The rhizosphere is the narrow region where plant roots and the soil interact vigorously and intensive microbial metabolism occurs. The properties of rhizosphere soil are usually different from that of non-rhizosphere soil. This is called rhizosphere effects (REs). 

The decomposition of rhizospheric soil organic carbon (SOC) plays an important role in driving carbon cycling in forest ecosystems. However, how rhizospheric SOC decomposition responds to simulated global warming, is rarely understood. 

Recently, a research team led by Prof. Wang Qingkui from the Institute of Applied Ecology (IAE) of the Chinese Academy of Sciences (CAS) conducted a laboratory incubation experiment to examine the rhizosphere effects of Cunninghamia lanceolata (i.e., China fir) and its understory ferns on the temperature sensitivity (expressed as Q₁₀) of SOC decomposition. 

The researchers found all plant species they tested had positive rhizosphere effects on Q₁₀ of SOC decomposition. And the positive REs on Q₁₀ could be attributed to the high rhizospheric nitrogen (N) availability and the high microbial activity (i.e., positive REs on N components, microbial biomass and microbial residues). 

This study shows that the decomposition of rhizospheric soil organic carbon is more sensitive to climate warming than the decomposition of SOC in the bulk soil, so that highlights the need for discriminating between the rhizospheric and non-rhizospheric soil when predicting the feedback of SOC pool to future climate changes. 

The study titled "Cunninghamia lanceolata and understory ferns had positive rhizosphere effects on the temperature sensitivity of soil microbial respiration in a subtropical forest", published in Geoderma, was supported by the National Natural Science Foundation of China.