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农田土壤中含真菌群落的特征及真菌反硝化作用的一氧化氮排放

Characterization of Fungal -Containing Communities and NO Emission From Fungal Denitrification in Arable Soils.

作者信息

Xu Huifang, Sheng Rong, Xing Xiaoyi, Zhang Wenzhao, Hou Haijun, Liu Yi, Qin Hongling, Chen Chunlan, Wei Wenxue

机构信息

Key Laboratory of Agro-Ecological Processes in Subtropical Regions and Taoyuan Station of Agro-Ecology Research, Institute of Subtropical Agriculture, Chinese Academy of Sciences, Changsha, China.

College of Resource and Environment, University of Chinese Academy of Sciences, Beijing, China.

出版信息

Front Microbiol. 2019 Feb 4;10:117. doi: 10.3389/fmicb.2019.00117. eCollection 2019.

Abstract

Fungal denitrifiers play important roles in soil nitrogen cycling, but we have very limited knowledge about their distribution and functions in ecosystems. In this study, three types of arable soils were collected across different climate zones in China, including quaternary red clay soils, alluvial soils, and black soils. The composition and abundance of fungal -containing denitrifiers was determined by MiSeq high-throughput sequencing and qPCR, respectively. Furthermore, a substrate-induced inhibition approach was used to explore NO emissions from fungal denitrification. The results showed that the arable soils contained a wide range of -containing fungal denitrifiers, with four orders and eight genera. Additionally, approximately 57.30% of operational taxonomic unit (OTUs) belonged to unclassified -containing fungi. Hypocreales was the most predominant order, with approximately 40.51% of the total number of OTUs, followed by Sordariales, Eurotiales, and Mucorales. It was further indicated that 53% of fungal OTUs were shared by the three types of soils (common), and this group of fungi comprised about 98% of the total relative abundance of the -containing population, indicating that the distribution of fungal -containing denitrifiers was quite homogenous among the soil types. These common OTUs were determined by multiple soil characteristics, while the composition of unique OTUs was manipulated by the specific properties of each soil type. Furthermore, fungal NO emissions were significantly and positively correlated with fungal abundance in the soils, whereas it was not clearly related to fungal compositions. In conclusion, although the arable soils hosted diverse -containing fungal denitrifiers, fungal compositions were highly homogenous among the soil types, which could be a consequence of enduring agricultural practices. The abundance of fungal -containing denitrifiers, rather than their composition, may play more significant roles in relation to NO emission from fungal denitrification.

摘要

真菌反硝化菌在土壤氮循环中发挥着重要作用,但我们对它们在生态系统中的分布和功能了解非常有限。在本研究中,采集了中国不同气候区的三种耕地土壤,包括第四纪红粘土、冲积土和黑土。分别通过MiSeq高通量测序和qPCR确定含真菌反硝化菌的组成和丰度。此外,采用底物诱导抑制法探究真菌反硝化作用产生的一氧化氮排放。结果表明,耕地土壤中含有多种含真菌反硝化菌,分属四个目和八个属。此外,约57.30%的可操作分类单元(OTU)属于未分类的含真菌。肉座菌目是最主要的目,约占OTU总数的40.51%,其次是粪壳菌目、散囊菌目和毛霉目。进一步表明,三种土壤类型共有53%的真菌OTU(共有),这组真菌约占含菌种群总相对丰度的98%,表明含真菌反硝化菌在不同土壤类型中的分布相当均匀。这些共有OTU由多种土壤特性决定,而独特OTU的组成则受每种土壤类型的特定性质影响。此外,真菌一氧化氮排放与土壤中真菌丰度显著正相关,而与真菌组成无明显关系。总之,尽管耕地土壤中存在多种含真菌反硝化菌,但不同土壤类型间真菌组成高度均匀,这可能是长期农业实践的结果。含真菌反硝化菌的丰度而非其组成,可能在真菌反硝化产生一氧化氮的过程中发挥更重要的作用。

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