Once upon a time, only about 650 million years ago, our Earth was a snowball. What was the aftermath #greenhouse #climate triggering deglaciation and the ocean's role in it?
We addressed this intriguing scientific question via a set of #EarthSystemModel experiments in the new Nature Communication paper "Moderate greenhouse climate and rapid carbonate formation after Marinoan snowball Earth" led by Lennart Ramme within his PhD project.
https://doi.org/10.1038/s41467-024-47873-6
Moderate greenhouse climate and rapid carbonate formation after Marinoan snowball Earth - Nature Communications
When the Marinoan snowball Earth deglaciated, the ocean’s chemistry determined the strength and duration of the ensuing supergreenhouse climate, while the sudden warming and biological activity could have led to a rapid formation of cap dolostones.Nature