Ultrastructure and biochemistry of Methanococcus voltae.
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Purified flagellar filaments isolated from six methanogens were composed of multiple flagellins. Two flagellins were present in Methanococcus deltae (Mr = 34,000 and 32,000), Methanoculleus marisnigri (Mr = 31,000 and 25,500) and Methanococcus jannaschii (Mr = 31,000 and 27,500), three in Methanothermus fervidus (Mr = 34,000, 25,000 and 24,000) and four or more in both Methanococcus vannielii and Methanococcus maripaludis (Mr ranging from 27,500 to 32,000). The flagellins of M. fervidus and M. deltae reacted positively with glycoprotein-specific stains. The flagellins of M. deltae, M. maripaludis and M. vannielii were closely related to those of M. voltae based on cross-reactivity with antisera raised against M. voltae flagellins and homology with flagellin-specific oligonucleotide probes to the N-terminus and leader peptide of M. voltae flagellins. Similarities appear to exist among the flagellins of M. fervidus, M. marisnigri and Halobacterium halobium based on cross-reactivity with antisera produced against the flagella of Methanospirillum hungatei JF1. The N-termini of the flagellins from the mesophilic Methanococcus spp. and M. marisnigri show homology with the N-termini of other archaebacterial flagellins. These N-termini may undergo a modification involving removal of a leader peptide.
Post-transcriptional modifications in archaeal RNA are known to be phylogenetically distinct but relatively little is known of tRNA from the Methanococci, a lineage of methanogenic marine euryarchaea that grow over an unusually broad temperature range. Transfer RNAs from Methanococcus vannielii, Methanococcus maripaludis, the thermophile Methanococcus thermolithotrophicus, and hyperthermophiles Methanococcus jannaschii and Methanococcus igneus were studied to determine whether modification patterns reflect the close phylogenetic relationships inferred from small ribosomal subunit RNA sequences, and to examine modification differences associated with temperature of growth. Twenty-four modified nucleosides were characterized, including the complex tricyclic nucleoside wyosine characteristic of position 37 in tRNA(Phe) and known previously only in eukarya, plus two new wye family members of presently unknown structure. The hypermodified nucleoside 5-methylaminomethyl-2-thiouridine, reported previously only in bacterial tRNA at the first position of the anticodon, was identified by liquid chromatography-electrospray ionization mass spectrometry in four of the five organisms. The ribose-methylated nucleosides, 2'-O-methyladenosine, N(2),2'-O-dimethylguanosine and N(2),N(2),2'-O-trimethylguanosine, were found only in hyperthermophile tRNA, consistent with their proposed roles in thermal stabilization of tRNA.
Asymmetrical patterns of amino acid substitution in proteins of organisms living at moderate and high temperatures (mesophiles and thermophiles, respectively) are generally taken to indicate selection favoring different amino acids at different temperatures due to their biochemical properties. If that were the case, comparisons of different pairs of mesophilic and thermophilic taxa would exhibit similar patterns of substitutional asymmetry. A previous comparison of mesophilic versus thermophilic Methanococcus with mesophilic versus thermophilic Bacillus revealed several pairs of amino acids for which one amino acid was favored in thermophilic Bacillus and the other was favored in thermophilic Methanococcus. Most of this could be explained by the higher G+C content of the DNA of thermophilic Bacillus, a phenomenon not seen in the Methanococcus comparison. Here, I compared the mesophilic bacterium Deinococcus radiodurans and its thermophilic relative Thermus thermophilus, which are similar in G+C content. Of the 190 pairs of amino acids, 83 exhibited significant substitutional asymmetry, consistent with the pervasive effects of selection. Most of these significantly asymmetrical pairs of amino acids were asymmetrical in the direction predicted from the Methanococcus data, consistent with thermal adaptation resulting from universal biochemical properties of the amino acids. However, 12 pairs of amino acids exhibited asymmetry significantly different from and in the opposite direction of that found in the Methanococcus comparison, and 21 pairs of amino acids exhibited asymmetry that was significantly different from that found in the Bacillus comparison and could not be explained by the greater G+C content in thermophilic Bacillus. This suggests that selection due to universal biochemical properties of the amino acids and differences in G+C content are not the only causes of substitutional asymmetry between mesophiles and thermophiles. Instead, selection on taxon-specific properties of amino acids, such as their metabolic cost, may play a role in causing asymmetrical patterns of substitution.
