Shifts in methanogenic archaea communities and methane dynamics along a subtropical estuarine land use gradient

In coastal aquatic ecosystems, prokaryotic communities play an important role in regulating the cycling of nutrients and greenhouse gases. In the coastal zone, estuaries are complex and delicately balanced systems containing a multitude of specific ecological niches for resident microbes. Anthropogenic influences (i.e. urban, industrial and agricultural land uses) along the estuarine continuum can invoke physical and biochemical changes that impact these niches. In this study, we investigate the relative abundance of methanogenic archaea and other prokaryotic communities, distributed along a land use gradient in the subtropical Burnett River Estuary, situated within the Great Barrier Reef catchment, Australia. Microbiological assemblages were compared to physicochemical, nutrient and greenhouse gas distributions in both pore and surface water. Pore water samples from within the most urbanised site showed a high relative abundance of methanogenic Euryarchaeota (7.8% of all detected prokaryotes), which coincided with elevated methane concentrations in the water column, ranging from 0.51 to 0.68 μM at the urban and sewage treatment plant (STP) sites, respectively. These sites also featured elevated dissolved organic carbon (DOC) concentrations (0.66 to 1.16 mM), potentially fuelling methanogenesis. At the upstream freshwater site, both methane and DOC concentrations were considerably higher (2.68 μM and 1.8 mM respectively) than at the estuarine sites (0.02 to 0.66 μM and 0.39 to 1.16 mM respectively) and corresponded to the highest relative abundance of methanotrophic bacteria. The proportion of sulfate reducing bacteria in the prokaryotic community was elevated within the urban and STP sites (relative abundances of 8.0%– 10.5%), consistent with electron acceptors with higher redox potentials (e.g. O₂, NO₃^-) being scarce. Overall, this study showed that ecological niches in anthropogenically altered environments appear to give an advantage to specialized prokaryotes invoking a potential change in the thermodynamic landscape of the ecosystem and in turn facilitating the generation of methane–a potent greenhouse gas.

Identification of the enzyme responsible for N1-methylation of pseudouridine 54 in archaeal tRNAs

tRNAs from all three kingdoms of life contain a variety of modified nucleotides required for their stability, proper folding, and accurate decoding. One prominent example is the eponymous ribothymidine (rT) modification at position 54 in the T-arm of eukaryotic and bacterial tRNAs. In contrast, in most archaea this position is occupied by another hypermodified nucleotide: the isosteric N1-methylated pseudouridine. While the enzyme catalyzing pseudouridine formation at this position is known, the pseudouridine N1-specific methyltransferase responsible for this modification has not yet been experimentally identified. Here, we present biochemical and genetic evidence that the two homologous proteins, Mja_1640 (COG 1901, Pfam DUF358) and Hvo_1989 (Pfam DUF358) from Methanocaldococcus jannaschii and Haloferax volcanii, respectively, are representatives of the methyltransferase responsible for this modification. However, the in-frame deletion of the pseudouridine N1-methyltransferase gene in H. volcanii did not result in a discernable phenotype in line with similar observations for knockouts of other T-arm methylating enzymes.

The archaeal COG1901/DUF358 SPOUT-methyltransferase members, together with pseudouridine synthase Pus10, catalyze the formation of 1-methylpseudouridine at position 54 of tRNA

The methylation of pseudouridine (Ψ) at position 54 of tRNA, producing m(1)Ψ, is a hallmark of many archaeal species, but the specific methylase involved in the formation of this modification had yet to be characterized. A comparative genomics analysis had previously identified COG1901 (DUF358), part of the SPOUT superfamily, as a candidate for this missing methylase family. To test this prediction, the COG1901 encoding gene, HVO_1989, was deleted from the Haloferax volcanii genome. Analyses of modified base contents indicated that while m(1)Ψ was present in tRNA extracted from the wild-type strain, it was absent from tRNA extracted from the mutant strain. Expression of the gene encoding COG1901 from Halobacterium sp. NRC-1, VNG1980C, complemented the m(1)Ψ minus phenotype of the ΔHVO_1989 strain. This in vivo validation was extended with in vitro tests. Using the COG1901 recombinant enzyme from Methanocaldococcus jannaschii (Mj1640), purified enzyme Pus10 from M. jannaschii and full-size tRNA transcripts or TΨ-arm (17-mer) fragments as substrates, the sequential pathway of m(1)Ψ54 formation in Archaea was reconstituted. The methylation reaction is AdoMet dependent. The efficiency of the methylase reaction depended on the identity of the residue at position 55 of the TΨ-loop. The presence of Ψ55 allowed the efficient conversion of Ψ54 to m(1)Ψ54, whereas in the presence of C55, the reaction was rather inefficient and no methylation reaction occurred if a purine was present at this position. These results led to renaming the Archaeal COG1901 members as TrmY proteins.

