Seven hundred million years ago, Earth apparently couldn’t make up its mind.
A new study in PNAS suggests that the Sturtian glacial period, which lasted around 56 million years, wasn’t actually one long continuous deep freeze. Instead, it was a series of repeated ice ages, cycling in and out of glaciation over and over again. Snowball. Melt. Snowball. Melt. For fifty-six million years.
The mechanism is beautifully weird. A massive volcanic province called the Franklin Large Igneous Province, in what’s now the Canadian Arctic, triggered the whole thing by weathering down and sucking CO2 out of the atmosphere. Once Earth froze, the weathering stopped, CO2 built up from volcanoes, things warmed up, the basalt started weathering again, CO2 crashed back down, and the planet froze again. Rinse and repeat until the basalt ran out.

