The pigment was originally discovered in 1849 by Swiss botanist Carl Nägeli,[3] although the structure remained unsolved until 1993.[4] It is an aromaticindole alkaloid built from two identical condensation products of tryptophanyl- and tyrosyl-derived subunits linked through a carbon-carbon bond.[4] Depending on the redox conditions it can exist in two inter-convertible forms: a more common oxidized yellow-brown form which is insoluble in water and only slightly soluble in organic solvents, such as pyridine, and a reduced form with bright red color that is more soluble in organic solvents.[5] Scytonemin absorbs very strongly and very broadly across the UV-C-UV-B-UV-A-violet-bluespectral region, with an in vivo maximum absorption at 370 nm and an in vitro maximum absorption at 386 and 252 nm, and with smaller peaks at 212, 278 and 300 nm.[6]
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.[10] This effect is due to the dissipation of the absorbed photons by the scytonemin molecules into heat.
^ abProteau, P. J.; Gerwick, W. H.; Garcia-Pichel, F.; Castenholz, R. (1993). "The structure of scytonemin, an ultraviolet sunscreen pigment from the sheaths of cyanobacteria". Experientia. 49 (9): 825–9. doi:10.1007/BF01923559. PMID8405307. S2CID22975257.