Delta EQ Research Articles

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 Mössbauer 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 Mössbauer 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, Mössbauer and EPR measurements.

Mononuclear (nitrido)iron(V) and (oxo)iron(IV) complexes via photolysis of [(cyclam-acetato)FeIII(N3)]+ and ozonolysis of [(cyclam-acetato)FeIII(O3SCF3)]+ in water/acetone mixtures.

Reaction of the monoanionic, pentacoordinate ligand lithium 1,4,8,11-tetraazacyclotetradecane-1-acetate, Li(cyclam-acetate), with FeCl3 yields, upon addition of KPF6, [(cyclam-acetato)FeCl]PF6 (1) as a red microcrystalline solid. Addition of excess NaN3 prior to addition of KPF6 yields the azide derivative [(cyclam-acetato)FeN3]PF6 (2a) as orange microcrystals. The X-ray crystal structure of the azide derivative has been determined as the tetraphenylborate salt (2b). Reaction of 1 with silver triflate yields [(cyclam-acetato)Fe(O3SCF3)]PF6 (3), which partially dissociates triflate in nondried solvents to yield a mixture of triflate and aqua bound species. Each of the iron(III) derivatives is low-spin (d5, S = 1/2) as determined by variable-temperature magnetic susceptibility measurements, Mössbauer and EPR spectroscopy. The low-spin iron(II) (d6, S = 0) complexes 1red and 2ared have been prepared by electrochemical and chemical methods and have been characterized by Mössbauer spectroscopy. Photolysis of 2a at 419 nm in frozen acetonitrile yields a nearly colorless species in approximately 80% conversion with an isomer shift delta = -0.04 mm/s and a quadrupole splitting delta EQ = -1.67 mm/s. A spin-Hamiltonian analysis of the magnetic Mössbauer spectra is consistent with an FeV ion (d3, S = 3/2). The proposed [(cyclam-acetato)FeV=N]+ results from the photooxidation of 2a via heterolytic N-N cleavage of coordinated azide. Photolysis of 2a in acetonitrile solution at -35 degrees C (300 nm) or 20 degrees C (Hg immersion lamp) results primarily in photoreduction via homolytic Fe-Nazide cleavage yielding FeII (d,6 S = 0) with an isomer shift delta = 0.56 mm/s and quadrupole splitting delta EQ = 0.54 mm/s. A minor product containing high-valent iron is suggested by Mössbauer spectroscopy and is proposed to originate from [((cyclam-acetato)Fe)2(mu-N)]2+ with a mixed-valent (FeIV(mu-N)FeIII))4+S = 1/2 core. Exposure of 3 to a stream of oxygen/ozone at low temperatures (-80 degrees C) in acetone/water results in a single oxidized product with an isomer shift delta = 0.01 mm/s and quadrupole splitting delta EQ = 1.37 mm/s. A spin-Hamiltonian analysis of the magnetic Mössbauer yields parameters similar to those of compound II of horseradish peroxidase which are consistent with an FeIV=O monomeric complex (S = 1).

Iron coordination geometry in full-length, truncated, and dehydrated forms of human tyrosine hydroxylase studied by Mössbauer and X-ray absorption spectroscopy.

