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dc.contributor.authorPessarrodona, Albert
dc.contributor.authorAssis, Jorge
dc.contributor.authorFilbee-Dexter, Karen
dc.contributor.authorBurrows, Michael T.
dc.contributor.authorGattuso, Jean-Pierre
dc.contributor.authorDuarte, Carlos M.
dc.contributor.authorKrause-Jensen, Dorte
dc.contributor.authorMoore, Pippa J.
dc.contributor.authorSmale, Dan A.
dc.contributor.authorWernberg, Thomas
dc.date.accessioned2023-03-08T12:14:12Z
dc.date.available2023-03-08T12:14:12Z
dc.date.created2023-01-27T13:00:25Z
dc.date.issued2022
dc.identifier.citationScience Advances. 2022, 8 (37), .en_US
dc.identifier.issn2375-2548
dc.identifier.urihttps://hdl.handle.net/11250/3057056
dc.description.abstractThe magnitude and distribution of net primary production (NPP) in the coastal ocean remains poorly constrained, particularly for shallow marine vegetation. Here, using a compilation of in situ annual NPP measurements across >400 sites in 72 geographic ecoregions, we provide global predictions of the productivity of seaweed habitats, which form the largest vegetated coastal biome on the planet. We find that seaweed NPP is strongly coupled to climatic variables, peaks at temperate latitudes, and is dominated by forests of large brown seaweeds. Seaweed forests exhibit exceptionally high per-area production rates (a global average of 656 and 1711 gC m−2 year−1 in the subtidal and intertidal, respectively), being up to 10 times higher than coastal phytoplankton in temperate and polar seas. Our results show that seaweed NPP is a strong driver of production in the coastal ocean and call for its integration in the oceanic carbon cycle, where it has traditionally been overlooked.en_US
dc.language.isoengen_US
dc.titleGlobal seaweed productivityen_US
dc.title.alternativeGlobal seaweed productivityen_US
dc.typePeer revieweden_US
dc.typeJournal articleen_US
dc.description.versionpublishedVersionen_US
dc.source.pagenumber10en_US
dc.source.volume8en_US
dc.source.journalScience Advancesen_US
dc.source.issue37en_US
dc.identifier.doi10.1126/sciadv.abn2465
dc.identifier.cristin2116487
dc.relation.projectEC/H2020/869154en_US
dc.relation.projectNorges forskningsråd: 287191en_US
cristin.ispublishedtrue
cristin.fulltextoriginal
cristin.qualitycode1


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