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CTRing: An R package to extract wood density profiles from computed tomography images of discs and logs CTRing:从圆盘和原木的计算机断层扫描图像中提取木材密度剖面的 R 软件包
IF 2.7 3区 农林科学 Q1 FORESTRY Pub Date : 2024-11-08 DOI: 10.1016/j.dendro.2024.126274
Dipak Mahatara , Filipe Campelo , Laurent Houle , Alain Caron , Julie Barrette , Pierre Francus , Robert Schneider
Accurately determining the position of pith and accessing tree-ring density profiles, including intra-ring variations, is important for both the forest industry and dendroclimatology. Although several available methods exist for acquiring this information, such as X-ray computed tomography (CT), micro-CT, and X-ray films, the availability of open-source programs for extracting data remains limited. The CTRing package in the R environment integrates a series of functions to detect precisely the pith and tree-ring boundaries and generate tree-ring density profiles using CT images of tree cross sections. Before processing, grey values are transformed into density using a calibration function. Pith position is then detected by combining an adapted Hough Transform method and a one-dimensional edge detector. Tree-ring profiles along the pith-to-bark path of interest are inspected visually, and tree-ring boundaries can be easily added or removed manually via a graphical user interface. After correcting for tree-ring boundaries, the inflection points of a 3rd-degree polynomial obtained from density profiles are used to delimit the earlywood–latewood transition. We tested this package using 60 CT-scanned images of white spruce (Picea glauca (Moench) Voss) discs collected at various tree heights (0 %, 25 %, 50 % and 75 % of the total tree height as well as at 1.3 m). The pith detection function had an average mean error of 0.72 mm with 95 % of the automatically detected pith locations that differed by less than 2 mm from their manually located positions. Error decreased toward the apex of the tree. The functions of the CTRing package are flexible and can be easily implemented or adapted. The package could also be used with simple images of discs to obtain ring-width time series; however, this use must be evaluated further. Future work with this package involves assessing the use of low-quality images and ring-porous species.
准确确定髓部位置和获取树环密度剖面,包括环内变化,对林业和树木气候学都很重要。虽然有多种可用的方法来获取这些信息,如 X 射线计算机断层扫描(CT)、显微 CT 和 X 射线胶片,但用于提取数据的开源程序仍然有限。R 环境中的 CTRing 软件包集成了一系列函数,可精确检测髓部和树环边界,并利用树木横截面的 CT 图像生成树环密度剖面图。处理前,使用校准函数将灰度值转换为密度。然后,结合改良的 Hough 变换方法和一维边缘检测器检测髓部位置。沿着感兴趣的髓部到树皮路径的树环剖面可通过视觉进行检查,树环边界可通过图形用户界面轻松手动添加或删除。校正树环边界后,利用从密度剖面获得的三度多项式的拐点来划定早材-晚材的过渡。我们使用在不同树高(总树高的 0%、25%、50% 和 75%,以及 1.3 米处)采集的 60 张白云杉(Picea glauca (Moench) Voss)圆盘 CT 扫描图像对该软件包进行了测试。髓部检测功能的平均误差为 0.72 毫米,95% 自动检测到的髓部位置与人工定位的位置相差不到 2 毫米。误差向树顶方向减小。CTRing 软件包的功能非常灵活,易于实施或调整。该软件包还可与简单的圆盘图像一起使用,以获得环宽时间序列;不过,这一用途还需进一步评估。该软件包的未来工作包括评估低质量图像和多孔环树种的使用情况。
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引用次数: 0
A critical source of noise in tree-ring based chronologies of landslide movements 以树龄为基础的滑坡运动年代学中的一个关键噪声源
IF 2.7 3区 农林科学 Q1 FORESTRY Pub Date : 2024-11-05 DOI: 10.1016/j.dendro.2024.126273
Karel Šilhán
Tree-ring based analysis is currently a widely used tool for obtaining data on the spatio-temporal behaviour of past landslides, which is key information for determining hazard or estimating potential triggers. However, even this approach has its limitations, which may induce a lot of noise in the obtained results. In doing so, the sources of this noise, which in some cases can even simulate a spurious landslide event, are not well known. Thus, this study highlights one of the possible significant sources of noise in tree-ring based landslide chronologies, which is the effect of wind combined with the soft landslide surface, which causes instability of trees that can easily lean to simulate a landslide movement. For this purpose, 197 individuals of common spruce (Picea abies (L.) Karst.) on the flat parts of two flow-like landslides were analyzed. 280 growth disturbances were identified and 17 events were reconstructed. In order to assess the landslide origin of the collected data, this study included analyses of the nature and relative contribution of different types of growth disturbances, their spatial distribution, analyses of the direction and magnitude of tree trunk leaning, as well as analyses of extreme precipitation and wind events. By combining the results obtained, it can be concluded that most of the detected growth disturbances and reconstructed events were induced by wind in combination with the soft landslide surface into which the trees sink. Since these growth disturbances cannot be filtered out by standard reference trees, they are an extremely serious source of noise that can completely invalidate the dendrogeomorphic results of the study. The study thus identifies which parameters should be newly considered in dendrogeomorphic analyses of landslide movements.
