Development of bog-like vegetation during terrestrialization of polyhumic lakes in north-eastern Poland is not accompanied by ecosystem ombrotrophication
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- 作者：Pawe? Pawlikowski (1)
Ewelina Rutkowska (1)
Stanis?aw K?osowski (2)
Ewa Jab?ońska (1)
Danuta Drzymulska (3) - 关键词：Polyhumic lake ; Dystrophic lake ; Lake overgrowing ; Poor fen ; Bog ; Surface water chemistry
- 刊名：Hydrobiologia
- 出版年：2014
- 出版时间：October 2014
- 年：2014
- 卷：737
- 期：1
- 页码：87-95
- 全文大小：374 KB
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Ewelina Rutkowska (1)
Stanis?aw K?osowski (2)
Ewa Jab?ońska (1)
Danuta Drzymulska (3)
1. Department of Plant Ecology and Environmental Conservation, Institute of Botany, Faculty of Biology, University of Warsaw, Biological and Chemical Research Centre, ul. ?wirki i Wigury 101, 02-089, Warsaw, Poland
2. Department of Environmental Protection and Modelling, The Jan Kochanowski University, ul. ?wi?tokrzyska 15, 25-406, Kielce, Poland
3. Department of Botany, Institute of Biology, University of Bia?ystok, ?wierkowa 20b, 15-950, Bia?ystok, Poland - ISSN：1573-5117
文摘
The aim of the present study was to use the analysis of surface water chemistry to understand vegetation succession pathways in terrestrializing polyhumic lakes. We hypothesized that Sphagnum mire development was accompanied by a decrease in the mineral content in water. A total of 111 vegetation plots along 23 transects were analysed in 11 lakes and adjacent peat lands in the Wigry National Park (NE Poland). The vegetation of the lake-mire systems forms distinct zones: (1) nymphaeid-, bladderwort- and bryophyte-dominated aquatic vegetation; (2) sedge-dominated edge of the Sphagnumcarpet; (3) quaking, extremely poor fen with various Cyperaceae; (4) non-quaking, Eriophorum vaginatum-dominated bog-like vegetation and (5) pine woodland. Surface water corrected conductivity (ECcorr.), pH, COD-KMnO4 and Ca2+, Mg2+, Fetot. and SiO2 were measured along the transects. The environmental gradients best explaining the observed pattern were pH (with the highest values in the lake and the lowest in the bog-like vegetation) and COD-KMnO4 (showing an inverse direction). At least in some Sphagnum-mires conditions were more minerotrophic than in the lakes. The process of humic lake overgrowing by Sphagnum-mires in NE Poland results in pine woodlands on mineralised peat. The climate conditions in NE Poland, combined with evapotranspiration accelerated by encroaching trees, do not seem to support the development of ombrotrophic bogs.