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Sökning: onr:"swepub:oai:gup.ub.gu.se/311760" > Enhanced benthic ni...

Enhanced benthic nitrous oxide and ammonium production after natural oxygenation of long-term anoxic sediments

Hylén, Astrid, 1991 (författare)
Gothenburg University,Göteborgs universitet,Institutionen för marina vetenskaper,Department of marine sciences
Bonaglia, Stefano, 1983 (författare)
Stockholms universitet,Gothenburg University,Göteborgs universitet,Institutionen för marina vetenskaper,Department of marine sciences,Institutionen för ekologi, miljö och botanik,University of Gothenburg, Sweden; University of Southern Denmark, Denmark
Robertson, Elizabeth, 1987 (författare)
Gothenburg University,Göteborgs universitet,Institutionen för marina vetenskaper,Department of marine sciences
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Marzocchi, Ugo (författare)
Kononets, Mikhail Y, 1978 (författare)
Gothenburg University,Göteborgs universitet,Institutionen för marina vetenskaper,Department of marine sciences
Hall, Per, 1954 (författare)
Gothenburg University,Göteborgs universitet,Institutionen för marina vetenskaper,Department of marine sciences
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 (creator_code:org_t)
2021-12-29
2022
Engelska.
Ingår i: Limnology and Oceanography. - : Wiley. - 0024-3590 .- 1939-5590. ; 67:2, s. 419-433
  • Tidskriftsartikel (refereegranskat)
Abstract Ämnesord
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  • Coastal and shelf sediments are central in the global nitrogen (N) cycle as important sites for the removal offixed N. However, this ecosystem service can be hampered by ongoing deoxygenation in many coastal areas.Natural reoxygenation could reinstate anoxic sediments as sites wherefixed N is removed efficiently. To investi-gate this further, we studied benthic N cycling in previously long-term anoxic sediments, following a largeintrusion of oxygenated water to the Baltic Sea. During three campaigns in 2016–2018, we measured in situsediment–waterfluxes of ammonium (NHþ4), nitrate (NO3), oxygen (O2), dissolved inorganic carbon, and NO3reduction processes using benthic chamber landers. Sediment microprofiles of O2, nitrous oxide (N2O), andhydrogen sulfide were measured in sediment cores. At a permanently oxic station, denitrification to N2was themain NO3reduction process. Benthic N2O production appeared to be linked to nitrification, although no netN2Ofluxes from the sediment were detected. At newly oxygenated sites, dissimilatory NO3reduction to NHþ4comprised almost half of the total NO3reduction. At these stations, the removal offixed N was inefficient dueto high effluxes of NHþ4. Sedimentary N2O production was associated with incomplete denitrification, account-ing for 41–88% of the total denitrification rate. Microprofiling revealed algae aggregates as potential hotspots ofseafloor N2O production. Our results show that transient oxygenation of euxinic systems initiates benthic NO3reduction, but may not lead to efficient sedimentary removal offixed N. Instead, recycling of N compounds ispromoted, which may accelerate the return to anoxia.

Ämnesord

NATURVETENSKAP  -- Geovetenskap och miljövetenskap -- Annan geovetenskap och miljövetenskap (hsv//swe)
NATURAL SCIENCES  -- Earth and Related Environmental Sciences -- Other Earth and Related Environmental Sciences (hsv//eng)
NATURVETENSKAP  -- Geovetenskap och miljövetenskap -- Geokemi (hsv//swe)
NATURAL SCIENCES  -- Earth and Related Environmental Sciences -- Geochemistry (hsv//eng)
NATURVETENSKAP  -- Geovetenskap och miljövetenskap -- Oceanografi, hydrologi och vattenresurser (hsv//swe)
NATURAL SCIENCES  -- Earth and Related Environmental Sciences -- Oceanography, Hydrology and Water Resources (hsv//eng)
NATURVETENSKAP  -- Biologi (hsv//swe)
NATURAL SCIENCES  -- Biological Sciences (hsv//eng)
NATURVETENSKAP  -- Geovetenskap och miljövetenskap (hsv//swe)
NATURAL SCIENCES  -- Earth and Related Environmental Sciences (hsv//eng)

Nyckelord

Nitrogen Sediment Baltic Sea Denitrification Eutrophication

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