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Summary Thaumarchaeota are globally distributed and abundant microorganisms occurring in diverse habitats and thus represent a major source of archaeal lipids. The scope of lipids as taxonomic markers in microbial ecological studies is limited by the scarcity of comparative data on the membrane lipid composition of cultivated representatives, including the phylum Thaumarchaeota. Here, we comprehensively describe the core and intact polar lipid (IPL) inventory of ten ammonia-oxidising thaumarchaeal cultures representing all four characterized phylogenetic clades. IPLs of these thaumarchaeal strains are generally similar and consist of membrane-spanning, glycerol dibiphytanyl glycerol tetraethers with monoglycosyl, diglycosyl, phosphohexose and hexose-phosphohexose headgroups. However, the relative abundances of these IPLs and their core lipid compositions differ systematically between the phylogenetic subgroups, indicating high potential for chemotaxonomic distinction of thaumarchaeal clades. Comparative lipidomic analyses of 19 euryarchaeal and crenarchaeal strains suggested that the lipid methoxy archaeol is synthesized exclusively by Thaumarchaeota and may thus represent a diagnostic lipid biomarker for this phylum. The unprecedented diversity of the thaumarchaeal lipidome with 118 different lipids suggests that membrane lipid composition and adaptation mechanisms in Thaumarchaeota are more complex than previously thought and include unique lipids with as yet unresolved properties.

The majority of cells in nature probably exist in a stationary-phase-like state, due to nutrient limitation in most environments. Studies on bacteria and yeast reveal morphological and physiological changes throughout the stationary phase, which lead to an increased ability to survive prolonged nutrient limitation. However, there is little information on archaeal stationary phase responses. We investigated protein- and lipid-level changes inThermococcus kodakarensiswith extended time in the stationary phase. Adaptations to time in stationary phase included increased proportion of membrane lipids with a tetraether backbone, synthesis of proteins that ensure translational fidelity, specific regulation of ABC transporters (upregulation of some, downregulation of others), and upregulation of proteins involved in coenzyme production. Given that the biological mechanism of tetraether synthesis is unknown, we also considered whether any of the protein-level changes inT. kodakarensismight shed light on the production of tetraether lipids across the same period. A putative carbon-nitrogen hydrolase, a TldE (a protease inEscherichia coli) homologue, and a membrane bound hydrogenase complex subunit were candidates for possible involvement in tetraether-related reactions, while upregulation of adenosylcobalamin synthesis proteins might lend support to a possible radical mechanism as a trigger for tetraether synthesis.

Transcription initiation by archaeal RNA polymerase (RNAP) and eukaryotic RNAP II requires the general transcription factor (TF) B/ IIB. Structural analyses of eukaryotic transcription initiation complexes locate the B-reader domain of TFIIB in close proximity to the active site of RNAP II. Here, we present the first crosslinking mapping data that describe the dynamic transitions of an archaeal TFB to provide evidence for structural rearrangements within the transcription complex during transition from initiation to early elongation phase of transcription. Using a highly specific UV-inducible crosslinking system based on the unnatural amino acid para-benzoyl-phenylalanine allowed us to analyze contacts of the Pyrococcus furiosus TFB B-reader domain with site-specific radiolabeled DNA templates in preinitiation and initially transcribing complexes. Crosslink reactions at different initiation steps demonstrate interactions of TFB with DNA at registers +6 to +14, and reduced contacts at +15, with structural transitions of the B-reader domain detected at register +10. Our data suggest that the B-reader domain of TFB interacts with nascent RNA at register +6 and +8 and it is displaced from the transcribed-strand during the transition from +9 to +10, followed by the collapse of the transcription bubble and release of TFB from register +15 onwards.

The distribution of respiratory quinone electron carriers among cultivated organisms provides clues on both the taxonomy of their producers and the redox processes these are mediating. Our study of the quinone inventories of 25 archaeal species belonging to the phyla Eury-, Cren- and Thaumarchaeota facilitates their use as chemotaxonomic markers for ecologically important archaeal clades. Saturated and monounsaturated menaquinones with six isoprenoid units forming the alkyl chain may serve as chemotaxonomic markers for Thaumarchaeota. Other diagnostic biomarkers are thiophene-bearing quinones for Sulfolobales and methanophenazines as functional quinone analogues of the Methanosarcinales. The ubiquity of saturated menaquinones in the Archaea in comparison to Bacteria suggests that these compounds may represent an ancestral and diagnostic feature of the Archaea. Overlap between quinone compositions of distinct thermophilic and halophilic archaea and bacteria may indicate lateral gene transfer. The biomarker potential of thaumarchaeal quinones was exemplarily demonstrated on a water column profile of the Black Sea. Both, thaumarchaeal quinones and membrane lipids showed similar distributions with maxima at the chemocline. Quinone distributions indicate that Thaumarchaeota dominate respiratory activity at a narrow interval in the chemocline, while they contribute only 9% to the microbial biomass at this depth, as determined by membrane lipid analysis.

To obtain new insights into community compositions of hyperthermophilic microorganisms, defined as having optimal growth temperatures of 80 degrees C and above, sediment and water samples were taken from two shallow marine hydrothermal vents (I and II) with temperatures of 100 degrees C at Vulcano Island, Italy. A combinatorial approach of denaturant gradient gel electrophoresis (DGGE) and metagenomic sequencing was used for microbial community analyses of the samples. In addition, enrichment cultures, growing anaerobically on selected polysaccharides such as starch and cellulose, were also analyzed by the combinatorial approach. Our results showed a high abundance of hyperthermophilic archaea, especially in sample II, and a comparable diverse archaeal community composition in both samples. In particular, the strains of the hyperthermophilic anaerobic genera Staphylothermus and Thermococcus, and strains of the aerobic hyperthermophilic genus Aeropyrum, were abundant. Regarding the bacterial community, e-Proteobacteria, especially the genera Sulfurimonas and Sulfurovum, were highly abundant. The microbial diversity of the enrichment cultures changed significantly by showing a high dominance of archaea, particularly the genera Thermococcus and Palaeococcus, depending on the carbon source and the selected temperature.

The archaeal transcription apparatus is closely related to the eukaryotic RNA polymerase (RNAP) II system, while\ud archaeal genomes are more similar to bacteria with densely packed genes organized in operons. This makes understanding\ud transcription in archaea vital, both in terms of molecular mechanisms and evolution. Very little is known about how\ud archaeal cells orchestrate transcription on a systems level. We have characterized the genome-wide occupancy of the\ud Methanocaldococcus jannaschii transcription machinery and its transcriptome. Our data reveal how the TATA and BRE\ud promoter elements facilitate recruitment of the essential initiation factors TATA-binding protein and transcription factor B,\ud respectively, which in turn are responsible for the loading of RNAP into the transcription units. The occupancies of\ud RNAP and Spt4/5 strongly correlate with each other and with RNA levels. Our results show that Spt4/5 is a general\ud elongation factor in archaea as its presence on all genes matches RNAP. Spt4/5 is recruited proximal to the transcription\ud start site on the majority of transcription units, while on a subset of genes, including rRNA and CRISPR loci, Spt4/5 is\ud recruited to the transcription elongation complex during early elongation within 500 base pairs of the transcription start\ud site and akin to its bacterial homologue NusG.

