Characterization of an Extremely Thermophilic Archaebacterium Isolated from a Black Smoker Polychaete (Paralvinella sp.) at the Juan de Fuca Ridge

New insights into thermostable iron-containing/activated alcohol dehydrogenases from hyperthermophiles

Alcohol dehydrogenase (ADH) is an important enzyme that catalyzes alcohol oxidation and/or aldehyde reduction. As one of NAD+-dependent ADH types, iron-containing/activated ADH (Fe-ADH) is ubiquitous in Bacteria, Archaea, and Eukaryotes, possessing a similar "tunnel-like" structure that is composed of a domain A in its N-terminus and a domain B in its C-terminus. A conserved "GGGS" sequence in the domain A of Fe-ADH associates with NAD+, and one conserved Asp residue and three conserved His residues in the domain B are its catalytic active sites by surrounding with Fe atom, suggesting that it might employ similar catalytic mechanism. Notably, all the biochemically characterized Fe-ADHs from hyperthermophiles that thrive in above 80 °C possess two unique characteristics that are absent in other Fe-ADHs: thermophilicity and thermostability, thereby demonstrating that they can oxidize alcohol and reduce aldehyde at high temperature. Considering these two unique characteristics, Fe-ADHs from hyperthermophiles are potentially industrial biocatalysts for alcohol and aldehyde biotransformation at high temperature. Herein, we reviewed structural and biochemical characteristics of Fe-ADHs from hyperthermophiles, focusing on similarity and difference between Fe-ADHs from hyperthermophiles and their homologs from non-hyperthermophiles, and between hyperthermophilic archaeal Fe-ADHs and bacterial homologs. Furthermore, we proposed future directions of Fe-ADHs from hyperthermophiles.

A moderately thermophilic origin of a novel family of marine group II euryarchaeota from deep ocean

Marine group II (MGII) is the most abundant planktonic heterotrophic archaea in the ocean. The evolutionary history of MGII archaea is elusive. In this study, 13 new MGII metagenome-assembled genomes were recovered from surface to the hadal zone in Challenger Deep of the Mariana Trench; four of them from the deep ocean represent a novel group. The optimal growth temperature (OGT) of the common ancestor of MGII has been estimated to be at about 60°C and OGTs of MGIIc, MGIIb, and MGIIa at 47°C-50ºC, 37°C-44ºC, and 30°C-37ºC, respectively, suggesting the adaptation of these species to different temperatures during evolution. The estimated OGT range of MGIIc was supported by experimental measurements of cloned β-galactosidase that showed optimal enzyme activity around 50°C. These results indicate that MGIIc may have originated from a common ancestor that lived in warm or even hot marine environment, such as hydrothermal vents.

Optimizing Strategies for Bio-Based Ethanol Production Using Genome-Scale Metabolic Modeling of the Hyperthermophilic Archaeon, Pyrococcus furiosus

A genome-scale metabolic model, encompassing a total of 623 genes, 727 reactions, and 865 metabolites, was developed for Pyrococcus furiosus, an archaeon that grows optimally at 100°C by carbohydrate and peptide fermentation. The model uses subsystem-based genome annotation, along with extensive manual curation of 237 gene-reaction associations including those involved in central carbon metabolism, amino acid metabolism, and energy metabolism. The redox and energy balance of P. furiosus was investigated through random sampling of flux distributions in the model during growth on disaccharides. The core energy balance of the model was shown to depend on high acetate production and the coupling of a sodium-dependent ATP synthase and membrane-bound hydrogenase, which generates a sodium gradient in a ferredoxin-dependent manner, aligning with existing understanding of P. furiosus metabolism. The model was utilized to inform genetic engineering designs that favor the production of ethanol over acetate by implementing an NADPH and CO-dependent energy economy. The P. furiosus model is a powerful tool for understanding the relationship between generation of end products and redox/energy balance at a systems-level that will aid in the design of optimal engineering strategies for production of bio-based chemicals and fuels. IMPORTANCE The bio-based production of organic chemicals provides a sustainable alternative to fossil-based production in the face of today's climate challenges. In this work, we present a genome-scale metabolic reconstruction of Pyrococcus furiosus, a well-established platform organism that has been engineered to produce a variety of chemicals and fuels. The metabolic model was used to design optimal engineering strategies to produce ethanol. The redox and energy balance of P. furiosus was examined in detail, which provided useful insights that will guide future engineering designs.

