At the Gray Fossil Site Northeastern TN
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Cour. Forsch.-Inst. Senckenberg 256 43–56 4 Figs, 2 Tabs Frankfurt a. M., 15. 11. 2006 Neogene Rhinoceroses of the Linxia Basin (Gansu, China) With 4 fi gs, 2 tabs Tao DENG Abstract Ten genera and thirteen species are recognized among the rhinocerotid remains from the Miocene and Pliocene deposits of the Linxia Basin in Gansu, China. Chilotherium anderssoni is reported for the fi rst time in the Linxia Basin, while Aprotodon sp. is found for the fi rst time in Lower Miocene deposits of the basin. The Late Miocene corresponds to a period of highest diversity with eight species, accompanying very abundant macromammals of the Hipparion fauna. Chilotherium wimani is absolutely dominant in number and present in all sites of MN 10–11 age. Compared with other regions in Eurasia and other ages, elasmotheres are more diversifi ed in the Linxia Basin during the Late Miocene. Coelodonta nihowanensis in the Linxia Basin indicates the known earliest appearance of the woolly rhino. The distribution of the Neogene rhinocerotids in the Linxia Basin can be correlated with paleoclimatic changes. Key words: Neogene, rhinoceros, biostratigraphy, systematic paleontology, Linxia Basin, China Introduction mens of mammalian fossils at Hezheng Paleozoological Museum in Gansu and Institute of Vertebrate Paleontology The Linxia Basin is situated in the northeastern corner of and Paleoanthropology in Beijing. the Tibetan Plateau, in the arid southeastern part ofeschweizerbartxxx Gansusng- Several hundred skulls of the Neogene rhinoceroses Province, China. In this basin, the Cenozoic deposits are are known from the Linxia Basin, but most of them belong very thick and well exposed, and produce abundant mam- to the Late Miocene aceratheriine Chilotherium wimani. -
GFS Fungal Remains from Late Neogene Deposits at the Gray
GFS Mycosphere 9(5): 1014–1024 (2018) www.mycosphere.org ISSN 2077 7019 Article Doi 10.5943/mycosphere/9/5/5 Fungal remains from late Neogene deposits at the Gray Fossil Site, Tennessee, USA Worobiec G1, Worobiec E1 and Liu YC2 1 W. Szafer Institute of Botany, Polish Academy of Sciences, Lubicz 46, PL-31-512 Kraków, Poland 2 Department of Biological Sciences and Office of Research & Sponsored Projects, California State University, Fullerton, CA 92831, U.S.A. Worobiec G, Worobiec E, Liu YC 2018 – Fungal remains from late Neogene deposits at the Gray Fossil Site, Tennessee, USA. Mycosphere 9(5), 1014–1024, Doi 10.5943/mycosphere/9/5/5 Abstract Interesting fungal remains were encountered during palynological investigation of the Neogene deposits at the Gray Fossil Site, Washington County, Tennessee, USA. Both Cephalothecoidomyces neogenicus and Trichothyrites cf. padappakarensis are new for the Neogene of North America, while remains of cephalothecoid fungus Cephalothecoidomyces neogenicus G. Worobiec, Neumann & E. Worobiec, fragments of mantle tissue of mycorrhizal Cenococcum and sporocarp of epiphyllous Trichothyrites cf. padappakarensis (Jain & Gupta) Kalgutkar & Jansonius were reported. Remains of mantle tissue of Cenococcum for the fossil state are reported for the first time. The presence of Cephalothecoidomyces, Trichothyrites, and other fungal remains previously reported from the Gray Fossil Site suggest warm and humid palaeoclimatic conditions in the southeast USA during the late Neogene, which is in accordance with data previously obtained from other palaeontological analyses at the Gray Fossil Site. Key words – Cephalothecoid fungus – Epiphyllous fungus – Miocene/Pliocene – Mycorrhizal fungus – North America – palaeoecology – taxonomy Introduction Fungal organic remains, usually fungal spores and dispersed sporocarps, are frequently found in a routine palynological investigation (Elsik 1996). -
