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dc.contributor.authorRooks, Christine
dc.contributor.authorFang, James Kar-Hei
dc.contributor.authorMørkved, Pål Tore
dc.contributor.authorZhao, Rui
dc.contributor.authorRapp v/dødsbo, Hans Tore
dc.contributor.authorXavier, Joana R
dc.contributor.authorHoffmann, Friederike
dc.date.accessioned2021-02-16T12:25:14Z
dc.date.available2021-02-16T12:25:14Z
dc.date.created2020-07-21T14:21:31Z
dc.date.issued2020-03
dc.PublishedBiogeosciences. 2020, 17 (5), 1231-1245.
dc.identifier.issn1726-4170
dc.identifier.urihttps://hdl.handle.net/11250/2728383
dc.description.abstractSponges are commonly known as general nutrient providers for the marine ecosystem, recycling organic matter into various forms of bioavailable nutrients such as ammonium and nitrate. In this study we challenge this view. We show that nutrient removal through microbial denitrification is a common feature in six cold-water sponge species from boreal and Arctic sponge grounds. Denitrification rates were quantified by incubating sponge tissue sections with 15NO−3-amended oxygen-saturated seawater, mimicking conditions in pumping sponges, and de-oxygenated seawater, mimicking non-pumping sponges. It was not possible to detect any rates of anaerobic ammonium oxidation (anammox) using incubations with 15NH+4. Denitrification rates of the different sponge species ranged from below detection to 97 nmol N cm−3 sponge d−1 under oxic conditions, and from 24 to 279 nmol N cm−3 sponge d−1 under anoxic conditions. A positive relationship between the highest potential rates of denitrification (in the absence of oxygen) and the species-specific abundances of nirS and nirK genes encoding nitrite reductase, a key enzyme for denitrification, suggests that the denitrifying community in these sponge species is active and prepared for denitrification. The lack of a lag phase in the linear accumulation of the 15N-labelled N2 gas in any of our tissue incubations is another indicator for an active community of denitrifiers in the investigated sponge species. Low rates for coupled nitrification–denitrification indicate that also under oxic conditions, the nitrate used to fuel denitrification rates was derived rather from the ambient seawater than from sponge nitrification. The lack of nifH genes encoding nitrogenase, the key enzyme for nitrogen fixation, shows that the nitrogen cycle is not closed in the sponge grounds. The denitrified nitrogen, no matter its origin, is then no longer available as a nutrient for the marine ecosystem. These results suggest a high potential denitrification capacity of deep-sea sponge grounds based on typical sponge biomass on boreal and Arctic sponge grounds, with areal denitrification rates of 0.6 mmol N m−2 d−1 assuming non-pumping sponges and still 0.3 mmol N m−2 d−1 assuming pumping sponges. This is well within the range of denitrification rates of continental shelf sediments. Anthropogenic impact and global change processes affecting the sponge redox state may thus lead to deep-sea sponge grounds changing their role in marine ecosystem from being mainly nutrient sources to becoming mainly nutrient sinks.en_US
dc.language.isoengen_US
dc.publisherEuropean Geosciences Unionen_US
dc.rightsNavngivelse 4.0 Internasjonal*
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/deed.no*
dc.titleDeep-sea sponge grounds as nutrient sinks: Denitrification is common in boreo-Arctic spongesen_US
dc.typeJournal articleen_US
dc.typePeer revieweden_US
dc.description.versionpublishedVersionen_US
dc.rights.holderCopyright Author(s)en_US
cristin.ispublishedtrue
cristin.fulltextoriginal
cristin.qualitycode1
dc.identifier.doi10.5194/bg-17-1231-2020
dc.identifier.cristin1820058
dc.source.journalBiogeosciencesen_US
dc.source.4017
dc.source.145
dc.source.pagenumber1231-1245en_US
dc.relation.projectEC/H2020/679849en_US
dc.relation.projectNorges forskningsråd: 225283en_US
dc.relation.projectNorges forskningsråd: 245907en_US
dc.source.volume17en_US
dc.source.issue5en_US


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