白垩纪-古近纪大灭绝期间的四足动物物种-区域关系

Roger Adam Close, Bouwe Rutger Reijenga
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引用次数: 0

摘要

物种大灭绝是罕见的灾难性事件,会严重破坏生物多样性。生物多样性丧失和临时性 "灾难类群 "的出现等大规模灭绝的后果已被广泛接受,这意味着嵌套的物种-面积关系(SARs,或生物多样性如何随面积而缩放)应在这些事件中发生巨大变化:具体而言,幂律关系的斜率(反映新物种随面积增加而积累的速度)和截距(反映局部尺度的物种密度)都应下降。然而,这些假设并没有得到验证,SAR的变化对深部时间多样性动态的贡献也被忽视了。我们利用化石数据量化了北美陆生四足动物在白垩纪-古近纪(K/Pg)大灭绝(坎帕期-Ypresian)期间的嵌套SAR。不同时期和不同类群的 SARs 有很大差异。在生物大灭绝之前的时期(马斯特里赫特),异常浅的 SAR 斜坡(表明贝塔多样性或省区性较低)导致恐龙、哺乳动物和其他四足类动物的总区域多样性较低。在恐龙灭绝后不久的时期(达尼安纪),哺乳动物爆炸性的多样化通过 SAR 斜率的大幅增加(表明较高的β多样性或省区性)以及 SAR 截距的有限增加(表明小尺度上有限的多样性变化)驱动了较高的区域多样性。这与灭绝后的生物群落应该因灾害类群的扩散而区域同质化、因多样性丧失而贫乏的预期相矛盾。生物大灭绝后早期 SAR 斜率的增加在萨尼特-志留纪(约 4.4 百万年后)又出现了截距的增加,这表明局部和区域尺度的多样性动态变化并不同步。这些结果表明了 SAR 对于理解深时多样性动态,特别是大灭绝后恢复的空间动态的重要性。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Tetrapod species-area relationships across the Cretaceous-Paleogene mass extinction
Mass extinctions are rare but catastrophic events that profoundly disrupt biodiversity. Widely-accepted consequences of mass extinctions, such as biodiversity loss and the appearance of temporary 'disaster taxa,' imply that nested species-area relationships (SARs, or how biodiversity scales with area) should change dramatically across these events: specifically, both the slope (reflecting the rate of accumulation of new species with increasing area) and intercept (reflecting the density of species at local scales) of the power-law relationship should decrease. However, these hypotheses have not been tested, and the contribution of variation in the SAR to diversity dynamics in deep time has been neglected. We use fossil data to quantify nested SARs in North American terrestrial tetrapods through the Cretaceous- Paleogene (K/Pg) mass extinction (Campanian-Ypresian). SARs vary substantially through time and among groups. In the pre-extinction interval (Maastrichtian), unusually shallow SAR slopes (indicating low beta diversity or provinciality) drive low total regional diversity in dinosaurs, mammals and other tetrapods. In the immediate post-extinction interval (Danian), the explosive diversification of mammals drove high regional diversity via a large increase in SAR slope (indicating higher beta diversity or provinciality), and only a limited increase in SAR intercept (suggesting limited diversity change at small scales). This contradicts the expectation that post-extinction biotas should be regionally homogenized by the spread of disaster taxa and impoverished by diversity loss. This early post-extinction increase in SAR slope was followed in the Thanetian-Selandian (~4.4. myr later) by increases in the intercept, indicating that diversity dynamics at local and regional scales did not change in synchrony. These results demonstrate the importance of SARs for understanding deep-time diversity dynamics, particularly the spatial dynamics of recovery from mass extinctions.
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