<p>The roles of multiple global change are expected for many terrestrial ecosystems in future. As two main global change factors, the impact of drought and nitrogen deposition and their interaction on soil respiration and its components (R) remains unclear. To explore the responses of soil respiration (R<sub>s</sub>), autotrophic respiration (R<sub>a</sub>) and heterotrophic respiration (R<sub>h</sub>) to multiple global change factors, we established a field experiment of throughfall reduction and nitrogen additions in a subtropical Moso bamboo (<em>Phyllostachys heterocycla</em>) forest in the Southwest China, using a 4 &#215; 4 completely randomized design. Results showed that bivariate exponential equation with soil temperature (T) and soil moisture (SWC) (R=a.e<sup>bT</sup>.SWC<sup>c</sup>) was fitted to predict R<sub>s</sub>, R<sub>a</sub> and R<sub>h</sub>. Throughfall reduction, nitrogen additions and their interaction had no effect on annual mean R<sub>s</sub> and R<sub>a</sub>, but nitrogen additions significantly depressed annual mean R<sub>h</sub>. Nitrogen additions significantly decreased contribution of R<sub>h</sub> to R<sub>s</sub> and increased contribution of R<sub>a</sub> to R<sub>s</sub>, however, the contributions were non-responsive under throughfall reduction. The more positive effect of nitrogen additions on the contribution of R<sub>a</sub> to R<sub>s</sub> was appeared compared with that of throughfall reduction, thereby more negative effect on the contribution of R<sub>h</sub> to R<sub>s</sub>. The fine root biomass, fine root carbon and nitrogen storage regulated R<sub>s</sub>, while fine root phosphorus storage determined R<sub>a</sub>. The R<sub>h</sub> was negatively correlated with vector lengths, thus suggesting that microbial carbon limitation caused the decline of R<sub>h</sub>. Our findings demonstrate that the nitrogen additions played overriding role than throughfall reduction in affecting the contribution of R<sub>a</sub> and R<sub>h</sub> to R<sub>s</sub>. Moreover, the negative response of temperature sensitivity of R<sub>s</sub> and R<sub>h</sub> to nitrogen additions, suggesting that that the nitrogen additions may weaken the positive response of soil CO<sub>2</sub> emission to global climate warming. Our study highlights asymmetrical responses of R<sub>s</sub>, R<sub>a</sub> and R<sub>h </sub>to throughfall reduction and nitrogen additions and could enhance accurate predictions of soil carbon dynamics in response to multiple global climate change in future.</p>
Biotic interactions mediate soil microbial feedbacks to climate change