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  • 1
    Keywords: Hochschulschrift
    Type of Medium: Online Resource
    Pages: 1 Online-Ressource (225 Blatt = 13 MB)
    DDC: 570
    Language: English
    Note: Zusammenfassung in deutscher und englischer Sprache
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  • 2
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    American Society of Limnology and Oceanography
    In:  Limnology and Oceanography: Methods, 12 . pp. 25-45.
    Publication Date: 2019-09-23
    Description: The efficiency of the “benthic microbial methane filter” at marine cold seeps is controlled by diffusive sulfate supply from the overlying seawater and advective methane flux from deep reservoirs. High fluid fluxes reduce the penetration depth of sulfate and limit the filter to a very narrow zone close to the sediment-water interface. Here, we introduce a new sediment-flow-through (SLOT) system, to mimic the balance between fluid/methane flow and sulfate supply in natural sediments. SLOT enables anaerobic incubations of intact sediment cores under natural flow regimes. In addition to traditional in- and outflow sampling, geochemical parameters can be monitored along the sediment core using microsensors and rhizons. In a first test run, two cores with gassy sediments from the Eckernförde Bay (Baltic Sea) were incubated and monitored for 310 days under low (11.2 cm y–1) and high fluid flow (112.1 cm y–1) conditions. Rates of anaerobic oxidation of methane (AOM) were one order of magnitude higher (3.07 mmol m–2 d–1) in the high flow compared to the low flow regime (0.29 mmol m–2 d–1), whereas methane efflux was twice as high (0.063 and 0.033 mmol m–2 d–1, respectively). Sediment profiles of sulfide, sulfate, total alkalinity, pH, redox, and other parameters offered important information on the nature and dynamics of the biogeochemical reactions in the sediment cores including methanotrophy, sulfate reduction, carbonate precipitation, and sulfide oxidation. The SLOT system proofed to be an effective device to study the temporal evolution of biogeochemical parameters in intact sediments subjected to advective fluid transport.
    Type: Article , PeerReviewed
    Format: text
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  • 3
    Publication Date: 2019-09-23
    Description: Subduction of the oceanic Cocos plate offshore Costa Rica causes strong advection of methane-charged fluids. Presented here are the first direct measurements of microbial anaerobic oxidation of methane (AOM) and sulfate reduction (SR) rates in sediments from the two mounds, applying radiotracer techniques in combination with numerical modeling. In addition, analysis of carbonate δ18O, δ13C, and 87Sr / 86Sr signatures constrain the origin of the carbonate-precipitating fluid. Average rates of microbial activities showed differences with a factor of 4.8 to 6.3 between Mound 11 [AOM 140.71 (±40.84 SD); SR 117.25 (±82.06 SD) mmol m−2 d−1, respectively] and Mound 12 [AOM 22.37 (±0.85 SD); SR 23.99 (±5.79 SD) mmol m−2 d−1, respectively]. Modeling results yielded flow velocities of 50 cm a−1 at Mound 11 and 8–15 cm a−1 at Mound 12. Analysis of oxygen and carbon isotope variations of authigenic carbonates from the two locations revealed higher values for Mound 11 (δ18O: 4.7 to 5.9‰, δ13C: −21.0 to −29.6‰), compared to Mound 12 (δ18O: 4.1 to 4.5‰, δ13C: −45.7 to −48.9‰). Analysis of carbonates 87Sr / 86Sr indicated temporal changes of deep-source fluid admixture at Mound 12. The present study is in accordance with previous work supporting considerable differences of methane flux between the two Mounds. It also strengthens the hypothesis of a predominantly deep fluid source for Mound 11 versus a rather shallow source of biogenic methane for Mound 12. The results demonstrate that methane-driven microbial activity is a valid ground truthing tool for geophysical measurements of fluid advection and constraining of recent methane fluxes in the study area. The study further shows that the combination of microbial rate measurements, numerical modeling, and authigenic carbonate analysis provide a suitable approach to constrain temporal and spatial variations of methane charged fluid flow at the Pacific Costa Rican margin.
    Type: Article , PeerReviewed
    Format: text
    Format: text
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  • 4
    Publication Date: 2019-09-23
    Description: Large amounts of methane are delivered by fluids through the erosive forearc of the convergent margin offshore Costa Rica and lead to the formation of cold seeps at the sediment surface. Besides mud extrusion, numerous cold seeps are created by landslides induced by seamount subduction or fluid migration along major faults. Most of the dissolved methane reaching the seafloor at cold seeps is oxidized within the benthic microbial methane filter by anaerobic oxidation of methane (AOM). Measurements of AOM and sulfate reduction as well as numerical modeling of porewater profiles revealed a highly active and efficient benthic methane filter at Quepos Slide site; a landslide on the continental slope between the Nicoya and Osa Peninsula. Integrated areal rates of AOM ranged from 12.9 ± 6.0 to 45.2 ± 11.5 mmol m-2 d-1, with only 1 to 2.5% of the upward methane flux being released into the water column. Additionally, two parallel sediment cores from Quepos Slide were used for in vitro experiments in a recently developed Sediment-F low-Through (SLOT) system to simulate an increased fluid and methane flux from the bottom of the sediment core. The benthic methane filter revealed a high adaptability whereby the methane oxidation efficiency responded to the increased fluid flow within 150–170 days. To our knowledge, this study provides the first estimation of the natural biogeochemical response of seep sediments to changes in fluid flow.
