The multiple chronological techniques applied to the <scp>L</scp>ake <scp>S</scp>uigetsu <scp>SG</scp>06 sediment core, central <scp>J</scp>apan

DOI HANDLE HANDLE Web Site Web Site 被引用文献13件 参考文献25件 オープンアクセス
  • Richard A. Staff
    Research Laboratory for Archaeology and the History of Art (RLAHA) University of Oxford Dyson Perrins Building, South Parks Road Oxford OX1 3QY UK
  • Takeshi Nakagawa
    Department of Geography University of Newcastle Newcastle‐upon‐Tyne NE1 7RU UK
  • Gordon Schlolaut
    Section 5.2: Climate Dynamics and Landscape Evolution German Research Center for Geoscience (GFZ) Telegrafenberg D‐14473 Potsdam Germany
  • Michael H. Marshall
    Institute of Geography and Earth Sciences Aberystwyth University Aberystwyth SY23 3DB UK
  • Achim Brauer
    Section 5.2: Climate Dynamics and Landscape Evolution German Research Center for Geoscience (GFZ) Telegrafenberg D‐14473 Potsdam Germany
  • Henry F. Lamb
    Institute of Geography and Earth Sciences Aberystwyth University Aberystwyth SY23 3DB UK
  • Christopher Bronk Ramsey
    Research Laboratory for Archaeology and the History of Art (RLAHA) University of Oxford Dyson Perrins Building, South Parks Road Oxford OX1 3QY UK
  • Charlotte L. Bryant
    NERC Radiocarbon Facility – Environment (NRCF‐E) Scottish Enterprise Technology Park, Rankine Avenue East Kilbride G75 0QF UK
  • Fiona Brock
    Research Laboratory for Archaeology and the History of Art (RLAHA) University of Oxford Dyson Perrins Building, South Parks Road Oxford OX1 3QY UK
  • Hiroyuki Kitagawa
    Department of Earth and Environmental Sciences Nagoya University Furo‐cho, Chikusa‐ku Nagoya 464‐8601 Japan
  • Johannes van der Plicht
    Department of Isotope Research Energy and Sustainability Research Institute University of Groningen Nijenborgh 4 9747 AG Groningen Netherlands
  • Rebecca L. Payne
    Department of Geography University of Newcastle Newcastle‐upon‐Tyne NE1 7RU UK
  • Victoria C. Smith
    Research Laboratory for Archaeology and the History of Art (RLAHA) University of Oxford Dyson Perrins Building, South Parks Road Oxford OX1 3QY UK
  • Darren F. Mark
    NERC Argon Isotope Facility Scottish Universities Environmental Research Centre Scottish Enterprise Technology Park, Rankine Avenue East Kilbride G75 0QF UK
  • Alison Macleod
    Department of Geography Royal Holloway, University of London Egham TW20 0EX UK
  • Simon P. E. Blockley
    Department of Geography Royal Holloway, University of London Egham TW20 0EX UK
  • Jean‐Luc Schwenninger
    Research Laboratory for Archaeology and the History of Art (RLAHA) University of Oxford Dyson Perrins Building, South Parks Road Oxford OX1 3QY UK
  • Pavel E. Tarasov
    Institute of Geological Sciences Palaeontology, Freie Universität Berlin Malteserstrasse 74‐100, Building D 12249 Berlin Germany
  • Tsuyoshi Haraguchi
    Department of Biology and Geosciences Osaka City University 3‐3‐138 Sugimoto Japan
  • Katsuya Gotanda
    Faculty of Policy Informatics Chiba University of Commerce Chiba 272‐8512 Japan
  • Hitoshi Yonenobu
    College of Education Naruto University of Education Naruto 772‐8502 Japan
  • Yusuke Yokoyama
    Atmosphere and Ocean Research Institute Department of Earth and Planetary Sciences University of Tokyo 5‐1‐5 Kashiwanoha Chiba 277‐8564 Japan

書誌事項

公開日
2012-09-28
資源種別
journal article
権利情報
  • http://onlinelibrary.wiley.com/termsAndConditions#vor
DOI
  • 10.1111/j.1502-3885.2012.00278.x
公開者
Wiley

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説明

<jats:p>The varved sediment of Lake Suigetsu (central <jats:styled-content style="fixed-case">J</jats:styled-content>apan) provides a valuable opportunity to obtain high‐resolution, multi‐proxy palaeoenvironmental data across the last glacial/interglacial cycle. In order to maximize the potential of this archive, a well‐constrained chronology is required. This paper outlines the multiple geochronological techniques being applied – namely varve counting, radiocarbon dating, tephrochronology (including argon–argon dating) and optically stimulated luminescence (<jats:styled-content style="fixed-case">OSL</jats:styled-content>) – and the approaches by which these techniques are being integrated to form a single, coherent, robust chronology. Importantly, we also describe here the linkage of the floating <jats:styled-content style="fixed-case">L</jats:styled-content>ake <jats:styled-content style="fixed-case">S</jats:styled-content>uigetsu (<jats:styled-content style="fixed-case">SG</jats:styled-content>06) varve chronology and the absolute (<jats:styled-content style="fixed-case">I</jats:styled-content>nt<jats:styled-content style="fixed-case">C</jats:styled-content>al09 tree‐ring) time scale, as derived using radiocarbon data from the uppermost (non‐varved) portion of the core. This tie‐point, defined as a distinct (flood) marker horizon in <jats:styled-content style="fixed-case">SG</jats:styled-content>06 (event layer <jats:styled-content style="fixed-case">B</jats:styled-content>‐07–08 at 1397.4 cm composite depth), is thus derived to be 11 255 to 11 222 <jats:styled-content style="fixed-case">I</jats:styled-content>nt<jats:styled-content style="fixed-case">C</jats:styled-content>al09 cal. years <jats:styled-content style="fixed-case">BP</jats:styled-content> (68.2% probability range).</jats:p>

収録刊行物

  • Boreas

    Boreas 42 (2), 259-266, 2012-09-28

    Wiley

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