The holotype of P. cuifengshanensis is IVPP V4225.3, a nearly complete trunk shield, and it was found in the Xitun Formation, near Cuifengshan.[2] The paratype is IVPP V4425.6, a posterior median dorsal plate, and several other specimens of varying completeness have also been referred to Phymolepis,[3] with some specimens also being recovered from the Xishancun Formation.[4]
References
^ abChang, K-J. (1978). Symposium on the Devonian System of South China: Early devonian antiarchs from Cuifengshan, Yunnan. Institute of Geology and Mineral Resources of the Chinese Academy of Geological Sciences, ed. Geological Press; Beijing: 1978; pp. 292–297.
^ abZhang, G. (1978). The antiarchs from the Early Devonian of Yunnan. Vertebrata PalAsiatica. 1978;16:147–186.