¹H, ¹⁵N, and ¹³C chemical shift assignments for the winged helix domains of two archeal MCM C-termini

High-fidelity replication guarantees the stable inheritance of genetic information stored in the DNA of living organisms. The minichromosome maintenance (MCM) complex functions as replicative DNA-unwinding helicase and has been identified as one key player in the replication process of archea and eukarya. Despite the availability of considerable structural information on archeal MCMs, such information was missing for their C-terminal domain. In order to obtain more detailed structural information, we assigned the NMR chemical shifts for backbone and side chain nuclei for the MCM C-terminal winged helix domains of the archeal species Methanothermobacter thermautrophicus and Sulfolobus solfataricus.

De novo modeling of the F(420)-reducing [NiFe]-hydrogenase from a methanogenic archaeon by cryo-electron microscopy

Methanogenic archaea use a [NiFe]-hydrogenase, Frh, for oxidation/reduction of F420, an important hydride carrier in the methanogenesis pathway from H2 and CO2. Frh accounts for about 1% of the cytoplasmic protein and forms a huge complex consisting of FrhABG heterotrimers with each a [NiFe] center, four Fe-S clusters and an FAD. Here, we report the structure determined by near-atomic resolution cryo-EM of Frh with and without bound substrate F420. The polypeptide chains of FrhB, for which there was no homolog, was traced de novo from the EM map. The 1.2-MDa complex contains 12 copies of the heterotrimer, which unexpectedly form a spherical protein shell with a hollow core. The cryo-EM map reveals strong electron density of the chains of metal clusters running parallel to the protein shell, and the F420-binding site is located at the end of the chain near the outside of the spherical structure. DOI:http://dx.doi.org/10.7554/eLife.00218.001.

Overexpression of a protein disulfide isomerase-like protein from Methanothermobacter thermoautotrophicum enhances mercury tolerance in transgenic rice

MTH1745, from thermophilic archaea Methanothermobacter thermoautotrophicum, is a protein disulfide isomerase-like protein (PDIL) with a chaperone function and disulfide isomerase activity. Mercuric cations have a high affinity for sulfhydryl groups and consequently inhibit plant growth. Disulfide compounds (e.g., copper-zinc superoxide dismutase, Cu/Zn SOD) and sulfhydryl compounds (e.g., glutathione, phytochelatins, and metallothioneins) play important roles in mercury (Hg) response. To study the relationship between Hg detoxification and PDILs, we overexpressed MTH1745 in Oryza sativa L. cv. Nipponbare by Agrobacterium-mediated transformation. The transgenic rice seedlings displayed Hg tolerance with obvious phenotypes and more effective photosynthesis compared to wild-type plants. Furthermore, lower levels of superoxide anion radicals, hydrogen peroxide, and malondialdehyde were observed in leaves or roots of transgenic plants. Antioxidant enzyme activities of superoxide dismutase and peroxidase were notably higher in transgenic seedlings under different concentrations of mercuric chloride. Moreover, increased content of non-protein thiols, reduced glutathione (GSH), and GSH/GSSG (GSSG, oxidized glutathione) ratio were also observed in the detoxification of Hg. These results indicated that heterologous expression of a PDIL from extremophiles in rice could protect the synthesis, increase stability of proteins, and enhance Hg tolerance in rice.

Product deuterium isotope effects for orotidine 5'-monophosphate decarboxylase: effect of changing substrate and enzyme structure on the partitioning of the vinyl carbanion reaction intermediate

A product deuterium isotope effect (PIE) of 1.0 was determined as the ratio of the yields of [6-(1)H]-uridine 5'-monophosphate (50%) and [6-(2)H]-uridine 5'-monophosphate (50%) from the decarboxylation of orotidine 5'-monophosphate (OMP) in 50/50 (v/v) HOH/DOD catalyzed by orotidine 5'-monophosphate decarboxylase (OMPDC) from Saccharomyces cerevisiae, Methanothermobacter thermautotrophicus, and Escherichia coli. This unitary PIE eliminates a proposed mechanism for enzyme-catalyzed decarboxylation in which proton transfer from Lys-93 to C-6 of OMP provides electrophilic push to the loss of CO(2) in a concerted reaction. We propose that the complete lack of selectivity for the reaction of solvent H and D, which is implied by the value of PIE = 1.0, is enforced by restricted C-N bond rotation of the -CH(2)-NL(3)(+) group of the side chain of Lys-93. A smaller PIE of 0.93 was determined as the ratio of the product yields for OMPDC-catalyzed decarboxylation of 5-fluoroorotidine 5'-monophosphate (5-FOMP) in 50/50 (v/v) HOH/DOD. Mutations on the following important active-site residues of OMPDC from S. cerevisiae have no effect on the PIE on OMPDC-catalyzed decarboxylation of OMP or decarboxylation of 5-FOMP: R235A, Y217A, Q215A, S124A, and S154A/Q215A.

1H, 13C and 15N resonance assignment of a zinc-binding methionine sulfoxide reductase type-B from the thermophilic archeabacterium Methanothermobacter thermoautotrophicus

The (1)H, (13)C and (15)N resonance assignment of a type-B zinc-binding methionine sulfoxide reductase lacking a 'recycling' cysteine from the thermophilic archeabacterium Methanothermobacter thermoautotrophicus is reported.

A novel biosynthetic pathway of archaetidyl-myo-inositol via archaetidyl-myo-inositol phosphate from CDP-archaeol and D-glucose 6-phosphate in methanoarchaeon Methanothermobacter thermautotrophicus cells

Ether-type inositol phospholipids are ubiquitously distributed in Archaea membranes. The present paper describes a novel biosynthetic pathway of the archaeal inositol phospholipid. To study the biosynthesis of archaetidylinositol in vitro, we prepared two possible substrates: CDP-archaeol, which was chemically synthesized, and myo-[(14)C]inositol 1-phosphate, which was enzymatically prepared from [(14)C]glucose 6-phosphate with the inositol 1-phosphate (IP) synthase of this organism. The complete structure of the IP synthase reaction product was determined to be 1l-myo-inositol 1-phosphate, based on gas liquid chromatography with a chiral column. When the two substrates were incubated with the Methanothermobacter thermautotrophicus membrane fraction, archaetidylinositol phosphate (AIP) was formed along with a small amount of archaetidylinositol (AI). The two products were identified by fast atom bombardment-mass spectrometry and chemical analyses. AI was formed from AIP by incubation with the membrane fraction, but AIP was not formed from AI. This finding indicates that archaeal AI was synthesized from CDP-archaeol and d-glucose 6-phosphate via myo-inositol 1-phosphate and AIP. Although the relevant enzymes were not isolated, three enzymes are implied: IP synthase, AIP synthase, and AIP phosphatase. AIP synthase was homologous to yeast phosphatidylinositol synthase, and we confirmed AIP synthase activity by cloning the encoding gene (MTH1691) and expressing it in Escherichia coli. AIP synthase is a newly found member of the enzyme superfamily CDP-alcohol phosphatidyltransferase, which includes a wide range of enzymes that attach polar head groups to ester- and ether-type phospholipids of bacterial and archaeal origin. This is the first report of the biosynthesis of ether-type inositol phospholipids in Archaea.

DNA uracil repair initiated by the archaeal ExoIII homologue Mth212 via direct strand incision

No genes for any of the known uracil DNA glycosylases of the UDG superfamily are present in the genome of Methanothermobacter thermautotrophicus DeltaH, making it difficult to imagine how DNA-U repair might be initiated in this organism. Recently, Mth212, the ExoIII homologue of M. thermautotrophicus DeltaH has been characterized as a DNA uridine endonuclease, which suggested the possibility of a novel endonucleolytic entry mechanism for DNA uracil repair. With no system of genetic experimentation available, the problem was approached biochemically. Assays of DNA uracil repair in vitro, promoted by crude cellular extracts, provide unequivocal confirmation that this mechanism does indeed operate in M. thermautotrophicus DeltaH.

