大气氧化是由火山脱气压力变化引起的
Fabrice Gaillard1, Bruno Scaillet, Nicholas T Arndt
1Institut des Sciences de la Terre d'Orléans, CNRS-INSU/Université d'Orléans/Université de Tours, Orléans cedex 2, France. gaillard@cnrs-orleans.fr
Nature
|October 14, 2011
概括
在前坎布里亚时代,火山活动从海底到空中喷发的转变改变了火山气体的组成,导致大气氧化. 这种变化启动了现代的硫循环,并引发了大氧化事件.
科学领域:
- 地质化学 地质化学
- 火山学 火山学是一门学科.
- 前坎布里亚时期的地质学
背景情况:
- 在大约245亿年前,甲纪前的地球经历了显著的地形成和大气氧化 (大氧化事件).
- 以前的理论将氧化与菌和火山气体变化联系在一起,但不是岩组成,自35亿年前以来一直保持不变.
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