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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">sergeogr</journal-id><journal-title-group><journal-title xml:lang="ru">Известия Российской академии наук. Серия географическая</journal-title><trans-title-group xml:lang="en"><trans-title>Izvestiya Rossiiskoi Akademii Nauk. Seriya Geograficheskaya</trans-title></trans-title-group></journal-title-group><issn pub-type="ppub">2587-5566</issn><issn pub-type="epub">2658-6975</issn><publisher><publisher-name></publisher-name></publisher></journal-meta><article-meta><article-id pub-id-type="doi">10.31857/S2587-55662019578-95</article-id><article-id custom-type="elpub" pub-id-type="custom">sergeogr-953</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>Эволюция природных систем</subject></subj-group><subj-group subj-group-type="section-heading" xml:lang="en"><subject>Evolution of Natural System</subject></subj-group></article-categories><title-group><article-title>Ладожская трансгрессия и ландшафты второй половины голоцена в Южном Приладожье  (по данным изучения археологического памятника Подолье-1)</article-title><trans-title-group xml:lang="en"><trans-title>Ladoga Transgression and Landscapes of the holocene Second half  in the Southern Ladoga area (according to the Study  of the archaeological Site Podolje-1)</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>Сапелко</surname><given-names>Т. В.</given-names></name><name name-style="western" xml:lang="en"><surname>Sapelko</surname><given-names>T. V.</given-names></name></name-alternatives><email xlink:type="simple">tsapelko@mail.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>Гусенцова</surname><given-names>Т. М.</given-names></name><name name-style="western" xml:lang="en"><surname>Gusentsova</surname><given-names>T. M.</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>Кулькова</surname><given-names>М. А.</given-names></name><name name-style="western" xml:lang="en"><surname>Kulkova</surname><given-names>M. A.</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>Лудикова</surname><given-names>А. В.</given-names></name><name name-style="western" xml:lang="en"><surname>Ludikova</surname><given-names>A. V.</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>Денисенков</surname><given-names>В. П.</given-names></name><name name-style="western" xml:lang="en"><surname>Denisenkov</surname><given-names>V. P.</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>Корнеенкова</surname><given-names>Н. Ю.</given-names></name><name name-style="western" xml:lang="en"><surname>Korneenkova</surname><given-names>N. Yu.</given-names></name></name-alternatives><xref ref-type="aff" rid="aff-1"/></contrib></contrib-group><aff-alternatives id="aff-1"><aff xml:lang="ru"><institution>Институт озероведения РАН</institution><country>Россия</country></aff><aff xml:lang="en"><institution>Institute of Limnology Russian Academy of Sciences</institution><country>Russian Federation</country></aff></aff-alternatives><aff-alternatives id="aff-2"><aff xml:lang="ru"><institution>АНО НИИ культурного и природного наследия</institution><country>Россия</country></aff><aff xml:lang="en"><institution>ANO Scientific and Research Institute for Cultural and Natural Heritage</institution><country>Russian Federation</country></aff></aff-alternatives><aff-alternatives id="aff-3"><aff xml:lang="ru"><institution>Российский государственный педагогический университет им. А.И. Герцена</institution><country>Россия</country></aff><aff xml:lang="en"><institution>Herzen State Pedagogical University</institution><country>Russian Federation</country></aff></aff-alternatives><aff-alternatives id="aff-4"><aff xml:lang="ru"><institution>Санкт-Петербургский государственный университет</institution><country>Россия</country></aff><aff xml:lang="en"><institution>St. Petersburg State University</institution><country>Russian Federation</country></aff></aff-alternatives><pub-date pub-type="collection"><year>2019</year></pub-date><pub-date pub-type="epub"><day>10</day><month>11</month><year>2019</year></pub-date><volume>0</volume><issue>5</issue><fpage>78</fpage><lpage>95</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Сапелко Т.В., Гусенцова Т.М., Кулькова М.А., Лудикова А.В., Денисенков В.П., Корнеенкова Н.Ю., 2019</copyright-statement><copyright-year>2019</copyright-year><copyright-holder xml:lang="ru">Сапелко Т.В., Гусенцова Т.М., Кулькова М.А., Лудикова А.В., Денисенков В.П., Корнеенкова Н.Ю.</copyright-holder><copyright-holder xml:lang="en">Sapelko T.V., Gusentsova T.M., Kulkova M.A., Ludikova A.V., Denisenkov V.P., Korneenkova N.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://izvestia.igras.ru/jour/article/view/953">https://izvestia.igras.ru/jour/article/view/953</self-uri><abstract><p>В Южном Приладожье проведены комплексные исследования нового археологического памятника Подолье-1, расположенного в 4-х км от Ладожского озера. Исследования включали в себя археологический, литологический, геохимический, палинологический, ботанический, диатомовый и радиоуглеродный анализы. В результате получены новые данные, уточняющие развитие Ладожской трансгрессии во второй половине голоцена в Южном Приладожье. Установлена зависимость формирования культурных слоев от изменения гидродинамических условий его существования. Нижний культурный слой формировался перед началом Ладожской трансгрессии. Верхний культурный слой приурочен к  завершению трансгрессивной стадии. На абсолютных отметках от 10 до 12 м над ур.м. в Южном Приладожье с 6480 до 4446 кал. лет назад формировались торфяники. При этом 6480–5944 кал. лет назад отмечен период некоторого увлажнения климата. 4534–4446 кал. лет назад на территории памятника фиксируется начало Ладожской трансгрессии. завершение Ладожской трансгрессии на рассматриваемой территории отмечается в начале субатлантического периода.</p></abstract><trans-abstract xml:lang="en"><p>In Southern Ladoga area, we studied the new archaeological site Podolje 1, located 4 km from Lake Ladoga. Studies included archaeological, lithological, geochemical, pollen, botanical, diatom and radiocarbon analyzes. As a result, new data were obtained that specified the development of the Ladoga transgression in the second half of the Holocene in the Southern Ladoga area. The dependence of the formation of cultural layers on changes in the hydrodynamic conditions of its existence is established. The lower cultural layer was formed before the beginning of the Ladoga transgression. The upper cultural layer was formed after the transgressive stage. At absolute elevations from 10 to 12 m above Sea level in the Southern Ladoga area from 6480 to 4446 cal. BP peatlands were formed. In this case, 6480–5944 cal. BP there was a period of some humid climate. 4534–4446 cal. BP, the beginning of the Ladoga transgression is recorded on the territory of the site. The completion of the Ladoga transgression was marked at the beginning of the Subatlantic period.</p></trans-abstract><kwd-group xml:lang="ru"><kwd>Ладожская трансгрессия</kwd><kwd>торфяники</kwd><kwd>археологический памятник</kwd><kwd>голоцен</kwd><kwd>палинология</kwd><kwd>диатомовые водоросли</kwd><kwd>ботанический анализ торфа</kwd><kwd>геохимия</kwd></kwd-group><kwd-group xml:lang="en"><kwd>Ladoga transgression</kwd><kwd>peatlands</kwd><kwd>archaeological site</kwd><kwd>Holocene</kwd><kwd>palynology</kwd><kwd>diatoms</kwd><kwd>macrofossils</kwd><kwd>geochemistry</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">Александровский А.Л., Арсланов Х.А., Давыдова Н.Н., Долуханов П.М., Зайцева Г.И., Кирпичников А.Н., Кузнецов Д.Д., Лавенто М., Лудикова А.В., Носов Е.Н., Савельева Л.А., Сапелко Т.В., Субетто Д.А. 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