Structural insight into the ion-exchange mechanism of the sodium/calcium exchanger

Sodium/calcium (Na(+)/Ca(2+)) exchangers (NCX) are membrane transporters that play an essential role in maintaining the homeostasis of cytosolic Ca(2+) for cell signaling. We demonstrated the Na(+)/Ca(2+)-exchange function of an NCX from Methanococcus jannaschii (NCX_Mj) and report its 1.9 angstrom crystal structure in an outward-facing conformation. Containing 10 transmembrane helices, the two halves of NCX_Mj share a similar structure with opposite orientation. Four ion-binding sites cluster at the center of the protein: one specific for Ca(2+) and three that likely bind Na(+). Two passageways allow for Na(+) and Ca(2+) access to the central ion-binding sites from the extracellular side. Based on the symmetry of NCX_Mj and its ability to catalyze bidirectional ion-exchange reactions, we propose a structure model for the inward-facing NCX_Mj.

Metalloproteins and the pyrite-based origin of life: a critical assessment

We critically examine the proposal by Wächtershäuser (Prokaryotes 1:275-283, 2006a, Philos Trans R Soc Lond B Biol Sci 361: 787-1808, 2006b) that putative transition metal binding sites in protein components of the translation machinery of hyperthermophiles provide evidence of a direct relationship with the FeS clusters of pyrite and thus indicate an autotrophic origin of life in volcanic environments. Analysis of completely sequenced cellular genomes of Bacteria, Archaea and Eucarya does not support the suggestion by Wächtershäuser (Prokaryotes 1:275-283, 2006a, Philos Trans R Soc Lond B Biol Sci 361: 787-1808, 2006b) that aminoacyl-tRNA synthetases and ribosomal proteins bear sequence signatures typical of strong covalent metal bonding whose absence in mesophilic species reveals a process of adaptation towards less extreme environments.

Experimental silicification of the extremophilic Archaea Pyrococcus abyssi and Methanocaldococcus jannaschii: applications in the search for evidence of life in early Earth and extraterrestrial rocks

Hydrothermal activity was common on the early Earth and associated micro-organisms would most likely have included thermophilic to hyperthermophilic species. 3.5-3.3 billion-year-old, hydrothermally influenced rocks contain silicified microbial mats and colonies that must have been bathed in warm to hot hydrothermal emanations. Could they represent thermophilic or hyperthermophilic micro-organisms and if so, how were they preserved? We present the results of an experiment to silicify anaerobic, hyperthermophilic micro-organisms from the Archaea Domain Pyrococcus abyssi and Methanocaldococcus jannaschii, that could have lived on the early Earth. The micro-organisms were placed in a silica-saturated medium for periods up to 1 year. Pyrococcus abyssi cells were fossilized but the M. jannaschii cells lysed naturally after the exponential growth phase, apart from a few cells and cell remains, and were not silicified although their extracellular polymeric substances were. In this first simulated fossilization of archaeal strains, our results suggest that differences between species have a strong influence on the potential for different micro-organisms to be preserved by fossilization and that those found in the fossil record represent probably only a part of the original diversity. Our results have important consequences for biosignatures in hydrothermal or hydrothermally influenced deposits on Earth, as well as on early Mars, as environmental conditions were similar on the young terrestrial planets and traces of early Martian life may have been similarly preserved as silicified microfossils.