Full-length human tyrosine hydroxylase 1 (hTH1) and a truncated enzyme lacking the 150 N-terminal amino acids were expressed in Escherichia coli and purified either with or without (6 x histidine) N-terminal tags. After reconstitution with 57Fe(II), the Mössbauer and X-ray absorption spectra of the enzymes were compared before and after dehydration by lyophilization. Before dehydration, > 90% of the iron in hTH1 had Mössbauer parameters typical for high-spin Fe(II) in a six-coordinate environment [isomer shift delta (1.8-77 K) = 1.26-1.24 mm s-1 and quadrupole splitting delta EQ = 2.68 mm s-1]. After dehydration, the Mössbauer spectrum changed and 63% of the area could be attributed to five-coordinate high-spin Fe(II) (delta = 1.07 mm s-1 and delta EQ = 2.89 mm s-1 at 77 K), whereas 28% of the iron remained as six-coordinate high-spin Fe(II) (delta = 1.24 mm s-1 and delta EQ = 2.87 mm s-1 at 77 K). Similar changes upon dehydration were observed for truncated TH either with or without the histidine tag. After rehydration of hTH1 the spectroscopic changes were completely reversed. The X-ray absorption spectra of hTH1 in solution and in lyophilized form, and for the truncated protein in solution, corroborate the findings derived from the Mössbauer spectra. The pre-edge peak intensity of the protein in solution indicates six-coordination of the iron, while that of the dehydrated protein is typical for a five-coordinate iron center. Thus, the active-site iron can exist in different coordination states, which can be interconverted depending on the hydration state of the protein, indicating the presence or absence of a water molecule as a coordinating ligand to the iron. The present study explains the difference in iron coordination determined by X-ray crystallography, which has shown a five-coordinate iron center in rat TH, and by our recent spectroscopic study of human TH in solution, which showed a six-coordinated iron center.

FhuF, an iron-regulated protein of Escherichia coli with a new type of [2Fe-2S] center.

We previously used fhuF as a sensitive reporter gene of the iron status of Escherichia coli. In this report, the fhuF gene was identified as open reading frame f262b at 99.2 min on the genome sequence map of E. coli K-12. The FhuF protein was labeled with a His-tag and then purified to electrophoretic homogeneity. Based on sulfur determinations and Mössbauer and EPR spectroscopy, FhuF was identified as a [2Fe-2S] protein. The g values (gx = 1.886, gy = 1.961, gz = 1.994) and some of the Mössbauer parameters of FhuF obtained [oxidized protein as isolated: delta EQ,4.2K = 0.474 mm s-1; Fe3+ (reduced protein): delta EQ = 0.978 mm s-1] are not typical of common [2Fe-2S] proteins and indicate that FhuF has unusual structural properties. The primary sequence of FhuF does not show any sequence similarities to known [2Fe-2S] proteins. By site-directed mutagenesis, each of the six cysteines of FhuF was replaced by serine. EPR of the six reduced mutant proteins revealed that the terminal cysteine residues 244, 245, 256, and 259 form the [2Fe-2S]Cys4 cluster. Mutants having the Cys-to-Ser replacement at positions 244, 245, 256, or 259 did not complement a fhuF mutant. The motif Cys-Cys-Xaa10-Cys-Xaa2-Cys in FhuF differs considerably from the motif Cys-Xaa2-Cys-Xaa9-15-Cys-Xaa2-Cys found in other [2Fe-2S] proteins. The unusual Cys-Cys terminal group of the cluster may explain the atypical EPR and Mössbauer spectroscopic properties of the FhuF protein; possibly the tetrahedral symmetry at the ferric ion site is distorted. The phenotype of fhuF mutants and the structural features of the FhuF protein suggest that FhuF is involved in the reduction of ferric iron in cytoplasmic ferrioxamine B.

Iron uptake and intracellular metal transfer in mycobacteria mediated by xenosiderophores.

Growth promotion was tested using M. smegmatis wild type strain, an exochelin-deficient mutant, and M. fortuitum employing a broad variety of xenosiderophores including hydroxamates, catecholates and alpha-hydroxy carboxylic acids. The experiments revealed that utilization of siderophore-bound iron is substrate specific suggesting high-affinity siderophore receptor and transport systems. Concentration-dependent uptake of a selected xenosiderophore (fericrocin) in M. smegmatis showed saturation kinetics and uptake was inhibited by respiratory poisons. In situ Mössbauer spectroscopy of ferricrocin uptake in M. smegmatis indicated rapid intracellular reductive removal of the metal excluding intracellular ferricrocin accumulation. The ultimate intracellular iron pool is represented by a compound (delta = 0.43 mm s-1, delta EQ = 1.03 mm s-1) which has also been found in many other microorganisms and does not represent a bacterioferritin, cytochrome or iron-sulfur cluster. By contrast, iron uptake via citrate-a compound exhibiting a very low complex stability constant-involves ligand exchange with mycobactin. Mycobactin has merely a transient role. The ultimate storage compound is an E. coli-type bacterioferritin, in which over 90% of cellular iron is located.

