Return to LIBRARY OF MARINE BIOLOGICAL LABORATORY WOODS HOLE, MASS. Loaned by American Museum of Natural History PROCEEDINGS OF THE ACADEMY OF NATURAL SCIENCES OF PHILADELPHIA. 1859. PHILADELPHIA: PRINTED FOR THE ACADEMY. 1860. \ AS9 t-4 INDEX. Abbott, Charles C, don. to mus. iii. vii. Academy, American, of Arts and Sciences, don. to lib. xv. Academy, C. L. C. Naturae Curiosorum, don. to lib. xiv. xvii. Academy, Imp. of Arts, Belles-Lettres, and Sciences, Bordeaux, don. to lib. ix. xix. Academy Imp. of Arts, Belles-Lettres and Sciences, Caen, don. to lib. ix. Academy, Imp. of Sciences, Vienna, don. to lib. xvi. Academy, Imp. of Sciences, &c, Dijon, don. to lib. xiv. Academy, Royal of Sciences, Berlin, don. to lib. x. xx. Academy, Royal of Sciences, Munich, don. to lib. xiii. xiv. Academy, Royal Swedish, Stockholm, don. to lib. x. Academy of Sciences, St. Louis, don. to lib. xix. xxii. Agassiz, Prof. L., letter from, 185. Agnew, Rev. W. Gr. E., don. to mus. ii. x. Akademie der Koninklijke Van Weten- schappen, don. to lib. iv. Allibone, S. Austin, don. to lib. v. Association, American, for Advance- ment of Science, don. to lib. vi. vii. Association, Mercantile Library of New York, don. to lib. xviii. Association, Young Men's Mercantile Library, Cincinnati, don. to lib. v. Bache, Prof. A. D., don. to lib. xiv. Baer, C. E. de, don. to lib. xxii. Baird, D., don. to mus. ii. Baird, Prof. S. F., notes on a collection of Birds made by Mr. John Xantus, at Cape San Lucas, Lower California, 293, 299. Beok, Dr. C. F., announcement of death of, 91; Executors of, 164; don. to mus. iv. Beck, Mrs. S. R. G., resolution of thanks to, 164 ; don. to lib. xi. Bell, J. J., don. to mus. v. 1859.] Bertholet, Dr. P. P., don. to mus. i. Betton, Dr. Thos. F., don. to lib. xxiii. Binney, W. Gr., Notes on American Land Shells, No. 5, 187; don. to mus. vii. don. to lib. ii. Biological Department, Report of Pro- ceedings for Jan. 4 ; do. for Feb. 90 : do. for March, 93 ; do. for April, 112 ; do. for Mav, 151 ; do. for June, 165 : do. for Sept. 256; do. for Nov. 294: don. to lib. xxii. xxiii. xxiv. Boker, Dr. C. S., don. to mus. vi. Bologna, Municipality of, don. to lib. viii. Borda, Eugene, letter from, on locality of two specimens of Lepidodendron. 293; don. to mus. vii. Bowditch, H. Gr., M.D., don. to lib. v. Bridges, Dr. Robert, V. Pres. Acad. Nat. Sc, announced the death of Dr. Mutter, 92 ; don. to lib. v., don. to mus. vii. Broderip. W. J., announcement of death of, 110. Broun, Dr. H. C, don. to lib. ix. xiv. xx. xxiii. Brown, Dr. S. P., don. to mus. iv. Bruns, Dr. J. Dickson, don. to mus. v Bryant, Dr. Alexander, vote of thanks to, 110, don. to mus. ii. Buckalew, Hon. Charles R., don. to mus. vi. Buckley, S. B., don. to mus. i. Caldwell, Dr. H. C, announcement of death of, 330. Carbonell, Celedonio, don. to lib. viii. Carpenter, P. P., notice of a collection of shells made at Cape San Lucas. Lower California, &c, 331. Carson, Dr. J., Remarks on Chines- chemicals, 150 ; don. to lib. xxiv. Cassin, John, read letter from P. B. Duchaillu, 1 ; Catalogue of Bird* collected by P. B. Duchaillu, on the rivers Camma and Ogobai, Western Africa, 3, 3D ; Motion for a vote of thanks to James Hammill, 55 , Cata- IT. INDEX. logne of Birds collected by P. B. Du- chaillu, on the rivers Camma and Ogobai, Western Africa in 1858, &c, 91, 133, 172; don. to lib. i. Claparede, Edouard, don. to lib. xv. xvii. Clark, Edward L., don. to mus. iv. Clark. J. Hinckley, don. to mus. iv. Clemens, Dr. Brackenridge, Synopsis of North American Sphingidae, 161 ; Contributions to American Lepidop- terology, 256, 293. Coates, B. H., don. to lib. i. Collet, Dr. M. W., don. to lib. i. Committee, Publication, don. to lib. i. xviii. Committee of five appointed to take measures for the formation of a per- manent fund, 90. Committees, Election of Standing, 55. Commit ees on scientific papers : by Spencer F. Baird, Notes on a collec- tion of Birds made by Mr. Xantus, at Cape San Lucas, Lower California, 293 ; by Wm. G. Binney, Notes on American land shells, No. 5, 187 ; by P. P. Carpenter, Notice of a col- lection of shells made at Cape San Lucas, Lower California, &c. 331 ; by John Cassin, Catalogue of Birds collected by P. B. Duchaillu, on the Rivers Camma and Ogobai, Western Africa, in 1858, with notes and de- scriptions of new species, 3, 91 ; by Brackenridge Clemens, Synopsis of North American Sphingidae, 1G2 ; Contributions to American Lepidop- terology, 256, 293 ; by E. D. Cope, On the primary divisions of the Sala- mandridre, 111 ; Notes and descrip- tions of foreign Reptiles, 292 ; Cata- logue of the venomous Serpents in the museum of the Academy, with notes on the Families, Genera, and Hpecies. 331 ; by T. A. Cor.rad, De- scriptions of new Cretaceous and Eo- cene shells of Mississippi and Ala- bama, .and with notes on Eocene fos- sil shells, 330 ; by Wm. M. Gabb, Catalogue of the Invertebrate fossils of the Cretaceous formation of the U. States, 2o5 ; Description of two new species of Carboniferous Fossils, 292; by Theodore Gill, on Dacty- loscopus and Leptoscopus, two new genera of the family of Uranosco- pidae ; on the genus Callionymus of authors ; on description of Hypo- rhampus, a new genus of fishes al- lied to Hem rhampus ; on notes on a collection of fishes from Jap:m, made by Dr. J. Morrow, 109 ; Description of a third genus of Hemiramphinae, 150 ; Description of a new genus of Salarianse, 162 ; Description of a new species of Callinidea, and description of new generic types of Cottoids, 164 ; Description of a type ofGobioids in- termediate between Solinae and Tri- dentigerinse, and description of a new South American type of Siluroids allied to Callophysus, 194; by Chae. Girard, M. D., Ichthyological No- tices, 164; by R. Kennicott, Notes on Coluber calligaster, Say, and de- scription of new species of Serpents in the collection of the North-wesi- ern University of Evanston, 111., 91 : by Isaac Lea, Description of 8 new species of Unionidse from Georgia. Mississippi, and Texas, 109 ; De- scription of twenty-one new species of Exotic Unionidae, and description of two new species from Georgia. Ill ; Description of seven new spe- cies of Uniones, 150 ; New Unionidae of the United States, 151 ; Descrip- tion of twelve new species of Uniones from Georgia, 164 ; Descriptions of four new species of Unionidas, 177 : Description of anew species of Unio, 280 ; Descriptions of three specie;- of Exotic Unionidae, 329 ; Descriptions of Exotic Unionida?, 330 ; by John Le Conte, descriptions of two new spe- cies of tortoises, 3 ; Observations on the species of Nicotiana, 56 ; de- scriptions of new species of the Coleopterous family Histeridae, 293 : by John L. Le Conte, Catalogue of the Coleoptera of Fort Tejon. California, 56 ; Additions to the Co- leopterous Fauna of Northern Cali- fornia and Oregon, 280 ; by F. B. Meek, and F. V. Hayden, Geological Explorations in Kansas Territory, 3 ; by Dr. J. Aitken Meigs, Descrip- tion of a deformed fragmentary Hu- man Skull found in an ancient quarry cave at Jerusalem, with an attempt to determine by its configuration alone the Ethnical type to which it belongs, 256 ; by R. Osten Sacken. new genera and species of North American Tipulidae with short Palpi, &c. 194 ; by Wm. J Taylor, Minerab ogical Notes, No. 2 ; by Wm. Stimp- son, Prodromus descriptionis ani- [18S INDEX. v. malium Evertebratoruni quae in ex- peditione ad Oceanum Pacificum, Septentr. a Rep. Fed. missa Cad. Ringgold et Job. Rogers ducibus, &c, pars vii. Crustacea macrura, 331; by A. Wilcocks, Reflections upon the nature of the temporary star of 1572, an application of the nebular hypothesis, 330 ; by John Xantus, Catalogue of Birds collected in the vicinity of Fort Tejon, Cali- fornia, with a description of a new species of Syrnium, 187 ; Descrip- tions of new species of Birds from Cape San Lucas, Lower California, 292. Connaroe, Geo. M., don. to lib. v. Conrad, T. A., Descriptions of new Cretaceous and Eocene shells from Miss., and Ala., and also with notes on Eocene fossil shells, 330 ; don. to mus. vii. Cooper, Dr. J. G., don. to mus. vi. don. to lib. xvi. Cope, E. D. on the primary divisions of the Salamandridse, with a descrip tion of two new species, 111, 112 ; Notes and descriptions of foreign Reptiles, 292, 294 ; Catalogue of the venomous serpents in the museum of the Academy, with notes on the Families, Genera and Species, 331. 332. Corse, Dr. J. M., don. to mus. vi. Dana, J. D., don. to lib. i. v. Darrach, Dr. James A., don. to lib. xvi. Davids, R. W., don. to mus. vi. Davidson, George, letter from, 293 ; thanks of the Academy to, for dona- tion, 294 ; don. to mus. ii. v. vi. Davidson, R. 0., don. to lib. xii. Davis, J. Barnard, remarks of, review- ing the method of measurement as a diagnostic means of distinguishing human races, (adopted by Drs. Schertzer and Schwarz,) 330. Dawson, J. W., don. to lib. vii. viii. xxii. De Camp, Dr. W. H., don. to mus. v. Department of War, don. to lib. ix. Dinipfels, Mr. F. don. to mus. i. Dowler, Dr. Bennet, don. to lib. i. ix. Duchaillu, P. B., Letter from, read, i. Dunn, Dr. Theophilus, don. to mus. vi. Durand, Mr. E., Remarks on cones of Pinus pungens, 1. 1859.] East India Company, don. to lib. xviii. Editors of Allgemeine Zeituiigfur Wis senschaften, don. to lib. xv. Editors of American Journal of Medi- cal Sciences, don. to lib. xxi. Editor of American Journal of Phar- macy, don. to lib. ii. vi. viii. xv. xvii. xxii. Editors of American Journal of Science and Arts, don. to lib. ii. iv. xv. xvii. xx. Editors of Architects and Mechanics Joiirnal, don. to lib. xix. Editors of Archiv fur Naturgeschichte. don. to lib. iv. x. Editors of Atlantis, Dublin, don. to lib. xiv. xxi. Editors of Charleston Medical Journ- al, &c, don. to lib. ii. iv. x. xv. xvii. xviii. xxi. Editors of Dental Cosmos, don. to lib. xviii. xix. xxii. Editors of Druggist, don. to lib. xv. Editors of Edinburgh New Philosphi- cal Journal, don. to lib. xvii. xxii. Editors of Farmer and Gardener, don. to lib. xix. Editors of Gardener's Monthly, &c. don. to lib. xv. Editors of Hutching's California Maga- zine, don. to lib. xvii. xx. Editors of Journal of the Indian Archi- pelago, don. to lib. v. Editors of La Bourgogne Revue cenolo- gique et Viticole, don. to lib. xiv. Editors of Medical and Surgical Re- porter, don. to lib. xii. Editors of Natural History Review, don. to lib. x. Editors of Neues Jahrbuch fur Miner. &c.j don. to lib. ix. iv. Editors of New Orleans Medical and Surgical Journal, don. to lib. ii. vi. xv. xvii. xxi. Editors of New York Journal of Medi- cine, don. to lib. ii. vi. Editors of North American Medico- Chirurgical Review, don. to lib. xv. xviii. xxi. Editors of Pacific Medical and Surgical Journal, don. to lib. x. Editors of Revue et Magasin de Zoolo- gie, &c, don. to lib. xvii. xviii. xix. xxii. Editors of Southern Medical and Surgi- cal Journal, don. to lib. v. vi. viii. x. xi. xv. xvi. xvii. xix. xxi. Editors of Weiner Entomologische VI INDEX. Mouatschrift, don. to lib. xiii. xv. xvii. xviii. xix. xxii. Edwards, Arthur M. don. to lib. Election, Annual, of Officers, 353 ; of members and correspondents, 354. Emmons, Prof. E., Remarks on head of Clepsysaurus, 151 ; Remarks on the debituminization of coal 162 ; don. to mus. iii. iv.; don. to lib. ii. Kngelmann, Dr., don. to mus. vii.; don. to lib. xxi. Etting, Henry, U. S. N., don. to mus. iii. Evans, Dr. John, don. to mus. v. Pahnestock, G. W., don. to mus. v. Farquhar, G. W., don. to mus. v. Field, Lieut. Thos. Y., U. S. N., don. to mus. v. vi. Fisher, Dr. James C, elected Libra- rian, 176 ; presented for publication Index to the genera described or referred to in the Proceedings of the Academy, Vols. I. VIII., 329 ; Re- marks on changing Argynnis Astarte to A. Ashtaroth, 352 ; don. to lib. xxii. Fisher, Dr. G. J., Letter from, 194. Florat, J. A., don. to mus. vi. Forman, Mr., don. to mus. ii. Foulke, Wm. Parker, presented pine cones, 1 ; announced death of Dr. C. F. Beck, 91 ; don. to mus. i. ii. v. vi. Fricke, Dr. don. to lib. xix. Gabb, Wm. M., Catalogue of the inver- tebrate fossils of the cretaceous for- mation of the United States, 255, 256 ; Description of two new species of carboniferous fossils. 292, 297 ; don. to mus. i. ii. iv. v. vii. Gallaer, Dr. John, don. to mus. i. Gill, Theodore, on Dactyloscopus and Leptoscopus, two new genera of the family of Uranoscopidse ; on the genus Callionymus of authors ; De- scription of Hyporhaniphus, a new genus of fishes allied to Hemiram- phus ; Notes on a collection of Japa- nese fishes, made by Dr. J. Morrow, 109 ; Description of a third genus of Hemiramphinse, 150 ; Description of anew genus of Salariana?, 162; description of a new species Collini- dea, 164 ; Description of new generic types of Cottoids from the collection of the North Pacific Exploring Ex- pedition, under Com. John Rodgers, 164 ; Description of a type of Gobi- oids intermediate between Solinre and Tridentigerince, 194, 195 ; De- scription of a new South American type of Siluroids allied to Callophy- sus, 194, 196 ; don. to lib. x. Girard, Charles, M. D., Ichthyological notices, 91, 111, 151 ; Herpetologi- cal notices, 164. Goodrich, S. G., don. to lib. xxii. Goucher, Mr. J., don. to mus. ii. Gould, B. A., Jr., don. to lib. iv. Graham, Col. J. D., don. to lib. v. vi. Gray, Prof. Asa, M. D.. don. to mus. iv.; don. to lib. xxi. Gregory, J. W., vote of thanks to, 112: don. to mus iii. Grier, Dr. W. P., don. to mus. vi. Guerin-Meneville, M. F. E., don. to lib. vii. Hall, Prof. James, don. to lib. xi. Hamilton, Wm. J., don. to lib. xvii. Hammill, Mr. James, vote of thanks to, 55 ; don. to mus. i. Hammond, Dr. Wm. A., Observations on the colorless blood-corpuscle, 56; Read letter from Miss M. H. Morris, 193 ; don. to nrus. iv. Hankel, W. G., don. to lib. iv. Hanson, H. C, don. to mus. iv. Hanson, Joseph B,, don. to mus. iii. v. Hanson, P. A., don. to lib. iv. Hare, Lieut. Geo. H., don. to mus. i. vi. Harris, Thomas, don. to mus. i. Harrison, Joseph, don. to mus. i. Hartman, Dr., don. to mus. iv. Hass & Brenizer, don. to mus. iii. Hawkins, J. S., don. to mus. i. Hayes, Dr. I. I., don. to mus. iii. Helmuth, Dr. C. A., letter from, 164. Holbrook, Dr. J. C, don. to mus. vi. Holmes, Prof. F. S., Remarks on Post- Pleiocene fossils of South Carolina. 177 ; don. to mus. v. Henderson, Dr. A. A., U. S. N., don. to mus. ii. Henry, Dr. T. Charlton, U. S. A., Catalogue of the birds of New Mexico, as compiled from notes and observations made while in that Territory, d\iring a residence of six years, 104 ; don. to mus. i. ii. Hering, C- J., don. to mus. v.; don. to lib. xvi. Hoopes, B. A., don. to mus. 1. Hoopes, Joshua, don. to mus. iv. [1859. INDEX. vn. Horsfield, Dr. Thomas, announcement of death of, 292. Humboldt, Baron Alex, von, announce- ment of death of, 154. Institute, Albany, don. to lib. iii. Institute, Canadian, don. to lib. iii. v. viii. xi. xv. xix. xxii, Institute, Essex, don. to lib. v. Institute, Franklin, don. to lib. v. Institute, Imperial Royal Geological of Vienna, don. to lib. iv. xiv. xx. xxiii. Institute, Imperial Royal, of Science, Lombardy, don. to lib. iv. xix. Institute, Maryland, don. to lib. i. xvi. Institute, Pennsylvania, for instruc- tion of the Blind, don. to lib. ix. Jan, Prof. M. Le, don. to lib. xiv. feanes, Joseph, elected to Committee on Library, 109 ; don. to mus. i. Jessup, Augustus E., announcement of death of, 352, Jones, John Matthew, don. to lib. xviii. Kane, Dr. John K., don. to lib. xxi. Kennicott, R., Notes on Coluber cali- gaster Say. and description of new species of serpents in the collection of the North-western University of Evanston, 111., 91. Kintzing, W. F., don. to lib. xvii. Kolenati; Dr. F. A., don. to lib. vii. Kollar, Dr. Noah, don. to mus. iv. Krider, Mr. John, don. to mus. iv. v. vii. Lacordaire, Prof. Th., don. to lib. xxii. Lapham, F. A., don. to mus. i. Latour, M. Huguet, don. to lib. iii. v. Lea, Isaac, LL. D., Prest. Acad. Nat. Sciences, Description of eight new species of Unionida?, from Georgia, Mississippi and Texas, 109 ; Descrip- tion of twenty-one new species of Exotic Unionidse, and descriptions of two new species of Uniones from Georgia, 111 ; Descriptions of seven new species of Uniones, &c, 150; New Unionidse of the United States, 151 ; Notice of the death of Baron von Humboldt, 162; Resolutions by, 163 ; Description of twelve new species of Uniones from Georgia, 164 ; Descriptions of four new species of Unionida?, and Remarks 1859.] on dead shells Anodonta Lewisii, 177 ; Description of a new species of Unio from the Isthmus of Darien, 280, 281 ; change of name of Mar- garitana Etowahensis to M. Georgi- ana, 280 ; Resolutions by, on the death of Thomas Nuttall, 281 ; De- scriptions of three new species of Exotic Uniones, 329, 331 ; Descrip- tions of Exotic Unionida?, 330 ; Remarks on embryonic shells of Uniones, 329 ; don. to mus. i. ii. vii.; don. to lib. xviii. xxii. Le Conte, Maj. John, V. Pres. Acad. Nat. Sci., Descriptions of two new species of Tortoises, 3 ; Observations on the species of Nicotiana, 56; De- scriptions of new species of the Cole- opterous family Histeridae, 293, 310; don. to mus. v. Le Conte, Dr. John L., Catalogue of the Coleoptera of Fort Tejon, Cali- fornia, 56, 69 ; Remarks on Paleo- trochus from Keewenaw Point, 150 ; Additions to the Coleopterous Fauna of Northern California and Oregon, 280, 281 ; don. to mus. iv., don. to lib. xi. Leidy, Prof. Joseph, M.D., Remarks on Manayunkia speciosa, 2 ; Re- marks on Xystiacanthus Arcuatus, and Cladodus occidentalis, 3 ; Re- marks on tooth of Mastodon and bones of Mosasaurus, 91 ; Remarks on teeth of Clepsysaurus, Eurydorus serridens, and Compsosaurus, from Phoenixville tunnel, Chester co., 110 ; Remarks on fossils from Beth- any, Va., and also from the Green Sand, Monmouth co., N. J., 110; Remarks on Ossite from Sombrero, W. I., on skull of Ursus Americanus from the drift, Claiborne, Miss., Ill ; Remarks on fragment of jaw of Mo- sasaurus, 150 ; On specimens of Palseotrochus from snb-silurian strata, 150 ; Remarks on Droma- therium sylvestre and other fossils from Chatham co., N. C, 162; Ex- tract of letter from, 1 80 ; Letter from Dr. J. G. Fisher, and remarks on antler of the Reindeer found at Sing- Sing, and remarks on Freija ameri- cana from Newport, 194 ; On the seat of the vesicating principle of Lytta vittata, 256 ; don. to mus. i. ii. iii. vii. don. to lib. i. v. vii. viii. x. xix. Lennig, Charles, don. to mus. iii. via. INDEX. Leonhard, Prof., don. to lib. xiv. xx. xxiii. Lesley, J. P., elected to Committee on Palaeontology, 109 ; Read letter from Ed. A. Spring on capture of a fish by a spider, 255. Letterman, Dr. J., U. S. A., don. to mus. i. Lewis, Miss Maria, don. to mus. vi. Lyceum of Nat. History, New York, don. to lib. viii. Marcou, Jules, don. to lib. i. xii. xxii. Meek, F. B. and F. V. Hayden, M.D., Geological explorations in Kansas Territory, 3. Meigs, Dr. J. Aitken, resignation as Librarian, 161 ; Description of a deformed fragmentary human skull found in an ancient quarry cave at Jerusalem, with an attempt to deter- mine by its configuration alone tbe Ethnical type to which it belongs, 256, 262; Read remarks of J. Bar- nard Davis, 330 ; don. to mus. iii. Minister of Public Works, France, don. to lib. iii. v. xi. xiv. xix. Mitchell, S. Weir, M. D., observations on exposed hearts of animals, 56. Moore, Cornelius, don. to mus. v. Moore, Dr. Francis, don. to mus. v. vi. vii. Moore, W. D., don. to mus. iii. Morris, Dr. J. Cheston, description of a new species of Pomotis, 3. Mosblech, P. W., don. to mus. ii. Mueller, Charles, don. to lib. xiv. xviii. Mueller, Ferdinand, don. to lib. xvii. Mutter, Dr. Thomas D., announcement of death of, 92. Norcom, Dr., don. to mus. ii. Norton, C. B., don. to lib. i. Nuttall, Thomas, announcement of death of, 280 ; don. to lib. xviii. Ondarza, Col. Juan, don. to lib. xi. Osborn, H. S., don. to mus. ii. Osten-Sacken, Baron R., new genera and species of N. American Tipulidse with short palpi, with an attempt at a new classification of the tribe, 194, 197 ; don. to lib. vi. Owen, Dr. David Dale, don. to lib. xv. Owen, Richard, don. to lib. vii. Peale, Franklin, don. to mus. vi. Pea'rsall, Robt., don. to mus. vi. Perrine, F. M., don. to mus. ii. Postell, James, don. to mus. vii. Powel, Miss Mary, don. to mus. i. Powel, Samuel, read extracts from a letter on fossil bones near Enfield, North Carolina, 56 ; don. to mus. ii. vii. Prime, Temple, don. to lib. xii. Publication Committee, don. to lib. i. xviii. Queen, J. W., don. to mus. ii. Rand, Dr. B. IL, announced death of Capt. McMichael, 56 ; don. to mus. iii. Rand, Theodore D., don. to mus. ii. Reed, A. G., don. to mus. vii. Remont, J. R., don. to mus. iii. Report of Committee of Biological De- partment on paper of Dr. Wm. A. Hammond, 56, 165, 151 ; Of Dr. J. J. Hayes, 149 ; On paper of Dr. S. Weir Mitchell, 56, 151, 165 ; Of Dr. .'. H. Packard, 151 : Of J. J. Wood- ward, 93. Report of Committee on paper of Prof. S. F. Baird, 299 ; Of Wm. G. Binney, 188 ; Of John Cassin, 30, 133 ; Of P, P. Carpenter, 331; Of Dr. Bracken- ridge Clemens, 163, 317; Of E. D. Cope, 122, 294, 332 ; Of Wm. M. Gabb, 297 ; Of Theodore Gill, 128, 131, 132, 144, 155, 165, 167, 168, 195, 196 ; Of Dr. Charles Girard. 56, 100, 113, 157, 169 ; Of Dr. T. Charl- ton Henry, 104; Of Robert Kenni- cott, 98 ; Of Isaac Lea, LL.D., 112. 151, 154, 170, 187, 221, 331 ; Of John LeConte, 4, 93,310; Of; Dr. John L. Le Conte, 69, 281 ; Of Dr. Joseph Leidy, 256 ; Of F. B. Meek and F. V. Hayden, M.D., 8; Of Dr. J. Aitken Meigs, 262 ; Of Dr. S. Weir Mitchell, 281 ; Of Baron R. Osten- Sacken, 197 ; Of H. D. Schmidt, 256: Of Wm. J. Tavlor, 306 ; Of John Xantus, 189, 297. Report of Curators, Annual, 351. " Librarian, Annual, 350. ' ' Recording Secretary, Annual, 343. Resolutions of Committee of Proceed- ings, 149, 150. Richards, Francis, don. to mus. v. Richardson, Dr. F. G., don. to mus. i. Roepper, W. Thomas, don. to mus. vii. Rogers, Prof. R. E., M.D., exhibited Ritchie's Riihmkorff apparatus and Wagner's electrical machine, with [1859. tNDEX. IX. his alteration, 90; Lecture on the cor- relation of forces 150 ; Remarks on coal, 162; Remarks on specimens from the Geysers of Pluton Canon, Cal., 294; don. to mus. iii. Rue, Mr. M. P., vote of thanks to, 92 ; don. to mus. ii. Ruschenberger, Dr.*W. S. W., don. to mus. v. Safford, Prof. J. M., don. to mus. v. Sandberger, Dr. G., don. to lib. vii. Say, Mrs. Lucy W., don. to lib. xxi. Saussure, H. de, don. to lib. ix. xiv. Schell, Dr. William, don. to lib. xx. Schmidt, Dr. H. D., abstract of the most important points of researches on the minute anatomy of the liver, 256. Secretary of the Commonwealth of Penn., don. to lib. iii. Semple, Dr. J. E , U. S. N., don. to lib. iii. Sergeant, J. D., don. to mus. ii. vi. vii. Slack, J. H., don. to mus. i. ii. iii. v. vi. vii. Smith, Aubrey H., don. to. mus. vi. Smith, E., don. to lib. ix. Smithsonian Institution, don. to mus. i. ii. iii. v. vi. vii., don. to lib. ii. vii. viii. Society, American Antiquarian, don. to lib. i. vi. vii. Society, American Geographical and Statistical, don. to lib. xxi. xxii. xxiv. Society, American Philosophical, don. to lib. vii. xix. Society, Arts and Institutions in Union, don. to lib. v. x. xi. xx. xxii. Society, Batavian Nat. Hist'y &c, don. to lib. iv. vii. Society, Belfast Nat. History, S. Phil., don. to lib. xii. Society, Boston, of Nat. History, don. to lib. vi. xi. xv. xvii. Xix. Society, Deutschen Geoiogischen, Ber- lin, don. to lib. iv. x. xiv. Society, Drontheim, R. Nat. History, don. to lib. iv. Society, Dublin Geological, don. to lib. x. Society, Elliot Nat. History, Charles- ton, S. C, don. to lib. xv. xviii. Society, Entomological, of Berlin, don. to lib. xviii. Society, Entomological, of Stettin, don. to lib. xiv. 1859.] Society, Finnish, of Sciences, Helsim fors, don. to lib. ix. Society, Imp. of Nat. Sciences, Cher- bourg, don. to lib. ix. Society, Imp. of Naturalists, Moscow, don. to lib. iv. Society, Leeds Philosophical, &c, don to lib. xv. xx. Society, Linnean, of Normandy, don. to lib. xx. Society, Literary and Philos., Liver- pool, don. to lib. xxiii. Society, Literary and Philos., Man- chester, don. to lib. x. Society, London Geological, don. to lib. viii. xii. xix. Society, Medical, Frankfurt, A. M., don. to lib. xx. Society, Natura Artis Magistra, Am- sterdam, don. to lib. iv. Society, Natural History, Augsburg. don. to. lib. xiv. Society, Natural History, Basel, don. to lib. iv. Society, Nat. History, Montreal, don. to lib. iii. vi. viii. xv. xviii. xx. Society, Nat. History, Prussian Rhine- land, &c, don. to lib. xx. Society, Natural History, Saxony and Thuringia in Halle, don. to lib. xx. Society, Natural History, Wiesbaden, don. to lib. x. Society, Nat. History, Wiirttemban.