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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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. |
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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 |
AuthorAffiliation_xml | – name: 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,Krasnoyarsk 660036,Russia |
Author_xml | – sequence: 1 givenname: Elena A. surname: Babushkina fullname: Babushkina, Elena A. organization: Khakass Technical Institute, Siberian Federal University, Institute of Ecology and Geography, Siberian Federal University – sequence: 2 givenname: Dmitry R. surname: Dergunov fullname: Dergunov, Dmitry R. organization: Institute of Ecology and Geography, Siberian Federal University – sequence: 3 givenname: Mikhail S. orcidid: 0000-0003-0522-1892 surname: Zharkov fullname: Zharkov, Mikhail S. organization: Mathematical Methods and IT Department, Siberian Federal University – sequence: 4 givenname: Liliana V. surname: Belokopytova fullname: Belokopytova, Liliana V. email: white-lili@mail.ru organization: Khakass Technical Institute, Siberian Federal University, Institute of Ecology and Geography, Siberian Federal University – sequence: 5 givenname: Dina F. surname: Zhirnova fullname: Zhirnova, Dina F. organization: Khakass Technical Institute, Siberian Federal University, Institute of Ecology and Geography, Siberian Federal University – sequence: 6 givenname: Bao surname: Yang fullname: Yang, Bao organization: Key Laboratory of Desert and Desertification, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, School of Geographic and Oceanographic Sciences, Nanjing University – sequence: 7 givenname: Jingjing surname: Liu fullname: Liu, Jingjing organization: Key Laboratory of Desert and Desertification, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences – sequence: 8 givenname: Xiaomei surname: Peng fullname: Peng, Xiaomei organization: Key Laboratory of Desert and Desertification, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences – sequence: 9 givenname: Eugene A. surname: Vaganov fullname: Vaganov, Eugene A. organization: Institute of Ecology and Geography, Siberian Federal University, Department of Dendroecology, V.N. Sukachev Institute of Forest, Siberian Branch of the Russian Academy of Science |
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Keywords | Quantitative wood anatomy Cell radial size Cell wall thickness Climatic response Pinus sylvestris |
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PublicationTitle | Journal of forestry research |
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Publisher | Springer Nature Singapore 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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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) |
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