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STAT OF ROaID* -AE OARD Of C-n-EvAT E.n.. U..,.. ..r.-or ORIDOA OLrnCAL SUR a -L Mnow .-I CONTRIBUTIONS TO FLORIDA VERTEBRATE PALEONTOLOGY pApER No. X A HEW SPECIES OF OSTEOBORUS FROM THE BONE VALLEY FORMATION OF FLORIDA By s. J. Ol.on Juno e, 1l o 9,, 6147 4 6 PLATE 1 Ok.'usrbi~l G.Z.c / .../,-d FOIG3 /, P.-/S i-- -f O.Oeob5crajsipineatv,01 F.n G.S.NVS644X]I A NEW SPECIES OF OSTEOBORUS FROM THE BONE VALLEY FORMATION OF FLORIDA S. J. Olsen Vertebrate Paleontologist Florida Geological Survey The phosphate pits of Floridahave produced many inter- esting and scientifically important vertebrate fossils in the past and specimens recently acquired by the Florida Geolog- ical Survey indicate that more new forms may indeed turn up n the future from these mineral deposits. Due to themethods employedinthe mining of phosphates, it is only through the keen observations of the men engaged m ths work that anyof the larger vertebratesare saved from complete destruct-on by the mnnog machinery. Although Dr. T. E. White described a borophagme skull from the Bone Valley gravels, this is the first additional material representing these carnivores that is complete enough for a comparison to be made between it and other related forms. Faily CANIDAE Subfamily BOROPHAGINAE Osteoborus crasa n. sp. Referred material. F.G.S. V-5644 (plate 1). Partial right mandible lacking anterior portion of syphysis and ascending ramus. C, P-M present and alveolus of PY Horizon and ocalty Bon Valley formatlonI. Pit of the American Agricultural Chemical Company, Pierce, Polk County, Florida. i Investigatons are underwayto deter the exact age of the Bone Valley formation but present ndlcations place this formation m the middle and upper Miocene. The re- ferred specimen was collected with insufficient data to pinpoint it stratlgraphlcally, but because of its distrbu- tional importance i s worthy of recording. 64746 FLo11101 GOLOGICIL IsuREY Characters. Aboophagne havng .th.e s.me e.s Discussion. White erected a new genus for the borophagne that hT described from the same beds n which 0. crassa- .occurred. His description was based on-the char- acters of the skull, all denttiion except p3 being absent (Whlte 1941). Among the unidentified specimens m the collections of the Florida GeologIcal Survey was a lower Jaw of a camd; although fragmentary, it is important enough to warrant descript-on. In view of the fact that enough of the lower den- titlon of this new form is present to definitely place it in the genus Osteoborus, a re-exu nation and comparison of Pou may abolish this genus and place Whlte's species in the genus Osteoborus. DOripto The mandibl of O crassaetus when com- pared with other members of this genus is more massive and heavier in build than 0. cyonode (U.C.Mus. Pal. 30663) and more closely approaches 0. hill m size (Johnston 1939). 0. validus has similar massive characteristics, but has an overall se which is considerably larger. ThIs form was first des.ribeda a mutationbecauseof the shorter andmore crowded premolar region, the reduction of the tubercular teeth, and the slight enlargement of the carnassial (Matthew and Cook 1909). Mditional material of this carnivore was collected from the Pliocene of Texas and described by C. S. Johnston (1939). The canine was not preserved m either of these speci- mens, but the a1vealus of the camnne was preserved in the Teas form, indicating a smaller tooth proportionally than that which is present n O.crassa pineatus. Although the -terior portion of the symphystal surface has been restored, the root of the canine is in place, estab- lishing its position in the jaw. The huge canine is completely outside the observed ranges of variation for any sample of CoTu,1uTIONS To FLOR,- A VERTeSR-TE P*LEONTOtoY a borophagine dogs and may be just an anmalous individual that wouldn't be representative of theborophaginepopulation from the Bone Valley formation. Enough of the bottom of the alveolus of the double rooted P3 is preserved to restore it as indicated (p. 1, fig. 2). Thealveolus of P2 was restored by comparing with that of 0. cyo de P is a subtrigonid tooth with the principal cusp pitched backward. The heel is a wide transvere crest having a posterior accessory cusp which is small ad close to the heel crest and tends to fuse with it. These characters, along with the metaconid on MI. which is present in the referred specimen, were listed as S., des by Drs. Matthew S ...y. y of this material by S- in erectmg the new genus Osteoborus for these specimens (Richey 1938). CHART Measurements (in millimeters) of Mandible and teeth 0. 0. 0. cyonoides hill crassapmeatus Depth of jaw below P4 27.5 34.9 34.5 Width of jaw below P4 16.7 18.7 17.5 Depth of jaw below MI 31.6 36.4 33.0 Width of jaw below M1 16.7 18.2 16.5 Anteroposterior diameter P4 16.5 19.0 18.0 Trasverse diameter P4 11.0 12.8 13.0 Anteroposterior dieter Ml 27.7 30.0 31.0 Trasverse diameter MI 12.7 12.0 13.0 A more thorough check of the phosphate pits of Pol Couty, Florida, may n tue yield more of this interesting carnivore and help in establishing its phyletic position. FLORIDA GEOLOGICAL sURvEY ACKNOWLEDGMENTS I grateful to Dr. H. Gunter for his permission to describe this specimen and to Dr. R.A. Stirton for the oan of a specimen of O. cyonoides for comparison. I also wish to thank Dr. D.E. Savage for his helpful suggestions in pre- paring this description. The figure is the work of Adrew Janson, Scientific Illus- trator of the Florida Geological Survey. REFERENCES Johnston, C. 5. 1939 Preliminary rort on the late middle Plio- c0ne, A0tel lo it, and the dOesto ofa ew meber of th lgns Osteoborus: Am. Jour. Sci., ol. 13, pp. 895-898. 1939 A skull of Osteoborus -alidus from the early middle Plioceneof Texas: Jour. Paleontology, vol. 13, pp. 526-538. Matthew, W. D. 1909 (and Cook, J. H.) A Pliocene fauna from western Nebraska: m. Mus. Nat. History Bull. vo. 26, art. 27, pp. 361-414. 1930 (and Stirton, R. o I . 19, pp. 171-216. Richy, K. A. 1938 Osteoborus diabloensis, a new d from the Black Hawk Ranch fauna, Mt. Diablo, Cal- fornia. California Univ., Dept. Geol. Sci., Bull., vol. 24. pp. 303-308. Stirton, A. 93 (and Vanderhoof, V. L.) Osteoborus, a new 00of d20,aa.nd0tsrelations toBoophisg COe: CaliforniaUniv., Dept. Geol. Sc., Bull., vo. 23, pp. 175-182. IIIRIIBUTIOJ ITOI$ 1 1 ITBI* IP*E*T LO White.T.E L41 70. |
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