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GEOL 204 the Fossil Record Spring 2020 Section 0109 Luke Buczynski, Eamon, Doolan, Emmy Hudak, and Shutian Wang
ENTELODONT: The Hellacious Pigs of the Cenozoic GEOL 204 The Fossil Record Spring 2020 Section 0109 Luke Buczynski, Eamon, Doolan, Emmy Hudak, and Shutian Wang Entelodont Overview: From the family Entelodontidae, these omnivorous mammals had a wide geographic variety, as seen in image B. They first inhabited Mongolia then spread into Eurasia and North America, while in North America they preferred flood plains and woodlands. Entelodont were fairly aggressive and would fight with their own kind, using their strong jaws and large heads. They survived from the middle of Eocene to the middle of Miocene. Size and Diet: Skull Features: Figure D shows one of the largest Entelodont, Daedon, compared to an As seen on Figure C, the skull of the Entelodont is massive. They all 1.8 meter tall human, illustrating how immense they really were. contained large Neural Spines, most likely to hold up their huge head, Entelodont weighed from 150 kg on the small size, up to 900 kg (330 to which in turn created a hump. Entelodont contained a pretty small 2,000 pounds) and 1 to 2 meters in height. They had teeth that made them brain, but large olfactory lobes, giving them an acute sense of smell. capable of consuming meat, but the overall structure and wear on the the They held sturdy canines, long incisors, sharp serrated premolars, and suggest the consumption of plant matter as well. Although these large blunt square molars (a sign of omnivory), all of which were covered in a animals might not look it, their limbs were fully terrestrial and adept for very thick layer of enamel. -
Agate Fossil Beds
University of Nebraska - Lincoln DigitalCommons@University of Nebraska - Lincoln U.S. National Park Service Publications and Papers National Park Service 1980 Agate Fossil Beds Follow this and additional works at: http://digitalcommons.unl.edu/natlpark "Agate Fossil Beds" (1980). U.S. National Park Service Publications and Papers. 160. http://digitalcommons.unl.edu/natlpark/160 This Article is brought to you for free and open access by the National Park Service at DigitalCommons@University of Nebraska - Lincoln. It has been accepted for inclusion in U.S. National Park Service Publications and Papers by an authorized administrator of DigitalCommons@University of Nebraska - Lincoln. Agate Fossil Beds cap. tfs*Af Clemson Universit A *?* jfcti *JpRPP* - - - . Agate Fossil Beds Agate Fossil Beds National Monument Nebraska Produced by the Division of Publications National Park Service U.S. Department of the Interior Washington, D.C. 1980 — — The National Park Handbook Series National Park Handbooks, compact introductions to the great natural and historic places adminis- tered by the National Park Service, are designed to promote understanding and enjoyment of the parks. Each is intended to be informative reading and a useful guide before, during, and after a park visit. More than 100 titles are in print. This is Handbook 107. You may purchase the handbooks through the mail by writing to Superintendent of Documents, U.S. Government Printing Office, Washington DC 20402. About This Book What was life like in North America 21 million years ago? Agate Fossil Beds provides a glimpse of that time, long before the arrival of man, when now-extinct creatures roamed the land which we know today as Nebraska. -
A Revision of the Entelodontidae
MEMOIRS OF THE CARNEGIE MUSEUM. VOL. IV. NO. 3. A REVISION OF THE ENTELODONTIDyE.' By O. A. Peterson. Introductory Remarks. 227-242)- Since A. Aymard (1, pp. and S. A. Pomel (73, p. 307 ; 74, p. 1083) described the genus Entclodon from the Tertiary deposits of France, much material has been found, which represents this unique family of mammals, especially in the Oligoceneand Miocene formations of the North American Tertiary. The object of the present Memoir is first to give a systematic review of the known genera and species of this family ; and secondly to describe and illustrate in detail the type specimen of Dinohyus hoUandi, which was discovered in the Agate Spring Fossil (Quarries, Sioux County, Nebraska, by the Carnegie Museum Expedition of 1 905, and briefly described in Science (78, pp. 211-212) and the Annals of the Carnegie Museum (81, pp. 49-51). At the very outset of his work the writer became fully aware of the fact that generic and specific determinations in this family have sometimes been based on rather inadequate types, which present few and unsatisfactory characters. Frag- 'Pomel's (lesoription (73, 74) of Elotherium did probably appear before that of Aymard on Fnlelodon, but, iiias- luuch as the type of the former was rather inadequate, no illustrations were published, and the type has been since lost (see page 43), the present writer is of the opinion that the latter name should be used, as both text and figures are clear. ' For the references in parentheses, see the Bibliography appended. ( Publislied May, 1909.) 41 42 MEMOIRS OF THE CARNEGIE MUSEUM mentary types, which very often are most exasperating to the student of paleontol- ogy, cannot be regarded as finally determining genera and species, and in the pres- ent case we must still await the slow process of discovery before a number of questions can be satisfactorily determined. -
Agate Fossil Beds National Monument, Paleontological Resources Management Plan (Public Version)
University of Nebraska - Lincoln DigitalCommons@University of Nebraska - Lincoln U.S. National Park Service Publications and Papers National Park Service 9-2020 Agate Fossil Beds National Monument, Paleontological Resources Management Plan (Public Version) Scott Kottkamp United States National Park Service, Agate Fossil Beds National Monument Vincent L. Santucci United States National Park Service, Geologic Resources Division Justin S. Tweet United States National Park Service Jessica De Smet University of Oregon Ellen Stark United States National Park Service, Badlands National Park Follow this and additional works at: https://digitalcommons.unl.edu/natlpark Part of the Environmental Education Commons, Environmental Policy Commons, Environmental Studies Commons, Fire Science and Firefighting Commons, Leisure Studies Commons, Natural Resource Economics Commons, Natural Resources Management and Policy Commons, Nature and Society Relations Commons, Other Environmental Sciences Commons, Other Life Sciences Commons, Paleontology Commons, Physical and Environmental Geography Commons, Public Administration Commons, and the Recreation, Parks and Tourism Administration Commons Kottkamp, Scott; Santucci, Vincent L.; Tweet, Justin S.; De Smet, Jessica; and Stark, Ellen, "Agate Fossil Beds National Monument, Paleontological Resources Management Plan (Public Version)" (2020). U.S. National Park Service Publications and Papers. 238. https://digitalcommons.unl.edu/natlpark/238 This Article is brought to you for free and open access by the National Park -
2014BOYDANDWELSH.Pdf
Proceedings of the 10th Conference on Fossil Resources Rapid City, SD May 2014 Dakoterra Vol. 6:124–147 ARTICLE DESCRIPTION OF AN EARLIEST ORELLAN FAUNA FROM BADLANDS NATIONAL PARK, INTERIOR, SOUTH DAKOTA AND IMPLICATIONS FOR THE STRATIGRAPHIC POSITION OF THE BLOOM BASIN LIMESTONE BED CLINT A. BOYD1 AND ED WELSH2 1Department of Geology and Geologic Engineering, South Dakota School of Mines and Technology, Rapid City, South Dakota 57701 U.S.A., [email protected]; 2Division of Resource Management, Badlands National Park, Interior, South Dakota 57750 U.S.A., [email protected] ABSTRACT—Three new vertebrate localities are reported from within the Bloom Basin of the North Unit of Badlands National Park, Interior, South Dakota. These sites were discovered during paleontological surveys and monitoring of the park’s boundary fence construction activities. This report focuses on a new fauna recovered from one of these localities (BADL-LOC-0293) that is designated the Bloom Basin local fauna. This locality is situated approximately three meters below the Bloom Basin limestone bed, a geographically restricted strati- graphic unit only present within the Bloom Basin. Previous researchers have placed the Bloom Basin limestone bed at the contact between the Chadron and Brule formations. Given the unconformity known to occur between these formations in South Dakota, the recovery of a Chadronian (Late Eocene) fauna was expected from this locality. However, detailed collection and examination of fossils from BADL-LOC-0293 reveals an abundance of specimens referable to the characteristic Orellan taxa Hypertragulus calcaratus and Leptomeryx evansi. This fauna also includes new records for the taxa Adjidaumo lophatus and Brachygaulus, a biostratigraphic verifica- tion for the biochronologically ambiguous taxon Megaleptictis, and the possible presence of new leporid and hypertragulid taxa. -
