日本地球惑星科学連合2018年大会

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[JJ] 口頭発表

セッション記号 S (固体地球科学) » S-GC 固体地球化学

[S-GC46] 固体地球化学・惑星化学

2018年5月22日(火) 10:45 〜 12:15 202 (幕張メッセ国際会議場 2F)

コンビーナ:下田 玄(産業技術総合研究所地質調査総合センター)、鈴木 勝彦(国立研究開発法人海洋研究開発機構・海底資源研究開発センター)、山下 勝行(岡山大学大学院自然科学研究科、共同)、石川 晃(東京大学大学院総合文化研究科)、座長:若木 重行(国立研究開発法人海洋研究開発機構)、石川 晃(東京工業大学)、下田 玄(産業操業技術研究所)

10:45 〜 11:00

[SGC46-01] 放射起源・安定Sr同位体分析により明らかになった出土人骨の続成変質作用

*若木 重行1椋本 ひかり2南 雅代3 (1.海洋研究開発機構 高知コア研究所、2.名古屋大学 環境学研究科、3.名古屋大学 宇宙地球環境研究所)

キーワード:Sr同位体、考古科学、続成変質、アパタイト、火葬人骨

Hydroxyapatite, a main inorganic component in bones, contains Sr at high concentration up to the order of several hundreds of ppm. Radiogenic strontium isotope ratio (87Sr/86Sr) of bone hydroxyapatites has been used to study residential mobility of ancient humans and mammals in archeological fields. Strontium in human body is derived from the background geological system via foods such as plants and animals. Therefore, 87Sr/86Sr value of bone hydroxyapatite directly reflects 87Sr/86Sr value of the bedrocks in the region where the foods came from.
Archeological human remains have been buried in soils for hundreds of years or more. There is a strong possibility that the buried human bones have been affected by diagenetic process and the original 87Sr/86Sr values of the bone hydroxyapatites have been changed by such secondary alteration. Although evaluation of the effect of possible diagenetic alteration is essential in reconstructing the residential mobility of ancient humans from the bone hydroxyapatite 87Sr/86Sr data, reactivity of bone hydroxyapatite during diagenetic processes is not well understood.
In this study, we attempt to make a quantitative evaluation of secondary alteration effect on the bone hydroxyapatite 87Sr/86Sr during diagenesis. Hydroxyapatite fractions were extracted from a cremated human remain of a Buddhist priest Jokei (AD1155-1213) and three different cremated bodies excavated from Middle age sites in Binman-ji, Shiga, Japan. Bulk soil samples from the excavation sites as well as exchangeable phases of these soils were also prepared. Both the radiogenic (87Sr/86Sr) and stable (δ88Sr/86Sr) isotope ratios were analyzed for these samples. The results will be discussed in the presentation.