The effect of methanogen growth on mineral substrates: will Ni markers of methanogen-based communities be detectable in the rock record?

Methanogens, thought to be present on early Earth, have a high requirement for Ni, suggesting that Ni utilization could be a potential biosignature for methanogens if enhanced Ni extraction from surrounding minerals accompanies methanogenic growth. To test the potential for such Ni extraction from minerals by methanogens, Ni release from Ni-containing silicate glass was measured in Ni-free growth medium in the presence of the methanogen Methanothermobacter thermoautotrophicus (average pH ∼7.0) and observed to be higher than an abiotic control (average pH ∼6.8). However, batch dissolution experiments and a siderophore assay indicate that cell exudates such as siderophores, low molecular weight organic acids, or lysates accompanying cell death are not responsible for the observed increase in Ni release rate. In addition, scanning electron microscopy (SEM) shows little to no evidence of direct microbe-mineral interactions such as biofilms or pitting. Instead, comparison with abiotic experiments suggests that changes in pH due to CO₂ uptake may be responsible for enhanced dissolution in the presence of metabolizing cells. These results document that methanogens may not preferentially extract Ni from surrounding minerals although they may indirectly affect mineral reaction rates that are pH sensitive. Thus identifiable Ni biosignatures may not exist in the rock record to document the presence of methanogens on early Earth or Mars.

An unconventional pathway for reduction of CO2 to methane in CO-grown Methanosarcina acetivorans revealed by proteomics

Methanosarcina acetivorans produces acetate, formate, and methane when cultured with CO as the growth substrate [Rother M, Metcalf WW (2004) Proc Natl Acad Sci USA 101:], which suggests novel features of CO metabolism. Here we present a genome-wide proteomic approach to identify and quantify proteins differentially abundant in response to growth on CO versus methanol or acetate. The results indicate that oxidation of CO to CO2 supplies electrons for reduction of CO2 to a methyl group by steps and enzymes of the pathway for CO2 reduction determined for other methane-producing species. However, proteomic and quantitative RT-PCR results suggest that reduction of the methyl group to methane involves novel methyltransferases and a coenzyme F420H2:heterodisulfide oxidoreductase system that generates a proton gradient for ATP synthesis not previously described for pathways reducing CO2 to methane. Biochemical assays support a role for the oxidoreductase, and transcriptional mapping identified an unusual operon structure encoding the oxidoreductase. The proteomic results further indicate that acetate is synthesized from the methyl group and CO by a reversal of initial steps in the pathway for conversion of acetate to methane that yields ATP by substrate level phosphorylation. The results indicate that M. acetivorans utilizes a pathway distinct from all known CO2 reduction pathways for methane formation that reflects an adaptation to the marine environment. Finally, the pathway supports the basis for a recently proposed primitive CO-dependent energy-conservation cycle that drove and directed the early evolution of life on Earth.

New Algorithm for 15N/14N Quantitation with LC−ESI−MS Using an LTQ-FT Mass Spectrometer

A new algorithm (QN) for the (15)N /(14)N quantitation of relative protein abundances in complex proteomic samples is described. QN takes advantage of the high resolution, mass accuracy and throughput of the hybrid mass spectrometer LTQ-FT MS. Peptide quantitation is based on MS peak intensity (measured in the FT MS), while peptide identification is performed in the MS/MS mode (measured in the LTQ linear ion trap). Accuracy of the protein abundance is enhanced by a novel scoring procedure, allowing filtering of less reliable measurements of peptide abundances. The performance of QN is illustrated in the relative quantitative analysis of M. acetivorans C2A cultures grown with carbon monoxide vs methanol as substrate. Roughly 1,000 proteins were quantitated with an average CV of 9% for the protein abundance ratios. QN performs quantitation without manual intervention, does not require high processing power, and generates files compatible with the Guidelines for Proteomic Data Publication.

WrbA from Escherichia coli and Archaeoglobus fulgidus is an NAD(P)H:quinone oxidoreductase

WrbA (tryptophan [W] repressor-binding protein) was discovered in Escherichia coli, where it was proposed to play a role in regulation of the tryptophan operon; however, this has been put in question, leaving the function unknown. Here we report a phylogenetic analysis of 30 sequences which indicated that WrbA is the prototype of a distinct family of flavoproteins which exists in a diversity of cell types across all three domains of life and includes documented NAD(P)H:quinone oxidoreductases (NQOs) from the Fungi and Viridiplantae kingdoms. Biochemical characterization of the prototypic WrbA protein from E. coli and WrbA from Archaeoglobus fulgidus, a hyperthermophilic species from the Archaea domain, shows that these enzymes have NQO activity, suggesting that this activity is a defining characteristic of the WrbA family that we designate a new type of NQO (type IV). For E. coli WrbA, the K(m)(NADH) was 14 +/- 0.43 microM and the K(m)(benzoquinone) was 5.8 +/- 0.12 microM. For A. fulgidus WrbA, the K(m)(NADH) was 19 +/- 1.7 microM and the K(m)(benzoquinone) was 37 +/- 3.6 microM. Both enzymes were found to be homodimeric by gel filtration chromatography and homotetrameric by dynamic light scattering and to contain one flavin mononucleotide molecule per monomer. The NQO activity of each enzyme is retained over a broad pH range, and apparent initial velocities indicate that maximal activities are comparable to the optimum growth temperature for the respective organisms. The results are discussed and implicate WrbA in the two-electron reduction of quinones, protecting against oxidative stress.

Structural and functional studies suggest a catalytic mechanism for the phosphotransacetylase from Methanosarcina thermophila

Phosphotransacetylase (EC 2.3.1.8) catalyzes reversible transfer of the acetyl group from acetyl phosphate to coenzyme A (CoA), forming acetyl-CoA and inorganic phosphate. Two crystal structures of phosphotransacetylase from the methanogenic archaeon Methanosarcina thermophila in complex with the substrate CoA revealed one CoA (CoA1) bound in the proposed active site cleft and an additional CoA (CoA2) bound at the periphery of the cleft. The results of isothermal titration calorimetry experiments are described, and they support the hypothesis that there are distinct high-affinity (equilibrium dissociation constant [KD], 20 microM) and low-affinity (KD, 2 mM) CoA binding sites. The crystal structures indicated that binding of CoA1 is mediated by a series of hydrogen bonds and extensive van der Waals interactions with the enzyme and that there are fewer of these interactions between CoA2 and the enzyme. Different conformations of the protein observed in the crystal structures suggest that domain movements which alter the geometry of the active site cleft may contribute to catalysis. Kinetic and calorimetric analyses of site-specific replacement variants indicated that there are catalytic roles for Ser309 and Arg310, which are proximal to the reactive sulfhydryl of CoA1. The reaction is hypothesized to proceed through base-catalyzed abstraction of the thiol proton of CoA by the adjacent and invariant residue Asp316, followed by nucleophilic attack of the thiolate anion of CoA on the carbonyl carbon of acetyl phosphate. We propose that Arg310 binds acetyl phosphate and orients it for optimal nucleophilic attack. The hypothesized mechanism proceeds through a negatively charged transition state stabilized by hydrogen bond donation from Ser309.

Steady-state kinetic analysis of phosphotransacetylase from Methanosarcina thermophila

Phosphotransacetylase (EC 2.3.1.8) catalyzes the reversible transfer of the acetyl group from acetyl phosphate to coenzyme A (CoA), forming acetyl-CoA and inorganic phosphate. A steady-state kinetic analysis of the phosphotransacetylase from Methanosarcina thermophila indicated that there is a ternary complex kinetic mechanism rather than a ping-pong kinetic mechanism. Additionally, inhibition patterns of products and a nonreactive substrate analog suggested that the substrates bind to the enzyme in a random order. Dynamic light scattering revealed that the enzyme is dimeric in solution.

