The role of P availability on soil C sequestration is poorly understood in no-tillage production. The objective of this study was to examine the long-term phosphorus (P) fertilization effect on soil organic C (SOC), N, and C:N ratio in soil aggregates at different depths in no-till corn (Zea mays L.)-wheat (Triticum aestivum L.)-soybean (Glycine max L.) rotations. The experiment was conducted on low to medium P soils at Springfield and Milan, TN during 2013-2015 from 0-15 cm and from 0-5, 5-10, 10-15, and 15-30 cm in 2018 using Latin square design with five replications of five P rates (0, 29, 59, 88, and 117 kg P ha(-1)) applied annually. Bulk soil and aggregate sizes > 2, 0.25-2, 0.053-0.25, and < 0.053 mm were analyzed for SOC and N. Phosphorus rate of 88 kg ha(-1) resulted in high soil testing P and had higher SOC and N than all other treatments on low P soil. However, over-application of P at 117 kg ha(-1) decreased SOC on low P soil. No response of SOC or N to P fertilization was observed on medium P soil. Application of 29 kg P ha(-1) increased large macroaggregate (> 2 mm) weight. Concentrations of SOC and N were higher in microaggregates (0.053-0.25 mm) than the other aggregates. In conclusion, SOC and N stocks are increased on low P soils with appropriate P application, which is crucial for simultaneous improvements of soil C sequestration and crop yield.