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<article article-type="research-article" dtd-version="1.3" xmlns:mml="http://www.w3.org/1998/Math/MathML" xmlns:xlink="http://www.w3.org/1999/xlink" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xml:lang="ru"><front><journal-meta><journal-id journal-id-type="publisher-id">sevin</journal-id><journal-title-group><journal-title xml:lang="ru">ПОВОЛЖСКИЙ ЭКОЛОГИЧЕСКИЙ ЖУРНАЛ</journal-title><trans-title-group xml:lang="en"><trans-title>Povolzhskiy Journal of Ecology</trans-title></trans-title-group></journal-title-group><issn pub-type="ppub">1684-7318</issn><issn pub-type="epub">2541-8963</issn><publisher><publisher-name>Федеральное государственное бюджетное учреждение науки Институт проблем экологии и эволюции им. А. Н. Северцова РАН; Товарищество научных изданий КМК.</publisher-name></publisher></journal-meta><article-meta><article-id pub-id-type="doi">10.35885/1684-7318-2022-4-415-430</article-id><article-id custom-type="elpub" pub-id-type="custom">sevin-381</article-id><article-categories><subj-group subj-group-type="heading"><subject>Research Article</subject></subj-group><subj-group subj-group-type="section-heading" xml:lang="ru"><subject>СТАТЬИ</subject></subj-group><subj-group subj-group-type="section-heading" xml:lang="en"><subject>ARTICLES</subject></subj-group></article-categories><title-group><article-title>Распространение высших ракообразных (Malacostraca, Arthropoda) в реках полупустынной зоны (на примере притоков Волгоградского водохранилища)</article-title><trans-title-group xml:lang="en"><trans-title>Distribution of crustaceans (Malacostraca, Arthropoda) in rivers of the semi-desert zone (with the example of the Volgograd reservoir tributes)</trans-title></trans-title-group></title-group><contrib-group><contrib contrib-type="author" corresp="yes"><contrib-id contrib-id-type="orcid">https://orcid.org/0000-0001-5484-2949</contrib-id><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Курина</surname><given-names>Е. М.</given-names></name><name name-style="western" xml:lang="en"><surname>Kurina</surname><given-names>E. M.</given-names></name></name-alternatives><bio xml:lang="ru"><p> Курина Екатерина Михайловна</p><p> 119071, г. Москва, Ленинский просп., д. 33 </p></bio><bio xml:lang="en"><p>33 Leninsky Prosp., Moscow 119071 </p></bio><email xlink:type="simple">ekaterina_kurina@mail.ru</email><xref ref-type="aff" rid="aff-1"/></contrib><contrib contrib-type="author" corresp="yes"><contrib-id contrib-id-type="orcid">https://orcid.org/0000-0003-4773-5277</contrib-id><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Головатюк</surname><given-names>Л. В.</given-names></name><name name-style="western" xml:lang="en"><surname>Golovatyuk</surname><given-names>L. V.</given-names></name></name-alternatives><bio xml:lang="ru"><p>   Головатюк Лариса Владимировна</p><p>445003, г. Тольятти, ул. Комзина, д. 10</p><p>152742, Ярославская обл., Некоузский р-н, пос. Борок </p></bio><bio xml:lang="en"><p>10 Komzina St., Togiatti 445003, RussiaBorok, Nekouzsky district, Yaroslavl oblast 152742 </p></bio><email xlink:type="simple">gollarisa@mail.ru</email><xref ref-type="aff" rid="aff-2"/></contrib></contrib-group><aff-alternatives id="aff-1"><aff xml:lang="ru"><institution>Институт проблем экологии и эволюции им. А. Н. Северцова РАН</institution><country>Россия</country></aff><aff xml:lang="en"><institution>A. N. Severtsov Institute of Ecology and Evolution of the Russian Academy of Sciences</institution><country>Russian Federation</country></aff></aff-alternatives><aff-alternatives id="aff-2"><aff xml:lang="ru"><institution>Самарский федеральный исследовательский центр РАН,&#13;
Институт экологии Волжского бассейна РАН; Институт биологии внутренних вод им. И. Д. Папанина РАН</institution><country>Россия</country></aff><aff xml:lang="en"><institution>Samara Federal Research Center of the Russian Academy of Sciences, Institute of Ecology of the Volga River Basin of Russian Academy of Sciences; I. D. Papanin Institute for Biology of Inland Waters of the Russian Academy of Sciences</institution><country>Russian Federation</country></aff></aff-alternatives><pub-date pub-type="collection"><year>2022</year></pub-date><pub-date pub-type="epub"><day>22</day><month>12</month><year>2022</year></pub-date><volume>0</volume><issue>4</issue><fpage>415</fpage><lpage>430</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Курина Е.М., Головатюк Л.В., 2022</copyright-statement><copyright-year>2022</copyright-year><copyright-holder xml:lang="ru">Курина Е.М., Головатюк Л.В.</copyright-holder><copyright-holder xml:lang="en">Kurina E.M., Golovatyuk L.V.</copyright-holder><license xml:lang="ru" license-type="creative-commons-attribution" xlink:href="https://creativecommons.org/licenses/by/4.0/" xlink:type="simple"><license-p>Данная работа распространяется под лицензией Creative Commons Attribution 4.0.