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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 custom-type="elpub" pub-id-type="custom">geomorf-2618</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>Научные сообщения</subject></subj-group><subj-group subj-group-type="section-heading" xml:lang="en"><subject>Short communications</subject></subj-group></article-categories><title-group><article-title>Влияние палеогеографических условий голоцена на эволюцию карста в бассейне нижней Оки</article-title><trans-title-group xml:lang="en"><trans-title>Holocene environment impact on the karst evolution in the lower Oka drainage basin</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>Копосов</surname><given-names>Е. В.</given-names></name><name name-style="western" xml:lang="en"><surname>Koposov</surname><given-names>E. V.</given-names></name></name-alternatives><xref ref-type="aff" rid="aff-1"/></contrib></contrib-group><aff xml:lang="ru" id="aff-1"><institution>ПНИИИС</institution><country>Russian Federation</country></aff><pub-date pub-type="collection"><year>1986</year></pub-date><pub-date pub-type="epub"><day>09</day><month>11</month><year>2022</year></pub-date><volume>0</volume><issue>2</issue><issue-title>Геоморфология</issue-title><fpage>59</fpage><lpage>64</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Копосов Е.В., 2022</copyright-statement><copyright-year>2022</copyright-year><copyright-holder xml:lang="ru">Копосов Е.В.</copyright-holder><copyright-holder xml:lang="en">Koposov E.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://geomorphology.igras.ru/jour/article/view/2618">https://geomorphology.igras.ru/jour/article/view/2618</self-uri><abstract><p>Palynological studies together with radiocarbon dating of the deposits in sinkholes permit to reconstruct paleogeographic conditions during various periods of the Holocene in the lower reaches of the Oka River. The Holocene karst is shown to be controlled by paleoenvironments.</p></abstract><trans-abstract xml:lang="en"><p>Palynological studies together with radiocarbon dating of the deposits in sinkholes permit to reconstruct paleogeographic conditions during various periods of the Holocene in the lower reaches of the Oka River. The Holocene karst is shown to be controlled by paleoenvironments.</p></trans-abstract></article-meta></front><back><ref-list><title>References</title></ref-list><fn-group><fn fn-type="conflict"><p>The authors declare that there are no conflicts of interest present.</p></fn></fn-group></back></article>
