Hominin-Carnivore Interactions: Evidence from Modern
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Carnivora from the Late Miocene Love Bone Bed of Florida
Bull. Fla. Mus. Nat. Hist. (2005) 45(4): 413-434 413 CARNIVORA FROM THE LATE MIOCENE LOVE BONE BED OF FLORIDA Jon A. Baskin1 Eleven genera and twelve species of Carnivora are known from the late Miocene Love Bone Bed Local Fauna, Alachua County, Florida. Taxa from there described in detail for the first time include the canid cf. Urocyon sp., the hemicyonine ursid cf. Plithocyon sp., and the mustelids Leptarctus webbi n. sp., Hoplictis sp., and ?Sthenictis near ?S. lacota. Postcrania of the nimravid Barbourofelis indicate that it had a subdigitigrade posture and most likely stalked and ambushed its prey in dense cover. The postcranial morphology of Nimravides (Felidae) is most similar to the jaguar, Panthera onca. The carnivorans strongly support a latest Clarendonian age assignment for the Love Bone Bed. Although the Love Bone Bed local fauna does show some evidence of endemism at the species level, it demonstrates that by the late Clarendonian, Florida had become part of the Clarendonian chronofauna of the midcontinent, in contrast to the higher endemism present in the early Miocene and in the later Miocene and Pliocene of Florida. Key Words: Carnivora; Miocene; Clarendonian; Florida; Love Bone Bed; Leptarctus webbi n. sp. INTRODUCTION can Museum of Natural History, New York; F:AM, Frick The Love Bone Bed Local Fauna, Alachua County, fossil mammal collection, part of the AMNH; UF, Florida Florida, has produced the largest and most diverse late Museum of Natural History, University of Florida. Miocene vertebrate fauna known from eastern North All measurements are in millimeters. The follow- America, including 43 species of mammals (Webb et al. -
Carnivora, Mammalia) in the Blancan of North America
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 of North America Bjorn Kurten* INTRODUCTION The Blanco fauna was described by Meade (1945), who created the new on a felid species Panthera palaeoonca , based 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 tenta- tively 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 Dino- felis which has hitherto only been recorded from the Old World. Checking back 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 study collections in their care. The abbreviation TMM is used to signify collections of the Texas Memorial Museum, the University of Texas at Austin. These were formerly in the collections of the Bureau of Economic Geology and in previous reports bore the prefix BEG. -
Mammalia, Felidae, Canidae, and Mustelidae) from the Earliest Hemphillian Screw Bean Local Fauna, Big Bend National Park, Brewster County, Texas
Chapter 9 Carnivora (Mammalia, Felidae, Canidae, and Mustelidae) From the Earliest Hemphillian Screw Bean Local Fauna, Big Bend National Park, Brewster County, Texas MARGARET SKEELS STEVENS1 AND JAMES BOWIE STEVENS2 ABSTRACT The Screw Bean Local Fauna is the earliest Hemphillian fauna of the southwestern United States. The fossil remains occur in all parts of the informal Banta Shut-in formation, nowhere very fossiliferous. The formation is informally subdivided on the basis of stepwise ®ning and slowing deposition into Lower (least fossiliferous), Middle, and Red clay members, succeeded by the valley-®lling, Bench member (most fossiliferous). Identi®ed Carnivora include: cf. Pseudaelurus sp. and cf. Nimravides catocopis, medium and large extinct cats; Epicyon haydeni, large borophagine dog; Vulpes sp., small fox; cf. Eucyon sp., extinct primitive canine; Buisnictis chisoensis, n. sp., extinct skunk; and Martes sp., marten. B. chisoensis may be allied with Spilogale on the basis of mastoid specialization. Some of the Screw Bean taxa are late survivors of the Clarendonian Chronofauna, which extended through most or all of the early Hemphillian. The early early Hemphillian, late Miocene age attributed to the fauna is based on the Screw Bean assemblage postdating or- eodont and predating North American edentate occurrences, on lack of de®ning Hemphillian taxa, and on stage of evolution. INTRODUCTION southwestern North America, and ®ll a pa- leobiogeographic gap. In Trans-Pecos Texas NAMING AND IMPORTANCE OF THE SCREW and adjacent Chihuahua and Coahuila, Mex- BEAN LOCAL FAUNA: The name ``Screw Bean ico, they provide an age determination for Local Fauna,'' Banta Shut-in formation, postvolcanic (,18±20 Ma; Henry et al., Trans-Pecos Texas (®g. -