Proposal for a Hydrogen Bond Network in the Active Site of the Prototypic γ-Class Carbonic Anhydrase

The crystal structure of Cam, the prototypic gamma-class carbonic anhydrase, reveals active site residues Gln75, Asn73, and Asn 202 previously hypothesized to participate in catalysis. These potential roles were investigated for the first time by kinetic analyses of site-specific replacement variants of the zinc and cobalt forms of Cam. Gln75 replacement variants showed large decreases in k(cat)/K(m) relative to wild-type. Further, the Gln75 variants showed a loss of the pK(a) in pH versus k(cat)/K(m) profiles previously attributed to ionization of the metal-bound water yielding the hydroxyl group attacking CO(2). These results support the previously proposed role for Gln75 in hydrogen bonding with the catalytic hydroxyl orienting it for attack on CO(2). Kinetic analyses of Asn73 variants were consistent with a role in hydrogen bonding with Gln75 to position it for optimal interaction with the catalytic hydroxyl. Kinetic analyses of Asn202 variants showed substantial decreases in k(cat)/K(m) relative to the wild-type enzyme supporting the previously hypothesized role in polarizing CO(2) and facilitating attack from the metal-bound hydroxyl. On the basis of results presented here, and previously reported structural analyses, we present a catalytic mechanism involving Gln75, Asn73, and Asn202 that also suggests a role for Glu62 not previously recognized. Finally, the results suggest that the gamma-, beta-, and alpha-class carbonic anhydrases each independently evolved variations of a fundamental hydrogen bond network essential for catalysis.

The stepwise evolution of early life driven by energy conservation

Two main theories have emerged for the origin and early evolution of life based on heterotrophic versus chemoautotrophic metabolisms. With the exception of a role for CO, the theories have little common ground. Here we propose an alternative theory for the early evolution of the cell which combines principal features of the widely disparate theories. The theory is based on the extant pathway for conversion of CO to methane and acetate, largely deduced from the genomic analysis of the archaeon Methanosarcina acetivorans. In contrast to current paradigms, we propose that an energy-conservation pathway was the major force which powered and directed the early evolution of the cell. We envision the proposed primitive energy-conservation pathway to have developed sometime after a period of chemical evolution but prior to the establishment of diverse protein-based anaerobic metabolisms. We further propose that energy conservation played the predominant role in the later evolution of anaerobic metabolisms which explains the origin and evolution of extant methanogenic pathways.

Interaction of iron-sulfur flavoprotein with oxygen and hydrogen peroxide

The dimeric iron-sulfur flavoprotein (Isf) from Methanosarcina thermophila contains one 4Fe-4S center and one FMN per monomer, and is the prototype of a family widely distributed among strictly anaerobic prokaryotes. Although Isf is able to oxidize ferredoxin, the physiological electron acceptor is unknown; thus, the ability of Isf to reduce O2 and H2O2 was investigated. The product of O2 or H2O2 reduction by Isf was determined to be water. The kinetic parameters of the oxidative half-reactions with O2 and H2O2 as electron acceptors were consistent with a role for Isf in combating oxidative stress. Isf depleted of the 4Fe-4S cluster was unable to oxidize ferredoxin and reduce the FMN cofactor, supporting a role for the cluster in transfer of electrons from ferredoxin to the cofactor. The implications of these properties on the possible function and mechanism of Isf are discussed.

Electron transport in the pathway of acetate conversion to methane in the marine archaeon Methanosarcina acetivorans

A liquid chromatography-hybrid linear ion trap-Fourier transform ion cyclotron resonance mass spectrometry approach was used to determine the differential abundance of proteins in acetate-grown cells compared to that of proteins in methanol-grown cells of the marine isolate Methanosarcina acetivorans metabolically labeled with 14N versus 15N. The 246 differentially abundant proteins in M. acetivorans were compared with the previously reported 240 differentially expressed genes of the freshwater isolate Methanosarcina mazei determined by transcriptional profiling of acetate-grown cells compared to methanol-grown cells. Profound differences were revealed for proteins involved in electron transport and energy conservation. Compared to methanol-grown cells, acetate-grown M. acetivorans synthesized greater amounts of subunits encoded in an eight-gene transcriptional unit homologous to operons encoding the ion-translocating Rnf electron transport complex previously characterized from the Bacteria domain. Combined with sequence and physiological analyses, these results suggest that M. acetivorans replaces the H2-evolving Ech hydrogenase complex of freshwater Methanosarcina species with the Rnf complex, which generates a transmembrane ion gradient for ATP synthesis. Compared to methanol-grown cells, acetate-grown M. acetivorans synthesized a greater abundance of proteins encoded in a seven-gene transcriptional unit annotated for the Mrp complex previously reported to function as a sodium/proton antiporter in the Bacteria domain. The differences reported here between M. acetivorans and M. mazei can be attributed to an adaptation of M. acetivorans to the marine environment.

Proteome of Methanosarcina acetivorans Part I: an expanded view of the biology of the cell

Methanosarcina acetivorans is representative of the genus that is distinguished from all other methane-producing genera by extensive metabolic diversity predicted from the large genome. In Part I of this study, two-dimensional gel electrophoresis and MALDI-TOF-TOF mass spectrometry was used to investigate the proteome of methanol- or acetate-grown M. acetivorans, with the goal of an initial characterization of the diversity of the proteins synthesized. A total of 412 proteins were identified, representing nearly 10% of the ORFs, with nearly 30% conserved hypothetical or hypothetical. Of the 412 proteins, 188 were found in both acetate- and methanol-grown cells, 122 were detected only in acetate-grown cells, and 102 only in methanol-grown cells. The results revealed the expression of a remarkable number of redundant genes which encode enzymes involved in the pathways for methanogenesis from methanol or acetate, suggesting an important role for the unusually high percentage of redundant genes in Methanosarcina species. Evidence was obtained for synthesis of a sodium-transporting oxidoreductase in acetate-grown cells, with the potential to function in energy conservation. Several transcriptional regulatory proteins were identified that also function in the Bacteria domain, raising questions regarding their interaction with the Archaea/Eucarya-type basal transcription apparatus. In addition, a significant number of proteins involved in protein folding were shown to be synthesized in methanol- and acetate-grown cells. These studies provide the first examination of the protein diversity of M. acetivorans.

Proteome of Methanosarcina acetivorans Part II: comparison of protein levels in acetate- and methanol-grown cells

Methanosarcina acetivorans is an archaeon isolated from marine sediments which utilizes a diversity of substrates for growth and methanogenesis. Part I of a two-part investigation has profiled proteins of this microorganism cultured with both methanol and acetate as growth substrates, utilizing two-dimensional gel electrophoresis and MALDI-TOF-TOF mass spectrometry. In this report, Part II, the analyses were extended to identify 34 proteins found to be present in different amounts between methanol- and acetate-grown M. acetivorans. Among these proteins are enzymes which function in pathways for methanogenesis from either acetate or methanol. Several of the 34 proteins were determined to have redundant functions based on annotations of the genomic sequence. Enzymes which function in ATP synthesis and steps common to both methanogenic pathways were elevated in acetate- versus methanol-grown cells, whereas enzymes that have a more general function in protein synthesis were in greater amounts in methanol- compared to acetate-grown cells. Several group I chaperonins were present in greater amounts in methanol- versus acetate-grown cells, whereas lower amounts of several stress related proteins were found in methanol- versus acetate-grown cells. The potential physiological basis for these novel patterns of protein synthesis are discussed.

Structures of the iron-sulfur flavoproteins from Methanosarcina thermophila and Archaeoglobus fulgidus

Iron-sulfur flavoproteins (ISF) constitute a widespread family of redox-active proteins in anaerobic prokaryotes. Based on sequence homologies, their overall structure is expected to be similar to that of flavodoxins, but in addition to a flavin mononucleotide cofactor they also contain a cubane-type [4Fe:4S] cluster. In order to gain further insight into the function and properties of ISF, the three-dimensional structures of two ISF homologs, one from the thermophilic methanogen Methanosarcina thermophila and one from the hyperthermophilic sulfate-reducing archaeon Archaeoglobus fulgidus, were determined. The structures indicate that ISF assembles to form a tetramer and that electron transfer between the two types of redox cofactors requires oligomerization to juxtapose the flavin mononucleotide and [4Fe:4S] cluster bound to different subunits. This is only possible between different monomers upon oligomerization. Fundamental differences in the surface properties of the two ISF homologs underscore the diversity encountered within this protein family.

