Body Size Evolution in Leptomeryx and Rhinocerotinae

Total Page:16

File Type:pdf, Size:1020Kb

Body Size Evolution in Leptomeryx and Rhinocerotinae BODY SIZE EVOLUTION IN LEPTOMERYX AND RHINOCEROTINAE (SUBHYRACODON AND TRIGONIAS) ACROSS THE EOCENE – OLIGOCENE (CHADRONIAN – ORELLAN) BOUNDARY by WENDY A. SCHULTZ B. S. University of Nebraska – Lincoln, 2006 A thesis submitted to the Faculty of the Graduate School of the University of Colorado in partial fulfillment of the requirement of the degree of Master of Science Museum and Field Studies 2009 UMI Number: 1473682 All rights reserved INFORMATION TO ALL USERS The quality of this reproduction is dependent upon the quality of the copy submitted. In the unlikely event that the author did not send a complete manuscript and there are missing pages, these will be noted. Also, if material had to be removed, a note will indicate the deletion. UMI 1473682 Copyright 2010 by ProQuest LLC. All rights reserved. This edition of the work is protected against unauthorized copying under Title 17, United States Code. ProQuest LLC 789 East Eisenhower Parkway P.O. Box 1346 Ann Arbor, MI 48106-1346 This thesis entitled: Body size Evolution in Leptomeryx and Rhinocerotinae (Subhyracodon and Trigonias) Across the Eocene – Oligocene (Chadronian – Orellan) boundary Written by Wendy A. Schultz has been approved for the Department of Museum and Field Studies _____________________________________ Dr. Jaelyn Eberle, Committee Chair ____________________________________ Dr. Richard Stucky, Committee Member ____________________________________ Dr. Christy McCain, Committee Member Date ______________ The final copy of this thesis has been examined by the signatories, and we find that both the content and the form meet acceptable presentation standards of scholarly work in the above mentioned discipline iii Schultz, Wendy A. (M.S., Museum and Field Studies [Vertebrate Paleontology]) Body size Evolution in Leptomeryx and Rhinocerotinae (Subhyracodon and Trigonias) Across the Eocene – Oligocene (Chadronian – Orellan) boundary Thesis directed by Assistant Professor Jaelyn J. Eberle Research has shown that there was dramatic climate change, specifically a significant drop in temperature, across the Eocene – Oligocene (Chadronian – Orellan) boundary. However, few studies have looked at the effects of this climatic cooling on the terrestrial vertebrate fauna. My study focused on changes in mammalian body size across the Chadronian – Orellan transition, in particular within the small artiodactyl Leptomeryx and the large rhinocerotine perissodactyls, based upon fossils from the White River Group in the Northern Plains (Colorado, Wyoming, Nebraska, and South Dakota). Specifically, I tested whether Bergmann’s Rule (which suggests that in a given taxon, those individuals inhabiting colder climates will be larger-bodied than those living in a warmer climate) occurred with climatic cooling across the Chadronian-Orellan boundary. With regard to the rhinocerotines, I used Trigonias, Subhyracodon, and specimens identified as Rhinocerotinae gen. indet. Rhinocerotineae gen.indet. specimens are missing their anterior dentition (which is what differentiates teeth of Trigonias from Subhyracodon), and consequently were simply identified only as Rhinocerotinae genus indet. Length and width measurements of upper and lower molars were used as a proxy for body size of both Chadronian and Orellan representatives of two lineages of Leptomeryx, (L. speciosus – L. evansi lineage and L. yoderi – L. mammifer – L. exilis lineage). The two lineages of iv Leptomeryx showed a statistically significant decrease in tooth size in the Orellan. The Rhinocerotinae show a significant decrease in tooth size across the Chadronian – Orellan transition. Although other researchers have noted that only one Leptomeryx lineage survived the Eocene-Oligocene transition, this research suggests that both lineages survived this boundary. The decrease in body size with decrease in temperature in Leptomeryx and Rhinocerotinae is opposite of the expected pattern of Bergmann’s Rule. My data suggest that other factors, besides climatic cooling, also need to be considered in mammalian body size evolution across the Eocene-Oligocene boundary. v Acknowledgments I would like to thank my committee members, Richard Stucky and Christy McCain, and my committee chair, Jaelyn Eberle for always being willing to meet with me when I had questions or concerns about localities or my data. Additional thanks to Jaelyn for her guidance and editing through the course of this thesis project. Thank you to the collections managers and curators at the four museums I visited. Bill Simpson