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First pan-Arctic assessment of dissolved organic carbon in lakes of the permafrost region

机译:多年冻土区湖泊溶解有机碳的第一次泛北极评估

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Lakes in permafrost regions are dynamic landscape components and play an important role for climate change feedbacks. Lake processes such as mineralization and flocculation of dissolved organic carbon (DOC), one of the main carbon fractions in lakes, contribute to the greenhouse effect and are part of the global carbon cycle. These processes are in the focus of climate research, but studies so far are limited to specific study regions. In our synthesis, we analyzed 2167 water samples from 1833 lakes across the Arctic in permafrost regions of Alaska, Canada, Greenland, and Siberia to provide first pan-Arctic insights for linkages between DOC concentrations and the environment. Using published data and unpublished datasets from the author team, we report regional DOC differences linked to latitude, permafrost zones, ecoregions, geology, near-surface soil organic carbon contents, and ground ice classification of each lake region. The lake DOC concentrations in our dataset range from 0 to 1130?mg?L ?1 (10.8?mg?L ?1 median DOC concentration). Regarding the permafrost regions of our synthesis, we found median lake DOC concentrations of 12.4?mg?L ?1 (Siberia), 12.3?mg?L ?1 (Alaska), 10.3?mg?L ?1 (Greenland), and 4.5?mg?L ?1 (Canada). Our synthesis shows a significant relationship between lake DOC concentration and lake ecoregion. We found higher lake DOC concentrations at boreal permafrost sites compared to tundra sites. We found significantly higher DOC concentrations in lakes in regions with ice-rich syngenetic permafrost deposits (yedoma) compared to non-yedoma lakes and a weak but significant relationship between soil organic carbon content and lake DOC concentration as well as between ground ice content and lake DOC. Our pan-Arctic dataset shows that the DOC concentration of a lake depends on its environmental properties, especially on permafrost extent and ecoregion, as well as vegetation, which is the most important driver of lake DOC in this study. This new dataset will be fundamental to quantify a pan-Arctic lake DOC pool for estimations of the impact of lake DOC on the global carbon cycle and climate change.
机译:永久冻土地区的湖泊是动态景观组件,并为气候变化反馈发挥着重要作用。湖泊工艺如溶解有机碳(DOC)的矿化和絮凝,湖泊中主要碳分数之一,有助于温室效应,是全球碳循环的一部分。这些过程处于气候研究的重点,但到目前为止的研究仅限于特定的研究区域。在我们的合成中,我们分析了在阿拉斯加,格陵兰岛,格陵兰岛和西伯利亚的永久冻土地区的1833年北极地区的2167个水样,以便为DOC浓度和环境之间的联系提供持续的泛北极洞察力。使用来自作者团队的已发布的数据和未发表的数据集,我们向每个湖泊区域的纬度,永久性区域,生态,地质,近地面土壤有机碳内容物和地面冰分类报告了与纬度,永久性区域,生态,地质,近地表土壤有机碳含量和地面冰分类相关的区域Doc差异。在我们的数据集中的湖泊中的浓度范围为0至1130?mg?1?1(10.8?mg?l?1名doc浓度)。关于我们合成的永久冻土区域,我们发现12.4毫克的中位数湖Doc浓度为12.4毫克?1(西伯利亚),12.3?mg?l?1(阿拉斯加),10.3?mg?l?1(格陵兰)和4.5 ?MG?L?1(加拿大)。我们的综合表明了湖泊DOC浓度和湖泊融化之间的重要关系。与苔原网站相比,我们在Boreal Permafrost地点找到了更高的Lake Doc浓度。与非yedoma湖泊相比,我们发现具有富含冰的子冻土沉积沉积物(yedoma)在地区湖泊中的湖泊中的高档浓度提高了较高的。 DOC。我们的泛北极数据集显示湖泊的DOC集中浓度取决于其环境属性,特别是在永久冻土范围和eCOREGION以及植被上,以及植被,这是本研究中湖泊中最重要的驾驶员。这个新数据集将是量化泛北极湖Doc池的基础,以便估算Lake Doc在全球碳循环和气候变化中的影响。

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