Overview
- Thawing permafrost is exposing sulfide-rich rock, driving oxidation that produces sulfuric acid and mobilizes iron, cadmium, and aluminum into the river.
- Nine of ten tributaries in the watershed exceeded federal thresholds for at least one metal, signaling widespread degradation beyond the main channel.
- Cadmium is accumulating in fish organs and iron-rich water is smothering insect larvae, threatening salmon and other species vital to local food webs.
- The chemical signature matches acid mine drainage even though no mining is present in the area.
- Authors warn similar transformations could emerge across Arctic watersheds with suitable geology, and they describe conventional remediation as impractical in these remote settings.