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来自阿根廷南部的一新古新世鳄类揭示了凯门鳄类的早期历史。

A new Palaeocene crocodylian from southern Argentina sheds light on the early history of caimanines.

机构信息

CONICET, Buenos Aires, Argentina

División Paleontología Vertebrados, Museo de La Plata, Paseo del Bosque s/n, 1900 La Plata, Argentina.

出版信息

Proc Biol Sci. 2018 Aug 22;285(1885):20180843. doi: 10.1098/rspb.2018.0843.

Abstract

Caimanines are crocodylians currently restricted to South and Central America and the oldest members are from lower Palaeocene localities of the Salamanca Formation (Chubut Province, Argentina). We report here a new caimanine from this same unit represented by a skull roof and partial braincase. Its phylogenetic relationships were explored in a cladistic analysis using standard characters and a morphogeometric two-dimensional configuration of the skull roof. The phylogenetic results were used for an event-based supermodel quantitative palaeobiogeographic analysis. The new species is recovered as the most basal member of the South American caimanines, and the Cretaceous North American lineage ' and related forms' as the most basal Caimaninae. The biogeographic results estimated north-central North America as the ancestral area of Caimaninae, showing that the Cretaceous and Palaeocene species of the group were more widespread than thought and became regionally extinct in North America around the Cretaceous-Palaeocene boundary. A dispersal event from north-central North America during the middle Late Cretaceous explains the arrival of the group to South America. The Palaeogene assemblage of Patagonian crocodylians is composed of three lineages of caimanines as a consequence of independent dispersal events that occurred between North and South America and within South America around the Cretaceous-Palaeogene boundary.

摘要

凯门鳄类是现今局限于中南美洲的鳄形目动物,最古老的成员来自下古新统的萨拉曼卡组(阿根廷丘布特省)。本文报道了一个来自同一地层的新的凯门鳄类头骨顶骨和部分脑颅。我们通过使用标准特征和头骨顶骨的二维形态几何结构进行分支分析,探讨了其系统发育关系。系统发育结果用于基于事件的超模型定量古生物地理分析。新种被恢复为南美凯门鳄类最基干的成员,而白垩纪北美的“谱系”和相关形式则为最基干的凯门鳄科。生物地理结果估计中北部北美是凯门鳄科的祖先地区,表明该组的白垩纪和古新世物种的分布范围比以前认为的更广,并在白垩纪-古近纪边界附近在北美地区区域性灭绝。从中晚白垩纪时期从中北部北美发生的扩散事件解释了该组到达南美洲的原因。巴塔哥尼亚鳄类的古近纪组合由三个凯门鳄类谱系组成,这是由于在白垩纪-古近纪边界时期发生了在北美和南美之间以及在南美的独立扩散事件。

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