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 in | Geochemistry, geophysics, geosystems : G3 Vol. 7; no. 11; pp. Q11019 - n/a |
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Main Authors | , , , , , |
Format | Journal Article |
Language | English |
Published |
American Geophysical Union
01.11.2006
Blackwell Publishing Ltd AGU and the Geochemical Society |
Subjects | |
Online Access | Get full text |
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