OF CONTRIBUTORS. Gunther, Alb. Some remarks on Labrus pulcher (Ayres) 77 Helmutb, C. A. New species of Mordellidee collected in Illinois 96 Lawrence, Geo. N. Descriptions of new species of Birds of the Families Paridae, Vireonidas, Tyrannidae and Trochilidae, with notes on Myiarchus Panamensis , 37 Descriptions of four new species of Birds from the Isthmus of Panama, New Granada 106 Lea, Isaac, Descriptions of Three New Species of Exotic Uniones 75 Descriptions of Eight New Species of Unio of the United States 88 Le Conte, Dr. J. L. Note on the Species of Myodites, Latr., inhabiting the UnitedStates 96 Notes on the Species of Harpalus inhabiting America north of Mexico... 98 On the Species of Galeruca and allied Genera inhabiting North America, 204 Prodromus of a Monograph of the Species of the Tribe Anobiinii of the Family Ptinidae, inhabiting North America 222 Lewis, Dr. F. W. On Extreme and Exceptional Variations of Diatoms, in some White Mountain localities 7 Meek, F. B., and A. H. Worthen. Notice of some New Types of Organic Remains, from the Coal Measures of Illinois. 41 Remarks on the Genus Taxocrinus (Phillips) McCoy, 1844; and its rela- tions to Forbesiocrinus, Koninck and Le Hon, 1854, with descrip- tions of New Species 138 Descriptions of New Species of Crinoidea, &c, from the Palaeozoic Rocks of Illinois and some of the adjoining States 143 Descriptions of New Crinoidea, &c, from the Carboniferous Rocks of Illinois and some of the adjoining States 155 Note on the Genus Gilbertsocrinus, Phillips, by F. B. Meek... 166 Contributions to the Palaeontology of Illinois and other Western States, 245 Observations on the Microscopic Shell Structure of Spirifcr cuspidatus, Sowerby, and some similar American Forms, by F. B. Meek 275 Tryon, Geo. W. Synonomy of the Species of Strepomatidae, a Family of Fluviatile Mollusca inhabiting North America. Part 4 19 Winchell, Alex. Descriptions of New Species of Fossils, from the Marshall Group of Michigan, and its supposed Equivalents in other States ; with Notes on some Fossils of the same Age previously described, 109 Wood, Dr. H. C. New Polyzonidas * 172 Worthen, A. H. See Meek. PROCEEDINGS OP THE ACADEMY OF NATURAL SCIENCES OP PHILADELPHIA 1865. January 3d. Mr. Joseph Jeanes in the Chair. • Thirteen members present. The following paper was presented for publication and referred to a committee : " On extreme and exceptional variations of species of Diatomacese. etc." By F. W. Lewis, M. D. January 10th. The President, Dr. Bridges, in the Chair. Twelve members present. January 17 th. The President, Dr. Bridges, in the Chair. Fifteen members present. The following paper was presented and referred to a committee : " Eemarks on the genera Semicossyphus and Trochocopus." By Dr. A. Giinther. January 24th. The President, Dr. Bridges, in the Chair. Ten members present. The following paper was presented and referred to a committee : " Synopsis of the Strepomatidae, &c, Part IV." By George W. Tryon, Jr. The Secretary announced the recent death of Dr. R. M. S. Jackson, late a Correspondent of this Academy. 1865.] 1 PROCEEDINGS OP THE ACADEMY OP January 31st. The President, Dr. Bridges, in the Chair, members present. On report of the respective Committees, the following papers were ordered to be published : Notes on some new and little known Eapacions BIRDS. BY JOHN CASSIN. 1. Polyborus Audubosii, nobis. Polyborus vulgaris (Vieill.), Aud., Orn. Biog., ii. p. 350 (1834). Polyborus brasiliensis (Gm.), Aud., B. of Am., Oct. ed. i. p. 21 (1840). Polyborus tharus (Mol.), Cass., B. of Cal. and Texas, i. p. 113. Aud., B. of Am., pi. 161 ; Oct. ed., i. pi. 4. Back and rump brownish black in all ages and stages of plumage, (not transversely banded as in P. tharus.) Under tail coverts white, nearly pure, or with a few indistinct traces of dark transverse bands on the longer fea- thers. In all other respects very similar to P. tharus of Chili and other coun- tries on the Pacific coast of South America. In P. tharus the back and rump are transversely banded with brownish black and white, in all ages, and the under tail coverts are white, with well defined transverse narrow bands of dark brown. In size, the present bird seems to be rather the larger. The specimen now described is Mr. Audubon's type from Florida, presented by him to this Academy, and is very accurately given in the plates above cited, the upper figures in which represent the black upper parts as above described. In his descriptions, he says " cere carmine" which color is also given in his plates ; but in the South American species, seen in abundance in Patagonia by Dr. Charles Pickering, during the voyage of the United States Exploring Expedition in the Vincennes and Peacock, that distin- guished naturalist says explicitly, " The skin about the bill has not the bright red color as given in Mr. Audubon's figure from a Florida specimen." (Mamm. and Orn. U. S. Expl. Exp., p. 100.) This difference in the color of the cere may be characteristic, though more probably, in my opinion, it is dependent on season only, the brighter or red color being that accompanying the more mature or nuptial plumage, which is the case in the Rasorial or Gallinaceous birds, and analogous groups throughout the circle of Birds. Numerous spe- cimens of this species, from Texas and Mexico, are in the collection of the Smithsonian Institution. 2. SriLORNis Bacha, (Daudin.) Falco Bacha, Baud., Traite" d'Orn., ii. p. 43 (1800). Spilornis Bacha, (Daud.) Cass., Proc. Acad. Philada., 1859, p. 31. Le Vaill., Ois. d'Afr., i. pi. 5. In a Catalogue of birds collected by Mr. DuChaillu in the countries on the Gamma and Ogobai Rivers, Western Africa, printed in the Proceedings of the Academy, as above cited, I applied the name Spilornis Bacha to a species, one specimen of which was in that collection and is now in the Academy Museum. This specimen is evidently that of a young bird bearing little resemblance in colors to the adult, and I have seen no other of the same species from West- ern Africa. In the statement in the Catalogue alluded to, that this species is "quite identical with the Bacha of Southern Africa, of which a very com- plete series is in the Academy Museum," I may have been mistaken in relying on such specimens as being from that continent. I do not know, however, ihat such is certainly the case ; the specimen now before me from Western Africa so nearly resembling other young birds in the Academy Museum, un- [Jan. NATURAL SCIENCES OF PHILADELPHIA. 6 ■doubtedly the species usually regarded as S. Bacha, and variously labelled as Asiatic and African, that I am not quite sure that Bacha is not an African species, whatever else may have been advanced in any other behalf. There are in the Academy Museum, several specimens of the bird usually regarded as F. bacha, which have been labelled in Europe as from South Africa. If I committed an error, it was not because I relied on those la- bels, of the authority of which I know nothing, nor can now discover any- thing, but that I took them only as confirmatory of an impression that F. bacha was an African as well as Asiatic species. If in error, I was directly misled by the statement of that great naturalist, Temminck, in PI. Col., i. liv. iv., to this effect : " La Buse bacha, Falco bacha, des catalogues me'tho- diques, est re"pandue non-seulement dans l'Afrique m6ridionale, mais on la trouve aussi dans l'lndie, a Java et a Sumatra." Statements of a similar import I have seen elsewhere. It is, of course, possible, that Temminck and others may have relied solely on Le Vaillant without other information. But, notwithstanding the impeachment of the veracity of Le Vaillant, and the opinions on that point that have, in some instances, been freely ex- pressed, and seem to be rather fashionable, I shall not admit, I beg to say, either that Spilornis Bacha is not an African bird, or that Le Vaillant's ac- count of the species to which he applied the name Bacha is not reliable, without further occasion. Those opinions I do by no means participate in nor approve, and instances of the expression of such have occurred, which present themselves to me in no other aspect than that of unqualified imper- tinence, and as demonstrative not only of deficient information on the part of the writers, but of a disposition to seek a short and easy road to notoriety by rude assaults on the reputation of a great practical, and most useful natu- ralist, whose only faults were an enthusiastic devotion to Natural History, and failure to elicit the appreciation of men of dissimilar temperament and greater stolidity of ambition. The fair fame of Le Vaillant has passed the ordeal of one-half century productive of great naturalists, and its impeach- ment will not, I suspect, blazon the reputation of any one likely to be such in the present cycle of similar period ! , There are now before me, a series of fourteen specimens of the bird pur- porting to be F. Bacha, from the Academy Museum, about half of which are in various stages of young plumage, and of the whole of which scarcely any two are precisely alike in colors. One stage of young plumage is un- doubtedly that given by Temminck, under the name liFalco albidas, Cuv.," in PI. Col., 19. As stated above, a few of these specimens have been labelled in Europe as coming from " South Africa," of the validity of which locality I know nothing. Other specimens are undoubtedly Asiatic, and, though differing from each other in some particulars of character, and, per- haps, representing several supposed species, they are all probably to be re- garded as that entitled to the name Spilornis cheela, (Daudin). Several specimens so nearly resemble Temminck's figure of F. albidus, above cited, that they cannot be mistaken for any other species. I do not clearly recog- nise the nearly allied species, though they may be quite valid, especially F. bido, Horsfield. Le Vaillant's figure of " Le Bacha," Ois. d'Afr., i. pi. 15, does assuredly bear a strong resemblance to the Asiatic bird, and I am not prepared to deny that it represents either an Indian or Malayan species ; but it is also a fact, that the young bird from Mr. DuChaillu's collection bears a most unmistake- able resemblance to young birds, undoubtedly Asiatic, in the Academy Mu- seum. On inspection and comparison of any of the Asiatic with the African specimen, few naturalists would hesitate in pronouncing them identical, and the conclusion is most directly indicated that, if this African specimen is not of the same species as the Asiatic specimens, it is of a very nearly allied species. I regard it as possible, that Le Vaillant may have given a figure 1865.] 4 PROCEEDINGS OF THE ACADEMY OF from an Indian or Malayan specimen, under the full and honest conviction that it was exactly the bird seen by him in the mountains of the Great Nama- quois, — a description of error (if it is such) in which he is by no means singular. One of the most eminent ornithologists of our own times is stated to have given figures of a species of Loxia from American specimens, in his Splendid work, " The Birds of Europe," — and if so, entirely justifiably, the European and American species never having then been suspected of being different species. The specimen now before me, from Western Africa, I regard as proving conclusively that a species, at least nearly allied to Spilornis ckeela and 8. bido, inhabits Africa, and I have no doubt that this species was seen and described by Le Vaillant with entire truthfulness. He may not have figured a specimen obtained by himself, but even on this point there is only hypothetical conjec- ture, not evidence. The bird described by him is, moreover, entitled to the name Falco Bacha; an appellation given by Daudin, as cited above, entirely on the faith of the description in Oiseaux d;Afrique. No Indian nor Malayan species is fairly entitled to this appellation, though it has been applied to both, with observations thereon not quite warranted by the facts. Various, not remotely allied, forms have recently been discovered in Africa, (Circaetus zonurus, fasciolatus, and others.) and my opinion is, that the adult of this species of Le Vaillant will yet be forthcoming. 3. Haliaetus Blagrus, (Daudin). Falco blagrus, Daud., Traite d'Orn., ii. p. 70, (1800). Le Vaill., Ois. d'Afr., i. pi. 5. In the Catalogue of Mr. DuChaillu's collection in the Camma and Ogobai country, above alluded to, I gave this name to a specimen of a young bird which I regarded as identical with others in the Academy Museum. On re- examination of this specimen, I am inclined to doubt its identity with any species known to me, though it is in plumage not sufficiently mature to com- pare satisfactorily or to determine from my present materials. It is so much smaller than the young H. vocifer that I cannot believe it identical, though bearing some resemblan»e to the youngest specimen of that species (H. voci- fer) in the Academy Museum. The feet, especially, are disproportionately smaller and weaker. In the Haliaeti of North America, there is a very con- siderable diversity of size, but never so great in the same species, to my knowledge, as in the specimens here mentioned. Though, perhaps, too young to present even structural characters in a re- liable degree, the present specimen seems to show relations to the Asiatic group of which H. leucog aster is a well known species, and of which Mr. Blyth and Dr. Jerdon give the name Falco blagrus, Daudin, as a synonyme. Without being able, at present, to assent to this disposition of F. blagrus, I regard the views of those excellent naturalists as at least an important ap- proximation to its relationship, but am disposed also to suspect that my specimen may be the young of a species the adult plumage of which remains to be discovered. I regard it as undoubtedly the young of the Blagre of Le Vaillant, as above cited, the credibility of whose narrative in relation to which I do not doubt in any particular. The relative size of the feet in this species and in H. vocifer may readily be seen in plates 4 and 5 of that author's Oise- aux d'Afrique. 4. Limnaetus akricanus, nobis. Belongs to the same group as L. cirrhatus (= Falco limnaetus, Horsf.) and L. Kieneri, and bears a general resemblance to both of those species, and is about the same size. Upper parts black, under parts white. General form very strong ; bill rather short, fully curved ; edge of upper mandible lobed ; wing moderate, fourth and fifth quills longest, and nearly equal; tail rather long ; tarsi thick, and densely feathered to the toes, the bases [Jan. \ NATURAL SCIENCES OP PHILADELPHIA. 5 of which are also feathered ; toes and claws very strong. Entire upper parts brownish black ; plumage of the back and neck behind white at base ; rump and upper tail coverts with concealed large spots of white ; quills brownish black on their outer surface, with a few transverse bands of a darker shade of the same color, and with a large space on their inner webs white ; under surface of quills white, with about three transverse bands of black. Entire under parts white ; flanks, under tail coverts and tibial plumes externally with large spots of brownish black ; tail on its upper surface dark ashy brown, with about five wide transverse bands of brownish black, and nar- rowly tipped with white, on its under surface ashy white, with a few trans- verse bauds of black. Under wing, coverts white, with large spots of black ; tarsi white ; cere and toes yellow; bill dark bluish brown. Axillary feathers brownish black, the black spots on the under wing coverts unitedly form a large space of that color on the under surface of the wing. Total length about 22 inches; wing 14; tail 9^; tarsus 2| ; bill, from corner of mouth direct to tip of upper mandible, 1£ inches. Ilab. — Ogobai River, a tributary of the Camma River, Western Africa. Spec, in Acad. Mus., from Mr. DuChaillu's collection. Two specimens of this Hawk-Eagle are in the collection from the Camma River, above mentioned, and appear to represent a species hitherto unknown, probably generically different from any other of Western Africa. Though, in my opinion, properly to be included in the group Limnaetus, this bird is more strongly organized than either L. niveus, cirrhatus, Kienerii, or other of the Asiatic species that have come under my notice, and more decidedly aquiline in some points of character. The tirsi are very thick and densely covered, much more so than in either of the species just mentioned, and quite as much so as in the larger Aquilse, or as in the Owls of the genus Bubo. The bill also is strong and fully curved. No crest is apparent in either specimen, though there is, perhaps, a slight elongation of the occipital feathers. 5. Otus stygius, (Wagler.) Ni/ctalops stygius, Wagl., Isis, 1832, p. 1221. Archives du Mus., Paris, 1844, pi. 24. Several specimens of this little known species have been received at the Smithsonian Institution in the valuable collections presented by Mr. Sarto- rius, and obtained hy him at Mirador, near Vera Cruz, Mexico. All of them correspond with the descriptions of both Wagler and Pucheran, though darker than the figure given by the latter, as above cited. On anew CORMORANT from the Farallone Islands, California. BY J. G. COOPER, M. D. Gkaculus Bairdii, Gruber, MSS. The White-patch Cormorant. ? Graculus leuconotus, Audubon. Specific Characters. — Male in spring. Head and neck changeable violet and purple with green reflections ; body dark green. Back and wings greenish purple, the quills brownish towards their ends and beneath. Flanks with a large while patch on each side about equal in size to the bird's foot, mostly concealed by the wings when folded. Tail like the wings. Head with a crest of narrow loose feathers about an inch long, arising on the middle of ver- tex above the eyes ; another similar crest arising just behind the occiput, rather longer. Bill very slender, subquadrangular, strongly and abruptly hooked. Length 27 inches ; extent 40.00, wing 10-75 ; tail 7, bill along ridge 1*90, along gape 3'00, its height and width at base each about 0-50 inch ; tarsus 1"50 ; outer toe and claw 3-76 ; inner do. 1-30; second and third quills about equal, longest ; half an inch longer than secondaries and an inch 1865.] 0 PROCEEDINGS OP THE ACADEMY OF longer than tertiaries. Iris green, bill horn-black ; feet pure black. Gular sac black, with red marks (shrinking and looking dull red when dry). A nar- row patch of skin around eye, extending as far back as that around angle of mouth and gular sac. A sharp angle covered with feathers extends on middle line of throat, a little further forward than eyes. Forehead feathered down to bill, leaving only a narrow loral space bare. This species is closely related to the G. violaceus of the Oregon and Wash- ington coasts, and replaces it as on the coast of upper and lower California. According to Mr. James Hepburn, it differs in a much more slender bill and other points of structure, as well as in the presence of the conspicuous white patches on the flanks. In 1834 Mr. J. K. Townsend saw "at Cape Disappointment ten Cormorants, one with a white tail, the others with a white rump," which, without further description, Mr. Audubon called Phalacrocorax leucurus and P. leuconotus. It is quite possible that Townsend might have referred to P. bairdii, in his notes as above quoted, but as neither attribute applies to the present species the names would be inadmissible, even if accompanied by a diagnosis. I myself saw what I believed to be this species at the mouth of the Columbia River, in July, 1854, but could not obtain specimens. Mr. F. Gruber, of this city, was the first to secure specimens of the species and distribute them as P. bairdii, (named after Prof. S. F. Baird, of the Smithsonian Institution) and informs me that the species was published under that name in Germany, al- though I have not been able to find it, and think it is possible that it may still be a manuscript communication. It is with great pleasure that I append the following note on this species : Note on Graculus Bairdii, the White patched Cormorant of the Farrallone Islands, California, by James Hepburn, San Francisco. (From a letter addressed to the Smithsonian Institution, dated Dec. 30tb, 1862. "While at Barclay Sound, I noticed that there appeared to be a Cormorant there about the size of the one from the Farallones — but without any white spot. I could only get one of them, and that on the last day I was out. On examining it, I found that it was of the same size as the other, but it had an orange gular pouch, as described by Audubon, whereas the other, as I have already insisted, has a dusky pouch, with numerous bright red papillae, much too striking a point to be overlooked by any one who sees the bird while in the flesh. Another difference is that the irides of the former are brown, those of the latter sea-green. The plumage too is dissimilar in color, though both of them might fairly be called violet green. In the Farallones' bird, however, the green greatly predominates, in the other the violet. With respect to the white spot, I have seen the bird with it as early as February, and as late as the middle of July, at which time it showed no signs of disappearing, though the G. dilophus had months previously lost its crests. I have never been able to see the bird in autumn, which I am very anxious to do. If, as I think, it then appears with the white patch, the question of its being the breeding plumage is disposed of. At any rate the birds in Barclay Sound had no patch at the end of March. The only remaining conjecture is that one may be the young of the other ; and this I find is Dr. Suckley's idea, who appears to have remarked both kinds at Cape Disappointment. To this I object that I do not know of the patchless bird having been noticed in California, and I am very certain that I saw none with a patch about Vancouver Island. As to their frequenting Cape Disappointment, that would only prove that to be the boundary line of their respective habitats. I am aware that it is danger- ous work to build speculations as I am doing, on a single specimen ; but I shall do my best to find out where the northern bird breeds, and to obtain a sitting bird with its eggs ; and then should the differences be equally marked at that period, if there is any such thing as species, the two birds must, I think, be pronounced distinct." [Jan. NATURAL SCIENCES OF PHILADELPHIA. i On extreme and exceptional variation of DIATOMS, in some White Mountain localities, &c. BY F. W. LEWIS, M. D. In my notice of some new and singular intermediate forms of Diatomaceie from the Saco headwaters, in the Proceedings of the Academy for December. 1863, I advanced a theory based ou the comparative absence of Synedra and Nitzschia in the sub-peat of this country, that these curious species were trans- ilionary or comprehensive types conducting from Surirella and allied genera, to- wards the more modern Synedra and Nitzschia ; and that their continuance as living organisms probably depended on exceptional conditions of soil and water, more or less limited in their influence, peculiar to the Saco and similar localities. Since the publication of that paper I have received from my friend, Mr. C. Stodder, of Boston, a very interesting lot of slides containing all of these anomalous species, prepared by himself and Mr. R. C. Greenleaf, of Boston, from gatherings at various points along the White Mountain range. His localities are as follows : (1.) " Brook near the Flume," (Franconia Notch) — thirty miles from the Saco pond, and near the western outlet of the valley; contains Surirella Baileyi, S. intermedia, Actinella punctata, Eunotia incisa. (2.) " Lafayette Mountain Lake," not many miles distant from the preceding- This lake is at a considerable elevation ; a still sheet of water ; contains Su- rirella intermedia, Actinella punctata, Eunotia incisa, Synedra hemicyclus. (3.) "Brook near Bethlehem," on the S. E. side of the Crawford Notch (Saco) about 15 miles distant, also in the valley ; contains Surirella intermedia, S. anceps, S. delicatissima, S. Baileyi, Synedra hemicyclus. (4.) " Maurans Lake," on the Cannon Mountain, near Franconia; contains Surirella Baileyi, S. anceps, S. delicatissima, Actinella punctata, Synedra hemicyclus. Of this locality Mr. S. writes, " This Lake is on the Cannon Mountain at a high level rarely visited by travellers. The gathering is surface water." (5.) " Bemis Pond," not many miles from the Saco spring, is a small Lake. The gathering, according to Mr. S., is " a peculiar sub-aqueous deposit" form- ing the bottom of the pond, " about six feet thick, and composed of nearly pure diatoms." The contained species are Surirella Baileyi, S. intermedia, S. anceps, Eunotia incisa. Mr. Stodder adds, " that in his opinion the only explanation of the origin of this and other similar deposits is afforded on the supposition that these diatoms were originally carried out into the still waters of the lake by small streams, and there deposited," an explanation not altogether satisfactory, as most of the species are still-water forms : Navicula rhomboides, N. firma, N. major, Eunotia robicsta," §c, usually found in ponds and boggy pools. Similar deposits, not containing any of the transitionary species, occur at other localities in New England. One of the most remarkable, ten feet in thickness, is at Randolph, Massachusetts, another at Bristol, N. H. Mr. S. thinks, also, that these beds have been deposited at varying periods since the glacial period. (6.) "Echo Lake" (Franconia Notch,) a remarkably beautiful pond lying in. the very gorge of the Notch ; contains Surirella intermedia, Synedra hemicy- clus, Eunotia incisa, and curious varieties of Navicula serians and Odontidium tabellaria, hereafter to be noticed. (7.) " Gibbs Falls," a short distance from the Saco springs to the west, contains Surirella intermedia, S. delicatissima, Actinella punctata, Eunotia incisa, along with recent species. (8.) " Milldam at Gorham," on the Glen side of Mount Washington, con- 1865.] 8 PROCEEDINGS OP THE ACADEMY OF tains Surirella intermedia, S. anceps, S. delicatissima, Eunotia incisa, §c, along with recent species. These localities are all within the range of glacial influence. After a careful examination of the slides, prepared from gatherings from these localities, I have been struck not only by a general correspondence in their species and varieties to those of the Saco and Wolfboro muds, but also by their unlikeness to species and varieties outside the White Mountain tract. In speaking of the Saco and Wolfboro species I alluded to their general re- semblance to those of the sub-peat and peat deposits ; the same remark of course holds good in reference to Mr. Stodder's localities. I will here simply confine myself to the statement of this general resemblance which further on will be illustrated by a table of species. There is one point, however, relating to the curious tendency to variation, usually on a definite direction, apparent in many of these localities in com- mon with post-tertiary deposits in other northern sections of this country, which requires ft passing notice. This tendency, which for convenience I shall call metamorphic, seems to co- incide with the abundant introduction of certain genera in new localities. It is marked by a singular relaxation of the laws governing what I have before termed the non-essential characters of genus ; in other words, while respecting the more fixed and positive generic characters (essential,) as alee, canaliculi, median lines, nodules, §c, it would seem to exhaust its influence on the more general and unimportant ones, as size, outline, striation, &c, common to all diatoms (non-essential.) Besides the intermediate or comprehensive type already spoken of, there would appear to result from this metamorphic tendency a subjective variation in many co-existing genera whether allied or not to the incoming one. This variation, which is not always special in its direction towards any type or genus, affects principally the size, form, valvular outline and striation of many species, manifesting itself oftenest in a disposition to assume an undulate, crenulate, apiculate or even cruciform shape ; more rarely to lose these characters. It would seem to originate in a superabundance of the sporangial element, and frequently begets irregular, abnormal or unsymmetrical forms, according to the more or less spasmodic or intermittent action of the disturbing force. I may add that, in accordance with a well known law, most of these so formed varieties, where involving alteration of generic characters, as Surirella interme- dia, S. anceps, &c, or where irregular and unsymmetrical, as Actinella, either rapidly disappear by a process of degeneration (visible in S. intermedia,) or revert to the normal type, while the extreme varieties, not implicating generic character, on the other hand may often become more or less permanent, as in Navicula Jirma, N. rhomboides, N. serians, and others. To render more intelligible what I have tried to explain above, I shall now notice a few of the most remarkable varieties contained in the Saco spring, Wolfboro, and Mr. Stodder's localities. (1.) " Navicula sekians" (Kutz.) " V. acute ; transverse stria? faint, 60 in •100; longitudinal distinct, 36 in -100 :" frustules often cohering: Length •0017" "to -0035"," (Smith.) (2.) Var. a {apiculate.) V. varying from lanceolate elliptic to rhomboid, with apices more or less produced and capitate (fig. 5a, pi. ii.) (3.) Var. b (cruciform.)— N.follis, (Ehr.) =N. inflata, (Ehr.) ? "V. much inflated, compressed, sloping abruptly towards the produced and often trun- cate apices ; extreme variety cruciform," (fig. bb, pi. ii.) Var. a. (apiculate) about two-thirds, and Var. b. (cruciform) less than one- half the length of the typical form. Striation in both varieties beyond a certain distortion on the latter variety precisely resembling that of the typical form. [Jan. NATURAL SCIENCES OF PHILADELPHIA. 9 My attention was attracted long since, by the singular likeness, in striation, median nodule, and general character, of Navicula serians to N. follis, (Ehr.), a form not uncommon in northern post glacial deposits. Ehrenberg's loose figures of the latter (Ar. follis), give so many varieties of outline, and his description is so vague, that in time it seems to have become confounded by the English writers, with Navicula' inflat a, a species having no analogies to it beyond a slight resemblance in outline. Indeed it is probable, that Ehrenberg himself, owing to the use of im- perfect microscopes may have been led to associate these two very distinct species, and in distributing specimens may thus have originated the mistake. However this may be, it is evident that in describing the form called N. follis, in the Bridgewater peat, (Mass.,) he did mean the one figured as var. b. [cruciform), of N. serians, fig. 5 6. pi. ii.* The general resemblance in character, however, would not have sufficed to prove the specific identity of these two forms, viz. N. serians and its var. b. cruciform, — had it not been for the discovery of a second variety which bridges over the interspace — that figured as N. serians, var. a. fig. 5, a. pi. ii. This variety occurs in two of the White Mountain localities, Bemis Lake, and Echo Lake, along with the typical form and the cruciform, var. b, a strong corroborative evidence beside that afforded by numerous intermediate vari- eties of a common derivation. As this is a fact which, if recognized, involves a most important point in its bearing on the laws which determine species, I have drawn with utmost care (fig. 5, a. b. pi. ii.) the valves of what appear to be average specimens of these two varieties. The Bemis Lake' slides of Mr. Samuels, now very difficult to obtain, are very carefully mounted, and afford beautiful illustra- tions of these forms, — as well as of Stauroneis Stodderii, n. sp. (Greenleaf,) (fig. 6, pi. ii.) The material is quite scarce at the present time, although it could no doubt readily be procured from the original locality. (1). "Navicula firma" (Kutz). — Large, turgid, oblong, lanceolate, with obtuse, cuneate ends, thick borders, and large median nodule ; striae wanting, or obscure." (2). "Varieties." — (a), linear oblong, (Navicula iridis.) p. pointed elliptic, (2V. dilatatd). y. cuneate (N. amphigomphus.) (3). " Secondary or metamorphic varieties." S. triundulate, (not the same as N. Ilitchcockii). i produced (iV. producta. 2V. affinis). £. apiculate. (iV. amphirynchus). The specific identity of N. iridis, N. dilatata, N. amphigomphus, and perhaps one or two other reputed species has, I believe, been generally suspected, if not recognized. Certainly, it would be difficult for any one carefully studying the Northern deposits of this country, whether recent or fossil, to resist the conviction, that they really have a common origin. With regard, however, to some of those I have termed secondary or metamorphic, their common deriva- tion from N. firma is not so obvious. I believe them, notwithstanding, to be all varieties of that species, a conclusion I have arrived at, after a careful comparison of gatherings from numerous localities. As, however, a conclusion so formed may be regarded as more a matter of prepossession than admitting of proof, I shall not undertake to illustrate it by elaborate descriptions of these varieties ; but this much may be said, that what has hitherto kept apart many of the best known of them, is simply difference in valvular outline and number of striae. If, hereafter, my view with regard to the unimportance and mutability of these characters be proved correct, the union of some, if not all these reputed species will probably be necessary. Taking all the enumerated varieties, there appear to be certain general (*I am the more certain of this, from my friend Prof. H. L Smith, of Kenyon College, 0., haTing recently written to me, calling attention to this very fact.) 1865.] 10 PROCEEDINGS OF THE ACADEMY OF points of resemblance between them. These are — (1). " The large open median nodular space." (2). The infra-marginal, dark, and more or less broken line or lines, with separa- tion and distortion on the peculiar wavy longitudinal striation at that point." (3). " The sharp, clear, parallel, transverse strirn. This last character seems to me, to afford a valuable clue for determining the primary or secondary nature of any undulate or apiculate form. As a general rule, it will be found, I think, that parallel transverse strice, coinciding with an undulate margin, imply a secondary or metamorphic action on a species whose original outline was smooth; while on the other hand, a radiant trans- verse striation, or, rather, one constantly perpendicular to the marginal line, indi- cates that an undulate outline mprimary. Thus, e.^.the triundulate oatline of Na- vicula Hilchcockii, concurring with & parallel, transverse, striation, is most likely, secondary ; also the crenulate dorsum of Himantidium undulation (extreme variety). While the large and showy Navicula Sillimanornum, (fig. 8, pi. ii.) ought by the same rule to possess & primary outline, although much exagger- ated and intensified. In the apiculate forms, the metamorphic force being operative over but a small terminal portion of the valvular margin, renders the rule less valuable. Although liable to many exceptions, this rule may be sufficiently general to possess a practical value, when taken in connection with other means of proof. I cannot leave these varieties of N. firma, without adverting to the species known as 2V. Hilchcockii, which has been regarded by some, as a variety of the former species. There is a triundulate variety of iV. firma approaching very near to it in size and outline, but differing essentially in the median line, which in N. Hilchcockii is remarkable as having on either side a double line, nearly parallel to its course throughout. That it is of the habit of iV. firma, however, can hardly be questioned; and although not clearly traceable to that species, may it not, perhaps, be a compound variety, resulting from the conjugation of species reputed distinct, but in reality, only so sporangially ? I take occasion here to quote some very interesting remarks of Professor H. L. Smith, who has long been studying the habits of living dialomacex, and whose observations bearing on this and other points in that connection, will, I trust, shortly be made public. In a recent letter to me, speaking on this very subject of extreme variation, he says : " The variety of 2V. firma 9 like iV. Hilchcockii, somewhat, on one of the slides you recently sent me (Saco River,) is curious ; but if you will examine the Bridgewater deposit, I think you will see something about N. follis of Ehr., that makes one almost say it is only a variety of N. serians. The departure is greater, even as to form alone, than that of the specimen of N. firma ? like Hilchcockii is from the type of that species." — He adds; " when I find N. amphirhynchus conjugating and pro- ducing N. firma, Stauroneis gracilis producing St. phenic enter on, and Surirella splendida, S. nobilis, quite different in form and striation, I cannot but doubt the propriety of making a new species out of every different shape and marking." The views of Prof. Smith here expressed, cannot fail to awaken a lively interest in all who desire to have light thrown upon this perplexing question, and it is earnestly to be hoped, that the matured result of his investigations will not long be delayed. Navicula rhomboides is, with one or two exceptions, of all northern species the most common and widely distributed. It offers a broad range of form and outline. Like N. firma, it has its elliptic, produced and apiculate forms. I may preface what I have to say of this species, by remarking that it is, in my opinion, impossible to determine on any positive characters, which shall distinguish it from N. crassinervia. The small apiculate variety which I have [Jan. NATURAL SCIENCES OF PHILADELPHIA. 11 been accustomed to regard as that species, clearly runs into the typical iV. rhomboides, of which it is most probably a colletonemoid (sporangial) offset. Two of the numerous varieties of this species, seem to be permanently distinct — more so, in fact, than in most permanent varieties — although con- nected by intermediate forms with the ordinary type. iV. rhomboides, (Ehr.) V. nearly quadrangular, striae, faint, parallel 85 in. •001". Length -0022", to 0037". (Smith). Sporangial Varieties, (1). (a). " Frustule large, V. rhomboid to lanceolate — median line double, presenting at the terminal nodules a peculiar arrangement, somewhat similar to the " porte crayon" of Dr. Greville, as it exists in If. Lewisiana — only much less obvious." (pi. ii., fig. 11). The transverse striae in this form, are about, 60 in -001", "the longitudinal, about, 45 in -001"." Length variable. Hab. — In nearly all fossil and recent northern deposits. (2). (b). N. diaphana? (Ehr.) V. lanceolate— extremities slightly pro- duced— obtuse, median line thicker than in var. a, terminating in obtuse, rounded, nodular expansions rarely attenuated laterally — striae transverse , about 50 a 55 in -00 L". Longitudinal, coarser and more wavy than in var. a, more or less indistinct for some distance round the central nodule. Hab. — Bemis Lake, abundant, Saco pond, Wolfboro, and other New Eng- land deposits. It is not so common as var. a. (pi. ii., fig, 10). The former of these, is probably the ordinary sporangial variety of iV. rhomboides ; the latter, I have found more rarely in gatherings along the Saco Valley, and — I think, elsewhere in New England — I have been struck with the rarity of both these varieties, particularly, of var. b. on foreign slides.* Var. a, sometimes approaches var. b in outline ; but I have never seen the latter of a quadrangular or rhomboid shape. Occasionally the terminal nodule undergoes a trifling modification, becoming slightly indented at the rounded corners. This may, perhaps, be a compound variety. Figured at pi. ii., fig. 21, is what I believe to be N. Carassius, (Ehr)., (iV. cocconeiformis, (Smith). (Gregory's new British sp. Mic. Jour. vol. iv. pi. L, fig. 22). This is a rare American species, usually fossil. The strias are very hard to resolve. Some of the varieties of this diatom, suggest an affinity to 2V. rhomboides ; but not sufficiently marked to warrant notice. " Navicula Sillimanorum," (Ehr.) An exaggerated variety of this species, I have figured, (pi. ii., fig 8). I nave found it only in the Wolfboro mud. The typical form of Ehrenberg, occurs in some of the N. Hampshire deposits. It is a singularly compact and beautiful diatom — more nearly allied to N. nobilis, than to N. tabellaria — as is shown by the relations of the striae to the marginal line, "which according to the rule before mentioned, indicate the in- tensification of a, primary undulate outline. Navicula gastrum, (Ehr.)? fig. 17, pi. ii). Rare in the Wolfboro mud. I have not come across it elsewhere. The striation is more or less irregularly punctate around the median nodule, and along the median line, as in N. granulata. (Bailey). The striae are radiant — otherwise, it might be set down as a degenerate variety of N. firma. 11 Naviccla placenta," Ehr. fig. 4, pi. ii. — N. apiculata, Greg. (Mic. Jour., vol. iv., pi. L, fig. 13) — N. rostellum. (Smith). This little species is ventricose or elliptic, with a nipple-like projection, at each apex. It corresponds per- fectly in outline, with Dr. Gregory's figure; but the striation is so peculiar in its arrangement, that I have thought it best to figure the valve. The stria; are of two kinds. (1). transverse, sharp, radiant, close. (2). obliquely curved (*Tlie slides coming from abroad, labelled "Amician test," are, I believe, prepared from material obtained from this country.) 1865.] 12 PROCEEDINGS OF THE ACADEMY OP in both directions towards the median line, crossing as in Hyalodiscus subtilis. (Bailey). — coarser than the transverse. These characters are constant in all the specimens I have of this species, from this and other localities.— Wolf- boro, N. H., Duck creek, Del. river. Stauroneis. This genus is very abundantly represented, particularly in the Wolfboro mud. It is common in all post tertiary deposits, and presents a bewildering looseness of character. I have long tried to understand the meaning of S. Baileyi, (Ehr.) and its varieties. Some time ago, I came to the conclusion, that the one having the quadrangular shape and terminal inflexion of St. acuta was a sporangial var. of that species; and that the other (Pteroidea) bore the same relation to St. phenicenteron. This belief has recently been shaken, by my finding the latter variety (Pteroidea) in the " Nova Scotia" deposit, with a very strongly marked terminal inflexion, and the other characters of size, striation, and outline, so variable as to compel the conclusion, that they are both inter- changeable varieties of a common species — possibly St. phenicenteron. A very interesting study of these forms is afforded, by the Nova Scotia, Blue Hill pond, (Me.) and, in fact, by nearly all the northern deposits, recent and fossil. Stauroneis legumen, (Ehr.) The aberrant variety, (pi. ii., fig. 14), will show the range of outline in this species. Frustules of this shape occur sparingly in the Wolfboro mud, along with the ordinary form. Stauroneis amphicephala, (Kutz.) This species I notice, to direct atten- tion to the figure of S. anceps in Prof. Smith's "Synopsis," which, in all re- spects, answers to the description and figure of Kutziug's (Bacillarien, p. 105, pi. 30, fig. 25). S. amphicephala. S. anceps, (Ehr.), is subcapitate with truncate apices, S. amphicephala, capitate with rounded ends. Very likely, these two species are identical. The mere length or relations of the stauros to the margin not constituting a valid reason for keeping them apart. I cannot close what I have to say about Stauroneis and its varieties, without alluding to a stauroneiform tendency which seems to prevail in certain locali- ties. This is marked in the Wolfboro, where seven species of Stauroneis co- exist with a number of stauroneiform varieties of Navicula. I now pass on to notice some varieties of — Himantidium and Eonotia. I have before spoken of the prevalence of these genera in the Saco and cotemporarj' deposits, and likewise of the remarkable subordination of their specific character to the mctamorphic force, as exempli- fied in Himantidium pectinate , and H. arcus, Eunotia robusta and E. incisa. I now give a few illustrations of the most common of these metamorphic varieties, (pi. ii., fig. 12, 13, etc.) which strongly corroborate the view entertained by the late Prof. W. Smith, of the probable common derivation of many of the known British species of Himantidium, from two types ; viz. : II. pectinate and H. arcus. (vide Synopsis, vol. ii., p. 11). Of these varieties, pi. ii., fig. 13a, represents a common sporangial form of Himantidium undulation. It will be seen that the dorsum is already hollowed out as a preliminary step towards another common variety (sporangial) of the same diatom* of which variety I have figured only the extreme and last stage, at pi. ii., fig. b. This last, represents quite nearly two conjoined frus- tules of H. undulalum (type), as does the intermediate variety, two of H. pectinate. Whether or no these remarkable sporangial frustules ever undergo trans- *(Those slides prepared by Mr. Samuels, of Boston, labelled Himantidium undulatum, afford a very fine illustration of this variety, which is abundant in fresh water streams throughout Massa- chusetts) [Jan. NATURAL SCIENCES OP PHILADELPHIA. 13 verge division, I am unable to say from actual observation ; but their ap- pearance is certainly suggestive of that phenomenon. I ought to add, that the secondary gibbosities on the ventral aspect of var. b., are rarely as well marked as shown in the figure (13 b. pi. ii). Of Eunotia incisa, pi. ii., fig. 12a., represents an extreme variety. The ex- traordinary attenuation of the valve well illustrates the synedroid bias, no- ticeable in the Saco, and, to a lesser degree, in the Wolfboro muds. The inflexion peculiar to the terminal portion of the valve in these bacillar varieties of E. incisa, often nearly reaches the dorsum. On the other hand, an opposite variety of E. incisa occurs, which is nearly as broad as long.* Eunotia camelusl (fig. 126. pi. ii.) is probably allied to E. incisa. Some of the frustules are long and narrow, with hardly any perceptible undulation. = Eu. impressa, (Ehr.), occurs sparsely at Wolfboro and Bemis Lake. Eunotia bactriana, (Ehr.), (fig. 16, pi. ii.) is quite common. There appears to be considerable range of variation in this species. Eunotia pentaglyphis, (Ehr.), as figured (fig. 4, pi. ii.) is also a changeable form. It is widely distributed in the post-tertiary deposits, and has all the characters of a metamorphic variety of Eu. robusta. Odontidium tabellaria, (Smith) = Dimereyramma tabellaria, (Ralfs.) I have retained this name, as that by which this diatom is best known. The two varieties figured in Smith's British Diatomaceae, and which may, for convenience, be termed primary and secondary, seem to be peculiarly obnoxious to the metamorphic force. Figs. 1 and 2, pi. ii., represent a series of elongated varieties from the Saco river, (Synedroid). Of these, two are specially notice- able, 2b, and 2d. The first of these has strong marginal puncta ; (Nitzschoid ?) while the second exemplifies the same suggestive principle of symmetrical variation seen in Himantidium undulatum, fig. 13, var. b. pi. ii. The punctate tendency, which is quite exceptional, manifesting itself only on a few frustules, is to a lesser degree observable in Tabellaria, in the same deposit. There remain to be considered, one or two forms in these deposits, which are not clearly traceable to any known species. (1). Navicula (stauroneiform) n. sp. ? (pi. ii. fig. 9). F. V. not ascertained. V. lanceolate, gradually attenuated towards the capitate or sub-capitate ex- tremities. Striae sub-marginal, interrupted for a considerable space oppo- site the central nodule. Hob. — Wolfboro. Common. (Fig. 9, pi. ii.) This little form I have not named, as it may possibly prove a stauroneiform variety of some known species. This stauroneiform habit is very obvious in the Wolfboro varieties ; as is the synedroid, in the Saco. (2). Stauroneis Stodderii, n. sp. (Greenleaf), pi. ii. fig. 6.) F. V. Linear, with slightly rounded ends ; connecting membrane slight and fragile. V. elliptic lanceolate, with more or less produced and slender extremities. Stauros linear, reaching the margin. Strive (longitudinal) parallel, sharp and clear. Variable in number. Stria (transverse), radiant, distinct, about 55 in •001. Length variable. Hab. of St. phenkenteron and St. amphicephala. Bemis Lake, Wolfboro, Gor- ham pond. This beautiful species was first made known to me by Mr. Stodder, who had it from Mr. R. C. Greenleaf, of Boston, who names it St. Stodderii, in com- pliment to the former observer. He has permitted me to describe it. *(Eunotia nodosa. Var. Himantidium pectinate? in the Bemis Lake, presents a remarkable variety, analogous to the above in proportions. It is also nearly as broad as long, and slightly constricted.) 1865.] 14 PROCEEDINGS OP THE ACADEMY OF The valves which are singularly light and graceful, the linear striation giving the surface much the aspect of a scale of Lepisma, are rarely found united by the connecting membrane. Mr. Greenleaf communicates the following facts, with relation to this diatom; " The longitudinal lines are parallel throughout, gradually fading away, so that they are not seen near the apices ; they are faintly visible with careful illumination and focussing over the stauros ; margin beaded." I have not been able to verify Mr. G.'s observations. It seems to me, that the longitudinal striae are internal, and underlie the stauros, and that they are traceable up to the apex, in that limited number of parallel stria; which the narrow area of the extremity can accommodate. The beaded marginal appearance, is probably due to the effect produced by the inflexion of the striae. Mr. Stodder believes the longitudinal striae to be corrugations of the internal membrane, designed io strengthen the valve. The figure (fig. 6, pi. ii.) is not sufficiently elongate for an average speci- men of this species. " Tetracyclic" (abnormal) ? (pi. ii., fig. 3a, & b.) F. V., much as iu the typical form, (genus) ; filament with a central constriction ; frustules small ; septa alternate, equal ; V. deeply constricted in the centre, (not unlike a dumb-bell crystal of oxalate of lime). Hab. of Tabellaria and Tetracyclus. Lafayette Mt. Lake. This singular form occurs only at the above locality. Being minute and much intermixed with Tabellaria and Odontidium tabellaria, it is apt to be overlooked on a crowded slide. The septa are quite insignificant. They exist at both ends of the valve. This anomalous form suggests a metamorphic variation, mediate between Tabellaria and Tetracyclus, and is a true comprehen- sive type, although less perfect than Surirella intermedia. The relations of the septa, small as they are to the valve, and to each other, are constantly those of Tetracyclus, (never of Tabellaria), though the impressible character of outline, passively yielding to the disturbing force, has wandered far away from the typical pattern of that genus.* I will now, as briefly as possible, sum up the conclusions I have tried to establish in this and the previous paper. After which summary will be found a comparative table of some of these species. These are — (1). That the genera Syncdra, Nitzschia, Tabellaria, and perhaps, Odontidium and Himantidium, made their first appearance as prevalent forms on this continent, at varying epochs, since the Glacial period. (2). That there are epochs, which may be termed transitionary, coinciding with the abundant introduction of genera, (as above), marked by a singular relaxation of the laws which govern generic character, (melainorphic force.) (3). This metamorphic force while respecting the more fixed and positive generic characters, {essential), usually attacks the more variable and unimpor- tant characters, (i. e. those common to most diatoms), {non-essential), of those genera most nearly allied to the incoming one, giving rise to comprehensive or synthetic forms ; as Surirella intermedia, Sanceps Sec. (4). During these epochs, there would also seem to exist a subjective variation in many of the cotemporary genera, whether allied or not to the prevailing one — originating in this objective force — still affecting the non-essen- tial characters, principally form and outline, e. g. objective genera Synedra, *(The metamorphic force seems to run riot in this particular locality, (Mt. Lafayette Lake), and nearly all the species appear to participate in this tendency to depart from their normal type. The largest and showiest frustules of the pointed elliptic, which is by far the finest variety of N. firma, pass down through many intermediate forms into a minute and characterless N. affiriie, N. rhnmboides ranges from tho smallest apiculate, up to the magnificent var. b. (pi. ii., fig. 11), curious and anomalous varieties of Tabellaria, of Odontidium tabellaria, some punctate, others Synedroid, eccentric varieties of Synedra hemicyclus, of Eunotia incisa, Eu. camelus, Eu. pentagly- phis, Eu. robusta, of Himantidium gractU, concurring with the abnormal ,Actinella punctata, Surirella intermedia, and & delicatissima, altogether form a grouping confused and incoherent beyond precedent.) [Jan. NATURAL SCIENCES OF PHILADELPHIA. 15 Nitzschia ; subjective genera, Surirella, Himantidium, Odontidium, Tabellaria, Eunolia, and resultant varieties. (PI. ii., figs. 1, 2, 12, 13). (5). An extreme variation, not special in its direction towards any type or genus, extending to the valvular outline of many altogether distinct genera, characterizes these metamorphic epochs ; manifesting itself in disposition to assume an undulate, apiculate or crenulatc contour, or to lose these characters, e. g. Eunotia incisa, Himantidium, Navicula serians, iV. firma ; or in irregular, abnormal or unsymmetrical forms, due probably, to unequal or spasmodic action of the metamorphic force, e. g. Actinella, Tetracyclic, (fig. 3, pi. ii.) (6). These so-formed varieties, where based upon changes of generic char- acter, or where abnormal or unsymmetrical, are always short-lived; on the other hand, varieties not involving generic character, often become fixed and permanent, as Navicula firma, (var. iridis, amphigomphus, §c.) N. serians, var. /?., N. rhomboides. (7). That it is not improbable, that many species not reputed distinct, are capable of conjugating with each other ; and that peculiarities of outline and striation constitute but uncertain data for division of species. Table of Species. (*) Indicates the presence of species at the locality. Localities where the " intermediate type" species occur. Surirella Baileyi " intermedia " anceps " delicatissima. Actinella punctata a> o 6 o JQ 'o CD C0 4-< D M OS en 3 £ 19 -3S S a cS S3 * o M oS O DO "oS "«] 0 a oi t- OS 02 * OS * * 63 (S o * * * * * * * * # #■ * * * * * * * * * * * * * * * * * * Localities of species usu- ally fossil, and of those metamorphic in the direc- tion of Synedra, and c B aS is CD ttf. - a o £ CD 3 6 o OS 02 6 o 3 CD o >-> sS h3 1 .SS ■3 X V * oj 5 * a V a CD * oj oS a S3 = * - ! o 63 CO oj ft "cfj iQ -3 3 * 5 o 'J Some of these species also il- lustrate the ir- regular varia- tion of the next section, (No. 3). Eunotia nodo- * * * * * sa, I have not noted, as it is * * * * * * * * * ■* * but a doubtful Eunotia incisa (long var.) ... ? ? * * # * * * * * * species. * * * * * * * * ■V: •? ? * ? * * * * * * * * 7 ? * ? * * * Jf * 1 1865.] 16 PROCEEDINGS OF THE ACADEMY OP 1 Species illustrating irregular variation not in any special direction. :3 o bL -3 * * ? * * 1 1 * V ? ? * T3 O S oq * * * * * o o a * * * * * * -X- # * 6 c J3 0 * * * * * * * # * *-> HI 0 >J .« 03 * * # * * * 0 Jbt X -3 CO a * * * * * £ a * * * 9 u £1 ■i S3 I =q * * oi v. OS - 03 — * * •X- oj Jd 03 -; 0 — * * * * -:;■ "3 03 * -:;■ * a 03 ■a o * * # " " var. b " " var. b 1 1 I add a list of the ordinary grouping of species in these localities. This is necessarily incomplete and liable to error, owing to the fact that in some of these muds, within the immediate influence of mountain streams, as parts of the Saco spring — the Flume — Bethel — there is a large dilution with more modern forms. These I have excluded and placed in a list by themselves. The absence of these species in the still pond localities of the White Mountains, is, I think, sufficient evidence of their extraneous habitat, when found along with the grouping below. Cymbclla cuspidata, C. helvetica, Epilhemia ventricosa, E. argus, Eunotia robusta, Eu. incisa, Surirella nobilis, S. oblonga, S. decora, Navicula firma, N. serians, N. rhomboides, N. major, N. tabellaria, N. viridis, N. acrospheria, N. radiosa, N. mesolepta, N. borealis, iV. Staureiformis, N. elliptica, JV. cuspidata, Stauroneis phenicenteron, St. gracilis, St. Baileyi, St. anceps, St. legumen, Cocconema lanceolatum, G. cymbiforme, Gomphonema coronalum, G. turgidum, (var. G. capitatum) ? Gomphonema, (var. G. acuminatum), Himantidium areas, IT. pectinate, Odontidium tabellaria, Fragillaria, (doubtful?) — Achnanthidium ? Tetracyclic lacuslris, (rare). Diatoma elongatum, (rare), Tabellaria vulgaris and vars. Orlhosira orichalcea, Cocconeis Thivaitesii, (rare), Nitzschia spectabilis, (rare), Synedra ulna, (rare), Navicula=Amphiprora navicular is, (Ehr.)? (common in sub-peat and peat), Navicula scutelloides, (rare). The following are, probably, extraneous species : — Odontidium mesodon, 0. mutabile, Meridion circulare, Cocconeis placentula, Synedra radians, Nitzchla am- phioxys, N. tenuis, Pleurosigma Spencerii, Gomphonema capitatum, G. geminatum, Asterionella formosa, Colletonema vulgar e. Denticula and Amphiprora are not represented in any of these deposits, unless by one or two doubtful forms, one of which is figured in (pi. i., fig. 6), Amp. ornata, the only fresh water species, is not common so far north. *(I have omitted to notice an abnormal variety of Surirella decora t in 'the Wolfboro mud. This is ovate; the median line extending for little more than one half the length of the valve, leaving an equal open area at either end. From the extremities of the median line, the faint costse branch out with a beautifully radiant arrangement, appearing as if they all arose from the same point. I have found this form also at Montmorency Falls, Canada.) [Jan. NATURAL SCIENCES OP PHILADELPHIA. 17 I had intended, in the present communication, to give a resume of species contained in the "blue clay" of the Delaware river alluvium, and in adjacent localities along the river. This last I shall be obliged to defer; but as several of the figures published in my last paper were designed to illustrate it, I will briefly describe them. "Amphora intermedia," n. sp. ? (pi. i., 7 a, b and c). F. V. linear elliptic, or elliptic ; margin of the inflected portion of the valve recurved, resembling a small ala; marginal puncta distinct, V. arcuate, with rounded apices finely striated. Hab. — Atlantic, N. J., rare. This delicate and beautiful species, belongs to the complex Amphoric of Dr. Gregory. Its outline and appearance on the F. V. are suggestive of Amphi- prora, from which genus, however, the absence of the terminal nodules and its valvular outline remove it. The few specimens I have found, do not en- able me to judge accurately as to its average length or striation. Navicula — n. sp. ? (pi. i., fig. 8) V. rhomboid, with cuneate slightly pro- duced extremities, stria? radiant, moniliform. The only specimen I have of this diatom, is a detached valve, from which the figure (pi. L, fig. 8), is taken. Hab. — Blue clay, Kaighn's point, Del. river. « Amphiprora puLCHRA,var. p. A. convpicua (Greville )? (pi. i., fig. 10, a and b). I am not sure, whether this fine diatom is identical with that figured in the Mic. Journal as A. conspicua. (Trans. Mic. Soc, vol. ix.,pl. 10, fig. 16). My figure, which is carefully drawn from a slide of Rockaway mud, differs certainly from that of the Mic. Journal. The frustules are always twisted, as shown in fig. 10a, pi. i., and the elongated nodules have much the look of canaliculi. Its habit is that of A. pulchra, of which species I have thought it a variety. It rarely attains half the size of that species ; occurs sparingly in many brackish and marine localities. Mastogloia elegans, n. sp. (pi. i., fig. 9). F. V. as shown at pi. ii., fig. 16. V. large, lanceolate, elliptic ; extremities sometimes a little produced ; loculi numerous; very minute ; marginal; striae sharp, clear, parallel ; about 36 a 40 in •001//. Median ?wdule laterally produced into a fine point. Habit and growth of M. apiculata, of which species it may be a permanent variety. I have not, however, been able to trace the connection. It occurs along with M. angulata, and the above, at Atlantic, N. J., Cape May, (Schellinger's Inlet), and as a pure gathering ; abundant. Mastogloia kinsmanii, n. sp. (pi. ii., fig. 15 a and b.) F. V. as shown at fig. 186. V. lanceolate or elliptic, with more or less produced ends ; loculi less numerous than in 31. apiculata or M. elegans ; the central 4 or 5, larger than the others ; (this is a constant character). Median line with a narrow blank space on either side, connivent at the apices; slrice sharp, radiant, about 40 in -001. Habit and growth of the pre. cedirg. Hab. — Cape May, Cold spring, Atlantic marshes. Not an uncommon species at the above localities. The frustule is quite thick, and of a dark, chocolate, brown color, when dry. This somewhat doubtful species I have named (provisionally) after my friend Mr. Kinsman, of this city, who first directed my attention to it, and to whom I am under great obligations for aid in mounting and preserving specimens, and for many valuable hints in their study. There remain to be noticed, two very similar Naviculae, having strong affinities with JY. Lewisiana, (Grew) One of them (pi. ii., fig. 19.) frequently occurs along with it, and is probably, an early stage of that diatom ; and the 1865.] 2 18 PROCEEDINGS OF THE ACADEMY OP other, (pi. ii., fig. 20,) is a not uncommon coastal species. Both are brackish. For convenience of reference, I have provisionally named these forms, whose claims to rank as distinct species are very questionable : (1.) Navicula incomperta, (pi. ii.. fig. 20.) — Y. lanceolate elliptic, with a thick double median line; terminal nodules inconspicuous; transverse stria parallel; about 70 in •00l// ; longitudinal strix wavy, faint, about 55 to 60, in •001. Cape May, Atlantic, and Rockaway Salt marshes, common. (2.) Navicula intkrposita, (pi. ii.,fig. 19.) — V. elliptic, elongated, shorter than in the preceding; terminal nodules usually inconspicuous. Transverse strice sharp, parallel, about 50 a 55 in •001//. Longitudinal, straight, parallel, about 45 a 50 in -001. Paraiba Harbor, S. A. ; Wilmington R., Savannah, Ga. — C. Febiger. The front view of both these species is linear, or sometimes slightly con- stricted, with abruptly rounded ends, to which the suddenly inflected terminal nodule gives an emarginate appearance, as is sometimes seen ia N. rhomhoides. In N. Lewisiana, on the other hand, the front view is commonly a little infla- ted, and the terminal curves much more gradual. The straight and long ter- minal nodule of this last species, subtends the arc formed by this curve, whence, probably, arises a good deal of that apparent inflation of the " extra median" lines, spoken of by Dr. Greville. (Trans. Mic. Soc, vol. xi. N. S. p. 16.) The variation in size, form and number of striaj is very considerable in all of these species from different localities, and for the reason this measures T have given above are only approximate. As opportunity offers, I hope to continue the notice of the Delaware river, and adjacent coastal diatoms. Plate II. Fig. (1.) Odontidium tabellaria. — Sporangial varieties of primary form, (a), ordinary form, /? and y, elongated frustules. (2.) Odontidium tabellaria. — Sporangial varieties of secondary form. (6), punc- tate variety of, c. elongated form, d. double sporangial frustule. (3.) Telracyclus? (abnormal)— a. V. b. F. V. (4.) Eunotia pentaglyphis, (Ehr.) (5.) Navicula serians, a. (apiculale), b. (cruciform) variety=2Vr. follii. (6.) Stauroneis Stodderii, n. sp. (Greenleaf). (7.) Navicula placenta, Ehr. (8.) Navicula Sillimanorum, Ehr. (9.) Navicula (Stauroneiform,) n. sp. ? (10.) Navicula rhomboides. Sporangial var. b. (11.) Navicula rhomboides, Sporangial var. a. (12.) Eunotia incisa. (a) extreme variety, (Synedroid), b. Biundulate variety = Eu. camelus. (13.) Himantidium undulatum. Sporangial, var. a and b. (14.) Stauroneis legumen, Ehr. (15.) Mastogloia Kinsmanii, n. sp. a. V. b. F. V. (16.) Mastoglia elegans, n. sp. F. V. (17.) Navicula gaslrum, Ehr. (18.) Eunotia bactriana, Ehr. (19.) Navicula interposita, n. sp. (20.) Navicula incomperta, n. sp. (15.) Navicula carassius, Ehr. These figures are all magnified 500 diameters. The representations of striae are only designed to give a. general idea of their direction and character, not of aumber, actual or comparative. [Jan. NATURAL SCIENCES OF PHILADELPHIA. 19 Synonymy of the Species of STREPOMATIDJE, a Family of Fluviatile Mollusca inhabiting North America. Part 4. BY GEORGE W. TRYON, JR. The first, second and third parts of this paper* included all the species then known to science, except a peculiar group, of about sixty species of Gonio- basis, inhabiting principally the Coosa River, Alabama. The species of this group are distinguished from others of the genus by their heavy, bulbous or cylindrical, or pupseform shapes, and their very short spires. I was not sat- isfied that they belonged to the genus Goniobasis, and therefore reserved them for further study. Mr. Lea has since eliminated from this group principally, his excellent ge- nus Euryccelon, which still leaves most of the species, however, in Goniobasis. Finding that I am still unable to make a satisfactory separation, I have con- cluded to finish the synonymy, treating these shells as Goniobases. I avail myself of this opportunity to publish those additions and corrections in the synonymy of the first three parts, which the kind assistance of my friends, and particularly of Mr. Lea, together with my own investigations have enabled me to make. Including the species of the present paper, my Catalogue now embraces about five hundred species and three hundred synonymsf. 10, Lea. 1. I. f 1 u viali s, Say. Iojluviatilis, H. and A. Adams' Genera i. p. 299. Brot, Malaco Blatt. ii. p. 114, July, 1860. Io fusiformis, Lea, Chenu, Man. Conchyl. i. f. 1977. Io fusiformis, Say, H. and A. Adams' Genera i. p. 299. Jo tenebrosa, Lea, H. and A. Adams' Genera i. p. 299. Troschel, Archiv fur Naturgesch. ii. p. 130, 1843. 3. 1. s p i n o s a, Lea. Io spinosa, Lea, Chenu, Man. de Conchyl. i. f. 1973. Morcli, Yoldi, Cat. p. 56. Adams' Genera i. p. 299. PLEUROCERA, Raf. 1. P. alveare, Con. Melania alveare, Conr., Midler, Synopsis, p. 46, 1836. Megara alveare, Con., Adams' Genera i. p. 306. Megara torquata, Lea, Adams' Genera i. p. 306. Io pernodosa, Lea, Adams' Genera i. p. 299. 2. P. Foreman i, Lea. Gyrotoma Foremani, Lea, ? Adams' Genera i. p. 305. 3. P. undulatum, Say. Melania undulata, Say, Brot, Mai. Blatt. ii. p. 106, July, 1860. Megara undulata, Say, Adams' Genera i. p. 306. 4. P. e x c u r a t u m, Conrad. Melania excurata, Conr., Midler, Synopsis, p. 43, 1836. ♦Proceedings Acad. Nat. Sciences, Nov., 1863, p. 306; Feb., 1864, p. 24; April, 1864, p. 92. t The species, published by Mr. Lea in the Proceedings of the Academy for 1864, are not all in- cluded in this paper, as the short diagnoses do not allow me to place them in a satisfactory manner. As soon as the full descriptions and figures ate published in our Journal. I will indicate their proper places in this list 1865.] 20 PROCEEDINGS OF THE ACADEMY OF 6. P. n obile, Lea. Io nobilis, Lea, Adams' Genera i. p. 299. S. P.canaliculatum, Say. Io canaliculata, Say, Morch, Yoldi, Cat. p. 56. Ceripliasia canaliculata, Say, Adams' Genera i. p. 297. Melania conica, Say, Sowerby, Mollusca, Fauna Boreali Aineiicana, iii. p. 316, 1836. Gyrotoma conica, Say, Adams' Genera i. p. 305. Melania Sayi, Deshayes, Encyc. Meth. Vers. ii. p. 427, 1S30. 9. P. filum, Lea. Elimiafilum, Lea, Adams' Genera i. p. 300. 11. P. oli vaceu m, Lea. This species should follow No. 21. 16a. P. trivittatum, Lea.* Synonymy, Part 1st, No. 79. 17a. P. fastigiatum. Anthony. Synonymy, Part 1st, No. 44. 28. P. unciale, Haldeman. P. unciale, Hald., Synonymy, Part 1st, No. 67. P. bicostatum and rigidum, Anth., ibid. No. 28. P. sugillatum, Reeve, ibid. No. 68. G. oblita, Lea, Synonymy, Part 2, No. 126. 29. P. subulare, Lea. Ceriphasia subularis, Lea, Adams' Genera i. p. 297. 29a. P. intensum, Anthony. Melania intensa, Anthony, Reeve, Monog. sp. 371. Brot, List, p. 30. 33. P. an nuliferu m, Conrad. Melania annulifera, Conr., Midler, Synopsis, p. 44. Ceriphasia annulifera, Conr., Adams' Genera i. p. 297. Ceriphasia Ordiana, Lea, ibid. p. 297. 38. P. elevatum, Say. Elimia elevata, Lea, Adams' Genera i. p. 300. Ceriphasia elongata, Lea, ibid. p. 297, not Ceriph. elevata, Say, of Chenu, Man. i. f. 1961. 40. P. aratum, Lea. Ceriphasia exarata, Lea, Adams' Genera i. p. 297. 44. P. fasti giatum, Anthony. Should be No. 17a. 49. P. pyrene 1 lum, Conrad. Melania pyrenella, Conrad, Midler, Synopsis, p. 45. 51. P. regulare, Lea. Ceriphasia regidaris, Lea, Adams' Genera i. p. 297. 55. P. labiatum, Lea. 55a. P. pallidum, Lea.f 57. P. v e s t i t u m, Conrad. :f * Perhaps = Thnrntonii. f After a thorough examination of the specimens of labiatum and pallidum, I incline to the be- lief that they are distinct. J G. spinalis, Lea, may be identical with this species. [Jan. NATURAL SCIENCES OP PHILADELPHIA. 21 Melania vestita, Conrad, Mailer, Synopsis, p. 47. 57«. P. lugubre, Lea. Melania lugubris, Lea, Philos. Proc. iv. p. 166, August, 1845. Philos. Trans. x. p. 58, t. 9, f. 29. Obs. iv. p. 58. Binney, Check List, No. 164. Brot, List, p. 31. Goniobasis spurca, Lea, Synopsis, Part 2d, No. 177. Ceriphasia spurca, Lea, H. and A, Adams' Genera i. p. 297. 58a. P. pic turn, Lea. Melania picta, Lea, Philos. Proc. ii. p. 82, Oct., 1841. Philos. Trans, ix. p. 19. Obs. iv. p. 19. Wheatley, Cat. Shells, U. S. p. 26. Binney, Check List, No. 205. Reeve, Monog. Melania, sp. 290. Melania picturata, Reeve,* Errata to Monog. Melania. Brot, List, p. 38. 63a. P. Ocoeense, Lea. Goniobasis Ocoeensis, Lea, Synonymy, Part 2d, No. 181. 67. P. u n c i a 1 e, Haldeman. Synonymy, Part 1st, = No. 28. 68. P. sugi 11a turn, Reeve, Synonymy, Part 1st, = No. 28. 76. P. curvatum, Lea. Gyrotoma curvata, Say, ? Adams' Genera i. p. 305. 79. P. trivitt atum, Lea. Synonymy, Part 1st, = No. 16a. 83. P. opaca, Anthony. G. opaca, iostoma and nigrostoma, Anthony, Synonymy, Part 2d, No. 119. P. Tennesseense, Lea, Synonymy, Part 1st, No. 83. ANGITREMA, Haldeman. 1. A. geniculata, Haldeman. Lithasia genicula, Lea, Adams' Genera i. p. 308. 2. A. s a 1 e b r o s a, Conrad. Melania salebrosa, Conrad, Midler, Synopsis, p. 44. Lithasia salebrosa, Conrad, Adams' Genera i. p. 308. 5. A. J ay an a, Lea. , To Jayana, Lea, Brot, Mai. Blatt. ii. p. 115, July, 1860. lo robulina, Anthony, Chenu, Manuel de Conchyl. i. f. 1976. Adams' Ge- nera i. p. 299. 7. A. armi gera, Say. Io armigera, Say, Adams' Genera i. p. 299. 8. A. Du ttonian a, Lea. Io Duttoniana, Lea, Chenu, Man. de Conchyl. i. f. 1974. Adams' Genera i. p. 299. 9. A. stygia, Say. lo tuberculata, Lea, Adams' Genera i. p. 299. 11. A. lima, Conrad. Melania lima, Conr. Midler, Synopsis, p. 46. Megara lima, Conr., Adams' Genera i. p. 306. 12. A. verrucosa, Rafinesque. Potadoma depygis, Say, Chenu, Manuel de Conchyl. i. f. 1970. Lithasia semigranulosa, Deshayes, Adams' Genera i. p. 308. * As a Phurocera, the name of picta is not preoccupied. 1864.] 22 PROCEEDINGS OF THE ACADEMY OF LITHASIA, Haldeman. 1. L. fuliginosa, Lea. Leptoxis fuliginosa, Lea, Adams' Genera i. p. 307. 2. L. Florentiana, Lea. Io Florentiana, Lea, H. and A. Adams' Genera i. p. 299. 9. L. n u c 1 e o 1 a, Anthony. L. obliqua, Anthony, Synonymy, Part 1st, No. 14, 11. L. obovata, Say. Lithasia obovata, Say, Adams' Genera i. p. 308. Leptoxis Hildrethiana, Lea, Adams' Genera i. p. 307. 14. L. obliqua, Anthony. Synonymy, Part 1st, = L. nvcleola, Anthony, No. 9. STREPHOBASIS, Lea. 1. S. cur ta, Haldeman. Megara solida, Lea, Adams' Genera i. p. 306. 2. S. p umila, Lea. Megara pumila, Lea, Adams' Genera i. p. 306. 8. S. bit a en i at a, Conrad. Melania bitaniata, Conrad, Muller, Synopsis, p. 45. GONIOBASIS, Lea. 2. G. gr atios a, Lea. 2a. G. 1 a c h r y m a, Anthony. Botll = EDRYCJELON. 3. G. gibberosa, Lea. =EuRYCiELON. 4. G. n u b i 1 a, Lea. = El7RYCJELON. 6. G. H y d e i i, Conrad. Melania Hydeii, Conrad, Muller, Synopsis, p. 44. 8. G. c a e 1 a t u r a, Conrad. 8a. G. Stewardsoniana, Lea.* 8b. G. llavescens, Lea.f Goniobasis flavescens, Lea, Proc. Acad. Nat. Sciences, p. 271, 1862 — Journal Acad. Nat. Sol., v. pt. 3, p. 339, t. 38, f. 202, March, 1863. Obs. ix. p. 161. 10. G. cat en aria, Say. Elimia catenaria, Lea, Adams' Genera i. p. 300. 11. G. cat en o ides, Lea. Elimia catenoides, Lea, Adams' Genera i. p. 300. 14. G. Boykiniana, Lea. Elimia Boykiniana, Lea, Adams' Genera i. p. 300. Juga Troostiana, Lea, Chenu, Man. de Conchyl. i. f. 2017. 22. G. carinifera, Lamarck. Elimia bella, Conrad, Adams' Genera i. p. 300. *Differs from G. cxlatura in color, being dark green. It is also a more inflated species, with shorter spire. fNearly allied to cxlatura, but is narrower, more cylindical and lighter in color. [Jan NATURAL SCIENCES OF PHILADELPHIA. 28 22a. G. abbreviata, Anthony. Melania abbreviata, Anth., Bost. Proc, iii. p. 360, Dec, 1850. Binney, Check List, No. 433. Reeve, Monog. Melania, sp. 424. Melania elegantula, Anthony, Ann. N. Y. Lye, vi. p. 103, t. 3, f. 2, Mar., 1854. Binney, Check List, No. 96. Brot. List, p. 32. Reeve, Monog. Melania sp. 346. Melania coronilla, Anth., Ann. Lye, N. H., New York, vi. p. 126, t. 3, f. 27, Mar., 1854. Binney, Check List, No. 69. Brot. List, p. 32, Reeve, Monog. Mel., sp. 418. Melania chalybcea, Anth., Brot. List, p. 37. 22b. G. vesicula, Lea. Synonymy, Part. 2, No. 41. 25. G-. subs'tricta, Haldeman. Synonymy, Part 2=No. 31. G, obtusa, Lea. 28. G. carinocostata, Lea. Elimia carinocostata, Lea, Adams' Genera, i. p. 300. 28a. G. s t r e n u a, Lea. G. Leidyana, Lea. G. carinocostata, Lea, Synonymy, Part 2. 286. G. perstriata, Lea. Synonymy, Part 2, No. 73. 29. G. Lecontiana, Lea. Melasma Lecontiana, Lea, Adams' Genera i. p. 300. 30. G. c a dus, Lea. Synonymy, Part 2=G. obtusa, Lea, No. 31. 31. G. obtu sa, Lea. G. substricta, Haldeman, Synonymy, Part 2, No. 25. G. cadus, Lea, Synonymy, Part 2, No. 30. 34. G. C h r i s t y i, Lea, is a Synonym of No. 37. 37. G. interrupta, Haldeman. G. Christyi, Lea. G. instabilis, Lea, Synonymy, Part 2, No. 34. G. ornatella, Lea, is a Synonym, of No. 39. 39. G. form os a, Conrad. G. ornatella, Lea, Synonymy, Part 2, No. 37. 41. G. vesicula, Lea. See No. 22, b. 43. G. laqueta, Say. Melasma laqueata, Say, Adams' Genera i. p. 300. 47. G. gracilis, Lea. Potadoma gracilis, Lea, H. and A. Adams' Genera i. p. 299. 53. G. bland a, Lea. Melasma blancla, Lea, Adams' Genera i. p. 300. 54. G. nit ens, Lea. Melasma nitens, Lea, Adams' Genera i. p. 300. 55. G. mutata, Brot.* 59. G. C urreyana, Lea. Melasma Curreijana, Lea, Adams' Genera i. p. 300. *Mucb resembles G. dijjicilis, Lea, No. 81. 1865.] 24 PROCEEDINGS OF THE ACADEMY OF 61. G. D e s li a y e s i a n a, Lea. Melasma plicatul a, Lea, Adams' Genera i. p. 300. Melasma Deshayesiana, Lea, Adams' Genera i. p. 300. 69a. G. L i n d s 1 e y i,* Lea. Syn. of dis locata, Rav., Part 2, Synonymy, No. 69. 72. G. n a s s u 1 a, Conrad. Melania nassula, Conr., Miiller, Synopsis, p. 46. G. Edgariana, Lea, Synonymy, Fait 2, No. 77. Melasma Edgariana, Lea, Adams' Genera i. p. 300. 75. G. c o s t u 1 a t a, Lea. Melasma costulata, Lea, Adams' Genera i. p. 300. 77. G. Edgariana, Lea. Vide, No. 72. 78. G. c a 1 i g i n o s a, Lea. Elima caliginosa, Lea, Adams' Genera i. p. 300. 79. G. nodulosa, Lea. Elimia nodulosa, Lea, Adams' Genera, No. 300. 80. G. glauca, Anthony. = G. atkleta, Anthony, No. 86. 84. G. c a n c e 1 1 a t a, Say. Elimia cancellata, Say, Adams" Genera i. No. S4. 85. G. circincta, Lea. Juga circincta, Lea, Adams' Genera i. p. 294. 86. G. a t li 1 e t a, Anthony. G. glauca, Anthony, Synonymy, Part 2, No. 80. S8. G. stria tula, Lea. Juga striata, Lea, Adams' Genera i. p. 304. 91. G. crebicostata, Lea. Melasma crebricostata, Lea, Adams' Genera i. p. 300. 92. G. c o m m a, Conrad. Melania comma, Conr., Miiller, Synopsis, p. 45. Melasma comma, Conr., Adams' Genera i. p. 300. 93. G. acuta, Lea. Ceriphasia acuta, Lea, Adams' Genera i. p. 297. 94. G. subcylindracea, Lea. Potadoma subcijli)idracea, Lea, Adams' Genera i. p. 299. 96. G. concinna, Lea. Melasma concinna, Lea, Adams' Genera i. p. 300. 103. G. p lici f er a, Lea. Melania plicifera, Lea, Troschel, Archiv fur Naturgesch. ii. p. 227. Melasma plicifera, Adams' Genera i. p. 300. 104. G. s i 1 i c u 1 a, Gould. Juga silicula, Gould, Adams' Genera i. p. 304. 108. G. trochiformis, Conrad. Melania trochiformis, Conr., Miiller, Synopsis, p. 47. * The aperture is differently shaped from dislocata. The plicae are also more crowded, and decussated by one or two lines under the sutures. [Jan. NATURAL SCIENCES OP PHILADELPHIA. 25 Ilia. G. ex pa ns a, Lea.* 118. G. p 1 e b e i u s, Anthony. = G.sordida, Lea, No. 186. 119. G. op aca, Anthony. = Pleurocera opaca, Anthony, No. 83. 123. G. m o d e s t a, Lea.f 124. G. pagodiformis, Anthony. = G. acutocarinata, Lea, No. 127- 125. G. Gerhard tii, Lea.t 126. G. o h 1 i t a, Lea. =Pleurocera unciale, Hald., Synonymy, Part 1, No. 28. 127. G. acutocarinata, Lea. G. pagodiformis, Anthony. G. tondosa, Anth., No. 124. Eiimia acutocarinata, Lea, Adams' Genera i. p. 300. 129. G. C a t aw b a e a, Haldeman. Goniobasis Catawbcea, Hald., Amer. Jour. Conch, vol. 1, No. 1, Feb. 25, 1865. 132. G. symmetrica, Haldeman. Ceripha'sia symmetrica, Hald. Adams' Genera i. p. 297. 138. G. cong e st a, Conrad. Melania congesta, Conr., Midler, Synopsis, p. 43. 139. G. aur iculae formis, Lea. Megara auriculceformis, Lea, Adams' Genera i. p. 306. 140. G. Nic klin i ana, Lea. Leptoxis Nickliniana, Lea, Adams' Genera i. p. 307. 143. G. ebenum, Lea.§ Nitocris eberia, Lea, Adams' Genera i. p. 308. Melania brunnea, Anth.= G. sordida, Lea, No. 186. 148. G. graminea, Haldeman. Goniobasis graminea, Hald., American Journ. Conch, i. No.l. Feb. 25, 1865. 150. G. Vanuxemii, Lea. Changed to G. Prestoniana, Proc. Acad., 1864, p. 3, Vanuxemii being preoccupied. = G. simplex, Say, No. 157. 153. G. a b r u p t a, Lea. Leptoxis abrupta, Lea, Adams' Genera i. p. 307. 154. G. d e p y g i s, Say. Potadoma depygis, Say, Adams' Genera i. p. 298. 155. G. li ve s c e n s, Menke. Potadoma Niagarensis, Lea, Adams' Genera i. p. 299. 157. G. simplex, Say. G. subsolida, Lea, No. 186, cxcl. synonyms. *Very closely allied to, or perhaps=(?. Whitei, No. 111. tPerhaps_P/ewrocera lugubris, Lea. JThis is probably the same as G. semigradata, No. 27. (5Mr. Lea agrees with me in considering this species distinct from iostoma, Anth.; and also in making brunneu a synonym oSsordida instead of ebenum. 1865.] ^6 PROCEEDINGS OF THE ACADEMY OP G. Vanuxemii, Lea, No. 150. Pachycheilus simplex, Say, Adams' Genera i. p. 298. Potadoma Warderiana, Lea, Adams' Genera i. p. 299 , Chenu, Manuel, i. f. 1972. 158. G. Potosiensis, Lea. Elimia Potosiensis, Lea, H. and A. Adams' Genera i. p. 300. 160a. G. virens, Anthony.* Syn. of G. Sqffbrdi. Synonymy, Part 2d, No. 160. 167. G. cinerea, Lea.f 170. G. translucens, Anthony. Goniobasis translucens, Anthony, Am. Journ. Conch, i., Feb. 25, 1865. 171. G. ovoid e a, Lea. Potadoma ovoideus, Lea, Adams' Genera i. p. 299. 173. G. quadricincta, Lea. Goniobasis quadricincta, Lea, Proc. Acad. Nat. Sci., Apr. 1864, p. 112. 177. G. s pur c a, Lea. = Pleurocera, No. 57a. 181. G. Ocoeensis, Lea. Potadoma Ocoeensis, Lea, Adams' Genera i. p. 299. = Pleurocera, No. 63a. 184. G. Estahrookii, Lea. = G. dubiosa. 186. G. subsolida, Lea~ = G. simplex, Say, No. 157. Potadoma subsolida, Lea, H. and A. Adams' Genera i. p. 299. 186a. G. sordida, Lea. Potadoma sordida, Lea, H. and A. Adams' Genera i. p. 299. G. plebeia, Anth., Synonymy, Part 2d, No. 118. G. brunnea, Anth., Synonymy, Part 2d, No. 143. 187. G. clavaeformis, Lea. Melasma clavaeformis, Lea, H. and A. Adams' Genera i. p. 300. 191. G. adust a, Anthony. G. Cumberlandicnsis, Lea, Synonymy, Part 2d, No. 189. G. funebralis, Anthony, Synonymy, Part 2d, No. 190. 193. G. dubiosa, Lea, G. Estabroohii, Lea, Synonymy, Part 2d, No. 184. 194. G. laevigata, Lea. Potadoma laevigata, Lea, H. and A. Adams' Genera i. p. 299. 195. G. interlinear a, Anthony. Goniobasis interlineata, Anthony, Am. Jour. Conch, vol. i., Feb. 25, 1865. 196. G. O hi ens is, Lea.f 197. G. b r e v i s p i r a, Anthony. Melasma brevispira, Anth. , Adams' Genera i. p. 300. * Appears to be distinct from G. Saffnrdi. The shell is less solid, the aperature is not exactly of the same form, and the c olor is lighter and more brilliant. fMost likely the locality given for this species is incorrect. It is probably identical with pulchella, Anthony. X Probably = G. semicarinata, Say. No. 193. [Jan. NATURAL SCIENCES OF PHILADELPHIA. 