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  • Data  (4)
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  • 1
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    Unknown
    PANGAEA
    In:  Supplement to: You, Chen-Feng; Gieskes, Joris M; Chen, Robert F; Spivack, Arthur J; Gamo, Toshitaka (1993): Iodide, bromide, manganese, boron, and dissolved organic carbon in interstitial waters of organic carbon-rich marine sediments: observations in the Nankai accretionary prism. In: Hill, IA; Taira, A; Firth, JV; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 131, 165-174, https://doi.org/10.2973/odp.proc.sr.131.116.1993
    Publication Date: 2024-03-09
    Description: This study of the interstitial water concentration-depth distributions of iodide, bromide, boron, d11B, and dissolved organic carbon, as represented by absorbance at 325 nm (yellow substance: YS) and laser-induced fluorescence (LIF), is a follow-up of the extensive shipboard program of interstitial water analysis during ODP Leg 131. Most of the components studied are associated with processes involving the diagenesis of organic matter in these sediments. Three zones of the sediment column are discussed separately because of the different processes involved in causing concentration changes: 1. The upper few hundreds of meters: In this zone, characterized by very high sedimentation rates (〉1200 m/m.y.), interstitial waters show very sharp increases in alkalinity, ammonia, iodide, bromide, YS, and LIF, mainly as a result of the diagenesis of organic carbon; 2. Whereas below 200 mbsf concentration gradients all show a decreasing trend, the zone at ~ 365 mbsf is characterized by concentration reversals, mainly due to the recent emplacement of deeper sediments above this depth as a result of thrust-faulting; 3. The décollement zone (945-964 mbsf) is characterized by concentration anomalies in various constituents (bromide, boron, d11B, manganese, LIF). These data are interpreted as resulting from an advective input of fluids along the zone of décollement as recent as ~ 200 ka. Possibly periodic inputs of anomalous fluids still seem to occur along this décollement zone.
    Keywords: 131-808A; 131-808B; 131-808C; Boron; Bromine; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; Event label; Fluorescence; Iodide; Joides Resolution; Leg131; Manganese; Ocean Drilling Program; ODP; Philippine Sea; Sample code/label; Yellow substance; δ11B
    Type: Dataset
    Format: text/tab-separated-values, 334 data points
    Location Call Number Limitation Availability
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  • 2
    Publication Date: 2024-03-09
    Keywords: Alkalinity, total; Carbon, organic, dissolved; DEPTH, sediment/rock; Fluorescence; LATITUDE; LONGITUDE; Sample code/label
    Type: Dataset
    Format: text/tab-separated-values, 171 data points
    Location Call Number Limitation Availability
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  • 3
    Publication Date: 2024-03-09
    Keywords: 131-808A; 131-808B; 131-808C; 64-478; 64-479; 67-496; 67-499_Site; 74-525_Site; Absorbance; Alkalinity, total; Carbon, organic, dissolved; COMPCORE; Composite Core; Deep Sea Drilling Project; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Event label; Fluorescence; Glomar Challenger; Joides Resolution; Leg131; Leg64; Leg67; Leg74; North Pacific/Gulf of California/BASIN; North Pacific/Gulf of California/CHANNEL; North Pacific/TRENCH; Ocean Drilling Program; ODP; Philippine Sea; Sample code/label; South Atlantic/CREST
    Type: Dataset
    Format: text/tab-separated-values, 313 data points
    Location Call Number Limitation Availability
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  • 4
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    Unknown
    PANGAEA
    In:  Supplement to: Chen, Robert F; Bada, Jeffrey L (1994): The fluorescence of dissolved organic matter in porewaters of marine sediments. Marine Chemistry, 45(1-2), 31-42, https://doi.org/10.1016/0304-4203(94)90089-2
    Publication Date: 2024-03-09
    Description: The fluorescence of porewaters from marine sediment cores from six different areas was measured. In most cases, fluorescence was affected primarily by the diagenesis of organic carbon first through sulfate reduction and subsequently by methane generation. Typically, fluorescence, dissolved organic carbon (DOC), absorbance, alkalinity, and ammonium ion concentrations correlate quite well, increasing in the upper sections of anoxic sediments and co-varying in deeper sections of these cores. The good correlation of DOC with fluorescence in the three cores in which DOC was measured indicates that fluorescence can be used to make a first order estimate of DOC concentration in anoxic porewaters. Data are consistent with a model in which labile organic matter in the sediments is broken down by sulfur reducing bacteria to low molecular weight monomers. These monomers are either remineralized to CO2 or polymerize to form dissolved, fluorescent, high molecular weight molecules. The few exceptions to this model involve hydrothermally generated hydrocarbons that are formed in situ in the Guaymas Basin or are horizontally advected along the decollement in the Nankai Trench.
    Keywords: 131-808A; 131-808B; 131-808C; 64-478; 64-479; 67-496; 67-499_Site; 74-525_Site; COMPCORE; Composite Core; Deep Sea Drilling Project; DRILL; Drilling/drill rig; DSDP; Glomar Challenger; Joides Resolution; Leg131; Leg64; Leg67; Leg74; North Pacific/Gulf of California/BASIN; North Pacific/Gulf of California/CHANNEL; North Pacific/TRENCH; Ocean Drilling Program; ODP; Philippine Sea; South Atlantic/CREST
    Type: Dataset
    Format: application/zip, 2 datasets
    Location Call Number Limitation Availability
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