Finding the Path to Earth's Early Oxygen

Jena Johnson
Geologist Jena Johnson examines an outcrop of the Koegas Subgroup (2.415 billion years old), Northern Cape Province, South Africa.
(Image credit: Woodward Fischer/Caltech)

The game changer for life on Earth was photosynthesis. Now scientists think they've found a molecular stepping-stone for this complicated chemical process, which flooded the atmosphere with oxygen about 2.4 billion years ago.

Tiny single-celled organisms called cyanobacteria were the first life on Earth to master photosynthesis. They use light from the sun to split water molecules, releasing oxygen as waste. Many researchers suspect the oxidation of the element manganese by earlier life-forms was the first step in developing this molecular machinery — the metal still plays a critical role in photosynthesis today.

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Becky Oskin
Contributing Writer
Becky Oskin covers Earth science, climate change and space, as well as general science topics. Becky was a science reporter at Live Science and The Pasadena Star-News; she has freelanced for New Scientist and the American Institute of Physics. She earned a master's degree in geology from Caltech, a bachelor's degree from Washington State University, and a graduate certificate in science writing from the University of California, Santa Cruz.