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Investigation of Hg uptake and transport between paddy soil and rice seeds combining Hg isotopic composition and speciation

Bibliographic Data

ID19569113
AuthorsCaiyan Feng (0000-0003-0153-5720, Centre National de la Recherche Scientifique), Zoyne Pedrero (0000-0001-6226-152X, Centre National de la Recherche Scientifique), Ping Li (0000-0002-0813-0980, Chinese Academy of Sciences), Buyun Du (0000-0001-6902-1131, Chinese Academy of Sciences), Xinbin Feng (0000-0002-7462-8998, Chinese Academy of Sciences), Mathilde Monperrus (0000-0002-6337-1672, Centre National de la Recherche Scientifique), Emmanuel Tessier (0000-0003-1672-9894, Centre National de la Recherche Scientifique), Sylvain Bérail (0000-0002-5637-3696, Centre National de la Recherche Scientifique), David Amouroux (0000-0002-0056-8590, Centre National de la Recherche Scientifique)
EditorsJoel D Blum (0000-0001-5389-8633), Holger Hintelmann (0000-0002-5287-483X)
Year2016
Volume4
Publication date2016-01-01
Open AccessYes
TypeARTICLE
VenueElementa Science of the Anthropocene (JOURNAL)
Journal identifiersISSN: 2325-1026 • E-ISSN: 2325-1026
PublisherUniversity of California Press (PUBLISHER • US)
DOI10.12952/journal.elementa.000087
OpenAlexW2280763286
LanguageEN
References cited51

Human consumption of rice constitutes a potential toxicological risk in mercury (Hg) polluted areas such as Hg mining regions in China. It is recognized to be an important source of Hg for the local human diet considering the efficient bioaccumulation of methylmercury (MeHg) in rice seed. To assess Hg sources and uptake pathways to the rice plants, Hg speciation and isotopic composition were investigated in rice seeds and their corresponding paddy soils from different locations within the Wanshan Hg mining area (Guizhou Province, China). A large variation of Hg speciation is observed in rice seeds and paddy soils irrespective of the sampling location. Mass dependent fractionation (MDF) of Hg in rice seeds differs by up to ∼4.0 ‰ in δ202Hg values, while mass independent fractionation (MIF) of Hg isotopes remains constant (Δ199Hg ∼ 0‰). Hg isotopic composition in rice seeds covaries with that of paddy soils but exhibits lighter isotopic signature (δ202Hg). Such isotopic offset is mainly attributed to plant uptake and translocation processes. Also, seeds containing higher MeHg (MeHg/total Hg > 50%) have significantly heavier Hg isotopes suggesting that MeHg uptake and transport to the seed in such rice plants is facilitated compared to inorganic Hg

Agronomy · Bioaccumulation · Bioconcentration · Biology · Fractionation · Genetic algorithm · Isotope · Isotope fractionation · Isotopic signature · Methylmercury · Paddy field · Rice plant · Soil water · Chemistry · Environmental Science · Heavy Metal Exposure and Toxicity · Heavy metals in environment · Mercury impact and mitigation studies · Ecology · Environmental Chemistry · Soil Science

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