Global warming accelerates uptake of atmospheric mercury in regions experiencing glacier retreat

As global climate continues to warm, melting of glaciers releases a large quantity of mercury (Hg) originally locked in ice into the atmosphere and downstream ecosystems. Here, we show an opposite process that captures atmospheric Hg through glacier-to-vegetation succession. Our study using stable i...

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Published in:Proceedings of the National Academy of Sciences
Main Authors: Wang, Xun, Luo, Ji, Yuan, Wei, Lin, Che-Jen, Wang, Feiyue, Liu, Chen, Wang, Genxu, Feng, Xinbin
Format: Text
Language:English
Published: National Academy of Sciences 2020
Subjects:
Online Access:http://www.ncbi.nlm.nih.gov/pmc/articles/PMC6995023/
http://www.ncbi.nlm.nih.gov/pubmed/31932430
https://doi.org/10.1073/pnas.1906930117
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author Wang, Xun
Luo, Ji
Yuan, Wei
Lin, Che-Jen
Wang, Feiyue
Liu, Chen
Wang, Genxu
Feng, Xinbin
author_facet Wang, Xun
Luo, Ji
Yuan, Wei
Lin, Che-Jen
Wang, Feiyue
Liu, Chen
Wang, Genxu
Feng, Xinbin
author_sort Wang, Xun
collection PubMed Central (PMC)
container_issue 4
container_start_page 2049
container_title Proceedings of the National Academy of Sciences
container_volume 117
description As global climate continues to warm, melting of glaciers releases a large quantity of mercury (Hg) originally locked in ice into the atmosphere and downstream ecosystems. Here, we show an opposite process that captures atmospheric Hg through glacier-to-vegetation succession. Our study using stable isotope techniques at 3 succession sites on the Tibetan Plateau reveals that evolving vegetation serves as an active “pump” to take up gaseous elemental mercury (Hg(0)) from the atmosphere. The accelerated uptake enriches the Hg pool size in glacier-retreated areas by a factor of ∼10 compared with the original pool size in the glacier. Through an assessment of Hg source–sink relationship observed in documented glacier-retreated areas in the world (7 sites of tundra/steppe succession and 5 sites of forest succession), we estimate that 400 to 600 Mg of Hg has been accumulated in glacier-retreated areas (5‰ of the global land surface) since the Little Ice Age (∼1850). By 2100, an additional ∼300 Mg of Hg will be sequestered from the atmosphere in glacier-retreated regions globally, which is ∼3 times the total Hg mass loss by meltwater efflux (∼95 Mg) in alpine and subpolar glacier regions. The recapturing of atmospheric Hg by vegetation in glacier-retreated areas is not accounted for in current global Hg models. Similar processes are likely to occur in other regions that experience increased vegetation due to climate or land use changes, which need to be considered in the assessment of global Hg cycling.
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spelling ftpubmed:oai:pubmedcentral.nih.gov:6995023 2025-01-17T01:12:18+00:00 Global warming accelerates uptake of atmospheric mercury in regions experiencing glacier retreat Wang, Xun Luo, Ji Yuan, Wei Lin, Che-Jen Wang, Feiyue Liu, Chen Wang, Genxu Feng, Xinbin 2020-01-28 http://www.ncbi.nlm.nih.gov/pmc/articles/PMC6995023/ http://www.ncbi.nlm.nih.gov/pubmed/31932430 https://doi.org/10.1073/pnas.1906930117 en eng National Academy of Sciences http://www.ncbi.nlm.nih.gov/pmc/articles/PMC6995023/ http://www.ncbi.nlm.nih.gov/pubmed/31932430 http://dx.doi.org/10.1073/pnas.1906930117 https://www.pnas.org/site/aboutpnas/licenses.xhtmlPublished under the PNAS license (https://www.pnas.org/site/aboutpnas/licenses.xhtml) . Proc Natl Acad Sci U S A Biological Sciences Text 2020 ftpubmed https://doi.org/10.1073/pnas.1906930117 2020-07-19T00:16:34Z As global climate continues to warm, melting of glaciers releases a large quantity of mercury (Hg) originally locked in ice into the atmosphere and downstream ecosystems. Here, we show an opposite process that captures atmospheric Hg through glacier-to-vegetation succession. Our study using stable isotope techniques at 3 succession sites on the Tibetan Plateau reveals that evolving vegetation serves as an active “pump” to take up gaseous elemental mercury (Hg(0)) from the atmosphere. The accelerated uptake enriches the Hg pool size in glacier-retreated areas by a factor of ∼10 compared with the original pool size in the glacier. Through an assessment of Hg source–sink relationship observed in documented glacier-retreated areas in the world (7 sites of tundra/steppe succession and 5 sites of forest succession), we estimate that 400 to 600 Mg of Hg has been accumulated in glacier-retreated areas (5‰ of the global land surface) since the Little Ice Age (∼1850). By 2100, an additional ∼300 Mg of Hg will be sequestered from the atmosphere in glacier-retreated regions globally, which is ∼3 times the total Hg mass loss by meltwater efflux (∼95 Mg) in alpine and subpolar glacier regions. The recapturing of atmospheric Hg by vegetation in glacier-retreated areas is not accounted for in current global Hg models. Similar processes are likely to occur in other regions that experience increased vegetation due to climate or land use changes, which need to be considered in the assessment of global Hg cycling. Text Tundra PubMed Central (PMC) Proceedings of the National Academy of Sciences 117 4 2049 2055
spellingShingle Biological Sciences
Wang, Xun
Luo, Ji
Yuan, Wei
Lin, Che-Jen
Wang, Feiyue
Liu, Chen
Wang, Genxu
Feng, Xinbin
Global warming accelerates uptake of atmospheric mercury in regions experiencing glacier retreat
title Global warming accelerates uptake of atmospheric mercury in regions experiencing glacier retreat
title_full Global warming accelerates uptake of atmospheric mercury in regions experiencing glacier retreat
title_fullStr Global warming accelerates uptake of atmospheric mercury in regions experiencing glacier retreat
title_full_unstemmed Global warming accelerates uptake of atmospheric mercury in regions experiencing glacier retreat
title_short Global warming accelerates uptake of atmospheric mercury in regions experiencing glacier retreat
title_sort global warming accelerates uptake of atmospheric mercury in regions experiencing glacier retreat
topic Biological Sciences
topic_facet Biological Sciences
url http://www.ncbi.nlm.nih.gov/pmc/articles/PMC6995023/
http://www.ncbi.nlm.nih.gov/pubmed/31932430
https://doi.org/10.1073/pnas.1906930117