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Flujo de manganeso de los sedimentos del margen continental en un transecto a través del mínimo de oxígeno

K S Johnson, W M Berelson, K H Coale

    Science (New York, N.Y.)
    |August 28, 1992
    PubMed
    Resumen

    El flujo de manganeso de los sedimentos del margen continental es más alto en la plataforma poco profunda. El flujo de manganeso de los sedimentos disminuye con el oxígeno, y no explica los máximos de manganeso subterráneo del Océano Pacífico.

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