Geosmin is produced as a
secondary metabolite by various blue-green algae (
cyanobacteria), filamentous bacteria in the class
Actinomyces, other prokaryotes, and various eukaryotes. The main genera in the cyanobacteria that have been shown to produce geosmin include
Anabaena,
Phormidium, and
Planktothrix, while the main genus in the Actinomyces that produces geosmin is
Streptomyces. In
beetroots, geosmin is produced endogenously, not by environmental nor
endophytic microbes, suggesting beets possess separate or acquired means of geosmin biosynthesis. Communities whose
water supplies depend on surface water can periodically experience episodes of unpleasant-tasting water when a sharp drop in the population of these bacteria releases geosmin into the local water supply. Under
acidic conditions, geosmin decomposes into odorless substances. In 2006, geosmin was
biosynthesized by a bifunctional
Streptomyces coelicolor enzyme. A single enzyme,
geosmin synthase, converts
farnesyl diphosphate to geosmin in a two-step reaction. The production and dispersal of the compound may give an evolutionary advantage to the producers. Geosmin and 2-methylisoborneol have been shown to attract
springtails,
Folsomia candida, which are believed to feed on and spread the spores of
Streptomyces both through their feces and by attachment to their cuticle. Not all blue-green algae produce geosmin. Identification of species that might produce geosmin is traditionally done through microscopic identification of geosmin-producing algae, a process that is labor-intensive and requires specialized knowledge. Recently a geosmin synthase gene
geoA, was identified, which is present in cyanobacterial species that produce geosmin, but is not present in other cyanobacterial species. Amplification of this gene from water samples using
real-time PCR may permit predictions of taste and odor events caused by cyanobacteria in fresh water. == Effects ==