Reduced forms of the C56S and C60S variants of the thioredoxin-like Clostridium pasteurianum [Fe2S2] ferredoxin (CpFd) provide the only known examples of valence-delocalized [Fe2S2](+) clusters, which constitute a fundamental building block of all higher nuclearity Fe-S clusters. In this work, we have revisited earlier work on the CpFd variants and carried out redox and spectroscopic studies on the [Fe2S2](2+,+) centers in wild-type and equivalent variants of the highly homologous and structurally characterized Aquifex aeolicus ferredoxin 4 (AaeFd4) using EPR, UVvisibleNIR absorption, CD and variable-temperature MCD, and proteinfilm electrochemistry. The results indicate that the [Fe2S2](+) centers in the equivalent AaeFd4 and CpFd variants reversibly interconvert between similar valence-localized S = 1/2 and valence-delocalized S = 9/2 forms as a function of pH, with pK(a) values in the range 8.3-9.0, because of protonation of the coordinated serinate residue. However, freezing high-pH samples results in partial or full conversion from valence-delocalized S = 9/2 to valence-localized S = 1/2 [Fe2S2](+) clusters. MCD saturation magnetization data for valence-delocalized S = 9/2 [Fe2S2](+) centers facilitated determination of transition polarizations and thereby assignments of low-energy MCD bands associated with the FeFe interaction. The assignments provide experimental assessment of the double exchange parameter, B, for valence-delocalized [Fe2S2](+) centers and demonstrate that variable-temperature MCD spectroscopy provides a means of detecting and investigating the properties of valence-delocalized S = 9/2 [Fe2S2](+) fragments in higher nuclearity FeS clusters. The origin of valence delocalization in thioredoxin-like ferredoxin Cys-to-Ser variants and FeS clusters in general is discussed in light of these results.

We have employed EPR and a set of recently developed electron nuclear double resonance (ENDOR) spectroscopies to characterize a suite of [2Fe–2S] ferredoxin clusters from Aquifex aeolicus (Aae Fd1, Fd4, and Fd5). Antiferromagnetic coupling between the FeII, S = 2, and FeIII, S = 5/2, sites of the [2Fe–2S]+ cluster in these proteins creates an S = 1/2 ground state. A complete discussion of the spin-Hamiltonian contributions to g includes new symmetry arguments along with references to related FeS model compounds and their symmetry and EPR properties. Complete 57Fe hyperfine coupling (hfc) tensors for each iron, with respective orientations relative to g, have been determined by the use of “stochastic” continuous wave and/or “random hopped” pulsed ENDOR, with the relative utility of the two approaches being emphasized. The reported hyperfine tensors include absolute signs determined by a modified pulsed ENDOR saturation and recovery (PESTRE) technique, RD-PESTRE—a post-processing protocol of the “raw data” that comprises an ENDOR spectrum. The 57Fe hyperfine tensor components found by ENDOR are nicely consistent with those previously found by Mössbauer spectroscopy, while accurate tensor orientations are unique to the ENDOR approach. These measurements demonstrate the capabilities of the newly developed methods. The high-precision hfc tensors serve as a benchmark for this class of FeS proteins, while the variation in the 57Fe hfc tensors as a function of symmetry in these small FeS clusters provides a reference for higher-nuclearity FeS clusters, such as those found in nitrogenase.

