
Sturtian Snowball Wasn’t One Long Freeze—It Repeatedly Thawed and Refroze
Harvard researchers simulate the Sturtian glaciation (about 717–660 million years ago) as a cycle of glaciation and thaw driven by carbon-cycle feedbacks: volcanic CO₂ input and basalt weathering lowered CO₂ to trigger ice cover, while ongoing volcanism and reduced weathering during ice cover allowed CO₂ to build and melt, repeating for ~56 million years—reconciling the geological record and the survival of early aerobic life, with implications for exoplanet climates.













