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  • Accession number, genetics; Area/locality; Candidate Divisions; Endmember fluid portion; Epsilonproteobacteria; fish; Gene name; Hydrogen; Hydrogen sulfide; Iron 2+; Iron 3+; low-temperature hydrothermal fluids; M64/1; M64/1_Lilliput-hydrothermal-field; M68/1; M68/1_Lilliput-hydrothermal-field; MARSUED2; MARSUED3; Meteor (1986); Methane; microbial community; Mid-Atlantic Ridge; pH; Remote operated vehicle QUEST; ROVQ; Sampling date; sulfur oxidation; Temperature, water; Thiomicrospira; δ13C, methane  (1)
  • Anaerobic sulfide oxidation  (1)
Document type
Keywords
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Years
  • 1
    ISSN: 1432-072X
    Keywords: Phototrophic bacteria ; Ectothiorhodospira vacuolata ; Gas vacuoles ; Alkaliphilic bacteria ; Halophilic bacteria ; Anaerobic sulfide oxidation
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology
    Notes: Abstract A new phototrophic bacterium was isolated from Jordanian and Kenyan alkaline salt lakes. Cells are rod shaped, 1.5 μm wide and 2–4 μm long, and motile by polar flagella. They divide by binary fission, and possess photosynthetic membranes as lamellar stacks similar to those in the other species of the genus Ectothiorhodospira and the brown colored Rhodospirillum species. The presence of bacteriochlorophyll a and carotenoids of the normal spirilloxanthin series is indicated by the absorption spectra of living cells. Under certain growth conditions the cells form gas vacuoles, may become immotile and float to the top of the culture medium. Sulfide and thiosulfate are used as photosynthetic electron donors. During the oxidation of sulfide to sulfate, elemental sulfur is formed, which is accumulated outside the cells. The organisms are strictly anaerobic, do not require vitamins, are moderately halophilic and need alkaline pH-values for growth. The new species Ectothiorhodospira vacuolata is proposed.
    Type of Medium: Electronic Resource
    Location Call Number Limitation Availability
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  • 2
    Publication Date: 2024-02-02
    Description: Hydrothermal vent fluids were sampled with a pumped flow-through system with PFA sampling bottles (Kiel Pumping System KIPS) by the ROV QUEST. Fuid chemical parameters were determined immediately after sample recovery. Ph was measured at 20°C in unfiltered sample aliquots. Sulfide concentrations were measured colorimetrcally following the methylene blue method. Fe(II) and Fe(III) was measured colorimetrically with the phenantroline assay. Total Fe was measured by reducing all Fe(III) to Fe(II) with ascorbic acid. Fe(III) was calculated from the diffrence between Fe(II) and total Fe. Light dissolved hydrocharbons were analysed on board applying a purge and trap technique. Dissolved hydrogen was mesured onboard by a GC equipped with a PDD. Stable carbon isotope signatures of methane were analysed using coupled gas chromatography-combustion-isotope ration mass spectrometry. The abundance of bacterial and archaeal taxa was investigated by sequencing of the 16S rRNA gene. The diversity of the cbbL, cbbM and aclb was investigated by sequencing of the genes.
    Keywords: Accession number, genetics; Area/locality; Candidate Divisions; Endmember fluid portion; Epsilonproteobacteria; fish; Gene name; Hydrogen; Hydrogen sulfide; Iron 2+; Iron 3+; low-temperature hydrothermal fluids; M64/1; M64/1_Lilliput-hydrothermal-field; M68/1; M68/1_Lilliput-hydrothermal-field; MARSUED2; MARSUED3; Meteor (1986); Methane; microbial community; Mid-Atlantic Ridge; pH; Remote operated vehicle QUEST; ROVQ; Sampling date; sulfur oxidation; Temperature, water; Thiomicrospira; δ13C, methane
    Type: Dataset
    Format: text/tab-separated-values, 42 data points
    Location Call Number Limitation Availability
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