Collaborative Research: Ecology of microbial mats at seamount associated Fe-rich hydrothermal vent systems

合作研究：海山相关富铁热液喷口系统微生物垫的生态学

• 批准号: 1155756
• 负责人: Craig Moyer
• 金额: $ 60.26万
• 依托单位: Western Washington University
• 依托单位国家: 美国
• 项目类别: Standard Grant
• 财政年份: 2012
• 资助国家: 美国
• 起止时间: 2012-07-01 至 2017-12-31
• 项目状态: 已结题
• 来源: https://www.nsf.gov/awardsearch/showAward?AWD_ID=1155756&HistoricalAwards=false
• 关键词: Collaborative; Research; Ecology; microbial; mats

A grand challenge in microbial ecology is to understand what drives the structure of microbial communities. A recently discovered novel class of Proteobacteria, the Zetaproteobacteria, are associated with microbial mats at iron rich hydrothermal vents at submarine volcanoes deep in the ocean. These bacteria only grow using iron as an energy source and fix carbon dioxide. Within iron rich microbial mats, Zetaproteobacteria are the dominant bacterial population; however they are rare in most other deep-sea or marine habitats, suggesting they may be restricted to specific niches characterized by gradients of oxygen and iron. Recent discoveries have expanded their range to fluids collected from deep ocean crust boreholes, iron deposits in coastal saltmarshes, and with steel associated bio-corrosion, demonstrating that marine Zetaproteobacteria are cosmopolitan. A unique property of these marine iron oxidizing bacteria is that they produce morphologically distinct iron oxide structures in the form of filamentous sheaths or stalk-like structures. These structures are easily recognized by light microscopy, and electron microscopy is beginning to reveal subtle differences among them that may be diagnostic of different populations of iron oxidizing bacteria. Another unusual aspect of iron oxidizing bacteria is that they produce large quantities of oxides with relatively little bacterial biomass. As a result, the oxides form a matrix that influences water and nutrient flow in the microbial mats where they grow, and in turn, may influence the growth of other groups of bacteria and archaea that live in the mats. In an ecological context, the PIs believe this makes them a keystone species that form the predominant structural matrix of the mat, and engineer an environment conducive for growth of specific bacterial populations within the mat ecosystem. The PIs propose to use high resolution mat sampling techniques to investigate the architecture of mat ecosystems and couple these with modern molecular methods (i.e., single-cell metagenomics) and geochemical measurements of the vent fluid to couple morphological and functional diversity to phylogenetic and physiological diversity. Because the Zetaproteobacteria are ancient, have unique metabolic and morphological attributes, and appear to be restricted to a well-defined habitat, they offer an interesting model for understanding fundamental ecological concepts that drive microbial diversity and evolution. Broader Impacts: A better understanding of iron oxidizing bacteria that include Zetaproteobacteria is of fundamental interest to scientists interested in areas of earth science and oceanography because they illustrate how microbes can fundamentally influence geochemical cycling and mineral deposition. Furthermore, morphological structures similar to those produced by Zetaproteobacteria can still be identified hundreds of millions (and possibly billions) of years back in the geological record, making them of paleontological, and potentially of exobiological, interest. As knowledge of extant populations grow, it is possible they will also help to inform us of environmental change in past Earth history. A wealth of educational and outreach opportunities will be made possible by this work, including graduate and postdoctoral education, research experiences for undergraduates, and teacher training. In addition the participating scientists are involved in a number of programs to make the general public aware of the process of how scientific research is conducted, and how discoveries of a fundamental nature can ultimately benefit humankind.

微生物生态学的一个重大挑战是了解是什么驱动了微生物群落的结构。最近发现的一类新的变形菌，Zetaproteobacteria，与海洋深处海底火山富铁热液喷口的微生物垫有关。这些细菌只以铁作为能源生长，并固定二氧化碳。在富含铁的微生物垫中，Zetaproteobacteria是占主导地位的细菌种群;然而，它们在大多数其他深海或海洋栖息地中很少见，这表明它们可能仅限于以氧和铁梯度为特征的特定生态位。最近的发现已将其范围扩大到从深海地壳钻孔收集的流体、沿海盐沼中的铁矿床以及与钢铁相关的生物腐蚀，表明海洋Zetaproteobacteria是世界性的。这些海洋铁氧化细菌的一个独特性质是它们以丝状鞘或茎状结构的形式产生形态上不同的氧化铁结构。这些结构很容易通过光学显微镜识别，电子显微镜开始揭示它们之间的细微差异，这些差异可能是不同铁氧化细菌种群的诊断。铁氧化细菌的另一个不寻常的方面是，它们产生大量的氧化物，而细菌生物量相对较少。因此，氧化物形成一种基质，影响它们生长的微生物垫中的水和营养物流动，进而可能影响生活在垫中的其他细菌和古菌群的生长。在生态背景下，PI认为这使它们成为形成垫的主要结构基质的关键物种，并设计有利于垫生态系统内特定细菌种群生长的环境。PI建议使用高分辨率垫采样技术来研究垫生态系统的结构，并将其与现代分子方法（即，单细胞宏基因组学）和对喷口流体的地球化学测量，将形态和功能多样性与系统发育和生理多样性联系起来。由于Zetaproteobacteria是古老的，具有独特的代谢和形态属性，并且似乎仅限于一个明确的栖息地，它们为理解驱动微生物多样性和进化的基本生态概念提供了一个有趣的模型。更广泛的影响：更好地了解包括Zetaproteobacteria在内的铁氧化细菌对于对地球科学和海洋学领域感兴趣的科学家来说具有根本意义，因为它们说明了微生物如何从根本上影响地球化学循环和矿物沉积。 此外，与Zetaproteobacteria产生的形态结构相似的形态结构仍然可以在数亿年（可能是数十亿年）前的地质记录中找到，使它们成为古生物学和潜在的外星生物学的兴趣。随着对现存种群的了解的增加，它们也可能有助于我们了解过去地球历史中的环境变化。 这项工作将提供丰富的教育和推广机会，包括研究生和博士后教育，本科生的研究经验和教师培训。此外，参与的科学家还参与了一些方案，以使公众了解科学研究的进行过程，以及基本性质的发现如何最终造福人类。