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Radiocarbon age offsets between two surface dwelling planktonic foraminifera species during abrupt climate events in the SW Iberian Margin

dc.contributor.authorAusín, Blanca
dc.contributor.authorHaghipour, Negar
dc.contributor.authorWacker, Lukas
dc.contributor.authorVoelker, Antje
dc.contributor.authorHodell, David
dc.contributor.authorMagill, Clayton
dc.contributor.authorLooser, Nathan
dc.contributor.authorBernasconi, Stefano M.
dc.contributor.authorEglinton, Timothy I.
dc.date.accessioned2020-07-24T10:31:29Z
dc.date.available2020-07-24T10:31:29Z
dc.date.issued2019-01-26
dc.date.updated2020-07-23T21:16:42Z
dc.description.abstractThis study identifies temporal biases in the radiocarbon ages of the planktonic foraminifera species Globigerina bulloides and Globigerinoides ruber (white) in a sediment core from the SW Iberian margin (so‐called Shackleton site). Leaching of the outer shell and measurement of the radiocarbon content of both the leachate and leached sample enabled us to identify surface contamination of the tests and its impact on their 14C ages. Incorporation of younger radiocarbon on the outer shell affected both species and had a larger impact downcore. Interspecies comparison of the 14C ages of the leached samples reveal systematic offsets with 14C ages for G. ruber being younger than G. bulloides ages during the last deglaciation and part of the Early and mid‐Holocene. The greatest offsets (up to 1,030 years) were found during Heinrich Stadial 1, the Younger Dryas, and part of the Holocene. The potential factors differentially affecting these two planktonic species were assessed by complementary 14C, oxygen and carbon isotopes, and species abundance determinations. The coupled effect of bioturbation with changes in the abundance of G. ruber is invoked to account for the large age offsets. Our results highlight that 14C ages of planktonic foraminifera might be largely compromised even in settings characterized by high sediment accumulation rates. Thus, a careful assessment of potential temporal biases must be performed prior to using 14C ages for paleoclimate investigations or radiocarbon calibrations (e.g., marine calibration curve Marine13, Reimer et al., 2013, https://doi.org/10.2458/azu_js_rc.55.16947).
dc.description.sponsorshipUID/Multi/04326/2019, IF/01500/2014pt_PT
dc.description.versioninfo:eu-repo/semantics/publishedVersionpt_PT
dc.identifier.doi10.1029/2018PA003490pt_PT
dc.identifier.issn2572-4525
dc.identifier.slugcv-prod-423420
dc.identifier.urihttp://hdl.handle.net/10400.1/14138
dc.language.isoengpt_PT
dc.peerreviewedyespt_PT
dc.publisherWileypt_PT
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/pt_PT
dc.subjectWestern Iberian marginpt_PT
dc.subjectPlanktonic foraminiferapt_PT
dc.subjectRadiocarbon datingpt_PT
dc.titleRadiocarbon age offsets between two surface dwelling planktonic foraminifera species during abrupt climate events in the SW Iberian Marginpt_PT
dc.typejournal article
dspace.entity.typePublication
oaire.awardURIinfo:eu-repo/grantAgreement/FCT/5876/UID%2FMulti%2F04326%2F2013/PT
oaire.citation.conferencePlaceUnited Statespt_PT
oaire.citation.endPage78pt_PT
oaire.citation.startPage63pt_PT
oaire.citation.titlePaleoceanography and Paleoclimatologypt_PT
oaire.citation.volume34pt_PT
oaire.fundingStream5876
person.familyNameVoelker
person.givenNameAntje
person.identifier2315310
person.identifier.ciencia-idC11E-D8E6-CDFA
person.identifier.orcid0000-0001-6465-6023
person.identifier.ridC-5427-2012
person.identifier.scopus-author-id8784446000
project.funder.identifierhttp://doi.org/10.13039/501100001871
project.funder.nameFundação para a Ciência e a Tecnologia
rcaap.cv.cienciaidC11E-D8E6-CDFA | Antje Helga Luise Voelker
rcaap.rightsopenAccesspt_PT
rcaap.typearticlept_PT
relation.isAuthorOfPublicationbca80a86-eb35-4bca-a4ba-85b53831d69e
relation.isAuthorOfPublication.latestForDiscoverybca80a86-eb35-4bca-a4ba-85b53831d69e
relation.isProjectOfPublication868b4818-3efa-4edb-9202-c464d64fd38f
relation.isProjectOfPublication.latestForDiscovery868b4818-3efa-4edb-9202-c464d64fd38f

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