在全球海洋中新一代的有机碳埋葬
Ziye Li1,2,3, Yi Ge Zhang4, Mark Torres5
1College of Marine Geosciences, Key Laboratory of Submarine Geosciences and Prospecting Techniques, Ocean University of China, Qingdao, China.
Nature
|January 4, 2023
概括
海洋沉积物中的有机碳埋葬, 是一个关键的气候调节剂, 代中期的埋葬被抑制了,可能放大了过去的全球变暖.
科学领域:
- 古代海洋学
- 地质化学
- 气候科学
背景情况:
- 海洋有机碳埋葬是大气二氧化碳和氧气来源的关键沉积点.
- 估计过去有机碳埋葬率的常规方法依赖于具有显著不确定性的质量平衡计算.
研究的目的:
- 开发和应用一种新的"自下而上的"方法来计算有机碳埋葬率,独立于质量平衡方法.
- 使用全球数据重建新纪 (23-3万年前) 的有机碳埋葬历史.
主要方法:
- 使用来自全球81个地点的数据来计算有机碳埋葬率.
- 使用一种独立于传统质量平衡计算的新方法.
- 有机和无机碳的分析碳同位素值 (δ13C).
主要成果:
- 发现有机碳埋葬率的空间时间变化比以前估计的要大.
- 在米奥森和奥森早期发现了高埋葬率,在米奥森中期发现了最低埋葬率.
- 在米欧纪中期观察到最低的有机与碳酸盐埋葬比率,这与蒙特雷假说相矛盾.
结论:
- 世中期被抑制的有机碳埋葬与温度依赖的细菌降解有关,这表明有机碳循环对全球变暖起到了积极的反作用.
- 这项研究为过去的碳循环动态及其对气候的影响提供了更强大的理解.
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