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Phylogenetic composition of bacterial communities in small boreal lakes and ombrotrophic bogs of the upper Volga basin

机译:伏尔加盆地上游的小型北方湖泊和滋养沼泽中细菌群落的系统发育组成。

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摘要

Fluorescent in situ hybridization (FISH) with rRNA-specific oligonucleotide probes was used to assess the numbers and phylogenetic diversity of prokaryotic microorganisms in the water of small boreal lakes and peatland catchments of the swampy upper Volga basin. The abundance of bacterioplankton in lake water was found to vary from 1. 6 to 8. 7 × 10~6 cells ml~(-1), with the highest values detected in neutral eutrophic lakes. The total cell numbers in the peat of ombrotrophic bogs were 3. 9-4. 3 × 10~8 cells g~(-1) of wet peat. The proportion of bacteria identified by the group-specific probes decreased from 79-85% in neutral (pH 6. 6-6. 9) mesotrophic and eutrophic lakes to 65-69% in acidic (pH 4. 4-5. 5) dystrophic lakes and to 51-58% in the peat of acidic (pH 3. 6-3. 9) ombrotrophic bogs. The diversity of bacterial communities was highest in lakes with neutral water. These communities were dominated by members of the phylum Actinobacteria (31-44% of the total bacterial number), while the contribution of Alphaproteobacteria (16-19%), Bacteroidetes (6-16%), Betaproteobacteria (6-7%), Planctomycetes (2-8%), and Gammaproteobacteria (4-5%) was also significant. In acidic dystrophic lakes, Actinobacteria (25-35%) and Betaproteobacteria (25-34%) predominated, while peatland catchments were dominated by the Alphaproteobacteria (20-23%). The presence of acidobacteria and some planctomycetes common for bogs in the water of acidic dystrophic lakes, as well as the high proportion of bacteria (31-49%) that were not identified by the group-specific probes, suggest the impact of microbial processes in peatland catchments on the microbial composition of the receiving waters.
机译:使用rRNA特异性寡核苷酸探针的荧光原位杂交(FISH)来评估伏尔加河上游沼泽地的小型北方湖泊和泥炭地集水区原核微生物的数量和系统发育多样性。湖泊水中浮游细菌的丰度变化范围为1. 6到8。7×10〜6细胞ml〜(-1),在中性富营养化湖泊中检测到最高。滋养沼泽泥炭中的总细胞数为3。9-4。 3×10〜8个细胞g〜(-1)的湿泥炭。通过组特异性探针鉴定的细菌比例从中性和富营养化湖泊中性(pH 6. 6-6。9)的79-85%降至酸性(pH 4. 4-5。5)中的65-69%。营养不良的湖泊和泥炭中的酸性(pH 3. 6-3。9)混养营养泥达到51-58%。在中性水的湖泊中,细菌群落的多样性最高。这些群落主要是放线菌门的成员(占细菌总数的31-44%),而丙酸杆菌(16-19%),拟杆菌(6-16%),贝氏杆菌(6-7%),扁平菌(2-8%)和γ-变形杆菌(4-5%)也很重要。在酸性营养不良的湖泊中,放线菌(25-35%)和贝塔蛋白细菌(25-34%)占主导地位,而泥炭地集水区则由Alphaproteobacteria(20-23%)占据主导地位。酸性营养不良湖泊水中沼泽所存在的酸性细菌和一些扁平菌类细菌,以及未被组特异性探针鉴定出的高比例细菌(31-49%),提示了微生物过程的影响。泥炭地流域接受水域的微生物组成。

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