Bahr, André; Pape, Thomas; Bohrmann, Gerhard; Mazzini, Adriano; Haeckel, Matthias; Reitz, Anja; Ivanov, Michael (2009): Mineralogical, geochemical, and lipid biomarker study of cabonate precipitates at station GeoB9908-1. PANGAEA, https://doi.org/10.1594/PANGAEA.743257, Supplement to: Bahr, A et al. (2009): Authigenic carbonate precipitates from the NE Black Sea: a mineralogical, geochemical, and lipid biomarker study. International Journal of Earth Sciences, 98, 677-695, https://doi.org/10.1007/s00531-007-0264-1
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Carbonate precipitates recovered from 2,000 m water depth at the Dolgovskoy Mound (Shatsky Ridge, north eastern Black Sea) were studied using mineralogical, geochemical and lipid biomarker analyses. The carbonates differ in shape from simple pavements to cavernous structures with thick microbial mats attached to their lower side and within cavities. Low d13C values measured on carbonates (-41 to -32 per mill V-PDB) and extracted lipid biomarkers indicate that anaerobic oxidation of methane (AOM) played a crucial role in precipitating these carbonates. The internal structure of the carbonates is dominated by finely laminated coccolith ooze and homogeneous clay layers, both cemented by micritic high-magnesium calcite (HMC), and pure, botryoidal, yellowish low-magnesium calcite (LMC) grown in direct contact to microbial mats. d18O measurements suggest that the authigenic HMC precipitated in equilibrium with the Black Sea bottom water while the yellowish LMC rims have been growing in slightly 18O-depleted interstitial water. Although precipitated under significantly different environmental conditions, especially with respect to methane availability, all analysed carbonate samples show lipid patterns that are typical for ANME-1 dominated AOM consortia, in the case of the HMC samples with significant contributions of allochthonous components of marine and terrestrial origin, reflecting the hemipelagic nature of the primary sediment.
Median Latitude: 44.017417 * Median Longitude: 36.689583 * South-bound Latitude: 44.016000 * West-bound Longitude: 36.689167 * North-bound Latitude: 44.018833 * East-bound Longitude: 36.690000
Date/Time Start: 2005-06-15T01:00:00 * Date/Time End: 2005-06-15T03:23:00
GeoB9908-1 (BS346GR) * Latitude Start: 44.016000 * Longitude Start: 36.689167 * Latitude End: 44.018833 * Longitude End: 36.690000 * Date/Time Start: 2005-06-15T01:00:00 * Date/Time End: 2005-06-15T03:23:00 * Elevation Start: -1985.0 m * Elevation End: -2004.0 m * Location: Dolgovskoy mound * Campaign: TTR-15 * Basis: Professor Logachev * Method/Device: Television-Grab (TVG) * Comment: 0,5 t
Datasets listed in this publication series
- Bahr, A; Pape, T; Bohrmann, G et al. (2009): (Table 3) Concentrations and δ¹³C values of selected compounds from diverse source organisms as well as concentrations of compound classes of sample A-2 at station GeoB9908-1. https://doi.org/10.1594/PANGAEA.743248
- Bahr, A; Pape, T; Bohrmann, G et al. (2009): (Table 2) Stable carbon and oxygen isotope of station GeoB9908-1. https://doi.org/10.1594/PANGAEA.743242
- Bahr, A; Pape, T; Bohrmann, G et al. (2009): Sulphate concentration, Mg/Ca ratio, Cl- content and δ¹⁸O of interstitial water from station GeoB9908-1. https://doi.org/10.1594/PANGAEA.743251
- Bahr, A; Pape, T; Bohrmann, G et al. (2009): (Table 1) XRD and geochemical bulk sediment analyses on specific lithological facies of station GeoB9908-1. https://doi.org/10.1594/PANGAEA.743241