地表温度和大气中的二氧化碳度在古世时期的结合
Rosemarie E Came1, John M Eiler, Ján Veizer
1Division of Geological and Planetary Sciences, California Institute of Technology, Pasadena, California 91125, USA. rcame@gps.caltech.edu
当大气中的二氧化碳水平较高时,古生态时代的海洋更温暖,当二氧化碳水平与今天相似时,海洋更冷. 这表明二氧化碳和全球气温之间存在强烈联系.
科学领域:
- 古气候学 古气候学
- 地质化学 地质化学
背景情况:
- 古老时代大气中的二氧化碳 (CO2) 度明显高于现在的水平.
- 之前的研究表明,这个时代全球气温较高,但关于海面温度 (SST) 的数据有限.
- 考古时代二氧化碳与全球气候之间的关系仍在争论中.
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