全球海洋氧化由南大洋控制,直到最后一次脱冰
Yi Wang1,2,3, Kassandra M Costa1, Wanyi Lu1
1Department of Geology and Geophysics, Woods Hole Oceanographic Institution, Woods Hole, MA 02543, USA.
Science advances
|January 19, 2024
概括
全球海洋氧气水平在最后一次冰川最大期期间较低. 南大洋通风,而不是北大西洋海流,控制海洋氧气和大气二氧化碳在脱冰过程中的变化.
科学领域:
- 古海洋学是古海洋学.
- 气候科学 气候科学
- 海洋生物地质化学海洋生物地质化学
背景情况:
- 海洋溶解氧 (DO) 对于了解海洋碳循环及其对全球气候变化的影响至关重要.
- 在过去的降冰期间控制全球DO变化的机制仍然不确定.
研究的目的:
- 为了重建在最后一次脱冰过程中的全球DO变化.
- 确定这些DO变化的主要驱动因素.
主要方法:
- 利用同位素进行全球整合的DO重建.
- 与古气候事件相关的DO变化,如Heinrich Stadial 1,Bølling-Allerød和年轻的Dryas.
主要成果:
- 与全新纪相比,在最后一个冰川最大期期间确认了全球较低的DO.
- 在脱冰过程中记录了不同的脱氧和再氧化阶段.
- 观察到除冰期的DO变化与北大西洋深水形成无关.
结论:
- 南大洋的通风是控制海洋脱冰过程中的氧气水平的关键机制.
- 全球二氧化碳排放量和大气中的二氧化碳呈现出千年规模的连贯性,强调了南大洋在二氧化碳上升中的作用.
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