B. Berg et al., LITTER MASS-LOSS RATES IN PINE FORESTS OF EUROPE AND EASTERN UNITED-STATES - SOME RELATIONSHIPS WITH CLIMATE AND LITTER QUALITY, Biogeochemistry, 20(3), 1993, pp. 127-159
The purpose of this study was to relate regional variation in litter m
ass-loss rates (first year) in pine forests to climate across a large,
continental-scale area. The variation in mass-loss rate was analyzed
using 39 experimental sites spanning climatic regions from the subarct
ic to subtropical and Mediterranean: the latitudinal gradient ranged f
rom 31-degrees-N to 70-degrees-N and may represent the the largest geo
graphical area that has ever been sampled and observed for the purpose
of studying biogeochemical processes. Because of unified site design
and uniform laboratory procedures, data from all sites were directly c
omparable and permitted a determination of the relative influence of c
limate versus substrate quality viewed from the perspective of broad r
egional scales. Simple correlation applied to the entire data set indi
cated that annual actual evapotranspiration (AET) should be the leadin
g climatic constraint on mass-loss rates (R(adj)2 = 0.496). The combin
ation of AET, average July temp. and average annual temp. could explai
n about 70% of the sites' variability on litter mass-loss. In an analy
sis of 23 Scots pine sites north of the Alps and Carpatians AET alone
could account for about 65% of the variation and the addition of a sub
strate-quality variable was sufficiently significant to be used in a m
odel. The influence of litter quality was introduced into a model, usi
ng data from 11 sites at which litter of different quality had been in
cubated. These sites are found in Germany, the Netherlands, Sweden and
Finland. At any one site most (> 90%) of the variation in mass-loss r
ates could be explained by one of the litter-quality variables giving
concentration of nitrogen, phosphorus or water solubles. However, even
when these models included nitrogen or phosphorus even small changes
in potential evapotranspiration resulted in large changes in early-pha
se decay rates. Further regional subdivision of the data set, resulted
in a range of strength in the relationship between loss rate and clim
atic variables, from very weak in Central Europe to strong for the Sca
ndinavian and Atlantic coast sites (R(adj)2 = 0.912; AET versus litter
mass loss). Much of the variation in observed loss rates could be rel
ated to continental versus marine/Atlantic influences. Inland location
s had mass-loss rates lower than should be expected on the basis of fo
r example AET alone. Attempts to include seasonality variables were no
t successful. It is clear that either unknown errors and biases, or, u
nknown variables are causing these regional differences in response to
climatic variables. Nevertheless these results show the powerful infl
uence of climate as a control of the broad-scale geography of mass-los
s rates and substrate quality at the stand level. Some of these relati
onships between mass-loss rate and climatic variables are among the hi
ghest ever reported, probably because of the care taken to select unif
orm sites and experimental methods. This suggest that superior, base l
ine maps of predicted mass-loss rates could be produced using climatic
data. These models should be useful to predict the changing equilibri
um litter dynamics resulting from climatic change.