早期白时期海洋脱氧的气候门
Kohen W Bauer1,2, N Ryan McKenzie3, Chris T L Cheung4
1Department of Earth Science, The University of Hong Kong, Pok Fu Lam, Hong Kong. kohenbauer@gmail.com.
Nature
|September 4, 2024
概括
海洋无氧事件 (OAE) 与火山二氧化碳 (CO2) 排放和气候值有关. 越过这一门导致了长期的海洋脱氧, 由于缓慢的气候反机制而延迟恢复.
科学领域:
- 古气候学
- 地质化学
- 海洋学
背景情况:
- 海洋无氧事件 (OAE) 代表了与气候变暖和生物危机相关的全球缺氧.
- 火山二氧化碳 (CO2) 排放被认为是气候变暖导致的OAE的驱动因素.
- 早期白时期的OAE1a是一个重要的OAE,但它的驱动因素和动态仍然不清楚.
研究的目的:
- 解决OAE1a驱动过程的时间和动态.
- 在OAE1a期间调查气候强迫和海洋氧化之间的因果关系.
- 了解OAE1a对地球系统动态的长期影响.
主要方法:
- 在OAE1a的海洋化学和气候记录分析.
- 模拟火山二氧化碳排放,气候值和海洋脱氧之间的相互作用.
- 研究酸盐气候反和轨道强迫的作用.
主要成果:
- 在OAE1a期间的快速脱氧与火山二氧化碳排放和跨越气候值相关.
- 酸盐气候反的缓慢恢复延迟了再氧化超过100万年.
- 在OAE1a之后,残留热量和轨道强迫导致周期性脱氧,持续了100万年.
结论:
- 在OAE1a期间的海洋脱氧是由于火山二氧化碳排放超过了关键气候值引起的.
- 地球系统从OAE1a的恢复由于缓慢的气候反而延长.
- 火山活动,气候变化和海洋氧含量之间存在密切的联系,由气候值调节.
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