Omomyidae) from the Bighorn Basin, Wyoming
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The World at the Time of Messel: Conference Volume
T. Lehmann & S.F.K. Schaal (eds) The World at the Time of Messel - Conference Volume Time at the The World The World at the Time of Messel: Puzzles in Palaeobiology, Palaeoenvironment and the History of Early Primates 22nd International Senckenberg Conference 2011 Frankfurt am Main, 15th - 19th November 2011 ISBN 978-3-929907-86-5 Conference Volume SENCKENBERG Gesellschaft für Naturforschung THOMAS LEHMANN & STEPHAN F.K. SCHAAL (eds) The World at the Time of Messel: Puzzles in Palaeobiology, Palaeoenvironment, and the History of Early Primates 22nd International Senckenberg Conference Frankfurt am Main, 15th – 19th November 2011 Conference Volume Senckenberg Gesellschaft für Naturforschung IMPRINT The World at the Time of Messel: Puzzles in Palaeobiology, Palaeoenvironment, and the History of Early Primates 22nd International Senckenberg Conference 15th – 19th November 2011, Frankfurt am Main, Germany Conference Volume Publisher PROF. DR. DR. H.C. VOLKER MOSBRUGGER Senckenberg Gesellschaft für Naturforschung Senckenberganlage 25, 60325 Frankfurt am Main, Germany Editors DR. THOMAS LEHMANN & DR. STEPHAN F.K. SCHAAL Senckenberg Research Institute and Natural History Museum Frankfurt Senckenberganlage 25, 60325 Frankfurt am Main, Germany [email protected]; [email protected] Language editors JOSEPH E.B. HOGAN & DR. KRISTER T. SMITH Layout JULIANE EBERHARDT & ANIKA VOGEL Cover Illustration EVELINE JUNQUEIRA Print Rhein-Main-Geschäftsdrucke, Hofheim-Wallau, Germany Citation LEHMANN, T. & SCHAAL, S.F.K. (eds) (2011). The World at the Time of Messel: Puzzles in Palaeobiology, Palaeoenvironment, and the History of Early Primates. 22nd International Senckenberg Conference. 15th – 19th November 2011, Frankfurt am Main. Conference Volume. Senckenberg Gesellschaft für Naturforschung, Frankfurt am Main. pp. 203. -
New Fossils of Oldest American Primate 16 November 2011
New fossils of oldest American primate 16 November 2011 (PhysOrg.com) -- Johns Hopkins researchers have Prior excavations in the same region revealed identified the first ankle and toe bone fossils from fossils of early relatives of horses, carnivores and the earliest North American true primate, which rodents, as well as Teilhardina. The researchers they say suggests that our earliest forerunners screened through hundreds of pounds of may have dwelled or moved primarily in trees, like sedimentary rock, reducing it to fine-grained modern day lemurs and similar mammals. concentrate, which was transported back to the lab for examination under the microscope. Some early Previous excavations have yielded pieces of the primate teeth specimens are known to be many jaw and teeth of Teilhardina, primates that first times smaller than a grain of rice and only appear appeared just after the beginning of the Eocene as specks to the human eye. Under the Epoch about 55.5 million years ago. In a report on microscope, the researchers discovered not only their analysis of the fossils, published in the teeth and jawbones from Teilhardina as before, but October issue of the American Journal of Physical also three fossilized toe bones and three ankle Anthropology, the Johns Hopkins team said they bones, which Rose says are the first found in North identified the latest bones when they went America. The bones were relatively free of attached prospecting for evidence of the earliest Eocene sediment and appeared smooth and dark - due to mammals in the badlands of the Bighorn Basin, the type of minerals accumulated during Wyoming, an area rich in fossils. -
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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. -
Diagnosis and Differentiation of the Order Primates
