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Experimental recolonisation of Baltic Sea reduced sediments: survival of benthic macrofauna and effects on nutrient cycling

Karlson, Karin, 1961 (författare)
Gothenburg University,Göteborgs universitet,Institutionen för marin ekologi,Department of Marine Ecology
Hulth, Stefan, 1965 (författare)
Gothenburg University,Göteborgs universitet,Institutionen för kemi,Department of Chemistry
Ringdahl, Katja (författare)
Gothenburg University,Göteborgs universitet,Institutionen för marin ekologi,Department of Marine Ecology
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Rosenberg, Rutger, 1943 (författare)
Gothenburg University,Göteborgs universitet,Institutionen för marin ekologi,Department of Marine Ecology
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 (creator_code:org_t)
Inter-Research Science Center, 2005
2005
Engelska.
Ingår i: Marine Ecology-Progress Series. - : Inter-Research Science Center. - 0171-8630 .- 1616-1599. ; 294, s. 35-49
  • Tidskriftsartikel (refereegranskat)
Abstract Ämnesord
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  • A recolonisation experiment was performed in vitro on highly reduced laminated Baltic Sea sediments initially devoid of larger benthic fauna. The survival capacity of 3 common benthic species Monoporeia affinis, Macoma balthica and Marenzelleria viridis was investigated along with overall effects of bioturbation and bioirrigation on benthic reaction and transport processes. Benthic fluxes of oxygen and nutrients, sediment denitrification and nutrients in the porewater were measured. Survival of M. affinis increased with time and sediment reworking, while no such feedback was observed for M balthica and M. viridis, Macrofaunal irrigation and bioturbating activities significantly enhanced solute fluxes in the manipulated cores compared to the control. Mass balance calculations indicated that net N-mineralisation in the manipulated cores was stimulated by 1 to 2 orders of magnitude compared to the control. Despite relatively high nitrate fluxes from the overlying water to the sediment (similar to 1 mmol m(-2) d(-1)), measured rates Of total denitrification were in general low (20 to 45 mu mol N-2 m(-2) d(-1)) in all cores. Denitrification, using nitrate supplied from the overlying water (D-w), was similar to coupled nitrification/denitrification (D-n), although D-w was significantly higher than D-n in the M. affinis cores. In conjunction with high nitrate fluxes into the sediment and high ammonium fluxes to the overlying water, the generally low denitrification rates indicated dissimilatory nitrate reduction to ammonium (DNRA) as the main pathway for nitrate removal. Thus, the main source of bottom water ammonium was overlying water nitrate, rather than ammonium produced in surface sediments during mineralisation of organic N.

Ämnesord

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

Nyckelord

recolonisation
bioturbation
macrofauna
Baltic sea
reduced
sediments
benthic fluxes
denitrification
mineralisation
AMPHIPOD MONOPOREIA-AFFINIS
MACOMA-BALTHICA BIVALVIA
COASTAL MARINE
SEDIMENT
PONTOPOREIA-AFFINIS
ORGANIC-MATTER
ESTUARINE SEDIMENTS
LAMINATED SEDIMENTS
POREWATER PROFILES
HYDROGEN-SULFIDE
REACTION-RATES

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Karlson, Karin, ...
Hulth, Stefan, 1 ...
Ringdahl, Katja
Rosenberg, Rutge ...
Om ämnet
NATURVETENSKAP
NATURVETENSKAP
och Biologi
och Ekologi
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Marine Ecology-P ...
Av lärosätet
Göteborgs universitet

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