Papineau Dominic, Walker Jeffrey J, Mojzsis Stephen J, Pace Norman R
Department of Molecular, Cellular, and Developmental Biology, University of Colorado, Boulder, CO 80309-0347, USA.
Appl Environ Microbiol. 2005 Aug;71(8):4822-32. doi: 10.1128/AEM.71.8.4822-4832.2005.
Stromatolites, organosedimentary structures formed by microbial activity, are found throughout the geological record and are important markers of biological history. More conspicuous in the past, stromatolites occur today in a few shallow marine environments, including Hamelin Pool in Shark Bay, Western Australia. Hamelin Pool stromatolites often have been considered contemporary analogs to ancient stromatolites, yet little is known about the microbial communities that build them. We used DNA-based molecular phylogenetic methods that do not require cultivation to study the microbial diversity of an irregular stromatolite and of the surface and interior of a domal stromatolite. To identify the constituents of the stromatolite communities, small subunit rRNA genes were amplified by PCR from community genomic DNA with universal primers, cloned, sequenced, and compared to known rRNA genes. The communities were highly diverse and novel. The average sequence identity of Hamelin Pool sequences compared to the >200,000 known rRNA sequences was only approximately 92%. Clone libraries were approximately 90% bacterial and approximately 10% archaeal, and eucaryotic rRNA genes were not detected in the libraries. The most abundant sequences were representative of novel proteobacteria (approximately 28%), planctomycetes ( approximately 17%), and actinobacteria (approximately 14%). Sequences representative of cyanobacteria, long considered to dominate these communities, comprised <5% of clones. Approximately 10% of the sequences were most closely related to those of alpha-proteobacterial anoxygenic phototrophs. These results provide a framework for understanding the kinds of organisms that build contemporary stromatolites, their ecology, and their relevance to stromatolites preserved in the geological record.
叠层石是由微生物活动形成的有机沉积结构,在整个地质记录中都有发现,是生物历史的重要标志。叠层石在过去更为显著,如今在一些浅海环境中仍有出现,包括西澳大利亚鲨鱼湾的哈梅林池。哈梅林池叠层石常被视为古代叠层石的现代类似物,但对于形成它们的微生物群落却知之甚少。我们使用基于DNA的分子系统发育方法(无需培养)来研究不规则叠层石以及穹顶状叠层石的表面和内部的微生物多样性。为了确定叠层石群落的组成成分,用通用引物通过PCR从群落基因组DNA中扩增小亚基rRNA基因,进行克隆、测序,并与已知的rRNA基因进行比较。这些群落具有高度的多样性和新颖性。与超过200,000个已知rRNA序列相比,哈梅林池序列的平均序列同一性仅约为92%。克隆文库中约90%为细菌,约10%为古细菌,文库中未检测到真核rRNA基因。最丰富的序列代表了新型变形菌(约28%)、浮霉菌(约17%)和放线菌(约14%)。长期以来被认为在这些群落中占主导地位的蓝细菌的序列占克隆的比例不到5%。约10%的序列与α-变形菌无氧光合营养菌的序列关系最为密切。这些结果为理解构建现代叠层石的生物种类、它们的生态学以及它们与地质记录中保存的叠层石的相关性提供了一个框架。