Peculiarities of forming and functioning of Siberian stone pine forests of Altai
Our long-term (more than 20 years) studies of Altai forests formed by Siberian stone pine (Pinus sibirica du Tour) allowed us to fetch out many pecularities of forming of these forests and their functioning. The representativeness of the Aktru mountain glacier basin by hydroglacioclimatologic showin...
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ftzenodo:oai:zenodo.org:7142226 2024-09-15T18:39:56+00:00 Peculiarities of forming and functioning of Siberian stone pine forests of Altai Timoshok Eugeny Timoshok Elena Raiskaia Yulia 2022-10-04 https://doi.org/10.5281/zenodo.7142226 rus rus Zenodo https://doi.org/10.5281/zenodo.7142225 https://doi.org/10.5281/zenodo.7142226 oai:zenodo.org:7142226 info:eu-repo/semantics/openAccess Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode Siberian stone pine forests primary successions secondary succession cyclic succession Altai info:eu-repo/semantics/article 2022 ftzenodo https://doi.org/10.5281/zenodo.714222610.5281/zenodo.7142225 2024-07-25T13:06:00Z Our long-term (more than 20 years) studies of Altai forests formed by Siberian stone pine (Pinus sibirica du Tour) allowed us to fetch out many pecularities of forming of these forests and their functioning. The representativeness of the Aktru mountain glacier basin by hydroglacioclimatologic showings (Tronov, 1973) allowed us to assume the general trends and tendencies are common for the Altai, though influ - ence of local factors still define the details (Timoshok et al., 2008). We found almost all successions in mountain glacier basin Aktru is directed to the forming of Siberian stone forests. This forming may be direct, like transformation of tundra to stone pine forest during raising of treeline and forest line or during post-fire secondary succession in the larch forests of the Aktru river valley (Timoshok, 2020a) or be indirect as during primary successions at Malyi Aktru glacier forelands and gla- cionfluvial deposits of the Aktru river (Timoshok, 2020b,c). This common direction allow us to assume the si- berian stone pine forests serve as kind of attractor, similar to F. Clements conception of ecosystem climax. Signs of similar changes in the past was confirmed by the data of spore and pollen analysis (Blyakharchuk T.A. et al., 2004). The analysis also confirms that changes of Altai forest composition occurred in the past: Siberian stone pine forest were much more common than now in the humid periods with lower impact of fire distur- bances while larch was as common as now in dryer periods. Siberian stone pine forests have high stability because of longevity of Pinus sibirica and its ability to pro- duce cones and seeds until the moment of physical death of the stone pine individual. Their stability is proven by the fact these forests survived Little Ice Age without significant changes (Timoshok at al., 2016). These for- ests have complex mosaics of forest types. Each element of mosaic exist in its own cyclic succession. These elements of the forest changed when trees become older and die, but new Stone ... Article in Journal/Newspaper Tundra Zenodo |
institution |
Open Polar |
collection |
Zenodo |
op_collection_id |
ftzenodo |
language |
Russian |
topic |
Siberian stone pine forests primary successions secondary succession cyclic succession Altai |
spellingShingle |
Siberian stone pine forests primary successions secondary succession cyclic succession Altai Timoshok Eugeny Timoshok Elena Raiskaia Yulia Peculiarities of forming and functioning of Siberian stone pine forests of Altai |
topic_facet |
Siberian stone pine forests primary successions secondary succession cyclic succession Altai |
description |
Our long-term (more than 20 years) studies of Altai forests formed by Siberian stone pine (Pinus sibirica du Tour) allowed us to fetch out many pecularities of forming of these forests and their functioning. The representativeness of the Aktru mountain glacier basin by hydroglacioclimatologic showings (Tronov, 1973) allowed us to assume the general trends and tendencies are common for the Altai, though influ - ence of local factors still define the details (Timoshok et al., 2008). We found almost all successions in mountain glacier basin Aktru is directed to the forming of Siberian stone forests. This forming may be direct, like transformation of tundra to stone pine forest during raising of treeline and forest line or during post-fire secondary succession in the larch forests of the Aktru river valley (Timoshok, 2020a) or be indirect as during primary successions at Malyi Aktru glacier forelands and gla- cionfluvial deposits of the Aktru river (Timoshok, 2020b,c). This common direction allow us to assume the si- berian stone pine forests serve as kind of attractor, similar to F. Clements conception of ecosystem climax. Signs of similar changes in the past was confirmed by the data of spore and pollen analysis (Blyakharchuk T.A. et al., 2004). The analysis also confirms that changes of Altai forest composition occurred in the past: Siberian stone pine forest were much more common than now in the humid periods with lower impact of fire distur- bances while larch was as common as now in dryer periods. Siberian stone pine forests have high stability because of longevity of Pinus sibirica and its ability to pro- duce cones and seeds until the moment of physical death of the stone pine individual. Their stability is proven by the fact these forests survived Little Ice Age without significant changes (Timoshok at al., 2016). These for- ests have complex mosaics of forest types. Each element of mosaic exist in its own cyclic succession. These elements of the forest changed when trees become older and die, but new Stone ... |
format |
Article in Journal/Newspaper |
author |
Timoshok Eugeny Timoshok Elena Raiskaia Yulia |
author_facet |
Timoshok Eugeny Timoshok Elena Raiskaia Yulia |
author_sort |
Timoshok Eugeny |
title |
Peculiarities of forming and functioning of Siberian stone pine forests of Altai |
title_short |
Peculiarities of forming and functioning of Siberian stone pine forests of Altai |
title_full |
Peculiarities of forming and functioning of Siberian stone pine forests of Altai |
title_fullStr |
Peculiarities of forming and functioning of Siberian stone pine forests of Altai |
title_full_unstemmed |
Peculiarities of forming and functioning of Siberian stone pine forests of Altai |
title_sort |
peculiarities of forming and functioning of siberian stone pine forests of altai |
publisher |
Zenodo |
publishDate |
2022 |
url |
https://doi.org/10.5281/zenodo.7142226 |
genre |
Tundra |
genre_facet |
Tundra |
op_relation |
https://doi.org/10.5281/zenodo.7142225 https://doi.org/10.5281/zenodo.7142226 oai:zenodo.org:7142226 |
op_rights |
info:eu-repo/semantics/openAccess Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode |
op_doi |
https://doi.org/10.5281/zenodo.714222610.5281/zenodo.7142225 |
_version_ |
1810484276283572224 |