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Updated: May 3, 2026

Laboratory Simulation of an IronII-rich Precambrian Marine Upwelling System to Explore the Growth of Photosynthetic Bacteria
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オリゴセンの初期,北大西洋の深水形成が始まった

R Davies1, J Cartwright, J Pike

  • 1ExxonMobil International Limited, St Catherine's House, 2 Kingsway, PO Box 393, London WC2B 6WF, UK.

Nature
|April 20, 2001
PubMed
まとめ

北極海と北大西洋の間の深水の流れは,これまで考えられていたよりも早く,約3500万年前に始まった. この発見は,気候変動モデルの影響と,世界の海洋循環の理解に影響を与えます.

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