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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. -
Paleobiology of Archaeohippus (Mammalia; Equidae), a Three-Toed Horse from the Oligocene-Miocene of North America
PALEOBIOLOGY OF ARCHAEOHIPPUS (MAMMALIA; EQUIDAE), A THREE-TOED HORSE FROM THE OLIGOCENE-MIOCENE OF NORTH AMERICA JAY ALFRED O’SULLIVAN A DISSERTATION PRESENTED TO THE GRADUATE SCHOOL OF THE UNIVERSITY OF FLORIDA IN PARTIAL FULFILLMENT OF THE REQUIREMENTS FOR THE DEGREE OF DOCTOR OF PHILOSOPHY UNIVERSITY OF FLORIDA 2002 Copyright 2002 by Jay Alfred O’Sullivan This study is dedicated to my wife, Kym. She provided all of the love, strength, patience, and encouragement I needed to get this started and to see it through to completion. She also provided me with the incentive to make this investment of time and energy in the pursuit of my dream to become a scientist and teacher. That incentive comes with a variety of names - Sylvan, Joanna, Quinn. This effort is dedicated to them also. Additionally, I would like to recognize the people who planted the first seeds of a dream that has come to fruition - my parents, Joseph and Joan. Support (emotional, and financial!) came to my rescue also from my other parents—Dot O’Sullivan, Jim Jaffe and Leslie Sewell, Bill and Lois Grigsby, and Jerry Sewell. To all of these people, this work is dedicated, with love. ACKNOWLEDGMENTS I thank Dr. Bruce J. MacFadden for suggesting that I take a look at an interesting little fossil horse, for always having fresh ideas when mine were dry, and for keeping me moving ever forward. I thank also Drs. S. David Webb and Riehard C. Hulbert Jr. for completing the Triple Threat of Florida Museum vertebrate paleontology. In each his own way, these three men are an inspiration for their professionalism and their scholarly devotion to Florida paleontology. -
Hipparion” Cf
©Verein zur Förderung der Paläontologie am Institut für Paläontologie, Geozentrum Wien Beitr. Paläont., 30:15-24, Wien 2006 Hooijer’s Hypodigm for “ Hipparion” cf. ethiopicum (Equidae, Hipparioninae) from Olduvai, Tanzania and comparative Material from the East African Plio-Pleistocene by Miranda A rmour -Chelu 1}, Raymond L. Bernor 1} & Hans-Walter Mittmann * 2) A rmour -C helu , M., Bernor , R.L. & M ittmann , H.-W., 2006. Hooijer’s Hypodigm for “ Hipparion” cf. ethiopicum (Equidae, Hipparioninae) from Olduvai, Tanzania and comparative Material from the East African Plio-Pleistocene. — Beitr. Palaont., 30:15-24, Wien. Abstract cranialen Elemente die Hooijer zu diesem Taxon gestellt hat, auf die er sich bezogen hat oder die in irgendeiner We review here the problematic history of the nomen Beziehung dazu stehen, haben wir wiedergefunden. Selbst “Hipparion”cf. ethiopicum and Hooijer’s efforts to bring zusätzliche Fundstücke aus zeitgleichen Horizonten haben some taxonomic sense to the later Pliocene - Pleistocene wir miteinbezogen, in der Absicht, die Gültigkeit von Eu hipparion record. We review his reasoning, and the shifts rygnathohippus cf.“ethiopicum" und seines Verwandten in taxonomic allocation made by him and other equid Eurygnathohippus cornelianus und weiterer Formen, von researchers during the 1970’s. We have relocated many denen Hooijer geglaubt hat, dass sie in einem evolutionären of the postcranial specimens attributed by Hooijer to Zusammenhang mit „ Hipparion“ cf. ethiopicum stehen, “Hipparion” cf. ethiopicum, as well as other specimens zu testen. Wir machen statistische und vergleichende which he referred to, or related to this species. We have Analysen um dieses Hypodigma zu klären. also considered additional specimens from contempo raneous horizons, in order to reevaluate the efficacy of Eurygnathohippus cf “ethiopicum” and its apparent rela 1. -
Late Miocene Tapirus(Mammalia
