(Puercan) Periptychid 'Condylarths'
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
(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. -
A Review of William Diller Matthew's Contributions to Mammalian Paleontology
AMERICAN MUSEUM NOVITATES Published by THE AmzRICAN MUSeum oF NATURAL HISTORY May 14, 1931 Number 473 New York City 56.9:091 M A REVIEW OF WILLIAM DILLER MATTHEW'S CONTRI- BUTIONS TO MAMMALIAN PALEONTOLOGY BY WILLIAM K. GREGORY The late William Diller Matthew, Professor of Paleontology and Director of the Museum of Palaeontology in the University of California, and for many years Curator of the Department of Vertebrate Paleon- tology in the American Museum of Natural History, left to the world a legacy in the form of some two hundred and forty-four scientific papers, which deal for the most part with mammalian palseontology. He also imparted to many of his students and junior colleagues an active interest in palaeontological exploration and in the advancement of the great theme of mammalian evolution to which he had contributed so much. Various general biographical articles' on Doctor Matthew having already been published, it would now seem both timely and useful to attempt a special review of his chief contributions to mammalian palmeontology. HIS EARLIER CONTRIBUTIONS TO KNOWLEDGE OF RECENT AND FOSSIL MAMMALS Soon after Doctor Matthew's coming to the American Museum of Natural History in 1895, he was sent by Professor Osborn to Philadelphia to catalogue, pack up and ship to New York the great collections of Professor E. D. Cope, which had been purchased by the Museum. In this way Matthew came to know and admire Professor Cope and began the detailed task of checking Cope's identifications and revising his classifications, which was to occupy him, along with many other matters, for the next thirty-odd years. -
J. David Archibald
CURRICULUM VITAE J. DAVID ARCHIBALD AFFILIATION Department of Biology MAILING ADDRESS 4615 48th St San Diego State University San Diego, CA 92115-3206 5500 Campanile Dr. San Diego State University San Diego, CA 92182-4614 PHONE (619) 286-5521 FAX (619) 501-9587 E-MAIL [email protected] FACULTY PAGE http://www.bio.sdsu.edu/faculty/archibald.html EDUCATION B. Sc. in Geology, Kent State University, 1972, Magna cum Laude Ph. D. in Paleontology, University of California, Berkeley 1977 TEACHING EXPERIENCE AND ACADEMIC POSITIONS 1974-75: Teaching Assistant, Paleontology, University of California, Berkeley Courses assisted for: Introduction to Paleontology, undergraduate Morphology of the Vertebrate Skeleton, undergraduate Floras of the Past, undergraduate Phylogeny and Evolution, undergraduate 1977-79: J. Willard Gibbs Instructor (a postdoctoral fellowship), Dept. of Geology & Geophysics,Yale University Problems in Cretaceous-Paleogene Vertebrate Evolution, graduate seminar Evolution of Vertebrates to Man, undergraduate Paleobiology of Mammals, graduate Seminar in Primate Paleobiology (with D. Pilbeam) 1979-83: Assistant Professor (1979-1983) Associate Professor (promoted 1983, but did not accept promotion), Department of Biology, Yale University Vertebrate Anatomy, undergraduate Biologic Processes and Paleontologic Patterns, graduate seminar (with faculty from Biology, Geology, and Anthropology) Biology of Mammals, undergraduate Evolution, undergraduate (team taught) Paleobiology of Mammals, graduate Variability seminar (with faculty -
Proceedings of the United States National Museum
1 PROCEEDINGS OF THE UNITED STATES NATIONAL MUSEUM issued iMf^rvi^.sjIMH h '^* SMITHSONIAN INSTITUTION U. S. NATIONAL MUSEUM Vol.91 W«il,ington:I94l No. 3121 THE MAMMALIAN FAUNAS OF THE PALEOCENE OF CENTRAL UTAH, WITH NOTES ON THE GEOLOGY By C. Lewis Gazin Further investigation of the Paleocene deposits of central Utah by the 1939 and 1940 Smithsonian Institution expeditions has added considerably to the collections representative of the upper portion of the North Horn deposits and has resulted in the discovery of a second and distinct horizon for mammals within the Paleocene series. The investigations of these years have led also to a better understanding of the geologic relations pertaining to the fossil-bearing deposits in and about Dragon Canyon and North Horn Mountain. The area investigated lies within the region of the Manti National Forest and along the eastern part of the Wasatch Plateau. Physio- graphically, it