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Oligocene - Early Miocene Ruminants from the Valley of Lakes (Central Mongolia) 213-235 ©Naturhistorisches Museum Wien, Download Unter
ZOBODAT - www.zobodat.at Zoologisch-Botanische Datenbank/Zoological-Botanical Database Digitale Literatur/Digital Literature Zeitschrift/Journal: Annalen des Naturhistorischen Museums in Wien Jahr/Year: 2002 Band/Volume: 103A Autor(en)/Author(s): Vislobokova Inesa, Daxner-Höck [Daxner] Gudrun Artikel/Article: Oligocene - Early Miocene Ruminants from the Valley of Lakes (Central Mongolia) 213-235 ©Naturhistorisches Museum Wien, download unter www.biologiezentrum.at Ann. Naturhist. Mus. Wien 103 A 213–235 Wien, März 2002 Oligocene - Early Miocene Ruminants from the Valley of Lakes (Central Mongolia) 1 2 by Inesa VISLOBOKOVA & Gudrun DAXNER-HÖCK (With 9 text-figures, 1 table and 1 plate) Manuscript submitted on July 30th 2001, the revised manuscript on November 20th 2001 Abstract Fossil ruminants from Oligocene and Lower Miocene deposits in Mongolia are referred to six families and 17 genera. New data support the stratigraphic model based on rodent biozonation and 40Ar/39Ar-dating of basalts. The occurrence of the gelocids Paragelocus and Pseudogelocus and diverse bovids are first recor- ded from the Late Oligocene of Asia. Pseudogelocus mongolicus n. sp. is described. Zusammenfassung Aus dem Oligozän und Unter-Miozän der Mongolei wurden Ruminantia beschrieben, die 6 Familien und insgesamt 17 Gattungen angehören. Sie unterstützen das Stratigraphie-Konzept das auf der Biozonierung nach Nagetieren und auf der 40Ar/39Ar-Datierung von Basalten beruht. Es gelang der erste Nachweis der Gelocidae Paragelocus und Pseudogelocus und einer Vielfalt von Boviden des Ober-Oligozäns in Asien. Pseudogelocus mongolicus n. sp. wird neu beschrieben. Introduction The present paper describes ruminant remains collected in the Valley of Lakes in Central Mongolia during the 1995-1997 field seasons. -
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. -
Paleoenvironment of the Late Eocene Chadronian-Age Whitehead Creek Locality (Northwestern Nebraska)
St. Cloud State University theRepository at St. Cloud State Culminating Projects in Cultural Resource Management Department of Anthropology 10-2019 Paleoenvironment of the Late Eocene Chadronian-Age Whitehead Creek Locality (Northwestern Nebraska) Samantha Mills Follow this and additional works at: https://repository.stcloudstate.edu/crm_etds Part of the Archaeological Anthropology Commons Recommended Citation Mills, Samantha, "Paleoenvironment of the Late Eocene Chadronian-Age Whitehead Creek Locality (Northwestern Nebraska)" (2019). Culminating Projects in Cultural Resource Management. 28. https://repository.stcloudstate.edu/crm_etds/28 This Thesis is brought to you for free and open access by the Department of Anthropology at theRepository at St. Cloud State. It has been accepted for inclusion in Culminating Projects in Cultural Resource Management by an authorized administrator of theRepository at St. Cloud State. For more information, please contact [email protected]. Paleoenvironment of the Late Eocene Chadronian-Age Whitehead Creek Locality (Northwestern Nebraska) by Samantha M. Mills A Thesis Submitted to the Graduate Faculty of St. Cloud State University in Partial Fulfillment of the Requirements for the Degree of Master of Science in Functional Morphology October, 2019 Thesis Committee: Matthew Tornow, Chairperson Mark Muñiz Bill Cook Tafline Arbor 2 Abstract Toward the end of the Middle Eocene (40-37mya), the environment started to decline on a global scale. It was becoming more arid, the tropical forests were disappearing from the northern latitudes, and there was an increase in seasonality. Research of the Chadronian (37- 33.7mya) in the Great Plains region of North America has documented the persistence of several mammalian taxa (e.g. primates) that are extinct in other parts of North America. -
First Nimravid Skull from Asia Alexander Averianov1,2, Ekaterina Obraztsova3, Igor Danilov1,2, Pavel Skutschas3 & Jianhua Jin1
