Toward the Establishment of a Continental Asian Biostratigraphic and Geochronologic Framework
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Updated Aragonian Biostratigraphy: Small Mammal Distribution and Its Implications for the Miocene European Chronology
Geologica Acta, Vol.10, Nº 2, June 2012, 159-179 DOI: 10.1344/105.000001710 Available online at www.geologica-acta.com Updated Aragonian biostratigraphy: Small Mammal distribution and its implications for the Miocene European Chronology 1 2 3 4 3 1 A.J. VAN DER MEULEN I. GARCÍA-PAREDES M.A. ÁLVAREZ-SIERRA L.W. VAN DEN HOEK OSTENDE K. HORDIJK 2 2 A. OLIVER P. PELÁEZ-CAMPOMANES * 1 Faculty of Earth Sciences, Utrecht University Budapestlaan 4, 3584 CD Utrecht, The Netherlands. Van der Meulen E-mail: [email protected] Hordijk E-mail: [email protected] 2 Departamento de Paleobiología, Museo Nacional de Ciencias Naturales MNCN-CSIC C/ José Gutiérrez Abascal 2, 28006 Madrid, Spain. García-Paredes E-mail: [email protected] Oliver E-mail: [email protected] Peláez-Campomanes E-mail: [email protected] 3 Netherlands Centre for Biodiversity-Naturalis Darwinweg 2, 2333 CR Leiden, The Netherlands. Van den Hoek Ostende E-mail: [email protected] 4 Departamento de Paleontología, Facultad de Ciencias Geológicas, Universidad Complutense de Madrid. IGEO-CSIC C/ José Antonio Novais 2, 28040 Madrid, Spain. Álvarez-Sierra E-mail: [email protected] * Corresponding author ABSTRACT This paper contains formal definitions of the Early to Middle Aragonian (Late Early–Middle Miocene) small- mammal biozones from the Aragonian type area in North Central Spain. The stratigraphical schemes of two of the best studied areas for the Lower and Middle Miocene, the Aragonian type area in Spain and the Upper Freshwater Molasse from the North Alpine Foreland Basin in Switzerland, have been compared. -
Mammalia: Bovidae) from the Late Miocene Qingyang Area, Gansu, China
Palaeontologia Electronica palaeo-electronica.org “Gazella” (Mammalia: Bovidae) from the late Miocene Qingyang area, Gansu, China Yikun Li, Qinqin Shi, Shaokun Chen, and Tao Deng ABSTRACT The rich collection from the late Miocene sediments from the Qingyang area, Gansu, China was discovered by E. Licent in the 1920s, and previous studies focused on the equids and hyaenids whereas little attention was given to the accompanying bovid material. The collection of Bovidae dug up from the Qingyang area and pre- served at Musée Hoangho Paiho, Tianjin, China, is dominated by “Gazella”. We describe and identify two species: “Gazella” paotehensis and “G.” dorcadoides. The nomenclatural issues surrounding those two species of gazelles are reviewed in this paper, and although the questionable mandible illustrated by Teilhard de Chardin and Young in 1931 may be excluded from “G.” paotehensis metrically and morphologically, the species is still considered valid. The subcomplete cranium M 3956, kept at Uppsala Universitet Evolutionsmuseet and studied by B. Bohlin, is selected here as the neotype of “G.” paotehensis, and emended diagnoses are given. Based on previous studies and insights from new material from the Qingyang area, we provide a table summarizing diagnostic morphological characters of “G.” paotehensis and “G.” dorcadoides. Yikun Li. Key Laboratory of Vertebrate Evolution and Human Origins of Chinese Academy of Sciences, Institute of Vertebrate Paleontology and Paleoanthropology, Chinese Academy of Sciences, Beijing 100044, China; University of Chinese Academy of Sciences, Beijing 100049, China; Museum für Naturkunde, Leibniz Institute for Evolution and Biodiversity Science, Berlin 10115, Germany. [email protected] Qinqin Shi. Key Laboratory of Vertebrate Evolution and Human Origins of Chinese Academy of Sciences, Institute of Vertebrate Paleontology and Paleoanthropology, Chinese Academy of Sciences, Beijing 100044, China. -
Redalyc.An Updated Biostratigraphy for the Late Aragonian and Vallesian
