

Author: Bosiacka Beata Podlasinski Marek Pienkowski Paweł
Publisher: E. Schweizerbart'sche Verlagsbuchhandlung
ISSN: 0340-269X
Source: Phytocoenologia, Vol.41, Iss.3, 2011-12, pp. : 201-213
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Abstract
Most of the European salt and brackish marshes are linked to sea water ingression. Inland salt marshes supplied with saline subterranean waters are more uncommon. In Poland due to the natural factors limiting the development of coastal salt marshes, they are dispersed and cover a surface comparable to inland saline habitats. Two halophilous vegetation sites located at the coastal zone but determined mainly by ascension of relic Mesozoic saline waters have a unique status. The aim of the study was to provide a characteristic of these sites including land-use changes during 1925–2005, physicochemical soil and ground water properties, relations between habitat conditions and species composition, differentiation and qualities of halophilous vegetation and environmental protection prospects. It was shown that a development of drainage network in the Parsęta Valley and Chrząszczewska Island as well as urban infrastructure affected the first site leading to reduction of the wetlands (mainly salt marshes) by 44% and 29%, respectively. The cessation or reduction of traditional salt grassland-use in 1980s led to further decrease in salt meadow area. Primarily, soil and ground water salinity (almost four times higher than in the local Baltic Sea water) determined species and habitat differentiation.
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