OLIGOCENE MAMMALS from ROMANIA Remains of Oligocene
THE OLIGOCENE FROM THE TRANSYLVANIAN BASIN, P. 301-312. Cluj-Napoca, 1989. OLIGOCENE MAMMALS FROM ROMANIA C. RADULESCU*, P. SAMSON* Nine species of Oligocene mammals representing three orders and six families are known from Romania. The main area of interest is the Transylvanian basin which yielded the majority of finds of large mammals. Lower Oligocene mammals include "Ronzotherium" kochi (lower Stampian, Ronzon level), Entelodon aff. deguilhemi (lower Stampian, Villebramar level or somewhat older), Kochictis cen tennii, Entelodontidae indet. cf. Pamentelodon sp., Anthracotherium sp. (large size) (upper Stampian,? La Ferte-"Alais level); a new species of indricothere, Benarathe rium gabuniai n. sp. (upper Stampian, ? Etampes level) is described and its rela tionships discussed. Upper Oligocene mammals include Anthracotherium sp. (me dium size), an indricothere (Paraceratherium prohorovi) and a new species of amynodontid. Other mammalian remains are recorded from the Petro~ani basin and adjacent area: Entelodon magnus, Hateg basin, lower Oligocene (lower Stam pian, Ronzon level) and Anthracotherium sp. (large size), Petro~ani basin (coal layers), upper Oligocene (Chattian). No micromammals has been reported from Romariia. Key words: macromammals, Oligocene, Transylvania, Romania, systematics, chro nology. 1. Introduction. Remains of Oligocene macromammals are known in Romania from two areas of unequal importance. The most significant fossils were dis covered in the northweastern part of the Transylvanian basin. Some other remains were described from the Hateg and Petro$ani basins. In the present paper the geologic age of the mammalian fossils is reviewd in the light of recent stratigraphic interpretations (foraminifera, ostracoda, nannoplankton, mollusca, fossil flora) (see references in A. R u s u , 1977, 1983). -
Early Miocene Hippopotamids (Cetartiodactyla) Constrain the Phylogenetic and Spatiotemporal Settings of Hippopotamid Origin
Early Miocene hippopotamids (Cetartiodactyla) constrain the phylogenetic and spatiotemporal settings of hippopotamid origin Maeva Orliaca,1, Jean-Renaud Boisserieb,c, Laura MacLatchyd, and Fabrice Lihoreaua aInstitut des Sciences de l’Evolution, Unité Mixte de Recherche 5554, Université Montpellier 2, 34000 Montpellier, France; bCentre Français des Etudes Ethiopiennes/French Centre for Ethiopian Studies, Centre National de la Recherche Scientifique Unité de Service et de Recherche 3137, Addis Ababa, Ethiopia; cInstitut International de Paléoprimatologie, Paléontologie Humaine: Evolution et Paléoenvironnements, Unité Mixte de Recherche 6046, Université de Poitiers, F-86022 Poitiers, France; and dDepartment of Anthropology, University of Michigan, Ann Arbor, MI 48109 Edited* by David Pilbeam, Harvard University, Cambridge, MA, and approved May 5, 2010 (received for review February 3, 2010) The affinities of the Hippopotamidae are at the core of the phy- ctyl clades (Cetancodonta, Ruminantia, Suoidea, and Tylopoda) logeny of Cetartiodactyla (even-toed mammals: cetaceans, ru- remained unresolved in recent combined analyses of extinct and minants, camels, suoids, and hippos). Molecular phylogenies extant data (ref. 9, figure 2; refs. 15 and 16). However, these and support Cetacea as sister group of the Hippopotamidae, implying other recent large-scale analyses aiming at clarifying cetartio- a long ghost lineage between the earliest cetaceans (∼53 Ma) and dactyl basal relationships (10, 11, 17–20) included none or only the earliest hippopotamids (∼16 Ma). Morphological studies have a limited subset of fossil “suiforms” classically and more con- proposed two different sister taxa for hippopotamids: suoids (no- troversially interpreted as hippopotamid stem groups and, in all tably palaeochoerids) or anthracotheriids. Evaluating these phylo- cases, no fossil hippopotamids. -
