Structural and dendrochronological characterization of mountain pine persistent woodlands on the Monti del Sole – Dolomiti Bellunesi National Park

C. Palombo, C. Lasen, M. Scirè, V. Garfì, F. Lombardi, R. Tognetti, M. Marchetti
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引用次数: 2

Abstract

High-mountain ecosystems, located at the geographical distribution limit of the species, may provide valuable information about tree-growth responses to changes in climate conditions and land uses. In order to provide a first description of a mountain pine ecotone, at the alpine treeline, three plots were sampled along an altitudinal gradient in the Monti del Sole (Dolomiti Bellunesi National Park, Veneto, Italy) on a northwestern slope from 1850 to 2000 m a.s.l. In order to reconstruct recent dynamics of Pinus mugo Turra ssp. mugo (mountain pine) at this altitudinal range dendroecological methods were used,which allowed reconstructing the age structures of tree populations. Raw mean chronologies showed the long-term variability, related to non-climatic signals due to age, size and stand dynamics. The raw mean chronology of Plot 1 followed the typical exponential negative trend, while raw mean chronologies of Plot 2 and Plot 3 depicted an increasing growth trend, starting from early fifties of 20th century. There was a greater ring width in Plot 2,than the other two plots. These mountain pine scrublands belong the Sorbo chamaemespili - Pinetum mugi association and form persistent woodlands.
Monti del Sole - Dolomiti Bellunesi国家公园山地松林的结构和年代学特征
高山生态系统位于树种的地理分布极限,可以提供树木生长对气候条件和土地利用变化的响应的宝贵信息。为了对高山松林带进行首次描述,在意大利威尼托的Dolomiti Bellunesi国家公园,沿着海拔梯度在西北坡上的三个样地进行了1850 - 2000 m的采样,以重建mugo Turra spp的近期动态。采用树木生态学方法重建了该海拔范围内的山松种群年龄结构。原始平均年代学表现出长期变异,与年龄、大小和林分动态等非气候信号有关。图1的原始平均年表呈现典型的指数负趋势,而图2和图3的原始平均年表从20世纪50年代初开始呈现增长趋势。样地2的环宽大于其他2个样地。这些山地松灌丛属于Sorbo chamaemespili - Pinetum mugi组合,形成持久林地。
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