The Features of Floristic Composition and Community Structure of the Birch Forests in the Forest-to-Bog Ecotones in the South of the Vasyugan Plain

The present study addresses the floristic composition and ecological and community structure of paludified birch forests (peat depth reaching 30 cm) in the southern taiga. The growing conditions were evaluated based on the indicator values of plants and soil chemical properties. The study plots were...

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Main Authors: Nina V. Klimova, Natalia A. Chernova, Art’em N. Nikiforov, Anatoliy G. Dyukarev
Format: Article
Language:English
Published: Siberian Federal University 2020-03-01
Series:Журнал Сибирского федерального университета: Серия Биология
Subjects:
Online Access:http://elib.sfu-kras.ru/bitstream/2311/135170/1/03_Klimova.pdf
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author Nina V. Klimova
Natalia A. Chernova
Art’em N. Nikiforov
Anatoliy G. Dyukarev
author_facet Nina V. Klimova
Natalia A. Chernova
Art’em N. Nikiforov
Anatoliy G. Dyukarev
author_sort Nina V. Klimova
collection DOAJ
description The present study addresses the floristic composition and ecological and community structure of paludified birch forests (peat depth reaching 30 cm) in the southern taiga. The growing conditions were evaluated based on the indicator values of plants and soil chemical properties. The study plots were located on transects directed from upland forests through peripheral wetland forests to bogs, which are situated in topographic lows, at the North-East edge of the Great Vasyugan mire. The sites of the forest-to-bog ecotone that are transformed to various degrees by the bog water regime are considered as successive stages of paludification. Because of the high carbonate content of the soil-forming rocks dominated by heavy clay particles and waterlogging by ground-mire waters, wet green forests without a developed moss cover form here on rich peat-humus soils at the initial stages of hydromorphic transformation of the plant community. This is in contrast to typical plant successions, which develop on carbonate-free sediments and whose development is associated with the effect of acid bog waters. Reed grass (Calamagrostis phragmitoides C. Hartman) dominates the ground vegetation, which also includes sedges (Carex canescens L., C. vaginata Tausch., C. disperma Dew.). The high contents of mineral nutrients in organics-accumulating dark humus soils determines the high floristic diversity of paludified birch forests, comparable with the diversity of upland communities. A significant part of the ground cover of these forests (25% of the species composition, up to 50% of the projective cover) is represented by nutrient-demanding forest- and meadow-swamp plant species, which commonly occur in eutrophic boreal forested swamps of West Siberia with groundwater input. These species are absent in the mesotrophic paludified taiga forests. At a later stage of hydromorphic transformation, pine-birch shrub-moss forests form on peat-humus-gley and peat-gley soils. As the nutrient availability of soils declines, the number of plant species decreases, and plant species with lower nutrient requirements begin to predominate. This leads to the ecological restructuring of wet communities and makes them similar to paludified forests on carbonate-free sediments; peat accumulation begins with the deposition of mesotrophic peat. Thus, a more substantial change occurs in the ecological structure of plant communities on high-carbonate clays during their hydromorphic transformation compared to the typical mesotrophic paludification of dark-coniferous forests on loams
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spelling doaj.art-903df0f8257a4e8589d825903135d26a2022-12-21T22:32:06ZengSiberian Federal UniversityЖурнал Сибирского федерального университета: Серия Биология1997-13892313-55302020-03-01131254310.17516/1997-1389-0314http://elib.sfu-kras.ru/handle/2311/135170The Features of Floristic Composition and Community Structure of the Birch Forests in the Forest-to-Bog Ecotones in the South of the Vasyugan PlainNina V. Klimova0Natalia A. Chernova1Art’em N. Nikiforov2Anatoliy G. Dyukarev3Institute of Monitoring of Climatic and Ecological Systems SB RAS Tomsk, Russian FederationInstitute of Monitoring of Climatic and Ecological Systems SB RAS Tomsk, Russian FederationInstitute of Monitoring of Climatic and Ecological Systems SB RAS Tomsk, Russian FederationInstitute of Monitoring of Climatic and