Pub Date : 2025-07-16DOI: 10.1016/j.dendro.2025.126393
Jiuqi Chen , Yonghui Wang , Tongwen Zhang , Kexiang Liu , Shulong Yu , Kailong Guo , Zhihao He , Beihua Liang
Vegetation growth is influenced not only by current climatic conditions but also by growth legacy signals and preceding climate variability. To investigate the impacts of vegetation growth carryover (VGC) and lagged climate effects (LCE) on vegetation at two distinct scales, tree-ring width (TRW) and enhanced vegetation index (EVI), we focused on Juniperus seravschanica, a dominant species in Tajikistan. Using both TRW and EVI datasets, we employed a vector autoregression (VAR) model to analyze the intensity and duration of vegetation responses to climate through VGC and LCE at different spatial and temporal scales. Our results revealed that both the VGC and LCE effects were stronger in TRW than in EVI. For both indicators, the peak intensity of LCE responses occurred within a lag of 0–3 years, suggesting that this time window is optimal for studying lagged climate effects on vegetation. Except in ZTW (EVI), the contribution of VGC to vegetation growth is much stronger than that of LCE. Moreover, VGC and LCE were found to be decoupled, indicating that their influences on vegetation growth are independent of each other. Ultimately, Juniperus seravschanica appears to adapt to harsh environmental conditions by modulating its growth through both VGC and LCE mechanisms. Investigating VGC and LCE using multi-scale vegetation indicators provides deeper insights into forest ecosystem functioning and offers a more comprehensive perspective for studying vegetation dynamics over time. These findings enhance our understanding of vegetation–climate interactions and offer valuable guidance for vegetation management in arid regions under the context of global climate change.
{"title":"Vegetation growth carryover and lagged climatic effect at Juniperus seravschanica different scales: From tree rings to remote sensing data","authors":"Jiuqi Chen , Yonghui Wang , Tongwen Zhang , Kexiang Liu , Shulong Yu , Kailong Guo , Zhihao He , Beihua Liang","doi":"10.1016/j.dendro.2025.126393","DOIUrl":"10.1016/j.dendro.2025.126393","url":null,"abstract":"<div><div>Vegetation growth is influenced not only by current climatic conditions but also by growth legacy signals and preceding climate variability. To investigate the impacts of vegetation growth carryover (VGC) and lagged climate effects (LCE) on vegetation at two distinct scales, tree-ring width (TRW) and enhanced vegetation index (EVI), we focused on <em>Juniperus seravschanica</em>, a dominant species in Tajikistan. Using both TRW and EVI datasets, we employed a vector autoregression (VAR) model to analyze the intensity and duration of vegetation responses to climate through VGC and LCE at different spatial and temporal scales. Our results revealed that both the VGC and LCE effects were stronger in TRW than in EVI. For both indicators, the peak intensity of LCE responses occurred within a lag of 0–3 years, suggesting that this time window is optimal for studying lagged climate effects on vegetation. Except in ZTW (EVI), the contribution of VGC to vegetation growth is much stronger than that of LCE. Moreover, VGC and LCE were found to be decoupled, indicating that their influences on vegetation growth are independent of each other. Ultimately, <em>Juniperus seravschanica</em> appears to adapt to harsh environmental conditions by modulating its growth through both VGC and LCE mechanisms. Investigating VGC and LCE using multi-scale vegetation indicators provides deeper insights into forest ecosystem functioning and offers a more comprehensive perspective for studying vegetation dynamics over time. These findings enhance our understanding of vegetation–climate interactions and offer valuable guidance for vegetation management in arid regions under the context of global climate change.</div></div>","PeriodicalId":50595,"journal":{"name":"Dendrochronologia","volume":"93 ","pages":"Article 126393"},"PeriodicalIF":2.7,"publicationDate":"2025-07-16","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"144694960","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":3,"RegionCategory":"农林科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Pub Date : 2025-07-16DOI: 10.1016/j.dendro.2025.126392
Nela Altmanová , Martina Hrádková , Eva Návratová , Vít Pejcha , Václav Bažant , Savannah Collins-Key , Jiří Doležal , Daniel Druckenbrod , Tsutomu Enoki , Keyan Fang , Pavel Fibich , Grant L. Harley , Kazuhiko Hoshizaki , Hideyuki Ida , Masae I. Ishihara , Akira Kagawa , Kirill A. Korznikov , Justin Maxwell , Masahiro Nakamura , Mahoko Noguchi , Jan Altman
Tree-growth patterns encode valuable information about forest dynamics, ecological processes, and environmental changes. However, extracting this information requires precise visualization of tree-ring boundaries. While species with distinct tree-ring boundaries (e.g., conifers and ring-porous hardwoods) have been extensively studied, diffuse-porous and semi-ring-porous species remain understudied, despite their ecological importance. Addressing this knowledge gap requires improved tree-ring visualization techniques for these challenging species to enable their reliable measurement and crossdating. In this study, we evaluated the effectiveness of various sample preparation and imaging techniques for enhancing tree-ring visibility in 62 temperate tree species sensu lato from East Asia and North America. We compared three preparation methods: increment cores surfaced with a core microtome with and without chalk, and double-stained thin sections. These were combined with four imaging techniques: visible light microscopy and fluorescence microscopy using ultraviolet (UV), green fluorescent protein A (GFPA), and red fluorescent protein 1 (RFP1) filters. The results demonstrated that double-stained thin sections under visible light yielded the clearest tree-ring boundaries, followed by chalked surfaced cores under visible light. Among the fluorescence techniques, UV fluorescence imaging outperformed GFPA and RFP1 fluorescence. Although double-stained thin-section preparation requires greater expertise, it is a reliable, relatively fast, and cost-effective approach that can expand the scope of dendrochronological studies and support broader applications in forest management, climate research, and biodiversity conservation.