</license-p></license><license xml:lang="en" license-type="creative-commons-attribution" xlink:href="https://creativecommons.org/licenses/by/4.0/" xlink:type="simple"><license-p>This work is licensed under a Creative Commons Attribution 4.0 License.</license-p></license></permissions><self-uri xlink:href="https://sevin.elpub.ru/jour/article/view/381">https://sevin.elpub.ru/jour/article/view/381</self-uri><abstract><p>В результате исследований макро- и нектозообентоса рек полупустынной зоны (бассейн Волгоградского водохранилища) зарегистрировано 16 видов высших ракообразных, большинство из которых − представители понто-каспийского комплекса. По сравнению с Волгоградским водохранилищем в реках полупустынной зоны происходит увеличение количественных показателей мизид и изопод и снижение числа видов, численности и биомассы амфипод и кумовых ракообразных. Средняя численность и биомасса ракообразных в изученных реках примерно в 2.5 раза ниже, чем в Волгоградском водохранилище. Ракообразные понто-каспийского и понто-азовского комплексов, а также изоподы Asellus aquaticus (Linné, 1758) обитают в пресных и олигогалинных водах, гаммариды Gammarus lacustris (Sars, 1863) – олигогалинных и полигалинных. Наибольшим количеством видов характеризуются амфиподы, которые с учетом их морфологии и типа субстрата, на котором они обитают, отнесены к трем экоморфам: «цепляющиеся» (clingers), «ползающие» (crawlers) и «копающие» (diggers). Cимбионты (symbionts) в реках бассейна р. Еруслан не обнаружены. Отмеченные экоморфы амфипод распространены относительно равномерно с незначительным доминированием «ползающих» (45%). Выявлено, что в изученных реках образуется два типа ценозов ракообразных. Первый тип образован в основном консорционными взаимодействиями моллюсков-эдификаторов р. Dreissena c амфиподами Chelicorophium curvispinum Sars, 1895, Dikerogammarus haemobaphes (Eichwald, 1841), мизидами Paramysis ullskyi Czerniavsky, 1882, P. lacustris (Czerniavsky, 1882) и ассоциированных с ними видами. Второй ценоз в реках представлен комплексом мелких прибрежных видов мизид Katamysis warpachowskyi Czerniavsky, 1882 и Limnomysis benedeni Sars, 1893 и амфипод Chaetogammarus warpachowsky (Sars, 1894), связи в котором основаны на общности биотопических условий и характере питания.</p></abstract><trans-abstract xml:lang="en"><p>As a result of our studies of the macro- and nectozoobenthos of the rivers of the semidesert zone (the Volgograd reservoir basin), 16 Malacostraca species were recorded, most of which are representatives of the Ponto-Caspian complex. Compared to the Volgograd reservoir, there is an increase in the quantitative indicators  of mysids and isopods and a decrease in the number of species, abundance and biomass of amphipods and cumaceans in the semi-desert zone rivers. The average abundance and biomass of crustaceans in the surveyed rivers are approximately 2.5 times lower than in the Volgograd Reservoir. Crustaceans of the Ponto-Caspian and PontoAzov complexes, as well as the isopods Asellus aquaticus (Linné, 1758) inhabit fresh and oligohaline waters, while the gammarids Gammarus lacustris (Sars, 1863) live in oligohaline and polyhaline waters. Amphipods are characterized by the largest number of species, which, taking into account their morphology and the type of substrate which they live on, are assigned to three ecomorphs, namely: clingers, crawlers, and diggers. No symbionts in the Yeruslan basin rivers were found. The noted amphipod ecomorphs are distributed relatively evenly with a slight dominance of crawlers (45%). It has been revealed that two types of crustacean cenoses are formed in the surveyed rivers. The first type is formed mainly by consortium interactions of the edificatory mollusks Dreissena with amphipods Chelicorophium curvispinum Sars, 1895, Dikerogammarus haemobaphes (Eichwald, 1841), mysids Paramysis ullskyi Czerniavsky, 1882, P. lacustris (Czerniavsky, 1882), and associated species. The second cenosis in the rivers is represented by a complex of small coastal mysid species Katamysis warpachowskyi Czerniavsky, 1882, Limnomysis benedeni Sars, 1893, and amphipods Chaetogammarus warpachowsky (Sars, 1894), the relationships within which are based on common biotopic conditions and feeding patterns.</p></trans-abstract><kwd-group xml:lang="ru"><kwd>высшие ракообразные</kwd><kwd>реки полупустынной зоны</kwd><kwd>Волгоградское водохранилище</kwd><kwd>ценотические комплексы</kwd><kwd>распространение</kwd></kwd-group><kwd-group xml:lang="en"><kwd>crustaceans</kwd><kwd>semi-desert zone rivers</kwd><kwd>Volgograd Reservoir</kwd><kwd>coenotic complexes</kwd><kwd>distribution</kwd></kwd-group></article-meta></front><back><ref-list><title>References</title><ref id="cit1"><label>1</label><citation-alternatives><mixed-citation xml:lang="ru">Атлас беспозвоночных / под ред. В. Я. Бирштейна, Л. Г. Виноградова, Н. Н. Кондакова. 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