PRA Melting-ICE 项目:斯瓦尔巴 2022 年考察报告。

Open research Europe Pub Date : 2024-12-04 eCollection Date: 2024-01-01 DOI:10.12688/openreseurope.17772.1
Francesco Montemagno, Martina Cascone, Carlo Cardellini, Jacopo Pasotti, Elena Manini, Elisa Baldrighi, Enrico Maiero, Delia Segato, Riccardo Cerrato, Mauro Mazzola, Massimiliano Vardè, Angelina Cordone, Stefano Caliro, Iain Rudnik, Margaret Cramm, James Bradley, Donato Giovannelli
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引用次数: 0

摘要

北极地区是地球上变暖最快的地区之一。过去五十年来,平均气温不断升高,加深了整个北极地区最上层永久冻土的解冻,其中含有大量有机碳。季节性解冻的逐渐加深释放出的碳被活跃的微生物所利用,这些微生物也会产生温室气体,有可能对全球变暖产生正反馈。尽管微生物在控制有机物降解和温室气体向大气通量方面非常重要,但目前还缺乏有关北极高纬度地区土壤中微生物群落随季节性解冻而产生的活动和动态的数据。本报告介绍了 2022 年 2 月至 10 月期间在意大利北极研究计划(PRA)项目 Melting-ICE 框架内对斯瓦尔巴群岛进行的三次具体考察,报告了考察地点的特征和采集的样本。该项目旨在研究活动层微生物群落在整个季节解冻周期中的多样性和活性,将微生物多样性与气体通量和组成联系起来。在这些考察中,共选择了八个不同的地点调查土壤的微生物学和地球化学,并估算从土壤到大气的气体通量。实地收集的数据与实验室获得的结果相结合,将为永冻土活动层中微生物群落的季节性活动提供快照。这三次活动将提供数据,以估计永久冻土融化对碳循环的影响以及微生物在温室气体释放中的作用。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
PRA Melting-ICE Project: Svalbard 2022 Expeditions Report.

Arctic regions are among the fastest warming areas of the planet. Increasing average temperatures over the last five decades have deepened the thawing of the upper-most layer of permafrost across the Arctic, which contains significant amounts of organic carbon. The progressive deepening of seasonal thawing releases carbon that is used by active microorganisms which also produce greenhouse gases, potentially onsetting a positive feedback on global warming. Despite their importance in controlling organic matter degradation and greenhouse gas fluxes to the atmosphere, there is a lack of data on activity and dynamics of microbial communities in High Arctic soils in response to seasonal thaw. This report describes three specific expeditions performed on the Svalbard archipelago, carried out within the framework of the PRA (Italian Arctic Research Program) project Melting-ICE, performed between February and October 2022, reporting site characteristics and samples collected. The project aims to investigate the diversity and activity of active layer microbial communities across a full season thaw cycle, correlating microbial diversity with gas fluxes and composition. During these expeditions, a total of eight different sites were selected to investigate the microbiology and geochemistry of soils, as well as to estimate the gas fluxes from the soil to the atmosphere. The data collected in the field, combined with the results obtained in the laboratory, will provide a snapshot of the seasonal activity of the microbial communities present in the permafrost's active layer. The three campaigns will provide data to estimate the impact of permafrost melting on the carbon cycle and the role of microorganisms in the release of greenhouse gases.

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