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Un cambio de los lagos termokarst de fuentes de carbono a sumideros durante la época del Holoceno

K M Walter Anthony1, S A Zimov2, G Grosse3

  • 1Water and Environmental Research Center, University of Alaska, Fairbanks, Alaska 99775-5860, USA.

Nature
|July 22, 2014
PubMed
Resumen

Los lagos de termokarst en Siberia y Alaska secuestran más carbono del que liberan, pasando del calentamiento al enfriamiento del clima hace 5.000 años. Este almacenamiento de carbono en los sedimentos de los lagos es crucial para comprender las regiones de permafrost.

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