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Changes in Diversity of Silica-Scaled Chrysophytes during Lake–River–Reservoir Transition (Baikal–Angara–Irkutsk Reservoir)

Hydroelectric dams create new ecosystems such as reservoirs. Several hydroelectric dams forming shallow reservoirs were built on the Angara River flowing out of Lake Baikal. The first of them in downstream Angara is Irkutsk Reservoir, with several shallow bays. Since silica-scaled chrysophytes are e...

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Autores principales: Bessudova, Anna, Galachyants, Yuri, Firsova, Alena, Hilkhanova, Diana, Nalimova, Maria, Marchenkov, Artyom, Mikhailov, Ivan, Sakirko, Maria, Likhoshway, Yelena
Formato: Online Artículo Texto
Lenguaje:English
Publicado: MDPI 2023
Materias:
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC10608308/
https://www.ncbi.nlm.nih.gov/pubmed/37895433
http://dx.doi.org/10.3390/life13102052
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author Bessudova, Anna
Galachyants, Yuri
Firsova, Alena
Hilkhanova, Diana
Nalimova, Maria
Marchenkov, Artyom
Mikhailov, Ivan
Sakirko, Maria
Likhoshway, Yelena
author_facet Bessudova, Anna
Galachyants, Yuri
Firsova, Alena
Hilkhanova, Diana
Nalimova, Maria
Marchenkov, Artyom
Mikhailov, Ivan
Sakirko, Maria
Likhoshway, Yelena
author_sort Bessudova, Anna
collection PubMed
description Hydroelectric dams create new ecosystems such as reservoirs. Several hydroelectric dams forming shallow reservoirs were built on the Angara River flowing out of Lake Baikal. The first of them in downstream Angara is Irkutsk Reservoir, with several shallow bays. Since silica-scaled chrysophytes are effective bioindicators for aquatic ecosystems, this paper aimed to determine their distribution, taxonomic structure and species richness in South Baikal and Irkutsk Reservoir, which have different environmental parameters. Thirty-one species were found using scanning and transmission electron microscopy. Only seven of them inhabited South Baikal in June 2023 at 3.66–4.51 °C and pH 7.80–8.24, with Chrysosphaerella baicalensis, Spiniferomonas trioralis f. cuspidata and Mallomonas alpina being prevalent. Only one species (M. alpina) was dominant in Irkutsk Reservoir at all stations at a water temperature of 5.33–11.55 °C and pH 8.10–8.52, alongside three other abundant species, Synura cf. glabra, Mallomonas acaroides and M. crassisquama. The maximum number of species (23) was found in a shallow bay of the reservoir at maximal values of temperature (11.5 °C) and pH (8.57) and minimal values of phosphate and nitrate concentrations during the study. The enrichment of Irkutsk Reservoir in species of silica-scaled chrysophytes was due both to cosmopolitan widespread and polyzonal species as well as to rare boreal, arctic–boreal, and unknown, possibly new species.
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spelling pubmed-106083082023-10-28 Changes in Diversity of Silica-Scaled Chrysophytes during Lake–River–Reservoir Transition (Baikal–Angara–Irkutsk Reservoir) Bessudova, Anna Galachyants, Yuri Firsova, Alena Hilkhanova, Diana Nalimova, Maria Marchenkov, Artyom Mikhailov, Ivan Sakirko, Maria Likhoshway, Yelena Life (Basel) Article Hydroelectric dams create new ecosystems such as reservoirs. Several hydroelectric dams forming shallow reservoirs were built on the Angara River flowing out of Lake Baikal. The first of them in downstream Angara is Irkutsk Reservoir, with several shallow bays. Since silica-scaled chrysophytes are effective bioindicators for aquatic ecosystems, this paper aimed to determine their distribution, taxonomic structure and species richness in South Baikal and Irkutsk Reservoir, which have different environmental parameters. Thirty-one species were found using scanning and transmission electron microscopy. Only seven of them inhabited South Baikal in June 2023 at 3.66–4.51 °C and pH 7.80–8.24, with Chrysosphaerella baicalensis, Spiniferomonas trioralis f. cuspidata and Mallomonas alpina being prevalent. Only one species (M. alpina) was dominant in Irkutsk Reservoir at all stations at a water temperature of 5.33–11.55 °C and pH 8.10–8.52, alongside three other abundant species, Synura cf. glabra, Mallomonas acaroides and M. crassisquama. The maximum number of species (23) was found in a shallow bay of the reservoir at maximal values of temperature (11.5 °C) and pH (8.57) and minimal values of phosphate and nitrate concentrations during the study. The enrichment of Irkutsk Reservoir in species of silica-scaled chrysophytes was due both to cosmopolitan widespread and polyzonal species as well as to rare boreal, arctic–boreal, and unknown, possibly new species. MDPI 2023-10-13 /pmc/articles/PMC10608308/ /pubmed/37895433 http://dx.doi.org/10.3390/life13102052 Text en © 2023 by the authors. https://creativecommons.org/licenses/by/4.0/Licensee MDPI, Basel, Switzerland. This article is an open access article distributed under the terms and conditions of the Creative Commons Attribution (CC BY) license (https://creativecommons.org/licenses/by/4.0/).
spellingShingle Article
Bessudova, Anna
Galachyants, Yuri
Firsova, Alena
Hilkhanova, Diana
Nalimova, Maria
Marchenkov, Artyom
Mikhailov, Ivan
Sakirko, Maria
Likhoshway, Yelena
Changes in Diversity of Silica-Scaled Chrysophytes during Lake–River–Reservoir Transition (Baikal–Angara–Irkutsk Reservoir)
title Changes in Diversity of Silica-Scaled Chrysophytes during Lake–River–Reservoir Transition (Baikal–Angara–Irkutsk Reservoir)
title_full Changes in Diversity of Silica-Scaled Chrysophytes during Lake–River–Reservoir Transition (Baikal–Angara–Irkutsk Reservoir)
title_fullStr Changes in Diversity of Silica-Scaled Chrysophytes during Lake–River–Reservoir Transition (Baikal–Angara–Irkutsk Reservoir)
title_full_unstemmed Changes in Diversity of Silica-Scaled Chrysophytes during Lake–River–Reservoir Transition (Baikal–Angara–Irkutsk Reservoir)
title_short Changes in Diversity of Silica-Scaled Chrysophytes during Lake–River–Reservoir Transition (Baikal–Angara–Irkutsk Reservoir)
title_sort changes in diversity of silica-scaled chrysophytes during lake–river–reservoir transition (baikal–angara–irkutsk reservoir)
topic Article
url https://www.ncbi.nlm.nih.gov/pmc/articles/PMC10608308/
https://www.ncbi.nlm.nih.gov/pubmed/37895433
http://dx.doi.org/10.3390/life13102052
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