False Thumb” of Tremarctos Ornatus (Carnivora, Ursidae, Tremarctinae): Phylogenetic and Functional Implications
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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. -
Classification of Mammals 61
© Jones & Bartlett Learning, LLC © Jones & Bartlett Learning, LLC NOT FORCHAPTER SALE OR DISTRIBUTION NOT FOR SALE OR DISTRIBUTION Classification © Jones & Bartlett Learning, LLC © Jones & Bartlett Learning, LLC 4 NOT FORof SALE MammalsOR DISTRIBUTION NOT FOR SALE OR DISTRIBUTION © Jones & Bartlett Learning, LLC © Jones & Bartlett Learning, LLC NOT FOR SALE OR DISTRIBUTION NOT FOR SALE OR DISTRIBUTION © Jones & Bartlett Learning, LLC © Jones & Bartlett Learning, LLC NOT FOR SALE OR DISTRIBUTION NOT FOR SALE OR DISTRIBUTION © Jones & Bartlett Learning, LLC © Jones & Bartlett Learning, LLC NOT FOR SALE OR DISTRIBUTION NOT FOR SALE OR DISTRIBUTION © Jones & Bartlett Learning, LLC © Jones & Bartlett Learning, LLC NOT FOR SALE OR DISTRIBUTION NOT FOR SALE OR DISTRIBUTION © Jones & Bartlett Learning, LLC © Jones & Bartlett Learning, LLC NOT FOR SALE OR DISTRIBUTION NOT FOR SALE OR DISTRIBUTION © Jones & Bartlett Learning, LLC © Jones & Bartlett Learning, LLC NOT FOR SALE OR DISTRIBUTION NOT FOR SALE OR DISTRIBUTION © Jones & Bartlett Learning, LLC © Jones & Bartlett Learning, LLC NOT FOR SALE OR DISTRIBUTION NOT FOR SALE OR DISTRIBUTION © Jones & Bartlett Learning, LLC © Jones & Bartlett Learning, LLC NOT FOR SALE OR DISTRIBUTION NOT FOR SALE OR DISTRIBUTION © Jones & Bartlett Learning, LLC. NOT FOR SALE OR DISTRIBUTION. 2ND PAGES 9781284032093_CH04_0060.indd 60 8/28/13 12:08 PM CHAPTER 4: Classification of Mammals 61 © Jones Despite& Bartlett their Learning,remarkable success, LLC mammals are much less© Jones stress & onBartlett the taxonomic Learning, aspect LLCof mammalogy, but rather as diverse than are most invertebrate groups. This is probably an attempt to provide students with sufficient information NOT FOR SALE OR DISTRIBUTION NOT FORattributable SALE OR to theirDISTRIBUTION far greater individual size, to the high on the various kinds of mammals to make the subsequent energy requirements of endothermy, and thus to the inabil- discussions of mammalian biology meaningful. -
The Carnivora (Mammalia) from the Middle Miocene Locality of Gračanica (Bugojno Basin, Gornji Vakuf, Bosnia and Herzegovina)
Palaeobiodiversity and Palaeoenvironments https://doi.org/10.1007/s12549-018-0353-0 ORIGINAL PAPER The Carnivora (Mammalia) from the middle Miocene locality of Gračanica (Bugojno Basin, Gornji Vakuf, Bosnia and Herzegovina) Katharina Bastl1,2 & Doris Nagel2 & Michael Morlo3 & Ursula B. Göhlich4 Received: 23 March 2018 /Revised: 4 June 2018 /Accepted: 18 September 2018 # The Author(s) 2018 Abstract The Carnivora (Mammalia) yielded in the coal mine Gračanica in Bosnia and Herzegovina are composed of the caniform families Amphicyonidae (Amphicyon giganteus), Ursidae (Hemicyon goeriachensis, Ursavus brevirhinus) and Mustelidae (indet.) and the feliform family Percrocutidae (Percrocuta miocenica). The site is of middle Miocene age and the biostratigraphical interpretation based on molluscs indicates Langhium, correlating Mammal Zone MN 5. The carnivore faunal assemblage suggests a possible assignement to MN 6 defined by the late occurrence of A. giganteus and the early occurrence of H. goeriachensis and P. miocenica. Despite the scarcity of remains belonging to the order Carnivora, the fossils suggest a diverse fauna including omnivores, mesocarnivores and hypercarnivores of a meat/bone diet as well as Carnivora of small (Mustelidae indet.) to large size (A. giganteus). Faunal similarities can be found with Prebreza (Serbia), Mordoğan, Çandır, Paşalar and Inönü (all Turkey), which are of comparable age. The absence of Felidae is worthy of remark, but could be explained by the general scarcity of carnivoran fossils. Gračanica records the most eastern European occurrence of H. goeriachensis and the first occurrence of A. giganteus outside central Europe except for Namibia (Africa). The Gračanica Carnivora fauna is mostly composed of European elements. Keywords Amphicyon . Hemicyon . -
