Frequency of Pathology in a Large Natural Sample from Natural Trap
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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. -
Research Article Extinctions of Late Ice Age Cave Bears As a Result of Climate/Habitat Change and Large Carnivore Lion/Hyena/Wolf Predation Stress in Europe
Hindawi Publishing Corporation ISRN Zoology Volume 2013, Article ID 138319, 25 pages http://dx.doi.org/10.1155/2013/138319 Research Article Extinctions of Late Ice Age Cave Bears as a Result of Climate/Habitat Change and Large Carnivore Lion/Hyena/Wolf Predation Stress in Europe Cajus G. Diedrich Paleologic, Private Research Institute, Petra Bezruce 96, CZ-26751 Zdice, Czech Republic Correspondence should be addressed to Cajus G. Diedrich; [email protected] Received 16 September 2012; Accepted 5 October 2012 Academic Editors: L. Kaczmarek and C.-F. Weng Copyright © 2013 Cajus G. Diedrich. This is an open access article distributed under the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited. Predation onto cave bears (especially cubs) took place mainly by lion Panthera leo spelaea (Goldfuss),asnocturnalhuntersdeep in the dark caves in hibernation areas. Several cave bear vertebral columns in Sophie’s Cave have large carnivore bite damages. Different cave bear bones are chewed or punctured. Those lets reconstruct carcass decomposition and feeding technique caused only/mainlybyIceAgespottedhyenasCrocuta crocuta spelaea, which are the only of all three predators that crushed finally the long bones. Both large top predators left large tooth puncture marks on the inner side of cave bear vertebral columns, presumably a result of feeding first on their intestines/inner organs. Cave bear hibernation areas, also demonstrated in the Sophie’s Cave, were far from the cave entrances, carefully chosen for protection against the large predators. The predation stress must have increased on the last and larger cave bear populations of U. -
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. -
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. -
Māhā'ulepū, Island of Kaua'i Reconnaissance Survey
National Park Service U.S. Department of the Interior Pacific West Region, Honolulu Office February 2008 Māhā‘ulepū, Island of Kaua‘i Reconnaissance Survey THIS PAGE INTENTIONALLY LEFT BLANK TABLE OF CONTENTS 1 SUMMARY………………………………………………………………………………. 1 2 BACKGROUND OF THE STUDY……………………………………………………..3 2.1 Background of the Study…………………………………………………………………..……… 3 2.2 Purpose and Scope of an NPS Reconnaissance Survey………………………………………4 2.2.1 Criterion 1: National Significance………………………………………………………..4 2.2.2 Criterion 2: Suitability…………………………………………………………………….. 4 2.2.3 Criterion 3: Feasibility……………………………………………………………………. 4 2.2.4 Criterion 4: Management Options………………………………………………………. 4 3 OVERVIEW OF THE STUDY AREA…………………………………………………. 5 3.1 Regional Context………………………………………………………………………………….. 5 3.2 Geography and Climate…………………………………………………………………………… 6 3.3 Land Use and Ownership………………………………………………………………….……… 8 3.4. Maps……………………………………………………………………………………………….. 10 4 STUDY AREA RESOURCES………………………………………..………………. 11 4.1 Geological Resources……………………………………………………………………………. 11 4.2 Vegetation………………………….……………………………………………………...……… 16 4.2.1 Coastal Vegetation……………………………………………………………………… 16 4.2.2 Upper Elevation…………………………………………………………………………. 17 4.3 Terrestrial Wildlife………………..........…………………………………………………………. 19 4.3.1 Birds……………….………………………………………………………………………19 4.3.2 Terrestrial Invertebrates………………………………………………………………... 22 4.4 Marine Resources………………………………………………………………………...……… 23 4.4.1 Large Marine Vertebrates……………………………………………………………… 24 4.4.2 Fishes……………………………………………………………………………………..26 -
Figurative and Decorative Art of Kostenki: Chronological and Cultural Differentiation
CLOTTES J. (dir.) 2012. — L’art pléistocène dans le monde / Pleistocene art of the world / Arte pleistoceno en el mundo Actes du Congrès IFRAO, Tarascon-sur-Ariège, septembre 2010 – Symposium « Art mobilier pléistocène » Figurative and decorative art of Kostenki: chronological and cultural differentiation Andrei A. SINITSYN* To the memory of N.D. Praslov The very high concentration of open-air sites within a small territory is one of the main characteristics of the Palaeolithic group of Kostenki. As a matter of fact, twenty- six Palaeolithic sites are known from the territory of the actual villages of Kostenki and Borshchevo: almost half of them are stratified sites, containing up to ten archaeological layers (Fig. 1). Fig. 1. Kostenki-Borshchevo locality of Palaeolithic sites. A. Geographic position. * Institute for the History of Material Culture, Russian Academy of Sciences, Dvortsovaia nab., 18, Saint- Petersburg 191186 Russia – [email protected] Symposium Art mobilier In general, we deal here with the remnants of over sixty well stratified settlements. Equal high concentrations of Palaeolithic sites are known from the locality of Les Eyzies (Dordogne, France) with its numerous stratified deposits in caves and rock- shelters and from the slopes of the Pavlov hill in Moravia with a series of open-air sites. However, a second characteristics associated with the group of Kostenki does not present any analogies: the record of the assemblages in this area allows to construct a specific model of the cultural evolution during the Palaeolithic period that differs significantly from the models proposed in other eastern European regions, for example the Middle Dniepr region, the Pontic steppe, the Dniestr, the North-East and probably the Urals (Sinitsyn 2010b). -
