| Literature DB >> 27836473 |
Hong-Wei Luo1, Xiangping Yin2, Aaron M Jubb2, Hongmei Chen2, Xia Lu2, Weihua Zhang3, Hui Lin2, Han-Qing Yu4, Liyuan Liang5, Guo-Ping Sheng4, Baohua Gu6.
Abstract
Atmospheric deposition of mercury (Hg) to surface water is one of the dominant sources of Hg in aquatic environments and ultimately drives methylmercury (MeHg) toxin accumulation in fish. It is known that freshly deposited Hg is more readily methylated by microorganisms than aged or preexisting Hg; however the underlying mechanism of this process is unclear. We report that Hg bioavailability is decreased by photochemical reactions between Hg and dissolved organic matter (DOM) in water. Photo-irradiation of Hg-DOM complexes results in loss of Sn(II)-reducible (i.e. reactive) Hg and up to an 80% decrease in MeHg production by the methylating bacterium Geobacter sulfurreducens PCA. Loss of reactive Hg proceeded at a faster rate with a decrease in the Hg to DOM ratio and is attributed to the possible formation of mercury sulfide (HgS). These results suggest a new pathway of abiotic photochemical formation of HgS in surface water and provide a mechanism whereby freshly deposited Hg is readily methylated but, over time, progressively becomes less available for microbial uptake and methylation. Copyright ÂEntities:
Keywords: Biogeochemical transformation; Dissolved organic matter; Hg-DOM photolysis; HgS precipitation; Methylmercury
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Year: 2016 PMID: 27836473 DOI: 10.1016/j.envpol.2016.10.099
Source DB: PubMed Journal: Environ Pollut ISSN: 0269-7491 Impact factor: 8.071