CORDIS Project
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This project investigates the recycling of carbon into the Earth's deep mantle through subduction of oceanic crust. By conducting high-pressure experiments, it aims to understand how carbon behaves under extreme conditions and its implications for geological processes and carbon cycling.
The key aspect of the Earth’s deep carbon cycle is how exogene carbon is recycled into the deeper earth via subduction of altered, carbonated, mafic oceanic crust.
We aim to use ultrahigh-pressure experimental petrology to investigate the behaviour of subducted carbonate at pressures corresponding to the deep upper mantle, the mantle transition zone and the uppermost lower mantle.
Earlier experimental studies showed that some residual crystalline carbonate in oceanic crust remains stable in subd…
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