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dc.contributor.authorDumont, Matthew Declan
dc.contributor.authorPichevin, L.
dc.contributor.authorGeibert, W.
dc.contributor.authorCrosta, X.
dc.contributor.authorMichel, E.
dc.contributor.authorMoreton, S.
dc.contributor.authorGaneshram, R.
dc.date.accessioned2020-03-25T11:30:01Z
dc.date.available2020-03-25T11:30:01Z
dc.date.issued2020-03-24
dc.identifier.citationDumont , M D , Pichevin , L , Geibert , W , Crosta , X , Michel , E , Moreton , S & Ganeshram , R 2020 , ' The nature of deep overturning and reconfigurations of the silicon cycle across the last deglaciation ' , Nature Communications , vol. 11 , 1534 . https://doi.org/10.1038/s41467-020-15101-6en
dc.identifier.issn2041-1723
dc.identifier.otherPURE: 266187007
dc.identifier.otherPURE UUID: be5e20ab-b7d5-47fb-a492-74089a35977f
dc.identifier.otherScopus: 85082380118
dc.identifier.otherWOS: 000530024600004
dc.identifier.urihttps://hdl.handle.net/10023/19704
dc.descriptionFunding: NERC E3 DTP studentship awarded to M. Dumont and NERC Grant (NE/J02371X/1) award to R.S. Ganeshram and L.E. Pichevin.en
dc.description.abstractChanges in ocean circulation and the biological carbon pump have been implicated as the drivers behind the rise in atmospheric CO2 across the last deglaciation; however, the processes involved remain uncertain. Previous records have hinted at a partitioning of deep ocean ventilation across the two major intervals of atmospheric CO2 rise, but the consequences of differential ventilation on the Si cycle has not been explored. Here we present three new records of silicon isotopes in diatoms and sponges from the Southern Ocean that together show increased Si supply from deep mixing during the deglaciation with a maximum during the Younger Dryas (YD). We suggest Antarctic sea ice and Atlantic overturning conditions favoured abyssal ocean ventilation at the YD and marked an interval of Si cycle reorganisation. By regulating the strength of the biological pump, the glacial–interglacial shift in the Si cycle may present an important control on Pleistocene CO2 concentrations.
dc.format.extent11
dc.language.isoeng
dc.relation.ispartofNature Communicationsen
dc.rightsCopyright © The Author(s) 2020. Open Access. This article is licensed under a Creative Commons Attribution 4.0 International License, which permits use, sharing, adaptation, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons license, and indicate if changes were made. The images or other third party material in this article are included in the article’s Creative Commons license, unless indicated otherwise in a credit line to the material. If material is not included in the article’s Creative Commons license and your intended use is not permitted by statutory regulation or exceeds the permitted use, you will need to obtain permission directly from the copyright holder. To view a copy of this license, visit http://creativecommons.org/licenses/by/4.0/.en
dc.subjectGE Environmental Sciencesen
dc.subjectDASen
dc.subject.lccGEen
dc.titleThe nature of deep overturning and reconfigurations of the silicon cycle across the last deglaciationen
dc.typeJournal articleen
dc.description.versionPublisher PDFen
dc.contributor.institutionUniversity of St Andrews. School of Earth & Environmental Sciencesen
dc.identifier.doihttps://doi.org/10.1038/s41467-020-15101-6
dc.description.statusPeer revieweden
dc.date.embargoedUntil2020-03-24


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