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云南石林石炭纪古盘虫类有孔虫及其沉积环境初探
引用本文:王超,施贵军,刘家润,吴祥和.云南石林石炭纪古盘虫类有孔虫及其沉积环境初探[J].微体古生物学报,2004,21(2):183-193.
作者姓名:王超  施贵军  刘家润  吴祥和
作者单位:1. 南京大学地球科学系,南京,210093
2. 贵州省地质调查院,贵阳,550004
基金项目:石林研究中心资助项目 ( 0 1-0 6-2 7)部分内容
摘    要:本文报道云南石林地区石炭纪中间界线附近地层的有孔虫动物群古盘虫类4属8种。分析数据显示,这类具有独特壳壁类型和形态特征的小有孔虫类群分布,与碳酸盐岩中的亮晶、团块、海百合茎以及双壳瓣类等成分的相关系数较大。综合分析结果认为,该区古盘虫类有孔虫分布与较浅水、具中等搅动、温暖及盐度正常的潮间带环境关系密切。

关 键 词:云南  石林  石炭纪  古盘虫类  有孔虫  沉积环境  化石
修稿时间:2003年11月12

The Archaediscacea from the Carboniferous of Stone Forest, Yunnan and the depositional environment
WANG Chao ,SHI Gui-jun ,LIU Jia-run and WU Xiang-he.The Archaediscacea from the Carboniferous of Stone Forest, Yunnan and the depositional environment[J].Acta Micropalaeontologica Sinica,2004,21(2):183-193.
Authors:WANG Chao  SHI Gui-jun  LIU Jia-run and WU Xiang-he
Institution:WANG Chao 1),SHI Gui-jun 1),LIU Jia-run 1) and WU Xiang-he 2) 1) Department of Earth Sciences,Nanjing University,Nanjing 210093 2) Institute of Geologic Survey,Guizhou Bureau of Geology and Mineral Exploration & Development,Guiyang 550004)
Abstract:Eight species belonging to 4 gene- ra of Archaediscacea have been described from the foraminiferal fauna of Middle Carboniferous Strata in Stone Forest Area, Yunnan Province. The data show that this foraminiferal fauna, characterized by distinctive wall structure and morphology, has been observed to be closely related to the presence of sparite, pelletoid, crinoid and bivalve fragments in the carbonate rocks. The result of analysis reveals that the distribution of the foraminiferal fauna is closely associated with the mid-tidal environment of shallow, warm water, medium turbulence , and normal salinity.
Keywords:Archaediscacea    foraminifera  depositional environment    Carboniferous    Stone Forest  Yunnan
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