Atmospheric <sup>14</sup> C/ <sup>12</sup> C changes during the last glacial period from Hulu Cave

  • Hai Cheng
    Institute of Global Environmental Change, Xi’an Jiaotong University, China.
  • R. Lawrence Edwards
    Department of Earth Sciences, University of Minnesota, Minneapolis, MN, USA.
  • John Southon
    Department of Earth System Science, University of California, Irvine, CA, USA.
  • Katsumi Matsumoto
    Department of Earth Sciences, University of Minnesota, Minneapolis, MN, USA.
  • Joshua M. Feinberg
    Department of Earth Sciences, University of Minnesota, Minneapolis, MN, USA.
  • Ashish Sinha
    Department of Earth Science, California State University Dominguez Hills, Carson, CA, USA.
  • Weijian Zhou
    Institute of Earth Environment, Chinese Academy of Sciences, Xi’an, China.
  • Hanying Li
    Institute of Global Environmental Change, Xi’an Jiaotong University, China.
  • Xianglei Li
    Institute of Global Environmental Change, Xi’an Jiaotong University, China.
  • Yao Xu
    Institute of Global Environmental Change, Xi’an Jiaotong University, China.
  • Shitao Chen
    College of Geography Science, Nanjing Normal University, Nanjing, China.
  • Ming Tan
    Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing, China.
  • Quan Wang
    College of Geography Science, Nanjing Normal University, Nanjing, China.
  • Yongjin Wang
    College of Geography Science, Nanjing Normal University, Nanjing, China.
  • Youfeng Ning
    Institute of Global Environmental Change, Xi’an Jiaotong University, China.

書誌事項

公開日
2018-12-14
DOI
  • 10.1126/science.aau0747
公開者
American Association for the Advancement of Science (AAAS)

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説明

<jats:title>The whole story</jats:title> <jats:p> An accurate, precise record of the carbon-14 ( <jats:sup>14</jats:sup> C) content of the atmosphere is important for developing chronologies in climate change, archaeology, and many other disciplines. Cheng <jats:italic>et al.</jats:italic> provide a record that covers the full range of the <jats:sup>14</jats:sup> C dating method (∼54,000 years), using paired measurements of <jats:sup>14</jats:sup> C/ <jats:sup>12</jats:sup> C and thorium-230 ( <jats:sup>230</jats:sup> Th) ages from two stalagmites from Hulu Cave, China. The advantage of matching absolute <jats:sup>230</jats:sup> Th ages and <jats:sup>14</jats:sup> C/ <jats:sup>12</jats:sup> C allowed the authors to fashion a seamless record from a single source with low uncertainties, particularly in the older sections. </jats:p> <jats:p> <jats:italic>Science</jats:italic> , this issue p. <jats:related-article xmlns:xlink="http://www.w3.org/1999/xlink" ext-link-type="doi" issue="6420" page="1293" related-article-type="in-this-issue" vol="362" xlink:href="10.1126/science.aau0747">1293</jats:related-article> </jats:p>

収録刊行物

  • Science

    Science 362 (6420), 1293-1297, 2018-12-14

    American Association for the Advancement of Science (AAAS)

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