27 198. G. semicarinata, Say. Juga exilis, Hald., Adams' Genera i. p. 304. Ceriphasia Kirtlandiana, Adams' Genera i. p. 297. Potadoma inornatus, Adams' Genera i. p. 299. 199. G. Haldemani, Tryon. Goniobasis Haldemani, Tryon, Am. Journ. Conch, i., Feb. 25, 1865. 203. G. Alexandrensis, Lea.* Ceriphasia Alexandrensis, Lea, Adams' Genera i. p. 297. 204. G. Haleiana, Lea. Ceriphasia Haleiana, Lea, Adams' Genera i. p. 297. 208. G. p r o x i m a, Say. Juga proximo, Say, Adams' Genera i. p. 304. 208a. G. rufescens, Lea.f Potadoma rufescens, Lea, Adams' Genera i. p. 299. 209. G. Virginica, Gmel. Buccinum Virginica, Gmel. Syst. Nat. p. 3505. Schroter, Einleit. i. p. 414, 1783. Martini, Berlin Mag. if. p. 348, t. 10, f. 48. Schreibers, Ein- leit. Conchyl. t. 113, f. 7. Melania Virginica, Say, Villa., Cat. Syst. p. 36, 1841. Io Virginica, Say, Morch, Yoldi Cat. p. 56. Ceriphasia Virginica, Gmel., Adams' Genera i. p. 297. Juga Virginica, Say, Adams' Genera i. p. 304. Juga multilineata, Say, Adams' Genera i. p. 304. 210. G. Sulcosa, Lea. Ceriphasia sidcosa, Lea, Adams' Genera i. p. 297. 211. G. Buddii, Lea. Juga Buddii, Say, H. and A. Adams' Genera i. p. 304. 212. G. Troostiana, Lea. Melania Troostiana, Lea, Troschel, Archiv fur Naturgesch. ii. p. 227. Juga Troostiana, Lea, Adams' Genera i. p. 304. ■ J. Heavy, pupreform or cylindrical species. 217. G. cylindracea, Conrad. Melania cylindracea, Con., New Fresh- Water Shells, p. 55, t. 8, f. 10, 1834. Midler, Synopsis, p. 47, 1836. Binney, Check List, No. 84. Melania cylindrica, Con., Wheatley, Cat. Shells, U. S., p. 25. Reeve, Mo- nog. Melania, sp. 311. Brot, List, p. 32. Melania oppugnata, Lea, Philos. Trans, x. p. 300, t. 30, f. 9. Observations, v. p. 56. Binney, Check List, No. 190. 218. G. p u p o i d e a, Anthony. J Melania pupoidea, Anthony, Ann. Lye. Nat. Hist. N. Y., vi. p. 104, t. 3, f. 3, April, 1854. Brot, List, p. 33. Binney, Check List, No. 224. Reeve, Monog. Melania, sp. 249. Melania propinqua, Lea, Proc. Acad. Nat. Sci., p. 119, 1861. Goniobasis propinqua, Lea, Journ. Acad, Nat. Sci., v, pt. 3, p. 234, t. 34, f. 29, March, 1863. Obs. ix. p. 56. * May be a Pleurocera. tl'bis is a longer and narrower species than G. proximo,, the color is also darker. X Without the large series of specimens before me, I should have acquiesced in the institution of propinqua as a distinct species ; but I find every grade of form between the two. The shorter forms approach closely to olivula, Con., with which they have been confounded. They are dis- tinguished by difference in color, and principally of texture, olicula being much heavier. 1865.] 28 PROCEEDINGS OF THE ACADEMY OP 219. Gk lit a, Lea.* Melania lita, Lea, Proc. Acad. Nat. Sciences, 18G1, p. 121. Goniobasis lita, Lea, Journ. Acad. Nat. Sci., v. pt. 3, p. 239, t. 34, f. 40, March, 1863. Obs. ix. p. 61. 220. G. fall ax, Lea. Melania fallax , Lea, Proc. Acad. Nat. Sciences, 1861, p. 120. Goniobasis fallax, Lea, Journ. Acad. Nat. Sci. v. pt. 3, p. 231, t. 34, f. 24, March* 1863. Obs. ix. p. 53. 221. G. inosculata, Lea.f Goniobasis inosculata, Lea, Proc. Acad Nat. Sci. p. 263, 1862. Journ. Acad. Nat. Sci. v. pt. 3, p. 296, t. 37, f. 126, March, 1863. Obs. ix. p. 118. 222. G. Alabamensis, Lea. Melania Alabamensis, Lea, Proc. Acad. Nat. Sci. 1861, p. 121. Goniobasis Alabamensis, Lea, Jour. Acad. Nat. Sci. v. pt. 3, p. 232, t. 34, f. 26, March, 1863. Obs. ix. p. 54. 223. G. rara, Lea. Melania rara, Lea, Proc. Acad. Nat. Sci. p. 121, 1861. Goniobasis rara, Lea, Journ. Acad. Nat. Sci. v. pt. 3, p. 220, t. 34, f. 3, March, 1863. Obs. ix. p. 42. 224. G. punicea, Lea. J Melania punicea, Lea, Proc. Acad. Nat. Sci., p. 119, 1861. Goniobasis punicea, Lea, Journ. Acad. Nat. Sci. v. pt. 3. p. 232, t. 34, f. 27, March, 1863. Obs. ix. p. 54. 225. G. pud i ca, Lea. Melania pudica, Lea, Proc. Acad. Nat. Sci. v. pt. 3, p. 222, t. 34, f. 7, Mar. 1863. Obs. ix. 226. G. fabalis, Lea. Goniobasis fabalis, Lea, Proc. Acad. Nat. Sci. p. 266, 1862. Journ. Acad. Nat. Sci. v. pt. 3, p. 311, t. 37, f. 154, March, 1863. Obs. ix. p. 133. 227. G. Shelbyensis, Lea § Melania Shelbyensis, Lea, Proc. Acad. Nat. Sci. p. 121, 1861. Goniobasis Shelbyensis, Lea, Journ. Acad. Nat. Sci. v. pt. 3, p. 228, t. 34, f. 18, March, 1S63. Obs. ix. p. 50. 228. G. fume a, Lea. Melania fumea, Lea, Proc. Acad. Nat. Sci. 1861, p. 123. Goniobasis fumea, Lea, Journ. Acad. Nat. Sci. v. pt. 3, p. 222, t, 34, f. 6, March, 1863. Obs. ix. p. 44. 229. G. aequ a, Lea. Melania aqua, Lea, Proc Acad. Nat. Sci. 1861, p. 122. Goniobasis aqua, Lea, Journ. Acad. Nat. Sci. v. pt. 3, p. 240, t. 34, f. 41, March, 1863. Obs. ix. p. 62. 230. G. s o 1 i d u 1 a, Lea. Melania solidula, Lea, Proc. Acad. Nat. Sci. 1861, p. 121. Goniobasis solidula, Lea, Journ, Acad. Nat. Sci. v. pt. 3, p. 230, t. 34, f. 23. Obs. ix. p. 52. *I doubt whether this is distinct from G. Haysiana. In all the specimens I have examined, the aperture is white within, instead of purple as described by Mr. Lea, •f The whorls are more convex and brighter in color than G. fallax. This species is constantly ornamented by four dark bands. 1 Very closely allied to pudica, if not identical with that species. j> Differs from pudica in the form of the aperture, the whorls are also flatter. . [Jan. NATURAL SCIENCES OP PHILADELPHIA. 29 231. G. olivula, Conrad. Melania olivula, Con., Am. Journ. Science, 1st Series, xxv. p. 342, t. 1, f. 13, Jan., 1834. Miiller, Synopsis, p. 42, 1836. Wheatley, Cat. Shells, U. S., 26. DeKay, Moll. New York, p. 98. Jay, Cat. Shells, 4th Edit. p. 274. Reeve, Monog. Melania, sp. 455.* Bianey, Check List, No. 188. Brot, List, p. 33. Hanley, Conch. Miscellany, t. 1, f. 2. Megara olivula, Con., Chenu, Manuel, i. f. 2027. Adams' Genera i. p. 306. Melania olivata, Con., Jay, Cat. 3d Edit. p. 45. Catlow, Conch. Nomenc. p. 188. Melania propria, Lea, Proc. Acad. Nat. Sciences, 1861, p. 123. f Goniobasis lepida, Lea, Journ. Acad. Nat. Sciences, v. pt. 3, p. 227, t. 34, f. 17, March, 1863. Obs. ix. p. 49. 232. G. f a s c i n a n s, Lea. Melania fascinans, Lea, Proc. Acad. Nat. Sciences, p. 119, 1861. Goniobasis fascinans, Lea, Journ. Acad. Nat. Sci. v. pt. 3, p. 229, t. 34. f. 20, March, 1863. Obs. ix. p. 51. 233. G. Showalterii, Lea. Melania Showalterii, Lea, Proc. Acad. Nat. Sciences, 1861, p. 120. Goniobasis Showalterii, Lea, Jour. Acad. Nat. Sci. v. pt. 3, p. 220, t. 34, f. 4. Obs. ix. p. 42. 234. G. clausa, Lea. Melania clausa, Lea, Proc. Acad. Nat. Sciences, 1861, p. 120. Goniobasis clausa, Lea, Jour. Acad. Nat. Sci. v. pt. 3, p. 231, t. 34, f. 25, March, 1863. Obs. ix. p. 53. 235. G. c rep era, Lea. Melania crepera, Lea, Proc. Acad. Nat. Sci. 1861, p. 123. Goniobasis crepera, Lea, Journ. Acad. Nat. Sci. v. pt. 3, p. 240, t. 34, f. 42, March, 1863. Obs. ix. p. 62. 236. G. abscida, Anthony. Melania abscida, Anthony, Proc. Acad. Nat. Sciences, 1860, p. 56. Binney, Check List, No. 435. Brot, List, p. 32. Reeve, Monog. Melania, sp. 395. 237. G. Vanuxemiana, Lea. Melania Vanuxemiana, Lea, Proc. Philos. Soc. ii. p. 242, Dec, 1842. Philos. Trans, ix. p. 25. Obs. ix. p. 25. Reeve, Monog. Melania, sp. 453. Brot, List, p. 33.. Melania Vanuxemensis, Lea, Wheatlev, Cat. Shells, U. S., p. 27. Binney, Check List, No. 283. Megara Vanuxemiana, Lea, Adams' Genera i. p. 306. 238. G. Coosaensis, Lea.J Melania Coosaensis, Lea, Proc. Acad. Nat. Sci. 1861, p. 118. Goniobasis Coosaensis, Lea, Journ. Acad. Nat. Sciences, v. pt. 3, p. 234, t. 34, f. 30. March, 1863. Obs. ix. p. 56. 238. G. rubicund a, Lea. Melania rubicunda, Lea, Proc. Acad. Nat. Sciences, 1861, p. 118. Goniobasis rubicunda, Lea, Journ. Acad. Nat. Sci., v. pt. 3, p. 235 t. 34, f. 32, March, 1863. Obs. ix. p. 57. 240. G. H a y s i a n a, Lea. Melania Haysiana, Lea, Philos. Proc. ii. p. 242, Dec, 1842. Philos. Trans. # Reeve figures for this shell also sp. 309, but the figure does not represent the species, ■f Preoccupied. Showalterii and fascinans are also probably synonyms of olivula. X Differs from G. Haysiana in the form of the aperture. 1865.] 30 PROCEEDINGS OF THE ACADEMY OP ix. p. 25. Obs. iv. p. 25. Wheatley, Cat. Shells, U. S., p. 25. Jay, Cat. Shells, 4th Edit. p. 273. Binney, Check List, No. 137. Brot, List, p. 32. Brot, Mai. Blatt. ii. p. 108, July, I860.* Reeve, Monog. Melania, sp. 310. Hanley, Conch. Miscel. Melania, t. 1, f. 6. Megara Haysiana, Lea, Chenu, Manuel, i. f. 1981. Adams' Genera i. p. 306. 241. G. arctata, Lea. Melania arctata, Lea, Philos. Proc. iv. p. 166. Philos. Trans, x. p. 64, t. 9. f. 46. Obs. iv. p. 64. Binney, Check List, No. 20. Brot, List, p. 32. Megara arctata, Lea, Chenu, Manuel, i. f. 2024. Adams' Genera i. f. 306. 242. G. a m p 1 a, Anthony. Melania ampla, Anthony, Ann. N. Y. Lyceum, vi. p. 93, t. 2, f. 12, 1854. Binney, Check List, No. 13. Brot, List, p. 39. Reeve, Monog. Mela- nia, sp. 312. Melania Hartmaniana, Lea, Proc. Acad. Nat. Sciences, 1861. Goniobasis Hartmanii, Lea, Journ. Acad. Nat. Sci. v. pt. 3, p. 218, t. 34, f. 1, 1863. Obs. ix. p. 40. 243. G. m e 1 1 e a, Lea. Melania mellea, Lea, Proc. Acad. Nat. Sciences, 1861, p. 120. Goniobasis mellea, Lea, Journ. Acad. Nat. Sci. v. pt. 3, p. 224, t. 34, f. 10. 1863. Obs. ix. p. 46. 244. G. am b u s t a, Anthony. Melania ambusta, Anthony, Ann. Lye. Nat. Hist. vi. p. 94, t. 2, f. 13, 1854. Binney, Check List, No. 12. Brot, List, p. 39. Reeve, Monog. Mela- nia, sp. 352. 245. G. lae ta, Jay. Melania laeta, Jay, Cat. Shells, 3d Edit. p. 122, t. 7, f. 11, 1839. Jay, Cat. Shells, 4th Edit. p. 274. Wheatley, Cat. Shells, U. S., p. 26. Binney, Check List, No. 156. Catlow, Conch. Nomenc. p. 187. Brot, List, p. 32. Melania robusta, Lea, Philos. Proc. ii. p. 83, October, 1841. Philos. Trans, ix. p. 19. Obs. iv. p. 19. Wheatley, Cat. Shells, U. S., p. 26. Bin- ney, Check List, No. 231. Melatoma Buddii, Lea,f Reeve, Monog. Melatoma, sp. 3. Melania tceniolata,% Anthony, Proc. Acad. Nat. Sciences, 1860, p. 59. Bin- ney, Check List, No. 263. Brot, List, p. 31. Reeve, Monog. Melania, sp. 392. 246. G. h a r p a, Lea. Melania harpa, Lea, Philos. Proc. iv. p. 166, August, 1845. Philos. Trans. x. p. 64, t. 9, f. 45. Obs. iv. p. 64. Binney, Check List, No. 135. Brot, List, p. 32. Reeve, Monog. Melania, sp. 313, 314. Megara harpa, Lea, Adams' Genera i. p. 306. Melania textilosa, Anthony, § Ann. Lye. Nat. Hist. vi. p. 101, t. 2, f. 20, 1854. Binney, Check List, No. 270. Brot, List, p. 40. Reeve, Monog. Melania, sp. 391. 247. G. oliva, Lea.|| * Dr. Brot considers arctata, robusta, brevis and basalts synonyms. t It is curious that Mr. Reeve has figured and described this shell for the Schizostoma {Melalorrui, Huddii, Lea. t Half grown shell. It presents a very different appearance from the adult. | Half grown shell. D This shell is narrower than G. laeta, resembling harpa in form ; but the aperture is wider ami more rounded below. It is very closely allied to G. excavata, — which is a smooth species, however [Jan. NATURAL SCIENCES OF PHILADELPHIA. 31 Melania oliva, Lea, Philos. Proc. ii. p. 242, 1842. Philos. Trans., ix. p. 27. Obs. iv. p. 127. Wheatley, Cat. Shells U. S., p. 26. Binney, Check List, No. 187. Brot, List, p. 33. Megara oliva, Lea, Adams' Genera i. p. 306. 248. G. proteus, Lea. Melania proteus, Lea, Philos. Proc. iv. p. 166, 1845. Philos. Trans., x. p. 57, t. 9, f. 28. Obs. iv. p. 57. Binney, Check List, No. 219. Brot, List, p. 33. Juga proteus, Lea, Adams' Genera i. p. 304. 249. G. g r i s e a, Anthony. Melania grisea, Anthony, Proc. Acad. Nat. Sciences, 1S60, p. 61. Reeve, Monog. Melania, sp. 390. Brot, List, p. 32. 250. G. cul ta, Lea. Melania culla, Lea, Proc. Acad. Nat. Sciences, p. 121, 1861. Goniobasis culla, Lea, Jour. Acad. Nat. Sci., v. p. 13, p. 237, t. 34, f. 36. Mar., 1863. Obs. ix. p. 59. Melania suavis,* Lea, Proc. Acad. Nat. Sci., p. 169, 1861. Goniobasis suavis, Lea, Jour. Acad. Nat. Sci., v. pt. 3, p. 228 t. 34, f. 19. Mar., 1863. Obs. ix. p. 50. 251. G. 1 u t e o 1 a, Lea. Melania luteola, Lea, Proc. Acad. Nat. Sci., p. 119, 1861. Goniobasis luteola, Lea, Jour. Acad. Nat. Sci., v. pt. 3, p. 230, t. 34, f. 22, Mar., 1863. Obs. ix. p. 52. Melania straminea,\ Lea, Proc. Acad. Nat. Sci., 1861, p. 121. Goniobasis straminea, Lea, Jour. Acad. Nat. Sci., v. pt. 3, p. 227, t. 34, f. 16, Mar., 1863. Obs. ix. p. 49. 252. G. gravida, Anthony. Melania gravida, Anth., Proc. Acad. Nat. Sci. p. 59, Feb., 1860. Reeve, Monog. Melania. Brot, List. 253. G. ger man a, Anthony. Melania germana, Anth., Proc. Acad. Nat. Sci. p. 61, Feb., 1S60. Binney, Check List, No. 120. Brot, List, p. 40. Iteeve, Monog. Melania, sp. 383. 254. G. v a r i a t a, Lea. Melania variata, Lea, Proc. Acad. Nat. Sci. p. 119, 1861. Goniobasis variata, Lea, Jour. Acad. Nat. Sci. v. pt. 3, p. 224, t. 34, 1". 11, March, 1863. Obs. ix. p. 46. 255. G. ova lis, Lea. Melania ovalis, Lea, Philos. Proc. ii. p. 242, Dec. 1842. Philos. Trans, ix, p. 25. Obs. ix. p. 25. Wheatley, Cat. Shells U. S. p. 26. Binney, Check List, No. 192. Reeve, Monog. Melania, sp. 448 and sp. 309. J Megara ovalis, Lea, Adams' Genera i. p. 306. Melania copiosa, Lea, Proc. Acad. Nat. Sci. p. 122, 1861. Goniobasis copiosa, Lea, Jour. Acad. Nat. Sci. v. pt. 3, p. 239, t. 34, f. 39. Obs. ix. p. 61. Melania orbicula, Lea, Proc. Acad. Nat. Sci. p. 118, 1861. Goniobasis orbicula, Lea, Jour. Acad. Nat. Sci. v. pt. 3, p, 238, t. 34, f. 37, March, 1863. Obs. ix. p. 60. 256. G. vi rgulata, Lea. Melania virgulata,\ Lea, Proc. Acad. Nat. Sci. p. 119, 1861. 1864.] * Young shell. •fYonng shell. \ Figured as olivula, Conr, but name corrected in Errata. 32 PROCEEDINGS OF THE ACADEMY OF Goniobasis virgulata, Lea, Jour. Acad. Nat. Sci. v. pt. 3, p. 223, t. 34, f. 9, March, 1863. Obs. ix. p. 45. Melania glandaria,* Lea, Proc. Acad. Nat. Sci. p. 120, 1861. Goniobasis glandaria, Lea, Jour. Acad. Nat. Sci. v. pt. 3, p. 226, t. 34, f. 14, March, 1863. Obs. ix. p. 48. 257. G. c 1 a r a, Anthony. Melania clara, Anth., Ann. N. Y. Lye. vi. p. 119, t. 3, f. 19, March, 1854. Binney, Check List, No. 55. Brot, List, p. 32. 258. G. in flat a, Haldeman.f Melania inflata, Hald., Cover of No. 3, Monog. Limniades, March, 1841. Binney, Check List, No. 146. Brot, List, p. 40. Reeve, Monog. Melania, sp. 410. 259. GL f u sif o r m is, Lea. % Melania fusiformis, Lea, Philos. Proc. ii. p. 12, Feb., 1841. Philos. Trans., viii. p. 167, t. 5, f. 9. Obs. iii. p. 5. DeKay, Moll. N. Y., p. 93. Troost. Cat. Shells Tenn. Wheatley, Cat. Shells U. S., p. 25. Binney, Check List, No. 117. Catlow, Conch. Nomenc, p. 186. Brot, List, p. 40. 260. G. bellula, Lea. Melania bellula, Lea, Proc. Acad. Nat. Sci., p. 122, 1861. Goniobasis belhda, Lea, Jour. Acad. Nat. Sci., v. pt. 3, p. 237, t. 34, f. 35, Mar., 1863. Obs. ix. p. 59. 261. Gr. calculoides, Lea. Mdania calculoides, Lea, Proc. Acad. Nat. Sci., p. 118, 1861. Goniobasis calculoides, Lea, Jour. Acad. Nat. Sci. v. pt. 3, p. 238, t. 34, f. 38, Mar., 1863. Obs. ix. p. 60. 262. Gr. has a lis, Lea,§ Melania basalts, Lea, Philos. Proc. iv. p. 166. Philos. Trans., x. p. 50, t. 9, f. 33. Obs. iv. p. 59. Binney, Check List, No. 28. Brot, List, p. 32. Reeve, Monog. Melania, sp. 471. Anculotis basalis, Lea, Reeve, Monog. Anculotus, t. 5. f. 40. Megara basalis, Lea, Adams' Genera i. p. 306. 263. G. Lewisii, Lea. Melania Lewisii, Lea, Proc. Acad. Nat. Sci. p. 118, 1S61. Goniobasis Lewisii, Lea, Jour. Acad. Nat. Sci. v. pt. 3, p. 243, t. 35, f. 46, Mar., 1863. Obs. ix. p. 65. 264. G. ellipsoides, Lea. Melania gracilior, Lea, || Proc. Acad. Nat. Sci. 1861, p. 118. Goniobasis ellipsoides, Lea, Jour. Acad. Nat. Sci. v. pt. 3, p. 234, t. 34, f. 31, Mar., 1863. Obs. ix. p. 56. 265. G. elliptic a, Lea. Melania elliptica, Lea, Proc. Acad. Nat. Sci. p. 118, 1861. Goniobasis elliptica, Lea, Jour. Acad. Nat. Sci. v. pt. 3, p. 225, t. 34, f. 13, Mar., 1863. Obs. ix. p. 47. 266. G. bull u la, Lea. Melania bullula, Lea, Proc. Acad. Nat. Sci. p. 121, 1861. * This is the young, and glandaria the adult shell of the same species. f Differs from G. virgulata by its obtusely angled whorls and somewhat diamond-shaped aper- ture. JMuch like G. ambusta when young, but more inflated, and the aperture more obtusely rounded below. 2 Resembles glandaria, but is thinnor. the outer lip is more expanded, and the aperture rather larger. It is closely allied also to fusiformis, Lea. || Preoccupied. [Jan. NATURAL SCIENCES OF PHILADELPHIA. 33 Goniobasis bullala, Lea, Jour. Acad. Nat. Sci. v. pt. 3, p. 221, Mar., 1863. Obs. ix. p. 43, t. 34, f. 5. 267. G. exoavata, Anthony.* Melania excavata, Anthony, Ann. Lye. N. Y., vi. p. 99, t. 2, f. 18, Mar., 1854. Binney, Check List, No. 102. Brot, List, p. 32. Reeve, Monog. Melania, sp. 385. 268. G. purpurea, Lea. Melania purpurea, Lea, Proc. Acad. Nat. Sci. p. 120. Goniobasis purpurea, Lea, Jour. Acad. Nat. Sci. v. pt. 3, p. 225, t. 34, f. 12, Mar., 1863. Obs. ix. p. 47. 269. G. quadrivittata, Lea. Melania quadrivittata, Lea, Proc. Acad. Nat. Sci. 1861, p. 119. Goniobasis quadrivittata, Lea. Jour. Acad. Nat. Sci. v. pt. 3, p. 226, Mar., 1863. Obs. ix. p. 48. 270. G. propria, Lea. Melania propria, Lea, Proc. Acad. Nat. Sci., p. 118, 1861. Goniobasis propria, Lea, Jour. Acad. Nat. Sci., v. pt. 3, p. 229, t. 34, f. 21, Mar., 1863. Obs. ix. p. 52. 271. G. n eg at a, Lea. Goniobasis negata, Lea, Proc. Acad. Nat. Sci., p. 271, 1862. Jour. Acad. Nat. Sci., v. pt. 3, p. 337, t. 38, f. 200, Mar. 1863. Obs. ix. p. 159. 272. G. i m p r e s s a, Lea. Melania impressa, Lea, Philos. Proc. ii. p. 83, Oct. 1841. Philos. Trans , ix. p. 19. Obs. iv. p. 19. Wheatley, Cat. Shells U. S., p. 25. Jay, Cat. Shells, p. 274. Binney, Check List, No. 143. Brot, List, p. 32. Reeve, Monog. Melania, sp. 316, 349. Hanley, Coach. Miscel. Melania, t. 8, f. 69. Megara impressa, Lea, Chenu, Manuel i. f. 2023, Adams' Genera i. p. 306. Melania crebristriala, Lea,f Philos. Proc. iv. p. 166. Philos. Traus., x. p. 65, t. 9, f. 47. Obs. iv p. 65. Binney, Check List, No. 75. Catlow, Conch. Nomenc, p. 186. Brot, List, p. 32. Megara crebristriata, Lea, Adams' Genera i. p. 306. 273. G. pergrata, Lea. J Melania pergrata, Lea, Proc. Acad. Nat. Sci., p. 122, 1861. Goniobasis pergrata, Lea, Jour. Acad. Nat. Sci. v. pt. 3, p. 243, Mar., 1863. Obs. ix. p. 65. 274. G. c a p i 1 1 a r i s, Lea. Melania capillaris, Lea, Proc. Acad. Nat. Sci., p. 122, 1861. Goniobasis capillaris, Lea, Jour. Acad. Nat. Sci. v. pt. 3, p. 236, t. 34 f. 34, Mar., 1863. Obs. ix. p. 58. EURYC^ELON, Lea. Eurycxlon, Lea, Proc. Acad. Nat. Sci., p. 3, Jan., 1864. / 1. E. umbonata, Lea. Goniobasis umbonata, Lea, Proc. Acad. Nat. Sci., p. 3, 1864. 2. E. M i d a s, Lea. Melania Midas, Lea, Proc. Acad. Nat. Sci., p. 119, 1861. Goniobasis Midas, Lea, Jour. Acad. Nat. Sci., v. pt. 3, p. 233, t. 34 f 28 Mar., 1863. Obs. ix. p. 55. 3. E. g r a t i os a, Lea. Goniobasis gratiosa, Lea, Synonymy, Part 2, No. 2. *Mr. AnthoDy'a type specimen exhibits unmistakable evidence of diseased growth. fThe difference iu the number of striae pointed out by Mr. Lea, is not a good distinctive charac- ter; they vary much in number on undoubted specimens of impressa. G. crebristriata ia not full grown. JI fear this is only a variety of impressa. 1865.] 3 34 PROCEEDINGS OF THE ACADEMY OF 3a. E. lachryma, Anthony. Goniobasis lachryma, Anthony, Syn., Part 2, No. 2a. 4. E. gibberosa, Lea. Goniobasis gibberosa, Lea, Syn., Part 2, No. 3. 5. E. n u b i 1 a, Lea. Goniobasis nubila, Lea, Syn., Part 2, No. 4. 6. E. A n t h o n y i, Budd. Anculosa Anthonyi, Budd., Syn., Part 3, No. 1. 7. E. crass a, Haldeman. Anculosa crassa, Hald., Syn., Part 3, No. 15. Leptoxis crassa, Hald., Adams' Genera i. p. 307. Anculosa pisum* Hald., Syn., Part 3, No. 19. Leptoxis pisum, Hald., Adams' Genera i. p. 307. 8. E. turbinata, Lea. Anculosa turbinata. Lea, Syn., Part 3, No. 33. MESESCHIZA, Lea. Meseschiza, Lea, Proc. Acad. Nat. Sci., p. 2, Jan., 1864. 1. M.Grosvenorii, Lea. Meseschiza Grosvenorii, Lea, Proc. Acad. Nat. Sci., p. 2, Jan. 18G4. SCHJZOSTOMA, Lea. 3. S.ovoideu m, ShutOeworth. Gyrotoma ovoidea, Shutt., Adams' Genera i. p. 305. 4. S. e xci s u m, Lea. Gyrotoma excisa, Lea, Adams' Genera i. p. 305. 7. S. laciniatum, Lea. Gyrotoma laciniala, Lea, Adams' Genera i. p. 305. 10. S. cy lindraceum, Mighels. Gyrotoma cylindracea, Migh., Adams' Genera i. p. 305. 12. S. cu r turn, Mighels. Gyrotoma curta, Migh., Adams' Genera i. p. 305. 15. S. p ag o d a, Lea. Gyrotoma pagoda, Lea, Adams' Genera i. p. 305. 16. S p y r a m i d a t n m, Shuttleworth. Gyrotoma pyramidaium, Shutt., Adams' Genera i. p. 305. 20. S. babylonicum, Lea. Gyrotoma babylonicum, Lea, Adams' Genera i. p. 305. Gyrotoma funiculi ta, Lea, Adams' Genera i. p. 305. 23. S.constrictu no, Lea. Gyrotoma constricta, Lea, Adams' Genera i. p. 305. .26. S. incisum, Lea. Gyrotoma incisa, Lea, Adams' Genera i. p. 305. ANCULOSA. Say. 1. A. Anthonyi, Budd. — Eurycxlon. 2. A. p lie at a, Conrad. Aneulotus plicatus, Conrad, Miiller, Synopsis, p. 40, 1836. Leptoxis pltcata, Conrad, Adams' Genera i. p. 307. 5. A. 1 i 1 1 o r i n a, Haldeman. Melania pdula, Lea, Adams' Gemra i. p. 307. *Toung shell. [Jan. NATURAL SCIENCES OP PHILADELPHIA. 35 6. A. c o s t a t a, Anthony. Niloais coslata, Lea, H. and A. Adams' Genera i. p. 308. Nitocris occidcntalis, Lea, Adams' Geuera i. p. 308. 7. A. rubiginosa, Lea. Anculosa rubiginosa, Lea, Brot, Mai. Blatt, ii. p. Ill, July, 1840. Leptoxis rubiginosa, Lea, Adams' Genera i. p. 307. Leptoxis Griffithiana, Lea, Adams' Genera i. p. 307. 8. A. c a r i n a t a, Brug.* A. dissimilis, Say, Synopsis, Part 3. Bulirnus carinatus, Brug., Ency. Meth., vers. i. p. 301, 1792. Nitocris dissimilis, Say, Adams' Genera i. p. 308. Leptoxis dissimilis, Say, Chenu, Manuel, i. f. 2049 — 54. —Lister t. Ill, f. 5 and t. 112, f. 6. Petiver, Gazophjl, t. 104, f. 67. Nitocris carinala, Lea, Adams' Genera i. p. 308. Leptoxis variabilis, Lea, Adams' Genera i. p. 307. Anculotus nigrescens, Conrad, Miiller, Synopsis, p. 36, 1836. Leptoxis nigrescens, Conrad, Adams' Genera i. p. 307. Ijeptoxis trivittata, DeKay, Adams' Genera i. p. 307. Anculotus monodontoides, Conrad, Miiller, Synopsis, p. 41, 1836. Nitocris monodontoides, Conrad, Adams' Genera i. p. 308. Nitocris deniata, Couth., Adams' Genera i. p. 308. 9. A. dilatata, Conrad. Nitocris dilatata, Conrad, Adams' Genera i. p. 308. Leptoxis dilatatus, Conrad, Chenu, Manuel, i. f. 2043 — 5. Nitocris Rogersii, Conrad, Adams' Genera i. p. 308. Nitocris Kirtlandianus, Anthony, Adams' Genera i. p. 308. Nitocris inflatus, Lea, Adams' Geuera i. p. 308. Melania inflata, Lea, Troschel, Archiv fur Naturgesch. ii. p. 226. 11. A. m e Ian o i d e s, Conrad. Nitocris melanoides, Conrad, Adams' Gerera i. p. 308. Anculotus melanoides, Conrad, Miiller, Synopsis, p. 42, 1836. Leptoxis turgida, Hald., Adams' Genera i. p. 307. Leptoxis viridis, Lea, Adams' Genera i. p. 308. 13. A. subglobosa, Say. Leptoxis subglobosa, Say, Adams' Genera i. p. 307. Lzptoxis gibbosa, Lea, Adams' Genera i. p. 307. Leptoxis globula, Lea, Adams' General, p. 307. Ijeptoxis tintinnabulum, Lea, Adams' Genera i. p. 307. Leptoxis virgata, Lea, Adams' Genera i. p. 307. 14. A. praerosa, Say. Anculosa prserosa, Say, Synonymy, Part 3. Leptoxis prxrosa, Say, Adams' Genera i. p. 307. Morch, Yoldi, Cat., p. 56. Lithasia meritiformis, Desh., Adams' Genera i. p. 308. Anculotus angulatus, Conrad, Miiller, Synopsis, p. 40, 1836. Leptoxis angulata, Conrad, Adams' Geoera i. p. 307. 15. A. c r a s s a, Haldeman. =Eurycsclon. A.pisum, Hald., Synonymy, Part 3, No. 19. Leptoxis pis urn, Hald., Adams' General, p. 307. 16. A. t a e n i a t a, Conrad. Anculotus tieniatus, Conrad, Miiller, Synopsis, p. 41, 1836. Leptoxis txniata, Conrad, Adams' Genera i. p. 307. 1865.] ♦Has 27 years priority over disimifo. 36 PROCEEDINGS OF THE ACADEMY OF 17. A.Troostiana, Lea. Leptoxis Troostiana, Lea, Adams' Genera i. p. 307. 25. A. p i c ta, Conrad. Anculosa picta, Conrad, Muller, Synopsis, p. 39, 1836. Leptoxis picta, Conrad, Adams' Genera i. p. 307. Leptoxis flammata, Conrad, Adams' Genera i. p. 307. 28. A. s qu a 1 i d a, Lea. Leptoxis squalida, Lea, Adams' Genera i. p. 307. 29. A. p a t u 1 a, Anthony. =dilatata, Conrad.? 30. A. v i r i d u 1 a, Anthony. ==dilalata, Conrad.? 33. A. t u r b i n a t a, Lea. =Euryaelon. Pursuant to the By-Laws, an election of members of the Standing Committees for 1865 was held, as follows : ETHNOLOGY. J. A. Meigs, S. S. Haldeman, I. I. Hayes. COMP. AN AT. AND GEN. ZOOLOGY. Joseph Leidy, J. M. Corse, J. H. Slack. MAMMALOGY. J. H. Slack, J. L. Le Conte, W. S. W. RUSCHENBERGER. ORNITHOLOGY. John Cassin, J. H. Slack, B. A. Hoopes. HERPETOLOGY $ ICHTHYOLOGY. E. D. Cope, E. Bridges, Th. Norris. CONCHOLOGY. T. A. Conrad, W. G. Binney, G. W. Tryon, Jr. ENTOMOLOGY AND CRUSTACEA. R. Bridges, E. T. Cresson, J. F. Knight. BOTANY. E. Durand, Joseph Carson, Aubrey H. Smith. GEOLOGY. Isaac Lea, Charles E. Smith, J. P. Lesley. MINERALOGY. Wm. S. Vaux, J. C. Trautwine, T. D. Rand. PALAEONTOLOGY. Joseph Leidy, T. A. Conrad, J. L. Le Conte. PHYSICS. B. Howard Rand, Wm. M. Uhler, R. E. Rogers. LIBRARY. Joseph Jeanes, Joseph Leidy, John Cassin. PROCEEDINGS. Joseph Leidy, Wm. S. Vaux, John Cassin, Thomas Stewardson, Robert Bridges. [Jan. NATURAL SCIENCES OP PHILADELPHIA. 37 February 14 th. The President, Dr. Bridges, in the Chair. Seven members present. The following paper was presented for publication and referred to a Committee : '; Descriptions of new species of Birds of the Families Paridas, Vire- onidae," &c. By Geo. N. Lawrence. The Committee on Proceedings placed on the table the published number for November and December, 1864. February 21st. Vice-President, Cassin, in the Chair. Sixteen members present. February 28th. The President, Dr. Bridges, in the Chair. Twelve members present. On report of the Committee, the following paper was ordered to be published : Descriptions of new species of BIRDS of the Families PARIDJ2, VIRECWIDJE, TYRANNIDJE and TROCHILID.E, with a note on Myiarchus Panamensis. BY GEO. N. LAWRENCE. 1. POLIOPTILA PLU1IBICEPS . Male. Entire crown and occiput dark plumbeous, bordered on each side by a black line which begins at the bill, running to and over the eye, and as far beyond as the dark cap extends ; upper plumage dark, bluish grey ; outer tail feather white, the next white except one third of the inner web at the base, where it is black, the third feather black with the end white for _5- of an inch, the other tail feathers are glossy black ; primaries blackish brown, secondaries black, broadly margined with white ; under wing coverts white ; sides of the head, lower eyelid, chin and abdomen white; throat, breast and sides bluish grey, lightest on the throat ; bill black ; tarsi and toes plumbeous black. First primary half the length of the second, the fourth longest, tail much graduated. Length 4£ in. ; wing 1 1|; tail 1 Ig ; bill T7_ tarsi f. Habitat. — Venezuela Collected by Mr. S. C. Nash. Prof. Baird in "Review of American Birds," p. 67, (now in course of publi- cation) has given a synopsis of the genus PAioptila, which he has divided into three sections, as follows : 1. Whole top of head black. 2. Sides of head black ; top gray. 3. Top of head gray ; sides whitish. The species now described cannot be placed in either of these, but will form the foundation of a fourth section, having the entire crown dark plumbeous. The color of the back and wing coverts comes nearest to that of 1'. leucogas- ter, but is of a lighter shade ; below it is rather more plumbeous, and the tail feathers are much narrower than in that species. 2. HYLOPHILUS ACDTICAUD0S. Head above and hind neck olive brown ; back greenish olive, brownish on the upper part, and gradually becoming brighter green on the rump ; tail dull 1865.] 38 PROCEEDINGS OF THE ACADEMY OP greenish olive, the shafts brown, the outer two feathers narrowly margined on their inner wel>s with pale yellow ; quills dark umber brown, edged with olive green ; sides of the head, throat and upper part of the breast dull ful- vous ash ; breast and abdomen pale fulvous ; sides olive green ; under lining of wings, inner edges of quills and under tail coverts pale yellow; upper mandible light hazel brown, the under whitish ; tarsi and toes pale yellowish brown. The first primary is § of an inch long, or about half the length of the fourth, which is the longest ; the tail feathers are relatively long, quite narrow and pointed at their ends ; bill rather short. Length 4^ in.; wing 2 ; tail If; billf ; tarsi Ii. Habitat. — Venezuela. Collected by S. C. Nash, In its narrow pointed tail feathers it appears to differ from all others that I have seen. 3. Myiarchus venezuelensis. Plumage above of a dark olivaceous brown, darker on the crown ; tail dark umber brown, the outer feather with the outer web dull white, tinged with brownish next the shaft ; the other tail feathers have a narrow edging of bright rufous on their outer webs, the extreme ends of all dull white ; quill feathers dark umber brown, the primaries with a very narrow margining of pale rufous, the secondaries and tertiaries edged with white ; the wing coverts dark brown with margins of soiled white ; under wing coverts pale yellow, inner edges of quills pale buffy white ; throat, upper part and sides of breast bluish grey, sides under the wings slightly olivaceous ; abdomen and under tail coverts very pale yellow, a little brighter only in the middle of the former ; bill and feet black. Fourth quill slightly the longest, first and ninth equal. Length 7| in. ; wing 3^ ; tail 3£ ; bill II ; tarsi j. Hnbitat. — Venezuela. Collected by S. C. Nash. This species is closely related to my M. Panamensis ; it is a little smaller, darker and more brown above, and the yellow of the under parts paler ; it differs also in the bright rufous margins on the tail feathers, in the whiter edges of the wing coverts and smaller quill feathers, and in having the feet black ; it is likewise more grey on the breast. Note. The typical specimen of M. Panamensis was not in very good con- dition, the feathers of the wings and tail being somewhat worn ; since descri- bing it I have received specimens in perfect plumage, which enable me to note some differences as follows : the color of the back is olive green ; the throat is of a lighter grey than in the type, and the sides of the breast are olive green ; the edges of the tail feathers are dull olive with a slight sandy tinge at the base, in the type from their worn and rusty appearance I described them as edged with pale rufous, this edging, however, is slight and not at all of marked character ; the outer web of the lateral feather is pale ashy brown : the bill is dark brown, lighter underneath ; the tarsi, though at first sight appearing black, have a tinge of dark reddish or vinous color ; this I find to be their color also in the type. These differences are probably owing to the season when killed. The irides are stated by Mr. Galbraith to be brown. The sexes are alike in plumage. 4. Chalybuka .eneicauda. Mule. Plumage above and below shining dark green, the head, throat and neck of a golden tinge, deepening to reddish orange on the front, chin and throat ; upper tail coverts reddish or coppery bronze ; two middle tail feath- ers coppery bronze (not so bright as the tail coverts), the other tail feathers deep steel blue, all except the outer one margined with the same bronze color as the central ones, decreasing in extent from the central feathers ; wings brownish purple ; under tail coverts white ; bill black ; feet blackish brown, the toes underneath pale yellow. fFeb. NATURAL SCIENCES OF PHILADELPHIA. 39 Length 5 in. ; wing 2' 3 ; tail If ; bill 1. Habitat. — Venezuela. Collected by S. C. Nash. This species is of the same size as C. Btffoni, which it also most resembles, it differs from it in the golden hue of the front and throat, and in the decidedly bronzed taiJ, the bronzing on the tail of Buffo ni being very slight, and is just perceptible on the edges of some of the feathers. G. urochri/sea, Gould, has the "tail rich golden bronze both above and beneath," aud the " lower mandible fleshy red," whereas in my species the upper surface of the tail only is bronzed, and the bill is wholly black. 5. Chalybura Carnioli. Mule. Upper plumige dark green with a tinge of golden on the wing cov- erts and lower part of the back ; upper tail coverts dark violet purple, the tail has both the upper and under surface bronzed violet purple, lighter in color than the coverts; wings brownish purple; throat of a shining deep green ; breast and abdomen dull green ; under tail coverts dull violet purple : upper mandible black, under yellow with the tip black ; tarsi and toes yellow. Length 5 in. ; wing 2| ; tail 1| ; bill J. The female differs in having the middle of the throat, the lower part of the abdomen and the under tail coverts dull ash ; the outer three tail feathers marked at their ends with pale ash, most so on the outer feather. Habitat. — Costa Rica, Angostura. In museum of the Smithsonian Institu- tion. This species appears to be somewhat like C. Isaurre in the coloring of the tail, but differs remarkably from that species as well as from all others of the genus, in having its under tail coverts of a dark color, instead of pure white. I have named it in compliment to Mr. Julian Carniol whose large collections sent to the Smithsonian Institution (containing many new species besides thi>) give evidence of his energy and industry as an explorer. (5. Panychlora parvirostris. Female. Upper plumage of a rather light grass green with a golden tinge : upper tail coverts and central feathers golden bronze, much deeper in color on the coverts ; the other tail feathers are white at their bases for more than half their length, succeeded by a broad band of brownish black and ending in white, the outer feather being most largely tipped with white ; under surface pale ashy grey ; under tail coverts white ; bill black ; toes blackish brown, underneath pale yellow. Length 3 in. ; wing If ; tail J ; bill J. Habitat. — Costa Rica, Angostura. Collected by J. Carniol. Museum of Smithsonian Institution. The bill is strikingly small compared with that of P. AUci(v, although in their other measurements they are much alike ; it also differs from the female of that species in the upper tail coverts being golden orange instead of pure green, and in the bases of the tail feathers being white instead of green. The male will, without doubt, be found to possess the glittering green plumage of its allies. March 1th. Vice-President Cassin in the Chair. Eighteen members present. March 14th. The President, Dr. Bridges, in the Chair. Twenty members present. 1865.] 40 PROCEEDINGS OP THE ACADEMY OP Special Meeting, March \Q>th. The President, Dr. Bridges, in the Chair. Twentv-one members present. The President announced the death of Dr. Thomas B. Wilson, aged 59 years, at Newark, Del., on the 15th inst., at 7 J o'clock, A. M., of typhus fever. A Committee having been appointed to draught a series of resolutions in reference to the sad event, the following were pre- sented and adopted : Whereas, The Academy of Natural Sciences of Philadelphia having sustained a most serious loss in the death of its late distinguished President, Thomas B. Wilson, M. D., Resolved, That our late fellow member, Dr. Thomas B. Wilson, is eminently entitled to be regarded as the most judicious and liberal patron of the zoolo- gical sciences that our country has yet produced, and that we have heard his death announced with sentiments of the most profound sorrow. Resolved, That in his great abilities and vast scientific acquirements, as well as in all the relations of private life, we recognize in Dr. Wilson the character of a true man of genius, a thorough, earnest and most conscientious cultivator and friend of the sciences, and a most valuable and patriotic citizen. Resolved, That in the infancy of the study of the natural sciences in the United States, the gratuitous and ready aid afforded by Dr. Wilson con- tributed largely to that development of those sciences which now places this Academy in rank with similar institutions of the old world. Resolved, That the liberality of Dr. Wilson to this Academy, and the large facilities thereby provided for study and research, do fully entitle him to the unqualified gratitude, not only of our members, but of all students of the natural sciences in this country, and that we are justified in regarding and we sincerely recommend our successors as members of this Academy to regard, his munificent and unparalleled contributions to our library, and especially to our museum, (nearly the whole of which, in several departments, we owe to his liberality), as an honorable and perpetual monument to his zeal in behalf of the natural sciences. Resolved, That a copy of these resolutions be presented to each of the bro- thers and sisters of Dr. Wilson, and that they be published in the public journals of this city and in the scientific journals of the United States. On resolution of the Academy, the President appointed Mr. Cassin to prepare a memoir of Dr. Wilson, to be published in the Proceed- ings : On motion, it was resolved to adjourn to meet in the Hall of the Academy on Saturday, 18th inst., at 2\ o'clock, P. M., to attend the funeral of Dr. Wilson. [Mar. NATURAL SCIENCES OP PHILADELPHIA. 41 March ISth. The President, Dr. Bridges in the Chair. Twenty-eight members present. This meeting having been held for the purpose of attending the funeral of our late lamented and distinguished member, Dr. Thomas B. Wilson, it was immediately adjourned for that purpose. March 21st. The President, Dr. Bridges, in the Chair. Eighteen members present. A paper was presented for publication entitled " Notice of some new types of Organic Remains from the Coal Measures of Illinois." By F. B. Meek and A. H. Worthen. March 28th. The President, Dr. Bridges, in the Chair. Fifteen members present. On the report of the Committee, the following paper was ordered to be published : Notice of some New Types of Organic Eemains, from the Coal Measures of Illinois. BY P. B. MEEK AND A. H. WORTHEN. The fossils described in this paper were discovered at a locality on the south side of the Illinois River, at Morris, Grundy County, Illinois, near the northern boundary of the Coal Measures of that State. This locality is al- ready well known from the numerous beautiful specimens of fossil ferns it has afforded, as well as from the discovery there of a remarkable extinct Neurop- terous Insect, described by Prof. Dana in vol. xxxvi. 2d ser. p. 34, Am. Journ. Sci. The bed from which all these interesting fossils were obtained, holds a position near the base of the Illinois Coal Measures, somewhat above the horizon of the second seam of coal. At the out-crop, where these specimens were collected, a thickness of about twenty feet of strata is exposed, consisting of sandy shale, passing downwards into a more argillaceous shale, forming the bed of a small stream ; while a short distance further down this little stream, and at a lower horizon, a thin seam of coal crops out. No workable beds of coal are known in the State north of this County, and the Coal Measures here rest directly upon Silurian Rocks. The fossils at this locality are immediately enveloped in biscuit-shaped iron-stone nodules. These nodules are not generally composed of concentric layers, but show, on weathered surfaces, a tendency to a laminated structure, the planes of lamination being flat, parallel lo the greater diameter of the con- cretions, and probably also coincident with those of the shale, as they lie in the bed. On breaking open these concretions, the laminated structure is gen- erally found not to extend within ; the interior having a homogeneous, rather compact structure, and a grey or brownish grey color, (the iron beis:g usu- 1865.] 42 PROCEEDINGS OF THE ACADEMY OF ally in the condition of a carbonate), while more or less arenaceous and ar- gillaceous matters also enter into their composition. Some of the concre- tions seem to contain no organic remains, but often in breaking open others, a fossil is found to have formed the nucleus around which the concretionary action took place. It is an interesting fact that we find here, near the base of the Illinois Coal Measures, a species of the remarkable genus Bellinurus, an intermediate link, (hitherto only known to occur in the lower Coal Measures of England and Ire. land,) between the older Trilobites, and the existing genus Limulus. In Eng- land it is found enveloped in similar iron-stone nodules, at Cole-Brook-Dale, where three species have been discovered, one of which [B. bcllulus, Koenig, = B. rotundatus, Prestwich) is closely related to our Illinois species. We likewise find at the Morris locality a species of the genus Anthrapalse- mon, Salter, (or a closely allied type) which in Scotland also occurs in the lower Coal Measures, while neither of these genera are known in the subcar- boniferous, or any lower formation. These facts furnish additional evi- dences, if any were necessary, (coinciding with all the other palaeontological, as well as stratigraphical, evidence) of the fallacy of an opinion recently ex- pressed by a writer in the Bulletin of the Geological Society of France, that our western Coal Measures, and particularly those of Illinois and the adjoin- ing States, belong not to the horizon of the true Coal Measures of Europe, but to the subcarboniferous or mouhtain limestone series. In a paper by one of the writers, published in the March number of the American Journal of Science, 1865, after speaking of the general distribu- tion of marine remains in our western Coal Measures, he remarked (which was strictly in accordance with his observations up to that time) that after more than twenty years familiarity with the fossils of the coal formation of the Western States, he had never seen amongst them any terrestrial or fresh- water types, other than plants. Since investigating the fossils described in this paper, however, amongst which it will be seen there is believed to be a Caterpillar, we can but regard the Morris bed as an exception to this general rule. If the fossil to which we allude is a true Caterpillar, its presence there, along with the insect described by Prof. Dana, would indicate that this bed was probably deposited in an estuary, into which this little worm- like larva, and the other insect, were doubtless carried from the land by an inflowing stream or the ebbing tide. This suggestion also receives some support from the affinities of the associated Crustacea, since the genus Bellinurus, from its relations to the existing genus Limulus, might have been capable of living at least in brackish waters, although the English species are associated with marine forms. The genus Anthrupalsemon is also supposed, by Prof. Dana, to have been related to JEglea, a fresh-water type. In addition to these facts, no unquestionable, strictly marine forms of any kind have, so far as we know, been yet found in this bed. The existence of this exceptional case (if it is such) of terrestrialand fresh or brackish-water fossils in our western Coal Measures, has no bearing, how- ever, against the general conclusions in connection with which the statement above alluded to was made ; nor even, indeed, against the general accuracy of the statement itself, since the fact of the almost exclusive and general distribution of marine animal remains in our western Coal Measures, stands unshaken. The fossils here noticed will be fully illustrated and described, and such additional facts given as we'may in the mean time learn from other speci- mens, in the forthcoming report of the Illinois Geological Survey, for the publication of which we are happy to announce the Legislature has made a liberal appropriation. We are indebted to Prof. Dana for the use of several specimens of some of the Crustacea described in this paper, as well as for suggestions in regard to their affinities; also to Dr. Stimpson for suggestions respecting the same. [Mar. NATURAL SCIENCES OF PHILADELPHIA. 43 We are likewise under obligations to Mr. Joseph Evans, of Morris, Illinois, who first discovered the fossils at this locality, for the use of several speci- mens. Amongst others, the form we have supposed to be a Caterpillar and that we have referred to Anthrapalcemon, belonging to him. CRUSTACEA. ENTOMOSTRACA. XYPHOSURA. Genus BELLINURUS, Koenig. Not having had an opportunity to consult Kcenig's original diagnosis of this genus, nor indeed a good description of it by any other author, we are not aware what characters were assigned it, or how its author proposed to distinguish it from the existing genus Limulus. Most authors, including Milne Edwards, Bronn, Prestwich, Mantell, Portlock, Murchison and others, referred the species to Limulus, though Portlock in doing so remarks that the distinct trilobation and segmencation of the abdomen in these fossil species, seem to constitute a generic distinction. Pictet admits the genus in his Trait de Palceont., ii. 538, and remarks that it is distinguished from Limulus " by the articulation of the tail, and above all by the abdominal buckler presenting two distinct longitudinal furrows." Prof. Owen also admits the genus, in his valuable " Palaeontology, or Systematic Summary of Extinct Animals," (p. 43) and says it differs from the " King-Crab, {Limulus) in the movable condition of the body segments." A careful study, however, of fine specimens of the species described below, has satisfied us that the segments of its abdomen are not movable, but as firmly and completely united into a single shield as in the genus Limulus. We are, therefore, led to believe that this genus is mainly distinguished from Lim- ulus, (so far as its characters have yet been made out) by the more transverse form of its cephalo-thoracic shield, its proportionally much longer and more slender legs*, the transversely or subcircular form, and distinct trilobation and segmentation (not complete division, however,) of its abdomen ; as well as by its flattened borders without movable spines. There are also some dif- ferences in the more anterior position of the eyes, the stronger and more con- tinuous character of the ocular ridges, as well as in the subdivisions of the area circumscribed by these ridges in Bellinurus. Other differences, of perhaps greater importance, will probably be observed, when the appendages of the under side can be seen. None of our specimens are in a condition to show the small anterior pair of simple eyes, though from the general analogy of this interesting crustacean to the genus Limulus, it is more than probable better specimens may show them. And yet it is possible, from the more anterior position of the eyes, corresponding to the larger reticulated pair in the genus Limulus, that the small supplementary pair may not have been needed. As in LAmulus, it shows a row of six small pits in each of the longitudinal furrows of the abdomen, marking the position of the muscular apophyses within ; while the condyle, for the articulation of the abdomen with the cephalothorax, seems to agree exactly with that of Limulus. We are not aware of the nature of the peculiarities in the articulation of the caudal segment mentioned by Pictet, none of our specimens being in a condition to show the connection of these parts satisfactorily, while he does not explain in what the difference consists. *One of our specimens of the following described species, as well as one of B. anthrax, figured by Prestwieh, (Trans. Geol. Soc, London, v. p. xli. fig 1,) shows that at least one pair of the legs (if they were articulated around the mouth, at the middle of the cephalothorax, as in Limulus) must have been quite as long as the abdominal and cephalothoracic shields together; which would be proportionally more than twice the length of any of the legs in Limulus. 1865.] 44 PROCEEDINGS OF THE ACADEMY OF Bbllinuros Dan^i, M. & W. V Cephalo-thoracic shield transversely crescentric, more than twice as wide as long, moderately convex, the height nearly equalling half its length ; ante- rior and antero-lateral margins broadly and regularly rounded ; lateral angles produced obliquely backwards and outwards, with a very slight inward curve, into slender mucronate spines, terminating remote from, and nearly opposite the middle of the abdomen ; posterior margin on each side for about two- thirds of the way in from the lateral angles, toward the middle, concave in outline ; nearly straight or very slightly concave along the middle between these two points. Mesial lobe small, somewhat lower than the ocular ridge on either side, but rounded and well defined behind, where it supports a small central tubercle (or short spine?), thence narrowing forward, and sometimes showing a slight tendency to develope a second much smaller tubercle, at about one-third the length of the shield from its posterior margin ; near which point it suddenly contracts into a mere linear carina that extends forward to the anterior transverse division of the ocular ridge. Area cir- cumscribed by the ocular ridge, crown-shaped, or subquadrangular in out- line, and composing the central third of the cephalo-thoracic shield ; a little wider anteriorly than its length, which equals about five-sixths that of the shield ; lateral margins concave in outline ; anterior side convex, with a central emargination ; internal surface divided into four irregular subordi- nate areas, by the mesial lobe with its linear anterior continuation, and a less distinctly defined, secondary transverse linear ridge. Ocular ridge narrow, but distinct, its lateral divisions arching inwards behind the eyes, and terminating posteriorly at the margin of the shield nearly opposite the middle of each lateral lobe of the abdomen, in a (triangular ?) spine, which is directed backwards, outwards and a little upwards ; anterior transverse di- vision arching forwards on each side, and curving backwards in the middle. Compound ? eyes small, remote, and located one at each antero-lateral angle of the crown-shaped central area, at points about one-third the length of the shield from its anterior margin. (Simple eyes, if they existed, unknown.) Abdomen transversely suboval, or truncato-subcircular in outline, being wider than long, and nearly straight anteriorly, with lateral margins rounding in abruptly in front, and more gradually into the regularly rounded posterior outline ; generally rather more depressed than the cephalo-thorax, particularly in'front. Flattened lateral border rather narrow, and regularly scolloped be- tw'een its projecting marginal spines. Mesial lobe narrow, or of about the same breadth as that of the cephalo-thorax, and near half as broad as, aud a little more elevated than, the lateral lobes ; segments well defined ; first and third each provided with a small central tubercle ; sixth as long as any three of the others, rather abruptly narrowed and depressed behind, and surmounted anteriorly by a large tubercle (or spine ?). Lateral lobes somewhat flattened on the inner half, and rounding down rather abruptly to the flattened free borders on each side and behind ; segments defined by distinct linear ridges, which are separated by flattened spaces four or five times as wide; these ridges extend obliquely outwards and a little backwards across the lateral lobes and their flattened borders, beyond which they are produced into slender mucronate spines, of nearly equal length, curved obliquely backwards. Caudal segment, or stylet, apparently nearly two-thirds as long as the ab- domen ; gradually tapering, and trigonal or sub-trigonal, being flat below, angular on each side, and angular or rounded above. Appendages of the under side unknown, excepting one of the legs, which is seen in one specimen, projecting out from under the cephalo-thoracic shield, between its posterior margin and the abdomen. It is long and slender, and shows of the first segment projecting from under the shield, a length of about 0-12 inch. The next segment appears to be 0-25 inch in length, with a breadth of only 004 inch. The succeeding segment can be traced in [Mar. NATURAL SCIENCES OP PHILADELPHIA. 45 the matrix for a distance of about 0-30 inch, being slightly curved near the extremity, and apparently tapering to a point, this was probably also pro- vided with a movable finger as in Limulus, but the specimen is not in a con- dition to show it. It is not possible to determine which one of the legs this is. Entire length from the extremity of the caudal segment to the anterior margin of the cephalo-thorax, about 1-90 inches. Length of cephalo-thorax, 0-51 inch, breadth of do. to the extremities of postero-lateral spines, 1-70 inches ; length of area included within the ocular ridge, 0-50 inch ; greatest breadth of do. (which is the distance between the eyes,) 0.60 inch. Length of abdomen, 0*65 inch ; breadth of do., exclusive of the flattened margin, 0-94 inch, including it, 1-06 inch; breadth of mesial lobe, 0-23 inch ; length of caudal segment, about 0-60 inch. Of the known species of Bellinurus, ours seems to be most nearly related to B. bellulus, Koenig, (the type of the genus, if we mistake not), which is re- garded as being identical with Limulus rotundatus, of Prestwich, (Trans. Geol. Soc, London, v. p. 413, pi. XLI. figs. 4, 6 and 7.) From this species, however, it may be at once distinguished by having the lateral angles of its cephalo-thorax produced into long, slender spines, and the flattened border of its abdomen proportionally much narrower, and armed with a series of sharp-curved spines, instead of being merely serrated. We should also remark here, that Prof. Owen's figure of B. bellulus, (Palae- ontology, p. 42,) as well as that given by Murchison of the same, under Prest- wich's name rotundatus, (Siluria, p. 318,) represent the eyes as being located at the lateral extremities of a large, transversely oval or subelliptical area ; while within this, there is a smaller, crown-shaped area, circumscribed by a ridge, and in all its principal features, corresponding to that which in our species has the eyes located at its anterior lateral angles. This wide dif- ference in the position of the eyes, as well as in the ridges of the central region of the cephalo-thoracic shield, if they really exist, would apparently be of more than specific importance. The close general agreement, however, of these forms, in all their other essential characters, renders it very impro- bable that they belong to different genera. Hence, we would suggest that there may have been some error in the figures cited above, representing the eyes (which are with difficulty seen in any but well preserved specimens) in this outer position, and the presence of a large outer ocular area surrounding that corresponding to the quadrangular one in our species. We are the more inclined to think this is the case, from the fact that Owen's and Murehison's figures appear to have been reduced from Prestwich's figures 5 and 6, cited above ; which represent the two halves of a nodule, containing a specimen and its mould, of B. bellulus, with a large transversely oval space in the cen- tral region of the cephalo-thorax, as we must think, accidentally crushed in. This view seems to be sustained, too, by Mantell's figures of the same species, from specimens collected by him at the same locality, (see Medals of Crea- tion, p. 550,) which show no traces of this outer transversely oval ocular area. In the elongated, spine-like character of the lateral angle of its cephalo- thoracic shield, as well as in having the margins of the abdomen armed with sharp spines, our species agrees more nearly with B. anthrax (= Limulus an- thrax, Prestwich), but it differs in the form of the outline of the anterior side of the cephalo-thorax, as well as in the direction of its prolonged lateral angles, and its less produced spines around the flattened margins of the ab- domen. Hence, it appears to be intermediate in its characters between B. anthrax and B. bellulus. We are gratified to be able to dedicate this fine species, the first of the genus hitherto discovered in America, to Prof James D. Dana, the author of one of the most important works on the Crustacea ever published ; to whom we are indebted for the loan of one of the specimens from which the fore- going description was drawn up. 1865.] 46 PROCEEDINGS OF THE ACADEMY OP TETRADECAPODA. ISOPODA. (ANISOPODA.) ? Family ACANTHOTELSONIDJE. Genus ACANTHOTELSON, Meek & Worthen. Superior antennae nearly as long as the inferior, and provided with well developed accessory appendages ; flagella of both pairs longer than the pe- duncles ; head about equalling the length of the first two anterior thoracic segments. Thoracic and abdominal segments (except the last one) not dif- fering materially in length, and each shorter than the head. Anterior thora- cic legs longer than the others, not chelate. Telson or terminal segment eimple, long, spiniform, and laterally compressed. Stylets with second seg- ments (bifid?) much longer than the first, and similar to the telson. The fact that the oral apparatus, and other appendages of the head, as well as the branchiae, always so important in the classification of the Crus- tacea, are so rarely preserved in fossil species, especially those of smaller sizes, renders their study more difficult than that of most other organic re- mains. Hence, in describing new species, genera, or other groups, the palae- ontologist is often unable to give any information in regard to the very parts that would be the first to claim the attention of the Carcinologist in the in- vestigation of recent species. Another difficulty also arises from the fact that, as in other departments of palaeontology, it often happens in the study of fossil Crustacea, we meet with types presenting a combinatiou of cha- racters which in existing species are distributed in widely distinct groups. So that on finding a new type showing only a part of its characters, we would often be led at once to place it in a group with which probably the next specimen found would show it to possess some one or more wholly in- compatible peculiarities. On first examining specimens of the typical species of the genus above described, our impression was, that it must be, beyond all doubt, a true Am- phipod. A more careful examination, however, soon showed that it presented the radical difference from all the known types of that extensive group, of having only one pair of the abdominal appendages styliform, and the other five natatory, instead of three pairs styliform and three natatory ; thus com- bining with its Amphipodan abdomen, thorax, head, anterior appendages, and general physiognomy, the single pair of styliform appendages of the hopoda. Being therefore left in doubt in regard to its affinities, we sent sketches of some of the best specimens to Prof. Dana, who had also previously received some imperfect specimens of the same species from Illinois. On examining these sketches and specimens, Prof. Dana wrote that he thinks this crusta- cean most probably belongs to a group holding an intermediate position be- tween the typical hopoda and the Amphipoda, for which he has proposed the name Anisopoda. This intermediate group, as first shown by Prof. Dana, is characterized, like the Amphipoda, by having the three posterior pairs of thoracic legs in one series, and the four anterior in another ; while, as in the hopoda, the branchiae are abdominal, and only one pair of abdominal appen- dages are styliform, and five branchial. In regard to the division of the thoracic legs into two series, we would remark, that we have observed no evidences of it in all the specimens we have seen, excepting one of those kindly loaned us by Prof. Dana. In this, however, four pairs of these legs seem to be directed backwards, and only three forward; which, if not produced by accidental distortion, would indi- cate Jsopod affinities. Yet, in all the other specimens seen, the whole seven pairs are directed forward. Although much inclined to believe the latter their normal arrangement, it should be remembered, as suggested by Prof. [Mar, NATURAL SCIENCES OF PHILADELPHIA. 47 Dana, that however important this character may be in the study of the re- cent Tetradecapod Crustacea, it can scarcely be made available in the inves- tigation of crushed fossil species, where so many accidents might have oc- curred to place the legs in an unnatural position. We have not been able to clearly satisfy ourselves whether or not our crus- tacean had squamiformly developed epimerals, as in the normal groups of Amphipoda ; though some of the specimens appear to show indications of such development; while the shortening of the vertical diameter of the tho- racic segments, as compared with those of the abdomen, would seem to be, as it were, an arrangement to make room for such scale-like epimerals. In addition to this, the fact that all of the six or eight specimens we have yet seen, lie in the concretions upon one side or the other, would appear to indi- cate that the lateral motion of the thoracic legs was in some way restrained so as to prevent the animal from taking an erect position, which is precisely the effect produced in the normal Amphipoda by the possession of well de- veloped squamose epimerals. If this should prove to be the case, it would show that the remarkable combination of Amphipod and Isopod, or Anisopod characters, already alluded to in this fossil, are real, and not simulative ; since it would thus present mainly the anterior structure (possibly even to the thoracic position of the branchiae) of a normal Amphipod, combined with the single pair of styliform, and five natatory abdominal appendages of the Itsopoda or Anisopoda. It must be evident, we think, that such an ensemble of characters as that presented by our fossil, would exclude it from any known family of the Te- tradecapoda ; hence we can but regard it as the type of a new family. ACANTHOTELSON SlIMPSONII, M. & W. Linear or sublinear in form. Upper antennas at least as long as the head and first five thoracic segments ; peduncle moderately stout, rather longer than the head ; first joint a little longer and wider than the two others, which are of nearly equal length ; flagellum slender and very minutely jointed ; acces- sory appendage nearly or quite as long as the flagellum, and like it, minutely jointed. Inferior antennae as long as the head and seven thoracic segments; peduncle slightly longer, but otherwise similar to that of the upper antenna? ; flagellum a Utile stouter and longer, but in other respects as in the upper pair. Head, as seen in the (compressed) side view, subquadrangular, longer on the upper than the lower side, in consequence of the obliquity of anterior side ; eyes small, round, placed just below the bases of the upper antennae. The (fourteen) thoracic and abdominal segments distinct, and (excepting the last one) of nearly equal length, — a few of those nearest the head being a little shorter than the others ; all diminishing in depth (side view) from about the antepenultimate one forward ; their anterior baBal margins rounded ; posterior rectangular, or a little rounded. First pair of thoracic legs about one-fourth longer, and a little stouter than the succeeding five pairs, and apparently terminating in a slender, sharp dactylus ; first joint above, a little shorter, narrower, and more tapering than the next — neither more enlarged than the other joints above. Five succeed- ing pairs of legs of nearly equal size and form ; their upper two (or three?) joints very short, and not enlarged ; seventh pair nearly as long as the first, and more slender than the others. Natatory abdominal appendages long and slender; styliform pair with first joint short and quadrangular; second and only other joint (double ?) with each branch (if there are two) simple, equal and as long as the telson, which they nearly exactly resemble in form ; their upper and lower margins each with a row of short, oblique, rather distant setae, between which may be seen by the aid of a magnifier, a series of much more minute, closely-arranged seta?. Telson as long as the last four abdomi- nal segments ; at its base one-half as wide, vertically, as the penultimate 1865.] 48 PROCEEDINGS OP THE ACADEMY OP abdominal segment; thence tapering, at first rapidly, and then very gradu- ally, to a mucronate point, — upper and lower margins setigerous, like those of the stylets. It is possible that when we can have an opportunity to examine additional specimens, we may have to modify some of the characters given in the fore- going generic or specific description ; though not, we believe, in any very essential particular. We hope, however, to be able, hereafter, to clear up several doubtful points in the structure of this interesting type, when we can have better specimens for study. Length from anterior side of head to the extremity of the penultimate ab- dominal segment 1.30 inches ; length of telson 0-31 inch ; length of the first six abdominal segments 0*52 inch ; length of the seven thoracic segments about 0-64 inch. Height of third abdominal segment 0-20 ; height of each first two or three thoracic segments 0-12 inch ; length of stylets about 0-31 inch, of which the first joint forms only about 0-06 inch. Length of outer antennae, including its peduncle, 0-66 inch. It is with pleasure that we dedicate this typical species of a new and remarkable extinct genus to our friend Dr. William Stimpson, whose labors in carcinology, and various other departments of zoology, are well known iu this country and Europe. ACANTHOTELSON IN^EQUALIS, M. & W. The specimen upon which we propose to found this species, appears to agree with the last in almost every respect, excepting in the proportional size and the form of the segments. In the first place, the penultimate ab- dominal segment is nearly twice the length of any of the others, instead of being nearly or quite of the same length ; while the other abdominal seg- ments (as seen in a side view) are more cuneiform than in the last. Again, the fifth and sixth thoracic segments are longer, particularly above, and the fourth shorter, than any of the others, instead of all being of about the same length. We have not been able to see the stylets, nor to make out the nature of the legs, but from a part of one of those of the anterior pair, they would seem to be rather stouter than in the last described species. As these differences can scarcely be due to accidental distortion, we can but regard this form, with the material now at hand for comparison, as a distinct species. If we are correct in this view, it is probable good examples will show other differences than those mentioned above. Length of head, thorax and abdomen 0-90 inch ; length of head 0-12 inch ; length of the seven thoracic segments about 0-50 ; length of first five ab- dominal segments 0-26 inch ; length of penultimate abdominal segment 0-09. Height of third abdominal segment (flattened side view) 0-13 inch ; height of anterior thoracic segments about 0 07 inch. Length of lower antennae at least 0-43 inch ; length of upper not less than 0-36 inch, and probably a little more. ? Family PAL.EOCARIDJE. Genus PALJ30CARIS, Meek k Worthen. Inner and outer pairs of antennas of nearly equal length, the former each bearing a well developed accessory appendage ; peduncles of both pairs shorter than the flagella. Head about as long as the first two abdominal segments. Thoracic legs long and slender ; anterior pair not chelate. Tel- son long, tapering and horizontally flattened ; stylets with first joint very small, second double, and also flattened horizontally. This is another remarkable type, presenting, so far as can be determined, even a more puzzling combination of characters than that we have described under the name Ac.anthotelson. In the nature of its antennae, with their ap- parently well-developed basal scales, the structure of its caudal appendages, and its lono-, slender legs, spread out on each side, for walking in an erect [Mar. NATURAL SCIENCES OF PHILADELPHIA. 49 attitude ; as well as in the depressed, slender form of its abdomen and thorax, U seems to present decidedly the aspect of a Macrural Decapod. Yet, on a closer examination, we can see no traces of a carapace, — the thorax being apparently divided into seven segments, like those of the abdomen, and each provided with a pair of legs, as in the Tetradecapoda. If we are not mistaken in these latter characters, and we certainly believe we are not, it must show a most extraordinary union of characters, which, amongst recent Crustacea, belong to different primary divisions. From all that can be made out of its structure, we are therefore inclined to view it as one of the " embryonic" or " comprehensive" types, so often met with in various departments of palaeon- tology, and which furnish the advocates of the Darwinian hypothesis with some of their strongest arguments. For the present, this genus is placed, provisionally, along with the Tetra- decapoda, though it cannot, we think, be included in any known family of that division ; while if it should prove to be an embryonic or low type of the Decapoda, it may be even necessary to establish for its reception, a division of more than family importance. It is proper to remark here, however, that we have not seen any one specimen showing the caudal appendages we have described, along with the other characters of the thoracic and cephalic members, mentioned above. One imperfect specimen shows the seven tho- racic and five or six of the abdominal segments, with their legs and nata- tory appendages, the head, antennae, and apparently their basal scales; while another shows the caudal appendages, and all of the thoracic and abdominal segments, very distinctly, without any of the other members. The general agreement, however, of these specimens, in the parts preserved in each, is such that scarcely a doubt can be entertained that they belong to the same species. Yet, in order to prevent confusion, we would remark, that in case they should prove to belong to different genera, or species, that it is the form showing the head, antennae, thoracic and abdominal segments, with their appendages, &c, that we regard as the type of the genus. Pal^iocaris typos, M. & W. Linear, with thorax slightly wider near the middle than the abdomen ; thoracic and abdominal segments of nearly equal length. Inner antennae equalling the length of the head and thorax ; peduncles stout, first joint a little longer and wider than either of the other two, which are of nearly equal length, aud minutely and closely setigerous on their inner margins ; flagel- lum very slender, and minutely jointed ; accessory appendage nearly or quite as long as the flagellum, and scarcely differing from it otherwise. Outer antenna possibly a little longer than the others, peduncles slightly longer than those of the other pair, and like them minutely setigerous in front ; basal scales (?) oblong, about as long as first joint of peduncles, squarely trun- cated. Thoracic legs slender and long, anterior ones apparently not longer or larger than the others, none of them (so far as can be seen) chelate, or with any of the segments enlarged ; all the others with the first two or three joints very short ; fourth ? joint horizontally extended, tapering, and about as long as four segments of the body; succeeding joints (in the specimen ex- amined) very slender and abruptly bent downwards and backwards. Na- tatory abdominal appendages acutely lancelinear, and some of them as long as four of the abdominal segments. Telson nearly as broad at the base as the penultimate segment, tapering, and as long as two and a half of the abdominal segments ; minutely setigerous on each side. Stylets, with first joint very minute; second with each division as long as the telson, and lan- celinear in form, with pointed extremities, and parallel, more or less setiger- ous margins. Length of head, thorax, and first six abdominal segments, 0-78 inch ; do. of head, 012 inch; do. of the seven thoracic segments, 0-35 inch ; do. of 1865.] 4 50 PROCEEDINGS OF THE ACADEMY OP the first six abdominal segments, about 0-31. Length of telson, about 0*14 inch ; do. of stylets, near 0-13 inch. Length of lower or outer antennae, not less than 0-38 inch, (probably more), of which the peduncle forms 0-15 inch ; do. of inner, near 0*40 inch. Breadth of thorax, 0-13 inch. DECAPODA. MACRURA. ? Genus ANTHRAPALiEMON, Salter, 1861. The genus Anthrapahcmon was proposed by Mr. Salter in the Quarterly Jour- nal of tbe Geological Society of London, vol. xvii., p. 529, for the reception of a Crustacean from the Coal Measures of Scotland. His description of the genus reads as follows : — " Carapace scarcely so broad as long, (except when crushed flat), simple, Hatter than semicylindrical, the sides a little arched outwards. A strong central ridge in front, projecting as a thick (serrate?) spine is separated by a concave space, or slight furrow, from a posterior central ridge, which only occupies (in the type species, Grossarii) a small portion of the length. Front margin serrated. The outer antennas have wide, square basal joints, appar- ently without any advantage ;* the 2d and 3d joints not much oblique ; the rest about as broad as long. Abdomen as broad as long, of six joints (besides the telson), broad and very short ; the pleurae, except the 2d, pointed. Tel- son very broad ; appendages to the penultimate joint, double on each side, subtrigonal, broad." The name Anthrapalxmon was proposed from its supposed affinities to the recent genus Palxmon, but Prof. Dana thinks it more nearly related to uftjlea and Galathea. Anthkapal.emon gracilis, M. & W. It is with considerable doubt that we venture to refer this species to Mr. Salter's genus, the only specimen we have seen being imperfect, and not in a condition to show the more important characters. In form and general appearance, however, as well as in such of its details .as can be made out, it seems to agree well with that genus. The specimen consists of the abdomen and caudal appendages, (in a crushed condition), and an impression in the matrix of the under side of the carapace, the outer pair of antennas, and ap- parently of the eyes. The carapace, as seen from above, presents nearly an oblong form, excepting that the lateral margins are moderately convex in outline; the two extremities are truncated, and the breadth nearly or quite equalling three-fourths the length. Its lateral margins, in front of the mid- dle, are each finely serrated by six small, sharp, projecting points as in the type of the genus, excepting that they are sharper, and directed more oblique- ly forward. At each antero-lateral angle, there is also a considerably larger projecting point, forming a short spine, exactly as in the type of the genus, excepting that it is extended more nearly directly forward. The outer pair of antennae are moderately stout: each peduncle showing three joints, di- minishing rather gradually in size, the first longer than wide, and the other two apparently of nearly equal length and breadth, aud obliquely articulated. The flagellum is narrower at its base than the last joint of the peduncle, and composed of very short segments, which are scarcely more than one third as long as wide. The entire length of the antennas cannot be determined, as neither flagellum is entire in the specimen examined, but as the portion re- maining tapers very gradually, they were probably rather long. They are both, in the specinu-D examined, deflected abruptly outwards, nearly at right angles to the longer diameter of the carapace, which would seem from the He not this a misprint of the word appendage t [Mar. NATURAL SCIENCES OP PHILADELPHIA. 51 oblique articulation of the second and third joints of the peduncles, to be their natural position. (Inner antennae unknown.) Immediately between the bases of the two outer antennae, the specimen shows what appear to be impressions of the two globose eyes, which with their peduncles extend forward about two-thirds as far as the peduncles of the antennre. These may possibly be the peduncles of the inner antennae; but they look very much like globular eyes, on more slender peduncles. The abdomen is more than half the length, and about two-thirds the breadth, of the widest part of the carapace. It shows five short segments, and apparently part of another, the first of which is a little smaller, and the second a little larger than the others. None of them, however, are more than one-fifth as long as the breadth of the abdomen. The caudal appendages being unfortunately bent down and crushed, it is not possible to make out the form of the telson or the details of the other parts, though the whole together seem to have been wider than the abdomen, and as wide as the carapace. No surface sculpturing can be clear- ly made out, though there is some appearance of a few irregular scattering granules near the margins of the carapace. (Other parts unknown ) Entire length, from the stalked eyes? to the extremity of the caudal ap- pendages, about 1-13 inches; length of carapace, 0-63 inch ; breadth of do. near the middle, 0-45 inch; at the extremities 0-31 inch; length of abdo- men, 0-30 inch ; breadth of do. near the middle, 0-26 inch. Length of pe- duncles of the antenna? 0-15 inch ; do. of eyes ? and their peduncles, 0-13 inch. It will be observed from the foregoing description that our specimen shows no traces of the central spine or beak, extending forward from the anterior extremity of the carapace, nor of the longitudinal carina connected with it, which constitutes such a marked feature in Anlhrapalsemon. It is possible, however, that this character may have been obliterated in breaking open the concretion, since our specimen only shows an impression of the under side of the carapace, while the appendage alluded to projects forward from the upper side, and may consequently be embedded in the other half of the concretion, which we have been unable to obtain. Still as it is possible that this appendage may be wauting in our fossil, we should not be sur- prised if it would prove to belong to an allied but distinct genus. Specifically at least, it differs from A. Grossartii, of Salter, in the propor- tionally much shorter joints of the flagella of its outer antennae, and the oblique articulations of the segments of their peduncles ; while the latter, as well as the surface of other parts, are without any traces of the fine pitting represented by Mr. Salter's figures. Our specimen also shows traces of what appear to be squarely truncated basal scales to the outer antennae, about as long as their first joints, while. Mr. Salter's figure (1), represents apparently a triangular scale over the left antenna. Length from the end of the caudal extremity, to the anterior margin of the carapace, 1 inch. Length of carapace, 060 inch; breadth of do. 0-43 inch. Length of abdomen, about 030 inch; breadth of do. 0-27 inch. Length of caudal appendages, 0-10 inch. MYRIAPODA. ? Genus ANTHRACERPES, Meek & Worthen. Anthracrrpes typus, M. & W. This genus and species are founded upon a slender worm-like fossil, the relations of which have not been very clearly determined. The specimen consists of a well defined mo^ld or impression left in a concretion, and meas- ures 1-50 inches in length, and about 0-09 inch in breadth, (height) as seen lying upon one side. It is regularly arched from end to end, so as to form about one-third of a circle of 0-65 inch radius. For most of its length, it is 1865.] 52 PROCEEDINGS OP THE ACADEMY OF of very uniform breadth or height, but it tapers very gradually towards what appears to be the posterior end, where the last segment terminates in three or four short, slender, spine-like appendages, directed backwards on a line with the general curve of the body. The other end being broken away in the only specimen yet known, the nature of the head and its appendages cannot be determined. The entire body is distinctly articulated, and shows clearly nineteen seg- ments, and part of another. The segments are of nearly uniform size, or only vary from 008 to 0-10 inch in length ; the last one, however, has only a breadth or height of about 0 03 inch, and the next about twice that. Cross- ing the segments near the upper side, may be seen in the mould an undefined furrow, (produced by a ridge in the fossil itself) which bends downwards and then up again as it passes across from side to side of each segment. Anteriorly it is less distinct and placed very near the dorsal margin, but in tracing it backwards it is found to descend and become more defined, until it reaches the fourth segment from the extremity ; on this it passes obliquely downward to its posterior inferior corner, so as not to be seen on any of the succeeding divisions behind. Below the middle of each segment, there is in the mould a small prominence, evidently marking the position of a corres- ponding pit in the fossil. These agree in position and appearance with the spiracles or breathing apertures in the Myriapoda. We have not been able to make otit very clearly, any indications of feet or other appendages ; though there is near the base of each segment of the mould, a short oblique impres- sion, that may possibly have been left by very small feeble legs folded back- wards. As this fossil shows too many segments for a larval insect, and has not the aspect of an Annelid, we are rather inclined to view it as a Myriapod. INSECTA. LEPIDOPTERA. Genus PALiEOCAMPA, Meek and Worthen. Paljeocampa anthrax, M. & W. The fossil for which the above generic name is proposed, is about 0-70 inch in length, and some 0*13 inch in breadth, exclusive of the projecting tufts of hairs. It is an arcuate, worm-like body, that has been divided or split lengthwise in breaking open the concretion in which it is enveloped ; so that it is only a longitudinal section we see in looking at either half of the con- cretion. At both extremities, and along the upper or convex side of the curve, we observe densely packed tufts or fascicles of hairs individually radi- ating, as if from small wart-like protuberances. These hairs are straight, and about 0-30 inch in length. At one extremity, which appears to be the anterior, two of the bundles of hairs are more radiating than the others, and directed forward. The bundles distributed over the curved or dorsal side are regularly arranged, and have each a general direction at right angles from the part of the arched side from which they spring. At the posterior ex- tremity there are also two tufts directed backwards, the individual hairs of which are less radiating than those at the other extremity. Between some of the bundles ranged along the upper side, some shorter tufts are seen, which appear as if they originate in another series of protuberances farther over on the other side embedded in the matrix. If we suppose each of these principal bundles along the curved side, and the two bundles at either end to each belong to a single segment, it would make about ten or eleven seg- ments to the entire body. The specimen is not in a condition to show the head or feet ; yet we are strongly inclined to believe from its form, and peculiar regularly arranged bundles of hairs, that it is a Caterpillar. If we are right in this suggestion, [Mar. NATURAL SCIENCES OP PHILADELPHIA. 