首页> 美国卫生研究院文献>Proceedings of the Royal Society B: Biological Sciences >Biogeography of Triassic tetrapods: evidence for provincialism and driven sympatric cladogenesis in the early evolution of modern tetrapod lineages
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Biogeography of Triassic tetrapods: evidence for provincialism and driven sympatric cladogenesis in the early evolution of modern tetrapod lineages

机译:三叠纪四足动物的生物地理学:现代四足动物谱系早期进化中的地方主义和驱动的同伴生殖系统发生的证据

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摘要

Triassic tetrapods are of key importance in understanding their evolutionary history, because several tetrapod clades, including most of their modern lineages, first appeared or experienced their initial evolutionary radiation during this Period. In order to test previous palaeobiogeographical hypotheses of Triassic tetrapod faunas, tree reconciliation analyses (TRA) were performed with the aim of recovering biogeographical patterns based on phylogenetic signals provided by a composite tree of Middle and Late Triassic tetrapods. The TRA found significant evidence for the presence of different palaeobiogeographical patterns during the analysed time spans. First, a Pangaean distribution is observed during the Middle Triassic, in which several cosmopolitan tetrapod groups are found. During the early Late Triassic a strongly palaeolatitudinally influenced pattern is recovered, with some tetrapod lineages restricted to palaeolatitudinal belts. During the latest Triassic, Gondwanan territories were more closely related to each other than to Laurasian ones, with a distinct tetrapod fauna at low palaeolatitudes. Finally, more than 75 per cent of the cladogenetic events recorded in the tetrapod phylogeny occurred as sympatric splits or within-area vicariance, indicating that evolutionary processes at the regional level were the main drivers in the radiation of Middle and Late Triassic tetrapods and the early evolution of several modern tetrapod lineages.
机译:三叠纪的四足动物在理解它们的进化史上至关重要,因为在此期间,几个四足动物进化枝,包括大多数现代谱系,首次出现或经历了它们最初的进化辐射。为了检验先前的三叠纪四足动物群的古生物地理假说,进行了树木和解分析(TRA),目的是根据中,晚三叠纪四足动物的复合树提供的系统发育信号恢复生物地理模式。 TRA发现了在分析的时间跨度中存在不同古生物地理模式的重要证据。首先,在中三叠纪期间观察到Pangaean分布,其中发现了几个国际四足动物群。在晚三叠世早期,恢复了强烈的古纬度影响模式,一些四足动物谱系仅限于古纬度带。在最新的三叠纪期间,冈瓦南领土彼此之间的联系比与劳拉斯地区的联系更紧密,在低古大陆上有独特的四足动物区系。最后,记录在四足动物系统发育史中的75%以上的克拉多米尼事件是同胞分裂或区域内变异,表明区域水平的演化过程是中,晚三叠纪四足动物和早期辐射的主要驱动力。几种现代四足动物谱系的进化。

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