NMR structure of a KlbA intein precursor from Methanococcus jannaschii

Certain proteins of unicellular organisms are translated as precursor polypeptides containing inteins (intervening proteins), which are domains capable of performing protein splicing. These domains, in conjunction with a single residue following the intein, catalyze their own excision from the surrounding protein (extein) in a multistep reaction involving the cleavage of two intein-extein peptide bonds and the formation of a new peptide bond that ligates the two exteins to yield the mature protein. We report here the solution NMR structure of a 186-residue precursor of the KlbA intein from Methanococcus jannaschii, comprising the intein together with N- and C-extein segments of 7 and 11 residues, respectively. The intein is shown to adopt a single, well-defined globular domain, representing a HINT (Hedgehog/Intein)-type topology. Fourteen beta-strands are arranged in a complex fold that includes four beta-hairpins and an antiparallel beta-ribbon, and there is one alpha-helix, which is packed against the beta-ribbon, and one turn of 3(10)-helix in the loop between the beta-strands 8 and 9. The two extein segments show increased disorder, and form only minimal nonbonding contacts with the intein domain. Structure-based mutation experiments resulted in a proposal for functional roles of individual residues in the intein catalytic mechanism.

Structural features of the guide:target RNA duplex required for archaeal box C/D sRNA-guided nucleotide 2'-O-methylation

Archaeal box C/D sRNAs guide the 2'-O-methylation of target nucleotides using both terminal box C/D and internal C'/D' RNP complexes. In vitro assembly of a catalytically active Methanocaldococcus jannaschii sR8 box C/D RNP provides a model complex to determine those structural features of the guide:target RNA duplex important for sRNA-guided nucleotide methylation. Watson-Crick pairing of guide and target nucleotides was found to be essential for methylation, and mismatched bases within the guide:target RNA duplex also disrupted nucleotide modification. However, dependence upon Watson-Crick base-paired guide:target nucleotides for methylation was compromised in elevated Mg(2+) concentrations where mismatched target nucleotides were modified. Nucleotide methylation required that the guide:target duplex consist of an RNA:RNA duplex as a target ribonucleotide within a guide RNA:target DNA duplex that was not methylated. Interestingly, D and D' target RNAs exhibited different levels of methylation when deoxynucleotides were inserted into the target RNA or when target methylation was carried out in elevated Mg(2+) concentrations. These observations suggested that unique structural features of the box C/D and C'/D' RNPs differentially affect their respective methylation capabilities. The ability of the sR8 box C/D sRNP to methylate target nucleotides positioned within highly structured RNA hairpins suggested that the sRNP can facilitate unwinding of double-stranded target RNAs. Finally, increasing target RNA length to extend beyond those nucleotides that base pair with the sRNA guide sequence significantly increased sRNP turnover and thus nucleotide methylation. This suggests that target RNA interaction with the sRNP core proteins is also important for box C/D sRNP-guided nucleotide methylation.

Structure and function of methanogens along a short-term restoration chronosequence in the Florida Everglades

The removal of plants and soil to bedrock to eradicate exotic invasive plants within the Hole-in-the-Donut (HID) region, part of the Everglades National Park (Florida), presented a unique opportunity to study the redevelopment of soil and the associated microbial communities in the context of short-term primary succession and ecosystem restoration. The goal of this study was to identify relationships between soil redevelopment and activity and composition of methanogenic assemblages in HID soils. Methane production potentials indicated a general decline in methanogenic activity with restoration age. Microcosm incubations strongly suggested hydrogenotrophic methanogenesis as the most favorable pathway for methane formation in HID soils from all sites. Culture-independent techniques targeting methyl coenzyme M reductase genes (mcrA) were used to assess the dynamics of methanogenic assemblages. Clone libraries were dominated by sequences related to hydrogenotrophic methanogens of the orders Methanobacteriales and Methanococcales and suggested a general decline in the relative abundance of Methanobacteriales mcrA with time since restoration. Terminal restriction fragment length polymorphism analysis indicated methanogenic assemblages remain relatively stable between wet and dry seasons. Interestingly, analysis of soils across the restoration chronosequence indicated a shift in Methanobacteriales populations with restoration age, suggesting genotypic shifts due to site-specific factors.

