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(Mammalia) in the Early Eocene Ofeurope
The presence of Taeniodonta (Mammalia) in the Early Eocene ofEurope Carmen ESTRAVIS* Donald E. RUSSELL** * Centro de Estratigrafia e Palcobiologia da UNL, Faculdade de Ciencias e Tecnologia, Quinta da Torre, P-2825 Monte de Caparica, Portugal. ** Institut de Paleontologic (URA 12, CNRS), 8 rue Buffon, 75005 Paris, France. pp.191-201 Ciencias da Terra (UNL) Lisboa NQ 11 1992 1 pI. RESUMO Palavras-chave: Eurodon- Taeniodonta- Eocenico-:- Silveirinha - Portugal. Eurodon silveirinhensis nov. gen., nov. sp., do Eocenico inferior de Silveirinha (portugal) econsiderado o primeiro representante, na Europa, da extinta ordem de mamiferosTaeniodonta.0 enigrnaticogeneroLessnessina Hooker, 1979, de Abbey Wood(lnglaterra), sensive1mente contcrnporaneo de Eurodon, e tambern atribufdo aos teniodontes. RESUME Mots-dis: Eurodon - Taeniodonta - Eocene Silveirinha - Portugal. Eurodon silveirinhensis nov. gen., nov. sp., de I'Eocene infericur de Silveirinha (portugal) est interpretee commeIapremiererepresentanteen Europedes Taeniodonta (ordre eteint de mammiferes). L'enigmatique genre Lessnessina Hooker, 1979, de Abbey Wood (Angleterre), apeu pres contemporainde Eurodon,estrapporteegalement aux Taeniodonta. ABSTRACT Key-words: Eurodon - Taeniodonta - Eocene Silveirinha - Portugal. The first representative of the extinct mammalian order Taeniodonta in Europe is described, Eurodon silveirinhensis n. gen., n. sp., from the early Eocene local ity of Silveirinha, Portugal. A formerly enigmatic form, Lessnessina Hooker, 1979, from Abbey Wood, England, and approximately contemporary, is also referred to the Taeniodonta. 193 INTRODUCTION Type species - Eurodon silveirinhensis, new species. Study of the early Eocene mammalian fauna Diagnosis - Small mammal, smaller than any from Silveirinha, Portugal (ANTUNES, 1981; described taeniodont. M3 with large hypoconulid, ANTUNES & RUSSELL, 1981), is the subject of a apparently subequal hypoconid and slightly smaller, doctoral dissertation for one ofus (c. -
United States
DEPARTMENT OF THE INTERIOR BULLETIN OF THE UNITED STATES ISTo. 146 WASHINGTON GOVERNMENT Pit IN TING OFFICE 189C UNITED STATES GEOLOGICAL SURVEY CHAKLES D. WALCOTT, DI11ECTOK BIBLIOGRAPHY AND INDEX NORTH AMEEICAN GEOLOGY, PALEONTOLOGY, PETEOLOGT, AND MINERALOGY THE YEA.R 1895 FEED BOUGHTON WEEKS WASHINGTON Cr O V E U N M K N T P K 1 N T I N G OFFICE 1890 CONTENTS. Page. Letter of trail smittal...... ....................... .......................... 7 Introduction.............'................................................... 9 List of publications examined............................................... 11 Classified key to tlio index .......................................... ........ 15 Bibliography ............................................................... 21 Index....................................................................... 89 LETTER OF TRANSMITTAL DEPARTMENT OF THE INTEEIOE, UNITED STATES GEOLOGICAL SURVEY, DIVISION OF GEOLOGY, Washington, D. 0., June 23, 1896. SIR: I have the honor to transmit herewith the manuscript of a Bibliography and Index of North American Geology, Paleontology, Petrology, and Mineralogy for the year 1895, and to request that it be published as a bulletin of the Survey. Very respectfully, F. B. WEEKS. Hon. CHARLES D. WALCOTT, Director United States Geological Survey. 1 BIBLIOGRAPHY AND INDEX OF NORTH AMERICAN GEOLOGY, PALEONTOLOGY, PETROLOGY, AND MINER ALOGY FOR THE YEAR 1895. By FRED BOUGHTON WEEKS. INTRODUCTION. The present work comprises a record of publications on North Ameri can geology, paleontology, petrology, and mineralogy for the year 1895. It is planned on the same lines as the previous bulletins (Nos. 130 and 135), excepting that abstracts appearing in regular periodicals have been omitted in this volume. Bibliography. The bibliography consists of full titles of separate papers, classified by authors, an abbreviated reference to the publica tion in which the paper is printed, and a brief summary of the con tents, each paper being numbered for index reference. -
