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  • 2010-2014  (54)
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  • 1
    Keywords: Datensammlung
    Description / Table of Contents: High-resolution sedimentary records of major and minor elements (Al, Ba, Ca, Sr, Ti), total organic carbon (TOC), and profiles of pore water constituents (SO42-, CH4, Ca2+, Ba2+, Mg2+, alkalinity) were obtained for two gravity cores (core 755, 501 m water depth and core 214, 1686 m water depth) from the northwestern Black Sea. The records were examined in order to gain insight into the cycling of Ba in anoxic marine sediments characterized by a shallow sulfate-methane transition (SMT) as well as the applicability of barite as a primary productivity proxy in such a setting. The Ba records are strongly overprinted by diagenetic barite (BaSO4) precipitation and remobilization; authigenic Ba enrichments were found at both sites at and slightly above the current SMT. Transport reaction modeling was applied to simulate the migration of the SMT during the changing geochemical conditions after the Holocene seawater intrusion into the Black Sea. Based on this, sediment intervals affected by diagenetic Ba redistribution were identified. Results reveal that the intense overprint of Ba and Baxs (Ba excess above detrital average) strongly limits its correlation to primary productivity. These findings have implications for other modern and ancient anoxic basins, such as sections covering the Oceanic Anoxic Events for which Ba is frequently used as a primary productivity indicator. Our study also demonstrates the limitations concerning the use of Baxs as a tracer for downward migrations of the SMT: due to high sedimentation rates at the investigated sites, diagenetic barite fronts are buried below the SMT within a relatively short period. Thus, 'relict' barite fronts would only be preserved for a few thousands of years, if at all.〈br〉〈br〉REFERENCE:〈br〉Blumenberg, Martin; Seifert, Richard; Kasten, Sabine; Bahlmann, E; Michaelis, Walter (2009): Euphotic zone bacterioplankton sources major bacteriohopanepolyols in the Holocene Black Sea. Geochimica et Cosmochimica Acta, 73(3), 750-766
    Type of Medium: Online Resource
    Pages: 4 Datasets , Format: application/zip
    Language: English
    Note: This dataset is supplement to doi:10.1016/j.gca.2012.04.021 , This dataset is cited by doi:10.1016/j.gca.2008.11.005
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  • 2
    Publication Date: 2017-05-19
    Description: The geochemical cycling of barium was investigated in sediments of pockmarks of the northern Congo Fan, characterized by surface and subsurface gas hydrates, chemosynthetic fauna, and authigenic carbonates. Two gravity cores retrieved from the so-called Hydrate Hole and Worm Hole pockmarks were examined using high-resolution pore-water and solid-phase analyses. The results indicate that, although gas hydrates in the study area are stable with respect to pressure and temperature, they are and have been subject to dissolution due to methane-undersaturated pore waters. The process significantly driving dissolution is the anaerobic oxidation of methane (AOM) above the shallowest hydrate-bearing sediment layer. It is suggested that episodic seep events temporarily increase the upward flux of methane, and induce hydrate formation close to the sediment surface. AOM establishes at a sediment depth where the upward flux of methane from the uppermost hydrate layer counterbalances the downward flux of seawater sulfate. After seepage ceases, AOM continues to consume methane at the sulfate/methane transition (SMT) above the hydrates, thereby driving the progressive dissolution of the hydrates “from above”. As a result the SMT migrates downward, leaving behind enrichments of authigenic barite and carbonates that typically precipitate at this biogeochemical reaction front. Calculation of the time needed to produce the observed solid-phase barium enrichments above the present-day depths of the SMT served to track the net downward migration of the SMT and to estimate the total time of hydrate dissolution in the recovered sediments. Methane fluxes were higher, and the SMT was located closer to the sediment surface in the past at both sites. Active seepage and hydrate formation are inferred to have occurred only a few thousands of years ago at the Hydrate Hole site. By contrast, AOM-driven hydrate dissolution as a consequence of an overall net decrease in upward methane flux seems to have persisted for a considerably longer time at the Worm Hole site, amounting to a few tens of thousands of years.
