The DOI matches its Crossref record; 66 of the 66 references it cites were found in a registry or an index.
Long-term fluxes and budget of ferric iron: implication for the redox states of the Earth's mantle and atmosphere
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Claims the paper makes
Claims other papers make about this one
Each is checked against this paper’s own text: does it say what the citing paper says it does?
In the citing paper
“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]
Citations
Cites
(1985) · Academic Commons (Stony Brook University) · Cited by 12,330
(1985) · Academic Commons (Stony Brook University) · Cited by 11,328
Orogenic Andesites and Plate Tectonics
Gill, J. B. (1981) · Minerals and rocks · doi:10.1007/978-3-642-68012-0 · Cited by 3,593
The Chemical Evolution of the Atmosphere and Oceans
Holland, H. D. (1984) · doi:10.1515/9780691220239 · Cited by 1,836
Large igneous provinces: Crustal structure, dimensions, and external consequences
Coffin, M. F., & Eldholm, O. (1994) · Reviews of Geophysics · doi:10.1029/93rg02508 · Cited by 1,538
Sedimentary Rocks and Crustal Evolution: Tectonic Setting and Secular Trends
McLennan, S. M., & Taylor, S. R. (1991) · The Journal of Geology · doi:10.1086/629470 · Cited by 861
David, C., Wong, T.-F., Zhu, W., & Zhang, J. (1994) · Pure and Applied Geophysics · doi:10.1007/bf00874337 · Cited by 684
Leffmann, H. (1920) · Journal of the Franklin Institute · doi:10.1016/s0016-0032(20)90415-5 · Cited by 668
Origin of diamonds in old enriched mantle
Richardson, S. H., Gurney, J. J., Erlank, A. J., & Harris, J. W. (1984) · Nature · doi:10.1038/310198a0 · Cited by 646
Mantle Oxidation State and Its Relationship to Tectonic Environment and Fluid Speciation
Wood, B. J., Bryndzia, L. T., & Johnson, K. E. (1990) · Science · doi:10.1126/science.248.4953.337 · Cited by 517
Research works printed but not linked: 3
- Ronov, 1976, A new model for the chemical structure of the Earth's crust, Geochem. Int., 13, 89
- H.D. Holland, The Chemistry of Atmosphere and Oceans, Wiley, New York, 1978, 351 pp.
- J. Hoefs, Isotope geochemistry of carbon, in: H.-L. Schmidt, H. Forstel, K. Heinzinger (Eds.), Stable Isotopes, Elsevier, Amsterdam, 1982, pp. 103–113.
Cited by
Sorted by citations
The Redox State of Earth's Mantle
Frost, D. J., & McCammon, C. A. (2008) · Annual Review of Earth and Planetary Sciences · doi:10.1146/annurev.earth.36.031207.124322 · Cited by 1,134
THE EARLY HISTORY OF ATMOSPHERIC OXYGEN: Homage to Robert M. Garrels
Canfield, D. E. (2005) · Annual Review of Earth and Planetary Sciences · doi:10.1146/annurev.earth.33.092203.122711 · Cited by 1,032
Water and the Oxidation State of Subduction Zone Magmas
Kelley, K. A., & Cottrell, E. (2009) · Science · doi:10.1126/science.1174156 · Cited by 896
Extreme Water Loss and Abiotic O 2 Buildup on Planets Throughout the Habitable Zones of M Dwarfs
Luger, R., & Barnes, R. (2015) · Astrobiology · doi:10.1089/ast.2014.1231 · Cited by 585
Evolution of a Habitable Planet
Kasting, J. F., & Catling, D. C. (2003) · Annual Review of Astronomy and Astrophysics · doi:10.1146/annurev.astro.41.071601.170049 · Cited by 566
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.
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