Biological N 2 fixation (or N 2 fixation hereafter), the process that converts atmospheric N 2 to ammonia by diazotrophs with the catalysis of nitrogenase, is one major pathway of new nitrogen (N) inputs for terrestrial ecosystems (Vitousek et al., 2013). N 2 fixation can be classified into symbiotic N 2 fixation (SNF hereafter) and free-living N 2 fixation (FNF hereafter) (Reed et al., 2011). For SNF, the diazotrophs are symbiotically related to host plants by forming nodules, which are specialized for N 2 fixation, and the other types are classified as FNF, including N 2 fixation carried out by free-living diazotrophs in soil (soil FNF hereafter), litter, foliage, moss, and lichen (Reed et al., 2011). Due to limited field measurements and poor understanding of the underlying mechanisms, there is a huge uncertainty in N 2 fixation estimates for global terrestrial natural ecosystems with current estimates ranging from 40 to 290 Tg N yr −1 (Cleveland et al., 1999;Davies-Barnard & Friedlingstein, 2020;Vitousek et al., 2013). According to the existing limited measurements for terrestrial natural ecosystems, SNF rates vary between 0.1 and 160 kg N ha −1 yr −1 , and the FNF rates range from 0.01 to 60 kg N ha −1 yr −1 (Reed et al., 2011). However, few studies have simultaneously measured SNF and FNF rates within the same ecosystem. According to a model analysis, FNF contributes a smaller fraction to total N 2 fixation in the tropical region (17%) and the other regions (44%) (Wang & Houlton, 2009). However, recent evidence shows that FNF is equally important as or may exceed SNF in some secondary and Abstract Biological N 2 fixation plays crucial roles in determining the pattern and pace of ecological succession and carbon sequestration. Nevertheless, the rates and controls of symbiotic (SNF) and freeliving (FNF) N 2 fixation have rarely been investigated simultaneously. Here we measured SNF and soil FNF rates for eight early succession ecosystems dominated by kudzu (Pueraria lobata (Willd.) Ohwi) in a subtropical region of China in growing and nongrowing seasons. N 2 fixation rates were measured using acetylene reduction assay against a 15 N 2 uptake method. Both SNF and soil FNF rates were significantly higher in the growing season than in the nongrowing season. The two forms of N 2 fixation contributed equally to total N 2 fixation rate across the eight sites with soil FNF being higher than SNF in half of the sites. Total N 2 fixation rates ranged from 7.12 to 61.93 kg N ha −1 yr −1 with an average of 22.93 ± 6.52 kg N ha −1 yr −1 . N 2 fixation contributed significantly to soil nitrogen and carbon accumulation. Both SNF and FNF were significantly related to soil moisture. Additionally, SNF and soil FNF were strongly correlated with phosphorus availability and vanadium/iron availability, respectively, most likely implying that SNF was limited by phosphorus and soil FNF was limited by vanadium or iron. Our findings suggest that SNF and soil FNF may be limited by different sets of nutrients within an ecosystem.Plain L...