53 its discovery is certainly an interesting one, as it would present an evidence of the existence of Lepidopterous Insects, at a much earlier period in our world's history than has hitherto been suspected. As this fossil will doubtless be met with in the Coal Measures at other lo- calities, whether or not its connection with the mature Butterfly or Moth can ever be positively established, it seems desirable, for convenience of refer- ence, that it should receive a name ; although we are unable to point out any well defined characters from the only specimen seen, by which it can be distinguished from the larva of several existing types. That there is any probability, however, of its belonging to any existing genus, will, we think, not be maintained by any person familiar with the range of generic types in time. April 4:th. Vice-President, Cassin, in the Chair. Twentv-two members present. The following paper was presented and referred to a Committee : " Diagnoses Specierum et varietatum novarum Molluscorum," etc. By Philip P. Carpenter. JlprilWth. The President, Dr. Bridges, in the Chair. Twenty-five members present. The following were presented and referred to a Committee : " Synopsis of the genus Pomoxys," " On the genus Caulolatilus," " Oo the cranial characteristics of Gadus proximus," and " Note on several genera of Cyprinoids." By Theo. Gill. The Curators exhibited a large living specimen of the Great Crab- Spider, Mygale cancerides, recently brought from Brazil, and presented by Mr. Newton. The Secretary announced the death, on the 30th ult., of Major Charles I. Maceuen, late a member of the Academy. April \%th. The President, Dr. Bridges, in the Chair. Twenty members present. The following papers were presented and referred to Committees : " Observations on the Eocene Lignite Formation of the United States," and " Catalogue of the Eocene Annelides, etc." By T. A. Conrad. " Descriptions of three new species of Exotic Uniones." By Isaac Lea. The Secretary read the following : 1865.] 54 PROCEEDINGS OP THE ACADEMY OF Extract from the last Will and Testament of Thomas B. Wilson, deceased, late of Newark, State of Delaware, and on record in the Register's Office, New- castle, Delaware. " I will and bequeath to the Academy of Natural Sciences, of Philadelphia, my collection of Birds and all my other specimens of Natural History deposited by me in the hall or building of the said Academy of Natural Sciences, on Broad street, Philadelphia. And I further give and bequeath to the said Academy of Natural Sciences of Philadelphia, the sum of Ten Thousand dollars, to be by them invested in some safe and productive fund, and as often as it may be necessary to change the said investment, to re-invest the said sum in like manner ; which fund shall be called the Library Fund, and the income therefrom shall be exclusively appropriated to the purposes, preservation and income of the Library of the said Academy, in the following manner : Three hundred dollars of the yearly income arising therefrom, I direct to be paid as a yearly salary to a Librarian, to be appointed by the said Academy, whose duties shall be by them fixed and determined ; and the residue of the yearly income arising from the said fund I direct to be applied, firstly, to the con- tinuance, by purchase, of such works published periodically or in numbers as are now contained in and belonging to the Library of the said Academy. And, secondly, to the purchase and procuring of such works relating to Natural History as may be designated and selected by the said Librarian and the Li- brary Committee of the said Academy jointly." The said Will is dated the seventeenth day of March, Anno Domini, one thousand eight hundred and fifty-four, (1854.) Attest, Rathmell Wilson, Surviving Executor. April 2hth. The President, Dr. Bridges, in the Chair. Eighteen members present. On the favorable report of the respective Committees, the following papers were ordered to be published : Diagnoses Speciemm et "Varietatum novarum MOLTTSCORTJM, prope Sinum Pugetianum a Ktmuerlio Doctore, nuper decesso, collectoium. SCRIBEBAT PHILIP P. CARPENTER, B.A., PH.D. Academiae Alumnus Corresponded. SfliENIA OVOIDKA, n. S. S. t. parva,, albida., ovoidea ; epidermide cinerea, parum rugosa, induta ; marginibus, antico et ventrali regulariter excurvatis ; dorsalibus rectis ad angulum circiter 150° ; parte postica angustiore, obtuse angulata, parum trun- cata ; umbonibus prominentibus, circiter ad duas inter quinque partes totius longitudinis sitis ; intus, lamina cartilaginea lata, parum extante ; sinu pallii ovali, usque ad medium interstitii porrecto. Long. -3, lat. -16, alt. -02, poll. Hab. — In sinu Pugetiano specimen unicum piscavit Kennerley. A "Sph. ?Binghami" Searles Wood Crag Moll., vix differt. NejEra pectinata, n. s. N.t. globosa, albida, subdiaphana ; epidermide tenui induta; ventraliter antice products, postice subito angustato, rostrato ; rostro haud insculpto, duabus inter quinque partes totius longitudinis sequante ; parte globosa acute costata ; costis posticis paullum majoribus, magis distantibus ; margines dor- [April, NATURAL SCIENCES OP PHILADELPHIA. 55 sales versus obsoletis ; interstitiis latis, quadratis, minutissime concentrice striatis bus, umboL viculato ; cicatricibus adductoribus subrotundatis, deorsum sitia ; siuu pallii parvo, lato : margine a costis pectinate Long. -24, lat. -14, alt. -12. Hab. — In sinu Pugetiano specimen junior legit Kennerley. Apud iusulam Catalinam et Sanct. Barbaram adultum piscavit Cooper. Genus PANDORA. Subgenus Kennerlia. Testa Pandoris veris siraillima ; cartilago ossiculam gerens ; ligamentum elongatum. tenuissimum; lamina externa prismatica valva, planata plerum- que radiatim sulcata ; cardo simplex ; linea pallii baud sinuata. Ex. — Kennerlia filosa. ■ Kennerlia bicarinata. [?An P. biliratx, Conr., sequalis.] Kennerlia glacialis. Kennerlia filosa, n. s. K. t. tenui, planoconvexa, maxime rostrata, ; marginibus dorsalibus rectis, ad angulum circ. 160°; ventrali regulariter et modice excurvato, postice vix sinuato ; epidermide olivacea, plerumque erosa, postice corrugata ; lamina externa prismatica spongiosa, valva, planata radiatim sulcata, (quasi filosa,,) sulcis distantibus ; valva convexa costa, obtussissima, postice decurrente ; lineis seu undis incrementi conspicuis : intus, dente cardinali uno, parvo, extante ; callositate claviculoidea antica, margini contigua, ; fossa cartilagi- nali postice sita; cicatricibus adductoribus rotundatis, margini dorsali con- tiguis; linea, pallii simplici. Long. -8, lat. -4, alt. -12. Hab. — In sinu Pugctiano satis rare piscavit Kennerley. PSAMMOBIA RDBRORADIATA, (Nutt. MS.) Ps. t. seu omnino lilacina, seu albida, lilacino plus minusve radiata ; mag- na, solida, lata, subrequilaterali, haud planata, rugis incrementi irregularibus instructa ; epidermide olivacea induta; marginibus, dorsalibus antice et pos- tice rectis, ad angulum 160°, umbonibus prominentibus, obtusis ; ventrali subplanato, antico rotundato, postico subquadrato : intus, albida ; dentibus cardinalibus utraque valva duobus, parvis ; nymphis planatis, latioribus, ligamento extante ; cicatricibus adductoribus, antico ovali, postico rotundato ; sinu pallii subquadrata, usque ad medium porrecta,, a margine ventrali linea solum separata ; costis duaous ab umbonibus ad marginem internum cica- tricum diagonaliter decurrentibus. = " Sanguinolaria rubro-radiata, Conr." [?ubi] Nutt. MS. ; B. A. Rep., p. 195. Macoma yoldiformis, n. s. M. t. parva, valde transversa, subplanata, yoldiformi ; alba, tenui, subdia- phana, politissima, ; epidermide nitente, pallide straminea induta ; lineis in- crementi, postice conspicuis, exceptis, lsevi ; parum ina?quilaterali, umbonibus postice intiectis ; marginibus undique (regione ligamenti excepta) regulariter excurva'is: intus, nympba, ligamentali concava, subcelata ; postice secta, dein parum alata ; dentibus cardinalibus valva sinistrali ii., quorum unus bifidus ; margine dorsali antico excurvato ; sinu pallii obscure triangulato, paullo plus quam duns trientes interstitii inter cicatrices adductores minores porrecto. Long. -68, lat. -4, alt. *15. Eab. — In Pacifico Boreali primum piscavit Belcher: dein valvas duas in sinu Pugetiano, Kennerley : postea prope San Diegonem, Cooper : rarissime. 1865.] 56 PROCEEDINGS OF THE ACADEMY OF Macoma (Ivar.) expansa. M. t. " M. prozimse" simili, sed majore, multo tenuiore ; antice minus, pos- tice plus expansa, regulariter excurvata ; t. jun. subdiaphana, subepidermi- dem tenuem, stramineam, subnacrea; t. adulta alba, nitida ; dentibus cardi- nalibus ii. — i. minimis, haud bifidis ; sinu palii valva altera per tres quad- rantes, altera per quinque inter septem partes interstitii porrecto. Long. 1-55, lat. 1-13, alt. -5. Mai. — In sinu Pugetiano rarissime legit Kennerley. A "M. laid, Gmel." Desh. MS. in Mus. Brit, vix differt, specimine Grcen- landico ; sed M. latse et calcane in Mus. Cumingiano textura et dentibus haud convenit. Species quaedam hujusce formse, extus similiores, intus dentibus et sinu pallii satis differunt. (Tellina) Angulus modestus, n. s. A. t. "A. tenero," Sayii simillima ; sed callositate conspicua interna antica ab umbonibus deeurrente, sinum pallii et cicatricem adductorem utrdque valva, separante ; parva, subdiaphana, nitidissima, donaciformi ; epidermide cornea tenuissima, striulis incrementi, plus minusve conspicuis, induta ; margine antico dorsali subplanato ; umbonibus extantibus ; area postica truncata, haud acute definita ; margine ventrali subplanata : intus, dentibus cardinalibus utraque valva ii., quorum alternati bifidi ; valva sinistrali lat. antico curto, extante, contiguo, posticis nullis ; sinu pallii usque ad callosi- tatem porrecto ; nymphis paullum concavis. Long. *36, lat. -22, alt. -08. Hub. — In sinu Pugetiano, specimina duo juniora legit Kennerley. Anqulus modestos, var. obtusus. A. t. "A. modesto" simili ; sed majore, umbonibus obtusis, vix donaciformi, marginibus dorsalibus et ventrali excurvatis ; candidiore, vix diaphana; epi- dermide pallidissime straminea. Long. -72, lat. -44, alt. "15. Hab. — In sinu Pugetiano legit Kennerley ; apud "Neah Bay," Swan ; prope S. Pedro, Cooper. ?Clementia subdiaphana, n. s. ?C. t. ovali, quoad genus valde transversa, tumida, tenuissima; pallide cinerea, epidermide pallide straminea; subdiaphana, sed subcalcarea, haud porcellana ; laevi, nisi striis incrementi ; haud lunulata, umbouibus satis pro- minentibus : intus, valva dextra, dentibus anticis duobus acutis, contiguis, elevatis, postico elongato, acuto, bifido, ligamento parallelo ; valva sinistra dentibus anticis duobus, umbonem versus junctis, acutis, divergentibus, postico elongato, acuto, simplici ; sinu pallii, ut in Dosinia, angusto, angu- lato, per dimidium interstitii umbones versus porrecto. Long. -72, lat. -58, alt. -34. Genus PSEPHIS * Animal Veneri simile, sed viviparum. Testa inter Pacbydesma et Circem intermedia; lasvis, seu concentrice sculpta, nitida ; cardine dentibus iii. — iii. variantibus, quorum anticus saepe porrectus ; marginibus haud crenulatis, dorsali intus sulcato ; sinu pallii parvo, lato, interdum obsoleto ; ligamento tenui, umbones obtusus circum- eunte. * Th. 4«^*C) » calculus. [April, NATURAL SCIENCES OP PHILADELPHIA. 57 Exeinplum typicum : Psephis Lordi == Chione Lordi, Baird, Proc. Zool. Soc, 1863, p. 69. Hab. — In sinu Pugetiano primum legit Kennerley : postea, in insula Van- cover legit Lord : in insula Catalina, Cooper. Venus Kennerleyi, n. s. V. t. ovali, solida, calcarea, squalide alba ; marginibus sequaliter excur- vatis ; valde inaequilaterali, haud tumida, ; rugis concentricis, validis, crebris, irregularibus, haud acutis, instructa ; interstitiis concentrice striatis, (t. juniore suborbiculari, striis radiantibus ornata ;) lunula lineis impressis definita, rugis appressis instructa; area, haud definita; intus, dentibus utra- que valva, iii., quorum altera i. altera ii. plus minusve bifidis ; fulchro valido ; cicatricibus muscularibus validis ; sinu pallii parvo, anguste angulato ; mar- ginibus tenuiter crenulatis. Long. 2-5, lat. 1*8, alt. 1-25. Hab. — In sinu Pugetiano legit Kennerley: testas juniores, "V. astartese" Midd. similes, legerunt juxta Neeah Bay, Swannii Indianuli. ASTARTE (? COMPRESSA, VCir.) COMPACTA. A. t. " A. compressse" simili, sed compacta, minus transversa ; liris concen- tricis expressis, paucioribus, marginem posticam versus obsoletis ; umboni- bus valde prominentibus, acutioribus ; marginibus dorsalibus rectis, ad angulum 100° ; lunula minus impressa, longiore ; area ligamentali minus angulata ; dente laterali antico valva dextra magis extante. Long. -4, lat. •33, div. -21. Hab. — In sinu Pugetiano specimen unicum piscavit Kennerley. LUCINA TENUISCULPTA, n. S. L. t. UL. Mazatlanicse" forma, simili ; sed magis convexa, sculptura multo tenuiore ; epidermide olivaceo-cinerea induta; t. juniore lam ; postea, rugis incrementi concentricis, plus minusve conspicuis, distantibus, irregularibus ; costulis radiantibus subobsoletis, latis, crebrioribus, antice et postice evani- dis ; area postica vix subquadrata, haud definita : intus, dentibus cardinali- bus et lateralibus normahbus, satis extantibus ; ligamento externo, elongato ; cicatrice antica normaliter prolongate ; margine crenulato. Long. -23, lat. •21, alt. -13. Hab. — In sinu Pugetiano legit Kennerley. Cryptodon serricatus, n.s. C. t. parva, subplanata, subcirculari, tenui, alba, haud flexuosa ; epider- mide tenuissima, vix straminea, serricata, induta ; laevi, seu lineis incrementi vix ornata, nitente ; suborbiculari, seu ventraliter producta ; marginibus undique valde et regulariter rotundatis, regione lunulari incurvata ; utnbo- nibus antice hamatis ; lunula planata, haud exacte definita : intus, ligamento tenui, omnino celato ; dentibus cardinalibus in utraque valva uno, extante, lateribus nullis ; cicatricibus adductoribus subovalibus, haud prolongatis ; linea. pallii a margine haud crenato satis remota. Long. *16, lat. -18, alt. *1. Hab. — In sinu Pugetiano legit Kennerley : in insula Vancouver, Swannii Indianuli. Pythina rugifera, n. s. P. t. majore, tenuissima, valde transversa, subquadrata, vix inaequilaterali; lineis incrementi et epidermide rugosa, confertissime laminata, ornata ; um- bonibus latis, valde prominentibus, antice flutentibus ; marginibus, dorsali- bus satis regulariter excurvatis, regione postica paulum majore ; ventrali planato, seu medio concavo : intus, cardine maxime delicatulo ; dente cardi- 1865.] 58 PROCEEDINGS OP THE ACADEMY OP nali uno minore, clavicula antica laterali inconspicua ; laterali postico nullo. Long. 77, lat. -44, alt. -3. Ilab. — la sinu Pugetiano specimina duo, (quorum unum fractum,) piscavit Kennerley. Inter Pythinas typicas et Kellias locum tenet. Tellimya tumida, n. s. T. t. subtriangulari, subovata, laevi, solidiore, tumidiore, valde inequilate- ral i ; cinerea, epidermide pallide olivacea, concentrice striata induta ; mar- ginibus dorsalibus subrectis, ventrali excurvato : intus, dentibus cardinalibus valva, sinistra validissimis, curtis, extantibus, postico longiore ; valva dextra callositatibus marginalibus, dentibus nullis ; cartilagine validiore, ossiculum parvum in medio gerente ; cicatricibus adductoribus a cardine valde remotis. Long. -155, lat. -125, alt. -06. Hab. — In sinu Pugetiano specimen unicum legit Kennerley; apud Neeah Bay, Swan ; prope San Diegonem, Cooper. Lkda fossa, Baird. L. t. UL. minutse" simili; sed parte antica minore ; postica magis porrecta, angustiore ; umbonibus parvis, valde prominentibus ; lirulis concentricis crebris, haud expressis, postice et testa adulta. ventrUiter omnino obsoletis ; regione siphonali haud lirata, obtuse biangulata, angulis contiguis, subno- dosis ; regionibus dorsalibus utroque latere laevibus ; parte antica sulco radiante obsoleto definita, liris illuc interdum interruptis : intus, dentibus cardinalibus utroque latere xiv., posticis magis elongatis ; sinu pallii minimo. Hab. — In sinu Pugetiano specimen unicum legit Kennerley : in porto Es- quimalto, idem, Lyall. Proc. Zool. Soc, 1863, p. 71. = L./oveata, Baird MS., in Mus. Brit. Pecten {?var.) Hindsii. P. t. "P. hastati" varietatibus simili, sed latiore ; radiis multo crebriori- bus, aequalibus, laevioribus, minoribus, ventraliter bifurcantibus ; interstitiis latis, minutissime granulosis ; intus albida,. Long. 1-6, lat. 1-7, alt. -57. Hab. — In sinu Pugetiano juniorem legit U. S. E. E., adultum Kennerley: in insula Vancouver legit Lord. = P. Fabricii, Gld. in B. A. Rep., p. 211, (non Phil. = P. islandicus, jun.) Tornatina exima, Baird. T. t. cylindracea, majore, laevi, pallide albolutescente ; epidermide strami- nea, spiraliter tenuissime striulata, induta ; spira saepius erosa; suturis an- gustis, acutissime canaliculars ; labro acuto, antice sinuato, medio porrecto, postice exciso, supra suturam valde et acute elevato ; apertura, antice valde elongata.; columella valde excavaia, antrorsura labrum versus arcuata. ; labio tenui; plica, angustissima, obsoleta, parieti appressa. Long. -26, lat. -12. Hab. — In sinu Pugetiano primum legit Kennerley : postea in insula Van- couver legit Lord. Speciminibus typicis comparitis, conchilias Kennerlianas Dullinx eximue, Bairdj in Proc. Zool. Soc, 1863, p. 67, conspecificas esse certissime constat. Cylichna (?cymndkacea, var.) attonsa. C. t. " C. cylindracese" aliter simillima; sed postice rotundata, haud um- bilicata, vix lacunata, labro regulariter incurvato. Long. -38, lat. -15. Hab.— In sinu Pugetiano specimen unicum legit Kennerley. Specimina Californica, a Jewett Cooperque collecta, C. cylindracese typicoa magis conveniunt. [April, NATURAL SCIENCES OP PHILADELPHIA. 59 Dentalium rectids, n. s. D. t. valde elongata, valde tereti, lentissime augente, vix arcuata ; laevi, tenuiore, albida, subdiaphana, valde nitente ; aperturam versus tenuissima. Long. 1-9, lat. -13. Hab. — In sinu Pugetiano legit Kennerley. Varina D. eburneo, Singaporensi, convenit ; sed annulis falacibus caren, textura, valde differt. Mopalia Kennerleyi, n. s. M. t. UM. muscoso" formd, indole, sculpturaque simili ; sed multo magis elevata ; plus minusve rubente, plus minusve olivaceo variegata, intus pal- lida ; granis lateralibus fere aequalibus ; liris centralibus haud acutis, inter- stitiis rarius cancellatis ; suturis undatis, apicibus valvaruni prominentibus ; valva antica octoradiata, radiis granulosis, margine octies inciso ; valvis intermediis utraque semel incisis ; valva postica mucrone obsoleto, sinu pos- tico alto, angustiore, marginibus anticis valde alatis, lateribus posticis semel ineisis. Sab.— In sinu Pugetiano : sp. unicum legit Kennerley. ?M0PAHA SIN0ATA, n. S. ?M. t. parva, subelongata, elevata, jugo angulato ; rubido et cajruleo ele- ganter maculata,; valvis' elongatis, subquadratis ; areis lateralibus costa, an- gusta, subelevata,, granulosa, utraque defiuiiis; suturis quoque granulosis; tota, superfice clarissime reticulata, punctis areis centralibus valde, areis late- ralibus et valvis terminalibus modice impressis ; valvis terminalibus ut in areis lateralibus sculptis, costis acutis radiantibus, interstitiis reticulars ; valva postica maxime incisa, sinu alto, acuto mucronem tenus haud con- spicuam effossa : intus rosacea; marginibus apicinis granulosis tota longi- tudine intortis ; sinu laminarum sadiralium parvo, angusto ; laminis externis, valvis centralibus semel incisis ; valva antica, fissuris circiter viii., costis convenientibus ; valva postica, fissura laterali utraque costae conveniente, postice maxime sinuata: limbo pallii coriaceo, pilulis paucis ; poro rotun- dato parvo suturis utroque latere conveniente. Hab. — In sinu Pugetiano specimina duo legit Kennerley. Mopaliis typicus structura valvae posticae convenit : poris suturalibus vix definitis, difiert. 7MOPALIA IMPORCATA, n. S. ?M. t. parva, valde elevata, satis elongata ; jugo acuto, rectangulato ; pal- lida, rufotincta ; areis lateralibus, costa elevata, dense granulosa, definitis ; suturis dense granosis, marginibus intus implicatis ; valva antica circiter octies granoso-costata ; arearum lateralium et valvse anticas interstitiis intri- catim ruguloso-indentatis ; areis centralibus costis longitudinalibus crebris, validissimis, acutis, subparallelis, interstitiis crenulato-decussatis ; valva, pos- tica mucrone haud conspicuo, submarginali, sinu parvo, angusto : intus, sinu laminarum suturalium angusto : valvis centralibus fissura una ; valva, antica fissuris ? — ; valva, postica fissura utraque una, postice sinu parvo, angulato : limbo coriaceo, poris suturalibus aliisque hue et illuc sparsis, minutis, setulis albidis instructis. Hab. — In sinu Pugetiano specimina duo legit Kennerley. Ut in ?M. sinuata, a Mopaliis typicis difiert. Ischnochtton (Trachydermon) retiporosus, n. s. I. t. parva, subelongata, cinerea, valde elevata, jugo arcuato ; valvis sub- quadratis, apicibus celatis, marginibus suturalibus intus reglicatis ; areis lateralibus parum definitis, costulis iii. — vi. obsoletis, rotundatis, hue et 1865.] 60 PROCEEDINGS OF THE ACADEMY OP llluc grams acutis, expressis, instructis; areis centralibus omnino scrobicu- latis, interstitiis parvis, alte punctatis ; valvis terminalibus costulis crebris, angustis, acutioribus; mucrone parum eonspicuo, antrorsum sito : intus, sinu suturali lato ; laminis, utroque latere semel, valvis terminalibus circ. xn. incisis : limbo pallii graauloso, graaulis confertis, minimis, vix elon^atis, vix regularibus, haud sculptis. Long. -44, lat. -28, div. 90°. Hab. — In sinu Pugetiano specimen unicum legit Kennerley. Forma 1. interscincto, Gld. et /. scrobkulato, Midd. convenit ; indole sculp- ture differt. r Ischnochiton (Trachtdermon) trifidis, n. s. I. t. elevata,, ovali, rubida ; valvis latis, subquadratis, apicibus vix intortis ; are is lateralibus subelevatis, costis obsoletis rotundatis ii.— iv.; areis cen- tralibus punctis distantibus, valde impressis ; valvis terminalibus ut in areis lateralibus costatis ; valva postica mucrone submediana, haud elevata : intus albida, subrosacea; valvis utraque latere maculo aurantio elongato ornatis, sinuibus centralibus parvis, expansis ; marginibus externis subgrunda typice obtectis; laminis lateralibus bis, terminalibus circiter xii. incisis: limbo palln, granuloso, granis ovalibus, vix imbricatis haud striatis. Lone:. -75, lat. -45, div. 110°. 5 ' Bab. — In sinu Pugetiano specimen unicum piscavit Kennerley. Ischnochiton (Trachydermon) pseudodentiens, ? n. s. I. t. parva, ovata, subelevata, jugo angulato ; cinerea, olivaceo eleganter maculata, suturis albido et fusco-olivaceo haud regulariter tessellatis ; areis lateralibus haud valde definitis ; totasuperficie gran-ulis creberrimis instructa ; apicibus valvarum distinctis ; mucrone eonspicuo, submediano : intus, sinu suturali lato, medio planato : subgrundis parvis, haud extantibus, subspon- giosis ; laminis lateralibus unofissatis ; terminalibus quoad xi., valde obtusis : limbo pallii minute granuloso, granis laevibus, confertis. subovalibus. Lone1. •44, lat. -24, div. 110°. & Hab.— In sinu Pugetiano legerunt primum Expeditio Explorans, demum Kennerley : in insula Vancouver legit Lord: apud San Diegonem legit Cooper. Specimini typicali " Ch. denlientis, Gouldii" convenit: a diagnosi et figura, haud dentiens, differt. Ischnochiton (Trachydermon) flectens, n. s. I. t. parva, subelongata, rosea, elevata ; jugo acuto ; areis lateralibus vix definitis ; marginibus valvarum excurvatis, suturis incurvatis, apicibus valde prominentibus ; valvis granulis miautis, haud crebris, subradiatim sparsis, omniuoque minutissime punctulatis ; mucrone eonspicuo, antico : intus, sinu suturali lato, planato ; subgrundis haud porrectis ; laminis lateralibus uno- terminalibus quoad xi.-fissatis : limbo pallii vix minutissime granulate Long. -35, lat. -24, div. 110°. Hab. — In sinu Pugetiano legit Kennerley: in insula Vancouver legit Lord: prope Monterey, Taylor : apud San Diegonem, Cooper. Lepeta CjECOIdes, n. s. L. t. " L. csecse " simili ; t. alba, ancyloidea, tenui, juniore subdiaphana ; apice obtuso, antice verso; parte postica parum excurvatd; lateribus haud compressis ; margine regulariter ovato ; tota superficie sub lente minutissime striata, striulis valde distantibus, haud elevatis, haud granulatis, subobsoletis ; ci- catrice musculari haud impressa. Long. (t. adolesc.) -45, lat. -37, alt. -19 (speciminis multo majoris pars solum superest : long. -94, lat. -73, alt. -55.) div. 90°. Hab. — Specimina juniora perpauca viventia in sinu Pugetiano piscavit Kennerley: ex insulis Farallonibus adulta affertur, teste Darbishire. [April, NATURAL SCIENCES OP PHILADELPHIA. 61 Calliostoma (?var.) variegatcm. C. t. parva, conica, variegata ; nucleo rosacco ; anfr. vi. planatis, suturis haud iinpressis ; costulis in spira. iii. regularibus, nodulosis ; nodulis albidis, subdistantibus ; interstitiis elegantissinie rosaceis ; lirulis basalibus viii. haud nodulosis, rosaceo maculatis. Long. -24, long. spir. -13, lat. -21, div. 50°. Hab. — Puget Sd., sp. un. legit Kennerley. This may prove to be an extreme variety of Cal. annulatum, Martyn. Margarita (?wz?\)tenuisculpta. M. t. " M. Vahlii" forma, colore, et operculo simillima; sed striulis spirali- bus, plus minusve obsoletis cincta,, quarum iv.-vi. in spira, monstrantur. Long. -22, long, spir. -11, lat. -13, div. 70°. Hab. — Puget Sd., Kennerley. Neeah Bay, Swan. Except in the very faint spiral sculpture, which does not always appear a constant character in Margaritas (v. M. undulata in Fbs. and Hani. Br. Moll.,) these shells might stand for M. Vahlii, a ? variety of which was found spar- ingly by Dr. Kennerley. They are sometimes painted with infrasutural flam- mules of darker ash. Both the smooth and the striated forms have a promi- nent spiral rib on the whorls of the operculum. Margarita lirulata, n. s. M. t. parva, cineracea, tenui, tumentiore, nacreo rosaceo ; anfr. v. plerumque subdepressis, suturis distinctis : interdum purpureo-fusco pallide maculata ; lirulis acutfs spiralibus haud elevatis, supra valde distantibus, in spira ii., circa basim rotundatum circ. viii. ; apertura subquadratu ; umbilico magno, infundibuliformi,angulato ; interstitiis lirularum laevibus, seu ab incrementi9 epidermidis decussatis : operculo tenuissimo, pallido, subplanato, suturis dis- tinctis. Long. -18, long. spir. '07, lat. -2, div. 80°. Hab. — Puget Sd., Kennerley. ? Var. a. subelevata ; t. elatiore ; colore livido, intensiore ; lirulis vix acutis. Bab.— Puget Sd., Kennerley. Neeah Bay, Swan. ? Var. p. obsoleta ; t. ut in 1 \&v . subelevata ; lirulis evanescentibus ; oper- culo planato, tenuissimo, suturis indistinctis. Hab. — Neeah Bay, Swan. ? Var. y. conica ; t. valde elevata ; lirulis acutis, aliis interdum intercalan- tibus ; umbilico parvo. Long. -33, long. spir. -2, lat. -25, div. 58°. Hab. — Puget Sd., Kennerley, sp. un. The shells above described constitute what might be called a Darwinian group of specific forms. With the exception of the typical shells dredged by Dr. Kennerley, they are all in very bad condition. The Pugetian speci- mens are flattened, with open umbilicus, as might be expected from quiet water. Two specimens, however, form an exact transition to the Neeah Bay shells, of which a fair number (var. a) were sent by Mr. Swan, though worn and generally decorticated. They are more elevated, with fainter sculpture ; and pass, by insensible gradations, into M. tenuisculpta, the two principal spiral lines becoming evanescent, and a few others intercalating. In this state (var. /?) the species can only be separated by the operculum, which is pale and thin, and destitute of the strongly expressed rib of the 'Vahlii' group. A third form (var. y) would certainly claim specific rank, but for the intermediate series of a. and /?. The diagnostic characters for the whole se- ries are the smooth operculum, the eight narrow riblets round the base, with angular umbilicus and the sharp, narrow, principal riblets above, with wide interspaces, smooth except from the lines of growth, which are principally 1865.] 62 PROCEEDINGS OP THE ACADEMY OP visible in the epidermis. There may be three (so-called) species in the group, viz. : lirulata, subelevata and conica. Margarita inflata. M. t. tumida, tenui, albida,, narceo pallide aureo ; anfr. vi. valde inflatis, suturis ad angulum fere rectum impressis ; tota superficie tenuissime spira- liter lirulata; lirulis acutis, haud elevatis ; in spira, circ. viii., minoribus sa?pe intercalantibus ; interstitiis a lineis increinenti extantibus creberrimis tenu- issime decussatis ; basi obtuse subangulata, striis creberrimis circ. xx. orna- ta; apertura. subquadrata ; columella arcuata ; umbilico infundibuliformi, laevi, angulato : operculo tenui, planato, suturis distinctis. Long. -44, long, spir. -22, lat. -45, div. 85°. Eab. — Puget Sd., Kennerley. Vancouver, Lyall. Neeah Bay, Swan. Only two adult specimens of this remarkably elegant species have been seen. It resembles the sbell from Greenland called M. striata, Brod. and Sby., in the British Museum, but that under the same name from Behring Straits appears distinct. In many respects it is like M. undulata, but differs in the greater swelling of the whorls meeting at a nearly rectangular suture, in the far more delicate sculpture without waves the keeling of the umbilicus and the bend in the pillar which causes a slight spiral hollow inside the umbilical rib. Mesalia lacteola, ? n. s. M. t. parva., tereti, tenui, albida ; epidermide tenui, flavidii, induta ; anfr. x. rotuudatis, suturis valde impressis, lcevious ; costis circ. xii. radiantibus, tumentibus, suturam versus evanidis, interstitiis parvis ; costis spiralibus ro- tundatis, costas radiantes transeuntibus, supra spiram iii. validioribus, aliis interdum intercalantibus ; costulis suturalibus parvis, antice ii. ; basi rotun- data, vix striata ; columella recta, paullum effusa ; labro tenuissimo, parum arcuato. Long. -33, long. spir. -24, lat. -14, div. 30°. Eab. — In sinu Pugetiano legit Kennerley. In insula Vancouver legit Forbes. Anne " M. lactelce" varietas insignis, sculpturae indole satis discrepans. Mesaua (? lacteola, var.) subplanata. M. t. " M. lacteolm" simili ; sed sculptura minus extante anfractibus 3ub- planatis ; costis radiantibus pluribus minoribus, costulis spiralibus interdum intercalantibus, aperturam versus saepe obsoletis. JJab. — In sinu Pugetiano specimina viventia sed maxime erosa legit Ken- nerley: juxta "Neeah Bay" legerunt Indianuli, Swannii discipuli. Rissoa compacta, n. s. R. t. parva, rufofusca, haud turrita, compacta, marginibus spirae excurva- tis ; anfr. nucleosis iii. globosis, lsevibus, apice mamillato ; normalibus iii. subplanatis, latis ; lirulis spiralibus obtusis circiter xv., quarum circ. vi. in spira. monstrantur, interstitiis vix aequantibus ; lirulis radiantibus circ. xxx., peripheriam tenus evanidis, anfractibus primis superantibus, anfractu ultimo Bfepe obsoletis ; basi rotundata, haud (nisi testa juniore) umbilicata ; aper- tura suborbiculari, peritremati continuo ; operculo tenui, paucispirali, rapid- issime augente. Long. -06, long. spir. -04, lat. -045, div. 45°. Eab. — In sinu Pugetiano satis abundanter legit Kennerley ; prope Neeah Bay, Swannii discipuli. Drillia incisa, n. s. D. t. u D. inermi" forma et indole simili; sed cinerea, rufofusco copiose spiraliter lineata; anfr. nucleosis majoribus, subplanatis; anfr. normalibus vii. subplanatis, epiraliter subobsoletc ccelatis ; sulcis in spira circiter viii., quarum quarta radiatim sinuata ; canali quoad genus longiore, aperta ; co- [ April, NATURAL SCIENCES OF PHILADELPHIA. 63 lumella arcuata ; labio distincto ; labro tenui, parum sinuato ; epidermide subfugaci, laminis incrementi subrugosa, ; operculo pyriformi, haud angulato, apice antico. Long. 1-13, long. spir. -65, lat. -4, div. 30°. Hab. — la sinu Pugetiano legit Kennerley: prope " Neeah Bay" legerunt Swannii Indianuli. A Drilliis typicis sinu minimo et operculo haud angulato conspicue differt : Clionellae, Grayi, magis convenit. Drilua cancellata, ?n. s. D. t. " D. incisse juniore" siruili, sed omnino albido, sculptura elevata, haud coelata epidermide tenui; anfr. nucleosis ? [detritis ;] normalibus iv. planatis, suturis distinctis; costulis radiantibus circ. xx. angustis, acuti- oribus, et costulis spiralibus subaequantibus, quarum circiter v. in spira, monstrantur, eleganter cancellatis, ad intersectiones subnodulosis ; apertura obovali, in canalem longiorem, subarcuatam, apertam, producta ; labro acuto, medio producto, ad costulam spiralem ex sutura tertiam eleganter sinuato, sinu altiore. Hab. — In sinu Pugetiano duo specimina legit Kennerley; quorum altero labium subcallosum, altero planatum. Mangelia levidensis, n. s. M. t. rudi, fusca, elatiore ; anfr. nucleosis iii. subelongatis, vertice haud mamillato ; anfr. normalibus vi.'subplanatis, suturis distinctis, quarum primi costis radiantibus circiter xii. latis, interstiiiis parvis, et costulis spiralibus crebrioribus, quarum v. magis insculptte supra costas transeunt, rude ornan- tur ; anfr. ultimis sculptura subobsoleta ; apertura elongata, subquadrata in canalem brevem arcuatim producta, intus hepatica; labro juxta suturam vix sinuato ; labio vix conspicuo. Long. -86, long. spir. -53, lat. -29, div. 27°. Hab. — In sinu Pugetiano legit Kennerley : prope " Neeah Bay " collegit, per Indianulos, Swan. A Mangeliis typicis columella torta differt. Bela exccrvata, ? n. s. B. t. " B. Trevzyliante" simili, sed alba, curtiore, marginibus spiraR valde excurvatis; anfr. nucleosis ? [erosis ;] dein iv. normalibus, subplanatis, fere rectangulatim prope suturas tabulatis ; costis obtusis radiautibus circiter xviii., medio anfractus et prope suturam obsoletis, postice retrorsum valde arcuatis ; sulcis spiralibus subdistantibus impressis, costas superautibus, in spira. circiter v., postice evanidis, antice crebrioribus ; aperatura longius ovali, antice brevissime canaliculato, postice aite sinuato; labro acuto, medio valde excurvato ; columella regione labii eroso. Long. -28, long. spir. -13, lat. -15, div. 55°. Hab. — In sinu Pugetiano ante decessum prematuram specimen unicum pis- cavit Kennerley, eheu deploratus ! EULIMA MICANS, ? n. S. E. t. u E. politce" simillima, sed minore ; anfr. nucleosis stylinis, apice sub- decliviter sito ; anfr. normalibus xii. omnino planatis, maxiine nitentibus, suturis nullis ; albida, rosaceo tincta ; basi arcuatim rotundata. ; apertura ovali; labro postice, et paullum antice sinuato, calloso ; labio calloso ; co- lumella, vix torta. Long. -52, long. spir. -3G, lat. -16, div. 25°. Hab. — la sinu Pugetiano specimen juniore legit Kennerley. Juxta Neeah Bay idem legerunt fiwannii Indianuli. Plurimos adultos viventes inter S. Pedronem et S. Diegonem, in insula quoque Catalinam piscavit Cooper. An Eu. politue varietas Pacinca ? 1865.] 64 PROCEEDINGS OP THE ACADEMY OP OCINEBRA INTERFOSSA. 0. t. satis elongata, purpureo-fusca, ; anfr. nucleosis ii., laevibus, elongatis ; anfr. normalibus v. convexis.suturis valde irapressis ; costis radiantibus sub- varicosis circ. xi., et spiralibus subaequantibus, quarum iii.-v. in spira, mon- strantur, decussata ; interstitiis altis, quadratis, laminulis incrementi, et in- terdurn costulis spiralibus obtusis intercalantibus, ssepe ornatis ; aperturd ovata, labro (t. adulta) iatus dentato ; canali satis longa, saspius clausa. Long. -85, long. spir. -4, lat. -45, div. 60°. Hab. — Neeah Bay, Swan: Vancouver, Lord, (named Fusus orpheus, as of Gld. in Br. Mus.) Variat. : t. atropurpured; costis spiralibus distantibus, in spira. duabus, foveis majoribus. Variat quoque t. albido zonata. 1 Chrysodomus rectirostris, n. s. ?Chr. t. parva, albida, carueo maculata, gracili epidermide tenui, cornea induta, ; anfr. nucleosis ? . . . [decollatis ;] anfr. normalibus vi. planatis, su- turis parum distinctis ; adolescente, costulis radiantibus circiter xiv. latis, haud expressis, adulta obsoletis ; lineis spiralibus baud conspicuis : apertura elongato-pyriformi, in canalem valde productum, apertum, rectum, subito attenuata; labro acuto, parum arcuato, haud sinuato ; labio inconspicuo. Long. -88, long. spir. -43, lat. -32, div. 33°. jjab — In sinu Pugetiano, specimen unicum legit Kennerley. Aspectu Belam, forma Perronam, nisi labro haud sinuato, commemorat : characteribus plurimis subgeneri Siphoni convcnit. Synopsis of the Genus POMOXYS, Raf. BY THEODORE GILL. In order to dissipate part of the confusion iDto which the nomenclature of this genus has fallen, and to make known several new species, the present article is submitted. Genus POMOXYS, (Raf.) I. Caudal peduncle with its height in front (-14) greater than its length (-11 — -12); anal fin extending back- wards nearly to base of caudal. P. brevicauda. II. Caudal peduncle longer (-13— -15) than high ('11— *13) ; anal fin not passing beyond the second third of pe- duncle. Height exceeding three-tenths ("31) of length ; head less than three-tenths (-24). P. intermedins. Height less than averaging three-tenths ('29) of length, and scarcely longer than head. Caudal peduncle slender ("15 long, '11J high). First dorsal spine less than half ("02^) an eye's diameter. P. storerius. Caudal peduncle stout, little longer than high (*13^ long, *13 high). First dorsal spine equal to two-thirds (04^) of an eye's diameter. P. protacanthus. POMOXYS BREVICAUDA, Gill. D. VI. 15. A. VI. 17. P. 15. (3 Scales (12—29-) 42 — .* 14 * The twelfth and twenty- ninth scales of the lateral line, respectively, correspond with the vertical of the anterior and posterior ends of the dorsal fin. The total number of scales through which the lateral line runs, exclusive of those on the caudal fin, is forty-two. At the region of great- est height, there are six rows above and fourteen below the lateral line. [April, NATURAL SCIENCES OF PHILADELPHIA. 65 This species is readily distinguished by its abbreviated caudal peduncle and the consequent extension of the anal fin backwards nearly to its end. The back is also considerably more gibbous and decurved than that of any con- gener. 4564. North Grand River, Livingston Co., Mo. Dr. Hoy. POMOXTS INTERMEDIUS Gill. D. VI. 15. A. VI. 17. 6 Scales (12—31—) 45 — . 14 This species distinguished by its comparatively longer caudal peduncle and the height of the body, as well as by the smaller size of the scales. POMOXTS STOREKIUS Gill. ?Pomoxis annularis Raf. f Ag. Cichla storeria Kirtland, MSS. Centrarchus hexacanthus Cuv. et Val., fide Storer (nee Cuv. et Val.) Pomoxis nitidus Girard. Centrarchus nitidus Giinther. D. VI. 15. A. VI. 17. P. 15. 6 Scales (14—30—) 43 — . 14 The Pomoxys storerius is remarkable among all its known congeners on ac- count of the slender caudal peduncle. The species has been quite unfortunate in its nomenclature. It is possible that it is the species described and figured (!) by Rafinesque, but it would be an act of injustice to any other naturalist to suppose that his figure could so disagree with nature as does that of Rafinesque with the species in question. Agassiz has adopted Rafinesque's name for a species found in the Tennessee River,* and, while he has remarked that it does not have the caudal ring mentioned by that author, has not alluded to any other disagreement with the fish of Rafinesque ; the normal inaccuracy of that man is, however, so well known, that Agassiz has doubtless considered it superfluous to allude to any such discrepancies, and, consequently nothing may be predicated from his silence on that subject. The species was first intelligibly noticed by Dr. Kirtland ; in the "Report on the Zoology of Ohio," p. 191, he introduced it under the name Cichla Sto- rsrin. Being subsequently informed by Dr. Storer " that Cuvier had pre- viously described it in the third volume of his " Histoire Naturelle des Pois- sons," from specimens taken by Lesueur in the river Wabash," he referred it to the latter species, called Centrarchus hexacanthus Val. The fishes of Kirtland and the French naturalists, not only belong to different species, but even to different genera. The name Cichla Storeria must therefore be ac- cepted as the specific appellation of the species described by Kirtland, if Ra- finesque's is deemed unworthy of adoption. Subsequently, the species was described and figured by Girard under the new name of Pomoxis nitida, while the name of Kirtland was retained as a synonym of the Centrarchus hexacanthus, which was erroneously called Pomoxis sparoides, and the name of Rafinesque was preserved for a third nominal species. * Agaspiz remarks, that the species of the Tennessee Kirer '-agrees fully with the description given hy Kafint-wjiu- of his Pomoxis annularis, with the sole exception of a golden ring at the base of the tail, which may be faded io the specimens sent by Dr. Newman from Huntsville ;" but this i agreement surely can scarcely extend to the figure, which remains unnoticed bv Agassiz. 1865.] 5 66 PROCEEDINGS OF THE ACADEMY OP POMOXYS PKOTACANTHUS Gill. D. VI. 15. A. VI. 17. 6 Scales (13—30—) 43—. 14 The Pomoxys protacanthtis may be at once distinguished among the other Bpecies here enumerated by the comparative elongation of the anterior dorsal and anal spines. A single specimen (4565), from Tarboro, North Carolina, is in the Smithsonian collection, and has no opercular spot. The absence of this latter furnishes another specific character, unless it has been obliterated by the alcohol. The following table gives the relative proportions of the several species : 4564 4563 4565 Extreme length 8£ 6| 6| C Body— Greatest height 35 31 29° 29 Heightof tail behind anal fin 14 12 11$ 13 Least height of tail 11$ 10 9* 10 Length of tail 11$ 13 15 13$ Head— Greatest length 31 29 29 28 Height at pupil 15.} 14 14 15 Length of snout 6} 6 6 6$ Orbit — Diameter 5.} 6 6 6 Dorsal— Length of base 27 25 24 24 Height at first spine 3 2} 2$ 4$ Height at last spine 11$ 13} 14 12 Height at longest ray 16 16 16 Anal— Height at first spine 4 2$ 2$ 3} Height at last spine 9$ 12 11 10" Caudal— Length of middle rays 17 18 17 19} Length of external rays 21 22 22 24 Pectoral— Length 16} 17 17 16 Ventral— Length 15 15 15 14 On the Genus CAULOLATILUS, BY THEODORE GILL. CAULOLATILUS Gill. *=CauloTatilas Gill, Proc. Academy of Natural Sciences, of Philadelphia, 1862, p. 340. Dekaya Cooper, Proc. California Academy of Natural Sciences, iii. p. 70, 1864. Latilus sp. Car. et Val. Body much compressed, elongated, with the height nearly uniform to the anus ; thence gradually decreasing to the caudal peduncle, which is moderately narrowed. Scales small, oblong, with a rather large central, minutely granular and estriate area, from the posterior portion of which the rhipidal ridges radiate ; and with a wiflo muricated posterior border ; the exposed surfaces are vertical, especially near the head. Lateral line indistinct, parallel with the back ; median on the caudal peduncle. Head compressed, scarcely oblong, with the profile boldly decurved, the forehead flattened. Forehead behind cheeks and opercula, except interoper- uilum, covered with ctenoid scales like those of the body. Eyes subcircular, large. Preorbital bone cUnyated rhomboid, with the height less than the di- [April, NATURAL SCIENCES OP PHILADELPHIA. 67 ameter of the eye ; cheeks longer than high. Nostrils approximated, simple. Pre.operculum esinuate, pectinated. Operculum with a blunt, bony projection behind. Suboperculum narrow. Mouth moderate, with the cleft little oblique. Jaws even ; sitpramaxillaries nearly straight behind, and subtruncated at end. Lips thick, the lower attached by a frsenum in front. Teeth on the jaws alone, in a broad, villiform band in front, preceded by a row of larger acute ones continued to the corners of the mouth ; the hindmost teeth enlarged canines directed forwards. Branchiostegal rays six. (Branchial membrane well developed, and free below.) Dorsal fin with seven or eight graduated, pungent spines, and rather nu- merous (22—27) uniform branched rays ; antepenultimate normally longest. Anal similar to^the soft dorsal, armed with one or two pungent spines ; first spine, when present, extremely small. Caudal fin emarginated, with its lobes pointed. Pectoral fins well developed, longer than the ventrals. Ventrals thoracic or subbrachial, with the spine slender but acute, and with second ray longest. Type Caulolatilus chrysops Gill. The genus Caulolatilus is widely separated from Latilus by the form of the body, structure of the scales and especially by the form of "the head and the structure of the fins. It is also related to Prohitilus,* but is readily distin- guished by the general form, the form of the head, the thoracic position of the ventral fins, as well as the number of dorsal spines and form of the cau- dal fin. Caulolatilus was first separated from Latilus in an article entitled " Remarks on the relations of the genera, and other groups of Cuban Fishes ;" it was said to be distinguished by its form and the structure of the fins, and was founded for the reception of the Latilus chrysops C. et V. Subsequently Dr. Cooper described as a new generic type allied to Hetero- gnathodon Blkr., a Californian species of the same genus, and considered it "to be a very aberrant form of the Percoid family, having many characters of other orders. Four species of the genus are known to me ; their relations and differential characters may be expressed by the following scheme : I. D. vii (-viii.) 24. A. i. (ii.)22.f Profile quadrantiform. C. chrysops. C. affinis. II. D. viii. 25—26. A. ii. 25—26. Profile less decurved, the snout being produced. a.. Dorsal spines behind longer than the space between the fin and lateral line ; pectoral fin equal to distance from snout to middle of operculum C. anomalus. p. Dorsal spines behind about equal to space between fin and lateral line ; pectoral fin about three-fourths the length of the head (Jenyns.) C. princeps. Caulolatilus chrysops. Latilus chrysops C. et V., ix. 496 ; Guict., in Sayra,, tab. 2, f. 1 ; Gthr., ii. 253. * Prohitilus Gill, (type Latilus Jugularis Cuv, Val.,) is distinguished by its general form, a« well as the form of the head, scaly forehead aud approximated eyes ; few (4) dorsal spines, entire caudal and subjugular ventrals. + My own enumeration of the dorsal and anal ray exactly coincides with Gunther's; Cuvier as- signs D. -viii. 24. A. ii. 22. I cannot discover the small spine in front of the anal one, and there are certainly only seven dorsal spines, 1865.] ' 68 PROCEEDINGS OP THE ACADEMY OP Caulolatilus chrysops Gill, Phil. 1862, 340. Hab. — West Indies. D. vii. (-viii.) 24. A. i. (-ii.) 22. C. v. 1, 7, 6, 1, v. P. 18. V. I. 5. Caulolatilus affinis Gill. In a young specimen the following peculiarities are exhibited : The profile describes the outline of a quadrant, and in front is almost ver- tical. The greatest height is contained less than four times (*27) in the length, exclusive of caudal ; that of the caudal peduncle about nine times. The head forms more than three-tenths of the length, while its height bears to its length the proportion of 22£ : 31. The diameter of the eye equals almost half the height of the head. The preorbital is very narrow. The teeth of the preoperculum are strong and distant, and those of the middle di- rected obliquely upwards. The sixth dorsal spine equals a, ninth of the length. The anus is behind the middle of the length. The caudal rather ex- ceeds the height of the head. The pectoral equals a fifth of the length ; the ventral is shorter ("18,) and is inserted beneath the base of the pectoral, its spine being at the vertical of the upper axil. D. vii. 25. A. ii. 22. P. 18. The color is reddish brown on the head and back, lighter on the sides. A very distinct blackish spot is present above the axilla of the pectoral. This species is very closely related to C. chrysops, but the single individual which is a young one about three inches long, differs from adults of the latter, of which I have seen none less than fifteen inches long, by the greater height of the spinous dorsal and the proportions of the other fins, and the situation of the ventrals, strongly serrated preoperculum, as well as as the large eyes and narrow preorbital. The last two characteristics are doubtless those of youth. The value of the others yet remains to be ascertained, but it is pro- hable that they will be found to be specific, although, perhaps, slightly modi- fied with age. The species has been known to me for three years, but I have felt reluctant to^describe from so small a specimen. The specimen was ob- tained by Mr. Xantus at Cape St. Lucas. Caulolatilus anomalus. Dekaya anomala Cooper, Proc. California Academy Natural Sciences, vol. iii. p. 71, fig. 17, 1864. Hab. — Catalina Island, California. D. viii. 25. A. ii. 25. P. 18. Sq. 135— 140-1 5 pm, Caulolatilus anomalus is very closely related to the C. princeps of the Gala- pagos Archipelago, but appears to differ in the more elongated spines of the dorsal fin, as well as the longer pectoral and ventral fins. A critical compari- son of fresh or wet specimens of both species is, however, requisite not only to verify the differences 'referred to, but to ascertain the other differential characters. It is scarcely probable that the two forms are co-specific, but at the same time we must remember that at least one species is common to Lower California and the Galapagos Islands. The type specimen of C. anomalus was kindly forwarded for examination by Dr. Cooper, the discoverer. It is an adult, and belongs to the collection of the Geological Survey of the State of California. Caulolatilus princeps. Latilus princeps Jenyvs, Fishes Beagle, 52, pi. 11. Gthr., ii. 253. Hab. — Galapagos Islands (Chatham Island.) [April, NATURAL SCIENCES OF PHILADELPHIA. 69 On the Cranial Characteristics of GADUS PROXIMUS Grd. BY THEODORE GILL. While engaged in the investigation of the comparative anatomy of the Gadoids and allied families, my attention was arrested by the very distinctive characters exhibited by the Californian Gadoid named by Girard Gadus prox- imus or Morrhua proxima. The title of that form to generic separation from the typical Gadi, is fully confirmed. I may remark, that I had long distrusted its pertinence to Gadus on account of its small size, but the few and trivial outward peculiarities exhibited by it, almost forbade a separation, until more should be known concerning its organization. The affinities of the new genus are, perhaps, rather with Brachygadus than Gadus itself; but the form of the head sufficiently distinguishes it from thai type. The distinctive external characters are the angular form of the fins, especially of the first dorsal, the small size and the immaculate body. All the osteological characters, herewith given, are contrasted with those of Gadus, and the peculiarities are indicated by the italicized portions. If, as I suspect, the Gadus pygmaus of Pallas belongs to Boreogadus, as restricted by myself, at least three genera of Gadinoz are represented along the western American coast. MICROGADUS Gill. The cranium is proportionally broader towards the front and less flattened, while the brain case is flattened below, decidedly swollen laterally and on each side of a depressed sphenoidal groove, and has an ovate cordiform shape. The paroccipital or epiotic is not produced into an angle behind, but is ob- tusely rounded, and its posterior or outiuardly descending ridge blunt. The pe- trosal or opisthotic is well developed, oblong, and with its re-entering angle high up, and, on a line with it, the surface is divided into two parts ; an upper narrow and flattened one, and a lower expanded one, much swollen ; the alisphenoid or pro-otic is oblong, acutely emarginated in front, swollen from the region of the high anterior sinus, and above it little produced forwards. The great frontal is little longer than broad, with supraoccipital crest continued only along its posterior third, but an anterior low crest continued forwards on the bone, and near the front expanded upwards, and with the expanded por- tion behind dividing into narrow lateral wings ; the lateral tectiform ridges of the frontal are continued forwards and curved outwards towards the antero- lateral angles. The anterior frontals are mostly covered in front by £he great frontal, and are much developed in the direction of the antero-lateral angles ; the inferior expanded axillar portion being very narrow. The nasal has a rounded ridge in front continued well below, and its posterior crest is laminar" and trenchant. The rest of the bones offer less decided peculiarities, and, therefore, their immediate consideration is less requisite. Gadus tomcodus Mitchill exhibits similar modifications of the cranium, and should be approximated to G. proximus. Note on several Genera of CYPRINOIDS. BY THEODORE GILL. As considerable misapprehension appears to have prevailed regarding several genera of Cyprinoids, established for forms characteristic of the Pacific slope of North America by Girard, due, perhaps, to the vague or erroneous ideas enter- tained by that gentleman himself, it may be advisable to give the partial results of a renewed examination. 1865.] 70 PROCEEDINGS OP THE ACADEMY OP The genera Lavinia, Siboma, Algansea, Tigoma, Cheonda, Gila, Ptycho* chilus aad Mylochilus, are closely related to each other, and cannot be dis- tributed among different subfamilies, as has been attempted. Indeed, some of the genera so separated are so intimately allied, that their claims to generic distinction are extremely doubtful. Siboma appears to be nearly allied to Lavinia, and includes only the S. crassicauda, the ^'; tarsi |I. I determined this species to be A. rufus from specimens in the Phil. Acad.; these being mounted, the comparison could not be made satisfactorily, except as regards general appearance, in which they are much alike. The Panama species, however, is smaller, the lengths of the two sexes taken from fresh specimens, are respectively 4| and 4^ inches, the dried skins measuring half an inch less. Since my first determination of it, I have received specimens of A. rufus (as I suppose them to be) from Bahia, Brazil; these now measure 5\ in., and probably the length of recent specimens would be fully 6 inches. The under plumage of the Brazil species is more decidedly yellow ; and in several specimens there are none resembling the female of the other species, in its tawny under plumage. The Brazil bird has the outer tail feather white, with the margin of the inner web broadly brown nearly to the end; the next feather is brown, with a wedge shaped white stripe in the centre, terminating half way from the end. Birds from the two localities are certainly different, though I may err in calling ihose from Brazil, A- rufus. However, as it differs in its diminutive size, together with some other characters from all described species, I have no hesitation in deciding that it is new. Prof. Baird (Kev. Am. Birds, p. 157) considers its nearest ally to be Neo- corys Spraguei, which species I state that it resembles in habits, in my first account of it. Prof. Baird proposes for it a new subgenus, viz. Notiocorys. He also expresses a doubt of my identification of it as A. rufus being correct. 3. Thamnophilus nigricristatits. Male. Crown deep black, on the front a few feathers are narrowly pencil- led with white ; upper plumage black, regularly banded with lines of white ; the feathers of the throat and the sides of the head have black centres, with their outer edges white ; tail black, all the feathers marked on the margins of both webs With roundish white spots, six on each side ; quills black, the outer webs marked with white spots of a quadrate form ; wing coverts black, all terminating in white ; the feathers of the under plumage marked with al- ternate bars of greyish white and black ; upper mandible black, the lower plumbeous, paler at the end ; irides yellow ; feet black. Length (fresh) 6 in. ; wing 2| ; tail 2§ ; bill 1 1 ; tarsi 1. Habitat. — Line of Pan. R. R., Lion Hill Station. Female. Crown dark cinnamon, the feathers of the hind neck and sides of the head pale cinnamon, with black centres ; wing coverts and outer margins of quills and back bright cinnamon ; tail dark cinnamon ; inner webs and ends of the quill feathers blackish brown ; throat grey with a slight cinnamon tinge, under plumage clear cinnamon, much paler than the back; the mid- dle of the abdomen whitish ; under lining of wings pale cinnamon; inner margins of quills of a light salmon color ; bill and feet as in the male. This species differs from doliatus and affinis in having no white in the crest; doliatus is darker below, the black bands being nearer together ; it also differs from affinis in having the white markings above smaller and more distinct ; in that species they are more linear in form ; the female of the new species is very different from that of affinis, being much brighter and clearer in color ; it is 1865.] 10S PROCEEDINGS OF THE ACADEMY OF destitute of all markings except on the hind neck and sides of the head, whereas the female of affinis, besides its duller plumage, has the wing coverts brownish black barred and tipped with rufous, and the smaller quills barred and spotted with black ; there are also black spots on the upper part of the breast, and faint indications of narrow bars on the upper and under plu- mage. I have enlarged more in pointing out wherein this species differs from affinis for the reason, that I sent it to Mr. Sclater for publication (with some other birds) in the Ibis, more than two years since. He returned it marked "affi- nis;" to this opinion I demurred on the ground of that species having the crest largely white, which in this is entirely black. I so wrote him; he replied that not Laving the specimens before him he could uot then determine, but would do so when examining Mr. Salvin's collection received from Panama. In the List of that collection given, Proc. Zool. Soc. June, 1864, I notice T. affinis is given, and referring the bird I called T. doliatus, (Ann. Lye. N. Y. vol. vii. p. 293,) to the same species ; this specimen was in McLeannan's first collec- tion ; when I received the collection made by Messrs. McLeannan and Gal- braith, I noticed that the species now described was not doliatus, but supposed it was similar to the one so called in my Catalogue, without comparing them. I thereby misled Mr. Sclater, as I have since found that the specimen in Mr. McL.'s first collection is T. radiatus. But as Mr. Sclater only saw the speci- mens now described, of course these are the ones alluded to as being " affi- nis." I do not pretend to say that the specimens received by Mr. Salvin from the Isthmus and put in the List as affinis, are the same as mine now described. There is every probability of affinis being found there, and I should not like to give an opinion about their specimens without seeing them, therefore only speak of my own. 4. Geotrygon albiventer. Geotrygon violacea, Lawr., nee Temrn. Ann. Lye. of N. Y., vol. vii. p. 477. Geotrygon ? Scl. et Salv. P. Z. S. 1864. Male. Front pale rosaceous, crown dull brownish violet ; region of the ears to hind neck bluish cinerous ; upper part of back of a rich reddish violet; back, wing coverts and tail dark cinnamon or rufous brown, tinged with vio- let ; the primaries are of a lighter cinnamon color than the tail, with their inner webs dusky near their ends, the other quills are darker, becoming brown- ish next the back ; all the quills and larger wing coverts have their ends margined with light cinnamon, inside of which is a dusky narrow subterminal band ; the under wing coverts are white with their ends blackish brown ; the axillars are blackish brown at the base, remaining half white ; throat, sides, abdomen and under tail coverts pure white ; feathers of thighs brown ending in white : the feathers on the middle of the breast are of a light brownish ash, with their ends pale rufous, the lower part and sides of the breast are of a light pinkish lilac, these seem like new feathers ; and the whole breast in a more mature bird is probably of this color ; it becomes paler as it extends downwards, and gradually merges into the pure white of the abdomen ; bill and legs in the dried specimen brownish yellow. Length 9 in. ; wing 5^ ; tail 3| ; bill § ; tarsi f. Hab. — Line of Pan. R. Road, near Lion Hill Station. My identification of this species as violacea, Temm., was made from his de- scription and plate, Knip, Pig. t. 29, but I had misgivings as to it's correct- ness. I then was not aware of their being two specimens of that species in the Mus. of the Phil. Acad., which came from the Rivoli Collection. I have since compared my specimen with these and find it quite distinct. G. violacea has the crown, back and wings greenish bronze; the upper part of the back violet blue, and the tail and quills of a lighter red than in my species. [June, NATURAL SCIENCES OP PHILADELPHIA 109 July Wth. Mr. Cassin, Vice President, in the Chair. Thirteen members present. The resignation of Dr. B H. Rand, as Recording Secretary, was read. The following papers were read and referred to a committee : 11 Remarks oo the genus Taxocrinus, &c, with descriptions of new species,'! and " Descriptions of new species of Crinoidea, &c." By F. B. Meek and A. H. Worthen. The deaths of Joseph Hopkinson, M. D., Mr James Dundas, Mr. J. Reese Fry, and Mr. Richard Price, late members, were announced. July \%tli. Mr. Cassin, Vice President, in the Chair. Eleven members present. The following paper was read and referred to a committee : " On Amphibamus grandicep3, &c." By Prof. E. D. Cope. July 25th. Mr. Cassin, Vice President, in the Chair. Nine members present. On Report of the respective Committees, the following papers were ordered to be published. Descriptions of New Species of FOSSILS, from the Marshall Group of Michi- gan, and its supposed equivalent, in other States; with Notes on some Fossils of the same age previously described. BY PROFESSOR ALEXANDER WINCHELL. The following paper is intended to constitute a further contribution to our knowledge of certain western rocks occupying a position near the boundary line between the carboniferous and Devonian systems.* The materials for this paper have been in part collected by the writer in Michigan, Ohio, Indi- ana, and towa. Further material has been found amongst the inrestigandu of the " White Collection " of the University of Michigan. Col. Charles Whit- tlesey's collection of fossils from the "Fine Grained Sandstone " of Ohio, has also been placed in the writer's hands for study. In addition to this, the lat- ter has spent several days with Prof. James Hall in .his cabinet, engaged in making direct comparisons between the fossils of the rocks under considera- tion, and the types of the Chemung group, preserved in his magnificent col- lection. An opportunity has also been enjoyed of making a hasty survey of the fossils from the same horizon, contained in the extensive collection of the Illinois Geological Survey, for which the writer's acknowledgments are due to the Director, A. H. Worthen, Esq. The reader will observe that all the identifications heretofore made with typical Chemung fossils from New York and Pennsylvania, have been aban- nial 352 * Former papers by the writer, cm the same subject, may be referred to as follows : " First Bien- al Report" of the Geological Survey of Mich. I860; Amer. Jour. Sci. and Arte, [2J Vol. xxxiii. p. i2; ib. [2] xxxv. p. 61 ; Proe. Aeal. Nat. Sci. Phil., Sept. 1862, p. 405 ; ib. Jan. 1863, p 2. 1865.] 110 PROCEEDINGS OF THE ACADEMY OF doned. On critical comparison between actual specimens, it has appeared that the differences — some of which have always been admitted — are of too important a character to permit the identification formerly assumed. On the other hand, the following paper discloses an extended network of identifica- tions amongst the fossils from States west of Pennsylvania. But perhaps the most interesting feature of all is the identification of four western species with fossils, contained in the supposed carboniferous conglomerate of western New York. These are Euomplialu.s depressus, Hall, ( = Straparollus Ammon, White), Cypricardia contracta, Hall, (= Edmondia ? bicarinata, Winchell), Edmondia oeqmmarginalis, Win., and A'lorixma Hannibal.ensi*, Shumard.* Considering the small number of fossils as yet discovered in this conglomerate, in New York — and these only at one locality (four miJes north of Panama, Chautau- aue County) — so considerable a number of identifications is calculated to ex- cite some surprise, and not a little hope, that we are getting glimpses of the clue to a solution of geological difficulties of long standing. But further than this, two of the above species— Edmondia cequimarginalis and Allorisma Hannibalensin — occur in what has been regarded as another con- glomerate, whose position is beneath the first and at the top of the Chemung rocks of Western New York. In the light of these identifications, and in the absence of all identifications between western species and those of the Chemung, as well as between the species of this conglomerate and those of the Chemung, it might not seem un- reasonable to doubt its affinities with recognized Chemung rocks, and to sus- pect its continuity with the supposed "carboniferous conglomerate," until observation shall have demonstrated that its stratigraphical position is really below that formation. And further, since we must probably abandon the at- tempt to coordinate the Chemung of New York with the fossiliferous portions of the sandstones and shales of the west lying between the ''Black Slate " and the coal conglomerate, it stems not unlikely that we may yet be able to prove the conglomerates of Western New York to be the attenuated and lit- toral eastern prolongation of those western sandstones and shales — at least of the superior and fossiliferous portions of them ; so that the latter would ^tand as a hitherto unrecognized group of strata lying at the very base of the carboniferous system ; while the Chemung rocks of New York fall within the Devonian system, toward which the writer is now inclined to think that their paleontological affinities attract them. It yet remains to determine by observations in the field, whether the so- ,;alled "carboniferous conglomerate" of Western New York is really the equi- valent of the coal conglomerate of Ohio ; and whether any actual junction of superposition can be discovered in Western Pennsylvania or Eastern Ohio, be- tween the Chemung rocks in their westward prolongation and the fine grained sandstones and gritstones of the Western States. The total number of species at present described from the rocks under con- sideration is about 379, of which 170 were first described by the writer, and four have been recognized as belonging to undescribed genera". The number of .-pecies neticed in the. present paper is 94, of which 3b' are described as new species, and two are made the types of new genera. Descriptions and Notes of Species. COXOPOTERIUM n. gen. Etymology. K^v&c, a cone, and ttoth^iov, a little cup. Generic Characters. Corallum compound, generally free, sometimes adhe- rent, but without a distinct base of attachment. Cells somewhat crowded, * The writer is under special obligations to Prof. Hall for the unreserved liberality with which he has been allowed to examine the specimens in his cabinet, as well as for many kind- nesses incident to the generous hospitality of his house. [July, NATURAL SCIENCES OP PHILADELPHIA. Ill rapidly enlarging, inseparable, with only occasional and rudimentary dia- phragms, and no radial lamellae. Walls marked internally by vertical striae, and a few pores which communicate between the cells. Exterior, where ex- posed, covered by an epitheca, marked only by irregular encircling striae. Cells increasing laterally and interstitially. This genus, perhaps, approaches nearest to Sphenopoterium, Meek and Wor- then. It differs in the absence of the cuneate form of the base even in Sphen- opoterium— the cell mouths in this genus being turned indifferently in all directions. The cells also are smaller and more numerous ; and the fewer mural pores communicate from cell to cell, instead of terminating in the in- tercellular substance. But one species has thus far been observed. Conopoterium EFFPS0M n. sp. Corallum small, spheroidal, consisting of 20 to 50 cells, which are crowded, subcircular or irregularly angulated in trans- verse section, feebly striated internally, and having a thick, feebly wrinkled epitheca. Specimens presenting cells of all sizes. Some tendency is manifest toward a proliferous growth ; some of the lateral cells becoming adherent by their sides to a foreign body. Diameter of largest mass, "58 ; diameter of mouth of largest cells, about •20. From the Lithographic Limestone, Clarksville, Mo., " White Collection " of the University of Michigan. ZAPHRENTIS, Rafmesque et Clifford. Zaphrentis Ida n. sp. Coral simple, of medium dimensions, in the general form of an inverted cone, strongly curved, with numerous encircling wrinkles of growth, and an occasional deep constriction. Epitheca rather thick, though the vertical lamellae show faintly on the exterior. Cup very oblique, turned toward the shorter side, with a distinct fossette -reaching from the centre to the shorter side. Radial lamellae 31 in a specimen -62 inch in dia- meter. On the side opposite the fossette is a thick lamella reaching from the periphery to the centre ; one-sixth of the circumference on each side of this is another lamella reaching to the centre, and at the same interval from these are two others ; in the fossette, near the periphery, is the rudiment of a sixth. The remaining lamellae do not extend to the centre but become confluent in each sextant, with the principal lamella which lies between them and the fos- sette— the fossette taking the place of a principal lamella. There are thus, in each sextant, four subordinate lamellae joining their primaries, except that in one of the sextants adjacent to the fossette there appears a supernumery lam- ella, caused apparently by the splitting of the shortest subordinate or the one next the fossette. Taking no account of this anomaly, the whole number of lamellae is 30, a multiple of six instead of four. The spaces between the lamellae are intersected by thin trans verse dia- phragms arranged at unequal distances,, and either flat or concave upwards. There is no correspondence in the positions of the diaphragms in contiguous interlamellar spaces ; and the wrinkles of the epitheca sustain no relation to them, since they are not continuous, but are intercepted by vertical interlam- illar walls ; and besides, they nearly disappear in the peripheral region of the internal cavity. Collected by A. Winchell, in the Goniatite Limestone at Rockford, Indiana. The septal system of this coral is described above as senary instead of quaternary. The senary arrangement, as a fact, is sufficiently apparent ; and yet it must probably be regarded as illusory — the primary lamellae being four instead of six, and the illusion being produced by the mode of confluence of the lamellae of the second and third cycles. Zaphrentis acutus ? White and Whitfield. Occurs in the Lithographic Limestone of Clarksville, Missouri. "White Collection" of the University of Michigan 1865.] 112 PROCEEDINGS OF THE ACADEMY OF FAVOSITES, Lamark. Favosites ? mancus ii. sp. Coral a small hemispherical mass, with an ob- tuse apex.; principal cell-mouths very small, sub-circular; those occupying the interstices smaller and angular ; cell-walls strong, prominently raised above the general surface. Cells rapidly enlarging and multiplying by fre quent gemmation. No pores, stria? or diaphragms have been discerned. Diameter of polypary, "68 inch; largest cell-mouths, -05 inch in diameter. This differs from F. divergent, White and Whitfield — the only other species described from rocks of this age — in its extremely diminutive proportions, and in the apparent absence of diaphragms. There is perhaps as much reason for referring this species to Conopotcrium as to Favosites. Collected by A. Wiuchell, in the Goniatite limestone of Rockford, Indiana. Trematopora ? vesiculosa, Win. Specimens undistinguishable from the Iowa species, in their existing state of preservation, have been collected by A. Winchell, at Alan's quarry, in Hillsdale, Michigan. Lingula Cuyahoga, Hall. Numerous specimens, not distinguishable from this species, were obtained by the writer from fragments of a hard, calcareous, brecciated rock, quarried from a well on the premises of Judge Alan, at Hills- dale, Michigan. The geological position is apparently in the lower part of the Marshall group. The rock here is the nearest approach in physical charac- ters that has yet been seen to the Goniatite limestone at Rockford, Indiana. Occurs also in the "Fine-grained sandstone beneath the coal at Ward's mine, Wethersfield, Trumbull County, Ohio— conglomerate wanting." Whit- tlesey's collection. DISCINA, Davidson. DlSCINA GrALLAHERI, n. Sp. Shell of medium size, nearly circular. Ventral valve with the apex sligrTtly excentric ; foramen lanceolate, reaching from near the apex four-fifths the distance to the margin, and acute at both extremities. Surface marked by about fifteen rigid, sharp, sub-equidistant stria3, which are somewhat more approximated toward the apex. The striae are less distinct on the shell than upon the cast. Dorso-ventral diameter about l'O ; transverse diameter about 1*0 ; distance from apex to dorsal side, *48 ; length of foramen, -33. Found at Hillsdale, Michigan, on the premises of Rev. F. A. Gallaher, in a small loose fragment having the lithological characters of the lower gray portions of the neighboring Marshall sandstone. It occurs also in Col. Whit- tlesey's collection from Girard and Wethersfield, in Trumbull County, Ohio. I at first referred the specimens to D. Newb&rryi, Hall, (xvi. Rep. N. Y. Regents, p. 30,) but direct comparison with the types of that species shows that it differs in having more remote, stronger and more regularly equidistant concentric stria?. In its striation it resembles D. grandis, Hall, from the Ham- ilton group, but the form is more circular and the striae are relatively less remote. Discina capax, White, (1S64.) Identified in Whittlesey's collection, "from rocks next below the coal canal level, one mile below Girard," and also at " Girard, Trumbull County," Ohio. The types of D. Nezvberryi, Hall, (1864,) do not seem to be distinguishable from this species. PRODUCTA, Sowerby. Producta gracilis, n. sp. Shell small, aperture of the ventral valve form- ing a little more than a semicircle. Ventral valve moderately inflated for a Producta, with flattened, smooth, triangular auriculations ; hinge-line equal [July, NATURAL SCIENCES OP PHILADELPHIA. 113 to greatest width of shell ; mesial sinus wanting or barely perceptible ; exter- nal surface marked by fine, rigid, sharp, once dichotomizing radial lines or ribs, numbering about 40. No indications of spines have been detected. Length of hinge line, "29 (100) ; length from beak to anterior margin, •21 (72). Described from an imperfect ventral valve ; but its peculiar characters easily distinguish it. Museum of University of Michigan, Collected by A. Winchell at Valley Forge, one and a half miles below Cuyahoga Falls, Ohio. PfiODtjcTA duplicostata, n. sp. Shell rather large with subcircular outline. Ventral valve very ventricose and greatly arched, with steep slopes to the right and left margins, not enlarged at the aperture, and entirely destitute of mesial sinus ; marked with numerous interruptedly and irregularly striate sinuous ribs, which dichotomize once or twice in the middle region of the valve, and towards the front resolve themselves each into a fascicule of three or four smaller ribs, themselves raised into a wider rib-like elevation around the anterior margin. The tubular spines are scattered over the whole exte- rior, but become much more abundant at the commencement of the marginal costate ridges. The whole exterior of the cast is marked also by oblique punctations, which are placed mostly in irregular lines between the ribs, and become consequently most abundant toward the margin. On the sides of the cast the punctations become elongated into short furrows which cross the surface obliquely. Length, 1*19 ; breadth, 1*24; convexity of ventral valve, "58; number of marginal ridges, 15 to 20. Collected by A. Winchell, at Battle Creek, Michigan. Occurs also in Lick- ing County, Ohio. Producta morbilliana, n. sp. Shell smal', transversely subelliptic, only moderately produced. Hinge line seven-eighths the greatest width of the shell; ears small, nearly right angled. The shell regularly contracts from the aperture to the beak, which is small, subacute, and projects slightly be- yond the hinge. The arching of the shell is such that when resting on the aperture the greatest height is equal to one-half the greatest width. No sinus or flattening present. The surface is marked by a series of deep, con- tinuous, equidistant wrinkles, ten or eleven in number, becoming obscure toward the beak ; between the wrinkles are numerous fine concentric stris not easily seen without a magnifier. These features are crossed by a longitu- dinal system which, near the beak, is a set of fine regular costae, which near the middle become interrupted by the wrinkles, and, losing their identity, result in several concentric bands of short longitudinal tubes buried in the substance of the shell, and gradually emerging and presenting their apertures anteriorly. Transverse diameter of aperture, '58 (100) ; length of hinge line, -51 (88) ; distance from hinge line across the aperture to opposite side, -44 (76) ; height of shell when resting on the aperture, "26 (45). From the base of the Burlington limestone, Burlington, Iowa. "White Collection " of the University of Michigan. A cast from the yellow sandstone below (probably "No. 5,") is probably identical with this. This beautiful species is most nearly related to P. speciosa, Hall, (xth Rep. N. Y. Reg. p. 176.) The resemblance, however, is not striking, except in the cast referred to. This differs in having the pustules more regularly ar- ranged in concentric bands. P. morbilliana may also be compared with P. Rogersi, Nor. and Prat., (Jour. Acad. Nat. Sci. Phil. [2] iii. 9, pi. i. 3, a, b, c, not P. aspera McChesney.) It is, however, a much neater species, without trace of sinus, not so full near the beak, while the rib-like tubes arranged 1865.] 