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Foraminifera of the Eocene of Belgium
FORAMINIFERA OF THE EOCENE OF BELGIUM CHAPTER I STRATI GRAPHIC REVIEW INTRODUCTION In 1833 L\ELL ubdivided the Tertiary period into four groups : Eocene, Miocene, Older Pliocene and Newer Pliocene. He based his subdivisions on the percentages of living species of molluscs of the variou known fossil faunas of northwestern Europe. For these percentages he adopted the countings given by DESHAYES (1830) . The percentage of the Eocene ·was mainly based on the rich faunas of the Paris basin. Since LrnLL's proposal, the Eocene suffered the separation of the Oligocene (BEYRICB, 1854) and of the Paleocene ( CHDIPER, 1874), but it still represents the central and main part of the Paleogene (NAmrAK:\', 1866) or Nummulitique (REl'iEYIER, 1873; HAUG, 1911). Paleogene trata appear at the surface in a large part of Belgium. They belong to a m uch larger area of form er deposition which included southern England (London and Hamp shire ba ins) , northern France (Paris basin) and the southern Netherlands. The relationship between this great anglo-franco-belgian basin and the depositional areas in the northern .:\etherlands, northern Germany, and Denmark is not quite clear. According to stratigraphic maps, published by PA NNEKOEK (1956), the Belgian basin was separated from the 'orthern German-Dani h basin by a SE-1'vV striking swell. During at least part of the Eocene there must have been orne connection between the two basins. Since L\ELL' time the Eocen e has been subdivided into a number of stages. These stage , such as those e tablished by Dm roNT, were originally merely names for rock-units. -
Stopover Ecology of a Migratory Ungulate
Journal of Animal Ecology 2011, 80, 1078–1087 doi: 10.1111/j.1365-2656.2011.01845.x Stopover ecology of a migratory ungulate Hall Sawyer1,2* and Matthew J. Kauffman3 1Department of Zoology and Physiology, Wyoming Cooperative Fish and Wildlife Research Unit, University of Wyoming, Laramie, WY 82071, USA; 2Western Ecosystems Technology, Inc., 200 South 2nd St., Laramie, WY 82070, USA; and 3Department of Zoology and Physiology, United States Geological Survey, Wyoming Cooperative Fish and Wildlife Research Unit, University of Wyoming, Laramie, WY, USA Summary 1. Birds that migrate long distances use stopover sites to optimize fuel loads and complete migra- tion as quickly as possible. Stopover use has been predicted to facilitate a time-minimization strat- egy in land migrants as well, but empirical tests have been lacking, and alternative migration strategies have not been considered. 2. We used fine-scale movement data to evaluate the ecological role of stopovers in migratory mule deer Odocoileus hemionus – a land migrant whose fitness is strongly influenced by energy intake rather than migration speed. 3. Although deer could easily complete migrations (range 18–144 km) in several days, they took an average of 3 weeks and spent 95% of that time in a series of stopover sites that had higher for- age quality than movement corridors. Forage quality of stopovers increased with elevation and distance from winter range. Mule deer use of stopovers corresponded with a narrow phenological range, such that deer occupied stopovers 44 days prior to peak green-up, when forage quality was presumed to be highest. Mule deer used one stopover for every 5Æ3 and 6Æ7 km travelled during spring and autumn migrations, respectively, and used the same stopovers in consecutive years. -
Artiodactyla and Perissodactyla (Mammalia) from the Early-Middle Eocene Kuldana Formation of Kohat (Pakistan)
CO"uTK1BL 11015 FKOLI IHt \lC5tLL1 OF I' ALEO\ IOLOG1 THE UNIVERSITY OF IVICHIGAN VOI 77 Lo 10 p 717-37.1 October 33 1987 ARTIODACTYLA AND PERISSODACTYLA (MAMMALIA) FROM THE EARLY-MIDDLE EOCENE KULDANA FORMATION OF KOHAT (PAKISTAN) BY J. G. M. THEWISSEN. P. D. GINGERICH and D. E. RUSSELL MUSEUM OF PALEONTOLOGY THE UNIVERSITY OF MICHIGAN ANN ARBOR CONTRIBUTIONS FROM THE MUSEUM OF PALEONTOLOGY Charles B. Beck, Director Jennifer A. Kitchell, Editor This series of contributions from the Museum of Paleontology is a medium for publication of papers based chiefly on collections 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 issues may also be obtained by request. Correspond- ence should be directed to the Museum of Paleontology, The University of Michigan, Ann Arbor, Michigan 48109. VOLS. II-XXVII. Parts of volumes may be obtained if available. Price lists are available upon inquiry. I ARTIODACTI L .-I A\D PERISSODACTYL4 (kl.iihlhlAL1A) FROM THE EARLY-h1IDDLE EOCEUE KCLD..I\4 FORMATIO\ OF KOHAT (PAKISTAY) J. G. M. THEWISSEN. P. D. GINGERICH AND D. E. RUSSELL Ah.strcict.-Chorlakki. yielding approximately 400 specimens (mostly isolated teeth and bone fragments). is one of four major early-to-middle Eocene niammal localities on the Indo-Pakistan subcontinent. On the basis of ung~~latesclescribed in this paper we consider the Chorlakki fauna to be younger than that from Barbora Banda. -
