RESUMEN
This paper documents the changes that followed large nutrient (N and P) and organic matter input reductions to a major metropolitan marine bay, Boston Harbor (USA). Before input reduction, its N and P inputs fell in the upper range of the < 1-> 300 gN m-2 year-1 and < 0.1-> 40 gP m-2 year-1 for coastal systems. Elevated nutrient and organic matter inputs are recognized causes of coastal eutrophication. Treatment upgrades and then diversion of its wastewater discharges offshore, lowered its N, P, and organic C inputs by 80-90%. The input decreases lowered its trophic status from hypereutrophic to eutrophic-mesotrophic. With the reversal of hypereutrophication, pelagic production and phytoplankton biomass decreased, and the nitrogen limitation relative to phosphorus limitation increased. Benthic metabolism and dissolved inorganic N fluxes decreased, and benthic-pelagic coupling was altered. Bottom-water dissolved oxygen, already at healthy levels, increased, and seagrass expanded. Coastal management requires that the changes, following the nutrient and organic matter input reductions implemented to address eutrophication, be understood. Boston Harbor's recovery, because its water column was vertically well mixed and marine, was more pronounced than in many other systems.
Asunto(s)
Eutrofización , Aguas Residuales , Boston , Monitoreo del Ambiente , Nitrógeno , Fósforo , FitoplanctonRESUMEN
Since 2011, tropical beaches from Africa to Brazil, Central America, and the Caribbean have been inundated by tons of sargassum seaweed from a new equatorial source of pelagic sargassum in the Atlantic. In recent years the extraordinary accumulations of sargassum make this a nuisance algal bloom for tropical coasts. In 2018 satellite data indicated floating mats of sargassum that extended throughout the Caribbean to the northeast coast of Brazil with the highest percent coverage over the water yet recorded. A literature review suggests that Atlantic equatorial recirculation of seaweed mats combined with nutrients from several possible sources may be stimulating the growth and accumulations of sargassum. In the western equatorial recirculation area, new nutrient sources may include Amazon River floods and hurricanes; in the eastern equatorial recirculation area, nutrient sources that could sustain the sargassum blooms include coastal upwelling and Congo River freshwater and nutrients.
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Sargassum/crecimiento & desarrollo , África , Playas , Región del Caribe , Tormentas Ciclónicas , Eutrofización , Sargassum/fisiología , Algas Marinas/crecimiento & desarrollo , Algas Marinas/fisiologíaRESUMEN
The present state of knowledge regarding the input of anthropogenic pollutants into Narragansett Bay, Rhode Island was reviewed and benthic infaunal communities present at four depositional environments within the upper Bay were characterized. Inter-station differences in species composition and abundance of these assemblages were examined in relation to established pollution gradients. Using diversity curves and multivariate statistics, evidence of significant anthropogenic impact on the structure of benthic macrofaunal communities in Narragansett Bay was identified. The magnitude of this impact was greatest at stations closest to the Bay's urban centers, where exposure to multiple stressors had resulted in communities of opportunistic taxa which persisted in a state of low faunal diversity characteristic of early stages of species succession. As was expected based on historic models of faunal succession; the apparent maturity of benthic assemblages in Narragansett Bay increased along the north-south gradient of decreasing anthropogenic stress.
Asunto(s)
Monitoreo del Ambiente , Actividades Humanas , Invertebrados/fisiología , Animales , Ecosistema , Océanos y Mares , Rhode IslandRESUMEN
A mussel bed dominated by Mytilus edulis contained large concentrations of living consumer biomass, with over 14 kg dry weight/m2 distributed among eleven species. An additional 14.4 kg dry weight/m2 was present as empty shell fragments that contributed to community structure. Field measurements of community respiration for this dense animal system showed a roughly hyperbolic response to increasing current speed. In still water, oxygen uptake was 0.2g O2/m2/hr while in currents over 0.1 m/sec it quickly rose to about 2.7 g O2/m2/hr.