Wood anatomy chronologies of Scots pine in the foothills of the Western Sayan (Siberia)

Recent methodological advances in quantitative wood anatomy have provided new insights into the climatic responses of radial growth at the scale of cell structure of tree rings. This study considered long-term chronologies of tracheid measurements, indexed by a novel approach to separate their speci...

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Published inJournal of forestry research Vol. 35; no. 1; p. 45
Main Authors Babushkina, Elena A., Dergunov, Dmitry R., Zharkov, Mikhail S., Belokopytova, Liliana V., Zhirnova, Dina F., Yang, Bao, Liu, Jingjing, Peng, Xiaomei, Vaganov, Eugene A.
Format Journal Article
LanguageEnglish
Published Singapore Springer Nature Singapore 01.12.2024
Springer Nature B.V
Department of Dendroecology,V.N.Sukachev Institute of Forest,Siberian Branch of the Russian Academy of Science,Krasnoyarsk 660036,Russia
Institute of Ecology and Geography,Siberian Federal University,Krasnoyarsk 660036,Russia%Institute of Ecology and Geography,Siberian Federal University,Krasnoyarsk 660036,Russia%Mathematical Methods and IT Department,Siberian Federal University,Krasnoyarsk 660036,Russia%Key Laboratory of Desert and Desertification,Northwest Institute of Eco-Environment and Resources,Chinese Academy of Sciences,Lanzhou 730000,People's Republic of China
Khakass Technical Institute,Siberian Federal University,Abakan 655017,Russia
School of Geographic and Oceanographic Sciences,Nanjing University,Nanjing 210093,People's Republic of China%Key Laboratory of Desert and Desertification,Northwest Institute of Eco-Environment and Resources,Chinese Academy of Sciences,Lanzhou 730000,People's Republic of China%Institute of Ecology and Geography,Siberian Federal University,Krasnoyarsk 660036,Russia
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Abstract Recent methodological advances in quantitative wood anatomy have provided new insights into the climatic responses of radial growth at the scale of cell structure of tree rings. This study considered long-term chronologies of tracheid measurements, indexed by a novel approach to separate their specific climatic responses from signal recorded in cell production (closely reflected in tree-ring width). To fill gaps in understanding the impact of climate on conifer xylem structure, Scots pine ( Pinus sylvestris L.) trees > 200 years old were selected within the forest-steppe zone in southern Siberia. Such habitats undergo mild moisture deficits and the resulting climatic regulation of growth processes. Mean and maximum values of cell radial diameter and cell wall thickness were recorded for each tree ring. Despite a low level of climatogenic stress, components of cell chronologies independent of cambial activity were separated to obtain significant climatic signals revealing the timing of the specific stages of tracheid differentiation. Cell expansion lasted from mid-April to July and was impacted similarly to tree-ring width (stimulated by precipitation and stressed by heat), maximum cell size formed late June. A switch in the climatic responses of mean anatomical traits indicated transition to latewood in mid-July. Secondary wall deposition lasted until mid-September, suppressed by end of season temperatures. Generally, anatomical climatic responses were modulated by a less dry May and September compared with summer months.
AbstractList Recent methodological advances in quantitative wood anatomy have provided new insights into the climatic responses of radial growth at the scale of cell structure of tree rings. This study considered long-term chronologies of tracheid measurements, indexed by a novel approach to separate their specific climatic responses from signal recorded in cell production (closely reflected in tree-ring width). To fill gaps in understanding the impact of climate on conifer xylem structure, Scots pine (Pinus sylvestris L.) trees > 200 years old were selected within the forest-steppe zone in southern Siberia. Such habitats undergo mild moisture deficits and the resulting climatic regulation of growth processes. Mean and maximum values of cell radial diameter and cell wall thickness were recorded for each tree ring. Despite a low level of climatogenic stress, components of cell chronologies independent of cambial activity were separated to obtain significant climatic signals revealing the timing of the specific stages of tracheid differentiation. Cell expansion lasted from mid-April to July and was impacted similarly to tree-ring width (stimulated by precipitation and stressed by heat), maximum cell size formed late June. A switch in the climatic responses of mean anatomical traits indicated transition to latewood in mid-July. Secondary wall deposition lasted until mid-September, suppressed by end of season temperatures. Generally, anatomical climatic responses were modulated by a less dry May and September compared with summer months.
Recent methodological advances in quantitative wood anatomy have provided new insights into the climatic responses of radial growth at the scale of cell structure of tree rings. This study considered long-term chronologies of tracheid measurements, indexed by a novel approach to separate their specific climatic responses from signal recorded in cell production (closely reflected in tree-ring width). To fill gaps in understanding the impact of climate on conifer xylem structure, Scots pine ( Pinus sylvestris L.) trees > 200 years old were selected within the forest-steppe zone in southern Siberia. Such habitats undergo mild moisture deficits and the resulting climatic regulation of growth processes. Mean and maximum values of cell radial diameter and cell wall thickness were recorded for each tree ring. Despite a low level of climatogenic stress, components of cell chronologies independent of cambial activity were separated to obtain significant climatic signals revealing the timing of the specific stages of tracheid differentiation. Cell expansion lasted from mid-April to July and was impacted similarly to tree-ring width (stimulated by precipitation and stressed by heat), maximum cell size formed late June. A switch in the climatic responses of mean anatomical traits indicated transition to latewood in mid-July. Secondary wall deposition lasted until mid-September, suppressed by end of season temperatures. Generally, anatomical climatic responses were modulated by a less dry May and September compared with summer months.
