SCIENTIFIC AMERICAN
The planet’s spin may have mediated critical atmospheric oxygen
When Judith Klatt began studying the colorful mats of primitive microbes living in a sinkhole at the bottom of Lake Huron, she thought she might learn something about Earth’s early ecosystems. Instead Klatt, a biogeochemist at the Max Planck Institute for Marine Microbiology in Bremen, Germany, wound up confronting one of geology’s greatest unsolved mysteries: How, exactly, did Earth become the only planet known to have an oxygen-rich atmosphere?
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