The colonization of land by vascular plants is an extremely important phase in Earth's life history. This key evolutionary process is thought to have begun during the Middle Cambrian 1 period and culminated in the Silurian/Early Devonian period (interval about 509-393 million years ago (Ma)), and is documented primarily by microfossils (that is, by dispersed spores, phytodebris including fragments of algae, tissues, sporangia and cuticles), tubes and rare megafossils 2 . A newly recognized fossil cooksonioid plant with in situ spores from the Barrandian area, Czech Republic, is of the highest importance because it represents extremely ancient megafossil evidence of land plant diploid generation: sporophytes (~432 Ma). The robust size of this plant places it among the largest known early polysporangiate land plants and it is probable that it attained adequate size for both aeration and effective photosynthetic competence. This would mean not only that sporophytes were photosynthetically autonomous but also that the they might have been able to sustain a relatively gametophyte-independent existence.

Department of Experimental Plant Biology Faculty of Science Charles University Prague Czech Republic

Department of Palaeontology National Museum Prague Prague Czech Republic

Institute of Geology v v i Academy of Sciences of the Czech Republic Prague Czech Republic

References provided by Crossref.org

Silurian Climatic Zonation of Cryptospore, Trilete Spore and Plant Megafossils, with Emphasis on the Přídolí Epoch

Spore Evidence for the Origin of Isoetalean Lycopsids?

Dynamics of Silurian Plants as Response to Climate Changes