Bull. Fla. Mus. Nat. Hist. (2005) 45(4): 465-494 465 LATE MIOCENE TAPIRUS (MAMMALIA, PERISSODACTYLA) FROM FLORIDA, WITH DESCRIPTION OF A NEW SPECIES, TAPIRUS WEBBI Richard C. Hulbert Jr.1 Tapirus webbi n. sp. is a relatively large tapir from north-central Florida with a chronologic range of very late Clarendonian (Cl3) to very early Hemphillian (Hh1), or ca. 9.5 to 7.5 Ma. It is about the size of extant Tapirus indicus but with longer limbs. Tapirus webbi differs from Tapirus johnsoni (Cl3 of Nebraska) by its larger size, relatively shorter diastema, thicker nasal, and better developed transverse lophs on premolars. Tapirus webbi is more similar to Tapirus simpsoni from the late early Hemphillian (Hh2, ca. 7 Ma) of Nebraska, but differs in having narrower upper premolars and weaker transverse lophs on P1 and P2. Tapirus webbi differs from North American Plio-Pleistocene species such as Tapirus veroensis and Tapirus haysii in its polygonal (not triangu- lar) interparietal, spicular posterior lacrimal process, relatively narrow P2-M3, and lack of an extensive meatal diverticulum fossa on the dorsal surface of the nasal. In Florida, Hh2 Tapirus is known only from relatively incomplete specimens, but at least two species are represented, both of significantly smaller size than Tapirus webbi or Tapirus simpsoni. One appears to be the dwarf Tapirus polkensis (Olsen), previously known from the very late Hemphillian (Hh4) in Florida and the Hemphillian of Tennessee (referred specimens from Nebraska need to be reexamined). Previous interpretations that the age of T. polkensis is middle Miocene are incorrect; its chronologic range in Florida is Hh2 to Hh4 based on direct association with biochronologic indicator taxa such as Neohipparion eurystyle, Dinohippus mexicanus and Agriotherium schneideri. -
Miocene Paleontology and Stratigraphy of the Suwannee River Basin of North Florida and South Georgia
MIOCENE PALEONTOLOGY AND STRATIGRAPHY OF THE SUWANNEE RIVER BASIN OF NORTH FLORIDA AND SOUTH GEORGIA SOUTHEASTERN GEOLOGICAL SOCIETY Guidebook Number 30 October 7, 1989 MIOCENE PALEONTOLOGY AND STRATIGRAPHY OF THE SUWANNEE RIVER BASIN OF NORTH FLORIDA AND SOUTH GEORGIA Compiled and edit e d by GARY S . MORGAN GUIDEBOOK NUMBER 30 A Guidebook for the Annual Field Trip of the Southeastern Geological Society October 7, 1989 Published by the Southeastern Geological Society P. 0 . Box 1634 Tallahassee, Florida 32303 TABLE OF CONTENTS Map of field trip area ...... ... ................................... 1 Road log . ....................................... ..... ..... ... .... 2 Preface . .................. ....................................... 4 The lithostratigraphy of the sediments exposed along the Suwannee River in the vicinity of White Springs by Thomas M. scott ........................................... 6 Fossil invertebrates from the banks of the Suwannee River at White Springs, Florida by Roger W. Portell ...... ......................... ......... 14 Miocene vertebrate faunas from the Suwannee River Basin of North Florida and South Georgia by Gary s. Morgan .................................. ........ 2 6 Fossil sirenians from the Suwannee River, Florida and Georgia by Daryl P. Damning . .................................... .... 54 1 HAMIL TON CO. MAP OF FIELD TRIP AREA 2 ROAD LOG Total Mileage from Reference Points Mileage Last Point 0.0 0.0 Begin at Holiday Inn, Lake City, intersection of I-75 and US 90. 7.3 7.3 Pass under I-10. 12 . 6 5.3 Turn right (east) on SR 136. 15.8 3 . 2 SR 136 Bridge over Suwannee River. 16.0 0.2 Turn left (west) on us 41. 19 . 5 3 . 5 Turn right (northeast) on CR 137. 23.1 3.6 On right-main office of Occidental Chemical Corporation. -
Bruce J. Macfadden*
MacFadden, B.J., 2006, Early Pliocene (latest Hemphillian) horses from the Yepómera Local 33 Fauna, Chihuahua, Mexico, in Carranza-Castañeda, Óscar, and Lindsay, E.H., eds., Advances in late Tertiary vertebrate paleontology in Mexico and the Great American Biotic Interchange: Universidad Nacional Autónoma de México, Instituto de Geología and Centro de Geociencias, Publicación Especial 4, p. 33–43. EARLY PLIOCENE (LATEST HEMPHILLIAN) HORSES FROM THE YEPÓMERA LOCAL FAUNA, CHIHUAHUA, MEXICO Bruce J. MacFadden* ABSTRACT The latest Hemphillian (Hh4) is characterized by a distinctive equid assemblage, four