Although Pyrococcus furiosus is one of the best studied hyperthermophilic archaea, to date no experimental investigation of the extent of protein secretion has been performed. We describe experimental verification of the extracellular proteome of P. furiosus grown on starch. LC–MS/MS-based analysis of culture supernatants led to the identification of 58 proteins. Fifteen of these proteins had a putative N-terminal signal peptide (SP), tagging the proteins for translocation across the membrane. The detected proteins with predicted SPs and known function were almost exclusively involved in important extracellular functions, like substrate degradation or transport. Most of the 43 proteins without predicted N-terminal signal sequences are known to have intracellular functions, mainly (70 %) related to intracellular metabolism. In silico analyses indicated that the genome of P. furiosus encodes 145 proteins with N-terminal SPs, including 21 putative lipoproteins and 17 with a class III peptide. From these we identified 15 (10 %; 7 SPI, 3 SPIII and 5 lipoproteins) under the specific growth conditions of this study. The putative lipoprotein signal peptides have a unique sequence motif, distinct from the motifs in bacteria and other archaeal orders. Electronic supplementary material The online version of this article (doi:10.1007/s00792-013-0574-0) contains supplementary material, which is available to authorized users.

Thaumarchaeota are globally distributed and abundant microorganisms occurring in diverse habitats and thus represent a major source of archaeal lipids. The scope of lipids as taxonomic markers in microbial ecological studies is limited by the scarcity of comparative data on the membrane lipid composition of cultivated representatives, including the phylum Thaumarchaeota. Here, we comprehensively describe the core and intact polar lipid (IPL) inventory of ten ammonia-oxidising thaumarchaeal cultures representing all four characterized phylogenetic clades. IPLs of these thaumarchaeal strains are generally similar and consist of membrane-spanning, glycerol dibiphytanyl glycerol tetraethers with monoglycosyl, diglycosyl, phosphohexose and hexose-phosphohexose headgroups. However, the relative abundances of these IPLs and their core lipid compositions differ systematically between the phylogenetic subgroups, indicating high potential for chemotaxonomic distinction of thaumarchaeal clades. Comparative lipidomic analyses of 19 euryarchaeal and crenarchaeal strains suggested that the lipid methoxy archaeol is synthesized exclusively by Thaumarchaeota and may thus represent a diagnostic lipid biomarker for this phylum. The unprecedented diversity of the thaumarchaeal lipidome with 118 different lipids suggests that membrane lipid composition and adaptation mechanisms in Thaumarchaeota are more complex than previously thought and include unique lipids with as yet unresolved properties.

In all living cells, protein synthesis occurs on ribonucleoprotein particles called ribosomes. Molecular models have been reported for complete bacterial 70S and eukaryotic 80S ribosomes; however, only molecular models of large 50S subunits have been reported for archaea. Here, we present a complete molecular model for the Pyrococcus furiosus 70S ribosome based on a 6.6 A cryo-electron microscopy map. Moreover, we have determined cryo-electron microscopy reconstructions of the Euryarchaeota Methanococcus igneus and Thermococcus kodakaraensis 70S ribosomes and Crenarchaeota Staphylothermus marinus 50S subunit. Examination of these structures reveals a surprising promiscuous behavior of archaeal ribosomal proteins: We observe intersubunit promiscuity of S24e and L8e (L7ae), the latter binding to the head of the small subunit, analogous to S12e in eukaryotes. Moreover, L8e and L14e exhibit intrasubunit promiscuity, being present in two copies per archaeal 50S subunit, with the additional binding site of L14e analogous to the related eukaryotic r-protein L27e. Collectively, these findings suggest insights into the evolution of eukaryotic ribosomal proteins through increased copy number and binding site promiscuity.

Ribosome-driven protein biosynthesis is comprised of four phases: initiation, elongation, termination and recycling. In bacteria, ribosome recycling requires ribosome recycling factor and elongation factor G, and several structures of bacterial recycling complexes have been determined. In the eukaryotic and archaeal kingdoms, however, recycling involves the ABC-type ATPase ABCE1 and little is known about its structural basis. Here we present cryo-electron microscopy reconstructions of eukaryotic and archaeal ribosome recycling complexes containing ABCE1 and the termination factor paralogue Pelota. These structures reveal the overall binding mode of ABCE1 to be similar to canonical translation factors. Moreover, the iron–sulphur cluster domain of ABCE1 interacts with and stabilizes Pelota in a conformation that reaches towards the peptidyl transferase centre, thus explaining how ABCE1 may stimulate peptide-release activity of canonical termination factors. Using the mechanochemical properties of ABCE1, a conserved mechanism in archaea and eukaryotes is suggested that couples translation termination to recycling, and eventually to re-initiation. Cryo-electron-microscopy reconstructions of eukaryotic and archaeal ribosomes bound by ABCE1 and Pelota suggest a conserved mechanism for ribosome recycling. Once a ribosome completes translation of an RNA messenger, it must recycle itself by dissociating its large and small subunits. In archaea and eukaryotes, the ABCE1 protein promotes recycling in combination with termination release factors. Roland Beckmann and colleagues have performed cryoelectron-microscopy reconstructions of the eukaryotic and archaeal ribosomes bound by ABCE1 and Pelota, an mRNA surveillance factor that is a paralogue of release factors. They find that ABCE1 binds between the two subunits, and that its iron–sulphur domain places Pelota in a conformation that promotes peptide release by canonical release factors. This work suggests a remarkable degree of structural and functional conservation over the more than one billion years of evolution that separates eukaryotes and archaea. The observed ribosomal structures suggest a model for an ATP-driven power stroke that would disassemble the subunits.

