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Measuring Carbon-based Contaminant Mineralization Using Combined CO2 Flux and Radiocarbon Analyses
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Registro de hielo de delta13C para el CH4 atmosférico a través de la transición Younger Dryas-Preboreal

Hinrich Schaefer1, Michael J Whiticar, Edward J Brook

  • 1School of Earth and Ocean Sciences, University of Victoria, Post Office Box 3055, V8W 3P6, Canada. schaefeh@geo.oregonstate.edu

Science (New York, N.Y.)
|August 26, 2006
PubMed
Resumen

Las proporciones de isótopos de carbono de metano atmosférico de Groenlandia durante la transición del Dryas más joven al Prebóreo sugieren mayores emisiones de metano natural o una fraccionamiento del sumidero más fuerte de lo que se suponía anteriormente. Esto indica un complejo ciclo de metano durante este antiguo cambio climático.

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