Cited by 306Paleontology and Stratigraphy of FossilsGeochemistry and Elemental AnalysisOrigins and Evolution of Life

Photo-oxidation of hydrated Fe2+—significance for banded iron formations

Braterman, Paul S., Cairns-Smith, A. Graham, Sloper, Robert W.·1983·Nature

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Crossref · 10.1038/303163a0

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17 of 17 references verified0 citation errors · 0 not checkable

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  • Dissolved ferrous iron species, such as Fe2+ or Fe(OH)+, absorb radiation in the 200-400 nm range, leading to photochemical formation of dissolved ferric iron, which hydrolyses to form Fe(III)-oxyhydroxides at circumneutral pH.

    “Under such conditions, dissolved ferrous iron species, such as Fe 2+ or Fe(OH) + , absorb radiation in the 200-400 nm range, leading to the photochemical formation of dissolved ferric iron [reaction 1], which in turn, hydrolyses to form Fe(III)-oxyhydroxides at circumneutral pH (Cairns-Smith, 1978; Braterman et al., 1983; Anbar and Holland, 1992).”

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Authors
Braterman, P. S., Cairns-Smith, A. G., & Sloper, R. W.
Affiliations
University of Glasgow (GB)
Venue
Nature
Published
1983-05
Volume
303
Issue
5913
Pages
163-164
ISSN
  • 0028-0836 (ISSN-L)
  • 1476-4687
OpenAlex
W2039687431
Cited by
306
References
17
Citations by year
2026: 9 · 2025: 12 · 2024: 15 · 2023: 5 · 2022: 11 · 2021: 11 · 2020: 9 · 2019: 9 · 2018: 3 · 2017: 11 · 2016: 12 · 2015: 9 · 2014: 11 · 2013: 19 · 2012: 8
FWCI
10.32
Type
journal article
Language
en
Open access
closed
Locations
Nature (publishedVersion)
Topics
  • 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
  • Physical Sciences › Physics and Astronomy › Astronomy and Astrophysics › Origins and Evolution of Life
Keywords
banded iron formations, photooxidation, ferrous iron, Fe(OH)2, iron precipitation, UV photolysis, Precambrian atmosphere, iron ore formation

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