Siderophores and Iron‐Transport in Microorganisms

Abstract

AbstractIron is an essential element in many biological systems, and in spite of its abundance (5% of the earth crust), its availability is dramatically limited by the very high insolubility of iron(III) at physiological pHs where the concentration of free iron(III) is less than 10−17 M, a value which is much too low to allow any possible growth to aerobic microorganisms.Iron metabolization by the microorganisms necessitates generally the biosynthesis of low molecular weight compounds (300 to 2000 Da) called siderophores. These molecules which are generally excreted into the culture medium, chelate very strongly iron(III), solubilize it and transport it into the cells using an ATP‐dependent high affinity transport system.For nearly fourty years, the structural studies on siderophores have shown a great diversity of structures for these iron‐chelating molecules synthesized by microorganisms. These structures are characterized by the presence of one, two and in most cases, three bidentate chelating groups, generally oxygenated, necessary for the formation of very stable hexacoordinated octahedric complexes between the siderophores and iron(III). These groups are generally either catecholates, or hydroxamates or hydroxyacids, but can be any other bidentate groupsIn what follows several typical examples of siderophores belonging to each of these categories are given. It is clear that considering the very high number of siderophores having so many different structures so far isolated and characterized (more than 200), we have restricted this report to the most representative structures of each category, with a special emphasis to pyoverdins, the fluorescent peptidic siderophores of the fluorescent pseudomonads.Similarly the siderophore‐mediated iron‐transport mechanisms of Gram‐negative bacteria described therafter will report mainly on those of Escherichia coli with a special emphasis to Pseudomonas when information is available.The pyoverdin‐mediated iron‐transport in fluorescent pseudomonads implies biochemical mechanisms which involve signal and energy exchanges between the two membranes across the periplasmic space. The energy transduction mechanism in the case of the pyoverdin‐mediated active transport in P. aeruginosa has not been completely elucidated so far. Nevertheless from the data obtained for ferric enterobactin and ferrichrome in E. coli, it is plausible that a common mechanism of transport can take place for all the enterobacteria. The key element of this mechanism is protein TonB in E. coli, head of a series of TonB proteins having a very close structure and characterized in P. putida WCS358 and P. aeruginosa ATCC 156942. The striking similarities existing between the various iron‐transport steps in these different bacterial species is highly in favour of a common energy‐dependent siderophore‐mediated iron‐transport mechanism in microorganisms.