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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">tinro</journal-id><journal-title-group><journal-title xml:lang="ru">Известия ТИНРО</journal-title><trans-title-group xml:lang="en"><trans-title>Izvestiya TINRO</trans-title></trans-title-group></journal-title-group><issn pub-type="ppub">1606-9919</issn><issn pub-type="epub">2658-5510</issn><publisher><publisher-name>ТИНРО</publisher-name></publisher></journal-meta><article-meta><article-id pub-id-type="doi">10.26428/1606-9919-2021-201-600-639</article-id><article-id custom-type="elpub" pub-id-type="custom">tinro-659</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>УСЛОВИЯ ОБИТАНИЯ ПРОМЫСЛОВЫХ ОБЪЕКТОВ</subject></subj-group><subj-group subj-group-type="section-heading" xml:lang="en"><subject>ENVIRONMENTS OF FISHERIES RESOURCES</subject></subj-group></article-categories><title-group><article-title>Гипоксия залива Петра Великого</article-title><trans-title-group xml:lang="en"><trans-title>Hypoxia in Peter the Great Bay</trans-title></trans-title-group></title-group><contrib-group><contrib contrib-type="author" corresp="yes"><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Тищенко</surname><given-names>П. П.</given-names></name><name name-style="western" xml:lang="en"><surname>Tishchenko</surname><given-names>P. P.</given-names></name></name-alternatives><bio xml:lang="ru"><p>Тищенко Петр Павлович, кандидат географических наук, старший научный сотрудник</p><p>690041, г. Владивосток, ул. Балтийская, 43</p></bio><bio xml:lang="en"><p>Tishchenko Petr P., Ph.D., senior researcher</p><p>43, Baltiyskaya Street, Vladivostok, 690041</p></bio><email xlink:type="simple">eq15@poi.dvo.ru</email><xref ref-type="aff" rid="aff-1"/></contrib><contrib contrib-type="author" corresp="yes"><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Звалинский</surname><given-names>В. И.</given-names></name><name name-style="western" xml:lang="en"><surname>Zvalinsky</surname><given-names>V. I.</given-names></name></name-alternatives><bio xml:lang="ru"><p>Звалинский Владимир Иванович, доктор биологических наук, главный научный сотрудник</p><p>690041, г. Владивосток, ул. Балтийская, 43</p></bio><bio xml:lang="en"><p>Zvalinsky Vladimir I., D.Biol., principal researcher</p><p>43, Baltiyskaya Street, Vladivostok, 690041</p></bio><email xlink:type="simple">biomar@mail.ru</email><xref ref-type="aff" rid="aff-1"/></contrib><contrib contrib-type="author" corresp="yes"><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Михайлик</surname><given-names>Т. А.</given-names></name><name name-style="western" xml:lang="en"><surname>Mikhaylik</surname><given-names>T. A.</given-names></name></name-alternatives><bio xml:lang="ru"><p>Михайлик Татьяна Александровна, научный сотрудник</p><p>690041, г. Владивосток, ул. Балтийская, 43</p></bio><bio xml:lang="en"><p>Mikhaylik Tatyana A., researcher</p><p>43, Baltiyskaya Street, Vladivostok, 690041</p></bio><email xlink:type="simple">tatyana.mikhaylik.00@mail.ru</email><xref ref-type="aff" rid="aff-1"/></contrib><contrib contrib-type="author" corresp="yes"><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Тищенко</surname><given-names>П. Я.</given-names></name><name name-style="western" xml:lang="en"><surname>Tishchenko</surname><given-names>P. Ya.</given-names></name></name-alternatives><bio xml:lang="ru"><p>Тищенко Павел Яковлевич, доктор химических наук, заведующий лабораторией</p><p>690041, г. Владивосток, ул. Балтийская, 43</p></bio><bio xml:lang="en"><p>Tishchenko Pavel Ya., D.Chem., head of laboratory</p><p>43, Baltiyskaya Street, Vladivostok, 690041</p></bio><email xlink:type="simple">tpavel@poi.dvo.ru</email><xref ref-type="aff" rid="aff-1"/></contrib></contrib-group><aff-alternatives id="aff-1"><aff xml:lang="ru"><institution>Тихоокеанский океанологический институт им. В.И. Ильичева ДВО РАН</institution><country>Россия</country></aff><aff xml:lang="en"><institution>Pacific Oceanological Institute, Russian Ac. Sci.</institution><country>Russian Federation</country></aff></aff-alternatives><pub-date pub-type="collection"><year>2021</year></pub-date><pub-date pub-type="epub"><day>05</day><month>10</month><year>2021</year></pub-date><volume>201</volume><issue>3</issue><fpage>600</fpage><lpage>639</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Тищенко П.