oa. ae eee te Seo ihe ar Tap carter it aes peaks : AR ere ney Bras pet ee te a oy “ tn : Set See npeat8 Wirk ed cits Poa ~ aor 2 r ‘ dl oe" wines ‘ a a peat 2 t “1 ies a, y ‘ ues — ee BULLETIN OF THE AMERICAN MUSEUM OF NATURAL HISTORY. Volume V, 1893. NEW YORK: PUBLISHED BY ORDER OF THE TRUSTEES. 1893. COMMITTEE RP. Wuirriei, — _ Henry Fairrierp O CONTENTS OF VOLUME V. PAGE ArT. Il.—Artionyx, a New Genus of Ancylopoda. By Henry Farr- FIELD OSBORN and JAcoB L. WoRTMAN.................- I II.—Notes on some North American Moths, with Descriptions of New Species. By WILLIAM BEUTENMOLLER.... .......... 19 III.—List of Mammals and Birds collected in Northeastern Sonora and Northwestern Chihuahua, Mexico, on the Lumholtz Archzo- logical Expedition, 1890-92. By J. A. ALLEN.............. 27 IV.—Description of a New Subspecies of Oryzomys from the Gulf memes. De PANE MM. CHAPMAN. 2. ice oso ene ve 43 V.—Descriptions of Four New Species of 7omomys, with Remarks on other Species of the Genus. By J. A. ALLEN............ 47 VI.—List of Mammals collected by Mr. Charles P. Rowley in the San Juan Region of Colorado, New Mexico and Utah, with Descrip- tions of New Species. By J. A. ALLEN..........5......... 69 VIl.—Aceratherium tridactylum from the Lower Miocene of Dakota. Mee Pee ST PAIRPINL TD): OGRORI ou ook Sacicse dis peu seecewees 85 VIII.—Notes on Transformations of some North American Moths. DP WILLIAM BEUTEMMOLLER. | 60S Sci de accuse 5 gees -¥ IX.—On the Divisions of the White River or Lower Miocene of Dakota. By J. L. Worrman, M.D...... .. See ab eeneee 95 2 a ; La , 4 " Iv. Contents. Art. X.—On a Collection of Birds from Chapada, Matto Grosso, Brazil, made by Mr. H. H. Smith. Part III, Pipridz to Rheide. By XI.—Ancestors of the Tapir from the Lower Miocene of Dakota. By J. L. WorRTMAN and CHARLES EARLE............- - 159 XII.—On a Collection of Mammals from the San Pedro Martir Region of Lower California, with Notes on other Species, particularly of the Genus Sitomys. By J. A. ALLEN....... 181 XIII.—On a Collection of Mammals from the Island of Trinidad, with Descriptions of New Species. By J. A. ALLEN and FRANK M.. CHAPMAN: 0.3520 05.0 oad oe x ele ee 203 XIV.—Description of a New Species of Opossum from the Isthmus of Tehuantepec, Mexico. By J. A. ALLEN........ .. «.. 235 XV.—Further Notes on Costa Rica Mammals, with Description of a New Species of Oryzomys. By J. A. ALLEN.... .. ....-. 237 XVI.—Descriptive Catalogue of the Butterflies found within fifty miles of New York City, together with a Brief Account of their Life Histories and Habits. By WILLIAM BrEUTEN- MULLER ooie0oS 5 cae cbse ee Se eae ae) we an ae 241 XVII.—Fossil Mammals of the Upper Cretaceous Beds. By HENRY FAIRFIELD OSBORN. 000.5. a5 sae wes ook 6 alee ee ere 311 XVIII.—Description of a New Mouse from Southern New Mexico and Arizona. By GERRIT S. MILLER, Jt. 0.5 05 see. cee 331 XIX.—Description of a New Mouse from Lake County, California. By J. A; ALLEN. 000. ue ce ced eee te et vecsces® «nen 335 XX.—Description of a New Species of Geomys from Costa Rica. By J. A. ALLEN. < occ ccwsns vesessseesees 5s otpes eae 337 X XI.—Description of Two New Races of Mammals from Florida, with Remarks on Sitomys nivetventris Chapm. By FRANK M. CHAPMAN, . oa55 5 0s Ub be Sa ese Sate ae eR ee ere ee 339 JTilustrations. V. LIST OF ILLUSTRATIONS. Cuts. PAGE Right pes of Artionyx vaudryi, front view. ........-.- -sseee eee cree 2 Right pes of Chalicotherium magnum .....+.-.0+..005 52sec reece ees 3 Right pes of or Pitidr yi, Mamet WOW sc rh oie ies oak ces 9 Nk 7 = = ie ORIET VIEW ecco eae ae 10 Median digits of Chalicotherium sansaniense, Artionyx gaudryi, Hoplopho- neus occidentalis, and Megalonyx jeffersoni ...... .-.+-.-++++00+++- II Variation of bill in Galbula rufoviridis. ©... 02... cece cece ce ete ee eee ee 133 Evolution of molars in Protapirus and Tapirus........- rere eee igves SO Protapirus obliguidens, crown view of lower dentition .....-........-.-- 165 = = Side view Of lowe? jaW eso = oes ne eens 166 sik cy anterior view of left manus ....... ..........-. 167 Crown view of second superior molar of Colodom sp?.... -...-.+-+-+-+++- 175 Colodon occidentalis, crown view of inferior dentition .. ..-.......--.--. 175 oe anterior view of right manus....... Pee ee 177 Type of Ptilodus trovesartianus..........- +--+ 20ers eee e teens eee ee Fourth inferior premolar of species of Ptilodus......... Baas ahr Site eh 315 Relations of typical Tritubercular molars............ .--.-+-+---+-++---- 321 Type specimens of Didelphops vorax, Cimolestes incisus, Pediomys elegans, Platacodon nanus, — nitor, Telacodon levis, and Batodon Plates. Plate I.—Top view of skulls of various species of Thomomys. Plates II-VI.—Butterflies of the vicinity of New York. Plates VII, VIII.—Cretaceous Mammals (PI. VII, Laramie Multitubercu- lates ; Pl. VIII, Laramie Trituberculates). DATES OF PUBLICATION OF AUTHOR’S SEPARATES. Art. I, February, 1893. Art. II, February, 1893. Art. III, March 16, 1893. Art. IV, March 17, 1893. Art. V, April 28, 1893. Art. VI, April 28, 1893. Art. VII, April 29, 1893. Art. VIII, May 1g, 1893. Art. IX, June 27, 1893. Art. X, July 19, 1893. Art. XI, August 18, 1893. Art. XII, Aug. 18, 1893. Art. XIII, Sept. 21, 1893. Art. XIV, Sept. 22, 1893. Art. XV, Sept. 22, 1893. Art. XVI, Nov. 29, 1893. Art. XVII, Dec. 15, 1893. Art. XVIII, Dec. 16, 1893. Art. XIX, Dec. 16, 1893. Art. XX, Dec. 16, 1893. Art. XXI, Dec. 22, 1893. Besides the author's separates, and in addition to the regular edition of the Bulletin, 100 as god were issued in signatures as printed, each signature bearing at the bottom of the first page the date of publication. ee st BULLETIN OF THE AMERICAN MUSEUM OF NATURAL HISTORY. Volume V, 1898. Article I—ARTIONYX, A NEW GENUS OF ANCYLO- PODA. By Henry FAIRFIELD OsporNn and Jacosp L. WorTMAN. In the last volume of this Bulletin (1V, pp. 351-371) we described a new Artiodactyl, Protoceras, and in the present paper we record the discovery of remains of a mammal of even greater interest. It is, so far as can be judged from the foot structure alone, a Chalicotherioid with an Artiodactyl type of foot; that is, with the astragalus, calcaneum, cuboid, all modified as in the Artiodactyla, with toes in pairs on either side of the median line, and with phalanges like those in the Carnivora. Besides these four functional toes in the hind foot there are portions of the hallux, indicating that this digit, although much smaller than the others, was still of considerable size, and provided with phalanges. Another distinctive feature is that none of the phalanges are cleft, whereas in Cha/icotherium they are all deeply cleft. We had anticipated finding skeletal remains of Chalicotherium | in the Lower Miocene of America, because the teeth have recently 3 been found both in the Lower and Upper Miocene, indicating ) that this form was distributed over this continent, and this foot was at first supposed to belong to Chalicotherium. But a closer examination showed that while Chalicotherium may be described as a clawed Perissodactyl, this new form, which we have named Artionyx, may with equal fitness be termed a clawed Artiodactyl. [February, 1893.] [1] 1 ny ee hae 2 Bulletin American Museum of Natural History. |Vol. V, Thus the group Ancylopoda must be enlarged to embrace two distinct subdivisions: the Perissonychia—animals resembling the odd-toed Ungulates in foot structure; and the Artionychia— animals resembling the even-toed Ungulates in foot structure. It will be remembered that the species of Chalicotherium have long been known under two sets of names; one set, under the ~ genus Chalicotherium, being applied to its teeth, and the other, under the genera Schizotherium, Macrotherium, Ancylotherium and Moropus, being applied to its feet. Filhol, in 1888, first conject- ured that these two forms might really be one. We recall also that Filhol confirmed this conjecture by his discoveries in Sansan, and that Forsyth Major arrived at the same conclusions in his explorations of Pikermi beds. Quite re- cently Depéret has described parts of a skeleton and skull found together at Grive St. Alban, in beds nearly contemporaneous with Sansan. It is probable that a similar 1877 Marsh described three species of Moropus (distans, senex and elatus) from the Middle and Upper Miocene of Oregon and Nebraska, considering them as large Eden- . tates. The types consisted of a number of ' loose phalanges, and the author compared them with those of Ancylotherium (now — known to be identical with Chalicotherium) rather than with any true Edentates; AZoro- — pus being considered distinct because of. the coalescence of its first two phalanges. — page STS ee Undoubted remains of Chalicotherium in — front view of right pes. this country were found later by Garman confusion has arisen in this country. In in the Loup Fork (Upper Miocene), and described by Scott and Osborn. Cope has also described the teeth of a Lower Miocene © species (C. di/obatum) from the White River beds (Swift Current — Creek) of Canada. It is probable that all these species belonged — to the order Ancylopoda, and as the distribution of members of this order in America and Europe is known to have been extended at least to the Siwaliks in Asia, we reach the conclusion that this order, which has become very recently known, was widely dis- 1893.] Osborn and Wortman on the Genus Artionyx. 3 tributed in the Miocene, and, as proved by the differences between the Sansan and Pikermi forms, and still more by the differences between Chalicotherium and Artionyx, was highly differentiated. The remains known to us at present indicate, therefore, that we have mere glimpses of a very important order, the remains of which have for some reason been rarely preserved fossil. In a recent number of the ‘Revue Scientifique,” Ameghino has re- peated the opinion expressed in 1891* that the Homalodontotheridz are the ancestors of the Chalicotheriidz. This ancestry is impossi- ble because Homalodontotherium has a typical lophodont dentition while Chalicotherium is buno-selenodont; it is by no means im- possible, however, that this Patagonian genus is a member of the Ancylopoda. Ameghino has pointed out many features of the skeleton in which it strikingly resembles Chalicotherium. ‘The carpals and tarsals are alternating or diplarthrous ; there are five _ digits upon the robust fore and hind feet, and the ungual phalanges are shaped as in Chalicotherium with deep median clefts. The humerus has an epitrochlear perforation, and in general the limbs are modified as in the Edentates. The calcaneum is described as of the Litopterna type, with a very convex facet for the fibula. The head of the astragalus is extended and convex, with a nearly plane tibial trochlea. If Ameghino’s supposition is correct this still further widens the distribution of the Ancylopoda. The structure of the limbs of Cha/icotherium, which has been mainly made known by Gervais, Filhol and Depéret, indicates that it was a digitigrade, not a plantigrade, as restored by Filhol. Osborn pointed out the perissodactyl character of the carpus and _ tarsus. The limbs are now com- pletely known, and indi- cate that there was little or no prehensile power. It is a peculiarity of both fore and hind feet that Fic. 2. Chalicotherium magnum, outer view of hey are turned somewha eet one rae. agn they are ed ewhat 1 Mammiiferes Fossiles de la Patagonie Australe. , 33: mm, There are apparently no diagnostic cranial characters. ReMARKS.—There are two interesting points developed by the range of this new form. First, it is somewhat unexpected to find Texas specimens resembling those from Florida. For example, the Seaside Finches of Florida (Ammodramus nigrescens and A. maritimus peninsula) are the darkest of the genus, while the race from Texas (A. m. sennetti) is the palest. Still Orvsemys inhabits the same marshes in which these Finches abound, and is apparently subjected to the same environmental influences, I say apparently, for a field experience in both Florida and Texas marshes gives 1893.] Chapman, Description of a New Oryzomys. 45 me reason to believe that while these localities are separated by a thousand miles, and are included in different faunz, in the case of these Rats at least, the character of their haunts in Florida is in effect so like that in Texas that no real difference exists in their immediate surroundings. The Finches before mentioned, which show in their respective plumages the effects of climates char- acterized respectively by heavy and comparatively light rainfall, are diurnal inhabitants of the air, where they are exposed to the full force of climatic influences. The Rats, on the contrary, are noc- turnal, and almost subterranean. That is, their runways are made beneath the dense mat of grasses which cover the marshes border- ing the gulf. In these half-flooded situations there can be little difference in the humidity of their habitats ; existing thus, under similar conditions, they exhibit similar phases of coloration. To illustrate further the effect of environment I may instance a series of Sigmodon collected by myself at Corpus Christi, Texas, the same locality in which Oryzomys was observed. Sigmodon is very abundant there, inhabiting in large numbers both the dry, scrubby chapparal and swampy marshes. In the former case its runways were easily observable as well-worn paths ; in the latter they led beneath the dense mat of marsh grass, indeed were the same as those used by Oryzomys. Series of Sigmodon were col- lected in both the chapparal and marsh, each specimen being labeled with its exact locality. On comparison these series are easily distinguishable from each other, the specimens from the marsh being darker, and thus showing the result of their more humid home and protection from the sun’s rays afforded by their covered run ways. Both this instance and the preceding show the importance of field-study. The second point of interest in the range of O. f. natator is the near approach of its habitat to that of the very distinct Oryzomys aquaticus Allen. Although I have but one specimen from the known southern limit of the range of natator (Rockport, Texas), I have examined several specimens caught at Corpus Christi, but which unfortu- nately were too decayed to preserve. They showed, however, no approach to Orysomys aguaticus. This species is known only from from its Mexican ancestors, whether zs e at some point between Corpus Christi and J i aa A lO a i am = ee Nee ee iil be cl Tae Pe re Article V.—DESCRIPTIONS OF FOUR NEW SPECIES OF THOMOMYS, WITH REMARKS ON OTHER SPECIES OF THE GENUS. 3 By J. A. ALLEN. In working up a collection of mammals from the San Juan region of Colorado, New Mexico and Utah (see next paper), two apparently very distinct new species of Zhomomys were recognized. In attempting to define their status and relationships it became necessary to take into account the previously described species, which further involved the consideration of many vexed questions of synonymy. From this investigation has resulted the present paper, which consists essentially of four parts : 1, Descrip- tions of New Species; II, Discussion of various questions of Nomenclature ; III, Remarks on Cranial Characters in the genus Thomomys ; 1V, List of Species and Subspecies. In this connection I wish to express my hearty acknowledg- ments for the invaluable assistance kindly rendered me by various institutions and persons, through the loan of types and other material to facilitate my investigation. To the authorities of the Academy of Natural Sciences of Philadelphia, through the kind intervention of Mr. Witmer Stone, Curator of Birds and Mammals, for the loan of the historic Townsend specimens which served as the basis of Dr. Bachman’s descriptions of his Geomys borealis and G. townsendit. To Mr. F. W. True, Curator of Mammals at the United States National Museum, for the type of Prof. Baird’s Thomomys laticeps,and for many of the specimens on which Baird based his revision of the genus in 1857, and which later formed part of the material used by Dr. Coues in his monograph of the genus, including the type of his Zomomys c/usius—in other words, for authentic specimens of the various forms recognized by these two authors. To Dr. C. Hart Merriam, Chief of the Division of Ornithology and Mammalogy, United States Department of Agri- culture, for specimens identified by him as 7. clusius, and for authentic specimens of his 7. c/usius fuscus. To Prof. C. H. [47] 48 Bulletin American Museum of Natural History. |Vol. V, Gilbert, of the Leland Stanford Junior University, of California, for the series of specimens described below as a new species, under the name Zhomomy monticolus. And finally to Mr. Gerrit S. Miller, Jr., of Cambridge, Mass., for specimens of Richardson’s “Diplostoma? bulbivorum,” from the type locality of the species, and for permission to publish as inedited matter extracts from an unpublished paper of his on this important discovery. I.—DeEscCRIPTIONS OF NEw SPECIES. Thomomys monticolus, sp. nov. Size medium. Skull long and narrow. A strong ridge on the inner edge of the outer face of the upper incisors. Claws long and rather slender. Ears — prominent. Pelage very long and soft. Above dull pale reddish brown, strongly — tinged with gray ; below ashy white, sometimes with a faint tinge of buff ; feet and tail whitish ; mouth parts and entrance to pouches blackish ; no white throat spot ; ears in a large blackish area, of more than the usual extent. Measurements.—Total length (from skin), 210 mm.; tail, 55 ; hind foot, 28; fore foot, 20; middle fore claw (arc), Id. , Skull,—The skull (Pl. I, Figs. 3 and 4) is narrow and elongated, the anteorbital portion especially narrow and slender. Interparietal bone very broad, about half the width of the skull, rounded in front, twice as broad as long. The nasals terminate a little in front of the fronto-intermaxillary suture. Upper incisors with a strong ridge on the inner margin of the outer face. Total length of skull, 37 mm.; basilar length, 34; greatest breadth, 22; least interorbital breadth, 6; length of nasals, 14; width of nasals at posterior border, 2; length of interparietal bone, 4; its greatest width, 11. Type, é ad., No. 59, Mus. Leland Stanford Junior University, W. W. Price, coll., Mt. Tallac, El Dorado Co., Cal., Aug. 8, 1892 (altitude, 7500 feet). This species most resembles in coloration specimens of 7.— douglasii from Ducks, B. C., but is grayer and of a dull pale chest- nut instead of yellowish brown above, and purer gray below. The claws are longer and much weaker. ‘The size and form of the interparietal bone is somewhat similar in the two, as are the general form and proportions of the skull. The sulcus at the inner border of the upper incisors is rather more developed, being readily distinguishable without the use of a lens, It is, however, apparently a much larger animal. 1893.] Allen, New Species of Thomomys. 