The electronic structure of Fe2+ in reaction centers from Rhodopseudomonas sphaeroides. I. Static magnetization measurements.

We have measured the static magnetization of unreduced and reduced reaction centers that vary in their quinone content. Measurements were performed in the temperature range 0.7 degrees K less than T less than 200 degrees K and magnetic fields of up to 10 kG. The electronic g-value, crystal field parameters D, E, and the exchange interaction, J, between the quinone spin and Fe2+ were determined using the spin Hamiltonian formalism. The effective moment mu eff/Fe2+ of both reduced and unreduced samples were determined to be 5.35 +/- 0.15 Bohr magnetons. This shows, in agreement with previous findings, that Fe2+ does not change its valence state when the reaction centers are reduced. Typical values of D congruent to +5 cm-1 and E/D congruent to 0.27 are consistent with Fe being in an octahedral environment with rhombic distortion. The values of D and E were approximately the same for reaction centers having one and two quinones. These findings imply that quinone is most likely not a ligand of Fe. The Fe2+ and the spin on the quinone in reduced reaction centers were found to be coupled with an exchange interaction 0 less than /J/ less than 1 cm-1. The validity of the spin Hamiltonian was checked by using an orbital Hamiltonian to calculate energy levels of the 25 states of the S = 2, L = 2 manifold and comparing the magnetization of the lowest five states with those obtained from the spin Hamiltonian. Using the orbital Hamiltonian, we calculated the position of the first excited quintet state to be 340 cm-1 above the ground state quintet. This is in good agreement with the temperature dependence of the quadrupole splitting as determined by Mossbauer spectroscopy.     

Evidence for variable metal-radical spin coupling in oxoferrylporphyrin cation radical complexes

Oxoferrylporphyrin cation radical complexes were generated by m-chloroperoxybenzoic acid oxidation of the chloro and trifluoromethanesulfonato complexes of tetramesitylporphyrinatoiron(III) [(TMP)Fe] and the trifluoromethanesulfonato complex of tetra(2,6-dichlorophenyl)porphyrinatoiron(III) [TPP(2,6-Cl)Fe]. Coupling between ferryl iron (S = 1) and porphyrin radical (S' = 1/2) spin systems was investigated by M?ssbauer and EPR spectroscopy. The oxoferrylporphyrin cation radical systems generated from the TMP complexes show strong ferromagnetic coupling. Analysis of the magnetic M?ssbauer spectra, using a spin Hamiltonian explicitly including a coupling tensor J, suggests an exchange-coupling constant J greater than 80 cm-1. The EPR spectra show non-zero rhombicity, the origin of which is discussed in terms of contributions from the usual zero-field effects of iron and from iron-radical spin-dipolar interaction. A consistent estimate of zero-field splitting parameter D approximately + 6 cm-1 was obtained by EPR and M?ssbauer measurements. EPR and M?ssbauer parameters are shown to be slightly dependent on solvent, but not on the axial ligand in the starting (TMP)Fe complex. In contrast to the TMP complex, the oxoferrylporphyrin cation radical system generated from [TPP(2,6-Cl)FeOSO2CF3] exhibits M?ssbauer and EPR spectra consistent with weak iron-porphyrin radical coupling of magnitude of J approximately 1 cm-1.     

1H NMR studies of porcine uteroferrin. Magnetic interactions and active site structure

