Ancient DNA and multimethod dating confirm the late arrival of anatomically modern humans in southern China
The expansion of anatomically modern humans (AMHs) from Africa around 65,000 to 45,000 y ago (ca. 65 to 45 ka) led to the establishment of present-day non-African populations. Some paleoanthropologists have argued that fossil discoveries from Huanglong, Zhiren, Luna, and Fuyan caves in southern Chin...
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creator | Sun, Xue-feng Wen, Shao-qing Lu, Cheng-qiu Zhou, Bo-yan Curnoe, Darren Lu, Hua-yu Li, Hong-chun Wang, Wei Cheng, Hai Yi, Shuang-wen Jia, Xin Du, Pan-xin Xu, Xing-hua Lu, Yi-ming Lu, Ying Zhang, Hong Sun, Chang Wei, Lan-hai Han, Fei Huang, Juan Edwards, R. Lawrence Jin, Li Li, Hui 李辉 |
description | The expansion of anatomically modern humans (AMHs) from Africa around 65,000 to 45,000 y ago (ca. 65 to 45 ka) led to the establishment of present-day non-African populations. Some paleoanthropologists have argued that fossil discoveries from Huanglong, Zhiren, Luna, and Fuyan caves in southern China indicate one or more prior dispersals, perhaps as early as ca. 120 ka. We investigated the age of the human remains from three of these localities and two additional early AMH sites (Yangjiapo and Sanyou caves, Hubei) by combining ancient DNA (aDNA) analysis with a multimethod geological dating strategy. Although U–Th dating of capping flowstones suggested they lie within the range ca. 168 to 70 ka, analyses of aDNA and direct AMS 14C dating on human teeth from Fuyan and Yangjiapo caves showed they derive from the Holocene. OSL dating of sediments and AMS 14C analysis of mammal teeth and charcoal also demonstrated major discrepancies from the flowstone ages; the difference between them being an order of magnitude or more at most of these localities. Our work highlights the surprisingly complex depositional history recorded at these subtropical caves which involved one or more episodes of erosion and redeposition or intrusion as recently as the late Holocene. In light of our findings, the first appearance datum for AMHs in southern China should probably lie within the timeframe set by molecular data of ca. 50 to 45 ka. |
doi_str_mv | 10.1073/pnas.2019158118 |
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Lawrence ; Jin, Li ; Li, Hui ; 李辉</creator><creatorcontrib>Sun, Xue-feng ; Wen, Shao-qing ; Lu, Cheng-qiu ; Zhou, Bo-yan ; Curnoe, Darren ; Lu, Hua-yu ; Li, Hong-chun ; Wang, Wei ; Cheng, Hai ; Yi, Shuang-wen ; Jia, Xin ; Du, Pan-xin ; Xu, Xing-hua ; Lu, Yi-ming ; Lu, Ying ; Zhang, Hong ; Sun, Chang ; Wei, Lan-hai ; Han, Fei ; Huang, Juan ; Edwards, R. Lawrence ; Jin, Li ; Li, Hui ; 李辉</creatorcontrib><description>The expansion of anatomically modern humans (AMHs) from Africa around 65,000 to 45,000 y ago (ca. 65 to 45 ka) led to the establishment of present-day non-African populations. Some paleoanthropologists have argued that fossil discoveries from Huanglong, Zhiren, Luna, and Fuyan caves in southern China indicate one or more prior dispersals, perhaps as early as ca. 120 ka. We investigated the age of the human remains from three of these localities and two additional early AMH sites (Yangjiapo and Sanyou caves, Hubei) by combining ancient DNA (aDNA) analysis with a multimethod geological dating strategy. Although U–Th dating of capping flowstones suggested they lie within the range ca. 168 to 70 ka, analyses of aDNA and direct AMS 14C dating on human teeth from Fuyan and Yangjiapo caves showed they derive from the Holocene. OSL dating of sediments and AMS 14C analysis of mammal teeth and charcoal also demonstrated major discrepancies from the flowstone ages; the difference between them being an order of magnitude or more at most of these localities. Our work highlights the surprisingly complex depositional history recorded at these subtropical caves which involved one or more episodes of erosion and redeposition or intrusion as recently as the late Holocene. In light of our findings, the first appearance datum for AMHs in southern China should probably lie within the timeframe set by molecular data of ca. 50 to 45 ka.