Extinct Giants, a New Wolf and the Key to Understanding Climate Change
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Mizzoualumnus1975novp16-19.Pdf (3.318Mb)
THE GAUE THAT TRAPPED HISTORY Natural Trap Cave has been collecting bones of unwary animals for at least 13,000 years. Expeditions led by a Mizzou anthropologist are digging up those bones and clues about the cycles of climatic change. Text and Photos by Dave Holman IIi / m ISSOllRI ilLUrnrus The only entrenee to Natural Trap Ceve la the hole In the roof. Any enlmal that might have survived the fallatlll became a victim. Workera at theahe, below, ehherrappellnto theeave or descend theacafloldlng. A herd of small horses stampeded through the tall grass across a plateau near the edge of a canyon, pur sued by a large, long-legged cat. The cat closed on the slowest horse, forcing her along the canyon edge onto a peninsula of limestone. The cat sprang, fas tened its claws and teeth in the horse's neck, and suddenly, horse and cat disappeared from the face of the earth. Twelve thousand years later, a green panel truck and a dusty jeep bounced along a dirt road over the same plateau, now covered with sage and prickly pear. On the limestone peninsula where the horse and cat disappeared, the vehicles stopped by a 15- foot-wide hole in the rock. Eighty feet below is the floor of Natural Trap Cave. The cave floor is covered with the accumulated dust of centuries, clearly stratified and containing thou sands of bones of animals that failed to see the hole. This summer was the second consecutive year that Bob Gilbert, research associate in Mizzou's an thropology department had led an organized ex pedition to the trap. -
Ursus Americanus) Versus Brown Bears (U. Arctos
East Tennessee State University Digital Commons @ East Tennessee State University Electronic Theses and Dissertations Student Works 5-2017 Black Bears (Ursus americanus) versus Brown Bears (U. arctos): Combining Morphometrics and Niche Modeling to Differentiate Species and Predict Distributions Through Time Theron Michael Kantelis East Tennessee State University Follow this and additional works at: https://dc.etsu.edu/etd Part of the Other Environmental Sciences Commons, Paleobiology Commons, and the Paleontology Commons Recommended Citation Kantelis, Theron Michael, "Black Bears (Ursus americanus) versus Brown Bears (U. arctos): Combining Morphometrics and Niche Modeling to Differentiate Species and Predict Distributions Through Time" (2017). Electronic Theses and Dissertations. Paper 3262. https://dc.etsu.edu/etd/3262 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]. Black Bears (Ursus americanus) versus Brown Bears (U. arctos): Combining Morphometrics and Niche Modeling to Differentiate Species and Predict Distributions Through Time 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 _____________________ -
Quaternary Records of the Dire Wolf, Canis Dirus, in North and South America
Quaternary records of the dire wolf, Canis dirus, in North and South America ROBERT G. DUNDAS Dundas, R. G. 1999 (September): Quaternary records of the dire wolf, Canis dirus, in North and South Ameri- ca. Boreas, Vol. 28, pp. 375–385. Oslo. ISSN 0300-9483. The dire wolf was an important large, late Pleistocene predator in North and South America, well adapted to preying on megaherbivores. Geographically widespread, Canis dirus is reported from 136 localities in North America from Alberta, Canada, southward and from three localities in South America (Muaco, Venezuela; Ta- lara, Peru; and Tarija, Bolivia). The species lived in a variety of environments, from forested mountains to open grasslands and plains ranging in elevation from sea level to 2255 m (7400 feet). Canis dirus is assigned to the Rancholabrean land mammal age of North America and the Lujanian land mammal age of South Amer- ica and was among the many large carnivores and megaherbivores that became extinct in North and South America near the end of the Pleistocene Epoch. Robert G. Dundas, Department of Geology, California State University, Fresno, California 93740-8031, USA. E-mail: [email protected]; received 20th May 1998, accepted 23rd March 1999 Because of the large number of Canis dirus localities Rancho La Brea, comparing them with Canis lupus and and individuals recovered from the fossil record, the dire wolf specimens from other localities. Although dire wolf is the most commonly occurring large knowledge of the animal’s biology had greatly predator in the Pleistocene of North America. By increased by 1912, little was known about its strati- contrast, the species is rare in South America. -
