@article {1718, title = {Hydrogen and thiosulfate limits for growth of a thermophilic, autotrophic Desulfurobacterium species from a deep-sea hydrothermal vent.}, journal = {Environ Microbiol Rep}, volume = {8}, year = {2016}, month = {2016 Apr}, pages = {196-200}, abstract = {

Hydrothermal fluids (341{\textdegree}C and 19{\textdegree}C) were collected < 1 m apart from a black smoker chimney and a tubeworm mound on the Boardwalk edifice at the Endeavour Segment in the northeastern Pacific Ocean to study anaerobic microbial growth in hydrothermal mineral deposits. Geochemical modelling of mixed vent fluid and seawater suggests the mixture was anoxic above 55{\textdegree}C and that low H2 concentrations (79 μmol kg(-1) in end-member hydrothermal fluid) limit anaerobic hydrogenotrophic growth above this temperature. A thermophilic, hydrogenotrophic sulfur reducer, Desulfurobacterium strain HR11, was isolated from the 19{\textdegree}C fluid raising questions about its H2 -dependent growth kinetics. Strain HR11 grew at 40-77{\textdegree}C (Topt 72-75{\textdegree}C), pH 5-8.5 (pHopt 6-7) and 1-5\% (wt vol(-1) ) NaCl (NaClopt 3-4\%). The highest growth rates occurred when S2 O3 (2-) and S{\textdegree} were reduced to H2 S. Modest growth occurred by NO3 (-) reduction. Monod constants for its growth were Ks of 30 μM for H2 and Ks of 20 μM for S2 O3 (2-) with a μmax of 2.0 h(-1) . The minimum H2 and S2 O3 (2-) concentrations for growth were 3 μM and 5 μM respectively. Possible sources of S2 O3 (2-) and S{\textdegree} are from abiotic dissolved sulfide and pyrite oxidation by O2 .

}, issn = {1758-2229}, doi = {10.1111/1758-2229.12368}, author = {Stewart, Lucy C and Llewellyn, James G and Butterfield, David A and Lilley, Marvin D and Holden, James F} } @article {1708, title = {Hydrogen Production and Enzyme Activities in the Hyperthermophile Thermococcus paralvinellae Grown on Maltose, Tryptone, and Agricultural Waste.}, journal = {Front Microbiol}, volume = {7}, year = {2016}, month = {2016}, pages = {167}, abstract = {

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{\textdegree}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{\textdegree}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{\textquoteright}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{\textdegree}C. Ceftiofur, which is heat labile, was below the detection limit following incubation at 82{\textdegree}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.

}, issn = {1664-302X}, doi = {10.3389/fmicb.2016.00167}, author = {Hensley, Sarah A and Moreira, Emily and Holden, James F} } @article {1728, title = {Complete genome sequence of the hyperthermophilic methanogen Methanocaldococcus bathoardescens JH146(T) isolated from the basalt subseafloor.}, journal = {Mar Genomics}, volume = {24 Pt 3}, year = {2015}, month = {2015 Dec}, pages = {229-30}, abstract = {

Methanocaldococcus bathoardescens JH146(T) is a hyperthermophilic and obligate hydrogenotrophic methanogen isolated from low-temperature (26 {\textdegree}C) hydrothermal vent fluid at Axial Seamount in the northeastern Pacific Ocean. It is most closely related to the N2-fixing methanogen Methanocaldococcus sp. FS406-22; however, they differ in that JH146 cannot fix N2 or reductively assimilate nitrate. In this study, we present the complete genome sequence of strain JH146(T) (1,607,556 bp) with its 1635 protein coding genes, and 41 RNA genes. Our analysis focuses on its methane production via the acetyl-CoA pathway and its deleted gene clusters related to nitrogen assimilation. This study extends our understanding of methanogenesis at high temperatures and the impact of these organisms on the biogeochemistry of subseafloor hydrothermal environments and the deep sea.

}, issn = {1876-7478}, doi = {10.1016/j.margen.2015.06.002}, author = {Kim, You-Tae and Jung, Jong-Hyun and Stewart, Lucy C and Kwon, Soon-Wo and Holden, James F and Park, Cheon-Seok} } @article {1737, title = {Methane cycling. Nonequilibrium clumped isotope signals in microbial methane.}, journal = {Science}, volume = {348}, year = {2015}, month = {2015 Apr 24}, pages = {428-31}, abstract = {

Methane is a key component in the global carbon cycle, with a wide range of anthropogenic and natural sources. Although isotopic compositions of methane have traditionally aided source identification, the abundance of its multiply substituted "clumped" isotopologues (for example, (13)CH3D) has recently emerged as a proxy for determining methane-formation temperatures. However, the effect of biological processes on methane{\textquoteright}s clumped isotopologue signature is poorly constrained. We show that methanogenesis proceeding at relatively high rates in cattle, surface environments, and laboratory cultures exerts kinetic control on (13)CH3D abundances and results in anomalously elevated formation-temperature estimates. We demonstrate quantitatively that H2 availability accounts for this effect. Clumped methane thermometry can therefore provide constraints on the generation of methane in diverse settings, including continental serpentinization sites and ancient, deep groundwaters.

