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Ecological description of the sodium chloride mineral springs in the Kirenga River basin and the upper reaches of the Lena River: 1. General characteristics of the springs and their hydrofauna
The aquatic microecosystems and their environment have been studied in 12 mineral springs located in the Cis-Baikal Depression and in the basin of the upper reaches of the Lena River (Eastern Siberia). The hydrochemical characteristics of the springs, originating from the Cambrian salt deposits, are...
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Published in: | Inland water biology 2017-10, Vol.10 (4), p.331-341, Article 331 |
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description | The aquatic microecosystems and their environment have been studied in 12 mineral springs located in the Cis-Baikal Depression and in the basin of the upper reaches of the Lena River (Eastern Siberia). The hydrochemical characteristics of the springs, originating from the Cambrian salt deposits, are given. Their total mineralization varies from 1.1 to 123.0 g/L and the water is sodium chloride. The soils formed under the influence of the mineral waters (“para-soils”) are described. The data on the composition and quantitative abundance of aquatic fauna are presented. Six types of macroinvertebrate communities are described. The communities where Turbellaria, Gastropoda, and Psychodidae dominate are recorded in weakly mineralized waters (97% of the biomass) is described for the concentrated brines in Ust’-Kutskii spring. Halophilic species of crustaceans are recorded in the meiofauna. The presence of Foraminifera (marine organisms) in the two studied springs attracts specific interest. |
doi_str_mv | 10.1134/S1995082917040101 |
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Gammarus lacustris
Sars. are formed. A unique type of community where Ephydridae larvae dominate (>97% of the biomass) is described for the concentrated brines in Ust’-Kutskii spring. Halophilic species of crustaceans are recorded in the meiofauna. The presence of Foraminifera (marine organisms) in the two studied springs attracts specific interest.</description><identifier>ISSN: 1995-0829</identifier><identifier>EISSN: 1995-0837</identifier><identifier>DOI: 10.1134/S1995082917040101</identifier><language>eng</language><publisher>Moscow: Pleiades Publishing</publisher><subject>Aquatic animals ; Aquatic crustaceans ; Aquatic environment ; Aquatic fauna ; Aquatic Flora and Fauna ; Aquatic insects ; Aquatic invertebrates ; Biodiversity ; Biomass ; Biomedical and Life Sciences ; Brines ; Cambrian ; Communities ; Composition ; Crustaceans ; Fauna ; Fluvial deposits ; Foraminifera ; Freshwater & Marine Ecology ; Geoecology/Natural Processes ; Geologic depressions ; Larvae ; Life Sciences ; Macroinvertebrates ; Marine invertebrates ; Marine molluscs ; Marine organisms ; Meiobenthos ; Meiofauna ; Microecosystems ; Mineral springs ; Mineral waters ; Mineralization ; River basins ; Rivers ; Salinity ; Salinity effects ; Salt deposits ; Salts ; Sodium ; Sodium chloride ; Soil ; Water salinity ; Water springs ; Zoobenthos</subject><ispartof>Inland water biology, 2017-10, Vol.10 (4), p.331-341, Article 331</ispartof><rights>Pleiades Publishing, Ltd. 2017</rights><rights>Copyright Springer Science & Business Media 2017</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c316t-93dc81b948c3a799ee896b4b209442ee2351da7c17b5abae004599ce4c211a863</citedby><cites>FETCH-LOGICAL-c316t-93dc81b948c3a799ee896b4b209442ee2351da7c17b5abae004599ce4c211a863</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>314,780,784,27924,27925</link.rule.ids></links><search><creatorcontrib>Takhteev, V. V.</creatorcontrib><creatorcontrib>Lopatovskaya, O. G.</creatorcontrib><creatorcontrib>Okuneva, G. L.</creatorcontrib><creatorcontrib>Pomazkova, G. I.</creatorcontrib><creatorcontrib>Samoilova, E. A.</creatorcontrib><creatorcontrib>Rozhkova, N. A.