{"title":"Enhancing tree-ring visibility: A comparative study of sample and imaging techniques for 62 temperate tree species","authors":"Nela Altmanová , Martina Hrádková , Eva Návratová , Vít Pejcha , Václav Bažant , Savannah Collins-Key , Jiří Doležal , Daniel Druckenbrod , Tsutomu Enoki , Keyan Fang , Pavel Fibich , Grant L. Harley , Kazuhiko Hoshizaki , Hideyuki Ida , Masae I. Ishihara , Akira Kagawa , Kirill A. Korznikov , Justin Maxwell , Masahiro Nakamura , Mahoko Noguchi , Jan Altman","doi":"10.1016/j.dendro.2025.126392","DOIUrl":"10.1016/j.dendro.2025.126392","url":null,"abstract":"<div><div>Tree-growth patterns encode valuable information about forest dynamics, ecological processes, and environmental changes. However, extracting this information requires precise visualization of tree-ring boundaries. While species with distinct tree-ring boundaries (e.g., conifers and ring-porous hardwoods) have been extensively studied, diffuse-porous and semi-ring-porous species remain understudied, despite their ecological importance. Addressing this knowledge gap requires improved tree-ring visualization techniques for these challenging species to enable their reliable measurement and crossdating. In this study, we evaluated the effectiveness of various sample preparation and imaging techniques for enhancing tree-ring visibility in 62 temperate tree species <em>sensu lato</em> from East Asia and North America. We compared three preparation methods: increment cores surfaced with a core microtome with and without chalk, and double-stained thin sections. These were combined with four imaging techniques: visible light microscopy and fluorescence microscopy using ultraviolet (UV), green fluorescent protein A (GFPA), and red fluorescent protein 1 (RFP1) filters. The results demonstrated that double-stained thin sections under visible light yielded the clearest tree-ring boundaries, followed by chalked surfaced cores under visible light. Among the fluorescence techniques, UV fluorescence imaging outperformed GFPA and RFP1 fluorescence. Although double-stained thin-section preparation requires greater expertise, it is a reliable, relatively fast, and cost-effective approach that can expand the scope of dendrochronological studies and support broader applications in forest management, climate research, and biodiversity conservation.</div></div>","PeriodicalId":50595,"journal":{"name":"Dendrochronologia","volume":"93 ","pages":"Article 126392"},"PeriodicalIF":2.7,"publicationDate":"2025-07-16","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"144695067","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":3,"RegionCategory":"农林科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Pub Date : 2025-07-09DOI: 10.1016/j.dendro.2025.126385
Darren Davies , Neil J. Loader , Danny McCarroll , Dan Miles , Christopher Bronk Ramsey
ISODATE is a complete dating package for stable oxygen isotope dendrochronology that offers a user-friendly workspace for processing, crossmatching and precisely dating stable isotope chronologies. ISODATE provides the first standardisation of approach for isotope laboratories and the heritage sector for dating and the reporting of dates. The software produces downloadable figures and CSV files containing series alignments and statistical results. The application is freely and publicly available online (isodate.swansea.ac.uk). A manual and guided example accompanies the software. It is hoped that community-led refinements and additional reference chronologies will be added to ISODATE as the technique develops and is adopted more widely.
{"title":"ISODATE – Software for stable isotope dendrochronology","authors":"Darren Davies , Neil J. Loader , Danny McCarroll , Dan Miles , Christopher Bronk Ramsey","doi":"10.1016/j.dendro.2025.126385","DOIUrl":"10.1016/j.dendro.2025.126385","url":null,"abstract":"<div><div>ISODATE is a complete dating package for stable oxygen isotope dendrochronology that offers a user-friendly workspace for processing, crossmatching and precisely dating stable isotope chronologies. ISODATE provides the first standardisation of approach for isotope laboratories and the heritage sector for dating and the reporting of dates. The software produces downloadable figures and CSV files containing series alignments and statistical results. The application is freely and publicly available online (isodate.swansea.ac.uk). A manual and guided example accompanies the software. It is hoped that community-led refinements and additional reference chronologies will be added to ISODATE as the technique develops and is adopted more widely.</div></div>","PeriodicalId":50595,"journal":{"name":"Dendrochronologia","volume":"93 ","pages":"Article 126385"},"PeriodicalIF":2.7,"publicationDate":"2025-07-09","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"144680083","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":3,"RegionCategory":"农林科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Pub Date : 2025-07-07DOI: 10.1016/j.dendro.2025.126384
Balázs Garamszegi , Michael Grabner , Elisabeth Wächter , Josef Gadermaier , Klaus Katzensteiner
Silver fir (Abies alba Mill.) is a key forest tree species in Central Europe growing commonly in mixtures with beech and spruce. In forest sciences, the species has received wide attention due to the complex forest decline phase peaking in the late 1970s and the early 1980s in Central Europe, highlighting the negative effects of air pollution of that time. In the era of accelerating climate change with its adverse effects becoming apparent, the species is gaining renewed interest, especially for its further admixing potential to more resilient forest stands. In our study, we investigate the low-frequency radial growth patterns and changes, as well as the interannual variations and the corresponding climatic signal manifested in the tree-ring width chronologies of seven monospecific stands of silver fir. The study sites represent a broad climatic and elevational gradient along the distribution of the species. We compared the identified changes to recent climatic trends with more frequent dry periods since the 1980s, with specific attention to the timescale of the preceding forest decline phenomena. Following decades of radial growth decrease, culminating in severe decline at some sites, a quick recovery and increasing growth marked a period after the early 1980s, regardless of tree age and most pronounced at lower-elevation sites. The period of growth depression and recovery was accompanied by weakened or altered interannual climatic signals. During the recent decades, mean growth has been decreasing again at lower-elevation sites coinciding with drier conditions and shows signs of similar tendencies at some of the humid sites. A recent strengthening of the hydroclimatic signal, however, was not uniform in its timing among the sites. The interpretation of the results can help to further assess the resilience of silver fir to environmental stress, at the crossroads of past legacies, current and predicted challenges.
