Abstract
Abstract. Oxygen and nitrate availabilities impact the marine nitrogen cycle at a range of spatial and temporal scales. Here, we demonstrate the impact of
denitrifying foraminifera on the nitrogen cycle at two oxygen and nitrate contrasting stations in a fjord environment (Gullmar Fjord,
Sweden). Denitrification by benthic foraminifera was determined through the combination of specific density counting per microhabitat and specific
nitrate respiration rates obtained through incubation experiments using N2O microsensors. Benthic nitrate removal was calculated from
submillimeter chemical gradients extracted from 2D porewater images of the porewater nitrate concentration. These were acquired by combining the DET
technique (diffusive equilibrium in thin film) with chemical colorimetry and hyperspectral imagery. Sediments with high nitrate concentrations in
the porewater and oxygenated overlying water were dominated by the non-indigenous species (NIS) Nonionella sp. T1. Denitrification by this
species could account for 50 %–100 % of the nitrate loss estimated from the nitrate gradients. In contrast sediments below hypoxic bottom
waters had low inventories of porewater nitrate, and denitrifying foraminifera were rare. Their contribution to benthic nitrate removal was
negligible (< 5 %). Our study showed that benthic foraminifera can be a major contributor to nitrogen mitigation in oxic coastal ecosystems
and should be included in ecological and diagenetic models aiming to understand biogeochemical cycles coupled to nitrogen.
Subject
Earth-Surface Processes,Ecology, Evolution, Behavior and Systematics
Cited by
18 articles.
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