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同步气候-碳循环心跳在Phanerozoic植被冰库中的心跳
Qiang Fang1,2,3, Huaichun Wu4,5,6, Isabel P Montañez7
1State Key Laboratory of Geomicrobiology and Environmental Changes, China University of Geosciences, Beijing, China.
Nature communications
|October 16, 2025
概括
晚古冰河时代 (LPIA) 期间的气候碳循环反显示出国家特定的动态. 这些由天文强迫驱动的模式,类似于晚代热带冰河时代 (LCIA) 的模式.
科学领域:
- 古气候学 古气候学
- 地质化学 地质化学
- 地球系统科学 地球系统科学
背景情况:
- 地球的气候已经展现出明显的气候-碳循环反在晚凯诺纪冰河时代 (LCIA).
- 在之前的晚古冰河时代 (LPIA) 期间存在类似的反反应尚未得到充分理解.
研究的目的:
- 在LPIA (约337-300万年前) 期间调查气候周期和碳同位素之间的相位关系.
- 将LPIA的气候碳动态与LCIA的气候碳动态进行比较.
主要方法:
- 碳酸碳同位素记录的分析.
- 检查异常节奏的气候周期.
- 气候与碳同位素之间的相位关系分析.
主要成果:
- 直到307万年前,低度的碳储库在冷却过程中扩大,反映了LCIA的动态.
- 307万年后,这种关系发生了逆转,类似于普利奥-普莱斯托时代的动态.
- 在LPIA和LCIA的天文强迫,碳循环和冰化之间观察到一个准同步.
结论:
- LPIA展示了州特定的气候-碳循环反,显著的反转约为307万年前.
- 高度生物群动态可能影响了观察到的逆转,类似于LCIA中的事件.
- 天文学强迫在塑造植物冰川的进化过程中起到了至关重要的作用.
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