Methanothermus Fervidus Research Articles

Structural characterization of a novel cyclic 2,3-diphosphoglycerate synthetase involved in extremolyte production in the archaeon Methanothermus fervidus.

The enzyme cyclic di-phosphoglycerate synthetase that is involved in the production of the osmolyte cyclic 2,3-diphosphoglycerate has been studied both biochemically and structurally. Cyclic 2,3-diphosphoglycerate is found exclusively in the hyperthermophilic archaeal methanogens, such as Methanothermus fervidus, Methanopyrus kandleri, and Methanothermobacter thermoautotrophicus. Its presence increases the thermostability of archaeal proteins and protects the DNA against oxidative damage caused by hydroxyl radicals. The cyclic 2,3-diphosphoglycerate synthetase enzyme has been crystallized and its structure solved to 1.7 Å resolution by experimental phasing. It has also been crystallized in complex with its substrate 2,3 diphosphoglycerate and the co-factor ADP and this structure has been solved to 2.2 Å resolution. The enzyme structure has two domains, the core domain shares some structural similarity with other NTP-dependent enzymes. A significant proportion of the structure, including a 127 amino acid N-terminal domain, has no structural similarity to other known enzyme structures. The structure of the complex shows a large conformational change that occurs in the enzyme during catalytic turnover. The reaction involves the transfer of the γ-phosphate group from ATP to the substrate 2,3 -diphosphoglycerate and the subsequent SN2 attack to form a phosphoanhydride. This results in the production of the unusual extremolyte cyclic 2,3 -diphosphoglycerate which has important industrial applications.

Specific DNA binding of archaeal histones HMfA and HMfB.

In archaea, histones play a role in genome compaction and are involved in transcription regulation. Whereas archaeal histones bind DNA without sequence specificity, they bind preferentially to DNA containing repeats of alternating A/T and G/C motifs. These motifs are also present on the artificial sequence "Clone20," a high-affinity model sequence for binding of the histones from Methanothermus fervidus. Here, we investigate the binding of HMfA and HMfB to Clone20 DNA. We show that specific binding at low protein concentrations (<30 nM) yields a modest level of DNA compaction, attributed to tetrameric nucleosome formation, whereas nonspecific binding strongly compacts DNA. We also demonstrate that histones impaired in hypernucleosome formation are still able to recognize the Clone20 sequence. Histone tetramers indeed exhibit a higher binding affinity for Clone20 than nonspecific DNA. Our results indicate that a high-affinity DNA sequence does not act as a nucleation site, but is bound by a tetramer which we propose is geometrically different from the hypernucleosome. Such a mode of histone binding might permit sequence-driven modulation of hypernucleosome size. These findings might be extrapolated to histone variants that do not form hypernucleosomes. Versatile binding modes of histones could provide a platform for functional interplay between genome compaction and transcription.

Production of the Extremolyte Cyclic 2,3-Diphosphoglycerate Using Thermus thermophilus as a Whole-Cell Factory

Osmolytes protect microbial cells against temperature, osmolarity and other stresses. The osmolyte cyclic 2,3-diphosphoglycerate, originally isolated from the thermophilic archaeon Methanothermus fervidus, naturally protects cellular proteins under extreme conditions. The biosynthetic pathway for cyclic 2,3-diphosphoglycerate has been introduced into the thermophilic bacterium Thermus thermophilus. The two enzymes in this synthetic pathway, 2-phosphoglycerate kinase and cyclic diphosphoglycerate synthetase, were incorporated into a newly designed modular BioBricks vector. The expression of this two-enzyme cascade resulted in the whole cell production of cyclic 2,3 diphosphoglycerate. In vivo production of cyclic 2,3-diphosphoglycerate was confirmed by mass spectrometry to a concentration up to 650 µM. This study demonstrates the feasibility of using this well studied thermophilic bacterium as a host in a whole-cell factory approach to produce cyclic 2,3 diphosphoglycerate. This raises the potential for commercialisation of cDPG for cosmetic and healthcare applications. Our work demonstrates the application of Thermus thermophilus as an alternative host for other high value small organic molecules of industrial interest.

