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High-Precision 14C Measurement of Irish Oaks to Show the Natural 14C Variations from AD 1840 to 5210 BC

Published online by Cambridge University Press:  18 July 2016

G W Pearson ,
J R Pilcher ,
M G L Baillie ,
D M Corbett  and
F Qua
G W Pearson
Affiliation:
Palaeoecology Centre, The Queen's University of Belfast, Northern Ireland
J R Pilcher
Affiliation:
Palaeoecology Centre, The Queen's University of Belfast, Northern Ireland
M G L Baillie
Affiliation:
Palaeoecology Centre, The Queen's University of Belfast, Northern Ireland
D M Corbett
Affiliation:
Palaeoecology Centre, The Queen's University of Belfast, Northern Ireland
F Qua
Affiliation:
Palaeoecology Centre, The Queen's University of Belfast, Northern Ireland
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Abstract

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High-precision measurement of dendrochronologically dated Irish oak at bi-decade/decade intervals has continued in the Belfast laboratory, extending the 14C data base from ca AD 1840 to 5210 BC. The dendrochronology is now considered absolute (see Belfast dendrochronology this conference) (Brown et al, 1986) and a continuous detailed curve is presented, showing the natural variations in the atmospheric concentration of 14C over >7000 years. Each data point has a precision of <2.5., and some 4500 years have now been compared with Seattle, giving excellent agreement. Discussion of this data base and the justification of the claimed accuracy is given together with a comparison of other chronologies. Some of the advantages and limitations of the above are discussed.

Type
Research Article
Information
Radiocarbon , Volume 28 , Issue 2B , 1986 , pp. 911 - 934
Copyright
Copyright © The American Journal of Science 

References

Baillie, M G L, Pilcher, J R, and Pearson, G W, 1983, Dendrochronology at Belfast as a background to high precision calibration, in Stuiver, M and Kra, R S, eds, Internatl 14C conf, 11th, Proc: Radiocarbon, v 25, no. 2, p 171–178.Google Scholar
Brown, D M, Munro, M A R, Baillie, M G L and Pilcher, J R, 1986, Dendrochronology—The Absolute Irish Standard, in Stuiver, M and Kra, R S, eds, Internatl 14C conf, 12th, Proc: Radiocarbon, v 28, no. 2A.Google Scholar
Dresser, P Q (ms), 1970, A study of sampling and pretreatments of materials for radiocarbon dating; PhD dissert, The Queen's University of Belfast.Google Scholar
Klein, J, Lerman, J C, Damon, P E and Ralph, E K, 1982, Calibration of radiocarbon dates: tables based on the consensus data of the Workshop on Calibrating the Radiocarbon Time Scale: Radiocarbon, v 24, p 103–150.Google Scholar
Pearson, G W, 1979, Precise C measurement by liquid scintillation counting: Radiocarbon, v 21, p 1–21.Google Scholar
Pearson, G W, 1980, High precision radiocarbon dating by liquid scintillation counting applied to radiocarbon time-scale calibration, in Stuiver, M and Kra, R S, eds, Internatl 4C conf, 10th, Proc: Radiocarbon, v 22, no. 2, p 337–345.Google Scholar
Pearson, G W (ms), 1983, The development of high precision 14C measurement and its application to archaeological time-scale problems: PhD dissert, The Queen's University of Belfast.Google Scholar
Pearson, G W, 1986, Precise calendric dating of known growth period samples using a ‘curve fitting’ technique, in Stuiver, M and Kra, R S, eds, Internatl 14C conf, 12th, Proc: Radiocarbon, v 28, no. 2A.Google Scholar
Pearson, G W and Baillie, M G L, 1983, High-precision 14C measurement of Irish Oaks to show the natural atmospheric 14C variations of the AD time period, in Stuiver, M and Kra, R S, eds, Internatl 14C conf, 11th, Proc: Radiocarbon, v 25, no. 2, p 187–196.Google Scholar
Pearson, G W, Pilcher, J R and Baillie, M G L, 1983, High-precision 14C measurement of Irish Oaks to show the natural 14C variations from 200 BC to 4000 BC, in Stuiver, M and Kra, R S, eds, Internatl 14C conf, 11th, Proc: Radiocarbon, v 25, no. 2, p 179–186.Google Scholar
Pearson, G W and Stuiver, M, 1986, High-precision radiocarbon time-scale calibration from 500 BC to 2500 BC, in Stuiver, M and Kra, R S, eds, Internatl 14C conf, 12th, Proc: Radiocarbon, this issue.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, no. 5990, p 150–152.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 radiocarbon time-scale calibration from the present to 500 BC, in Stuiver, M and Kra, R S, eds, Internatl 14C conf, 12th, Proc: Radiocarbon, this issue.Google Scholar
Stuiver, M and Polach, H, 1977, Discussion: Reporting of 14C data: Radiocarbon, v 19, p 355–363.CrossRefGoogle Scholar