The Maunder Minimum: An Interlaboratory Comparison of Δ14C from AD 1688 to AD 1710

Author:

Damon Paul E,Eastoe Christopher J,Mikheeva Irina B

Abstract

Measurements on same-age tree-ring samples from proximal Ural Mountain trees by the Ioffe Institute research group and at the University of Arizona demonstrate a variance corresponding to a standard deviation of ±5.1% for Ioffe compared to ±2.1% for Tucson. There is also a calibration difference of 4.3 ±1.2 ‰. Comparison of the same years measured in Seattle on wood from the Pacific Northwest shows an offset of 2.2 ± 0.5 ‰. This is not a calibration error, but rather is expected from the well-documented evidence for divergence and upwelling of 14C-depleted CO2 along the west coast of North America.

Publisher

Cambridge University Press (CUP)

Subject

General Earth and Planetary Sciences,Archaeology

Reference13 articles.

1. On the variation of 14C in the Earth's atmosphere in the last 400 years;Konstantinov;Izvestiia Akademii Nauk, seriia fizicheskaia,1997

2. Anthropogenic and solar components of hemispheric14C

3. Fine and Hyperfine Structure in the Spectrum of Secular Variations of Atmospheric 14C

4. Secular variation of Δ14C during the Medieval Solar Maximum: a progress report;Damon;Radiocarbon,1998

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