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  • 117-720A; 117-721; 117-722; 117-723; 117-724; 117-725A; 117-725B; 117-725C; 117-726A; 117-727A; 117-728; 117-729A; 117-730A; 117-731A; 117-731B; 117-731C; Alkalinity, total; Ammonium; Arabian Sea; Calcium; Carbon, organic, dissolved; Chloride; COMPCORE; Composite Core; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; Event label; Joides Resolution; Leg117; Magnesium; Magnesium/Calcium ratio; Ocean Drilling Program; ODP; pH; Phosphate; Salinity; Sample code/label; Silicon dioxide; Sulfate  (1)
  • 117-724C; 117-725C; Arabian Sea; DRILL; Drilling/drill rig; Joides Resolution; Leg117; Ocean Drilling Program; ODP  (1)
  • 117-724C; Arabian Sea; Carbon, organic, total; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; Joides Resolution; Leg117; Mass spectrometer VG Micromass Prism; Ocean Drilling Program; ODP; Sample code/label; δ13C, organic carbon; δ15N, organic matter  (1)
  • PANGAEA  (3)
  • Macmillian Magazines Ltd.
Collection
Keywords
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  • PANGAEA  (3)
  • Macmillian Magazines Ltd.
Years
  • 1
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    Unknown
    PANGAEA
    In:  Supplement to: Muzuka, Alfred N N; Macko, Stephen A; Pedersen, Thomas F (1991): Stable carbon and nitrogen isotope compositions of organic matter from Sites 724 and 725, Oman Margin. In: Prell, WL; Niitsuma, N; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 117, 571-586, https://doi.org/10.2973/odp.proc.sr.117.163.1991
    Publication Date: 2024-01-09
    Description: Stable isotopic compositions of carbon and nitrogen and organic carbon content of sediments ranging from the Pliocene to the Pleistocene-Holocene in age from the Oman Margin (ODP Sites 724 and 725) are reported. In general, the organic carbon content is greater than 2% at Site 724. Prior to the Pleistocene-Holocene at this site, sediments with higher content of organic matter were deposited owing to favorable preservation conditions and/or higher productivity. In the Pleistocene, lower amounts of organic matter have been preserved; this material generally has more enriched nitrogen isotopic compositions. This may indicate intensification of the Oxygen Minimum Zone and denitrification with the onset of the Pleistocene. A correlation of carbon isotope content of these sediments with oxygen isotope stages at Site 724 indicates an enrichment in 13C during glacial events. Based on the stable isotope evidence of both carbon and nitrogen, there does not appear to be major input of terrigenous-derived allochthonous material in this marine environment. The timing and extent of monsoon winds on the productivity of this region are not evident, but require further studies for collaborative interpretation of small-scale features in the isotopic and carbon content of this environment.
    Keywords: 117-724C; 117-725C; Arabian Sea; DRILL; Drilling/drill rig; Joides Resolution; Leg117; Ocean Drilling Program; ODP
    Type: Dataset
    Format: application/zip, 2 datasets
    Location Call Number Expected Availability
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  • 2
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    Unknown
    PANGAEA
    In:  Supplement to: Pedersen, Thomas F; Shimmield, Graham (1991): Interstitial water chemistry, Leg 117: contrasts with the Peru margin. In: Prell, WL; Niitsuma, N; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 117, 499-513, https://doi.org/10.2973/odp.proc.sr.117.152.1991
    Publication Date: 2024-01-09
    Description: Interstitial water analyses made at 12 sites during Leg 117 are used to define the nature of diagenetic reactions in organic-rich sediments on the Owen Ridge and Oman Margin. Minor variations in chloride concentration profiles are ascribed to past changes in bottom water salinity at two mid-depth margin sites and to upward migration of low salinity water at another. There is no evidence for subsurface brine movement, unlike the case on the Peru Margin. Dolomitization is widespread and accounts for the depletions of magnesium observed in pore waters at variable depths at nearly all sites. The mineral occurs both as disseminated euhedral limpid crystals and, in at least one location, in massive stringers. Formation of the latter is suggested to reflect precipitation during sea level transgressions when the sedimentation rate was low, but when productivity was high. Authigenic carbonate fluorapatite is also widespread, the phosphorus being derived from the breakdown of organic matter. Sulfate is quantitatively depleted at depth at most locations but the rate of depletion is markedly less than that observed on the Peru Margin where sedimentation is also similarly influenced by high rates of upwelling. The reason for this contrast is not clear and merits further investigation.
    Keywords: 117-720A; 117-721; 117-722; 117-723; 117-724; 117-725A; 117-725B; 117-725C; 117-726A; 117-727A; 117-728; 117-729A; 117-730A; 117-731A; 117-731B; 117-731C; Alkalinity, total; Ammonium; Arabian Sea; Calcium; Carbon, organic, dissolved; Chloride; COMPCORE; Composite Core; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; Event label; Joides Resolution; Leg117; Magnesium; Magnesium/Calcium ratio; Ocean Drilling Program; ODP; pH; Phosphate; Salinity; Sample code/label; Silicon dioxide; Sulfate
    Type: Dataset
    Format: text/tab-separated-values, 2195 data points
    Location Call Number Expected Availability
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  • 3
    Publication Date: 2024-01-09
    Keywords: 117-724C; Arabian Sea; Carbon, organic, total; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; Joides Resolution; Leg117; Mass spectrometer VG Micromass Prism; Ocean Drilling Program; ODP; Sample code/label; δ13C, organic carbon; δ15N, organic matter
    Type: Dataset
    Format: text/tab-separated-values, 3186 data points
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
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