The Zhuganpo Formation is a Triassic geologic unit found in southern China. It has historically been known as the Zhuganpo Member of the Falang Formation. A diverse fossil assemblage known as the Xingyi biota or Xingyi Fauna can be found in the upper part of the Zhuganpo Formation. Fossils of the Xingyi biota include articulated skeletons of marine reptiles, abundant fish, and a plentiful assortment of invertebrates indicating a Ladinian to Carnian age for the sediments of the formation.
Paleobiota
Invertebrates
- Ammonites: Clionitites sp., Detoniceras sp., Haoceras xingyiense, Parasturia sp., Protrachyceras sp., Ptychites sp., Sinomeginoceras (S. wangi, S. xingyiense), Trachyceras sp., Xenoprotrachyceras cf. primum, Yangites densicostatus,
- Bivalves: Daonella sp.
- Conodonts: Gladigondolella malayensis, Metapolygnathus / Paragondolella / Quadralella (Q. aff. acuminatus, P. foliata, P. inclinata, Q. intermedius, Q. langdaiensis, P. maantangensis, P. navicula, M. nodosus, M. parafoliata, Q. aff. praelindae, P. polygnathiformis, Q. shijiangjunensis, Q. tadpole, Q. uniformis, Q. wanlanensis, Q. aff. wayaoensis, Q. yongueensis, Q. aff. zonneveldi)
- Crinoids: Traumatocrinus hsui
- Crustaceans ("shrimps"): Schimperella acanthocercus (Lophogastrida)'
Fish
Reptiles
References