A Whiff of Oxygen Before the Great Oxidation Event?
By A. Anbar, Y. Duan, T. Lyons, G. L. Arnold, B. Kendall, R. Creaser, A. J. Kaufman, G. Gordon, C. Scott, J. Garvin and 1 more. Science, 2007
905 citations recorded by the source corpus.
Subfields: Artificial Intelligence, Geochemistry and Petrology, Paleontology
View Paper: https://www.semanticscholar.org/paper/a8de5e39edde5e57b564bab620dc9f252f2ef192
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In Artificial Intelligence
In Geochemistry and Petrology
In Paleontology
- R. Summons
- Andrew H. Knoll
- P. Sánchez‐Baracaldo
- N. Arndt
- Euan G. Nisbet
- A. Kappler
- E. Roden
- N. Butterfield
Citations in the corpus
- Microbiological processes in banded iron formation deposition (2013, background): “They are not abundant in fluvial systems younger than 2 3 Ga. 2 High-resolution chemostratigraphy reveals an episode of enrichment of the redox-sensitive transition metals molybdenum and rhenium in the 2 5 Ga Mount McRae Shale in Western Australia (Anbar et al., 2007).”
- Biological Fe oxidation controlled deposition of banded iron formation in the ca. 3770 Ma Isua Supracrustal Belt (West Greenland) (2013, background): “45 Ga based on geochemical and biomarker evidence (e.g., Brocks et al., 1999; Anbar et al., 2007; Kaufman et al., 2007; Eigenbrode et al., 2008; Waldbauer et al., 2009; Kendall et al., 2010; Czaja et al., 2012; Stüeken et al., 2012).”
- Rapid, direct and non-destructive assessment of fossil organic matter via microRaman spectroscopy (2016, methodology): “Such flexibility is particularly of interest for its application to detection and characterization of organic matter were sample preservation is essential, such as for organic fossils, both in terrestrial and - potentially - extraterrestrial samples [4-6].”
- Cyanobacterial evolution during the Precambrian (2016, background): “…and rhenium (Re) in * 2.5 Ga sediments have provided evidence for localized oxidative weathering (also known as ‘ whiffs of oxygen ’ ) before the GOE (Anbar et al. 2007; Wille et al. 2007), while evidence from Mo isotopes from the 2.9 Ga Sinqeni Formation, Pongola Supergroup, South Africa,…”
- Tidal obliquity evolution of potentially habitable planets (2011, background): “During this period, before the so-called Great Oxidation Event≈ 2.5 Gyr ago (Anbar et al. 2007), microorganisms may have played a major role in the evolution of Earth’s atmosphere (Kasting & Siefert 2002), probably enriching it with CH4 (methane) and CO2 (carbon dioxide).”
- Processes on the Young Earth and the Habitats of Early Life (2012, background): “From a wide variety of multiproxy studies, Anbar et al. (2007) showed evidence that there was a “whiff of oxygen” in the Late Archean.”