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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">dan</journal-id><journal-title-group><journal-title xml:lang="ru">Доклады Национальной академии наук Беларуси</journal-title><trans-title-group xml:lang="en"><trans-title>Doklady of the National Academy of Sciences of Belarus</trans-title></trans-title-group></journal-title-group><issn pub-type="ppub">1561-8323</issn><issn pub-type="epub">2524-2431</issn><publisher><publisher-name>The Republican Unitary Enterprise Publishing House "Belaruskaya Navuka"</publisher-name></publisher></journal-meta><article-meta><article-id pub-id-type="doi">10.29235/1561-8323-2019-63-3-350-359</article-id><article-id custom-type="elpub" pub-id-type="custom">dan-622</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>НАУКИ О ЗЕМЛЕ</subject></subj-group><subj-group subj-group-type="section-heading" xml:lang="en"><subject>EARTH SCIENCES</subject></subj-group></article-categories><title-group><article-title>Изменения в стратиграфических схемах неогеновых и четвертичных отложений Беларуси в связи с пересмотром границы между системами</article-title><trans-title-group xml:lang="en"><trans-title>Changes in stratigraphic charts of neogene and quaternary deposits of Belarus due to the revision of the boundary between systems</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>Матвеев</surname><given-names>А. В.</given-names></name><name name-style="western" xml:lang="en"><surname>Маtveyev</surname><given-names>A. V.</given-names></name></name-alternatives><bio xml:lang="ru"><p>Матвеев Алексей Васильевич – академик, д-р геол.-минералог. наук, профессор, гл. науч. сотрудник</p><p>ул. Ф. Скорины, 10, 220114, Минск, Республика Беларусь</p></bio><bio xml:lang="en"><p>Matveev Aleksej Vasil’evich – Academician, D. Sc. (Geology), Professor, Chief researcher</p><p>10, F. Skoryna Str., 220114, Minsk, Republic of Belarus</p></bio><email xlink:type="simple">matveyev@ecology.basnet.by</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>Рылова</surname><given-names>Т. Б.</given-names></name><name name-style="western" xml:lang="en"><surname>Rylova</surname><given-names>Т. B.</given-names></name></name-alternatives><bio xml:lang="ru"><p>Рылова Татьяна Борисовна – д-р геол.-минералог. наук, доцент, гл. науч. сотрудник</p><p>ул. Ф. Скорины, 10, 220114, Минск, Республика Беларусь</p></bio><bio xml:lang="en"><p>Rylova Tat’yana Borisovna – D. Sc. (Geology), Assistant professor, Chief researcher</p><p>10, F. Skoryna Str., 220114, Minsk, Republic of Belarus</p></bio><email xlink:type="simple">rylova@ecology.basnet.by</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>Демидова</surname><given-names>С. В.</given-names></name><name name-style="western" xml:lang="en"><surname>Demidova</surname><given-names>S. V.</given-names></name></name-alternatives><bio xml:lang="ru"><p>Демидова Светлана Владимировна – канд. геол.-минералог. наук, заместитель директора.</p><p>ул. Купревича, 7, 220141, Минск, Республика Беларусь</p></bio><bio xml:lang="en"><p>Demidova Svetlana Vladimirovna – Ph. D. (Geology), Deputy director</p><p>7, Kuprevich Str., 220141, Minsk, Republic of Belarus</p></bio><email xlink:type="simple">demidovasvet@mail.ru</email><xref ref-type="aff" rid="aff-2"/></contrib><contrib contrib-type="author" corresp="yes"><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Якубовская</surname><given-names>Т. В.</given-names></name><name name-style="western" xml:lang="en"><surname>Yakubovskaya</surname><given-names>Т. V.</given-names></name></name-alternatives><bio xml:lang="ru"><p>Якубовская Татьяна Васильевна – канд. геол.