4.7 Article

Chemical kinetic isotope fractionation of mercury during abiotic methylation of Hg(II) by methylcobalamin in aqueous chloride media

Journal

CHEMICAL GEOLOGY
Volume 336, Issue -, Pages 26-36

Publisher

ELSEVIER
DOI: 10.1016/j.chemgeo.2012.08.029

Keywords

Mercury (Hg); Stable isotope fractionation; Abiotic methylation; Hg-chloro complexes; Methylcobalamin

Funding

  1. Castilla-La Mancha Government
  2. European Social Fund
  3. Ministere de l'enseignement superieur et de la recherche [ED211]
  4. French National Research Agency (ANR)
  5. IDEA project [ANR-08-CES-013]

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Mercury (Hg) is assumed to be predominantly methylated by microorganisms in the environment. However, the mechanisms and extent of abiotic methylation are poorly appreciated. The understanding of the mechanisms leading to abiotic methylation and demethylation in the aquatic environment is of special concern since methylmercury (MeHg) biomagnifies in the food web. Bioaccumulating organisms have also been found to preserve specific Hg isotopic signatures that provide direct insight into aquatic Hg transformations. In this study we investigated the influence of chloride on the magnitude of Hg isotope fractionation during abiotic methylation of inorganic Hg (Hg(II)) using methylcobalamin as methyl donor compound. Coupling of gas chromatography with multi-collector inductively coupled plasma mass spectrometry has allowed to determine simultaneously isotopic ratios of inorganic and methyl-Hg species. Kinetic experiments demonstrated that the presence of chloride not only slowed the chemical alkylation of Hg(II) by methylcobalamin, but also decreased the extent of the methylation, which it is especially significant under visible light conditions due to the enhancement of MeHg photodecomposition. Abiotic methylation of Hg(II) by methylcobalamin in the presence of chloride caused significant Hg mass-dependent isotope fractionation (MDF) for both Hg(II) substrate (delta Hg-202(II) from -0.74 parts per thousand to 2.48 parts per thousand) and produced MeHg (delta(MeHg)-Me-202 from -1.44 parts per thousand to 0.38 parts per thousand) both under dark and visible light conditions. The value of this MDF under such saline conditions was higher than that previously reported (delta(MeHg)-Me-202 from -0.73 parts per thousand to 0.09 parts per thousand) in the absence of chloride and appeared mainly related to inorganic Hg speciation in solution, which is predominantly mercuric chloro-complexes (i.e. HgCl42-). Different isotopic signatures were observed for the different Hg species at the same time of reaction for either dark or visible light (450-650 nm wavelengths) conditions. However, no significant mass-independent fractionation (MIF) was induced under any conditions within the analytical uncertainties (-0.17 +/- 0.31

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