1 中国地质大学生物地质与环境地质国家重点实验室，湖北武汉 430074 2 School of Life and Environment，Deakin University， Melbourne Campus，Victoria 3125，Australia 3 贵州省地质调查院，贵州贵阳 550005
The Devonian trace fossils and ichnofacies from South China
Zhang Lijun1,2, Gong Yiming1, Ma Huizhen3
1 State Key Laboratory of Biogeology and Environmental Geology，China University of Geosciences，Wuhan 430074，Hubei 2 School of Life and Environment，Deakin University，Melbourne Campus， Victoria 3125，Australia 3 Guizhou Academy of Geologic Survey，Guiyang 550005，Guizhou
Abstract：Fifteeen ichnogenera and twenty-four ichnospecies were recognized on the basis of detailed ichnosedimentology studies of six Devonian sections from South China.They included Arenicolites carbonaria，Arenicolites isp.，Chondries cf.intricatus，Chondrites fenxiangensis，Chondrites filifalx， Chondrites isp.， Chondrites maqianensis，Circulichnis isp.， Dushanichnus dahekouensis， Diplocraterion parallelum， Rusophycus lungmenshanensis，？Helminthopsis isp.， Palaeophycus tubularis，Palaeophycus curvatus，Phycodes palmatus， Planolites beverleyensis， Planolites isp.， Planolites kwangsiensis， Rosselia socialis， Rhizocorallium jenense， Rhizocorallium isp.，Skolithos linearis， Thalassinoides isp.，Zoophycus isp.. These trace fossils can be grouped into four ichnofacies of Skolithos，Rhizocorallium，Cruziana，Zoophycos ichnofacies in terms of body fossils and other facies indicators.Skolithos，Rhizocorallium，Cruziana and Zoophycos ichnofacies indicated tidal flat and barrier island-lagoon environments，intertidal-subtidal zones，upper-middle neritic shelf and lower neritic-bathyal environments，respectively.From the Early to Late Devonian，the replacement of ichnofacies was from Skolithos ichnofacies→ Rhizocorallium ichnofacies → Cruziana ichnofacies → Zoophycos ichnofacies → Rhizocorallium ichnofacies.
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