Pink (reduced) uteroferrin exhibits well resolved paramagnetic NMR spectra with resonances ranging from 90 ppm downfield to 70 ppm upfield. The intensities of these signals depend on the degree of reduction and correlate well with the intensity of the EPR signals with gave = 1.74. Analyses of chemical shifts and the temperature dependence of the paramagnetically shifted resonances indicate that the Fe(III)-Fe(II) cluster in the reduced protein exhibits weak antiferromagnetic exchange coupling (-J approximately equal to 10 cm-1), in agreement with the estimate derived from the temperature dependence of the EPR signal intensity. Purple (oxidized) uteroferrin, on the other hand, exhibits no discernible paramagnetically shifted resonances, reflecting either strong antiferromagnetic coupling or an unfavorable electron spin-lattice relaxation time. Evans susceptibility comparisons between pink and purple uteroferrin show that the Fe(III)-Fe(III) cluster in the oxidized protein is more strongly coupled (-J greater than 40 cm-1). This value concurs with low temperature magnetic susceptibility measurements on both the porcine and splenic purple acid phosphatases. The isotropically shifted protons of tyrosine coordinated to the cluster are assigned by comparison with synthetic complexes. Tyrosine, earlier implicated as a ligand by resonance Raman spectroscopy, appears to coordinate only to the ferric site in pink uteroferrin. This is consistent with the relatively invariant extinction coefficients of uteroferrin in its oxidized and reduced forms and the ease of reduction of the nonchromophoric iron compared to its chromophoric partner. Other possible ligands to the cluster include histidine, suggested by the presence of downfield-shifted solvent-exchangeable resonances with appropriate isotropic shifts.     

Magnetization of manganese superoxide dismutase from Thermus thermophilus.

The ground state magnetic properties of manganese superoxide dismutase from Thermus thermophilus in its native and reduced forms have been determined using saturation magnetization data. Parallel EPR measurements were used to verify that commonly encountered paramagnetic impurities were at low concentration relative to the metalloprotein. The native enzyme contains high spin Mn(III) (S = 2) with D = +2.44(5) cm-1 and E/D = 0. The reduced enzyme contains high spin Mn(II) (S = 5/2) with D = +0.50(5) cm-1 and E/D = 0.027. These results are in keeping with the suggestions of several previous groups of workers concerning the permissible oxidation and spin states of the manganese, but the zero field splitting parameters are unlike those of known manganese model compounds. In addition, the extinction coefficient for the visible region absorption maximum of the native enzyme and the corresponding difference extinction coefficient (native minus reduced) have been measured using saturation magnetization data to quantitate Mn(III) present. The result, epsilon 480 = 950(80) M-1 cm-1 (delta epsilon 480 = 740(60) M-1 cm-1) agrees with the previously reported value of epsilon 480 = 910 M-1 cm-1 found by total manganese determination (Sato, S. and Nakazawa, K. (1978) J. Biochem. 83, 1165-1171). The wide variation in the reported visible region extinction coefficients of manganese superoxide dismutases from different sources is discussed.     

The nature of the nitric oxide complexes of lipoxygenase.

The NO complex of lipoxygenase with EPR signals near g = 4.0 is an S = 3/2 system with D approximately 15 cm-1 similar to Fe2+-EDTA-NO. This may result from antiferromagnetic coupling of axial (D greater than E) high spin ferrous iron to NO. The other NO complex of lipoxygenase, with EPR signals below ge, may result from rhombic high spin ferrous iron coupled to NO with D greater than J. The quenching of both signals by a hydroperoxy derivative of linoleic acid probably represents replacement of NO by an oxygen ligand.     

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 binding of molybdate to uteroferrin. Hyperfine interactions of the binuclear center with 95Mo, 1H, and 2H

Uteroferrin, an acid phosphatase with a spin-coupled and redox-active binuclear iron center, is paramagnetic in its pink, enzymatically active, mixed-valence (S = 1/2) state. Phosphate, a product and inhibitor of the enzymatic activity of uteroferrin, converts the pink, EPR-active form of the protein to a purple, EPR-silent species. In contrast, molybdate, a tetrahedral oxyanion analog of phosphate, transforms the EPR spectrum of uteroferrin from a rhombic to an axial form. With both electron spin echo envelope modulation (ESEEM) and electron nuclear double resonance (ENDOR) spectroscopies, we observe a hyperfine interaction of [95Mo]molybdate with the S = 1/2, Fe(II)-Fe(III) center of the protein. A pair of 95Mo resonances centered at the 95Mo Larmor frequency at the applied magnetic field and separated by a hyperfine coupling constant of 1.2 MHz is evident. Therefore, a single monomeric species of molybdate is close to, and likely a ligand of, the binuclear cluster. 1H ENDOR studies on uteroferrin reveal at least six sets of lines mirrored about the 1H Larmor frequency. Two pairs of these lines become reduced in intensity when the protein is exchanged against D2O. Moreover, ESEEM and 2H ENDOR spectra display resonances at the 2H Larmor frequency. Therefore, the metal-binding region of the protein is accessible to solvent. Additional deuterium lines observable by ESEEM spectroscopy provide evidence for a population of strongly coupled, readily exchangeable protons associated with the binuclear center. The measured hyperfine coupling constants for these deuterons are orientation-dependent with splittings of nearly 4 MHz at g3 = 1.59 and less than 1 MHz at g1 = 1.94. In the presence of molybdate, ESEEM spectra of D2O-exchanged samples reveal a resonance at the 2H Larmor frequency, with no evidence of spectral components due to strongly coupled deuterons. 1H ENDOR studies of the uteroferrin-molybdate complex show at least seven pairs of lines, mirrored about the 1H Larmor frequency, of which one pair becomes attenuated in amplitude upon deuteration. The active site thus remains accessible to solvent in the presence of molybdate.     

