“…In oxygenated, aqueous environments, Fe is found mostly in its oxidized (Fe 3+ ), non‐soluble form (Brand et al ., ; Morel, ; Kranzler et al ., ). Manganese is found mostly in its soluble Mn 2+ state (Salomon et al ., ). Nevertheless, Mn 2+ can be oxidized to the non‐soluble Mn 3+ state by biological or geochemical activities (Rona, ; Pittman, ).…”