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Transición glacial-holoceno en carbonatos de aguas profundas: disolución selectiva y la señal de isótopos estables

W H Berger, J S Killingley

    Science (New York, N.Y.)
    |August 5, 1977
    PubMed
    Resumen

    El pulso de disolución del Holoceno impactó significativamente las señales isotópicas del plancton Foraminifera en el Pacífico ecuatorial occidental. Este evento de disolución, que comenzó hace unos 12.000 años, afectó a los isótopos de oxígeno y carbono durante la transición glacial al Holoceno.

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