Amino Acid Interaction with and Adsorption on Clays: FT-IR and Mössbauer Spectroscopy and X-ray Diffractometry Investigations

In the present paper, the adsorption of amino acids (Ala, Met, Gln, Cys, Asp, Lys, His) on clays (bentonite, kaolinite) was studied at different pH (3.00, 6.00, 8.00). The amino acids were dissolved in seawater, which contains the major elements. There were two main findings in this study. First, amino acids with a charged R group (Asp, Lys, His) and Cys were adsorbed on clays more than Ala, Met and Gln (uncharged R groups). However, 74% of the amino acids in the proteins of modern organisms have uncharged R groups. These results raise some questions about the role of minerals in providing a prebiotic concentration mechanism for amino acids. Several mechanisms are also discussed that could produce peptide with a greater proportion of amino acids with uncharged R groups. Second, Cys could play an important role in prebiotic chemistry besides participating in the structure of peptides/proteins. The FT-IR spectra showed that the adsorption of amino acids on the clays occurs through the amine group. However, the Cys/clay interaction occurs through the sulfhydryl and amine groups. X-ray diffractometry showed that pH affects the bentonite interlayer, and at pH 3.00 the expansion of Cys/bentonite was greater than that of the samples of ethylene glycol/bentonite saturated with Mg. The Mössbauer spectrum for the sample with absorbed Cys showed a large increase (～20%) in ferrous ions. This means that Cys was able to partially reduce iron present in bentonite. This result is similar to that which occurs with aconitase where the ferric ions are reduced to Fe 2.5.     

Adsorption of cysteine on hematite,magnetite and ferrihydrite: FT-IR,Mössbauer,EPR spectroscopy and X-ray diffractometry studies

In the present paper, the adsorption of cysteine on hematite, magnetite and ferrihydrite was studied using FT-IR, electron paramagnetic resonance (EPR), Mössbauer spectroscopy and X-ray diffractometry. Cysteine was dissolved in artificial seawater (two different pHs) which contains the major constituents. There were two main findings described in this paper. First, after the cysteine adsorption, the FT-IR spectroscopy and X-ray diffractometry data showed the formation of cystine. Second, the Mössbauer spectroscopy did not show any increase in the amount of Fe²⁺ as expected due the oxidation of cysteine to cystine. An explanation could be that Fe²⁺ was oxidized by the oxygen present in the seawater or there occurred a reduction of cystine by Fe²⁺ generating cysteine and Fe³⁺. The specific surface area and pH at point of zero charge of the iron oxides were influenced by adsorption of cysteine. When compared to other iron oxides, ferrihydrite adsorbed significantly (p < 0.05) more cysteine. The pH has a significant (p < 0.05) effect only on cysteine adsorption on hematite. The FT-IR spectroscopy results showed that cystine remains adsorbed on the surface of the iron oxides even after being mixed with KCl and the amine and carboxylic groups are involved in this interaction. X-ray diffractometry showed no changes on iron oxides mineralogy and the following precipitated substances were found along with the iron oxides after drying the samples: cysteine, cystine and seawater salts. The EPR spectroscopy showed that cysteine interacts with iron oxides, changing the relative amounts of iron oxides and hydroxide.     

Cysteine, thiourea and thiocyanate interactions with clays: FT-IR, Mössbauer and EPR spectroscopy and X-ray diffractometry studies

