Results/Conclusions After the first six years of the Duke Forest experiment, an additional 52 + 16 gC m-2 yr-1 accumulated in the forest floor under elevated CO2. The C and N contents of the forest floor increased linearly under both the treatment and the control before leveling off in the subsequent six years, apparently reaching a steady state with elevated CO2 producing 34% and 31% more forest-floor C and N, respectively. Over the entire twelve-year period, an additional ~30 gC m-2 yr-1 was detected in the forest floor of the elevated CO2 plots in response to increased litterfall and root turnover. No differences in C and N contents were detected in the mineral soil; however, a significant widening of the C:N ratio of the upper mineral soil under elevated CO2 indicates that N is likely being mined from the soil and being transferred to plants, thereby supporting the additional productivity associated with elevated CO2. SOM fractionations will be completed to determine from which SOM pools nitrogen was removed and to understand the long-term sustainability of this process.