Banfield Jillian F, Verberkmoes Nathan C, Hettich Robert L, Thelen Michael P
Department of Earth and Planetary Science, and Environmental Science, Policy, and Management, University of California, Berkeley, CA 94720, USA.
OMICS. 2005 Winter;9(4):301-33. doi: 10.1089/omi.2005.9.301.
At the present time we know little about how microbial communities function in their natural habitats. For example, how do microorganisms interact with each other and their physical and chemical surroundings and respond to environmental perturbations? We might begin to answer these questions if we could monitor the ways in which metabolic roles are partitioned amongst members as microbial communities assemble, determine how resources such as carbon, nitrogen, and energy are allocated into metabolic pathways, and understand the mechanisms by which organisms and communities respond to changes in their surroundings. Because many organisms cannot be cultivated, and given that the metabolisms of those growing in monoculture are likely to differ from those of organisms growing as part of consortia, it is vital to develop methods to study microbial communities in situ. Chemoautotrophic biofilms growing in mine tunnels hundreds of meters underground drive pyrite (FeS(2)) dissolution and acid and metal release, creating habitats that select for a small number of organism types. The geochemical and microbial simplicity of these systems, the significant biomass, and clearly defined biological-inorganic feedbacks make these ecosystem microcosms ideal for development of methods for the study of uncultivated microbial consortia. Our approach begins with the acquisition of genomic data from biofilms that are sampled over time and in different growth conditions. We have demonstrated that it is possible to assemble shotgun sequence data to reveal the gene complement of the dominant community members and to use these data to confidently identify a significant fraction of proteins from the dominant organisms by mass spectrometry (MS)-based proteomics. However, there are technical obstacles currently restricting this type of "proteogenomic" analysis. Composite genomic sequences assembled from environmental data from natural microbial communities do not capture the full range of genetic potential of the associated populations. Thus, it is necessary to develop bioinformatics approaches to generate relatively comprehensive gene inventories for each organism type. These inventories are critical for expression and functional analyses. In proteomic studies, for example, peptides that differ from those predicted from gene sequences can be measured, but they generally cannot be identified by database matching, even if the difference is only a single amino acid residue. Furthermore, many of the identified proteins have no known function. We propose that these challenges can be addressed by development of proteogenomic, biochemical, and geochemical methods that will be initially deployed in a simple, natural model ecosystem. The resulting approach should be broadly applicable and will enhance the utility and significance of genomic data from isolates and consortia for study of organisms in many habitats. Solutions draining pyrite-rich deposits are referred to as acid mine drainage (AMD). AMD is a very prevalent, international environmental problem associated with energy and metal resources. The biological-mineralogical interactions that define these systems can be harnessed for energy-efficient metal recovery and removal of sulfur from coal. The detailed understanding of microbial ecology and ecosystem dynamics resulting from the proposed work will provide a scientific foundation for dealing with the environmental challenges and technological opportunities, and yield new methods for analysis of more complex natural communities.
目前,我们对微生物群落如何在其自然栖息地发挥功能知之甚少。例如,微生物如何相互作用以及与它们的物理和化学环境相互作用,并对环境扰动做出反应?如果我们能够监测代谢角色在微生物群落组装过程中如何在成员之间进行分配,确定碳、氮和能量等资源如何分配到代谢途径中,并了解生物体和群落对其周围环境变化做出反应的机制,我们或许就能开始回答这些问题。由于许多生物体无法培养,而且鉴于单一培养中生长的生物体的代谢可能与作为共生体一部分生长的生物体的代谢不同,因此开发原位研究微生物群落的方法至关重要。在地下数百米的矿井隧道中生长的化学自养生物膜驱动黄铁矿(FeS₂)溶解以及酸和金属的释放,创造了选择少数生物体类型的栖息地。这些系统的地球化学和微生物简单性、大量的生物量以及明确的生物 - 无机反馈使得这些生态系统微观世界成为开发研究未培养微生物共生体方法的理想选择。我们的方法始于从随时间和在不同生长条件下采样的生物膜中获取基因组数据。我们已经证明,可以组装鸟枪法序列数据以揭示主要群落成员的基因组成,并使用这些数据通过基于质谱(MS)的蛋白质组学自信地鉴定主要生物体中很大一部分蛋白质。然而,目前存在技术障碍限制了这种“蛋白质基因组”分析。从天然微生物群落的环境数据组装的复合基因组序列并未涵盖相关种群的全部遗传潜力。因此,有必要开发生物信息学方法来为每种生物体类型生成相对全面详尽的基因清单。这些清单对于表达和功能分析至关重要。例如,在蛋白质组学研究中,可以测量与基因序列预测不同的肽段,但即使差异仅为单个氨基酸残基,它们通常也无法通过数据库匹配来鉴定。此外,许多已鉴定的蛋白质没有已知功能。我们建议,可以通过开发蛋白质基因组学、生物化学和地球化学方法来应对这些挑战,这些方法最初将部署在一个简单的自然模型生态系统中。由此产生的方法应该具有广泛的适用性,并将提高来自分离株和共生体基因组数据在研究许多栖息地生物体方面的效用和重要性。从富含黄铁矿的矿床中排出的溶液被称为酸性矿山排水(AMD)。AMD是一个与能源和金属资源相关的非常普遍的国际环境问题。定义这些系统的生物 - 矿物学相互作用可用于高效能的金属回收和从煤中去除硫。拟开展的工作所产生的对微生物生态学和生态系统动态的详细理解将为应对环境挑战和技术机遇提供科学基础,并产生用于分析更复杂自然群落的新方法。