Chemical and geological evidence indicate that photosynthetic
cyanobacteria existed about 2.6 billion years ago and
anoxygenic photosynthesis had been taking place since a billion years before that. Oxygenic
photosynthesis was the primary source of free oxygen and led to the
Great Oxidation Event roughly 2.4 to 2.1 billion years ago during the
Neoarchean-
Paleoproterozoic boundary. Although the end of the Great Oxidation Event was marked by a significant decrease in gross
primary productivity that eclipsed extinction events, the development of
aerobic respiration enabled more energetic metabolism of organic molecules, leading to
symbiogenesis and the
evolution of
eukaryotes, and allowing the diversification of
complex life on Earth. == Prokaryotic photoautotrophs ==