Collaborative research: Climate controls on carbon accumulation in upland permafrost at millennial scales

永久冻土层，或永久冻土，拥有大量的碳储存库。这项研究的首要目标是研究最近的地质历史，以提高对未来气候变化如何影响碳积累和释放的理解。研究人员结合了古生态学、古气候学、地表地质学、地质年代学和定量地貌学方面的专业知识。他们将一起量化气候与过去4万年中北极丘陵高地地区在不同气候条件下积累的碳量之间的关系，这将补充之前关于气候变化对低洼地区湖泊和泥炭地永久冻土碳影响的研究。研究结果将为永久冻土碳网络（北极环境变化研究的一部分）增加古视角。该项目将为研究生和本科生提供培训，调查团队包括一名早期职业科学家。在这项研究中，研究人员将结合实地收集、沉积物岩心分析和建模，量化阿拉斯加山脉北麓八英里湖流域一个高地研究地点气候与永久冻土碳积累之间的千年尺度关系。他们将沿着山坡样带采集多个沉积物岩心，绘制下垫地层格架；对比覆盖短坡和长坡的地表物质，推断坡长和坡角相关输运过程的相对作用；并在数值模型中使用这些数据来模拟山坡的演变，并评估下坡的地貌过程，这些过程会转移沉积物和封存碳。研究人员还将使用大型化石的放射性碳定年法来确定有机质在地层上混合的程度，并区分千年尺度的聚集期；评估花粉和大化石的群落特征和粒度分布；并分析沉积物序列，以获得一套生物物理特性，以量化碳质量，积累和分解。该奖项反映了美国国家科学基金会的法定使命，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。

Permafrost, or perennially frozen ground, holds a large reservoir of carbon. The overarching goal of this study is to look to the recent geologic past to improve understanding of how future changes in climate may impact carbon accumulation and release. The investigators have combined expertise in paleoecology, paleoclimatology, surficial geology, geochronology, and quantitiative geomorphology. Together, they will quantify the relationship between climate and the mass of carbon that accumulated under distinctly different climates of the past 40,000 years in hilly upland regions of the Arctic, which will complment previous work on the effects of climate change on permafrost carbon in lakes and peatlands of low-lying terrain. Results will add paleo perspectives to the Permafrost Carbon Network, part of the Study of Environmental Arctic Change. The project will provide training for graduate and undergraduate students, and the team of investigators includes an early career scientist.In this study, the investigators will combine field-collections, analysis of sediment cores, and modeling to quantify the millennial scale relationship between climate and permafrost carbon accumulation at an upland study site in the Eight Mile Lake watershed in the northern foothills of the Alaska Range. They will take multiple sediment cores along hillslope transects to map the underlying stratigraphic framework; contrast the surficial materials mantling both a short and a long slope to infer the relative roles of slope-length- versus slope-angle-dependent transport processes; and use these data in a numerical model to simulate hillslope evolution and assess downslope geomorphic processes that transfer sediment and sequester carbon. The investigators will also use radiocarbon dating of macrofossils to determine the extent to which organic matter has been stratigraphically mixed and to distninguish millennial-scale periods of accumulation; evaluate pollen and macrofossiles for community characteristics and grain size distributions; and analyze sediment sequences for a suite of bio-physical properties to quantify carbon mass, accumulation, and decomposition.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.