A Partial Short-Faced Bear Skeleton from an Ozark Cave with Comments on the Paleobiology of the Species
Blaine W. Schubert and James E. Kaufmann - A partial short-faced bear skeleton from an Ozark cave with comments on the paleobiology of the species. Journal of Cave and Karst Studies 65(2): 101-110. A PARTIAL SHORT-FACED BEAR SKELETON FROM AN OZARK CAVE WITH COMMENTS ON THE PALEOBIOLOGY OF THE SPECIES BLAINE W. SCHUBERT Environmental Dynamics, 113 Ozark Hall, University of Arkansas, Fayetteville, AR 72701, and Geology Section, Research and Collections, Illinois State Museum, Springfield, IL 62703 USA JAMES E. KAUFMANN Department of Geology and Geophysics, University of Missouri-Rolla, Rolla, MO 65409 USA Portions of an extinct giant short-faced bear, Arctodus simus, were recovered from a remote area with- in an Ozark cave, herein named Big Bear Cave. The partially articulated skeleton was found in banded silt and clay sediments near a small entrenched stream. The sediment covered and preserved skeletal ele- ments of low vertical relief (e.g., feet) in articulation. Examination of a thin layer of manganese and clay under and adjacent to some skeletal remains revealed fossilized hair. The manganese in this layer is con- sidered to be a by-product of microorganisms feeding on the bear carcass. Although the skeleton was incomplete, the recovered material represents one of the more complete skeletons for this species. The stage of epiphyseal fusion in the skeleton indicates an osteologically immature individual. The specimen is considered to be a female because measurements of teeth and fused postcranial elements lie at the small end of the size range for A. simus. Like all other bears, the giant short-faced bear is sexually dimorphic. -
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. -
Cranial Morphological Distinctiveness Between Ursus Arctos and U
East Tennessee State University Digital Commons @ East Tennessee State University Electronic Theses and Dissertations Student Works 5-2017 Cranial Morphological Distinctiveness Between Ursus arctos and U. americanus Benjamin James Hillesheim East Tennessee State University Follow this and additional works at: https://dc.etsu.edu/etd Part of the Biodiversity Commons, Evolution Commons, and the Paleontology Commons Recommended Citation Hillesheim, Benjamin James, "Cranial Morphological Distinctiveness Between Ursus arctos and U. americanus" (2017). Electronic Theses and Dissertations. Paper 3261. https://dc.etsu.edu/etd/3261 This Thesis - Open Access is brought to you for free and open access by the Student Works at Digital Commons @ East Tennessee State University. It has been accepted for inclusion in Electronic Theses and Dissertations by an authorized administrator of Digital Commons @ East Tennessee State University. For more information, please contact [email protected]. Cranial Morphological Distinctiveness Between Ursus arctos and U. americanus ____________________________________ A thesis presented to the Department of Geosciences East Tennessee State University In partial fulfillment of the requirements for the degree Master of Science in Geosciences ____________________________________ by Benjamin Hillesheim May 2017 ____________________________________ Dr. Blaine W. Schubert, Chair Dr. Steven C. Wallace Dr. Josh X. Samuels Keywords: Ursidae, Geometric morphometrics, Ursus americanus, Ursus arctos, Last Glacial Maximum ABSTRACT Cranial Morphological Distinctiveness Between Ursus arctos and U. americanus by Benjamin J. Hillesheim Despite being separated by millions of years of evolution, black bears (Ursus americanus) and brown bears (Ursus arctos) can be difficult to distinguish based on skeletal and dental material alone. Complicating matters, some Late Pleistocene U. americanus are significantly larger in size than their modern relatives, obscuring the identification of the two bears. -
What Size Were Arctodus Simus and Ursus Spelaeus (Carnivora: Ursidae)?
