Map of the study area.

• Main Authors: Brittany C. Astles (14290341), John Chételat (529889), Michael J. Palmer (3189375), Jesse C. Vermaire (5464793)
• Format: Still Image
• Language: unknown
• Published: 2022
• Subjects: Ecology; Inorganic Chemistry; Environmental Sciences not elsewhere classified; Biological Sciences not elsewhere classified; low organic matter; contained predominately clay; 7 ° c; 21 ° c; strongly enhance sediment; sediment redox conditions; lower martin lake; great slave lake; experimental incubation approach; either sediment type; warmer temperatures associated; reported temperature enhancement; overlying oxic waters; duplicate sediment batches; div >< p; lake sediments either; yellowknife bay sediments; warmer temperatures; yellowknife bay; surface waters; overlying water; experimental investigation; contaminated sediment; yellowknife area; contaminated sediments; warming effects; thermal stratification; term warming; temperature treatments; study assessed; published studies; northwest territories; microbial metabolism; legacy arsenic; internal loading; indirect effects; higher solid; fluxes ranging; evaluating climate; environmental concern; duplicate cores; direct effect; controlled chamber; continued remobilization; climate change; arsenic fluxes; Canada; Great Slave Lake; Northwest Territories; Yellowknife; Yellowknife Bay
• Online Access: https://doi.org/10.1371/journal.pone.0279412.g001

Approximate locations where the sediment cores were collected from Lower Martin Lake and Yellowknife Bay in relation to the closed Giant Mine and Con Mine, and the capital of the Northwest Territories, Yellowknife, Canada. Spatial data presented in the figure are licensed under an Open Government Licence–Canada from the National Hydro Network (NHN) dataset https://open.canada.ca/data/en/dataset/a4b190fe-e090-4e6d-881e-b87956c07977 .