Mfs. Goni et Ge. Hannon, High-altitude vegetational pattern on the Iberian Mountain Chain (north-central Spain) during the Holocene, HOLOCENE, 9(1), 1999, pp. 39-57
Pollen, plant macrofossil, charcoal, sedimentary analyses and magnetic susc
eptibility measurements have been carried out on a C-14 dated sediment sequ
ence from Las Pardillas Lake (1850 m a.s.l., Iberian Mountain Chain). The i
nterpretation of the pollen diagram has been assisted by the analysis of an
altitudinal transect of moss-polsters collected in the same area. After 93
10 BP, a Pinus-Betula-Quercus open woodland developed. Between c. 9000 BP a
nd 7100 BP, the woodland became a mixed forest with Pinus sylvestris. The b
eginning of the continuous curve of Corylus c. 9000 BP dated the local popu
lation expansion of this tree and is 1000 yeats earlier than the age previo
usly attributed to its expansion in north-central Spain. At c. 7400 BP a lo
cal fire is associated with a possible first establishment of Fagus in the
area. From c. 7100 BP to c. 3700 BP, Taxus, Ilex and Hedera were present in
the forest vegetation. During this interval, the pollen and sedimentologic
al record indicated a stable period of rich, mixed Quercus forest. At the s
ame time, the community of floating-leaved aquatics was replaced by submerg
ed plants, suggesting that a rise in lake water level may have occurred bet
ween 7200 and 6400 BP. Fagus became continuously present in the Las Pardill
as Lake area c. 3200 BP. As Fagus is fire-sensitive, the expansion and stan
d scale establishment may be linked to an increase in fire regime, a type o
f disturbance which has facilitated the spread of this taxon elsewhere in E
urope. A significant forest reduction, involving all the trees, took place
c. 1500 BP. Between 1000 and 400 BP, Pinus and Fagus re-expanded associated
with the first clear evidence of agricultural activity. The well-represent
ed mixed Quercus forest around Las Pardillas Lake, and the early developmen
t of Corylus compared to other Mediterranean zones, suggests that oceanic c
onditions prevailed on the northern slopes of these mountains in north-cent
ral Spain.