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在天山志留系、石炭系和东昆仑 西秦岭三叠系浊积岩系中遗迹化石发育 ,经研究计有 :Helminthopsishieroglyphica ,Neonereitesbiserialis,N .uniserialis,Palaeophycusisp .,P .serratus,P .striatus,P .tubularis,Paleodictyonimperfectum ,Phycodescircinnatum ,Phycosiphonincertum ,Planolitesannularis,P .bev erleyensis,P .montanus,Rhizocoralliumisp .,Scalaritubamissouriensis,Skolithosisp .,?Spirorhapheisp .,Sublorenziniaisp .Tambiaisp .,Taphrhelminthopsisauricularis,Teichichnusisp .,Thalassinoidesisp .。它们构成 4种遗迹化石组合 :Phycosiphon Palaeophycus组合、Neonereites Scalarituba组合、Paleodictyon组合和Phycodes Skolithos组合 ,分别代表局限缺氧深海盆地浊流沉积、半深海环境的中 上扇沉积、多岛洋环境的中 下扇沉积、半深海环境的中扇浊流沉积。
In the Tianshan Silurian, Carboniferous and the East Qinlong Triassic turbidite strata in East Kunlun, there are some fossil development: Helminthopsishieroglyphica, Neonereites biserialis, N.uniserialis, Palaeophycusisp., P.serratus, P.striatus, P .tubularis, Paleodictyonimperfectum, Phycodescircinnatum, Phycosiphonincertum, Planolitesannularis, P.bev erleyensis, P.montanus, Rhizocoralliumisp., Scalaritubamissouriensis, Skolithosisp.,? Spirorhapheisp., Sublorenziniaisp. Tambiaisp., Taphrhelminthopsisauricularis, Teichichnusisp., Thalassinoidesisp. They constitute four types of trace fossil assemblages: the Phycosiphon Palaeophycus assemblage, the Neonereites Scalarituba assemblage, the Paleodictyon assemblage and the Phycodes Skolithos assemblages, respectively representing turbidite sediments in localized anoxic deep-sea basins, mid-upper fan deposits in semi-deep sea environments, Fan deposition, semi-deep sea environment turbidite deposition.