首页> 外文会议>International Symposium on the Cambrian System and Field Conference of the Cambrian Stage Subdivision Working Group; 200508; Nanjing(CN) >EDIACARAN-CAMBRIAN BOUNDARY SECTIONS AND EARLY CAMBRIAN CHENGJIANG NONMINERALIZED FOSSILS IN EASTERN YUNNAN PROVINCE, SOUTHWESTERN CHINA: INTRODUCTION
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EDIACARAN-CAMBRIAN BOUNDARY SECTIONS AND EARLY CAMBRIAN CHENGJIANG NONMINERALIZED FOSSILS IN EASTERN YUNNAN PROVINCE, SOUTHWESTERN CHINA: INTRODUCTION

机译:云南省东部东部地区的EDIACARAN-CAMBRIAN边界断面和成都市的早期CAMBRIAN化石化石:简介

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摘要

Eastern Yunnan lies on the southwestern margin of the Yangtze Platform, South China. Lower Cambrian strata are extensively developed and well exposed in the area (Fig. 1). Since the beginning of the last century (Depret, 1912), eastern Yunnan has been a special place for the study on the Neoproterozoic-lower Cambrian in China (Zhu et al., 2001), because of the following reasons: 1, the presence of well developed, well exposed Lower Cambrian strata containing the most complete sequence of lower Cambrian shallow-water environments in China; and 2, the presence of abundant fossils recording a clear succession of Early Cambrian communities.
机译:云南东部位于中国南方扬子台地西南缘。下寒武纪地层发育广泛,并在该地区充分暴露(图1)。自上世纪初(Depret,1912)以来,云南东部一直是中国新元古代-下寒武统研究的特殊场所(Zhu等,2001),原因如下:1,存在发育良好,暴露良好的下寒武统地层,其中包括中国下寒武统浅水环境的最完整序列; 2,大量化石的存在记录了早期寒武纪群落的明显继承。

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