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Large Cretaceous sphenodontian from Patagonia provides insight into lepidosaur evolution in Gondwana

机译:来自巴塔哥尼亚的大型白垩纪蝶齿动物洞察了冈瓦纳的鳞翅目进化

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Sphenodontian reptiles successfully radiated during Triassic and Jurassic times, but were driven almost to extinction during the Cretaceous period(1). The sparse Early Cretaceous record of sphenodontians has been interpreted as reflecting the decline of the group in favour of lizards, their suspected ecological successors(2). However, recent discoveries in Late Cretaceous beds in Patagonia partially modify this interpretation. Numerous skeletons of a new sphenodontian, Priosphenodon avelasi gen. et sp. nov., were collected from a single locality in the Cenomanian-Turonian Candeleros Formation, where it is more abundant than any other tetrapod group recorded in the quarry (for example, Crocodyliformes, Serpentes, Dinosauria and Mammalia)(3,4). Adult specimens of Priosphenodon reached one metre in length, larger than any previously known terrestrial sphenodontian. Here we propose, using available evidence, that sphenodontians were not a minor component of the Cretaceous terrestrial ecosystems of South America, and that their ecological replacement by squamates was delayed until the early Tertiary. The new discovery helps to bridge the considerable gap in the fossil record (around 120 million years) that separates the Early Cretaceous sphenodontians(5-7) from their living relatives (Sphenodon). [References: 29]
机译:Sphenodontian爬行动物在三叠纪和侏罗纪时期成功辐射,但在白垩纪时期几乎被灭绝(1)。 Sphenodontians的稀少的早白垩纪记录被解释为反映了该群体对蜥蜴的减少,而蜥蜴被认为是其生态继任者(2)。但是,最近在巴塔哥尼亚的晚白垩世层发现发现部分地改变了这一解释。一种新的齿科,Priosphenodon avelasi gen的骨骼。等。 nov。,是从Cenomanian-Turonian Candeleros组中的一个地方收集的,它比采石场中记录的任何其他四足动物组(例如,鳄形目,蛇形目,恐龙和哺乳动物)都丰富(3,4)。成年独角兽标本的长度达到一米,比任何以前已知的陆生齿像都大。在这里,我们建议使用现有证据表明,齿影动物不是南美白垩纪陆地生态系统的次要组成部分,并且它们的鳞茎替代生态被推迟到第三纪初期。这一新发现有助于弥合化石记录(大约1.2亿年)中的巨大差距,从而使白垩纪早期的齿科(5-7)与他们的亲属(Sphenodon)分开。 [参考:29]

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