Archaeal pseudomurein and bacterial murein cell wall biosynthesis share a common evolutionary ancestry.

Bacteria near-universally contain a cell wall sacculus of murein (peptidoglycan), the synthesis of which has been intensively studied for over 50 years. In striking contrast, archaeal species possess a variety of other cell wall types, none of them closely resembling murein. Interestingly though, one type of archaeal cell wall termed pseudomurein found in the methanogen orders Methanobacteriales and Methanopyrales is a structural analogue of murein in that it contains a glycan backbone that is cross-linked by a L-amino acid peptide. Here, we present taxonomic distribution, gene cluster and phylogenetic analyses that confirm orthologues of 13 bacterial murein biosynthesis enzymes in pseudomurein-containing methanogens, most of which are distantly related to their bacterial counterparts. We also present the first structure of an archaeal pseudomurein peptide ligase from Methanothermus fervidus DSM1088 (Mfer336) to a resolution of 2.5Å and show that it possesses a similar overall tertiary three domain structure to bacterial MurC and MurD type murein peptide ligases. Taken together the data strongly indicate that murein and pseudomurein biosynthetic pathways share a common evolutionary history.

Acidic Solutions to Archaeal Chromatin

Cells must organize their genomes to provide compact structure and coordinate genome regulation. Like eukaryotes, most known archaea also encode histones, albeit with shorter sequences (∼68 amino acids) that span only the three-helix motif without additional domains. Most studies of histone structure-function relationships in archaea have focused on hyperthermophiles, such as Thermococcus kodakorensis and Methanothermus fervidus, where histones have been observed to wrap DNA into long super-helical ramps, referred to as archaeasomes. On the other hand, how histones function in other archaea is not well understood, especially in species that encode histones that have acidic isoelectric points. Normally, such acidic proteins would not be thought to bind nucleic acids. However, these histones maintain a basic ridge that may facilitate DNA binding despite their global acidic character. Here, we utilize biophysical assays and computational models to explore how acidic archaeal histones bind DNA and structure chromatin. Understanding how these archaeal species utilize acidic histones is essential for mapping how pressures from extreme environments has driven histone evolution and diversification.

Molecular Logic of Prokaryotic Surface Layer Structures.

Most prokaryotic cells are encased in a surface layer (S-layer) consisting of a paracrystalline array of repeating lattice-forming proteins. S-layer proteins populate a vast and diverse sequence space, performing disparate functions in prokaryotic cells, including cellular defense, cell-shape maintenance, and regulation of import and export of materials. This article highlights recent advances in the understanding of S-layer structure and assembly, made possible by rapidly evolving structural and cell biology methods. We underscore shared assembly principles revealed by recent work and discuss a common molecular framework that may be used to understand the structural organization of S-layer proteins across bacteria and archaea.

Chromatinization of Escherichia coli with archaeal histones.

Nucleosomes restrict DNA accessibility throughout eukaryotic genomes, with repercussions for replication, transcription, and other DNA-templated processes. How this globally restrictive organization emerged during evolution remains poorly understood. Here, to better understand the challenges associated with establishing globally restrictive chromatin, we express histones in a naive system that has not evolved to deal with nucleosomal structures: Escherichia coli. We find that histone proteins from the archaeon Methanothermus fervidus assemble on the E. coli chromosome in vivo and protect DNA from micrococcal nuclease digestion, allowing us to map binding footprints genome-wide. We show that higher nucleosome occupancy at promoters is associated with lower transcript levels, consistent with local repressive effects. Surprisingly, however, this sudden enforced chromatinization has only mild repercussions for growth unless cells experience topological stress. Our results suggest that histones can become established as ubiquitous chromatin proteins without interfering critically with key DNA-templated processes.

MtrA of the sodium ion pumping methyltransferase binds cobalamin in a unique mode.