allowed me to conduct research while at the Field Museum of Natural History for my internship, and Olivier Rieppel for authorized a loan of Leptomeryx specimens. Sally Shelton gave me access to the collections at South Dakota School of Mines and Technology, and I thank Ed Walsh for his help in the collection and for showing me around town. Logan Ivy at Denver Museum of Nature & Science helped in collections, specifically in tracking down specimens and accessory information, and Richard Stucky granted access to the collections. I thank Toni Culver at the Colorado Museum of Natural History, for not only lending me undergraduates to help find specimens in the collections, but also for answering many questions I had about our collection database. Extra thanks to Toni for being an awesome boss by allowing me a very flexible work schedule so I could work around my thesis. This project could not have been completed without my fiancé, Nathan Beins, who listened to me when I would talk about my research and writing (even if he didn’t understand anything of what I was saying), and put up with all of my complaints during the whole process. Thank you to my friend Nick Walker for discussing statistics and math, and to Hannah Johnson for letting me borrow him. Thank you so much to Hobbes Hayden for helping me put Adobe Photoshop on both of my computers, vi teaching me how to use it, being my tech support when I couldn’t remember what he taught me, and for allowing me to work on my thesis at his place when I needed a change in scenery. A huge thank you to my office mates, Ben Burger, Alex Dutchak, and Laura Wilson for answering my many questions and helping me along this process. Especially a huge thank you to Laura who is the best office mate, co-worker, and good friend a graduate student could ask for. She was always there, even at midnight, to answer my many, many questions, help me with phrasing, and proofread parts of my thesis before I sent them to Jaelyn, even when we were in different states and she was out in the field. She also made sure I still took time to relax and didn’t get too stressed out. Project and research funding came from the University of Colorado Museum of Natural History. Funding for my research trip to the Field Museum in Chicago was provided by the Walker Van Riper fund. Funding for my research trip to South Dakota School of Mines and Technology came from the University of Colorado Museum of Natural History Paleontology Section. vii TABLE OF CONTENTS I. Introduction……………………………………………………………..………….1 1. The EOT Cooling Event………………..………………………………………...5 2. Bergmann’s Rule……………………………………………………………......…7 3. Background to Biostratigraphy………………………………………....…15 4. Sedimentology and Stratigraphy ……………………………………..…..19 a. Nebraska……………………………………………………………………22 b. South Dakota…………………………………………………………...…23 c. Wyoming…………………………………………………………...………24 d. Colorado………………………………………………………...…….……25 5. Mammalian Taxa…………………………………………………..……………25 a. Rhinocerotinae…………………………………………………………...26 i. Subhyracodon………………………………………………….……..….….27 ii. Trigonias………………………………………………………………..……28 b. Leptomeryx……………………………………………………………..….29 II. Materials and Methods……………………………………………………….33 1. Age Categories……………………………………………………………..……..41 2. Methods of Estimating Body Mass…………………………….…………..43 3. Statistical Methods……………………………………………………...………45 III. Results……………………………………………………………………...……….47 1. Leptomeryx……………………………………………………………….….…….47 2. Rhinocerotinae…………………………………………………….……….…….55 IV. Discussion and Conclusions………………………………………….…….64 1. Future Research…………………………………………………………...……..69 V. Bibliography………………………………………………………………………71 VI. Appendix 1: Statistical analysis of dental elements of all adult Leptomeryx used in this study ……………………………………………………………81 VII. Appendix 2………………………………………………………...………………82 1. Table 1: Measurements of Leptomeryx lower dentition……………………..82 2. Table 2: Measurements of Leptomeryx upper dentition…………………….94 VIII. Appendix 3……………………………………………………………………....101 1. Table 1: Measurements of Rhinocerotinae lower dentition……………….101 2. Table 2: Measurements of Rhinocerotinae upper dentition…………...……..107 viii LIST OF TABLES Table 1: Comparison of the right and left sides of the skull and jaws in all Leptomeryx used in this study……………………………………………………………...47 Table 2: Statistical analysis of dental elements of L. speciosus – L. evansi used in this study…………………………………………………………………………..48 Table 3: Statistical analysis of dental elements of L. mammifer – L. exilis lineage used in this study ……………………………………………………………………..49 Table 4: Statistical analysis of dental elements of Colorado Leptomeryx used in this study ………………………………………………………………………………..51 Table 5: Statistical analysis of dental elements of non-Colorado Leptomeryx used in this study ……………………………………………………………………….....52 Table 6: Univariate body mass estimates of Leptomeryx based on m2 length………...…55 Table 7: Statistical analysis of dental elements of Rhinocerotinae used in this study…...57 Table 8: Statistical analysis of dental
