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Eoarchean Earth
770 million
years after the formation of the Earth--3.8 billion years ago--the
first life may have appeared in the form of simple, single-celled organisms.
Bacteria and archaea may have even found a way to populate the otherwise
sterile and calamitous surface. The atmosphere would likely have consisted
of gases vented by volcanoes: carbon dioxide, carbon monoxide, sulfur
dioxide, nitrogen, methane, hydrogen, methane, ammonia, and water vapor.
There was probably very little oxygen and no protective ozone layer to
filter the shorter wavelengths of ultraviolet light from the Sun that are
harmful to most forms of life.
In this
image, a variety of single-celled organisms have ventured out of the ocean
and onto the rocky remains of two volcanic calderas, adding color to an
otherwise monochromatic landscape. While the lack of breathable
oxygen and shortwave ultraviolet light from the Sun would be anathema to complex life forms like ourselves, this
primitive environment was a rich source of sustenance for these terrestrial
vanguards.
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