Carbon emissions along divergent plate boundaries modulate icehouse-greenhouse climates
Carbon emissions along divergent plate boundaries modulate icehouse-greenhouse climate transitions through mid-ocean ridge and rift degassing.
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Carbon emissions along divergent plate boundaries modulate icehouse-greenhouse climate transitions through mid-ocean ridge and rift degassing.
Reconstructing regional carbonate compensation depth variability in the Pacific Ocean since the Oligocene to understand deep-sea carbon cycling.
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.