银杉(Abies alba Mill.)是中欧重要的森林树种,通常与山毛榉和云杉混合生长。在森林科学中,由于复杂的森林衰退阶段在20世纪70年代末和80年代初在中欧达到顶峰,突出了当时空气污染的负面影响,该物种受到了广泛关注。在气候变化加速及其不利影响日益明显的时代,该物种正重新引起人们的兴趣,特别是因为它具有进一步混入更有弹性的林分的潜力。本文研究了7个银杉单株林分的树轮宽度年代学中所表现出的低频径向生长模式和变化、年际变化及其相应的气候信号。研究地点代表了沿物种分布的广泛的气候和海拔梯度。我们将已确定的变化与自20世纪80年代以来干旱期更为频繁的近期气候趋势进行了比较,并特别关注了之前森林衰退现象的时间尺度。经过几十年的径向生长下降,在一些地点达到严重下降的顶峰,在20世纪80年代初之后,无论树龄如何,树木的快速恢复和增长都标志着一段时间,在低海拔地区最为明显。生长萧条期和恢复期伴随着年际气候信号减弱或改变。在最近的几十年里,在低海拔地区,平均生长再次下降,与干旱条件相一致,在一些潮湿地区也显示出类似的趋势。然而,最近水文气候信号的加强在各地点的时间上并不一致。对结果的解释可以帮助进一步评估银杉对环境压力的恢复能力,在过去的遗产,当前和预测的挑战的十字路口。
{"title":"Site and environmental legacies shape the growth–climate response of silver fir along a climatic and elevational gradient in Austria","authors":"Balázs Garamszegi , Michael Grabner , Elisabeth Wächter , Josef Gadermaier , Klaus Katzensteiner","doi":"10.1016/j.dendro.2025.126384","DOIUrl":"10.1016/j.dendro.2025.126384","url":null,"abstract":"<div><div>Silver fir (<em>Abies alba</em> Mill.) is a key forest tree species in Central Europe growing commonly in mixtures with beech and spruce. In forest sciences, the species has received wide attention due to the complex forest decline phase peaking in the late 1970s and the early 1980s in Central Europe, highlighting the negative effects of air pollution of that time. In the era of accelerating climate change with its adverse effects becoming apparent, the species is gaining renewed interest, especially for its further admixing potential to more resilient forest stands. In our study, we investigate the low-frequency radial growth patterns and changes, as well as the interannual variations and the corresponding climatic signal manifested in the tree-ring width chronologies of seven monospecific stands of silver fir. The study sites represent a broad climatic and elevational gradient along the distribution of the species. We compared the identified changes to recent climatic trends with more frequent dry periods since the 1980s, with specific attention to the timescale of the preceding forest decline phenomena. Following decades of radial growth decrease, culminating in severe decline at some sites, a quick recovery and increasing growth marked a period after the early 1980s, regardless of tree age and most pronounced at lower-elevation sites. The period of growth depression and recovery was accompanied by weakened or altered interannual climatic signals. During the recent decades, mean growth has been decreasing again at lower-elevation sites coinciding with drier conditions and shows signs of similar tendencies at some of the humid sites. A recent strengthening of the hydroclimatic signal, however, was not uniform in its timing among the sites. The interpretation of the results can help to further assess the resilience of silver fir to environmental stress, at the crossroads of past legacies, current and predicted challenges.</div></div>","PeriodicalId":50595,"journal":{"name":"Dendrochronologia","volume":"93 ","pages":"Article 126384"},"PeriodicalIF":2.7,"publicationDate":"2025-07-07","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"144653361","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":3,"RegionCategory":"农林科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Pub Date : 2025-07-03DOI: 10.1016/j.dendro.2025.126383
Mengdan Jing , Changfeng Sun , Yu Liu , Huiming Song , Xuan Wu , Qiufang Cai , Meng Ren , Zhuoying Li , Yongyong Ma , Qiang Li
The Altai and Tianshan Mountains in Xinjiang, located in northwest China, are considered important natural boundaries in Asia. However, the scarcity of long-term meteorological data in these regions has hindered a comprehensive understanding of historical climate variations and their influences on ecology. This study constructed a new tree-ring width chronology of Larix sibirica in the Altai Mountains. Correlation analysis results showed that the average minimum temperature from June to July (Tmin67) was significantly positively correlated with the tree-ring width chronology and was the primary limiting factor for tree radial growth Based on these findings, the Tmin67 for the Altai Mountains from 1730 to 2018 was reconstructed and the warmest and coldest years occurred in 2012 and 1743, respectively. In the past decade, the Tmin67 in the Altai Mountains has risen by 0.86 °C compared to pre-industrial levels. The summer North Atlantic Oscillation (NAO) was found to have an inverse effect on temperature variations in the Altai Mountains. This is the first reconstruction of summer minimum temperatures in the Altai Mountains of central Asia based on a standardized tree-ring width chronology of L. sibirica. Additionally, the combined influences of geographical features and environmental factors contribute to substantial differences in temperature changes between the Altai and Tianshan Mountains. These not only enhance our understanding of past temperature fluctuations but also for projecting future temperature changes through climate modeling.
