Lake Sediments High-resolution Recorder of Environmental Changes. Organic Carbon Accumulation Rate During the Last 8,000 Years in Lake Nakaumi, Southwest Japan: Coastal Lagoon Sediments as Carbon Sink.

  • Sampei Yoshikazu
    Department of Geoscience, Faculty of Science and Engineering, Shimane University
  • Matsumoto Eiji
    Institute for Hydrospheric-Atmospheric Sciences, Nagoya University
  • Tokuoka Takao
    Department of Geoscience, Faculty of Science and Engineering, Shimane University
  • Inoue Daiei
    Abiko Research Laboratory CRIEPI

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Other Title
  • 湖沼堆積物 地球環境変動の“高精度検出計” (その1) 中海における過去8,000年間の有機炭素埋積速度 Carbon Sinkとしての汽水域堆積物
  • ナカウミ ニ オケル カコ 8 000ネンカン ノ ユウキ タンソ マイセキ
  • Coastal Lagoon Sediments as Carbon Sink
  • Carbon sinkとしての汽水域堆積物

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Abstract

The organic carbon (Corg.) accumulation rate and its relation to climate change during the last 8, 000 years as recorded in the sediment core from the semi-closed coastal lagoon Lake Nakaumi were reconstructed. High-resolution downcore profiles of 14C by fifteen shells enabled us to conclude that the Corg. accumulation rate in a warming climate (7, 000-7, 500cal yrs BP; Calendar age) was about two times higher than that in a cooling climate (2, 500-3, 000cal yrs BP). The coastal lagoon could provide a small negative feedback on global warming and an effective small sink (ca. 0.01 GtC yr-1) for atmospheric CO2.

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