M?ssbauer study of Clostridium pasteurianum hydrogenase II. Evidence for a novel three-iron cluster

Hydrogenase II contains two iron-sulfur clusters, one of the [4Fe-4S] type and one of unknown structure with unusual spectral properties (H-cluster). Using M?ssbauer spectroscopy we have studied the H-cluster under a variety of conditions. In the reduced state the cluster exhibits, in zero magnetic field, spectra with the typical 2:1 quadrupole pattern of reduced [3Fe-4S] clusters. However, whereas the latter are paramagnetic (S = 2) the H-cluster is diamagnetic (S = 0). Upon oxidation and exposure to CO the H-cluster exhibits an S = 1/2 EPR spectrum with g values at 2.03, 2.02, and 2.00. In this state, the M?ssbauer spectra reveal two cluster subsites with magnetic hyperfine coupling constants AI = +26.5 MHz and AII = -30 MHz. ENDOR data obtained by Hoffman and co-workers (Telser, J., Benecky, M. J., Adams, M. W. W., Mortenson, L. E., and Hoffman, B. M. (1986) J. Biol. Chem. 261, 13536-13541) show a 57Fe resonance at AIII approximately equal to 9.5 MHz. Analysis of the M?ssbauer spectra shows that this resonance represents one iron site. Our studies of the reduced and CO-bound oxidized states of hydrogenase II suggest that the H-cluster contains three iron atoms. The data obtained for the oxidized H-cluster suggest a novel type of 3-Fe cluster and bear little resemblance to those reported for oxidized [3Fe-4S] clusters with g = 2.01 EPR signals. In the reduced sample the [4Fe-4S]1+ cluster appears to occur in a mixture of two distinct electronic states.     

Endonuclease III is an iron-sulfur protein

Elemental analyses, M?ssbauer, and EPR data are reported to show that endonuclease III of Escherichia coli is an iron-sulfur protein. M?ssbauer spectra of protein freshly prepared from E. coli grown on 57Fe-enriched medium demonstrate that the native enzyme contains a single 4Fe-4S cluster in the 2+ oxidation state, with a net spin of zero. Upon treatment with ferricyanide, a fraction (less than 25%) of the clusters is oxidized into a state which yields an EPR spectrum near g = 2.01 typical of a 3Fe-4S cluster. The magnetic field dependence of the linear electric field effect verifies this assignment. Electron spin echo modulation on the g = 2.01 form of the protein in deuterated solvent indicates the presence of exchangeable protons in the vicinity of the 3Fe-4S cluster. The data obtained show that the [4Fe-4S]2+ cluster of the native enzyme is resistant to either oxidation or reduction, although photoreduction elicited a g = 1.94 type EPR signal characteristic of a [4Fe-4S]1+ cluster. These studies show that endonuclease III is unique in being both a DNA repair enzyme and an iron-sulfur protein. The function of the 4Fe-4S cluster remains to be established.     

The anaerobic ribonucleotide reductase from Escherichia coli. The small protein is an activating enzyme containing a [4fe-4s](2+) center.

For deoxyribonucleotide synthesis during anaerobic growth, Escherichia coli cells depend on an oxygen-sensitive class III ribonucleotide reductase. The enzyme system consists of two proteins: protein alpha, on which ribonucleotides bind and are reduced, and protein beta, of which the function is to introduce a catalytically essential glycyl radical on protein alpha. Protein beta can assemble one [4Fe-4S] center per polypeptide enjoying both the [4Fe-4S](2+) and [4Fe-4S](1+) redox state, as shown by iron and sulfide analysis, M?ssbauer spectroscopy (delta = 0.43 mm.s(-1), DeltaE(Q) = 1.0 mm.s(-1), [4Fe-4S](2+)), and EPR spectroscopy (g = 2. 03 and 1.93, [4Fe-4S](1+)). This iron center is sensitive to oxygen and can decompose into stable [2Fe-2S](2+) centers during exposure to air. This degraded form is nevertheless active, albeit to a lesser extent because of the conversion of the cluster into [4Fe-4S] forms during the strongly reductive conditions of the assay. Furthermore, protein beta has the potential to activate several molecules of protein alpha, suggesting that protein beta is an activating enzyme rather than a component of an alpha(2)beta(2) complex as previously claimed.     

The purification and characterization of arsenite oxidase from Alcaligenes faecalis, a molybdenum-containing hydroxylase.

