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Main Contents
The geologic history of the Devonian in the Nanning Distriet, Central
Guangxi, Southern China, is developed from analysis of the strata and
fossils, with special emphasis on the systematic description of the brachioplds,
conodonts and corals. Devonian rocks are widely distributed and well exposed
in the vicinity of Daliancun Village, Nanning and in the area between
the Wuhe and Liujing ( formerly Luching) railway stations of the Xiang
(Hunan)-Gui (Guangxi) Railway, especially in the Luujing area, Hengxian
County , Central Guangxi (Text-figs. 1,3,4), This region is herein called
the Nanning-Liujing District. Most of our Eollections have been gathered
from the Liujing area. Detailed stratigraphic sections and biostratigraphic
data are presented, from which faunal assemblages, based mainly on brachiopods,
ate given in detail. The age of the brachiopods with reference to evidence
provided by conodonts and dacryoconariids is discussed. Paleozoogeographic
and community ecologic conclusions are also tentatively drawn |
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