“…In general, lower nutrient uptake capacity in agricultural streams than in less impacted/pristine streams can be attributed to (a) saturation of the biological community (Bernot et al, ); (b) reduced hydrological complexity of the channel (Argerich, Martí, Sabater, Haggerty, & Ribot, ; Sheibley et al, ); (c) loss of riparian vegetation (Weigelhofer, ); (d) restricted hyporheic water exchange with the sediments (Macrae, English, Schiff, & Stone, ); and (e) reduced adsorption capacities of the sediments (Stutter & Lumsdon, ). A rapid development of agriculture has been occurring in South America in recent decades (Ceddia, Sedlacek, Bardsley, & Gomez‐y‐Paloma, ; Garrett et al, ), and specific climate/hydrological features make this region more vulnerable to the detrimental effects of croplands (Taniwaki et al, ). As our study suggested that agricultural streams are generally less nutrient retentive, progressive agricultural intensification or expansion is expected to increase the role of streams in watershed nutrient export.…”