Collaborative Research: Manganese(III)-driven carbon oxidation at oxic-anoxic interfaces

合作研究：含氧-缺氧界面上锰(III)驱动的碳氧化

• 批准号: 1852759
• 负责人: Jingdong Mao
• 金额: $ 5.8万
• 依托单位: Old Dominion University Research Foundation
• 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: 2019-05-01 至 2024-04-30
• 项目状态: 已结题
• 来源: https://www.nsf.gov/awardsearch/showAward?AWD_ID=1852759&HistoricalAwards=false
• 关键词: Collaborative; Research; Manganese; III; driven

Soils are a large and dynamic terrestrial of carbon on earth. How fast microbes oxidize carbon determines how much either stays in soils or is emitted as carbon dioxide. Even a small increase in soil carbon oxidation rate could increase the amount of carbon dioxide in the atmosphere, impacting global climate. Manganese (Mn) is an abundant and potent oxidizer, but its impact on the rate of soil carbon oxidation is not known. This project will provide new understanding of how manganese compounds change how fast carbon is oxidized in soils. This new scientific knowledge will help improve our predictions of future carbon dioxide emissions and will help society develop new strategies to limit emissions. This project will work with diversity programs on campus and in the local community to empower women and minority students to pursue STEM careers. The formation of Mn-based oxidants is emerging as a key regulator of C oxidation rates, and thus CO2 emissions, in soils. Although dissolved Mn(III) species are among the most potent oxidants in environmental systems, the controls on Mn(III)-driven carbon oxidation are virtually unknown. The overall objective of this project is to identify fundamental geochemical and microbial factors controlling the rate of Mn(III)-mediated carbon oxidation in soils. Our central hypothesis is that oxic-anoxic interfaces are "hotspots" for the enzymatic formation of dissolved Mn(III), which subsequently depolymerizes and solubilizes otherwise resistant organic matter, and so enhances microbial CO2 production. The proposed research integrates microsensor, spectroscopic, and multi-omics approaches to resolve coupled Mn and carbon cycles across fine-scale gradients in soils. To accomplish the overall objective, the specific aims are to (i) define the geochemical controls on Mn(III) formation along oxic-, (ii) identify the microbial drivers of Mn(III) formation, and (iii) assess the impact of Mn(III) formation on C oxidation at oxic-anoxic interfaces in soils. Disseminating the resulting dataset will support efforts to incorporate the coupling of Mn and C redox cycles into biogeochemical models. Integrating the highly significant Mn-dependence of C oxidation into models for the first time is expected to vastly improve accuracy in predicting environmental and human impacts on soil CO2 emissions. The project team will work to incorporate this multidisciplinary research effort into strategies to empower women and minority graduate, undergraduate and high school students to pursue STEM careers. A three-point plan integrates this research with direct interdisciplinary education and public outreach, which includes: (i) graduate training in biogeochemistry for one minority PhD student, (ii) opportunities for independent research for three minority undergraduate students in partnership with the Harvard Forest REU program, and (iii) multi-day workshops for a total of 45 female minority students from a local high school hosted in collaboration with Girls Inc. Holyoke, Massachusetts. Educational materials developed for the workshops will be disseminated through participation in the annual Massachusetts Envirothon. A thorough evaluation plan was developed in collaboration with Harvard Forest and Girls Inc. staff to measure the success of the proposed Broader Impacts activities.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.

土壤是地球上一个巨大且充满活力的碳陆地。微生物氧化碳的速度决定了有多少碳留在土壤中或以二氧化碳的形式排放。 即使土壤碳氧化率略有增加，也会增加大气中二氧化碳的含量，从而影响全球气候。锰（Mn）是一种丰富且有效的氧化剂，但其对土壤碳氧化速率的影响尚不清楚。该项目将为锰化合物如何改变土壤中碳的氧化速度提供新的认识。这些新的科学知识将有助于改善我们对未来二氧化碳排放的预测，并将帮助社会制定限制排放的新战略。该项目将与校园和当地社区的多元化计划合作，赋予女性和少数族裔学生追求 STEM 职业的能力。锰基氧化剂的形成正在成为土壤中碳氧化速率以及二氧化碳排放的关键调节剂。尽管溶解的 Mn(III) 物质是环境系统中最有效的氧化剂之一，但对 Mn(III) 驱动的碳氧化的控制实际上是未知的。该项目的总体目标是确定控制土壤中 Mn(III) 介导的碳氧化速率的基本地球化学和微生物因素。我们的中心假设是，含氧-缺氧界面是酶促形成溶解的 Mn(III) 的“热点”，随后 Mn(III) 解聚并溶解原本具有抗性的有机物，从而增强微生物 CO2 的产生。拟议的研究整合了微传感器、光谱学和多组学方法来解决土壤中细尺度梯度的耦合锰和碳循环。为了实现总体目标，具体目标是（i）定义沿好氧方向对 Mn(III) 形成的地球化学控制，(ii) 确定 Mn(III) 形成的微生物驱动因素，以及 (iii) 评估 Mn(III) 形成对土壤含氧-缺氧界面处 C 氧化的影响。传播所得数据集将支持将锰和碳氧化还原循环耦合纳入生物地球化学模型的努力。首次将碳氧化对锰的高度依赖性整合到模型中，预计将大大提高预测环境和人类对土壤二氧化碳排放影响的准确性。 该项目团队将努力将这一多学科研究工作纳入战略中，以赋予女性和少数族裔研究生、本科生和高中生追求 STEM 职业的能力。一项三点计划将这项研究与直接的跨学科教育和公共宣传相结合，其中包括：(i) 为一名少数族裔博士生提供生物地球化学研究生培训，(ii) 与哈佛森林 REU 项目合作，为三名少数族裔本科生提供独立研究的机会，以及 (iii) 与 Girls Inc. Holyoke 合作，为来自当地一所高中的总共​​ 45 名少数族裔女性学生举办多日讲习班， 马萨诸塞州。为讲习班编写的教育材料将通过参加一年一度的马萨诸塞州环境马拉松活动进行传播。与哈佛森林和女孩公司的工作人员合作制定了一项全面的评估计划，以衡量拟议的更广泛影响活动的成功程度。该奖项反映了 NSF 的法定使命，并通过使用基金会的智力优点和更广泛影响审查标准进行评估，被认为值得支持。