Key Laboratory of Ecosystem Network Observation and Modeling, Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences, Beijing, China; University of Chinese Academy of Sciences, Beijing, China.
Key Laboratory of Ecosystem Network Observation and Modeling, Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences, Beijing, China; CAS Center for Excellence in Tibetan Plateau Earth Sciences, Beijing, China; College of Resources and Environment, University of Chinese Academy of Sciences, Beijing, China.
Sci Total Environ. 2022 Mar 20;813:151907. doi: 10.1016/j.scitotenv.2021.151907. Epub 2021 Nov 24.
Global atmospheric CO keeps rising and brings about significant effects on ecosystem carbon (C) cycling by altering C processes in soils. Soil C responses to elevated CO are highly uncertain, and how elevated CO interacts with other factors, such as nitrogen (N) availability, to influence soil C flux comprises an important source of this uncertainty, especially for those under-studied ecosystems. By conducting a manipulated CO concentration and N availability experiment on typical alpine grassland (4600 m asl), we combined the five-year in-situ measurement of soil respiration (SR) with an incubation experiment of microbial metabolic efficiency in the lab to explore the response of SR to elevated CO and N availability. The results showed that elevated CO at ambient N conditions and enriched N equally stimulated SR during the experimental period, whereas N supply had no significant effect. Elevated CO enhanced soil dissolved organic C and enzyme activity, while had marginal effects on microbial biomass and C use efficiency (CUE). Strengthened microbial activity dominated SR stimulation under elevated CO. Enriched N boosted enzyme activity and microbial CUE. N availability played divergent roles in mediating SR. The negliable regulation of N supply on elevated CO effects on SR was the offset consequences of the negative impacts of enhanced CUE and the positive contribution of heightened enzyme activity. Our findings suggest that rising CO would accelerate soil C cycling of the alpine grassland under various N regimes by stimulating microbial activity instead of lowering microbial metabolic efficiency. Such results are crucial for understanding the role of alpine ecosystems in the global C cycle.
全球大气 CO 持续上升,通过改变土壤中的 C 过程,对生态系统碳(C)循环产生重大影响。土壤 C 对升高 CO 的响应高度不确定,升高 CO 如何与其他因素(如氮(N)供应)相互作用以影响土壤 C 通量,是这种不确定性的一个重要来源,特别是对于那些研究不足的生态系统。通过在典型高山草原(4600 米海拔)上进行受控 CO 浓度和 N 供应实验,我们将五年的原位土壤呼吸(SR)测量与实验室微生物代谢效率的培养实验相结合,以探索 SR 对升高 CO 和 N 供应的响应。结果表明,在实验期间,在环境 N 条件下升高 CO 和富 N 同样刺激了 SR,而 N 供应没有显著影响。升高 CO 增强了土壤溶解有机 C 和酶活性,而对微生物生物量和 C 利用效率(CUE)的影响较小。在升高 CO 下,微生物活性的增强主导了 SR 的刺激。富 N 促进了酶活性和微生物 CUE。N 供应在介导 SR 方面发挥了不同的作用。N 供应对升高 CO 对 SR 的影响的调节作用较小,这是增强的 CUE 和提高的酶活性的积极贡献抵消了负面影响的结果。我们的研究结果表明,升高的 CO 将通过刺激微生物活性而不是降低微生物代谢效率,加速各种 N 制度下高山草原的土壤 C 循环。这些结果对于理解高山生态系统在全球 C 循环中的作用至关重要。