-, don. to lib. xxiii. Society, Nat. History, Wurzburg, don. to lib. xx. Society, Naturalists of New Grenada, don. to lib. xiv. Society, Natural Sciences, Emden, don. to lib. iv. xx. Society, Natural Sciences, NeucL don. to lib. xx. Society, Oberhessischen fiirNatur.- und Heilkunde, don. to lib. xiv. Society, Palaeontolcgical, Belgium, don, to lib. xviii. Society, Physics and Natural History. Geneva, don. to lib. xiv. Society, Royal Gardeners, Berlin, den. to lib. xx. xxiii. Society, Imp. Geological, St. Peters- burg, don. to lib. ix. Society, Royal of London, don. to lib. xii. xviii. xx. Society, Royal of Northern Antique ries, don. to lib. v. Society, Royal Saxon in Leipzig, don, to lib. iv. xxiii. INDEX. Society, Royal of Sciences at Gottiugen, don. to lib. xx. Society, Royal of Stuttgart, don. to lib. xiii. Society, Senckenburg Natural History, don. to lib. x. Society, Vaudois, of Nat. Sciences, don. to lib. iv. ix. Society, Zoological and Mineralogical, Regensberg, don. to lib. xiv. Sorby, H. C, don. to lib. i. Spring, Edward A., letter from, on capture of a fish by a spider, 255. Storer D. Humphreys, don. to lib. vi. Stimpson, Wm., Prodromus Descrip- tions Animalium evertebratorum qufe in expeditione ad Oceanuni Pa- cificum Septentrionalem a Repub. Feder. missa, Cad. Ringgold, et Job.. ' Rodgers ducibus, observavit et de- scripsit, pars viii. Crustacea macrou- ra, 331 ; don. to nius. vi. Struthers, Mr., don. to mus. ii. Survey Geological of India, don. to lib. xi. Swallow, G. C, don. to lib. xviii. xxii. Swift, Robt., don. to mus. vi. Taylor, Alex. S., don. to lib. xx. Taylor, Wm. J., Mineralogical notes No. II. 293, 30G ; don. to mus. iv. vii. Thomas, Dr. J., don. to mus. iv. Thurman, J., don. to lib. xi. Trautwine, J. C, don. to mus. i. ii. Troschel, Prof., don. to lib. xiv. xx. xxiii. Trustees New York State Library, don. to lib. xv. Tufts, S. Jr., don. to mus. vi. Turner, Dr. S. J., U. S. N. don. to mus. iii. Ukler, Dr. Wm. M., remarks on anes- thetic effect of bi-sulphide of carbon, 164. Union Deutscher Aerzte in Paris, don. to lib. iii. Oniversity of Michigan, don. to lib. v. Vanderslice, Mr. Andrew, don. to mus. 90, i. Vaux, Wm. S., don. to mus. i. ii. Verreaux, E. S. & J. G., don. to lib. xxii. War Department, don. to lib. xv. Warren, David M., don. to lib. xviii. Warren, Lieut. G. H., don. to lib. vii. Weigel, F. 0. don. to lib. xx. Weiss, Adolf, don. to lib. xiii. Westermau, B. & Co. don. to lib. xxii. Wheatley, Charles M., don. to nms. vii. Whelen, Edward S., don. to mus. ii. viii. Wilcoxks, Dr. Alexander, reflections on the nature of the temporary star of 1572, an application of the Nebu- lar hypothesis, 330. Willcox, Edward J., don. to mus. vii. Williams, John, don. to mus. vii. Willis, 0. R., don. to mus. iii. Wilson, Dr. G. B. don. to mus. i. Wilson, Dr. S. W., don. to mus. v. Wilson, Dr. Thomas B., resigna- tion of, from Committee on Pahe- ontology and Library 55 ; don. to mus. i. don. to lib. i. ii. iii. v. vi. vii. viii. ix. xi. xii. xiii. xv. xvi. xvii. xviii. xix. xxi. xxii. xxiii. xxiv. Wood Horatio C. Jr., don. to mus. vii. Woodhouse, Dr. S. W. don. to mil*, ii. v. Woodward, Dr. J. J., on suppuration in cancerous growths, 93. Worrell, Wm. don. to mus. vi. Xantus, John, Catalogue of birds col- lected in the vicinity of Fort Tejon. California, with a description of a new species of Syrnium, 189 ; Cata- logue of Birds from Cape San Lucas. Lower California, 292, 297; don. to mus. iii. Zigno, Barone Achille, don. xiv. to lib. [1859. INDEX TO PROCEEDINGS OF THE BIOLOGICAL DEPARTMENT For 1859. Atlee, Dr. Walter F., Remarks oa white corpuscles in dried blood, 3; Remarks on a Hydatid Mole, 6. Election of officers for 18G0, 20. Hammond, Dr. Wrn. A., Remarks on stomach of Fiber zibethicus, Castor fiber, Arvicola, 1 ; Observations on the colorless blood corpuscles, and remarks on eggs of parasites, in the liver of a rabbit and the spleen of Chelonian reptiles, 4 ; Remarks on the excitability of heart containing blood, 6. Hammond and Mitchell, Experimental researches relating to Corroval and Vao, two new varieties of Woorara, the South American arrow poison, 11 ; Experimental examination of the physiological effects of Sassy-bark, the ordeal poison of the Western Coast of Africa, 13. Hayes, Dr. I. I., On the relations exist- ing between food and the capacity of man to resist low temperatures, 8. Leidy, Dr. Joseph, Remarks on impos- sibility of determining the source of dried blood, 3 .; exhibited specimen of a Trichina found in human mus- cle, 3 ; Remarks on human muscle containing peculiar cysts, 4 ; Re- marks on dipterous larvae from man, 7 ; on the vesicating principle of the Lytta vittata, 18. Mitchell, Dr. S. Weir, Remarks on blood crystals of the opossum and muskrat, 1 ; Gall stone found in the gall-bladder of a muskrat, 3 ; Re- marks on the death of an infant in ulero. before the mother, 4; Remarks on the circulatory apparatus of the Lepidosteus, 5 ; Remarks on peculiar contraction of muscles not bound by fascia, when struck, 5 ; Remarks on the effect of sugar in rendering the eyes of frogs cataractous, 16; On the production of cataract in frogs by the injection of large doses of sugar, 20. Morris, Dr. J. Cheston, Remarks on human Embryo in its membranes, 7 : Remarks on poisoning from the sting of the common bee, 18 ; Remarks on the digestive principle, 19. Packard, Dr. A. F., Remarks on the swimming bladder of Lepidosteus, 4 ; On the pathological relations of Can- cer and Tubercle, 10. Woodward, Dr. J. J., Remarks on im- possibility of determining to what mammal dried blood has belonged, 2 ; Remarks on cysts in human muscle, 4 ; On suppuration in cancerous growths, 7 ; Remarks on phosphates in urine, and also on highly acid urine, 20. Uhler, Dr. Win. M., Remarks on or- ganic substances not found in the organism during life, 3. 1859.] PROCEEDINGS OF THE ACADEMY OF NATURAL SCIENCES OF PHILADELPHIA. 1859. January 4tli. President Lea in the Chair. Forty-eight members present. Mr. W. Parker Foulke presented some cones found in April, 1858, by Mr. Samuel I. Goucher, on a peak of the Blue Mountain, near Mount Holly Springs, Cumberland County, Pennsylvania. Mr. Durand stated that he had examined these cones, with a few leaves ac- companying them, and had no doubt they were from the Pinuspungens, or table mountain pine, which he believed had not been previously recognized so far north. January Will. Dr. Carson in the Chair. Thirty-seven members present. Mr. Cassin read a letter from Mr, P. B. Duchaillu, dated Fernando Vaz River, Western Africa, September 28th, 1858, containing the following passages: " Since I left the Gaboon in 1857, I have explored the Camma or Fernando Vaz river and the Ogobai river, which is a branch of the Camma, but was pre- vented from ascending the latter by the natives. I have ascended also to the distance of about two hundred miles the Rembo and the Ovenga rivers. "The country of the Nazareth and the Camma is intercepted by large rivers, creeks and lagoons going in every direction into the interior, and to all of which the natives have given distinct names. Some of these rivers are wide and deep, and would be navigable for steamers to a great distance. In some places the soil is very rich and in others sandy ; the ebony and red wood trees are very abundant. " One of the most interesting facts that I have determined is, that the Cannibal tribe (the Paueins) which I met with on the head waters of the river Muni, seem to terminate in the interior, up the Nazareth river, the banks of which are inhabited by various tribes calling themselves Orounga, Ogobai, Pandjai, Aninga, Okanda and Apindgi ; none of these are cannibals, and they speak of the Paueins as farther north and in the interior, and my conclusion is, that this cannibal people either follow the mountains, which I think take here an eastern direction, or that they cease. Up the Rernbo, which is the main branch 1 [Jan. 2 PROCEEDINGS OP THE ACADEMY OP of the Fernando Vaz, the Bakalai tribes disappear ; then follow a people calling themselves Ashira, and next to them come the Apindgi. "Up the Oveuga, I left it and went into the interior amidst the Bakalai people and afterwards into the Ashira country. The Ashiras are quite a different peo- ple from any that I have yet seen in Western Africa. They cultivate tobacco extensively, and cotton to some extent also, but the principal cloth made by them is from a kind of grass which is very fine. Food with this people is abundant, and they are the only people I have yet seen in this country that had domesticated hogs. " Immense forests, in which the ebony tree is very abundant, border the banks of the Fernando Vaz, but at the highest point that I reached, the coun- try was more open, and grassy plains frequently presented themselves. I was assured by the natives that this was the character of the country still higher up the river and its branches, and they speak of a large prairie and of a large lake also further in the interior. The latter, as far as I can judge from the accounts of the natives, is about 600 miles from the coast. At present my intention is to make another journey about in the latitude of the Fernando Vaz in search of this lake, which I have some hopes may prove to be the source of the Congo. In this journey I may perhaps also ascertain the course of the mountains that I reached in ascending the Muni river. I have made maps of all the rivers that I have ascended, and have, with much difficulty, kept my journal without intermission, and hope to lay it before the Academy on my return to the United States. I send by this vessel four boxes and three barrels containing collections of quadrupeds and birds, in which are many interesting specimens, and some that I have never collected before. All are from the Fernando Vaz or Camma, the Ogobai, Rembo and Ovenga rivers." Dr. Leidy exhibited a drawing of the worm described by him at a former meeting as Manayunkia speciosa. Dr. Leidy remarked, that perhaps some of the members present would recol- lect he had some time since, (Proc. 1858, p. 90,) described a curious fresh water worm, Manayunkia speciosa, from the river Schuylkill. It was observed that it appeared to be most nearly allied to the marine genus Fabricia. During the last summer, Dr. L. in company with Mr. Powel sought for the latter at Newport, R. I. They found it in very great abundance at the foot of the cliffs bathed by the ocean. In its curved tubes of tenacious mud, adhering to stones, and with ito projecting tentacles, it very much resembles a ciliated polype, es- pecially Plumatella. The worm is about U lines long, demi-cylindroid, with 12 annuli, of which all except the first are setigerous. The cephalic annulus has a short proboscis ; is provided with one or two pairs of eyes, and supports six arms with about 80 ciliated tentacles. The succeeding 7 or 8 annuli are provided on each side with fascicles of from 5 to 7 setae and as many podal spines. The posterior three annuli are provided on each side with fascicles of 2 setae and from 12 to 15 short podal spines. Anterior setae terminating in a linear lanceolate blade ; posterior setae aristate. Anterior spines terminating in a hook which is dentate on its convex border; posterior spines expanded at the extremity, which is dentated on the convex border. Caudal annulus with a pair of eyes. Eyes exist in the cephalic and caudal annuli, also in the young worm. From the "want of a good description and figures of the European species of Fabricia., it was not to be determined whether the American species was different from it. January Y&tli. President Lea in the Chair. Forty-one members present. The following papers were presented for publication in the Proceedings. [Jan. NATURAL SCIENCES OF PHILADELPHIA. 3 Catalogue of Birds collected on the rivers Camma and Ogobai, Wes- tern Africa, by Mr. P. B. Duchaillu, in 1858, with notes and descrip- tions of new species, by John Cassin. Descriptions of two new species of tortoises, by John Le Conte. Geological Explorations in Kansas Territory, by F. B. Meek and F. V. Hayden, M. D., And were referred to Committees. Dr. Morris described a new species of Pomotis very common in the vicinity of Philadelphia, and characterised by a short auricular appendage and rounded caudal fin. The numbers of the rays are as follows : D. 9-10. A. 3-9. P. 9. C. 16. V. 1-5. The dorsal, anal and caudal fins are covered with spots of a lighter color than the fins themselves. The body of the fish is traversed by seven or eight blackish bands, the first passing through the eye, the second near the margin of the opercle, the third behind the pectoral, the fourth and fifth opposite the dorsal, the sixth, seventh and eighth from opposite the end of the dorsal to the root of the caudal. An opaline bluish spot is found on the opercular appen- dage, the general color of which is black. This species approaches the P. catesbei of Cuv. and Val. but is believed to be distinct. Dr. M. proposed for it the name of Pomotis guttatus. Dr. Leidy called the attention of the members to some remains of cartila- ginous fishes, discovered by Dr. F. V. Hayden and F. B. Meek, during the last summer, in the carboniferous formations of Kansas. One of these is a muti- lated dorsal spine included in a fragment of rock, from ihe upper carbonife- rous formation of Leavenworth City. The spine may perhaps belong to one of the same fishes, to which the other specimens appertain, but there was no means at present to determine this fact. It was characterised as follows : Xystracanthus arcuatus Leidy. Spine much curved ; its posterior border formiDg the segment of a circle whose diameter would be about 2 inches. Length along the convex border, when perfect, about 2| inches. Lower ex- tremity 3| lines wide. Section ovoid with the broader part posterior. Sides of the spine finely ridged longitudinally, and furnished anteriorly with small, oblique, hemi-elliptical tubercles ; posteriorly provided, on the two sides together, with six rows of odontoid tubercles, of which those of the first row on each side are minute, and of the last row are the largest. Osseous structure of the specimen brown ; odontoid tubercles invested with smooth, shining gray, ename- loid substance, demi-conoidal, those of the posterior pair of rows sometimes coalescing across the back border of the spine and assuming a crescentoid form. The second specimen was the fragment of a tooth, of a species of Cla- dodus, obtained from the Manhattan upper coal measures. It was characterised as follows : Cladodus occidentalis Leidy. Enameled crown, when perfect, about an inch in length, demi-conical ; the outer convex side provided with narrow ob- lique folds. Lateral denticles two, the outer one the larger. Base of the tooth reniform, with a breadth of about an inch, and the short diameter about 5 lines ; lateral extremities provided with a pair of large ovoid tubercles, one above the inner margin, the other below the outer margin. The third specimen is a tooth, apparently of Petalodus alleghaniensis,* from the upper carboniferous rocks, near Fort Riley. It differs from the tooth, upon which the species was originally founded, in no important point, except that it is larger. The breadth of the crown is about twenty lines ; its height on the convex side 10 lines, on the concave side 1 inch. * Journ. Acad. Nat. Sci. iii, 161. 1859.] 4 PROCEEDINGS OP THE ACADEMY OP January 25(h. Vice-President Bridges in the Chair. Forty-six members present. The Report of Proceedings of the Biological Department for the present month was read. On report of the respective committees, the following papers were ordered to be printed in the Proceedings. Description of two New Species of Tortoises . BY JOHN LE CONTE. Kinosternum Henrici. Testa regulari-ovali, convexa, dorso subcarinato, postice valde decliva, margine non dispanso, laterali perpendiculari, sterno testam non omnino occludente, cauda longa, unguiculata. Habitat New Mexico. Head and neck dusky, on the top slightly varied with paler, beneath and on the sides, including the jaws, thickly speckled with yellow. Upper jaw entire, hooked. Chin with two small warts. Legs and tail dusky, fore feet with two folds on the upper side ; hind legs squamous on the hinder side and likewise with two folds ; tail black and rather long, furnished with a long, broad and rather pointed nail. Shell brownish yellow, regularly elliptic, convex, very declivous behind, with the remains of an evident keel on the three last scut;e, anterior and posterior margins not expanded, the lateral perpendicular with a considerable furrow for the greatest part of its length. Vertebral scutae im- bricate, the first one triangular with the apex truncate, applied to the nuchal and first marginal scuta, second, third and fourth urceolate, six-sided, the lower side of the fourth very short, the fifth triangular with all the angles truncate, so as to form a six-sided figure, of which the apical side is very short, the two upper lateral sides long and incurved, the two lower lateral short and perpendicular to the base which is doubly incurved so as to form a waving line ; this scuta is applied to the two caudal marginals, the first lateral is irregularly four-sided, the second and third five-sided, the fourth four-sided, the anterior side straight, the superior oblique, the posterior curved first outward and then inward, so as to fit into the sides of the fifth vertebral and the last marginal ; the nuchal scuta is small and square ; the rest of the marginals except the last one, the caudals being excluded, are oblong, more or less angled on the top; the last one is larger than the rest, three-sided, pointed above and entering a cavity between the last vertebral and the last lateral ; the base is straight and the two sides curved ; the caudals are four-sided, the upper side curved. Ster- num large and yellow, emarginate behind, jointed before by a ligament, be- hind by a suture anteriorly closing up the box of the shell, posteriorly very partially so ; gular scuta very large, triangular, pectorals irregularly four-sided, the outer side a little wider than the inner, the lower side curved, the interior anterior angle very obtuse, the interior posterior rather acute, the two exterior right ; brachials triangular with the apex truncate, and the upper side incurved; abdominals quadrangular, the membrane joining them with the femorals so wide as to make the joint appear double, femorals quadrangular, the inner side short, caudals right angled triangular. Length of the shell 4-7 inches, height 1-9, of head and neck 2'8, of the tail 2. This new tortoise was brought from New Mexico by Dr. T. C. Henry of the United States Army, and by him through Mr. Cassin presented to the Academy. It is an old individual. It appears that when young the scutas of the back are marked with concentric striae, and no doubt the whole of the upper surface varied in some degree with darker. When the K. odoratum is found in clear water streams it is beautifully varied, thus, for instance, those found in the Ogeechee river, in Georgia, which has a sandy bottom and is seldom or never [Jan. NATURAL SCIENCES OF PHILADELPHIA. polluted with mud, they are marked on each scuta with diverging or radiating lines of dnrker. I have not adopted Mr. Agassiz's name in describing this animal, as I do not think that his arrangement of Kinosternoids founded on a proper basis. If I were to adopt his classification, I should describe three of his genera as follows, premising that I think it is offering a violence to nature to separate the two first. KlNOSTERNUM. Sternum entirely closing up the box of the shell, with eleven scutae and eight bones, there being no entosternal, but the whole piece may be divided longitu- dinally from front to rear into two pieces, which are afterwards subdivided. The sternum is bilobed, each lobe moveable from the side of the abdominals on the posterior joint of the hyosternals and the anterior of the hyosternal bones. By closing the two lobes it is enabled to cover entirely the head and limbs ; the posterior lobe being as wide as any part of the sternum, there can be of course but very small wings by which it is attached to the carapace. In fact they are scarcely perceptible. The upper jaw is most frequently hooked and the tail armed with a nail. Thyrosternum. This genus differs from the preceding in the shape and mode of attachment of the sternum to the carapace, the number of bones and of scutae is the same, but the wings are much longer; it has likewise two moveable lobes, the anterior attached by suture at the sides and by ligament in the centre ; the posterior one entirely by suture, both of them narrower than the opening of the carapace, particularly the posterior one ; consequently the animal is not able to with- draw its softer parts entirely from view. It is always emarginate behind, the upper jaw is almost always hooked, and the tail generally armed with a nail. The transitus from Kinosternum to Thyrosternum is so perfect, that it becomes difficult in some instances to say to which genus a specimen belongs. Ozotheca. Sternum very much shorter and narrower than in the other two genera, con- stituted in the same manner, but the gular plate is generally very small. It is jointed like the others both before and behind. The upper lobe is quite movea- ble, but the lower little so, inasmuch as the fourth scuta projects somewhat beyond the suture connecting this part with the abdominals, but there is a wide space above it filled with ligamentous matter, which allows of some degree of motion. This joint early in life becomes immoveable. The anterior joint in old animals is apt to become permanently soldered to the adjoining bone. The wings are longer and uarrower than in the others. The following characteristics are common to all these three genera. The chin is furnished with two or more small warts, and the feet have some folds or large scales, the fore feet on the anterior side, the hind feet on the posterior. They all have a strong musky odor. ' Although it may appear perfectly proper to separate the last genus from the two others, yet in Wagler's K. hirtipes a very near approach is made to Ozotheca, it has a very narrow sternum, emarginate behind and the branchial plate is quadrangular, very much resembling what we see in 0. odo?-ata, the jugular scuta is large and triangular, the upper jaw hooked, and the tail ungi- culate ; in these three particulars exactly like the T. Pennsylvanicum. In the young of the 0. odorata it is impossible to distinguish the sternum from that of the T. Pennsylvanicum, except by the form of the brachial scuta ; it is very remarkable, however, that the first which in the adult state has the nuchal scuta small and irregular in shape, when very young has it very large and perfectly triangular. The most of the Kinosterna and Thyrosterna have the tail armed with a nail. Whether any of the Ozotheca are thus furnished I do not know, never having had an opportunity of examining more than two species (unless Wagler's K. hirtipes is admitted to be one). Should one, however, be found 1859.] 