Geologica Acta: an international earth science journal ISSN: 1695-6133 [email protected] Universitat de Barcelona España CASANOVAS-VILAR, I.; GARCÉS, M.; VAN DAM, J.; GARCÍA-PAREDES, I.; ROBLES, J.M.; ALBA, D.M. An updated biostratigraphy for the late Aragonian and Vallesian of the Vallès-Penedès Basin (Catalonia) Geologica Acta: an international earth science journal, vol. 14, núm. 3, septiembre, 2016, pp. 195-217 Universitat de Barcelona Barcelona, España Available in: http://www.redalyc.org/articulo.oa?id=50547614001 How to cite Complete issue Scientific Information System More information about this article Network of Scientific Journals from Latin America, the Caribbean, Spain and Portugal Journal's homepage in redalyc.org Non-profit academic project, developed under the open access initiative Geologica Acta, Vol.14, Nº 3, September 2016, 195-217 DOI: 10.1344/GeologicaActa2016.14.3.1 An updated biostratigraphy for the late Aragonian and Vallesian of the Vallès-Penedès Basin (Catalonia) I. CASANOVAS-VILAR1 M. GARCÉS2,3 J. VAN DAM4,1 I. GARCÍA-PAREDES5 J.M. ROBLES1 D.M. ALBA1 1Institut Català de Paleontologia Miquel Crusafont, Universitat Autònoma de Barcelona Edifici ICTA-ICP, Carrer de les Columnes s/n, Campus de la UAB, 08193 Cerdanyola del Vallès, Barcelona, Spain. Casanovas- Vilar E-mail: [email protected] Van Dam E-mail: [email protected] Robles E-mail: [email protected] Alba E-mail: [email protected] 2Departament de Dinàmica de la Terra i l’oceà, Facultat de Geologia, Universitat de Barcelona Martí i Franqués s/n, 08028 Barcelona, Spain. Garcés E-mail: [email protected] 3Institut Geomodels, Grup de Recerca Consolidat de Geodinàmica i Anàlisis de Conques, Universitat de Barcelona Martí i Franqués s/n, 08028 Barcelona, Spain 4Department of Earth Sciences, Utrecht University Budapestlaan 4, 3584 CD Utrecht, the Netherlands. -
The 1St Asian Palaeontological Congress - with Celebrations on the 90Th Anniversary of the Palaeontological Society of China
The 1st Asian Palaeontological Congress - with celebrations on the 90th Anniversary of the Palaeontological Society of China November 17-19, 2019, Beijing, China GENERAL INFORMATION The Organizing Committees of the First Asia Palaeontological Congress (APC2019), representing the Palaeontolgical Society of China and other scientific institutions, cordially invite you to participate in the: 1ST ASIAN PALAEONTOLOGICAL CONGRESS (APC2019) IN BEIJING, PEOPLE’S REPUBLIC OF CHINA NOVEMBER 17- 20, 2019 The 1st Asian Palaeontological Congress (APC 2019) will be held with celebrations on the 90th Anniversary of the Palaeontological Society of China. This congress is co-sponsored by the Palaeontological Society of China (PSC), the Palaeontological Society of Japan (PSJ) and Paleontological Society of Korea (PSK). The topic of APC 2019 will be “Palaeontology of New Eras in Asia: collaboration and innovation”. During the congress, the Asian Palaeontological Association (APA) will be officially established. This congress will exhibit the recent progresses achieved by a variety of topics of the palaeontological studies in Asian regions, and will strengthen the collaborations and communications for palaeontological societies among Asian countries in the fields of scientific research, education, fossil protection and museum displays. CONGRESS VENUE The conference venue is located in the China Hall of Science and Technology (CHST), located in No.3 Fuxin Road, Haidian District of central Beijing. APC2019 congress venue in China Hall of Science and Technology -
A Giant Ostrich from the Lower Pleistocene Nihewan Formation of North China, with a Review of the Fossil Ostriches of China
diversity Review A Giant Ostrich from the Lower Pleistocene Nihewan Formation of North China, with a Review of the Fossil Ostriches of China Eric Buffetaut 1,2,* and Delphine Angst 3 1 Centre National de la Recherche Scientifique—CNRS (UMR 8538), Laboratoire de Géologie de l’Ecole Normale Supérieure, PSL Research University, 24 rue Lhomond, CEDEX 05, 75231 Paris, France 2 Palaeontological Research and Education Centre, Maha Sarakham University, Maha Sarakham 44150, Thailand 3 School of Earth Sciences, University of Bristol, Life Sciences Building, 24 Tyndall Avenue, Bristol BS8 1TQ, UK; [email protected] * Correspondence: [email protected] Abstract: A large incomplete ostrich femur from the Lower Pleistocene of North China, kept at the Muséum National d’Histoire Naturelle (Paris), is described. It was found by Father Emile Licent in 1925 in the Nihewan Formation (dated at about 1.8 Ma) of Hebei Province. On the basis of the minimum circumference of the shaft, a mass of 300 kg, twice that of a modern ostrich, was obtained. The bone is remarkably robust, more so than the femur of the more recent, Late Pleistocene, Struthio anderssoni from China, and resembles in that regard Pachystruthio Kretzoi, 1954, a genus known from the Lower Pleistocene of Hungary, Georgia and the Crimea, to which the Nihewan specimen is referred, as Pachystruthio indet. This find testifies to the wide geographical distribution Citation: Buffetaut, E.; Angst, D. A of very massive ostriches in the Early Pleistocene of Eurasia. The giant ostrich from Nihewan was Giant Ostrich from the Lower contemporaneous with the early hominins who inhabited that region in the Early Pleistocene. -
