Abstract
With the exception of mainly lactic acid bacteria (Archibald, 1983; Pandey et al., 1994), iron is required as an oligoelement by all living organisms and particularly by aerobic bacteria, such as Pseudomonas. Because of its redox potentialities, this element is involved in many, if not all, primary biological functions, e. g., electron transport, carbon metabolism, nitrogen fixation, and nucleic acid biosynthesis. Although abundant in nature, iron is, however, not readily available for bacteria because of its profound tendency to hydrolyze and polymerize at physiological pH under aerobiosis. Thus, solubilization of environmental iron by excretion of powerful iron-chelating secondary metabolites, i. e., the siderophores, is the most common way used by microorganisms to sustain their iron requirement.
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References
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Meyer, JM., Stintzi, A. (1998). Iron Metabolism and Siderophores in Pseudomonas and Related Species. In: Montie, T.C. (eds) Pseudomonas. Biotechnology Handbooks, vol 10. Springer, Boston, MA. https://doi.org/10.1007/978-1-4899-0120-0_7
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