Hostname: page-component-78c5997874-xbtfd Total loading time: 0 Render date: 2024-11-10T09:38:36.054Z Has data issue: false hasContentIssue false
  • English
  • Français

Radiocarbon Age Calibration Back to 13,300 Years BP and the 14C Age Matching of the German Oak and US Bristlecone Pine Chronologies

Published online by Cambridge University Press:  18 July 2016

Minze Stuiver ,
Bernd Kromer ,
Bernd Becker  and
C W Ferguson
Minze Stuiver
Affiliation:
University of Washington, Seattle
Bernd Kromer
Affiliation:
Universität Heidelberg
Bernd Becker
Affiliation:
Universität Hohenheim, Stuttgart
C W Ferguson
Affiliation:
University of Arizona, Tucson; deceased March 24, 1986.
Rights & Permissions [Opens in a new window]

Extract

Core share and HTML view are not available for this content. However, as you have access to this content, a full PDF is available via the ‘Save PDF’ action button.

With the recent establishment of an unbroken West European tree-ring sequence spanning the past 7272 years (Pilcher et al, 1984) the calibration of the 14C time scale was advanced considerably. It is now possible to use this chronology as an independent cross-check on the 8681-year US Bristlecone Pine series (Ferguson & Graybill, 1983). There also are opportunities for 14C matching (wiggle matching) between the older portion of the Bristlecone Pine series and floating (not tied to the present) parts of the South German Oak sequence. Linick, Suess and Becker (1985) used this approach in matching the earliest part of the Bristlecone Pine series with the Donau 6 Main 4/11 (Becker, 1983) series and thus established a D6M4/11 “zero” point (tree-ring no. 1) of 7215 bc.

Type
Research Article
Information
Radiocarbon , Volume 28 , Issue 2B , 1986 , pp. 969 - 979
Copyright
Copyright © The American Journal of Science 

References

Becker, B, 1983, The long-term radiocarbon trend of the absolute German Oak tree-ring chronology, 2800 to 800 BC, in Stuiver, M and Kra, RS, eds, Internatl 14C conf, 11th, Proc: Radiocarbon, v 25, no. 2, p 197–203.Google Scholar
Bruns, M, Rhein, M, Linick, R W and Suess, H E, 1983, The atmospheric 14C level in the 7th millenium bc: PACT, v 8, p 511–516.Google Scholar
Cato, I, 1985, The definitive connection of the Swedish geochronological time scale with the present, and the new date of the zero year in Döviken, northern Sweden: Boreas, v 14, p 117–122.Google Scholar
Ferguson, C W and Graybill, D A, 1983, Dendrochronology of Bristlecone Pine: A progress report, in Stuiver, M and Kra, R S, eds, Internatl 14C conf, 11th, Proc: Radiocarbon, v 25, no. 2, p 287–288.Google Scholar
Fromm, E, 1970, An estimation of errors in the Swedish varve chronology, in Olsson, I U, ed, Radiocarbon variations and absolute chronology, Nobel symposium, 12th: New York, John Wiley & Sons, p 163–172.Google Scholar
Hammer, C U, Clausen, H B and Tauber, H, 1986, Ice-core dating of the Pleistocene-Holocene boundary applied to a calibration of the 14C time scale, in Stuiver, M and Kra, R S, eds, Internatl 14C conf, 12th, Proc: Radiocarbon, v 28, no. 2A.Google Scholar
International Study Group, 1982, An interlaboratory comparison of radiocarbon measurements in tree-rings: Nature, v 298, p 619–623.CrossRefGoogle Scholar
Linick, T W, Long, A, Damon, P E and Ferguson, C W, 1986, High precision radiocarbon dating of Bristlecone Pine from 6550 to 5350 BC, in Stuiver, M and Kra, R S, eds, Internatl 14C conf, 12th, Proc: Radiocarbon, this issue.Google Scholar
Linick, T W, Suess, H E and Becker, B, 1985, La Jolla measurements of radiocarbon in south German Oak tree-ring chronologies: Radiocarbon, v 27, p 20–32.Google Scholar
Pilcher, J R, Baillie, M G L, Schmidt, B and Becker, B, 1984, A 7,272-year tree-ring chronology for western Europe: Nature, v 312, p 150–152.CrossRefGoogle Scholar
Strömberg, B, 1985, Revision of the lateglacial Swedish varve chronology: Boreas, v 14, p 101–105.Google Scholar
Stuiver, M, 1970, Long-term 14C variations, in Olsson, I U, ed, Radiocarbon variations and absolute chronology, Nobel symposium, 12th: New York, John Wiley & Sons, p 197–213.Google Scholar
Stuiver, M, 1971, Evidence for the variation of atmospheric 14C content in the Late Quaternary, in Turekian, K K, ed, The Late Cenozoic glacial ages: New Haven, Yale Univ Press, p 57–70.Google Scholar
Stuiver, M, 1982, A high-precision calibration of the AD radiocarbon time scale: Radiocarbon, v 24, p 1–26.Google Scholar
Stuiver, M and Pearson, G W, 1986, High-precision calibration of the radiocarbon time scale, 1950 AD–500 BC, in Stuiver, M and Kra, R S, eds, Internatl 14C conf, 12th, Proc: Radiocarbon, this issue.Google Scholar
Stuiver, M and Quay, P D, 1980, Changes in atmospheric carbon-14 attributed to a variable sun: Science, v 207, p 11–19.CrossRefGoogle ScholarPubMed
Stuiver, M and Quay, P D, 1981, Atmospheric 14C changes resulting from fossil fuel CO2 release and cosmic ray flux variability: Earth Planetary Sci Letters, v 53, p 349–362.Google Scholar
Stuiver, M, Robinson, S W and Yang, I C, 1979, 14C dating to 60,000 years BP with proportional counters, in Berger, R and Suess, H E, eds, Radiocarbon dating, Internatl 14C conf, 9th, Proc: Berkeley, Univ California Press, p 202–215.Google Scholar
Tauber, H, 1970, The Scandinavian varve chronology and C14 dating, in Olsson, I U, ed, Radiocarbon variations and absolute chronology, Nobel symposium, 12th: New York, John Wiley & Sons, p 173–196.Google Scholar