在中世温暖时期加强海洋氧化
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
概括
古气候数据显示,海洋缺氧区 (ODZ) 在过去的温暖时期收缩,与目前的扩张预测相反. 这表明全球变暖最终可能导致ODZ的收缩.
科学领域:
- 古代海洋学
- 海洋地质化学
背景情况:
- 溶解氧 (O2) 对海洋生态系统和营养循环至关重要.
- 海洋缺氧区 (ODZ) 由于全球变暖而扩大,但模型预测不确定.
- 古气候记录提供了持续温暖下潜在的ODZ动态的见解.
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