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. 2019 Oct 28;116(46):22972–22976. doi: 10.1073/pnas.1908179116

Fig. 1.

Fig. 1.

(A) Location of the 632 study sites and changes in lake sediment rates over the last 10,000 y. Increases in lake sediment rates (red dots) were observed in 35.1% of the watersheds according to M-K τ coefficients; the rest of the sites show a decrease (green dots) or steady (white dots) rates. (B) Distribution of M-K trend τ coefficients. (C) Number of dated cores containing a pollen record and distribution of 14C dates (intervals = 12,000 y) used to calculate SARs.