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dc.contributor.authorMcCammon, Catherine
dc.contributor.authorBureau, Hélène
dc.contributor.authorCleaves II, H. James
dc.contributor.authorCottrell, Elizabeth
dc.contributor.authorDorfman, Susannah M.
dc.contributor.authorKellogg, Louise H
dc.contributor.authorLi, Jie
dc.contributor.authorMikhail, Sami
dc.contributor.authorMoussallam, Yves
dc.contributor.authorSanloup, Chrystele
dc.contributor.authorThomson, Andrew R
dc.contributor.authorBrovarone, Alberto Vitale
dc.date.accessioned2020-01-06T12:30:08Z
dc.date.available2020-01-06T12:30:08Z
dc.date.issued2020-01-02
dc.identifier.citationMcCammon , C , Bureau , H , Cleaves II , H J , Cottrell , E , Dorfman , S M , Kellogg , L H , Li , J , Mikhail , S , Moussallam , Y , Sanloup , C , Thomson , A R & Brovarone , A V 2020 , ' Deep Earth carbon reactions through time and space ' , American Mineralogist , vol. 105 , no. 1 , pp. 22-27 . https://doi.org/10.2138/am-2020-6888CCBYen
dc.identifier.issn0003-004X
dc.identifier.otherPURE: 261244649
dc.identifier.otherPURE UUID: 94239993-7c57-41f6-8c3d-7283efe6ed4a
dc.identifier.otherORCID: /0000-0001-5276-0229/work/67167751
dc.identifier.otherScopus: 85078556531
dc.identifier.otherWOS: 000505007500003
dc.identifier.urihttp://hdl.handle.net/10023/19223
dc.descriptionThe authors acknowledge partial support from the Sloan Foundation grant G-2016-7157.en
dc.description.abstractReactions involving carbon in the deep Earth have limited manifestation on Earth’s surface, yet they have played a critical role in the evolution of our planet. The metal-silicate partitioning reaction promoted carbon capture during Earth’s accretion and may have sequestered substantial carbon in Earth’s core. The freezing reaction involving iron-carbon liquid could have contributed to the growth of Earth’s inner core and the geodynamo. The redox melting/freezing reaction largely controls the movement of carbon in the modern mantle, and reactions between carbonates and silicates in the deep mantle also promote carbon mobility. The ten-year activity of the Deep Carbon Observatory has made important contributions to our knowledge of how these reactions are involved in the cycling of carbon throughout our planet, both past and present, and helped to identify gaps in our understanding that motivate and give direction to future studies.
dc.format.extent6
dc.language.isoeng
dc.relation.ispartofAmerican Mineralogisten
dc.rightsCopyright © 2020 Mineralogical Society of America. Open Access. This article is CC-BY 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.en
dc.subjectInner coreen
dc.subjectGeodynamoen
dc.subjectSubductionen
dc.subjectDiamonden
dc.subjectCarbonateen
dc.subjectCarbon-rich fluids and meltsen
dc.subjectOxygen fugacityen
dc.subjectMetal-silicate partitioningen
dc.subjectRedox freezing and meltingen
dc.subjectGE Environmental Sciencesen
dc.subject.lccGEen
dc.titleDeep Earth carbon reactions through time and spaceen
dc.typeJournal itemen
dc.description.versionPublisher PDFen
dc.contributor.institutionUniversity of St Andrews.School of Earth & Environmental Sciencesen
dc.contributor.institutionUniversity of St Andrews.St Andrews Centre for Exoplanet Scienceen
dc.contributor.institutionUniversity of St Andrews.St Andrews Isotope Geochemistryen
dc.identifier.doihttps://doi.org/10.2138/am-2020-6888CCBY
dc.description.statusPeer revieweden


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