Abstract

The release of inorganic nutrients by nekton (fish and shrimp) assemblages through excretion and bioturbation was quantified for intertidal creeks in a warm-temperate estuary, North Inlet, South Carolina, USA. Excretion rates for individual nekton taxa were determined for captive animals maintained in the field. Nutrient production by nekton assemblages was determined in laboratory tank experiments in which the effects of nutrient releases through excretion and bioturbation could be separated. These values and field-measured biomass data were used to calculate and compare nutrient generation rates by nekton to those of other biotic and abiotic sources in intertidal creeks. Mass specific ammonium excretion rates ranged from 5.7–11.9 μmol g dw −1 h −1 in early spring to 8.3–20.7 μmol g dw −1 h −1 in the summer. Orthophosphate excretion rates were distinctly lower and never exceeded 3 μmol g dw −1 h −1. The N/P ratio in the excretory products of the different taxa was generally higher during summer than in early spring. In the summer, experiments on nekton assemblages in tanks indicated that mass specific ammonium production rates based on excretion plus bioturbation were on average 40% higher than rates based on excretion alone. Orthophosphate production was unaffected by bioturbation during both seasons. Nekton, oyster reefs, and benthic remineralization were identified as the major sources for inorganic nutrients. These observations and the fact that consumer driven nutrient cycling through nekton has not been recognized as an important process in coastal ecosystems suggest that additional efforts to quantify the role of large motile animals are needed.

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