1 Ocak 2015 Dergi makalesi Açık Erişim

Pickarski, N.; Kwiecien, O.; Langgut, D.; Litt, T.

Dublin Core

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  <dc:creator>Pickarski, N.</dc:creator>
  <dc:creator>Kwiecien, O.</dc:creator>
  <dc:creator>Langgut, D.</dc:creator>
  <dc:creator>Litt, T.</dc:creator>
  <dc:date>2015-01-01</dc:date>
  <dc:description>Detailed analyses of the Lake Van pollen, Ca/K ratio, and stable oxygen isotope record allow the identification of millennial-scale vegetation and environmental changes in eastern Anatolia throughout the last glacial (similar to 111.5-11.7 ka BP). The climate of the last glacial was cold and dry, indicated by low arboreal pollen (AP) levels. The driest and coldest period corresponds to Marine Isotope Stage (MIS) 2 (similar to 28-14.5 ka BP), which was dominated by highest values of xerophytic steppe vegetation.</dc:description>
  <dc:identifier>https://aperta.ulakbim.gov.trrecord/81155</dc:identifier>
  <dc:identifier>oai:zenodo.org:81155</dc:identifier>
  <dc:rights>info:eu-repo/semantics/openAccess</dc:rights>
  <dc:rights>http://www.opendefinition.org/licenses/cc-by</dc:rights>
  <dc:source>CLIMATE OF THE PAST 11(11) 1491-1505</dc:source>
  <dc:title>Abrupt climate and vegetation variability of eastern Anatolia during the last glacial</dc:title>
  <dc:type>info:eu-repo/semantics/article</dc:type>
  <dc:type>publication-article</dc:type>
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