49 T. monticolus differs from Nicasio (Cal.) specimens of Thomomys botte (=bulbivorus Baird, nec Richardson—see beyond, pp. 56-58) very markedly in the color and texture of the pelage throughout, lacking entirely the yellowish cast in that species, both above and below. The claws are longer and more curved. It-also differs from the Nicasio species in the general form and proportions of the skull, in the latter the skull being short and broad, especially the anteorbital portion, while in 7. monticolus the whole skull is attenuated, and hence much narrower and longer, giving a slender, lengthened nose, instead of a short broad nose. In Nicasio speci- mens also the sulcus near the inner border of the incisors is usually _ obsolete and often wholly wanting. In Plate I are represented skulls of 7. monticolus, T. douglasii and T. botte, showing the differences in the cranial characters above noted. This species is based on four specimens, kindly loaned for identification and description by Prof. Charles H. Gilbert, of the Leland Stanford Junior University, at Palo Alto, California. Two are adult and two young, one of the latter being about half grown and the other apparently only a few weeks old. The half- grown one differs but little in color from the adults, being rather _ paler and grayer. The very young one is dull brownish gray above, passing into clear grayish white below. Respecting these specimens the collector, Mr. W. W. Price, has kindly furnished me with the following memoranda : “The specimens of Zhomomys were taken on Mt. Tallac, at altitudes varying from 6500 feet to g500 feet. The specimens were abundant in grassy glades and during the day were often seen throwing up earth about their burrows. “The smallest specimen was taken in level meadow land at the ___ base of Mt. Tallac at about 6500 feet. The largest specimen was taken on the slope of Tallac at about 7500 feet elevation. The other two skins were taken near the summit, at over gooo feet altitude.” Thomomys aureus, sp. nov. Size large. Claws strongly developed. Skull, as seen from above, much as in Nicasio (California) specimens of 7. Joffe, but with many differences in details of structure. Coloration very different from that of any form hitherto described (April, 1893.) 4 5° Bulletin American Museum of Natural History. [Vol. V, Post-breeding Pelage.—Fur short, thin and soft. Above uniform strong sandy yellow or golden with a few dusky-tipped hairs on the crown, and in some specimens along the back ; below entirely white to the base of the hairs ; muzzle blackish, the dusky tint extending on to the edge of the pouches, there passing into white. A small blackish area below and behind the ear ; upper surface of feet white ; basal half of tail yellowish, passing into whitish apleatiie Breeding Pelage.—Above dull yellowish with a dusky shade due to the plum- beous base of the fur showing through the slight surface wash of yellowish buff ; below grayish white, due to the dusky plumbeous basal portion showing —— the clear grayish white surface tint. ; Measurements.—Average of 12 specimens, from collector’s measurements taken in the flesh: Total length, 296 mm.; tail, 66; hind foot, 35. Skull.—(Pl. 1, Figs. 6 and 7.) Similar in size and general outlines to that of 7. botte, but broader in proportion to its length, with the interorbital and rostral portions especially broadened, and the whole skull much more heavily ossified throughout. In respect to the size and form of the interparietal bone, and the posterior extension of the nasal bones, the two forms present much similarity. The auditory bulle in 7. aureus are larger and somewhat different in outline ; the crown surfaces of the teeth are broader in proportion to their length; the position of both palatine and the infraorbital foramina are more posterior than in 7. dotte ; and there are minor but very appreciable differences in other parts. In general details the skull of 7. aureus perhaps more closely approaches that of 7. perpallidus, but the two are readily separable, aside from the great differ- ence in size. No comparison is necessary with the skull of 7. /s/vus, as shown by a comparison of the figures in Plate I. An average full-grown skull measures as follows: Total length, 41 mm.; basilar length, 37; greatest breadth, 24; least interorbital breadth, 6; length of nasals, 14. Type, No. $243, Am. Mus. Nat. Hist., Bluff City, Utah, May 12, 1892, Charles P. Rowley, collector. Thomomys aureus needs no comparison with any of its allies. It is nearly twice the size of 7. fudvus, and differs from all the other species of the genus in its peculiar deep yellow coloration. The 12 specimens on which 7. aureus is based were collected by Mr. Charles P. Rowley, at Bluff City, Utah (altitude 4500 feet), May 10-24, 1892. ‘Two are young adults (probably young of the previous year), the others middle aged or old. Most of the speci- mens are in molt, and hence in the patchy, transition stage. Two or three have nearly completed the new dress, described above as the post-breeding pelage ; several others retain for the most part the preceding pelage, or that of winter (described above as’ 1893.] Allen, New Species of Thomomys. 51 the breeding pelage) ; the others are in mixed dress. They thus present a wide range of color variation, those in old worn pelage being yellowish gray, with the dusky under fur showing through the surface, while those in the new dress are deep golden with the _ pelage of the lower surface entirely clear white to the roots of the hair; others combine both colorations, arranged more or less in _ patches. Several females which probably had young show the number of mammz to be 6, two pairs being pectoral and one pair inguinal, the two axillary pairs found in some of the other species of the genus (as 7. c/usius) being absent. Thomomys fossor, sp. nov. Size large. Claws strongly developed. Interparietal large, strongly convex in front ; nasals terminating posteriorly on a line with the intermaxillaries. Above dusky brown, the hairs slightly tinged with gray, the middle of the dorsal region, from the front of the head posteriorly, with a strong wash of very dark chocolate brown; sides grayer with less brown; under surface grayish plumbeous, the hairs slightly tipped with pale buff or whitish (in different speci- mens). Muzzle plumbeous black, extending laterally into the cheek pouches ; chin and middle of throat pure white ; the usual blackish aural area, extending posteriorly as a sharply defined black streak ; feet whitish ; basal two-thirds of _ tail blackish, passing into clear white at the tip. Measurements.—Total length, 293 mm.; tail, 64; hind foot, 30. (Average - of two adult specimens, male and female, measured by the collector before k LAS . .) Skull.—The skull (P1. I, Figs. 10 and 11) is of about the size and general form of the skull of 7. 4udbivorus, except that the interorbital portion is much broader, < and the rostral portion much stouter. The interparietal is large, subtriangular, and the nasals and intermaxillaries terminate posteriorly on the same line. A large full-grown skull (No. 4120, ¢ ad.) measures as follows: Total i length, 40 mm.; basilar length, 37; greatest breadth, 23; least interorbital breadth, 6; length of nasals, 15; interparietal, breadth transversely, 7, anteroposteriorly, 6. Type, No. $44, 4 ad., Florida, La Plata Co., Colorado (altitude 7200 feet), June 25, 1892, Charles P. Rowley, collector. This species, in its dark chocolate brown color, and in the posterior termination of the nasals and intermaxillaries on the same line, and in the large size and subtriangular form of the interparietal, is very distinct from any other known to me. It 52 Bulletin American Museum of Natural History. |Vol. V, certainly needs no comparison with any of the species whose habitats immediately adjoin its own. Thomomys fossor is based on five specimens, two old adults and three nearly adult, collected at Florida, La Plata Co., Colorado (altitude 7200 feet), June 21-26, 1892, by Mr. Charles P. Rowley. - Thomomys toltecus, sp. nov. Thomomys umbrinus ALLEN, Bull. Am. Mus., V., p. 28, March, 1893. Above grayish pale rufescent brown, the middle of the back strongly varied with blackish ; below pale grayish buff. Feet and tail like the lower surface ; tail scantily haired ; nose and sides of face blackish ; chin and throat nearly concolor with the lower surface ; inner edge of cheek-pouches broadly pure white. Measurements (approximate from unfilled skins).—Total length, 230 mm. ; tail vertebrze, 60; hind foot, 27; middle claw of fore foot, 12. Skull.—(Plate I, Fig. 13.) Total length, 43; basilar length, 40; greatest zygomatic breadth, 27; least interorbital breadth, 7; length of nasals, 14. Type, No. 8449, Juarez, northern Chihauhau ; Lumholtz Collection, ea ‘Dz Meed, collector. This species is based on six specimens, collected at the Mormon settlement of Juarez, northern Chihuahua (not Sonora as first stated, anfea, p. 28). They are unfilled, much shrunken skins, with the skulls inside, a part of which have been removed for study, but they prove to be more or less defective, from muti- lation of the occipital portion. The best one is that figured in Plate I (Fig. 13). The skulls are heavily ossified, and indicate an animal of about the size of 7. do¢te@. The coloration above is a peculiar pale grayish brown, lighter on the sides and nearly black along the median line of the back. The upper incisors have a slight sulcus at the inner margin of their anterior face. T. toltecus needs no comparison with 7. /u/vus, its nearest geographical ally, which it exceeds greatly in size, and from ‘which it differs widely in coloration, and radically in cranial characters. The specimens above described were at first (1. c.) referred to Thomomys umbrinus, as defined by Baird, but subsequent study of the group (as detailed below), has shown that at least a portion of Soe a ee Cl aa ts ete 4 pM Nata ke Ni i ate 1893.] Allen, New Species of Thomomys. 53 Baird’s specimens thus indentified by him were really 7. fudous ; and also that the 7. umérinus of Richardson is probably hope- lessly unidentifiable, and thus must be ignored. Il.—QUESTIONS OF NOMENCLATURE. As is well known, the genus Z/omomys has an unfortunate history, as regards especially the type localities of the six species named by Richardson during the years 1828 to 1839, very few of them being definitely known to even Richardson himself. This, together with the faulty descriptions and lack of proper figures, laid the foundation for endless complications of nomenclature and doubt as to the real nature of Richardson’s species. Of the twelve names given to members of this group prior to 1885, six were contributed by Richardson, one by Schinz (who simply re- named arbitrarily one of Richardson’s species), one by Eydoux and Gervais, one by Woodhouse, one by Wied, one by Baird, and one by Coues. Two of Richardson’s species, however, were simultaneously published by Bachman under Richardson’s manu- script names. As shown by Dr. Coues, in his review of the group in 1875, “the literature of the whole subject, so far as original work in determination of species is concerned, focuses only in _ two authors—Richardson, 1829, and Baird, 1857 ;” to which of course must now be added a third—Coues, 1875. Various com- pilers had, in the time between Richardson and Baird, gone over the ground, without of course contributing anything of im- portance to the subject. In 1857 the late Professor Baird (Mam. N. Amer., pp. 388-404) recognized eight species of Z/omomys, as follows : “1. Thomomys bulbivorus——Coast of California, from Tejon Pass to some distance north of San Francisco. “2. Thomomys laticeps.—Coast of northern California (Hum- boldt Bay). “3. Thomomys douglassii—Lower valley of the Columbia River, and Puget Sound. “4. 2? Thomomys borealis—Upper valleys of the Columbia, towards Rocky Mountains; probably at higher elevations than T. douglassit. 54 Bulletin American Museum of Natural pci Bhi: Vv, “5. Thomomys rufescens.—Upper Missouri and Saskatchewan. “6. Thomomys talpoides—Shores of Hudson’s Bay. “4. Thomomys umbrinus.—Western ‘Texas and New Mexico, along eastern slope of Rocky Mountains, and along the mountains into Sonora. “8. Thomomys fulvus.—V alley of the Colorado and tributaries, from the San Francisco Mountains to Fort Yuma, and across to San Diego.” “Of these,” he adds, ‘I am inclined to believe that 7omomys borealis may hereafter be referred either to Z. douglassit or to 7. rufescens. What other combinations may be required can only be ascertained hereafter.” Dr. Coues, in 1875 (Powell’s Explor. of the Colorado River, 1875, pp. 243-265), reduced the preceding list to one species with three subspecies, and described an additional species, presenting the following tabular combination (I. C., p. 247) : Sw AONE n sn BAIRD, 1857. COUES, 187s. Thomomys bulbivorus. ) ) 8 2 A Thomomys laticeps.. Pacific coast region. . BULBIVORUS.. be © Thomomys dune S 3 ss Thomomys ? borealis... q gs j Thomomys rufescens .. 7 Northeren Interior . . TALPOIDES... { © © si Thomomys talpoides.. 33 eg Thomomys umbrinus.. \ Southern Interior and . 3 dicta fulvus..... Lower California. . epiesagitt ets j 2g Within recent years Dr. Merriam has revived (N. Am. Fauna, No. 3, 1890, p. 71) as a full species the Zhomomys fulvus of Woodhouse, and described as new Zhomomys perpallidus (Science, VIII, p. 588, Dec. 24, 1886), from the Colorado Desert, and Thomomys clusius fuscus (N. Am. Fauna, No. 5, 1891, p. 69), from the mountains of central Idaho, apparently with good reason. From the material now in hand it is evident that the group as a whole needs careful revision, as regards both the nomenclature and the number and the status of the forms. While it is not pro- posed to attempt such a revision in the present connection, I venture to offer a few comments on the general subject. Richardson, in the years 1828 and 1829, described four species referable to the genus Zhomomys, namely, (1) Cricetus talpotdes, 1893.] Allen, New Species of Thomomys. 55 (2) Geomys douglasti (not “ douglassii,” as usually written, (3) Geomys umbrinus, (4) Diplostoma ? bulbivorum. The first (Cricetus talpoides) was based on a skin (apparently without skull) “from Hudson’s Bay” (Zoél. Jour. III, 1828, p. 118), “but it was not accompanied by any notice of its precise habitat,” though Richardson was “inclined to identify it with a small animal inhabiting the banks of the Saskatchewan” (Faun. Bor.-Am., I, p.204). Coues in 1875 identified Richardson’s animal, satisfactorily to himself, with the Saskatchewan species ; and in view of what is at present known of the distribution of the genus in the region north of the United States, the Saskatchewan region may be assumed as the habitat of 7. ¢alpoides.’ The second (Geomys douglasii) was based on a skin and skull (an old female) obtained, “by Mr. Douglas, near the mouth of the Columbia” (F. B.-A., I, p. 200, pl. xviii c, fig. 1-6, skull). It is added, “ These little sand rats are numerous in the neighbor- hood of Fort Vancouver,” situated on the north side of the Columbia River, opposite the mouth of the Willamette, about half-way between the Cascade Mountains and the Pacific Coast. Hence the vicinity of Portland, Oregon, may be taken as the type locality of 7. douglasit. The figures of the skull are un- fortunately too crude to afford decisive characters; yet from these and from the account of the external characters I have little hesitation in accepting Baird’s identification of the species, and of refering to it specimens from Fort Steilacoom and north- ward into British Columbia. (See Plate I, Fig. 1, for an outline drawing of a skull from Ducks, B. C.) The third (Geomys umbrinus) was based on a specimen (a skin with apparently the skull in place) “from Cadadaguios, a town in _ the southwestern part of Louisiana” (F. B.-A., I, p. 202)—at pres- ent,and for many years past, an unknown locality. As Dr. Coues has: suggested, “more likely Texas,” the probability of this, he adds, being “ heightened by the Spanish appearance of the name, as if a corruption of Cuidad de Aguas, City of Waters” (I. c., p. 261). Baird referred to it specimens from southern New Mexico and Sonora. Of what Baird’s series as a whole may have con- enya 1 Very strangely, Richardson in ae gave the habitat of his G. talfoides as ** Florida,’ and eB the Saskatchewan animal G. dorea/is. C/. Rep. Brit. Ass. Adv. Sci., 1836 (1837) p. 156. 56 Bulletin American Museum of Natural History. [Vol. V, sisted I cannot at present state, but two of them (No. 45, Sand Creek, on Cimarron River, N. Mex., and No. 74%, Santa Cruz, Sonora), are unquestionably referable to 7. fulvus (Woodh.). Before seeing these specimens I had referred to 7. umbrinus (see antea, pp. 28 and 52) a series of specimens from Juarez, northern Chihuahua, representing a species very different from 7. fulvus. (See outline figure of skull, Plate I; Fig 13, in comparison with Fig. 5 of same plate, representing skull of Z. fulvus.) In the absence of a definite locality, and owing to the difficulty of recognizing species in this group from a description of merely the external characters, it would seem better to allow the name umbrinus to lapse as undeterminable. The fourth (Diplosioma ? bulbivorum) was based on the skin of | a “Camas-rat,” from the “banks of the Columbia,” an animal said to be very common on the plains of the Multnomah River” (F. B.-A., I, p. 206, pl. xviilid, wrongly lettered ‘“ Diplostoma douglasit”’). The large size of this animal, as shown by Richard- son’s measurements, caused it to prove a stumbling block to — Prof. Baird, who assumed that the specimen must have been greatly overstuffed, and that the locality was really somewhere in California. He therefore adopted this name for the “California Gopher,” named by Eydoux and Gervais, in 1836, Oryetomys (Saccophorus) botte, and this determination was accepted by Coues and generally adopted by subsequent writers. It turns out, however, that neither Baird nor Coues ever saw a specimen of true 7. dulbivorus, which has strangely escaped collectors till a recent date, and proves to be much the largest species of the genus thus far known, fully equaling in size large specimens of Geomys bursarius (see Pl. I, Fig. 14). The discovery of this long lost species is due entirely to my friend, Mr. Gerrit S. Miller, Jr., of Cambridge, Mass., who, in response to my request for specimens of Zhomomys from the lower Columbia River region has kindly transmitted for examination two fine adult specimens (male and female), collected at Beaverton, Oregon, in May, 1890, identified by him as the true Diplostoma bulbiverum of Richardson, In order to give him full credit for this important discovery I re- quested him to furnish me with something for publication on the subject. He has accordingly done me the great favor to forward 1893] Allen, New Species of Thomomys. 57 the following extracts from an unpublished paper of his, which I take great pleasure in here introducing : “Three examples of a Zhomomys collected at Beaverton, Washington Co., Oregon, in the spring of 1890, by Mr. A. W. Anthony, differ greatly from the California animal commonly called Thomomys bulbiverus (Rich.). The Oregon specimens are larger and much darker colored than any California examples that I have seen; they differ also in the extent of white markings _ about the mouth and anus, and in certain cranial characters. Most noticeable of the latter is the peculiar form of the ptery- goyds, which are larger and strongly concave internally, with _ hamulars converging at the tips, thus very different from the form usually found in the genus. “ Richardson (F. B.-A., I, 1829, p. 206) based his ‘Diplostoma ? bulbivorum’ on a specimen said to have come from the Columbia River, which circumstance, in connection with the minute de- scription given, leaves no room for doubt that the Anthony _ specimens represent this long lost species. . . . The first name based on an animal from California is the Oryctomys (Saccophorus) botte of Eydoux and Gervais (Mag. de Zool. VI, 1836, p. 23, pl. xxi) .