Scytonemin
Scytonemin is a secondary metabolite and an extracellular matrix (sheath) pigment synthesized by many strains of cyanobacteria, including Nostoc, Scytonema, Calothrix, Lyngbya, Rivularia, Chlorogloeopsis, and Hyella. Scytonemin-synthesizing cyanobacteria often inhabit highly insolated terrestrial, freshwater and coastal environments such as deserts, semideserts, rocks, cliffs, marine intertidal flats, and hot springs.
The pigment was originally discovered in 1849 by Swiss botanist Carl Nägeli, although the structure remained unsolved until 1993. It is an aromatic indole alkaloid built from two identical condensation products of tryptophan
It is believed that scytonemin acts as a highly efficient protective biomolecule that filters out damaging high frequency UV rays while at the same time allowing the transmittance of wavelengths necessary for photosynthesis. Its biosynthesis in cyanobacteria is mostly triggered by exposure to [UV light|UV-A and UV-B wavelengths.]
Recently, Couradeau and coworkers found that cyanobacterial soil crusts warm the soil surface by as much as 10 °C through the production and accumulation of scytonemin pigments. This effect is due to the dissipation of the absorbed photons by the scytonemin molecules into heat.
Biosynthesis
The biosynthesis in Lyngbya aestuarii was recently explored by Balskus, Case, and Walsh. It proceeds by the conversion of L-tryptophan to 3-indole pyruvic acid, followed by coupling to p-hydroxyphenylpyruvic acid. Cyclization of the resultant β-ketoacid yields a tricyclic ketone. Oxidation and dimerization yields the completed natural product. Three scytonemin biosynthetic enzymes are necessary, denoted as ScyA-C.[Image:Scytonemin biosynthesis.png|880x880px|center|Scytonemin biosynthesis in Lyngbya aestuarii.]