Mutations in subdomain B of the minichromosome maintenance (MCM) helicase affect DNA binding and modulate conformational transitions

Minichromosome maintenance (MCM) proteins are believed to provide the replicative helicase activity in eukaryotes and archaea. The single MCM orthologue from Methanothermobacter thermautotrophicus (MthMCM) has been extensively characterized as a model of the eukaryotic heterohexameric MCM complex. MthMCM forms high molecular weight complexes in solution consistent with a dodecamer. Visualization of this complex by electron microscopy suggests that single and double heptameric or hexameric rings can form. We have mutated two arginine residues (Arg-137, Arg-160) in the N-terminal subdomain B of MthMCM based on their apparent potential to form inter-ring hydrogen bonds. Both the single R137A and the double R137A,R160A mutants were characterized by a combination of biophysical, biochemical, and electron microscopy techniques. Biophysical analysis coupled with electron microscopy studies shows that the R137A mutant forms a double heptameric ring, whereas the R137A,R160A protein assembles as a single heptamer. They both show a defect in DNA binding and a concomitant conformational change in subdomain A, with the double mutant displaying significant defects in helicase activity as well. We propose a model in which MCM loading and the subsequent activation of the helicase activity involve a conformational transition that is connected to a DNA binding event.

MTH1745, a protein disulfide isomerase-like protein from thermophilic archaea, Methanothermobacter thermoautotrophicum involving in stress response

MTH1745 is a putative protein disulfide isomerase characterized with 151 amino acid residues and a CPAC active-site from the anaerobic archaea Methanothermobacter thermoautotrophicum. The potential functions of MTH1745 are not clear. In the present study, we show a crucial role of MTH1745 in protecting cells against stress which may be related to its functions as a disulfide isomerase and its chaperone properties. Using real-time polymerase chain reaction analyses, the level of MTH1745 messenger RNA (mRNA) in the thermophilic archaea M. thermoautotrophicum was found to be stress-induced in that it was significantly higher under low (50 degrees C) and high (70 degrees C) growth temperatures than under the optimal growth temperature for the organism (65 degrees C). Additionally, the expression of MTH1745 mRNA was up-regulated by cold shock (4 degrees C). Furthermore, the survival of MTH1745 expressing Escherichia coli cells was markedly higher than that of control cells in response to heat shock (51.0 degrees C). These results indicated that MTH1745 plays an important role in the resistance of stress. By assay of enzyme activities in vitro, MTH1745 also exhibited a chaperone function by promoting the functional folding of citrate synthase after thermodenaturation. On the other hand, MTH1745 was also shown to function as a disulfide isomerase on the refolding of denatured and reduced ribonuclease A. On the basis of its single thioredoxin domain, function as a disulfide isomerase, and its chaperone activity, we suggest that MTH1745 may be an ancient protein disulfide isomerase. These studies may provide clues to the understanding of the function of protein disulfide isomerase in archaea.

A cysteine-rich CCG domain contains a novel [4Fe-4S] cluster binding motif as deduced from studies with subunit B of heterodisulfide reductase from Methanothermobacter marburgensis

Heterodisulfide reductase (HDR) of methanogenic archaea with its active-site [4Fe-4S] cluster catalyzes the reversible reduction of the heterodisulfide (CoM-S-S-CoB) of the methanogenic coenzyme M (CoM-SH) and coenzyme B (CoB-SH). CoM-HDR, a mechanistic-based paramagnetic intermediate generated upon half-reaction of the oxidized enzyme with CoM-SH, is a novel type of [4Fe-4S]3+ cluster with CoM-SH as a ligand. Subunit HdrB of the Methanothermobacter marburgensis HdrABC holoenzyme contains two cysteine-rich sequence motifs (CX31-39CCX35-36CXXC), designated as CCG domain in the Pfam database and conserved in many proteins. Here we present experimental evidence that the C-terminal CCG domain of HdrB binds this unusual [4Fe-4S] cluster. HdrB was produced in Escherichia coli, and an iron-sulfur cluster was subsequently inserted by in vitro reconstitution. In the oxidized state the cluster without the substrate exhibited a rhombic EPR signal (gzyx = 2.015, 1.995, and 1.950) reminiscent of the CoM-HDR signal. 57Fe ENDOR spectroscopy revealed that this paramagnetic species is a [4Fe-4S] cluster with 57Fe hyperfine couplings very similar to that of CoM-HDR. CoM-33SH resulted in a broadening of the EPR signal, and upon addition of CoM-SH the midpoint potential of the cluster was shifted to values observed for CoM-HDR, both indicating binding of CoM-SH to the cluster. Site-directed mutagenesis of all 12 cysteine residues in HdrB identified four cysteines of the C-terminal CCG domain as cluster ligands. Combined with the previous detection of CoM-HDR-like EPR signals in other CCG domain-containing proteins our data indicate a general role of the C-terminal CCG domain in coordination of this novel [4Fe-4S] cluster. In addition, Zn K-edge X-ray absorption spectroscopy identified an isolated Zn site with an S3(O/N)1 geometry in HdrB and the HDR holoenzyme. The N-terminal CCG domain is suggested to provide ligands to the Zn site.

Characterization of alkyl-nickel adducts generated by reaction of methyl-coenzyme m reductase with brominated acids

Methyl-coenzyme M reductase (MCR) from methanogenic archaea catalyzes the final step in the biological synthesis of methane. Using coenzyme B (CoBSH) as the two-electron donor, MCR reduces methyl-coenzyme M (methyl-SCoM) to methane and the mixed disulfide, CoB-S-S-CoM. MCR contains coenzyme F430, an essential redox-active nickel tetrahydrocorphin, at its active site. The active form of MCR (MCRred1) contains Ni(I)-F430. When 3-bromopropane sulfonate (BPS) is incubated with MCRred1, an alkyl-Ni(III) species is formed that elicits the MCRPS EPR signal. Here we used EPR and UV-visible spectroscopy and transient kinetics to study the reaction between MCR from Methanothermobacter marburgensis and a series of brominated carboxylic acids, with carbon chain lengths of 4-16. All of these compounds give rise to an alkyl-Ni intermediate with an EPR signal similar to that of the MCRPS species. Reaction of the alkyl-Ni(III) adduct, formed from brominated acids with eight or fewer total carbons, with HSCoM as nucleophile at pH 10.0 results in the formation of a thioether coupled to regeneration of the active MCRred1 state. When reacted with 4-bromobutyrate, MCRred1 forms the alkyl-Ni(III) MCRXA state and then, surprisingly, undergoes "self-reactivation" to regenerate the Ni(I) MCRred1 state and a bromocarboxy ester. The results demonstrate an unexpected reactivity and flexibility of the MCR active site in accommodating a broad range of substrates, which act as molecular rulers for the substrate channel in MCR.

An aminoacyl-tRNA synthetase:elongation factor complex for substrate channeling in archaeal translation

Translation requires the specific attachment of amino acids to tRNAs by aminoacyl-tRNA synthetases (aaRSs) and the subsequent delivery of aminoacyl-tRNAs to the ribosome by elongation factor 1 alpha (EF-1α). Interactions between EF-1α and various aaRSs have been described in eukaryotes, but the role of these complexes remains unclear. To investigate possible interactions between EF-1α and other cellular components, a yeast two-hybrid screen was performed for the archaeon Methanothermobacter thermautotrophicus. EF-1α was found to form a stable complex with leucyl-tRNA synthetase (LeuRS; K_D = 0.7 μM). Complex formation had little effect on EF-1α activity, but increased the k_cat for Leu-tRNA^Leu synthesis ∼8-fold. In addition, EF-1α co-purified with the archaeal multi-synthetase complex (MSC) comprised of LeuRS, LysRS and ProRS, suggesting the existence of a larger aaRS:EF-1α complex in archaea. These interactions between EF-1α and the archaeal MSC contribute to translational fidelity both by enhancing the aminoacylation efficiencies of the three aaRSs in the complex and by coupling two stages of translation: aminoacylation of cognate tRNAs and their subsequent channeling to the ribosome.

