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Las plantas fósiles y el calentamiento global en el límite triásico-jurásico

McElwain1, Beerling, Woodward

  • 1Department of Animal and Plant Sciences, University of Sheffield, Sheffield, S10 2TN, UK.

Science (New York, N.Y.)
|August 28, 1999
PubMed
Resumen

Un importante evento de extinción masiva en el límite Triásico-Jurásico se relacionó con un aumento de cuatro veces en el dióxido de carbono atmosférico y un calentamiento del efecto invernadero de 3-4 ° C, causando temperaturas letales de las hojas y extinciones masivas de plantas.

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