Olivier Averbuch

A 485-million-year history of Earth’s surface temperature

Rapid groundwater decline and some cases of recovery in aquifers globally

Is there a remnant Variscan subducted slab in the mantle beneath the Paris basin? Implications for the late Variscan lithospheric delamination process and the Paris basin formation

Mountain building‐enhanced continental weathering and organic carbon burial as major causes for climatic cooling at the Frasnian–Famennian boundary (c. 376 Ma)?