Characterization of the Iron-binding Site in Mammalian Ferrochelatase by Kinetic and Mössbauer Methods

All organisms utilize ferrochelatase (protoheme ferrolyase, EC 4.99.1.1) to catalyze the terminal step of the heme biosynthetic pathway, which involves the insertion of ferrous ion into protoporphyrin IX. Kinetic methods and Mössbauer spectroscopy have been used in an effort to characterize the ferrous ion-binding active site of recombinant murine ferrochelatase. The kinetic studies indicate that dithiothreitol, a reducing agent commonly used in ferrochelatase activity assays, interferes with the enzymatic production of heme. Ferrochelatase specific activity values determined under strictly anaerobic conditions are much greater than those obtained for the same enzyme under aerobic conditions and in the presence of dithiothreitol. Mössbauer spectroscopy conclusively demonstrates that, under the commonly used assay conditions, dithiothreitol chelates ferrous ion and hence competes with the enzyme for binding the ferrous substrate. Mössbauer spectroscopy of ferrous ion incubated with ferrochelatase in the absence of dithiothreitol shows a somewhat broad quadrupole doublet. Spectral analysis indicates that when 0.1 mM Fe(II) is added to 1.75 mM ferrochelatase, the overwhelming majority of the added ferrous ion is bound to the protein. The spectroscopic parameters for this bound species are delta = 1.36 +/- 0.03 mm/s and delta EQ = 3.04 +/- 0.06 mm/s, distinct from the larger delta EQ of a control sample of Fe(II) in buffer only. The parameters for the bound species are consistent with an active site composed of nitrogenous/oxygenous ligands and inconsistent with the presence of sulfur ligands. This finding is in accord with the absence of conserved cysteines among the known ferrochelatase sequences. The implications these results have with regard to the mechanism of ferrochelatase activity are discussed.

Reaction of NO with the reduced R2 protein of ribonucleotide reductase from Escherichia coli.

The active R2 protein of ribonucleotide reductase from Escherichia coli contains a catalytically essential tyrosine radical at position 122 (Tyr122.) that is formed during the reaction of dioxygen with the nearby diiron(II) center. To gain insight into the mode of dioxygen binding, the reaction of the O2 analog NO with the diiron(II) centers of R2red has been investigated by spectroscopic methods. R2red reacts with NO to form an adduct with visible absorption features at 450 and 620 nm and Mössbauer parameters (delta = 0.75 mm/s, delta EQ = -2.13 and -1.73 mm/s) typical of those observed for S = 3/2 [FeNO]7 complexes of other non-heme iron proteins. However, unlike other non-heme [FeNO]7 complexes, this adduct is EPR silent. Our Mössbauer studies show that each iron site of R2red binds one NO to form local S = 3/2 [FeNO]7 centers which then couple antiferromagnetically (J approximately 5 cm-1, H = JS1.S2) to afford an [FeNO]2 center (77% of total iron). This [FeNO]2 center decomposes with a first-order rate constant of 0.013 min-1 to form R2met, accompanied by the release of N2O. These observations suggest that both iron(II) ions of the two diiron(II) centers of R2red have available sites for NO binding, in agreement with the crystallographic results on R2red, and that the bound NO molecules are sufficiently close to each other to permit N-N bond formation to produce N2O. These observations support the proposal that dioxygen binding may also involve both metal ions of the diiron(II) center to form a (mu-1,1-, or mu-1,2-peroxo)-diiron(III) center. This observed reactivity of R2red with NO may contribute to the in vivo inhibition of ribonucleotide reductase by NO.

Mössbauer characterization of the metal clusters in Azotobacter vinelandii nitrogenase VFe protein.