Recommended publications
  • Hyracodons and Subhyracodons Early Rhinoceros by Ryan C
    The Fossils of the White River Badlands http://whiteriver.weebly.com/hyracodons.html Hyracodons and Subhyracodons Early rhinoceros by Ryan C. The discovery of rhinoceros in the Badlands of the American West was very exciting, most people never suspecting that such primitive forms of rhinoceros existed in North America. Today, living rhinoceroses consist of four genera that contain five species. Two are found in Africa; three others are restricted to Asia. Most are browsing animals but the largest species, the white rhinoceros of Africa, is a grazer. All living species possess "horns" that are composed of keratinized hair which decomposes at death and are not normally preserved in the fossil record. Although most New World rhinoceroses did not have horns, the widely distributed, males of the pig-sized Menoceros of the early Miocene had a lateral pair of horns. In North America, "rhinoceroses" of three similar lineages appeared from Asia during the Middle Eocene. Consisting of hippo-like Amynodontidae, "running rhinos" or Hyracodontidae, and true rhinoceroses, Rhinocerotidae, only true rhinoceroses adapted and diversified enough to survive into the early Pliocene. Amynodontids entered North America during the Bridgerian NALMA. Apparently adapted for a warm humid environment typified by lush forests, most amynodontids physically and ecologically resembled the hippopotamus of Africa. Remaining undiversified, only four genera are recognized and three of them contain but a single species. The massive and best known species is Metamynodon planifrons, a form characterized by having massive teeth with large tusks that give it the appearance of a hippopotamus. Some skeletons were 10 ft in length. Due to their skull structure, some believe this group supported a proboscis similar to that of a modern tapir.
    [Show full text]
  • SUPPLEMENTARY INFORMATION: Tables, Figures and References
    Samuels, Regnault & Hutchinson, PeerJ Evolution of the patellar sesamoid bone in mammals SUPPLEMENTARY INFORMATION: Tables, Figures and References Supplementary Table S1: Mammaliaform patellar status$ Inclusive clades Genus and Stratigraphic age of Patellar Comments# (partial) species (and taxon, and location(s) state reference(s) used for 0/1/2 patellar status) (absent/ ‘patelloid’/ present) Sinoconodonta Sinoconodon Jurassic, China 0 Patellar groove absent, suggests no rigneyi (Kielan- patella Jaworowska et al., 2004) Sinoconodon is included on our phylogeny within tritylodontids. Morganucodonta Megazostrodon Late Triassic, southern 0 rudnerae (Jenkins Africa & Parrington, 1976) Morganucodonta Eozostrodon sp. Late Triassic, Wales 0 Asymmetric patellar groove, (Jenkins et al., specimens disarticulated so it is hard 1976) to assess the patella but appears absent Docodonta Castorocauda 164 Mya, mid-Jurassic, 0 Semi-aquatic adaptations lutrasimilis (Ji et China al., 2006) Docodonta Agilodocodon 164 Mya, mid-Jurassic, 0 scansorius (Meng China et al., 2015) Docodonta Docofossor 160 Mya, China 0 brachydactylus (Luo et al., 2015b) Docodonta Haldanodon 150-155 Mya, Late 0 Shallow patellar groove exspectatus Jurassic, Portugal (Martin, 2005b) Australosphenida Asfaltomylos Mid-Jurassic, South ? Postcranial material absent patagonicus America (Martin, 2005a) Australosphenida Ornithorhynchus Extant 2 Platypus, genome sequenced Monotremata anatinus (Warren, Hillier, Marshall Graves et (Herzmark, 1938; al., 2008) Rowe, 1988) Australosphenida Tachyglossus
    [Show full text]
  • Aplodontid, Sciurid, Castorid, Zapodid and Geomyoid Rodents of the Rodent Hill Locality, Cypress Hills Formation, Southwest Saskatchewan