П., Звалинский В.И., Михайлик Т.А., Тищенко П.Я., 2021</copyright-statement><copyright-year>2021</copyright-year><copyright-holder xml:lang="ru">Тищенко П.П., Звалинский В.И., Михайлик Т.А., Тищенко П.Я.</copyright-holder><copyright-holder xml:lang="en">Tishchenko P.P., Zvalinsky V.I., Mikhaylik T.A., Tishchenko P.Y.</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://izvestiya.tinro-center.ru/jour/article/view/659">https://izvestiya.tinro-center.ru/jour/article/view/659</self-uri><abstract><p>Дан обзор исследований гипоксии придонных вод зал. Петра Великого (ЗПВ), которая возникает, как правило, во второй половине лета. Рассмотрены три акватории залива, подверженные гипоксии в летний сезон: Амурский залив, Уссурийский залив и южный район Дальневосточного морского биосферного заповедника (ЮРЗ). Гипоксия формируется во всех акваториях в депрессиях морского дна и является автохтонной по происхождению. Адвекция гипоксийных придонных вод из впадин формирует аллохтонный тип гипоксии вод в северной части Амурского залива, в прол. БосфорВосточный. Образование гипоксии обусловлено микробиологической деструкцией «избыточного» фитопланктона, который является результатом эвтрофикации вод ЗПВ. Основными источниками биогенных веществ являются эвтрофированные реки Туманная (для ЮРЗ), Раздольная (для Амурского залива) и Кневичанка (для Уссурийского залива). Большой вклад в эвтрофикацию вод Уссурийского и Амурского заливов вносят коммунальные стоки Владивостока и Артема. На основе литературных данных установлен временной тренд уменьшения концентрации кислорода в придонных водах Амурского залива в летний сезон. Сравнение исторических и собственных данных по содержанию кислорода в придонных водах Амурского залива указывает на синхронизацию глобальных и региональных процессов эвтрофикации, деоксигенации, а также ацидификации придонных вод.</p></abstract><trans-abstract xml:lang="en"><p>Studies on hypoxia in Peter the Great Bay (Japan Sea) are reviewed. Seasonal hypoxia is observed in warm season at the bottom of three areas: Amur Bay, Ussuri Bay, and the southwestern part of Peter the Great Bay occupied by the Far-Eastern Marine Biosphere Reserve (FEMBR). Processes of the hypoxia forming are similar in all these areas. The main reason is the dissolved oxygen consumption by microbial degradation of organic matter within topographic depressions in conditions of limited ventilation because of strong summer stratification. The bottom depressions prevent horizontal water exchange and provide accumulation of organic and inorganic suspension, that is another factor important for development of hypoxia. The Amur Bay is the most subjected to hypoxia, being a semiclosed estuarine basin eutrophed by nutrients input from the Razdolnaya River and waste waters of Vladivostok city. The Ussuri Bay has better water exchange and less eutrophication, therefore there are scarce data about hypoxia in this area. FEMBR area has good water exchange and is only episodically influenced by nutrients discharge from the Tumen River, so hypoxia is observed there occasionally. Another consequence of microbial degradation of organic matter in these areas is acidification: pH decreased in 0.5 unit in the bottom water of the Amur Bay in eight decades from 1932 to 2013. Synchronism between regional and global processes of eutrophication, deoxygenation, and acidification of bottom waters is discussed.</p></trans-abstract><kwd-group xml:lang="ru"><kwd>гипоксия</kwd><kwd>эвтрофикация</kwd><kwd>биогенные вещества</kwd><kwd>растворенный кислород</kwd><kwd>продукционно/деструкционные процессы</kwd><kwd>залив Петра Великого</kwd></kwd-group><kwd-group xml:lang="en"><kwd>hypoxia</kwd><kwd>eutrophication</kwd><kwd>nutrients</kwd><kwd>dissolved oxygen</kwd><kwd>production/destruction</kwd><kwd>Peter the Great Bay</kwd></kwd-group><funding-group><funding-statement xml:lang="ru">Работа выполнена при финансовой поддержке гранта РФФИ 21-55-53015 и госбюджетных тем 121-21500052-9 и 121021700346-7.</funding-statement></funding-group></article-meta></front><back><ref-list><title>References</title><ref id="cit1"><label>1</label><citation-alternatives><mixed-citation xml:lang="ru">Барабанщиков Ю.А., Тищенко П.Я., Семкин П.Ю. и др. 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