作者: P. J. Reimer , F. G. McCormac , J. Moore , F. McCormick , E. V. Murray
DOI: 10.1191/0959683602HL528RP
关键词:
摘要: The time dependency of the regional difference ΔR in marine radiocarbon reservoir correction is an important issue for calibration ages and also provides information about past ocean circulation changes. Few measurements Holocene corrections are available climatically North Atlantic. We determined intervals during 6100 years before present (BP) by comparing 31 terrestrial sample pairs from 14 archaeological sites coast Ireland, Scotland Orkney Islands. find that, while a this region cannot be ruled out, within error determinations, appears to have been constant at least last 2000 possibly 6000 years. This work results recommendation 33 +93 region.