Stability of iron-bearing carbonates in the deep Earth’s interior

Carbonates are shown to exist in the lower mantle as seen in diamond inclusions, but thermodynamic constraints are poorly understood. Here, the authors synthesise two new iron carbonate compounds and find that self-oxidation-reduction reactions can preserve carbonates in the mantle.

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Autores principales: Valerio Cerantola, Elena Bykova, Ilya Kupenko, Marco Merlini, Leyla Ismailova, Catherine McCammon, Maxim Bykov, Alexandr I. Chumakov, Sylvain Petitgirard, Innokenty Kantor, Volodymyr Svitlyk, Jeroen Jacobs, Michael Hanfland, Mohamed Mezouar, Clemens Prescher, Rudolf Rüffer, Vitali B. Prakapenka, Leonid Dubrovinsky
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Lenguaje:EN
Publicado: Nature Portfolio 2017
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Acceso en línea:https://doaj.org/article/a79c8bed1e1f4228b309b4cf46722b2c
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spelling oai:doaj.org-article:a79c8bed1e1f4228b309b4cf46722b2c2021-12-02T14:40:26ZStability of iron-bearing carbonates in the deep Earth’s interior10.1038/ncomms159602041-1723https://doaj.org/article/a79c8bed1e1f4228b309b4cf46722b2c2017-07-01T00:00:00Zhttps://doi.org/10.1038/ncomms15960https://doaj.org/toc/2041-1723Carbonates are shown to exist in the lower mantle as seen in diamond inclusions, but thermodynamic constraints are poorly understood. Here, the authors synthesise two new iron carbonate compounds and find that self-oxidation-reduction reactions can preserve carbonates in the mantle.Valerio CerantolaElena BykovaIlya KupenkoMarco MerliniLeyla IsmailovaCatherine McCammonMaxim BykovAlexandr I. ChumakovSylvain PetitgirardInnokenty KantorVolodymyr SvitlykJeroen JacobsMichael HanflandMohamed MezouarClemens PrescherRudolf RüfferVitali B. PrakapenkaLeonid DubrovinskyNature PortfolioarticleScienceQENNature Communications, Vol 8, Iss 1, Pp 1-9 (2017)
institution DOAJ
collection DOAJ
language EN
topic Science
Q
spellingShingle Science
Q
Valerio Cerantola
Elena Bykova
Ilya Kupenko
Marco Merlini
Leyla Ismailova
Catherine McCammon
Maxim Bykov
Alexandr I. Chumakov
Sylvain Petitgirard
Innokenty Kantor
Volodymyr Svitlyk
Jeroen Jacobs
Michael Hanfland
Mohamed Mezouar
Clemens Prescher
Rudolf Rüffer
Vitali B. Prakapenka
Leonid Dubrovinsky
Stability of iron-bearing carbonates in the deep Earth’s interior
description Carbonates are shown to exist in the lower mantle as seen in diamond inclusions, but thermodynamic constraints are poorly understood. Here, the authors synthesise two new iron carbonate compounds and find that self-oxidation-reduction reactions can preserve carbonates in the mantle.
format article
author Valerio Cerantola
Elena Bykova
Ilya Kupenko
Marco Merlini
Leyla Ismailova
Catherine McCammon
Maxim Bykov
Alexandr I. Chumakov
Sylvain Petitgirard
Innokenty Kantor
Volodymyr Svitlyk
Jeroen Jacobs
Michael Hanfland
Mohamed Mezouar
Clemens Prescher
Rudolf Rüffer
Vitali B. Prakapenka
Leonid Dubrovinsky
author_facet Valerio Cerantola
Elena Bykova
Ilya Kupenko
Marco Merlini
Leyla Ismailova
Catherine McCammon
Maxim Bykov
Alexandr I. Chumakov
Sylvain Petitgirard
Innokenty Kantor
Volodymyr Svitlyk
Jeroen Jacobs
Michael Hanfland
Mohamed Mezouar
Clemens Prescher
Rudolf Rüffer
Vitali B. Prakapenka
Leonid Dubrovinsky
author_sort Valerio Cerantola
title Stability of iron-bearing carbonates in the deep Earth’s interior
title_short Stability of iron-bearing carbonates in the deep Earth’s interior
title_full Stability of iron-bearing carbonates in the deep Earth’s interior
title_fullStr Stability of iron-bearing carbonates in the deep Earth’s interior
title_full_unstemmed Stability of iron-bearing carbonates in the deep Earth’s interior
title_sort stability of iron-bearing carbonates in the deep earth’s interior
publisher Nature Portfolio
publishDate 2017
url https://doaj.org/article/a79c8bed1e1f4228b309b4cf46722b2c
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