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Digital Reconstruction of the Inner Ear of Leptictidium Auderiense
View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by RERO DOC Digital Library Published in "Paläontologische Zeitschrift 90(1): 153–171, 2016" which should be cited to refer to this work. Digital reconstruction of the inner ear of Leptictidium auderiense (Leptictida, Mammalia) and North American leptictids reveals new insight into leptictidan locomotor agility Irina Ruf1,2 • Virginie Volpato1,3 • Kenneth D. Rose4 • Guillaume Billet2,5 • Christian de Muizon5 • Thomas Lehmann1 Abstract Leptictida are basal Paleocene to Oligocene semicircular canals than the leptictids under study. Our eutherians from Europe and North America comprising estimations reveal that Leptictidium was a very agile ani- species with highly specialized postcranial features mal with agility score values (4.6 and 5.5, respectively) including elongated hind limbs. Among them, the Euro- comparable to Macroscelidea and extant bipedal saltatory pean Leptictidium was probably a bipedal runner or jum- placentals. Leptictis and Palaeictops have lower agility per. Because the semicircular canals of the inner ear are scores (3.4 to 4.1), which correspond to the more gener- involved in detecting angular acceleration of the head, their alized types of locomotion (e.g., terrestrial, cursorial) of morphometry can be used as a proxy to elucidate the agility most extant mammals. In contrast, the angular velocity in fossil mammals. Here we provide the first insight into magnitude predicted from semicircular canal angles sup- inner ear anatomy and morphometry of Leptictida based on ports a conflicting pattern of agility among leptictidans, but high-resolution computed tomography of a new specimen the significance of these differences might be challenged of Leptictidium auderiense from the middle Eocene Messel when more is known about intraspecific variation and the Pit (Germany) and specimens of the North American pattern of semicircular canal angles in non-primate Leptictis and Palaeictops. -
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. -
Learning About Mammals
Learning About Mammals The mammals (Class Mammalia) includes everything from mice to elephants, bats to whales and, of course, man. The amazing diversity of mammals is what has allowed them to live in any habitat from desert to arctic to the deep ocean. They live in trees, they live on the ground, they live underground, and in caves. Some are active during the day (diurnal), while some are active at night (nocturnal) and some are just active at dawn and dusk (crepuscular). They live alone (solitary) or in great herds (gregarious). They mate for life (monogamous) or form harems (polygamous). They eat meat (carnivores), they eat plants (herbivores) and they eat both (omnivores). They fill every niche imaginable. Mammals come in all shapes and sizes from the tiny pygmy shrew, weighing 1/10 of an ounce (2.8 grams), to the blue whale, weighing more than 300,000 pounds! They have a huge variation in life span from a small rodent living one year to an elephant living 70 years. Generally, the bigger the mammal, the longer the life span, except for bats, which are as small as rodents, but can live for up to 20 years. Though huge variation exists in mammals, there are a few physical traits that unite them. 1) Mammals are covered with body hair (fur). Though marine mammals, like dolphins and whales, have traded the benefits of body hair for better aerodynamics for traveling in water, they do still have some bristly hair on their faces (and embryonically - before birth). Hair is important for keeping mammals warm in cold climates, protecting them from sunburn and scratches, and used to warn off others, like when a dog raises the hair on its neck. -
New Large Leptictid Insectivore from the Late Paleogene of South Dakota, USA
