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    Radiocarbon Chronology of Late Glacial and Holocene Sedimentation and Water-Level Changes in the Area of the Gościąż Lake Basin

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    Author
    Pazdur, Anna
    Pazdur, M. F.
    Goslar, Tomasz
    Wicik, Bogumił
    Arnold, Maurice
    Issue Date
    1994-01-01
    Keywords
    levels
    Plock Depression
    Plock Poland
    Vistulian
    Vistula River valley
    Lake Gościąż
    terraces
    basins
    laminations
    corrections
    climate
    gyttja
    Poland
    lacustrine environment
    ice sheets
    planar bedding structures
    sedimentary structures
    varves
    global change
    sedimentation
    clastic rocks
    marl
    isotope ratios
    Holocene
    Central Europe
    last glacial maximum
    glacial geology
    Pleistocene
    upper Pleistocene
    time scales
    Europe
    organic residues
    seeds
    sediments
    Cenozoic
    Quaternary
    wood
    C 14
    carbon
    isotopes
    radioactive isotopes
    C 13 C 12
    stable isotopes
    absolute age
    sedimentary rocks
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    Citation
    Pazdur, A., Pazdur, M. F., Goslar, T., Wicik, B., & Arnold, M. (1994). Radiocarbon chronology of Late Glacial and Holocene sedimentation and water-level changes in the area of the Gościąż Lake basin. Radiocarbon, 36(2), 187-202.
    Publisher
    Department of Geosciences, The University of Arizona
    Journal
    Radiocarbon
    URI
    http://hdl.handle.net/10150/653385
    DOI
    10.1017/S0033822200040492
    Additional Links
    http://radiocarbon.webhost.uits.arizona.edu/
    Abstract
    We obtained 14C ages on samples of lake marl and other sediments from cores taken in Gościąż Lake and its environs. Comparison of 14C dates of bulk samples of laminated sediment with varve chronology and available AMS dates of terrestrial macrofossils indicates a reservoir correction of 2000 +/120 yr for the basal series of lake sediments. 14C dates obtained on peat layers underlying the oldest lacustrine sediments in Gościąż and other lakes consistently locate the beginning of organogenic sedimentation in this area at ca. 13 ka BP. We distinguished three periods of lacustrine gyttja sedimentation in cores taken in Gościąż and adjacent lakes: 11.8-10.2 ka, 8-7 ka and 2.7-2.1 ka BP. From the 14C dates of lithological boundaries in these cores, we reconstruct a pattern of lake-level changes during the last 12 ka, remarkably similar to Swedish lakes and generally agreeing with available records from European and American lakes. The behavior of Gościąż Lake during the last 12 ka fairly well reflects global climate changes in the temperate zone during the Late Glacial and Holocene periods..
    Type
    Article
    text
    Language
    en
    ISSN
    0033-8222
    ae974a485f413a2113503eed53cd6c53
    10.1017/S0033822200040492
    Scopus Count
    Collections
    Radiocarbon, Volume 36, Number 2 (1994)

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