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千年时间尺度的热源性CO2释放在古世 - 世热极限之前
Shijun Jiang1,2, Ying Cui3, Yasu Wang4
1State Key Laboratory of Marine Resource Utilization in South China Sea, Hainan University, Haikou, China. sjiang@hainanu.edu.cn.
Nature communications
|June 30, 2025
概括
在古世 - 世热极限 (PETM) 发生之前的预发行 (POE) 是由热源性CO2驱动的全球事件. 地球系统建模表明火山,而不是火山爆发,引发了这种碳释放.
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:
- 地质记录显示,一段短暂的碳释放,即预发行 (POE),在大约5600万年前的古世 - 世热极值 (PETM) 之前发生.
- 由于POE与PETM的起源,时间和联系尚不清楚,因此需要进一步调查早期的纪气候事件.
研究的目的:
- 调查POE碳释放的来源和速度.
- 为了澄清POE和PETM之间的关系.
- 确认POE的全球范围及其对环境的影响.
主要方法:
- 高时间分辨率地层学分析来自东部泰西斯海洋的沉积物记录,跨越POE和PETM.
- 生物标志物提取和分析以评估环境变化.
- 地球系统建模受古气候数据 (δ13C和pH) 的限制.
主要成果:
- 这项研究证实了POE的全球性,通过来自东部泰提斯海洋的平流图记录.
- 与PETM相比,生物标志物数据显示,POE期间的环境干扰在研究区域的PETM相比,不那么严重.
- 地球系统建模表明,热源的二氧化碳来源,可能来自北大西洋火山前的入侵,驱动了POE,可能被甲释放放放大.
结论:
- POE是一个由热性CO2驱动的全球性事件,可能与早期的岩活动有关.
- 与PETM相比,POE对环境的影响不那么明显.
- 生物地化学反,包括甲释放,可能影响了POE的碳循环动态.
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