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晚泥盆世大灭绝期间的生态位保守性和生态变化。

Niche conservatism and ecological change during the Late Devonian mass extinction.

机构信息

Department of Earth Sciences, University of Connecticut, Storrs, CT 06269, USA.

Earth and Atmospheric Sciences Department, Cornell University, Ithaca, NY 14850, USA.

出版信息

Proc Biol Sci. 2023 Apr 12;290(1996):20222524. doi: 10.1098/rspb.2022.2524. Epub 2023 Apr 5.

Abstract

Studies of the fossil record can inform our understanding of not only the causes of mass extinctions, but also their effects on biodiversity, ecology and evolution. Here, we examine regional-scale ecological changes resulting from a Late Devonian mass extinction event using brachiopod fossil assemblages from the Appalachian Basin. About half of the species went extinct, but were largely replaced by new immigrant taxa. Both before and after the extinction, the primary gradient in faunal composition was correlated with onshore-offshore position, with a second gradient attributed to frequency of disturbance. Survivors of the extinction displayed a strong degree of niche conservatism along these gradients. Despite these indicators of ecological stability, the pre- and post-extinction faunas were quite distinct at the order level, with atrypids and strophomenids largely replaced by productids, whose spiny shells may have provided greater resistance to disturbance and/or predation. Thus, extinction survivors persisted in similar ecological niches despite environmental perturbations and considerable change in the taxonomic and ecological composition of the regional species pool.

摘要

对化石记录的研究不仅可以帮助我们了解大规模灭绝的原因,还可以帮助我们了解其对生物多样性、生态学和进化的影响。在这里,我们利用阿巴拉契亚盆地的腕足动物化石组合,研究了晚泥盆世大灭绝事件所导致的区域尺度的生态变化。大约有一半的物种灭绝了,但它们在很大程度上被新的外来分类群所取代。在灭绝之前和之后,动物群组成的主要梯度与近岸-远岸位置相关,第二个梯度归因于干扰频率。灭绝的幸存者在这些梯度上表现出很强的生态位保守性。尽管存在这些生态稳定性的指标,但灭绝前后的动物群在属级水平上有很大的不同,无洞贝类和石燕贝类主要被具刺壳的有孔虫类所取代,这些具刺壳可能提供了更大的抗干扰和/或捕食能力。因此,尽管环境受到干扰,区域物种库的分类和生态组成发生了很大变化,但灭绝的幸存者仍在相似的生态位中生存。

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A model of onshore-offshore change in faunal diversity.动物多样性海陆变化模型。
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