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A giant rhinocerotoid (Mammalia, Perissodactyla) from the Late Oligocene of north-central Anatolia (Turkey)
Authors:PIERRE-OLIVIER ANTOINE ,LEVENT KARADENIZLI,GERÇ  EK SARAÇ  , SEVKET SEN
Affiliation:Laboratoire des Mécanismes de Transfert en Géologie, Universitéde Toulouse, CNRS, IRD, OMP, 14 Avenue Édouard Belin, F-31400 Toulouse, France;
Geology Department, Maden ve Tektik Arama Genel Müdürlügü, 06520 Ankara, Turkey;
Natural History Museum, Maden ve Tektik Arama Genel Müdürlügü, 06520 Ankara, Turkey;
Laboratoire de Paléontologie, UMR 5143 CNRS, Muséum National d'Histoire Naturelle, 8 rue Buffon, F-75005 Paris Cedex 5, France
Abstract:A giant rhinocerotoid is described for the first time south of the Black Sea, in Turkey. The single specimen, a fragmentary radius referred to Paraceratherium sp., originates from conglomerates nearby at Gözükizilli, in the Çankiri–Çorum Tertiary basin. These layers correspond to the Lower member of the Kizilirmak Formation. The same locality (Gözükizilli-2) yields also the small rhinocerotid Protaceratherium sp., cf. P. albigense (Roman, 1912). Three other mammal localities (Gözükizilli-1, in the Lower Member of the formation, with several rodent species; Tepe 641 and Kizilirmak, in the Upper Member, with a diversified micro- and macro-mammal fauna) allow us to refer the Kizilirmak Formation as a whole to the Late Oligocene. All the observed taxa have strong Asian and/or European affinities, which precludes any geographical insulation for this part of Anatolia during the Late Oligocene.  © 2008 The Linnean Society of London, Zoological Journal of the Linnean Society, 2008, 152 , 581–592.
Keywords:indricothere    palaeogeography    Paraceratherium    vertebrate palaeontology
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