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. 2008 Feb 11;363(1498):1795–1802. doi: 10.1098/rstb.2007.0014

Figure 1.

Figure 1

The pre-Columbian peak of Amazonian soil charcoal. (a) Map of seasonality (number of months with more than 100 mm of rain) as determined from tropical rainfall monitoring mission (TRMM; Silman 2007), showing locations of soil charcoal 14C dated samples. (b) Two hundred and twenty-eight 14C ages for dated charcoal horizons in Amazonian soils (see Bush & Silman 2007 for review). All ages were calibrated using Calib v. 5.0.2 (Stuiver & Reimer 1993), and midpoint ages per 50-year period plotted against time (pink). Purple indicates atmospheric Δ14C as a proxy for solar output (Bard 1998). M, maunder; S, sporer; W, wolf solar minima. Turquoise indicates number of El Niño events per century (Moy et al. 2002).‘?’ indicates uncertainty as to the timing of a shift in Amazonian cultural adaptations.