基于树环的分析是目前广泛使用的一种工具,用于获取有关过去山体滑坡时空行为的数据,这是确定危害或估计潜在触发因素的关键信息。然而,即使是这种方法也有其局限性,可能会在获得的结果中产生大量噪声。在这种情况下,这些噪声(在某些情况下甚至可以模拟虚假的滑坡事件)的来源并不为人所知。因此,本研究强调了基于树环的滑坡年代学中可能存在的重要噪声源之一,即风与松软的滑坡表面相结合的影响,这会导致树木的不稳定性,从而很容易倾斜以模拟滑坡运动。为此,对两处流状滑坡平地上的 197 株普通云杉(Picea abies (L.) Karst.)进行了分析。确定了 280 次生长扰动,重建了 17 次事件。为了评估所收集数据的滑坡起源,这项研究包括分析不同类型生长扰动的性质和相对贡献、其空间分布、树干倾斜方向和幅度分析,以及极端降水和大风事件分析。综合所得结果,可以得出结论,大部分检测到的生长扰动和重建事件都是由风力与树木下沉的松软滑坡面共同引起的。由于这些生长扰动无法被标准参考树过滤掉,因此它们是一个极其严重的噪声源,会使研究的树枝地貌结果完全失效。因此,本研究确定了在对滑坡运动进行树枝地貌分析时应新考虑的参数。
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引用次数: 0
Stand structure and disturbance history of old-growth blue pine (Pinus wallichiana) forests in the Bhutan Himalaya 不丹喜马拉雅山脉古老蓝松(Pinus wallichiana)林的林分结构和干扰史
IF 2.7 3区 农林科学 Q1 FORESTRY Pub Date : 2024-10-15 DOI: 10.1016/j.dendro.2024.126272
Karma Tenzin , Craig R. Nitschke , Kathryn J. Allen , Benjamin Wagner , Thiet V. Nguyen , Patrick J. Baker
Blue pine (Pinus wallichiana) forests are of significant ecological, economic, and cultural importance in the Himalayas. We used dendrochronological methods to investigate the role of natural and human disturbance in shaping the development of these forests. Analyses of the age structure and growth patterns of blue pine populations over the period 1760–2020 at two different sites in central Bhutan revealed that blue pine tends to establish as single-cohort stands following relatively intense disturbances and as multi-cohort stands after low-to-moderate severity disturbances. Shifting cultivation, which was common across the region, likely led to the establishment of single-cohort stands, particularly near human settlements, whereas natural disturbances are likely responsible for the development of multi-cohort stands. Tree-ring records revealed an acute change in recruitment patterns in the early 1970s associated with the 1969 Forest Act of Bhutan, which limited traditional practices, such as firewood collection and grazing, within the forests. This led to a sudden and sustained increase in the recruitment of broadleaf tree species and effectively curtailed blue pine regeneration over the past half century due to thick understory and midstory vegetation reducing the amount of light reaching the forest floor. These results highlight the role of disturbances, both human and natural, in driving forest stand dynamics in Himalayan forests and how forest policy and traditional practices can alter those dynamics.
