Interpreting Paleontology, Evolving Ecosystems, and Climate Change in the Cenozoic Fossil Parks
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Aspects of the Functional Morphology in the Cranial and Cervical Skeleton of the Sabre-Toothed Cat Paramachairodus Ogygia (Kaup, 1832) (Felidae
Blackwell Science, LtdOxford, UKZOJZoological Journal of the Linnean Society0024-4082The Lin- nean Society of London, 2005? 2005 1443 363377 Original Article FUNCTIONAL MORPHOLOGY OF P. OGYGIAM. J. SALESA ET AL. Zoological Journal of the Linnean Society, 2005, 144, 363–377. With 11 figures Aspects of the functional morphology in the cranial and cervical skeleton of the sabre-toothed cat Paramachairodus ogygia (Kaup, 1832) (Felidae, Machairodontinae) from the Late Miocene of Spain: Downloaded from https://academic.oup.com/zoolinnean/article-abstract/144/3/363/2627519 by guest on 18 May 2020 implications for the origins of the machairodont killing bite MANUEL J. SALESA1*, MAURICIO ANTÓN2, ALAN TURNER1 and JORGE MORALES2 1School of Biological & Earth Sciences, Byrom Street, Liverpool John Moores University, Liverpool, L3 3AF, UK 2Departamento de Palaeobiología, Museo Nacional de Ciencias Naturales-CSIC, José Gutiérrez Abascal, 2. 28006 Madrid, Spain Received January 2004; accepted for publication March 2005 The skull and cervical anatomy of the sabre-toothed felid Paramachairodus ogygia (Kaup, 1832) is described in this paper, with special attention paid to its functional morphology. Because of the scarcity of fossil remains, the anatomy of this felid has been very poorly known. However, the recently discovered Miocene carnivore trap of Batallones-1, near Madrid, Spain, has yielded almost complete skeletons of this animal, which is now one of the best known machairodontines. Consequently, the machairodont adaptations of this primitive sabre-toothed felid can be assessed for the first time. Some characters, such as the morphology of the mastoid area, reveal an intermediate state between that of felines and machairodontines, while others, such as the flattened upper canines and verticalized mandibular symphysis, show clear machairodont affinities. -
South Dakota to Nebraska
Geological Society of America Special Paper 325 1998 Lithostratigraphic revision and correlation of the lower part of the White River Group: South Dakota to Nebraska Dennis O. Terry, Jr. Department of Geology, University of Nebraska—Lincoln, Lincoln, Nebraska 68588-0340 ABSTRACT Lithologic correlations between type areas of the White River Group in Nebraska and South Dakota have resulted in a revised lithostratigraphy for the lower part of the White River Group. The following pedostratigraphic and lithostratigraphic units, from oldest to youngest, are newly recognized in northwestern Nebraska and can be correlated with units in the Big Badlands of South Dakota: the Yellow Mounds Pale- osol Equivalent, Interior and Weta Paleosol Equivalents, Chamberlain Pass Forma- tion, and Peanut Peak Member of the Chadron Formation. The term “Interior Paleosol Complex,” used for the brightly colored zone at the base of the White River Group in northwestern Nebraska, is abandoned in favor of a two-part division. The lower part is related to the Yellow Mounds Paleosol Series of South Dakota and rep- resents the pedogenically modified Cretaceous Pierre Shale. The upper part is com- posed of the unconformably overlying, pedogenically modified overbank mudstone facies of the Chamberlain Pass Formation (which contains the Interior and Weta Paleosol Series in South Dakota). Greenish-white channel sandstones at the base of the Chadron Formation in Nebraska (previously correlated to the Ahearn Member of the Chadron Formation in South Dakota) herein are correlated to the channel sand- stone facies of the Chamberlain Pass Formation in South Dakota. The Chamberlain Pass Formation is unconformably overlain by the Chadron Formation in South Dakota and Nebraska. -
The World at the Time of Messel: Conference Volume
T. Lehmann & S.F.K. Schaal (eds) The World at the Time of Messel - Conference Volume Time at the The World The World at the Time of Messel: Puzzles in Palaeobiology, Palaeoenvironment and the History of Early Primates 22nd International Senckenberg Conference 2011 Frankfurt am Main, 15th - 19th November 2011 ISBN 978-3-929907-86-5 Conference Volume SENCKENBERG Gesellschaft für Naturforschung THOMAS LEHMANN & STEPHAN F.K. SCHAAL (eds) The World at the Time of Messel: Puzzles in Palaeobiology, Palaeoenvironment, and the History of Early Primates 22nd International Senckenberg Conference Frankfurt am Main, 15th – 19th November 2011 Conference Volume Senckenberg Gesellschaft für Naturforschung IMPRINT The World at the Time of Messel: Puzzles in Palaeobiology, Palaeoenvironment, and the History of Early Primates 22nd International Senckenberg Conference 