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A New Sebecid from the Paleogene of Brazil and the Crocodyliform Radiation after the K–Pg Boundary

机译:K–Pg边界后巴西古近纪的新陆相和鳄状辐射

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摘要

A new crocodyliform, Sahitisuchus fluminensis gen. et sp. nov., is described based on a complete skull, lower jaw and anterior cervical vertebrae collected in the São José de Itaboraí Basin of Rio de Janeiro, Brazil. The specimen is one of the best preserved crocodyliforms from Paleocene deposits recovered so far and represents a sebecosuchian, one of the few clades that survived the Cretaceous-Paleogene biotic crisis. The new taxon is found in the same deposit as an alligatoroid, a group that experienced large diversification in the Paleogene. The sebecosuchian record suggests that after the Cretaceous-Paleogene biotic crisis, the less specialized members of this clade characterized by a higher number of teeth compared to the baurusuchid sebecosuchians survived, some having terrestrial habits while others developed a semi-aquatic life style (e.g., Lorosuchus). Starting in the Eocene, sebecid sebecosuchians became specialized with a more accentuated oreinirostry as observed in Sebecus and in Langstonia, but not showing the typical reduced dentition developed by the Cretaceous baurusuchid sebecosuchians. The basal position of Barinasuchus arveloi, a high-snouted Miocene sebecid, indicates the occurrence of an independent lineage sometime after the K-Pg biotic crisis that developed accentuated oreinirostry, suggesting a more complex history of the post-K-Pg crocodyliform radiation.
机译:一种新的鳄形,Sahitisuchus fluminensis gen。等。根据在巴西里约热内卢的圣何塞·德伊塔博拉伊盆地收集的完整头骨,下颌和颈前椎骨描述了11月。该标本是迄今从古新世沉积物中保存得最好的鳄形动物之一,代表了一个sebecosuchian,这是在白垩纪-古生物危机中幸存下来的少数进化枝之一。新的分类单元与鳄鱼一样,在古近纪经历了广泛的多样化。 sebecosuchian的记录表明,在白垩纪-古生代生物危机之后,该进化枝中较不专业的成员得以存活,与baurusuchid sebecosuchians相比,它们的牙齿数量更高,其中一些具有陆地习性,而另一些则发展为半水生生活方式(例如, Lorosuchus)。从始新世开始,sebecid sebecosuchians变得专门化,如在Sebecus和Langstonia中观察到的那样,突出了更严谨的矿石技术,但是没有显示出白垩纪baurusuchid sebecosuchians发展出的典型的牙列减少。 Baranosuchus arveloi的基础位置,是一种高鼻梁的中新世沉积物,表明在K-Pg生物危机爆发后的某个时期,发生了独立的血统,这加剧了矿石运动,这说明了K-Pg后鳄形辐射的历史更为复杂。

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