}, keywords = {Animals, Carbon Cycle, Carbon Isotopes, Cattle, Groundwater, Hydrogen, Methane, Methanomicrobiales, Temperature}, issn = {1095-9203}, doi = {10.1126/science.aaa4326}, author = {Wang, David T and Gruen, Danielle S and Lollar, Barbara Sherwood and Hinrichs, Kai-Uwe and Stewart, Lucy C and Holden, James F and Hristov, Alexander N and Pohlman, John W and Morrill, Penny L and K{\"o}nneke, Martin and Delwiche, Kyle B and Reeves, Eoghan P and Sutcliffe, Chelsea N and Ritter, Daniel J and Seewald, Jeffrey S and McIntosh, Jennifer C and Hemond, Harold F and Kubo, Michael D and Cardace, Dawn and Hoehler, Tori M and Ono, Shuhei} } @article {1743, title = {Methanocaldococcus bathoardescens sp. nov., a hyperthermophilic methanogen isolated from a volcanically active deep-sea hydrothermal vent.}, journal = {Int J Syst Evol Microbiol}, volume = {65}, year = {2015}, month = {2015 Apr}, pages = {1280-3}, abstract = {

A hyperthermophilic methanogen, strain JH146(T), was isolated from 26 {\textdegree}C hydrothermal vent fluid emanating from a crack in basaltic rock at Marker 113 vent, Axial Seamount in the northeastern Pacific Ocean. It was identified as an obligate anaerobe that uses only H2 and CO2 for growth. Phylogenetic analysis based on 16S rRNA gene sequences showed that the strain is more than 97\% similar to other species of the genus Methanocaldococcus . Therefore, overall genome relatedness index analyses were performed to establish that strain JH146(T) represents a novel species. For each analysis, strain JH146(T) was most similar to Methanocaldococcus sp. FS406-22, which can fix N2 and also comes from Marker 113 vent. However, strain JH146(T) differs from strain FS406-22 in that it cannot fix N2. The average nucleotide identity score for strain JH146(T) was 87\%, the genome-to-genome direct comparison score was 33-55\% and the species identification score was 93\%. For each analysis, strain JH146(T) was below the species delineation cut-off. Full-genome gene synteny analysis showed that strain JH146(T) and strain FS406-22 have 97\% genome synteny, but strain JH146(T) was missing the operons necessary for N2 fixation and assimilatory nitrate reduction that are present in strain FS406-22. Based on its whole genome sequence, strain JH146(T) is suggested to represent a novel species of the genus Methanocaldococcus for which the name Methanocaldococcus bathoardescens is proposed. The type strain is JH146(T) ( = DSM 27223(T) = KACC 18232(T)).

}, keywords = {DNA, Bacterial, Hydrothermal Vents, Methanocaldococcus, Molecular Sequence Data, Pacific Ocean, Phylogeny, RNA, Ribosomal, 16S, Seawater, Sequence Analysis, DNA}, issn = {1466-5034}, doi = {10.1099/ijs.0.000097}, author = {Stewart, Lucy C and Jung, Jong-Hyun and Kim, You-Tae and Kwon, Soon-Wo and Park, Cheon-Seok and Holden, James F} } @article {1413, title = {Bioinformatic and biochemical analysis of a novel maltose-forming α-amylase of the GH57 family in the hyperthermophilic archaeon Thermococcus sp. CL1.}, journal = {Enzyme Microb Technol}, volume = {60}, year = {2014}, month = {2014 Jun 10}, pages = {9-15}, abstract = {

Maltose-forming \α-amylase is a glycoside hydrolase family 57 (GH57) member that is unique because it displays dual hydrolysis activity toward \α-1,4- and \α-1,6-glycosidic linkages and only recognizes maltose. This enzyme was previously identified only in Pyrococcus sp. ST04 (PSMA); however, we recently found two homologs subgroups in Thermococcus species. One subgroup (subgroup A) showed relatively high amino acid sequence similarity to PSMA (\>71\%), while the other subgroup (subgroup B) showed lower homology with PSMA (\<59\%). To characterize the subgroup B maltose-forming \α-amylase from Thermococcus species (TCMA), we cloned the CL1_0868 gene from Thermococcus sp. CL1 and then successfully expressed the gene in Escherichia coli. Although TCMA has a different oligomeric state relative to PSMA, TCMA showed similar substrate specificity. However, TCMA was shown to hydrolyze maltooligosaccharides more easily than PSMA. Also, TCMA displayed different optimum conditions depending on the glycosidic linkage of the substrate. TCMA had the highest activity at 85\°C and at pH 5.0 for \α-1,4-glycosidic linkage hydrolysis whereas it showed its maximal activity to cleave \α-1,6-glycosidic linkages at 98\°C and pH 6.0.

}, issn = {1879-0909}, doi = {10.1016/j.enzmictec.2014.03.009}, author = {Jeon, Eun-Jung and Jung, Jong-Hyun and Seo, Dong-Ho and Jung, Dong-Hyun and Holden, James F and Park, Cheon-Seok} } @article {1200, title = {Complete genome sequence of hyperthermophilic archaeon Thermococcus sp. ES1.}, journal = {J Biotechnol}, volume = {174C}, year = {2014}, month = {2014 Jan 25}, pages = {14-15}, abstract = {

Thermococcus sp. strain ES1 is an anaerobic, hyperthermophilic archaeon from a hydrothermal vent that catabolizes sugars and peptides and produces H2S from S{\textdegree}, H2, acetate and CO2 as its primary metabolites. We present the complete genome sequence of this strain (1,957,742bp) with a focus on its substrate utilization and metabolite production capabilities. The sequence will contribute to the development of heterotrophic archaea for bioenergy production and biogeochemical modeling in hydrothermal environments.