In the three domains of life, vitamin B12 (cobalamin) is primarily used in methyltransferase and isomerase reactions. The methyltransferase complex MtrA–H of methanogenic archaea has a key function in energy conservation by catalysing the methyl transfer from methyl-tetrahydromethanopterin to coenzyme M and its coupling with sodium-ion translocation. The cobalamin-binding subunit MtrA is not homologous to any known B12-binding proteins and is proposed as the motor of the sodium-ion pump. Here, we present crystal structures of the soluble domain of the membrane-associated MtrA from Methanocaldococcus jannaschii and the cytoplasmic MtrA homologue/cobalamin complex from Methanothermus fervidus. The MtrA fold corresponds to the Rossmann-type α/β fold, which is also found in many cobalamin-containing proteins. Surprisingly, the cobalamin-binding site of MtrA differed greatly from all the other cobalamin-binding sites. Nevertheless, the hydrogen-bond linkage at the lower axial-ligand site of cobalt was equivalently constructed to that found in other methyltransferases and mutases. A distinct polypeptide segment fixed through the hydrogen-bond linkage in the relaxed Co(III) state might be involved in propagating the energy released upon corrinoid demethylation to the sodium-translocation site by a conformational change.

Chemical Synthesis of Asparagine-Linked Archaeal N-Glycan fromMethanothermus fervidus

Several N-linked glycoproteins have been identified in archaea and there is growing evidence that the N-glycan is involved in survival and functioning of archaea in extreme conditions. Chemical synthesis of the archaeal N-glycans represents a crucial step towards understanding the putative function of protein glycosylation in archaea. Herein the first total synthesis of the archaeal L-asparagine linked hexasaccharide from Methanothermus fervidus is reported using a highly convergent [3+3] glycosylation approach in high overall yields. The synthesis relies on efficient preparation of regioselectively protected thioglycoside building blocks for orthogonal glycosylations and late stage N-aspartylation.

Application of Universal Stress Proteins in Probing the Dynamics of Potent Degraders in Complex Terephthalate Metagenome

The culture-independent strategies to study microbial diversity and function have led to a revolution in environmental genomics, enabling fundamental questions about the distribution of microbes and their influence on bioremediation to be addressed. In this research we used the expression of universal stress proteins as a probe to determine the changes in degrading microbial population from a highly toxic terephthalate wastewater to a less toxic activated sludge bioreactor. The impact of relative toxicities was significantly elaborated at the levels of genus and species. The results indicated that 23 similar prokaryotic phyla were represented in both metagenomes irrespective of their relative abundance. Furthermore, the following bacteria taxa Micromonosporaceae, Streptomyces, Cyanothece sp. PCC 7822, Alicyclobacillus acidocaldarius, Bacillus halodurans, Leuconostoc mesenteroides, Lactococcus garvieae, Brucellaceae, Ralstonia solanacearum, Verminephrobacter eiseniae, Azoarcus, Acidithiobacillus ferrooxidans, Francisella tularensis, Methanothermus fervidus, and Methanocorpusculum labreanum were represented only in the activated sludge bioreactor. These highly dynamic microbes could serve as taxonomic biomarkers for toxic thresholds related to terephthalate and its derivatives. This paper, highlights the application of universal stress proteins in metagenomics analysis. Dynamics of microbial consortium of this nature can have future in biotechnological applications in bioremediation of toxic chemicals and radionuclides.

Complete genome sequence of Methanothermus fervidus type strain (V24S).

Methanothermus fervidus Stetter 1982 is the type strain of the genus Methanothermus. This hyperthermophilic genus is of a thought to be endemic in Icelandic hot springs. M. fervidus was not only the first characterized organism with a maximal growth temperature (97°C) close to the boiling point of water, but also the first archaeon in which a detailed functional analysis of its histone protein was reported and the first one in which the function of 2,3-cyclodiphosphoglycerate in thermoadaptation was characterized. Strain V24ST is of interest because of its very low substrate ranges, it grows only on H2 + CO2. This is the first completed genome sequence of the family Methanothermaceae. Here we describe the features of this organism, together with the complete genome sequence and annotation. The 1,243,342 bp long genome with its 1,311 protein-coding and 50 RNA genes is a part of the Genomic Encyclopedia of Bacteria and Archaea project.

