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Chronology and Faunal Evolution of the Middle Eocene Bridgerian North American Land Mammal “Age”: Achieving High Precision Geochronology Kaori Tsukui Submitted in partial fulfillment of the requirements for the degree of Doctor of Philosophy in the Graduate School of Arts and Sciences COLUMBIA UNIVERSITY 2016 © 2015 Kaori Tsukui All rights reserved ABSTRACT Chronology and Faunal Evolution of the Middle Eocene Bridgerian North American Land Mammal “Age”: Achieving High Precision Geochronology Kaori Tsukui The age of the Bridgerian/Uintan boundary has been regarded as one of the most important outstanding problems in North American Land Mammal “Age” (NALMA) biochronology. The Bridger Basin in southwestern Wyoming preserves one of the best stratigraphic records of the faunal boundary as well as the preceding Bridgerian NALMA. In this dissertation, I first developed a chronological framework for the Eocene Bridger Formation including the age of the boundary, based on a combination of magnetostratigraphy and U-Pb ID-TIMS geochronology. Within the temporal framework, I attempted at making a regional correlation of the boundary-bearing strata within the western U.S., and also assessed the body size evolution of three representative taxa from the Bridger Basin within the context of Early Eocene Climatic Optimum. Integrating radioisotopic, magnetostratigraphic and astronomical data from the early to middle Eocene, I reviewed various calibration models for the Geological Time Scale and intercalibration of 40Ar/39Ar data among laboratories and against U-Pb data, toward the community goal of achieving a high precision and well integrated Geological Time Scale. In Chapter 2, I present a magnetostratigraphy and U-Pb zircon geochronology of the Bridger Formation from the Bridger Basin in southwestern Wyoming. -
Attachment J Assessment of Existing Paleontologic Data Along with Field Survey Results for the Jonah Field
Attachment J Assessment of Existing Paleontologic Data Along with Field Survey Results for the Jonah Field June 12, 2007 ABSTRACT This is compilation of a technical analysis of existing paleontological data and a limited, selective paleontological field survey of the geologic bedrock formations that will be impacted on Federal lands by construction associated with energy development in the Jonah Field, Sublette County, Wyoming. The field survey was done on approximately 20% of the field, primarily where good bedrock was exposed or where there were existing, debris piles from recent construction. Some potentially rich areas were inaccessible due to biological restrictions. Heavily vegetated areas were not examined. All locality data are compiled in the separate confidential appendix D. Uinta Paleontological Associates Inc. was contracted to do this work through EnCana Oil & Gas Inc. In addition BP and Ultra Resources are partners in this project as they also have holdings in the Jonah Field. For this project, we reviewed a variety of geologic maps for the area (approximately 47 sections); none of maps have a scale better than 1:100,000. The Wyoming 1:500,000 geology map (Love and Christiansen, 1985) reveals two Eocene geologic formations with four members mapped within or near the Jonah Field (Wasatch – Alkali Creek and Main Body; Green River – Laney and Wilkins Peak members). In addition, Winterfeld’s 1997 paleontology report for the proposed Jonah Field II Project was reviewed carefully. After considerable review of the literature and museum data, it became obvious that the portion of the mapped Alkali Creek Member in the Jonah Field is probably misinterpreted. -
Description and Correlation of Eocene Rocks in Stratigraphie Reference Sections for the Green River and Washakie Basins, Southwest Wyoiming