Formate and hydrogen in hydrothermal vents and their use by extremely thermophilic methanogens and heterotrophs

Extremely thermophilic methanogens in the Methanococci and heterotrophs in the Thermococci are common in deep-sea hydrothermal vents. All Methanococci use H₂ as an electron donor, and a few species can also use formate. Most Methanococci have a coenzyme F₄₂₀-reducing formate dehydrogenase. All Thermococci reduce S⁰ but have hydrogenases and produce H₂ in the absence of S⁰. Some Thermococci have formate hydrogenlyase (Fhl) that reversibly converts H₂ and CO₂ to formate or an NAD(P)⁺-reducing formate dehydrogenase (Nfd). Questions remain if Methanococci or Thermococci use or produce formate in nature, why only certain species can grow on or produce formate, and what the physiological role of formate is? Formate forms abiotically in hydrothermal fluids through chemical equilibrium with primarily H₂, CO₂, and CO and is strongly dependent upon H₂ concentration, pH, and temperature. Formate concentrations are highest in hydrothermal fluids where H₂ concentrations are also high, such as in ultramafic systems where serpentinization reactions occur. In nature, Methanococci are likely to use formate as an electron donor when H₂ is limiting. Thermococci with Fhl likely convert H₂ and CO₂ to formate when H₂ concentrations become inhibitory for growth. They are unlikely to grow on formate in nature unless formate is more abundant than H₂ in the environment. Nearly all Methanococci and Thermococci have a gene for at least one formate dehydrogenase catalytic subunit, which may be used to provide free formate for de novo purine biosynthesis. However, only species with a membrane-bound formate transporter can grow on or secrete formate. Interspecies H₂ transfer occurs between Thermococci and Methanococci. This and putative interspecies formate transfer may support Methanococci in low H₂ environments, which in turn may prevent growth inhibition of Thermococci by its own H₂. Future research directions include understanding when, where, and how formate is used and produced by these organisms in nature, and how transcription of Thermococci genes encoding formate-related enzymes are regulated.

Hydrogen Limitation and Syntrophic Growth among Natural Assemblages of Thermophilic Methanogens at Deep-sea Hydrothermal Vents

Thermophilic methanogens are common autotrophs at hydrothermal vents, but their growth constraints and dependence on H2 syntrophy in situ are poorly understood. Between 2012 and 2015, methanogens and H2-producing heterotrophs were detected by growth at 80°C and 55°C at most diffuse (7-40°C) hydrothermal vent sites at Axial Seamount. Microcosm incubations of diffuse hydrothermal fluids at 80°C and 55°C demonstrated that growth of thermophilic and hyperthermophilic methanogens is primarily limited by H2 availability. Amendment of microcosms with NH4 (+) generally had no effect on CH4 production. However, annual variations in abundance and CH4 production were observed in relation to the eruption cycle of the seamount. Microcosm incubations of hydrothermal fluids at 80°C and 55°C supplemented with tryptone and no added H2 showed CH4 production indicating the capacity in situ for methanogenic H2 syntrophy. 16S rRNA genes were found in 80°C microcosms from H2-producing archaea and H2-consuming methanogens, but not for any bacteria. In 55°C microcosms, sequences were found from H2-producing bacteria and H2-consuming methanogens and sulfate-reducing bacteria. A co-culture of representative organisms showed that Thermococcus paralvinellae supported the syntrophic growth of Methanocaldococcus bathoardescens at 82°C and Methanothermococcus sp. strain BW11 at 60°C. The results demonstrate that modeling of subseafloor methanogenesis should focus primarily on H2 availability and temperature, and that thermophilic H2 syntrophy can support methanogenesis within natural microbial assemblages and may be an important energy source for thermophilic autotrophs in marine geothermal environments.

Hydrogen Production and Enzyme Activities in the Hyperthermophile Thermococcus paralvinellae Grown on Maltose, Tryptone, and Agricultural Waste

Thermococcus may be an important alternative source of H2 in the hot subseafloor in otherwise low H2 environments such as some hydrothermal vents and oil reservoirs. It may also be useful in industry for rapid agricultural waste treatment and concomitant H2 production. Thermococcus paralvinellae grown at 82°C without sulfur produced up to 5 mmol of H2 L(-1) at rates of 5-36 fmol H2 cell(-1) h(-1) on 0.5% (wt vol(-1)) maltose, 0.5% (wt vol(-1)) tryptone, and 0.5% maltose + 0.05% tryptone media. Two potentially inhibiting conditions, the presence of 10 mM acetate and low pH (pH 5) in maltose-only medium, did not significantly affect growth or H2 production. Growth rates, H2 production rates, and cell yields based on H2 production were the same as those for Pyrococcus furiosus grown at 95°C on the same media for comparison. Acetate, butyrate, succinate, isovalerate, and formate were also detected as end products. After 100 h, T. paralvinellae produced up to 5 mmol of H2 L(-1) of medium when grown on up to 70% (vol vol(-1)) waste milk from cows undergoing treatment for mastitis with the bacterial antibiotic Ceftiofur and from untreated cows. The amount of H2 produced by T. paralvinellae increased with increasing waste concentrations, but decreased in P. furiosus cultures supplemented with waste milk above 1% concentration. All mesophilic bacteria from the waste milk that grew on Luria Bertani, Sheep's Blood (selective for Staphylococcus, the typical cause of mastitis), and MacConkey (selective for Gram-negative enteric bacteria) agar plates were killed by heat during incubation at 82°C. Ceftiofur, which is heat labile, was below the detection limit following incubation at 82°C. T. paralvinellae also produced up to 6 mmol of H2 L(-1) of medium when grown on 0.1-10% (wt vol(-1)) spent brewery grain while P. furiosus produced < 1 mmol of H2 L(-1). Twelve of 13 enzyme activities in T. paralvinellae showed significant (p < 0.05) differences across six different growth conditions; however, methyl viologen-dependent membrane hydrogenase activity remained constant across all media types. The results demonstrate the potential of at least some Thermococcus species to produce H2 if protein and α-glucosides are present as substrates.

