Quantifying The Impact of Recent Climate Change on Sedimentary Biogeochemical Cycles and The Organic Carbon Sink

量化近期气候变化对沉积生物地球化学循环和有机碳汇的影响

• 批准号: RGPIN-2022-04305
• 负责人: Pellerin, Andre
• 金额: $ 1.89万
• 依托单位: Université du Québec à Rimouski
• 依托单位国家: 加拿大
• 项目类别: Discovery Grants Program - Individual
• 财政年份: 2022
• 资助国家: 加拿大
• 起止时间: 2022-01-01 至 2023-12-31
• 项目状态: 已结题
• 来源: https://www.nserc-crsng.gc.ca/ase-oro/Details-Detailles_eng.asp?id=765289
• 关键词: Quantifying; Impact; Recent; Climate; Change

Global warming is modifying the storage and release of organic carbon (OC) in the Arctic environment both on land and at sea. To understand how climate change influences the Arctic carbon cycle, it is necessary to understand its journey from release by permafrost thaw to final destination, in the atmosphere or in the seafloor. The Mackenzie watershed and Beaufort Shelf is a key region that is affected by changing Arctic conditions and which may be an indicator of what will happen across the broader Arctic. When permafrost thaws, it releases OC that has been accumulating frozen for thousands of years, all at once. Microbes living in soil, lakes, streams and the sea, can then use this OC to grow by degrading it into greenhouse gases (GHG) such as carbon dioxide or methane, leading to more warming and, more thaw, in a positive feedback. Microbes use electron acceptors such as oxygen, nitrate, manganese, iron oxides and sulfate to degrade OC. In the seafloor, OC is likely to degrade into carbon dioxide. On land, electron acceptors are often scarce and microbes ferment OC into methane gas, which is a more potent greenhouse gas. The place, and the pathway taken to degrade OC therefore has a direct impact on the climate and can exacerbate warming. Rapid shift in biogeochemical cycles, have been observed in response to the recent warming trends, which may affect OC degradation. My long-term research goal is to forecast the responses and feedbacks between microbial-sedimentary systems and the changing Arctic. Two short-term (5-year) science objectives are (1) quantify the present and the historical distribution of organic carbon (OC) mineralization on the Beaufort shelf and the fate of marine and terrestrial sources and (2) balance the carbon budgets of production and emissions of greenhouse gases from sites undergoing abrupt permafrost thaw. Both (1) and (2) are at the forefront of Arctic research and are experimentally accessible due to the development and fine-tuning of new techniques and multidisciplinary international collaborations. The analytical program relies on the sampling of porewater, sediment and gas from field sites and analysis of microbial catabolic rates with both stable and radioactive isotope tracers in the lab. Results are then incorporated in diagenetic models that considers deposition rates, chemical fluxes in porewater and gas migration. Stable isotopes of carbon and sulfur play a critical role in this analysis. The program will anticipate changes in the carbon sink of the Mackenzie-Beaufort fluvial system. It ties into pan-Arctic assessments of OC transport, burial and degradation. This could shape government policy and relations between Arctic nations. The program is the proving ground for nine HQP that will increase their capacity to conduct respectful research alongside local communities. It will maintain Canada at the forefront of Arctic scientific research and a leader in assessing the consequences of climate change.

全球变暖正在改变北极环境中有机碳(OC)在陆地和海洋中的储存和释放。为了了解气候变化如何影响北极的碳循环，有必要了解其从永久冻土融化释放到最终目的地、大气或海底的过程。麦肯齐分水岭和博福特大陆架是一个关键地区，受到北极条件变化的影响，可能是整个北极地区将发生什么的一个指标。当永久冻土融化时，它会一下子释放出冻结了数千年的有机碳。然后，生活在土壤、湖泊、溪流和海洋中的微生物可以利用这种有机碳通过将其降解为二氧化碳或甲烷等温室气体(GHG)来生长，从而在积极的反馈中导致更多的变暖和更多的融化。微生物利用氧、硝酸盐、锰、氧化铁和硫酸盐等电子受体降解有机碳。在海底，有机碳很可能会降解成二氧化碳。在陆地上，电子受体通常很稀缺，微生物将有机碳发酵成甲烷气体，这是一种更有效的温室气体。因此，降解有机碳的地点和途径对气候有直接影响，并可能加剧变暖。生物地球化学循环的快速变化已被观察到，以响应最近的变暖趋势，这可能会影响有机碳的降解。我的长期研究目标是预测微生物沉积系统与不断变化的北极之间的反应和反馈。两个短期(5年)科学目标是(1)量化波弗特陆架有机碳(OC)矿化的现在和历史分布以及海洋和陆地来源的命运；(2)平衡正在经历突然永久冻土融化的地点的生产和温室气体排放的碳收支。(1)和(2)都处于北极研究的前沿，由于新技术的开发和微调以及多学科的国际合作，可以通过实验获得。该分析计划依赖于从野外现场采集的孔隙水、沉积物和气体的样本，以及在实验室中使用稳定和放射性同位素示踪剂分析微生物分解代谢率。然后将结果纳入成岩模型，该模型考虑了沉积速率、孔隙水中的化学通量和天然气迁移。碳和硫的稳定同位素在这一分析中起着关键作用。该计划将预测麦肯齐-博福特河流系统碳汇的变化。它与对有机碳运输、埋葬和退化的泛北极评估挂钩。这可能会影响政府政策和北极国家之间的关系。该项目是九个HQP的试验场，这些HQP将提高他们与当地社区一起进行尊重研究的能力。它将使加拿大保持在北极科学研究的前沿，并在评估气候变化后果方面处于领先地位。