“…A common feature of all of these anthropogenic activities is the modification of terrestrial ecosystems leading to soil erosion and increased flow of fine sediments to the aquatic ecosystems (Sponseller & Benfield, ; Wagenhoff, Townsend, Phillips, & Matthaei, ; Wood, Armitage, Hill, Mathers, & Millett, ). Although fine sediments are a natural and integrant part of streams structure, where biological and chemical processes take place (Boulton, Datry, Kasahara, Mutz, & Stanford, ; Frossard, Gerull, Mutz, & Gessner, ), excessive sediment inputs represent one of the greatest threats to the stream ecosystem integrity (Benoy, Sutherland, Culp, & Brua, ; Bruder, Salis, McHugh, & Matthaei, ; Wood & Armitage, ). Sediment deposition in the stream bottom—which leads to burial, reduction of habitat heterogeneity and limitation of oxygen exchange within interstitial spaces (Kaufmann, Larsen, & Faustini, ; Owens et al, )—and/or transport in suspension, which elevates turbidity (Wood & Armitage, ), have deleterious effects on primary producers (Jones, Duerdoth, Collins, Naden, & Sear, ), heterotrophic microorganisms (Danger, Cornut, Elger, & Chauvet, ), macroinvertebrates (Descloux, Datry, & Usseglio‐Polatera, ), and fishes (Kemp, Sear, Collins, Naden, & Jones, ).…”