熱帯ケノゾイク期における海洋酸化の強化
Alexandra Auderset1,2, Simone Moretti3,4, Björn Taphorn3
1Climate Geochemistry Department, Max Planck Institute for Chemistry, Mainz, Germany. a.auderset@mpic.de.
Nature
|August 31, 2022
まとめ
古代気候のデータは,現在の膨張予測とは対照的に,過去温暖期に海洋の酸素不足地帯 (ODZ) が収縮したことを明らかにしています. これは,地球温暖化が最終的にODZの収縮につながる可能性があることを示唆しています.
科学分野:
- 古代海洋学
- 海洋生物化学
背景:
- 溶けた酸素 (O2) は海洋生態系と栄養循環に不可欠です.
- 海洋の酸素不足地帯 (ODZ) は地球温暖化により拡大していると考えられていますが,モデル予測は不確実です.
- 古気候記録は,持続的な温暖化下での潜在的なODZダイナミクスに関する洞察を提供します.
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