Abstract
BACKGROUND: Soil aggregate-size classes and microbial communities within the aggregates are important factors regulating the soil organic carbon (SOC) turnover. However, the response of soil bacterial and fungal communities in aggregates to litter decomposition in different aggregate-size classes is poorly understand. METHODS: Soil samples from un-grazed natural grassland were separated into four dry aggregate classes of different sizes (2-4 mm, 1-2 mm, 0.25-1 mm and <0.25 mm). Two types of plant litter (leaf and stem) of Leymus chinensis were added to each of the four aggregate class samples. The CO(2) release rate, SOC storage and soil microbial communities were measured at the end of the 56-day incubation. RESULTS: The results showed that the 1-2 mm aggregate had the highest bacterial Shannon and CO(2) release in CK and leaf addition treatments, and the SOC in the <0.25 mm aggregate was higher than that in the others across the treatments. The relative abundance of Ascomycota was higher in the 2-4 mm and <0.25 mm aggregates than in the 1-2 mm and 0.25-1 mm aggregates in the treatment without litter addition, and the relative abundance of Aphelidiomycota was lower in the 2-4 mm and <0.25 mm aggregates than in the 1-2 mm and 0.25-1 mm aggregates. Also, litter addition increased the relative abundance of Proteobacteria and Bacteroidetes, but decreased the relative abundance of Acidobacteria, Gemmatimonadetes, and Actinobacteria. The relative abundance of Ascomycota and Aphelidiomycota increased by more than 10% following leaf litter addition. The bacterial Shannon index had a significantly positive and direct effect on SOC concentration and CO(2) release, while the fungal Shannon index was significantly correlated with SOC concentration. Our results indicate that the soil bacterial diversity contributes positively to both carbon emissions and carbon storage, whereas soil fungal diversity can promote carbon storage and decrease carbon emissions.