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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">geomorf</journal-id><journal-title-group><journal-title xml:lang="ru">Геоморфология и палеогеография</journal-title><trans-title-group xml:lang="en"><trans-title>Geomorfologiya i Paleogeografiya</trans-title></trans-title-group></journal-title-group><issn pub-type="ppub">2949-1789</issn><issn pub-type="epub">2949-1797</issn><publisher><publisher-name></publisher-name></publisher></journal-meta><article-meta><article-id pub-id-type="doi">10.31857/10.7868/S2949179726020052</article-id><article-id custom-type="elpub" pub-id-type="custom">geomorf-3734</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>Палеоэкология и динамика культуры в плейстоцене Евразии</subject></subj-group></article-categories><title-group><article-title>Хроностратиграфия, палеопедогенез и региональные корреляции почвенно-осадочных серий среднепалеолитического памятника Хотылёво I</article-title><trans-title-group xml:lang="en"><trans-title>Chronostratigraphy, paleopedogenesis and regional correlations in the soil-sedimentary sequences of the Khotylevo I Middle Paleolithic site</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>Коркка</surname><given-names>М. А.</given-names></name><name name-style="western" xml:lang="en"><surname>Korkka</surname><given-names>M. A.</given-names></name></name-alternatives><email xlink:type="simple">maria.a.korkka@gmail.com</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>Седов</surname><given-names>С. Н.</given-names></name><name name-style="western" xml:lang="en"><surname>Sedov</surname><given-names>S. N.</given-names></name></name-alternatives><xref ref-type="aff" rid="aff-2"/></contrib><contrib contrib-type="author" corresp="yes"><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Романис</surname><given-names>Т. В.</given-names></name><name name-style="western" xml:lang="en"><surname>Romanis</surname><given-names>T. V.</given-names></name></name-alternatives><xref ref-type="aff" rid="aff-3"/></contrib><contrib contrib-type="author" corresp="yes"><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Хайн</surname><given-names>М.</given-names></name><name name-style="western" xml:lang="en"><surname>Hein</surname><given-names>M.</given-names></name></name-alternatives><xref ref-type="aff" rid="aff-4"/></contrib><contrib contrib-type="author" corresp="yes"><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Савельева</surname><given-names>Л. А.</given-names></name><name name-style="western" xml:lang="en"><surname>Savelieva</surname><given-names>L. A.</given-names></name></name-alternatives><xref ref-type="aff" rid="aff-1"/></contrib><contrib contrib-type="author" corresp="yes"><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Иванов</surname><given-names>Я. Д.</given-names></name><name name-style="western" xml:lang="en"><surname>Ivanov</surname><given-names>Ya. D.</given-names></name></name-alternatives><xref ref-type="aff" rid="aff-5"/></contrib><contrib contrib-type="author" corresp="yes"><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Очередной</surname><given-names>А. К.</given-names></name><name name-style="western" xml:lang="en"><surname>Otcherednoy</surname><given-names>A. K.</given-names></name></name-alternatives><xref ref-type="aff" rid="aff-5"/></contrib></contrib-group><aff-alternatives id="aff-1"><aff xml:lang="ru"><institution>Санкт-Петербургский государственный университет, Санкт-Петербург</institution><country>Россия</country></aff><aff xml:lang="en"><institution>Saint Petersburg State University, Saint Petersburg</institution><country>Russian Federation</country></aff></aff-alternatives><aff-alternatives id="aff-2"><aff xml:lang="ru"><institution>Институт геологии Национального автономного университета Мексики, Койоакан, Мехико, Мексика&#13;