Protein synthesis occurs in macromolecular particles called ribosomes. All ribosomes are composed of RNA and proteins. While the protein composition of bacterial and eukaryotic ribosomes has been well-characterized, a systematic analysis of archaeal ribosomes has been lacking. Here we report the first comprehensive two-dimensional PAGE and mass spectrometry analysis of archaeal ribosomes isolated from the thermophilic Pyrobaculum aerophilum and the thermoacidophilic Sulfolobus acidocaldarius Crenarchaeota. Our analysis identified all 66 ribosomal proteins (r-proteins) of the P. aerophilum small and large subunits, as well as all but two (62 of 64; 97%) r-proteins of the S. acidocaldarius small and large subunits that are predicted genomically. Some r-proteins were identified with one or two lysine methylations and N-terminal acetylations. In addition, we identify three hypothetical proteins that appear to be bona fide r-proteins of the S. acidocaldarius large subunit. Dissociation of r-proteins from the S. acidocaldarius large subunit indicates that the novel r-proteins establish tighter interactions with the large subunit than some integral r-proteins. Furthermore, cryo electron microscopy reconstructions of the S. acidocaldarius and P. aerophilum 50S subunits allow for a tentative localization of the binding site of the novel r-proteins. This study illustrates not only the potential diversity of the archaeal ribosomes but also the necessity to experimentally analyze the archaeal ribosomes to ascertain their protein composition. The discovery of novel archaeal r-proteins and factors may be the first step to understanding how archaeal ribosomes cope with extreme environmental conditions.

Anaerobic digestion of mainly energy crops gains more and more importance in developing a sustainable energy supply. Therefore, the optimization of gas yield plays a major role in specific research attempts and economical considerations. One possibility to increase natural polymer degradation and concomitantly energy efficiency is the addition of exoenzymes to biogas facilities to enforce the primary degradation steps for biogas production. Therefore, in the present study, the stability and activity of five externally added enzyme mixtures to anaerobic biogas processes were investigated. Protein assays using soluble fractions of different biogas plants incubated together with the enzyme mixtures revealed that, within about 10 min, the externally added enzymes were mostly degraded. This very low stability in biogas reactors makes it unlikely that the addition of enzymes contributes significantly to degradation of macromolecules in the biogas process. Even the addition of protease inhibitors did not protect the added enzyme mixtures from degradation in most experiments. Furthermore, the influence of added enzymes on the viscosity of the biomass was tested. Only a marginal effect was obtained, when applying a tenfold higher concentration of added enzymes as proposed for practical use. The same result was achieved when commercially available enzymes were added to technical-scale fermentations using corn silage as monosubstrate. Therefore, these studies did not provide evidence that the addition of external enzymes into anaerobic degradation systems increases the methane yield in biogas facilities.

We present structural and biochemical evidence for a redox switch in the archaeal transcriptional regulator SurR of Pyrococcus furiosus, a hyperthermophilic anaerobe. P. furiosus produces H(2) during fermentation, but undergoes a metabolic shift to produce H(2) S when elemental sulfur (S(0) ) becomes available. Changes in gene expression occur within minutes of S(0) addition, and the majority of these S(0) -responsive genes are regulatory targets of SurR, a key regulator involved in primary S(0) response. SurR was shown in vitro to have dual functionality, activating transcription of some of these genes, notably the hydrogenase operons, and repressing others, including a gene-encoding sulfur reductase. This work demonstrates via biochemical and structural evidence that the activity of SurR is modulated by cysteine residues in a CxxC motif that constitutes a redox switch. Oxidation of the switch with S(0) inhibits sequence-specific DNA binding by SurR, leading to deactivation of genes related to H(2) production and derepression of genes involved in S(0) metabolism.

Pyrococcus furiosus is a model organism for analyses of molecular biology and biochemistry of archaea, but so far no useful genetic tools for this species have been described. We report here a genetic transformation system for P. furiosus based on the shuttle vector system pYS2 from Pyrococcus abyssi . In the redesigned vector, the pyrE gene from Sulfolobus was replaced as a selectable marker by the 3-hydroxy-3-methylglutaryl coenzyme A reductase gene (HMG-CoA) conferring resistance of transformants to the antibiotic simvastatin. Use of this modified plasmid resulted in the overexpression of the HMG-CoA reductase in P. furiosus , allowing the selection of strains by growth in the presence of simvastatin. The modified shuttle vector replicated in P. furio s us , but the copy number was only one to two per chromosome. This system was used for overexpression of His 6 -tagged subunit D of the RNA polymerase (RNAP) in Pyrococcus cells. Functional RNAP was purified from transformed cells in two steps by Ni-NTA and gel filtration chromatography. Our data provide evidence that expression of transformed genes can be controlled from a regulated gluconeogenetic promoter.

The hyperthermophilic archaeon Pyrococcus furiosus grows optimally near 100°C and undergoes a heat shock response at 105°C, mediated at least in part by the heat shock regulator Phr. Genes encoding a small heat shock protein (HSP20) and a member of the AAA + ATPase are the only known targets of the regulator, but a genetic mutant of Phr has yet to be characterized. We describe here an alternative approach for the identification of the regulon of Phr based on cell-free transcription of fragmented chromosomal DNA in the presence or absence of the regulator and hybridization of in vitro RNA to P. furiosus whole-genome microarrays. Our results confirmed the phr , the hsp20 , and the aaa + ATPase genes as targets of Phr and also identified six additional open reading frames, PF0624, PF1042, PF1291, PF1292, PF1488, and PF1616, as Phr-responsive genes, which include that encoding di-myo-inositol phosphate synthase. Transcription of the identified novel genes was inhibited by Phr in standard transcription assays, and the novel consensus sequence 5′-TTTAnnnACnnnnnGTnAnnAAAA-3′ (uppercase letters denote a high conservation of the bases) was inferred from our data as the Phr recognition motif. Mutational evidence for the significance of this sequence as Phr recognition was provided in DNA-binding experiments.

The recent success in reconstitution of RNAPs (RNA polymerases) from hyperthermophilic archaea from bacterially expressed purified subunits opens the way for detailed structure–function analyses of multisubunit RNAPs. The archaeal enzyme shows close structural similarity to eukaryotic RNAP, particularly to polymerase II, and can therefore be used as model for analyses of the eukaryotic transcriptional machinery. The cleft loops in the active centre of RNAP were deleted and modified to unravel their function in interaction with nucleic acids during transcription. The rudder, lid and fork 2 cleft loops were required for promoter-directed initiation and elongation, the rudder was essential for open complex formation. Analyses of transcripts from heteroduplex templates containing stable open complexes revealed that bubble reclosure is required for RNA displacement during elongation. Archaeal transcription systems contain, besides the orthologues of the eukaryotic transcription factors TBP (TATA-box-binding protein) and TF (transcription factor) IIB, an orthologue of the N-terminal part of the α subunit of eukaryotic TFIIE, called TFE, whose function is poorly understood. Recent analyses revealed that TFE is involved in open complex formation and, in striking contrast with eukaryotic TFIIE, is also present in elongation complexes. Recombinant archaeal RNAPs lacking specific subunits were used to investigate the functions of smaller subunits. These studies revealed that the subunits P and H, the orthologues of eukaryotic Rpb12 and Rpb5, were not required for RNAP assembly. Subunit P was essential for open complex formation, and the ΔH enzyme was greatly impaired in all assays, with the exception of promoter recruitment. Recent reconstitution studies indicate that Rpb12 and Rpb5 can be incorporated into archaeal RNAP and can complement for the function of the corresponding archaeal subunit in in vitro transcription assays.