</description><identifier>ISSN: 0027-8424</identifier><identifier>EISSN: 1091-6490</identifier><identifier>DOI: 10.1073/pnas.2019158118</identifier><identifier>PMID: 33558418</identifier><language>eng</language><publisher>United States: National Academy of Sciences</publisher><subject>Biological Sciences ; Caves ; Charcoal ; Dating ; Deoxyribonucleic acid ; DNA ; Holocene ; Hominids ; Sediments ; Social Sciences</subject><ispartof>Proceedings of the National Academy of Sciences - PNAS, 2021-02, Vol.118 (8), p.1-10</ispartof><rights>Copyright National Academy of Sciences Feb 23, 2021</rights><rights>2021</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a532t-6c1be913b3a27d7cc286592cb07207e0a2a54e398fbcf8383038c2e99b7bf4113</citedby><cites>FETCH-LOGICAL-a532t-6c1be913b3a27d7cc286592cb07207e0a2a54e398fbcf8383038c2e99b7bf4113</cites><orcidid>0000-0001-8622-4141 ; 0000-0002-6306-6985 ; 0000-0003-1223-4720 ; 0000-0001-9614-7119 ; 0000-0002-5305-9458 ; 0000-0002-2688-4663 ; 0000-0003-4690-0621 ; 0000-0002-5804-8563</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://www.jstor.org/stable/pdf/27006333$$EPDF$$P50$$Gjstor$$H</linktopdf><linktohtml>$$Uhttps://www.jstor.org/stable/27006333$$EHTML$$P50$$Gjstor$$H</linktohtml><link.rule.ids>230,314,723,776,780,799,881,27901,27902,53766,53768,57992,58225</link.rule.ids><backlink>$$Uhttps://www.ncbi.nlm.nih.gov/pubmed/33558418$$D View this record in MEDLINE/PubMed$$Hfree_for_read</backlink></links><search><creatorcontrib>Sun, Xue-feng</creatorcontrib><creatorcontrib>Wen, Shao-qing</creatorcontrib><creatorcontrib>Lu, Cheng-qiu</creatorcontrib><creatorcontrib>Zhou, Bo-yan</creatorcontrib><creatorcontrib>Curnoe, Darren</creatorcontrib><creatorcontrib>Lu, Hua-yu</creatorcontrib><creatorcontrib>Li, Hong-chun</creatorcontrib><creatorcontrib>Wang, Wei</creatorcontrib><creatorcontrib>Cheng, Hai</creatorcontrib><creatorcontrib>Yi, Shuang-wen</creatorcontrib><creatorcontrib>Jia, Xin</creatorcontrib><creatorcontrib>Du, Pan-xin</creatorcontrib><creatorcontrib>Xu, Xing-hua</creatorcontrib><creatorcontrib>Lu, Yi-ming</creatorcontrib><creatorcontrib>Lu, Ying</creatorcontrib><creatorcontrib>Zhang, Hong</creatorcontrib><creatorcontrib>Sun, Chang</creatorcontrib><creatorcontrib>Wei, Lan-hai</creatorcontrib><creatorcontrib>Han, Fei</creatorcontrib><creatorcontrib>Huang, Juan</creatorcontrib><creatorcontrib>Edwards, R. Lawrence</creatorcontrib><creatorcontrib>Jin, Li</creatorcontrib><creatorcontrib>Li, Hui</creatorcontrib><creatorcontrib>李辉</creatorcontrib><title>Ancient DNA and multimethod dating confirm the late arrival of anatomically modern humans in southern China</title><title>Proceedings of the National Academy of Sciences - PNAS</title><addtitle>Proc Natl Acad Sci U S A</addtitle><description>The expansion of anatomically modern humans (AMHs) from Africa around 65,000 to 45,000 y ago (ca. 65 to 45 ka) led to the establishment of present-day non-African populations. Some paleoanthropologists have argued that fossil discoveries from Huanglong, Zhiren, Luna, and Fuyan caves in southern China indicate one or more prior dispersals, perhaps as early as ca. 120 ka. We investigated the age of the human remains from three of these localities and two additional early AMH sites (Yangjiapo and Sanyou caves, Hubei) by combining ancient DNA (aDNA) analysis with a multimethod geological dating strategy. Although U–Th dating of capping flowstones suggested they lie within the range ca. 168 to 70 ka, analyses of aDNA and direct AMS 14C dating on human teeth from Fuyan and Yangjiapo caves showed they derive from the Holocene. OSL dating of sediments and AMS 14C analysis of mammal teeth and charcoal also demonstrated major discrepancies from the flowstone ages; the difference between them being an order of magnitude or more at most of these localities. Our work highlights the surprisingly complex depositional history recorded at these subtropical caves which involved one or more episodes of erosion and redeposition or intrusion as recently as the late Holocene. In light of our findings, the first appearance datum for AMHs in southern China should probably lie within the timeframe set by molecular data of ca. 50 to 45 ka.