Ant nests can affect the process and seasonal dynamics of forest soil methane emissions through mediating methane oxidation/reduction microorganisms and physicochemical environments. To explore the process and mechanism by which ant nests affect soil methane emissions from Hevea brasiliensis plantation in Xishuangbanna, we measured the seasonal dynamics of methane emissions from ant nest and non-nest soils by using static chamber-gas chromatography method, and analyzed the effect of ant nesting on the changes in functional microbial diversity, microhabitats, and soil nutrients in the plantations. The results showed that: 1) Ant nests significantly affected the mean annual soil methane emissions in tropical plantation. Methane emissions in ant nest were decreased by 59.9% than the non-nest soil. In the dry season, ant nest soil was a methane sink (-1.770 μg·m-2·h-1), which decreased by 87.2% compared with the non-nest soil, while it was a methane source (0.703 μg·m-2·h-1) that increased by 152.7% in the wet season. 2) Ant nesting affected methane emissions via changing soil temperature, humidity, carbon and nitrogen concentrations. In contrast to the control, the mean annual temperature, humidity, and carbon and nitrogen content increased by 4.9%-138.5% in ant nest soils, which explained 90.1%, 97.3%, 27.3%-90.0% of the variation in methane emissions, respectively. 3) Ant nesting affected the emission dynamics through changing the diversity and community structure of methane functional microbe. Compared with the control, the average annual methanogen diversity (Ace, Chao1, Shannon, and Simpson indices) in the ant nest ranged from -9.9% to 61.2%, which were higher than those (-8.7%-31.2%) of the methane-oxidising bacterial communities. The relative abundance fluctuations of methanogens and methanotrophic bacteria were 46.76% and -6.33%, respectively. The explaining rate of methanogen diversity to methane emissions (78.4%) was higher than that of oxidizing bacterial diversity (54.5%), the relative abundance explained by the dominant genus of methanogens was 68.9%. 4) The structural equation model showed that methanogen diversity, methanotroph diversity, and soil moisture were the main factors controlling methane emissions, contributing 95.6%, 95.0%, and 91.2% to the variations of emissions, respectively. The contribution (73.1%-87.7%) of soil temperature and carbon and nitrogen components to the emission dynamics was ranked the second. Our results suggest that ant nesting mediates the seasonal dynamics of soil methane emissions, primarily through changing the diversity of methane-function microorganisms and soil water conditions. The research results deepen the understanding of the mechanism of biological regulation of methane emission in tropical forest soil.
蚂蚁筑巢能够通过改变土壤甲烷氧化/还原微生物及理化环境,调控森林土壤甲烷排放过程及季节动态。以西双版纳热带橡胶人工林群落为研究样地,采用静态箱-气相色谱法测定蚁巢和非巢土壤甲烷排放通量的季节变化,分析蚂蚁筑巢引起热带人工林土壤功能微生物、微生境及土壤养分改变对甲烷排放通量的影响规律。结果表明: 1)与非巢地相比,蚂蚁筑巢显著降低了橡胶人工林土壤甲烷排放,年均通量减少59.9%。干季蚁巢土壤是甲烷汇(-1.770 μg·m-2·h-1),相较非巢地减少了87.2%;湿季蚁巢土壤则为源(0.703 μg·m-2·h-1),其甲烷排放量增加了152.7%。2)蚂蚁筑巢改变了土壤温湿度及碳氮养分含量。相较于非巢地,蚁巢土壤温度、湿度及碳氮组分含量年均增幅达4.9%~138.5%,其对甲烷排放通量的解释率分别为90.1%、97.3%、27.3%~90.0%。3)蚂蚁筑巢改变功能微生物多样性及群落结构。相较非巢地,蚁巢年均甲烷产生菌群落多样性指数(Ace、Chao1、Shannon和Simpson)变幅为-9.9%~61.2%,且高于甲烷氧化菌群落(-8.7%~31.1%),产甲烷菌和甲烷氧化菌优势属相对丰度变幅分别为46.8%和-6.3%。甲烷产生菌对排放通量的解释率(78.4%)高于氧化菌(54.5%),甲烷产生菌与甲烷氧化菌优势属对排放通量的解释率共为68.9%。4)结构方程表明,甲烷产生菌、氧化菌、土壤含水率为甲烷排放通量的主控因子,其对土壤甲烷排放的贡献率分别为95.6%、95.0%和91.2%,而土壤温度、碳氮组分的贡献(73.1%~87.7%)次之。因此,蚂蚁筑巢主要通过改变甲烷功能微生物多样性及土壤水分状况而影响甲烷排放季节动态。.
Keywords: ant nesting; methane emission; methanogen; methanotroph; tropical rubber forest.