Dating the rise of atmospheric oxygen

By A. Bekker, Heinrich Dick Holland, Pei-Ling Wang, D. Rumble, H. Stein, J. Hannah, Louis Coetzee, N. Beukes. Nature, 2004

1,378 citations recorded by the source corpus.

Subfields: Geochemistry and Petrology, Geophysics, Paleontology

View Paper: https://www.semanticscholar.org/paper/1583390146d2d10059581bc2a2cabc93e9351703

How researchers see this paper

The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.

In Geochemistry and Petrology

1. Paul G. Falkowski
2. Heinrich Dick Holland
3. K. Konhauser
4. Oscar Schofield
5. J. Raven
6. Andrew H. Knoll
7. A. Kappler

In Geophysics

1. Andrew H. Knoll
2. G. Feulner
3. David C. Catling
4. Heinrich Dick Holland
5. K. Zahnle
6. P. Strother
7. C. Wellman

In Paleontology

1. Andrew H. Knoll
2. Paul G. Falkowski
3. David C. Catling
4. Z. Finkel
5. Heinrich Dick Holland
6. G. Feulner
7. Oscar Schofield
8. M. Katz

Citations in the corpus

• Microbiological processes in banded iron formation deposition (2013, background): “…2006; Godfrey & Falkowski, 2009; Kendall et al., 2010), to its spread throughout the atmosphere between 2 45 Ga and 2 32 Ga, the so-called Great Oxidation Event (GOE) (Rye & Holland, 1998; Pavlov & Kasting, 2002; Bekker et al., 2004; Buick, 2008; Farquhar et al., 2011; Konhauser et al., 2011a,b).”
• Water and astrobiology (2007, background): “32Ga (Bekker et al., 2004), signifying that the first organisms on Earth developed under anoxic conditions (Nealson and Rye, 2003; Schulze-Makuch and Irwin, 2004; Canfield et al.”
• Evolutionary Trajectories and Biogeochemical Impacts of Marine Eukaryotic Phytoplankton (2004, background): “Perhaps more convincingly, fossil lipid biomarkers indicate that oxygenic photoautotrophs were present in the oceans by ca. 2,800 Ma (Brocks et al. 2003) and by ca. 2,300 Ma they had oxidized Earth’s atmosphere (Bekker et al. 2004).”
• CO2 concentrating mechanisms in algae: mechanisms, environmental modulation, and evolution. (2005, background): “7 Gyr ago (24, 30, 85, 191), such a diffusive supply of CO2 to a phytoplankton cell would have been adequate even if its RUBISCO had a low CO2 affinity and a low CO2/O2 selectivity.”
• The faint young Sun problem (2012, background): “…events is obviously crucial, and it now appears that the first global glaciation occurred close to 2.4 Ga [Kirschvink et al., 2000] and thus before the Great Oxidation Event which is dated closer to 2.3 Ga and thus around the time of the second of three Huronian glaciations [Bekker et al., 2004].”
• The oxygenation of the atmosphere and oceans (2006, background): “These contain no significant MIF-S signal (Bekker et al .”