6 PROCEEDINGS OF THE ACADEMY OE perfectly agreeing in every respect with the 0. odorata, with the tail unguicu- late, I would not hesitate to say at once, that my learned friend's division was unnatural. In all species that I have seen, except those brought from Mexico by Mr. Pease, the posterior lobe of the sternum is emarginate behind, and is but slightly moveable ; in the Mexican species, on the contrary, it is entire and capable of entirely closing up the box of the shell ; in both cases the faculty arises from the peculiar formation of the joint, being either sutural or liga- mentous. The following is the distribution according to Mr. Agassiz's system of such Kinosternoids as I have had an opportunity of examining. KlNOSTERNUM. Mexicanum, integrum, triliratum. Thyrosternum. Scorpioides, leucostomum, longe caudatum, pennsylvanicum, sonoriense and Henrici. Ozotheca. Odorata, guttata, hirtipes ? The animal, the description of which follows, was somehow omitted in my monograph in vol. vii. Proc. A. N. S.; it differs remarkably from others of Mr. Agassiz's genus Kinosternum, in having the upper jaw not hooked, and the tail not unguiculate. K. triliratdm. Head and neck above spotted with yellow, the spots on the cheeks larger, beneath yellowish irregularly varied with dusky, jaws yellow varied with black, the upper entire, not hooked. Chin with four small warts. Fore legs above dusky, beneath yellowish brown with three plicae or large scales ; hind legs cinereous brown with four large scales near the heel. Tail short, black, pointed, without a nail at the end. Shell regularly oval, brown, very convex, strongly tricarinate on the back, very declivous on the sides, the outer edge of the margin sharp and projecting, the scutae with more or less concentric striae, and others radiating from behind. Vertebral scuta? elon- gated, imbricate, emarginate behind, the first triangular with the apex some- what truncate and the base angled, applied to the nuchal and first marginal only, the second, third and fourth hexagonal, the anterior and posterior sides very short, the fourth with the two lower sides much shorter than the upper, the fifth triangular with the apex truncate and the base a little angled ; the first lateral is four-sided, the lower side with four facets, second and third pen- tagonal, fourth irregularly five-sided ; the nuchal scuta is wider at the base, the rest of the marginals square and oblong, increasing in size to the extremity of the shell : sternum yellow, varied with black, entire and rather poised be- hind, bivalved, completely closing up the box of the shell, wings very short, applied partially to the fourth and entirely to the fifth, sixth and seventh mar- ginal scuta?, all the scuta? of the sternum are concentrically striate; the gular large, triangular, pectorals irregularly four-sided, the anterior side curved, brachials triangular with the apices truncate and the base rounded, caudals right angled triangular ; inguinal scuta long, rather wide, joining the axillary. Length of the shell 5 inches, height 2-5, tail -8. Brought from Mexico by Mr. Pease. I conclude by observing that Mr. Agassiz thinks my K. Mexicanum is the same as Mr. Bell's K. Shavianum. The author last named supposed that he possessed the identical specimen from which Dr. Shaw made his figure. There can be no doubt that Dr. Shaw's figure represents my K. Mexicanum, although the shell is represented without a nuchal and without caudal marginals. Mr. Bell's species has the tternum narrower than the shell, and emarginate behind ; it undoubtedly belongs to the scorpioides. In the seventh volume of Proc. A. N. S., in my description of this species, it is said that the sternum is entire ; it is really shallowly emarginate. They [J; an. NATURAL SCIENCES OF PHILADELPHIA. 7 both belong to the genus Thyrosternum. Mr. Agassiz likewise thinks that my Emys concinna and Dr. Holbrook's E. Floridana are the same. My friend will pardon me when I say, that he probably has not had an opportunity of examin- ing my species. There is no specimen in the collection of the Academy which I can recognise as the animal once described by me. These two species are by no means alike. The E. concinna is most beautifully smooth, nothing can be more so; the E. Floridana is extremely rough with longitudinal rugae, it is besides sometimes three times the size of the other, and the marks on the head and neck are entirely different. According to this excellent naturalist the K. lonyicau- datum and K. brevicaudalum of Spix, form but one species. They differ, however ; the first has the sternum sharply emarginate behind, and the brachial scuta is narrow, triangular and very much truncate at the apex. In the other the sternum is bluntly emarginate behind and the brachial perfectly and acutely triangular. Mr. Bell's scorpioides is not the animal described so long ago under that name, as the want of the caudal nail sufficiently shews ; the specific name of this tortoise was given it on account of that appendage. Neither is it the K. brevi- caudatum nor the lonyicaudatum of Spix. This author thinks that the female tortoises have long and the males short tails ; it is just the reverse. When my son was in Honduras, he obtained a species of tortoise much larger than any that we have seen in the United States. The shell was nearly two feet long; unfortunately this was afterwards destroj'ed, but the head and limbs having been put into a jar of alcohol reached here in safety. In order to keep alive the remembrance of this animal and to induce others to look for it, I add a description of the head and tail, the only parts to which I can have access at present, premising that it belongs to the genus Emys (Ptjxhe- mys Agass.) and has the jaws serrate in the same manner as the E. niobiliensis . Emys valida. Head and neck above dusky inclining to brown, striped with yellow, the stripes on the top very few, on the sides very numerous, one of them running from the middle of the orbit to the back part of the neck, widens con- siderably after it passes the superior part of the cheek; beneath yellow with numerous lines of dusky; nose and jaws striped with yellow, jaws serrate, the lower one hooked, the upper emarginate. Tail dusky with two yellow lines on the top and three on the under side, the outer one of which on each side branches off in such a manner as to surround the vent, above which it crosses the tail transversely. Head 4 inches long, tail 3 inches. Sixty years ago, in the Tammany Museum in New York, there was the shell of an Emys three feet long ; it had been used by an Indian as a shield and had varied devices painted on it ; it was said to come from Lake Erie. Nothing like this has since been seen, but I am told that in the head waters of the Missis- sippi tortoises of an immense size and in great quantity have been observed. Since writing the above, Prof. Baird has called my attention to the Atlantic Journal of Mr. Rafinesque, where there are some remarks on the tortoises of the United States. This author names the Testudo Carolina, the Kerobates of Agassiz, Gopherus ; his Cheliphus appears to be the true Kinosternum Agassiz, the Vronyx the Thyrosternum of the same ; Didicla is the Cistudo, Chelopus is Nanemys and Cheliurus is the Chelydra. Although it has become customary to pay no attention to any thing publish- ed by this very indefatigable explorer of the productions of our country, I do not think it right when a genus or a species has been announced as suggested or discovered by him, to pass it over without notice. From an unfortunate shipwreck in which he lost every thing that he possessed in the world, he be- came disordered in his intellect. Notwithstanding his propensity for seeing differences which were not apparent to others, many of his observations are truly valuable, and no naturalist should think his labors perfect unless he has searched through the many publications of this unfortunate naturalist, and dis- covered whether or no he had been anticipated by him. No one seems ever to have looked for his Opalone, a soft shelled tortoise with five nails, found in the upper branches of the Hudson River. 1859.] 8 PROCEEDINGS OF THE ACADEMY OF / Geological Explorations in Kansas Territory. BY F. B. MEEK and F. V. HAYDEN. As it is merely our purpose, on the present occasion, to give rather briefly, the results of some geological examinations made by us last summer in eastern Kansas, it will perhaps scarcely be expected that we should here enter into a historical review of the valuable labors of other explorers in that region. Hence we proceed at once to present such facts as came under our observa- tion, and the conclusions they seem to warrant. The route pursued by us while making these investigations, was first from Leavenworth city on the Missouri, accross the country to Indianola, near the mouth of Soldier creek, on the Kansas ; thence up the north side of Kansas and and Smoky Hill rivers, to the mouth of Solomon's fork. Here we crossed the Smoky Hill, and followed it up on the south side to a point near the ninety- eighth degree of west longitude ; from which point we struck across the country in a south east direction to the Santa Fe road, which we followed north east- ward to the head of Cottonwood creek. Leaving the road here, we went down the Cottonwood valley some thirty miles, when we turned across the country nearly due northward to Council Grove. From the latter place we followed the Santa Fe road back southwestward about twenty-four miles to a watering place known as " Lost Spring ;" here we again left the road and struck across the country in a northwest direction to Smoky Hill river, at a point nearly op- posite the mouth of Solomon's fork. We then traveled down the south side of Smoky Hill and Kansas rivers to Lawrence, where we crossed the Kansas and proceeded in a northeast direction back to Leavenworth city. The first outcrop of rocks examined by us during the expedition is at a point just below the steamboat landing at Leavenworth city. At this place and for some distance above on the river, the formation is well known to belong to the upper, but not the highest portions, of the great western coal measures. The section here near the Leavenworth landing, presents the following beds, in descending order : Feet. 1. Bluish gray clay, exposing a thickness of about 3 2. Hard gray layer of Fusulina limestone l 3. Yellow laminated clay 7 4. Hard gray argillaceous limestone with Fasulina 1 5. Gray fine grained argillaceous sandstone with fucoidal markings, sometimes contains seams of limestone lto3 6. Gray, green and blue, rather indurated clay, with sometimes near the base many compact concretions limestone 2 7. Hard light yellowish gray limestone, usually of bluish tinge far in beyond the effects of weathering. Contains Spirifer cameratus, S. Ken- tuckensis, S. lineatus, Spirigera subtilita, Orthisina 3Iissouriensis, Productus splendens ? P. semireticulatus ? P. puslulosus and Fusulina cylindrica, together with colums of Crinoids, and spines and plates of Archceocidaris ; also jaws teeth of Xystracanthus arcuatus 15 8. Dark shale, passing up into gray less distinctly laminated clay 5 9. Hard dark bluish impure limestone, containing Fusulina cylindrica, Spirigera subtilita, Productus Rogersi, P. Prattenianus, Area carbonaria? an undetermined Monotis, Attorisma 9 Leavenworthensis, A. subcuneala, Mgalina subquadrata, Leptodomus granosus, and a large Belerophon lg-2 10. Gray, more or less laminated clay, becoming darker near the upper part, rising above the river 11 Attached to the surfaces of bed No. 9 there is usually from one to two inches of soft dark argillo-calcareous matter containing great numbers of Orthisina crassa, with the undetermined species of Pecten, Mytilus, Sckizodus, Pleuroto- maria, &c. All this section above No. 1 appears to vary considerably, at different places [Jan. NATURAL SCIENCES OF PHILADELPHIA. 9 some of the beds, being entirely wanting, or presenting quite different litbologi- cal characters at other localities not far from here. Owing to the dip of the strata, and partly to the fall of the river, the bed of limestone No. 7, which is elevated eighteen feet above the river where this section was taken, rises as much as twenty-five feet above the level of the river, at a distance of one mile or less below ; and on following the outcrop of these rocks along the shore above Leavenworth city, they were found to sink gradually beneath the water, so that at Fort Leavenworth landing, two miles above, (in a north direction from the exposure first examined) all of beds No. 8, 9 and 10, as well as two or three feet of No. 7, were submerged. Should this dip continue at the same rate, without local undulations, the whole of No. 7 must pass beneath the river in less than two miles above the Fort. Immediately above No. 1 of this section, we saw no exposures of rock in place, but on a small stream about two and a half miles below Leavenworth city, and perhaps one and a half miles back from the river, there is an outcrop of soft fine grained yellow sandstone, showing a thickness of twenty-four feet, underlaid by a bed of blue clay of which a thickness of about four feet was ex- posed. We had no opportunity to determine the elevation of these beds above the river with sufficient accuracy to form a definite conclusion whether or not they hold a position above the section seen near the Leavenworth land- ing, though we incline to the opinion that they come in above it. In ascending the hills back of Leavenworth city we observed no outcrops of rock along the slopes, until near the summit, where at an (estimated) elevation of about two hundred feet above the highest bed of the section at the river, there is an exposure of hard bluish-gray impure limestone, weathering to a yellowish tinge, the beds of which are separated at places, by partings of clay. Of this rock we saw a thickness of sixteen feet. It is much used for building purposes and quarried rather extensively back of Fort Leavenworth .At one of these quarries, amongst the loose material thrown out by the workmen we found specimens of Spirifer cameratus, S. Kentuckensis, S. planoconvexa, S. hemipli- cata, Spirigera subtilita, Productus semireticulatus, P. Noriooodi, Leplodomus Topekaensis, Fusulina cylindrica, Tercbratula millepunctata, and fragments of Crinoids, with Chtztetes and Fenestella of undetermined species. Above the quarry there is a slope of some forty or more feet to the summit of the hills, apparently occupied by clays ; and the quarrymen informed us that there is immediately under the bed of limestone an eight feet bed of clay, beneath which they had made no excavations. West of this locality, the surface of the country soon descends gradually into a depression connected on the north with the valley of a small stream flowing into the Missouri above Fort Leavenworth. In this immediate neighborhood the face of the country is slightly inclined to be hilly, but the soil is rich, and the long gentle slopes are clothed in the spring and summer months with a luxuriant growth of prairie grass. From several points near here, we had a fine view of the broad rich valley, with its beautiful groves and scattering farm houses along the little stream to the north of us. Beyond this, the road after passing over some undulations, ascends to the summit of the country, which is rich elevated prairie land. At several places near the upper part of the slopes some five or six miles from Leavenworth, we met with outcrops of light grey limestone, apparently in ten to twelve inch layers, containing Fusulina, Productus semireticulatus, Chcetetes, and small Cyathophylloid corals. These beds probably belong to the same horizon as the limestone near the top of the bluff's back of Leavenworth, or may even hold a higher position. At Big Stranger creek, some fourteen or fifteen miles west of Leavenworth city, the following section was abserved in descending order : Feet. 1. Slope, without any exposure of rocks, 60 2. Layers of limestone, weathering yellowish, containing Spirifer came- ratus and Fusulina cylindrica 8 1859.] 10 PROCEEDINGS OP THE ACADEMY OF 3. Slope probably occupied by shale or clay 40 4. Grayish yellow limestone, with Fusulina cylindrica and Spirigera sub- tilita 5 5. Bluish gray soft shale, or laminated clay with occasional harder sandy seams 38 6. Coal immediately overlaid by one inch of cone-in-cone J 7. Bluish gray laminated clay or soft shale, extending down to the creek 18 Again, on Little Stranger creek, some twelve miles south west of Leaven- worth city, there is a somewhat similar exposure, containing a twenty inch bed of coal. This bed is worked to some extent on the land of Mr. Charles Stone, where the following section may be seen in the descending order : Feet, 1. Light gray, or bluish gray, soft calcareous sandstone with harder layers containing much argillaceous matter, with Productus splendens ? Myalina subquadrata, an undetermined Jllonotis, and many fucoidal mark- ings ; exposing a thickness of 15 2. Blue laminated clays more or less arenaceous above 26 3. Coal If 4. Bluish gray somewhat ferruginous clay rising above the creek 4 We have no means of determining what relations the rocks composing these two sections bear to the exposure at Leavenworth, but we think- they hold a position between the bed of limestone seen near the top of the hills back of Leavenworth city, and the upper bed of the section near the Leavenworth landing. Between Big Stranger and Grasshopper creeks, the road passes over a beauti- ful rich prairie, elevated about 350 or 400 feet above the Missouri. In cross- ing this prairie we met with no exposures of rock, the whole being covered by heavy Quaternary deposits, into which wells have been sunk at several places, from thirty to seventy feet without striking solid rock in situ. At one or two places, however, we saw masses of limestone which had been quarried for building purposes along a little stream two or three miles north of the road. These contained amongst other fossils Spirifer cameratus, Orthisina umbraculum? Fusulina cylindrica, and fragments of Fenestella, with spines and plates of Archao- cidaris. We had no opportunity to examine the quarry from which this rock was obtained, but were informed that the bed is some sixty or seventy feet below the summit of the higher portions of the surrounding country. In descending from this elevated prairie into the valley of Grasshopper creek, at Osawkee village, we observed, Feet. 1. A bed of hard gray limestone near the summit of the slopes, contain- ing great numbers of Fusulina 8 2. Slope, no rocks exposed, about 55 3. Outcrop of Fusulina limestone, apparently 3 4. Slope, no rocks exposed ."." ^ 5. Gray or bluish gray limestone, weathering yellowish, containing Pleurotomaria humerosa, P. subturbinata, and a large undetermined species of Bellerophon ; also Allorisma ? Leavemuorthensis, Myalina subquadrata, Pinna undt., Spirifer cameratus, S. planoconvcza and Productus aquicostatus, with great numbers of Fusulina cylindrica 3 6. Dark gray indurated clay 2 7. Rather soft argillaceous limestone 4 The fact that several of the fossils seen here in bed No. 4 are the same spe- cies found in No. 5, of the section at Leavenworth landing, would seem to in- dicate that these beds occupy the same geological horizon. It is very difficult, however, to identify the same beds at different localities amongst these forma- tions, in consequence of the fact that the fossils found in them usually have a great vertical range, and exactly similar strata are often repeated in various parts of the series. Should it prove *o be the case that they do occupy the same geological horizon, it would show that there is here a gentle eastward [Jan. NATURAL SCIENCES OP PHILADELPHIA. 11 dip ; for the lowest bed of this section on Grasshopper creek, cannot be less than 100 feet higher than the base of the section at Leavenworth city. Still we incline to the opinion that the strata near here, if not almost hori- zontal, or merely undulating, have a general inclination towards the west, or somewhat north of west, and that the exposure on Grasshopper creek, is com- posed of much more modern beds than those near the landing at Leavenworth city. At any rate we saw an exposure at Lawrence landing, on the Kan- sas, composed of ledges of limestone, overlaid by clay, and having a decided dip to the west or north of west, at a rate of not less than fifty feet to the mile. This limestone consists of an upper hard gray layer, about three feet in thick- ness, resting on a soft gray arenaceous bed, of which some one or two feet were visible above the surface of the river when examined by us. In these beds we saw Spirigera subtilita, Productus splendens? and Myalina subquadrata. Above these, about eleven feet of gray laminated clay were exposed, the upper part of the bed having a more yellowish tinge, and containing more arenaceous matter than the lower. If these beds continue to rise at the same rate towards the east, they must of course run out on the summit of the highest part of the country not far east of Lawrence ; and the same inclination to the west or north west, would take them far beneath the horizon of the base of the section seen on Grasshopper creek. Above this exposure at Lawrence landing, there is a space of about 160 feet in which no outcrops were seen excepting some red and blue clays near the upper part of the hills, back of the town. Just above these clays, some ledges of gray limestone were seen, apparently altogether about eight feet in thick- ness, containing Fusulina cylindrica, Spirigera subtilita, and Spirifer cameratus. West of Grasshopper creek, on both sides of the Kansas, the country becomes lower near the river, but at a distance of some ten or twelve miles back, on the north side, it appears to be nearly as elevated as on the east of Grasshopper creek. Between this higher country and the Kansas, there is a plateau, appa- rently elevated not more than sixty feet above the broad level prairie bottoms along the river; while on the south of the Kansas, some five or six miles south west of Topeka, there are some isolated hills apparently of the same elevation as the high country north of the Kansas. At several places soon after crossing Grasshopper creek, we met with some highly fossiliferous beds along the small streams, at an elevation of apparently about eighty feet above the Kansas. Below we give a section of these beds seen at a locality some eight miles south west of the point where the exposures mentioned on Grasshopper creek were observed : Feet. 1. Rough seams and layers of concretionary limestone of bluish tinge with partings of clay, containing Terebr alula millepunctata, Spirigera subtilita, Spirifer cameratus, S. Kenluckensis, Retzia Mormonii, Rhynchonella Uta, Pro- ductus Norwoodii,P. splendens ?P. semireticulatus, P. Prattenianus, Orthisina, similar to 0. umbraculum, also Fenestella and Chcetetes of undetermined species 4 2. Black shale, shading upwards gradually into laminated blue clay 2\ 3. Hard blue or gray limestone, with Spirifer cameratus, Spirigera subtilita, Myalina, Fecial, c 1 4. Bluish gray soft clay, with seams of hard limestone 3 5. Light gray, somewhat granular limestone with a few round grains, and very small pebbles of quartz 2 At another place on the south side of the Kansas, about twelve miles south west of the point where the last section was seen, there is an abrupt bluff near the old Baptist Mission, composed of the following beds in the descending order : Feet, 1. Slope, no rocks exposed 20 2. Hard yellowish gray limestone, with fragments of fossils 4 3. Slope, no rock exposed IS 1859.] 12 PROCEEDINGS OF THE ACADEMY OF 4. Light gray, rather hard fine grained sandstone 3 5. Slope 20 6. Fine grained sandstone, in thin layers, not well exposed apparently 2 7. Slope, with occasional outcrops hard gray limestone 16 8. Yellowish and dark gray laminated clay, or soft shale, with layers and nodular concretions of argillaceous carbonate of iron, near base* 90 9. Hard bluish argillaceous limestone, of which there was exposed in the bed of a small stream, not more than 13 or 15 feet above the river, a thick- ness of 1 After passing this locality, we heard of a coal mine some three or four miles south of here, near the base of an isolated hill, known as Shunganunga Mound. We did not visit this mine, but were informed that it is considerably above the summit of the last section, and that the bed is about 18 inches in thickness. The coal is said to be of good quality. Above here on both sides of the Kansas, the country continues to be rather low, no part of it being apparently more than two hundred feet above the river. For a long distance above this, there is a beautiful broad, level bottom prairie, on the nonh side of the Kansas, extending back from four to six miles, and as much as eighteen or twenty miles along the river. Bounding this on the north, the country rises by a gentle grassy slope to an elevation of from sixty to about one hundred feet, furnishing the most beautiful sites for dwelling houses. For a considerable distance above the locality where the exposure near the old Baptist Mission was examined, the hills especially near the river on the south side, appear to be mainly composed of rather heavy deposits of laminated clays and shales, with soft sandstones and occasional thin beds of limestone, containing the usual fossils of the upper carboniferous series. At the crossing of Mission creek, at an elevation of perhaps not more than twenty-five or thirty feet above the Kansas, exposures were observed consisting first above of five feet of light gray laminated clay, resting upon two or three feet of soft yellow sandstone, which passes down into laminated arenaceous clays, of which some eight or ten feet were exposed above the creek. Some fifteen or sixteen miles west of the point where the road crosses Mis- sion creek, at a locality six or seven miles south of the Kansas, there is a high elevation known by the name of Buffalo mound, rising as much as four hun- dred and fifty or sixty feet above the river. At one place a large creek called on the maps, Upper Mill creek, sweeps close along the northern base of this elevation, and has carried away the loose debris so as to leave the lower strata well exposed. The section here beginning at the summit of this hill is, Feet. 1. A slope of about 160 feet, along the lower forty feet of which we found loose specimens of Spirifer cameratus, S. planoconvexa, Eetzia Mor- monii, Productus splendens? Chenctes Verneuiliana, C. mucronata, and Fusulina cylindrica, var. veniricosa, with fragments of Chcetetes, Crinoids, c, of unde- termined species 2. Bluish gray limestone in two layers, the upper of which contains columns of Crinoids, Productus Calhounianus, #c, while Myalina subquad- rata, Orthisina Missouriensis, Allorisma, Pinna, Monolis, Sfc, of undetermined species, occur in the lower 3 3. Slope with no exposures of rock 96 4. Rather hard mottled brown and light gray compact limestone, with a few Orinoid columns ; may be thicker, but only showing a thickness of.... 3 5. Brown, whitish and green clays, with rugged white calcareous con- cretions 4 6. Fine argillaceous sandstone, with streaks of yellow and brown colors.. l 7. Ash colored clay 10 *There may be some thin beds of limestone in this portion of the section, as every part of this ninety foot bed was not well exposed, [[Jan. NATURAL SCIENCES OF PHILADELPHIA. 