We heterologously overproduced a hyperthermostable archaeal low potential (E m ؍ ؊62 mV) Rieske-type ferredoxin (ARF) from Sulfolobus solfataricus strain P-1 and its variants in Escherichia coli to examine the influence of ligand substitutions on the properties of the [2Fe-2S] cluster. While two cysteine ligand residues (Cys 42 and Cys 61 ) are essential for the cluster assembly and/or stability, the contributions of the two histidine ligands to the cluster assembly in the archaeal Riesketype ferredoxin appear to be inequivalent as indicated by much higher stability of the His 64 Proteins containing Rieske-type [2Fe-2S] clusters are widespread in nature from hyperthermophilic Archaea and Bacteria to Eukarya and play critical electron transfer roles in various pathways such as aerobic respiration, photosynthesis, and biodegradation of various alkene and aromatic compounds (1-4). In contrast to regular plant-and vertebrate-type ferredoxins having complete cysteinyl ligations, the Rieske-type cluster has an asymmetric iron-sulfur core with the S ␥ atom of each of the two cysteine residues coordinated to one iron site and the N ␦ atom of each of the two histidine residues coordinated to the other iron site. This asymmetric ligation results in some unique redox and spectroscopic properties (for reviews, see Refs. 1 and 3-5). This cluster coordination was firmly established by recent x-ray crystal structures of several different Rieske-type protein domains (6 -11).Two different types of Rieske clusters are observed in proteins. One type displays higher reduction potentials (E m ) 1 of approximately ϩ150 to ϩ490 mV and occurs in proton-translocating respiratory complexes (cytochrome bc 1 /b 6 f complexes and their archaeal homologs without c-type cytochromes), being involved in not only electron transfer but also substrate binding and oxidation at the quinol-oxidizing Q o site (2-5, 12-15). The other type displays lower E m values of approximately Ϫ150 to Ϫ50 mV and has been found in a diverse group of bacterial multicomponent terminal oxygenases and soluble Rieske-type ferredoxins (1, 3, 8, 9, 16 -27). However, none of the latter class has been characterized in detail from any archaeal species.We recently found that the genomic DNA sequence of the thermoacidophilic archaeon Sulfolobus solfataricus strain P-1 (DSM 1616T) encodes an archaeal homolog of bacterial small Rieske-type ferredoxins with no consensus disulfide signature (DDBJ accession number AB047031 (27)). This arf gene was found by homology search against the deduced amino acid sequence of Sulfolobus tokodaii sulredoxin, a water-soluble homolog of a high potential Rieske protein (E m,low pH ϳ ϩ190 mV) with a consensus disulfide linkage (DDBJ accession number AB023295) 2 (28 -30) (Fig. 1). Subsequent cloning and heterologous overexpression in Escherichia coli of this S. solfataricus arf gene encoding the archaeal Rieske-type ferredoxin (ARF) (27) have provided an opportunity to define the influence of surrounding amino acid residues on the electronic and s...
The purified 2-oxoacid:ferredoxin oxidoreductase of a thermoacidophilic and aerobic crenarchaeote, Sulfolobus sp. strain 7, consists of 70-kDa alpha and 37-kDa beta subunits, and contains one thiamine pyrophosphate (TPP), one [4Fe-4S]2+.1+ cluster, and two magnesium atoms per alpha beta structure. It exhibits a broad substrate specificity toward 2-oxoacids such as 2-oxoglutarate, 2-oxobutyrate, and pyruvate. The gene encoding the archaeal oxidoreductase was cloned, and the two open reading frames encoding the alpha (632 amino acids) and beta subunits (305 amino acids), respectively, were sequenced. Careful sequence alignment revealed several consensus motifs of this enzyme family, as well as possible cofactor binding residues of the Sulfolobus enzyme. This new structural information also indicates that (i) several genetic fusions and reorganization of the early, possibly alpha beta gamma delta-type enzyme similar to those from hyperthermophiles have taken place during evolution of the 2-oxoacid:ferredoxin (flavodoxin) oxidoreductase superfamily, which might have occurred in different ways in early aerobic archaea and early anaerobic bacteria, and that (ii) enzymes with different subunit compositions should have an essentially similar catalytic mechanism with one TPP and at least one [4Fe-4S] cluster as the minimal set of redox centers.
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