Cited by 127Paleontology and Stratigraphy of FossilsGeochemistry and Elemental AnalysisMarine and coastal ecosystems

Cobalt and marine redox evolution

Open access
Swanner, Elizabeth D., Planavsky, Noah J., Lalonde, Stefan V., Robbins, Leslie J., Bekker, Andrey, Rouxel, Olivier J., Saito, Mak A., Kappler, Andreas +2 more·2014·Earth and Planetary Science Letters

Integrity signals

Registry

Crossref · 10.1016/j.epsl.2014.01.001

Cites

121 of 121 references verified0 citation errors · 0 not checkable

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Claims the paper makes

We couldn’t retrieve this paper’s full text, so its claims and self-check weren’t run. The registry and citation checks still apply.

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?

  • Despite predicted decreases in seawater Co over time, biological utilization of Co is suggested to have increased over time and remains relatively high.

    “Despite the predicted decreases in the seawater concentration of Co over time, the biological utilization of Co is suggested to have increased over time, and remains relatively high”

    From Trace elements at the intersection of marine biological and geochemical evolution (2016) · cites this paper as Swanner et al., 2014

  • Pervasive anoxic conditions would help keep Co in solution, so the residence time of Co would be higher in more anoxic oceans compared to modern well-oxygenated oceans.

    “Pervasive anoxic conditions would help keep Co in solution, and as such the residence time of Co would be higher in more anoxic oceans compared to modern, welloxygenated oceans”

    From Trace elements at the intersection of marine biological and geochemical evolution (2016) · cites this paper as Swanner et al., 2014

  • This conclusion is indicated by a large increase in Co/Ti ratios in iron formations, euxinic shales, and pyrite relative to the evolving continental crust, with a peak at about 2.4 Ga.

    “This conclusion is indicated by a large increase in Co/Ti ratios in IF (Fig. 8), euxinic shales, and pyrite relative to the evolving continental crust, with a peak in Co/Ti values observed at ~2.4 Ga.”

    From Trace elements at the intersection of marine biological and geochemical evolution (2016) · cites this paper as Swanner et al., 2014

  • The expansion of the Co reservoir between 2.8 and 1.8 Ga may be coincident with increased mantle plume activity and associated hydrothermal inputs.

    “The expansion of the Co reservoir between 2.8 and 1.8 Ga (Fig. 8) may be coincident with increased mantle plume activity and associated hydrothermal inputs”

    From Trace elements at the intersection of marine biological and geochemical evolution (2016) · cites this paper as Swanner et al., 2014

  • An examination of Co concentrations in iron formations and pyrite through time suggests an expansion of the paleomarine Co reservoir between 2.8 and 1.8 Ga.

    “An examination of Co concentrations in IF and pyrite through time suggests an expansion of the paleomarine Co reservoir between 2.8 and 1.8 Ga”

    From Trace elements at the intersection of marine biological and geochemical evolution (2016) · cites this paper as Swanner et al., 2014

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Authors
Swanner, E. D., Planavsky, N. J., Lalonde, S. V., Robbins, L. J., Bekker, A., Rouxel, O. J., Saito, M. A., Kappler, A., Mojzsis, S. J., & Konhauser, K. O.
Affiliations
  • University of Tübingen (DE)
  • Yale University (US)
  • Institut Universitaire Européen de la Mer (FR)
  • University of Alberta (CA)
  • University of Manitoba (CA)
  • Ifremer (FR)
  • Woods Hole Oceanographic Institution (US)
  • Lyon 1 Université (FR)
Corresponding author
Swanner, Elizabeth D.
Venue
Earth and Planetary Science Letters
Publisher
Elsevier BV
Published
2014-03
Volume
390
Pages
253-263
ISSN
0012-821X (ISSN-L)
OpenAlex
W2109966375
Cited by
127
References
124
Citations by year
2026: 4 · 2025: 9 · 2024: 11 · 2023: 6 · 2022: 16 · 2021: 14 · 2020: 13 · 2019: 16 · 2018: 8 · 2017: 14 · 2016: 5 · 2015: 8 · 2014: 2
FWCI
7.06
Type
journal article
Language
en
Open access
Locations
  • Earth and Planetary Science Letters (publishedVersion)
  • HAL (submittedVersion, other-oa)
  • Institutional Archive of Ifremer (French Research Institute for Exploitation of the Sea) (submittedVersion)
Funders
  • National Science Foundation (NSF)
  • Deutsche Forschungsgemeinschaft (KA 1736/24-1)
  • NSF EAR-PF
  • NSF ELT
  • NSERC
  • LabexMER
  • Europole Mer
  • IFREMER
  • Gordon and Betty Moore Foundation
  • NSF
  • NASA's Astrobiology Institute Fund for International Cooperation
  • University of Colorado Center for Astrobiology
  • J.W. Fulbright Foundation
  • University of Colorado's Office of the Vice Chancellor for Research
  • Centre de Recherches Pétrographiques et Géochimiques (CRPG-Nancy)
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 › Oceanography › Marine and coastal ecosystems
Keywords
cobalt, iron-formation, authigenic pyrite, Precambrian oceans, oceanic anoxic events, trace elements in seawater

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Registry, retraction, Cites and statistics results are computed, not judged, with one exception: a printed reference that no index lists is read once by a model before it counts as a citation error. Claims are extracted by a model and kept only when their quote appears verbatim in the text; each cited source is then checked, with a model’s help, for whether it says what the claim relies on. Those verdicts can be wrong — read the claim’s quote and the cited source before relying on one.

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