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Rapid climate change-related growth decline at the southern range edge of Fagus sylvatica

机译:与气候有关的快速增长在西格斯青冈的南部边缘下降

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Studies on Fagus sylvatica show that growth in populations toward the southern limit of this species' distribution is limited strongly by drought. Warming temperatures in the Mediterranean region are expected to exacerbate drought where they are not accompanied by increases in precipitation. We studied levels of annual growth in mature F. sylvatica trees over the last half-century in the Montseny Mountains in Catalonia (northeast Spain). Our results show significantly lower growth of mature trees at the lower limit of this species' distribution when compared with trees at higher altitudes. Growth at the lower Fagus limit is characterized by a rapid recent decline starting in approximately 1975. By 2003, growth of mature trees had fallen by 49% when compared with predecline levels. This is not an age-related phenomenon, nor is it seen in comparable populations at higher altitudes. Analysis of climate-growth relationships suggests that the observed decline in growth is a result of warming temperatures and that, as precipitation in the region has not increased, precipitation is now insufficient to ameliorate the negative effects of increased temperatures on tree growth. As the climate-response of the studied forest is comparable with that of F. sylvatica forests in other southern European regions, it is possible that this growth decline is a more widespread phenomenon. Warming temperatures may lead to a rapid decline in the growth of range-edge populations and a consequent retreat of the species distribution in southern Europe. Assessment of long-term growth trends across the southern range edge of F. sylvatica therefore merits further attention.
机译:对青冈(Fagus sylvatica)的研究表明,干旱导致该种群向南向该物种分布的南部增长。预计地中海地区变暖不会加剧降水,而干旱会加剧干旱。我们研究了加泰罗尼亚(西班牙东北部)的蒙塞尼山近半个世纪以来成熟的西番莲树木的年生长水平。我们的结果表明,与海拔较高的树木相比,处于该物种分布下限的成熟树木的生长明显较低。 Fagus下限的生长特征是大约从1975年开始迅速下降。到2003年,成熟树木的生长与下降前的水平相比下降了49%。这不是与年龄有关的现象,也没有在较高海拔的类似人群中看到。对气候增长关系的分析表明,观察到的生长下降是温度升高的结果,而且由于该地区的降水量并未增加,因此降水不足以减轻温度升高对树木生长的负面影响。由于所研究森林的气候响应与其他南欧地区的西番莲森林具有相似的气候响应,因此这种增长下降可能是更为普遍的现象。气温升高可能导致范围边缘种群的增长迅速下降,从而导致南欧物种分布减少。因此,需要对整个西欧F. sylvatica南部边缘的长期增长趋势进行评估。

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