Hugenholtz P, Pitulle C, Hershberger K L, Pace N R
Department of Plant and Microbial Biology, University of California, Berkeley 94720-3102, USA.
J Bacteriol. 1998 Jan;180(2):366-76. doi: 10.1128/JB.180.2.366-376.1998.
A culture-independent molecular phylogenetic survey was carried out for the bacterial community in Obsidian Pool (OP), a Yellowstone National Park hot spring previously shown to contain remarkable archaeal diversity (S. M. Barns, R. E. Fundyga, M. W. Jeffries, and N. R. Page, Proc. Natl. Acad. Sci. USA 91:1609-1613, 1994). Small-subunit rRNA genes (rDNA) were amplified directly from OP sediment DNA by PCR with universally conserved or Bacteria-specific rDNA primers and cloned. Unique rDNA types among > 300 clones were identified by restriction fragment length polymorphism, and 122 representative rDNA sequences were determined. These were found to represent 54 distinct bacterial sequence types or clusters (> or = 98% identity) of sequences. A majority (70%) of the sequence types were affiliated with 14 previously recognized bacterial divisions (main phyla; kingdoms); 30% were unaffiliated with recognized bacterial divisions. The unaffiliated sequence types (represented by 38 sequences) nominally comprise 12 novel, division level lineages termed candidate divisions. Several OP sequences were nearly identical to those of cultivated chemolithotrophic thermophiles, including the hydrogen-oxidizing Calderobacterium and the sulfate reducers Thermodesulfovibrio and Thermodesulfobacterium, or belonged to monophyletic assemblages recognized for a particular type of metabolism, such as the hydrogen-oxidizing Aquificales and the sulfate-reducing delta-Proteobacteria. The occurrence of such organisms is consistent with the chemical composition of OP (high in reduced iron and sulfur) and suggests a lithotrophic base for primary productivity in this hot spring, through hydrogen oxidation and sulfate reduction. Unexpectedly, no archaeal sequences were encountered in OP clone libraries made with universal primers. Hybridization analysis of amplified OP DNA with domain-specific probes confirmed that the analyzed community rDNA from OP sediment was predominantly bacterial. These results expand substantially our knowledge of the extent of bacterial diversity and call into question the commonly held notion that Archaea dominate hydrothermal environments. Finally, the currently known extent of division level bacterial phylogenetic diversity is collated and summarized.
对黑曜石池(OP)中的细菌群落进行了一项不依赖培养的分子系统发育调查,黑曜石池是黄石国家公园的一个温泉,此前已证明其中含有显著的古菌多样性(S.M. 巴恩斯、R.E. 芬迪加、M.W. 杰弗里斯和N.R. 佩奇,《美国国家科学院院刊》91:1609 - 1613, 1994)。通过使用通用保守或细菌特异性rDNA引物进行PCR,从小亚基rRNA基因(rDNA)直接从OP沉积物DNA中扩增并克隆。通过限制性片段长度多态性鉴定了300多个克隆中的独特rDNA类型,并测定了122个代表性rDNA序列。发现这些序列代表54种不同的细菌序列类型或序列簇(≥98% 同一性)。大多数(70%)序列类型隶属于14个先前已识别的细菌门类(主要门;界);30% 与已识别的细菌门类无关。这些无关的序列类型(由38个序列代表)名义上包含12个新的、门类水平的谱系,称为候选门类。OP的几个序列与已培养的化能无机营养嗜热菌的序列几乎相同,包括氢氧化卡尔德杆菌以及硫酸盐还原菌嗜热脱硫弧菌和嗜热脱硫杆菌,或者属于因特定代谢类型而被认可的单系类群,如氢氧化水生菌目和硫酸盐还原的δ - 变形菌纲。这些生物体的出现与OP的化学成分(高铁和硫含量高)一致,并表明通过氢氧化和硫酸盐还原,该温泉的初级生产力存在一个无机营养基础。出乎意料的是,在用通用引物构建的OP克隆文库中未遇到古菌序列。用域特异性探针对扩增的OP DNA进行杂交分析证实,来自OP沉积物的分析群落rDNA主要是细菌的。这些结果极大地扩展了我们对细菌多样性程度的认识,并对普遍认为古菌主导热液环境的观念提出了质疑。最后,对目前已知的门类水平细菌系统发育多样性程度进行了整理和总结。