Cursorial Adaptations in the Forelimb of the Giant Short-Faced Bear, <Em

Total Page:16

File Type:pdf, Size:1020Kb

Cursorial Adaptations in the Forelimb of the Giant Short-Faced Bear, <Em East Tennessee State University Digital Commons @ East Tennessee State University Electronic Theses and Dissertations Student Works 8-2012 Cursorial Adaptations in the Forelimb of the Giant Short-Faced Bear, Arctodus simus, Revealed by Traditional and 3D Landmark Morphometrics Eric Randally Lynch East Tennessee State University Follow this and additional works at: https://dc.etsu.edu/etd Part of the Paleobiology Commons Recommended Citation Lynch, Eric Randally, "Cursorial Adaptations in the Forelimb of the Giant Short-Faced Bear, Arctodus simus, Revealed by Traditional and 3D Landmark Morphometrics" (2012). Electronic Theses and Dissertations. Paper 1477. https://dc.etsu.edu/etd/1477 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]. Cursorial Adaptations in the Forelimb of the Giant Short-Faced Bear, Arctodus simus, Revealed by Traditional and 3D Landmark Morphometrics _________________________ A thesis presented to the faculty of the Department of Geosciences East Tennessee State University In partial fulfillment of the requirements for the degree Master of Science in Geosciences _________________________ by Eric R. Lynch August 2012 _________________________ Blaine W. Schubert, Chair Steven C. Wallace Jim I. Mead Keywords: Arctodus simus, Ursidae, geometric morphometrics, three-dimensional landmark, locomotion, posture ABSTRACT Cursorial Adaptations in the Forelimb of the Giant Short-Faced Bear, Arctodus simus, Revealed by Traditional and 3D Landmark Morphometrics by Eric R. Lynch The paleobiology of the Pleistocene North American giant short-faced bear, Arctodus simus, has eluded paleontologists for decades. Its more gracile form has led past researchers to myriad intepretations of the locomotion and feeding ecology of this species. While earlier studies have focused on craniodental morphology and simple postcranial indices, it is forelimb morphology that represents a direct compromise between locomotor and foraging behavior. The study here uses traditional and 3D landmark morphometrics to more completely compare the 3-dimensional shape of the major forelimb elements and their muscle attachment sites between A. simus, extant ursids, and other carnivorans. Results herein agree well with previous studies and provide additional evidence for reduced abductor/adductor and supinator/pronator musculature, more restricted parasagittal motion, increased stride length, and lighter and more packed distal elements. Forelimb skeletal morphology therefore supports the hypothesis that A. simmus represents a bear in the early stages of cursorial evolution. 2 DEDICATION This Master’s thesis is dedicated to my grandparents: Doris Lynch, Polly Marple, George Marple, Alfred Lynch, and Dale Lynch. Thank you for creating such a wonderful, loving family, for always encouraging me to follow my dreams, and for meeting me with understanding and open arms when I get the chance to come home. I picture your smiles every day. 3 ACKNOWLEDGEMENTS I am deeply grateful to Darrin Lunde (Division of Mammals, NMNH), Michael Brett- Surman and Fred Grady (Division of Paleobiology, NMNH), Eileen Westwig (AMNH), and Aisling Farrell (The George C. Page Museum, Los Angeles, CA) for access to specimens and assistance in collections as well as to Jim Mead and Sandy Swift for help in the ETSU collections and access to photography equipment. I thank Blaine Schubert, Steven Wallace, and Jim Mead for serving on my committee and for offering enthusiastic support and critical feedback and revisions on the written thesis. Anneke Van Heteren, Joshua Samuels, Blaire Van Valkenburgh, Xiaoming Wang, and Peter Dodson offered insightful discussions of concepts and methodologies. I happily thank Leigha King, David Moscato, Steven Jaskinski, and Sharon Holte for enlightening, encouraging, and mostly entertaining office room discussions, and Amanda Geisler, Kevin Chovanec, and Kyle Jansky for feedback and ideas in our weekly meetings with Blaine. I am grateful to Randy and Carol Lynch for offering me, Leigha, and our crazy dog a place to stay while visiting the AMNH and to Violeta Castro and Aaron Stolpen for lending me a couch to sleep on while visiting the Smithsonian. I am eternally thankful for the Interlibrary Loan program, particularly for Dan Heuer and the ILL Staff at Bucknell University, and all institutions that were involved in the procurement of particularly difficult-to-reach articles and dissertations that were essential to my research. I thank Enterprise for its always friendly customer service and quick and easy rent-a-car experience for my trip to Washington, D.C. Funding was made available through the Don Sundquist Center of Excellence in Paleontology and National Science Foundation GK-12 Fellowship. As always, I extend a heartfelt thank you to my parents, sister, and grandparents for supporting my research endeavors and welcoming me with open arms when I get the chance to come home. 4 CONTENTS Page ABSTRACT .................................................................................................................................... 2 DEDICATION ................................................................................................................................ 3 ACKNOWLEDGEMENTS ............................................................................................................ 4 LIST OF TABLES .......................................................................................................................... 