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Evidencia de isótopos de boro para la fuga de dióxido de carbono oceánico durante la última deglaciación

M A Martínez-Botí1, G Marino2, G L Foster1

  • 1Ocean and Earth Science, National Oceanography Centre Southampton, University of Southampton Waterfront Campus, Southampton SO14 3ZH, UK.

Nature
|February 13, 2015
PubMed
Resumen

Los niveles de dióxido de carbono (CO2) en la atmósfera fluctuaron significativamente durante los períodos glaciales. Este estudio revela que el Océano Austral liberó CO2 durante las deglaciaciones, apoyando su papel en la regulación del clima de la Tierra.

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