A study of Late Carboniferous and Early Permian plant assemblages from the Boskovice Basin, Czech Republic

Late Stephanian and Early Permian floras were collected in eight localities of the Boskovice Basin. More than 2700 specimens were studied. The Carboniferous wet-type flora (Rosice-Oslavany Formation) is relatively hygrophilous with a dominance of ferns (Pecopteris cyathea and P. densifolia) and a smaller representation of sphenopsids (Annularia sphenophylloides). Pteridosperms and cordaitaleans are rare. Conifers (Ernestiodendron filiciforme), as drier-type elements, occur locally above the 1st (uppermost) coal seam of the Rosice-Oslavany coals together with many representatives of pteridosperms (medullosans, Odontopteris schlotheimii). This indicates the beginning of seasonality and aridisation of the climate. The Permian flora is dominated by conifers and is of an and character. Some horizons contain a relatively high proportion of pteridosperms (Zbysov, Ricany and Zbonek-Svitavka horizons), however, the species spectrum differs and the Permian pteridosperms are mainly represented by peltasperms (Autunia conferta). Ferns and sphenopsids are extremely rare in the Permian horizons. The flora reflects changes in the basin from relatively wet climate in the Rosice-Oslavany Formation to the seasonal and dry climate during the Permian. The Permian extrabasinal floral elements preserved in fossiliferous horizons grew in the basin during the seasonal climate. The red sediments outside the fossiliferous horizons are barren, presumably reflecting a semi-arid climate. The seasonality and less or more dry periods during the Permian are documented changes in diversity and dominance of the flora, and by cluster analysis. Using unconstrained Jaccard's analysis, the Carboniferous wet-type flora is clearly separated from the dry-type Permian flora. Even though the Chudcice Horizon is approximately in the middle of the section, it is placed in this analysis at the top of the dendrogram together with the dry-type floral clusters. This analysis reflects an aridisation trend rather than biostratigraphically determined changes. As a result of four excavations, 15 species are here for the first time reported from the Boskovice Basin: Pecopteris cf. bredovii, Remia pinnatifida, Odontoptenis lingulata, Neurocallipteris gallica, N. planchardii, Rhachiphyllum aff. curretiensis, ?R. subauriculata, Dicranophyllum longifolium, Culmitzschia angustifolia, Hermitia arnhardtii, H. germanica, H. rigidula, H. schlotheimii, and bifurcated leaves of uncertain affinity. (C) 2008 Elsevier B.V. All rights reserved.