114 PROCEEDINGS OF THE ACADEMY OF along the concentric bands are smaller and more regular. Its nearest foreign analogue is P. punctata, Sowerby, (Min. Conch, iv. 22, pi. 323.) Its surface features, in point of regularity, are intermediate between the extremes pre- sented by that variable species ; but it differs constantly in the absence of a sinus. Producta curtirostka, n. sp. Shell of moderate size, semi-globoid, with- out mesial sinus. Hinge line nearly equal to greatest width of valve, with but slight flattening in the region of the extremities. Beak scarcely surpass- ing the hinge line, extremely flattened ; general surface regularly convex, marked by numerous interrupted, sub-obsolete costse, and, in the umbonal region, by numerous concentric wrinkles, most distinct upon the ears. The inside of the dorsal valve presents an appearance very similar to the outside of the ventral valve. This is the species formerly referred by me (Proc. Acad. Nat. Sci. Phil., Jan. 1863, p. 4,) to P. speciosa, Hall. A careful comparison of specimens, how- ever, fail to justify this identification. It most nearly approaches P. lacry- rnosa, Hall. The remarkable features of the beak of the ventral valve, and the great concavity of the dorsal, are, however, characters which distinguish this species from all others. P. lacrymosa has less fulness in the region of the cardinal extremities, giving the umbo less breadth and greater isolation from the ears. From the yellow sandstone, Burlington, Iowa. " White Collection" of the University of Michigan. Producta dolorosa, n. sp. Shell of medium size, somewhat hemispherical, outline subcircular or somewhat transverse, truncated along the hinge line, which is considerably shorter than the greatest width of the shell. Ventral valve regularly convex, with scarcely an apparent flattening at the hinge ex- tremities ; beak depressed, obtuse, slightly surpassing the cardinal line. Dorsal valve but slightly concave, with a low and inconspicuous median sep- tum reaching to the middle of the valve ; the muscular scars presenting together a somewhat semicircular contour, in front of which the interior of the shell presents a finely papillose area. External surface presenting a series of elongated pustules, or interrupted, irregular depressed costse, and a few coarse concentric wrinkles, between which the surface is covered with fine concentric stria?. Length from hinge, in a straight line to front margin, -54 (66) ; transverse diameter, -82 (100); length of hinge line, *56 (68) ; depth of ventral valve, •24 (29). This species, on casual observation, would be referred to P. lacrymosa, Hall, (x. Report New York Regents, p. 177.) The beak, however, is less acute and projecting, the ears less flattened, the dorsal valve less concave, and tlie ventral less produced. If possessed of cardinal spines it might be taken for Chonetes truncata, Hall. Figures D and Dd, Whittlesey, (Proc. Amer. Assoc. Cincinnati, p. 220,) may be intended for this species. "Weymouth, Medina County, Ohio, 60 feet below the conglomerate." Whittlesey's Collection. Producta concentrica, Hall. In quoting this species from Michigan, (Proc. Acad. Nat. Sci. Phil., Sept. 1862, p. 411,) it was stated that only the interior of dorsal valves had been seen in the southern part of the State. Since then I have obtained good ventral valves from Battle Creek, which agree in every respect with specimens from Burlington, Iowa. A dorsal valve of this species was found at Rockford, Indiana, in the bluish argillaceous brecciated limestone of the famous " Goniatite bed." This spe- cies is now known to occur in Northern and Southern Michigan, at Burlington and Rockford, and probablv in Missouri and Illinois. [July, NATURAL SCIENCES OF PHILADELPHIA. 115 The young of P. concentrica, Shumardiana, pyxidata, Cooperensis and arcu- ata, present resemblances so strong that it is scarcely possible to distinguish them from each other. In the adult state, however, the last may be distin- guished by its much stronger and regular costae, its less rapid expansion and greater arcuation. P. Cooperensis has the form of P. arcuata, without its strongly marked ribs. The other three species are not satisfactorily distin- guishable, even in the adult state. P. pyxidata was described by Hall from the so-called Hamilton shale and limestone of Hamburgh, 111., and Louisiana, _ Mo*; P. Shumardiana was described by Hall from the so-called Hamilton of Clarksville, Mo., and the so-called Chemung of Burlington ; P. concent rim only from the latter locality. It is probable that the rocks at all of these localities are of nearly the same age. This being the case, the probabi'ity be- comes strengthened that the three species first named are one and the same. If so, P. concentrica, having been first published, will displace the other two names. Peoducta semireticuxata, Fleming, (P. Martini, (De Kow) Win. Proc. Acad. Nat. Sci. Phil. Jan. 1863, p. 4; figs. B. and Bb, Whittlesey, Proc. Amer. Assoc. Cincinnati, p. 219.) This species occurs plentifully at Battle Creek, Michigan. Collected by A. Winchell. Also in Hillsdale County. Collected by Rev. J. D. Parker. A large specimen from the sands'ones at Burlington, Iowa, resembles, in its want of mesial sinus, the forms of P. semireticulata occurring in the Burlington limestone, rather than its associates in the same strata. It pos- sesses in addition, a peculiar sharpness of the ribs not seen in othrr speci mens. Occurs also in Whittlesey's Collection from "Weymouth, Medina county. Ohio, 60 feet below the conglomerate;" and " Sheldo 's sawmill, Orange. Cuyahoga county, below the grindstone grit." P. Newberryi, Hall, (x. Rep N. Y. Regents, p. 180,) from Ohio, is perhaps too closely related to this species. Dorsal valves cannot be distinguished- from dorsal valves of P. semireticulata, as they occur at Battle Creek, Mich. The ventral valve of P. Newberryi does not become so much arcuate, the con centric wrinkling is a little more wavy, and less regular, the beak is less at- tenuate, and projects less beyond the hinge, and the mesial depression is smaller. Prodccta Cooperensis, Swallow, (Trans. St. Louis Acad. Nat. Sci. i. 640.) The hinge line is shorter than in the typical specimens, but otherwise the agreement is good. Bed "No. 1," Burlington, Iowa. " White Collection " of the University of Michigan. Chonetes pulchella, Win., (Proc. Acad. Nat. Sci. Phila., Sept.. 1S62, p. 410). Collected by A. Winchell at Germain's and Alan's Quarries, Hillsdale, Michigan. Oue specimen from this locality is larger than usual, presenting a greater elongation of hinge line, which is drawn out at the extremities to an abrupt acumination. The number of ribs is about 60. Two cardinal spines are seen on each side of the beak, making an angle of about 60° with the hinge line. Occurs also in Ohio, at " Howland, Trumbull County, one half mile east from Center, at " Warren, Trumbull County, in coarse bedded sandstone, next below the conglomerate," and at "Tallmadge, Summit County, in a boul- der, supposed to be from the shales next below the conglomerate," Whittle- sey's Collection. C. pulchella, in the number of its ribs, is. intermediate between C. Logani, Nor. and Prat, and C. Illinoisensis, Worthen. In this character it most re- sembles the former, while it differs from it in the smoothness of the ribs. It 1865.] 116 PROCEEDINGS OF THE ACADEMY OF resembles C. setigera, Hall, and C. nana, but differs from the former in having oblique instead of erect spines, and from the latter in the smaller area of the ventral valve. C. setigera occurs in the Hamilton and Chemung of New York, and I have identified it in the blue argillaceous shales of the Huron group of Michigan. C nana is found in the corniferous limestone ; and Euro- pean geologists regard it as a Devonian species. Ciionetes Illinoisensis, Worthen, (Trans. St. Louis Acad. Nat. Sci. i. 571) ; C. Logani, Hall, (Iowa Rep. p. 598, pi. xii. fig. la— e and 2) ; not C. Logani, ' Norwood and Pratten, (Jour. Acad. Nat. Sci. Phil. [2] iii. 30, pi. ii. fig 12, a, b, c] ; C. Illinoisensis, Winchell, (Proc. Acad. Nat. Sci. Phil., Jan., 1863, p. 5). This wide spread species occurs at the Grindstone quarries at Pt. aux Barques, Mich. The specimens are smaller than the typical ones from Bur- lington, Iowa, and perhaps for this reason do not number as many striae around the margin ; but specimens from Burlington of the same age cannot be distinguished. Collected also by A. Winchell at Rockford, Indiana. It also occurs in the base of the Burlington limestone at Burlington, Iowa, (" White Collection") and in the fine grained sandstones of Licking County, Ohio. This species may be confounded with C. Shumardianq, De Koninck ; but the latter has 270 to 280 or more radiating striae, which are less distinctly isolated from each other. The former has from 100 to 125 striae. Cheilitis geniculates, White, (Proc. Bos. Soc. Nat. Hist. ix. 29). A single ventral valve, collected by A. Winchell at Rockford, Indiana, cannot be dis- tinguished from this species. Choketes Logani, Norwood and Pratten. In a former paper I pointed out the error of Hall's identification of C. Logani, N. & P., though this species had not at that time fallen under my observation, and, I believe, has been seldom seen since first described. I have now, however, in some later addi- tions to the " White Collection " of the University, a number of examples of •C. Logani, N. & P., fully answering to the original description and figure. These specimens are from the base of the Burlington limestone, and the ma- trix holds C. Illinoisensis in the same association, as previously believed. C. Logani, N. & P., as far as I have observed, is restricted to the horizon of the Marshall or Burlington sandstone — including the base of the Burlington limestone, which belongs evidently to the same epoch. Prof. Hall, however, has a small Ciionetes from the Tully limestone, which, he informs me, he has decided to refer to C. Logani, (see 11th volume Paleontology of N. Y.), a reference to which, with full acknowledgement of his superior authority, I cannot, at present, give my assent. The Tully limestone species presents a series of concentric rugosities or wrinkles, which extend both across the ribs and the intervals between the ribs ; while in C. Logani the rugosities are feebler, and are confined to the crests of the ribs. C. Logani is also recognized in Ohio, with about 40 to 50 ribs. It hence appears that the species, like C. Illinoisensis, Worthen, and C. multicosta, WiDchell, ranges from the Burliugton limestone into the sandstone below. I may perhaps be permitted to add that some typical specimens of C. Logani in Prof. Hall's cabinet, sent to him by Dr. Norwood, are imbedded in a matrix .if oolitic limestone, such as occurs at the base of the Burlington limestone. Ortiiis Michelini, L'Eveille, occurs in Whittlesey's collection from "Wa- verly sandstone, near Newark, Licking County, Ohio." Another Ortiiis from Akron, Ohio, resembles the Burlington species commonly referred to O. Va- nuxemi (?), but differs in the parallel direction of the dental lamellae, and in the very indistinct character of the radial striation. Still another Orthis, received from Dr. Shumard and collected at Sulphur Springs, St. Louis County, Missouri, is perhaps the species referred by the [July, NATURAL SCIENCES OP PHILADELPHIA. 117 » Missouri geologists to 0. Michelini (?). It is a small circular species, with extremely fine ribs or strise, apparently too obscure for either 0. Michelini or 0. Vanuxemi. Orthis flava, n. sp. Shell small, transversely oval, slightly truncate on the cardinal side. Ventral valve convex, perceptibly flattened toward the anterior margin, though without a marked sinus ; most elevated near the slightly projecting beak ; area rather high and broad, triangular, with an equilaterally triangular foramen ; dental lamella? slender, short, diverging at an angle of about 80° ; occlusor scars small, together enclosing a longitudinally oval space, which readies one-third the distance from the beak to the anterior margin ; a median internal ridge reaches froin the beak to beyond the middle of the valve. The shell was evidently thin ; its surface marked by one hun- dred or more delicate radiating ribs, which increase by implantation. Transverse diameter of shell -50 (100) ; longitudinal diameter -39 (78) ; depth of ventral valve .12 (24). ~ Burlington, Iowa, apparently from Bed " No. 1." at the lbase of the yellow sandstones. " White Collection," of the University of Michigan. This species is less circular than the forms referred to 0. Michelini, and has a more convex ventral valve and larger area. It differs from 0. impressa, Hall, (Geol. Rep. 11th Dist. N. Y., p. 267, fig. 2), in its more transverse shape, smaller size, more convex ventral valve, and feebler sinus. Streptorhynchus lens? White, (Proc. Bos. Soc. Nat. Hist. ix. 28), /'Wey- mouth, Medina County, Ohio, 80 feet below the conglomerate." Whittlesey's Collection. Streptorhynchus umbraculum ? Schloth. sp. From "coarse bedded sand- stone, next below conglomerate, Warren, Trumbull County, Ohio." Whittle- sey's Collection. A large, undetermined species from oolitic limestone, "No. 6," Burlington, Iowa, probably belongs here. Collected by A. Winchell. Streptorhynchus inequalis, White sp. From Weymouth, Medina County, Ohio, 80 feet below conglomerate." Whittlesey's Collection. Streptorhynchus sp. ? A single interior of a ventral valve from "near Ashland, Ashland County, Ohio," resembles S. Chemungensis, var. pectinacea, Hall. (Pal. N. Y., Vol. iv.) It differs, however, in the possession of a longer hinge line, and distinct auriculations, and lacks the alternation in the size of the radial ridges. Pentamerus lenticularis, White and Whitfield. This species, described from the yellow sandstone of Burlington, occurs also in the base of the Bur- lington limestone. " White Collection " of the University of Michigan. SPIRIGERA, D'Orbigny. Spirigera Missouriensis, n. sp. Shell of moderate size, broadly ovate, mo- derately ventricose, with lamellose exterior. Ventral valve with an extended beak, turned up at right angles with the plane of the shell, and having a cir- cular perforation at its extremity. Between the beak and the dorsal valve is an external flattening simulating an area, but traversed by the incremental lines. Sinus a shallow but distinct groove, beginning at the beak, widening and deepening anterior to the middle, and near the middle becoming well characterized. Dorsal valve nearly circular, with straight hinge slopes, and obtuse, beak closely incurved and concealed, though not in contact with the ventral beak. Mesial fold less distinct than the sinus of the ventral valve, arising near the middle of the valve. Both valves are marked by numerous strongly imbricating lamella? of growth. Greatest thickness through the middle of the ventral valve. 1865.] 118 PROCEEDINGS OP THE ACADEMY OP Length -69 (100) ; width -65 (94) ; thickness of both valves -41 (59). From the Lithographic limestone of Louisiana, Missouri. White Collection of the University of Michigan. Also from the sandstone at Weymouth, Me- dina County, Ohio, 60 feet below the conglomerate. Whittlesey's Collection. Close observation is necessary to distinguish this species from 5. subtilita, Hall. That species, however, is less lamellose, the ventral sinus does not extend above the middle of the shell, and the flattening beneath the beaks of the ventral valve is wanting. Spirigera biloba, n. sp. Shell broadly ovate in outline. Ventral valve rather ventricose, with a prominent beak which is gradually recurved, and apparently minutely perforate at apex. A deep, narrow, median furrow begins at the apex and extends to the anterior margin ; from the bottom of this the surface rises with a convex curvature to the summits of the two rounded ridges which constitute the most prominent portion of the valve ; from these summits the curvatures continue to the right and left margins, which are thus rendered quite obtuse. The external surface is marked only by a few faint incremental lines. Shell structure fibrous. Characters of dorsal valve unknown. Length -16 ; breadth -16. Collected by A. Winchell in the Goniatite limestone at Rookford, Indiana. This shell has somewhat the aspect of a CentronAla or Terebratula, but its structure is not punctate. The unique character of the mesial furrow distin- guishes it from any known species of Spirigera. Spirigera Ohiensis, n sp., (Figs. A and Aa, Whittlesey, Proceedings Amer. Assoc. Cincinnati, p. 220). Shell large, subcircular in outline, moderately ventricose. Ventral valve regularly arched from beak to anterior margin, having the cardinal slopes somewhat straight, and the lateral margins con- siderablv compressed. Sinus shallow and broad, extending half way to the beak. Surface marked by numerous delicate, subequidistant, rigid, concen- tric stria?. Length 1*18 ; breadth 1'40. Akron, Ohio, 50 feet below the conglomerate. Whittlesey's Collection.^ This species differs from S. Hannibalen.tis, Swallow, in its less ventricosity, especially around the margin, and in the absence of concentric lamellae ; it differs from S. Missouriensis, Win., in its transverse form, more compressed lateral margins, and its numerous and regular concentric stria?. In the last character it resembles S. concentrica, but the mesial sinus (and probably fold) is much less marked. Spirigera Hannibalensis, Swallow, occurs in the Lithographic limestone at Clarksville, Missouri. White Collection of University of Michigan. SPIRIFERA, Sowerby. Spirifera centronata, n. sp. Shell of medium size, with an elongate, cus- pidate hinge margin, and, aside from the cardinal extremities, a somewhat semicircular general outline. Ventral valve of medium fulness near the umbo, somewhat depressed between there and the margins ; beak elevated above the cardinal line more than one-fifth the whole length of the valve, in- curved and overhanging a very narrow area. A distinct and comparatively deep sinus begins at the extremity of the beak, very gradually widening and becoming ill-defined in the middle of the valve and beyond. External surface marked by 36 to 40 ribs, of which from three to five fall in the mesial sinus. The ribs disappear on the alate cardinal expansions. One or two concentric furrows marking the middle region of the valve. Length along cardinal line, 1-23 (100); length from beak to anterior mar- gin, *52 (42); greatest convexity of ventral valve, -11 (9). NATURAL SCIENCES OP PHILADELPHIA. 119 i Museum of the University of Michigan. Collected by A. Winchell, at Cuya- hoga Falls, Ohio, in the flagstones below the conglomerate. Occurs also in Col. Whittlesey's collection from Akron, Ohio, 50 feet below the conglome- rate. This species is distinguished from all other spirifers by the association of cuspidate hinge extremities with a ribbed mesial sinus, and semicircular front margin. When the cuspidations are removed, the shell recalls S. Marionen- sis, Shumard, from the so-called Chemung of Missouri and Iowa ; and, in all except the semicircular outline it corresponds with S. cuspidatus, Hall, (not of Martin, ) from the Chemung of New York. Spirifera Sillana, n. sp. Shell transverse, broadest at about the middle ; anterior margin somewhat straight ; ends rounded anteriorly, sub-truncate from the extremity of the greatest diameter to the cardinal side. Dorsal valve of medium convexity, arched regularly from beak to anterior margin ; beak but slightly elevated above the hinge, incurved ; area narrow. A well de- fined mesial fold extends from the beak to the front margin, rising abruptly from the general surface, and arching regularly over. The fold is marked only by incremental lines, save a faint indication of two radial ribs in the vicinity of the umbo ; the other portions of the external surface are marked by one or two imbricating lamellae of growth, and regularly formed ribs which radiate without increase in number, from the beak ; eighteen or twenty of these can be distinguished on each side of the mesial fold. Greatest transverse length, 2-1 ; length from beak to anterior margin, 1-05; greatest convexity of dorsal valve, *20 ; width of mesial fold at anterior mar- gin, -45. This species is readily distinguished by having an elongate form, without having its greatest length along the hinge line. Collected by A. Winchell, at Valley Forge, one and a half miles below Cuya- hoga Falls, Ohio, in fine ferruginous sandstone underlying the conglomerate. Museum of the University of Michigan. Named in honor of Judge E. N. Sill, of Cuyahoga Falls, in acknowledgment of facilities afforded the writer in the examination of the rocks of his vicinity. Spirifera extenuata, Hall. This Burlington species occurs at Battle Creek, Calhoun county, and Germain's quarry, Hillsdale county, Michigan. •Collected by A. Winchell. Spirifera hirta ? White and Whitfield. A ventral valve of a spirifer dif- fering from the above only in the absence of all trace of a mesial sinus, and in its somewhat fainter radial lines. Bed "No. 6," Burlington, Iowa, while the typical specimens seem to come from Bed "No. 1." "White Collection" of the University of Michigan. Spirifera Vernonensis, Swallow, 1860. (Trans. St. Louis Acad. Sci. i. 644.) A specimen labelled as above by Dr. B. F. Shumard, from Sulphur Springs, St. Louis county, Missouri, too strongly resembles S. Carteri, Hall, 1858, (xth Rep. N. Y. Regents, p. 170,) judging by a specimen of the latter from Cuyahoga Falls, Ohio, which Prof. Hall admitted to be S. Carteri. Coll. A. W. Stringothtris Halli, Win. This peculiar form occurs at Battle Creek, Michigan. Collected by A. Winchell. SPIRIFERINA, d'Orbigny. Spiriferina Clarksvillensis, n. sp. Shell small, transverse, semielliptic, with coarse plications. Ventral valve rather ventricose, most elevated to- ward the beak, regularly arched from beak to anterior margin ; beak broad, projecting much beyond the hinge, strongly recurved ; hinge line nearly as 1865.] 120 PROCEEDINGS OP THE ACADEMY OP long as the greatest width of the shell, forming a rounded right angle with the short lateral margins ; area triangular, three and a half times as long as high, arched in the quadrant of a cylinder, striated in both directions, pierced by a foramen reaching to the very apex of the beak, nearly twice as high as broad, rounded at its upper angle. Mesial sinus deep, broad, regular, beginning at the apex of the beak, the bounding ribs forming with each other an angle of about 22° ; on each side of the sinus five large plications, of which only the first three reach the beak, the others terminating at the area ; these are crossed by sharp, neat, imbricating lamellae of -growth, of which, in the middle of the valve, about four occur in one-tenth of an inch. Dental plates short, columnar ; a median internal septum reaching from a point a little posterior to the teeth, as far as the middle of the valve, thick at the bottom, thinned to an edge above. Internal surface of valve marked with numerous indented punctations. Dorsal valve unknown. Length, -48 (71) ; breadth, -68(100); length of hinge line, -52(79); height of area, -15 (22) ; convexity of ventral valve, -22 (33). From the Lithographic limestone, Clarksville, Missouri. " White Collec- tion " of the University of Michigan. This species bears perhaps too close a resemblance to S. solidirostris, White. The single valve, however, on which the species is founded, is more convex, with more rounded ribs, less regular lamella?, a higher area and more incur- ved beak. This is the specimen referred to by White, (Boston Proc. ix. 25,) and doubtfully identified with S. subtexta, White— a Burlington limestone species. Spiriferina binacuta, n. sp. Shell of moderate size, transverse, with nu- merous rounded ribs and attenuate hinge extremities. Dorsal valve some- what ventricose in the middle, regularly arched from anterior margin to the beak, becoming depressed toward the lateral extremities. Hinge line elon- gate, thickened at the margin, abruptly acuminate. Area narrow and long. Mesial fold little elevated above the general surface, divided by a furrow into two ribs, which, in old specimens, are again divided ; ten or eleven rounded ribs on each side of the mesiaf fold, of which the last two or three are subob- solete. External surface finely and regularly lamellose. Substance of shell thin and apparently possessing a rather coarsely punctate structure. Length of hinge line, -78 ; length from beak to base, -30. This species is readily distinguished by its auricular acuminations and pli- cate mesial fold. From the base of the Burlington limestone. "White Collection" of the University of Michigan. Spiriferina solidirostris, White. From near Hamburg, Illinois. "White Collection." The ribs are more rounded than in the specimens from the Bur- lington sandstone. The same species occurs associated with S. binacuta in the base of the Burlington limestone. RHYNCHONELLA, Fischer de Waldheim. Rhtnchonella ? tetrapttx, n. sp. Shell minute, subcircular in outline, with few and deep plications. Ventral valve moderately convex, highest in the middle, with a straight projecting beak, which is circularly perforate at apex, with a triangular opening below to the hinge. Along the middle of this valve is a very deep and very narrow sinus reaching nearly to the beak, and bound- ed by a very prominent rib on each side, beyond which is another smaller rib, making four in all. Dorsal valve almost strictly circular, with the same con- vexity as the ventral, highest also in the middle, with the inconspicuous beak closely appressed, and the middle raised into a strong plication or rib corres- ponding to the sinus or furrow of the ventral valve ; on each side of this rib [July, NATURAL SCIENCES OF PHILADELPHIA. 121 is another strong one, and still beyond, a very feeble one. None of the shejl being preserved, no revelations are made of the minute structure. Length, -17 (100) ; breadth, -15 (88) ; thickness, -09 (53). Collected by A. Winehell, at Rockford, Indiana. Tbe straight beak of the ventral valve, and the general aspect of the shell, render the above generic reference unsatisfactory. Externally it seems to have some relations with Trematospira and Leptoccelia, of Hall, while it still more strikingly resembles Spififer Buchianus, de Kow, (Anim. Foss. pi. xv. bis fig. 3, and xix. fig. 6 ;) but until its internal characters are known, I leave it where it stands. Rhyxchonella heteropsis, n. sp. Shell small, varying from sectoriform to transversely elliptic, with moderately projecting be*£k ; very young speci- mens in tbe shape of a barley-corn. Plications sharp, ranging in number from ten to twenty ; of which three generally (sometimes two or four,) occupy the sinus of the ventral valve. This valve has a moderately sharp beak, turned back in an angle of 45° with the plane of the shell, and slit (in the cast) from the apex to the hinge ; sinus deep toward the front of the mature shell, wanting in the young one ; the plications on each side of the sinus vari- able ; four in those with two plications in the stnus, six, seven or eight in those with three, and five in those with four, making the whole number of plications ten to nineteen. These lateral plications are bent backwards in approaching the margin. Greatest prominence of ventral valve near the beak. Dorsal valve more ventricose than the ventral, most prominent at the ante- rior margin ; mesial fold much less marked than the sinus opposite, consist- ing of two, three, four or five plications, elevated at their extremities some- what above the lateral plications, the remotest of which exhibit a strong downward curvature -Beak of this valve concealed beneath that of its fel- low. Length, 38 (90) ; breadth, -42 (100) ; thickness of both valves, -28 (67). From one of the calcareous beds, "No. 4," of the yellow sandstone, Bur- lington. " White Collection" of the University of Michigan. Also near Ham- burg, Illinois, and at Weymouth, Medina county, Ohio. Whittlesey's Collec- tion. I had hoped that these varying forms could be brought under one of the numerous species already described from this group. It is a much smaller shell, with more abrupt sinus than R. pustulosa, White, from the same loca- lity. It is about the size of R. cameriftrn, Win., from Pt. aux Barques, but, besides wanting the long dental and median plates of that species, the sinus and fold are much more strongly marked, and the transverse diameter is re- latively greater, giving the rostral region less relative prominence ; and the mean number of plications is considerably less. In the rostral region it dif- fers from R. Sugeriana, Win., in the same manner, besides being a smaller shell with shallower sinus. Rhyxchoxella persinuata, n. sp. Shell of medium size, transversely oval, with abbreviated rostral extension. Cardinal slopes nearly straight, sides rounded, front straight. Ventral valve depressed, with about twenty straight plications, of which eight occupy the broad and rather shallow sinus. Ante- jior margin of valve abruptly deflected. Dental lamellae extending nearly one-third the length of the valve. The beak of this valve projects nearly in the plane of the shell, and the lateral portions of the valve are continued, without convexity, to the borders, thus giving this valve a peculiarly flatten- ed surface — the broad sinus forming a similar plane lying at a lower level. Transverse diameter, -67 (100); length, '52 (77); thickness of ventral valve, -16 (24). Burlington, Iowa, in the yellow sandstone. "White Collection ". of the University of Michigan. 1865.] 122 PROCEEDINGS OF THE ACADEMY OP This shell suggests Terebratula pleurodon, variety polyodonta, Phillips, (Geol. Yorks, pi. ii. p. 222, pi. xii. fig. 27.) It is a smaller species than that, with a shallower sinus and an abruptly deflected margin. Rhynchonella unica, n. sp. Shell minute, longitudinally ovate in outline, the sides and front equally rounded, the cardinal slopes somewhat straight and the beak acute. The peculiarity consists in the arrangement of the me- dian plications of the two valves. In the middle of the ventral valve are five sharp plications which extend to the beak ; the two outer of these are very prominent, projecting above the general surface like vertical laminae ; the middle three are anteriorly depressed considerably below the general surface, and constitute the mesial sinus, which extends to the middle of the valve, and thence rises above the general surface to the level of the two outer plica- tions. On each side of the median plications are four others, which, instead of converging toward the beak in conformity with the median ones, converge toward an imaginary point some distance in front of the beak, in consequence of which the posterior extremities of two or three are overlapped by the median set. In the dorsal valve four median plications rise in an elevated band and attain an equal elevation near the front of the valve, but posteriorly, the two middle ones of the four sink below the level of the others, and are lost from sight before reaching the beak. In consequence of these arrangements, the ventral valve presents a sinus anteriorly and an elevation posteriorly ; while the dorsal valve presents an elevation anteriorly and a sinus posteriorly. The two valves are about equally convex. The beak of the ventral valve projects in a tubular form slightly beyond that of the dorsal, and exhibits a circular perforation of the extremity. Length, -24 (100; ; breadth, -19 (79) ; thickness of both valves, -15 (62). From Bed " No. 4," Burlington, Iowa. " White Collection " of the Univer- sity of Michigan. Rhynchonella (Retzia ?) micropleura, n. sp. Shell of medium size, Retzia- like externally. Ventral valve ovate, somewhat produced rostrally, with rather straight lateral margins, and a semi-circular anterior margin ; most tumid near the beak, slightly flattened anteriorly ; beak somewhat incurved ; mesial sinus wanting or represented only by a slight flattening of the anterior portion ; surface with two or three varices of growth, and about 50 rigid, con- tinuous, rounded, radiating ribs, which are separated by narrower spaces. Length of ventral valve, -59(100); width, -48(81); convexity, -15 (25). Collected by A. Winchell, at Battle Creek, Michigan. It much resembles Retzia polypleura, Win., of the Huron group, but the beak is less prolonged and less straight, and the width of the shell is greater. 1 know of no Rhynchonella which like this is without a sinus, and so finely ribbed at the same time. In the first of these characters it is approached by R. Hubbardi and R. Sageriana, from the same rocks. Rhynchonella Hubbardi, Win. This species originally described from Mar- shall and Pt. aux Barques, Michigan, has since been found by the writer at Napoleon Cut in Jackson county ; and also rather plentifully in some of the thin layers of sandstone at Valley Forge, near Cuyahoga Falls, Ohio. It oc- curs also at Talmadge, Summit county, Ohio, in beds next below the conglo- merate. Whittlesey's collection. Rhynchonella Sageriana, Win. Identified in Whittlesey's collection from Weymouth, Medina county ; near Ashland, Ashland county ; Drew's saw- mill, Big Brook, Orange, Cuyahoga county, and two miles southwest of North- field Centre, Summit county, Ohio. R. Sageriana has remote relations to some of the forms of R. pleurodon, Phillips. Compare var. Vevreuxiana, De Kon. (Davidson's Mono. Brit. Carb. [July, NATURAL SCIENCES OP PHILADELPHIA. 123 Brach. pi. xxiii. iig. 19-21.) The ribs, however, are more numerous, and the frontal commissure more deeply sinuate. CENTRONELLA, Billings. Centronella Allei, n. sp. Shell large to medium size, terebratuliform, greatest width a little anterior to the middle, contained one and one fourth times in the greatest length. Ventral valve somewhat ventricose, full to the immediate vicinity of the margin, especially along the cardinal slopes ; regu- larly arching from beak to anterior margin, highest in the middle ; anterior margin with a barely perceptible truncation ; no -sinus or fold present ; beak produced beyond that of the dorsal valve, truncated and circularly perforate at the extremity ; dental lamellae more than one-fifth the whole length of the valve ; muscular scars, consisting of one faint median linear impression, on each side of which is another, all reaching to the middle of the valve. Dor- sal valve with its short imperforate beak closely concealed under that of its fellow, slightly truncate in front, but without mesial fold or sinus ; regularly arched from beak to front, highest in the middle, exhibiting a convexity equal to that of the opposite valve. Muscular scars consisting of a faint but distinct linear median impression, with a much deeper linear impression on each side, and a very faint one exterior to each of these — the three principal impressions reaching to the middle of the valve. Shell thin, stony and solid ; structure beautifully punctate under a lens ; general surface polished, mark- ed by a few feeble concentric lines of growth. Length of ventral valve, -66 (100) ; breadth, -41 (62) ; convexity, -19 (29). The dorsal valve above referred to comes from bed " No. b'," at Burlington; the other specimens are apparently from "No. 5." " White collection " of the University of Michigan. Also near Hamburg, Illinois, and at Talmadge, Summit county, Ohio. Whittlesey's collection. Though the peculiar loop of Centronella has not been seen in these speci- mens, the characters given are so closely conformable with that genus that the reference can scarcely be questioned in the present state of our knowledge. It is a larger, more ventricose and more elongated shell than C. Julia. Centronella Julia, Win. A single small specimen of this northern spe- cies occurs in Whittlesey's Collection, from "one mile east of Orange Center, Cuyahoga county, Ohio." Specimens of this species from Pt. aux Barques, have been employed by Prof. Hall to illustrate the characters of his genus Cryptonella, (Trans. Albany Inst. Feb. 3, 18(53, p. 4 ; reprinted Amer. Jour. Sci. [2] xxav. 399. J The re- ference of this species to Centronella was made solely in the light of Billings7 description and figure of that genus and comparisons with the internal struc- ture of Centronella glansfagea, the type of the genus. Prof. Hall asserts that the description and figure do not bear out the reference ; and, having pre- viously founded Cryptonella on the external characters of certain terebratuli- form species, he assumes that Centronella Julia affords an exhibition of the internal characters of Cryptonella. There is not the least doubt that the ori- ginal reference of Centronella Julia was correct ; and since its internal char- acters are assumed by Prof. Hall as being those of Cryptonella, the latter genus is thus admitted by its author to cover the same ground as the older genus Centronella, and must consequently pass out of use. Prof. Hall seems to have suspected this result ; for in a note interpolated in the New Haven edition of his paper, (p. 405,) he refers to a drawing of a specimen of C. glansfagea, showing the loop, (sent him by Dr. Rominger of Ann Arbor,) and admits that the loop " shows essentially the same character as that of Cryptonella.'''' He yet insists that this character is not to be inferred from Billings' original descrip- tion and figure ; and, expressing a doubt about the identity of Billings' type species (C. glansfagea) and the one figured by Rominger, "hesitates to 1865.] 12-1 PROCEEDINGS OF THE ACADEMY OF unite" Cryptonella and Centronella "until a reexamination of the original specimens of Mr. Billings shall confirm his first observations, or show them to correspond with" Cryptonella. It is this hesitation to admit the inevitable consequence, and to retract his honorable and friendly, but unfounded criti- cism, which induces me to reassert the correctness of my generic reference of Centronella Julia, resting as it does upon the original description and figure, and the observed characters of the type of the genus, as well as the subsequent confirmation of the author of the genus, himself. OSTREA, Linmuus. Ostkea rATERCCLA, n. sp. Shell adherent, thin, small, ovate, deeply boat- shaped, with the deeply excavated beak of the lower valve prominent, incur- ved and somewhat posterior. The muscular scar is large, transversely broad- reniform, concave on the cardinal side, situated nearly midway between the centre of the valve and its posterior margin, and is marked by two transverse lamellose lines. The deepest part of the valve is midway between the centre and the beak ; the depth is nearly the same for as great a distance on the other side of the centre. The exterior of the shell is irregular with concen- tric lamellose lines of growth. Greatest length, "65 (100) ; greatest width, *40 (61) ; greatest depth of lower valve, '25 (35) ; depth of cavity of the beak, *15 (23). From the buff sandstone at the base of the Burlington limestone, Burling- ton, Iowa. " White Collection " of the University of Michigan. The unexpected discovery of this oyster — believed to be the most ancient at present known — together with its somewhat cretaceous aspect, awakened a suspicion that it had not been found in place. To certify myself on this point, I addressed Dr. White on the subject, and received the following reply : "The Ostrea, if I remember rightly, was imbedded in a white or light gray, silicious material, of chalky appearance, containing some remains of dririoids and shells. My impression is, also, that it was from a quarry about half a mile north of my residence, and in the lower bed of the Burlington limestone, and not far from its base. I think the label which accompanied it, and also my letter at the time, may be entirely relied on. I admit the possibility of error, but I do not believe there is any." Ptebinea ceenistbiata, Win. (Carcliopsis crenistriata, Win., Proc. Acad. Nat. Sci. Phil. Sept. 1862, p. 417.) More perfect specimens from the typical locality of C. crenistriata reveal the fact that the species is possessed of an an- terior wing, which is a mere flattened portion of the anterior angle of the car- dinal line, with a barely perceptible sinus beneath. This feature does not belong to Carcliopsis as defined, and establishes a probable conformity with Pterinea. The right valves— recently discovered — might be mistaken for another spe- cies. They show no radiating lines, except near the hinge, behind the beak. The concentric markings are only small, irregular wrinkles of growth, with none of the sharply raised lines which characterize the other valve. It is of course possible that these right valves belong to another species, but as they have exactly the form of the crenistriated valves, and the latter are all left valves, it seems probable that they belong together. Ptekinea spinalata, n. sp. (Avicula acanthoptera t Win., Proc. Acad. Nat. Sci. Jan. 1863, p. 8 ; not A. acanthoptera, Hall, Geol. Rep. 10th Dist. N. Y. p. 263.) Careful comparison with the types of A. acanthoptera, Hall, convinces me that the Iowa specimens ought to be separated. The left valve of A. acan- thoptera, Hall, has the body of the shell broader than in the Iowa specimens, and. both wings are less defined. The right valves, also, are much Hatter. Amongst the Iowa specimens appear to be two types — one with the body of the valve arcuate, and the other with it straight. The former type was [July, NATURAL SCIENCES OF PHILADELPHIA. 125 adopted for the specific description, (see the paper referred to.) The latter may constitute the type of still another species. The species described as Avicula Whiter, Win., and Gervillia strigosa, White and Whitfield, should probably be referred to Pterinea in accordance with views recently put forth by Mr. Meek. Aviculopecten Caroli, Win. This species first described from the yellow sandstone at Burlington, Iowa, is found also in the base of the Burlington limestone at the same locality. "White Collection." Aviculopecten texuicostus, Win. A very small specimen, collected by A. Winchell, at Rockford, Indiana, seems to agree with the above Burlington species. Other specimens collected at Germain's quarry, Hillsdale, Michigan, have the same proportions and general surface characters, but they are once and a half as large as the Burlington types, and the anterior auriculation is marked by coarser, instead of finer striae. The body of the shell presents about 57 striae and the anterior ear 8. The foreign analogue of this species seems to be Pecten arenosus, Phillips. PERNOPECTEN, new genus. Etymology. — Perna and Pecten, from a combination of some of the charac- ters of the two genera. Generic Characters. — Shell bivalve, sub-equivalve, monomyary. Valves more or less inequilateral and auriculate. Hinge line straight ; hinge fur- nished with a central, triangular cartilage pit, and a transverse plate bearing on each side of the middle a series of smaller pits diminishing in size and depth from the centre outwards. The shell seems to be thin, and probably has a structure more like Pecten than Perna. This genus, or subgenus is founded on Aviculopecten linueformis, White and, Whitfield, (Proc. Bos. Soc. Nat. Hist. vol. viii. p. 295.) My attention was. first directed to the peculiarity of the hinge structure in two or three speci- mens sent me by Dr. White himself; and an examination of a number of spe- cimens previously referred to this species shows that they all possess it. The- genus Aviculopecten, happily constituted by McCoy to receive a number of paleozoic species having affinities with Pecten in their external form, and with. Avicula in their cardinal structure, is made by its author to differ from Pecten by the absence of a central ligameutary pit, and from Avicula by its nearly equilateral outline. The present genus differs from Avicula and Aviculopec- ten, and approaches Pecten and Monatis, in the presence of a mesial ligament- ary pit ; and it ditfers equally from Pecten, Aviculopecten and Avicula, and ap- proaches Perna, by the presence of a series of isolated ligameutary pits in the cardinal area. It differs from Perna in its sub-central beaks, with ligamentary pits on both sides. It agrees with Amusium in its sub-symmetrical ears, cen- tral cartilage pit, and the absence of radiating ridges, but differs in its straight hinge line and lateral cartilage pits. The position of the genus i* apparently between Perna and Pecten, with a preponderance of affinities for the latter, sufficient, perhaps, to throw it into the family of Pectinidw, White. Aviculo- pecten is grouped with the Aviculida. It is probable that in addition to the two following species,, others referred i to Avicula, Pterinea, and more especially Aviculopecten, Amusium, and Pecten, will be found to possess the assemblage of characters shown in Pemopecten Lima ? obsoleta, Hall, (Rep. 10th Dist. N. Y., p. 265,) = Pecten. subobsoletus, d'Orb., is stated to have a " crenulated hinge line," while its external char- acters are quite conformable to Pemopecten. Not improbably Lima glaber, Hall, belongs in the same association. The same may be said of, Pecten den- sistria, Sandb., from the Posidonomyenschie/er of Nassau ;- Avicula, tumida and. 1865.] 9 126 PROCEEDINGS OF THE ACADEMY OF Avicula laevigata, de Koninck, from the carboniferous limestone of Belgium, &c. &c. This genus is known to have existed in the Chemung of Phillipsburg, New York,* whence it probably continued to the epoch of the Burlington lime- stone. An uudescribed species occurs iu the fine grained sandstone of Ohio. Pernopecten lim^formis, Winchell. {Aviculopecten limceformis, White and Whitfield.) In this typical species, the number of ligamentary pits is about seven on each side of the mesial one. The hinge line is short, and the auri- culations are small and Lima- like. Pernopecten limatus, n. sp. Shell rather small, moderately ventricose, subcircular. Body of shell bounded by two straight lines diverging from the beak at an angle of 126°, and proceeding to the superior lateral margins, from which points the outline of the .^hell is very nearly circular. Hinge line straight, a little more than one-third the greatest width of the shell ; ears very small, flattened, subequal ; the anterior (of the left valve) making an angle of about 10(5* with the hinge line, and 120° with the body of the valve ; the posterior ear forming an angle of 129^ with the hinge line and 146° with the body of the shell. Beak small, inconspicuous, not projecting beyond the hinge line. Convexity of the valve nearly a segment of a sphere, a little more elevated in the umbonal region. Surface extremely smooth. Dimensions parallel with the hinge 1*20; at right angles with the hinge 1*05 ; length of hinge line *40 ; length of anterior slope of body of valve -59 ; of posterior slope -47 ; convexity of left valve '17. From the base of the Burlington limestone, Burlington, Iowa, a horizon identified by its fauna with the yellow sandstones below, (compare my paper, Proc. Acad. Nat. Sci. Phila., Jan., 1863, p. 25). "White Collection " of the University of Michigan. * The internal hinge structure of this species has not been observed, but the auriuulations are scarcely such as belong to Aviculopecten, as defined by McCoy, while they present a close conformity with the foregoing species. Aviculopecten occidental it, Win., differs from this in its longer cardinal slopes, making a smaller angle with each other, and in its longer hinge line, with larger and distinctly ribbed auriculations. Pernopecten Shumardanus, Winchell, {Avicula circulus, Hall, not Shu- mard). It is scarcely possible that the species identified by Hall (Iowa Rep. 022, pi. vii. fig. 9) as A. circulus, Shum., (Missouri Rep. 206, pi. c. fig. 14), can be the same species. Prof. Hall's figure and description do not show it ; nor do specimens from the same bed, commonly regarded as A. circulus, Hall, present satisfactory correspondence. The shell has a much shorter hinge line, with smaller ears, joining the cardinal slopes by obtuse angles. More- over the concentric lines are very regular, and the radial ones are faint, irre- gular dashes, entirely unlike the continuous and distinct though diminutive ribs of A. circulus, Shumard. Yielding to the suggestion of Dr. White, I formerly identified A. circulus, Hall -before I had seen actual specimens — with Aviculopecten limceformis, White and Whitfield. I am convinced, however, on careful comparison of specimens, that we must regard A. circulus, Hall, as a distinct species. In general characters this species resembles P. limatus, and only differs in its shorter and less sharply defined cardinal slopes, and the presence of the two systems of superficial markings. PINNA, Linnaeus. Pinna ? Marshallensis, n. sp. Shell small, equivalve, compressed, lance- olate, squarely truncate and gaping at the extremity opposite the hinge, and * I find tbat Prof. Hall has also marked this form as a distinct frenus. [July, NATURAL SCIENCES OF PHILADELPHIA. 127 acuniiiiately tapering toward the opposite extremity. Anterior side nearly straight, or distinctly hollowed. Posterior side parallel with the anterior for half its length ; toward the hinge gradually approaching the opposite side. The truncation is at right angles with the anterior side, leaving a broadly gaping ventral margin. External surface smooth. Length dorso-ventrally "97 (100) ; greatest dimension at right angles with this -26 (27) ; thickness of both valves -12 (12). Collected by A. Winchell at Napoleon cut, Jackson County, Michigan. MYALINA, DeKoninck. Myalina Lowensis, n. sp. Shell rather small, ventricose, obliquely elon- gate-quadrate. Umbonal ridge elevated, arched, highest about midway be- tween the beak and the opposite end, forming an angle of 50° with the straight, somewhat elongate hinge line ; anterior and posterior sides parallel, the former distended in a very shallow pouch just beneath the beak, the latter very slightly hollowed throughout its upper half ; basal region regularly rounded, with an obtuse angulation next the posterior side. From the umbonal ridge the slope is precipitous to the anterior margin, much less so toward the pos- terior, and it gradually subsides into a flattening toward the dorso-lateral angle. Surface of shell nearly smooth, marked with fine incremental lines. Greatest dimension — from beak to opposite extremity — -83 (100) ; length of hinge line *46 (55) ; diameter, at right angles with umbonal ridge, "41 (50). From the base of the Burlington limestone. "White Collection," of the University of Michigan. This species resembles M. angulata, Meek and Worthen, from the Chester limestone of Illinois, and M. Michiganensis, Winchell, from the Marshall group of Michigan. From the former it differs greatly in its smaller size, its shal- lower posterior concavity, and its less abruptly rounded base. From the latter it differs in having straighter anterior and posterior sides, giving it a more quadrate outline, a more elevated umbonal ridge, and a shorter antero- posterior dimension. Myalina Michiganensis, Win. Collected by A. Winchell at Napoleon Cut, Jackson County, and at Germain's Quarry, Hillsdale, Hillsdale County, Mich. Edmondia ? bicarinata, Win. A species apparently identical with this occurs in a conglomerate four miles north of Panama, Chataque County, New York, supposed by Prof. Hall, in his Report on the Fourth District of New York, to constitute a portion of the Millstone Grit of Pennsylvania. It was figured and briefly characterized under the name of Cypricardia contracta, Hall. The later specific name must therefore be abandoned. Edmondia jequimarginalis, Win. Specimens clearly identical with this occur in the same conglomerate with the above, as also in a conglomerate at another locality, supposed by Prof. Hall to underlie the Millstone Grit, and to constitute the terminal member of the Chemung Group. The specimens of these two species occurring in New York, as well as the two others to be mentioned, are preserved in Prof. Hall's cabinet ; and I desire to acknowledge my great obligations for the opportunity afforded of making the direct comparisons. Edmondia Burungtonensis ? White and Whitfield. A lamellibranch, too imperfect for certain determination, but closely resembling the above, occurs in Whittlesey's Collection, from a place "one mile east of Orange Center, Cuyahoga County, Ohio, 25 or 30 feet below the Grindstone Grit." SANGUINOLITES, McCoy. Sangdinolites sthigatcs, n. sp. A small species, resembling Area modesta Win., from Burlington, Iowa. Unfortunately the specimen was lost while awaiting a description. It had, however, been investigated and its generic 1865.] 128 PROCEEDINGS OF THE ACADEMY OF position fixed. Coming from a locality difficult of access, and poor in fossils, it seems proper to admit this reference to its existence. Collected by A. Wincliell at Point aux Barques, Huron County, Michigan, at the base of the Marshall group. Sanguinolites concentkica, Win., (Cardinia concentrica, Win., Proc. Acad. Nat. Sci. Phila., Sept., 1862, p. 413). Collected by A. Wine-hell at Alan's and Germain's quarries, Hillsdale, Hillsdale County, Michigan. This species is the analogue of Cardinia tdlinaria, Goldf. sp., (Petr. Germ, ii. ISO, pi. 131, fig. 17), but is more enrolled and more distinctly furrowed. It resembles also, in external characters, Allorisma Hannilmlensis, Shum. In the.original description of this species, "ventral," in the second line, should be changed to " vertical." Sanguinolites Hannibalensis, Win., {Allorisma Hannibalensis, Shum.) The single specimen collected by the writer at Alan's quarry, Hillsdale, Michigan, less resembles the original figure than it does the Burlington specimens re- ferred to this species. The Hannibal type is more elongate, with broader furrows. This species also occurs, satisfactorily identifiable, in both the conglome- rates spoken of under Edmondia. Cardiomorpha Julia, Win. Occurs at Napoleon Cut, Jackson County, Michigan. Collected by A. Winchell. Leda bellistriata, Stevens. This has been collected by A. W. at Alan's and Germain's quarries, Hillsdale, Michigan. CTENODONTA, Salter. Ctenodonta Hubbardi, Win., Nucula Hubbardi, Win., Proc. Acad. Nat. Sci. Phila., Sept., 1862, p. 417; ? = Nuculites sulcatina, Conrad, Jour. Acad. Nat. Phila., viii. p. 250, pi. xv. fig. 10). Collected by A. W. at Napoleon Cut, Jackson County. Amongst my collections from the Marshall group are numerous specimens generically closely allied to, if not identical with, Nucula, from which I have described N. Hubbardi, sectoralis, stella and lowensis — the latter having been originally described by White and Whitfield from the yellow sandstones at Burlington, Iowa. To the Iowa species I have added another — N. microdonta. These five species all present a line of teeth continuous from one side of the beaks to the other, without the ligamental pit which belongs to the modern species of Nucula. This variation attracted my attention at the very first ; and I observed that )the hinge characters seemed to identify the species with Tellinomya, Hall, and Ctenodonta, Salter. A species from the Hamilton group, and identified again in the Chemung group, had been described by the subse- quent founder of Tellinomya, as Nucula bellatula, (Rep. 10th Dist. N. Y., p. 196) ; and Nucula hians had also been recently described by him (xiii. Rep. N. Y. Regents, p. 110) from rocks of nearly the same age in Indiana, to say nothing of the description by Stevens of N. Eoughtoni, from the Marshall group. Without being acquainted with the details of the hinge structure of these species last mentioned, I yielded to the influence of example in referring my species to Nucula. I did this the more readily, as Prof. Hall had expressed the conviction (x. Report N. Y. Regents, p. 184) that Tellinomya would prove to be a Silurian genus. It may be added to this, that Nucula ventricosa, Hall, (Iowa Rep. p. 716, pi. 29, fig. 4, 5) does not possess the ligamental pit of a modern Nucula, although it offers rather important departures from Telli- nomya.* * A fossil from the Coal Measures of Lasalle, Illinois, usually identified with JV. venlricosa, Hall, exhibits no teeth whatever on the anterior side of the beaks, and thus presents generic characteis heretofore unobserved. This feature is shown in several separated valves mineralized by Pyrites. This character would seem to possess equal importance with the absence of the ligamentary pit, on which Ctenodonta has been founded. [July, NATURAL SCIENCES OF PHILADELPHIA. 129 The uninterrupted series of teeth possessed by the Nuculoid shells already referred to, from the Marshall group and its supposed equivalents, seems to constitute good grounds for a generic separation. For this hinge structure three names have been suggested. Nuculites was assigned by Conrad to shells having a continuous series of teeth and an internal clavicular ridge like C/i- dophorus. This genus has a real existence in the Hamilton group. Tellinomya has been applied by Hall, and Ctenodonta by Salter, to shells having the ge- neric charactersvof the species under consideration. As, however, objec- tions have been urged against the import of the name Tellinomya, and, on the other hand, Prof. Hall insists upon the rights of priority over Ctenodonta, (x. Report N. Y. Regents, p. 181), it becomes a delicate matter to decide between the two. But since the genus Tellinomya was not founded upon characters possessing generic value, while the real generic characters, owing to the state of preservation of the specimens, entirely escaped observation ; and, since the name proposed actually conveys a false idea of the relations of the genus, I feel constrained, in spite of my desire to perpetuate an American name, to pursue the same course as I do in regard to Athyris and other terms founded upon a misapprehension, and, in their meaning, at variance with facts. In regard to Ctenodonta Hubbardi, I desire further to admit the possibility that this is the species described by Conrad under the name of Nuculites sirt- catina. All that is stated in the description applies to this species ; and the figure also agrees. Nothing, however, is said or shown respecting the hino-e structure ; and both the description and figure will apply nearly as well to Sanguinolites concentrica, Win., which occurs abundantly at the locality whence Conrad's specimens were obtained ; while Ctenodonta Hubbardi, so far as I have observed, is unknown at that locality. The latter, nevertheless approaches nearest to Nuculites ; and it may be fair to presume that Conrad had a view of the hinge structure of the specimens he described. But it must be stated, finally, that not one of the hundreds of specimens that I have had in my hands, furnishes evidence of the existence of the internal septum which is essential to Nuculites and Cucullela. For the present, therefore, I feel compelled to regard Nuculites sulcatina, Con., as a species that has not \'et fallen under my observation. Conrad, in the paper referred to, has described Nuculites maclroides. If this is really a Nuculoid shell it approaches Ctenodonta sectoralis, Win., without being identical. If not a Nuculoid shell, as I suspect, it approximates Ed- mondia cequimarginalis, Win^ but at the same time, I could scarcely identify it. For the present, therefore, I leave it as I have left the species just refer- red to. Ctenodonta stella, Win. {—Nucula stella, Win.,) also occurs at Napoleon Cut, Jackson county, Michigan. SANGTJINOLARIA, Lamarck. Sanguinolaria rostrata, n. sp. Shell rather large, transverse, cuneate- ovate in outline, of medium convexity. Beaks two-fifths the shell length, from the anterior end, quite prominent, and rather strongly incurved. Great- est convexity above the middle, continuing along the postero-dorsal slope. Hinge line somewhat rmore than one-third the length of theNshell, slightlv an- gulated between the beaks ; buccal slope slightly curved, the anal nearly straight ; extremities obtusely rounded ; ventral margin nearly straight in the middle region, curved rapidly beyond. Longest dimension equidistant be- tween the beaks and venter. Pallial impression deep, without sinus (?) ; an- terior muscular pit deep on the rostral side, roundish-oval, striate radiately and concentrically ; equidistant between the beaks and extremity ; posterior muscular pit more elongate ; a feeble ridge extends from the beak ajong the inner border of each muscular pit — more perceptibly the posterior. In the right valve a strong triangular cardinal tooth stands just anterior to the point 1865.] 130 PROCEEDINGS OF THE ACADEMY OF of the beak, and is bounded posteriorly by a deep triangular pit, and ante- riorly by a shallower and narrower one. Nothing further is clearly known in reference to the hinge. The shell seems to be thick and externally smooth. Length, 1-72 (100) ; height, 1-13 (66) ; convexity of one valve, '34 (20); distance from beak to anterior extremity, "55 (32); to posterior extremity, 1 21 (70). Collected at Battle Creek, Michigan, by A. W. Resembles S. similis, Win., but differs in more prominent beak, greater convexity and straight ventral margin. Sanguinolaria similis, Win., occurs at Napoleon Cut, Jackson county, Michigan. CONULARIA, Miller. Conularia Newberryi, n. sp. Shell very small, in the form of a quadran- gular pyramid, (the apex of which has been broken off in the specimen de- scribed.) The pyramid is inclined over one of the angles. Angles of the pyramid slightly rounded, and marked by a shallow groove running longitu- dinally. Each side is marked by sharp, raised, transverse lines, which, in- stead of running directly across, are angulated in the middle, so that at this point they are nearer the base of the shell by a distance equal to once and a half the distance between two lines. The distance between the lines in- creases from above downwards, and is everywhere equal to about one-ninth the width of the side. These transverse lines have the appearance of the pro- jecting e'lges of septa, and are continuous from the middle of one of the shorter sides of the pyramid around to the same point, though the ends do not join but alternate in position. The sides of the pyramid are inclined at an angle of 30°, and, if they met at a point in the perfect specimen, it must have been about half an inch in length, with a width at base of about '17 inch. Collected by A. Winchell, at Cuyahoga Falls, Ohio, in the water limestone below the conglomerate. Named in honor of Prof. J. S. Newberry, M. D , equally distinguished in the service of science and of his country. BELLEROPHUN, Montfort. Bellerophon Whittleseyi, n. sp. (" Goniatitfi," figs. 1 and 2, Whittlesey, Proc. Amer. Assoc. Cincin., p. 219.) Shell rather large, globoid, rapidly en- larging, umbilicus moderately large, exposing one anterior whorl. Trans- verse section triangularly and broadly lunate, the dorsum being slightly ele- vated, and the dorso-lateral slopes slightly flattened; greatest diameter of section near the umbilicus. Keel rather distinct but with an indistinct band. Surface marked by raised, rather distant striae, which emerge from the umbi- licus with a slight backward inclination, and, curving forwards, pursue a course directly across the lateral surfaces for two-thirds the distance from the lateral to the dorsal angle, where they undergo a sudden deflection back- wards, making with themselves very nearly a right angle, and forming on the dorsum, by the meeting of opposite branches, a retral angle of 45°. Sinus not seen, but probably triangular and broad. Greatest diameter of whorl, *87 ; dorso-ventral diameter of aperture, '57 ; number of striae in one-tenth of an inch, near the aperture at the point where they turn backwards, 3 to 3J. This species resembles B. rugosiusculus, Win., in general features, but lacks the longitudinal decussating striae. It may be distinguished from all related species by the peculiar geniculation of the striae in the dorso-lateral region. One mile east of Orange Center, Cuyahoga county, Ohio, 20 or 30 feet below the grindstone grit. Whittlesey's collection. [July, NATURAL SCIENCES OF PHILADELPHIA. 131 Bellerophon nautiloides, Win., (Proc. Acad. 'Nat. Sci. Phil. Sept. 1862, p. 427.) Collected by A. W., at Alan's quarry, Hillsdale, Michigan. Conrad has described B. stamineus, from Moscow, Hillsdale county, Michi- gan, at which place I have observed both B. nautiloides and B. galericulatus, Win., and it is probable that he had one of these species in view in his de- scription. The ten words employed in the description, however, will apply equally well to half a dozen species of Bellerophon ; and it is hence utterly im- possible to avail myself of the results of his studies.* Bellerophon cyrtolites, Hall. This widely distributed species has been found at Alan's quarry, Hillsdale, Michigan. I Pugiuncuxps ? AC0LEATUS, Ha"ll. This Rockford species has been collected by A. W., at Alan's and Germain's quarries, Hillsdale, Michigan. Dentalium ? Barquense, Win., (Proc. Acad. Nat Sci. Phil., Sept. 1862, p. 425.) Additional specimens from the same locality, show that the short tubes supposed to belong to the shell structure, are not always normal to the sur- face ; and that when the internal cylinder is removed, so as to afford a view of the inner surface of the prismatic coating, the oblong sections of the prisms as they were applied to the cylinder, look somewhat like the polyp cells shown in longitudinal sections of some branching corals ; and there is seen also something like the same divergent disposition of the tubes. Moreover, the structure is extremely like that referred to in the last paragraph of my paper in the Proceedings for Sept. 1862, p. 430. This latter structure U folia- ceous, but occurs at the same locality. Can these rigid stems, then, be corals with very large hollow axes ? METOPTOMA, Phillips. Metoptoma undata, n. sp. Shell of medium size, nearly erect, apex nearly central, aperture transversely slightly elliptic; body of shell most inflated in the middle, somewhat acuminate toward the apex, and contracted at the aperture. Cast nearly smooth over the body of the shell, longitudinally un- dulate near and at the aperture, with a few wavy concentric lines of incre- ment. Height of shell, 1*15 (100) ; longest diameter of aperture, T06 (92). From Bed "No. 5," Burlington, Iowa. " White Collection" of the Uni- versity of Michigan. The inferior side of the only specimen seen is defective ; yet there are in- dications that it was flattened, as in the typical species of Prof. Phillips. Platyceras paralkjm, White and Whitfield. Identified in the Lithographic- limestone of Clarksville, Missouri. " White Collection." A variety more robust than the typical form, and wanting in the longitudi- nal folds which characterize the latter, occurs in the base of the Burlington limestone at Burlington. Platyceras vomerium, Winchell. From Sheldon's saw-mill, Big Brook, Orange, Cuyahoga county, Ohio, below grindstone grit. Whittlesey's collec- tion. The Ohio specimens have a dorsum not quite so acute as the Iowa types, and an aperture a little less expanded. PLEUROTOMARIA, Defrance. Pleurotomaria quinquesulcata, n. sp. Shell of medium size depressed — conical, consisting of three or four rapidly enlarging whorls. Outer whorl * In the 4th line of my description of B. galericulatus, (!oc. cit. p, 426,) fur " ventrally," read " retrally." 1865.] 132 PROCEEDINGS OF THE ACADEMY OF nearly as wide as all the others, having a nearly circular section, and pre- senting on its exterior about five broad longitudinal furrows, covering the space from the suture above to the base below ; shell otherwise apparently smooth. Diameter of last whorl, 1-07 (100) ; height of spire, about -72 (67). From the oolitic bed "No. 6," Burlington, Iowa. " White Collection" of the University of Michigan. This species is imperfectly known, though clearly distinct from all other species of this age, and hence deserving of notice. It is probable that the base is regularly rounded into a broad and deep umbilicus, and that the aperture is nearly circular. It calls to mind Euomphalus carinaius, Sow., from the " Aymesbuty limestone," but the sulcations are only half as numerous. A similar species exists in Whittlesey's collection, from " Sheldon's saw- mill, Big Brook, Orange, Cuyahoga county, Ohio, below grindstone grit." Pleurotomaria vadosa, Hall, (xiii. Rep. N. Y. Regents, p. 108.) To Prof. Hall's description of this species, founded upon casts, may be added the fol- lowing observations on the shell: The periphery of the body whorl is flat- tened into a sharp carina, just above which is another, heavier one, but not quite so projecting ; a concave belt separates these from another pair of ridges which lie near the suture, and are interrupted by numerous regular transverse rugulations rising into minute nodes, on the ridges. Collected at Rockford, Indiana, by A. Winchell. Straparollus macromphalus, Win. Specimens having twice the diameter of the types of the species, showing the tube septate a little more than one whorl back from the aperture. One specimen preserving the shell, shows that it was marked only by incremental lines. From bed " No. 1," and the oolitic layer, "No. 6." " White Collection " of the University of Michigan. Straparollus ammon, White. This Burlington species occurs in the so- called millstone grit of Western New York, and was figured as Euomphalus depressus, Hall, (Geol. Rep. ivth Dist. New York, p. 291.) Orthoceras Indianense, Hall. Collected by A. W., at Alan's and Ger- main's quarries, Hillsdale, and Napoleon Cut, Jackson county, Michigan. Nautilus (Trematodiscus) discoidalis? Win. A small fragment from Rockford, Indiana, affords strong presumption that this species existed at that locality. CYRTOCERAS, Goldfuss. Cyrtoceras Rockfordense, n. sp. Shell rather large, rapidly expanding, especially toward the aperture, apparently forming, in adult age, nearly a complete* whorl. In some specimens the transverse section is subcircular or laterally compressed, in others decidedly elliptic, being flattened dorso-ven- trally. The curvature is rapid for a shell of so large size, which renders it necessary that the chambers should be about four times as deep on the outer as on the inner side of the whorl. Septa deeply and regularly concave ; siphon small, situated close to the dorsal side. No surface markings are pre- served on casts. Transverse diameter of the last chamber, in a specimen wholly septate, 1-86 (100); dorso-ventral diameter, 1-35 (72) ; depth of chamber on the dor- sal side, -5;i (32); on the ventral side, -13 (7); diameter of siphon, -10 (5). In another specimen the transverse diameter of a section is 1-60; the dorso- ventral diameter, 170. Collected by A. Winchell, at Rockford, Indiana. It is impossible to affirm that this species did not describe one or more de- tached volutions. In case such was its character, it must have borne a close resemblance to Nuvtilus cyelostomus (Phillips) de Kon., (Anim. Foss. 553, pi. xxv. 1, a, b ; xlix 1, a, b.) [July NATURAL SCIENCES OF PHILADELPHIA. 133 Goniatites Allei, Win. The most perfect specimens seen were collected by A. W., at Germain's quarry, Hillsdale, Michigan. Apertural constrictions occur at regular intervals. Goniatites Marshallensis, Win. Collected by A. W., at Napoleon Cut, Jackson county, Michigan. Occurs also at Weymouth, Medina county, Ohio, 80 feet below the conglo- merate. Whittlesey's collection. PHILLIPSIA, Portlock. Phillipsia Doris, Win. (=Proetus Doris, Hall, xiiith Rep. N. Y. Regents, p. 112.) This species was established by Hall on some pygidia occurring in the Goniatite limestone at Rockford, Indiana. I am in possession of several pygidia from this locality which agree with his description, though in the ab- sence of measurements, it may be that his specimens are much larger. Associa- ted with these are numerous fragments of bucklers, which prove that the trilo- bite is a Phillipsia. The head is furnished with a border sloping downwards, and separated from the cheeks by a deep but narrow groove ; the middle of the border is marked by a groove which reaches from a point opposite one eye, to the corresponding point on the other side of the head ; in some speci- mens the latter groove reaches backward to the posterior borders of the buck- ler. The cheeks are raised abruptly above the border, and terminated by spinous points which are ornamented with raised longitudinal striae, aud ex- tend backwards a distance equal to one-third the whole length of the cepha- lic shield. The principal lobe of the glabella is in the form of a prolate semi-ellipsoid, is almost destitute of furrows, and is supported on each side by a large complementary lobe. The surface is obscurely granulose. The pygidium is in the form of a semi-ellipse, with the longer diameter trans- verse ; it is convex, with a gibbous axis, obtuse posteriorly, and articulated to the extremity. The lateral lobes are a little narrower than the axis, and their terminal points join the extremity of the axis. The pygidium is bor- dered by a plain belt curved downwards around its margin, and barely mark- ed by a continuation of the articulations* — except the two which bound it anteriorly. Number of segments in the axis, 1 1 ; in the side lobe, 7 ; surface the same as in the buckler. Width of pygidium, -35 ; length, *21 ; width of axis at anterior end, -12 ; width of border, -04. Length of buckler of another specimen, -31. Proetus Missouriensis, Shumard, (Missouri Report, p. 196, pi. B, fig. 13, a, b,) would seem also to be a Phillipsia, as well as its Ohio representative, Proetus auriculatus, Hall, (xv. Rep. N. Y. Regents, p. 107.) Pictet says of Proetus, "La glabelle est lob6e par des sillons," and of Phillipsia, "La glabelle est com- posee d'un grande lobe median simple, et de deux petits lobes latero-poste- rieurs."' Furthermore, Proetus Swallovi, Shumard, (loc. cit.J does not pre- sent the posterior termination of the great suture required by the genus to which it stands referred. Phillipsia Rockfordensis, n. sp. Cephalic shield surrounded by a nar- row, convex border, which is bounded internally by a narrow but deep groove, and terminates posteriorly in conically tapering genal points. The principal lobe of the glabella is relatively very large, convex, highest in the middle, widened anteriorly, circularly rounded in front, and gently curved on the sides ; no glabellar furrows are present. The complementary lobes are large, oval, and project laterally farther than the main lobe. The surface of the test of the glabella is finely, but sharply granulated ; that of the border is finely striated. Size about the same as that of P. Doris. Collected by A. W., at Rockford, Indiana. Cythere crassimarginata, Win. Collected by A. W., at Alan's and Ger- main's quarries, Hillsdale, Michigan. University of Michigan, Ann Arbor, 13th May, 1865. 1865.] 134 PROCEEDINGS OP THE ACADEMY OF On AMPHIBAMUS GRANDICEPS, a new Batrachian from the Coal Measures. BY PROF. EDW. D. COPE. The recent additions to oar knowledge of the air-breathing vertebrates of the carboniferous period, are of great interest to the comparative anatomist, as furnishing new points in the series of structures between the Ganoidea and Lacertilia, or new " generalized " types combining the structures of these and of the Batrachia. I owe to Prof. Jos. Leidy, of our University, a specimen of a reptile, belong- ing to the Illinois State Survey, in charge of Messrs. Meek and Worthen. It was discovered by the latter near Morris, Grundy Co., 111., in a bed belonging to the lower part of the coal measures. It is imbedded in a concretion of brown limestone. The casts of the bones are. occupied by a white friable mineral, which has probably percolated into them. This animal combines with its Batrachian, a few Lacertilian characters, having some resemblance to Dawson's genus Hylonomus, and much affinity with Prof. Wyman's Ranceps 1 y e 1 1 i i . Its squamous integument and narrow nasal roof give it the somewhat Lacertilian physiognomy, more especially Geccotian, in its broad cranium and orbits, its large marginal palpebral scales, and rather short digits. Its true affinities are indicated by the presence of two premaxillaries, with a squamoso-postorbital arch, as in Labyrinthodontia, some Batrachia Gradientia, and Crocodilia ; its quadratojugal arch as in Labyrinthodontia and Batrachia Salientia ; its posteriorly directed oblique quadratum and lack of ribs, as in Batrachia Salientia ; its probably short pelvis, short separate bones of the leg and fore-arm ; its opisthocaeliau dorsal vertebra;, and long caudal neural spines, as in Batrachia Gradientia. It is then the type of a group intermediate between the Labyrinthodontian and Gradient Batrachians, distinguished from the former by the opisthocoelian vertebrae, absence of ribs, and pleurodont dentition ; and from the latter by the scaly integument, absence of ribs, and structure of the nasal and pre- frontal regions. But one genus of Salamanders, Glossolega, has a similar os quadrato-jugale, and but a part of one family, the Salamandridte, the post- fronto-squamosal or posterior zygomatic arch. A ribless type might, however, well exist among Gradientia, when we consider the great difference between their developement in Pleurodeles on the one hand, and Amphiurna on the other. From the Salientia the dentigerous mandible, squamosal arch, form of vertebrae, sacrum and extremities, etc., widely distinguish it. To the Ba- trachian orders Labyrinthodontia, Gradientia, Gymnophidia and Salientia, the present may be added, under the name Xenorachia. The general form of the skull is much that of a frog, and large in proportion to the size of the animal; its length is one-half that of the spinal axis from the occiput to the middle of the sacral region, and five-sixths its own breadth in the flattened specimen. The outline is not broadly rounded, as is usual among Salamanders, but is slightly contracted, as in many frogs. The orbits are large, regularly rounded, their longitudinal diameter one 'and one-half times the frontal width ; their point of nearest approach is behind opposite the position of the iris; one diameter measured obliquely, in advance of each extends a little beyond the common premaxillary suture. The premaxillary bones have considerable horizontal extent, terminating opposite the narial openings, each bearing eleven or twelve teeth. Their nasal spines were in close contact, and do not appear to be prolonged backwards, as in most Gradientia. The external nares are rather widely separated, as in most Gradientia, the integument which they pierced roofing a large space be- tween the median and peripheric bones of the muzzle. The roof of the nasal cavities is a truncate cuneiform plate, whose apex joins that of the premax- illaries. Its composition can only be conjectured, from the appearances pre- sented by the specimen. It may be a superior ethmoid plate, as in the frogs [July, NATURAL SCIENCES OF PHILADELPHIA. 135 Borborocoetes and others, or, more probably, a united or separate pair of free frontal, as in Dactylethra or Rana. There is no trace of the composition of nasals and frontals which occurs in the Gradientia, nor is such an arrange- ment probable, in view of the regular elongate cuneiform outline of this singular piece. A moderately distinct suture crossing the front at the ante- rior third of the interorbital space, which presents a regular convexity for- wards, appears to be the anterior border of the frontal ; the latter can scarcely be an interorbital plate of ethmoid, as it appears to unite behind by suture with the parietals. There are bosses on the prefrontal region indicating prefrontal or " lachrymal " bones similar to those in Sceloporus and other Lacertilian genera. What I suppose to be the coronal suture, since it appears to be too regular to be a fracture, crosses the narrowest part of the interorbital space ; it is a zigzag, presenting posteriorly a median angle, and one on each side. The posterior zygomatic arches are strong, and bound a cranial plane, which is broader than long, and exhibits nearly parallel lateral outlines. The probably small " crotaphite foramina " of the temporal fossae appear to have been roofed over by perhaps the strong scales of the cranial integument. The quadratum is convex externally, and is directed obliquely backward to oppo- site the occiput; it is strongly concave in its posterior outline, indicating a large auricular meatus. Whether this was covered by scales or by an exposed tympanic drum, cannot be, determined. The quadratojugale is broad and strong. The postorbital arch is continuous with the quadratum; the breadth of the two equals the frontal width. The angular process of the mandible is but little prolonged beyond the quadratum. The maxillary is toothed at least as far as opposite the malar process. The dentition is pleurodont ; the teeth are only visible on the mandible and the outer edge of the upper jaw ; they are there of but one kind, small, closely set, acute-conic, not compressed, hollow, and without any inflections of the enamel. The integument of the head was squamous. The scales appear not to have been imbricate, and were perhaps more dense on the posterior regions, where their position is occupied by the white material before spoken of, which has here a somewhat ganoid appearance. They were more elongate on the muz- zle. There appears to have been a distinct superciliary, and a postorbital row, as well as a series on the border of the upper lip. A whorl of elongate scales arranged like the pieces of an arch, surrounded the one on each side which marked the crotaphite foramen. In the specimen these are connected by a suture or line, which is regularly convex posteriorly. The superior pal- pebrae were covered by small separated scales, as are seen among Geccos and Anoles, and were bordered by a larger and continuous series, of about four- teen subquadrate scales. These have evidently bordered the lid, extending transversely across the orbit, and were not sclerotic scales, which are arranged round the pupil as a centre. The vertebral column is much injured, especially in the cervical region. The dorsal vertebra? appear to have been short, and probably thirteen in number between the interscapular and sacral regions. They appear to have been constricted medially. Traces of ribs or of transverse processes are not to be found. The impression of a sacral vertebra is distinctly preserved. The caudal vertebrae were perhaps without osseous centra, as no definite im- pressions can be traced, and their place is occupied by the matrix. There are traces of osseous neural arches, perhaps similar to those of Archegosaurus, and apparently disconnected, long, compressed neural spines, and slender pleurapophyses ; the latter were probably united as chevron bones. Of the former, twelve very distinct impressions maybe counted to the sacral region ; the posterior are most slender, the median most elevated, the anterior lower, and of greater longitudinal extent. They are more expanded in the direction 1865.] 