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大气O2度的普莱斯托时代冰芯记录
D A Stolper1, M L Bender2, G B Dreyfus3
1Department of Geosciences, Princeton University, Princeton, NJ 08544, USA.
概括
在过去的80万年里,大气中的氧气 (O2) 水平下降了0.7%. 这一发现基于古老的空气样本, 表明氧气流量超过了来源, 影响了地球的生态化学循环.
科学领域:
- 地球科学
- 古气候学
- 生物地质化学
背景情况:
- 重建过去的大气氧的部分压力 (Po2) 对于理解地球与生命的共同进化至关重要.
- 现有的Po2重建通常显示出显著的差异,突出了需要更强大的方法.
研究的目的:
- 建立一个可靠的,长期记录大气Po2使用新的代理.
- 调查氧气水平,生物化学循环和过去一百万年气候之间的关系.
主要方法:
- 在南极冰芯中被困的气泡中的O2/N2比率的分析.
- 氧气槽和来源的建模,包括有机碳埋葬和 pyrite 风化.
主要成果:
- 大气中的二氧化持续产生了80万年.
- 在此期间,PO2下降了大约0.7% (每毫升7).
- 氧气总是比氧气源高出约2%.
结论:
- 观察到的PO2下降与碳和流的变化有关,可能是由新世纪冷却或世侵蚀驱动的.
- 尽管二氧化碳下降,但同一时期大气中二氧化碳局部压力 (Pco2) 稳定,支持酸盐气候反在气候调节中的作用.
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