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Influence of late-Holocene climate change on the solid-phase speciation and long-term stability of arsenic in sub-Arctic lake sediments.
Miller, Clare B; Parsons, Michael B; Jamieson, Heather E; Ardakani, Omid H; Gregory, Braden R B; Galloway, Jennifer M.
Afiliação
  • Miller CB; Department of Geological Sciences and Geological Engineering, Queen's University, Kingston, ON K7L 3N6, Canada. Electronic address: miller.clare@queensu.ca.
  • Parsons MB; Department of Geological Sciences and Geological Engineering, Queen's University, Kingston, ON K7L 3N6, Canada; Geological Survey of Canada/Commission géologique du Canada, Natural Resources Canada/Ressources naturelles Canada, 1 Challenger Drive, Dartmouth, NS B2Y 4A2, Canada.
  • Jamieson HE; Department of Geological Sciences and Geological Engineering, Queen's University, Kingston, ON K7L 3N6, Canada.
  • Ardakani OH; Geological Survey of Canada/Commission géologique du Canada, Natural Resources Canada/Ressources naturelles Canada, 3303 33rd Street N.W., Calgary, AB T2L 2A7, Canada.
  • Gregory BRB; Ottawa-Carleton Geoscience Centre, Department of Earth Sciences, Carleton University, Ottawa, ON KIS 5B6, Canada.
  • Galloway JM; Geological Survey of Canada/Commission géologique du Canada, Natural Resources Canada/Ressources naturelles Canada, 3303 33rd Street N.W., Calgary, AB T2L 2A7, Canada; Ottawa-Carleton Geoscience Centre, Department of Earth Sciences, Carleton University, Ottawa, ON KIS 5B6, Canada; Aarhus Institute o
Sci Total Environ ; 709: 136115, 2020 Mar 20.
Article em En | MEDLINE | ID: mdl-31887529
ABSTRACT
Sediment cores were collected from two lakes in the Courageous Lake Greenstone Belt (CLGB), central Northwest Territories, Canada, to examine the influence of late-Holocene warming on the transport and fate of arsenic (As) in sub-Arctic lakes. In both lakes, allochthonous As-bearing minerals (i.e. arsenopyrite and scorodite) were identified in sediment deposited during times of both regional warming and cooling, suggesting that weathering of bedrock and derived surficial materials provides a continual source of As to lakes of the CLGB. However, maximum porewater As (84 µg·L-1 and 15 µg·L-1) and reactive organic matter (OM; aquatic and terrestrial-derived) concentrations in each lake are coincident with known periods of regional climate warming. It is inferred that increased biological production in surface waters and influx of terrigenous OM led to the release of sedimentary As to porewater through reductive dissolution of As-bearing Fe-(oxy)hydroxides and scorodite during episodes of regional warming. Elevated sedimentary As concentrations (median 36 mg·kg-1; range 29 to 49 mg·kg-1) are observed in sediment coeval with the Holocene Thermal Maximum (ca. 5430 ± 110 to 4070 ± 130 cal. years BP); at these depths, authigenic As-bearing framboidal pyrite is the primary host of As in sediment and the influence of organic matter on the precipitation of As-bearing framboidal pyrite is apparent petrographically. These findings suggest that increased biological productivity and weathering of terrestrial OM associated with climate warming influences redox cycles in the near-surface sediment and enhances the mobility of As in northern lakes. Knowledge generated from this study is relevant for predicting future climate change-driven variations in metal(loid) cycling in aquatic systems and can be used to interpret trends in long-term environmental monitoring data at historical, modern, and future metal mines in northern environments.
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Texto completo: 1 Coleções: 01-internacional Base de dados: MEDLINE Contexto em Saúde: 2_ODS3 Problema de saúde: 2_quimicos_contaminacion Tipo de estudo: Prognostic_studies Idioma: En Revista: Sci Total Environ Ano de publicação: 2020 Tipo de documento: Article

Texto completo: 1 Coleções: 01-internacional Base de dados: MEDLINE Contexto em Saúde: 2_ODS3 Problema de saúde: 2_quimicos_contaminacion Tipo de estudo: Prognostic_studies Idioma: En Revista: Sci Total Environ Ano de publicação: 2020 Tipo de documento: Article
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