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Updated: May 1, 2026

Laboratory Simulation of an IronII-rich Precambrian Marine Upwelling System to Explore the Growth of Photosynthetic Bacteria
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Published on: July 24, 2016

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アエロビックバクテリアのピライト酸化と酸性岩の排水は,グレート・オキシデーション・イベントの間に発生した

Kurt O Konhauser1, Stefan V Lalonde, Noah J Planavsky

  • 1Department of Earth & Atmospheric Sciences, University of Alberta, Edmonton, Alberta T6G 2E3, Canada. kurtk@ualberta.ca

Nature
|October 21, 2011
PubMed
まとめ

古代の岩石は,約248億年前,陸上でのクローム (Cr) の動員を明らかにしています. エアロビック細菌と酸性岩の排水によって引き起こされるこの動員は,これらのプロセスに関する最も初期の地化学的証拠を記しています.

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