Magnetization of the oxidized and reduced three-iron cluster of Desulfovibrio gigas ferredoxin II

The saturation magnetizations of the three iron cluster of ferredoxin II of Desulfovibrio gigas in both the oxidized and reduced states have been studied at fixed magnetic fields up to 4.5 tesla over the temperature range from 1.8 to 200 K. The low field (0.3 tesla) susceptibility of oxidized ferredoxin II obeys the Curie law over this entire temperature range. This establishes -2Jox greater than 200 cm-1 as the lower limit for the antiferromagnetic exchange coupling of oxidized ferredoxin II. The saturation magnetizations of reduced ferredoxin II at several fixed fields yield a nested family of curves which can be fit with spin S = 2 and D = -2.7(4) cm-1 (with E/D assigned the value 0.23 as determined by M?ssbauer and EPR spectra). The low field susceptibility of reduced ferredoxin II also obeys the Curie law from approximately 4 up to 200 K. This establishes -2Jred greater than 40 cm-1 as the lower limit for the antiferromagnetic coupling of reduced ferredoxin II.     

Initial iron oxidation in horse spleen apoferritin. Characterization of a mixed-valence iron(II)-iron(III) complex.

In ferritin, iron is stored by oxidative deposition of the ferrous ion to form a hydrous ferric oxide mineral core. Two intermediates, formed during the initial stages of iron accumulation in apoferritin, have been observed previously in our laboratory and have been identified as a mononuclear Fe3(+)-protein complex and a mixed-valence Fe2(+)-Fe3(+)-protein complex. The physical characteristics of the mixed-valence Fe2(+)-Fe3+ complex and its relationship to the mononuclear Fe3+ complex in horse spleen apoferritin samples to which 0-240 iron atoms were added was examined by EPR spectroscopy. The results indicate that the mononuclear complex is not a precursor to the formation of the mixed-valence complex. Competitive binding studies with Cd2+, Zn2+, Tb3+, and UO2+(2) suggest that the mixed-valence complex is formed on the interior of the protein in the vicinity of the 2-fold axis of the subunit dimer. The mixed-valence complex could be generated by the partial oxidation of Fe2+ in apoferritin containing 120 Fe2+ or by the addition of up to 120 Fe2+ to ferritin already containing 18 Fe3+/protein molecule. The fact that the complex is generated during early Fe2+ oxidation suggests that it may be a key intermediate during the initial oxidative deposition of iron in the protein. The unusual EPR powder lineshape at 9.3 GHz of the mixed-valence complex was simulated with a rhombic g-tensor (gx = 1.95, gy = 1.88, gz = 1.77) and large linewidths and g-strain parameters. The presence of significant g-strain in the complex probably accounts for the failure to observe an EPR signal at 35 GHz and likely reflect considerable flexibility in the structure of the metal site. The temperature dependence of the EPR intensity in the range 8-38 K was modeled successfully by an effective spin Hamiltonian including exchange coupling (-2JS1.S2) and zero-field terms, from which an antiferromagnetic coupling of J = -4.0 +/- 0.5 cm-1 was obtained. This low value for J may reflect the presence of a mu-oxo bridge(s) in the dimer.     

