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This study investigates the role of a natural microbial consortium in the precipitation of iron minerals from Shield surface water. The consortium can leach iron from minerals, generating a colloidal Fe(III) suspension that can be reduced back to Fe(II) by iron-reducing bacteria, leading to the formation of various iron compounds. The findings suggest that microbial communities significantly influence the geochemical cycling of iron and the types of minerals that are formed in natural environments.

Author

Andrea Molinari

Language

EN