AMP-forming acetyl-CoA synthetases in Archaea show unexpected diversity in substrate utilization

Adenosine monophosphate (AMP)-forming acetyl-CoA synthetase (ACS; acetate:CoA ligase (AMP-forming), EC 6.2.1.1) is a key enzyme for conversion of acetate to acetyl-CoA, an essential intermediate at the junction of anabolic and catabolic pathways. Phylogenetic analysis of putative short and medium chain acyl-CoA synthetase sequences indicates that the ACSs form a distinct clade from other acyl-CoA synthetases. Within this clade, the archaeal ACSs are not monophyletic and fall into three groups composed of both bacterial and archaeal sequences. Kinetic analysis of two archaeal enzymes, an ACS from Methanothermobacter thermautotrophicus (designated as MT-ACS1) and an ACS from Archaeoglobus fulgidus (designated as AF-ACS2), revealed that these enzymes have very different properties. MT-ACS1 has nearly 11-fold higher affinity and 14-fold higher catalytic efficiency with acetate than with propionate, a property shared by most ACSs. However, AF-ACS2 has only 2.3-fold higher affinity and catalytic efficiency with acetate than with propionate. This enzyme has an affinity for propionate that is almost identical to that of MT-ACS1 for acetate and nearly tenfold higher than the affinity of MT-ACS1 for propionate. Furthermore, MT-ACS1 is limited to acetate and propionate as acyl substrates, whereas AF-ACS2 can also utilize longer straight and branched chain acyl substrates. Phylogenetic analysis, sequence alignment and structural modeling suggest a molecular basis for the altered substrate preference and expanded substrate range of AF-ACS2 versus MT-ACS1.

Two sub-states of the red2 state of methyl-coenzyme M reductase revealed by high-field EPR spectroscopy

Methyl-coenzyme M reductase (MCR) catalyzes the formation of methane from methyl-coenzyme M and coenzyme B in methanogenic archaea. The enzyme has two structurally interlinked active sites embedded in an alpha(2)beta(2)gamma(2) subunit structure. Each active site has the nickel porphyrinoid F(430) as a prosthetic group. In the active state, F(430) contains the transition metal in the Ni(I) oxidation state. The active enzyme exhibits an axial Ni(I)-based continuous wave (CW) electron paramagnetic resonance (EPR) signal, called red1a in the absence of substrates or red1c in the presence of coenzyme M. Addition of coenzyme B to the MCR-red1 state can partially and reversibly convert it into the MCR-red2 form, which shows a rhombic Ni(I)-based EPR signal (at X-band microwave frequencies of approximately 9.4 GHz). In this report we present evidence from high-field/high-frequency CW EPR spectroscopy (W-band, microwave frequency of approximately 94 GHz) that the red2 state consists of two substates that could not be resolved by EPR spectroscopy at X-band frequencies. At W-band it becomes apparent that upon addition of coenzyme B to MCR in the red1c state, two red2 EPR signals are induced, not one as was previously believed. The first signal is the well-characterized (ortho)rhombic EPR signal, thus far called red2, while the second previously unidentified signal is axial. We have named the two substates MCR-red2r and MCR-red2a after their rhombic and axial signals, respectively.

Identification of pseudomurein cell wall binding domains

Methanothermobacter thermautotrophicus is a methanogenic Gram-positive microorganism with a cell wall consisting of pseudomurein. Currently, no information is available on extracellular pseudomurein biology and so far only two prophage pseudomurein autolysins, PeiW and PeiP, have been reported. In this paper we show that PeiW and PeiP contain two different N-terminal pseudomurein cell wall binding domains. This finding was used to identify a novel domain, PB007923, on the M. thermautotrophicus genome present in 10 predicted open reading frames. Three homologues were identified in the Methanosphaera stadtmanae genome. Binding studies of fusion constructs of three separate PB007923 domains to green fluorescent protein revealed that it also constituted a cell wall binding domain. Both prophage domains and the PB007923 domain bound to the cell walls of Methanothermobacter species and fluorescence microscopy showed a preference for the septal region. Domain specificities were revealed by binding studies with other pseudomurein-containing archaea. Localized binding was observed for M. stadtmanae and Methanobrevibacter species, while others stained evenly. The identification of the first pseudomurein cell wall binding domains reveals the dynamics of the pseudomurein cell wall and provides marker proteins to study the extracellular pseudomurein biology of M. thermautotrophicus and of other pseudomurein-containing archaea.

Elucidation of substrate specificity in the cobalamin (vitamin B12) biosynthetic methyltransferases. Structure and function of the C20 methyltransferase (CbiL) from Methanothermobacter thermautotrophicus

Ring contraction during cobalamin (vitamin B12) biosynthesis requires a seemingly futile methylation of the C20 position of the tetrapyrrole framework. Along the anaerobic route, this reaction is catalyzed by CbiL, which transfers a methyl group from S-adenosyl-L-methionine to cobalt factor II to generate cobalt factor III. CbiL belongs to the class III methyltransferases and displays similarity to other cobalamin biosynthetic methyltransferases that are responsible for the regiospecific methylation of a number of positions on the tetrapyrrole molecular canvas. In an attempt to understand how CbiL selectively methylates the C20 position, a detailed structure function analysis of the enzyme has been undertaken. In this paper, we demonstrate that the enzyme methylates the C20 position, that its preferred substrate is cobalt factor II, and that the metal ion does not undergo any oxidation change during the course of the reaction. The enzyme was crystallized, and its structure was determined by x-ray crystallography, revealing that the 26-kDa protein has a similar overall topology to other class III enzymes. This helped in the identification of some key amino acid residues (Asp(104), Lys(176), and Tyr(220)). Analysis of mutant variants of these groups has allowed us to suggest potential roles that these side chains may play in substrate binding and catalysis. EPR analysis of binary and ternary complexes indicate that the protein donates a fifth ligand to the cobalt ion via a gated mechanism to prevent transfer of the methyl group to water. The chemical logic underpinning the methylation is discussed.

In vitro biosynthesis of ether-type glycolipids in the methanoarchaeon Methanothermobacter thermautotrophicus

The biosynthesis of archaeal ether-type glycolipids was investigated in vitro using Methanothermobacter thermautotrophicus cell-free homogenates. The sole sugar moiety of glycolipids and phosphoglycolipids of the organism is the beta-D-glucosyl-(1-->6)-D-glucosyl (gentiobiosyl) unit. The enzyme activities of archaeol:UDP-glucose beta-glucosyltransferase (monoglucosylarchaeol [MGA] synthase) and MGA:UDP-glucose beta-1,6-glucosyltransferase (diglucosylarchaeol [DGA] synthase) were found in the methanoarchaeon. The synthesis of DGA is probably a two-step glucosylation: (i) archaeol + UDP-glucose --> MGA + UDP, and (ii) MGA + UDP-glucose --> DGA + UDP. Both enzymes required the addition of K(+) ions and archaetidylinositol for their activities. DGA synthase was stimulated by 10 mM MgCl(2), in contrast to MGA synthase, which did not require Mg(2+). It was likely that the activities of MGA synthesis and DGA synthesis were carried out by different proteins because of the Mg(2+) requirement and their cellular localization. MGA synthase and DGA synthase can be distinguished in cell extracts greatly enriched for each activity by demonstrating the differing Mg(2+) requirements of each enzyme. MGA synthase preferred a lipid substrate with the sn-2,3 stereostructure of the glycerol backbone on which two saturated isoprenoid chains are bound at the sn-2 and sn-3 positions. A lipid substrate with unsaturated isoprenoid chains or sn-1,2-dialkylglycerol configuration exhibited low activity. Tetraether-type caldarchaetidylinositol was also actively glucosylated by the homogenates to form monoglucosyl caldarchaetidylinositol and a small amount of diglucosyl caldarchaetidylinositol. The addition of Mg(2+) increased the formation of diglucosyl caldarchaetidylinositol. This suggested that the same enzyme set synthesized the sole sugar moiety of diether-type glycolipids and tetraether-type phosphoglycolipids.

