Litterfall is the first phase of the biogeochemical cycle and returns nutri
ents to the soil. This paper demonstrates the quantitative distribution of
the different components throughout the year in four stands of a beech time
sequence. Litterfall increases as the forest evolves and as basal area inc
reases: from 2.1 t/ha/an in the thicket to 4.7 t/ha/an in the mature high f
orest. Leaves represent 90% of the total litterfall in the young stand and
70% in the oldest stand. The proportion of leaves decreases during forest r
otation. Most of the categories are related to the age and basal area, beca
use of the architecture and maturity of the trees. Other factors could expl
ain litterfall dynamics, e.g. human management or animals. Climate is a pre
ponderant factor for the litterfall production and plays a role in the spec
ies phenology. The litterfall dynamics during the time sequence, and the ob
served shifts in phenology give rise to different pedogenetic processes.