The present study examined the adsorption of cysteine, thiourea and thiocyanate on bentonite and montmorillonite at two different pHs (3.00, 8.00). The conditions used here are closer to those of prebiotic earth. As shown by FT-IR, Mössbauer and EPR spectroscopy and X-ray diffractometry, the most important finding of this work is that cysteine and thiourea penetrate into the interlayer of the clays and reduce Fe³⁺ to Fe²⁺, and as consequence, cystine and c,c′-dithiodiformamidinium ion are formed. This mechanism resembles that which occurs with aconitase. This is a very important result for prebiotic chemistry; we should think about clays not just sink of molecules, but as primitive vessels of production of biomolecules. At pH 8.00, an increasing expansion was observed in the following order for both minerals: thiourea > thiocyanate > cysteine. At pH 3.00, the same order was not observed and thiourea had an opposite behavior, being the compound producing the lowest expansion. Mössbauer spectroscopy showed that at pH 8.00, the proportion of Fe²⁺ ions in bentonite increased, doubling for thiourea, or more than doubling for cysteine, in both clays. However, at pH 3.00, cysteine and thiourea did not change significantly the relative amount of Fe²⁺ and Fe³⁺ ions, when compared to clays without adsorption. For thiocyanate, the amount of Fe²⁺ produced was independent of the pH or clay used, probably because the interlayers of clays are very acidic and HSCN formed does not reduce Fe³⁺ to Fe²⁺. For the interaction of thiocyanate with the clays, it was not possible to identify any potential compound formed. For the samples of bentonite and montmorillonite at pH 8.00 with cysteine, EPR spectroscopy showed that intensity of the lines due to Fe³⁺ decreased because the reaction of Fe³⁺/cysteine. Intensity of EPR lines did not change when the samples of bentonite at pH 3.00 with and without cysteine were compared. These results are in accordance with those obtained using Mössbauer and FT-IR spectroscopy.     

Effect of glutaraldehyde on hemoglobin: functional aspects and M?ssbauer parameters

Glutaraldehyde is widely used for the cross-linking of hemoglobin for blood substitute research or for technological purposes. The effects of this reagent on the biochemical properties of hemoglobin were correlated with M?ssbauer data. Human hemoglobin was cross-linked by glutaraldehyde as soluble polymers and insoluble particles. Effects of cross-linking on oxygen affinity, oxidation-reduction potential, autoxidation kinetics, and thermal stability were studied. Stability of cross-linked hemoglobin was specifically studied by M?ssbauer spectroscopy. Oxygen affinity is increased, redox potential is decreased, autoxidation rates are increased, and stability towards thermal denaturation is increased. The regeneration of partially denatured hemoglobin by glutaraldehyde cross-linking is shown. Effects of cross-linking on biochemical properties are explained by the hypothesis of the opening of the heme pocket on the distal-histidine side and the concomitant charge transfer from the iron to the oxygen.     

Optical, EPR and M?ssbauer spectroscopic studies on the NO derivatives of cytochrome cd1 from Thiobacillus denitrificans

We have used optical, EPR and M?ssbauer spectroscopies to study the formation of heme-NO complex upon the addition of nitrite to reduced cytochrome cd1 from Thiobacillus denitrificans. The reduced d1 heme binds NO under both alkaline and acidic conditions, but the binding of NO to the reduced c heme was strongly pH-dependent. The M?ssbauer data showed unambiguously that at pH 7.6 the c heme does not complex NO, whereas at pH 5.8 approximately half of the reduced c heme binds NO. This observation was confirmed by EPR studies, which showed that the spin concentration of the heme-NO EPR signal increased from 2 spins/molecule at pH 8.0 to approximately 3 spins/molecule at pH 5.8. Optical absorption study also showed strong pH dependence in the binding of NO to the reduced c heme. We have also analyzed the M?ssbauer spectra of the ferrous d1 heme-NO complex using a spin-Hamiltonian formalism. The magnetic hyperfine coupling tensor was found to be consistent with the unpaired electron residing on a sigma orbital.     

Semi-met oxidation level of chalcogenide derivatives of methemerythrin. M?ssbauer and EPR studies

Conclusive evidence is presented for an S = 1/2 spincoupled pair of high spin ferric and ferrous ions in the major reaction product of sulfide with the met form of the non-heme iron oxygen-carrying protein hemerythrin. Evidence for an analogous selenide derivative is also reported. M?ssbauer and EPR spectroscopy establish (a) the charge and spin states of the individual iron atoms in sulfidehemerythrin as Fe(III), S = 5/2, and Fe(II), S = 2, and (b) the existence of an antiferromagnetic exchange interaction that couples the two spins to a resultant spin S = 1/2. The combined M?ssbauer and EPR data confirm the correctness of the formulation first proposed for semi-methemerythrin by Harrington, P.C., de Waal, D.J.A., and Wilkins, R.G. ((1978) Arch. Biochem. Biophys. 191, 444-451) and furthermore show that a majority of the iron centers in the protein can be stabilized at this oxidation level. The results also demonstrate a new route to semi-methemerythrin. A titration of methemerythrin with selenide indicates that this derivative forms by a two step process consisting of first, reduction to the semi-met oxidation level by selenide and second, binding of selenide to either one or both irons.     

