New isotope constraints on the Mg oceanic budget point to cryptic modern dolomite formation

Earth’s carbon cycle and oceanic magnesium cycle are controlled by processes such as weathering, volcanism and precipitation of carbonates, such as dolomite. Here, the authors contradict the view that modern dolomite formation is rare and suggest instead that dolomite accounts for ~40–60% of the glo...

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Main Authors: Netta Shalev, Tomaso R. R. Bontognali, C. Geoffrey Wheat, Derek Vance
Format: Article
Language:English
Published: Nature Portfolio 2019-12-01
Series:Nature Communications
Online Access:https://doi.org/10.1038/s41467-019-13514-6
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author Netta Shalev
Tomaso R. R. Bontognali
C. Geoffrey Wheat
Derek Vance
author_facet Netta Shalev
Tomaso R. R. Bontognali
C. Geoffrey Wheat
Derek Vance
author_sort Netta Shalev
collection DOAJ
description Earth’s carbon cycle and oceanic magnesium cycle are controlled by processes such as weathering, volcanism and precipitation of carbonates, such as dolomite. Here, the authors contradict the view that modern dolomite formation is rare and suggest instead that dolomite accounts for ~40–60% of the global oceanic Mg output in the last 20 Ma.
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spelling doaj.art-5bd1046a68be40d681c47a2db39adb322022-12-21T22:58:13ZengNature PortfolioNature Communications2041-17232019-12-0110111010.1038/s41467-019-13514-6New isotope constraints on the Mg oceanic budget point to cryptic modern dolomite formationNetta Shalev0Tomaso R. R. Bontognali1C. Geoffrey Wheat2Derek Vance3Department of Earth Sciences, Institute of Geochemistry and Petrology, ETH ZürichDepartment of Earth Sciences, Institute of Geochemistry and Petrology, ETH ZürichUniversity of Alaska FairbanksDepartment of Earth Sciences, Institute of Geochemistry and Petrology, ETH ZürichEarth’s carbon cycle and oceanic magnesium cycle are controlled by processes such as weathering, volcanism and precipitation of carbonates, such as dolomite. Here, the authors contradict the view that modern dolomite formation is rare and suggest instead that dolomite accounts for ~40–60% of the global oceanic Mg output in the last 20 Ma.https://doi.org/10.1038/s41467-019-13514-6
spellingShingle Netta Shalev
Tomaso R. R. Bontognali
C. Geoffrey Wheat
Derek Vance
New isotope constraints on the Mg oceanic budget point to cryptic modern dolomite formation
Nature Communications
title New isotope constraints on the Mg oceanic budget point to cryptic modern dolomite formation
title_full New isotope constraints on the Mg oceanic budget point to cryptic modern dolomite formation
title_fullStr New isotope constraints on the Mg oceanic budget point to cryptic modern dolomite formation
title_full_unstemmed New isotope constraints on the Mg oceanic budget point to cryptic modern dolomite formation
title_short New isotope constraints on the Mg oceanic budget point to cryptic modern dolomite formation
title_sort new isotope constraints on the mg oceanic budget point to cryptic modern dolomite formation
url https://doi.org/10.1038/s41467-019-13514-6
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