Abstract
Abstract Leaf macroremains collected in the Bełchatów Lignite Mine (central Poland) were investigated. The fossil assemblage consists of leaves of Acer, Betula, Carpinus, Dicotylophyllum, Fagus, ?Magnolia, “Parrotia”, Pinus, Quercus, and Zelkova. Mesophytic (zonal) elements dominate, with admixture of riparian (azonal) leaf taxa. The floristic composition points to late Neogene (late Miocene to late Pliocene) age and suggests favourable temperate climate with mild winters.
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