{"title":"Tree rings reveal spatial differences in temperature changes between the Altai and Tianshan Mountains over the past 289 years","authors":"Mengdan Jing , Changfeng Sun , Yu Liu , Huiming Song , Xuan Wu , Qiufang Cai , Meng Ren , Zhuoying Li , Yongyong Ma , Qiang Li","doi":"10.1016/j.dendro.2025.126383","DOIUrl":"10.1016/j.dendro.2025.126383","url":null,"abstract":"<div><div>The Altai and Tianshan Mountains in Xinjiang, located in northwest China, are considered important natural boundaries in Asia. However, the scarcity of long-term meteorological data in these regions has hindered a comprehensive understanding of historical climate variations and their influences on ecology. This study constructed a new tree-ring width chronology of <em>Larix sibirica</em> in the Altai Mountains. Correlation analysis results showed that the average minimum temperature from June to July (Tmin<sub>67</sub>) was significantly positively correlated with the tree-ring width chronology and was the primary limiting factor for tree radial growth Based on these findings, the Tmin<sub>67</sub> for the Altai Mountains from 1730 to 2018 was reconstructed and the warmest and coldest years occurred in 2012 and 1743, respectively. In the past decade, the Tmin<sub>67</sub> in the Altai Mountains has risen by 0.86 °C compared to pre-industrial levels. The summer North Atlantic Oscillation (NAO) was found to have an inverse effect on temperature variations in the Altai Mountains. This is the first reconstruction of summer minimum temperatures in the Altai Mountains of central Asia based on a standardized tree-ring width chronology of <em>L. sibirica</em>. Additionally, the combined influences of geographical features and environmental factors contribute to substantial differences in temperature changes between the Altai and Tianshan Mountains. These not only enhance our understanding of past temperature fluctuations but also for projecting future temperature changes through climate modeling.</div></div>","PeriodicalId":50595,"journal":{"name":"Dendrochronologia","volume":"93 ","pages":"Article 126383"},"PeriodicalIF":2.7,"publicationDate":"2025-07-03","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"144580018","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":3,"RegionCategory":"农林科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Pub Date : 2025-07-03DOI: 10.1016/j.dendro.2025.126382
Alberto Arzac , Alexander V. Kirdyanov , Viktoria V. Agapova , Alina A. Kirdyanova , Daniel Diaz de Quijano , Nikolay I. Bykov , Ulf Büntgen
The Altai in southern Siberia is one of the few mid-latitude mountain ranges where summer temperatures have been reconstructed over the past 2000 years. While tree-ring width (TRW) measurements have traditionally been used, the paleoclimatic potential of more advanced wood density parameters from different tree species remains largely unexplored in this region. Here, we examine the climatic response of three co-existing conifer species (Larix sibirica Ledeb., Pinus sibirica Du Tour and Picea obovata Ledeb.) from the Russian Altai at ∼1600 m a.s.l. We develop TRW, latewood blue intensity (LWBI), and delta blue intensity (DBI) chronologies, and compare them against monthly temperature means and precipitation totals over the 1951–2021 period. Our results show that all three species respond positively to summer temperatures. The LWBI and DBI chronologies exhibit stronger and more consistent summer temperature signals than TRW, with the highest correlations found in P. obovata (r = 0.7) and P. sibirica (r = 0.5). Despite species-specific differences in temperature sensitivity, our findings demonstrate the potential of LWBI and DBI for robust summer temperature reconstructions in inner Eurasia.
