对于冰川期和冰川间大气二氧化碳的变化而产生的化反应
Stephen Barker1, Henry Elderfield
1Department of Earth Sciences, University of Cambridge, Cambridge CB2 3EQ, UK. sbar98@esc.cam.ac.uk
概括
海洋的外重量揭示了过去的二氧化碳水平. 较高的大气二氧化碳直接影响海洋化,影响全球碳循环和古海洋学代理应用.
科学领域:
- 古海洋学是古海洋学.
- 海洋地质化学海洋地质化学
- 气候科学是气候科学.
背景情况:
- 藻类是主要的海洋化物.
- 海水碳酸离子度影响的形成.
- 大气中的二氧化碳水平在冰川-冰川间周期中波动.
研究的目的:
- 重建表面海水二氧化碳记录.
- 研究大气中的二氧化碳对海洋化的影响.
- 评估海洋化和大气CO2之间的反机制.
主要方法:
- 在终结I.上分析菌体重量.
- 与海水碳酸离子度相关联的贝重量.
- 重建过去的表面海水二氧化碳度.
主要成果:
- 对于的外重量记录,可以追踪海水中的碳酸离子度.
- 重建的表面海水二氧化碳记录与大气记录一致.
- 大气中较高的二氧化碳与海洋化变化直接相关.
结论:
- 海洋化对大气中的二氧化碳水平敏感.
- 这种灵敏度对大气二氧化碳产生负面反.
- 这些发现对于解释古海洋学代理和了解气候动态至关重要.
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