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Earth's breathable atmosphere a result of continents taking control of the carbon cycle

Date:
June 9, 2014
Source:
University of Exeter
Summary:
Scientists investigating one of the greatest riddles of the Earth's past may have discovered a mechanism to help determine how oxygen levels in the atmosphere expanded to allow life to evolve.

How did oxygen levels in the atmosphere expand enough to allow life to evolve? Researchers may have solved one of the biggest puzzles in geochemistry.
Credit: Copyright Michele Hogan

Scientists investigating one of the greatest riddles of Earth's past may have discovered a mechanism to help determine how oxygen levels in the atmosphere expanded to allow life to evolve.

High concentrations of atmospheric oxygen have been essential for the evolution of complex life on Earth. Over the 4.5 billion years of Earth history, oxygen concentration has risen from trace amounts to 21% of the atmosphere today. However, the mechanisms behind this rise are uncertain, and it remains one of the biggest puzzles in geochemistry.

A research group from the University of Exeter has discovered one possible mechanism, relating to the way in which carbon dioxide is removed from the atmosphere over long timescales.

Dr Benjamin Mills, of Geography, said: "On the early Earth, CO2 levels were controlled by hydrothermal processes on the seafloor. As Earth cooled, and the continents grew, chemical processes on the continents took over."

Using computer models, the group has shown that this switch may explain increasing oxygen concentration over Earth's middle age (the Proterozoic era), which ultimately led to conditions suitable for complex life. According to the authors, the oxygen rise is caused by a gradual increase in marine limiting nutrients, which are a product of chemical weathering of the continents.

Dr Mills added: "The more CO2 that is sequestered by continental weathering, the larger the phosphate source to the oceans. Phosphate availability controls the long term photosynthetic productivity, which leads to oxygen production."

"This is not the only reason oxygen rose to high levels, but it seems to be an important piece of the puzzle. Whilst the carbon cycle can function without large continents, it seems that their emergence was critical to our own evolution."


Story Source:

The above story is based on materials provided by University of Exeter. Note: Materials may be edited for content and length.


Journal Reference:

  1. Benjamin Mills, Timothy M. Lenton, and Andrew J. Watson. Proterozoic oxygen rise linked to shifting balance between seafloor and terrestrial weathering. PNAS, June 9, 2014 DOI: 10.1073/pnas.1321679111

Cite This Page:

University of Exeter. "Earth's breathable atmosphere a result of continents taking control of the carbon cycle." ScienceDaily. ScienceDaily, 9 June 2014. <www.sciencedaily.com/releases/2014/06/140609153433.htm>.
University of Exeter. (2014, June 9). Earth's breathable atmosphere a result of continents taking control of the carbon cycle. ScienceDaily. Retrieved September 2, 2014 from www.sciencedaily.com/releases/2014/06/140609153433.htm
University of Exeter. "Earth's breathable atmosphere a result of continents taking control of the carbon cycle." ScienceDaily. www.sciencedaily.com/releases/2014/06/140609153433.htm (accessed September 2, 2014).

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