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Palaeoclimatology: Archaean atmosphere and climate
1Department of Geosciences, Pennsylvania State University, University Park, Pennsylvania 16801, USA. kasting@geosc.psu.edu
Nature
|December 8, 2004
Abstract:
Ohmoto et al. argue that carbon dioxide was abundant in the late Archaean and early Proterozoic atmosphere and that methane was probably scarce, based on a reanalysis of the occurrence of siderite, FeCO3, in ancient rocks. Here I consider several factors that may undermine their conclusions.
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