    Type: Article , PeerReviewed
    Format: text
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  • 3
    Publication Date: 2015-11-24
    Description: High-resolution sedimentary records of major and minor elements (Al, Ba, Ca, Sr, Ti), total organic carbon (TOC), and profiles of pore water constituents (View the MathML sourceSO42-, CH4, Ca2+, Ba2+, Mg2+, alkalinity) were obtained for two gravity cores (core 755, 501 m water depth and core 214, 1686 m water depth) from the northwestern Black Sea. The records were examined in order to gain insight into the cycling of Ba in anoxic marine sediments characterized by a shallow sulfate–methane transition (SMT) as well as the applicability of barite as a primary productivity proxy in such a setting. The Ba records are strongly overprinted by diagenetic barite (BaSO4) precipitation and remobilization; authigenic Ba enrichments were found at both sites at and slightly above the current SMT. Transport reaction modeling was applied to simulate the migration of the SMT during the changing geochemical conditions after the Holocene seawater intrusion into the Black Sea. Based on this, sediment intervals affected by diagenetic Ba redistribution were identified. Results reveal that the intense overprint of Ba and Baxs (Ba excess above detrital average) strongly limits its correlation to primary productivity. These findings have implications for other modern and ancient anoxic basins, such as sections covering the Oceanic Anoxic Events which Ba is frequently used as a primary productivity indicator. Our study also demonstrates the limitations concerning the use of Baxs as a tracer for downward migrations of the SMT: due to high sedimentation rates at the investigated sites, diagenetic barite fronts are buried below the SMT within a relatively short period. Thus, ‘relict’ barite fronts would only be preserved for a few thousands of years, if at all.
    Type: Article , PeerReviewed
    Format: text
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  • 4
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    PANGAEA
    In:  Supplement to: Fischer, David; Sahling, Heiko; Nöthen, Kerstin; Bohrmann, Gerhard; Zabel, Matthias; Kasten, Sabine (2012): Interaction between hydrocarbon seepage, chemosynthetic communities, and bottom water redox at cold seeps of the Makran accretionary prism: insights from habitat-specific pore water sampling and modeling. Biogeosciences, 9(6), 2012-2031, https://doi.org/10.5194/bg-9-2013-2012
    Publication Date: 2023-06-15
    Description: The interaction between fluid seepage, bottom water redox, and chemosynthetic communities was studied at cold seeps across one of the world's largest oxygen minimum zones (OMZ) located at the Makran convergent continental margin. Push cores were obtained from seeps within and below the core-OMZ with a remotely operated vehicle. Extracted sediment pore water was analyzed for sulfide and sulfate concentrations. Depending on oxygen availability in the bottom water, seeps were either colonized by microbial mats or by mats and macrofauna. The latter, including ampharetid polychaetes and vesicomyid clams, occurred in distinct benthic habitats, which were arranged in a concentric fashion around gas orifices. At most sites colonized by microbial mats, hydrogen sulfide was exported into the bottom water. Where macrofauna was widely abundant, hydrogen sulfide was retained within the sediment. Numerical modeling of pore water profiles was performed in order to assess rates of fluid advection and bioirrigation. While the magnitude of upward fluid flow decreased from 11 cm yr**-1 to 〈1 cm yr**-1 and the sulfate/methane transition (SMT) deepened with increasing distance from the central gas orifice, the fluxes of sulfate into the SMT did not significantly differ (6.6-9.3 mol m**-2 yr**-1). Depth-integrated rates of bioirrigation increased from 120 cm yr**-1 in the central habitat, characterized by microbial mats and sparse macrofauna, to 297 cm yr**-1 in the habitat of large and few small vesicomyid clams. These results reveal that chemosynthetic macrofauna inhabiting the outer seep habitats below the core-OMZ efficiently bioirrigate and thus transport sulfate down into the upper 10 to 15 cm of the sediment. In this way the animals deal with the lower upward flux of methane in outer habitats by stimulating rates of anaerobic oxidation of methane (AOM) with sulfate high enough to provide hydrogen sulfide for chemosynthesis. Through bioirrigation, macrofauna engineer their geochemical environment and fuel upward sulfide flux via AOM. Furthermore, due to the introduction of oxygenated bottom water into the sediment via bioirrigation, the depth of the sulfide sink gradually deepens towards outer habitats. We therefore suggest that - in addition to the oxygen levels in the water column, which determine whether macrofaunal communities can develop or not - it is the depth of the SMT and thus of sulfide production that determines which chemosynthetic communities are able to exploit the sulfide at depth. We hypothesize that large vesicomyid clams, by efficiently expanding the sulfate zone down into the sediment, could cut off smaller or less mobile organisms, as e.g. small clams and sulfur bacteria, from the sulfide source.
