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首页> 外文期刊>Zoological Journal of the Linnean Society >A new turtle from the Palaeogene of Patagonia (Argentina) sheds new light on the diversity and evolution of the bizarre clade of horned turtles (Meiolaniidae, Testudinata)
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A new turtle from the Palaeogene of Patagonia (Argentina) sheds new light on the diversity and evolution of the bizarre clade of horned turtles (Meiolaniidae, Testudinata)

机译:巴塔哥尼亚古生物的新龟(阿根廷)为角龟离奇进化枝(Meiolaniidae,Testudinata)的多样性和进化提供了新的思路。

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In this contribution we present a new species of horned turtle, Gaffneylania auricularis gen. et sp. nov., from the Paleogene of Patagonia. The specimens come from the lower section of the Sarmiento Formation (Middle Eocene) at Cerro Verde (Canadon Hondo area, Province of Chubut, Argentina). The level containing turtles and crocodyliforrmes is located at the base of the section and it consists of laminated, fine tuffs interpreted as shallow pond sediments. It underlies another fossiliferous level comprising lenticular, massive sandstones bearing skeletal remains of mammals, referred by previous authors to the Casamayoran SALMA. Gaffneylania auricularis represents one of the most complete meiolaniids from South America found to date and it is distinguished from other meiolaniids by the presence of a peculiar half-moon-shaped, thick rim surrounding the cavum tympani, the presence of three cranial scutes K and an unenclosed canalis chorda tympani mandibularis, among others. This new species sheds new light on the evolution and palaeobiogeographical history of the clade Meiolaniidae in Australasia and South America during the Cainozoic. The break up of southern Gondwana provoked major global climatic changes during the Cainozoic that probably influenced the evolution of meiolaniid turtles. The co-evolution of meiolaniids with other amniotes (e.g. chelid turtles, mammals) suggests a common palaeobiogeographical history of those clades in southern Gondwana. (C) 2015 The Linnean Society of London.
机译:在这项贡献中,我们提出了一种新的角龟,Gaffneylania auricularis gen。等。十一月,来自巴塔哥尼亚的古近纪。这些标本来自塞罗维德(阿根廷丘布特省卡纳登·洪多地区)萨尔门托组(中新世)的下部。包含海龟和鳄形纲的水平面位于剖面的底部,由层状细密的凝灰岩组成,被解释为浅池沉积物。它是另一个化石层的基础,包括具哺乳动物骨骼残留物的柱状大块砂岩,以前的作者将其称为Casamayoran SALMA。 Gaffneylania auricularis代表迄今发现的南美洲最完整的meiolaniids之一,它与其他meiolaniids的区别在于,在鼓腔周围有奇特的半月形,厚边,三个颅骨K和一个未封闭的canalis chorda tympani mandibularis等。这个新物种为新生代期间在澳大拉西亚和南美的Meiolananiidae进化枝和古生物地理史提供了新的线索。冈瓦纳南部的破裂引发了新生代主要的全球气候变化,这可能影响了龟甲类龟的进化。犬齿兰类动物与其他羊膜动物(例如螯鱼,哺乳动物)的共同进化表明,冈瓦纳南部这些进化枝具有共同的古生物地理历史。 (C)2015年伦敦林奈学会。

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