}, issn = {1873-4863}, doi = {10.1016/j.jbiotec.2014.01.022}, author = {Jung, Jong-Hyun and Kim, You-Tae and Jeon, Eun-Jung and Seo, Dong-Ho and Hensley, Sarah A and Holden, James F and Lee, Ju-Hoon and Park, Cheon-Seok} } @article {1201, title = {Identification and Characterization of an Archaeal Kojibiose Catabolic Pathway in the Hyperthermophilic Pyrococcus sp. Strain ST04.}, journal = {J Bacteriol}, volume = {196}, year = {2014}, month = {2014 Mar}, pages = {1122-31}, abstract = {

A unique gene cluster responsible for kojibiose utilization was identified in the genome of Pyrococcus sp. strain ST04. The proteins it encodes hydrolyze kojibiose, a disaccharide product of glucose caramelization, and form glucose-6-phosphate (G6P) in two steps. Heterologous expression of the kojibiose-related enzymes in Escherichia coli revealed that two genes, Py04_1502 and Py04_1503, encode kojibiose phosphorylase (designated PsKP, for Pyrococcus sp. strain ST04 kojibiose phosphorylase) and β-phosphoglucomutase (PsPGM), respectively. Enzymatic assays show that PsKP hydrolyzes kojibiose to glucose and β-glucose-1-phosphate (β-G1P). The Km values for kojibiose and phosphate were determined to be 2.53 {\textpm} 0.21 mM and 1.34 {\textpm} 0.04 mM, respectively. PsPGM then converts β-G1P into G6P in the presence of 6 mM MgCl2. Conversion activity from β-G1P to G6P was 46.81 {\textpm} 3.66 U/mg, and reverse conversion activity from G6P to β-G1P was 3.51 {\textpm} 0.13 U/mg. The proteins are highly thermostable, with optimal temperatures of 90{\textdegree}C for PsKP and 95{\textdegree}C for PsPGM. These results indicate that Pyrococcus sp. strain ST04 converts kojibiose into G6P, a substrate of the glycolytic pathway. This is the first report of a disaccharide utilization pathway via phosphorolysis in hyperthermophilic archaea.

}, issn = {1098-5530}, doi = {10.1128/JB.01222-13}, author = {Jung, Jong-Hyun and Seo, Dong-Ho and Holden, James F and Park, Cheon-Seok} } @article {1203, title = {Maltose-forming α-amylase from the hyperthermophilic archaeon Pyrococcus sp. ST04.}, journal = {Appl Microbiol Biotechnol}, volume = {98}, year = {2014}, month = {2014 Mar}, pages = {2121-31}, abstract = {

The deduced amino acid sequence from a gene of the hyperthermophilic archaeon Pyrococcus sp. ST04 (Py04_0872) contained a conserved glycoside hydrolase family 57 (GH57) motif, but showed <13~\% sequence identity with other known Pyrococcus GH57 enzymes, such as 4-α-glucanotransferase (EC 2.4.1.25), amylopullulanase (EC 3.2.1.41), and branching enzyme (EC 2.4.1.18). This gene was cloned and expressed in Escherichia coli, and the recombinant product (P yrococcus sp. ST04 maltose-forming α-amylase, PSMA) was a novel 70-kDa maltose-forming α-amylase. PSMA only recognized maltose (G2) units with α-1,4 and α-1,6 linkages in polysaccharides (e.g., starch, amylopectin, and glycogen) and hydrolyzed pullulan very poorly. G2 was the primary end product of hydrolysis. Branched cyclodextrin (CD) was only hydrolyzed along its branched maltooligosaccharides. 6-O-glucosyl-β-cyclodextrin (G1-β-CD) and β-cyclodextrin (β-CD) were resistant to PSMA suggesting that PSMA is an exo-type glucan hydrolase with α-1,4- and α-1,6-glucan hydrolytic activities. The half-saturation value (K m) for the α-1,4 linkage of maltotriose (G3) was 8.4~mM while that of the α-1,6 linkage of 6-O-maltosyl-β-cyclodextrin (G2-β-CD) was 0.3~mM. The k cat values were 381.0~min(-1) for G3 and 1,545.0~min(-1) for G2-β-CD. The enzyme was inhibited competitively by the reaction product G2, and the K i constant was 0.7~mM. PSMA bridges the gap between amylases that hydrolyze larger maltodextrins and α-glucosidase that feeds G2 into glycolysis by hydrolyzing smaller glucans into G2 units.

}, issn = {1432-0614}, doi = {10.1007/s00253-013-5068-6}, author = {Jung, Jong-Hyun and Seo, Dong-Ho and Holden, James F and Park, Cheon-Seok} } @article {1412, title = {Structural features underlying the selective cleavage of a novel exo-type maltose-forming amylase from Pyrococcus sp. ST04.}, journal = {Acta Crystallogr D Biol Crystallogr}, volume = {70}, year = {2014}, month = {2014 Jun}, pages = {1659-68}, abstract = {

