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<article 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" xmlns:ali="http://www.niso.org/schemas/ali/1.0/" article-type="research-article" dtd-version="1.2" xml:lang="en"><front><journal-meta><journal-id journal-id-type="publisher-id">Priroda</journal-id><journal-title-group><journal-title xml:lang="en">Priroda</journal-title><trans-title-group xml:lang="ru"><trans-title>Природа</trans-title></trans-title-group></journal-title-group><issn publication-format="print">0032-874X</issn><publisher><publisher-name xml:lang="en">Akademizdatcenter Nauka</publisher-name></publisher></journal-meta><article-meta><article-id pub-id-type="publisher-id">627872</article-id><article-id pub-id-type="doi">10.7868/S0032874X23120013</article-id><article-categories><subj-group subj-group-type="toc-heading" xml:lang="en"><subject>Articles</subject></subj-group><subj-group subj-group-type="toc-heading" xml:lang="ru"><subject>Статьи</subject></subj-group><subj-group subj-group-type="article-type"><subject>Research Article</subject></subj-group></article-categories><title-group><article-title xml:lang="en">Lakes: a Barcode of Time</article-title><trans-title-group xml:lang="ru"><trans-title>Озера: Штрихкод Времени</trans-title></trans-title-group></title-group><contrib-group><contrib contrib-type="author"><name-alternatives><name xml:lang="en"><surname>Rudaya</surname><given-names>N. A</given-names></name><name xml:lang="ru"><surname>Рудая</surname><given-names>Н. А</given-names></name></name-alternatives><email>nrudaya@gmail.com</email><xref ref-type="aff" rid="aff1"/><xref ref-type="aff" rid="aff2"/></contrib></contrib-group><aff-alternatives id="aff1"><aff><institution xml:lang="en">Institute of Archaeology and Ethnography, Siberian Branch of the Russian Academy of Sciences</institution></aff><aff><institution xml:lang="ru">Институт Археологии и Этнографии СО РАН</institution></aff></aff-alternatives><aff-alternatives id="aff2"><aff><institution xml:lang="en">Tomsk State University</institution></aff><aff><institution xml:lang="ru">Томский Государственный Университет</institution></aff></aff-alternatives><pub-date date-type="pub" iso-8601-date="2023-12-29" publication-format="electronic"><day>29</day><month>12</month><year>2023</year></pub-date><issue>12</issue><issue-title xml:lang="en">№12 (2023)</issue-title><issue-title xml:lang="ru">№12 (2023)</issue-title><fpage>3</fpage><lpage>15</lpage><history><date date-type="received" iso-8601-date="2024-03-01"><day>01</day><month>03</month><year>2024</year></date></history><permissions><copyright-statement xml:lang="ru">Copyright ©; 2023, Издательство «Наука»</copyright-statement><copyright-year>2023</copyright-year><copyright-holder xml:lang="ru">Издательство «Наука»</copyright-holder></permissions><self-uri xlink:href="https://journals.eco-vector.com/0032-874X/article/view/627872">https://journals.eco-vector.com/0032-874X/article/view/627872</self-uri><abstract xml:lang="en"><p>Palaeolimnology is the science that focuses on of ancient natural archives preserved in lake sediments. Lakes accumulate gigabytes of information on the evolution of the natural landscapes of the lake’s catchment area as well as the entire region in which the lake is located. The data contained in these palaeorecords can span millennia or even millions of years for large, long-lived lakes. The lake preserves information about vegetation, climate, geology, aquatic life, and even the people who inhabited its shores. This information creates some kind of a barcode of the time period that we seek to read. Lake palaeoarchives are used to reconstruct past environmental conditions both qualitatively and quantitatively. They are also used in the global climate modeling.</p></abstract><trans-abstract xml:lang="ru"><p>Наука, которая изучает ископаемые природные архивы, заключенные в донных осадках озер, называется палеолимнология. Озера накапливают гигабайты информации о развитии природных ландшафтов водосбора озера, а также и всего региона, в котором это озеро расположено. Для некоторых озер это данные за последние тысячелетия, но для части крупных долгоживущих озер такие палеозаписи отражают историю нашей планеты за несколько миллионов лет. Слой за слоем озеро сохраняет информацию о растительности, климате, геологии, водных обитателях и даже людях, живших на берегу, создавая тем самым штрихкод времени, который мы стремимся прочитать. Результаты исследования озерных палеоархивов современными естественнонаучными методами используются как для качественных и количественных реконструкций природных условий прошлого, так и при глобальном климатическом моделировании.</p></trans-abstract><kwd-group xml:lang="en"><kwd>lakes</kwd><kwd>bottom sediments</kwd><kwd>climate</kwd><kwd>palaeoreconstructions</kwd><kwd>global modeling</kwd></kwd-group><kwd-group xml:lang="ru"><kwd>озера</kwd><kwd>донные осадки</kwd><kwd>климат</kwd><kwd>палеореконструкции</kwd><kwd>глобальное моделирование</kwd></kwd-group></article-meta></front><body></body><back><ref-list><ref id="B1"><label>1.</label><mixed-citation>Lozhkin A. V., Anderson P. M., Matrosova T. V., Minyuk P. The pollen record from El’gygytgyn Lake: implications for vegetation and climate histories of northern Chukotka since the late middle Pleistocene. Journal of Paleolimnology. 2007; 37: 135–153. 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