Abstract

The oxidized and reduced forms of the [4Fe-4S]-containing ferredoxin from the hyperthermophilic archaeon Pyrococcus furiosus, Pf, have been investigated by 1H nuclear magnetic resonance spectroscopy, electron paramagnetic resonance spectroscopy and thiol titrations. We have identified and isolated at Ambient temperature four distinct redox states for the [4Fe-4S] form of the ferredoxin. These states differ in the redox state of the cluster, which is coordinated by Cys 11, Asp 14, Cys 17, and Cys 56, and of a disulfide bridge between Cys 21 and Cys 48. The protein, as isolated under anaerobic conditions, designated 4Fe FdBred, contains the reduced cluster and two free thiols. The cluster, but not the thiols, is readily oxidized by brief exposure to O2 to yield 4Fe FdBOX. Prolonged O2 treatment (> 24 h at 30 degrees C) is required to generate the protein with a disulfide (4Fe FdAOX) while this fully oxidized form is readily converted by brief reduction with sodium dithionite to the protein with a reduced cluster and a disulfide (4Fe FdAred). Analyses of the magnitude and the number of hyperfine-shifted resonances in each of the four redox states are discussed.

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