1. the Fossils of the Przewalski's Horse and the Climatic Variations Of
9th12 ICAZ Conference, Durham 2002 Deng Tao Equids in Time and Space (ed. Marjan Mashkour) pp. 12–19 1. The Fossils of the Przewalski’s horse and the climatic variations of the Late Pleistocene in China Deng Tao Fossils of the Przewalski’s horse were discovered widespread in a lot of the Late Pleistocene faunas and the Paleolithic sites in northern China. The ecological environment of the extant Przewalski’s horse proves that it exists in the winter monsoon region, and adapts to dry and cold climate. During the stage of strong summer monsoon in the Late Pleistocene, the Przewalski’s horse was absent in northern China. During strong winter monsoon, on the other hand, it appeared frequently among the mammalian faunas in this region. An analysis on the enamel carbon isotope of the Przewalski’s horse indicates that C3 grass was dominant in the habitats of the Przewalski’s horse in northern China during the Late Pleistocene. The geological distribution of the Przewalski’s horse was related to the temporal and spatial variation of the East-Asian monsoon. The distribution of the Przewalski’s horse in northern China can sensitively reflect the variation of the East-Asian monsoon. As a result, the fossils of the Przewalski’s horse can be regarded as an indicator of the climatic variation in northern China since the Late Pleistocene. Introduction a long time without water; they frequently use fore feet to The Przewalski’s horse (Equus przewalskii) distributed dig small pits in low-lying place where salty water widely in the Late Pleistocene of China, and its fossils accumulates for drinking; their main diet is composed of are discovered from many Late Pleistocene mammalian desert vegetation such as Haloxylon ammodendron, faunas and Paleolithic sites, with a vast range from Artemisia incana, Salicornia herbacea, Equisetum, western Xinjiang (Jin 1991) as far as the Taiwan Channel Scorzonera, Phragmites, and Salsola; they satisfy their (Gao 1982). -
Linxia Basin: an Ancient Paradise for Late Cenozoic Rhinoceroses in North China
Vol.24 No.2 2010 Paleomammalogy Linxia Basin: An Ancient Paradise for Late Cenozoic Rhinoceroses in North China DENG Tao * Institute of Vertebrate Paleontology and Paleoanthropology, CAS, Beijing 100044 he Linxia Basin is located and sometimes partially articulated several hundred skulls of the late on the triple-junction of the bones of large mammals, which often Cenozoic rhinoceroses are known from Tnortheastern Tibetan Plateau, occur in dense concentrations. Many the Linxia Basin. In addition, more western Qinling Mountains and the new species of the Late Oligocene abundant limb bones and isolated teeth Loess Plateau. The basin is filled with Dzungariotherium fauna, the Middle of rhinoceroses are found in this basin, 700−2000 m of late Cenozoic deposits, Miocene Platybelodon fauna, the Late especially from the Late Miocene mainly red in color and dominated by Miocene Hipparion fauna, and the Early red clay deposits. Rhinoceroses were lacustrine siltstones and mudstones, and Pleistocene Equus fauna have been over 70% in diversity during the Late the Linxia sequence represents the most described from the Linxia Basin since Oligocene, and they were dominant in complete and successive late Cenozoic 2000, including rodents, lagomorphs, population during the Late Miocene. section in China. The localities in the primates, carnivores, proboscideans, In the Middle Miocene and Early Linxia Basin are notable for abundant, perissodactyls and artiodactyls. Pleistocene faunas, rhinoceroses were relatively complete, well-preserved, Among these mammalian fossils, important members. Late Oligocene The Late Oligocene fauna of findings in Europe (Qiu and Wang, is estimated at 24 tons, and another the Linxia Basin comes from the 2007). -
A Classification of the Glirtdae (Rodentia) on the Basis of Dental Morphology