Ann. Zool. Fennici 36: 93–102 ISSN 0003-455X Helsinki 15 June 1999 © Finnish Zoological and Botanical Publishing Board 1999 What size were Arctodus simus and Ursus spelaeus (Carnivora: Ursidae)? Per Christiansen Christiansen, P., Zoological Museum, Department of Vertebrates, Universitetsparken 15, DK-2100 København Ø, Denmark Received 23 October 1998, accepted 10 February 1999 Christiansen, P. 1999: What size were Arctodus simus and Ursus spelaeus (Carnivora: Ursidae)? — Ann. Zool. Fennici 36: 93–102. Body masses of the giant short-faced bear (Arctodus simus Cope) and the cave bear (Ursus spelaeus Rosenmüller & Heinroth) were calculated with equations based on a long-bone dimensions:body mass proportion ratio in extant carnivores. Despite its more long-limbed, gracile and felid-like anatomy as compared with large extant ursids, large Arctodus specimens considerably exceeded even the largest extant ursids in mass. Large males weighed around 700–800 kg, and on rare occasions may have approached, or even exceeded one tonne. Ursus spelaeus is comparable in size to the largest extant ursids; large males weighed 400–500 kg, females 225–250 kg. Suggestions that large cave bears could reach weights of one tonne are not supported. 1. Introduction thera atrox) (Anyonge 1993), appear to have equalled the largest ursids in size. The giant short-faced bear (Arctodus simus Cope, Extant ursids vary markedly in size from the Ursidae: Tremarctinae) from North America, and small, partly arboreal Malayan sunbear (Ursus ma- the cave bear (Ursus spelaeus Rosenmüller & layanus), which reaches a body mass of only 27– Heinroth, Ursidae: Ursinae) from Europe were 65 kg (Nowak 1991), to the Kodiak bear (U. -
Wiszniowska T Autor Structure.Pdf
MORPHOLOGY AND SY S TE M ATIC S OF FO ss IL VERTEBRATE S I II Morphology and Systematics of Fossil Vertebrates Edited by Dariusz Nowakowski DN Publisher Wrocław - Poland 2010 III Morphology and Systematics of Fossil Vertebrates Edited by Dariusz Nowakowski Krzysztof Borysławski, Stanislav Čermak, Michał Ginter, Michael Hansen, Piotr Jadwiszczak, Katarzyna Anna Lech, Paweł Mackiewicz, Adam Nadachowski, Robert Niedźwiedzki, Dariusz Nowakowski, Anthony J. Olejniczak, Tomasz Płoszaj, Leonid Rekovets, Piotr Skrzycki, Dawid Surmik, Paweł Socha, Krzysztof Stefaniak, Jacek Tomczyk, Zuzanna Wawrzyniak, Teresa Wiszniowska, Henryk W. Witas Reviewers: Alexander Averianov (Russia) Paweł Bergman (Poland) Nina G. Bogutskaya (Russia) Ivan Horáček (Czech Republic) Grzegorz Kopij (Poland) Barbara Kosowska (Poland) Lutz Maul (Germany) Kenshu Shimada (USA) ©DN Publisher Wrocław - Poland ISBN 987-83-928020-1-3 First edition Circulation 150 copies 2010 IV Contents Preface 1 An application of computed tomography in studies of human remains (for example Egyptian mummy) 3 The Late Miocene and Pliocene Ochotoninae (Lagomorpha, Mammalia) of Europe – the present state of knowledge 9 Teeth of the cladodont shark Denaea from the Carboniferous of central 29 North America New data on the appendicular skeleton and diversity of Eocene Antarctic penguins 45 Reconstruction of forelimb movement of Cyclotosaurus intermedius Sulej et Majer, 2005 from Late Triassic of Poland 52 Analysis of dental enamel thickness in bears with special attention to Ursus spelaeus and U. wenzensis -
International Bear News