M?ssbauer and EPR spectroscopy of protocatechuate 3,4-dioxygenase from Pseudomonas aeruginosa.

Protocatechuate 3,4-dioxygenase (EC 1.13.11.3) from Pseudomonas aeruginosa has been investigated by EPR and M?ssbauer spectroscopy. Low temperature M?ssbauer data on the native enzyme (Fe3+, S = 5/2) yields a hyperfine field Hsat=-525 kG at the nucleus. This observation is inconsistent with earlier suggestions, based on EPR data of a rubredoxin-like ligand environment around the iron, i.e. a tetrahedral sulfur coordination. Likewise, the dithionite-reduced enzyme has M?ssbauer parameters unlike those of reduced rubredoxin. We conclude that the iron atoms are in a previously unrecognized environment. The ternary complex of the enzyme with 3,4-dihydroxyphenylpropionate and O2 yields EPR signals at g = 6.7 and g = 5.3; these signals result from an excited state Kramers doublet. The kinetics of the disappearance of these signals parallels product formation and the decay of the ternary complex as observed in the optical spectrum. The M?ssbauer and EPR data on the ternary complex establish the iron atoms to be a high-spin ferric state characterized by a large and negative zero-field splitting, D = approximately -2 cm-1.     

EPR and M?ssbauer studies of nucleotide-bound nitrogenase iron protein from Azotobacter vinelandii

We have recently shown (Lindahl, P. A., Day, E. P., Kent, T. A., Orme-Johnson, W. H., and Münck, E. (1985) J. Biol. Chem. 260, 11160-11173) that the [4Fe-4S]1+ cluster of the native Fe protein can exist in two forms characterized by different cluster spin: an S = 1/2 state exhibiting a g = 1.94 type EPR signal and an S = 3/2 state yielding signals at g approximately 5.8 and 5.1. We have now extended our study of the Fe protein to include the MgATP- and MgADP-bound forms. The [4Fe-4S]1+ cluster of the nucleotide-bound Fe protein exists in a similar S = 1/2, S = 3/2 spin mixture. The S = 3/2 cluster exhibits a broad EPR signal at g approximately 4.8. In spectra of the MgATP-bound protein, we have also observed a g = 4.3 signal from an S = 5/2 state (D = 1 - 3 cm-1, E/D approximately 0.32). Various experiments strongly suggest that this signal does not originate from adventitiously bound Fe3+. The g = 4.3 signal may arise from approximately 2% of the [4Fe-4S]1+ clusters when MgATP is protein-bound. We have also discovered substoichiometric amounts of what appears to be ADP in some nominally nucleotide-free Fe protein samples. MgATP binds to Fe protein in the presence of perturbing solvents, resulting in EPR spectra similar to those of MgATP-bound samples in aqueous solutions; MgADP binding, on the other hand, results in signals more typical of the solvent state. Spectra of samples frozen during turnover of the nitrogenase system exhibit a mixture of spin states. Characterization of the Fe protein EPR signature described here should aid future mechanistic and nucleotide-binding studies.     

Quantum chemical calculations of spectroscopic properties of metalloproteins and model compounds: EPR and Mössbauer properties

Recently developed theoretical methods to predict EPR and M?ssbauer parameters open the way for close interactions between theorists and experimentalists to elucidate the geometric and electronic structures of metalloenzymes and model complexes and to obtain insight into their reactive properties. Spectral calculations (g-values, hyperfine couplings, zero-field splittings, isomer shifts and quadrupole splittings) are also a means to validate theoretical approaches and therefore complement the prediction of geometries, reaction energies and transition states.     

