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《Acta Sedimentologica Sinica》 2009-03
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Trace Fossils and Their Depositional Environments of the Early Triassic Daye Formation in Huaxi Area,Guiyang

SHI Guo1 YU Mei-yi2 LUO Mao3 TIAN Jing-chun1(1.Institute of Sedimentary Geology,Chengdu University of Technology,Chengdu,610059;2.School of Resource and Environment Technology,Guizhou University,Guiyang 550003;3.Guangzhou Institute of Geochemistry;Chinese Acndery of Sciences;Guangzhou 510640)  
There are lots of trace fossils preserved in the Lower Triassic Daye Formation in Huaxi area of Guiyang.Eighteen ichnogenera have been found in this region:Beaconichnus,Circulichnis,Cosmorhaphe,Dendrohaphe,Glockerichnus,Gyrochorte,Gordia,Maeandropolydora,Micatuba,Mammillichnis,Megagrapton,Planolites,Palaeophycus,Phycodes,Phycosiphon,Rhizocorallium,Thalassinoides and Undichna.Some trace fossils have been found for the first time,and they are Circulichnis,Glockerichnus,Maeandropolydora.Three ichnofabrics have been found in Daye Formation,including:Phycodes ichnofabric,Phycosiphon-Mammillichnis ichnofabric and Thalassinoides ichnofabric.Based on the relative abundance of the ichnogenera in Daye Formation,four ichnofacies have been distinguished:Cruziana ichnofacies of the first and third member,Zoophycos ichnofacies and Nereites ichnofacies of the second member.Combined with the analysis on ichnofabrics,the ichnofacies research shows that the study area located the front line of carbonate platform slope margin,and reflected less energy and anoxia environment.Phycodes ichnofabric and Thalassinoides ichnofabric can be assigned to Cruziana ichnofacies,Phycosiphon-Mammillichnis ichnofabric can be assigned to Zoophycos ichnofacies-Nereites ichnofacies.
【Fund】: 国家自然科学基金重点项目(批准号:40262001)资助
【CateGory Index】: Q915
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