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g. Piper & Fajardo 2011); at the very (abrupt) tree line, tree ages were about 40 and 70?years for Cerro Castillo and El Fraile, respectively. A total of 348 trees and more than 500 cores were used to compute tree-ring chronologies that spanned from 13 (N.?pumilio and P.?albicaulis at the tree line) to 620?years (P.?albicaulis in Pioneer site below tree line altitude). The LQC model was clearly superior to the other simpler models (AICs: L?=?61621, LQ?=?60931, LQC?=?60409). The LQC was highly successful in describing the variation (R2?=?0.894), in part http://www.selleckchem.com/products/Rapamycin.html due to the smooth fits for ontogeny and size (See Table?S2 for full anova table). From this model, detrended tree growth (dBAI, cm2?year?1) increased with time at all sites (a positive slope on the linear year term, ��?=?0.0038?��?0.00031, http://www.selleck.cn/products/PD-98059.html P? http://www.selleckchem.com/products/Everolimus(RAD001).html negative at all sites with a 10- to 50-year lag, that is, recruitment events happened 10�C50?years after poor growth years (Fig.?6, upper graphs). Taking into account the underestimate of recruitment date (due to coring above the root collar), this suggests that bad periods for growth are good periods for recruitment at tree line. At lower elevations, that is, in the closed canopy forests, a wide range of synchrony patterns are visible and include long-term positive and negative gradients (Montana sites) and periodic relationships with positive and negative lags (Patagonia sites). When examining all elevations together, but divided by century (Fig.?7), synchronizing patterns are shifting at all sites.