Институт криосферы Земли, ФИЦ ТюмНЦ СО РАН, Тюмень, Россия</institution><country>Мексика</country></aff><aff xml:lang="en"><institution>Institute of Geology, National Autonomous University of Mexico, University City, Coyoacán, Mexico City</institution><country>Mexico</country></aff></aff-alternatives><aff-alternatives id="aff-3"><aff xml:lang="ru"><institution>Институт Мерзлотоведения им. П. И. Мельникова СО РАН, Якутск</institution><country>Россия</country></aff><aff xml:lang="en"><institution>Melnikov Permafrost Institute, Yakutsk</institution><country>Russian Federation</country></aff></aff-alternatives><aff-alternatives id="aff-4"><aff xml:lang="ru"><institution>Люнебургский университет Лёйфана, Люнебург</institution><country>Германия</country></aff><aff xml:lang="en"><institution>Leuphana University Lüneburg, Lüneburg</institution><country>Germany</country></aff></aff-alternatives><aff-alternatives id="aff-5"><aff xml:lang="ru"><institution>Институт истории материальной культуры РАН, Санкт-Петербург</institution><country>Россия</country></aff><aff xml:lang="en"><institution>Institute for the History of Material Culture RAS, Saint Petersburg</institution><country>Russian Federation</country></aff></aff-alternatives><pub-date pub-type="collection"><year>2026</year></pub-date><pub-date pub-type="epub"><day>03</day><month>07</month><year>2026</year></pub-date><volume>57</volume><issue>2</issue><fpage>260</fpage><lpage>284</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Коркка М.А., Седов С.Н., Романис Т.В., Хайн М., Савельева Л.А., Иванов Я.Д., Очередной А.К., 2026</copyright-statement><copyright-year>2026</copyright-year><copyright-holder xml:lang="ru">Коркка М.А., Седов С.Н., Романис Т.В., Хайн М., Савельева Л.А., Иванов Я.Д., Очередной А.К.</copyright-holder><copyright-holder xml:lang="en">Korkka M.A., Sedov S.N., Romanis T.V., Hein M., Savelieva L.A., Ivanov Y.D., Otcherednoy A.K.</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://geomorphology.igras.ru/jour/article/view/3734">https://geomorphology.igras.ru/jour/article/view/3734</self-uri><abstract><p>Почвенно-осадочная серия археологического памятника среднего палеолита Хотылёво I включает пять педогенетических уровней MIS 5a–MIS 1: ранневалдайские органогенные озерно-болотные отложения MIS5a и связанные с ними синседиментационные гидроморфные палеопочвы; педокомплекс интерстадиальных почв MIS 3, состоящий из двух развитых палеопочв, одна из которых имеет сложную полигенетическую историю формирования; блок эфемерных, слаборазвитых глеевых палеопочвенных горизонтов MIS 2; этап поздневалдайского почвообразования, без ярких признаков оглеения или криогенеза, в виде горизонта Bw трубчевской палеопочвы. На основании выделенных палеопочвенных маркеров был составлен сводный хроностратиграфический почвенно-осадочный разрез памятника Хотылёво I, который дополняет схему, разработанную А. А. Величко и коллегами в 1961–1997 гг., являясь более подробным в интервале MIS 3–MIS 2. Также была проведена локальная корреляция почвенно-осадочной серии среднего и позднего валдая с разрезами памятников верхнего палеолита Хотылёво 2 и Хотылёво 6. Эта корреляция ставит под сомнение отнесение педоседиментов, вмещающих верхнепалеолитические индустрии, к крутицкой фазе мезинского педокомплекса (MIS 5a), которое предполагали исследователи упомянутых памятников. По результатам наших исследований, данные педоседименты соотносятся с гумусово-аккумулятивным горизонтом палеопочвы MIS 3, что лучше согласуется с представлениями о возрасте верхнего палеолита Восточной Европы.</p></abstract><trans-abstract xml:lang="en"><p>The soil-sedimentary sequence of the Middle Paleolithic archaeological site Khotylevo I includes five pedogenetic levels MIS 5a–MIS 2: MIS 5a Early Valday oxbow lake gyttja and related synsedimentary hydromorphic paleosols; a sequence of interstadial MIS 3 soils consisting of two well-developed paleosols, one of which has a complex polygenetic history of formation; a block of ephemeral, poorly developed MIS 2 gleyic paleosol horizons; and a Late Valday pedogenesis stage, without prominent signs of gleization or cryogenesis, presented by a Bw horizon of Trubchevskaya soil. Based on the highlighted