YEARBOOK OF PHYSICAL ANTHROPOLOGY 30:75-105 (1987) Diagnosis and Differentiation of the Order Primates FREDERICK S. SZALAY, ALFRED L. ROSENBERGER, AND MARIAN DAGOSTO Department of Anthropolog* Hunter College, City University of New York, New York, New York 10021 (F.S.S.); University of Illinois, Urbanq Illinois 61801 (A.L. R.1; School of Medicine, Johns Hopkins University/ Baltimore, h4D 21218 (M.B.) KEY WORDS Semiorders Paromomyiformes and Euprimates, Suborders Strepsirhini and Haplorhini, Semisuborder Anthropoidea, Cranioskeletal morphology, Adapidae, Omomyidae, Grades vs. monophyletic (paraphyletic or holophyletic) taxa ABSTRACT We contrast our approach to a phylogenetic diagnosis of the order Primates, and its various supraspecific taxa, with definitional proce- dures. The order, which we divide into the semiorders Paromomyiformes and Euprimates, is clearly diagnosable on the basis of well-corroborated informa- tion from the fossil record. Lists of derived features which we hypothesize to have been fixed in the first representative species of the Primates, Eupri- mates, Strepsirhini, Haplorhini, and Anthropoidea, are presented. Our clas- sification of the order includes both holophyletic and paraphyletic groups, depending on the nature of the available evidence. We discuss in detail the problematic evidence of the basicranium in Paleo- gene primates and present new evidence for the resolution of previously controversial interpretations. We renew and expand our emphasis on postcra- nial analysis of fossil and living primates to show the importance of under- standing their evolutionary morphology and subsequent to this their use for understanding taxon phylogeny. We reject the much advocated %ladograms first, phylogeny next, and scenario third” approach which maintains that biologically founded character analysis, i.e., functional-adaptive analysis and paleontology, is irrelevant to genealogy hypotheses. -
Surface Geology Wind/Bighorn River Basin Wyoming and Montana
WYOMING STATE GEOLOGICAL SURVEY Plate I Thomas A. Drean, State Geologist Wind/Bighorn Basin Plan II - Available Groundwater Determination Technical Memorandum Surface Geology - Wind/Bighorn River Basin SWEET GRASS R25E R5E R15E R30E R10E R20E MONTANA Mm PM Jsg T7S KJ !c Pp Jsg KJ water Qt Surface Geology Ti ! Red Lodge PM DO PM PM Ts Ts p^r PM N ^r DO KJ DO !c Wind/Bighorn River Basin Tts Mm water Mm Ti Ti ^r DO Kmt Ti LOCATION MAP p^r ^r ^r Qt WYOMING Wyoming and Montana Kf Qt Ti p^r !c p^r PM 0 100 250 Miles Tts ^r PM DO Ti Jsg MD Ts Ti MzPz Kmv !Pg Qt compiled DO DO Tts Ts Taw DO DO DO water Qt Kc PM ^r Twl Qt Ob O^ by ^r Mm DO !c MD MONTANA Thr Ti Kc Qr Klc p^r Kmv Kc : # Ts ^r : O^ Nikolaus Gribb, Brett Worman, # Ts # water : PM Taw # Kf : PM !cd : Ket Qb Taw Qu Twp Thr # Ki Twl 345 P$Ma : Thr O^ Qa KJg Tfu : Jsg ^r Qu : :: # Kl (! KJk : Qr Qls Tomas Gracias, and Scott Quillinan Qb : Thr Ts Taw # Tfu 37 PM Kft: : # :: T10S Qls # Thr : # ^r Kc (! Kft Kmt # :::::: p^r :: : Qu KJk Kc MD Taw DO Qu # p^r Qg :: Km KJ WYOMING Taw Ti : Kl 2012 Thr : Qb # # # Qg : water DO Qls ::: !c !Pg !cd MDO water water Kc Qa :::::: :: Kmt ::: : Twl 90 : Ti Ts Qu Qa Qg Kmv !Pcg Mm KJk : Qg : 212 : Qu Qg £¤ Kmv KJ ¨¦§ Tts Taw p^r ^r # Kl : Kf Kf 338 Ob !cd Qu Qu Ttp # (! : : : p^r ::: !Pg O^ MD P$Ma Thr : Qa # DO Km Qls 343 ^r Qls Taw : Qb Qg Qls Qa Km Jsg water (! : Qb # !cd ^r Kc BighornLake : MD # Taw Qa Qls Qt MD A′ MD MD Qg Twl !Pg Qu Qb Tii # Twp ^r water MzPz Qg Tfu Kl ::: Taw Taw Twp Qls : Qt Kmv Qa Ob P$Ma : Thr Qa # Tcr ^r water Qa Kft # Qt O^ -
Mammal Faunal Change in the Zone of the Paleogene Hyperthermals ETM2 and H2
Clim. Past, 11, 1223–1237, 2015 www.clim-past.net/11/1223/2015/ doi:10.5194/cp-11-1223-2015 © Author(s) 2015. CC Attribution 3.0 License. Mammal faunal change in the zone of the Paleogene hyperthermals ETM2 and H2 A. E. Chew Department of Anatomy, Western University of Health Sciences, 309 E Second St., Pomona, CA 91767, USA Correspondence to: A. E. Chew ([email protected]) Received: 13 March 2015 – Published in Clim. Past Discuss.: 16 April 2015 Revised: 4 August 2015 – Accepted: 19 August 2015 – Published: 24 September 2015 Abstract. “Hyperthermals” are past intervals of geologically vulnerability in response to changes