Unexpected Evolutionary Patterns of Dental Ontogenetic Traits in Cetartiodactyl Mammals Helder Gomes Rodrigues, Fabrice Lihoreau, Maëva Orliac, J
Unexpected evolutionary patterns of dental ontogenetic traits in cetartiodactyl mammals Helder Gomes Rodrigues, Fabrice Lihoreau, Maëva Orliac, J. Thewissen, Jean-Renaud Boisserie To cite this version: Helder Gomes Rodrigues, Fabrice Lihoreau, Maëva Orliac, J. Thewissen, Jean-Renaud Boisserie. Un- expected evolutionary patterns of dental ontogenetic traits in cetartiodactyl mammals. Proceed- ings of the Royal Society B: Biological Sciences, Royal Society, The, 2019, 286 (1896), pp.20182417. 10.1098/rspb.2018.2417. hal-03098504 HAL Id: hal-03098504 https://hal.archives-ouvertes.fr/hal-03098504 Submitted on 5 Jan 2021 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. Unexpected evolutionary patterns of dental ontogenetic traits in cetartiodactyl mammals Helder GOMES RODRIGUES1, Fabrice LIHOREAU1, Maëva ORLIAC1, J.G.M. THEWISSEN2, Jean-Renaud BOISSERIE3 1Institut des Sciences de l’Evolution de Montpellier (ISEM), Univ Montpellier, CNRS, IRD, Montpellier, France 2Department of Anatomy, Northeastern Ohio Universities College of Medicine, Rootstown, Ohio 44272, USA 3Laboratoire Paléontologie Evolution Paléoécosystèmes Paléoprimatologie, CNRS, Université de Poitiers - UFR SFA, Bât B35 - TSA 51106, 86073 Poitiers Cedex 9, France Corresponding author: Helder Gomes Rodrigues Email address: [email protected] Telephone: +33 1 40 79 36 73 1 Abstract Studying ontogeny in both extant and extinct species can unravel the mechanisms underlying mammal diversification and specialization. -
OREGON GEOLOGY Published by The
OREGON GEOLOGY published by the Oregon Department of Geology and Mineral Industries 1931 VOLUME 58, NUMBER 3 MAY 1996 Hyrachus eximius Alnus heterodonta Telmatherium manteoceras Orohippus major corsonr Patriofelis ferox IN THIS ISSUE: Reconstructions of Eocene and Oligocene Plants and Animals of Central Oregon OREGON GEOLOGY In memoriam: Volunteer Shirley O'Dell IISSN 0164-3304) Shirley O'Dell, volunteer at the Nature of the North west Information Center, died March 30, 1996. VOLUME 58, NUMBER 3 MAY 1996 Born in Minneapolis, Minnesota, she spent most of her Published bimonthly in Jaooary, Mardl, May, July, Sq:Kember, Md November by the Oregon Dcp.vncn of life in Portland, Oregon. She was a secretary at Charles F. Geology and MintnI IrnkJstries. (Volumes 1 tl'I'ough 40 wereemtJed The On Bin.) Berg, at an investment company, and at Columbia Grain Governing Board John W. Stephens, Chair .......................................................... Portland Company. After her retirement, she worked as a volunteer Jacqueline G. Haggerty ............................................ Weston Mountain at St. Vincent's Medical Center Gift Shop and at the Na Ronald K. Culbertson ...................................................... Myrtle Creek ture of the Northwest Infomation Center. She was a mem ber of the Geological Society of the Oregon Country State Geologist ............................................................ Donald A Hull Deputy State Geologist ........................................... John D. Beaulieu (GSOC) for more than 30 years -
Proceedings of the Tenth Conference on Fossil Resources May 13-15, 2014 Rapid City, South Dakota
PROCEEDINGS OF THE TENTH CONFERENCE ON FOSSIL RESOURCES May 13-15, 2014 Rapid City, South Dakota Edited by Vincent L. Santucci, Gregory A. Liggett, Barbara A. Beasley, H. Gregory McDonald and Justin Tweet Dakoterra Vol. 6 Eocene-Oligocene rocks in Badlands National Park, South Dakoata. Table of Contents Dedication ....................................................................................8 Introduction ..................................................................................9 Presentation Abstracts *Preserving THE PYGMY MAMMOTH: TWENTY YEARS OF collaboration BETWEEN CHANNEL ISLANDS National PARK AND THE MAMMOTH SITE OF HOT SPRINGS, S. D., INC. LARRY D. AGENBROAD, MONICA M. BUGBEE, DON P. MORRIS and W. JUSTIN WILKINS .......................10 PERMITS AND PALEONTOLOGY ON BLM COLORADO: RESULTS FROM 2009 TO 2013 HARLEY J. ARMSTRONG .....................................................................................................................................10 DEVIL’S COULEE DINOSAUR EGG SITE AND THE WILLOW CREEK HOODOOS: HOW SITE VARIABLES INFLUENCE DECISIONS MADE REGARDING PUBLIC ACCESS AND USE AT TWO DESIGNATED PROVINCIAL HISTORIC SITES IN ALBERTA, CANADA JENNIFER M. BANCESCU ...................................................................................................................................12 USDA FOREST SERVICE PALEONTOLOGY PASSPORT IN TIME PROGRAM: COST EFFECTIVE WAY TO GET FEDERAL PALEONTOLOGY PROJECTS COMPLETED BARBARA A. BEASLEY and SALLY SHELTON ...................................................................................................17 -
