Abstract
Globally, at least 5 Mt yr−1 of chloromethane (CH3Cl) must originate from natural sources, according to estimates based on environmental concentrations, man-made emissions of 26 kt yr−1 being insignificant in comparison1–3. Although CH3C1 is a natural product of several fungal species4,5, no quantitative investigations of its biological production have been reported. We have measured CH3C1 production by a common wood-rotting fungus, and report that on glucose-based media, the chloride ion (Cl−) at concentrations <4 mM was methylated with >90% efficiency. The pattern of CH3C1 biogenesis was typical of a secondary metabolite and paralleled loss of Cl− from the medium. With cellulosic substrates, CH3C1 yields ranged between 80 and 95% at Cl− concentrations as high as 25 mM, although production extended over a longer period. Bromo- and iodomethane were formed in high yield from the corresponding halide ions. Such high-efficiency methylation of the halide ion indicates that fungi could make a substantial contribution to the atmospheric CH3C1 burden.
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Harper, D. Halomethane from halide ion—a highly efficient fungal conversion of environmental significance. Nature 315, 55–57 (1985). https://doi.org/10.1038/315055a0
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DOI: https://doi.org/10.1038/315055a0
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