Ventilation of CO2 from a reduced mantle and consequences for the early Martian greenhouse
Integrity signals
Registry
Cites
Statistics
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?
During later events such as the formation of the Tharsis bulge, 40 mbar to 1.4 bars of CO2 could have been outgassed.
“During later events (such as the formation of the Tharsis bulge), they estimate that 40 mbar to 1.4 bars could have been outgassed.”
From The Climate of Early Mars (2016) · cites this paper as Hirschmann & Withers 2008
Between 70 mbar and 13 bar of CO2 could have been outgassed during the initial formation of the Martian crust, with the lower estimate for the most reducing conditions.
“Given this, Hirschmann & Withers (2008) estimate that between 70 mbar and 13 bar of CO 2 could have been outgassed during the initial formation of the Martian crust, with the lower estimate for the most reducing conditions.”
From The Climate of Early Mars (2016) · cites this paper as Hirschmann & Withers 2008
A high atmospheric CO2 content required for CO2-H2 warming may be inconsistent with a highly reducing mantle.
“It also requires a high atmospheric CO 2 content, which as discussed in Section 3.1 may be inconsistent with a highly reducing mantle (Hirschmann & Withers 2008).”
From The Climate of Early Mars (2016) · cites this paper as Hirschmann & Withers 2008
The citation lists haven’t been fetched yet
References 98 · Cited by 131
- Authors
- Hirschmann, M. M., & Withers, A. C.
- Affiliations
- University of Minnesota (US)
- Corresponding author
- Hirschmann, Marc M.
- Venue
- Earth and Planetary Science Letters
- Publisher
- Elsevier BV
- Published
- 2008-06
- Volume
- 270
- Issue
- 1-2
- Pages
- 147-155
- ISSN
- 0012-821X (ISSN-L)
- OpenAlex
- W2082336068
- Cited by
- 131
- References
- 98
- Citations by year
- 2026: 3 · 2025: 3 · 2024: 10 · 2023: 3 · 2022: 8 · 2021: 10 · 2020: 4 · 2019: 8 · 2018: 8 · 2017: 9 · 2016: 8 · 2015: 7 · 2014: 7 · 2013: 13 · 2012: 14
- FWCI
- 2.96
- Type
- journal article
- Language
- en
- Open access
- closed
- Locations
- Earth and Planetary Science Letters (publishedVersion)
- Funders
- National Science Foundation
- National Aeronautics and Space Administration
- Topics
- Physical Sciences › Physics and Astronomy › Astronomy and Astrophysics › Planetary Science and Exploration
- Physical Sciences › Physics and Astronomy › Astronomy and Astrophysics › Astro and Planetary Science
- Physical Sciences › Earth and Planetary Sciences › Geophysics › Geological and Geochemical Analysis
- Keywords
- Martian mantle, oxygen fugacity, iron-wüstite buffer, graphite, CO2 degassing, greenhouse, Martian basalts, partial melting, magma ocean, diamond, Martian crust, liquid water on Mars, CO2 solubility
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 ›
Are you an author, or do you see a problem with this page? Request a review
