Solid Earth Carbon Degassing and Sequestration Since 1 Billion Years Ago
Coupling plate tectonic models with thermodynamic carbon outflux estimates to reconstruct solid Earth carbon degassing over the last billion years.

Coupling plate tectonic models with thermodynamic carbon outflux estimates to reconstruct solid Earth carbon degassing over the last billion years.
Exceptionally low mid-ocean ridge CO2 outgassing sustained the Sturtian Snowball Earth glaciation for over 50 million years.
GPlately: a Python interface for deep-time spatio-temporal data analysis using pyGPlates, simplifying plate tectonic reconstructions.