Short Communication the Comparative Method and the Inference of Venom-Delivery Systems in Fossil Mammals
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
Paleocene Mammalian Faunas of the Bison Basin in South-Central Wyoming
SMITHSONIAN MISCELLANEOUS COLLECTIONS VOLUME 131, NUMBER 6 Cftarlesi ©, anb JHarp ^aux SKHalcott 3Res!earcf) Jf unb PALEOCENE MAMMALIAN FAUNAS OF THE BISON BASIN IN SOUTH-CENTRAL WYOMING (With 16 Plates) By C. LEWIS GAZIN Curator, Division of Vertebrate Paleontology United States National Museum Smithsonian Institution (Publication 4229) CITY OF WASHINGTON PUBLISHED BY THE SMITHSONIAN INSTITUTION FEBRUARY 28, 1956 THE LORD BALTIMORE PRESS, INC. BALTIMORE, MD., U. S. A. CONTENTS Page Introduction i Acknowledgments 2 History of investigation 2 Occurrence and preservation of material 3 The Bison basin faunas 4 Environment and relationships between the Bison basin faunas 7 Age and correlation of the faunas lo Systematic description of vertebrate remains I2 Reptilia 12 Sauria 12 Anguidae 12 Mammalia 12 Multitubcrculata 12 Ptilodontidae 12 Marsupialia 14 Didelphidae 14 Insectivora 15 Leptictidae 15 Pantolestidae 17 Primates 19 Plesiadapidae 19 Carnivora 25 Arctocyonidae 25 Mesonychidae 35 Miacidae 35 Condylarthra 36 Hyopsodontidae 36 Phenacodontidae 42 Pantodonta 47 Coryphodontidae 47 References 51 Explanation of plates 54 ILLUSTRATIONS Plates (All plates following page 58.) 1. Mullituberculates and insectivores from the Bison basin Paleocene. 2. Primates and marsupials from the Bison basin Paleocene. 3. Pronothodcctes from the Bison basin Paleocene. 4. Plcsiadapis from the Bison basin Paleocene. 5. Triccntcs and Chriacus from the Bison basin Paleocene. 6. Thryptacodon from the Bison basin Paleocene. 7. Clacnodon from the Bison basin Paleocene. 8. Litomylus and Protoselcnc? from the Bison basin Paleocene. 9. Haplaletes and Gidleyina from the Bison basin Paleocene. 10. Phcnacodusl from the Bison basin Paleocene. 11. Condylarths and Titanoidcs from the Bison basin Paleocene. 12. Caenolambda from the Bison basin Paleocene. -
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. -
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. -
Sept 2005 APS Bulletin
Palæontological S o c i e t y Bulletin VOLUMEAlberta 20 • NUMBER 3 www.albertapaleo.org SEPTEMBER 2005 ALBERTA PALÆONTOLOGICAL SOCIETY OFFICERS c. Provide information and expertise to other collectors. President Dan Quinsey 247-3022 d. Work with professionals at museums and universities Vice-President Ron Fortier 285-8041 to add to the palaeontological collections of the Treasurer Mona Marsovsky 547-0182 province (preserve Alberta’s heritage). Secretary Wendy Morrison 646-3186 Past-President Vaclav Marsovsky 547-0182 MEMBERSHIP: Any person with a sincere interest in palaeontology is eligible to present their application DIRECTORS for membership in the Society. (Please enclose mem- Editor Howard Allen 274-1858 bership dues with your request for application.) Membership Howard Allen 274-1858 Program Coordinator Philip Benham 280-6283 Single membership $20.00 annually Field Trip Coordinator Wayne Braunberger 278-5154 Family or Institution $25.00 annually COMMITTEES THE BULLETIN WILL BE PUBLISHED QUARTERLY: APAC† Howard Allen 274-1858 March, June, September and December. Deadline for sub- APS 20th Anniversary Dan Quinsey 247-3022 mitting material for publication is the 15th of the month Wayne Braunberger 278-5154 prior to publication. CRLC Show Dan Quinsey 247-3022 Wayne Braunberger 278-5154 Society Mailing Address: Education Dan Quinsey 247-3022 Alberta Palaeontological Society Fossil Collections Ron Fortier 285-8041 P.O. Box 35111, Sarcee Postal Outlet Fund Raising Dan Quinsey 247-3022 Calgary, Alberta, Canada T3E 7C7 Library Mona Marsovsky 547-0182 (Web: www.albertapaleo.org) Paleo Rangers Dan Quinsey 247-3022 Ron Fortier 285-8041 Material for the Bulletin: Social (position unfilled) Howard Allen, Editor, APS Website Vaclav Marsovsky 547-0182 7828 Hunterslea Crescent, N.W. -