    APLODONTID, SCIURID, CASTORID, ZAPODID AND GEOMYOID RODENTS OF THE RODENT HILL LOCALITY, CYPRESS HILLS FORMATION, SOUTHWEST SASKATCHEWAN A Thesis Submitted to the College of Graduate Studies and Research in Partial Fulfillment of the Requirements for the Degree of Master of Science in the Department of Geological Sciences University of Saskatchewan Saskatoon By Sean D. Bell © Copyright Sean D. Bell, December 2004. All rights reserved. PERMISSION TO USE In presenting this thesis in partial fulfilment of the requirements for a Master’s degree from the University of Saskatchewan, I agree that the libraries of the University of Saskatchewan may make it freely available for inspection. I further agree that permission for copying of this thesis in any manner, in whole or in part, for scholarly purposes may be granted by the professors who supervised my thesis work or, in their absence, by the Head of the Department of Geological Sciences or the Dean of the College of Graduate Studies and Research. It is understood that any copying or publication or use of this thesis or parts thereof for financial gain shall not be allowed without my written permission. It is also understood that due recognition shall be given to me and to the University of Saskatchewan in any scholarly use which may be made of any material in my thesis. Requests for permission to copy or to make other use of material in this thesis in whole or part should be addressed to: Head of the Department of Geological Sciences 114 Science Place University of Saskatchewan Saskatoon, Saskatchewan S7N 5E2 i ABSTRACT The Rodent Hill Locality is a fossil-bearing site that is part of the Cypress Hills Formation, and is located roughly 15 km northwest of the town of Eastend, Saskatchewan.
    [Show full text]
  • Depositional History of the Chadron Formation in North Dakota
    Depositional History of the Chadron Formation in North Dakota by Clint A. Boyd1 and John R. Webster2 1North Dakota Geological Survey 2Geosciences, Minot State University REPORT OF INVESTIGATION NO. 120 NORTH DAKOTA GEOLOGICAL SURVEY Edward C. Murphy, State Geologist Lynn D. Helms, Director Dept. of Mineral Resources 2018 Table of Contents Abstract ........................................................................................................................................... v Acknowledgements ........................................................................................................................ vi Introduction ..................................................................................................................................... 1 Late Eocene Paleosols of North Dakota ......................................................................................... 3 Paleosols at White and Haystack Buttes (Stark County) ............................................................ 4 Description of Section 1 .......................................................................................................... 5 Description of Section 2 .......................................................................................................... 7 History of Paleosol Development ......................................................................................... 13 Interpretation ......................................................................................................................... 16
    [Show full text]
  • 2014BOYDANDWELSH.Pdf
    Proceedings of the 10th Conference on Fossil Resources Rapid City, SD May 2014 Dakoterra Vol. 6:124–147 ARTICLE DESCRIPTION OF AN EARLIEST ORELLAN FAUNA FROM BADLANDS NATIONAL PARK, INTERIOR, SOUTH DAKOTA AND IMPLICATIONS FOR THE STRATIGRAPHIC POSITION OF THE BLOOM BASIN LIMESTONE BED CLINT A. BOYD1 AND ED WELSH2 1Department of Geology and Geologic Engineering, South Dakota School of Mines and Technology, Rapid City, South Dakota 57701 U.S.A., [email protected]; 2Division of Resource Management, Badlands National Park, Interior, South Dakota 57750 U.S.A., [email protected] ABSTRACT—Three new vertebrate localities are reported from within the Bloom Basin of the North Unit of Badlands National Park, Interior, South Dakota. These sites were discovered during paleontological surveys and monitoring of the park’s boundary fence construction activities. This report focuses on a new fauna recovered from one of these localities (BADL-LOC-0293) that is designated the Bloom Basin local fauna. This locality is situated approximately three meters below the Bloom Basin limestone bed, a geographically restricted strati- graphic unit only present within the Bloom Basin. Previous researchers have placed the Bloom Basin limestone bed at the contact between the Chadron and Brule formations. Given the unconformity known to occur between these formations in South Dakota, the recovery of a Chadronian (Late Eocene) fauna was expected from this locality. However, detailed collection and examination of fossils from BADL-LOC-0293 reveals an abundance of specimens referable to the characteristic Orellan taxa Hypertragulus calcaratus and Leptomeryx evansi. This fauna also includes new records for the taxa Adjidaumo lophatus and Brachygaulus, a biostratigraphic verifica- tion for the biochronologically ambiguous taxon Megaleptictis, and the possible presence of new leporid and hypertragulid taxa.
