Most Earth-surface calcites precipitate out of isotopic equilibrium
Most Earth-surface calcites precipitate out of isotopic equilibrium
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London: Nature Publishing Group UK
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English
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London: Nature Publishing Group UK
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Oxygen-isotope thermometry played a critical role in the rise of modern geochemistry and remains extensively used in (bio-)geoscience. Its theoretical foundations rest on the assumption that
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O/
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O partitioning among water and carbonate minerals primarily reflects thermodynamic equilibrium. However, after decades of research, there...
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Most Earth-surface calcites precipitate out of isotopic equilibrium
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TN_cdi_doaj_primary_oai_doaj_org_article_7f71bb6639164d8895d5625b539d49ba
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https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_doaj_primary_oai_doaj_org_article_7f71bb6639164d8895d5625b539d49ba
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ISSN
2041-1723
E-ISSN
2041-1723
DOI
10.1038/s41467-019-08336-5