Hystrix, (11s.) 6 (1 -2) (1 994): 3-50 (1995) Proc. I1 Conf. on Dormice A CLASSIFICATION OF THE GLIRTDAE (RODENTIA) ON THE BASIS OF DENTAL MORPHOLOGY REMMERT DAAMS (*) & HANSDE BRUIJN (**) (*) Depto. de Paleontologia, Facultad de Ciencias Geoldgicas, Universidad Complutense, Ciudad Universituria, 28040 Madrid, Spain. (**) Dept. ofStratigraphy/Pulcontolo~,Institute ofEarth Sciences, State University of Utrecht, Budapestlaan 4, 3508 TA Utrecht, The Netherlands. ABSTRACT - The supra-familiar relationships of the Gliridae are discussed. The criterion used for subdividing the Gliridae is the morphology of the cheek teeth because this is the only character known for all taxa. This limitation leads to the undesirable "synonymy" of Glamys and Gliravirs, two genera whose type species have a very different skull morphology, and to the incorporation into the Dryomyinae of Gruphiurzis and Leithiu, despite the fact that Dryonzys has a myomorph, Graphizrrus a hystricomorph and Leithiu a sciurornorph skull. The hundred and seventy-seven species and thirty eight genera of dormice are grouped into five subfamilies. One of these, the Bransatoglirinae, is new. The subfamily Graphiurinae is supressed and Graphiumrs is assigned to the Dryomyinae. The genera of the Gliridae and the species allocated to them are listed in the appendix in alphabetical order. The original diagnoses of the genera are given in English and the type locality, type level and synonymy of each species is given. Key words: Gliridae, Systematics, Taxonomy, Dental morphology, Palaentology. RIASSUNTO - (Jna classijkuzione di Gliridae (Rodentiu) szrllu base della morfologiu dentale - Vengono discusse le relazioni soprafamiliari dei Gliridi. I1 criterio utilizzato per la suddivisione dei Gliridi 6 la morfologia dei denti molari poiche e I'unico carattere noto per tutti i taxa. -
Wessels, W (2009). Miocene Rodent Evolution and Migration. Muroidea
Miocene rodent evolution and migration Muroidea from Pakistan, Turkey and Northern Africa W. Wessels GEOLOGICA ULTRAIECTINA Mededelingen van de Faculteit Geowetenschappen departement Aardwetenschappen Universiteit Utrecht No. 307 ISBN 978-90-5744-170-7 Graphic design and figures: GeoMedia, Faculty of Geosciences, Utrecht University (7497) Miocene rodent evolution and migration Muroidea from Pakistan, Turkey and Northern Africa Evolutie en migratie van Miocene knaagdieren Muroidea afkomstig uit Pakistan, Turkije en Noord Afrika (met een samenvatting in het Nederlands) PROEFSCHRIFT ter verkrijging van de graad van doctor aan de Universiteit Utrecht op gezag van de rector magnificus, prof.dr. J.C. Stoof, ingevolge het besluit van het college voor promoties in het openbaar te verdedigen op maandag 8 juni 2009 des middags te 4.15 uur door Wilma Wessels geboren op 9 december 1955 te Vriezenveen Promotor: Prof.dr. J.W.F. Reumer Contents Part 1 Introduction 1 Introduction 13 2 Correlation of some Miocene faunas from Northern Africa, Turkey and Pakistan 17 by means of Myocricetodontidae Published in Proceedings of the Koninklijke Nederlandse Akademie van Wetenschappen B 90(1): 65-82 (1987), Wessels W., Ünay. E. & Tobien H. 2.1 Abstract 17 2.2 Introduction 17 2.3 The Pakistani Myocricetodontinae 19 2.3.2 Taxonomy 19 2.3.3 Discussion of the Pakistani Myocricetodontinae 24 2.4 The Turkish Myocricetodontinae 24 2.4.2 Taxonomy 25 2.4.3 Discussion of the Turkish Myocricetodontinae 31 2.5 Conclusions 31 2.6 Acknowledgements 31 Part 2 Rodents from Europe, Turkey and Northern Africa 3 Gerbillidae from the Miocene and Pliocene of Europe 35 Published in Mitteilungen der Bayerischen Staatssammlung für Paläontologie und Historische Geologie 38: 187-207 (1998), Wessels W. -
First Record of Fossil Anguines (Squamata; Anguidae) from the Oligocene and Miocene of Turkey