already underway in the rapid global warming that provide the opportunity to study lead-up to the EECO. Faunal response at faunal events B-1 the effects of climate change on existing faunas over thou- and B-2 is also distinctive in that it shows high proportions sands of years. A series of hyperthermals is known from of beta richness, suggestive of increased geographic disper- the early Eocene ( ∼ 56–54 million years ago), including sal related to transient increases in habitat (floral) complexity the Paleocene–Eocene Thermal Maximum (PETM) and two and/or precipitation or seasonality of precipitation. subsequent hyperthermals (Eocene Thermal Maximum 2 – ETM2 – and H2). The later hyperthermals occurred during warming that resulted in the Early Eocene Climatic Opti- mum (EECO), the hottest sustained period of the Cenozoic. 1 Introduction The PETM has been comprehensively studied in marine and terrestrial settings, but the terrestrial biotic effects of ETM2 The late Paleocene and early Eocene (ca. -
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. -
New Paleocene Skeletons and the Relationship of Plesiadapiforms to Crown-Clade Primates
New Paleocene skeletons and the relationship of plesiadapiforms to crown-clade primates Jonathan I. Bloch*†, Mary T. Silcox‡, Doug M. Boyer§, and Eric J. Sargis¶ʈ *Florida Museum of Natural History, University of Florida, P. O. Box 117800, Gainesville, FL 32611; ‡Department of Anthropology, University of Winnipeg, 515 Portage Avenue, Winnipeg, MB, Canada, R3B 2E9; §Department of Anatomical Science, Stony Brook University, Stony Brook, NY 11794-8081; ¶Department of Anthropology, Yale University, P. O. Box 208277, New Haven, CT 06520; and ʈDivision of Vertebrate Zoology, Peabody Museum of Natural History, Yale University, New Haven, CT 06520 Communicated by Alan Walker, Pennsylvania State University, University Park, PA, November 30, 2006 (received for review December 6, 2005) Plesiadapiforms are central to studies of the origin and evolution preserved cranium of a paromomyid (10) seemed to independently of primates and other euarchontan mammals (tree shrews and support a plesiadapiform–dermopteran link, leading to the wide- flying lemurs). We report results from a comprehensive cladistic spread acceptance of this phylogenetic hypothesis. The evidence analysis using cranial, postcranial, and dental evidence including supporting this interpretation has been questioned (7, 9, 13, 15, 16, data from recently discovered Paleocene plesiadapiform skeletons 19, 20), but no previous study has evaluated the plesiadapiform– (Ignacius clarkforkensis sp. nov.; Dryomomys szalayi, gen. et sp. dermopteran link by using cranial, postcranial, and dental evidence, -
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. -
Tobey-Dawn-Msc-ERTH-September
Water and Wind: The Fluvial and Eolian Forces Behind the Pennsylvanian-Permian Halgaito Formation, Utah By Dawn E. Tobey Submitted in partial fulfillment of the requirements for the degree of Masters of Science at Dalhousie University Halifax, Nova Scotia September 2020 © Copyright by Dawn E. Tobey, 2020 Table Of Contents List of Tables ............................................................................................................................... v List of Figures ........................................................................................................................... vi Abstract ..................................................................................................................................... vii List of Abbreviations Used ................................................................................................. viii Acknowledgements .................................................................................................................ix Chapter 1: Introduction .......................................................................................................... 1 1.1 Statement of Problem................................................................................................................ 1 1.2 Objectives ....................................................................................................................................... 6 1.3 Contributions of the Author .................................................................................................. -
