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    Chronology of Vegetation and Paleoclimatic Stages of Northwestern Russia During the Late Glacial and Holocene

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    Author
    Arslanov, Kh A.
    Saveljeva, L. A.
    Gey, N. A.
    Klimanov, V. A.
    Chernov, S. B.
    Chernova, G. M.
    Kuzmin, G. F.
    Tertychnaya, T. V.
    Subetto, D. A.
    Denisenkov, V. P.
    Issue Date
    1999-01-01
    Keywords
    spores
    Bog soils
    northwestern Russia
    Boreal
    Leningrad Oblast Russian Federation
    Novgorod Russian Federation
    Atlantic
    gyttja
    lake sediments
    lacustrine environment
    upper Weichselian
    Weichselian
    Younger Dryas
    C 14 C 12
    Holocene
    microfossils
    miospores
    palynomorphs
    pollen
    soils
    paleoclimatology
    Pleistocene
    Russian Federation
    upper Pleistocene
    Europe
    peat
    Commonwealth of Independent States
    sediments
    Cenozoic
    Quaternary
    C 14
    carbon
    dates
    isotopes
    radioactive isotopes
    stable isotopes
    absolute age
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    Citation
    Arslanov, K. A., Saveljeva, L. A., Gey, N. A., Klimanov, V. A., Chernov, S. B., Chernova, G. M., ... & Denisenkov, V. (1999). Chronology of vegetation and paleoclimatic stages of northwestern Russia during the Late Glacial and Holocene. Radiocarbon, 41(1), 25-45.
    Publisher
    Department of Geosciences, The University of Arizona
    Journal
    Radiocarbon
    URI
    http://hdl.handle.net/10150/654467
    DOI
    10.1017/S0033822200019317
    Additional Links
    http://radiocarbon.webhost.uits.arizona.edu/
    Abstract
    We have studied 6 reference sections of bog and lake sediments in the Leningrad and Novgorod provinces to develop a geochronological scale for vegetational and paleoclimatic changes in northwestern Russia during the Late Glacial and Holocene. Every 10-cm layer along the peat and gyttja sections (4-8.5 m thick) was investigated palynologically and the great majority of them were radiocarbon dated. Using the data obtained, standard palynological diagrams were plotted and vegetation history reconstructed. The palynozones indicated on the diagrams were related to the climatic periods and subperiods (phases) of the Blytt-Sernander scheme. On the basis of 230 14C dates obtained, we derived the geochronology of climatic periods and phases, as well as the chronology for the appearance and areal distribution of forest-forming tree species. The uppermost peat layers were dated by using the "bomb effect". We compared the stages of Holocene vegetation and paleoclimatic changes discovered for the Leningrad and Novgorod provinces with the those obtained for Karelia, which we had studied earlier using the same methodology.
    Type
    Article
    text
    Language
    en
    ISSN
    0033-8222
    ae974a485f413a2113503eed53cd6c53
    10.1017/S0033822200019317
    Scopus Count
    Collections
    Radiocarbon, Volume 41, Number 1 (1999)

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