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十五年来昆虫化石记录的变化

Changes to the Fossil Record of Insects through Fifteen Years of Discovery.

作者信息

Nicholson David B, Mayhew Peter J, Ross Andrew J

机构信息

Department of Biology, University of York, York, United Kingdom; Department of Natural Sciences, National Museum of Scotland, Edinburgh, United Kingdom.

Department of Biology, University of York, York, United Kingdom.

出版信息

PLoS One. 2015 Jul 15;10(7):e0128554. doi: 10.1371/journal.pone.0128554. eCollection 2015.

Abstract

The first and last occurrences of hexapod families in the fossil record are compiled from publications up to end-2009. The major features of these data are compared with those of previous datasets (1993 and 1994). About a third of families (>400) are new to the fossil record since 1994, over half of the earlier, existing families have experienced changes in their known stratigraphic range and only about ten percent have unchanged ranges. Despite these significant additions to knowledge, the broad pattern of described richness through time remains similar, with described richness increasing steadily through geological history and a shift in dominant taxa, from Palaeoptera and Polyneoptera to Paraneoptera and Holometabola, after the Palaeozoic. However, after detrending, described richness is not well correlated with the earlier datasets, indicating significant changes in shorter-term patterns. There is reduced Palaeozoic richness, peaking at a different time, and a less pronounced Permian decline. A pronounced Triassic peak and decline is shown, and the plateau from the mid Early Cretaceous to the end of the period remains, albeit at substantially higher richness compared to earlier datasets. Origination and extinction rates are broadly similar to before, with a broad decline in both through time but episodic peaks, including end-Permian turnover. Origination more consistently exceeds extinction compared to previous datasets and exceptions are mainly in the Palaeozoic. These changes suggest that some inferences about causal mechanisms in insect macroevolution are likely to differ as well.

摘要

六足动物类群在化石记录中的首次和末次出现情况是根据截至2009年底的出版物汇编而成的。这些数据的主要特征与先前数据集(1993年和1994年)的数据特征进行了比较。自1994年以来,约三分之一的类群(超过400个)是化石记录中的新成员,超过一半的早期已存在类群在其已知地层范围上发生了变化,只有约10%的类群范围未变。尽管在知识方面有了这些显著增加,但随时间推移所描述的丰富度的总体模式仍然相似,即随地质历史时间推移所描述的丰富度稳步增加,并且优势类群发生了转变,从古翅类和多新翅类转变为副新翅类和全变态类,这一转变发生在古生代之后。然而,在去除趋势后,所描述的丰富度与早期数据集的相关性不佳,这表明短期模式发生了显著变化。古生代的丰富度有所降低,在不同时间达到峰值,二叠纪的下降也不那么明显。显示出一个明显的三叠纪峰值和下降,并且从早白垩世中期到该时期末的平稳期仍然存在,尽管与早期数据集相比丰富度大幅提高。起源和灭绝速率大致与以前相似,两者都随时间大致下降,但有一些阶段性峰值,包括二叠纪末的更替。与先前数据集相比,起源更持续地超过灭绝,例外情况主要出现在古生代。这些变化表明,关于昆虫宏观进化因果机制的一些推断可能也会有所不同。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/158a/4503423/e345ee0564de/pone.0128554.g001.jpg

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