蓝松(Pinus wallichiana)林在喜马拉雅山地区具有重要的生态、经济和文化意义。我们利用树木年代学方法研究了自然和人为干扰对这些森林发展的影响。对不丹中部两个不同地点的蓝松种群在 1760-2020 年间的年龄结构和生长模式的分析表明,蓝松往往在受到相对强烈的干扰后形成单群林分,而在受到中低度干扰后形成多群林分。该地区普遍存在的轮垦可能导致了单株林的形成,尤其是在人类居住区附近,而自然干扰则可能导致多株林的形成。树环记录显示,在 20 世纪 70 年代初,由于 1969 年《不丹森林法》的颁布,森林中的木柴采集和放牧等传统习俗受到了限制,因此树木的生长模式发生了急剧的变化。在过去的半个世纪里,由于茂密的林下和林中植被减少了到达林地的光照量,这导致阔叶树种突然持续增加,并有效地抑制了蓝松的再生。这些结果突显了人为和自然干扰在喜马拉雅森林林分动态中的推动作用,以及森林政策和传统做法如何改变这些动态。
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引用次数: 0
Exploring the potential for a 9000-year tree-ring chronology consisting of subfossil oak material from southern Scandinavia 探索由斯堪的纳维亚半岛南部橡树亚化石材料组成的 9000 年树龄年表的潜力
IF 2.7 3区 农林科学 Q1 FORESTRY Pub Date : 2024-10-06 DOI: 10.1016/j.dendro.2024.126268
Johannes Edvardsson , Kjeld Christensen , Jonas Ogdal Jensen , Hans Linderson , Claudia Baittinger
In this study, we present the initial results from a long-term initiative to develop a multi-millennial tree-ring width (TRW) chronology for subfossil oak (Quercus spp.) trees in South Scandinavia. We have constructed 40 TRW chronologies, primarily from oak trunks extracted from peatlands, archaeological sites, drainage ditches, and infrastructure projects, as well as some submerged material. The trees included in these chronologies have been dendrochronologically dated and/or dated by radiocarbon, showing a temporal spread from 6911 ± 246 BCE to 1117 CE. Significant assemblages of trees are found during the periods 6000–4500 BCE, 3500–2600 BCE, 1750–1200 BCE, 900–400 BCE, and 200 BCE–500 CE, with intervening periods exhibiting low sample replication or gaps. The paleoclimatic information extracted from TRW and replication data may vary based on the substrate in which the trees were rooted, geographical locations, and the prevailing climate conditions during their growth. Nevertheless, extending the oak TRW chronologies is crucial because (1) no such long and annually resolved climate records from southern Scandinavia exist, (2) there is a widespread lack of detailed paleoclimatic proxies spanning multi-millennial periods, and (3) it will provide an essential dating tool for wooden archaeological artifacts. This study is the first in a series aimed at refining paleoclimatic and ecological reconstructions in southern Scandinavia. It demonstrates the potential to develop South Scandinavian TRW chronologies covering the last 9000 years, filling a geographical gap in an ecologically sensitive region.
在本研究中,我们介绍了为南斯堪的纳维亚半岛的亚化石橡树(栎属)建立多千年树环宽度(TRW)年代学的长期计划的初步成果。我们已经构建了 40 个 TRW 年表,主要取材于从泥炭地、考古遗址、排水沟和基础设施项目中提取的橡树树干,以及一些沉水材料。这些年表中的树木都经过了树木年代学测定和/或放射性碳测定,时间跨度从公元前 6911 ± 246 年到公元前 1117 年。在公元前 6000 年至 4500 年、公元前 3500 年至 2600 年、公元前 1750 年至 1200 年、公元前 900 年至 400 年以及公元前 200 年至公元前 500 年期间,发现了重要的树木群,而在这期间,样本复制率较低或存在空白。从 TRW 和复制数据中提取的古气候信息可能会因树木扎根的基质、地理位置及其生长期间的主要气候条件而有所不同。然而,扩展橡树 TRW 年代学至关重要,因为:(1)斯堪的纳维亚半岛南部不存在如此长的、每年分辨的气候记录;(2)普遍缺乏跨越多千年期的详细古气候代用指标;(3)它将为木质考古文物提供重要的年代测定工具。本研究是旨在完善斯堪的纳维亚半岛南部古气候和生态重建的一系列研究中的第一项。它展示了开发涵盖过去 9000 年的南斯堪的纳维亚 TRW 年代学的潜力,填补了这一生态敏感地区的地理空白。
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引用次数: 0
Salinity regulates radial growth of Cynometra ramiflora L. in the Sundarbans mangrove ecosystem 盐度调节孙德尔本斯红树林生态系统中苎麻属植物的径向生长
IF 2.7 3区 农林科学 Q1 FORESTRY Pub Date : 2024-10-04 DOI: 10.1016/j.dendro.2024.126270
Md. Qumruzzaman Chowdhury , Swapan Kumar Sarker , Shahadat Hossain, Md. Imam Hossain Imran, Anup Datta
The mangrove biome is threatened by global environmental changes (including sea level rise, SLR) and anthropogenic disturbances. In this context, understanding the growth dynamics of mangrove species is essential for designing effective management plans for critical mangrove ecosystems such as the Bangladesh Sundarbans. Therefore, this study aims to (1) identify the growth-ring boundaries and tested their periodicity (annual nature) in one of the ecologically important understory mangrove species, Cynometra ramiflora in the Bangladesh Sundarbans, (2) determine the influences of climate and river discharge on radial growth, and (3) examine the influence of habitat variables (e.g., regulators, resources and forest structure) on radial growth. The growth-ring boundaries of C. ramiflora were distinct on the polished wood discs and marked by a layer of flattened fibers mixed with parenchyma. The agreement between individual growth-ring series and chronology statistics enabled us to develop for the first time a 42-year-long chronology spanning from 1979 to 2021. The results indicate that growth rings are annual and could be used for age and growth rate estimations. Monsoonal and annual precipitation enhanced radial growth. Growth was also positively influenced by the amount of river discharge received prior to the onset of growth, particularly during the pre-monsoon. Generalized additive models (GAMs) revealed that among the habitat variables, salinity had a strong negative influence on radial growth of the studied species in the Sundarbans, while tree density and diameter heterogeneity (coefficient of variation, CoV of diameter at breast height) had positive influences. This study revealed that C. ramiflora growth is strongly dependent on soil salinity and highlighted the potential of this approach for improving the prediction of future tree growth and distribution in the face of projected global changes, in particular, SLR.
红树林生物群落受到全球环境变化(包括海平面上升)和人为干扰的威胁。在此背景下,了解红树林物种的生长动态对于为孟加拉国孙德尔本斯等关键红树林生态系统设计有效的管理计划至关重要。因此,本研究旨在:(1)确定孟加拉国孙德尔本斯具有重要生态意义的底层红树林物种之一 Cynometra ramiflora 的生长环边界并测试其周期性(年度性);(2)确定气候和河流排水量对径向生长的影响;以及(3)研究生境变量(如调节器、资源和森林结构)对径向生长的影响。在打磨过的木盘上,苧麻的生长环边界明显,并有一层扁平的纤维与实质混合在一起。单个生长年轮序列与年轮统计之间的一致性使我们首次建立了从 1979 年到 2021 年的 42 年年轮。结果表明,生长年轮是年轮,可用于年龄和生长率的估算。季风和年降水量促进了径向生长。生长还受到生长开始前,特别是季风前的河流排水量的积极影响。广义加法模型(GAMs)显示,在生境变量中,盐度对所研究物种在孙德尔本斯的径向生长有很大的负面影响,而树木密度和直径异质性(胸径变异系数)则有正面影响。这项研究揭示了苧麻的生长在很大程度上依赖于土壤盐度,并强调了这种方法在面对预计的全球变化(尤其是可持续土地退化和干旱)时改善未来树木生长和分布预测的潜力。
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引用次数: 0
Changes in the radial growth patterns of two dominant tree species in north-central China under climate warming 气候变暖下中国中北部两种优势树种径向生长模式的变化
IF 2.7 3区 农林科学 Q1 FORESTRY Pub Date : 2024-10-04 DOI: 10.1016/j.dendro.2024.126269
Jiachuan Wang , Shuheng Li , Yili Guo , Yijie Han , Qi Liu , Yiqi Zhao , Qiang Li
The radial growth pattern of alpine coniferous trees in the mid-high latitudes of the Northern Hemisphere has an unstable and inconsistent response to climate warming. Understanding the growth trends of trees in the past and future is crucial for forest cultivation against the background of climate change. Thus, we used traditional dendroclimatological methods to analyze the radial growth patterns and stability in response to climate change of the two dominant species on Guancen Mountain and concluded that: (1) the radial growth of Larix principis-rupprechtii was more sensitive than that of Picea meyeri to climatic factors; (2) before and after the abrupt temperature change, the major controlling climatic factors for the radial growth of the two dominant species were spring precipitation and mean temperature, respectively; (3) before the abrupt temperature change, the radial growth of L. principis-rupprechtii was affected by the mean temperature in autumn, while that of P. meyeri was restricted by the standardized precipitation evapotranspiration index in spring; after the abrupt temperature change, the major controlling climate factors of L. principis-rupprechtii and P. meyeri were winter drought and the combination of water and heat in summer, respectively; and (4) after the abrupt temperature change, the interannual basal area increments of the two species followed an upward trend, however, the radial growth rate of both species decreased after detrending, and the growth and development of both species were seriously stressed by drought. Under the background of climate warming, to explore the coping situation of different tree species in the same habitat, to provide theoretical and mechanism support for the future cultivation of forests according to local conditions, and to provide suggestions for the "greening" problem fundamentally.
