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    Extension of the Holocene Dendrochronology by the Preboreal Pine Series, 8800 to 10,100 BP

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    Author
    Becker, Bernd
    Kromer, Bernd
    Issue Date
    1986-01-01
    Keywords
    south central Europe
    Preboreal
    tree rings
    Holocene
    Europe
    Cenozoic
    Quaternary
    wood
    geochronology
    C 14
    carbon
    dates
    isotopes
    radioactive isotopes
    absolute age
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    Citation
    Becker, B., & Kromer, B. (1986). Extension of the Holocene dendrochronology by the Preboreal pine series, 8800 to 10,100 BP. Radiocarbon, 28(2B), 961-967.
    Publisher
    American Journal of Science
    Journal
    Radiocarbon
    Description
    From the 12th International Radiocarbon Conference held in Trondheim, June 24-28, 1985.
    URI
    http://hdl.handle.net/10150/652668
    DOI
    10.1017/S0033822200060240
    Additional Links
    http://radiocarbon.webhost.uits.arizona.edu/
    Abstract
    Holocene tree-ring chronologies have been established for south-central Europe covering the past 11,000 years. The Hohenheim absolute oak chronology extends to 4089 BC. The 14C-calibrated mid-Holocene floating oak master covers a 3181-year period from ca 4045 to 7225 BC. The earliest well-replicated floating oak master (estimated calendar age 7215 to 7825 BC) extends the European oak dendrochronology back to Boreal times. Further extension of the Holocene dendrochronology has been achieved by subfossil oak and pine trees from the Rhine, Main, and Danube Rivers. A 774-year floating series of Preboreal pine has been established. 14C ages range (from younger to older end) from 9200 to 9800 BP. Within this series a major atmospheric 14C variation is indicated, resulting in nearly constant 14C ages (9600 BP) over a period of 370 tree-rings. The European oak and pine tree-ring chronologies cover without major gaps the entire Holocene epoch. Based on the length of the dendro-records, an approximate solar year age of 11,280 years is calculate for the Holocene/Pleistocene boundary. The Preboreal pine forests along the rivers were replaced by mixed oak forests between 9200 and 8800 BP. By linking the earliest oak masters and the Preboreal pine series, the European dendrochronology can be extended up to the end of Late Glacial times.
    Type
    Proceedings
    text
    Language
    en
    ISSN
    0033-8222
    ae974a485f413a2113503eed53cd6c53
    10.1017/S0033822200060240
    Scopus Count
    Collections
    Radiocarbon, Volume 28, Number 2B (1986)

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