Perissodactyla: Tapirus) Hints at Subtle Variations in Locomotor Ecology
JOURNAL OF MORPHOLOGY 277:1469–1485 (2016) A Three-Dimensional Morphometric Analysis of Upper Forelimb Morphology in the Enigmatic Tapir (Perissodactyla: Tapirus) Hints at Subtle Variations in Locomotor Ecology Jamie A. MacLaren1* and Sandra Nauwelaerts1,2 1Department of Biology, Universiteit Antwerpen, Building D, Campus Drie Eiken, Universiteitsplein, Wilrijk, Antwerp 2610, Belgium 2Centre for Research and Conservation, Koninklijke Maatschappij Voor Dierkunde (KMDA), Koningin Astridplein 26, Antwerp 2018, Belgium ABSTRACT Forelimb morphology is an indicator for order Perissodactyla (odd-toed ungulates). Modern terrestrial locomotor ecology. The limb morphology of the tapirs are widely accepted to belong to a single enigmatic tapir (Perissodactyla: Tapirus) has often been genus (Tapirus), containing four extant species compared to that of basal perissodactyls, despite the lack (Hulbert, 1973; Ruiz-Garcıa et al., 1985) and sev- of quantitative studies comparing forelimb variation in eral regional subspecies (Padilla and Dowler, 1965; modern tapirs. Here, we present a quantitative assess- ment of tapir upper forelimb osteology using three- Wilson and Reeder, 2005): the Baird’s tapir (T. dimensional geometric morphometrics to test whether bairdii), lowland tapir (T. terrestris), mountain the four modern tapir species are monomorphic in their tapir (T. pinchaque), and the Malayan tapir (T. forelimb skeleton. The shape of the upper forelimb bones indicus). Extant tapirs primarily inhabit tropical across four species (T. indicus; T. bairdii; T. terrestris; T. rainforest, with some populations also occupying pinchaque) was investigated. Bones were laser scanned wet grassland and chaparral biomes (Padilla and to capture surface morphology and 3D landmark analysis Dowler, 1965; Padilla et al., 1996). was used to quantify shape. -
Annualreportofdi72fiel.Pdf
mmmmm , THE UNIVERSITY OF ILLINOIS LIBRARY SOT CENTRAL CIRCULATION BOOKSTACKS The person charging this material is re- sponsible for its renewal or its return to the library from which it was borrowed on or before the Latest Date stamped below. The Minimum Fee for each Lost Book is $50.00. Theft/ mutilation, and underlining of books are reasons for disciplinary action and may result in dismissal from the University. TO RENEW CALL TELEPHONE CENTER, 333-8400 UNIVERSITY OF ILLINOIS LIBRARY AT URBANA-CHAMPAIGN MAR 9 1991 When renewing by phone, write new due date below previous due date. L162 Field Museum of Natural History Reports, Vol. VII, Plate XXI ERNEST R. GRAHAM Trustee of the Museum and member of the Building Committee Field Museum of Natural History Founded by Marshall Field, 1893 Publication 248 Report Series Vol. VII, No. 2 ANNUAL REPORT OF THE DIRECTOR TO THE BOARD OF TRUSTEES FOR THE YEAR 1927 nf -"^ THE imm JUL 3 1323 Of 'LUNOIS UNlVWSltY Chicago, U. S. A. January, 1928 OF THE tiW^ViiuSHY Of ILimOlS PRINTED IN THE UNITED STATES OF AMERICA BY FIELD MUSEUM PRESS ^ i V BEQUESTS Bequests to Field Museum of Natural History may be made in securities, money, books or collections. They may, if desired, take the form of a memorial to the memory of a person or cause, to be named by the giver. For those desirous of making bequests to the Museum, the following form is suggested: FORM OF BEQUEST I do hereby give and bequeath to Field Museum of Natural History of the City of Chicago, State of Illinois, Cash contributions made within the taxable year to Field Museum of Natural History to an amount not in excess of 15 per cent of the taxpayer's net income are allowable as deduc- tions in computing net income under Article 251 of Regula- tion 69 relating to the income tax under the Revenue Act of 1926. -
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. -
Investigating Sexual Dimorphism in Ceratopsid Horncores
