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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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在大氧化事件期间,有氧细菌酸氧化和酸性岩石排水

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
概括

古代岩石揭示了大约2480亿年前在陆地上 (Cr) 的动员. 这种动员是由有氧细菌和酸性岩石排水驱动的,标志着这些过程的最早的地化学证据.

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