Boselaphus Tragocamelus</I>
University of Nebraska - Lincoln DigitalCommons@University of Nebraska - Lincoln USGS Staff -- Published Research US Geological Survey 2008 Boselaphus tragocamelus (Artiodactyla: Bovidae) David M. Leslie Jr. U.S. Geological Survey, [email protected] Follow this and additional works at: https://digitalcommons.unl.edu/usgsstaffpub Leslie, David M. Jr., "Boselaphus tragocamelus (Artiodactyla: Bovidae)" (2008). USGS Staff -- Published Research. 723. https://digitalcommons.unl.edu/usgsstaffpub/723 This Article is brought to you for free and open access by the US Geological Survey at DigitalCommons@University of Nebraska - Lincoln. It has been accepted for inclusion in USGS Staff -- Published Research by an authorized administrator of DigitalCommons@University of Nebraska - Lincoln. MAMMALIAN SPECIES 813:1–16 Boselaphus tragocamelus (Artiodactyla: Bovidae) DAVID M. LESLIE,JR. United States Geological Survey, Oklahoma Cooperative Fish and Wildlife Research Unit and Department of Natural Resource Ecology and Management, Oklahoma State University, Stillwater, OK 74078-3051, USA; [email protected] Abstract: Boselaphus tragocamelus (Pallas, 1766) is a bovid commonly called the nilgai or blue bull and is Asia’s largest antelope. A sexually dimorphic ungulate of large stature and unique coloration, it is the only species in the genus Boselaphus. It is endemic to peninsular India and small parts of Pakistan and Nepal, has been extirpated from Bangladesh, and has been introduced in the United States (Texas), Mexico, South Africa, and Italy. It prefers open grassland and savannas and locally is a significant agricultural pest in India. It is not of special conservation concern and is well represented in zoos and private collections throughout the world. DOI: 10.1644/813.1. -
A New Middle Eocene Protocetid Whale (Mammalia: Cetacea: Archaeoceti) and Associated Biota from Georgia Author(S): Richard C
A New Middle Eocene Protocetid Whale (Mammalia: Cetacea: Archaeoceti) and Associated Biota from Georgia Author(s): Richard C. Hulbert, Jr., Richard M. Petkewich, Gale A. Bishop, David Bukry and David P. Aleshire Source: Journal of Paleontology , Sep., 1998, Vol. 72, No. 5 (Sep., 1998), pp. 907-927 Published by: Paleontological Society Stable URL: https://www.jstor.org/stable/1306667 REFERENCES Linked references are available on JSTOR for this article: https://www.jstor.org/stable/1306667?seq=1&cid=pdf- reference#references_tab_contents You may need to log in to JSTOR to access the linked references. JSTOR is a not-for-profit service that helps scholars, researchers, and students discover, use, and build upon a wide range of content in a trusted digital archive. We use information technology and tools to increase productivity and facilitate new forms of scholarship. For more information about JSTOR, please contact [email protected]. Your use of the JSTOR archive indicates your acceptance of the Terms & Conditions of Use, available at https://about.jstor.org/terms SEPM Society for Sedimentary Geology and are collaborating with JSTOR to digitize, preserve and extend access to Journal of Paleontology This content downloaded from 131.204.154.192 on Thu, 08 Apr 2021 18:43:05 UTC All use subject to https://about.jstor.org/terms J. Paleont., 72(5), 1998, pp. 907-927 Copyright ? 1998, The Paleontological Society 0022-3360/98/0072-0907$03.00 A NEW MIDDLE EOCENE PROTOCETID WHALE (MAMMALIA: CETACEA: ARCHAEOCETI) AND ASSOCIATED BIOTA FROM GEORGIA RICHARD C. HULBERT, JR.,1 RICHARD M. PETKEWICH,"4 GALE A. -
Thomas Jefferson Meg Tooth