This work describes the identification and characterization of SurR, Pyrococcus furiosus sulphur (S(0)) response regulator. SurR was captured from cell extract using promoter DNA of a hydrogenase operon that is downregulated in the primary response of P. furiosus to S(0), as revealed by DNA microarray experiments. SurR was validated as a sequence-specific DNA binding protein, and characterization of the SurR DNA binding motif GTTn(3)AAC led to the identification of several target genes that contain an extended motif in their promoters. A number of these were validated to contain upstream SurR binding sites. These SurR targets strongly correspond with open reading frames and operons both up- and downregulated in the primary response to S(0). In vitro transcription revealed that SurR is an activator for its own gene as well as for two hydrogenase operons whose expression is downregulated during the primary S(0) response; it is also a repressor for two genes upregulated during the primary S(0) response, one of which encodes the primary S(0)-reducing enzyme NAD(P)H sulphur reductase. Herein we give evidence for the role of SurR in both mediating the primary response to S(0) and controlling hydrogen production in P. furiosus.

To improve our understanding of microbially mediated pyrite dissolution, the influence of different archaeal metabolisms and crystallographic orientations of pyrite surfaces was studied. Therefore, synthetic pyrite surfaces of different orientations, including octahedral {111} and pentagondodecahedral {210} faces, were etched by Metallosphaera sedula and Sulfolobus metallicus during a time period of up to 16 days. A ferrozine assay was used in order to determine the concentration of iron ions in the solution as result of pyrite oxidation. It revealed that M. sedula produces more ferric iron in the solution than S. metallicus, indicating M. sedula as the more active organism. Epifluorescence microscopy observations showed that cells of both strains partly attach to the mineral surface whereas the rest remains planktonic, suggesting that both organisms might act through both, the 'contact' and 'non-contact' mechanisms of the indirect biooxidation mechanisms for the dissolution of pyrite. Studies with Scanning Electron Microscopy (SEM) showed cell attachment and etching effects during the whole time period. Surface alteration forms features depending on surface crystallography up to 30 mu m in size in 16 days of etching, while the shape of the features varies with face-symmetry. (C) 2008 Elsevier B.V. All rights reserved.

Related multisubunit RNA polymerases (RNAPs) carry out gene transcription in all kingdoms of life. Since structural information is limited to bacterial and eukaryotic RNAPs, we determined the cryo-electron microscopic structure of the RNAP from the thermophilic archaeon Pyrococcus furiosus at 13 A resolution. Comparison with eukaryotic RNAP II reveals a conserved architecture, no homologues for subunits Rpb8 and Rpb9, and significant deviation in the polymerase foot, jaws, pore, and protrusion. The structural organization of the archaeal RNA polymerase serves as a reference for future structure-function analysis of the transcription mechanism and allows for evolutionary comparisons.

The genome of the hyperthermophile archaeon Pyrococcus furiosus encodes two transcription factor B (TFB) paralogs, one of which (TFB1) was previously characterized in transcription initiation. The second TFB (TFB2) is unusual in that it lacks recognizable homology to the archaeal TFB/eukaryotic TFIIB B-finger motif. TFB2 functions poorly in promoter-dependent transcription initiation, but photochemical cross-linking experiments indicated that the orientation and occupancy of transcription complexes formed with TFB2 at the strong gdh promoter are similar to the orientation and occupancy of transcription complexes formed with TFB1. Initiation complexes formed by TFB2 display a promoter opening defect that can be bypassed with a preformed transcription bubble, suggesting a mechanism to explain the low TFB2 transcription activity. Domain swaps between TFB1 and TFB2 showed that the low activity of TFB2 is determined mainly by its N terminus. The low activity of TFB2 in promoter opening and transcription can be partially relieved by transcription factor E (TFE). The results indicate that the TFB N-terminal region, containing conserved Zn ribbon and B-finger motifs, is important in promoter opening and that TFE can compensate for defects in the N terminus through enhancement of promoter opening.

A homologue of the N-terminal domain of the alpha subunit of the general eukaryotic transcription factor TFE is encoded in the genomes of all sequenced archaea, but the position of archaeal TFE in transcription complexes has not yet been defined. We show here that TFE binds nonspecifically to single-stranded DNA, and photochemical cross-linking revealed TFE binding to a preformed open transcription bubble. In preinitiation complexes, the N-terminal part of TFE containing a winged helix-turn-helix motif is cross-linked specifically to DNA of the nontemplate DNA strand at positions -9 and -11. In complexes stalled at +20, TFE cross-linked specifically to positions +9, +11, and +16 of the non-template strand. Analyses of transcription complexes stalled at position +20 revealed a TFE-dependent increase of the resumption efficiency of stalled RNA polymerase and a TFE-induced enhanced permanganate sensitivity of thymine residues in the transcription bubble. These results demonstrate the presence of TFE in early elongation complexes and suggest a role of TFE in stabilization of the transcription bubble during elongation.

The rotor subunit c of the A(1)A(O) ATP synthase of the hyperthermophilic archaeon Pyrococcus furiosus contains a conserved Na(+)-binding motif, indicating that Na(+) is a coupling ion. To experimentally address the nature of the coupling ion, we isolated the enzyme by detergent solubilization from native membranes followed by chromatographic separation techniques. The entire membrane-embedded motor domain was present in the preparation. The rotor subunit c was found to form an SDS-resistant oligomer. Under the conditions tested, the enzyme had maximal activity at 100 degrees C, had a rather broad pH optimum between pH 5.5 and 8.0, and was inhibited by diethystilbestrol and derivatives thereof. ATP hydrolysis was strictly dependent on Na(+), with a K(m) of 0.6 mM. Li(+), but not K(+), could substitute for Na(+). The Na(+) dependence was less pronounced at higher proton concentrations, indicating competition between Na(+) and H(+) for a common binding site. Moreover, inhibition of the ATPase by N',N'-dicyclohexylcarbodiimide could be relieved by Na(+). Taken together, these data demonstrate the use of Na(+) as coupling ion for the A(1)A(O) ATP synthase of Pyrococcus furiosus, the first Na(+) A(1)A(O) ATP synthase described.

