Three scientists discuss the cause of the Great Oxidation Event (GOE) approximately 2.4 billion years ago, during which atmospheric oxygen () levels rose from virtually zero to significant fractions of modern levels.
Scientist 1
The GOE was driven entirely by the biological evolution of oxygenic photosynthesis in cyanobacteria. Prior to the GOE, cyanobacteria produced , but it was immediately consumed by abundant reducing agents, primarily dissolved ferrous iron () and volcanic gases. The GOE occurred when these local chemical sinks were finally saturated. The timing and rate of the rise were controlled strictly by the burial rate of organic carbon. The burial of organic matter prevented it from reacting with to reform , thereby leaving a net surplus of in the atmosphere.
Scientist 2
Biological production of was necessary but not sufficient for the GOE. Cyanobacteria evolved hundreds of millions of years before the GOE, but atmospheric could not accumulate due to the continuous input of highly reduced volcanic gases ( and ) from submarine volcanoes. The GOE was triggered by a major tectonic shift: a transition from predominantly submarine volcanism to subaerial (land-based) volcanism. Subaerial volcanoes release more oxidized gases ( and ) because they erupt at lower pressures and react with the atmosphere. This tectonic transition reduced the planetary volcanic sink for , allowing to accumulate without requiring any change in the rate of organic carbon burial.
Scientist 3
The GOE was caused by a permanent change in Earth's overall redox state driven by hydrogen escape to space. Early Earth had an atmosphere rich in methane () produced by methanotrophic and methanogenic archaea. When cyanobacteria produced , it reacted with methane, but solar ultraviolet radiation also photolyzed methane in the upper atmosphere. The resulting hydrogen gas (), being extremely light, escaped Earth's gravity into space. This loss of hydrogen represents a permanent oxidation of the planet. Cyanobacteria and carbon burial rates were stable; the GOE occurred only when the cumulative loss of hydrogen reduced the abundance of reducing agents to the point that could persist.
Match each of the following statements with the scientist whose viewpoint it represents.
- The accumulation of atmospheric was enabled by a decrease in the chemical reactivity of volcanic emissions, independent of organic carbon burial rates.Scientist 2
- The timing of the GOE was determined by the saturation of chemical sinks, regulated strictly by the preservation of organic carbon in sediments.Scientist 1
- The transition to an oxygen-rich atmosphere was a consequence of planetary mass loss to space that altered the global redox balance.Scientist 3