136 PROCEEDINGS OP THE ACADEMY OP of the axis of the body near their superior extremities, and evidently supported a flattened natatory tail, as that of Protonopsis. These neural spines were continued on the posterior third of the dorsal series. The visible, which is probably the greater part of the tail, enters the remainder of the column two and a quarter times, by measurement. Sternal and hyoid pieces are not recognizable, though sundry fragments are no doubt to be referred to these regions. An impression resembling that of a raniform scapula, was probably made by that piece. The anterior limbs were short and weak. The humerus is slender; its length equals the distance between the centres of the external nares ; it is apparently not much dilated, nor furnished with a process proximally, but is dilated and grooved distally, and has no condyles. The ulna and radius are separate and slender : the distal extremities of these, with the remaining bones of the anterior limbs, have been lost. Of pelvis nothing is recognizable. The femur is slender, much dilated distally, slightly curved in the posterior direction, and without condyles. Its length is equal to the breadth of the cranial table. The tibia and fibula are one-half the length of the femur, are slender, most dilated proximally ; the autero-exterfor bone is a little longer', not in contact with the inner distally, which relation I believe to be normal. The tarsus was probably cartilaginous, as in Protonopsis (Menopoma), a faint impression of the outer border remaining. It was broader than long, and without heel-like projections. While the great shortness of the lower leg is a Salamandrine peculiarity, the length and slenderness of the digits are quite Lacertian. The leg being extended backward, the exterior or first digit is shortest, and a little less than the second. This is equal to two and one-half phalanges of the fifth, (reckon- ing from its base,) or the. proximal pair of phalanges of the fourth. The fifth is a little shorter than the third, which is scarcely equal to the three proximal phalanges of the fourth. The number of phalanges is 3—3—4—5 — 4 : among the Salamanders the last two numbers are usually 4—3. They are without condyles, but exhibit one or two emarginations at their articu- lating surfaces. The length of the basal phalanx of the first digit is two- thirds that of the second ; the latter equals that of the fifth and the second phalanx of the fourth ; these are very little shorter than the basal of the third and fourth. The terminal phalanges are elongate acute, those of the first and fourth slightly curved. They are much less obtuse than in Salamanders, and the animal has probably had weak claws : of these no trace remains. A few traces indicate that the dermal integument was covered on the an- terior part of the body, at least, with small and subgranular_ scales. There have been abdominal scales arranged in narrow imbricate series, directed in- ward and posteriorly. Traces of plates are wanting, excepting a small frag- ment lying beside the cervical vertebrae. The length of this species from the sacral centre to the interscapular re- gion, was 13 lines ; from the latter point to the end of the muzzle, 12 lines ; to the occipital border, 4-5 lines. Longitudinal diameter of orbit, 3 lines ; frontal breadth, 2 lines ; from border of orbit to border of nostril, 1-5 lines ; breadth of cranial table, 3-75 lines. Length of humerus 3 lines; of femur, 3-6 lines; of tibia, 2-3 lines ; of fifth digit, 2-75 lines ; of fourth, 4-2 lines ; of first, 1-8 lines. The portion of the tail preserved measures 5-2 lines. If we compare the peculiarities of this genus with those of the Batrachia of the same period, we find it to be distinguished, independently of the ordi- nal characters, from such genera as Osteophorus, Melosaurus, Sclerocephalus, Xestorrhytias, Baphetes, and Brachyops, by the absence of the sculpturing of the cranial bones, the lack of dermal shields, characteristic of most of these, and by the presence of cranial and palpebral scales. The crania of the first genera are much more elongate, and imitate those of some Croco- [July, NATURAL SCIENCKS OF PHILADELPHIA. 137 dilia. Similar differences exist between the Illinois Batrachian and Dendrer- peton (Owen) ; the latter possesses also a double row of teeth. Hylonomus, (Dawson), supposed to possess Lacertilian affinities, exhibits ribs and bicon- cave vertebra. The ribs of Telerpeton will distinguish it also. The only genus as yet known to approach closely that under consideration, has been described by Prof. J. Wyman under the name of Raniceps.* This animal is only known from a study of the inferior aspect of a portion of the skeleton ; nevertheless it is certainly different, being nearly double the size, and having relatively longer and stronger anterior limbs. The angles of the mandible appear to have been considerably more incurved than in the Illinois species. They may have belonged to the same genus ; in that case the name here given will not prove superfluous, as the older appellation was previously applied to a genus of Gadid fishes. The name Amphibamus grandiceps has reference, first, to its two modes of progression ; its flattened oar-like tail enabled it to swim in the waters of the swamps. of the coal period, and its elongate, clawed digits indi- cate ambulatory power ; perhaps it climbed upon the low limbs of the Sigil- lariaa that rose above the water. The animal was most probably nocturnal in its habits. The humors of the eye could not have escaped far beyond their natural envelopes, so that the subsequently formed limestone has been hardened, and so fractured in nearly the form of the ball. On the fractured surface below and under the remaining palpebral scales, the mineral is dis- tinctly blackened, as by the pigmentum nigrum ; below the margin of the lid this is interrupted by a discoid spot of the form and dimensions of an iris, which presents a median lenticular vacuity, again revealing the pigment, ob- viously the vertical pupil of a nocturnal animal. The preservation of the out- line of color is certainly remarkable in a specimen of such great antiquity. A somewhat parallel case occurs in the preservation of the ink-bags of the Sepia? ; these do not date further back th*n the Jurassic. These appearances cannot be explained on any supposition of artificial production. August 1st. Mr. Cassin, Vice President, in the Chair. Twelve members present. The following paper was read and referred to a committee : " Descriptions of new species of fossil Crinoidea, &c." By F. B. Meek and A. H. Worthen. August Sth. Dr Ruschenberger, in the Chair. Ten members present. The following papers were read and referred to committees : " Notes on a species of Whale found in the River Delaware," By E. D. Cope. " On some Conirostral Birds from Costa Rica." By John Cassin. * Anier. Journ. Sci. and Arts, 1858, p. 158. 1865.] 138 PROCEEDINGS OF THE ACADEMY OF August 15 th. Mr. Cassin, Vice President, in the Chair. Eight members present. The following papers were read and referred to committees : « New Polyzonidse." By H. C. Wood, Jr., M. D. " On a new genus of Vespertilionidae." By H. Allen, M. D. August 22 J. Mr. Cassin, Vice President, in the Chair. Eight members present. August 29 th. The President, Dr. Bridges, in the Chair. Eleven members present. On report of the respective committees, the following were ordered to be published. Remarks on the genus TAXOCRINTJS, (Phillips) McCoy, 1844; and its relations to FORBESIOCRINUS, Koninck and Le Hon, 1854, with descriptions of new species. BY F. B. MEEK AND A. H. WORTHEN. The genus Taxocrinus, Phillips, as published by McCoy in 1844, (Carb. Foss. Ireland, p. 178,) was founded upon Cyathocrinus ? macrodaclylus, Phillips, and Taxocrinus polydactylus, McCoy, both of which are described, and the latter figured by McCoy, as if- composed of five basal pieces directly alternating with the five radial series, the latter forming free arms without any interra- dial or anal pieces between. Phillips' figures of T. macrodactylus, however, (Palaeozoic Fossils, pi. xv.,) particularly his figure b, certainly shows a small interradial piece wedged in between the truncated superior lateral angles of two of the first radial pieces. From these illustrations, therefore, as well as from the fact that in redescribing the genus in 1851, according to the later im- proved nomenclature of the parts, (Brit. Pal. Foss. p. 51,) McCoy distinctly says " five hexagonal interradial plates intervene between the second primary radials, resting on the upper lateral edges of the 1st do.,"* it is manifest that there is generally, if not always, one or two ranges of interradial pieces, in adult examples of what are regarded in Europe as typical species of this genus, when found entire. * From the species included, as well as from that author's usual method of describing these parts of crinuids, it is obvious that by,the words " five hexagonal interradial plates intervening, Ac," he means a single piece occupies each of the five interradial, or rather four interradial, and one anal spaces. [Aug. NATURAL SCIENCES OP PHILADELPHIA. 139 The genus Forbesiocrinus, proposed by Koninck and Le Hon, in 1854, (Re- cherch. sur les Crinoides, p. 118,) was founded upon their F. nobilis, which they think probably the same as Poteriocrinus? iiobilis, Phillips, originally included by the latter author in his lsocrinitis, for which the name Taxocrinus was af- terwards substituted, when he became aware of the fact that Isocrinus had been previously used by Meyer for another group. In their description of Forbesiocrinus, Koninck and Lehon characterize it as having five basal pieces, alternating with five series of primary radials consisting of four pieces each, with the anal and interradial spaces each occupied by from 12 to 13 pieces, and the axillary spaces by three small pieces each. From all the descriptions and illustrations yet published, of the groups Taxocrinus and Forbesiocrinus, it is therefore clearly evident that these two types as understood by European authors, are distinguished by Taxocrinus having but one or two ranges of interradial pieces, or none, and Forbesiocrinus having from 12 to 13 of these pieces occupying each interradial spaces, and a few small pieces in the axillary spaces above. In all other points of struc- ture, and arrangement of parts, whether of the column, basal, radial or arm pieces, they are understood and acknowledged to agree exactly. But as it has been found that typical species of Forbesiocrinus, possess three more or less developed basal pieces within or beneath those regarded as such by Kon- inck and Le Hon, (Iowa Report, p. 628,) it might be supposed this character would aid in distinguishing the two groups. It is well known, however, that American typical species of Taxocrinus, without interradial or anal pieces, or with but a single range of the two, such as T. Thiemei and T. juvenis,= [Forbesiocrinus Thiemei and F. fuvenis, Hall, Jour. Bost. Soc. N. H. vii., 317 and 318,) possess precisely the same structure, being both described as having small basal and subradial pieces.* Nor can we make the presence of inter- axillary pieces, or the small patelliform supplementary pieces, so often seen at the sutures of the radials in well defined Forbesiocrinus, a means of distinc- tion, since neither are always present in otherwise typical forms of that group with the interradial spaces filled with plates ; while well marked spe- cies of Taxocrinus, such as T. Thiemei and T. juvenis, Hall, (sp.,) the first with- out anal or interradial pieces, and the latter with the " interradial and anal series consisting of one plate each," are described, the first as having " arm joints showing the small patelloid plates very distinct," and the latter, with " the small patelloid plates indicated by the strong curvature of the suture lines of the radial plates, becoming more distinct in the arm plates." So if we attempt to distinguish ihese groups at all, we must fall back upon the dif- ference of the one group being without anals or interradials, or with but one or two ranges of these pieces, and the other with a greater number. Now, however well this difference may serve to separate into two groups the few known European species, an attentive study of our more nume- rous American forms has shaken our confidence in the possibility of separa- ting all the species hitherto discovered, into two sharply defined genera, until some more reliable characters can be pointed out. Our reasons for this conclusion will be better understood by consulting the following list of 22 American and European species and varieties, with a tabular statement of the number of the various parts of each.f * Our Taxocrinus gracilis, of this paper, with a single series of interradials, shows clearly three small pieces uuder the five considered the basale, by most authors. t We have not included Taxocrinus inter scapular is, Hall, (Iowa Report, pi. i. fig. 3,) in this list, because it deviates from the typical forma of the genus, and seems allied to Dimerocrinus. Phillips, though differing trom that genus in not having the arms composed of a double series of minute interlocking pieces, as well as in some other points of structure. 18H5.] 140 PROCEEDINGS OE THE ACADEMY OF D SB HH e o o m W is K O Ph D 5 o o o EH S ^ O «J4 -O C3 ■a . a o o T3 a < c4 CD 3 fl o o ^3 c- bD =3 V CO o to o to o m tj< ro in ^ co o "* CO o o >Tt- ! d 3 c3 : is a ■ 0 co a> : a * a i a O O -* •— ' f-r 3 r-i co CM ^ O . q a, a, Ex O ^h —i .—1 .— i ~ a — .-. CO -^^ ^ ST CO o a o CO (75 o o o i— IHHOtOH«0H 3 o 3 S ►»§ = a s O ■^ o © ** co in o 2 © CM Sin in cm cm o ° ° ■^ © © —I •M i— i — CM (M + By referring to the description and diagram of Forbesiocrinus Agassizi, (Sup. Iowa Report,) nages 6fi and 67. it will be seen that one ofthe subradial pieces is there by an oversight described as the first anal. It is also worthy of note, that the diagram there given, shows clearly five basal pieces. If this is correct we may doubt the propriety of placing this species in the genus It has not b?en considered necessary to mention in this table the number of basal pieces, be- cause both groups agree in having three of these pieces. t Messrs Lyon and Casseday described this species as the type of a new genus Onyctwcrinus, in 1859. We do not see, however, that it can be distinguished from Furbesiocrinus, as now under- stood. r . [Aug. NATURAL SCIENCES OP PHILADELPHIA. 141 From this statement, it will be seen that, starting from such forms as Taxo- crinus poly daclylus, T. Thiemei, &c., without interradial or anal pieces, we pass by a very easy gradation through the young of T. communis, having a single range of granules representing interradials, to the adult of the same, with one well developed interradial in each space, and one anal surmounted by two or three granules. Then we have several other species, with a single range of interradial and anal pieces, after which we pass to T. ramulosus, with one interradial, three to six anals, and three interaxillary pieces, and then to T. tuberculatum, with two interradial and two anal pieces in each space ; after which we have F. asterixformis, with its four interradials and four anal pieces. Continuing down the list, we find, as we pass from species to species, the number of these intermediate plates increasing as gradually as we could ex- pect these pieces in species of the same genus of crinoids to do, until we ar- rive at F. Worlkeni, with its thirty or more interradials, and twenty or more anals. Nor is it probable this is the maximum number of these pieces some- times visible between the rays, since it is known that in some species, such as F. exculptus, Lyon and Casseday (sp.), they continue on up, and pass with- out change or interruption, into a series forming a solid dome above. Hence it is probable that in the typical forms of Taxocrinus, without interradials, or but one or two rauges, and long ponderous rays, such as T. macrodactylus, T. polydactylus and T. ramulosus, the visceral sac corresponded in size with that of the column and rays, or in other words, extended as far up at least as the second bifurcation, and that it was merely protected by a dermal enve- lope between the rays aud above. The fact that this integument protecting the softer parts, may have, in some instances, merely secreted a rudimentary piece at the bottom of each interradial space, or one or two well developed plates, or filled the whole space partly or entirely, or continued the process of secreting calcareous matter, until the whole summit was arched over with a solid vault, although probably presenting in the various degrees of this process good specific differences, can scarcely, we should think, be regarded in this group as presenting sufficiently important characters for the distinc- tion of genera, especially when these differences are not coincident with any other peculiarities. In addition to this, when we bear in mind that different sized individuals of the same species, as in Forbesiocrinus Agassizi and F. ez- culptus, the number of interradial pieces are acknowledged to vary in the first instance from fifteen to twenty five, and in the second from twenty to twenty- five, we can readily understand that some caution is necessary in basing even specific distinctions on these differences alone. Nor on the other hand, if we direct our attention to the primary or second- ary radial pieces, or to the arms, do we see anything to sustain the generally accepted distinction of two genera in this group ; for, if we make the radial series, for instance, a basis of classification, we would have, as may be seen by glancing at the 5th and 6th columns of the foregoing table, to place Taxo- crinus nuntius, without anals or interradials, not only along with Forbesiocri- nus spimfer, with its single range of interradials, but with F. Agassizi, -with its thirty to forty anals, and twenty-five to thirty interradials. The same me- thod would also place a variety of F. Meeki with seven interradials in the same group with Taxocrinus juvenis, Hall, with its single range of interradial pieces. Now from these facts, it must be evident, we think, that if Forbesiocrinus is to be retained as a distinct genus from Taxocrinus, it will have to be separated upon some characters or differences not yet observed. Hence, although we shall continue to use the two names, for the sake of convenience, ranging un- der Taxocrinus species without interradial or anal pieces, as well as those with one or two of each ; and under Forbesiocrinus, those with a greater num- ber of these pieces, we shall do so — at least until better evidences of their being distinct genera have been adduced — with the understanding that we 1865.] • 10 142 PROCEEDINGS OF THE ACADEMY OF regard the latter group as a section or subgenus under the old name Taxocrinus. In this sense, then, we leave under the names Forbesiocrinus, our F. Monroensis and T. Nonvoodi, as well as all those mentioned in the foregoing list from No. 12 to 22 inclusive. Our FJ semiovatus, however, seems to be a typical Taxo- crinus, and its name should be written Taxocrinus semiovatus. The species Forbesiocrinus nun tins, F. Thiemei, F. communis, F. Kellogi, F. spinifer, and F. juvenis, of Hall, we regard as likewise typical forms of Taxocrinus, and hence their names should be written Taxocrinus nuntius, T. theimei, T. communis, T. Kellogi, T. spinifer, and T. juvenis. Taxocrinus gracilis, Meek and Worthen. Body small, expanding moderately from the base. Basal pieces small, and looking like the last joint of the column divided into three pieces ; subradial pieces so small and narrow as to allow the lower middle extremity of the first radials to come nearly, or in some instances, quite down upon the basal pieces ; four of them triangular and more or less wedge-shaped so as to pro- ject up between the first radials as much as half the length of the latter ; the fifth one larger than the others, but slightly tapering, and truncated above by the anal? piece, so as to present a quadrangular or subpentagonal outline. First radial pieces considerably larger than the subradial, of nearly equal length and breadth, or a little wider than long, hexagonal in form, the infe- rior sloping, and upper horizontal sides much longer than the others. Se- cond radials, in four of the rays, shorter than the first, wider than long, and generally hexagonal ; in the fifth ray of the specimen under investigation, the second piece has its right margin enormously, and perhaps abnormally, developed, and extended obliquely upwards, so as to fill the whole interra- dial space above the comparatively minute interradial piece, quite up as far as the second bifurcation of the rays, with one solid plate. In the ray con- taining this singularly developed second piece, there are two other primary radial pieces succeeding it, of near the natural size and form, upon the last (fourth) one of which the first bifurcation takes place ; after this each of the divisions bifurcates again on the fourth piece, and the two inner subdivi- sions again on the fourth piece, while the two outer ones send off" subdivi- sions, one on the sixth, and one on the seventh piece. In the ray immedi- ately to the right of that just described, and apparently the anterior one, no division takes place until upon the eighth piece, all the pieces between the se- cond and eighth being transversely oblong or about twice as wide as long, and gradually diminishing in size. In the other three rays, the first division takes place on the third piece, and the second and third divisions also on the third piece, the arms rather rapidly diminishing in size with each bifurca- tion. Interradial pieces very small, rather longer than wide, somewhat wedge- shaped above, and resting between the short superior lateral sloping sides of the first radials, and supporting on each superior sloping side a short trun- cated margin of the contiguous second radials, which generally meet over the little interradial, so as to isolate it from the free space above, though not always. Anal piece a little larger than the interradials hexagonal in form, and resting with one short side upon a truncated upper side of the largest subradial ; while it connects on the right with a first and second primary radial, and on the left with a second and third primary radial, and one first secondary radial. Surface of body apparently smooth, but showing granules on some of the divisions of arms. Patelliform accessory pieces not developed between the primary radial pieces, but quite distinct between some of the secondary. Column, as in other species of the group, round and tapering downwards from the base, near which it is composed of very thin pieces. This species, although somewhat like T. intemcapularis, Hall, (Iowa Report, [Aug. NATURAL SCIENCES OF PHILADELPHIA. 143 pi. 1, f. 3,) from the same locality, will be at once distinguished by its more spreading rays, greater interradial and interbranchial spaces, and particu- larly by its proportionally, smaller and shorter interradial pieces, as well as by haying the latter resting upon the superior lateral truncated sides of the first radials, instead of upon one of the second, while it has no interaxillary pieces as seen in T. inter scapular is It likewise shows some differences in the bifurcations of its arms, after the first division. A marked feature in the specimen from which the description was made out, is the extraordinary development of the right margin of one of the se- cond primary radial pieces, by which it is made to fill the entire adjacent in- terradial space. This, however, as already stated, is probably abnormal. Locality and position. New Buffalo, Iowa. Hamilton division of the Devon- ian. Descriptions of new species of CRINOIDEA, &c , from the Palseozoic rocks of Illinois and some of the adjoining States, BY F. B. MEKK AND A H. WORTHEN". RADIATA. ECHINODERMATA. CYSTIDEA. Genus COMAROCYSTITES. Billings, 1854. Comarocystites, Billings, Canadian Journal, vol. ii. p. 269, 1854; Report Geol. Survey Canada, p. 288, 185(3 ; Decade iii. Canadian Organic Remains, p. 61, 1859. "Body ovate, the smaller extremity being the base ; pelvis small, of three plates, above which are from eight to eleven irregular rows of plates, mostly hexagonal; mouth near the summit provided with a valvular apparatus; arms free, grooved, and composed of a single series of joints bearing pinnulse ; ambulacral orifice in the apex between the arms ; celumn round and smooth. The plates of the only species that has been collected present, in some conditions of preservation, a peculiar vesicular structure of their exte- rior surfaces, while sometimes they are solid and smooth." "Generic name Comaron, a strawberry." Comarocystites Shumardi, M. & W. Body obovate, the summit being more broadly rounded than the lower ex- tremity ; height about one-tenth greater than the breadth. Basal pieces wider than long, irregularly heptagonal and octagonal, extending out hori- zontally from the column, and having, at two of the sutures, small supple- mentary pieces wedged in between, so as to come nearly in contact with the end of the column. Succeeding ranges of plates above, five, very irregularly arranged, and differing in size and form, but increasing in diameter from below upwards, mostly hexagonal or heptagonal in form ; all deeply con- cave on the outside, with prominent sharp carinse at the sutures ; when these angular prominences are weathered or worn, slit-like pores are se«n passing through the sutures, which they cross at right angles, being partly common to each of the contiguous plates. Height, 1*50 inch ; breadth, 1-30 inch; greatest breadth of one of the plates next 10 upper range, O-M inch. Arms and openings of the summit unknown. This species is nearly allied to C. punctatus, Billings, the type of the genus, from which it may be distinguished by having only five ranges of plates above the base, instead of seven or eight, as well as by the greater size. of the plates 1865.] 144 PROCEEDINGS OF THE ACADEMY OF i near the summit, some of which measure as much as three times the diameter of those of the corresponding pieces in the Canadian species of equal size. It is true these are probably, to some degree, variable characters in this genus, but not, we should think, to the extent exhibited between the Canadian species and our specimens, in which latter they are constant. Again, where the sutures of our species have been worn so as to expose the perforations, they are seen to be less crowded, and not so numerous as in C. punctatus, while none of the plates, even where apparently perfectly preserved, show any traces of surface stria?. The deep concavity of the external surface of the plates in this genus, and the sharply carinated character of the sutures between, together with the irregularity in the size, firm and arrangement of the plates, give a very pecu- liar appearance to the fossil, that might, at a first glance, cause it to be mis taken for a coial. When only found in the condition of detached plates, they present a singular appearance, well calculated to mislead even an experienced palaeontologist who had not seen the entire fossil, or enough of the plates united, to show their true characters. The fact that they are all deeply con- cave, and when unworn, smooth on the outside, while the inner side is convex and strongly rayed, would naturally lead to the conclusion that the outside is the inner side, and vice versa. When a few of the plates are found united, however, it is at once seen that the deep concavity is on the outside, and the convexity and rajs within. These rays extend one from the prominent middle of each plate to each of its sides, where they connect with those coming from the middle of the adjacent plates. When three or four of the united plates are placed with the inside upwards, the spaces between the rays are seen to present the form of deep, triangular pyramidal cavities, the apex of each cavity terminating at the meeting of the corners of each three of the con- tiguous plates. The rays are as prominent as the convex centres of the plates, and quite narrow or linear within, but widen rapidly towards the outside of the plates. They are also each split longitudinally into parallel laminae by a series of profound tdits extending nearly to the outer surface of the plates, and it is these slits that are seen, like pores, at the prominent angular sutures, where the edges of the plates at the latter have been worn partly away. It is difficult to understand the use of these deep slits, or divisions of the internal rays, since, as noticed by Mr. Billings, they seem never to pass entirely through the plates, excepting where the prominent edges of the latter have been worn away. Named in honor of Dr. B. F. Shumard, of St. Louis, whose labors in western geology and palaeontology are well known. Locality and position. —Cape Girardeau, Missouri. Trenton division of Lower Silurian. Comakocystites Shumakdi, var. obconicds, M. & W. A single specimen in the collection from the same locality and position as the species, just described, differs in being obconical instead of obovate, its lower half tapering downwards gradually to the column. Its basal plates also rise nearly vertically from the column, instead of extending out horizontally as in the typical form of C. Shumardi. It has a part of the column attached, showing it to be very nearly cylindrical, and composed of thin plates. In form this specimen agrees nearly with Mr. Billings' figure 2, plate 5, decade iii., Geol. Survey of Canada, from which it differs in having only five ranges of plates above the base. It also agrees with the species we have just de- scribed, ia having its plates above the middle proportionally larger, one of these plates in a specimen only 0-72 inch in height, measuring nearly a third more in diameter than those of Mr. Billings' species near 1*50 inches in height. It is quite probable this form may belong to a distinct species, but as we [Aug. NATURAL SCIENCES OF PHILADELPHIA. li.r> are not clearly satisfied that this is the case, we merely call attention to it as a variety of C. Shumardi. Locality and position, same as last. CRINOIDEA. Genus POROCRINUS, Billings, 1856. Porocrinus, Billings, Report Geol. Survey of Canada, 1856, p. 279 ; Canadiau Org. Rem. 1859, Decade iw, p. 33. Generic formula. — Basal plates 5. Proper interradials 0. Subradials 5. Anals . 2. Radials 1x5. "Cup conical; basal plates five, pentagonal; subradials five, three hexa- gonal and two heptagonal ; primary radials five ; one large azygos interradial supported on the truncated summit of the anterior subradial, and one small one, situated over the suture between the anterior subradials, and having above it on one side the large azygos, and on the other the left anterior primary radial; several small pectinate! rhombs similar to those of the C)Jstidea.,, [Billings]. As remarked by Mr. Billings, this genus has the structure, so far as the form and arrangement of the plates forming the base and lateral walls of the cup are concerned, of Poteriocrinus and Cyathocriims ; from botli of which it differs in the important character of having pectinated openings analogous to those of the Cystidea. Our specimens of the following described species also show that this inte- resting type also presents another character in common with some of the Cys- tidea— that is, the possession of several large rounded, non-pectinated open- ings above. Of these openings there are three, one on the anal side, and two on the anterior side. They are all nearly on the same horizon as the bases of the free arms, though the anal opening is a little lower than the other two. So it would seem this genus presents, as it were, a combination of the cha- racters of the Orinoidea and Cystidea. With the regularity of structure and arrangement of parts of a true Crinoid, it has the pectinated and other open- ings of a Cystidean. It differs, however, from the Cystidea in having the pec- tinated openings located at the junction of the corners of the plates, instead of passing through them near one of the sides, while the little bars protecting these openings are arranged obliquely, instead of at right angles to the mar- gins of the plates, as in the Cystidea. Our species also shows that the conical form of the cup is not a generic character. POROCRINUS CKASSOS, M. & W. Body subovoid or a little higher than wide. Base depressed, rather widely truncated below, pentagonal in outline, two and a half to three times as wide as high, with a comparatively large pentagonal central perforation ; basal pieces wider than long, pentagonal in outline. Subradial pieces twice to three times as large as the basal, about as high as wide, three hexagonal, and two on the anal side heptagonal. First radial pieces of about the same size as the subradials, apparently all irregularly heptagonal, each with, near its upper extremity, a small outward sloping subcordate, or oval, flattened sur- face for the articulation of the second (first free) radial piece ; four of them with each* one, and the fifth with two, of the superior lateral margins deeply sinuous and forming in part the margins of the large rounded openings of the summit. Anal pieces two ; the first smaller than the other, quadrangular in form, resting between the superior sloping sides of two of the subradials, and supporting, on its right upper sloping edge, one side of one of the first radials, and on its left one of the oblique sides of the second anal piece. 1865.] 1 4G PROCEEDINGS OF THE ACADEMY OF Second anal oblique, wider (obliquely) than its diameter in the direction of its vertical axis, irregularly pentagonal, resting with its base upon the upper truncated side of one of the subradials, and its left side against one of the first radials ; while its upper right margin connects with another, and its sinu- ous oblique superior side forms the under margin of the anal opening. Pec- tinated areas situated in deep excavations, those at the angles of the basal and subradial pieces largest, and obscurely trilobate ; the smaller ones at the angles above oval or subcircular. Surface ornamented with strong radiating costse extending from the centre to each of the sides of the plates, and all widening from the centre outwards. Sutures distinctly furrowed, even on the truncated under side of the base. Length 0-72 inch ; breadth about O66 inch. This species will be at once distinguished from P. conicus, of Billings, the typical species of the genus, by its oval instead of obconic form, (being widest a little below the arms, and rounded in above), and the strong radiating cos- tse of its plates. We know of no other form with which it need be compared. Like the typical species, its free arms commenced with the second radial, and were evidently slender, and nearly cylindrical, or a little compressed late- rally, and provided with a very small furrow above. We have not seen the column, but it appears to have been large at its connection with the base. Nor have we been able to see the structure of the small crown occupying the narrow space within the area surrounded by the arms, but it seems to consist of about three or four comparatively large plates. Locality and position. Oswego, Kendall Co., 111. Cincinnati Group,* Lower Silurian System. POROCRINUS PENTAG0NIUS, M. & W. Body pentagonal-obovoid, being more or less rounded above, and tapering at an angle of about sixty degrees from the middle of the prominent sub- radials to the summit of the column ; base forming about one-fifth of the entire height, and having the form of an expanding pentagonal basin, with flattened sides ; basal pieces pentagonal, and nearly twice as wide as high. Subradial pieces as long as wide, and equalling nearly half the length of the body. — the only one visible on all sides in our specimens, hexagonal in form ; each prominent in the middle, from which point a well-defined ridge radiates so as to connect with similar ridges on each of the surrounding plates ; the ridges passing laterally and upwards intersect the sides of the plates, but the one passing downwards from the middle of each subradial coincides with its central inferior angle, where it connects with a corresponding ridge extending up the sutures between the basal pieces ; the arrangement of the ridges being such us to divide the surface into a series of large triangular, slightly concave areas, in which are placed the pectinated openings. These openings at the corners of the basal and subradial pieces consist of about twelve of the linear fissures to ea< h plate ; those at the junction of the plates above smaller, with a proportionally smaller number of fissures. Form and arrangement of the anal and radial pieces, as well as of the arms, unknown. Surface finely granulo-striate, the granules being ranged in lines parallel to the ridges, particularly on the ridges below the middle of the subradials, so as to present, as seen under a good magnifier, a finely substriated appearance. Column rounded, and expanding rapidly upwards near the base, where it is composed of very thin segments with minutely crenated edges ; farther down the segments are proportionally thicker and more coarsely crenate. Length of body, 0*43 inch ; breadth at the middle of the subradials, 0-40 inch. Breadth of column at its connection with the base, 0-15 inch ; do. 0-72 inch below, 0-05 inch. * See Note at the end of this paper. CA«g. NATURAL SCIENCES OF PHILADELPHIA. 147 This species will be readily distinguished from P. conicus, of Billings, by its broader, more ovoid, and more angular form, owing to the much greater prominence of its subradial pieces, and particularly by the well-defined ridges radiating from the centre of the plates. In the latter character, it approaches more nearly the last described species, P. crassus, from which it differs in a marked degree, in having its under side below the middle of the subradial pieces greatly more tapering, and base much smaller, and not wider than the head of the column, as well as proportionally higher. It also differs in having its greatest breadth at the middle of the subradial pieces, which are much more prominent ; while its pectinated openings are not sunken, nor its sutures furrowed as in the last. Locality and position. — Trenton Limestone, of Lower Silurian; Dixon, 111. Genus HETEROCRINE, Hall, 1847. Heterocrinus crassus, M. & W. Body robust, but rather small compared with the arms and column, wider above than the length from the base to the summit of the first radials ; dis- tinctly truncated at its connection with the column, from which point the sides expand rather distinctly upwards ; subpentagonal in outline as seen from below. Basal pieces pentagonal, wider than long, and all excavated or indented on the outside at the superior angle and down the middle. First radial pieces longer than the basal, about three-fourths as long as wide, broadly truncated above, and regularly pentagonal in form, excepting two on the anal side, which appear to each have one of the superior lateral angles a little truncated for the reception of a small anal piece ; all deeply indented at their inferior lateral angles, so as to leave a broad, rounded, undefined ridge or prominence descending from the middle to the basal pieces. Succeeding radial pieces forming free arms, nearly as wide as, but much shorter than, the first; in four of the rays all transversely oblong, and about three or four times as wide as long, excepting the fourth or fifth pieces, which is pentagonal, and supports, on its sloping upper side, the first divisions. In one ray on the anal side the second piece is pentagonal, larger than that of any of the others, and gives off a lateral branch from its short sloping side on the left,* above which the other pieces present the same size and form seen in the other rays. Arms after the first division on last radial, bifurcating again on the sixth or seventh piece, after which they are known to divide again in one arm, on the sixth piece, which is as far as our specimens show the structure. Surface usually appearing smooth, but sometimes showing traces of scatter- ing granules. Column comparatively large, distinctly pentagonal, and ex- panding upwards near the base of the body, where it is composed of irregu- larly alternating thicker and thinner segments ; central perforation small and round. Height of body from base to the summit of first radial pieces, 0*35 inch ; breadth at summit of first radials, about 0-67 inch ; length of five succeeding radial pieces, 0-4(j inch ; breadth of do. about 0*15 inch. Breadth of column at its connection with the base, 03:2 inch. This is perhaps the largest and most robust species of the genus known. It is composed of thick, strong plates, and the indentations or excavations at the points where the superior angle of each basal plate connects with the inferior lateral angles of the first radials, together with the more shallow depressions extending down from these points to the lower margin of the basal pieces, give a pentagonal outline to the body — the five angles being coincident with those of the column. * From some of the specimens it appears somewhat doubtful whether this may not be. a range of anal pieces, instead of a branch of the arm. 1865.] 148 PROCEEDINGS OF THE ACADEMY OF Locality and position. — Cincinnati Group of the Lower Silurian series ; Kendall Co., Illinois. Heterocrinps subcrassus, M. & W. This species agrees so nearly with the last in most of its characters as to render a detailed description unnecessary. It will be readily distinguished, however, by its smaller size, as well as its less robust appearance, and the different aspect of its arms. This latter difference consists in the more slender appearance of all the divisions, and particularly in the joints of which they are composed having their upper margins projecting beyond the base of each succeeding piece above, so as to present a kind of upward imbricating appear- ance and roughness, not seen in the arms of H. crassus. As in the last, its rays bifurcate first on the fifth and sixth pieces, and one of them gives offabranch (?) on the leftside ofthe second radial, abovewhichit bifurcates regularly on the sixth piece. After the first regular division on the last radial piece, some of the arms are seen to divide again on the fourth, others on the fifth, and others on the sixth pieces, after which one division is known to bifurcate on the sixth piece, and still again on the thirteenth. Breadth of body at the summit of the first radial pieces, 0*27 inch ; height of do., 0-13 inch ; length of rays from top of first radial pieces to the first bifurcation, 0.21 inch ; entire length of arms from first division to extremities, about 1-50 inches. Breadth of column at its connection with the base, 0-15 inch. Locality and position. — Cincinnati, Ohio. Cincinnati Group of Lower Silu- rian . Heterocrine ? incurvus, M. & W. Subgenus Anomalocrinus, M. & W. Body expanding rapidly from the base to the summit of the first and second radial pieces, where it is more than twice as wide as high; composed of the five basal, five first radial, and two second radial pieces. Basal pieces pen- tagonal, of moderate size, wider than long, and forming together a low rapidly- expanding, pentagonal cup. First radial pieces in three of the rays from three to five times as large as the basal pieces, wider than long, two hexagonal and one heptagonal, — all with their superior lateral angles strongly incurved between the arms, and each with a small protuberant, rounded facet above, for the reception ofthe small succeeding radials. In the remaining two rays, the first pieces are smaller and lower than those of the others, and each pen- tagonal in form, with the upper side horizontally truncated its entire breadth, for the reception of a larger second radial, which in these two rays agrees in size and form, as well as in being included as a part of the walls of the body, with the large first pieces of the other rays. Succeeding radials not more than one-third as wide as those included in the walls of the cup, and forming small, rounded, widely separated free arms, consisting of one to three quad- rangular and one pentagonal pieces to each ray. Arms above the first bifur- cation on the second or third pentagonal free radial, in two of the rays seen, bifurcating again on the third piece, and, in one instance, sending off nearly at right angles from the second piece after the first division, a strong tentacle, or small lateral branch. First anal piece pentagonal, longer than wide, and resting between the left sloping side of a large second primary radial and the right sloping side of a first primary radial, with rather less than half its length projecting above the focmer, and without extending down so as to bring its base in contact with any of the other plates below. In the individual examined, this piece is strongly incurved, and supports on its inner truncated end an oblong, narrow second anal, which in its turn supports a smaller third piece, all of which are arranged in a right line, and probably form one side of a proboscis. [Aug. NATURAL SCIENCES OF PHILADELPHIA. 149 Surface smooth, or only with traces of flue granules. Sutures a little con- cave. Column comparatively strong and rounded near the base, where it is composed of short joints, and marked with obscure, regular longitudinal striae. Height of body on the anal side, 0.28 inch; do. on the opposite side, 0.22 inch ; greatest breadth above (allowing for a slight accidental compression) about 0.38 inch ; breadth of free arms at their connection with the body, 0.08 inch ; breadth of column at its connection with the base, 0.16 inch. This species presents points of analogy both to Heterocrinus, Hall, and Hybo- crinus, Billings, and yet seems to differ from both to such an extent, that if we could be sure some of its peculiarities are not abnormal in our specimen, we would be inclined to view it as the type of a new genus. As we have seen but the one specimen, however, which is not complete in all its parts, we have concluded to place it, for the present at least, as the type of a subgenus under Heterocrinus. It differs from the typical species of that genus in having the column round instead of pentagonal, and in having only the first primary radial pieces in three of the rays, and two in each of the others, included as a part of the walls of the body ; while its preceding primary radials are very narrow, and form small, rounded, distantly separated arms, instead of being nearly as wide as those soldered in the walls of the cup. Another peculiarity is the strongly incurved superior lateral angles of the large radial pieces around the margin of the cup between the arms. In the rather unsymmetrical form of the body, the slender proportions of the free arms, and its general aspect, it resembles Hybocrinus, from which it differs in having but one anal piece connected with the walls of the cup, and in having two of the rays and two of the primary pieces included in the wall, while its free arms bifurcate twice or oftener, instead of being simple from their origin. Locality and position. — Cincinnati, Ohio. Cincinnati Group of Lower Si- lurian. Genus ERISOCRINUS, M. & W. Erisocrinus, M. & W., Am. Jour. Sci. xxix. p. 174, March, 1865. Philocrinus, M. & W., ib., May, 1865 ; not Koninck, 1863. Generic formula. Basal pieces, 5 \ Subradials, 5 > united to form the walls of the body. Radials, 2 X 5 } Anals and interradials, 0. Soon after publishing the description of this genus, we were led by its simi- larity to a genus described by Prof. Koninck, from the Carboniferous rocks of India, to believe it identical, and ranged our species under that name. Later comparisons have caused us, however, to doubt the correctness of this con- clusion. If there is no mistake in regard to Philocrinus being without a range of subradial pieces, then the two types would be clearly distinct. The fact, however, that the basal pieces in Erisocrinus are small, and might be easily overlooked in imperfect specimens, taken in connection with the fact that the lowest range of pieces represented in Prof. Koninck's figure, if true basals, would have to present a singularly elongated cuneiform outline, leads us to suspect there may be another range of small true basal pieces below them, but not visible, from some imperfection in the speeimen in Prof. Koninck's type. If so, then the identity of our Crinoid with our Indian type would be complete. Until this question can be satisfactorily settled, however, we have concluded to retain our name Erisocrinus for the American type. Should they prove identical, however, of course Prof. Koninck's name will have to take precedence, since it has priority of date. 1865.] 150 PROCEEDINGS OF THE ACADEMY OF Erisocrinus conoideds, M. & W. Body small, below the summit of the first radials obconic, nearly twice as wide as high ; basal pieces a little wider than long, pentagonal as seen pro- jecting beyond the column, and forming together a small low cup with di- verging sides ; subradials near three times as large as the basal pieces, a little wider than long, and all hexagonal ; first radial pieces half as long as wide, about twice as large as the subradials, and all broadly truncated on the same horizontal plane above, for the reception of the second radial pieces. Surface smooth ; sutures linear, not impressed ; plates not convex. Column and all the parts above the first radial pieces unknown. Height to summit of first radials, 0-20 inch ; breadth of do. 0-34 inch. This species will be at once distinguished from young specimens of the last of its own size, by its obconic, instead of basin-shaped cup. From Prof. Ko- ninck's species cometa (in case our species should really belong to his genus) it will be distinguished specifically by the less convex outline of the sloping under sides of its cup, as well as by its shorter and proportionally wide first radial pieces. It will of course have to take the name P.hilocrinus conoideus, in case Prof. Koninck's species should prove generically identical with these American forms. Locality and position. — Springfield, 111., Coal Measures. Erisocrinus tuberculatus, M. & W. Although we only know this fine species from its detached plates, these agree so exactly in form with the corresponding parts of our Erisocrinus typus from the same beds, that scarcely a doubt can be entertained in regard to their belonging to the same genus ; while they differ so remarkably in their surface characters as to be distinguished at a glance, specifically, from that or any other Crinoid known in our Coal Measures. This difference consists in their entire external surface being covered with regularly disposed, narrow, prominent tubercles, instead of being smooth. Of these tubercles there are, on a first radial plate measuring 0-00 inch in breadth and 0-54 inch in height, about thirty in number, arranged so as to form two rows of about eight each, ranging parallel to the inferior sloping margins, and one row of about eight along the superior margin. Between this latter row and those below, there are usually a few tubercles either iso- lated or forming a third transverse row. There is likewise usually one or several others at the lower middle angle outside of the regular rows. This arrangement of the tubercles into rows is not, however, always obvious at a first glance, but a tendency to such a disposition can always be seen. On the second radials the tubercles are arranged in a single row along the lower and eachaeuperior sloping margin, with one or more in the middle be- tween the rows. In the articulating, or connecting surfaces of the radial plates, we observe no differences between these pieces and those of the corre- sponding parts of E. typus. Some of the plates indicate a transverse diameter of 1*40 inch for the entire body. If our proposed genus Erisocrinus is, as we have suspected, identical with Pkilocrinus of Koninck, the name of this species will have to be written Pliilo- crinus tuberculatus. Locality and position. Upper Coal Measures. Sugar Creek, Sangamon Co., 111., and near Brighton, Jersey Co. Genus CYATHOCRINUS, Miller, 1821. Cyathocrinus quinquelobus, M. & W. Body broad baain-shaped, composed of very thick, strong plates ; height to [Aug. NATURAL SCIENCES OF PHILADELPHIA. 151 summit of first radial pieces, less than half the width. Base small, a little concave below, or forming a nearly flat pentagonal disk ; basal pieces about half hidden by the column— the portion of each exposed pentagonal in form. Subradial pieces much larger than the basal, four of them hexagonal, and one on the anal side heptagonal ; each having a strongly elevated, bicarinate pro- tuberance, extending out horizontally almost its entire length, like the rays of a star, upon which the body rests when placed with the under side down. First radial pieces two and a half to three times as wide as high, pentagonal, and all transversely truncate their entire breadth above, for the reception of the succeeding radials, so as to present a broad, moderately concave, outward sloping facet above ; those of the two antero-lateral rays each nearly twice as long as the others, and provided ne^r the middle of the upper margin with two angular nodes or prominences ; sutures close fitting, and not very appa- rent. First anal piece small, quadrangular, a little wider than high ; resting upon the truncated upper side of one of the subradials, and connecting on each side with a first radial, above which it does not project. Columnar facet of moderate size, a little concave, with a rather small, rounded, central perforation, and traces of radiating striae around the margin. Surface finely and regularly granulose. Height to summit of first radial pieces, 0-55 inch ; greater transverse diame- ter, at summit of first radials, l-04 inches. This species is evidently allied to C. sculptilis* of Hall, from the Burlington limestone ; but it is much more robust, and has more prominent subradial pieces, with the prominences more grooved along the middle. Its base is also more concave, and its first radial pieces, particularly the anterior and postero- lateral, proportionately shorter ; while it shows no tendency to develop ridges across from the subradials to first radials, nor has it any surface striae. Locality and position. — Warsaw, 111. Keokuk division of subcarboniferous series. Cyathocrinus subtumidus, M. & W. Body below the summit of the first radial pieces, cup-shaped, robust, rather deep, somewhat rounded below, with nearly vertical sides. Basal pieces well developed, pentagonal, convex, about as wide as long. Subradials four or five times as large as the basal pieces, thick, and very strongly convex, slightly higher than wide, four hexagonal and one apparently heptagonal. First radial plates about the size of the subradials, having a general pentago- nal outline, with the two superior lateral angles usually a little truncated, apparently by the first series of the vault pieces — not tumid, like the plates below ; each with a moderately concave outward-sloping facet for the recep- tion of the next radial above. Succeeding primary radials (of which one ray shows two, and another three,) about half as wide as the first radial pieces, all rounded on the back, two in one ray, and one in another, trans- versely oblong ; the last one in each of these rays proportionally a little larger than the others, and supporting on its superior sloping sides the arms, which, in the anterior ray, bifurcate again on the second piece. (Number and arrangement of the anal pieces unknown.) Breadth of body, 0-90 inch ; height of body to summit of first radials, 0*72 inch. This species has the general aspect of Cyathocrinus bullatus and C. protube- rans, Hall, (Iowa Report, 624 and 626, ) but differs from both in having its * We now regard our C.scilulus( Proceed. Acad. Nat. Sci., Phila., Sept., 1860, p. 393,) as a synonym of C. sculptilis. Hall. Our description was going through the press when we first saw Prof. Hall's Supplement to the Iowa Report, in which he described his C. sculptilis, and, owing to the necessa- ry haste with which our comparisons hail to be made, and the fact that Prof. Hall had inadvert- ently described oue of the subradi 1 pieces of his species as the first anal piece, and the first anal as the second, caused us to overlook their probable identity. 1865.] 152 PROCEEDINGS OF THE A^.iDEMY OF basal pieces proportionally much larger and more tumid, and its radials above the first narrower and proportionally longer. From C. protuberans it also differs in not having its first radial pieces tumid, while one of its arms after the first division is seen to bifurcate again on the third piece, instead of merely giving off small lateral branches, as in C. protuberans. Our specimen being defective on the anal side, we have been unable to de- termine whether it has one only, or two anal pieces soldered in the wall of the cup, though it appears to have but one. Locality and position. — Keokuk limestone, of subcarboniferous series. Near White Hall, Green County, 111. CYATHOCRINUS ENORMIS, M. & W. Poteriocrinus ? enormis,M. & W. Proceed. Acad. Nat. Sci., June", 1861, p. 137. Although this species possesses the structure and arrangement of the parts composing the walls of the body, including the anal pieces, of Poteriocrinus. the fact that it has a slender lateral proboscis, not larger than one of its armsj instead of a large trunk nearly as wide as the body, as seen in typical species of Poteriocrinus, leads us to the conclusion that it more properly belongs to the allied group of Ci/athocrinus. This conclusion is also sustained by the appearance of an opening in the summit, near the small lateral proboscis. These differences in the structure of the summit will probably be found of more importance as a distinction between these two groups, than the fact of one or two more or less anal pieces being included as a portion of the walls of the body. Genus POTERIOCRINUS, Miller, 1821. POTERIOCRINUS (ZEACRINUS) CARBONARIUS, M. & W. Poteriocrinus (Scarphiocrinus?) carbonarius, M. & W. Proceed. Acad. Nat. Sci., June, 1861, p. 140. This species has the elongated and constricted second radial pieces, as well as the gaping sutures between these and the first radials, characterizing Scar- phiocrinus, but differs from the typical forms of that group in having a con- cave base. In the latter, as well as some of its other characters, it agrees with Zeacrinus, to which it seems to more properly belong. Genus ACTINOCRINUS, Miller, 1821. ACTINOCRINUS PISTILLUS, M. & W. Body, exclusive of the proboscis, sub-pyriform ; the sides rising nearly ver- tically from the base to the summit of the first radial pieces ; thence gradually expanding to the secondary radials, after which they expand very rapidly, so as to cause the brachial pieces to be directed horizontally outwards, or nearly so, at about the middle of the body. Above the horizon of the arm bases, the dome rises at first vertically, but very soon rounds inward, and rises with a moderately convex slope to the base of the subcentral proboscis. Base trun- cated and flat below, with a thick dilated margin notched at the suture, so as to present a trilobate outline, as seen from beneath ; columnar facet a little concave, and about one-third as wide as the base. Basal pieces twice as wide as high, and hexagonal in form, the inferior margin being much longer than any of the others. First radial pieces wider than long, smaller than the basal ; three of them heptagonal, and two hexagonal. Second radial pieces very small, twice as wide as high, and transversely oblong, or sometimes with one of the superior lateral angles truncated by one of the interradials, so as to pre- sent an irregular pentagonal form. Third radials a little larger than the second, pentagonal or hexagonal in form, and supporting on each superior sloping side, a secondary radial piece, [Aug. NATURAL SCIENCES OF PHILADELPHIA. 153 each one of which is succeeded by another. Upon the superior sloping sides of the latter, in the anterior and one of the lateral rays, commence the brachial pieces, of which there are two ranges, upon the last of which commence the free arms, thus giving origin to four arms in each of these rays. In the two posterior rays, however, and one of the lateral, after the second bifurcation on the last secondary radial, the latter supports on the outer sloping side a tertiary radial, which gives origin to two brachial pieces, making live arms to each of these rays, or twenty-three to the whole series. After the first bifurcation on the third radial pieces, all the succeeding pieces of each ray are in di ect contact, so as to leave no spaces for interaxil- lary plates : while the outer brachial pieces of each two contiguous rays con- nect over the anal aud interradial spaces, so as to nearly or quite isolate the pieces filling those spaces, from the dome. First anal piece of the same form as the subradials, but rather smaller than those of the anterior and antero-lateral rays ; surmounted by three smaller hexagonal and heptagonal pieces in the second range, and three or four in the third, making seven or eight altogether. Interradial pieces four, (rarely five, ) those of the inferior range being larger than the others. Surface without costse or visible granules, but roughened by the tubercular character of the plates. The tubercle occupying each first radial and the first anal, is larger than those on any of the other pieces of the side walls above ; where they become smaller and less distinct with each succeeding range, un- til they are nearly or quite obsolete a few ranges below the arms. Upon the dome, however, the tubercles are prominent and well defined. The proboscis is unknown, but its base is stout, and rises rather abruptly from the dome, being placed nearly its own breadth nearer the anal than the opposite side. The arms are also unknown. They evidently projected at first horizontally outwards from the body, and their bases are so crowded as to form an almost continuous rim around the body. Height from base to horizon of arm openings, about Ot)4 inch ; height to base of proboscis, 1*22 inches. Breadth of dilated margin of base, 0-46 inch ; breadth of same just above, 0-38 ; breadth of body at top of first radials, 0-55 inch ; breadth of same at arm openings, 1"05 inches ; breadth of base of pro- boscis, 0'43 inch. This species belongs to a peculiar group of Actinocritius, as generally under- stood in this country, of which A. piriformis, tthumard, (Missouri Report, pi. A, figs. 6a, b, ) may be regarded as the type. It also includes our A. pistilliformis* and A. clavigerus, Hall. These species differ remark- ably in form from typical species of Actinocrinus, such as A. triacontadactylus, A. lavis, &c, of the old world, in having the body very narrow and attenuate below the arms, so as to form, as it were, a kind of handle to the upper half, giving the whole, when the arms and pioboscis are removed, somewhat the form and appearance of a pestle. They also differ from the old world species regarded as typical forms of Actinocrinus, in having the arms springing from the body in a continuous series, instead of being in five groups. Should it be considered desirable to separate this little group as a section of Actinocrinus, it may be called Uperocrinus, from its resemblance, when the arms and proboscis are removed, to a short-handled pestle. If Casseday's group Batocrinus, bow- ever, should be adopted as a distinct genus from Actinocrinus, this should be ranged under it as a subgenus. Specifically, the form under consideration differs from A. piriformis in having its first anal, first radial, and basal pieces, proportionally much shorter, its base more flattened below, and more dilated around the margin ; * In indicating this form under the name A. rudis, (Proc. Acad. Nat. Sci , Juue, 1S61, p. 131,) we ha'l over ooked the fact of that name having been used by Prof. Hall for another species, in the tfupplemuuc of the; Iowa Report, p. 33: hence we now propose to call it A. pialiUi/urrais. 18U5.] 154 PROCEEDINGS OP THE ACADEMY OP as well as in the plates of the lower part of its body being much more dis- tinctly tubercular, and in the greater number and more crowded arrangement of its arms, which were evidently, at their bases, directed outwards, instead of being, from their origin, directed obliquely upwards. From our A. pistilliformis, with which it agrees more nearly in some re- spects, it differs, not only in having three more arms, but in the less abruptly contracted form of its body immediately below the arms, as well as in having from four to six interradial pieces to each space, instead of only two or three. There were doubtless other more important differences that would be apparent on comparing perfect specimens of each, judging from the different geological positions of these two forms. Locality and position. — Burlington limestone, of subcarboniferous series, Burlington, Iowa. Subgenus SPHiEROCRINUS, M. & W. Actinocrinus (Sph^erocrinus) concavus, M. & W. Actinocrinus {Amphoracrinus) concavus, M. & W. Proceed. Acad. Nat- Sci., Phila., June, 1861, p. 132. This curious little species may be regarded as the type of a section of the group Actinocrinus, as usually understood, for which we would propose the name Sphcerocrinus. Its peculiarities consist in the deep convexity of the base, and the tumid and curved character of its first radial and first anal pie- ces. These characters are so marked, that when placed with the under side down, it rests directly upon a broad base formed of the first radial and first anal pieces, which curve under to connect with the sunken basal pieces, and upwards to form a part of the vertical walls of the cup. In the lateral position of its anal and oral opening, it agrees with Agarricocrinus and Amphoracrinus ; but it differs from the first, with which it also agrees in being concave below, in the tumid and curved character of its first radial and anal pieces, as well as in having the succeeding radials, anals, and interradials forming a vertical wall, instead of extending out on a horizontal plane, while its arms are very much weaker, and rise from around the summit, instead of from the horizon of the lower part of the body. Its interradial and second range of anal pieces are also much shorter. From Amphoracrinus, it not only differs in tbe concavity of its base and the curved character of its first radial and first anal pieces, but in all the other peculiarities of form, and the weakness and position of its arms. From Dolatocrinus, Lyon, (Cacabocrinus, Troost ?) with which it agrees in form, the number of basal pieces, and the sunken condition of its base, as well as in the incurved character of its first radials, it differs in having its first anal piece down on the same range with the first radials, and connecting with the base as in the typical forms of Actinocrinus, instead of being up on a range with the first interradials. It also differs in its lateral anal and oral opening, as well as in not having protuberant arm bases. MOLLUSC A. CEPHALOPODA. GoNIATITES COMPACTUS. Shell subdiscoid ; umbilicus wide, or about twice the dorso-ventral diame- ter of the last turn near the aperture, moderately deep, and showing about half of each inner turn. Volutions four, near twice as wide as their diameter in the direction of the plane of the shell, broadly rounded externally, and each provided with a broad moderately deep concavity on the inner side, for the reception of the next whorl within ; sides rather narrowly rounded near the umbilicus, and rounding off more gradually to the periphery, the most [Aug. NATURAL SCIENCES OF PHILADELPHIA. 155 prominent part being within the middle. Aperture (as inferred from sections of the whorls) transversely subreniform. Septa with a single pointed lobe on each side ; dorsal lobe infundibuliform, the narrow portion being lanceolate ; dorsal saddle broadly and very obtusely rounded ; superior lateral lobe from one-fourth to one-third larger than the dorsal, and having much the same shape, excepting that it is proportionally wider ; inferior lateral lobe consisting merely of a broad rounded sinuosity. (Surface unknown.) Should Montfort's name Aganides be retained for this genus, the name of this species would become Aganides compactus. Greatest diameter 2-50 inches ; convexity (or breadth of aperture) 1'33 inch ; breadth of umbilicus, about 1\12 inch. Locality and position. — Coal Measures. Macoupin Co., 111. Note in regard to the name "Cincinnati Group," used in the foregoing paper. As it is now acknowledged that the rocks along the Hudson river valley, to which the name Hudson River Group had been applied, belong, as long maintained by Dr. Emmons, to a different horizon from the so-called Hudson River rocks of western New York, and the states farther westward, it seems to be an awkward misnomer to continue to apply the name Hudson River Group to these western deposits. Hence it is certainly desirable that this group should receive some appropriate and generally applicable name. Its subdi- visions, it is true, have already received various lithological names, such as " Utica Slate," "Frankfort Slate," "Lorraine Shale," &c. ; but as each of these names will probably be always directly associated, in the minds of geologists, with the particular subdivision to which it was originally applied, while neither of them is applicable to the lithological characters of the whole series, we cannot, without creating confusion, so extend its signification. It has recently been proposed to designate this series as the " Green and Blue Shales and Limestones;" this, however, is not a name, but descriptive phrase, and has the disadvantage of being based upon lithological characters not everywhere characteristic of these beds. In view of all the facts, we have concluded to propose the name Cincinnati Group — (which will be adopted in the forthcoming reports of the Illinois Geo- logical Survey) — for this series. This name possesses the advantage of being equally applicable to rocks of any color or composition, while it carries the mind to a well-known locality, where the formation referred to is extensively developed, and its fossils so abundant that they have been thence widely distributed, both in this country and Europe. Consequently, geologists will everywhere at once understand to what particular horizon of the Lower Silu- rian this name refers. Descriptions of New Crinoidea, &c, from the Carboniferous Rocks of Illinois and some of the adjoining States. BY F. B. MEEK AND A. H. WORTHEN. Genus POTERIOCRINUS, Miller, 1821. POTERIOCRINUS InDIANKNSIS, M. & W. Body rather deeply cup-shaped or truncato obconic. Base basin-shaped, comparatively rather broadly truncated below by the columnar facet. Basal pieces well developed, pentagonal, about one-third wider than high. Sub- radials large, three pentagonal, and two on the anal side hexagonal, there being no defined angle at the middle of the under side of any of these plates. First radial pieces about half as large as the subradials, wider than long, rounded on the outside, and nearly pentagonal, or with one or both of the superior 1865.] 156 PROCEEDINGS OF THE ACADEMY OF lateral angles slightly truncated, so as to give an obscurely hexagonal or hep- tagonal outline ; all broadly truncated nearly their entire breadtb above, and one on the immediate right of the anal series, resting in part directly upon the upper truncated side of one of the subradials, and elevated almost its entire length above the horizon of those of the other rays. In this latter ray, and the one on the immediate left of the anal series, the second piece is quadran- gular, and wider than long, while the third is pentagonal, and supports the first division of the arms on its superior sloping sides. These divisions in the ray on the right are simple, rounded, and each composed of a single series of somewhat wedge-shaped pieces; while the left branch of the one on the left of the anal series, bifurcates again on the second piece, making three arms in this ray, which are constructed like those already described, and continue simple as far as they can be traced. In the only other ray preserved in the specimen, the bifurcation takes place on the second radial, beyond which the arms continue simple. First anal piece nearly as large as one of the first radials, hexagonal, and resting between the upper sloping sides of two of the subradials, partly under the first radial on the right, while it connects on the left with the second anal, and supports a third on its truncated upper side. Second anal piece rather large, longer than wide, hexagonal, and resting upon the superior truncated side of one of the subradials. Third anal piece smaller than the others, hexa- gonal, and surmounted by several other hexagonal pieces in direct succession, belonging to the. proboscis. Surface apparently smooth. Columnar facet rather large and marked with distinct radiating stria? around the margins. Length of body to summit of first radials, about 0-48, excepting in the ray on the immediate left of the anal series, where it is 0-58 inch; breadth about 0-56 inch. Breadth of columnar facet, 0-26 inch. Usual diameter of the arms after the bifurcations, 012 inch. Locality and position. — Crawfordsville, Indiana. Keokuk division of the Subcarboniferous series. POTERIOCRINDS (SCAPHIOCRINUS) TENUIDACTYLUS, M. & W. Body in comparison with the length of the arms small, inversely campanu- late below the summit of the first radial pieces ; being narrowly rounded below and rather expanded above, where the breadth is nearly twice the height. Base less than half as wide as high, basin-shaped, the sides rounding under to the columnar facet, which is of medium size and a little concave. Basal pieces well developed, pentagonal, and wider than long. Subradial pieces twice or three times as large as the basal ; those on the anterior side (the only ones seen) hexagonal. First radials wider but shorter than the subradials ; transversely truncated about three-fourths their entire breadth above, for the reception of the succeeding radial pieces ; those on the anterior side curving a little outwards and having an irregular pentagonal outline, the superior lateral angles being more or less truncated, or rounding inwards. Second radials pentagonal, nearly as long as wide, separated by interradial pieces of nearly their own breadtb, rounded and constricted around the middle, with the central superior angle prominent, and the sloping margins on each side of it supporting the arms. Anal pieces unknown. Arms long, slender, and in two of the anterior rays known to bifurcate on the tenth piece above the third primary radials, after which they are seen to be extended to a considerable length, without, showing distinctly another division, though there is some appearance of such bifurca- tion in one of the branches, on the twentieth piece. Immediately after the division of the rays on the third primary radials, the arms are rounded and composed of wedge-shaped pieces, wider than long, and alternately thicker and thinner on opposite sides, each one supporting at its larger end a stout [Aug. NATURAL SCIENCES OF PHILADELPHIA. 157 tentacle. Above the bifurcation on the tenth piece, the divisions are very- long, slender, somewhat angular on the outer side, and still composed of a single series of wedge-shaped pieces, each one of which is strongly protuberant laterally, for the reception of a tentacle at its larger end, — the protuberances and the sinuosities between giving the divisions of the arms a zigzag appear- ance, somewhat like those of Platycrinus nodobrachiatus, Hall.* Surface apparently smooth, or only finely granulose. Suture not impressed between the plates of the body, but somewhat gaping between the first and second radials. Height of body to top of first radials, 0-41 inch ; breadth, 0-60 inch. Length of arms to first bifurcation, 0-70 inch; entire length nearly 3 inches. This species seems to be related to several of those described by Prof. Hall from the same locality and position, but on comparison will be found not to agree in all its characters with the description of any of them. From his S. spinobrachiatus it evidently differs in not having the plates of the body convex, nor the sutures indented at their angles, as well as in not having the arms subspinous, and the whole body is less broadly cup-shaped. From S. Whitei, Hall, it differs in not having the " surface of cup marked by deeply impressed pits " at the junction of the sides of the subradials, and between the first radial pieces: and from S. Halli, Hall, it differs in not having the arms simple after the first division on the second primary radial, as well as in some of the details of their divisions. Locality and position. — Burlington, Iowa. Burlington Limestone of Snb- carboniferous series. POTERIOCEINUS (SCAPHIOCRINUS) BaYENSIS, M. & W. Body of medium size, rather depressed obconic below the top of the first radials. Base about twice as wide as high, expanding directly from the head of the column on a line with the subradial and first radial pieces. Basal pieces moderately developed, wider than long, pentagonal, and showing the whole surface of each in a side view. Subradials about three times as large as the basal, somewhat wider than long, three hexagonal, and two on the anal side apparently heptagonal, the angle on the middle of the under side of all being very obtuse. First radial pieces wider and a little shorter than the subra- dials, all pentagonal, apparently transversely truncated their entire breadth above. Second radials of nearly the same size as the first, and like them pen- tagonal, but having the middle angle above and more salient, while the two superior sloping sides each supports an arm, thus giving origin to two arms to each ray, or ten to the entire series ; all of which are nearly in contact all around below, excepting on the anal side. First anal piece smaller than the subradials, hexagonal in form, and resting between the upper sloping sides of two of the subradials, with its upper right edge supporting one side of one of the first radials, and its left connecting apparently with a second anal piece, the form of which cannot be made out in our specimen. In the third range, one piece evidently rested upon the upper truncated edge of the first anal piece, but its form and connection with the other pieces on the left have not been determined. Arms long, and, as far as can be determined, apparently simple after the first division of each ray on the second radial piece ; each composed of a single series of wedge-shaped pieces, alternately longer and shorter on opposite sides, but not protuberant on either side ; those near the lower part about as long on the longer side as their breadth. Tentacles numerous, rather stout, and com- posed of joints three or four times as long as wide, and not swollen or dilated at the ends. Column of moderate thickness near the base, where it is round and com- *Iowa Report, p. 542. 1865.] 