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Phylogenetic diversity in the Iberian flora through the Cenozoic

机译:通过新生代伊伯利亚植物植物的系统发育多样性

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摘要

Phylogenetic diversity reflects both community assembly and evolutionary diversification processes. Communities with low phylogenetic diversity might be the outcome of environmental filters favouring the occurrence and/or the diversification of lineages from particular clades. This rationale applies for regional assemblages. Here we propose to integrate phylogenetic diversity into paleobotanical studies aimed to reconstruct temporal shifts in plant assemblages in the past. To do so we first compiled a fossil dataset of 619 vascular plant taxa occurring through the Cenozoic in the Iberian flora, then we reconstructed their phylogenetic relationships, and finally we calculated temporal changes in phylogenetic diversity. The results reveal high phylogenetic diversity in the early Cenozoic (Danian to Lutetian) followed by an abrupt decline around 40 million years ago and a time interval of lower values during the Oligocene and the Miocene. A decreasing trend of phylogenetic diversity was also detected over the Piacenzian and the Early Pleistocene. Early values of high phylogenetic diversity were not explained by null models, and we speculate on putative causes related to climate. Overall, we propose to combine paleobotanical and phylogenetic information for detecting evolutionary changes that shaped our biodiversity across relevant geological scales.
机译:系统发育多样性反映了社区组装和进化多样化过程。具有低系统发育多样性的群体可能是环境过滤器的结果,偏好于特定植物的发生和/或谱系的多样化。这个理由适用于区域汇编。在这里,我们建议将系统发育多样性纳入古孤单研究,旨在在过去的植物组合中重建时间变化。为此,我们首先编译了通过伊比利亚植物中生成的血管植物分类群的化石数据集,然后我们重建了它们的系统发育关系,最后我们计算了系统发育多样性的时间变化。结果揭示了早期新生代(Danian至卢特蒂安)的高系统多样性,然后突然下降约4000万年前,寡烯烯及中新世期间的较低值的时间间隔。在Piacenzian和早期更新世中也检测到系统发育多样性的降低趋势。零模型未解释高音发育多样性的早期值,我们推测了与气候相关的推定原因。总体而言,我们建议将古蝴蝶结和系统发育信息组合以检测相关地质尺度的生物多样性的进化变化。

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