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2015 Fiscal Year Final Research Report

Development of paleothermometry using reptile-bone-hosting nodule

Research Project

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Project/Area Number 26610168
Research Category

Grant-in-Aid for Challenging Exploratory Research

Allocation TypeMulti-year Fund
Research Field Stratigraphy/Paleontology
Research InstitutionKanazawa University

Principal Investigator

Hasegawa Takashi  金沢大学, 自然システム学系, 教授 (50272943)

Co-Investigator(Kenkyū-buntansha) JENKYNS Robert  金沢大学, 自然システム学系, 助教 (10451824)
Project Period (FY) 2014-04-01 – 2016-03-31
Keywords古水温 / ノジュール / 酸素同位体比 / 古環境
Outline of Final Research Achievements

Stable isotope analyses of carbonate carbon and oxygen, and carbonate-associated sulfate on reptile-bone nodules indicated that the reptile corpse had been surrounded by oxic water but it became anoxic because of the organic decomposition resulting calcareous nodule formation. The stable isotope results also showed progressive process of nodule formation. Interpretation of the isotope data and visual observation of the nodule demonstrated that the calcium carbonate precipitated closest to bone (calcium carbonate attached on the bone in vacant space inside of a bone) is most recommended material for paleothermometry.

Free Research Field

地質学・古環境学

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Published: 2017-05-10  

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