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PNAS Study Links Alaska’s Orange Rivers to Permafrost Thaw and Toxic Metal Release

Researchers warn the same chemistry is emerging across Arctic watersheds due to thaw exposing sulfide-rich soils.

Overview

  • The analysis of the Salmon River finds dissolved metals and turbidity at levels that exceed U.S. EPA thresholds for aquatic life.
  • Thaw lets water and oxygen oxidize sulfide minerals, generating sulfuric acid that mobilizes iron, cadmium and aluminum into the water.
  • Cadmium is accumulating in fish organs while iron-driven turbidity reduces light and suffocates insect larvae that support salmon and other fish.
  • The changes threaten chum salmon spawning habitat and indirectly jeopardize Indigenous subsistence fisheries in northern Alaska.
  • Authors describe a process that mimics acid mine drainage yet arises naturally from permafrost loss, cautioning it may persist without permafrost recovery.