Formylmethanofuran: Tetrahydromethanopterin Formyltransferase (Ftr) from the Hyperthermophilic Methanopyrus kandleri

Methanopyrus kandleri is a methanogenic Archaeon that grows on H2 and CO2 at a temperature optimum of 98 °C. The gene ftr encoding the formylmethanofuran: tetrahydromethanopterin formyl-transferase, an enzyme involved in CO2 reduction to methane, has been cloned, sequenced, and overexpressed in Escherichia coli. The overproduced enzyme could be purified in yields above 90% by simply heating the cell extract to 90°C in 1.5 M K2HPO4 pH 8.0 for 30 min. From 1 g wet cells (70 mg protein) approximately 14 mg formyltransferase was obtained. The purified enzyme showed essentially the same catalytic properties as that purified from M. kandleri cells. The primary structure and properties of the formyltransferase are compared with those of the enzyme from Methanobacterium thermoautotrophicum (growth temperature optimum 65 °C) and Methanothermus fervidus (83 °C). Of the three enzymes that from M. kandleri had the lowest isoelectric point (4.2) and the lowest hydrophobicity of the amino acid composition. The enzyme from M. kandleri had the relatively highest content in alanine, glutamate and glutamine and the relatively lowest content in isoleucine, leucine and lysine. These properties, some of which are unusual for enzymes from other hyperthermophilic organisms, may reflect that the formyltransferase from M. kandleri is adapted to both hyperthermophilic and halophilic conditions.

Unique fluorophores in the dimeric archaeal histones hMfB and hPyA1 reveal the impact of nonnative structure in a monomeric kinetic intermediate

Homodimeric archaeal histones and heterodimeric eukaryotic histones share a conserved structure but fold through different kinetic mechanisms, with a correlation between faster folding/association rates and the population of kinetic intermediates. Wild-type hMfB (from Methanothermus fervidus) has no intrinsic fluorophores; Met35, which is Tyr in hyperthermophilic archaeal histones such as hPyA1 (from Pyrococcus strain GB-3A), was mutated to Tyr and Trp. Two Tyr-to-Trp mutants of hPyA1 were also characterized. All fluorophores were introduced into the long, central alpha-helix of the histone fold. Far-UV circular dichroism (CD) indicated that the fluorophores did not significantly alter the helical content of the histones. The equilibrium unfolding transitions of the histone variants were two-state, reversible processes, with DeltaG degrees (H2O) values within 1 kcal/mol of the wild-type dimers. The hPyA1 Trp variants fold by two-state kinetic mechanisms like wild-type hPyA1, but with increased folding and unfolding rates, suggesting that the mutated residues (Tyr-32 and Tyr-36) contribute to transition state structure. Like wild-type hMfB, M35Y and M35W hMfB fold by a three-state mechanism, with a stopped-flow CD burst-phase monomeric intermediate. The M35 mutants populate monomeric intermediates with increased secondary structure and stability but exhibit decreased folding rates; this suggests that nonnative interactions occur from burial of the hydrophobic Tyr and Trp residues in this kinetic intermediate. These results implicate the long central helix as a key component of the structure in the kinetic monomeric intermediates of hMfB as well as the dimerization transition state in the folding of hPyA1.

Using archaeal histones for precise DNA fragmentation

The fragmentation of DNA is a useful procedure for many molecular biology procedures. However, most methods used to fragment DNA are poorly controllable, and cannot be used to create small fragments. We describe a method to generate random DNA fragments of a predictable size to be cloned in expression vectors for the construction of display libraries. The DNA is allowed to form complexes with archaeal histones from Methanothermus fervidus (HMf) and the HMf/DNA core complex is naturally protected from nuclease DNaseI activity, giving rise to DNA fragments of approximately 60 bp and multiples thereof. We found that by varying the wt/wt ratio between DNA and HMf, the concentration of DNA and the incubation time with DNaseI, DNA fragments of desired size can be obtained. This approach should be applicable to the efficient fragmentation of DNA for the construction of phage display polypeptide libraries, as well as any other molecular biology procedures in which small DNA fragments of defined size are required.