Electron paramagnetic resonance investigation of photosynthetic reaction centers from Rhodobacter sphaeroides R-26 in which Fe2+ was replaced by Cu2+. Determination of hyperfine interactions and exchange and dipole-dipole interactions between Cu2+ and QA-.

We report electron paramagnetic resonance (EPR) experiments in frozen solutions of unreduced and reduced photosynthetic reaction centers (RCs) from Rhodobacter sphaeroides R-26 in which Fe2+ has been chemically replaced by the isotope 65Cu2+. Samples in which the primary quinone acceptor QA is unreduced (Cu2+QA:RCs) give a powder EPR spectrum typical for Cu2+ having axial symmetry, corresponding to a d(x2 - y2) ground state orbital, with g values g parallel = 2.314 +/- 0.001 and g perpendicular = 2.060 +/- 0.003. The spectrum shows a hyperfine structure for the nuclear spin of copper (65I = 3/2) with A parallel = (-167 +/- 1) x 10(-4) cm-1 and /A perpendicular/ = (16 +/- 2) x 10(-4) cm-1, and hyperfine couplings with three nitrogen ligands. This has been verified in samples containing the naturally occurring 14N isotope (l = 1), and in samples where the nitrogen ligands to copper were replaced by the isotope 15N (l = 1/2). We introduce a model for the electronic structure at the position of the metal ion which reflects the recently determined three-dimensional structure of the RCs of Rb. sphaeroides (Allen, J. P., G. Feher, T. O. Yeates, H. Komiya, and D. C. Rees. 1987. Proc. Natl. Acad. Sci. USA. 84:5730: Allen, J. P., G. Feher, T. O. Yeates, H. Komiya, and D. C. Rees. 1988. Proc. Natl. Acad. Sci. USA, 85:8487) as well as our EPR results. In this model the copper ion is octahedrally coordinated to three nitrogens from histidine residues and to one carboxylate oxygen from a glutamic acid, forming a distorted square in the plane of the d(x2 = y2) ground state orbital. It is also bound to a nitrogen of another histidine and to the other carboxylate oxygen of the same glutamic acid residue, in a direction approximately normal to this plane. The EPR spectrum changes drastically when the quinone acceptor QA is chemically reduced (Cu2+QA-:RCs); the change is due to the exchange and dipole-dipole interactions between the Cu2+ and QA- spins. A model spin Hamiltonian proposed for this exchange coupled cooper-quinone spin dimer accounts well for the observed spectra. From a comparison of the EPR spectra of the Cu2+QA:RC and CU2+QA-:RC complexes we obtain the values /J0/ = (0.30 +/- 0.02) K for the isotropic exchange coupling, and /d/ = (0.010 +/- 0.002) K for the projection of the dipole-dipole interaction tensor on the symmetry axis of the copper spin. From the EPR experiments only the relative signs of J0 and d can be deduced; it was determined that they have the same sign. The magnitude of the exchange coupling calculated for Cu2+QA-:RC is similar to that observed for the Fe2+QA-:RC complex (J0 = -0.43K). The exchange coupling is discussed in terms of the superexchange paths connecting the Cu2+ ion and the quinone radical using the structural data for the RCs of Rb. sphaeroides. From the value of the dipole-dipole interaction, d, we determined R approximately 8.4 A for the weighted distance between the metal ion and the quinone in reduced RCs, which is to be compared with 10 A obtained from x-ray analysis of unreduced RCs. This points to a shortening of the Cu2+ -QA- distance upon reduction of the quinone, as has been proposed by Allen et al. (1988).     

Fe(II)-substituted horse liver alcohol dehydrogenase, a model for non-heme iron enzymes. Various states of iron-dioxygen interaction investigated by M?ssbauer and EPR spectroscopy

