The fate of the hydroxamic acid-iron transport cofactors during iron uptake from the "'Fe3+ chelates of the 'H-labeled hydroxamates schizokinen and aerobactin was studied by assay of simultaneous incorporation of both ",Fe3+ and 3H. In the schizokinen-producing organism Bacillus megaterium ATCC 19213 transport of 59Fe'+ from the 3H-schizokinen-59Fe+ chelate at 37 C was accompanied by rapid uptake and release (within 2 min) of 3H-schizokinen, although 3H-schizokinen discharge was temperature-dependent and did not occur at 0 C. In the schizokinen-requiring strain B. megaterium SK11 similar release of 3H-schizokinen occurred only at elevated concentrations of the double-labeled chelate; at lower chelate concentrations, 'H-schizokinen remained cell-associated. Temperature-dependent uptake of deferri (iron-free) 3H-schizokinen to levels equivalent to those incorporated from the chelate form was noted in strain SK11, but strain ATCC 19213 showed only temperature-independent binding of low concentrations of deferri 3H-schizokinen. These results indicate an initial temperature-independent binding of the ferric hydroxamate which is followed rapidly by temperature-dependent transport of the chelate into the cell and an enzyme catalyzed separation of iron from the chelate. The resulting deferri hydroxamate is discharged from the cell only when a characteristic intracellular concentration of the hydroxamate is exceeded, which happens in the schizokinenrequiring strain only at elevated concentrations of the chelate. This strain also appears to draw the deferri hydroxamate into the cell by a temperature-dependent mechanism. The aerobactin-producing organism Aerobacter aerogenes 62-1 also demonstrated rapid initial uptake and temperature-dependent discharge of 'H-aerobactin during iron transport from 3H-aerobactin-59Fe'+, suggesting a similar ferric hydroxamate transport system in this organism.