An inventory of unique local protein folds around Fe-S clusters has been derived from the analysis of protein structure databases. Nearly 50 such folds have been identified, and over 90% of them harbor low-potential [2Fe-2S](2+,+) or [4Fe-4S](2+,+) clusters. In contrast, high-potential Fe-S clusters, notwithstanding their structural diversity, occur in only three different protein folds. These observations suggest that the extant population of Fe-S protein folds has to a large extent been shaped in the reducing iron- and sulfur-rich environment that is believed to have predominated on this planet until approximately two billion years ago. High-potential active sites are then surmised to be rarer because they emerged later, in a more oxidizing biosphere, in conditions where iron and sulfide had become poorly available, Fe-S clusters were less stable, and in addition faced competition from heme iron and copper active sites. Among the low-potential Fe-S active sites, protein folds hosting [4Fe-4S](2+,+) clusters outnumber those with [2Fe-2S](2+,+) ones by a factor of 3 at least. This is in keeping with the higher chemical stability and versatility of the tetranuclear clusters, compared with the binuclear ones. It is therefore suggested that, at least while novel Fe-S sites are evolving within proteins, the intrinsic chemical stability of the inorganic moiety may be more important than the stabilizing effect of the polypeptide chain. The discovery rate of novel Fe-S-containing protein folds underwent a sharp increase around 1995, and has remained stable to this day. The current trend suggests that the mapping of the Fe-S fold space is not near completion, in agreement with predictions made for protein folds in general. Altogether, the data collected and analyzed here suggest that the extant structural landscape of Fe-S proteins has been shaped to a large extent by primeval geochemical conditions on one hand, and iron-sulfur chemistry on the other.

We have used (57)Fe nuclear resonance vibrational spectroscopy (NRVS) to study the Fe(2)S(2)(Cys)(4) sites in oxidized and reduced [2Fe-2S] ferredoxins from Rhodobacter capsulatus (Rc FdVI) and Aquifex aeolicus (Aa Fd5). In the oxidized forms, nearly identical NRVS patterns are observed, with strong bands from Fe-S stretching modes peaking around 335 cm(-1), and additional features observed as high as the B(2u) mode at approximately 421 cm(-1). Both forms of Rc FdVI have also been investigated by resonance Raman (RR) spectroscopy. There is good correspondence between NRVS and Raman frequencies, but because of different selection rules, intensities vary dramatically between the two kinds of spectra. For example, the B(3u) mode at approximately 288 cm(-1), attributed to an asymmetric combination of the two FeS(4) breathing modes, is often the strongest resonance Raman feature. In contrast, it is nearly invisible in the NRVS, as there is almost no Fe motion in such FeS(4) breathing. NRVS and RR analysis of isotope shifts with (36)S-substituted into bridging S(2-) ions in Rc FdVI allowed quantitation of S(2-) motion in different normal modes. We observed the symmetric Fe-Fe stretching mode at approximately 190 cm(-1) in both NRVS and RR spectra. At still lower energies, the NRVS presents a complex envelope of bending, torsion, and protein modes, with a maximum at 78 cm(-1). The (57)Fe partial vibrational densities of states (PVDOS) were interpreted by normal-mode analysis with optimization of Urey-Bradley force fields. Progressively more complex D(2h) Fe(2)S(2)S'(4), C(2h) Fe(2)S(2)(SCC)(4), and C(1) Fe(2)S(2)(Cys)(4) models were optimized by comparison with the experimental spectra. After modification of the CHARMM22 all-atom force field by the addition of refined Fe-S force constants, a simulation employing the complete protein structure was used to reproduce the PVDOS, with better results in the low frequency protein mode region. This process was then repeated for analysis of data on the reduced FdVI. Finally, the degree of collectivity was used to quantitate the delocalization of the dynamic properties of the redox-active Fe site. The NRVS technique demonstrates great promise for the observation and quantitative interpretation of the dynamical properties of Fe-S proteins.

A method is presented to derive anomalous scattering contributions for individual atoms within a protein crystal by collecting several sets of diffraction data at energies spread along an X-ray absorption edge of the element in question. The method has been applied to a [2Fe:2S] ferredoxin model system with localized charges in the reduced state of the iron−sulfur cluster. The analysis shows that upon reduction the electron resides at the iron atom closer to the protein surface. The technique should be sufficiently sensitive for more complex clusters with noninteger redox states and is generally applicable given that crystals are available.

Most hydrogenases (H2ases), the enzymes that produce or oxidize dihydrogen, possess dimetallic active sites and belong to either one of two phylogenetically distinct classes, the [NiFe] and the [FeFe] H2ases. These families of H2ases share a number of similarities regarding active site structure and reaction mechanism, as a result of convergent evolution. They are otherwise alien to each other, in particular with respect to protein sequence and structure, maturation mechanisms, and distribution among the realms of life. One of the interesting features of [FeFe] H2ases is their occurrence in anaerobic bacteria, anaerobic protists, and mitochondriate eukaryotes. They thus have the potential to report on important evolutionary events, including transitions from the prokaryote to the eukaryote lifestyle. Genome sequences yield a variety of [FeFe] H2ase sequences that have been implemented to shed light on the evolution of these proteins and their host organisms.