北半球中高纬度地区高山针叶树的径向生长模式对气候变暖的反应不稳定,也不一致。在气候变化的背景下,了解树木过去和未来的生长趋势对于森林培育至关重要。因此,我们采用传统的树木气候学方法,分析了冠豸山两种优势树种的径向生长模式及其对气候变化响应的稳定性,并得出以下结论:(1)Larix principis-rupprechtii 的径向生长比 Picea meyeri 对气候因子更敏感;(2)在气温骤变前后,控制两种优势树种径向生长的主要气候因子分别是春季降水量和平均气温;(3)在气温骤变前,L. principis-rupprechtii 的径向生长受秋季平均气温的影响,而 P. principis-rupprechtii 的径向生长受秋季平均气温的限制。meyeri的径向生长受春季标准化降水蒸散指数的限制;气温骤变后,L. principis-rupprechtii和P. meyeri的主要气候控制因子分别为冬季干旱和夏季水热同期;以及(4)气温骤变后,两种植物的年际基部面积增量呈上升趋势,但径向生长速率在去趋势化后均有所下降,两种植物的生长发育均受到干旱的严重胁迫。在气候变暖的背景下,探讨同一生境下不同树种的应对情况,为今后因地制宜培育森林提供理论和机制支撑,从根本上为 "绿化 "问题提供建议。
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引用次数: 0
Tree-ring anomalies as time markers for ice-core chronologies, with special reference to 5281 BCE as the possible date of the Kikai volcanic event 作为冰核年代学时间标记的树环异常,特别是公元前 5281 年作为基开火山事件的可能日期
IF 2.7 3区 农林科学 Q1 FORESTRY Pub Date : 2024-10-04 DOI: 10.1016/j.dendro.2024.126271
Varvara A. Bessonova , Ludmila A. Gorlanova , Rashit M. Hantemirov
The synchronization of Greenland and Antarctica ice core data with tree-ring data, other proxies, and direct observations of natural processes and events is important to understand past climatic variation and environmental change. One of the methods that is used to correct the dating of ice layers is to match volcanic eruption footprints in ice cores with tree rings, manifested as sulphate spikes and anomalous rings, respectively. In this study, we inventoried the occurrence of tree-ring anatomical anomalies and extremes in ring width during three 200-year periods. These periods included three of the eight largest Holocene volcanic eruptions, each with a Volcanic Explosivity Index (VEI) of 7. The initial period spanned from 6560 to 6360 BCE and included the eruption of Ilyinsky Volcano in Kamchatka. The second period was from 5780 to 5580 BCE, during which Mount Mazama Volcano in North America erupted. The third period was from 5380 to 5180 BCE when the Kikai Volcano in the Japanese Islands erupted. Throughout the first two periods, no substantial tree-ring anomalies were observed suggesting the absence of any significant climate consequences of a major volcanic eruption. However, in the 5380–5180 BCE period, a clear sharp decline in tree growth and an exceptionally high frequency of tree-ring anomalies were identified in 5281 BCE and the subsequent 5 years. We propose that the exceptionally narrow light rings in these 6 years are indicative of the climatic impact resulting from the Kikai volcanic eruption. We suggest utilising the year 5281 BCE as the reference year for synchronising the Greenland and Antarctica ice core chronologies. In the case that our assumption is correct, this would imply the necessity to adjust the time of the event to an earlier date compared to the dates indicated by the existing ice core chronologies of the GICC05 (Greenland Ice Core Chronology 2005), adjusted according to Kobashi (2017), and WD2014 used for creating HolVol 1.0 (Holocene ice-core volcanic eruption catalogue from 9500 BCE - 1900 CE) by 67 and 54 years, respectively, for the period around 5300 BCE. A verification of our assumption could be conducted by examining the nearby Miyake event, a spike in cosmogenic radiocarbon, of 5258 BCE. Ice core layers displaying potential signs of this event should be approximately 25 years later than the markers of the Kikai volcanic eruption.