Trace methane oxidation studied in several Euryarchaeota under diverse conditions

We used (13)C-labeled methane to document the extent of trace methane oxidation by Archaeoglobus fulgidus, Archaeoglobus lithotrophicus, Archaeoglobus profundus, Methanobacterium thermoautotrophicum, Methanosarcina barkeri and Methanosarcina acetivorans. The results indicate trace methane oxidation during growth varied among different species and among methanogen cultures grown on different substrates. The extent of trace methane oxidation by Mb. thermoautotrophicum (0.05 +/- 0.04%, +/- 2 standard deviations of the methane produced during growth) was less than that by M. barkeri (0.15 +/- 0.04%), grown under similar conditions with H(2) and CO(2). Methanosarcina acetivorans oxidized more methane during growth on trimethylamine (0.36 +/- 0.05%) than during growth on methanol (0.07 +/- 0.03%). This may indicate that, in M. acetivorans, either a methyltransferase related to growth on trimethylamine plays a role in methane oxidation, or that methanol is an intermediate of methane oxidation. Addition of possible electron acceptors (O(2), NO(3) (-), SO(4) (2-), SO(3) (2-)) or H(2) to the headspace did not substantially enhance or diminish methane oxidation in M. acetivorans cultures. Separate growth experiments with FAD and NAD(+) showed that inclusion of these electron carriers also did not enhance methane oxidation. Our results suggest trace methane oxidized during methanogenesis cannot be coupled to the reduction of these electron acceptors in pure cultures, and that the mechanism by which methane is oxidized in methanogens is independent of H(2) concentration. In contrast to the methanogens, species of the sulfate-reducing genus Archaeoglobus did not significantly oxidize methane during growth (oxidizing 0.003 +/- 0.01% of the methane provided to A. fulgidus, 0.002 +/- 0.009% to A. lithotrophicus and 0.003 +/- 0.02% to A. profundus). Lack of observable methane oxidation in the three Archaeoglobus species examined may indicate that methyl-coenzyme M reductase, which is not present in this genus, is required for the anaerobic oxidation of methane, consistent with the "reverse methanogenesis" hypothesis.

Characterization of the acetate binding pocket in the Methanosarcina thermophila acetate kinase

Acetate kinase catalyzes the reversible magnesium-dependent synthesis of acetyl phosphate by transfer of the ATP gamma-phosphoryl group to acetate. Inspection of the crystal structure of the Methanosarcina thermophila enzyme containing only ADP revealed a solvent-accessible hydrophobic pocket formed by residues Val(93), Leu(122), Phe(179), and Pro(232) in the active site cleft, which identified a potential acetate binding site. The hypothesis that this was a binding site was further supported by alignment of all acetate kinase sequences available from databases, which showed strict conservation of all four residues, and the recent crystal structure of the M. thermophila enzyme with acetate bound in this pocket. Replacement of each residue in the pocket produced variants with K(m) values for acetate that were 7- to 26-fold greater than that of the wild type, and perturbations of this binding pocket also altered the specificity for longer-chain carboxylic acids and acetyl phosphate. The kinetic analyses of variants combined with structural modeling indicated that the pocket has roles in binding the methyl group of acetate, influencing substrate specificity, and orienting the carboxyl group. The kinetic analyses also indicated that binding of acetyl phosphate is more dependent on interactions of the phosphate group with an unidentified residue than on interactions between the methyl group and the hydrophobic pocket. The analyses also indicated that Phe(179) is essential for catalysis, possibly for domain closure. Alignments of acetate kinase, propionate kinase, and butyrate kinase sequences obtained from databases suggested that these enzymes have similar catalytic mechanisms and carboxylic acid substrate binding sites.

Structural and kinetic analyses of arginine residues in the active site of the acetate kinase from Methanosarcina thermophila

Acetate kinase catalyzes transfer of the gamma-phosphate of ATP to acetate. The only crystal structure reported for acetate kinase is the homodimeric enzyme from Methanosarcina thermophila containing ADP and sulfate in the active site (Buss, K. A., Cooper, D. C., Ingram-Smith, C., Ferry, J. G., Sanders, D. A., and Hasson, M. S. (2001) J. Bacteriol. 193, 680-686). Here we report two new crystal structure of the M. thermophila enzyme in the presence of substrate and transition state analogs. The enzyme co-crystallized with the ATP analog adenosine 5'-[gamma-thio]triphosphate contained AMP adjacent to thiopyrophosphate in the active site cleft of monomer B. The enzyme co-crystallized with ADP, acetate, Al(3+), and F(-) contained a linear array of ADP-AlF(3)-acetate in the active site cleft of monomer B. Together, the structures clarify the substrate binding sites and support a direct in-line transfer mechanism in which AlF(3) mimics the meta-phosphate transition state. Monomers A of both structures contained ADP and sulfate, and the active site clefts were closed less than in monomers B, suggesting that domain movement contributes to catalysis. The finding that His(180) was in close proximity to AlF(3) is consistent with a role for stabilization of the meta-phosphate that is in agreement with a previous report indicating that this residue is essential for catalysis. Residue Arg(241) was also found adjacent to AlF(3), consistent with a role for stabilization of the transition state. Kinetic analyses of Arg(241) and Arg(91) replacement variants indicated that these residues are essential for catalysis and also indicated a role in binding acetate.

Carbonic anhydrase inhibitors. Inhibition of the prokariotic beta and gamma-class enzymes from Archaea with sulfonamides

A detailed inhibition study of carbonic anhydrases (CAs, EC 4.2.1.1) belonging to the beta- and gamma-families from Archaea with sulfonamides has been performed. Compounds included in this study were the clinically used sulfonamide CA inhibitors, such as acetazolamide, methazolamide, ethoxzolamide, topiramate, valdecoxib, celecoxib, dorzolamide, sulfanilamide, dichlorophanamide, as well as sulfanilamide analogs, halogenated sulfanilamides, and some 1,3-benzenedisulfonamide derivatives. The two gamma-CAs from Methanosarcina thermophila (Zn-Cam and Co-Cam) showed very different inhibitory properties with these compounds, as compared to the alpha-CA isozymes hCA I, II, and IX, and the beta-CA from Methanobacterium thermoautotrophicum (Cab). The best Zn-Cam inhibitors were sulfamic acid and acetazolamide, with inhibition constants in the range of 63-96 nM, whereas other investigated aromatic/heterocylic sulfonamides showed a rather levelled behavior, with KIs in the range of 0.12-1.70 microM. The best Co-Cam inhibitors were topiramate and p-aminoethyl-benzenesulfonamide, with KIs in the range of 0.12-0.13 microM, whereas the worst one was homosulfanilamide (KI of 8.50 microM). In the case of Cab, the inhibitory power of these compounds varied to a much larger extent, with sulfamic acid and sulfamide showing millimolar affinities (KIs in the range of 44-103 mM), whereas the best inhibitor was ethoxzolamide, with a KI of 5.35 microM. Most of these sulfonamides showed inhibition constants in the range of 12-100 microM against Cab. Thus, the three CA families investigated up to now possess a very diverse affinity for sulfonamides, the inhibitors with important medicinal, and environmental applications.

Carbonic anhydrase inhibitors. Inhibition of the beta-class enzyme from the methanoarchaeon Methanobacterium thermoautotrophicum (Cab) with anions

The first inhibition study of the beta-class carbonic anhydrase (CA, EC 4.2.1.1) from the methanoarchaeon Methanobacterium thermoautotrophicum (Cab) with anions is reported here. Inhibition data of the alpha-class human isozymes hCA I and hCA II (cytosolic) as well as the membrane-bound isozyme hCA IV and the gamma-class enzyme from another archaeon, Methanosarcina thermophila (Cam) with a large number of anionic species such as halides, pseudohalides, bicarbonate, carbonate, nitrate, nitrite, hydrosulfide, bisulfite, sulfate, etc., are also provided for comparison. The best Cab anion inhibitors were thiocyanate and hydrogen sulfide, with inhibition constants in the range of 0.52-0.70 mM, whereas cyanate, iodide, carbonate, and nitrate were weaker inhibitors (Ki's in the range of 7.8-13.2 mM). Fluoride, chloride, and sulfate do not inhibit this enzyme appreciably, whereas the CA substrate bicarbonate, or other anions, such as bromide, nitrite, bisulfite, or sulfamate behave as weak inhibitors (Ki in the range of 40-45 mM). It is interesting to note that the metal poison, coordinating anions cyanide and azide are also rather weak Cab inhibitors (Ki in the range of 27-55 mM), whereas sulfamide is a very weak Cab inhibitor (Ki of 103 mM), although it strongly inhibits Cam (Ki of 70 microM). Surprisingly, phenylboronic and phenylarsonic acids, which have been investigated for the inhibition of all these CAs for the first time, showed very weak activity against the alpha-CA isozymes, but were effective Cab and Cam inhibitors. The best Cab inhibitors were just these two compounds (Ki's of 0.20-0.33 mM), whereas the best Cam inhibitor was sulfamic acid (Ki of 96 nM). These major differences of behavior between the diverse CAs investigated here toward anion inhibitors can be difficultly explained considering the convergent evolution of so diverse enzymes for the binding and turnover of small molecules such as carbon dioxide and anions.

