Ammonium Ion Concentration in the Primitive Ocean

Mathematics – Logic

Scientific paper

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Scientific paper

If ion exchange on clay minerals regulated the cations in the primitive ocean as it does in the present ocean, the pH would have been 8 and the K+ concentration 0.01M. Since NH4{}+ and K+ are similar in their clay-mineral equilibria, the maximum NH4{}+ concentration in the primitive ocean would also have been 0.01M. An estimate of the minimum NH4{}+ concentration is 1 × 10-3M, based on the reversible deamination of aspartic acid and the assumption that aspartic acid is necessary for the origin of life. The rate of this nonenzymic deamination is rapid on the geological time scale.

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