将格陵兰岛和南极洲的冰芯数据与树年轮数据、其他代用指标以及对自然过程和事件的直接观测结果同步,对于了解过去的气候变异和环境变化非常重要。用于校正冰层年代的方法之一是将冰芯中的火山喷发足迹与树年轮(分别表现为硫酸盐峰和异常年轮)相匹配。在这项研究中,我们清查了三个 200 年期间出现的树环解剖异常和极端环宽。这三个时期包括全新世八次最大火山爆发中的三次,每次火山爆发指数(VEI)均为 7。第一个时期为公元前 6560 年至公元前 6360 年,包括堪察加半岛伊林斯基火山的爆发。第二个时期为公元前 5780 年至公元前 5580 年,期间北美的马扎玛火山喷发。第三个时期是公元前 5380 年至 5180 年,日本列岛的纪海火山在此期间爆发。在前两个时期,没有观察到明显的树环异常,这表明火山大爆发没有对气候造成任何重大影响。然而,在公元前 5380-5180 年期间,树木生长明显急剧下降,并且在公元前 5281 年及其后的 5 年中发现了频率极高的树环异常。我们认为,这 6 年中异常狭窄的光环表明了基开火山爆发造成的气候影响。我们建议将公元前 5281 年作为同步格陵兰和南极洲冰芯年代学的参考年份。如果我们的假设是正确的,这将意味着有必要将事件发生的时间调整到一个更早的日期,与根据 Kobashi(2017 年)调整的 GICC05(格陵兰冰芯年表 2005)和用于创建 HolVol 1.0(公元前 9500 年至公元前 1900 年全新世冰芯火山喷发目录)的 WD2014 现有冰芯年表所显示的日期相比,公元前 5300 年左右的时期分别提前了 67 年和 54 年。可以通过研究附近的三宅事件(公元前 5258 年的宇宙放射性碳峰值)来验证我们的假设。显示出这一事件潜在迹象的冰芯层应该比 Kikai 火山喷发的标记晚约 25 年。
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引用次数: 0
Tree-ring blue intensity measurements from treeline sites in the Ural Mountains exhibit a strong summer temperature signal 乌拉尔山脉树线地点的树环蓝强度测量显示出强烈的夏季温度信号
IF 2.7 3区 农林科学 Q1 FORESTRY Pub Date : 2024-09-17 DOI: 10.1016/j.dendro.2024.126267
Viktoria V. Agapova , Alberto Arzac , Vladimir V. Kukarskih , Ulf Büntgen , Jan Esper , Alexander V. Kirdyanov
The high northern latitudes offer an ideal environment to analyze tree growth responses to unprecedented recent warming. In this study, for the first time, we explore the dendroclimatological potential of latewood blue intensity (LWBI) and delta blue intensity (DBI) at two Siberian larch (Larix sibirica Ledeb.) sites in the upper treeline ecotone of the Ural Mountains, northern Russia. To assess the climate signals encoded in LWBI and DBI, as well as tree-ring width (TRW) and maximum latewood density (MXD), we correlated these parameter-specific chronologies against monthly temperature means, precipitation totals, and the SPEI index. LWBI and BDI exhibit robust and stable positive correlations with summer temperature, higher than TRW but slightly lower than MXD at both sites, with marginal negative effects from precipitation and strong negative correlations with SPEI. As direct surrogates for MXD, LWBI and DBI from larch trees offer reasonable alternatives as proxies for temperatures in northern latitudes.
