The Riddle of Atmospheric Oxygen: Photosynthesis or Photolysis?

Abstract

The stoichiometry of the photosynthetic reaction requires that the quantities of the end products (organic biomaterial and free oxygen) be equal. However, the correct balance of the amounts of oxygen and organic matter that could have been produced by green plants on the land and in the ocean since the emergence of unique oxygenic photosynthetic systems (no more than 2.7 billion years ago) is virtually impossible, since the vast majority of oxygen was lost in oxidizing the initially reducing matter of the planet, and the bulk of organic carbon is scattered in sedimentary rocks. In recent decades, convincing information has been obtained in favor of the large-scale photolysis of water molecules in the upper atmosphere with the scattering of light hydrogen into space and the retention of heavier oxygen by gravity. This process has been operating continuously since the formation of the Earth. It is accompanied by huge losses of water and the oxidation of salts of ferrous iron and sulfide sulfur in the oceans and methane in the atmosphere. The main stages of the evolution of the atmosphere and surface layers of the Earth’s crust are analyzed for the first time in this work by considering the parallel processes of photosynthesis and photolysis. Large-scale photolysis of water also provides consistent explanations for the main stages in the evolution of the nearest planets of our Solar System.

Chance and Necessity in the Evolution of Matter to Life: A Comprehensive Hypothesis

“…The ideas of water photolysis developed in [105,108], when applied to the situation of our neighboring planets Venus and Mars, logically explain both the practically complete loss of their initially acquired water and the drastic difference in the mass and composition of their atmospheres. Specialists in astrophysics have already accepted our photolysis hypothesis in their recent studies and publications [109].…”