Eocene Green River Formation, Western United States
Synoptic reconstruction of a major ancient lake system: Eocene Green River Formation, western United States M. Elliot Smith* Alan R. Carroll Brad S. Singer Department of Geology and Geophysics, University of Wisconsin, 1215 West Dayton Street, Madison, Wisconsin 53706, USA ABSTRACT Members. Sediment accumulation patterns than being confi ned to a single episode of arid thus refl ect basin-center–focused accumula- climate. Evaporative terminal sinks were Numerous 40Ar/39Ar experiments on sani- tion rates when the basin was underfi lled, initially located in the Greater Green River dine and biotite from 22 ash beds and 3 and supply-limited accumulation when the and Piceance Creek Basins (51.3–48.9 Ma), volcaniclastic sand beds from the Greater basin was balanced fi lled to overfi lled. Sedi- then gradually migrated southward to the Green River, Piceance Creek, and Uinta ment accumulation in the Uinta Basin, at Uinta Basin (47.1–45.2 Ma). This history is Basins of Wyoming, Colorado, and Utah Indian Canyon, Utah, was relatively con- likely related to progressive southward con- constrain ~8 m.y. of the Eocene Epoch. Mul- stant at ~150 mm/k.y. during deposition of struction of the Absaroka Volcanic Prov- tiple analyses were conducted per sample over 5 m.y. of both evaporative and fl uctuat- ince, which constituted a major topographic using laser fusion and incremental heating ing profundal facies, which likely refl ects the and thermal anomaly that contributed to a techniques to differentiate inheritance, 40Ar basin-margin position of the measured sec- regional north to south hydrologic gradient. loss, and 39Ar recoil. -
From the Gulf Coastal Plain
Bull. Fla. Mus. Nat. Hist. (2005) 45(4): 355-361 355 EKGMOWECHASHALA (MAMMALIA, ?PRIMATES) FROM THE GULF COASTAL PLAIN L. Barry Albright III1 A single, small, water-worn tooth from the “middle” Arikareean Toledo Bend Local Fauna of the Gulf Coastal Plain closely resembles the lower fourth premolar of the questionable primate Ekgmowechashala. The only known species of the genus, Ekgmowechashala philotau Macdonald (1963), was originally recovered from the early Arikareean Sharps Formation of South Dakota, but is also known from similar aged strata of the John Day Formation, Oregon. Although the Toledo Bend specimen differs somewhat in morphology from the p4 of E. philotau, a new species is not named in this report because of such limited material and because the specimen is incomplete. Unfortunately, the specimen does not provide information that helps clarify current arguments regarding the affinities of Ekgmowechashala with primates or plagiomenids. It does, however, provide (1) a temporal range extension for the genus to the early late Arikareean, or about four million years younger than previously known, and (2) a geographic extension east and considerably south of its prior distribution. If Ekgmowechashala is ultimately deter- mined to belong to the Primates, then the Toledo Bend species would become the last known North American representative of the order. Key Words: Ekgmowechashala; Primates; Plagiomenidae; Texas Gulf Coastal Plain; Arikareean INTRODUCTION brate paleontology collections of the Louisiana State Uni- In 1990, while screen-washing matrix from the “middle” versity Museum of Geoscience (LSUMG V). Arikareean Toledo Bend site in the Fleming Formation of easternmost Texas (Albright 1994, 1996, 1998a, 1998b, BACKGROUND 1999), a small, unusual, water-worn tooth was recov- Ekgmowechashala philotau is a small “enigmatic late ered that differed considerably from the site’s more com- Oligocene mammal” (McKenna, 1990:226) heretofore mon and readily identifiable rodent teeth.