The ECPHORA The Newsletter of the Calvert Marine Museum Fossil Club Volume 30 Number 3 September 2015 Thomas Jefferson Meg Tooth Features Thomas Jefferson Meg The catalogue number Review; Walking is: ANSP 959 Whales Inside The tooth came from Ricehope Estate, Snaggletooth Shark Cooper River, Exhibit South Carolina. Tiktaalik Clavatulidae In 1806, it was Juvenile Bald Eagle originally collected or Sculpting Whale Shark owned by Dr. William Moroccan Fossils Reid. Prints in the Sahara Volunteer Outing to Miocene-Pliocene National Geographic coastal plain sediments. Dolphins in the Chesapeake Sloth Tooth Found SharkFest Shark Iconography in Pre-Columbian Panama Hippo Skulls CT- Scanned Squalus sp. Teeth Sperm Whale Teeth On a recent trip to the Academy of Natural Sciences of Drexel University (Philadelphia), Collections Manager Ned Gilmore gave John Nance and me a behind -the-scenes highlights tour. Among the fossils that belonged to Thomas☼ Jefferson (left; American Founding Father, principal author of the Declaration of Independence, and third President of the United States) was this Carcharocles megalodon tooth. Jefferson’s interests and knowledge were encyclopedic; a delight to know that they included paleontology. Hand by J. Nance. Photo by S. Godfrey. Jefferson portrait from: http://www.biography.com/people/thomas-jefferson-9353715 ☼ CALVERT MARINE MUSEUM www.calvertmarinemuseum.com 2 The Ecphora September 2015 Book Review: The Walking 41 million years ago and has worldwide distribution. It was fully aquatic, although it did have residual Whales hind limbs. In later chapters, Professor Thewissen George F. Klein discusses limb development and various genetic factors that make whales, whales. This is a The full title of this book is The Walking complicated topic, but I found these chapters very Whales — From Land to Water in Eight Million clear and readable. -
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. -
Intervertebral and Epiphyseal Fusion in the Postnatal Ontogeny of Cetaceans and Terrestrial Mammals
J Mammal Evol DOI 10.1007/s10914-014-9256-7 ORIGINAL PAPER Intervertebral and Epiphyseal Fusion in the Postnatal Ontogeny of Cetaceans and Terrestrial Mammals Meghan M. Moran & Sunil Bajpai & J. Craig George & Robert Suydam & Sharon Usip & J. G. M. Thewissen # Springer Science+Business Media New York 2014 Abstract In this paper we studied three related aspects of the Introduction ontogeny of the vertebral centrum of cetaceans and terrestrial mammals in an evolutionary context. We determined patterns The vertebral column provides support for the body and of ontogenetic fusion of the vertebral epiphyses in bowhead allows for flexibility and mobility (Gegenbaur and Bell whale (Balaena mysticetus) and beluga whale 1878;Hristovaetal.2011; Bruggeman et al. 2012). To (Delphinapterus leucas), comparing those to terrestrial mam- achieve this mobility, individual vertebrae articulate with each mals and Eocene cetaceans. We found that epiphyseal fusion other through cartilaginous intervertebral joints between the is initiated in the neck and the sacral region of terrestrial centra and synovial joints between the pre- and post- mammals, while in recent aquatic mammals epiphyseal fusion zygapophyses. The mobility of each vertebral joint varies is initiated in the neck and caudal regions, suggesting loco- greatly between species as well as along the vertebral column motor pattern and environment affect fusion pattern. We also within a single species. Vertebral column mobility greatly studied bony fusion of the sacrum and evaluated criteria used impacts locomotor style, whether the animal is terrestrial or to homologize cetacean vertebrae with the fused sacrum of aquatic. In aquatic Cetacea, buoyancy counteracts gravity, and terrestrial mammals. We found that the initial ossification of the tail is the main propulsive organ (Fish 1996;Fishetal. -
Hyaenodontidae (Creodonta, Mammalia) and the Position of Systematics in Evolutionary Biology
Hyaenodontidae (Creodonta, Mammalia) and the Position of Systematics in Evolutionary Biology by Paul David Polly B.A. (University of Texas at Austin) 1987 A dissertation submitted in partial satisfaction of the requirements for the degree of Doctor of Philosophy in Paleontology in the GRADUATE DIVISION of the UNIVERSITY of CALIFORNIA at BERKELEY Committee in charge: Professor William A. Clemens, Chair Professor Kevin Padian Professor James L. Patton Professor F. Clark Howell 1993 Hyaenodontidae (Creodonta, Mammalia) and the Position of Systematics in Evolutionary Biology © 1993 by Paul David Polly To P. Reid Hamilton, in memory. iii TABLE OF CONTENTS Introduction ix Acknowledgments xi Chapter One--Revolution and Evolution in Taxonomy: Mammalian Classification Before and After Darwin 1 Introduction 2 The Beginning of Modern Taxonomy: Linnaeus and his Predecessors 5 Cuvier's Classification 10 Owen's Classification 18 Post-Darwinian Taxonomy: Revolution and Evolution in Classification 24 Kovalevskii's Classification 25 Huxley's Classification 28 Cope's Classification 33 Early 20th Century Taxonomy 42 Simpson and the Evolutionary Synthesis 46 A Box Model of Classification 48 The Content of Simpson's 1945 Classification 50 