9 LIST OF FIGURES ...................................................................................................................... 11 1. INTRODUCTION .................................................................................................................... 13 An Unresolved Debate ...................................................................................................... 14 A Fresh Attempt at Resolution ......................................................................................... 16 Phylogeny and Ecology of Comparative Species ............................................................. 18 2. MATERIALS AND METHODS .............................................................................................. 25 Specimens ......................................................................................................................... 25 Traditional Morphometrics ............................................................................................... 25 Geometric Morphometrics ................................................................................................ 42 Orientation of Specimens for Digital Photography .......................................................... 57 3. RESULTS ................................................................................................................................. 61 Scapula .............................................................................................................................. 61 Traditional Morphometrics – All Species ............................................................. 61 PCA ........................................................................................................... 61 StepDFA .................................................................................................... 64 PCA2 ......................................................................................................... 64 Taditional Morphometrics – Ursidae Only ........................................................... 66 PCA ........................................................................................................... 66 StepDFA .................................................................................................... 66 PCA2 ......................................................................................................... 68 Geometric Morphometrics – All Species .............................................................. 68 Humerus ............................................................................................................................ 69 Traditional Morphometrics – All Species ............................................................. 69 PCA ........................................................................................................... 69 5 StepDFA .................................................................................................... 74 PCA2 ......................................................................................................... 75 Traditional Morphometrics – Ursidae Only .......................................................... 75 PCA ........................................................................................................... 75 StepDFA .................................................................................................... 78 PCA2 ......................................................................................................... 78 Geometric Morphometrics – All Species .............................................................. 78 Ulna ..................................................................................................................................
Recommended publications
  • Selective Foraging on Bromeliads by Andean Bears in the Ecuadorian Pa´Ramo
    SHORT COMMUNICATION N DeMay et al. Selective foraging on bromeliads by Andean bears in the Ecuadorian pa´ramo Stephanie M. DeMay1,4, David A. Roon2, locating new resource sites, quality of known sites, Janet L. Rachlow2, and Rodrigo Cisneros3 avoiding predation, temporal variance in resource availability) at multiple scales (Compton et al. 2002, 1Environmental Science Program, University of Idaho, Fortin et al. 2003, Sergio et al. 2003, Bee et al. 2009). Moscow, ID 83844-3006, USA Optimal foraging theory predicts that the resultant 2Department of Fish and Wildlife Sciences, University of foraging patterns will be based on maximizing Idaho, Moscow, ID 83844-1136, USA energy uptake per unit of effort expended (Pyke et al. 3 Departamento de Ciencias Naturales, Universidad 1977, Hamilton and Bunnell 1987). Bailey at al. Te´cnica Particular de Loja, Loja, Ecuador (1996) described a spatial hierarchy for considering foraging behavior and the mechanisms that influence Abstract: The Andean bear (Tremarctos ornatus), decisions. The smallest scale is a bite of food, the only extant ursid in South America, lives in followed by feeding station, patch, feeding site, pa´ramo and montane forest ecosystems and is camp, and home range. Foraging decisions at each classified as vulnerable on the International Union scale have a wide range of ecological consequences, for Conservation of Nature Red List (Goldstein et from defining niche occupancy to affecting patterns al. 2008). In Podocarpus National Park in southern of competition and coexistence and constraining Ecuador, Andean bears exhibit patchy foraging adaptive potential. behavior on Puya eryngioides, a small terrestrial Foraging strategies are particularly interesting in bromeliad.
