Spatial variability in oceanic redox structure 1.8 billion years ago
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Speciation of iron-bearing minerals in marginal siliciclastic sedimentary rocks suggests that anoxic bottom waters were common on shelf and slope environments but were buffered by dissolved Fe2+ rather than hydrogen sulfide, termed ferruginous conditions.
“The speciation of iron-bearing minerals in marginal siliciclastic sedimentary rocks (Guilbaud et al. 2015, Planavsky et al. 2011, Poulton et al. 2010, Sperling et al. 2015) suggests that anoxic bottom waters were common on shelf and slope environments but were buffered by dissolved Fe 2+ rather than hydrogen sulfide (termed ferruginous conditions).”
From The History of Ocean Oxygenation (2022) · cites this paper as Poulton et al. 2010
All available data that constrain the marine landscape in the mid-Proterozoic ocean are consistent with only locally developed euxinic conditions along productive continental margins or within intracratonic basins.
“All available data that constrain the marine landscape in the midProterozoic ocean are consistent with only locally developed euxinic conditions along productive continental margins (e.g., in oxygen-minimum zones) or within intracratonic basins”
From Iron formations: A global record of Neoarchaean to Palaeoproterozoic environmental history (2017) · cites this paper as Poulton et al., 2010
Studies of ancient environments have shown basin-scale differences in water column chemistry due to stratification with depth or proximity to shoreline.
“Further, studies of ancient environments have already shown that there can be basin scale differences in water column chemistry that as the result of stratification with depth or proximity to shoreline (e.g., Poulton et al., 2010).”
From Trace elements at the intersection of marine biological and geochemical evolution (2016) · cites this paper as Poulton et al., 2010
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Controls on the evolution of Ediacaran metazoan ecosystems: A redox perspective
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Searching for an oxygenation event in the fossiliferous Ediacaran of northwestern Canada
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Earth’s Great Oxidation Event facilitated by the rise of sedimentary phosphorus recycling
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Self-citationThe History of Ocean Oxygenation
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- Authors
- Poulton, S. W., Fralick, P. W., & Canfield, D. E.
- Affiliations
- Newcastle University (GB)
- Lakehead University (CA)
- University of Southern Denmark (DK)
- Corresponding author
- Poulton, Simon W.
- Venue
- Nature Geoscience
- Published
- 2010-06-20
- Volume
- 3
- Issue
- 7
- Pages
- 486-490
- ISSN
- 1752-0894 (ISSN-L)
- 1752-0908
- OpenAlex
- W1506354302
- Cited by
- 406
- References
- 31
- Citations by year
- 2026: 14 · 2025: 26 · 2024: 19 · 2023: 21 · 2022: 29 · 2021: 37 · 2020: 34 · 2019: 21 · 2018: 35 · 2017: 22 · 2016: 24 · 2015: 32 · 2014: 21 · 2013: 29 · 2012: 21
- FWCI
- 16.02
- Type
- journal article
- Language
- en
- Open access
- green
- doi.org
- Licence
- www.springer.com/tdm (tdm)
- Locations
- Nature Geoscience (publishedVersion)
- University of Southern Denmark Research Portal (University of Southern Denmark) (publishedVersion)
- Newcastle University ePrints (Newcastle Univesity)
- Funders
- Minnesota Department of Natural Resources
- Natural Environment Research Council
- 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
- iron-formation, euxinia, pyrite precipitation, dissolved iron, sulfide, eukaryotic evolution, Precambrian, paleoshorelines
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