Modern wood was subjected to an artificial decay process to investigate its
behaviour with respect to the stable carbon isotope composition of wood an
d the corresponding cellulose. Four different woods were used, namely: oak
(Quercus robur), beech (Fagus sylvatica), pine (Pinus sylvestris), sequoia
(Sequoiadendron giganteum) and pure spruce cellulose. The process of decay
was simulated by heating samples in water at 180 degrees C from minutes to
months. During the decay period, the carbon content of wood increased to al
most 70% while the cellulose content decreased gradually to zero. The degra
dation proceeds according to a two stage process: an initial Very fast brea
k down is followed by a rather slow degradation. After a strong discriminat
ion against C-13 during the initial phase, the C-13/C-12 ratio increases ag
ain, mostly up to its initial value. The carbon isotope trend for cellulose
shows a similar pattern though it is less pronounced. Maximum discriminati
on was 1 parts per thousand relative to the untreated wood. delta(13)C valu
es of cellulose decreased by up to 0.3 parts per thousand. The C-13 depleti
on is presumably a consequence of the preferential decomposition of cellulo
se as compared to lignin. Data on fossil trees are compared with the result
s obtained from this treatment of aging. The C-13 decrease is in line with
observations from these fossil woods, but the ensuing C-13 enrichment is at
most weakly to be seen. (C) 1999 Elsevier Science B.V. All rights reserved
.