The deep population history of northern East Asia from the Late Pleistocene to the HoloceneMao et al. demonstrate that the ancestry of the ca. 40 ka individual from Tianyuan Cave near Beijing was widespread geographically and temporally before the Last Glacial Maximum (LGM; ca. 26.5–19 ka). At the end of the LGM, the earliest northern East Asian appeared. After 14 ka, populations in the Amur region comprised the closest East Asian source known for Ancient Paleo-Siberians. Among adaptive genetic variants, EDAR V370A was likely to have been elevated to high frequency after the LGM.Mao et al. demonstrate that the ancestry of the ca. 40 ka individual from Tianyuan Cave near Beijing was widespread geographically and temporally before the Last Glacial Maximum (LGM; ca. 26.5–19 ka). At the end of the LGM, the earliest northern East Asian appeared. After 14 ka, populations in the Amur region comprised the closest East Asian source known for Ancient Paleo-Siberians. Among adaptive genetic variants, EDAR V370A was likely to have been elevated to high frequency after the LGM.Xiaowei Mao, Hucai Zhang, Shiyu Qiao, Yichen Liu, Fengqin Chang, Ping Xie, Ming Zhang, Tianyi Wang, Mian Li, Peng Cao, Ruowei Yang, Feng Liu, Qingyan Dai, Xiaotian Feng, Wanjing Ping, Chuzhao Lei, John W. Olsen, E. Andrew Bennett, Qiaomei Fuhttps://secure.jbs.elsevierhealth.com/action/getSharedSiteSession?redirect=https%3A%2F%2Fwww.cell.com%2Fcell%2Ffulltext%2FS0092-8674%2821%2900575-4%3Frss%3Dyes&rc=0http://www.cell.com/cell/inpress.rssCellCell RSS feed.Wireless News CampaignMay 28, 2021

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