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出 处:《沉积与特提斯地质》2005年第4期37-41,共5页Sedimentary Geology and Tethyan Geology
基 金:国土资源大调查项目"贵州1:25万安顺市幅区域地质调查(修测)"
摘 要:六枝—盘县地区的早二叠世隆林期地层,相区分异明显、类化石数量巨大。各相区类化石群落特征差异较大:半局限台地相为Staffella-Nankinella-Pisolina;台地边缘生物滩(礁)相为Parafusulina-Pseudofusulina;斜坡-盆地相为Pseudofusulina,进一步划分为近岸碳酸盐上缓坡环境的Staffella-Parafusulina-Wentzellophyllum群落、远岸碳酸盐上缓坡环境的Pamirina-Schwagerina-Pseudofusulina群落、碳酸盐下缓坡环境的Pseudofusulina-Robustoschwagerina-Kepingophyllum群落和盆地环境的Pseudofusulina-Schwagerina-Verbeekiella群落。The fusulinid communities are quite variable in the Longlinian (Early Permian) strata in distinct sedimentary environments in the Liuzhi-Panxian region, Guizhou: StaffeUa-Nankinella-Pisolina community in the seml-restricted platform facies; Parafusulina-Pseudofusulina community in the platform-margin organic shoal (reefs) facies, and Pseudofusulina community in the slope-basin facies. Four communities may further be recognized for the last one outlined above, including: Sta.ffeUa-Parafusulina-Wentzellophyllum community in the nearshore upper carbonate ramp environment; Pamirina-Schwagerina-Pseudofusulina community in the offshore upper carbonate ramp environment; Pseudofusulina-Robustoschwagerina-Kepingophyllum community in the lower carbonate ramp environment, and Pseudofusulina-Schwagerina-Verbeekiella community in the basin environment .
关 键 词:早二叠世 隆林期 竹蜓类群落 沉积环境 六枝-盘县 贵州
分 类 号:P534.46[天文地球—古生物学与地层学]
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