Charophytes in the estuarine Curonian Lagoon: Have the changes in diversity, abundance and distribution occurred since the late 1940s?

The results of the recent (2014-2015) inventory and three historical datasets (1949-1959, 1960-1980 and 1997-2007) were analyzed in order to track the long-term changes of charophytes in the largest estuarine lagoon of the Baltic Sea. The present species composition of charophytes in the estuarine p...

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Bibliographic Details
Published in:Oceanological and hydrobiological studies Vol. 46; no. 2; pp. 186 - 198
Main Authors: Sinkevicene, Z, Bucas, M, Ilgine, R, Vaiciute, D, Katarzyte, M, Petkuviene, J
Format: Journal Article
Language:English
Published: Berlin De Gruyter 01-06-2017
Walter de Gruyter GmbH
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Summary:The results of the recent (2014-2015) inventory and three historical datasets (1949-1959, 1960-1980 and 1997-2007) were analyzed in order to track the long-term changes of charophytes in the largest estuarine lagoon of the Baltic Sea. The present species composition of charophytes in the estuarine part of the Curonian Lagoon consisted of 7 species, including tolerant to salinity ( , , and ) and typical brackish-water species ( , and ). The highest congruence of species was between the 1997-2007 and 2014-2015 datasets, which covered respectively eutrophication and post-eutrophication periods. The 1949-1959 dataset (closest to the reference conditions) differed by the absence of typical brackish-water species. The 1960-1980 dataset (the major period of eutrophication) was relatively poor in study sites and species. During the last 6 decades, only tolerant to salinity freshwater species were constant and abundant; only can be considered as extinct. Recently, became dominant and widespread. The changes in the charophyte species composition, abundance and distribution can be explained by different intensity of surveys and/or density of study sites, but also by the increased exposure to brackish waters since 1980s and/or recently reduced effect of eutrophication.
ISSN:1897-3191
1730-413X
1897-3191
DOI:10.1515/ohs-2017-0019