www.nature.com/scientificreports OPEN First nimravid skull from Asia Alexander Averianov1,2, Ekaterina Obraztsova3, Igor Danilov1,2, Pavel Skutschas3 & Jianhua Jin1 Maofelis cantonensis gen. and sp. nov. is described based on a complete cranium from the middle- upper Eocene Youganwo Formation of Maoming Basin, Guangdong Province, China. The new taxon Received: 08 September 2015 has characters diagnostic for Nimravidae such as a short cat-like skull, short palate, ventral surface of petrosal dorsal to that of basioccipital, serrations on the distal carina of canine, reduced anterior Accepted: 21 April 2016 premolars, and absence of posterior molars (M2-3). It is plesiomorphic nimravid taxon similar to Published: 10 May 2016 Nimravidae indet. from Quercy (France) in having the glenoid pedicle and mastoid process without ventral projections, a planar basicranium in which the lateral rim is not ventrally buttressed, and P1 present. The upper canine is less flattened than in other Nimravidae.Maofelis cantonensis gen. and sp. nov. exemplifies the earliest stage of development of sabertooth specialization characteristic of Nimravidae. This taxon, together with other middle-late Eocene nimravid records in South Asia, suggests origin and initial diversification of Nimravidae in Asia. We propose that this group dispersed to North America in the late Eocene and to Europe in the early Oligocene. The subsequent Oligocene diversification of Nimravidae took place in North America and Europe, while in Asia this group declined in the Oligocene, likely because of the earlier development of open habitats on that continent. Nimravids are cat-like hypercarnivores that developed saber-tooth morphology early in the Cenozoic and were top predators in the late Eocene – late Oligocene mammal communities of the Northern Hemisphere1–3. -
6-3 Korth 2007A
Paludicola 6(3):111-117 October 2007 © by the Rochester Institute of Vertebrate Paleontology MAMMALS FROM THE BLUE ASH LOCAL FAUNA (LATE OLIGOCENE), SOUTH DAKOTA, MARSUPIALIA AND LAGOMORPHA William W. Korth Rochester Institute of Vertebrate Paleontology, 265 Carling Road, Rochester, New York 14610 ABSTRACT Two marsupials (Herpetotherium fugax and Herpetotherium sp.) and three lagomorphs (Palaeolagus subhypsodus n. sp., Palaeolagus sp. cf. P. philoi, and Palaeolagus sp.) are identified from the Blue Ash local fauna of South Dakota. Of the species identified here, H. fugax is otherwise known from the Orellan to early Arikareean, Herpetotherium sp. is morphologically closest to the middle to late Arikareean H. youngi but is smaller in size, Palaeolagus subhypsodus is intermediate between the Whitneyan P. burkei and the Arikareean P. hypsodus, and the other lagomorphs are closest to Arikareean species morphologically. The age of the fauna is still not definite based on these species but it is suggested that it is slightly earlier than previously described Arikareean faunas. INTRODUCTION increases the number of formally described taxa from the fauna that can potentially help in the determination To date, only rodent species have been formally of the biochronologic age of the fauna. recognized from the Blue Ash local fauna (Martin, Dental nomenclature for marsupials is from 1974; Korth, 2007, in press; Emry and Korth, in press). Crochet (1980); that for lagomorphs is from White Earlier preliminary faunal lists presented by Martin (1987) for P2 and p3, and Dawson (1958) for the (1974) and Simpson (1985) included all of the molariform cheek teeth. Capital letters (e.g., M1) mammalian species present. -
Treebase: an R Package for Discovery, Access and Manipulation of Online Phylogenies
