Collaborative Research: MSB: Links Between Soil Biogeochemistry and Microbial Community Dynamics Along Recently Deglaciated Chronosequences

合作研究：MSB：土壤生物地球化学和微生物群落动态与最近消融时间序列之间的联系

• 批准号: 0922306
• 负责人: Cory Cleveland
• 金额: $ 17.64万
• 依托单位: University of Montana
• 依托单位国家: 美国
• 项目类别: Standard Grant
• 财政年份: 2009
• 资助国家: 美国
• 起止时间: 2009-09-01 至 2014-08-31
• 项目状态: 已结题
• 来源: https://www.nsf.gov/awardsearch/showAward?AWD_ID=0922306&HistoricalAwards=false
• 关键词: Collaborative; Research; MSB; Links; Between

Studies of how plant communities assemble and shift on landscapes created by receding glaciers have been integral in developing the theoretical bases of nutrient cycling, organismal interactions, and community dynamics in the face of environmental change. Indeed, the relative simplicity of these 'young' (geologically speaking) systems has revealed patterns in ecosystem structure and function that often also apply across a wide range of older, more complex environments. Although soil microorganisms regulate nutrient cycling reactions with regional to global importance, there is no parallel understanding of how these communities come together and change through time. This work will address three hypotheses which relate microbial community structure and soil nutrient status across newly deglaciated sites in three geographically, geologically and climatically disparate locations (Alaska, Peru and Montana). An array of techniques, including newly developed methods in high-throughput DNA sequencing and bioinformatics, microbial process measurements, and field manipulations will be replicated at the three different sites, and are designed to reveal broadly applicable patterns that govern early microbial community development. The project will support three graduate and two undergraduate students, including broadening participation from Native Alaskans at the University of Alaska, Southeast. Additionally, ecosystem science learning will be extended to a high school that serves "at risk" students, and students from underrepresented groups in science, by developing a new course using recently deglaciated soils as model systems for students to understand the relationships between nutrient cycling and biodiversity. The PIs will also work closely with the United States Forest Service staff at the Mendenhall Visitor Center to integrate the results of this project into interpretive programs and displays.

关于植物群落如何在冰川消退所形成的景观上聚集和转移的研究，对于发展面对环境变化的养分循环、有机相互作用和群落动态的理论基础是不可或缺的。事实上，这些“年轻”（从地质学角度来说）系统的相对简单性揭示了生态系统结构和功能的模式，这些模式通常也适用于各种更古老、更复杂的环境。尽管土壤微生物调节养分循环反应具有区域性和全球性的重要性，但对于这些群落如何聚集在一起并随着时间的推移而变化，还没有类似的理解。这项工作将提出三个假设，这些假设涉及三个地理、地质和气候不同的地点（阿拉斯加、秘鲁和蒙大拿）新消融地点的微生物群落结构和土壤养分状况。一系列技术，包括新开发的高通量 DNA 测序和生物信息学方法、微生物过程测量和现场操作，将在三个不同的地点进行复制，旨在揭示控制早期微生物群落发展的广泛适用的模式。 该项目将支持三名研究生和两名本科生，包括扩大东南阿拉斯加大学阿拉斯加原住民的参与。此外，生态系统科学学习将扩展到为“处于危险中”的学生和来自科学领域代表性不足群体的学生提供服务的高中，通过开发一门新课程，使用最近消融的土壤作为模型系统，让学生了解养分循环与生态系统之间的关系。生物多样性。 PI 还将与门登霍尔游客中心的美国林务局工作人员密切合作，将该项目的成果整合到解说节目和展示中。