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Active DNRA and denitrification in oxic hypereutrophic waters

Broman, Elias (author)
Stockholms universitet,Institutionen för ekologi, miljö och botanik,Stockholms universitets Östersjöcentrum
Zilius, Mindaugas (author)
Samuiloviene, Aurelija (author)
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Vybernaite-Lubiene, Irma (author)
Politi, Tobia (author)
Klawonn, Isabell (author)
Voss, Maren (author)
Nascimento, Francisco J. A (author)
Stockholms universitet,Institutionen för ekologi, miljö och botanik,Stockholms universitets Östersjöcentrum
Bonaglia, Stefano (author)
Gothenburg University,Göteborgs universitet,Stockholms universitet,Institutionen för ekologi, miljö och botanik,Klaipėda University, Lithuania; University of Southern Denmark, Denmark,Institutionen för marina vetenskaper,Department of marine sciences
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 (creator_code:org_t)
Elsevier BV, 2021
2021
English.
In: Water Research. - : Elsevier BV. - 0043-1354 .- 1879-2448. ; 194
  • Journal article (peer-reviewed)
Abstract Subject headings
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  • Since the start of synthetic fertilizer production more than a hundred years ago, the coastal ocean has been exposed to increasing nutrient loading, which has led to eutrophication and extensive algal blooms. Such hypereutrophic waters might harbor anaerobic nitrogen (N) cycling processes due to low-oxygen mi- croniches associated with abundant organic particles, but studies on nitrate reduction in coastal pelagic environments are scarce. Here, we report on 15 N isotope-labeling experiments, metagenome, and RT-qPCR data from a large hypereutrophic lagoon indicating that dissimilatory nitrate reduction to ammonium (DNRA) and denitrification were active processes, even though the bulk water was fully oxygenated ( > 224 μM O 2 ). DNRA in the bottom water corresponded to 83% of whole-ecosystem DNRA (water + sedi- ment), while denitrification was predominant in the sediment. Microbial taxa important for DNRA accord- ing to the metagenomic data were dominated by Bacteroidetes (genus Parabacteroides ) and Proteobac- teria (genus Wolinella ), while denitrification was mainly associated with proteobacterial genera Pseu- domonas, Achromobacter , and Brucella . The metagenomic and microscopy data suggest that these anaero- bic processes were likely occurring in low-oxygen microniches related to extensive growth of filamentous cyanobacteria, including diazotrophic Dolichospermum and non-diazotrophic Planktothrix . By summing the total nitrate fluxes through DNRA and denitrification, it results that DNRA retains approximately one fifth (19%) of the fixed N that goes through the nitrate pool. This is noteworthy as DNRA represents thus a very important recycling mechanism for fixed N, which sustains algal proliferation and leads to further enhancement of eutrophication in these endangered ecosystems.

Subject headings

NATURVETENSKAP  -- Biologi -- Ekologi (hsv//swe)
NATURAL SCIENCES  -- Biological Sciences -- Ecology (hsv//eng)
NATURVETENSKAP  -- Biologi -- Mikrobiologi (hsv//swe)
NATURAL SCIENCES  -- Biological Sciences -- Microbiology (hsv//eng)
NATURVETENSKAP  -- Geovetenskap och miljövetenskap -- Geokemi (hsv//swe)
NATURAL SCIENCES  -- Earth and Related Environmental Sciences -- Geochemistry (hsv//eng)
NATURVETENSKAP  -- Geovetenskap och miljövetenskap -- Miljövetenskap (hsv//swe)
NATURAL SCIENCES  -- Earth and Related Environmental Sciences -- Environmental Sciences (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)

Keyword

Cyanobacteria
Estuarine ecosystem
Eutrophication
Metagenome
Nitrogen cycling
Nutrients

Publication and Content Type

ref (subject category)
art (subject category)

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