Cited by 147Paleontology and Stratigraphy of FossilsGeological and Geochemical AnalysisGeological formations and processes

Evidence for Paleoproterozoic cap carbonates in North America

BEKKER, A, KAUFMAN, A, KARHU, J, ERIKSSON, K·2005·Precambrian Research

Integrity signals

Registry

Crossref · 10.1016/j.precamres.2005.03.009

Cites

9 of 9 references verified0 citation errors · 0 not checkable

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  • A wide range of observations from Earth's rock record indicate a transition to a more oxidizing Earth surface environment after approximately 2.3 Gya, the Great Oxidation Event.

    “A wide range of observations from Earth's rock record indicate a transition to a more oxidizing Earth surface environment after ∼2.3 Gya-the Great Oxidation Event (Bekker et al. 2005 and references therein).”

    From The History of Ocean Oxygenation (2022) · cites this paper as Bekker et al. 2005

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Authors
BEKKER, A., KAUFMAN, A., KARHU, J., & ERIKSSON, K.
Affiliations
  • Harvard University (US)
  • University of Maryland, College Park (US)
  • University of Helsinki (FI)
  • Virginia Tech (US)
Corresponding author
BEKKER, A
Venue
Precambrian Research
Publisher
Elsevier BV
Published
2005-06-30
Volume
137
Issue
3-4
Pages
167-206
ISSN
0301-9268 (ISSN-L)
OpenAlex
W2114547434
Cited by
147
References
9
Citations by year
2026: 3 · 2025: 4 · 2024: 6 · 2023: 6 · 2022: 5 · 2021: 8 · 2020: 5 · 2019: 4 · 2018: 7 · 2017: 5 · 2016: 10 · 2015: 8 · 2014: 10 · 2013: 12 · 2012: 12
FWCI
5.46
Type
journal article
Language
en
Open access
closed
Locations
Precambrian Research (publishedVersion)
Funders
  • National Science Foundation
  • National Aeronautics and Space Administration
Topics
  • Physical Sciences › Earth and Planetary Sciences › Paleontology › Paleontology and Stratigraphy of Fossils
  • Physical Sciences › Earth and Planetary Sciences › Geophysics › Geological and Geochemical Analysis
  • Physical Sciences › Earth and Planetary Sciences › Earth-Surface Processes › Geological formations and processes
Keywords
Huronian Supergroup, glacial diamictites, carbon isotopes, oxygen isotopes, carbonate recrystallization, postglacial transgression, carbonate alkalinity, atmospheric oxygen rise, methane oxidation, greenhouse gases, Neoproterozoic glaciation

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