大気中の酸素のバイスタビリティと大酸化過程
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
まとめ
酸素光合成が2つの安定した大気状態を生み出したため,大酸化イベントが遅れた. 地球は酸素濃度が臨界値を超え,オゾン形成を可能にした後に,高酸素大気へと移行した.
科学分野:
- 地質化学 地質化学
- 大気科学 大気科学
- 天体生物学 アストロバイオロジー
背景:
- 地球の歴史は,主要な化学的移行によって断たれた長い安定期を特徴としています.
- 約24億年前の大酸化期には,大気中の酸素が著しく上昇した.
- 酸素 fotosynthesisの進化に関連してこのイベントのタイミングは不明のままです.
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