Morphological forms of Siberian Stone Pine (Pinus sibirica Du Tour) Trees in High Altitudinal Forests of the Severo-Chuisky Range. Dendrochronological Aspect

At the upper forest belt in the primary Siberian stone pine–Siberian larch forests in the headwater Aktru, Severo-Chuisky Range, the Altai Mountains, Russia the qualitative analysis of tree and branch radial increment was made in the main growth form (upright–trunk tree) of Siberian stone pine (Pinu...

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Main Authors: Svetlana А. Nikolaeva, Dmitry А. Savchuk
Format: Article
Language:English
Published: Siberian Federal University 2015-12-01
Series:Журнал Сибирского федерального университета: Серия Биология
Subjects:
Online Access:http://elib.sfu-kras.ru/bitstream/2311/20001/1/06_Nikolaeva.pdf
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spelling doaj-44eb26dc8239452bb408213d8e38815e2020-11-25T01:20:32ZengSiberian Federal UniversityЖурнал Сибирского федерального университета: Серия Биология1997-13892313-55302015-12-0184459477http://elib.sfu-kras.ru/handle/2311/20001Morphological forms of Siberian Stone Pine (Pinus sibirica Du Tour) Trees in High Altitudinal Forests of the Severo-Chuisky Range. Dendrochronological AspectSvetlana А. Nikolaeva0Dmitry А. Savchuk1Institute of Monitoring of Climatic and Ecological Systems of the SB RAS 10/3 Academichesky, Tomsk, 634055, RussiaInstitute of Monitoring of Climatic and Ecological Systems of the SB RAS 10/3 Academichesky, Tomsk, 634055, RussiaAt the upper forest belt in the primary Siberian stone pine–Siberian larch forests in the headwater Aktru, Severo-Chuisky Range, the Altai Mountains, Russia the qualitative analysis of tree and branch radial increment was made in the main growth form (upright–trunk tree) of Siberian stone pine (Pinus sibirica Du Tour), its relatively autonomic structures (power candelabra branches and elfin wood form), and the transitional morphological (“living” stumps, “living” windfallen trees, shrub-like form, and trees with multi-storey root system) and other growth (clump-like trees) forms. The external (weather and climatic processes, geomorphological events, and phytocoenotic interactions) and the internal factors effect on initiation and existence of the morphological structures and the transitional morphological forms and their growth. The internal factors are 1) absolute and biological age of the trees, 2) primary or secondary origin of the branches, 3) degree of development of the roots, and 4) the connection between the morphological structures and the mother trunk and root. Under favourable growth conditions in the Siberian stone pine trees the form of the curve of the trunk increment is close to the bell with maximum increment in the earlier age when growth temp and acceleration are maximum in the sites. The forms of growth curves can be approximate the equations of the parabola or the exponential curves with the positive or negative accelerations as well as the horizon straight line when the growth curves become planehttp://elib.sfu-kras.ru/bitstream/2311/20001/1/06_Nikolaeva.pdfPinus sibiricaPinus sibiricamorphological formliving formradial incrementtree ringshigh elevationSevero-Chuisky RangeAltai Mountains
collection DOAJ
language English
format Article
sources DOAJ
author Svetlana А. Nikolaeva
Dmitry А. Savchuk
spellingShingle Svetlana А. Nikolaeva
Dmitry А. Savchuk
Morphological forms of Siberian Stone Pine (Pinus sibirica Du Tour) Trees in High Altitudinal Forests of the Severo-Chuisky Range. Dendrochronological Aspect
Журнал Сибирского федерального университета: Серия Биология
Pinus sibirica
Pinus sibirica
morphological form
living form
radial increment
tree rings
high elevation
Severo-Chuisky Range
Altai Mountains
author_facet Svetlana А. Nikolaeva
Dmitry А. Savchuk
author_sort Svetlana А. Nikolaeva
title Morphological forms of Siberian Stone Pine (Pinus sibirica Du Tour) Trees in High Altitudinal Forests of the Severo-Chuisky Range. Dendrochronological Aspect
title_short Morphological forms of Siberian Stone Pine (Pinus sibirica Du Tour) Trees in High Altitudinal Forests of the Severo-Chuisky Range. Dendrochronological Aspect
title_full Morphological forms of Siberian Stone Pine (Pinus sibirica Du Tour) Trees in High Altitudinal Forests of the Severo-Chuisky Range. Dendrochronological Aspect
title_fullStr Morphological forms of Siberian Stone Pine (Pinus sibirica Du Tour) Trees in High Altitudinal Forests of the Severo-Chuisky Range. Dendrochronological Aspect
title_full_unstemmed Morphological forms of Siberian Stone Pine (Pinus sibirica Du Tour) Trees in High Altitudinal Forests of the Severo-Chuisky Range. Dendrochronological Aspect
title_sort morphological forms of siberian stone pine (pinus sibirica du tour) trees in high altitudinal forests of the severo-chuisky range. dendrochronological aspect
publisher Siberian Federal University
series Журнал Сибирского федерального университета: Серия Биология
issn 1997-1389
2313-5530
publishDate 2015-12-01
description At the upper forest belt in the primary Siberian stone pine–Siberian larch forests in the headwater Aktru, Severo-Chuisky Range, the Altai Mountains, Russia the qualitative analysis of tree and branch radial increment was made in the main growth form (upright–trunk tree) of Siberian stone pine (Pinus sibirica Du Tour), its relatively autonomic structures (power candelabra branches and elfin wood form), and the transitional morphological (“living” stumps, “living” windfallen trees, shrub-like form, and trees with multi-storey root system) and other growth (clump-like trees) forms. The external (weather and climatic processes, geomorphological events, and phytocoenotic interactions) and the internal factors effect on initiation and existence of the morphological structures and the transitional morphological forms and their growth. The internal factors are 1) absolute and biological age of the trees, 2) primary or secondary origin of the branches, 3) degree of development of the roots, and 4) the connection between the morphological structures and the mother trunk and root. Under favourable growth conditions in the Siberian stone pine trees the form of the curve of the trunk increment is close to the bell with maximum increment in the earlier age when growth temp and acceleration are maximum in the sites. The forms of growth curves can be approximate the equations of the parabola or the exponential curves with the positive or negative accelerations as well as the horizon straight line when the growth curves become plane
topic Pinus sibirica
Pinus sibirica
morphological form
living form
radial increment
tree rings
high elevation
Severo-Chuisky Range
Altai Mountains
url http://elib.sfu-kras.ru/bitstream/2311/20001/1/06_Nikolaeva.pdf
work_keys_str_mv AT svetlanaanikolaeva morphologicalformsofsiberianstonepinepinussibiricadutourtreesinhighaltitudinalforestsoftheseverochuiskyrangedendrochronologicalaspect
AT dmitryasavchuk morphologicalformsofsiberianstonepinepinussibiricadutourtreesinhighaltitudinalforestsoftheseverochuiskyrangedendrochronologicalaspect
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