13 pagesImportant progresses have been made in palaeo- climatological studies by using statistical methods. But they are in somewhere limited as they take the present as an ab- solute reference. This is particularly true for the modern analogue technique. The availability of mechanistic mod- els to simulate the proxies measured in the sediment cores gives now the possibility to relax this constraint. In particu- lar, vegetation models provide outputs comparable to pollen data (assuming that there is a relationship between plant pro- ductivity and pollen counts). The input of such models is, among others, climate. The idea behind paleo-climatological reconstructions is then to obtain inputs, given outputs. This procedure, called model invers...