A 400 million year carbon isotope record of pedogenic carbonate: Implications for paleoatmospheric carbon dioxide

A 400 my record of atmospheric carbon dioxide levels has been estimated by applying a CO2 paleobarometer to a database of 758 analyses of paleosol (fo ssil soil) carbonates. This database is a compilation of new data and previ ously published values from the literature. Many new analyses of Mesozoic p aleosols are reported, an era poorly represented in the literature. Results indicate that large fluctuations in atmospheric carbon dioxide levels have occurred over the study interval, ranging from the current level up to ten times the current level. Declining pCO(2) levels through the middle Paleoz oic culminate in low levels in the Early Permian. An abrupt increase in pCO (2) in the Early Permian is followed by a decrease prior to the Permo-Trias sic boundary. Carbon dioxide levels increase through the Triassic to approx 3000 ppmV, a level maintained through the Jurassic period. Levels lowered through the Cretaceous, dropping to less than 1000 ppmV prior to the Cretac eous-Tertiary boundary Relatively low levels persisted throughout the Cenoz oic, with some evidence of higher levels in the Eocene and Oligocene.