摘要
According to C. Y. Wang’s report, the Upper Eocene in most part of Guangxi is represented by Dongjun and Nadu Formations, with its type section lying around Nadu area of Bose Basin. Palynoflora from the Tertiary sediments in Ningming, Changdun and Shangsi of southwest Guangxi indicates the Upper Eocene features, while the sediments are also comparable with Nadu Formation of the Bose Basin in lithological character. The present note concerns the pollen result from the sections of the above-mentioned
