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  • 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
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  • 2
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    AAPG
    In:  In: Hydrocarbon migration and its near-surface expression. , ed. by Schumacher, D. and Abrams, M. A. AAPG Memoir, 66 . AAPG, Tulsa, Okla., pp. 169-171.
    Publication Date: 2018-03-29
    Description: Rates of petroleum seepage must ultimately be related to the rate of supply from below. This could be either from a leaking accumulation or directly from the source rock itself. However, many things can happen during migration to the surface, such that the relationship between trap leakage rates and surface seep rates remains obscure. We calculate the potential flux rates of gas leakage across seals and compare these with measurements of fluxes for three seepage sites on the European continental shelf. We conclude that seepage flow rates can be modeled effectively by assuming Poiseuille flow through the matrix of mudstone seals. Flow rates calculated in this way are about 0.4-1.0 m3 gas/m2/year, consistent with field observations.
    Type: Book chapter , NonPeerReviewed
    Format: text
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