The primary structure of the split-Soret cytochrome c from Desulfovibrio desulfuricans ATCC 27774 reveals an unusual type of diheme cytochrome c.

The complete amino acid sequence of the unusual diheme split-Soret cytochrome c from the sulphate-reducing Desulfovibrio desulfuricans strain ATCC 27774 has been determined using classical chemical sequencing techniques and mass spectrometry. The 247-residue sequence shows almost no similarity with any other known diheme cytochrome c, but the heme-binding site of the protein is similar to that of the cytochromes c3 from the sulphate reducers. The cytochrome-c-like domain of the protein covers only the C-terminal part of the molecule, and there is evidence for at least one more domain containing four cysteine residues, which might bind another cofactor, possibly a non-heme iron-containing cluster. This domain is similar to a sequence fragment of the genome of Archaeoglobus fulgidus, which confirms the high conservation of the genes involved in sulfate reduction.

Thiol/disulfide formation associated with the redox activity of the [Fe3S4] cluster of Desulfovibrio gigas ferredoxin II. 1H NMR and Mössbauer spectroscopic study.

Desulfovibrio gigas ferredoxin II (FdII) is a small protein (alpha 4 subunit structure as isolated; M(r) approximately 6400 per subunit; 6 cysteine residues) containing one Fe3S4 cluster per alpha-subunit. The x-ray structure of FdII has revealed a disulfide bridge formed by Cys-18 and Cys-42 approximately 13 A away from the center of the cluster; moreover, the x-ray structure indicates that Cys-11 forms a disulfide bridge with a methanethiol. In the oxidized state, FdIIoxm the 1H NMR spectra, exhibit four low-field contact-shifted resonances at 29, 24, 18, and 15.5 ppm whereas the reduced state, FdIIR (S = 2), yields two features at +18.5 and -11 ppm. In the course of studying the redox behavior of FdII, we have discovered a stable intermediate, FdIIint, that yields 1H resonances at 24, 21.5, 21, and 14 ppm. This intermediate appears in the potential range where the cluster (E'0 approximately -130 mV) is reduced from the [Fe3S4]1+ to the [Fe3S4]0 state. FdIIint is observed during reductive titrations with dithionite or hydrogen/hydrogenase or after partial oxidation of FdIIR by 2,6-dichlorophenolindophenol or air. Our studies show that a total of three electrons per alpha-subunit are transferred to FdII. Our experiments demonstrate the absence of a methanethiol-Cys-11 linkage in our preparations, and we propose that two of the three electrons are used for the reduction of the disulfide bridge. Mössbauer (and EPR) studies show that the Fe3S4 cluster of FdIIint is at the same oxidation level as FdIIox, but indicate some changes in the exchange couplings among the three ferric sites. Our data suggest that the differences in the NMR and Mössbauer spectra of FdIIox and FdIIint result from conformational changes attending the breaking or formation of the disulfide bridge. The present study suggests that experiments be undertaken to explore an in vivo redox function for the disulfide bridge.

Mössbauer studies of solid thionin-oxidized MoFe protein of nitrogenase.

Recently Hagen et al. (Hagen, W. R., Wassink, H., Eady, R. R., Smith, B. E., and Haaker, H. (1987) Eur. J. Biochem. 169, 457-465) reported the observation of S = 7/2 EPR signals for thionin-oxidized nitrogenase MoFe protein. Here we have studied the protein from Azotobacter vinelandii and Klebsiella pneumoniae with Mössbauer and EPR spectroscopies, with the following results: when the MoFe protein is oxidized by addition of stoichiometric amounts (6-8 equivalents) of dissolved thionin, the well characterized P-cluster state Pox results. Pox has an as yet undetermined, but half-integer electronic spin; however, the state is EPR-silent. In contrast, oxidation by addition of a large excess of solid thionin powder, the method used by Hagen et al., yields mixtures with variable proportions of two oxidized P-cluster forms, namely the familiar Pox and the new state Pox(S = 7/2) observed by Hagen et al. The Mössbauer data suggest that Pox and Pox(S = 7/2) are isoelectronic. The two states, however, have distinct electronic structures; the Mössbauer spectra of Pox exhibit the characteristic trapped-valence Fe2+ site, whereas the spectra of Pox(S = 7/2) lack this feature. Hagen et al. have proposed two new P-cluster models. We conclude that one of the models is incompatible with the Mössbauer data and that the basic assumptions of the other model are not supported by the available data. Finally, the Mössbauer data show that either oxidation method puts the cofactor centers into the diamagnetic state Mox.

Isotopic hybrids of nitrogenase. Mössbauer study of MoFe protein with selective 57Fe enrichment of the P-cluster.

Previous Mössbauer and EPR studies of the MoFe protein (approximately 30 Fe and 2 Mo) of nitrogenase have revealed the presence of two unique clusters, namely, the P-clusters (presumably of the Fe4S4 type) and the molybdenum- and iron-containing cofactors (or M-clusters). Mössbauer components D (approximately 10-12 Fe) and Fe2+ (approximately 4 Fe) represent subsites of the P-clusters while component S (approximately 2 Fe) appeared to belong to a separate, unidentified cluster. In order to refine the analyses of Mössbauer spectra, we have constructed an isotopic hybrid of the Klebsiella pneumoniae protein which contains 57Fe-enriched P-clusters and 56Fe-enriched M-clusters. The highly resolved 57Fe Mössbauer spectra of this hybrid show that component S behaves spectroscopically like the P-cluster sites D and Fe2+ in oxidized and reduced MoFe protein. This suggests that S is a subset of the P-clusters rather than a different cluster type. The present study shows, for the first time, that the Debye-Waller factors of different P-cluster subsites have a different temperature dependence. Thus, the Fe2+/D absorption ratio is 4.0:10.0 at 4.2 K and 4.0:11.6 at 173 K. We propose that the reduced MoFe protein contains two pairs of P-clusters: one pair containing one Fe2+ and three D-sites and the other one Fe2+, two D, and one S-site. We have argued previously that the oxidized P-clusters occur in pairs as well.