The DOI matches its Crossref record; 25 of the 25 references it cites were found in a registry or an index.
Water and the Oxidation State of Subduction Zone Magmas
Open accessAbstract
Tracing Mantle Oxidation: The chemical composition of the Earth's mantle varies with tectonic setting. For example, basaltic melts near subduction zones are more oxidized than magma near divergent plate boundaries. Kelley and Cottrell (p. 605 ; see the Perspective by Hirschmann ) examined melts formed in different tectonic environments, using highly sensitive synchrotron-based analytical methods. The oxidation state of Fe increased with water content and mobile trace elements concentrations. Thus, fluids released from wet subducting plates drive mantle oxidation above subduction zones, which may help to explain the spatial differences in oxygen fugacity of the mantle.
Overview
The claims and statistics of this paper haven’t been checked yet.
Run the check — free, no account needed. It reads the open-access text and checks the sources it cites.
Integrity signals
Registry
Cites
Statistics
Verification
Claims the paper makes
The claims and statistics of this paper haven’t been checked yet.
Run the check — free, no account needed. It reads the open-access text and checks the sources it cites.
Self-check
Percentages, sums and reported differences re-computed from the paper’s own numbers.
The self-check needs the paper’s full text.
Citations
Cites
Kessel, R., Schmidt, M. W., Ulmer, P., & Pettke, T. (2005) · Nature · doi:10.1038/nature03971 · Cited by 1,436
Kress, V. C., & Carmichael, I. S. E. (1991) · Contributions to Mineralogy and Petrology · doi:10.1007/bf00307328 · Cited by 1,155
Wallace, P. J. (2005) · Journal of Volcanology and Geothermal Research · doi:10.1016/j.jvolgeores.2004.07.023 · Cited by 1,053
The chemistry of subduction-zone fluids
MANNING, C. (2004) · Earth and Planetary Science Letters · doi:10.1016/j.epsl.2004.04.030 · Cited by 850
Dehydration and melting experiments constrain the fate of subducted sediments
Johnson, M. C., & Plank, T. (2000) · Geochemistry, Geophysics, Geosystems · doi:10.1029/1999gc000014 · Cited by 844
The role of water in the petrogenesis of Mariana trough magmas
Stolper, E., & Newman, S. (1994) · Earth and Planetary Science Letters · doi:10.1016/0012-821x(94)90074-4 · Cited by 768
The influence of water on melting of mantle peridotite
Gaetani, G. A., & Grove, T. L. (1998) · Contributions to Mineralogy and Petrology · doi:10.1007/s004100050396 · Cited by 737
The redox state of subduction zones: insights from arc-peridotites
Parkinson, I. J., & Arculus, R. J. (1999) · Chemical Geology · doi:10.1016/s0009-2541(99)00110-2 · Cited by 527
Reduction of CO2 during serpentinization of olivine at 300 °C and 500 bar
Berndt, M. E., Allen, D. E., & Seyfried, W. E. (1996) · Geology · doi:10.1130/0091-7613(1996)024<0351:rocdso>2.3.co;2 · Cited by 523
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 514
Cited by
Origin and evolution of the atmospheres of early Venus, Earth and Mars
Lammer, H., Zerkle, A. L., Gebauer, S., Tosi, N., Noack, L., Scherf, M., Pilat-Lohinger, E., Güdel, M., Grenfell, J. L., Godolt, M., et al. (2018) · The Astronomy and Astrophysics Review · doi:10.1007/s00159-018-0108-y · Cited by 202
Nitrogen speciation in upper mantle fluids and the origin of Earth's nitrogen-rich atmosphere
Mikhail, S., & Sverjensky, D. A. (2014) · Nature Geoscience · doi:10.1038/ngeo2271 · Cited by 185
A record of deep-ocean dissolved O2 from the oxidation state of iron in submarine basalts
Stolper, D. A., & Keller, C. B. (2018) · Nature · doi:10.1038/nature25009 · Cited by 173
Highly oxidising fluids generated during serpentinite breakdown in subduction zones
Debret, B., & Sverjensky, D. A. (2017) · Scientific Reports · doi:10.1038/s41598-017-09626-y · Cited by 165
A hydrogen-based oxidation mechanism relevant to planetary formation
Sharp, Z. D., McCubbin, F. M., & Shearer, C. K. (2013) · Earth and Planetary Science Letters · doi:10.1016/j.epsl.2013.08.015 · Cited by 147
Metadata
- Authors
- Kelley, K. A., & Cottrell, E.
- Venue
- Science
- Published
- 2009-07-31
- Volume
- 325
- Issue
- 5940
- Pages
- 605-607
- ISSN
- 0036-8075 (ISSN-L)
- 1095-9203
- OpenAlex
- W2111173087
- Cited by
- 893
- References
- 25
- FWCI
- 20.28
- Type
- journal article
- Language
- en
- Open access
- green
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
How to cite
Cite CoChat for the checks on this page, and the paper for its own findings.
- This page
- CoChat. (2026). Citation check: Water and the Oxidation State of Subduction Zone Magmas. https://app.cochat.ai/papers/10.1126/science.1174156
- The paper
- Kelley, K. A., & Cottrell, E. (2009). Water and the Oxidation State of Subduction Zone Magmas. Science. https://doi.org/10.1126/science.1174156
Data sources
Bibliographic data: Semantic Scholar, OpenAlex, Crossref.
Contains information from the Semantic Scholar Academic Graph Datasets, made available under the ODC Attribution License (ODC-BY 1.0).
Semantic Scholar’s data is described in: Kinney, R., et al. (2023). The Semantic Scholar Open Data Platform. arXiv:2301.10140.
