• Correcting 14C Histograms for the Non-Linearity of the 14C Time Scale

      Stolk, A.; Hogervorst, Koos; Berendsen, Henk (Department of Geosciences, The University of Arizona, 1989-01-01)
      Large numbers of 14C dates of the base and top of Holocene peat layers may be plotted in 14C histograms in order to establish statistically a chronology of periods of essentially elastic sedimentation and peat formation. Due to the non-linearity of the 14C time scale in terms of calendar years, clustering of 14C dates on random peat growth may occur. This seriously hampers the interpretation of histograms. A quantitative method and computer program were developed to correct the histograms for this effect. The correction factor that has to be applied depends on the calibration curve and the interval width of the correction parameter dy. For peat samples, an interval width of 100 14C yr and a calibration curve based on a 100-yr moving average seems to be a reasonable choice.
    • Temporal 10Be and 14C Variations: A Tool for Paleomagnetic Research

      Kocharov, G. E.; Blinov, A. V.; Konstantinov, A. N.; Levchenko, V. A. (Department of Geosciences, The University of Arizona, 1989-01-01)
      Temporal variations of cosmogenic radionuclide atmospheric concentrations can be caused by such global phenomena as solar activity and geomagnetic field changes as well as atmospheric circulation processes. These causes can be distinguished by the comparison of several isotope records corresponding to the same time period. We discuss a possibility for reconstructing the geomagnetic moment during the last 30,000 years from the comparison of 10Be and 14C concentrations in terrestrial archives. The results agree with conventional paleomagnetic data and promise to enrich our knowledge of geomagnetic field variations and reversals.