A novel maltose-forming \α-amylase (PSMA) was recently found in the hyperthermophilic archaeon Pyrococcus sp. ST04. This enzyme shows \<13\% amino-acid sequence identity to other known \α-amylases and displays a unique enzymatic property in that it hydrolyzes both \α-1,4-glucosidic and \α-1,6-glucosidic linkages of substrates, recognizing only maltose units, in an exo-type manner. Here, the crystal structure of PSMA at a resolution of 1.8 \Å is reported, showing a tight ring-shaped tetramer with monomers composed of two domains: an N-domain (amino acids 1-341) with a typical GH57 family (\β/\α)7-barrel fold and a C-domain (amino acids 342-597) composed of \α-helical bundles. A small closed cavity observed in proximity to the catalytic residues Glu153 and Asp253 at the domain interface has the appropriate volume and geometry to bind a maltose unit, accounting for the selective exo-type maltose hydrolysis of the enzyme. A narrow gate at the putative subsite +1 formed by residue Phe218 and Phe452 is essential for specific cleavage of glucosidic bonds. The closed cavity at the active site is connected to a short substrate-binding channel that extends to the central hole of the tetramer, exhibiting a geometry that is significantly different from classical maltogenic amylases or \β-amylases. The structural features of this novel exo-type maltose-forming \α-amylase provide a molecular basis for its unique enzymatic characteristics and for its potential use in industrial applications and protein engineering.

}, keywords = {Amylases, Catalytic Domain, Maltose, Models, Molecular, Mutagenesis, Site-Directed, Protein Conformation, Proteolysis, Pyrococcus, Substrate Specificity}, issn = {1399-0047}, doi = {10.1107/S1399004714006567}, author = {Park, Kwang-Hyun and Jung, Jong-Hyun and Park, Sung-Goo and Lee, Myeong-Eun and Holden, James F and Park, Cheon-Seok and Woo, Eui-Jeon} } @article {1410, title = {Thermococcus paralvinellae sp. nov. and Thermococcus cleftensis sp. nov. of hyperthermophilic heterotrophs from deep-sea hydrothermal vents.}, journal = {Int J Syst Evol Microbiol}, volume = {64}, year = {2014}, month = {2014 Nov}, pages = {3655-9}, abstract = {

Two heterotrophic hyperthermophilic strains, ES1(T) and CL1(T), 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 ES1(T) was determined to be most similar to Thermococcus barophilus MP(T), while strain CL1(T) was determined to be most similar to Thermococcus sp. 4557. The average nucleotide identity scores for these strains were 84\% for strain ES1(T) and 81\% for strain CL1(T), genome-to-genome direct comparison scores were 23\% for strain ES1(T) and 47\% for strain CL1(T), and the species identification scores were 89\% for strain ES1(T) and 88\% for strain CL1(T). For each analysis, strains ES1(T) and CL1(T) were below the species delineation cut-off. Therefore, based on their whole genome sequences, strains ES1(T) and CL1(T) 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 ES1(T) ( =DSM 27261(T) =KACC 17923(T)) and CL1(T) ( =DSM 27260(T) =KACC 17922(T)).

}, keywords = {Animals, DNA, Archaeal, Hydrothermal Vents, Molecular Sequence Data, Pacific Ocean, Phylogeny, Polychaeta, RNA, Ribosomal, 16S, Sequence Analysis, DNA, Thermococcus}, issn = {1466-5034}, doi = {10.1099/ijs.0.066100-0}, author = {Hensley, Sarah A and Jung, Jong-Hyun and Park, Cheon-Seok and Holden, James F} } @article {1202, title = {Growth kinetics and energetics of a deep-sea hyperthermophilic methanogen under varying environmental conditions.}, journal = {Environ Microbiol Rep}, volume = {5}, year = {2013}, month = {2013 Oct}, pages = {665-71}, abstract = {

A hyperthermophilic deep-sea methanogen, Methanocaldococcus strain JH146, was isolated from 26{\textdegree}C hydrothermal fluid at Axial Volcano to model high temperature methanogenesis in the subseafloor. Emphasis was placed on defining growth kinetics, cell yields and growth energy demand (GE) across a range of conditions. The organism uses H2 and CO2 as its sole carbon and energy sources. At various temperatures, pHs, and chlorinities, its growth rates and cell yields co-varied while GE remained uniform at 1.69 {\texttimes} 10(-11) J cell(-1)s(-1) {\textpm} 0.68 {\texttimes} 10(-11) J cell(-1)s(-1) (s.d., n = 23). An exception was at superoptimal growth temperatures where GE increased to 7.25 {\texttimes} 10(-11) J cell(-1)s(-1) presumably due to heat shock. GE also increased from 5.1 {\texttimes} 10(-12) J cell(-1)s(-1) to 7.61 {\texttimes} 10(-11) J cell(-1)s(-1) as NH4 (+) concentrations decreased from 9.4 mM to 0.14 mM. JH146 did not fix N2 or assimilate NO3 (-), lacked the N2-fixing (cluster II) nifH gene, and became nitrogen limited below 0.14 mM NH4Cl. Nitrogen availability may impact growth in situ since ammonia concentrations at Axial Volcano are < 18 μM. Our approach contributes to refining bioenergetic and carbon flux models for methanogens and other organisms in hydrothermal vents and other environments.

