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Updated: Jul 9, 2026

Removal of Exogenous Materials from the Outer Portion of Frozen Cores to Investigate the Ancient Biological Communities Harbored Inside
09:06

Removal of Exogenous Materials from the Outer Portion of Frozen Cores to Investigate the Ancient Biological Communities Harbored Inside

Published on: July 3, 2016

深海における炭酸イオンの氷河期からホロセーン期への再分布

W S Broecker1, E Clark

  • 1Lamont-Doherty Earth Observatory of Columbia University, Palisades, NY 10964, USA. broecker@ldeo.columbia.edu

Science (New York, N.Y.)
|December 12, 2001
PubMed
まとめ

氷河期の海は,炭酸イオン濃度グラデーションが顕著であった. 今日とは異なり,太平洋の深い水域では,濃度が深さとともに上昇し,大西洋の水域では減少し,より大きな海洋学的なコントラストを示しました.

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