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

机译:侏罗纪/白垩纪海平面调节的四足动物多样性动态

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摘要

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.
机译:重建生物多样性的深层趋势仍然是古生物学家的主要目标,但由于对化石记录的不均匀采样,我们对灭绝和辐射的强度和速度的理解令人困惑。特别是,1.45亿年前的侏罗纪/白垩纪(J / K)边界,尽管表面上的小物种灭绝和大量重要进化枝的辐射,仍然知之甚少。在这里,我们对全面的四足动物化石发生数据集采用严格的二次采样方法,以评估通过J / K转换而产生的该群体的宏观进化动力学。尽管大部分信号完全来自欧洲,但几乎每个更高的四足动物群都受到跨界大幅下降的影响,最终导致几个重要进化枝的灭绝以及许多现代四足动物群的生态释放和放射化。欢乐海平面的变化是这些模式的主要驱动力,它们通过利用浅海环境和通过陆地的异地物种形成来控制生物多样性。

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