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. 2009 May 18;106(22):8830–8834. doi: 10.1073/pnas.0900517106

Fig. 2.

Fig. 2.

Age models for the 3 lake-sediment cores. Age models for LY1 and Negrilla are based on linear interpolation between 210Pb dates and median ages of calibrated 14C dates, whereas a best-fit line was used between dates at LY2. AMS 14C ages were measured on terrestrial charcoal and calibrated age ranges are 2 σ.