From the Paleogene of Mongolia
HYRACODONTIDS AND RHINOCEROTIDS (MAMMALIA, PERISSODACTYLA, RHINOCEROTOIDEA) FROM THE PALEOGENE OF MONGOLIA by Demberelyin DASHZEVEG· CONTENTS Page Abstract, Resulue ............. , .......... ,................................................ 2 Introduction ......................... , ................................. "., ............. 3 The key localities of the Paleogene of Mongolia and adjacent territories of Northern China with fossil hyracodontids and rhinocerotids .......................... , . 5 Mongolia ........................................................................... 5 Eastern Gobi Desert ........................................ ,...................... 5 The Valley of Lakes ............................................................... 9 Northern China: Inner Mongolia .............. , ........................ , .... , ......... '. 11 The Basin of Irell Dabasu .......... , .......... , .................................. " 11 Tbe Valley of tbe Shara MUfun River ................................................. 13 The EoceneJOligocene Boundary in Mongolia and Northern China ................................. 14 Mongolia: Eastern Gobi Desert . .. .. .. .. .. 16 Northern China: Inner Mongolia ......................................................... 17 Eocene and Oligocene correlation in the Eastern Gobi Desert (Mongolia) and North China .............. 18 Systenlatics .......................... , ........ , ...................................... " 22 Family Hyracodolltidae ............................................................ -
New Postcranial Bones of the Extinct Mammalian Family Nyctitheriidae (Paleogene, UK): Primitive Euarchontans with Scansorial Locomotion
Palaeontologia Electronica palaeo-electronica.org New postcranial bones of the extinct mammalian family Nyctitheriidae (Paleogene, UK): Primitive euarchontans with scansorial locomotion Jerry J. Hooker ABSTRACT New postcranial bones from the Late Eocene and earliest Oligocene of the Hamp- shire Basin, UK, are identified as belonging to the extinct family Nyctitheriidae. Previ- ously, astragali and calcanea were the only elements apart from teeth and jaws to be unequivocally recognized. Now, humeri, radii, a metacarpal, femora, distal tibiae, naviculars, cuboids, an ectocuneiform, metatarsals and phalanges, together with addi- tional astragali and calcanea, have been collected. These are shown to belong to a diversity of nyctithere taxa previously named from dental remains. Functional analysis shows that nyctitheres had mobile shoulder and hip joints, could pronate and supinate the radius, partially invert the foot at the astragalocalcaneal and upper ankle joints using powerful flexor muscles, all indicative of a scansorial lifestyle and allowing head- first descent on vertical surfaces. Climbing appears to have been dominated by flexion of the forearms and feet. Cladistic analysis employing a range of primitive eutherian mammals shows that nyctitheres are stem euarchontans, rather than lipotyphlans, with which they had previously been classified based on dental characters. Earlier ideas of relationships with the extinct Adapisoriculidae, recently considered stem eutherians, are not upheld. Jerry J. Hooker. Department of Earth Sciences, Natural History Museum, Cromwell Road, London SW7 5BD, UK. [email protected] Keywords: Eutheria; Lipotyphla; placental; Scandentia; shrews; Soricidae INTRODUCTION basis of some straight slender limb bone shafts, apparently associated with teeth (on which this Nyctitherium Marsh, 1872, the type genus of genus was based), returned to Marsh’s original the eutherian family Nyctitheriidae Simpson, 1928a idea that Nyctitherium was a chiropteran.