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The study aimed to gauge the influence of freshwater inflows on a restored intertidal oyster reef in the Yangtze River estuary by examining spatial and temporal changes in reef area, oyster densities, and resident macrofaunal communities from 2011 to 2021. Regression analysis indicated that freshwater inflows exceeding 56000 m/s resulted in hyposaline conditions (salinity <1) at the upstream reef. The reef's upstream boundary moved downstream during the study period. The reef area declined from 260 ha in 2011 to 170 ha in 2021, representing a net loss of 35 %. The restored reef experienced more than 30 % decrease in oyster densities and a 40 % decline in resident macrofauna densities. The pattern of loss and decrease was non-random and concentrated on the upstream section. Multivariate analysis revealed significant changes and increased relative dispersion in resident macrofaunal communities from 2011 to 2021, driven by the greater dominances of soft-habitat species, and decreased densities of mollusks and annelids in 2021 relative to 2011. The increased multivariate variations indicated that resident communities faced significant environmental stress from high freshwater inflows. This study concluded that freshwater input was the primary driver of declines in reef area, oyster densities, and macrofaunal abundances at the restored oyster reef. Predicted increases in precipitation in Yangtze River basin due to climate changes are expected to further lower salinities in the estuary, leading to the transitions of intermediate salinities to hyposaline condition that negatively impacts oyster survival, potentially disrupting oyster meta-population and impeding oyster restoration efforts.
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http://dx.doi.org/10.1016/j.marenvres.2025.107172 | DOI Listing |
Environ Monit Assess
September 2025
State Key Laboratory of Lake and Watershed Science for Water Security, Institute of Geography and Limnology, Chinese Academy of Sciences, Beijing East Road 73, Nanjing, 210008, China.
Dissolved carbon is a crucial component of freshwater ecosystems and plays an important role in the Earth's carbon cycle. This paper delivers a groundbreaking exploration of dissolved carbon (DOC and DIC) variations spanning 12 years in a eutrophic lake where nutrient levels are gradually declining to reveal their spatial and temporal distribution patterns and the key drivers behind this variation. Our findings indicate that both DIC and DOC concentrations in Lake Chaohu exhibit a westward spatial gradient, with an overall upward trend in DIC levels from 2012 to 2023, contrasting with a downward trend in DOC.
View Article and Find Full Text PDFYing Yong Sheng Tai Xue Bao
July 2025
State Key Laboratory of Water Resources Engineering and Management, Wuhan University, Wuhan 430072, China.
The Anqing-Wuhu mainstem segment in the middle and lower reaches of the Yangtze River serves as a critical habitat for diverse species, where the ecological quality of floodplain wetlands directly governs the stability of the entire ecosystem. Utilizing 30-meter resolution Landsat satellite imagery from 1994 to 2022, we classified the floodplain wetlands in the Anqing-Wuhu mainstem segment in the middle and lower reaches of the Yangtze River using fractional vegetation coverage (FVC). Through dynamic degree analysis and transition matrices method, we quantified vegetation cover transitions across different FVC tiers and analyzed their spatiotemporal variations.
View Article and Find Full Text PDFCamb Prism Coast Futur
January 2025
Institute for Coastal and Marine Research, Department of Botany, Nelson Mandela University, Gqeberha, South Africa.
Wetlands in hypersaline environments are especially vulnerable to loss and degradation, as increasing coastal urbanization and climate change rapidly exacerbate freshwater supply stressors. Hypersaline wetlands pose unique management challenges that require innovative restoration perspectives and approaches that consider complex local and regional socioecological dynamics. In part, this challenge stems from multiple co-occurring stressors and anthropogenic alterations, including estuary mouth closure and freshwater diversions at the catchment scale.
View Article and Find Full Text PDFSci Rep
August 2025
Environment and Climate Change Canada, National Wildlife Research Centre, Ottawa, ON, Canada.
Rivers are major conduits that connect terrestrial carbon cycling with downstream receiving environments. In large lakes, the utilization of river-transported carbon in biological production remains poorly constrained. Lake Athabasca, the eighth largest lake in Canada, receives inflow from the Athabasca River and a large boreal wetland, the Peace-Athabasca Delta.
View Article and Find Full Text PDFMar Pollut Bull
August 2025
Centre for Marine Living Resources and Ecology, Ministry of Earth Sciences, Kochi 682508, India.
Coastal ocean acidification is a growing global concern, especially in densely populated regions where terrestrial inputs complicate its dynamics. Unlike the open ocean, coastal waters are heavily influenced by freshwater inflows. This study investigates the impact of riverine and groundwater inputs on seawater pH variability in the coastal Arabian Sea.
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