The purification and initial characterization of arsenite oxidase from Alcaligenes faecalis are described. The enzyme consists of a monomer of 85 kDa containing one molybdenum, five or six irons, and inorganic sulfide. In the presence of denaturants arsenite oxidase releases a fluorescent material with spectral properties identical to the pterin cofactor released by the hydroxylase class of molybdenum-containing enzymes. Azurin and a c-type cytochrome, both isolated from A. faecalis, each serves as an electron acceptor to arsenite oxidase and may form a periplasmic electron transfer pathway for arsenite detoxification. Full reduction of arsenite oxidase requires 3-4 reducing equivalents, using either arsenite or dithionite as the electron source. Below 20 K, oxidized arsenite oxidase exhibits an EPR signal with g values of 2.03, 2.01, and 2.00, which integrates to approximately 0.4 spins/protein. Since enrichment in 57Fe results in broadening of this EPR signal, the center giving rise to this signal must contain iron. The most plausible candidates are a [4Fe-4S] high potential iron protein center or a [3Fe-4S] center. The EPR signal observed in oxidized arsenite oxidase disappears upon reduction of the protein with either arsenite or dithionite. Concomitantly, a rhombic EPR signal (g = 2.03, 1.89, 1.76) appears which is similar to that of Rieske-type [2Fe-2S] clusters and spin quantifies to one spin/protein.     

M?ssbauer, EPR, and magnetization studies of the Azotobacter vinelandii Fe protein. Evidence for a [4Fe-4S]1+ cluster with spin S = 3/2

We have studied the Fe protein (Av2) of the Azotobacter vinelandii nitrogenase system with M?ssbauer and EPR spectroscopies and magnetic susceptometry. In the oxidized state the protein exhibits M?ssbauer spectra typical of diamagnetic [4Fe-4S]2+ clusters. Addition of Mg.ATP or Mg.ADP causes a pronounced decline in the quadrupole splitting of the M?ssbauer spectra of the oxidized protein. Our studies show that reduced Av2 in the native state is heterogeneous. Approximately half of the molecules contain a [4Fe-4S]1+ cluster with electronic spin S = 1/2 and half contain a [4Fe-4S]1+ cluster with spin S = 3/2. The former yields the characteristic g = 1.94 EPR signal whereas the latter exhibits signals around g = 5. The magnetization of reduced Av2 is dominated by the spin S = 3/2 form of its [4Fe-4S]1+ clusters. These results explain a long standing puzzle, namely why the integrated spin intensity of the g = 1.94 EPR signal is substantially less than 1 spin/4 Fe atoms. In 50% ethylene glycol, 90% of the clusters are in the spin S = 1/2 form whereas, in 0.4 M urea, 85% are in the S = 3/2 form. In 0.4 M urea, the EPR spectrum of reduced Av2 exhibits well defined resonances at g = 5.8 and 5.15, which we assign to the S = 3/2 system. The EPR and M?ssbauer studies yield a zero-field splitting of 2D approximately equal to -5 cm-1 for this S = 3/2 state.     

The fluidity of plasma membranes of Dictyostelium discoideum. The effects of polyunsaturated fatty acid incorporation assessed by fluorescence depolarization and electron paramagnetic resonance

The absorption spectrum of the hydrogenase from Chromatium, which contains four iron atoms and four atoms of acid-labile sulfide, in 80% dimethylsulfoxide or hexamethylphosphoramide suggests the presence of a single [4Fe-4S] cluster. The EPR spectra of the oxidized enzyme in air, argon or carbon monoxide are the same with signals centered at g = 2.01. The enzyme reduced by hydrogen is EPR silent. The EPR spectrum is consistent with a [4Fe-4S] cluster. Chromatium hydrogenase and the hydrogenase from Proteus vulgaris show relative stability towards denaturation by sodium dodecyl sulfate (SDS), urea, guanidine and organic solvents.     