    [Show full text]
  • New Materials of Chalicotherium Brevirostris (Perissodactyla, Chalicotheriidae)
    Geobios 45 (2012) 369–376 Available online at www.sciencedirect.com Original article New materials of Chalicotherium brevirostris (Perissodactyla, Chalicotheriidae) § from the Tunggur Formation, Inner Mongolia Yan Liu *, Zhaoqun Zhang Laboratory of Evolutionary Systematics of Vertebrate, Institute of Vertebrate Paleontology and Paleoanthropology, Chinese Academy of Sciences, 142, Xizhimenwai Street, PO Box 643, Beijing 100044, PR China A R T I C L E I N F O A B S T R A C T Article history: Chalicotherium brevirostris was named by Colbert based on a skull lacking mandibles from the late Middle Received 23 March 2011 Miocene Tunggur Formation, Tunggur, Inner Mongolia, China. Here we describe new mandibular Accepted 6 October 2011 materials collected from the same area. In contrast to previous expectations, the new mandibular Available online 14 July 2012 materials show a long snout, long diastema, a three lower incisors and a canine. C. brevirostris shows some sexual dimorphism and intraspecific variation in morphologic characters. The new materials differ Keywords: from previously described C. cf. brevirostris from Cixian County (Hebei Province) and the Tsaidam Basin, Tunggur which may represent a different, new species close to C. brevirostris. The diagnosis of C. brevirostris is Middle Miocene revised. Chalicotheriinae Chalicotherium ß 2012 Elsevier Masson SAS. All rights reserved. 1. Abbreviations progress in understanding the Tunggur geology and paleontology (Qiu et al., 1988). The most important result of this expedition so far is
    [Show full text]
  • 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 .
    [Show full text]
  • 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.
    [Show full text]
  • 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.
    [Show full text]
  • A Bibliography of Klamath Mountains Geology, California and Oregon
    U.S. DEPARTMENT OF THE INTERIOR U.S. GEOLOGICAL SURVEY A bibliography of Klamath Mountains geology, California and Oregon, listing authors from Aalto to Zucca for the years 1849 to mid-1995 Compiled by William P. Irwin Menlo Park, California Open-File Report 95-558 1995 This report is preliminary and has not been reviewed for conformity with U.S. Geological Survey editorial standards (or with the North American Stratigraphic Code). Any use of trade, product, or firm names is for descriptive purposes only and does not imply endorsement by the U.S. Government. PREFACE This bibliography of Klamath Mountains geology was begun, although not in a systematic or comprehensive way, when, in 1953, I was assigned the task of preparing a report on the geology and mineral resources of the drainage basins of the Trinity, Klamath, and Eel Rivers in northwestern California. During the following 40 or more years, I maintained an active interest in the Klamath Mountains region and continued to collect bibliographic references to the various reports and maps of Klamath geology that came to my attention. When I retired in 1989 and became a Geologist Emeritus with the Geological Survey, I had a large amount of bibliographic material in my files. Believing that a comprehensive bibliography of a region is a valuable research tool, I have expended substantial effort to make this bibliography of the Klamath Mountains as complete as is reasonably feasible. My aim was to include all published reports and maps that pertain primarily to the Klamath Mountains, as well as all pertinent doctoral and master's theses.
    [Show full text]
  • Michael O. Woodburne1,* Alberto L. Cione2,**, and Eduardo P. Tonni2,***
    Woodburne, M.O.; Cione, A.L.; and Tonni, E.P., 2006, Central American provincialism and the 73 Great American Biotic Interchange, in Carranza-Castañeda, Óscar, and Lindsay, E.H., eds., Ad- vances in late Tertiary vertebrate paleontology in Mexico and the Great American Biotic In- terchange: Universidad Nacional Autónoma de México, Instituto de Geología and Centro de Geociencias, Publicación Especial 4, p. 73–101. CENTRAL AMERICAN PROVINCIALISM AND THE GREAT AMERICAN BIOTIC INTERCHANGE Michael O. Woodburne1,* Alberto L. Cione2,**, and Eduardo P. Tonni2,*** ABSTRACT The age and phyletic context of mammals that dispersed between North and South America during the past 9 m.y. is summarized. The presence of a Central American province of cladogenesis and faunal differentiation is explored. One apparent aspect of such a province is to delay dispersals of some taxa northward from Mexico into the continental United States, largely during the Blancan. Examples are recognized among the various xenar- thrans, and cervid artiodactyls. Whereas the concept of a Central American province has been mentioned in past investigations it is upgraded here. Paratoceras (protoceratid artio- dactyl) and rhynchotheriine proboscideans provide perhaps the most compelling examples of Central American cladogenesis (late Arikareean to early Barstovian and Hemphillian to Rancholabrean, respectively), but this category includes Hemphillian sigmodontine rodents, and perhaps a variety of carnivores and ungulates from Honduras in the medial Miocene, as well as peccaries and equids from Mexico. For South America, Mexican canids and hy- drochoerid rodents may have had an earlier development in Mexico. Remarkably, the first South American immigrants to Mexico (after the Miocene heralds; the xenarthrans Plaina and Glossotherium) apparently dispersed northward at the same time as the first Holarctic taxa dispersed to South America (sigmodontine rodents and the tayassuid artiodactyls).
    [Show full text]
  • 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.
    [Show full text]
  • 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.
    [Show full text]
  • 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
    [Show full text]
  • 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.
    [Show full text]
  • 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.
    [Show full text]