Centennial Scots pine chronologies for western,central and eastern Lithuania

Although two centennial Scots pine chronologies for the dating of timber in Lithuania were constructed in the 2000 s, the Baltic countries still lack a network of regional chronologies. To fill this gap, we constructed three Scots pine chronologies for western, central and eastern Lithuania. Here we present chronologies covering the fifteen to the twentieth centuries. Our analysis revealed a strong teleconnection of the compiled chronologies with Scots pine chronologies constructed in Poland, Latvia, Estonia, and Belarus. The established link with Belarus chronologies and the fact that some of the timber in Lithuanian buildings could be of Belarus origin is important in the long-distance timber trade during the last 500 years. Dendroclimatological analysis has shown that constructed tree-ring chronologies are sensitive to air temperatures in February and March. Therefore, the constructed chronologies have a potential for climate reconstructions and dendroprovenancing.     

Tree-ring isotopes from Araucaria araucana as useful proxies for climate reconstructions

Tree-ring width (TRW) chronologies have been widely and long-time used to reconstruct past climate variations in the Andes in South America. The use of tree-ring isotopic chronologies is still not widespread in this region although they have proved to be very efficient climate proxies. Araucaria araucana (Molina) K. Koch is a conifer tree species with some multi-century-old individuals that offers an excellent opportunity to measure stable carbon (δ¹³C) and oxygen (δ¹⁸O) isotopes in cellulose from long tree-ring records. Here, we explore whether current or stored carbohydrates are used for A. araucana radial growth and we assess the potential of a tree-ring isotopic record of to study past climate variability. Eleven A. araucana cores from a dry and high-elevation forest at the northern border of Patagonia, Argentina (38°55’S, 70°44’W) were selected for stable isotopes analyses. The strong correlation between the isotopic composition of the first and second parts of the same ring, but also the strong relationships between δ¹³C and δ¹⁸O records with climate parameters of the current growing season such as temperature, show that tree-rings are built mostly with carbohydrates produced during the current growing season with little or no supply from storage or reserves. This finding leads to reconsidering the interpretation of the legacy effect (i.e. ecological memory effects) based on the previously described strong negative correlation between A. araucana TRW chronologies and previous growing season temperature and suggests a dependence of radial tree growth on the level of development of organs. Regarding climate sensitivity, the A. araucana tree-ring δ¹³C chronology is strongly related to current summer temperature (r = 0.82, p < 0.001), vapour pressure deficit (VPD; r = 0.79, p < 0.001), precipitation (r = −0.53, p < 0.001) and SPEI2 (r = −0.73, p < 0.001). These strong relationships support the use of δ¹³C of A. araucana tree-ring cellulose to reconstruct past temperature variations at regional scale in relation with large-atmospheric drivers of climate variability such as the Southern Annular Mode. The A. araucana tree-ring δ¹⁸O chronology is also correlated with temperature (r = 0.42, p < 0.01) and VPD (r = 0.45, p < 0.01) of the winter preceding the growing season. This suggests that trees are using water from precipitation infiltrated in the soil during the previous recharge period (autumn-winter). The weak correlations of δ¹⁸O with current summer atmospheric conditions and the decoupling between δ¹⁸O and δ¹³C, may be due to a high rate of oxygen exchange between sugars and xylem water (P_ex) during cellulose synthesis, which dampens evaporative isotopic fractionation.     

Radial growth response of Pinus sylvestris L. and Fagus sylvatica L. to technological solutions applied in rope climbing parks