A variety of sulfur-containing compounds were investigated for use as medium reductants and sulfur sources for growth of four methanogenic bacteria. Sulfide (1 to 2 mM) served all methanogens investigated well. Methanococcus thermolithotrophicus and Methanobacterium thermoautotrophicum Marburg and delta H grew well with S0, SO3(2-), or thiosulfate as the sole sulfur source. Only Methanococcus thermolithotrophicus was able to grow with SO4(2-) as the sole sulfur source. 2-Mercaptoethanol at 20 mM was greatly inhibitory to growth of Methanococcus thermolithotrophicus on SO4(2-) or SO2(2-) and Methanobacterium thermoautotrophicum Marburg on SO3(2-) but not to growth of strain delta H on SO3(2-). Sulfite was metabolized during growth by Methanococcus thermolithotrophicus. Sulfide was produced in cultures of Methanococcus thermolithotrophicus growing on SO4(2-), SO3(2-), thiosulfate, and S0. Methanobacterium thermoautotrophicum Marburg was successfully grown in a 10-liter fermentor with S0, SO3(2-), or thiosulfate as the sole sulfur source.
The unusual compound beta-aminoglutaric acid (beta-glutamate) has been identified by 13C nuclear magnetic resonance spectroscopy in soluble extracts of marine methanogenic bacteria. We examined several methanogen species representing nine genera and found that beta-glutamate occurred in methanococci and two methanogenium strains (Methanogenium cariaci JR1 and "Methanogenium anulus" AN9). The presence of this compound in the methanococci examined was further restricted to thermophilic members of the genus Methanococcus, including Methanococcus thermolithotrophicus strains, Methanococcus jannaschii, and "Methanococcus igneus." The two Methanogenium strains examined were mesophiles. Studies using Methanococcus thermolithotrophicus showed that levels of beta-glutamate in cells of that species were not affected by variation in growth temperature (40 to 65 degrees C), NH4+ (2 to 80 mM), Mg2+ (10 to 50 mM), or K+ (2 to 10 mM) in the medium. In contrast, soluble pools of beta-glutamate and L-alpha-glutamate (the other major free amino acid in all the methanococci) were proportional to NaCl levels in the growth medium. This dependence of beta-glutamate and L-alpha-glutamate concentrations on salt levels in the medium suggests that they function as osmolytes in these cells.
16S rDNAs amplified by PCR from 22 hyperthermophilic methanococci isolated from deep-sea hydrothermal vents were compared with those of the six type strains of the genus Methanococcus by RFLP analysis. Restriction fragments obtained with Haelli enabied four of the type species to be distinguished. Restrictions with HhaI, BstUI and MspI were necessary to differentiate Methanococcus jannaschii and Methanococcus fervens. The results indicate that the 16S rDNA PCR-RFLP method provides a rapid and reliable tool for the identification of newly isolated hyperthermophilic Methanococcus spp.