Identification of FX in the heliobacterial reaction center as a [4Fe-4S] cluster with an S = 3/2 ground spin state

Type I homodimeric reaction centers, particularly the class present in heliobacteria, are not well understood. Even though the primary amino acid sequence of PshA in Heliobacillus mobilis has been shown to contain an F(X) binding site, a functional Fe-S cluster has not been detected by EPR spectroscopy. Recently, we reported that PshB, which contains F(A)- and F(B)-like Fe-S clusters, could be removed from the Heliobacterium modesticaldum reaction center (HbRC), resulting in 15 ms lifetime charge recombination between P798(+) and an unidentified electron acceptor [Heinnickel, M., Shen, G., Agalarov, R., and Golbeck, J. H. (2005) Biochemistry 44, 9950-9960]. We report here that when a HbRC core is incubated with sodium dithionite in the presence of light, the 15 ms charge recombination is replaced with a kinetic transient in the sub-microsecond time domain, consistent with the reduction of this electron acceptor. Concomitantly, a broad and intense EPR signal arises around g = 5 along with a minor set of resonances around g = 2 similar to the spectrum of the [4Fe-4S](+) cluster in the Fe protein of Azotobacter vinelandii nitrogenase, which exists in two conformations having S = (3)/(2) and S = (1)/(2) ground spin states. The M?ssbauer spectrum in the as-isolated HbRC core shows that all of the Fe is present in the form of a [4Fe-4S](2+) cluster. After reduction with sodium dithionite in the presence of light, approximately 65% of the Fe appears in the form of a [4Fe-4S](+) cluster; the remainder is in the [4Fe-4S](2+) state. Analysis of the non-heme iron content of HbRC cores indicates an antenna size of 21.6 +/- 1.1 BChl g molecules/P798. The evidence indicates that the HbRC contains a [4Fe-4S] cluster identified as F(X) that is coordinated between the PshA homodimer; in contrast to F(X) in other type I reaction centers, this [4Fe-4S] cluster exhibits an S = (3)/(2) ground spin state.     

Spectroscopic studies of the nature of the iron clusters in the soluble hydrogenase from Desulfovibrio desulfuricans (strain Norway 4)

57Fe-enriched samples of the soluble hydrogenase from Desulfovibrio desulfuricans (Norway) have been investigated in both the native (oxidized) and the dithionite-reduced states using M?ssbauer spectroscopy. The data clearly show that the iron in this enzyme is predominantly in the form of iron-sulphur clusters which are closely similar to the [4Fe-4S] clusters found in a large number of ferredoxins, such as that from Bacillus stearothermophilus. There appear to be two [4Fe-4S] clusters. The iron-sulphur clusters in the oxidized protein are virtually diamagnetic, as indicated by M?ssbauer, electron spin resonance and magnetic circular dichroic spectroscopy. On reduction by dithionite + methyl viologen, M?ssbauer spectroscopy showed that only 50% of the [4Fe-4S] clusters were reduced. Even reduction with hydrogen up to a pressure of 23 GPa did not reduce the iron-sulphur clusters completely. An ESR signal due to a rapidly relaxing species with g = 2.03, 1.89 was observed in the reduced protein, together with a weaker spectrum from a slower-relaxing species at g = 2.34, 2.12.     

Biogenesis of iron-sulfur clusters in photosystem I: holo-NfuA from the cyanobacterium Synechococcus sp. PCC 7002 rapidly and efficiently transfers [4Fe-4S] clusters to apo-PsaC in vitro

The NfuA protein has been postulated to act as a scaffolding protein in the biogenesis of photosystem (PS) I and other iron-sulfur (Fe/S) proteins in cyanobacteria and chloroplasts. To determine the properties of NfuA, recombinant NfuA from Synechococcus sp. PCC 7002 was overproduced and purified. In vitro reconstituted NfuA contained oxygen- and EDTA-labile Fe/S cluster(s), which had EPR properties consistent with [4Fe-4S] clusters. After reconstitution with 57Fe2+, M?ssbauer studies of NfuA showed a broad quadrupole doublet that confirmed the presence of [4Fe-4S]2+ clusters. Native gel electrophoresis under anoxic conditions and chemical cross-linking showed that holo-NfuA forms dimers and tetramers harboring Fe/S cluster(s). Combined with iron and sulfide analyses, the results indicated that one [4Fe-4S] cluster was bound per NfuA dimer. Fe/S cluster transfer from holo-NfuA to apo-PsaC of PS I was studied by reconstitution of PS I complexes using P700-F(X) core complexes, PsaD, apo-PsaC, and holo-NfuA. Electron transfer measurements by time-resolved optical spectroscopy showed that holo-NfuA rapidly and efficiently transferred [4Fe-4S] clusters to PsaC in a reaction that required contact between the two proteins. The NfuA-reconstituted PS I complexes had typical charge recombination kinetics from [F(A)/F(B)](-) to P700+ and light-induced low-temperature EPR spectra. These results establish that cyanobacterial NfuA can act as a scaffolding protein for the insertion of [4Fe-4S] clusters into PsaC of PS I in vitro.     

