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Limited variability in the phytoplankton Emiliania huxleyi since the pre-industrial era in the Subantarctic Southern Ocean

dc.contributor.authorRigual-Hernández, A. S.
dc.contributor.authorSánchez-Santos, J. M.
dc.contributor.authorEriksen, R.
dc.contributor.authorMoy, A. D.
dc.contributor.authorSierro, F. J.
dc.contributor.authorFlores, J. A.
dc.contributor.authorAbrantes, Fatima
dc.contributor.authorBostock, H.
dc.contributor.authorNodder, S. D.
dc.contributor.authorGonzález-Lanchas, A.
dc.contributor.authorTrull, T. W.
dc.date.accessioned2020-10-15T12:25:35Z
dc.date.available2020-10-15T12:25:35Z
dc.date.issued2020
dc.description.abstractThe Southern Ocean is warming faster than the average global ocean and is particularly vulnerable to ocean acidification due to its low temperatures and moderate alkalinity. Coccolithophores are the most productive calcifying phytoplankton and an important component of Southern Ocean ecosystems. Laboratory observations on the most abundant coccolithophore, Emiliania huxleyi, suggest that this species is susceptible to variations in seawater carbonate chemistry, with consequent impacts in the carbon cycle. Whether anthropogenic environmental change during the industrial era has modified coccolithophore populations in the Southern Ocean, however, remains uncertain. This study analysed the coccolithophore assemblage composition and morphometric parameters of E. huxleyi coccoliths of a suite of Holocene-aged sediment samples from south of Tasmania. The analysis suggests that dissolution diminished the mass and length of E. huxleyi coccoliths in the sediments, but the thickness of the coccoliths was decoupled from dissolution allowing direct comparison of samples with different degree of preservation. The latitudinal distribution pattern of coccolith thickness mirrors the latitudinal environmental gradient in the surface layer, highlighting the importance of the geographic distribution of E. huxleyi morphotypes on the control of coccolith morphometrics. Additionally, comparison of the E. huxleyi coccolith assemblages in the sediments with those of annual subantarctic sediment trap records found that modern E. huxleyi coccoliths are 2% thinner than those from the pre-industrial era. The subtle variation in coccolith thickness contrasts sharply with earlier work that documented a pronounced reduction in shell calcification and consequent shell-weight decrease of 30-35% on the planktonic foraminifera Globigerina bulloides induced by ocean acidification. Results of this study underscore the varying sensitivity of different marine calcifying plankton groups to ongoing environmental change.pt_PT
dc.description.sponsorshipFCT: UIDB/04326/2020;pt_PT
dc.description.versioninfo:eu-repo/semantics/publishedVersionpt_PT
dc.identifier.doi10.1016/j.ancene.2020.100254pt_PT
dc.identifier.issn2213-3054
dc.identifier.urihttp://hdl.handle.net/10400.1/14778
dc.language.isoengpt_PT
dc.peerreviewedyespt_PT
dc.publisherElsevierpt_PT
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/4.0/pt_PT
dc.subjectCO2 emissionspt_PT
dc.subjectEmiliania huxleyipt_PT
dc.subjectOcean acidificationpt_PT
dc.subjectEnvironmental changept_PT
dc.subjectSouthern Oceanpt_PT
dc.subjectCoccolithophorespt_PT
dc.titleLimited variability in the phytoplankton Emiliania huxleyi since the pre-industrial era in the Subantarctic Southern Oceanpt_PT
dc.typejournal article
dspace.entity.typePublication
oaire.citation.startPage100254pt_PT
oaire.citation.titleAnthropocenept_PT
oaire.citation.volume31pt_PT
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
rcaap.rightsopenAccesspt_PT
rcaap.typearticlept_PT
relation.isAuthorOfPublication45b2d36a-1a11-4b6c-81b3-47f657904207
relation.isAuthorOfPublication.latestForDiscovery45b2d36a-1a11-4b6c-81b3-47f657904207

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