“…At OE area, a deeper and wider main channel near one the main RF lagoon inlets (Jacob and Cravo, 2019), high tidal exchange rate promotes rapid advection, mixing, dispersion, and dilution of WWTPs effluents and related constituents, explaining the relative improvement in water quality, in respect with FNW area, and the absence of along transect variability. High exchange of lagoon water and adjacent coastal seawater dilutes and horizontally exports bacterial indicators of faecal contamination (Martins et al, 2006;Cravo et al, 2015;Veríssimo et al, 2019), nutrients (ammonium, phosphate; Newton et al, 2003;Newton and Mudge, 2005;Falcão and Vale, 2003;Cravo et al, 2015), and phytoplankton biomass into the coastal area (Barbosa, 2006(Barbosa, , 2010Cravo et al, 2019;Rosa et al, 2019), being generally responsible for the reduced susceptibility of the RF lagoon to eutrophication (Tett et al, 2003;Newton and Mudge, 2005;Mudge et al, 2008;Domingues et al, 2015Domingues et al, , 2017aDomingues et al, , 2017b.…”