Methods in Ecology and Evolution 2012, 3, 1060–1066 doi: 10.1111/j.2041-210X.2012.00247.x APPLICATION Treebase: an R package for discovery, access and manipulation of online phylogenies Carl Boettiger1* and Duncan Temple Lang2 1Center for Population Biology, University of California, Davis, CA,95616,USA; and 2Department of Statistics, University of California, Davis, CA,95616,USA Summary 1. The TreeBASE portal is an important and rapidly growing repository of phylogenetic data. The R statistical environment has also become a primary tool for applied phylogenetic analyses across a range of questions, from comparative evolution to community ecology to conservation planning. 2. We have developed treebase, an open-source software package (freely available from http://cran.r-project. org/web/packages/treebase) for the R programming environment, providing simplified, programmatic and inter- active access to phylogenetic data in the TreeBASE repository. 3. We illustrate how this package creates a bridge between the TreeBASE repository and the rapidly growing collection of R packages for phylogenetics that can reduce barriers to discovery and integration across phyloge- netic research. 4. We show how the treebase package can be used to facilitate replication of previous studies and testing of methods and hypotheses across a large sample of phylogenies, which may help make such important reproduc- ibility practices more common. Key-words: application programming interface, database, programmatic, R, software, TreeBASE, workflow include, but are not limited to, ancestral state reconstruction Introduction (Paradis 2004; Butler & King 2004), diversification analysis Applications that use phylogenetic information as part of their (Paradis 2004; Rabosky 2006; Harmon et al. -
Constraints on the Timescale of Animal Evolutionary History
Palaeontologia Electronica palaeo-electronica.org Constraints on the timescale of animal evolutionary history Michael J. Benton, Philip C.J. Donoghue, Robert J. Asher, Matt Friedman, Thomas J. Near, and Jakob Vinther ABSTRACT Dating the tree of life is a core endeavor in evolutionary biology. Rates of evolution are fundamental to nearly every evolutionary model and process. Rates need dates. There is much debate on the most appropriate and reasonable ways in which to date the tree of life, and recent work has highlighted some confusions and complexities that can be avoided. Whether phylogenetic trees are dated after they have been estab- lished, or as part of the process of tree finding, practitioners need to know which cali- brations to use. We emphasize the importance of identifying crown (not stem) fossils, levels of confidence in their attribution to the crown, current chronostratigraphic preci- sion, the primacy of the host geological formation and asymmetric confidence intervals. Here we present calibrations for 88 key nodes across the phylogeny of animals, rang- ing from the root of Metazoa to the last common ancestor of Homo sapiens. Close attention to detail is constantly required: for example, the classic bird-mammal date (base of crown Amniota) has often been given as 310-315 Ma; the 2014 international time scale indicates a minimum age of 318 Ma. Michael J. Benton. School of Earth Sciences, University of Bristol, Bristol, BS8 1RJ, U.K. [email protected] Philip C.J. Donoghue. School of Earth Sciences, University of Bristol, Bristol, BS8 1RJ, U.K. [email protected] Robert J. -
NASP: an Accurate, Rapid Method for the Identification of Snps in WGS Datasets That Supports Flexible Input and Output Formats Jason Sahl
Himmelfarb Health Sciences Library, The George Washington University Health Sciences Research Commons Environmental and Occupational Health Faculty Environmental and Occupational Health Publications 8-2016 NASP: an accurate, rapid method for the identification of SNPs in WGS datasets that supports flexible input and output formats Jason Sahl Darrin Lemmer Jason Travis James Schupp John Gillece See next page for additional authors Follow this and additional works at: http://hsrc.himmelfarb.gwu.edu/sphhs_enviro_facpubs Part of the Bioinformatics Commons, Integrative Biology Commons, Research Methods in Life Sciences Commons, and the Systems Biology Commons APA Citation Sahl, J., Lemmer, D., Travis, J., Schupp, J., Gillece, J., Aziz, M., & +several additional authors (2016). NASP: an accurate, rapid method for the identification of SNPs in WGS datasets that supports flexible input and output formats. Microbial Genomics, 2 (8). http://dx.doi.org/10.1099/mgen.0.000074 This Journal Article is brought to you for free and open access by the Environmental and Occupational Health at Health Sciences Research Commons. It has been accepted for inclusion in Environmental and Occupational Health Faculty Publications by an authorized administrator of Health Sciences Research Commons. For more information, please contact [email protected]. Authors Jason Sahl, Darrin Lemmer, Jason Travis, James Schupp, John Gillece, Maliha Aziz, and +several additional authors This journal article is available at Health Sciences Research Commons: http://hsrc.himmelfarb.gwu.edu/sphhs_enviro_facpubs/212 Methods Paper NASP: an accurate, rapid method for the identification of SNPs in WGS datasets that supports flexible input and output formats Jason W. Sahl,1,2† Darrin Lemmer,1† Jason Travis,1 James M. -
Supplementary Information
Supplementary Information Table S1. List of samples that yielded DNA in this study (EE2-EE26), followed by successfully amplified samples of cave lion from the study by Barnett et al. 2009. ALA=Alaska, EUR=Europe, SIB=Siberia, NC=not calibrated as out of range. The asterisk (*) denotes the approximate age as reported in Barnett et al. 2009. Sample CR haplotype/ Uncalibrated Calendar years Site and geographic region ID Genbank nr. 14C date before present EE2 D/ DQ899903 Schusterlucke cave (EUR) 15400 ± 130 18521 ± 1844 EE4 - Tyung, C Siberia (SIB) 46700±1300 48181 ± 6747 EE3 Y3 Tain cave, Urals (EUR) >49600 NC EE6 Y1 Elovka, Baikal (SIB) 18350 ± 75 21634 ± 1504 EE7 Y1 Volchika, C Siberia (SIB) 20085 ± 80 23266 ± 576 EE13 J/ DQ899909 New Siberian Islands (SIB) 47700 ± 800 48970 ± 6009 EE14 Y4 Yakutia, NE Siberia (SIB) >55400 NC EE15 B/ DQ899901 Yakutia, NE Siberia (SIB) 27720 ± 140 30880 ± 1543 EE16 Y2 Irkutsk, Baikal (SIB) 17910 ± 75 21024 ± 1041 EE17 B/ DQ899901 Khroma river, Yakutia (SIB) 19755 ± 80 20006 ± 404 EE19 - New Siberian Islands (SIB) 52000±1500 54373 ± 6396 EE20 J/ DQ899909 Yakutia, NE Siberia (SIB) >62400 NC EE21 G/ DQ899906 Nizhnyaya, C Siberia (SIB) 50500 ± 290 52785 ± 10541 EE26 Y5 (partial) Kyttyk Peninsula (SIB) 36550 ± 290 41025 ± 970 IB133 A/ DQ899900 Gold Run Creek, Yukon (ALA) 12640 ± 75 15016 ± 1463 RB112 A Caribou Creek, Yukon (ALA) n/a - RB74 A Fairbanks Creek, Alaska (ALA) n/a - RB75 A Ester Creek, Alaska (ALA) 12090 ± 80 13822 ± 341 IB134 B/ DQ899901 Gold Hill, Alaska (ALA) 18240 ± 90 21533 ± 1335 IB136 B Hunker -
8. Primate Evolution
8. Primate Evolution Jonathan M. G. Perry, Ph.D., The Johns Hopkins University School of Medicine Stephanie L. Canington, B.A., The Johns Hopkins University School of Medicine Learning Objectives • Understand the major trends in primate evolution from the origin of primates to the origin of our own species • Learn about primate adaptations and how they characterize major primate groups • Discuss the kinds of evidence that anthropologists use to find out how extinct primates are related to each other and to living primates • Recognize how the changing geography and climate of Earth have influenced where and when primates have thrived or gone extinct The first fifty million years of primate evolution was a series of adaptive radiations leading to the diversification of the earliest lemurs, monkeys, and apes. The primate story begins in the canopy and understory of conifer-dominated forests, with our small, furtive ancestors subsisting at night, beneath the notice of day-active dinosaurs. From the archaic plesiadapiforms (archaic primates) to the earliest groups of true primates (euprimates), the origin of our own order is characterized by the struggle for new food sources and microhabitats in the arboreal setting. Climate change forced major extinctions as the northern continents became increasingly dry, cold, and seasonal and as tropical rainforests gave way to deciduous forests, woodlands, and eventually grasslands. Lemurs, lorises, and tarsiers—once diverse groups containing many species—became rare, except for lemurs in Madagascar where there were no anthropoid competitors and perhaps few predators. Meanwhile, anthropoids (monkeys and apes) emerged in the Old World, then dispersed across parts of the northern hemisphere, Africa, and ultimately South America. -