Carbonic anhydrase inhibitors. Inhibition of the zinc and cobalt γ-class enzyme from the archaeon Methanosarcina thermophila with anions

Anions represent the second class of inhibitors of the zinc enzyme carbonic anhydrase (CA, EC 4.2.1.1), in addition to sulfonamides, which possess clinical applications. The first inhibition study of the zinc and cobalt gamma-class enzyme from the archaeon Methanosarcina thermophila (Cam) with anions is reported here. Inhibition data of the alpha-class human isozymes hCA I and hCA II (cytosolic) as well as the membrane-bound isozyme hCA IV with a large number of anionic species such as halides, pseudohalides, bicarbonate, carbonate, nitrate, nitrite, hydrosulfide, bisulfite, and sulfate, etc., are also provided for comparison. The best Zn-Cam anion inhibitors were hydrogen sulfide and cyanate, with inhibition constants in the range of 50-90 microM, whereas thiocyanate, azide, carbonate, nitrite, and bisulfite were weaker inhibitors (K(I)s in the range of 5.8-11.7 mM). Fluoride, chloride, and sulfate do not inhibit this enzyme appreciably up to concentrations of 200 mM, whereas the substrate bicarbonate behaves as a weak inhibitor (K(I)s of 42 mM). The best Co-Cam inhibitor was carbonate, with an inhibition constant of 9 microM, followed by nitrate and bicarbonate (K(I)s in the range of 90-100 microM). The metal poisons were much more ineffective inhibitors of this enzyme, with cyanide possessing an inhibition constant of 51.5mM, whereas cyanate, thiocyanate, azide, iodide, and hydrogen sulfide showed K(I)s in the range of 2.0-6.1mM. As for Zn-Cam, fluoride, chloride, and sulfate are not inhibitors of Co-Cam. These major differences between the two gamma-CAs investigated here can be explained only in part by the different geometries of the metal ions present within their active sites.

Gamma carbonic anhydrases in plant mitochondria

Three genes from Arabidopsis thaliana with high sequence similarity to gamma carbonic anhydrase (gammaCA), a Zn containing enzyme from Methanosarcina thermophila (CAM), were identified and characterized. Evolutionary and structural analyses predict that these genes code for active forms of gammaCA. Phylogenetic analyses reveal that these Arabidopsis gene products cluster together with CAM and related sequences from alpha and gamma proteobacteria, organisms proposed as the mitochondrial endosymbiont ancestor. Indeed, in vitro and in vivo experiments indicate that these gene products are transported into the mitochondria as occurs with several mitochondrial protein genes transferred, during evolution, from the endosymbiotic bacteria to the host genome. Moreover, putative CAM orthologous genes are detected in other plants and green algae and were predicted to be imported to mitochondria. Structural modeling and sequence analysis performed in more than a hundred homologous sequences show a high conservation of functionally important active site residues. Thus, the three histidine residues involved in Zn coordination (His 81, 117 and 122), Arg 59, Asp 61, Gin 75, and Asp 76 of CAM are conserved and properly arranged in the active site cavity of the models. Two other functionally important residues (Glu 62 and Glu 84 of CAM) are lacking, but alternative amino acids that might serve to their roles are postulated. Accordingly, we propose that photosynthetic eukaryotic organisms (green algae and plants) contain gammaCAs and that these enzymes codified by nuclear genes are imported into mitochondria to accomplish their biological function.

Crystal Structure of Phosphotransacetylase from the Methanogenic Archaeon Methanosarcina thermophila

Phosphotransacetylase (Pta) [EC 2.3.1.8] is ubiquitous in the carbon assimilation and energy-yielding pathways in anaerobic prokaryotes where it catalyzes the reversible transfer of the acetyl group from acetyl phosphate to CoA forming acetyl CoA and inorganic phosphate. The crystal structure of Pta from the methane-producing archaeon Methanosarcina thermophila, representing the first crystal structure of any Pta, was determined by multiwavelength anomalous diffraction at 2.7 A resolution. In solution and in the crystal, the enzyme forms a homodimer. Each monomer consists of two alpha/beta domains with a cleft along the domain boundary, which presumably contains the substrate binding sites. Comparison of the four monomers present in the asymmetric unit indicates substantial variations in the relative orientation of the two domains and the structure of the putative active site cleft. A search for structural homologs revealed the NADP(+)-dependent isocitrate and isopropylmalate dehydrogenases as the only homologs with a similar two-domain architecture.

Flavin mononucleotide-binding flavoprotein family in the domain Archaea

The protein (AfpA, for archaeoflavoprotein) encoded by AF1518 in the genome of Archaeoglobus fulgidus was produced in Escherichia coli and characterized. AfpA was found to be a homodimer with a native molecular mass of 43 kDa and containing two noncovalently bound flavin mononucleotides (FMNs). The cell extract of A. fulgidus catalyzed the CO-dependent reduction of AfpA that was stimulated by the addition of ferredoxin. Ferredoxin was found to be a direct electron donor to purified AfpA, whereas rubredoxin was unable to substitute. Neither NADH nor NADPH was an electron donor. Ferricyanide, 2,6-dichlorophenolindophenol, several quinones, ferric citrate, bovine cytochrome c, and O(2) accepted electrons from reduced AfpA, whereas coenzyme F(420) did not. The rate of cytochrome c reduction was enhanced in the presence of O(2) suggesting that superoxide is a product of the interaction of reduced AfpA with O(2). Although AF1518 was previously annotated as encoding a decarboxylase involved in coenzyme A biosynthesis, the results establish that AfpA is an electron carrier protein with ferredoxin as the physiological electron donor. The genomes of several diverse Archaea contained afpA homologs clustered with open reading frames annotated as homologs of genes encoding reductases involved in the oxidative stress response of anaerobes from the domain Bacteria. A potential role for AfpA in coupling electron flow from ferredoxin to the putative reductases is discussed. A search of the databases suggests that AfpA is the prototype of a previously unrecognized flavoprotein family unique to the domain Archaea for which the name archaeoflavoprotein is proposed.

A role for iron in an ancient carbonic anhydrase

Since 1933, carbonic anhydrase research has focused on enzymes from mammals (alpha class) and plants (beta class); however, two additional classes (gamma and delta) were discovered recently. Cam, from the procaryote Methanosarcina thermophila, is the prototype of the gamma class and the first carbonic anhydrase to be characterized from either an anaerobic organism or the Archaea domain. All of the enzymes characterized from the four classes have been purified aerobically and are reported to contain a catalytic zinc. Herein, we report the anaerobic reconstitution of apo-Cam with Fe2+, which yielded Cam with an effective kcat that exceeded that for the Zn2+-reconstituted enzyme. Mössbauer spectroscopy showed that the Fe2+-reconstituted enzyme contained high spin Fe2+ that, when oxidized to Fe3+, inactivated the enzyme. Reconstitution with Fe3+ was unsuccessful. Reconstitution with Cu2+, Mn2+, Ni2+, or Cd2+ yielded enzymes with effective kcat values that were 10% or less than the value for the Zn2+-reconstituted Cam. Cam produced in Escherichia coli and purified anaerobically contained iron with effective kcat and kcat/Km values exceeding the values for Zn2+-reconstituted Cam. The results identify a previously unrecognized biological function for iron.

Expression, purification, crystallization and preliminary X-ray analysis of phosphotransacetylase from Methanosarcina thermophila

Phosphotransacetylase (Pta) from the anaerobic archaeon Methanosarcina thermophila has been heterologously expressed in a soluble form which facilitated crystallization using the hanging-drop vapor-diffusion method with ammonium sulfate as a precipitant. This is the first report of the crystallization of any Pta. While the M. thermophila Pta has high sequence identity to Ptas from other organisms, it has no homology to any previously crystallized proteins. The protein crystallized in space group I4(1), with unit-cell parameters a = b = 114.8, c = 127.8 A, alpha = beta = gamma = 90 degrees. The crystals diffracted to 2.5 A resolution using Cu Kalpha radiation. The enzyme had previously been reported to exist as a monomer; however, the self-rotation function showed the presence of a non-crystallographic symmetry axis at psi = 90, phi = 90, kappa = 180 degrees, suggesting oligomerization. Dynamic light-scattering analysis supported a dimeric state for Pta in solution.