Description and Correlation of Eocene Rocks in Stratigraphie Reference Sections for the Green River and Washakie Basins, Southwest Wyoiming U.S. GEOLOGICAL SURVEY PROFESSIONAE PAPER 1506-D Description and Correlation of Eocene Rocks in Stratigraphic Reference Sections for the Green River and Washakie Basins, Southwest Wyoming By HENRY W. ROEHLER GEOLOGY OF THE EOCENE WASATCH, GREEN RIVER, AND BRIDGER (WASHAKIE) FORMATIONS, GREATER GREEN RIVER BASIN, WYOMING, UTAH, AND COLORADO U.S. GEOLOGICAL SURVEY PROFESSIONAL PAPER 1506-D Includes analyses of Eocene rocks in the Washakie basin UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1992 U.S. DEPARTMENT OF THE INTERIOR MANUEL LUJAN, JR., Secretary U.S. GEOLOGICAL SURVEY Dallas L. Peck, Director Any use of trade, product, or firm names in this publication is for descriptive purposes only and does not imply endorsement by the U.S. Government Library of Congress Cataloging in Publication Data Roehler, Henry W. Description and correlation of Eocene rocks in stratigraphic reference sections for the Green River and Washakie basins, Southwest Wyoming : includes analyses of Eocene rocks in the Washakie Basin / by Henry W. Roehler. p. cm. (Geology of the Eocene Wasatch, Green River and Bridger (Washakie) formations, greater Green River Basin, Wyoming, Utah, and Colorado) (U.S. Geological Survey professional paper ; 1506-D) Includes bibliographical references. Supt. of Docs, no.: I 19.16:1506-D 1. Geology, Stratigraphic Eocene. 2. Stratigraphic correlation Wyoming. 3. Geology Wyoming. I. Title. II. Series. III. Series: U.S. Geological Survey professional paper : 1506-D. QE692.2.R58 1992 551.7'84'09787 dc20 91-4442 CIP For sale by Book and Open-File Report Sales, U.S. -
Rapid and Early Post-Flood Mammalian Diversification Videncede in the Green River Formation
The Proceedings of the International Conference on Creationism Volume 6 Print Reference: Pages 449-457 Article 36 2008 Rapid and Early Post-Flood Mammalian Diversification videncedE in the Green River Formation John H. Whitmore Cedarville University Kurt P. Wise Southern Baptist Theological Seminary Follow this and additional works at: https://digitalcommons.cedarville.edu/icc_proceedings DigitalCommons@Cedarville provides a publication platform for fully open access journals, which means that all articles are available on the Internet to all users immediately upon publication. However, the opinions and sentiments expressed by the authors of articles published in our journals do not necessarily indicate the endorsement or reflect the views of DigitalCommons@Cedarville, the Centennial Library, or Cedarville University and its employees. The authors are solely responsible for the content of their work. Please address questions to [email protected]. Browse the contents of this volume of The Proceedings of the International Conference on Creationism. Recommended Citation Whitmore, John H. and Wise, Kurt P. (2008) "Rapid and Early Post-Flood Mammalian Diversification Evidenced in the Green River Formation," The Proceedings of the International Conference on Creationism: Vol. 6 , Article 36. Available at: https://digitalcommons.cedarville.edu/icc_proceedings/vol6/iss1/36 In A. A. Snelling (Ed.) (2008). Proceedings of the Sixth International Conference on Creationism (pp. 449–457). Pittsburgh, PA: Creation Science Fellowship and Dallas, TX: Institute for Creation Research. Rapid and Early Post-Flood Mammalian Diversification Evidenced in the Green River Formation John H. Whitmore, Ph.D., Cedarville University, 251 N. Main Street, Cedarville, OH 45314 Kurt P. Wise, Ph.D., Southern Baptist Theological Seminary, 2825 Lexington Road. -
Phylogeny of Early Tertiary Carnivora, with a Description of a New Species of Protictis from the Middle Eocene of Northwestern Wyoming
AMERICAN MUSEUM Nov itates PUBLISHED BY THE AMERICAN MUSEUM OF NATURAL HISTORY CENTRAL PARK WEST AT 79TH STREET, NEW YORK, N.Y. 10024 Number 2725, pp. 1-64, figs. 1-9, tables 1, 2 April 15, 1982 Phylogeny of Early Tertiary Carnivora, With a Description of a New Species of Protictis From the Middle Eocene of Northwestern Wyoming JOHN J. FLYNN1 AND HENRY GALIANO2 ABSTRACT Since Cope erected the Miacidae in 1880, all for the suprageneric taxa Carnivora, Feliformia, early Tertiary carnivorans have generally been Caniformia, Didymictidae (Didymictida) (new), grouped in this family because of their overall Aeluroida (new), Feloidea, and Viverravidae. primitive morphology. A historical review of the Protictis, including the subgenera P. (Protictis), classifications and definitions of the Miacidae is P. (Bryanictis), and P. (Protictoides) (new), is provided. Discovery of a new subgenus of Pro- diagnosed and discussed. Simpsonictis is consid- tictis from the Uintan (mid Eocene) of north- ered a valid genus and is allied with Viverravus western Wyoming led to a reevaluation of the in the Viverravidae (Aeluroida, Feliformia). Pa- phylogeny of the Carnivora. The Miacidae (Mia- laeogale is removed from the Mustelidae (Cani- coidea), as previously constructed, is a paraphy- formia) and is considered a close relative of the letic assemblage of all the early Tertiary Carniv- Viverravidae. Ictidopappus is placed incertae ora. Phylogenetic analysis of the distribution of sedis within the Aeluroida. "Plesiomiacis" and cranial, dental, and postcranial morphology indi- Quercygale, which were previously considered cates that the bipartite division recognized in liv- members of the "Viverravinae," are considered ing Carnivora may be traced to the earliest Ter- members of the Caniformia. -
