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Oxygenation history of the Neoproterozoic to early Phanerozoic and the rise of land plants
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“The apparent expansion of well-oxygenated ocean conditions correlates temporally with the rise of vascular land plants, and specifically with putative increases in the depth and intensity of rooting in terrestrial ecosystems (e.g., Wallace et al. 2017).”
From The History of Ocean Oxygenation (2022) · cites this paper as Wallace et al. 2017
In the citing paper
“Specifically, combined evidence from local (Sperling et al. 2015), regional (Lu et al. 2018, Wallace et al. 2017), and global (Dahl et al. 2019, Wei et al. 2020) redox proxies suggests extensive anoxia during the Cambrian (∼541-485 Mya), Ordovician (∼485-444 Mya), and Silurian (∼444-420 Mya).”
From The History of Ocean Oxygenation (2022) · cites this paper as Wallace et al. 2017
Citations
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Metadata
- Authors
- Wallace, M. W., Hood, A. V., Shuster, A., Greig, A., Planavsky, N. J., & Reed, C. P.
- Affiliations
- The University of Melbourne (AU)
- Yale University (US)
- Corresponding author
- Wallace, Malcolm W.
- Venue
- Earth and Planetary Science Letters
- Publisher
- Elsevier BV
- Published
- 2017-05
- Volume
- 466
- Pages
- 12-19
- ISSN
- 0012-821X (ISSN-L)
- OpenAlex
- W2595024260
- Cited by
- 299
- References
- 53
- Citations by year
- 2026: 24 · 2025: 31 · 2024: 42 · 2023: 30 · 2022: 48 · 2021: 36 · 2020: 23 · 2019: 26 · 2018: 35 · 2017: 4
- FWCI
- 17.17
- Type
- journal article
- Language
- en
- Open access
- closed
- Locations
- Earth and Planetary Science Letters (publishedVersion)
- Funders
- ARC (DP130102240)
- NAI
- NSF-ELT
- Alternative Earths NASA Astrobiology Institute
- 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 › Environmental Science › Global and Planetary Change › Earth Systems and Cosmic Evolution
- Keywords
- Neoproterozoic, land plant evolution, cerium anomaly, rare earth elements, marine carbonates, marine redox conditions, ocean anoxia, Ediacaran, Cambrian, Devonian, Late Devonian, marine cements, atmospheric oxygen
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