The catalytic Zn(II) ion of horse liver alcohol dehydrogenase (EE isozyme) was replaced by Fe(II), providing a novel iron protein with the unusual coordination of Fe(II) to two cysteines residues, one histine residue and water. The electronic structure of iron in this system was characterized by M?ssbauer spectroscopy at various temperatures as well as applied magnetic fields and analysed in terms of the spin Hamiltonian formalism. The novelty we found is an unusually weak spin coupling (/J/ less than 0.1 cm-1) of a paramagnet (S = 1) with iron (S = 2). From EPR and biochemical studies we conclude that the corresponding chemical species is triplet oxygen (O2). The quantitative determination of the coupling energy was possible utilizing the competition between Zeemann interaction and spin coupling at weak magnetic fields and low temperature. Oxidation experiments followed by M?ssbauer spectroscopy showed that the spin-coupled system is an outer-sphere Fe(II) . (O2)aq complex occurring as an intermediate during a Fe(II)-catalyzed dioxygen activation. We observed two additional Fe(II) species after treatment with O2 and dithionite. The spin Hamiltonian parameters of iron in the coupled system are presented. The results are compared with those of iron in other non-heme iron proteins.     

Spectroscopic studies on the interaction of phosphate with uteroferrin

The effect of phosphate on the binuclear iron center of pink (reduced) uteroferrin was examined by magnetic resonance and optical spectroscopy. The purple (oxidized) protein, which contains 1 mol of tightly bound phosphate per mol of enzyme at isolation, does not give rise to a 31P NMR signal. Phosphate binding to phosphate-stripped pink uteroferrin is indistinguishable from that in the native purple phosphoprotein. As measured by EPR and optical spectroscopy, the rate of reaction between phosphate and pink uteroferrin is pH-dependent, decreasing as the pH increases. Phosphate is capable of binding to the reduced protein between pH 3 and 7.8, resulting in formation of the purple uteroferrin-phosphate complex. Evans susceptibility measurements at pH 4.9 indicate that the EPR silent species with a maximum absorption at 535 nm, generated upon phosphate addition to pink uteroferrin, is diamagnetic. Moreover, phosphate causes disappearance of the hyperfine-shifted resonances in the 1H NMR spectra of the reduced protein. We therefore have not been able to identify the paramagnetic "purple reduced enzyme-phosphate complex" reported by Pyrz et al. (Pyrz, J. W., Sage, J. T., Debrunner, P. G., and Que, Jr., L. (1986) J. Biol Chem. 261, 11015-11020) using Mossbauer spectroscopy and dithionite-reduced 57Fe-reconstituted uteroferrin. Our present data with native unmodified enzyme are in accord with our earlier results (Antanaitis, B. C., and Aisen, P. (1985) J. Biol. Chem. 260, 751-756) and with the results of Burman et al. (Burman, S., Davis, J. C., Weber, M. J., and Averill, B. A. (1986) Biochem. Biophys. Res. Commun. 136, 490-497) on bovine spleen phosphatase, suggesting that phosphate binding to reduced protein rapidly induces oxidation of the binuclear iron center.     

The interaction of phosphate with uteroferrin. Characterization of a reduced uteroferrin-phosphate complex

The interaction of phosphate with reduced uteroferrin has been re-examined in light of disagreements on the oxidation state of the binuclear iron cluster (Keough, D. T., Beck, J. L., de Jersey, J., and Zerner, B. (1982) Biochem. Biophys. Res. Commun. 108, 1643-1648; Antanaitis, B. C., and Aisen, P. (1985) J. Biol. Chem. 260, 751-756). Our results based on Mossbauer observations and the kinetics of spectral change and activity loss show clearly that phosphate binds to reduced uteroferrin to form a reduced uteroferrin-phosphate complex. This complex exhibits a pair of quadrupole doublets at 119 K with parameters typical of a high spin ferric and a high spin ferrous center, respectively, but distinct from those of the native reduced enzyme. The reduced phosphate complex exhibits a pH-dependent visible absorption maximum ranging from 530 to 561 nm. In air, the reduced phosphate complex converts to the oxidized phosphate complex with a first order rate constant of 4 X 10(-3) min-1, as monitored by spectral changes and loss of enzyme activity.     

Magnetization of the sulfite and nitrite complexes of oxidized sulfite and nitrite reductases: EPR silent spin S = 1/2 states

The saturation magnetizations of the sulfite complex of oxidized sulfite reductase and the nitrite complex of oxidized nitrite reductase have been measured to determine their spin state. Each shows the saturation magnetization signal of a spin S = 1/2 state with sigma g2 = 16, which is typical of low-spin ferrihemes. However, the EPR spectra of these complexes lack the expected signal intensity of a spin S = 1/2 state. Indeed, one of these complexes is EPR silent. The reasons for this unexpectedly low EPR signal intensity are considered.     

