“…Excess nutrient input aggravates the degree of eutrophication in estuaries and offshore waters, coupled with global warming, and leads to an increase in the occurrence and intensity of hypoxic conditions (Breitburg et al, 2018). Since 1950, more than 500 coastal systems of hypoxia have been identified, with a total area of more than 245,000 km 2 (Diaz and Rosenberg, 2008;Breitburg et al, 2018), including the Gulf of Mexico (Del Giudice et al, 2019), Chesapeake Bay (Da et al, 2018), Lower St. Lawrence Estuary (Lefort et al, 2012), and the Yangtze River Estuary (Tian et al, 2021). The lack of oxygen in the sea area has gradually developed into a major global ecological and environmental problem.…”