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The Last Deglaciation: Absolute and Radiocarbon Chronologies (Paperback, Softcover reprint of the original 1st ed. 1992)
Loot Price: R4,372
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The Last Deglaciation: Absolute and Radiocarbon Chronologies (Paperback, Softcover reprint of the original 1st ed. 1992)
Series: Nato ASI Subseries I:, 2
Expected to ship within 10 - 15 working days
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Time is a major factor in Quaternary science. Without a trustworthy
chronometer any interpretation of changes in proxy data of
stratigraphical origin is on weak ground. In fact, any attempt at a
sound reconstruction of timing and rates of past climatic change as
well as the response of the biosphere can only be achieved on the
basis of a reliable chronology. Moreover, all correlations and
comparisons through time on a continental or global scale depend
heavily on the reliability of the time-scale used. Therefore the
establishment of an absolute time-scale is a fundamental goal. In
this contribution we refer to the term "absolute time-scale" as a
time-scale consisting of ages determined on the basis of sidereal
years. Traditional stratigraphical methods of absolute dating
include the Swedish glacial varve chronology, already developed
early in this century by De Geer (1912) and since then continuously
improved (e.g. Stromberg 1985; Cato 1987). Unfortunately, however,
a spatial correlation with other stratigraphies outside
Fennoscandia is difficult.
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