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《Journal of Stratigraphy》 2013-04
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BIOSTRATIGRAPHY OF THE WUFENG-LUNGMACHI BLACK SHALES AT QILIN,XINGWEN COUNTY,SICHUAN PROVINCE

FAN Jun-xuan;WU Lei;CHEN Zhong-yang;CHEN Qing;ZHANG Lin-na;SOO Kwong-Yin;SINGH Navpreet;LI Xue-kang;WANG Yuan;State Key laboratory of Palaeobiology and Stratigraphy,Nanjing Institute of Geology and Palaeontology,Chinese Academy of Science;Key Laboratory of Economic Stratigraphy and Palaeogeography,Chinese Academy of Sciences;Shell China Exploration and Production Limited;Branch of Shunan Gas Field,PetroChina Southwest Oil and Gas Field Company;  
The Sichuan Basin is the most important area for the exploration and development of shale gas in South China.Recently we investigated two sections at Qilin,Xingwen County,Sichuan Province,the Qixinqiao section and the Qilin Well section.The biostratigraphic sequence of the Wufeng to Lungmachi black shales has been recognized,including eleven graptolite biozones and one shelly assemblage from the Dicellograptus complexus Zone of the Katian Stage(Upper Ordovician)to the Stimulograptus sedgwickii Zone of the Aeronian Stage(Llandovery,Silurian).The sequence can be correlated regionally and globally.From the unweathered outcrop at the Qixinqiao section,we found a continuous transition of litho-facies and bio-facies from the Kuanyinchiao Formation to the Lungmachi Formation,which represents the rapid change from the Hirnantiashelly fauna to the graptolite fauna of the Metabolograptus persculptus Zone,and the change from the well-oxygenated water to the anaerobic or dysaerobic water.This transition also represents the global sea-level rising resulted from the rapid glacial melting after the Hirnantian icehouse.
【Fund】: 国家自然科学基金(No.41221001、41272042、41290260);; 中国科学院知识创新工程重要方向性项目(KZCX2-EW-111)资助
【CateGory Index】: P539
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