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A new specimen of Prolacerta broomi from the lower Fremouw Formation (Early Triassic) of Antarctica its biogeographical implications and a taxonomic revision

机译:南极下部Fremouw组(早三叠世)的Prolacerta broomi新标本其生物地理意义和分类学修订

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摘要

Prolacerta broomi is an Early Triassic archosauromorph of particular importance to the early evolution of archosaurs. It is well known from many specimens from South Africa and a few relatively small specimens from Antarctica. Here, a new articulated specimen from the Fremouw Formation of Antarctica is described in detail. It represents the largest specimen of Prolacerta described to date with a nearly fully articulated and complete postcranium in addition to four skull elements. The study of this specimen and the re-evaluation of other Prolacerta specimens from both Antarctica and South Africa reveal several important new insights into its morphology, most notably regarding the premaxilla, manus, and pelvic girdle. Although well-preserved skull material from Antarctica is still lacking for Prolacerta, a detailed comparison of Prolacerta specimens from Antarctica and South Africa corroborates previous findings that there are no characters clearly distinguishing the specimens from these different regions and therefore the Antarctic material is assigned to Prolacerta broomi. The biogeographical implications of these new findings are discussed. Finally, some osteological characters for Prolacerta are revised and an updated diagnosis and phylogenetic analysis are provided.
机译:Prolacerta broomi是早期三叠纪的始祖龙,对始祖的早期进化特别重要。从南非的许多标本和南极洲的一些相对较小的标本中众所周知。在此,详细描述了南极的弗雷莫(Fremouw)地层的一个新的关节标本。它代表了迄今为止描述的最大的Prolacerta标本,除了四个颅骨元素外,还具有几乎完全铰接和完整的后颅骨。对该标本的研究以及对来自南极和南非的其他Prolacerta标本的重新评估,揭示了对其形态的一些重要的新见解,其中最显着的方面涉及前颌骨,手掌和骨盆带。尽管对于Prolacerta仍然缺少保存良好的南极头骨材料,但是对南极洲和南非的Prolacerta标本进行的详细比较证实了以前的发现,即没有明显区分这些标本与这些不同区域的特征,因此将南极材料指定为Prolacerta布鲁米讨论了这些新发现的生物地理意义。最后,修订了泌乳生殖器的一些骨学特征,并提供了更新的诊断和系统发育分析。

著录项

  • 期刊名称 Scientific Reports
  • 作者

    Stephan N. F. Spiekman;

  • 作者单位
  • 年(卷),期 -1(8),-1
  • 年度 -1
  • 页码 17996
  • 总页数 21
  • 原文格式 PDF
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