Methylglyoxal is an intermediate in the biosynthesis of 6-deoxy-5-ketofructose-1-phosphate: a precursor for aromatic amino acid biosynthesis in Methanocaldococcus jannaschii

A biosynthetic pathway is proposed for creating 6-deoxy-5-ketofructose-1-phosphate (DKFP), a precursor sugar for aromatic amino acid biosynthesis in Methanocaldococcus jannaschii. First, two possible routes were investigated to determine if a modified, established biosynthetic pathway could be responsible for generating 6-deoxyhexoses in M. jannaschii. Both the nucleoside diphosphate mannose pathway and a pathway involving nucleoside diphosphate derivatives of fructose-1-P, fructose-2-P, or fructose-1,6-bisP were tested and eliminated. The established pathways did not produce the expected intermediates nor did the anticipated enzymes have the predicted enzymatic activities. Because neither anticipated pathway could produce DKFP, M. jannaschii glucose-6-P metabolism was studied in detail to establish exactly how glucose-6-P is converted into DKFP. This detailed analysis showed that methylglyoxal and a fructose-1-P- or fructose-1,6-bisP-derived dihydroxyacetone-P fragment are key intermediates in DKFP production. Glucose-6-P readily converts to fructose-6-P, which in turn converts to fructose-1,6-bisP. Fructose-6-P and fructose-1,6-bisP convert into glyceraldehyde-3-P (Ga-P-3), which converts into methylglyoxal by a 2,3-elimination of phosphate. The MJ1585-derived enzyme catalyzes the condensation of methylglyoxal with a dihydroxyacetone-P fragment, which is derived from fructose-1-P and/or fructose-1,6-bisP, generating DKFP. The elimination of phosphate from Ga-P-3 proceeds by both enzymatic and chemical routes in cell extracts, producing sufficient concentrations of methylglyoxal to support the reaction. This work is the first report of methylglyoxal functioning in central metabolism.

Biosynthesis of phosphoserine in the Methanococcales

Methanococcus maripaludis and Methanocaldococcus jannaschii produce cysteine for protein synthesis using a tRNA-dependent pathway. These methanogens charge tRNA(Cys) with l-phosphoserine, which is also an intermediate in the predicted pathways for serine and cystathionine biosynthesis. To establish the mode of phosphoserine production in Methanococcales, cell extracts of M. maripaludis were shown to have phosphoglycerate dehydrogenase and phosphoserine aminotransferase activities. The heterologously expressed and purified phosphoglycerate dehydrogenase from M. maripaludis had enzymological properties similar to those of its bacterial homologs but was poorly inhibited by serine. While bacterial enzymes are inhibited by micromolar concentrations of serine bound to an allosteric site, the low sensitivity of the archaeal protein to serine is consistent with phosphoserine's position as a branch point in several pathways. A broad-specificity class V aspartate aminotransferase from M. jannaschii converted the phosphohydroxypyruvate product to phosphoserine. This enzyme catalyzed the transamination of aspartate, glutamate, phosphoserine, alanine, and cysteate. The M. maripaludis homolog complemented a serC mutation in the Escherichia coli phosphoserine aminotransferase. All methanogenic archaea apparently share this pathway, providing sufficient phosphoserine for the tRNA-dependent cysteine biosynthetic pathway.

The Elongator subunit Elp3 contains a Fe4S4 cluster and binds S-adenosylmethionine

The Elp3 subunit of the Elongator complex is highly conserved from archaea to humans and contains a well-characterized C-terminal histone acetyltransferase (HAT) domain. The central region of Elp3 shares significant sequence homology to the Radical SAM superfamily. Members of this large family of bacterial proteins contain a FeS cluster and use S-adenosylmethionine (SAM) to catalyse a variety of radical reactions. To biochemically characterize this domain we have expressed and purified the corresponding fragment of the Methanocaldococcus jannaschii Elp3 protein. The presence of a Fe4S4 cluster has been confirmed by UV-visible spectroscopy and electron paramagnetic resonance (EPR) spectroscopy and the Fe content determined by both a colorimetric assay and atomic absorption spectroscopy. The cysteine residues involved in cluster formation have been identified by site-directed mutagenesis. The protein binds SAM and the binding alters the EPR spectrum of the FeS cluster. Our results provide biochemical support to the hypothesis that Elp3 does indeed contain the Fe4S4 cluster which characterizes the Radical SAM superfamily and binds SAM, suggesting that Elp3, in addition to its HAT activity, has a second as yet uncharacterized catalytic function. We also present preliminary data to show that the protein cleaves SAM.

