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<article 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" xmlns:ali="http://www.niso.org/schemas/ali/1.0/" article-type="research-article" dtd-version="1.2" xml:lang="en"><front><journal-meta><journal-id journal-id-type="publisher-id">Stratigraphy and Geological Correlation</journal-id><journal-title-group><journal-title xml:lang="en">Stratigraphy and Geological Correlation</journal-title><trans-title-group xml:lang="ru"><trans-title>Стратиграфия. Геологическая корреляция</trans-title></trans-title-group></journal-title-group><issn publication-format="print">0869-592X</issn><issn publication-format="electronic">3034-6037</issn><publisher><publisher-name xml:lang="en">The Russian Academy of Sciences</publisher-name></publisher></journal-meta><article-meta><article-id pub-id-type="publisher-id">693061</article-id><article-id pub-id-type="doi">10.31857/S0869592X25040026</article-id><article-categories><subj-group subj-group-type="toc-heading" xml:lang="en"><subject>Articles</subject></subj-group><subj-group subj-group-type="toc-heading" xml:lang="ru"><subject>Статьи</subject></subj-group><subj-group subj-group-type="article-type"><subject>Research Article</subject></subj-group></article-categories><title-group><article-title xml:lang="en">Paleobiogeography of the late Paleozoic family Annuliconchidae (Bivalvia: Pectinida) and its relation to paleoclimate and paleogeographic changes</article-title><trans-title-group xml:lang="ru"><trans-title>Палеобиогеография позднепалеозойского семейства Annuliconchidae (Bivalvia: Pectinida) и ее связь с палеоклиматом и палеогеографическими перестройками</trans-title></trans-title-group></title-group><contrib-group><contrib contrib-type="author"><name-alternatives><name xml:lang="en"><surname>Shilekhin</surname><given-names>L. E.</given-names></name><name xml:lang="ru"><surname>Шилехин</surname><given-names>Л. Е.</given-names></name></name-alternatives><email>levia4an@mail.ru</email><xref ref-type="aff" rid="aff1"/><xref ref-type="aff" rid="aff2"/></contrib><contrib contrib-type="author"><name-alternatives><name xml:lang="en"><surname>Biakov</surname><given-names>A. S.</given-names></name><name xml:lang="ru"><surname>Бяков</surname><given-names>А. С.</given-names></name></name-alternatives><email>levia4an@mail.ru</email><xref ref-type="aff" rid="aff3"/></contrib></contrib-group><aff-alternatives id="aff1"><aff><institution xml:lang="en">Geological Institute, Russian Academy of Sciences</institution></aff><aff><institution xml:lang="ru">Геологический институт РАН</institution></aff></aff-alternatives><aff-alternatives id="aff2"><aff><institution xml:lang="en">Lomonosov Moscow State University</institution></aff><aff><institution xml:lang="ru">Московский государственный университет им. М.В. Ломоносова</institution></aff></aff-alternatives><aff-alternatives id="aff3"><aff><institution xml:lang="en">Shilo North-East Interdisciplinary Scientific Research Institute, Far East Branch of the Russian Academy of Sciences</institution></aff><aff><institution xml:lang="ru">Северо-Восточный комплексный научно-исследовательский институт им. Н.А. Шило ДВО РАН</institution></aff></aff-alternatives><pub-date date-type="pub" iso-8601-date="2025-08-15" publication-format="electronic"><day>15</day><month>08</month><year>2025</year></pub-date><volume>33</volume><issue>4</issue><issue-title xml:lang="en">VOL 33, NO4 (2025)</issue-title><issue-title xml:lang="ru">ТОМ 33, №4 (2025)</issue-title><fpage>25</fpage><lpage>39</lpage><history><date date-type="received" iso-8601-date="2025-10-13"><day>13</day><month>10</month><year>2025</year></date></history><permissions><copyright-statement xml:lang="en">Copyright ©; 2025, Russian Academy of Sciences</copyright-statement><copyright-statement xml:lang="ru">Copyright ©; 2025, Российская академия наук</copyright-statement><copyright-year>2025</copyright-year><copyright-holder xml:lang="en">Russian Academy of Sciences</copyright-holder><copyright-holder xml:lang="ru">Российская академия наук</copyright-holder></permissions><self-uri xlink:href="https://journals.eco-vector.com/0869-592X/article/view/693061">https://journals.eco-vector.com/0869-592X/article/view/693061</self-uri><abstract xml:lang="en"><p>The paleobiogeographic distribution of the fam. Annuliconchidae of bivalves in the late Paleozoic is analyzed. A list of all Annuliconchid localities with reconstructions of their paleolatitudes has been compiled. The stratigraphic interval of the family’s existence has been adjusted (Bashkirian Age of the Middle Carboniferous–Capitanian Age of the Middle Permian). It is shown that the family representatives had a low-latitude distribution in Laurasia and microcontinents located in the Paleotethys and Pantalassa. In the Northern Hemisphere, annuliconchids are not recorded north of the 32° paleolatitude, and in the Southern Hemisphere they are limited to 14° of the paleolatitudes. The change in the distribution range of the family demonstrates a connection with the climatic and paleogeographic events of the late Paleozoic. During the cold time, marked by an increase in the area of cover glaciations in the Southern Hemisphere, the range of distribution of annuliconchids shifted to the north, during the warming – to the south. The narrowing of the range in the Middle Permian was caused by the closure of the Ural Strait and the disappearance of the normal marine basin associated with Paleothesis on the territory of the East European Platform.</p></abstract><trans-abstract xml:lang="ru"><p>Проведен анализ палеобиогеографического распространения двустворчатых моллюсков позднепалеозойского семейства Annuliconchidae. Составлен перечень всех местонахождений аннуликонхид с реконструкциями их палеоширот. Скорректирован стратиграфический интервал существования семейства (башкирский век среднего карбона–кепитенский век средней перми). Показано, что представители семейства имели низкоширотное распространение на территории Лавразии и микроконтинентах, расположенных в Палеотетисе и Панталассе. В Северном полушарии аннуликонхиды не фиксируются севернее 32° палеошироты, а в Южном ограничены 14° южной палеошироты. Изменение ареала семейства демонстрирует связь с климатическими и палеогеографическими событиями позднего палеозоя. Во время похолоданий, маркированных увеличением площади покровных оледенений в Южном полушарии, ареал аннуликонхид смещался на север, во время потеплений – на юг. Сужение ареала в средней перми было вызвано закрытием Уральского пролива и исчезновением связанного с Палеотетисом нормально-морского бассейна на территории Восточно-Европейской платформы.</p></trans-abstract><kwd-group xml:lang="en"><kwd>Bivalvia</kwd><kwd>Annuliconcha</kwd><kwd>Lineaspina</kwd><kwd>distribution</kwd><kwd>glaciations</kwd><kwd>Carboniferous</kwd><kwd>Permian</kwd><kwd>paleoclimate change</kwd></kwd-group><kwd-group xml:lang="ru"><kwd>двустворчатые моллюски</kwd><kwd>Annuliconcha</kwd><kwd>Lineaspina</kwd><kwd>распространение</kwd><kwd>оледенения</kwd><kwd>карбон</kwd><kwd>пермь</kwd><kwd>изменение палеоклимата</kwd></kwd-group><funding-group><funding-statement xml:lang="ru">Исследование выполнено в рамках госзаданий ГИН РАН и СВКНИИ ДВО РАН.</funding-statement></funding-group></article-meta></front><body></body><back><ref-list><ref id="B1"><label>1.</label><mixed-citation>Астафьева М.М. 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