Temperature sensitivity of SOM decomposition is linked with a K‐selected microbial community

微生物种群生物学 土壤有机质 有机质 环境化学 优势(遗传学) 土壤碳 分解 环境科学 溶解有机碳 碳循环 总有机碳 生物 生态学 生态系统 土壤水分 化学 细菌 基因 生物化学 遗传学
作者
Hui Li,Shan Yang,M. V. Semenov,Fei Yao,Ji Ye,Rencang Bu,Ruiao Ma,Junjie Lin,I. N. Kurganova,Xugao Wang,Ye Deng,И. К. Кравченко,Yong Jiang,Yakov Kuzyakov
出处
期刊:Global Change Biology [Wiley]
卷期号:27 (12): 2763-2779 被引量:464
标识
DOI:10.1111/gcb.15593
摘要

Temperature sensitivity (Q10 ) of soil organic matter (SOM) decomposition is a crucial parameter to predict the fate of soil carbon (C) under global warming. Nonetheless, the response pattern of Q10 to continuous warming and the underlying mechanisms are still under debate, especially considering the complex interactions between Q10 , SOM quality, and soil microorganisms. We examined the Q10 of SOM decomposition across a mean annual temperature (MAT) gradient from -1.9 to 5.1°C in temperate mixed forest ecosystems in parallel with SOM quality and bioavailability, microbial taxonomic composition, and functional genes responsible for organic carbon decomposition. Within this temperature gradient of 7.0°C, the Q10 values increased with MAT, but decreased with SOM bioavailability. The Q10 values increased with the prevalence of K-strategy of soil microbial community, which was characterized by: (i) high ratios of oligotrophic to copiotrophic taxa, (ii) ectomycorrhizal to saprotrophic fungi, (iii) functional genes responsible for degradation of recalcitrant to that of labile C, and (iv) low average 16S rRNA operon copy number. Because the recalcitrant organic matter was mainly utilized by the K-strategists, these findings independently support the carbon quality-temperature theory from the perspective of microbial taxonomic composition and functions. A year-long incubation experiment was performed to determine the response of labile and recalcitrant C pools to warming based on the two-pool model. The decomposition of recalcitrant SOM was more sensitive to increased temperature in southern warm regions, which might attribute to the dominance of K-selected microbial communities. It implies that climate warming would mobilize the larger recalcitrant pools in warm regions, exacerbating the positive feedback between increased MAT and CO2 efflux. This is the first attempt to link temperature sensitivity of SOM decomposition with microbial eco-strategies by incorporating the genetic information and disentangling the complex relationship between Q10 and soil microorganisms.
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