Chemical rescue of proton transfer in catalysis by carbonic anhydrases in the beta- and gamma-class

Catalysis of the dehydration of HCO(3)(-) by carbonic anhydrase requires proton transfer from solution to the zinc-bound hydroxide. Carbonic anhydrases in each of the alpha, beta, and gamma classes, examples of convergent evolution, appear to have a side chain extending into the active site cavity that acts as a proton shuttle to facilitate this proton transfer, with His 64 being the most prominent example in the alpha class. We have investigated chemical rescue of mutants in two of these classes in which a proton shuttle has been replaced with a residue that does not transfer protons: H216N carbonic anhydrase from Arabidopsis thaliana (beta class) and E84A carbonic anhydrase from the archeon Methanosarcina thermophila (gamma class). A series of structurally homologous imidazole and pyridine buffers were used as proton acceptors in the activation of CO(2) hydration at steady state and as proton donors of the exchange of (18)O between CO(2) and water at chemical equilibrium. Free energy plots of the rate constants for this intermolecular proton transfer as a function of the difference in pK(a) of donor and acceptor showed extensive curvature, indicating a small intrinsic kinetic barrier for the proton transfers. Application of Marcus rate theory allowed quantitative estimates of the intrinsic kinetic barrier which were near 0.3 kcal/mol with work functions in the range of 7-11 kcal/mol for mutants in the beta and gamma class, similar to results obtained for mutants of carbonic anhydrase in the alpha class. The low values of the intrinsic kinetic barrier for all three classes of carbonic anhydrase reflect proton transfer processes that are consistent with a model of very rapid proton transfer through a flexible matrix of hydrogen-bonded solvent structures sequestered within the active sites of the carbonic anhydrases.

Genomic and proteomic analyses reveal multiple homologs of genes encoding enzymes of the methanol:coenzyme M methyltransferase system that are differentially expressed in methanol- and acetate-grown Methanosarcina thermophila

Each of the genomic sequences of Methanosarcina acetivorans, Methanosarcina mazei, and Methanosarcina thermophila revealed two homologs of mtaA, three homologs of mtaB, and three homologs of mtaC encoding enzymes specific for methanogenesis from methanol. Two-dimensional gel electrophoretic analyses of polypeptides from M. thermophila established that methanol induces the expression of mtaA-1, mtaB-1, mtaB-2, mtaB-3, mtaC-1, mtaC-2, and mtaC-3 whereas mtaB-3 and mtaC-3 are constitutively expressed in acetate-grown cells. The gene product of one of three mttC homologs, encoding trimethylamine-specific methyltransferase I, was detected in methanol- but not acetate-grown M. thermophila. A postulated role for the multiple homologs is discussed.

Roles of the conserved aspartate and arginine in the catalytic mechanism of an archaeal beta-class carbonic anhydrase

The roles of an aspartate and an arginine, which are completely conserved in the active sites of beta-class carbonic anhydrases, were investigated by steady-state kinetic analyses of replacement variants of the beta-class enzyme (Cab) from the archaeon Methanobacterium thermoautotrophicum. Previous kinetic analyses of wild-type Cab indicated a two-step zinc-hydroxide mechanism of catalysis in which the k(cat)/K(m) value depends only on the rate constants for the CO(2) hydration step, whereas k(cat) also depends on rate constants from the proton transfer step (K. S. Smith, N. J. Cosper, C. Stalhandske, R. A. Scott, and J. G. Ferry, J. Bacteriol. 182:6605-6613, 2000). The recently solved crystal structure of Cab shows the presence of a buffer molecule within hydrogen bonding distance of Asp-34, implying a role for this residue in the proton transport step (P. Strop, K. S. Smith, T. M. Iverson, J. G. Ferry, and D. C. Rees, J. Biol. Chem. 276:10299-10305, 2001). The k(cat)/K(m) values of Asp-34 variants were decreased relative to those of the wild type, although not to an extent which supports an essential role for this residue in the CO(2) hydration step. Parallel decreases in k(cat) and k(cat)/K(m) values for the variants precluded any conclusions regarding a role for Asp-34 in the proton transfer step; however, the k(cat) of the D34A variant was chemically rescued by replacement of 2-(N-morpholino)propanesulfonic acid buffer with imidazole at pH 7.2, supporting a role for the conserved aspartate in the proton transfer step. The crystal structure of Cab also shows Arg-36 with two hydrogen bonds to Asp-34. Arg-36 variants had both k(cat) and k(cat)/K(m) values that were decreased at least 250-fold relative to those of the wild type, establishing an essential function for this residue. Imidazole was unable to rescue the k(cat) of the R36A variant; however, partial rescue of the kinetic parameter was obtained with guanidine-HCl indicating that the guanido group of this residue is important.

Evidence for a transition state analog, MgADP-aluminum fluoride-acetate, in acetate kinase from Methanosarcina thermophila

Aluminum fluoride has become an important tool for investigating the mechanism of phosphoryl transfer, an essential reaction that controls a host of vital cell functions. Planar AlF(3) or AlF(4)(-) molecules are proposed to mimic the phosphoryl group in the catalytic transition state. Acetate kinase catalyzes phosphoryl transfer of the ATP gamma-phosphate to acetate. Here we describe the inhibition of acetate kinase from Methanosarcina thermophila by preincubation with MgCl(2), ADP, AlCl(3), NaF, and acetate. Preincubation with butyrate in place of acetate did not significantly inhibit the enzyme. Several NTPs can substitute for ATP in the reaction, and the corresponding NDPs, in conjunction with MgCl(2), AlCl(3), NaF, and acetate, inhibit acetate kinase activity. Fluorescence quenching experiments indicated an increase in binding affinity of acetate kinase for MgADP in the presence of AlCl(3), NaF, and acetate. These and other characteristics of the inhibition indicate that the transition state analog, MgADP-aluminum fluoride-acetate, forms an abortive complex in the active site. The protection from inhibition by a non-hydrolyzable ATP analog or acetylphosphate, in conjunction with the strict dependence of inhibition on the presence of both ADP and acetate, supports a direct in-line mechanism for acetate kinase.

The genome of M. acetivorans reveals extensive metabolic and physiological diversity

Methanogenesis, the biological production of methane, plays a pivotal role in the global carbon cycle and contributes significantly to global warming. The majority of methane in nature is derived from acetate. Here we report the complete genome sequence of an acetate-utilizing methanogen, Methanosarcina acetivorans C2A. Methanosarcineae are the most metabolically diverse methanogens, thrive in a broad range of environments, and are unique among the Archaea in forming complex multicellular structures. This diversity is reflected in the genome of M. acetivorans. At 5,751,492 base pairs it is by far the largest known archaeal genome. The 4524 open reading frames code for a strikingly wide and unanticipated variety of metabolic and cellular capabilities. The presence of novel methyltransferases indicates the likelihood of undiscovered natural energy sources for methanogenesis, whereas the presence of single-subunit carbon monoxide dehydrogenases raises the possibility of nonmethanogenic growth. Although motility has not been observed in any Methanosarcineae, a flagellin gene cluster and two complete chemotaxis gene clusters were identified. The availability of genetic methods, coupled with its physiological and metabolic diversity, makes M. acetivorans a powerful model organism for the study of archaeal biology. [Sequence, data, annotations and analyses are available at http://www-genome.wi.mit.edu/.]

Role of arginine 59 in the gamma-class carbonic anhydrases

The functional role of the highly conserved active site Arg 59 in the prototype of the gamma-class carbonic anhydrase Cam (carbonic anhydrase from Methanosarcina thermophila) was investigated. Variants (R59A, -C, -E, -H, -K, -M, and -Q) were prepared by site-directed mutagenesis and characterized by size exclusion chromatography (SEC), circular dichroism (CD) spectroscopy, and stopped-flow kinetic analyses. CD spectra indicated similar secondary structures for the wild type and the R59A and -K variants, independent of nondenaturing concentrations of guanidine hydrochloride (GdnHCl). SEC indicated that all variants purified as homotrimers like the wild type. SEC also revealed that the R59A and -K variants unfolded at > or = 1.5 M GdnHCl, compared to 3.0 M GdnHCl for the wild type. These results indicate that Arg 59 contributes to the thermodynamic stability of the Cam trimer. The R59K variant had k(cat) and k(cat)/K(m) values that were 8 and 5% of the wild-type values, respectively, while all other variants had k(cat) and k(cat)/K(m) values 10-100-fold lower than those of the wild type. The R59A, -C, -E, -M, and -Q variants exhibited 4-63-fold increases in k(cat) and 9-120-fold increases in k(cat)/K(m) upon addition of 100 mM GdnHCl, with the largest increases observed for the R59A variant, which was comparable to the R59K variant. The kinetic results indicate that a positive charge at position 59 is essential for the CO(2) hydration step of the overall catalytic mechanism.

