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最後の氷河間期間に南大西洋の深い海域で起きた停滞現象
Christopher T Hayes1, Alfredo Martínez-García2, Adam P Hasenfratz2
1Department of Earth, Atmospheric and Planetary Sciences, Massachusetts Institute of Technology (MIT), Cambridge, MA 02142, USA. Lamont-Doherty Earth Observatory of Columbia University, Palisades, NY 10964, USA. cthayes@mit.edu.
まとめ
過去の氷河期間の間,地球温暖化により,南極底水 (AABW) の形成が減少し,海洋の酸素化に影響を与えました. これは,氷河期だけでなく,暖かい気候でも深海循環のシフトが起こることを示唆しています.
科学分野:
- パレオセアノグラフィー
- 気候科学 気候科学
- 海洋学 海洋学とは
背景:
- 前回の氷河間期 (約12万7千年前) は,現在のより温暖で,海面が上昇した.
- 南洋の沈殿物は,過去の深海の状況についての洞察を提供します.
研究 の 目的:
- 最後の氷河期間の深海の酸素化が減少した原因を調査する.
- 深海循環パターンが氷河期と氷河間期の間に異なるかどうかを判断する.
主な方法:
- 南大洋の沈殿体核におけるオーチジェニックウランの分析.
- 深海の酸素化と循環パターンの再構築.
主要な成果:
- オーチジェニックウランの急上昇は,12万7000年前,南極地底水 (AABW) による酸素化の減少を示しています.
- このAABWの減少は,南極の氷床の融水と関連しているように見えますが,公海の状態ではありません.
- AABWの減少は,北大西洋深水 (NADW) の形成の増加と一致し,その逆も同様でした.
結論:
- 深海の循環は,AABWとNADWの形成の交互によって特徴付けられ,冷たい (氷河期) と暖かい (氷間期) の気候の両方で発生します.
- 南極の氷床の質量減少は,深水の形成と海洋循環に大きく影響を与えます.
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