首页> 外文期刊>Proceedings of the Royal Society. Biological sciences >Delayed recovery of non-marine tetrapods after the end-permian mass extinction tracks global carbon cycle
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Delayed recovery of non-marine tetrapods after the end-permian mass extinction tracks global carbon cycle

机译:二叠纪末大灭绝追踪全球碳循环后非海洋四足动物的延迟恢复

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摘要

During the end-Permian mass extinction, marine ecosystems suffered a major drop in diversity, which was maintained throughout the Early Triassic until delayed recovery during the Middle Triassic. This depressed diversity in the Early Triassic correlates with multiple major perturbations to the global carbon cycle, interpreted as either intrinsic ecosystem or external palaeoenvironmental effects. In contrast, the terrestrial record of extinction and recovery is less clear; the effects and magnitude of the end-Permian extinction on non-marine vertebrates are particularly controversial. We use specimenlevel data from southern Africa and Russia to investigate the palaeodiversity dynamics of non-marine tetrapods across the Permo-Triassic boundary by analysing sample-standardized generic richness, evenness and relative abundance. In addition, we investigate the potential effects of sampling, geological and taxonomic biases on these data. Our analyses demonstrate that non-marine tetrapods were severely affected by the end-Permian mass extinction, and that these assemblages did not begin to recover until the Middle Triassic. These data are congruent with those from land plants and marine invertebrates. Furthermore, they are consistent with the idea that unstable low-diversity post-extinction ecosystems were subject to boom-bust cycles, reflected in multiple Early Triassic perturbations of the carbon cycle.
机译:在二叠纪末期大灭绝期间,海洋生态系统的多样性大幅度下降,在整个三叠纪早期一直保持这种多样性,直到中三叠纪期间恢复缓慢。三叠纪早期的这种低迷的多样性与对全球碳循环的多种主要扰动有关,被解释为内在的生态系统或外部的古环境效应。相比之下,地球灭绝和恢复的记录还不清楚。二叠纪末期灭绝对非海洋脊椎动物的影响和程度尤其引起争议。我们使用来自南部非洲和俄罗斯的标本水平数据,通过分析样本标准化的通用丰富度,均匀度和相对丰度,调查跨三叠纪边界的非海洋四足动物的古生物动态。此外,我们调查了采样,地质和分类学偏见对这些数据的潜在影响。我们的分析表明,非海洋四足动物受到二叠纪末期生物大灭绝的严重影响,并且这些组合直到中三叠纪才开始恢复。这些数据与陆生植物和海洋无脊椎动物的数据一致。此外,它们与这样的观点是一致的,即不稳定的低多样性灭绝后的生态系统会经历繁荣-萧条的循环,这反映在碳循环的三叠纪早期多次扰动中。

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