Cave Bear, Cave Lion and Cave Hyena Skulls from The
COBISS: 1.01 CAVE BEAR, CAVE LION AND CAVE HYENA SKULLS FROM THE PUBLIC COLLECTION AT THE HUMBOLDT MUSEUM IN BERLIN Lobanje jamskega medveda, jamskega leva in jamske hijene iz zbirke Humboldtovega muzeja V Berlinu Stephan KEMPE1 & Doris DÖPPES2 Abstract UDC 569(069.5)(430 Berlin) Izvleček UDK 569(069.5)(430 Berlin) 069.02:569(430 Berlin) 069.02:569(430 Berlin) Stephan Kempe and Doris Döppes: Cave bear, cave lion and Stephan Kempe and Doris Döppes: Lobanje jamskega medve- cave hyena skulls from the public collection at the Humboldt da, jamskega leva in jamske hijene iz zbirke Humboldtovega Museum in Berlin muzeja v Berlinu The Linnean binomial system rests on the description of a ho- Linnejev binomski sistem poimenovanja temelji na opisu ho- lotype. The first fossil vertebrate species named accordingly was lotipa. Jamski medved je bil prva vrsta fosilnih vretenčarjev za- Ursus spelaeus, the cave bear. It was described by Rosenmüller pisana v tem sistemu. V svoji disertaciji ga je opisal Rosenmül- in 1794 in his dissertation using a skull from the Zoolithen Cave ler leta 1794, pri čemer je uporabil okostje iz jame Zoolithen (Gailenreuth Cave) in Frankonia, Germany. The whereabouts of (Gailenreuthska jama) v Frankoniji. Okoliščine oziroma usoda this skull is unknown. In the Humboldt Museum, Berlin, histor- tega skeleta je neznana. Humboldtov muzej v Berlinu hrani tri ic skulls of the three “spelaeus species” (cave bear, cave lion, cave fosilne vrste jamskih vretenčarjev: jamskega medveda, hijeno in hyena) are displayed. We were allowed to investigate them and jamskega leva. Omogočeno nam je bilo raziskovanje teh okostij further material in the Museum’s archive in an attempt to locate in ostalega arhivskega gradiva, pri čemer je bil naš namen od- the holotype skull. -
Human Origin Sites and the World Heritage Convention in Eurasia
World Heritage papers41 HEADWORLD HERITAGES 4 Human Origin Sites and the World Heritage Convention in Eurasia VOLUME I In support of UNESCO’s 70th Anniversary Celebrations United Nations [ Cultural Organization Human Origin Sites and the World Heritage Convention in Eurasia Nuria Sanz, Editor General Coordinator of HEADS Programme on Human Evolution HEADS 4 VOLUME I Published in 2015 by the United Nations Educational, Scientific and Cultural Organization, 7, place de Fontenoy, 75352 Paris 07 SP, France and the UNESCO Office in Mexico, Presidente Masaryk 526, Polanco, Miguel Hidalgo, 11550 Ciudad de Mexico, D.F., Mexico. © UNESCO 2015 ISBN 978-92-3-100107-9 This publication is available in Open Access under the Attribution-ShareAlike 3.0 IGO (CC-BY-SA 3.0 IGO) license (http://creativecommons.org/licenses/by-sa/3.0/igo/). By using the content of this publication, the users accept to be bound by the terms of use of the UNESCO Open Access Repository (http://www.unesco.org/open-access/terms-use-ccbysa-en). The designations employed and the presentation of material throughout this publication do not imply the expression of any opinion whatsoever on the part of UNESCO concerning the legal status of any country, territory, city or area or of its authorities, or concerning the delimitation of its frontiers or boundaries. The ideas and opinions expressed in this publication are those of the authors; they are not necessarily those of UNESCO and do not commit the Organization. Cover Photos: Top: Hohle Fels excavation. © Harry Vetter bottom (from left to right): Petroglyphs from Sikachi-Alyan rock art site. -
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. -
2003-2004 Recovery Report to Congress
U.S. Fish & Wildlife Service Report to Congress on the Recovery of Threatened and Endangered Species Fiscal Years 2003-2004 U.S. Fish & Wildlife Service Endangered Species Program www.fws.gov/endangered December 2006 The U.S. Fish and Wildlife Service is responsible under the Endangered Species Act for conserving and recovering our nation’s rarest plant and animal species and their habitats, working in cooperation with other public and private partners. From the Director Endangered Species Program Contacts Do you want more information on a particular threatened or endangered species or recovery effort near you? Please contact the Regional Office that covers the This 2004 report provides an update on the State(s) you are interested in. If they cannot help you, they will gladly direct you recovery of threatened and endangered species to the nearest Service office. for the period between October 1, 2002, and Region Six — Mountain-Prairie September 30, 2004, and chronicles the progress Washington D.C. Office Region Four — Southeast 134 Union Boulevard, Suite 650 of efforts by the Fish and Wildlife Service and Endangered Species Program 1875 Century Boulevard, Suite 200 Lakewood, CO 80228 the many partners involved in recovery efforts. 4401 N. Fairfax Drive, Room 420 Atlanta, GA 30345 http://mountain-prairie.fws.gov/endspp Arlington, VA 22203 http://www.fws.gov/southeast/es/ During this time, recovery efforts enabled three http://www.fws.gov/endangered Chief, Division of Ecological Services: species to be removed from the Endangered and Chief, -
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