11 158 PROCEEDINGS OP THE ACADEMY OF posed of alternately thicker and thinner pieces. Surface apparently smooth Sutures slightly furrowed excepting those between the first and second radial pieces, which are distinctly gaping when the arms are folded together. Height of body to the top of the first radial pieces, 0-25 inch; breadth of do. 0-48 inch. Length of arms above the second radials, 1-90 inches or more; diameter of column at its connection with the base, 0-13 inch. This species seems to be closely related to S. decabrachiatus, Hall, (Iowa Report, p. 679, pi. xxv. fig. 1,) but is larger and more robust, and its second radial pieces differ materially in form, being nearly or quite twice as wide as long, while in S. decabrachiatus they are ''nearly once and a half as long as wide." Its basal pieces are also proportionally about twice as large. Other differences would doubtless be apparent, if we had the means of comparing all the corresponding parts of each with those of the other. Locality and position. — Bay City, Pope Co., Illinois. Chester division of the Subcarboniferous limestone series. POTERIOCRINDS (SCAPHIOCRINUS) ? NoRWOODI, M. & W. Body small, depressed basin-shaped, rounded and concave below, breadth three times as great as the height to summit of first radial pieces. Basal pieces very small, deeply impressed within the concavity of the under side, and almost entirely hidden by the column. Subradial pieces comparatively well developed, curving under to connect with the concave base ; three pentagonal, (exclusive of. the scarcely-defined angle at the middle below,) and two on the anal side hexagonal. First radial pieces short, and about twice as wide as high, pen- tagonal, with the upper side transversely truncated its entire breadth. Second radials as wide as the first, and twice as long, pentagonal, and at the middle above acutely angular. Arms after the first division on the second radial bifurcating at least once more, on the third or fourth piece, the joints beyond being slightly longer than wide, and supporting alternately on opposite sides of the arms strong, long-jointed, rather remotely-separated tentacles. First anal piece nearly as large as one of the subradials, pentagonal, and resting between the upper sloping sides of two of the subradials, with its right superior sloping side supporting the left under side of a first radial, and its left upper side a third anal piece, while its short left vertical side connects with the second anal piece. Second anal about the size of the first, and resting upon the short upper truncated side of one of the subradials, with its left side con- necting with one of the first radials, and its right with another anal piece. Above these several other anal pieces are seen to rise so as to form apparently a narrow, rounded, lateral proboscis, on a range with the arms, which it ap- pears to scarcely exceed in thickness. Summit and column unknown. Surface nearly or quite smooth, excepting an angular ridge or carina, which extends up each second radial its entire length. Sutures distinct and indented a little at the connections of the corners of the first radials and the subradial pieces ; that between the first and second anal pieces gaping. Height to summit of first radial pieces, 005 inch; breadth, 0-15 inch. This little species presents rather a combination of characters belo"ging to several groups. In the number and arrangement of its anal pieces forming a part of the walls, as well as in the general structure of its body, it agrees with Poteriocrinus, and its depressed form and round deeply-concave underside are characters belonging to the group Zeacrinus, while the form of its arms, and the distinctly gaping character of the sutures between its first and second radial pieces, suggest relations to Scaphiocrinus. Its apparently distinctly lateral, slender, rounded proboscis, however, would remove it entirely from the genus Poteriocrinus to Cyathocrinus. Indeed if we could be sure the latter character is real, and not produced by the accidental folding together into a cylindrical form of merely a part of the external wall of the large trunk bo characteristic of the genus Poteriocrinus, we would not hesitate to call [Auj »g- NATURAL SCIENCES OP PHILADELPHIA. 159 it Cyathocrinus Norwoodi, since the absence of the large trunk-like summit, and the presence of a slender lateral proboscis, are characters probably of more importance, than the presence of a few more anal pieces and the differences in the form of the body. Named in honor of Prof. J. G. Norwood, of the University of Missouri. LocaUty and position. — Hancock Co., Illinois. St. Louis division of the Sub- carboniferous series. POTERIOCRINDS (ScAPHIOCRINDS) SUBTUMIDUS, M. & W. Body basin-shaped below the summit of the first radial pieces, three times as wide as high, composed of thick tumid plates. Basal plates very small, deeply impressed, and hidden by the column. Subradials comparatively large, very convex, and extending out nearly horizontally, but curving upward at their outer extremities; about as long as wide, three of them subhexagonal, and two subheptagonal, the angle at the basal or inner side being nearly obsolete. First radials convex, about twice as large as the subradials, half as high as wide, regularly pentagonal, and all nearly evenly truncated above, their emire breadth. Anal plates like the others, tumid; first one one half to one-third as large as the subradials, irregularly pentagonal, and resting obliquely beneath one side of a first radial, between the upper sloping sides of two subradials, while its left and upper side connect with the other anals. Second anal piece .resting upon the truncated upper side ot one of the subradials, and connecting on the left with a first radial, above which it projects nearly half its length. Third anal piece hexagonal, supported upon a shoit truncated upper side of the first anal, and connecting on the left with the second, and on the right with a first radial, above which it projects a little. Second radials and parts above unknown. Surface smooth ; sutures strongly defined, in consequence of the tumid character of the body plates. Height of body to summit of first radial pieces, 0-27 iuch ; breadth of do. O-TS inch; breadth of base, 0-13 inch. Until specimens of this species can be examined, showing the struc'ure of the parts yet unknown, it will be difficult to determine whether its name should not be more properly Zeacrinus subtumidus, or whether it may not belong to another group, of which Graphiocrinus li-brachialis, of Lyon, is the type* This latter form differs widely, not only from Poteriocrinus proper, but from Scaphiocrinus, Zeacrinus, and also from Graphiocrinus, in having its arms com- posed each of a double series of interlocking pieces, as well as in its unusually massive tumid plates and general physiognomy. In some families of the Cri- noidea, such for instance as the Platycrinus group, a difference like this in the structure of the arms may be of less importance, but in that including Poterio- crinus and the allied genera, we believe it to be of more significance, if not indeed of generic value, especially when accompanied by the other differences of habit presented in this instance. Hence we would propose fur this group the name Eupachycrinus, with Eupachycrinus 14- brachialis = {Graphiocrinus 14- brachialis, Lyon) as the type. It will also doubtless include E. pentalobus = (Cyathocrinus? pentalobus, Hall,) and possibly also Scaphiocrinus orbicularis, Hall. Should our species here under consideration prove to have its arms con- structed of a double series of pieces, we should unhesitatingly call it Eupachy- crinus subtumidus, since in the massive tumid character of its body pieces, small sunken base, and general form and appearance, it agrees, so far as its parts are known, essentially with the type of that group. Specifically, however, it will be readily distinguished by its subradial pieces being proportionally smaller and so much less protuberant as to give a different outline to the under side of the body, as seen in a side view. It also differs entirely in the form and arrangement of its anal pieces. Locality and position. — Bay City, Pope Co., Illinois. Chester division of the Subcarboniferous series. * See Kentucky Geological Eeport, vol. iii. p. 477, pi. i. figs. 2 and 2a. 1865.] 1<30 PROCEEDINGS OF THE ACADEMY OF Genus CYATHOCRINUS, Miller, 1821. Cyathocrintjs arboreus, M. & W. Body rather under medium size, conoidal-semiovate below the top of the first radial pieces, about as wide as high. Basal pieces well developed, form- ing a low basin-shaped cup; all pentagonal, and about as long as wide, the greater breadth being slightly above the middle. Subradial pieces three or four times as large as the basal, about as long as wide, usually arcuate, or a little concave on the outside along the lateral margins — four hexagonal and one heptagonal. First radial pieces of near the same size as the subradials, ar.d presenting a more or less nearly pentagonal outline ; facet for the recep- tion of the second radials nearly equalling one-third the breadth of the first radial pieces, slightly protuberant, and sloping outwards. Succeeding radials small, rounded on the outside, and varying from two to five in the different rays; there being but two in one of the posterior rays and five in the other, while the anterior ray has four, one of the antero-lateral three, and the other four, — all excepting the last or axillary piece being quadrangular. After the first division into two arms on the fourth primary radial piece, (at least in one of the antero-lateral rays,) another division immediately takes pla "e on the first piece of each principal branch, and of the four branchlets thus foumed, the inner two ascend directly upwards, and each bifurcates again on the second piece, and the subdivisions each again on the third piece; while the two main lateral branchlets spread out on either side, each giving off above two or more subordinate branchlets, the first of which is seen to bifurcate at least once. The whole of the divisions and subdivisions being thus spread out to as to resemble the trained limbs of a tree spread upon a wall. The divisions of the other rays cannot be traced out in the specimen examined, in the same detail, but some e>f them appear to divide much in the same way, and others somewhat differently. All the arms and their divisions aie rounded, and the smaller divisions com- posed of joints that are longer than wide, while no tentacles have been observed connected with any of them. The first anal piece is quadrangular, a little longer than one of the basal pieces, and rests directly upon the superior truncated side of one of the sub- radials, while it connects on each side with one of the large first radial pieces, above which it does not project. Other anal pieces unknown. The sutures are slightly impressed, and the surface nearly smooth, or only obscurely granulose. The column and summit are unknown. Height to summit of first jadial pieces, 0-66 inch, on the anal side, and 0*55 inch on the other; breadth at top of first radial pieces, 0-53 inch ; breadth of second and succeeding primary radial pieces, 015 inch. Locality and position. — Crawfordstille, Indiana. Keokuk division of Sub- carboniferous series. Genus PLATYCRINUS, Miller, 1821. As first proposed by Miller, this genus was badly defined, and it is manifest that its author himself, had no very clear ideas of its limits, since he also in- cluded in it species of Pentremites, Say, Dichocrmus, Munster, and of his own genus Actinocrinus. Later writers, however, have restricted it within far more natural limits, and, as now generally understood, Miller's first species, P. Icevis, seems to be regarded as the typical form of the genus. In this and the closely allied species, the body is more or less hemispherical below the arms, while the dome terminates above in a long, generally slender, central or subcentral proboscis, closed at the summit, but apparently pierced by a small aperture on one side near the upper extremity. In these typical forms the arms bifurcate once or oftener near the body, beyond which they are simple, and composed at first, of a single series of wedge-shape pieces, passing more or less gradually fAug. NATURAL SCIENCES OF PHILADELPHIA 161 into a double series of small interlocking pieces supporting numerous tenta- cles. Other species, however, generally included in the genus, have no pro- boscis, but a simple aperture in the summit, located either laterally, or nearly centrally ; while some of these have the arms composed of a double series of interlocking pieces, and others of a single series of wedge-shaped pieces,* neither of these peculiarities in the structure of the arms being always especial- ly coincident with apparently any one of the other characters mentioned. As defined by Koninck and Le Honf , in accordance with their improved nomenclature of the parts, the structural formula of this group is as follows : — Basal pieces, 3 ; forming a wide cup. Radials, 2 ; one large aud one small. X 5. J Anals, 1 large, or 3 small. Interradials, 1, X 4. Arms, 10, 20, 25, 30 or 35, according to the species. From the foregoing remarks, it will be seen, that the group including species agreeing with the above formula, may be divided, as (in part) suggested by the Messrs. Austin, $ into the following four sections : — 1. Platgcrinus, (typical). — With the summit terminating in a more or less elongated, central, or subcentral proboscis, bearing the opening on one side near the upper extremity. Type. P. Ixvis, Miller. Also includes P. spinosus, and P. 30-dactylug, Austin ; P. Miillerianus, Koninck; and P. granulatus, Miller. 2. Centrocrinus, Austin. — Opening of summit nearly or quite central, but not elevated upon a proboscis. Type. P. \_Centroer.~\ gigas, Gilbertson. 3. Cupellseocrinus, Troost. — Differs from the last only in having its second radial pieces merely rudimentary, or so small as to allow the first brachials to rest partly upon the first radials. Type. P. Tennesseensis , Roemer. 4. Pleurocrinus, Austin. — Diifers from Centrocrinus only in having the open- ing of the summit lateral, and nearly or quits on a line with the arm bases Examples. — P. [Pleurocr.~\ mucronatus, Austin;' P. \_Pleurocr .] tuberculatus, Miller; P. [Pleurocr.~\ tub eros us, and P. [Pleurocr.~\ subspi?iosus,H>i\l; P. [Plev- rocrA asper, Meek & Worthen, &c, &c. In regard to the value and importance of the characters distinguishing these sections, Palaeontologists will probably always differ. Hitherto these differ- ences have scarcely been noticed, even by the most respectable authorities, excepting as one of the means of distinguishing species. From all analogy, however, it seems reasonable to suppose that they were accompanied by cor- responding modifications in the structure of the softer parts of the animal. It will also be observed, that they correspond, in part, almost exactly to the charac- ters distinguishing sections of the allied Aclinocrinus group. For instance the species embraced in the section Pleurocrinus, differ from the typical forms of Platgcrinus, almost precisely as Agaricocrinus and Amphoracrinus do from the *P. nodobrachialus, Hall, is an American example with the arms composed of a single series of pieces. We allude here to a species described under that name by Prof. Hall, in the Iowa Report, p. 542, 1S58, aud not to another form described by him under the same name, in his " Descriptions of New Species of Crinoidea, Ac." Albany, Feb. 25, 1851, p. 17. The inconvenience and confusion liable to result from the use of the same specific name for two forms of the same genus, makes it necessary that another name should be applied to one of these species ; hence we would propose to call that described at the latter date, P. perasper. fRecherches Sur les Criuoides du Terrain Carbonifere de Le Belgique, p. 155, 1854. Jit is worthy tf note that although Koninck and Le Hon give two radials (one large and one small) as the number, that their figure 1 a, pi. vi. of P. Ixvis, Miller, shows clearly 3 radials, one large and two small. As others figure and describe it as having only two. this may be only an accidental variety. It will be seen, however, that our P. parvulus, described on another page of this paper, has 3 radials, one large and two small. Still two seems to be the normal number in this genus. J Monograph of Recent and Fossil Crinoidea, p. 6. 1865.] 162 PROCEEDINGS OF THE ACADEMY OP typical species of Actinocrinus. Hence, if we admit these latter groups, either as genera or subgenera, consistency at least, if not indeed a philosophical system of classification, would require that equal prominence should be given to these corresponding sections of the Platycrinus group. Whatever theoretical views may be entertained on this subject, however, the practical difficulty of ascer- taining the nature of the summit, and the position of the aperture in palaeozoic crinoids, will prevent the general distribution of the species into groups, upon characters of this kind, unless a more profound study of great collections of the remains of these animals, may yet bring to light some coincident, but more easily observed characters, in the structure of the body, or other parts. Platycrinus Niotensis, M. and W. Body below the summit of the first radial pieces cup-sbaped, wider than high ; sides slightly ventricose above the base. Base basin-shaped, several times as wide as high, moderately expanding, rather broadly truncated below, its lower margins projecting slightly downwards around the end of the column, and provided with three very small projections, one at the lower extremity of each of i's sutures. First radial plates large, higher than wide, widening slightly from below upwards, subquadrangular or with the superior lateral angles a- \ittle truncated by the interradial pieces ; each with a concave facet for the reception of the second radials, equalling about half its breadth above, and excavated near one-fourth its length on the outer side, below the upper margin. Second radial pieces trigonal, very small, or scarcely filling the facet or excavation in the upper side of the first radials ; rounded below, with each superior sloping side supporting secondary radials, on the second of which another bifurcation takes place, making four arms to each ray. Arms after the second division described above, simple, and at first composed each of a single series of wedge-shaped plates, but soon passing into a double series of small interlocking pieces, supporting on each side of the arms closely arranged series of long-jointed tentacles. Column near the base compressed and tortuous, being composed of alter- nately thicker and thinner elliptic pieces, with a very minute central per- foration. Surface somewhat granulose ; sutures not grooved, nor distinctly apparent ; those between the basal pieces indicated by a faint linear ridge. Height to summit of first radials, 0-30 inch ; breadth about 0-40 inch. Grea'er diameter of column at base of body, 012 inch ; smaller do. 0-09. Breadth of one of the arms, 006 inch; length of do. apparently an inch or more. In its general appearance, this species is not unlike P. sarce of Hall, (Iowa Report, p. 673, pi. 18, fig. 4), though it is much smaller, has a proportionally much shorter base, and also differs in having but four, instead of six arms to each ray. Locality and position. — Niota, Hancock County, Illinois. Keokuk division of Subcarboniferous Limestone. Platycrinus hemisph^ricus, M. and W. Body rather above medium size, hemispherical, being rounded below, and about twice as wide as high ; base broad basin-shaped, and forming about one third the entire height of the cup, with a pentagonal outline as seen from below; columnar facet between one-third, and one-fourth the diameter of the base, and subelliptical in outline. First radial pieces larger than the basal, wider than high, nearly quadrangular, and widening moderately from below upwards; facet for the reception of the second radial one third as wide as the summit, and extending down about one fourth the length of the plates, — con- cave and sloping outwards, with a deep notch within. Second radial pieces very small, but filling the cavity in each of the first radials, from which they [Aug. NATURAL SCIENCES OP PHILADELPHIA. 163 extend out nearly horizontally — pentagonal in outline, and each supporting on its superior lateral sloping margins the first divisions of the arms, which are comparatively small and bifurcate again on the second piece ; beyond this the two outer divisions remain simple, but the two inner divide again on the second piece, making six arms to each ray, or thirty to the entire series. Arms after the last divisions long, slender, cylindrical, and composed at first of a simple series of quadrangular pieces, but passing gradually upwards into interlocking triangular pieces, and still farther up forming a double series of small alterna- ting cuneiform pieces, supporting closely arranged, long-jointed tentacles. Anal, interradial, and vault pieces unknown. Sutures, excepting between the basal pieces, distinctly, but not widely or deeply channeled. Surface ornamented with rather small, but well denned, prominent nodes. On the base, tnese nodes are arranged in ten rows, five of which radiate from the columnar facet, one to each of the corners ; while those between each of these form intermediate radiating rows, consisting at first of a single range, but becoming a double or triple range near the margin, when the three some- times coalesce laterally. On the first radial pieces two rows pass from just beneath the facet for the reception of the second radials, to each of the inferior lateral angles, while between these there is, at first, a single node, but farther down two or three rows, consisting of nodes which show a disposition to elongate, or coalesce laterally, so as to form little transverse ridges. Above, there is also a row extending horizontally to each superior lateral angle, with a few less regularly arranged nodes on the sides below these. A single trans- versely elongated node sometimes also occurs on the little radials, and one less distinctly defined also sometimes on each of the pieces between this and the next bifurcation. Breadth of body at summit of first radial pieces, 1-07 inches ; height of do. 0-60 inch ; breadth of base 067 inch; breadth of second radial pieces at the summit, 0-54 inch ; do. of second radials, 0-19 inch. From the description, it will be seen this species is rather closely related to P. granulatus of IMiller, which it nearly resembles in form and general ap- pearance. It is a larger and more robust species, however, and differs, not only in the arrangement of the pustules on the base into distinct radiating rows, but according to Austin's figures and description (Monogr., Recent and fossil Crinoidea, p. 33, pi. 3, f. 2,) in having but six instead of seven arms to each ray, as well as in having the arms above the middle composed of a double series of small wedge-shaped pieces, instead of consisting of a single series throughout. From its analogy to P. granulatus, of Miller, it will probably be found to possess, like that species, a long subcentral proboscis. Locality and position. — Crawfordsville, Indiana. Keokuk division of Sub- carboniferous Series. Platycrinus parvulus, M. and W. Body very small, short subcylindrical, or deeply cup-shaped. Base depressed basin-shaped, or several times as wide as high, columnar facet about one third as wide as the base, with a small marginal rim. First radial plates nearly ob- long, being longer than wide, with nearly parallel sides ; some of them with two obscure linear ridges extending from the middle of the upper side, and slightly diverging to the base ; each moderately concave above for the recep- tion of the next range of pieces. Second radial pieces very minute, about twice as wide as long, but not equalling the breadth of the slight concavity in the upper side of the first radials. Third radial pieces, slightly wider than the second, and about of the same length, pentagonal, and each supporting an arm on each superior sloping side. Arms each dividing on the second piece be- yond which they are simple, at least for four or five pieces above, and com- posed of a single series of quadrangular pieces, about as long as wide, ex- cepting the first, which is near twice as long as wide. Tentacles apparently 1865.] 164 PROCEEDINGS OP THE ACADEMY OP comparatively stout. Column near the base nearly or quite round, and com- posed of very thin pieces. Surface smooth. Length of body to summit of first radial pieces 0-12 inch ; breadth of do. 0-12 inch. Length of arm about 0-30 inch; thickness of column, 0-02 inch. This very small species, differs remarkably from all the others with which we are acquainted, resembling it in other respects, not only in its small size, but in having two minute radial pieces in each ray, above the larger first radial piece, making three radials to each ray. Locality and position. — Pope County, Illinois. Chester division of Subcarbo- niferous Series. Genus ACTINOCRINUS, Miller, 1821. Subgenus ALLOPROSALLOCRINUS, Lyon & Casseday, 1860. Actinocrinos (Alloprosallocrinus) euconds, M. & W. Body having the form of the subgenus remarkably well developed, being perfectly flat or slightly concave below the arm bases, and regularly conical above, where it terminates in a rather slender central proboscis. Base very small, with a round, deep, conical depression for the reception of the column, occupying almost its entire area, and surrounded by a narrow, slightly pro- jecting ring-like margin. Radial, interradial, anal and first brachial pieces, all extending out horizontally from the base. First radial pieces hexagonal and about twice as wide as long. Second radials transversely oblong, and rather, smaller than the first. Third radials a little larger than the second, pentagonal or hexagonal in form, and each supporting on its superior (more properly outer) sloping sides two slightly larger secondary radials, each of which is succeeded by another, and the latter each by two brachial pieces, making four arms to each of two rays seen, or twenty to the entire series, if the others have the same number. First interradial pieces larger than any of the radials, heptagonal or octagonal, and supporting two smaller pieces in the next range, beyond which are two others, making altogether five pieces in the only interradial area we have been able to make out clearly. Anal pieces un- known. Vault regularly conical, with slightly eonvex slopes, and armed around the middle with two or three rows of irregularly disposed, short, conical spines, or spine-like tubercles. Proboscis slender and apparently not inclined to either side. Surface smooth, or indistinctly granulose ; sutures very close fitting and difficult to see. Arm bases forming an almost continuous series (being but very slightly interrupted at the anal and interradial spaces) around the base of the abruptly truncated conical body. Column unknown. Height to base of proboscis, about 0.70 inch ; breadth, 1.13 inches. This species is remarkable for its conical form, being almost perfectly flat, or a little concave below the horizon of the arm bases, and rising with slightly convex slopes above, to the base of the proboscis. Hence the whole of the cavity occupied by the viscera of the animal corresponds to the dome only of species of the usual form of Actinocrinus. For the group to which it belongs. Messrs. Lyon & Casseday proposed the name Alloprosallocrinus in 1860, and Dr. Troost had proposed for it the name Conocrinus, in a list published without a description in 1850. Since the above was in type, a more careful comparison with Lyon & Casse- day's description of their A. conicus leads us to suspect that our crinoid may be identical with their species. Still we do not feel satisfied that this is the case, particularly as they describe the columnar facet as involving the basal and part of the surrounding range of pieces ; while it is very small in our crinoid, not even covering the small basal pieces. In addition to this, our specimens seem to show the bases of a more numerous series of arms. [Aug. NATURAL SCIENCES OF PHILADELPHIA. 165 Locality and position. — Six miles southeast of Anna, Union Co., Illinois ; from the St. Louis division of th*e Subcarboniferous series. Collected by Mr. Henry Engelmann. PENTREMITES (GRANATOCRINUS?) granulosus, M. & W. Body small, subglobosus, base deeply concave, particularly in the middle, and not visible in a side view. Radial plates a little longer than wide, about two-thirds as long as the entire body, and tapering from above to the base, each divided by the narrow pseudo-ambulacral areas, down almost to the very base ; lateral margins moderately promiuent. Interradial pieces subtrigonal, or with a fourth obscure angle in the middle below; longer than wide, and each narrowing from below to the summit, where they are perforated by two minute openings. Anal piece of the same size and form as the interradial, with its opening circular, and comparatively large, its outer margin being pro- tected by a small, rather pointed node. Pseudo-ambulacral areas narrow, or sublinear, rather impressed, and each with a distinct longitudinal, linear, mesial furrow ; pore pieces from twenty-five to thirty. Surface marked by comparatively distinct granules, most strongly defined on the interradial and anal pieces, where they sometimes show a tendency to arrange themselves in transverse lines parallel to the lower margin. Height of body, 0-22 inch; breadth of do. 0-23 inch. Breadth of pseudo- ambulacral areas, 0-05 inch. Not having at hand a specimen or figure of the type of Troost's Granatocrinus, we are not quite sure this form belongs to that group, though we have no doubt in regard to the propriety of separating such species from the typical forms of Pentremites. Our species has somewhat the general form and appear- ance of P. Roemeri of Shumard, (Missouri Report, pi. b, figs. 2a, 2b, 2c and 2d,), but differs too widely to render a detailed comparison necessary. Locality and position. — Keokuk division of Subcarboniferous series, near War- saw. Illinois. POLYZOA. Genus EVACTINOPORA, M. & W. EVACTINOPORA RADIATA, M. & W. The interesting fossil upon which we propose to found this genus and species is entirely silicified, and, as seen from below, presents the form of a regular eight-rayed star, the rays being slender, and nearly equalling in length the diameter of the nucleus. In a side view, however, it is seen to be regu- larly rounded in outline below, while the slender rays are observed to be pro- duced upwards in the form of thin vertical laminae, which converge to the centre over the nucleus. The specimen is not in a condition to show whether or not there is a central axis extending all the way up, but there probably is. The rays are thickest below, and taper gradually upwards on their outer margins, which are beveled or carinated all the way down to where they meet at the middle of the under side. Within, they each pass abruptly into a thin lamina, which is poriferous on both sides, and extends to the middle over the nucleus. The pores are circular, with a slightly prominent margin, and regularly dis- posed nearly in quincunx, at intervals about equalling their own diameter, or sometimes less. They only exist in the thin portion of each ray, while the thicker outer and inferior portions seem to be nearly or quite solid. We are not able to determine satisfactorily whether this was a free or an attached Bryozoon; but if attached, the stem or point of attachment was pro- bably very small. Greatest transverse diameter to the extremity of the rays, 0-90 inch ; do. of nucleus between the rays, 0-35 inch ; thickness of the outer margin of each ray near the nucleus, 0-10 inch ; diameter of pores about 0-02 inch. 1865.] 166 PROCEEDINGS OF THE ACADEMY OF Locality and position. — The only specimen of this fossil we have seen is in a granular mass of decomposing chert, containing some fragments of small cri- noid columns. It was obtained from the Subcarboniferous rocks of Missouri, but the exact locality and position we have been unable to ascertain. Note on the genus GILBERTSOCRINUS, Phillips. BY F. B. MEEK. Genus GILBERTSOCRINUS, Phillips, 1836. Gilbertsocrinus, Phillips, Geol. Yorkshire, part ii., p. 207, 1836. Goniasteroidocrinus, Lyon and Casseday, Am. Jour. Sci. xxviii. p. 233, 1859. Trematocrinus, Hall, Sup. Iowa Report, p. 10, 1860. Phillips' diagnosis of this genus reads as follows : " Basal joints five, forming a pentagon ; suprabasal [subradials] five, hexa- gonal, forming a decagon with five re-entering angles, from which proceed five heptagonal first costals [first radials] and five hexagonal second costals, [second radials], bearing a pentagonal scapula [third radial] supporting joints [secondary radials] which combine into rounded arms perforated in the centre. First in.tercostals [first interradials] pentagonal. The following species have been usually referred to Rhodocrinus, Miller, from which, it appears to me, they differ entirely." (Phillips.) He mentions but the following three species, viz., G. calcaratus, G. mammil- laris and G. bursa, all from the subcarboniferous. His specific descriptions are very brief and unsatisfactory, but his figures are tolerably good, and give a , sufficiently intelligible idea of the generic characters of the group. From these .figures, and his description, it is therefore evident that the formula, in accord- ance with the later improved nomenclature, may be stated as follows: Generic formula of Gilbertsocrinus. Basal pieces 5. Subradials 5. Radials 3x5. Secondary or supraradials 3 or 4x10. Anal and interradial pieces 12 to 15x5. Pseudo-brachial appendages (arms of some authors) 5, located over the rays. Arm-openings (ambulacral,) 10, located directly under the pseudo-brachial appendages. On comparing this formula with the following, given by Messrs. Lyon and Casseday, of Goniasteroidocrinus, cited above, the close relations of these crinoids will be, apparent. Generic formula of Goniasteroidocrinus. Basal pieces 1x5, pentagonal, perforation not visible. Subradial pieces 5, hexagonal, nearly equal in size. Primary radial pieces 3x5, first spiniferous. Secondary radials 3X 10, hexagonal. Interradial fields [including the anal area] 5x13 to 14, [pieces each]. Interbrachial fields 5x1 to 9, [pieces each]. It may be proper to explain that the term pseudo-brachial appendages is used in the formula of Gilbertsocrinus, for the parts regarded by Phillips and by Messrs. Lyon and Casseday as arms, and that arm-openings, not alluded to by Phillips in his description, though clearly shown in his figur. s, are men- tioned. These openings were not observed by Lyon and Casseday, because they were hidden in their specimens by the attachment of the small pendulous true arms, or, in the absence of the latter, by portions of the matrix, as is known to the writer from the examination of specimens of their typical species loaned by Mr. Lyon. / [Aug. NATURAL SCIENCES OF PHILADELPHIA. 167 It will therefore be seen that, excepting, in mere specific details, these formu- las, as far as they go, agree exactly. There is, however, a character which, although not apparent in Messrs. Lyon and Casseday's formula, was neverthe- less mentioned in their description, in which the types of these groups differ, that is, in the position of the pseudo-brachial appendages (arms of Phillips and of L. and C.) with relation to the other parts. In Gilbertsocrinus these appendages are placed directly over the arm-openings and above the inter- brachial spaces, while in Goniasteroidocrinus they stand over the interradial spaces. There may be various opinions in regard to the value of such a difference, but to the writer it seems of not more than subgeneric importance. If these appen- dages were true arms, or like the arms in other crinoids, designed to support the reproductive organs, (" conceptacula,") little doubt could be entertained in regard to the full generic value of such a difference in their position. The fact, however, that although provided with a central cavity through their entire length, theyr have nowhere any external openings, being as it were hermetically sealed, is conclusive evidence that they could have performed no such function. Hence it is probable they should be viewed rather as being in some respects analogous to the lateral branches, or verticils, so often given off from the columns of Platycrinus and other crinoids. This opinion seems to derive sup- port from the fact that, in some of the typical forms of Gilbertsocrinus, as well as in American species of Goniasteroidocriniis, these appendages, at their origin, consist of a double series of pieces, pierced each through the centre by the only cavity they posses, exactly like the joints of a column, or those of its lateral branches, for which latter they might readily be mistaken, if found detached. From all the facts it seems probable, therefore, that the only relations these false arms bore to the reproductive system, was that of strong rigid guards thrown off from the margins of the dome, for the protection of the slender, true ova-bearing arms hanging beneath them. Hence, although their existence or absence may be a good generic distinction, ihe'ir position over the interradial, or interbrachial spaces, can scarcely be regarded as such. It will probably be remembered that, in a paper read before the Academy by Prof. Worthen and the writer, in September, 1860, and published in the Pro- ceedings for that month, (p. 383), we suggested that a genus proposed by Prof. Hall at about the same time, under the name Trematocrinus, was apparently very closely related to Goniasteroidocrinus, Lyon and Casseday, 1859, and that we should not be surprised if it would prove to be the same. Having recently had an opportunity, through the politeness of Mr. Lyon, to examine good spe- cimens of the typical species of the latter, the writer is completely satisfied that there is not the slightest generic or even subgeneric difference between the types for which these two names were proposed,* and as Lyon and Casseday's name has priority, it will have to be retained for the group, whether we regard it as a genus or a subgenus. It is true the later name is shorter and more euphonious, but we have no right for that reason to make it an exception to the generally accepted law of priority. It is surely not greatly more objec- tionable than Macrostyloerin.ua, Hall, still retained by its author instead of the later name Cytocrinus, Roemer. The following are the American species of this group, viz. : Gilbertsocrinus (Goniasteroidocrinus) tuberosus, Lyon and Casseday; Gilbertsocrinus (Goniast.) fiscellus, = Trematocrinus fiscellus, Meek and Worthen ; Gilbertsocrinus {Goniast.) typus, G. (Goniast.) tuberculatus, G. (Goniast.) papillatus, G. (Goniast.) robustus, and G. (Goiiiast.) spinigerus, = Trematocrinus typus, T. tuberculatus, T. papilla- tus, T. robustus and T. spinigerus, Hall. * As already stated, it was ascertained from the examination of Mr. Lyon's typical species, that it possesses the same ambulacral openings as the species upon -which Trematocrinus was founded ; and that the slender pendulous "plumose cilia' of Lyon and Casseday (here regarded as true arms) are connected with these openings, as the arms of other palaeozoic crinoids connect with the arm openings, excepting that they hang down, iustead of ascending. • 1865.] 168 PROCEEDINGS OF THE ACADEMY OF Note on a Species of WHALE occurring on the coasts of the United States. BY E. D. COPE. As a contribution to the history of the cetaceans of the Atlantic, I desire to give a brief account of the osteological characters of a species of whale- bone whale, the Black Whale of the whalers of our coast. Individuals are frequently cast ashore Eastward, and some are known to enter New York harbor. They were formerly abundant about the mouth of the Delaware : a letter of Wm. Penn's, dated 1683, states that eleven were taken that year about the capes. Five specimens are stated to have been seen in the Delaware river since that time, and two of great size are recorded to have been found on the coast of Maryland.* Three have come under my notice, one taken opposite this city three years ago, one cast ashore in Reho- both Bay, Del., and one in Mobjack Bay, Va. The first of these, a half grown individual, was taken and exhibited for some time, and its nearly complete skeleton, presented by George Davidson, occupies a prominent place in the Academy's museum, and has afforded the best means of determining the affinities of the species. From an examination it is' evident that it is a species of the genus Eubalaena, Gray, therefore widely different from the right whale, Balaena mysticetus, and congeneric with the B. australis and antipodarum of the Southern seas. While dif- fering in many points from the first, it is strongly separated from the last two, and has no doubt remained without proper notice up to thepresent time. The total length of the specimen, in which all the epiphyses are as yet un- united, is thirty-one and a half feet ; which the presence of the intervertebral cartilages would extend to thirty-seven ; of this the head, measured axially, is eight feet five inches, or a little less than one-fourth. This proportion is similar to that of the australis. The vertebrae are fifty-six, of which the seven cervicals are all united, the posterior three in the lower part of their centra only ; above, they form a solid crest, the atlas and the last attached by the superior part of their neural arches only. The fourth, fifth and sixth cervical diapophyses are distinctly united .on one side, while the remainder are separate ; on the other side the seventh is united with the three posterior, and the three anterior are united. The first, second and third only have inferior transverse processes. The thirty-first vertebra from the cervicals, or sixteenth from the last rib is the first that encloses the vertical foramen with the diapophysis, and the neural spine is strong on the thirty-seventh. Of the ribs, which appear to have been all preserved, there are fourteen pairs ; the an- terior are single headed. Of the dorsal vertebrae the first four have slender elongate diapophyses ; the anterior zygapophysis is first definitely separated on the tenth. The scapula is 29 inches broad by 23 high. The outline of the top of the muzzle is much arched ; the frontal orbital processes are subtransverse and rather broad. The supraoccipital is more produced anteriorly than represented by Cuvier in the a u s t r a 1 i s.f Nasals heavy, nine inches and a half long by three, or distally four inches broad, much as represented for the B. mysticetus. J with the posterior outline oblique inward, attached by a plicate suture. They are much narrower than in the Leyden Eubalaena, which is evidently not the true australis, whose skeleton I have studied in the Jardin des Plantes. In the periotic bones there is much peculiarity discoverable. The specific characters are confirmed by the same portion of a much larger individual from Newport, R. I. The meatus is narrow, occupying nearly the whole length of the bulla, but is nearly closed by the curved marginal anterior pro- cess. Its form from below is that of a rounded trapezium, with a deep ante- * Watson's Annals of Philadelphia, ii. 428. t Ossemens Fossiles, pi. 226. J Flower P. Z. S. London, 1864, 390. [Aug. NATURAL SCIENCES OF PHILADELPHIA. 169 rior groove. Anteriorly it is much more obliquely transverse than figured by Cuvier : the posterior process of the periotic is only half as long as the anterior, and the latter is cylindrical acuminate not spatuliform at the extre- mity. From above, these processes are nearly parallel, while they are very widely divergent, and equal in the auatralis ; the interior outline instead of being truncate, has a massive acumination. On the posterior view the anterior process is nearly concealed. The humerus is short and furnished with a large bicipital process, marking one-third of its length. The points in which this species differs from the austral is, as yet im- perfectly made known, are the more acuminate parietals, the presence of four more vertebrae, where the last neural spine stands on the thirty-seventh in- stead of the thirty-fourth ; and one more pair of ribs ; the considerably greater breadth of the scapula, and strongly peculiar periotic bones. This species may readily occur on the European coasts, and is no doubt allied to, or the same as, the species pursued by the Biscay whalers, which Eschricht* says is related to the australis. This does not appear to have been described, though catalogued without reference by Gray and Flower, under the name of biscayensis. The former saysf its head is two-fifths the length, by what authority does not appear, as he states that he has not seen specimens. The characters which separate the genus Eubalaena of this au- thor, from Balaena, appear to be very slight. Harlan, in Fauna Americana, includes a species Balaena glacialis Klein, or Nord-Caper of some old authors. There is no real description of this ani- mal extant, and Scoresby and Cuvier regard it, with good reason, as imaginary. The species above described maybe called Balaena cisarctica; its skeleton will be more fully illustrated in a future publication. On some Conirostral BIRDS from Costa Rica in the Collection of the Smith- sonian Institution. BY JOHN CASSIN. 1. Sporophila corvina, (Sclater.) Spermophila corvina, Sclat., Proc. Zool. Soc. London, 1859, p. 379. One specimen only, which is in adult plumage, and presents all the charac- ters of this species given by Mr. Sclater, as above. San Jose, Mr. J. Carmiol. 2. Phonipara pusilla, (Swainson.) Tiaris pusilla, Swains., Philos. Mag., 1827, p. 438. San Jose, Mr. J. Carmiol. 3. Pyrgisoma Kieneri, Bonaparte. Pyrgisoma Kieneri, Bonap., Consp. At. i. p. 486, (1850.) One specimen only, which is in adult plumage, and is the first that I have ever seen. This species is clearly distinct from P. biarcuatum, though strictly of the same genus, being smaller, and having a strong character in the wide transverse band on the breast. It is sufficiently described by the Prince Bona- parte, as above. Dr. Cabanis' note on this species and P. biarcuatum in Journ. Orn., 1860, p. 412, is to me difficult to understand, especially as he seems never to have seen the latter bird nor the description of it in Voy. Venus, Zoologie, vol. v. p. 216, (Paris, 1855.) The two species are quite distinct. Mr. J. Carmiol. 4. Melozone ledcotis, Cabanis. Melozone leucotis, Cab., Jour. Orn. 1860, p. 413. Specimens in adult plumage. This species is not, in my opinion, of the same genus as the preceding and P. biarcuatum. Angostura, Costa Rica March 2, 1864. Mr. Carmiol. *Comptf s Rendus, 1860, p. 924. * Ann. Mag. Nat Hist. 1860, d 348 1865.] P 170 PROCEEDINGS OF THE ACADEMY OF 5. Pitylus grossus, (Linnseus.) Loxia grossa, Linn., Syst. Nat. i. p. 307, (1766.) One specimen in young plumage. Paqua, Mr. J. Carmiol. 6. Embernagra striaticeps, Lafresnaye. Embernagra striaticeps, Lafres., Rev. Zool., 1843, p. 154. Clearly this species, and quite similar to specimens in the Academy Museum bearing the valuable labels of M. Jules Verreaux. Specimens of Arremon coni- rostris, Bonap., are also in the Academy Museum, from the same excellent naturalist, and labelled with his usual great care and accuracy. The dis- tinctions between these two species are indicated correctly by Messrs. Sclater and Salvin in Proc. Zool. Soc. London, 1864, p. 352, but unfortunately with their usual great economy of words! Angostura, June 8, 1864. Mr. Carmiol. , 7. Arremon rufidorsams, nobis. Allied to A. aurantiirostris, spectabilis and erythrorhynchus, and about the same size, but with the back chestnut. Bill red ; edges of wings at shoulders yellowish-red. Head above black, with a medial longitudinal band of dark ashy; cheeks black, long superciliary line white. Back chestnut; rump and upper tail coverts dark olive green; wings dark green, the outer coverts tinged with chestnut; shoulders narrowly edged with yellowish red; tail brownish black. A wide pectoral band, black, edged below with dull greenish ; chin black ; throat and middle of the abdomen white; flanks and under tail coverts dark olive green, (especially the under tail coverts;) under wing coverts green ; bill bright yellowish red ; feet greenish brown. Total length about 6J inches, wing 3, tail 2£ inches. Hob. — Turrialba, Costa Rica. May 24, 1865, Mr. J. Carmiol. Resembles most nearly A. spectabilis, Sclater, Proc. Zool Soc. LondoD, 1854, pi. 67, but has a wide pectoral band and dark green under tail coverts, and differs from that and all other allied species in having the back chestnut. In the present specimen the bill is bright yellowish carmine, paler at the base of the under mandible. 8. Buarremon brunneindchds, (Lafresnaye.) Embernagra brunneinucha, Lafres., Rev. Zool., 1839, p. 97. Dota, Costa Rica, July 24, 1864. Mr. J. Carmiol. 9. Buarremon crassirostris, nobis. Bill strong and larger than usual in this genus ; wing short, rounded ; tail rather long; feet strong. Head above dark chestnut, which color extends somewhat on the back of the neck ; throat and sides of the head fully encircling the eyes dark greenish brown, (nearly black,) some feathers of the throat and others forming an obscure line from the corner of the under inaudible white at their bases. Entire upper parts of body dark olive green, lighter on the rump, a few of the longer upper tail- coverts tinged with brown ; wing dark brown, all the quills and coverts widely edged with green, uniform with the back. Middle of breast and abdomen bright greenish yellow, sides, tibia? and under tail-coverts dark green, very nearly uniform with upper parts of body ; tail dark brown, nearly black. Bill light colored, (in specimen, the upper mandible is light yellowish horn color, under mandible pale yellowish ;) feet reddish- brown. Total length about 6 inches ; wing 3, tail 2f inches. ffab. — Barranca, Costa Rica. Aprill4, 1864, £, Mr. J. Carmiol. This bird forms a new subdivision of the genus Buarremon, easily character- ized by its strong and more Pyranga-like bill. It is most nearly related to the species of the group Pipilopsis, but does not intimately resemble any of those nor other species known to me. [Aug. NATURAL SCIENCES OP PHILADELPHIA. 171 10. Buarremon chrysopogon, (Bonaparte.) Chrysopoga typica, Bonap. Consp. A v. i. p. 480, (1850.) Ataleptes chrysopogon, Bonap. Buarremon gutturalis, Lafres., Rev. Zool., 1842, p. 97? This bird seems to be regarded by authors as entitled to the name here adopted, but specimens in the Academy Museum bear Paris labels : " Arremon gutturalis, Lafres." Dota, Costa Rica, July 24, 1864. Mr. J. Carmiol. 11. Chlorospingcs albitemporams, (Lafresnaye.) Tachyphonus albitemp oralis, Lafres., Rev. Zool., 1848, p. 12. San Jose, Gosta Rica. Dr. A. von Frantzius. 12. PHffiNicoTHRAUPis rubicoides, (Lafresnaye.) Saltator rubicoides, Lafres., Rev. Zool., 1844, p. 41. Grecia, Costa Rica, Dec. 12, 1864. Mr. Carmiol. 13. Tachyphonus DeLattrei, (Lafresnaye.) Tachyphonus DeLattrii, Lafr., Rev. Zool., 1847, p. 42. One specimen only of this species in very fine adult plumage, but not dif- ferent in any respect from others in the Academy Museum from New Grenada. This bird is scarcely a Tachyphonus, nor congeneric, properly, in my opinion, with any other bird with which I am acquainted. Paqua, Costa Rica, March 23, 1865. Mr. J. Carmiol. 14. Tachyphonds luctuosus, D'Orbigny et Lafresnaye. Tachyphonus luctuosus, D'Orb. et Lafres., Mag. Zool., 1837, p. 29. D'Orb. Voy. Am. Ois., pi. 20. Numerous specimens, in nearly all of which the males have a partially con- cealed but well defined coronal spot of pale yellow, a character not previously known in this species. Those evidently in quite mature plumage are larger than D'Orbigny's specimens in the Academy Museum, but not larger than his figure above cited. The coronal spot is not present in D'Orbigny's specimens, nor in numerous others which I have examined, and I suspect it appears only at maturity, or in full nuptial plumage. No other peculiar character is appa- rent to me in the present specimens. Angostura, March 10 and June 7, 1864, and March 16, 1865. Mr. J. Carmiol. 15. Tan agra Diaconus, Lesson. Tanagra Diaconus, Less., Rev. Zool., 1842, p. 175. San Jose, Costa Rica, April 5, 1864. Mr. J. Carmiol. 16. Tanagra melanoptera, Hartlaub. Tanagra melanoptera, Hartl., Rev. Zool. Turrialba, Costa Rica, March 9, 1864. Mr. J. Carmiol. 17. Pykanga bidentata, Swainson. Pyranga bidentata, Swains., Phil. Mag., 1827, p. 428. "Iris Yellow." Birris, Costa Rica, May 17, 1865. Dr. A. von Frantzius. 18. Lanio ledcothorax, Salvin. Lanio leucothoraz, Salv., Proc. Zool. Soc. London, 1864, p. 581. Numerous specimens, all of which present with much uniformity the peculiar characters of this curious species as given by its discoverer, that excellent naturalist and most judicious and liberal patron of the zoological sciences, Osbert Salvin, Esq., of London. Angostura and Payariqui, Costa Rica, March, 1865. Mr. J. Carmiol. 19. Euphonia fulvicrissa, Sclater. Euphonia fulvicrissa Sclat., Proc. Zool. Soc. London, 1856, p. 276. Specimens apparently quite identical with others from New Grenada in Oipt. Michler's collection in the Smithsonian Museum. Angostura and Paqua, Costa Rica, March, 1865. Mr. J. Carmiol. 1865.] X72 PROCEEDINGS OF THE ACADEMY OF 20. Euphonia hirundinacea, Bonaparte. Euphonia hirundinacea, Bonap., Proc. Zool. Soc. London, 1837, p. 117. Turrialba, Costa Rica, March 10, 1864. Mr. J. Carmiol. 21. Eophonia gracilis, (Cabanis)? Fhonasca gracilis, Cab., Jour. Orn., 1860, p. 333? Young birds, which seem to be this species. Mr. J. Carmiol. 22. Eophonia Annexe, nobis. About the size of and resembling E. ruficeps, D'Orb. et Lafres., but with the under parts of body clear yellow, and the under tail coverts white. Bill mode- rate, rather wide at base; wing short, with the third quill longest; tail short. Head above to occiput dark yellowish chestnut, other parts of head, including throat, black; body above, wings and tail fine dark violet-purple, (not steel blue, as in E. ruficeps;) under parts of body clear yellow; under tail-coverts white. Quills black ; inner webs of secondaries and tertiaries with large white spaces ; tail feathers black, edged with violet purple, the outer feathers with large while spots in their terminal halves. Bill and feet dark bluish, (in skin.) Total length about 4£ inches ; wing 2J, tail If inches. Bab. — Sauta Rosa, Costa Rica, March 3, 1865. Mr. J. Carmiol. Specimen in Museum Smithsonian Institution, Washington. Of this interesting species one specimen only is in the collection of Mr. Car- miol, and is fortunately in adult plumage. It is allied to the South American E. ruficeps, zanlhogaslra and others, belonging to the subgroup designated Acroleptes by Dr. Cabanis. (Jour. Orn., 1861, p. 90.) This bird has the upper pans fine lustrous violet-purple, quite different from the steel blue and violet of E. ruficeps, and it differs also in having the under parts clear yellow without orange or darker shade, as in that species. The under tail coverts are white in this species, but yellow in all its allies. Tail slightly emarginate. This handsome liitle bird is dedicated to the lady of my friend Daniel CUraud Elliot, Esq., of New York, whose excellent judgment and exquisite taste have most efficiently aided her husband in the production of the most splendid orni- thological works ever produced in this country. New P0LYZ0NIID.E, Gervais. BY HORATIO C. WOOD, JR., M. D. Glomeris bicolob. G. parvus ; dorso olivaceo-nigro, linea mediana brunnea (interdum obso leta) ornata ; lateribus dilute brunneis; oculi utrinque 6. The eyes are arranged in two straight linear series, of six each, on the outer edge of the head. The antenna are somewhat elongate, filiform, and com- posed of seven joints. Their last article is very small and inconspicuous, but the penultimate is very large and long. The first scutum is semilunar and of a brownish tint. The second is not very large, and has the anterior half of its surface chased with numerous parallel transverse lines. Each scutum has a transverse, somewhat semilunar, dark olive blotch, which, from the second to the last, covers the whole of its dorsal surface. The second scutum has a blotch of about the same size as the others, and another very small one in front of this. The last scutum is brown- ish with a rather indistinct olive blotch on each side. This species is very interesting from the fact of its being the first Glomeris found in Asia. As it has only 12 eyes, some naturalists would consider it as representing a new genus, and if it is hereafter found that there are other Asia- tic species with this peculiarity, I myself would regard it generic. Almost, if not quite, all the European and African species have 16 eyes ; but a genus has been described with the name Gervaisia, from the Carpathian mountains, which has but five pairs of eyes. Taking this fact into consideration, I have [Aug. NATURAL SCIENCES OF PHILADELPHIA. 173 hesitated to consider this one character sufficient to indicate a new genus in a single species. Hah. Hong Kong. Wm. Stirapson, M. D. OLIGASPIS* n. g. Corporis segmenta 9 ; antennae brevissimas, quinque articulatae. Oculi aggre- gati. This genus is allied to Zephronia, from which it differs entirely in the num- ber of its segments. The antennae are very short and thick. 0. PUNCTICEPS. O. dilute olivaceo brutmeus, capite et segmento cephalico castaneis ; capitis superficie anticafere rude punctata; segmeutis postice obscure rubido-brun- ' neo marginatis. The head superiorily is emarginate and a little swollen at its external angles so as to give somewhat of a reniform appearance. Its vertex is smooth. Many of the scuta have a large dark olive blotch or even blotches. Their sur- face is mostly smooth and polished. The last scutum is very closely and dis- tinctly punctate. The male genital organs have a pair of very heavy forceps on each side, resembling the claws of a crab. These are placed at an angle with one another, their bases attached to opposite sides of a broad plate. On one side of their lower part is a curious surface corrugated by close, straight, parallel furrows. Springing from the top and centre of this broad plate are a pair of straight diverging small processes, with a conical central tongue or process. I have never had an opportunity of examining a female. For figures, illustrating this species, see my forthcoming Monograph of North American Myriapoda. [Trans. Philos. Soc] "Hab. Port Natal. Rev. Alden Grout. Mus. A. N. S. On a New Genus of VE3PESTILI0NID2E. BY H. ALLEN, jM. D. The genus Synotus, founded by Keyserling and Blasius,f had for its type the common Barbastelle. But Dr. GrayJ and Buonaparte, § having previously defined Barbastellus as a distinct genus, it follows that Synotus is but a syn- onym of Barbastellus. In my memoir on N. A. Bats,|| I followed Wagner,^ who placed both the American and European species under Synotus. A more extended study of this group has convinced me that this course is untenable. There is not sufficient evidence in the diagnosis of Synotus, as given by K. and B., to warrant the conclusion that it was intended to apply to the Amer- ican species ; and since they cannot be received by either Plecotus or Vesper- tilio, it is necessary to propose a new genus to include them. CORYNDRHINUS, n. g. Skull slightly depressed at vertex ; supra-occipital region inflated, sides inconspicuous ; frontal bones without crest. Nasal bones, broad, flat, not depressed ; median fossa marked, — linear ; superior border of anterior nares rounded ; summits convex and somewhat higher than orbital processes of superior maxillae. The latter processes are swollen, and extend anteriorly * Oxiyoc d(T7ri;, Scutum. * 1 Wirbel thier* Europas, 1S40, 55. J Zoological Journal, ii. 1826, 243. $ Fauna Italica Fasiculo 15, tab. 15, 1836. j Monag. N. A. Bats, Smithsonian Inst.. June, 1864. f Schreb. Sang. y. 1855, 719. 1865.] 12 174 PROCEEDINGS OP THE ACADEMY OP beyond the incomplete infra-orbital ridges, to which the infra-orbital fora- mina are nearly contiguous. Zygomatic arch expanded at posterior third. Molars 5. Cochlea? not visible. Internal basal lobe of ear rounded, thicken- ed, gradually losing its distinctness along the marked fold at inner border. Inter-auricular membrane rudimentary ; external basal lobe terminating on a line with the angle of the mouth ; it possesses a manifest lobe on the internal surface. Antitragus scarcely perceptible. Tragus pointed gradually, ex- ternal basal lobe conspicuously cupped. Nose with two lateral hairy con- Terging excrescences — nostrils wider than long, subtriangular. No rounded swelling at base of foot. Vertebrae of tail, <.* C. MACROTIS.f Head half the length of body. Upper lips tumid, — on sides of face rather thickly set with pendant hairs. Excrescences on a line with the lateral border of nostrils sparsely haired ; tuberosities at base flattened, well defined posteriorly. Nostrils terminal, of an irregular triangular shape, the apices pointing inward ; exterior lateral angle acute, borders not everted ; mental space narrow, crescentric. Ears, length of body, with internal fold one-fifth width of auricle, sparsely haired at internal border, tips turned slightly out- wards ■ outer half of auricle marked with irregular transverse lines ; the inner lip to external basal lobe convex, nearly as high as long. Antitragus simple, linear. Tragus nearly half the height of auricle, interior border' thickish and marked with a few hairs, tip rather blunt; exterior basal lobe longer than wide inner and outer borders deflected upwards. Outer end of the free edo-e of the sigmoid internal lobe thickened. Fur long and silky, that of the back of a blackish hue at base, verging to an obscure fawn or brown at tip. The hair is, therefore, indistinctly bi-colored. The extent of the tip colora- tion varies but in all specimens that of the color of the base predominates. The hair of the belly is blackish at root, in some specTmens slightly plumbe- ous. Tips grayish, running to white toward the pubis. ♦Compare Plecotug {P. auriius.) Skul!#not depressed at vertex; supra-occipital space well defined but little inflated; frontal bone crested. .Nasal bones narrow, depressed, no median fossa. Orbital process produced, bounded anteriorly by the infra-orbital ridge, which is sharply defined, complete, and protects the infra-orbital foramen immediately in front. Zygomatic arch expanded at middle third. Molars £; cochleae not visible.— Internal, basal lobe of ear obscure; a thin papery fold terminating the internal border, and rung thence upwards and inwards, terminates in a prominent, thickish lobe, forming the outer boundary of the large inter-auricular membrane. Antitragus salient, convex, external basal lobe simple. Tragus bread, points sharply; external basal lobe developed, incurred upon itself. Nose simple— nostrils longer than wide, with tumid inner, walls. Base of foot with small rounded spelling. Joints of tail, 8. Vespertilio. {V. subulatus.)— Skull not depressed at vertex; supra-occipital region greatly swollen; par-occipital process trenchant, matly as long as condyles; nasal bones narrow, convex, higher than orbital process, and tape ing from above downwards. Orbital process slight, swollen, not involving side ot face ; infra-orbital foramen at posterior fourth of orbito-nasal space. Zygo- matic arch convex, not expanded, becoming more slender posteriorly, depressed in middle. Cochleae visible. Molars £.— Internal basal lobe of ear simple, acute, inner border of auricle simple. No swelling at. base of foot. Vertebrae of tail, 9. BarbasUlius. (B. communis.)— Skull scarcely depressed at parietal suture. Nasal bones flat, depressed below the level of the orbital process; internal process produced inferiorly at anterior nares. Infraorbital ridge rudimentary, foramen midway between orbit and anterior nares. Zygo- matic arch straight, and of uniform tenuity. Molars A. Cochleae visible posteriorly. — Internal basal lobe of ear scarcely perceptible, not joining the small inter-auricular membrane; internal border of ear not folded backwards, but erect; external border sinuate; external basal lobe simple, terminating above the angle ot the mouth. Antitragus sharp, well defined, convex. Tragus points gradually, external border obscurely bi-eiuarginated ; basal lobe simple, inferior border alone curved, to form a minute wart. Nose simple, truncate; nostrils irregular, inner border produced laterally* not tumid. No rounded swelling at base of foot. Joints of tail 9. (This genus has remote affinities with Nycteris aud Megaderma.)* t (Mon. N. A. Bats, loc. cit.) • Histiotus, Gervais, (Castelnau's L' Amerique du sud Mam. 1855, p. 7" , pi. xiii. f. 6) apparently belongs to this group. 1 have not had an opportunity of examining it. [Aug. NATURAL SCIENCES OF PHILADELPHIA. 175 C. TOWNSENDI. Head length' of body. Upper lip slightly tumid on sides of face, a line of delicate hairs pendant. Excrescences sparsely haired ; tuberosities swollen at base, bulging, outline obscure iuferiorly. Nostrils terminal, of an irregu- lar trilobed shape ; external lateral angle obtuse, edges everted, with internal inferior border rimmed. Chin with a wide triangular mentum. Ears with internal fold one-fourth width of auricle, sparingly dotted with hair. Inner lip to external basal lobe convex, much longer than high. Antitragus inconspicu- ous. Tragus nearly half the height of auricle ; internal border thickened, and slightly haired ; exterior basal lobe indistinctly quadrangular, wider than long, and somewhat flattened externally, border convex ; central inci- sions of upper jaw almost unicuspid.* Fur long and silky, on back less distinctly bi-colored than in the preceding species, verging in some individuals to unicolor. The tips are of a darkish brown mixed with grey, verging to the style seen in macrotis. The fur of the belly is also blackish at base, with occasionally a ferruginous tinge ; the tips are of two kinds, either a whitish hue, as in macrotis, or of an indistinct yel- lowish brown. The points mentioned in the above descriptions with reference to the " in- ternal basal lobe" and "inter-auricular membrane," may need explanation. A simple auricle is seen in V. subulatus with a clearly defined internal border and basal lobe. In Plecotus, Barbastellus and Synotus a crescentic fold of membrane is seen at basal region of internal portion of auricle, which is evidently homologous with the free lobe of the simple auricle. But surrounding and extending upwards from it along the inner border .is a membranous fold, which renders the true outline obscure. Such growths I consider to be appendages to the auricle, and, while complicating the detail of structure, in no Fay affect the plan. Should these folds meet across the head, there woulcrbe formed an "inter-auricular membrane ;" this may be complete, (that is, extending the entire length of auricles), as in some genera of Noctilionida? and Megadertnatidas ; or it may be rudimentary, as in the above genera. In the latter class the appendages are quite largely de- veloped, though not touching ; and in this connection they may be considered to be rudiments of an inter-auricular membrane. September 5 th. The President, Dr. Bridges, in the Chair. Fifteen members present. Dr. Leidy remarked, that of the two fishes from the Isle of Shoals, N. H., presented this evening by Mr. W. M. Canby, one was of unusual interest. It was a foetal Dog-fish, or Dog-shark, with the vitelline sac appended to its ab- domen, which Mr. Canby had obtained, together with others, from a gravid parent fish. Mr. C. had heard a dispute among several persons as to whether the Dog-fish (Acanthias Americanus) laid eggs or brought forth living young, and, having mentioned the matter to a fisherman, the latter said they brought forth living young; and an opportunity offering shortly afterwards, proved it by opening a gravid female and taking out the living young, of which the specimen presented was one. • The deaths of Sir Wm. Jackson Hooker, of England, and Mr. Charles J. Wistar, of Germantown, correspondents of the Academy, were an- nounced. * In Mon. loc cit. p. 66, read, on 7th line, leu " distinctly bifid at cutting edge." 1865.] 176 PROCEEDINGS OF THE ACADEMY OF September I2ih. The President, Dr. Bridges, in the Chair. Eighteen members present. The deaths of Mr. Jacob R. Smith and Mr. Joseph D. Brown, mem- bers of the Academy, were announced. September 19th. The President, Dr. Bridges, in the Chair. Twenty members present. The following papers were offered for publication : " On a new generic type of Sharks," and " On two species of Del- phinidae." By Prof. Theo. Gill. " Notes on a species of Hunchback Whale." By Prof. E. D. Cope. Dr. Leidy directed the attention of the Academy to some fossil remains of Rhinoceros from Texas and California, which, he observed, together with those already described by him from the Mauvaises Terres of White River, and from the Niobrara or L'eau-qui-court River, of Nebraska, were probable evidence of the former existence of five species of the genus within the boundaries of the United States. One of the species, previously described, from White River, is so peculiar as to constitute a subgenus apart from the others. It was a small animal, with a hornless skull, and possessed six incisors and a pair of canines in each jaw, besides the usual series of seven molars on each side. It was named Hyraco- don nebraskensis (Proc. Acad. Nat. Sci. 1856, 92.^ The second species, Rhinoceros occidentalism from White River, has the same formula of dentition as the Indian or Javan Rhinoceros, and was about half the size of that animal. Rhinoceros crassus, (Pr. Ac. 1858, 28), from L'eau-qui-court, has the same formula of dentitiou as the Indian Rhinoceros, and was about the same size. The incisors appear to have held the same proportionate size as in the latter, but in R. occidcnlalis they were proportionately very much smaller. A worn superior incisor of R. crassus measures 28 lines antero-posteriorly and 10 lines transversely. The corresponding tooth of R. occidentals measures 11 lines by 5 lines. A broken superior last molar of the former is estimated to have measured 28 lines obliquely and externally, the same diameter transversely and anteriorly, and 24 lines antero-posteriorly and internally. In R. occidentalis corresponding measurements hold the relationship of 18 lines, 18 lines, and 16 lines. The Texan Rhinoceros is indicated by the greater and more characteristic portion of the crown of an upper molar tooth, probably the penultimate. It was obtained from a tertiary deposit, probably miocene, and submitted to Dr. L. for examination, by Dr. Benj. F. Shumard. It presents much the general appearance of preservation of the Mauvaises Terres fossils of White River. It evidently indicates a species different from those of the latter locality, and was larger than either, approaching in size R. crassus, though it was smaller. The estimated measurements of the restored tooth are two inches for the an- tero-posterior diameter externally, 22 lines for the transverse diameter ante- riorly, and 18 lines in the latter direction posteriorly. The median valley is strongly sigmoid, arising from each of the inner lobes being provided with an oblique offset extending into the valley in a parallel manner. For the species the name of Rhinoceros meridianus was proposed. The California Rhinoceros is indicated by the greater portion of the right' [Sept. NATURAL SCIENCES OF PHILADELPHIA. 177 side of a lower jaw retaining the symphysis ; from Chili Gulch, Calaveras Co., and was submitted to Dr. L.'s inspection by Prof. J. D. Whitney, who is in charge of the California State Survey. The specimen resembles, in its con- dition of preservation, the Mauvaises Terres fossils of White River, Nebraska. The formula of dentition is the same as in the Indian Rhinoceros, and the proportionate size of the teeth was the same. It was about the size of R. oc- cidentalism or perhaps a trifling degree larger, but its lateral incisors were triple the size. The estimated length of the jaw is about 16 inches. The space occupied by the molar series is 8 inches. Regarding the specimen as indicating a species distinct from any of the preceding, the name of Rhinoceros hesperius was proposed for it. September 2Qth. The President. Dr. Bridges, in the Chair. Thirty-two members present. On report of the respective Committees, the following papers were ordered to be published : On a New Generic Type of SHARKS. BY THEODORE GILL. In the year 1858 the Smithsonian Institution received, from Capt. Stone, the jaws and vertebrae of an enormous species of shark existing in the Gulf of California and known to the inhabitants of the neighboring regions as the " Tiburon ballenas," or " whale shark." The specimen represented by the spoils was said to have been "twenty feet long," with a " head six feet wide," " pectorals three feet long " and " flukes six feet between tips.'' " The back from the head to first dorsal fin, brown with reddish spots." The head is re- presented as truncated in front. The dried dentigerous band of the upper jaw is slightly curved forwards, about nineteen inches between the extremities, and somewhat more than an inch in width in front. The teeth are fixed and extremely minute, the largest being little more than a line in length, and decrease towards the ends of the jaw ; they are disposed in regularly transverse rows, of which there are over one hundred and sixty (164 — 167) on each side, while in front there are from thirteen to sixteen in each transverse row ; each tooth is recurved back- wards and acutely pointed, swollen and with a heel-like projection in front rising from its base. This type will be seen, therefore, to be very distinct, but is evidently re- lated to the South African genus Rhinodon, and must be referred to the family of Rhinodontidee with the name of Micristodus punctatus. On two species of DELPHINIDiE, from California, in the Smithsonian Institution. BY THEODORE GILL. While examining the species of Cetaceans, represented by skulls and skins, in the Smithsonian Institution, I discovered two species of Delphiuidse sup- posed to have been hitherto undescribed. Brief descriptions of these are now submitted ; at another time, it is proposed to give more extended descriptions as well as figures. Lagenorhynchus obliqoidens, Gill. The skull in its generic characters agrees with that of L. leucopleurus, the 1865.] 178 PROCEEDINGS OP THE ACADEMY OP type of the genus. The beak is rather robust, its greatest width being con- tained about three times and a half in the length of the skull ; thence it de- creases gradually forwards, the lateral contour .describing a sigmoid outline, while the surface above towards the end is moderately and quite regularly arched from side to side, no groove separating the intermaxillaries and supra- maxillaries. The triangular or deltoid area, in front of the nostrils, is nearly plane but elevated, and its surface corrugated ; it gradually ascends back- wards to the posterior angles of the intermaxillaries, while forwards it is in- curved, and continued as a narrow internal margin of the maxilliaries, almost to the anterior fourth of the beak ; its greatest width is less than half the width of the cranium. The interspace between the intermaxillaries is wide, and scarcely contracted at the middle. The supraoccipital projects forwards, and its point almost or quite touches the nasals. The temporal fossae project far backwards. The lower jaw is nearly uniformly high for the posterior fourth of its length, and at its symphisis is again enlarged and deeper. The teeth are elongated, boldly curved, in the upper jaw about thirty-two in number ; all are directed obliquely forwards and outwards ; the distance between the last and the posterior notch of the supramaxillary equalling the width of the bone ; in the lower jaw there are about thirty or thirty-one teeth on each side, directed somewhat outwards, and the posterior one also slightly backwards. Three skulls of adults of this species, obtained at San Francisco, California, are in the Smithsonian collection. They indicate a species different from any that lias yet been intelligibly described. I refer it to Larjenorhynchus, as con- tradistinguished from De.lphinus by its flat palate, destitute of lateral grooves ; the differences between skulls of this genus and Cephalorhynchus are not evi- dent from the published accounts. Phocaena vomerina, Gill. The skull is very similar to that of P. communis, and the proportions gene- rally differ little or none, but it is at once distinguished by the development of the vomerine bone, which is more developed and recurrent backwards, ex- panding below into a more or less enlarged horizontal process behind the palatines. The teeth appear also to be more numerous ; in the upper jaw, on each side, there are about thirty-nine or forty teeth, disposed in two divaricating series, in the front of which are about eighteen, and in the pos- terior eleven. In other respects no decided specific differences seem to exist. This species is represented in the collection of the Smithsonian Institution by the much injured skull of an animal obtained by Dr. Kennerly at Puget's Sound, and by the skin and skull of a younger animal, procured at San Fran- cisco by Dr. William Stimpson as naturalist of the North Pacific Exploring Expedition. Note on a Species of HUNCHBACK WHALE. BY PROF. E. D. COPE. The author has had an opportunity of studying the skeleton of a hunch- backed whale of our coast, preserved in the museum at Niagara Falls, in Canada. A label on the specimen explained that the animal was found dead at'sea, forty miles from Petit Menan lighthouse, off the coast of Maine, and was towed to shore by a Capt. Taylor. It was carefully cleaned, and appeared to be perfect, except in the lack of the sternal, pelvic, and periotic elements. Its length, when fresh, was fifty feet. It presents all the characters of the genus Megaptera, Gray, especially of the northern species, including the lack of coracoid process, and presence of a small coronoid process of the mandible. Its subordinate characters differ [Sept NATURAL SCIENCES OF PHILADELPHIA. 179 from those of the M. longimana and gig as, the known north Atlantic species, as figured and described by Rudolphi and Gray. The transverse pro- cess of the atlas is directed obliquely upward, truncate, deeper than long, measuring half the depth of the articular face, its upper origin above the lat- ter, and at the base of the neural arch. A rounded process, bearing the pos- terior articular surface, projects into the upper part of the spinal canal. Of the transverse processes of the axis, the superior is longer ; the canal is not depressed, a little over half the diameter of the centrum. The superior transverse processes increase in length to the fifth cervical, where they are straight and slightly descending ; those of the sixth and seventh are well developed. The last is the only one without inferior process ; the others are well developed ; that of the fifth, three-fifths the diameter of the centrum, and slightly angulated near the middle. Total number of vertebra?, 48, all free; the neural spine is first smaller than the zygapophysis on the fortieth. The neural arches and spines are remarkably elevated on the dorsal and lumbar regions, somewhat as in the Catodontidae : e. g., in the 33d vertebrae, the ver- tical diameter of the centrum is 9.75 inches, and the height of the arch and spine, 17.87 inches, or nearly double ; the position of the zygapophysis measures half the elevation. The caudal series is short, and though a few vertebrae have pos- sibly been lost, the series appears as though complete ; there are attachments for eight chevron bones. There are fourteen pairs of ribs, of which the anterior are simple-headed, and flattened distally ; the first is especially dilated, double the width of the median, and presents a process on its pos- terior edge near the extremity. This is present on the two following, being successively nearer the extremity in each. Those of the last pair are slender, and longer than iu Balaena, exceeding the second pair. The length of the humerus and remainder of the fore limb is 9.05 feet, equal the length of the cranium ; they supported a fluke equal in life to one-fifth the total length. The breadth of the cranium measured below, from tip to tip of the orbital processes of the frontal, 6.41 feet, or to the length as 8 to 11 ; in Rudolphrs figure of the longimana, the proportions are as 8 to 14. Breadth between coronoids of mandible, 5.75 feet. The ulna is much curved, and with two proximal heads. Scapula, height, 29.6 inches; breadth, 44.4 inches. This specimen differs from those described by Gray * and Rudolphi, f in the long inferior lateral processes of the posterior cervical vertebrae ; in the former, they are said to exist on the anterior only. W. P. Flower, however, in a valuable paperj on cetacean skeletons, describes two specimens, one in the museum at Louvain, and the other at Brussels, which exhibit these processes as far as the sixth and fifth vertebrae, respectively, but of diminished length. In the specimen under consideration, that of the fifth is as long as that of the second. The parallelopiped form and elevated position of the transverse processes, and the internal process of the atlas, are not represented in Dr. Gray's figures. The cranium is broader, in proportion to its length, than represented by Rudolphi, and shorter in proportion to the total, than in the measurements of Flower and Moore : in these it is one-fourth, or more ; in the Maine speci- men, one-fifth, or less. The fins are, also, relatively shorter, measuring one- fifth of the length, instead of one-third. A most striking peculiarity of the species is the great elevation of the arches and spinous processes of the dorsal, and especially the lumbar verte- brae, reminding one of the structure in the toothed whales. The outline of the skeleton is thus somewhat humped behind, presenting a contrast to that represented by Rudolphi in the type specimen of the longimana, where the elevation of the arches and spines does not exceed the diameter of the cen- trum, on the lumbar region at least : on the 33d vertebra, the zygapophysis * Proc. Zool. Soc. Lond., 1864, 208. t Mem. Acad. Berlin, 1829, 13:. 1 Pr. Z. S. Lond., 1864, 416-18. 1865.] 