“…In addition, we found an increase in the diversity, abundance, and richness from the main river to the lake, and this result was in accordance with other studies of large rivers, showing an increase in complexity from the main channel to the floodplain waterbodies (Tockner et al, 1998;Garcia and Laville, 2001;Amoros and Bornette, 2002;Arscott et al, 2005;Ezcurra de Drago et al, 2007;Reese and Batzer, 2007;Gallardo et al, 2008;Behrend et al, 2009). Lower species diversity, richness, and density near the bank of the main channel may be explained by low organic matter content and granulometry of the sediments, and by high current velocity that excludes lentic organisms as these are not adapted to maintain their position to prevent accidental loss under high current velocity (Bogatov et al, 1995;Dudgeon, 1995;Takeda et al, 2001;Ezcurra de Drago et al, 2004, 2007.…”