13 8. Clays of red or brownish colors above ; blue and green below 3| 9. Deep brown clay, with rugged concretions of same color ... 3 10. Hard light bluish limestone, with some rather large columns of Crinoids, Choneles, Vernez/iliana, Sfc 2J 11. Brown, ash colored, and blue laminated clays, which are more or less arenaceous, with near the middle some 5 or 6 inches black shale 46 12. Gray and purple argillaceous limestone, with Pinna, Productus, and a few Fusulina 1^ 13. Green laminated clay 4 14. Two or three layers of soft fine grained sandstone, more or less ar- gillaceous, and separated by seams of clay 2 15. Bluish and ash colored clays 21 16. Alternate layers of hard bluish gray limestone, and seams of clay with sandy concretions 3 17. Rather hard yellowish limestone, with Fusulina 2 18. Ash colored clay, not very well exposed 15 19. Yellowish impure limestone with Fusulina 2 20. Ash colored laminated clays above the creek 5 About three hundred yards below where this section was taken, the creek was observed to fall nearly a foot, over a ledge of hard limestone ; and one mile further down, the bed of the creek is composed of a hard yellow lime- stone containing great numbers of Fusulina. At these localities Mill creek is probably not elevated more than thirty feet above the Kansas. Near half a mile east, or south east, of the point where the Fusulina lime- stone was seen in the bed of Mill creek, and at a somewhat higher elevation, we saw apparently the same bed of Fusulina limestone showing a thickness of three feet. Under this there was at one place exposed a thickness of some four or five feet of very fine yellow sandstone with minute specks of Mica. These exposures indicate a moderate dip of the strata towards the west or north west. On the north side of Kansas, in a direction a little west of north, and about sixteen miles from the last mentioned localities, we observed an outcrop on a small stream marked " Last Creek" on the maps, presenting the following sec- tion, descending : Feet. 1. Seams yellow magnesian limestone, alternating with clay, showing a thickness of about 8 2. Yellow soft granular magnesian limestone, containing Productus Nor- woodi, and an undetermined species of Myalina 4 3. Fine laminated black shale 1 4. Gray rather soft argillaceous limestone 1 5. Blue somewhat indurated very fine calcareous clay containing at its junction with the next bed below, Chonctes, Synocladia biserialis, Chcstetes, and fragments of Crinoids 9 6. Seams hard, compact gray limestone, alternating with softer argillo- calcareous matter, and containing casts of many small Cypricardia-like shells, small Murchisonia, Pleurotomaria, Macrocheilus, Naticopsis, Bcllero- phon } &c 2 7. Bluish laminated clays weathering to drab color 4 8. Yellow rather soft granular magnesian limestone, with embedded fragments of harder more compact do o 9. Bluish indurated calcareous clays 3 The base of this section is evidently not elevated much above the Kansas, as it extends down to the bottom of a deep ravine formed by the creek, while its top appeared to be nearly on a level with the surface of the bottom prairie in the Kansas valley. These beds dip a little to the north west, and are very si- milar, especially the magnesian limestones, to some of the Permian strata hold- ing a position far above this in the series, some considerable distance west of 1859.] 14 PROCEEDINGS OF THE ACADEMY OP here. Only about three miles further west, we saw the following exposure on Vermilion creek : Feet. 1. Slope of about fifteen feet, with near the base some ledges of gray lime- stone, amongst loose fragments of which we picked up specimens of" Spiri- gera subtilita, Spirifer hemiplicata, Productus Norwoodi, and P. splendens? ... 15 2. Slope, no rock seen 26 3. Soft bluish and gray more or less laminated clays with irregular sandy seams and concretions 12 4. Irregular hard blue calcareous seam one to six inches & 5. Blue clay 2 6. Soft decomposing more or less laminated sandstone 4 7. Blue clay one foot above the creek 1 Almost directly opposite these localities, on the south side of the Kansas, some three or four miles back from the river, and nearly on a line between the locality where we saw the exposures on " Last Creek " and Buffalo mound, but considerably below the level of the summit of the latter, we examined some exposures presenting beneath a slope of about eighty feet, in descend- ing order : Feet. 1. Hard bluish gray limestone of which there was exposed 1 2. Rough yellowish magnesian limestone with cavities lined with chal- cedony 3 3. Bluish and ash colored clays 5 4. Layer much like No. 2 1 5. Yellowish green clay 20 6. Bluish gray limestone in two layers, the upper of which contains columns of Crinoids, Productus Calhounianus, &c, while Myalina subquad- rata, Orthisina Missouricnsis, Allorisma, Pinna, Monotis, &c, occur in the lower 3 7. Bluish and ash colored clays exposing a thickness of 5 The bed No. 6 of this section is evidently the same as No. 2 of the section at Buffalo mound (page 12), though here the dip of the strata has brought it lower. Its elevation above the Kansas at Buffalo mound must be about two hundred and fifty feet. "We had no means of estimating very accurately its elevation where the last section was taken, though we do not think it as much as one hundred and seventy-five feet above tbe Kansas. Ten miles farther west, on the same side of the river, along a small, stream marked " Deep creek " on the maps, at a point some four or five miles back from the Kansas, and elevated perhaps as much as forty feet above it, some outcrops were examined near Zeandale, presenting the following section, de- scending : Feet. 1. Long slope of about one hundred feet, no rocks seen 100 2. Dark argillaceous limestone, stained with iron, and containing frag- ments of Crinoids 4 3. Soft decomposing argillaceous limestone 2 4. Very hard light yellow compact limestone in one massive bed, con- taining great numbers of Fusulina, also Productus Calhounianus, &c 6 5. Ash-colored laminated clay 22 6. Hard decomposing argillaceous limestone with Fusulina 3 7. Blue, green, and ash-colored clay 18 8. Gray argillaceous limestone, with more or less ferruginous matter... 3 9. Light bluish clay somewhat laminated..... 7 10. White decomposing argillaceous limestone with Productus Calhoun- ianus 1 We heard of a bed of coal some four or five miles above this on the same creek, but were unsuccessful in an attempt to find the locality where it crops out. We were informed, however, by Mr. Pillsbury, an intelligent gentleman [Jan. NATURAL SCIENCES OP PHILADELPHIA. 15 living at Zeandale, that the bed is from four to six inches in thickness, and overlaid by about three and a half feet of blue shale, strongly impregnated with alum. Above the latter, he said there is an eight or ten inch layer of dark argillaceous material, weathering to an iron rust color, and containing many nodular concretions, perhaps of carbonate of iron. From the information obtained in regard to the location and elevation of this coal bed, we are in- clined to believe it must hold a position a little below the horizon of the mid- dle of the slope at the top of the foregoing section. It is probably the highest bed of coal in the whole series of this region, at any rate we saw no indications of coal above it. About a mile or a mile and a half north of the locality where this coal bed has been seen, the dividing ridge between the Kansas and Deep creek, rises to an elevation of near three hundred and twenty feet above the latter stream at the nearest point. Here at the summit of this ridge there are some thin out- crops of gray and whitish argillaceous limestone, showing on weathered sur- faces a somewhat laminated structure, and containing at places large spines of a species of Archaocidaris ; beneath this there is about two feet of gray frag- mentary limestone reposing on a more compact bed of hard gray limestone near three feet in thickness, and often cellular in the middle. Along the slope about one hundred and twenty feet below the horizon of these beds, we found loose specimens of Spirifer cameratus, Orthisina wnbraculum? Rhynchonella Ula,Al- lorisma, Synocladia biserialis, &c. Just below these, there were many loose slabs of light yellowish fine grained calcareous sandstone, containing Productus, Pecten, and Fucoidal markings. About forty-seven feet lower down the slope, and near one hundred and fifteen feet above the level of the Kansas, there is an exposure of light grayish yellow granular limestone, showing a thickness of three feet, in which we only saw fragments of a Choneles, and Crinoid columns : large tabular masses of this rock were strewed along the slope for some distance below. At the mouth of Big Blue river, on the south side of the Kansas, there is an abrupt bluff, along which several slides have exposed many of the beds com- posing the high ridge mentioned six or seven miles below here. The dip, how- ever, of the strata towards the west, or north west, is so great that the lime- stone containing spines of Archceocidaris, seen on the summit of the ridge be- low this, at an elevation of about 320 feet above the Kansas, is here, opposite the mouth of Big Blue river, only elevated about 214 feet above the Kansas ; consequently the three feet of grayish yellow limestone cropping out 115 feet above the Kansas along the slope of the ridge above mentioned, at the mouth of Blue river, has sunk beneath the level of the Kansas. This far we have scarcely attempted to draw parallels between the various beds seen by us at different places, in consequence of the fact that our obser- vations were isolated, as must necessarily be the case in a mere reconnois- sance, extended over a large area in a short space of time. In addition to this, the group of rocks examined presents no extensive beds of limestone or other hard material, forming well marked horizons, or continuous lines of outcrop, by which the relations between strata seen at different localities could be traced out. This difficulty is also greatly increased by the frequent repetition of pre- cisely similar beds at different horizons in the series, and above all by the great vertical range of the organic remains. Consequently we have pre- ferred to present separately the local sections examined, instead of attempting to construct a continuous general vertical section showing the order of super- position of the various strata. To do this successfully throughout all the va- rious rocks of the whole Kansas valley, would require much more time than we had at our command. As our examinations along the Kansas and Smoky Hill rivers above this point were made in more detail, where the outcrops were more frequent and continuous, we have, as we believe, been able to trace out the connections and order of succession of the various strata with considerable accuracy. Hence, we give below a general section of the rocks in this region, commencing with 1859.] 16 PROCEEDINGS OP THE ACADEMY OF the Cretaceous sandstones on the summits of the Smoky Hills, lat. 38 30 / N., long. 98 W., and descending through the various intermediate formations seen along the Smoky Hill and Kansas rivers, to the base of the bluff already mentioned, opposite the mouth of Big Blue river, on the Kansas. It is true, there are a few gaps in this section, where we were unable to see the beds along some of the slopes, but as we know the position in the series, as well as the extent of these gaps, it will be easy to determine, when a greater number of exposures have been examined, the nature of the beds occupying them. General section of the Rocks of Kansas Valley from the Cretaceous down, so as to include portions of the upper Coal measures. Feet. 1. Red, brown, and yellowish, rather coarse grained sandstone, often obliquely laminated, and containing many ferruginous concretions ; also, fossil wood and many leaves of dicotyledonous trees, some of which belong to existing genera, and others to genera peculiar to the Cretaceous epoch. Locality, summit of Smoky Hills 60 2. Whitish, very fine grained argillaceous sandstone, underlaid by bluish purple and ash colored clays. Locality same as preceding 15 3. Long, gentle slope, with occasional outcrops of ash colored red, blue, and whitish, more or less laminated clays, with thin beds of sandstone. Locality same as preceding, and extending down at places nearly or quite to the bluffs of Smoky IIUl river; thickness about 200 4. Red sandstone, with some layers of hard, light gray calcareous, do., and both containing ferruginous concretions. Locality, bluffs Smoky Hill river, five or six miles above Grand Saline river. Probably local, thick- ness seen about 15 5. Bluish, red, light yellow, and gray clays, and soft claystones, with sometimes a few thin layers of magnesian limestone. In many places these clays have been traversed in every direction by cracks, into which calcareous and argillaceous matter have found their way, and subsequently become consolidated so as to form thin seams of impure yellowish limestone, which cross and intersect each other at every angle. The red clays are usually less distinctly laminated, contain more arenaceous matter, and often show ripple marks on the surfaces. Locality, Bluffs along Smoky Hill river, above the mouth of the Grand Salme 60 6. Light gray, ash colored, and red clays, sometimes arenaceous, and often traversed by cracks, filled with calcareous matter as in the bed above, alternating with thin layers and seams of gypsum. Locality, near mouth Smoky Hill river 40 7. Rather compact amorphous white gypsum, with near the base dissemi- nated crystals, dark colored do. Locality same as last 4 -J to 5 8. Alternations of ash colored, more or less arenaceous clays, with thin beds and seams of gypsum above ; towards lower part, thin layers of clay- stone, and at some places soft magnesian limestone. Locality same as last.. 50 9. Rough conglomerated mass, composed of fragments magnesian lime- stone and sandstone, with sometimes a few quartz pebbles, cemented by calcareous and arenaceous matter ; variable in the thickness and probably local. Locality, south side Smoky Hill river, ten or twelve miles below Solo- mon's Fork seen 18 10. Bluish, light gray, and red laminated clays, with seams and beds of yellowish magnesian limestone, containing Monotis Hawni, Myalina perat- tenuata, Pleurophorous? subcuneata, Edmondia"? Calhouni, Pecten undt. and Spirigera near S. subtilita ; also Nautilus eccentricus, Bakevellia parva, Leda subscilula, Axinus rotundatus, and undetermined species of Eellerophon, Murchisonia, $c. Locality, near Smoky Hill river, on high country south of Fort Riley, as well as on Cottonwood creek 90 11. Light grayish and yellow magnesian limestone, in layers and beds sometimes alternating with bluish and other colored clays, and containing [Jan NATURAL SCIENCES OF PHILADELPHIA. 17 Solemya, a Myalina near M. squamosa, Pleurophorous? subcuneata, Bakevellia parva, Pecten undt., and a Euomphalus near E. rugosus ; also, a Spirigera allied to S. subtilita, but more gibbous, Orthisina umbraculum? 0. Shumardi- ana, &c. Locality, summit of the hills, near Fort Riley and above there ; also seen on Cottonwood creek 25 to 3." 12. Light grayish yellow, rather granular magnesian limestone, con- taining spines and plates of Archaocidaris ; a few fragments of small Crinoid columns, Spirifer similar to S. linealus, but perhaps distinct ; 'also same Spirigera seen in beds above, Orthisina Shumardiana, 0. umbraculum? and Pro- ductus Calhounianus. Forms distinct horizon near summit of hills in vicinity of Fort Riley, also seen on Cottonwood creek 7 to 8 13. Soft argillo-calcareous bed, apparently local. Kansas Falls 5 14. Light grayish and yellowish magnesian limestone, containing many concretions of flint, also the same Spirigera found in beds above, and Pro- ductus Norwoodi P. Calhounianus, with Discina tenuilineata and an undeter- mined Monotis. Fort Riley and below, also at Kansas Falls and on Cotton- wood creek 38 15. Alternations, bluish, yellowish and brown clays, with a few thin seams of limestone. Fort Riley, Kansas Falls; also beloiv Fort Riley, and on Cottonwood creek 35 16. Light yellowish magnesian limestone, containing fucoidal markings, fragments of small Crinoid columns, Pecten, Allorisma, Spirigera, Orthisina umbraculum? 0. Shumardiana, Discina tenuilineata, c. Lower quarry at Fort Riley, and at other places above and beloiv Fort R., as well as on Cottonwood creek 4 to 17. Alternations of blue, red, and light gray clays, with sometimes thin layers and seams of magnesian limestone. Fort Riley 28 18. Light gray and whitish magnesian limestone, containing Spirigera, Orthisina umbraculum? 0. Shumardiana, Productus Calhounianus, Acantho- ctadia Americana, and undt. sp. Cyathocrinus. Lower part containing many concretions of flint. Fort Riley and on Cottonwood creek. Whole thickness about 40 19. Brown, green, and very light gray clays, alternating ; contains near the upper part fragments of Crinoid columns, Synocladia biserialis, spirigera, Productus Norwoodi, Chonetes mucronata, Orthisina Shumardiana, Orthisina umbraculum, fix., with teeth of Petalodus Alleghaniensis. Fort Riley 14 20. Alternations of rather thin layers light yellowish magnesian lime- stone, and various colored clays ; the limestone layers containing 3Ionotis, Synocladia biserialis, <$fc. Locality same as last 33 21. Slope, no rocks seen. Beloiv Fort Riley 25 22. Whitish, or very light gray magnesian limestone, rendered porous by cavities left by the weathering out of numerous Fusulina. This is the high- est horizon at which any remains of Fusulina were met with. Some four miles below Fort Riley, along a creek on the south side of the Kansas, and appa- rently not more than ten feet above it 2 23. Bluish, light gray, and brown clays, with occasional layers of mag- nesian limestone. Chonetes mucronata, Orthisina umbraculum? Monotis, Fu- sulina, Qc. Ten miles beloiv Fort Riley 35 24 Hard, very light yellowish gray magnesian limestone, with Fusulina, and spines of Archaocidaris. Forms a marked horizon near the same locality as last 6 25. Slope, with occasional exposures, thin layers of Fusulina, limestone, and seams of gray limestone containing Myalina, Monotis, Pecten and frag- ments of Synocladia biserialis. Near same locality as last 36 26. Light gray argillaceous limestone, showing on weathered surfaces a somewhat laminated structure; contains large spines of Archaocidaris. Near Ogden Ferry, and Manhattan 9 27. Gray limestone, often fragmentary, with much clay above ; lower part hard, and more or less cellular in middle. Locality, same as last 5 1859.] 18 PROCEEDINGS OF THE ACADEMY OF 28. Whitish clays and claystones, with a thin layer of hard compact gray limestone near the middle. Locality same as last 10 29. Light greenish indurated clays. Same locality.. 3 30. Hard, heavy bedded, white argillaceous limestone, containing Mono- lis and Avicula. Ogden Ferry, and below there 5 31. Very thinly laminated dark green shale. Three miles nearly east of Ogden Ferry, on McDoioelVs creek ; also at Manhattan, on the Kansas 1 32. Light greenish and flesh-colored hard argillaceous limestone, with Spirifer cameratvs. This is the highest horizon at which we found this species. Same localities 3 33. Alternations of bluish, green, and red more or less calcareous lami- nated clays, light gray limestones and claystones, with Pecten, Monotis and fragments of Crinoid columns. Same localities 30 34. Alternations bluish, purple, and ash colored calcareous clays, passing at places into claystones, and containing in a thin bed near the middle, Spirifer planoconvexa, Spirigera subtilita, Productus splendens? Rhynchonella Uta,kc. Locality same as preceding 12 35. Blue, light gray, and greenish clays, with occasional harder seams and layers of claystone and limestone. Same locality 33 36. Somewhat laminated claystone of light gray color, with more or less calc spar near lower part. Manhattan 19 37. Alternations of dark gray and blue, soft decomposing argillaceous limestone, with dark laminated clays, or soft shale, containing great quan- tities of Fusulina cylindrica, F. cylindrica, var. ventricosa, Discina Manhattan- ensis, Uhoztetes, and fragments Crinoids; also, Choneles, Verneuiliana, C. mucro- nata, Productus splendens? Retzia Mormonii, Rhynchonella Uta, Spirigera subti- lita, Spirifer cameratus, S. planoconvexa, Euomphalus, near E. rugosus and Synocladia biserialis ; also Cladodus occidentalis. Locality , same as last 18 38. Soft bluish shale, with yellow laminated arenaceous seams below, containing Fucoidal markings. Same locality 25 39. Two layers gray argillo-calcareous rock, separated by two feet of dark green and ash colored clays. The calcareous beds contain fragments of Crinoids, Chonetes, and Myalina of undt. species. Same locality as last... 4J 40. Light greenish, yellow, and gray clays and claystones, extending down nearly to high water mark of the Kansas, opposite the mouth of Blue River 27 The foregoing general section of the strata seen along the valley of Kansas and Smoky Hil! rivers, from the mouth of Blue river to the 98th degree of west longitude, is presented in its present form more with a view of illustrat- ing the vertical range of the organic remains found in these rocks, than as an attempt to group the beds into formations that may be expected to preserve their distinctive lithological characters throughout areas of any great extent. As this has necessarily been done from a knowledge of only a portion of the fossils characterizing these strata, it is quite probable, when more extensive collections are obtained, that it may be found necessary even on this principle, to classify and group the beds somewhat differently. We are also aware that, some of these beds probably increase or diminish greatly in thickness, or may even entirely thin out, at no very great distances from the localities where we saw them. Among the more peculiar features of the series of rocks represented by this general section, and in part by the preceding local sections, may be mentioned first, the great number of thin layers and beds ; and secondly, the frequent repetition of similar beds at various horizons. Again, the almost entire ab- sence of heavy massive strata of limestone, or other hard material possessing sufficient durability to form perpendicular escarpments of much extent, is worthy of note. As a general thing, the limestones vary from only a few inches in thickness, to from one to three or four feet, and rarely, as in Nos. 14 and 18, attain a thickness of from thirty-eight to forty feet. Although various light colored laminated clays, and soft argillaceous shaly beds predominate, and [Jan. NATURAL SCIENCES OP PHILADELPHIA. 