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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

Glacial-postglacial temperature difference deduced from aspartic Acid racemization in fossil bones

R A Schroeder, J L Bada

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

    Paleoclimatology research reveals continental warming after the last ice age. Aspartic acid racemization in fossil bones indicates a 4-6°C temperature increase in key regions.

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