@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 {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 {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 {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} }