NHS Dissertation4
Patterns and Processes in the Dental Evolution of North American Plesiadapiforms and Euprimates from the Late Paleocene and Early Eocene DISSERTATION Presented in Partial Fulfillment of the Requirements for the Degree of Doctor of Philosophy in the Graduate School of The Ohio State University By Naava Hadassah Schottenstein, B.S. Graduate Program in Evolution, Ecology and Organismal Biology The Ohio State University 2020 Dissertation Committee: John P. Hunter, Advisor Mark Hubbe Bryan Carstens Debbie Guatelli-Steinberg Copyright by Naava Hadassah Schottenstein 2020 Abstract This dissertation explores the radiation of Primates during the Paleogene. The first radiation of Primates began with the plesiadapiforms near the Cretaceous-Paleogene boundary and the second radiation marked the introduction and diversification of euprimates at the beginning of the Eocene. Questions surrounding these radiations include their general patterns of evolution, rates of dental evolution, and potential influences of abiotic and biotic drivers. I explore these questions in euprimates by presenting a study of the Tetonius- Pseudotetonius primate lineage. Rates of evolution and the roles of neutral and adaptive processes across this lineage remain unclear. Linking Tetonius and Pseudotetonius are a series of stratigraphic and morphologic intermediates revealing possible functional and developmental reorganization within the dentition. Notable changes involved a reduction of the P3 and the P4 became a robust tall-cusped tooth. I test whether neutral evolution can explain the phenotypic differences in the lineage, and whether P4 lost developmental association with P3 and became integrated with the molars. I calculate the rate of evolutionary differentiation, based on the ratio between inter- and intra-species variation in length and width of the premolars and molars, between lineage segments and the entire lineage. -
A Review of the Proteutheria and Insectivora of the Willwood Formation (Lower Eocene), Bighorn Basin, Wyoming
b 60 ~ r A Review of the Proteutheria and Insectivora of the Willwood Formation (lower Eocene), Bighorn Basin, Wyoming GEOLOGICAL SURVEY BULLETIN 1523 A Review of the Proteutheria and Insectivora of the Willwood Formation (lower Eocene), Bighorn Basin, Wyoming By THOMAS M BOWN and DAVID SCHANKLER GEOLOGICAL SURVEY BULLETIN 152: The Wzllwood sample of proteutherzans and znsectwores zs the largest and most dwerse known for lower Eocene rocks of the world UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON 1982 J UNITED STATES DEPARTMENT OF THE INTERIOR JAMES G. WATT, Secretary GEOLOGICAL SURVEY Dallas L. Peck, Dzrector Library of Congress Catalogmg m Publication Data Bown, Thomas M A rev1ew of the Proteuthena and Insectlvora of the Willwood Formation (Lower Eocene), B1ghom Basm, Wyom- mg (Geolog•cal Survey Bulletm 1523) Bibliography p 73 Supt ofDocs No I 19 3 1523 I Proteuthena 2 Insecllvora, Foss1l Paleontology-Eocene 4 Paleontology-B1ghom R1ver water-shed, Wyo and Mont I Schankler, Dav1d M II T1tle III Senes QE75 B9 No 1523 [QE882 15] 557 3s 81-607068 [569' 12] AACR2 For sale by the Branch of Dtstnbutton, U S Geologtcal Survey 604 South Ptckett Street, Alexandna, VA 22304 CONTENTS Page Absttact--------------------------------------------------- 1 InttoductiOn ------------------------ 2 History and purpose of mvestigation ---------------- 2 Prehmmary faunal zonation of the Willwood Formation-------- 3 Abbreviations ---------------------- 4 Acknowledgments ---------------------- 4 Systematic paleontology-------------------------- -
