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    14C Dating of Late Pleistocene-Holocene Events on Kunashir Island, Kuril Islands

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    Author
    Bazarova, V. B.
    Razjigaeva, N. G.
    Grebennikova, T. A.
    Ganzey, L. A.
    Mokhova, L. M.
    Korotky, A. M.
    Sulerzhitsky, L. D.
    Issue Date
    1998-01-01
    Keywords
    ocean currents
    currents
    forests
    paleoenvironment
    climate change
    geomorphology
    marine environment
    vegetation
    Holocene
    microfossils
    miospores
    palynomorphs
    pollen
    Plantae
    algae
    volcanism
    Kunashir Island
    Kuril Islands
    Russian Pacific region
    Sakhalin Russian Federation
    diatoms
    soils
    Pleistocene
    Russian Federation
    upper Pleistocene
    peat
    Commonwealth of Independent States
    sediments
    Asia
    Cenozoic
    charcoal
    Quaternary
    wood
    C 14
    carbon
    dates
    isotopes
    radioactive isotopes
    shells
    absolute age
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    Citation
    Bazarova, V. B., Razjigaeva, N. G., Grebennikova, T. A., Ganzey, L. A., Mokhova, L. M., Korotky, A. M., & Sulerzhitsky, L. D. (1998). 14 C Dating of Late Pleistocene–Holocene Events on Kunashir Island, Kuril Islands. Radiocarbon, 40(2), 775-780.
    Publisher
    Department of Geosciences, The University of Arizona
    Journal
    Radiocarbon
    Description
    From the 16th International Radiocarbon Conference held in Gronigen, Netherlands, June 16-20, 1997.
    URI
    http://hdl.handle.net/10150/654102
    DOI
    10.1017/S0033822200018725
    Additional Links
    http://radiocarbon.webhost.uits.arizona.edu/
    Abstract
    Kunashir Island is a very important site for paleoenvironmental reconstructions. Until recently, very little information on Quaternary deposits was available. We studied the environmental evolution of this oceanic island under the influence of geomorphological processes, volcanism and strong marine currents. This paper presents new data that allow a detailed reconstruction of the environmental development of Kunashir Island during the Late Pleistocene-Holocene, based on ca. 80 radiocarbon dates and diatom, pollen and sedimentological data. The vegetation development reflects climate changes and warm/cold current migrations.
    Type
    Proceedings
    text
    Language
    en
    ISSN
    0033-8222
    ae974a485f413a2113503eed53cd6c53
    10.1017/S0033822200018725
    Scopus Count
    Collections
    Radiocarbon, Volume 40, Number 2 (1998)

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