Collaborative Research: Key Microbial Processes in Oxygen Minimum Zones: From In Situ Community Rate Measurements to Single Cells

合作研究：最低氧气区的关键微生物过程：从原位群落速率测量到单细胞

• 批准号: 1924424
• 负责人: Gordon Taylor
• 金额: $ 51.5万
• 依托单位: SUNY at Stony Brook
• 依托单位国家: 美国
• 项目类别: Standard Grant
• 财政年份: 2019
• 资助国家: 美国
• 起止时间: 2019-10-01 至 2024-09-30
• 项目状态: 已结题
• 来源: https://www.nsf.gov/awardsearch/showAward?AWD_ID=1924424&HistoricalAwards=false
• 关键词: Collaborative; Research; Key; Microbial; Processes

Oxygen availability shapes the distributions and activities of marine organisms. Ongoing human activities and climate change are expected to lead to expansion and intensification of already large oxygen-stressed areas of the coastal and open ocean. Decreases in ocean oxygen have significant ecological consequences, including habitat loss for migratory and bottom-dwelling organisms, modification of the marine food web, and production of trace gases with pronounced feedbacks on climate, such as methane and nitrous oxide. Intense chemical cycling by microorganisms occurs in oxygen-depleted marine habitats. However, a full understanding of the consequences for marine ecosystems is hampered by limited knowledge of actual rates of key microbiological processes and dynamics of the microorganisms mediating them. This study combines novel methods and sampling techniques to understand how these processes are influenced by changes in oxygen concentration to inform predictions of important chemical exchanges within a changing ocean and its production of climate-active gases. This deeply collaborative project trains undergraduates (four of whom participate on the cruise), a graduate student and a postdoctoral fellow. Outreach takes place in middle and high schools and through social media. Data and samples from the cruise are integrated in coursework.Oxygen depletion alters cycling of major elements (especially carbon, nitrogen, and sulfur) as well as food web functionality. This project addresses major gaps in our knowledge of oxygen minimum zone (OMZ) processes by applying in situ approaches to more accurately measure rates of several key microbial processes (chemoautotrophy, denitrification, anammox, sulfate reduction and sulfide oxidation) central to marine biogeochemical cycling. This work studies the Eastern Tropical North Pacific OMZ, the largest open ocean oxygen-depleted system, to 1) determine the in situ rates of microbial processes involved in carbon, nitrogen, and sulfur cycling, 2) reveal the genomic blueprint of active single cells involved in these processes, and 3) obtain estimates of the relative contributions of the dominant chemoautotrophic and heterotrophic groups to the measured rates. This work include applies cutting-edge equipment for in situ sampling and incubations that minimize artifacts associated with traditional water sampling approaches, allowing more accurate estimates of rates of important biogeochemical processes. Additionally, rate measurements of relatively undisturbed bulk and fractionated water samples make it easier to distinguish the potential role of particle-associated microorganisms in these OMZ processes. Single cell sorting of microorganisms using a fluorescent dye indicative of cell activity together with metatranscriptomics informs on metabolic pathways used for key processes by active microbial community members, as well as the potential coupling of chemoautotrophy and nitrogen or/and sulfur cycling. By combining stable isotope probing, fluorescence in situ hybridization and single cell Raman microspectrometry the relative activity levels of different microbial phylotypes involved in chemoautotrophic and heterotrophic elemental cycling are assessed.This award reflects NSF's statutory mission and has been deemed worthy of support through evaluation using the Foundation's intellectual merit and broader impacts review criteria.

氧气的可用性决定了海洋生物的分布和活动。持续的人类活动和气候变化预计将导致沿海和公海本已大片缺氧区域的扩大和加剧。海洋氧气的减少会产生重大的生态后果，包括迁徙和底栖生物的栖息地丧失、海洋食物网的改变以及对气候有明显反馈作用的痕量气体的产生，例如甲烷和一氧化二氮。微生物的强烈化学循环发生在缺氧的海洋栖息地。然而，对关键微生物过程的实际速率和介导这些过程的微生物动态的了解有限，阻碍了对海洋生态系统后果的充分了解。这项研究结合了新颖的方法和采样技术，以了解这些过程如何受到氧气浓度变化的影响，从而为不断变化的海洋内重要的化学交换及其气候活跃气体的产生提供预测。这个深度合作项目培训本科生（其中四人参加了邮轮）、研究生和博士后。外展活动在初中和高中通过社交媒体进行。来自巡航的数据和样本被整合到课程作业中。缺氧会改变主要元素（特别是碳、氮和硫）的循环以及食物网功能。该项目通过应用原位方法更准确地测量海洋生物地球化学循环核心的几个关键微生物过程（化学自养、反硝化、厌氧氨氧化、硫酸盐还原和硫化物氧化）的速率，弥补了我们对最低氧区（OMZ）过程知识的主要空白。这项工作研究东部热带北太平洋 OMZ（最大的公海缺氧系统），目的是 1) 确定参与碳、氮和硫循环的微生物过程的原位速率，2) 揭示参与这些过程的活跃单细胞的基因组蓝图，以及 3) 获得主要化能自养和异养群对 测量的速率。这项工作包括应用尖端设备进行原位采样和孵化，最大限度地减少与传统水采样方法相关的人工制品，从而能够更准确地估计重要生物地球化学过程的速率。此外，相对未受干扰的大量水样和分馏水样的速率测量使得更容易区分颗粒相关微生物在这些 OMZ 过程中的潜在作用。使用指示细胞活性的荧光染料对微生物进行单细胞分选，并结合元转录组学，了解活跃微生物群落成员用于关键过程的代谢途径，以及化学自养与氮或/和硫循环的潜在耦合。通过结合稳定同位素探测、荧光原位杂交和单细胞拉曼显微光谱法，评估参与化能自养和异养元素循环的不同微生物系统型的相对活性水平。该奖项反映了 NSF 的法定使命，并通过使用基金会的智力价值和更广泛的影响审查标准进行评估，被认为值得支持。