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Measuring Carbon-based Contaminant Mineralization Using Combined CO2 Flux and Radiocarbon Analyses
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La inyección de carbono atmosférico vinculada a la extinción masiva de finales del Triásico

Micha Ruhl1, Nina R Bonis, Gert-Jan Reichart

  • 1Palaeoecology, Institute of Environmental Biology, Faculty of Science, Utrecht University, Budapestlaan 4, NL-3584 CD, Utrecht, Netherlands. micharuhl@gmail.com

Science (New York, N.Y.)
|July 23, 2011
PubMed
Resumen

La extinción masiva de finales del Triásico fue impulsada por la liberación masiva de metano, causando un cambio climático severo y una excursión de isótopos de carbono de ~8,5 por mil. Este evento condujo a una importante rotación del ecosistema terrestre y a la pérdida de biodiversidad marina.

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