An Experimental Study of Calcium Acquisition and its Effects on the Calcifuge Moss Pleurozium schreberi

In a field experiment to investigate the sources and effectson growth of Ca in the calcifuge moss Pleurozium schreberi,significant quantities of Ca reached the growing shoot apicesfrom a CaCO₃ layer placed on the mineral soil surface Top applicationsof 0.5 and 5 mol m^–3 CaCl₂ raised the exchangeable andintracellular Ca concentrations and displaced natural exchangeableK and Mg The 5 mol m^–3 CaCl₂ treatment also caused a significantreduction in intracellular Mg indicating that Mg uptake is dependenton an initial exchange step No growth differences were notedbetween treatments, possibly because ionic changes had not reacheda detrimental level within the 28 weeks of the experiment ina second experiment, shoot apices of Pleurozium schreberi, Pseudoscleropodiumpurum and Calliergon cuspidatum were grown on nylon gauze underintermittent distilled-water mist At weekly intervals the shootswere saturated with CaCl₂ solutions providing factorial combinationsof Ca and pH Growth of C cuspidatum and P purum from chalk soilwas reduced at high (0.01) Ca concentration whereas Pleuroziumschreberi and Pseudoscleropodium purum from acidic clay wereunaffected The pH treatments did not significantly affect mossgrowth Initial tissue levels of K and Mg were lower in the mossesfrom chalk and it is suggested that the CaCl₂ treatments causednutrient deficiencies in these plants Mosses from acidic soilcontained less exchangeable Ca than the chalk plants and grewpoorly in the absence of CaCl₂, perhaps due to the developmentof Ca deficiency Bryophyte growth, calcium uptake, pH, mineral nutrition, Pleurozium schreberi, Pseudoscleropodium purum, Calliergon cuspidatum