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espanolSe realiza una reconstruccion dendroclimatica a partir de los datos de nueve cronologias del taxon Fagus sylvatica repartidas en Polaciones, un valle de la montana central cantabrica. El trabajo se basa en una relacion estadistica fiable y replicable entre los datos climaticos de referencia de la Climatic Research Unity las cronologias de anillos de crecimiento. Los resultados obtenidos en la relacion crecimiento-clima para la precipitacion resultan estadisticamente significativos para los meses entre abril a agosto, lo que permite reconstruir las variaciones interanuales de esta entre 1798 y 2011, cubriendo asi un periodo en el que no se dispone de registros instrumentales. Por otro lado, se elabora una serie de referencia para el area de analisis y se calculan los anos favorables y desfavorables en el crecimiento de la especie. La busqueda de coincidencias que ayuden a comprender el comportamiento de Fagus sylvatica en respuesta al clima en su ambito meridional de distribucion en Europa, lleva a estimar los anos secos y humedos obtenidos de la reconstruccion, que son puestos en relacion con los crecimientos. EnglishA dendroclimatic reconstruction is carried out using the data from nine chronologies of the Fagus sylvatica taxon spread out in Polaciones, a valley of the central Cantabrian Mountains. The paper is based on a reliable and replicable statistical relationship between the climatic reference data of the Climatic Research Unit and the growth ring chronologies. The results obtained in the growth-climate relationship for the precipitation are statistically significant for the months of April to August, which helps reconstruct the interannual variations of this between 1798 and 2011, thus covering a period in which instrumental records are not available. Moreover, a reference series for the analysis area is drawn up and the favourable and unfavourable years in the growth of the species are calculated. The search for coincidences that help understand the behaviour of Fagus sylvatica in response to the climate in its southern area of distribution in Europe calls for the estimation of the dry and wet years obtained from the reconstruction, which are related to the growth.

Reconstrucción dendroclimática de la serie de precipitaciones en el Valle de Polaciones (Cantabria)