The final models for moist, dry, and caatinga old-growth AGB were highly significant ( r 2 = 0.39, n = 874,222; r 2 = 0.66, n = 239,764; and r 2 = 0.55, n = 101,050, respectively) and highlighted the different controls over AGB in these regions, with moist forest AGB being predicted primarily by CWD and BIO4, dry forest AGB being predicted primarily by CWD and CEC, and caatinga AGB being predicted by CWD and mean annual precipitation.
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Carbon sequestration potential of second-growth forest regeneration in the Latin American tropics.
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