Subalpine tree growth on serpentine soil: a dendroecological analysis

In this study dendrochronological methods are used to investigate tree growth of several coniferous species growing on serpentine outcrops in the subalpine region. Though stands are thriving on the same parent material, almost barren sites covered with Scots pine trees (Pinus sylvestris/ L.) contrast sharply with adjacent dense stands composed of mixed coniferous species. To find a reasonable explanation for this vegetation pattern and to evaluate the influence of serpentine soil on radial tree growth annual variability in ring-widths was analyzed and compared between both types of stands. Tree-ring analyses show that sparse tree cover on steep slopes might be caused by environmental stress factors especially unfavourable physical soil properties such as instability and dryness. Several abrupt growth reductions followed by slow release in ring-widths indicate repeated mechanical injury to the root system due to soil erosion. On the other hand the aggravating impact of anthropogenic disturbances (tree felling) on this ecologically fragile serpentine area could be determined and dated. There was no evidence that radial tree growth of coniferous species at this site could be limited by toxic heavy metals in the soil.