Frontiers | Mechanisms of Pyrite Formation Promoted by Sulfate-Reducing
Pyrite, or iron disulfide, is the most common sulfide mineral on the Earth's surface and is widespread through the geological record. Because sulfides are mainly produced by sulfate-reducing bacteria (SRB) in modern sedimentary environments, microorganisms are assumed to drive the formation of iron sulfides, in particular, pyrite. However, the exact …