University of Zagreb. Faculty of Science. Department of Biology.
Abstract
Paleoflora Europe od paleozoika do formiranja samog kontinenta sastavom prati evolucijsku sukcesiju. Nakon ustaljenja okolišnih uvjeta, prevladavaju termofilne vrste koje se sredinom miocena zbog zahlađenja počinju zamjenjivati mezofilnim vrstama i travnjacima. U kvartaru brojne glacijacije uništavaju raznolikost flore. Nakon glacijacija počinje se formirati današnja distribucija flore čiji je izvorni oblik izmijenjen antropogenim djelovanjem.Since the Paleozoic era, the constitution of European paleoflora follows succession dictated by evolution. After the stabilisation of environmental conditions, the flora is dominated by termophilous species which by the middle miocene period start to get replaced by mezophilous species and grasslands. In the Quarternary era numerous glaciations destroy the floral diversity. After the glaciations, today's floral distribution starts to form whose primal form is modified by anthropogenic influence