The Earliest Known Venomous Animals Recognized Among Conodonts
The earliest known venomous animals recognized among conodonts HUBERT SZANIAWSKI Szaniawski, H. 2009. The earliest known venomous animals recognized among conodonts. Acta Palaeontologica Polo− nica 54 (4): 669–676. doi:10.4202/app.2009.0045 Conodonts, a large group of tiny extinct marine animals ranging in age from the Late Cambrian to Late Triassic (ca. 500 to 200 Mya), are usually considered as jawless vertebrates. Their only commonly occurring fossilized remains are minute, phosphatic, teeth−like elements of their feeding apparatuses. In most of the early conodonts the elements were conical and strongly elongated. Many of them are characterized by possession of a deep, longitudinal groove, usually associated with sharp edges or ridges. A comparative study of the grooved elements and venomous teeth and spines of living and extinct vertebrates strongly suggests that the groove in conodonts was also used for delivery of venom. Structural convergence of the conodont apparatus Panderodus with the grasping apparatus of chaetognaths, a group of extant, venomous inverte− brate predators of similarly ancient origin, provides additional support for this conclusion. Key words: Vertebrata, Conodonta, venomous animals. Hubert Szaniawski [[email protected]], Instytut Paleobiologii PAN, ul. Twarda 51/55, PL−00−818 Warszawa, Poland. Received 27 March 2009, accepted 6 October 2009, available online 12 October 2009. Introduction later identified as grasping spines of chaetognaths (Szaniaw− ski 2002). Conodonts are well known to geologists because the fossil− Wide geographic distribution shows that conodonts led a ized elements of their feeding apparatuses are exceedingly nektonic mode of life while their strong feeding apparatus sug− useful for stratigraphy. -
Venom Use in Eulipotyphlans: an Evolutionary and Ecological Approach
toxins Review Venom Use in Eulipotyphlans: An Evolutionary and Ecological Approach Krzysztof Kowalski 1 and Leszek Rychlik 2,* 1 Department of Vertebrate Zoology and Ecology, Institute of Biology, Faculty of Biological and Veterinary Sciences, Nicolaus Copernicus University in Toru´n,87-100 Toru´n,Poland; [email protected] 2 Department of Systematic Zoology, Institute of Environmental Biology, Faculty of Biology, Adam Mickiewicz University in Pozna´n,61-614 Pozna´n,Poland * Correspondence: [email protected] Abstract: Venomousness is a complex functional trait that has evolved independently many times in the animal kingdom, although it is rare among mammals. Intriguingly, most venomous mammal species belong to Eulipotyphla (solenodons, shrews). This fact may be linked to their high metabolic rate and a nearly continuous demand of nutritious food, and thus it relates the venom functions to facilitation of their efficient foraging. While mammalian venoms have been investigated using biochemical and molecular assays, studies of their ecological functions have been neglected for a long time. Therefore, we provide here an overview of what is currently known about eulipotyphlan venoms, followed by a discussion of how these venoms