Le pic de détritisme de 2440-2150 calBP se corrèle beaucoup moins bien avec ces deux reconstitutions (figure V-8) Toutefois Arnaud et al. (2005) reconnaissent l'existence d'une crise de détritisme vers 2300 calBP que l'on retrouve aussi dans le lac de Constance en Allemagne, 1998. ,
895-985 AD et 1240-1340) correspondent exactement aux deux périodes d'impact anthropique déjà caractérisées dans le lac d'Annecy Dearing Le déboisement massif du Moyen-Age documenté dans la région (Chavoutier, 1977) pourrait à lui seul être responsable de ces épisodes, Les deux périodes très courtes d'augmentation du détritisme, 1997. ,
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