琉球海溝斜面から得られたピストン・コアの解析に基づく,過去6万年間にわたる海洋表層の生物生産性の変化

書誌事項

タイトル別名
  • Primary Production Changes for the Past 60,000 Years: Deduced by the Analyses on a Piston Core from the Ryukyu Trench Slope, Northwest Pacific Ocean.
  • Deduced by the Analyses on a Piston Core from the Ryukyu Trench Slope, Northwest Pacific Ocean

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抄録

A piston core (RN95-PC4) collected from the central Ryukyu Trench slope is investigated concerning the down-core fluctuations in planktic and benthic δ18O and δ13C values, total organic carbon contents (TOC), organic carbon/nitrogen (C/N) ratios, calcium carbonate contents, benthic foraminiferal crops, and planktic foraminiferal fauna. Based upon the oxygen isotope stratigraphy and three AMS14C dates, this core reveals a continued sedimentation for the past -60ka; from the early oxygen isotope Stage 3 to the present. The primary production in surface water increased during the last glacial period, particularly in Stage 2, judging from the significant signals in down-core changes of benthic δ13C values, TOC, C/N ratios, and so on. Analysis of planktic foraminiferal fauna suggests that the increased primary production in Stage 2 might be ascribed to relative development of upwelling with cold water invasion.

収録刊行物

  • 第四紀研究

    第四紀研究 37 (5), 361-370, 1998

    日本第四紀学会

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