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Evolution of the Nitrogen Biogeochemical Cycle

In the anoxic atmosphere the closed anaerobic cycle of nitrogen would have consisted of the following thermodynamically permissible reactions  [Pg.54]

Ammonium oxidation to dinitrogen by carbon dioxide, sulfate or ferric iron  [Pg.55]

Dinitrogen fixation by various organic and inorganic reductants  [Pg.55]

Ammonium oxidation by nitrite or nitrate producing dinitrogen  [Pg.55]

Ferric iron oxidation of ammonium to nitrite or nitrate  [Pg.55]


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