{"title":"Tree-ring width and blue intensity chronologies of three co-existing conifer species from the Russian Altai mountains reveal different climate signals","authors":"Alberto Arzac , Alexander V. Kirdyanov , Viktoria V. Agapova , Alina A. Kirdyanova , Daniel Diaz de Quijano , Nikolay I. Bykov , Ulf Büntgen","doi":"10.1016/j.dendro.2025.126382","DOIUrl":"10.1016/j.dendro.2025.126382","url":null,"abstract":"<div><div>The Altai in southern Siberia is one of the few mid-latitude mountain ranges where summer temperatures have been reconstructed over the past 2000 years. While tree-ring width (TRW) measurements have traditionally been used, the paleoclimatic potential of more advanced wood density parameters from different tree species remains largely unexplored in this region. Here, we examine the climatic response of three co-existing conifer species (<em>Larix sibirica</em> Ledeb., <em>Pinus sibirica</em> Du Tour and <em>Picea obovata</em> Ledeb.) from the Russian Altai at ∼1600 m a.s.l. We develop TRW, latewood blue intensity (LWBI), and delta blue intensity (DBI) chronologies, and compare them against monthly temperature means and precipitation totals over the 1951–2021 period. Our results show that all three species respond positively to summer temperatures. The LWBI and DBI chronologies exhibit stronger and more consistent summer temperature signals than TRW, with the highest correlations found in <em>P. obovata</em> (r = 0.7) and <em>P. sibirica</em> (r = 0.5). Despite species-specific differences in temperature sensitivity, our findings demonstrate the potential of LWBI and DBI for robust summer temperature reconstructions in inner Eurasia.</div></div>","PeriodicalId":50595,"journal":{"name":"Dendrochronologia","volume":"93 ","pages":"Article 126382"},"PeriodicalIF":2.7,"publicationDate":"2025-07-03","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"144604169","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":3,"RegionCategory":"农林科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
The study aimed to evaluate and compare growth resilience to hotter droughts of three common sub-Mediterranean species: black pine (Pinus nigra Arnold), manna ash (Fraxinus ornus L.) and pubescent oak (Quercus pubescens Willd). Over 200 trees were sampled across eight different sites in two countries, Slovenia and Italy. Our primary objective was to evaluate and compare diversity in response to drought within individual species. Increment cores were extracted from trees from each site, which were then processed and their tree-ring width measured. Potential droughts were identified using a Summer-Heat moisture index in the following years 1983, 1985, 1992, 2000 and 2003. Radial growth resilience was analyzed using two indices, post-drought recovery period and average relative growth reduction. Climate-growth relationships were also examined. The individual droughts affected the majority of studied trees. Of the three examined species, F. ornus appears to be the least sensitive to drought stress. Across sites, species or individual droughts, a small proportion of trees always remained unaffected by the droughts. Some of the affected trees never recovered their radial growth within the studied period, indicating that their recovery period exceeded 20 years after individual drought events. The proportion of both varied between species, site and drought. These facts would indicate that more emphasis should be given in the future to studying “winner” trees, since they may hold the answer to species’ better adaptability to the occurrence of hotter droughts.
该研究旨在评估和比较三种常见的亚地中海物种:黑松(Pinus nigra Arnold),甘露灰(Fraxinus ornus L.)和短毛栎(Quercus pubescens wildl)的生长适应能力。在斯洛文尼亚和意大利两个国家的八个不同地点采集了200多棵树的样本。我们的主要目标是评估和比较个体物种对干旱的反应多样性。从每个站点的树木中提取增量核,然后对其进行处理并测量其树轮宽度。在随后的1983年、1985年、1992年、2000年和2003年,利用夏热水分指数确定了潜在干旱。采用干旱后恢复期和平均相对生长量两个指标分析径向生长弹性。还研究了气候与增长的关系。个别干旱影响了大多数被研究的树木。在这三种被调查的物种中,F. ornus似乎对干旱压力最不敏感。在不同的地点、物种或个体干旱中,有一小部分树木始终不受干旱的影响。部分受影响树木的径向生长在研究期间未恢复,表明个别干旱事件后恢复期超过20年。两者的比例因物种、地点和干旱而异。这些事实表明,未来应该更加重视对“赢家”树的研究,因为它们可能掌握物种对更热干旱的更好适应性的答案。
{"title":"Examining post-drought recovery in three sub-Mediterranean species: Some trees not affected while some never recover","authors":"Luka Krajnc , Polona Hafner , Jernej Jevšenak , Şule Ceyda Izmir , Mitja Ferlan , Jožica Gričar","doi":"10.1016/j.dendro.2025.126378","DOIUrl":"10.1016/j.dendro.2025.126378","url":null,"abstract":"<div><div>The study aimed to evaluate and compare growth resilience to hotter droughts of three common sub-Mediterranean species: black pine (<em>Pinus nigra</em> Arnold), manna ash (<em>Fraxinus ornus</em> L.) and pubescent oak (<em>Quercus pubescens</em> Willd). Over 200 trees were sampled across eight different sites in two countries, Slovenia and Italy. Our primary objective was to evaluate and compare diversity in response to drought within individual species. Increment cores were extracted from trees from each site, which were then processed and their tree-ring width measured. Potential droughts were identified using a Summer-Heat moisture index in the following years 1983, 1985, 1992, 2000 and 2003. Radial growth resilience was analyzed using two indices, post-drought recovery period and average relative growth reduction. Climate-growth relationships were also examined. The individual droughts affected the majority of studied trees. Of the three examined species, <em>F. ornus</em> appears to be the least sensitive to drought stress. Across sites, species or individual droughts, a small proportion of trees always remained unaffected by the droughts. Some of the affected trees never recovered their radial growth within the studied period, indicating that their recovery period exceeded 20 years after individual drought events. The proportion of both varied between species, site and drought. These facts would indicate that more emphasis should be given in the future to studying “winner” trees, since they may hold the answer to species’ better adaptability to the occurrence of hotter droughts.</div></div>","PeriodicalId":50595,"journal":{"name":"Dendrochronologia","volume":"93 ","pages":"Article 126378"},"PeriodicalIF":2.7,"publicationDate":"2025-07-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"144580019","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":3,"RegionCategory":"农林科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Pub Date : 2025-06-24DOI: 10.1016/j.dendro.2025.126381
Silvia Passardi , Paolo Cherubini , Brendan M. Buckley , Nam Le Cahn , Holger Gärtner
Dendrochronological studies conducted in tropical regions in recent decades revealed that some species exhibit annual rings. In Southeast Asia, several ring-width chronologies of Fokienia hodginsii (Dunn) A. Henry & H H.Thomas were established to reconstruct past climatic conditions.
