Comments on the BLAG model:  the carbonate-silicate geochemical cycle and its effect on atmospheric carbon dioxide over the past 100 million years.
A self-consistent method of determining initial conditions for the model presented by Berner, Lasaga, and Garrels (1983) (henceforth, the BLAG model) is derived, based on the assumption that the CO2 geochemical cycle was in steady state at t = -100 my (million years).  This initialization procedure leads to a dissolved magnesium concentration higher than that calculated by Berner, Lasaga, and Garrels and to a low ratio of dissolved calcium to bicarbonate prior to 60 my ago.  The latter prediction conflicts with the geologic record of evaporite deposits, which requires that this ratio remain greater than 0.5.  The contradiction is probably caused by oversimplifications in the BLAG model, such as the neglect of the cycles of organic carbon and sulfur.
Kasting
J F
JF
Space Science Division, NASA Ames Research Center, Moffett Field, California 94035, USA.
D001272:Atmosphere; D001639:Bicarbonates; D002118:Calcium; D002119:Calcium Carbonate; D002245:Carbon Dioxide; D018534:Earth, Planet; D019419:Evolution, Planetary; D055593:Geological Phenomena; D005844:Geology; D008274:Magnesium; D008903:Minerals; D008956:Models, Chemical; D012623:Seawater
D001639:Bicarbonates; D008903:Minerals; D002245:Carbon Dioxide; D002119:Calcium Carbonate; D008274:Magnesium; D002118:Calcium; C028042:calcium magnesium carbonate