Coastal sediments maintain potential for N 2 O cycling under seasonally varying redox conditions

Coastal eutrophication can lead to deoxygenation and sulfide accumulation in sediments, which could strongly impact the dynamics of the potent greenhouse gas nitrous oxide (N 2 O). Here, we investigated the effects of oxygen (O 2 ) and sulfide on microbial N 2 O production and consumption in surface sediments of a seasonally euxinic (anoxic and sulfidic) coastal basin. In spring, these surface sediments are oxygenated, while they are highly sulfidic during stratification of the water column in summer. During oxygenated spring conditions, rapid depletion of the substrates O 2 and nitrate (NO 3 - ) in the surface sediment limited net in situ N 2 O production, despite potential for nitrification and for N 2 O production through incomplete denitrification as observed in batch incubations. Based on metagenome and metatranscriptome analyses the N 2 O-consuming microbial community was shown to be highly diverse and dominated by clade II nosZ -possessing Flavobacteriia . Assessing the summer sulfidic conditions in surface sediments via batch incubations, we found that moderate sulfide concentrations (0.2–1 mM) enhanced N 2 O consumption, whereas high concentrations (4 mM) inhibited all steps of denitrification. These findings highlight the redox controls on N 2 O dynamics, by indicating that coastal sediments can maintain significant N 2 O turnover potential despite substrate limitations and elevated sulfide concentrations. Consequently, ecosystem restoration strategies that alter O 2 , NO 3 - and sulfide availability may fundamentally impact coastal N 2 O budgets.