Thermococcus paralvinellae sp. nov. and Thermococcus cleftensis sp. nov. of hyperthermophilic heterotrophs from deep-sea hydrothermal vents

Two heterotrophic hyperthermophilic strains, ES1T and CL1T, were isolated from Paralvinella sp. polychaete worms collected from active hydrothermal vent chimneys in the north-eastern Pacific Ocean. Both were obligately anaerobic and produced H2S in the presence of elemental sulfur and H2. Complete genome sequences are available for both strains. Phylogenetic analyses based on 16S rRNA gene sequences showed that the strains are more than 97 % similar to most other species of the genus Thermococcus . Therefore, overall genome relatedness index analyses were performed to establish that these strains are novel species. For each analysis, strain ES1T was determined to be most similar to Thermococcus barophilus MPT, while strain CL1T was determined to be most similar to Thermococcus sp. 4557. The average nucleotide identity scores for these strains were 84 % for strain ES1T and 81 % for strain CL1T, genome-to-genome direct comparison scores were 23 % for strain ES1T and 47 % for strain CL1T, and the species identification scores were 89 % for strain ES1T and 88 % for strain CL1T. For each analysis, strains ES1T and CL1T were below the species delineation cut-off. Therefore, based on their whole genome sequences, strains ES1T and CL1T are suggested to represent novel species of the genus Thermococcus for which the names Thermococcus paralvinellae sp. nov. and Thermococcus cleftensis sp. nov. are proposed, respectively. The type strains are ES1T ( = DSM 27261T = KACC 17923T) and CL1T ( = DSM 27260T = KACC 17922T).

Production of hydrogen from α-1,4- and β-1,4-linked saccharides by marine hyperthermophilic Archaea

Nineteen hyperthermophilic heterotrophs from deep-sea hydrothermal vents, plus the control organism Pyrococcus furiosus, were examined for their ability to grow and produce H₂ on maltose, cellobiose, and peptides and for the presence of the genes encoding proteins that hydrolyze starch and cellulose. All of the strains grew on these disaccharides and peptides and converted maltose and peptides to H₂ even when elemental sulfur was present as a terminal electron acceptor. Half of the strains had at least one gene for an extracellular starch hydrolase, but only P. furiosus had a gene for an extracellular β-1,4-endoglucanase. P. furiosus was serially adapted for growth on CF11 cellulose and H₂ production, which is the first reported instance of hyperthermophilic growth on cellulose, with a doubling time of 64 min. Cell-specific H₂ production rates were 29 fmol, 37 fmol, and 54 fmol of H₂ produced cell⁻¹ doubling⁻¹ on α-1,4-linked sugars, β-1,4-linked sugars, and peptides, respectively. The highest total community H₂ production rate came from growth on starch (2.6 mM H₂ produced h⁻¹). Hyperthermophilic heterotrophs may serve as an important alternate source of H₂ for hydrogenotrophic microorganisms in low-H₂ hydrothermal environments, and some are candidates for H₂ bioenergy production in bioreactors.

Abundances of hyperthermophilic autotrophic Fe(III) oxide reducers and heterotrophs in hydrothermal sulfide chimneys of the northeastern Pacific Ocean

The abundances of hyperthermophilic heterotrophs, methanogens, and autotrophic reducers of amorphous Fe(III) oxide in 18 samples of deep-sea hydrothermal vent sulfide chimneys of the Endeavour Segment were measured. The results indicate that conditions favor the growth of iron reducers toward the interiors of these deposits and that of heterotrophs toward the outer surfaces near high-temperature polychaete worms (Paralvinella sulfincola).

Molecular characterization of the recombinant iron-containing alcohol dehydrogenase from the hyperthermophilic Archaeon, Thermococcus strain ES1

The gene encoding a thermostable iron-containing alcohol dehydrogenase from Thermococcus Strain ES1 (ES1 ADH) was cloned, sequenced and expressed in Escherichia coli. The recombinant and native ES1 ADHs were purified using multistep column chromatography under anaerobic conditions. Both enzymes appeared to be homotetramers with a subunit size of 45+/-1 kDa as revealed by SDS-PAGE, which was close to the calculated value (44.8 kDa). The recombinant ADH contained 1.0+/-0.1 g-atom iron per subunit. Both enzymes were sensitive to oxygen with a half-life upon exposure to air of about 4 min. The recombinant enzyme exhibited a specific activity of 105+/-2 U mg(-1), which was very similar to that of the native enzyme (110+/-3 U mg(-1)). The optimal pH-values for both enzymes for ethanol oxidation and acetaldehyde reduction were 10.4 and 7.0, respectively. Both enzymes also showed similar temperature-dependent activities, and catalyzed the oxidation of primary alcohols, but there was no activity towards methanol and secondary alcohols. Kinetic parameters of the enzymes showed lower K (m)-values for acetaldehyde and NADPH and higher K (m)-values for ethanol and NADP(+). It is concluded that the gene encoding ES1 ADH was expressed successfully in E. coli. This is the first report of a fully active recombinant version of an iron-containing ADH from a hyperthermophile.