A novel function for the N-terminal nucleophile hydrolase fold demonstrated by the structure of an archaeal inosine monophosphate cyclohydrolase

Inosine 5'-monophosphate (IMP) cyclohydrolase catalyzes the cyclization of 5-formaminoimidazole-4-carboxamide ribonucleotide (FAICAR) to IMP in the final step of de novo purine biosynthesis. Two major types of this enzyme have been discovered to date: PurH in Bacteria and Eukarya and PurO in Archaea. The structure of the MTH1020 gene product from Methanothermobacter thermoautotrophicus was previously solved without functional annotation but shows high amino acid sequence similarity to other PurOs. We determined the crystal structure of the MTH1020 gene product in complex with either IMP or 5-aminoimidazole-4-carboxamide ribonucleotide (AICAR) at 2.0 and 2.6 A resolution, respectively. On the basis of the sequence analysis, ligand-bound structures, and biochemical data, MTH1020 is confirmed as an archaeal IMP cyclohydrolase, thus designated as MthPurO. MthPurO has a four-layered alphabeta betaalpha core structure, showing an N-terminal nucleophile (NTN) hydrolase fold. The active site is located at the deep pocket between two central beta-sheets and contains residues strictly conserved within PurOs. Comparisons of the two types of IMP cyclohydrolase, PurO and PurH, revealed that there are no similarities in sequence, structure, or the active site architecture, suggesting that they are evolutionarily not related to each other. The MjR31K mutant of PurO from Methanocaldococcus jannaschii showed 76% decreased activity and the MjE102Q mutation completely abolished enzymatic activity, suggesting that these highly conserved residues play critical roles in catalysis. Interestingly, green fluorescent protein (GFP), which has no structural homology to either PurO or PurH but catalyzes a similar intramolecular cyclohydrolase reaction required for chromophore maturation, utilizes Arg96 and Glu222 in a mechanism analogous to that of PurO.

Farnesyl diphosphate synthase: the art of compromise between substrate selectivity and stereoselectivity

Farnesyl diphosphate (FPP) synthase catalyzes the consecutive head-to-tail condensations of isopentenyl diphosphate (IPP, C5) with dimethylallyl diphosphate (DMAPP, C5) and geranyl diphosphate (GPP, C10) to give (E,E)-FPP (C15). The enzyme belongs to a genetically distinct family of chain elongation enzymes that install E-double bonds during each addition of a five-carbon isoprene unit. Analysis of the C10 and C15 products from incubations with avian FPP synthase reveals that small amounts of neryl diphosphate (Z-C10) and (Z,E)-FPP are formed along with the E-isomers during the C5 --> C10 and C10 --> C15 reactions. Similar results were obtained for FPP synthase from Escherichia coli, Artemisia tridentata (sage brush), Pyrococcus furiosus, and Methanobacter thermautotrophicus and for GPP and FPP synthesized in vivo by E. coli FPP synthase. When (R)-[2-2H]IPP was a substrate for chain elongation, no deuterium was found in the chain elongation products. In contrast, the deuterium in (S)-[2-2H]IPP was incorporated into all of the products. Thus, the pro-R hydrogen at C2 of IPP is lost when the E- and Z-double bond isomers are formed. The synthesis of Z-double bond isomers by FPP synthase during chain elongation is unexpected for a highly evolved enzyme and probably reflects a compromise between optimizing double bond stereoselectivity and the need to exclude DMAPP from the IPP binding site.

Characterization of theanine-forming enzyme from Methylovorus mays no. 9 in respect to utilization of theanine production

For development of theanine production from glutamic acid and ethylamine by coupling yeast sugar fermentation as an ATP-regenerating system, several strains were selected from among about 200 methylamine- and/or methanol-assimilating bacteria depending on the theanine-forming activity of their permeated cells. The amount of theanine formed by the cells of the selected strains was much larger than that by the cells of Escherichia coli AD494 (DE3) expressing Pseudomonas taetrolens Y-30 glutamine synthetase (GS), which has been found to be a usable enzyme for theanine production. A GS-like enzyme responsible for the theanine-forming reaction was obtained from an obligate methylotroph isolate, Methylovorus mays No. 9. The enzyme was induced by methylamine in the culture medium. A molecular mass of 410-470 kDa was obtained by gel filtration of the enzyme, and 51 kDa by SDS-PAGE analysis. The enzyme showed high activity toward methylamine rather than ammonia, which indicates that it is similar to known gamma-glutamylmethylamide synthetase. The isolated enzyme also had high reactivity to ethylamine in a neutral pH range, and formed theanine from glutamic acid and ethylamine in a reaction mixture containing a yeast sugar fermentation system for ATP-regeneration.

Co-evolution of the archaeal tRNA-dependent amidotransferase GatCAB with tRNA(Asn)

The important identity elements in tRNA(Gln) and tRNA(Asn) for bacterial GatCAB and in tRNA(Gln) for archaeal GatDE are the D-loop and the first base pair of the acceptor stem. Here we show that Methanothermobacter thermautotrophicus GatCAB, the archaeal enzyme, is different as it discriminates Asp-tRNA(Asp) and Asp-tRNA(Asn) by use of U49, the D-loop and to a lesser extent the variable loop. Since archaea possess the tRNA(Gln)-specific amidotransferase GatDE, the archaeal GatCAB enzyme evolved to recognize different elements in tRNA(Asn) than those recognized by GatDE or by the bacterial GatCAB enzyme in their tRNA substrates.

Functional association between three archaeal aminoacyl-tRNA synthetases

Aminoacyl-tRNA synthetases (aaRSs) are responsible for attaching amino acids to their cognate tRNAs during protein synthesis. In eukaryotes aaRSs are commonly found in multi-enzyme complexes, although the role of these complexes is still not completely clear. Associations between aaRSs have also been reported in archaea, including a complex between prolyl-(ProRS) and leucyl-tRNA synthetases (LeuRS) in Methanothermobacter thermautotrophicus that enhances tRNA(Pro) aminoacylation. Yeast two-hybrid screens suggested that lysyl-tRNA synthetase (LysRS) also associates with LeuRS in M. thermautotrophicus. Co-purification experiments confirmed that LeuRS, LysRS, and ProRS associate in cell-free extracts. LeuRS bound LysRS and ProRS with a comparable K(D) of about 0.3-0.9 microm, further supporting the formation of a stable multi-synthetase complex. The steady-state kinetics of aminoacylation by LysRS indicated that LeuRS specifically reduced the Km for tRNA(Lys) over 3-fold, with no additional change seen upon the addition of ProRS. No significant changes in aminoacylation by LeuRS or ProRS were observed upon the addition of LysRS. These findings, together with earlier data, indicate the existence of a functional complex of three aminoacyl-tRNA synthetases in archaea in which LeuRS improves the catalytic efficiency of tRNA aminoacylation by both LysRS and ProRS.

Archaeal minichromosome maintenance (MCM) helicase can unwind DNA bound by archaeal histones and transcription factors

Protein-DNA complexes must be disassembled to facilitate DNA replication. Replication forks contain a helicase that unwinds the duplex DNA at the front of the fork. The minichromosome maintenance helicase from the archaeon Methanothermobacter thermautotrophicus required only ATP to unwind DNA bound into complexes by the M. thermautotrophicus archaeal histone HMtA2, transcription repressor TrpY, or into a transcription pre-initiation complex by M. thermautotrophicus TATA-box-binding protein, transcription factor B, and RNA polymerase. In contrast, the minichromosome maintenance helicase was unable to unwind DNA bound by this archaeal RNA polymerase in a stalled transcript-elongating complex.

Crystallization and preliminary X-ray characterization of two thermostable DNA nucleases

Temperature-tolerant organisms are an important source to enhance the stability of enzymes used in biotechnological processes. The DNA-cleaving enzyme exonuclease III from Escherichia coli is used in several applications in gene technology. A thermostable variant could expand the applicability of the enzyme in these methods. Two homologous nucleases from Archaeoglobus fulgidus (ExoAf) and Methanothermobacter thermoautrophicus (ExoMt) were studied for this purpose. Both enzymes were crystallized in different space groups using (poly)ethylene glycols, 2,4-methyl pentandiol, dioxane, ethanol or 2-propanol as precipitants. The addition of a 10-mer DNA oligonucleotide was important to obtain monoclinic crystals of ExoAf and ExoMt that diffracted to resolutions better than 2 A using synchrotron radiation. The crystal structures of the homologous proteins can serve as templates for genetic engineering of the E. coli exonuclease III and will aid in understanding the different catalytic properties of the enzymes.