Hexaheme nitrite reductase from Desulfovibrio desulfuricans. M?ssbauer and EPR characterization of the heme groups

M?ssbauer and EPR spectroscopy were used to characterize the heme prosthetic groups of the nitrite reductase isolated from Desulfovibrio desulfuricans (ATCC 27774), which is a membrane-bound multiheme cytochrome capable of catalyzing the 6-electron reduction of nitrite to ammonia. At pH 7.6, the as-isolated enzyme exhibited a complex EPR spectrum consisting of a low-spin ferric heme signal at g = 2.96, 2.28, and 1.50 plus several broad resonances indicative of spin-spin interactions among the heme groups. EPR redox titration studies revealed yet another low-spin ferric heme signal at g = 3.2 and 2.14 (the third g value was undetected) and the presence of a high-spin ferric heme. M?ssbauer measurements demonstrated further that this enzyme contained six distinct heme groups: one high-spin (S = 5/2) and five low-spin (S = 1/2) ferric hemes. Characteristic hyperfine parameters for all six hemes were obtained through a detailed analysis of the M?ssbauer spectra. D. desulfuricans nitrite reductase can be reduced by chemical reductants, such as dithionite or reduced methyl viologen, or by hydrogenase under hydrogen atmosphere. Addition of nitrite to the fully reduced enzyme reoxidized all five low-spin hemes to their ferric states. The high-spin heme, however, was found to complex NO, suggesting that the high-spin heme could be the substrate binding site and that NO could be an intermediate present in an enzyme-bound form.     

Identification of FeS clusters in the glycyl-radical enzyme benzylsuccinate synthase via EPR and M?ssbauer spectroscopy

The anaerobic degradation pathway of toluene is initiated by the addition of the methyl group of toluene to the double bond of fumarate. This reaction is catalyzed by a novel glycyl-radical enzyme, (R)-benzylsuccinate synthase (BSS). The enzyme consists of three subunits, α, β, and γ, and differs from most other glycyl-radical enzymes in having additional cofactors. We have purified a Strep-tagged nonactivated BSS from recombinant Escherichia coli and identified the additional cofactors as FeS clusters by UV/vis, EPR, and M?ssbauer spectroscopy. Analysis of the metal content as well as the EPR and M?ssbauer spectra indicated that BSS contains magnetically coupled low-potential [4Fe–4S] clusters. Several enzyme preparations showed differing amounts of [3Fe–4S] clusters that could be reconstituted to [4Fe–4S] clusters, indicating that they arise from partial decay of the initial [4Fe–4S] clusters. The most likely location of these FeS clusters in the enzyme are the small β and γ subunits, which are unique for the BSS subfamily of glycyl-radical enzymes and contain conserved cysteines as potential ligands.     

Unusual NMR, EPR, and M?ssbauer properties of Chromatium vinosum 2[4Fe-4S] ferredoxin.

The ferredoxin from Chromatium vinosum (CvFd) exhibits sequence and structure peculiarities. Its two Fe4S4(SCys)4 clusters have unusually low potential transitions that have been unambiguously assigned here through NMR, EPR, and M?ssbauer spectroscopy in combination with site-directed mutagenesis. The [4Fe-4S]2+/1+ cluster (cluster II) whose coordination sphere includes a two-turn loop between cysteines 40 and 49 was reduced by dithionite with an E degrees ' of -460 mV. Its S = 1/2 EPR signal was fast relaxing and severely broadened by g-strain, and its M?ssbauer spectra were broad and unresolved. These spectroscopic features were sensitive to small perturbations of the coordination environment, and they were associated with the particular structural elements of CvFd, including the two-turn loop between two ligands and the C-terminal alpha-helix. Bulk reduction of cluster I (E degrees ' = -660 mV) was not possible for spectroscopic studies, but the full reduction of the protein was achieved by replacing valine 13 with glycine due to an approximately 60 mV positive shift of the potential. At low temperatures, the EPR spectrum of the fully reduced protein was typical of two interacting S = 1/2 [4Fe-4S]1+ centers, but because the electronic relaxation of cluster I is much slower than that of cluster II, the resolved signal of cluster I was observed at temperatures above 20 K. Contact-shifted NMR resonances of beta-CH2 protons were detected in all combinations of redox states. These results establish that electron transfer reactions involving CvFd are quantitatively different from similar reactions in isopotential 2[4Fe-4S] ferredoxins. However, the reduced clusters of CvFd have electronic distributions that are similar to those of clusters coordinated by the CysIxxCysIIxxCysIII.CysIVP sequence motif found in other ferredoxins with different biochemical properties. In all these cases, the electron added to the oxidized clusters is mainly accommodated in the pair of iron ions coordinated by CysII and CysIV.     