M?ssbauer and electron nuclear double resonance study of oxidized bidirectional hydrogenase from Clostridium pasteurianum W5

The bidirectional hydrogenase from Clostridium pasteurianum W5 is an iron-sulfur protein containing approximately 12 Fe atoms and 12 labile sulfides. We have studied oxidized samples of the enzyme with M?ssbauer and electron nuclear double resonance (ENDOR) spectroscopy to elucidate the nature of the center that gives rise to the EPR signal with principal g-values at 2.10, 2.04, and 2.01. The g = 2.10 center exhibits two well-resolved 57Fe ENDOR resonances. One is isotropic with A1 = 9.5 MHz; the other is nearly isotropic with A2 = 17 MHz. These magnetic hyperfine coupling constants are substantially (approximately 50%) smaller than those observed for [2Fe-2S], [3Fe-4S], and [4Fe-4S] clusters. The M?ssbauer and ENDOR data, taken together, suggest that the g = 2.10 center contains at least two but not more than four iron atoms. Comparison of our data with recent results reported for Escherichia coli sulfite reductase and the ferricyanide-treated [4Fe-4S] cluster from Azotobacter vinelandii ferredoxin I suggests that the g = 2.10 center may possibly be formed, by oxidation, from a structure with a [4Fe-4S] core. The M?ssbauer spectra give evidence that at least 8 of the 12 Fe atoms of oxidized hydrogenase are organized in two ferredoxin-type [4Fe-4S] clusters, supporting conclusions derived previously from EPR studies of the reduced enzyme.     

Characterization of a sulfite reductase from Desulfovibrio vulgaris. Evidence for the presence of a low-spin siroheme and an exchange-coupled siroheme-[4Fe-4S] unit

We have studied a low-molecular-weight (Mr = 27,200) sulfite reductase from Desulfovibrio vulgaris (Hildenborough, NCIB 8303) with M?ssbauer, EPR, and chemical techniques. This sulfite reductase was found to contain one siroheme and one [4Fe-4S] cluster. As purified, the siroheme is low-spin ferric (S = 1/2) which exhibits characteristic EPR resonances at g = 2.44, 2.36, and 1.77. At 150 K, the observed M?ssbauer parameters, delta EQ = 2.49 +/- 0.02 mm/s and delta = 0.31 +/- 0.02 mm/s, for the siroheme are typical for low-spin ferric complexes. The [4Fe-4S] cluster is in the 2+ state. The M?ssbauer parameters, delta EQ = 0.95 +/- 0.02 mm/s and delta = 0.38 +/- 0.02 mm/s, for the cluster are almost identical to those observed for the [4Fe-4S]2+ cluster in the hemoprotein subunit of the sulfite reductase from Escherichia coli. Similar to the hemoprotein subunit of E. coli sulfite reductase, low-temperature M?ssbauer spectra of D. vulgaris sulfite reductase recorded with weak and strong applied fields also show evidence for an exchange-coupled siroheme-[4Fe-4S] unit.     

Unusual features in EPR and M?ssbauer spectra of the 2[4Fe-4Se]+ ferredoxin from Clostridium pasteurianum

The electronic and magnetic properties of the selenium-substituted 2[4Fe-4Se]2+/+ ferredoxin (Fd) from Clostridium pasteurianum have been investigated by EPR and M?ssbauer spectroscopy. The [4Fe-4Se]2+ clusters of oxidized Fd are diamagnetic and the M?ssbauer spectra are nearly identical to those of oxidized 2[4Fe-4S]2+ Fd. The addition of 2e- per molecule of Se-substituted Fd causes the simultaneous appearance of three EPR signals: one (g1,2,3 = 2.103, 1.940, 1.888) is reminiscent of [4Fe-4S]+ EPR spectra and accounts for 0.7 to 0.8 spin/molecule. The two others consist of a broad signal with g = 4.5, 3.5, and approximately 2 (0.7 to 0.8 spin/molecule) and of a narrow peak at g = 5.172 which is observed up to 60 K. Peculiar features are also present in the M?ssbauer spectra of 2[4Fe-4Se]+ Fd below 20 K: a subcomponent with lines near to +/- 4 mm/s and accounting for 20% of the total iron corresponds to two antiferromagnetically coupled sites in approximately a 3:1 ratio and displays fully developed paramagnetic hyperfine interactions at 4.2 K without any applied field. At 77 K, however, the reduced Se-substituted Fd yields a M?ssbauer spectrum similar to that of 2[4Fe-4S]+ Fd. The new EPR and M?ssbauer spectroscopic features of the 2[4Fe-4Se]+ Fd are attributed to S = 3/2 and S = 7/2 spin states which accompany the classical S = 1/2 state of [4Fe-4X]+ (X = S, Se) structures.     

