岩石有机碳氧化CO2释放抵消剂 酸盐气候沉积槽
Jesse R Zondervan1,2, Robert G Hilton3, Mathieu Dellinger4
1Department of Earth Sciences, University of Oxford, Oxford, UK. j.zondervan@ucl.ac.uk.
Nature
|October 4, 2023
概括
岩石有机碳 (OCpetro) 的气候变化释放出大量的二氧化碳,可能与酸盐气候变化的减排相美. 这一发现突显了地质碳流在调节地球气候中的关键作用.
科学领域:
- 地质化学
- 气候科学
- 地质学
背景情况:
- 山脉的升起和侵蚀影响了地球的碳平衡.
- 酸盐气候吸收了大气中的二氧化碳,稳定了气候.
- 岩石有机碳 (OCpetro) 的气候变化释放CO2,但量化程度不佳.
研究的目的:
- 通过气候变化释放的二氧化碳的全球流量.
- 评估这种地质CO2流与酸盐气候变化的意义.
- 确定高OCpetro气候变化的地区.
主要方法:
- 使用微量元素作为替代物.
- 使用空间推断模型.
- 在全球河流流域的量化OCpetro气候流.
主要成果:
- 估计每年的CO2排放来自OC石油的气候变化,相当于或超过全球的化物气候减排.
- 在高升速和细粒度沉积岩 (例如喜马拉雅山脉,洛基山脉,安第斯山脉) 的山脉中发现了CO2释放的热点.
- 证明OCpetro不是惰性的,并且对区域碳预算产生重大影响.
结论:
- 石油的气候变化代表了一个主要的地质CO2流.
- 侵蚀和气候变化在长期碳循环中起着复杂的作用,影响大气中的二氧化碳水平.
- 需要进一步研究以了解这些流动对地球气候系统的全部影响.
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