To enhance our understanding of effects of microbially mediated pyrite dissolution and the influence parameters such as varied metabolism and crystallographic orientation of pyrite surfaces some dissolution experiments were performed. Microbial etching experiments on pyrite surfaces of different orientation, including {111} and {210} were devised. The experiments were performed using two strains of thermophilic Archaea (Sulfolobus metallicus, Metallosphaera sedula). Epifluorescence microscopy observations showed that the strains attach to the mineral surface. Studies with Scanning Electron Microscopy (SEM) showed cell attachment and etching effects after one week of incubation. Surface alteration produced structures following crystallographic orientation up to several 10 μm in size. For all incubated pyrite samples it became apparent that surface alteration was more pronounced with M. sedula than with S. metallicus.

The characterization of the transcriptional regulator TrmBL1 of the hyperthermophilic archaeon Pyrococcus furiosus, homologous to TrmB (transcriptional regulator of the maltose system), was studied. The genome of P. furiosus contains three TrmB paralogues. One of the TrmB-like proteins (TrmBL), PF0124 (TrmBL1), was analysed in more detail. It regulated the expression of the genes encoding enzymes of the glycolytic pathway as well as the maltodextrin (MD) ABC transporter. By molecular sieve chromatography, purified TrmBL1 behaved at ambient temperature as a tetramer of 148.8 kDa. In the presence of 1 mM maltotriose or 5 mM maltose TrmBL1 formed octamers. As shown by electrophoretic mobility shift assay (EMSA) TrmBL1 was found to bind the MD (maltodextrin ABC transport genes) promoter DNA with sixfold higher binding affinity (K(d) 0.2 microM) than to the trehalose/maltose ABC transporter (TM) promoter (K(d) 1.2 microM). Maltotriose and maltose interfered in these assays indicating inducer function. In vitro transcription assays using purified transcription components corroborated the data obtained with EMSA and showed inhibition of transcription of the MD promoter by TrmBL1. Recently, van de Werken et al. (FEMS Microbiol Lett 2006; 260: 69-76) identified TGM, a conserved sequence (Thermococcales-Glycolytic-Motif) upstream of genes encoding glycolytic enzymes and the MD ABC transporter. The position of TGM is invariably located downstream of the BRE-TATA box and overlapping the transcription start site on each promoter. By footprint analysis TrmBL1 was found to recognize the TGM sequence in several TGM-containing promoter sequences. We identified the recognition helix in TrmBL1 revealing tyrosine (Y49) to be essential for target DNA binding. However, the TGM motif was not essential for TrmBL1 binding. We conclude that TrmBL1 is a global sugar-sensing transcriptional regulator controlling the genes of transport systems and of sugar-metabolizing enzymes.

We report here the crystal structure of a protein from Pyrococcus furiosus (Phr) that represents the first characterized heat shock transcription factor in archaea. Phr specifically represses the expression of heat shock genes at physiological temperature in vitro and in vivo but is released from the promoters upon heat shock response. Structure analysis revealed a stable homodimer, each subunit consisting of an N-terminal winged helix DNA-binding domain (wH-DBD) and a C-terminal antiparallel coiled coil helical domain. The overall structure shows as a molecular chimera with significant folding similarity of its DBD to the bacterial SmtB/ArsR family, while its C-terminal part was found to be a remote homologue of the eukaryotic BAG domain. The dimeric protein recognizes a palindromic DNA sequence. Molecular docking and mutational analyses suggested a novel binding mode in which the major specific contacts occur at the minor groove interacting with the strongly basic wing containing a cluster of three arginine residues.

TrmB is a transcriptional repressor of the hyperthermophilic archaeon Pyrococcus furiosus serving at least two operons. TrmB represses genes encoding an ABC transporter for trehalose and maltose (the TM system) with trehalose and maltose as inducers. TrmB also represses genes encoding another ABC transporter for maltodextrins (the MD system) with maltotriose and sucrose as inducers. Here we report that glucose which was also bound by TrmB acted as a corepressor (causing stronger repression) for both the TM and the MD system. Binding of glucose by TrmB was increased in the presence of TM promoter DNA. Maltose which acted as inducer for the TM system acted as a corepressor for the MD system intensifying repression. We propose that the differential conformational changes of TrmB in response to binding the different sugars governs the ability of TrmB to interact with the promoter region and represents a simple mechanism for selecting the usage of one carbon source over the other, reminiscent of catabolite repression in bacteria.

The crystal structure of TrmBL2 from the archaeon Pyrococcus furiosus shows an association of two pseudosymmetric dimers. The dimers follow the prototypical design of known bacterial repressors with two helix–turn–helix (HTH) domains binding to successive major grooves of the DNA. However, in TrmBL2, the two dimers are arranged at a mutual displacement of approximately 2 bp so that they associate with the DNA along the double-helical axis at an angle of approximately 80°.While the deoxyribose phosphate groups of the double-stranded DNA (dsDNA) used for co-crystallization are clearly seen in the electron density map, most of the nucleobases are averaged out. Refinement required to assume a superposition of at least three mutually displaced dsDNAs. The HTH domains interact primarily with the deoxyribose phosphate groups and polar interactions with the nucleobases are almost absent.This hitherto unseen mode of DNA binding by TrmBL2 seems to arise from nonoptimal protein–DNA contacts made by its four HTH domains resulting in a low-affinity, nonspecific binding to DNA.

The distribution of respiratory quinone electron carriers among cultivated organisms provides clues on both the taxonomy of their producers and the redox processes these are mediating. Our study of the quinone inventories of 25 archaeal species belonging to the phyla Eury-, Cren- and Thaumarchaeota facilitates their use as chemotaxonomic markers for ecologically important archaeal clades. Saturated and monounsaturated menaquinones with six isoprenoid units forming the alkyl chain may serve as chemotaxonomic markers for Thaumarchaeota. Other diagnostic biomarkers are thiophene-bearing quinones for Sulfolobales and methanophenazines as functional quinone analogues of the Methanosarcinales. The ubiquity of saturated menaquinones in the Archaea in comparison to Bacteria suggests that these compounds may represent an ancestral and diagnostic feature of the Archaea. Overlap between quinone compositions of distinct thermophilic and halophilic archaea and bacteria may indicate lateral gene transfer. The biomarker potential of thaumarchaeal quinones was exemplarily demonstrated on a water column profile of the Black Sea. Both, thaumarchaeal quinones and membrane lipids showed similar distributions with maxima at the chemocline. Quinone distributions indicate that Thaumarchaeota dominate respiratory activity at a narrow interval in the chemocline, while they contribute only 9% to the microbial biomass at this depth, as determined by membrane lipid analysis.

