SIDEROPHORE-MEDIATED IRON DISSOLUTION FROM NONTRONITES IS CONTROLLED BY MINERAL CRISTALLOCHEMISTRY

Bacteria living in oxic environments experience iron deficiency due to limited solubility and slow dissolution kinetics of iron-bearing minerals.To cope with iron deprivation, aerobic bacteria have evolved various strategies, including release of siderophores or other organic acids that scavenge external Fe(III) and deliver it to the cells.This res

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