Invasive, non-native organisms pose a serious threat to native biodiversity and the overall ecological balance of the ecosystem at risk. Some non-native, invasive plants have been shown to alter ecosystem functioning through plant-soil feedbacks which alter soil nutrient availability. We hypothesized that non-native bluestems invading south
Results/Conclusions Our data indicate that soil Ninorg pools vary dramatically across time, vegetation, and soil types. In early summer 2007, soil Ninorg pools (mg N kg-1 soil-1) tended to be higher in the native bluestem patches in the sandy loam soils (14.1 and 11.6 mg N kg-1 soil-1 in native versus non-native bluestem patches, respectively). However, this trend reversed in sandy loam soils throughout the remainder of 2007 (i.e., Ninorg was higher in non-native than native patches, 14 versus 9.7 mg N kg-1 soil-1, respectively). In the clay soils, soil Ninorg pools fluctuated dramatically over time, but also tended to be slightly lower in the non-native bluestem patches (14 and 17.4 mg N kg-1 soil-1 in non-native versus native bluestem patches, respectively, in August 2007). Nitrogen mineralization rates were not different between patches in sandy loam soils (0.15 mg N/kg soil/day for both vegetation types), but it was higher in the non-native bluestem patches (0.05 mg N/kg soil/day) than the adjacent native (0.01 mg N/kg soil/day) on clay soils. Interestingly, percent soil moisture was higher in the non-native bluestem patches on sandy loam throughout the 2007 growing season (2% to 5% higher than native patches) We conclude that alterations in N cycling may accompany non-native bluestem invasion into coastal prairie, but these effects are relatively small and strongly influenced by soil texture and seasonal variability. The striking differences in soil moisture between the two vegetation types suggest that alterations to the hydrologic cycle and/or rain use efficiency of the vegetation may be important in driving this particular invasion process.