University of Calgary PRISM: University of Calgary's Digital Repository Graduate Studies The Vault: Electronic Theses and Dissertations 2013-01-25 Investigating Sexual Dimorphism in Ceratopsid Horncores Borkovic, Benjamin Borkovic, B. (2013). Investigating Sexual Dimorphism in Ceratopsid Horncores (Unpublished master's thesis). University of Calgary, Calgary, AB. doi:10.11575/PRISM/26635 http://hdl.handle.net/11023/498 master thesis University of Calgary graduate students retain copyright ownership and moral rights for their thesis. You may use this material in any way that is permitted by the Copyright Act or through licensing that has been assigned to the document. For uses that are not allowable under copyright legislation or licensing, you are required to seek permission. Downloaded from PRISM: https://prism.ucalgary.ca UNIVERSITY OF CALGARY Investigating Sexual Dimorphism in Ceratopsid Horncores by Benjamin Borkovic A THESIS SUBMITTED TO THE FACULTY OF GRADUATE STUDIES IN PARTIAL FULFILMENT OF THE REQUIREMENTS FOR THE DEGREE OF MASTER OF SCIENCE DEPARTMENT OF BIOLOGICAL SCIENCES CALGARY, ALBERTA JANUARY, 2013 © Benjamin Borkovic 2013 Abstract Evidence for sexual dimorphism was investigated in the horncores of two ceratopsid dinosaurs, Triceratops and Centrosaurus apertus. A review of studies of sexual dimorphism in the vertebrate fossil record revealed methods that were selected for use in ceratopsids. Mountain goats, bison, and pronghorn were selected as exemplar taxa for a proof of principle study that tested the selected methods, and informed and guided the investigation of sexual dimorphism in dinosaurs. Skulls of these exemplar taxa were measured in museum collections, and methods of analysing morphological variation were tested for their ability to demonstrate sexual dimorphism in their horns and horncores. -
Paleoecological Comparison Between Late Miocene Localities of China and Greece Based on Hipparion Faunas
Paleoecological comparison between late Miocene localities of China and Greece based on Hipparion faunas Tao DENG Institute of Vertebrate Paleontology and Paleoanthropology, Chinese Academy of Sciences, Beijing 100044 (China) [email protected] Deng T. 2006. — Paleoecological comparison between late Miocene localities of China and Greece based on Hipparion faunas. Geodiversitas 28 (3) : 499-516. ABSTRACT Both China and Greece have abundant fossils of the late Miocene Hipparion fauna. Th e habitat of the Hipparion fauna in Greece was a sclerophyllous ever- green woodland. Th e Chinese late Miocene Hipparion fauna is represented respectively in the Guonigou fauna (MN 9), the Dashengou fauna (MN 10), and the Yangjiashan fauna (MN 11) from Linxia, Gansu, and the Baode fauna (MN 12) from Baode, Shanxi. According to the evidence from lithology, carbon isotopes, paleobotany, taxonomic framework, mammalian diversity and faunal similarity, the paleoenvironment of the Hipparion fauna in China was a subarid open steppe, which is diff erent from that of Greece. Th e red clay bearing the Hipparion fauna in China is windblown in origin, i.e. eolian deposits. Stable carbon isotopes from tooth enamel and paleosols indicate that C3 plants domi- nated the vegetation during the late Miocene in China. Pollens of xerophilous and sub-xerophilous grasses show a signal of steppe or dry grassland. Forest mammals, such as primates and chalicotheres, are absent or scarce, but grass- land mammals, such as horses and rhinoceroses, are abundant in the Chinese Hipparion fauna. Th e species richness of China and Greece exhibits a similar KEY WORDS trend with a clear increase from MN 9 to MN 12, but the two regions have Hipparion fauna, low similarities at the species level. -
New Records of Colubrids from the Late Hemphillian Gray Fossil Site of Northeastern Tennessee Derek J