180 PROCEEDINGS OF THE ACADEMY OF measures one-third this height. The length of the diapophyses is considerable, and similar in both. Rudolphi represents eleven chevron bones, and the anterior ribs are not flattened, or furnished with an inner process in his figure. In the M. gigas, the spinal canal is relatively larger, and the cervical superior and inferior transverse processes of one side are more symmetrical and similar. An American fin-backed whale has been named Megaptera americana, from a very brief and indefinite description in the Philosophical Transactions, I. p. 11. A species named on such a basis can never be recognized; but, if we must accept it, the only character given, the relative lengths of the body and fin, are entirely at variance with those of the present species : the length of the latter is said to be one-third of the total. Supposing the reduced number of vertebra? and chevron bones to be the result of accident, and the form of the anterior ribs to have been unnoticed by Rudolphi, the shorter head and fins, the peculiarly high neural spines and peculiarities of some of the cervical vertebrae, would seem to distinguish this specifically from the 1 o n g i m a n a, if, as is most probable from the recent researches of Gray, such characters are invariable in the species of Cetaceans. On such premises this animal may be called Megaptera os phy ia. A species of this genus has left its remains in the miocene of Eastern Vir- ginia, judging from periotic and other bones sent me by my friend Edw. Hol- way, of Yorktown. Probably it is one of the species described by Leidy, Proc. Acad., 1851, 308. A pair of bullae without their other periotic elements has been sent me from the Museum, Salem, Mass., by Frederick W. Putnam, Secretary of the Essex Institute. They-,were presented to the Museum by Capt. J. W. Clever, and are said to have belonged to a hunchbacked whale. Their locality is unknown. The transverse section represents a cylinder. Taking the bulla of the left side, the incurved lip of the interior face (position derived from the figures of Balaena australis in Ossemens Fossiles) forming no angle with the inferior aspect : this lip rolls regularly inward without compression or fold ; with its laminae the smooth surface terminates, all the remaining surface of the bulla being closely rugose. Viewed from above, the anterior extremity is more contracted than the posterior, and the outer face presents three inflations, while the inner is medially straight. Of the superoexterior inflations, the middle is prolonged into the usual superior process, which is much recurved, and constricts mode- rately the great fissure at two-fifths its length from its posterior extremity ; it is separated by a deep fissure from the posterior inflation. The main fissure is in one plane, and is expanded into both lips anteriorly. The portion sup- porting the other periotic elements postero-interiorly stands on a strong pedicel. Greatest length, 4 in. 5 1. ; breadth at middle inflations, 2 in. 8'4 1. Huxley's figure of the periotic bones of Balaena australis (Elem. Corn- par. Anat. 273) represents the longer process as Cuvier, longer and not so acuminate as in our specimens of the B. cisarctica, but the shorter process as much shorter than in the former figure, and more as in our specimens. A pair of earbones of one individual from the Museum Salem, differ con- siderably from those of three individuals of the B. c i s a r c t i c a in the Academy collection of nearly the same size. In them an arched ridge descends from the upper elongate lip process, on its inner side, and, describing a curve, rises to the pedestal of the longer periotic process. In the cisarctica the ridge is inconspicuous, and includes but a groove between it and the labial border, while in the Salem specimen it is very strong, and, descending farther, in- cludes a pocket with the lip border. In the latter there is a broad smooth rim on the rising outer lip margin of the other end ; in the cisarctica none at all. Viewed from below, the end next the long processes is broader and more nearly truncate, owing to the strong development of the exterior inflation [Sept. NATURAL SCIENCES OP PHILADELPHIA. 181 of that end into a strong solid basal angle, and the expansion of the inner basal outline. The angle formed by the meeting of the inner and nnder faces of the bulla is more acute, from the greater flattening of the former. These differ as much from Balsena mysticetus angulata,* Gray. The long section of the opening is narrower, and the short portion shorter ; the external basal angle opposite this portion, as well as the "pocket, is not represented in Gray's figure. The former feature, with the greater prominence of the long external inflations at the other end, gives a very different inferior view, from the greater breadth, etc. The characteristic angle of Dr. Gray's figure is also wanting in the Salem species or variety. Another bulla from Mus. Salem (No. 113) is narrower on the inferior view than even the cisarctica, and the outer lip of the opening is considerably higher. The inner inferior outline below the long process is very obliquely truncate, and the outer prominence near it is directed more outward. The inner or thick lip is not heavy, and is much plicate. The inner inferior com- pressed margin is much less flattened than the other Salem variety, (111 — 112.) Locality unknown. October 3d. Mr. Cassin, Vice-President, in the Chair. Fifteen members preserjt. Dr. Leidy observed that the fine specimen of Cryolite, presented this evening by Edmund A. Souder, Esq., was from Ivigtut, Aiksuk Fiord, Greenland, and was a sample from a ship load, one of a number of similar loads imported to this place for the manufacture of soda alum. Prof. Carson stated that he recently had an opportunity of ascertaining the plants from which the so-called American Tea is made. The variety called Green Tea is the product of the Ctanolhus Amtricanus ; the Black Tea, the pro- duct of the Lysimachia quadrifolia. The death of Dr. Francis M. Moore, member of the Academy, was announced. October 10th. The President, Dr. Bridges, in the Chair. Twenty-four members present. Dr. Leidy made some remarks in relation to the specimens of oolitic phos- phates of lime and alumina, from the Island of Navassa, W. I., presented this evening. The material, he stated, was imported in large quantities to this place, by Messrs. Potts and Klett, and was employed in the manufacture of a fertilizer. The mineral presents several varieties of color, but is especially remarkable for its constitution, resembling that of ordinary oolite. Dr. L. sup- posed that it was probably of organic origin, though the reverse opinion was held by persons of judgment. Dr. Leidy further called the attention of the members to a collection of bones and stone implements, presented this evening by Mr. Frederick Klett. The remains were obtained from the Island of Orchilla, W. I., from a deposit of guano, eight inches below the surface. The bones are parts of three human * Proc. ZjoI. Soc. 1S64, 201. 1865.] 182 PROCEEDINGS OF THE ACADEMY OF skeletons, together with a few fragments of bird and turtle bones. They are all very friable and appear much eroded on the surface. The human bones are all of mature age, and rather small. Most of them are portions of two skeletons, apparently a male and female ; a few belonged to a third skeleton, apparently male. Of portions of three skulls, the most perfect is the greater part of a small- cranium, judging from its size, that of a female. The base in advance of the occipital bone is broken away. The cranium is of the brachycephalic type and bears a near resemblance to that of the ancient Peruvian pattern. It is rounded or ovoidal, with a high compressed occipital region, with a quadrate outline viewed posteriorly, and an ovoidal outline viewed above and laterally. The forehead recedes in a gentle curve from the supra-orbital margins, and the supra-ciliary ridges are feebly developed. The greatest height of the cranium is on a line with the anterior glenoid tubercle and the centre of the sagittal suture. The biparietal diameter is 64 lines; the antero-posterior, from the glabella to the occipital protuberance, 76 lines ; and the height from the anterior margin of the occipital foramen to the centre of the sagittal suture 64 lines. The breadth of the forehead at its narrowest part, just above the external angular processes of the frontal bone, is 44 lines ; the height of the latter bone from the root of the nose to its summit is 49 lines. Fragments of the other skulls indicate a larger size but the same form, except larger superciliary ridges. A fragment of the face of one of them ex- hibits the cheek bones prominent anteriorly, and the orbital and nasal orifices large. The jaws are of moderate proportions and orthognathous. The teeth of all three skulls are of the ordinary 'forms. Those of two of the skulls are much worn. In one of the skulls some of the teeth had been lost during life, and the alveoli obliterated. In a lower jaw containing an entire series of teeth but little worn, the back two molars on one side present on the top of the crown a small cavity, probably the result of caries. The remaining human bones consist of a few vertebra? with fragments of others, fragments of two scapulae and innominata, a number of long bones of the extremities, and a few small bones of the feet. The collection contains four humeri belonging to three skeletons. Two from one of the larger skeletons measure 12 inches in length from the summit of the head to the edge of the inner articular condyle, and 2 inches 10 lines in cir- cumference, just below the deltoid insertion. A third humerus, apparently from the same skeleton as the more perfect cranium before indicated, is of more delicate form, II J inches in length, and 2 inches 8 lines in circumference at the middle of the shaft. The fourth specimen, intermediate in proportions to the others, has lost the head, and is peculiar from the very prominent sharp angular character of the shaft internally. All the humeri present a small in- tercommunication between the fossse above the ulnar trochlea. The bones of both fore-arms of a larger and smaller skeleton exhibit the following measurements : larger ulna 1 0£ inches long ; smaller one 9h inches : larger radius 9} inches long; smaller one 8 inches 8 lines long. Of two femora from a larger and a smaller skeleton, both without the head and condyles, one has measured about 17 inches in length, the other about 16J inches. They are more bowed anteriorly than is usual, and both present a greater degree of prominence of the linea aspera. Four tibia?, without the head, belong to the same skeletons as the femora. The larger, when perfect, measured about 13£ inches long from the front of the head to the end of the inner malleolus; the smaller 13 inches. The former present nothing peculiar, but the latter are remarkable for their laterally com- pressed character; the antero-posterior diameter nf the middle of the shaft or the breadth of the internal surface being 16 lines, while the transverse diame- ter is but 9 lines. The stone implements found with the bones are six stone axes, of compressed conical form, with a sharp trenchant basal border and a pointed apex. [Oct. NATURAL SCIENCES OF PHILADELPHIA. 183 Prof. Gill offered a communication on a new generic type of the family 7a- piridce, of which two skulls, representing adult and very young individuals, are contained in the Museum of the Smithsonian Institution. The former in- dicates that the species attains a size superior even to that of Tapirns ameri- canus, and that it is consequently much larger than the Tapir of Roulin. Both skulls were obtained, by Dr. W. S. White, on the Isthmus of Panama. The outline of the skull resembles that of the Pinchaque, (T. Roulinii, Fischer, 1829, = T. villosus, Wagner, = T. andicola, Gloger, 1842, = T. pinchaque, Goudot,) but the new type is distinguished at once by the peculiar develop- ment of the supramaxillaries, which are swollen above and in front of the infraorbital foramina, and thence extend upwards and backwards into a squamous portion which embraces with its fellow a thick, bony, nasal sep- tum continuous with the vomer, and which is elevated to a line with the forehead, and has a widened upper edge, which still further enlarges behind and embraces the nasal bones. The grooves for the muscles of the proboscis are in front straight, entirely confined to the frontals, and do not encroach on the supramaxillaries ; while behind they describe a spiral curve around a pit between the nasals and frontals. Other peculiar characters exist and will be hereafter illustrated. The species may be named Elasmognathus Bairdii. Mr. Glenn, of the Museum of Comparative Anatomy and Zoology of Cambridge, exhibited to the Academy various beautiful microscopic preparations made by him. October \lth. The President, Dr. Bridges, in the Chair. Twenty- two members present. The following papers were offered for publication : " Observations on American Fossils, with descriptions of new spe- cies." By T. A. Conrad. " Third Contribution to the Herpetol >gy of Tropical America," and "A Contribution to the knowledge of the Delphinidce." By Prof. E. D. Cope. October 24th. The President, Dr. Bridges, in the Chair. Eighteen members present. The following papers were offered for publication : " On species of Galeruca and allied genera," and " Prodromus of the Anobiini inhabiting North America." By Dr. John L. LeConte. " Notes of a study of the family Icteridae." By John Cassin. October 31st. The President, Dr. Bridges, in the Chair. Seventeen members present. The resignation of Dr. Band as Recording Secretary was accepted, and Dr. H. C. Wood, Jr.. was unanimously elected. 1865.] 184 PKOCEEDINGS OP THE ACADEMY OP On report of the respective Committees, the following papers were ordered to be published : Observations on American FOSSILS, with descriptions of two new species. BY T. A. CONRAD. Prof. Cook, of New Brunswick, N. J., has lately received a few fossils from Ocala, Florida, which prove the limestone of that locality to be of the same age as the Shark River marl of New Jersey. The species consist of Globulus alveatus, Con., Venericardia prima, Con., Dosiniopsis alta, Con. These are all Eocene species of California, Maryland and New Jersey. In this rock no doubt occurs Carcharodon angustidens, Agass., of which I obtained a specimen at Tampa Bay, Florida. Among Prof. Cook's fossils are a few species from Jasper Co.. Miss. The rock of this county, in which the fossils occur, is stated by Hilgard to be of the Jackson Group, (Upper Eocene.) The species are Ostrea Tuomeyi, Con., Mor- tonia turgida, Con., Pecten Poulsoni, Morton, P. perplanvs, Morton, Carcharodon angustidens, Agass., Orbitolitcs Mantelli, Morton. The former of these I sup- pose to be the shell which Tuomey found so common in the Basilosaurus lime- stone of Alabama, and which he referred to Pycnodonla vesicularis (Gryphsca mutabilis, Morton.) It is very different, however, and may be distinguished by the following characters : Ostrea Tuomeyi. — Ovate, sublobate, lower valve deep, umbo narrow, rough and unequal in surface, with rough lines of growth; not distinctly plicate ; upper valve convex above, slightly convex below ; with a rough and unequal surface; concentric lamination very prominent, when weathered. It differs from P. vesicularis especially in wanting the inner plications about the upper submargins of the interior, and the umbo is much narrower ; it is also a true Ostrea, whilst the vesicularis is the type of the genus Pycnodonta, Fischer, and characterizes the cretaceous era. Echinodermata. MORTONIA, Desor. Mortonia turgida. — Suboval or subpentagonal, swelling medially, with a convex outline ; thin on the submarginal portion of the disc ; ambulacra ellip- tical. Allied to M. Rogersi, but larger, thinner round the central prominence, more elevated medially, the depression about the mouth greater, and the anus smaller. It bears about the same relation to Rogersi as Sismendia alta, Con., bears to S. Lyelli, Con. Testacea. LIODERMA, Conrad. Volutilithes lioderma. — This shell has not the characters of Volutililhes, but is covered entirely by enamel, has very oblique columnellar folds, and an, outer lip somewhat ernarginate on the upper part to its juncture with the body whorl ; base deeply emarginate. I have not met with this genus in any American Eocene bed. SOLENA, Browne. Subgenus Leptosolen, Conrad. Solena BiPUCATA (siliquaria) Con. — Cretaceous. [Oct. NATURAL SCIENCES OF PHILADELPHIA. 185 Third contribution to the HERPETOLOGY of Tropical America. BY E. D. COPE. Alligator h el o i s. Muzzle 6| inches from end to lines connecting orbits, 5| inches wide near the middle. Two keels behind and between the eyes, diverging posteriorly, a short and nearly transverse keel in front of the eyes. Upper eye-lid divided by grooves into three areas ; an elevated keel, above each ear opening. Two oblique rows of elevated horn-like shields^n each side of the neck, of rather small size, four on the inner, three on the outer rows ; the third of the inner and second of the outer form, with two large elevated median plates, a trans- verse row. Four very high, short, keel-like postcervicals. Eight rows of dorsal shields, excepting anteriorly where there are six in the first cross-row. and four in the two succeeding ; all are like heads of spikes keeled. Four rows on the tail at its middle. Lateral caudal shields continuous, abrttptly elevated. like the dorsals, subquadrate. Sides with small rounded scales ; width between dorsals and ventrals equal to length of third dorsal cross series. A large row of plates on the inner side of the fore arm. Claws long ; no pal- mar webs. Abdominal rows eleven, each plate with a thin ossification ; two or three large plates in the thoracic cross-row. End of tail little serrate above, scarcely compressed. From end of muzzle to occipital 12 inches ; to between femora 32 inches ; from latter point to end of tail 50 inches ; total 7 feet 10 inches. Color dark brown with vertical yellow bars on the sides and tail, the former very irregular. Chin, throat, under and upper lips yellow, without spots. This rugged looking species belongs to the genus Alligator, as restricted by Gray, in which the prolongation of the nasal bones separates the external nares, and there is no cross ridge between the orbits. It approaches Jacare in that an external portion of this cross-ridge exists on each side. The hab- itat is not known, as the single specimen I have seen is preserved without label in the Museum of the University of Munich. Through the courtesy of Prof. C. Von Siebold, I was enabled to make the above description. I may mention here that the crocodile described by me (Proc. Acad. 1860, 550) as Mecistops bathyrhynchus, is the species identified by Dr. Gray (Catal. Brit. Mus.) with the C. intermedins Graves; with the limited pub- lished material as a basis, I have reached a different conclusion. Chelopus punctularius, Emys punctularia Daud., E. scabra Bell, Gray, Linnaeus (fide Agass. At first sight, the female of this animal gives the impression of a Testudinid form, with separate caudal plates, but an examination of the phalanges shows their number to be that in the Emydidae, two for the longest digits, (exclusive of ungueal,) instead of but one remaining upon the extinction of the proximal, as in the former. The proximal phalanx is articulated somewhat, as in Cistudo, but is shorter, and nearly excluded from a serial connection ; its proximal glenoid cavity is superior, and near the distal condyle. The inferior projec- tion of the proximal end gives the foot its angulated outline. The structure is not unlike that in Chelopus muhlenbergii, and there are really more pha- langes than in Cistudo, where the foot is longer ; the external digit behind having two internal phalanges instead of but one. In similar manner the re- duction of the penultimate phalanx in the parallel Sternothaerus, prepares us for its absence in Pelomedusa*, the extreme of the Pleurodera in this direc- tion, and representative of the Testudinidae. Podocnemys and Peltocephalus imitate the Cheloniidae in their overarched temporal fossae, as observed by Wagler, while intermediate forms are more or less similar to some Emydidae. After a consideration of various osteological peculiarities, I incline to differ •Which has not, I believe, been previously noticed. 1865.] 186 PROCEEDINGS OF THE ACADEMY OF from Agassiz, who mingles these types with those of Amydse, and to regard the Testudinata as primarily divisible into three orders or suborders, Chelo- nii, Amydse and Pleurodira.* The name Chelopus Rafinesque has been recalled by Leconte, as identical with Calcmys, Ag., to which Nanemys, Ag., must probably be united, and which have been previously named Geoclemmys, by Gray. The present spe- cies is in any case congeneric with G. annulata, Gray, which is of terres- trial habit. Pectoral plates normal, broad, sternum notched behind. Feet very short, clubbed, quite as in the Testudhfidse, digits flattened above* last phalanges only distinct, not webbed ; claws short, obtuse. Head very small, covered with a smooth skin, without sub-divisions. Eyes lateral, with a transverse depression between them ; muzzle short, nearly vertical, swollen above, nos- trils anterior. Alveolar plate narrow, without median ridge, cutting edge smooth, neither notched, hooked nor toothed at the symphysis. Mandible broad. A strong zygomatic arch. In a 9 specimen the dorsal region is elevated with a trace of a broad keel, as in Cistudo, and the sides are steep. The outline is parallelogrammic, rounded at the extremities. Posterior slope regularly oblique. Margin no- where reflexed, posteriorly weakly serrate. Twenty-five subquadrate margi- nals, the nuchal broad behind. Vertebrals, the four anterior of equal breadth, the anterior pentagonal, the remainder hexagonal. All the plates concentri- cally sulcate, with a slightly rugose areola. Inguinals very small ; sterno- costal bridge very broad. Lobes of sternum short, free outlines, subquinque- lateral. Large scales all round the forearm and foot, (seven rows anteriorly, two rows of three each behind,) on the sole and heel only of the hind foot. Above dark brown ; sternum black, bordered with yellow ; remaining under surfaces yellow ; forelegs with a black stripe on ou'er edge. Top of head black ; a narrow red band from behind and above the eye to the middle of the neck, above and below which are black lines on a yellowish ground ; neck below immaculate. This species is more elongate than C. annulatus; anal and gular plates larger; color of head and extremities different. It is nearer the C. areola- tus,f A. Dum., but is even more testudiniform. The latter is less elevated, the hind feet a little webbed ; the carapace more elongate and narrowed ante- riorly ; the artist has given six vertebral shields ; the anterior lobe of the plas- tron is considerably shorter. One 9 specimen in the Smithsonian Museum, obtained in Yucatan by Arthur Schott, naturalist to the Scientific Exploration of that country. In a female from Tabasco the frontal depression is less marked and the muzzle not quite so rounded. In a male from the same locality the muzzle is elongate and the vertex and front fiat. This is evidently the E. scabra fi- gured by Bell, agreeing with it in the superior position of the head bands, etc., thus differing from the allied dorsalis Gray, Spix. The carapace differs from that of the Yucatan female in sexual characters, as the revolution of the margins, but has a very small nuchal shield, and the first vertebral prolonged between the marginals, while the former exhibits a short broad shield. This is the only difference which cannot be regarded as sexual. This, with the following seven species of Tortoises below enumerated, was presented to the Smithsonian Institution by Dr. Berendt, who, during a resi- dence at Tabasco, Mexico, devoted much attention to the natural products and features of the country. He has furnished me with the following notes on the Testudinata. The specimens are complete and of adult age. The Chelopus punctularius is the Mojina of the natives of Tabasco. " Mojina is often found tame in the houses, and attaches itself very much to men. The very same specimen which I brought living with me, and left * Vid. Proc. Acad. Phil., 18C4, 181. t Suspectod by Agassiz to be thn Malacoelemuiys palustrisof North America. [Oct. NATURAL SCIENCES OF PHILADELPHIA. 187 with Prof. Baird, I got from an Indian woman, living in a hut on the Tabas- quillo River. I asked for turtles, when she said she had one, but it was in the woods behind the house. She went to the door and called, 'Mohina, Mohina !' and the turtle came out of the bushes to the house, and was sold to me. I could never induce her to eat any thing for more than three months, until I gave her, in Washington, some cherries, which she tried, and after- warcfe commenced to eat. It was told me that the Mojina eats animal food (?)" Ptychemys o r n a t a, Aga ss. et Bell. " Hicotea " of the natives. Dermatemys mavei, Gray. " Emys berardi, Dum." Two specimens, eighteen inches long, of this remarkable species, agreeing with Gray's figure, except in the single gular plate, and presence of a minute gemmiform intergular plate, as in some Hydraspididae. This is the first in- stance of the kind among the Emydidse, of which family this species presents every character. Called Tortuga blanca. " Hicotea and Tortuga live ou vegetable food, leaves, grass, and, principally, the fruits of Tobillo (Spondias mombin) and Amate (a Ficus.) At the time the amate is ripe, the tortugas are caught easily, and in numbers, under these trees. They distingui? h in Tabasco three kinds of Tortuga : T. blanca, or del rio, (white or river turtle ;) T. negra, or de popal, (black or swamp turtle,) perhaps the same ; and T. de Chilapa, (a village,) or de Chichicaste, (a very bitter Euphorbiacse, ) which I have not seen. It is not eaten, as the former two are ; the flesh is bitter and of a bug smell ; their form is said to be not elliptic, but nearly round. It is believed that they feed on chichicaste. (Chichic is Mexican, and means bitter.)" Prof. Poey has sent me from Cuba some living specimens of the Ptychemys decussata, (Emys rugosa, Sagra, and Trachemys rugosa, Agass. = 9 fide Poey,) whose habits contrast with those of the P. ornata and Dermatemys. They devour flesh eagerly, but reject bread and vegetables, unless soaked with fresh gravy, and dislike apples, the only fruit offered them, Chelydra sp. Called Chiquihuau. This variety is well marked, but that it will eventually be found to be a different species seems very doubtful. In the single individual at my disposal, the only peculiarity observable in the shell is the broader and shorter poste- rior sternal lobe, which scarcely measures three-quarters the anterior, and has not the gradual acumination of the ordinary variety. The axillary plates are- only distinguishable upon close examination, owing to the obsolescence of the sutures. The lateral processes of.the pubis are more than double the length of the median ; in a specimen of the northern variety, the former are only a little longer than the latter. The skin of the occiput and neck, instead of being tuberculate, is furnished with numerous flexible dermal appendages, and one side or angle of the warts on other regions of the skin is free. The large scales of the row on the outside of the antebracliium are larger and almost entirely free, forming a broad serrate dermal border. The caudal crest is not so elevated as in the common form, but one large process being higher than long. The color of all the under surfaces is very light. Claudius a n g u s t a t u s, sp. nov. Character gencricus. A single row of marginal plates. Plastron small, cru- ciform, solid; hyo- and hyposternal bones connate, forming an exceedingly slender bridge, which connects the plastron with the carapace, and is not cov- ered by a corneous axillary plate, but by thin epidermis. No inguinal or gular plates ; anals united. Carapace completely ossified, extending much beyond plastron anteriorly and posteriorly, elevated and narrowed in front, neither dilated nor steeply descending behind; vertebral line nearly plane. Verte- bral neural segments eight, the last pair of costals meeting on the median line, but separated from the small posterior marginal by a large penultimate 1865-] 188 PROCEEDINGS OP THE ACADEMY OP shield. Anterior in contact with a very large anterior marginal, making to- gether eleven vertebrals in an interrupted series. ' This interesting genus is nearest to Chelydra, though widely different ; its general appearance and interrupted vertebral series approximate it to the Cino- sternidse, especially Aroniochelys and Staurotypus s a 1 v i n i i,* Gray. Indeed it only differs from the latter species in the immobility of the anterior lobe of the sternum, and absence of inguinal and axillary plates, as well $s the presence of the mesosternal bone, if the latter belong truly to the Cinosterni- dsef. Claudius must be placed on the confines of the Emydidse in this direc- tion, as Chelopus marks the extreme in the other. Character specijicus. — Marginal scales all very narrow, especially anteriorly; four lateral grooved ; nuchal very small, transverse. Anterior vertebral longest, broad as long, posteriorly rounded, acuminate, in contact with second marginal. Third and fourth vertebrals broader than long ; last narrowed above. Anterior costal li the length of the third. Epidermoid layer rather thin, concentrically ridged anteriorly and externally on the plates ; a median and lateral keel on each side, all quite weak. Sternum rounded in front, acute behind, equal portions before and behind the abdomino preanal suture. Abdominal three- fifths of pectoro-gular plate. Above blackish brown, the plates paler medially, below yellow, unspotted. The head is disproportionately large, and of an elongate form, with narrow postorbital arches ; baove plane, covered with a soft skin, except an oval plate of horn on the top of the nose. Maxillary sheath hooked in front, and with a sharp tooth below the anterior margin of each orbit ; edges sharp. Mandible with a remarkably long symphyseal hook, which is received into a correspondingly deep premaxillary pit. A pair of barbels ; skin of neck with- out warts or appendages. Toes and claws rather slender, very fully webbed ; tbe forearm with three anterior curved corneous ridges, and the heel with four series. Tail (of 9 ) very short, without terminal claw, and with a double dorsal row of skin warts. Color blackish plumbeous, the inferior surfaces paler. Called Talmame by the natives. Museum Smithsonian, 6518. " Talmame lives in swamps, and digs itself in to a depth of two and three feet ; eats small fish, crustaceans, snails, etc. Animal food I have found also in the stomach of Chiquihuau, (entire ampullarias,) Huau and Pochitoque." ritaurotypus triporcatus, Wagl. Called by the natives Huau. Travellers relate that the alligator is often killed by a turtle, which he swallows alive, and which devours the intestines to get out. Heller (Reisen iu Mexico, p. 313) says that he has seen a living turtle " of the genus Cynixis" within a fresh-killed alligator. Waldeck, whose imaginatory power exceeds far his observatory, says (in Voyage pittoresque) that he has found in every killed alligator's stomach a living " Ticotea or potohitoque, which is the same known in Egypt, (thirse,) and also the Testudo triunguis of Torskal." (!) I have it from a number of different and reliable persons that they have witnessed the fact ; either found a living Huau in the body of a dead alligator, who was supposed to have run on shore and died, or even seen the Huau just breaking out of the dead body of the alligator ; but never any other kind of turtles ; only the Huau. Huau has two very distinct voices ; one imitated in the name, a strong expiration in the given vowels, not intoned with the larynx, but only with the fauces and mouth, — and a squeak, like that of dry carriage wheels or of a large door. The first seems an expression of anger, when teased ; the second perhaps a call, as I heard them often when at night ; once alone in a corner of my house ; never when male and female were near each other. * Proe. Zool. Sob., Lond., 18t 4, 127. fVid. Le Conto's system, Pr. A. N. S., 1854, 1S2. ["Oct. NATURAL SCIENCES OP PHILADELPHIA. 189 Mohina has a soft, melancholy piping, which is rather touching when they are killed." Cinosternum leucostoniuui, Dume'ril. Arch, du Mus. 18, p. The number of specimens of this species would indicate it to be the most abundant. Called Pochitoque camatotl. The Mus. Smithsonian possesses also a specimen from Turbo, in New Grenada, from the Michler Surveying Expe- dition. Cinosternum b e r e n d t i a n u m, sp. nov. Most nearly allied to the preceding, agreeing with it in the contracted rounded outline of the posterior lobe of the sternum, which fits the carapace accurately, and is without emargination, in the large size of the caudal mar- ginals, and the absence of lateral dorsal keels. , The carapace, though more or less keeled, is more depressed tlrm in 1 e u c o s t o m u m, the outline rising behind, and the fixed plastron has greater longitudinal breadth. leucostomum. berendtianum. Shorter than front, three- Middle plastron ; Longer than front, four- fifths of hind lobe. fifths of hind lobe. Rounded, without external Marginal bones ; Strongly angnlated. angle ; a groove near upper margin. First vertebral plate; Lanceolate rarely touch- Equilateral, bordering sec- ing second marginal, ond marginal. Gular plate ; Two-fifths longer than Long as remaining me- remaining median su- dian suture. ture. Broader. Last vertebral ; Narrower. The shell is a very dark brown above ; below, a dark brownish yellow, with reddish stains on the sutures, or over portions not touching the ground. Length of carapace, 3 in. 9 1. ; of plastron, 3 in. 6 1. ; breadth of carapace, 2 in. 6 1. Mus. Smithsonian, No. 6,517- Called in Tabasco, Pochitoque jaquactero and negro. " I have heard of a third Cinosternum in Tabasco called Pochitoque huau- gito, (the little huau, ) which is said to be smaller than the leucosternum, and lias the same three longitudinal keels as the Huau on the upper shell." Berendt. Probably the C. shavianum (mexicanum, Lee, fide Agass.) " Tortugas, Hicoteas, Mohinas and Pochitoques are generally eaten in Ta- basco. The Staurotypus is considered good enough for the Indians, who like it much, but it is despised by the whites. I had«it cooked, and found it better than the Derm itemys. The flesh is reddish when boiled. " I was told that, in Tabasco, Staurotypus and Dermatemys lay their eggs in, November and December ; Hicotea in February ; Pochitoque in March and April. " Staurotypus lays 10 to 30 eggs ; Dermatemys, 20 eggs ; Hicotea, 12 to 15 eggs ; the Mojina, Pochitoque and Talmame, only a few." On the etymological character of the native names, Dr. Berendt states as follows : — "In Tabasco come together three languages of entirely different families ; the principal language is the Chontal, closely related to the Tzendal (Chiapas) and belonging to the Maya family, — the Zoque to the South, and the Mexican to the West. We find, consequently, a great mixture of languages in names of natural objects ; besides those names introduced by the Spaniards, eithe.r from the Spanish or from the West Indian language, (Haiti, Cuba, ) and ap- plied to the same or similar things found on the continent " Huau is Maya. (' Uauu— unos (• cfef. No postorbital process. Tongue elongate, extensively free ; inferior palpebra reticulate with white fibres : vomerine teeth Agalychnis. Tongue short, attached or little free ; palpebra usually transparent; vomerine teeth Hyla. Tongue short ; palpebra transparent ; no vomerine teeth Hylella. Tongue extensively free ; dilatations minute, palmation extensive behind ; vomerine teeth Acris. yy. Brain case and ethmoid elongate, fontanelle narrow ; inner finger opposed to the others. Tongue slightly free Litoria. /?/?. Posterior digits free. Superior ethmoid plate osseous ; prefrontal bones sepa- rated Chorophilus. Superior ethmoid plate cartilaginous, the prefrontals developed, in contact medially Thoropa. Hyla gracilipes. Tonvue elongate, free one-third its length. Inferior palpebra not veined. * Type Hyla nurantiaca auctorum. t S d aulinia, sp. nov. This species I only know from a skeleton in the private anatomical museum of llyrtl, Professor of Anatomy in the University of Vienna. The head is a little broader than long; the interorbital width greater than from external nares to orbit ; vomerine teeth in short transverse series; general form similar to the Acrodytes venulosus. [Oct. NATURAL SCIENCES OF PHILADELPHIA. 195 Fingers elongate, free ; toes webbed at base only, remarkably elongate, tbe foot from tarsus a Utile longer than tbe tibia, and equal from axilla to middle of origin of femur, the width of head. Head flat, longer than broad, eyes little prominent, one-half tympanic disc ; canthus rostralis little concave. Body elongate, skin entirely smooth above : vomerine teeth in two almost connate fasciculi which present a convexity to each narial opening and pos- teriory where they are opposite the hind outline of the latter. Sacral diapophyses much dilated, presenting a prolongation posteriorly. Length of fore limb, 9 lines ; posterior limb, 24.4 lines ; from end of muz- zle to behind tympanum, 4.4 lines; muzzle to vent, 15 lines. Color above, bright leek green, with a brown band from the nostril through the tympanum to the middle of the side, white-bordered above ; and a short band on each side the ilium, white-bordered. Femora not spotted behind ; limbs not cross-banded. Upper lip with a brown border ; its green becoming yellow under the tympanum. Below whitish. Habitat. — Mexican table land, north-east of city of Mexico. A species near in technical characters to the ewingii, r.egilla, and squirella, but abundantly distinct from all, in its sacrum, feet, head, etc. Hyla stau fferi. Tongue rounded, a border only free ; a large gular vocal vesicle ; vomerine teeth in fasciculi between nares, which are a little larger than the choanse. Digits all short, with pallettes large ; the anterior free, the posterior short, the palmation measuring half the length of the longest digit. The heel extends to in front of orbit. Head plane, depressed, muzzle very prominent, rounded. .Outline from above elongate oval, canthus rostralis weak, straight, lores flat, oblique. Length of orbit equals frontal width. Skin of sides rugulose, otherwise smooth above ; no appendages. Mizzle to rictus oris, 4 lines ; anterior limb, 6.4 lines ; muzzle to vent, 11.7 lines ; posterior limb, 17.1 lines. Color above dark olive, with a short longitudinal black bar over each scapula, and one from eye to eye, with a trace along the coccyx. Below yellowish, deeper to brown on the extremities. Upper lip olive, sending a pale line to near axilla, sides minutely varied with dorsal and ventral tints. Habitat. — Orizava, Mexico. Obtained by Prof. T. Sumichrast. The species sent from Orizava by Prof. Sumichrast to the Smithsonian Institution are : — Spelerpes chiropterus. Geotriton carbonarius. Hyla baudinii. Hyla staufferi. Hyla mio tympanum. Hylodes conspicillatus. Bufo valliceps (nebulifer, Gird.) Ran a sp. Sceloporus. Sceloperus. Sceloporus. Anolis nanno lea. Corythaeolus cristatus (Thysanodacty- lus, Gray, Dracontura, Hallow.) Gerrhonotus gramineus. Diploglossus steindachneri. Oligosoma gemmingeri. Catostoma semidoliatum. Ninia collaris. Ninia diademata. Coniophanes fissidens ( Glaj hi rophis lateralis, Jan Elenco.) Spilotes poeeilonotus. Atropus uudulatus. Hemidactylium pacificum. This species is of some interest, inasmuch as our native species of this genus has hitherto been the only representative of its form. It differs from this in its uniform brown color above and below, and in some more important points. Vertebrse and costal folds between axilla and groin, seventeen, the latter not prolonged dorsally, as in the scutatum. Head oval, elongate, lip rounded, eyes large, prominent, longitudinal diameter longer than length of muzzle. Muzzle to humerus, half length from latter to groin. Tongue elongate oval ; 1865.] 196 PROCEEDINGS OF THE ACADEMY OP sphenoid teeth approaching near to the short oblique series of vomerines. Fore limb to orbit, hind limb scarcely longer, reaching the eight fold from behind. The inner digit on both extremities is so short, as to render the numbers almost 3-3. Tail elongate, slender subcylindrical. Gular fold represented by a line. Length of head to angle of mouth 2*5 lines. Breadth of head behind eyes 2 lines. Froni muzzle to humerus 5 lines. From muzzle to groin 16*5 lines. Length of tail 17 lines. Length of posterior limb 3-5. Hub. -Santa Barbara, on the coast of Southern California. Sent to the Smithsonian Institution by Dr. Hays. Spelerpes cephalicus. With the present addition to the Batrachian fauna of tropical America, it is appropriate to enumerate the salamanders so far known from this region. They are mostly natives of the mountainous sections, or of that elevated plateau which presents us with most of the northern forms found in Mexico. Geotriton* carbonarius, Cope, Pr. Ac. Nat. Sci., Phil., 1860, 373. North Eastern Mexico. Geotriton adspersus, Peters, Monatsber. Acad. Berlin, 1863, 468. Bogota, New Grenada. Spelerpes cephalicus, sp. nov. Table Land, Mexico. Spelerpes orculus, sp. nov. Table Land, Mexico. Spelerpes chiropterus, Cope, Pr. Ac. Nat. Sci., 1S63, p. 54. North Eastern Mexico. Spelerpes bellii, Gray, Cat. Brit. Mus., 46, 1850. Cope, 1. c, 1860, 372. North Eastern Mexico. Spelerpes lineolus, sp. nov. Table Land, Mexico. The form of the present species is more that of Amblystoma o p a c n m, and is the shortest and stoutest seen in th% genus. Muzzle rounded, truncate, with obtuse angles at the nares, its length from line connecting anterior can- thus oculorum equal length of eyte. Distance between these canthus equal from hinder canthus to nares. Breadth behind orbits equal length of tibia and foot. Muzzle to axilla equal | distance from axilla to groin. Costal folds (i. e., dorsal and lumbar vtsrtebrae) eleven. Tail swollen, little compressed, constricted at base. Posterior limb stout, extending to sixth fold from be- hind ; toes flat, depressed, margined, inner very rudimental. Inner and outer digit of anterior limb similar ; the longest extend to the middle of the orbit. Series of vomerine teeth nearly straight, not in contact. A post gular fold. Skin everywhere finely wrinkled. Color dull black, paler on the sides : lips and gular region minutely marbled with ashen. Length of rictus oris 2-75 lines. Length to axilla 6'8 lines. Length to groin 16 lines. Length of tail 15 lines. Length of hind limb 5*2 lines. Habitat. — Mexican Table Lands, Dr. C. Sartorius. Spelerpes orculus. Form like that of S. chiropterus, (the inner digits being similarly ru- dimental; but stouter, a body of equal length being thicker, and the head and neck longer and larger ; the lip is not angularly truncate, and the color is uni- form black. Costal folds eleven. Head elongate, broader behind ; muzzle rounded, truncate, lip rounded ; eyes little prominent ; length of orbit equal from orbit to nostril, and greater than between their anterior canthi. Ante- rior digits to middle of orbit ; posterior extends to the sixth from the groin. Tail' compressed, flat above. The digits are all short and flattened, not pal- mate. Series of vomeiiue teeth very oblique, in contact medially. Postgular fold distinct. From end of muzzle to postgular fold 3-8 lines. From end of muzzle to ax- *The genus recently named, by Du Bocage, Chioglossa, 1*. Z ?., 1S64, p. 204, appears to be not different from Neurergus, Cope, Pr. A. N. S., 1862, 343. [Oct. NATURAL SCIENCES OF PHILADELPHIA. 197 ilia 5*4 lines. From end of mu#zle to groin 13 • 9 lines, of tail 21 "1 lines. Length of hind limb 4'4 lines. Habitat. — Mexican Table Land, Dr. C. Sartorius. From groin to end Spelerpes 1 i n e o 1 u s. The species has the general form of Batrachoseps attenuatus, but, as the number of digits is as in Spelerpes, I retain it for the present in that ge- nus. Form very slender ; fourteen costal folds from femur to axilla, the first at the femur. Muzzle short, rather thick, regularly rounded ; eye large, di- ameter equals frontal width between middle supercilia, longer than length of muzzle. A delicate linear supraoccipital crest on the cranium. Limbs very small, each extending backwards or forwards over but two costal folds. Digits obtuse, rudimental ; no web. Tail compressed, slightly flattened above and below, two and a half times length of body. Head to axilla a little less than half from axilla to groin.- A delicate postgular fold. Color, above and below, uniform glossy black. Length from end^f muzzle to rictus oris 1*4 lines. Length from end of muzzle to axilla S-SWines. Length from axilla to groin 8*2 lines. Length from groin to end of tail 20 "4 lines. Length of anterior limb 1-2 lines. Length of posterior limb 1-5 lines. Habitat. — Table Land of Mexico. Dr. Chas. Sartorius. The species sent by Dr. Sartorius to the Smithsonian Institute, are as fol- lows : From near Vera Cruz. From Table Land and Southern Mount- Spelerpes chiropterus, s. n. Spelerpes bellii Geotriton carbonarius. Hyla miotympanum, s. n. Hyla baudinii. Rana, sp. Sceloporus. Sceloporus. Laeninnctus longipes, Corythaeolus vittatus. Anolis biporcatus. Gerrhonotus tessellatus. Ameiva undulata. Boa eques. Catostoma semidoliatum. Tantilla miniata, s. n. Stenorhina ventralis. Ophibolus polyzonus, (Coronella for- mosa, Schleg.,) s. n. Diadophis ?stictogenys, (D. texensis, Kenn.) Ninia collaris. Ninia diademata. Che'sodromus liebmanni. Thamnophis, sp. Spilotes auribundus,t s. n. ains. Siredon, sp. Spelerpes cephalicus, s. n. Spelerpes orculus, s. n. Spelerpes lineolus, s. n. Hyla gracilipes, s. n. Hyla miotympanum, var. Rana ruontezuni3e*(Miex icana, Ruppel.) Sceloporus. Sceloporus. Sceloporus. Anolis biporcatus. Gerrhonotus. Ameiva. Ameiva. Plistodon lynxe. Catostoma semidoliatum. Catostoma chalybaeum. Tantilla. Ophibolus micropholis. Rkadinsea decorata. Pliocercus elapoides. Thamnophis. Thamnophis. Tropidoclonium storerioides, s. n. Arizona deppei, {lineaticollis, Cope.) Drymobius margaritiferus. * The species from Natal, supposed by me toba R. mascariensis, from Natal, Pr. Acad. Phil., 1862, 340 is very different, and may be called it s p i n i d a c t y 1 a. t The so-called diacranterian and allied genus Stegonotus, D. B., has but a slight development of the posterior tooth, and might be as well considered coryphodont. Giiuther's Lidaphis is identi- cal. 1865.] 198 PROCEEDINGS OP THE ACADEMY OF Tropidodipsas sartorii, (Leptognathus Himaotodes cenchoa. dumerili, Jan Elenco,) s. n. Elaps, sp. .Sibon septentrionale et var. Trigonocephaly atrox. Himantodes leucomelas, s. n. Crotalus ravus, s. n. Elaps elegans. Caudisona polysticta, s. n. Trigonocephaly atrox. Bothriechis mexicanus. A Contribution to a Knowledge of the DELPHINIDJ2. BY E. D. COPE. Thirty specimens of species of this family at my disposal indicate twenty- two species, of which ten are in the Museum of the Academy. They are : Monodon monocerus. Specimens from Drs. Hayes and Kane; the latter complete. Beluga c a t o d o n . Three complete skeletons, from Drs. Kane and Hayes. Phocaena, undetermined. 0 Globicephalus intermedins Gray, Harlan. Jour, Acad. Nat. Sci., 1829, 51 ; Gray, Catalogue B. Mus. One specimen from Cape Cod, Mass , kiDdly lent me from the Mus. Salem, Mass., (No. 223,) through my friend F. W. Putnam, indicates a form differing little from the European G. m e las, or Pilot Whale. The muzzl.e from the maxillary notch is longer, and the premaxillaries a little narrower on its terminal two-thirds than represented by Cuvier's plate (Ossemens Fo?siles 222), or Gray's measurements of the me las. Like the m e 1 a s, it is characterized by the straightness of the plane between the fora- men magnum and the supraoccipital crest, by the large exposure of the vomer to beyond the maxillary notch, and of the inner portion of the maxillaries from the nasal meatus to opposite the notch. The concavity of the cranium at this point is 1 in. 4 1. below the plane connecting maxillary alue at the notch, and the intermaxillaries fall very much out of view, except on the terminal half of the mu/zle. In this specimen the supraoccipital crest and spine and the protuberance of the nasal bones are remarkably developed ; and the palatines and ptery- goids regularly rounded and without angle in section. In. Lines. Length from end of muzzle to occipital condyle 24 6 " " to maxillary notch 13 6 " " " to occipital crest.... 22 4 " from occipital crest to foramen magnum 6 2 Breadth of muzzle at middle 7 2 " " at notch 9 3 " of premaxillaries at front of blow hole 6 4 between orbits 15 4 " , " temporal crests ' 11 Elevation of nasals above maxillary plate 2 6 Teeth 9or]0 ? Orca meridionalis Flower, Proc. Zool. Soc. London, 1864, 420. A muzzle and jaws of this formidable tyrant of the Australian seas are in the Mus. Salem, Mass., unfortunately without locality. The specimens in its museum are derived from the merchant vessels which trade between that port and various parts of the world. The form is massive, and agrees closely with the description and figure above cited ; the end of the muzzle is perhaps a little more arched. The out- line is more acuminate and the intermaxillaries broader, the mandibular rami [Oct. NATURAL SCIENCES OP PHILADELPHIA. 199 are narrower, and the end of the muzzle more prolonged into an edentulous beak than appears in Prof. Reinhardt's figure, in his memoir on Orea eras- si d e n s. The triangle extends to opposite the posterior tooth ; the premaxillaries below, to opposite the third from behind. At the latter point the width of the intermaxillaries is double the width from their border to the plane of that of the maxillaries, and it increases from that point to the end of the muzzle, where they are rugose and decurved. Teeth JL, very strong, cylindrical, and incurved, except the posterior superior, whicn is weak and straighter. W In. Lines- Breadth of muzzle at notch 8 " at fifth tooth 6 6 " at anterior tooth 3 Length from notch 12 8-8 of ramus maudibuli from condyle 20 of series of mandibular teeth 9 8 " gonys 3 7 Depth of ramus behind last tooth 2 9 " " at coronoid process •. 5 5 Lagenorhynchus leucopleurus Gray. One cranium Mus. Academy, loc. unknown, with long styloid process and deciduous maxillary teeth. • m Iu Lines. Length from end of muzzle to occipital condyle 13 8 " " to supraoccipital crest :. 11 6-8 " " " to maxillary notch.... 6 11 " of temporal fossa 2 8 " of styloid bone 3 1-8 Breadth at middle of muzzle ." 2 7 " at notch 3 10 of nasal meatus 2 1-4 between postorbital processes 7 8 " " temporal ridges " 6 5-8 Teeth 27 ? Delphinus tursio, Fab. A half grown specimen, judging from the dis- tinctness of the epiphyses. Though differing in various points from the description of Cuvier, the most exact we possess, the peculiarities can be mostly ascribed to immaturity. The specimen is complete, and is supposed, with some degree of probability, to have been taken on our coast. Breadth of muzzle at notch, two and one-sixth times its length ; latter dis- tance, five-ninths total length of cranium. Occiput fuller in profile than in Cuvier's figure, and considerably broader when viewed from above : this breadth enters length of cranium two and one-sixth times. Parasphenoid alas not excessively prominent. Vertebra C. 7, D. 11, L. 22, to first pierced laterally; C. 13. Eleven pairs of ribs. Cuvier gives D. 13, L. & C. 3S, and thirteen pairs of ribs. It is evident that six vertebrae have not been lost from our specimen, though some may be wanting, and possibly one pair of ribs : the limit of variation in this respect among the dolphins is not known. Compared with Cuvier's figure, the diapophyses of the atlas are narrower and more acuminate, and the superior and inferior processes of the fifth cervical verteba-a less developed and convergent. The dorsal diapophyses are thinner, and destitute of a marked anterior ridge. In the twelfth caudal the chevron bone is as large as the neural spine in profile. The anterior sternal piece is less emarginate and not laterally projecting in our specimen: the nosterior * K. Danske vid. Selskab. Forhandl. 1862, 101. 1865.] 200 PROCEEDINGS OP THE ACADEMY OP piece is cartilaginous, with the anterior fourth alone ossified. The trifling differences in the scapula would probably vanish with age, as the less extent of the superior and supero-anterior outline. Teeth acute, incurved. Length from end of muzzle to notch 9 in. " (straight) from end of muzzle to occ. condyle ;. 17 " " " " atlas to last dorsal 14-25 in. " " " " " caudal 40 in. " of anterior limb 9-75 in. " of scapula ! 6-5 " Height of " % 4-5 " Breadth of occiput between temporal crests 7 in. " muzzle at notch 4 " " " middle 2-75 in. Other characters are apparent in the following comparison : A. Palate without lateral grooves : teeth 53. Premaxillaries forming an elevated, rounded ridge tursio. B. Palate do. : teeth 34—42. a. Outline from foramen magnum to frontal crest nearly straight. Diameter of temporal fossa, made longer than preorbital process ; muzzle flat ; paroccipital most curved outward and developed ; width of muzzle at notch two and a half times in length clymene. aa. Outline from foramen to crest curved, cranium rounded ; temporal fossa much longer than pre- orbital process. Occiput rounded, broad ; paroccipital well developed ; tri- angle to tooth line. Muzzle shorter, 2J its width at notch, flat at the end, premaxillaries" a high ridge me- dially doris. Occiput rounded ; paroccipital ala strongly curved outwards ; width of flat muzzle at notch two and a half times in length. Triangle short styx. Occiput elevated ; paroccipital ala very little developed ; muzzle flat, narrow ; width at notch nearly three times in length; triangle long asthenops, var. Occiput broad, subtruncate, prominent behind the temporal fossae ; width of muzzle at nqtch two and a half times or less in length ; frontal regions broader — otherwise as last, asthenops. a.aa. Supraoccipital rounded in profile ; diameter of tem- poral fossa shorter than preorbital process. Muzzle very flat, 2£ times breadth at notch ; a keel in front of nasal meatus crot aphis c us. C. Palate do. : teeth 48—54. Muzzle ridged by the elevated premaxillary bones ; width at the notch one-fourth the length ; triangle short ; occiput rounded; teeth below 49—51 mi crops. D. Palate with deep lateral grooves. Teeth ^ | ; occiput rounded ; premaxillaries forming an ele- vated angular ridge, subtrigonal in section ; paroccipital little developed. Smaller nasal meatus delphis? var. Teeth 37 — 42 ; occiput short, rounded ; breadth of muzzle to length as 1 : 2§ ; premaxillaries forming a rounded ridge. Larger nasal meatus delphis. The form of the fossa of the orbitospheuoid which is overhung by the plate [Oct. NATURAL SCIENCES OF PHILADELPHIA. 201 of the maxillary, appears to coincide to some extent with other peculiarities of the species. It appears under the following modifications : a. Deep, enclosed, so as to be a blind canal ; D. doris, clymene. /?. Shallower, open, but strongly marked ; D. s ty x, Delphinapterus peronii, D. delphis, (less marked.) y. Very shallow, little marked ; D. asthenops et var., microps, crotaphiscus. Delphinus doris Gray, Catal. Brit. Mus. Zool. Erebus, Terror tab. One specimen, habitat unknown, from the Museum at Salem, Mass., agrees closely with Gray's indications, with, however, a shorter occiput than repre- sented in his figure. The triangle is marked with numerous curved grooves which converge, and are convex, backwards. The cranium is quite as heavy as that of the t u r s i o. The sella turcica is more strongly marked than in the other species, and the processus olivaris much more prominent and solid. The basioccipital is not grooved for the medulla oblongata ; the paroccipital alae are well developed. The glenoid cavity sends a groove upwards on the inner border of the squamosal process, but its inner border is not pro- longed into an extended lamina towards the sphenoid bounding the periotic elements in front, as in the Delphinapterus. The palatines have not the strong external ridge seen in the latter and the D. crotaphiscus. Teeth 3 5* , i- in. lines Length from end of muzzle to convexity of occ. condyle. 16 4 " •« " notch 9 9 " from notch to middle of occipital crest 5 4 " ofgonys 1 11 Width at notch 4 " at postorbital processes 7 10 " between temporal crests 6 5 Delphinus clymene, Gray, Cat. Cetac, p. 115. Zool. Ereb. & Terror, 39. That this species is an inhabitant of the coasts of the United States, is proven by the specimen in the Museum of the Academy from off New Jersey, pre- sented by John Krider, of this city. Its peculiarly flat occiput distinguishes the cranium at once from that of its congeners ; in other respects it is not un- like the s t y x of our collection. Length of muzzle to notch 11*25 in. From end of muzzle to foramen magnum 18 Length of gonys 1*5 " from notch of muzzle to foramen magnum 6-25 " " foramen magnum to occipital crest 4 Breadth between temporal ridges 6*5 " " angles of mandible 3-87 " at notch of muzzle 4*25 Delphinus styx, Gray, 1. c. 117. Zool. E. T., pi. 21. One cranium, Morton collection. Habitat unknown. Length from end of muzzle to notch 10 in. " " notch (straight) to foramen magnum 7 " " " " to occipital crest 5 " " ofgonys 1*75 in. Breadth at notch of muzzle 4*25 " " between temporal ridges (straight) 6*75 " " " angles of mandible 3*50 " Delphinus asthenops, sp. nov. Two crania of this species before me are light and rather slender, though 1865.] 202 PROCEEDINGS OF THE ACADEMY OP less so than those of the D. euphrosyne and rniorops. The muzzle, though convex in section, is more depressed than in any of the other species, especially opposite the posterior extremity of the dental series. The acumi- nate basal triangle extends an inch or more beyond this point. The prernax- illaries are in one specimen quite continuous with the surface of the maxil- laries ; in the other specimen, a slight groove marks the suture. The blow- holes are rather small, and the nasal bones prominent. The breadth and de- pression of the occipital region is the most striking feature. The temporal crests are as. far apart as one-half the length of the muzzle measured in front of the blow-holes, (in the variety b^low it enters two and two-fifth times,) and the outline of the occiput between them nearly transverse. Its breadth is more than double the height of the occipital crest above the foramen magnum, (one- half in the variety.)" The frontal bones are broad and large ; the width at the blow-holes enters the length of muzzle from the same point one and three- fifth times ; in the variety very nearly twice. These differences are not greater than occur in human skulls, yet it is probable that in a state of nature they accompany other differences, which are together preserved isolated, indi- cating the existence of species. The gutter between the occipital condyles is narrow. In one specimen (596) the anterior basi-occipital suture is but little concave; in the second, (595,) its sphenoid portion is a little distance be- hind its pterygoid, while in the variety (499) the sphenoid encroaches much more upon the occipital. In the latter, the supraoccipital crest is slightly developed ; in asthenops, (595,) a larger individual, it is more so, though slight ; in 596, neither it nor the temporal crest exist. In this the muzzle is a little shorter ; it is evidently a younger individual of a larger specimen than the variety. The following measurements will explain their other features : 595 596 Length from notch to occipital condyle 5J in. 5| in. " " " to middle supraoccipital crest... 4| " 4| " " " " to end of muzzle 9i " 9 " Width of muzzle at notch 3 , (j in. 3T. The species which I have referred to this genus differs from C. t a b a c i, the type described by Gucrin (Rev. et Mag. Zool. 1850, 431.) by the last joint of the palpi being truncate, but not emarginate. There is, however, not a complete uni- formity in the different species of Xyletinus in this respect, and I have, there- [Oct. NATURAL SCIENCES OP PHILADELPHIA. 239 fore, preferred placing the insect in question in the present genus, to multiply- ing unnecessarily the divisions already proposed. The body is oval and convex, very similar to Hemiptychus, but the first ventral segment is not excavated for the reception of the hind feet. The metasternum is declivous in front, with the declivous part limited by a transverse line, pre- cisely as in Lasioderma s e rr ic o rn e, (which it resembles in appearance, though larger), except that the line becomes obsolete towards the sides. The anterior and middle coxae are contiguous, as in the species just named. The antenna? are 11-jointed, with the first joint curved and moderately dilated, the second longer and thicker than the third ; 3 — 8 equal in thickness, the third longer, the others about as loDg as their width ; ninth and tenth large, com- pressed, triangular, ninth as long as the five preceding united, tenth a little longer, eleventh as long as the tenth, and a little narrower, oval, rounded at the tip. The head beneath is as deeply excavated as in L. serricorne; the front is obtusely impressed in the same manner. The tibiae are compressed, with two elevated lines externally ; the tarsi are dilated, with the first joint moderately elongated, the second equal to the third, and the fifth clavated and depressed. The eyes are uniformly convex, moderately granulated, as in La- sioderma, and not at all emarginate. 1. C. s i m p 1 e x, longius ovale, convexum, nigro-fuscum, pube helva sericeo- pubescens, opacum alutaceum, punctulatum ; thorace medio dense, lateribus parce punctato, brevi antice subtruncato, basi cum lateribus rotundatis, an- gulis posticis nullis, anticis impressis valde deflexis, (lateraliter visis acutis,) elytris thorace triplo longioribus, baud punctatis ; antennis pedibusque testa- ceis. Long. -14 — -18. Two specimens, collected in Kentucky, by Mr. J. H. Wild. HEMIPTYCHUS Lee. Synonym. Dorcatoma Zee, Class. Col., 204. This new genus completes the passage from the preceding genera to Dorcato- ma, from which it differs by the anterior coxae being contiguous, as'in Lasio- derma; by the prosternum being short, and not prolonged into two processes behind ; the mesosternum being flat, perpendicular and triangular, and the metasternum without medial channel, not produced in front, but straight, with a very small protuberance at the middle between the middle coxae. The eyes are coarsely granulated, not uniformly convex as in Catorama, but compressed longitudinally at tne side, and very feebly emarginated in front. The antennae are 10-jointed, the first joint large auriculate, second much smaller, somewhat dilated, 3 — 7 narrow, very small, closely united, eighth triangular, as long as the six preceding united, -ninth a little narrower than the eighth, tenth oval, longer than the ninth, and rounded at the tip. ' Palpi with the last joint dilated, truncate. Feet robust, tibiae, compressed, with a deep, longitudinal furrow on the outer surface, tarsi stout. First joint as long as the two following united. First ventral segment excavated for reception of hind feet. Elytra with two submarginal striae, extending from the middle to the tip.* Our species may be distinguished as follows : Elytral striae faintly visible at base ; pubescence coarse : Body elongate, elytra densely punctured 1. punctatus. Body oval, elytra sparsely punctured 2. gravis. Body almost rounded, elytra sparsely punctured 3. p u si 11 u s. Elytral striae not prolonged in front; pubescence fine : Surface very finely and densely punctulate: Stria fine, body broadly oval 4. borealis. Striae deep, body elongate oval 5. v entr a li s. * Dorcatoma externa Muls. A Rty, TSiediles, 367, probably belongs to this genus. 1865.] 240 PROCEEDINGS OP THE ACADEMY OP Strife very fine and short, body oval 6. obsoletus. Surface sparsely and finely punctulate, body elongate oval, striae deep 7. nigritulus. 1. H. punctatus, elongato-ovalis, subcylindricus, piceus, dense minus subtiliter helro-pubesceus, subtilissime punctulatus, elytris praecipue versus latera punctatis et rugosis, striis duabus externis a medio ad apicem profun- dis, antice obliteratis, externa ad humerum paulo impressa ; antennis flavo-tes- taceis. Long. -11. Two specimens, one from Louisiana, the other from Georgia. The species of this genus agree so nearly in most of the characters, that it is only desirable to mention the distinctive marks under each species. Tbis oue is narrower than the other coarsely pubescent species, and the elytra are twice as long as their width, and decidedly more punctured, especially at the sides ; the two ex- ternal strife are deep, and extend from the middle to the tip, before the middle they are obliterated, but at the base the outer oue again becomes visible ; there are faint traces of strius near the sides and tip. 2. H. gravis, ovalis, piceus, dense minus subtiliter helvo-pubescens, sub- tilissime punfUulatus, elytris parce punctatis, striis duabus externis a medio ad apicam profundis, antice obliteratis, externa ad basin paulo impressa, an- tennis flavo-testaceis. Long. -12 — -15. Dorcatoma grave Lee, Proc. Acad. Nat. Sc. Phila., 1858, 72. Pennsylvania, Dr. Melsheimer ; Texas. " More )egularly oval than the prece- ding, with the elytra only sparsely punctured. There are some faint traces of strife inside of the two outer ones, which are deep from the tip to the middle and then obliterated ; the outer one is visible near the base. Two smaller specimens (-10 unc.) collected in Illinois, by Mr. B. D. Walsh, differ by the elytra being more finely punctulate, and more sparsely but dis- tinctly punctured ; I do not regard them as indicating a distinct species. 3. H. pu sill us, rotundato-ovalis, convexus, rufo-piceus, dense minus sub- tiliter helvo-pubescens, elytris parce punctulatis, striis duabus externis antice obliteratis, antennis flavo-testaceis. Long. -08. Dorcatoma piikillum Lee, Proc. Acad. Nat. Sc. Phila., 1858, 72. Found at Fort Yuma, (junction of Colorado and Gila), California. The smaller size and more rounded form readily distinguish this species. The surface appears nearly smooth, with scattered very fine punctures on the ely- tra, almost concealed by the pubescence. 4. H. b o r e a 1 i s, rotundato-ovalis, convexus piceus, subtiliter griseo-pubes- ens, vix conspicue punctulatus, elytris striis externis duabus ad medium antice abbre'viatis, capite rufescente, antennis testsceis. Long. -12. One specimen, Lake Superior. The thorax is somewhat more compressed at the sides, so that the outline is straight, and the body becomes more acuminate in front, than in the preceding species. The surface is scarcely visibly punc- tulate, and there are no scattered punctures on the elytra; the strife are finely, but well impressed, and are absolutely abbreviated, not obliterated in front as in the preceding three species, and without any traces of prolongation near the base. 5. II. ve n t r al i s, elongato-ovalis, niger nitidus, subtiliter griseo-pubes- cens, subtilissime punctulatus, elytris striis duabus externis profundis, ad medi- um antice abbreviatis, capite abdomine pedibusque obscure rufo-piceis, anten- nis flavo-testaceis. Long. -07 — -09. Illinois, Mr. B. D. Walsh. The elongate oval body, equally rounded at each end, and not at all acuminate in front, will readily distinguish this species. The pubescence is very fine, and there are very fioe scattered punctures on the elytra. 6. H obsoletus, ovalis, convexus, niger nitidus, subtiliter griseo-pubes- [Oct. NATURAL SCIENCES OF PHILADELPHIA. 241 cens, vix subtilissime punctulatus, elytris parce subtiliter punctulatis, striis ex- ternis duabus subtilibus, pone medium antice abbreviatis, antennis testaceis. Long. -10. One specimen collected at Cape San Lucas, Lower California, by Mr. John Xantus, and given me by Mr. Ulke. This species has also a regularly oval form, equally rounded at eacb end, but is broader than H. n i g r i t u 1 u s, with the striae of the elytra finer and shorter, extending scarcely more than one- third of their length. 7. H. n igr i t u lu s, elongato-ovalis, niger nitidus, subtiliter griseo-pubes- cens, minus dense subtiliter punctulatus, elytris striis duabus externis profun- dis pone medium antice abbreviatis, antennis tarsisque testaceis. Long. -09. One specimen, Pennsylvania. Of the same form and size as H. v e n t r a 1 i s, but distinguished by. the body being entirely black, with the upper surface less finely and not densely punctulate. PROTHECA Lee. The two species constituting this genus are small, short, cylindrical insects, having more the appearance of minute Hylesinus than of any genera of this group. The head is deeply excavated beneath, with a medial gular pro- minence, as in Lasioderma serricorne, near which the antennae are curved in a state of repose. The eyes are entire, slightly convex, and moderately finely granulated. Palpi with the last joint triangular, broadly truncate. An- tennae with the first joint long and thick, slightly curved, but scarcely auricu- late ; second joint rounded, thicker than the following; 3 — 8 small, triangular, the third, fifth and seventh being broader thau the others ; ninth and tenth subtriangular, one-half longer than wide ; eleventh longer, oval, the three to- gether as long as the preceding joints united. Prothorax convex, transverse, gradually narrowed in front, with the sides nearly straight, hind angles rounded, front angles very much deflexed ; prosternum very short, acute behind ; front coxae almost contiguous, conical, depressed ; mesosternum perpendicular, slightly concave in the middle; metasternum deeply channelled, declivous in front each side, somewhat prominent and deeply foveate between the middle coxaj, declivous portion scarcely excavated for reception of middle feet, but defined posteriorly by a transverse line, extending to the medial furrow. First ventral segment excavated for reception of hind feet, and almost entirely con- cealed by them. Feet slender, tibiae not compressed, tarsi moderate. First joint slightly elongated ; front tarsi visible in repose, folded over the tip of the mandibles, and along the anterior margin of the metasternum. Epipleurse ex- cavated beneath the humeri for the reception of the middle knees, sinuate at the margin, and foveate for the reception of the hind knees (as in Pe ta li u m and T h e c a) ; strife composed of punctures, scarcely impressed, even at the sides. Our two species may be distinguished as follows: Striae of elytra not obsolete behind p u b e r u la. Striae of elytra obliterated behind h isp i d a. 1. P. p u b e r u 1 a, ovalis, subcylindrica, picea, pubescens, thorace subtiliter dense punctulato, elytris nitidis, seriebus punctorum postice haud obliteratis, interstitiis rugosis, antennis Mavis. Long. -08. Pennsylvania, three specimens ; Georgia, one specimen. The pubescence of the elytra is arranged in lines, the hairs are not rigid, and the rugosities of the intervals are quite obvious ; the striae are composed of punctures, which are large at the base, and become small towards the tip. 2. P. h i s p i d a, ovalis, nigro-picea, opaca, pube rigida cinerea induta, tho- race punctulato, elytris seriebus punctorum subtilibus pone medium oblitera- tis, interstitiis alutaceis, parce punctulatis, antennis flavis. Long. -08. 1865.] 242 PROCEEDINGS OF THE ACADEMY OP Georgia, several specimens. Shorter and more robust than the preceding, and easily distinguished by the difference in sculpture. Subgroup IV. DORCATOMATA. The body is oval convex, or even globose, capable of being closely contracted. The head when deflesed is received into a deep cavity of the prothorax, aud the mandibles abut against the anterior margin of the metasternum, which ia prolonged between the middle coxa? into a short, broad lobe, nearly truncate in front. The antenna? are received in a sternal cavity between the front coxae, and in the mesosternum, which is deeply buried under the metasternum. The first joini is large and auricnlate, and the last three joints dilated and very large, forming a loose club much longer than the preceding portion. The pro- gternum is very short and broad, and separates widely the front coxa?, which are small, conical and ascend perpendicularly along the sides of the cavity. The middle legs are received in deep excavation.? of the meso- and metaster- num, the tarsi resting in small, deep grooves behind the metasternal lobe, and the knees in subhumeral cavities of the epipleurae. The first ventral segment is deeply excavated each side for the reception of the hind legs ; the knees are not received in epipleural foveas. The ventral segments seem disposed to be- come connate. Our genera are but two, distinguished as follows: Prosternnm produced behind into two long horns. Dorcatoma. Prosternum broadly truncate behind Ccenocara. DORCATOMA Herbst, (emend. Thomson, Skand. Col. i. 90.) This genus, as restricted by Thomson, and subsequently by Mulsant and Rey, contains species of oval form, having the eyes slightly emarginated and rather finely granulated. The head is not excavated beneath, but only impressed, and the antenna? are received upon the breast, between the anterior coxa?. Antenna? 10-jointed ; first joint large, auricnlate, second much smaller, di- lated ; 3 — 7 narrow, very small ; eighth triangular, as long as the six preceding united; ninth triangular, as broad as the eighth in the males, but in the fe- males a little narrower; tenth, oval, about one-third longer than the ninth, more or less curved, rounded at tip. Palpi with the last joint securiform. Prosternum (visible only on dissection) broad, short, concave, produced be- hind into two slender and divergent horns, which fit into excavations of the mesosternum ; anterior coxa? small, perpendicular, widely distant. Mescster- num deeply excavated, concealed under the metasternum, which is produced be- tween the middle coxa?, and truncate in front; medial channel well marked. Feet moderate, tibia? slender, tarsi moderate, first joint somewhat longer. First ventral segment excavated for the reception of hind feet. Elytra generally with two entire marginal stria?, and a short one near the humerus, more or less visible, sometimes with stria? abbreviated near the base. The punctures in our species are arranged so as to leave intervening, narrow, smooth vitta? ; the epipleura? are not at all foveate for the reception of the knees of the hind feel. Our two species may be readily distinguished by the sculpture of the elytra. Elytra sparsely punctulate in rows, stria? entire setulosum. Elytra densely punctulate in bands, striae abbreviated in front incomptum. 1. D. setulosum. ovale convexum nigrum nitidum, pube brevi erecta fusca vestitum, thorace subtiliter punctulnto, elytris subseriatim baud dense punctulatis, seriebus fere per paria approximatis, striis duabus externis pro- fundis, 3ia brevi antennis pedibusque piceo-testaceis. Long. -09. Lake Superior, Pennsylvania, G-orgia, also in North Carolina, (Dr. Zimmer- mann.) The punctures of the elytra are fine, not densely placed, arranged al- most in regular rows, which are approximated by pairs ; the pubescence is [Oct. NATURAL SCIENCES OF PHILADELPHIA. 243 brown, rigid and erect; the two outer strife are deep, the third is short at the base, but continued by punctures of large size almost to the middle. The ab- domen is finely and densely punctured, the segments apparently connate, the metasternum coarsely and irregularly punctured. 2. D.incomptura, ovale convexum, nigrum nitidum, pube longiore fusca vestitum, thorace punctulato, capite abdomineque rufescentibus, elytris dense punctulatis, vitiis angustis impunctalis ornatis, pilis bifariam positis, striis du- abus externis profundis, antice paulo abbreviatis ; antennis testaceis, pedibu3 piceis. Long. 09. South Carolina (Dr. Zimmermann,) and Pennsylvania ; two specimens. The punctures of the elytra are very fine and close set, arranged in bands, with in- tervening, narrow, smooth bands ; the pubescence is brown, and the hairs lie some longitudinally, some obliquely directed outwards ; the striae are deep, do not extend to the base, but are abbreviated about the anterior fourth ; no vestige of a short humeral stria is seen. The abdomen is finely, the metasternum more coarsely and less densely, but equally punctured. CCENOCARA Thorns., Skand. Col. i. 90, (1859.) Synonyms. Tylistus Lee, Class. Col. 203, (1862.) Enneatoma Muls. $'Rey, Col. Fr. Terediles, 367, (1863.) In this genus the body is broadly ovate, nearly globose ; the eyes are deeply emarginate, and nearly divided by an impression. The antennae are 9-jointed ; first joint long, auriculate, second small, rather broader than its length ; 3 — 6 very small, indistinct; seventh large, transverse triangular, very much pro- duced inwards in the male ; eighth elongate, subtriangular, as long as the transverse diameter of the preceding joint, ninth longer than the eighth, elon- gate oval, somewhat curved, very small at point of attachment to preceding joint. Palpi with the last joint triangular, truncate : head transversely vaguely excavated beneath. Piosternum very short, concave, broadly truncate behind, widely separating the anterior coxae; mesosternum entirely concealed under metasternum, deeply concave. Metasternum large, not channelled ; produced between the middle coxae, and widely truncate in front. First ventral segment excavated for reception of hind feet. Feet slender, tibiae not compressed, tarsi moderate. First joint longer than the two following united. Elytra with three striae towards the sides, the two outer ones entire, the inner one extending from the humerus to near the middle. The larvae live in species of Lycoperdon (puff balls,) and before being transformed construct small, ellipsoidal cells, in which the subsequent changes take place. The perfect insects are found on leaves, chiefly of oak. The two species in my collection are easily distinguished. Elytra coarsely punctured, pubescence hispid o c u 1 a ta. Elytra finely punctured, pubescence short, prostrate scymnoides. To this genus probably belongs Dorcatoma bi color Germ., Ins. Nov. 79, which is unknown to me. The antennae, head, thorax and feet are red, the rest of the body black. 1. C. oculata. Dorcatoma oculata Say, Long's Exped. St. Peters., ii. 273, ((-^); (ed. LeConte, i. 180 ;) Bore, simile Say, Bost. Journ. Nat. Hist., i. 166, ( 9 ) ; (ed. LeConte, ii. 642 ;) Tylistus similis Lee, Class. Col. N. Amer., 204. Abuudant throughout the Atlantic States, from Lake Superior to Louisiana, and from Maine to Kansas. The punctures of the elytra are coarse and distant, and the pubescence rigid and snberect, some of the hairs directed longitudi- nally, others obliquely outwards. In the female the seventh joint of the an- tennae is almost regularly triangular, and but little produced inwards; the eighth joint is less slender than in the male, and the last joint less arcuated. These differences account for the two specific names given by Say. The striae are deep, and the inner one extends from the base nearly to the middle. 1865.] 244 PROCEEDINGS OP THE ACADEMY OP • 2. C. seymnoides, rotundata convexa nigra subnitida, confertim subtili- us punctata, pube brevi cinerea depressa vestita, striis externis duabus integris, 3ia ante medium postice abbreviata, antennis tibiis tarsisque piceo-testaceis. Long. -10. One specimen (female) collected in Vermont, by the late Prof. C. B. Adams. The fine, short cinereous pubescence produces a pruinose appearance ; the striaft are less deep than in C. o c u 1 at a. The under surface is less coarsely and more densely punctured than in that species. The seventh joint of the an- tenna? has the form of an equilateral triangle ; the eighth is narrower, and sub- triangular, the ninth elongate, oval and not curved. The general appearance, dependent on the form and pubescence, is that of aScymnus. November 7 th. Mr. Cassin, Vice-President, in the Chair. Twenty-five members present. November 14 th. The President, Dr. Bridges, in the Chair. Thirty-four members present. The following paper was offered for publication : " Contributions to tbe Palaeontology of Illinois," &c. By F. B. Meek and A. H. Worthen. November 21 st. The President, Dr. Bridges, in the Chair. Thirty-one members present. November ,28th. The President, Dr. Bridges, in the Chair. Thirty-four members present. December bth. Mr. Vaux, Vice-President, in the Chair. Twenty-nine members present. The following paper was offered for publication : " Observations on the microscopic shell structure of the Spirifer cupidatus," &c. By F. B. Meek. Adjourned Business Meeting from November 28th. On report of the Committee the following paper was ordered to be published : [Dec. NATURAL SCIENCES OP PHILADELPHIA. 