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Quantifying the effects of the break up of Pangaea on global terrestrial diversification with neutral theory

机译:用中性理论量化Pangea分手对全球陆地多样化的影响

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摘要

The historic richness of most taxonomic groups increases substantially over geological time. Explanations for this fall broadly into two categories: bias in the fossil record and elevated net rates of diversification in recent periods. For example, the break up of Pangaea and isolation between continents might have increased net diversification rates. In this study, we investigate the effect on terrestrial diversification rates of the increased isolation between land masses brought about by continental drift. We use ecological neutral theory as a means to study geologically complex scenarios tractably. Our models show the effects of simulated geological events that affect all species equally, without the added complexity of further ecological processes. We find that continental drift leads to an increase in diversity only where isolation between continents leads to additional speciation through vicariance, and where higher taxa with very low global diversity are considered. We conclude that continental drift by itself is not sufficient to account for the increase in terrestrial species richness observed in the fossil record.
机译:随着时间的推移,大多数生物分类群的历史丰富性大大增加。对此的解释大致可分为两类:化石记录的偏见和最近时期多样化的净比率上升。例如,Pangea的解体和各大洲之间的孤立可能会增加净多样化率。在这项研究中,我们调查了由大陆漂移带来的土地块之间的隔离度增加对陆地多样化速率的影响。我们使用生态中立理论作为一种手段来研究地质复杂情况。我们的模型显示了模拟地质事件对所有物种的影响均等,而没有进一步生态过程的复杂性。我们发现,仅当大洲之间的孤立导致通过世俗形成额外物种形成以及考虑到全球生物多样性非常低的较高分类群时,大陆漂移才导致多样性的增加。我们得出的结论是,大陆漂移本身不足以解释化石记录中观测到的陆地物种丰富度的增加。

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