Cited by 615Paleontology and Stratigraphy of FossilsGeochemistry and Elemental AnalysisGeological and Geochemical Analysis

Evidence for oxygenic photosynthesis half a billion years before the Great Oxidation Event

Open access
Planavsky, Noah J., Asael, Dan, Hofmann, Axel, Reinhard, Christopher T., Lalonde, Stefan V., Knudsen, Andrew, Wang, Xiangli, Ossa Ossa, Frantz +8 more·2014·Nature Geoscience

Integrity signals

Registry

Crossref · 10.1038/ngeo2122

Cites

31 of 31 references verified0 citation errors · 0 not checkable

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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?

  • Fractionated iron and molybdenum isotopes and levels of redox-sensitive metals suggest marine photic zone O2 at 3.2 to 3.0 Ga ago.

    “Fractionated iron and molybdenum isotopes and levels of redox-sensitive metals suggest marine photic zone O2 (96–99).”

    From The Archean atmosphere (2020) · cites this paper as [97]

  • Petrographic, geochemical, sedimentological, and isotopic data suggest rapid and effective production, stabilization, and delivery of manganese mineral phases to sediments during deposition of the Sinqeni Formation.

    “Petrographic, geochemical, sedimentological, and isotopic data all suggest rapid and effective production, stabilization, and delivery of manganese mineral phases to sediments during the deposition of the Sinqeni Formation (Ossa Ossa et al. 2016, 2018;Planavsky et al. 2014).”

    From The History of Ocean Oxygenation (2022) · cites this paper as Planavsky et al. 2014

  • The most negative δ98Mo compositions observed in Archean sediments are consistent with the delivery of manganese-oxide phases to the sediments and thus imply appreciable dissolved O2 in surface-ocean environments.

    “The most negative δ 98 Mo compositions observed in Archean sediments are consistent with the delivery of manganese-oxide phases to the sediments and thus imply appreciable dissolved O 2 in surface-ocean environments.”

    From The History of Ocean Oxygenation (2022) · cites this paper as Planavsky et al. 2014

  • Oxygenic photosynthesis possibly originated by 3.0 Ga.

    “despite the possible origin of oxygenic photosynthesis by 3.0 Ga (13)”

Cites

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Research works printed but not linked: 1

  1. Hammerbeck, E. C. I. The Usushwana Complex in the Southeastern Transvaal with Special References to its Economic Potential Ph.D. thesis, Univ. Pretoria (1977)

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Authors
Planavsky, N. J., Asael, D., Hofmann, A., Reinhard, C. T., Lalonde, S. V., Knudsen, A., Wang, X., Ossa Ossa, F., Pecoits, E., Smith, A. J. B., Beukes, N. J., Bekker, A., Johnson, T. M., Konhauser, K. O., Lyons, T. W., & Rouxel, O. J.
Affiliations
  • Yale University (US)
  • Ifremer (FR)
  • University of Johannesburg (ZA)
  • California Institute of Technology (US)
  • Institut Universitaire Européen de la Mer (FR)
  • Lawrence University (US)
  • University of Illinois Urbana-Champaign (US)
  • University of California, Riverside (US)
  • University of Alberta (CA)
Corresponding author
Planavsky, Noah J.
Venue
Nature Geoscience
Published
2014-03-23
Volume
7
Issue
4
Pages
283-286
ISSN
  • 1752-0894 (ISSN-L)
  • 1752-0908
OpenAlex
W2045036940
Cited by
615
References
31
Citations by year
2026: 30 · 2025: 63 · 2024: 59 · 2023: 46 · 2022: 53 · 2021: 55 · 2020: 47 · 2019: 55 · 2018: 58 · 2017: 54 · 2016: 38 · 2015: 40 · 2014: 15
FWCI
35.78
Type
journal article
Language
en
Open access
Locations
  • Nature Geoscience (publishedVersion)
  • CaltechAUTHORS (California Institute of Technology) (submittedVersion)
  • HAL (submittedVersion, other-oa)
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 › Earth and Planetary Sciences › Geophysics › Geological and Geochemical Analysis
Keywords
oxygenic photosynthesis, Great Oxidation Event, molybdenum isotopes, manganese oxide, early Earth atmosphere, atmospheric oxygenation, Pongola Supergroup, evolution of photosynthesis

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