O2 and H2S coexistence in stromatolites: A model for the origin of mineralogical lamination in stromatolites and banded iron formations

The coexistence of O₂ and H₂S in recent microbial mats is demonstrated. Oxygen and H₂S are not only coexisting in considerable concentrations within recent stromatolites but high concentrations of the respective gases occur in alternating laminae. This "sandwich structure" is produced by alternating populations of oxygenic and anoxygenic photosynthetic bacteria and cyanobaeteria. The finding of such conditions may explain the alternation of oxidized and reduced iron minerals in Precambrian stromatolites and possibly also in the banded iron formations (BIFs).