Who Formed All That Iron?: A Novel Antarctic Chemolithotroph Drives Iron Biomineralization

Iron mineralization has profoundly influenced Earths biogeochemical history1,2, yet the specific mechanisms underlying banded iron formation (BIF) remain unresolved3-5. Here we profile the microbiomes of Holocene sediments beneath the Larsen C Ice Shelf (LCIS), Antarctica6-8, through stratigraphic analysis of sedimentary ancient DNA combined with metagenomics. Distinct microbial phases aligned with glacial facies boundaries, with sub-ice shelf communities dominated by chemolithoautotrophs including an uncultured Thermodesulfovibrionia. This bacterium, visualized by fluorescence in situ hybridization and designated Candidatus Mariimomonas ferrooxydans (phylum Nitrospirota), emerged as a keystone taxon with high network centrality. Its genome encodes Cyc2, a fused porin-cytochrome outer membrane protein implicated in Fe(II) oxidation. Heterologous expression of Cyc2 in Escherichia coli confirmed its ability to catalyze iron oxidation, supporting iron precipitation under dark, anoxic conditions. These pristine LCIS sediments, unaltered since the last glacial maximum, provide a modern analogue for synglacial BIFs deposited during Neoproterozoic Snowball Earth events. Our findings deliver direct genomic and functional evidence for chemolithotrophic iron oxidation, challenge phototroph-centric models of BIF genesis, and highlight microbial iron cycling as a recurring force in Earths geochemical evolution. Beyond Earth, these insights inform interpretations of iron deposits on other planetary bodies.