CO2 levels in the Late Palaeozoic and Mesozoic atmosphere from soil carbonate and organic matter, Satpura basin, Central India

A number of calcic palaeosols have been identified within the fluvial depos its of the Motur (Permian), the Denwa (Triassic), the Bagra (Jurassic) and the Lameta (Cretaceous) Formations of the Satpura sedimentary succession, C entral India. These palaeosols show accumulation of pedogenic carbonates in rhizocretions and glaebules. The carbon isotopic compositions of these car bonates and the coexisting soil organic matters are used to determine the i sotopic composition and the partial pressure of atmospheric CO2 using the C O2 palaeobarometer developed by Cerling [Am. J. Sci., 291 (1991) 377]. It i s seen that the atmospheric CO2 level increased by a factor of 8 from the P ermian to the Jurassic and declined again during the Cretaceous. The nature of the changes agrees with the result of the CO2 evolution model of Berner (GEOCARB II) but the magnitude of the CO2 increase in the Middle Jurassic and the Late Cretaceous was higher than the predicted value. Degassing of E arth's interior due to rapid break-up of the Gondwana landmass during the T riassic and Jurassic period could have caused the rapid CO increase. (C) 20 01 Elsevier Science B.V. All rights reserved.