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The last diadectomorph sheds light on Late Palaeozoic tetrapod biogeography

机译:最后的十二齿生物揭示了晚古生代四足动物的生物地理学

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摘要

Diadectomorpha is a clade of Late Palaeozoic vertebrates widely recognized as the sister group of crown-group Amniota and the first tetrapod lineage to evolve high-fibre herbivory. Despite their evolutionary importance, diadectomorphs are restricted stratigraphically and geographically, with all records being from the Upper Carboniferous and Lower Permian of North America and Germany. We describe a new diadectomorph, Alveusdectes fenestralis, based on a partial skull from the Upper Permian of China. The new species exhibits the derived mechanism for herbivory and is recovered phylogenetically as a deeply nested diadectid. Approximately 16 Myr younger than any other diadectomorph, Alveusdectes is the product of at least a 46 Myr ghost lineage. How much of this time was probably spent in Russia and/or central Asia will remain unclear until a specimen is described that subdivides this cryptic history, but the lineage assuredly crossed this region before entering the relatively isolated continent of North China. The discovery of Alveusdectes raises important questions regarding diadectomorph extinction dynamics including what, if any, ecological factors limited the diversity of this group in eastern Pangea. It also suggests that increased sampling in Asia will likely significantly affect our views of clade and faunal insularity leading up to the Permo-Triassic extinction.
机译:Diadectomorpha是晚期古生代脊椎动物的进化枝,被广泛认为是冠群羊膜动物的姊妹群和第一个进化出高纤维草食动物的四足动物谱系。尽管它们在进化上很重要,但地变和地层受到地层和地理的限制,所有记录都来自北美和德国的上石炭统和下二叠统。我们基于来自中国上二叠纪的部分颅骨描述了一种新的十二齿变种,类孔膜。新物种显示出食草性的衍生机制,并在系统发育上以深嵌套的双壁昆虫的形式被回收。 Alveusdectes比任何其他十二齿变态动物年龄都要小大约16 Myr,它是至少46 Myr幽灵血统的产物。在描述一个可以细分这种神秘历史的标本之前,目前尚不清楚在俄罗斯和/或中亚花费了多少时间,但是这些血统肯定进入了该地区,然后才进入相对偏远的华北大陆。破囊动物的发现引起了有关十二齿动物灭绝动力学的重要问题,包括哪些生态因素限制了该物种在东潘吉亚的多样性。这也表明,亚洲采样的增加可能会极大地影响我们对导致二叠纪-三叠纪灭绝的进化枝和动物群孤立的看法。

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