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Coccolithophore biodiversity controls carbonate export in the Southern Ocean

dc.contributor.authorRigual Hernández, Andrés S.
dc.contributor.authorTrull, Thomas W.
dc.contributor.authorNodder, Scott D.
dc.contributor.authorFlores, José A.
dc.contributor.authorBostock, Helen
dc.contributor.authorAbrantes, Fatima
dc.contributor.authorEriksen, Ruth S.
dc.contributor.authorSierro, Francisco J.
dc.contributor.authorDavies, Diana M.
dc.contributor.authorBallegeer, Anne-Marie
dc.contributor.authorFuertes, Miguel A.
dc.contributor.authorNorthcote, Lisa C.
dc.date.accessioned2020-02-19T18:09:01Z
dc.date.available2020-02-19T18:09:01Z
dc.date.issued2020
dc.description.abstractSouthern Ocean waters are projected to undergo profound changes in their physical and chemical properties in the coming decades. Coccolithophore blooms in the Southern Ocean are thought to account for a major fraction of the global marine calcium carbonate (CaCO3) production and export to the deep sea. Therefore, changes in the composition and abundance of Southern Ocean coccolithophore populations are likely to alter the marine carbon cycle, with feedbacks to the rate of global climate change. However, the contribution of coccolithophores to CaCO3 export in the Southern Ocean is uncertain, particularly in the circumpolar subantarctic zone that represents about half of the areal extent of the Southern Ocean and where coccolithophores are most abundant. Here, we present measurements of annual CaCO3 flux and quantitatively partition them amongst coccolithophore species and heterotrophic calcifiers at two sites representative of a large portion of the subantarctic zone. We find that coccolithophores account for a major fraction of the annual CaCO3 export, with the highest contributions in waters with low algal biomass accumulations. Notably, our analysis reveals that although Emiliania huxleyi is an important vector for CaCO3 export to the deep sea, less abundant but larger species account for most of the annual coccolithophore CaCO3 flux. This observation contrasts with the generally accepted notion that high particulate inorganic carbon accumulations during the austral summer in the subantarctic Southern Ocean are mainly caused by E. huxleyi blooms. It appears likely that the climate-induced migration of oceanic fronts will initially result in the poleward expansion of large coccolithophore species increasing CaCO3 production. However, subantarctic coccolithophore populations will eventually diminish as acidification overwhelms those changes. Overall, our analysis emphasizes the need for species-centred studies to improve our ability to project future changes in phytoplankton communities and their influence on marine biogeochemical cycles.pt_PT
dc.description.versioninfo:eu-repo/semantics/publishedVersionpt_PT
dc.identifier.doihttps://doi.org/10.5194/bg-17-245-2020pt_PT
dc.identifier.issn1726-4170
dc.identifier.urihttp://hdl.handle.net/10400.1/13536
dc.language.isoengpt_PT
dc.peerreviewedyespt_PT
dc.publisherCopernicus Publicationspt_PT
dc.relationSouthern Ocean Nanoplankton Response to CO2
dc.relation.publisherversionhttps://www.biogeosciences.net/17/245/2020/pt_PT
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/pt_PT
dc.titleCoccolithophore biodiversity controls carbonate export in the Southern Oceanpt_PT
dc.typejournal article
dspace.entity.typePublication
oaire.awardTitleSouthern Ocean Nanoplankton Response to CO2
oaire.awardURIinfo:eu-repo/grantAgreement/EC/H2020/748690/EU
oaire.citation.endPage263pt_PT
oaire.citation.issue1pt_PT
oaire.citation.startPage245pt_PT
oaire.citation.titleBiogeosciencespt_PT
oaire.citation.volume17pt_PT
oaire.fundingStreamH2020
person.familyNameAbrantes
person.givenNameFatima
person.identifier.ciencia-id021D-CA76-20D2
person.identifier.orcid0000-0002-9110-0212
person.identifier.ridB-5985-2013
person.identifier.scopus-author-id16030759200
project.funder.identifierhttp://doi.org/10.13039/501100008530
project.funder.nameEuropean Commission
rcaap.rightsopenAccesspt_PT
rcaap.typearticlept_PT
relation.isAuthorOfPublication45b2d36a-1a11-4b6c-81b3-47f657904207
relation.isAuthorOfPublication.latestForDiscovery45b2d36a-1a11-4b6c-81b3-47f657904207
relation.isProjectOfPublicatione87a97f4-0edb-4b9b-a2c7-e072f8e70bdd
relation.isProjectOfPublication.latestForDiscoverye87a97f4-0edb-4b9b-a2c7-e072f8e70bdd

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