19 arenaceous material is not unfrequently present, it is somewhat remarkable, that dark bituminous shales and beds of coal are rarely met with, even among the outcrops seen along the Kansas, below the mouth of Blue river, belonging to the upper coal measures, and holding a position below the base of the fore- going general section ; while through a considerable thickness of beds belong- ing to higher portions of the coal measures included in the lower part of this section, as well as through the strata containing Permian fossils above, beds of coal and dark carbonaceous shales appear to be almost, if not entirely wanting. It will be observed we have in this general section, without attempting to draw lines between the systems or great primary divisions, presented in regular succession the various beds with the fossils found in each, from the Cretaceous sandstone on the summits of the Smoky Hills, down through several hundred feet of intermediate doubtful strata, so as to include the beds containing Permian types of fossils, and a considerable thickness of rocks in which we find great numbers of upper coal measure forms. We have preferred to give the section in this form because, in the first place, the upper Coal measures of this region pass by such imperceptible gradations into the Permian above, that it is very difficult to determine, with our present information, at what particular horizon we should draw the line between them, while on the other hand, it is equally difficult to define the limits between the Permian and beds above, in which we found no fossils. Beginning near the base of this section, we find we have in great numbers the following well known and widely distributed Coal measure fossils, viz. : Fusulina cylindrical Chonetes Verneuiliana, Productus splendens, (or a closely al- lied species,) Retzia Mormonii, Rhynchonella Uta, Spirigera subtilita, Spirifer ca- meratus, S. planoconvexa, and a Euomphalus similar to E. rugosus of the Coal measures, while the few new and undetermined species associated with these, are, tor the most part, also decidedly more nearly allied to Carboniferous than Permian forms. We should here remark, however, that we occasionally met with a species of Monotis, allied to the Permian species M. Speluncaria and Sy- nocladia biserialis, also regarded in the old world as a Permian genus, at horizons far beneath the base of this section, between Manhattan and the Missouri. We even found a single specimen of this Monotis as low down as bed No. 9, of the section taken near the landing at Leavenworth City, which must occupy a position several hundred feet below the lowest beds of the above section. Still as this shell is very rare in these lower rocks, and the Synocladia is a distinct species from the well known Permian form of the old world, while they are both, at these horizons, associated with great numbers of the common well known Coal measure species we can only regard their presence in these beds as establishing the existence of these genera at an earlier period in this country, than in the old world. This, it seems to us, is more philosophical than it would be to place all this great thickness of strata, with their vast numbers of well known Coal measure species, in the Permian, merely because we also find with these occasionally a few forms which would in the old world be regarded as characteristic of the Permian epoch. Taking it for granted then, that we have carried this section down far enough to include, not only all the beds containing almost exclusively Permian forms, but a considerable portion of the upper Coal measures, it will be interesting to notice, as we ascend in the series, how far each of the Coal measure species mentioned in the lower part of the section, as well as of a few others that occur above and below, range upwards. Thus we see that Fusulina cylindrica var. Ventricosa, Chonetes Verneuiliana and Retzia Mormonii were not met with above division No. 37 ; while Spirifer planoconvexa,Productus splendens ? and Rhynchonella Uta, were not observed above 34, nor Spirifer cameralus above 32. Fusulina * In Russia, Fusulina cylindrica is said to occur only in the upper part of the lower Carboniferous series; but the fossil generally referred to that species in this country, appears to be confined to the Coal measures. We have some doubts in regard to it* identity with the Russian species. 1859.] 20 PROCEEDINGS OF THE ACADEMY OF cylindrica, of the slender variety so common in the Coal measures of Kansas and Missouri, was not seen above 22; nor was any species or variety of that genus observed above this horizon. Apparently, the same species of Monotis, mentioned at various horizons far beneath, were occasionally met with in 30, 25, 23, and 20, generally associated with the same species of Synocladia, ranging far down into the upper Coal measures. In division No. 19, we again met with the Synocladia biserialis, and a Spirigera allied to S. subtilita, if not identical, along with a new species of Chonetes we have called C. murcronata, which ranges down into the beds near the base of the section. Along with these, were also Productus N~orwoodi, and Orthisina, Shumardiana, both of which are common in the Coal measures far below, and a large Orthisina similar to 0. umbraculum, but apparently more findy striate. Ascending through the intermediate beds to No. 12, we continue to meet with nearly all the species mentioned in 19, with the exception of Chonetes mucronata. We also have, first in 18, a large species of Productus, called P. Calhounianus by Professor Swallow ; very similar to some varieties of P. semireticulatus, but thought by Prof. S.,to present well marked internal differences. There is likewise added in 16, a large Allorisma and a Spiriger similar to S. subtilita, hut much more gibbous ; and in 14, Distina tenuilineatus, together with apparently the same Monotis, so often mentioned below. In 12, we also have added a small Spirifer, similar to S. lineatus, but perhaps more nearly allied to the Permian species Martinia Clannyana, King. The succeeding bed above, No. 11, appears also to contain a mingling of Permian with Coal measure forms, for we have in it the following Permian types, viz.: My aim a very similar to M. Squamosa, Pleurophorus ? subcuneata, Bakevellia parva and Monotis Haumi along with a Euomplialus near E. rugosus, the same gibbous Spirigera, similar to S. subtilita, Orthisina umbraculum? and O. Shumardiana. On passing into the next division above, No. 10, we find we have lost sight of all the characteristic Carboniferous forms, unless the Spirigera mentioned in some of the beds below be regarded as only a variety of S. subtilita, from which however, we think it specifically distinct ; for with this exception, nearly all the fossils seen by us in this division, are such as would be regarded as Permian types. Although the number of species found by us in No. 10 is not great, individual specimens are often numerous. Above this horizon we saw no more fossils through a great thickness of various colored clays, claystoues, &c, until ascending to the Cretaceous sandstones crowning the Smoky Hills. If we do not admit the existence in this region of an intermediate group of rocks, connecting by slight gradations the Permian above, with the Coal meas- ures below, and must draw a line somewhere, below which all is to be regarded as Carboniferous, and all above as Permian, we should certainly, upon palae- ontological principles alone, carry this line up as far as the top of division No. 11. The passage from the Carboniferous to the strata, containing Per- mian types, however, is so gradual here, that it seems to us no one, under- taking to classify these rocks without any knowledge of the classification adopted in the old world, would have separated them into distinct systems, either upon lithological or palaeontological grounds, especially as they are not, so far as our knowledge extends, separated by any discordance of stratifica- tion, or other physical break.* Indeed the fact that some of the Permian types occurring in No. 10, were first introduced in beds below this, containing many Carboniferous species, would seem to indicate that even No. 10, may possibly * We have been informed by Dr. J. G. Norwood, former State Geologist of Illinois, that the rocks in that State, referred by him and others to the same epoch as the Kansas Permian beds, rest unconformably upon the Coal measures. This, however, would be impossible in Kansas, since no disturbances of the strata occurred there, until after the close of the Cretaceous era, which would, of course, not only cause the Cretaceous and Carboniferous, but all intermediate beds, to dip at the same angle. [Jan. NATURAL SCIENCES OF PHILADELPHIA. 21 have been deposited just before the close of a period of transition from the con- ditions of the Carboniferous, to those of the Permian epoch. The apparent absence of fossils in the beds above No. 10, renders it impossi- ble, with our present information, to determine with certainty the upper limits of the series containing Permian forms. It is true, there is at places a kind of conglomerated mass, occupying the horizon No. 9, which might appear to form a natural line of division between the beds containing the Permian fossils, and those above, in which we found no organic remains ; but this seems to be local, and although there is a new feature presented by the zone of gypsum deposits above it, we find between the beds and layers of gypsum, and far above the horizon at which they occur, bluish, greenish, and other colored clays, not only similar to those between the beds and layers of limestone containing the Permian fossils in division No. 10, but also precisely like the laminated clays between the beds of limestone of the upper Carboniferous series far below. Again, in these clays of the gypsum zone, as well as through a considerable thickness of clays above it, there are occasional seams of clay- stone, which sometimes pass into seams of magnesian limestone, exactly like some of those containing Permian fossils, in division No. 10. We saw no fossils in these seams amongst the gypsum bearing beds, nor higher in the series, but it is probable they may yet be found in some of the more calcareous portions. Another fact apparently indicating some kind of relation between the gypsum- bearing beds, as well as some of the higher deposits, and the rocks below, is, that we often find both in the clays between the beds of gypsum, and those between the limestone containing the Permian fossils, the same peculiar appear- ance caused by the cracking of the clays and subsequent infiltration of calcare- ous matter, seen in division No. 5. At some places the thin plates of limestone formed by the impure calcareous matter filling these cracks, may be seen rami- fying through some rather thin beds of these clays in all directions, so as to cross and intersect each other at every angle. Where beds of this kind have been exposed for any length of time along near the tops of bluffs, the softer clays filling the interstices, often weather out, so as to have a curious cellular mass, with the numerous angular cavities. From these fact3 we are inclined to suspect, though we are fully aware that it is a question which can only be determined upon evidence derived from or- ganic remains, that not only the gypsum-bearing deposits, but a large portion, if not all, of division No. 5, belongs to the same epoch as the beds containing the Permian fossils below. Between No. 5, and the Cretaceous above, there is still a rather extensive series of beds in which we found no organic remains ; these may be Jurassic or Triassic, or both, though as we have elsewhere suggested, we rather incline to the opinion that they may prove to belong to the former. As we have fully discussed the question in regard to the Cretaceous age of the highest division of the foregoing section in a paper read before the Academy in December last, and in an article in the American Journal of Science, January, 1859, it is un- necessary for us to add any thing further on that subject here. As already stated, our observations along the Kansas valley, to within twelve or fourteen miles of the mouth of the Big Blue river, were too isolated to a deter- mine in all cases the relations between outcrops seen at different places. Con- sequently, although we saw at several points along this part of the valley, in- dications of a westward or north-westward inclination of the strata, we were left in some doubt whether or not there is a general inclination of the rocks in that direction, between Wabounse and the Missouri. Above this point, how- ever, our observations being more connected, and the exposuies more continu- ous, we were able to determine very satisfactorily that there is at least from near Wabounse, a uniform dip towards the west or north-west, so that in as- cending the Kansas valley from this region, we are constantly meeting with more and more modern rocks, as those we leave behind pass beneath the level of Kansas. 1859.] 22 PROCEEDINGS OF THE ACADEMY OF To illustrate this more clearly, we would, in the first place, remark that a bed of light greyish yellow granular magnesian limestone, mentioned on page 12, as occupying a horizon about 115 feet above the Kansas, two or three miles west of Zeandale, passes beneath the level of Kansas before reaching the mouth of the Big Blue river, a distance of near seven miles ; while another bed (No. 26 of the foregoing section) seen on the very summit of the hills two or three miles north of Zeandale, at an elevation of about 320 feet above the Kansas, was observed opposite Manhattan at the mouth of Big Blue river, only some 214 feet above the Kansas. Again, bed No. 12 of the foregoing general section, which was seen at a locality nearly opposite Ogden, at an elevation of about 363 feet above the Kansas, is at Fort Riley, eight or nine miles further west, elevated only some 215 feet above Kansas. Above Fort Riley tbis bed forms a marked horizon, and can be followed by the eye without interruption for several miles along the hills on both sides of the river. We observed it gradually sinking as we ascended the Kansas valley, until at a point on Chap- man's Creek, some fifteen miles a little south of west from Fort Riley, we saw it nearly down on a level with the Kansas ; beyond this it was not again met with on the noith side of the Kansas, but we saw it at somewhat higher elevations on the south side of the river a little west of this. As the distance by an air-line, from the locality nearly opposite Ogden, where this rock occupies a horizon at an elevation of 363 feet above the Kansas to the mouth of Chapman's Creek, is about 23 miles, the dip would appear to be not far from 15^ feet to the mile. It must be borne in mind, however, that the average fall of the Kansas, at least below Fort Riley, according to the Barometrical observations of Col. Fremont and others, is near one and a half feet to the mile, and that if we assume the distance by the windings of the river between Chapman's Creek and Ogden, to be about thirty miles, it would make the elevation of the Kansas at the former locality some forty-five feet greater than at Ogden, which would reduce the dip to a fraction less than 14 feet to the mile. Still as the direction of the dip in this region is to the north of west, and the direction of the mouth of Chapman's Creek from Ogden is considerably south of west, it is probable the inclination of the strata here is greater than the above figures would indicate, and that it may not be less than twenty feet to the mile, in a north-west direction. From the foregoing statements it will be seen that in consequence of the dip of tbe strata to the north-west, and in some slight degree to the fall of the Kansas and Smoky Hill rivers, the whole of the foregoing general section be- low No. 12 passes beneath the level of the Smoky Hill, between the mouth of Blue river and Chapman's Creek. Consequently, the limestones of the succeed- ing beds above being thinner and less durable than those below, and separated by heavy beds of clay; we find, as might be expected, that the country here in the region of the mouth of Chapman's Creek, is much lower than at Fort Riley and. below. On reaching the mouth of Solomon's Fork, we found the face of the country characterized by long gentle grassy slopes, no part of it near the river being apparently elevated more than about 60 or TO feet above its surface. A short distance beyond this, we caught the first glimpse of the Smoky Hills, which were seen in a direction a little south of west from us, rising above the sur- rounding low country like dark blue clouds above the horizon. On approach- ing these, we found them always situated several miles back from the river, and rising some tbree hundred and fifty feet above it. The immediate bluffs of the river here, are generally composed of divisions No. 4 and 5 of the fore- going general section, and that portion of these hills above the level of the summits of the bluffs along the river, is made up of division Nos. 3, 2, 1, of the same section. On the south side of the river these hill have but a compara- tively thin capping of the sandstone No. 1, but on the north side we saw it showing a thickening on some of them of sixty feet. From some of these hills on the north side of Smoky Hill river, between it and the Grand Saline, we had an extensive and beautiful view of the surround- [J an. NATURAL SCIENCES OF PHILADELPHIA 23 ing country. In the north and north-west, many similar hills were in sight, and as the dip of the strata here is in that direction, it is probable some of this are not only chiefly made up of the sandstone No. 1, but surmounted by the other Cretaceous beds Nos. 2 and 3 of the Nebraska Cretaceous series ; in- deed, Dr. Engleman found all these formations occupying this relation on Re- publican river, not more than seventy miles north of this.* Although this paper is merely designed to give a brief sketch of the leading geological feature of those portions of north-eastern Kansas visited by us, we cannot close it without alluding to the truly great agricultural and other natural resources of this new and interesting Territory. We mean no disparagement to other portions of the Mississippi valley, when we state, that after having travelled extensively in the Great West, and after having seen many of its most favored spots, we have met with no country combining more attractive features than Kansas Territory. Her geographical position gives her a com- paratively mild and genial climate, intermediate between the extremes of heat and cold, while the rich virgin soil of her beautiful prairies is admirably adapted to the growth of all the great staple grain and root crops of the west. It is true that in some districts there is rather a deficiency of timber, but as a general thing there is along the streams sufficient for the immediate wants of the country. In addition to this, the wonderful rapidity with which forests are known to have sprung up on similar prairie lands in Missouri, as the country became settled so as to keep out the annual fires, shows that the present scarcity of timber should not be regarded as presenting any serious obstacle to the settlement of the most extensive prairie district in Kansas. Before going out into the interior of the Territory, we had expected to find the whole country immediately west of Fort Riley comparatively sterile ; on the contrary, however, we were agreeably disappointed at meeting with scarcely any indications of decreasing fertility as far as our travels extended, which was about sixty miles west of Fort Riley. Here we found the prairies clothed with a luxuriant growth of grass, and literally alive with vast herds of Buffalo that were seen quietly grazing as far as the eye could reach in every direction. Even on the high divide between the Smoky Hill and Arkansas rivers, south of this, we found the soil rich and supporting a dense growth of grass ; and from all we could learn from persons who have gone further out, the same kind of country extends for a long distance beyond this, towards the west. Hence we infer that the belt of unproductive lands between the rich country on the east, and the eastern base of the Rocky Mountains on the west, is much narrower than is generally supposed ; and even this so-called desert country is known to pos- sess a good soil, which may be rendered fruitful by artificial irrigation. In regard to the mineral resources of Kansas, we have at present only time and space to say a few words. As already stated, coal is known to exist, though its extent is not yet fully determined, at several localities in the region of Leavenworth City, while the geological structure of the country, as well as discoveries already made, warrant the conclusion that this important and useful mineral abounds at many localities south of there. Limestone suitable for building purposes, and the production of quicklime, exist throughout large areas, while inexhaustible beds of gypsum are known to occur at several places not far west of the mouth of Solomon's river. Near this place we likewise saw in the lower Cretaceous rocks crowning the summits of the Smoky Hills, deposits of iron ore, but were unable to determine in the limited time at our command, whether or not it exists in large quantities. Of the discoveries of gold in the mountains on the western borders of Kan- sas, much has been said ; nothing, however, but a thorough geological survey, by authority of the Territorial or State government, (for Kansas must soon be a State,) can lay before the public such full, accurate, and reliable information on these subjects as will bring from the older States the capital, skill and enterprise necessary to develop the great natural resources of the country. 1859.] 1 See Report of Secretary of War, Dec. 5th, 1857, page 497. 24 PROCEEDINGS OP THE ACADEMY OF Note. It affords us much pleasure to acknowledge here our obligations to Prof. Henry, of the Smithsonian Institution, for free access to the extensive series of books on Geology, Palaeontology, &c, in the Smithsonian Library, while investigating these and our former collections from the west : also for the use of rooms in the Institution, and for many other favors of great value to us. We are likewise under especial obligations to Capt. Stewart Vanvliet, and Mr. Levi Wilson of Fort Leavenworth, for favors while out in Kansas, without which we could have accomplished nothing : we also received many civilities from Major Sedgwick, Dr. T. G. Madison, Capt. W. S. Walker, and other officers of the army at Fort Riley. List of the species mentioned in this paper with some remarks on the synonymy, and references to the works, in which they are described. FORAMINIPERA. Fusulina cylindrica, Fischer, Oryct. Moscow, p. 126, p. 18, fag. 1 5. In Russia this species is said to occur only in the upper part of lower carbo- niferous or mountain limestone. Yet the species usually referred to F. cylin- drica in this country, so far as our knowledge extends, is not found below the coal measures. From this fact, and some slight differences we observe between our specimens and the figures of the Russian species, we suspect a careful comparison of good specimens may possibly prove them to be distinct. Ranges in Kansas from division No. 22, of the foregoing section, far down into the coal measures. Found at numerous localities between Manhattan and the Missouri, usually in great numbers. Fusulina cylindrica, Tar. ventricosa, Meek and Hayden, Proc. Acad. Nat. Sci. Phila. Dec. 1858, page 261. Division No. 37, of foregoing general sectional Manhattan on the Kansas, and at Juniata on big Blue river. Bryozoa. Synocladia biserialis. Prof. Swallow refers this species with doubt to S. virgu- lacea, Philips, sp. in Transactions Acad. Sci. St. Louis, vol. 1, p. 179, and points out some of the characters in which it differs, stating at the same time, in case it should prove to be distinct, that biserialis would be a good specific name for it. We regard it as quite distinct from Phillips' species, not only in scarcely ever having more than two rows of cellules, but also because the ?gemuliferous vesicles, instead of being merely " tubercular and open at the summit," have the form of short, but distinct spines apparently closed and rather obtusely pointed at the apex. The branches or connecting process are likewise less distinctly angulated between the longitudinal stems, than in S. viryulacea. Occurs at Fort Riley in No. 19 of foregoing general section, and at various lower horizons on the Kansas below there, down into the upper coal measures. Acanthocladia Americana. In the Trans. Acad. Sci. St. Louis, vol. 1, p. 180, Prof. Swallow refers this species with a query to A. anceps, Schlot. sp. and re- marks that it differs from that species in having "the rows of cellules diagonal to the axis of the stems, instead of longitudinal, as represented by King, and on ridges like that figured by Goldfuss.'' He also further remarks that " it is less regularly branched, and not so distinctly pinnated as those delineated by Goldfuss and King." In the specimens in our collection, the cellules are more numerous, and much more crowded, than in A. anceps as figured by King The specific name Americana, was suggested by Prof. Swallow. We found this species in Division No. 18, of the foregoing general section, on Cottonwood Creek. ECHINODERMATA. Cyathocrinus ? A few scapular plates bearing some similarity to those of C. ramosus, Schlot. sp. were met with by us in division No. 18, but they are pro- portionably much thicker, and the articulating surfaces quite different. Cottonwood Creek. [Jan. NATURAL SCIENCES OP PHILADELPHIA. 