Atmospheric carbon dioxide linked with Mesozoic and early Cenozoic climate change
Carbon isotopes of fossil plants and model simulations suggest that atmospheric carbon dioxide levels were variable during the period 200 to 60 million years ago. The large decreases in the partial pressure of CO 2 coincide with glaciations, providing evidence against climate–CO 2 decoupling during...
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Veröffentlicht in: | Nature geoscience 2008-01, Vol.1 (1), p.43-48 |
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Format: | Artikel |
Sprache: | eng |
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