Status of the zooplankton in the central Syvash Bay in the summer season of 2019

The Syvash Bay is located in the Western Azov Sea and is separated from it by the Arabat Spit. After the channel was shut off in 2014, the water salinity in the bay gradually increased, which leads to the changes in the Syvash biota. During the desalinization period, the bay served as an important spawning and feeding ground for the juveniles of the Azov Sea fish species that mainly feed on zooplankton. The increase in salinity has inevitably influenced its state. It is shown that the highest indices of zooplankton development have been recorded in the northern part, the most desalinated one, and the lowest values have been observed in the southern part, characterized by the highest salinity. That said, in the northern part of the bay, zooplankton abundance was 1.2–1.4 and biomass was 2.7–2.9 times lower in July than in June. At the same time, in the southern part of the bay, characterized by the highest salinity, the average abundance of zooplankton in July was 2.1–4.4 times lower as compared to June, and for zooplankton biomass, this value was 1.5–4.1 times lower. Furthermore, rotifers and isopods were virtually absent in this area, and no nematodes and flatworms were recorded. The study has shown that, as the result of the further salinization, the Syvash Bay has the possibility to become a hypersaline water body again. In this case, the species richness of zooplankton will deteriorate considerably, and ultrasaline species will be prevalent in its species composition. This work was aimed at the investigation of the status of the zooplanktonic community in the summer season (June–July) of 2019.

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Bibliographic Details
Main Authors: Terentyev, A.S., Zaremba, N.B.
Format: Journal Contribution biblioteca
Language:Russian
Published: 2021
Subjects:Copepods, Salinization, Species composition, Abundance, Ultrasaline species, Biomass, Копеподы, Осолонение, Видовой состав, Ультрагалинные виды, Биомасса, ASFA_2015::Y::Zooplankton, ASFA_2015::E::Eutrophication, ASFA_2015::S::Salt lakes,
Online Access:http://hdl.handle.net/1834/41892
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spelling dig-aquadocs-1834-418922022-03-16T03:25:32Z Status of the zooplankton in the central Syvash Bay in the summer season of 2019 Состояние зоопланктона центральной части залива Сиваш в летний период 2019 г. Terentyev, A.S. Zaremba, N.B. Copepods Salinization Species composition Abundance Ultrasaline species Biomass Копеподы Осолонение Видовой состав Ультрагалинные виды Биомасса ASFA_2015::Y::Zooplankton ASFA_2015::E::Eutrophication ASFA_2015::S::Salt lakes The Syvash Bay is located in the Western Azov Sea and is separated from it by the Arabat Spit. After the channel was shut off in 2014, the water salinity in the bay gradually increased, which leads to the changes in the Syvash biota. During the desalinization period, the bay served as an important spawning and feeding ground for the juveniles of the Azov Sea fish species that mainly feed on zooplankton. The increase in salinity has inevitably influenced its state. It is shown that the highest indices of zooplankton development have been recorded in the northern part, the most desalinated one, and the lowest values have been observed in the southern part, characterized by the highest salinity. That said, in the northern part of the bay, zooplankton abundance was 1.2–1.4 and biomass was 2.7–2.9 times lower in July than in June. At the same time, in the southern part of the bay, characterized by the highest salinity, the average abundance of zooplankton in July was 2.1–4.4 times lower as compared to June, and for zooplankton biomass, this value was 1.5–4.1 times lower. Furthermore, rotifers and isopods were virtually absent in this area, and no nematodes and flatworms were recorded. The study has shown that, as the result of the further salinization, the Syvash Bay has the possibility to become a hypersaline water body again. In this case, the species richness of zooplankton will deteriorate considerably, and ultrasaline species will be prevalent in its species composition. This work was aimed at the investigation of the status of the zooplanktonic community in the summer season (June–July) of 2019. Залив Сиваш расположен в западной части Азовского моря и отделен от него косой Арабатская стрелка. Перекрытие канала в 2014 г. привело к повышению солености залива и изменению биоты Сиваша. В период распреснения залив являлся важным районом нереста и нагула молоди рыб Азовского моря, основным кормом для которых является зоопланктон. Повышение солености залива не могло не сказаться на его состоянии. Показано, что в северной, наиболее опресненной, части наблюдались наиболее высокие показатели уровня развития зоопланктона, а в южной, наиболее соленой, — низкие. При этом, в июле в северной части численность зоопланктона была в 1,2–1,4 раза, а биомасса в 2,7–2,9 раза меньше, чем в июне. В южной, наиболее соленой части, средняя численность зоопланктона в