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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">reggeomet</journal-id><journal-title-group><journal-title xml:lang="ru">Региональная геология и металлогения</journal-title><trans-title-group xml:lang="en"><trans-title>Regional Geology and Metallogeny</trans-title></trans-title-group></journal-title-group><issn pub-type="ppub">0869-7892</issn><publisher><publisher-name>(ФГБУ "Институт Карпинского")</publisher-name></publisher></journal-meta><article-meta><article-id custom-type="elpub" pub-id-type="custom">reggeomet-283</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>РЕГИОНАЛЬНАЯ ГЕОЛОГИЯ</subject></subj-group><subj-group subj-group-type="section-heading" xml:lang="en"><subject>REGIONAL GEOLOGY</subject></subj-group></article-categories><title-group><article-title>Новые данные о нижнеюрских аммонитах бассейна реки Бодрак (Юго-Западный Крым)</article-title><trans-title-group xml:lang="en"><trans-title>New data on the Lower Jurassic ammonites of the Bodrak River Basin (Southwestern Crimea)</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>Зайцев</surname><given-names>Б. А.</given-names></name><name name-style="western" xml:lang="en"><surname>Zaitsev</surname><given-names>B. A.</given-names></name></name-alternatives><bio xml:lang="ru"><p>аспирант</p></bio><bio xml:lang="en"><p>Ph. D. Student</p></bio><email xlink:type="simple">pogrom_karerov@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>Аркадьев</surname><given-names>В. В.</given-names></name><name name-style="western" xml:lang="en"><surname>Arkad’ev</surname><given-names>V. V.</given-names></name></name-alternatives><bio xml:lang="ru"><p>доктор геол.-минерал. наук, профессор</p></bio><bio xml:lang="en"><p>Doctor of Geological and Mineralogical Sciences, Professor</p></bio><email xlink:type="simple">arkadievvv@mail.ru</email><xref ref-type="aff" rid="aff-2"/></contrib></contrib-group><aff-alternatives id="aff-1"><aff xml:lang="ru"><institution>Всероссийский научно-исследовательский геологический&#13;
институт им. А. П. Карпинского (ВСЕГЕИ)</institution><country>Россия</country></aff><aff xml:lang="en"><institution>A. P. Karpinsky Russian Geological Research Institute (VSEGEI)</institution><country>Russian Federation</country></aff></aff-alternatives><aff-alternatives id="aff-2"><aff xml:lang="ru"><institution>Институт наук о Земле Санкт-Петербургского государственного университета (Институт наук о Земле СПбГУ)</institution><country>Россия</country></aff><aff xml:lang="en"><institution>Institute of Earth Sciences of St. Petersburg University (Institute of Earth Sciences of SPbGU)</institution><country>Russian Federation</country></aff></aff-alternatives><pub-date pub-type="collection"><year>2019</year></pub-date><pub-date pub-type="epub"><day>24</day><month>06</month><year>2025</year></pub-date><volume>0</volume><issue>78</issue><elocation-id>21–30</elocation-id><permissions><copyright-statement>Copyright &amp;#x00A9; Зайцев Б.А., Аркадьев В.В., 2025</copyright-statement><copyright-year>2025</copyright-year><copyright-holder xml:lang="ru">Зайцев Б.А., Аркадьев В.В.</copyright-holder><copyright-holder xml:lang="en">Zaitsev B.A., Arkad’ev V.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://reggeomet.elpub.ru/jour/article/view/283">https://reggeomet.elpub.ru/jour/article/view/283</self-uri><abstract><p>Из зоны тектонического меланжа («эскиординской серии») и флиша таврической серии басс. р. Бодрак Юго-Западного Крыма описаны нижнеюрские аммониты Dactylioceras (Orthodactylites) semicelatum (Simpson), Dactylioceras (Dactylioceras) ex gr. commune (Sowerby), Arnioceras ex gr. ceratitoides (Quenstedt), Angulaticeras (Boucaulticeras) dumortieri (Fucini), Angulaticeras sp. и Eleganticeras sp. (?). Первые три  вида определены из этого района впервые. Представители родов Angulaticeras и Arnioceras характеризуют синемюрский ярус, родов Dactylioceras и Eleganticeras (?) – нижний подъярус тоарского яруса. Некоторые из описанных видов аммонитов определяют зоны, установленные в Западной Европе: A. (B.) dumortieri – зону Oxynotum синемюра, D. (O.) semicelatum – зону Tenuicostatum нижнего тоара. Вид D. (D.) ex gr. commune позволяет наметить корреляцию с нижним тоаром Северо-Востока России, Северной Аляски, Арктической Канады, архипелага Шпицберген и Южной Америки.</p></abstract><trans-abstract xml:lang="en"><p>Lower Jurassic ammonites Dactylioceras (Orthodactylites) semicelatum (Simpson), Dactylioceras (Dactylioceras) ex gr. commune (Sowerby), Arnioceras ex gr. ceratitoides (Quenstedt), Angulaticeras (Boucaulticeras) dumortieri (Fucini), Angulaticeras sp. and Eleganticeras (?) sp. from the zone of tectonic melange (“Eskiordinsky series”) and flysch of the Tauriс series of the Bodrak River Basin were described. The first three species have been identified in this area for the first time. Representatives of the Angulaticeras and Arnioceras genera are typical of the Sinemurian stage, the Dactylioceras and Eleganticeras (?) genera for the lower substage of the Toarcian stage. Some of the described ammonite species correspond to the zones established in Western Europe: A. (B.) dumortieri to the Lower Sinemurian Oxynotum zone, D. (O.) semicelatum to the Lower Toarcian Tenuicostatum zone. In addition, the D. (D.) ex gr. commune suggests the correlation with the Lower Toarcian of the Northeast of Russia, Northern Alaska, Arctic Canada, Spitsbergenarchipelago and South America.</p></trans-abstract><kwd-group xml:lang="ru"><kwd>Горный Крым</kwd><kwd>нижняя юра</kwd><kwd>аммониты</kwd><kwd>монографическое описание</kwd></kwd-group><kwd-group xml:lang="en"><kwd>Mountain Crimea</kwd><kwd>Lower Jurassic</kwd><kwd>ammonites</kwd><kwd>monographic description</kwd></kwd-group><funding-group><funding-statement xml:lang="ru">Авторы благодарят старшего научного сотрудника ВСЕГЕИ, кандидата геол.-минерал. наук Т. Н. 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