Thomas Gernon

Enriched-mantle oceanic volcanism driven by prolonged convective erosion of continental roots

Mantle upwelling at Afar triple junction shaped by overriding plate dynamics

Melt generation and evolution in the Adda’do rift segment of the Afar rift from trace elements and petrography

Afar triple junction fed by single asymmetric mantle upwelling

We detected deep pulses beneath Africa – what we learned could help us understand volcanic activity

Solid Earth forcing of Mesozoic oceanic anoxic events

Transient mobilization of subcrustal carbon coincident with Palaeocene–Eocene Thermal Maximum

Global chemical weathering dominated by continental arcs since the mid-Palaeozoic

Neoproterozoic glacial origin of the Great Unconformity

The relationship between eruptive activity, flank collapse, and sea level at volcanic islands: A long‐term (>1 Ma) record offshore Montserrat, Lesser Antilles

Rapid onset of mafic magmatism facilitated by volcanic edifice collapse