1 Supplemental Material for Matzke and Wright (2016), “Inferring Node
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The Impact of Large Terrestrial Carnivores on Pleistocene Ecosystems Blaire Van Valkenburgh, Matthew W
The impact of large terrestrial carnivores on SPECIAL FEATURE Pleistocene ecosystems Blaire Van Valkenburgha,1, Matthew W. Haywardb,c,d, William J. Ripplee, Carlo Melorof, and V. Louise Rothg aDepartment of Ecology and Evolutionary Biology, University of California, Los Angeles, CA 90095; bCollege of Natural Sciences, Bangor University, Bangor, Gwynedd LL57 2UW, United Kingdom; cCentre for African Conservation Ecology, Nelson Mandela Metropolitan University, Port Elizabeth, South Africa; dCentre for Wildlife Management, University of Pretoria, Pretoria, South Africa; eTrophic Cascades Program, Department of Forest Ecosystems and Society, Oregon State University, Corvallis, OR 97331; fResearch Centre in Evolutionary Anthropology and Palaeoecology, School of Natural Sciences and Psychology, Liverpool John Moores University, Liverpool L3 3AF, United Kingdom; and gDepartment of Biology, Duke University, Durham, NC 27708-0338 Edited by Yadvinder Malhi, Oxford University, Oxford, United Kingdom, and accepted by the Editorial Board August 6, 2015 (received for review February 28, 2015) Large mammalian terrestrial herbivores, such as elephants, have analogs, making their prey preferences a matter of inference, dramatic effects on the ecosystems they inhabit and at high rather than observation. population densities their environmental impacts can be devas- In this article, we estimate the predatory impact of large (>21 tating. Pleistocene terrestrial ecosystems included a much greater kg, ref. 11) Pleistocene carnivores using a variety of data from diversity of megaherbivores (e.g., mammoths, mastodons, giant the fossil record, including species richness within guilds, pop- ground sloths) and thus a greater potential for widespread habitat ulation density inferences based on tooth wear, and dietary in- degradation if population sizes were not limited. -
Shape Evolution and Sexual Dimorphism in the Mandible of the Dire Wolf, Canis Dirus, at Rancho La Brea Alexandria L
Marshall University Marshall Digital Scholar Theses, Dissertations and Capstones 2014 Shape evolution and sexual dimorphism in the mandible of the dire wolf, Canis Dirus, at Rancho la Brea Alexandria L. Brannick [email protected] Follow this and additional works at: http://mds.marshall.edu/etd Part of the Animal Sciences Commons, and the Paleontology Commons Recommended Citation Brannick, Alexandria L., "Shape evolution and sexual dimorphism in the mandible of the dire wolf, Canis Dirus, at Rancho la Brea" (2014). Theses, Dissertations and Capstones. Paper 804. This Thesis is brought to you for free and open access by Marshall Digital Scholar. It has been accepted for inclusion in Theses, Dissertations and Capstones by an authorized administrator of Marshall Digital Scholar. For more information, please contact [email protected]. SHAPE EVOLUTION AND SEXUAL DIMORPHISM IN THE MANDIBLE OF THE DIRE WOLF, CANIS DIRUS, AT RANCHO LA BREA A thesis submitted to the Graduate College of Marshall University In partial fulfillment of the requirements for the degree of Master of Science in Biological Sciences by Alexandria L. Brannick Approved by Dr. F. Robin O’Keefe, Committee Chairperson Dr. Julie Meachen Dr. Paul Constantino Marshall University May 2014 ©2014 Alexandria L. Brannick ALL RIGHTS RESERVED ii ACKNOWLEDGEMENTS I thank my advisor, Dr. F. Robin O’Keefe, for all of his help with this project, the many scientific opportunities he has given me, and his guidance throughout my graduate education. I thank Dr. Julie Meachen for her help with collecting data from the Page Museum, her insight and advice, as well as her support. I learned so much from Dr. -
