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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">47034</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">&quot;Back-arc&quot; marine ice sheet in the Sea of Okhotsk</article-title>
    <trans-title-group xml:lang="ru">
     <trans-title>&quot;Back-arc&quot; marine ice sheet in the Sea of Okhotsk</trans-title>
    </trans-title-group>
   </title-group>
   <contrib-group content-type="authors">
    <contrib contrib-type="author">
     <name-alternatives>
      <name xml:lang="ru">
       <surname>Grosswald</surname>
       <given-names>M G</given-names>
      </name>
      <name xml:lang="en">
       <surname>Grosswald</surname>
       <given-names>M G</given-names>
      </name>
     </name-alternatives>
     <xref ref-type="aff" rid="aff-1"/>
    </contrib>
    <contrib contrib-type="author">
     <name-alternatives>
      <name xml:lang="ru">
       <surname>Hughes</surname>
       <given-names>T J</given-names>
      </name>
      <name xml:lang="en">
       <surname>Hughes</surname>
       <given-names>T J</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">Institute of Geography, Russian Academy of Sciences, Moscow, Russia</institution>
     <country>ru</country>
    </aff>
    <aff>
     <institution xml:lang="en">Institute of Geography, Russian Academy of Sciences, Moscow, Russia</institution>
     <country>ru</country>
    </aff>
   </aff-alternatives>
   <aff-alternatives id="aff-2">
    <aff>
     <institution xml:lang="ru">Climate Change Institute and Department of Earth Sciences, University of Maine, Orono, USA</institution>
     <country>ru</country>
    </aff>
    <aff>
     <institution xml:lang="en">Climate Change Institute and Department of Earth Sciences, University of Maine, Orono, USA</institution>
     <country>ru</country>
    </aff>
   </aff-alternatives>
   <volume>7</volume>
   <issue>5</issue>
   <fpage>1</fpage>
   <lpage>15</lpage>
   <history>
    <date date-type="received" iso-8601-date="2021-11-10T20:38:31+03:00">
     <day>10</day>
     <month>11</month>
     <year>2021</year>
    </date>
   </history>
   <self-uri xlink:href="https://rjes.ru/en/nauka/article/47034/view">https://rjes.ru/en/nauka/article/47034/view</self-uri>
   <abstract xml:lang="ru">
    <p>Geomorphologic, marine geological, and paleoclimatic evidence, along with modeling results, indicate that, during the Late Pleistocene, the Sea of Okhotsk was glaciated by a &quot;back-arc&quot; marine ice-sheet, which was a continuous spillover of glaciation from the highlands of Northeast Siberia, buttressed by a submarine ridge of the Kurile Island Arc. That marine ice sheet also impounded and deflected the Lower Amur and Uda Rivers which resulted in reorganization of their drainage systems. The Okhotsk marine ice sheet was grounded on seafloor and reached to the outer southern edge of the submarine Academy Sill. From that limit, the ice sheet extended farther south, across the deep Kurile Basin, as a floating ice shelf. The Okhotsk Sea and Beringian Ice Sheets were the only &quot;back-arc&quot; Quaternary glaciers; they were two major sources of icebergs, meltwater, and ice-rafted debris supplied to the North Pacific Ocean during the Ice Ages.</p>
   </abstract>
   <trans-abstract xml:lang="en">
    <p>Geomorphologic, marine geological, and paleoclimatic evidence, along with modeling results, indicate that, during the Late Pleistocene, the Sea of Okhotsk was glaciated by a &quot;back-arc&quot; marine ice-sheet, which was a continuous spillover of glaciation from the highlands of Northeast Siberia, buttressed by a submarine ridge of the Kurile Island Arc. That marine ice sheet also impounded and deflected the Lower Amur and Uda Rivers which resulted in reorganization of their drainage systems. The Okhotsk marine ice sheet was grounded on seafloor and reached to the outer southern edge of the submarine Academy Sill. From that limit, the ice sheet extended farther south, across the deep Kurile Basin, as a floating ice shelf. The Okhotsk Sea and Beringian Ice Sheets were the only &quot;back-arc&quot; Quaternary glaciers; they were two major sources of icebergs, meltwater, and ice-rafted debris supplied to the North Pacific Ocean during the Ice Ages.</p>
   </trans-abstract>
   <kwd-group xml:lang="ru">
    <kwd>marine ice sheet</kwd>
    <kwd>Sea of Okhotsk</kwd>
    <kwd>Last Glacial Maximum</kwd>
    <kwd>Kuril Islands</kwd>
    <kwd>last deglaciation</kwd>
    <kwd>climate change</kwd>
    <kwd>Ice sheet buttressing</kwd>
    <kwd>Iceberg armadas.</kwd>
   </kwd-group>
   <kwd-group xml:lang="en">
    <kwd>marine ice sheet</kwd>
    <kwd>Sea of Okhotsk</kwd>
    <kwd>Last Glacial Maximum</kwd>
    <kwd>Kuril Islands</kwd>
    <kwd>last deglaciation</kwd>
    <kwd>climate change</kwd>
    <kwd>Ice sheet buttressing</kwd>
    <kwd>Iceberg armadas.</kwd>
   </kwd-group>
  </article-meta>
 </front>
 <body>
  <p></p>
 </body>
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