Arsenic and mercury contamination and complex aquatic bioindicator responses to historical gold mining and modern watershed stressors in urban Nova Scotia, Canada.


Journal

The Science of the total environment
ISSN: 1879-1026
Titre abrégé: Sci Total Environ
Pays: Netherlands
ID NLM: 0330500

Informations de publication

Date de publication:
15 Sep 2021
Historique:
received: 28 01 2021
revised: 21 04 2021
accepted: 21 04 2021
pubmed: 29 5 2021
medline: 16 6 2021
entrez: 28 5 2021
Statut: ppublish

Résumé

Beginning in the late-1800s, gold mining activities throughout Nova Scotia, eastern Canada, released contaminants, notably geogenic arsenic from milled ore and anthropogenic mercury from amalgamation, to local environments via surface water flows through tailings fields. We investigated recovery from and legacy effects of the tailings field at the Montague Gold District (~1863-1940) on nearby urban lake ecosystems using geochemical measures and zooplankton remains archived in dated sediment cores from an impact (Lake Charles) and a reference (Loon Lake) lake. Sedimentary levels of total arsenic and total mercury were used to assess mining-related inputs. Arsenic concentrations remain elevated at nearly 300 times above sediment guidelines in Lake Charles surface sediments, due to its upward mobilization from enriched sediment intervals and sequestration by iron oxyhydroxides in surficial sediments. Peak mercury concentrations at Lake Charles were eight times above sediment guidelines during the mining period, and since ~1990 have recovered to levels observed before mining began. Legacy mining impacts at Lake Charles and non-mining related environmental changes in the post-1950 sediments at both lakes have thus combined to structure assemblage compositions of primary consumers. At both lakes, assemblages of pelagic-dominated Cladocera differed (p ≤ 0.05) during the mining period compared to periods before and after mining. Taxon richness differed (p ≤ 0.01) only between the pre- and post-mining periods at mining-impacted Lake Charles and reflects long-term declines of substrate-dwelling littoral taxa. Geochemical and biological recovery have not completely occurred at Lake Charles despite the mine district's closure ~80 years ago. Our findings demonstrate that impacts of ore processing and amalgamation from historical gold mining, combined with recent watershed stressors, continue to affect sedimentary arsenic geochemistry and intermediate trophic levels of nearby, downstream aquatic habitats.

Identifiants

pubmed: 34045077
pii: S0048-9697(21)02445-1
doi: 10.1016/j.scitotenv.2021.147374
pii:
doi:

Substances chimiques

Environmental Biomarkers 0
Water Pollutants, Chemical 0
Gold 7440-57-5
Mercury FXS1BY2PGL
Arsenic N712M78A8G

Types de publication

Journal Article

Langues

eng

Sous-ensembles de citation

IM

Pagination

147374

Informations de copyright

Copyright © 2021 Elsevier B.V. All rights reserved.

Déclaration de conflit d'intérêts

Declaration of competing interest The authors declare that they have no known competing financial interests or personal relationships that could have appeared to influence the work reported in this paper.

Auteurs

Allison J Clark (AJ)

Department of Geography and Environment, Mount Allison University, Sackville, New Brunswick, Canada.

Andrew L Labaj (AL)

Department of Geography and Environment, Mount Allison University, Sackville, New Brunswick, Canada.

John P Smol (JP)

Paleoecological Environmental Assessment and Research Laboratory, Department of Biology, Queen's University, Kingston, Ontario, Canada.

Linda M Campbell (LM)

Environmental Sciences Department, Saint Mary's University, Halifax, Nova Scotia, Canada.

Joshua Kurek (J)

Department of Geography and Environment, Mount Allison University, Sackville, New Brunswick, Canada. Electronic address: jkurek@mta.ca.

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