Pyruvate: ferredoxin oxidoreductase and 2‐oxoglutarate: ferredoxin oxidoreductase were obtained from cell‐free extracts of Halobacterium halobium as homogeneous proteins after ammonium sulfate precipitation, salting‐out chromatography with ammonium sulfate on unsubstituted agarose, gel filtration and chromatography on hydroxyapatite. The respective molecular weights are 256000 and 248000. Both enzymes consist of two sets of nonidentical subunits of Mr 86000 and 42000 in the case of the pyruvate‐degrading enzyme and of 88000 and 36000 in the case of the 2‐oxoglutarate‐degrading enzyme. Analyses indicate that an intact enzyme molecule contains two [4 Fe‐4S]2+(2+.1+) clusters and two molecules of thiamin diphosphate. Flavin nucleotides, lipoic acid and pantetheine are absent. Thus the enzymes are very similar to the 2‐oxoacid: ferredoxin oxidoreductases from fermentative and photosynthetic anaerobes described previously, but are clearly different from the 2‐oxoacid dehydrogenase multienzyme complexes which commonly occur in aerobic organisms.

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The catalytic cycle of the 2-oxoacid: ferredoxin oxidoreductases from Halobacterium halobium was investigated. The first step is binding of the 2-oxoacid to the enzyme followed by decarboxylation and transfer of one electron to the [4Fe-4S] cluster of the functional unit. The cluster is then reoxidized by ferredoxin or, in the absence of the physiological electron acceptor, by oxygen. In the resulting stable enzyme-intermediate radical the decarboxylation product of the 2-oxoacid remains tightly bound until reaction with coenzyme A causes formation of acyl-CoA and concomitant transfer of the second electron to the cluster, which again is reoxidized by ferredoxin or oxygen. After purification, part of the enzyme molecules still contain the intermediate radical. Enzyme preparations either free of radical or containing enhanced amounts are obtained by treatment with coenzyme A or 2-oxoacid, respectively. Whenever the radical is present in an enzyme molecule the respective binding site for the 2-oxoacid is blocked.

The amino acid sequence of a ferredoxin from a thermoacidophilic archaebacterium, Sulfolobus acidocaldarius, was determined by a combination of various conventional methods to be as follows: Gly-Ile-Asp-Pro-Tyr-Arg-Thr-His-Lys-Pro-Val-Val-Gly-Asp-Ser-Ser-Gly-His- Lys-Ile -Tyr-Gly-Pro-Val-Glu-Ser-Pro-Lys(Me)-Val-Leu-Gly-Val-His-Gly-Thr-Ile-Val -Gly-Va l-Asp-Phe-Asp-Leu-Cys-Ile-Ala-Asp-Gly-Ser-Cys-Ile-Thr-Ala-Cys-Pro-Val-As n-Val-P he-Gln-Trp-Tyr-Glu-Thr-Pro-Gly-His-Pro-Ala-Ser-Glu-Lys-Lys-Ala-Asp-Pro-V al-Asn- Glu-Gln-Ala-Cys-Ile-Phe-Cys-Met-Ala-Cys-Val-Asn-Val-Cys-Pro-Val-Ala-Ala- Ile-Asp -Val-Lys-Pro-Pro. It was composed of 103 amino acid residues giving a molecular weight of 10,908 excluding Fe and S atoms. This ferredoxin contained an N6-monomethyllysine residue at position 29 which was determined by a comparison of the elution profile of the acid hydrolysates of the protein and peptides on an amino acid analyzer with three methyl derivatives of lysine and also by field desorption mass spectrometry of a purified peptide. The ferredoxin has only 7 cysteine residues, which probably participate in constructing the Fe-S clusters of this ferredoxin, indicating the presence of a unique chelate structure. Comparison of this ferredoxin with other archaebacterial ferredoxins indicated that the archaebacteria might have multiple origins in an evolutionary tree.