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[2]
Organic Carbon Isotopic Evolution during the Ediacaran-Cambrian Transition Interval in Eastern Guizhou,South China: Paleoenvironmental and Stratigraphic Implications[J]. YANG Xinglian, ZHU Maoyan, GUO Qingjun and ZHAO Yuanlong College of Resource and Environment, Guizhou University, Guiyang, Guizhou 550003 State Key Laboratory of Palaeobiology and Stratigraphy, Nanjing Institute of Geology and Palaeontology, Chinese Academy of Sciences, Nanjing, Jiangsu 210008 State Key Laboratory of Environment
[3]
Discovery of sponge body fossils from the late Meishucunian (Cambrian) at Jinsha, Guizhou, south China[J]. YANG Xinglian 1,2*, ZHAO Yuanlong2, WANG Yue2 and WANG Pingli2(1. Nanjing Institute of Geology and Palaeontology, Chinese Academy of Sciences, Nanjing 210008, China;2. Institute of Resource and Environment, Guizhou University, Guiyang 550003, China).Progress in Natural Science. 2005(08)
[7]
Re-Os isotopes and PGE geochemistry of black shales and intercalated Ni-Mo polymetallic sulfide bed from the Lower Cambrian Niutitang Formation, South China[J]. JIANG Shaoyong*, YANG Jinghong, LING Hongfei, FENG Hongzhen, CHEN Yongquan and CHEN Jianhua(State Key Laboratory for Mineral Deposits Research, Department of Earth Sciences, Nanjing University, Nanjing 210093, China).Progress in Natural Science. 2003(10)