Cobalt and marine redox evolution
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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
The Co/Ti trend shows an expansion of authigenic Co enrichments in iron formations between ~2.8 and 1.8 Ga.
“The Co/Ti trend shows an expansion of authigenic Co enrichments in iron formations between ~2.8-1.8Ga.”
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.
- ORCID
- 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
- green
- insu.hal.science
- Licence
- 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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