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Updated: May 5, 2026

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Evolution of Staircase Structures in Diffusive Convection
Published on: September 5, 2018
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北極海における換気循環体制の初期ミオセンの始まりである
Martin Jakobsson1, Jan Backman, Bert Rudels
1Department of Geology and Geochemistry, Stockholm University, SE-106 91 Stockholm, Sweden. martin.jakobsson@geo.su.se
Nature
|June 22, 2007
まとめ
北極海は1750万年前にフラム海峡の開口により完全に酸素化された. このイベントは,地球規模の熱ハリン循環と気候に重大な影響を及ぼしました.
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 海洋学
背景:
- 北極と北大西洋の深海形成は,地球規模の熱ハリン循環と気候を牽引しています.
- 北極からの限られたケノゾイク期の堆積物コアのデータは,その循環の歴史の理解を妨げました.
- 北極と北大西洋の間の深海交差のタイミングは,依然として弱々しく制限されていた.
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