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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">litosphere</journal-id><journal-title-group><journal-title xml:lang="ru">Литосфера</journal-title><trans-title-group xml:lang="en"><trans-title>LITHOSPHERE (Russia)</trans-title></trans-title-group></journal-title-group><issn pub-type="ppub">1681-9004</issn><issn pub-type="epub">2500-302X</issn><publisher><publisher-name>A.N. Zavaritsky Institute of Geology and Geochemistry</publisher-name></publisher></journal-meta><article-meta><article-id pub-id-type="doi">10.24930/2500-302X-2024-24-6-986-1013</article-id><article-id custom-type="elpub" pub-id-type="custom">litosphere-2192</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>Статьи</subject></subj-group><subj-group subj-group-type="section-heading" xml:lang="en"><subject>Articles</subject></subj-group></article-categories><title-group><article-title>Ландшафтно-климатические обстановки формирования средне-, верхнеголоценовых отложений на северо-западе Большеземельской тундры (в долине р. Куи)</article-title><trans-title-group xml:lang="en"><trans-title>Depositional environment of the Middle- and Upper-Holocene sediments in the North-West of the Bol’shezemel’skaya tundra (in the Kuya river valley)</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>Голубева</surname><given-names>Ю. В.</given-names></name><name name-style="western" xml:lang="en"><surname>Golubeva</surname><given-names>Yu. V.</given-names></name></name-alternatives><bio xml:lang="ru"><p>167982, г. Сыктывкар, ул. Первомайская, 54</p></bio><bio xml:lang="en"><p>Yulia V. Golubeva</p><p>54 Pervomaiskaya st., Syktyvkar 167982</p></bio><email xlink:type="simple">yvgolubeva@geo.komisc.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>Марченко-Вагапова</surname><given-names>Т. И.</given-names></name><name name-style="western" xml:lang="en"><surname>Marchenko-Vagapova</surname><given-names>T. I.</given-names></name></name-alternatives><bio xml:lang="ru"><p>167982, г. Сыктывкар, ул. Первомайская, 54</p></bio><bio xml:lang="en"><p>Tatyana I. Marchenko-Vagapova</p><p>54 Pervomaiskaya st., Syktyvkar 167982</p></bio><xref ref-type="aff" rid="aff-1"/></contrib><contrib contrib-type="author" corresp="yes"><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Исаков</surname><given-names>В. А.</given-names></name><name name-style="western" xml:lang="en"><surname>Isakov</surname><given-names>V. A.</given-names></name></name-alternatives><bio xml:lang="ru"><p>167982, г. Сыктывкар, ул. Первомайская, 54</p></bio><bio xml:lang="en"><p>Vladislav A. Isakov</p><p>54 Pervomaiskaya st., Syktyvkar 167982</p></bio><xref ref-type="aff" rid="aff-1"/></contrib></contrib-group><aff-alternatives id="aff-1"><aff xml:lang="ru"><institution>Институт геологии им. академика Н.П. Юшкина ФИЦ Коми НЦ УрО РАН</institution><country>Россия</country></aff><aff xml:lang="en"><institution>N.P. Yushkin Institute of Geology, FRC Komi SC UB RAS</institution><country>Russian Federation</country></aff></aff-alternatives><pub-date pub-type="collection"><year>2024</year></pub-date><pub-date pub-type="epub"><day>15</day><month>01</month><year>2025</year></pub-date><volume>24</volume><issue>6</issue><fpage>986</fpage><lpage>1013</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Голубева Ю.В., Марченко-Вагапова Т.И., Исаков В.А., 2025</copyright-statement><copyright-year>2025</copyright-year><copyright-holder xml:lang="ru">Голубева Ю.В., Марченко-Вагапова Т.И., Исаков В.А.</copyright-holder><copyright-holder xml:lang="en">Golubeva Y.V., Marchenko-Vagapova T.I., Isakov V.A.</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://www.lithosphere.ru/jour/article/view/2192">https://www.lithosphere.ru/jour/article/view/2192</self-uri><abstract><p>Объект исследований. Аллювиальные и озерно-болотные отложения среднего и верхнего голоцена нижнего течения р. Куи – правого притока р. Печоры (Ненецкий автономный округ, Большеземельская тундра). Цель. Изучение образований пойменно-руслового комплекса для их литостратиграфического расчленения и реконструкции ландшафтно-климатических условий седиментации. Материал и методы. Исследовались текстурно-структурные особенности осадков пойменно-руслового комплекса с помощью гранулометрического и минералогического анализов. Морфоструктурные элементы рельефа выявлялись по спутниковым космоснимкам высокого разрешения и цифровой модели рельефа ArcticDEM. Представлены результаты спорово-пыльцевого и диатомового анализов, сопровождаемые радиоуглеродным