大气中的氧气和大氧化过程的双重性
Colin Goldblatt1, Timothy M Lenton, Andrew J Watson
1School of Environmental Sciences, University of East Anglia, Norwich, NR4 7TJ, UK. c.goldblatt@uea.ac.uk
Nature
|October 13, 2006
概括
大氧化事件被推迟了,因为氧光合作用创造了两个稳定的大气状态. 只有在氧气水平超过了关键值后,地球才过渡到高氧气大气层,从而使臭氧形成.
科学领域:
- 地质化学 地质化学
- 大气科学 大气科学
- 天体生物学 天体生物学
背景情况:
- 地球历史的特点是长期的稳定时期,经历了主要的化学转变.
- 大约24亿年前的大氧化,标志着大气氧气的显著增加.
- 这一事件相对于氧气光合作用进化的时间仍然不清楚.
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