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Sincrónicos eventos abruptos centenarios en el océano y la atmósfera durante la última deglaciación

Tianyu Chen1, Laura F Robinson2, Andrea Burke3

  • 1Bristol Isotope Group, School of Earth Sciences, University of Bristol, Bristol, UK. tc14502@bristol.ac.uk.

Science (New York, N.Y.)
|September 26, 2015
PubMed
Resumen

Los cambios en la circulación oceánica impulsaron rápidos aumentos de CO2 atmosférico durante la última deglaciación. Los datos de radiocarbono de los corales de aguas profundas revelan dos eventos "excesivos" vinculados a una mayor circulación atlántica, que tienen un impacto en los cambios climáticos.

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