Evidence for siroheme-Fe4S4 interaction in spinach ferredoxin-sulfite reductase

Spinach ferredoxin-sulfite reductase (SiR) contains one siroheme and one Fe4S4 center per polypeptide subunit. The heme is entirely in the high-spin Fe3+ state in the oxidized enzyme. When SiR is photochemically reduced with ethylenediaminetetraacetate (EDTA)-deazaflavin, the free enzyme and its CN- and CO complexes show changes in absorption spectra associated with the heme even after the heme has been reduced from the Fe3+ to the Fe2+ state. With CO- or CN--SiR, these spectral changes are associated with the appearance of a classical "g = 1.94" type of EPR spectrum characteristic of reduced Fe4S4 centers. The line shapes and exact g values of the g = 1.94 EPR spectra vary with the nature of the ligand bound to the heme Fe. Photoreduction of free SiR results in production of a novel type of EPR signal, with g = 2.48, 2.34, and 2.08 in the fully reduced enzyme; this signal accounts for 0.6 spin per heme. (A small g = 1.94 type EPR signal, representing 0.2 spin per heme, is also found.) These data suggest the presence of a strong magnetic interaction between the siroheme and Fe4S4 centers in spinach SiR, this interaction giving rise to different EPR signals depending on the spin state of the heme Fe in the reduced enzyme.     

Multi-frequency EPR and high-resolution M?ssbauer spectroscopy of a putative [6Fe-6S] prismane-cluster-containing protein from Desulfovibrio vulgaris (Hildenborough). Characterization of a supercluster and superspin model protein.

The putative [6Fe-6S] prismane cluster in the 6-Fe/S-containing protein from Desulfovibrio vulgaris, strain Hildenborough, has been enriched to 80% in 57Fe, and has been characterized in detail by S-, X-, P- and Q-band EPR spectroscopy, parallel-mode EPR spectroscopy and high-resolution 57Fe M?ssbauer spectroscopy. In EPR-monitored redox-equilibrium titrations, the cluster is found to be capable of three one-electron transitions with midpoint potentials at pH 7.5 of +285, +5 and -165 mV. As the fully reduced protein is assumed to carry the [6Fe-6S]3+ cluster, by spectroscopic analogy to prismane model compounds, four valency states are identified in the titration experiments: [6Fe-6S]3+, [6Fe-6S]4+, [6Fe-6S]5+, [6Fe-6S]6+. The fully oxidized 6+ state appears to be diamagnetic at low temperature. The prismane protein is aerobically isolated predominantly in the one-electron-reduced 5+ state. In this intermediate state, the cluster exists in two magnetic forms: 10% is low-spin S = 1/2; the remainder has an unusually high spin S = 9/2. The S = 1/2 EPR spectrum is significantly broadened by ligand (2.3 mT) and 57Fe (3.0 mT) hyperfine interaction, consistent with a delocalization of the unpaired electron over 6Fe and indicative of at least some nitrogen ligation. At 35 GHz, the g tensor is determined as 1.971, 1.951 and 1.898. EPR signals from the S = 9/2 multiplet have their maximal amplitude at a temperature of 12 K due to the axial zero-field splitting being negative, D approximately -0.86 cm-1. Effective g = 15.3, 5.75, 5.65 and 5.23 are observed, consistent with a rhombicity of [E/D] = 0.061. A second component has g = 9.7, 8.1 and 6.65 and [E/D] = 0.108. When the protein is reduced to the 4+ intermediate state, the cluster is silent in normal-mode EPR. An asymmetric feature with effective g approximately 16 is observed in parallel-mode EPR from an integer spin system with, presumably, S = 4. The fully reduced 3+ state consists of a mixture of two S = 1/2 ground state. The g tensor of the major component is 2.010, 1.825 and 1.32; the minor component has g = 1.941 and 1.79, with the third value undetermined. The sharp line at g = 2.010 exhibits significant convoluted hyperfine broadening from ligands (2.1 mT) and from 57Fe (4.6 mT). Zero-field high-temperature M?ssbauer spectra of the protein, isolated in the 5+ state, quantitatively account for the 0.8 fractional enrichment in 57Fe, as determined with inductively coupled plasma mass spectrometry.(ABSTRACT TRUNCATED AT 400 WORDS)     

Paramagnetic centers and acetyl-coenzyme A/CO exchange activity of carbon monoxide dehydrogenase from Methanothrix soehngenii.