Frequency of Pathology in a Large Natural Sample from Natural Trap
Reumatismo, 2003; 55(1):58-65 RUBRICA DALLA RICERCA ALLA PRATICA Frequency of pathology in a large natural sample from Natural Trap Cave with special remarks on erosive disease in the Pleistocene La patologia osteoarticolare, con particolare riguardo a quella di tipo erosivo, nel Pleistocene: studio di un campione di reperti paleopatologici provenienti dalla Natural Trap Cave (Wyoming, USA) B.M. Rothschild1, L.D. Martin2 1The Arthritis Center of Northeast Ohio, University of Kansas Museum of Natural History, Carnegie Museum of Natural History, Northeastern Ohio Universities College of Medicine and University of Akron; 2Museum of Natural History and Department of Systematics and Ecology, University of Kansas, Lawrence, Kansas 66045 RIASSUNTO Nel presente studio vengono riportati i rilievi paleopatologici, con particolare riguardo alla presenza di artrite ero- siva, di osteoartrosi, di DISH , nonché ai segni di danno della dentizione, relativi ad un’ampia popolazione di mam- miferi, i cui resti (più di 30.000 ossa di 24 specie diverse) sono stati ritrovati nella Natural Trap Cave, Wyoming, USA. L’evidenza di artrite erosiva è confinata ai bovidi, Bison, Ovis e Bootherium, fatto osservabile anche in bisonti del tardo Pleistocene ritrovati nel Kansas (Twelve Mile Creek) e in un’altra località del Wisconsin, riferibile cronologi- camente al primo Olocene. Questi dati, ovvero la restrizione di tali segni di patologia articolare ad un singolo gene- re animale (Bovidi) e ad un determinato periodo storico, rende plausibile l’ipotesi che un agente patogeno, identifi- cabile col Mycobacterium tubercolosis, possa essere stato implicato nella genesi dell’artrite erosiva. Osteoartrosi e DISH sono risultate poco rappresentate nella popolazione animale della Natural Trap Cave, anche se il genere Bi- son ha dimostrato una discreta prevalenza di segni di osteoartrosi. -
The Holocene
The Holocene http://hol.sagepub.com The Holocene history of bighorn sheep (Ovis canadensis) in eastern Washington state, northwestern USA R. Lee Lyman The Holocene 2009; 19; 143 DOI: 10.1177/0959683608098958 The online version of this article can be found at: http://hol.sagepub.com/cgi/content/abstract/19/1/143 Published by: http://www.sagepublications.com Additional services and information for The Holocene can be found at: Email Alerts: http://hol.sagepub.com/cgi/alerts Subscriptions: http://hol.sagepub.com/subscriptions Reprints: http://www.sagepub.com/journalsReprints.nav Permissions: http://www.sagepub.co.uk/journalsPermissions.nav Citations http://hol.sagepub.com/cgi/content/refs/19/1/143 Downloaded from http://hol.sagepub.com at University of Missouri-Columbia on January 13, 2009 The Holocene 19,1 (2009) pp. 143–150 The Holocene history of bighorn sheep (Ovis canadensis) in eastern Washington state, northwestern USA R. Lee Lyman* (Department of Anthropology, 107 Swallow Hall, University of Missouri-Columbia, Columbia MO 65211, USA) Received 9 May 2008; revised manuscript accepted 30 June 2008 Abstract: Historical data are incomplete regarding the presence/absence and distribution of bighorn sheep (Ovis canadensis) in eastern Washington State. Palaeozoological (archaeological and palaeontological) data indicate bighorn were present in many areas there during most of the last 10 000 years. Bighorn occupied the xeric shrub-steppe habitats of the Channeled Scablands, likely because the Scablands provided the steep escape terrain bighorn prefer. The relative abundance of bighorn is greatest during climatically dry intervals and low during a moist period. Bighorn remains tend to increase in relative abundance over the last 6000 years. -