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. -
Entre Chien Et Loup
ANNEE 2003 THESE : 2003 – TOU 3 – 4102 ENTRE CHIEN ET LOUP : ETUDE BIOLOGIQUE ET COMPORTEMENTALE _________________ THESE pour obtenir le grade de DOCTEUR VETERINAIRE DIPLOME D’ETAT présentée et soutenue publiquement en 2003 devant l’Université Paul-Sabatier de Toulouse par Laurent, Sylvain, Patrice NEAULT Né, le 7 janvier 1976 à BELFORT (Territoire de Belfort) ___________ Directeur de thèse : M. le Professeur Roland DARRE ___________ JURY PRESIDENT : M. Henri DABERNAT Professeur à l’Université Paul-Sabatier de TOULOUSE ASSESSEUR : M. Roland DARRE Professeur à l’Ecole Nationale Vétérinaire de TOULOUSE M. Guy BODIN Professeur à l’Ecole Nationale Vétérinaire de TOULOUSE MINISTERE DE L'AGRICULTURE ET DE LA PECHE ECOLE NATIONALE VETERINAIRE DE TOULOUSE Directeur : M. P. DESNOYERS Directeurs honoraires……. : M. R. FLORIO M. J. FERNEY M. G. VAN HAVERBEKE Professeurs honoraires….. : M. A. BRIZARD M. L. FALIU M. C. LABIE M. C. PAVAUX M. F. LESCURE M. A. RICO M. A. CAZIEUX Mme V. BURGAT M. D. GRIESS PROFESSEURS CLASSE EXCEPTIONNELLE M. CABANIE Paul, Histologie, Anatomie pathologique M. CHANTAL Jean, Pathologie infectieuse M. DARRE Roland, Productions animales M. DORCHIES Philippe, Parasitologie et Maladies Parasitaires M. GUELFI Jean-François, Pathologie médicale des Equidés et Carnivores M. TOUTAIN Pierre-Louis, Physiologie et Thérapeutique PROFESSEURS 1ère CLASSE M. AUTEFAGE André, Pathologie chirurgicale M. BODIN ROZAT DE MANDRES NEGRE Guy, Pathologie générale, Microbiologie, Immunologie M. BRAUN Jean-Pierre, Physique et Chimie biologiques et médicales M. DELVERDIER Maxence, Histologie, Anatomie pathologique M. EECKHOUTTE Michel, Hygiène et Industrie des Denrées Alimentaires d'Origine Animale M. EUZEBY Jean, Pathologie générale, Microbiologie, Immunologie M. FRANC Michel, Parasitologie et Maladies Parasitaires M. -
Coyote Canis Latrans in 2007 IUCN Red List (Canis Latrans)
MAMMALS OF MISSISSIPPI 10:1–9 Coyote (Canis latrans) CHRISTOPHER L. MAGEE Department of Wildlife and Fisheries, Mississippi State University, Mississippi State, Mississippi, 39762, USA Abstract—Canis latrans (Say 1823) is a canid commonly called the coyote. It is dog-like in appearance with varied colorations throughout its range. Originally restricted to the western portion of North America, coyotes have expanded across the majority of the continent. Coyotes are omnivorous and extremely adaptable, often populating urban and suburban environments. Preferred habitats include a mixture of forested, open, and brushy areas. Currently, there exist no threats or conservation concerns for the coyote in any part of its range. This species is currently experiencing an increasing population trend. Published 5 December 2008 by the Department of Wildlife and Fisheries, Mississippi State University Coyote location (Jackson 1951; Young 1951; Berg and Canis latrans (Say, 1823) Chesness 1978; Way 2007). The species is sexually dimorphic, with adult females distinctly CONTEXT AND CONTENT. lighter and smaller than adult males (Kennedy Order Carnivora, suborder Caniformia, et al. 2003; Way 2007). Average head and infraorder Cynoidea, family Canidae, subfamily body lengths are about 1.0–1.5 m with a tail Caninae, tribe Canini. Genus Canis consists length of about Young 1951). The skull of the of six species: C. aureus, C. latrans, C. lupus, coyote (Fig. 2) progresses through 6 distinct C. mesomelas, C. simensis, and C. adustus. developmental stages allowing delineation Canis latrans has 19 recognized subspecies between the age classes of juvenile, immature, (Wilson and Reeder 2005). young, young adult, adult, and old adult (Jackson 1951). -
