Human activities caused hypoxia expansion in a large eutrophic estuary: non-negligible role of riverine suspended sediments

作者：Yue Nan, Zheng Chen, Bin Wang, Bo Liang, Jiatang Hu · 发表于：Biogeosciences · 年份：2025 · DOI：10.5194/bg-22-5573-2025 · 被引用次数：4 · 研究领域：Marine and coastal ecosystems、Marine Biology and Ecology Research、Oceanographic and Atmospheric Processes

Abstract. An increase in riverine nutrient loads has generally been recognized as the primary cause of coastal deoxygenation, whereas the role of other riverine factors, especially suspended sediments, has received less attention. This study aims to discern the impacts of anthropogenic alterations in various riverine inputs on the subsurface deoxygenation over the past three decades in a large river-dominated estuary, the Pearl River estuary (PRE). Using a physical–biogeochemical model, we reproduced the observed dissolved oxygen (DO) conditions off the PRE in the historical period (the 1990s, with a high suspended sediment concentration (SSC), high DO, and low nutrients) and the present period (the 2010s, with low SSC, low DO, and high nutrients). In the 2010s, the PRE exhibited more extensive and persistent summer hypoxia, with the low-oxygen area (DO<4mgL-1) expanding by ∼148 % (to ∼2926 km2) and the hypoxia area (DO<3mgL-1) increasing by 192 % (to ∼617 km2). Low-oxygen durations extended to 15–35 d, and three distinct hypoxic centers formed under different controlling factors. Single-factor experiments suggested that the decreased riverine DO content (46 %) alone expanded low-oxygen areas in the upper estuarine regions by 44 %, the decreased SSC (by 60 %) alone caused a 47 % expansion in the lower reaches of the PRE, and the increased nutrients alone (100 % in dissolved inorganic nitrogen and 225 % in phosphate) drove a 31 % expansion. In comparison, the combined nu...