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Mathew Anderson

“Oxygen wasn’t always part of Earth’s atmosphere. It took a couple of billion years for the gas to accumulate, continually generated mainly as a byproduct of single cellular life. After enough oxygen saturated the oceans and then started building up in the atmosphere, it was only at this point that the ozone layer formed through the above process.”

Mathew Anderson, Habitable Exoplanets: Red Dwarf Systems Like TRAPPIST-1
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Habitable Exoplanets: Red Dwarf Systems Like TRAPPIST-1 Habitable Exoplanets: Red Dwarf Systems Like TRAPPIST-1 by Mathew Anderson
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