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绿色撒哈拉时期的动态及其在人类进化中的作用。

Dynamics of green Sahara periods and their role in hominin evolution.

机构信息

Instituto Geológico y Minero de España, Unidad de Zaragoza, Zaragoza, Spain ; Research School of Earth Sciences, The Australian National University, Canberra, Australia.

出版信息

PLoS One. 2013 Oct 16;8(10):e76514. doi: 10.1371/journal.pone.0076514. eCollection 2013.

Abstract

Astronomically forced insolation changes have driven monsoon dynamics and recurrent humid episodes in North Africa, resulting in green Sahara Periods (GSPs) with savannah expansion throughout most of the desert. Despite their potential for expanding the area of prime hominin habitats and favouring out-of-Africa dispersals, GSPs have not been incorporated into the narrative of hominin evolution due to poor knowledge of their timing, dynamics and landscape composition at evolutionary timescales. We present a compilation of continental and marine paleoenvironmental records from within and around North Africa, which enables identification of over 230 GSPs within the last 8 million years. By combining the main climatological determinants of woody cover in tropical Africa with paleoenvironmental and paleoclimatic data for representative (Holocene and Eemian) GSPs, we estimate precipitation regimes and habitat distributions during GSPs. Their chronology is consistent with the ages of Saharan archeological and fossil hominin sites. Each GSP took 2-3 kyr to develop, peaked over 4-8 kyr, biogeographically connected the African tropics to African and Eurasian mid latitudes, and ended within 2-3 kyr, which resulted in rapid habitat fragmentation. We argue that the well-dated succession of GSPs presented here may have played an important role in migration and evolution of hominins.

摘要

天文强迫的太阳辐射变化驱动了北非季风动态和反复出现的湿润事件,导致撒哈拉绿色时期(GSP)出现,整个沙漠地区的热带稀树草原扩张。尽管它们有潜力扩大原始人类栖息地的面积,并有利于走出非洲的扩散,但由于对 GSP 时间、动态和景观组成在进化时间尺度上的了解有限,它们并未被纳入人类进化的叙述中。我们展示了来自北非内部和周围的大陆和海洋古环境记录的汇编,这些记录使我们能够在过去 800 万年中确定 230 多个 GSP。通过将非洲热带木本覆盖物的主要气候决定因素与代表(全新世和 Eemian)GSP 的古环境和古气候数据相结合,我们估计了 GSP 期间的降水模式和栖息地分布。它们的年代与撒哈拉考古和化石人类遗址的年代一致。每个 GSP 的发展需要 2-3 千年,达到峰值需要 4-8 千年,将非洲热带地区与非洲和欧亚大陆中纬度地区在生物地理上连接起来,并在 2-3 千年内结束,导致栖息地迅速破碎化。我们认为,这里提出的 GSP 的良好定年序列可能在人类的迁移和进化中发挥了重要作用。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/b409/3797788/26e6b3c66edd/pone.0076514.g001.jpg

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