Transcription in Archaea is directed by a pol II-like RNA polymerase and homologues of TBP and TFIIB (TFB) but the crystal structure of the archaeal enzyme and the subunits involved in recruitment of RNA polymerase to the promoter-TBP-TFB-complex are unknown. We described here the cloning expression and purification of 11 bacterially expressed subunits of the Pyrococcus furiosus RNAP. Protein interactions of subunits with each other and of archaeal transcription factors TFB and TFB with RNAP subunits were studied by Far-Western blotting and reconstitution of subcomplexes from single subunits in solution. In silico comparison of a consensus sequence of archaeal RNAP subunits with the sequence of yeast pol II subunits revealed a high degree of conservation of domains of the enzymes forming the cleft and catalytic center of the enzyme. Interaction studies with the large subunits were complicated by the low solubility of isolated subunits B, A', and A'', but an interaction network of the smaller subunits of the enzyme was established. Far-Western analyses identified subunit D as structurally important key polypeptide of RNAP involved in interactions with subunits B, L, N, and P and revealed also a strong interaction of subunits E' and F. Stable complexes consisting of subunits E' and F, of D and L and a BDLNP-subcomplex were reconstituted and purified. Gel shift analyses revealed an association of the BDLNP subcomplex with promoter-bound TBP-TFB. These results suggest a major role of subunit B (Rpb2) in RNAP recruitment to the TBP-TFB promoter complex.

TrmB is the transcriptional repressor for the gene cluster of the trehalose/maltose ABC transporter of the hyperthermophilic archaea Thermococcus litoralis and Pyrococcus furiosus (malE or TM operon), with maltose and trehalose acting as inducers. We found that TrmB (the protein is identical in both organisms) also regulated the transcription of genes encoding a separate maltodextrin ABC transporter in P. furiosus (mdxE or MD operon) with maltotriose, longer maltodextrins and sucrose acting as inducers, but not with maltose or trehalose. In vitro transcription of the malE and the mdxE operons was inhibited by TrmB binding to the different operator sequences. Inhibition of the TM operon was released by maltose and trehalose whereas inhibition of the MD operon was released by maltotriose and larger maltodextrins as well as by sucrose. Scanning mutagenesis of the TM operator revealed the role of the palindromic TACTNNNAGTA sequence for TrmB recognition. TrmB exhibits a broad spectrum of sugar-binding specificity, binding maltose, sucrose, maltotriose and trehalose in decreasing order of affinity, half-maximal binding occurring at 20, 60, 250 and 500 microM substrate concentration respectively. Of all substrates, only maltose shows sigmoidal binding characteristics with a Hill coefficient of 2. As measured by molecular sieve chromatography and cross-linking TrmB behaved as dimer in dilute buffer solution at room temperature. We conclude that TrmB acts as a bifunctional transcriptional regulator acting on two different promoters and being differentially controlled by binding to different sugars. We believe this to represent a novel strategy of prokaryotic transcription regulation.

Transcription in the Archaea is carried out by RNA polymerases and transcription factors that are highly homologous to their eukaryotic counterparts, but little is known about the structural organization of the archaeal transcription complex. To address this, transcription initiation complexes have been formed with Pyrococcus furiosus transcription factors (TBP and TFB1), RNA polymerase, and a linear DNA fragment containing a strong promoter. The arrangement of proteins from base pair -35 to +20 (relative to the transcriptional start site) has been analyzed by photochemical protein-DNA cross-linking. TBP cross-links to the TATA box and TFB1 cross-links both upstream and downstream of the TATA box, as expected, but the sites of most prominent TFB1 cross-linking are located well downstream of the TATA box, reaching as far as the start site of transcription, suggesting a role for TFB1 in initiation of transcription that extends beyond polymerase recruitment. These cross-links indicate the transcription factor orientation in the initiation complex. The pattern of cross-linking of four RNA polymerase subunits (B, A', A", and H) to the promoter suggests a path for promoter DNA relative to the RNA polymerase surface in this archaeal transcription initiation complex. In addition, an unidentified protein approximately the size of TBP cross-links to the non-transcribed DNA strand near the upstream edge of the transcription bubble. Cross-linking is specific to the polymerase-containing initiation complex and requires the gdh promoter TATA box. The location of this protein suggests that it, like TFB1, could also have a role in transcription initiation following RNA polymerase recruitment.

The posttranscriptional processing of tRNA produces a diverse wealth of modified nucleotides (29, 30, 41), most of which occur at conserved RNA sequence locations in all three phylogenetic domains (4, 45). Many of the functional roles of these modifications, in addition to other factors, such as G-C and metal ion content, are associated with their influence on secondary and tertiary structures in RNA (1, 14, 43). Thus, RNA modifications offer an important means of mediation of RNA structure across the entire temperature range of natural habitats for microorganisms: in low-temperature organisms, a degree of conformational flexibility in tRNA must be maintained during translation, while in the case of thermophiles, protection against environmental temperatures which may exceed the melting point of unmodified base-paired stems is required (27, 50). For example, it has been shown with increases in growth temperature for a single species (2, 27, 51) or through comparison of closely related organisms growing optimally at different temperatures (32) that selected stabilizing tRNA modifications are associated with increased culture temperature. By contrast, in bacterial psychrophiles, low levels of modification have been reported, with the exception of dihydrouridine (10), a modified tRNA nucleoside which is associated with enhancement and maintenance of molecular flexibility at low temperatures (12). From a phylogenetic perspective, it is interesting that the nucleoside structural motifs used for RNA stabilization at higher temperatures are known to be different in bacterial thermophiles (13, 24) and archaeal thermophiles (17), but tRNA modifications in low-temperature archaea have not previously been examined. We report here a detailed study of the identities and levels of nucleoside modifications in unfractionated tRNA from the psychrotolerant archaeon Methanococcoides burtonii (20). Cultures were grown at 23°C (the optimum growth temperature) and at 4°C (closer to the natural habitat temperature of 1 to 2°C [20]) in order to examine the overall level of tRNA modifications in comparison with that in bacteria, as well as recently studied mesophilic and thermophilic methanococci (32), and to assess the influence of a significant reduction in culture temperature upon modification. For contrast within the archaeal domain, we examined tRNA from the hyperthermophile Stetteria hydrogenophila (25) cultured at 93°C, near the growth optimum of 95°C. In both cases nucleoside modifications were measured by analysis of total enzymatic digests of tRNA using combined LC/MS, a definitive method for structural identification of RNA nucleoside modifications (7, 39).