Resolving the Relationships of Paleocene Placental Mammals
Biol. Rev. (2015), pp. 000–000. 1 doi: 10.1111/brv.12242 Resolving the relationships of Paleocene placental mammals Thomas J. D. Halliday1,2,∗, Paul Upchurch1 and Anjali Goswami1,2 1Department of Earth Sciences, University College London, Gower Street, London WC1E 6BT, U.K. 2Department of Genetics, Evolution and Environment, University College London, Gower Street, London WC1E 6BT, U.K. ABSTRACT The ‘Age of Mammals’ began in the Paleocene epoch, the 10 million year interval immediately following the Cretaceous–Palaeogene mass extinction. The apparently rapid shift in mammalian ecomorphs from small, largely insectivorous forms to many small-to-large-bodied, diverse taxa has driven a hypothesis that the end-Cretaceous heralded an adaptive radiation in placental mammal evolution. However, the affinities of most Paleocene mammals have remained unresolved, despite significant advances in understanding the relationships of the extant orders, hindering efforts to reconstruct robustly the origin and early evolution of placental mammals. Here we present the largest cladistic analysis of Paleocene placentals to date, from a data matrix including 177 taxa (130 of which are Palaeogene) and 680 morphological characters. We improve the resolution of the relationships of several enigmatic Paleocene clades, including families of ‘condylarths’. Protungulatum is resolved as a stem eutherian, meaning that no crown-placental mammal unambiguously pre-dates the Cretaceous–Palaeogene boundary. Our results support an Atlantogenata–Boreoeutheria split at the root of crown Placentalia, the presence of phenacodontids as closest relatives of Perissodactyla, the validity of Euungulata, and the placement of Arctocyonidae close to Carnivora. Periptychidae and Pantodonta are resolved as sister taxa, Leptictida and Cimolestidae are found to be stem eutherians, and Hyopsodontidae is highly polyphyletic. -
Additions to Knowledge of Paleocene Mammals from the North Horn Formation, Central Utah
Great Basin Naturalist Volume 55 Number 4 Article 2 10-31-1995 Additions to knowledge of Paleocene mammals from the North Horn Formation, central Utah Richard L. Cifelli University of Oklahoma, Norman Nicholas J. Czaplewski Johns Hopkins University School of Medicine, Baltimore, Maryland Kenneth D. Rose Follow this and additional works at: https://scholarsarchive.byu.edu/gbn Recommended Citation Cifelli, Richard L.; Czaplewski, Nicholas J.; and Rose, Kenneth D. (1995) "Additions to knowledge of Paleocene mammals from the North Horn Formation, central Utah," Great Basin Naturalist: Vol. 55 : No. 4 , Article 2. Available at: https://scholarsarchive.byu.edu/gbn/vol55/iss4/2 This Article is brought to you for free and open access by the Western North American Naturalist Publications at BYU ScholarsArchive. It has been accepted for inclusion in Great Basin Naturalist by an authorized editor of BYU ScholarsArchive. For more information, please contact [email protected], [email protected]. Great Basin Naturalisl55(3), C 1995, pr. 304-314 ADDITIONS TO KNOWLEDGE OF PALEOCENE MAMMALS FROM THE NORTH HORN FORMATION, CENTRAL UTAH Richard L. CifellP, Nicholas J. Czaplewsk;l, and Kenoeth D. Rose· AIlf,-n\llCT.-111e distinctive lmt inade<Juately known Paleocene faunas of central Utah are significant in that they .<;.ample ;l time interval not well represented by sequences in other areas. New materials from the Wagon Road 0ate Puercan) and Dragon (early Torrejonian) local faunas, North Horn Rlrmation, provide additional information on the c;mnposition of the assemblage.'> and systematics of included mammal taxa. The proteutherian ?PropaIaeosinopa is l"CClmled, fol' thc first time, from the Wagon Road fauna, indicating a signi6cant extension for the enigmatic family Pal1tolestidac. -
