Plants have the capacity to store and reallocate stored nonstructural C, but little is known about the age and ecological roles of these pools. It was thought that plants allocate recently assimilated C to produce new fine roots. However, there is recent evidence that plants can allocate old stored C for the production of fine roots following a large-infrequent disturbance (LID) providing a new dimension of the fate and the implied role of stored C in plants. Here, I explore other possible adaptations of plants to allocate stored C reserves, and provide a series of open questions on the fate of old stored C in plants. Specifically, I propose that another metabolic function of old stored C may be for supporting mycorrhizal fungi colonization after a largeinfrequent disturbance, because the production of hyphae may be more economical in terms of C to the plant under stressful conditions. Finally, in order to better understand plant resilience to LIDs it is critical to understand the mechanisms that regulate the fate of old stored C in plants.Plants have the capacity to store non-structural C, but little is known about the sizes, ages and ecological roles of these pools. Radiocarbon ( 14 C) dating has shown that plants allocate recently assimilated C to produce new fine roots in temperate, 1,2 and tropical forests. 3 However, Vargas et al. 4 provided evidence that plants can allocate old stored C (up to 11 years in mature forests) for the production of fine roots following a large-infrequent disturbance (LID), and provided a new dimension of the fate and the implied role of stored C in plants. Here, I present new data on a young forest stand and explore other possible adaptations of plants to allocate stored C reserves, and provide a series of questions for further lines of research in plant physiology and plant biochemistry research in this regard.The study was conducted at El Eden Ecological Reserve (lat 21°12.6'N, long 87°10.93'W) in the northeast Yucatan Peninsula, Mexico. The study site is a seasonally dry tropical forest where recurrent LIDs (e.g., fires and hurricanes) have created a landscape of forests of different ages. 5,6 During September and December of 2005, nine soil cores were collected at a 16-year old forest stand as described in Vargas et al. 4 The soil cores were sieved through a 2 mm mesh and fine roots were sorted by hand to determine AM colonization and radiocarbon ( 14 C) values of live roots. Additionally, root in-growth cores were buried (10 cm depth) in duplicates at the forest stand. Sieved and clean fine roots were prepared for analysis of percentage colonization of AM structures 7 (e.g., hyphae, arbuscules and vesicles). Radiocarbon ( 14 C) was used to estimate the mean age of structural C in fine roots. Briefly, roots were treated with an acid-base-acid procedure to remove nonstructural C, oven dried at 65°C and then ground following previous studies. 1,4 Radiocarbon values of structural C in live roots before the hurricane showed that these roots were produced from recently fixed ...