Brief Report Acta Palaeontologica Polonica 55 (4): 761–764, 2010
Brief report Acta Palaeontologica Polonica 55 (4): 761–764, 2010 A new genus of “miacid” carnivoran from the earliest Eocene of Europe and North America THIERRY SMITH and RICHARD SMITH “Miacid” carnivorans comprise one of the modern mammal groups from North America (Smith et al. 1996; Smith and groups appearing around the Palaeocene–Eocene Thermal Smith 2001; Smith et al. 2006). Here we describe a new genus Maximum (PETM) in the Northern Hemisphere. Here we of a very small and primitive “miacid” carnivoran that is pres− describe a new very small “miacid” carnivoran from the ent in Dormaal and other early Eocene localities of northwest− earliest Eocene of Dormaal, Belgium, that shares a particu− ern Europe and in the early Eocene of Wyoming (Wa−0 to lar dental morphology with the species “Miacis” winkleri Wa−2, early Wasatchian NALMA). It shows characters that are and “Miacis” rosei from the early Eocene of North America. quite distinct from those of other “miacid” genera, indicating The three species present very gracile and sharp teeth, and higher morphological diversity among basal “miacids” than are hereby placed in the new genus Gracilocyon.Compara− previously thought. tive dental analysis of Gracilocyon with other early “mia− cids” contributes to better resolve the polarity of dental Institutional abbreviations.—IRSNB, Institut royal des Scien− characters and indicates that this genus is one of the most ces naturelles de Belgique, Brussels, Belgium; UCMP, Univer− primitive members of the family. Diversity of early modern sity of California Museum of Paleontology, Berkeley, USA; carnivorans is greater than previously considered and early UM(VP), University of Michigan (Vertebrate Paleontology), “miacids” seem to have dispersed into North America from Ann Arbor, USA; YPM, Yale Peabody Museum−Princeton Col− two different geographic origins. -
On the Origin of Cats and Carnivores
On the Origin of Cats and Carnivores A.W. (BILL) MEHLERT ABSTRACT Creation scientists are working on ways to identify the biblical ‘kinds’; the created units or groups as described in the book of Genesis. Evolutionists classify on the assumption of common ancestry and morphological similarities and differences. These two approaches are diametrically opposed. Creationists can reasonably employ similarities to construct non- evolutionary ‘trees’ which are in accord with scriptural constraints and do not clash with known scientific facts. It is proposed to study the cats of the world and the origins of the felines and carnivores, and to suggest a non- macroevolutionary hypothesis; one which is in accord with creationist thinking. INTRODUCTION bears, raccoons, etc. in one single order, are the following: (i) Most are predators, with the exception of the pandas. Cats, large and small, are among the most beautiful and (ii) Most modern forms possess slicing or shearing teeth graceful of all God’s creatures. They are classified by called carnassials.4 The triangular cusps of the evolutionists as carnivores along with dogs, weasels, bears carnassials allow cats and other carnivores to slice and hyenas, and are quite varied in morphology and through the toughest of flesh and gristle, which results behaviour. Cats have so far not been the subject of detailed in the familiar eating habit of turning the head to one creationist discussion, and the time is now opportune for side as the animal shears off chunks of meat. The such an examination. carnassials are believed by transformists to have evolved Most of the differences between and within the four from ancestors whose fourth upper premolar (P4) and existing feline genera relate to size, colour and behaviour; first lower molar (M1) became adapted to slice or shear yet the unmistakeable stamp of their type can be clearly seen the flesh of their prey. -
