Collaborative Research: "GOE-ing DEEP" into the Paleoproterozoic of Gabon to elucidate the causes and effects of Earth's Great Oxidation
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Oxygen is crucial for macroscopic life, yet the causes and repercussions of its accumulation in the atmosphere are poorly understood. A key question for resolving the trajectory of planetary habitability is if chemical shifts recorded in ~2.4-2.0 billion-year-old rocks reflect global-scale oxygen changes or regional-local conditions. To answer…
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