Characterization of the acyl substrate binding pocket of acetyl-CoA synthetase

AMP-forming acetyl-CoA synthetase [ACS; acetate:CoA ligase (AMP-forming), EC 6.2.1.1] catalyzes the activation of acetate to acetyl-CoA in a two-step reaction. This enzyme is a member of the adenylate-forming enzyme superfamily that includes firefly luciferase, nonribosomal peptide synthetases, and acyl- and aryl-CoA synthetases/ligases. Although the structures of several superfamily members demonstrate that these enzymes have a similar fold and domain structure, the low sequence conservation and diversity of the substrates utilized have limited the utility of these structures in understanding substrate binding in more distantly related enzymes in this superfamily. The crystal structures of the Salmonella enterica ACS and Saccharomyces cerevisiae ACS1 have allowed a directed approach to investigating substrate binding and catalysis in ACS. In the S. enterica ACS structure, the propyl group of adenosine 5'-propylphosphate, which mimics the acyl-adenylate intermediate, lies in a hydrophobic pocket. Modeling of the Methanothermobacter thermautotrophicus Z245 ACS (MT-ACS1) on the S. cerevisiae ACS structure showed similar active site architecture, and alignment of the amino acid sequences of proven ACSs indicates that the four residues that compose the putative acetate binding pocket are well conserved. These four residues, Ile312, Thr313, Val388, and Trp416 of MT-ACS1, were targeted for alteration, and our results support that they do indeed form the acetate binding pocket and that alterations at these positions significantly alter the enzyme's affinity for acetate as well as the range of acyl substrates that can be utilized. In particular, Trp416 appears to be the primary determinant for acyl chain length that can be accommodated in the binding site.

Structural basis of the Methanothermobacter thermautotrophicus MCM helicase activity

The MCM complex from the archaeon Methanother-mobacter thermautotrophicus is a model for the eukaryotic MCM2-7 helicase. We present electron-microscopy single-particle reconstructions of a DNA treated M.thermautotrophicus MCM sample and a ADP.AlF(x) treated sample, respectively assembling as double hexamers and double heptamers. The electron-density maps display an unexpected asymmetry between the two rings, suggesting that large conformational changes can occur within the complex. The structure of the MCM N-terminal domain, as well as the AAA+ and the C-terminal HTH dom-ains of ZraR can be fitted into the reconstructions. Distinct configurations can be modelled for the AAA+ and the HTH domains, suggesting the nature of the conformational change within the complex. The pre-sensor 1 and the helix 2 insertions, important for the activity, can be located pointing towards the centre of the channel in the presence of DNA. We propose a mechanistic model for the helicase activity, based on a ligand-controlled rotation of the AAA+ subunits.

Spectroscopic and computational studies of reduction of the metal versus the tetrapyrrole ring of coenzyme F430 from methyl-coenzyme M reductase

Methyl-coenzyme M reductase (MCR) catalyzes the final step in methane biosynthesis by methanogenic archaea and contains a redox-active nickel tetrahydrocorphin, coenzyme F430, at its active site. Spectroscopic and computational methods have been used to study a novel form of the coenzyme, called F330, which is obtained by reducing F430 with sodium borohydride (NaBH4). F330 exhibits a prominent absorption peak at 330 nm, which is blue shifted by 100 nm relative to F430. Mass spectrometric studies demonstrate that the tetrapyrrole ring in F330 has undergone reduction, on the basis of the incorporation of protium (or deuterium), upon treatment of F430 with NaBH4 (or NaBD4). One- and two-dimensional NMR studies show that the site of reduction is the exocyclic ketone group of the tetrahydrocorphin. Resonance Raman studies indicate that elimination of this pi-bond increases the overall pi-bond order in the conjugative framework. X-ray absorption, magnetic circular dichroism, and computational results show that F330 contains low-spin Ni(II). Thus, conversion of F430 to F330 reduces the hydrocorphin ring but not the metal. Conversely, reduction of F430 with Ti(III) citrate to generate F380 (corresponding to the active MCR(red1) state) reduces the Ni(II) to Ni(I) but does not reduce the tetrapyrrole ring system, which is consistent with other studies [Piskorski, R., and Jaun, B. (2003) J. Am. Chem. Soc. 125, 13120-13125; Craft, J. L., et al. (2004) J. Biol. Inorg. Chem. 9, 77-89]. The distinct origins of the absorption band shifts associated with the formation of F330 and F380 are discussed within the framework of our computational results. These studies on the nature of the product(s) of reduction of F430 are of interest in the context of the mechanism of methane formation by MCR and in relation to the chemistry of hydroporphinoid systems in general. The spectroscopic and time-dependent DFT calculations add important insight into the electronic structure of the nickel hydrocorphinate in its Ni(II) and Ni(I) valence states.

The Methanothermobacter thermautotrophicus ExoIII homologue Mth212 is a DNA uridine endonuclease

The genome of Methanothermobacter thermautotrophicus, as a hitherto unique case, is apparently devoid of genes coding for general uracil DNA glycosylases, the universal mediators of base excision repair following hydrolytic deamination of DNA cytosine residues. We have now identified protein Mth212, a member of the ExoIII family of nucleases, as a possible initiator of DNA uracil repair in this organism. This enzyme, in addition to bearing all the enzymological hallmarks of an ExoIII homologue, is a DNA uridine endonuclease (U-endo) that nicks double-stranded DNA at the 5'-side of a 2'-d-uridine residue, irrespective of the nature of the opposing nucleotide. This type of activity has not been described before; it is absent from the ExoIII homologues of Escherichia coli, Homo sapiens and Methanosarcina mazei, all of which are equipped with uracil DNA repair glycosylases. The U-endo activity of Mth212 is served by the same catalytic center as its AP-endo activity.

The iron-sulfur cluster-free hydrogenase (Hmd) is a metalloenzyme with a novel iron binding motif

The iron-sulfur cluster-free hydrogenase (Hmd) from methanogenic archaea harbors an iron-containing cofactor of yet unknown structure. X-ray absorption spectroscopy of the active, as isolated enzyme from Methanothermobacter marburgensis (mHmd) and of the active, reconstituted enzyme from Methanocaldococcus jannaschii (jHmd) revealed the presence of mononuclear iron with two CO, one sulfur and one or two N/O in coordination distance. In jHmd, the single sulfur ligand is most probably provided by Cys176, as deduced from a comparison of the activity and of the x-ray absorption and Mössbauer spectra of the enzyme mutated in any of the three conserved cysteines. In the isolated Hmd cofactor, two CO, one sulfur, and two nitrogen/oxygen atoms coordinate the iron, the sulfur ligand being most probably provided by mercaptoethanol, which is absolutely required for the extraction of the iron-containing cofactor from the holoenzyme and for the stabilization of the extracted cofactor. In active mHmd holoenzyme, the number of iron ligands increased by one when one of the Hmd inhibitors (CO or KCN) were present, indicating that in active Hmd, the iron contains an open coordination site, which is proposed to be the site of H2 interaction.

Structural basis of RNA-dependent recruitment of glutamine to the genetic code

Glutaminyl-transfer RNA (Gln-tRNA(Gln)) in archaea is synthesized in a pretranslational amidation of misacylated Glu-tRNA(Gln) by the heterodimeric Glu-tRNA(Gln) amidotransferase GatDE. Here we report the crystal structure of the Methanothermobacter thermautotrophicus GatDE complexed to tRNA(Gln) at 3.15 angstroms resolution. Biochemical analysis of GatDE and of tRNA(Gln) mutants characterized the catalytic centers for the enzyme's three reactions (glutaminase, kinase, and amidotransferase activity). A 40 angstrom-long channel for ammonia transport connects the active sites in GatD and GatE. tRNA(Gln) recognition by indirect readout based on shape complementarity of the D loop suggests an early anticodon-independent RNA-based mechanism for adding glutamine to the genetic code.

