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. 2015 Apr 20;112(18):5607–5612. doi: 10.1073/pnas.1419133112

Fig. 4.

Fig. 4.

(A) The δDwax-corr records from Lakes Chichancanab and Salpeten, fit with a smoothing spline (thicker lines) to highlight centennial-scale trends. Colored envelopes indicate 1σ error in δDwax-corr values (±7‰) applied to the smoothing spline fits. Horizontal bands indicate the mean δDwax-corr values for lake surface sediments and soils from three regions within the Maya Lowlands with different mean annual precipitation (Fig. 2); the width of the bands indicates the SEM of regional mean values. (B) The δ18O records from two speleothems from the northern (Chaac) and southern (Yok I) Maya Lowlands (8, 9) (Fig. 1), plotted on a common scale to highlight differences in the range and amplitude of δ18O variability for these two records. E, Early; M, Middle; L, Late; T, Terminal; VPDB, Vienna Pee Dee Belemnite.