spe- cies of which are widespread in North America. One of the largest collections of Hh4 equids is from Yepómera, located in Chihuahua, Mexico. Although Yepómera is actually a series of sub-localities, the equids are morphologically similar from each of these and therefore can be considered as a local faunal assemblage of four sympatric species. The distinctive dental patterns, size of the cheek teeth, and (in most cases) metapodial dimensions, make these horses readily distinguishable in the field. Yepómera equids include the monodactyl Astrohippus stockii and Dinohippus mexicanus, and tridactyl Neohipparion eurystyle and Nannippus aztecus. Yepómera is the type locality for the species A. stockii and D. mexica- nus, both described by Lance in 1950. Neohipparion eurystyle and the genus Neohipparion and A. stockii and the genus Astrohippus become extinct at the end of Hh4. Nannippus aztecus is a sister taxon of later Nannippus and D. mexicanus is the sister taxon of Equus, the equid genera that survived in North America during the Plio-Pleistocene. With hypsodonty indices between 2.6 and 3.7, all of the Yepómera horse species have high-crowned teeth, traditionally interpreted as a grazing adaptation. -
Carcharodon Megalodon in a Time Capsule
Inside The Newsletter of the - Highlights Calvert Marine Museum • Bowhead Support Services • Reinecke's Gomphothere Art Fossil Club Sponsors New Whale Exhibit • Gomphotherium calvertensis Volume 19 • Number 2 The Margaret Clark Smith • Upcoming Field Trips Collection on Display July 2004 Whole Number 63 • Miocene Rhino tooth from Calvert Cliffs The Carcharodon megalodon in a Bowhead Support Services, an Alaska Time Capsule Native Corporation (www.Bowhead.com). deriving its name from the Bowhead Whale, has partnered As part of Calvert County's 350th with the Calvert Marine Museum to sponsor a new Anniversary celebrations, a time capsule was just exhibit on the fossil baleen whale found by Jeff buried in the Courthouse to be opened 100 years DiMeglio last year after Hurricane Isabel. Their two from now. I suggested they include a Carcharodon year sponsorship will fund the preparation of the megalodon tooth, with which they agreed. Chris O. skull as well as the development of an exhibit on this Donaldson donated the tooth that was "reburied," to .J.<..:velyspecimen. Our sincerest thanks go out to the Museum in 1998. He found it by flashlight early Jwhead for their interest in furthering our one morning in 1998 as float along Scientists Cliffs. understanding of the history and diversity of Pat Fink catalogued the tooth, giving it CMM- V-10, prehistoric whales! V 000 (highest vertebrate number now is CMM -V• 2400) with the expectation that the tooth will be Former Calvert Marine Museum Director returned to our permanent collections in 100 years and Vertebrate Paleontologist, Dr. Ralph Eshelman (at which time I'll throw a really big party f9r has added numerous valuable and important surviving members of the fossil club). -
Adiciones a La Mastofauna Local Santa Cruz Nuevo, Pleistoceno Tardío De Puebla, México
Santa Cruz Nuevo: Adiciones taxonómicas 29 Paleontología Mexicana Volumen 8, núm. 1, 2019, p. 29 – 39 Adiciones a la mastofauna local Santa Cruz Nuevo, Pleistoceno Tardío de Puebla, México Edwing Jarquin-Abundiza,*, Ismael Ferrusquía-Villafrancaa, José E. Ruiz-Gonzáleze a Instituto de Geología, Universidad Nacional Autónoma de México; Circuito de la Investigación S/N, Ciudad Universitaria, Coyoacán, Ciudad de México, 04510, México. * [email protected] Resumen Con el objetivo de complementar y mejorar el entendimiento de la vertebradofauna pleistocénica mexicana, el presente estudio incluye nuevos reportes sobre la composición taxonómica de la siguiente localidad Rancholabreana: fauna local Santa Cruz Nuevo, Puebla. Los siguientes taxones son reportados por primera vez para el área de estudio: cf. Stockoceros sp., Tetrameryx sp., Glyptotherium aff. G. cylindricum y Cuvieronius aff. C. hyodon. Además, se describe nuevo material fósil perteneciente a Cervidae, Equus cf. E. conversidens