DNA binding by the Methanothermobacter thermautotrophicus Cdc6 protein is inhibited by the minichromosome maintenance helicase

The Cdc6 proteins from the archaeon Methanothermobacter thermautotrophicus were previously shown to bind double-stranded DNA. It is shown here that the proteins also bind single-stranded DNA. Using minichromosome maintenance (MCM) helicase mutant proteins unable to bind DNA, it was found that the interaction of MCM with Cdc6 inhibits the DNA binding activity of Cdc6.

Minichromosome maintenance helicase activity is controlled by N- and C-terminal motifs and requires the ATPase domain helix-2 insert

The minichromosome maintenance (MCM) proteins are essential conserved proteins required for DNA replication in archaea and eukaryotes. MCM proteins are believed to provide the replicative helicase activity that unwinds template DNA ahead of the replication fork. Consistent with this hypothesis, MCM proteins can form hexameric complexes that possess ATP-dependent DNA unwinding activity. The molecular mechanism by which the energy of ATP hydrolysis is harnessed to DNA unwinding is unknown, although the ATPase activity has been attributed to a highly conserved AAA+ family ATPase domain. Here we show that changes to N- and C-terminal motifs in the single MCM protein from the archaeon Methanothermobacter thermautotrophicus (MthMCM) can modulate ATP hydrolysis, DNA binding, and duplex unwinding. Furthermore, these motifs appear to influence the movement of the beta-alpha-beta insert in helix-2 of the MCM ATPase domain. Removal of this motif from MthMCM increased dsDNA-stimulated ATP hydrolysis and increased the affinity of the mutant complex for ssDNA and dsDNA. Deletion of the helix-2 insert additionally resulted in the abrogation of DNA unwinding. Our results provide significant insight into the molecular mechanisms used by the MCM helicase to both regulate and execute DNA unwinding.

Structural studies of the archaeal MCM complex in different functional states

The primary candidate for the eukaryotic replicative helicase is the MCM2-7 complex, a hetero-oligomer formed by six AAA+ paralogous polypeptides. A simplified model for structure-function studies is the homo-oligomeric orthologue from the archaeon Methanothermobacter thermoautotrophicus. The crystal structure of the DNA-interacting N-terminal domain of this homo-oligomer revealed a double hexamer in a head-to-head configuration; single-particle electron microscopy studies have shown that the full-length protein complex can form both single and double rings, in which each ring can consist of a cyclical arrangement of six or seven subunits. Using single-particle techniques and especially multivariate statistical symmetry analysis, we have assessed the changes in stoichiometry that the complex undergoes when treated with various nucleotide analogues or when binding a double-stranded DNA fragment. We found that the binding of nucleotides or of double-stranded DNA leads to the preferred formation of double-ring structures. Specifically, the protein complex is present as a double heptamer when treated with a nucleotide analogue, but it is rather found as a double hexamer when complexed with double-stranded DNA. The possible physiological role of the various stoichiometries of the complex is discussed in the light of the proposed mechanisms of helicase activity.

The thermal adaptation of the nitrogenase Fe protein from thermophilic Methanobacter thermoautotrophicus

The nitrogenase Fe protein is a key component of the biochemical machinery responsible for the process of biological nitrogen fixation. The Fe protein is a member of a class of nucleotide-binding proteins that couple the binding and hydrolysis of nucleoside triphosphates to conformational changes. The nucleotide-dependent conformational changes modulate the formation of a macromolecular complex, and some members of the class include Galpha, EF-Tu, and myosin. The members of this class are highly interesting model systems for the analysis of aspects of thermal adaptability, since their mechanisms involve protein conformational change and protein-protein interactions. In this study, we have used our extensive knowledge of the structure of the Azotobacter vinelandii nitrogenase Fe protein in multiple structural conformations, and standard homology modeling approaches have been used to generate reliable models of the Fe protein from thermophilic Methanobacter thermoautotrophicus in the analogous structural conformations. The resulting structural comparison reveals that thermal adaptation of the M. thermoautotrophicus Fe protein is conferred by a number of factors, including increased structural rigidity that results from various structural changes within the protein interior. The analysis of hypothetical docking models and nitrogenase complex structures provides insights into the thermal adaptation of the protein-protein interactions that support macromolecular complex formation and catalysis at higher temperatures.

Heterodisulfide reductase from methanogenic archaea: a new catalytic role for an iron-sulfur cluster

Heterodisulfide reductase (HDR) from methanogenic archaea is an iron-sulfur protein that catalyzes reversible reduction of the heterodisulfide (CoM-S-S-CoB) of the methanogenic thiol-coenzymes, coenzyme M (CoM-SH) and coenzyme B (CoB-SH). Via the characterization of a paramagnetic reaction intermediate generated upon oxidation of the enzyme in the presence of coenzyme M, the enzyme was shown to contain a [4Fe-4S] cluster in its active site that catalyzes reduction of the disulfide substrate in two one-electron reduction steps. The formal thiyl radical generated by the initial one-electron reduction of the disulfide is stabilized via reduction and coordination of the resultant thiol to the [4Fe-4S] cluster.

Spin Density and Coenzyme M Coordination Geometry of the ox1 Form of Methyl-Coenzyme M Reductase: A Pulse EPR Study

Methyl-coenzyme M reductase (MCR) catalyses the reduction of methyl-coenzyme M (CH3-S-CoM) with coenzyme B (H-S-CoB) to CH4 and CoM-S-S-CoB in methanogenic archaea. Here we present a pulse EPR study of the "ready" form MCR(ox1), providing a detailed description of the spin density and the coordination of coenzyme M (CoM) to the Ni cofactor F430. To achieve this, MCR was purified from cells grown in a 61Ni enriched medium and samples were prepared in D2O with the substrate analogue CoM either deuterated in the beta-position or with 33S in the thiol group. To obtain the magnetic parameters ENDOR and HYSCORE measurements were done at X- and Q-band, and CW EPR, at X- and W-band. The hyperfine couplings of the beta-protons of CoM indicate that the nickel to beta-proton distances in MCR(ox1) are very similar to those in Ni(II)-MCR(ox1-silent), and thus the position of CoM relative to F430 is very similar in both species. Our thiolate sulfur and nickel EPR data prove a Ni-S coordination, with an unpaired spin density on the sulfur of 7 +/- 3%. These results highlight the redox-active or noninnocent nature of the sulfur ligand on the oxidation state. Assuming that MCR(ox1) is oxidized relative to the Ni(II) species, the complex is formally best described as a Ni(III) (d7) thiolate in resonance with a thiyl radical/high-spin Ni(II) complex, Ni(III)-(-)SR <--> Ni(II)-*SR.

Archaeal RNA polymerase is sensitive to intrinsic termination directed by transcribed and remote sequences

Archaea are prokaryotes with a single DNA-dependent RNA polymerase (RNAP) that is homologous to, and likely resembles the ancestor of all three eukaryotic RNAPs. In vitro studies have confirmed that initiation by archaeal RNAPs resembles the Pol II system, and we report the first detailed in vitro investigation of archaeal transcription termination. Methanothermobacter thermautotrophicus (M.t.) RNAP is susceptible to intrinsic termination at an intergenic sequence that conforms to a bacterial intrinsic terminator, as well as at bona fide bacterial intrinsic terminators. In contrast to bacterial RNAPs, M.t. RNAP also terminated in response to synthetic and natural oligo-T-rich sequences that were not preceded by sequences with any recognizable potential to form a stable RNA hairpin. Both template topology and temperature influenced the position and extent of termination in vitro, and the results argue that transcription of an upstream sequence can alter the termination response of the archaeal RNAP at a remote downstream sequence.

