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Journal Article

Hydrogen Cyanide Accumulation and Transformations in Non-polluted Salt Marsh Sediments


Kamyshny,  A.
Department of Biogeochemistry, Max Planck Institute for Marine Microbiology, Max Planck Society;

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Kamyshny, A., Oduro, H., Mansaray, Z. F., & Farquhar, J. (2013). Hydrogen Cyanide Accumulation and Transformations in Non-polluted Salt Marsh Sediments. Aquatic Geochemistry, 19(2), 97-113.

Cite as: https://hdl.handle.net/21.11116/0000-0001-C713-9
While cyanide is known to be produced by many organisms, including plants, bacteria, algae, fungi and some animals, it is generally thought that high levels of cyanide in aquatic systems require anthropogenic sources. Here, we report accumulation of relatively high levels of cyanide in non-polluted salt marsh sediments (up to 230 mu mol kg(-1)). Concentrations of free cyanide up to 1.92 mu mol L-1, which are toxic to aquatic life, were detected in the pore-waters. Concentration of total (free and complexed) cyanide in the pore-waters was up to 6.94 mu mol L-1. Free cyanide, which is released to the marsh sediments, is attributed to processes associated with decomposition of cord grass, Spartina alterniflora, roots and possibly from other sources. This cyanide is rapidly complexed with iron and adsorbed on sedimentary organic matter. The ultimate cyanide sink is, however, associated with formation of thiocyanate by reaction with products of sulfide oxidation by Fe(III) minerals, especially polysulfides. The formation of thiocyanate by this pathway detoxifies two poisonous compounds, polysulfides and hydrogen cyanide, preventing release of free hydrogen cyanide from salt marsh sediments into overlying water or air.