Obligate Heterodimerization of the Archaeal Alba2 Protein with Alba1 Provides a Mechanism for Control of DNA Packaging

Organisms growing at elevated temperatures face a particular challenge to maintain the integrity of their genetic material. All thermophilic and hyperthermophilic archaea encode one or more copies of the Alba (Sac10b) gene. Alba is an abundant, dimeric, highly basic protein that binds cooperatively and at high density to DNA. Sulfolobus solfataricus encodes a second copy of the Alba gene, and the Alba2 protein is expressed at approximately 5% of the level of Alba1. We demonstrate by NMR, ITC, and crystallography that Alba2 exists exclusively as a heterodimer with Alba1 at physiological concentrations and that heterodimerization exerts a clear effect upon the DNA packaging, as observed by EM, potentially by changing the interface between adjacent Alba dimers in DNA complexes. A functional role for Alba2 in modulation of higher order chromatin structure and DNA condensation is suggested.

Stability and folding mechanism of mesophilic, thermophilic and hyperthermophilic archael histones: the importance of folding intermediates.

The equilibrium stabilities to guanidinium chloride (GdmCl)-induced denaturation and kinetic folding mechanisms have been characterized for three archael histones: hFoB from the mesophile Methanobacterium formicicum; hMfB from the thermophile Methanothermus fervidus; and hPyA1 from the hyperthermophile Pyrococcus strain GB-3a. These histones are homodimers of 67 to 69 residues per monomer. The equilibrium unfolding transitions, as measured by far-UV circular dichroism (CD) are highly reversible, two-state processes. The mesophilic hFoB is very unstable and requires approximately 1 M trimethyl-amine-N-oxide (TMAO) to completely populate the native state. The thermophilic histones are more stable, with deltaG degrees (H2O) values of 14 and 16 kcal mol(-1) for hMfB and hPyA1, respectively. The kinetic folding of hFoB and hPyA1 are two-state processes, with no detectable transient kinetic intermediates. For hMfB, there is significant development of CD signal in the stopped-flow dead time, indicative of the formation of a monomeric intermediate, which then folds/associates in a single, second-order step to form the native dimer. While the equilibrium stability to chemical denaturation correlates very well with host growth temperature, there is no simple relationship between folding rates and stability for the archael histones. In the absence of denaturant, the log of the unfolding rates correlate with equilibrium stability. The folding/association of the moderately stable hMfB is the most rapid, with a rate constant in the absence of GdmCl of 3 x 10(6) M(-1) s(-1), compared to 9 x 10(5) M(-1) s(-1) for the more stable hPyA1. It appears that the formation of the hMfB burst-phase monomeric ensemble serves to enhance folding efficiency, rather than act as a kinetic trap. The folding mechanism of the archael histones is compared to the folding of other intertwined, segment-swapped, alpha-helical, DNA-binding dimers (ISSADD), including the eukaryotic heterodimeric histones, which fold more rapidly. The importance of monomeric and dimeric kinetic intermediates in accelerating ISSADD folding reactions is discussed.

Hyperthermophilic dehydrogenase enzymes.

Archaeal dehydrogenases are often found to be of a specific class of dehydrogenase which has low sequence identity to the equivalent bacterial and eukaryotic counterparts. This paper focuses on two different types of hyperthermophilic dehydrogenase enzyme that have been cloned and over-expressed in Escherichia coli. The crystallographic structures of the apo form of GAPDH (glyceraldehyde-3-phosphate dehydrogenase) from Sulfolobus solfataricus and the related holo form of GAPDH from Methanothermus fervidus have been solved to high resolution. The zinc-containing structure of ADH (alcohol dehydrogenase) from Aeropyrum pernix has also been solved as a quaternary complex with the cofactor NADH and the inhibitor octanoic acid. The results show that despite the low sequence identity to the related enzymes found in other organisms the fold of the protein chain is similar. The archaeal GAPDH enzymes show a relocation of the active site which is a feature of evolutionary interest. The high thermostability of these three archaeal dehydrogenases can be attributed to a combination of factors including an increase in the number of salt bridges and hydrophobic interactions, a higher percentage of secondary structure and the presence of disulphide bonds.

