“…Most studies on abandoned channels have focused on processes and patterns in the aquatic zone, particularly gradients of hydrological connectivity (Hudson et al, 2012;Phillips, 2013), sedimentation and geomorphological patterns (Bravard, 1982;Gagliano and Howard, 1984;Shields and Abt, 1989;Citterio and Piégay, 2009;Constantine et al, 2010;Delhomme et al, 2013;Dieras et al, 2013), impacts of nutrient load and hydrogeological fluxes (Bornette et al, 2001), and diversity of aquatic vegetation and animal communities (Amoros and Bornette, 2002;Obolewski, 2011;Besacier-Monbertrand et al, 2012;Meyer et al, 2013;Toth et al, 2013). However, the larger floodplain environment that develops as abandoned channels fill has received much less attention, in particular the composition, biodiversity and temporal changes of the terrestrial plant community and its distribution along hydrogeomorphic gradients (but see Shankman, 1993;Holland et al, 2000).…”