@article{oai:nagoya.repo.nii.ac.jp:00016134,
 author = {渡邊, 隆広 and 奈良, 郁子 and FAGEL, Nathalie and 松中, 哲也 and 中村, 俊夫 and 箕浦, 幸治 and ZHU, Liping and WANG, Junbo and 掛川, 武 and 西村, 弥亜 and WATANABE, Takahiro and NARA, Fumiko Watanabe and MATSUNAKA, Tetsuya and NAKAMURA, Toshio and MINOURA, Koji and KAKEGAWA, Takeshi and NISHIMURA, Mitsugu},
 journal = {名古屋大学加速器質量分析計業績報告書},
 month = {Mar},
 note = {To reconstruct climatic and environmental changes in the south Tibetan Plateau, a 3.77-m-long sediment core (PY608E-PC) was obtained from Lake Pumoyum Co in August 2006. Because terrestrial plant residues are extremely rare in this core, radiocarbon dating was performed on the total organic carbon fraction. We also estimated the old carbon effect and radiocarbon reservoir age of the total organic carbon fraction. Using these estimates, a new radiocarbon chronology for past climatic changes from ca. 12,500 to 700 cal BP was established. The linear sedimentation rate of the core was founded to be constant at 32.0 cm/kyr, indicating stable sedimentation conditions in Lake Pumoyum Co from the period of the Younger Dryas to the Holocene., 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 = {149--155},
 title = {チベット湖沼堆積物の年代決定とモンスーン活動の復元},
 volume = {23},
 year = {2012}
}