Fossil Primates
AccessScience from McGraw-Hill Education Page 1 of 16 www.accessscience.com Fossil primates Contributed by: Eric Delson Publication year: 2014 Extinct members of the order of mammals to which humans belong. All current classifications divide the living primates into two major groups (suborders): the Strepsirhini or “lower” primates (lemurs, lorises, and bushbabies) and the Haplorhini or “higher” primates [tarsiers and anthropoids (New and Old World monkeys, greater and lesser apes, and humans)]. Some fossil groups (omomyiforms and adapiforms) can be placed with or near these two extant groupings; however, there is contention whether the Plesiadapiformes represent the earliest relatives of primates and are best placed within the order (as here) or outside it. See also: FOSSIL; MAMMALIA; PHYLOGENY; PHYSICAL ANTHROPOLOGY; PRIMATES. Vast evidence suggests that the order Primates is a monophyletic group, that is, the primates have a common genetic origin. Although several peculiarities of the primate bauplan (body plan) appear to be inherited from an inferred common ancestor, it seems that the order as a whole is characterized by showing a variety of parallel adaptations in different groups to a predominantly arboreal lifestyle, including anatomical and behavioral complexes related to improved grasping and manipulative capacities, a variety of locomotor styles, and enlargement of the higher centers of the brain. Among the extant primates, the lower primates more closely resemble forms that evolved relatively early in the history of the order, whereas the higher primates represent a group that evolved more recently (Fig. 1). A classification of the primates, as accepted here, appears above. Early primates The earliest primates are placed in their own semiorder, Plesiadapiformes (as contrasted with the semiorder Euprimates for all living forms), because they have no direct evolutionary links with, and bear few adaptive resemblances to, any group of living primates. -
New Genus of Amphicyonid Carnivoran (Mammalia, Carnivora, Amphicyonidae) from the Phosphorites of Quercy (France)
FOSSIL IMPRINT • vol. 76 • 2020 • no. 1 • pp. 201–208 (formerly ACTA MUSEI NATIONALIS PRAGAE, Series B – Historia Naturalis) NEW GENUS OF AMPHICYONID CARNIVORAN (MAMMALIA, CARNIVORA, AMPHICYONIDAE) FROM THE PHOSPHORITES OF QUERCY (FRANCE) LOUIS DE BONIS Palevoprim: Laboratoire de Paléontologie, Evolution, Paléoécosystèmes, Paléoprimatologie, Bât B35 TSA51106 – 6 rue Michel Brunet, 86073 Poitiers cedex 9, France; e-mail: [email protected]. Bonis, L. de (2020): New genus of amphicyonid carnivoran (Mammalia, Carnivora, Amphicyonidae) from the phosphorites of Quercy (France). – Fossil Imprint, 76(1): 201–208, Praha. ISSN 2533-4050 (print), ISSN 2533-4069 (on-line). Abstract: An isolated mandible of Carnivora (Mammalia) from the phosphorites of Quercy (France) is described as a new genus. It is compared with the amphicyonid genus Cynodictis, some primitive North American amphicyonids, and with European and North American Eocene carnivoraforms. I conclude that it is a primitive amphicyonid which may be dated to the middle or late Eocene. Key words: Eocene, Europe, North America, Carnivoraformes Received: March 11, 2019 | Accepted: March 21, 2020 | Issued: November 9, 2020 Introduction The order Carnivora is present among the fauna recorded in the phosphorites of Quercy (Filhol 1872a, b, 1873, 1874, There is a large Jurassic limestone plateau in the French 1876, 1877, 1882, Schlosser 1887, 1888, 1899, Teilhard departments of Lot, Aveyron, and Tarn and Garonne. It de Chardin 1915, Piveteau 1931, 1943, 1962, Ginsburg emerged during the Cenozoic. During the middle of the 1966, 1979, Bonis 1966, 1971, 1974, 1978, 2011, 2019, Cenozoic it included a karstic system with a net of fissures, Springhorn 1977) and there have been many publications caves, and galleries that were filled by red clays containing on their species.