Resonance Raman spectra of native 2[4Fe-4S] ferredoxin from Clostridium pasteurianum and of its selenium-substituted analogue 2[4Fe-4Se] are compared. The experimental conditions used in this study included low temperature (approx. 25 K) and the absence of a glass sample cell, thus ensuring high signal-to-noise ratios. The spectra of the 2[4Fe-4S] and 2[4Fe-4Se] ferredoxins display similar numbers of bands, but the resonance Raman patterns differ largely, except for two bands observed at 353 cm - I and 365 cm- 1 in spectra of the native ferredoxin, which are only moderately shifted upon S-+Se substitution and are attributed to Fe-S(cysteine) stretching modes. The activities of the latter modes, enhanced by 457.9nm excitation, are nearly equal in both ferredoxins. These data were used to demonstrate the presence ofhybrid clusters [4Fe-(4 - n)S-nSe] (n = 1, 2, 3) in a ferredoxin the active sites of which had been reconstituted in the presence of both S and Se.

Up to 25% of plastic waste in Europe is still disposed of in landfills, despite recycling efforts. The plastic waste in the landfill plot may be exposed both to abiotic and biotic degradation processes, although it is thought that most of the plastic materials tend to be resistant to biodegradation or biodeterioration even after a long time. To verify if polypropylene (PP) can undergo the process of short-term biodegradation and how this process is manifested in a municipal waste landfill, we collected a plastic sample from an already closed landfill plot estimating its age at approximately 5 years. Fourier-Transform Infrared Spectroscopy led to sample identification as PP as well as showed additional bands which are not specific to polymer structure but rather result from microbial metabolism. Differential Scanning Calorimetry was performed to examine the influence of the environmental degradation process on the degree of crystallisation of the tested PP. Moreover, significant changes on the surface of an old PP packaging were observed with Scanning Electron Microscopy (SEM) showing clear signs of PP delamination which resulted in microplastic particles formation (smaller than 5 μm in diameter). Additionally, several round and oval shaped structures were observed with SEM leading to the suspicion of biofilm formation on the PP surface. Indeed, the microorganisms were present in a vast amount on the old PP surface and possibly formed a viable biofilm as it was confirmed with fluorescence microscopy. These data show that plastic waste can be inhabited by microorganisms from the ambient environment which may probably lead to its faster degradation. However, this process should be investigated in more detail in order to shed light upon the possible risk factors of plastic biodegradation in waste landfills to the environment and human health. Even after five years, polypropylene can undergo deterioration/biodegradation in a waste landfill with viable microbial cells on its surface, possibly involved in its degradation.

Recent shotgun sequencing of filtered Sargasso Sea water samples has yielded data in astounding amount and diversity. Iron–sulfur proteins, which are ancient, diverse and ubiquitous, have been implemented here to further probe the sequence diversity of the Sargasso Sea database (SSDB). Sequence searches and comparisons confirm that the SSDB by and large equals in diversity the combined currently available databases. The data thus suggest that microbial diversity has so far been underestimated by orders of magnitude.

Analysis of the genome of the hyperthermophilic bacterium Aquifex aeolicus has revealed the presence of a previously undetected gene potentially encoding a plant- and mammalian-type [2Fe-2S] ferredoxin. Expression of that gene in Escherichia coli has yielded a novel thermostable [2Fe-2S] ferredoxin (designated ferredoxin 5) whose sequence is most similar to those of ferredoxins involved in the assembly of iron-sulfur clusters (Isc-Fd). It nevertheless differs from the latter proteins by having deletions near its N- and C-termini, and no cysteine residues other than those involved in [2Fe-2S] cluster coordination. Resonance Raman, low-temperature MCD and EPR studies show close spectral similarities between ferredoxin 5 and the Isc-Fd from Azotobacter vinelandii. Mössbauer spectra of the reduced protein were analyzed with an S = 1/2 spin Hamiltonian and interpreted in the framework of the ligand field model proposed by Bertrand and Gayda. The redox potential of A. aeolicus ferredoxin 5 (-390 mV) is in keeping with its relatedness to Isc-Fd. Unfolding experiments showed that A. aeolicus ferredoxin 5 is highly thermostable (T(m) = 106 degrees C at pH 7), despite being devoid of features (e.g., high content of charged residues) usually associated with extreme thermal stability. Searches for genes potentially encoding plant-type [2Fe-2S] ferredoxins have been performed on the sequenced genomes of hyperthermophilic organisms. None other than the two proteins from A. aeolicus were retrieved, indicating that this otherwise widely distributed group of proteins is barely represented among hyperthermophiles.

