Department of Anthropology, University of California, 95616, Davis, USA.
Department of Human Evolution, Max-Planck Institute for Evolutionary Anthropology, 04103, Leipzig, Germany.
Sci Rep. 2019 Aug 13;9(1):11759. doi: 10.1038/s41598-019-47972-1.
The fossil record suggests that at least two major human dispersals occurred across the Eurasian steppe during the Late Pleistocene. Neanderthals and Modern Humans moved eastward into Central Asia, a region intermittently occupied by the enigmatic Denisovans. Genetic data indicates that the Denisovans interbred with Neanderthals near the Altai Mountains (South Siberia) but where and when they met H. sapiens is yet to be determined. Here we present archaeological evidence that document the timing and environmental context of a third long-distance population movement in Central Asia, during a temperate climatic event around 45,000 years ago. The early occurrence of the Initial Upper Palaeolithic, a techno-complex whose sudden appearance coincides with the first occurrence of H. sapiens in the Eurasian steppes, establishes an essential archaeological link between the Siberian Altai and Northwestern China . Such connection between regions provides empirical ground to discuss contacts between local and exogenous populations in Central and Northeast Asia during the Late Pleistocene.
化石记录表明,在晚更新世期间,至少有两次人类大规模迁徙跨越了欧亚大草原。尼安德特人和现代人向东迁移到中亚地区,该地区曾间歇性地被神秘的丹尼索瓦人占据。遗传数据表明,丹尼索瓦人与尼安德特人在阿尔泰山脉(南西伯利亚)附近杂交,但他们何时何地与智人相遇仍有待确定。在这里,我们提供了考古证据,记录了大约 45000 年前一个温带气候事件期间中亚地区的第三次长途人口迁移的时间和环境背景。初始上层旧石器时代的早期出现,这一技术综合体的突然出现与智人在欧亚大草原上的首次出现相吻合,在西伯利亚阿尔泰山脉和中国西北地区之间建立了一个重要的考古联系。这些地区之间的联系为讨论晚更新世期间中亚和东北亚地区本地和外来人口之间的接触提供了经验基础。