The VFe protein of alternative nitrogenase, isolated from Azotobacter vinelandii, strain LS15 and designated as Av1', has been investigated by Mössbauer spectroscopy. The Mössbauer spectrum of the dithionite-reduced Av1', recorded at 4.2 K with a 60-millitesla magnetic field applied parallel to the gamma-beam, is a superposition of three spectral components: 1) a complex spectrum (the M component) with magnetic hyperfine structures attributed to the paramagnetic FeV cofactor, 2) a component (the P component) consisting of three quadrupole doublets identifiable as the Fe2+, D, and S doublets similar to those observed for the P cluster pairs in MoFe proteins, and 3) a minor (4% of total absorption) quadrupole doublet attributable to adventitiously bound iron. The observed 4.2-K parameters for the Fe2+ (delta EQ = 2.99 mm/s and delta = 0.64 mm/s), D (delta EQ = 0.75 mm/s and delta = 0.63 mm/s), and S (delta EQ = 1.2 mm/s and delta = 0.65 mm/s) iron sites and their temperature dependence are very similar to those observed for the P cluster pairs in the conventional MoFe proteins. Similar to those of the MoFe protein, strong field spectra indicate that these doublets are associated with a diamagnetic system. Their percent absorption intensities (Fe(2+)/D/S = 13.0:32.2:6.8) determined at 4.2 K after the removal of the contributions from the adventitiously bound iron are comparable to those of the P cluster pairs in MoFe proteins. These observations established that Av1' also contains P cluster pairs that are identical, in both composition and quantity, to those of the MoFe proteins; i.e. each molecule contains two P cluster pairs and each pair is formed by two Fe2+, five D, and one S iron sites. Considering that 52% absorption of the P component corresponding to two 8Fe clusters, the remaining 48% absorption determined for the M component is consistent with two 7Fe-containing FeV cofactors/molecule of Av1'. The fact that both P cluster pairs are found in the diamagnetic states implies that the S = 3/2 and S = 1/2 signals detected in earlier EPR measurements are associated with the FeV cofactor and suggests a spin mixture for the FeV cofactor in the dithionite-reduced Av1'.

Mössbauer study of the native, reduced and substrate-reacted Desulfovibrio gigas aldehyde oxido-reductase.

The Desulfovibrio gigas aldehyde-oxido-reductase contains molybdenum and iron-sulfur clusters. Mössbauer spectroscopy was used to characterize the iron-sulfur clusters. Spectra of the enzyme in its oxidized, partially reduced and benzaldehyde-reacted states were recorded at different temperatures and applied magnetic fields. All the iron atoms in D. gigas aldehyde oxido-reductase are organized as [2Fe-2S] clusters. In the oxidized enzyme, the clusters are diamagnetic and exhibit a single quadrupole doublet with parameters (delta EQ = 0.62 +/- 0.02 mm/s and delta = 0.27 +/- 0.01 mm/s) typical for the [2Fe-2S]2+ state. Mössbauer spectra of the reduced clusters also show the characteristics of a [2Fe-2S]1+ cluster and can be explained by a spin-coupling model proposed for the [2Fe-2S] cluster where a high-spin ferrous ion (S = 2) is antiferromagnetically coupled to a high-spin ferric ion (S = 5/2) to form a S = 1/2 system. Two ferrous sites with different delta EQ values (3.42 mm/s and 2.93 mm/s at 85 K) are observed for the reduced enzyme, indicating the presence of two types of [2Fe-2S] clusters in the D. gigas enzyme. Taking this observation together with the re-evaluated value of iron content (3.5 +/- 0.1 Fe/molecule), it is concluded that, similar to other Mo-hydroxylases, the D. gigas aldehyde oxido-reductase also contains two spectroscopically distinguishable [2Fe-2S] clusters.

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. Mössbauer 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 Mössbauer 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.

Mössbauer study of CO dehydrogenase from Clostridium thermoaceticum.