Dire Wolves Were the Last of an Ancient New World Canid Lineage Angela
Dire wolves were the last of an ancient New World canid lineage Angela R. Perri1,*§, Kieren J. Mitchell2,*§, Alice Mouton3,*, Sandra Álvarez-Carretero4,*, Ardern Hulme-Beaman5,6, James Haile 7, Alexandra Jamieson7, Julie Meachen8, Audrey T. Lin7,9,10, Blaine W. Schubert11, Carly Ameen12, Ekaterina E. Antipina13, Pere Bover14, Selina Brace15, Alberto Carmagnini4, Christian Carøe16, Jose A. Samaniego Castruita16, James C. Chatters17, Keith Dobney5, Mario dos Reis4, Allowen Evin18, Philippe Gaubert19, Shyam Gopalakrishnan16, Graham Gower2, Holly Heiniger2, Kristofer M. Helgen20, Josh Kapp21, Pavel A. Kosintsev22,23, Anna Linderholm7, 24, Andrew T. Ozga25, 26, 27, Samantha Presslee28, Alexander T. Salis2, Nedda F. Saremi21, Colin Shew3, Katherine Skerry26, Dmitry E. Taranenko29, Mary Thompson30, Mikhail V. Sablin31,Yaroslav V. Kuzmin32, 33, Matthew J. Collins34, 35, Mikkel-Holger S. Sinding16, 36, M. Thomas P. Gilbert16, 37, Anne C. Stone25 ,26, Beth Shapiro21, 38, Blaire Van Valkenburgh3, Robert K. Wayne3, Greger Larson7, and Alan Cooper39, Laurent A. F. Frantz4, 40§. 1Department of Archaeology, Durham University, Durham, UK 2Australian Centre for Ancient DNA, School of Biological Sciences, University of Adelaide, Australia 3Department of Ecology and Evolutionary Biology, University of California, Los Angeles, CA, USA 4School of Biological and Chemical Sciences, Queen Mary University of London, London, UK 5Department of Archaeology, Classics and Egyptology, University of Liverpool, Liverpool, UK 6School of Natural Sciences and Psychology, -
Small Mammal Faunal Stasis in Natural Trap Cave (Pleistocene– Holocene), Bighorn Mountains, Wyoming
SMALL MAMMAL FAUNAL STASIS IN NATURAL TRAP CAVE (PLEISTOCENE– HOLOCENE), BIGHORN MOUNTAINS, WYOMING BY C2009 Daniel R. Williams Submitted to the graduate degree program in Ecology and Evolutionary Biology and the Graduate Faculty of the University of Kansas in partial fulfillment of the requirements for the degree of Doctor of Philosophy. ______________________ Larry D. Martin/Chairperson Committee members* _____________________* Bruce S. Lieberman _____________________* Robert M. Timm _____________________* Bryan L. Foster _____________________* William C. Johnson Date defended: April 21, 2009 ii The Dissertation Committee for Daniel Williams certifies that this is the approved version of the following dissertation: SMALL MAMMAL FAUNAL STASIS IN NATURAL TRAP CAVE (PLEISTOCENE– HOLOCENE), BIGHORN MOUNTAINS, WYOMING Commmittee: ____________________________________ Larry D. Martin/Chairperson* ____________________________________ Bruce S. Lieberman ____________________________________ Robert M. Timm ____________________________________ Bryan L. Foster ____________________________________ William C. Johnson Date approved: April, 29, 2009 iii ABSTRACT Paleocommunity behavior through time is a topic of fierce debate in paleoecology, one with ramifications for the general study of macroevolution. The predominant viewpoint is that communities are ephemeral objects during the Quaternary that easily fall apart, but evidence exists that suggests geography and spatial scale plays a role. Natural Trap Cave is a prime testing ground for observing how paleocommunities react to large-scale climate change. Natural Trap Cave has a continuous faunal record (100 ka–recent) that spans the last glacial cycle, large portions of which are replicated in local rockshelters, which is used here to test for local causes of stasis. The Quaternary fauna of North America is relatively well sampled and dated, so the influence of spatial scale and biogeography on local community change can also be tested for. -
Rancholabrean Vertebrates from the Las Vegas Formation, Nevada
