不同蚁种如何调节刀耕火种热带森林土壤中CH4的通量?

Lingling Xie, Shaojun Wang, Mei Lu, Bo Xiao, Zhengjun Wang, Zhipeng Guo, Xiaofei Guo, Shuang Luo, Ru Li, Jiahui Xia, Shengqiu Yang, Mengjie Lan
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引用次数: 0

摘要

蚂蚁作为生态系统中重要的结构力量,通过一系列生物和非生物途径,在驱动土壤甲烷(CH4)源库过程中起着至关重要的作用。然而,关于不同蚂蚁物种如何调节刀耕火种热带土壤中的CH4通量仍然存在不确定性。本研究旨在探讨西双版纳热带森林不同蚁种(Pheidole capellini-honeydew harvester, Odontoponera -横掠捕食者和Pheidologeton affin食腐者)控制土壤CH4通量的途径。我们观察到三种蚂蚁巢穴的CH4净排放量(1.29 ± 0.047 μg m−2 h−1)和参考土壤的净吸收率(-1.60 ± 0.043 μg m−2 h−1)。3种蚂蚁对减少森林年地表CH4总吸收率的贡献范围为0.06 % ~ 4.82 %。与对照土壤相比,capellini土壤的CH4排放量增加了144.18 %,而o.s transversa和affinis土壤的CH4排放量分别增加了124.65 %和111.71 %。与对照土壤相比,P. capellini巢穴的优势产甲烷菌群(Candidatus Thermoplasmatota和Euryarchaeota)丰度、产甲烷菌Sobs指数、土壤含水量、总有机碳和微生物生物量碳增加幅度最大(33.7-511.1 %)。与此相反,亲和燕窝中硝酸盐氮的增幅最高(92.0 %)。特别是,CH4通量直接或间接受到热浆候选菌丰度(26.04 %)、土壤含水量(15.41 %)和微生物生物量碳(11.70 %)增加的驱动,而甲基化菌丰度解释了CH4通量变化的7.76 %。研究结果表明,不同蚁种对西双版市热带土壤甲烷细菌丰度、微生境和微生物碳的不同影响可能导致了CH4通量的变化。这一结果将进一步深入了解土壤动物对热带森林温室气体排放的贡献。
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How do different ant species mediate CH4 fluxes in slash-burn tropical forest soils?
As important structuring force in ecosystems, ants play crucial roles in driving source-sink processes of soil methane (CH4) through a series of biotic and abiotic pathways. However, there is still uncertainty about how different ant species regulate CH4 fluxes in slash-burn tropical soils. This study aimed to identify the pathways by which the different ant species (i.e., Pheidole capellini-honeydew harvester, Odontoponera transversa-predator, and Pheidologeton affinis-scavenger) control soil CH4 fluxes in Xishuangbanna tropical forests, southwestern China. We observed a net CH4 emission in the nests of three ant species (1.29 ± 0.047 μg m−2 h−1) and a net uptake in the reference soils (-1.60 ± 0.043 μg m−2 h−1). The contribution of three ant species to the reduction of annual total forest surface CH4 uptake ranged from 0.06 % to 4.82 %. The P. capellini nests increased CH4 emissions by 144.18 % compared with the reference soils, whereas O. transversa and P. affinis nests increased by 124.65 % and 111.71 %, respectively. In contrast with the reference soils, the greatest increase (33.7–511.1 %) in abundance of dominant methanogen taxa (Candidatus Thermoplasmatota and Euryarchaeota), methanogen Sobs index, soil water content, total organic carbon, and microbial biomass carbon was found in P. capellini nests. In contrast, the highest increase (92.0 %) in nitrate nitrogen was recorded in P. affinis nests. In particular, CH4 fluxes were directly or indirectly driven by increased Candidatus Thermoplasmatota abundance (26.04 %), soil water content (15.41 %), and microbial biomass carbon (11.70 %), while the abundance of Methylomirabilota bacteria explained 7.76 % of variation in CH4 fluxes. Our data indicate that CH4 fluxes vary with ant species probably due to their differentiated modification on methanogenic bacterial abundance, micro-habitat, and microbial carbon in Xishuangbann tropical soils. This results would provide further insight into the contribution of soil fauna to greenhouse gas emissions from tropical forests.
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