A [2Fe-2S] ferredoxin (Fd1) from the hyperthermophilic bacterium Aquifex aeolicus has been obtained by heterologous expression of the encoding gene in Escherichia coli. Sequence comparisons show that this protein belongs to the extended family of plant- and mammalian-type [2Fe-2S] ferredoxins but also indicate that it is not closely similar to either the plant-type or mammalian-type subfamilies. Instead, it appears to bear some similarity to novel members of this family, in particular the Isc-type ferredoxins involved in the assembly of iron-sulfur clusters in vivo. The two redox levels of the [2Fe2S](2+/+) metal site of A. aeolicus ferredoxin have been studied by UV-visible, resonance Raman, EPR, variable temperature magnetic circular dichroism, and Mossbauer spectroscopies. A full-spin Hamiltonian analysis is given for the Mossbauer spectra. In aggregate, the spectroscopic data reveal differences with both the plant-type and mammalian-type ferredoxins, in keeping with the sequence comparisons. The midpoint potential of the [2Fe-2S](2+/+) couple, at -375 mV versus the normal hydrogen electrode, is more negative than those of mammalian-type ferredoxins and at the upper end of the range covered by plant-type ferredoxins. A. aeolicus ferredoxin contains two cysteines in addition to the four that are committed as ligands of the [2Fe-2S] cluster. These two residues have been shown by chemical modification and site-directed mutagenesis to form a disulfide bridge in the native protein. While that cystine unit plays a significant role in the exceptional thermostability of A. aeolicus ferredoxin (T-m = 121 degreesC at pH 7 versus T-m = 113 degreesC in a molecular variant where the disulfide bridge has been removed), it does not bear on the properties of the [2Fe-2S](2+/+) chromophore. This observation is consistent with the large distance (ca. 20 Angstrom) that is predicted to separate the iron-sulfur chromophore from the disulfide bridge.

The [Fe(II)(Cys)(4)](2-) site of rubredoxin from Clostridium pasteurianum (Rd(red)) has been studied by Mössbauer spectroscopy in both purified protein and whole cells of Escherichia coli overproducing it. Excellent fits were obtained to an S = 2 spin Hamiltonian for D = 5.7(3) cm(-1), E/D = 0.25(2), delta = 0.70(3) mm/s, DeltaE(Q) = -3.25(2) mm/s, eta = 0.75(5), A(x) = -20.1(7) MHz, A(y) = -11.3(2) MHz, and A(z) = -33.4(14) MHz. These parameters were analyzed with crystal-field theory for the (5)D manifold of iron(II), revealing a d(z(2)) orbital ground state that is admixed by approximately 0.21 d(x(2) - y(2)). The spin-Hamiltonian parameters are consistent within the (5)D theory, apart from the zero-field splitting parameter, D. This problem was solved by extending the crystal-field treatment with spin-orbit coupling to spin-triplet d-d excited states of the iron. Theoretical estimates are given for the spin-triplet (D(T)) and spin-quintet contributions (D(Q)) to D based on excitation energies derived from time-dependent density functional theory, TD-DFT. The computational results were interpreted in terms of crystal-field theory, yielding the Racah parameters B = 682 cm(-1) and C = 2583 cm(-1). The theoretical analysis gives the relative magnitudes D(Q):D(T):D(ss) = 51%: 42%:7% (D(ss) originates from spin-spin interaction). The DFT analysis corroborates the pivotal role of the torsion angles (omega(i)) of the C-S(i) bonds in shaping the electronic structure of the iron(II) site. Rd(red) in overexpressing whole cells accounts for 60% of the Mössbauer absorption. The Rd(red) spectra from whole cells are virtually identical to those of the purified protein. By using the theoretical omega dependence of the spin Hamiltonian parameters, the torsions for Rd(red) in whole cells and purified protein samples are estimated to be the same within 2 degrees. These findings establish Mössbauer spectroscopy as a structural tool for investigating iron sites in whole cells.