4'-phosphopantetheine biosynthesis in Archaea

Coenzyme A as the principal acyl carrier is required for many synthetic and degradative reactions in intermediary metabolism. It is synthesized in five steps from pantothenate, and recently the CoaA biosynthetic genes of eubacteria, plants, and human were all identified and cloned. In most bacteria, the so-called Dfp proteins catalyze the synthesis of the coenzyme A precursor 4'-phosphopantetheine. Dfp proteins are bifunctional enzymes catalyzing the synthesis of 4'-phosphopantothenoylcysteine (CoaB activity) and its decarboxylation to 4'-phosphopantetheine (CoaC activity). Here, we demonstrate the functional characterization of the CoaB and CoaC domains of an archaebacterial Dfp protein. Both domains of the Methanocaldococcus jannaschii Dfp protein were purified as His tag proteins, and their enzymatic activities were then identified and characterized by site-directed mutagenesis. Although the nucleotide binding motif II of the CoaB domain resembles that of eukaryotic enzymes, Methanocaldococcus CoaB is a CTP- and not an ATP-dependent enzyme, as shown by detection of the 4'-phosphopantothenoyl-CMP intermediate. The proposed 4'-phosphopantothenoylcysteine binding clamp of the Methanocaldococcus CoaC activity differs significantly from those of other characterized CoaC proteins. In particular, the active site cysteine residue, which otherwise is involved in the reduction of an aminoenethiol reaction intermediate, is not present. Moreover, the conserved Asn residue of the PXMNXXMW motif, which contacts the carboxyl group of 4'-phosphopantothenoylcysteine, is exchanged for His.

Aerobic methane oxidation and methanotroph community composition during seasonal stratification in Mono Lake, California (USA)

Patterns of aerobic methane (CH4) oxidation and associated methanotroph community composition were investigated during the development of seasonal stratification in Mono Lake, California (USA). CH4 oxidation rates were measured using a tritiated CH4 radiotracer technique. Fluorescence in situ hybridization (FISH), denaturing gradient gel electrophoresis (DGGE) and sequence analysis were used to characterize methanotroph community composition. A temporally shifting zone of elevated CH4 oxidation (59-123 nM day(-1)) was consistently associated with a suboxycline, microaerophilic zone that migrated upwards in the water column as stratification progressed. FISH analysis revealed stable numbers of type I (4.1-9.3 x 10(5) cells ml(-1)) and type II (1.4-3.4 x 10(5) cells ml(-1)) methanotrophs over depth and over time. Denaturing gradient gel electrophoresis and sequence analysis indicated slight shifts in methanotroph community composition despite stable absolute cell numbers. Variable CH4 oxidation rates in the presence of a relatively stable methanotroph population suggested that zones of high CH4 oxidation resulted from an increase in activity of a subset of the existing methanotroph population. These results challenge existing paradigms suggesting that zones of elevated CH4 oxidation activity result from the accumulation of methanotrophic biomass and illustrate that type II methanotrophs may be an important component of the methanotroph population in saline and/or alkaline pelagic environments.

Direct modulation of RNA polymerase core functions by basal transcription factors

Archaeal RNA polymerases (RNAPs) are recruited to promoters through the joint action of three basal transcription factors: TATA-binding protein, TFB (archaeal homolog of TFIIB), and TFE (archaeal homolog of TFIIE). Our results demonstrate several new insights into the mechanisms of TFB and TFE during the transcription cycle. (i) The N-terminal Zn ribbon of TFB displays a surprising degree of redundancy for the recruitment of RNAP during transcription initiation in the archaeal system. (ii) The B-finger domain of TFB participates in transcription initiation events by stimulating abortive and productive transcription in a recruitment-independent function. TFB thus combines physical recruitment of the RNAP with an active role in influencing the catalytic properties of RNAP during transcription initiation. (iii) TFB mutations are complemented by TFE, thereby demonstrating that both factors act synergistically during transcription initiation. (iv) An additional function of TFE is to dynamically alter the nucleic acid-binding properties of RNAP by stabilizing the initiation complex and destabilizing elongation complexes.

Promoter architecture and response to a positive regulator of archaeal transcription

The archaeal transcription apparatus is chimeric: its core components (RNA polymerase and basal factors) closely resemble those of eukaryotic RNA polymerase II, but the putative archaeal transcriptional regulators are overwhelmingly of bacterial type. Particular interest attaches to how these bacterial-type effectors, especially activators, regulate a eukaryote-like transcription system. The hyperthermophilic archaeon Methanocaldococcus jannaschii encodes a potent transcriptional activator, Ptr2, related to the Lrp/AsnC family of bacterial regulators. Ptr2 activates rubredoxin 2 (rb2) transcription through a bipartite upstream activating site (UAS), and conveys its stimulatory effects on its cognate transcription machinery through direct recruitment of the TATA binding protein (TBP). A functional dissection of the highly constrained architecture of the rb2 promoter shows that a 'one-site' minimal UAS suffices for activation by Ptr2, and specifies the required placement of this site. The presence of such a simplified UAS upstream of the natural rubrerythrin (rbr) promoter also suffices for positive regulation by Ptr2 in vitro, and TBP recruitment remains the primary means of transcriptional activation at this promoter.

