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  • Geological Society of America (GSA)  (1)
  • Springer  (1)
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  • 1
    Electronic Resource
    Electronic Resource
    Springer
    Aquatic geochemistry 6 (2000), S. 385-411 
    ISSN: 1573-1421
    Keywords: hydrogeochemistry ; element ratios ; 87Sr/86 ; Ba/Sr ; weathering ; semi-arid ; Kafue River ; Zambezi River
    Source: Springer Online Journal Archives 1860-2000
    Topics: Chemistry and Pharmacology , Geosciences
    Notes: Abstract Frequent sampling during an annual cycle of dissolved(〈0.45 μm) and suspended (〉0.45 μm) elementshas been conducted in the Kafue River at Raglan'sFarm, upstream from the mining activities within theCopperbelt Province, Zambia. Additional sampling ofsediment and interstitial pore water was conductedduring low water discharge. The presence of carbonateswithin the drainage basin naturally gives rise to highelement concentrations in the dissolved phase(Ca = 626, Mg = 494, Na = 360 and K = 24 mmol l-1).During the rainy season the relative composition ofthe dissolved elements indicated a wash out ofaccumulated weathering products and mineralisedorganic material from the unsaturated zone of the soilprofile. High concentrations of dissolved Al, Fe andMn were measured during high water discharge. At lowwater discharge the sediment was a major source of Fe,Mn and associated Co and Cu to the water column.Enhanced concentrations of dissolved and suspended S,Co and Cu during the rainy season indicated thatatmospheric deposited particles from the mining areawere washed out into the river. Autochthonousformation of particles rich in Si indicated diatomproduction during low water discharge.
    Type of Medium: Electronic Resource
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  • 2
    Publication Date: 2011-02-01
    Description: Strontium isotopic composition (87Sr/86Sr) data from subfossil 14C-dated mollusk shells in raised beach sediments are used as a paleosalinity proxy in the brackish Baltic Sea, the precision ({+/-}5%) and accuracy ({+/-}0.7{per thousand}) of the method being judged from replicate analyses of modern shells. Paleosalinity data with an average time resolution of [~]200 yr for the period 7130-2775 calibrated 14C yr B.P. indicate maximum surface salinities of 10{per thousand}-11{per thousand}, 11{per thousand}-12{per thousand}, and 12{per thousand}-13{per thousand} for the Bothnian Bay, Bothnian Sea, and Baltic Proper (the three major Baltic subbasins). The relative salinity differences between the basins were small ([≤]30%) compared to the as much as eightfold present-day relative salinity differences (Bothnian Bay 1{per thousand}-3{per thousand}; Bothnian Sea 4{per thousand}-5{per thousand}; Baltic Proper 6{per thousand}-8{per thousand}). Late Holocene freshening (ca. 3000 calibrated 14C yr B.P. to present) is most pronounced in the northernmost subbasin, the Bothnian Bay, consistent with the absence of a permanent halocline, sequestering of phosphorus in well-oxygenated bottom sediments, and phosphorus limitation of primary production in the present-day Bothnian Bay. This study suggests that paleosalinity data may be crucial to improving our understanding of the possible effects of any future, climate-induced freshening of the Baltic Sea.
    Print ISSN: 0091-7613
    Electronic ISSN: 1943-2682
    Topics: Geosciences
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