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Drought-driven growth reduction in old beech (Fagus sylvatica L.) forests of the central Apennines, Italy

机译:意大利亚平宁山脉中部的老山毛榉森林(Fagus sylvatica L.)受干旱驱动的生长减少

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Productivity of old-growth beech forests in the Mediterranean Basin was measured by average stem basal area increment (BAI) of dominant trees at two mountain sites in the Italian Apennines. Both forests could be ascribed to the old-growth stage, but they differed markedly with regard to elevation (1000 vs. 1725 m a.s.l.), soil parent material (volcanic vs. calcareous), mean tree age (less than 200 years vs. 300 years), and stand structure (secondary old-growth vs. primary old-growth forest). Drought at the two sites was quantified by the self-calibrated Palmer Moisture Anomaly Index (Z-index), and by the self-calibrating Palmer Drought Severity Index (PDSI) for summer (June through August) and the growing season (May through September). Dendroclimatological analyses revealed a moisture limitation of beech BAI at interannual (water availability measured by Z-index) and decadal scales (water availability measured by PDSI). Both BAI and water availability increased from 1950 to 1970, and decreased afterwards. Trees were grouped according to their BAI trends in auxological groups (growth-type chronologies), which confirmed that growth of most trees at both sites declined in recent decades, in agreement with increased drought. Because BAI is not expected to decrease without an external forcing, the patterns we uncovered suggest that long-term drought stress has reduced the productivity of beech forests in the central Apennines, in agreement with similar trends identified in other Mediterranean mountains, but opposite to growth trends reported for many forests in central Europe.
机译:通过意大利亚平宁山脉两个山地优势树的平均茎基础面积增加量(BAI)来衡量地中海盆地老龄山毛榉森林的生产力。两种森林都可归因于成年期,但是它们在海拔高度(1000 vs. 1725 m asl),土壤母质(火山岩与钙质),平均树龄(不到200年vs. 300)方面存在显着差异。年和林分结构(次生老林与原生老林)。通过自校准的Palmer湿度异常指数(Z-index)以及夏季(6月至8月)和生长季节(5月至9月)的自校准Palmer干旱严重度指数(PDSI)对两个地点的干旱进行了量化。 )。树木气候学分析显示,山毛榉BAI在年际(通过Z指数测量的可利用水量)和年代际尺度(通过PDSI进行的利用水量)时的水分限制。从1950年到1970年,BAI和可用水量均增加,此后减少。根据树木的BAI趋势将树木分类为植物群(生长型年代),这证实了最近几十年这两个地点大多数树木的生长下降,这与干旱加剧一致。由于没有外部强迫,预计BAI不会减少,因此我们发现的模式表明,长期干旱胁迫已经降低了亚平宁山脉中部的山毛榉森林生产力,这与其他地中海山区的类似趋势一致,但与增长相反欧洲中部许多森林的趋势报告。

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