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Ichnocoenosis of the Lower Devonian Pingyipu Formation, Longmen Mountain, Sichuan
详细信息   
摘要
The littoral-neritic sediments of Lower Devonian Pingyipu Formation in the Ganxi Section are enriched with ichnocoenosis , which consists of at least 11ichnogenera of Arenicolites , Chondrites , Cylindrichnus , Diplocraterion , Palaeophycus , Planolites , Phycodes , Rhizocorallium , Rusophycus , Skolithos , Thalassinoides.The ichnocoenoses represent types of domichnia , fodinichnia and cubichnia.Five ichnocoenoses under different sedimentary environments have been recognized as follows : 1 ) Planolites-Palaeophycus ichnocoenosis mainly consists of fodinichnia from a lower-energy zone of nearshore ; 2 ) Rusophycus-Phycodes ichnocoenosis mainly consists of fodinichnia and cubichnia generated in lower-energy zone of nearshore ; 3 ) Chondrites-Palaeophycus ichnocoenosis mainly consists of domichnia and fodinichnia as indicator of the lower-energy and suboxic conditions of lower nearshore ; 4 ) Skolithos-Cylindrichnus ichnocoenosis is characterized by dwelling burrows from higher-energy foreshore ; 5 ) Skolithos-Diplocrate-rionichnocoenosis , including dwelling and feeding burrows formed in lower-energy zones of upper nearshore enriched with food.

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