Nevertheless, despite the strong correlations with meteorological data, the climate signal in the ring-width chronologies is robust for the shoulder season of the monsoon. For those interested in intra-annual climate signals, other parameters might prove useful. Information on intra-annual variability is crucial for understanding tree growth processes and climate dynamics in tropical regions. In this study, we explore the potential of wood anatomical parameters for climate reconstruction and for gaining a better understanding of the current climate of Southeast Asia. Microslides from cores of F. hodginsii in central Vietnam were analyzed. Notably, average lumen perimeter and lumen length demonstrated the most robust climate signals. They exhibit stronger correlations than ring width with maximum temperature, precipitation, and the Standardized Precipitation Evapotranspiration Index. The highest correlation (r = 0.5) was observed between lumen area and October-November-December precipitation. Furthermore, earlywood parameters show higher correlations with precipitation than whole ring parameters. The growth of earlywood in F. hodginsii appears to be influenced by climatic conditions during September-October-November of the previous year and April of the current year. Thus, earlywood is generally produced around April, whereas latewood grows during or after April-May-June. This study is the first attempt to use anatomical parameters to reconstruct climate in Southeast Asia and provides valuable insights into the intra-annual growth dynamics of tropical tree rings.
近几十年来在热带地区进行的树木年代学研究表明,一些物种表现出年轮。在东南亚,若干环宽hodginsii (Dunn) A. Henry &;H。H。thomas的建立是为了重建过去的气候条件。然而,尽管与气象数据有很强的相关性,环宽年表中的气候信号对于季风的肩季是稳健的。对于那些对年内气候信号感兴趣的人来说,其他参数可能是有用的。关于年内变率的信息对于了解热带地区树木生长过程和气候动态至关重要。在这项研究中,我们探索木材解剖参数对气候重建的潜力,并更好地了解东南亚当前的气候。对越南中部霍奇金孢子虫岩心的微玻片进行了分析。值得注意的是,平均流明周长和流明长度显示出最强大的气候信号。它们与最高温度、降水和标准化降水蒸散指数的相关性强于环宽。10 - 11 - 12月降水量与管腔面积相关性最高(r = 0.5)。此外,早期木材参数与降水的相关性高于全环参数。在前一年的9 - 10 - 11月和当年的4月,霍奇金银杏早木的生长受气候条件的影响。因此,早木通常在4月左右生产,而晚木在4月至5月至6月期间或之后生长。本研究首次尝试利用解剖学参数重建东南亚地区的气候,为热带树木年轮的年内生长动态提供了有价值的见解。
{"title":"Monsoon climatic signal is stronger in wood anatomical traits than in ring widths of Fokienia hodginsii in central Vietnam","authors":"Silvia Passardi , Paolo Cherubini , Brendan M. Buckley , Nam Le Cahn , Holger Gärtner","doi":"10.1016/j.dendro.2025.126381","DOIUrl":"10.1016/j.dendro.2025.126381","url":null,"abstract":"<div><div>Dendrochronological studies conducted in tropical regions in recent decades revealed that some species exhibit annual rings. In Southeast Asia, several ring-width chronologies of <em>Fokienia hodginsii</em> (Dunn) A. Henry & H H.Thomas were established to reconstruct past climatic conditions.</div><div>Nevertheless, despite the strong correlations with meteorological data, the climate signal in the ring-width chronologies is robust for the shoulder season of the monsoon. For those interested in intra-annual climate signals, other parameters might prove useful. Information on intra-annual variability is crucial for understanding tree growth processes and climate dynamics in tropical regions. In this study, we explore the potential of wood anatomical parameters for climate reconstruction and for gaining a better understanding of the current climate of Southeast Asia. Microslides from cores of <em>F. hodginsii</em> in central Vietnam were analyzed. Notably, average lumen perimeter and lumen length demonstrated the most robust climate signals. They exhibit stronger correlations than ring width with maximum temperature, precipitation, and the Standardized Precipitation Evapotranspiration Index. The highest correlation (r = 0.5) was observed between lumen area and October-November-December precipitation. Furthermore, earlywood parameters show higher correlations with precipitation than whole ring parameters. The growth of earlywood in <em>F. hodginsii</em> appears to be influenced by climatic conditions during September-October-November of the previous year and April of the current year. Thus, earlywood is generally produced around April, whereas latewood grows during or after April-May-June. This study is the first attempt to use anatomical parameters to reconstruct climate in Southeast Asia and provides valuable insights into the intra-annual growth dynamics of tropical tree rings.</div></div>","PeriodicalId":50595,"journal":{"name":"Dendrochronologia","volume":"92 ","pages":"Article 126381"},"PeriodicalIF":2.7,"publicationDate":"2025-06-24","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"144518541","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":3,"RegionCategory":"农林科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Pub Date : 2025-06-24DOI: 10.1016/j.dendro.2025.126380
Daigard Ricardo Ortega-Rodriguez , Andrea Hevia , Gabriela Morais Olmedo , Bruna Hornink , Fidel A. Roig , Mario Tomazello-Filho , Raúl Sánchez-Salguero , Luiz Santini , Laura Yáñez-Espinosa
