在古世时期大气中二氧化碳度明显下降
Mark Pagani1, James C Zachos, Katherine H Freeman
1Department of Geology and Geophysics, Yale University, 210 Whitney Avenue, New Haven, CT 06511, USA.
概括
大气中的二氧化碳 (CO2) 含量在埃奥生时代很高,在奥利戈生时代逐渐下降,达到现代水平. 这种二氧化碳的减少促进了南极冰盖的扩张和C4光合作用的演变.
科学领域:
- 古气候学 古气候学
- 古海洋学是古海洋学.
- 同位素地球化学 同位素地球化学
背景情况:
- 大气中的二氧化碳 (CO2) 和古世气候之间的关系仍然不清楚.
- 了解过去的二氧化碳水平对于重建气候动态至关重要.
研究的目的:
- 为了重建大气中的二氧化碳水平,在中期伊欧纪到晚期奥利古纪 (4500万至250万年前).
- 研究二氧化碳变化对古世气候和生态系统的影响.
主要方法:
- 从二不和基中分析稳定的碳同位素值.
- 从深海沉积物核中提取基.
主要成果:
- 大气中的二氧化碳含量在中后伊纪的每百万分之1000至1500 (ppm) 之间.
- 二氧化碳在整个奥利古纪的几个阶段下降,在奥利古纪晚期达到现代水平.
- 观察到的二氧化碳减少与南极冰盖的膨胀和C4光合作用的出现有关.
结论:
- 古世气候受到长期二氧化碳波动的强烈影响.
- 世 - 世过渡标志着地球气候系统的重大转变,这是由降低CO2驱动的.
- 重建的二氧化碳趋势为了解古世主要环境变化提供了一个框架.
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