Estrategias De Subsistencia De Los Primeros Grupos Humanos Que Poblaron Europa
ESTRATEGIAS DE SUBSISTENCIA DE LOS PRIMEROS GRUPOS HUMANOS QUE POBLARON EUROPA ESTRATEGIAS DE SUBSISTENCIA DE LOS PRIMEROS GRUPOS HUMANOS QUE POBLARON EUROPA: EVIDENCIAS CONSERVADAS EN BARRANCO LEÓN Y FUENTE NUEVA-3 (ORCE) M. PATROCINIO ESPIGARES* RESUMEN Varios yacimientos del Pleistoceno inferior de España, Francia e Italia preservan las evidencias de presencia humana más antiguas de Europa. En este contexto, son particularmente interesantes dos localidades ubicadas en las inmediaciones de la villa de Orce (Cuenca de Baza, Granada), Barranco León (BL) y Fuente Nueva-3 (FN-3), datadas en torno a 1,4 Ma. En estos yacimientos se han identificado evidencias de procesado de cadáveres de grandes mamíferos, realizado con herra- mientas líticas de factura Olduvayense. A estos hallazgos hay que sumarle la presencia de un diente de leche atribuido a Homo sp. en Barranco León. En este trabajo se describen en detalle las marcas de origen antrópico localizadas en estos yacimientos, se analizan los patrones de procesado de los cadáveres, y se discute sobre las estrategias de subsistencia de las primeras comunidades humanas que habitaron Europa. Palabras clave: Marcas de corte, Estrategias de subsistencia, Pleistoceno Inferior, Homo sp. ABSTRACT Several Early Pleistocene sites from Spain, France and Italy preserve ancient evidence of human presence. In this context are particularly interesting two localities placed near the town of Orce (Baza Basin, Granada), Barranco León (BL) and Fuente Nueva-3 (FN-3), dated to ~1.4 Ma. At these sites, evidence of processing of large mammal carcasses produced with Oldowan tools have been recovered. These findings are accompanied by the presence of a deciduous tooth, attributed to Homo sp., in Barranco León. -
Guidebook Contains Preliminary Findings of a Number of Concurrent Projects Being Worked on by the Trip Leaders
TH FRIENDS OF THE PLEISTOCENE, ROCKY MOUNTAIN-CELL, 45 FIELD CONFERENCE PLIO-PLEISTOCENE STRATIGRAPHY AND GEOMORPHOLOGY OF THE CENTRAL PART OF THE ALBUQUERQUE BASIN OCTOBER 12-14, 2001 SEAN D. CONNELL New Mexico Bureau of Geology and Mineral Resources-Albuquerque Office, New Mexico Institute of Mining and Technology, 2808 Central Ave. SE, Albuquerque, New Mexico 87106 DAVID W. LOVE New Mexico Bureau of Geology and Mineral Resources, New Mexico Institute of Mining and Technology, 801 Leroy Place, Socorro, NM 87801 JOHN D. SORRELL Tribal Hydrologist, Pueblo of Isleta, P.O. Box 1270, Isleta, NM 87022 J. BRUCE J. HARRISON Dept. of Earth and Environmental Sciences, New Mexico Institute of Mining and Technology 801 Leroy Place, Socorro, NM 87801 Open-File Report 454C and D Initial Release: October 11, 2001 New Mexico Bureau of Geology and Mineral Resources New Mexico Institute of Mining and Technology 801 Leroy Place, Socorro, NM 87801 NMBGMR OFR454 C & D INTRODUCTION This field-guide accompanies the 45th annual Rocky Mountain Cell of the Friends of the Pleistocene (FOP), held at Isleta Lakes, New Mexico. The Friends of the Pleistocene is an informal gathering of Quaternary geologists, geomorphologists, and pedologists who meet annually in the field. The field guide has been separated into two parts. Part C (open-file report 454C) contains the three-days of road logs and stop descriptions. Part D (open-file report 454D) contains a collection of mini-papers relevant to field-trip stops. This field guide is a companion to open-file report 454A and 454B, which accompanied a field trip for the annual meeting of the Rocky Mountain/South Central Section of the Geological Society of America, held in Albuquerque in late April. -