We have studied with Mössbauer spectroscopy the metal clusters of CO dehydrogenase from Clostridium thermoaceticum. At potentials greater than -200 mV, all of the approximately 12 irons reside in diamagnetic environments and contribute a quadrupole doublet characteristic of [Fe4S4]2+ clusters. At lower potentials a variety of components are observed. About 40% of the Fe appears to belong to one [Fe4S4]1+ cluster. We have also observed the Mössbauer spectrum (approximately 18% of Fe) of the complex which yields EPR with g = 2.01, 1.81, and 1.65. Also present is a doublet (9% of Fe) with delta EQ = 2.90 mm/s and delta = 0.70 mm/s, values typical of a ferrous FeS4 complex. This component seems to interact with a nickel site to form an EPR-silent complex with half-integral electronic spin. We have also characterized the iron environments of the S = 1/2 NiFeC complex. This complex contributes approximately 20% of the total Mössbauer absorption when the EPR signal has approximately 0.35 spins/12 Fe. From isomer shift comparisons in the oxidized and CO-reacted states of this center, we speculate that the NiFeC complex may consist of a nickel site exchange-coupled to a [Fe4S4]2+ cluster. Finally, the Mössbauer and EPR data, taken together, force us to conclude that current preparations, while homogeneous according to purifications standards, are spectroscopically heterogeneous, thus rendering the development of a model of the cluster types and compositions in this enzyme premature.

A M�ssbauer spectroscopy study of cellular acquisition of iron from pyoverdine byPseudomonas aeruginosa

Mössbauer spectroscopy was used to investigate the cellular acquisition of iron by Pseudomonas aeruginosa which had been incubated with ferripyoverdine for 20, 40, 60, 120 or 360 min. Studies revealed that no ferripyoverdine accumulated in the cells at any of these times and that the amounts and kinds of iron complexes produced by cellular metabolism vary with time. At 20 and 40 min a ferric species, with isomer shift delta = 0.38-0.42 mm/s and quadrupole splitting delta EQ = 0.94-0.92 mm/s, was the major iron metabolite comprising approximately 80% of the iron. At later times at least three other ferric species appeared with delta = 0.54----0.72, delta EQ = 0.84----1.07 mm/s. Ferrous species, delta = 1.43----1.77 mm/s and delta EQ = 2.69----1.82 mm/s, were also seen at times as early as 20 min and comprised as much as 17% of the total iron at 20 and 40 min. The parameters of all these species identify them as being six-coordinated high-spin complexes. In addition a low-spin species, delta = 0.19 mm/s delta EQ = 0.67----0.91 mm/s, never before reported in cells, appeared at 60, 120, and 360 min as one of the major iron metabolites (50% or more). All isomer shifts are measured with respect to natural iron.

Redox Intermediates of Desulfovibrio gigas [NiFe] Hydrogenase Generated Under Hydrogen: MÖssbauer and epr characterization of the metal centers

The hydrogenase (EC 1.2.2.1) of Desulfovibrio gigas is a complex enzyme containing one nickel center, one [3Fe-4S] and two [4Fe-4S] clusters. Redox intermediates of this enzyme were generated under hydrogen (the natural substrate) using a redox-titration technique and were studied by EPR and Mossbauer spectroscopy. In the oxidized states, the two [4Fe-4S]2+ clusters exhibit a broad quadrupole doublet with parameters (apparent delta EQ = 1.10 mm/s and delta = 0.35 mm/s) typical for this type of cluster. Upon reduction, the two [4Fe-4S]1+ clusters are spectroscopically distinguishable, allowing the determination of their midpoint redox potentials. The cluster with higher midpoint potential (-290 +/- 20 mV) was labeled Fe-S center I and the other with lower potential (-340 +/- 20 mV), Fe-S center II. Both reduced clusters show atypical magnetic hyperfine coupling constants, suggesting structural differences from the clusters of bacterial ferredoxins. Also, an unusually broad EPR signal, labeled Fe-S signal B', extending from approximately 150 to approximately 450 mT was observed concomitantly with the reduction of the [4Fe-4S] clusters. The following two EPR signals observed at the weak-field region were tentatively attributed to the reduced [3Fe-4S] cluster: (i) a signal with crossover point at g approximately 12, labeled the g = 12 signal, and (ii) a broad signal at the very weak-field region (approximately 3 mT), labeled the Fe-S signal B. The midpoint redox potential associated with the appearance of the g = 12 signal was determined to be -70 +/- 10 mV. At potentials below -250 mV, the g = 12 signal began to decrease in intensity, and simultaneously, the Fe-S signal B appeared. The transformation of the g = 12 signal into the Fe-S signal B was found to parallel the reduction of the two [4Fe-4S] clusters indicating that the [3Fe-4S]o cluster is sensitive to the redox state of the [4Fe-4S] clusters. Detailed redox profiles for the previously reported Ni-signal C and the g = 2.21 signal were obtained in this study, and evidence was found to indicate that these two signals represent two different oxidation states of the enzyme. Finally, the mechanistic implications of our results are discussed.

