Earliest record of ‘snowball Earth’ revealed by 720-million-year-old rocks

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Earliest record of ‘snowball Earth’ revealed by 720-million-year-old rocks
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The Port Askaig Formation reveals evidence of Earth's transition from a warm climate to a frozen snowball during the Sturtian glaciation.

Scottish rocks dating back 662 to 720 million years ago may serve as a ‘golden spike’ marking the start of the Cryogenian Period.Standing on limestone beds of the pre-glacial Garvellach Formation, looking North from Garbh Eileach over to Dun Chonnuil. Due to tectonic tilting, the sedimentary layers get younger, and closer to the onset of glaciation, as you move to the right.

“These rocks record a time when Earth was covered in ice,” said Graham Shields, a geologist from University College London and co-author of the study. “All complex, multicellular life, such as animals, arose out of this deep freeze, with the first evidence in the fossil record appearing shortly after the planet thawed.”, which spans from approximately 635 to 720 million years ago. This glaciation is one of two major freezing events during this era.

“The retreat of the ice would have been catastrophic. Life had been used to tens of millions of years of deep freeze,” Shields explained. “As soon as the world warmed up, all of life would have had to compete in an arms race to adapt. Whatever survived were the ancestors of all animals.”, a significant rock formation spanning parts of present-day Scotland and Ireland. The formation consists of layers up to half a mile thick, with crucial exposures found on the Scottish Garvellachs islands.

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