Ecological Systems SB RAS Tomsk, Russian FederationThe present study addresses the floristic composition and ecological and community structure of paludified birch forests (peat depth reaching 30 cm) in the southern taiga. The growing conditions were evaluated based on the indicator values of plants and soil chemical properties. The study plots were located on transects directed from upland forests through peripheral wetland forests to bogs, which are situated in topographic lows, at the North-East edge of the Great Vasyugan mire. The sites of the forest-to-bog ecotone that are transformed to various degrees by the bog water regime are considered as successive stages of paludification. Because of the high carbonate content of the soil-forming rocks dominated by heavy clay particles and waterlogging by ground-mire waters, wet green forests without a developed moss cover form here on rich peat-humus soils at the initial stages of hydromorphic transformation of the plant community. This is in contrast to typical plant successions, which develop on carbonate-free sediments and whose development is associated with the effect of acid bog waters. Reed grass (Calamagrostis phragmitoides C. Hartman) dominates the ground vegetation, which also includes sedges (Carex canescens L., C. vaginata Tausch., C. disperma Dew.). The high contents of mineral nutrients in organics-accumulating dark humus soils determines the high floristic diversity of paludified birch forests, comparable with the diversity of upland communities. A significant part of the ground cover of these forests (25% of the species composition, up to 50% of the projective cover) is represented by nutrient-demanding forest- and meadow-swamp plant species, which commonly occur in eutrophic boreal forested swamps of West Siberia with groundwater input. These species are absent in the mesotrophic paludified taiga forests. At a later stage of hydromorphic transformation, pine-birch shrub-moss forests form on peat-humus-gley and peat-gley soils. As the nutrient availability of soils declines, the number of plant species decreases, and plant species with lower nutrient requirements begin to predominate. This leads to the ecological restructuring of wet communities and makes them similar to paludified forests on carbonate-free sediments; peat accumulation begins with the deposition of mesotrophic peat. Thus, a more substantial change occurs in the ecological structure of plant communities on high-carbonate clays during their hydromorphic transformation compared to the typical mesotrophic paludification of dark-coniferous forests on loamshttp://elib.sfu-kras.ru/bitstream/2311/135170/1/03_Klimova.pdfpaludified forestsforest-to-bog ecotonesfloristic diversityecological structurecommunity structureindicator values of plantsphyto-indicationwest siberia
spellingShingle Nina V. Klimova
Natalia A. Chernova
Art’em N. Nikiforov
Anatoliy G. Dyukarev
The Features of Floristic Composition and Community Structure of the Birch Forests in the Forest-to-Bog Ecotones in the South of the Vasyugan Plain
Журнал Сибирского федерального университета: Серия Биология
paludified forests
forest-to-bog ecotones
floristic diversity
ecological structure
community structure
indicator values of plants
phyto-indication
west siberia
title The Features of Floristic Composition and Community Structure of the Birch Forests in the Forest-to-Bog Ecotones in the South of the Vasyugan Plain
title_full The Features of Floristic Composition and Community Structure of the Birch Forests in the Forest-to-Bog Ecotones in the South of the Vasyugan Plain
title_fullStr The Features of Floristic Composition and Community Structure of the Birch Forests in the Forest-to-Bog Ecotones in the South of the Vasyugan Plain
title_full_unstemmed The Features of Floristic Composition and Community Structure of the Birch Forests in the Forest-to-Bog Ecotones in the South of the Vasyugan Plain
title_short The Features of Floristic Composition and Community Structure of the Birch Forests in the Forest-to-Bog Ecotones in the South of the Vasyugan Plain
title_sort features of floristic composition and community structure of the birch forests in the forest to bog ecotones in the south of the vasyugan plain
topic paludified forests
forest-to-bog ecotones
floristic diversity
ecological structure
community structure
indicator values of plants
phyto-indication
west siberia
url http://elib.sfu-kras.ru/bitstream/2311/135170/1/03_Klimova.pdf
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