During the geological mapping in the Boskovice Basin, two new palaeobotanical localities in Veverské Knínice and a locality in Veverská Bítýška have been found. The most abundant flora comes from the Veverské Knínice localities. Conifers dominate in the floral assemblage. Pteridosperms are also relatively common, whereas ferns and sphenopsids are rare. These localities are assignable to the Padochov Formation, Říčany Horizon of the Permian (Rotliegend, Asselian) age. The subsequent Veverská Bítýška Formation belongs still to the Asselian. This formation contains Chudčice Horizon that yields very poor conifer flora at the Veverská Bítýška locality. Permian system is a period of progressing aridity in Moravia. Only fossiliferous horizons represent spans with higher humidity that enabled plants to live. However, the climate was not so humid, but it was rather seasonal, because pure hygrophyte plants lack in the assemblage, on the other hand, “xerophyte” plants, like conifers, dominate here.
