Centre for Earth Observation Science, and Department of Environment and Geography, University of Manitoba, Winnipeg, MB R3T 2N2, Canada.
Centre for Earth Observation Science, and Department of Environment and Geography, University of Manitoba, Winnipeg, MB R3T 2N2, Canada; Geological Survey of Canada, Natural Resources Canada, 601 Booth St., Ottawa, ON K1A 0E8, Canada.
Sci Total Environ. 2019 Jul 15;674:58-70. doi: 10.1016/j.scitotenv.2019.04.101. Epub 2019 Apr 9.
The Minamata Convention to reduce anthropogenic mercury (Hg) emissions entered into force in 2017, and attention is now focused on how to best monitor its effectiveness at reducing Hg exposure to humans. A key question is how closely Hg concentrations in the human food chain, especially in fish and other aquatic wildlife, will track the changes in atmospheric Hg that are expected to occur following anthropogenic emission reductions. We investigated this question by evaluating several regional groups of case studies where Hg concentrations in aquatic biota have been monitored continuously or intermittently for several decades. Our analysis shows that in most cases Hg time trends in biota did not agree with concurrent Hg trends in atmospheric deposition or concentrations, and the divergence between the two trends has become more apparent over the past two decades. An over-arching general explanation for these results is that the impact of changing atmospheric inputs on biotic Hg is masked by two factors: 1) The aquatic environment contains a large inventory of legacy emitted Hg that remains available for bio-uptake leading to a substantial lag in biotic response time to a change in external inputs; and 2) Biotic Hg trends reflect the dominant effects of changes in multi-causal, local and regional processes (e.g., aquatic or terrestrial biogeochemical processes, feeding ecology, climate) that control the speciation, bioavailability, and bio-uptake of both present-day and legacy emitted Hg. Globally, climate change has become the most prevalent contributor to the divergence. A wide range of biotic Hg outcomes can thus be expected as anthropogenic atmospheric Hg emissions decline, depending on how these processes operate on specific regions and specific organisms. Therefore, evaluating the effectiveness of the Minamata Convention will require biomonitoring of multiple species that represent different trophic and ecological niches in multiple regions of the world.
《水俣公约》旨在减少人为汞(Hg)排放,于 2017 年生效,目前人们关注的焦点是如何最好地监测其减少人类 Hg 暴露的有效性。一个关键问题是,人类食物链中 Hg 的浓度,尤其是鱼类和其他水生野生动物中的 Hg 浓度,将在多大程度上跟踪人为排放减少后预期发生的大气 Hg 变化。我们通过评估几十年来一直在持续或间歇性监测水生生物群 Hg 浓度的几个区域案例研究小组来研究这个问题。我们的分析表明,在大多数情况下,生物群 Hg 的时间趋势与大气沉降或浓度中的 Hg 趋势不一致,并且这两种趋势之间的差异在过去二十年中变得更加明显。对于这些结果的一个总体解释是,大气输入变化对生物 Hg 的影响被两个因素所掩盖:1)水生环境中含有大量的历史排放 Hg,这些 Hg 仍然可供生物吸收,导致生物对外部输入变化的响应时间存在很大的滞后;2)生物 Hg 的趋势反映了多种因果关系、地方和区域过程(例如,水生或陆地生物地球化学过程、摄食生态学、气候)变化的主导影响,这些过程控制着当前和历史排放 Hg 的形态、生物可利用性和生物吸收。在全球范围内,气候变化已成为导致这种差异的最主要因素。随着人为大气 Hg 排放的减少,预计会出现各种不同的生物 Hg 结果,具体取决于这些过程在特定地区和特定生物中的运作方式。因此,评估《水俣公约》的有效性需要对代表世界多个地区不同营养级和生态位的多种物种进行生物监测。