</creatorcontrib><title>Ecological description of the sodium chloride mineral springs in the Kirenga River basin and the upper reaches of the Lena River: 1. General characteristics of the springs and their hydrofauna</title><title>Inland water biology</title><addtitle>Inland Water Biol</addtitle><description>The aquatic microecosystems and their environment have been studied in 12 mineral springs located in the Cis-Baikal Depression and in the basin of the upper reaches of the Lena River (Eastern Siberia). The hydrochemical characteristics of the springs, originating from the Cambrian salt deposits, are given. Their total mineralization varies from 1.1 to 123.0 g/L and the water is sodium chloride. The soils formed under the influence of the mineral waters (“para-soils”) are described. The data on the composition and quantitative abundance of aquatic fauna are presented. Six types of macroinvertebrate communities are described. The communities where Turbellaria, Gastropoda, and Psychodidae dominate are recorded in weakly mineralized waters (<3 g/L). The communities where Chironomidae dominate are found in waters characterized both by low and high (up to 28 g/L) salinity. In springs with a water salinity of 2.5–11 g/L, communities characterized by the dominance and high biomass of amphipods
Gammarus lacustris
Sars. are formed. A unique type of community where Ephydridae larvae dominate (>97% of the biomass) is described for the concentrated brines in Ust’-Kutskii spring. Halophilic species of crustaceans are recorded in the meiofauna. The presence of Foraminifera (marine organisms) in the two studied springs attracts specific interest.</description><subject>Aquatic animals</subject><subject>Aquatic crustaceans</subject><subject>Aquatic environment</subject><subject>Aquatic fauna</subject><subject>Aquatic Flora and Fauna</subject><subject>Aquatic insects</subject><subject>Aquatic invertebrates</subject><subject>Biodiversity</subject><subject>Biomass</subject><subject>Biomedical and Life Sciences</subject><subject>Brines</subject><subject>Cambrian</subject><subject>Communities</subject><subject>Composition</subject><subject>Crustaceans</subject><subject>Fauna</subject><subject>Fluvial deposits</subject><subject>Foraminifera</subject><subject>Freshwater & Marine Ecology</subject><subject>Geoecology/Natural Processes</subject><subject>Geologic depressions</subject><subject>Larvae</subject><subject>Life Sciences</subject><subject>Macroinvertebrates</subject><subject>Marine invertebrates</subject><subject>Marine molluscs</subject><subject>Marine organisms</subject><subject>Meiobenthos</subject><subject>Meiofauna</subject><subject>Microecosystems</subject><subject>Mineral springs</subject><subject>Mineral waters</subject><subject>Mineralization</subject><subject>River basins</subject><subject>Rivers</subject><subject>Salinity</subject><subject>Salinity effects</subject><subject>Salt deposits</subject><subject>Salts</subject><subject>Sodium</subject><subject>Sodium chloride</subject><subject>Soil</subject><subject>Water salinity</subject><subject>Water springs</subject><subject>Zoobenthos</subject><issn>1995-0829</issn><issn>1995-0837</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2017</creationdate><recordtype>article</recordtype><recordid>eNp9kd1q3DAQhU1JoCHNA_RO0OtNNJK8tnJXQpqELhTyc23G8uxawSu5I7uQt-uj1RtvQmhpdCNx9J0zw0yWfQZ5CqDN2R1Ym8tSWSikkSDhQ3a0kxay1MXB61vZj9lJSo9yOhqM0uoo-33pYhc33mEnGkqOfT_4GERci6ElkWLjx61wbRfZNyS2PhBPaOrZh00SPjxj3z1T2KC49b-IRY1p0jE0z39j308aE7qW0kvuisKePhdwKq5ojnUtMrqB2KfBu1f6pdo-0rNonxqOaxwDfsoO19glOtnfx9nDt8v7i-vF6sfVzcXX1cJpWA4LqxtXQm1N6TQW1hKVdlmbWklrjCJSOocGCwdFnWONJKXJrXVknALAcqmPsy9zbs_x50hpqB7jyGEqWYEtijwHkPlEwUw5jikxraup9S3yUwWy2u2q-mdXk6f4y-P8gLstDIy-e9epZuc8IOI3Pf3X9AdUM6lf</recordid><startdate>20171001</startdate><enddate>20171001</enddate><creator>Takhteev, V. V.</creator><creator>Lopatovskaya, O. G.</creator><creator>Okuneva, G. L.</creator><creator>Pomazkova, G. I.</creator><creator>Samoilova, E. A.</creator><creator>Rozhkova, N. A.</creator><general>Pleiades Publishing</general><general>Springer Nature B.V</general><scope>AAYXX</scope><scope>CITATION</scope><scope>7QH</scope><scope>7UA</scope><scope>C1K</scope><scope>F1W</scope><scope>H95</scope><scope>L.G</scope></search><sort><creationdate>20171001</creationdate><title>Ecological description of the sodium chloride mineral springs in the Kirenga River basin and the upper reaches of the Lena River: 1. General characteristics of the springs and their hydrofauna</title><author>Takhteev, V. V. ; Lopatovskaya, O. G. ; Okuneva, G. L. ; Pomazkova, G. I. ; Samoilova, E. A. ; Rozhkova, N. 