A New Species of Machairodus from the Late Miocene Kalmakpai Locality in Eastern Kazakhstan (USSR)
Ann. Zool. Fennici 28:361 -369 ISSN 000 3-455X Helsinki 19 February 1992 © 1992 Finnish Zoological Publishing Board A new species of Machairodus from the late Miocene Kalmakpai locality in eastern Kazakhstan (USSR) M. V. Sotnikova Sotnikova, M. v., Geo logical Institute, USS R Academy ojSciences. Pysh evskii per. 7, 1090/7 Moscow, U.S.S.R. Received 20 August 1990, accepted November 1990 A new species, Machairodus kurt eni is described from the late Miocene locality Kalmakpai in eastern Kazakhstan (USSR). Other Vallesian and Turolian species of Ma chairodu s in the USSR are discussed. Evolutionary changes appear to have taken place in the genus Machairodus during the Turolian.In the morphology of the dentition, M. kurteni is intermediate between Ma chairodus and Homotherium . 1. Introduction the following mammal taxa: Vorm ela sp., Manes sp., Plesiogulo crassa Teilhard, Adcrocuta eximia The fossil locality of Kalmakpai (Fig. J) was (Roth & Wagner), Hyaenictitherium hyaenoides discovered by a geologist, B. A. Borisov in 1960. orlovi Semenov, Machairodus kurteni Sotnikova, It is located in the Zaisan depression, 160 km SE Hipparion hippidiodus Sefve, H. elegans Grornova, of the town Zaisan in Kazakhstan, USSR. The Chilot herium sp., Sin otherium zaisa nens is Karabulak suite on the right bank of the Kal Bayshashov, Cervavitus sp., Pro capreolus sp., makpai River is lithologically subdivided into Samotheriutn sp., Paleotrag us (Yuorlovia ) asia two parts: the upper, reddish-brown part, 30 m ticus Godina, Tragocerus sp., and Gazella dorca thick, and the lower, yellowish grey one, 29.4 m doides Schl.(Dmitrieva 1977, Zhegallo 1966, 1978, thick. -
Chapter 1 - Introduction
EURASIAN MIDDLE AND LATE MIOCENE HOMINOID PALEOBIOGEOGRAPHY AND THE GEOGRAPHIC ORIGINS OF THE HOMININAE by Mariam C. Nargolwalla A thesis submitted in conformity with the requirements for the degree of Doctor of Philosophy Graduate Department of Anthropology University of Toronto © Copyright by M. Nargolwalla (2009) Eurasian Middle and Late Miocene Hominoid Paleobiogeography and the Geographic Origins of the Homininae Mariam C. Nargolwalla Doctor of Philosophy Department of Anthropology University of Toronto 2009 Abstract The origin and diversification of great apes and humans is among the most researched and debated series of events in the evolutionary history of the Primates. A fundamental part of understanding these events involves reconstructing paleoenvironmental and paleogeographic patterns in the Eurasian Miocene; a time period and geographic expanse rich in evidence of lineage origins and dispersals of numerous mammalian lineages, including apes. Traditionally, the geographic origin of the African ape and human lineage is considered to have occurred in Africa, however, an alternative hypothesis favouring a Eurasian origin has been proposed. This hypothesis suggests that that after an initial dispersal from Africa to Eurasia at ~17Ma and subsequent radiation from Spain to China, fossil apes disperse back to Africa at least once and found the African ape and human lineage in the late Miocene. The purpose of this study is to test the Eurasian origin hypothesis through the analysis of spatial and temporal patterns of distribution, in situ evolution, interprovincial and intercontinental dispersals of Eurasian terrestrial mammals in response to environmental factors. Using the NOW and Paleobiology databases, together with data collected through survey and excavation of middle and late Miocene vertebrate localities in Hungary and Romania, taphonomic bias and sampling completeness of Eurasian faunas are assessed. -
O Ssakach Drapieżnych – Część 2 - Kotokształtne
