“…mariscus occurrence in Central Europe has decreased in recent centuries due to human activity (drainage), the oligotrophication of habitats and the lack of access to carbonate sediments (Salmina, 2004;Gałka and Tobolski, 2012). Presently C. mariscus is still occurs mainly around outflow depressions, where there is good supply of carbonate ions from the dissolution of the carbonate bedrock (Buczek, 2005), or around lakes as an emerged plant (Namura-Ochalska, 2005;Karcz, 2008;Gałka and Tobolski, 2012) where Ca 2+ ions are supplied from dissolution of carbonates in glacial sediments.…”