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Nitrogen removal in marine environments: recent findings and future research challenges

Hulth, Stefan, 1965 (författare)
Gothenburg University,Göteborgs universitet,Institutionen för kemi,Department of Chemistry,University of Gothenburg
Aller, R. C (författare)
Canfield, D. E (författare)
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Dalsgaard, T (författare)
Engström, Pia, 1970 (författare)
Gothenburg University,Göteborgs universitet,Institutionen för kemi,Department of Chemistry,University of Gothenburg
Gilbert, F. (författare)
Sundbäck, Kristina, 1949 (författare)
Gothenburg University,Göteborgs universitet,Institutionen för marin ekologi,Department of Marine Ecology,University of Gothenburg
Thamdrup, B (författare)
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 (creator_code:org_t)
Elsevier BV, 2005
2005
Engelska.
Ingår i: Marine Chemistry. - : Elsevier BV. - 0304-4203. ; 94:1-4, s. 125-145
  • Tidskriftsartikel (refereegranskat)
Abstract Ämnesord
Stäng  
  • Respiratory reduction of nitrate (denitrification) is recognized as the most important process converting biologically available (fixed) nitrogen to N-2. In current N cycle models, a major proportion of global marine denitrification (50-70%) is assumed to take place on the sea floor, particularly in organic rich continental margin sediments. Recent observations indicate that present conceptual views of denitrification and pathways of nitrate reduction and N, formation are incomplete. Alternative N cycle pathways, particularly in sediments. include anaerobic ammonium oxidation to nitrite, nitrate and N-2 by Mn-oxides, and anaerobic ammonium oxidation coupled to nitrite reduction and subsequent N, mobilization. The discovery of new links and feedback mechanisms between the redox cycles of, e.g., C, N, S, Mn and Fe casts doubt on the present general understanding of the global N cycle. Recent models of the oceanic N budget indicate that total inputs are significantly smaller than estimated fixed N removal. The occurrence of alternative N reaction pathways further exacerbates the apparent imbalance as they introduce additional routes of N removal. In this contribution, we give a brief historical background of the conceptual understanding of N cycling in marine ecosystems, emphasizing pathways of aerobic and anaerobic N mineralization in marine sediments, and the implications of recently recognized metabolic pathways for N removal in marine environments. (c) 2004 Elsevier B.V. All rights reserved.

Ämnesord

NATURVETENSKAP  -- Biologi -- Ekologi (hsv//swe)
NATURAL SCIENCES  -- Biological Sciences -- Ecology (hsv//eng)
NATURVETENSKAP  -- Kemi (hsv//swe)
NATURAL SCIENCES  -- Chemical Sciences (hsv//eng)

Nyckelord

nitrogen
removal
marine
ANAEROBIC AMMONIUM OXIDATION
EARTHS EARLY ATMOSPHERE
ORGANIC-MATTER
MINERALIZATION
PROTEROZOIC OCEAN CHEMISTRY
EARLY DIAGENETIC
PROCESSES
NITRATE-REDUCING BACTERIA
OXIC-ANOXIC INTERFACE
BIOGEOCHEMICAL CYCLES
ESTUARINE SEDIMENT
FERROUS IRON
FERROUS IRON

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