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Aumento de la estacionalidad a través de la transición del Eoceno al Oligoceno en latitudes altas del norte

James S Eldrett1, David R Greenwood, Ian C Harding

  • 1Shell Exploration and Production UK Ltd, 1 Altens Farm Road, Nigg, Aberdeen, AB12 3FY, UK. james.eldrett@shell.com

Nature
|June 19, 2009
PubMed
Resumen

El clima global cambió de las condiciones de invernadero a las de invernadero hace 33,5 millones de años. Nuevos datos revelan un enfriamiento significativo y una mayor estacionalidad en el Ártico antes del crecimiento de la capa de hielo antártica.

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