High affinity iron uptake in fungi is supported by a plasma membrane protein complex that includes a multicopper ferroxidase enzyme and a ferric iron permease. In Saccharomyces cerevisiae, this complex is composed of the ferroxidase Fet3p and the permease Ftr1p. Fe(II) serves as substrate for Fe-uptake by being substrate for Fet3p; the resulting Fet3p-produced Fe(III) is then transported across the membrane via Ftr1p. A model of metabolite channeling of this Fe(III) is tested here by first constructing and kinetically characterizing in Fe-uptake two Fet3p-Ftr1p chimeras in which the multicopper oxidase/ferroxidase domain of Fet3p has been fused to the Ftr1p iron permease. Although the bifunctional chimeras are as kinetically efficient in Fe-uptake as is the wild type two-component system, they lack the adaptability and fidelity in Fe-uptake of the wild type. Specifically, Fe-uptake through the Fet3p, Ftr1p complex is insensitive to a potential Fe(III) trapping agent - citrate - whereas Fe-uptake via the chimeric proteins is competitively inhibited by this Fe(III) chelator. This inhibition does not appear to be due to scavenging Fet3p-produced Fe(III) that is in equilibrium with bulk solvent but could be due to leakiness to citrate found in the bifunctional but not the two-component system. The data are consistent with a channeling model of Fe-trafficking in the Fet3p, Ftr1p complex and suggest that in this system, Fet3p serves as a redox sieve that presents Fe(III) specifically for permeation through Ftr1p.

• PMID: 16387364
• DOI full text
• PubMed

Reference Type

Journal Article | Research Support, N.I.H., Extramural

Authors

Kwok EY, Stoj CS, Severance S, Kosman DJ

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