Abstract
Benthic nutrient and oxygen fluxes were measured during summer in the nearshore zone of the Georgia Bight, USA. Ammonium nitrite, nitrate and phosphate were released by the sediments to the overlying water, while dissolved organic nitrogen was taken up by sediments. Oxygen uptake was equivalent to 1.1 g Cm-2 d-1. Based on other data available for this area the benthos accounted for the remineralization of approximately 55% of net primary production adn 25% of total community (benthic and pelagic) metabolism. To balance a simple carbon budget for the nearshore region during summer an outside source of organic matter, most likely originating in adjacent estuaries, is required. The benthos supplied 16% of the N adn 52% of the P required by phytoplankton. Pore water nutrient concentrations suggested substantial denitrification (estimated at 4.9mg Nm-2 d by mass balance) in sediments which may have caused lthe ow N:P benthic release ratios we observed. The results support the hypothesis that benthic processes in shallow marine areas control the availability of N and P for water column production.
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CITATION STYLE
Hopkinson, C., & Wetzel, R. (1982). In situ Measurements of Nutrient and Oxygen Fluxes in a Coastal Marine Benthic Community. Marine Ecology Progress Series, 10, 29–35. https://doi.org/10.3354/meps010029
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