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中生代四足动物长期多样化的近乎停滞状态。

Near-Stasis in the Long-Term Diversification of Mesozoic Tetrapods.

作者信息

Benson Roger B J, Butler Richard J, Alroy John, Mannion Philip D, Carrano Matthew T, Lloyd Graeme T

机构信息

Department of Earth Sciences, University of Oxford, Oxford, United Kingdom.

School of Geography, Earth and Environmental Sciences, University of Birmingham, Birmingham, United Kingdom.

出版信息

PLoS Biol. 2016 Jan 25;14(1):e1002359. doi: 10.1371/journal.pbio.1002359. eCollection 2016 Jan.

Abstract

How did evolution generate the extraordinary diversity of vertebrates on land? Zero species are known prior to ~380 million years ago, and more than 30,000 are present today. An expansionist model suggests this was achieved by large and unbounded increases, leading to substantially greater diversity in the present than at any time in the geological past. This model contrasts starkly with empirical support for constrained diversification in marine animals, suggesting different macroevolutionary processes on land and in the sea. We quantify patterns of vertebrate standing diversity on land during the Mesozoic-early Paleogene interval, applying sample-standardization to a global fossil dataset containing 27,260 occurrences of 4,898 non-marine tetrapod species. Our results show a highly stable pattern of Mesozoic tetrapod diversity at regional and local levels, underpinned by a weakly positive, but near-zero, long-term net diversification rate over 190 million years. Species diversity of non-flying terrestrial tetrapods less than doubled over this interval, despite the origins of exceptionally diverse extant groups within mammals, squamates, amphibians, and dinosaurs. Therefore, although speciose groups of modern tetrapods have Mesozoic origins, rates of Mesozoic diversification inferred from the fossil record are slow compared to those inferred from molecular phylogenies. If high speciation rates did occur in the Mesozoic, then they seem to have been balanced by extinctions among older clades. An apparent 4-fold expansion of species richness after the Cretaceous/Paleogene (K/Pg) boundary deserves further examination in light of potential taxonomic biases, but is consistent with the hypothesis that global environmental disturbances such as mass extinction events can rapidly adjust limits to diversity by restructuring ecosystems, and suggests that the gradualistic evolutionary diversification of tetrapods was punctuated by brief but dramatic episodes of radiation.

摘要

进化是如何在陆地上产生脊椎动物的非凡多样性的?在约3.8亿年前之前,已知的脊椎动物物种为零,而如今有超过3万种。一种扩张主义模型认为,这是通过大规模且无限制的增长实现的,导致如今的多样性比地质历史上的任何时期都要大得多。该模型与海洋动物受限制的多样化的实证支持形成鲜明对比,表明陆地和海洋存在不同的宏观进化过程。我们对中生代 - 古近纪早期陆地上脊椎动物现存多样性模式进行了量化,将样本标准化应用于一个包含4898种非海洋四足动物的27260个化石记录的全球数据集。我们的结果表明,中生代四足动物在区域和局部水平上具有高度稳定的多样性模式,在1.9亿年的时间里,长期净多样化率呈微弱的正向但接近零。在此期间,非飞行陆地四足动物的物种多样性增加不到一倍,尽管哺乳动物、有鳞目动物、两栖动物和恐龙中出现了极其多样的现存类群。因此,尽管现代四足动物的物种丰富类群起源于中生代,但从化石记录推断出的中生代多样化速率与从分子系统发育推断出的速率相比是缓慢的。如果中生代确实发生了高物种形成速率,那么它们似乎被较老分支中的灭绝所平衡。白垩纪 / 古近纪(K/Pg)边界之后物种丰富度明显的4倍增长,鉴于潜在的分类偏差值得进一步研究,但与这样的假设一致,即诸如大规模灭绝事件等全球环境干扰可以通过重组生态系统迅速调整多样性的限制,并表明四足动物的渐进式进化多样化被短暂但剧烈的辐射事件所打断。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/2634/4726655/1c3d0d6604c6/pbio.1002359.g001.jpg

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