Systematics of Early Eocene Miacidae (Mammalia, Carnivora) in the Clark's Fork Basin, Wyoming
CONTRIBUTIONS FROM THE MUSEUM OF PALEONTOLOGY THE UNIVERSITY OF MICHIGAN VOL. 26, NO. 10, p. 197-225 December 3 1, 1983 SYSTEMATICS OF EARLY EOCENE MIACIDAE (MAMMALIA, CARNIVORA) IN THE CLARK'S FORK BASIN, WYOMING BY PHILIP D. GINGERICH MUSEUM OF PALEONTOLOGY THE UNIVERSITY OF MICHIGAN ANN ARBOR CONTRIBUTIONS FROM THE MUSEUM OF PALEONTOLOGY Philip D. Gingerich, Director Gerald R. Smith, Editor This series of contributions from the Museum of Paleontology is a medium for the publication of papers based chiefly upon the collection in the Museum. When the number of pages issued is sufficient to make a volume, a title page and a table of contents will be sent to libraries on the mailing list, and to individuals upon request. A list of the separate papers may also be obtained. Correspondence should be directed to the Museum of Paleontology, The University of Michigan, Ann Arbor, Michigan, 48109. VOLS. 11-XXVI. Parts of volumes may be obtained if available. Price lists available upon inquiry. SYSTEMATICS OF EARLY EOCENE MIACIDAE (MAMMALIA, CARNIVORA) IN THE CLARK'S FORK BASIN, WYOMING BY Philip D. Gingerich Abstract.-Four genera and six species of Miacidae are known from faunas representing the Clarkforkian through middle Wasatchian land-mammal ages in the Clark's Fork Basin, Wyoming. These are, in order of appearance, Uintacyon rudis, Miacis winkleri (n. sp.), Miacis deutschi (n. sp.), Miacis exiguus, Vassacyon promicrodon, and Vulpavus cf. australis. In addition, one new miacid, Miacispetilus (n. sp.), is described from middle Wasatchian strata of the central Bighorn Basin. It includes many middle to late Wasatchian specimens formerly referred to M. -
New Specimens of Sparassodonta (Mammalia, Metatheria) From
NEW SPECIMENS OF SPARASSODONTA (MAMMALIA, METATHERIA) FROM CHILE AND BOLIVIA by RUSSELL K. ENGELMAN Submitted in partial fulfillment of the requirements for the degree of Master of Science Department of Biology CASE WESTERN RESERVE UNIVERSITY January, 2019 CASE WESTERN RESERVE UNIVERSITY SCHOOL OF GRADUATE STUDIES We hereby approve the thesis/dissertation of Russell K. Engelman candidate for the degree of Master of Science*. Committee Chair Hillel J. Chiel Committee Member Darin A. Croft Committee Member Scott W. Simpson Committee Member Michael F. Benard Date of Defense July 20, 2018 *We also certify that written approval has been obtained for any proprietary material contained therein. ii TABLE OF CONTENTS NEW SPECIMENS OF SPARASSODONTA (MAMMALIA, METATHERIA) FROM CHILE AND BOLIVIA ....................................................................................................... i TABLE OF CONTENTS ................................................................................................... iii LIST OF TABLES ............................................................................................................. vi LIST OF FIGURES .......................................................................................................... vii ACKNOWLEDGEMENTS ................................................................................................ 1 LIST OF ABBREVIATIONS ............................................................................................. 4 ABSTRACT ....................................................................................................................... -
The Sage Creek Mountain Local Fauna of the Bridger Formation Near Lonetree, Wyoming
Brigham Young University BYU ScholarsArchive Theses and Dissertations 1977-08-01 The Sage Creek Mountain local fauna of the Bridger Formation near Lonetree, Wyoming Steven W. Barker Brigham Young University - Provo Follow this and additional works at: https://scholarsarchive.byu.edu/etd Part of the Life Sciences Commons BYU ScholarsArchive Citation Barker, Steven W., "The Sage Creek Mountain local fauna of the Bridger Formation near Lonetree, Wyoming" (1977). Theses and Dissertations. 