Elshahed Mostafa S, Senko John M, Najar Fares Z, Kenton Stephen M, Roe Bruce A, Dewers Thomas A, Spear John R, Krumholz Lee R
Department of Botany and Microbiology, University of Oklahoma, Norman, Oklahoma, USA.
Appl Environ Microbiol. 2003 Sep;69(9):5609-21. doi: 10.1128/AEM.69.9.5609-5621.2003.
An artesian sulfide- and sulfur-rich spring in southwestern Oklahoma is shown to sustain an extremely rich and diverse microbial community. Laboratory incubations and autoradiography studies indicated that active sulfur cycling is occurring in the abundant microbial mats at Zodletone spring. Anoxygenic phototrophic bacteria oxidize sulfide to sulfate, which is reduced by sulfate-reducing bacterial populations. The microbial community at Zodletone spring was analyzed by cloning and sequencing 16S rRNA genes. A large fraction (83%) of the microbial mat clones belong to sulfur- and sulfate-reducing lineages within delta-Proteobacteria, purple sulfur gamma-Proteobacteria, epsilon -Proteobacteria, Chloroflexi, and filamentous Cyanobacteria of the order Oscillatoria as well as a novel group within gamma-Proteobacteria. The 16S clone library constructed from hydrocarbon-exposed sediments at the source of the spring had a higher diversity than the mat clone library (Shannon-Weiner index of 3.84 compared to 2.95 for the mat), with a higher percentage of clones belonging to nonphototrophic lineages (e.g., Cytophaga, Spirochaetes, Planctomycetes, Firmicutes, and Verrucomicrobiae). Many of these clones were closely related to clones retrieved from hydrocarbon-contaminated environments and anaerobic hydrocarbon-degrading enrichments. In addition, 18 of the source clones did not cluster with any of the previously described microbial divisions. These 18 clones, together with previously published or database-deposited related sequences retrieved from a wide variety of environments, could be clustered into at least four novel candidate divisions. The sulfate-reducing community at Zodletone spring was characterized by cloning and sequencing a 1.9-kb fragment of the dissimilatory sulfite reductase (DSR) gene. DSR clones belonged to the Desulfococcus-Desulfosarcina-Desulfonema group, Desulfobacter group, and Desulfovibrio group as well as to a deeply branched group in the DSR tree with no representatives from cultures. Overall, this work expands the division-level diversity of the bacterial domain and highlights the complexity of microbial communities involved in sulfur cycling in mesophilic microbial mats.
俄克拉荷马州西南部的一个自流硫化物和富含硫的泉被证明维持着一个极其丰富多样的微生物群落。实验室培养和放射自显影研究表明,在佐德莱特泉丰富的微生物垫中正在发生活跃的硫循环。无氧光合细菌将硫化物氧化为硫酸盐,而硫酸盐则被硫酸盐还原细菌种群还原。通过克隆和测序16S rRNA基因对佐德莱特泉的微生物群落进行了分析。大部分(83%)的微生物垫克隆属于δ-变形菌纲、紫色硫γ-变形菌纲、ε-变形菌纲、绿弯菌门以及颤藻目丝状蓝细菌内的硫和硫酸盐还原谱系,还有γ-变形菌纲内的一个新类群。从泉源处受烃类污染的沉积物构建的16S克隆文库比微生物垫克隆文库具有更高的多样性(香农-韦纳指数分别为3.84和2.95),属于非光合谱系(如噬纤维菌属、螺旋体属、浮霉菌属、厚壁菌门和疣微菌门)的克隆比例更高。这些克隆中有许多与从烃类污染环境和厌氧烃降解富集物中获得的克隆密切相关。此外,18个泉源克隆与任何先前描述的微生物门类都不聚类。这18个克隆,连同从各种环境中检索到的先前发表或存入数据库的相关序列,可聚类为至少四个新的候选门类。通过克隆和测序异化亚硫酸盐还原酶(DSR)基因的1.9 kb片段对佐德莱特泉的硫酸盐还原群落进行了表征。DSR克隆属于脱硫球菌-脱硫八叠球菌-脱硫线菌属组、脱硫杆菌属组、脱硫弧菌属组以及DSR树中一个没有培养代表的深分支类群。总体而言,这项工作扩展了细菌域在门类水平上的多样性,并突出了嗜温微生物垫中参与硫循环的微生物群落的复杂性。