East Tennessee State University Digital Commons @ East Tennessee State University Electronic Theses and Dissertations Student Works 5-2016 New Records of Colubrids from the late Hemphillian Gray Fossil Site of Northeastern Tennessee Derek J. Jurestovsky East Tennessee State University Follow this and additional works at: https://dc.etsu.edu/etd Part of the Geology Commons, and the Paleontology Commons Recommended Citation Jurestovsky, Derek J., "New Records of Colubrids from the late Hemphillian Gray Fossil Site of Northeastern Tennessee" (2016). Electronic Theses and Dissertations. Paper 3030. https://dc.etsu.edu/etd/3030 This Thesis - Open Access is brought to you for free and open access by the Student Works at Digital Commons @ East Tennessee State University. It has been accepted for inclusion in Electronic Theses and Dissertations by an authorized administrator of Digital Commons @ East Tennessee State University. For more information, please contact [email protected]. New Records of Colubrids from the late Hemphillian Gray Fossil Site of Northeastern Tennessee A thesis presented to the Department of Geosciences East Tennessee State University In partial fulfillment of the requirements for the degree Master of Science in Geosciences by Derek Jurestovsky May 2016 Dr. Jim I. Mead, Chair Dr. Steven C. Wallace Dr. Blaine W. Schubert Keywords: Colubridae, Gray Fossil Site, Hemphillian, Miocene, Natricinae, Serpentes ABSTRACT New Records of Colubrids from the late Hemphillian Gray Fossil Site of Northeastern Tennessee by Derek Jurestovsky The Gray Fossil Site is a rich Hemphillian (North American Land Mammal Age) locality located in northeastern Tennessee which has produced tens-of-thousands of fossils of multiple taxa including hundreds of individual snake skeletal remains. -
Sexual Dimorphism in Perissodactyl Rhinocerotid Chilotherium Wimani from the Late Miocene of the Linxia Basin (Gansu, China)
Sexual dimorphism in perissodactyl rhinocerotid Chilotherium wimani from the late Miocene of the Linxia Basin (Gansu, China) SHAOKUN CHEN, TAO DENG, SUKUAN HOU, QINQIN SHI, and LIBO PANG Chen, S., Deng, T., Hou, S., Shi, Q., and Pang, L. 2010. Sexual dimorphism in perissodactyl rhinocerotid Chilotherium wimani from the late Miocene of the Linxia Basin (Gansu, China). Acta Palaeontologica Polonica 55 (4): 587–597. Sexual dimorphism is reviewed and described in adult skulls of Chilotherium wimani from the Linxia Basin. Via the anal− ysis and comparison, several very significant sexually dimorphic features are recognized. Tusks (i2), symphysis and oc− cipital surface are larger in males. Sexual dimorphism in the mandible is significant. The anterior mandibular morphology is more sexually dimorphic than the posterior part. The most clearly dimorphic character is i2 length, and this is consistent with intrasexual competition where males invest large amounts of energy jousting with each other. The molar length, the height and the area of the occipital surface are correlated with body mass, and body mass sexual dimorphism is compared. Society behavior and paleoecology of C. wimani are different from most extinct or extant rhinos. M/F ratio indicates that the mortality of young males is higher than females. According to the suite of dimorphic features of the skull of C. wimani, the tentative sex discriminant functions are set up in order to identify the gender of the skulls. Key words: Mammalia, Perissodactyla, Chilotherium wimani, sexual dimorphism, statistics, late Miocene, China. Shaokun Chen [[email protected]], Chongqing Three Gorges Institute of Paleoanthropology, China Three Gorges Museum, 236 Ren−Min Road, Chongqing 400015, China and Institute of Vertebrate Paleontology and Paleoanthropology, Chinese Academy of Sciences, 142 Xi−Zhi−Men−Wai Street, P.O. -
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. -
99Th Annual Meeting & Centennial Celebration Of