Mössbauer and EPR studies of the binuclear iron center in ribonucleotide reductase from Escherichia coli: A new iron-to-protein stoichiometry

57Fe-enriched ribonucleotide reductase subunit B2 from Escherichia coli strain N6405/pSPS2 has been characterized by Mossbauer and EPR spectroscopy in its native diferric state and in a new differous form. The native protein exhibits two Mossbauer doublets in a 1:1 ratio with parameters that are in excellent agreement with those reported for the wild-type protein (Atkin, C. L., Thelander, L., Reichard, P., and Lang, G. (1983) J. Biol. Chem. 248, 7464-7472); in addition, our studies show the absence of adventitiously bound iron. The iron content in the present samples approached 4 per B2 subunit, and the tyrosyl radical content exceeded 1 per B2 subunit. The higher values are attributed to the use of a new epsilon 280 for the protein and more efficient methods for iron extraction. We thus propose that subunit B2 has two binuclear iron clusters, each associated with its own tyrosyl radical, in contradistinction from the prevailing model. Reduction of the native protein with dithionite or reconstitution of the apoprotein with Fe(II) afforded a protein complex with Mossbauer parameters, delta EQ = 3.13 mm/s and delta = 1.26 mm/s at 4.2 K, and a low field EPR signal associated with an integer spin system. These spectral properties resemble those of methane monooxygenase in its diferrous form. Upon exposure to O2, the reduced subunit B2 readily converts to the diferric state and yields active enzyme.

Isolation and characterization of rubrerythrin, a non-heme iron protein from Desulfovibrio vulgaris that contains rubredoxin centers and a hemerythrin-like binuclear iron cluster.

A new non-heme iron protein from the periplasmic fraction of Desulfovibrio vulgaris (Hildenbourough NCIB 8303) has been purified to homogeneity, and its amino acid composition, molecular weight, redox potential, iron content, and optical, EPR, and Mössbauer spectroscopic properties have been determined. This new protein is composed of two identical subunits with subunit molecular weight of 21,900 and contains four iron atoms per molecule. The as-purified oxidized protein exhibits an optical spectrum with absorption maxima at 492, 365, and 280 nm, and its EPR spectrum shows resonances at g = 4.3 and 9.4, characteristic of oxidized rubredoxin. The Mössbauer data indicate the presence of approximately equal amounts of two types of iron; we named them the Rd-like and the Hr-like iron due to their similarity to the iron centers of rubredoxins (Rds) and hemerythrins (Hrs), respectively. For the Rd-like iron, the measured fine and hyperfine parameters (D = 1.5 cm-1, E/D = 0.26, delta EQ = -0.55 mm/s, delta = 0.27 mm/s, Axx/gn beta n = -16.5 T, Ayy/gn beta n = -15.6 T, and Azz/gn beta n = -17.0 T) are almost identical with those obtained for the rubredoxin from Clostridium pasteurianum. Redox-titration studies monitored by EPR, however, showed that these Rd-like centers have a midpoint redox potential of +230 +/- 10 mV, approximately 250 mV more positive than those reported for rubredoxins. Another unusual feature of this protein is the presence of the Hr-like iron atoms.(ABSTRACT TRUNCATED AT 250 WORDS)

Mössbauer studies on the metal-thiolate cluster formation in Fe(II)-metallothionein.