245 Contributions to the PALEONTOLOGY of Illinois and other Western States. BY F. B. MEEK AND A. H. WORTHEN, (Of the Illinois State Geological Surrey.) MOLLUSCA. LAMELLIBRANCHIA TA . Genus LITHOPHAGA, Bolten, 1798. (Lithodomus, Cuvier, 1817.) LlTHOPHAGA? PERTENU1S, M. & W. Shell slender, elongated, narrowing anteriorly, extremely thin, moderately convex, in the central and anterior regions, more compressed and cuneate behind ; posterior margin narrowly rounded in outline; anterior extremity extremely short and very narrowly rounded ; basal margin straight along the middle, and curving up gradually towards the extremities ; hinge line straight, not exactly parallel to the base, and apparently about half as long as the shell, — passing imperceptibly into the posterior dorsal margin. Beaks almost terminal, very oblique, and nearly obsolete; umbonal gibbosity slightly raised above the hinge line. Surface smooth, or with only faint traces of fine concentric stri e, and very obscure, undefined concentric undu- lations. Length, 1*73 inch, height, 0'6"2 inch ; convexity, 0'50 inch. This species has very nearly the form of the following, but may be dis- tinguished by its smooth surface, which never shows the distinct thread-like concentric striae and regular wrinkles of that shell. As we know nothing of the hinge and interior of these species, we merely place them provisionally in the genus Lithophaga, from the similarity of their external characters, to the recent L. lithophaga. Possibly their names should be written Modiolus lin- gua/is and M. perlenuis, or more properly Volsella lingualis, and V. pertenuis, as they may belong to that genus, and Modiolus and M>diola are merely sy- nonyms with the older name Volsella. Locality and position. Warsaw, Illinois. Warsaw division of the subcar- boniferous series. Lithophaga ? lingualis, Phillips (?) sp. Modiola lingualis, Phillips, Geol. Yorkshire, ii, p. 209, pi. v, fig. 2. The shell we have referred with doubt to Phillips' species cited above, agrees with his figure in so many respects, that we are inclined to believe it probably identical, though it may prove to be distinct on comparison of speci- mens.*! It is an exceedingly thin shell, and ornamented by moderately strong thread-like concentric strise, which, on the umbonal slopes, sometimes form neat little ridges or undulations, while a few more irregular, distant marks of growth, are seen on other parts of the surface. Some of the speci- mens are much larger than that figured by Phillips, being nearly three inches in length. The direction of the marks of growth on these larger specimens, show that they were almost exactly like Phillips' figures, when of the same size. They also show that the hinge line is long, straight, and bordered by a slender marginal line within. Locality and position. Warsaw, Illinois. Keokuk division of subcarbonif- erous series. * Tt is much to be regretted that many of the species figured by Trof. Phillips in his Geology of Yorkshire, have not yet been fully and clearly described. 18G5.] 246 PROCEEDINGS OP THE ACADEMY OF Genus MODIOLOPSIS, Hall, 1847. MODIOLOPSIS PEROVATA, M. & W. Shell longitudinally ovate, the widest part being a little behind the middle, compressed, very thin, extremely inequilateral and oblique; posterior side compressed, cuneate, regularly rounded in outline ; anterior side very short, more narrowly rounded than the posterior margin. Dorsal outline forming a broad, nearly regular arch from the beaks into the posterior border ; base oblique, and somewhat straightened just in front of the middle, and round- ing up towards the extremities. Beaks compressed, scarcely projecting be- yond the rounded anterior outline, and placed directly over the anterior ex- tremity. Surface marked with regular concentric striae, and small, irregular furrows. Anterior muscular impression oval, distinct, located close to the margin, under the beak. Length, 1-92 inches ; height, 1-18 inches; convexity, (MO inch. This species has much the general appearance of Modiolopsis concentrica, (Hall, Geol. Fourth Dist. p. 19b', fig. 9,) but differs in having its anterior out- line rounded, instead of protuberant and subangular in outline. Its margin is also more prominent in the antero-ventral region, and without "a longitu- dinal impression directly below the beaks." Locality and position. White Sulphur Springs, Delaware County, Ohio. Hamilton Group, of Devonian series. Genus PLEUROPHORUS, King, 1844. Pleurophokus subcostatus. Shell elongate-oblong, moderately convex ; umbonal ridges the most convex part of the valves, and extending obliquely from the beaks towards the pos- tero-basal margin ; anteror ventral region somewhat compressed ; basal and cardinal margins very nearly straight and subparallel, the former being usu- ally somewhat sinuous or arcuate along the middle ; extremities rather nar- rowly rounded, the posterior being generally a little wider than the other, and sometimes faintly subtruncate obliquely. Hinge line long and nearly straight ; posterior lateral tooth of each valve elongated parallel to the hinge margin, very remote from the cardinal teeth, and extending back a little be- yond the posterior muscular impression. Beaks depressed upon a line with the dorsal margin, small, somewhat compressed, and placed about one-ninth the entire length of the shell behind the anterior margin. Scar of the ante- rior adductor muscle deep, trigonal-subovate, pointed above, and strongly de- fined by the prominent vertical ridge just behind it ; those of the pedal muscles small, nearly marginal, and located directly over the anterior ad- ductors ; posterior adductor scars larger and more shallow than the anterior, subquadr, te in outline, and placed close up under the posterior hinge teeth. Pallial impression well defined. Surface of casts showing traces of a few ob- scure concentric markings, crossed on the postero-dorsal region by traces of about three equal obscure radiating costse. Exterior surface and cardinal teeth unknown. Length of a medium sized specimen, (internal cast,) 0 88 inch ; height of do., 0-37 inch ; convexity, 0-26 inch. Some larger specimens of same pro- portion, measure 1*33 inches in length. This species is apparently related to P. costatus, of Brown (sp.), some vari- eties of which, as figured by Prof. King ly from the beaks to the posterior margin. Of these plica- tions, the lowest is the most prominent, and forms the umbonal ridge ; while the upper one runs parallel to the cardinul margin, aud forms the boundary of the long corselet or escutcheon. (Hinge and interior unknown.) Length, about 1'10 inch; height, 0 46 inch; convexity, 0-43 inch. At the same time that we propose to name this as a new species, we con- fess that if we had found it in Permian strata, we should have, from its 1865.] 248 PROCEEDINGS OP THE ACADEMY OF external characters at least, referred it to Pleurophorus costaim, Brown, (sp.) Indeed it seems to be as nearly like Prof. King's principal figure of that species, (f. 13, pi. xv, Perm. Foss. of England,) as any other individual speci- men could possibly be expected to be, and more nearly like it than any other figure of that shell we have ever seen. Nevertheless, from the different horizons occupied by these shells, we have scarcely a doubt that, if we could see the hinge and interior of that now before us, good specific differences would be observable. Locality and position. Keokuk division of the subcarboniferous series, Warsaw, Illinois. Genus GRAMMYSIA, De Verneuil, 1847. GkAMMYSIA ? RHOMBOIDALIS, M. & W. Shell rather large, very gibbous, presenting a rhombic form as seen in a Bide view, and a distinctly cordate outline as seen in an anterior or posterior view; umbonal slopes extremely prominent and very oblique ; beaks nearly terminal, approximate at their points, rising above the hinge line, and dis- tinctly curved inwards and forwards ; anterior and antero-ventral regions im- mediately in front of the oblique umbonal ridge, abruptly contracted, with a broad undefined depression extending from the front part of the beaks obliquely to a point near the middle of the base ; dorsal region between the umbonal ridge^ and the cardinal margin, a little concave near the beaks. Posterior margin obliquely truncated with a moderately convex outline to the posterior basal extremity, which is subangular, or very narrowly rounded ; base rather long, a little convex in outline behind the middle, and straight or slightly sinuous just in front of it, but rounding obliquely upward anteriorly. Anterior side (which is imperfect in our specimen) short, or apparently scarcely pro- jecting beyond the beaks, more or less obliquely rounded and somewhat gap- ing ; cardinal margin (judging from casts) rather short, and inflected so as to form behind the beaks a distinctly defined, rather wide depression or es- cutcheon. Surface, as near as can be determined from casts, ornamented with small, regular concentric ridges. Hinge, muscular and pallial impressions unknown. Length, about 3-55 inches ; height, 2-06 inches ; greatest breadth (near the middle of valves), 2-42 inches. The most marked peculiarities about this shell, are the remarkable promi- nence and obliquity of its umbonal ridges, —which near the beaks stand out as if compressed antero-posteriorly, — and the nearly terminal, obliquely in- curved character of the beaks. The specimen is not in a condition to show whether or not it has a distinct lunule in front of the beaks, but we suspect that it has. In some respects it resembles in form Ci/rtodonta Hindi of Billings, from the Cincinnati group, or so called Hudson riverbed of Canada, but diflers in having its umbonal ridges so much more prominent as to give greater con- vexity to the valves ; while its umbones, although more prominent, are much narrower in their antero posterior diameter. More important differences, howeve^ are the presence of a broad undefined sulcus extending obliquely from the anterior side of the beaks of our shell, to near the middle of its base, and the apparent slightly gaping character of its anterior side. Notwithstand- ing the general resemblance of these forms, there can be little doubt but they really belong to distinct families, since the Canadian shell doubtless belongs to the Arcidw, Avhile that before us appears to be related to the Anatinidce. Although we have placed our shell provisionally in the genus Grammysia, we strongly suspect that when its hinge and interior can be seen, it will be found to be either generic-ally or subgenerieally distinct from G. hi sulcata, Con. sp., the type upon which that genus was founded. At any rate, it dif- fers materially in form, and the prominence of its umbonal ridges, as well as [» ec. NATURAL SCIENCES OF PHILADELPHIA. 249 in the absence of a mesial ridge extending from the beaks to the middle of its basal margin, from that and other well determined species of the genus. Should it be found necessary to establish a new genus for this shell, we would propose to call it Rhombocardia. We remember a similar, but distinct species, from the New York Hamilton Group, which, if we mistake not, has been described by Mr. Conrad, though we cannot just now recall its name. Locality and position. — Bake-oven, Jackson Co., Illinois, Hamilton Group. Genus CONOCARDIUM, Bronn, 1837. CoNOCARDIUM OBLIQUUM, M. & W. Shell rather small, obliquely subtrigonal, gibbous ; anterior side (posterior of Woodward) very obliquely and abruptly truncated with a forward slope, and flattened so as to present a regular, cordate outline in a front view ; an- terior auricle narrow, but of unknown length ; base very short ; posterior margin sloping up from the base so as to intersect the hinge at an angle of about 45°, rather widely gaping, and crenate its entire length. Beaks mode- rately prominent, small, strongly incurved ; umbonal slopes very prominent, angular, and directed obliquely forward to the angular anterior basal extremity. Surface ornamented with rather sharply elevated, threadlike, subcrenate radia- ting ribs, narrower than the depressions between ; each of these depressions on the posterior and flattened anterior sides of the valves occupied by a smaller intermediate rib ; entire surface also marked by fine very regular radiating and concentric striae, so as to produce a neat minutely cancellated sculpturing, as seen under a magnifier. Length from the posterior extremity to the produced antero-basal angle, 0"70 inch ; height from the latter to the beaks, 0 50 inch ; length from the beaks to the posterior extremity, 0-37 inch ; convexity, 0-44 inch ; breadth of posterior hiatus, 0-17 inch. We know of no other species liable to be confounded with this. Its most marked features are the great backward obliquity of its umbonal axis, by which its beaks are placed even a little behind the middle of the body part of the shell ; and the beautiful regular cancellated style of ornament seen be- tween the ribs, under a magnifier. Locality and position.— Coal Measures. Wabash Cutoff, Posey County, Ind. Genus EDMONDIA, De Koninck, 1842. EDMONDIA ? PEROBLONGA, M. &. W. Shell oblong, the length being about double the height, very inequilateral, moderately convex ; the greatest convexity along the oblique umbonal slopes, above and below which the valves are cuneate postero-dorsally, and antero- ventrally. Posterior side distinctly compressed near the extremity, its mar- gin rounded or subtruncate in outline ; anterior side very short, less com- pressed and rather more narrowly rounded than the other ; basal and dorsal margins nearly straight and parallel, the former being very slightly convex in outline a little in advance of the middle. Beaks near the anterior end, very oblique, compressed, and but slightly elevated above the hinge margin ; umbo- nal slopes prominently rounded from the beaks obliquely to near the posterior inferior margin. Surface of caA showing only faint traces of a few irregular concentric undulations below the umbonal ridge. (Hinge and interior un- known.) Length, 2-46 inch ; height 1-25 inch. Convexity of a left valve, 0-47 inch. Although we have but a cast of this shell, showing neither the hinge, in- ternal characters, nor the surface markings, we have thought it should be in- dicated, as better specimens can scarcely be expected from such a matrix. We confess, however, that we are totally at a loss respecting its generic charac- ters, and merely place it provisionally in the genus EJmondia. 1865.] 250 PROCEEDINGS OF THE ACADEMY OP In general appearance this shell approaches Edmondia ? compressa, of McCoy, (Carb. Foss. Ireland, pi. 13, fig. 10,) but it is rather longer in proportion to its height, and has much less prominent, and more compressed beaks, as well as subangular, instead of rounded umbonal slopes. Locality and position. — Lasalle, Illinois. Siliceous limestone of the Upper Coal Measures. Genus CHiENOMYA, Meek, 1865.* CH/ENOMTA ? RHOMBOIDEA, M. & W. Shell rather small, short, moderately convex ; outline rhombic as seen in a side view ; basal and dorsal marg'ns nearly straight and parallel ; the former very abruptly curved upwards behind, and more gradually in front ; anterior aide very short and truncated or a little rounded ; posterior side distinctly truncated (obliquely) nearly the entire breadth or height of the valves, gap- ing but not dilated ; dorsal margin less than the entire length of the shell, and inflected so as to form a narrow but well defined escutcheon or false area. Beaks narrow, or compressed antero-posteriorly, rather pointed, prominent and incurved, nearly terminal or placed directly over the anterior margin. Umbonal slopes oblique, very prominent near the beaks, but less so aleng the central and postero-ventral regions ; anterior and ventral regions ab- ruptly cuneate, with a very faint undefined impression extending from the beaks obliquely backwards, towards the middle of the base, just in front of the umbonal prominence. Surface of cast ornamented with small, regular concentric undulations, with apparently very faint indications of very small radiating striae. Length 1-17 inches ; height from ventral to cardinal margin, 0-80 inch, do. to summit of beaks, 0-90 inch; convexity, 0-65 inch; gape of valves behind, 0-25 inch. Although this species seems to agree, in most of its known characters, with the types upon which the genus Chanomya was established, it differs in being a proportionally shorter and less widely gaping shell, while its beaks are much more prominent and oblique. As we know nothing of its hinge or interior, nor of its finer surface markings, it is only provisionally that we place it in the genus Chcenomya. Possibly we should call it Allorisma rhomboidalis, or Sedgwickia rhomboidalis. Locality and position.— St. Louis Limestone, of Subcarboniferous Series. Alton, Illinois. CHiENOMYA ? HYBEIDA, M. & W. Shell longitudinally oblong, moderately convex, somewhat arcuate ; dorsal margin concave in outline, ventral border longer than the dorsal, and forming a broad gentle curve nearly parallel to the dorsal outline, excepting a very faint sinuosity in advance of the middle ; posterior side a little compressed near the extremity, but rather distinctly gaping — truncated or somewhat rounded in outline ; anterior margin sloping forward from the beaks above, and apparently narrowly rounded below. Beaks moderately prominent, some- what compressed, and placed less than one-fourth the length of the valves from the anterior extremity ; umbonal slopes not prominent ; flanks evenly convex in the central region, and a little contacted anteriorly, so as to form a very faint undefined depression from the bfjpts to the base. Surface (of a cast)*showing small, obscure concentric ridges, which are most distinct and regular along the posterior umbonal slopes, where they are abruptly deflected upward at an obtuse angle ; anteriorly they are smaller, more closely arranged, and deflected obliquely forward and upward. * In describing the genus Chxnomya in the Palaeontology of Up. Mo., p. 42, 1865, some doubtn were expressed by me, in a foot note, whether or not it might bo identical with An'.hracomya, of Salter, a description of which i had not at that time seen. Since seeing Mr. Salter's figures axti description. I am entirely satisfied that these forms belong to clearly distinot genera.— K. B. M. [Dec. NATURAL SCIENCES OP PHILADELPHIA. 251 Length, 1*90 inches; height to cardinal margin, 0-90 inch ; to summit of beaks, 1 inch ; convexity, 0-68 inch. This is another form that can only be referred provisionally to the genns Chcenomya, since we know nothing of its hinge and muscular and pallial im- pressions. It has the form of the typical species of that group, excepting that its posterior extremity is more compressed, and not so widely gaping. Its most peculiar surface character, is the abrupt deflection of its obscure con- centric ridges, which give it much the appearance of a Goniomya. Indeed if found amongst Cretaceous or Jurassic fossils, we would not hesitate to refer it to that genus. As in some species of Goniomya, the ridges run parallel to the base along the middle of the valves, between the points where they are de- flected. Perhaps we should call it Allorisma hyhrida, but for the present we refer it provisionally to the genus Chcenomya. We know of no species with which it is liable to be confouuded. Locality and position. — Keokuk division of the Subcarboniferous Series ; Nauvoo, Illinois. Genus SEDGWICKIA, McCoy, 1844. Sedgwickia (Sangdinolites ?) subakcuata, M. and W. Shell elongate, suboval, somewhat arcuate, rather convex in the central auterior, and umbonal regions ; anterior side sloping, with a slightly convex outline from the beaks forward, and rather narrowly rounded at the extremity ; posterior side narrow and compressed above and behind the umbonal ridge, and obliquely truncated at the extremity ; dorsal outline horizontal and con- cave behind the beaks ; ventral margin forming a long gentle convex curve, nearly parallel to the dorsal margin, curving up gradually towards tho front, and very abruptly at the posterior basal extremity. Beaks moderately promi- nent, and placed about one-tkird the entire length of the shell from tho an- terior extremity ; umbonal ridge prominently rounded from the beaks to near the posterior basal extremity. Surface of cast without visible ci>neentrie ridges or other markings. Length, 2-20 inches ; height, 0-95 inch ; convexity, 0-72 inch. We are by no means sure that this shell belongs to the genus Sedgwickia, as properly restricted to such forms as S. attenuata and S. corruya/a of McCoy, since it is more elongated, and wants the concentric ridges usually seen on these shells. Iu general outline it approaches some species of Cercomya, Agassiz, such for instance as C. striata, from the upper jura, but its posterior umbonal ridge is not so angular, while its surface, judging from internal casts, seems to have been very nearly smooth. As we only know it from casts, nothing can be determined in regard to its hinge, nor have we any means of ascertaining the nature of its muscular and pallial impressions. Possibly we should call it Allorisma subarcuata, though its rather prominent umbonal ridg^, compressed posterior dorsal region, apparently smooth surface, and con- vex anterior slope, without a depression in front of the beaks, give it a kind of Lyonsia like aspect, not seen iu the known species of that genus. Locality and position. — Upper beds of the Keokuk division of the Subcarbo- niferous series. GASTEROPODA. Genus HOLOPEA, Hall, 1847. Subgenus ISONEMA, M. & W. ISONEMA DEPRESSA, M. & W. Shell much depressed, considerably wider than high : volutions nearly four, increasing rather rapidly in size, obliquely compressed, with a slightly convex outward slope above, — last one subangular around the middle, and 1865.] 252 PROCEEDINGS OF THE ACADEMY OF about as convex below as above tbe angle ; suture well denned ; aperture rhomboid suborbicular, more rounded on the inner than the outer side ; outer lip sharp and oblique in outline ; inner lip flattened, or somewhat furrowed below, apparently for the reception of the edge of an operculum ; umbilical region very slightly impressed, but not perforated. Surface ornamented with strong, very regular, transverse lines, most distinct on the upper side of the whorls, where they cross from the suture a little obliquely backwards, with a slight forward curve, to the periphery, over which they cross iu the same oblique direction, and pass on towards tbe umbilical region without any visi- ble curve. Height, 0-41 inch ; breadth, 0-50 inch. This shell may be regarded as the type of a group apparently related to Eolopea and Cyclonema, though it may be distinct from both. In some respects it seems more nearly related to the latter group, but differs from the known species of that genus, in having no traces of revolving lines. From the typical forms of Holopea, it differs in having its volutions much less rounded above, and more prominent or subangular around the middle, and its transverse lines much more distinct. In its surface markings, and general appearance, it very closely resembles Isonema bellatula (Loxonema bellatula,* Hall, Fifteenth Re- port of Regents, pi. 4, fig. 4,) evidently belonging to the same group, but it differs specifically in being much more depressed, or almost subdiscoidal. Judging from some Ohio specimens, apparently identical with Isonnna bd latula, Hall, (sp.,) it seems probable that some species of this group may be slightly umbilicate. Locality and position.— White Sulphur Springs, Delaware County, Ohio, Hamilton division of the Devonian series. Genus PLEUROTOMARIA, Defrance, 1825. Pleurotomaria (Murchisonia ?) META, M. & W. Shell rather small, conical ; spire elevated ; volutions six or seven, rounded, increasing regularly and gradually from the apex ; last one slightly produced below, and forming about one-third of the entire length. Suture deep and well defined, in consequence of the convexity of the whorls. Spiral band flat, smooth, scarcely impressed below the general surface, and placed near the middle of the whorls ; one third as wide as the volutions of the spire. Sur- face without revolving striae, or ridges, but ornamented by small, regular, oblique costae, which in crossing the upper side of the whorls, curve grace- fully backwards as they approach the band, below which they are nearly obsolete and curve forward. Aperture orbicular ; columella apparently per- forated by a very small umbilicus. Length, 0-37 inch; breadth, 0-23 inch; apical angle regular, divergence about 40°. . ' . This species will be distinguished by its produced conical spire, and rounded, gradually enlarging volutions, which characters give it an intermediate appearance between the genera Murchisonia and Pleiirotomaria. In form it is much like Pleurotemaria trilineata, Hall, but it differs from that species in being entirely without revolving markings. Locality and position. --Warsaw, Illinois. Keokuk division of Subcaibomf- erous Series. PTEROPODA. ? Genus CONULARIA, Miller, 1818. CONULARIA MULTICOSTATA, M. & W. Shell with sides equal and tapering to the apex at an angle of about 22£° ; \ * We cannot believe these forms can be properly included in the genus Loxonema, as restricted to such shells as the typical Terebra sinuosa, of Sowerby. [Dec NATURAL SCIENCES OF PHILADELPHIA. 253 furrows at the angles distinct and linear ; sides without a mesial furrow, (fostae exceedingly fine and closely arranged, arching gently towards the aper- ture, and sometimes interrupted or alternating at the middle ; most distant at about 0*80 inch from the apex, where there are 10 or 11 in the space of 0'20 inch, while about 18 occupy the same space near the aperture ; all, as well as the depressions between, very minutely crenate or granulose. Length, l-30 inches ; breadth, 0-80 inch. This species is remarkable for its extremely slender, and closely crowded costae, which are not readily seen at a little distance ; and it is only nnder a good magnifier that the very minute crenulations can be seen. The spaces between the costae are slightly wider than the costae themselves, and apparently marked by minute cross-lines, or crenulations, coincident with those of the costae. Sometimes they appear to be obsolete on the costae, and more distinct in the depressions. It is very distinct from all of the described species known to us. Locality and position. — Richfield, Summit County, Ohio. Waverley Sand- stone, 50 to 60 feet below the Millstone Grit. CoNULARIA SUBCARBONARIA, M. & W. Shell very large, very thin, more or less distinctly and nearly equally four- aided, the sides and angles being somewhat rounded, and converging towards the smaller extremity, at an angle of about 18° ; section quadrangular, mesial furrow along each side very obscure, those at the angles distinct ; aperture subquadrangular, or subrhombic and contracted ; lip very profoundly notched, or divided at the angles, so as to form four triangular flaps or appendages, with inflected lateral margins. Surface ornamented with numerous, slender, transverse costae, which arch slightly towards the aperture in crossing each side, without any interruption or backward curve at the obscure mesial sulcus ; costae regularly crenate, and separated by slightly wider depressions near the middle of the shell, but much more crowded towards the aperture ; depressions between the costae, with very obscure transverse furrows, coinci- dent with the crenatures of the costae. . Length, about 425 inches ; greatest breadth, measuring diagonally across between opposite angles of an obliquely compressed specimen, l-63 inches; greatest breadth of one side, 1-23 inches. Number of costae in the space of 0*20 inch, near the middle of the shell, 10 ; do. near the aperture, about 20. Number of crenatures in the same space on each of the costae, 20. In general appearance, the species of this genus usually present compara- tively little difference, and often they resemble so closely in their ornamenta- tion, as not to be very readily distinguished. Probably the most marked peculiarity of this species is the presence of sharply defined notches in the lip, at the corners, extending down nearly an inch from the margins of the aper- ture, and widening upwards, so as to divide the lip into four subtriangular flaps, which bend a little inwards, so as to contract the aperture, and cause the widest part of the shell to be an inch or more below its upper extremity. Our specimen is not in a condition to show whether these flaps are pointed or truncated at the extremity. This species will be readily distinguished from the last by its coarser, and more widely separated, as well as more coarsely crenate costae, even where the deep notches of its lip cannot be seen. Locality and position. — Keokuk division of the Subcarboniferou3 Series. Warsaw, Illinois. CONULARIA WHITEI, M. & W. Shell of medium size, tapering at an angle of about thirty degrees. Surface ornamented with distinct, linear, transverse, minutely crenate costae, whioh arch upward, or towards the aperiure, in crossing the sides, and either past without interruption, the imaginary mesial line, or more frequently terminate 1865.] 17 254 PROCEEDINGS OF THE ACADEMY OF there, those on opposite sides of this line alternating. Depressions between the costae several times as wide as the costae themselves, but diminishing regularly and gradually in breadth, from tin larger to the smaller extremity of the shell.. Length of a specimen incomplete at the larger end, 2-SO inches ; breadth, (as obliquely flattened by pressure), 1*20 inch. Number of costae near the larger end, in 0-30 inch, 6; do. in same space, 0*75 inch from the smaller extremity, 12. This species presents a marked contrast to the last, in its more widely sepa- rated costae, as well as in having the costae much more finely crenate ; indeed, to the natural eye, they seem to be perfectly smooth. When carefully exam- ined under a magnifier, however, they are seen to be very minutely crenate. Locality and position. — Waver ley Sandstone, Richfield, Summit County. Ohio, 50 to 60 feet below the Millstone Grit. ? Genus TENTACULITES, Schlotheim, 1820. Tentaculites tenuistkiatus, M. & W. Shell attaining a rather large size, gradually tapering, and a little curved : annulations large, prominent, rather obtuse near the smaller end ; separated by rounded constrictions of about 0*10 inch breadth at the larger extremity of a specimen one inch or more in length. Surface marked by numerous, very fine, regular, closely arranged longitudinal stria?, most distinctly marked in the rounded depressions between the annulations. Aperture circular. Length, 1*16 inches ; breadth at the aperture, measuring upon one of the rings, 0-25 inch ; do. between the rings, 0*19 inch ; space occupied by four rings and the three intervening spaces at the larger end, 0*30 inch ; while the same space includes six rings at the smaller end. This species resembles rather closely the enlarged figure of a form from the same horizon, referred by Prof. Hall to his T. flexuosa, (pi. 78 fig. 26, Palaeont. N. Y. Vol. 1.) ; but its annulations are sharper, and its longitudinal stria? more crowded ; while the natural size #of the New York species is much smaller. Dr. Shumardhas also described, under the name T. incurvus, (Missouri Re- port, p. 195,) a similar form, though bis species is much smaller, with more crowded rings, while it also differs in having minute annular striae. Locality and position. — Cincinnati Group of Lower Silurian Series. Alex- ander County, Illinois. Tentaculites Oswegoensis, M. & W. Shell attaining a rather large size, very gradually tapering to an acute point, distinctly arched, particularly towards the smaller extremity ; section circu- lar ; annulations rather prominent, somewhat obtuse, from three to three and a half in a space equalling the transverse diameter, diminishing very regular- ly in size, and in their distance apart, from the larger to the smaller extremity. Surface without longitudinal or (visible) transverse stria?. Length, 1*45 inches; greatest transverse diameter, 0-16 inch; space occu- pied by six annulations, and five of the intermediate constrictions, at the larger end, 0-35 inch. This species has much the general appearance of curved individuals of 7". etongatus, Hall, from the Lower Helderburg Group, (Upper Silurian) of New York, but is decidedly more strongly arched, proportionally more slender, and has more closely arranged annulations, while it shows no traces of the annn- lar"l8trise seen on the N. Y. species. • From our T. tenuistriatus, described on the preceding page, it will be dis- tinguished by its more slender form, more closely arranged rings, and the ab- sence of longitudinal striae. The last mentioned character, and its much [Dee NATURAL SCIENCES OF PHILADELPHIA. 255 larger size, will also distinguish it from T. incurvus, of Shumard, (Missouri Report, pi. B, fig. 6a, b.) Locality and position. Cincinnati Group, of Lower Silurian ; Oswego, Ken- dall Co., Ill » Tentaculites Sterlingensis, M. & W. Comp. T.flexuosus, Hall. Palaeont. N. Y., i. p. 2S4, (not ib, 92.) Shell small, slightly arched, and gradually tapering to a point ; section cir- cular ; annulations prominent, angular, rising abruptly from the surface, usu- ally about their own breadth apart ; constrictions between the annulations with fine, sharply elevated, longitudinal striae, which are not continued upon the rings. Lengtu, 056 inch ; breadth at the larger end, 0-08 inch ; annulations live in the space of £ of an inch at the larger end, and nine or ten in the same 6pace at the smaller end. Longitudinal striae, five in the space of 0*02 inch. It is not improbable that this will prove to be the form from the so-called Hudson River group, referred by Prof. Hall to his T. Jlexuosus, in vol. i. p. 284, Palaeont. N. Y. As that specific name, however, was founded upon a Trenton fossil, described as being septate, and having nine rings in £ of an inch, (being,«as is now supposed, the column of a Cystidian), the name /eiu- osus could not be properly applied to this form, even if identical with the New York species from the higher position. It will be distinguished from T. incurvus, of Shumard, from the Cape Girar- deau Limestone, which it resembles in size and form, by having its annula- lations arranged about their own breadth, instead of twice that distance apart, as well as in having the longitudinal stria? only defined between the rings, instead of also upon them. It seems to be very closely allied to T. distans, Hall, of the Clinton Group, but differs in being curved instead of straight, as well as in being less rapidly expanding towards the larger end. From the last of the two foregoing species it will be readily distinguished by its much smaller size, more sharply elevated rings, and distinct longitudi- nal striae. Locality and position. Sterling, Illinois. Cincinnati Group, of the Lower Silurian series. CEPHALOPODA. Genus ORTHOCERAS, Auct. Orthoceras crebristkiatum, M. & W. Shell attaining a medium size, rather rapidly tapering, compressed, (in part probably due to accidental pressure) ; section ellipitical ; septa transverse, rather deeply concave, distant less than one-third the greater diameter of the shell at the point of measurement ; siphon apparently subcentral. Surface ornamented with numerous, closely and very regularly arranged, equal, thread- like annular striae, of the same breadth as the depressions between, and dif- fering but slightly in size throughout the entire length of the shell. Length of the typical specimen (which is partly septate and imperfect at both extremities), 12*50 inches ; greater diameter at the larger end, 4*20 inches ; smaller do. of same, 2-56 inches. Greater diameter of the smaller end, about 2-13 inches ; smaller do. of same, l'OS inches. Angle of divergence, measuring along the narrower sides, 11°. Annular striae, 8 in 0*20 inch at the larger end, and 9 or 10 in the same space at the smaller end. The most marked character of this species is its very regularly arranged, equal striae, which seem to pass almost, if not quite, directly around the shell. They appear to be simple, uninterrupted and everywhere arranged their own breadth apart. It diners from O. Lqphami, from the same rock, in its much 1865.] 256 PROCEEDINGS OF THE ACADEMY OP more rapid expansion from the smaller to the larger extremity, and in its com- pressed instead of cylindrical form, as well as in having its striae passing di- rectly around, instead of obliquely. Locality and jposition. Joliet, Illinois ; Niagara Group, of Upper Silurian series. ORTHOCERAS SlTBBACtJLDM, M. & W. Shell attaining a moderately large size, slender and gradually tapering ; entire length, as inferred from the convergence of the sides towards the small- er extremity, about thirty inches ; section elliptical, the smaller diameter be- ing to the larger as about 17 to 24. Length of specimen, imperfect at both extremities, 18 inches, of which the outer or body chamber occupies a length of 7"50 inches, while twelve of the smaller chambers occupy the remaining 10-50 inches ; greater diameter at larger end, 3*23 inches ; smaller do. of same about 2*10 inches ; greater diameter at smaller end, 1*90 inches ; smaller do. of same, 1*45 inches. Septa transverse, rather deeply concave, separated by chambers, two and a half of which equal the greater diameter of the shell at the point of measurement. Surface and siphon unknown. At a first glance this species looks much like 0. Bigsbyi, Stokes, [= Ormo- ceras tenuifilum, Hall], from the Trenton and Black River Limestones, but on a closer inspection it is found to be more compressed and more gradually ta- pering, while its septa are considerably more distant, and show no backward curve on either side. Locality and position. Joliet, Illinois. Niagara division of Upper Silurian series. Orthoceras Jolietense, M. & W. Shell much elongated, very gradually tapering ; section oval or narrow el- liptic, (probably to some extent, at least, due to accidental pressure) ; septa very concave, unusually distant or separated by spaces, equalling three-fourths the greater diameter of the shell at the point of measurement. Siphon and surface unknown. Length of a septate specimen, imperfect at both extremities, 14*50 inches ; greater diameter of do. at larger end, 2-75 inches ; smaller do. of same, 1*77 inches; greater diameter at smaller end, 2-16 inches; smaller do. of same, 1*30 inches. Number of septa in the entire 14J inches, 8. This species is remarkable for its very gradually tapering form, and unusu- ally distant septa. The latter character will alone distinguish it from any Upper Silurian species known to us, excepting 0. pauciseptum, Hall, from the Shaly Limestone, of the Lower Heldeburg Group. From this New York species, to which it seems to be nearly related, it will be distinguished by its com- pressed, instead of cylindrical form. It is true this compression may be in some degree due to accidental pressure, but it seems to be too regular along the entire length of the shell not to be mainly the natural form. Locality and position. Joliet, Illinois. Niagara division of the Upper Silu- rian series. Orthoceras nobile, M. & W. Shell attaining a very large size, rather rapildy tapering ; section subcircu- lar, or very slightly flattened on one side. Septa deeply concave, extremely thin, distant about one-fifth the diameter of the shell at the point of measure- ment; siphon central, round. Surface unknown. Entire length of a septate specimen incomplete at both ends, 18 inches ; great- est diameter at larger end, 8| inches ; smaller do. of same, 7 inches. Greatest diameter at smaller end, 5 inches : angle of divergence about 14° ; diameter of siphon at larger end, 0*80 inch. The entire length of the shell was pro- bably not less than five feet, and its body chamber, owing to the large size and rapid expansion of the shell, must have been very capacious. [Dec. NATURAL SCIENCES OF PHILADELPHIA. 257 In form and proportions this large species seems to agree nearly with 0. Munsterianum, of Koninck, from the carboniferous rocks of Vise, Tournay, but it attains a greatly larger size, and also differs in having its siphon central. It is probably the largest species known in our carboniferous rocks. Locality and position. Randolph County, Illinois. Chester division of Sub- carboniferous Series. Orthoceras Winchellii, M. & W. Shell rather rapidly tapering ; section nearly circular, its greater and small- er diameter being as 10b' to 100 ; septa moderately concave, not oblique, dis- tant one -fifth the greater diameter of the shell at the point of measurement, and showing a gentle backward curve in crossing the dorsal and ventral sides ; siphon very small at the points where it passes through the septa (probably swollen or beaded between), placed on the shorter axis of the septa only about its own breadth from the margin. Surface nearly smooth, or with more ob- scure lines of growth, which, like the margins of the septa, make a slight backward curve in crossing the dorsal and ventral sides. Length of an entirely septate specimen, imperfect at both extremities, 3 inches ; greater diameter at the larger end, 1*50 inches ; apical angle 15°, ap- parently becoming greater towards the smaller end. This species seems to be somewhat similar to 0. occidentale, of Prof. Win- chell, from his Marshall Group (Am. Journ. Sci. vol. xxxiii. 18t>2, 356), but differs in being more rapidly tapering, and in having its siphon nearly margi- nal, instead of placed midway between the centre and margin of the septa. If much swollen between the septa, its siphon must be indeed quite marginal at these joints. Named in honor of Prof. A. Winchell, State Geologist of Michigan. Locality and position. White Sulphur Springs, Delaware County, Ohio. Hamilton Group. Devonian. Genus PHRAGMOCERAS, Broderip, 1834. Phragmoceras Walshii, M. & W. Shell very large, clavato-sublunate in form, moderately arched, increasing rather rapidly in size from the smaller end to near the middle, and thence ap- parently somewhat tapering towards the aperture ; more or less compressed. Outer or body chamber apparently rather short. Septa very oblique, (proba- bly to some extent due to compression and distortion), comparatively closely arranged, the chambers between scarcely equalling one-sixth the greater di- ameter of the shell at the widest part, and one-eighth towards the smaller end. (Siphon, surface and aperture unknown). Length of specimen, (imperfect at both extremities), measuring alon°- the middle of the side parallel to the curve, about 15 inches ; greatest breadth near the middle, 5 inches; smaller do. at same place, 3-50 inches. Greater breadth at smaller end, 240 inches. Of the whole length of the specimen 22 of the smaller chambers form 10 inches, and the remaining portion of the body chamber the other five inches. The only specimen of this large shell we have seen is very imperfect, and much distorted, so that it is qnite probable some of the characters given in the above description, will require more or less correction when good speci- mens can be obtained. Its large size, general form, and rather closely arranged septa, however, will probably render its identification not very difficult. The specific name is given in honor of B. D. Walsh, the well known Ento- mologist, of Rock Island, 111. Locality and position. Rock Island, Illinois. Hamilton division of the Devonian. 1865.] 258 PROCEEDINGS OF THE ACADEMY OP Genus GOMPHOCERAS, Sowerby, 1839. GOMPHOCERAS SACCULUM, M. & W. Shell *mall, subfusiform, or clavate, very slightly arched ; a little com- pressed at right angles to the plane of the curve, particularly the nonseptate part, which is more convex on the outer side of the curve than the inner; most ventricose a little above the last septum, thence tapering gradually to the lower extremity and towards the aperture, near which latter there is a slight constriction. Section transversely a little oval near the middle of the shell, and more decidedly so above, but nearly or 'quite circular towards the lower extremity. Aperture transversely oval, its smaller diameter being about two-thirds the greater ; lips faintly sinuous at each end of the aperture, and at the middle of the dorsal side. Septa but slightly concave ; (distance between them not distinctly determinable from the specimen examined). Siphon very small ; placed on the line of the shorter axis of the septa, about twice its own breadth from the dorsal or outer side of the curve. Surface marked only with small annular strise, slightly arched backwards near each end of the aperture, parallel to the faint sinuosities of the lip. Length of specimen, imperfect at the smaller extremity, 127 inch ; do. of nonseptate part, OG7 inch ; greatest transverse diameter of do., 053 inch ; shorter diameter of do. at same part, 0-42 inch. Apical angle of septate half of the shell, measuring along each lateral margin, 24p. Breadth of aperture, 0*33 inch ; smaller diameter of do., 0-22 inch. This little shell has the general habit and appearance of Gomphoccras, and yet differs from the typical forms of that genus in being slightly arched and not having its aperture so remarkably contracted. In being a little curved, it more nearly resembles Phragmoceras, though its curvature is less decided. It is also worthy of note, that the comparatively small contraction of its aperture is mainly on dorsal and ventral margins, while in Gomphoceras and Phragmoceras the contraction is mainly on each lateral margin. In several respects it approaches Oncoceras, Hall, and it is even possible that we would be more nearly correct if we were to call it Oncoceras sacculum. Still it differs from the type of that group in beiug less curved, and compressed dorso-ven- trally, instead of laterally, as well as in having its siphon not quite, though nearly marginal. Locality and position. — White Sulphur Springs, Delaware County, Ohio. Hamilton Group of Devonian Series. Gomphoceras (Apioceras) turbiniforme, M. & W. Shell rather small, turbinate, or obovate, very slightly unsymmetrical ; sec- tidn circular, or nearly so ; chambered part rapidly expanding, with sides slightly convex above. Non-septate part very short, or three times as wide as long, rounding in abruptly above ; aperture contracted, but exact form unknown. Septa only moderately concave, nearly equidistant at all points, excepting near the outer chamber and the apex, where they are more crowded ; at about the widest part of the shell, separated by spaces equalling one-eighth its greatest diameter. Siphon small and marginal. Surface nearly smooth, or with only fine lines of growth. Length of a specimen not quite complete at the smaller extremity, 1*16 inch. Greater breadth (at the junction of the septate and non-septate parts), 1 inch ; smaller diameter at the same place, 0-90 inch. Greater diameter at the smaller extremity, 0-32 inch ; smaller do. at same place, 0'30 inch. Di- vergence of apical angle, 30°. This is a very short turbinate species, somewhat like G. beta, Hall, (18th Report Regents, pi. 7, fig. 1), but diners in being proportionally shorter and more ventricose, and in having the septa proportionally more crowded. It shows eleven septa in a space of three-quarters of an inch below the last one, while G. beta is described as having only seven or eight in the same space. [Dec, NATURAL SCIENCES OF PHILADELPHIA. 259 Its last three septa are crowded within a space only equalling one of the uhambers below. Locality and position. — Charleston, Indiana. Devonian. Genus NAUTILUS, Linnaeus, 1758. Subgenus ENDOLOBUS, M. & W. Nautilus (Endolobus) teramplus, M. &. W. Shell attaining a very large size, compressed subglobose ; umbilicus rather deep, about as wide as the dorso-ventral diameter of the outer volution, and showing about three-fourths of each inner turn. Whorls three to three and* a half, increasing rather rapidly in size, broadly rounded. over the dorsal or outer side, and more narrowly round on each lateral margin, where tlie greatest prominence is a little within the middle ; lateral margins each pro- vided with a row of large, broad, depressed, orsubuodose prominences, about fourteen of which may be counted on each side of the last turn ; from these rows of nodes or mammillary protuberances, the inner side of each whorl rounds abruptly into the umbilicus, and is provided along the middle with a moderately deep, rounded concavity for the reception of each succeeding inner turn. Septa deeply concave on the side facing the aperture ; separated by intervals, measuring, on the dorsal side, more than one third the dorso-ven- tral diameter of the whorls at the point of measurement, passing nearly straight over the broad periphery, and with a very slight forward curve across the sides ; while on the inner concave side they are each deflected abruptly backwards, so as to form a deep, more or less funnel-shaped ventral lobe. Si- phon placed rather more than its own breadth nearer the inner than outer side. Surface of cast smooth. Greatest diameter, 20 inches ; transverse diameter, 12 inches ; dorso-ven- tral diameter of inner whorl, 8 inches; breadth of umbilicus, 8 50 inches ; circumference around the periphery, 4 feet 8 inches. We know of no shell with which this fine species is liable to be confounded, though it has mu'li the form and general appearance of our N. spectabilis, from the same position. It differs, however, in the position of the lobe on the inner side of septa ; and in having its siphon located farther in from the outer side. In a side view it presents some general resemblance to N. tubcrcufatus, of Sowerby, as figured by Phillip, in his Geol. Yorkshirei i. pi. 22, fig. 29, though even as thus seen, it will be observed to differ in its broader whorls, and in having the most prominent part of their sides, with their nodes, placed nearer the umbilicus, while in a profile view, it will be distinguished at a glance by its periphery being rounded, instead of nearly flat. As may be seen by the foregoing description, this species differs from tjie typical Nautili, in the. possession of a peculiar funnel-shaped ventral lobe, formed by the backward flexure of the septa. Hence it seems to bear almost exactly the relations to Nautilus that the genus Tretoceras does to Orthoceras ; ' hence we regard it as the type of a group for which we propose the name Endolobus. If Montfort's name, Bisiphites, is to be retained, the name of this shell should doubtless be Bisiphites peramplus, as the type upon which he pro- posed to found a genus under that name, seems to have had an inner lobe which he mistook for a second siphon. As his name, however, implies a plain contradiction of fact, we think it should not be used. Judging from Montfort's figure, his type not only differs from ours, in having the outer whorl enveloping all the others, so as to leave no open umbilicus, but in having the lobe of the septa a little removed from the inner side, in- stead of being directly in contact with it, as in our shell. He says his type was a large fossil species, attaining a diameter of two feet. Locality and position. —Randolph County, Illinois. Chester division of Subcarboniferous Series. 1865.] 260 PROCEEDINGS OF THE ACADEMY OF Nautilus (Temnocheilus) Niotensis, M. & W. Shell attaining a large size, globose-subdiscoidal ; umbilicus deep, and (con- sidering the lateral margins of the whorls its limits) about twice the dorso- ventral breadth of the outer turn. Volutions about three, contiguous but not embracing, broadly rounded over the dorsal and ventral sides, and promi- nently angular around the middle of each lateral margin ; section trans- versely elliptic, the two extremities of the ellipse being angular. Septa rather distinctly concave, and distant on the outer side less than half the dorso- ventral diameter of the whorls at the point of measurement, — making a broad backward curve in crossing the inner and outer sides of the whorls, and curving forward to each of the lateral angles ; siphon piercing the septa less than its own breadth outside of the middle. (Surface and aperture unknown1). Greatest diameter, measuring across the disk, about 8*50 inches ; convexity, or transverse diameter of the whorls, 5 inches ; dorso-ventral diameter of the last volution, about 3 inches. This species belongs to a group of carboniferous Nautili, including N. coro- natus, McCoy, and N. bianyulatu'', N. multicarinatus and N. cariniferous, Sow- erby, &c. These shells are characterized by having a broad, deep, open umbilicus, showing all the volutions, with the outer side of the whorls broadly rounded or flattened, and the middle of each lateral margin prominently angu- lar ; the angle being sometimes nodose, while the transverse diameter of the volutions is always greater than the dorso-ventral. The siphon in these ehells is generally, 'or perhaps always, between the middle and outer side of the whorls. Although Prof. McCoy included a much wider range of forms in his group Temnocheilus, we think it would be better to restrict it to such species as those mentioned above, all of which were originally included in the group by Prof. McCoy. Specifically, our shell is perhaps most nearly allied to Nautilus cariniftrous, of Sowerby, (Min. con. pi. 482, f. 3 and 4) though differing in its proportion- ally wider umbilicus, merely contiguous volutions, and particularly in never having longitudinal ridges on the outer side of the whorls, at any stages of growth. It also differs in having its septa crossing the outer side of the whorls with a broad backward curve, instead of passing nearly straight over. Locality and position. — Niota and Warsaw, Illinois. Keokuk Division of Subcarboniferous Series. Subgenus DISCITES, McCoy, 1844. Nautilus (Discites) oknatus, Hall. Var. amplds, M. & W. The shell we here place provisionally as a variety of Nautilus (Discites) ornatus, Hall, agrees very nearly in most of its characters with that species, but differs in its much larger size, and the proportionally greater dorso-ven- tral diameter of its volutions, (particularly the outer one), as compared with the breadth of its truncated periphery. In the New York form, these propor- tions, according to the published figure, (Thirteenth Regents Report, 1860, p. 102), are about as two and one-third to- one, in-the outer whorl, and nearly equal in the inner turns ; while in our shell they bear the proportions of three to one, the flattened sides of the outer volution being three times as wide as its truncated periphery. The type of the New York species is also described a9 having its " siphuucle dorsal." If by this it is meant that the siphon is in contact with the outer side of the shell, as in the Goniatites, then there can be little doubt in regard to the form under consideration being a distinct species, since its siphou is separated from the periphery by a space about equalling its own breadth. It is probably distinct from the New York species, but as individuals of these older types of Nautilida: seem to have varied more [Dee. NATURAL SCIENCES OP PHILADELPHIA. 261 in form than those of more modern date, we have concluded to place it for the present, as a variety of N. ornatus. To facilitate compxrison, we would remark that our shell, when entire, must have measured from 10 to 12 inches in its greatest diameter across the disc ; while its outer whorl measures about 5 inches in thickness or convexity at the umbilical side, and 1-50 inches at the periphery. The greatest breadth of the sides of the outer turn is about 4*50 inches. Its septa, as seen on each side, are arranged and curved very nearly as in the typical form of N. ornatus, and are deflected, backwards on the truncated periphery, so as to form a sub- trigonal lobe as deep as wide ; they also make a rather broad, deep, back- ward curve on the inner side- Surface markings unknown. The shells of this type seem to be very distinct from the typical recent forms of Nautilus, and whatever others may think, should, as we believe, be at least regarded as forming a marked subgeneric group. Objections have been raised to the use of McCoy's name, Discites, however, because De Haan had used it in 1825 for a type of Nautilidas ; but as De Haan merely used it in a kind of synoptical table, with no other characters than " Sensim incrq/satis," without a figure, or any allusion to any type by which the most remote con- jecture can be formed iu regard to what group of Nautilidae he meant, it must be evident we cannot regard him as having established either a genus or a subgenus, and the name was consequently free to be used by any other author. Locality and position. — Hamilton Group (Devonian) ; " Devil's Bake-oven, " Jackson County, Illinois. Nautilus (Discites) discifoiuii-, M. & W. Shell attaining a rather large size, discoid, much compressed ; umbilicus shallow, a little wider than the dorso-ventral diameter of the outer volution, and showing all the inner turns. Whorls about three and a half, nearly con- tiguous, or very slightly embracing, nearly flat on each side, the greatest con- vexity being about half way between the middle and the inner side, from which point the sides round into the umbilicus, and converge to the periphery, which is truncated, narrow and concave. Septa rather closely arranged, crossing the sides of the whorls with a broad, graceful backward curve and more abruptly flexed in the same direction on the truncated periphery, so as to form a subtrigonal lobe about as deep as wide ; also, somewhat curved backwards on the inner side of the whorls. Last chamber' long, or forming about half the outer volution ; others shallow, or usually about equalling one- fifth the dorso-ventral diameter of the volutions at the point of measurement. Siphon small, suboval, located about its own diameter outside of the middle of the whorls. Aperture and section strongly compressed, subovate, the inner side being rounded, and the outer, which is much narrower, truncated, somewhat emarginate, and biangular. (Surface unknown.) Greatest diameter across the disc, SJ to 9 inches ; dorso-ventral diameter of outer whorl nearly 3 inches; greatest convexity of whorls, about 1-50 inches ; breadth of truncated periphery, 0*68 inch. In size, form, proportions, breadth of umbilicus, &c, as well as in the arrangement aud curvature of its septa, this species seems to agree almost exactly with the discus of Sowerby. If that species has been correctly figured and described, however, our shell presents the important difference of having its siphon located a little outside of the middle, instead of near the inner margin of the whorls. Locality and position. — Niota, Hancock County, Illinois. Keokuk Division of Subca'bouiferous Series. Nautilus Lasallensis, M. & W. attaining a m is more than I860] Shell attaining a medium size, compressed, subglobose, or subdiscoidal ; umbilicus more than half as wide as the dorso-ventral diameter of the last 262 PROCEEDINGS OF THE ACADEMY OP whorl at the aperture, moderately deep, and showing ahout half of each inner turn. Volutions increasing rather gradually in size, very slightly compressed on the dorsal an 1 lateral surfaces, but wiihout the compression imparting any angularity to the dorsolateral and ventral margins, which are rounded ; each concave within for the reception of the inner turns. Septa moderately con- cave, separated by spaces measuring, on trie dorsal or outer side, less than one- third the dorso-ventral diameter of the whorls at the point of measurement, all crossing the sides and dorsum with a b oad backward curve. Siphon scarcely more than its own breadth from the ventral or inner side. Aperture, judging from the section of the whorls, about as wide transversely as its diam- eter, in the direction of the plane of the shell, subquadrilateral, or approach- ing subreniform, in consequence of the sinuosity of the inner side. Suiface unknown. Greatest diameter about 4-70 inches ; convexity about 2-75 inches ; breadth of umbilicus, l-45 inches. Locality and position. — Upper Coal Measures, Lasalle, Illinois. Subgenus CRYPTOCERAS, d'Orbigny, 1847. Nautilus (CitYrTOCERAs) cafax, M. & W. Shell attaining a moderately large size, subglobose in form. Umbilicus deep, with abruptly sloping walls, — one third as wide as the dorso ventral diameter of the outer whorl, and showing each of the inner turns. Whorls about two and a half, increasing rapidly in size, particularly in breadth ; last one so expanded laterally as to be apparently one third to one half wider than its dorso-ventral diameter ; inner ones proportionally narrower. All broadly rounded on the outer side, and more narrowly rounded with a flattened or slightly concave revolving space between the lidge bounding the umbilicus and the middle of each side ; each provided with a narrow, shallow impres- sion along the ventral side for the reception of the inner volutions. Septa separated by spaces which measure, on the outer side, less than one fourth the dorso-ventral diameter of the volution at the point of measurement ; a little arched backwards on the slightly concave inner side of the whorls, and less distinctly so on the narrow revolving flattened space just outside of the umbilicus, after which they cross over the broadly rounded outer side, with a very broad, scarcely perceptible backward curve. Aperture transversely oval, or subelliptic. Outer chamber very capacious, composing less than half of a volution. (Surface unknown). Greatest diameter across the disc, about 7 inches ; breadth (transverse di- ameter of the aperture), 6 inches ; dorso-ventral diameter 3-25 inches ; breadth of umbilicus 1 inch. The only specimen of this species we have seen is a cast, which shows, along the outer side of the whorls, the appearance of a tube 0'20 inch in di- ameter, extending backwards from each teptem. It is barely possible that this may be a small lobe, but we have scarcely any doubts in regard to its being the siphon, and hence that the species belongs to the group Cryp- toceras. Compared with N. dorsalis, Phillips (Geol. Yorks, ii. pi. xviii. fig. 1 and 2), the type of the group Cryptoceras, our shell will be found to differ in its much more broadly rounded dorsum, and much wider mouth, as well as in the pecu- liar revolving flattened space near the umbilical side of the whorls, which im- parts a slight angularity to the margin of the umbilicus, as well as an unde- fined longitudinal ridge, or prominence near the middle of the whorls on each side. Locality and position. — Charboniere, Missouri. Coal Measures. Nautilus (Cryptoceras ?) Leidyi, M. & W. We only know this shell from the non-septate portion, — forming about one [Dec. NATURAL SCIENCES OF PHILADELPHIA. 263 third of a volution. It indicates a subglobose form for the entire shell, and shows that the umbilicus was deep, with rather abrupt walls, and about as broad as three fourths the do; so-ventral diameter of the body whorl at the aperture. From the curve, and rapid increase in size of the outer chamber, it is evident there could not have been more than two and a half volution9, which are rather broadly rounded over the dorsum and sides, to the margins of the umbilicus, into which the sides round rather abruptly. Towards the aperture, the steep, somewhat flattened inner side of the volution forming the walls of the umbilicus, meets the lateral margins, so as to form a pinched out prominence, that must have imparted a p-culiar angularity to the inner mar- gin of the aperture on each side. Just outside of this prominence, the ventro- lateral sides of the outer whorl at the aperture are a little flattened. The aperture is one-fourth wider than its dorso-ventral diameter, and forms about three-fourths of a circle, being deeply rounded on the dorsal side, much flat- tened within, and angular or apparently abruptly sinuous at each inner lateral margin. These angles at the inner lateral margins, seem even to have pro- jected out somewhat, as in the recent Argonauta gondola, of Adams, though not to the same extent. The lip is rather deeply sinuous at the middle of the dorsal side. The septa were moderately concave, and slightly arched back- wards on each side. (Siphon and surface unknown). Greatest diameter of the shell, about 3 75 inches ; greatest breadth (at the inner side of aperture), 2.65 inches. As we have not seen the siphon of this species, we are not sure that it be- longs to the group Cnjptoceras, but from its analogy to the species just de- scribed under the name capax, which shows apparently a dorsal siphon, we are led to infer that it probably possesses the same character. It differs from that shell, however, in having its body whorl less rapidly expanding, and without a depression along the inner side forthe reception of the inner whorls. Named in honor of Prof. Joseph Leidy, of Philadelphia, Pa. Locality and position.— Warsaw, Illinois. Keokuk division of the Subcar- boniferous Series. Genus TROCHOCERAS, Barrande, 1847. Trochoceras ? Baeri, M. & W. Shell subdiscoidal, consisting of about two or three rather rapidly enlarging volutions, which are more broadly rounded ou the outer surface than on each side, and about one-fourth wider transversely than their dorso-ventral diame- ter ; each inner whorl slightly impressing the inner side of the succeeding turn. Umbilicus a little more than half the dorso-ventral diameter of the outer volution, and showing all the inner volutions. Spire apparently scarcely rising above the upper surface of the last turn. Septa rather distinctly con- cave on the side facing the aperture, separated on the outer side of the whorls, at a point where the dorso-lateral diameter is about 1*25 inches, by spaces measuring 0-35 inches — all showing a very slight backward jurve on the rounded periphery, and passing nearly straight across each side. Surface, siphon, and non-septate portion of the shell unknown. Greatest breadth of the septate part of the shell, 5 inches ; height, (estima- ted) about 2-50 inches. Dorso-ventral diameter of the volutions, increasing about three-fold each turn. The specimen from which this description was drawn up is defective on one side, so that it is not easy to determine whether or not its whorls are coiled in the same plane, though they have the appearance of being somewhat oblique, and hence we have placed it provisionally in the genus Trochoceras. Should it be found, however, when more nearly entire specimens can be ex- amined, that its whorls are coiled all upon the same plane, it would belong either to the genus Lituites or Nautilus, and hence its name would becoma Lituites Baeri, or Nautilus Baeri. 1865.1 264 PROCEEDINGS OE THE ACADEMY OF The typical specimen does not show the position of the siphon, hut a frag- ment found near the same locality, and at the same horizon, apparently of this species, though possibly belonging to another shell, lias the siphon placed about its own breadth outside of the centre. It pierces the septa from with- out inwards or backwards, as in Nautilus. At a first glance this shell would seem to resemble Cryptoceras (Lituite.s) undatus, as represented by fig. 3, pi. 13, vol. i. Pah-eontology of New York, but on a closer inspection, it will be at once seen to differ materially in the more rapid increase in the breadth of its whorls, and in the proportionally smaller size and greater depth of its umbilicus, as well as in being apparently not coiled on a plane. The specific name is given in honor of Dr. 0. P. Baer, of Richmond, Indi- ana, to whom we are indebted for the use of the typical specimen. Locality and position.— Richmond, Indiana. From the Cincinnati Group of the Lower Silurian Series. ARTICULATA. CRUSTACEA. TRILOBITA. Genus DALMANIA, Emmerich, 1845. Dalmania DanjE, M. & W. Attaining a large size, entire outline ovate, approaching subelliptic. Ce- phalic shield rather compressed, nearly semicircular, about twice as wide as long, rounded in front, and nearly straight or slightly concave in outline be- hind, with posterior lateral angles produced into mucronate spines extend- ing backwards to the fourth thoracic segment. Glabella composing rather more than one-third the entire area of the shield, but slightly more convex than the cheeks ; including the neck segment, as long as its greatest anterior breadth, and about twice as wide in front as behind ; separated from the cheeks on each side by a well defined furrow ; anterior lobe composing about half its entire area., transversely elliptical, and a little less than twice as wide as long ; lateral furrows well defined, anterior one oblique ; the other two transverse, and not always strongly defined quite out to the lateral margins ; anterior lateral lobe longer, more oblique, and at its outer end wider, than either of the other two. Occipital segment widest and most prominent in the middle, scarcely equalling the transverse diameter of the posterior extremity of the glabella ; neck furrow well defined, but deepest on each side, and arch- ing a little forward in the middle ; its continuations across the posterior sides of the cheeks broad, deep, and straighter than the posterior margin, — extending nearly to the lateral margins of the cheeks, where they curve a little back- wards. Cheeks sloping slightly around the outer side, to a broad, shallow, undefined marginal depression, outside of which there is a moderately thick, somewhat rfcunded border, which does not extend entirely around the front of the glabella, but continues back into the posterior lateral spine. Eyes reniform, not oblique, nearly half as long as the antero-posterior diameter of the front lobe of the glabella, and situated slightly more than their own length in advance of the posterior margin of the cheeks ; with (in casts) a moderately distinct marginal furrow around their outer bases, (height and other details unknown) ; palpebral lobes semicircular and depressed. Facial sutures cut- ting the lateral margins of the cheeks nearly opposite the posterior extremities of the eyes, and passiug around the antero-lateral and front margins of the glabella, so near the anterior border as scarcely to leave any perceptible band connecting the movable cheeks around the front. Hypostoma obscurely subtrigonal, about one-eighth wider posteriorly than its length, moderately convex ; anterior margin forming a broad, regular con- [Dec. NATURAL SCIENCES OF PHILADELPHIA. 265 vex curve ; lateral margins contracted behind the anterior lateral angles, and converging a little posteriorly, for about two-thirds the entire length, thence more abruptly to the posterior extremity, which is transversely truncated, and provided on each side with a minute, slightly projecting point ; while still farther forward on each lateral margin, there appears to be traces of another minute slightly projecting irregularity of outline. Around the anterior and lateral margins, there is a more or less distinct sulcus, behind which the pos- terior margin is flattened. Within this marginal sulcus there is, on each side a little behind the middle, au oblique eye-like depression. Thorax wider than long, the length being to the breadth, as 21 to 28, near- ly once and a half as long as the cephalic shield ; mesial lobe as wide anteriorly as the posterior extremity of the glabella, and very slightly broader near the middle, where it is about three-fourths as wide as the lateral lobes, from which it is only separated by narrow, rather shallow furrows — most convex along the middle and flattened on each side ; segments not clearly seen in the specimens examined. Lateral lobes somewhat more depressed than the mesial one, and sloping very gradually to the lateral margins. Segments equalling the antero-posterior diameter of the posterior lateral lobes of the glabella ; each curving abruptly backwards at the outer extremity, and terminating in a flat, sharply pointed, or lanceolate projection, most produced in the posterior ones ; provided with a deep, well defined, longitudinal furrow, which starts from the anterior side of the inner end, and passes at first a little obliquely outwards, and then straight outward, slightly nearer the posterior than the anterior margin, to the middle of the flattened scythe- shaped outer ends, where they usually curve a little backwards and become obsolete. Pygidium nearly semielliptic, or subtrigonal, the anterior lateral angles be- ing rounded, and the lateral margins converging to the more or less pointed posterior extremity, with a broad convex curv.e ; slightly longer than the ce- phalic shield, and rather more than two-thirds as wide ; mesial lobe somewhat more convex than, and two-thirds as wide as the lateral lobes, gently rounded, and tapering gradually to the posterior extremity, where it is apparently con- tinued into an abruptly projecting caudal appendage ; segments 12 to 13, straight well' defined (excepting near the termination) by distinct furrows, which are deeper on each side than at the middle. Lateral lobes with eight or nine well defined arched segments, which become more oblique posteriorly, and are defined to near the edge of the smooth margin ; each divided by a furrow deeper than those between, and like those of the thoracic ribs, the anterior division being slightly shorter than the other. Surface (of cast) smooth, excepting traces of small, scattering tubercles on the anterior lobe of 'he glabella. Entire length of the largest specimen seen (exclusive of the little caudal ap- pendage, the length of which is unknown), 4*93 inches. Length of pygidium, 1-43 inches ; breadth of do. 2 inches ; breadth of its axillary lobe, 0*57 inch. Length of thorax, 2-10 inches; breadth of do. 2-83 inches; breadth of its mesial lobe, 080 inch. Length of cephalic shield, 1-40 inches; breadth of do. 3 inches ; length of posterior lateral spines, near 0-95 inch ; length of glabella exclusive of neck segment, 1-30 inches ; anterior breadth of same, 1-35 inches ; posterior breadth of do. 0*84 inch. Length of eyes,0 '39 inch; distance of same from posterior margin of cheeks, 0 42 inch. Named in honor of Prof. James D. Dana, of New Haven. We have described this fine species in as much detail as possible, because it is somewhat nearly allied to several of the already described species. Per- haps it is most nearly allied to the well known European D. caudata of Bru- nich, with which it agrees in size, form aud many of its details. In the first place, it differs, however, from that species in having the anterior margin of its cephalic shield decidedly more rounded than even the variety or form re- garded by Mr. Salter as the female, while it shows no marginal rim (as seen from above) extending around the front of the glabella. Again, the eyes, in- 1865.] 266 PROCEEDINGS OF THE ACADEMY OF stead of being placed about half tbeir own length in advance of the posterior margin of the buckler, are rather more than their entire length from the pos- terior margin. The produced spine-like appendages of its cheeks are also, in all our specimens, uniformly distinctly smaller, and only extend back to about the termination of the fourth thoracic segment, instead of to the sixth, as in D. caudata. On comparing the hypostoma of our species with Mr. Sal- ter's excellent figures of that of Brunioh's species, it is found to present marked and decided differences, which it would be tedious to go over in detail, and which would scarcely be intelligible without the aid of figures.^ In the ribs of the thorax we also observe differences, those of our species being more distinctly deflected backwards, and more sharply produced at their outer ex- tremities, particularly the posterior ones. The differences in the pygidium are likewise well defined, its lateral margins forming almost a regular convex arch from the antero-lateral rounded angles to the caudal projection (which seems to be shorter, and is much narrower than D. caudata), instead of being nearly straight, or even concave in outline, posteriorly. Most of these differences we have ascertained from a careful study of a good series of specimens, to be constant in our species, so that they can be re- lied upon as not being individual or sexual peculiarities. In some respects this species is probably even more nearly allied to the common American D. limuturus, while in others it differs more widely. In size it far exceeds the largest examples of D. limulurus we have ever^ seen, while all our specimens show the difference in the obtusely rounded anterior ex- tremity of the head, and the absence of a marginal rim around the middle of the front to be constant. The convex outline of the lateral margins of its pygidium, already mentioned, also contrasts strongly with that of D. limulurus, and even the largest specimens of our species, five inches in length, only show twelve to thirteen segments in the mesial lobe, instead of fifteen, as in the New York species. The caudal appendage, if produced at all, must also be much narrower at its origin in our species. The greater number of segments in the mesial and lateral lobes of the pygidi- um, and the distinct granular surface of both D. plturoptyx and D. micrurus, will alone serve to distinguish them from the species under consideration : while the hypostoma of D. micrurus, at least, is entirely different. If the name Dalmania cannot be retained for this genus, in consequence of its having been previously used for a genus of Dlptera, Hawle and Corda's name Odonlocheile will probably have to be adopted for it, in which case thi$ species will have to be called Odontocheile Dana. Locality and position. Two miles above Thebes, Alexander County, Illinois. Upper Silurian. Genus LICHAS, Dalman, 1827- LlCHAS CUCDLLUS, M. & W. Glabella very convex ; middle lobe strongly elevated, or subconic, nearly three times as wide anteriorly (measuring around the front) as behind, slop- in" abruptly from the highest point behind the middle, with a straight, or slightly concave outline, back to the neck furrow, and rounding with a regu- lar convex, rapidly descending curve, to the rounded front; lateral slopes de- clining abruptly, and separated from the lateral lobes by a linear but well defined furrow, arching forward from the neck furrow, and curving laterally on the anterior slope. ' Lateral lobes about half as high, and three-fourths as long as the middle one, from which they slope abruptly outwards ; nearly as wide behind as the posterior extremity of the middle lobe at the neck furrow, but not more than half its breadth at the summit, and less than one-third its anterior breadth. Outside of these, on each side, the much smaller and low- er palpebral lobes are separated from them by a linear furrow, similar and nearly parallel to those separating the lateral lobes from the central one. [Dec. NATURAL SCIENCES OF PHILADELPHIA. 267 Neck farrow moderately well defined ; neck segment very much depressed be- low the other parts, and sloping backwards ; apparently equalling the breadth across between the two outer lobes. Surface showing, under a magnifier, small, unequal, ratlier scattering pus- tules, with smaller intermediate granules. Lengtb, including the neck segment, 0'70 incb, do. excluding sam inch. Length of thorax, 0*33 inch; breadth of do. 0.60 inch. Length of cephalic shield, 0-42 inch ; breadth of do. 0-64 inch. Length of glabella, exclusive of neck segment, 0-36 inch ; breadth of do. 0*24 inch. Length of eyes, 0-13 inch. This species is remarkable for the structure of its eyes, which, instead of being, as usual, cuvered by the palpebral lobes, have the form and appear- ance of distinct oval tubercles, with the palpebral lobes very small, depressed to, or a little below the elevation of the eyes, and merely connecting with their inner side. We have not been able to see any facets in the eyes, even under a good lens, but they doubtless existed beneath the external crust. 1865.] 18 270 PROCEEDINGS OF THE ACADEMY OP We know of no species with which it could be, for a moment, confounded. With the exception of the above mentioned peculiarities of the eyes, it agrees well with the characters of Griffithides, and doubtless must be called Griffi- t hides PoTtlockii, if that group is to be retained as a distinct genus. Named iu honor of Col. J. E. Portlock, of the Royal Ordinance Survey, of Ireland, and author of the genus. Locality and position. Warsaw, Illinois ; Keokuk Limestone, of Subcarbo- niferous series. Phillipsia (Griffithides) scitula, M. & W. Small, entire outline nearly elliptical. Cephalic shield semielliptic, very convex, about one-third its breadth wider than long, rounded anteriorly, and nearly straight, or more or less concave in outline behind, with posterior la- teral angles produced backwards into rather stout, carinated, pointed spines, which extend as far back as the fifth thoracic segment. Glabella broadly rounded and sloping in front, where it is destitute of a projecting marginal rim ; distinctly contracted posteriorly, in which region it is most elevated ; separated from the cheeks on each side by its much greater convexity, and a shallow furrow, which becomes obsolete around the front ; posterior lateral lobes comparatively large, subtrigonal, very oblique, depressed and isolated by the strongly defined lateral furrows in front of them being so very oblique, and produced, as to intersect the neck furrow ; midway between these two lobes there is a more prominent mesial node, isolated by an accessory furrow passing across in front of it, so as to cut it off, as it were, from the narrow posterior central part of the glabella ; second and third lateral lobes very small, transverse and obscurely defined by short, nearly obsolete linear fur- rows ; anterior lobe larger than all the remaining portions of the glabella be- tween it and the neck furrow. Neck segment a little higher in the middle (where it is provided with a minute tubercle) than the glabella, strongly arched upwards, (not forward) and more than twice as wide, antero-posteri- orly, as one of the thoracic segments ; neck farrow deep, broad, and arching with the neck segment. Eyes comparatively large, or half as lon