EPR and M?ssbauer studies of protocatechuate 4,5-dioxygenase. Characterization of a new Fe2+ environment

Protocatechuate 4,5-dioxygenase from Pseudomonas testosteroni has been purified to homogeneity and crystallized. The iron containing, extradiol dioxygenase is shown to be composed of two subunit types (alpha, Mr = 17,700 and beta, Mr = 33,800) in a 1:1 ratio; such a composition has not been observed for other extradiol dioxygenases. The 4.2 K M?ssbauer spectrum of native protocatechuate 4,5-dioxygenase prepared from cells grown in 57Fe-enriched media consists of a doublet with quadrupole splitting, delta EQ = 2.22 mm/s, and isomer shift delta Fe = 1.28 mm/s, demonstrating a high spin Fe2+ site. These parameters, and the temperature dependence of delta EQ, are unique among enzymes but are strikingly similar to those reported for the reaction center of the photosynthetic bacterium Rhodopseudomonas sphaeroides R-26, suggesting very similar ligand environments. The Fe2+ of protocatechuate 4,5-dioxygenase can be oxidized, for instance by H2O2, to yield high spin Fe3+ with EPR g values around g = 6 (and g = 4.3). In the oxidized state, protocatechuate 4,5-dioxygenase is inactive; the iron, however, can be rereduced by ascorbate to yield active enzyme. Our data suggest that protocatechuate binds to Fe2+; the spectra indicate that the ligand binding is heterogenous. The M?ssbauer spectra observed here are fundamentally different from those reported earlier (Zabinski, R., Münck, E., Champion, P., and Wood, J. M. (1972) Biochemistry 11, 3212-3219). The spectra of the earlier (reconstituted) preparations, which had substantially lower specific activities, probably reflect adventitiously bound Fe3+. We discuss here how adventitiously bound iron can be identified and removed. The Fe2+ which is present in native protocatechuate 4,5-dioxygenase and its complexes with substrates and inhibitors reacts quantitatively with nitric oxide to produce a species with electronic spin S = 3/2. The EPR and M?ssbauer spectra of these complexes compare favorably with EDTA . Fe(II) . NO. We have studied the latter complex extensively and have analyzed the M?ssbauer spectra with an S = 3/2 spin Hamiltonian. EPR spectra show that protocatechuate 4,5-dioxygenase-NO complexes with substrates or inhibitors are heterogeneous and consist of several well defined subspecies. The data show that NO, and presumably also O2, has access to the active site Fe2+ in the enzyme-substrate complex. The use of EPR-detectable NO complexes as a rapid and sensitive tool for the study of the EPR silent active site iron of extradiol dioxygenases is discussed.     

Nitrogenase X: M?ssbauer and EPR studies on reversibly oxidized MoFe protein from Azotobacter vinelandii OP. Nature of the iron centers.