The stepwise 57Fe(II)-thiolate cluster formation in rabbit liver metallothionein-2 (MT) has been followed at pH 8.5 using Mössbauer spectroscopy. The zero-field spectra recorded at 4.2 K exhibit at all stages of filling one virtually identical single quadrupole splitting delta EQ and isomer shift delta as found for reduced rubredoxin (Rdred) or the model compound [Fe(II)(SPh)4]2-, thus indicating an Fe(II)-tetrathiolate coordination. A similar conclusion was reached also in previous electronic absorption studies [M. Good and M. Vasák (1986) Biochemistry 25,8353--8356]. The Mössbauer spectra obtained in the presence of a magnetic field were analyzed on the basis of a spin-Hamiltonian formalism resulting in Mössbauer parameters similar to those for Rdred and the inorganic model compound [Fe(II)(SPh)4]2-. The identity of the Mössbauer parameters of partially and fully metal-occupied MT suggests that a comparable distortion of the metal binding sites must exist. Simulation of the spectra revealed that the Fe(II) ions in the partially metal-occupied 57Fe(II)4-MT form appear to be magnetically isolated, whereas in the fully metal-saturated 57Fe(II)7-MT form a ratio of 3:4 of paramagnetic to diamagnetic subspectra was obtained. The latter result suggests the existence of three isolated metal binding sites and a metal-thiolate cluster containing four metal ions. In the light of structure determinations of MT containing Zn(II) and/or Cd(II) [W. Braun et al. (1986) J. Mol. Biol. 187, 125-129, and W. F. Furrey et al. (1986) Science (Wash. DC) 231, 704-710], which revealed two metal-thiolate clusters containing three and four metal ions, respectively, and involving all 20 cysteine residues in metal binding, the appearance of Mössbauer parameters characteristic of three isolated Fe(II) sites in 57Fe(II)7-MT is peculiar and deserves further studies. It is concluded, moreover, that the four-metal cluster is diamagnetic with the four Fe(II) ions being antiferromagnetically coupled. The appearance of magnetic coupling above four Fe(II) equivalents bound to apoMT indicates that the cluster formation occurs in a two-step process.

Metabolic utilization of 57Fe-labeled coprogen in Neurospora crassa. An in vivo Mössbauer study.

Mössbauer spectra of whole cells of Neurospora crassa arg-5 ota aga (a siderophore-free mutant) show that the siderophore coprogen is accumulated inside the cell as an entity. 57Fe from 57Fe-labeled coprogen is slowly removed from the complex (45% in 27 h). The rate of removal depends on the degree of iron starvation of the cells. The distribution of 55Fe from [55Fe]coprogen in vacuoles, membranes, and cytoplasm has been also determined. From this it is clear that coprogen is accumulated in the cytoplasm. In addition to its role as a siderophore, coprogen serves as an iron-storage compound. No holoferritins could be detected. We therefore conclude that this type of iron-storage protein is lacking in N. crassa. Metabolized iron was found predominantly to exist as an envelope of Fe(II) high-spin (delta = 1.2-1.3 mm s-1; delta EQ = 3.0-3.1 mm s-1 at 4.2 K) and fast-relaxing Fe(III) high-spin species (delta approximately equal to 0.25 mm s-1 and 0.45 mm s-1; delta EQ approximately equal to 0.6 mm s-1 and 0.55 mm s-1, respectively, at 4.2 K). An assignment of these major iron metabolites is difficult. The Mössbauer data of the Fe(II) species do not fit those reported for heme, cytochromes and ferredoxins. We therefore assume that this iron metabolite represents a novel internal iron compound. One of the Fe(III) species becomes the dominant component of the cell spectra after 65 h of metabolization and might correspond to an iron-storage compound with iron oxide cores similar to bacterioferritin. After 27 h of growth in mycelia supplied with 57Fe-labeled coprogen, the siderophore ferricrocin was observed in the cell spectra. This is unexpected, since N. crassa arg-5 ota aga is unable to synthesize ornithine. We assume that ferricrocin is synthesized by the use of coprogen degradation products.

On the active sites of the [NiFe] hydrogenase from Desulfovibrio gigas. Mössbauer and redox-titration studies.

