A conodont-based Middle Triassic age assignment for the Luoping Biota of Yunnan, China  

作　　者：ZHANG QiYue ZHOU ChangYong LU Tao XIE Tao LOU XiongYing LIU Wei SUN YuanYuan HUANG JinYuan ZHAO LaiShi 

机构地区：[1]Chengdu Intitute of Geology and Mineral Resources,Geological Survey of China,Chengdu 610081,China [2]State Key Laboratory of Geological Processes and Mineral Resources,China University of Geosciences,Wuhan 430074,China

出　　处：《Science China Earth Sciences》2009年第10期1673-1678,共6页中国科学（地球科学英文版）

基　　金：Supported by China Geological Survey (Grant No. 1212010610211);National Natural Science Foundation of China (Grant Nos. 90714010, 40872003, 40621002);State Key Laboratory of the Ministry of Science and Technology of China and State MOST Special Fund from the Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences

摘　　要：The Luoping Biota consists of abundant and well-preserved marine fishes, reptiles, invertebrates, and plants. It occurs in the Middle Triassic Guanling Formation in Daaozi Village of Luoping County, Yun-nan Province, China. Based on conodonts, the Luoping Biota is determined to lie within the Nicoraella kockeli Zone, which is assigned to the Pelsonian substage of the Anisian.The Luoping Biota consists of abundant and well-preserved marine fishes, reptiles, invertebrates, and plants. It occurs in the Middle Triassic Guanling Formation in Daaozi Village of Luoping County, Yunnan Province, China. Based on conodonts, the Luoping Biota is determined to lie within the Nicoraella kockeli Zone, which is assigned to the Pelsonian substage of the Anisian.

关 键 词：Luoping BIOTA ANISIAN Guanling FORMATION CONODONT 

分 类 号：Q915[天文地球—古生物学与地层学]