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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/S0435428121030093</article-id><article-id custom-type="elpub" pub-id-type="custom">geomorf-1556</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>Article</subject></subj-group></article-categories><title-group><article-title>Динамика ландшафтов и климата в Центральной и Восточной Европе в голоцене – прогнозные оценки изменения природной среды</article-title><trans-title-group xml:lang="en"><trans-title>Landscape and climate dynamics in Central and Eastern Europe during the Holocene – assessment of future environmental changes</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>Новенко</surname><given-names>Е. Ю.</given-names></name><name name-style="western" xml:lang="en"><surname>Novenko</surname><given-names>E. Yu.</given-names></name></name-alternatives><bio xml:lang="ru"><p>географический факультет</p><p>Москва</p></bio><bio xml:lang="en"><p>Faculty of Geography</p><p>Moscow</p></bio><email xlink:type="simple">lenanov@mail.ru</email><xref ref-type="aff" rid="aff-1"/></contrib></contrib-group><aff-alternatives id="aff-1"><aff xml:lang="ru"><institution>Московский государственный университет им. М.В. Ломоносова; Институт географии РАН</institution><country>Россия</country></aff><aff xml:lang="en"><institution>Lomonosov Moscow State University; Institute of Geography RAS</institution><country>Russian Federation</country></aff></aff-alternatives><pub-date pub-type="collection"><year>2021</year></pub-date><pub-date pub-type="epub"><day>12</day><month>10</month><year>2021</year></pub-date><volume>52</volume><issue>3</issue><issue-title>Геоморфология</issue-title><fpage>24</fpage><lpage>47</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Новенко Е.Ю., 2021</copyright-statement><copyright-year>2021</copyright-year><copyright-holder xml:lang="ru">Новенко Е.Ю.</copyright-holder><copyright-holder xml:lang="en">Novenko E.Y.</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/1556">https://geomorphology.igras.ru/jour/article/view/1556</self-uri><abstract><p>В статье представлен обзор ландшафтно-климатических реконструкций для лесной зоны Центральной и Восточной Европы, выполненных различными методами, в сопоставлении с основными этапами развития рельефа и осадконакопления в голоцене. Рассмотрены ожидаемые климатические изменения согласно сценариям репрезентативных траекторий концентраций парниковых газов, разработанных Межправительственной группой экспертов по изменению климата (МГЭИК). Анализ данных показал, что в раннем голоцене (11.7–8.2 тыс. кал. л. н.) в условиях быстрого потепления климата происходила трансформация всех ландшафтных компонентов, значительные изменения претерпели рельефообразующие процессы. В этот период происходила деградация многолетней мерзлоты, сформировалась реликтовая криогенная морфоскульптура, кардинальные изменения претерпели гидрологический режим рек и флювиальное рельефообразование, имело место постепенное ослабление эоловых процессов. В среднем голоцене для временного интервала 8.2–5.7 тыс. кал. л. н. были характерны максимальная теплообеспеченность по сравнению с остальными периодами голоцена и ослабление градиента температур в направлении с запада на восток. В это время в среднеширотной области Европы существовала единая зона широколиственных лесов. Начиная с 5.7 тыс. кал. л. н., похолодание климата привело к усилению секторной дифференциации растительного покрова. В западных районах начинается экспансия бука и граба, на востоке увеличивается роль ели в лесных сообществах. Климатические реконструкции для позднего голоцена (4.2 тыс. кал. л. н. – настоящее время) показали, что на фоне общего тренда к снижению теплообеспеченности выделяются периоды потеплений и похолоданий. Сформировался современный ландшафтный покров, усилилось влияние антропогенного фактора. Согласно данным палеоботанических, изотопно-геохимических и палеогидрологических исследований в различных регионах Центральной и Восточной Европы в периоды потеплений климат был более сухой, чем в настоящее время, преимущественно за счет изменения баланса осадки/испарение, а похолодания сопровождались ростом увлажнения, увеличением частоты и высоты весенних половодий с соответствующим усилением осадконакопления на поймах рек, формированием вторичных врезов в оврагах и балках. Считая климатические реконструкции для голоцена изучаемой территории сценариями возможных изменений климата в текущем столетии, можно ожидать, что рост температур, особенно в летний период, будет причиной возрастания частоты засух и опасных геоморфологических процессов, связанных с неравномерностью выпадения осадков.</p></abstract><trans-abstract xml:lang="en"><p>The paper presents a review of the Holocene landscape and climate reconstructions for the forest zone of Central and Eastern Europe revealed from various proxies and comparison of the data obtained with the main stages of relief development and sedimentation during the Holocene. Projections of expected climate change are discussed according to IPCC scenarios (Coupled Model Intercomparison Project, Phase 5; Representative Concentration Pathways for possible range of radiative forcing). Analysis of the data showed that in the Early Holocene (11.7–8.2 ka BP), a rapid climate warming led to crucial transformation when all of landscape components were transformed, and relief-forming processes underwent significant changes. In the Middle Holocene, the time interval of 8.2–5.7 ka BP was characterized by the maximum heat supply in comparison with the whole Holocene and the weakening of the temperature gradient in the direction from west to east. At this time, a continuous zone of broad-leaved forests occupied the mid-latitude regions of Europe. Starting from 5.7 ka BP, the climatic cooling led to the sectoral differentiation of vegetation cover. In the western regions, the expansion of beech and hornbeam began, in the east, and the role of spruce in forest communities increased. Climate reconstructions for the Late Holocene (4.2 ka BP – present) have shown that against the background of the general climate trend towards a decrease in heat supply, periods of warming and cooling are distinguished. During the late Holocene the modern landscape cover was formed, the influence of the anthropogenic factor increased. According to paleobotanical, isotope-geochemical and paleohydrological studies in various regions of Central and Eastern Europe, the climate was drier than at present during periods of warming, mainly due to changes in the precipitation/evaporation balance, and climate cooling was accompanied by an increase in moisture. Bearing in mind the Holocene climate reconstructions as a possible scenario of climate changes during the current century, one can expect that an increase in temperatures, especially in the summer period, will cause the increase in the frequency of droughts and natural disasters, associated with irregular rainfall.</p></trans-abstract><kwd-group xml:lang="ru"><kwd>палеоклиматические реконструкции</kwd><kwd>палеогеоморфология</kwd><kwd>палеогеография</kwd><kwd>Европейская территория России</kwd><kwd>лесная зона</kwd></kwd-group><kwd-group xml:lang="en"><kwd>paleoclimatic reconstructions</kwd><kwd>paleogeomorphology</kwd><kwd>paleogeography</kwd><kwd>European part of Russia</kwd><kwd>forest zone</kwd></kwd-group><funding-group><funding-statement xml:lang="ru">Исследование выполнено при поддержке проекта РФФИ 19-15-50126.</funding-statement><funding-statement xml:lang="en">The study was funded by the Russian Foundation of Basic Research, № 19-15-50126.</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">Динамика ландшафтных компонентов и внутренних морских бассейнов Северной Евразии за последние 130000 лет (общая палеогеография). 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