Depleted Organic Matter In Banded Iron Formations Provides Clues For Extraterrestrial Life Biosignatures
BIFs are layers of sediment that are rich in iron and date to the Precambrian. Theories suggest that they are resulted from the interplay of microbial metabolisms that involved the biogeochemical cycling of iron and organic matter (OM). However, BIFs found on Earth today are depleted in OM. The new study examines whether or not the depletion of OM could be the result of the oxidation of this material during the process of iron reduction....