A GEOCLIM simulation of climatic and biogeochemical consequences of Pangea breakup

Large fluctuations in continental configuration occur throughout the Mesozoic. While it has long been recognized that paleogeography may potentially influence atmospheric CO2 via the continental silicate weathering feedback, no numerical simulations have been done, because of the lack of a spatially...

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Published inGeochemistry, geophysics, geosystems : G3 Vol. 7; no. 11; pp. Q11019 - n/a
Main Authors Donnadieu, Y., Goddéris, Y., Pierrehumbert, R., Dromart, G., Fluteau, F., Jacob, R.
Format Journal Article
LanguageEnglish
Published American Geophysical Union 01.11.2006
Blackwell Publishing Ltd
AGU and the Geochemical Society
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