Carbon monoxide (CO) dehydrogenase was purified, both aerobically and anaerobically, to apparent homogeneity from Methanothrix soehngenii. The enzyme contained 18 +/- 2 (n = 6) mol Fe/mol and 2.0 +/- 0.1 (n = 6) mol Ni/mol. Electron paramagnetic resonance (EPR) spectra of the aerobically purified CO dehydrogenase showed one sharp EPR signal at g = 2.014 with several characteristics of a [3Fe-4S]1+ cluster. The integrated intensity of this signal was low, 0.03 S = 1/2 spin/alpha beta dimer. The 3Fe spectrum was not affected by incubation with CO or acetyl-coenzyme A, but could be reduced by dithionite. The spectrum of the reduced, aerobically purified enzyme showed complex EPR spectra, which had several properties typical of two [4Fe-4S]1+ clusters, whose S = 1/2 spins weakly interacted by dipolar coupling. The integrated intensity was 0.1-0.2 spin/alpha beta dimer. The anaerobically isolated enzyme showed EPR spectra different from the reduced aerobically purified enzyme. Two major signals were apparent. One with g values of 2.05, 1.93 and 1.865, and an Em7.5 of -410 mV, which quantified to 0.9 S = 1/2 spin/alpha beta dimer. The other signal with g values of 1.997, 1.886 and 1.725, and an Em7.5 of -230 mV gave 0.1 spin/alpha beta dimer. When the enzyme was incubated with its physiological substrate acetyl-coenzyme A, these two major signals disappeared. Incubation of the enzyme under CO atmosphere resulted in a partial disappearance of the spectral component with g = 1.997, 1.886, 1.725. Acetyl-coenzyme A/CO exchange activity, 35 nmol.min-1.mg-1 protein, which corresponded to 7 mol CO exchanged min-1 mol-1 enzyme, could be detected in anaerobic enzyme preparations, but was absent in aerobic preparations. Carbon dioxide also exchanged with C-1 of acetyl-coenzyme A, but at a much lower rate than CO and to a much lower extent.     

Quantitative EPR of an S = 7/2 system in thionine-oxidized MoFe proteins of nitrogenase. A redefinition of the P-cluster concept

Thionine-oxidized nitrogenase MoFe proteins from Azotobacter vinelandii. Azotobacter chroococcum and Klebsiella pneumoniae exhibit excited-state EPR signals with g = 10.4, 5.8 and 5.5 with a maximal amplitude in the temperature range of 20-50 K. The magnitude of these effective g values, combined with the temperature dependence of the peak area at g = 10.4 from 12 K to 86 K, are consistent with an S = 7/2 system with spin Hamiltonian parameters D = -3.7 +/- 0.7 cm-1, [E] = 0.16 +/- 0.01 cm-1 and g = 2.00. This interpretation predicts nine additional effective g values some of which have been detected as broad features of low intensity at g approximately 10, approximately 2.5 and approximately 1.8. The S = 7/2 EPR is ascribed to the multi-iron exchange-coupled entities known as the P clusters. Quantification relative to the S = 3/2 EPR signal from dithionite-reduced MoFe protein indicates a stoichiometry of one P cluster per FeMo cofactor. Two possible interpretations for these observations, together with data from the literature, are proposed. In the first model there are two P clusters per tetrameric MoFe protein. Each P cluster encompasses approximately 8Fe ions and releases a total of three electrons on oxidation with excess thionine. In the second model the conventional view of four P clusters, each containing approximately 4Fe, is retained. This alternative requires that following one-electron oxidation, the P clusters factorize into two populations, Pa and Pb, only one of which is further oxidized with thionine resulting in the S = 7/2 system. Both models require eight-electron oxidation of tetrameric MoFe protein to reach the S = 7/2 state.     

