Abstract

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 14 C 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 14 C 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.

Keywords

Radiocarbon datingChronologySeries (stratigraphy)DendrochronologyGermanSequence (biology)CalibrationPaleontologyMatching (statistics)GeologyArchaeologyPhysical geographyHistoryGeographyMathematicsStatisticsChemistry

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Publication Info

Year
1986
Type
article
Volume
28
Issue
2B
Pages
969-979
Citations
144
Access
Closed

Citation Metrics

144
OpenAlex
4
Influential
120
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Cite This

Minze Stuiver, Bernd Kromer, Bernd Becker et al. (1986). Radiocarbon Age Calibration Back to 13,300 Years BP and the<sup>14</sup>C Age Matching of the German Oak and US Bristlecone Pine Chronologies. Radiocarbon , 28 (2B) , 969-979. https://doi.org/10.1017/s0033822200060252

Identifiers

DOI
10.1017/s0033822200060252

Data Quality

Data completeness: 81%