“…Fluvially‐integrated wetlands, such as floodplains and valley‐bottoms, support diverse and highly valued regulatory ecosystem services including the attenuation of ‘source‐to‐sink’ dispersal of water, sediment, particulate organic matter and dissolved solutes (Johnston, 1991; Kotze et al, 2009; Phillips, 1989). The relative effectiveness of a given wetland type in mediating these material fluxes has been attributed to the complex interplay between catchment‐scale hydrometeorological, geomorphological, ecological, biological and land‐use conditions (Grenfell et al, 2014; Kotze et al, 2009). There are also linkages between the rates of sediment trapping and local‐scale factors such as hydrogeomorphic setting, sediment supply, wetland morphometry, hydrological regime and surface roughness (Hupp, Woodside, & Yanosky, 1993; Olde Venterink et al, 2006).…”