y Sylvilagus sp. Con base en esta información, la fauna local Santa Cruz Nuevo está conformada por 14 órdenes, 30 familias, 36 géneros y 19 especies, referibles a las Clases Amphibia, Reptilia, Aves y Mammalia. Palabras clave: Mamíferos, Pleistoceno, Puebla, Rancholabreano. Abstract For the purpose of supplementing and improving the Mexican Pleistocene vertebrate fauna knowledge, the present study includes new records of the taxonomic composition of the following Rancholabrean locality: Santa Cruz Nuevo local fauna, Puebla. The following taxa are reported for the first time in the study area: cf. Stockoceros sp., Tetrameryx sp., Glyptotherium aff. G. cylindricum and Cuvieronius aff. C. hyodon. Furthermore, new fossil material belonging to Cervidae, Equus cf. E. conversidens and Sylvilagus sp. its also described. -
Neohipparion, a Three-Toed Horse by CHESTER STOCK
Neohipparion, A Three-Toed Horse By CHESTER STOCK 0 other lineage of mammal-' illustrates quite so are elevated above the ground and no longer function clearly or so full$ its growth or evolution in geo- a supporting elements of the foot. In the retention of Nlogic time as that of the horse. In the history of the the lateral digits the hipparions were distinctly less pro- Equidae many forms antecedent to the living animal are gressive than the contemporary and monodactyl Pliohip- now known, each marked by readily identifiable charac- pus, and it is from the latter that Equu~is now regarded ters in the teeth, skull and skeleton. From Eohippus, to have sprung. the "dawn horse" of approximately 50 million years The hipparion group persisted through the Pliocene, ago, to the equines of today, a score or more different hut disappeared with the coming of the Pleistocene or kind3 of genera and numerous species of extinct horse* Ice Age, at least in North America. During the late have been described. The changes that have produced Miocene or early Pliocene. the true hipparions are found the large and specialized animal of today from the in North America and Eurasia. By the middle of this diminutive and distinctly less specialized Eocene ancestor epoch. perhaps eight or nine millions of years ago. these of long ago are demonstrated by an amazing array of horses gave ua; to the larger. heavier neohipparions fossil remains. fonnd for the most part in the land-laid which were characteristically North American in distri- formations of the western United States. -
The Evolution of Occlusal Enamel Complexity in Middle
THE EVOLUTION OF OCCLUSAL ENAMEL COMPLEXITY IN MIDDLE MIOCENE TO RECENT EQUIDS (MAMMALIA: PERISSODACTYLA) OF NORTH AMERICA by NICHOLAS ANTHONY FAMOSO A THESIS Presented to the Department of Geological Sciences and the Graduate School of the University of Oregon in partial fulfillment of the requirements for the degree of Master of Science June 2013 THESIS APPROVAL PAGE Student: Nicholas Anthony Famoso Title: The Evolution of Occlusal Enamel Complexity in Middle Miocene to Recent Equids (Mammalia: Perissodactyla) of North America This thesis has been accepted and approved in partial fulfillment of the requirements for the Master of Science degree in the Department of Geological Sciences by: Dr. Edward Davis Chair Dr. Qusheng Jin Member Dr. Stephen Frost Outside Member and Kimberly Andrews Espy Vice President for Research & Innovation/Dean of the Graduate School Original approval signatures are on file with the University of Oregon Graduate School. Degree awarded June 2013 ii © 2013 Nicholas Anthony Famoso iii THESIS ABSTRACT Nicholas Anthony Famoso Master of Science Department of Geological Sciences June 2013 Title: The Evolution of Occlusal Enamel Complexity in Middle Miocene to Recent Equids (Mammalia: Perissodactyla) of North America Four groups of equids, “Anchitheriinae,” Merychippine-grade Equinae, Hipparionini, and Equini, coexisted in the middle Miocene, and only the Equini remains after 16 million years of evolution and extinction. Each group is distinct in its occlusal enamel pattern. These patterns have been compared qualitatively but rarely quantitatively. The processes controlling the evolution of these occlusal patterns have not been thoroughly investigated with respect to phylogeny, tooth position, and climate through geologic time. I investigated two methods of quantitative analysis, Occlusal Enamel Index for shape and fractal dimensionality for complexity. -
