Collaborative Research: New Roles for Reactive Oxygen Species in Mediating Carbon Fluxes at the Terrestrial-Aquatic Interface

合作研究：活性氧在调节陆地-水生界面碳通量中的新作用

• 批准号: 2029645
• 负责人: William Arnold
• 金额: $ 29.9万
• 依托单位: University of Minnesota-Twin Cities
• 依托单位国家: 美国
• 项目类别: Standard Grant
• 财政年份: 2021
• 资助国家: 美国
• 起止时间: 2021-07-01 至 2024-06-30
• 项目状态: 已结题
• 来源: https://www.nsf.gov/awardsearch/showAward?AWD_ID=2029645&HistoricalAwards=false
• 关键词: Collaborative; Research; New; Roles; Reactive

Wetlands in the north central region of the United States are important ecosystems that play critical roles in the regional carbon cycle and are likely to be dramatically affected by climate change. Rates of greenhouse gas release from these wetlands may increase with warming and offset their ability to sequester carbon. By studying the chemical and microbiological processes in wetland sediments over space and time, predictions of the effects of climate change on these critical habitats will be possible. Documentation of the ecological importance of this region via photography will demonstrate the value of wetlands to a broad audience.The drivers of biogeochemical activity that dictate the emissions of carbon dioxide and methane in small, inland waters are poorly constrained, yet processes in these water bodies play an oversized role in understanding climate change. One process that is poorly understood is the role of chemical reactions in mediating carbon dioxide and methane formation in small lakes and wetlands, especially the abiotic production of reactive oxygen species (ROS) at the sediment-water interface (SWI). The hypothesis for this project is that the reaction of reduced soluble and particulate forms of iron, sulfur, and carbon with trace level oxygen to form ROS at the SWI is an under-appreciated, yet critical, control on microbiological activity and the cycling of carbon in small inland water bodies. Using a combination of field work in the prairie pothole region of North Dakota, controlled laboratory experiments, and mesocosm studies, this work will 1) identify the geochemical drivers of ROS generation at the SWI, 2) determine spatiotemporal patterns of linked pore water chemistry and ROS at the SWI, and 3) track the generation of specific labile carbon substrates produced through ROS-DOM reactions that affect rates of carbon mineralization and methane production in small lake and wetland sediments. A combination of in situ voltammetry measurements, detailed characterization of dissolved and particulate organic matter, iron, and sulfur species, and microbial -omics analyses will be used to understand the coupled biogeochemical processes. A key component of this work is understanding how abiotic ROS driven reactions at the sediment-water interface lead to turnover of terminal electron acceptors and generation of labile microbial substrates. Establishing a baseline understanding of these processes is needed to predict changes in carbon dioxide and methane fluxes under different climate scenarios. The collected data will enable understanding of how biogeochemical cycles are maintained through coupled abiotic/biotic pathways, and how these processes impact carbon cycling in aquatic environments. This approach is also applicable to other systems and the cycling of other elements, such as nitrogen, which may be especially important in urban wetland regions. The societal benefit will be improved understanding of processes that influence, and are influenced by, climate change. To reach as broad an audience as possible regarding the importance of this region, a photographer will document the landscape and its ecological function during field sampling trips.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.

美国中北部地区的湿地是重要的生态系统，在区域碳循环中发挥着关键作用，并可能受到气候变化的严重影响。这些湿地的温室气体释放率可能会随着变暖而增加，并抵消其固碳能力。通过研究湿地沉积物在空间和时间上的化学和微生物过程，将有可能预测气候变化对这些重要生境的影响。通过摄影记录这一地区的生态重要性将向广大观众展示湿地的价值。决定内陆小沃茨二氧化碳和甲烷排放的生物地球化学活动的驱动因素受到很大的限制，但这些水体中的过程在理解气候变化方面发挥着巨大的作用。一个过程是知之甚少的是化学反应的作用，介导的二氧化碳和甲烷的形成在小湖泊和湿地，特别是非生物生产的活性氧（ROS）在沉积物-水界面（SWI）。该项目的假设是，减少可溶性和颗粒形式的铁，硫和碳与微量氧在SWI形成ROS的反应是一个未被重视的，但关键的，控制微生物活性和碳在小内陆水体中的循环。通过结合北达科他州大草原坑洞区的野外工作、受控实验室实验和围隔生态系统研究，这项工作将1）确定SWI处ROS生成的地球化学驱动因素，2）确定SWI处相关孔隙水化学和ROS的时空模式，和3）追踪通过活性氧产生的特定不稳定碳底物的产生-影响小型湖泊和湿地沉积物中碳矿化和甲烷生成速率的DOM反应。结合原位伏安法测量，溶解和颗粒有机物，铁和硫物种的详细表征，和微生物组学分析将被用来了解耦合的地球化学过程。这项工作的一个关键组成部分是了解如何在沉积物-水界面的非生物活性氧驱动的反应，导致终端电子受体的营业额和不稳定的微生物底物的产生。为了预测不同气候情景下二氧化碳和甲烷通量的变化，需要建立对这些过程的基线了解。收集的数据将有助于了解生物地球化学循环如何通过耦合的非生物/生物途径维持，以及这些过程如何影响水生环境中的碳循环。这种方法也适用于其他系统和其他元素的循环，如氮，这可能是特别重要的城市湿地地区。社会效益将是提高对影响气候变化和受气候变化影响的过程的理解。为了让尽可能广泛的观众了解该地区的重要性，摄影师将在实地采样旅行期间记录景观及其生态功能。该奖项反映了NSF的法定使命，并通过使用基金会的知识价值和更广泛的影响审查标准进行评估，被认为值得支持。