Quaternary International xxx (2017) 1e17 Contents lists available at ScienceDirect Quaternary International journal homepage: www.elsevier.com/locate/quaint The Tule Springs local fauna: Rancholabrean vertebrates from the Las Vegas Formation, Nevada * Eric Scott a, , Kathleen B. Springer b, James C. Sagebiel c a Dr. John D. Cooper Archaeological and Paleontological Center, California State University, Fullerton, CA 92834, USA b U.S. Geological Survey, Denver Federal Center, Box 25046, MS-980, Denver CO 80225, USA c Vertebrate Paleontology Laboratory, University of Texas at Austin R7600, 10100 Burnet Road, Building 6, Austin, TX 78758, USA article info abstract Article history: A middle to late Pleistocene sedimentary sequence in the upper Las Vegas Wash, north of Las Vegas, Received 8 March 2017 Nevada, has yielded the largest open-site Rancholabrean vertebrate fossil assemblage in the southern Received in revised form Great Basin and Mojave Deserts. Recent paleontologic field studies have led to the discovery of hundreds 19 May 2017 of fossil localities and specimens, greatly extending the geographic and temporal footprint of original Accepted 2 June 2017 investigations in the early 1960s. The significance of the deposits and their entombed fossils led to the Available online xxx preservation of 22,650 acres of the upper Las Vegas Wash as Tule Springs Fossil Beds National Monu- ment. These discoveries also warrant designation of the assemblage as a local fauna, named for the site of the original paleontologic studies at Tule Springs. The large mammal component of the Tule Springs local fauna is dominated by remains of Mammuthus columbi as well as Camelops hesternus, along with less common remains of Equus (including E. -
ABSTRACT Comparing the Genetic Diversity of Late Pleistocene Bison
ABSTRACT Comparing the Genetic Diversity of Late Pleistocene Bison with Modern Bison bison Using Ancient DNA Techniques and the Mitochondrial DNA Control Region Kory C. Douglas Mentors: Robert P. Adams, Ph.D., and Lori E. Baker, Ph.D. The transition between the Pleistocene and Holocene Epochs brought about a mass extinction of many large mammals. The genetic consequences of such widespread extinctions have not been well studied. Using ancient DNA and phylogenetic techniques, the genetic diversity and phylogenetic relatedness of extinct Pleistocene Bison ranging from Siberia to mid-latitude North America (10,000 ybp to 50,000 ybp) were compared to extant Bison bison. The mitochondrial DNA control region was sequenced from 10 Bison priscus skulls obtained from the Kolyma Region of Siberia, Russia. Control region sequences from other Pleistocene Bison species and Bison bison were obtained from Genbank. There is a measurable loss of genetic diversity in Bison bison compared to Pleistocene Bison. Furthermore, the Pleistocene Bison population was strongest in North America from a time period of 30,000 ybp to 10,000 ybp, and the genetic diversity present in this population is not represented in the Bison bison population. Copyright © 2006 Kory C. Douglas All rights reserved TABLE OF CONTENTS List of Figures iv List of Tables v Acknowledgments vi Chapter One: Introduction 1 Ancient DNA 2 Mitochondrial DNA 3 Pleistocene Epoch 5 Mass Extinctions 8 Bison 10 Phylogenetics 11 Research Hypotheses 14 Chapter Two: Materials and Methods 16 Sampling 16 -
Modern Wolves Trace Their Origin to a Late Pleistocene Expansion from Beringia
bioRxiv preprint doi: https://doi.org/10.1101/370122; this version posted July 18, 2018. The copyright holder for this preprint (which was not certified by peer review) is the author/funder, who has granted bioRxiv a license to display the preprint in perpetuity. It is made available under aCC-BY-NC-ND 4.0 International license. 1 Modern wolves trace their origin to a late Pleistocene expansion from Beringia 2 Liisa Loog1,2,3*, Olaf Thalmann4†, Mikkel-Holger S. Sinding5,6,7†, Verena J. Schuenemann8,9†, 3 Angela Perri10, Mietje Germonpré11, Herve Bocherens9,12, Kelsey E. Witt13, Jose A. 4 Samaniego Castruita5, Marcela S. Velasco5, Inge K. C. Lundstrøm5, Nathan Wales5, Gontran 5 Sonet15, Laurent Frantz2, Hannes Schroeder5,15, Jane Budd16, Elodie-Laure Jimenez 11, Sergey 6 Fedorov17, Boris Gasparyan18, Andrew W. Kandel19, Martina Lázničková-Galetová20,21,22, 7 Hannes Napierala23, Hans-Peter Uerpmann8, Pavel A. Nikolskiy24,25, Elena Y. Pavlova26,25, 8 Vladimir V. Pitulko25, Karl-Heinz Herzig4,27, Ripan S. Malhi26, Eske Willerslev2,5,29, Anders J. 9 Hansen5,7, Keith Dobney30,31,32, M. Thomas P. Gilbert5,33, Johannes Krause8,34, Greger 10 Larson1*, Anders Eriksson35,2*, Andrea Manica2* 11 12 *Corresponding Authors: L.L. ([email protected]), G.L. ([email protected]), 13 A.E. ([email protected]), A.M. ([email protected]) 14 15 †These authors contributed equally to this work 16 17 1 Palaeogenomics & Bio-Archaeology Research Network Research Laboratory for 18 Archaeology and History of Art, University of Oxford, Dyson Perrins Building, -
