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Pozzi, Francesca, Deborah Balk and Greg Yetman. 2003. The transition from an ice age to an ice-free planet 300 million years ago was highly unstable, marked by dips and rises in carbon dioxide, extreme swings in climate and drastic effects on tropical vegetation. "This is the best documented record we have of what happens to the climate system during long-term global warming following an ice age," said Isabel Montañez, professor of geology at the University of California, Davis, and lead author on the paper.

Pages: 20

Publisher: BiblioGov (August 2, 2012)

ISBN: 124921498X

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