might have evolved under ecological pressures related to food acquisition, ecological interactions, and defense and protection. We delineate six mutually nonexclusive functions of venom (prey hunting, food hoarding, food digestion, reducing intra- and interspecific conflicts, avoidance of predation risk, weapons in intraspecific competition) and a number of different subfunctions for eulipotyphlans, among which some are so far only hypothetical while others have some empirical confirmation. The functions resulting from the need Citation: Kowalski, K.; Rychlik, L. -
A New Middle Paleocene Mammalian Fauna from the Fort Union Formation, Great Divide Basin, Wyoming
A new middle Paleocene mammalian fauna from the Fort Union Formation, Great Divide Basin, Wyoming by Emily K. Lannoye B.S., University of Wisconsin-Madison, 2012 A thesis submitted to the Faculty of the Graduate School of the University of Colorado in partial fulfillment of the requirement for the degree of Masters of Science Department of Museum and Field Studies 2015 This thesis entitled: A new middle Paleocene mammalian fauna from the Fort Union Formation, Great Divide Basin, Wyoming Written by Emily K. Lannoye has been approved for the Department of Museum and Field Studies Dr. Jaelyn J. Eberle, Committee Chair Dr. Christy M. McCain, Committee Member Dr. Richard Stucky, Committee Member Date The final copy of this thesis has been examined by the signatories, and we find that both the content and the form meet acceptable presentation standards of scholarly work in the above mentioned discipline. iii Lannoye, Emily K. (M.S., Museum and Field Studies [Paleontology]) A new middle Paleocene mammalian fauna from the Fort Union Formation, Great Divide Basin, Wyoming Thesis directed by Associate Professor & Curator of Fossil Vertebrates Jaelyn J. Eberle Over the last three decades, mammalian faunas that span the Torrejonian-Tiffanian boundary have been reported by others from the Hanna and Bighorn Basins, and are important for assessing mammalian diversity and evolution during middle Paleocene time. Reported here is a Torrejonian – Tiffanian transitional fauna from the Overland Member of the Fort Union Formation in the Great Divide Basin, south-central Wyoming. The fauna, which is primarily comprised of isolated teeth, includes 20 species in five mammalian orders. -
Indice Dei NOMI - VOLUME I
INDICE DEI NOMI - VOLUME I A Adanson M. 32 Alberti (von Alberti) F. Alberto Magno di Bollstädt 37 Aldrovandi U. 14, Allee W.C. 154 Allen J.A. 117 Alvarez L. 207 Amici G.B. 86 Aristotele 8, 9, 25, 26, 28, 37, 38 Arduino G. 14, 179, Argand E. 18, 215, 217 Armstrong H. A. Ashlock P.D. 36, 43 Ashurnasirpal II 86, Avcin M.J. Avery O. 21 Avicenna 9 B Bacone F. (Francis Bacon) 215 Bacone R. (Bacon R. o Doctor Mirabilis) 8 Bachmann A. (Rivinus) 31 Bada J. Bailey W. 20 Banks Harlan P. Barrande J. 33 Barrell Y.J. Bateson W. 20, 21 Bauer G. (Agricola) 9, 73 Bauhin K. 28, 29 Beccari J.B. 87 Becquerel A.H. 23 Belon P. 27, 28 Bengtson P. 34, Berg L.S. 71 Bergmann C.G.L.C. 46, 117 Berry E.W. 20, Boccaccio 9, Bock H. 27, Bosellini F. 135 Brillouin L. 57, Bromley R.G. 104, Brown R. 19 Brunfels O. 27 Brunhes B. 197, 208, Bruno G. 9 Busch, D.A. 176 C F Carey S.W. 216, Fischer G. 86 Cardano G. 9, Fisher O. 216 Castle W. 63 Fisher R.A. 21, 63 Cavalier-Smith T. Fleming W. 19 Cesalpino A. 25, 28, 29, 32 Fortis A. 17 Cesi F. 31, Fracastoro G. 9 Chamberlin R.T. 20, 215 Fuchs L. 27, 28, Chambers R. 17, Clausius R. 57, G Colonna F. 9, 11 Galton F. 19, 58 Colosi G. 62, Garbari F. 43 Conrad V. 2 Garstang W. 51 Cope E.D. -
