3. Results and discussion
Our results showed that eCO2 increased the dissolved organic carbon in both the rhizosphere and bulk soil (Fig.1). This may have originated from the increase in plant exudate. This increase in exudates may cause the increase in bacterial abundance in the rhizosphere. The eCO2 also increased the SRB abundance in the rhizosphere, while it decreased the abundance in the bulk soil. However, the fungal abundance was not affected by the eCO2 and the archaeal abundance was reduced by the eCO2 in both the rhizosphere and bulk soil (Fig. 2). For the diversity, the eCO2 increased bacterial diversity but decreased the fungal and SRB diversity in the rhizosphere (Fig. 3). Although the bacterial abundance was increased by eCO2, the activities of the 3 types of extracellular enzymes were not significantly affected by the eCO2 (Fig. 1). However, the result of correlation analysis showed that bacterial abundance was positively correlated with the DOC, b-glucosidase, aminopeptidase, and SRB, while the archaeal abundance was negatively correlated with the enzyme activity, and the fungal abundance was not correlated with any parameters (Supplementary data Table S1). This suggests that bacterial groups play a key role in the degradation of organic compounds.