“…Organic matter, used as a tracer of fast circulation in karstic systems, associated with chemical components like Mg 2+ , NO 3 -and �iO 2 -concentrations, enables to understand the hydrogeological functioning of the aquifers (Emblanch, 1997;Emblanch et al, 1998aEmblanch et al, , 1998bBatiot et al, 2002;Batiot et al, 2003). TOC mean annual variation ranged from 0.93 mg/l for the B-point to 2,15 mg/l for the GA�-point, in unsaturated zone, and the mean calculated standard deviations vary from 0.19 for the A-point to 0.63 for the GA�-point.…”