--.The specific name Joffe will, as.first determined by Baird (Proc. Acad. Nat. Sci. Phila, 1855, p. 335), have to stand for the _ animal later identified by this author and by subsequent writers in general, with Richardson’s du/biverus.” (Gerrit S. Miller, Jr., MS.) As already intimated, I agree emphatically with Mr. Miller’s above-given determinations. The Anthony specimens are. per- haps a little darker (dusky, almost blackish, with a strong tinge _of chestnut) than Richardson’s description would lead one to expect ; but the agreement in all other particulars is so complete djhat, taking into account the color variability of the group in general, there seems to be no room for reasonable doubt in the case; and that the species which has so long been recognized as T. bulbivorus will have to pass in future under the hitherto little known name Jéoftz, based on specimens from the vicinity of Monterey, Cal. This completes our survey of the first batch of Richardson's species. In 1837 he mentioned a “Geomys borealis Rich., sp. nov.” (Rep. Brit. Assoc. for 1836, V, 1837, p. 156) as inhabiting “the 58 Bulletin American Museum of Natural History. (Vol. V, plains of the Saskatchewan.”’ Geomys borealis Rich. has generally been considered to have been a nomen nudum except as de- scribed by Bachman in 1839. This, however, seems not to have been strictly the case, as Dr. Richardson further referred to it casually in the Zodlogy of Beechey’s Voyage (Zoélogy of the Voyage of the Blossom, 1839, p. 12) under the head of Geomys townsendit, where he says: “ Townsendii differs [from G. Doug- Jasii | in having the wood-brown colored back of doreadis, and is distinguished from the latter by its longer tail. Total length of head and body of G. Townsendii, 7% inches, of tail, 234 inches. An individual of G. borealis of equal size of body, has the tail a very little exceeding an inch in length, and just equal to that of a young specimen of Zowmsendii, whose head and body measures only 5% inches.’’ These remarks relate, as Richardson states, to “specimens of two kinds of sand-rat taken by Mr. Townsend on the plains of Columbia,” which, he says, “Dr. Bachman kindly submitted to my [his] inspection.”” Nothing, however, is here said about the habitat of G. dorea/is ; and the natural infer- ence is that “the two kinds of sand-rat taken by Mr. Townsend on the plains of the Columbia” were his G. douglasii and G. townsendit, In the same year (1839) Dr. Bachman published descriptions of two species of Geomys based on specimens obtained by Townsend (the same specimens above referred to in the quota- tion from Dr. Richardson), under “ manuscript names” given them sometime previously by Richardson, namely, Geomys borealis and Geomys townsendit (Journ, Acad, Nat. Sci. Phila., VIII, 1839, pp. 103 and 105). Bachman’s Geomys borealis was based on two Townsend specimens “ procured on the Columbia River,” one of which, says Dr. Bachman, “I fined identical with one which had been procured by Mr. Douglass, and which was in the possession of Dr. Richardson.” As shown by the remarks of Dr. Richard- son under Geomys townsendit, a part of which have been quoted above (l. c.), Dr. Bachman had submitted these specimens to Richardson, who, as above stated, referred one of them to his G. douglasti, for he says: “‘ One, the G. dougdasit, has a rusty-brown colored fur above, hair brown on the abdomen, and blackish head. Tail, feet and pouches, white. ‘Townsendii differs....” ete, 1893.] Allen, New Species of Thomomys. 59 The inference is that Richardson identified one of these speci- mens as G. douglasii and the others as G. townsendit. The G. douglasit specimen is certainly one of the two specimens on which Bachman based his G. dorea/is, as will appear more fully later when we come to consider Bachman’s types. The third Town- send specimen formed the basis of Bachman’s “‘ Geomys town- sendii (Richardson’s Manuscripts),” respecting which he says : “Tam obliged to confess that I should not have ventured to pub- lish this species as distinct from the preceding on my own responsibility ;"" but he modestly defers to “the discriminating eye of Dr. Richardson,” who was then preparing a monograph (which appears never to have been published) “of this perplex- ing genus.” “As the species, however,” he continues, “will be given under the above name, I have found it necessary to indi- cate it here.” Later, however, in Audubon and Bachman’s “Quadrupeds of North America’ (III, 1853, p. 198, pl. exlii), “ Geomys townsendiit Rich.” is synonymized under “ Pseudostoma borealis.” The same disposition of Geomys townsendit was also made by Baird in 1857 (Mam. N. Am., p. 396), and practically also by Le Conte in 1852, after an examination of the Townsend specimens. _ Fortunately these historic specimens are still extant, and through the kind intervention of Mr. Witmer Stone, Curator of Birds and Mammals at the Philadelphia Academy of Natural Sciences, and the courtesy of the Council of the Society, they have been forwarded to me for examination. They each béar two labels, one of which is of recent origin, the other of very early date (at least prior to 1852, as will be shown later). The specimens have been mounted, and were for many years on exhi- tion, but not recently, as they were later dismounted and placed in drawers. They have unquestionably faded somewhat from exposure to light, but still can be distinguished on comparison with Bachman’s descriptions of them published half a century ago. The skulls are still in the skins and thus are unavailable for examination. The earlier (original ?) set of labels reads as follows, the numbers, however, being taken from the newer set : [146.] “ Pseudostoma Townsendit (Rich.). Rocky Mts. J. K. Townsend.” 60 Bulletin American Museum of Natural History. (Vol. V, [147.| “ Pseudostoma Richardsonit. Rocky Mts. J. K. Town- send.” The name “ Richardsonit” has been cancelled and the name “ Zownsendii” written below in pencil in what appears to be Prof. Baird’s handwriting. Apparently ‘‘ Richardsonii” was a dapsus penne for Townsendii.’ ie [144.] ‘‘ Pseudostoma borealis. Columbia River. J. K. Town- send.” (This specimen is now without its tail, which has appar- ently become quite recently detached.) ; This last is a small specimen, less than half the size of the others, and yet does not show any special marks of immaturity. It has a “‘ deep yellow wash” over the dorsal surface, and is thus evidently “the young specimen ” in which “‘ the back had a deep yellow wash,’’ mentioned by Bachman under Geomys borealis (I. c., p. 104). It is also beyond doubt the specimen referred to by Richardson (as cited above) to his Geomys douglasit. A careful comparison of the other specimens with Bachman’s paper shows that No. 147 is the type of his G. éownsendiz, and that No. 146 is the type of his G. borealis, Although No. 147 is rather darker, or more dingy gray, and less washed with yellowish than No. 146, there is nothing to suggest that they are not conspecific, in accordance with the decisions of Bachman, Le Conte, and Baird. Now a word as to questions of synonymy and type localities involved in the case of Geomys borealis Rich. versus Geomys borealis Bach. The names are practically of even date, as we must accept G. dorealis Rich. at 1839 instead of 1837, when it was first named but not described. The only clue to the type locality of G. borealis Rich. is that given in his first reference to the species, where it is stated that it “inhabits the plains of the Saskatchewan ” (Rep. Br. Ass. Adv. Sci. for 1836, p.156). There- fore until it is shown that two species of Z/omomys inhabit the Saskatchewan region, one of which is a short-tailed animal (tail an inch long with a head and body of 7™% inches), agreeing with Richardson’s later reference to his G. doreadis, this name may be 1 That these early labels were written many years ago is evident from the fact that in a paper on the genus Geomeys, pubaenes in 1852 Oy Dr. John L. Le Conte (Proc, Acad. Nat, Sci. Phila., 1852, p. 161), Dr. Le Conte says: ‘* There is a third specimen in the Museum of the Academy labeled ‘ Pseudostoma Richardsonii, Columbia River, J, K. Townsend,’ which only differs,...’’ etc., the reference being obviously to this specimen. 1893. ] Allen, New Species of Thomomys. 61 dismissed as a synonym of Zhomomys talpoides. In fact, it seems evident that Richardson here merely renamed the Saskatchewan animal which he had previously referred to his “Geomys? talpoides,” based on a specimen received from “ Mr. Leadbeater, who obtained it from Hudson’s Bay” (F. B.-A., I, p. 204); at the same time, for some unexplained reason, changing the habitat of sa/poides from “Hudson’s Bay” to “ Florida.”’' Bachman’s Geomys borealis was based on two specimens, a large and a small one, the first from the “ Rocky Mountains,” the other from the “‘ Columbia River,” taking the localities as entered on labels still attached to them and written at least prior to 1852. _ The smaller specimen is evidently referable to 7. douglasii, as determined long since by Richardson, who may be presumed to haye known his own species. The larger one, on which the de- scription is based, came presumably from near Bridger’s Pass in the Rocky Mountains. It is not therefore identical with G. borealis of Richardson, though so supposed by Bachman. The name is therefore practically preoccupied and must fall; but as Bachman’s G. townsendii, which is also Richardson's G. townsendii, was based on another specimen of the same species, as admitted by Bachman and later claimed by Le Conte and Baird, from an examination of the same specimens, the name Zhomomys town- sendit (Rich.) may stand for the large, rather pale form of Thomomys, known to occur in the Bridger country in common with the smaller 7. c/usius. Among the specimens kindly loaned me by Mr. True from the National Museum is a specimen (No. 43485, labeled Zhomomys clusius) from Fort D. A. Russell, Wyoming, collected in June, 1886, which so closely resembles the larger Townsend specimens that it seems unquestionably referable to the same species. This would seem to support the locality, namely, “ Rocky Mountains,” given on the labels of the larger Townsend specimens, and lead to the inference that they were collected somewhere in what is now southwestern Wyoming. SS alae als Richardson's Sella hs hc atolls 0 Gosteips s, in his celebrated * R: on North Douglactt and Enc is as follows: “* Geomys borealis in bits the plains of the tchewan, Poe ulbivorus those of the Columbia, ta/poides from Florida, umérinus from mondii from Texas, and mexicanus, as the name imports, from Mexico” gy Br. Ass. owate Sci. for 1836, “183). p- 156). 62 Bulletin American Museum of Natural History. [Vol. V, Prof. Baird doubtfully referred a specimen from Canoe Creek, Cal. (No. 4382), to Zhomomys borealis. Only the skull is now extant, which is before me. It is that of a quite young animal, and I have little doubt is referable to 7. cownsendii, as Baird’s account of the external characters favors this reference. The skull shows that it is not my 7. monticolus from the mountains of Central California. Through the kindness of Mr. True I have also before me the type of Zhomomys clusius Coues (No, 3051, skin with the skull inside), from Bridger’s Pass, collected July 28, 1857. As stated by Dr. Coues it is a female, which from the appearance of the teats may have suckled young, and hence is to be regarded as a full-grown animal, though so very small. It is in thin, worn pelage, with patches of the newer coat appearing along the median line of the back, especially anteriorly. I am also indebted to Dr. Merriam for a specimen (No. 33482) he has identified as 7homomys clustus (N. Am, Fauna, No. 5, 1891, p. 69), from Birch Creek, Idaho, and also for others from Bridger’s Pass. ‘They differ a little in color from the type of c/usius, and also among themselves, even irrespective of season. The skull of the type of clusius is unfortunately not available for examination. In 1839 (a memorable year in the history of the genus 7omomys), Prince Maximilian zu Wied described his Thomomys rufescens, gen. et spec. nov. What may be considered as the type specimen is still extant in this Museum (No. 637), bearing the following on the original label: “Zhomomys rufescens Wied, Mas. Missouri. Machtohpka indigen.”’ The exact locality is not indicated. In his original account of the species he says: “ Diese Wiihlmaus ist zalreich in den Prairies des oberen Missouri bis zu den Rocky- Mountains; ich kann aber nicht sagen, wie weit sie siidlich und nordlich verbreitet ist’? (Nov. Act. Acad. Czs.-Leop., XIX, pt. i, 1839, p. 382). After over fifty years of exposure as a mounted specimen the color has evidently greatly changed, it in fact closely resembling that of the type of Geomys townsendit Bach. (No. 146, Coll. Acad, Nat. Sci. Phila.) ! Both have the same faded yellowish gray tint, with the dorsal region strongly washed with yellowish brown, quite unlike the color of unfaded Upper Missouri speci- mens of Zhomomys. It has, however, the heavy claws of 7. 1893.] Allen, New Species of Thomomys. 63 talpoides as distinguished from the thinner smaller claws of the Townsend specimens. The original description calls for an animal not unlike the specimens collected by Dr. Coues (and now before me) at Pembina, Dakota, namely, with the upper parts uniform gray-brown, somewhat mixed with reddish brown and dark gray brown. The dark tint of the gray brown has dis- appeared, leaving only the reddish brown, which has faded to rather bright yellowish brown. Whether 7. rufescens is separable, even as a subspecies, from true /fa/poides of the Saskatchewan region I am unable at present to even consider, owing to lack of material. The type of Prof. Baird’s Thomomys /aticeps, from Humboldt Bay (No. #23%,), of which I am able to examine both skin and skull, is evidently closely related to 7. dotte, and hence has nothing to do with true 7. dudbiverus. The skull indicates a very old individual ; it is somewhat broken, but enough remains to show the essential characters. It differs from 7. dotte (Baird’s T. bulbivorus) in the much greater breadth and shortness of the rostral portion of the skull, resulting in very short and very broad nasal bones, as pointed out by Baird. I find no skull very, nearly approaching it in a large series from Marin Co., California, and from southern California. T. laticeps also differs from 4e¢fz in coloration, as well stated by Baird. For the present it seems proper to recognize 7. laticeps as a full species, although the comparison of further material may show that it intergrades with 7. Joffe, as seems not improbable. I refer to it also a series of five specimens from. Fort Crook, Cal., collected after the publication of Prof. Baird’s ‘ Mammals of North America,’ as they agree essentially in cranial characters and in coloration with the type of 7. daticeps. Thomomys clusius fuscus Merriam is apparently more closely related to 7. doug/asti than to 7. c/usius, the points through which it differs from c/usius—darker coloration, larger size, and thicker, stronger claws—being in the direction of doug/asit. Judging from Dr. Merriam’s description of c/usius and the two specimens he has kindly sent me for examination, it seems likely to prove a sub- species of doug/asii rather than of c/usius, and will be found thus entered in the subjoined list of the species of the genus. 64 Bulletin American Museum as Natural History. [Vol. V. One of the /uscus specimens seems quite indistinguishable from examples of douglasii from Fort Steilacoom, and Ducks, B. C, The cranial characters, and especially the relative size and the form of the interparietal bone, are very similar in douglasit, clusius and fuscus, and not very different in /a/poides. ‘The coloration and the size of the claws, however, appear to readily separate clusius from the others, which is also the smallest known form of the genus. III].—CRANIAL CHARACTERS. It is worthy of note that the cranial characters in the genus Thomomys are very important, even when the coloration and - external characters may fail to be satisfactorily diagnostic. Prof. Baird had very few skulls for examination at the time he wrote of the group in 1857, and appears to have made very little use of those he did have as a basis for classification. Dr. Coues must have been much better provided in this respect, but his distine- tions and generalizations appear to have been based entirely on external features, there being no reference to the skull in his long discussion of the relationships of the various species of previous authors. The importance of the cranial characters for the discrimination of the species of 7Zomomys is evident from a glance at the figures given in the accompanying plate (PI. I). The skull varies not only greatly in size and proportions in the different species, but in various important details of structure, as in the shape and relative size of the interparietal bone ; in the posterior extension of the nasals as compared with the inter- maxillaries ; and in the relative development of the muzzle in comparison with the rest of the skull. In fact, the case is quite parallel to that of the genera Dipedion, Perodipus and Perognathus, where, especially in the latter genus, Dr. Merriam has found such excellent cranial characters. It is hence evident that the group embraces not one or two species, as believed by Dr. Coues, or eight, as recognized by Prof. Baird, but a considerably larger number, easily characterized by cranial differences, and generally by more or less obvious external features, 4 ; 7 : , 4 _ 1893.] Allen, New Species of Thomomys. 65 The interparietal varies from nearly complete obsolescence, as in 7. dulbiverus (Fig. 14) to a large subquadrate bone, having a transverse breadth nearly equal to half of the intermastoid breadth of the skull, as in G. monticolus (Fig. 3) and G. doug/asii (Fig. 1). It may form a narrow triangle, with the base formed by the occip- ital border, and twice as long as broad, as in G. dotte (Fig. 8), or triangular with a broad base (the two extreme diameters about equal), as in 7. fossor (Fig. 10) ; or much smaller, but of the same general form, as in G. perpallidus (Fig. 12) ; or rather large and quadrate, as in 7. fu/vus (Fig. 5), or smaller and of the same form, as in 7. aureus (Fig. 6) and G. éoltecus (Fig. 13) ; with, of course, intermediate stages in other species, beween these leading types. The nasal bones may terminate far in advance of the nasal branch of the intermaxillaries, as in 7. dofte and 7. aureus, or on the same line with them, as in 7. fossor, or, in other species, at various intermediate points. They may be long and narrow, as in 7. monticolus and 7. douglasit, or short and narrow, as in 7. fulous, or short and broad, as in 7. /aticeps. ‘The form and position of the various foramina also vary more or less in different species, as do also the size and shape of the hamular processes of the pterygoids, and the outline of the crowns of the molar teeth. The slight sulcus at the inner edge of the anterior surface of the incisors may be nearly or quite obsolete or - well developed. The general size of the skull varies between wide extremes, as _ shown by a comparison of the skull of 7. /w/ous (Fig. 5) or 7. __elusius (Fig. 2) with the skull of 7. bulbivorus (Fig. 14). There is of course more or less individual variation in all of these features, and much variation in size due to age, even after the individual has reached the breeding age; but an effort has been made to eliminate this in selecting skulls for illustration by taking average specimens of the particular species in question. In several instances two skulls of the same species have been figured, for the purpose of showing variations in size, etc., due to age. [April, 1893.] 