Radioactive dating of animal bones of Jyomon-era by extremely low-level gamma-ray spectrometry.

Research Project

Project/Area Number	10480025
Research Category	Grant-in-Aid for Scientific Research (B)
Allocation Type	Single-year Grants
Section	一般
Research Field	Cultural property science
Research Institution	Kanazawa University
Principal Investigator	KOMURA Kazuhisa Faculty of Science, Kanazawa University Prof., 理学部, 教授 (00110601)
Co-Investigator(Kenkyū-buntansha)	IMAMURA Mineo Faculty of Science, Kanazawa University Prof., 理学部, 教授 (10011701) INOUE Mutsuo Faculty of Science, Kanazawa University Lecturer, 理学部, 助手 (60283090) YAMAMOTO Masayoshi Faculty of Science, Kanazawa University A. Prof., 理学部, 助教授 (10121295)
Project Period (FY)	1998 – 1999
Project Status	Completed (Fiscal Year 1999)
Budget Amount *help	¥10,400,000 (Direct Cost: ¥10,400,000) Fiscal Year 1999: ¥1,700,000 (Direct Cost: ¥1,700,000) Fiscal Year 1998: ¥8,700,000 (Direct Cost: ¥8,700,000)
Keywords	Radioactive dating / Uranium series / Animal bone / amma-ray measurement / Non-destructive method / Jyomon-era / α線計測 / 化石
Research Abstract	In order to estimate ages of animal bones excavated from shell mounds of Jyomon-era, non-destructive dating method using Ra-226/U-238 activity ratio has been examined as a new and simple dating technique. Gamma-ray measurements of animal bones were performed using extremely low background well type Ge detector set in underground laboratory (270 mwe of depth) in a tunnel of former Ogoya Copper Mine. It was found that there are three pattern of in-situ incorporation of uranium series nuclides ; (1) rather high amount of radium relative to uranium is incorporated during degradation stage of bone samples (Torihama shell mound Fukui Pref.), (2) rather high amount of uranium is selectively incorporated into bone sample (Tonodai shell mound, Chiba Pref.) and (3) small amount of uranium without radium is incorporated in bone sample in early stage (Toi shell mound, Hokkaido). Age of bone samples in case (2) and (3) can be calculated from Ra-226/U-238 activity ratios. Torihama sample could not be dated by non-destructive method because the concentration of Ra-226 is higher than parent uranium, therefore, age of Torihama sample was measured by alpha spectrometry. Present methods was found to give c.a. 1000 year older than archaeological ages. Even if non-destructive dating method cannot be applied to bone samples, gamma spectrometry was found to be very useful to get information on environmental circumstances of Jyomon-era.