июле, по сравнению с июнем, уменьшилась в 2,1–4,4 раза, а биомасса — в 1,5–4,1 раза. Также здесь практически полностью отсутствовали коловратки и равноногие раки, не были отмечены нематоды и плоские черви. Результаты исследования показали, что при дальнейшем осолонении залив Сиваш может снова стать гипергалинным водоемом. В этом случае видовое богатство зоопланктона значительно сократится, а в его составе будут преобладать ультрагалинные виды. Целью данной работы было изучение состояния зоопланктонного сообщества в летний период (июнь–июль) 2019 г. Published Non Refereed 2022-03-15T09:00:05Z 2022-03-15T09:00:05Z 2021 Journal Contribution http://hdl.handle.net/1834/41892 ru Attribution-NonCommercial-NoDerivatives 4.0 International http://creativecommons.org/licenses/by-nc-nd/4.0/ pp.121-129 Sivash Lagoon Azov Sea Залив Сиваш Азовское море Arabat Spit Арабатская стрелка
institution UNESCO
collection DSpace
country Francia
countrycode FR
component Bibliográfico
access En linea
databasecode dig-aquadocs
tag biblioteca
region Europa del Oeste
libraryname Repositorio AQUADOCS
language Russian
topic Copepods
Salinization
Species composition
Abundance
Ultrasaline species
Biomass
Копеподы
Осолонение
Видовой состав
Ультрагалинные виды
Биомасса
ASFA_2015::Y::Zooplankton
ASFA_2015::E::Eutrophication
ASFA_2015::S::Salt lakes
Copepods
Salinization
Species composition
Abundance
Ultrasaline species
Biomass
Копеподы
Осолонение
Видовой состав
Ультрагалинные виды
Биомасса
ASFA_2015::Y::Zooplankton
ASFA_2015::E::Eutrophication
ASFA_2015::S::Salt lakes
spellingShingle Copepods
Salinization
Species composition
Abundance
Ultrasaline species
Biomass
Копеподы
Осолонение
Видовой состав
Ультрагалинные виды
Биомасса
ASFA_2015::Y::Zooplankton
ASFA_2015::E::Eutrophication
ASFA_2015::S::Salt lakes
Copepods
Salinization
Species composition
Abundance
Ultrasaline species
Biomass
Копеподы
Осолонение
Видовой состав
Ультрагалинные виды
Биомасса
ASFA_2015::Y::Zooplankton
ASFA_2015::E::Eutrophication
ASFA_2015::S::Salt lakes
Terentyev, A.S.
Zaremba, N.B.
Status of the zooplankton in the central Syvash Bay in the summer season of 2019
description The Syvash Bay is located in the Western Azov Sea and is separated from it by the Arabat Spit. After the channel was shut off in 2014, the water salinity in the bay gradually increased, which leads to the changes in the Syvash biota. During the desalinization period, the bay served as an important spawning and feeding ground for the juveniles of the Azov Sea fish species that mainly feed on zooplankton. The increase in salinity has inevitably influenced its state. It is shown that the highest indices of zooplankton development have been recorded in the northern part, the most desalinated one, and the lowest values have been observed in the southern part, characterized by the highest salinity. That said, in the northern part of the bay, zooplankton abundance was 1.2–1.4 and biomass was 2.7–2.9 times lower in July than in June. At the same time, in the southern part of the bay, characterized by the highest salinity, the average abundance of zooplankton in July was 2.1–4.4 times lower as compared to June, and for zooplankton biomass, this value was 1.5–4.1 times lower. Furthermore, rotifers and isopods were virtually absent in this area, and no nematodes and flatworms were recorded. The study has shown that, as the result of the further salinization, the Syvash Bay has the possibility to become a hypersaline water body again. In this case, the species richness of zooplankton will deteriorate considerably, and ultrasaline species will be prevalent in its species composition. This work was aimed at the investigation of the status of the zooplanktonic community in the summer season (June–July) of 2019.
format Journal Contribution
topic_facet Copepods
Salinization
Species composition
Abundance
Ultrasaline species
Biomass
Копеподы
Осолонение
Видовой состав
Ультрагалинные виды
Биомасса
ASFA_2015::Y::Zooplankton
ASFA_2015::E::Eutrophication
ASFA_2015::S::Salt lakes
author Terentyev, A.S.
Zaremba, N.B.
author_facet Terentyev, A.S.
Zaremba, N.B.
author_sort Terentyev, A.S.
title Status of the zooplankton in the central Syvash Bay in the summer season of 2019
title_short Status of the zooplankton in the central Syvash Bay in the summer season of 2019
title_full Status of the zooplankton in the central Syvash Bay in the summer season of 2019
title_fullStr Status of the zooplankton in the central Syvash Bay in the summer season of 2019
title_full_unstemmed Status of the zooplankton in the central Syvash Bay in the summer season of 2019
title_sort status of the zooplankton in the central syvash bay in the summer season of 2019
publishDate 2021
url http://hdl.handle.net/1834/41892
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AT zarembanb statusofthezooplanktoninthecentralsyvashbayinthesummerseasonof2019
AT terentyevas sostoâniezooplanktonacentralʹnojčastizalivasivašvletnijperiod2019g
AT zarembanb sostoâniezooplanktonacentralʹnojčastizalivasivašvletnijperiod2019g
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