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dc.contributor.authorCastro de la Guardia, Laura
dc.contributor.authorFilbee-Dexter, Karen
dc.contributor.authorReimer, Jillian
dc.contributor.authorMacGregor, Kathleen A.
dc.contributor.authorGarrido, Ignacio
dc.contributor.authorSingh, Rakesh K.
dc.contributor.authorBélanger, Simon
dc.contributor.authorKonar, Brenda
dc.contributor.authorIken, Katrin
dc.contributor.authorJohnson, Ladd E.
dc.contributor.authorArchambault, Philippe
dc.contributor.authorSejr, Mikael K.
dc.contributor.authorSøreide, Janne
dc.contributor.authorMundy, C.J.
dc.date.accessioned2023-09-21T11:43:47Z
dc.date.available2023-09-21T11:43:47Z
dc.date.created2023-01-31T16:19:23Z
dc.date.issued2023
dc.identifier.citationElementa: Science of the Anthropocene. 2023, 11 (1), .
dc.identifier.issn2325-1026
dc.identifier.urihttps://hdl.handle.net/11250/3091073
dc.description.abstractKelps are a dominant macrophyte group and primary producer in Arctic nearshore waters that provide significant services to the coastal ecosystem. The quantification of these services in the Arctic is constrained, however, by limited estimates of kelp depth extent, which creates uncertainties in the area covered by kelp. Here, we test the environmental drivers of the depth extent of Arctic kelp. We used Southampton Island (SI), Nunavut, Canada, as an example region after an initial survey found deep Arctic kelp (at depths to at least 50 m) with relatively low grazing pressure within diverse hydrographic conditions. We found abundant rocky substrata, but no influence of substratum type on kelp cover. The kelp cover increased with depth until 20 m and then decreased (the median maximum depth for all stations was 37 m). The best predictor of kelp depth extent was the number of annual open (ice-free) water days with light (r2 = 44–52%); combining depth extent data from SI with published data from Greenland strengthened this relationship (r2 = 58–71%). Using these relationships we estimated the maximum kelp-covered area around SI to be 27,000–28,000 km2, yielding potential primary production between 0.6 and 1.9 Tg Cyr−1. Water transparency was a key determinant of the underwater light environment and was essential for explaining cross-regional differences in kelp depth extent in SI and Greenland. Around SI the minimum underwater light required by kelp was 49 mol photons m−2 yr−1, or 1.4% of annual integrated incident irradiance. Future consideration of seasonal variation in water transparency can improve these underwater light estimations, while future research seeking to understand the kelp depth extent relationship with nutrients and ocean dynamics can further advance estimates of their vertical distribution. Improving our understanding of the drivers of kelp depth extent can reduce uncertainties around the role of kelp in Arctic marine ecosystems.
dc.language.isoeng
dc.titleIncreasing depth distribution of Arctic kelp with increasing number of open water days with light
dc.title.alternativeIncreasing depth distribution of Arctic kelp with increasing number of open water days with light
dc.typePeer reviewed
dc.typeJournal article
dc.description.versionpublishedVersion
dc.source.pagenumber20
dc.source.volume11
dc.source.journalElementa: Science of the Anthropocene
dc.source.issue1
dc.identifier.doi10.1525/elementa.2022.00051
dc.identifier.cristin2120628
dc.relation.projectNorges forskningsråd: 296836
cristin.ispublishedtrue
cristin.fulltextoriginal
cristin.qualitycode1


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