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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">aari</journal-id><journal-title-group><journal-title xml:lang="ru">Проблемы Арктики и Антарктики</journal-title><trans-title-group xml:lang="en"><trans-title>Arctic and Antarctic Research</trans-title></trans-title-group></journal-title-group><issn pub-type="ppub">0555-2648</issn><issn pub-type="epub">2618-6713</issn><publisher><publisher-name>Государственный научный центр Российской Федерации Арктический и антарктический научно-исследовательский институт</publisher-name></publisher></journal-meta><article-meta><article-id pub-id-type="doi">10.30758/0555-2648-2018-64-4-391-406</article-id><article-id custom-type="elpub" pub-id-type="custom">aari-111</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>ГЕОМОРФОЛОГИЯ И ЭВОЛЮЦИОННАЯ ГЕОГРАФИЯ</subject></subj-group><subj-group subj-group-type="section-heading" xml:lang="en"><subject>GEOMORPHOLOGY AND EVOLUTIONARY GEOGRAPHY</subject></subj-group></article-categories><title-group><article-title>Палеоэкологическая характеристика побережья Баренцева моря  в позднем голоцене на примере полуострова Средний</article-title><trans-title-group xml:lang="en"><trans-title>Paleoecological characteristics of the Barents sea coast during the late holocene  by the example of Sredniy Peninsula</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><bio xml:lang="ru"><p>Санкт-Петербург</p></bio><bio xml:lang="en"><p>Saint Petersburg</p></bio><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>Носевич</surname><given-names>Е. С.</given-names></name><name name-style="western" xml:lang="en"><surname>Nosevich</surname><given-names>E. S.</given-names></name></name-alternatives><bio xml:lang="ru"><p>Санкт-Петербург</p></bio><bio xml:lang="en"><p>Saint Petersburg</p></bio><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><bio xml:lang="ru"><p>Санкт-Петербург</p></bio><bio xml:lang="en"><p>Saint Petersburg</p></bio><xref ref-type="aff" rid="aff-3"/></contrib><contrib contrib-type="author" corresp="yes"><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Мурашкин</surname><given-names>А. И.</given-names></name><name name-style="western" xml:lang="en"><surname>Murashkin</surname><given-names>A. I.</given-names></name></name-alternatives><bio xml:lang="ru"><p>Санкт-Петербург</p></bio><bio xml:lang="en"><p>Saint Petersburg</p></bio><xref ref-type="aff" rid="aff-4"/></contrib><contrib contrib-type="author" corresp="yes"><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Колпаков</surname><given-names>Е. М.</given-names></name><name name-style="western" xml:lang="en"><surname>Kolpakov</surname><given-names>E. M.</given-names></name></name-alternatives><bio xml:lang="ru"><p>Санкт-Петербург</p></bio><bio xml:lang="en"><p>Saint Petersburg</p></bio><xref ref-type="aff" rid="aff-5"/></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>ФГБУ «ВСЕГЕИ» им. А. П. Карпинского</institution><country>Россия</country></aff><aff xml:lang="en"><institution>A.P. Karpinsky Russian geological research institute</institution><country>Russian Federation</country></aff></aff-alternatives><aff-alternatives id="aff-3"><aff xml:lang="ru"><institution>Государственный педагогический университет им. А.И. Герцена</institution><country>Россия</country></aff><aff xml:lang="en"><institution>Herzen State Pedagogical University of Russia</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>Saint Petersburg State University</institution><country>Russian Federation</country></aff></aff-alternatives><aff-alternatives id="aff-5"><aff xml:lang="ru"><institution>Институт истории материальной культуры РАН</institution><country>Россия</country></aff><aff xml:lang="en"><institution>Institute for the History of Material Culture, Russian Academy of Sciences</institution><country>Russian Federation</country></aff></aff-alternatives><pub-date pub-type="collection"><year>2018</year></pub-date><pub-date pub-type="epub"><day>25</day><month>12</month><year>2018</year></pub-date><volume>64</volume><issue>4</issue><fpage>391</fpage><lpage>406</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Сапелко Т.В., Носевич Е.С., Кулькова М.А., Мурашкин А.И., Колпаков Е.М., 2018</copyright-statement><copyright-year>2018</copyright-year><copyright-holder xml:lang="ru">Сапелко Т.В., Носевич Е.С., Кулькова М.А., Мурашкин А.И., Колпаков Е.М.</copyright-holder><copyright-holder xml:lang="en">Sapelko T.V., Nosevich E.S., Kulkova M.A., Murashkin A.I., Kolpakov E.M.</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.aaresearch.science/jour/article/view/111">https://www.aaresearch.science/jour/article/view/111</self-uri><abstract><p>Получены результаты комплексных палеоэкологических исследований на юго-западном побережье Баренцева моря. На поселении Перяярви 1 (полуостров Средний), открытом В.Я. Шумкиным в 1994 г., проведены археологические раскопки двух жилищ. Разрез одного из жилищ эпохи раннего металла изучен с помощью археологического, палинологического, геохимического и радиоуглеродного методов, на основании чего проведена реконструкция природных условий в позднем голоцене на побережье Баренцева моря.</p></abstract><trans-abstract xml:lang="en"><p>We received results of complex palaeoecological research at south-west Barents Sea coast. In Periayarvi 1 settlement (Sredniy Peninsula) discovered by V. Ya. Shumkin in 1994, archeological excavations of two house-structures were performed. We sampled the sequence in the house-structure 16 date to the Early Metal Age and we studied it with archaeological, palynological, geochemical and radiocarbon methods. The sequence in the house-structure 16 settlement include sand layers in the bottom, the upper part consists of slightly decomposed peat. The radiocarbon data obtained from the charcoal sample from the fireplace in the middle of the house-structure is 2920±70 C14 BP, which correlates with result of pollen analysis. According ac to pollen data, the sequence formation started at the first half of the Subboreal period during the spread of tundra vegetation and then vegetation changed to forest tundra while the climate was getting more comfortable for humans. At the Subatlantic period tundra recovers because of temperature drop. The landscape is getting similar to the modern one. According geochemical indications main functional zones of house-structure were distinguished, and that provides necessary information about main characteristics of living conditions. The complex of methods allows to date Periayarvi 1 settlement to the Early Metal Age. In the results we made reconstruction of palaeoenvironmental conditions in the Late Holocene at the Barents Sea coast.</p></trans-abstract><kwd-group xml:lang="ru"><kwd>археология</kwd><kwd>Баренцево море</kwd><kwd>геохимия</kwd><kwd>Кольский полуостров</kwd><kwd>палеоэкология</kwd><kwd>палинология</kwd><kwd>поздний голоцен</kwd></kwd-group><kwd-group xml:lang="en"><kwd>archeology</kwd><kwd>Barents Sea</kwd><kwd>geochemistry</kwd><kwd>Kola Peninsula</kwd><kwd>Late Holocene</kwd><kwd>palaeoecology</kwd><kwd>palynology</kwd></kwd-group><funding-group><funding-statement xml:lang="ru">Работа выполнена в рамках государственного задания ИНОЗ РАН по теме № 0154-2018-0004 (государственная регистрация 01201363380).</funding-statement><funding-statement xml:lang="en">The research were performed at a base of state order to institute of Limnology, RAS № 0154-2018-0004 (registration number 01201363380).</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">Gervais B.R., MacDonald G.M. 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