Archaeal flagella are unique motility structures, and the absence of bacterial structural motility genes in the complete genome sequences of flagellated archaeal species suggests that archaeal flagellar biogenesis is likely mediated by novel components. In this study, a conserved flagellar gene family from each of Methanococcus voltae, Methanococcus maripaludis, Methanococcus thermolithotrophicus, and Methanococcus jannaschii has been characterized. These species possess multiple flagellin genes followed immediately by eight known and supposed flagellar accessory genes, flaCDEFGHIJ. Sequence analyses identified a conserved Walker box A motif in the putative nucleotide binding proteins FlaH and FlaI that may be involved in energy production for flagellin secretion or assembly. Northern blotting studies demonstrated that all the species have abundant polycistronic mRNAs corresponding to some of the structural flagellin genes, and in some cases several flagellar accessory genes were shown to be cotranscribed with the flagellin genes. Cloned flagellar accessory genes of M. voltae were successfully overexpressed as His-tagged proteins in Escherichia coli. These recombinant flagellar accessory proteins were affinity purified and used as antigens to raise polyclonal antibodies for localization studies. Immunoblotting of fractionated M. voltae cells demonstrated that FlaC, FlaD, FlaE, FlaH, and FlaI are all present in the cell as membrane-associated proteins but are not major components of isolated flagellar filaments. Interestingly, flaD was found to encode two proteins, each translated from a separate ribosome binding site. These protein expression data indicate for the first time that the putative flagellar accessory genes of M. voltae, and likely those of other archaeal species, do encode proteins that can be detected in the cell.
Archaea possess a broader range of cell envelope structural formats than eubacteria and their cell walls do not contain peptidoglycan. Some archaea have only a single S-layer as their cell wall (e.g. Methanococcus jannaschii and Sulfolobus acidocaldarius), whereas others have multiple layers (e.g. Methanospirillum hungatei). Sometimes there can also be a high proportion of tetraether lipids in membranes to make the envelope more resilient to environmental stress (e.g. Methanococcus jannaschii and Sulfolobus acidocaldarius grown at 70 degrees C). Since the Gram reaction depends on both the structural format and the chemical composition of the cell envelope of eubacteria, it was important to determine if the same is true for archaea. Methanospirillum hungatei, Methanosarcina mazei, Methanobacterium formicicum, Methanococcus jannaschii and Sulfolobus acidocaldarius, chosen because of their different envelope formats and chemistries, were subjected to a Gram stain that can be used for transmission electron microscopy. In this staining regimen, the iodine is replaced by potassium trichloro(eta 2-ethylene)platinate(II) as the mordant, and the platinum of the new compound is the electron-scattering agent for electron microscopy. Of all these archaea, only Methanobacterium formicicum stained Gram-positive since its pseudomurein wall remained intact; the platinum compound formed large electron-dense aggregates with the crystal violet that were located in the vicinity of the cell wall and the plasma membrane. All but the terminal filament cells of Methanospirillum hungatei stained Gram-negative because the limiting porosity of its external sheath was so small that the Gram reagents could not enter the cells. The terminal cells of filaments stained Gram-positive because the staining reagents gained entry through the terminal plugs. All other archaea stained Gram-negative because their cell walls were so disrupted during staining that the crystal violet-platinum complex could not be retained by the cells. Methanococcus jannaschii was grown at both 50 degrees C and 70 degrees C so that the tetraether lipids in its plasma membrane could be increased from 20% (50 degrees C) to 45% (70 degrees C) of the total lipids; in both cases the cells stained Gram-negative.
We describe the stabilization by pressure of enzymes, including a hydrogenase from Methanococcus jannaschii, an extremely thermophilic deep-sea methanogen. This is the first published report of proteins from thermophiles being stabilized by pressure. Inactivation studies of partially purified hydrogenases from an extreme thermophile (Methanococcus igneus), a moderate thermophile (Methanococcus thermolithotrophicus), and a mesophile (Methanococcus maripaludis), all from shallow marine sites, show that pressure stabilization is not unique to enzymes isolated from high-pressure environments. These studies suggest that pressure stabilization of an enzyme may be related to its thermophilicity. Further experiments comparing the effects of increased pressure on the stability of alpha-glucosidases from the hyperthermophile Pyrococcus furiosus and Saccharomyces cerevisiae support this possibility. We have also examined pressure effects on several highly homologous glyceraldehyde-3-phosphate dehydrogenases from mesophilic and thermophilic sources and a rubredoxin from P. furiosus. The results suggest that hydrophobic interactions, which have been implicated in the stabilization of many thermophilic proteins, contribute to the pressure stabilization of enzymes from thermophiles.
