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Long-term fluxes and budget of ferric iron: implication for the redox states of the Earth's mantle and atmosphere
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“On the modern Earth, H2 production is low because only 12% of crustal Fe2+ is converted to Fe3+ as water cannot permeate all the oceanic crust (45).”
From Disequilibrium biosignatures over Earth history and implications for detecting exoplanet life (2018) · cites this paper as [45]
In the citing paper
“Furthermore, only 1 to 2% is due to serpentinization; the remaining 10 to 11% is from oxidation by sulfate, which does not generate H2 [(26), chap. 10; (45)].”
From Disequilibrium biosignatures over Earth history and implications for detecting exoplanet life (2018) · cites this paper as [45]
In the citing paper
“Today, magma emplacement from ridges, arcs, and plumes is 5.7 × 1013 kg/year (45), and with a generous assumption that crustal production may have been 10× higher on the early Earth, we take crustal production, PCrust, to range from 5.7 × 1013 to 5.7 × 1014 kg/year.”
From Disequilibrium biosignatures over Earth history and implications for detecting exoplanet life (2018) · cites this paper as [45]
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Metadata
- Authors
- Lécuyer, C.
- Affiliations
- École Normale Supérieure de Lyon (FR)
- Corresponding author
- Lécuyer, C
- ORCID
- Lécuyer, C
- Venue
- Earth and Planetary Science Letters
- Publisher
- Elsevier BV
- Published
- 1999-01-30
- Volume
- 165
- Issue
- 2
- Pages
- 197-211
- ISSN
- 0012-821X (ISSN-L)
- OpenAlex
- W2022014152
- Cited by
- 156
- References
- 66
- Citations by year
- 2026: 3 · 2025: 7 · 2024: 5 · 2023: 4 · 2022: 3 · 2021: 11 · 2020: 7 · 2019: 8 · 2018: 10 · 2017: 6 · 2016: 6 · 2015: 10 · 2014: 7 · 2013: 7 · 2012: 8
- FWCI
- 2.13
- Type
- journal article
- Language
- en
- Open access
- closed
- Locations
- Earth and Planetary Science Letters (publishedVersion)
- HAL (submittedVersion)
- Topics
- Physical Sciences › Earth and Planetary Sciences › Geochemistry and Petrology › Geological and Geochemical Analysis
- Physical Sciences › Earth and Planetary Sciences › Paleontology › Paleontology and Stratigraphy of Fossils
- Physical Sciences › Earth and Planetary Sciences › Geochemistry and Petrology › Geochemistry and Elemental Analysis
- Keywords
- iron(III), mantle redox state, subducted oceanic crust, magnetite, hydrothermal alteration, deep mantle, core-mantle interaction, photosynthesis, spinel, garnet, perovskite
About these checks
Registry, retraction, Cites and statistics results are computed, not judged, with one exception: a printed reference that no index lists is read once by a model before it counts as a citation error. Claims are extracted by a model and kept only when their quote appears verbatim in the text; each cited source is then checked, with a model’s help, for whether it says what the claim relies on. Those verdicts can be wrong — read the claim’s quote and the cited source before relying on one.
Statistics and arithmetic are recomputed, not judged.
Confidence bands are shown only for fields calibrated on our annotated test set. None is calibrated yet, so no band is shown.
What counts as a claim ›How we measure confidence ›How we check this ›
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