Conclusion 52 Acknowledgments 56 Bibliography 56 Figures 69 Chapter Two: Hyaenodontidae (Creodonta, Mammalia) from the Early Eocene Four Mile Fauna and Their Biostratigraphic Implications 78 Abstract 79 Introduction 79 Materials and Methods 80 iv Systematic Paleontology 80 The Four Mile Fauna and Wasatchian Biostratigraphic Zonation 84 Conclusion 86 Acknowledgments 86 Bibliography 86 Figures 87 Chapter Three: A New Genus Eurotherium (Creodonta, Mammalia) in Reference to Taxonomic Problems with Some Eocene Hyaenodontids from Eurasia (With B. Lange-Badré) 89 Résumé 90 Abstract 90 Version française abrégéé 90 Introduction 93 Acknowledgments 96 Bibliography 96 Table 3.1: Original and Current Usages of Genera and Species 99 Table 3.2: Species Currently Included in Genera Discussed in Text 101 Chapter Four: The skeleton of Gazinocyon vulpeculus n. -
Functional Morphology of the Vertebral Column in Remingtonocetus (Mammalia, Cetacea) and the Evolution of Aquatic Locomotion in Early Archaeocetes
Functional Morphology of the Vertebral Column in Remingtonocetus (Mammalia, Cetacea) and the Evolution of Aquatic Locomotion in Early Archaeocetes by Ryan Matthew Bebej A dissertation submitted in partial fulfillment of the requirements for the degree of Doctor of Philosophy (Ecology and Evolutionary Biology) in The University of Michigan 2011 Doctoral Committee: Professor Philip D. Gingerich, Co-Chair Professor Philip Myers, Co-Chair Professor Daniel C. Fisher Professor Paul W. Webb © Ryan Matthew Bebej 2011 To my wonderful wife Melissa, for her infinite love and support ii Acknowledgments First, I would like to thank each of my committee members. I will be forever grateful to my primary mentor, Philip D. Gingerich, for providing me the opportunity of a lifetime, studying the very organisms that sparked my interest in evolution and paleontology in the first place. His encouragement, patience, instruction, and advice have been instrumental in my development as a scholar, and his dedication to his craft has instilled in me the importance of doing careful and solid research. I am extremely grateful to Philip Myers, who graciously consented to be my co-advisor and co-chair early in my career and guided me through some of the most stressful aspects of life as a Ph.D. student (e.g., preliminary examinations). I also thank Paul W. Webb, for his novel thoughts about living in and moving through water, and Daniel C. Fisher, for his insights into functional morphology, 3D modeling, and mammalian paleobiology. My research was almost entirely predicated on cetacean fossils collected through a collaboration of the University of Michigan and the Geological Survey of Pakistan before my arrival in Ann Arbor. -
Mammal and Plant Localities of the Fort Union, Willwood, and Iktman Formations, Southern Bighorn Basin* Wyoming
Distribution and Stratigraphip Correlation of Upper:UB_ • Ju Paleocene and Lower Eocene Fossil Mammal and Plant Localities of the Fort Union, Willwood, and Iktman Formations, Southern Bighorn Basin* Wyoming U,S. GEOLOGICAL SURVEY PROFESS IONAL PAPER 1540 Cover. A member of the American Museum of Natural History 1896 expedition enter ing the badlands of the Willwood Formation on Dorsey Creek, Wyoming, near what is now U.S. Geological Survey fossil vertebrate locality D1691 (Wardel Reservoir quadran gle). View to the southwest. Photograph by Walter Granger, courtesy of the Department of Library Services, American Museum of Natural History, New York, negative no. 35957. DISTRIBUTION AND STRATIGRAPHIC CORRELATION OF UPPER PALEOCENE AND LOWER EOCENE FOSSIL MAMMAL AND PLANT LOCALITIES OF THE FORT UNION, WILLWOOD, AND TATMAN FORMATIONS, SOUTHERN BIGHORN BASIN, WYOMING Upper part of the Will wood Formation on East Ridge, Middle Fork of Fifteenmile Creek, southern Bighorn Basin, Wyoming. The Kirwin intrusive complex of the Absaroka Range is in the background. View to the west. Distribution and Stratigraphic Correlation of Upper Paleocene and Lower Eocene Fossil Mammal and Plant Localities of the Fort Union, Willwood, and Tatman Formations, Southern Bighorn Basin, Wyoming By Thomas M. Down, Kenneth D. Rose, Elwyn L. Simons, and Scott L. Wing U.S. GEOLOGICAL SURVEY PROFESSIONAL PAPER 1540 UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1994 U.S. DEPARTMENT OF THE INTERIOR BRUCE BABBITT, Secretary U.S. GEOLOGICAL SURVEY Robert M. Hirsch, Acting Director For sale by U.S. Geological Survey, Map Distribution Box 25286, MS 306, Federal Center Denver, CO 80225 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. -
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.