15th – 19th November 2011, Frankfurt am Main, Germany Conference Volume Publisher PROF. DR. DR. H.C. VOLKER MOSBRUGGER Senckenberg Gesellschaft für Naturforschung Senckenberganlage 25, 60325 Frankfurt am Main, Germany Editors DR. THOMAS LEHMANN & DR. STEPHAN F.K. SCHAAL Senckenberg Research Institute and Natural History Museum Frankfurt Senckenberganlage 25, 60325 Frankfurt am Main, Germany [email protected]; [email protected] Language editors JOSEPH E.B. HOGAN & DR. KRISTER T. SMITH Layout JULIANE EBERHARDT & ANIKA VOGEL Cover Illustration EVELINE JUNQUEIRA Print Rhein-Main-Geschäftsdrucke, Hofheim-Wallau, Germany Citation LEHMANN, T. & SCHAAL, S.F.K. (eds) (2011). The World at the Time of Messel: Puzzles in Palaeobiology, Palaeoenvironment, and the History of Early Primates. 22nd International Senckenberg Conference. 15th – 19th November 2011, Frankfurt am Main. Conference Volume. Senckenberg Gesellschaft für Naturforschung, Frankfurt am Main. pp. 203. -
Proceedings of the Third Conference on Fossil Resources in the National Park Service
^^ ;&J Proceedings of the Third Conference on Fossil Resources in the National Park Service Rachel Benton and Ann Elder, Editors Natural Resources Report NPS/NRFOBU/NRR-94/14 °>%HIL M©^m United States Department of the Interior • National Park Service Rocky Mountain Region • Fossil Butte National Monument The National Park Service disseminates reports on high priority, current resource management information, with application for managers, through the Natural Resources Report Series. Technologies and resource management methods; how to resource management papers; popular articles through the yearly highlights report; proceedings on resource management workshops or conferences; and natural resources program recommendations and descriptions and resource action plans are also disseminated through this series. Documents in this series usually contain information of a preliminary nature and are prepared primarily for internal use within the National Park Service. This information is not intended for use in the open literature. Mention of trade names or commercial products does not constitute endorsement or recommenda- tion for use by the National Park Service. Copies of this report are available from the following: Publications Coordinator National Park Service Natural Resources Publication Office P.O. Box 25287 (WASO-NRPO) Denver, CO 80225-0287 CfO Printed on Recycled Paper Proceedings of the Third Conference on Fossil Resources in the National Park Service 14-17 September 1992 Fossil Butte National Monument, Wyoming Editors: Rachel Benton -
Unit-V Evolution of Horse
UNIT-V EVOLUTION OF HORSE Horses (Equus) are odd-toed hooped mammals belong- ing to the order Perissodactyla. Horse evolution is a straight line evolution and is a suitable example for orthogenesis. It started from Eocene period. The entire evolutionary sequence of horse history is recorded in North America. " Place of Origin The place of origin of horse is North America. From here, horses migrated to Europe and Asia. By the end of Pleis- tocene period, horses became extinct in the motherland (N. America). The horses now living in N. America are the de- scendants of migrants from other continents. Time of Origin The horse evolution started some 58 million years ago, m the beginning of Eocene period of Coenozoic era. The modem horse Equus originated in Pleistocene period about 2 million years ago. Evolutionary Trends The fossils of horses that lived in different periods, show that the body parts exhibited progressive changes towards a particular direction. These directional changes are called evo- lutionary trends. The evolutionary trends of horse evolution are summarized below: 1. Increase in size. 2. Increase in the length of limbs. 3. Increase in the length of the neck. 4. Increase in the length of preorbital region (face). 5. Increase in the length and size of III digit. 6. Increase in the size and complexity of brain. 7. Molarization of premolars. Olfactory bulb Hyracotherium Mesohippus Equus Fig.: Evolution of brain in horse. 8. Development of high crowns in premolars and molars. 9. Change of plantigrade gait to unguligrade gait. 10. Formation of diastema. 11. Disappearance of lateral digits. -
Hoganson, J.W., 2009. Corridor of Time Prehistoric Life of North