Under anaerobic conditions the molybdenum-iron protein (MoFe protein) from Azotobacter vinelandii can be reversibly oxidized with thionine. Electron paramagnetic resonance studies reveal that the oxidation proceeds in two distinct phases: the MoFe protein can be oxidized by four electrons without loss of the EPR signal from the S = 3/2 cofactor centers. A second oxidation step, involving two electrons, leads to the disappearance of the cofactor EPR signal. In order to correlate the events during the thionine titration with redox reactions involving individual iron centers we have studied the MoFe proteins from A vinelandii and Clostridium pasteurianum with M?ssbauer spectroscopy. Spectra were taken in the temperature range from 1.5 K to 200 K in applied magnetic fields of up to 54 kG. Analysis of the M?ssbauer data allows us to draw three major conclusions: (1) the holoprotein contains 30 +/- 2 iron atoms. (2) Most probably, 12 iron atoms belong to two, apparently identical, iron clusters (labeled M) which we have shown previously to be structural components of the iron and molybdenum containing cofactor of nitrogenase. The M-centers can be stabilized in three distinct oxidation states, MOXe- in equilibrium MNe- in equilibrium MR. The diamagnetic (S = 0) state MOX is attained by oxidation of the native state MN with either thionine or oxygen. MR is observed under nitrogen fixing conditions. (3) The data strongly suggest that 16 iron atoms are associated with four iron centers which we propose to call P-clusters. Each P-cluster contains four spin-coupled iron atoms. In the native protein the P-clusters are in the diamagnetic state PN, yielding the M?ssbauer signature which we have labeled previously 'components D and Fe2+'. Three irons of the D-type and one iron of the Fe2+-type appear to comprise a P-cluster. A one-electron oxidation yields the paramagnetic state POX. Although the state POX is characterized by half-integral electronic spin a peculiar combination of zero-field splitting parameters and spin relaxation renders this state EPR-silent. Spectroscopically, the P-clusters are novel structures; there is, however, evidence that they are closely related to familiar 4Fe-4S centers.     

Evidence for polynuclear aggregates of ferric daunomycin. A M?ssbauer, EPR, X-ray absorption spectroscopy and magnetic susceptibility study.

The interaction of the antitumor agent daunomycin (DN) with ferric iron has been analysed by M?ssbauer spectroscopy, EPR, extended X-ray absorption fine structure (EXAFS), and magnetic susceptibility measurements. In contrast to literature data, at millimolar iron and anthracycline concentrations no solitary Fe(DN)3 complexes are formed in appreciable amounts. The M?ssbauer spectroscopic analysis revealed severe dependencies on temperature, on the preparation procedure, the time allowed for equilibration, and on the metal/ligand ratio. The M?ssbauer spectra exhibit two components: a broad magnetic sextet and a quadrupole doublet at an Fe/DN molar ratio of 1:3 and exclusively a doublet at a molar ratio of 1:20, indicating an equilibrium of these two spectral components. The EPR spectra are dominated by a signal at g(eff) = 2. Double integration of the EPR signals enabled the determination of their spin density and a correlation between EPR and M?ssbauer spectra. The M?ssbauer sextet species is EPR invisible and corresponds to magnetically ordered polynuclear aggregates with high magnetic anisotropy. EXAFS and susceptibility measurements provide additional evidence for the formation of polynuclear aggregates of ferric daunomycin. The quadrupole doublet species in the M?ssbauer spectra correlates with the g = 2 signal in EPR. This species is also related to a magnetically ordered system, exhibiting, however, superparamagnetic behavior due to less magnetic anisotropy. Since daunomycin forms dimers in aqueous solution at millimolar concentrations, we conclude that the cooperative phenomena observed in EPR and M?ssbauer spectra are a consequence of its stacking effects.     

M?ssbauer spectroscopic studies of the cores of human, limpet and bacterial ferritins