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V.</creatorcontrib><creatorcontrib>Lopatovskaya, O. G.</creatorcontrib><creatorcontrib>Okuneva, G. L.</creatorcontrib><creatorcontrib>Pomazkova, G. I.</creatorcontrib><creatorcontrib>Samoilova, E. A.</creatorcontrib><creatorcontrib>Rozhkova, N. A.</creatorcontrib><collection>CrossRef</collection><collection>Aqualine</collection><collection>Water Resources Abstracts</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 1: Biological Sciences & Living Resources</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><jtitle>Inland water biology</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Takhteev, V. V.</au><au>Lopatovskaya, O. G.</au><au>Okuneva, G. L.</au><au>Pomazkova, G. I.</au><au>Samoilova, E. A.</au><au>Rozhkova, N. A.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Ecological description of the sodium chloride mineral springs in the Kirenga River basin and the upper reaches of the Lena River: 1. General characteristics of the springs and their hydrofauna</atitle><jtitle>Inland water biology</jtitle><stitle>Inland Water Biol</stitle><date>2017-10-01</date><risdate>2017</risdate><volume>10</volume><issue>4</issue><spage>331</spage><epage>341</epage><pages>331-341</pages><artnum>331</artnum><issn>1995-0829</issn><eissn>1995-0837</eissn><abstract>The aquatic microecosystems and their environment have been studied in 12 mineral springs located in the Cis-Baikal Depression and in the basin of the upper reaches of the Lena River (Eastern Siberia). The hydrochemical characteristics of the springs, originating from the Cambrian salt deposits, are given. Their total mineralization varies from 1.1 to 123.0 g/L and the water is sodium chloride. The soils formed under the influence of the mineral waters (“para-soils”) are described. The data on the composition and quantitative abundance of aquatic fauna are presented. Six types of macroinvertebrate communities are described. The communities where Turbellaria, Gastropoda, and Psychodidae dominate are recorded in weakly mineralized waters (<3 g/L). The communities where Chironomidae dominate are found in waters characterized both by low and high (up to 28 g/L) salinity. In springs with a water salinity of 2.5–11 g/L, communities characterized by the dominance and high biomass of amphipods
Gammarus lacustris
Sars. are formed. A unique type of community where Ephydridae larvae dominate (>97% of the biomass) is described for the concentrated brines in Ust’-Kutskii spring. Halophilic species of crustaceans are recorded in the meiofauna. The presence of Foraminifera (marine organisms) in the two studied springs attracts specific interest.</abstract><cop>Moscow</cop><pub>Pleiades Publishing</pub><doi>10.1134/S1995082917040101</doi><tpages>11</tpages></addata></record> |
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issn | 1995-0829 1995-0837 |
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subjects | Aquatic animals Aquatic crustaceans Aquatic environment Aquatic fauna Aquatic Flora and Fauna Aquatic insects Aquatic invertebrates Biodiversity Biomass Biomedical and Life Sciences Brines Cambrian Communities Composition Crustaceans Fauna Fluvial deposits Foraminifera Freshwater & Marine Ecology Geoecology/Natural Processes Geologic depressions Larvae Life Sciences Macroinvertebrates Marine invertebrates Marine molluscs Marine organisms Meiobenthos Meiofauna Microecosystems Mineral springs Mineral waters Mineralization River basins Rivers Salinity Salinity effects Salt deposits Salts Sodium Sodium chloride Soil Water salinity Water springs Zoobenthos |
title | Ecological description of the sodium chloride mineral springs in the Kirenga River basin and the upper reaches of the Lena River: 1. General characteristics of the springs and their hydrofauna |
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