Chételat John, McKinney Melissa A, Amyot Marc, Dastoor Ashu, Douglas Thomas A, Heimbürger-Boavida Lars-Eric, Kirk Jane, Kahilainen Kimmo K, Outridge Peter M, Pelletier Nicolas, Skov Henrik, St Pierre Kyra, Vuorenmaa Jussi, Wang Feiyue
Environment and Climate Change Canada, Ecotoxicology and Wildlife Health Division, National Wildlife Research Centre, Ottawa, ON K1A 0H3, Canada.
Department of Natural Resource Sciences, McGill University, Sainte-Anne-de-Bellevue, QC H9X 3V9, Canada.
Sci Total Environ. 2022 Jun 10;824:153715. doi: 10.1016/j.scitotenv.2022.153715. Epub 2022 Feb 9.
Dramatic environmental shifts are occuring throughout the Arctic from climate change, with consequences for the cycling of mercury (Hg). This review summarizes the latest science on how climate change is influencing Hg transport and biogeochemical cycling in Arctic terrestrial, freshwater and marine ecosystems. As environmental changes in the Arctic continue to accelerate, a clearer picture is emerging of the profound shifts in the climate and cryosphere, and their connections to Hg cycling. Modeling results suggest climate influences seasonal and interannual variability of atmospheric Hg deposition. The clearest evidence of current climate change effects is for Hg transport from terrestrial catchments, where widespread permafrost thaw, glacier melt and coastal erosion are increasing the export of Hg to downstream environments. Recent estimates suggest Arctic permafrost is a large global reservoir of Hg, which is vulnerable to degradation with climate warming, although the fate of permafrost soil Hg is unclear. The increasing development of thermokarst features, the formation and expansion of thaw lakes, and increased soil erosion in terrestrial landscapes are increasing river transport of particulate-bound Hg and altering conditions for aquatic Hg transformations. Greater organic matter transport may also be influencing the downstream transport and fate of Hg. More severe and frequent wildfires within the Arctic and across boreal regions may be contributing to the atmospheric pool of Hg. Climate change influences on Hg biogeochemical cycling remain poorly understood. Seasonal evasion and retention of inorganic Hg may be altered by reduced sea-ice cover and higher chloride content in snow. Experimental evidence indicates warmer temperatures enhance methylmercury production in ocean and lake sediments as well as in tundra soils. Improved geographic coverage of measurements and modeling approaches are needed to better evaluate net effects of climate change and long-term implications for Hg contamination in the Arctic.
由于气候变化,整个北极地区正在发生剧烈的环境变化,这对汞(Hg)的循环产生了影响。本综述总结了关于气候变化如何影响北极陆地、淡水和海洋生态系统中汞的迁移和生物地球化学循环的最新科学研究。随着北极地区的环境变化继续加速,气候和冰冻圈的深刻变化及其与汞循环的联系正日益清晰。模型结果表明,气候影响大气汞沉降的季节性和年际变化。当前气候变化影响的最明显证据是陆地集水区的汞迁移,那里广泛的永久冻土融化、冰川融化和海岸侵蚀正在增加汞向下游环境的输出。最近的估计表明,北极永久冻土是全球一个巨大的汞储存库,尽管永久冻土土壤汞的去向尚不清楚,但它很容易因气候变暖而退化。热喀斯特地貌的不断发展、解冻湖的形成和扩张以及陆地景观中土壤侵蚀的增加,正在增加河流中颗粒态汞的输送,并改变水生汞转化的条件。更多的有机物质输送也可能影响汞的下游输送和去向。北极地区和北方地区更严重、更频繁的野火可能导致了大气汞库的增加。气候变化对汞生物地球化学循环的影响仍然知之甚少。海冰覆盖减少和雪中氯化物含量增加可能会改变无机汞的季节性逸出和保留。实验证据表明,温度升高会促进海洋和湖泊沉积物以及苔原土壤中甲基汞的产生。需要改进测量和建模方法的地理覆盖范围,以更好地评估气候变化的净影响以及对北极汞污染的长期影响。