}, issn = {1758-2229}, doi = {10.1111/1758-2229.12065}, author = {Ver Eecke, Helene C and Akerman, Nancy H and Huber, Julie A and Butterfield, David A and Holden, James F} } @article {1204, title = {Molecular cloning and enzymatic characterization of cyclomaltodextrinase from hyperthermophilic archaeon Thermococcus sp. CL1.}, journal = {J Microbiol Biotechnol}, volume = {23}, year = {2013}, month = {2013 Aug}, pages = {1060-9}, abstract = {

Genome organization near cyclomaltodextrinases (CDases) was analyzed and compared for four different hyperthermophilic archaea: Thermococcus, Pyrococcus, Staphylothermus, and Thermofilum. A gene (CL1_0884) encoding a putative CDase from Thermococcus sp. CL1 (tccd) was cloned and expressed in Escherichia coli. TcCD was confirmed to be highly thermostable, with optimal activity at 85{\textcelsius}. The melting temperature of TcCD was determined to be 93oC by both differential scanning calorimetry and differential scanning fluorimetry. A size-exclusion chromatography experiment showed that TcCD exists as a monomer. TcCD preferentially hydrolyzed α-cyclodextrin (α-CD), and at the initial stage catalyzed a ring-opening reaction by cleaving one α-1,4-glycosidic linkage of the CD ring to produce the corresponding single maltooligosaccharide. Furthermore, TcCD could hydrolyze branched CDs (G1-α-CD, G1-β- CD, and G2-β-CD) to yield significant amounts (45\%, 40\%, and 46\%) of isomaltooligosaccharides (panose and 6(2)-α-maltosylmaltose) in addition to glucose and maltose. This enzyme is one of the most thermostable maltogenic amylases reported, and might be of potential value in the production of isomaltooligosaccharides in the food industry.

}, issn = {1738-8872}, author = {Lee, Jae-Eun and Kim, In-Hwan and Jung, Jong-Hyun and Seo, Dong-Ho and Kang, Sung-Gyun and Holden, James F and Cha, Jaeho and Park, Cheon-Seok} } @article {1207, title = {Complete genome sequence of the hyperthermophilic archaeon Pyrococcus sp. strain ST04, isolated from a deep-sea hydrothermal sulfide chimney on the Juan de Fuca Ridge.}, journal = {J Bacteriol}, volume = {194}, year = {2012}, month = {2012 Aug}, pages = {4434-5}, abstract = {

Pyrococcus sp. strain ST04 is a hyperthermophilic, anaerobic, and heterotrophic archaeon isolated from a deep-sea hydrothermal sulfide chimney on the Endeavour Segment of the Juan de Fuca Ridge in the northeastern Pacific Ocean. To further understand the distinct characteristics of this archaeon at the genome level (polysaccharide utilization at high temperature and ATP generation by a Na(+) gradient), the genome of strain ST04 was completely sequenced and analyzed. Here, we present the complete genome sequence analysis results of Pyrococcus sp. ST04 and report the major findings from the genome annotation, with a focus on its saccharolytic and metabolite production potential.

}, keywords = {Adenosine Triphosphate, Anaerobiosis, DNA, Archaeal, Genome, Archaeal, Heterotrophic Processes, Hydrothermal Vents, Molecular Sequence Data, Pacific Ocean, Polysaccharides, Pyrococcus, Seawater, Sequence Analysis, DNA, Sodium Chloride, Sulfides}, issn = {1098-5530}, doi = {10.1128/JB.00824-12}, author = {Jung, Jong-Hyun and Lee, Ju-Hoon and Holden, James F and Seo, Dong-Ho and Shin, Hakdong and Kim, Hae-Yeong and Kim, Wooki and Ryu, Sangryeol and Park, Cheon-Seok} } @article {1205, title = {Complete genome sequence of the hyperthermophilic archaeon Thermococcus sp. strain CL1, isolated from a Paralvinella sp. polychaete worm collected from a hydrothermal vent.}, journal = {J Bacteriol}, volume = {194}, year = {2012}, month = {2012 Sep}, pages = {4769-70}, abstract = {

Thermococcus sp. strain CL1 is a hyperthermophilic, anaerobic, and heterotrophic archaeon isolated from a Paralvinella sp. polychaete worm living on an active deep-sea hydrothermal sulfide chimney on the Cleft Segment of the Juan de Fuca Ridge. To further understand the distinct characteristics of this archaeon at the genome level, its genome was completely sequenced and analyzed. Here, we announce the complete genome sequence (1,950,313 bp) of Thermococcus sp. strain CL1, with a focus on H(2)- and energy-producing capabilities and its amino acid biosynthesis and acquisition in an extreme habitat.

}, keywords = {Animals, Base Sequence, Chromosome Mapping, DNA, Archaeal, DNA, Ribosomal, Genome, Bacterial, Hydrothermal Vents, Molecular Sequence Data, Phylogeny, Polychaeta, Sequence Analysis, DNA, Thermococcus}, issn = {1098-5530}, doi = {10.1128/JB.01016-12}, author = {Jung, Jong-Hyun and Holden, James F and Seo, Dong-Ho and Park, Kwan-Hwa and Shin, Hakdong and Ryu, Sangryeol and Lee, Ju-Hoon and Park, Cheon-Seok} } @article {1206, title = {Hydrogen-limited growth of hyperthermophilic methanogens at deep-sea hydrothermal vents.}, journal = {Proc Natl Acad Sci U S A}, volume = {109}, year = {2012}, month = {2012 Aug 21}, pages = {13674-9}, abstract = {

