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The Neoproterozoic oxygenation event: Environmental perturbations and biogeochemical cycling
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“The pattern of stable, likely intermediate levels of atmospheric O2 during the boring billion stands in contrast to the dramatic rising and falling levels that characterized the preceding GOE and the Neoproterozoic Oxidation Event (NOE; Och and Shields-Zhou, 2012) that followed (Fig. 3; reviewed in Lyons et al., 2014).”
From Oxygenation, Life, and the Planetary System during Earth's Middle History: An Overview (2021) · cites this paper as Och and Shields-Zhou, 2012
Citations
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Metadata
- Authors
- Och, L. M., & Shields-Zhou, G. A.
- Affiliations
- University College London (GB)
- Corresponding author
- Och, Lawrence M.
- ORCID
- Och, Lawrence M.
- Venue
- Earth-Science Reviews
- Publisher
- Elsevier BV
- Published
- 2012-01
- Volume
- 110
- Issue
- 1-4
- Pages
- 26-57
- ISSN
- 0012-8252 (ISSN-L)
- OpenAlex
- W1979315982
- Cited by
- 646
- References
- 660
- Citations by year
- 2026: 44 · 2025: 75 · 2024: 66 · 2023: 52 · 2022: 55 · 2021: 50 · 2020: 51 · 2019: 55 · 2018: 45 · 2017: 32 · 2016: 34 · 2015: 37 · 2014: 23 · 2013: 21 · 2012: 6
- FWCI
- 11.12
- Type
- journal article
- Language
- en
- Open access
- closed
- Locations
- Earth-Science Reviews (publishedVersion)
- UCL Discovery (University College London) (submittedVersion)
- Funders
- Deutsche Forschungsgemeinschaft
- Alexander von Humboldt-Stiftung
- Topics
- Physical Sciences › Earth and Planetary Sciences › Paleontology › Paleontology and Stratigraphy of Fossils
- Physical Sciences › Earth and Planetary Sciences › Geochemistry and Petrology › Geological and Geochemical Analysis
- Physical Sciences › Earth and Planetary Sciences › Geochemistry and Petrology › Geochemistry and Elemental Analysis
- Keywords
- Neoproterozoic Oxygenation Event, Great Oxidation Event, atmospheric oxygenation, Ediacaran biota, Cambrian explosion, carbon isotope stratigraphy, sulfur isotope fractionation, strontium isotopes, continental weathering, sulfur cycling, pyrite burial, molybdenum enrichment, redox-sensitive trace metals, Rodinia breakup, Precambrian-Cambrian transition, organic carbon burial, biogeochemical cycles
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