Identification of the iron-sulfur center of spinach ferredoxin-nitrite reductase as a tetranuclear center, and preliminary EPR studies of mechanism.

EPR spectroscopic and chemical analyses of spinach nitrite reductase show that the enzyme contains one reducible iron-sulfur center, and one site for binding either cyanide or nitrite, per siroheme. The heme is nearly all in the high spin ferric state in the enzyme as isolated. The extinction coefficient of the enzyme has been revised to E386 = 7.6 X 10(4) cm-1 (M heme)-1. The iron-sulfur center is reduced with difficulty by agents such as reduced methyl viologen (equilibrated with 1 atm of H2 at pH 7.7 in the presence of hydrogenase) or dithionite. Complexation of the enzyme with CO (a known ligand for nitrite reductase heme) markedly increases the reducibility of the iron-sulfur center. New chemical analyses and reinterpretation of previous data show that the enzyme contains 6 mol of iron and 4 mol of acid-labile S2-/mol of siroheme. The EPR spectrum of reduced nitrite reductase in 80% dimethyl sulfoxide establishes clearly that the enzyme contains a tetranuclear iron-sulfur (Fe4S4) center. The ferriheme and Fe4S4 centers are reduced at similar rates (k = 3 to 4 s-1) by dithionite. The dithionite-reduced Fe4S4 center is rapidly (k = 100 s-1) reoxidized by nitrite. These results indicate a role for the Fe4S4 center in catalysis.     

Nitrogenase. VIII. M?ssbauer and EPR spectroscopy. The MoFe protein component from Azotobacter vinelandii OP.

We have studied the molybdenum-iron protein (MoFe protein, also known as component I) from Azobacter vinelandi using M?ssbauer spectroscopy and electron paramagnetic resonance on samples enriched with 57Fe. These spectra can be interpreted in terms of two EPR active centers, each of which is reducible by one electron. A total of four different chemical environments of Fe can be discerned. One of them is a cluster of Fe atoms with a net electronic spin of 3/2, one of them is high-spin ferrous iron and the remaining two are iron in a reduced state (probably in clusters). The results are as follows: Chemical analysis yields 11.5 Fe atoms and 12.5 labile sulfur atoms per molybdenum atom; the molecule contains two Mo atoms per 300 000 daltons. The EPR spectrum of the MoFe protein exhibits g values at 4.32, 3.65 and 2.01, associated with the ground state doublet of a S = 3/2 spin system. The spin Hamiltonian H = D(S2/z minus 5/4 + lambda(S2/x minus S2/y)) + gbeta/o S-H fits the experimental data for go = 2.00 and lambda = 0.055. Quantitative analysis of the temperature dependence of the EPR spectrum yields D/k = 7.5 degrees K and 0.91 spins/molybdenum atom, which suggests that the MoFe protein has two EPR active centers. Quantitative evaluation of M?ssbauer spectra shows that approximately 8 iron atoms give rise to one quadrupole doublet; at lower temperatures magnetic spectra, associated with the groud electronic doublet, are observed; at least two magnetically inequivalent sites can be distinguished. Taken together the data suggest that each EPR center contains 4 iron atoms. The EPR and M?ssbauer data can only be reconciled if these iron atoms reside in a spin-coupled (S = 3/2) cluster. Under nitrogen fixing conditions the magnetic M?ssbauer spectra disappeared concurrently with the EPR signal and quadrupole doublets are obserced at all temperatures. The data suggest that each EPR active center is reduced by one electron. The M?ssbauer investigation reveals three other spectral components characteristic of iron nuclei in an environment of integer or zero electronic spin, i.e. they reside in complexes which are "EPR-silent". One of the components (3-4 iron atoms) has M?ssbauer parameters characteristic of the high-spin ferrous iron as in reduced ruberdoxin. However, measurements in strong fields indicate a diamagnetic environment. Another component, representing 9-11 iron atoms, seems to be diamagnetic also. It is suggested that these atoms are incorporated in spin-coupled clusters.