The [NiFe] hydrogenase isolated from Desulfovibrio gigas was poised at different redox potentials and studied by Mössbauer spectroscopy. The data firmly establish that this hydrogenase contains four prosthetic groups: one nickel center, one [3Fe-xS], and two [4Fe-4S] clusters. In the native enzyme, both the nickel and the [3Fe-xS] cluster are EPR-active. At low temperature (4.2 K), the [3Fe-xS] cluster exhibits a paramagnetic Mössbauer spectrum typical for oxidized [3Fe-xS] clusters. At higher temperatures (greater than 20 K), the paramagnetic spectrum collapses into a quadrupole doublet with parameters magnitude of delta EQ magnitude of = 0.7 +/- 0.06 mm/s and delta = 0.36 +/- 0.06 mm/s, typical of high-spin Fe(III). The observed isomer shift is slightly larger than those observed for the three-iron clusters in D. gigas ferredoxin II (Huynh, B. H., Moura, J. J. G., Moura, I., Kent, T. A., LeGall, J., Xavier, A. V., and Münck, E. (1980) J. Biol. Chem. 255, 3242-3244) and in Azotobacter vinelandii ferredoxin I (Emptage, M. H., Kent, T. A., Huynh, B. H., Rawlings, J., Orme-Johnson, W. H., and Münck, E. (1980) J. Biol. Chem. 255, 1793-1796) and may indicate a different iron coordination environment. When D. gigas hydrogenase is poised at potentials lower than -80 mV (versus normal hydrogen electrode), the [3Fe-xS] cluster is reduced and becomes EPR-silent. The Mössbauer data indicate that the reduced [3Fe-xS] cluster remains intact, i.e. it does not interconvert into a [4Fe-4S] cluster. Also, the electronic properties of the reduced [3Fe-xS] cluster suggest that it is magnetically isolated from the other paramagnetic centers.

Characterization of the cycle of iron-mediated electron transfer from Adriamycin to molecular oxygen.

The anticancer drug adriamycin binds iron and these complexes cycle to reduce molecular oxygen (Zweier, J. L. (1984) J. Biol. Chem. 259, 6056-6058). Optical absorption, EPR, and Mössbauer spectroscopic data are correlated with polarographic O2 consumption and chemical Fe2+ extraction measurements in order to characterize each step in this cycle. Fe3+ binds to adriamycin at physiologic pH forming a complex with an optical absorbance maximum at 600 nm. EPR signals at g = 4.2 and g = 2.01, and a doublet Mössbauer spectrum with isomer shift delta = 0.57 mm/s and quadrupole splitting delta EQ = 0.74 mm/s are observed indicating that the Fe3+ bound to adriamycin is high spin S = 5/2. Under anaerobic conditions the absorbance maximum at 600 nm decreases with an exponential decay constant = 0.77 h-1, and the EPR and Mössbauer spectra of Fe3+-adriamycin similarly decrease as the Fe3+ is reduced to EPR silent Fe2+. The Fe2+-adriamycin complex which is formed exhibits a Mössbauer spectrum with delta = 1.18 mm/s and delta EQ = 1.82 mm/s indicative of high spin Fe2+. As the EPR spectra of Fe3+-adriamycin decrease on reduction of the Fe3+ to Fe2+ a signal of the oxidized adriamycin free radical appears at g = 2.004 with line width of 8 G. On exposure to O2 the absorption maximum at 600 nm, the Fe3+ EPR, and the Fe3+ Mössbauer spectra all return. Polarographic measurements demonstrate that O2 is consumed and that H2O2 is formed. Addition of high affinity Fe2+ chelators block O2 consumption indicating that Fe2+ formation is essential for O2 reduction. This cycle of iron-mediated O2 reduction can explain the formation of the reactive reduced oxygen and adriamycin radicals which are thought to mediate the biological activity of adriamycin.

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 Mössbauer, 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 Mössbauer 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 Mössbauer 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 Mössbauer spectra of D. vulgaris sulfite reductase recorded with weak and strong applied fields also show evidence for an exchange-coupled siroheme-[4Fe-4S] unit.