Author-Title Index
AUTHOR-TITLE INDEX A ___. Paleoecology of cyclic sediments of the lower Green River Formation, central Utah. 1969. 16(1):3- Ahlborn, R. C. Mesozoic-Cenozoic structural develop 95. ment of the Kern Mountains, eastern Nevada-western Utah. 1977. 24(2):117-131. ___ and J. K. Rigby. Studies for students no. 10: Ge ologic guide to Provo Canyon and Weber Canyon, Alexander, D. W. Petrology and petrography of the Bridal Veil Limestone Member of the Oquirrh Formation at central Wasatch Mountains, Utah. 1980. 27(3):1-33. Cascade Mountain, Utah. 1978. 25(3):11-26. ___. See Chamberlain, C. K. 1973. 20(1):79-94. Anderson, R. E. Quaternary tectonics along the inter ___. See George, S. E. 1985. 32(1):39-61. mountain seismic belt south of Provo, Utah. 1978. ___. See Johnson, B. T. 1984. 31(1):29-46. 25(1):1-10. ___. See Young, R. B. 1984. 31(1):187-211. Anderson, S. R. Stratigraphy and structure of the Sunset Bagshaw, L. H. Paleoecology of the lower Carmel Forma- Peak area near Brighton, Utah. 1974. 21(1):131-150. tion of the San Rafael Swell, Emery County, Utah. Anderson, T. C. Compound faceted spurs and recurrent 1977. 24(2):51-62. movement in the Wasatch fault zone, north central Bagshaw, R. L. Foraminiferal abundance related to bento Utah. 1977. 24(2):83-101. nitic ash beds in the Tununk Member of the Mancos Armstrong, R. M. Environmental geology of the Provo Shale (Cretaceous) in southeasternUtah. 1977. Orem area. 1975. 22(1):39-67. 24(2):33-49. -
100 Years of Managing Fossils on Federal Lands
Bulletin 34 New Mexico Museum of Natural History & Science A Division of the DEPARTMENT OF CULTURAL AFFAIRS America’s Antiquities: 100 Years of Managing Fossils on Federal Lands edited by Spencer G. Lucas, Justin A. Spielmann, Patricia M. Hester, Jason P. Kenworthy and Vincent L. Santucci Albuquerque, 2006 Bulletin 34 New Mexico Museum of Natural History & Science A Division of the DEPARTMENT OF CULTURAL AFFAIRS America’s Antiquities: 100 Years of Managing Fossils on Federal Lands edited by Spencer G. Lucas, Justin A. Spielmann, Patricia M. Hester, Jason P. Kenworthy and Vincent L. Santucci Printed with the support of the U.S. Government Albuquerque, 2006 STATE OF NEW MEXICO Department of Cultural Affairs Stuart Ashman, Secretary NEW MEXICO MUSEUM OF NATURAL HISTORY AND SCIENCE Adrian P. Hunt, Ph.D., Director BOARD OF TRUSTEES Bill Richardson, Governor, State of New Mexico, ex officio Adrian P. Hunt, Ph.D., Director, ex officio Gary Friedman, President Mary B. Gavin, Emerita Peter F. Gerity, Ph.D. Jerry Langheim Laurence Lattman, Ph.D. Morton Lieberman, Ph. D. Imogene Lindsay, Emerita John Montgomery, Ph.D. Osbjorn Pearson, Ph.D. Joseph Powell, Ph.D. Alexa Tysseling Ron V. Wilmot Cover illustration: Seventh Federal Fossil Conference logo. Disclaimer: Opinions expressed in the papers of this volume are those of the author(s) and do not necessarily reflect those of the Bureau of Land Management, National Park Service, U.S. Forest Service, Bureau of Reclamation, or other federal agency. EDITORIAL BOARD Spencer G. Lucas, Ph.D., Managing editor Adrian P. Hunt, Ph.D. Gary S. Morgan, M.S. Justin A. -
(Puercan) Periptychid 'Condylarths'