Download a High Resolution
DENVER MUSEUM OF NATURE & SCIENCE ANNALS NUMBER 1, SEPTEMBER 1, 2009 Land Mammal Faunas of North America Rise and Fall During the Early Eocene Climatic Optimum Michael O. Woodburne, Gregg F. Gunnell, and Richard K. Stucky WWW.DMNS.ORG/MAIN/EN/GENERAL/SCIENCE/PUBLICATIONS The Denver Museum of Nature & Science Annals is an Frank Krell, PhD, Editor-in-Chief open-access, peer-reviewed scientific journal publishing original papers in the fields of anthropology, geology, EDITORIAL BOARD: paleontology, botany, zoology, space and planetary Kenneth Carpenter, PhD (subject editor, Paleontology and sciences, and health sciences. Papers are either authored Geology) by DMNS staff, associates, or volunteers, deal with DMNS Bridget Coughlin, PhD (subject editor, Health Sciences) specimens or holdings, or have a regional focus on the John Demboski, PhD (subject editor, Vertebrate Zoology) Rocky Mountains/Great Plains ecoregions. David Grinspoon, PhD (subject editor, Space Sciences) Frank Krell, PhD (subject editor, Invertebrate Zoology) The journal is available online at www.dmns.org/main/en/ Steve Nash, PhD (subject editor, Anthropology and General/Science/Publications free of charge. Paper copies Archaeology) are exchanged via the DMNS Library exchange program ([email protected]) or are available for purchase EDITORIAL AND PRODUCTION: from our print-on-demand publisher Lulu (www.lulu.com). Betsy R. Armstrong: project manager, production editor DMNS owns the copyright of the works published in the Ann W. Douden: design and production Annals, which are published under the Creative Commons Faith Marcovecchio: proofreader Attribution Non-Commercial license. For commercial use of published material contact Kris Haglund, Alfred M. Bailey Library & Archives ([email protected]). -
[Italic Page Numbers Indicate Major References] Aaron's Locality, Alberta, 59 Acarictis Ryani, 157 Achaenodon Sp., 214 Acheronod
Index [Italic page numbers indicate major references] Aaron's locality, Alberta, 59 Arfia, 118, 180 Biohorizon C, 144 Acarictis ryani, 157 sp., 88 Biomphalaria, 178 Achaenodon sp., 214 Arminto, 170, 179 biostratigraphic zonation, 2 Acheronodon, 59 Armintodelphys Bisonalveus, 61, 62, 87 acritarchs, 16 blacki, 177, 183 browni, 59 Adapidae, 88, 89, 91, 93, 94, 95, 96, dawsoni 177 sp., 60, 67 194 Artiodactyla, 74, 89, 91, 93, 94, 95, Black Butte, 45 Adrar Mgorn locality, 89, 93 96, 108, 129 Blackfalds, Alberta, 60 Africa, 72,74, 89, 91 Asia, 74 , 88, 93 Blindman River, 52, 58, 60, 62 Afrodon chleuhi, 94 Asiocoryphodon, 88 blue clay horizon, 175 Alberta, 2, 11, 16, 32, 52, 53, 56, assemblages Bobcat Draw, 140 57,58,59, 60, 61,62 , 65, 66, Buck Spring, 180,182 Bobcat Member, 16 67, 83 Elderberry Canyon, 207 bones Alberta Syncline, 52 lizard, 180 fossil, 188 Alberta Well, 56 microfossil, 9 fragments, 172 Allognath osuchus, 180 quarry, 180 Bow River, 52, 57, 58 alluvial fans, 170, 189 Tepee Trail, 208 braidplains, 170 alluvial paleosols, 135,149, 172 avulsion, 179 Bridger Formation, 108, 207 Alocodontulum, 108, 109, 114, 130 Brontotheriidae, 96 atopum, 109, 114 Baculites Bubogonia saskia, 55 Alphadon, 39, 40, 43, 44 asperiformis zone, 14, 18 Buck Spring Quarries, 169, 170, 172, sp., 45, 54, 55 clinolobatus zone, 11, 18 178 Alveojunctus, 180 gregoryensis zone, 4 B sequence, 174 Amia, 54, 56, 59, 63, 180 obtusus zone, 11 B-l horizon, 175 uintensis, 182 reduncus zone, 4 B-2 horizon, 169,175,176, 179, amphibians, 182 reesidei zone, 11 180,182 Amphidozotherium, 216 scotti zone, 4 blue clay horizon, 175 Amynodon advenus, 214 sp.