25 Archceocidaris ? In No. 12, we found spines and detached plates of apparent- ly an undescribed species of this genus, but they were too much weathered to show clearly the specific characters. The spines are rather slender, terete, nearly straight, and provided with short scattering spinous processes, directed rather obliquely outwards and forward. Cottonwood Creek. Archceocidaris ? The spines of this species are much larger than the last, and apparently destitute of spinous processes. They are as much as from three to four inches in length, nearly or quite straight, and not flattened or com- pressed. Division No. 26, Manhattan and in same position on Cottonwood Creek. Brachiopoda. Discina tenuilineata n. sp. We have only seen the lower valve of this species, which is extremely thin, nearly orbicular, and provided with a narrow perforation extending from very near the centre about half way out to the margin. The inner surface is ornamented by distant, extremely slender, distinctly elevated lines of growth, arranged concentrically around a point very nearly in the mid- dle of the valve. The apex of the upper valve was probably nearly central. Diameter 0-50 inch. Locality and position. Cottonwood Creek, division No. 16. Discina Manhattanensisn. sp. Shell rather small, nearly circular ; upper valve moderately elevated, apex rather obtusely pointed, located a little less than half the diameter of the shell from the posterior edge. Surface black and shining, marked by fine closely set concentric lines. Lower valve unknown. Greater diameter from 0-32 in. to 0-46. Found in great numbers in division No. 37, opposite Manhattan, on Kansas river. Productus splendens (.?), Norwood and Pratten, Jour. Acad. Nat. Sci. Phila. N. S. vol. 3, pi. fig. 5. We refer this shell to the above species with some doubt ; it is always smaller than the figure given by Norwood and Pratten, and rather more convex over the visceral region of the larger valve, while the smaller valve appears to want the band-like flattening around the border mentioned in the description of P. splendens. The ears extend beyond the body of the shell, are distinctly vaulted, and rarely have more than one spine on each, often none. The spines, however, are more numerous over the surface of the larger valve, being in this respect more like P. muricatus'8. and P., but both valves want the concentric wrinkles represented in the figures of that species. This neat little Productus is found in great numbers between Fort Riley and Manhattan, as well as at the latter place, in Division No. 34 ; also at various horizons below that in the upper coal measures of Kansas. Productus Norivoodi, Swallow, Trans. Acad. Sci. St, Louis, vol. 1, p. 182. A few specimens of this species in our possession have the extreme point of the beak of the larger valve flattened or truncate, aa though it had in the young state been attached to some marine body by that part of the shell. We have also in several instances found other shells associated with this species, with small discs not more than 0-20 inch in diameter, attached by the whole surface, as well as by a series of small spines seen radiating from the margin. May not these little bodies be the young of this species? We think the specimen figured by Prof. Marcou in his work on the Geology of North America, plate 6, fig. 1, as P. pustidosus, is the same as the above spe- cies, and quite distinct from P. pustidosus. It occurs in Kansas at various ho- rizons from No. 14 far down in the upper Coal measures. We found it at Fort Riley and numerous places between there and the Missouri, as well as at Leav- enworth city. 1859.] 26 PROCEEDINGS OF THE ACADEMY OF Productus Rogersi, Norwood and Pratten, Jour. Acad. Nat. Sci. Phil. N. S. vol. ill, page 9, pi. 1, fig. 3. This species is nearly related to the last, and when the shell is exfoliated, may be easily confounded with it. P. Nor- woodi, however, appears never to have the distinct concentric wrinkles of this species, nor do the pustules, at the base of the spines have the tendency to elon- gate into indistinct ribs as in P. Rogersi. Prof. Marcou has figured in N. Am. Geol. pi. 5, fig. 6, as Productus scabriculus, a shell very like this. Kansas valley below Mouth Blue river, in upper Coal measures. Productus pustulosus (?) Phillips' Geol. Yorkshire, vol. 2, p. 316, pi. 7, fig 15. We have a specimen agreeing very nearly with this species in its external markings, but it is much narrower, and the beak of the larger valve more ex- tended, in which respect it differs quite as much from P. punctatus. Near Steam Boat Landing at Leavenworth city, in Coal measures. Productus Prattenianus, Norwood, Jour. Acad. Nat. Sci. Phil. N. S. vol. 3, p. L7, pi. 1, fig. 10. In Coal measures at Indian creek and at Leavenworth city. Productus Calhounianus, Swallow, Trans. Acad. Sci. St. Louis, vol. 1, p. 181. This fine large shell is scarcely distinguishable from P. semireticulatus var. anti- qvus. but Prof. Swallow, who has seen the interior, thinks it presents well marked internal differences. It occurs in No. 12 and below, at Fort Riley, also on Cotton-wood creek. Prof. S. thinks it even ranges down into the lower Car- boniferous. Chonetes Verneuiliana, Norwood and Pratten, Jour. Acad. Nat. Sci. Phila. vol. 3, p. 26, pi. 2, fig. 6, N. S. Occurs in Kansas in division No. 37, at Manhattan, and perhaps in upper Coal measures at lower horizons. Chonetes mucronata, Meek and Hayden, Proceed. Acad. Nat. Sci. Phila. Dec, 1838, page 262. Lower part of the section at Fort Riley, (division 9) and down near the base of the foregoing general section, also in same position on Cotton- wood creek. Orthisina crassa, Meek and Hayden, Proceed. Acad. Nat. Sci. Phila. Dec. 1858, p. 261. Occurs in Coal measures near landing at Leavenworth city. Orthisina umbraculum? Schlot. sp. Petrefakt. 1, p. 256, et 2, p. 67. We find in Kansas, ranging from 16 to 19 of foregoing sections, many specimens of a large species of Orthisina having almost exactly the form and other characters of 0. umbraculum, excepting that the striae appear to be more numerous. Ac- cording to Koninck that species has about 108 striae on each valve, while on our Kansas specimens, we count from 160 to 200 ; consequently we suspect it may be a distinct but closely allied species; if so, we would propose to designate it by the name of O. multistriata. We found it at Fort Riley and at several lo- calities between there and Blue river; also in same position on Cottonwood creek. Orthisina Missouriensis, Swallow, Tra ns. Acad. Sci. St. Louis, vol. 1, p. 219. This is a very peculiar plicated species, often much distorted. When partly embedded in the matrix, it frequently bears a striking resemblance to Plicatula striato-costata, Cox, 3d vol. Dr. Owen ; s report on the Geol. Survey of Kentucky, page 558, pi. 8, fig. 7, of Atlas. Common in the upper Coal measures of Kan- sas, at Leavenworth city and west of there. Orthisina Shumardiana, Swallow, Trans, St. Louis Acad. Sci. vol. 1, p. 183- Although like the last, a plicated species, this is more symmetrical, and presents other well marked differences. Ranges from No. 11, down some dis- tance in upper Coal measures. Found at Fort Riley and between there and Blue River. Terebratula millepunctata, Hall, Pacific Rail Road Report, vol. 3, p. 101, plate 2, figs. 1 2. We have the impression that this species is probably identical with T. bovidens, Morton (Silliman's Jour. vol. 29, p. ) from Ohio. Our Kan- [Jan. NATURAL SCIENCES OP PHILADELPHIA. 27 sas specimens appear, however, to be more elongated than those figures by Dr. Morton, and may be distinct. In form they resemble very much some varieties of Epithyris elongata, Schlot. sp. as figured by King, in Perm. Fos. Eng. pi. vi., particularly the narrower varieties, such as fig. 35. The beak of our Kansas shell, however, is not truncate but pointed, the perforation being on the outside, and a little removed from the extremity. If it is identical with T. bovidcns, Morton's specific name will have to take precedence, being the older. It re- mains to be determined whether its internal characters agree with Terebratula, as now restricted. Thi3 is a rather common form in the upper Coal measures of Kansas, and southward. We found it near the summit of the hills back of Leavenworth city, also at Indian creek near Indianola, &c. Rhynchonella Uta. {Terebratula Ufa, Marcou, Geol. N. A., p. 51, pi. vi.'fig 12.) We have from the upper Coal measures in Kansas many specimens of a species agreeing exactly with Prof. Marcou's description of the above species. These we suspect may possibly go into the genus Carrier ophoria, King, if not into Rhyn- chonella] at any rate they are certainly not Terebratula. We are inclined to the opinion that ashell described by Prof. Swallow, in the Trans. Acad- Sci. St. Louis, vol. 1, page 219, under the name of Rhynchonella (Camerophoria) Osagen- $is, may be identical also with the above ; yet Prof. S. says his species has from " two to six " plications in the sinus of the dorsal valve, while in the shell before us, of which we have quite a number of specimens, there are invariably but two plications in the sinus. Quite common in division No. 94 at Manhattan and at several localities be- tween there and the Missouri, in the Upper Coal Measures. Prof. Marcou, cites it as a mountain limestone species, but we know nothing of its existence in rocks of that age. Retzia Mormonii. 'Terebratula Mormonii, Marcou, Geol. N. A., p. 51,pl.vi., f. 11.) We found this species quite abundant in division 37, at Manhattan, where it is associated with the last. It also ranges far below this in the upper Coal meas- ures between Manhattan and the Missouri, being quite common near the sum- mits of the hills back of Leavenworth city. Dr. B. F. Shumard has described a species in the Trans. Acad. Sci. St. Louis, under the name of Retzia punctilife- ra, which we suspect may possibly be a variety of the above; but as he de- scribes it as having usually in the dorsal valve " a moderately wide, shallow si- nus, which extends from the front nearly to the beak," and the species before us, of which we have many specimens, has no traces of a sinus, we are left in doubt. In other respects his description agrees exactly with our shell, and he also states that he has it from K. T. Prof. Marcou found this species at the Salt Like City, Utah, in a rock he refers to the mountain limestone. We have never seen it from below the Coal measures. Spirifer Kentuckensis, Shumard, Geol. Survey of Missouri, part 2, page 203. Found in upper Coal Measures near the top of bluffs, back of Fort Leavenworth, also near the landing at Leavenworth City, and at other localities between the Missouri and Blue river. Spirifer cameratus, Morton, American Jour. Sci. vol. 29, p. 150, plate 11, fig 3. This is the same species as has been determined by Prof. Hall, described by Dr. Roemer as S. Meusebachanus. (Kreid von Texas, p. 88, pi. xi. fig. 7) and sub- sequently by himself as S. triplicatus, in Stansburv's Rept. p. 420, pi. iv. fig. 5. Prof. Marcou has recently figured it in his work on the Geol. North America, page 49, pi. viii. fig. 3, as a variety of Spirifer striatus, Martin, from which it is quite distinct. He found it at Pecos Village in a rock he refers to the lower Carboniferous or mountain limestone. It has a great geographical range, be- ing common in the coal Measures from Pennsylvania to the Rocky Mountains, and from Nebraska to New Mexico; we have never seen it, however, from lower Carboniferous rocks. 1859.] 28 PROCEEDINGS OP THE ACADEMY OP Spirifer hemiplicata, Hall. Stansbury's report, p. 409, pi. 4, fig. 3. Upper Coal Measures near summit of hills back of Leavenworth, and at other local- ities between there and Blue River. Spirifer lineatus. Anomites lineatus, Martin. Spirifer lineatus of Phillips. Geol- Yorks., 2, p. 219, pi. 10, tig. 17, and of other authors. We have, from near Leavenworth landing, in the coal measures, a Spirifer, apparently identical with the above. It appears not to range very high in the upper coal measures of Kansas. Spirifer . In division No. 12, above Fort Riley, we found a few imperfect specimens of a small, smooth Spirifer, similar in some respects, to S. lineatus, but apparently more like Martinia Clannyana, King, from the Permian of Eng- land. Spirifer planoconvexa, Shumard. Geol. Report, Missouri, 2d part, p. 202. We found this handsome little shell quite abundant in the upper coal measures (divisions 34 and 37,) at Manhattan ; also at Juniata, on Big Blue River, and near summit of hills, back of Leavenworth City. Spirigera subtilita. (Terebratula subtilita, Hall. Stansbury's Report, p. 409, pi. 4. fig. 1-2.) Spirigera subtilita of Dr. George Shumard. Trans. St. Louis Acad. Sci., vol. i. This is a very abundant species in Kansas ; we found it ranging up, at least as far as division No. 37, at Manhattan, and met with some obscure forms re- sembling it, still higher in the series. From these horizons, it, ranges far down in the other members of the coal measures. Several of our specimens col- lected at Leavenworth City, show that it was provided with internal spiral ap- pendages, as in the Spirifer, and consequently cannot remain in the genus Te- rebratula, as now restricted. It has a wide geographical range, and is almost everywhere the companion of Spirifer earner atus. Prof. Marcou figures it in his work on the Geology of North America, pi. vi. fig. 9, from a formation in the Rocky Mountains, which he refers to, the lower carboniferous ; but we have never seen it from any position below the coal measures. Spirigera ? At Fort Riley, and above there, as well as in the same position on Cottonwood Creek, we found, ranging from division 18 up to 10 of the fore- going section, a Spirigera resembling S. subtilita, but much more gibbous in form ; it also appears to have a much thicker shell. If distinct from S. subtilita this might be designated by the specific name gibbosa. Lamellibranchiata. Monotis Hawni, Meek and Hayden. Trans. Albany Inst., vol. iv., March 2, 1858. Prof. Swallow thinks this species not distinct from M. speluncaria, Schot sp. Although, like that species, it is quite variable, and some of its varieties are very similar to it; after a careful comparison of a large number of indi- viduals with King's figures and descriptions, we still regard it as distinct. We have never seen any of its various forms with the beak of the larger valve ele- vated so far above the hinge, as in fig. 5, 6, 7 and 8, pi. 13, of King's work. Nor do any of our specimens possess the peculiar oblique posterior sulcus, seen in the figures cited above. High Country, south of Kansas Falls ; also above there, on Smoky Hill River and Cottonwood Creek, in division 10. Myalina [Mytilus) peraltenuata, Meek and Hayden. Trans. Albany Inst., vol. iv., March 2d, 1858. Our description of this species was made out from one of the more slender varieties of this shell, sent to us from near Smoky Hill River by Mr. Hawn. We were probably wrong, however, in refering to it a specimen in our possession from a locality on the Missouri, opposite the north- ern boundary of Missouri; and we even suspect the rock from which this latter specimen was obtained may belong to an older epoch. The species above cited, is we think identical with M. permianus of Swallow, Trans. Acad. Sci., St. Louis, vol. i. p. 187. And we also suspect the form he de- scribes in the same paper, as Mytilus {Myalina) concavus, is only a broader va- [Jan. NATURAL SCIENCES OP PHILADELPHIA. ' 29 riety of the same ; at any rate, we have these two forms, and every intermediate gradation between them, from the same bed. Locality and position same, as the preceding. Myalina squamosa. (Jfutilus squamosa, J. de C. Sowerby. Morris's Cata- logue, p. 93. Myalina squamosa of some other authors.) Of the form, we refer with doubt to the above species; we have but one im- perfect specimen. As far as the characters can be made out, it agrees with this species. We found it iu division No 11, at Kansas Falls, above Fort Riley. Myalina subquadraia, Shumard. Missouri Geol. Rept., 2d part, p. 207, pi. c, fig. 17. Upper coal measures, Leavenworth City, on t lie Kansas, at Lawrence and otber localities in Kansas Valley, below mouth of Big Blue River. Edmondia? Calhouni, Meek and Hayden. Trans. Albany Inst., vol. iv., March 2, 1858. We are still in doubt in regard to the generic relations of this species, having procured no better specimens thau that first described by us. We suspect it may be a Cardinia. NearSmoky Hill river, in division 10. Bakevellia parva, Meek and Hayden. Trans. Albauy Inst., vol. iv., March 2d, 1858. This is probably the same species referred by Prof. Swallow to Avicula antiqua, Minister, Bakevellia antiqua of King, and others. In describing this spe- cies, we spoke of its very near relation to B. antiqua, but pointed out some characters in which it differs. At that time we had seen but a few imperfect specimens; since then, however, we have obtained many others, a careful ex- amination of which causes us still to regard it as distinct from B. antiqua. Of a large number of individuals, we have never seen any one-half the size of the smallest, nor one-eighth the size of the largest figures of that species given by King, while the cardinal area is also proportionably much narrower iu our shell. Division No. 10. On Smoky Hill river and Cottonwood creek. Area carbonaria, Cox. Vol. iii. Geol. Report, Ky., p. 567, pi. 8, fig. 5. Our fossil is smaller, and less distinctly striate, but exactly the form of the above. Near Leavenworth landing, coal measures. Leda subscilula, Meek and Hayden. Trans. Albany Inst., vol. iv. March 2d, 1858. Division No. 10. Smoky Hill river and Cottonwood creek. Pleurophorus ? subcuneata, Meek and Hayden. Trans. Albany Inst,, vol. iv., March 2d, 185S. Our specimens of this species being casts we are left in doubt in regard to its generic relations. We suspect it may be a Cardinia. Same locality and position as preceding. Axinus (Schizodus) ovatus, Meek and Hayden. Proceed. Acad. Nat. Sci. Phila. Dec, 1858. This is very much like the Permian forms, S. roiundatus and t.-weria. 187. Bdcephala albeola. Much more rornnion on the mountain brooks than on the Rio Grande, but not often met with -southern New Mexico. 188. Erismatdra rubida. But few ever i-ict with. 189. Mergds Americanus. 190. Lophodytes cucullatus. Very common on the Mimbres, and occasion- ally met with on the Rio Grande. 191. Cyrtopelicanus erythborhynchus. Common above latitude 32. 192. Graculus Mexicanus. Very common during April. 193. Plotus Anhinga. Not many observed. 194. Larus Delawarensis. A very few v uet with on the Rio Grande, in win- ter and spring. 195. Sterna Wilsonii. Common in September on the Rio Grande. 196. S. fuliginosa. A few seen on the Hi Grande. 197. Colymbus torquatus. 198. Pooyumbus podiceps. Mr. J. P. Lesley was appointed to fill a vacancy in the Committee on Palaeontology, and Mr. Joseph Jeanes to fill one in the Committee on the Library. April 5th. Mr. Lea, President, in the Chair: Forty-eight numbers present. The following papers, by Theo. Gill, were presented for publication in the Proceedings. On Dactyloscopus and Leptoscopus, tsvo new genera of the family of Uranoscopidse. On the genus Callionymus of authors. Description of Hyporhamphus, a new genus of Fishes, allied to Hc- mirhamphus. Notes on a collection of Japanese Fishes, made by Dr. J. Morrow. And also the following : Description of eight new species of Unionidae, from Georgia, Missis- sippi and Texas, by Isaac Lea, And were referred to committees. 1859.] 9 110 PROCEEDINGS OP THE ACADEMY OP Dr. Leidy stated that, in company with Messrs. Vaux, Sergeant, Powel and Tilghman, he had the day before visited the vicinity of Phoenixville, Chester Co., with the view of examining the shales recently removed in widening the rail-way tunnel. The specimens of shales or black slates, supposed to be of triassic age, presented this evening to the Academy, are those which had been collected. Besides obscure vegetable remains, species of Cypridae and Posido- niae, they contain scales, bones and teeth of ganoid fishes, and also teeth of three apparently distinct genera of reptiles. Two of the teeth, elongated coni- cal in form, and finely striated, appear to belong to the genus Clepsysaurus, Lea, the remains of which were first discovered in the corresponding rocks of Lehigh Co. A third tooth, of large size, is compressed conical, and has oppo- site, acute, serrulated borders. It probably indicates a new genus and species, for which the name Eurydorus serridens is proposed. Fragments of similar teeth have been found in the rocks near Gwynned, Montgomery Co. A fourth tooth, much smaller than the one just indicated, has the same form, but has its borders without serrulation, and has the base fluted. It resembles the teeth of Couipsosaurus, of the coal of Chatham Co., North Carolina, but, nevertheless, belongs to a different species. The death of Mr. W. I. Broderip, of London, late a correspondent of the Academy was announced. On leave granted, a vote of thanks, was ordered to be tendered to Dr. Alexander Bryant, for his donation of fossils, received this evening. April 12th. Mr. Lea, President, in the Chair. Fifty-four members present. Dr. Leidy stated that the specimens of ferruginous rock containing remains of fishes, presented to the Academy this evening by Dr. P. W. Mosblech, of Bethany, Virginia, were of a very interesting character. Dr. Mosblech, in a let- ter, states that the locality of the remains is a horizontal, ferruginous deposit, about one inch in thickness, resting upon an old vegetable soil, overlying a limestone which is considered as the uppermost member of the coal forma- tion ; and it is covered with a soft, sandy, aluminous shale, destitute of or- ganic remains, so far as examined. The extent of the ferruginous deposit is unknown, but it seems to be confined to the College Hill, at Bethany, equal to about four acres. The fragments of rock contain a multitude of isolated scales of ganoid fishes, and numerous teeth and small fragments of bones. Most of the teeth are of small size, and have exactly the same form and construction as those of Saurichthys, a genus of the triassic formations of Europe; but others of large size belong to the genus Diplodus, which is also found in the coal formations of other parts of the United States, and of Europe. Dr. Leidy added that the fossils from the Green Sand, of Monmouth Co., pre- sented this evening by Mr. J. H. Slack, consisted of fragments of jaws with teeth of Mosas aurus, several bones apparently of a reptile, of unknown character, a jaw of Enchodus, a palate bone with teeth of Pycnodu s , and teeth of 1 o d u s and Galeocerdo. The Commitfee on Proceedings laid on the table the number of the Proceedings for March. [April, NATURAL SCIENCES OF PHILADELPHIA. Ill April \th. Mr. Lea, President, in the Chair. Forty-nine members present. The following were presented for publication in the Proceedings: Ichthyological Notices by Charles Grirard, M. D. On (he primary divisions of the Salamandridae, with a description of two new species, by E. D. Cope. Description of twenty one new species of Exotic Unionidae, by Isaac Lea. Description of two new species of Uniones, from Georgia, by Isaac Lea. Dr. Leidy remarked, that Mr. Jos. B. Hanson, an intelligent merchant of this city, had recently addressed to him a note, to call at his warehouse and examine some masses of the so-called Sombrero guano, containing fossil bones. Two large masses of this substance, now on the table and presented to the Academy by Mr. Hanson, include a number of turtle bones, among which the posterior portion of a sternum of an individual is well preserved. The included bone fragments significantly point to the origin of the rock, imported as a manure rich in phosphates, from the island Sombrero, W. I. This island, situated about 130 miles east of Porto Rico, Mr. Hanson informs us, is about 2J miles long, to | of a mile wide, and rises from 20 to 40 feet above the level of the ocean. It is a barren rock formerly avoided by navigators, and .appears to be entirely composed of the rich phosphatic mineral. Analyses of the substance, by competent chemists, indicate it to bear a resemblance in composition to bones deprived of their cartilage, and otherwise altered, as we might suppose bones to be, exposed to the influence of the ocean water. It contains about the same proportion of phosphate of lime as calcined bones ; and it is this circumstance which has directed the attention of enterprising merchants and agriculturalists to its value as a manure. When we recollect that the cereal grains, buckwheat, clover and other legu- minous seeds yield in their ash from 30 to 50 per cent, of phosphoric acid, we cannot but feel the conviction that the Sombrero substance, with its 75 per cent, of phosphates, must prove to be of far more permanent value than the true guano. From this, the Sombrero material deserves to be distinguished by a new name, and perhaps the easy one of O s i t e , from its resemblance in composition to bones and its probable origin, would not be inappropriate. But are we to ascribe the immense mass forming the Sombrero rock to animal origin ? Many reefs and shores of vast extent are known positively to have had their origin in the testaceous coverings of the lower animals, but Som- brero appears to be the first instance of an extensive island formed alone of the remains of the higher animals. The composition of the Sombrero substance, with its included bones, leads us to suspect that the island was once a shoal swarming with turtles and other vertebral animals, whose accumulated re- mains of ages have been cemented together, and gradually elevated above the ocean level to the present position of the island. Mr. Hanson informs us that no animals inhabit the latter, independently of birds, except a lizard, about one foot in length, specimens of which he has promised to obtain for the Academy. Dr. Leidy further remarked that the bear skull presented this evening by Mr. W. D. Moore, of Oxford, Mississippi, had been found, in association with two portions of jaws with teeth of the Mastodon, in the drift of Claiborne Co., Mississippi. The skull does not differ from that of the common black bear, Ursus Americanus. It is the fourth instance in which Dr. L. has no- ticed the occurrence of remains apparently of this species in association with those of Mastodon, Megalonyx, and other extinct animals. 