-минералог. наук, доцент</p><p>ул. Купревича, 7, 220141, Минск, Республика Беларусь</p></bio><bio xml:lang="en"><p>Yakubovskaya Tat’yana Vasil’evna – Ph. D. (Geology), Assistant Professor</p><p>7, Kuprevich Str., 220141, Minsk, Republic of Belarus</p></bio><email xlink:type="simple">tvyakub@tut.by</email><xref ref-type="aff" rid="aff-2"/></contrib></contrib-group><aff-alternatives id="aff-1"><aff xml:lang="ru"><institution>Институт природопользования Национальной академии наук Беларуси</institution></aff><aff xml:lang="en"><institution>Institute for Nature Management of the National Academy of Sciences of Belarus</institution></aff></aff-alternatives><aff-alternatives id="aff-2"><aff xml:lang="ru"><institution>Институт геологии Научно-производственного центра по геологии</institution></aff><aff xml:lang="en"><institution>Institute of Geology of the Research and Production Center for Geology</institution></aff></aff-alternatives><pub-date pub-type="collection"><year>2019</year></pub-date><pub-date pub-type="epub"><day>27</day><month>06</month><year>2019</year></pub-date><volume>63</volume><issue>3</issue><fpage>350</fpage><lpage>359</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Матвеев А.В., Рылова Т.Б., Демидова С.В., Якубовская Т.В., 2019</copyright-statement><copyright-year>2019</copyright-year><copyright-holder xml:lang="ru">Матвеев А.В., Рылова Т.Б., Демидова С.В., Якубовская Т.В.</copyright-holder><copyright-holder xml:lang="en">Маtveyev A.V., Rylova Т.B., Demidova S.V., Yakubovskaya Т.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://doklady.belnauka.by/jour/article/view/622">https://doklady.belnauka.by/jour/article/view/622</self-uri><abstract><p>В связи с решением Международного союза геологических наук о переносе нижней границы четвертичной системы/периода и плейстоценового отдела/эпохи с уровня 1,8 млн лет на уровень 2,58 млн лет (к основанию гелазского яруса/века плиоцена) вносятся изменения в Стратиграфические схемы неогеновых и четвертичных отложений Беларуси 2010 г. Неоген-четвертичная граница на территории Беларуси приведена в соответствие с Международной хроностратиграфической шкалой и проводится между холмечским горизонтом (аналог занклия и пьяченция, плиоцен) и дворецким горизонтом (аналог гелазия), перемещенным из плиоцена в основание нижнего плейстоцена квартера. Обоснование ее нового положения в разрезах выполнено по палеоботаническим данным. В региональные и местные подразделения стратиграфических схем неогена и квартера введены новые стратоны.</p></abstract><trans-abstract xml:lang="en"><p>Following the decision of the International Union of Geological Sciences on the transfer of the lower boundary of the Quaternary System/Period and the Pleistocene Series/Epoch from 1.8 Ma to 2.58 Ma (to the base of the Gelazian Stage/ Age of the Pliocene), the changes have been made in Stratigraphic charts of Neogene and Quaternary Deposits of Belarus (2010). The Neogene – Quaternary boundary in the territory of Belarus is aligned with the International Chronostratigraphic Chart and is made between the Kholmech horizon (analogue of Zanclean and Piacenzian, Pliocene) and the Dvorets horizon (analogue of Gelasian) displaced from the Pliocene to the lower base of the lowermost Pleistocene. Its new position in the sections is substantiated by paleobotanical data. New geological units were introduced into regional and local stratigraphic charts of the Neogene and Quaternary.</p></trans-abstract><kwd-group xml:lang="ru"><kwd>стратиграфическая схема</kwd><kwd>неогеновая система/период</kwd><kwd>четвертичная система/период</kwd><kwd>граница</kwd><kwd>гелазский ярус</kwd><kwd>дворецкий горизонт</kwd><kwd>палеоботанические исследования</kwd></kwd-group><kwd-group xml:lang="en"><kwd>stratigraphic chart</kwd><kwd>Neogene System/Period</kwd><kwd>Quaternary System/Period</kwd><kwd>boundary</kwd><kwd>Gelazian Stage</kwd><kwd>Dvorets horizon</kwd><kwd>palaeobotanical studies</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">Formal ratification of the Quaternary System/Period and the Pleistocene Series/Epoch with a base at 2.58 Ma / P. l. Gibbard [et al.] // J. Quat. 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