Potential impacts of mercury released from thawing permafrost
Kevin Schaefer (),
Yasin Elshorbany,
Elchin Jafarov,
Paul F. Schuster,
Robert G. Striegl,
Kimberly P. Wickland and
Elsie M. Sunderland
Additional contact information
Kevin Schaefer: University of Colorado Boulder
Yasin Elshorbany: University of South Florida
Elchin Jafarov: Computational Earth Sciences, Los Alamos National Laboratory
Paul F. Schuster: U.S. Geological Survey, Water Mission Area, Earth Systems Processes Division
Robert G. Striegl: U.S. Geological Survey, Water Mission Area, Earth Systems Processes Division
Kimberly P. Wickland: U.S. Geological Survey, Water Mission Area, Earth Systems Processes Division
Elsie M. Sunderland: Harvard University
Nature Communications, 2020, vol. 11, issue 1, 1-6
Abstract:
Abstract Mercury (Hg) is a naturally occurring element that bonds with organic matter and, when converted to methylmercury, is a potent neurotoxicant. Here we estimate potential future releases of Hg from thawing permafrost for low and high greenhouse gas emissions scenarios using a mechanistic model. By 2200, the high emissions scenario shows annual permafrost Hg emissions to the atmosphere comparable to current global anthropogenic emissions. By 2100, simulated Hg concentrations in the Yukon River increase by 14% for the low emissions scenario, but double for the high emissions scenario. Fish Hg concentrations do not exceed United States Environmental Protection Agency guidelines for the low emissions scenario by 2300, but for the high emissions scenario, fish in the Yukon River exceed EPA guidelines by 2050. Our results indicate minimal impacts to Hg concentrations in water and fish for the low emissions scenario and high impacts for the high emissions scenario.
Date: 2020
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Persistent link: https://EconPapers.repec.org/RePEc:nat:natcom:v:11:y:2020:i:1:d:10.1038_s41467-020-18398-5
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DOI: 10.1038/s41467-020-18398-5
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