“…At the time, these inputs represented 3.3 Â 10 9 m 3 y À1 of freshwater (3.7 times the lagoon volume) and 520,000 t y À1 of silt. Due to no or very few controls for a long time, the release of freshwater and silt in the lagoon led to modifications of the morphology (i.e., topography of the bottom, quality and size of sediments), the hydrodynamic and the ecological functioning of the entire lagoon, causing intense eutrophication (Minas, 1974(Minas, , 1976bArfi, 1989Arfi, , 1991Caddy, 2000;Gouze et al, 2008), leading to significant anoxia events (Minas, 1974(Minas, , 1976aNerini et al, 2000).…”