Extreme climatic events in the Amazon region open questions about how the interactions between exogenous and endogenous variables occur in the wood formation of widely distributed tree species such as Cedrela fissilis Vell. In this study, eleven mature-phase trees from a C. fissilis population growing on a non-flooded forest in the southern Amazon basin were selected to determine the interaction between climatic (precipitation, temperature, and moisture indicators: precipitation minus potential evapotranspiration - P-PET and standardized precipitation evapotranspiration index - SPEI), chemical (xylem concentrations of Al, P, S, Ca, K, Mn, Fe, Sr and their meaningful molar ratios) and anatomical (proportion of vessels – PV, fibres – PF, and parenchyma – PP) predictors to explain the variability of ring width (RW) and wood densities (average – RD, minimum – MND, and maximum – MXD). Decision tree regression was applied for understand this interaction in three datasets, values of narrow or less dense, complacent, and wide or dense rings. Narrow or wider rings vary manly associated to hydraulic tissues (PV) and SPEI. Less dense and complacent (in density values) rings vary manly associated to structural tissues (PF) and elements involved in soil-root interactions (Al) and resistance to water stress (Ca/Mn). Less dense MND vary associated to storage and transportation tissues (PP) and elements involved in soil-root interactions (Al and Mn), whereas dense MXD vary associated to structural (PF) and hydraulic (PV) tissues, precipitation and elements related to cambial activity (Ca and K/Ca). In the context of an increase in the frequency and intensity of droughts in the region, the formation of narrower and less dense rings in C. fissilis is expected. In this sense, our results suggest that higher values, which ensure the functionality of these variables under these extreme conditions, are associated with a higher proportion of structural tissues to the detriment of hydraulic ones, in addition to higher K, Mn, and Al storage in the xylem, which mediate cambial activity based on cell expansion, reduced vulnerability to water stress, and healthier root system conditions, respectively. Altogether, this study offers clues to understand variables combination associated with wood formation in the face of extreme water-availability stress that can lead hydraulic failure, carbon starvation, increasing vulnerability, and even specie´s dieback.
{"title":"Wood formation mechanisms of Cedrela fissilis Vell. in extreme years: Climatic, anatomical and chemical predictors","authors":"Daigard Ricardo Ortega-Rodriguez , Andrea Hevia , Gabriela Morais Olmedo , Bruna Hornink , Fidel A. Roig , Mario Tomazello-Filho , Raúl Sánchez-Salguero , Luiz Santini , Laura Yáñez-Espinosa","doi":"10.1016/j.dendro.2025.126380","DOIUrl":"10.1016/j.dendro.2025.126380","url":null,"abstract":"<div><div>Extreme climatic events in the Amazon region open questions about how the interactions between exogenous and endogenous variables occur in the wood formation of widely distributed tree species such as <em>Cedrela fissilis</em> Vell. In this study, eleven mature-phase trees from a <em>C. fissilis</em> population growing on a non-flooded forest in the southern Amazon basin were selected to determine the interaction between climatic (precipitation, temperature, and moisture indicators: precipitation minus potential evapotranspiration - P-PET and standardized precipitation evapotranspiration index - SPEI), chemical (xylem concentrations of Al, P, S, Ca, K, Mn, Fe, Sr and their meaningful molar ratios) and anatomical (proportion of vessels – PV, fibres – PF, and parenchyma – PP) predictors to explain the variability of ring width (RW) and wood densities (average – RD, minimum – MND, and maximum – MXD). Decision tree regression was applied for understand this interaction in three datasets, values of narrow or less dense, complacent, and wide or dense rings. Narrow or wider rings vary manly associated to hydraulic tissues (PV) and SPEI. Less dense and complacent (in density values) rings vary manly associated to structural tissues (PF) and elements involved in soil-root interactions (Al) and resistance to water stress (Ca/Mn). Less dense MND vary associated to storage and transportation tissues (PP) and elements involved in soil-root interactions (Al and Mn), whereas dense MXD vary associated to structural (PF) and hydraulic (PV) tissues, precipitation and elements related to cambial activity (Ca and K/Ca). In the context of an increase in the frequency and intensity of droughts in the region, the formation of narrower and less dense rings in <em>C. fissilis</em> is expected. In this sense, our results suggest that higher values, which ensure the functionality of these variables under these extreme conditions, are associated with a higher proportion of structural tissues to the detriment of hydraulic ones, in addition to higher K, Mn, and Al storage in the xylem, which mediate cambial activity based on cell expansion, reduced vulnerability to water stress, and healthier root system conditions, respectively. Altogether, this study offers clues to understand variables combination associated with wood formation in the face of extreme water-availability stress that can lead hydraulic failure, carbon starvation, increasing vulnerability, and even specie´s dieback.</div></div>","PeriodicalId":50595,"journal":{"name":"Dendrochronologia","volume":"92 ","pages":"Article 126380"},"PeriodicalIF":2.7,"publicationDate":"2025-06-24","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"144563699","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":3,"RegionCategory":"农林科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Pub Date : 2025-06-18DOI: 10.1016/j.dendro.2025.126379
