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Responses of soil microeukaryotic communities to short-term fumigation-incubation revealed by MiSeq amplicon sequencing

机译:MiSeq扩增子测序揭示的土壤微真核生物群落对短期熏蒸培养的响应

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摘要

In soil microbiology, there is a “paradox” of soil organic carbon (SOC) mineralization, which is that even though chloroform fumigation destroys majority of the soil microbial biomass, SOC mineralization continues at the same rate as in the non-fumigated soil during the incubation period. Soil microeukaryotes as important SOC decomposers, however, their community-level responses to chloroform fumigation are not well understood. Using the 18S rRNA gene amplicon sequencing, we analyzed the composition, diversity, and C-metabolic functions of a grassland soil and an arable soil microeukaryotic community in response to fumigation followed by a 30-day incubation. The grassland and arable soil microeukaryotic communities were dominated by the fungal Ascomycota (80.5–93.1% of the fungal sequences), followed by the protistan Cercozoa and Apicomplexa. In the arable soil fungal community, the predominance of the class Sordariomycetes was replaced by the class Eurotiomycetes after fumigation at days 7 and 30 of the incubation. Fumigation changed the microeukaryotic α-diversity in the grassland soil at days 0 and 7, and β-diversity in the arable soil at days 7 and 30. Network analysis indicated that after fumigation fungi were important groups closely related to other taxa. Most phylotypes (especially Sordariomycetes, Dothideomycetes, Coccidia, and uncultured Chytridiomycota) were inhibited, and only a few were positively stimulated by fumigation. Despite the inhibited Sordariomycetes, the fumigated communities mainly consisted of Eurotiomycetes and Sordariomycetes (21.9 and 36.5% relative frequency, respectively), which are able to produce hydrolytic enzymes associated with SOC mineralization. Our study suggests that fumigation not only decreases biomass size, but modulates the composition and diversity of the soil microeukaryotic communities, which are capable of driving SOC mineralization by release of hydrolytic enzymes during short-term fumigation-incubation.
机译:在土壤微生物学中,土壤有机碳(SOC)矿化存在一个“悖论”,即即使氯仿熏蒸破坏了大部分土壤微生物生物量,SOC矿化过程仍以与未熏蒸土壤相同的速率继续进行。潜伏期。土壤微真核生物是重要的SOC分解剂,但是,它们对氯仿熏蒸的社区水平反应还不十分清楚。使用18S rRNA基因扩增子测序,我们分析了熏蒸后30天孵育的草原土壤和可耕土壤微真核生物群落的组成,多样性和C代谢功能。草地和耕地的微真核生物群落以真菌子囊菌(占真菌序列的80.5–93.1%)为主,其次是原生动物Cercozoa和Apicomplexa。在耕地土壤真菌群落中,在孵化的第7天和第30天进行熏蒸后,Sordariomycetes类取代了Eurotiomycetes类。熏蒸在第0和7天改变了草地土壤中的微真核生物α-多样性,在第7和30天改变了耕地土壤中的β-多样性。网络分析表明,熏蒸后真菌是与其他类群密切相关的重要群体。大多数系统型(特别是Sordariomycetes,Dothideomycetes,Coccidia和未培养的Chytridiomycota)均受到抑制,而熏蒸却仅对少数阳性。尽管Sordariomycetes受到抑制,但熏蒸后的群落主要由Eurotiomycetes和Sordariomycetes组成(相对频率分别为21.9和36.5%),它们能够产生与SOC矿化相关的水解酶。我们的研究表明,熏蒸不仅减少了生物量,而且调节了土壤微真核生物群落的组成和多样性,能够在短期熏蒸孵化过程中通过释放水解酶来驱动SOC矿化。

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