Adenylate kinase has been isolated from four related methanogenic members of the Archaea. For each, the optimum temperature for enzyme activity was similar to the temperature for optimal microbial growth and was approximately 30 degrees C for Methanococcus voltae, 70 degrees C for Methanococcus thermolithotrophicus, 80 degrees C for Methanococcus igneus, and 80 to 90 degrees C for Methanococcus jannaschii. The enzymes were sensitive to the adenylate kinase inhibitor P1, P5-di(adenosine-5')pentaphosphate, a property that was exploited to purify the enzymes by CIBACRON Blue affinity chromatography. The enzymes had an estimated molecular mass (approximately 23 to 25 kDa) in the range common for adenylate kinases. Each of the enzymes had a region of amino acid sequence close to its N terminus that was similar to the canonical P-loop sequence reported for all adenylate kinases. However, the methanogen sequences lacked a lysine residue that has previously been found to be invariant in adenylate kinases, including an enzyme isolated from the archaeon Sulfolobus acidocaldarius. If verified as a nucleotide-binding domain, the methanogen sequence would represent a novel nucleotide-binding motif. There was no correlation between amino acid abundance and the optimal temperature for enzyme activity.
Cells of methanococci are covered by a single layer of protein subunits (S-layer) in hexagonal arrangement, which are directly exposed to the environment and which cannot be stabilized by cellular components. We have isolated S-layer proteins from cells of Methanococcus vannielii ( T(opt.)=37 degrees C), Methanococcus thermolithotrophicus ( T(opt.)=65 degrees C), and Methanococcus jannaschii ( T(opt.)=85 degrees C). The primary structure of the S-layer proteins was determined by sequencing the corresponding genes. According to the predicted amino acid sequence, the molecular masses of the S-layer proteins of the different methanococci are in a small range between 59,064 and 60,547 Da. Compared with its mesophilic counterparts, it is worth noting that in the S-layer protein of the extreme thermophile Mc. jannaschii the acidic amino acid Asp is predominant, the basic amino acid Lys occurs in higher amounts, and Cys and His are only present in this organism. Despite the differences in the growth optima and the predominance of some amino acids, the comparative total primary structure revealed a relatively high degree of identity (38%-45%) between the methanococci investigated. This observation indicates that the amino acid sequence of the S-layer proteins is significantly conserved from the mesophilic to the extremely thermophilic methanococci.
In Bacteria and Archaea (formerly Archaebacteria) ribosomal protein L1 has a dual function, as a primary rRNA-binding protein and as a translational repressor which binds to its own mRNA. The L1-binding site on the mRNA exhibits high similarity in both sequence and secondary structure to the binding site for L1 on the 23 S rRNA. A sensitive membrane-filter-binding assay has been used to examine the interactions between ribosomal L1 proteins from different archaeal and bacterial species, and 23S rRNA and mRNA fragments from Methanococcus vannielii containing the MvaL1-binding site. Under standard conditions (0 degrees C, pH 7.5, 20 mM Mg2+, 500 mM KCl), the apparent dissociation constant Kd of the homologous MvaL1-23S rRNA complex is 5 nM, the apparent dissociation constant Kd of the MvaL1-mRNA complex is 0.15 degrees M. L1 proteins from Escherichia coli (EcoL1) and from the thermophilic Bacterium Thermus thermophilus (TthL1), and from the thermophilic Archaea Methanococcus thermolithotrophicus (MthL1), Methanococcus jannaschii (MjaL1), and Sulfolobus solfataricus (SsoL1) were tested for their affinity to the specific L1-binding sites on the 23 S rRNA and mRNA. In general, the affinity of L1 proteins from thermophilic species to the binding sites on both 23 S rRNA and mRNA is about one order of magnitude higher than that of their mesophilic counterparts. This stronger protein-RNA interaction might make a substantial contribution to the thermal tolerance of ribosomes in thermophilic organisms.