i A DESCRIPTION AND PHYLOGENETIC ANALYSIS OF THREE NEW EARLIEST PALEOCENE (PUERCAN) PERIPTYCHID ‘CONDYLARTHS’ FROM THE GREAT DIVIDE BASIN, WY by MADELAINE ATTEBERRY B.S., University of Miami, 2016 A thesis submitted to the Faculty of the Graduate School of the University of Colorado in partial fulfillment of the requirement for the degree of Master of Science Department of Geological Sciences 2019 ii This thesis entitled: A description and phylogenetic analysis of three new earliest Paleocene (Puercan) periptychid ‘condylarths’ from the Great Divide Basin, WY Written by Madelaine Atteberry has been approved for the Department of Geological Sciences. ________________________________ Jaelyn J. Eberle ________________________________ Christy M. McCain ________________________________ Benjamin J. Burger ________________________________ Leilani Arthurs ____________________ 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 Atteberry, Madelaine (M.S., Geological Sciences) A description and phylogenetic analysis of three new earliest Paleocene (Puercan) periptychid ‘condylarths’ from the Great Divide Basin, WY Thesis directed by Professor & Curator of Fossil Vertebrates Dr. Jaelyn J. Eberle An earliest Paleocene (Puercan) locality discovered by James and Jeannine Honey in the lower China Butte Member of the Fort Union Formation in Wyoming’s Great Divide Basin (GDB) contains a diverse mammalian faunal assemblage, including a number of ‘condylarth’ taxa. Previous studies have suggested that this faunal assemblage may be correlative with the early Puercan (Pu1) Littleton fauna in the Denver Basin, due to multiple shared taxa. From the University of Colorado Museum of Natural History (UCM) locality 2011035, I describe three new periptychid ‘condylarths’, in addition to the first occurrences of Maiorana noctiluca, Ampliconus antoni, and Conacodon harbourae from the GDB. -
Palaeo Ecologv
GEOGRAPHY CUIMTOLOGV PALAEO ECOLOGV ELSEVIER Palaeogeography, Palaeoclimatology. Palaeoecology 115(1995) 117 155 —— Plant and mammal diversity in the Paleocene to Early Eocene of the Bighorn Basin Scott L. Wing \ John Alroy b, Leo J. Hickey c " Department of Paleobiology, 121 National Museum of Natural History, Smithsonian Institution, Washington, * Department of Geophysical Sciences, 5734 S. Ellis Ave., University of Chicago, Chicago, IL 60637, USA c Department of Geology and Geophysics, P.O. Box 6666, 170 Whitney Ave., Yale University, New Haven, CT 06520, USA Received 1 October 1993; revised and accepted 21 October 1994 Abstract Abundant plant and vertebrate fossils have been recovered from fluvial sediments deposited in the Bighorn Basin, Wyoming, during the first 13 m.y. of the Tertiary. Here we outline and discuss changes in the composition and diversity of floras and faunas during this period, which includes the recovery of terrestrial ecosystems from the K/T boundary extinctions, and later, during the Paleocene-Eocene transition, the greatest global warming of the Cenozoic. Floral diversity has been studied at three levels of spatial resolution: sub-local (at individual collecting sites), local (along a single bed or stratigraphic horizon), and basin-wide (regional). Sub-local diversity shows a moderate increase from the early to late Paleocene, followed by a decrease across the Paleocene/Eocene boundary, then an increase into the later early Eocene. Local heterogeneity was lower in Paleocene backswamp floras, although distinct groups of species dominated in different local fluvial settings such as backswamps and alluvial ridges. Heterogeneity of backswamp forests increased by about 65% from the early to late Wasatchian (early Eocene). -
University of Michigan University Library