Archaeal Histone Tetramerization Determines DNA Affinity and the Direction of DNA Supercoiling

DNA binding and the topology of DNA have been determined in complexes formed by >20 archaeal histone variants and archaeal histone dimer fusions with residue replacements at sites responsible for histone fold dimer:dimer interactions. Almost all of these variants have decreased affinity for DNA. They have also lost the flexibility of the wild type archaeal histones to wrap DNA into a negative or positive supercoil depending on the salt environment; they wrap DNA into positive supercoils under all salt conditions. The histone folds of the archaeal histones, HMfA and HMfB, from Methanothermus fervidus are almost identical, but (HMfA)(2) and (HMfB)(2) homodimers assemble into tetramers with sequence-dependent differences in DNA affinity. By construction and mutagenesis of HMfA+HMfB and HMfB+HMfA histone dimer fusions, the structure formed at the histone dimer:dimer interface within an archaeal histone tetramer has been shown to determine this difference in DNA affinity. Therefore, by regulating the assembly of different archaeal histone dimers into tetramers that have different sequence affinities, the assembly of archaeal histone-DNA complexes could be localized and used to regulate gene expression.

Phospholipid etherlipid and phospholipid fatty acid fingerprints in selected euryarchaeotal monocultures for taxonomic profiling

Phospholipid etherlipid (PLEL) derived isoprenoids and phospholipid fatty acids (PLFA) were determined in eight Euryarchaeotal monocultures for taxonomic profiling. For the first time significant amounts of fatty acids in the PLFA of Euryarchaeota were determined. The PLFA proportion varied between 11.3 and 35.5% of the total phospholipid side chains except in Methanothermus fervidus where PLFA accounted for 89.0% of the total phospholipid side chains. Fractionation of fatty acids prior to gas chromatography mass spectrometry analysis revealed that non-ester-linked fatty acids dominated which accounted for 85.5–95.2% of total PLFA in all investigated archaeal strains. PLEL concentration and composition was estimated in accordance with previous studies with two exceptions. In the polar (phospho)lipid fraction of Methanopyrus kandleri side chains possibly derived from hydroxyarchaeol as well as acyclic and cyclic caldarchaeol were identified. In phospholipid extracts of Methanothermus fervidus the ‘H-formed’ caldarchaeol could not be detected. Overall, PLEL derived isoprenoids as well as PLFA enabled taxonomic differentiation of the selected microorganisms into phylogenetically related groups.

Phospholipid etherlipid and phospholipid fatty acid fingerprints in selected euryarchaeotal monocultures for taxonomic profiling.

Phospholipid etherlipid (PLEL) derived isoprenoids and phospholipid fatty acids (PLFA) were determined in eight Euryarchaeotal monocultures for taxonomic profiling. For the first time significant amounts of fatty acids in the PLFA of Euryarchaeota were determined. The PLFA proportion varied between 11.3 and 35.5% of the total phospholipid side chains except in Methanothermus fervidus where PLFA accounted for 89.0% of the total phospholipid side chains. Fractionation of fatty acids prior to gas chromatography mass spectrometry analysis revealed that non-ester-linked fatty acids dominated which accounted for 85.5-95.2% of total PLFA in all investigated archaeal strains. PLEL concentration and composition was estimated in accordance with previous studies with two exceptions. In the polar (phospho)lipid fraction of Methanopyrus kandleri side chains possibly derived from hydroxyarchaeol as well as acyclic and cyclic caldarchaeol were identified. In phospholipid extracts of Methanothermus fervidus the 'H-formed' caldarchaeol could not be detected. Overall, PLEL derived isoprenoids as well as PLFA enabled taxonomic differentiation of the selected microorganisms into phylogenetically related groups.