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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">10.7868/S2587556618020061</article-id><article-id custom-type="elpub" pub-id-type="custom">sergeogr-686</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>РЕКОНСТРУКЦИЯ ТЕМПЕРАТУРЫ ЛЕТНИХ МЕСЯЦЕВ НА ОСНОВЕ ГОДИЧНЫХ КОЛЕЦ СОСНЫ ОБЫКНОВЕННОЙ PINUS SYLVESTRIS L., ПРОИЗРАСТАЮЩЕЙ В БАССЕЙНЕ Р. ПЕЧОРА</article-title><trans-title-group xml:lang="en"><trans-title>RECONSTRUCTION OF SUMMER MONTH TEMPERATURES BASED ON SCOTS PINE TREE RINGS (PINUS SYLVESTRIS L.), GROWING IN THE PECHORA RIVER 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>Гурская</surname><given-names>М. А.</given-names></name><name name-style="western" xml:lang="en"><surname>Gurskaya</surname><given-names>M. A.</given-names></name></name-alternatives><bio xml:lang="ru"><p>Марина А. Гурская </p><p>Екатеринбург</p></bio><bio xml:lang="en"><p>Marina A. Gurskaya </p><p>Yekaterinburg</p></bio><email xlink:type="simple">mgurskaya@yandex.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>Кукарских</surname><given-names>В. В.</given-names></name><name name-style="western" xml:lang="en"><surname>Kukarskih</surname><given-names>V. V.</given-names></name></name-alternatives><bio xml:lang="ru"><p>Владимир В. Кукарских </p><p>Екатеринбург</p></bio><bio xml:lang="en"><p>Vladimir V. Kukarskih</p><p>Yekaterinburg</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>Ланге</surname><given-names>Е.</given-names></name><name name-style="western" xml:lang="en"><surname>Lange</surname><given-names>E.</given-names></name></name-alternatives><bio xml:lang="ru"><p>Елена Ланге </p><p>Грайфсвальд</p></bio><bio xml:lang="en"><p>Elena Lange </p><p>Greifswald</p></bio><xref ref-type="aff" rid="aff-2"/></contrib></contrib-group><aff-alternatives id="aff-1"><aff xml:lang="ru"><institution>Институт экологии растений и животных УрО РАН</institution><country>Россия</country></aff><aff xml:lang="en"><institution>Institute of Plant and Animal Ecology, Ural Branch, Russian Academy of Sciences</institution><country>Russian Federation</country></aff></aff-alternatives><aff-alternatives id="aff-2"><aff xml:lang="ru"><institution>Институт ботаники и ландшафтной экологии Университета Грайфсвальда</institution><country>Германия</country></aff><aff xml:lang="en"><institution>Institute of Botany and Landscape Ecology, Greifswald University</institution><country>Germany</country></aff></aff-alternatives><pub-date pub-type="collection"><year>2018</year></pub-date><pub-date pub-type="epub"><day>08</day><month>05</month><year>2018</year></pub-date><volume>0</volume><issue>2</issue><fpage>59</fpage><lpage>73</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Гурская М.А., Кукарских В.В., Ланге Е., 2018</copyright-statement><copyright-year>2018</copyright-year><copyright-holder xml:lang="ru">Гурская М.А., Кукарских В.В., Ланге Е.</copyright-holder><copyright-holder xml:lang="en">Gurskaya M.A., Kukarskih V.V., Lange E.</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/686">https://izvestia.igras.ru/jour/article/view/686</self-uri><abstract><p>В бассейне реки Печора собраны керны сосны обыкновенной, произрастающей на северном пределе распространения в сосняках лишайниковых, с целью выявить параметры годичных колец, наиболее подходящих для реконструкции климатических факторов в районе исследования. Ширина годичных колец имеет слабый смешанный сигнал температуры и осадков предыдущего и текущего годов и не может быть использована для реконструкций. Максимальная оптическая плотность оказалась очень перспективной для реконструкции температуры в районе исследования, а северные островные боры имеют более сильный сигнал, по сравнению с сосняками, произрастающими на 100 км южнее в зоне сплошных сосновых лесов. Впервые выполнена реконструкция температуры летних месяцев за последние 200 лет в районе исследования. Полученные данные согласуются с реконструкциями, выполненными по хронологиям максимальной плотности сосны из Фенноскандии и Евразии.</p></abstract><trans-abstract xml:lang="en"><p>Cores of Scots pine growing in northern taiga on the northern limit of distribution in lichen pine forests in the Pechora River basin are collected with purpose to reveal most suitable for climatic reconstructions tree-ring parameters. Tree-ring width has a weak mixed signal of temperature and precipitations of previous and current years and, therefore, cannot be used for reconstruction. Maximum optical density has shown a very perspective temperature signal for reconstruction in area under study. Northern island pine forests have stronger signal, in comparison with the pine forests growing in 100 km to the south, in a zone of continuous pine forest. Reconstruction of June–August temperature for the last 200 years is executed for the first time. The obtained data have correlated with the reconstruction by chronologies of the maximal density of pine from Fennoskandia and Eurasia.</p></trans-abstract><kwd-group xml:lang="ru"><kwd>сосна</kwd><kwd>бассейн реки Печора</kwd><kwd>ширина годичных колец</kwd><kwd>максимальная плотность древесины</kwd><kwd>древесно-кольцевые хронологии</kwd><kwd>реконструкция температуры летних месяцев</kwd></kwd-group><kwd-group xml:lang="en"><kwd>Scots pine</kwd><kwd>Pechora River basin</kwd><kwd>tree-ring width</kwd><kwd>maximal wood density</kwd><kwd>tree-ring chronologies</kwd><kwd>reconstruction of June-August temperature</kwd></kwd-group><funding-group><funding-statement xml:lang="ru">Российский фонд фундаментальных исследований (гранты 14-04-91356 и 15-04-04933) и  УрО РАН (№ 15-2-4-22)</funding-statement><funding-statement xml:lang="en">Russian Foundation for Basic Research (projects no. 14-04-91356; 15-04-04933) and Urals Branch of the RAS (project no. 15-2-4-22)</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">Белецкий И.Б. 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