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Volatile C1–C8 organic compounds in macroalgae

Abstract

Small amounts of C1–C8 volatile organic compounds were found in macroalgae in concentrations high enough (generally in the range of 1–400 times those in sediments) to suggest that the seaweeds are a source for some of the volatile organic compounds identified in recent marine sediments. The types of compounds identified1–4 include alkanes, alkenes, aldehydes, ketones, furans, and sulphides. Both the light hydrocarbons and the volatile functionalized organic compounds are believed to originate from living organisms and from both biological and chemical low-temperature reactions in the sediments. Understanding their mechanism of formation may help in deciphering the thermal and biological history of the sediments. Traces of some of these compounds can be produced from bacterial degradation of naturally occurring terpenoids5. We consider here their occurrence in algae.

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Whelan, J., Tarafa, M. & Hunt, J. Volatile C1–C8 organic compounds in macroalgae. Nature 299, 50–52 (1982). https://doi.org/10.1038/299050a0

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