7620. https://scholarsarchive.byu.edu/etd/7620 This Thesis is brought to you for free and open access by BYU ScholarsArchive. It has been accepted for inclusion in Theses and Dissertations by an authorized administrator of BYU ScholarsArchive. For more information, please contact [email protected], [email protected]. I.dz. I f}1f-l Jf11 A 'lhesis De_pe:r.tment of Zoology Br1gham Young Universjty In Partial Fulfillment of the Requirements for the Degree Master of Science August 1977 'I.Li_ s tLesls by Steven W Barker is accepted in its present :fonr, bJ -Lbe Dep::i..Ttrr.ent of Zoolol::;y- o:r' Brigham Young University as satisf;yi1.tg the thed.s requi:remnit :fer the degree of Master of ScienC€. i:l A CKNOWLF:!DGBMRNTS Grateful acknowledsement lr; made for the guidance and assistance given by the chairma.n of my a.clvisory com.mittee, Dr. Wade E. Miller, and. the otba:r: ccmmi ttee members, Dr. J. Keith Rigby Sr, and Dr. Clive D. Jorgensen. Acknowledgement i.s also given to Dr. J, Keith Rigby Jr, a.nd Dr, Robert M. West for their valuable suggestions and guidance. -
Carnivorous Mammals from the Middle Eocene Washakie Formation, Wyoming, USA, and Their Diversity Trajectory in a Post-Warming World
Journal of Paleontology, Volume 95, Memoir 82, 2021, p. 1–115 Copyright © The Author(s), 2021. Published by Cambridge University Press on behalf of The Paleontological Society. All rights reserved. This is an Open Access article, distributed under the terms of the Creative Commons Attribution licence (http://creativecommons.org/licenses/ by/4.0/), which permits unrestricted re-use, distribution, and reproduction in any medium, provided the original work is properly cited. 0022-3360/21/1937-2337 doi: 10.1017/jpa.2020.74 Carnivorous mammals from the middle Eocene Washakie Formation, Wyoming, USA, and their diversity trajectory in a post-warming world Susumu Tomiya,1,2,3 Shawn P. Zack,4 Michelle Spaulding,5 and John J. Flynn2,6 1Center for International Collaboration and Advanced Studies in Primatology, Kyoto University Primate Research Institute, 41-2 Kanrin, Inuyama, Aichi 484-8506, Japan <[email protected]> 2Negaunee Integrative Research and Gantz Family Collections Centers, Field Museum of Natural History, 1400 South Lake Shore Drive, Chicago, Illinois 60605, USA 3University of California Museum of Paleontology, Berkeley, California 94720, USA 4Department of Basic Medical Sciences, University of Arizona College of Medicine, 425 N Fifth Street, Phoenix, Arizona 85004, USA <[email protected]> 5Department of Biological Sciences, Purdue University Northwest, 1401 S US Highway 421, Westville, Indiana 46391, USA <mspauldi@ pnw.edu> 6Richard Gilder Graduate School and Division of Paleontology, American Museum of Natural History, 200 Central Park West, New York, New York 10024, USA <jfl[email protected]> Abstract.—The middle Eocene Washakie Formation of Wyoming, USA, provides a rare window, within a single deposi- tional basin, into the faunal transition that followed the early Eocene warming events. -
FOSSIL MAMMALS and the AGE of the Changxindlan FORMATION, NORTHEASTERN CHINA
FOSSIL MAMMALS AND THE AGE OF THE CHANGXINDlAN FORMATION, NORTHEASTERN CHINA by Spencer G. LUCAS * CONTENTS Page Abstrac~ Resume. .. 134 Introduction ..................................................................... 134 Taxonomy ...................................................................... 134 Eutheria ................................................................... " 134 Hypsimilus beijingellsis ZHAI, 1977 .............................................. 135 ef. Miacis sp. ................................................................ 135 Forstercooperia grandis (PETERSON, 1919) ....................................... 136 Anthraeotheriidae ............................................................. 137 Age ..................................................... , ............ , , ...... " 137 Acknowledgments .............................................................. " 139 References ..................... ,................................................ 139 Legend of the plate. 140 * New Mexico Museum of Natural History & Science, 1801 Mountain Road N. W., Albuquerque, New Mexico 87104, U.S.A. Key-words: Fossil mammals, Eocene, China, Changxindian Fonnation. Mots-cles: Mammiteres fossiles, Eocene, Chine, Fonnation Changxindian, Palaeovertebrata, Montpellier, Vol. jubil. D,E. Russell CM Godinot & P.D. Gingerich Eels.), 25 (2-4): 133-140, 2 fig., 1 pI. (Rc9u le 17 Juin 1994, accepte le 21 Fevrier 1995, public le 16 Dccembre 1996) ABSTRACT Re-evaluation of the small collection of mammal fossils from the Changxindian