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海平面通过侏罗纪/白垩纪间隔调节了四足动物多样性的动态变化。

Sea level regulated tetrapod diversity dynamics through the Jurassic/Cretaceous interval.

机构信息

Department of Earth Science and Engineering, Imperial College London, London SW6 2AZ, UK.

Department of Earth Sciences, University College London, Gower Street, London WC1E 6BT, UK.

出版信息

Nat Commun. 2016 Sep 2;7:12737. doi: 10.1038/ncomms12737.

Abstract

Reconstructing deep time trends in biodiversity remains a central goal for palaeobiologists, but our understanding of the magnitude and tempo of extinctions and radiations is confounded by uneven sampling of the fossil record. In particular, the Jurassic/Cretaceous (J/K) boundary, 145 million years ago, remains poorly understood, despite an apparent minor extinction and the radiation of numerous important clades. Here we apply a rigorous subsampling approach to a comprehensive tetrapod fossil occurrence data set to assess the group's macroevolutionary dynamics through the J/K transition. Although much of the signal is exclusively European, almost every higher tetrapod group was affected by a substantial decline across the boundary, culminating in the extinction of several important clades and the ecological release and radiation of numerous modern tetrapod groups. Variation in eustatic sea level was the primary driver of these patterns, controlling biodiversity through availability of shallow marine environments and via allopatric speciation on land.

摘要

重建生物多样性的深层时间趋势仍然是古生物学家的核心目标,但由于化石记录的采样不均匀,我们对灭绝和辐射的幅度和速度的理解受到了混淆。特别是,1.45 亿年前的侏罗纪/白垩纪(J/K)边界仍然知之甚少,尽管存在明显的小规模灭绝和许多重要类群的辐射。在这里,我们应用严格的抽样方法来评估一个综合的四足动物化石出现数据集,以评估该群体在 J/K 过渡期间的宏观进化动态。尽管大部分信号仅来自欧洲,但几乎每个高等四足动物群体都受到了边界处的重大下降的影响,最终导致了几个重要类群的灭绝,以及许多现代四足动物群体的生态释放和辐射。海平面的变化是这些模式的主要驱动因素,通过浅海环境的可用性以及陆地的异域物种形成来控制生物多样性。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/fd6b/5025807/634b154933b9/ncomms12737-f1.jpg

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