CLIMATE VARIATION AND THE STABLE CARBON-ISOTOPE COMPOSITION OF TREE-RING CELLULOSE - AN INTERCOMPARISON OF QUERCUS-ROBUR, FAGUS-SYLVATICA AND PINUS-SILVESTRIS
Dl. Hemming et al., CLIMATE VARIATION AND THE STABLE CARBON-ISOTOPE COMPOSITION OF TREE-RING CELLULOSE - AN INTERCOMPARISON OF QUERCUS-ROBUR, FAGUS-SYLVATICA AND PINUS-SILVESTRIS, Tellus. Series B, Chemical and physical meteorology, 50(1), 1998, pp. 25-33
The relationship between climate parameters and the carbon stable isot
ope composition, (delta(13)C), of annual tree ring cellulose is examin
ed for three native British tree species; Common beech (Fagus sylvatic
a L.), Pedunculate oak (Quercus robur L.) and Scots pine (Pinus sylves
tris L.). The last 100 annual tree rings of six trees, two of each spe
cies, were cut into slivers and the ct-cellulose extracted. Annual del
ta(13)C values of each species were averaged to produce three species
delta(13)C chronologies. These were compared with climate parameters f
rom a nearby meteorological station. The carbon stable isotope discrim
ination (Delta(13)C) Of pine is consistently lower, by approximately 2
.5 parts per thousand, than that of beech and oak. Although the exact
cause of this offset cannot be identified, similar differences in carb
on isotope ratios have been noted between other gymnosperm and angiosp
erm species and attributed to inherent physiological differences. As t
his offset is consistent, once centered around the same mean delta(13)
C and Delta(13)C chronologies from these 3 species can be combined. De
lta(13)C chronologies of the three species demonstrate strong crosscor
relations in both high and low frequency fluctuations. Low frequency f
luctuations, although consistent between species, show no direct clima
te relationship, and may be linked with physiological responses to inc
reasing CO2 concentrations. Significant correlations do exist between
the high frequency delta(13)C fluctuations and climate parameters. The
high frequency delta(13)C series of all three species are most signif
icantly correlated with the same two climate parameters and have the s
ame seasonal timing; July-October average maximum temperature and June
-September average relative humidity. Pine delta(13)C is the most resp
onsive species to climate changes and displays the most significant co
rrelations with all the climate parameters studied However, an average
series of all three high frequency species delta(13)C series shows th
e most significant correlations with climate. Assuming these relations
hips are consistent spatially and temporally, high frequency delta(13)
C chronologies from the three species studied are climatically compara
ble and can be combined to reconstruct the same climatic information.