The comparison of the steam distillate from a 20 million years old Tax
odioxylon gypsaceum with that of a corresponding 1.5 million years old
sample has permitted the description of the last steps of terpene deg
radation of this species. The main feature is the reduced number of co
mponents in the older sample which contains over 97% of alpha-phyllocl
adane and traces of other components present, by contrast, in the youn
ger one. The lack of new compounds, related to the lost components, su
ggests leaching to be the cause of the losses. This seems to be confir
med by the analysis of the inner part of a trunk of one of the younger
samples presently subjected to a sort of natural leaching. Analyses i
ndicate an increase in alpha-phyllocladane and a severe reduction in s
imonellite as well as other terpenes, together with the formation of t
wo new compounds of 164 and 222 MWs. The occurrence of alpha-phyllocla
dane in other European lignites suggests the choice of this compound a
s a biomarker of the species Taxodioxylon gypsaceum.