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dc.contributor.authorDuncan, Rebecca J.
dc.contributor.authorSøreide, Janne
dc.contributor.authorVarpe, Øystein
dc.contributor.authorWiktor, Józef
dc.contributor.authorPitusi, Vanessa
dc.contributor.authorRunge, Elaine
dc.contributor.authorPetrou, Katherina
dc.coverage.spatialSvalbard, Norwayen_US
dc.date.accessioned2024-08-15T13:01:48Z
dc.date.available2024-08-15T13:01:48Z
dc.date.created2024-04-23T19:34:36Z
dc.date.issued2024
dc.identifier.citationProgress in Oceanography. 2024, 224 .en_US
dc.identifier.issn0079-6611
dc.identifier.urihttps://hdl.handle.net/11250/3146622
dc.description.abstractSea ice microalgae are an important source of energy for the polar marine food web, representing the primary carbon source prior to pelagic phytoplankton blooms. Here we investigate community dynamics of sea ice microalgal communities in land-fast sea ice across six different fjords in high-Arctic Svalbard, Norway, during Spring (April – May). We found that light (0.1 – 23% incoming PAR / 0.1 – 193 μmol photons m-2s -1) played a central role in determining community composition, with more diverse assemblages observed in sites with more light transmitted to the bottom ice community. In April, microalgal assemblages were similar when under-ice light transmittance was similar, independent of geographical location, however this light-derived separation of community structure was not evident in May. At all sites, assemblages were dominated by pennate diatoms, with the most abundant taxon being Nitzschia frigida. However, with increasing under-ice light transmittance, we saw an increase in the relative abundance of Dinophyceae, Navicula spp. and Thalassiosira spp.. A positive relationship between light and δ13C enrichment and C:N ratios in the ice algal biomass demonstrated the effect of light on the biochemical composition of ice algae. Light did not correlate with cell abundance or chlorophyll a concentration. With anticipated changes to Arctic sea ice extent and snow cover as a result of climate change, we will see shifts in the light transmitted to the bottom ice community. These shifts, whether caused by reduced light transmittance from increased snow cover or increased light transmittance from thinning ice, snow depth or increased rainfall, will likely alter sea ice microalgal community composition, which in turn, may influence the success of secondary production and biogeochemical cycling in polar watersen_US
dc.language.isoengen_US
dc.rightsNavngivelse 4.0 Internasjonal*
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/deed.no*
dc.subjectSea ice microalgaeen_US
dc.subjectSvalbarden_US
dc.subjectNitzschia frigidaen_US
dc.subjectbiogeochemical cyclingen_US
dc.subjectunder ice light transmittanceen_US
dc.titleSpatio-temporal dynamics in microalgal communities in Arctic land-fast sea iceen_US
dc.title.alternativeSpatio-temporal dynamics in microalgal communities in Arctic land-fast sea iceen_US
dc.typePeer revieweden_US
dc.typeJournal articleen_US
dc.description.versionpublishedVersionen_US
dc.rights.holder© 2024 The Authorsen_US
dc.subject.nsiVDP::Matematikk og Naturvitenskap: 400::Geofag: 450en_US
dc.source.pagenumber0en_US
dc.source.volume224en_US
dc.source.journalProgress in Oceanographyen_US
dc.identifier.doi10.1016/j.pocean.2024.103248
dc.identifier.cristin2263927
dc.relation.projectNorges forskningråd: 310692en_US
dc.relation.projectNorges forskningsråd: 310664en_US
cristin.ispublishedtrue
cristin.fulltextoriginal
cristin.qualitycode1


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