RNA-dependent cysteine biosynthesis in archaea

Several methanogenic archaea lack cysteinyl-transfer RNA (tRNA) synthetase (CysRS), the essential enzyme that provides Cys-tRNA(Cys) for translation in most organisms. Partial purification of the corresponding activity from Methanocaldococcus jannaschii indicated that tRNA(Cys) becomes acylated with O-phosphoserine (Sep) but not with cysteine. Further analyses identified a class II-type O-phosphoseryl-tRNA synthetase (SepRS) and Sep-tRNA:Cys-tRNA synthase (SepCysS). SepRS specifically forms Sep-tRNA(Cys), which is then converted to Cys-tRNA(Cys) by SepCysS. Comparative genomic analyses suggest that this pathway, encoded in all organisms lacking CysRS, can also act as the sole route for cysteine biosynthesis. This was proven for Methanococcus maripaludis, where deletion of the SepRS-encoding gene resulted in cysteine auxotrophy. As the conversions of Sep-tRNA to Cys-tRNA or to selenocysteinyl-tRNA are chemically analogous, the catalytic activity of SepCysS provides a means by which both cysteine and selenocysteine may have originally been added to the genetic code.

Optimization of diagnostic microarray for application in analysing landfill methanotroph communities under different plant covers

Landfill sites are responsible for 6-12% of global methane emission. Methanotrophs play a very important role in decreasing landfill site methane emissions. We investigated the methane oxidation capacity and methanotroph diversity in lysimeters simulating landfill sites with different plant vegetations. Methane oxidation rates were 35 g methane m-2 day-1 or higher for planted lysimeters and 18 g methane m-2 day-1 or less for bare soil controls. Best methane oxidation, as displayed by gas depth profiles, was found under a vegetation of grass and alfalfa. Methanotroph communities were analysed at high throughput and resolution using a microbial diagnostic microarray targeting the particulate methane monooxygenase (pmoA) gene of methanotrophs and functionally related bacteria. Members of the genera Methylocystis and Methylocaldum were found to be the dominant members in landfill site simulating lysimeters. Soil bacterial communities in biogas free control lysimeters, which were less abundant in methanotrophs, were dominated by Methylocaldum. Type Ia methanotrophs were found only in the top layers of bare soil lysimeters with relatively high oxygen and low methane concentrations. A competetive advantage of type II methanotrophs over type Ia methanotrophs was indicated under all plant covers investigated. Analysis of average and individual results from parallel samples was used to identify general trends and variations in methanotroph community structures in relation to depth, methane supply and plant cover. The applicability of the technology for the detection of environmental perturbations was proven by an erroneous result, where an unexpected community composition detected with the microarray indicated a potential gas leakage in the lysimeter being investigated.

Cold adaptation of archaeal elongation factor 2 (EF-2) proteins

Cell growth at low temperature is dependent on the ability of cells to perform protein synthesis. Cold adapted micro-organisms (psychrophilic or psychrotolerant) have a superior ability to perform translation at low temperature. This review addresses cold adaptation of protein synthesis in Archaea by examining what is presently known about thermal adaptation of elongation factor 2 (EF-2) proteins from Archaea. Despite the knowledge that Archaea are abundant in cold environments (e.g. the ocean), few cold adapted species have been isolated and studied. As a result this review is largely confined to comparative analyses of EF-2 proteins from psychrotolerant (Methanococcoides burtonii) and thermophilic (Methanosarcina thermophila) methanogens. A key finding from these studies is that in addition to inherent properties of the EF-2 proteins, intracellular factors (e.g. ribosomes and intracellular solutes) play a central role in thermal adaptation.

Post-transcriptional modification in archaeal tRNAs: identities and phylogenetic relations of nucleotides from mesophilic and hyperthermophilic Methanococcales

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.