The [2Fe-2S] ferredoxin (Fd4) from Aquifex aeolicus adopts a thioredoxin-like polypeptide fold that is distinct from other [2Fe-2S] ferredoxins. Crystal structures of the Cys-55 --> Ser (C55S) and Cys-59 --> Ser (C59S) variants of this protein have been determined to 1.25 Angstrom and 1.05 Angstrom resolution, respectively, whereas the resolution of the wild type (WT) has been extended to 1.5 Angstrom. The improved WT structure provides a detailed description of the [2Fe-2S] cluster, including two features that have not been noted previously in any [2Fe-2S] cluster-containing protein, namely, pronounced distortions in the cysteine coordination to the cluster and a Calpha-H-Sgamma hydrogen bond between cluster ligands Cys-55 and Cys-9. These features may contribute to the unusual electronic and magnetic properties of the [2Fe-2S] clusters in WT and variants of this ferredoxin. The structures of the two variants of Fd4, in which single cysteine ligands to the [2Fe-2S] cluster are replaced by serine, establish the metric details of serine-ligated Fe-S active sites with unprecedented accuracy. Both the cluster and its surrounding protein matrix change in subtle ways to accommodate this ligand substitution, particularly in terms of distortions of the Fe2S2 inorganic core from planarity and displacements of the polypeptide chain. These high resolution structures illustrate how the interactions between polypeptide chains and Fe-S active sites reflect combinations of flexibility and rigidity on the part of both partners; these themes are also evident in more complex systems, as exemplified by changes associated with serine ligation of the nitrogenase P cluster.

Aquifex aeolicus is the only hyperthermophile that is known to contain a plant- and mammalian-type [2Fe–2S] ferredoxin (Aae Fd1). This unique protein contains two cysteines, in addition to the four that act as ligands of the [2Fe–2S] cluster, which form a disulfide bridge. We have investigated the stability of Aae Fd1 with (wild-type) and without (C87A variant) the disulfide bond, with respect to pH, thermal and chemical perturbation, and compared the results to those for the mesophilic [2Fe–2S] ferredoxin from spinach. Unfolding reactions of all three proteins are irreversible due to cluster decomposition in the unfolded state. Wild-type and C87A Aae Fd1 proteins are extremely stable: unfolding at 20 °C requires high concentrations of the chemical denaturant and long incubation times. Moreover, their thermal-unfolding midpoints are 40–50° higher than that for spinach ferredoxin (pH 7). The stability of the Aae Fd1 protein is significantly lower at pH 2.5 than pH 7 and 10, suggesting that ionic interactions play a role in structural integrity. Interestingly, the iron–sulfur cluster in C87A Aae Fd1 rearranges into a transient species with absorption bands at 520 and 610 nm, presumably a linear three-iron cluster, in the high-pH unfolded state.

