Inland freshwater ecosystems—comprising rivers, lakes, and reservoirs—are critical reservoirs of biodiversity and essential sources of freshwater resources for human use. However, these ecosystems are facing an alarming threat from deoxygenation, a process characterized by declining levels of dissolved oxygen (DO) in surface and subsurface waters. Dissolved oxygen serves as a fundamental driver of aquatic life, facilitating aerobic respiration for myriad organisms and sustaining complex biogeochemical cycling. The rapid depletion of DO in freshwater systems threatens not only the ecological health of these habitats but also the socioeconomic stability of communities that depend on them for drinking water, fisheries, and recreation.
Recent studies reveal a stark global trend: surface water dissolved oxygen in inland freshwater bodies is declining at unprecedented rates. Over the last two decades, lakes have recorded an average DO decrease of approximately 0.034 mg per liter per decade during summer months, while rivers have exhibited a more pronounced year-round decline of 0.043 mg per liter per decade dating back to the early 1980s. These patterns are not uniform, with spatial variability linked to geographic and climatic heterogeneity. Notably, the most dramatic decreases have occurred in Asian lakes, where DO has dropped by 0.043 mg per liter per decade, and in the Amazon River Basin, where declines reach as much as 0.2 mg per liter per decade, a figure that signals profound disruption in one of the planet’s most vital freshwater systems.
The drivers behind this widespread deoxygenation are multifaceted, intricately interwoven with both natural processes and human influences. Climate warming emerges as a dominant force amplifying oxygen depletion through several mechanisms. Elevated temperatures exacerbate thermal stratification in lakes and reservoirs, prolonging the summer layering of water masses which prevents oxygen exchange between surface and bottom layers. Moreover, oxygen’s solubility in water inherently decreases as temperature rises, compounding DO shortages. Higher temperatures also stimulate microbial metabolism, escalating the respiration rates that consume available oxygen. In sum, climatic warming both directly and indirectly escalates the vulnerability of freshwater systems to hypoxia and anoxia.
Human activities intensify these natural stressors by accelerating nutrient inputs, primarily nitrogen and phosphorus, through agricultural runoff, sewage discharge, and industrial effluents. This nutrient enrichment leads to eutrophication—a process marked by excessive algal growth and subsequent decay, further depleting oxygen levels once the organic matter decomposes. Extreme rainfall events, which are increasing in frequency and intensity due to climate change, exacerbate this situation by facilitating nutrient transport and promoting the development of hypoxic zones. Globally, this complex interplay of anthropogenic nutrient loading and climate-induced changes is reshaping hydrological and biogeochemical cycles with alarming consequences.
The process of deoxygenation initiates a cascade of biogeochemical feedbacks that accelerate ecosystem deterioration. Oxygen-depleted conditions foster the proliferation of anaerobic microbial communities, altering the cycling of key elements such as nitrogen, sulfur, and carbon. For instance, in low-oxygen environments, increased denitrification and sulfate reduction processes release potent greenhouse gases like nitrous oxide and hydrogen sulfide, contributing to climate warming and further degrading water quality. These feedback loops not only diminish biodiversity through selective pressures on aerobic organisms but also impede ecosystem resilience by modifying essential nutrient fluxes.
Biological communities within freshwater habitats are profoundly restructured as DO levels decline. Aerobic species—ranging from fish and macroinvertebrates to key microbial taxa—often face physiological stress or mortality due to hypoxic conditions, leading to losses in biodiversity and shifts toward more tolerant but less ecologically functional assemblages. These shifts undermine the ecological integrity of freshwater systems, compromising ecosystem functions such as nutrient cycling, primary production, and organic matter decomposition. Consequently, trophic interactions become altered, disrupting food web dynamics and potentially promoting harmful algal blooms and invasive species that further degrade water quality.
In parallel, the socioeconomic dimensions of freshwater deoxygenation are vast and insidious. Diminished oxygen concentrations impair fishery productivity, reducing catch volumes and the livelihoods of millions dependent on inland fisheries worldwide. Deoxygenated waters often exhibit poorer recreational quality due to eutrophication-driven algal blooms and unpleasant odors, impacting tourism and associated economic benefits. Moreover, the quality of drinking water sourced from lakes and rivers can be severely compromised by hypoxia-induced processes, including the release of harmful contaminants and changes in microbial populations. These factors collectively jeopardize public health, food security, and economic stability.
Despite the gravity of freshwater deoxygenation, monitoring efforts remain insufficiently coordinated and under-resourced. Establishing comprehensive, real-time dissolved oxygen monitoring networks is critical for detecting early-stage deoxygenation events and informing rapid management responses. Coupled with these networks, the development of integrated predictive models that incorporate climatic, hydrological, and biogeochemical drivers can improve forecasting accuracy and guide adaptive management strategies. These models must consider complex feedback mechanisms and potential nonlinear responses to environmental changes to ensure reliability.
Mitigation requires a multifaceted approach emphasizing nutrient management through reduction of agricultural runoff, wastewater treatment improvements, and watershed restoration. Restoration efforts that reestablish hydrological connectivity and promote aquatic vegetation can enhance oxygen replenishment and buffer against extreme events. Ecological restoration not only targets oxygen replenishment but also fosters biodiversity recovery and resilience building. Coordinated governance frameworks integrating local stakeholder engagement, scientific expertise, and policy enforceability are vital to ensuring the sustainability of mitigation initiatives.
Furthermore, adaptation strategies must anticipate the compounding threats posed by future climate warming and land-use changes. Increasing community awareness and embedding scientific findings into policy decisions foster better resilience and stewardship at the local to global scales. Collaborative interdisciplinary research—and transboundary cooperation, especially in large, shared freshwater basins—is pivotal for confronting the complexities of freshwater deoxygenation.
In conclusion, the widespread deoxygenation of surface waters in inland freshwater systems represents a critical environmental challenge with far-reaching ecological and socioeconomic impacts. The synergistic effects of climate warming and human activities have set in motion a trajectory of oxygen loss that threatens the viability of aquatic ecosystems globally. Addressing this challenge mandates innovative science-policy interfaces, enhanced monitoring infrastructures, proactive nutrient and watershed management, and inclusive governance models. Only through integrated and adaptive strategies can the integrity and functionality of our planet’s freshwater ecosystems be safeguarded for future generations.
Subject of Research: Deoxygenation trends, drivers, and impacts in inland freshwater ecosystems
Article Title: Deoxygenation in inland freshwater systems
Article References:
Shi, K., Iestyn Woolway, R., Guan, Q. et al. Deoxygenation in inland freshwater systems. Nat Rev Earth Environ (2026). https://doi.org/10.1038/s43017-026-00795-x
Image Credits: AI Generated
