Excitation band dependence of sulfur isotope mass-independent fractionation during photochemistry of sulfur dioxide using broadband light sources
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Mass-independent fractionation of sulfur isotopes is thought to originate from photolysis and/or photoexcitation of volcanogenic SO2 by ultraviolet light in an anoxic atmosphere.
“Mass-independent fractionation of sulfur isotopes (S-MIF) is thought to originate from the photolysis and/or photoexcitation of volcanogenic SO2 by ultraviolet light in an anoxic atmosphere (1, 20–23).”
From Rapid oxygenation of Earth’s atmosphere 2.33 billion years ago (2016) · cites this paper as [21]
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- Authors
- Whitehill, A. R., & Ono, S.
- Affiliations
- Massachusetts Institute of Technology (US)
- Corresponding author
- Whitehill, Andrew R.
- Venue
- Geochimica et Cosmochimica Acta
- Publisher
- Elsevier BV
- Published
- 2012-10
- Volume
- 94
- Pages
- 238-253
- ISSN
- 0016-7037 (ISSN-L)
- OpenAlex
- W1972590340
- Cited by
- 84
- References
- 82
- Citations by year
- 2026: 3 · 2025: 2 · 2024: 5 · 2023: 3 · 2022: 6 · 2021: 4 · 2020: 8 · 2019: 9 · 2018: 11 · 2017: 5 · 2016: 7 · 2015: 7 · 2014: 5 · 2013: 9
- FWCI
- 4.99
- 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 › Atmospheric Science › Atmospheric chemistry and aerosols
- Physical Sciences › Earth and Planetary Sciences › Geophysics › Geological and Geochemical Analysis
- Keywords
- UV photolysis, elemental sulfur, sulfur trioxide, stratospheric sulfate aerosols, mass-dependent fractionation, Archean atmosphere
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