“…The Xishancun, Xitun, Guijiatun and Xujiachong formations (in ascending chronological order) represent the Early Devonian non-marine strata in Qujing District ( Liu & Wang, 1973 ; P’an et al, 1978 ; Zhu, Wang & Fan, 1994 ; Liu, Gai & Zhu, 2018 ). The Xitun Formation consists mainly of grayish-green muddy limestone and mudstone ( Fang et al, 1985 ; Xue, 2012 ), yielding a rich biota (Cuifengshan Assemblage) characterized by the diversification of sarcopterygians ( Chang & Yu, 1981 ; Chang & Yu, 1984 ; Zhu, Yu & Janvier, 1999 ; Zhu, Yu & Ahlberg, 2001 ; Zhu & Yu, 2002 ) and primitive antiarchs including Yunnanolepis, Parayunnanolepis , Zhanjilepis , Chuchinolepis and Phymolepis . Other fishes in the Xitun Formation include the endemic agnathans ( Liu et al, 2015 ), arthrodires ( Dupret, Zhu & Wang, 2017 ), actinopterygians ( Zhu et al, 2006 ; Lu et al, 2016 ), acanthodians and chondrichthyans, the latter two of which are mostly known from microvertebtrate remains ( Wang, 1984 ).…”