大气中的二氧化碳度在普莱斯托时代中期的过渡时期
Bärbel Hönisch1, N Gary Hemming, David Archer
1Department of Earth and Environmental Sciences, Lamont-Doherty Earth Observatory of Columbia University, NY 10964-8000, USA.
概括
普莱斯托时代的冰川周期从4万年转移到10万年. 这项研究显示,在这种转变之前,大气中的二氧化碳 (CO2) 水平稳定,挑战了长期的二氧化碳减排作为主要原因.
科学领域:
- 古气候学 古气候学
- 地质化学 地质化学
- 海洋学 海洋学 海洋学
背景情况:
- 普莱斯托时代中期过渡 (MPT) 标志着地球冰川周期周期的显著转变.
- 这种~4万年~10万年周期变化的根本驱动因素仍然不完全理解.
- 以前的假设表明,大气二氧化碳的长期下降是潜在的MPT触发因素.
研究的目的:
- 重建一个长期记录大气二氧化碳 (CO2) 水平在MPT.
- 为了研究二氧化碳变化和冰川周期动态之间的关系.
- 为了测试CO2吸收导致MPT的假设.
主要方法:
- 在浮游生物中分析的同位素,以确定过去的海面二氧化碳的部分压力 (Pco2).
- 建造了一个210万年Pco2记录.
- 在MPT前和MPT后的二氧化碳水平与冰川周期行为的比较.
主要成果:
- 大气中的Pco2在MPT之前相对稳定.
- 在MPT (>100万年前) 之前,冰川Pco2水平大约高出31个微大气层.
- 在MPT之后的冰川间Pco2水平与普世晚期 (<45万年前) 的水平相似.
结论:
- 这些发现支持大气中的二氧化碳与全球气候之间存在强烈联系.
- 在MPT之前的间冰期Pco2的稳定性与逐渐减少CO2的理论相矛盾.
- 长期减少大气中的二氧化碳不太可能是中普世过渡的主要驱动因素.
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