Mercury and Sulfur Redox Cycling Affect Methylmercury Levels in Rice Paddy Soils across a Contamination Gradient

Methylmercury (MeHg) contamination in rice via paddy soils is an emerging global environmental issue. An understanding of mercury (Hg) transformation processes in paddy soils is urgently needed in order to control Hg contamination of human food and related health impacts. Sulfur (S)-regulated Hg transformation is one important process that controls Hg cycling in agricultural fields. In this study, Hg transformation processes, such as methylation, demethylation, oxidation, and reduction, and their responses to S input (sulfate and thiosulfate) in paddy soils with a Hg contamination gradient were elucidated simultaneously using a multi-compound-specific isotope labeling technique ( 200 Hg II, Me 198 Hg, and 202 Hg 0 ). In addition to Hg II methylation and MeHg demethylation, this study revealed that microbially mediated reduction of Hg II, methylation of Hg 0, and oxidative demethylation–reduction of MeHg occurred under dark conditions; these processes served to transform Hg between different species (Hg 0, Hg II, and MeHg) in flooded paddy soils. Rapid redox recycling of Hg species contributed to Hg speciation resetting, which promoted the transformation between Hg 0 and MeHg by generating bioavailable Hg II for fuel methylation. Sulfur input also likely affected the microbial community structure and functional profile of Hg II methylators and, therefore, influenced Hg II methylation. The findings of this study contribute to our understanding of Hg transformation processes in paddy soils and provide much-needed knowledge for assessing Hg risks in hydrological fluctuation-regulated ecosystems.