Silvestro Daniele, Cascales-Miñana Borja, Bacon Christine D, Antonelli Alexandre
Department of Biological and Environmental Sciences, University of Gothenburg, Carl Skottsbergs gata 22B, SE-413 19, Göteborg, Sweden.
CNRS, UMR Botanique et Bioinformatique de l'Architecture des Plantes (AMAP), Montpellier, F-34000, France.
New Phytol. 2015 Jul;207(2):425-436. doi: 10.1111/nph.13247. Epub 2015 Jan 26.
Plants have a long evolutionary history, during which mass extinction events dramatically affected Earth's ecosystems and its biodiversity. The fossil record can shed light on the diversification dynamics of plant life and reveal how changes in the origination-extinction balance have contributed to shaping the current flora. We use a novel Bayesian approach to estimate origination and extinction rates in plants throughout their history. We focus on the effect of the 'Big Five' mass extinctions and on estimating the timing of origin of vascular plants, seed plants and angiosperms. Our analyses show that plant diversification is characterized by several shifts in origination and extinction rates, often matching the most important geological boundaries. The estimated origin of major plant clades predates the oldest macrofossils when considering the uncertainties associated with the fossil record and the preservation process. Our findings show that the commonly recognized mass extinctions have affected each plant group differently and that phases of high extinction often coincided with major floral turnovers. For instance, after the Cretaceous-Paleogene boundary we infer negligible shifts in diversification of nonflowering seed plants, but find significantly decreased extinction in spore-bearing plants and increased origination rates in angiosperms, contributing to their current ecological and evolutionary dominance.
植物有着漫长的进化史,在此期间,大规模灭绝事件对地球生态系统及其生物多样性产生了巨大影响。化石记录能够揭示植物生命的多样化动态,并揭示起源-灭绝平衡的变化如何促成了当前植物群的形成。我们采用一种新颖的贝叶斯方法来估计植物在其整个历史中的起源和灭绝速率。我们关注“五大”大规模灭绝的影响,并估计维管植物、种子植物和被子植物的起源时间。我们的分析表明,植物多样化的特征是起源和灭绝速率的几次转变,这些转变常常与最重要的地质界限相匹配。考虑到与化石记录和保存过程相关的不确定性,主要植物类群的估计起源时间早于最古老的宏观化石。我们的研究结果表明,普遍认可的大规模灭绝事件对每个植物类群的影响各不相同,而且高灭绝阶段往往与主要的植物更替同时发生。例如,在白垩纪-古近纪边界之后,我们推断非开花种子植物的多样化变化微不足道,但发现孢子植物的灭绝显著减少,被子植物的起源速率增加,这促成了它们目前在生态和进化上的优势地位。