Microbial productivity at hydrothermal vents is among the highest found anywhere in the deep ocean, but constraints on microbial growth and metabolism at vents are lacking. We used a combination of cultivation, molecular, and geochemical tools to verify pure culture H(2) threshold measurements for hyperthermophilic methanogenesis in low-temperature hydrothermal fluids from Axial Volcano and Endeavour Segment in the northeastern Pacific Ocean. Two Methanocaldococcus strains from Axial and Methanocaldococcus jannaschii showed similar Monod growth kinetics when grown in a bioreactor at varying H(2) concentrations. Their H(2) half-saturation value was 66 μM, and growth ceased below 17-23 μM H(2), 10-fold lower than previously predicted. By comparison, measured H(2) and CH(4) concentrations in fluids suggest that there was generally sufficient H(2) for Methanocaldococcus growth at Axial but not at Endeavour. Fluids from one vent at Axial (Marker 113) had anomalously high CH(4) concentrations and contained various thermal classes of methanogens based on cultivation and mcrA/mrtA analyses. At Endeavour, methanogens were largely undetectable in fluid samples based on cultivation and molecular screens, although abundances of hyperthermophilic heterotrophs were relatively high. Where present, Methanocaldococcus genes were the predominant mcrA/mrtA sequences recovered and comprised \~{}0.2-6\% of the total archaeal community. Field and coculture data suggest that H(2) limitation may be partly ameliorated by H(2) syntrophy with hyperthermophilic heterotrophs. These data support our estimated H(2) threshold for hyperthermophilic methanogenesis at vents and highlight the need for coupled laboratory and field measurements to constrain microbial distribution and biogeochemical impacts in the deep sea.

}, keywords = {Archaea, Biodiversity, Coculture Techniques, DNA, Ribosomal, Ecosystem, Gases, Geography, Hydrogen, Hydrothermal Vents, Kinetics, Methane, Molecular Sequence Data, Temperature, Time Factors, Water Microbiology}, issn = {1091-6490}, doi = {10.1073/pnas.1206632109}, author = {Ver Eecke, Helene C and Butterfield, David A and Huber, Julie A and Lilley, Marvin D and Olson, Eric J and Roe, Kevin K and Evans, Leigh J and Merkel, Alexandr Y and Cantin, Holly V and Holden, James F} } @article {1208, title = {Production of hydrogen from α-1,4- and β-1,4-linked saccharides by marine hyperthermophilic Archaea.}, journal = {Appl Environ Microbiol}, volume = {77}, year = {2011}, month = {2011 May}, pages = {3169-73}, abstract = {

Nineteen hyperthermophilic heterotrophs from deep-sea hydrothermal vents, plus the control organism Pyrococcus furiosus, were examined for their ability to grow and produce H$_{2}$ 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 H$_{2}$ 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 H$_{2}$ production, which is the first reported instance of hyperthermophilic growth on cellulose, with a doubling time of 64 min. Cell-specific H$_{2}$ production rates were 29 fmol, 37 fmol, and 54 fmol of H$_{2}$ produced cell$^{-}${\textonesuperior} doubling$^{-}${\textonesuperior} on α-1,4-linked sugars, β-1,4-linked sugars, and peptides, respectively. The highest total community H$_{2}$ production rate came from growth on starch (2.6 mM H$_{2}$ produced h$^{-}${\textonesuperior}). Hyperthermophilic heterotrophs may serve as an important alternate source of H$_{2}$ for hydrogenotrophic microorganisms in low-H$_{2}$ hydrothermal environments, and some are candidates for H$_{2}$ bioenergy production in bioreactors.

}, keywords = {Archaea, Carbohydrate Metabolism, Hot Springs, Hydro-Lyases, Hydrogen, Peptides, Seawater}, issn = {1098-5336}, doi = {10.1128/AEM.01366-10}, author = {Oslowski, Daniel M and Jung, Jong-Hyun and Seo, Dong-Ho and Park, Cheon-Seok and Holden, James F} } @article {1209, title = {Abundances of hyperthermophilic autotrophic Fe(III) oxide reducers and heterotrophs in hydrothermal sulfide chimneys of the northeastern Pacific Ocean.}, journal = {Appl Environ Microbiol}, volume = {75}, year = {2009}, month = {2009 Jan}, pages = {242-5}, abstract = {

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).

}, keywords = {Animals, Biodiversity, Ferric Compounds, Hot Springs, Methane, Oxidation-Reduction, Pacific Ocean, Polychaeta, Seawater}, issn = {1098-5336}, doi = {10.1128/AEM.01462-08}, author = {Ver Eecke, Helene C and Kelley, Deborah S and Holden, James F} } @article {1210, title = {Constraints on anaerobic respiration in the hyperthermophilic Archaea Pyrobaculum islandicum and Pyrobaculum aerophilum.}, journal = {Appl Environ Microbiol}, volume = {74}, year = {2008}, month = {2008 Jan}, pages = {396-402}, abstract = {

Pyrobaculum islandicum uses iron, thiosulfate, and elemental sulfur for anaerobic respiration, while Pyrobaculum aerophilum uses iron and nitrate; however, the constraints on these processes and their physiological mechanisms for iron and sulfur reduction are not well understood. Growth rates on sulfur compounds are highest at pH 5 to 6 and highly reduced (<-420-mV) conditions, while growth rates on nitrate and iron are highest at pH 7 to 9 and more-oxidized (>-210-mV) conditions. Growth on iron expands the known pH range of growth for both organisms. P. islandicum differs from P. aerophilum in that it requires direct contact with insoluble iron oxide for growth, it did not produce any extracellular compounds when grown on insoluble iron, and it lacked 2,6-anthrahydroquinone disulfonate oxidase activity. Furthermore, iron reduction in P. islandicum appears to be completely independent of c-type cytochromes. Like that in P. aerophilum, NADH-dependent ferric reductase activity in P. islandicum increased significantly in iron-grown cultures relative to that in non-iron-grown cultures. Proteomic analyses showed that there were significant increases in the amounts of a putative membrane-bound thiosulfate reductase in P. islandicum cultures grown on thiosulfate relative to those in cultures grown on iron and elemental sulfur. This is the first evidence of this enzyme being used in either a hyperthermophile or an archaeon. Pyrobaculum arsenaticum and Pyrobaculum calidifontis also grew on Fe(III) citrate and insoluble iron oxide, but only P. arsenaticum could grow on insoluble iron without direct contact.

