The Queen's University of Belfast, Northern Ireland and University of Waika
to, Hamilton, New Zealand radiocarbon laboratories have undertaken a series
of high-precision measurements on decadal samples of dendrochronologically
dated oak (Quercus patrea) and cedar (Libocedrus bidwillii) from Great Bri
tain and New Zealand, respectively. The results show a real atmospheric off
set of 3.4 +/- 0.6 parts per thousand (27.2 +/- 4.7 C-14 yr) between the tw
o locations for the interval AD 1725 to AD 1885, with the Southern Hemisphe
re being depleted in C-14. This result is less than the value currently use
d to correct Southern Hemisphere calibrations, possibly indicating a gradie
nt in Delta(14)C within the Southern Hemisphere.