Growth of thermophilic and hyperthermophilic Fe(III)-reducing microorganisms on a ferruginous smectite as the sole electron acceptor

Recent studies have suggested that the structural Fe(III) within phyllosilicate minerals, including smectite and illite, is an important electron acceptor for Fe(III)-reducing microorganisms in sedimentary environments at moderate temperatures. The reduction of structural Fe(III) by thermophiles, however, has not previously been described. A wide range of thermophilic and hyperthermophilic Archaea and Bacteria from marine and freshwater environments that are known to reduce poorly crystalline Fe(III) oxides were tested for their ability to reduce structural (octahedrally coordinated) Fe(III) in smectite (SWa-1) as the sole electron acceptor. Two out of the 10 organisms tested, Geoglobus ahangari and Geothermobacterium ferrireducens, were not able to conserve energy to support growth by reduction of Fe(III) in SWa-1 despite the fact that both organisms were originally isolated with solid-phase Fe(III) as the electron acceptor. The other organisms tested were able to grow on SWa-1 and reduced 6.3 to 15.1% of the Fe(III). This is 20 to 50% less than the reported amounts of Fe(III) reduced in the same smectite (SWa-1) by mesophilic Fe(III) reducers. Two organisms, Geothermobacter ehrlichii and archaeal strain 140, produced copious amounts of an exopolysaccharide material, which may have played an active role in the dissolution of the structural iron in SWa-1 smectite. The reduction of structural Fe(III) in SWa-1 by archaeal strain 140 was studied in detail. Microbial Fe(III) reduction was accompanied by an increase in interlayer and octahedral charges and some incorporation of potassium and magnesium into the smectite structure. However, these changes in the major element chemistry of SWa-1 smectite did not result in the formation of an illite-like structure, as reported for a mesophilic Fe(III) reducer. These results suggest that thermophilic Fe(III)-reducing organisms differ in their ability to reduce and solubilize structural Fe(III) in SWa-1 smectite and that SWa-1 is not easily transformed to illite by these organisms.

Thermophily in the Geobacteraceae: Geothermobacter ehrlichii gen. nov., sp. nov., a novel thermophilic member of the Geobacteraceae from the "Bag City" hydrothermal vent

Little is known about the microbiology of the "Bag City" hydrothermal vent, which is part of a new eruption site on the Juan de Fuca Ridge and which is notable for its accumulation of polysaccharide on the sediment surface. A pure culture, designated strain SS015, was recovered from a vent fluid sample from the Bag City site through serial dilution in liquid medium with malate as the electron donor and Fe(III) oxide as the electron acceptor and then isolation of single colonies on solid Fe(III) oxide medium. The cells were gram-negative rods, about 0.5 micro m by 1.2 to 1.5 micro m, and motile and contained c-type cytochromes. Analysis of the 16S ribosomal DNA (rDNA) sequence of strain SS015 placed it in the family Geobacteraceae in the delta subclass of the Proteobacteria. Unlike previously described members of the Geobacteraceae, which are mesophiles, strain SS015 was a thermophile and grew at temperatures of between 35 and 65 degrees C, with an optimum temperature of 55 degrees C. Like many previously described members of the Geobacteraceae, strain SS015 grew with organic acids as the electron donors and Fe(III) or nitrate as the electron acceptor, with nitrate being reduced to ammonia. Strain SS015 was unique among the Geobacteraceae in its ability to use sugars, starch, or amino acids as electron donors for Fe(III) reduction. Under stress conditions, strain SS015 produced copious quantities of extracellular polysaccharide, providing a model for the microbial production of the polysaccharide accumulation at the Bag City site. The 16S rDNA sequence of strain SS015 was less than 94% similar to the sequences of previously described members of the Geobacteraceae; this fact, coupled with its unique physiological properties, suggests that strain SS015 represents a new genus in the family Geobacteraceae. The name Geothermobacter ehrlichii gen. nov., sp. nov., is proposed (ATCC BAA-635 and DSM 15274). Although strains of Geobacteraceae are known to be the predominant Fe(III)-reducing microorganisms in a variety of Fe(III)-reducing environments at moderate temperatures, strain SS015 represents the first described thermophilic member of the Geobacteraceae and thus extends the known environmental range of this family to hydrothermal environments.

Deferribacter desulfuricans sp. nov., a novel sulfur-, nitrate- and arsenate-reducing thermophile isolated from a deep-sea hydrothermal vent

A novel anaerobic, heterotrophic thermophile was isolated from a deep-sea hydrothermal vent chimney at the Suiyo Seamount in the Izu-Bonin Arc, Japan. The cells were bent, flexible rods, with a single polar flagellum. Growth was observed between 40 and 70 degrees C (optimum temperature: 60-65 degrees C; doubling time, 40 min) and between pH 5.0 and 7.5(optimum pH 6.5). The isolate was a strictly anaerobic heterotroph capable of using complex organic compounds (yeast extract, tryptone, peptone, casein and Casamino acids), ethanol and various organic acids as energy and carbon sources. Hydrogen could serve as a supplementary energy source. Elemental sulfur (S(0)), nitrate or arsenate was required for growth as an electron acceptor. The G + C content of the genomic DNA was 38.6 mol%. Phylogenetic analysis based on 16S rDNA sequences indicated that isolate SSM1(T) is closely related to Deferribacter thermophilus BMA(T) (98.1%). However, the novel isolate could be clearly differentiated from D. thermophilus BMA(T) on the basis of its physiological and genetic properties. The name Deferribacter desulfuricans sp. nov. (type strain SSM1(T) = JCM 11476(T) = DSM 14783(T)) is proposed.

