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Aerobic and anaerob...
Aerobic and anaerobic nitrogen transformation processes in N-2-fixing cyanobacterial aggregates
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- Isabell, Klawonn (författare)
- Stockholms universitet,Institutionen för ekologi, miljö och botanik
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- Bonaglia, Stefano (författare)
- Stockholms universitet,Institutionen för geologiska vetenskaper
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- Brüchert, Volker (författare)
- Stockholms universitet,Institutionen för geologiska vetenskaper
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- Ploug, Helle (författare)
- Stockholms universitet,Gothenburg University,Göteborgs universitet,Institutionen för biologi och miljövetenskap,Department of Biological and Environmental Sciences,Institutionen för ekologi, miljö och botanik
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(creator_code:org_t)
- 2015-01-09
- 2015
- Engelska.
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Ingår i: Isme Journal. - : Springer Science and Business Media LLC. - 1751-7362 .- 1751-7370. ; 9:6, s. 1456-1466
- Relaterad länk:
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https://www.nature.c...
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https://gup.ub.gu.se...
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https://doi.org/10.1...
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https://urn.kb.se/re...
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Abstract
Ämnesord
Stäng
- Colonies of N-2-fixing cyanobacteria are key players in supplying new nitrogen to the ocean, but the biological fate of this fixed nitrogen remains poorly constrained. Here, we report on aerobic and anaerobic microbial nitrogen transformation processes that co-occur within millimetre-sized cyanobacterial aggregates (Nodularia spumigena) collected in aerated surface waters in the Baltic Sea. Microelectrode profiles showed steep oxygen gradients inside the aggregates and the potential for nitrous oxide production in the aggregates' anoxic centres. N-15-isotope labelling experiments and nutrient analyses revealed that N-2 fixation, ammonification, nitrification, nitrate reduction to ammonium, denitrification and possibly anaerobic ammonium oxidation (anammox) can co-occur within these consortia. Thus, N. spumigena aggregates are potential sites of nitrogen gain, recycling and loss. Rates of nitrate reduction to ammonium and N-2 were limited by low internal nitrification rates and low concentrations of nitrate in the ambient water. Presumably, patterns of N-transformation processes similar to those observed in this study arise also in other phytoplankton colonies, marine snow and fecal pellets. Anoxic microniches, as a pre-condition for anaerobic nitrogen transformations, may occur within large aggregates (>= 1 mm) even when suspended in fully oxygenated waters, whereas anoxia in small aggregates (<1 to >= 0.1 mm) may only arise in lowoxygenated waters (<= 25 mu M). We propose that the net effect of aggregates on nitrogen loss is negligible in NO3--depleted, fully oxygenated (surface) waters. In NO3--enriched (>1.5 mu M), O-2-depleted water layers, for example, in the chemocline of the Baltic Sea or the oceanic mesopelagic zone, aggregates may promote N-recycling and -loss processes.
Ämnesord
- 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 -- Geovetenskap och miljövetenskap (hsv//swe)
- NATURAL SCIENCES -- Earth and Related Environmental Sciences (hsv//eng)
- NATURVETENSKAP -- Biologi (hsv//swe)
- NATURAL SCIENCES -- Biological Sciences (hsv//eng)
Nyckelord
- OXYGEN MINIMUM ZONES
- CENTRAL BALTIC SEA
- MARINE SNOW
- NODULARIA-SPUMIGENA
- AMMONIUM OXIDATION
- SINKING VELOCITY
- DENITRIFYING
- BACTERIA
- DINITROGEN FIXATION
- NITRATE REDUCTION
- MICROBIAL ECOLOGY
- Ecology
- Microbiology
- Nitrogen cycle /Cyanobacteria/macroaggregates/O2 and N2O microsensors/isotope pairing technique/Oxygen Minimum Zones
- geokemi
- Marine Ecology
Publikations- och innehållstyp
- ref (ämneskategori)
- art (ämneskategori)
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