The ecohydrological consequences of dam sediment flushing remain poorly understood, particularly in lowland rivers and coastal systems. This study investigates the long-term impacts of uncontrolled flushing operations from the Manjil Dam on the downstream Sefidrud River and the ecologically sensitive Kiashahr and Zibakenar lagoons along the southern Caspian Sea. Using hydrochemical analyses, sediment core data, and satellite-derived indices of turbidity and eutrophication, we demonstrate that sediment flushing significantly altered riverine and lagoonal processes. Flushing-induced sediment discharge peaked at 8.3 times that of non-flushing days, raising suspended sediment concentrations above ecologically critical thresholds. These pulses led to widespread mass fish mortality and the degradation of benthic communities. Hydrochemical signatures shifted markedly, with elevated total dissolved solids, salinity, and ion concentrations, particularly Na⁺, Cl⁻, driven by evaporite dissolution and sediment remobilization. Remote sensing revealed a strong correlation between riverine turbidity and chlorophyll-a concentrations, evidencing enhanced eutrophication in the lagoons. Sediment core analysis confirmed long-term ecological degradation through the disappearance of charophytes and benthic foraminifera and the formation of azoic layers. Flushing disrupted natural flow regimes, shortened low-flow periods, and altered estuarine morphology. Despite rising Caspian Sea levels, accelerated sedimentation led to a 91 % and 32 % reduction in the area of Kiashahr and Zibakenar lagoons, respectively. A large portion of flushed sediments settled in the riverbed, elevating downstream suspended sediment concentration above upstream levels during non-flushing days, prolonging biotic stress. These findings reveal the lasting ecohydrological impacts of sediment flushing, highlighting its role in degrading the health and biodiversity of the freshwater-to-coastal continuum.
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