Recent methodological advances in quantitative wood anatomy have provided new insights into the climatic responses of radial growth at the scale of cell structure of tree rings.This study considered long-term chronologies of tracheid measurements,indexed by a novel approach to separate their specific climatic responses from signal recorded in cell production(closely reflected in tree-ring width).To fill gaps in understanding the impact of climate on conifer xylem structure,Scots pine(Pinus sylvestris L.)trees>200 years old were selected within the forest-steppe zone in southern Siberia.Such habitats undergo mild mois-ture deficits and the resulting climatic regulation of growth processes.Mean and maximum values of cell radial diameter and cell wall thickness were recorded for each tree ring.Despite a low level of climatogenic stress,components of cell chronologies independent of cambial activity were sep-arated to obtain significant climatic signals revealing the timing of the specific stages of tracheid differentiation.Cell expansion lasted from mid-April to July and was impacted similarly to tree-ring width(stimulated by precipitation and stressed by heat),maximum cell size formed late June.A switch in the climatic responses of mean anatomical traits indicated transition to latewood in mid-July.Secondary wall deposition lasted until mid-September,suppressed by end of season temperatures.Generally,anatomical climatic responses were modulated by a less dry May and September compared with summer months.
ArticleNumber 45
Author Liu, Jingjing
Dergunov, Dmitry R.
Yang, Bao
Belokopytova, Liliana V.
Vaganov, Eugene A.
Babushkina, Elena A.
Zharkov, Mikhail S.
Peng, Xiaomei
Zhirnova, Dina F.
AuthorAffiliation Khakass Technical Institute,Siberian Federal University,Abakan 655017,Russia;Institute of Ecology and Geography,Siberian Federal University,Krasnoyarsk 660036,Russia%Institute of Ecology and Geography,Siberian Federal University,Krasnoyarsk 660036,Russia%Mathematical Methods and IT Department,Siberian Federal University,Krasnoyarsk 660036,Russia%Key Laboratory of Desert and Desertification,Northwest Institute of Eco-Environment and Resources,Chinese Academy of Sciences,Lanzhou 730000,People's Republic of China;School of Geographic and Oceanographic Sciences,Nanjing University,Nanjing 210093,People's Republic of China%Key Laboratory of Desert and Desertification,Northwest Institute of Eco-Environment and Resources,Chinese Academy of Sciences,Lanzhou 730000,People's Republic of China%Institute of Ecology and Geography,Siberian Federal University,Krasnoyarsk 660036,Russia;Department of Dendroecology,V.N.Sukachev Institute of Forest,Siberian Branch of the Russian Academy of Science,Krasnoy
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Keywords Quantitative wood anatomy
Cell radial size
Cell wall thickness
Climatic response
Pinus sylvestris
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Department of Dendroecology,V.N.Sukachev Institute of Forest,Siberian Branch of the Russian Academy of Science,Krasnoyarsk 660036,Russia
Institute of Ecology and Geography,Siberian Federal University,Krasnoyarsk 660036,Russia%Institute of Ecology and Geography,Siberian Federal University,Krasnoyarsk 660036,Russia%Mathematical Methods and IT Department,Siberian Federal University,Krasnoyarsk 660036,Russia%Key Laboratory of Desert and Desertification,Northwest Institute of Eco-Environment and Resources,Chinese Academy of Sciences,Lanzhou 730000,People's Republic of China
Khakass Technical Institute,Siberian Federal University,Abakan 655017,Russia
School of Geographic and Oceanographic Sciences,Nanjing University,Nanjing 210093,People's Republic of China%Key Laboratory of Desert and Desertification,Northwest Institute of Eco-Environment and Resources,Chinese Academy of Sciences,Lanzhou 730000,People's Republic of China%Institute of Ecology and Geography,Siberian Federal University,Krasnoyarsk 660036,Russia
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– name: Department of Dendroecology,V.N.Sukachev Institute of Forest,Siberian Branch of the Russian Academy of Science,Krasnoyarsk 660036,Russia
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Snippet Recent methodological advances in quantitative wood anatomy have provided new insights into the climatic responses of radial growth at the scale of cell...
SourceID wanfang
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StartPage 45
SubjectTerms Anatomy
Biomedical and Life Sciences
cambium
Cell differentiation
Cell size
Cell walls
climate
conifers
Cytology
Diameters
Evergreen trees
Foothills
forest steppe
Forestry
heat
latewood
Life Sciences
Original Paper
Pine
Pine trees
Pinus sylvestris
Plant anatomy
Siberia
Steppes
summer
tracheids
Tree rings
trees
Wall deposition
Wood
Xylem
Title Wood anatomy chronologies of Scots pine in the foothills of the Western Sayan (Siberia)
URI https://link.springer.com/article/10.1007/s11676-023-01692-5
https://www.proquest.com/docview/2924290530
https://www.proquest.com/docview/3153617121
https://d.wanfangdata.com.cn/periodical/lyyj202403002
Volume 35
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