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Updated: Jul 11, 2026

Removal of Exogenous Materials from the Outer Portion of Frozen Cores to Investigate the Ancient Biological Communities Harbored Inside
09:06

Removal of Exogenous Materials from the Outer Portion of Frozen Cores to Investigate the Ancient Biological Communities Harbored Inside

Published on: July 3, 2016

氷期と氷期後の温度差は,化石の骨におけるアスパルチン酸のラセミ化から推論された

R A Schroeder, J L Bada

    Science (New York, N.Y.)
    |November 2, 1973
    PubMed
    まとめ

    古代気候学の研究は,最後の氷河期以降の大陸の温暖化を明らかにしています. 化石骨におけるアスパルティック酸のラセミゼーションは,重要な地域における4~6°Cの温度上昇を示している.

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