    [Show full text]
  • Novttates PUBLISHED by the AMERICAN MUSEUM of NATURAL HISTORY CENTRAL PARK WEST at 79TH STREET NEW YORK, N.Y
    NAMERICAN MUSEUM Novttates PUBLISHED BY THE AMERICAN MUSEUM OF NATURAL HISTORY CENTRAL PARK WEST AT 79TH STREET NEW YORK, N.Y. 10024 U.S.A. NUMBER 2596 JUNE 4, 1976 BERYL E. TAYLOR AND S. DAVID WEBB Miocene Leptomerycidae (Artiodactyla, Ruminantia) and Their Relationships 4 AMERICAN MUSEUM Norntates PUBLISHED BY THE AMERICAN MUSEUM OF NATURAL HISTORY CENTRAL PARK WEST AT 79TH STREET, NEW YORK, N.Y. 10024 Number 2596, pp. 1-22, figs. 1-7, tables 1-5 June 4, 1976 Miocene Leptomerycidae (Artiodactyla, Ruminantia) and Their Relationships BERYL E. TAYLOR1 AND S. DAVID WEBB2 ABSTRACT Leptomerycidae, previously thought to have Montana and possibly South Dakota is trans- survived only into the Arikareean, are here recog- ferred to the Leptomerycidae from incertae sedis nized from the medial Miocene (late Hemingford- in the Cervidae. ian into Valentinian) deposits of New Mexico, The relationships between these late Lepto- Texas, and Nebraska. These late-surviving Lepto- merycidae and contemporaneous Blastomery- merycidae belong to the species Pseudoparablas- cinae are shown to be remote despite several tomeryx scotti and P. francescita, previously parallel features in common. Separation of the assigned to the Blastomerycinae. Likewise, Pro- family Leptomerycidae from the family Hyper- nodens silberlingi from Arikareean deposits in tragulidae is advocated. INTRODUCTION The small Oligocene traguloid, Leptomeryx additional evidence to support the Leptomeryci- evansi, is probably the most abundant ungulate dae as.a distinct family and to recognize the sur- in the vast collections of fossil vertebrates from vival of two leptomerycid genera into much the White River Badlands of South Dakota (Clark younger stages of the Miocene.
    [Show full text]
  • Did Impacts, Volcanic Eruptions, Or Climate Change Affect Mammalian Evolution?
    Palaeogeography, Palaeoclimatology, Palaeoecology 214 (2004) 283–294 www.elsevier.com/locate/palaeo Did impacts, volcanic eruptions, or climate change affect mammalian evolution? Donald R. Prothero* Department of Geology, Occidental College, Los Angeles, CA 90041, USA Received 30 June 2003; received in revised form 13 April 2004; accepted 20 April 2004 Abstract In recent years, it has become popular to attribute faunal change and mass extinction to impacts, volcanic eruptions, or climatic change. How well do these supposed causes compare to the excellent record of Cenozoic life, especially that of fossil mammals? Two different Cenozoic mammal diversity curves were compared, and important climatic, volcanic, and impact horizons were examined in detail. In no case is there a strong correlation between impacts, eruptions, or climatic events and any episode of mammalian turnover. On the contrary, most of the known impact, eruption, and climatic events of the Cenozoic occurred during intervals of faunal stability. Conversely, episodes of high turnover and faunal change among Cenozoic mammals correlate with no known extrinsic causes. Apparently, extrinsic environmental factors such as impacts, eruptions, and climate change have a minimal effect, and intrinsic biological factors must be more important. D 2004 Elsevier B.V. All rights reserved. Keywords: Cenozoic; Mammals; Evolution 1. Introduction events. Specifically, the impacts of the late Eocene were originally blamed for the Eocene–Oligocene Conventional Neo-Darwinian theory has long extinctions (Alvarez et al., 1982; Asaro et al., 1982), argued that species are well adapted to their environ- although later work has not substantiated this (Pro- ment and should respond with adaptation and evolu- thero, 1994).