Vitality is a genetic preservation factor that keeps a tree in the right condition. Changes in tree vitality are a measure of the impact exerted on trees by environmental factors, such as injuries to trunks and branches, and are among the basic parameters of the state of their preservation. The dynamics of changes in the width of annual increments of trees is one of several parameters characterizing the level of their vitality. The aim of the study is to determine changes in radial increment and linking them to the level of the vitality of Scots pines (Pinus sylvestris L.) and European beeches (Fagus sylvatica L.), on which the standard (old system) and specially designed (new system) systems of fastening of wooden platforms were installed as part of adventure park infrastructure. In the old system, the platforms were installed on square wooden beams placed in milled tree trunks, while in the new system on semi-circular metal brackets matching the curvature of the trunks. The present research is aimed to determine the dynamics of incremental trends in trees with different platform systems in relation to the reference group, and to determine the impact of the tested support systems on trees with different levels of vitality. Most of the studied trees were in the optimum stage of increment. The initial tree vitality level recorded at the beginning of the experiment was clearly better for the beech stands. In the case of Scots pine, the average vitality was close to stable. Pines that were initially in better condition responded much worse to the installation of old system platforms compared to those with the specially new platform system. A similar trend was also visible in the case of beeches, but the differences were not that clear and the annual increments of the trees with platforms installed were slightly higher compared to the reference trees. The trees that were initially in worse condition, both pines and beeches on which the old system of platforms had been installed, responded by increasing the width of annual increments during the measurement period. The described response of trees most probably does not result from the lower harmfulness of the old support system, but from the defensive responses of trees subjected to stronger stress.     

Streamflow reconstruction of Eastern Himalaya River,Lachen ‘Chhu’, North Sikkim,based on tree-ring data of Larix griffithiana from Zemu Glacier basin

The relationship of streamflow records of the Lachen River with tree-ring parameters of total tree-ring width (TRW), earlywood width (EWW) and latewood width (LWW) chronologies of Larix griffithiana from Lachen, North Sikkim, Eastern Himalaya was generated. These chronologies correlate significantly with the observed discharge of the Lachen River where the EWW chronology explains 61.2% of the streamflow variance. Based on this result, Lachen River discharge for the period of previous year March to current year February was reconstructed using EWW chronology, which extends back to AD 1790. In the smoothed reconstructed data the period of extreme low streamflows were during AD 1791–1805, 1813–1822 and 1914–1925 and the extreme highs were during AD 1823–1835, 1879–1890, 1926–1946 and 1980–1989. The streamflow is also found to be lower than average during the monsoon failure (or East India Drought) of AD 1792–1796 and past great droughts of AD 1876–1878. The lower tree growth during AD 1816–1822 is consistent with that of the Tambora volcanic eruption of Indonesia in AD 1815. High spectral power at 4–8 years in the reconstructed streamflow is similar to that of ENSO range.     

Comparison of earlywood vessel variables in the wood of Quercus robur L. and Quercus petraea (Mattuschka) Liebl. growing at the same site

The differences in the microscopic structure of wood based on the variables of earlywood vessel area and tree ring width were analysed in 6 trees of Pedunculate oak (Quercus robur L.) and 6 trees of Sessile oak (Quercus petraea (Mattuschka) Liebl.) in the same forest stand at a site in the Vizovice Highland (Czech Republic). The aim of this paper was to assess any differences between the two oak species when grown in the same location. Also the effect of tree-ring width and the effect of age on earlywood vessel variables were analysed. Mean values of tree-ring widths were not different between species. Earlywood vessel area chronologies were synchronized well between species. The mean values of earlywood vessel area (average vessel area, average vessel area of the first row of vessels, area of the largest vessel) showed a significant difference. Finally, we can conclude that there were differences in vessel features between these oak species.     

Growth patterns of <Emphasis Type="Italic">Nothofagus pumilio</Emphasis> trees along altitudinal gradients in Tierra del Fuego,Argentina

The influence of ecological factors resulting from altitude on growth characteristics of Nothofagus pumilio was analyzed. N. pumilio forests grow in the southern Andes from near sea level to 600 m.a.s.l. Eight study sites were selected in the southwestern area of Tierra del Fuego, on north- and south-facing slopes, and distributed along an altitudinal gradient (200–600 m.a.s.l.). Growth cycles throughout time were identified. The correlation between climate and tree growth was determined. Tree diameter and height decreased whereas stand density increased towards tree-line. South-facing slopes showed higher values in common growth variability, probably because of stronger climatic controlling factors. Climate-growth correlation models revealed long-term temperature influences on growth variability, and showed variations among the different plots. Differences were detected in the spectral power component of the chronologies throughout the altitudinal profile. The series had a significant spectral peak at frequencies around 7 years, possibly related to mast seeding cycles. This signal became weaker as the altitude increased probably due to lower seed production. These results suggest a strong altitudinal component in growth variability of N. pumilio in Tierra del Fuego.     

