Los ríos de llanura tienen como característica particular presentar una interrelación con su valle de inundación y con los ambientes lénticos asociados a él (Amoros & Bornette, 2002; Vázquez et al., 2008). durante las inundaciones grandes, cantidades de sedimento son desplazados por los ríos y en esos sedimentos existe una gran variedad de estadios de resistencia. Pequeñas inun
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