6 66 Bulletin American Museum of Natural History. [Vol.V, I1V.—SPpECIES AND SUBSPECIES OF THE Genus THOMOMYS. The views reached in the preparation of the present paper may be summarized somewhat as follows, as regards the status of forms and questions of nomenclature. The sequence of the species here adopted is not intended to represent their genetic relationships ; it is essentially that of Prof. Baird’s list, with interpolations. 1. Thomomys bulbivorus (Rich.). — Lower Columbia River. (Beaverton, Washington Co., Oregon, Mi//er ; Multnomah Co., — Oregon, Richardson.) ks, 2. Thomomys laticeps Baird.—Northern California. (Humboldt Bay, Baird ; Fort Crook, Shasta Co., /ei/ner.) =a 3. Thomomys botte (E. & G.).—Central and Southern California. (=T. bulbivorus Baird, nec Rich.) an 4. Thomomys townsendii (Rich.).— Southwestern Wyoming? (=Geomys townsendii Bach. and G. borealis Bach., nec Rich., ne latter in part only.) 5. Zhomomys monticolus A\len.—Mt. Tallac, El Dorado Ge Cal. . 6. Thomomys douglastii (Rich.).—Lower Columbia River, and thence northward into British Columbia. 7. Thomomys douglasit fuscus (Merriam).—Mountains of Cen- f tral Idaho, 8. Thomomys clusius Coues. — Southwestern Wyoming and Southern and Central Idaho. (Fort Bridger, Cowes ; Snake Plains, Merriam.) — 9. Thomomys talpoides (Rich.).—Saskatchewan region, south to upper Missouri region, (= Geomys borealis Rich.; =? 7. rufescens Wied.) 10. Thomomys fulvus (Woodh.).—Southern New Mexico and northern Sonora westward to southern California. (= 7. fulous Baird and 7. umbrinus Baird, the latter at least in part.) . 1893. | Allen, New Species of Thomomys. 67 11. Thomomys perpallidus Merriam. — Colorado Desert in _ southern California, and northeastward to the Painted Desert in _ Arizona (Merriam). hay. Ae Thomomys aureus Allen.—San Juan region of southeastern Utah. | 13. Thomomys fossor Allen.—La Plata Co., Colorado (upper _ San Juan region). - 14. Thomomys toltecus Allen.—Northern Chihuahua (Juarez). As already stated, 7. /aticeps may prove to be only a subspecies of 7. botte. On the other hand, 7. rufescens Wied may prove _ subspecifically separable from 7. ‘a/poides, as it is quite unlikely that the Z/omomys occurring as far south as Fort Randall, in - South Dakota, will prove strictly identical with the form found _ over the Saskatchewan Plains. Again, a form of Tomomys occurs : in Los Angeles, San Bernardino, and San .Diego Counties, Cali- fornia, which is quite different from either 7. 4ofte or 7. fulvus, _and apparently intermediate, in both cranial and external char- acters, between them. Also the form occurring in southeastern New Mexico and western Texas may not be identical with either _T. fossor, T. toltecus or T. fulvus. These are left as open ques- tions, to be solved by some future investigator who may chance to have the requisite material. 68 Bulletin American Museum of Natural History. [Vol. V.] EXPLANATION OF PLATE I. (All the Figures are natural size.) Fig. 1. Thomomys douglasii, No. $43%,' A. M. N. H., Ducks, B. C., Aug. 8, 1889. Fig. 2. Thomomys clusius, No. $929, U.S. Dept. Agl., 6 ad., Birch Creek, Idaho. Fig. 3. Zhomomys monticolus, No. 86, Leland Stanford University, 4 ad., Mt. Tallac, El] Dorado Co., Cal., Aug. 8, 1892. 7 %#e. Fig. 4. Thomomys monticolus, N 0. 59, Leland Stanford University, Mt. Tallac, Aug., 1892. (A younger specimen than No. 86.) Fig. 5. Zhomomys fulvus, No. 735, A. M. N. H., 9 ad., San Francisco Mountain, Arizona, July 22, 1887. Fig. 6. Thomomys aureus, No. $433, A. M. N. H., 2 ad., Bluff City, Utah, May 12, 1892. Ze. Fig. 7. Zhomomys aureus, No. $3373, A. M. N. H., ¢ ad. (very old), Bluff City, Utah, May 18, 1892. Fig. 8. Thomomys botte, #Ads, A. M. N. H., 6 ad., Nicasio, Cal., Feb. 26, 1889. Fig. 9. ZThomomys botte, No. #;, 2 juv., Nicasio, Cal., Feb. 26, 1889. Fig. 10. Zhomomys fossor, No. 43%, A. M. N. H., é ad., Florida, La Plata Co., Colorado, June 25, 1892. 7vpe. Fig. 11. ZThomomys fossor, No. 4448, 2 juv., Florida, La Plata Co., Colorado, June 22, 1892. Fig. 12. Zhomomys perpallidus, No. }§44, A. M. N. H., ¢ ad., Baregas Springs, Colorado Desert, California, Dec. 21, 1889. Fig. 13. 7homomys toltecus, No. $}9%, A. M. N. H., adult, Juarez, northern Chihuahua, Autumn, 1890. 7'vpe. Fig. 14. Thomomys bulbivorus, No. 3%§, Coll. Gerrit S. Miller, Jr., 4 ad., Beaverton, Oregon, May 12, 1890, : 1 The number above the line denotes the skull, and that below the line the skin of the same specimen, Vor. V., Pirate 1. ys douglasii. — clusius. nt monticolus. 5- Thomomys fulvus. 6, 7- se aureus. 8, 9. = bottz. th fossor. Article VI—LIST OF MAMMALS COLLECTED BY MR. CHARLES P. ROWLEY IN THE SAN JUAN REGION OF COLORADO, NEW MEXICO AND UTAH, WITH DESCRIPTIONS OF NEW SPECIES. By J. A. ALLEN. The collection of mammals forming the basis of the present paper was made in a triangular area at the junction of Colorado, New Mexico and Utah, in the valley of the San Juan River, by Mr. Charles P. Rowley, from March 12 to July 11, 1892, in connec- tion with the ‘Illustrated American’ Exploring Expedition. The thanks of the Museum are due in this connection to the proprie- tors of the ‘Illustrated American’ magazine for inviting the Museum to send a representative to accompany its expedition, and for facilities afforded Mr. Rowley in prosecuting his work. Mr. Rowley began work at Durango, Colorado (altitude, 6500 feet), March 12, and after spending a few days here moved south twenty miles to Aztec, New Mexico (altitude, 5900 feet), where he remained from March 17 to March 27. He reached La Plata, New Mexico (altitude, 6100 feet), twenty miles south of Aztec, March 30, and remained there two weeks. A few days (April 20-23) were spent at Nolan’s Ranch, Utah (altitude, 5025 feet), sixty miles northwest of La Plata. Riverview, fifty miles further down the river, was reached April 25, where ten days were passed, when the party moved forty miles further down the San Juan to Bluff City (altitude, 4500 feet), Utah; here collecting was prosecuted till May 26. The expedition then returned to Durango, Colorado, the starting point, and disbanded. Mr. Rowley, however, remained in the field for another month, select- ing Florida, La Plata Co., Colorado, eighteen miles east of Durango, and at an altitude of 7200 feet, as his field of opera- tions. Durango and Florida, in Colorado, and Aztec and La Plata, in New Mexico, are at about the lower border of the pine region in the mountains, while Nolan’s Ranch, Riverview and Bluff City, in Utah, are in the open arid cafion country, with a very different [69] 79 ~=—s- Bulletin American Museum of Natural History. |Vol.V, fauna from that met with at the points named in Colorado and New Mexico. In Utah the underlying rock is a light-colored soft sandstone, much cut by denudation into gorges, giving a whitish sandy soil, which supports the usual scanty semi-desert vegetation of cactuses, sage-brush and greasewood, and associated characteristic plants; in the more mountainous country to the eastward the soil is dark, and the vegetation is much more abundant, with pines and aspens on the higher slopes and cotton- woods and willows along the river bottoms. The Mice, Ground Squirrels and Pocket Gophers of the mountains are replaced in the open cafion country by not only very different species, but by species characterized by yellowish or bright tawny colors instead of the darker and more rufous tints of their representa- tives in the mountains to the eastward. The collection obtained by Mr. Rowley numbers nearly 4oo specimens, representing thirty species, while his note books refer definitely to a number of others not obtained. ‘The collection includes two new and very distinct species of Thomomys (see antea, pp. 49-52), two new species of Sz/omys, one of Arvicola, one of Retthrodontomys, and one of Zapus. The collection helps to determine the eastern limit of a number of Great Basin species, and the western limit of several of the mountain forms. 1. Lepus sylvaticus, subsp.?—Represented by a skull found at Aztec, N. Mex. Mr. Rowley states that ‘Cotton-tails’ were not abundant, and that he saw but one, and that only two ‘Jack Rabbits’ were seen. The latter do not occur in the mountains, but are found lower down in the open country to the westward. 2. Cariacus macrotis (Szy)—‘‘Common at Florida in spring ; pass lower down to winter’’ (Rowley, MS. notes). No specimens were obtained. He also states that a few Elk (Cervus canadensis) still occur about Florida, and that Mountain Sheep (Quvis canadensis Shaw) are still taken at long intervals. ‘“‘ None seen or killed this year so far (July, 1892).” 3. Erethizon epizanthus Zrandt.—La Plata, N. Mex., April 8, one specimen, Locally common, 1893. | Allen, Mammals of the San Juan Region: 71 4. Thomomys fossor <4//en. — Florida, La Plata Co., Colorado, 5 specimens, June 21-26. (See anfea, p. 51.) 5. Thomomys aureus 4//en.—Bluff City, Utah, 14 speci- mens, May 10-24. (See avtea, p. 49.) 6. Perognathus apache J/erriam—The series of 35 speci- mens of this species was all taken at Riverview, Utah, April 25 to May 4, where it was a common species, but apparently it was not met with at other points. The identification has been made by direct comparison of some of the specimens with Dr. Merriam’s type, which “came from the high mesa on the east side of the Painted Desert,” Arizona, about 125 miles southwest of Riverview. The series presents considerable variation in color, even among the adults, the ful- vous of the upper parts varying from pale to strong bright fulvous, generally much varied with black above the lateral line, but in one specimen bright fulvous predominates over the black, while generally the black greatly predominates over the fulvous. In very young specimens the fulvous is pale and limited mainly to the post-auricular patch, and the broad lateral line, the dorsal surface approaching an olivaceous gray finely and slightly varied with black. This coloration is seen in some nearly full-grown examples. 7. Perodipus ordii ( /V00dhouse)—Two specimens, male and female, Bluff City, Utah, May 16 and 17. Not common, and not met with elsewhere. 8. Zapus princeps, sp. nov. Of the size of Z. insignis Miller, but with the dental formula of Z. hudsonius ; quite different from either in coloration. Above with the middle of the dorsal region pale yellowish brown, profusely mixed with blackish, so that sometimes the blackish color, sometimes the pale yellowish brown. predominates ; sides of the body, forming a band on either side about equal to the dark dorsal band, yellowish brown slightly varied with blackish, except over a narrow lateral line adjoining the white of the lower parts which is clear strong yellowish brown ; lower parts pure white to the base of the hairs, varying in some specimens to strong ochraceous ; tail indistinctly bicolor— grayish white below and pale brown above, and very thinly haired ; hind feet grayish white above, like the lower surface of the tail ; ears narrowly edged with yellowish white. 72 Bulletin American Museum of Natural History. (Vol. V, Measurements.—Total length (from collector’s measurements taken before skinning), 238 mm. ; tail, 144 ; hind foot, 36 ; ear from crown (measured from skin), 12. (Average of 12 adult specimens, 7 4, 5 2.) Skull, total length, 24.5 ; basilar length, 20.3 ; greatest cranial breadth, 11.5 ; least interorbital breadth, 5 ; length of nasals, Io. Type, No. $348, 2 ad., Florida, La Plata Co., Colorado, June 27, 1892 ; coll. Charles P. Rowley. : This species about equals in size Z. imsignis, 10 specimens of which average in total length 240 mm.; tail, 148; hind foot, 31.5; ear, 17.5. Z. hudsonius averages in length about 2z1o, tail about 128, hind foot about 29.5, and ear about 14." Z. princeps differs from both these species in its much paler coloration, and from Z. hudsonius in its much larger size, and from Z. insignis in the presence of a small upper premolar. Although this tooth, both absolutely as well as relatively, is smaller than in Z. hud- sonius, it is uniformly present, while in Z. ézs¢gnuis, as shown by a large series of specimens, it is uniformly absent. ‘This latter species also differs from both the others in its white-tipped tail, and the very large size of the ears. Z. princeps is based on a series of 12 specimens, all adult, col- lected at Florida, La Plata Co., Colorado, June 22 to July 3, 1892, by Mr. Rowley. The series is very uniform in coloration ; some, however, are a little paler, or grayer in general effect, above than others, while one is strongly marked below with ochraceus, as is frequently the case in Z. hudsonius, in fresh pelage. As regards size, one (No. £434, 2 ad.) is much above the average, having a total length of 262 and the tail 168, the total length of the skull being 25.5 and the basilar length 21. 9. Arvicola (Mynomes) alticolus Merriam.—This species is represented by 11 specimens taken at Florida, La Plata Co., Colorado, June 17—July 4. They are nearly all adult, most of the six females being in breeding condition. Nine adults give the following averages, based on measure- ments taken from the fresh specimens by the collector: Total length, 170 mm.; tail, 60; hind foot, 23. ' Tam indebted to Mr, Gerrit S, Miller, Jr., of Cambridge, Mass., for the opportunity to examine not only the type of Z. éxsignzs but also a large series of this species from Essex County, N. Y., and also a large series of 2. Audsonéus from Massachusetts and New York, on which the preceding generalizations are mainly based. 1893.] Allen, Mammals of the San Juan Region. 73 ¢. texture of pelage and coloration these specimens agree with two examples of 4. alticolus, from San Francisco Mountain, : Arizona, kindly loaned me for examination by Dr. Merriam, . except in the color of the feet and tail, which in the Colorado specimens are slaty gray instead of brownish gray, as in the Arizona examples. The Colorado series apparently averages larger in general size, and may perhaps be subspecifically separable _ from A. alticolus. to. Arvicola (Mynomes) aztecus, sp. nov. Size large ; pelage very full and soft ; tail short ; skull very narrow. Above grayish brown with a tinge of pale buff ; fur blackish plumbeous beneath the surface, tipped with pale yellowish brown, and varied with longer, projecting, black-tipped hairs ; below grayish white, the fur plumbeous beneath the surface and tipped with white, giving a whitish gray effect. Feet dusky ; tail dusky brown above, dull white below. Measurements.—Total length (average of 5 specimens, from collector's measurements taken before skinning), 162 mm. ; tail, 42; hind foot, 18 ; ear from crown (measured from skin), 7. The largest measurements are as follows :° total length, 170 ; tail, 44; hind foot, 21.5 ; the smallest are respectively, 146, 35, 17.3. All the specimens are apparently fully adult. Skull, total length, 28 ; basilar length, 27 ; greatest zygomatic breadth, 16 ; least interorbital breadth, 4 ; nasals, 8.2. Type, No. $4i§, éad., Aztec, New Mexico, April 23, 1892 ; coll. Charles P. Rowley. This species is not only a member of the subgenus M/ynomes, but belongs to the rifarius section, the middle upper molar having . the postero-internal loop characteristic of the rifarius group. It 4 is, however, somewhat larger, very different in coloration, and presents slight but obvious differences is details of cranial structure. Arvicola astecus is based on two specimens from Aztec, New 4 Mexico, and three specimens from La Plata, New Mexico, collected 4 April 20-May 9, 1892. 1 also refer to it a large Asvicola from Estes Park, Colorado, which I have before been unable to allocate. I am unable to find that it differs in any particular from the specimens from New Mexico. The type and only positively identified specimen of Baird’s Arvicola modesta, from Sawatch Pass, Colorado, is a very young specimen in poor condition. An examination of a series of adult 74 ‘Bulletin American Museum = Natural thi [ Vol. V, secokee pee a eee —_ and young examples from the type locality will be necessary in order to determine its relationships to A. alticolus and A. aztecus. I am indebted to Mr. True for the opportunity of — what remains of the type of A. modesta. 11. Onychomys leucogaster, subsp.?—One specimen, La Plata, N. Mex., April 4. 12. Sitomys' sonoriensis (Ze Conte)—The Rowley Collec- tion contains 186 specimens of Sztomys, 130 of which I refer to what is commonly recognized as Sééomys sonoriensis. These speci- mens were collected as follows: Durango, New Mexico, March 12 and 13, 4 specimens, all adults; Aztec, N. M., March 17-27, 14 specimens, all adults; La Plata, N. M., March 30-April 13, 52 specimens, 44 of which are adults and 8 young; Nolan’s Ranch, Utah, April 20-22, 6 adults and 1 young; Riverview, Utah, April 25-May 4, 16 adults and 18 young; Florida, La Plata Co., Colorado, June 11—July 11, 9 adults and 10 young. Aside fram the young specimens, which show every phase of | immaturity from half-grown individuals to those which have nearly lost the ‘ blue’ coat characteristic of immaturity, the adults vary widely in color and considerably in size, even in series taken at practically the same date. Thus in the La Plata (N. Mex.) | series, the white-rimmed ears and the sharply-bicolored tail are about the only color features that are constant ; there is, however, usually a more or less prominent mixture of pure white hairs at the anterior base of the ears, but they are frequently absent. An average specimen may be described as pale grayish fulvous, much varied with black along the middle of the back, with less black and more strongly fulvous on the sides. In some specimens there is a conspicuous bright golden brown lateral line at the junction of the dark dorsal pelage with the pure white of the lower parts; while in other specimens, taken at the same place and on the same day, this bright fulvous lateral line is entirely wanting. In still other specimens a bright fulvous tint suffuses the whole dorsal surface, but is stronger and less obscured by blackish along the sides of the body than along the middle of the back. In other 'Dr. Merriam has recently shown that the name Vesperimus Coues, with which 1 pe to replace //esferomys (see this Bulletin, I11, PP sormandh is antedated by Séfomys Fitainger (Proc, Biol. Soc, Washington, VII, p. 27, April, 1892). 1893] Allen, Mammals of the San Juan Region. 75 cases the fulvous tint is almost entirely lacking, the whole upper surface being pale grayish buff varied with black, giving almost an olivaceous effect. In other cases the general effect is more blackish ; in others there is a pale chestnut or russet effect. Taking the series as a whole, it is evident that some of these effects are due to season—to wear and bleaching ; but there is still left a wide range of color variation which has no very evident relation to sex, season, or locality, though possibly dependent to some extent upon age. The collector’s measurements of 40 adults, taken in the field — before skinning, give the average total length (from the nose to end of the tail-hairs) as 6.15 in. (156 mm.), and of the tail alone (including hairs), as 2.65 in.