Chauhan Ashvini, Ogram Andrew, Reddy K R
Soil and Water Science Department, University of Florida, Gainesville, FL 32611-0290, USA.
Appl Environ Microbiol. 2004 Jun;70(6):3475-84. doi: 10.1128/AEM.70.6.3475-3484.2004.
Nutrient runoff from the Everglades Agricultural Area resulted in a well-documented gradient of phosphorus concentrations in soil and water, with concomitant ecosystem-level changes, in the northern Florida Everglades. It was recently reported that sulfate-reducing prokaryote assemblage composition, numbers, and activities are dependent on position along the gradient (H. Castro, K. R. Reddy, and A. Ogram, Appl. Environ. Microbiol. 68:6129-6137, 2002). The present study utilized a combination of culture- and non-culture-based approaches to study differences in composition of assemblages of syntrophic and methanogenic microbial communities in eutrophic, transition, and oligotrophic areas along the phosphorus gradient. Methanogenesis rates were much higher in eutrophic and transition regions, and sequence analysis of 16S rRNA gene clone libraries constructed from samples taken from these regions revealed differences in composition and activities of syntroph-methanogen consortia. Methanogens from eutrophic and transition regions were almost exclusively composed of hydrogenotrophic methanogens, with approximately 10,000-fold-greater most probable numbers of hydrogenotrophs than of acetotrophs. Most cultivable strains from eutrophic and transition regions clustered within novel lineages. In non-culture-based studies to enrich syntrophs, most bacterial and archaeal clones were either members of novel lineages or closely related to uncultivated environmental clones. Novel cultivable Methanosaeta sp. and fatty acid-oxidizing bacteria related to the genera Syntrophomonas and Syntrophobacter were observed in microcosms containing soil from eutrophic regions, and different lines of evidence indicated the existence of novel syntrophic association in eutrophic regions.
来自大沼泽地农业区的营养物质径流导致佛罗里达州北部大沼泽地土壤和水中磷浓度呈现出有充分记录的梯度变化,并伴随着生态系统层面的改变。最近有报道称,硫酸盐还原原核生物的群落组成、数量和活性取决于沿该梯度的位置(H. 卡斯特罗、K. R. 雷迪和A. 奥格拉姆,《应用与环境微生物学》68:6129 - 6137,2002年)。本研究采用基于培养和非培养的方法相结合,来研究沿磷梯度的富营养、过渡和贫营养区域中互营和产甲烷微生物群落组合组成的差异。富营养和过渡区域的甲烷生成速率要高得多,对从这些区域采集的样本构建的16S rRNA基因克隆文库进行序列分析,揭示了互营产甲烷菌联合体在组成和活性上的差异。来自富营养和过渡区域的产甲烷菌几乎完全由氢营养型产甲烷菌组成,氢营养型产甲烷菌的最可能数量比乙酸营养型产甲烷菌大约多10000倍。来自富营养和过渡区域的大多数可培养菌株聚集在新的谱系内。在基于非培养的互营菌富集研究中,大多数细菌和古菌克隆要么是新谱系的成员,要么与未培养的环境克隆密切相关。在含有富营养区域土壤的微观世界中观察到了新的可培养甲烷八叠球菌属物种以及与互营单胞菌属和互营杆菌属相关的脂肪酸氧化细菌,不同的证据表明富营养区域存在新的互营关系。