</description><subject>Biological Sciences</subject><subject>Caves</subject><subject>Charcoal</subject><subject>Dating</subject><subject>Deoxyribonucleic acid</subject><subject>DNA</subject><subject>Holocene</subject><subject>Hominids</subject><subject>Sediments</subject><subject>Social Sciences</subject><issn>0027-8424</issn><issn>1091-6490</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2021</creationdate><recordtype>article</recordtype><recordid>eNpdkc1v3CAQxVHVqtlue-6pFVIuvTgZwDZwqbTafkpRc0nPCGMcs7VhCzhS_vuw2nTblMtIzO-N5s1D6C2BCwKcXe69ThcUiCSNIEQ8QysCklRtLeE5WgFQXoma1mfoVUo7AJCNgJfojLGmETURK_Rr442zPuNPPzZY-x7Py5TdbPMYetzr7PwtNsEPLs44jxZPOlusY3R3esJhKBKdw-yMnqZ7PIfeRo_HZdY-YedxCksRla_t6Lx-jV4Mekr2zWNdo59fPt9sv1VX11-_bzdXlW4YzVVrSGclYR3TlPfcGCraRlLTAafALWiqm9oyKYbODIIJBkwYaqXseDfUhLA1-nicu1-62fam2It6UvvoZh3vVdBOPe14N6rbcKe4pKwtZ12jD48DYvi92JTV7JKx06S9DUtStBacN0BqWdDz_9BdWKIv9g6UAMZIzQp1eaRMDClFO5yWIaAOQapDkOpvkEXx_l8PJ_5PcgV4dwR2KYd46lMO0LLyHgDu1qSB</recordid><startdate>20210223</startdate><enddate>20210223</enddate><creator>Sun, Xue-feng</creator><creator>Wen, Shao-qing</creator><creator>Lu, Cheng-qiu</creator><creator>Zhou, Bo-yan</creator><creator>Curnoe, Darren</creator><creator>Lu, Hua-yu</creator><creator>Li, Hong-chun</creator><creator>Wang, Wei</creator><creator>Cheng, Hai</creator><creator>Yi, Shuang-wen</creator><creator>Jia, Xin</creator><creator>Du, Pan-xin</creator><creator>Xu, Xing-hua</creator><creator>Lu, Yi-ming</creator><creator>Lu, Ying</creator><creator>Zhang, Hong</creator><creator>Sun, Chang</creator><creator>Wei, Lan-hai</creator><creator>Han, Fei</creator><creator>Huang, Juan</creator><creator>Edwards, R. 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Lawrence</au><au>Jin, Li</au><au>Li, Hui</au><au>李辉</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Ancient DNA and multimethod dating confirm the late arrival of anatomically modern humans in southern China</atitle><jtitle>Proceedings of the National Academy of Sciences - PNAS</jtitle><addtitle>Proc Natl Acad Sci U S A</addtitle><date>2021-02-23</date><risdate>2021</risdate><volume>118</volume><issue>8</issue><spage>1</spage><epage>10</epage><pages>1-10</pages><issn>0027-8424</issn><eissn>1091-6490</eissn><abstract>The expansion of anatomically modern humans (AMHs) from Africa around 65,000 to 45,000 y ago (ca. 65 to 45 ka) led to the establishment of present-day non-African populations. Some paleoanthropologists have argued that fossil discoveries from Huanglong, Zhiren, Luna, and Fuyan caves in southern China indicate one or more prior dispersals, perhaps as early as ca. 120 ka. We investigated the age of the human remains from three of these localities and two additional early AMH sites (Yangjiapo and Sanyou caves, Hubei) by combining ancient DNA (aDNA) analysis with a multimethod geological dating strategy. Although U–Th dating of capping flowstones suggested they lie within the range ca. 168 to 70 ka, analyses of aDNA and direct AMS 14C dating on human teeth from Fuyan and Yangjiapo caves showed they derive from the Holocene. OSL dating of sediments and AMS 14C analysis of mammal teeth and charcoal also demonstrated major discrepancies from the flowstone ages; the difference between them being an order of magnitude or more at most of these localities. Our work highlights the surprisingly complex depositional history recorded at these subtropical caves which involved one or more episodes of erosion and redeposition or intrusion as recently as the late Holocene. In light of our findings, the first appearance datum for AMHs in southern China should probably lie within the timeframe set by molecular data of ca. 50 to 45 ka.</abstract><cop>United States</cop><pub>National Academy of Sciences</pub><pmid>33558418</pmid><doi>10.1073/pnas.2019158118</doi><tpages>10</tpages><orcidid>https://orcid.org/0000-0001-8622-4141</orcidid><orcidid>https://orcid.org/0000-0002-6306-6985</orcidid><orcidid>https://orcid.org/0000-0003-1223-4720</orcidid><orcidid>https://orcid.org/0000-0001-9614-7119</orcidid><orcidid>https://orcid.org/0000-0002-5305-9458</orcidid><orcidid>https://orcid.org/0000-0002-2688-4663</orcidid><orcidid>https://orcid.org/0000-0003-4690-0621</orcidid><orcidid>https://orcid.org/0000-0002-5804-8563</orcidid><oa>free_for_read</oa></addata></record> |
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subjects | Biological Sciences Caves Charcoal Dating Deoxyribonucleic acid DNA Holocene Hominids Sediments Social Sciences |
title | Ancient DNA and multimethod dating confirm the late arrival of anatomically modern humans in southern China |
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