(67 mm.). Few specimens fall below 6 inches in total length, and very few below 5.85, ranging from this up to 6.62, though rarely exceeding 6.50. The tail rarely falls below 2.40, and as rarely reaches 3.00, averaging 2.65. The average for head and body is about 90 mm., and for tail vertebrz alone, 63 mm. ‘ Two breeding females preserved in alcohol have the teats }—$ =6, 2 of which are pectoral and 4 inguinal. ‘This species was very common at the points visited in Colorado and New Mexico, in the partially wooded districts, but not found in the desert country about Bluff City. 13. Sitomys auripectus, sp. nov. About the size of Sitomys sonoriensis, with larger and more naked ears, much longer, more heavily clothed and less sharply bicolor tail, which is conspicu- ously tufted at the end ; general color above paler or more yellowish, and less varied with black. Above pale yellowish brown, or golden brown, slightly varied with blackish- tipped hairs along the middle of the dorsal region ; sides of the body, from the cheeks to the rump, clear strong golden brown, this color extending to the car- pal and tarsal joints ; below pure white, with a broad roundish pectoral patch of yellowish brown, like that of the flanks ; basal half of all the hairs plumbeous ; tail white below, pale brown above, darkening to blackish apically, thickly haired throughout, the hairs above very long towards the tip of the tail and terminating in a conspicuous brush or heavy pencil of blackish hairs, fully half an inch in length ; ears pale brown, with a narrow whitish rim, nearly naked, being very thinly covered with very short hairs on both surfaces ; a very narrow, indistinct blackish eye-ring. Proximal third of soles clothed, but less heavily than in 5S. 76 Bulletin American Museum of Natural History. [Vol. V, Measurements.—Total length (collector's measurements taken before skin- ning), 172 mm. ; tail, 93 ; hind foot, 22 ; ear from crown (taken from skin) 16, (Average of 10 specimens.) The skull is similar in size and general form to that of S. sonoriensis, and apparently affords no diagnostic characters. Total length, 24.5 ; basilar length, 21 ; greatest cranial breadth, 12.5 ; least interorbital breadth, 5 ; length of nasals, 10.5. Type, No. $444, 2 ad., Bluff City, Utah, May 14; coll. Charles P. Rowley. This species is represented by 13 adult and 5 immature speci- mens, collected at Bluff City, May 8-17. The adults are very uniform in size and coloration, except that the bright yellowish breast patch is indistinct in one of the specimens, apparently quite absent in two others, and strongly developed in eleven. The young specimens are similar to the young of S. sonortensis in corresponding stages except that they are somewhat grayer and paler. Two breeding females in alcohol have the teats §, all inguinal, This species is not closely related to any other previously de- scribed. Its large ears, bushy tail, yellow breast spot and pale golden brown color are distinctive features. It does not, how- ever, belong to the big-eared section of the genus, containing S. truet, S. megalotis, S. nasutus, etc. The proximal third or half of the soles is well clothed with short, silky, yellowish white hairs, the covered portion extending in some specimens as far as the first tubercle; in others it is less extended. 14. Sitomys rowleyi, sp. nov. Somewhat similar to S. auripectus in general characters, but much larger, less yellowish above, and without the pectoral spot ; soles wholly naked as in S. eremicus, Above dull pale grayish cinnamon brown, varied slightly with blackish-tipped hairs, passing into a band of yellowish cinnamon along the sides of the body ; beneath white, the basal portion of the hairs plumbeous ; tail indistinctly bicolor— dull pale brown above and whitish below—well haired and with a conspicuous terminal pencil. The earsare large, naked, and not obviously edged with white, Teats 3, inguinal. Measurements.—Total length (collector’s measurements taken before skin- ning), 201 mm. ; tail, 106 ; hind foot, 23; ear from crown (taken from skin), 15-18. (Average of 12 adults, 64, 62.) 1893.] Allen, Mammals of the San Juan Region. 77 Skuil, total length, 27 ; basilar length, 23 ; greatest cranial breadth, 13 ; least interorbital breadth, 11 ; length of nasals, 5.5. The skull is much larger than in either Sifomys sonoriensis or S. auripectus, and differs from them in slight details of structure. Type, No. $338, $ad., Nolan’s Ranch, Utah, April 20, 1892; coll. Charles P. Rowley. This species is based on a series of 25 specimens, of which 5 were collected at Nolan’s Ranch, April 20-21, and 20 at Bluff City, May 8-24. Of this number 18 are fully adult and present little variation. A full-grown young specimen is nearly uniform mouse gray above, with an indistinct narrow lateral line of yel- lowish brown. Very young specimens are grayish plumbeous, lighter and more silvery than young of corresponding ages of either S. sonoriensis or S. aurtpectus. None of the series shows any trace of the fulvous pectoral spot of S. auripectus. S. rowleyi is very distinct from any other member of the genus known to me. It has a superficial resemblance to S. auripectus, but it is a much larger animal and very differently colored, at all ages. It is less yellow above and wholly lacks the pectoral spot ; the tail and soles are rather less hairy. In their large naked ears, partly naked soles, and long tails both S. rowleyi and S. auripectus would seem to belong near S. eremicus, which they resemble in proportions, rather than with S. sonoriensis, but neither is in any way very closely allied to S. eremicus. Some years since a series of 14 mice was received at the Museum from Mr. W. E. D. Scott, collected in October, Novem- ber and December, 1885, in Pinal County, Arizona, which were provisionally referred to S. eremicus. They presented, however, a wide range of variation in color, hairiness of tails and soles, and in size, which rendered them very puzzling. A re-examination of the series in the light of present material shows that only ten of them are to be referred to S. eremicus, the other four being apparently referable to the present species, which thus has probably quite a range to the southward. Since the above was written the Museum has received a series of 12 specimens of Sitomys, collected at Bradshaw City, Arizona, 78 Bulletin American Museum of Natural History. |Vol. V, in January and February, 1890, by Mr. H. H. Keays, which are also referable to this species. This species is named for Mr. Charles P. Rowley, whose col- lection here under notice has proved so rich in new forms and other valuable material. 15. Sitomys truei (.S/ufe/dt). Hesperomys truet SHUFELDT, Proc. U. S. Nat. Mus. VIII, p. 407, pl. xxi, Sept. 1885. (Fort Wingate, N. Mex.) ? Hesperomys megalotis MERRIAM, N, Am, Fauna, No. 3, p. 64, pll. iii and iv, Sept. 11, 1890. (Black Tank, Little Colorado Desert, Arizona.) Eight specimens collected as follows: 2, Aztec, New Mexico, March 20; 6, La Plata, N. Mex., April 2-8. Aztec is only a few miles south of the northern boundary of New Mexico ; La Plata is about thirty miles south of Aztec, and both are near the Arizona line. Fort Wingate is about one hundred miles (probably a little less) south of La Plata, and about one hundred miles or so east of the type locality of /. megalotis Merriam, who refers to “specimens of the same or a closely-related form” from Moccasin Springs, Arizona, near the boundary line of Utah and Arizona. Through Dr. Merriam’s kindness I have two of his original specimens (Nat. Mus. Nos. $3223 and $4244) for comparison with the Rowley series, which I am unable to distinguish as in any way different. The Rowley series is from near the type locality of H. ¢rue?, and is practically identical with the type, with which, through the kindness of Mr. True, I have been able to compare them. Vesperimus nasutus Allen, from Estes Park, Colorado, is evi- dently nearly related to S. ¢rwez, as already pointed out (this Bulletin, III, p. 300). Hesperomys crinitus Merriam, from Shoshone Falls, Idaho, proves to be apparently the same as .S. wasutus, the latter name, however, having a few weeks priority, the two names being pub- lished nearly simultaneously. This shows that the big-eared truet group of Sitomys has a wide geographical range, although everywhere apparently affecting similar situations—cafions or rocky gorges. — 1893.] Allen, Mammals of the San Juan Region. 79 16. Reithrodontomys' megalotis (air). Reithrodon megalotis BairpD, Mam. N. Am. 1857, p. 451 ; Zodl. Mex. Bound. Sur., Mam. 1859, p. 43, pl. vii, fig. 4, feet and ear, pl. xxiv, fig. 4, skull. (Between Janos, Sonora, and San Luis Springs, N. Mex.) I refer provisionally 13 specimens to this species, taken as follows: La Plata, N. Mex., 7 specimens (including three in alcohol), March 30—April 11; Aztec, N. Mex., 2 specimens, March 19 and 20; Riverview, Utah, 1 specimen, April 25 ; Bluff City, Utah, 1 specimen, May 18. Through the kindness of Mr. True I have the skull of Baird’s type for comparison with the present series, and I am unable to perceive any differences other than smaller size. Unfortunately the skin of the type, Mr. True writes me, has been mislaid, and thus is not available in this connection. ‘The series of specimens mentioned above seems to agree closely with Baird’s descrip- tion of his &. mega/otis, so far as proportions and coloration is concerned, but the measurements taken by the collector from the fresh specimens considerably exceed those given by Baird. ‘The subjoined description was drawn up some time since, under the impression that 2. mega/otis would prove more different from the Rowley specimens that seems to be the case. As the type locality of 2. mega/otis is near Janos, not far from the boundary line between Sonora and New Mexico, some four hundred miles south of La Plata and Aztec, and in a zéologically quite different region, I have thought best to append the follow- ing, in view of the probability that the two forms will prove at least subspecifically separable. Reithrodontomys aztecus A//en MS. Color above almost exactly like that of an average fully adult house mouse (Mus musculus), but with the pelage softer and fuller, and rather more yellowish on the flanks ; below clear grayish white, the fur plumbeous at base and white apically ; tail indistinctly bicolor, pale brown above, grayish white below ; ears concolor with the general tint of the dorsal surface, very scantily haired exter- nally, nearly naked within. Feet dull whitish ; hind feet with the soles well clothed posteriorly, naked anteriorly. As pointed out by Dr. Merriam Xeithrodontomys Gi : (187) 3 antedates Ochetodon aa (ora) (C/. Merriam, Proc. Biol. Soc. Washington, VIL, p. 26( Poctnate); April, 1892.) 80 Bulletin American Museum of Natural History. [Vol.V, Measurements (average of 7 adults, from collector’s measurements taken before skinning).—Total length, 135 mm. ; tail, 65 ; hind foot, 18 ; ear from crown (average from skin), 12. Skull, total length, 21 ; basilar length, 19 ; greatest cranial breadth, 11 ; least interorbital breadth, 4 ; length of nasals, 8. Type, No. 4498, 6 ad., La Plata, N. Mex., April 11, 1892; coll. C, P. Rowley. From Dr. Coues’s scanty material he was led to assume (Mon. N. Am. Roden., 1877, pp. 125, 126) that “the ezthrodon megalotis is the same as O. humilis,” and on this account appar- ently gave the habitat of the latter as extending from the “ Gulf States.into Sonora.” ‘They prove, however, to be as unlike in both size and coloration as two congeneric species can well be expected to be; and I have seen no evidence that 2. Aumilis extends even into Texas. Norte on Reithrodontomys montanus (Bairp).—Through the kindness of Mr. True, I have the skin of the type specimen of Baird’s Retthrodon montanus; the skull, however, is at present unavailable for examination. Although probably not fully mature, it is evident that it represents a species quite unlike either 2. humilis of the East or 2. megalotis. Dr. Coues was led to suspect (Mon. N. Am. Roden., p. 130) that the specimen had been immersed in alcohol, and it certainly has that appearance, though not so stated by Baird. The underparts, described originally as ‘‘ dull whitish,” are now yellowish, as though stained either by alcohol or insect powder. ‘The specimen was taken on Capt. Beckwith’s Expedition, from what is now eastern Kansas up the Arkansas River and across the divide between the head- waters of the Arkansas and the Grand Rivers, and thence westward. ‘The locality given for the type of 2. montanus is simply “Rocky Mountains, Lat. 38°.” Evidently the type locality was not known, even to Baird, and may have been east of the Rocky Mountains. This seems not improbable from the fact that a species of Reithrodontomys, entirely different from either 2. humilis or R. megalotis, occurs in both Kansas and Colorado; it greatly resembles Baird’s &. montanus, as shown ae a eae ee ess Le ee ee ee eee rm 1893.| Allen, Mammals of the San Juan Region. 81 by actual comparison of specimens. In comparison with all of the other known species of the genus, the ears are small and thickly covered with short coarse hair, and the anterior third of the outer surface is occupied by a well-defined blackish spot, conspicuously in contrast with the rest of the outer surface of the ear, which is yellowish brown. This spot is less strongly marked in Baird’s type than in other specimens from both Kansas and Colorado, and is not mentioned in Baird’s descrip- tion. I have therefore no hesitation in recognizing Reithrodon- tomys montanus (Baird) as a well-marked, valid species, which will probably be found to range from the eastern base of the Rocky Mountains eastward to middle Kansas. 17. Neotoma mexicana Aaird—One specimen, La Plata, N. Mex., April 4. 18. Mus musculus Zinn.—Florida, La Plata Co., Col., 13 specimens, June 11—July r. 19. Castor canadensis Xuw//.—No specimens taken, but Mr. Rowley reports them (MS. notes) as occurring in numbers along the Florida, Animas, Mancos, and San Juan Rivers. 20. Arctomys flaviventer Aud. & Bachm.—An adult female, Florida, La Plata Co., Col., June 16, is provisionally referred to this species. It is, however, very unlike Sierra Nevada specimens commonly referred to this species. ‘Woodchucks scarce, the only one found was up near timber line. They keep very high up.” (Rowley, MS. notes.) 21. Cynomys gunnisoni Zaird—Two specimens, Cortez, Col., and Aztec, N. Mex. Also a weathered skull from Aztec. These were the only specimens seen, no villages being met with throughout the journey of nearly 400 miles. 22. Spermophilus grammurus (.Say).—The six specimens in the collection ali belong to one family, consisting of an adult male and female and four young, collected at Florida, La Plata Co., Col., June 25-29. No others were seen, and the species was unknown to the ranchmen of the region. [/une, 1893.] 6 82 Bulletin American Museum of Natural History. [Vol. V, 23. Tamias lateralis (.Say).—A series of 36 specimens from Florida, La Plata Co., Colorado, collected June 11 to July rr, including all sizes and‘conditions from quarter-grown young to adults, in pre- and post-breeding pelage. The pre-breeding pelage is shown by a female, taken while still nursing young, which is in faded, much worn coat, with no traces of the new coat. It is very pale throughout, in strong contrast with the freshly- molted examples, in which the whole upper parts are much darker—blackish, finely varied with rusty gray, especially ante- riorly ; the lateral stripes and sides of the belly are grayish white instead of yellowish white ; the sides of the shoulders are only slightly washed with yellowish instead of being deep reddish orange, resulting in a very different and strongly contrasting gen- eral effect. Others present a patchy condition, in which the new coat is more or less irregularly displacing the old. Most of the July specimens have fully acquired the new coat. The young in first pelage have a much thinner, softer, paler coat than the post- breeding adults. Very common about Florida, but less numerous than 7. guadrivitiatus. 24. Tamias leucurus cinnamomeus JMZerriam.—A series of 14 specimens from Bluff City, Utah, May 9-25. They are mostly in worn, patchy, transition pelage, and show both the pre- and post-breeding pelages. One has nearly completed the molt, and one is a quarter-grown young one. Compared with a series of true 7. Zeucurus from San Diego Co., Cal., the difference in color between the two forms is very striking, as pointed out by Dr. Merriam in his description of T. Ll. cinnamomeus. (Cf. N. Am. Fauna, No. 3, 1890, p. 52.) Reported as met with only in the open cafion country about Bluff City. 25. Tamias quadrivittatus gracilis A//en—Bluff City, Utah, 9 specimens, May 9-21. They are mostly in worn, transi- tion pelage, showing a mixture of both pre- and post-breeding coats, One has nearly completed the new coat. ek ee ee Nt oy teed le i a i | ih 8b ea on, seh) os 1893.] Allen, Mammais of the San Juan Region. 83 These specimens agree very closely with the San Pedro, N. Mex., series on which this very striking form was originally based (this Bull., III, pp. 99-101). 26. Tamias quadrivittatus (Szy)—A series of 49 speci- mens, collected at Florida, La Plata Co., Colorado, seem to be typically referable to true 7. guadrivittatus. It consists of both young and adults, the latter in molt. Very common in the pine belt about Florida, among rocks and in the ground, but readily took to trees when pursued. (Rowley, MS. notes.) 27. Sciurus aberti Woodhouse —One specimen, 9 ad., Florida, La Plata Co., Colorado, June 2:. Veryrare. This was the only specimen seen, and the species was not known to the residents of the region. 28. Antrozous pallidus (Ze Conte).—Two specimens, Bluff City, May 18 and 25. 29. Vesperus fuscus (Aeauvois)—Two specimens, Bluff City, Utah ; one specimen, Florida, La Plata Co., Col. 30. Vesperugo hesperus (7. 4A//en).—Three specimens, Riverview, Utah, May 25. 31. Vesperugo (Lasionycteris) noctivagans Ze Conte.— Two specimens, Florida, La Plata Co., Col., June 30. 32. Vespertilio lucifugus Ze Conte. — Three specimens, provisionally referred to this species, Bluff City, May 11 and 16. 33. Lutreola vison (Schreber).—One specimen, La Plata, N. Mex. ‘ Minks are quite plentiful on all the streams of this region, but I was only lucky enough to catch one, on the La Plata River” (Rowley, MS. notes). 34. Felis concolor Zinn.—“ Scarce about here (Florida) ; one was killed at the head of Florida Creek in February, 1892” (Rowley, MS. notes). 84 Bulletin American Museum of Natu In addition to the foregoing Mr. poor in Article VII—ACERATHERIUM TRIDACTYLUM FROM THE LOWER MIOCENE OF DAKOTA. By Henry FatrFiELD Osborn. Aceratherium tridactylum, sp. nov. General Characters.