New research published in Communications Earth & Environment shows that the balance between volcanic outgassing and carbon sequestration into oceanic lithosphere is the key driver …
Carbon emissions along divergent plate boundaries modulate icehouse-greenhouse climate transitions through mid-ocean ridge and rift degassing.
Our paper in Frontiers in Earth Science presents six new regional reconstructions of the carbonate compensation depth across the Pacific Ocean over the last 30 million years, …
Reconstructing regional carbonate compensation depth variability in the Pacific Ocean since the Oligocene to understand deep-sea carbon cycling.
Our paper in G-Cubed couples plate tectonic models with thermodynamic carbon outflux estimates to build the most comprehensive reconstruction of solid Earth carbon degassing and …
Coupling plate tectonic models with thermodynamic carbon outflux estimates to reconstruct solid Earth carbon degassing over the last billion years.
This talk examines the deep-time tectonic carbon cycle by linking thermodynamic models of carbon storage and release with global plate tectonic reconstructions. We quantify carbon …
A new paper in Geology links the duration of the Sturtian Snowball Earth glaciation to exceptionally low CO2 outgassing from mid-ocean ridges — not volcanic arcs.
Exceptionally low mid-ocean ridge CO2 outgassing sustained the Sturtian Snowball Earth glaciation for over 50 million years.
