绿色撒哈拉时期西非季风渗透的研究进展对过去300万年人类进化和分散的影响

J. Larrasoaña
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引用次数: 7

摘要

绿色撒哈拉时期(GSPs)是指今天的撒哈拉因西非季风(WAM)加剧而转变为大草原的时期。虽然GSPs可能极大地改变了非洲和亚洲附近地区人口的规模、结构和连通性,但由于在进化时间尺度上测量WAM在撒哈拉沙漠上的渗透所涉及的问题,它们对人类进化的意义仍然未知。在这里,我重新分析了300万年前东地中海ODP站点967的季风径流和沙尘记录,并将它们与北非古环境数据同化,以证实在gsp期间WAM锋面对纬度超过28°N的渗透。这些结果,再加上现代狩猎采集者的人口统计和生态数据,表明与背景沙漠条件相比,在gsp期间人类人口显著扩大。鉴于在地球轨道离心率的长期最大值附近聚集了GSPs,我提出由GSPs驱动的人类人口扩张的周期性导致了有利突变数量的增加。伴随着有利于触发表观遗传变化的环境因素,这可能导致了表型可塑性增强的增加,从而支持了变异性选择假说所设想的高气候变异性时期人类谱系的物种形成。在上新世/更新世边界附近聚集的gsp,与东非和西奈半岛较长时间的湿润条件同时发生,进一步表明人类在欧亚大陆的初始殖民发生在2.6 Ma左右,比通常认为的要早得多。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
A review of West African monsoon penetration during Green Sahara periods; implications for human evolution and dispersals over the last three million years
Green Sahara periods (GSPs) represent episodes during which the present-day Sahara was transformed into a savannah in response to intensification of the West African monsoon (WAM). Although GSPs might have dramatically altered the size, structure, and connectivity of human populations in Africa and nearby regions of Asia, their significance for human evolution remains unknown due to the problems involved in gauging the penetration of the WAM over the Sahara at evolutionary timescales. Here I reanalyse monsoon run-off and dust records back to 3 million years ago from Eastern Mediterranean ODP Site 967, and assimilate them with North African palaeoenvironmental data to substantiate penetration of the WAM front during GSPs to latitudes beyond 28°N. These results, coupled with demographic and ecological data for modern hunter-gatherers, point to a significant expansion of human populations during GSPs compared with background desert conditions. Given the clustering of GSPs around long-term maxima in the eccentricity of the Earth´s orbit, I propose that recurrent periods of human population expansion driven by GSPs led to an increased number of favourable mutations. Along with environmental factors favourable for triggering epigenetic changes, this might have led to the rise in enhanced phenotypic plasticity that underpins the speciation of hominin lineages at times of high climate variability envisaged by the variability selection hypothesis. Clustering of GSPs around the Pliocene/Pleistocene boundary, simultaneously with a protracted period of wetter conditions in East Africa and the Sinai Peninsula, further suggests that the initial colonization of Eurasia by hominins occurred circa 2.6 Ma, much earlier than typically considered.
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