    Keywords: Center for Marine Environmental Sciences; Flare 1; Flare 15; Flare 2; GeoB12309-3; GeoB12312-3; GeoB12313-12; GeoB12313-13; GeoB12313-6; GeoB12315-4; GeoB12315-9; GeoB12320-4; GeoB12320-9; GeoB12353-3; GeoB12353-5; M74/3; MARUM; Meteor (1986); MUC; MUC-2; MUC-3; MultiCorer; OMZ 650; OMZ 950; Remote operated vehicle QUEST; ROVQ
    Type: Dataset
    Format: application/zip, 11 datasets
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  • 5
    Publication Date: 2023-06-15
    Keywords: Center for Marine Environmental Sciences; DEPTH, sediment/rock; GeoB12312-3; Ion chromatography (Metrohm); M74/3; MARUM; Meteor (1986); MUC; MUC-3; MultiCorer; OMZ 650; Sulfate
    Type: Dataset
    Format: text/tab-separated-values, 23 data points
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  • 6
    Publication Date: 2023-06-15
    Keywords: Center for Marine Environmental Sciences; DEPTH, sediment/rock; Flare 2; GeoB12313-13; Ion chromatography (Metrohm); M74/3; MARUM; Meteor (1986); Photometer, methylene blue (Cline 1969); Remote operated vehicle QUEST; ROVQ; Sulfate; Sulfide
    Type: Dataset
    Format: text/tab-separated-values, 39 data points
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  • 7
    Publication Date: 2023-06-15
    Keywords: Center for Marine Environmental Sciences; DEPTH, sediment/rock; GeoB12309-3; Ion chromatography (Metrohm); M74/3; MARUM; Meteor (1986); MUC; MUC-2; MultiCorer; OMZ 950; Sulfate
    Type: Dataset
    Format: text/tab-separated-values, 19 data points
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  • 8
    Publication Date: 2023-06-15
    Keywords: Center for Marine Environmental Sciences; DEPTH, sediment/rock; Flare 2; GeoB12313-12; Ion chromatography (Metrohm); M74/3; MARUM; Meteor (1986); Photometer, methylene blue (Cline 1969); Remote operated vehicle QUEST; ROVQ; Sulfate; Sulfide
    Type: Dataset
    Format: text/tab-separated-values, 34 data points
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  • 9
    Publication Date: 2023-06-15
    Keywords: Center for Marine Environmental Sciences; DEPTH, sediment/rock; Flare 2; GeoB12313-6; Ion chromatography (Metrohm); M74/3; MARUM; Meteor (1986); Photometer, methylene blue (Cline 1969); Remote operated vehicle QUEST; ROVQ; Sulfate; Sulfide
    Type: Dataset
    Format: text/tab-separated-values, 45 data points
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  • 10
    Publication Date: 2023-06-15
    Keywords: Center for Marine Environmental Sciences; DEPTH, sediment/rock; Flare 2; GeoB12315-4; Ion chromatography (Metrohm); M74/3; MARUM; Meteor (1986); Photometer, methylene blue (Cline 1969); Remote operated vehicle QUEST; ROVQ; Sulfate; Sulfide
    Type: Dataset
    Format: text/tab-separated-values, 41 data points
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