首页> 外文期刊>Zoological Journal of the Linnean Society >A giant rhinocerotoid (Mammalia, Perissodactyla) from the Late Oligocene of north-central Anatolia (Turkey)
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A giant rhinocerotoid (Mammalia, Perissodactyla) from the Late Oligocene of north-central Anatolia (Turkey)

机译:来自安那托利亚中北部(土耳其)晚渐新世的巨型鼻猴类(哺乳动物,Perissodactyla)

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摘要

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 Gozukizilli, in the Cankiri-Corum Tertiary basin. These layers correspond to the Lower member of the Kizilirmak Formation. The same locality (Gozukizilli-2) yields also the small rhinocerotid Protaceratherium sp., cf. P. albigense (Roman, 1912). Three other mammal localities (Gozukizilli-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. (c) 2008 The Linnean Society of London.
机译:在土耳其黑海以南,首次描述了一个巨大的犀牛类。单个标本的碎片半径称为Paraceratherium sp。,起源于Cankiri-Corum第三纪盆地Gozukizilli附近的砾岩。这些层对应于Kizilirmak组的下部。相同的位置(Gozukizilli-2)也产生小的犀牛角Protaceratherium sp。,请参见。 P. albigense(罗马,1912年)。其他三个哺乳动物种群(地层下部的Gozukizilli-1,有几种啮齿动物; Tepe 641和Kizilirmak,地上部的,有多种微型和大型哺乳动物群),我们可以参考Kizilirmak组整体为晚渐新世。所有观察到的分类单元都具有很强的亚洲和/或欧洲相似性,这使得渐新世晚期安那托利亚的这一部分无法进行地理隔离。 (c)2008年伦敦林奈学会。

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