Intra-annual tree-ring parameters indicating differences in drought stress of Pinus sylvestris forests within the Erico-Pinion in the Valais (Switzerland)

The effects of drought on radial growth of Pinussylvestris were investigated by comparing sites along hydricgradients. The gradients were located in Valais, an inner Alpine dry valley inSwitzerland, with each consisting of two site types, an extreme dry, xeric siteand a less dry, moderate site. The two site types were assigned tophytosociological associations within the Erico-Pinion. The investigationcovered the responses of tree growth to climate and particularly concentratedonintra-annual features of tree-rings such as earlywood/latewood ratio,intra-annual density fluctuations (IADFs) and traumatic tissues (TTs) as wellasthe sapwood/heartwood ratio. Radial growth differed according to the sitetypes,with trees on dry sites generally showing more missing rings, lower mean ringwidths, lower autocorrelation, higher mean sensitivities, reduced latewoodproportions and lower sapwood areas than trees on moderate sites. Therelationships between climate and tree-ring width, studied using responsefunction analysis, varied strongly between the site types within theErico-Pinion: Tree growth on dry sites was positively influenced byprecipitation at the end of the winter and the beginning of the growing seasonand negatively influenced by temperature in June. Winter precipitation waspositively correlated with radial growth, demonstrating its importance for thesuccessful root and shoot growth of the plants in spring on dry sites. Onmoderate sites, tree growth was less controlled by climate than by priorgrowth.The intra-annual density fluctuations (IADFs) provided a valuable means todifferentiate between the site types. In comparison to the moderate sites, thetrees on dry sites contained more IADFs, and their frequency was increased.Moist-cool conditions in the middle of the growing season were the triggeringfactor for IADFs on dry sites, whereas on moderate sites, there must be anadditional warm period in early summer in order to initiate IADFs. Most IADFswere found in latewood. We found no relationship between climate and traumatictissues (TTs). It is unclear whether other abiotic or biotic factors such aswounding by insects or birds are responsible for the development of TTs. Theassignment of these differences in tree growth behaviour to phytosociologicalassociations will enable a deeper understanding of the site types and willfacilitate the comparison with similar studies. Furthermore, the results can becombined with studies from other scientific disciplines concerning thesephytosociological associations. The ecological indicator values of thevegetation was a precise method for the distinction of site types.     

Partly decoupled tree-ring width and leaf phenology response to 20th century temperature change in Sweden

The recent warming trend, and associated shifts in growing season length, challenge the principle of uniformitarianism, i.e., that current relations are persistent over time, and complicates the uncritical inferences of past climate from tree-ring data. Here we conduct a comparison between tree-ring width chronologies of Pinus sylvestris L. (Scots pine), Picea abies (L.) Karst. (Norway spruce) and Betula pubescens Ehrh. (Downy birch) and phenological observations (budburst and leaf senescence) of Fagus sylvatica L. (European beech), Quercus robur L. (European oak), Betula sp. (Birch), Norway spruce and Scots pine) in Sweden to assess to what extent the tree-ring width–temperature relationship and the timing of phenological phases are affected by increased temperature. Daily meteorological observations confirm a prolongation of the thermal growing season, most consistently observed as an earlier onset of around 1–2 weeks since the beginning of the 20th century. Observations of budburst closely mimic this pattern, with budburst of the deciduous trees occurring 1–2.5 weeks earlier. In contrast to the changes seen in phenology and observational temperature data, the tree-ring width–temperature relationships remain surprisingly stable throughout the 20th century. Norway spruce, Scots pine and Downy birch all show consistently significant correlations with at least one 30 day-long window of temperature starting in late June–early July season. Norway spruce displays the largest degree of stability, with a consistent 60 day-long temperature window with significant correlation starting around Julian calendar day 150. Thus, our results suggest that the principle of uniformitarianism is not violated during the period covered by modern meteorological observations. Further research is needed to determine at what thresholds the temperature sensitivity of these species may alter or deteriorate as a consequence of the ongoing climate change.     

