Oxidation and Reduction of Iron by Acidophilic Bacteria

Redox reactions of iron in acidic environments are of economic and environmental significance, for example, for the leaching of metal ores and for the formation of acid mine drainage and acid sulfate soils. Until recently, research on microbial iron metabolism in acidic environments has mainly been focused on the role of aerobic, autotrophic ferrous iron‐oxidizing bacteria. In the present paper, recent new developments in the field of acidophilic iron metabolism are reviewed. In addition to the well‐known autotrophic ferrous iron‐oxidizing organisms, new heterotrophic isolates have been described that are capable of oxidizing ferrous iron. Microorganisms can also play an important role in the reductive part of the iron cycle. Both heterotrophic and autotrophic organisms may also be involved in this process. The contribution of heterotrophic organisms to acidophilic iron cycling can be twofold: In addition to their direct role as a catalyst, these organisms may scavenge organic compounds that inhibit their autotrophic counterparts. Detailed studies of acidophilic ecosystems are needed to assess the significance of the various types of microorganisms for the overall rate of iron cycling in these extreme environments.