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显生宙化石记录中捕食强度与多样性的强耦合关系。

Strong coupling of predation intensity and diversity in the Phanerozoic fossil record.

作者信息

Huntley John Warren, Kowalewski Michal

机构信息

Department of Geosciences, Virginia Polytechnic Institute and State University, Blacksburg, VA 24061, USA.

出版信息

Proc Natl Acad Sci U S A. 2007 Sep 18;104(38):15006-10. doi: 10.1073/pnas.0704960104. Epub 2007 Sep 12.

Abstract

The importance of ecological interactions in driving the evolution of animals has been the focus of intense debate among paleontologists, evolutionary biologists, and macroecologists. To test whether the intensity of such interactions covaries with the secular evolutionary trend in global biodiversity, we compiled a species-level database of predation intensity, as measured by the frequency of common predation traces (drillings and repair scars ranging in age from Ediacaran to Holocene). The results indicate that the frequency of predation traces increased notably by the Ordovician, and not in the mid-Paleozoic as suggested by multiple previous studies. Importantly, these estimates of predation intensity and global diversity of marine metazoans correlate throughout the Phanerozoic fossil record regardless of corrections and methods applied. This concordance may represent (i) an ecological signal: long-term coupling of diversity and predation; (ii) a diversity-driven diffusion of predatory behaviors: an increased probability of more complex predatory strategies to appear at higher diversity levels; or (iii) a spurious concordance in signal capture: an artifact where rare species and less-frequent (e.g., trace-producing) predatory behaviors are both more detectable at times when sampling improves. The coupling of predation and diversity records suggests that macroevolutionary and macroecological patterns share common causative mechanisms that may reflect either historical processes or sampling artifacts.

摘要

生态相互作用在推动动物进化过程中的重要性一直是古生物学家、进化生物学家和宏观生态学家激烈争论的焦点。为了检验这种相互作用的强度是否与全球生物多样性的长期进化趋势相关,我们编制了一个物种水平的捕食强度数据库,该强度通过常见捕食痕迹(钻孔和修复疤痕,年龄范围从埃迪卡拉纪到全新世)的频率来衡量。结果表明,捕食痕迹的频率在奥陶纪显著增加,而不是如之前多项研究所表明的在古生代中期增加。重要的是,在整个显生宙化石记录中,这些对海洋后生动物捕食强度和全球多样性的估计无论采用何种校正和方法都相互关联。这种一致性可能代表:(i)一种生态信号:多样性与捕食的长期耦合;(ii)由多样性驱动的捕食行为扩散:在更高的多样性水平出现更复杂捕食策略的可能性增加;或者(iii)信号捕获中的虚假一致性:一种假象,即在采样改善时,稀有物种和不太频繁(如产生痕迹的)捕食行为都更易被检测到。捕食与多样性记录的耦合表明,宏观进化和宏观生态模式共享共同的因果机制,这可能反映历史过程或采样假象。

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本文引用的文献

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Taxonomic Diversity during the Phanerozoic.显生宙时期的分类多样性。
Science. 1972 Sep 22;177(4054):1065-71. doi: 10.1126/science.177.4054.1065.
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Geologic constraints on the macroevolutionary history of marine animals.海洋动物宏观进化历史的地质限制因素。
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