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During the geological mapping in the Boskovice Basin, two new palaeobotanical localities in Veverske Kninice and a locality in Veverska Bitýska have been found. The most abundant flora comes from the Veverske Kninice 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, Řicany Horizon of the Permian (Rotliegend, Asselian) age. The subsequent Veverska Bitýska Formation belongs still to the Asselian. This formation contains Chudcice Horizon that yields very poor conifer flora at the Veverska Bitýska 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.

NOVÉ FYTOPALEONTOLOGICKÉ NÁLEZY V PERMU BOSKOVICKÉ PÁNVE U VEVERSKÉ BÍTÝŠKY