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  • 1995-1999  (1)
  • 1980-1984  (8)
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Year
  • 1
    Electronic Resource
    Electronic Resource
    Springer
    Geo-marine letters 16 (1996), S. 17-23 
    ISSN: 1432-1157
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Notes: Abstract Sedimentary carbon systematics on the Amazon continental shelf were investigated using14C andδ 13C measurements of sedimentary organic materials. Mass balance calculations indicate that the14C content of modern shelf muds results from burial of old (~ 5000 yr BP) terrestrial soil carbon and bomb-14C-enriched marine carbon, implying that most of the bomb-labeled riverine particulate carbon is not buried on the shelf. The14C signature of Amazon shelf deposits records the effects of both biogeochemical and sedimentary processes active in this dynamic environment.
    Type of Medium: Electronic Resource
    Location Call Number Limitation Availability
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  • 2
    Electronic Resource
    Electronic Resource
    Springer
    Geo-marine letters 4 (1984), S. 207-210 
    ISSN: 1432-1157
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Notes: Abstract Sedimentological, geochemical, and physical-oceanographic studies of the Brazilian continental shelf near the Amazon River help provide a broad understanding of this major sediment dispersal system. Amazon River sediment accumulates as a subaqueous delta, with the most rapid accumulation (∼10 cm/yr) occurring near the seaward edge of the topset beds and in the foreset beds. Amazon River sediment is dispersed northwestward along the shelf and is transported beyond the Brazilian border. Radiographic studies of sediment cores delineate three sedimentary environments: interbedded mud and sand, faintly laminated mud, and bioturbated mud. The distribution of these environments is a function of proximity to the river mouth and of sediment accumulation rate.
    Type of Medium: Electronic Resource
    Location Call Number Limitation Availability
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  • 3
    Publication Date: 2024-04-19
    Keywords: AII76-17; Alpha spectrometry; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; GC; Gravity corer; Ion-exchange-chromatography; Lead-210; Lead-210, standard deviation; Lead-210 excess; Lead-210 excess, standard deviation; Radium-226; Radium-226, standard deviation; South Atlantic
    Type: Dataset
    Format: text/tab-separated-values, 40 data points
    Location Call Number Limitation Availability
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  • 4
    Publication Date: 2024-04-19
    Keywords: Alpha spectrometry; B52-39; BC; Box corer; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Equatorial Pacific; Ion-exchange-chromatography; Lead-210; Lead-210, standard deviation; Lead-210 excess; Lead-210 excess, standard deviation; Radium-226; Radium-226, standard deviation
    Type: Dataset
    Format: text/tab-separated-values, 24 data points
    Location Call Number Limitation Availability
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  • 5
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    Unknown
    PANGAEA
    In:  Supplement to: DeMaster, David J; Cochran, James R (1982): Particle mixing rates in deep-sea sediments determined from excess 210Pb and 32Si profiles. Earth and Planetary Science Letters, 61(2), 257-271, https://doi.org/10.1016/0012-821X(82)90057-7
    Publication Date: 2024-04-19
    Description: Particle mixing rates have been determined for 5 South Atlantic/Antarctic and 3 equatorial Pacific deep-sea cores using excess 210Pb and 32Si measurements. Radionuclide profiles from these siliceous, calcareous, and clay-rich sediments have been evaluated using a steady state vertical advection diffusion model. In Antarctic siliceous sediments210Pb mixing coefficients (0.04-0.16 cm**2/y) are in reasonable agreement with the 32Si mixing coefficient (0.2 or 0.4 cm**2/y, depending on 32Si half-life). In an equatorial Pacific sediment core, however, the 210Pb mixing coefficient (0.22 cm**2/y) is 3-7 times greater than the 32Si mixing coefficient (0.03 or 0.07 cm**2/y). The difference in 210Pb and 32Si mixing rates in the Pacific sediments results from: (1) non-steady state mixing and differences in characteristic time and depth scales of the two radionuclides, (2) preferential mixing of fine-grained clay particles containing most of the 210Pb activity relative to coarser particles (large radiolaria) containing the 32Si activity, or (3) the supply of 222Rn from the bottom of manganese nodules which increases the measured excess 210Pb activity (relative to 226Ra) at depth and artificially increases the 210Pb mixing coefficient. Based on 32Si data and pore water silica profiles, dissolution of biogenic silica in the sediment column appears to have a minor effect on the 32Si profile in the mixed layer. Deep-sea particle mixing rates reported in this study and the literature do not correlate with sediment type, sediment accumulation rate, or surface productivity. Based on differences in mixing rate among three Antarctic cores collected within 50 km of each other, local variability in the intensity of deep-sea mixing appears to be as important as regional differences in sediment properties.
    Keywords: A47-16; AII76-12; AII76-16; AII76-17; AII76-18; AII76-3; B52-39; BC; Box corer; C57-58; Equatorial Pacific; GC; Gravity corer; South Atlantic
    Type: Dataset
    Format: application/zip, 10 datasets
    Location Call Number Limitation Availability
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  • 6
    Publication Date: 2024-04-19
    Keywords: AII76-18; Alpha spectrometry; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; GC; Gravity corer; Ion-exchange-chromatography; Lead-210; Lead-210, standard deviation; Lead-210 excess; Lead-210 excess, standard deviation; Radium-226; Radium-226, standard deviation; South Atlantic
    Type: Dataset
    Format: text/tab-separated-values, 40 data points
    Location Call Number Limitation Availability
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  • 7
    Publication Date: 2024-04-19
    Keywords: AII76-12; Alpha spectrometry; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; GC; Gravity corer; Ion-exchange-chromatography; Lead-210; Lead-210, standard deviation; Lead-210 excess; Lead-210 excess, standard deviation; Radium-226; Radium-226, standard deviation; South Atlantic
    Type: Dataset
    Format: text/tab-separated-values, 40 data points
    Location Call Number Limitation Availability
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  • 8
    Publication Date: 2024-04-19
    Keywords: AII76-3; Alpha spectrometry; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; GC; Gravity corer; Ion-exchange-chromatography; Lead-210; Lead-210, standard deviation; Lead-210 excess; Lead-210 excess, standard deviation; Radium-226; Radium-226, standard deviation; South Atlantic
    Type: Dataset
    Format: text/tab-separated-values, 40 data points
    Location Call Number Limitation Availability
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  • 9
    Publication Date: 2024-04-19
    Keywords: Alpha spectrometry; BC; Box corer; C57-58; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Equatorial Pacific; Ion-exchange-chromatography; Lead-210; Lead-210, standard deviation; Lead-210 excess; Lead-210 excess, standard deviation; Radium-226; Radium-226, standard deviation
    Type: Dataset
    Format: text/tab-separated-values, 32 data points
    Location Call Number Limitation Availability
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