Oxygenation by a changing crust

Oxygenation by a changing crust

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Serpentine minerals in Earth's early upper continental crust suppressed atmospheric oxygen levels until the upper crust became granitic. Access through your institution Buy or subscribe


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Geochemie, Freie Universität Berlin, Malteserstraße 74-100, Berlin, 12249, Germany J. Elis Hoffmann Authors * J. Elis Hoffmann View author publications You can also search for this author


inPubMed Google Scholar CORRESPONDING AUTHOR Correspondence to J. Elis Hoffmann. RIGHTS AND PERMISSIONS Reprints and permissions ABOUT THIS ARTICLE CITE THIS ARTICLE Hoffmann, J. Oxygenation


by a changing crust. _Nature Geosci_ 10, 713–714 (2017). https://doi.org/10.1038/ngeo3038 Download citation * Published: 18 September 2017 * Issue Date: 01 October 2017 * DOI:


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