Nonfusulinid Foraminiferal Fauna from the Permian Chihsia Formation, Northwestern Sichuan Basin

Abstract

Abstract:

The Permian nonfusulinid foraminifers of the Chihsia Formation are collected from Wangjiagou section in Wangcang County, Northwestern Sichuan Basin. The Chihsia Formation of Wangjiagou section is a suit of mediumbedded to thickbedded limestones, with thickness of about 108 meters. Based on the systematic study to the Chihsia Formation, 27 species of 14 genera (including conformis species and subspecies) of the nonfusulinid foraminiferal fauna have been recognized in the Wangjiagou section. The Globivalvulina assemblage is suggested as indicative fauna for recognition of the Permian largest transgressive period. The result of this study not only enriches the fossil database of Sichuan Basin, but also provides more palaeontological evidences for stratigraphic correlation in South China.

Key words: nonfusulinid foraminifer, Chihsia Formation, Permian, Wangjiagou section, Northwestern Sichuan Basin

ZHANG Zhou, ZHANG Ting-Shan, LA Guang-Zhi. Nonfusulinid Foraminiferal Fauna from the Permian Chihsia Formation, Northwestern Sichuan Basin[J]. Geoscience, 2011, 25(5): 987-994.

References

［1］郝诒纯,林甲兴.论粤、桂、湘、鄂二叠纪有孔虫的组合特征［J］.地球科学, 1982 ,16(1):19-33.
［2］王克良.华南小有孔虫Langella动物群及其地层意义［J］.微体古生物学报, 1988,5(3):275-282.
［3］王克良.横断山地区石炭纪和二叠纪有孔虫［J］.微体古生物学报, 2002,19(2):112-113.
［4］林甲兴.广东、湖南早石炭世的有孔虫及其地层意义［J］.中国地质科学院宜昌地质矿产研究所所刊.地层古生物专号,1981:1-14.
［5］林甲兴.广东加禾下二叠统栖霞组的有孔虫［J］.地质论评, 1985,31(4):289-294.
［6］林雪山.闽西晚石炭世晚期—早二叠世有孔虫动物群［J］.古生物学报, 1990,29(6):716-733.
［7］张祖辉,洪祖寅.福建宁化早二叠世早期的小有孔虫动物群［J］.微体古生物学报, 2001,18(3):254-262.
［8］董宝清,刘家润,施贵军.贵州紫云扁平剖面早二叠世非有孔虫动物群［J］.地层学杂志, 2007,31(4):317-324.
［9］傅瑜.应用有孔虫及藻类分布特征探讨四川盆地二叠纪阳新世沉积条件［M］//中国微体古生物学会.中国微体古生物学会第一次学术会议论文选集.北京:科学出版社,1981:19-25.
［10］傅瑜.四川早二叠世有孔虫［M］//中国油气区地层古生物论文集编辑委员会.中国油气区地层古生物论文集（一）.北京:石油工业出版社,1987:243-253.
［11］王克良.二叠纪、石炭纪有孔虫［M］//中国科学院南京地质古生物研究所.西南地区地层古生物手册.北京:科学出版社,1974:248-256.
［12］傅瑜.有孔虫目.西南地区古生物图册.四川分册（二）［M］.北京:地质出版社,1978:5-18.
［13］四川油气区地质志编写组.中国石油地质志（卷十）.四川油气区［M］.北京:石油工业出版社,1989:28-79.
［14］四川省地质矿产局.四川省区域地质志［M］.北京：地质出版社,1991:182-205.
［15］金玉玕,尚庆华，侯静鹏，等.中国地层典:二叠系［M］.北京：地质出版社,2000:1-143.
［16］谷峰,冯少南,张淼.二叠系［M］//汪啸风，陈孝红.中国各地质时代地层划分与对比.北京:地质出版社，2005：277-299.
［17］陈宗清.论四川盆地中二叠统栖霞组天然气勘探［J］.天然气地球科学, 2009,20(3):325-334.
［18］宋章强,王兴志,曾德铭.川西北二叠纪栖霞期沉积相及其与油气的关系［J］.西南石油学院学报,2005,27(6):20-23.
［19］郝诒纯,裘松余,林甲兴，等.有孔虫［M］.北京:科学出版社,1980:1-224.
［20］施贵军,董丽萍,刘庆国，等.滇东石林地区早—中二叠世Globivalvulina有孔虫动物群［J］.微体古生物学报, 2009,26(2):148-157.
［21］林甲兴,李家骧,孙家英.华南地区晚古生代有孔虫［M］.北京:科学出版社,1990:1-279.
［22］王克良.西藏石炭纪及二叠纪有孔虫\
[M\]//中国科学院南京地质古生物研究所.西藏古生物（四）.北京:科学出版社, 1982:1-32.
［23］张志存.海南岛栖霞期鹅顶组的小有孔虫化石［J］.科学通报, 1990,35(16):1279-1280.
［24］张祖辉,洪祖寅.福建武平中二叠统童子岩组的小有孔虫［J］.微体古生物学报, 2000,17(1):39-56.
［25］林甲兴.广东加禾下二叠统栖霞组的有孔虫［J］.地质论评, 1985,31(4):289-294.
［26］地质矿产部成都地质矿产研究所.四川盆地及其边缘地区早二叠世区域沉积相及油气关系研究［R］.1985:81-117.
［27］刘本培,全秋琦.地史学教程［M］.北京:地质出版社, 1996:165-179.
［28］颜佳新,杜远生.冰川发育对赤道地区碳酸盐沉积环境和沉积作用的影响［J］.地质科技情报, 1994,13(3):48-56.
［29］颜佳新.华南地区二叠纪栖霞组碳酸盐岩成因研究及其地质意义［J］.沉积学报, 2004,22(4):579-587.
［30］施春华,胡瑞忠,颜佳新.栖霞组沉积地球化学特征及其环境意义［J］.矿物岩石地球化学通报, 2004,23(2):144-148.
［31］李朋威,吴夏,白晓，等.四川广元上寺剖面二叠系栖霞组沉积碳库与有机碳埋藏［J］.古地理学报, 2010,12(3):302-306.
［32］李芝君,王大锐.浙江省桐庐县瑶琳地区下二叠统栖霞-茅口组有孔虫动物群及其环境探讨［J］.石油勘探与开发, 1985,1(1):29-35.

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Nonfusulinid Foraminiferal Fauna from the Permian Chihsia Formation, Northwestern Sichuan Basin

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