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通过土壤微生物群落分析揭示了在水稻(Oryzae sativa L.)种植中,与硅酸盐结合的龙仁芽孢杆菌DCY84对甲烷排放的缓解作用。

Methane emission mitigation of Paenibacillus yonginensis DCY84 incorporated with silicate on paddy rice (Oryzae sativa L.) plantation revealed in soil microbiome profiling.

作者信息

Justine Elsa Easter, Lee Hyo-Jun, Jung Ki-Hong, Lee Yoon-Sung, Kim Yeon-Ju

机构信息

Department of Oriental Medicine Biotechnology, College of Life Science, Kyung Hee University, Yongin 17104, Republic of Korea.

Graduate School of Biotechnology and Crop Biotech Institute, Kyung Hee University, Yongin 17104, Republic of Korea.

出版信息

Sci Total Environ. 2025 Jan 1;958:177996. doi: 10.1016/j.scitotenv.2024.177996. Epub 2024 Dec 12.

Abstract

Anthropogenic methane emissions from paddy cultivation contribute to greenhouse gas levels owing to the anaerobic conditions in flooded rice fields, which promotes the activity of methanogenic bacteria. This study explored bioremediation strategies to mitigate methane release through the application of plant growth-promoting rhizobacteria combined with silicate in rice cultivation. Rice seeds were coated with Paenibacillus yonginensis DCY84, with and without the addition of silicate, prior to sowing. Results revealed notable reduction in methane flux during the peak growth stage of rice in seeds treated with DCY84 (27.215 ± 1.975 mg m h), with a further reduction observed when silicate was also applied (23.592 ± 3.112 mg m h), compared to untreated seeds (37.305 ± 2.990 mg m h). Additionally, treatment with DCY84 (28.24 ± 0.55 g) resulted in an increase in rice yield (p < 0.05), as evidenced by a greater 1000-grain weight compared to both the control group (26.91 ± 0.09 g) and the application of silicate (27.37 ± 0.57 g). The beta diversity of the soil microbial community highlighted distinct differences between the treated and control groups, indicating DCY84 inoculation with or without silicate altered the soil microbial structure. Particularly, the treated groups showed dominance of the phylum Proteobacteria, especially the classes Alphaproteobacteria and Deltaproteobacteria. Furthermore, the addition of silicate to DCY84-coated rice seeds resulted in a higher abundance of bacterial families, such as Anaerolinaceae, Clostridiceae, and Nitrospirae which compete with methanogens for organic substrates, thereby reducing their methane production. Notably, the DCY84-silicate treatment group showed higher levels of methane metabolism biomarkers such as formate dehydrogenase within the soil microbiome, which correlated with the observed reduction in methane emissions. These findings suggest that coating rice seeds with DCY84 and silicate prior to sowing effectively mediates methane production and release during rice cultivation by promoting beneficial soil bacterial communities.

摘要

由于淹水稻田中的厌氧条件促进了产甲烷细菌的活性,水稻种植产生的人为甲烷排放导致了温室气体水平的上升。本研究探索了生物修复策略,通过在水稻种植中应用促植物生长根际细菌与硅酸盐相结合来减少甲烷排放。在播种前,用永仁芽孢杆菌DCY84对水稻种子进行包衣处理,分别添加和不添加硅酸盐。结果显示,用DCY84处理的种子在水稻生长高峰期的甲烷通量显著降低(27.215±1.975毫克/平方米·小时),与未处理的种子(37.305±2.990毫克/平方米·小时)相比,当同时施用硅酸盐时甲烷通量进一步降低(23.592±3.112毫克/平方米·小时)。此外,用DCY84处理(28.24±0.55克)使水稻产量增加(p<0.05),这表现为与对照组(26.91±0.09克)和施用硅酸盐组(27.37±0.57克)相比,千粒重更大。土壤微生物群落的β多样性突出了处理组和对照组之间的明显差异,表明接种DCY84(无论是否添加硅酸盐)改变了土壤微生物结构。特别是,处理组中变形菌门占主导地位,尤其是α-变形菌纲和δ-变形菌纲。此外,在包衣有DCY84的水稻种子中添加硅酸盐导致了如厌氧绳菌科、梭菌科和硝化螺旋菌科等细菌家族的丰度更高,这些细菌与产甲烷菌竞争有机底物,从而减少它们的甲烷产生。值得注意的是,DCY84-硅酸盐处理组在土壤微生物群落中显示出较高水平的甲烷代谢生物标志物,如甲酸脱氢酶,这与观察到的甲烷排放减少相关。这些发现表明,在播种前用DCY84和硅酸盐对水稻种子进行包衣处理,通过促进有益的土壤细菌群落,有效地调节了水稻种植过程中甲烷的产生和排放。

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