在前生代地球上增强的变态CO2释放
E M Stewart1, Donald E Penman2
1Department of Earth, Ocean and Atmospheric Science, Florida State University, Tallahassee, FL 32306.
概括
岩石转化在原生代期间释放出大量的二氧化碳 (CO2),可能导致早期地球变暖. 这种增强的二氧化碳释放可能解释了生命早期全球温度升高的原因.
科学领域:
- 地质化学 地质化学
- 古气候学 古气候学
- 地球科学 地球科学 地球科学
背景情况:
- 岩石转化是地质时间尺度上大气中二氧化碳 (CO2) 的重要来源.
- 变态CO2释放的速度受到碳酸盐沉积物组成和地热条件的影响.
- 变态二氧化碳脱气可能在地球历史上发生了变化.
研究的目的:
- 为了研究在原生代期间增强的变态二氧化碳释放对全球气候的影响.
- 为了量化大气二氧化碳水平的潜在增加,由于前生代的变态过程.
主要方法:
- 热力学相位平衡建模以预测变态碳流量.
- 使用碳循环模型PreCOSCIOUS进行分析和数值模拟.
- 估计对原生代碳循环和大气组成的影响.
主要成果:
- 在中原生态时代的变态碳流量大约是今天的1.7倍.
- 与现代速度相比,增强的变态二氧化碳释放可能会使二氧化碳的部分压力 (pCO2) 增加四倍或更多.
- 这种增加的二氧化碳排放有助于更强的温室效应和更高的全球温度.
结论:
- 原生态变态二氧化碳脱气率明显高于今天.
- 这种增强的脱气可能在生命早期扩张期间在维持更高的全球温度方面发挥了关键作用.
- 地状况和碳酸盐岩类型的变化影响了长期的气候趋势.
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