Optimization of the growth conditions of the extremely thermophilic microorganisms Thermococcus celer and Pyrococcus woesei

Growth medium components and cultivation conditions for the extremely thermophilic Archaea Thermococcus celer and Pyrococcus woesei were optimized. A culture media based in marine water was formulated. Both Archaea demonstrated to be strictly anaerobic with optimal growth temperature of 85 degrees and 95 degrees C, respectively. Sodium sulfide, but not cysteine, was used as a sulfur and reductive capacity source. It was observed that hydrogen sulfide could be replaced by 30 microM titanium (III) nitrile acetate. The addition of elemental S(o) enhanced growth of both microorganisms, with T. celer far more sensitive than P. woesei to the absence of S(o). P. woesei utilized maltose as a carbon source, while T. celer was able to use only peptides from yeast extract, peptone and tryptone as its carbon source. Optimum carbon source concentrations were 1.25 g/L for T. celer and 5 g/L for P. woesei. Although both Archaea required peptides as a nitrogen source, the addition of ammonia chloride to a nitrogen-limited media did not stimulate growth, which suggests that neither Archaea appear to metabolize ammonia. The growth of P. woesei, but not T. celer, was stimulated considerably in the presence of iron. Co, Ni, Zn, Mo. Mn and Mg were essential trace elements needed for optimal growth of both bacteria.

Isolation and characterization of Thermococcus barossii, sp. nov., a hyperthermophilic archaeon isolated from a hydrothermal vent flange formation

A new hyperthermophilic microorganism, Thermococcus barossii, was isolated from rock fragments of a hydrothermal vent flange formation, located along the East Pacific Rise of the Juan de Fuca Ridge. This organism is obligately anaerobic and grows over a temperature range of at least 60-92 degrees C in artificial seawater-based media, containing elemental sulfur, tryptone and yeast extract. The addition of a maltooligosaccharide mixture and tungsten to this medium improved growth to some extent. At the Topt for growth (82.5 degrees C), cell densities as high as 4 x 10(8) cells/ml could be obtained in 18-liter batch fermentations, with a doubling time of approximately 40 minutes, if culture access to elemental sulfur was sufficient. In continuous culture at the same temperature, comparable cell densities could be obtained but only at slower growth rates. Morphologically, T. barossii is coccoid-shaped, forming irregularly-shaped spheres; under optimal conditions, these coccoids become more regular and smaller, a characteristic of other hyperthermophilic archaea. Negatively-stained preparations showed no pili or flagella associated with the cell surface. 16S rRNA sequencing reveals that T. barossii is most similar to Thermococcus celer (99.7%). Yet, further comparisons with T. celer showed that T. barossii is a new Thermococcus species: different growth temperature optimum (82.5 degrees C vs. 88 degrees C), obligate requirement for sulfur, higher G + C content (60% vs. 56.7%) and 47.7% DNA-DNA hybridization. The nucleotide and translated amino acid sequence for the gene encoding a DNA polymerase from T. barossii was compared to sequences of related genes from other Thermacoccales. The polymerase phylogenies were congruent with those obtained from the 16S rRNA phylogenetic analyses. Based on the high degree of similarity among members of the genus Termococcus for the criteria used thus far, aspects of enzymology may be an important mechanism of differenting one species from another.

Distribution of microorganisms in deep-sea hydrothermal vent chimneys investigated by whole-cell hybridization and enrichment culture of thermophilic subpopulations

The microbial community structure of hydrothermal vent chimneys was evaluated by the combined use of enrichment cultures and whole-cell hybridizations with fluorescently labeled 16S rRNA-based oligonucleotide probes. Chimneys were collected during the Microsmoke cruise on the Mid-Atlantic Ridge and were subsampled on board and stored under reduced conditions or fixed. For estimation of culturable thermophiles, selective media were inoculated by dilution series of the samples and incubated at 65, 80, and 95(deg)C. To analyze the microbial diversity of the samples, cells were extracted from the fixed chimney structure samples and hybridized with domain- and kingdom-specific probes. Quantification of the extracted cells was assessed by whole-cell hybridization on membrane filters. By both methods, the largest amounts of microorganisms were found in the upper and outer parts of the chimneys, although even the inner parts contained culturable and detectable amounts of cells. Different morphotypes of thermophilic and hyperthermophilic microorganisms were enriched and detected in samples. Our data clearly indicate that the morphological diversity observed by using whole-cell hybridization is much larger than that assessed by use of culture-based enrichments. This new approach, including culture-independent and -dependent methods to study hydrothermal vent chimneys, showed an uneven distribution of a diverse microbial community. Application of lower-level specific probes for known families and genera within each domain by our approach will be useful to reveal the real extent and nature of the chimney microbial diversity and to support cultivation attempts.

