“…The palynomorph assemblages of the Guyang Basin are dominated by gymnosperm pollen and filicopsida spores. Most of the gymnosperm pollen are conifers pollen represented by Perinopollenites , Classopollis , Piceaepollenites , Taxodites and Araucariacites , contain a large amount of Ginkgoales and Cycad pollen grains, plant macrofossils discovered in the study area, and include Coniopteris simplex , Podozamites lanceolatus , Sequoia gracilis , Ginkgo lepida , Sabinites gracilis , Elatides manchurensis , Elatides sp., Sabinites neimngonglica , Torreya grandis , Stenorachis lepida , Equisetites sp., and Taxus guyangensis (Jin, Wang, & Du, ; Xu et al, ). Other paleontologists also found a large number of macrofossils in the Guyang Formation (Table ).…”