International Bear News Quarterly Newsletter of the International Association for Bear Research and Management (IBA) and the IUCN/SSC Bear Specialist Group Spring 2013 Vol. 22 no. 1 Ms. Jayanthi Natarajan (front row center), Union Minister for Environment and Forests, Government of India, opened the 21st IBA Conference in New Delhi, India that was attended by 373 delegates from 35 nations. Read more about the conference proceedings on page 21. IBA website: www.bearbiology.org Table of Contents IBA Student Forum 3 International Bear News, ISSN #1064-1564 29 Truman’s List Serve Council News Eurasia 4 From the President 30 News From Project “Rehabilitation, Release 6 Research and Conservation Grants and Behavioral/Ecology Research of Asiatic black (Ursus thibetanus) and Brown Bears (Ursus arctos) in Sikhote-Alin (Russian Far Bear Specialist Group East) 7 New Chairs Selected for Bear Specialist 31 A Novel Interaction Between a Sun Bear Group Expert Teams and Pangolin in the Wild 11 Bear Specialist Group Coordinating 32 Climate Change – No Thanks: German Committee (2013) Kids are Concerned About Polar Bears 12 Expert Teams of Bear Specialist Group 34 M13 and the Fate of Bears in Switzerland: Report on Projects A Short Note 16 New Co-Chair of Sloth Bear Expert Team Models BSG T-shirts with Students 17 Vietnam Bear Rescue Centre Prevails Americas against Eviction Challenge 35 Using Landscape-Scale Habitat Suitability 18 Irma: The “Swimmer” Brown Bear of Modeling to Identify Recovery Areas Kastoria Lake, Greece for the Louisiana Black Bear (Ursus -
University of Florida Thesis Or Dissertation Formatting
UNDERSTANDING CARNIVORAN ECOMORPHOLOGY THROUGH DEEP TIME, WITH A CASE STUDY DURING THE CAT-GAP OF FLORIDA By SHARON ELIZABETH HOLTE A DISSERTATION PRESENTED TO THE GRADUATE SCHOOL OF THE UNIVERSITY OF FLORIDA IN PARTIAL FULFILLMENT OF THE REQUIREMENTS FOR THE DEGREE OF DOCTOR OF PHILOSOPHY UNIVERSITY OF FLORIDA 2018 © 2018 Sharon Elizabeth Holte To Dr. Larry, thank you ACKNOWLEDGMENTS I would like to thank my family for encouraging me to pursue my interests. They have always believed in me and never doubted that I would reach my goals. I am eternally grateful to my mentors, Dr. Jim Mead and the late Dr. Larry Agenbroad, who have shaped me as a paleontologist and have provided me to the strength and knowledge to continue to grow as a scientist. I would like to thank my colleagues from the Florida Museum of Natural History who provided insight and open discussion on my research. In particular, I would like to thank Dr. Aldo Rincon for his help in researching procyonids. I am so grateful to Dr. Anne-Claire Fabre; without her understanding of R and knowledge of 3D morphometrics this project would have been an immense struggle. I would also to thank Rachel Short for the late-night work sessions and discussions. I am extremely grateful to my advisor Dr. David Steadman for his comments, feedback, and guidance through my time here at the University of Florida. I also thank my committee, Dr. Bruce MacFadden, Dr. Jon Bloch, Dr. Elizabeth Screaton, for their feedback and encouragement. I am grateful to the geosciences department at East Tennessee State University, the American Museum of Natural History, and the Museum of Comparative Zoology at Harvard for the loans of specimens. -
Giant Panda Facts (Ailuropoda Melanoleuca)