Characterization of UDP amino sugars as major phosphocompounds in the hyperthermophilic archaeon Pyrococcus furiosus

The archaeon Pyrococcus furiosus is a strictly anaerobic heterotroph that grows optimally at 100 degrees C by the fermentation of carbohydrates. It is known to contain high concentrations of novel intracellular solutes such as beta-mannosylglycerate and di-myo-inositol 1,1'-phosphate (DIP) (L. O. Martins and H. Santos, Appl. Environ. Microbiol. 61:3299-3303, 1995). Here, 31P nuclear magnetic resonance (NMR) spectroscopy was used to show that this organism also accumulates another type of phospho compound, as revealed by a major multiplet signal in the pyrophosphate region. The compounds were purified from cell extracts of P. furiosus by anion-exchange and gel filtration chromatographic procedures and were structurally analyzed by 1H, 13C, and 31P NMR spectroscopy. They were identified as two uridylated amino sugars, UDP N-acetylglucosamine and UDP N-acetylgalactosamine. Unambiguous characterizations and complete assignments of 1H and 13C resonances from such sugars have not been previously reported. In vitro 31P NMR spectroscopic analyses showed that, in contrast to DIP, which is maintained at a constant intracellular concentration (approximately 32 mM) throughout the growth phase of P. furiosus, the UDP amino sugars accumulated (to approximately 14 mM) only during the late log phase. The possible biochemical roles of these compounds in P. furiosus are discussed.

Characterization of 2-ketoisovalerate ferredoxin oxidoreductase, a new and reversible coenzyme A-dependent enzyme involved in peptide fermentation by hyperthermophilic archaea

Cell extracts of the proteolytic and hyperthermophilic archaea Thermococcus litoralis, Thermococcus sp. strain ES-1, Pyrococcus furiosus, and Pyrococcus sp. strain ES-4 contain an enzyme which catalyzes the coenzyme A-dependent oxidation of branched-chain 2-ketoacids coupled to the reduction of viologen dyes or ferredoxin. This enzyme, termed VOR (for keto-valine-ferredoxin oxidoreductase), has been purified from all four organisms. All four VORs comprise four different subunits and show amino-terminal sequence homology. T. litoralis VOR has an M(r) of ca. 230,000, with subunit M(r) values of 47,000 (alpha), 34,000 (beta), 23,000 (gamma), and 13,000 (delta). It contains about 11 iron and 12 acid-labile sulfide atoms and 13 cysteine residues per heterotetramer (alpha beta gamma delta), but thiamine pyrophosphate, which is required for catalytic activity, was lost during purification. The most efficient substrates (kcat/Km > 1.0 microM-1 s-1; Km < 100 microM) for the enzyme were the 2-ketoacid derivatives of valine, leucine, isoleucine, and methionine, while pyruvate and aryl pyruvates were very poor substrates (kcat/Km < 0.2 microM-1 s-1) and 2-ketoglutarate was not utilized. T. litoralis VOR also functioned as a 2-ketoisovalerate synthase at 85 degrees C, producing 2-ketoisovalerate and coenzyme A from isobutyryl-coenzyme A (apparent Km, 250 microM) and CO2 (apparent Km, 48 mM) with reduced viologen as the electron donor. The rate of 2-ketoisovalerate synthesis was about 5% of the rate of 2-ketoisovalerate oxidation. The optimum pH for both reactions was 7.0. A mechanism for 2-ketoisovalerate oxidation based on data from substrate-induced electron paramagnetic resonance spectra is proposed, and the physiological role of VOR is discussed.

Effects of elemental sulfur on the metabolism of the deep-sea hyperthermophilic archaeon Thermococcus strain ES-1: characterization of a sulfur-regulated, non-heme iron alcohol dehydrogenase

The strictly anaerobic archaeon Thermococcus strain ES-1 was recently isolated from near a deep-sea hydrothermal vent. It grows at temperatures up to 91 degrees C by the fermentation of peptides and reduces elemental sulfur (S(o)) to H2S. It is shown here that the growth rates and cell yields of strain ES-1 are dependent upon the concentration of S(o) in the medium, and no growth was observed in the absence of S(o). The activities of various catabolic enzymes in cells grown under conditions of sufficient and limiting S(o) concentrations were investigated. These enzymes included alcohol dehydrogenase (ADH); formate benzyl viologen oxidoreductase; hydrogenase; glutamate dehydrogenase; alanine dehydrogenase; aldehyde ferredoxin (Fd) oxidoreductase; formaldehyde Fd oxidoreductase; and coenzyme A-dependent, Fd-linked oxidoreductases specific for pyruvate, indolepyruvate, 2-ketoglutarate, and 2-ketoisovalerate. Of these, changes were observed only with ADH, formate benzyl viologen oxidoreductase, and hydrogenase, the specific activities of which all dramatically increased in cells grown under S(o) limitation. This was accompanied by increased amounts of H2 and alcohol (ethanol and butanol) from cultures grown with limiting S(o). Such cells were used to purify ADH to electrophoretic homogeneity. ADH is a homotetramer with a subunit M(r) of 46,000 and contains 1 g-atom of Fe per subunit, which, as determined by electron paramagnetic resonance analyses, is present as a mixture of ferrous and ferric forms. No other metals or acid-labile sulfide was detected by colorimetric and elemental analyses. ADH utilized NADP(H) as a cofactor and preferentially catalyzed aldehyde reduction. It is proposed that, under So limitation, ADH reduces to alcohols the aldehydes that are generated by fermentation, thereby serving to dispose of excess reductant.