Site-directed mutational analysis of active site residues in the acetate kinase from Methanosarcina thermophila

Acetate kinase catalyzes the magnesium-dependent transfer of the gamma-phosphate of ATP to acetate. The recently determined crystal structure of the Methanosarcina thermophila enzyme identifies it as a member of the sugar kinase/Hsc70/actin superfamily based on the fold and the presence of five putative nucleotide and metal binding motifs that characterize the superfamily. Residues from four of these motifs in M. thermophila acetate kinase were selected for site-directed replacement and analysis of the variants. Replacement of Asp(148) and Asn(7) resulted in variants with catalytic efficiencies less than 1% of that of the wild-type enzyme, indicating that these residues are essential for activity. Glu(384) was also found to be essential for catalysis. A 30-fold increase in the magnesium concentration required for half-maximal activity of the E384A variant relative to that of the wild type implicated Glu(384) in magnesium binding. The kinetic analysis of variants and structural data is consistent with nonessential roles for active site residues Ser(10), Ser(12), and Lys(14) in catalysis. The results are discussed with respect to the acetate kinase catalytic mechanism and the relationship to other sugar kinase/Hsc70/actin superfamily members.

Iron-sulfur flavoprotein (Isf) from Methanosarcina thermophila is the prototype of a widely distributed family

A total of 35 homologs of the iron-sulfur flavoprotein (Isf) from Methanosarcina thermophila were identified in databases. All three domains were represented, and multiple homologs were present in several species. An unusually compact cysteine motif ligating the 4Fe-4S cluster in Isf is conserved in all of the homologs except two, in which either an aspartate or a histidine has replaced the second cysteine in the motif. A phylogenetic analysis of Isf homologs identified four subgroups, two of which were supported by bootstrap data. Three homologs from metabolically and phylogenetically diverse species in the Bacteria and Archaea domains (Af3 from Archaeoglobus fulgidus, Cd1 from Clostridium difficile, and Mj2 from Methanococcus jannaschii) were overproduced in Escherichia coli. Each homolog purified as a homodimer, and the UV-visible absorption spectra were nearly identical to that of Isf. After reconstitution with iron, sulfide, and flavin mononucleotide (FMN) the homologs contained six to eight nonheme iron atoms and 1.6 to 1.7 FMN molecules per dimer, suggesting that two 4Fe-4S or 3Fe-4S clusters and two FMN cofactors were bound to each dimer, which is consistent with Isf data. Homologs Af3 and Mj2 were reduced by CO in reactions catalyzed by cell extract of acetate-grown M. thermophila, but Cd1 was not. Homologs Af3 and Mj2 were reduced by CO in reactions catalyzed by A. fulgidus and M. jannaschii cell extracts. Cell extract of Clostridium thermoaceticum catalyzed CO reduction of Cd1. Our database sequence analyses and biochemical characterizations indicate that Isf is the prototype of a family of iron-sulfur flavoproteins that occur in members of all three domains.

Role of arginines in coenzyme A binding and catalysis by the phosphotransacetylase from Methanosarcina thermophila

Phosphotransacetylase (EC 2.3.1.8) catalyzes the reversible transfer of the acetyl group from acetyl phosphate to coenzyme A (CoA): CH(3)COOPO(3)(2-) + CoASH <==> CH(3)COSCoA + HPO(4)(2-). The role of arginine residues was investigated for the phosphotransacetylase from Methanosarcina thermophila. Kinetic analysis of a suite of variants indicated that Arg 87 and Arg 133 interact with the substrate CoA. Arg 87 variants were reduced in the ability to discriminate between CoA and the CoA analog 3'-dephospho-CoA, indicating that Arg 87 forms a salt bridge with the 3'-phosphate of CoA. Arg 133 is postulated to interact with the 5'-phosphate of CoA. Large decreases in k(cat) and k(cat)/K(m) for all of the Arg 87 and Arg 133 variants indicated that these residues are also important, although not essential, for catalysis. Large decreases in k(cat) and k(cat)/K(m) were also observed for the variants in which lysine replaced Arg 87 and Arg 133, suggesting that the bidentate interaction of these residues with CoA or their greater bulk is important for optimal activity. Desulfo-CoA is a strong competitive inhibitor of the enzyme, suggesting that the sulfhydryl group of CoA is important for the optimization of CoA-binding energy but not for tight substrate binding. Chemical modification of the wild-type enzyme by 2,3-butanedione and substrate protection by CoA indicated that at least one reactive arginine is in the active site and is important for activity. The inhibition pattern of the R87Q variant indicated that Arg 87 is modified, which contributes to the inactivation; however, at least one additional active-site arginine is modified leading to enzyme inactivation, albeit at a lower rate.

Bicarbonate as a proton donor in catalysis by Zn(II)- and Co(II)-containing carbonic anhydrases

Catalysis of (18)O exchange between CO(2) and water catalyzed by a Co(II)-substituted mutant of human carbonic anhydrase II is analyzed to show the rate of release of H(2)(18)O from the active site. This rate, measured by mass spectrometry, is dependent on proton transfer to the metal-bound (18)O-labeled hydroxide, and was observed in a site-specific mutant of carbonic anhydrase II in which a prominent proton shuttle residue His64 was replaced by alanine, which does not support proton transport. Upon increasing the concentration of bicarbonate, the rate of release of H(2)(18)O increased in a saturable manner to a maximum of 4 x 10(5) s(-)(1), consistent with proton transfer from bicarbonate to the Co(II)-bound hydroxide. The same mutant of carbonic anhydrase containing Zn(II) had the rate of release of H(2)(18)O smaller by 10-fold, but rate of interconversion of CO(2) and HCO(3)(-) about the same as the Co(II)-containing enzyme. These data as well as solvent hydrogen isotope effects suggest that the bicarbonate transferring the proton is bound to the cobalt in the enzyme. The enhancement of (18)O exchange caused by increasing bicarbonate concentration during catalysis by the Zn(II)-containing carbonic anhydrase from the archaeon Methanosarcina thermophila suggests that a very similar mechanism for proton donation by bicarbonate occurs with this wild-type enzyme.

Crystal structure of the "cab"-type beta class carbonic anhydrase from the archaeon Methanobacterium thermoautotrophicum

The structure of the "cab"-type beta class carbonic anhydrase from the archaeon Methanobacterium thermoautotrophicum (Cab) has been determined to 2.1-A resolution using the multiwavelength anomalous diffraction phasing technique. Cab exists as a dimer with a subunit fold similar to that observed in "plant"-type beta class carbonic anhydrases. The active site zinc is coordinated by protein ligands Cys(32), His(87), and Cys(90), with the tetrahedral coordination completed by a water molecule. The major difference between plant- and cab-type beta class carbonic anhydrases is in the organization of the hydrophobic pocket. The structure reveals a Hepes buffer molecule bound 8 A away from the active site zinc, which suggests a possible proton transfer pathway from the active site to the solvent.

Urkinase: structure of acetate kinase, a member of the ASKHA superfamily of phosphotransferases

Acetate kinase, an enzyme widely distributed in the Bacteria and Archaea domains, catalyzes the phosphorylation of acetate. We have determined the three-dimensional structure of Methanosarcina thermophila acetate kinase bound to ADP through crystallography. As we previously predicted, acetate kinase contains a core fold that is topologically identical to that of the ADP-binding domains of glycerol kinase, hexokinase, the 70-kDa heat shock cognate (Hsc70), and actin. Numerous charged active-site residues are conserved within acetate kinases, but few are conserved within the phosphotransferase superfamily. The identity of the points of insertion of polypeptide segments into the core fold of the superfamily members indicates that the insertions existed in the common ancestor of the phosphotransferases. Another remarkable shared feature is the unusual, epsilon conformation of the residue that directly precedes a conserved glycine residue (Gly-331 in acetate kinase) that binds the alpha-phosphate of ADP. Structural, biochemical, and geochemical considerations indicate that an acetate kinase may be the ancestral enzyme of the ASKHA (acetate and sugar kinases/Hsc70/actin) superfamily of phosphotransferases.