belongs to the High Plateaus of Utah section of the Colorado Plateaus province, as defined by Fenneman and Johnson. North Horn Mountain (T. 18 S., R. 6 E.), due west of the towns of Orangeville and Castledale, is an outlying remnant of the plateau to the west, being separated from it by the troughlike depression known as North or Upper Dragon. Dragon Canyon, or the Lower Dragon, lies principally in the western half of T. 19 S., R. 6 E., and together with North Dragon is primarily the result of a complex graben struc- ture extending for a considerable distance both north and south. The writer wishes to acknowledge the courtesy extended by Dr. -
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. -
J. David Archibald
CURRICULUM VITAE J. DAVID ARCHIBALD AFFILIATION Department of Biology MAILING ADDRESS 4615 48th St San Diego State University San Diego, CA 92115-3206 5500 Campanile Dr. San Diego State University San Diego, CA 92182-4614 PHONE (619) 933-3075 E-MAIL [email protected] FACULTY PAGE http://www.bio.sdsu.edu/faculty/archibald.html EDUCATION B. Sc. in Geology, Kent State University, 1972, Magna cum Laude Ph. D. in Paleontology, University of California, Berkeley 1977 TEACHING EXPERIENCE AND ACADEMIC POSITIONS 1974-75: Teaching Assistant, Paleontology, University of California, Berkeley Courses assisted for: Introduction to Paleontology, undergraduate Morphology of the Vertebrate Skeleton, undergraduate Floras of the Past, undergraduate Phylogeny and Evolution, undergraduate 1977-79: J. Willard Gibbs Instructor (a postdoctoral fellowship), Dept. of Geology & Geophysics, Yale University Problems in Cretaceous-Paleogene Vertebrate Evolution, graduate seminar Evolution of Vertebrates to Man, undergraduate Paleobiology of Mammals, graduate Seminar in Primate Paleobiology (with D. Pilbeam) 1979-83: Assistant Professor (1979-1983) Associate Professor (promoted 1983, but declined promotion), Department of Biology, Yale University Vertebrate Anatomy, undergraduate Biologic Processes and Paleontologic Patterns, graduate seminar (with faculty from Biology, Geology, and Anthropology) Biology of Mammals, undergraduate Evolution, undergraduate (team taught) Paleobiology of Mammals, graduate Variability seminar (with faculty from Biology, Geology, Anthropology, -
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. -
Phylogenetic Tree of Litopterna and Perissodactyla Indicates a Complex Early History of Hoofed Mammals Nicolás R
www.nature.com/scientificreports OPEN Phylogenetic tree of Litopterna and Perissodactyla indicates a complex early history of hoofed mammals Nicolás R. Chimento1,2* & Federico L. Agnolin1,2,3 The Litopterna is an extinct clade of endemic South American ungulates that range from Paleocene up to late Pleistocene times. Because of their unique anatomy, litopterns are of uncertain phylogenetic afnities. However, some nineteenth century authors, considered litopterns as related to perissodactyl ungulates, a hypothesis recently sustained by molecular data. The aim of the present contribution is to include litopterns and other South American related taxa in a comprehensive phylogenetic analysis together with several extant and extinct basal perissodactyl ungulates. The analysis resulted in the nesting of litopterns and kin as successive stem-clades of crown Perissodactyla. Further, litopterns are not phylogenetically grouped with any North American basal ungulate, in agreement with some previous proposals. Presence of pan-perissodactyls in South America and India indicates that southern continents probably played an important role in the early evolution of hoofed mammals. Te mammalian group Litopterna was coined by Ameghino 1 as a Suborder of the Perissodactyla, with the aim to include the aberrant Macrauchenia and its kin. Ameghino recognized afnities with the Laurasian clade Perissodactyla, a hypothesis sustained by some old workers2,3. Tis idea was posteriorly criticized and refuted, and it was proposed that the similarities between litopterns and perissodactyls were acquired by convergence 4,5. In the same line of thought, together with xenar- thrans and marsupials, South American native ungulates were considered by Simpson6,7 as comprising the “Ancient Immigrants” Faunistic Stratum, coming from North America through a intercontinental bridge. -
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).