Purification, characterization, and metabolic function of tungsten-containing aldehyde ferredoxin oxidoreductase from the hyperthermophilic and proteolytic archaeon Thermococcus strain ES-1

Thermococcus strain ES-1 is a strictly anaerobic, hyperthermophilic archaeon that grows at temperatures up to 91 degrees C by the fermentation of peptides. It is obligately dependent upon elemental sulfur (S(o)) for growth, which it reduces to H2S. Cell extracts contain high aldehyde oxidation activity with viologen dyes as electron acceptors. The enzyme responsible, which we term aldehyde ferredoxin oxidoreductase (AOR), has been purified to electrophoretic homogeneity. AOR is a homodimeric protein with a subunit M(r) of approximately 67,000. It contains molybdopterin and one W, four to five Fe, one Mg, and two P atoms per subunit. Electron paramagnetic resonance analyses of the reduced enzyme indicated the presence of a single [4Fe-4S]+ cluster with an S = 3/2 ground state. While AOR oxidized a wide range of aliphatic and aromatic aldehydes, those with the highest apparent kcat/Km values (> 10 microM-1S-1) were acetaldehyde, isovalerylaldehyde, and phenylacetaldehyde (Km values of < 100 microM). The apparent Km value for Thermococcus strain ES-1 ferredoxin was 10 microM (with crotonaldehyde as the substrate). Thermococcus strain ES-1 AOR also catalyzed the reduction of acetate (apparent Km of 1.8 mM) below pH 6.0 (with reduced methyl viologen as the electron donor) but at much less than 1% of the rate of the oxidative reaction (with benzyl viologen as the electron acceptor at pH 6.0 to 10.0). The properties of Thermococcus strain ES-1 AOR are very similar to those of AOR previously purified from the saccharolytic hyperthermophile Pyrococcus furiosus, in which AOR was proposed to oxidize glyceraldehyde as part of a novel glycolytic pathway (S. Mukund and M. W. W. Adams, J. Biol. Chem. 266:14208-14216, 1991). However, Thermococcus strain ES-1 is not known to metabolize carbohydrates, and glyceraldehyde was a very poor substrate (kcat/Km of < 0.2 microM-1S-1) for its AOR. The most efficient substrates for Thermococcus strain ES-1 AOR were the aldehyde derivatives of transaminated amino acids. This suggests that the enzyme functions to oxidize aldehydes generated during amino acid catabolism, although the possibility that AOR generates aldehydes from organic acids produced by fermentation cannot be ruled out.

Dense Community of Hyperthermophilic Sulfur-Dependent Heterotrophs in a Geothermally Heated Shallow Submarine Biotope near Kodakara-Jima Island, Kagoshima, Japan

Microbial communities in marine hydrothermal sediments (0 to 30 cm deep) in an inlet of Kodakara-Jima Island, Kagoshima, Japan, were studied with reference to environmental factors, especially the presence of amino acids. The study area was shallow, and the sea floor was covered with sand through which hot volcanic gas bubbled and geothermally heated water seeped out. The total bacterial density increased with depth in the sediments in parallel with a rise in the ambient temperature (80(deg)C at the surface and 104(deg)C at a depth of 30 cm in the sediments). As estimated by most-probable-number studies, hyperthermophilic sulfur-dependent heterotrophs growing at 90(deg)C dominated the microbial community (3 x 10(sup7) cells (middot) g of sediment(sup-1) at a depth of 30 cm in the sediments), followed in abundance by hyperthermophilic sulfur-dependent facultative autotrophs (3.3 x 10(sup2) cells (middot) g of sediment(sup-1)). The cooler sandy or rocky floor surrounding the hot spots was covered with white bacterial mats which consisted of large Beggiatoa-like filaments. Both the total organic carbon content, most of which was particulate (75% in the surface sediments), and the amino acid concentration in void seawater in the sediments decreased with depth. Amino acids, both hydrolyzable and free, constituted approximately 23% of the dissolved organic carbon in the surface sediments. These results indicate that a lower amino acid concentration is probably due to consumption by dense populations of hyperthermophilic sulfur-dependent heterotrophs, which require amino acids for their growth and thus create a gradient of amino acid concentration in the sediments. The role of primary producers, which supply essential amino acids to sustain this microbial community, is also discussed.

