THE PEARCE­ SELLARDS Series NUMBER 19 THE GENUS DINOFELIS (CARNIVORA, MAMMALIA) IN THE BLANCAN OF NORTH AMERICA by BJORN KURTEN Submitted for publication May 30, 1972 TEXAS MEMORIAL MUSEUM / 24TH & TRINITY / AUSTIN, TEXAS W. W. NEWCOMB, JR., DIRECTOR The Genus Dinofelis (Carnivora, Mammalia) in the Blancan ofNorth America Bjorn Kurten* INTRODUCTION The Blanco fauna was described by Meade (1945), who created the new felid species Panthera palaeoonca based on a skull and associated mandible. , Comparing the new species with members of the genera Panthera and Felis,he concluded that it showed close affinity to the jaguar. This has been tenta­tively accepted by later workers (Savage, 1960). The species forms the basis for the record of the genus Panthera in the Blancan of North America. A restudy of the material in 1971 led to the discovery in the collections of the Texas Memorial Museum at the University of Texas at Austin, of an additional, better preserved specimen (an upper canine) which clearly did not belong to Panthera or Felis but showed close affinity to the genus Dino­felis which has hitherto only been recorded from the Old World. Checkingback on the type skull and mandible, the reference to Dinofelis could be fully substantiated. I wish to express my gratitude to Drs. John A. Wilson and Ernest L. Lundelius, the University of Texas at Austin, for the opportunity to studycollections in their care. The abbreviation TMM is used to signify collections ofthe Texas Memorial Museum, the University of Texas at Austin. These were formerly in the collections of the Bureau of Economic Geology and in previous reportsbore the prefix BEG. Genus Dinofelis Zdansky Dinofelis Zdansky, 1924 Therailurus Piveteau, 1948 DinofelisZdansky. Hemmer l965 (seethispaperformore detailedsynonymy). Type species: Dinofelis abeli Zdansky 1924 Diagnosis: Large Felidae with somewhat flattened, moderately enlarged, fairly straight upper canines; lower canine moderately reduced; incisors in shallow arch; no P2; cheek teeth relatively slender; P3 tending to reduc­tion; P4 with large accessory cusps; short postorbital processes; zygomaticarch relatively shallow; large mastoid process; mandible with slightly or moderately reduced coronoid process and with ventral border deflected downwardto angle;upperborderoframusrising steeplyfrom P3 to canine. Dinofelis palaeoonca (Meade) Panthera palaeoonca Meade, 1945 *Department of Zoology, University of Helsinki, Finland Type: TMM 31181-192, skull and mandible (Meade, op. cit., pi. 48, figs. 1,2; pi. 49. Referred: TMM 31176-63, fragment of P4; TMM 31176-4, right upper canine (fig. 1).Locality and horizon; Blanco beds, Crosby County, Texas; type from head of Blanco Canyon, Locality 31181, Site 11; referred specimens from Locality 31176, Site 6. Age: Blancan. Diagnosis: A Dinofelis slightly smaller than D. diastemata (Astre); frontals higher than occiput; P4 without distinct ectoparastyle; mandibular dia­ stema short; P3 moderately reduced; Mi with small talonid. DISCUSSION ” “ The type skull of Panthera palaeoonca unfortunately is badly cracked and deformed, and this, as Meade (1945) noted, makes it difficult to studythe various elements in relation to each other, and to compare them with other species. Still, a number of characters deviate significantly from the norm in the genus Panthera, and tend to ally this form to the Dinofelis group. The upper canines in the type are badly cracked and puffed up, which tends to mask their characteristics. Fortunately, a well preserved isolated canine has come to light in the Blanco collections. This is TMM 31176-4,which comes from the same site as the carnassial fragment referred by Meade to this species. The canine, which is of the same size as that in the type skull, is markedly flattened and saber-like in comparison with the Panthera canine (see comparative measurements in table 1). It has smooth sides, lacking the grooving so characteristic of Felis and Panthera. Both the front and hind edges are keeled, but there is no crenulation. The canine thus is quite differ­ent from its homologue in Panthera, and compares closely with Dinofelis. It differs, on the other hand, from true saber-tooths like Homotherium (= Dinobastis), Machairodus, and so on, by its relative straightness and mod­erate crown height, and the absence ofcrenulation. The genus Dinofelis was revised by Hemmer (1965), who showed that,in addition to the type species D. abeli from China, it should include the species D. diastemata (Astre) from Europe and D. piveteaui (Ewer) and