Pan Hong, Feng Haojie, Liu Yaowei, Lai Chun-Yu, Zhuge Yuping, Zhang Qichun, Tang Caixian, Di Hongjie, Jia Zhongjun, Gubry-Rangin Cécile, Li Yong, Xu Jianming
Institute of Soil and Water Resources and Environmental Science, College of Environmental and Resource Sciences, Zhejiang Provincial Key Laboratory of Agricultural Resources and Environment, Zhejiang University, Hangzhou, 310058, China.
National Engineering Laboratory for Efficient Utilization of Soil and Fertilizer Resources, College of Resources and Environment, Shandong Agricultural University, Daizong Road, Tai'an City, Shandong, 271018, China.
ISME Commun. 2021 Dec 9;1(1):74. doi: 10.1038/s43705-021-00068-2.
Grassland soils serve as a biological sink and source of the potent greenhouse gases (GHG) methane (CH) and nitrous oxide (NO). The underlying mechanisms responsible for those GHG emissions, specifically, the relationships between methane- and ammonia-oxidizing microorganisms in grazed grassland soils are still poorly understood. Here, we characterized the effects of grazing on in situ GHG emissions and elucidated the putative relations between the active microbes involving in methane oxidation and nitrification activity in grassland soils. Grazing significantly decreases CH uptake while it increases NO emissions basing on 14-month in situ measurement. DNA-based stable isotope probing (SIP) incubation experiment shows that grazing decreases both methane oxidation and nitrification processes and decreases the diversity of active methanotrophs and nitrifiers, and subsequently weakens the putative competition between active methanotrophs and nitrifiers in grassland soils. These results constitute a major advance in our understanding of putative relationships between methane- and ammonia-oxidizing microorganisms and subsequent effects on nitrification and methane oxidation, which contribute to a better prediction and modeling of future balance of GHG emissions and active microbial communities in grazed grassland ecosystems.
草原土壤是强效温室气体甲烷(CH₄)和一氧化二氮(N₂O)的生物汇和来源。导致这些温室气体排放的潜在机制,特别是放牧草原土壤中甲烷氧化微生物和氨氧化微生物之间的关系,目前仍知之甚少。在此,我们描述了放牧对原位温室气体排放的影响,并阐明了参与草原土壤甲烷氧化和硝化作用的活性微生物之间的假定关系。基于14个月的原位测量,放牧显著降低了CH₄吸收量,同时增加了N₂O排放量。基于DNA的稳定同位素探测(SIP)培养实验表明,放牧减少了甲烷氧化和硝化过程,降低了活性甲烷氧化菌和硝化菌的多样性,进而削弱了草原土壤中活性甲烷氧化菌和硝化菌之间的假定竞争。这些结果在我们对甲烷氧化微生物和氨氧化微生物之间的假定关系以及随后对硝化作用和甲烷氧化的影响的理解方面取得了重大进展,这有助于更好地预测和模拟放牧草原生态系统中温室气体排放和活性微生物群落的未来平衡。