Interactions between the archaeal Cdc6 and MCM proteins modulate their biochemical properties

The origin recognition complex, Cdc6 and the minichromosome maintenance (MCM) complex play essential roles in the initiation of eukaryotic DNA replication. Homologs of these proteins may play similar roles in archaeal replication initiation. While the interactions among the eukaryotic initiation proteins are well documented, the protein-protein interactions between the archaeal proteins have not yet been determined. Here, an extensive structural and functional analysis of the interactions between the Methanothermobacter thermautotrophicus MCM and the two Cdc6 proteins (Cdc6-1 and -2) identified in the organism is described. The main contact between Cdc6 and MCM occurs via the N-terminal portion of the MCM protein. It was found that Cdc6-MCM interaction, but not Cdc6-DNA binding, plays the predominant role in regulating MCM helicase activity. In addition, the data showed that the interactions with MCM modulate the autophosphorylation of Cdc6-1 and -2. The results also suggest that MCM and DNA may compete for Cdc6-1 protein binding. The implications of these observations for the initiation of archaeal DNA replication are discussed.

Interactions between RNase P protein subunits in archaea

A yeast two-hybrid system was used to identify protein-protein interactions between the ribonuclease P (RNase P) protein subunits Mth11p, Mth687p, Mth688p and Mth1618p from the archaeon Methanothermobacter thermoautotrophicus. Clear interactions between Mth688p and Mth687p, and between Mth1618p and Mth11p, were confirmed by HIS3 and LacZ reporter expression. Weaker interactions of Mth687p and Mth688p with Mth 11p, and Mth11p with itself, are also suggested. These interactions resemble, and confirm, those previously seen among the homologs of these proteins in the more complex yeast RNase P holoenzyme.

Mössbauer Studies of the Iron−Sulfur Cluster-Free Hydrogenase: The Electronic State of the Mononuclear Fe Active Site

The iron-sulfur cluster-free hydrogenase (Hmd) from methanogenic archaea harbors an iron-containing, light-sensitive cofactor of still unknown structure as prosthetic group. The enzyme is reversibly inhibited by CO and cyanide and is EPR silent. We report here on Mössbauer spectra of the (57)Fe-labeled enzyme and of the isolated cofactor. The spectrum of the holoenzyme measured at 80 K revealed a doublet peak with an isomer shift delta = 0.06 mm.s(-)(1) and a quadrupole splitting of DeltaE(Q) = 0.65 mm.s(-)(1) (at pH 8.0). The signal intensity corresponded to the enzyme concentration assuming 1 Fe per mol active site. Upon addition of CO or cyanide to the enzyme, the isomer shift decreased to -0.03 mm.s(-)(1) and -0.00(1) mm.s(-)(1), and the quadrupole splitting increased to 1.38 mm.s(-)(1) and 1.75 mm.s(-)(1), respectively. The three spectra could be perfectly simulated assuming the presence of only one type of iron in Hmd. The low isomer shift is characteristic for Fe in a low oxidation state (0, +1, +2). When the spectra of the holoenzyme and of the CO- or cyanide-inhibited enzyme were measured at 4 K in a magnetic field of 4 and 7 T, the spectra obtained could be simulated assuming the presence of only the external magnetic field, which excludes that the iron in the active site of Hmd is Fe(I), high-spin Fe(0), or high-spin Fe(II). Mössbauer spectra of the isolated Hmd cofactor are also reported.

Crystal structure of Mil (Mth680): internal duplication and similarity between the Imp4/Brix domain and the anticodon-binding domain of class IIa aminoacyl-tRNA synthetases

Proteins of the Imp4/Brix superfamily are involved in ribosomal RNA processing, an essential function in all cells. We report the first structure of an Imp4/Brix superfamily protein, the Mil (for Methanothermobacter thermautotrophicus Imp4-like) protein (gene product Mth680), from the archaeon M. thermautotrophicus. The amino- and carboxy-terminal halves of Mil show significant structural similarity to one another, suggesting an origin by means of an ancestral duplication. Both halves show the same fold as the anticodon-binding domain of class IIa aminoacyl-tRNA synthetases, with greater conservation seen in the N-terminal half. This structural similarity, together with the charge distribution in Mil, suggests that Imp4/Brix superfamily proteins could bind single-stranded segments of RNA along a concave surface formed by the N-terminal half of their beta-sheet and a central alpha-helix. The crystal structure of Mil is incompatible with the presence, in the Imp4/Brix domain, of a helix-turn-helix motif that was proposed to comprise the RNA-binding moiety of the Imp4/Brix proteins.

Biosynthesis of vitamin B2: diastereomeric reaction intermediates of archaeal and non-archaeal riboflavin synthases

The dismutation of 6,7-dimethyl-8-ribityllumazine catalyzed by riboflavin synthase affords riboflavin and 5-amino-6-ribitylamino-2,4(1H,3H)-pyrimidinedione. A pentacyclic adduct of two 6,7-dimethyl-8-ribityllumazines has been identified earlier as a catalytically competent reaction intermediate of the Escherichia coli enzyme. Acid quenching of reaction mixtures of riboflavin synthase of Methanococcus jannaschii, a paralog of 6,7-dimethyl-8-ribityllumazine synthase devoid of similarity with riboflavin synthases of eubacteria and eukaryotes, afforded a compound whose optical absorption and NMR spectra resemble that of the pentacyclic E. coli riboflavin synthase intermediate, whereas the circular dichroism spectra of the two compounds have similar envelopes but opposite signs. Each of the compounds could serve as a catalytically competent intermediate for the enzyme by which it was produced, but not vice versa. All available data indicate that the respective pentacyclic intermediates of the M. jannaschii and E. coli enzymes are diastereomers.

Temperature dependence of methyl-coenzyme M reductase activity and of the formation of the methyl-coenzyme M reductase red2 state induced by coenzyme B

Methyl-coenzyme M reductase (MCR) catalyses the formation of methane from methyl-coenzyme M (CH(3)-S-CoM) and coenzyme B (HS-CoB) in methanogenic archaea. The enzyme has an alpha(2)beta(2)gamma(2) subunit structure forming two structurally interlinked active sites each with a molecule F(430) as a prosthetic group. The nickel porphinoid must be in the Ni(I) oxidation state for the enzyme to be active. The active enzyme exhibits an axial Ni(I)-based electron paramagnetic resonance (EPR) signal and a UV-vis spectrum with an absorption maximum at 385 nm. This state is called the MCR-red1 state. In the presence of coenzyme M (HS-CoM) and coenzyme B the MCR-red1 state is in part converted reversibly into the MCR-red2 state, which shows a rhombic Ni(I)-based EPR signal and a UV-vis spectrum with an absorption maximum at 420 nm. We report here for MCR from Methanothermobacter marburgensis that the MCR-red2 state is also induced by several coenzyme B analogues and that the degree of induction by coenzyme B is temperature-dependent. When the temperature was lowered below 20 degrees C the percentage of MCR in the red2 state decreased and that in the red1 state increased. These changes with temperature were fully reversible. It was found that at most 50% of the enzyme was converted to the MCR-red2 state under all experimental conditions. These findings indicate that in the presence of both coenzyme M and coenzyme B only one of the two active sites of MCR can be in the red2 state (half-of-the-sites reactivity). On the basis of this interpretation a two-stroke engine mechanism for MCR is proposed.

Use of a restriction enzyme-digested PCR product as substrate for helicase assays

DNA helicases play essential roles in many cellular processes. The currently available techniques to generate substrates for helicase assays are fairly complicated and need some expertise not available in all laboratories. Here, a PCR-based method to generate a substrate for a helicase assay is described, and its application for several archaeal, bacterial and viral enzymes is demonstrated.

