1 Ocak 2014 Dergi makalesi Açık Erişim

Ulusoy, Ulku; Anbar, Gul; Bayari, Serdar; Uysal, Tonguc

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<oai_dc:dc xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:oai_dc="http://www.openarchives.org/OAI/2.0/oai_dc/" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xsi:schemaLocation="http://www.openarchives.org/OAI/2.0/oai_dc/ http://www.openarchives.org/OAI/2.0/oai_dc.xsd">
  <dc:creator>Ulusoy, Ulku</dc:creator>
  <dc:creator>Anbar, Gul</dc:creator>
  <dc:creator>Bayari, Serdar</dc:creator>
  <dc:creator>Uysal, Tonguc</dc:creator>
  <dc:date>2014-01-01</dc:date>
  <dc:description>Electron spin resonance (ESR) and Th-230/U-234 ages of speleothem samples collected from karstic caves located around 3000 m elevation in the Aladaglar Mountain Range (AMR), south-central Turkey, were determined in order to provide new insight and information regarding late Pleistocene climate. ESR ages were validated with the Th-230/U-234 ages of test samples. The ESR ages of 21 different layers of six speleothem samples were found to range mostly between about 59 and 4 ka, which cover the Marine Oxygen Isotope Stages (MIS) MIS 3 to MIS 1. Among all, only six layers appear to have deposited during MIS 8 and 5. Most of the samples dated were deposited during the late glacial stage (MIS 2). It appears that a cooler climate with a perennial and steady recharge was more conducive to speleothem development rather than a warmer climate with seasonal recharge in the AMR during the late Quaternary. This argument supports previous findings that suggest a two -fold increase in last glacial maximum mean precipitation in Turkey with respect to the present value. (c) 2013 University of Washington. Published by Elsevier Inc. All rights reserved.</dc:description>
  <dc:identifier>https://aperta.ulakbim.gov.trrecord/66831</dc:identifier>
  <dc:identifier>oai:zenodo.org:66831</dc:identifier>
  <dc:rights>info:eu-repo/semantics/openAccess</dc:rights>
  <dc:rights>http://www.opendefinition.org/licenses/cc-by</dc:rights>
  <dc:source>QUATERNARY RESEARCH 81(2) 367-380</dc:source>
  <dc:title>ESR and Th-230/U-234 dating of speleothems from Aladaglar Mountain Range (AMR) in Turkey</dc:title>
  <dc:type>info:eu-repo/semantics/article</dc:type>
  <dc:type>publication-article</dc:type>
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