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1
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Changes in the structure of tree stands on bog habitats in the Bialowieza forest

100%
Czerepko J.
Folia Forestalia Polonica. Series A . Forestry
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2010
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tom 52
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nr 1
The analyses of 4 permanent study plots located in the Białowieża forest (NE Poland, at 52º43´ N, 23º50´ E) were carried out 4 times, first time in 1973 or 1974 and next in 1985, 1998, 2008. The paper presents the results of a long–term study on natural forest dynamics in two forest communities: raised-bog pine forest of the association Ledo-Sphagnetum magellanici Sukopp 1959 em. Neuhäusl 1969 and transitional bogs represented by the boreal spruce forest Sphagno girgensohnii-Piceetum Polak. 1962. On each measurement date the DBH of all trees were recognized. At the same time, stems of shrub species as well as tree species with the height lower than 1.3 m were counted within the experimental areas. During the study period the structure of stands changed significantly. The major change observed on raised bog sites was an increase in numbers of Betula spp., Picea abies (L.) H. Karst. and Quercus robur L. After 34th-year of observations the boreal spruce forest stand partly passed the terminal phase and regenerated. New species occurred in the stands, especially in their lower layer, are typical for oak-lime-hornbeam forest, such as e.g. Carpinus betulus L., Q. robur, Acer platanoides L. Rapid development of Corylus avellana L. was also observed. During last decades, the decrease in the number of Pinus sylvestris L. trees has been observed. The results of analyses of stand data in four research periods show that the wetland habitat of the Białowieża forest has been a subject to the processes of succession conditioned by environmental changes such as desiccation through lowering of the water table as well as climatic changes entailing inter alia an increase of the air temperature and a decrease of precipitation.
2

The Pinus rotundata Link bog forests on mined peat bogs - is the conservation of undisturbed edge an effective tool for its protection?

100%
Unar P., Janik D., Soucek J., Vrska T., Adam D., Kral K., Hort L.
Polish Journal of Ecology
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2012
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tom 60
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nr 4
Peat mining has a serious impact on the Pinus rotundata Link habitat. The possibility of sustaining a vital Pinus rotundata bog forest on undisturbed edges of mined peat bog was assessed. 28.7 ha of undisturbed edge of Borkovicka blata peat bog were sampled by regular grid of circular sample plots. Data about tree layer, natural regeneration of woody species as well as herb layer were collected. The impact of mined area drainage on vegetation communities in the undisturbed edge of peat bogs was discovered. The original Pinus rotundata bog forest is getting older and it is gradually being replaced by forest stands dominated by Picea abies (L.) Karsten, Betula pendula Roth and B. pubescens Ehrh. The character of vegetation changes more rapidly with the increasing vertical distance of the remaining fragment and the mined part. This secondary elevation represents a serious problem in the water regime restoration and consequent revitalisation of the Pinus rotundata bog forest on the undisturbed edge of the mined peat bog.
3

Invasion of raised bogs by the Scots pine; a review of vegetation history and case study in selected peat-bogs in Bieszczady Mts. (Eastern Carpathians)

80%
Koczur A., Michalik S.
Polish Journal of Ecology
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2015
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tom 63
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nr 3
The objective of this study was to analyse the diversity of pine and spruce bog forests on the domes of Carpathian raised bogs located in the Upper San River Valley. In order to determine the present species composition, 59 phytosociological relevés were performed (32 within spruce forests, and 27 in pine forests). For all relevés, the Shannon-Wiener index, evenness index and mean Ellenberg indicator values were calculated. Detrended correspondence analysis was conducted in order to determine the degree of similarity between distinct units of vegetation and to identify the main environmental gradients that have an impact on species composition. The results revealed considerable similarities between the ground vegetation of both spruce and pine forests growing on peat substrate. Within pine forests there was a greater proportion of certain plant species characteristic of raised bogs, and plants typical of bog coniferous forests. The ground flora of spruce forests was more diverse. Although spruce forests predominantly contained species typical of raised bogs, there was also a group in which Molinia caerulea predominated. Ellenberg indicator values typical of pine forests lay within ranges that were characteristic of spruce forests, but pine forests occupy more humid, more acidic and poorer habitats than most patches of spruce forests. Both spruce and pine bog forests were developed as a result of the colonization of open bogs, but the time-scale and rate of intensity were different. Palaeobotanical and historical data indicate that the Scots pine first reappeared on the domes of raised bogs in the first half of the 20th century. The concept that the spruce forests are older than those of pine is supported by their greater habitat diversity. Conversely, the younger age of pine forests is confirmed by their low habitat diversity, and greater proportion of photophilous raised-bog species.
4
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Influence of the bog soil chemical properties on the floral composition of microcenoses in bog forests of the Stare Biele Reserve in the Knyszyn Forest

80%
Czubaszek R.
Acta Agrophysica
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2001
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tom 50
Studies considering hummocks and hollows structure of bog forests were carried out in the Stare Biele Reserve in the Knyszyn Forest. The aim of the study was better recognition of bog forests spatial structure including recognition of soil chemical composition of hummocks and hollows. The bog forest communities in Stare Biele Reserve have various percentage of hummocks. The hummocks have similar morphological structure and are distinctly separated from hollows in all four bog forest communities. Degree of hummocks development and their morphological structure have big impact on plant distribution on their surface. Soil chemical properties are one of the factors, which influence floral abundance and composition of microcenoses. Soil reaction and calcium content, among other measured properties, exert the biggest influence on the floral abundance and composition of microcenoses.
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