EARLY CENOZOIC PALEONTOLOGY AND STRATIGRAPHY OF THE BIGHORN BASIN, WYOMING PAPERS ON PALEONTOLOGY-RECENT NUMBERS 15. Cranial Anatomy and Evolution of Early Tertiary Plesiadapidae (Mammalia, Primates) by Philip D. Gingerich 16. Planning Photography of Microfossils by Robert V. Kesling 17. Devonian Strata of the Afton-Onaway Area, Michigan by R. V. Kesling, A. M. Johnson, and H. 0. Sorensen 18. Ostracods of the Middle Devonian Silica Formation (Volumes I and 11) by Robert V. Kesling and Ruth B. Chilman 19. Late Pleistocene Cold-blooded Vertebrate Faunas from the Mid-Continental United States. I. Reptilia; Testudines, Crocodilia. by Robert E. Preston 20. The Maple Block Knoll Reef in the Bush Bay Dolostone (Silurian, Engadine Group), Northern Peninsula of Michigan by Allan M. Johnson, Robert V. Kesling, Richard T. Lilienthal, and Harry 0. Sorensen 21. A Synopsis of Fossil Grasshopper Mice, Genus Onychomys, and their Relationships to Recent Species by Michael D. Carleton and Ralph E. Eshelman Museum of Paleontology The University of Michigan Ann Arbor, Michigan 48109 EARLY CENOZOIC PALEONTOLOGY AND STRATIGRAPHY OF THE BIGHORN BASIN Frontispiece: Sketch map of the Bighorn Basin, northwestern Wyoming, showing major physiographic features (from Bown, 1979) EARiY CENOZOIC PALEONTOLOGY AND STRATIGRAPHY OF THE BIGHORN BASIN, WYOMING Commemorating the 100th Anniversary of J. L. Wortman's Discovery of Fossil Mammals in the Bighorn Basin Edited by Philip D. Gingerich UNIVERSITY OF MICHIGAN PAPERS ON PALEONTOLOGY NO. 24 Papers on Paleontology No. 24 Museum of Paleontology The University of Michigan Ann Arbor, Michigan 48109 Gerald R. Smith, Director June 1, 1980 CONTENTS Preface and Acknowledgments .................................................... vi The Bighorn Basin-Why is it so Important? PHILIP D. -
Genozoic Mammal Horizons of Western North America
DEPARTMENT OF THE INTERIOR UNITED STATES GEOLOGICAL SURVEY GEORGE OTIS SMITH, DIRECTOR 361 GENOZOIC MAMMAL HORIZONS OF WESTERN NORTH AMERICA BY HENRY FAIRFIELD OSBORN WITH FAUNAL LISTS OF THE TERTIARY MAMMALIA OF THE WEST WILLIAM D1LLER MATTHEW WASHINGTON GOVERNMENT PRINTING OFFICE 1909 CONTENTS. Page. INTRODUCTION ........................................................... 7 Formations and zones................................................. 7 Life zones........................................................ 7 Geologic formations...........................'..................... 7 '. Correlation................................................................. 8 Bibliography........................................................... 9 CHAPTER I. General geologic and climatic history of the Tertiary............ 19 The Mountain Region................................................. 19 The Plains Region..................................................... 20 Resemblances and contrasts between Mountain and Plains regions........ 21 Resemblances..................................................... 21 Contrasts.......................................................... 21 Geologic history of Mountain basin deposits of the Eocene and Oligocene. 24 Geologic history of the Great Plains deposits of the .Oligocene to lower Pleistocene.......................................................... 26 Extent............................................................ 26 History of opinion as to mode of deposition.......................... 26 Summary......................................................... -
Paleobiogeography of Latest Cretaceous and Early Paleocene Mammals from North America
