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史前人类在巽他陆块和南亚之间的迁移是由海平面上升驱动的。

Prehistoric human migration between Sundaland and South Asia was driven by sea-level rise.

机构信息

Asian School of the Environment, Nanyang Technological University, 50 Nanyang Avenue, N2-01c-63, 639798, Singapore, Singapore.

Singapore Centre for Environmental Life Sciences Engineering, Nanyang Technological University, 60 Nanyang Drive, SBS-01n-27, 637551, Singapore, Singapore.

出版信息

Commun Biol. 2023 Feb 4;6(1):150. doi: 10.1038/s42003-023-04510-0.

Abstract

Rapid sea-level rise between the Last Glacial Maximum (LGM) and the mid-Holocene transformed the Southeast Asian coastal landscape, but the impact on human demography remains unclear. Here, we create a paleogeographic map, focusing on sea-level changes during the period spanning the LGM to the present-day and infer the human population history in Southeast and South Asia using 763 high-coverage whole-genome sequencing datasets from 59 ethnic groups. We show that sea-level rise, in particular meltwater pulses 1 A (MWP1A, ~14,500-14,000 years ago) and 1B (MWP1B, ~11,500-11,000 years ago), reduced land area by over 50% since the LGM, resulting in segregation of local human populations. Following periods of rapid sea-level rises, population pressure drove the migration of Malaysian Negritos into South Asia. Integrated paleogeographic and population genomic analysis demonstrates the earliest documented instance of forced human migration driven by sea-level rise.

摘要

末次冰期最大值(LGM)和全新世中期之间的海平面快速上升改变了东南亚沿海景观,但对人类人口结构的影响仍不清楚。在这里,我们创建了一幅古地理图,重点关注 LGM 到现在期间的海平面变化,并使用来自 59 个族群的 763 个高覆盖率全基因组测序数据集来推断东南亚和南亚的人口历史。我们表明,海平面上升,特别是融水脉冲 1A(MWP1A,约 14500-14000 年前)和 1B(MWP1B,约 11500-11000 年前),导致自 LGM 以来陆地面积减少了 50%以上,导致当地人口隔离。在快速海平面上升之后,人口压力促使马来西亚尼格利陀人迁移到南亚。综合古地理和人口基因组分析证明了由海平面上升驱动的最早有记录的强迫人类迁移实例。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/2d36/9899273/1f290aed2b83/42003_2023_4510_Fig1_HTML.jpg

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