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  • 1
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    PANGAEA
    In:  Supplement to: Gomez-Saez, Gonzalo V; Niggemann, Jutta; Dittmar, Thorsten; Pohlabeln, Anika M; Lang, Susan Q; Noowong, Ann; Pichler, Thomas; Wörmer, Lars; Bühring, Solveig I (2016): Molecular evidence for abiotic sulfurization of dissolved organic matter in marine shallow hydrothermal systems. Geochimica et Cosmochimica Acta, 190, 35-52, https://doi.org/10.1016/j.gca.2016.06.027
    Publikationsdatum: 2023-08-10
    Beschreibung: Shallow submarine hydrothermal systems are extreme environments with strong redox gradients at the interface of hot, reduced fluids and cold, oxygenated seawater. Hydrothermal fluids are often depleted in sulfate when compared to surrounding seawater and can contain high concentrations of hydrogen sulfide (H2S). It is well known that sulfur in its various oxidation states plays an important role in processing and transformation of organic matter. However, the formation and the reactivity of dissolved organic sulfur (DOS) in the water column at hydrothermal systems are so far not well understood. We investigated DOS dynamics and its relation to the physicochemical environment by studying the molecular composition of dissolved organic matter (DOM) in three contrasting shallow hydrothermal systems off Milos (Eastern Mediterranean), Dominica (Caribbean Sea) and Iceland (North Atlantic). We used ultra-high resolution Fourier transform ion cyclotron resonance mass spectrometry (FT-ICR-MS) to characterize the DOM on a molecular level. The molecular information was complemented with general geochemical data, quantitative dissolved organic carbon (DOC) and DOS analyses as well as isotopic measurements (d2H, d18O and F14C). In contrast to the predominantly meteoric fluids from Dominica and Iceland, hydrothermal fluids from Milos were mainly fed by recirculating seawater. The hydrothermal fluids from Milos were enriched in H2S and DOS, as indicated by high DOS/DOC ratios and by the fact that 〉90% of all assigned DOM formulas that were exclusively present in the fluids contained sulfur. In all three systems, DOS from hydrothermal fluids had on average lower O/C ratios (0.26?0.34) than surrounding surface seawater DOS (0.45?0.52), suggesting shallow hydrothermal systems as a source of reduced DOS, which will likely get oxidized upon contact with oxygenated seawater. Evaluation of hypothetical sulfurization reactions suggests DOM reduction and sulfurization during seawater recirculation in Milos seafloor. The four most effective potential sulfurization reactions were those exchanging an O atom by one S atom in the formula or the equivalent + H2S reaction, correspondingly exchanging H2O, H2 and/or O2 by a H2S molecule. Our study reveals novel insights into DOS dynamics in marine hydrothermal environments and provides a conceptual framework for molecular-scale mechanisms in organic sulfur geochemistry.
    Schlagwort(e): Center for Marine Environmental Sciences; MARUM
    Materialart: Dataset
    Format: application/zip, 2 datasets
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 2
    Publikationsdatum: 2023-08-10
    Schlagwort(e): Aromaticity index; Aromatics; Caribbean Sea; Center for Marine Environmental Sciences; Champagne_Hot_Springs; DIVER; Dominica; Dominica_Seawater; Dominica Island (Lesser Antilles, Caribbean Sea); Double bond equivalent; Event label; Hveravík-1; Hveravík-2; Hydrogen/Carbon ratio; Iceland; MARUM; Milos; Milos_Seawater; Milos, Greece; Molecular formula; MULT; Multiple investigations; Oxygen/Carbon ratio; Palaeochori_Bay; Sample comment; Sampling by diver; Soufriere; Spathi_Bay; Sulfur/Carbon ratio
    Materialart: Dataset
    Format: text/tab-separated-values, 117 data points
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 3
    Publikationsdatum: 2023-08-10
    Schlagwort(e): Boron; Bromine; Calcium; Calculated; Carbon, organic, dissolved; Caribbean Sea; Center for Marine Environmental Sciences; Champagne_Hot_Springs; Chlorine; DEPTH, water; DIVER; Dominica_Seawater; Event label; Fluorine; Fraction modern carbon; Hveravík-1; Hveravík-2; Hydrogen sulfide; Iceland; Iron; Lithium; Magnesium; Manganese; MARUM; Milos_Seawater; Milos, Greece; MULT; Multiple investigations; Palaeochori_Bay; pH; ph meter, WTW 3210 with Mic-D electrode; Potassium; Ratio; Salinity; Sample comment; Sampling by diver; Silicon; Sodium; Soufriere; Spathi_Bay; Strontium; Sulfate; Sulfur, organic, dissolved, extracted; Temperature, calculated; Temperature, water; δ18O, water; δ Deuterium
    Materialart: Dataset
    Format: text/tab-separated-values, 215 data points
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 4
    Publikationsdatum: 2014-05-12
