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Volcanic gases, black smokers, and the great oxidation event
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In the citing paper
“The Great Oxidation Event (GOE) thus began, which ended ~2.1 to 2.0 Ga ago (9, 10).”
From The Archean atmosphere (2020) · cites this paper as [9]
In the citing paper
“These O2 levels would have only been attained when the O2 flux from the burial of organic carbon exceeded the kinetically efficient sink from O2-consuming gases (CO, H2, H2S, and SO2) from volcanism and metamorphism plus fluxes of reducing cations such as Fe2+ from seafloor vents (9, 120, 121, 123, 124).”
From The Archean atmosphere (2020) · cites this paper as [9]
In the citing paper
“Hypotheses for a slowly decreasing O2 sink to the GOE tipping point rely on a decline in the ratio of reduced-to-oxidized species from volcanic, metamorphic, and hydrothermal sources (9, 123, 124, 133, 134).”
From The Archean atmosphere (2020) · cites this paper as [9]
In the citing paper
“Thus the ca. 2.22-2.10 Ga Lomagundi carbon isotope excursion may, together with the Cr enrichment and Cu isotope changes in early Palaeoproterozoic sediments, be a manifestation of acid-driven dissolution and the first sedimentary cycle of oxidative weathering (Holland, 2002; Bekker and Holland, 2012).”
From Iron formations: A global record of Neoarchaean to Palaeoproterozoic environmental history (2017) · cites this paper as Holland, 2002
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Edwards, C. T., Pufahl, P. K., Hiatt, E. E., & Kyser, T. K. (2012) · Precambrian Research · doi:10.1016/j.precamres.2012.04.020 · Cited by 29
Metadata
- Authors
- Holland, H. D.
- Affiliations
- Harvard University (US)
- Corresponding author
- Holland, Heinrich D.
- Venue
- Geochimica et Cosmochimica Acta
- Publisher
- Elsevier BV
- Published
- 2002-11
- Volume
- 66
- Issue
- 21
- Pages
- 3811-3826
- ISSN
- 0016-7037 (ISSN-L)
- OpenAlex
- W2165303310
- Cited by
- 920
- References
- 63
- Citations by year
- 2026: 36 · 2025: 58 · 2024: 52 · 2023: 63 · 2022: 57 · 2021: 58 · 2020: 60 · 2019: 48 · 2018: 52 · 2017: 42 · 2016: 31 · 2015: 34 · 2014: 33 · 2013: 48 · 2012: 35
- FWCI
- 22.32
- Type
- journal article
- Language
- en
- Open access
- closed
- Locations
- Geochimica et Cosmochimica Acta (publishedVersion)
- Topics
- Physical Sciences › Earth and Planetary Sciences › Paleontology › Paleontology and Stratigraphy of Fossils
- Physical Sciences › Earth and Planetary Sciences › Geochemistry and Petrology › Geological and Geochemical Analysis
- Physical Sciences › Earth and Planetary Sciences › Geochemistry and Petrology › Geochemistry and Elemental Analysis
- Keywords
- Great Oxidation Event, volcanic gases, black smokers, atmospheric oxygenation, early Earth atmosphere, sulfur gases, pyrite, organic matter production, Archean, Proterozoic
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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.
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