Iron (Fe) is the fourth most abundant element in the earth's crust and plays important roles in
both biological and chemical processes. The redox reactivity of various Fe (II) forms has …

Iron (Fe) minerals play an important role in stabilizing soil organic carbon (SOC). Fe-
mediated SOC protection is mainly achieved through adsorption, co-precipitation, or …

Electrochemically active bacteria can transport their metabolically generated electrons to
anodes, or accept electrons from cathodes to synthesize high‐value chemicals and fuels, via …

The dark production of reactive oxygen species (ROS) coupled to biogeochemical cycling of
iron (Fe) plays a pivotal role in controlling arsenic transformation and detoxification …

The family Geobacteraceae, with its only valid genus Geobacter, comprises
deltaproteobacteria ubiquitous in soil, sediments, and subsurface environments where metal …

The biochemical mechanisms by which microbes interact with extracellular soluble metal
ions and insoluble redox-active minerals have been the focus of intense research over the …

Feammox, that is, Fe (III) reduction coupled to anaerobic ammonium oxidation, has been
reported to play an important role in the nitrogen cycle in natural environments. However …

Redox reactions between iron and nitrogen drive the global biogeochemical cycles of these
two elements and, concomitantly, change the fate of nutrients in and the mineralogy of the …

Redox-active minerals are ubiquitous in the environment and are involved in numerous
electron transfer reactions that significantly affect biogeochemical processes and cycles as …

Nitrate-dependent ferrous iron [Fe (II)] oxidation (NDFO) is a well-recognized
chemolithotrophic pathway in anoxic sediments. The neutrophilic chemolithoautotrophic …