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. -
Rodentia, Mammalia) in Europe'
Resumen EI yacimiento de Trinchera Oolina es uno de los mas importantes de la Sierra de Atapuerca par su contenido en restos humanos, Homo antecessor en el nivel de Trinchera Dolina 6. Ade mas de esto la enorme riqueza en restos arqueol6gicos y paleontol6gicos hace de Trinchera Dolina un yacimiento unico, de referencia obligada para el Pleistoceno y Paleolitico de Euro pa. Bioestratigraficamente, el yacimiento de Trinchera Oolina (TO) puede dividirse en tres grandes unidades: la que comprende los niveles TD3 a T06; la de los niveles T07 a TOS infe rior y I. de TO 8 superior. T011. Palabras clave: Mamiferos, Pleistoceno. Abstract Gran Dolina is one of the Pleistocene sites located at the Sierra de Atapuerca (Spain). The Gran Dolina deposits belong to different chronological periods of the Early and Middle Pleistocene. The uppermost levels of Gran Dolina (TDII, TDIO and TD8b) contain Middle Pleistocene (post-Cromerian) macro- and micromammal assemblages. The excavation works have overpassed level TDII and have not concluded yet at TDIO: TDII is poor in macromammal remains (carnivores and herbivores) but rich in rodents. The macromammals fossil material from TDtt is very scarce and this enables (for the macromammals) definite conclusions about the chronology and type of community of these levels. The lowermost levels of Gran Dolina (TD3/4, TD5, TD6 and TD8a) contain a different mammal assemblage with typical late Early Pleistocene-Cromerian species. This radical substitution of taxa is placed at TD8 layer probably due to a stratigraphic gap in this level. The level TD6 of the Gran Dolina site contains the earliest fossil human remains of Europe, Homo antecessor, and it has also a rich and diverse micromammal assemblage. -
La Brea and Beyond: the Paleontology of Asphalt-Preserved Biotas
La Brea and Beyond: The Paleontology of Asphalt-Preserved Biotas Edited by John M. Harris Natural History Museum of Los Angeles County Science Series 42 September 15, 2015 Cover Illustration: Pit 91 in 1915 An asphaltic bone mass in Pit 91 was discovered and exposed by the Los Angeles County Museum of History, Science and Art in the summer of 1915. The Los Angeles County Museum of Natural History resumed excavation at this site in 1969. Retrieval of the “microfossils” from the asphaltic matrix has yielded a wealth of insect, mollusk, and plant remains, more than doubling the number of species recovered by earlier excavations. Today, the current excavation site is 900 square feet in extent, yielding fossils that range in age from about 15,000 to about 42,000 radiocarbon years. Natural History Museum of Los Angeles County Archives, RLB 347. LA BREA AND BEYOND: THE PALEONTOLOGY OF ASPHALT-PRESERVED BIOTAS Edited By John M. Harris NO. 42 SCIENCE SERIES NATURAL HISTORY MUSEUM OF LOS ANGELES COUNTY SCIENTIFIC PUBLICATIONS COMMITTEE Luis M. Chiappe, Vice President for Research and Collections John M. Harris, Committee Chairman Joel W. Martin Gregory Pauly Christine Thacker Xiaoming Wang K. Victoria Brown, Managing Editor Go Online to www.nhm.org/scholarlypublications for open access to volumes of Science Series and Contributions in Science. Natural History Museum of Los Angeles County Los Angeles, California 90007 ISSN 1-891276-27-1 Published on September 15, 2015 Printed at Allen Press, Inc., Lawrence, Kansas PREFACE Rancho La Brea was a Mexican land grant Basin during the Late Pleistocene—sagebrush located to the west of El Pueblo de Nuestra scrub dotted with groves of oak and juniper with Sen˜ora la Reina de los A´ ngeles del Rı´ode riparian woodland along the major stream courses Porciu´ncula, now better known as downtown and with chaparral vegetation on the surrounding Los Angeles. -
