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Updated: Jul 10, 2026

The Use of High-resolution Infrared Thermography (HRIT) for the Study of Ice Nucleation and Ice Propagation in Plants
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Published on: May 8, 2015

La inestabilidad del clima y la vegetación forzada por el CO2 durante la deglaciación del Paleozoico Tardío

Isabel P Montañez1, Neil J Tabor, Deb Niemeier

  • 1Department of Geology, University of California, Davis, CA 95616, USA. montanez@geology.ucdavis.edu

Science (New York, N.Y.)
|January 6, 2007
PubMed
Resumen

La deglaciación del Paleozoico tardío vio la transición de la Tierra de un invernadero de hielo a un estado de invernadero. Este estudio revela que los desplazamientos de dióxido de carbono (CO2) impulsaron cambios de temperatura y una importante reestructuración de la vida vegetal.

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