Abstract
Iron is essential for the growth of most cells since it participates in many key metabolic processes. However, under current environmental conditions, where oxygen is plentiful, most iron exists in the oxidized ferric or Fe(III) form. Ferric iron readily precipitates as highly insoluble ferric hydroxides at neutral pH, and these are not readily utilized by cells. The other biologically important oxidation state of iron is Fe(II), the ferrous form. Ferrous iron is much more soluble at neutral pH than ferric iron, but in the presence of oxygen it is efficiently oxidized to Fe(III). Thus, if organisms are to acquire enough iron to meet their metabolic requirements, they must evolve strategies for obtaining insoluble ferric iron from the environment.
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© 1994 Springer Science+Business Media New York
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Anderson, G.J., Dancis, A., Roman, D.G., Klausner, R.D. (1994). Ferric Iron Reduction and Iron Uptake in Eucaryotes: Studies with the Yeasts. In: Hershko, C., Konijn, A.M., Aisen, P. (eds) Progress in Iron Research. Advances in Experimental Medicine and Biology, vol 356. Springer, Boston, MA. https://doi.org/10.1007/978-1-4615-2554-7_9
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DOI: https://doi.org/10.1007/978-1-4615-2554-7_9
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