Chen Lin, Luo Yu, Xu Jianming, Yu Zhuyun, Zhang Kaile, Brookes Philip C
Institute of Soil and Water Resources and Environmental Science, Zhejiang Provincial Key Laboratory of Agricultural Resources and Environment, Zhejiang University, Hangzhou, 310058, People's Republic of China.
State Key Laboratory of Soil and Sustainable Agriculture, Institute of Soil Science, Chinese Academy of Sciences, Nanjing, 210008, People's Republic of China.
Microb Ecol. 2016 Jul;72(1):240-251. doi: 10.1007/s00248-016-0766-0. Epub 2016 Apr 14.
Previous investigations observed that when soil was fumigated with ethanol-free CHCl3 for 24 h and then incubated under appropriate conditions, after the initial flush of CO2 was over, soil organic carbon (SOC) mineralization continued at the same rate as in the non-fumigated soil. This indicates that, following fumigation, the much diminished microbial population still retained the same ability to mineralize SOC as the much larger non-fumigated population. We hypothesize that although fumigation drastically alters the soil bacterial community abundance, composition, and diversity, it has little influence on the bacterial C-metabolic functions. Here, we conducted a 30-day incubation experiment involving a grassland soil and an arable soil with and without CHCl3 fumigation. At days 0, 7, and 30 of the incubation, the bacterial abundances were determined by quantitative PCR, and the bacterial community composition and diversity were assessed via the 16S rRNA gene amplicon sequencing. PICRUSt was used to predict the metagenome functional content from the sequence data. Fumigation considerably changed the composition and decreased the abundance and diversity of bacterial community at the end of incubation. At day 30, Firmicutes (mainly Bacilli) accounted for 70.9 and 94.6 % of the total sequences in the fumigated grassland and arable soil communities, respectively. The two fumigated soil communities exhibited large compositional and structural differences during incubation. The families Paenibacillaceae, Bacillaceae, and Symbiobacteriaceae dominated the bacterial community in the grassland soil, and Alicyclobacillaceae in the arable soil. Fumigation had little influence on the predicted abundances of KEGG orthologs (KOs) assigned to the metabolism of the main acid esters, saccharides, amino acids, and lipids in the grassland soil community. The saccharide-metabolizing KO abundances were decreased, but the acid ester- and fatty acid-metabolizing KO abundances were elevated by fumigation in the arable soil community. Our study suggests functional redundancy regarding the bacterial genetic potential associated with SOC mineralization.
先前的研究发现,当用无乙醇的CHCl3对土壤熏蒸24小时,然后在适当条件下培养时,在最初的二氧化碳排放结束后,土壤有机碳(SOC)矿化继续以与未熏蒸土壤相同的速率进行。这表明,熏蒸后,数量大幅减少的微生物群落仍然保留了与数量多得多的未熏蒸群落相同的SOC矿化能力。我们假设,虽然熏蒸会极大地改变土壤细菌群落的丰度、组成和多样性,但对细菌的碳代谢功能影响很小。在这里,我们进行了一项为期30天的培养实验,涉及一块草地土壤和一块耕地土壤,分别进行了CHCl3熏蒸和未熏蒸处理。在培养的第0天、第7天和第30天,通过定量PCR测定细菌丰度,并通过16S rRNA基因扩增子测序评估细菌群落组成和多样性。利用PICRUSt从序列数据预测宏基因组功能内容。熏蒸在培养结束时显著改变了细菌群落的组成,降低了其丰度和多样性。在第30天,厚壁菌门(主要是芽孢杆菌)分别占熏蒸草地和耕地土壤群落总序列的70.9%和94.6%。在培养过程中,两个熏蒸土壤群落表现出很大的组成和结构差异。类芽孢杆菌科、芽孢杆菌科和共生杆菌科在草地土壤细菌群落中占主导地位,而嗜热栖热放线菌科在耕地土壤中占主导地位。熏蒸对草地土壤群落中参与主要酸酯、糖类、氨基酸和脂质代谢的KEGG直系同源物(KOs)的预测丰度影响很小。在耕地土壤群落中,熏蒸使糖类代谢的KO丰度降低,但使酸酯和脂肪酸代谢的KO丰度升高。我们的研究表明,与SOC矿化相关的细菌遗传潜力存在功能冗余。