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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="en"><front><journal-meta><journal-id journal-id-type="publisher-id">nsc</journal-id><journal-title-group><journal-title xml:lang="en">Archaeology, Ethnology &amp; Anthropology of Eurasia</journal-title><trans-title-group xml:lang="ru"><trans-title>Археология, этнография и антропология Евразии</trans-title></trans-title-group></journal-title-group><issn pub-type="ppub">1563-0110</issn><publisher><publisher-name>IAET SB RAS</publisher-name></publisher></journal-meta><article-meta><article-id pub-id-type="doi">10.17746/1563-0110.2025.53.2.054-062</article-id><article-id custom-type="elpub" pub-id-type="custom">nsc-2187</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="en"><subject>THE METAL AGES AND MEDIEVAL PERIOD</subject></subj-group><subj-group subj-group-type="section-heading" xml:lang="ru"><subject>ЭПОХА ПАЛЕОМЕТАЛЛА</subject></subj-group></article-categories><title-group><article-title>Raman Spectroscopy Analysis of Pigments from the Boyary I Rock Art Site, Khakassia</article-title><trans-title-group xml:lang="ru"><trans-title></trans-title></trans-title-group></title-group><contrib-group><contrib contrib-type="author" corresp="yes"><name-alternatives><name name-style="western" xml:lang="en"><surname>Davydov</surname><given-names>R. V.</given-names></name></name-alternatives><bio xml:lang="en"><p>Pr. Akademika Lavrentieva 17, Novosibirsk, 630090</p></bio><email xlink:type="simple">puer-viro@mail.ru</email><xref ref-type="aff" rid="aff-1"/></contrib><contrib contrib-type="author" corresp="yes"><name-alternatives><name name-style="western" xml:lang="en"><surname>Gubar</surname><given-names>Y. S.</given-names></name></name-alternatives><bio xml:lang="en"><p>Pr. Akademika Lavrentieva 17, Novosibirsk, 630090</p></bio><xref ref-type="aff" rid="aff-1"/></contrib><contrib contrib-type="author" corresp="yes"><name-alternatives><name name-style="western" xml:lang="en"><surname>Zotkina</surname><given-names>L. V.</given-names></name></name-alternatives><bio xml:lang="en"><p>Pr. Akademika Lavrentieva 17, Novosibirsk, 630090</p></bio><xref ref-type="aff" rid="aff-1"/></contrib></contrib-group><aff xml:lang="en" id="aff-1"><institution>Institute of Archaeology and Ethnography,  Siberian Branch</institution><country>Russian Federation</country></aff><pub-date pub-type="collection"><year>2025</year></pub-date><pub-date pub-type="epub"><day>03</day><month>07</month><year>2025</year></pub-date><volume>53</volume><issue>1</issue><fpage>54</fpage><lpage>62</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Davydov R.V., Gubar Y.S., Zotkina L.V., 2025</copyright-statement><copyright-year>2025</copyright-year><copyright-holder xml:lang="ru">Davydov R.V., Gubar Y.S., Zotkina L.V.</copyright-holder><copyright-holder xml:lang="en">Davydov R.V., Gubar Y.S., Zotkina L.V.</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://journal.archaeology.nsc.ru/jour/article/view/2187">https://journal.archaeology.nsc.ru/jour/article/view/2187</self-uri><abstract><p>This article describes previously unknown paintings at the Boyary I rock art site, Republic of Khakassia. They are especially important because they were situated in the part of the panel where a missing ledge could have been located. The petroglyphs could indicate the time of its disappearance. Based on stylistic features, it is possible that they date to the Karasuk period (late 2nd to early 1st millennium BC). The article presents the results of Raman spectroscopy analysis of pigments detected in the paintings. The method involved their context assessment with regard to the rock surface and the white paint of recent inscriptions, the composition of ancient pigments, and searching for organic binder residue. The study covered panel 7 and the adjacent panels 8 and 9. The results are based on 103 spectra of various compositions. All three surfaces mainly consist of sandstone, the predominant constituents being albite, quartzite, and anatase, with occasional natural ferruginization. Modern white paint of two types—chalk (panel 7) and styrene acrylic (panel 9)—were detected. The red pigment used for the paintings in the right part of panel 7 consists of hematite. Calcium oxalate (whewellite) was found only where residues of pigments were located, suggesting that it resulted from the decomposition of the organic binder of the ancient paint. </p></abstract><kwd-group xml:lang="en"><kwd>Rock art</kwd><kwd>paintings</kwd><kwd>pigments</kwd><kwd>binders</kwd><kwd>Raman spectroscopy</kwd><kwd>Minusinsk Basin</kwd></kwd-group><funding-group><funding-statement xml:lang="en">This study was supported by the Russian Science Foundation, project No. 22-18-00070. The authors express their deep gratitude to E.V. Karpova, Senior Researcher at the Vorozhtsov Novosibirsk Institute of Organic Chemistry of the SB RAS, for her consultation, and thank the reviewer for constructive criticism which made it possible to significantly improve the text of the article. 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