U.S. Fish & Wildlife Service Giant Panda Facts (Ailuropoda melanoleuca) Giant panda. John J. Mosesso What animal is black and white Giant pandas are bears with one or two cubs weighing 3 to 5 and loved all over the world? If you striking black and white markings. ounces each is born in a sheltered guessed the giant panda, you’re The ears, eye patches, legs and den. Usually only one cub survives. right! shoulder band are black; the rest The eyes open at 1 1/2 to 2 months of the body is whitish. They have and the cub becomes mobile at The giant panda is also known as thick, woolly coats to insulate them approximately three months of the panda bear, bamboo bear, or in from the cold. Adults are four to six age. At 12 months the cub becomes Chinese as Daxiongmao, the “large feet long and may weigh up to 350 totally independent. While their bear cat.” In fact, its scientific pounds—about the same size as average life span in the wild is name means “black and white cat- the American black bear. However, about 15 years, giant pandas in footed animal.” unlike the black bear, giant pandas captivity have been known to live do not hibernate and cannot walk well into their twenties. Giant pandas are found only in on their hind legs. the mountains of central China— Scientists have debated for more in small isolated areas of the The giant panda has unique front than a century whether giant north and central portions of the paws—one of the wrist bones is pandas belong to the bear family, Sichuan Province, in the mountains enlarged and elongated and is used the raccoon family, or a separate bordering the southernmost part of like a thumb, enabling the giant family of their own. -
Faced Bear, Arctotherium, from the Pleistocene of California
I. RELATIONSHIPS AND STRUCTURE OF THE SHORT~ FACED BEAR, ARCTOTHERIUM, FROM THE PLEISTOCENE OF CALIFORNIA. By JOHN C. MERRIAM and CHESTER STOCK. With ten plates and five text-figures. 1 CONTENTS. PAGE Introduct-ion. 3 Systematic position of Arctotherium and its allies with relation to the typical Ursidae. 4 Origin of the Tremarctinae. 5 Summary of species of Arctotherium in the Pleistocene of North America. 7 Occurrence in California of arctotheres and associated faunas . 9 Potter Creek Cave. 9 Rancho La Brea. 10 McKittrick. .......... .... .......... ....... ...... ................. 11 Odontolo~Y. and osteology of Arctotherium. 11 DentitiOn . 11 Axial skeleton. 16 Appendicular skeleton. 21 Bibliography . 34 2 RELATIONSHIPS AND STRUCTURE OF THE SHORT-FACED BEAR, ARCTOTHERIUM, FROM THE PLEISTOCENE OF CALIFORNIA. BY JoHN C . MERRIAM AND CHESTER STocK. INTRODUCTION. The peculiar short-faced Californian bear, known as Arctotherium simum, was described by Cope in 1879 from a single specimen, con sisting of a skull minus the lower jaw, found by J. A. Richardson in 1878 in Potter Creek Cave on the McCloud River in northern California. Since the description of A. simum, a nearly perfect skull with lower jaw and a large quantity of additional material, representing nearly all parts of the skeleton and dentition of this species, has been obtained from the deposits of Potter Creek Cave as a result of further work carried on for the University of California by E. L. Furlong and by W. J. Sinclair in 1902 and 1903. Splendid material of Arctotherium has also been secured in the Pleistocene asphalt beds at Rancho La Brea by the Los Angeles Museum of History, Science, and Art.