A subfossil larch, 14500 years old, collected in a clay quarry of Revi
ne (Venetian Prealps, Italy), was examined with respect to its dichlor
omethane extractives which were compared with those of a living ]arch.
Results have shown that most of terpenes were markedly changed and si
milarities with several samples of 1-3 million years Taxodioxylon gyps
aceum were evident. The particularly moist environment has modified mo
st of original wood extractives: monoterpenes and sesquiterpenes were
nearly all lost, diterpenes were transformed into stable diterpene-rel
ated hydrocarbons such as sandaracopimarane, abietane, alpha-phyllocla
dane and simonellite, whilst waxes were subjected to hydrolysis. Resul
ts seem to demonstrate that degradation of extractives during aging of
wood takes place in the early stages of this process.