西昆仑山两种针叶树种径向生长及其对气候变化的响应

利用西昆仑山的雪岭云杉和昆仑圆柏树芯样本,建立其树轮宽度年表。通过分析两种针叶树种树木径向生长特征与气候要素的相关关系,探讨了树种间的树木生长气候响应异同及响应关系的稳定性。结果表明：研究区域内的雪岭云杉和昆仑圆柏年表间存在显著正相关。两种针叶树种在1994年气温突变前树轮宽度年表指数和基部断面生长增量（BAI）呈上升趋势,在气温突变后年表和BAI则呈下降趋势,并且昆仑圆柏的树木径向生长速率高于雪岭云杉。与气候要素的相关性分析结果表明,雪岭云杉径向生长与上年生长季（5—6月和8—10月）和当年生长季（3—6月和10月）气温呈显著负相关,而昆仑圆柏径向生长与上年10月和当年生长季前期（4—6月）气温呈显著负相关;两者均与当年春季降水呈显著正相关。滑动相关分析结果显示,上年和当年生长季气温对两个树种树木径向生长的负响应在增强,特别是在当年生长季前期更为显著。此外,当年生长季前期降水对树木径向生长的促进作用也在增强。在有可能的气候突变年份（1994年）之后,两种针叶树种对气温和降水的响应敏感性均有所增强,并且雪岭云杉对气温的响应敏感性强于昆仑圆柏,而对降水响应敏感性要弱于昆仑圆柏。     

Comparison of growth-climate relationship of sabina przewalskii at different timberlines along a precipitation gradient in the northeast Qinghai-Xizang Plateau,China北大核心CSCD

Aims To test the hypothesis that water is the main limiting factor of tree growth at the arid alpine timberline, and to explore the effects of water on growth-climate relationships of Sabina przewalskii along a precipitation gradient in the northeast Qinghai-Xizang Plateau. Methods Three sides were selected to sample the alpine timberline along a precipitation gradient in the northeast Qinghai-Xizang Plateau: Halihatu National Forest Park in Wulan County (HL, annual precipitation 217 mm), Qushigang in Dulan County (QS, 281 mm) and Hebei Forest Farm in Tongde County (HB, 470 mm). The correlation and response analysis at seasonal and extreme climate year scales were used to examine the spatial variations of the growth-climate relationship of S. przewalskii at different timberlines. Important findings Our results do not support the hypothesis that water is the main limiting factor of tree growth at the arid alpine timberline. The effect of precipitation on the radial growth of S. przewalskii were consistent across all three sampling sites, while the effects of temperature were different across sites. At HL site (low precipitation), the winter and summer minimum temperature were the main limiting factor of S. przewalskii radial growth, and this relationship did not significantly change in different extreme climate years. At QS site (middle precipitation), the radial growth of S. przewalskii was mainly limited by the minimum temperature in spring and summer, but its effect was weaker than that at low precipitation site. At HB site (high precipitation), the spring temperature had a significant negative effect on tree growth, and the positive effect of spring precipitation on tree growth was significantly enhanced in comparison with those at low and middle precipitation sites, especially in extreme high temperature and drought years. Summer precipitation did not significantly affect tree growth at high precipitation site. Our results did not support the hypothesis that the radial growth of trees at alpine timberline in arid/humid area is mainly limited by water/temperature. However, precipitation at timberline will affect the relationship between tree growth and temperature at different seasons. With the warming and humidification of the northeastern Qinghai-Xizang Plateau, the climatic limiting factors of tree growth in different timberline areas may be complicated. © 2018 Editorial Office of Chinese Journal of Plant Ecology. All rights reserved.