99TH ANNUAL MEETING & CENTENNIAL CELEBRATION OF THE AMERICAN SOCIETY OF MAMMALOGISTS 28 JUNE-2 JULY 2019 HYATT REGENCY WASHINGTON ON CAPITOL HILL -WASHINGTON, DC- PROGRAM The 2019 American Society of Mammalogists Annual Meeting logo was designed by John Megahan. It features the African bush elephant (Loxodonta africana), which for decades has welcomed visitors to Smithsonian’s National Museum of Natural History. The Smithsonian Institution Building (aka, The Castle) is featured in the background. 99TH ANNUAL MEETING AND CENTENNIAL CELEBRATION OF THE AMERICAN SOCIETY OF MAMMALOGISTS 28 JUNE – 2 JULY 2019 HYATT REGENCY WASHINGTON ON CAPITOL HILL -WASHINGTON, DC- AMERICAN SOCIETY OF MAMMALOGISTS (ASM) The American Society of Mammalogists (ASM) was established in 1919 for the purpose of promoting interest in the study of mammals. AN OVERVIEW In addition to being among the most charismatic of animals, mammals are important in many disciplines from paleontology to ecology and evolution. We, of course, are mammals and thus are in the interesting position of studying ourselves in quest of a greater understanding of the role of mammals in the natural world. The ASM is currently composed of thousands of members, many of whom are professional scientists. Members of the Society have always had a strong interest in the public good, and this is reflected in their involvement in providing information for public policy, resources management, conservation, and education. The Society hosts annual meetings and maintains several publications. The flagship publication is the Journal of Mammalogy, a journal produced six times per year that accepts submissions on all aspects of mammalogy. The ASM also publishes Mammalian Species (accounts of individual species) and Special Publications (books that pertain to specific taxa or topics), and we maintain a mammal images library that contains many exceptional photographs of mammals. -
Title Faunal Change of Late Miocene Africa and Eurasia: Mammalian
Faunal Change of Late Miocene Africa and Eurasia: Title Mammalian Fauna from the Namurungule Formation, Samburu Hills, Northern Kenya Author(s) NAKAYA, Hideo African study monographs. Supplementary issue (1994), 20: 1- Citation 112 Issue Date 1994-03 URL http://dx.doi.org/10.14989/68370 Right Type Departmental Bulletin Paper Textversion publisher Kyoto University African Study Monographs, Supp!. 20: 1-112, March 1994 FAUNAL CHANGE OF LATE MIOCENE AFRICA AND EURASIA: MAMMALIAN FAUNA FROM THE NAMURUNGULE FORMATION, SAMBURU HILLS, NORTHERN KENYA Hideo NAKAYA Department ofEarth Sciences, Kagawa University ABSTRACT The Namurungule Formation yields a large amount of mammals of a formerly unknown and diversified vertebrate assemblage of the late Miocene. The Namurungule Formation has been dated as approximately 7 to 10 Ma. This age agrees with the mammalian assemblage of the Namurungule Formation. Sedimentological evidence of this formation supports that the Namurungule Formation was deposited in lacustrine and/or fluvial environments. Numerous equid and bovid remains were found from the Namurungule Formation. These taxa indicate the open woodland to savanna environments. Assemblage of the Namurungule Fauna indicates a close similarity to those of North Africa, Southwest and Central Europe, and some similarity to Sub Paratethys, Siwaliks and East Asia faunas. The Namurungule Fauna was the richest among late Miocene (Turolian) Sub-Saharan faunas. From an analysis of Neogene East African faunas, it became clear that mammalian faunal assemblage drastically has changed from woodland fauna to openland fauna during Astaracian to Turolian. The Namurungule Fauna is the forerunner of the modem Sub-Saharan (Ethiopian) faunas in savanna and woodland environments. Key Words: Mammal; Neogene; Miocene; Sub-Saharan Africa; Kenya; Paleobiogeography; Paleoecology; Faunal turnover.