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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Format: | Article |
Language: | English |
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Nature Portfolio
2019-12-01
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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. |
first_indexed | 2024-12-14T14:14:44Z |
format | Article |
id | doaj.art-5bd1046a68be40d681c47a2db39adb32 |
institution | Directory Open Access Journal |
issn | 2041-1723 |
language | English |
last_indexed | 2024-12-14T14:14:44Z |
publishDate | 2019-12-01 |
publisher | Nature Portfolio |
record_format | Article |
series | Nature Communications |
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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