北部高纬度地区为分析树木生长对近期前所未有的气候变暖的反应提供了理想的环境。在本研究中,我们首次在俄罗斯北部乌拉尔山脉上层树线生态区的两个西伯利亚落叶松(Larix sibirica Ledeb.)地点探索了晚材蓝强度(LWBI)和三角洲蓝强度(DBI)的树木气候学潜力。为了评估 LWBI 和 DBI 以及树环宽度(TRW)和最大晚材密度(MXD)中编码的气候信号,我们将这些特定参数的年代学与月平均气温、降水总量和 SPEI 指数相关联。在两个地点,LWBI 和 BDI 与夏季气温呈稳健而稳定的正相关,高于 TRW,但略低于 MXD,降水略有负作用,与 SPEI 呈强负相关。作为 MXD 的直接替代指标,落叶松的 LWBI 和 DBI 为北纬地区的温度提供了合理的替代指标。
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引用次数: 0
Climatic and disturbances influence on tree-rings of Larix gmelinii in the southeast coastal area 气候和干扰对东南沿海地区落叶松树环的影响
IF 2.7 3区 农林科学 Q1 FORESTRY Pub Date : 2024-09-15 DOI: 10.1016/j.dendro.2024.126264
Marina Evgenienva Rubleva , Anna Stepanovna Vozmishcheva , Svetlana Nikolaevna Bondarchuk
The vast region of North East Asia is covered by primary mixed conifer-broadleaved forests which include a range of different tree species. A key factor in the dynamics of these ecosystems is wind disturbance. According to reports, this factor will be increasingly important as a result of the poleward migration of tropical cyclones, a characteristic of which is strong wind. At the same time, global climate change may reduce the recovery potency of some species and lead to new combinations of species. Gmelin Larch is one of the key early succession species in the north of the region. In the southeastern part of its range (Russian Far East), this species has not been widely studied by dendroclimatologists and there are no dendroecological studies available. This study shows how the seasonal growth of Larix gmelinii responds to changes in climate, specifically to variations in precipitation and temperature. The study has established that these trees are more affected by rising temperatures than by consistent precipitation levels, provided there is no shortage of water. Interestingly, after the 1970s there was a change in the climate sensitivity of Larix gmelinii in June (the month with the strongest correlation). It went from a negative correlation with temperature to a positive correlation with precipitation. By using tree ring data, we were able to reconstruct the past history of forest disturbance. The peaks in this chronology coincide with those in earlier published dendroecological reconstructions for other species. They indicate that the radial growth of larch is sensitive to canopy changes. We recorded two release peaks in the 1960s and 2000s, during the period of meteorological observations. We attributed the first peak to the most powerful tropical cyclone Emma (1956). We assume also that the second peak reflects the recent intensification of tropical cyclones in the region. In our opinion, the change in microclimate as a result of disturbance has altered the relationship to climate in such a way that disturbance may cause tree growth to be dependent on precipitation. At the same time, such low correlations do not support a conclusion about the strong negative influence of the current climate on the trees.
