Carbon-13 Observations Necessitate Reduced Ocean Ventilation at the Last Glacial Maximum, but Biogeochemical Processes Explain Most of the Atmospheric Carbon Dioxide Decrease
Alessandro Giulio Tagliabue, Laurent Bopp, Didier M. Roche, Nathaëlle Bouttes, Jean‐Claude Dutay, Ramdane Alkama, Masa Kageyama, Élisabeth Michel, Didier Paillard
Abstract