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Ammonium-bearing clinopyroxene: A potential nitrogen reservoir in the Earth's mantle
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“Nitrogen-bearing crust may then be subducted, where some nitrogen may return to the atmosphere via arc volcanism, but the rest will continue to the mantle because of the stability of ammonium-bearing silicates at high temperatures (67).”
From Disequilibrium biosignatures over Earth history and implications for detecting exoplanet life (2018) · cites this paper as [67]
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Metadata
- Authors
- Watenphul, A., Wunder, B., Wirth, R., & Heinrich, W.
- Affiliations
- GFZ Helmholtz Centre for Geosciences (DE)
- Corresponding author
- Watenphul, Anke
- Venue
- Chemical Geology
- Publisher
- Elsevier BV
- Published
- 2010-02
- Volume
- 270
- Issue
- 1-4
- Pages
- 240-248
- ISSN
- 0009-2541 (ISSN-L)
- OpenAlex
- W2004695273
- Cited by
- 109
- References
- 62
- Citations by year
- 2026: 6 · 2025: 5 · 2024: 10 · 2023: 7 · 2022: 7 · 2021: 4 · 2020: 7 · 2019: 10 · 2018: 14 · 2017: 8 · 2016: 6 · 2015: 4 · 2014: 7 · 2013: 7 · 2012: 5
- FWCI
- 1.98
- Type
- journal article
- Language
- en
- Open access
- Licence
- Locations
- Chemical Geology (publishedVersion)
- Publication Database GFZ (GFZ German Research Centre for Geosciences) (submittedVersion, other-oa)
- Publication Database GFZ (GFZ German Research Centre for Geosciences) (submittedVersion)
- Geochimica et Cosmochimica Acta Supplement
- Funders
- German Science Foundation (2015/(8-1))
- Topics
- Physical Sciences › Earth and Planetary Sciences › Geophysics › High-pressure geophysics and materials
- Physical Sciences › Earth and Planetary Sciences › Geochemistry and Petrology › Geological and Geochemical Analysis
- Physical Sciences › Earth and Planetary Sciences › Space and Planetary Science › Astro and Planetary Science
- Keywords
- nitrogen reservoirs, Earth's mantle, diopside, nitrogen cycling, high-pressure mineralogy, coupled substitution
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