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Oxygen diffusion limitation and ammonium production within sinking diatom aggregates under hypoxic and anoxic conditions

Ploug, Helle (författare)
Gothenburg University,Göteborgs universitet,Institutionen för biologi och miljövetenskap,Institutionen för marina vetenskaper,Department of Biological and Environmental Sciences,Department of marine sciences
Bergkvist, Johanna, 1980 (författare)
Gothenburg University,Göteborgs universitet,Institutionen för biologi och miljövetenskap,Department of Biological and Environmental Sciences
 (creator_code:org_t)
Elsevier BV, 2015
2015
Engelska.
Ingår i: Marine Chemistry. - : Elsevier BV. - 0304-4203. ; 176, s. 142-149
  • Tidskriftsartikel (refereegranskat)
Abstract Ämnesord
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  • Sinking diatom aggregates are important components of vertical elemental fluxes and represent 'hotspots' of microbial-driven remineralization in the water column. A combined analytical approach of microsensors and fluorometry was used to measure oxygen (02) and ammonium (NH4+) concentrations in sinking diatom aggregates as a function of the ambient 02 concentrations. Diffusive fluxes of 02 and NH4+ within and around sinking aggregates were subsequently analyzed using a diffusion reaction model. Diffusion limitation of 02 within the diatom aggregates occurred when ambient 02 concentrations decreased beneath 100 mu M. At ambient 02 concentrations of 20 mu M, the measured flux of 02 to aggregates was equivalent to 33% of fluxes when 02 concentrations were in equilibrium with the atmosphere and approximately 50% of the aggregate volume was anoxic. When the diatom aggregates were maintained under hypoxic conditions, was produced in a ratio of 8.9 mol O-2 consumed:1 mol NH4+ produced which is within the expected range during ammonification. The average POC-specific respiration rate and the average PON-specific NH4+ production rate under hypoxic conditions were 0.065 d(-1) and 0.052 d(-1), respectively. Under anoxic conditions, the NH4+ release was 18% of that measured under hypoxic conditions. Our empirical and modeled data revealed diatom aggregates to be microenvironments of elevated NI-It concentrations ranging from 1 to 8 mu M and therefore to be potential sources of NH4+ in the oxygen minimum zones in the ocean. (C) 2015 Elsevier B.V. All rights reserved.

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)

Nyckelord

Diatom aggregates
Mass transfer
Microsensors
Fluorometry
Modeling
marine snow
pelagic environment
benthic microalgae
respiration rates
upwelling system
ballast minerals
carbon turnover
organic-matter
surface waters
sea-water
Chemistry
Oceanography

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Ploug, Helle
Bergkvist, Johan ...
Om ämnet
NATURVETENSKAP
NATURVETENSKAP
och Geovetenskap och ...
och Oceanografi hydr ...
Artiklar i publikationen
Marine Chemistry
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Göteborgs universitet

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