Corridor of Time Prehistoric Life of North Dakota Exhibit at the North Dakota Heritage Center Completed by John W. Hoganson Introduction In 1989, legislation was passed that directed the North Dakota and a laboratory specialist, a laboratory for preparation of Geological Survey to establish a public repository for North fossils, and a fossil storage area. The NDGS paleontology staff, Dakota fossils. Shortly thereafter, the Geological Survey signed now housed at the Heritage Center, consists of John Hoganson, a Memorandum of Agreement with the State Historical Society State Paleontologist, and paleontologists Jeff Person and Becky of North Dakota which provided space in the North Dakota Gould. This arrangement has allowed the Geological Survey, in Heritage Center for development of this North Dakota State collaboration with the State Historical Society of North Dakota, Fossil Collection, including offices for the curator of the collection to create prehistoric life of North Dakota exhibits at the Heritage Center and displays of North Dakota fossils at over 20 other museums and interpretive centers around the state. The first of the Heritage Center prehistoric life exhibits was the restoration of the Highgate Mastodon skeleton in the First People exhibit area (fig. 1). Mastodons were huge, elephant- like mammals that roamed North America at the end of the last Ice Age about 11,000 years ago. This exhibit was completed in 1992 and was the first restored skeleton of a prehistoric animal ever displayed in North Dakota. The mastodon exhibit was, and still is, a major attraction in the Heritage Center. Because of its popularity, it was decided that additional prehistoric life displays should be included in the Heritage Center exhibit plans. -
Origin and Beyond
EVOLUTION ORIGIN ANDBEYOND Gould, who alerted him to the fact the Galapagos finches ORIGIN AND BEYOND were distinct but closely related species. Darwin investigated ALFRED RUSSEL WALLACE (1823–1913) the breeding and artificial selection of domesticated animals, and learned about species, time, and the fossil record from despite the inspiration and wealth of data he had gathered during his years aboard the Alfred Russel Wallace was a school teacher and naturalist who gave up teaching the anatomist Richard Owen, who had worked on many of to earn his living as a professional collector of exotic plants and animals from beagle, darwin took many years to formulate his theory and ready it for publication – Darwin’s vertebrate specimens and, in 1842, had “invented” the tropics. He collected extensively in South America, and from 1854 in the so long, in fact, that he was almost beaten to publication. nevertheless, when it dinosaurs as a separate category of reptiles. islands of the Malay archipelago. From these experiences, Wallace realized By 1842, Darwin’s evolutionary ideas were sufficiently emerged, darwin’s work had a profound effect. that species exist in variant advanced for him to produce a 35-page sketch and, by forms and that changes in 1844, a 250-page synthesis, a copy of which he sent in 1847 the environment could lead During a long life, Charles After his five-year round the world voyage, Darwin arrived Darwin saw himself largely as a geologist, and published to the botanist, Joseph Dalton Hooker. This trusted friend to the loss of any ill-adapted Darwin wrote numerous back at the family home in Shrewsbury on 5 October 1836. -
GEOL 204 the Fossil Record Spring 2020 Section 0109 Luke Buczynski, Eamon, Doolan, Emmy Hudak, and Shutian Wang
ENTELODONT: The Hellacious Pigs of the Cenozoic GEOL 204 The Fossil Record Spring 2020 Section 0109 Luke Buczynski, Eamon, Doolan, Emmy Hudak, and Shutian Wang Entelodont Overview: From the family Entelodontidae, these omnivorous mammals had a wide geographic variety, as seen in image B. They first inhabited Mongolia then spread into Eurasia and North America, while in North America they preferred flood plains and woodlands. Entelodont were fairly aggressive and would fight with their own kind, using their strong jaws and large heads. They survived from the middle of Eocene to the middle of Miocene. Size and Diet: Skull Features: Figure D shows one of the largest Entelodont, Daedon, compared to an As seen on Figure C, the skull of the Entelodont is massive. They all 1.8 meter tall human, illustrating how immense they really were. contained large Neural Spines, most likely to hold up their huge head, Entelodont weighed from 150 kg on the small size, up to 900 kg (330 to which in turn created a hump. Entelodont contained a pretty small 2,000 pounds) and 1 to 2 meters in height. They had teeth that made them brain, but large olfactory lobes, giving them an acute sense of smell. capable of consuming meat, but the overall structure and wear on the the They held sturdy canines, long incisors, sharp serrated premolars, and suggest the consumption of plant matter as well. Although these large blunt square molars (a sign of omnivory), all of which were covered in a animals might not look it, their limbs were fully terrestrial and adept for very thick layer of enamel. -
Savor the Cryosphere
