@article{oai:nagoya.repo.nii.ac.jp:00016127,
 author = {中村, 俊夫 and 増田, 公明 and 三宅, 芙沙 and 永冶, 健太朗 and 吉光, 貴裕 and NAKAMURA, Toshio and MASUDA, Kimiaki and MIYAKE, Fusa and NAGAYA, Kentaro and YOSHIMITSU, Takahiro},
 journal = {名古屋大学加速器質量分析計業績報告書},
 month = {Mar},
 note = {In establishing the accurate chronology of any archeological events in Holocene, in particular, Yayoi, Kofun and younger periods in Japan by 14C dating, a proper calibration method of 14C age to calendar date is required. The calibration data, IntCal04/Intcal09, that are normally applied to 14C ages of terrestrial plant materials produced in the northern hemisphere, were tested for their consistency with the relevant relations between 14C age and dendro-age for tree-ring samples formed in the Japanese Archipelago. Some parts of dendro-dated tree-rings, formed from the 10th century BC to the AD 18th century, have been analyzed for 14C ages, and the resulting relations were almost consistent with those of IntCal04/IntCal09, except for a clear discrepancy at around AD50 to AD250; 14C ages for the tree ring samples formed in Japan were older than those of IntCal04/IntCal09 by about 50-80 14C years. In addition, more frequent periods in which such discrepancies had occurred were observed in the last two millennia for Yaku-sugi trees, grown in the southern part of Japan. The present status in the studies of the 14C-age-calibration issues for Japanese samples is discussed., 名古屋大学年代測定総合研究センターシンポジウム報告},
 pages = {69--75},
 title = {14C年代から暦年代への較正に関連する諸問題},
 volume = {23},
 year = {2012}
}