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Adaptation to common optimum in different populations of Norway spruce (<Emphasis Type="Italic">Picea abies</Emphasis> Karst.)
Authors:Du?an Gömöry  Roman Longauer  Tomá? Hlásny  Marián Pacalaj  Slavomír Strmeň  Diana Krajmerová
Institution:(1) Faculty of Forestry, Technical University in Zvolen, TG Masaryka 24, 96053 Zvolen, Slovakia;(2) National Forestry Centre, TG Masaryka 22, 96092 Zvolen, Slovakia
Abstract:Responses of Norway spruce populations to climatic transfer, in terms of growth and survival, were analyzed on the basis of a provenance experiment derived from the international provenance test IUFRO 1964/1968. The experiment comprises a series of five trial plots situated at contrasting elevations ranging from 484 to 1,275 m a.s.l., with 11 provenances represented at all trial plots that were used for the analysis. Transfer rates were defined as differences in altitudes or climatic variables between the site of plantation and the site of origin. Optimal transfer rates and optimal climates for individual provenances were derived from quadratic response functions. Spruce provenances generally responded positively by height and volume growth to transfer into lower altitudes, i.e., warmer conditions with less precipitations. The analysis at the level of provenances showed that optimal transfer rates were consistently negatively correlated with the underlying environmental variables and optimal climates were consequently nearly the same for all provenances irrespective of the response traits and ecodistance variables. Stability indices based on joint regression analysis indicate that provenances from higher altitudes, colder and wetter climates tend to be more stable, whereas provenances from lower altitudes, drier and warmer sites are more responsive to site quality. However, the differences in the stability are small and stability indices were generally close to 1. The results indicate that populations in different climates remain adapted to a common optimum and the extent of local adaptation is quite limited. Possible explanations of this observation are briefly discussed.
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