    Beschreibung: We investigated microbial life preserved in a hydrothermally inactive silica–barite chimney in comparison with an active barite chimney and sediment from the Loki’s Castle low-temperature venting area at the Arctic Mid-Ocean Ridge (AMOR) using lipid biomarkers. Carbon and sulfur isotopes were used to constrain possible metabolic pathways. Multiple sulfur (δ34S, ∆33S) isotopes on barite over a cross section of the extinct chimney range between 21.1 and 22.5 ‰ in δ34S, and between 0.020 and 0.034 ‰ in Δ33S, indicating direct precipitation from seawater. Biomarker distributions within two discrete zones of this silica–barite chimney indicate a considerable difference in abundance and diversity of microorganisms from the chimney exterior to the interior. Lipids in the active and inactive chimney barite and sediment were dominated by a range of 13C-depleted unsaturated and branched fatty acids with δ13C values between −39.7 and −26.7 ‰, indicating the presence of sulfur-oxidizing and sulfate-reducing bacteria. The majority of lipids (99.5 %) in the extinct chimney interior that experienced high temperatures were of archaeal origin. Unusual glycerol monoalkyl glycerol tetraethers (GMGT) with 0–4 rings were the dominant compounds suggesting the presence of mainly (hyper-) thermophilic archaea. Isoprenoid hydrocarbons with δ13C values as low as −46 ‰ also indicated the presence of methanogens and possibly methanotrophs.
    Repository-Name: EPIC Alfred Wegener Institut
    Materialart: Article , peerRev
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 5
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    Biological and Chemical Oceanography Data Management Office (BCO-DMO). Contact: bco-dmo-data@whoi.edu
    Publikationsdatum: 2022-10-31
    Beschreibung: Dataset: Lost City Fluids - Radium
    Beschreibung: This dataset includes radiochemistry data for fluids from 7 vent sites (Marker 2, Beehive, Marker 8, Marker 3, Calypso, Marker C. and Sombrero) at the Lost City Hydrothermal Field at the Atlantis Massif (30N, Mid-Atlantic Ridge). Fluid samples were collected in September 2018 during the AT42-01 expedition of the R/V Atlantis with the remotely operated vehicle (ROV) Jason II. For a complete list of measurements, refer to the full dataset description in the supplemental file 'Dataset_description.pdf'. The most current version of this dataset is available at: https://www.bco-dmo.org/dataset/864434
    Beschreibung: NSF Division of Ocean Sciences (NSF OCE) OCE-1536702, NSF Division of Ocean Sciences (NSF OCE) OCE-1736321
    Schlagwort(e): Serpentinization ; Radium ; Residence time ; Uranium ; Ultramafic
    Repository-Name: Woods Hole Open Access Server
    Materialart: Dataset
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 6
    Publikationsdatum: 2022-10-31
    Beschreibung: Dataset: Lost City Solids - Radiochemistry
    Beschreibung: Radiochemistry of serpentinite, carbonate-brucite chimney, and other solid samples from the Lost City Hydrothermal Field at the Atlantis Massif from 2018 and four previous expeditions in 2015, 2005, 2003, and 2000 (Kelley et al., 2001; Kelley et al., 2005; Früh-Green et al.,2018). For a complete list of measurements, refer to the full dataset description in the supplemental file 'Dataset_description.pdf'. The most current version of this dataset is available at: https://www.bco-dmo.org/dataset/864460
    Beschreibung: NSF Division of Ocean Sciences (NSF OCE) OCE-1536702, NSF Division of Ocean Sciences (NSF OCE) OCE-1736321
    Schlagwort(e): Serpentinization ; Radium ; Residence time ; Uranium ; Ultramafic
    Repository-Name: Woods Hole Open Access Server
    Materialart: Dataset
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 7
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    Biological and Chemical Oceanography Data Management Office (BCO-DMO). Contact: bco-dmo-data@whoi.edu
    Publikationsdatum: 2022-05-26
    Beschreibung: Dataset: M. jannaschii high/low H2: isotopes and fractionation factors
    Beschreibung: Carbon isotopic compositions and fractionation factors of amino acids and squalenoid lipids in Methanocaldococcus jannaschii in high and low hydrogen (H2) environments. For a complete list of measurements, refer to the full dataset description in the supplemental file 'Dataset_description.pdf'. The most current version of this dataset is available at: https://www.bco-dmo.org/dataset/812240
    Beschreibung: NSF Division of Ocean Sciences (NSF OCE) OCE-0939564
    Repository-Name: Woods Hole Open Access Server
    Materialart: Dataset
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 8
    Publikationsdatum: 2022-05-26
    Beschreibung: Dataset: Lost City AT42-01 Collected Fluids
    Beschreibung: Summary of samples collected by the Hydrothermal Organic Geochemistry (HOG) sampler on AT-4201 with ROV Jason, on dives J2_1107 through J2_1111, during R/V Atlantic cruise AT42-01, September 9 - October 1, 2018. For a complete list of measurements, refer to the full dataset description in the supplemental file 'Dataset_description.pdf'. The most current version of this dataset is available at: https://www.bco-dmo.org/dataset/782197
    Beschreibung: NSF Division of Ocean Sciences (NSF OCE) OCE-1536702, NSF Division of Ocean Sciences (NSF OCE) OCE-1536405, NSF Division of Ocean Sciences (NSF OCE) OCE-1535962
    Repository-Name: Woods Hole Open Access Server
    Materialart: Dataset
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 9
    Publikationsdatum: 2022-05-26
    Beschreibung: Author Posting. © The Author(s), 2016. This is the author's version of the work. It is posted here by permission of Arizona Board of Regents on behalf of the University of Arizona for personal use, not for redistribution. The definitive version was published in Radiocarbon 58 (2016): 505-515, doi: 10.1017/RDC.2016.17.