Many eubacterial genomes including those of Salmonella typhimurium, Streptococcus mutans, and Thermus aquaticus encode a dedicated flavoprotein reductase (AhpF, Nox1, or PrxR) just downstream of the structural gene for their peroxiredoxin (Prx, AhpC) homologue to reduce the latter protein during turnover. In contrast, the obligate anaerobe Clostridium pasteurianum codes for a two-component reducing system upstream of the ahpC homologue. These three structural genes, herein designated cp34, cp9, and cp20, were previously identified upstream of the rubredoxin gene in C. pasteurianum, but were not linked to expression of the latter gene [Mathieu, I., and Meyer, J. (1993) FEMS Microbiol. Lett. 112, 223-227]. cp34, cp9, and cp20 have been expressed in Escherichia coli, and their products have been purified and characterized. Cp34 and Cp9 together catalyze the NADH-dependent reduction of Cp20 to effect the reduction of various hydroperoxide substrates. Cp34, containing noncovalently bound FAD and a redox-active disulfide center, is an unusual member of the low-M(r) thioredoxin reductase (TrxR) family. Like Escherichia coli TrxR, Cp34 lacks the 200-residue N-terminal AhpC-reducing domain present in S. typhimurium AhpF. Although Cp34 is more similar to TrxR than to AhpF in sequence comparisons of the nucleotide-binding domains, experiments demonstrated that NADH was the preferred reductant (Km = 2.65 microM). Cp9 (a distant relative of bacterial glutaredoxins) is a direct electron acceptor for Cp34, possesses a redox-active CXXC active site, and mediates the transfer of electrons from Cp34 to several disulfide-containing substrates including 5,5'-dithiobis(2-nitrobenzoic acid), insulin, and Cp20. These three proteins are proposed to play a vital role in the defense of C. pasteurianum against oxidative damage and may help compensate for the putative lack of catalase activity in this organism.

Hydrogenases (H2ases) catalyze the reversible oxidation of molecular hydrogen and play a central role in microbial energy metabolism. Most of these enzymes are found in Archaea and Bacteria, but a few are present in Eucarya as well. They can be distributed into three classes: the [Fe]-H2ases, the [NiFe]-H2ases, and the metal-free H2ases. The vast majority of known H2ases belong to the first two classes, and over 100 of these enzymes have been characterized genetically and/or biochemically. Compelling evidence from sequences and structures indicates that the [NiFe]- and [Fe]-H2ases are phylogenetically distinct classes of proteins. The catalytic core of the [NiFe]-H2ases is a heterodimeric protein, although additional subunits are present in many of these enzymes. Functional classes of [NiFe]-H2ases have been defined, and they are consistent with categories defined by sequence similarity of the catalytic subunits. The catalytic core of the [Fe]-H2ases is a ca. 350-residue domain that accommodates the active site (H-cluster). A few monomeric [Fe]-H2ases are barely larger than the H-cluster domain. Many others are monomeric as well, but possess additional domains that contain redox centers, mostly iron-sulfur. Some [Fe]-H2ases are oligomeric. The modular structure of H2ases is strikingly illustrated in recently unveiled sequences and structures. It is also remarkable that most of the accessory domains and subunits of H2ases have counterparts in other redox complexes, in particular NADH-ubiquinone oxidoreductase (Complex I) of respiratory chains. Microbial genome sequences are bringing forth a significant body of additional H2ase sequence data and contribute to the understanding of H2ase distribution and evolution. Altogether, the available data suggest that [Fe]-H2ases are restricted to Bacteria and Eucarya, while [NiFe]-H2ases, with one possible exception, seem to be present only in Archaea and Bacteria. H2ase processing and maturation involve the products of several genes which have been identified and are currently being characterized in the case of the [NiFe]-H2ases. In contrast, near to nothing is known regarding the maturation of the [Fe]-H2ases. Inspection of the currently available genome sequences suggests that the [NiFe]-H2ase maturation proteins have no similar counterparts in the genomes of organisms possessing [Fe]-H2ases only. This observation, if confirmed, would be consistent with the phylogenetic distinctiveness of the two classes of H2ases. Sequence alignments of catalytic subunits of H2ases have been implemented to construct phylogenetic trees that were found to be consistent, in the main, with trees derived from other data. On the basis of the comparisons performed and discussed here, proposals are made to simplify and rationalize the nomenclature of H2ase-encoding genes.

Most low‐potential ferredoxins (Fds) are of the well‐known [2Fe–2S] plant or [4Fe–4S] bacterial type. Yet, an additional class of [2Fe–2S] Fds has been recognized on the basis of sequence and spectroscopic idiosyncrasies. A recent crystal structure has confirmed the uniqueness of this third kind of Fd, and shown that these proteins display an unexpected structural similarity to thioredoxin. The properties of these thioredoxin‐like [2Fe–2S] Fds are summarized, and hypotheses concerning their function are discussed.