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首页> 外文期刊>Applied Soil Ecology >Characterization of redox-related soil microbial communities along a river floodplain continuum by fatty acid methyl ester (FAME) and 16S rRNA genes
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Characterization of redox-related soil microbial communities along a river floodplain continuum by fatty acid methyl ester (FAME) and 16S rRNA genes

机译:脂肪酸甲酯(FAME)和16S rRNA基因表征河漫滩连续体中氧化还原相关的土壤微生物群落

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摘要

Redox states affect substrate availability and energy transformation, and, thus, play a crucial role in regulating soil microbial abundance, diversity, and community structure. We evaluated microbial communities in soils under oxic, intermittent, and anoxic conditions along a river floodplain continuum using fatty acid methyl ester (FAME) and 16S rRNA genes-based terminal-restriction fragment length polymorphism (T-RFLP) bacterial fingerprints. In all the soils tested, microbial communities clustered according to soil redox state by both evaluation techniques. Bacteria were dominant components of soil microbial communities, while mycorrhizal fungi composed about 12% of the microbial community in the oxic soils. Gram-positive bacteria consisted >10% of the community in all soils tested and their abundance increased with increasing soil depth when shifting from oxic to anoxic conditions. In the anoxic soils, Gram-positive bacteria composed about 16% of the total community, suggesting that their growth and maintenance were not as sensitive to oxygen supply as for other microbes. In general, microorganisms were more abundant and diverse, and distributed more evenly in the oxic layers than the anoxic layers. The decrease in abundance with increasing oxygen and substrate limitation, however, was considerably more drastic than the decrease in diversity, suggesting that growth of soil microorganisms is more energy demanding than maintenance. The lower diversity in the anoxic than the oxic soils was attributed primarily to the differences in oxygen availability in these soils.
机译:氧化还原状态影响底物的有效性和能量转换,因此,在调节土壤微生物的丰度,多样性和群落结构方面起着至关重要的作用。我们使用脂肪酸甲酯(FAME)和基于16S rRNA基因的末端限制性片段长度多态性(T-RFLP)细菌指纹图谱,评估了河漫滩连续体在有氧,间歇和缺氧条件下土壤中的微生物群落。通过两种评估技术,在所有测试的土壤中,微生物群落均根据土壤的氧化还原状态聚集。细菌是土壤微生物群落的主要成分,而菌根真菌约占有氧土壤微生物群落的12%。从有氧环境向无氧环境转变时,革兰氏阳性细菌占所有测试土壤的群落的10%以上,并且其丰度随着土壤深度的增加而增加。在缺氧的土壤中,革兰氏阳性细菌约占总群落的16%,这表明它们的生长和维持对氧气供应的敏感性不如其他微生物高。通常,微生物比无氧层更丰富和多样,并且在有氧层中分布更均匀。然而,随着氧气和底物限制的增加,丰度的降低比多样性的降低要剧烈得多,这表明土壤微生物的生长比维持土壤对能量的需求更大。与缺氧土壤相比,缺氧土壤多样性较低,这主要归因于这些土壤中氧的有效性不同。

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