—1 §?, C$, P 4, M%. Digits, 3-3. Vertebre, D Io, L 5, S 3, C 21. Occiput elevated. Postglenoid and post-tympanic enclose auditory meatus inferiorly. Superior molars with strong ‘ antecrochet’ and ‘crochet’ feeble or absent. First upper premolar well developed. Incomplete cingulum upon inner face of true molars. Occiput high and narrow. The very thorough search of the Lower Miocene (White River) exposures of South Dakota by the Museum Expedition of 1892 has resulted in the discovery of a complete series of Aceratheria in an horizon which has hitherto yielded but two well-determined species. The smallest of the series was found immediately over- lying the ‘ Titanotherium Beds,’ and the largest in the ‘ Protoceras Beds,’ which mark the top of the White River formation in this locality. These forms will be figured and described in a forth- coming bulletin. The present paper is a preliminary description of the largest type, 4. tridactylum. The type of this new species is a complete skeleton in excellent preservation, which was discovered by Mr. Peterson of the Museum party, and has now been mounted for exhibition by Mr. Hermann. The only parts lacking are the left forelimb, a few of the ribs, and the sternal bones. All the other parts are complete, the vertebral column being perfect to the tip of the tail. The skeleton measures seven feet nine inches in length, and four feet in height to the top of the lumbar vertebral spines. There are nineteen dorsal, five lumbar and three sacral vertebre. The pelvis is long and rather slender, and the limbs are of an intermediate type, heavier than in A. occidentale and much longer than in the Upper Miocene 4. /fossiger. There are only three digits in the manus, hence the name /ridactylum, there being no trace of the fifth digit, which is so characteristic of the lower Miocene Rhinoceroses of America and Europe, with the possible exception of A. mite Cope. [85] 86 Bulletin American Museum of Natural History. (Vol. V.] The total length of the skull is 51 centimeters, while in 4. occidentale it measures 44. The occiput is high and rather narrow, whereas in A. occidentale it is low and broad; the upper line of the skull thus curves upwards, and the sagittal crest is considerably shortened. Another progressive feature is that the molars show, besides the strong ‘antecrochet,’ a beginning of the ‘crochet,’ which is wholly undeveloped in A. occidentale. The median upper incisors are much larger than the outer pair, and the lower canines are correspondingly enlarged. The first lower premolar (Px) is rudimentary or wanting. Another distinctive feature of the skull is the union of the postglenoid and post-tympanic processes to enclose the external auditory meatus inferiorly. The upper view of the skull, especially in the great elongation of the nasals, which overhang the premaxillaries, suggests a close affinity to A. megalodus' Cope of the Upper Miocene or Loup Fork ; the molars are in a similar stage of evolution ; the occiput of A. tridactylum is constricted below and spreads above, while that of A. megalodus is broad at the base and narrows regularly to the top ; a partial cingulum is present upon the inner side of the true molars, and is said to be wanting in A. megalodus ; the first upper premolar is well developed in A. ¢ridactylum, and is variable or wanting in A. megalodus. ‘These features are such as usually separate Lower from Upper Miocene types. 1 Pal. Bulletin, No. 14, Proc. Am. Phil. Soc., July, 1873. ee et ee i a a <9 : i ai el ey Se ee Article VIII—NOTES ON TRANSFORMATIONS OF SOME NORTH AMERICAN MOTHS. By Wittiam BEUTENMULLER. The following are a few notes on the earlier stages of some Lepidoptera, made by me during the summer of 1891, to which are added the descriptions of several cocoons from Mexico, which are in the Hy. Edwards Collection, and as far as I am aware have not yet been described. Chionobus semidea Say. fgg.—Received from Dr. S. H. Scudder. Laid about July 15. Larva emerged July 26. Oblong oval, with numerous longitudinal wavy ridges. On the top is a small nipple. The base is nearly smooth and is somewhat flattened. The egg becomes somewhat narrower towards the top, and is of a pale yellow color, assuming a slaty gray as the young larva within develops. Height, 1 mm. ; width, .75 mm. Young Larva.—Head dirty greenish white. Body above mouse colored. Last segment with a fork-like process. Underside dull greenish gray. Length, 2 mm. I did not succeed in rearing this insect beyond this stage. Apatelodes torrefacta 4. & S. £gg.—Smooth, lenticular, semitransluscent, shining, rounded in outline and very much flattened above and below. Width, 2 mm.; height,.5; mm. Laid June 24. Larva emerged July 5. Received from Miss Emily Morton. Young Larva.—Yellowish white, with long flossy, white hairs covering the body. Head white, with a black spot on the ante- rior part of each side. Length, 3mm. Moulted July 1o. After First Moult—tLittle difference from the previous stage, except that the underside is now somewhat greenish, and the hairs are distinctly longer, with a single black pencil or tuft on the eleventh segment. Length,7 mm. Moulted July 14, [87] 88 Bulletin American Museum of Natural History. [Vol. V, After Second Moult.—In this stage the hairs are considerably longer, clearer white and more flossy. Mouth parts pitchy black. Along the dorsum is now a faint black longitudinal stripe, and a few black hairs of the same color are on the second and third segments. Length,1z1 mm. Moulted July 18. After Third Moult.—The hairs are still longer than in the previous moult, and the black pencil on the eleventh segment more distinct. The hair on the three anterior segments are longer than those of the posterior segments. ‘The black dorsal line is also more distinct and is broken. ‘lhe underside of the body is semitransluscent, showing the greenish contents. Length, zo mm. Moulted July 23. After Fourth Moult.—The hairs in this stage are pure white and are directed backwards. On the dorsum of each of the second and third segments is a long black pencil, and one on the eleventh segment. Along the dorsum is a narrow black line as in the previous stage, and a bunch of short hairs of the same color on each segment, dorsally. The body color is now of a bluish-white, and the spiracles are black. Body on the underside with a short transverse black patch on each segment. Some individuals of the brood are now yellowish in color. Length, 30mm. Moulted July 27. After Fifth Moult.—Head dirty white. A row of rather large spots on each side of the body, one spot on each segment. The dorsal stripe is much broader and more prominent than in the previous moult, and the three dorsal pencils are mouse color instead of black, and are tipped with white at the extreme ends. The abdominal legs are black, with their extremities pinkish. The thoracic feet are also black. The hairs are all directed backwards, except those on the anterior segment, which are direct- ed forwards. Mouth parts pitchy black. The short tufts of black hairs along the dorsum are also present. When fully grown the body is creamy white or pale yellow, with the black spots along the sides and dorsum quite conspicuous. The hairs in the yellow- bodied larvee are pale yellow, and in the whitish-bodied ones the hairs are pure white. In some yellow-bodied larve which I found outdoors the hairs were bright sulphur yellow. When fully grown Sere Res ee 1893.] Beutenmiiller, Transformations of Moths. 89 the extremities of the abdominal legs are much redder than im- mediately after moulting. Length, about 45 mm. Entered the ground August 2,at 10 A.M. Pupated August 4, -at4 P.M. Emerged August 27, 28 and 29. My brood of larve were raised on Wild Cherry (Prunus sero- tina). It also feeds on Willow, Alder, Blackberry, Bayberry (Myrica cerifera), Azalea, Sassafras and Hazel. Sisyrosea inornata G. & &. Full-grown Larva.—Bright yellowish green ; the body much flattened at the sides, the segments there being ornamented with flattened processes armed with spines and looking like the anten- nz of a Bombyx. These spinuous processes are nine on each side. The head is quite hidden by the overlapping of the other segment. It is smooth, pitchy. The second segment is darker green than the rest of the body. The third and fourth have shorter spines on the sides, and these are edged with orange speckled with black. The dorsum is elevated into a double ridge, pale cream color. On the eighth and tenth segments is a small orange mark in form of a maltese cross. The ridges over the head are produced into a short spine, orange, flecked with black. The spiracles are pale yellow, and on each segment there are six small fovea, which on the sides are continued by pale green waved lines, those on the dorsum the smallest. Underside pale green. Length, about 15 mm.; width, ro mm. (including spines). Food-plants—Oak, Cherry, Hickory. ' Anisota stigma 444. & Sm. (var. or nov. sp.). Before Last Moult-—The ground color is jet black and shining, becoming greenish or tea colored as it is more advanced towards the last moult. The whole of the tubercular spots, as well as the spines and longer processes, are also jet black. The white irrora- tions, so well marked in 4. s/igma, is entirely wanting, and there are no marks on the obsolete, double, broken, subdorsal sordid white line. Length, 30 mm. Full-grown Larva —TVhe head is now brick red. The obsolete broken subdorsal line is a little more distinct, and is treble instead 99 Bulletin American Museum of Natural History. (Vol. V, of double. The body has lost its shiny appearance, and is now dull black. The irrorations are jet black, shiny, save that on each segment is a double row of tubercular irrorations, sordid white. There is a dull claret-stained ventral line, broken at the junction of each segment, and the interior surface of the abdominal legs is also stained with a claret shade. They are black outwardly, as are also the thoracic feet. The broken line on the underside is really reduced to three lozenge-shaped dashes on each segment. Laterally the larve are stained with red. Length, about 60 mm. I have been unable to rear this singular larva to maturity. A number of them were taken by me last season at Scarsdale, N. Y. The late Henry Edwards and S. L. Elliot were also acquainted with this larva, and likewise did not succeed in raising it. Mr. Edwards considered it the larva of a new species of Anisota. It is certainly very different from all other Amisofa larva found in the vicinity of New York City. Hyperip BETWEEN Actias luna Mater, anp Actias selene FEMALE. Lgg.—Received from Miss Emily Morton. Ovate, smooth, not shining, covered with a brown substance, much the same as that of A. duna, in fact I cannot see any difference. Young Larva.—Pinkish brown, with two rows of deep brown spots on each side, and one row on the dorsum, which are quite indistinct ; on the third segment the spots are largest and deeper in color. The spots along the sides are two in number on each segment, while in the subdorsal row there is only one spot on each segment. The juncture of the segments are greenish in color, as is also the head, which has two transverse, black bands. On each side of the body are three rows of tubercles, bearing a number of long spine-like hairs. The first segment is yellowish, and without spots. Underside of body wholly greenish. Length, 6mm, Moulted July 2. After First Moult.—The larve are now greenish in color, with the three rows of tubercles on each side yellow, tipped with red- dish orange ; the two pairs of dorsal tubercles on the third and fourth segments are decidedly larger than the rest, and are tipped 1893.] Beutenmiiller, Transformations of Moths. g! with black. The rows of spots are also less distinct than in the previous stage, and the head lacks the transverse bands, and is of the same color as the body, with a small black dot on the anterior part of each side. Each of the tubercles has a few, rather long, brown hairs. Underside greenish. Thoracic feet jet black. Abdominal and anal legs tipped with black. One individual of the brood is flesh colored, and has the extremities of the tubercles black, and the lateral row of spots more distinct than the two other rows. Length, 15 mm. Moulted July 6. After Second Moult.—The body is now bright green, with a narrow, paler green line below the spiracles, which are orange. The spots are absent in this stage, and the tubercles more promi- nent with a few black hairs, and tipped with orange. The anal plates are half brown and half black, and are narrowly bordered with green. Head pale green, mouth parts pitchy. Thoracic feet black. Abdominal legs green, with a black patch on the outer side of each. Underside wholly green. Length, 25 mm. Moulted July rr. After Third Moult—No difference from the previous stage, except in size, and in the tubercles being somewhat brighter in color. Length, 35 mm. Moulted July 15. After Fourth Moult—The head in some individuals is now purplish green instead of wholly green, as in the foregoing stage. The tubercles are also more prominent. Length, 40 mm. Moulted July 19. After Fifth Moult-—The head in this stage is pale chestnut brown, as are also the thoracic feet, with a yellow ring at their bases. The anterior edge of the first segment is yellow. The _ anal plates are brown with a yellow margin. The spiracles are large and orange in color. The abdominal legs have a black band on the outerside of each. The two rows of tubercles along the sides are smaller than those on the dorsal region, as is the case throughout all the previous stages. The segments are much swollen, and deeply incised at junctures. The yellow line below the spiracles runs from the beginning of the fourth segment to the end of the eleventh. The hairs on the yellow tubercles are 92 Bulletin American Museum of Natural History. |Vol. V, pale brown, while those on the row of tubercles below the spiracles are black. One example has the bases of the tubercles on the third and fourth segments blackish. Fully grown July 31. Length, 65 mm. Euchromia bella Guer. Cocoon.—Oval, bright lemon yellow in color; very thin and composed of finely woven silk, which is intermixed with the larval | hairs, also of lemon-yellow color. These hairs penetrate through the cocoon, thus giving it a decidedly wooly appearance. Length, 15 mm.; width, 8 mm. One example, collected by Mr. Wm. Schaus, in Jalapa, Mexico. Coll. Hy. Edwards, Am. Mus. Nat. Hist. Euchetes fumidus Ay. Edwards. Cocoon.—Oval, very frail in structure, and composed of dark brown threads amongst which are mingled the larval hairs. Very much like that of Huchetes egle Dr., and hardly distinguishable from it. Length, about 18 mm.; width, about 8 mm. One specimen, collected by Wm. Schaus, in Jalapa, Mexico. Coll. Hy. Edwards, Am. Mus. Nat. Hist. Pericopis leucophza Wadker. Pupa.—Color, bronzy brown, with a slight bluish reflection on the thorax, if held in certain light. Thorax and anterior portions ' of the abdominal segments above, opaque. The posterior por- tions of the segments beneath, as well as the wing-cases, are shiny. A few very short reddish brown hairs are also scattered over the segments above. The first to fourth segments are decidedly elevated dorsally, and the remaining segments gradually decreas- ing in size toward the posterior end of the body, which is bluntly rounded. Length, 22 mm. ; width, about 7 mm. ‘Two examples, collected by Wm. Schaus, in Jalapa, Mexico. Coll. Hy. Edwards, Am. Mus, Nat. Hist. Callosoma calleta Westwood. Cocoon. —Ovate, base abruptly rounded and gradually becoming narrower towards the end from which the imago makes its escape. ee eee es Oe kine = a eee Oe i ie 1893.] Beutenmiiller, Transformations of Moths. 93 The outer cocoon is finely woven, very compact and cemented together with a glutinous substance, which makes the texture very tough and hard, giving the cocoon a rather smooth appearance. Inside the cocoon is entirely covered with the glutinous substance, except about one-third from the orifice, from where it consists of a coarse brown silk loosely woven and drawn together, so that the imago can readily escape. At one side at this end of the cocoon is a short band, by means of which it hangs to the twig. Length, about 45 mm. ; width near base, about 18 mm.; width near top, about ro mm. Four specimens, collected by Wm. Schaus, in Jalapa, Mexico. Coll. Hy. Edwards, Am. Mus. Nat. Hist. Platysamia orizaba Westwood. Cocoon.—Similar to that of Callosoma calleta, but may be dis- tinguished from it by being more regular in outline, and the lower end of cocoon bluntly rounded, but not so abruptly as in C. ca//eta. The sides are almost parallel, being only slightly rounded. The meshes of the outer coating are more loosely woven, and are not cemented together with the glutinous substance. In color the cocoon is dirty silvery white or pale golden brown. It is also fastened to the twig by a short band. Length, 45 mm.; width, 20 mm. Four examples, collected by Mr. Wm. Schaus, in Jalapa, Mexico. Coll. Hy. Edwards, Am. Mus. Nat. Hist. Gortyna nitela Guen. £gg.—Bluish or greenish white, changing to cream color before exclusion ; deposited in the axil of upper leaves. The young larva on being hatched, bores into the stalk, and eats upwards. On reaching the top of the stalk, it feeds upon the young and tender leaves ; when these are destroyed it descends again into the stalk and eats downwards. Sometimes the stalk swells from the disorder of its juices, through the punctation, and the young larva is often killed. Larva before Last Moult—Head, shining, very pale chestnut color, with the second segment of the same shade, and a black 94 Bulletin American Museum of Natural History. [Vol. V.| lateral stripe which is common to both. On the side of the second segment, below the black line, is a broad streak of clear white, which encloses the black spiracles. The third segment is purplish brown. One dorsal and two subdorsal stripes of clear white. The fourth, fifth, sixth and seventh segments are wholly purplish black, and are elevated by the caterpillar when walking. The remainder of the segments are purplish brown, with the dorsal and subdorsal white stripes as before. Beneath, the posterior and anterior segments are sordid white. The middle ones purplish brown. Feet blackish. Abdominal legs sordid white. Full-grown Larva.—The posterior segment is now a little paler in ground color, and the head and anal segment yellowish. Length, 30 mm. Bores in the stalks of Burdock and a variety of other plants. Gortyna cataphracta Grote. Full-grown Larva.—Head and second segment pale testaceous. Mouth parts pitchy. Body color purplish brown with dorsal whitish stripes continued throughout the whole length. On side of head and second segment is a black shining line. On the third and fourth segments are three warty black tubercles on each side, six smaller ones on the third, and four on the fourth, dorsally. The other segments have two large and two small tubercles dor- sally, and three smaller ones laterally. All the tubercles look like points of tar or pitch. Anal segment pale testaceous, black at sides. Thoracic feet black. Abdominal legs whitish. There are also a few sordid white hairs scattered over the whole of the © body. Length, 30 mm. Bores in the stalks of Lily (Zélium superbum). wf ee Oe, nee ee Te ae ere Ree Ete tg ee rer ee ie Piseg Article IX.