PAN Muzeum Ziemi – O ssakach drapieżnych – część 2 - kotokształtne O ssakach drapieżnych - część 2 - kotokształtne W niniejszym artykule przyjrzymy się ewolucji i zróżnicowaniu zwierząt reprezentujących jedną z dwóch głównych gałęzi ewolucyjnych w obrębie drapieżnych (Carnivora). Na wczesnym etapie ewolucji, drapieżne podzieliły się (ryc. 1) na psokształtne (Caniformia) oraz kotokształtne (Feliformia). Paradoksalnie, w obydwu grupach występują (bądź występowały w przeszłości) formy, które bardziej przypominają psy, bądź bardziej przypominają koty. Ryc. 1. Uproszczone drzewo pokrewieństw ewolucyjnych współczesnych grup drapieżnych (Carnivora). Ryc. Michał Loba, na podstawie Nyakatura i Bininda-Emonds, 2012. Tym, co w rzeczywistości dzieli te dwie grupy na poziomie anatomicznym jest budowa komory ucha środkowego (bulla tympanica, łac.; ryc. 2). U drapieżnych komora ta jest budowa przede wszystkim przez dwie kości – tylną kaudalną kość entotympaniczną i kość ektotympaniczną. U kotokształtnych, w miejscu ich spotkania się ze sobą powstaje ciągła przegroda. Obydwie części komory kontaktują się ze sobą tylko za pośrednictwem małego okienka. U psokształtnych 1 PAN Muzeum Ziemi – O ssakach drapieżnych – część 2 - kotokształtne Ryc. 2. Widziane od spodu czaszki: A. baribala (Ursus americanus, Ursidae, Caniformia), B. żenety zwyczajnej (Genetta genetta, Viverridae, Feliformia). Strzałkami zaznaczono komorę ucha środkowego u niedźwiedzia i miejsce występowania przegrody w komorze żenety. Zdj. (A, B) Phil Myers, Animal Diversity Web (CC BY-NC-SA -
71St Annual Meeting Society of Vertebrate Paleontology Paris Las Vegas Las Vegas, Nevada, USA November 2 – 5, 2011 SESSION CONCURRENT SESSION CONCURRENT
ISSN 1937-2809 online Journal of Supplement to the November 2011 Vertebrate Paleontology Vertebrate Society of Vertebrate Paleontology Society of Vertebrate 71st Annual Meeting Paleontology Society of Vertebrate Las Vegas Paris Nevada, USA Las Vegas, November 2 – 5, 2011 Program and Abstracts Society of Vertebrate Paleontology 71st Annual Meeting Program and Abstracts COMMITTEE MEETING ROOM POSTER SESSION/ CONCURRENT CONCURRENT SESSION EXHIBITS SESSION COMMITTEE MEETING ROOMS AUCTION EVENT REGISTRATION, CONCURRENT MERCHANDISE SESSION LOUNGE, EDUCATION & OUTREACH SPEAKER READY COMMITTEE MEETING POSTER SESSION ROOM ROOM SOCIETY OF VERTEBRATE PALEONTOLOGY ABSTRACTS OF PAPERS SEVENTY-FIRST ANNUAL MEETING PARIS LAS VEGAS HOTEL LAS VEGAS, NV, USA NOVEMBER 2–5, 2011 HOST COMMITTEE Stephen Rowland, Co-Chair; Aubrey Bonde, Co-Chair; Joshua Bonde; David Elliott; Lee Hall; Jerry Harris; Andrew Milner; Eric Roberts EXECUTIVE COMMITTEE Philip Currie, President; Blaire Van Valkenburgh, Past President; Catherine Forster, Vice President; Christopher Bell, Secretary; Ted Vlamis, Treasurer; Julia Clarke, Member at Large; Kristina Curry Rogers, Member at Large; Lars Werdelin, Member at Large SYMPOSIUM CONVENORS Roger B.J. Benson, Richard J. Butler, Nadia B. Fröbisch, Hans C.E. Larsson, Mark A. Loewen, Philip D. Mannion, Jim I. Mead, Eric M. Roberts, Scott D. Sampson, Eric D. Scott, Kathleen Springer PROGRAM COMMITTEE Jonathan Bloch, Co-Chair; Anjali Goswami, Co-Chair; Jason Anderson; Paul Barrett; Brian Beatty; Kerin Claeson; Kristina Curry Rogers; Ted Daeschler; David Evans; David Fox; Nadia B. Fröbisch; Christian Kammerer; Johannes Müller; Emily Rayfield; William Sanders; Bruce Shockey; Mary Silcox; Michelle Stocker; Rebecca Terry November 2011—PROGRAM AND ABSTRACTS 1 Members and Friends of the Society of Vertebrate Paleontology, The Host Committee cordially welcomes you to the 71st Annual Meeting of the Society of Vertebrate Paleontology in Las Vegas. -
On the Socio-Sexual Behaviour of the Extinct Ursid Indarctos Arctoides: an Approach Based on Its Baculum Size and Morphology
