Cited by 90Paleontology and Stratigraphy of FossilsGeochemistry and Elemental AnalysisGeological and Geochemical Analysis

Manganese oxide shuttling in pre-GOE oceans – evidence from molybdenum and iron isotopes

Kurzweil, Florian, Wille, Martin, Gantert, Niklas, Beukes, Nicolas J., Schoenberg, Ronny·2016·Earth and Planetary Science Letters

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Crossref · 10.1016/j.epsl.2016.07.013

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65 of 65 references verified0 citation errors · 0 not checkable

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  • Similar geochemical signatures are observed in slightly younger Archean iron formations.

    “Similar geochemical signatures are also observed in slightly younger Archean iron formations (Kurzweil et al. 2016).”

    From The History of Ocean Oxygenation (2022) · cites this paper as Kurzweil et al. 2016

  • In the pre-GOE BIFs of the Transvaal Supergroup, Mn is only present in its divalent form in carbonate minerals and its concentration increases significantly stratigraphically upwards from the Kuruman to the Griquatown and Koegas IFs.

    “In the pre-GOE BIFs of the Transvaal Supergroup, Mn is only present in its divalent form in carbonate minerals and its concentration increases significantly stratigraphically upwards from the Kuruman to the Griquatown and Koegas IFs (Kurzweil et al., 2016; Oonk, 2017)”
  • Magnetite and Fe carbonates are the major iron minerals within the South African IFs.

    “Magnetite and Fe carbonates are the major iron minerals within the South African IFs (Beukes and Klein, 1990; Kurzweil et al., 2016).”
  • Manganese, deposited as discrete Mn-oxide layers in the stratigraphically younger Hotazel Formation, is incorporated entirely in iron carbonate minerals in both the Griquatown and Koegas IFs, where its bulk-rock abundance locally reaches percent levels.

    “Manganese - deposited as discrete Mnoxide layers in the stratigraphically younger Hotazel Formation - is incorporated entirely in iron carbonate minerals in both the Griquatown and Koegas IFs, where its bulk-rock abundance locally reaches percent levels (Tsikos and Moore, 1997; Johnson et al., 2016; Kurzweil et al., 2016).”

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Authors
Kurzweil, F., Wille, M., Gantert, N., Beukes, N. J., & Schoenberg, R.
Affiliations
  • University of Cologne (DE)
  • University of Tübingen (DE)
  • University of Johannesburg (ZA)
Corresponding author
Kurzweil, Florian
Venue
Earth and Planetary Science Letters
Publisher
Elsevier BV
Published
2016-10
Volume
452
Pages
69-78
ISSN
0012-821X (ISSN-L)
OpenAlex
W2515532999
Cited by
90
References
65
Citations by year
2026: 3 · 2025: 11 · 2024: 8 · 2023: 3 · 2022: 4 · 2021: 16 · 2020: 11 · 2019: 15 · 2018: 13 · 2017: 6
FWCI
9.44
Type
journal article
Language
en
Open access
closed
Locations
  • Earth and Planetary Science Letters (publishedVersion)
  • Kölner Universitäts PublikationsServer (Universität zu Köln) (publishedVersion)
  • BORIS (University Library Bern) (submittedVersion)
Funders
  • German Research Foundation (WI3870/2-1)
  • Carl Zeiss Foundation
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
Great Oxidation Event, molybdenum isotopes, iron isotopes, redox stratification, Fe(II) oxidation, iron-formation, Paleoproterozoic, sediment pore water

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