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Denisovan DNA in Late Pleistocene sediments from Baishiya Karst Cave on the Tibetan Plateau

A late Middle Pleistocene mandible from Baishiya Karst Cave (BKC) on the Tibetan Plateau has been inferred to be from a Denisovan, an Asian hominin related to Neanderthals, on the basis of an amino acid substitution in its collagen. Here we describe the stratigraphy, chronology, and mitochondrial DN...

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Published in:Science (American Association for the Advancement of Science) 2020-10, Vol.370 (6516), p.584-587
Main Authors: Zhang, Dongju, Xia, Huan, Chen, Fahu, Li, Bo, Slon, Viviane, Cheng, Ting, Yang, Ruowei, Jacobs, Zenobia, Dai, Qingyan, Massilani, Diyendo, Shen, Xuke, Wang, Jian, Feng, Xiaotian, Cao, Peng, Yang, Melinda A, Yao, Juanting, Yang, Jishuai, Madsen, David B, Han, Yuanyuan, Ping, Wanjing, Liu, Feng, Perreault, Charles, Chen, Xiaoshan, Meyer, Matthias, Kelso, Janet, Pääbo, Svante, Fu, Qiaomei
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Language:English
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Summary:A late Middle Pleistocene mandible from Baishiya Karst Cave (BKC) on the Tibetan Plateau has been inferred to be from a Denisovan, an Asian hominin related to Neanderthals, on the basis of an amino acid substitution in its collagen. Here we describe the stratigraphy, chronology, and mitochondrial DNA extracted from the sediments in BKC. We recover Denisovan mitochondrial DNA from sediments deposited ~100 thousand and ~60 thousand years ago (ka) and possibly as recently as ~45 ka. The long-term occupation of BKC by Denisovans suggests that they may have adapted to life at high altitudes and may have contributed such adaptations to modern humans on the Tibetan Plateau.
ISSN:0036-8075
1095-9203
DOI:10.1126/science.abb6320