有机碳循环和黑页岩沉积:地球系统科学视角
Zhijun Jin1, Xiaomei Wang2, Huajian Wang2
1Institute of Energy, Peking University, Beijing100871, China.
National science review
|October 30, 2023
概括
黑色页岩,富含有机碳,通过地质时间的复杂地球系统相互作用形成. 这些岩石形成为地球的氧化,气候变化和宝贵资源提供了洞察力.
科学领域:
- 地球系统科学 地球系统科学
- 地质化学 地质化学
- 古气候学 古气候学
背景情况:
- 地球表现出不断循环的物质和能量.
- 有机碳的生产始于40亿年前,随着时间的推移,页岩沉积的变化.
研究的目的:
- 讨论有机碳循环和黑页岩开发.
- 提出黑色页岩形成的模型.
- 突出黑色页岩在理解地球过程中的重要性.
主要方法:
- 地球系统科学视角.
- 分析了岩层进化,轨道强迫,气候,光合作用和退化之间的相互作用.
主要成果:
- 黑页岩沉积是由多个地球系统组件的相互作用驱动的.
- 黑色页岩作为地球氧化历史的档案.
- 这些矿床含有宝贵的石油和金属矿产资源.
结论:
- 黑页岩提供了关于气候变化驱动因素和规模的关键数据.
- 未来的研究需要对黑页岩研究采取更广泛,多维的方法.
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