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  • 110-672A; 122-762B; 122-762C; 127-797B; DRILL; Drilling/drill rig; Japan Sea; Joides Resolution; Leg110; Leg122; Leg127; Ocean Drilling Program; ODP; South Atlantic Ocean; South Indian Ridge, South Indian Ocean  (1)
  • 2,2-Dimethylbutane; 2,3-Methylpentane; Al-Wajh Deep; Area/locality; Atlantis II Deep; DEPTH, sediment/rock; Elevation of event; Ethane; Ethene; Event label; Gas chromatography; Gases, dissolved; GIK/IfG; GIK17022-2; GIK17032-1; GIK17036-1; GIK17036-2; GIK17037-2; GIK17037-4; GIK17038-16; GIK17038-5; GIK17038-7; GIK17038-8; GIK17038-9; GIK17040-2; GIK17041-2; Institute for Geosciences, Christian Albrechts University, Kiel; i-Propanol; Isobutane; KAL; Kasten corer; Kebrit Deep; Latitude of event; Longitude of event; Methane; MUC; MultiCorer; n-Butane; n-Hexane; North Al-Wajh Deeps; Optional event label; Propane; Red Sea; ROTES MEER; Sample mass; SO121; SO121_16; SO121_48; SO121_58; SO121_59; SO121_62; SO121_64; SO121_70; SO121_72; SO121_75; SO121_76; SO121_86; SO121_91; SO121_93; SO121_96; SO121-96; Sonne; Umm Lajj Deep  (1)
  • Stetteria hydrogenophila  (1)
  • 1995-1999  (3)
Document type
Keywords
Publisher
Years
  • 1995-1999  (3)
Year
  • 1
    ISSN: 1433-4909
    Keywords: Key words Hyperthermophilic ; Crenarchaeota ; Hydrogen and sulfur dependence ; Hydrothermal ; Stetteria hydrogenophila
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology
    Notes: Abstract A new hyperthermophilic, strictly anaerobic crenarchaeote, Stetteria hydrogenophila DSM11227 representing a new genus within the family of Desulfurococcaceae, was isolated from the sediment of a marine hydrothermal system at Paleohori Bay in Milos, Greece. Cells are gram-negative irregular and disc-shaped cocci, 0.5–1.5 μm in diameter, which are flagellate and can form cytoplasmatic protrusions up to 2 μm in length. The strain grew optimally at 95°C at pH 6.0 and at a NaCl concentration of 3%. The organism grew mixotrophically on peptide substrates. It required elemental sulfur as an external electron acceptor, and in addition, its growth was completely dependent on the presence of molecular hydrogen. Sulfur could be replaced by thiosulfate. H2S, CO2, acetate, and ethanol were identified as products of metabolism. The G + C content of DNA was 65 mol%. Analysis of its phylogenetic position by sequence analysis of 16S rRNA placed this organism in the family of Desulfurococcaceae. The dependence of this organism on both hydrogen and sulfur during growth on peptide substrates distinguishes Stetteria from all previously described species of Crenarchaeota.
    Type of Medium: Electronic Resource
    Location Call Number Limitation Availability
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  • 2
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    PANGAEA
    In:  Supplement to: Nähr, Thomas H; Botz, Reiner; Bohrmann, Gerhard; Schmidt, Mark (1998): Oxygen isotopic composition of low-temperature authigenic clinoptilolite. Earth and Planetary Science Letters, 160(3-4), 369-381, https://doi.org/10.1016/S0012-821X(98)00097-1
    Publication Date: 2024-01-09
    Description: Oxygen isotope ratios were obtained from authigenic clinoptilolites from Barbados Accretionary Complex, Yamato Basin, and Exmouth Plateau sediments (ODP Sites 672, 797, and 762) in order to investigate the isotopic fractionation between clinoptilolite and pore water at early diagenetic stages and low temperatures. Dehydrated clinoptilolites display isotopic ratios for the zeolite framework (delta 18Of) that extend from +18.7 per mil to +32.8 per mil (vs. SMOW). In combination with associated pore water isotope data, the oxygen isotopic fractionation between clinoptilolite and pore fluids could be assessed in the temperature range from 25ºC to 40ºC. The resulting fractionation factors of 1.032 at 25ºC and 1.027 at 40ºC are in good agreement with the theoretically determined oxygen isotope fractionation between clinoptilolite and water. Calculations of isotopic temperatures illustrate that clinoptilolite formation occurred at relatively low temperatures of 17ºC to 29ºC in Barbados Ridge sediments and at 33ºC to 62ºC in the Yamato Basin. These data support a low-temperature origin of clinoptilolite and contradict the assumption that elevated temperatures are the main controlling factor for authigenic clinoptilolite formation. Increasing clinoptilolite delta18Of values with depth indicate that clinoptilolites which are now in the deeper parts of the zeolite-bearing intervals had either formed at lower temperatures (17-20ºC) or under closed system conditions.
    Keywords: 110-672A; 122-762B; 122-762C; 127-797B; DRILL; Drilling/drill rig; Japan Sea; Joides Resolution; Leg110; Leg122; Leg127; Ocean Drilling Program; ODP; South Atlantic Ocean; South Indian Ridge, South Indian Ocean
    Type: Dataset
    Format: application/zip, 3 datasets
    Location Call Number Limitation Availability
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  • 3
    Publication Date: 2024-06-26
    Keywords: 2,2-Dimethylbutane; 2,3-Methylpentane; Al-Wajh Deep; Area/locality; Atlantis II Deep; DEPTH, sediment/rock; Elevation of event; Ethane; Ethene; Event label; Gas chromatography; Gases, dissolved; GIK/IfG; GIK17022-2; GIK17032-1; GIK17036-1; GIK17036-2; GIK17037-2; GIK17037-4; GIK17038-16; GIK17038-5; GIK17038-7; GIK17038-8; GIK17038-9; GIK17040-2; GIK17041-2; Institute for Geosciences, Christian Albrechts University, Kiel; i-Propanol; Isobutane; KAL; Kasten corer; Kebrit Deep; Latitude of event; Longitude of event; Methane; MUC; MultiCorer; n-Butane; n-Hexane; North Al-Wajh Deeps; Optional event label; Propane; Red Sea; ROTES MEER; Sample mass; SO121; SO121_16; SO121_48; SO121_58; SO121_59; SO121_62; SO121_64; SO121_70; SO121_72; SO121_75; SO121_76; SO121_86; SO121_91; SO121_93; SO121_96; SO121-96; Sonne; Umm Lajj Deep
    Type: Dataset
    Format: text/tab-separated-values, 315 data points
    Location Call Number Limitation Availability
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