Although aerobic methane (CH 4 ) release from plants leads to an intense scientific and public controversy in the recent years, the potential functions of endogenous CH 4 production in plants are still largely unknown. Here, we reported that polyethylene glycol (PEG)-induced osmotic stress significantly increased CH 4 production and soluble sugar contents in maize (Zea mays L.) root tissues. These enhancements were more pronounced in the drought stress-tolerant cultivar Zhengdan 958 (ZD958) than in the drought stress-sensitive cultivar Zhongjiangyu No.1 (ZJY1). Exogenously applied 0.65 mM CH 4 not only increased endogenous CH 4 production, but also decreased the contents of thiobarbituric acid reactive substances. PEG-induced water deficit symptoms, such as decreased biomass and relative water contents in both root and shoot tissues, were also alleviated. These beneficial responses paralleled the increases in the contents of soluble sugar and the reduced ascorbic acid (AsA), and the ratio of AsA/dehydroascorbate (DHA). Further comparison of transcript profiles of some key enzymes in sugar and AsA metabolism suggested that CH 4 might participate in sugar signaling, which in turn increased AsA production and recycling. Together, these results suggested that CH 4 might function as a gaseous molecule that enhances osmotic stress tolerance in maize by modulating sugar and AsA metabolism.Methane (CH 4 ) is the most abundant reduced organic compound in the atmosphere, and also the second important greenhouse gas after carbon dioxide 1,2 . It was previously considered as a degradation product of organic substance by microbes under anoxic conditions 3 . Keppler et al. 4 further reported a surprising discovery that terrestrial plants can produce CH 4 under aerobic conditions. Although much controversy and debate followed this original work, a number of researchers have attempted to provide alternate explanations of the aerobic CH 4 formation from plants using different scales of measurement 5 . In fact, the non-microbial CH 4 production from plants constitutes a significant fraction of the global CH 4 sources 2,6 . A comprehensive understanding of CH 4 in plants is that the living plants and fungi can not only emit CH 4 to the atmosphere 7 , but also produce CH 4 in plants in vivo 8 . Interestingly, this phenomenon was observed in the researches of nitric oxide 9 , carbon monoxide 10 , as well as hydrogen gas 11 . In some plant species, several chemical compounds, such as lignin, cellulose, leaf surface wax, ascorbic acid (AsA), the methyl groups of sulphur-containing amino acid methionine (Met), were suggested to be the potential precursors of CH 4 2,5,12,13 .