Ireneusz Malik , Michael Maerker , Małgorzata Wistuba , Elżbieta Gorczyca , Patrizio Torrese , Manuel La Licata , Yang Yu , Beata Woskowicz-Ślęzak , Anna Bieniasz
We analysed landslide activity on a slope above the Lago di Trebecco reservoir (Northern Apennines, Italy) and indicated a hazard of future destructive landslide reactivation. We used dendrochronology in a variant of eccentric growth analysis to indicate the hazard of sudden slope failure, which could reach the water reservoir and form a tsunami. We use the previous pattern of eccentric growth of trees, found in the case of two landslides reactivated in a landslide catastrophe in Poland in 2010. Before the disaster, trees formed a specific eccentric growth pattern which preceded and can predict landslide catastrophe (sudden slope failure). This pattern was compared to trees growing on the Lago di Trebecco landslide to estimate the hazard of future destructive landslide occurrence. Trees sampled on the landslide above the Lago di Trebecco have recorded a gradual increase in activity over the last few decades. This means the landslide has become increasingly active. On the other hand, in the last two years, a significant decrease in landslide activity has been recorded on the Lago di Trebecco landslide; activity of landslides located in Poland increased significantly two years before the landslide catastrophe in 2010. This means no dendrochronological records indicate that the Lago di Trebecco landslide will be triggered in a short time, but the landslide should be monitored because of the increasing activity over the past decades. Dendrochronology can be a useful indicator for the hazard of a landslide catastrophe (sudden slope failure), which can enter lakes and induce tsunamis.
我们分析了Lago di Trebecco水库(意大利亚平宁山脉北部)上方斜坡的滑坡活动,并指出了未来破坏性滑坡重新激活的危险。我们在一种偏心生长分析的变型中使用树木年代学来表明斜坡突然破坏的危险性,这种破坏可能到达水库并形成海啸。我们使用了之前的树木偏心生长模式,在2010年波兰山体滑坡灾难中再次引发的两次山体滑坡中发现了这种模式。灾害发生前,树木形成了一种特殊的偏心生长模式,这种生长模式先于并可以预测滑坡灾害(边坡突变)。将这种模式与拉戈迪特雷贝科滑坡上生长的树木进行比较,以估计未来发生破坏性滑坡的危险性。在雷贝科湖(Lago di Trebecco)滑坡上采集的树木样本显示,在过去几十年里,滑坡活动逐渐增加。这意味着滑坡变得越来越活跃。另一方面,在过去两年中,拉戈迪特雷贝科滑坡的滑坡活动显著减少;在2010年的滑坡灾难发生前两年,波兰的滑坡活动明显增加。这意味着没有树木年代学记录表明Lago di Trebecco滑坡将在短时间内触发,但由于过去几十年的活动增加,滑坡应该受到监测。树木年代学可以作为滑坡灾害(突发性边坡破坏)危险性的有用指标,它可以进入湖泊并引发海啸。
{"title":"Tree rings indicate hazards related to a waterside landslide in the Northern Apennines, Italy – A preliminary step towards forecasting landslides and related tsunami","authors":"Ireneusz Malik , Michael Maerker , Małgorzata Wistuba , Elżbieta Gorczyca , Patrizio Torrese , Manuel La Licata , Yang Yu , Beata Woskowicz-Ślęzak , Anna Bieniasz","doi":"10.1016/j.dendro.2025.126379","DOIUrl":"10.1016/j.dendro.2025.126379","url":null,"abstract":"<div><div>We analysed landslide activity on a slope above the Lago di Trebecco reservoir (Northern Apennines, Italy) and indicated a hazard of future destructive landslide reactivation. We used dendrochronology in a variant of eccentric growth analysis to indicate the hazard of sudden slope failure, which could reach the water reservoir and form a tsunami. We use the previous pattern of eccentric growth of trees, found in the case of two landslides reactivated in a landslide catastrophe in Poland in 2010. Before the disaster, trees formed a specific eccentric growth pattern which preceded and can predict landslide catastrophe (sudden slope failure). This pattern was compared to trees growing on the Lago di Trebecco landslide to estimate the hazard of future destructive landslide occurrence. Trees sampled on the landslide above the Lago di Trebecco have recorded a gradual increase in activity over the last few decades. This means the landslide has become increasingly active. On the other hand, in the last two years, a significant decrease in landslide activity has been recorded on the Lago di Trebecco landslide; activity of landslides located in Poland increased significantly two years before the landslide catastrophe in 2010. This means no dendrochronological records indicate that the Lago di Trebecco landslide will be triggered in a short time, but the landslide should be monitored because of the increasing activity over the past decades. Dendrochronology can be a useful indicator for the hazard of a landslide catastrophe (sudden slope failure), which can enter lakes and induce tsunamis.</div></div>","PeriodicalId":50595,"journal":{"name":"Dendrochronologia","volume":"92 ","pages":"Article 126379"},"PeriodicalIF":2.7,"publicationDate":"2025-06-18","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"144479959","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":3,"RegionCategory":"农林科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}