DNA-bound redox activity of DNA repair glycosylases containing [4Fe-4S] clusters

MutY and endonuclease III, two DNA glycosylases from Escherichia coli, and AfUDG, a uracil DNA glycosylase from Archeoglobus fulgidus, are all base excision repair enzymes that contain the [4Fe-4S](2+) cofactor. Here we demonstrate that, when bound to DNA, these repair enzymes become redox-active; binding to DNA shifts the redox potential of the [4Fe-4S](3+/2+) couple to the range characteristic of high-potential iron proteins and activates the proteins toward oxidation. Electrochemistry on DNA-modified electrodes reveals potentials for Endo III and AfUDG of 58 and 95 mV versus NHE, respectively, comparable to 90 mV for MutY bound to DNA. In the absence of DNA modification of the electrode, no redox activity can be detected, and on electrodes modified with DNA containing an abasic site, the redox signals are dramatically attenuated; these observations show that the DNA base pair stack mediates electron transfer to the protein, and the potentials determined are for the DNA-bound protein. In EPR experiments at 10 K, redox activation upon DNA binding is also evident to yield the oxidized [4Fe-4S](3+) cluster and the partially degraded [3Fe-4S](1+) cluster. EPR signals at g = 2.02 and 1.99 for MutY and g = 2.03 and 2.01 for Endo III are seen upon oxidation of these proteins by Co(phen)(3)(3+) in the presence of DNA and are characteristic of [3Fe-4S](1+) clusters, while oxidation of AfUDG bound to DNA yields EPR signals at g = 2.13, 2.04, and 2.02, indicative of both [4Fe-4S](3+) and [3Fe-4S](1+) clusters. On the basis of this DNA-dependent redox activity, we propose a model for the rapid detection of DNA lesions using DNA-mediated electron transfer among these repair enzymes; redox activation upon DNA binding and charge transfer through well-matched DNA to an alternate bound repair protein can lead to the rapid redistribution of proteins onto genome sites in the vicinity of DNA lesions. This redox activation furthermore establishes a functional role for the ubiquitous [4Fe-4S] clusters in DNA repair enzymes that involves redox chemistry and provides a means to consider DNA-mediated signaling within the cell.     

Unifying principles in homodimeric type I photosynthetic reaction centers: properties of PscB and the FA, FB and FX iron-sulfur clusters in green sulfur bacteria

The photosynthetic reaction center from the green sulfur bacterium Chlorobium tepidum (CbRC) was solubilized from membranes using Triton X-100 and isolated by sucrose density ultra-centrifugation. The CbRC complexes were subsequently treated with 0.5 M NaCl and ultrafiltered over a 100 kDa cutoff membrane. The resulting CbRC cores did not exhibit the low-temperature EPR resonances from FA- and FB- and were unable to reduce NADP+. SDS-PAGE and mass spectrometric analysis showed that the PscB subunit, which harbors the FA and FB clusters, had become dissociated, and was now present in the filtrate. Attempts to rebind PscB onto CbRC cores were unsuccessful. M?ssbauer spectroscopy showed that recombinant PscB contains a heterogeneous mixture of [4Fe-4S]2+,1+ and other types of Fe/S clusters tentatively identified as [2Fe-2S]2+,1+ clusters and rubredoxin-like Fe3+,2+ centers, and that the [4Fe-4S]2+,1+ clusters which were present were degraded at high ionic strength. Quantitative analysis confirmed that the amount of iron and sulfide in the recombinant protein was sub-stoichiometric. A heme-staining assay indicated that cytochrome c551 remained firmly attached to the CbRC cores. Low-temperature EPR spectroscopy of photoaccumulated CbRC complexes and CbRC cores showed resonances between g=5.4 and 4.4 assigned to a S=3/2 ground spin state [4Fe-4S]1+ cluster and at g=1.77 assigned to a S=1/2 ground spin state [4Fe-4S]1+ cluster, both from FX-. These results unify the properties of the acceptor side of the Type I homodimeric reaction centers found in green sulfur bacteria and heliobacteria: in both, the FA and FB iron-sulfur clusters are present on a salt-dissociable subunit, and FX is present as an interpolypeptide [4Fe-4S]2+,1+ cluster with a significant population in a S=3/2 ground spin state.     