    [Show full text]
  • An Analysis of Anchitherine Equids Across the Eocene–Oligocene Boundary in the White River Group of the Western Great Plains
    University of Nebraska - Lincoln DigitalCommons@University of Nebraska - Lincoln Dissertations & Theses in Earth and Earth and Atmospheric Sciences, Department Atmospheric Sciences of 2010 An Analysis of Anchitherine Equids Across the Eocene–Oligocene Boundary in the White River Group of the Western Great Plains David M. Masciale University of Nebraska at Lincoln, [email protected] Follow this and additional works at: https://digitalcommons.unl.edu/geoscidiss Part of the Geology Commons, Paleobiology Commons, and the Paleontology Commons Masciale, David M., "An Analysis of Anchitherine Equids Across the Eocene–Oligocene Boundary in the White River Group of the Western Great Plains" (2010). Dissertations & Theses in Earth and Atmospheric Sciences. 11. https://digitalcommons.unl.edu/geoscidiss/11 This Article is brought to you for free and open access by the Earth and Atmospheric Sciences, Department of at DigitalCommons@University of Nebraska - Lincoln. It has been accepted for inclusion in Dissertations & Theses in Earth and Atmospheric Sciences by an authorized administrator of DigitalCommons@University of Nebraska - Lincoln. AN ANALYSIS OF ANCHITHERINE EQUIDS ACROSS THE EOCENE– OLIGOCENE BOUNDARY IN THE WHITE RIVER GROUP OF THE WESTERN GREAT PLAINS by David M. Masciale A THESIS Presented to the Faculty of The Graduate College at the University of Nebraska In Partial Fulfillment of Requirements For the Degree of Master of Science Major: Geosciences Under the Supervision of Professors Ross Secord and Robert M. Hunt, Jr. Lincoln, NE April, 2010 AN ANALYSIS OF ANCHITHERINE EQUIDS ACROSS THE EOCENE– OLIGOCENE BOUNDARY IN THE WHITE RIVER GROUP OF THE WESTERN GREAT PLAINS David M. Masciale, M.S. University of Nebraska, 2010 Advisers: Ross Secord and Robert M.
    [Show full text]
  • Postulating Pressures 8Th Grade
    Postulating Pressures 8th Grade Duration Concepts Pre-Visit: 30-50 minutes Natural Selection is the mechanism by which evolution occurs. Museum Visit: 60 minutes Genetic variation and environmental pressures are important parts of Post Visit: 50 minutes natural selection, and thus evolution. Location Evidence from geology, fossils and comparative anatomy provide the Age of Mammals Hall bases for the theory of evolution. Supplies Extinction of a species occurs when the environment changes and the characteristics of a species are insufficient for its survival. Worksheet Pencil Objectives Clipboard (optional) Students will formulate hypotheses about selection pressures on an Standards organism based on observations. NGSS MS-LS1-4, MS-LS2-1, MS-LS2 Students will research an organism to find if their hypotheses are -3, MS-LS4-1, MS-LS4-2, MS- supported by evidence. LS4-2, MS-LS4-4, LS4.A, LS4.B, LS4.C Students will choose a project in which they will use present and S+E Practices apply their research. 1, 2, 3, 4, 6, 7, 8 CCSS ELA Outline W.1.2.3.4.7.9, WHST.1.2.7.8.9, L.2 In one classroom session before visiting the Museum, review vocabulary and the concept of evolution by natural selection. Have CA State students select a mammal to focus on for their research paper and Writing Applications begin formulating hypotheses. 2.3.a.b.c.d Investigation and During a trip to the Museum, students will explore the Age of Experimentation 9.a Mammals hall and begin researching their animals natural history. Vocabulary Back in the classroom and or at home, students continue independent Evolution · Climate · research choose one project from the Task Sheet to showcase their Adaptation · Predator · findings.
    [Show full text]
  • Changes in Mammalian Abundance Through the Eocene-Oligocene
    University of Nebraska - Lincoln DigitalCommons@University of Nebraska - Lincoln Dissertations & Theses in Earth and Atmospheric Earth and Atmospheric Sciences, Department of Sciences Summer 7-30-2019 Changes in Mammalian Abundance Through the Eocene-Oligocene Climate Transition in the White River Group of Nebraska, USA Robert Gillham University of Nebraska - Lincoln, [email protected] Follow this and additional works at: https://digitalcommons.unl.edu/geoscidiss Part of the Oceanography and Atmospheric Sciences and Meteorology Commons, Paleobiology Commons, and the Paleontology Commons Gillham, Robert, "Changes in Mammalian Abundance Through the Eocene-Oligocene Climate Transition in the White River Group of Nebraska, USA" (2019). Dissertations & Theses in Earth and Atmospheric Sciences. 120. https://digitalcommons.unl.edu/geoscidiss/120 This Article is brought to you for free and open access by the Earth and Atmospheric Sciences, Department of at DigitalCommons@University of Nebraska - Lincoln. It has been accepted for inclusion in Dissertations & Theses in Earth and Atmospheric Sciences by an authorized administrator of DigitalCommons@University of Nebraska - Lincoln. Changes in Mammalian Abundance Through the Eocene- Oligocene Climate Transition in the White River Group of Nebraska, USA By Robert B. Gillham A THESIS Presented to the Faculty of The Graduate College at the University of Nebraska In Partial Fulfillment of Requirements For the Degree of Master of Science Major: Geosciences Under the Supervision of Professor Ross Secord Lincoln, NE August, 2019 Changes in Mammalian Abundance Through the Eocene- Oligocene Climate Transition in the White River Group of Nebraska, USA Robert B. Gillham M.S. University of Nebraska, 2019 Advisor: Ross Secord Marine records show major cooling during the Eocene-Oligocene Climate Transition (EOCT).
