NNA: Collaborative Research: MSB-FRA: Peat Expansion in Arctic Tundra - Pattern, Process, and the Implication for the Carbon Cycle (TundraPEAT)

NNA：合作研究：MSB-FRA：北极苔原泥炭扩张 - 模式、过程以及对碳循环的影响 (TundraPEAT)

• 批准号: 1802832
• 负责人: Qianlai Zhuang
• 金额: $ 30.45万
• 依托单位: Purdue University
• 依托单位国家: 美国
• 项目类别: Standard Grant
• 财政年份: 2018
• 资助国家: 美国
• 起止时间: 2018-08-01 至 2024-07-31
• 项目状态: 已结题
• 来源: https://www.nsf.gov/awardsearch/showAward?AWD_ID=1802832&HistoricalAwards=false
• 关键词: NNA; Collaborative; Research; MSB; FRA

Amplified Arctic warming in recent decades has caused a multitude of changes in terrestrial ecosystems that have potential for strong feedbacks to the global system. Arctic vegetation greening may not necessarily result in increases in carbon sequestration in Arctic tundra due to complex and uncertain soil processes. Arctic tundra tends to have a thicker organic soil horizon (peat) than most other zonal biomes; research shows that peatlands comprise a sustained carbon sink. If shallow peatlands are widespread throughout the Arctic, the overall net carbon storage capacity of tundra might be underestimated globally. However, the factors controlling the formation, distribution, and dynamics of these peat patches across the Arctic are not well understood. The overall goal of the project is to understand organic soil (peat) accumulation processes in the tundra biome and to assess the role of peat in regional and pan-Arctic carbon budgets at decadal and centennial timescales. The project will examine potential peat migration/expansion frontiers in a warming Arctic and their significance in the regional and pan-Arctic carbon cycle. The project will train undergraduates, graduate students, and postdocs from diverse socio-economic and cultural backgrounds in both data analysis and modeling. The public education and outreach program includes STEM activities involving middle and high school students and a symposium on Arctic environments. The understanding of environmental conditions and processes that control the formation and northward migrations of the green peat frontier will inform Arctic stakeholders in their use of natural resources.This multidisciplinary research team of researchers will integrate (1) new data collection from multiple tundra sites along the northernmost peat-forming frontiers of the North American Arctic, together with (2) laboratory incubation experiments, (3) a synthesis of existing data from the tundra and boreal biomes, and (4) ecosystem-scale process model simulations. The overarching question is: will the warming Arctic transform into a peat-rich landscape, as the boreal zone is now, or are there essential conditions lacking in a warming Arctic that will prevent this? To address this broad question, the research focuses on two key elements of the Arctic peat-forming ecosystems: peat patches, and the role of Sphagnum in the formation, persistence, and rapid rates of carbon sequestration of these potentially incipient peatlands. Using observational, experimental, and modeling results, along with synthesis products from a coordinated international research network, the research team will test hypotheses on (1) the ages, carbon accumulation rates, and continental pattern of these rapidly forming and migrating peat patches; (2) the various responses of production and decomposition processes to temperature and moisture change; and (3) the role of Sphagnum in modifying microclimate and shifting balance between their productivity and decomposability.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.

近几十年来，北极变暖加剧，导致陆地生态系统发生了许多变化，这些变化有可能对全球系统产生强烈的反馈。由于复杂和不确定的土壤过程，北极植被绿化不一定会导致北极苔原碳固存的增加。北极苔原的有机土壤层（泥炭）往往比大多数其他地带性生物群落更厚;研究表明，泥炭地包括一个持续的碳汇。如果浅泥炭地在整个北极地区广泛分布，那么全球冻土带的整体净碳储存能力可能会被低估。然而，控制这些泥炭斑块的形成，分布和动态的因素还没有得到很好的理解。该项目的总体目标是了解苔原生物群落中有机土壤（泥炭）的积累过程，并评估泥炭在十年和百年时间尺度上在区域和泛北极碳收支中的作用。该项目将研究北极变暖中潜在的泥炭迁移/扩张边界及其在区域和泛北极碳循环中的意义。该项目将培训来自不同社会经济和文化背景的本科生，研究生和博士后进行数据分析和建模。公共教育和推广计划包括涉及初中和高中学生的STEM活动以及关于北极环境的研讨会。对控制绿色泥炭边界形成和向北迁移的环境条件和过程的了解将为北极利益相关者利用自然资源提供信息。这个多学科研究团队的研究人员将整合（1）从北美北极最北端泥炭形成边界沿着多个苔原地点收集的新数据，以及（2）实验室孵化实验，（3）冻土带和北方生物群落现有数据的综合;（4）生态系统尺度过程模型模拟。首要问题是：变暖的北极是否会像现在的北方地区一样变成一个泥炭丰富的景观，或者在变暖的北极缺乏必要的条件来阻止这一点？为了解决这个广泛的问题，研究重点是北极泥炭形成生态系统的两个关键要素：泥炭斑块，泥炭藓在这些潜在的初期泥炭地的形成，持久性和快速固碳率中的作用。利用观测、实验和模拟结果，沿着来自一个协调的国际研究网络的综合产品，研究小组将检验以下假设：（1）这些快速形成和迁移的泥炭斑块的年龄、碳积累速率和大陆格局;（2）生产和分解过程对温度和湿度变化的各种反应;及（3）泥炭藓在改变微气候和改变其生产力与分解性之间的平衡方面的作用。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。

项目成果

Improved global wetland carbon isotopic signatures support post-2006 microbial methane emission increase

• DOI: 10.1038/s43247-022-00488-5
• 发表时间: 2022-07
• 期刊: Communications Earth & Environment
• 影响因子: 7.9
• 作者: Y. Oh;Q. Zhuang;L. Welp;Licheng Liu;X. Lan;S. Basu;E. Dlugokencky;L. Bruhwiler;John B. Miller;S. Michel;S. Schwietzke;P. Tans;P. Ciais;J. Chanton

Modeling Carbon Accumulation and Permafrost Dynamics of Northern Peatlands Since the Holocene

• DOI: 10.1029/2022jg007009
• 发表时间: 2022-11
• 期刊: Journal of Geophysical Research: Biogeosciences
• 作者: Bailu Zhao;Q. Zhuang;S. Frolking

Peatlands and their carbon dynamics in northern high latitudes from 1990 to 2300: a process-based biogeochemistry model analysis

• DOI: 10.5194/bg-20-251-2023
• 发表时间: 2023-01
• 期刊: Biogeosciences
• 影响因子: 4.9
• 作者: Bailu Zhao;Q. Zhuang

Modeling Holocene Peatland Carbon Accumulation in North America

模拟北美全新世泥炭地碳积累

• DOI: 10.1029/2019jg005230
• 发表时间: 2020
• 期刊: Journal of Geophysical Research: Biogeosciences
• 作者: Zhuang, Qianlai;Wang, Sirui;Zhao, Bailu;Aires, Filipe;Prigent, Catherine;Yu, Zicheng;Keller, Jason K.;Bridgham, Scott
• 通讯作者: Bridgham, Scott

Peatland Heterogeneity Impacts on Regional Carbon Flux and Its Radiative Effect Within a Boreal Landscape

• DOI: 10.1029/2021jg006774
• 发表时间: 2022-09
• 期刊: Journal of Geophysical Research: Biogeosciences
• 作者: D. Kou;T. Virtanen;C. Treat;J. Tuovinen;Aleksi Räsänen;S. Juutinen;J. Mikola;M. Aurela;L. Heiskanen