Structural and kinetic characterization of an archaeal beta-class carbonic anhydrase

The beta-class carbonic anhydrase from the archaeon Methanobacterium thermoautotrophicum (Cab) was structurally and kinetically characterized. Analytical ultracentrifugation experiments show that Cab is a tetramer. Circular dichroism studies of Cab and the Spinacia oleracea (spinach) beta-class carbonic anhydrase indicate that the secondary structure of the beta-class enzymes is predominantly alpha-helical, unlike that of the alpha- or gamma-class enzymes. Extended X-ray absorption fine structure results indicate the active zinc site of Cab is coordinated by two sulfur and two O/N ligands, with the possibility that one of the O/N ligands is derived from histidine and the other from water. Both the steady-state parameters k(cat) and k(cat)/K(m) for CO(2) hydration are pH dependent. The steady-state parameter k(cat) is buffer-dependent in a saturable manner at both pH 8.5 and 6.5, and the analysis suggested a ping-pong mechanism in which buffer is the second substrate. At saturating buffer conditions and pH 8.5, k(cat) is 2.1-fold higher in H(2)O than in D(2)O, consistent with an intramolecular proton transfer step being rate contributing. The steady-state parameter k(cat)/K(m) is not dependent on buffer, and no solvent hydrogen isotope effect was observed. The results suggest a zinc hydroxide mechanism for Cab. The overall results indicate that prokaryotic beta-class carbonic anhydrases have fundamental characteristics similar to the eukaryotic beta-class enzymes and firmly establish that the alpha-, beta-, and gamma-classes are convergently evolved enzymes that, although structurally distinct, are functionally equivalent.

The role of histidines in the acetate kinase from Methanosarcina thermophila

The role of histidine in the catalytic mechanism of acetate kinase from Methanosarcina thermophila was investigated by diethylpyrocarbonate inactivation and site-directed mutagenesis. Inactivation was accompanied by an increase in absorbance at 240 nm with no change in absorbance at 280 nm, and treatment of the inactivated enzyme with hydroxylamine restored 95% activity, results that indicated diethylpyrocarbonate inactivates the enzyme by the specific modification of histidine. The substrates ATP, ADP, acetate, and acetyl phosphate protected against inactivation suggesting at least one active site where histidine is modified. Correlation of residual activity with the number of histidines modified, as determined by absorbance at 240 nm, indicated that a maximum of three histidines are modified per subunit, two of which are essential for full inactivation. Comparison of the M. thermophila acetate kinase sequence with 56 putative acetate kinase sequences revealed eight highly conserved histidines, three of which (His-123, His-180, and His-208) are perfectly conserved. Diethylpyrocarbonate inactivation of the eight histidine --> alanine variants indicated that His-180 and His-123 are in the active site and that the modification of both is necessary for full inactivation. Kinetic analyses of the eight variants showed that no other histidines are important for activity. Analysis of additional His-180 variants indicated that phosphorylation of His-180 is not essential for catalysis. Possible functions of His-180 are discussed.

Site-specific mutational analysis of a novel cysteine motif proposed to ligate the 4Fe-4S cluster in the iron-sulfur flavoprotein of the thermophilic methanoarchaeon Methanosarcina thermophila

Isf (iron-sulfur flavoprotein) from Methanosarcina thermophila has been produced in Escherichia coli as a dimer containing two 4Fe-4S clusters and two FMN (flavin mononucleotide) cofactors. The deduced sequence of Isf contains six cysteines (Cys 16, Cys 47, Cys 50, Cys 53, Cys 59, and Cys 180), four of which (Cys 47, Cys 50, Cys 53, and Cys 59) comprise a motif with high identity to a motif (CX(2)CX(2)CX(4-7)C) present in all homologous Isf sequences available in the databases. The spacing of the motif is highly compact and atypical of motifs coordinating known 4Fe-4S clusters; therefore, all six cysteines in Isf from M. thermophila were altered to either alanine or serine to obtain corroborating biochemical evidence that the motif coordinates the 4Fe-4S cluster and to further characterize properties of the cluster dependent on ligation. All except the C16S variant were produced in inclusion bodies and were void of iron-sulfur clusters and FMN. Reconstitution of the iron-sulfur cluster and FMN was attempted for each variant. The UV-visible spectra of all reconstituted variants indicated the presence of iron-sulfur clusters and FMN. The reduced C16A/S variants showed the same electron paramagnetic resonance (EPR) spectra as wild-type Isf, whereas the reduced C180A/S variants showed EPR spectra identical to those of one of the two 4Fe-4S species present in the wild-type Isf spectrum. Conversely, EPR spectra of the oxidized C50A and C59A variants showed g values characteristic of a 3Fe-4S cluster. The spectra of the C47A and C53A variants indicated a 4Fe-4S cluster with g values and linewidths different from those for the wild type. The combined results of this study support a role for the novel CX(2)CX(2)CX(4-7)C motif in ligating the 4Fe-4S clusters in Isf and Isf homologues.

Prokaryotic carbonic anhydrases

Carbonic anhydrases catalyze the reversible hydration of CO(2) [CO(2)+H(2)Oright harpoon over left harpoon HCO(3)(-)+H(+)]. Since the discovery of this zinc (Zn) metalloenzyme in erythrocytes over 65 years ago, carbonic anhydrase has not only been found in virtually all mammalian tissues but is also abundant in plants and green unicellular algae. The enzyme is important to many eukaryotic physiological processes such as respiration, CO(2) transport and photosynthesis. Although ubiquitous in highly evolved organisms from the Eukarya domain, the enzyme has received scant attention in prokaryotes from the Bacteria and Archaea domains and has been purified from only five species since it was first identified in Neisseria sicca in 1963. Recent work has shown that carbonic anhydrase is widespread in metabolically diverse species from both the Archaea and Bacteria domains indicating that the enzyme has a more extensive and fundamental role in prokaryotic biology than previously recognized. A remarkable feature of carbonic anhydrase is the existence of three distinct classes (designated alpha, beta and gamma) that have no significant sequence identity and were invented independently. Thus, the carbonic anhydrase classes are excellent examples of convergent evolution of catalytic function. Genes encoding enzymes from all three classes have been identified in the prokaryotes with the beta and gamma classes predominating. All of the mammalian isozymes (including the 10 human isozymes) belong to the alpha class; however, only nine alpha class carbonic anhydrase genes have thus far been found in the Bacteria domain and none in the Archaea domain. The beta class is comprised of enzymes from the chloroplasts of both monocotyledonous and dicotyledonous plants as well as enzymes from phylogenetically diverse species from the Archaea and Bacteria domains. The only gamma class carbonic anhydrase that has thus far been isolated and characterized is from the methanoarchaeon Methanosarcina thermophila. Interestingly, many prokaryotes contain carbonic anhydrase genes from more than one class; some even contain genes from all three known classes. In addition, some prokaryotes contain multiple genes encoding carbonic anhydrases from the same class. The presence of multiple carbonic anhydrase genes within a species underscores the importance of this enzyme in prokaryotic physiology; however, the role(s) of this enzyme is still largely unknown. Even though most of the information known about the function(s) of carbonic anhydrase primarily relates to its role in cyanobacterial CO(2) fixation, the prokaryotic enzyme has also been shown to function in cyanate degradation and the survival of intracellular pathogens within their host. Investigations into prokaryotic carbonic anhydrase have already led to the identification of a new class (gamma) and future research will undoubtedly reveal novel functions for carbonic anhydrase in prokaryotes.

