Siderophore iron transport was followed in Ustilago sphaerogena using isotope transport assays coupled with EPR spectroscopy. EPR spectroscopy was used as a quantitative tool to follow the rate of reduction of siderophore iron(III) to iron(II) in the cell suspension by following the disappearance of the signal at g = 4.3. This rate was compared with the rate of iron transport, measured by the disappearance of radioactively labeled iron from the medium. The transport of three iron chelates was examined: the ferric siderophores ferrichrome and ferichrome A, and iron(III) chelated to excess citrate. For the transport of ferrichrome, an iron(III) ionophore, the rate of reduction of iron(III) to iron(II) was significantly lower than the rate of uptake of isotope from the medium supernatant, which is consistent with the established mechanism of uptake of the entire complex followed by intracellular reduction to remove the iron from the ligand. However, the rate of reduction of ferrichrome A, a non-ionophore, was identical with the rate of transport of iron into the cell. Iron(III) citrate was reduced at a rate slightly lower than the rate of transport. These data suggest that reduction of iron(III) is involved in the transport of iron from ferichrome A and possibly from iron(III) citrate.