“…Pollen assemblages are often used to reconstruct past climate during the Late-Glacial, because temperature and precipitation changes are identified as major determining factors for shifts in pollen assemblages . However, in French mountains such reconstructions are still lacking except for the Jura (Peyron et al, 2005), the Alps (Ortu et al, 2009) and the Massif Central (Duprat-Oualid, This Issue;Cubizolle et al, 2021;Dendievel et al, 2021).…”