4.7 Article

Impacts on aquatic biota from salinization and metalloid contamination by gold mine tailings in sub-Arctic lakes

Journal

ENVIRONMENTAL POLLUTION
Volume 278, Issue -, Pages -

Publisher

ELSEVIER SCI LTD
DOI: 10.1016/j.envpol.2021.116815

Keywords

Bio-indicators; Consolidated mine; Yellowknife; Climate warming; Urbanization; Paleolimnology

Funding

  1. Natural Science and Engineering Research Council of Canada [NSERC STPGP 462955-14]
  2. Polar Continental Shelf Program
  3. Northern Scientific Training Program
  4. Summer Work Experience Program at Queen's University
  5. Banting Postdoctoral Fellowship
  6. W. Garfield Weston Foundation
  7. NSERC Alexander Graham Bell Canada Graduate Scholarship - Doctoral

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This study examined the long-term impacts of past regional gold mining activities on sub-Arctic lakes near Con Mine, finding that the lakes were influenced by metal(loid) pollution and salt-rich mine drainage. The presence of halophilic diatom species in recent sediments suggests that extreme saline conditions continue to affect the biota over a decade after mining activities ceased. The lack of biological recovery indicates the ongoing challenges faced by mine-impacted lakes in terms of elevated contaminant levels and emerging stressors like climate warming and land-use changes.
Precious metal mining activities have left complex environmental legacies in lakes around the world, including some sites in climatically sensitive regions of the Canadian sub-Arctic. Here, we examined the long-term impacts of past regional gold mining activities on sub-Arctic lakes near Con Mine (Yellowknife, Northwest Territories) based on sediment core analysis (paleolimnology). In addition to receiving metal(loid)s from roaster stack emissions, the study lakes were also influenced by salt-rich mine drainage from Con Mine tailings. Water samples from these lakes had some of the highest concentrations for salinity-related variables (e.g. Ca2+, Cl-, Na+) and metal(loid)s (e.g. As, Cu, Ni, Sb) in the Yellowknife area. Furthermore, the presence of halophilic diatom (Bacillariophyceae) taxa (Achnanthes thermalis and Navicula incertata) in the recent sediments of Keg and Peg lakes suggest that the extreme saline con-ditions are strongly influencing the present biota, more than 10 years after the cessation of gold mining activities at Con Mine. The sedimentary metal(loid) profiles (e.g. As, Cu, Ni) of Kam Lake tracked the influence of regional gold mining activities, particularly those at Con Mine, while the algal assemblages recorded the biological responses to salinization and metal(loid) pollution (e.g. marked decreases in diatom species richness, Hill's N2 diversity, and chrysophyte cyst:diatom valve ratio). At Kam Lake, the algal assemblage changes in the post-mining era were indicative of climate-mediated changes to lake thermal properties (e.g. rise in planktonic diatoms), nutrient enrichment related to urbanization (e.g. increase in eutrophic Stephanodisucs taxa), and/or a combination of both stressors. The lack of biological recovery (i.e. return to pre-mining assemblages) is consistent with investigations of mine-impacted lakes in temperate regions where elevated contaminant levels and emerging stressors (e.g. climate warming, land-use changes) are influencing lake recovery. (C) 2021 Elsevier Ltd. All rights reserved.

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