A mass budget for mercury and methylmercury in the Arctic Ocean

Elevated biological concentrations of methylmercury (MeHg), a bioaccumulative neurotoxin, are observed throughout the Arctic Ocean, but major sources and degradation pathways in seawater are not well understood. We develop a mass budget for mercury species in the Arctic Ocean based on available data...

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Published in:Global Biogeochemical Cycles
Main Authors: Soerensen, Anne, Jacob, Daniel James, Schartup, Amina, Fisher, Jenny, Lehnherr, Igor, St. Louis, Vincent L., Heimbürger, Lars-Eric, Sonke, Jeroen E., Krabbenhoft, David P., Sunderland, Elynor M
Format: Article in Journal/Newspaper
Language:English
Published: Wiley-Blackwell 2016
Subjects:
Ice
Online Access:http://nrs.harvard.edu/urn-3:HUL.InstRepos:33983357
https://doi.org/10.1002/2015GB005280
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spelling ftharvardudash:oai:dash.harvard.edu:1/33983357 2023-05-15T14:27:04+02:00 A mass budget for mercury and methylmercury in the Arctic Ocean Soerensen, Anne Jacob, Daniel James Schartup, Amina Fisher, Jenny Lehnherr, Igor St. Louis, Vincent L. Heimbürger, Lars-Eric Sonke, Jeroen E. Krabbenhoft, David P. Sunderland, Elynor M 2016 application/pdf http://nrs.harvard.edu/urn-3:HUL.InstRepos:33983357 https://doi.org/10.1002/2015GB005280 en_US eng Wiley-Blackwell doi:10.1002/2015GB005280 Global Biogeochemical Cycles Soerensen, Anne L., Daniel J. Jacob, Amina T. Schartup, Jenny A. Fisher, Igor Lehnherr, Vincent L. St. Louis, Lars-Eric Heimbürger, Jeroen E. Sonke, David P. Krabbenhoft, and Elsie M. Sunderland. 2016. “A Mass Budget for Mercury and Methylmercury in the Arctic Ocean.” Global Biogeochemical Cycles 30 (4) (April): 560–575. Portico. doi:10.1002/2015gb005280. 0886-6236 http://nrs.harvard.edu/urn-3:HUL.InstRepos:33983357 Journal Article 2016 ftharvardudash https://doi.org/10.1002/2015GB005280 https://doi.org/10.1002/2015gb005280 2022-04-05T18:45:57Z Elevated biological concentrations of methylmercury (MeHg), a bioaccumulative neurotoxin, are observed throughout the Arctic Ocean, but major sources and degradation pathways in seawater are not well understood. We develop a mass budget for mercury species in the Arctic Ocean based on available data since 2004 and discuss implications and uncertainties. Our calculations show that high total mercury (Hg) in Arctic seawater relative to other basins reflect large freshwater inputs and sea ice cover that inhibits losses through evasion. We find that most net MeHg production (20 Mg a−1) occurs in the subsurface ocean (20–200 m). There it is converted to dimethylmercury (Me2Hg: 17 Mg a−1), which diffuses to the polar mixed layer and evades to the atmosphere (14 Mg a−1). Me2Hg has a short atmospheric lifetime and rapidly degrades back to MeHg. We postulate that most evaded Me2Hg is redeposited as MeHg and that atmospheric deposition is the largest net MeHg source (8 Mg a−1) to the biologically productive surface ocean. MeHg concentrations in Arctic Ocean seawater are elevated compared to lower latitudes. Riverine MeHg inputs account for approximately 15% of inputs to the surface ocean (2.5 Mg a−1) but greater importance in the future is likely given increasing freshwater discharges and permafrost melt. This may offset potential declines driven by increasing evasion from ice-free surface waters. Geochemical model simulations illustrate that for the most biologically relevant regions of the ocean, regulatory actions that decrease Hg inputs have the capacity to rapidly affect aquatic Hg concentrations. Engineering and Applied Sciences Version of Record Article in Journal/Newspaper Arctic Arctic Arctic Ocean Ice permafrost Sea ice Harvard University: DASH - Digital Access to Scholarship at Harvard Arctic Arctic Ocean Global Biogeochemical Cycles 30 4 560 575
institution Open Polar
collection Harvard University: DASH - Digital Access to Scholarship at Harvard
