Zhao Xingqing, Yang Liuyan, Yu Zhenyang, Peng Naiying, Xiao Lin, Yin Daqiang, Qin Boqiang
State Key Laboratory of Pollution Control and Resource Reuse, School of the Environment, Nanjing University, Nanjing 210093, China.
J Environ Sci (China). 2008;20(2):224-30. doi: 10.1016/s1001-0742(08)60035-2.
The characterization of microbial communities of different depth sediment samples was examined by a culture-independent method and compared with physicochemical parameters, those are organic matter (OM), total nitrogen (TN), total phosphorus (TP), pH and redox potential (Eh). Total genomic DNA was extracted from samples derived from different depths. After they were amplified with the GC-341f/907r primer sets of partial bacterial 16S rRNA genes, the products were separated by denaturing gradient gel electrophoresis (DGGE). The profile of DGGE fingerprints of different depth sediment samples revealed that the community structure remained relatively stable along the entire 45 cm sediment core, however, principal-component analysis of DGGE patterns revealed that at greater sediment depths, successional shifts in community structure were evident. The principle coordinates analysis suggested that the bacterial communities along the sediment core could be separated into two groups, which were located 0--20 cm and 21--45 cm, respectively. The sequencing dominant bands demonstrated that the major phylogenetic groups identified by DGGE belonged to Bacillus, Bacterium, Brevibacillus, Exiguobacterium, gamma-Proteobacterium, Acinetobacter sp. and some uncultured or unidentified bacteria. The results indicated the existence of highly diverse bacterial community in the lake sediment core.
采用非培养方法对不同深度沉积物样本的微生物群落进行了表征,并与理化参数进行了比较,这些理化参数包括有机质(OM)、总氮(TN)、总磷(TP)、pH值和氧化还原电位(Eh)。从不同深度的样本中提取了总基因组DNA。用部分细菌16S rRNA基因的GC-341f/907r引物对进行扩增后,产物通过变性梯度凝胶电泳(DGGE)进行分离。不同深度沉积物样本的DGGE指纹图谱显示,在整个45厘米的沉积物岩心中,群落结构保持相对稳定,然而,DGGE图谱的主成分分析表明,在沉积物深度较大时,群落结构的演替变化明显。主坐标分析表明,沿沉积物岩心的细菌群落可分为两组,分别位于0-20厘米和21-45厘米处。对优势条带的测序表明,DGGE鉴定出的主要系统发育类群属于芽孢杆菌属、杆菌属、短短芽孢杆菌属、微小杆菌属、γ-变形菌纲、不动杆菌属以及一些未培养或未鉴定的细菌。结果表明,湖泊沉积物岩心中存在高度多样的细菌群落。