Abstract

Research Highlights: This research highlights the importance of environmental gradients in shaping tree growth responses to global change drivers and the difficulty of attributing impacts to a single directional driver. Background and Objectives: Temperature increases associated with climate change might strongly influence tree growth and forest productivity in temperate forest species. However, the direction and intensity of these effects at the dry edge of species range are still unclear, particularly given the interaction between local factors and other global change drivers such as land use change, atmospheric CO2 increase and nitrogen deposition. While recent studies suggest that tree growth in cool temperate forests has accelerated during the last decades of the 20th century, other studies suggest a prevalence of declining growth, especially in dry-edge populations. Materials and Methods: Using historical forest inventories, we analyzed last century tree growth trends (1930–2010) along an elevation gradient (1350–1900 meters above sea level (m a.s.l.)) in a dry edge scots pine (Pinus sylvestris L.) forest in Central Iberian Peninsula. Growth was estimated as decadal volume increments in harvested trees of different size classes from 1930 to 2010 (1930–1940, 1939–1949, 1949–1959, 1959–1968, 1989–1999, 2000–2010). Results: Our results showed opposite growth trends over time depending on elevation. While tree growth has accelerated in the low end of the altitudinal gradient, tree growth slowed down at higher elevations (1624–1895 m a.s.l.). Moreover, the magnitude of growth reduction along the altitudinal gradient increased with tree age. Conclusions: Throughout the last 80 years, growth trends in a rear-edge Pinus. sylvestris forest has shown divergent patterns along an altitudinal gradient. Specifically, environmental conditions have become more adverse for growth at high altitudes and have improved at low altitudes. This suggests that local factors such as topography can modulate the impact of climate change on forest ecosystems.

Highlights

  • Global change drivers such as the increase in atmospheric CO2 concentrations (Ca ), increases mean temperature or nitrogen (N) deposition might affect forest productivity in temperate forests [1,2,3].A higher Ca and soil N may enhance net photosynthesis but have variable effects on stomatal conductance

  • Environmental conditions or other factors, may have become more adverse for growth at high altitudes and have improved at low altitudes. This suggests that local factors such as topography can modulate the impact of climate change on forest ecosystems

  • At low altitudes (1350–1623 m a.s.l.), tree growth increased over time, while at high altitudes

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Summary

Introduction

Global change drivers such as the increase in atmospheric CO2 concentrations (Ca ), increases mean temperature or nitrogen (N) deposition might affect forest productivity in temperate forests [1,2,3].A higher Ca and soil N may enhance net photosynthesis but have variable effects on stomatal conductance. If photosynthesis increases more rapidly than stomatal conductance, it can increase plant water use efficiency [4,5]. Models and inventory data indicate that tree growth has increased in boreal and temperate forest ecosystems during the last decades providing indirect support to the Ca and N “fertilizing” effects [7,8]. In conjunction with a rise in Ca , aridity has increased during the last decades in many regions [9,10] It is unclear whether “fertilization” effects can compensate or exceed the costs of increased aridity in drought-prone ecosystems This balance can be critically modulated by other local factors such as competition, evapotranspiration rate, or forest management (see for example [13,14])

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