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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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Oxidación de pirita bacteriana aeróbica y drenaje de roca ácida durante el Gran Evento de Oxidación

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
Resumen

Las rocas antiguas revelan la movilización de cromo (Cr) en la tierra hace unos 2.48 mil millones de años. Esta movilización, impulsada por bacterias aeróbicas y drenaje de rocas ácidas, marca la primera evidencia geoquímica de estos procesos.

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