Water chemistry of the Chascomus Pond (Province of Buenos Aires, Argen
tina) was studied during a year characterized by low precipitation. Su
persaturation of calcium carbonate up to a calcite saturation index of
about 20 in spring and summer was observed, together with a diminutio
n of the concentration of dissolved organic matter, in particular humi
c substances (HS). These results suggested an adsorption between organ
ic matter and calcium carbonate which should influence the growth of c
alcium carbonate crystals. A preferential removal of higher molecular
weight HS was observed by gel permeation chromatography experiments.