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 <front>
  <journal-meta>
   <journal-id journal-id-type="publisher-id">Russian Journal of Earth Sciences</journal-id>
   <journal-title-group>
    <journal-title xml:lang="en">Russian Journal of Earth Sciences</journal-title>
    <trans-title-group xml:lang="ru">
     <trans-title>Russian Journal of Earth Sciences</trans-title>
    </trans-title-group>
   </journal-title-group>
   <issn publication-format="online">1681-1208</issn>
  </journal-meta>
  <article-meta>
   <article-id pub-id-type="publisher-id">46849</article-id>
   <article-categories>
    <subj-group subj-group-type="toc-heading" xml:lang="ru">
     <subject>ОРИГИНАЛЬНЫЕ СТАТЬИ</subject>
    </subj-group>
    <subj-group subj-group-type="toc-heading" xml:lang="en">
     <subject>ORIGINAL ARTICLES</subject>
    </subj-group>
    <subj-group>
     <subject>ОРИГИНАЛЬНЫЕ СТАТЬИ</subject>
    </subj-group>
   </article-categories>
   <title-group>
    <article-title xml:lang="en">New evidence of the age of the Black Sea Pontian substage</article-title>
    <trans-title-group xml:lang="ru">
     <trans-title>New evidence of the age of the Black Sea Pontian substage</trans-title>
    </trans-title-group>
   </title-group>
   <contrib-group content-type="authors">
    <contrib contrib-type="author">
     <name-alternatives>
      <name xml:lang="ru">
       <surname>Rybkina</surname>
       <given-names>Alena I </given-names>
      </name>
      <name xml:lang="en">
       <surname>Rybkina</surname>
       <given-names>Alena I </given-names>
      </name>
     </name-alternatives>
     <xref ref-type="aff" rid="aff-1"/>
    </contrib>
    <contrib contrib-type="author">
     <name-alternatives>
      <name xml:lang="ru">
       <surname>Rostovtseva</surname>
       <given-names>Yuliana V </given-names>
      </name>
      <name xml:lang="en">
       <surname>Rostovtseva</surname>
       <given-names>Yuliana V </given-names>
      </name>
     </name-alternatives>
     <xref ref-type="aff" rid="aff-2"/>
    </contrib>
   </contrib-group>
   <aff-alternatives id="aff-1">
    <aff>
     <institution xml:lang="ru">Geophysical Center of the Russian Academy of Sciences</institution>
     <country>ru</country>
    </aff>
    <aff>
     <institution xml:lang="en">Geophysical Center of the Russian Academy of Sciences</institution>
     <country>ru</country>
    </aff>
   </aff-alternatives>
   <aff-alternatives id="aff-2">
    <aff>
     <institution xml:lang="ru">Geological Faculty, Lomonosov Moscow State University</institution>
     <country>ru</country>
    </aff>
    <aff>
     <institution xml:lang="en">Geological Faculty, Lomonosov Moscow State University</institution>
     <country>ru</country>
    </aff>
   </aff-alternatives>
   <volume>17</volume>
   <issue>5</issue>
   <fpage>1</fpage>
   <lpage>4</lpage>
   <history>
    <date date-type="received" iso-8601-date="2021-11-09T23:38:39+03:00">
     <day>09</day>
     <month>11</month>
     <year>2021</year>
    </date>
   </history>
   <self-uri xlink:href="https://rjes.ru/en/nauka/article/46849/view">https://rjes.ru/en/nauka/article/46849/view</self-uri>
   <abstract xml:lang="ru">
    <p>For the five years a set of various data was obtained from the relatively deep-water Upper Miocene sediments exposed in the Zheleznyi Rog section (Taman Peninsula, Russia). The data includes measurements of magnetic susceptibility (MS) and its further time-series analysis. The aim of these studies is to recognize the astronomic cycles correspond to the obliquity and precession variations. The results of this study reflect the strong correlations to the Messinian Salinity Crisis (MSC) of the Mediterranean. The study was supported by the RFBR 17-05-01085~A.</p>
   </abstract>
   <trans-abstract xml:lang="en">
    <p>For the five years a set of various data was obtained from the relatively deep-water Upper Miocene sediments exposed in the Zheleznyi Rog section (Taman Peninsula, Russia). The data includes measurements of magnetic susceptibility (MS) and its further time-series analysis. The aim of these studies is to recognize the astronomic cycles correspond to the obliquity and precession variations. The results of this study reflect the strong correlations to the Messinian Salinity Crisis (MSC) of the Mediterranean. The study was supported by the RFBR 17-05-01085~A.</p>
   </trans-abstract>
   <kwd-group xml:lang="ru">
    <kwd>Messinian event</kwd>
    <kwd>Pontian</kwd>
    <kwd>Black sea</kwd>
    <kwd>cyclostratigraphy</kwd>
    <kwd>magnetic susceptibility</kwd>
   </kwd-group>
   <kwd-group xml:lang="en">
    <kwd>Messinian event</kwd>
    <kwd>Pontian</kwd>
    <kwd>Black sea</kwd>
    <kwd>cyclostratigraphy</kwd>
    <kwd>magnetic susceptibility</kwd>
   </kwd-group>
  </article-meta>
 </front>
 <body>
  <p></p>
 </body>
 <back>
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