过去的极端变暖事件与永久土解导致的大规模碳释放有关
Robert M DeConto1, Simone Galeotti, Mark Pagani
1Department of Geosciences, University of Massachusetts, Amherst, Massachusetts 01002, USA. deconto@geo.umass.edu
Nature
|April 7, 2012
概括
地球的古老超热气候,包括古世 - 世热极量 (PETM),是由轨道循环引发的,导致永久土释放碳. 这解释了这些极端的全球变暖事件的时间和规模.
科学领域:
- 古气候学 古气候学
- 地质化学 地质化学
- 气候建模气候模型
背景情况:
- 地球在5550万到5200万年前经历了极端的全球变暖事件 (超热).
- 古世 - 世热极值 (PETM) 涉及大规模的碳释放,海洋酸化和5°C的温度上升.
- 现有的模型很难解释这些超热的碳来源,大小和时间.
研究的目的:
- 调查早期伊欧纪高温物体背后的驱动因素,包括PETM.
- 开发一个统一的模型,用于这些变暖事件期间的碳释放.
主要方法:
- 利用来自意大利的新天文校准的循环平行图谱记录.
- 进行了气候-生态系统-土壤模拟,包括温室气体和轨道强迫.
主要成果:
- 早期欧时代的高热流与特定的地球轨道配置 (高偏心和倾斜) 相吻合.
- 模拟表明永久土土壤有机碳的轨道触发分解解释了PETM和随后的超热.
- 数以千计的克碳从永久土中释放出来,由PETM前的升温值放大.
结论:
- 地球的轨道属性是引发永久土大量碳释放的关键因素.
- 永久土充当了一种敏感的碳储备,影响了超热波的规模和频率.
- 随着背景温度的上升,永久土范围的下降导致随后的超热层变小.
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