268
Antoni Escarrt~, Ferran Roda, Jaume Terradas and Xavier Mayor
fluxes, as measured by the coefficient of variation, were 19%, the same as for
the amount of litterfall; for K and Mg the coefficient of variation was 3033%, i.e. the spatial variation of litterfall fluxes for these cations was much
higher than for the amount of litterfall.
Nand P fluxes in litterfall did not vary significantly either among the
range of altitudes considered (800-1000 m a.s.l.) or between the two contrasting slope aspects within the catchment (north-facing and east-facing). K
and Mg fluxes varied significantly with altitude, the highest mean fluxes being obtained at 1000 m a.s.l., where the plots having the highest basal area
were located.
Litterfall nutrient fluxes were positively correlated to aboveground net
primary production (ANPP) across the 18 plots (Mayor and Roda 1992), but
this correlation was probably forced by the participation of litterfall amount
in estimating both ANPP and litterfall nutrient fluxes. Moreover, spatial
variations in ANPP over the Montseny catchment were uncorrelated with
nutrient concentrations in mature leaves and in leaf litterfall, with absolute
and relative nutrient· retranslocation from senescing leaves, and with the
concentration and content (kg ha- 1 ) of nutrients in the upper mineral soil.
Thus, no correlational evidence was found that primary production was nutrient-limited in this forest. This is not to say that nutrients are of little importance in holm oak forests, as the strong response of canopy dynamics to
N fertilization dearly demonstrates (Chap. 13).
References
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124:561-582
Bellot J, Sanchez JR, Lled6 MJ, Martinez P, Escarrc! A (1992) Litterfall as a measure of primary
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