D. barlowi (Broom) from Africa. The three latter species had previouslybeen placed in a separate genus, Therailurus, which as Hemmer shows, falls into the synonymy of Dinofelis. Hemmer lists a number of distinctive characters for the genus. Owing to the poor preservation of the Blanco specimen, not all of them could be studied in the present case; on the other hand, I have added some charac­ters that seem important. In addition to Hemmer’s study, my comparisons are based on original studies of the following Old World specimens of Dinofelis: University of Uppsala, Paleontological Institute: Dinofelis abeli, type skull and mandible (Zdansky, 1924, pi. 31, figs. 1-4). The specimen comes from Locality B in Honan, northern China, and is of post-Pontian age, not Pon­tian as assumed by Hemmer (1965). University of Lyon, Institute of Geology and Paleontology; Dinofelis diastemata, p. 29, cast of type skull (original in Astre, 1929, figs. 1-3). The original comes from Perpignan, France, and is Astian in age. Measurements of these specimens are given in table 1, which also lists comparative measurements of a Recent specimen of Panthera onca: Univer­sity of Cambridge Museum of Zoology No. K 5782 (from Guatemala). The following is a listing of a number of salient characters in Dinofelis palaeoonca (D p.), in Old World species of Dinofelis (D.), and in Panthera onca (P.0.). SKULL Dp. Frontalia higher than occiput D. Frontalia and occiput at same level or occiput slightly higher P.o. Frontalia slightly higher than occiput D.p. Crista sagittalis and lambdoidea well developed D. Crista sagittalis and lambdoidea well developed P.o. Crista sagittalis and lambdoidea well developed D.p. Postorbital processes short D. Postorbital processes short P.o. Postorbital processes relatively long D.p. Zygomatic arch relatively shallow, especially hind part D. Zygomatic arch relatively shallow, especially hind part P.o. Zygomatic arch deeper, especially hind part D.p. Mastoid process well developed D. Mastoid process well developed P.o. Mastoid process less developed D.p. Incisors forming shallow arch D. Incisors forming shallow arch P.o. Incisors in transverse line TEETH D.p. Incisors relatively large D. Incisors relatively large P.o. Incisors relatively small D.p. Upper canine long, narrow, high-crowned, flattened with smooth sides: front and hind edge keeled but not crenulated D. Same as above P.o. Upper canine stout, grooved, with feebly keeled edges lackingcrenulation D.p. No D. No P.o. P-present D.p. with short but high main cusp D. P3 with short but high main cusp P.o. with longer main cusp D.p. without distinct ectoparastyle: metastyle relatively short D. P4 with or without distinct ectoparastyle; metastyle relatively short P.o. P4 without distinct ectoparastyle; metastyle relatively longer D.p. Lower canine markedly smaller than upper D. Lower canine markedly smaller than upper P.o. Lower canine only slightly smaller than upper D.p. P3 somewhat reduced D. P3 moderately to strongly reduced P.o. P3 fairly large D.p. P4 slender with short but high main cusp and large secondary cusps D. P4 slender with short but high main cusp and large secondary cusps P.o. P4 stouter with longer main cusp and shorter secondary cusps D.p. Mj slender with small talonid D. Mi slender, mostly without talonid P.o. Mj stouter, mostly with small talonid MANDIBLE D.p. Ventral border ofmandible deflected downward to angle D. Ventral border of mandible deflected downward to angle P.o. Ventral border of mandible nearly straight D.p. Diastema of medium length, border of mandible rises steeply from P3 to C D. Diastema long, border rises steeply P.o. Diastemaofmediumlength,borderalmosthorizontal The list shows the Blancan form to agree with Dinofelis in the majority of the characters in which that genus differs from Panthera; the few excep­ tions are of minor importance but probably suffice to validate palaeoonca as a distinct species within Dinofelis. It would seem to be a relatively primi­ tive species within that genus, perhaps closer to D. diastemata than to D. abeli (in which P3 is much more reduced), and definitely less specialized than the Pleistocene forms in southern Africa. Hemmer (1965) discusses the probable ancestry of Dinofelis and points to important resemblances to the Oligocene Nimravus of Europe and North America (see Toohey, 1958), in which, however, the dentition is much more primitive. In dental characters Dinofelis is rather close to the Pseudae­ lurus-Metailurus group (see Zdansky, 1924), but the skull of these last- mentioned felids does not show any close approximation to the type seen in Dinofelis. It should be remembered, however, that the species of Dinofelis are much larger than any members of thePseudaelurus group and that some ofthedifferencesmaybe duetoallometricgrowth. Fig. 1.