View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by Digital.CSIC On the Socio-Sexual Behaviour of the Extinct Ursid Indarctos arctoides: An Approach Based on Its Baculum Size and Morphology Juan Abella1,2*, Alberto Valenciano3,4, Alejandro Pe´rez-Ramos5, Plinio Montoya6, Jorge Morales2 1 Institut Catala` de Paleontologia Miquel Crusafont, Universitat Auto`noma de Barcelona. Edifici ICP, Campus de la UAB s/n, Barcelona, Spain, 2 Museo Nacional de Ciencias Naturales-CSIC, Madrid, Spain, 3 Departamento de Geologı´a Sedimentaria y Cambio Medioambiental. Instituto de Geociencias (CSIC, UCM), Madrid, Spain, 4 Departamento de Paleontologı´a, Facultad de Ciencias Geolo´gicas UCM, Madrid, Spain, 5 Institut Cavanilles de Biodiversitat i Biologia Evolutiva, Universitat de Vale`ncia, Paterna, Spain, 6 Departament de Geologia, A` rea de Paleontologia, Universitat de Vale`ncia, Burjassot, Spain Abstract The fossil bacula, or os penis, constitutes a rare subject of study due to its scarcity in the fossil record. In the present paper we describe five bacula attributed to the bear Indarctos arctoides Depe´ret, 1895 from the Batallones-3 site (Madrid Basin, Spain). Both the length and morphology of this fossil bacula enabled us to make interpretative approaches to a series of ecological and ethological characters of this bear. Thus, we suggest that I. arctoides could have had prolonged periods of intromission and/or maintenance of intromission during the post-ejaculatory intervals, a multi-male mating system and large home range sizes and/or lower population density. Its size might also have helped females to choose from among the available males. -
A Contextual Review of the Carnivora of Kanapoi
A contextual review of the Carnivora of Kanapoi Lars Werdelin1* and Margaret E. Lewis2 1Department of Palaeobiology, Swedish Museum of Natural History, Box 50007, S-10405 Stockholm, Swe- den; [email protected] 2Biology Program, School of Natural Sciences and Mathematics, Stockton University, 101 Vera King Farris Drive, Galloway, NJ 08205, USA; [email protected] *Corresponding author Abstract The Early Pliocene is a crucial time period in carnivoran evolution. Holarctic carnivoran faunas suffered a turnover event at the Miocene-Pliocene boundary. This event is also observed in Africa but its onset is later and the process more drawn-out. Kanapoi is one of the earliest faunas in Africa to show evidence of a fauna that is more typical Pliocene than Miocene in character. The taxa recovered from Kanapoi are: Torolutra sp., Enhydriodon (2 species), Genetta sp., Helogale sp., Homotherium sp., Dinofelis petteri, Felis sp., and Par- ahyaena howelli. Analysis of the broader carnivoran context of which Kanapoi is an example shows that all these taxa are characteristic of Plio-Pleistocene African faunas, rather than Miocene ones. While some are still extant and some went extinct in the Early Pleistocene, Parahyaena howelli is unique in both originating and going extinct in the Early Pliocene. Keywords: Africa, Kenya, Miocene, Pliocene, Pleistocene, Carnivora Introduction Dehghani, 2011; Werdelin and Lewis, 2013a, b). In Kanapoi stands at a crossroads of carnivoran this contribution we will investigate this pattern and evolution. The Miocene –Pliocene boundary (5.33 its significance in detail. Ma: base of the Zanclean Stage; Gradstein et al., 2012) saw a global turnover among carnivores (e.g., Material and methods Werdelin and Turner, 1996). -
Basic Anatomy
Bone Clones® Pricelist 2014 2014 Retail Retail Product SKU# Product Description Prices Product SKU# Product Description Prices BASIC ANATOMY basic anatomy Skeletons: Adult Human Male Skeleton, Asian, Articulated, uses BC‐253 basic anatomy Skulls: Adult SC‐092‐A skull $2,350.00 BC‐016 Human Male Asian Skull and jaw $220.00 SC‐092‐D Human Male Skeleton, Asian, Disarticulated $1,400.00 BC‐031 Human Male Australian Aboriginal Skull $230.00 Human Male Half Skeleton, Asian, Disarticulated, uses BC‐ Human Male Australian Aboriginal Skull (Painted to SC‐092‐DH 212 calvarium‐cut skull $969.00 BC‐031‐P match original) $255.00 Human Female Skeleton, Asian, Articulated, uses BC‐211 BC‐059E Human Female Asian Skull, economy $135.00 SC‐211‐A skull $2,350.00 BC‐107 Human Male European Skull $220.00 SC‐211‐D Human Female Skeleton, Asian, Disarticulated $1,400.00 BC‐110 Human Male African Skull $220.00 Human Female Half Skeleton, Asian, Disarticulated, uses BC‐133 Human Female European Skull $220.00 SC‐211‐DH BC‐150‐ calvarium‐cut skull $969.00 BC‐149 Human Female Asian Skull $220.00 Human Male Asian Skeleton, Robust , Articulated, flexible BC‐178 Human Female African American Skull $230.00 SC‐287‐A uses BC‐287 skull $2,350.00 BC‐203 Human Male African‐American Skull $230.00 SC‐287‐D Human Male Asian Skeleton, Robust. Disarticulated $1,400.00 BC‐204 Human Male European, Elderly Skull $290.00 SC‐287‐DH Human Adult Male Half Skeleton, Disarticulated $990.00 BC‐211 Human Female Asian Skull $220.00 Human Male Asian Skeleton, Robust , Articulated, rigid in -
