Fluorescence In Situ Hybridization (FISH)
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by the reduction of Fe(III) to Fe(II) and hence Fe(III)reducing prokaryotes have to reduce large quantities of Fe(III) to sustain cell metabolism. Due to the complex geochemistry of iron, acidophilic and neutrophilic Fe(III)-reducing prokaryotes have to cope with different iron species: Fe(III) minerals are soluble only below a pH value of 3. At circumneutral pH, Fe(III) is only poorly soluble and significantly less energy can be gained by Fe(III) respiration compared to aerobic respiration. However, Fe(III) is the dominant electron acceptor in many anoxic habitats and prokaryotes developed different strategies for its utilization.
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Bibliography
FERMENTATION
Appelo, C. A. J., and Postma, D., 2007. Geochemistry, Groundwater and Pollution. Leiden: Balkema. Balashova, V. V., and Zavarzin, G. A., 1979. Anaerobic reduction of ferric iron by hydrogen bacteria. Microbiologiia, 48, 773–778. Balashova, V. V., and Zavarzin, G. A., 1980. Anaerobic reduction of ferric iron by hydrogen bacteria. Microbiology, 48, 635–639. Canfield, D. E., Thamdrup, B., and Kirstensen, E., 2005. Aquatic Geomicrobiology. San Diego: Elsevier. Cornell, R. M., and Schwertmann, U., 2003. The Iron Oxides Structure, Properties, Reactions, Occurrence and Uses. Weinheim: Wiley-VCH. Johnson, D. B., 2007. Physiology and ecology of acidophilic microorganisms. In Gerday, C., and Glansdorff, N. (eds.), Physiology and Biochemistry of Extremophiles. Washington, DC: ASM, pp 257–270. Johnson, D. B., Ghauri, M. A., and McGinness, S., 1993. Biogeochemical cycling of iron and sulphur in leaching environments. FEMS Microbiology Reviews, 11, 63–70. Johnson, C. M., Beard, B. L., and Roden, E. E., 2008. The iron isotope fingerprints of redox and biogeochemical cycling in modern and ancient Earth. Annual Review of Earth and Planetary Sciences, 36, 457–493. Kappler, A., and Straub, K. L., 2005. Geomicrobiological cycling of iron. Reviews in Mineralogy and Geochemistry, 59, 85–108. Lovley, D. R., 1991. Dissimilatory Fe(III) and Mn(IV) reduction. Microbiological Reviews, 55, 259–287. Lovley, D. R., and Phillips, E. J. P., 1988. Novel mode of microbial energy metabolism: organic carbon oxidation coupled to dissimilatory reduction of iron or manganese. Applied and Environmental Microbiology, 54, 1472–1480. Lovley, D. R., Coates, J. D., Blunt-Harris, E. L., Phillips, E. J. P., and Woodward, J. C., 1996. Humic substances as electron acceptors for microbial respiration. Nature, 382, 445–448. Lovley, D. R., Holmes, D. E., and Nevin, K. P., 2004. Dissimilatory Fe(III) and Mn(IV) reduction. Advances in Microbial Physiology, 49, 219–286. Myers, C. R., and Nealson, K. H., 1988. Bacterial manganese reduction and growth with manganese oxide as the sole electron acceptor. Science, 240, 1319–1321. Straub, K. L., and Schink, B., 2004. Ferrihydrite-dependent growth of Sulfurospirillum deleyianum by electron transfer via sulfur cycling. Applied and Environmental Microbiology, 70, 5744–5749. Straub, K. L., Benz, M., and Schink, B., 2001. Iron metabolism in anoxic environm
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