“…The inflow was low, water retention time was long, and the backwater from the Yangtze River severely disrupted the thermal stratification and there was rapid mixing of water bodies in the Daning River. These conditions led to the decline of group Lo in the midstream, because this group is sensitive to prolonged or deep mixing (Huszar et al, 2003;Reynolds et al, 2002). Meanwhile, groups C and B increased in the midstream and estuary.…”