Hyperthermophilic life at deep-sea hydrothermal vents

The discovery of deep-sea hydrothermal vents in 1977 considerably modified the views on deep-sea biology. For the first time, an ecosystem totally based on primary production achieved by chemosynthetic bacteria was discovered. Besides the warm vents where dense invertebrate communities and their symbiotic bacteria are located, the "black smokers" venting fluids at temperatures up to 350 degrees C were also investigated by microbiologists. Several strains of hyperthermophilic Archaea (methanogens, sulfate-reducers, sulfur-reducers) were isolated from smokers and surrounding materials. Deep-sea isolates that have been totally described, have been assigned to new species, within genera previously found in coastal geothermally heated environments. However, some species appear to exist in both deep and shallow ecosystems. Some deep-sea hyperthermophiles appear to be adapted to hydrostatic pressure and showed a barophilic response. The distribution of hyperthermophiles in the hot ecosystems of the planet, and their adaptation to pressure are presented and discussed.

Metabolism in hyperthermophilic microorganisms

Hyperthermophilic microorganisms grow at temperatures of 90 degrees C and above and are a recent discovery in the microbial world. They are considered to be the most ancient of all extant life forms, and have been isolated mainly from near shallow and deep sea hydrothermal vents. All but two of the nearly twenty known genera are classified as Archaea (formerly archaebacteria). Virtually all of them are strict anaerobes. The majority are obligate heterotrophs that utilize proteinaceous materials as carbon and energy sources, although a few species are also saccharolytic. Most also depend on the reduction of elemental sulfur to hydrogen sulfide (H2S) for significant growth. Peptide fermentation involves transaminases and glutamate dehydrogenase, together with several unusual ferredoxin-linked oxidoreductases not found in mesophilic organisms. Similarly, a novel pathway based on a partially non-phosphorylated Entner-Doudoroff scheme has been postulated to convert carbohydrates to acetate, H2 and CO2, although a more conventional Embden-Meyerhof pathway has also been identified in one saccharolytic species. The few hypethermophiles known that can assimilate CO2 do so via a reductive citric acid cycle. Two S(o)-reducing enzymes termed sulfhydrogenase and sulfide dehydrogenase have been purified from the cytoplasm of a hyperthermophile that is able to grow either with or without S(o). A scheme for electron flow during the oxidation of carbohydrates and peptides and the reduction of S(o) has been proposed. However, the mechanisms by which S(o) reduction is coupled to energy conservation in this organism and in obligate S(o)-reducing hyperthermophiles is not known.

Deep-sea smokers: windows to a subsurface biosphere?

Since the discovery of hyperthermophilic microbial activity in hydrothermal fluids recovered from "smoker" vents on the East Pacific Rise, the widely accepted upper temperature limit for life (based on pure culture data) has risen from below the boiling point of water at atmospheric pressure to approximately 115 degrees C. Many microbiologists seem willing to speculate that the maximum may be closer to 150 degrees C. We have postulated not only higher temperatures than these (under deep-sea hydrostatic pressures), but also the existence of a biosphere subsurface to accessible seafloor vents. New geochemical information from the Endeavour Segment of the Juan de Fuca Ridge indicative of subsurface organic material caused us to re-examine both the literature on hyperthermophilic microorganisms cultured from deep-sea smoker environments and recent results of microbial sampling efforts at actively discharging smokers on the Endeavour Segment. Here we offer the case for a subsurface biosphere based on an interdisciplinary view of microbial and geochemical analyses of Endeavour smoker fluids, a case in keeping with rapidly evolving geophysical understanding of organic stability under deep-sea hydrothermal conditions.

Amino Acid Requirements of Two Hyperthermophilic Archaeal Isolates from Deep-Sea Vents, Desulfurococcus Strain SY and Pyrococcus Strain GB-D

Two sulfur-dependent hyperthermophilic archaea, Desulfurococcus strain SY and Pyrococcus strain GB-D, which were isolated from deep-sea hydrothermal vents, utilized free amino acids and peptides obtained from various molecular size fractions of yeast extract. It was found that 11 amino acids were essential for growth. The metabolic products were acetate, i -butyrate, and i -valerate.

Preliminary description and nutritional characterization of a chemoorganotrophic archaeobacterium growing at temperatures of up to 110 ° isolated from a submarine hydrothermal vent environment

Summary: An extremely thermophilic coccoid bacterium, designated strain ES4, was isolated from a flange (a newly described geological structure associated with massive sulphide mounds) at the Juan de Fuca Ridge hydrothermal vent system. The organism is a salt-requiring obligately anaerobic chemoorganotroph which reduces elemental sulphur but can grow very poorly in the absence of sulphur. Organic substrates utilized include yeast extract, peptone and amino acid hydrolysate as well as individual amino acids, the peptide Leu-Ser and starch. When growing on a defined medium, ES4 requires a supplement of vitamins and 20 amino acids at trace concentrations. Growth is most rapid in the temperature range 90-99 °C, with a maximum growth temperature of about 110 °C. In the optimal temperature range for growth, ES4 has a doubling time of about 1 h and can reach densities of 109 cells ml-1. Insensitivity to the antibiotics vancomycin, streptomycin and chloramphenicol, and the presence of di- and tetra-ether phytanyl lipids, indicate that ES4 is an archaeobacterium.