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火山の脱ガス圧力の変化によって引き起こされる大気中の酸素化
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
まとめ
プレカンブリア時代における海底から空中噴火への火山活動の変化は,火山ガスの組成を変化させ,大気の酸素化につながった. この変化が現代の硫黄の循環を開始し,大酸化現象を引き起こした.
科学分野:
- 地質化学 地質化学
- 火山学 火山学とは
- プレカンブリア時代以前の地質学
背景:
- 紀元前地球は,約24億5千万年前に重要な地殻形成と大気中酸素化 (大酸化現象) を経験しました.
- 以前の理論では,酸素化とシアノバクテリア,火山ガスによる変化を結びつけていたが,35億年前から不変のままの溶岩の組成はそうではなかった.
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