Direct spectroscopic evidence for the presence of a 6Fe cluster in an iron-sulfur protein isolated from Desulfovibrio desulfuricans (ATCC 27774)

A novel iron-sulfur protein was purified from the extract of Desulfovibrio desulfuricans (ATCC 27774) to homogeneity as judged by polyacrylamide gel electrophoresis. The purified protein is a monomer of 57 kDa molecular mass. It contains comparable amounts of iron and inorganic labile sulfur atoms and exhibits an optical spectrum typical of iron-sulfur proteins with maxima at 400, 305, and 280 nm. M?ssbauer data of the as-isolated protein show two spectral components, a paramagnetic and a diamagnetic, of equal intensity. Detailed analysis of the paramagnetic component reveals six distinct antiferromagnetically coupled iron sites, providing direct spectroscopic evidence for the presence of a 6Fe cluster in this newly purified protein. One of the iron sites exhibits parameters (delta EQ = 2.67 +/- 0.03 mm/s and delta = 1.09 +/- 0.02 mm/s at 140 K) typical for high spin ferrous ion; the observed large isomer shift indicates an iron environment that is distinct from the tetrahedral sulfur coordination commonly observed for the iron atoms in iron-sulfur clusters and is consistent with a penta- or hexacoordination containing N and/or O ligands. The other five iron sites are most probably high spin ferric. Three of them show parameters characteristic for tetrahedral sulfur coordination. In correlation with the EPR spectrum of the as-purified protein which shows a resonance signal at g = 15.3 and a group of signals between g = 9.8 and 5.4, this 6Fe cluster is assigned to an unusual spin state of 9/2 with zero field splitting parameters D = -1.3 cm-1 and E/D = 0.062. Other EPR signals attributable to minor impurities are also observed at the g = 4.3 and 2.0 regions. The diamagnetic M?ssbauer component represents a second iron cluster, which, upon reduction with dithionite, displays an intense S = 1/2 EPR signal with g values at 2.00, 1.83, and 1.31. In addition, an EPR signal of the S = 3/2 type is also observed for the dithionite-reduced protein.     

Elucidation of a [4Fe-4S] cluster degradation pathway: rapid kinetic studies of the degradation of Chromatium vinosum HiPIP

Irreversible disassembly of the 4Fe-4S cluster in Chromatium vinosum high-potential iron protein (HiPIP) has been investigated in the presence of a low concentration of guanidinium hydrochloride. From the dependence of degradation rate on [H+], it is deduced that at least three protons are required to trigger efficient cluster degradation. Under these conditions the protonated cluster shows broadened M?ssbauer signals, but delta EQ (1.1 mm/s) and delta (0.44 mm/s) are similar to the native form. Collapse of the protonated transition state complex, revealed by rapid-quench M?ssbauer experiments, occurs with a measured rate constant kobs approximately 0.72 +/- 0.35 s-1 that is consistent with results from time-resolved electronic absorption and fluorescence (kobs approximately 0.4 +/- 0.1 s-1) and EPR (kobs approximately 0.62 +/- 0.18 s-1) measurements. Apparently, guanidinium hydrochloride serves to perturb the tertiary structure of the protein, facilitating protonation of the cluster, but not degradation per se. Release of iron ions occurs even more slowly with kobs approximately 0.07 +/- 0.02 s-1, as determined by the appearance of the g = 4.3 EPR signal. Proton-mediated cluster degradation is sensitive to the oxidation state of the cluster, with the oxidized state showing a two-fold slower rate in acidic solutions as a result of increased electrostatic repulsion with the cluster. Consistent results are obtained from absorption, fluorescence, M?ssbauer and EPR measurements.     

A pure S = 3/2 [Fe4S4]+ cluster in the A33Y variant of Pyrococcus furiosus ferredoxin.

