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El dióxido de carbono atmosférico a través de la transición climática del Eoceno-Oligoceno

Paul N Pearson1, Gavin L Foster, Bridget S Wade

  • 1School of Earth and Ocean Sciences, Cardiff University, Cardiff CF10 3YE, UK. pearsonp@cardiff.ac.uk

Nature
|September 15, 2009
PubMed
Resumen

La formación de la capa de hielo antártica fue provocada por una caída significativa en los niveles de dióxido de carbono (CO2) atmosférico. La reducción de CO2 precedió al crecimiento del hielo, con niveles estabilizados alrededor de 760 partes por millón durante la glaciación máxima.

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