Swiss J Geosci (2017) 110:741–751 DOI 10.1007/s00015-017-0272-5 First record of fossil anguines (Squamata; Anguidae) from the Oligocene and Miocene of Turkey 1 2,3 3,4 5 Andrej Cˇ ernˇansky´ • Davit Vasilyan • Georgios L. Georgalis • Peter Joniak • 6 1 Serdar Mayda • Jozef Klembara Received: 6 December 2016 / Accepted: 16 March 2017 / Published online: 4 April 2017 Ó Swiss Geological Society 2017 Abstract Fossil anguine lizard specimens from several to Asia and significantly enhance our understanding of Turkish localities are described in this paper. The material their biogeography. comes from ten different localities, spanning a large geo- graphic area consisting of both parts of the European Keywords Anguimorpha Á Cenozoic Á Dispersion Á Asia Turkey and Anatolia, and ranging in age from the Oligo- cene to the Late Miocene. In certain cases, the generic determination was possible and, accordingly, members of 1 Introduction Ophisaurus and Anguis were identified and described in detail. The specimens of Anguis, found in different, Middle The clade Anguinae (Anguimorpha, Anguidae) comprises and Late Miocene localities from Anatolia, represent two legless lizards and includes three extant taxa: Pseudopus of only a few fossil occurrences of this taxon. Moreover, (Southeast Europe to Central Asia), Anguis (Europe, Wes- the material reported herein represents the oldest occur- tern Asia) and Ophisaurus (North America, Northern Africa rences of anguine lizards, not only from Turkey, but from and Southeast Asia). On the basis of the fossil finds as well as southeastern Europe and the Eastern Mediterranean basin the mitochondrial DNA of the extant species it is believed as a whole. -
Miocene Carnivorans from the Vallès-Penedès Basin (NE Iberian Peninsula)
Departament de Biologia Animal, de Biologia Vegetal i d’Ecologia Unitat d’Antropologia Biològica Miocene carnivorans from the Vallès-Penedès Basin (NE Iberian Peninsula) Josep Maria Robles Giménez Tesi Doctoral 2014 A mi padre y familia. INDEX Index .......................................................................................................................... 7 Preface and Acknowledgments [in Spanish] ....................................................... 13 I.–Introduction and Methodology ........................................................................ 19 Chapter 1. General introduction and aims of this dissertation .......................... 21 1.1. Aims and structure of this work .............................................................. 21 Motivation of this dissertation ................................................................ 21 Type of dissertation and general overview ............................................. 22 1.2. An introduction to the Carnivora ............................................................ 24 What is a carnivoran? ............................................................................. 24 Biology .................................................................................................... 25 Systematics and phylogeny ...................................................................... 28 Evolutionary history ................................................................................ 42 1.3. Carnivoran anatomy ............................................................................... -
Body Size Development of Large Mammals During the European Neogene: Trends and Some Environmental Considerations
Body size development of large mammals during the European Neogene: Trends and some environmental considerations. By Jussi Eronen Master’s Thesis University of Helsinki Department of Geology Division of Geology & Paleontology 2003 1 Contents 1. Introduction 4 2. Biological basis 6 2.1. Metabolism 6 2.2. Respiration 7 2.3. Ingestion 7 2.4. Locomotion 8 2.5. Water balance and temperature 8 2.6. Time 9 2.7 Growth & reproduction 9 2.8. Population density 9 2.9. Home range size 10 3. Paleobiology & paleontological context 11 3.1. Stratigraphy 11 3.2. Mammals 14 4. Methods 18 5. Results 38 6. Paleogeography 46 6.1. The forming of the Gomphotherium landbridge 46 6.2. Development of central Paratethys and Lower Rhine Embayment during the Miocene 48 6.3. The Messinian salinity crisis 50 2 7. Discussion 52 8. Conclusions 57 9. Acknowledgements 59 10. References 60 Appendix I: The hypsodonty maps 70 Appendix II: Locality list 73 3 1. Introduction Body size (whether it means lenght, volume or mass) is one of the easiest characteristics to estimate in a living mammal. It is also a very valuable characteristic, because it is connected to a multitude of physiological and ecological characteristics. This makes body size a unique characteristic. On the other hand, this also complicates things. Because body size is connected to so many other parameters, it is also affected by many variables. Therefore one can rarely conclude something solid about body size alone. Usually body size gives a signal that is a mix of environmental adaptations, inherited characteristics and in situ adaptations.