Peculiarities of macrozoobenthos structure formation in riffles of the Karelian coast of the White sea

Species composition, abundance and biomass of macrozoobenthos were investigated in the riffles of the Karelian coast of the White Sea. The longitudinal dynamics of benthic communities’ structure is weak due to the stony-bottomed riffles almost throughout the rivers. Local factors can cause significa...

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Format: Article
Language:English
Published: Karelian Research Centre of the Russian Academy of Sciences 2015-02-01
Series:Transactions of the Karelian Research Centre of the Russian Academy of Sciences
Subjects:
Online Access:http://journals.krc.karelia.ru/index.php/ecology/article/view/89
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collection DOAJ
description Species composition, abundance and biomass of macrozoobenthos were investigated in the riffles of the Karelian coast of the White Sea. The longitudinal dynamics of benthic communities’ structure is weak due to the stony-bottomed riffles almost throughout the rivers. Local factors can cause significant changes in the structure of macrozoobenthos. Thus, the communities with high level of filter-feeders biomass (net-weaving caddis fly larvae, the midge larvae, bivalves) are formed in the river sites downstream from the drainage lakes. In the areas affected by salty sea waters (parts of the river mouth), macrozoobenthos structure is significantly depleted. Local landscape features should be considered when describing the longitudinal changes in macrozoobenthos structure of rivers.
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spelling doaj.art-732fa3558e57491f91498ecc8668ecd62022-12-22T02:37:31ZengKarelian Research Centre of the Russian Academy of SciencesTransactions of the Karelian Research Centre of the Russian Academy of Sciences1997-32172312-45042015-02-011293610.17076/eco3621Peculiarities of macrozoobenthos structure formation in riffles of the Karelian coast of the White seaSpecies composition, abundance and biomass of macrozoobenthos were investigated in the riffles of the Karelian coast of the White Sea. The longitudinal dynamics of benthic communities’ structure is weak due to the stony-bottomed riffles almost throughout the rivers. Local factors can cause significant changes in the structure of macrozoobenthos. Thus, the communities with high level of filter-feeders biomass (net-weaving caddis fly larvae, the midge larvae, bivalves) are formed in the river sites downstream from the drainage lakes. In the areas affected by salty sea waters (parts of the river mouth), macrozoobenthos structure is significantly depleted. Local landscape features should be considered when describing the longitudinal changes in macrozoobenthos structure of rivers.http://journals.krc.karelia.ru/index.php/ecology/article/view/89benthosmacrozoobenthosbottom communitiesstructureriversthe white seakarelian coast
spellingShingle Peculiarities of macrozoobenthos structure formation in riffles of the Karelian coast of the White sea
Transactions of the Karelian Research Centre of the Russian Academy of Sciences
benthos
macrozoobenthos
bottom communities
structure
rivers
the white sea
karelian coast
title Peculiarities of macrozoobenthos structure formation in riffles of the Karelian coast of the White sea
title_full Peculiarities of macrozoobenthos structure formation in riffles of the Karelian coast of the White sea
title_fullStr Peculiarities of macrozoobenthos structure formation in riffles of the Karelian coast of the White sea
title_full_unstemmed Peculiarities of macrozoobenthos structure formation in riffles of the Karelian coast of the White sea
title_short Peculiarities of macrozoobenthos structure formation in riffles of the Karelian coast of the White sea
title_sort peculiarities of macrozoobenthos structure formation in riffles of the karelian coast of the white sea
topic benthos
macrozoobenthos
bottom communities
structure
rivers
the white sea
karelian coast
url http://journals.krc.karelia.ru/index.php/ecology/article/view/89