—ON THE DIVISIONS OF THE WHITE RIVER OR LOWER MIOCENE OF DAKOTA. By J. L. Wortman, M.D. The paleontological expedition from the American Museum of Natural History into the Miocene deposits of Dakota during the past summer was exceedingly fortunate in bringing to light a comparatively new fauna for this horizon. Notwithstanding the fact that these localities have been collected over for the past fifty years, and have yielded perhaps a greater number of indi- vidual specimens of fossil mammals than almost any other in North America, it has never apparently been suspected that the uppermost strata of this deposit contain a fauna, in many respects different from those of the middle and lower divisions, Fossils have undoubtedly been collected in these upper beds and are not unknown in the rich collections from this horizon in our various museums, but no systematic attempt has to my knowledge ever been made to point out their more exact faunal characters. Especial attention was given to this part of the sub- ject during our exploration of these bad-lands, and each specimen was carefully marked with reference to its exact position in the sedimentary mass. .From these data I have found it possible to construct a catalogue of our collections showing the more im- portant facts relating to the succession of genera and species during the time that this sediment was being laid down. The very considerable thickness of the deposit indicates of itself a long period of time, and it is not at all unnatural to suppose that important changes in the evolution of genera and species should have taken place, and be indicated by the fossils from the dif- ferent levels of the sediment. That such is the case I will attempt to show in this present communication. Before passing to a discussion of this important problem, however, I will notice briefly the physical characters of the sediments themselves to- gether with their divisions. That part of the White River deposits to which our attention was especially directed is that which forms the main divide [9s] 96 Bulletin American Museum of Natural History. [{Vol. V, between the White and Cheyenne Rivers in South Dakota in the vicinity of the Black Hills. This is the thickest portion of the White River sediment with which I am acquainted, and it is probable that it represents somewhere near the entire thickness of the accumulation which took place in the Miocene lake. Although no accurate measurements were taken its vertical depth was estimated to be about 800 feet. In this region it rests upon the black shale (Cretaceous No. 4), and in many places has been cut through by the streams, so that a complete section is exposed. I.—DESCRIPTION OF THE SEDIMENT AND ITS Martin DIvISIoNns. Heretofore there have been two main divisions recognized in the classification of the White River sediments, viz.: a lower division, under the name of the Z%tanotherium Beds, and an - upper division, known as the Oreodon Beds. ‘This latter division was made to include all those strata lying above the Titano- therium Beds, and was estimated at somewhere in the vicinity of 600 feet in thickness. I now propose a third primary division, which will include the uppermost strata of the Oreodon Beds of other authors. ‘This division may be called the Protoceras Beds, from the relative abundance of this characteristic fossil. As in the other two divisions, the separation is made largely upon the faunal characters which will be discussed later on. THE TITANOTHERIUM BEDs. This division of the Miocene has recently formed the subject of a very exhaustive and excellent article by Mr. J. B. Hatcher,’ and what is here said upon this topic is drawn largely from his statements. The beds are composed of clays, sandstones and conglomerates ; the clays greatly predominate. Near the bottom of the beds the color is often red or variegated, but the prevailing color is a very characteristic and delicate greenish white. The sandstones are never entirely continuous, and never more than a ! The Titanotherium Beds. American Naturalist, March, 1893. 1893.] Wortman on the Lower Miocene of Dakota. 97 few feet in thickness. They present every degree of compact- ness, from beds of loose sand to the most solid sandstones. The conglomerates are very similar in character, with the exception that they are usually harder. By actual measurements, Mr. Hatcher found the Titanothe- rium Beds in this locality to present a total thickness of 180 feet. Of this the first 50 feet constitutes the lower division, the next 100 feet the middle division, and the remaining 30 feet the upper division. These divisions are made upon the characteristic forms of Titanotheriide found in each layer. This is well shown in the accompanying table which is taken from Mr. Hatcher’s article. The fauna of the Titanotherium Beds is very limited, so far as the variety of forms is concerned. While the remains of the Titanotheriide are relatively very numerous other genera are but very sparsely represented by the merest fragments. The only remains other than Z?/anotherium which | could identify with any degree of certainty were those of a small Aceratherium, a species of Hyopotamus, and probably of Elotherium mortoni and : Mesohippus. With the exception of the Hyopotamus none of these E remains were found in place, but I am inclined to the opinion ; , that these genera will yet be found well down in the Titano- therium Beds. At the point where the Titanotherium Beds pass into the overlying Oreodon Beds, mingled remains of 7Zitano- therium, Aceratherium, Mesohippus, and Elotherium mortont occur ; and it is a matter of the greatest interest to note that the Acera- therium here found is not only the oldest but the most primitive member of the true rhinoceroses which has been found in this | country. Our collection contains two fairly good specimens from this layer, and they are sufficiently well preserved to fully make out the characters of the dentition. I will again refer to this subject later on. | Tue Oreopon BeEps. The changes which led up to and caused the extinction of the gigantic Titanotheriide also witnessed a remarkable transforma- tion in the fauna on the shores of the White River lake, for no sooner do we pass from the Titanotherium Beds into the Oreodon | June, 7893.) 7 [Vol. V, Bulletin American Museum of Natural History. 98 *b6g-z6g ‘sXuuorhyosy "169 -6g9 ‘syonday “g ‘xfsowioyda'yT *SSQ -1S9 ‘oSg ‘snauoydojdoyy = ‘6hg ‘Lhg ‘uop -ouwkzy *LEg-of9 ‘unueyjoiqaog *LS9 ‘org-S6S ‘POS ‘uopoay ‘LLS ‘snurejodo -AY ‘oLS-o98 ‘umuayjojq = “LL9-1L9 ‘gQ9 -bog ‘snddiyosayy “6SS-9S$ ‘uopooei{yy *€gS—19S ‘zES-OzS ‘gz ‘SzS ‘umuueyieIo0y *rgg ‘(z)snd -diyosapy “9fS *(2) SES ‘PES ‘EES ‘wnayeI20y "LS ‘gLS ‘snurejodo “AT LS Swinuayjoyq «= “LES Swintayj}e10 -oy ‘969 ‘ghS ‘uopouAuejayy ‘ghg ‘uopo -uxfyT ‘“gfg ‘unuayjoIqeog ‘11g ‘uopoag --uoo A1aa ‘Sulivaq-aynpou *S10]9a][09 Jo Jefe] pry, “OPIXO snoulsni19j Jo ayeos YUM parieaaod sAemye souog ‘sajnpou Ul pappequIl sayjin} pue suOposz1g sno -19UNN ‘“peynqujsip Ajapim pue jurys : sake uopo2g *peiojoo Ajsnissuog ‘sAej> pue sauojspues ‘auYM sauog “uNyeI}s AvjO snojnpON - Jaa} OF 0} OF ‘saaq Nodoaio > 399} OOI 03 SL *sAB]O pos0joo-jyBry] “SAVID NaAWVYG “bos ‘ShS—gES ‘umusyyeisoy “€6S ‘16S ‘6gS-SgS ‘snuejodoAzy ‘og ‘uopooeiA yy © ‘Egqg-gL9 ‘umieyyyouy “26S ‘06S ‘bes -og$ ‘snurejodoAyy “PLS ‘ELS ‘winteyjo[q *Egg-199 ‘6Sq ‘snuidejoig ‘“Sgg ‘xAuoniy *9Sg ‘(2) uopouosog ‘gbg-6£g ‘sei900}01g ‘6z9g-029 ‘e1uayonejdary ‘*619-zI1g ‘(uoposiody) snydejo19ng “snonuljuos jou ‘s[aAa] JUdIayIp SutAdnos0 sauojspues asivod *peinqiysip Ajaprm sAejo pesojoo -yuid ‘Suireaq-ajnpou : zoe] erusyonejdo'yT ‘saaq SVUIOOLOUg | | 3293 $L-0S ‘anSojejyeD winasny_ 241 Jo asoyy are siaquinu ayy, ‘26gr jo uontpedx™q Aq pourejqo eisuas) Spod jo r9JOVILYD jeI9UeD pue sotsadg dIysLIO]DVIeYD “Spee 243.59 SSOUYIY} OY} JO o]BuII}se oJeuIIxosddy “ANSOOIP, UFATY ALIHAA AO ATAV] OLHdVASILVALS 99 Wortman on the Lower Miocene of Dakota. ba 38 | ve & _ *SULIOJ }S91[1¥9 UL JUOSeId UINIzades Ty ‘AIVUSWIpNs § JeYMOUIOS 4aIUBYIO’ ply *rejour zoddn yse¥] uo 9u09 s9uUut JoLaj}sod ON ‘A[UO saTeur ut savjowoid soddn uo winjnSur jeusojut Fuoazg “ft se Auvut se Ajjeuoiseoo0 ssosiouy = ‘pajyurod puv Buoy] WSEN “UO1}99S-$$019 UT ABPNDIID “Buol “ur b—-1 wosy 40 VIUIWIPN SUIOF{ ‘“9ZIS [[VUIS JO menL4aYjJ0UnI2 “wUNEaYIOULIL L ‘yuasqe winizodesy *quasoid s9juKYyoos3 paryy, ‘sejour aaddn ys] uo a0 49uut s0uN9;s0qg “Ajuo Sayeur jo sxvjoursad asddn uo winjnZur jeusaiut Juows *% ueYy) 910Ul J9A9U Ss0STOUT *sanjturesyxe payurod 40 posse yatm *q1 Bus] 9ye4epour jo S[BSEN “UOTI998-S80I9 UT AU[NSuvIIy-qns 07 A¥[NII19 ‘Buoy ‘Ul O1—b SUIO}{ ‘9718 WINIPOU Jo mn749YjoUnILT *xAUOLL |, ‘(@) snddiqosey ‘(2) wnueyioyq ‘snure} -ododyy = ‘(2) wnweyess0y = ‘wnayqjouRN | ‘quasqe wnizodesy = *juasoad s93UeY90I) Paty T, ‘avjou s9ddn ysv|[ uo 9U09 J9UUT AOLIa}SOg 9 *X98 A9YII0 UT poxseu AjZu0.138 jou savjousad saddn uo wnjnBur pea “A9jUT ‘2 UY) 210UI J9A9U S10SIDU] ‘payutod puv yOYs AIOA S[BSENT “*UOTIO9S-SH019 Ut 91BAO-qns O3 [eoLNdIT[> ‘Suol ‘Ul gi-o1 suloPy ‘azIs aBrV] Jo mnzaayjounj7] "SQS ‘(2) UNLAyIO[| =“ WNeYyjouRI | *AYSN sow -9W0s ‘d}IYM 10 pasojoo WYysy sAvmye ore Ssouog ‘dM Ystusesd ay¥orep B SI ‘419A -moy ‘10[09 Burpreasid oy y = ‘poyedariea JO ‘YSipper uajjo aseq ay} spieMmo} ‘sXe[D ‘saqvsawo[su0d pur seuojspurs ‘sket> > “yaay OS ‘spag Jamo] } 399} OOF ‘spag PIPPI ("3995 Ogl ‘ssouyory) [e101 ) ‘Saag WOAMWAHLONVIL] ‘yaaj OF ‘spag seddy ‘snuvjodod py pue tuojiow wneyo[ay ‘bes ‘snddiyosay ‘gzS ‘€zS ‘wntiusyyeis0y ‘snddiyosayw ‘wniuey3 “eidoy “UNayIOUR] jo survUleI palsut ndd bol ‘zzS ‘12 beidlsae ‘snddiyosayy “bol ‘zzS ‘1z¢ ‘wnusyieid0y *glS ‘SLS sapamapdel ps ‘1L$ ag aye ‘89 ‘uopo ‘099 ‘snudejoig ‘snddiyosay ‘SSS ‘Lbs ‘gbS ‘uopoudumjay = ‘Lz ‘bzS ‘wnueyywss0y ‘avIYM souog ‘ysintq «saupjewos ‘Axj> AW8 YysIppey *‘pasojoo Aysna Ajyensn wets *skepo uasseq pes0joo-1431] = pacejdas sown -auios ‘sauojspuvs :iadey uopoudumjay 100 Bulletin American Museum of Natural History. [Vol. V, Beds than we find the remains of a fauna remarkable alike for its" richness and variety. Just what caused this change I am ata loss to even conjecture. The dividing line between these two primary divisions of the White River sediment is sharply indi- cated, not only by the extinction of the Titanotheriidz, but by the introduction of the variety of forms which followed with little or no previous announcement in the underlying strata. Like the Titanotherium division the Oreodon Beds are com- posed of sandstones and clays, of which the latter largely pre- dominate. These strata are seldom continuous over a wide area. They change not only in color but in the materials of which the sediment is composed sometimes with considerable abruptness. In some places the Titanotherium Beds are overlaid by a reddish gritty clay, while in others it is light or buff-colored clay, which may be interrupted by layers of sandstone. There is one layer found in the Oreodon Beds which is highly characteristic and is perhaps more constant and widely distributed than any other single stratum in the whole White River formation, This is a buff-colored clay carrying numerous calcareous nodules in which are imbedded remains of turtles and oreodons. ‘The fossils are almost invariably covered with a scale of ferruginous oxide when first removed from the matrix, and are of a decidedly reddish cast. Upon this account this stratum is known to the collector as the ‘red layer.’ It is situated somewhere between 4o and 50 feet above the top of the Titanotherium Beds and can almost always be easily identified. It varies in thickness from 10 to 20 feet, and in some rare instances it is replaced by sandstone. I have also found it without the nodules in places, but this is also quite a rare occurrence. In the particular region examined. by us there is a very con- siderable belt of sandstone found just below the Oreodon or red layer just described. It has an average thickness of about 20 feet, and as nearly as could be determined covers an area of 12 miles in length by a mile or a mile and a half in width. I men- tion this belt of sandstone in particular for the reason that it has with a single exception produced the only remains of AZe¢amy- nodon so far known. Upon either side it is replaced by a bluish or light-colored clay which appears to be entirely barren of » Sais Sahm *! a J ; E i, 1893.] Wortman on the Lower Miocene of Dakota. Iol vertebrate remains. Between this Metamynodon layer and the top of the Titanotherium Beds is found the reddish-colored gritty clay already mentioned. It has a thickness of about 25 feet and contains numerous remains of Aceratherium, Mesohippus, Elotherium, Oreodon, Hyopotamus, and in fact nearly all the genera which are found in the Oreodon Beds proper. The character of the strata overlying the typical nodule-bearing Oreodon layer is very various in different parts of the bed. Sometimes it is a moderately thick bluish-colored standstone containing numerous remains of Aceratherium, but more fre- quently it is a light-colored clay containing few fossils. In one stratum of this sandstone we obtained the remains of a Me‘amy- nodon at the highest point in which it has been known to occur. Ata distance of from 75 to 100 feet above the Oreodon layer there is a second distinct and tolerably constant nodule-bearing layer from which we obtained Oreodon, Poébrotherium and Hyenodon crucians. This appears to be the uppermost limit of the fossil-bearing Oreodon Beds, so far at least as this region is concerned, and it is at this point, therefore, that I draw the line between the middle primary division (Oreodon Beds) and the uppermost division, Protoceras Beds. If it is desirable to sub- divide the Oreodon Beds I would suggest that all those strata between the top of the Titanotherium Beds and the typical Oreodon layer would constitute the first division, the Oreodon layer itself would form a second division, and all those strata above the Oreodon layer, between it and the Protoceras Beds, would constitute the third division. PrROTOCERAS BEDs. Between what I have taken to represent the uppermost limit of the Oreodon Beds and the Protoceras Beds there is a very con- siderable thickness of light-colored clay in which very few fossils occur. ‘These strata reach a thickness of 1oo feet or more, and upon this account it is easy to distinguish, in this region at least, between the Oreodon and Protoceras Beds. In other localities, however, these clays may yet be found to be fossiliferous, in which event the line of demarkation between these two divisions will be found to be much less distinct, and their separation 102 Bulletin American Museum of Natural History. |Vol. V, accomplished with much more difficulty. They are in many places capped by isolated patches of coarse sandstone which occupy different levels. They are almost always highly fossil- iferous, and it was mostly in them that our collections from this horizon were obtained. These sandstone ledges are seldom continuous for any great distance, and often change abruptly into a fine-grained clay, which, according to our experience, is almost always barren. Immediately overlying the sandstones comes a tolerably constant, pinkish-colored, nodule-bearing clay, in which numerous remains of Lporeodon (Lucrotaphus) and Leptauchenia occur. The thickness of sediment above this is somewhat diffi- cult to determine, but judging from the highest points in the Vicinity it cannot be less than 75 or 100 feet. ‘The strata, there- fore, which constitute the Protoceras Beds are the sandstones, the nodule-bearing layer and its capping. The entire thickness of these beds is estimated at 150 feet. IIl.—FAuUNAL DISTRIBUTION AND SUCCESSION OF TYPES. FAUNAL DISTRIBUTION. 1. Zitanotherium Beds——The ‘Titanotherium Beds contain Titanotherium with its several forms, Aceratherium, Hyopotamus, Elotherium (?), Mesohippus (?). We also discovered fragmentary remains of turtles of the genera Amys and Trionyx. ‘his latter genus is apparently new to this formation, since it has been sup- posed that they disappeared from the interior lakes at the close of the Eocene. 2. Oreodon Beds.—The Oreodon Beds contain the following genera: Oreodon, Agriocherus, Poébrotherium, Leptomeryx, Hyopota- mus, Elotherium, Thinohyus, Aceratherium, Hyracodon, Mesohippus, Colodon, Protapirus, Metamynodon, Hyenodon, Dinictis, Hoplo- phoneus, Daphenus, Leplictis, Ictops, Mesodectis, Ischyromys, Paleolagus. 3. Protoceras Beds—In the Protoceras Beds are Protoceras, Eporeodon (Eucrotaphus), Leptauchenia, Cameloids, Hyopotamus, 1893.] Wortman on the Lower Miocene of Dakota. 103 Elotherium, Peccaries, BH allt a t 7 ne ne ee 1893.) Osborn, Upper Cretaceous Mammals. 319 4, 3, 2 to 4, 4,3. This comparison proves that the type of A/ents- coéssus conguistus Cope was also a second molar (type of Z7ripri- odon celaius Marsh), in which the formula is 4, 4, 4-2. One of the most interesting features about these molars, and one which enables us to recognize them readily, is, that in the upper molars the crescents open forwards, while in the lower molars they open backwards. The crescents are thus reversed in the two jaws, forming a very effective grinding apparatus. This recalls the fact that the crescents are similarly reversed in the upper and lower jaws of the Ruminant Artiodactyla, although in this case they open respectively outwards and inwards, instead of forwards and backwards. In the type of Stereognathus Charles- worth, a form which still remains éncerte sedis, there are three rows of crescents opening forwards in what Owen described as a lower jaw. Marsh has suggested that this type may be an wffper jaw ; if this were the case it would conform with the cusp arrange- ment of Meniscoéssus. No teeth are found which can with certainty be considered the upper promolars of Aeniscoéssus ; we naturally look for some- thing similar to the upper premolars of P#/odus, and we find it represented most nearly in the types of Oracodon anceps and O. conulus Marsh. Several similar teeth are represented in this collec- tion, and they are distinguished from those of P#i/odus by tubercles upon both the inner and outer bases of the main ridge; these irregularly tubercular teeth very possibly represent the third and fourth upper premolars of A/eniscoéssus ; none have been found, however, in which the main shear is quite equal in size to the shear of the fourth lower premolar. In earlier reviews of the dentition of Meniscoéssus, the writer was led to confuse the upper and lower molars by Prof. Marsh's description of Meniscoéssus (Dipriodon) robustus as a tooth with tubercles in two rows,which has a supposed zygomatic portion of the superior maxillary bone attached. This, together with the supposed lower jaw of Stereognathus, which has crescentic tubercles in three rows, led the writer to suppose that Memiscoéssus and Stereognathus together represented a family, Stereognathide, char- acterized by crescentic tubercles placed in three rows in the lower jaw and in two rows in the upper jaw. ‘This proves to be an 322 Bulletin American Museum ad Natural hares: Ss Vv, what older in type than the Puerco because they lack all traces of quadrituberculy. Sexituberculy in the lower molars is the main type (see Pl. VIII, Figs. A-H/7), but there are some in which the antero-inter- nal cusp (paraconid) is wanting, and others in which the talonid bears only one cusp instead of three. These lower teeth are of two types : first, the ‘secodont’ or tuberculo-sectorial, with an elevated anterior triangle (trigonid), and a low heel (talonid) ; second, the ‘ bunodont,’ very similar to that of the small Eocene Primates ; in this type the trigonid and talonid are on the same level. The heel usually consists of a broad basin with three well- developed cusps (hypoconid, hypoconulid and entoconid) ; this strong development of the talonid and depression of the anterior portions of the crown to the same level with the posterior portion affiliates these teeth with those of the Puerco in their general evolution. Summary of Molar Characters. Upper Molars.—a. Cusps of medium height, trigon not elevated as in the known Jarassic mammals. 6. Protocone, or main internal cusp, on or above the level of the external cusps (paracone and metacone), except in one type. c. Intermediate tubercles wanting or feebly developed on the spurs of the protocone. d. External cingulum usually well developed, with one or more supplementary cusps. e. Internal cingulum entirely wanting, except in one type. Jf. No trace of hypocone or postero-internal cusp. Lower Molars.—a. Trigonid usually elevated; sometimes depressed to level of talonid. 