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Temperatura y equilibrio de aguas superficiales y oceánicas del medio holoceno tropical del Pacífico occidental

Gagan1, Ayliffe, Hopley

  • 1M. K. Gagan, L. K. Ayliffe, J. A. Cali, G. E. Mortimer, M. T. McCulloch, Research School of Earth Sciences, Australian National University, Canberra, ACT 0200, Australia. D. Hopley, Sir George Fisher Centre, James Cook University, Townsvil.

Science (New York, N.Y.)
|February 27, 1998
PubMed
Resumen

Datos de arrecifes de coral de hace 5350 años revelan una superficie oceánica tropical 1°C más cálida y 0,5‰ enriquecida en oxígeno-18 (18O). Este calentamiento aumentó la evaporación, influyendo potencialmente en los patrones climáticos globales y reconciliando los registros paleoclimáticos.

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