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Regulation of atmospheric oxygen during the Proterozoic
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“As a result, there is widespread agreement that the most effective mechanism for stabilizing low atmospheric O2 is reducing global rates of biospheric productivity (Laakso and Schrag, 2014; Derry, 2015; Reinhard et al., 2017a).”
From Oxygenation, Life, and the Planetary System during Earth's Middle History: An Overview (2021) · cites this paper as Laakso and Schrag, 2014
In the citing paper
“For example, it is widely accepted that a decrease in atmospheric O2 levels should, in general, lead to an increase in organic matter burial (and thus O2 release), while also leading to a decrease in organic matter weathering and thus reduced O2 consumption (Laakso and Schrag, 2014).”
From Oxygenation, Life, and the Planetary System during Earth's Middle History: An Overview (2021) · cites this paper as Laakso and Schrag, 2014
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Metadata
- Authors
- Laakso, T. A., & Schrag, D. P.
- Affiliations
- Harvard University (US)
- Corresponding author
- Laakso, Thomas A.
- Venue
- Earth and Planetary Science Letters
- Publisher
- Elsevier BV
- Published
- 2014-02
- Volume
- 388
- Pages
- 81-91
- ISSN
- 0012-821X (ISSN-L)
- OpenAlex
- W2058786960
- Cited by
- 159
- References
- 84
- Citations by year
- 2026: 5 · 2025: 5 · 2024: 12 · 2023: 9 · 2022: 19 · 2021: 14 · 2020: 16 · 2019: 19 · 2018: 22 · 2017: 14 · 2016: 10 · 2015: 11 · 2014: 3
- FWCI
- 5.44
- Type
- journal article
- Language
- en
- Open access
- closed
- Locations
- Earth and Planetary Science Letters (publishedVersion)
- Funders
- National Aeronautics and Space Administration (NNX11AP89H)
- Topics
- Physical Sciences › Earth and Planetary Sciences › Paleontology › Paleontology and Stratigraphy of Fossils
- Physical Sciences › Environmental Science › Global and Planetary Change › Earth Systems and Cosmic Evolution
- Physical Sciences › Earth and Planetary Sciences › Geochemistry and Petrology › Geological and Geochemical Analysis
- Keywords
- atmospheric oxygen, Proterozoic, Great Oxidation Event, Neoproterozoic, phosphorus flux, phosphate scavenging, carbon cycle, sulfur cycling, iron cycle, biogeochemical feedbacks, stable equilibrium, paleo-oxygenation
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