在温暖的中世时期,一个充满氧气的东部热带太平洋
Anya V Hess1, Alexandra Auderset2,3, Yair Rosenthal4,5
1Department of Earth and Planetary Sciences, Rutgers, The State University of New Jersey, Piscataway, NJ, USA. anya.hess@gmail.com.
Nature
|June 28, 2023
概括
在温暖的中世气候最佳时期,海洋缺氧区 (ODZ) 扩大. 这表明目前东部热带太平洋的脱氧趋势可能会随着全球变暖而逆转.
科学领域:
- 古代海洋学
- 气候科学
- 海洋地质化学
背景情况:
- 由于气候变化,海洋中的氧含量正在下降,特别是在缺氧区域 (ODZ).
- 地球系统模型预测ODZ扩张到2100年,但长期反应仍然不确定.
研究的目的:
- 在比现在更温暖的中世纪气候最佳时期 (MCO) 调查海洋氧化变化.
- 了解海洋氧化对变暖事件的长期反应.
主要方法:
- 作为ODZ范围和强度的代理数据,分析了浮游生物I/Ca和δ15N数据.
- 使用Mg/Ca数据重建海面温度.
- 将古海洋学数据与地球系统模型模拟进行比较.
主要成果:
- 在MCO期间,东部热带太平洋 (ETP) 的溶氧度超过了100μmol kg-1.
- 由于西向东的温度梯度增加和ETP热线的积聚,形成了一个ODZ.
- 在温暖时期较弱的贸易风可能会减少ETP上升,使生产力和氧气需求向东集中.
结论:
- 温暖的气候状态,如MCO,影响海洋氧化模式.
- 根据未来的气候变暖情景,研究结果支持推测近期脱氧趋势可能发生逆转和ETP ODZ扩张的模型.
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