6. Talonid, a broad tiene usually bearing three distinct cusps (hypoconid, hypoconulid, entoconid). ¢. Protoconé,: or antero-external cusp, invariably the most elevated. d. Paraconid usually strong; depressed and degenerate ul one type. Metaconid strong. 2.—ANALYSIS OF MARSH’sS TYPES. The second step is to examine the types figured by Marsh of the six genera of Trituberculates which he has proposed. For the sake of clearness his figures are here reproduced. The type - 1893.] _ Osborn, Upper Cretaceous Mammals. 323 of Didelphops (Didelphodon) vorax (Fig. 4, 2) is a low-crowned symmetrically tritubercular upper molar, with all three cusps on nearly the same level, and two small intermediate tubercles externally placed ; there is a strong external cingulum notched in the median line. The type of Cimolestes incisus (Fig. 4, 14-15) is a lower tuberculo-sectorial molar, quite similar to a third lower molar of Didelphys. The type of Pediomys elegans (Fig. 4, 23-24) Fig. ‘ Type specimens of genera proposed by Marsh. 2, Didelphops vorax. 14, 15, Cimo- lestes incisus 23, 24, Pediomys elegans. 4.5.6. Platacodon nanus. 22-25, Stagodon nitor. 3, Telacodon lavis. 5, Batodon tenuis. Sizes as indicated. is an asymmetrical upper molar distinguished by a strong anterior spur on the external border; the intermediate tubercles are very small and internally placed. The type of Stagodon nitor (Fig. 4, 22-25) is characterized by Marsh by the resemblance of the crown to a drop of viscous fluid; the mammalian nature of the fossil is doubtful. The type of Platacodon nanus (Fig. 4, 4-6) is also of doubtful mammalian affinity. The type of TZv/acodon levis (Fig. 4, 3) is a right lower jaw containing three premolars _and three alveoli, which are believed by Marsh to have contained Bet Bulletin American Museum ee Natural wink Bs. V, what older in type than the Puerco because they lack all traces of quadrituberculy. Sexituberculy in the lower molars is the main type (see Pl. VIII, Figs. A-H7/), but there are some in which the antero-inter- nal cusp (paraconid) is wanting, and others in which the talonid bears only one cusp instead of three. These lower teeth are of two types : first, the ‘secodont’ or tuberculo-sectorial, with an elevated anterior triangle (trigonid), and a low heel (talonid) ; second, the ‘ bunodont,’ very similar to that of the small Eocene Primates ; in this type the trigonid and talonid are on the same level. The heel usually consists of a broad basin with three well- developed cusps (hypoconid, hypoconulid and entoconid) ; this strong development of the talonid and depression of the anterior portions of the crown to the same level with the posterior portion affiliates these teeth with those of the Puerco in their general evolution. Summary of Molar Characters. Upper Molars.—a. Cusps of medium height, trigon not elevated as in the known Jarassic mammals. 6. Protocone, or main internal cusp, on or above the level of the external cusps (paracone and metacone), except in one type. c. Intermediate tubercles wanting or feebly developed on the spurs of the protocone. d. External cingulum usually well developed, with one or more supplementary cusps. e. Internal cingulum entirely wanting, except in one type. jf. No trace of hypocone or postero-internal cusp. Lower Molars.—a. Trigonid usually elevated; sometimes depressed to level of talonid. 4. Talonid, a broad Hawt usually bearing three distinct cusps (hypoconid, hypoconulid, entoconid). ¢. Protoconé,: or antero-external cusp, invariably the “most elevated. d. Paraconid usually strong; depressed and degenerate in one type. Metaconid strong. 2.—ANALYSIS OF MARSH’s TYPES. The second step is to examine the types figured by Marsh of the six genera of Trituberculates which he has proposed. For the sake of clearness his figures are here reproduced. The type St _1893.] Osborn, Upper Cretaceous Mammals. 323 of Didelphops (Didelphodon) vorax (Fig. 4, 2) is a low-crowned symmetrically tritubercular upper molar, with all three cusps on nearly the same level, and two small intermediate tubercles externally placed ; there is a strong external cinguium notched in the median line. The type of Cimolestes incisus (Fig. 4, 14-15) is a lower tuberculo-sectorial molar, quite similar to a third lower molar of Dide/phys. The type of Pediomys elegans (Fig. 4, 23-24) Fig. 4. Type specimens of genera proposed by Marsh. 2, Didelphofs vorax. 14, 15, Cimo- testes incisus 23,24, Pediomys elegans. 4.5.6. Platacodon nanus. 22-25, Stagodon nitor. 3, Telacodon levis. 5, Batodon tenuis. Sizes as indicated. is an asymmetrical upper molar distinguished by a strong anterior spur on the external border; the intermediate tubercles are very small and internally placed. The type of Stagodon nitor (Fig. 4, 22-25) is characterized by Marsh by the resemblance of the crown to a drop of viscous fluid ; the mammalian nature of the fossil is doubtful. The type of Platacodon nanus (Fig. 4, 4-6) is also of doubtful mammalian affinity. The type of Zvlacodon levis (Fig. 4, 3) is a right lower jaw containing three premolars and three alveoli, which are believed by Marsh to have contained 324 Bulletin American Museum of Natural History. [Vol. V, two more premolars and a canine. The type of Batodon tenius (Fig. 4, 25) is also the anterior portion of a lower jaw containing three premolars and the alveolus of a fourth. It is evident that at present no characters can be assigned to separate the types of Cimolestes and of Didelphops, or to separate the types of Batodon and of Ze/acodon from that of Pediomys. A careful study of these generic types, together with the isolated upper and lower molars associated with them under a number of different specific names by Marsh, shows that many teeth have been placed together which evidently do not belong together, asin types of the various species of Stagodon, and that it is premature to attempt to associate many of the upper and lower teeth. Zhe dentition and taxonomy of these mammals cannot be definitely determined until we procure upper and lower jaws with the teeth in sitd. A step in this direction has recently been made by the discovery of Cope of a lower jaw, the type of Zhleodon, from another exposure of the Laramie. The best course to pursue in order to advance our knowledge of the Cretaceous Trituberculates is to lay principal emphasis upon the forms of the upper and lower teeth, and avoid the pro- posal of new generic and specific terms which cannot be defined. The accompanying comparative figures (Pl. VIII) have been pre- pared in order to bring out the chief types of upper and lower molars. 3.—SuUPERIOR AND INFERIOR DENTITION, PLATE VIII. We may pass from the most primitive to the most specialized types, taking the upper molars as a standard. Primitive features of the upper molars are: Symmetrical form of the trigon or main triangle of cones; large size of the internal cusp or proto- cone ; symmetry of external cusps or paracone and metacone ; feeble or non-development of conules ; absence of cingulum ; absence of external cingular cusps or styles (parastyle and meta- style). Primitive features of lower molars are : Elevation of the three main cusps or trigonid ; narrowness of the heel or talonid ; development of but a single cusp on the talonid. - 1893.] Osborn, Upper Cretaceous Mammats. 325 Superior Molars. A.—Crown triangular; flattened exter- nal border with an anterior cin- gulum bearing small cusps ; main cones, pr, pa, me, subequal ; con- ules, #/, small, close to protocone. Genus Pediomys Marsh. 8B.—Smaller; trigon similar to type 4 ; external border with strong ante- rior cingular spur ; conules inter- mediate in position, p/, m/. C.—Trigon greatly compressed trans- versely ; no external cingulum ; cones, pr, fa, me, subequal. Ap- parently associated with the lower ‘molar C7. D.—Trigon extended transversely; ex- ternal border symmetrical, with fairly developed cingulum ; inter- nal cone, fr, and external cone, pa and mie, separate; protocone prominent ; conules small, exter- _ nally placed. Genus Didelphops J/arsh. £.—Trigon greatly extended trans- versely ; external border sym- metrical, with strong cingulum, and deep median notch; well- developed parastyle, fs ; conules small, papain pce This specimen is the type of D. vorax (after Marsh). ¥,.—Crown extended transversely; tri- proper compressed by approx- Seed a of external cones, fa and me, to protocone ; external bor- der broad, bilobate, with strong parastyle and metastyle, gs and mts, and small mesostyle. Teeth of this type are mistak- enly referred by Marsh to Dide/- phops, species D. comptus. are similar in type to the upper molars of Ectoconus, a mem- ber of the Puerco Periptychide. G.—Trigon extended transversely : three external cusps in line ; pro- tocone depressed ; ? paracone ele- vated ; partial internal cingulum. U molars of this type are doubtfully referred to. Batodon tenuis by Marsh. They are somewhat similar in type to Dissacus, a member of Puerco Mesonychide. Inferior Molars. Al—Trigon is less elevated; paraconid as lofty as protocone; talonid somewhat depressed with large hypoconid and entoconid and small hypoconulid. These teeth agree in size with Type A, superior molar. They are more nearly of the bunodont type than any other teeth known from the Laramie. #1.—Protoconid and metaconid de- pressed ; paraconid elevated ; tal- onid rather narrow, with a single cusp. Ci.—Trigonid and talonid greatly com- pressed transversely; sexicuspi- date. This transversely compressed crown is somewhat similar in type to Haploconus xiphodon Cope, also to Zetodon, another aberrant member of the Puerco Peripty- chide. Genus Cimolestes Marsh. //.—Protoconid and metaconid eleva- ted ; paraconid extremely de- pressed ; talonid supporting three cusps broader than trigonid. The type of Cimolestes incisus Marsh, although larger than this tooth, has similar characters. £i—tTrigonid elevated; protocone elevated above conid and metaconid ; Sinai beced. The tooth mds in size with the type of Didelphops vorax ; its association is uncer- tain. 326 Bulletin American Museum of Natural History. |Vol.V, It thus appears that there are six or seven quite distinct types of superior molars (4-G), and a similar number of inferior molar types. The upper and lower molars referred by Marsh to various species of Pediomys, Didelphops, Cimolestes, Batodon and Telacodon conform more or less closely to one or the other of these types ; some of the lower molars figured by Marsh are even more strikingly bunodont than our type A/. The premolars determined by Marsh as Stagodon validus, tumti- dus and nitor are as his terms indicate of a stout character, which we should expect to find associated with our Type /, superior molar. They are also somewhat similar to the premolars of some of the Periptychide, such as certain species of Haploconus, Ecto- conus and Periptychus. | III.—FauNAL RELATIONS OF THE LARAMIE MAMMALS. The first question is one of age. These mammals are found in the Laramie, or uppermost of the six great divisions of the Cretaceous. Their exact stratigraphical position is in the middle or lower half of the Laramie Beds. Thus far they are only known to occur in the Wyoming exposures associated with remains of the large Dinosaurians such as Agathaumus ( Triceratops), Diclonius, Lelaps. In New Mexico, as observed by Wortman, some of these Dinosaurs continue to the very top strata of the Laramie, which in turn are conformably overlaid by the basal Eocene or Puerco. Therefore the Puerco mammals, although they are separated by a considerable interval (of Upper Laramie) in which no mammals have been found, are still much nearer to these Laramie mammals than the latter are to the Middle Jurassic mammals of the Atlan- — tosaurus Beds. The second question is one of faunal relations. In his latest paper upon the Cretaceous Mammalia (March, 1892), Prof. Marsh draws two general conclusions as to the structure and relations of these mammals. First, as to their geological rela- tions and age, he says : “They are mainly Mesozoic in type, and more nearly related to the Jurassic forms below than to those in the Tertiary above. - 1893.] Osborn, Upper Cretaceous Mammals. 3 327 .---Bearing in mind all that is known to-day of the develop- ment and succession of vertebrate life in America, from the early Silurian on to the present time, it is safe to say that the faunal break as now known between the Laramie and Lower Wahsatch, is far more profound than would be the case if the en- tire Jurassic and the Cretaceous below the Laramie were wanting.” Second, as to the faunal relations of these mammals, he says : “ The geological lesson now taught by these mammalian relics and their associated vertebrate fossils is no less important, but hardly what was expected. These remains are not transitional between Mesozoic and Tertiary forms, but their affinities are with the former without a doubt; thus indicating a great faunal break between the time in the Cretaceous when they lived, and the earliest known Tertiary, or between the Ceratops horizon and the Coryphodon Beds of the Eocene Wahsatch. The lower divi- sion of the Coryphodon Beds or Lower Wahsatch (Puerco) is clearly Tertiary, and the great break is between this horizon and the Ceratops Beds of the Laramie. Each of these faunas is now known by many species of vertebrate fossils represented by hun- dreds of specimens, and the more the two are compared the stronger becomes the contrast between them. Instead of placing them close together, as some geologists seem inclined to do, it _ will be more profitable in future to search for the great series of intervening strata containing the forms that lead from one to the other.” Both of these conclusions appear to the writer to be directly the reverse of the lesson taught by a comparison of the Laramie fauna with the Jurassic and the Puerco or basal division of the Eocene. The fact is, these Laramie mammals are surprisingly near those of the Puerco, and in some cases almost identical with them; in other cases they are of a somewhat older type. Therefore, the greatest gap to be filled by future discovery is between this Laramie fauna and the Jurassic. For this Laramie fauna is separated from the Puerco about as widely as the Puerco is from the Wahsatch, but no more widely ; whereas it is separated by a profound gap from the Jurassic fauna, as proved, first, by a com- parison of the general stages of evolution seen in mammals which belong to both periods; second, by the advanced special 328 Bulletin American Museum of Natural History. [Vol. V, evolution of the molar pattern, which is of a modern type in the Laramie, while it is wholly of antique type in the Jurassic, and finally by the difference between the typical modern or Eutherian dental formula seen in the Cretaceous, and the primitive formula found in the Jurassic. A valuable key to the relative age of the Jurassic and Laramie faunas is seen in the stages of dental evolution of the Plagiau- lacide. The Laramie stage is very close to that observed in the Puerco of America, and the Cernaysian of France. As long ago pointed out by the writer, these little mammals serve admirably to mark the progress of geological time by the absolute regu- larity of their evolution, indicated in the steady loss of the anterior premolars, by the regular addition of ridges to the fourth lower premolar, and of tubercles to the upper and lower molars. COMPARATIVE TABLE OF THE PLAGIAULACIDA, Jurassic. | CRETACEOUS. Lower Eocene. Purbeck. Laramie. Puerco. / Cernaysian. Number of lower premolars.....) 4-3 2 2-1 I t grooves on pm, 4..... 7-9 II-14 12-15 14 a tubercles on first lower molar, outer, inner... 4-2 6-4 6-4 9-6 There can remain no doubt from this comparison that the Laramie Plagiaulacids stand much nearer the Puerco and Cernay- sian types than they do to their Jurassic ancestors. In fact it is nearly impossible to distinguish the larger members of the Creta- ceous Ptilodus from the Puerco Péilodus ; they are in substantially the same stage of dental evolution, and so nearly alike that the writer was for a long time tempted to believe that the Laramie and Puerco faunz were contemporaneous. ‘This must still be re- garded as a possibility, although the Puerco in its exposure in north- western New Mexico is plainly seen to overlie the Cretaceous. We find entirely analogous proof of the gap between the Laramie and the Jurassic, and of the affinity of the Laramie with the Puerco among the Trituberculates, using this term to cover animals possibly belonging to the Marsupials, Insectivores, Creo- donts, and the like. eee 1). 1893. | Osborn, Upper Cretaceous Mammals. 329 CoMPARATIVE TABLE OF JURASSIC AND UPPER CRETACEOUS TRITUBERCULATES. Jurassic. - CRETACEOUS, Lower Eocene. Purbeck. Laramie. Puerco. Typical dental formula a. ty 4. 8. BE. 4-S.. Ss ee ae, Molar types.... --- Triconodont and Tritubercular seco-|The same. tritubercular, se-| dont and buno- codont only. dont. Upper Molars....... High crowned. |Low crowned. The same. No intermediate} Small intermedi-|The same. cusps. ate cusps. No hypocone. A hypocone, vari- able. Lower Molars....... Narrow spur-like|Broad heel-like ta-/The same. talon cusp. lon, bearing I-3 cusps. In this table the transition from the Jurassic to the Laramie is seen to be very wide. In the Laramie the modern placental or marsupial dental formule are established—the teeth behind the canine are usually seven, and do not usually exceed eight. Marsh observes in one jaw what he considers five premolar alveoli. Second, out of the high crowned upper molars of the Jurassic, such as those of Amblotherium and Spalacotherium, a relatively low-crowned or bunodont tritubercular molar has been evolved; as this is a possible parent form of the ungulate and primate upper molars, it is an essentially Tertiary type. Third, the lower molars have evolved a broad talonid or heel, which in many cases present three cusps, whereas in Jurassic types the talonid is a spur or a narrow simple basin. Fourth, the trigonid, which is always very elevated in the Jurassic types, sinks in some cases to the level of the talonid—another modernization looking towards ungulate and primate ancestry. Two features make the Laramie fauna appear more ancient than the Puerco: first, the non-development of an internal cingu- lum, which is common in the Puerco; second, the entire absence of the hypocone, which is quite strong in some Puerco mammals. On the other hand the upper and lower molars of Types /, G, /, Ci, respectively, are analogous to Zctoconus, Dissacus, Diacodon and Haploconus of the Puerco, 330 Bulletin American Museum of Natural History. |Vol. V.| The zodélogical affinities of this fauna are at present hard to determine. P#i/odus and Meniscoéssus are still provisionally re- ferred with the Multituberculates to the Monotremes. Zhl@odon exhibits a jaw without an angle, and with a surprising resemblance to that of Polymastodon ; the jaw is certainly neither of the typi- cal placental nor of the marsupial type; this animal may there- fore be provisionally considered a trituberculate Monotreme. The placentals and marsupials, and the question whether one or both of these orders is represented in this fauna, is still unset- tled. Not a single jaw has been found or reported sufficiently complete in the delicate region of the angle to determine posi- tively its placental or marsupial structure. Portions of the jaws which are preserved indicate the presence of the marsupial type of inflection, while others point to distinct placental angulation. BIBLIOGRAPHY. E. D. Corpr.—Mammalia in the Laramie Formation: