• 责任者：Tang Feng (Institute of Geology ; Chinese Academy of Geological Sciences ; Beijing 100037 ; China) ; Yin Chongyu
• 刊名：Geological Review
• 出版年：2009
• 卷期：55(3)
• 关键词：新元古代 ; Neoproterozoic Era ; 生物地层学 ; biostratigraphy ; 生物年代学 ; biochronology ; 华北地台 ; North China Platform
• 页码：p.305-317
• 图表：2 illus., 59 refs.
• 分类号：1200
• issnNo：ISSN0371-5736
• isbnNo：CN11-1952/P

The most complete and continuous strata of Late Precambrian in China are known to occur in the east area of North China Craton, especially in the east margin of North China Craton yield the whole Neoproterozoic sedimentary sequences from bottom to top, which are the crucial strata for stratigraphic correlation and linking the Neoproterozoic between North and South China. The macrofossil assemblage (i.e. Longfengshan Biota, Liaonan Biota and Huainan Biota) discovered and established in this area might have been recognized as several distinctive and diverse communities preceded or followed “the Nanhuan Glaciation” during the Neoproterozoic era. Large quantities of these Neoproterozoic macrofossils have generally been interpreted as multicellular metaphytes and metazoans which are the important representatives of the ancient life in the surface of the 1 000～542 Ma.