“…Recent restoration measures, where external phosphorus (P) input and water turbidity were experimentally reduced, have led to the return of dense charophyte beds (Van den Berg et al, 1998a;Meijer et al, 1999;Ibelings et al, 2007). These restoration measures, however, were performed in sandy lakes, whereas peaty lakes are suffering from high internal loading of P from the sediment and are more prone to sediment resuspension (Cooke et al, 1993;Jeppesen et al, 1998;Søndergaard et al, 2003). Under natural conditions, peaty lakes in the Netherlands would not suffer from internal P loading, as upwelling iron rich groundwater binds to phosphorus (in the form of phosphate, PO 4 ) in the sediment.…”