}, keywords = {Anaerobiosis, FMN Reductase, Hydrogen-Ion Concentration, Iron, Nitrates, Oxidation-Reduction, Pyrobaculum, Species Specificity, Sulfur, Sulfurtransferases, Thiosulfates}, issn = {1098-5336}, doi = {10.1128/AEM.02033-07}, author = {Feinberg, Lawrence F and Srikanth, R and Vachet, Richard W and Holden, James F} } @article {1212, title = {Characterization of malate dehydrogenase from the hyperthermophilic archaeon Pyrobaculum islandicum.}, journal = {Extremophiles}, volume = {11}, year = {2007}, month = {2007 Sep}, pages = {741-6}, abstract = {

Native and recombinant malate dehydrogenase (MDH) was characterized from the hyperthermophilic, facultatively autotrophic archaeon Pyrobaculum islandicum. The enzyme is a homotetramer with a subunit mass of 33 kDa. The activity kinetics of the native and recombinant proteins are the same. The apparent K ( m ) values of the recombinant protein for oxaloacetate (OAA) and NADH (at 80 degrees C and pH 8.0) were 15 and 86 microM, respectively, with specific activity as high as 470 U mg(-1). Activity decreased more than 90\% when NADPH was used. The catalytic efficiency of OAA reduction by P. islandicum MDH using NADH was significantly higher than that reported for any other archaeal MDH. Unlike other archaeal MDHs, specific activity of the P. islandicum MDH back-reaction also decreased more than 90\% when malate and NAD(+) were used as substrates and was not detected with NADP(+). A phylogenetic tree of 31 archaeal MDHs shows that they fall into 5 distinct groups separated largely along taxonomic lines suggesting minimal lateral mdh transfer between Archaea.

}, keywords = {Citric Acid Cycle, Hydrogen-Ion Concentration, Kinetics, Malate Dehydrogenase, Malates, Molecular Weight, NAD, NADP, Oxaloacetic Acid, Phylogeny, Protein Conformation, Protein Subunits, Pyrobaculum, Recombinant Proteins, Sequence Analysis, Protein, Substrate Specificity, Temperature}, issn = {1431-0651}, doi = {10.1007/s00792-007-0081-2}, author = {Yennaco, Lynda J and Hu, Yajing and Holden, James F} } @article {1214, title = {Characterization of dissimilatory Fe(III) versus NO3- reduction in the hyperthermophilic archaeon Pyrobaculum aerophilum.}, journal = {J Bacteriol}, volume = {188}, year = {2006}, month = {2006 Jan}, pages = {525-31}, abstract = {

The hyperthermophilic archaeon Pyrobaculum aerophilum used 20 mM Fe(III) citrate, 100 mM poorly crystalline Fe(III) oxide, and 10 mM KNO3 as terminal electron acceptors. The two forms of iron were reduced at different rates but with equal growth yields. The insoluble iron was reduced when segregated spatially by dialysis tubing, indicating that direct contact with the iron was not necessary for growth. When partitioned, there was no detectable Fe(III) or Fe(II) outside of the tubing after growth, suggesting that an electron shuttle, not a chelator, may be used as an extracellular mediator of iron reduction. The addition of 25 and 50\% (vol vol(-1)) cell-free spent insoluble iron media to fresh media led to growth without a lag phase. Liquid chromatography analysis of spent media showed that cultures grown in iron, especially insoluble iron, produced soluble extracellular compounds that were absent or less abundant in spent nitrate medium. NADH-dependent ferric reductase activity increased approximately 100-fold, while nitrate reductase activity decreased 10-fold in whole-cell extracts from iron-grown cells relative to those from nitrate-grown cells, suggesting that dissimilatory iron reduction was regulated. A novel 2,6-anthrahydroquinone disulfonate oxidase activity was more than 580-fold higher in iron-grown cells than in nitrate-grown cells. The activity was primarily (>95\%) associated with the membrane cellular fraction, but its physiological function is unknown. Nitrate-grown cultures produced two membrane-bound, c-type cytochromes that are predicted to be monoheme and part of nitrite reductase and a bc1 complex using genome analyses. Only one cytochrome was present in cells grown on Fe(III) citrate whose relative abundance was unchanged.

}, keywords = {Cytochromes c, Ferric Compounds, FMN Reductase, Hot Temperature, NAD, Nitrates, Oxidation-Reduction, Pyrobaculum}, issn = {0021-9193}, doi = {10.1128/JB.188.2.525-531.2006}, author = {Feinberg, Lawrence F and Holden, James F} } @article {1213, title = {Citric acid cycle in the hyperthermophilic archaeon Pyrobaculum islandicum grown autotrophically, heterotrophically, and mixotrophically with acetate.}, journal = {J Bacteriol}, volume = {188}, year = {2006}, month = {2006 Jun}, pages = {4350-5}, abstract = {

