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东部热带太平洋缺氧海水的冰川扩张
Babette A A Hoogakker1,2, Zunli Lu3,4, Natalie Umling5
1The Lyell Centre, Heriot-Watt University, Edinburgh, UK. b.hoogakker@hw.ac.uk.
Nature
|October 19, 2018
概括
海洋的碳储存可以解释冰河时代大气中较低的二氧化碳. 新的研究显示,太平洋冰川的氧气耗尽增加了碳储量.
科学领域:
- 古代海洋学
- 海洋地质化学
- 气候科学
背景情况:
- 海洋碳储存是冰河时代大气二氧化碳减少的一个建议机制.
- 之前的研究表明, 深海的氧气含量较低,
- 这种垂直对立表明海洋碳储量的净变化很小.
研究的目的:
- 为了重建自上个冰河时代以来东部热带太平洋低氧水域的变化.
- 研究太平洋碳储备在冰川大气二氧化碳减排中的作用.
主要方法:
- 使用双代理方法,结合上方水柱和下方水氧重建.
- 应用深水氧气量的数据来估计呼吸的碳储量.
主要成果:
- 在最后一个冰川时期, 东太平洋的氧气耗尽向下扩张的证据.
- 没有迹象表明在冰川期间上层水柱氧化增加.
- 显著增加了太平洋冰川中的呼吸碳储量.
结论:
- 太平洋冰川经历了扩大氧气耗尽,增加了碳储存能力.
- 这种在太平洋扩大的碳储备是降低大气二氧化碳的关键因素.
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