Cryogenian glacial habitats as a plant terrestrialization cradle – the origin of Anydrophyta and Zygnematophyceae split Jakub Žárský1*, Vojtěch Žárský2,3, Martin Hanáček4,5, Viktor Žárský6,7 1CryoEco research group, Department of Ecology, Faculty of Science, Charles University, Praha, Czechia 2Department of Botany, University of British Columbia, 3529-6270 University Boulevard, Vancouver, BC, V6T 1Z4, Canada 3Department of Parasitology, Faculty of Science, Charles University, BIOCEV, Průmyslová 595, 25242 Vestec, Czechia 4Polar-Geo-Lab, Department of Geography, Faculty of Science, Masaryk University, Kotlářská 267/2, 611 37 Brno, Czechia 5Regional Museum in Jeseník, Zámecké náměstí 1, 790 01 Jeseník, Czechia 6Laboratory of Cell Biology, Institute of Experimental Botany of the Czech Academy of Sciences, Prague, Czechia 7Department of Experimental Plant Biology, Faculty of Science, Charles University, Prague, Czechia * Correspondence:
[email protected] Keywords: Plant evolution, Cryogenian glaciation, Streptophyta, Charophyta, Anydrophyta, Zygnematophyceae, Embryophyta, Snowball Earth. Abstract For tens of millions of years (Ma) the terrestrial habitats of Snowball Earth during the Cryogenian period (between 720 to 635 Ma before present - Neoproterozoic Era) were possibly dominated by global snow and ice cover up to the equatorial sublimative desert. The most recent time-calibrated phylogenies calibrated not only on plants, but on a comprehensive set of eukaryotes, indicate within the Streptophyta, multicellular Charophyceae evolved