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Evidence for oxygenic photosynthesis half a billion years before the Great Oxidation Event
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In the citing paper
“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]
In the citing paper
“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
In the citing paper
“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
In the citing paper
“despite the possible origin of oxygenic photosynthesis by 3.0 Ga (13)”
From Disequilibrium biosignatures over Earth history and implications for detecting exoplanet life (2018) · cites this paper as [13]
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“0 Ga (Crowe et al., 2013; Planavsky et al., 2014) – the 1st study arguing for the presence of atmospheric oxygen”
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“Environmental differences include a greater flux of nutrients, in particular trace metals and phosphorus, that were liberated during weathering (Crowe et al., 2013; Planavsky et al., 2014; Satkoski et al., 2016) and were thus perhaps more bioavailable in freshwater.”
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Planktonic marine iron-oxidizers drive iron mineralization under low oxygen conditions
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“There is also mounting evidence that oxygen was present prior to the GOE, as early as 3.0–3.2 Gya (Crowe et al., 2013; Lyons et al., 2014; Planavsky et al., 2014; Satkoski et al., 2015), initially in oases in which oxygen concentrations have been modeled to be ~1–10 lM O2 (Olson et al., 2013;…”
BackgroundInfluentialArchean to early Paleoproterozoic iron formations document a transition in iron oxidation mechanisms
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Metadata
- 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.
- ORCID
- Venue
- Nature Geoscience
- Published
- 2014-03-23
- Volume
- 7
- Issue
- 4
- Pages
- 283-286
- ISSN
- 1752-0894 (ISSN-L)
- 1752-0908
- OpenAlex
- W2045036940
- Semantic Scholar
- 428b0233112c8b5ca3ca7f0f4086ffb7f2356ce3
- 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
- green
- insu.hal.science
- Licence
- other-oa
- www.springer.com/tdm (tdm)
- 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 › Geochemistry and Petrology › 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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