Prokaryotic carbonic anhydrases

Carbonic anhydrases catalyze the reversible hydration of CO(2) [CO(2)+H(2)Oright harpoon over left harpoon HCO(3)(-)+H(+)]. Since the discovery of this zinc (Zn) metalloenzyme in erythrocytes over 65 years ago, carbonic anhydrase has not only been found in virtually all mammalian tissues but is also abundant in plants and green unicellular algae. The enzyme is important to many eukaryotic physiological processes such as respiration, CO(2) transport and photosynthesis. Although ubiquitous in highly evolved organisms from the Eukarya domain, the enzyme has received scant attention in prokaryotes from the Bacteria and Archaea domains and has been purified from only five species since it was first identified in Neisseria sicca in 1963. Recent work has shown that carbonic anhydrase is widespread in metabolically diverse species from both the Archaea and Bacteria domains indicating that the enzyme has a more extensive and fundamental role in prokaryotic biology than previously recognized. A remarkable feature of carbonic anhydrase is the existence of three distinct classes (designated alpha, beta and gamma) that have no significant sequence identity and were invented independently. Thus, the carbonic anhydrase classes are excellent examples of convergent evolution of catalytic function. Genes encoding enzymes from all three classes have been identified in the prokaryotes with the beta and gamma classes predominating. All of the mammalian isozymes (including the 10 human isozymes) belong to the alpha class; however, only nine alpha class carbonic anhydrase genes have thus far been found in the Bacteria domain and none in the Archaea domain. The beta class is comprised of enzymes from the chloroplasts of both monocotyledonous and dicotyledonous plants as well as enzymes from phylogenetically diverse species from the Archaea and Bacteria domains. The only gamma class carbonic anhydrase that has thus far been isolated and characterized is from the methanoarchaeon Methanosarcina thermophila. Interestingly, many prokaryotes contain carbonic anhydrase genes from more than one class; some even contain genes from all three known classes. In addition, some prokaryotes contain multiple genes encoding carbonic anhydrases from the same class. The presence of multiple carbonic anhydrase genes within a species underscores the importance of this enzyme in prokaryotic physiology; however, the role(s) of this enzyme is still largely unknown. Even though most of the information known about the function(s) of carbonic anhydrase primarily relates to its role in cyanobacterial CO(2) fixation, the prokaryotic enzyme has also been shown to function in cyanate degradation and the survival of intracellular pathogens within their host. Investigations into prokaryotic carbonic anhydrase have already led to the identification of a new class (gamma) and future research will undoubtedly reveal novel functions for carbonic anhydrase in prokaryotes.

Cysteine biosynthesis in the Archaea: Methanosarcina thermophila utilizes O-acetylserine sulfhydrylase

Two pathways for cysteine biosynthesis are known in nature; however, it is not known which, if either, the Archaea utilize. Enzyme activities in extracts of Methanosarcina thermophila grown with combinations of cysteine and sulfide as sulfur sources indicated that this archaeon utilizes the pathway found in the Bacteria domain. The genes encoding serine transacetylase and O-acetylserine sulfhydrylase (cysE and cysK) are adjacent on the chromosome of M. thermophila and possibly form an operon. When M. thermophila is grown with cysteine as the sole sulfur source, O-acetylserine sulfhydrylase activity is maximally expressed suggesting alternative roles for this enzyme apart from cysteine biosynthesis.

A closer look at the active site of gamma-class carbonic anhydrases: high-resolution crystallographic studies of the carbonic anhydrase from Methanosarcina thermophila

The prototype of the gamma-class of carbonic anhydrase has been characterized from the methanogenic archaeon Methanosarcina thermophila. Previously reported kinetic studies of the gamma-class carbonic anhydrase are consistent with this enzyme having a reaction mechanism similar to that of the mammalian alpha-class carbonic anhydrase. However, the overall folds of these two enzymes are dissimilar, and apart from the zinc-coordinating histidines, the active site residues bear little resemblance to one another. The crystal structures of zinc-containing and cobalt-substituted gamma-class carbonic anhydrases from M. thermophila are reported here between 1.46 and 1.95 A resolution in the unbound form and cocrystallized with either SO(4)(2)(-) or HCO(3)(-). Relative to the tetrahedral coordination geometry seen at the active site in the alpha-class of carbonic anhydrases, the active site of the gamma-class enzyme contains additional metal-bound water ligands, so the overall coordination geometry is trigonal bipyramidal for the zinc-containing enzyme and octahedral for the cobalt-substituted enzyme. Ligands bound to the active site all make contacts with the side chain of Glu 62 in manners that suggest the side chain is likely protonated. In the uncomplexed zinc-containing enzyme, the side chains of Glu 62 and Glu 84 appear to share a proton; additionally, Glu 84 exhibits multiple conformations. This suggests that Glu 84 may act as a proton shuttle, which is an important aspect of the reaction mechanism of alpha-class carbonic anhydrases. A hydrophobic pocket on the surface of the enzyme may participate in the trapping of CO(2) at the active site. On the basis of the coordination geometry at the active site, ligand binding modes, the behavior of the side chains of Glu 62 and Glu 84, and analogies to the well-characterized alpha-class of carbonic anhydrases, a more-defined reaction mechanism is proposed for the gamma-class of carbonic anhydrases.

A structure-function study of a proton transport pathway in the gamma-class carbonic anhydrase from Methanosarcina thermophila

Four glutamate residues in the prototypic gamma-class carbonic anhydrase from Methanosarcina thermophila (Cam) were characterized by site-directed mutagenesis and chemical rescue studies. Alanine substitution indicated that an external loop residue, Glu 84, and an internal active site residue, Glu 62, are both important for CO(2) hydration activity. Two other external loop residues, Glu 88 and Glu 89, are less important for enzyme function. The two E84D and -H variants exhibited significant activity relative to wild-type activity in pH 7.5 MOPS buffer, suggesting that the original glutamate residue could be substituted with other ionizable residues with similar pK(a) values. The E84A, -C, -K, -Q, -S, and -Y variants exhibited large decreases in k(cat) values in pH 7.5 MOPS buffer, but only exhibited small changes in k(cat)/K(m). These same six variants were all chemically rescued by pH 7.5 imidazole buffer, with 23-46-fold increases in the apparent k(cat). These results are consistent with Glu 84 functioning as a proton shuttle residue. The E62D variant exhibited a 3-fold decrease in k(cat) and a 2-fold decrease in k(cat)/K(m) relative to those of the wild type in pH 7.5 MOPS buffer, while other substitutions (E62A, -C, -H, -Q, -T, and -Y) resulted in much larger decreases in both k(cat) and k(cat)/K(m). Imidazole did not significantly increase the k(cat) values and slightly decreased the k(cat)/K(m) values of most of the Glu 62 variants. These results indicate a primary preference for a carboxylate group at position 62, and support a proposed catalytic role for residue Glu 62 in the CO(2) hydration step, but do not definitively establish its role in the proton transport step.

Identification of essential arginines in the acetate kinase from Methanosarcina thermophila

Site-directed mutagenesis is a powerful tool for identifying active-site residues essential for catalysis; however, this approach has only recently become available for acetate kinase. The enzyme from Methanosarcina thermophila has been cloned and hyper-produced in a highly active form in Escherichia coli (recombinant wild-type). The role of arginines in this acetate kinase was investigated. Five arginines (R91, R175, R241, R285, and R340) in the M. thermophila enzyme were selected for individual replacement based on their high conservation among sequences of acetate kinase homologues. Replacement of R91 or R241 with alanine or leucine produced variants with specific activities less than 0.1% of the recombinant wild-type enzyme. The circular dichroism spectra and other properties of these variants were comparable to those of recombinant wild-type, indicating no global conformational changes. These results indicate that R91 and R241 are essential for activity, consistent with roles in catalysis. The variant produced by conservative replacement of R91 with lysine had approximately 2% of recombinant wild-type activity, suggesting a positive charge is important in this position. The K(m) value for acetate of the R91K variant increased greater than 10-fold relative to recombinant wild-type, suggesting an additional role for R91 in binding this substrate. Activities of both the R91A and R241A variants were rescued 20-fold when guanidine or derivatives were added to the reaction mixture. The K(m) values for ATP of the rescued variants were similar to those of recombinant wild-type, suggesting that the rescued activities are the consequence of replacement of important functional groups and not changes in the catalytic mechanism. These results further support roles for R91 and R241 in catalysis. Replacement of R285 with alanine, leucine, or lysine had no significant effect on activity; however, the K(m) values for acetate increased 6-10-fold, suggesting R285 influences the binding of this substrate. Phenylglyoxal inhibition and substrate protection experiments with the recombinant wild-type enzyme and variants were consistent with the presence of one or more essential arginine residues in the active site as well as with roles for R91 and R241 in catalysis. It is proposed that R91 and R241 function to stabilize the previously proposed pentacoordinate transition state during direct in-line transfer of the gamma-phosphate of ATP to acetate. The kinetic characterization of variants produced by replacement of R175 and R340 with alanine, leucine, or lysine indicated that these residues are not involved in catalysis but fulfill important structural roles.