Abstract:This study focuses on analyzing the growth rate and growth–climate relationship in Scots pine (Pinus sylvestris L.) growing on coastal dunes of different ages on the Southern Baltic coast. Podzols have developed on these dunes. Depending on dune age, however, podzols are characterized by a different degree of development and richness, which represents the main factor differentiating the studied habitats: the oldest brown dunes (BD), younger yellow dunes (YD), and the youngest white dunes (WD). Samples were tak… Show more
“…Also, the pointer years designated for this species mostly overlap and are determined by the same weather conditions [7,44,49]. The studied trees are also sensitive to thermal conditions in the autumn of the previous growing season, which is also confirmed by other studies [47,49,50].…”
Section: Discussionsupporting
confidence: 72%
“…For the main native coniferous species that forms most of the tree stands in Poland, P. sylvestris (PS), similar growth-climate relationships are observed as those obtained by other researchers from the south coast of the Baltic Sea. The results confirm the sensitivity of this species to low temperatures in winter/early spring and to rainfall deficits in the summer season [7,8,[44][45][46][47][48][49]. The mechanism of the relationship in February and March has not been fully explained, but the following climate changes (mainly warmer winters and earlier spring) should have a positive impact on the tree ring width for pine [47].…”
Section: Discussionsupporting
confidence: 70%
“…The mechanism of the relationship in February and March has not been fully explained, but the following climate changes (mainly warmer winters and earlier spring) should have a positive impact on the tree ring width for pine [47]. Also, the pointer years designated for this species mostly overlap and are determined by the same weather conditions [7,44,49]. The studied trees are also sensitive to thermal conditions in the autumn of the previous growing season, which is also confirmed by other studies [47,49,50].…”
The ongoing climatic changes are causing the extinction of numerous species or their withdrawal from previously occupied areas. The environmental and economic significance of introduced species may increase. The aim of the present study was to examine the rate of growth of coniferous species growing in northwestern Poland and to analyze the tree ring width–climate relationships. Six tree species were selected for this study. Two of these species have natural occurrences in Poland: Pinus sylvestris and Larix decidua. The remaining four species were introduced from North America: Chamaecyparis lawsoniana, Thuja plicata, Pseudotsuga menziesii, and Pinus strobus. Samples were collected from 131 trees using a Pressler borer at 1.3 m above ground. Tree ring widths were measured down to 0.01 mm. Climatic data were retrieved from a weather station located 23 km from the study plot. The average tree ring width reaches the lowest value for the P. sylvestris chronology (1.62 mm/year) and for P. strobus (1.69 mm/year), and the highest value is reached for T. plicata (2.80 mm/year) and P. menziesii (2.56 mm/year). The analysis of weather conditions in the designated pointer years and the response function analysis indicate that winter and early spring air temperature is the factor responsible for the formation of wide tree rings in the following species studied: P. sylvestris, C. lawsoniana, P. menziesii, and T. plicata. For L. decidua and P. strobus, the climate–growth relationships are different: weather conditions in the previous growth year are important, and it is the weather in the late spring and summer months. Two of the investigated introduced species (T. plicata and P. menziesii) are characterized by very good acclimatization and are best adapted to the new habitat during the current climate changes. These tree species can constitute a basis for replacing native species, which, due to increasingly severe droughts and higher temperatures, are doing less and less well in their current habitats. Foresters wanting to conduct sustainable forest management will look for replacement species that are well adapted to new habitat conditions in order to maintain the continuity of forest cover.
“…Also, the pointer years designated for this species mostly overlap and are determined by the same weather conditions [7,44,49]. The studied trees are also sensitive to thermal conditions in the autumn of the previous growing season, which is also confirmed by other studies [47,49,50].…”
Section: Discussionsupporting
confidence: 72%
“…For the main native coniferous species that forms most of the tree stands in Poland, P. sylvestris (PS), similar growth-climate relationships are observed as those obtained by other researchers from the south coast of the Baltic Sea. The results confirm the sensitivity of this species to low temperatures in winter/early spring and to rainfall deficits in the summer season [7,8,[44][45][46][47][48][49]. The mechanism of the relationship in February and March has not been fully explained, but the following climate changes (mainly warmer winters and earlier spring) should have a positive impact on the tree ring width for pine [47].…”
Section: Discussionsupporting
confidence: 70%
“…The mechanism of the relationship in February and March has not been fully explained, but the following climate changes (mainly warmer winters and earlier spring) should have a positive impact on the tree ring width for pine [47]. Also, the pointer years designated for this species mostly overlap and are determined by the same weather conditions [7,44,49]. The studied trees are also sensitive to thermal conditions in the autumn of the previous growing season, which is also confirmed by other studies [47,49,50].…”
The ongoing climatic changes are causing the extinction of numerous species or their withdrawal from previously occupied areas. The environmental and economic significance of introduced species may increase. The aim of the present study was to examine the rate of growth of coniferous species growing in northwestern Poland and to analyze the tree ring width–climate relationships. Six tree species were selected for this study. Two of these species have natural occurrences in Poland: Pinus sylvestris and Larix decidua. The remaining four species were introduced from North America: Chamaecyparis lawsoniana, Thuja plicata, Pseudotsuga menziesii, and Pinus strobus. Samples were collected from 131 trees using a Pressler borer at 1.3 m above ground. Tree ring widths were measured down to 0.01 mm. Climatic data were retrieved from a weather station located 23 km from the study plot. The average tree ring width reaches the lowest value for the P. sylvestris chronology (1.62 mm/year) and for P. strobus (1.69 mm/year), and the highest value is reached for T. plicata (2.80 mm/year) and P. menziesii (2.56 mm/year). The analysis of weather conditions in the designated pointer years and the response function analysis indicate that winter and early spring air temperature is the factor responsible for the formation of wide tree rings in the following species studied: P. sylvestris, C. lawsoniana, P. menziesii, and T. plicata. For L. decidua and P. strobus, the climate–growth relationships are different: weather conditions in the previous growth year are important, and it is the weather in the late spring and summer months. Two of the investigated introduced species (T. plicata and P. menziesii) are characterized by very good acclimatization and are best adapted to the new habitat during the current climate changes. These tree species can constitute a basis for replacing native species, which, due to increasingly severe droughts and higher temperatures, are doing less and less well in their current habitats. Foresters wanting to conduct sustainable forest management will look for replacement species that are well adapted to new habitat conditions in order to maintain the continuity of forest cover.
“…A.4). Site-specific climate-growth relationships reported for pine species in Europe were related either to marginal populations under mountain climate conditions (Herrero et al, 2013) or to lowland populations in the species' core range (Cedro et al, 2022). Therefore, our results may reflect a more general pattern for the effects of local conditions on the radial growth of pine species.…”
Section: Site-specific Response To Climatementioning
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