Biostratigraphic and Chemostratigraphic Correlation for the Base of the Middle Ordovician between Yichang and Western Zhejiang Areas,South China

作     者：ZHANG Yuandong Axel MUNNECKE CHEN Xu CHENG Junfeng LIU Xiao 

作者机构：State Key Laboratory of Palaeobiology and Stratigraphy Nanjing Institute of Geology and Palaeontology Nanjing 210008 China GeoZentrum Nordbayern FG Palaoumwelt University Erlangen-Nuremberg D-91054 Erlangen Germany Research Institute of Petroleum Exploration and Development East China Company SINOPEC Nanjing 210011 China 

出 版 物：《Acta Geologica Sinica(English Edition)》 (地质学报（英文版）)

年 卷 期：2011年第85卷第2期

页      面：320-329页

核心收录：

学科分类：0820[工学-石油与天然气工程] 081803[工学-地质工程] 0709[理学-地质学] 0819[工学-矿业工程] 08[工学] 0818[工学-地质资源与地质工程] 0708[理学-地球物理学] 0816[工学-测绘科学与技术] 082002[工学-油气田开发工程] 

基　　金：support from the Chinese Academy of Sciences (KZCX2-YW-122, CAS/SAFEA Program) the Ministry of Science and Technology of China (2006FY120300-4, 2008ZX05008-001) A.M. is grateful to the Deutsche Forschungsgemeinschaft (DFG Mu 2352/1) the Robert-Bosch-Stiftung (grant no. Nr. 32.5.8003.0009.0) the Uni-Bund Erlangen for their support 

主　　题：Graptolite biostratigraphy chemostratigraphy Middle Ordovician slope facies South China 

摘      要：The base of the Middle Ordovician （i.e. Dapingian Stage） has been defined at the first appearance datum （FAD） of conodont Baltoniodus？ triangularis at Huanghuachang, Yichang, China,but the precise correlation of the boundary to regions of other facies remain to be resolved. Herein we review the biostratigraphy and chemostratigraphy of the Huanghuachang Global Standard Stratotype-Section and Point （GSSP） section, and present our latest stratigraphic work on the nearby Chenjiahe s ection in Yichang, and the Hengtang Quarry section, Jiangshan, Zhejiang, which is regarded as representative of slope facies. The conodont and graptolite biostratigraphy as well as chemostratigraphy of the Chenjiahe section indicate that the base of the Middle Ordovician also falls within the graptolite Azygograptus suecicus Zone, and coincides with a high or maximum δ13C value within a minor positive carbon isotope excursion, suggesting that the base boundary can be readily recognized across the entire Yangtze Gorges area. The integrated graptolite and conodont biostratigraphy and chemostratigraphy of the Hengtang section, Jiangshan, indicates that the basal boundary probably falls within the graptolite lsograptus caduceus imitatus Zone that overlies the Azygograptus suecicus Zone, and coincides with a remarkable drop of δ13C. This difference indicates that a multi-disciplinary approach is critical to identify the base boundary in those regions where the Baltoniodus ？ triangularis is absent.