Seghers Dave, Top Eva M, Reheul Dirk, Bulcke Robert, Boeckx Pascal, Verstraete Willy, Siciliano Steven D
Laboratory of Microbial Ecology and Technology, Ghent University, Coupure Links 653, B-9000 Gent, Belgium.
Environ Microbiol. 2003 Oct;5(10):867-77. doi: 10.1046/j.1462-2920.2003.00477.x.
Agricultural practices, such as mineral nitrogen fertilization, have an impact on the soil's ability to oxidize methane, but little is known about the shifts in the methanotrophic community composition associated with these practices. Therefore, the long-term effect of both mineral (NH4NO3) and organic (manure and GFT-compost) fertilizer applications on the soil methanotrophic community activity and structure were investigated. Both high and low affinity methane oxidation rates were lower in the soil treated with mineral fertilizer compared to the other soils. An enhanced nitrate concentration was observed in the mineral fertilized soil but nitrate did not show a direct affect on the high affinity methane oxidation. In contrast, the low affinity methane oxidation was slowed down by increased nitrate concentrations, which suggests a direct effect of nitrate on low affinity methane oxidation. Denaturing gradient gel electrophoresis (DGGE) analysis of 16S rRNA gene fragments specific for methanotrophs revealed a distinct community between the mineral and organic fertilized soils as extra Type I methanotrophic bands (phylotypes) became visible in the organic fertilized soils. These phylotypes were not visible in the patterns of the added organic fertilizers suggesting an indirect effect of the organic fertilizers on the methanotrophic community. Additionally, a molecular analysis was performed after the low affinity methane oxidation test. The enhanced methane concentrations used in the test enriched certain low affinity methanotrophs in the organic fertilized soils but not in the mineral fertilized soil. Supporting the molecular and functional observations, fatty acids characteristic for methanotrophs were less abundant in the soil treated with mineral fertilizer compared to the soil treated with compost. In conclusion, the function and molecular and chemical composition of the methanotrophic community are all altered in soil fertilized with mineral fertilizer.
农业实践,如矿物氮肥施用,会对土壤氧化甲烷的能力产生影响,但对于与这些实践相关的甲烷氧化菌群落组成的变化却知之甚少。因此,研究了矿物肥料(硝酸铵)和有机肥料(粪肥和绿肥堆肥)长期施用对土壤甲烷氧化菌群落活性和结构的影响。与其他土壤相比,施用矿物肥料的土壤中高亲和力和低亲和力甲烷氧化速率均较低。在施用矿物肥料的土壤中观察到硝酸盐浓度升高,但硝酸盐对高亲和力甲烷氧化没有直接影响。相反,硝酸盐浓度增加会减缓低亲和力甲烷氧化,这表明硝酸盐对低亲和力甲烷氧化有直接影响。对甲烷氧化菌特异性的16S rRNA基因片段进行变性梯度凝胶电泳(DGGE)分析,结果显示,矿物肥料和有机肥料处理的土壤之间存在明显的群落差异,因为在有机肥料处理的土壤中出现了额外的I型甲烷氧化菌条带(系统发育型)。这些系统发育型在添加的有机肥料模式中不可见,这表明有机肥料对甲烷氧化菌群落有间接影响。此外,在低亲和力甲烷氧化试验后进行了分子分析。试验中使用的增加的甲烷浓度在有机肥料处理的土壤中富集了某些低亲和力甲烷氧化菌,但在矿物肥料处理的土壤中没有。与堆肥处理的土壤相比,矿物肥料处理土壤中甲烷氧化菌特有的脂肪酸含量较少,这支持了分子和功能观察结果。总之,施用矿物肥料的土壤中甲烷氧化菌群落的功能、分子和化学组成均发生了改变。