A recombinant exonuclease III homologue of the thermophilic archaeon Methanothermobacter thermautotrophicus

AP endonucleases catalyse an important step in the base excision repair (BER) pathway by incising the phosphodiester backbone of damaged DNA immediately 5' to an abasic site. Here, we report the cloning and expression of the 774 bp Mth0212 gene from the thermophilic archaeon Methanothermobacter thermautotrophicus, which codes for a putative AP endonuclease. The 30.3 kDa protein shares 30% sequence identity with exonuclease III (ExoIII) of Escherichia coli and 40% sequence identity with the human AP endonuclease Ape1. The gene was amplified from a culture sample and cloned into an expression vector. Using an E. coli host, the thermophilic protein could be produced and purified. Characterization of the enzymatic activity revealed strong binding and Mg2+-dependent nicking activity on undamaged double-stranded (ds) DNA at low ionic strength, even at temperatures below the optimum growth temperature of M. thermautotrophicus (65 degrees C). Additionally, a much faster nicking activity on AP site containing DNA was demonstrated. Unspecific incision of undamaged ds DNA was nearly inhibited at KCl concentration of approximately 0.5 M, whereas incision at AP sites was still complete at such salt concentrations. Nicked DNA was further degraded at temperatures above 50 degrees C, probably by an exonucleolytic activity of the enzyme, which was also found on recessed 3' ends of linearized ds DNA. The enzyme was active at temperatures up to 70 degrees C and, using circular dichroism spectroscopy, shown to denature at temperatures approaching 80 degrees C. Considering the high intracellular potassium ion concentration in M. thermautotrophicus, our results suggest that the characterized thermophilic enzyme acts as an AP endonuclease in vivo with similar activities as Ape1.

Gln-tRNAGln formation from Glu-tRNAGln requires cooperation of an asparaginase and a Glu-tRNAGln kinase

Gln-tRNA(Gln) is synthesized from Glu-tRNA(Gln) in most microorganisms by a tRNA-dependent amidotransferase in a reaction requiring ATP and an amide donor such as glutamine. GatDE is a heterodimeric amidotransferase that is ubiquitous in Archaea. GatD resembles bacterial asparaginases and is expected to function in amide donor hydrolysis. We show here that Methanothermobacter thermautotrophicus GatD acts as a glutaminase but only in the presence of both Glu-tRNA(Gln) and the other subunit, GatE. The fact that only Glu-tRNA(Gln) but not tRNA(Gln) could activate the glutaminase activity of GatD suggests that glutamine hydrolysis is coupled tightly to transamidation. M. thermautotrophicus GatDE enzymes that were mutated in GatD at each of the four critical asparaginase-active site residues lost the ability to hydrolyze glutamine and were unable to convert Glu-tRNA(Gln) to Gln-tRNA(Gln) when glutamine was the amide donor. However, ammonium chloride rescued the activities of these mutants, suggesting that the integrity of the ATPase and the transferase activities in the mutant GatDE enzymes was maintained. In addition, pyroglutamyl-tRNA(Gln) accumulated during the reaction catalyzed by the glutaminase-deficient mutants or by GatE alone. The pyroglutamyl-tRNA is most likely a cyclized by-product derived from gamma-phosphoryl-Glu-tRNA(Gln), the proposed high energy intermediate in Glu-tRNA(Gln) transamidation. That GatE alone could form the intermediate indicates that GatE is a Glu-tRNA(Gln) kinase. The activation of Glu-tRNA(Gln) via gamma-phosphorylation bears a similarity to the mechanism used by glutamine synthetase, which may point to an ancient link between glutamine synthesized for metabolism and translation.

A novel nuclease-ATPase (Nar71) from archaea is part of a proposed thermophilic DNA repair system

We have identified a novel structure-specific nuclease in highly fractionated extracts of the thermophilic archaeon Methanothermobacter thermautotrophicus (Mth). The 71 kDa protein product of open reading frame mth1090 is a nuclease with ATPase activity, which we call Nar71 (Nuclease-ATPase in Repair, 71 kDa). The nar71 gene is located in a gene neighbourhood proposed by genomics to encode a novel DNA repair system conserved in thermophiles. The biochemical characterization of Nar71 presented here is the first analysis from within this neighbourhood, and it supports the insight from genomics. Nuclease activity of Nar71 is specific for 3' flaps and flayed duplexes, targeting single-stranded DNA (ssDNA) regions. This activity requires Mg2+ or Mn2+ and is greatly reduced in ATP. In ATP, Nar71 displaces ssDNA, also with high specificity for 3' flap and flayed duplex DNA. Strand displacement is weak compared with nuclease activity, but in ATPS it is abolished, suggesting that Nar71 couples ATP hydrolysis to DNA strand separation. ATPase assays confirmed that Nar71 is stimulated by ssDNA, though not double-stranded DNA. Mutation of Lys-117 in Nar71 abolished ATPase and nuclease activity, and we describe a separation-of-function mutant (K68A) that has lost ATPase activity but retains nuclease activity. A model of possible Nar71 function in DNA repair is presented.

Carbon Monoxide as an Intrinsic Ligand to Iron in the Active Site of the Iron−Sulfur-Cluster-Free Hydrogenase H2-Forming Methylenetetrahydromethanopterin Dehydrogenase As Revealed by Infrared Spectroscopy

The iron-sulfur-cluster-free hydrogenase Hmd (H(2)-forming methylenetetrahydromethanopterin dehydrogenase) from methanogenic archaea has recently been found to contain one iron associated tightly with an extractable cofactor of yet unknown structure. We report here that Hmd contains intrinsic CO bound to the Fe. Chemical analysis of Hmd revealed the presence of 2.4 +/- 0.2 mol of CO/mol of iron. Fourier transform infrared spectra of the native enzyme showed two bands of almost equal intensity at 2011 and 1944 cm(-)(1), interpreted as the stretching frequencies of two CO molecules bound to the same iron in an angle of 90 degrees . We also report on the effect of extrinsic (12)CO, (13)CO, (12)CN(-), and (13)CN(-) on the IR spectrum of Hmd.

Transcription by Methanothermobacter thermautotrophicus RNA polymerase in vitro releases archaeal transcription factor B but not TATA-box binding protein from the template DNA

Transcription initiation in Archaea requires the assembly of a preinitiation complex containing the TATA- box binding protein (TBP), transcription factor B (TFB), and RNA polymerase (RNAP). The results reported establish the fate of Methanothermobacter thermautotrophicus TBP and TFB following transcription initiation by M. thermautotrophicus RNAP in vitro. TFB is released after initiation, during extension of the transcript from 4 to 24 nucleotides, but TBP remains bound to the template DNA. Regulation of archaeal transcription initiation by a repressor competition with TBP for TATA-box region binding must accommodate this observation.

F420H2 oxidase (FprA) from Methanobrevibacter arboriphilus, a coenzyme F420-dependent enzyme involved in O2 detoxification

Cell suspensions of Methanobrevibacter arboriphilus catalyzed the reduction of O(2) with H(2) at a maximal specific rate of 0.4 U (micromol/min) per mg protein with an apparent K(m) for O(2) of 30 microM. The reaction was not inhibited by cyanide. The oxidase activity was traced back to a coenzyme F(420)-dependent enzyme that was purified to apparent homogeneity and that catalyzed the oxidation of 2 F(420)H(2) with 1 O(2) to 2 F(420) and 2 H(2)O. The apparent K(m) for F(420) was 30 microM and that for O(2) was 2 microM with a V(max) of 240 U/mg at 37 degrees C and pH 7.6, the pH optimum of the oxidase. The enzyme did not use NADH or NADPH as electron donor or H(2)O(2) as electron acceptor and was not inhibited by cyanide. The 45-kDa protein, whose gene was cloned and sequenced, contained 1 FMN per mol and harbored a binuclear iron center as indicated by the sequence motif H-X-E-X-D-X(62)-H-X(18)-D-X(60)-H. Sequence comparisons revealed that the F(420)H(2) oxidase from M. arboriphilus is phylogenetically closely related to FprA from Methanothermobacter marburgensis (71% sequence identity), a 45-kDa flavoprotein of hitherto unknown function, and to A-type flavoproteins from bacteria (30-40%), which all have dioxygen reductase activity. With heterologously produced FprA from M. marburgensis it is shown that this protein is also a highly efficient F(420)H(2) oxidase and that it contains 1 FMN and 2 iron atoms. The presence of F(420)H(2) oxidase in methanogenic archaea may explain why some methanogens, e.g., the Methanobrevibacter species in the termite hindgut, cannot only tolerate but thrive under microoxic conditions.