One-fifth of anthropogenic greenhouse gas emissions are sequestered by the terrestrial biosphere, where forests serve as an important "natural solution" to climate change (1). Forests are expected to persist as a substantial carbon sink, dampening future rises in atmospheric CO 2 levels (2-4). However, a significant part of this carbon uptake occurs in forests regrowing from past land-use changes or natural disturbances. A clear example is the landscape history of central New England in the United States, where significant transformations have occurred: from pristine old-growth forests to clear-cut areas giving way to agriculture, to old-field succession, and to expansion of regrowth forests ( Fig. 1). As more forests approach old-growth conditions, their rate of carbon uptake may begin to decline. To anticipate the future of the global carbon sink, Pugh et al. (5) show that it is necessary to account for forest regrowth and demography and to consider the broader issue of the terrestrial biosphere's ultimate capacity to sequester carbon.In PNAS, Pugh et al. (5) utilize a new global database of forest age to inform a vegetation model and find that regrowth forests constitute a carbon sink that is even greater than that of old-growth forests. Nearly half of the carbon uptake in regrowth forests, however, can be attributed to changes in forest demography instead of environmental change. Pugh et al. (5) demonstrate that this demographic approach estimates a greater global regrowth sink but a smaller tropical regrowth sink in comparison with the traditional land-use-change approach. Combining the unique and shared strengths of forest age and landuse datasets significantly improves our understanding of carbon sink estimates, especially for regrowth forests. Projecting into the future, Pugh et al. (5) calculate the total amount of carbon in live biomass that is missing in forests relative to a world in which forests were allowed to readjust to a business-as-usual disturbance rate. Their assessment suggests that the current forest carbon sink is largely transient in nature.This study has several implications for our understanding and predictions of the global carbon sink.First, Pugh et al. (5) highlight the importance of present-day forest regrowth in driving carbon sequestration. Many studies so far have attributed the recent increase in the forest carbon sink to environmental changes such as CO 2 fertilization, nitrogen deposition, and climate change (6, 7). Those findings suggest that forest growth may continue to buffer the negative impacts of anthropogenic carbon emissions. However, more researchers are starting to find that the forest carbon sink might be dominated by regrowth and driven by postdisturbance recovery (8,9). Using a global forest age dataset that informs disturbance history, Pugh et al. (5) show that the regrowth process alone drives about one-fourth of the carbon uptake, while the remainder is driven by environmental change. This is a great step forward in recognizing the key factors causing the chan...