Savor the Cryosphere Patrick A. Burkhart, Dept. of Geography, Geology, and the Environment, Slippery Rock University, Slippery Rock, Pennsylvania 16057, USA; Richard B. Alley, Dept. of Geosciences, Pennsylvania State University, University Park, Pennsylvania 16802, USA; Lonnie G. Thompson, School of Earth Sciences, Byrd Polar and Climate Research Center, Ohio State University, Columbus, Ohio 43210, USA; James D. Balog, Earth Vision Institute/Extreme Ice Survey, 2334 Broadway Street, Suite D, Boulder, Colorado 80304, USA; Paul E. Baldauf, Dept. of Marine and Environmental Sciences, Nova Southeastern University, 3301 College Ave., Fort Lauderdale, Florida 33314, USA; and Gregory S. Baker, Dept. of Geology, University of Kansas, 1475 Jayhawk Blvd., Lawrence, Kansas 66045, USA ABSTRACT Cryosphere,” a Pardee Keynote Symposium loss of ice will pass to the future. The This article provides concise documen- at the 2015 Annual Meeting in Baltimore, extent of ice can be measured by satellites tation of the ongoing retreat of glaciers, Maryland, USA, for which the GSA or by ground-based glaciology. While we along with the implications that the ice loss recorded supporting interviews and a provide a brief assessment of the first presents, as well as suggestions for geosci- webinar. method, our focus on the latter is key to ence educators to better convey this story informing broad audiences of non-special- INTRODUCTION to both students and citizens. We present ists. The cornerstone of our approach is the the retreat of glaciers—the loss of ice—as The cryosphere is the portion of Earth use of repeat photography so that the scale emblematic of the recent, rapid contraction that is frozen, which includes glacial and and rate of retreat are vividly depicted. -
Mcabee Fossil Site Assessment
1 McAbee Fossil Site Assessment Final Report July 30, 2007 Revised August 5, 2007 Further revised October 24, 2008 Contract CCLAL08009 by Mark V. H. Wilson, Ph.D. Edmonton, Alberta, Canada Phone 780 435 6501; email [email protected] 2 Table of Contents Executive Summary ..............................................................................................................................................................3 McAbee Fossil Site Assessment ..........................................................................................................................................4 Introduction .......................................................................................................................................................................4 Geological Context ...........................................................................................................................................................8 Claim Use and Impact ....................................................................................................................................................10 Quality, Abundance, and Importance of the Fossils from McAbee ............................................................................11 Sale and Private Use of Fossils from McAbee..............................................................................................................12 Educational Use of Fossils from McAbee.....................................................................................................................13 -
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. -
2009 BLM Facts
BLM Oregon & Washington Bureau of Land Management of Bureau U.S. Department of the Interior the Interior of U.S. Department Oregon & Washington Bureau of Land Management BLM/OR/WA/AE-10/074+1792 The Bureau of Land Management Welcomes You to Oregon & Washington! Oregon & Washington i Welcome n early 2010, President Obama announced America’s Great Outdoors initiative Ito conserve our cherished lands and encourage Americans to enjoy the outdoors. And in this I’m reminded of William Shakespeare’s quote, “One touch of nature makes the whole world kin.” Throughout my years of experience, this great notion still rings true. I can attest that Americans have grown closer by the simple virtue of spending time together in nature. And it is on this note that I am thrilled to present our 2009 edition of BLM Facts. Between 96 pages of photos, maps, and detailed facts, I’m very pleased to highlight the diversity of the BLM’s multiple use mission. We serve the public lands by accomplishing what is perhaps the most extensive range of duties by any one agency. BLM foresters use scientific methods to plan for a sustainable growth of trees which also provide a healthy environment while still affording Americans homes, offices, and jobs. Our recreation planners and interpretive specialists present inspirational educational events and breathtaking locations for Americans to visit and create long-lasting memories. Resource specialists care for our special areas protected under the National Landscape Conservation System. Scientists at the BLM complete crucial research using the most current data to ensure we maintain these lands for future generations.