Collaborative Research (ETBC): Climate Warming and Northern Peatland Decomposition, Accumulation and Carbon Sequestration Examined Through Molecular and Paleohydrological Analysis

合作研究（ETBC）：通过分子和古水文分析检查气候变暖和北部泥炭地的分解、积累和碳封存

• 批准号: 0843685
• 负责人: Glen MacDonald
• 金额: $ 18.93万
• 依托单位: University of California-Los Angeles
• 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: 2009-10-01 至 2013-09-30
• 项目状态: 已结题
• 来源: https://www.nsf.gov/awardsearch/showAward?AWD_ID=0843685&HistoricalAwards=false
• 关键词: Collaborative; Research; ETBC; Climate; Warming

The widespread occurrence of northern peatlands (above 50°N) is a distinctive and important attribute of the subarctic system that has global ramifications. The net sequestration of atmospheric carbon in northern peatlands (274-489 Pg C) has played a significant role in the global carbon cycle during the Holocene and will continue to be an important factor in the carbon cycle of the Anthropocene. A clearer understanding of how climate affects peat accumulation and decomposition rates, and ultimately net carbon sequestration, is critical for predicting how current and future warming will impact northern peatlands and the global carbon cycle. We propose a novel approach to gain a mechanistic understanding of the role of climate warming on rates of peat decomposition and net accumulation in a network of cores collected from the West Siberian Lowland (Russia), under a previous NSF-supported project, and the James Bay Lowland (Canada), under a separate NSF-supported project. Net rates of peat accumulation and carbon sequestration will be calculated from radiocarbon-dated cores. Hydrological changes, represented by changes in water table depth, will be directly calculated for the core sites using testate amoebae analysis. Detailed chemical characterizations of peat samples will be used to develop molecular indicators of peat decomposition. These molecular indicators and diagenesis models will then be applied to quantify rates and extent of peat decomposition and the relative importance of production and decomposition in determining carbon sequestration rates. Instrumental climate data and published paleoclimate research will be used to examine linkages among climate, hydrology, decomposition and accumulation and the mechanisms controlling the balance between peat production and decomposition. In view of current and anticipated warming of the subarctic over the next century, the proposed studies will focus on the Holocene Thermal Maximum (~8,000-4,000 Cal yr BP), the Medieval Warm Period (~1,100 to 700 Cal yr BP) and the comparative impacts of Modern Warming. Climate warming is having a disproportionately large affect on the hydrology, biota and biogeochemical cycles of the subarctic system. Northern peatlands have been major players in soil and atmospheric carbon cycling during the Holocene, and this study will provide a clearer picture of how climate shapes these processes. Novel approaches and potentially transformative concepts will be developed to provide a quantitative understanding of the mechanisms controlling carbon sequestration and release in northern peatlands. The research will provide a data base of over 20,000 detailed assays on past and present peatland biogeochemical conditions from ~40 core sites and ~100 surface sites in Siberia and central Canada. This project will provide training, experience and support for a postdoctoral associate in Benner?s laboratory at USC and a graduate student in MacDonald?s laboratory at UCLA. They will present their data at scientific meetings and prepare articles for publication in peer-reviewed journals. Benner and MacDonald teach undergraduate and graduate classes that cover various aspects of the global carbon cycle and climate change, and data collected from this project will be used as specific examples in these classes. This approach of bringing information from active research programs into the classroom has proven to be very effective for increasing student awareness and interest in science. An undergraduate student will be recruited to participate in this project (Benner?s laboratory) as part of the Magellan Scholars program at USC to provide research experiences for undergraduates. Results will be posted on research websites and data contributed to appropriate national and international data bases for widespread use.

北方泥炭地（50°N以上）的广泛存在是具有全球影响的亚北极系统的一个独特而重要的属性。北方泥炭地大气碳的净固存（274-489 Pg C）在全新世全球碳循环中发挥了重要作用，并将继续成为人类世碳循环的重要因素。更清楚地了解气候如何影响泥炭的积累和分解速率，以及最终的净碳固存，对于预测当前和未来的变暖将如何影响北方泥炭地和全球碳循环至关重要。我们提出了一种新的方法，以获得一个机械的理解，从西西伯利亚低地（俄罗斯），根据以前的NSF支持的项目，和詹姆斯湾低地（加拿大），根据一个单独的NSF支持的项目收集的核心网络的泥炭分解和净积累率的气候变暖的作用。泥炭积累和碳固存的净速率将根据放射性碳定年岩心计算。水文变化，表现为地下水位深度的变化，将直接计算为核心网站使用遗嘱变形虫分析。泥炭样品的详细化学特征将被用来开发泥炭分解的分子指标。这些分子指标和成岩作用模型将被应用于量化泥炭分解的速率和程度，以及生产和分解在确定碳固存率方面的相对重要性。将利用仪器气候数据和已发表的古气候研究成果来研究气候、水文、分解和积累之间的联系以及控制泥炭生产和分解之间平衡的机制。考虑到目前和下个世纪亚北极变暖的预期，拟议的研究将侧重于全新世热最大期（约8000 - 4000 Cal yr BP）、中世纪温暖期（约1,100 - 700 Cal yr BP）和现代变暖的比较影响。气候变暖正在对亚北极系统的水文、生物区系和地球化学循环产生不成比例的巨大影响。北方泥炭地一直是全新世土壤和大气碳循环的主要参与者，这项研究将更清楚地了解气候如何塑造这些过程。将开发新的方法和潜在的变革性概念，以提供对控制北方泥炭地碳固存和释放机制的定量理解。这项研究将提供一个数据库，其中包含来自西伯利亚和加拿大中部约40个核心站点和约100个地表站点的过去和现在泥炭地地球化学条件的20，000多个详细分析。这个项目将提供培训，经验和支持的博士后助理在本纳？在南加州大学的实验室和麦克唐纳的研究生？在加州大学洛杉矶分校的实验室。他们将在科学会议上展示他们的数据，并准备在同行评审的期刊上发表文章。Benner和MacDonald教授本科和研究生课程，涵盖全球碳循环和气候变化的各个方面，从该项目收集的数据将用作这些课程的具体示例。这种将积极研究项目的信息带入课堂的方法已被证明对提高学生对科学的认识和兴趣非常有效。一名本科生将被招募参加这个项目（本纳？作为南加州大学麦哲伦学者计划的一部分，为本科生提供研究经验。研究结果将公布在研究网站上，数据将输入适当的国家和国际数据库，供广泛使用。