Microbial carbon and sulfur cycling in the hydrothermally altered sediments of Guaymas Basin

瓜伊马斯盆地热液蚀变沉积物中的微生物碳和硫循环

• 批准号: 0647633
• 负责人: Andreas Teske
• 金额: $ 69.65万
• 依托单位: University of North Carolina at Chapel Hill
• 依托单位国家: 美国
• 项目类别: Standard Grant
• 财政年份: 2007
• 资助国家: 美国
• 起止时间: 2007-06-01 至 2012-05-31
• 项目状态: 已结题
• 来源: https://www.nsf.gov/awardsearch/showAward?AWD_ID=0647633&HistoricalAwards=false
• 关键词: Microbial; carbon; sulfur; cycling; hydrothermally

While microbial communities in marine sediments are generally sustained by sedimentation of organic matter from the water column, the Guaymas Basin hydrothermal sediments provide a model system for the microbial utilization and transformation of thermally released microbial substrates from deeply buried marine organic matter. As a working hypothesis, the physiologically distinct, layered microbial communities force the geothermally produced substrates through a double "microbial gauntlet" of anaerobic metabolism and autotrophic carbon fixation, where terminal anaerobic degradation of organic matter is performed by methanogenic and methane-oxidizing archaea, by sulfate-reducing bacteria and archaea, and potentially by novel subsurface archaeal populations within the upper sediments, while inorganic and organic remineralization products are assimilated by sulfur-oxidizing Beggiatoa mats at the sediment surface. This project will provide a quantitative understanding of how the dense and highly active benthic microbial populations of the Guaymas system utilize and recycle organic and inorganic carbon and sulfur of subsurface origin, how geochemical controls affect the community structure, and how uncultured, globally occurring subsurface archaea and bacteria thrive in their sediment habitat. To analyze the complex interplay of thermogenic and biogenic carbon sources and sinks, and the role of uncultured microbial populations in these processes, geochemical and molecular-biological approaches will be undertaken. The microbial community composition and activity patterns will be analyzed quantitatively. Carbon substrate profiles and microbial process rates (sulfate reduction, methanogenesis, methane oxidation) across hydrothermally active sediment sites will be measured and correlated to variations in microbial populations. The Guaymas Basin vents can serve as a model system for key linkages of the microbial and geological carbon and sulfur cycles, and shed new light on the roles of microorganisms as chemical catalysts of the marine environment and the marine subsurface. To tap into the great potential of Guaymas for teaching of biological-geological linkages in marine science, this project has initiated outreach projects with the Biodiversity Education and Public Outreach (BEPO) team and its Micros*cope resource at the Marine Biological Laboratory in Woods Hole, which also targets science educators and schools of non-english speaking minority communities. In addition, the Guaymas project will enhance undergraduate and graduate teaching, and provide hands-on research opportunities for graduate and undergraduate students.

虽然海洋沉积物中的微生物群落通常是由水柱中有机物的沉积维持的，但瓜伊马斯盆地热液沉积物为微生物利用和转化深埋海洋有机物中热释放的微生物基质提供了一个模型系统。 作为一个工作假设，生理上不同的分层微生物群落迫使地热产生的基质通过厌氧代谢和自养碳固定的双重“微生物手套”，其中有机物质的终端厌氧降解由产甲烷和甲烷氧化古菌、硫酸盐还原菌和古菌以及可能由上部沉积物内的新型地下古菌种群进行，而无机和有机矿化产物则被沉积物表面的硫氧化贝氏垫同化。 该项目将提供一个定量的了解，瓜伊马斯系统的密集和高度活跃的底栖微生物种群如何利用和回收地下来源的有机和无机碳和硫，地球化学控制如何影响社区结构，以及未培养的，全球发生的地下古菌和细菌如何在其沉积物栖息地茁壮成长。为了分析生热和生物源碳源和汇的复杂相互作用，以及未培养的微生物种群在这些过程中的作用，将采用地球化学和分子生物学方法。将对微生物群落组成和活动模式进行定量分析。 将测量热液活跃沉积物地点的碳基质概况和微生物过程速率（硫酸盐还原、甲烷生成、甲烷氧化），并将其与微生物种群的变化联系起来。瓜伊马斯盆地喷口可以作为微生物和地质碳硫循环关键联系的模型系统，并为微生物作为海洋环境和海洋地下化学催化剂的作用提供新的线索。为了挖掘瓜伊马斯在海洋科学生物-地质联系教学方面的巨大潜力，该项目与生物多样性教育和公共宣传小组及其在伍兹霍尔海洋生物实验室的微型科普资源一起发起了宣传项目，其对象也是科学教育工作者和非英语少数民族社区的学校。此外，瓜伊马斯项目将加强本科生和研究生的教学，并为研究生和本科生提供动手研究的机会。