датированием. Результаты. Выделены литотипы отложений голоцена, слагающие долину в нижнем течении р. Куи, и представлена хронология палеогеографических событий в районе исследований. Построена геолого-геоморфологическая схема пойменно-руслового комплекса долины р. Куи. Реконструирована динамика растительности и климата в среднем и позднем голоцене на основе палиностратиграфического расчленения аллювиальных и озерно-болотных осадков. Получены новые данные, подтверждающие мнение о расположении нижней границы позднесубатлантического периода, соотносимого с малым ледниковым периодом, на уровне 800 л. н. Выводы. Формирование пойменно-руслового комплекса происходило в четыре этапа, а слагающие его отложения отнесены к русловой, озерной, озерно-болотной и пойменной фациям. По морфометрическим признакам в геоморфологическом строении долины реки выделен эрозионно-аккумулятивный рельеф надпойменной террасы, высокой и низкой пойм. Прослежены изменения растительности: от тундровых сообществ в наиболее холодных условиях раннего суббореала, сменившихся лесами среднетаежного типа в суббореальный термический максимум, датированный 3360 ± 70 л. н. (3602 кал. л. н.), до современных лесотундровых и южно-тундровых сообществ. Пойменные отложения формировались в мелководных слабоминерализованных, заболачивающихся водоемах.</p></abstract><trans-abstract xml:lang="en"><p>Research subject. The Holocene alluvium, lake-bog and oxbow-lake sediments in the lower reaches of the Kuya river valley, the right tributary of the Pechora river (Nenets Autonomous Okrug, northwest of the Bol`shezemel`skaya tundra). Aim. Investigation of the morphological types of fluvial formations, their lithostratigraphic subdivision, and reconstruction of the environmental conditions of sedimentation. Materials and methods. The sediments texture and structure features of the floodplain-channel complex were studied by granulometric and mineralogical analyses. The morphostructural features of the relief were identified by high-resolution satellite imagery and an ArcticDEM digital relief model. The spore-pollen and diatom analyses and radiocarbon dating results are presented. Results. The lithotypes of Holocene sediments that make up the valley in the lower reaches of the Kuya River are distinguished, and the chronology of paleogeographic events in the study area is presented. A geological and geomorphological scheme of the floodplain-channel complex of the Kuya River valley is constructed. The geological profile of alluvium and underlying sediments is constructed. Reconstructions of vegetation and climate dynamics in the mid- and late-Holocene based on the palynostratigraphic subdivision of alluvium sediments is carried out. The lower boundary of the late Sub-Atlantic period, correlated with the Little Ice Age, is clarified. Conclusions. The formation of the floodplain-channel complex occurred in four stages, with its constituent deposits being attributed to the channel, lacustrine, bog, and floodplain facies. According to morphometric features in the geomorphological structure of the river valley, an erosion-accumulative relief of the above-floodplain terraces of high and low floodplains is identified. The following stages of vegetation changes are traced: from tundra communities in the coldest conditions of the early Subboreal, which were replaced by forests of the middle taiga type to the Subboreal thermal maximum, dated 3360 ± 70 years ago (3602 cal. BP) to modern forest-tundra and south-tundra communities. The formation fluvial plain sediments occurred in shallow, slightly mineralized, and waterlogged reservoirs.</p></trans-abstract><kwd-group xml:lang="ru"><kwd>палеогеография</kwd><kwd>голоцен</kwd><kwd>литологический состав</kwd><kwd>спорово-пыльцевой анализ</kwd><kwd>диатомовый анализ</kwd><kwd>реконструкция растительности и климата</kwd><kwd>Большеземельская тундра</kwd></kwd-group><kwd-group xml:lang="en"><kwd>paleogeography</kwd><kwd>Holocene</kwd><kwd>lithological composition</kwd><kwd>spore-pollen analysis</kwd><kwd>diatom analysis</kwd><kwd>vegetation and climate reconstruction</kwd><kwd>Bolʼshezemelʼskaya tundra</kwd></kwd-group><funding-group><funding-statement xml:lang="ru">Работа выполнена при финансовой поддержке РНФ, проект № 23-27-00281</funding-statement><funding-statement xml:lang="en">The work was supported by the Russian Science Foundation, project No. 23-27-00281</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">Агаджанян А.К., Борисов Б.А., Брайцева О.А. 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