CORDIS Project
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This project investigates the rise of atmospheric oxygen and its impact on Earth's biogeochemical cycles. By integrating laboratory experiments and geological observations, it aims to develop models that explain the dynamics of elemental cycles during this critical transition in Earth's history.
The rise of atmospheric O2 ~2,500 million years ago is one of the most profound transitions in Earth's history.
Yet, despite its central role in shaping Earth's surface environment, the cause for the rise of O2 remains poorly understood.
Tight coupling between the O2 cycle and the biogeochemical cycles of redox-active elements, such as C, Fe and S, implies radical changes in these cycles before, during and after the rise of O2.
These changes, too, are incompletely understood, but have left valua…
WEIZMANN INSTITUTE OF SCIENCE
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