'Felis' Pamiri Ozansoy, 1959 (Carnivora, Felidae) from the Upper Miocene Of
1 Re-appraisal of 'Felis' pamiri Ozansoy, 1959 (Carnivora, Felidae) from the upper Miocene of 2 Turkey: the earliest pantherin cat? 3 4 Denis GERAADS and Stéphane PEIGNE 5 Centre de Recherche sur la Paléobiodiversité et les Paléoenvironnements (UMR 7207), Sorbonne 6 Universités, MNHN, CNRS, UPMC, CP 38, 8 rue Buffon, 75231 PARIS Cedex 05, France 7 8 Running head: 'Felis' pamiri from Turkey 9 10 Abstract 11 Although the divergence of the Panthera clade from other Felidae might be as old as the 12 earliest middle Miocene, its fossil record before the Pliocene is virtually non-existent. Here we 13 reassess the affinities of a felid from the early upper Miocene of Turkey, known by well-preserved 14 associated upper and lower dentitions. We conclude that it belongs to the same genus 15 (Miopanthera Kretzoi, 1938) as the middle Miocene 'Styriofelis' lorteti (Gaillard, 1899), and that 16 this genus is close to, if not part of, the Panthera clade. 17 18 Keywords: Carnivora – Felidae – Pantherini – Phylogeny – Upper Miocene – Turkey 19 20 Introduction 21 The Felidae can be divided in two subfamilies (Johnson et al. 2006; Werdelin et al. 2010) 22 Felinae (= Pantherinae, or big cats, plus Felinae, or smaller cats, in e.g., Wilson and Mittermeier 23 2009) and Machairodontinae, although their monophyly is hard to demonstrate, the second one 24 being extinct. The Neogene fossil record of the Machairodontinae, or saber-toothed felids, is 25 satisfactory, but that of other members of the family, conveniently called conical-toothed felids 26 (although several of them have compressed, flattened canines) is much more patchy. -
Endemism and Migration in the Kochkor Basin? Identification and Description of Adcrocuta Eximia (Mammalia: Carnivora: Hyaenidae) and C.F
Palaeontologia Electronica palaeo-electronica.org Endemism and migration in the Kochkor Basin? Identification and description of Adcrocuta eximia (Mammalia: Carnivora: Hyaenidae) and c.f. Paramachaerodus (Mammalia: Carnivora: Felidae) fossils at the Miocene locality of Ortok, Kyrgyzstan Sophie A. Miller, Paul Z. Barrett, Win N.F. McLaughlin, and Samantha S.B. Hopkins ABSTRACT Dentition from a Miocene hyaenid and a saber-toothed felid are described from the Chu Formation of Kyrgyzstan. Identified as Adcrocuta eximia (UOMNH F-70508) and c.f. Paramachaerodus (UOMNH F-70509), these represent one of the only formal- ized descriptions of fossil taxa from the Miocene in Kyrgyzstan. These specimens were recovered from the Ortok locality at the northwestern corner of the Kochkor Basin, the youngest of the known bone-bed localities in the Chu Formation. Using bio- and mag- netostratigraphy, the Chu Formation is attributed to the late Miocene to Pliocene, deposited approximately at 8 to 4 Ma. The Adcrocuta specimen consists of a partial dentary with condylar and angular processes, one upper, five lower teeth, and the par- tial root and alveoli of a fifth mandibular tooth. The c.f. Paramachaerodus specimen includes a partial M1, P4, and C1, and exhibits the features of the “scimitar-toothed” machairodontines. Preserved diagnostic characters place the Kyrgyz specimen closest to P. ogygia, although with certain features similar to that of P. transasiaticus, such as incipient crenulations on the canine. However, the age of the Kyrgyz specimen, approximately 6 Ma, is substantially younger than what is known for either of these taxa. We therefore hypothesize this Paramachaerodus specimen could be evidence of an endemic taxon in Kyrgyzstan from earlier migrating Asian species, potentially due to geological uplift with the Tien Shan Mountains.