International audienceLead concentrations and isotopic ratios were measured along two well-dated sediment cores from two distant lakes: Anterne (2100 m a.s.l.) and Le Bourget (270 m a.s.l.), submitted to low and high direct human impact and covering the last 250 and 600 years, respectively. The measurement of lead in old sediment samples (>3000 BP) permits, in using mixing-models, the determination of lead concentration, flux and isotopic composition of purely anthropogenic origin. We thus show that since ca. 1800 AD the regional increase in lead contamination was mostly driven by coal consumption (206Pb/207Pb ∼ 1.17–1.19; 206Pb/204Pb ∼ 18.3–18.6), which peaks around 1915 AD. The increasing usage of leaded gasoline, introduced in the 1920s,...