Research news on Eutrophication

Eutrophication is a biological process in aquatic ecosystems driven by excess input of bioavailable nutrients, primarily nitrogen and phosphorus, that stimulates rapid primary production, especially phytoplankton and cyanobacterial blooms. The resulting high biomass alters food-web structure and increases particulate organic matter sedimentation, enhancing microbial respiration in bottom waters and sediments. This elevated oxygen demand often exceeds resupply via mixing and diffusion, leading to hypoxia or anoxia and associated shifts in community composition, loss of aerobic organisms, and promotion of anaerobic microbial pathways. Eutrophication thereby modifies biogeochemical cycling, including nitrogen and phosphorus regeneration, trace gas production, and redox dynamics across water column and sediment interfaces.

Green seaweed replaces seagrass, but slugs pose new threats

Seagrasses are critical to coastal ecosystems—offering habitat, stabilizing the seafloor and buffering wave energy—but globally they're increasingly under threat. Beginning in 2011, a series of intense algal blooms—fueled ...

Why not every saltwater inflow benefits the Baltic Sea equally

Eutrophication and oxygen depletion are well-known threats to the ecological balance of the Baltic Sea, which is increasingly under pressure due to climate change. In this context, large saltwater inflows from the North Sea ...