ABSTRACT
The carbon isotopic composition (delta(13)C) of wood and leaf cellulose of beech trees (Fagus sylvatica L.) was studied at 80 sites in northeastern France. We sampled sites with contrasting water balance, depending on soil type and precipitation. We tested the hypothesis that inter-site variations in plant delta(13)C reflect the spatial distribution of soil water availability, and we assessed whether delta(13)C could be used as a bioindicator of soil water availability. Patterns of variation in delta(13)C were compared with estimates of monthly water balance and with other soil characteristics. Between-site variability in delta(13)C was high (2.9 per thousand range in wood cellulose, 2.1 per thousand in leaf cellulose), but variation in water availability appeared to be only a minor factor contributing to this variation in delta(13)C. Unexpectedly, spatial variations in wood and leaf cellulose delta(13)C were significantly and positively related to soil fertility expressed by soil pH (r = 0.42 and 0.43, respectively) and cation content. On average, trees growing on acidic soils displayed 0.5 per thousand lower delta(13)C in both wood and leaf material than trees growing on neutral or calcareous soils. Our initial hypothesis of a strong negative relationship between delta(13)C and site water availability was not confirmed. In the study zone, neither wood nor leaf delta(13)C appeared to be a reliable bioindicator of spatial variations in water availability. Possible causes for the lack of a relationship are discussed. Our findings confirm, under natural conditions, the strong effect of soil fertility on water-use efficiency previously observed in experiments. This effect needs to be considered in isotopic studies involving different sites.
Subject(s)
Fagus/metabolism , Soil , Water/metabolism , Carbon/metabolism , Carbon Isotopes/metabolism , Ecosystem , Fagus/growth & development , France , GeographyABSTRACT
Surveys of ground layer vegetation are a reliable tool for monitoring spatial and temporal variations of the forest environment. In 1991, 47 vegetation plots first sampled in 1972 in a forest of the Lorraine Plain, North-East France, were resampled. This beech-oak forest had both acidic and calcareous soils depending on the thickness of alluvial deposits above the calcareous bedrock. The mean number of species per sample increased from 32 to 39 during this period and the frequency of nitrophilic species increased throughout the forest. On acidic soils, acidophilic species increased in frequency, while on calcareous soils there were no systematic changes. Multivariate statistical analysis clearly distinguished two gradients in this set of vegetation samples: acidity and nitrogen availability of soils. Along the first gradient, a shift of the plots towards a more acidic state occurred during the past 19 years on acidic soils only. Along the second one. a strong eutrophication happened on both acidic and calcareous soils, indicating an enrichment in nitrogen of forest ecosystems. Possible causes of these changes are discussed, namely sylviculture changes, aging of the stands and pollution. Atmospheric nitrogen inputs seem to be the most probable cause of eutrophication.
