Widespread deoxygenation of freshwater ecosystems regularly reversed by nutrient management

IF 20.6 1区 地球科学 Q1 GEOSCIENCES, MULTIDISCIPLINARY
Yongqiang Zhou, Jinling Wang, Lei Zhou, Yinjun Zhang, Jianming Deng, Wei Zhi, Yunlin Zhang, Boqiang Qin, Fengchang Wu, R. Iestyn Woolway, Stephen F. Jane, Kevin C. Rose, Erik Jeppesen, David P. Hamilton, Marguerite A. Xenopoulos, Peter R. Leavitt
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Abstract

Dissolved oxygen concentrations regulate diverse aquatic ecosystem processes from organismal respiration to biogeochemical cycles, yet concentrations have declined markedly in flowing and standing waters in Europe and North America during recent decades. While atmospheric warming partially explains this deoxygenation, land-use changes such as farming and urbanization have also intensified depletion of dissolved oxygen, which suggests that improved land management could prevent widespread oxygen loss from freshwaters. Here we analysed monthly dissolved oxygen concentration, percent oxygen saturation and coeval environmental variables in 972 river and 354 lake sites in China from January 2005 to December 2022 to assess how extensive restoration efforts to control nutrient pollution correspond with changes in freshwater oxygen levels. Despite surface water warming of +1.2 °C per decade, dissolved oxygen concentration and percent saturation increased markedly in rivers and lakes resulting in a rapid and substantial decrease in the incidence of hypoxia and anoxia. Long-term increases in dissolved oxygen were correlated negatively with biochemical oxygen demand, but not with phytoplankton abundance. We conclude that effective nutrient management at the sub-continental scale can reverse widespread freshwater deoxygenation, thereby improving fisheries, biodiversity and ecosystem health, while reducing the risk of exceeding critical planetary boundaries even in the face of global warming. Dissolved oxygen concentrations increased in rivers and lakes across China between 2005 and 2022 due to nutrient management and despite climate warming-related decreases, according to a study of dissolved oxygen and environmental variables.

Abstract Image

淡水生态系统的广泛脱氧经常被营养物管理逆转
溶解氧浓度调节着从生物呼吸到生物地球化学循环的各种水生生态系统过程,但近几十年来,欧洲和北美流动和静水中的溶解氧浓度显著下降。虽然大气变暖部分解释了这种脱氧,但农业和城市化等土地利用变化也加剧了溶解氧的消耗,这表明改善土地管理可以防止淡水中广泛的氧气损失。在这里,我们分析了2005年1月至2022年12月中国972条河流和354个湖泊站点的每月溶解氧浓度、氧饱和度百分比和同期环境变量,以评估控制营养污染的广泛恢复努力如何与淡水氧水平的变化相对应。尽管地表水每十年变暖+1.2°C,但河流和湖泊的溶解氧浓度和饱和度显著增加,导致缺氧和缺氧发生率迅速大幅下降。溶解氧的长期增加与生化需氧量呈负相关,而与浮游植物丰度不相关。我们得出的结论是,在次大陆尺度上进行有效的营养管理可以逆转广泛的淡水脱氧,从而改善渔业、生物多样性和生态系统健康,同时减少即使在全球变暖的情况下也会超出临界地球边界的风险。
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来源期刊
Nature Geoscience
Nature Geoscience 地学-地球科学综合
CiteScore
26.70
自引率
1.60%
发文量
187
审稿时长
3.3 months
期刊介绍: Nature Geoscience is a monthly interdisciplinary journal that gathers top-tier research spanning Earth Sciences and related fields. The journal covers all geoscience disciplines, including fieldwork, modeling, and theoretical studies. Topics include atmospheric science, biogeochemistry, climate science, geobiology, geochemistry, geoinformatics, remote sensing, geology, geomagnetism, paleomagnetism, geomorphology, geophysics, glaciology, hydrology, limnology, mineralogy, oceanography, paleontology, paleoclimatology, paleoceanography, petrology, planetary science, seismology, space physics, tectonics, and volcanology. Nature Geoscience upholds its commitment to publishing significant, high-quality Earth Sciences research through fair, rapid, and rigorous peer review, overseen by a team of full-time professional editors.
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