New large leptictid insectivore from the Late Paleogene of South Dakota, USA TJ MEEHAN and LARRY D. MARTIN Meehan, T.J. and Martin, L.D. 2012. New large leptictid insectivore from the Late Paleogene of South Dakota, USA. Acta Palaeontologica Polonica 57 (3): 509–518. From a skull and mandible, we describe a new genus and species of a primitive insectivore (Mammalia: Insectivora: Leptictida: Leptictidae). Its large body size and higher−crowned teeth indicate a different feeding ecology from other leptictid insectivores. With evidence of some heavy, flat wear on the molariform teeth, its shift in diet was likely to greater herbivory. Unlike the narrow snout of Blacktops, this new leptictid retains a broad snout, suggesting that small verte− brates were still important dietary components. The specimen was collected from the floodplain deposits of the lower or middle White River Group of South Dakota, which represent the latest Eocene to earliest Oligocene (Chadronian and Orellan North American Land Mammal “Ages”). Key words: Mammalia, Leptictidae, Leptictis, Megaleptictis, Eocene, Oligocene, White River Group, South Dakota, North America. TJ Meehan [[email protected]], Research Associate, Section of Vertebrate Paleontology, Carnegie Museum of Natural History, 4400 Forbes Avenue, Pittsburgh, PA 15213, USA; Larry D. Martin [[email protected]], Division of Vertebrate Paleontology, Natural History Museum and Biodiversity Re− search Center, University of Kansas, Lawrence, KS 66045, USA. Received 4 April 2011, accepted 25 July 2011, available online 17 August 2011. Introduction molariform teeth. A fossa in this region at least suggests in− creased snout mobility, but no definitive anatomical argument Leptictida is a primitive order of placental, insectivorous has been made to support a highly mobile cartilaginous snout mammals convergent to extant sengis or elephant “shrews” tip, as in sengis. -
71St Annual Meeting Society of Vertebrate Paleontology Paris Las Vegas Las Vegas, Nevada, USA November 2 – 5, 2011 SESSION CONCURRENT SESSION CONCURRENT
ISSN 1937-2809 online Journal of Supplement to the November 2011 Vertebrate Paleontology Vertebrate Society of Vertebrate Paleontology Society of Vertebrate 71st Annual Meeting Paleontology Society of Vertebrate Las Vegas Paris Nevada, USA Las Vegas, November 2 – 5, 2011 Program and Abstracts Society of Vertebrate Paleontology 71st Annual Meeting Program and Abstracts COMMITTEE MEETING ROOM POSTER SESSION/ CONCURRENT CONCURRENT SESSION EXHIBITS SESSION COMMITTEE MEETING ROOMS AUCTION EVENT REGISTRATION, CONCURRENT MERCHANDISE SESSION LOUNGE, EDUCATION & OUTREACH SPEAKER READY COMMITTEE MEETING POSTER SESSION ROOM ROOM SOCIETY OF VERTEBRATE PALEONTOLOGY ABSTRACTS OF PAPERS SEVENTY-FIRST ANNUAL MEETING PARIS LAS VEGAS HOTEL LAS VEGAS, NV, USA NOVEMBER 2–5, 2011 HOST COMMITTEE Stephen Rowland, Co-Chair; Aubrey Bonde, Co-Chair; Joshua Bonde; David Elliott; Lee Hall; Jerry Harris; Andrew Milner; Eric Roberts EXECUTIVE COMMITTEE Philip Currie, President; Blaire Van Valkenburgh, Past President; Catherine Forster, Vice President; Christopher Bell, Secretary; Ted Vlamis, Treasurer; Julia Clarke, Member at Large; Kristina Curry Rogers, Member at Large; Lars Werdelin, Member at Large SYMPOSIUM CONVENORS Roger B.J. Benson, Richard J. Butler, Nadia B. Fröbisch, Hans C.E. Larsson, Mark A. Loewen, Philip D. Mannion, Jim I. Mead, Eric M. Roberts, Scott D. Sampson, Eric D. Scott, Kathleen Springer PROGRAM COMMITTEE Jonathan Bloch, Co-Chair; Anjali Goswami, Co-Chair; Jason Anderson; Paul Barrett; Brian Beatty; Kerin Claeson; Kristina Curry Rogers; Ted Daeschler; David Evans; David Fox; Nadia B. Fröbisch; Christian Kammerer; Johannes Müller; Emily Rayfield; William Sanders; Bruce Shockey; Mary Silcox; Michelle Stocker; Rebecca Terry November 2011—PROGRAM AND ABSTRACTS 1 Members and Friends of the Society of Vertebrate Paleontology, The Host Committee cordially welcomes you to the 71st Annual Meeting of the Society of Vertebrate Paleontology in Las Vegas. -