paleosol markers, we compiled a consolidated soil-stratigraphic profile of the Khotylevo I site, which supplements the scheme developed by A. A. Velichko and colleagues in 1961–1997, being more detailed in the MIS 3–MIS 2 interval. The Middle and Late Valday soil-sedimentary sequence presented in the section was used as a tool for local correlation with the Upper Paleolithic sites Khotylevo 2 and Khotylevo 6. This correlation casts doubt on the assignment of pedosediments which contain Upper Paleolithic industries to the Krutitskaya phase of the Mezin soil complex (MIS 5a) by the researchers of the aforementioned sites. Based on the results of our research, these pedosediments correlate with the humus-accumulative horizon of the MIS 3 paleosol, which more closely agrees with the understanding of the age of Eastern Europe’s Upper Paleolithic.</p></trans-abstract><kwd-group xml:lang="ru"><kwd>палеопочвы MIS 3</kwd><kwd>полигенез почв</kwd><kwd>поздний плейстоцен</kwd><kwd>палеолит</kwd><kwd>радиоуглеродное датирование</kwd></kwd-group><kwd-group xml:lang="en"><kwd>MIS 3 paleosols</kwd><kwd>paleosol polygenesis</kwd><kwd>Late Pleistocene</kwd><kwd>radiocarbon dating</kwd><kwd>micromorphology</kwd></kwd-group><funding-group><funding-statement xml:lang="ru">Исследование проводится в рамках ФНИ ГАН “Север Евразии в каменном веке: проблемы расселения человека, культурной адаптации и технологического развития” (FMZF-2025- 0007). Полевые работы поддержаны общественным движением поддержки науки “Проекты Дробышевского”. Микроморфологическое исследование почв выполнено при поддержке базового проекта 126020516709-1. Авторы выражают глубокую благодарность Е. И. Куренковой, К. Н. Степановой и К. Н. Гаврилову за активное обсуждение материалов палеолитических памятников и за совместную работу по комплексному изучению и интерпретации позднеплейстоценовых отложений Хотылёво; а также Д. К. Будник за активную помощь на всех этапах подготовки этой публикации. Изучение палеопочв Хотылёво было бы невозможно без постоянной надежной поддержки сотрудников ВДЭ ИИМК РАН, ХАЭ ИА РАН и НПЦ “Хотылёво”. Авторы благодарят Лабораторию геоморфологических и палеогеографических исследований полярных регионов и Мирового океана им. В. Кёппена, ИНоЗ СПбГУ, за полученные радиоуглеродные данные</funding-statement><funding-statement xml:lang="en">This work was supported by the Program of Fundamental Scientific Research of the State Academies of Sciences “The Eurasian north in the Stone Age: problems of human dispersal, cultural adaptation and technological development” (State Assignment No. FMZF-2025-0007). Field work is supported by the social movement for the popularization of science “Drobyshevsky Projects”. Study of soil micromorphology was supported by base project 126020516709-1. The authors extend their deep gratitude to E. I. Kurenkova, K. N. Stepanova and K. N. Gavrilov for their active discussion of Paleolithic site materials and for collaborating in the comprehensive study and interpretation of Late Pleistocene deposits in Khotylevo, as well as D. K. Boudnik for actively helping during all stages of preparation of this publication. The study of Khotylevo paleosols would not be possible without the unceasing reliable support of our colleagues from the Verkhnedesninskaya Ekspeditsiya (Upper Desna Expedition) of the RAS Institute for the History of Material Culture, the Khotylevskaya Arkheologicheskaya Ekspeditsiya (Khotylevo Archaeological Expedition) of the RAS Institute of Archaeology, and the Khotylevo Center for Applied Research. The authors thank the Köppen Laboratory for the Geomorphological and Paleogeographic Research of the Polar Region and the World Ocean, Institute of Earth Sciences, Saint Petersburg State University, for the obtained radiocarbon data.</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">Арсланов Х.А. (1992) Геохронологическая шкала позднего плейстоцена Русской равнины. В сб.: Геохронология четвертичного периода. М.: Наука. 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