op_collection_id ftharvardudash
language English
description Elevated biological concentrations of methylmercury (MeHg), a bioaccumulative neurotoxin, are observed throughout the Arctic Ocean, but major sources and degradation pathways in seawater are not well understood. We develop a mass budget for mercury species in the Arctic Ocean based on available data since 2004 and discuss implications and uncertainties. Our calculations show that high total mercury (Hg) in Arctic seawater relative to other basins reflect large freshwater inputs and sea ice cover that inhibits losses through evasion. We find that most net MeHg production (20 Mg a−1) occurs in the subsurface ocean (20–200 m). There it is converted to dimethylmercury (Me2Hg: 17 Mg a−1), which diffuses to the polar mixed layer and evades to the atmosphere (14 Mg a−1). Me2Hg has a short atmospheric lifetime and rapidly degrades back to MeHg. We postulate that most evaded Me2Hg is redeposited as MeHg and that atmospheric deposition is the largest net MeHg source (8 Mg a−1) to the biologically productive surface ocean. MeHg concentrations in Arctic Ocean seawater are elevated compared to lower latitudes. Riverine MeHg inputs account for approximately 15% of inputs to the surface ocean (2.5 Mg a−1) but greater importance in the future is likely given increasing freshwater discharges and permafrost melt. This may offset potential declines driven by increasing evasion from ice-free surface waters. Geochemical model simulations illustrate that for the most biologically relevant regions of the ocean, regulatory actions that decrease Hg inputs have the capacity to rapidly affect aquatic Hg concentrations. Engineering and Applied Sciences Version of Record
format Article in Journal/Newspaper
author Soerensen, Anne
Jacob, Daniel James
Schartup, Amina
Fisher, Jenny
Lehnherr, Igor
St. Louis, Vincent L.
Heimbürger, Lars-Eric
Sonke, Jeroen E.
Krabbenhoft, David P.
Sunderland, Elynor M
spellingShingle Soerensen, Anne
Jacob, Daniel James
Schartup, Amina
Fisher, Jenny
Lehnherr, Igor
St. Louis, Vincent L.
Heimbürger, Lars-Eric
Sonke, Jeroen E.
Krabbenhoft, David P.
Sunderland, Elynor M
A mass budget for mercury and methylmercury in the Arctic Ocean
author_facet Soerensen, Anne
Jacob, Daniel James
Schartup, Amina
Fisher, Jenny
Lehnherr, Igor
St. Louis, Vincent L.
Heimbürger, Lars-Eric
Sonke, Jeroen E.
Krabbenhoft, David P.
Sunderland, Elynor M
author_sort Soerensen, Anne
title A mass budget for mercury and methylmercury in the Arctic Ocean
title_short A mass budget for mercury and methylmercury in the Arctic Ocean
title_full A mass budget for mercury and methylmercury in the Arctic Ocean
title_fullStr A mass budget for mercury and methylmercury in the Arctic Ocean
title_full_unstemmed A mass budget for mercury and methylmercury in the Arctic Ocean
title_sort mass budget for mercury and methylmercury in the arctic ocean
publisher Wiley-Blackwell
publishDate 2016
url http://nrs.harvard.edu/urn-3:HUL.InstRepos:33983357
https://doi.org/10.1002/2015GB005280
geographic Arctic
Arctic Ocean
geographic_facet Arctic
Arctic Ocean
genre Arctic
Arctic
Arctic Ocean
Ice
permafrost
Sea ice
genre_facet Arctic
Arctic
Arctic Ocean
Ice
permafrost
Sea ice
op_relation doi:10.1002/2015GB005280
Global Biogeochemical Cycles
Soerensen, Anne L., Daniel J. Jacob, Amina T. Schartup, Jenny A. Fisher, Igor Lehnherr, Vincent L. St. Louis, Lars-Eric Heimbürger, Jeroen E. Sonke, David P. Krabbenhoft, and Elsie M. Sunderland. 2016. “A Mass Budget for Mercury and Methylmercury in the Arctic Ocean.” Global Biogeochemical Cycles 30 (4) (April): 560–575. Portico. doi:10.1002/2015gb005280.
0886-6236
http://nrs.harvard.edu/urn-3:HUL.InstRepos:33983357
op_doi https://doi.org/10.1002/2015GB005280
https://doi.org/10.1002/2015gb005280
container_title Global Biogeochemical Cycles
container_volume 30
container_issue 4
container_start_page 560
op_container_end_page 575
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