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首页> 外文期刊>Applied and Environmental Microbiology >Variation in microbial community structure in two boreal peatlands as determined by analysis of phospholipid Fatty Acid profiles.
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Variation in microbial community structure in two boreal peatlands as determined by analysis of phospholipid Fatty Acid profiles.

机译:通过分析磷脂脂肪酸谱确定两个北方泥炭地微生物群落结构的变化。

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Analyses of phospholipid fatty acids (PLFAs) were used to assess variation in community structure and total microbial biomass in two boreal peatlands in Sweden. The total PLFA concentration in peat ranged from 0.16 to 7.0 nmol g of wet peat(sup-1) (median, 0.70 nmol g of wet peat(sup-1)). Principal-component analysis of PLFA data revealed that the degree of depth-related variation in PLFA composition was high among peatland habitats, with general differences between wet sites, with water tables within a few centimeters of the moss surface, and dry sites, with water tables >10 cm below the moss surface. However, variation in PLFA composition over the growing season was negligible. In the principal-component analyses, most PLFAs were determined to be parts of clusters of covarying fatty acids, suggesting that they originated in the same functional groups of microorganisms. Major clusters were formed by monounsaturated (typical of gram-negative eubacteria), terminally branched (gram-positive or anaerobic gram-negative eubacteria), methyl-branched and branched unsaturated (sulfate-reducing bacteria and/or actinomycetes), (omega)8 monounsaturated (methane-oxidizing bacteria), and polyunsaturated (eucaryotes) PLFAs. Within the clusters, PLFAs had rather distinct concentration-depth distributions. For example, PLFAs from sulfate-reducing bacteria and/or actinomycetes and those from methane-oxidizing bacteria had maximum concentrations slightly below and at the average water table depth, respectively.
机译:磷脂脂肪酸(PLFA)的分析用于评估瑞典两个北方泥炭地群落结构和总微生物量的变化。泥炭中的总PLFA浓度范围为湿泥炭(sup-1)的0.16至7.0nmol g(中位数为湿泥炭(sup-1)的0.70nmol g)。 PLFA数据的主成分分析显示,泥炭地生境中PLFA组成的深度相关变化程度很高,湿地之间的一般差异很大,水位在苔藓表面的几厘米之内,而干地之间则是水分,桌子在苔藓表面以下10厘米以下。但是,整个生长季节PLFA组成的变化可以忽略不计。在主成分分析中,大多数PLFA被确定为共变脂肪酸簇的一部分,这表明它们起源于相同的微生物功能组。主要簇由单不饱和(典型的革兰氏阴性真细菌),末端分支(革兰氏阳性或厌氧革兰氏阴性细菌),甲基支链和不饱和的(硫酸盐还原细菌和/或放线菌),(ω)8形成。单不饱和(甲烷氧化细菌)和多不饱和(真核生物)PLFA。在集群中,PLFA具有相当不同的集中深度分布。例如,来自硫酸盐还原细菌和/或放线菌的PLFA和来自甲烷氧化细菌的PLFA的最大浓度分别略低于平均水深和平均水深。

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