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首页> 外文期刊>Communications in Soil Science and Plant Analysis >Identification of Metabolically Active Rhizosphere Microorganisms by Stable Isotopic Probing of PLFA in Switchgrass
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Identification of Metabolically Active Rhizosphere Microorganisms by Stable Isotopic Probing of PLFA in Switchgrass

机译:柳枝PL PLFA的稳定同位素探测鉴定代谢活性根际微生物

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Root-derived rhizodeposits of recent photosynthetic carbon (C) are the foremost source of energy for microbial growth and development in rhizosphere soil. A substantial amount of photosynthesized C by the plants is translocated to belowground and is released as root exudates that influence the structure and function of soil microbial communities with potential inference in nutrient and C cycling in the ecosystem. We applied the C-13 pulse chase labeling technique to evaluate the incorporation of rhizodeposit-C into the phospholipid fatty acids (PLFAs) in the bulk and rhizosphere soils of switchgrass (Panicum virgatum L.). Soil samples of bulk and rhizosphere were taken at 1, 5, 10 and 20 days after labeling and analyzed for C-13 enrichment in the microbial PLFAs. Temporal differences of C-13 enrichment in PLFAs were more prominent than spatial differences. Among the microbial PLFA biomarkers, fungi and Gram-negative (GM-ve) bacterial PLFAs showed rapid enrichment with C-13 compared to Gram-positive (GM+ve) and actinomycetes in rhizosphere soil. The C-13 enrichment of actinomycetes biomarker PLFA significantly increased along with sampling time in both soils. PLFAs indicative to fungi, GM-ve and GM+ ve showed a significant decrease in C-13 enrichment over sampling time in the rhizosphere, but a decrease was also observed in GM-ve (16: 1.5c) and fungal biomarker PLFAs in the bulk soil. The relative C-13 concentration in fungal PLFA decreased on day 10, whereas those of GM-ve increased on day 5 and GM+ ve remained constant in the rhizosphere soil. However, the relative C-13 concentrations of GM-ve and GM+ve increased on days 5 and 10, respectively, and those of fungal remain constant in the bulk soil. The present study demonstrates the usefulness of C-13 pulse chase labeling together with PLFA analysis to evaluate the active involvement of microbial community groups for utilizing rhizodeposit-C.
机译:最近的光合碳(C)的根源根际沉积物是根际土壤微生物生长和发育的最主要能源。植物将大量光合作用的C转移到地下,并以根系分泌物的形式释放,影响土壤微生物群落的结构和功能,并可能推断生态系统中的养分和C循环。我们应用了C-13脉冲追逐标记技术,评价了柳枝posit(Panicum virgatum L.)的块状和根际土壤中根状沉积C掺入磷脂脂肪酸(PLFA)中的情况。标记后第1、5、10和20天采集散装和根际土壤样品,并分析微生物PLFA中的C-13富集。 PLFA中C-13富集的时间差异比空间差异更为突出。在微生物PLFA生物标志物中,与根际土壤中的革兰氏阳性菌(GM + ve)和放线菌相比,真菌和革兰氏阴性菌(GM-ve)细菌PLFAs快速富集C-13。在两种土壤中,放线菌生物标志物PLFA的C-13富集随着采样时间的增加而显着增加。指示真菌,GM-ve和GM + ve的PLFA在根际采样时间内显示C-13富集度显着降低,但是在整体中GM-ve(16:1.5c)和真菌生物标志物PLFA也观察到了降低泥。真菌PLFA中C-13的相对浓度在第10天下降,而GM-ve的相对C-13浓度在第5天增加,而GM + ve在根际土壤中保持恒定。但是,GM-ve和GM + ve的相对C-13浓度分别在第5天和第10天增加,而真菌的相对浓度在散装土壤中保持恒定。本研究证明了C-13脉冲追踪标记和PLFA分析的有效性,以评估微生物群落群对根瘤菌C的积极参与。

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