The hyperthermophilic archaeon Pyrobaculum islandicum uses the citric acid cycle in the oxidative and reductive directions for heterotrophic and autotrophic growth, respectively, but the control of carbon flow is poorly understood. P. islandicum was grown at 95 degrees C autotrophically, heterotrophically, and mixotrophically with acetate, H2, and small amounts of yeast extract and with thiosulfate as the terminal electron acceptor. The autotrophic growth rates and maximum concentrations of cells were significantly lower than those in other media. The growth rates on H2 and 0.001\% yeast extract with and without 0.05\% acetate were the same, but the maximum concentration of cells was fourfold higher with acetate. There was no growth with acetate if 0.001\% yeast extract was not present, and addition of H2 to acetate-containing medium greatly increased the growth rates and maximum concentrations of cells. P. islandicum cultures assimilated 14C-labeled acetate in the presence of H2 and yeast extract with an efficiency of 55\%. The activities of 11 of 19 enzymes involved in the central metabolism of P. islandicum were regulated under the three different growth conditions. Pyruvate synthase and acetate:coenzyme A (CoA) ligase (ADP-forming) activities were detected only in heterotrophically grown cultures. Citrate synthase activity decreased in autotrophic and acetate-containing cultures compared to the activity in heterotrophic cultures. Acetylated citrate lyase, acetate:CoA ligase (AMP forming), and phosphoenolpyruvate carboxylase activities increased in autotrophic and acetate-containing cultures. Citrate lyase activity was higher than ATP citrate synthase activity in autotrophic cultures. These data suggest that citrate lyase and AMP-forming acetate:CoA ligase, but not ATP citrate synthase, work opposite citrate synthase to control the direction of carbon flow in the citric acid cycle.

}, keywords = {Acetates, Carbon Dioxide, Citric Acid, Citric Acid Cycle, Culture Media, Deuterium, Ligases, Lyases, Pyrobaculum, Pyruvate Synthase, Substrate Specificity}, issn = {0021-9193}, doi = {10.1128/JB.00138-06}, author = {Hu, Yajing and Holden, James F} } @article {1215, title = {Identification of 2D-gel proteins: a comparison of MALDI/TOF peptide mass mapping to mu LC-ESI tandem mass spectrometry.}, journal = {J Am Soc Mass Spectrom}, volume = {14}, year = {2003}, month = {2003 Sep}, pages = {957-70}, abstract = {

A comparative analysis of protein identification for a total of 162 protein spots separated by two-dimensional gel electrophoresis from two fully sequenced archaea, Methanococcus jannaschii and Pyrococcus furiosus, using MALDI-TOF peptide mass mapping (PMM) and mu LC-MS/MS is presented. 100\% of the gel spots analyzed were successfully matched to the predicted proteins in the two corresponding open reading frame databases by mu LC-MS/MS while 97\% of them were identified by MALDI-TOF PMM. The high success rate from the PMM resulted from sample desalting/concentrating with ZipTip(C18) and optimization of several PMM search parameters including a 25 ppm average mass tolerance and the application of two different protein molecular weight search windows. By using this strategy, low-molecular weight (<23 kDa) proteins could be identified unambiguously with less than 5 peptide matches. Nine percent of spots were identified as containing multiple proteins. By using mu LC-MS/MS, 50\% of the spots analyzed were identified as containing multiple proteins. mu LC-MS/MS demonstrated better protein sequence coverage than MALDI-TOF PMM over the entire mass range of proteins identified. MALDI-TOF and PMM produced unique peptide molecular weight matches that were not identified by mu LC-MS/MS. By incorporating amino acid sequence modifications into database searches, combined sequence coverage obtained from these two complimentary ionization methods exceeded 50\% for approximately 70\% of the 162 spots analyzed. This improved sequence coverage in combination with enzymatic digestions of different specificity is proposed as a method for analysis of post-translational modification from 2D-gel separated proteins.

}, keywords = {Amino Acid Sequence, Chromatography, Liquid, Databases, Protein, Electrophoresis, Gel, Two-Dimensional, Methanococcus, Molecular Sequence Data, Molecular Weight, Peptide Mapping, Proteins, Pyrococcus furiosus, Sensitivity and Specificity, Software, Spectrometry, Mass, Electrospray Ionization, Spectrometry, Mass, Matrix-Assisted Laser Desorption-Ionization, Trypsin}, issn = {1044-0305}, author = {Lim, Hanjo and Eng, Jimmy and Yates, John R and Tollaksen, Sandra L and Giometti, Carol S and Holden, James F and Adams, Michael W W and Reich, Claudia I and Olsen, Gary J and Hays, Lara G} } @article {1216, title = {Microbe-metal interactions in marine hydrothermal environments.}, journal = {Curr Opin Chem Biol}, volume = {7}, year = {2003}, month = {2003 Apr}, pages = {160-5}, abstract = {

Marine hydrothermal microorganisms respond rapidly to changes in the concentrations and availability of metals within their environment. Hyperthermophilic archaea appear to possess novel mechanisms for metal detoxification, dissimilatory metal reduction and metal assimilation that may be absent in their mesophilic and bacterial counterparts. For example, tungsten was found in high concentrations in a hydrothermal sulfide deposit where hyperthermophiles were also most abundant, consistent with the unique requirement of these organisms for this element. Furthermore, newly isolated genera of iron-reducing hyperthermophiles expand the scope of carbon cycling in hydrothermal environments. The advent of genome sequences and new molecular techniques will facilitate our further understanding of microbe-mineral interactions in these environments.

}, keywords = {Archaea, Bacteria, Environment, Marine Biology, Metals, Seawater, Temperature}, issn = {1367-5931}, author = {Holden, James F and Adams, Michael W W} }