Hostname: page-component-586b7cd67f-rcrh6 Total loading time: 0 Render date: 2024-11-25T02:52:36.096Z Has data issue: false hasContentIssue false

German Oak and Pine 14C Calibration, 7200–9439 BC

Published online by Cambridge University Press:  18 July 2016

Bernd Kromer
Affiliation:
Institut für Umweltphysik, Universität Heidelberg, D-6900 Heidelberg, Germany
Bernd Becker
Affiliation:
Institut für Botanik, Universität Hohenheim, D-7000 Stuttgart 70 Germany
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.

Radiocarbon calibration data derived from German oak chronologies, ranging back to 7200 BC, have been published in the previous Calibration Issue (Stuiver & Kra 1986). In recent years, the German oak chronology has been extended to 7938 BC (Becker, this issue). For earlier intervals, tree-ring chronologies must be based on pine, because oak re-emigrated to central Europe at the Preboreal/Boreal transition, at about 8000 BC. We have established a 1784-yr pine chronology centered in the Preboreal, and have linked it tentatively to the absolutely dated oak master. We present here calibration data based on this link, for the age range, 7145–9439 BC.

Type
Articles
Copyright
Copyright © The American Journal of Science 

References

Becker, B. 1992. A 11,000 year long German oak and pine dendrochronology for radiocarbon calibration. Radiocarbon, this issue.Google Scholar
Becker, B., Kromer, B. and Trimborn, P. 1991 A stable isotope tree-ring timescale of the Late Glacial/Holocene boundary. Nature 353: 647649.Google Scholar
Stuiver, M. and Kra, R. S., eds., 1986 Calibration Issue. in Stuiver, M. and Kra, R. S., eds., Proceedings of the 12th International 14C Conference. Radiocarbon 28(2B): 8051030.CrossRefGoogle Scholar
Stuiver, M. and Polach, H. 1977 Discussion: Reporting of 14C data. Radiocarbon 19(3): 355363.CrossRefGoogle Scholar