    [Show full text]
  • Fossil Catalog #29
    GEOLOGICAL ENTERPRISES P.O. BOX 996 -- ARDMORE, OKLAHOMA 73402 USA phone 580-223-8537 fax 580-223-6965 email [email protected] website WWW.GEOLOGICALENTERPRISES.COM FOSSIL CATALOG #29 GEOLOGICAL ENTERPRISES, INC. P.O. BOX 996 ARDMORE, OKLAHOMA U.S.A. 73402 Phone 580-223-8537 Fax 580-223-6965 email [email protected] VISIT US ON THE WEB @ www.geologicalenterprises.com PLEASE TAKE CARE OF THIS CATALOG: Due to the high costs of printing and mailing, we will only issue a new catalog periodically. We literally send out thousands of these to Universities worldwide at no charge. These catalogs are used by Professors and students, for reference, and in some cases, as text books. We will continue to issue our yearly bulletin, which will contain additions to this catalog. We pledge to keep the quality of the specimens listed here as high as possible. We attempt to secure the finest available specimens at all times. Complete geological data accompanies all specimens. TERMS: We accept VISA, MasterCard, Discover Card, Personal or Company Checks, Money Orders and Pay Pal. (Please use our regular email address [email protected] for PayPal) To recognized educational and corporate institutions, our terms are Net-30 days. All other orders should be prepaid. We accept only checks drawn on U.S. Banks. Wire transfers are also acceptable. Please be aware Wire transfers may incur a fee. All prices are F.O.B. Ardmore, Oklahoma. Please allow for postage(5% is usually sufficient. $8.00 minimum). Overpayments will be promptly refunded. WEBSITE: Our Catalog is also available on our website in color! It’s truly beautiful.
    [Show full text]
  • 0520237315.Pdf
    Beasts of Eden The publisher gratefully acknowledges the generous contribution to this book provided by the General Endowment Fund of the University of California Press Associates. Beasts of Eden walking whales, dawn horses, and other enigmas of mammal evolution David Rains Wallace university of california press berkeley los angeles london University of California Press Berkeley and Los Angeles, California University of California Press, Ltd. London, England © 2004 by the Regents of the University of California Library of Congress Cataloging-in-Publication Data Wallace, David Rains, 1945–. Beasts of Eden : walking whales, dawn horses, and other enigmas of mammal evolution / David Rains Wallace. p. cm. Includes bibliographical references and index. isbn 0-520-23731-5 (alk. paper). 1. Mammals—Evolution. 2. Mammals, Fossil. I. Title. ql708.5.w25 2004 599.138—dc22 2003022857 Manufactured in the United States of America 13 12 11 10 09 08 07 06 05 04 10987654 321 Printed on Ecobook 50 containing a minimum 50% post-consumer waste, processed chlorine free. The balance contains virgin pulp, including 25% Forest Stewardship Council Certified for no old growth tree cutting, processed either tcf or ecf. The sheet is acid-free and meets the minimum requirements of ansi/niso z39.48-1992 (r 1997) (Permanence of Paper). ᭺ϱ to steve fisher, who brings art to science Actually most scientific problems are far better understood by studying their history than their logic. ernst mayr quoted in Leo F. Laporte, George Gaylord Simpson: Paleontologist and Evolutionist contents list of illustrations /xi acknowledgments / xiii prologue. the fresco and the fossil /xv 1 / Pachyderms in the Catacombs /1 2 / Dr.
    [Show full text]