    Type: Article , PeerReviewed
    Format: text
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  • 5
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    Unknown
    In:  [Talk] In: EGU General Assembly 2014, 27.04.-02.05.2014, Vienna, Austria .
    Publication Date: 2014-07-30
    Type: Conference or Workshop Item , NonPeerReviewed
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  • 6
    Publication Date: 2014-07-30
    Type: Conference or Workshop Item , NonPeerReviewed
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  • 7
    Publication Date: 2019-09-23
    Description: The Chilean methane seepage area (CMSA) is characterized by patchy islands of chemosynthetic communities embedded in carbonate outcrops or plain sediment areas. The communities were often found to be dominated by one type of chemosynthetic organism: bacterial mat (Beggiatoa Sp.), clam fields (Calyptogena Sp., Archivesica Sp.), tubeworms (Lamellibrachia), and pogonophorans. Some samples revealed chemosynthetic organisms below the surface such as the clam Tyosira Sp. and the sulfur bacteria Thioploca. Other sites revealed indications of successions from a less to a more active seepage site (e.g., high-sulfidic sediments containing clam shells) or vice versa (e.g., sulfide-free sediments containing clam shells). This presentation will provide a preliminary overview of chemosynthetic communities and geochemical profiles at the CMSA and their implications for methane seepage and consumption activity in sediments.
    Type: Conference or Workshop Item , NonPeerReviewed
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  • 8
    Publication Date: 2019-09-23
    Description: The overarching goal of SFB 574 is to understand the role and fate of volatiles and fluids in subduction zones. Both components have a major influence on, e.g., short- and long-term climate change, the geochemical evolution of the hydrosphere and atmosphere, as well as subduction-related natural hazards, such as earthquakes, volcanic eruptions and tsunamis, because they are cycled through the entire subduction system. The Chilean margin, which switched from erosion to accretion within the last several million years, has been chosen for the remainder of the SFB. Major goals of cruise SO-210 are: 1) to investigate and quantify the dewatering processes in the forearc of the central Chilean subduction zone, in particular the origin and output flux of vent fluids and volatiles, 2) to study biological processes fuelled by this discharge, 3) to use cold seep carbonates as a geochemical archive of cold seep activity, 4) to evaluate the role of forearc fluids in triggering mass wasting events that could generate tsunamis, 5) to characterize geochemically the subducting sediments to determine the input flux of climate-relevant volatiles and a variety of trace elements, and 6) to investigate the distribution of volcanic ashes to improve estimates on the volume of material emitted by volcanic eruptions and to date distinct events within the sedimentary sequence. Preliminary investigations by Chilean colleagues revealed definite indications of fluid venting which together with recent geophysical investigations are the basis for the present cruise. Here, we will present preliminary results and new discoveries made during the cruise.
    Type: Conference or Workshop Item , NonPeerReviewed
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  • 9
    Publication Date: 2019-09-23
    Description: As a consequence of sediment compaction at the forearc of subduction zones, fluids ascend in sediments and are discharged in cold seeps. These fluids include the greenhouse gas methane, which is to a larger proportion depleted by anaerobic oxidization of methane (AOM) next to sediment-water interface. This microbial methane filter consists of archaea (methane oxidizers) and bacteria (sulfate reducers) that are living in syntrophic consortia. During AOM, the microbes produce hydrogen sulfide, which feeds chemoautotrophic “seep-organism”. A new sediment-flow-through-system was developed, to investigate the efficiency of AOM, the range of methane turnover rates, as well as key parameters controlling microbial filter. The system includes two different seawater media. The first medium supplies the microbes with sulfate from the top, (transported by diffusion); the second carries methane and is supplied from the bottom by advective transport. Sampling holes, sealed with silicon, allow the measurement of key parameters such as sulfate, sulfide, pH, redox potential, and total alkalinity as well as sediment sub-sampling to determine the abundance, e.g., of methanotrophic microbial groups. In this presentation the technical details of the sediment-flow-through-system will be introduced. Preliminary results from the first experiments with seep sediments and insights into ongoing studies will be provided.
    Type: Conference or Workshop Item , NonPeerReviewed
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  • 10
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    In:  [Poster] In: EGU General Assembly 2011, 03.-08.04.2011, Vienna, Austria .
    Publication Date: 2014-07-21
    Type: Conference or Workshop Item , NonPeerReviewed
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