Ferritin cores from human spleen, limpet (Patella vulgata) haemolymph and bacterial (Pseudomonas aeruginosa) cells have been investigated using 57Fe M?ssbauer spectroscopy. The M?ssbauer spectra were recorded over a range of temperatures from 1.3 to 78 K, all the spectra are quadrupole-split doublets with similar quadrupole splittings and isomer shifts, characteristic of iron(III), while at sufficiently low temperatures the spectra of all the samples show well-resolved magnetic splitting. At intermediate temperatures, the spectra from the human ferritin exhibit typical superparamagnetic behaviour, while those from the bacterial ferritin show behaviour corresponding to a transition from a magnetically ordered to a paramagnetic state. The spectra from the limpet ferritin show a complex combination of the two effects. The results are discussed in terms of the magnetic behaviour of small particles. The data are consistent with magnetic ordering temperatures of about 3 and 30 K for the bacterial and limpet ferritin cores, respectively, while the data indicate that the magnetic ordering temperature for the human ferritin cores must be above 50 K. These differences are interpreted as being related to different densities of iron in the cores and to variations in the composition of the cores. The human ferritin cores are observed to have a mean superparamagnetic blocking temperature of about 40 K, while that of the limpet ferritin cores is about 25 K. This difference is interpreted as being due not only to different mean numbers of iron atoms in the two types of core but also to the higher degree of crystallinity in the cores of the human ferritin.     

M?ssbauer spectroscopy on nonequilibrium states of myoglobin: a study of r-t relaxation.

A frozen solution of 57Fe-enriched metmyoglobin was irradiated by x rays at 77 K. Mössbauer spectra showed a reduction of Fe(III) high spin by thermalized electrons and a production of a metastable Fe(II) low spin myoglobin complex with H2O at its sixth coordination site. The relaxation of the intermediate was investigated by Mössbauer spectroscopy as a function of temperature and time. The relaxation process starts above 140 K and is fully completed at approximately 200 K. At temperatures between 140 and 200 K, the relaxation lasts for hours and is nonexponential in time. Up to 180 K, the process can be described satisfactorily by a gamma distribution of activation enthalpies with an Arrhenius relation for the rate coefficient. The temperature and time dependence of the Mössbauer parameters indicates structural changes in the active center of the protein as early as 109 K that continue for several hours at higher temperatures. Above 180 K, structural rearrangements involving the whole protein molecule lead to a shift and narrowing of the barrier height distribution.     

M?ssbauer, EPR, and optical studies of the corrinoid/iron-sulfur protein involved in the synthesis of acetyl coenzyme A by Clostridium thermoaceticum

We have purified to homogeneity the 88-kDa corrinoid protein from Clostridium thermoaceticum which acts as a methyl carrier in the synthesis of acetyl-CoA. As shown here, this protein contains a [4Fe-4S]1+/2+ cluster in addition to a corrinoid. The corrinoid is 5-methoxybenzimidazolylcobamide, with an OH- group probably present as the upper axial ligand. Co+ is present in the reduced form, Co2+ in the as-isolated form, and Co3+ in the methylated form of the protein. The as-isolated corrinoid/Fe-S protein exhibits a Co2+ EPR signal lacking nitrogen superhyperfine splittings, indicating that the benzimidazole base is uncoordinated ("base-off") in the Co2+ state. Optical studies suggest that the Co3+-CH3 corrinoid is also base-off. In the as-isolated and methylated forms, the iron-sulfur cluster is diamagnetic, with quadrupole splittings and isomer shifts characteristic of [4Fe-4S]2+ clusters. The protein can be reduced by CO and CO dehydrogenase in the absence of ferredoxin. The EPR spectra of the reduced cluster exhibit two components: one with principal g-values at 2.07, 1.93, and 1.82 and the other at 2.02, 1.94, and 1.86. The M?ssbauer data show that these signals result from [4Fe-4S]1+ clusters. Chemical analysis shows that the iron:cobalt atomic ratio is close to 4:1, suggesting that a single [4Fe-4S]1+ cluster occurs in two distinct S = 1/2 spin states in the reduced state. Treatment with 1-2.5 M urea converts the two cluster forms into a single one, with EPR and M?ssbauer spectra of typical [4Fe-4S]1+ clusters. A 27-kDa corrinoid protein (Ljungdahl, L.G., LeGall, J., and Lee, J.P. (1973) Biochemistry 12, 1802-1808) also was purified and found to be inactive in the synthesis of acetyl-CoA, contrary to the suggestion of Ljungdahl et al. (1973).