古代的回收利用由紫外线辐射促进
Orion Farr1,2, Jihua Hao3,4, Winnie Liu1
1Department of Earth and Planetary Science, Rutgers University, Piscataway, NJ 08854-8066.
概括
在无氧早期海洋中有机化合物的光降解释放酸盐,这是一个关键的营养素. 这一过程很可能在阿凯纪时期推动了初级生产.
科学领域:
- 地质化学 地质化学
- 生物地质化学生物地质化学
- 早期地球的条件.
- 摄影化学的使用.
背景情况:
- 是一种限制生命的营养素,在全球范围内稀缺.
- 现代海洋通过有机物质再矿化来回收.
- 古代的海洋是无毒和减少的,不同于现代的条件.
研究的目的:
- 通过在模拟的古代条件下对有机进行光降解来研究回收.
- 为了确定光化学过程是否可以在早期的海洋中提供可生物利用的.
主要方法:
- 模拟古代海洋条件的光化学实验.
- 对各种有机化合物的光降解率的分析.
- 理论计算以评估光降解的意义.
主要成果:
- 有机化合物 (生物原和石衍生) 在无毒条件下快速光降解.
- 光降解释放无机酸盐到溶液中.
- 观察到的降解速度表明,对早期的海洋供应有显著的贡献.
结论:
- 有机的光降解是回收的关键机制,在无氧的Archean海洋.
- 这一过程可能提供了必要的生物可用,以支持早期地球海洋的初级生产.
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