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Effects of CO2 enrichment on benthic primary production and inorganic nitrogen fluxes in two coastal sediments.


ABSTRACT: Ocean acidification may alter the cycling of nitrogen in coastal sediment and so the sediment-seawater nitrogen flux, an important driver of pelagic productivity. To investigate how this perturbation affects the fluxes of NOX- (nitrite/nitrate), NH4+ and O2, we incubated estuarine sand and subtidal silt in recirculating seawater with a CO2-adjusted pH of 8.1 and 7.9. During a 41-day incubation, the seawater kept at pH 8.1 lost 97% of its NOX- content but the seawater kept at pH 7.9 lost only 18%. Excess CO2 increased benthic photosynthesis. In the silt, this was accompanied by a reversal of the initial NOX- efflux into influx. The estuarine sand sustained its initial NOX- influx but, by the end of the incubation, released more NH4+ at pH 7.9 than at pH 8.1. We hypothesise that these effects share a common cause; excess CO2 increased the growth of benthic microalgae and so nutrient competition with ammonia oxidising bacteria (AOB). In the silt, diatoms likely outcompeted AOB for NH4+ and photosynthesis increased the dark/light fluctuations in the pore water oxygenation inhibiting nitrification and coupled nitrification/denitrification. If this is correct, then excess CO2 may lead to retention of inorganic nitrogen adding to the pressures of increasing coastal eutrophication.

SUBMITTER: Vopel K 

PROVIDER: S-EPMC5773597 | biostudies-literature | 2018 Jan

REPOSITORIES: biostudies-literature

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Effects of CO<sub>2</sub> enrichment on benthic primary production and inorganic nitrogen fluxes in two coastal sediments.

Vopel Kay K   Del-Río Cintya C   Pilditch Conrad A CA  

Scientific reports 20180118 1


Ocean acidification may alter the cycling of nitrogen in coastal sediment and so the sediment-seawater nitrogen flux, an important driver of pelagic productivity. To investigate how this perturbation affects the fluxes of NO<sub>X</sub><sup>-</sup> (nitrite/nitrate), NH<sub>4</sub><sup>+</sup> and O<sub>2</sub>, we incubated estuarine sand and subtidal silt in recirculating seawater with a CO<sub>2</sub>-adjusted pH of 8.1 and 7.9. During a 41-day incubation, the seawater kept at pH 8.1 lost 97%  ...[more]

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