    Beschreibung: The radiocarbon content of dissolved organic carbon (DOC) in rivers, lakes, and other non-saline waters can provide valuable information on carbon cycling dynamics in the environment. DOC is typically prepared for 14C analysis by accelerator mass spectrometry (AMS) either by ultraviolet (UV) oxidation or by freeze-drying and sealed tube combustion. We present here a new method for the rapid analysis of 14C of DOC using wet chemical oxidation (WCO) and automated headspace sampling of CO2. The approach is an adaption of recently developed methods using aqueous persulfate oxidant to determine the δ13C of DOC in non-saline water samples and the 14C content of volatile organic acids. One advantage of the current method over UV oxidation is higher throughput: 22 samples and 10 processing standards can be prepared in one day and analyzed in a second day, allowing a full suite of 14C processing standards and blanks to be run in conjunction with samples. A second advantage is that there is less potential for cross-contamination between samples.
    Beschreibung: SQL and GF-G gratefully acknowledge support by the Swiss National Science Foundation project 200020-143891 and the Deep Carbon Observatory–Deep Energy subaward 60040915. BMV and Fraser River sampling were supported by US National Science Foundation grant OCE-0851015.
    Repository-Name: Woods Hole Open Access Server
    Materialart: Preprint
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 10
    Publikationsdatum: 2022-11-04
    Beschreibung: © The Author(s), 2022. This article is distributed under the terms of the Creative Commons Attribution License. The definitive version was published in Voss, B., Eglinton, T., Peucker-Ehrenbrink, B., Galy, V., Lang, S., McIntyre, C., Spencer, R., Bulygina, E., Wang, Z., & Guay, K. Isotopic evidence for sources of dissolved carbon and the role of organic matter respiration in the Fraser River basin, Canada. Biogeochemistry. (2022), https://doi.org/10.1007/s10533-022-00945-5.
    Beschreibung: Sources of dissolved and particulate carbon to the Fraser River system vary significantly in space and time. Tributaries in the northern interior of the basin consistently deliver higher concentrations of dissolved organic carbon (DOC) to the main stem than other tributaries. Based on samples collected near the Fraser River mouth throughout 2013, the radiocarbon age of DOC exported from the Fraser River does not change significantly across seasons despite a spike in DOC concentration during the freshet, suggesting modulation of heterogeneous upstream chemical and isotopic signals during transit through the river basin. Dissolved inorganic carbon (DIC) concentrations are highest in the Rocky Mountain headwater region where carbonate weathering is evident, but also in tributaries with high DOC concentrations, suggesting that DOC respiration may be responsible for a significant portion of DIC in this basin. Using an isotope and major ion mass balance approach to constrain the contributions of carbonate and silicate weathering and DOC respiration, we estimate that up to 33 ± 11% of DIC is derived from DOC respiration in some parts of the Fraser River basin. Overall, these results indicate close coupling between the cycling of DOC and DIC, and that carbon is actively processed and transformed during transport through the river network.
    Beschreibung: Open Access funding provided by the MIT Libraries. This work was supported by the WHOI Academic Programs Office, the MIT EAPS Department Student Assistance Fund, and the PAOC Houghton Fund to BMV; NSF-ETBC grants OCE-0851015 to BPE, VG, and TIE and OCE-0851101 to RGMS; NSF grant EAR-1226818 to BPE; NSF grant OCE-0928582 to TIE and VG; and a WHOI Arctic Research Initiative grant to ZAW.
    Schlagwort(e): River ; Carbon isotopes ; Radiocarbon ; Weathering ; Carbon cycle
    Repository-Name: Woods Hole Open Access Server
    Materialart: Article
    Standort Signatur Einschränkungen Verfügbarkeit
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