The archaeal transcriptional machinery is polymerase II (pol II)-like but does not require ATP or TFIIH for open complex formation. We have used enzymatic and chemical probes to follow the movement of Pyrococcus RNA polymerase (RNAP) along the glutamate dehydrogenase gene during transcription initiation and transition to elongation. RNAP was stalled between registers +5 and +20 using C-minus cassettes. The upstream edge of RNAP was in close contact with the archaeal transcription factors TATA box-binding protein/transcription factor B in complexes stalled at position +5. Movement of the downstream edge of the RNAP was not detected by exonuclease III footprinting until register +8. A first structural transition characterized by movement of the upstream edge of RNAP was observed at registers +6/+7. A major transition was observed at registers +10/+11. In complexes stalled at these positions also the downstream edge of RNA polymerase started translocation, and reclosure of the initially open complex occurred indicating promoter clearance. Between registers +11 and +20 both RNAP and transcription bubble moved synchronously with RNA synthesis. The distance of the catalytic center to the front edge of the exo III footprint was approximately 12 nucleotides in all registers. The size of the RNA-DNA hybrid in an early archaeal elongation complex was estimated between 9 and 12 nucleotides. For complexes stalled between positions +10 and +20 the size of the transcription bubble was around 17 nucleotides. This study shows characteristic mechanistic properties of the archaeal system and also similarities to prokaryotic RNAP and pol II.

Archaea have a eukaryotic type of transcriptional machinery containing homologues of the transcription factors TATA-binding protein (TBP) and TFIIB (TFB) and a pol II type of RNA polymerase, whereas transcriptional regulators identified in archaeal genomes have bacterial counterparts. We describe here a novel regulator of heat shock response, Phr, from the hyperthermophilic archaeon Pyrococcus furiosus that is conserved among Euryarchaeota. The protein specifically inhibited cell-free transcription of its own gene and from promoters of a small heat shock protein, Hsp20, and of an AAA(+) ATPase. Inhibition of transcription was brought about by abrogating RNA polymerase recruitment to the TBP/TFB promoter complex. Phr bound to a 29-bp DNA sequence overlapping the transcription start site. Three sequences conserved in the binding sites of Phr, TTTA at -10, TGGTAA at the transcription start site, and AAAA at position +10, were required for Phr binding and are proposed as consensus regulatory sequences of Pyrococcus heat shock promoters. Shifting the growth temperature from 95 to 103 degrees C caused a dramatic increase of mRNA levels for the aaa(+) atpase and phr genes, but expression of the Phr protein was only weakly stimulated. Our findings suggest that heat shock response in Archaea is negatively regulated by a mechanism involving binding of Phr to conserved sequences.

A novel methanogen, Methanosarcina baltica GS1-AT, DSM 14042, JCM 11281, was isolated from sediment at a depth of 241 m in the Gotland Deep of the Baltic Sea. Cells were irregular, monopolar monotrichous flagellated cocci 1.5-3 microm in diameter often occurring in pairs or tetrads. The catabolic substrates used included methanol, methylated amines, and acetate, but not formate or H2/CO2. Growth was observed in a temperature range between 4 degrees and 27 degrees C with an optimum at 25 degrees C. The doubling time with methanol as substrate was 84 h at 25 degrees C, 120 h at 9 degrees C, and 167 h at 4 degrees C. The doubling time with acetate as substrate was 252 h at 25 degrees C and 425 h at 20 degrees C. After the transfer of methanol-grown cultures, long lag phases were observed that lasted 15-20 days at 25 degrees C and 25 days at 4 degrees -9 degrees C. The NaCl optimum for growth was 2%-4%, and the fastest growth occurred within a pH range of 6.5-7.5. Analysis of the 16S rDNA sequence revealed that the strain was phylogenetically related to Methanosarcina. The sequence similarity to described species of95.7% and its physiological properties distinguished strain GS1-A(T) from all described species of the genus Methanosarcina.

The biochemical machinery involved in the processes of DNA replication, transcription, and translation shows a striking similarity and phylogenetic relationship to the equivalent machinery in eucarya. In particular, RNA polymerase (RNAP) and the basal transcriptional machinery of archaea share many properties with the eucaryal RNA polymerase II (RNAP II) transcription apparatus. Regulators of archaeal transcription repress initiation by preventing TFB/TBP access to the TATA-box region or RNAP recruitment to the transcription start site. The DNA-binding site of LrpA overlaps the RNAP-binding site, and DNA-bound LrpA inhibits transcription by blocking RNA polymerase recruitment. NrpR controls the transcription of the nif operon by binding cooperatively to two tandem operator sequences, OR1 and OR2, located downstream of the transcription start site. The stronger and promoter proximal NrpR-binding site (OR1) can mediate repression of nif transcription during growth on ammonia. Heat shock-induced upregulation of some TFB genes from haloarchaea and of TFB2 from Pyrococcus have been reported. In cell-free transcription reactions, the addition of the substrate (maltodextrins) of this transporter system causes TrmB to dissociate from the promoter and relieves inhibition of RNA synthesis. The lack of genetic systems in many archaea hampers analysis of transcriptional regulation in vivo. The striking similarity of the archaeal and eucaryal genetic machinery is described in this chapter.

Microbes are organisms which are well adapted to their habitat. Their survival depends on the regulation of gene expression levels in response to environmental signals. The most important step in regulation of gene expression takes place at the transcriptional level. This regulation is intriguing in Archaea because the eu-karyotic-like transcription apparatus is modulated by bacterial-like transcription regulators. The transcriptional regulator of mal operon (TrmB) family is well known as a very large group of regulators in Archaea with more than 250 members to date. One special feature of these regulators is that some of them can act as repressor, some as activator and others as both repressor and activator. This review gives a short updated overview of the TrmB family and their regulatory patterns in different Archaea as a lot of new data have been published on this topic since the last review from 2008.

Transcription in Archaea is initiated by association of a TATA box binding protein (TBP) with a TATA box. This interaction is stabilized by the binding of the transcription factor IIB (TFIIB) orthologue TFB. We show here that the RNA polymerase of the archaeon Methanococcus , in contrast to polymerase II, does not require hydrolysis of the β-γ bond of ATP for initiation of transcription and open complex formation on linearized DNA. Permanganate probing revealed that the archaeal open complex spanned at least the DNA region from −11 to −1 at a tRNA Val promoter. The Methanococcus TBP-TFB promoter complex protected the DNA region from −40 to −14 on the noncoding DNA strand and the DNA segment from −36 to −17 on the coding DNA strand from DNase I digestion. This DNase I footprint was extended only to the downstream end by the addition of the RNA polymerase to position +17 on the noncoding strand and to position +13 on the coding DNA strand.