1859.] 112 PROCEEDINGS OF THE ACADEMY OF On leave granted, a vote of thanks was ordered to be tendered to Mr. I. W. Gregory, for the body of the Bengal tiger, presented this even- ing. April 26$. Vice-President Bridges in the Chair. Forty members present. The report of the Biological Department for the present month was read. On report of the respective Committees, the following papers were ordered to be printed in the Proceedings : Descriptions of Eight New Species of UNIONID-E, from Georgia, Mississippi, and Texas. BY ISAAC LEA. TJnio spissus. Testa laevi, elliptica, subventricosa, postice obtuse angulata subaequilaterali ; valvulis crassis ; natibus prominulis ; epidermide striata, rufo-fusca, obsolete radiata ; dentibus cardinalibus magnis, erectis, compressis, crenulaiis, in utroque valvulo subduplicibus ; lateralibus longis, crassis subcur- visque ; margarita vel purpurea, vel salmonis colore tincta et iridescente. Hab. Satilla River, Wayne County, Georgia. T. C. Downie. TJnio corvus. Testa, laevi, subtriaDgulari, subcompressa, inaequilaterali, pos- tice obtuse biangulata ; valvulis crassis, antice crassioribus ; natibus subpro- minentibus ; epidermide nigricante, superne glabra, polita, inferne striata ; dentibus cardinalibus subgrandibus, subconicis striatisque ; lateralibus longis curvisque ; margarita alba et iridescente. Hab. Buckhead Creek, Burke County, Georgia. Bishop Elliott ; and Ogee- chee River, Georgia. Prof. Hanley. TJnio Burkensis. Testa laevi, transversa, compressa, ad latere planulata., in- aequilaterali, postice biangulata ; valvulis crassiusculis ; natibus prominulis ; epidermide fusco-flavicante, inicante et obsolete radiata; dentibus cardinalibus breviusculis, compressis, acuminatis ; lateralibus longis rectisque ; margarita purpurascente et iridescente. Hab. Buckhead Creek, Burke County, Georgia. Bishop Elliott. TJnio aureus. Testa laevi, subtriangulari, compressa, ad latere paulisper planulata, subinaequilaterali ; valvulis subcrassis, antice crassioribus ; natibus subelevatis, ad apices acuminatis ; epidermide aurea, striata, obsolete radiata; dentibus cardinalibus crassis, erectis, striatis, in utroque valvulo duplicibus ; lateralibus curtis et obliquis ; margarita alba, et iridescente. Hab. Texa3. W. Newcomb, M. D. TJnio curtus. Testa laevi, obliqua, ad umbones valde tumida, antice trun- cata, postice obtuse angulata, valde inaequilaterali ; valvulis percrassis, antice crassioribus ; natibus elevatis, crassis, t'ere terminalibus; epidermide tenebroso- castanea, ad apices virescente, obsolete radiata; dentibus cardinalibus sub- grandibus, compressis, acuminatis, obliquis ; lateralibus crassis subcurvisque ; margarita argenteil et iridescente. Hab. Tombigbee River, Columbus, Mississippi. Wm. Spillman, M. D. TJnio permiscens. Testa laevi, obovata, inflata, postice late rotundata, valde in33quilaterali ; valvulis tenuibus ; natibus prominulis; epidermide tenebroso- fusca, nigricante, obsolete perradiata, nitida ; dentibus cardinalibus parvulis, [April, NATURAL SCIENCES OF PHILADELPHIA. 113 compressis, obliquis ; lateralibus praelongis, lamellatis subcurvisque ; ruargarita cajruleo-alba et valde iridescente. Hab. Tombigbee River, Columbus, Mississippi. Wm. Spillman, M. D. Margaritaxa elliptica. Testa lasvi, elliptica, subinflata, subaequilaterali, postice obtuse angulata ; valvulis ttmuibus ; natibus subprominentibus, ad apices subconcentrice undulatis ; epidermide luteo-virente, glabra, nidda } perradiata; dentibus cardinalibus parvis, compressis, in utroque valvulo singu- lis; margarita. casruleo-alba et iridescente. Hab. Tombigbee River, Columbus, Mississippi. Wm. Spillman, M. D. Anodo.vta Texasensis. Testa, lajvi, elliptica, inflata, ad latere, rotunda, inae- quilaterali, postice subangulata ; valvulis pertenuibus ; natibus subprominenti- bus, ad apices biundulata ; epidermide dilute lutea, glabra, fulgida, obsolete radiata; margarita caeruleo-alba, diaphana et valde iridescente. Hab. Texas. W. Newcomb, M. D. ICHTHYOLOGICAL NOTICES. BY CHARLES GIRARD, M. D. XL1. Since we are again called upon to mention the genus Zygonecles, we will venture to point out such structural peculiarities, as, in our opinion, may be considered its generical characters. Body rather slender and elongated, com- pressed, subfusiform in its profile, and covered with well developed scales. Head rather small, depressed, subpyramidal. Mouth very protractile, its gape being horizontal, whether in a protracted or a retracted condition. Teeth upon the premaxillar bones and upon the lower jaw ; an external series slender and acerated, behind which may be observed a band of velvet-like ones. The ori- gin of the anal fin is opposite the anterior margin of the dorsal, or in advance of it. The genus Zjigonect.es appears to be intermediate between Hydrargyra and Gimbusia, resembling more the former by its general aspect, and the latter by its structure. Specimens of a species of this genus, and which we call Z. pulchdlus, were collected in Sugar Loaf Creek, Arkansas, by the party under Capt. A. W. Whipple. The largest one measures two inches and a half in total length, of which the head constitutes rather more than the fifth. The eye is large and circular ; its diameter entering four times in the length of the side of the head. The dorsal and anal fins are deeper than long ; the anal being larger than the dorsal, and placed more anteriorly, so that its anterior margin is nearly equi- distant between the apex of the snout and the posterior margin of the caudal fin. The tip of the posterior rays of the dorsal extend as far as the insertion of the caudal, that is, a little further backwards than the tip of the posterior rays of the anal fin. The ventrals and the pectorals are but moderately de- veloped ; the tip of the former extends to the vent, whilst the latter do not quite reach the insertion of the ventrals. The ravs of the various fins are as follows : D 9 ; A 12 ; C 3, 1, 7, 6, 1, 3 ; V 6 ; P 13. There are twelve longi- tudinal rows of scales between the anterior margin of the dorsal and that of the anal fin. The surface of the scales has a rather rugose appearance, owing to the conspicuousness of the concentric lines of growth. The scales them- selves are deeper than long, anteriorly subtruncated or subconvex ; undulating and rounded off upon the remaining edges. The ground color is olivaceous brown, of a darker tint along the dorsal re- gion than over the abdomen. A black band or streak extends from the nose, across the eye, along the middle of the flank to the base of the caudal fin. Small black dots, constituting four or five irregular longitudinal series, may bo observed on either side of the dorsal region, above the lateral streak ; the dorsal, anal, and caudal fins being likewise dotted with black, whilst the ven- trals and pectorals are unicolor, like the abdomen. 1859.] 114 PROCEEDINGS OP THE ACADEMY OF XLII. Having had, recently, an opportunity of examining authentic specimens of either species of Limia, inhabiting ihe island of Cuba, and described by Prof. Poey, we are now better prepared to speak of those species which occur along our own shores and in the Mexican provinces bordering the Rio Grande Boundary. And before we proceed any further into the history of these fishes, we deem it expedient to recapitulate the characiers of that genus. The body, generally speaking, is rather short and deep, very much compressed, and covered with comparatively large scales. The upper surface of the head is depressed, sloping forwards, wedge-shaped in general appearance. The mouth is small, or else, of moderate size, very protractile, directed upwards when in a retracted condition, tlia lower jaw then appearing longer than the upper; but when protracted, the aperture is directed horizontally forwards, and somewhat downwards, assuming the shape of a flattened (depressed) tube, the jaws being equal. Either jaw exhibits a row of slender, curved and acerated teeth, behind which a narrow patch of minute, velvet-like ones may be observed. The anal fin is inserted posteriorly to the an'erior margin of the dorsal, and differently constructed according to the sexes. The dorsal fin itself is higher and longer in the male than in the female. The posterior edge of the caudal is subtruncated or rounded off. In the above diagnosis of the generical characters to be assigned to Limia, it is easy to perceive a most intimate affinity between that genus and Pacilia. Indeed, the only difference which is noticeable, resides in the structure of the anal 6n of the male sex, which is narrower and deeper than in the female, and inserted more anteriorly, close to the ventrals ; the anterior rays being much more developed than the posterior ones, which are partly atrophied. Now. such a distinction may not appear of sufficient importance, and ichthyologists might raise the question of preserving these two genera in the nomenclature. In the present state of our personal knowledge regarding these fishes, we should not have established a generic distinction upon that character alone. But, since these genera exist, we shall, for the present at least, speak of them under separate heads, leaving it with future investigations to decide upon their in- trinsic value. Our reason for so doing is the lack of specimens of most of the species referred to the genus Pcecilia, in the " Histoire naturelle des Poissons," and described from specimens of the female sex alone. Moreover, we may ex- pect many new species from Mexico and Central America, which may throw considerable light upon the natural history, yet so imperfectly known, of these little fishes. We have examined specimens of Pcecilia multilineata, collected at Palatka, East Florida, by T. Glover. Lesueur himself admits their identity with those he obtained from Lake Ponchartrain. Not having at our command specimens of the latter locality, we are not prepared to express any opinion regarding that point. But we have had under examination from that locality, Mollinesia lati- pinna, which is considered now as the male sex of Pcecilia multilineata. These exhibit the same generical characters which we have assigned to Limia ; there- fore, should further investigations corroborate a generic distinction between Pcecilia and Limia, the latter appellation will have to give way to Mollinesia, as having priority over it. Male and female specimens of this same species were collected at Galveston, Texas, by Dr. C. B. R. Kennedy, under Capt. A. W. Whipple. XLIII. The species which we have described under the name of P. lineolata, in the " Ichthyology of the U. S. and Mex. Boundary Survey," from specimens collected at Brownsville, near the mouth of the Rio Grande del Norte (Rio Bravo), belongs to the same genus as the former species. It is closely allied to P. multilineata, the female sex being compared, the male sex having not yet come under observations. It differs from the latter by a smaller head, a smaller [April, NATURAL SCIENCES OF PHILADELPHIA. 115 eye, and a smaller mouth ; the dorsal fin is also placed more anteriorly. The system of coloration being exactly the same in either species. XL1V. The species which we have called Limia paciloides is but very imper- fectly characterised in the " Ichthyology of the U. S. and Mex. Boundary. '" Moreover, figs. 12 14, of plate xxxviii, do not belong to the same species. Hence the male sex only is so far known ; it is represented on the plate just alluded to, fijs. 811. Now then, if we recapitulate the characters to be assigned to this species, we shall have the following diagnosis : The back is arched and the abdomen qui'e convex; the greatest depth taken in advance of the anterior edge of the dorsal fin enters somewhat less than four times in the total length. The head is contained four times and a half in the total length ; external series of teeth very slender and exiguous. Diameter of eye entering three times and a half in the length of the fide of the head. Dorsal fin neatly as long as deep, superiorly convex, its anterior margin being nearer the apex of the snout than the inser- tion of the caudal. The caudal itself is posteriorly rounded oft* or convex. The anal fin is inserted opposite the middle portion of the base of the dorsal. Ven- trals small and slender, inserted immediately in advance of the anterior edge of the dorsal ; their posterior extremity stretching beyond the anterior edge of the anal fin and overlap, consequently, the vent. The pectorals being rather short and broad, subelliptical in their outline. The rays are : D 13 ; A 6 ; C 2. 1, 7, 7, 1, 2 ; V 6 ; P 13. The ground color is reddish-brown, with transverse narrow bands of a darker tint and a small blackish spot at the base of each scale, constituting about seven longitudinal serit s on eitbtr eide of the body. The caudal fin is likewise transversely spotted, whilst the other fins are uni- color. Specimens of this species were collected at Indianola, Texas, by John H. Clark, under Col. J. D. Graham. XLV. A very pretty little species of Limia, which we call L. formosa, was likewise caught by John H. Clark, under Major Emory, in a lagoon at Paolo Alto. Of this, we have a specimen of either sex, the female differing widely from the male. We will proceed describing them, one after the other. The male resembles somewhat the same sex in L. poeciloicfes, from which it may, however, be distinguished at first glance, by a greater depth at the pe- duncle of the tail. The back is likewise less arched, and the abdomen less con- vex; the greatest depth of the body, at the origin of the dorsal, entering some- what over four times in the total length. The head constitutes about the fourth of the total length ; the eye, which is large and circular, enters three times in the length of the side of the head by its diameter. The snout is rather abbre- viated. The dorsal fin is longer than high, and convex or subconvex upon its upper margin. The caudal is rounded off posteriorly. The anal fin is inserted nearly opposite the anterior margin of the dorsal ; it is slender and deep, but far from extending as far back as the posterior rays of the dorsal. The ventrals. which are slender, are inserted in advance of the anterior margin of the dorsal, at a short distance from the anal, between which there is just space enough for the anal aperture. Their extremities project beyond the base of the anal fin, particularly the second ray, which is longer than the rest. As to the pectorals, they are rather broad and proportionally well developed. The female specimen, which measures one inch and a half, is more slender than the male. We take it, however, that when adult and full of roe, the pro- portions of the body may assume a different aspect. The greatest depth is equal to the length of the head, which constitutes the fourth of the total length. We notice the same abbreviated snout and large eyes, as in the male sex. The dorsal fin is nearly as high as long, and almost of equal depth throughout, its upper margin being straight or subconvex ; the anterior margin of that fin is somewhat nearer the insertion of the caudal than the apex of the snout. The 1859.] 116 PROCEEDINGS OF THE ACADEMY OF anal fin, which is deeper than long, is inserted opposite the posterior portion of the base of the dorsal. The ventrals are small, subtriangular when expanded, their posterior extremity not extending as far as the anterior edge of the anal. The pectorals are well developed, elongated, posteriorly rounded off, their ex- tremities projecting beyond a line drawn at the origin of the ventrals. The rays of the fins are : D 12 ; A 10 ; C 7, 1, 8, 7, 1, 6 ; V 6 ; P 9. We have counted thirteen rays in the dorsal fin of the male sex, and seven in the anal. The structure of the latter is as follows : First and second ray simple, short, and slender; third and fourth most developed, third one stoutest; fifth, sixth, and seventh slender, but deeper than the first and second, and bifurcated. The scales are very similar in either sex, much deeper than long, anteriorly trun- cated, with numerous radiating furrows upon the latter section only, and rounded off upon the remaining edges, with very fine concentric lines of growth. The ground color is olivaceous brown ; the dorsal region assuming a darker tint, owing to a biowu spot which may be observed on the scales, whilst the abdominal region has a lighter and more yellowish aspect. The dorsal fin alone exhibiting transverse series of blackish spots : the other fins being unicolor. XLVI. Lieut. D. N. Couch has collected, in the waters of the Rio San Juan, at Cadarecta and Monterey, in the Province of New Leon, a species of Limia, which differs widely from its congeners, as will be shown presently. Unfortunately, all the specimens are of the female sex. The largest of these measure one and five-eighths of an inch, being apparently full grown, or, at any rate, adult, for the abdomen is distended by the presence of numerous embryos. The body appears to be rather short and contracted ; the back being convex and gently sloping forwards. The head is small, constituting about the fifth of the total length. The orbit occupies the third of the side of the head. The dorsal fin is longer than high, superiorly subconvex, its anterior margin being nearer the insertion of the caudal than the apex of the snout. Its entire base is placed upon the posterior declivity of the back. The posterior margin of the caudal is. as usual, convex. The anal fin is inserted opposite the posterior portion of the base of the dorsal ; it is narrow and rather deep, and its extremity extends further back than theposterior rays of the dorsal. The ventrals are compara- tively of moderate size, sublanceolate, their extremity extending to the vent. As to the pectorals, they are narrow and elongated, rounded off posteriorly, not reaching a vertical line drawn nt the insertion of the ventrals. The rays are : D 9 ; A 6 ; 4,1,9,8,1,3; V 6 ; P 11. The scales are very large, and exhibit the general structure alluded to in the other species. The dorsal re- gion to the middle of the flanks is almost entirely chestnut-brown, so large are the spots which are observed on every scale. An obsolete band of black exists along the sides. The abdomen and inferior region of the tail are yellowish, with a golden reflect. The fins are unicolor, except the dorsal, which exhibits a few blackish spots. We call this species Limia couchiana. XLVII. Another species of Limia appears to be common about Matamoras, where it was first collected by the late L. Berlandier, whose collection has since been purchased by Lieut. D. N. Couch, a lover and. cultivator of natural sciences. Specimens of the male sex measure nearly two inches in total length, of which the head, which is rather small, constitutes about the fifth part. The body is very much compressed, rather deep, maintaining its depth along the peduncle of the tail. The upper surface of the head, as usual, is very much depressed and flattened. The profile is gently sloping from the origin of the dorsal fin to the apex of the snout. The eye is well developed, subcircular, its diameter entering about three times in the length of the side of the head. The dorsal fin is longer than high, and equally elevated throughout its whole length, the tip of its posterior rays not extending as far as the insertion of the caudal fin. The anal is inserted somewhat posteriorly to the anterior margin of the [April, NATURAL SCIENCES OF PHILADELPHIA. 