The Hypocone As a Key Innovation in Mammalian Evolution (Adaptive Zone/Convergent Evolution/Dentition/Diversity/Theria) JOHN P
Proc. Natl. Acad. Sci. USA Vol. 92, pp. 10718-10722, November 1995 Evolution The hypocone as a key innovation in mammalian evolution (adaptive zone/convergent evolution/dentition/diversity/Theria) JOHN P. HUNTER* AND JUKKA JERNVALLt *Department of Anatomical Sciences, State University of New York, Stony Brook, NY 11794-8081; and tDepartment of Ecology and Systematics and Institute of Biotechnology, University of Helsinki, P.O. Box 17, FIN-00014, Finland Communicated by Elwyn L. Simons, Duke University Primate Center, Durham, NC, June 19, 1995 ABSTRACT The hypocone, a cusp added to the primi- occlusal contact between metacrista and paracristid (16), tively triangular upper molar teeth of therian mammals, has crests that are well developed in carnivorous mammals. Thus, evolved convergently >20 times among mammals during the possession of a hypocone is generally thought to be associated Cenozoic. Acquisition of the hypocone itself involves little with herbivory. phenotypic change, but subsequent diversification of groups We investigated the evolutionary potential of the hypocone possessing the hypocone may be greatly enhanced. Our anal- in two ways. First, we compared taxonomic diversity of living, ysis of the Cenozoic mammalian radiations, including the terrestrial, nonvolant mammals with different molar types Recent fauna, shows that high species diversity of mammals across dietary groups to determine whether the hypocone is with hypocones and association of the hypocone with her- indeed associated with herbivorous habits and whether mam- bivory strongly support recognition of the hypocone as a key mals with hypocones are more diverse today than those lacking innovation that has allowed invasion of, and diversification hypocones. Second, we compared the taxonomic diversity of within, herbivorous adaptive zones. -
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. -
A Aardvark, 96 Abderites, 15, 162 Abderitidae, 11, 159, 200 Aboriginal, 15, 17 Adamantina, 79, 83 Africa, 79, 96, 116, 127, 130
Index A Antarctic Circumpolar Current (ACC), 126, Aardvark, 96 188, 210 Abderites, 15, 162 Antarctic Counter Current, 104 Abderitidae, 11, 159, 200 Antarctic Peninsula, 12, 80, 83, 97, 109, Aboriginal, 15, 17 113–116, 165, 187, 216 Adamantina, 79, 83 Antarctic Region, 113, 133 Africa, 79, 96, 116, 127, 130, 141 Antarctodonas, 110 Afrotemperate Region, 133 Antechinus, 56 Afrothere, 96 Aonken Sea, 139 Afrotheria, 96, 97 Aptian, 79, 98, 129 Alamitan, 83, 90, 95, 141, 211 Aquatic, 130 Alchornea, 113 Araceae, 113 Alcidedorbignia, 94 Araucaria, 130 Alisphenoid, 10, 11 Arboreal, 6, 12, 38, 58–61, 64, 65 Allen, 80 Archaeodolops, 195 Allenian, 211 Archaeohyracidae, 143 Allotherian, 212 Archaeonothos, 109 Allqokirus, 95, 214 Arctodictis, 166 Alphadelphian, 214 Arecaceae, 113 Altiplano, 127 Argentina, 13, 17, 19, 22, 61, 80, 83, 95, 107, Altricial, 203 112, 116, 130, 135, 136, 138, 157 Ameghinichnus, 140 Argentodites, 212 Ameridelphia, 157, 165, 166, 186, 192, 195 Argyrolagidae, 13, 158, 196, 220 Ameridelphian, 91, 95, 106, 107, 110, 157, Argyrolagoidea, 13, 143, 195, 201, 220 166, 200, 213, 215, 216 Argyrolagus, 158, 220 Amphidolops, 195, 200 Arid diagonal, 135, 136, 138 Anachlysictis, 23, 161 Arminiheringia, 166, 194 Andean Range, 133 A1 scenario, 138 Andean Region, 127, 132, 133, 135, 136 Ascending ramus, 170 Andes, 12, 127 Asia, 6, 127, 156, 202 Andinodelphys, 95, 157, 159 Astragalar, 10 Angiosperm, 114, 115, 129, 190 Astrapotheria, 3 Angular process, 10, 11, 171, 175 Atacama Desert, 130, 133, 136 Animalivore, 47 Atlantic Forest, 61, 130 Animalivorous, 47 Atlantic Ocean, 137 Ankle bone, 96, 107 Atlantogenata, 97 Antarctica, 8, 12, 79, 98–100, 104, 109, 112, Australasia, 218 115, 116, 126, 127, 133, 135, 137, 210, 220 © Springer Science+Business Media Dordrecht 2016 227 F.J. -
