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- 岡 俊太郎
- 北海道大学大学院地球環境科学研究科
書誌事項
- タイトル別名
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- 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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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
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- 第四紀研究
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第四紀研究 37 (5), 361-370, 1998
日本第四紀学会
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詳細情報 詳細情報について
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- CRID
- 1390282681473560576
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- NII論文ID
- 10002510699
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- NII書誌ID
- AN0034136X
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- ISSN
- 18818129
- 04182642
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- NDL書誌ID
- 105858
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- 本文言語コード
- en
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- データソース種別
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- JaLC
- NDL
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- 使用不可