Pliocene (Latest Hemphillian and Blancan) Vertebrate Fossils from the Mangas Basin, Southwestern New Mexico
Lucas, S.G., Estep, J.W., Williamson, T.E. and Morgan, G.S. eds., 1997, New Mexico's Fossil Record 1. New Mexico Museum of Natural History and Science Bulletin No. 11. 97 PLIOCENE (LATEST HEMPHILLIAN AND BLANCAN) VERTEBRATE FOSSILS FROM THE MANGAS BASIN, SOUTHWESTERN NEW MEXICO Gary S. Morgan!, Paul L. Sealey!, Spencer G. Lucas!, and Andrew B. Heckerf 1 New Mexico Museum of Natural History and Science, 1801 Mountain Road NW, Albuquerque, NM 87104; 2 Department of Earth and Planetary Sciences, University of New Mexico, Albuquerque, NM 87131 ABSTRACT-Two vertebrate faunas of Pliocene age, the Walnut Canyon and Buckhorn local faunas, are described from sediments of the Gila Group in the Mangas basin in northern Grant County, southwestern New Mexico. Stratigraphic sections and lithologic descriptions are provided for the three unnamed formations in the upper part of the Gila Group that produced these two faunas. The Walnut Canyon local fauna includes one major locality, the Walnut Canyon Horse Quarry, and three smaller sites located 5 km southeast of Gila. The fauna is composed of 12 species of mammals, including one lagomorph, one rodent, two carnivores, two horses, one peccary, three camels, one cervid, and one antilocaprid. The most common members of the fauna are the equids Astrohippus stockii and Dinohippus mexicanus and two genera of camelids (Hemiauchenia and Alforjas). The remaining species in the fauna are represented by very small samples. A. stockii, D. mexicanus, the canid Vulpes stenognathus, the tayassuid d. Catagonus brachydontus, and the camelid Alforjas are typical of late Hemphillian (late Miocene and early Pliocene) faunas. -
Evolution of Horse
UNIT 11 EVOLUTION OF HORSE Structure____________________________________________________ 11.1 Introduction 11.3 Role of Climate in the Evolution of Horse Expected Learning Outcomes 11.4 Activity 11.2 Evolution of Horse 11.5 Summary Systematic Palaeontology 11.6 Terminal Questions Place and Time of Origin 11.7 References Major Evolutionary Transitions 11.8 Further/Suggested Readings Phylogeny of Horse 11.9 Answers 11.1 INTRODUCTION Vertebrates are a diverse group of organisms ranging from lampreys to human beings. The group includes animals with backbone, such as fishes, amphibians, reptiles, birds and mammals. The dinosaurs that have caught public attention by making their appearance in several films and books too are vertebrates. Vertebrates have a long geological history on the planet Earth beginning more than 500 million years (Myr) ago, starting from the Cambrian to the present. They first appeared in the fossil record during the Cambrian period of the Palaeozoic era. Fishes, amphibians and reptiles were the most dominant groups of vertebrates in the Palaeozoic and Mesozoic eras. In the Mesozoic era, dinosaurs- a group of reptiles, and mammals made their appearance. Dinosaurs had a wide geographic distribution, being reported from all continents and were the largest animals to roam the Earth during the Mesozoic era. The mammals began to diversify only after the demise of dinosaurs at the close of the Mesozoic era at around 66 Myr ago. In the Cenozoic era, mammals rapidly occupied every niche and corner of the globe and therefore, the Cenozoic era is also known as the “Age of Mammals”. Introduction to Palaeontology Block……………………………………………………………………………………………….….............….…........ 3 Mammals of the Cenozoic era belong to three groups: placentals (that give birth to young ones), marsupials (in which an offspring after birth continues to develop within the pouch of the mother) and monotremes (egg laying mammals).