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《Journal of Stratigraphy》 1993-03
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A preliminary study of the Kaili Formation in the transitional area in South China and its synchronous strata

Zhao Yuan-long, Yuan Jin-hang, Zhang Zheng-hua, Mao Jia-ren, Huang You-zhuang, Gong Xian-ying and Wang Kun  
The Kaili Formation (Lower-Middle Cambrian) and its synchronous strata are widely distributed in the transitional belt between the Yangtze platform and the Southeast China geosyncline. This formation is characterized by well-developed shale, mudstone containing abundant trilobites and other organisms, such as echinoderms, medusae, hyolithes, sponges, brachiopods, vermes, gastropods and algae, which are named the Kaili Fauna by the authors. The synchronous strata of the Kaili Formation from northern Hunan, Jiangxi, southern Anhui are characterized by the developed shale, mudstone, limestone, dolomite yielding trilobites. The four trilobite zones of Kaili Formation are erected by Zhou Zhi-yi and others in ascending order, namely, 1. Nangaops-Kunmingaspis Zone, 2. Wuxunaspis Zone, 3. Oryctocephalus-Xingrenaspis Zone, and 4. Kootenia jialaoensis Zone. In the present paper we propose Bathynotus-Nangaops Zone instead of Nangaops-Kunmingaspis Zone, because this zone is restricted to the lowest part of the Kaili Formation and widely distributed in the transitional belt. By studying the Kaili Formation and its synchronous strata we suggest that the extinction of trilobite genera Bathynotus and Redlichia should be regarded as the end of the Lower Cambrian and the beginning of the Middle Cambrian, so that the Lower-Middle Cambrian boundary should be drawn between the Bathynotus-Nangaops Zone and the Wuxunaspis Zone.
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