-Dinofelis palaeoonca (Meade), right upper canine. X1 TABLE 1 Skull and dental dimensions in Dinofelis and in Panthera onca Dinofelis Dinofelis Dinofelis Panthera palaeoonca diastemata abeli onca isol. type type cast type C Lyon Uppsala K 5782 Cs anteroposterior 18.6 ca. 20 23Vi 26.5 18.1 — — transverse 11.7 13 17.5 14.4 anteroposterior 19.8 21.5 23.4 17.0 — transverse 10.8 10 11.0 9.0 p4 anteroposterior 33.4 32.2 36.3 26.7 — transverse 16.5 15.5 17.1 13.5 — blade width 10.8 11.0 11.3 9.6 Ci anteroposterior 14.9 15.0 20.1 18.0 — transverse 11.0 10.5 14.5 13.2 P3 anteroposterior 15.0 16* 13.8 14.5 — — transverse 7.9 8.0 7.3 P4 anteroposterior 23.0 23 24.7 18.9 — —— transverse 11.0 8.8 — — — main cusp anteroposterior 9.3 8.8 Mi anteroposterior 24.3 24 27.0 20.2 —— transverse 10.0 13.3 10.5 Basal length of skull 208 231 267 214 Condylobasal length 222 246 280 227 Zygomatic width ca. 145 169 170 — — Mastoid width 88 93 103 — Width of muzzle at canines ca. 63 64V2 72 — Bicondylar width SOVi 48.5 48.7 — Height of zygoma at orbit 28.4 30.7 29.8 *Measurementsofmandibular teethfrom Hemmer(1965) REFERENCES ASTRE, G. 1929. Sur un Felin a particularity oursoides des Limons Pliocenes du Roussillon. Bull. Soc. Geol. France, ser. 4, Vol. 29, pp. 199-204. HEMMER, H. 1965. Zur Nomenklatur und Verbreitung des Genus Diuofelis Zdansky,1924 (Therailurus Piveteau, 1948). Palaeont. Africana, Vol. 9, pp. 78-89.' MEADE, G. E. 1945. The Blanco fauna. Univ. Texas Publ., Vol. 4401, pp. 509-556. PIVETEAU, J. 1948. Un Felide du Pliocene de Roussillon. Ann. Paleont., Vol. 34, pp. 97-124. SAVAGE, D. E. 1960. A survey of various Late Cenozoic vertebrate faunas of the Pan­handle of Texas. Part 111. Felidae. Univ. California Publ. Geol. Sci., Vol. 36, pp. 317-344. TOOHEY, L. 1958. The species of Nimravus (Carnivora, Felidae). Bull. Amer. Mus. Nat. Hist., Vol. 118, art. 2, pp. 73-112. ZDANSKY, O. 1924. Jungteriare Carnivoren Chinas. Palaeont. Sinica, ser. C, Vol. 1, fasc. 1, pp. 1-155. The Pearce-Sellards Series The Pearce-Sellards Series are occasional papers published by the Texas Me­morial Museum, 24th & Trinity, Austin, Texas. Other publications include the Bulletin series, Notes, and mimeographed information circulars. A complete list will be sent upon request. No. 1. Fossil Bears from Texas, By Bjbm Kurten, 1963 35 No. 2. Post-Pleistocene Raccoons from Central Texas and their Zoogeo­graphic Significance, by Thomas Wright & Ernest Lundelius, Jr.,1963 40 No. 3. A New Fossil Tortoise from the Texas Miocene, by Walter Auffen­berg, 1964 25 No. 4. The Osteology and Relationships of the Piocene Ground Squirrel.Citelhis dotti Hibbard, from the Ogallala Formation of Beaver Countv, Oklahoma, by Margaret Skeels Stevens, 1966 75 No. 5. The Status of Bootherium brazosisby Clayton E. Ray, 1966 .25 , No. 6. Geologic Reconnaissance of the Fort Davis National Historic...Site, Texas, by Gordon Everett, 1967 35 No. 7. Mammalian Remains from Rattlesnake Cave, Kinney County,Texas, by Holmes A. Semken, 1967 35 No. 8. Development of Terminal Buds in Pinyon Pine and Douglas-firTrees, by Charles L. Douglas & James A. Erdman, 1967 35 No. 9. Toxotherium (Mammalia: Rhinocerotoidea) from Western Jeff Davis County, Texas, by John M. Harris, 1967 35 No. 10. New Brazilian Forms of Hyla, by Bertha Lutz, 1968 35 No. 11. Taxonomy of the Neotropical Hylidae, by Bertha Lutz, 1968 .35 ... No. 12. Geographic Variation of Brazilian Species of HyJa, by Bertha Lutz, 1968 35 No. 13. Remarks on the Geographic Distribution and Phyletic Trends of South American Toads, by Jose Cei, 1968 35 No. 14. A New Genus of Eomyid Rodent from the Oligocene Ash SpringLocal Fauna of Trans-Pecos Texas, by John M. Harris & Albert E. Wood 315 No. 15. New Earlv Miocene Formation and Vertebrate Local Fauna, BigBend National Park, Brewster County, Texas, by Margaret S. Stevens, James B. Stevens, & Mary R. Dawson 75 No. 16.NewFossilRodentsfromtheEarlyOligoceneRanchoGaitanLocal Fauna, Northeastern Chihuahua, Mexico, by Ismael Ferrusquia­ 35 Villafranca and Albert E. Wood, 1969 No. 17.Earlv Tertiary Vertebrate Faunas, Vieja Group, Trans-Pecos Texas; Entelodontidae, by John A. Wilson, 19/1 35 No. 18. Earlv Tertiary Vertebrate Faunas, Vieja Group, Trans-Pecos Texas: Equidae, by Ann-Marie Forsten and Paul O. McGrew, 1971 . . .35