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Carbon dioxide on the early earth.

J C Walker1

  • 1Department of Atmospheric and Oceanic Science, The University of Michigan, Ann Arbor 48109, USA.

Origins of Life and Evolution of the Biosphere : the Journal of the International Society for the Study of the Origin of Life
|January 1, 1985
PubMed
Summary

Early Earth

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Area of Science:

  • Geochemistry
  • Planetary Science
  • Earth Science

Background:

  • The composition of Earth's early atmosphere is crucial for understanding planetary habitability.
  • Previous models have not fully accounted for early Earth's unique geological conditions.

Purpose of the Study:

  • To estimate the partial pressure of carbon dioxide in Earth's primordial atmosphere.
  • To investigate the factors controlling early atmospheric composition.

Main Methods:

  • Utilizing geochemical mass balance principles.
  • Analyzing models of early Earth's accretion and interior dynamics.
  • Considering the absence of stable continental platforms.

Main Results:

  • The partial pressure of carbon dioxide may have reached as high as 10 bars.
  • Early Earth experienced significant volatile outgassing due to rapid accretion.
  • Limited carbonate mineral storage capacity due to lack of stable continents.

Conclusions:

  • Early Earth's atmosphere likely had a much higher carbon dioxide concentration than previously thought.
  • Geochemical processes and geological conditions profoundly influenced early atmospheric evolution.
  • Understanding these conditions is key to reconstructing Earth's ancient climate.

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