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Updated: May 6, 2026

Unraveling the Unseen Players in the Ocean - A Field Guide to Water Chemistry and Marine Microbiology
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沈殿物の炭素酸化率が低いため,太平洋の中間水域で溶けた酸素が増えた

L D Stott1, W Berelson, R Douglas

  • 1Department of Earth Sciences, University of Southern California, Los Angeles 90089, USA. stott@usc.edu

Nature
|October 3, 2000
PubMed
まとめ

海洋溶解酸素のレベルは,1970年代以降上昇しており,これは海底堆積物の変化によって示されています. この酸素濃度の上昇は,北太平洋の気候変化が海洋の生産性に影響を与えていることと関連しています.

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