Abstract
On the basis of study of fossil plants, the climate in southwestern Siberia in the Early Senonian was reconstructed to be warm temperate humid with the mean annual temperature of about 13°C. The CLAMP analysis (Climate Leaf Analysis Multivariate Program) was applied for the first time to Cretaceous floras of Western Siberia. The comparison results of climatic variables estimated show that the climate in Western Siberia in the Early Senonian was more humid and warmer than in Northeast Asia.
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