A strong evidence of this is found in the rusty iron-rich layers in geological stratum corresponding to the period mentioned before. Oceans had changed its color to green while oxygen was reacting with minerals. When the reactions stopped, oxygen could finally enter the atmosphere. Even though each cell only produced a small amount of oxygen, the combined metabolism of many cells during a vast period transformed the atmosphere to what is today. It allowed cells to colonize the surface of the ocean and ultimately the dry
A strong evidence of this is found in the rusty iron-rich layers in geological stratum corresponding to the period mentioned before. Oceans had changed its color to green while oxygen was reacting with minerals. When the reactions stopped, oxygen could finally enter the atmosphere. Even though each cell only produced a small amount of oxygen, the combined metabolism of many cells during a vast period transformed the atmosphere to what is today. It allowed cells to colonize the surface of the ocean and ultimately the dry