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首页> 外文期刊>Palaeontology >A LARGE PHOLIDOSAURID IN THE PHU KRADUNG FORMATION OF NORTH-EASTERN THAILAND
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A LARGE PHOLIDOSAURID IN THE PHU KRADUNG FORMATION OF NORTH-EASTERN THAILAND

机译:东北泰国PHU KRADUNG组的大型蛇绿龙

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摘要

In the early 1980s, the remains of a large crocodilian, consisting of a nearly complete lower jaw, were referred to a distinct species of Sunosuchus, S. thailandicus. The specimen was recovered from a road-cut near Nong Bua Lamphu, north-eastern Thailand, in the upper part of the continental Phu Kradung Formation, and then considered Early to Middle Jurassic in age. Since then, this age has been revised and most of the formation is now considered Early Cretaceous, although a Late Jurassic age is possible for its lowermost part. Here, we report for the first time cranial elements associated with mandibular remains assignable to 'S'. thailandicus. An attribution to Pholidosauridae is proposed on the basis of premaxillary morphology, and the original referral of this taxon to the goniopholidid Sunosuchus is discarded. A new genus name Chalawan now designates the originally described material of S. thailandicus. Nevertheless, the newly described specimen shares a characteristic with both 'traditional' Goniopholididae and Pholidosauridae: the presence of a depression located on the lateral wall of the maxilla and jugal. A phylogenetic analysis confirms the inclusion of both Goniopholididae and Pholidosauridae into a common clade, Coelognathosuchia tax. nov. Although the new Thai skull is much fragmented, its original shape is reconstructed and is compared with other pholidosaurid genera, namely Elosuchus, Meridiosaurus, Oceanosuchus, Pholidosaurus, Sarcosuchus and Terminonaris. The presence of the genus Sunosuchus being highly questionable in Thailand, it cannot be used as evidence to link the Chinese and Indochinese blocks. Instead, the recognition of a freshwater pholidosaurid in a continental formation of the Indochinese block suggests that early in their evolutionary history, these crocodilians, already known from Europe, Africa and South America, were more widely distributed along the northern margin of the Tethys than previously recognized.
机译:在1980年代初期,一条大鳄鱼的遗骸由几乎完整的下颌组成,被称为Sunosuchus,S. thailandicus的不同物种。该标本是从位于泰国东北部的富卡丹洞组上部的农布纳普附近的一处道路开挖的,然后被认为是早侏罗世至中侏罗世。从那时起,这个年龄已经被修改,现在大部分地层被认为是早白垩纪,尽管侏罗纪晚期可能是最低年龄。在这里,我们首次报告与下颌骨相关的颅骨元素可分配给“ S”。泰国。在前颌前形态学的基础上,提出了对剑龙科的一种归因,并且放弃了该分类单元原代至性鞘磷脂Sunosuchus的转介。现在,一种新的名称Chalawan代表了最初描述的S. thailandicus的材料。尽管如此,新近描述的标本与“传统的”虎科和蛇头科有一个共同特征:在上颌和颌骨的侧壁上存在凹陷。系统发育分析证实,将淋病科和蛇形纲科都包括在普通进化枝中,即Coelognathosuchia税。十一月尽管新的泰国头骨碎片很多,但其原始形状得以重建,并与其他腓骨龙属(Elosuchus,Meridiosaurus,Oceanosuchus,Pholidosaurus,Sarcosuchus和Terminonaris)进行了比较。在泰国,Sunosuchus属的存在值得怀疑,它不能用作将中国和印度支那地块联系起来的证据。取而代之的是,在印度支那大陆块的大陆形成中发现了淡水棘甲龙,这表明在进化史的早期,这些在欧洲,非洲和南美已广为人知的鳄鱼在特提斯北部边缘分布较广。公认的。

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