A methanogenic bacterial consortium was obtained after inoculation of benzoate medium under N2/CO2 atmosphere with intertidal sediment. A hydrogen donating organotroph and Methanococcus mazei were isolated from this enrichment. H2-utilising sulphate reducing bacteria were isolated under H2/CO2 in the absence of organic electron donors. The Methanococcus was able to produce methane in yeast extract medium under N2/CO2 if the H2 donating organism was present, and sulphate reduction occurred if the hydrogen utilising sulphate reducing bacteria were grown with the H2 donating organism. The ability of the H2 utilising sulphate reducing bacteria to inhibit Methanococcus competitively was shown in clutures containing both of these H2 utilising bacteria.
The flagellins of Methanospirillum hungatei strains JF1 and GP1, Methanococcus deltae, and Methanothermus fervidus are glycosylated. Isolated flagellar filaments from these organisms are dissociated by low concentrations (0.5% (v/v)) of Triton X-100. Flagellar filaments from other methanogens (Methanococcus voltae, Methanococcus vannielii and Methanoculleus marisnigri) composed of non-glycosylated flagellins are resistant to Triton X-100 treatment. Consequently, the isolation techniques (employing Triton X-100) used to isolate basal body-hook-filament complexes in eubacteria may not be applicable to many methanogens.
Analyses of complete genomes indicate that a massive prokaryotic gene transfer (or transfers) preceded the formation of the eukaryotic cell. In comparisons of the entire set of Methanococcus jannaschii genes with their orthologs from Escherichia coli, Synechocystis 6803, and the yeast Saccharomyces cerevisiae, it is shown that prokaryotic genomes consist of two different groups of genes. The deeper, diverging informational lineage codes for genes which function in translation, transcription, and replication, and also includes GTPases, vacuolar ATPase homologs, and most tRNA synthetases. The more recently diverging operational lineage codes for amino acid synthesis, the biosynthesis of cofactors, the cell envelope, energy metabolism, intermediary metabolism, fatty acid and phospholipid biosynthesis, nucleotide biosynthesis, and regulatory functions. In eukaryotes, the informational genes are most closely related to those of Methanococcus, whereas the majority of operational genes are most closely related to those of Escherichia, but some are closest to Methanococcus or to Synechocystis.
By comparing the gene order in the completely sequenced archaeal genomes complemented by sequence profile analysis, we predict the existence and protein composition of the archaeal counterpart of the eukaryotic exosome, a complex of RNAses, RNA-binding proteins, and helicases that mediates processing and 3'->5' degradation of a variety of RNA species. The majority of the predicted archaeal exosome subunits are encoded in what appears to be a previously undetected superoperon. In Methanobacterium thermoautotrophicum, this predicted superoperon consists of 15 genes; in the Crenarchaea, Sulfolobus solfataricus and Aeropyrum pernix, one and two of the genes from the superoperon, respectively, are relocated in the genome, whereas in other Euryarchaeota, the superoperon is split into a variable number of predicted operons and solitary genes. Methanococcus jannaschii partially retains the superoperon, but lacks the three core exosome subunits, and in Halobacterium sp., the superoperon is divided into two predicted operons, with the same three exosome subunits missing. This suggests concerted gene loss and an alteration of the structure and function of the predicted exosome in the Methanococcus and Halobacterium lineages. Additional potential components of the exosome are encoded by partially conserved predicted small operons. Along with the orthologs of eukaryotic exosome subunits, namely an RNase PH and two RNA-binding proteins, the predicted archaeal exosomal superoperon also encodes orthologs of two protein subunits of RNase P. This suggests a functional and possibly a physical interaction between RNase P and the postulated archaeal exosome, a connection that has not been reported in eukaryotes. In a pattern of apparent gene loss complementary to that seen in Methanococcus and Halobacterium, Thermoplasma acidophilum lacks the RNase P subunits. Unexpectedly, the identified exosomal superoperon, in addition to the predicted exosome components, encodes the catalytic subunits of the archaeal proteasome, two ribosomal proteins and a DNA-directed RNA polymerase subunit. These observations suggest that in archaea, a tight functional coupling exists between translation, RNA processing and degradation, (apparently mediated by the predicted exosome) and protein degradation (mediated by the proteasome), and may have implications for cross-talk between these processes in eukaryotes.