A spore-forming, halophilic bacterium was isolated from surface sediment located on the beach of Palaeochori Bay near to a shallow water hydrothermal vent area, Milos, Greece. The bacterium, designated SH 714T, consisted of motile, strictly aerobic rods which contained an Orn-D-Glu type murein and a G+C content of 35 mol%. Thin sections showed a cell wall typical for Gram-positive bacteria; the peptidoglycan layer, however, was very thin. The Gram-reaction of the organism was negative. Comparative 16S rRNA gene sequencing demonstrated that the isolate represents a new line of descent within the spore-forming rods branching at the periphery of the rRNA group 1 Bacillus (Bacillus sensu stricto). The nearest phylogenetic neighbours of the unknown bacterium were Bacillus haloalkaliphilus, Marinococcus albus and Halobacillus species. Based on phylogenetic and phenotypic evidence it is proposed that the unknown bacterium be classified as Filobacillus milensis gen. nov., sp. nov. The type strain is SH 714T (= DSM 13259T = ATCC 700960T).

The archaeal transcriptional initiation machinery closely resembles core elements of the eukaryal polymerase II system. However, apart from the established basal archaeal transcription system, little is known about the modulation of gene expression in archaea. At present, no obvious eukaryal-like transcriptional regulators have been identified in archaea. Instead, we have previously isolated an archaeal gene, the Pyrococcus furiosus lrpA, that potentially encodes a bacterial-like transcriptional regulator. In the present study, we have for the first time addressed the actual involvement of an archaeal Lrp homologue in transcription modulation. For that purpose, we have produced LrpA in Escherichia coli. In a cell-free P. furiosus transcription system we used wild-type and mutated lrpA promoter fragments to demonstrate thai the purified LrpA negatively regulates its own transcription. In addition, gel retardation analyses revealed a single protein-DNA complex, in which LrpA appeared to be present in (at least) a tetrameric conformation. The location of the LrpA binding site was further identified by DNaseI and hydroxyl radical footprinting, indicating that LrpA binds to a 46-base pair sequence thai overlaps the transcriptional start site of its own promoter. The molecular basis of the transcription inhibition by LrpA is discussed.

RNA polymerase from the hyperthermophile archaeon Pyrococcus furiosus (Pfu) forms specific and transcriptionally active complexes with its conjugate transcription factors TBP (the archaeal TATA binding protein homolog) and TFB (the archaeal homolog of eukaryotic RNA polymerase II and III transcription factors TFIIB and Brf) at the Pfu glutamate dehydrogenase promoter. A photochemical crosslinking method was used to map the vicinity of the catalytic subunits of Pfu RNA polymerase to DNA locations distributed along the polymerase–promoter interface. The largest component of this archaeal polymerase is split into two subunits, A′ and A″, whose relatively sharp boundary of DNA crosslinking (probed on the transcribed strand) is centered five to six base pairs downstream of the transcriptional start site. A strong argument based on this information, on the well-defined homology between the core bacterial, archaeal and eukaryotic RNA polymerase subunits, and on the recently determined structure of a bacterial RNA polymerase specifies the directionality of DNA in the archaeal transcription complex and its trajectory downstream of the transcriptional start site.

The extreme sensitivity of many Archaea to oxygen is a major obstacle for their cultivation in the laboratory and the development of archaeal genetic exchange systems. The technique of Balch and Wolfe (1976) is suitable for the cultivation of anaerobic Archaea but involves time-consuming procedures such as the use of air locks and glove boxes. We describe here a procedure for the cultivation of anaerobic Archaea that is more convenient and faster and allows the preparation of liquid media without the use of an anaerobic chamber. When the reducing agent sodium sulfide (Na2S) was replaced by sodium sulfite (Na2SO3), anaerobic media could be prepared without protection from oxygen outside an anaerobic chamber. Exchange of the headspace of serum bottles by appropriate gases was sufficient to maintain anaerobic conditions in the culture media. Organisms that were unable to utilize sulfite as a source for cellular sulfur were supplemented with hydrogen sulfide. H2S was simply added to the headspace of serum bottles by a syringe. The use of H2S as a source for sulfur minimized the precipitation of cations by sulfide. Representatives of 12 genera of anaerobic Archaea studied here were able to grow in media prepared by this procedure. For the extremely oxygen-sensitive organism Methanococcus thermolithotrophicus, we show that plates could be prepared outside an anaerobic chamber when sulfite was used as reducing agent. The application of this method may faciliate the cultivation and handling of extreme anaerobic Archaea considerably.

Cell-free transcription of archaeal promoters is mediated by two archaeal transcription factors, aTBP and TFB, which are orthologues of the eukaryotic transcription factors TBP and TFIIB. Using the cell-free transcription system described for the hyperthermophilic Archaeon Pyrococcus furiosus by Hethke et al., the temperature limits and template topology requirements of archaeal transcription were investigated. aTBP activity was not affected after incubation for 1 hr at 100°. In contrast, the half-life of RNA polymerase activity was 23 min and that of TFB activity was 3 min. The half-life of a 328-nt RNA product was 10 min at 100°. Best stability of RNA was observed at pH 6, at 400 mm K-glutamate in the absence of Mg2+ ions. Physiological concentrations of K-glutamate were found to stabilize protein components in addition, indicating that salt is an important extrinsic factor contributing to thermostability. Both RNA and proteins were stabilized by the osmolyte betaine at a concentration of 1 m. The highest activity for RNA synthesis at 95° was obtained in the presence of 1 m betaine and 400 mm K-glutamate. Positively supercoiled DNA, which was found to exist in Pyrococcus cells, can be transcribed in vitro both at 70° and 90°. However, negatively supercoiled DNA was the preferred template at all temperatures tested. Analyses of transcripts from plasmid topoisomers harboring the glutamate dehydrogenase promoter and of transcription reactions conducted in the presence of reverse gyrase indicate that positive supercoiling of DNA inhibits transcription from this promoter.

The fermentative conversion of glucose in anaerobic hyperthermophilic Archaea is a variant of the classical Embden-Meyerhof pathway found in Bacteria and Eukarya. A major difference of the archaeal glycolytic pathway concerns the conversion of glyceraldehyde-3-phosphate. In the hyperthermophilic archaeon Pyrococcus furiosus, this reaction is catalyzed by an unique enzyme, glyceraldehyde-3-phosphate ferredoxin oxidoreductase (GAPOR). Here, we report the isolation, characterization, and transcriptional analysis of the GAPOR-encoding gene. GAPOR is related to a family of ferredoxin-dependent tungsten enzymes in (hyper)thermophilic Archaea and, in addition, to a hypothetical protein in Escherichia coli. Electron paramagnetic resonance analysis of the purified P. furiosus GAPOR protein confirms the anticipated involvement of tungsten in catalysis. During glycolysis in P. furiosus, GAPOR gene expression is induced, whereas the activity of glyceraldehyde-3-phosphate dehydrogenase is repressed. It is discussed that this unprecedented unidirectional reaction couple in the pyrococcal glycolysis and gluconeogenesis gives rise to a novel site of glycolytic regulation that might be widespread among Archaea.