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首页> 外文期刊>Australian Journal of Earth Sciences >Faunal diversity, heterogeneity and body size in the Early Triassic: testing post-extinction paradigms in the Virgin Limestone of Utah, USA
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Faunal diversity, heterogeneity and body size in the Early Triassic: testing post-extinction paradigms in the Virgin Limestone of Utah, USA

机译:三叠纪早期的动物多样性,异质性和体型:在美国犹他州的维尔京石灰石中测试灭绝后的范式

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The recovery intervals after mass extinction events are portrayed as times of ecological stress, with effects including reduced body size (Lilliput Effect), reduced taxonomic diversity and lowered ecological complexity. As the end-Permian mass extinction is the largest of the ‘Big Five’ events, with a prolonged recovery interval postulated during the Early Triassic, we expect these effects to be most pronounced in Early Triassic faunas. We have used new data and analytical techniques on the fauna of the Spathian Virgin Limestone to test whether the Lilliput Effect can be observed, whether the fauna is vertically and laterally homogeneous, and whether taxonomic diversity is significantly lower than that of comparable nearshore marine deposits transgressive over redbed sequences from other deposits not regarded as falling into post-extinction recovery intervals. The Lilliput Effect can be observed in some cases, but no uniform trend in body size reduction emerged. When the distributions of the body size across a range of marine invertebrate taxa was compared between the Virgin Limestone and the latest Triassic Penarth Group of Britain there was no support for a significant reduction in body size among the Virgin Limestone fauna. Evidence for faunal homogeneity was also limited. The alpha diversity of individual sites in the Middle Triassic Muschelkalk of central Europe was generally higher than Virgin Limestone sites, after accounting for differences in sample size using rarefaction, but there was some overlap. Although the beta diversity of the Muschelkalk is also apparently higher, a number of biases may be elevating Muschelkalk diversity. Future comparisons between recovery and ‘normal’ faunas need to ensure that as many confounding factors as possible are controlled for and that multiple samples are tested.
机译:物种灭绝事件后的恢复间隔被描述为生态压力的时间,其影响包括减小体型(小人称效应),减少分类学多样性和降低生态复杂性。由于二叠纪末期大灭绝是“五巨头”事件中最大的一次,并且在三叠纪早期被假定恢复期延长,因此我们预计这些影响在三叠纪早期动物群中最为明显。我们已经使用新的资料和分析技术来分析Spathian初生石灰岩的动物群,是否可以观察到小轮效应,该动物群在纵向和横向上是否均一,以及分类学多样性是否明显低于海侵性海相沉积物的可比性。在其他沉积物的红床序列上不被认为属于灭绝后的恢复间隔。在某些情况下可以观察到小轮效应,但没有出现统一的减小身材的趋势。在比较维尔京石灰石和英国最新的三叠纪Penarth群的一系列海洋无脊椎动物类群的体型分布时,没有支持大幅减少维尔京石灰石动物群的体型的支持。动物同质性的证据也很有限。考虑到使用稀有度的样本量差异后,中欧中三叠世Muschelkalk各个地点的alpha多样性通常高于处女石灰石地点,但存在一些重叠。尽管Muschelkalk的beta多样性也明显更高,但许多偏见可能会提高Muschelkalk的多样性。恢复和“正常”动物区系之间的未来比较需要确保控制尽可能多的混杂因素,并测试多个样本。

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