The properties of the [4Fe-4S]2+/+ cluster in wild-type and the A33Y variant of Pyrococcus furiosus ferredoxin have been investigated by the combination of EPR, variable-temperature magnetic circular dichroism (VTMCD) and resonance Raman (RR) spectroscopies. The A33Y variant involves the replacement of an alanine whose alpha-C is less than 4 A from one of the cluster iron atoms by a tyrosine residue. Although the spectroscopic results give no indication of tyrosyl cluster ligation, the presence of a tyrosine residue in close proximity to the cluster results in a 38-mV decrease in the midpoint potential of the [4Fe-4S]2+/+ couple and has a marked effect on the ground state properties of the reduced cluster. The mixed spin [4Fe-4S]+ cluster in the wild-type protein, 80% S = 3/2 (E/D = 0.22, D = +3.3 cm(-1)) and 20% S = 1/2 (g = 2.10, 1.87, 1.80), is converted into a homogeneous S = 3/2 (E/D = 0.30, D = -0.7 cm(-1)) form in the A33Y variant. As the first example of a pure S = 3/2 [4Fe-4S]+ cluster in a ferredoxin, this variant affords the opportunity for detailed characterization of the excited electronic properties via VTMCD studies and demonstrates that the protein environment can play a crucial role in determining the ground state properties of [4Fe-4S]+ clusters.     

M?ssbauer studies of Escherichia coli sulfite reductase complexes with carbon monoxide and cyanide. Exchange coupling and intrinsic properties of the [4Fe-4S] cluster

M?ssbauer studies of the hemoprotein subunit (SiR) of E. coli sulfite reductase have shown that the siroheme and the [4Fe-4S] cluster are exchange-coupled. Here we report M?ssbauer studies of SiR complexed with either CO or CN- and of SiR in the presence of the chaotropic agent dimethyl sulfoxide (Me2SO). The spectra of one-electron-reduced SiR X CN show that all five iron atoms reside in a diamagnetic environment; the ferroheme X CN complex is low spin and the [4Fe-4S] cluster is in the 2+ oxidation state. Titration with ferricyanide affords a CN- complex of oxidized SiR in which the siroheme iron is low spin ferric, with the cluster remaining in the 2+ state. At low temperatures, paramagnetic hyperfine interactions are observed for the iron sites of the cluster, suggesting that it is exchange-coupled to the heme iron. Reduction of one-electron-reduced SiR X CN and SiR X CO yields complexes with "g = 1.94"-type EPR signals showing that the second electron is accommodated by the iron-sulfur cluster. The fully reduced complexes yield well resolved M?ssbauer spectra which were analyzed in the spin Hamiltonian formalism. The analysis shows that the cluster subsites are equivalent in pairs, one pair having properties reminiscent of ferric sites whereas the other pair has features more typical of ferrous sites. The M?ssbauer spectra of oxidized SiR kept in 60% (v/v) Me2SO are virtually identical with those observed for SiR in standard buffer, implying that the coupling is maintained in the presence of the chaotrope. Fully reduced SiR displays an EPR signal with g values of g = 2.53, 2.29, and 2.07. In 60% Me2SO, this signal vanishes and a g = 1.94 signal develops; this transition is accompanied by a change in the spin state of the heme iron from S = 1 (or 2) to S = O.     

Plant adenosine 5'-phosphosulfate reductase is a novel iron-sulfur protein.

Adenosine 5'-phosphosulfate reductase (APR) catalyzes the two-electron reduction of adenosine 5'-phosphosulfate to sulfite and AMP, which represents the key step of sulfate assimilation in higher plants. Recombinant APRs from both Lemna minor and Arabidopsis thaliana were overexpressed in Escherichia coli and isolated as yellow-brown proteins. UV-visible spectra of these recombinant proteins indicated the presence of iron-sulfur centers, whereas flavin was absent. This result was confirmed by quantitative analysis of iron and acid-labile sulfide, suggesting a [4Fe-4S] cluster as the cofactor. EPR spectroscopy of freshly purified enzyme showed, however, only a minor signal at g = 2.01. Therefore, M?ssbauer spectra of (57)Fe-enriched APR were obtained at 4.2 K in magnetic fields of up to 7 tesla, which were assigned to a diamagnetic [4Fe-4S](2+) cluster. This cluster was unusual because only three of the iron sites exhibited the same M?ssbauer parameters. The fourth iron site gave, because of the bistability of the fit, a significantly smaller isomer shift or larger quadrupole splitting than the other three sites. Thus, plant assimilatory APR represents a novel type of adenosine 5'-phosphosulfate reductase with a [4Fe-4S] center as the sole cofactor, which is clearly different from the dissimilatory adenosine 5'-phosphosulfate reductases found in sulfate reducing bacteria.