University of Calgary PRISM: University of Calgary's Digital Repository Graduate Studies The Vault: Electronic Theses and Dissertations 2015-06-25 Paleobiogeography of Latest Cretaceous and Early Paleocene Mammals from North America Rankin, Brian Rankin, B. (2015). Paleobiogeography of Latest Cretaceous and Early Paleocene Mammals from North America (Unpublished doctoral thesis). University of Calgary, Calgary, AB. doi:10.11575/PRISM/27248 http://hdl.handle.net/11023/2318 doctoral thesis University of Calgary graduate students retain copyright ownership and moral rights for their thesis. You may use this material in any way that is permitted by the Copyright Act or through licensing that has been assigned to the document. For uses that are not allowable under copyright legislation or licensing, you are required to seek permission. Downloaded from PRISM: https://prism.ucalgary.ca UNIVERSITY OF CALGARY Paleobiogeography of Latest Cretaceous and Early Paleocene Mammals from North America by Brian Daniel Rankin A THESIS SUBMITTED TO THE FACULTY OF GRADUATE STUDIES IN PARTIAL FULFILMENT OF THE REQUIREMENTS FOR THE DEGREE OF DOCTOR OF PHILOSOPHY DEPARTMENT OF BIOLOGICAL SCIENCES CALGARY, ALBERTA JUNE, 2015 © Brian Daniel Rankin 2015 Abstract Nearly all of what is known of the patterns of latest Cretaceous and early Paleogene mammalian evolution (from approximately 69 to 57 million years ago) is documented in stratigraphic sequences from the Western Interior of North America. Throughout much of the latest Cretaceous and early Paleogene this region was tectonically active, with the emergence of the Rocky Mountains and Western Interior foreland basin. Several major marine transgressions also occurred during this interval and, at times, the Western Interior epicontinental seaway bisected the continent. -
Mammalia) Dental Proportions
UC Berkeley UC Berkeley Previously Published Works Title Evidence of strong stabilizing effects on the evolution of boreoeutherian (Mammalia) dental proportions. Permalink https://escholarship.org/uc/item/30v521f4 Journal Ecology and evolution, 9(13) ISSN 2045-7758 Authors Monson, Tesla A Boisserie, Jean-Renaud Brasil, Marianne F et al. Publication Date 2019-07-01 DOI 10.1002/ece3.5309 Peer reviewed eScholarship.org Powered by the California Digital Library University of California Received: 11 March 2019 | Revised: 25 April 2019 | Accepted: 28 April 2019 DOI: 10.1002/ece3.5309 ORIGINAL RESEARCH Evidence of strong stabilizing effects on the evolution of boreoeutherian (Mammalia) dental proportions Tesla A. Monson1,2,3,4 | Jean‐Renaud Boisserie5 | Marianne F. Brasil1,2 | Selene M. Clay1,6 | Rena Dvoretzky1 | Shruti Ravindramurthy1 | Christopher A. Schmitt7 | Antoine Souron8 | Risa Takenaka1,3 | Peter S. Ungar9 | Sunwoo Yoo1 | Michael Zhou1 | Madeleine E. Zuercher1 | Leslea J. Hlusko1,2,3 1Department of Integrative Biology, University of California, Berkeley, California 2Human Evolution Research Center, University of California, Berkeley, California 3Museum of Vertebrate Zoology, University of California, Berkeley, California 4Anthropologisches Institut und Museum, Universität Zürich, Zürich, Switzerland 5PALEVOPRIM, CNRS & Université de Poitiers, POITIERS Cedex 9, France 6Department of Human Genetics, University of Chicago, Chicago, Illinois 7Department of Anthropology and Biology, Boston University, Boston, Massachusetts 8UMR 5199 PACEA, Université de Bordeaux, PESSAC, France 9Department of Anthropology, University of Arkansas, Fayetteville, Arkansas Correspondence Tesla A. Monson, Anthropologisches Abstract Institut und Museum, Universität Zürich, The dentition is an extremely important organ in mammals with variation in timing and 190 Winterthurerstrasse, CH‐8057 Zürich, Switzerland. sequence of eruption, crown morphology, and tooth size enabling a range of behavio‐ Email: [email protected] ral, dietary, and functional adaptations across the class.