Long-term fertilization alters nutrient availability and microbial community composition in soil, thereby modulating the decomposition of microbial necromass and its influence on soil organic carbon (SOC) turnover. However, the microbial taxa that drive necromass recycling and how their activity translates into positive or negative priming effects (PEs) on SOC mineralization in rice paddies remain unknown. We combined 13C isotope probing and high-throughput sequencing to investigate the microbial groups involved in necromass decomposition and their associated PEs on SOC mineralization in paddy soils subjected to 34 years of mineral fertilization or chicken manure application as compared to unfertilized control soil. Following the addition of 13C-labeled bacterial necromass, 50–60 % of the 13C was mineralized to CO