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Plant assemblage from Opole,southern Poland: New data on Late Cretaceous vegetation of the northern part of the European Province
Authors:Bartosz J P?achno  Agata Jurkowska  Grzegorz Pacyna  El?bieta Worobiec  Przemys?aw Gedl  Ewa ?wierczewska-G?adysz
Institution:1. Department of Plant Cytology and Embryology, Jagiellonian University in Kraków, Gronostajowa 9 St., 30-387 Kraków, Poland;2. AGH University of Science and Technology in Kraków, Faculty of Geology, Geophysics and Environmental Protection, Mickiewicza 30?St., 30-059 Kraków, Poland;3. Department of Taxonomy, Phytogeography and Palaeobotany, Institute of Botany, Jagiellonian University in Kraków, Kopernika 27 St., 31-501 Kraków, Poland;4. W. Szafer Institute of Botany, Polish Academy of Sciences, Lubicz 46 St., 31-512 Kraków, Poland;5. Institute of Geological Sciences, Polish Academy of Sciences, Research Center in Kraków, Senacka 1 St., 31-002 Kraków, Poland;6. Institute of Earth Sciences, University of ?ód?, Narutowicza 88 St., 90-139 ?ód?, Poland
Abstract:This paper presents the results of studies on plant macroremains found in the upper Turonian of the Folwark Quarry, Opole, Poland, associated with palynological studies of the host rocks. In addition to a few macrofossils (gymnosperm wood, conifer Geinitzia reichenbachii and fern ?Didymosorus) rich sporomorphs (bryophyte, lycopod and fern spores, conifer and angiosperm pollen grains) and marine palynomorphs (mainly dinoflagellate cysts) were recorded. The palynological analysis revealed that the vegetation on the neighbouring land (the East Sudetic Island) in the late Turonian was much more diverse than could be reconstructed based on only macrofossil remains. The latter are taxonomically restricted and dominated by one gymnosperm species (Geinitzia reichenbachii), which make them similar to most neighbouring, coeval Central European assemblages. Its over representation is, thus, a result of taphonomy.
Keywords:Cretaceous  Upper Turonian  Palynomorphs  Palaeoenvironment  Poland
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