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1.08 1.19 1.46 Nimravus brachyops Nandinia binotata Neofelis nebulosa 115 Panthera onca 111 114 Panthera atrox 113 Uncia uncia 116 Panthera leo 112 Panthera pardus Panthera tigris Lynx issiodorensis 220 Lynx rufus 221 Lynx pardinus 222 223 Lynx canadensis Lynx lynx 119 Acinonyx jubatus 110 225 226 Puma concolor Puma yagouaroundi 224 Felis nigripes 228 Felis chaus 229 Felis margarita 118 330 227 331Felis catus Felis silvestris 332 Otocolobus manul Prionailurus bengalensis Felis rexroadensis 99 117 334 335 Leopardus pardalis 44 333 Leopardus wiedii 336 Leopardus geoffroyi Leopardus tigrinus 337 Pardofelis marmorata Pardofelis temminckii 440 Pseudaelurus intrepidus Pseudaelurus stouti 88 339 Nimravides pedionomus 442 443 Nimravides galiani 22 338 441 Nimravides thinobates Pseudaelurus marshi Pseudaelurus validus 446 Machairodus alberdiae 77 Machairodus coloradensis 445 Homotherium serum 447 444 448 Smilodon fatalis Smilodon gracilis 66 Pseudaelurus quadridentatus Barbourofelis morrisi 449 Barbourofelis whitfordi 550 551 Barbourofelis fricki Barbourofelis loveorum Stenogale Hemigalus derbyanus 554 555 Arctictis binturong 55 Paradoxurus hermaphroditus Genetta victoriae 553 558 Genetta maculata 559 557 660 Genetta genetta Genetta servalina Poiana richardsonii 556 Civettictis civetta 662 Viverra tangalunga 661 663 552 Viverra zibetha Viverricula indica Crocuta crocuta 666 667 Hyaena brunnea 665 Hyaena hyaena Proteles cristata Fossa fossana 664 669 770 Cryptoprocta ferox Salanoia concolor 668 772 Crossarchus alexandri 33 Suricata suricatta 775 -
Large Mammal Biochronology Framework in Europe at Jaramillo: the Epivillafranchian As a Formal Biochron
Quaternary International 389 (2015) 84e89 Contents lists available at ScienceDirect Quaternary International journal homepage: www.elsevier.com/locate/quaint Large mammal biochronology framework in Europe at Jaramillo: The Epivillafranchian as a formal biochron Luca Bellucci a, Raffaele Sardella a, Lorenzo Rook b, * a Dipartimento di Scienze della Terra, “Sapienza e Universita di Roma”, P.le A. Moro 5, 00185, Roma, Italy b Dipartimento di Scienze della Terra, Universita di Firenze, via G. La Pira 4, 50121, Firenze, Italy article info abstract Article history: European large mammal assemblages in the 1.2e0.9 Ma timespan included Villafranchian taxa together Available online 3 December 2014 with newcomers, mostly from Asia, persisting in the Middle Pleistocene. A number of biochronological schemes have been suggested to define these “transitional” faunas. The term Epivillafranchian, originally Keywords: proposed by Bourdier in 1961 and reconsidered as a biochron by Kahlke in the 1990s, is at present widely Biochronology introduced in the literature. This contribution, after selecting the most representative European large Jaramillo mammal assemblages within this chronological interval, provides a new definition proposal for the Epivillafranchian Epivillafranchian as a biochron included within the Praemegaceros verticornis FO/Bison menneri FO, and Late Villafranchian Crocuta crocuta Galerian FO. Europe © 2014 Elsevier Ltd and INQUA. All rights reserved. 1. Historical background communities of this time span primarily include survivors from the latest Villafranchian, as well as more evolved taxa characteristic of The Villafranchian Mammal Age corresponds, in the Interna- the beginning Middle Pleistocene (Kahlke, 2007; Rook and tional Stratigraphic Scale, to a timespan from Late Pliocene to most Martinez Navarro, 2010).