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Large subglacial source of mercury from the southwestern margin of the Greenland Ice Sheet

The result's identifiers

  • Result code in IS VaVaI

    <a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F61388971%3A_____%2F21%3A00546869" target="_blank" >RIV/61388971:_____/21:00546869 - isvavai.cz</a>

  • Alternative codes found

    RIV/00216208:11310/21:10431643

  • Result on the web

    <a href="https://www.nature.com/articles/s41561-021-00753-w" target="_blank" >https://www.nature.com/articles/s41561-021-00753-w</a>

  • DOI - Digital Object Identifier

    <a href="http://dx.doi.org/10.1038/s41561-021-00753-w" target="_blank" >10.1038/s41561-021-00753-w</a>

Alternative languages

  • Result language

    angličtina

  • Original language name

    Large subglacial source of mercury from the southwestern margin of the Greenland Ice Sheet

  • Original language description

    The Greenland Ice Sheet is currently not accounted for in Arctic mercury budgets, despite large and increasing annual runoff to the ocean and the socio-economic concerns of high mercury levels in Arctic organisms. Here we present concentrations of mercury in meltwaters from three glacial catchments on the southwestern margin of the Greenland Ice Sheet and evaluate the export of mercury to downstream fjords based on samples collected during summer ablation seasons. We show that concentrations of dissolved mercury are among the highest recorded in natural waters and mercury yields from these glacial catchments (521-3,300 mmol km(-2) year(-1)) are two orders of magnitude higher than from Arctic rivers (4-20 mmol km(-2) year(-1)). Fluxes of dissolved mercury from the southwestern region of Greenland are estimated to be globally significant (15.4-212 kmol year(-1)), accounting for about 10% of the estimated global riverine flux, and include export of bioaccumulating methylmercury (0.31-1.97 kmol year(-1)). High dissolved mercury concentrations (similar to 20 pM inorganic mercury and similar to 2 pM methylmercury) were found to persist across salinity gradients of fjords. Mean particulate mercury concentrations were among the highest recorded in the literature (similar to 51,000 pM), and dissolved mercury concentrations in runoff exceed reported surface snow and ice values. These results suggest a geological source of mercury at the ice sheet bed. The high concentrations of mercury and its large export to the downstream fjords have important implications for Arctic ecosystems, highlighting an urgent need to better understand mercury dynamics in ice sheet runoff under global warming.

  • Czech name

  • Czech description

Classification

  • Type

    J<sub>imp</sub> - Article in a specialist periodical, which is included in the Web of Science database

  • CEP classification

  • OECD FORD branch

    10606 - Microbiology

Result continuities

  • Project

    Result was created during the realization of more than one project. More information in the Projects tab.

  • Continuities

    I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Others

  • Publication year

    2021

  • Confidentiality

    S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Data specific for result type

  • Name of the periodical

    Nature Geoscience

  • ISSN

    1752-0894

  • e-ISSN

    1752-0908

  • Volume of the periodical

    14

  • Issue of the periodical within the volume

    7

  • Country of publishing house

    GB - UNITED KINGDOM

  • Number of pages

    7

  • Pages from-to

    496-502

  • UT code for WoS article

    000653667000001

  • EID of the result in the Scopus database

    2-s2.0-85106294398