Paleoecological Environmental Assessment and Research Lab (PEARL), Department of Biology, Queen's University, 116 Barrie St., Kingston, ON K7L 3N6, Canada.
Paleoecological Environmental Assessment and Research Lab (PEARL), Department of Biology, Queen's University, 116 Barrie St., Kingston, ON K7L 3N6, Canada.
Sci Total Environ. 2022 Mar 10;811:152299. doi: 10.1016/j.scitotenv.2021.152299. Epub 2021 Dec 9.
The copper-zinc smelter at Flin Flon (Manitoba) operated between 1930 and 2010 and emitted large amounts of metal(loid)s and sulphur dioxide into the atmosphere, damaging the surrounding terrestrial landscapes and depositing airborne industrial pollutants into aquatic ecosystems. However, the extent of biological impairment in regional lakes is largely unknown. Here, we analysed biological and geochemical proxies preserved in a dated sediment core from Phantom Lake, collected seven years after the smelter closed in 2010. Our objectives were to determine how smelting history affected long-term trends in (1) sedimentary elements, (2) biota across multiple trophic levels, and (3) spectrally-inferred chlorophyll a and lake-water total organic carbon. The effects of smelting activities were clearest in the diatom record, in concordance with modest responses in chironomid and cladoceran assemblages. Several metal(loid)s were naturally high and exceeded sediment quality guidelines during the pre-smelting era. With the opening of the smelter, metal(loid) concentrations in sediments increased through the 1930s, peaked in the 1960s, and declined thereafter with technological improvements but remained above background to this day. Although modest declines in inferred lake-water total organic carbon indicate reduced terrestrial carbon supply following sulphate deposition in the catchment, the diatom record showed no evidence of acidification as the lake was and remained well-buffered. Pre-smelting diatom and invertebrate assemblages were diverse and indicated oligo-mesotrophic conditions. Smelting was associated with the loss of metal-sensitive biological indicators and the emergence of assemblages dominated by metal-tolerant, generalist taxa. Diatoms tracked substantial reductions in aerial emissions since the 1990s, particularly after the smelter closed, but also indicated that the biological effects of metal pollution persist in Phantom Lake. Examining the effects of a base metal smelter on a well-buffered lake offered insights into multi-trophic level responses to severe metal contamination and potential recovery without the confounding effects of concurrent changes in lake acidity.
弗林弗隆(加拿大马尼托巴省)的铜锌冶炼厂于 1930 年至 2010 年间运营,向大气中排放了大量金属(类)和二氧化硫,破坏了周围的陆地景观,并将空气中的工业污染物沉积到水生态系统中。然而,该地区湖泊的生物受损程度在很大程度上是未知的。在这里,我们分析了 2010 年冶炼厂关闭后 7 年从幻影湖采集的有日期沉积物岩芯中保存的生物和地球化学示踪剂。我们的目标是确定冶炼历史如何影响(1)沉积物元素、(2)多个营养级别的生物群和(3)光谱推断的叶绿素 a 和湖水总有机碳的长期趋势。在与前冶炼时期自然高浓度且超过沉积物质量指南的中一致,在硅藻记录中可以最清楚地看到冶炼活动的影响。随着冶炼厂的开放,沉积物中的金属(类)浓度在 20 世纪 30 年代增加,在 20 世纪 60 年代达到峰值,此后随着技术的改进而下降,但至今仍高于背景水平。虽然推断的湖水总有机碳略有下降表明硫酸盐在集水区的沉积导致陆地碳供应减少,但硅藻记录表明,由于湖泊缓冲良好,没有酸化的证据。前冶炼时期的硅藻和无脊椎动物组合多样,表明贫营养至中营养条件。冶炼与对生物敏感的生物指标的丧失以及由耐金属、广食性分类群主导的组合的出现有关。自 20 世纪 90 年代以来,硅藻记录跟踪了大气排放的大量减少,特别是在冶炼厂关闭后,但也表明金属污染的生物效应在幻影湖中仍然存在。检查基本金属冶炼厂对缓冲良好的湖泊的影响提供了对多营养级生物对严重金属污染的反应以及在没有同时发生的酸度变化的情况下潜在恢复的见解。