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.
“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]
Only 1 to 2% of H2 production is due to serpentinization; the remaining 10 to 11% is from oxidation by sulfate, which does not generate H2.
“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]
Today, magma emplacement from ridges, arcs, and plumes is 5.7 × 1013 kg/year.
“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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- 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 › Geophysics › 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
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