117 dorsal, and close to the ventrals, from which it is separated by the anal aper- ture alone. The ventrals themselves are of moderate development, overlapping the vent and projecting beyond the insertion of the anal ; the second ray is much longer than the rest. The pectorals are elongated, their tips extending beyond the insertion of the ventrals and the origin of the anal without reaching as far as the tip of the ventrals. The rays are : D 14 ; A 7 ; C 5, 1, 9, 8, 1, 5; V 6; P 12. The largest specimens of the female sex which have come under our observa- tion, measure but an inch and a half. The general aspect of the body is the same as in the male sex; the head, however, is somewhat larger, being con- tained about four times and a half in the total length. The dorsal fin is much smaller than in the male, and convex upon its upper margin. The anal fin is rather small and inserted opposite the middle region of the dorsal. The ven- trals overlap the vent, but tueir extremities do not quite reach the anterior margin of the anal. The tip of the pectorals extends beyond the origin of the ventrals, but not as far as the anal fin. The anal fin has nine rays. The sec- ond ray of the ventrals is even with the rest. The scales are large, much deeper than long, anteriorly subtruncated, and rounded off upon the rest of the peri- phery. Radiating furrows may be observed upon their anterior section only. The ground color is reddish brown, lighter beneath than above, with longi- tudinal series of d^rk spots corresponding to the series of scales, and more con- spicuous along the dorsal region than elsewhere. The dorsal flu is transvers- ally barred with series of blackish spots, as well as the upper lobe of the cau- dai. The other fins being unicolor. The above species we propose to designate under the name of Limia matamo- rensis. XLVIII. A new genus to which we give the name of Actinia, has the general physiognomy of Limia, but differs from it, as well as from Pcecilia, by the struc- ture of its mouth. The latter is protractile, rather cleft, dearly horizontal when retracted, and slightly directed downwards when protracted ; the jaws being equal, the snout subcorneal, instead of being truncated as in Limia and Pctcilia. The lower jaw is also better developed than in the genera just alluded to, and the upper one is convex instead of being depressed. The male sex differs but little from the female; the dorsal and anal fins holding the same relative po- sition in either of them, being simply larger in the male than in the female. The posterior margin of the caudal fin is subtruncated. Specimens of the typical species of this genus, and, as yet, the only one known, were collected at Galveston, Texas, by Dr. C. B. Kennerly, under Capt. A. W. Whipple, at St. Joseph's Island, Tex., by Gustavus Wurdemann, and at Indi- anola, Tex., by John H. Clark, under Col. J. D. Graham. The largest ones observed measure less than an inch and a half in total length, in which the head enters about three times and a half. The head is, therefore, well devel- oped, wedge-shaped, the profile being quite declivous from the origin of the dorsal fin to the apex of the snout. The greatest depth of the body corresponds to the anterior margin of the dorsal, and diminishes rapidly backwards. The eye is la r ge and circular, its diameter entering three times and a half in the length of the side of the head: once in advance of its anterior rim. The dor- sal fin is higher than long, and quite elevated in the male sex ; its anterior mar- gin is nearly equidistant between the apex of the snout and the posterior edge of the caudal fin. The anal fin is deeper than long, and deeper in the male than iu the female ; its anterior margin corresponding to the middle of the base of the dorsal, and extends more backwards than the latter fin. Its exterior mar- gin is rounded off, or convex. The ventrals are rather broad and overlap the vent, whilst the pectorals are elongated and extend beyond the origin of the ventrals. The second ray of the latter fins does not project beyond the others, as is the case with the species of Limia. The rays are: D 9 ; All; C 4,1, 1859.] 118 PROCEEDINGS OP THE ACADEMY OF 8, 7, 1, 4 ; V 6 ; P 15 The scales are somewhat deeper than long, anteriorly truncated and posteriorly rounded, whilst the upper and lower margins are nearly straight and parallel. The concentric lines of growth are very fine and numerous, and short radiating farrows occupy almost the entire anterior mar- gin. The dorsal region and tipper surface of the head are greyish olive or oliva- ceous brown, with a darker line at the periphery of the scales. The flanks are fasciated alternatively with greyish brown and light yellowish transverse nar- row bands, the more conspicuous as they approach the peduncle of the tail ; the brown *bands being wider than the light yellowish ones ; there are how- ever instances in which light streaks subdivide the brown bands. The oper- cular apparatus is silvery : the lower part of the bead and the belly exhibit- ing a uniform light olivaceous or yellowish tint. The name of Adinia multifasciata appears to us quite characteristic of the species which is here described. An immature female specimen is figured on Plate xxxviii, figs. 12-14 of the "Ichthyology of the U. S. and Mexican Boun- dary," where it is given as the female sex of Limia pceciloides, an error which we now rectify. XLIX. Another new genus, which we call Lucania, has the general appear- ance of Fundulus, from which it differs by the presence, upon the jaws, of one row of teeth only ; the mouth itself being fashioned as in Fundulus : the up- per jaw being smaller and somewhat shorter than the upper, arched sideways and subdepressed superiorly. The head is somewhat rounded off and blunt. The insertion of the anal fin is more posteriorly than the dorsal. The caudal is rounded off. The scales are of but moderate development, deeper than long, with fine concentric strife, and furrowed upon their anterior section. The sexes afford no greater differences than in Fundulus and Hydrargyra. The typical species of the genus which is here instituted, was figured and described by us under the name of Limia venusta in the "Ichthyology of the U. S. and Mexican Boundary," plate xxxix, figs. 20 23, p. 71. Its present systematic name, therefore, will be Lucania venusta. Fig. 21 gives a most perfect idea of the shape and structure of the mouth. The lateral line is not always so conspicuous as represented in fig. 20. The teeth themselves are proportionally larger than in the following species. The anterior margin of the dorsal fin is nearly equidistant between the apex of the snout and the in- sertion of the caudal. The anal is placed opposite the posterior half of the dorsal, and consequently projects further back. The ventrals are slender, extending as far as the vent, and composed of six rays and not five, as formerly stated. The pectorals are elongated, posteriorly rounded off, and projecting beyond the insertion of the ventrals. The rays are : D 13 ; A 11 ; C 3, 1, 8, 8, 1, 2 ; V 6 ; P 10. The scales are deeper than long, anteriorly subtruncated, rounded off upon the remaining edges, with radiating furrows upon the anterior section only, the concentric lines of growth being very fine. The ground color is reddish brown, with groups of dark dots on the centre of the scales ; the fins being unicolor, of a yellowish olive tint. A specimen of this species was collected at Indianola, Tex., by John H. Clark, under Col. J. D. Graham, while on the U. S. and Mexiean Boundary Survey. L. We find in the collection of the late L. Berlandier two specimens of a species of Lucania, collected in the neighborhood of Matamoras, resembling very closely the preceding one. The only differences which we are able to detect consist in a larger mouth and larger scales, a more backward position of the dorsal and anal, together with the following formula of the fins : D 12 ; A 11 ; C 4, 1, 7, 7, 1, 3 ; V 6 ; P 12. The coloration is the same. The speci- mens not being perfect, a further comparison could not be instituted. We shall designate them provisionally under the name of Lucania affiiiis. LI. Amongst the fishes collected in the vicinity of the city of Mexico, by Maj. [April, NATURAL SCIENCES OF PHILADELPHIA. 119 W. Rich, in 1853, we notice a cyprinodont of a very peculiar external appear- ance, belonging nevertheless to the genus Lucania, as characterized above. One of the female specimens measures two inches and a half in total length. The dorsal region is very much arched from the insertion of the dorsal fin to the nape, which is quite swollen. The head is rather small, constituting the fifth of the total length, its upper surface is subdepressed, the occipital region appearing concave from the sudden rising of the nape, a trait less conspicuous in smaller specimens of the same sex and in the males also. The snout is short, thick and blunt. The gape of the mouth is oblique upwards as in the other species of this genus. The eye is subcircular, its diameter entering three times and a half in the length of the side of the head. There are three slender branchiostegal rays on either side, the outermost being exiguous. The anterior margin of the dorsal fin is nearly equidistant between the apex of the snout and the posterior margin of the caudal fin ; its upper margin is convex and its base is longer than the height of the middle rays. The caudal fin enters a little short of seven times in the total length. The anal, is smaller than the dorsal, but has the same shape, and the same propor- tions between its base and its depth. Its anterior margin is placed poste- riorly to that of the dorsal ; the tip of its rays extending but very slightly further back than those of the latter, so that the two fins are nearly even posteriorly. The ventrals are very small and reach the vent with their extremities. The pectorals are of moderate development, rounded off, not ex- tending as far as the origin of the ventrals. The rays are : D 20 ; A 23 ; C 5, 1, 10, 10, 1, 6 ; V 6 ; P 12. The scales are comparatively small, deeper than long, snbelliptical in their outline, exhibiting extremely fine concentric lines of growth, and provided with radiating furrows upon their anterior section alone. The ground color is olivaceous brown, with transverse dark brown bands which run occasionally together giving the entire body, head and fins, a greyish black appearance. Otherwise the fins assume a greyish olive tint. The male sex is more slender than the female ; the dorsal and anal fins being somewhat more developed, and the back less arched. The coloration is similar in either sex. LII. In speaking of the generical characters to be assigned to Girardinus, and especially of the structure of the mouth, we ought to have stated that the latter is depressed, instead of being rounded, and constructed after the fashion of that of Pacilia and Limia, so that its gape is directed upwards when con- tracted, and downwards when protracted. Accordingly its affinities with the latter two genera are more intimate than with Gambusia. The specimen of Girardinus occidentalis, figured, size of life, on plate xxxix, of the " Ichthyology of the U. S. and Mex. Boundary," is the largest of those collected in the Rio Santa Crux, by John H. Clark, under Col. J. D. Graham. Specimens two inches and a quarter in total length were subsequently collected at Tuczon, Sonora, by Arthur Schott, under Major Emory. All these speci- mens belong to the female sex. The following formula of the fins is to super- sede that which has been previously published : D 7 ; A 7 ; C 4, 1, 7, 7, 1, 3 : V 6 ; P 12. The scales are subelliptical, deeper than long, with radiating fur- rows upon the anterior section alone. The ground color is either reddish or olivaceous brown above, and yellowish white beneath, with a golden reflect during the breeding season. The periphery of the scales exhibits blackish dots occasionally so crowded as to assume a dark appearance. Along the middle of the flanks may be seen a black fillet which imitates a lateral line ; the series of scales over which it runs is sometimes entirely black. A black streak is observed along the under edge of the peduncle of the tail. The fins are of a uniform light yellowish tint. We refer, for the present, to the same species, numerous specimens in a rather indifferent state of preservation, collected at Tuczon, by Dr. A. L. H er- mann, under Lt. J. G. Parke. Amongst them we observe several individuals 1859.] 120 PROCEEDINGS OF THE ACADEMY OF of the male sex, measuring about an inch and a quarter in total length, rather slender in general appearance, and resembling somewhat the same sex in Gam- busia. The anal fin, however, is more slender and deeper than in the latter genus, it being composed of but two developed rays preceded and followed by inconspicuous rudimentary ones. The other fins are so much mutilated as not to allow counting their rays with any degree of certainty. The coloration is the same as in the female sex, just alluded to above. LIII. Specimens of a species closely, allied to the foregoing one, were collected in San Bernardino creek, Mex., by Dr. C. B. R. Kennerly, under Major Emory. That creek, it will be remembered, flows westwards of the Sierra Madre, ming- ling its waters with those of the Rio Yaqui, which empties itself into the Gulf of California. The largest of these specimens belonging to the female sex measure two inches and a quarter in total length, being therefore of the same size as some of those of the preceding species. Nothing is more alike than the general aspect of these two species ; the present one, however, is more stoutly built. The head constitutes about the fifth of the total length. The caudal fin is pos- teriorly subtruncated. The dorsal and anal fin are inserted somewhat farther back, each beine; provided with eight rays instead of seven ; otherwise the for- mula is the same : D 8 ; A 8 ; C 4, 1, 7, 7, 1, 3 ; V 6 ; P 12. The scales have the same shape and structure, but they are proportionally smaller, than in the preceding species. The specimens of the male sex, measure about an inch and a quarter or a little more. They bear the same relations to their females as those of the pre- ceding species. The dorsal fin exhibits likewise eight rays. The ground color, in either sex, is of a dark chestnut brown, with black dots at the periphery of the scales, and a lateral black fillet covered by a lateral streak of the width of a scale. A narrow dark streak may also be observed under the peduncle of the tail. In its coloration, therefore, this species does not differ very materially from the foregoing one. The lateral streak alone ap- pears as a more constant feature. We shall designate it provisionally under the name of G. sonoriensis. LIV. Let it be recalled to mind here, that the mouth in Gambusia is construct- ed after the fashion of Hydrargyra and Zygonectes, and that its gape is horizontal when protracted, and oblique upwards when in a contracted state. Indeed, the affinities between Gambusia and Zygonectes are of the most intimate kind, since in Zygonectes the anterior margin of the anal fin is sometimes situated in advance of the anterior margin of the dorsal. It is true, we find a slight dif- ference between these two genera, in the gape of the mouth when in a pro- tracted condition, and also in the sexes, which assume a different aspect in Gambusia, whilst in Zygonectes the differences between the male and the female are a great deal more restricted. The party under Lt. J. G. Parke, on its way home, collected in Caman- che Spring specimens of both sexes of Gambusia nobilis, the male of which we had not observed so far. It has the same general aspect as its female, figured on plate xxxix, of the "Ichthyology of the U. S. and Mex. Boundary," being rather short and deep bodied compared to its congeners. In coloration both sexes agree. The largest specimens of the female sex measure two inches and those of the male one inch in total length. LV. Specimens of Gambusia affinis were also collected in San Pedro creek, Tex., and in Dry creek near Victoria, Tex., by Dr. C. B. R. Kennerly, under Major Emory. The male sex measures one and a tenth of an inch in total length, and compares well with the female figured on plate xxxix, of the ' ' Ich- thyology of the U. S. and Mex. Boundary," having the same slender appear- ance and general aspect. The anal finis somewhat deeper than in G. patruelis represented on the plate just alluded to. The color is similar in either sex. [April; NATURAL SCIENCES OF PHILADELPHIA. 121 LVI. As to Gambusia pa'ruelis, numerous specimens of that species were col- lected in the upper affluents of the Rio Nueces, by Dr. C. B. R. Kennerly, under Capt. A. W. Whipple, during the Exploration near the thirty-fifth parallel, for a railroad route to the Pacific. The average size of either sex corresponds pretty nearly to the specimens figured on plate xxxix, of the "Ichthyology of the U. S. and Mex. Boundary." Specimens from the Rio Leona, Rio Blanco, and Rio Seco, exhibit a somewhat lighter tint than those from the lower part of the same hydrographic basin. But this may be an alteration subsequent to their immersion in alcohol. LVII. A curious little species of Gambusia from the hydrographic basin of the Rio San Juan, specimens of which having been collected in Rio San Diego, one of its affluents, near Cadereita, New Leon, by D. N. Couch. The largest ones measure an inch and a half in total length, and belong to the female sex alone. The body is deep upon its middle and the tail tapering. The head enters about four times and a half in the total length. The eye is proportionally large and circular ; its diameter entering three times in the length of the side of the head. The dorsal fin is very narrow and elevated, and proportionally higher than in the other species so far known of this genus. The anal fin is likewise nar- row and deep, and resembles the dorsal in that respect. The ventrals are small, and the pectorals well developed. We have not been able to count with accuracy the rays of the fins, owing to the desiccated condition of the specimens preserved ; in the dorsal and anal fins they are less numerous than in the other species of the genus. The color of the body is reddish-brown, except the belly, which is yellowish or whitish. Small black spots may be observed along the dorsal region near the base of the scales. The dorsal and anal fins are greyish ; the caudal ventrals and pectorals, olivaceous. The species might be designated under the appellation of Gambusia speciosa. LVIII. In the collection of the late Louis Berlandier, of Matamoras, we find another species of Gambusia, which differs from its congeners by the slender- ness of its form and general appearance : hence the name of G. gracilis by which we propose to record it. The largest female specimens measure about an inch and a half in total length, of which the head constitutes a little more than the fifth. The mouth is rather large compared to that of the foregoing species. The diameter of the eye enters about three times in the length of the side of the head. The body in its profile is subfusiform. The dorsal fin is higher than long, superiorly convex. The caudal is rounded off posteriorly. The anal is larger than the dorsal, deeper than long and exteriorly convex, the posterior extremity of its insertion being nearly opposite the anterior margin of the dorsal. The tip of the ventrals extends almost to the anterior margin of the anal. The pectorals are well developed and project beyond the insertion of the ventrals. The rays are : D 6 ; A 9 ; C 5, 1, 6, 6, 1, 4 ; V 6 ; P 13. The scales are moderate sized, much deeper than long, subelliptical in their outline, more convex posteriorly than anteriorly with numerous and well developed radiating furrows upon the anterior portion alone. The largest male specimens which have come under our observation mea- sure a little over an inch in total length. They are very similar to the female sex, rather more slender. The anal fin exhibits the usual structure peculiar to that genus. The first ray is a mere rudiment ; the second being the stoutest and longest ; the third forms, with the second, the elongation of that fin, and is followed by four shorter rays somewhat better developed, however, than in the other species, which we have examined. The color is olivaceous brown ; the dorsal and caudal fin exhibits narrow transverse, blackish bars ; the other fins being olivaceous. LIX. Mr. John Potts has collected in Chihuahua River another species of Gam- busia which appears to reach a larger size than any of the foregoing spe- 1859.] 122 PROCEEDINGS OF THE ACADEMY OF cies, reminding us somewhat by its general appearance those occurring in Cuba. The specimens before us are all of the female sex, and measure two inches and a quarter in total length, in which the head enters about five times. The head itself is rather short, whilst the mouth is proportionally large. The dia- meter of the eye enters thrice in the length of the side of the head. The dorsal fin is higher than long, somewhat convex superiorly. The caudal is rather short and subtruncated posteriorly. The anal is deeper than long and a little broader than the dorsal ; the middle of its insertion corresponding to the anterior margin of the dorsal. The ventrals are very small and far from reaching the vent with their extremities. The pectorals are of moderate de- velopment, spear-shaped when not expanded. The rays are : D 9 ; A 10 ; C 6, 1, 7, 7, 1, 6 ; V 6; P 12. The middle rays of the dorsal and anal fins exhibit bifurcations of the second degree conspicuously developed. The scales are of moderate development. The body is chestnut brown, and the abdomen yellowish golden, with blackish specks along the middle of the flanks to the caudal fin. The periphery of the scales is margined with black. The dorsal, caudal and anal fins are greyish and speckled, the ventrals and pectorals being olivaceous. To distinguish this species from its congeners, the name of G. senilis is here proposed. On the Primary Divisions of the SALAMANDRIDJE, with Descriptions of Two New Species. BY E. D. COPE. Class AMPHIBIA. Order CADUCIBRANCHIATA. Sub. Ord. URODELA. Fam. 1. PROTONOPSID^E. Branchial apertures persistent. (Trematoderes Duin. & Bibr). Fain. 2. SALAMANDRIDJ3. Branchial apertures none. (Aretoderes Dum. & Bibr.) The characters of the following subfamilies are taken from the position, etc., of the palatine and sphenoidal teeth, and we are of the opinion that the groups thus formed will be found to be more natural than those established exclusively upon the form of the tongue. 1. AMBYSTOMIN,. Palatine teeth upon elevated processes of the vomero-palatine bones, in straight or arched transverse series only, sphenoidal teeth absent. Tongue larg>\ thick, papillose, but slightly free. Form stout. Skin mostly smooth. North America. 1. Mf.galobatrachus (Tschudi) 1838. Syn. Cryptobranchus Van der Hoeven, 1838. Sieboldia Bonaparte, 1850. Tritomegas Dumeril & Bibron, 1850. The great aquatic Salamander of Japan is closely allied to our Protonop- Bis (Menopoma Harlan), but the absence of branchial slits places it among the true Salamanders. By the position of the palatine teeth it evidently belongs to the present subfamily, and not among the Tritons, as placed by Dr. Hallowell. (Journ. Acad. Nat. Sci., vol. iii. Second Series, p. 357). 2. Camarataxis Nob. Palatine teeth upon four processes, the two posterior short oblique, and behind the internal nares ; the anterior forming an arch, interrupted at the palatine suture, and concentric with the maxillary series. Tongue broad, thick, papillose, attached by the whole posterior border, slightly free laterally. Extremities stout, digits free, 4 5. Tail not long, compressed [April," NATURAL SCIENCES OP PHILADELPHIA. 123 C. maculata. Ambystoma maculatum Hallowell, Journ. Acad. Nat. Sci., Second Series, vol. iii. p. 355. This species, which inhabits New Mexico, makes the nearest approach to the preceding genus in the form of the series of palatine teeth. In this respect it also exhibits too great a departure from the straight or slightly angular series of Ambystoma, to remain in that genus. 3. Ambystoma (Tsch.) The nearest approach to the preceding species, in general appearance and form of the palatine series, is seen in the Ambystoma nebulosumof Dr. Hal- lowell : but the processes are not arched, but straight, presenting an obtuse angle forward. The genus Xiphonura Tschudi (Heterotriton Gray) does not seem to be suffi- ciently distinct either with respect to dental peculiarities, or the form of the tail. Though Ambystoma ingens, luridnum, and Californiense re- semble each other in these points, and are quite different from the A. opacam, yet by the intervention of such species as A. tigrinum (Green) 1 uscnm (Hallowell) b i c o 1 o r (Hall.) p u n c t a t um (Linn.), which show a regular gradatiou of form, the hiatus is filled, and no generic division can be made. The following species appears to be undescribed : A. c o n s pe r s um . Head oval, rather large ; extremities slender, fourth toe twice as long as second ; tail not longer than body, much compressed; tongue elliptical, very slightly free at the sides ; palatine teeth in two short patches between the internal nares, presenting a concavity backwards. Length 1 inch 10 lines : head 4 1. : body 9 1. : tail 9 1. Head, back and tail cinereous brown, finely speckled with white dots, which are confluent on the snout. An indis- tinct row of white spots on the sides. Beneath dirty white. Londongrove, Chester Co., Pennsylvania. The animal described was probably not fully grown, so that though the measurements indicate the smallest known Ambystoma, the adult may be larger. We are unable to refer it as the young of any of our Pennsylvania Ambystomata. The form of the tail would indicate aquatic habits, but it was found in the woods, and when placed in water showed the greatest aversion to it. It resembles Ambystoma porphyritic um of the Academy's collection, but differs in color of abdomen, lateral series of spots, and larger head and mouth. (We allude to the specimen f