Evolution of a Dystrophic Crisis in a Non-Tidal Lagoon Through Microphyte Blooms

In July–August 2024, a severe dystrophic process occurred in the Orbetello lagoon (Italy). This study reports the following: (1) the macroalgal biomass and the sediment labile organic matter (LOM) between 2018 and 2024; (2) the water temperature and dissolved oxygen values between June and September 2024 and the T-mean, T-max, and T-min in July and August between 2013 and 2024; (3) the list of microphyte taxa that occurred during the dystrophy; (4) satellite images documenting the evolution of the dystrophic process. The results suggest that the dystrophy was caused by the decay of a large macroalgal mass and high accumulations of LOM in the sediment, which triggered anaerobic processes, particularly intense sulphate-reductive activity. This virulent process was facilitated by a record increase in temperatures (with T-min and T-max higher than those of the previous years), in a context of poor hydrodynamics, typical of non-tidal lagoons. Microphyte blooms, which occurred during the dystrophy, were at the basis of the evolution of the phenomenon, allowing for the most critical phase to be overcome through intense oxygen production. Microphytic blooms, with intense water colouring, although constituting an evident sign of a eutrophic/hypertrophic state of the lagoon, could lead to a rapid evolution of the dystrophy and mitigate the environmental conditions.