2007
DOI: 10.1017/s0033822200042260
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Radiocarbon Wiggle-Matching of Japanese Historical Materials with a Possible Systematic Age Offset

Abstract: Progress in radiocarbon accelerator mass spectrometry (AMS) techniques enables much more access to wiggle-matching techniques for high-precision 14C dating with relatively low costs than before. Recently, we have applied wiggle-matching for a number of wood samples where dendrochronology is difficult because of various limitations imposed for dendro-dating. In most cases, wiggle-matching gave rather unambiguous calendar ages, but we found that in some cases the calibrated date was very sensitive to a systemati… Show more

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Cited by 20 publications
(15 citation statements)
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“…These results suggest that 14 C ages of the Yakusugi tree tend to be older than those estimated by IntCal09 and show values intermediate to those of IntCal09 and SHCal04 14 C ages. A similar tendency has been reported for 14 C age values of other Japanese trees collected from Ashinoko Lake, central Japan, when compared with those of IntCal98, for the restricted calendar age range (AD 50-250) (Sakamoto et al 2003), and also for several other 14 C measurements on Japanese trees (Imamura et al 2007). In the present research, the 14 C age trends between Japanese trees and IntCal09 data are clear, and our data suggest that air…”
supporting
confidence: 90%
“…These results suggest that 14 C ages of the Yakusugi tree tend to be older than those estimated by IntCal09 and show values intermediate to those of IntCal09 and SHCal04 14 C ages. A similar tendency has been reported for 14 C age values of other Japanese trees collected from Ashinoko Lake, central Japan, when compared with those of IntCal98, for the restricted calendar age range (AD 50-250) (Sakamoto et al 2003), and also for several other 14 C measurements on Japanese trees (Imamura et al 2007). In the present research, the 14 C age trends between Japanese trees and IntCal09 data are clear, and our data suggest that air…”
supporting
confidence: 90%
“…The average shifts of Nagoya 14 C ages from the IntCal09 ones and 1 errors were determined to be +26 ± 36, +24 ± 30, +16 ± 22, +5 ± 21, and +14 ± 22 14 C yr, for the calendar-year intervals AD 72-382, 589-1072, 1413-1615, 1617-1739, and 1790-1860, respectively ( (Sakamoto et al 2003), and also for several other 14 C measurements on Japanese trees (Imamura et al 2007). In the present research, the 14 C age trends between Japanese trees and IntCal09 data are clear, and our data suggest that air Figure 3a Comparison of 14 C ages among tree rings analyzed (AD 72-382), and the IntCal09 and SHCal04 standard data sets.…”
Section: Resultsmentioning
confidence: 93%
“…As an example of such an application we can consider the data set of Imamura et al (2007). They give data for 2 tree-ring sequences from Japan, one of which is a reference data set of known age (outer ring AD 350) and another sample data set from a short 43-ring sequence that has been dendrochronologically dated (outer ring AD 389).…”
Section: Systematic Offsets Relative To the Calibration Curvementioning
confidence: 99%