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更新世晚期气候变化与解剖学意义上的现代人的全球扩张。

Late Pleistocene climate change and the global expansion of anatomically modern humans.

机构信息

Department of Zoology, University of Cambridge, Cambridge CB2 3EJ, England.

出版信息

Proc Natl Acad Sci U S A. 2012 Oct 2;109(40):16089-94. doi: 10.1073/pnas.1209494109. Epub 2012 Sep 17.

Abstract

The extent to which past climate change has dictated the pattern and timing of the out-of-Africa expansion by anatomically modern humans is currently unclear [Stewart JR, Stringer CB (2012) Science 335:1317-1321]. In particular, the incompleteness of the fossil record makes it difficult to quantify the effect of climate. Here, we take a different approach to this problem; rather than relying on the appearance of fossils or archaeological evidence to determine arrival times in different parts of the world, we use patterns of genetic variation in modern human populations to determine the plausibility of past demographic parameters. We develop a spatially explicit model of the expansion of anatomically modern humans and use climate reconstructions over the past 120 ky based on the Hadley Centre global climate model HadCM3 to quantify the possible effects of climate on human demography. The combinations of demographic parameters compatible with the current genetic makeup of worldwide populations indicate a clear effect of climate on past population densities. Our estimates of this effect, based on population genetics, capture the observed relationship between current climate and population density in modern hunter-gatherers worldwide, providing supporting evidence for the realism of our approach. Furthermore, although we did not use any archaeological and anthropological data to inform the model, the arrival times in different continents predicted by our model are also broadly consistent with the fossil and archaeological records. Our framework provides the most accurate spatiotemporal reconstruction of human demographic history available at present and will allow for a greater integration of genetic and archaeological evidence.

摘要

过去的气候变化在何种程度上决定了现代人类走出非洲的模式和时间,目前还不清楚[Stewart JR, Stringer CB(2012)Science 335:1317-1321]。特别是,化石记录的不完整使得很难量化气候的影响。在这里,我们采用了一种不同的方法来解决这个问题;我们不是依靠化石或考古证据的出现来确定在世界不同地区的到达时间,而是利用现代人类群体中的遗传变异模式来确定过去人口参数的合理性。我们开发了一个明确的解剖学上的现代人类扩张的空间模型,并使用过去 12 万年的气候重建基于 Hadley 中心全球气候模型 HadCM3 来量化气候对人类人口统计学的可能影响。与世界范围内人口的当前遗传构成相容的人口参数组合表明气候对过去人口密度有明显影响。我们基于群体遗传学对这种影响的估计,捕捉了现代狩猎采集者中当前气候与人口密度之间的观察到的关系,为我们方法的现实性提供了支持证据。此外,尽管我们没有使用任何考古学和人类学数据来为模型提供信息,但我们的模型预测的不同大陆的到达时间也与化石和考古记录大致一致。我们的框架提供了目前可用的最准确的人类人口历史时空重建,将允许遗传和考古证据更好地整合。

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