东北亚广大地区覆盖着针阔混交原始森林,其中包括一系列不同的树种。影响这些生态系统动态的一个关键因素是风的干扰。据报道,由于热带气旋向极地迁移,这一因素将变得越来越重要,而热带气旋的一个特点就是风力强劲。同时,全球气候变化可能会降低一些物种的恢复能力,并导致新的物种组合。格梅林落叶松是该地区北部重要的早期演替物种之一。在其分布区的东南部(俄罗斯远东地区),树木气候学家尚未对该物种进行广泛研究,也没有树木生态学方面的研究。这项研究显示了 Larix gmelinii 的季节性生长如何应对气候变化,特别是降水量和温度的变化。研究证实,只要不缺水,这些树木受气温上升的影响比受持续降水量的影响更大。有趣的是,20 世纪 70 年代后,6 月份(相关性最强的月份)的 Larix gmelinii 对气候的敏感性发生了变化。它从与温度的负相关变成了与降水的正相关。通过使用树环数据,我们能够重建过去的森林干扰史。该年表中的峰值与早先发表的其他物种树生态重建中的峰值相吻合。它们表明落叶松的径向生长对树冠变化很敏感。我们记录了 20 世纪 60 年代和 2000 年代气象观测期间的两个释放峰值。我们将第一个峰值归因于最强的热带气旋艾玛(1956 年)。我们还认为,第二个峰值也反映了该地区近期热带气旋的加强。我们认为,干扰导致的小气候变化改变了与气候的关系,干扰可能导致树木生长依赖降水。同时,这种低相关性并不支持当前气候对树木产生强烈负面影响的结论。
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引用次数: 0
Local and regional climatic constraints of shrub and tree growth near the treeline 当地和区域气候对林木线附近灌木和乔木生长的制约因素
IF 2.7 3区 农林科学 Q1 FORESTRY Pub Date : 2024-09-05 DOI: 10.1016/j.dendro.2024.126256
J. Julio Camarero , Antonio Gazol , Elisa Tamudo , Pavel A. Moiseev , Michele Colangelo , Cristina Valeriano

Many treeline and shrublines are not responding to climate warming as fast as expected. This lack of responsiveness could be explained by other non-thermal, climate drivers operating at the cold edge of distribution of trees and shrubs. To determine which are the main climate drivers of tree and shrub radial growth near the treeline we measured ring width and related it to climate variables (temperature, precipitation, snow depth) and vegetation greenness (NDVI, Normalized Different Vegetation Index). We compared two dwarf shrub (Vaccinium uliginosum, Dryas octopetala) and three tree species (Larix sibirica, Picea obovata, Pinus uncinata) sampled in three treeline sites: Polar or Northern Urals, Southern Urals, and Spanish Pyrenees. Dwarf shrubs presented lower first-order autocorrelation (AR1) than trees, excepting in the N. Urals site. In this site, V. uliginosum showed a negative growth trend, whereas this tendency was observed in P. obovata and P. uncinata trees from the S. Urals and Pyrenees sites, respectively. Shrub and tree growth indices correlated with NDVI at different months. Trees showed stronger and positive growth responses to warmer summer conditions and also negative responses to precipitation in the N. and S. Urals. The growth of D. octopetala in the Pyrenees was enhanced by prior-winter and current-spring precipitation showing a strong correlation with May snow depth (r = 0.66, p = 0.0006, period 1998−2020). Dwarf shrubs and trees coexisting near the treeline differently responded to regional climate variability. Our findings indicate a strong dependence of shrubs and trees on local (e.g., snow depth) and regional (e.g., growing-season air temperature) climate conditions, respectively.

许多林木线和灌木线对气候变暖的反应没有预期的那么快。在树木和灌木分布的寒冷边缘运行的其他非热气候驱动因素可以解释这种缺乏响应的现象。为了确定林木和灌木在林线附近径向生长的主要气候驱动因素,我们测量了林环宽度,并将其与气候变量(温度、降水、积雪深度)和植被绿度(归一化差异植被指数 NDVI)联系起来。我们比较了在三个树线地点采样的两种矮灌木(Vaccinium uliginosum、Dryas octopetala)和三种树种(Larix sibirica、Picea obovata、Pinus uncinata):极地或北乌拉尔山脉、南乌拉尔山脉和西班牙比利牛斯山脉。矮小灌木的一阶自相关性(AR1)低于乔木,乌拉尔北部地区除外。在该地,V. uliginosum呈现负增长趋势,而在乌拉尔南部和比利牛斯地区,P. obovata和P. uncinata树木也分别呈现负增长趋势。灌木和树木的生长指数与不同月份的归一化差异植被指数相关。在乌拉尔北部和南部,树木对较暖的夏季条件表现出较强的正生长反应,而对降水则表现出负生长反应。比利牛斯山脉的八爪金龙(D. octopetala)的生长受前冬和今春降水的影响,与五月积雪深度有很强的相关性(r = 0.66,p = 0.0006,1998-2020 年)。在林线附近共存的矮小灌木和乔木对区域气候变化的反应不同。我们的研究结果表明,灌木和乔木分别对当地气候条件(如积雪深度)和区域气候条件(如生长季气温)具有很强的依赖性。
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引用次数: 0
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Dendrochronologia
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