A Wild Boar Dominated Ungulate Assemblage from an Early Holocene Natural Pit Fall Trap
596837 HOL0010.1177/0959683615596837The HoloceneLord et al. research-article2015 Research report The Holocene 1 –7 A wild boar dominated ungulate © The Author(s) 2015 Reprints and permissions: sagepub.co.uk/journalsPermissions.nav assemblage from an early Holocene DOI: 10.1177/0959683615596837 natural pit fall trap: Cave shaft hol.sagepub.com sediments in northwest England associated with the 9.3 ka BP cold event Tom C Lord,1 John A Thorp2 and Peter Wilson3 Abstract A highly unusual pit fall ungulate assemblage dominated by wild boar (Sus scrofa) was recovered during the recent exploration of a cave shaft in the upland karstic landscape of northwest England. Both the opening of the cave shaft to the surface and its infilling by clastic sediments are attributable to accelerated landscape erosion associated with the 9.3 ka BP climatic deterioration. Evidence that wild boar had died in winter or spring suggests that their deaths relate to the prolonged periods of annual snow cover experienced by the uplands of northwest England during the 9.3 ka BP event. The dominance of wild boar in the pit fall assemblage is explained by the snow pack concealing the open shaft and turning it into a baited trap for wild boar whenever it contained carrion. Wild boar bones splintered and chewed by wild boar demonstrate carrion cannibalism. Human presence is attested by slight butchery to an aurochs (Bos primigenius). How Mesolithic people adapted to climate change associated with the 9.3 ka BP event is a subject well worth pursuing. Keywords 9.3 ka BP event, animal bones, karstic caves, northwest England Received 9 March 2015; revised manuscript accepted 6 June 2015 Introduction as Sites of Special Scientific Interest (Hinde et al., 2012). -
(Ovis Canadensis) of Natural Trap Cave, Wyoming
University of Nebraska - Lincoln DigitalCommons@University of Nebraska - Lincoln Transactions of the Nebraska Academy of Sciences and Affiliated Societies Nebraska Academy of Sciences 1988 Systematics and Population Ecology of Late Pleistocene Bighorn Sheep (Ovis Canadensis) of Natural Trap Cave, Wyoming Xiaoming Wang University of Kansas Main Campus Follow this and additional works at: https://digitalcommons.unl.edu/tnas Part of the Life Sciences Commons Wang, Xiaoming, "Systematics and Population Ecology of Late Pleistocene Bighorn Sheep (Ovis Canadensis) of Natural Trap Cave, Wyoming" (1988). Transactions of the Nebraska Academy of Sciences and Affiliated Societies. 194. https://digitalcommons.unl.edu/tnas/194 This Article is brought to you for free and open access by the Nebraska Academy of Sciences at DigitalCommons@University of Nebraska - Lincoln. It has been accepted for inclusion in Transactions of the Nebraska Academy of Sciences and Affiliated Societiesy b an authorized administrator of DigitalCommons@University of Nebraska - Lincoln. 1988. Transactions of the Nebraska Academy of Sciences, XVI: 173-183. SYSTEMATICS AND POPULATION ECOLOGY OF LATE PLEISTOCENE BIGHORN SHEEP (aVIS CANADENSIS) OF NATURAL TRAP CAVE, WYOMING Xiaoming Wang Museum of Natural History and Department of Systematics and Ecology University of Kansas Lawrence, Kansas 66045 Large numbers of Late Pleistocene bighorn sheep (total counts of identifi INTRODUCTION able elements: 4,497) Ovis canadensis. are described from the Natural Trap Cave, northern Wyoming. The specimens consist of nearly-intact skulls and enough post-cranial materials to assemble several complete sheep skeletons. Natural Trap Cave, south of the Wyoming-Montana border Most of the fossils yield radiocarbon dates from 12,000 to 21,000 BP, while the and Crow Indian Reservation, NW Y4, SE Y4, SEC.