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. -
Rapid and Early Post-Flood Mammalian Diversification Videncede in the Green River Formation
The Proceedings of the International Conference on Creationism Volume 6 Print Reference: Pages 449-457 Article 36 2008 Rapid and Early Post-Flood Mammalian Diversification videncedE in the Green River Formation John H. Whitmore Cedarville University Kurt P. Wise Southern Baptist Theological Seminary Follow this and additional works at: https://digitalcommons.cedarville.edu/icc_proceedings DigitalCommons@Cedarville provides a publication platform for fully open access journals, which means that all articles are available on the Internet to all users immediately upon publication. However, the opinions and sentiments expressed by the authors of articles published in our journals do not necessarily indicate the endorsement or reflect the views of DigitalCommons@Cedarville, the Centennial Library, or Cedarville University and its employees. The authors are solely responsible for the content of their work. Please address questions to [email protected]. Browse the contents of this volume of The Proceedings of the International Conference on Creationism. Recommended Citation Whitmore, John H. and Wise, Kurt P. (2008) "Rapid and Early Post-Flood Mammalian Diversification Evidenced in the Green River Formation," The Proceedings of the International Conference on Creationism: Vol. 6 , Article 36. Available at: https://digitalcommons.cedarville.edu/icc_proceedings/vol6/iss1/36 In A. A. Snelling (Ed.) (2008). Proceedings of the Sixth International Conference on Creationism (pp. 449–457). Pittsburgh, PA: Creation Science Fellowship and Dallas, TX: Institute for Creation Research. Rapid and Early Post-Flood Mammalian Diversification Evidenced in the Green River Formation John H. Whitmore, Ph.D., Cedarville University, 251 N. Main Street, Cedarville, OH 45314 Kurt P. Wise, Ph.D., Southern Baptist Theological Seminary, 2825 Lexington Road. -
Late Paleocene) of the Eastern Crazy Mountain Basin, Montana
CONTRIBUTIONS FROM THE MUSEUM OF PALEONTOLOGY THE UNIVERSITY OF MICHIGAN VOL. 26, NO. 9, p. 157-196 December 3 1, 1983 MAMMALIAN FAUNA FROM DOUGLASS QUARRY, EARLIEST TIFFANIAN (LATE PALEOCENE) OF THE EASTERN CRAZY MOUNTAIN BASIN, MONTANA BY DAVID W. KRAUSE AND PHILIP D. GINGERICH MUSEUM OF PALEONTOLOGY THE UNIVERSITY OF MICHIGAN ANN ARBOR CONTRIBUTIONS FROM THE MUSEUM OF PALEONTOLOGY Philip D. Gingerich, Director Gerald R. Smith, Editor This series of contributions from the Museum of Paleontology is a medium for the publication of papers based chiefly upon the collection 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 papers may also be obtained. Correspondence should be directed to the Museum of Paleontology, The University of Michigan, Ann Arbor, Michigan, 48 109. VOLS. 11-XXVI. Parts of volumes may be obtained if available. Price lists available upon inquiry. MAMMALIAN FAUNA FROM DOUGLASS QUARRY, EARLIEST TIFFANIAN (LATE PALEOCENE) OF THE EASTERN CRAZY MOUNTAIN BASIN, MONTANA BY David W. ~rause'and Philip D. ~in~erich' Abstract.-Douglass Quarry is the fourth major locality to yield fossil mammals in the eastern Crazy Mountain Basin of south-central Montana. It is stratigraphically intermediate between Gidley and Silberling quarries below, which are late Torrejonian (middle Paleocene) in age, and Scarritt Quarry above, which is early Tiffanian (late Paleocene) in age. The stratigraphic position of Douglass Quarry and the presence of primitive species of Plesiadapis, Nannodectes, Phenacodus, and Ectocion (genera first appearing at the Torrejonian-Tiffanian boundary) combine to indicate an earliest Tiffanian age.