<?xml version="1.0" encoding="UTF-8"?>
<collection xmlns="http://www.loc.gov/MARC21/slim">
 <record>
  <leader>     caa a22        4500</leader>
  <controlfield tag="001">445800852</controlfield>
  <controlfield tag="003">CHVBK</controlfield>
  <controlfield tag="005">20180317145140.0</controlfield>
  <controlfield tag="007">cr unu---uuuuu</controlfield>
  <controlfield tag="008">170323e20110801xx      s     000 0 eng  </controlfield>
  <datafield tag="024" ind1="7" ind2="0">
   <subfield code="a">10.1007/s00704-010-0370-z</subfield>
   <subfield code="2">doi</subfield>
  </datafield>
  <datafield tag="035" ind1=" " ind2=" ">
   <subfield code="a">(NATIONALLICENCE)springer-10.1007/s00704-010-0370-z</subfield>
  </datafield>
  <datafield tag="245" ind1="0" ind2="0">
   <subfield code="a">Summer temperature variations recorded in tree-ring δ13C values on the northeastern Tibetan Plateau</subfield>
   <subfield code="h">[Elektronische Daten]</subfield>
   <subfield code="c">[Guobao Xu, Tuo Chen, Xiaohong Liu, Liya Jin, Wenling An, Wenzhi Wang]</subfield>
  </datafield>
  <datafield tag="520" ind1="3" ind2=" ">
   <subfield code="a">The source region of the Yangtze River is experiencing ever-faster glacier retreat and land deterioration as a result of climate change; however, understanding the past climate variability in the region is still limited by lack of long-term climate records. Here, we report a temperature-sensitive annual stable carbon isotope (δ13C) series of Tibetan juniper (Sabina tibetica) tree rings from 1850 to 2002 in natural forests in the source region of the Yangtze River on the northeastern Tibetan Plateau. The stable carbon discrimination (Δ13C) is significantly negatively correlated with the regional mean summer (May, June, and July) temperature, as well as with large-scale temperature variations. The reconstructed mean summer temperature explained about 44.3% of the total variance. It also agreed well with neighboring temperature proxies, including the ice-core δ18O series from the Guoqu glacier and from Dasuopu glacier and other tree-ring proxies. The cold and warm periods indicated by the climate reconstruction also coincide well with documented glacier advances and retreats in the eastern and southeastern Tibetan Plateau. The significant correlations among the reconstructed temperature, sea surface temperature (SSTNino3), and the Southern Oscillation index suggest the influences of synoptic atmospheric circulation on low-frequency variations in temperature on the region of the Yangtze River.</subfield>
  </datafield>
  <datafield tag="540" ind1=" " ind2=" ">
   <subfield code="a">Springer-Verlag, 2010</subfield>
  </datafield>
  <datafield tag="700" ind1="1" ind2=" ">
   <subfield code="a">Xu</subfield>
   <subfield code="D">Guobao</subfield>
   <subfield code="u">State Key Laboratory of Cryospheric Sciences, Cold and Arid Regions Environmental and Engineering Institute, Chinese Academy of Sciences, Donggang West Road No. 320, 730000, Lanzhou, People's Republic of China</subfield>
   <subfield code="4">aut</subfield>
  </datafield>
  <datafield tag="700" ind1="1" ind2=" ">
   <subfield code="a">Chen</subfield>
   <subfield code="D">Tuo</subfield>
   <subfield code="u">State Key Laboratory of Cryospheric Sciences, Cold and Arid Regions Environmental and Engineering Institute, Chinese Academy of Sciences, Donggang West Road No. 320, 730000, Lanzhou, People's Republic of China</subfield>
   <subfield code="4">aut</subfield>
  </datafield>
  <datafield tag="700" ind1="1" ind2=" ">
   <subfield code="a">Liu</subfield>
   <subfield code="D">Xiaohong</subfield>
   <subfield code="u">State Key Laboratory of Cryospheric Sciences, Cold and Arid Regions Environmental and Engineering Institute, Chinese Academy of Sciences, Donggang West Road No. 320, 730000, Lanzhou, People's Republic of China</subfield>
   <subfield code="4">aut</subfield>
  </datafield>
  <datafield tag="700" ind1="1" ind2=" ">
   <subfield code="a">Jin</subfield>
   <subfield code="D">Liya</subfield>
   <subfield code="u">Center for Arid Environment and Paleoclimate Research (CAEP), Key Laboratory of Western China's Environmental System (Ministry of Education), Lanzhou University, 730000, Lanzhou, People's Republic of China</subfield>
   <subfield code="4">aut</subfield>
  </datafield>
  <datafield tag="700" ind1="1" ind2=" ">
   <subfield code="a">An</subfield>
   <subfield code="D">Wenling</subfield>
   <subfield code="u">State Key Laboratory of Cryospheric Sciences, Cold and Arid Regions Environmental and Engineering Institute, Chinese Academy of Sciences, Donggang West Road No. 320, 730000, Lanzhou, People's Republic of China</subfield>
   <subfield code="4">aut</subfield>
  </datafield>
  <datafield tag="700" ind1="1" ind2=" ">
   <subfield code="a">Wang</subfield>
   <subfield code="D">Wenzhi</subfield>
   <subfield code="u">State Key Laboratory of Cryospheric Sciences, Cold and Arid Regions Environmental and Engineering Institute, Chinese Academy of Sciences, Donggang West Road No. 320, 730000, Lanzhou, People's Republic of China</subfield>
   <subfield code="4">aut</subfield>
  </datafield>
  <datafield tag="773" ind1="0" ind2=" ">
   <subfield code="t">Theoretical and Applied Climatology</subfield>
   <subfield code="d">Springer Vienna</subfield>
   <subfield code="g">105/1-2(2011-08-01), 51-63</subfield>
   <subfield code="x">0177-798X</subfield>
   <subfield code="q">105:1-2&lt;51</subfield>
   <subfield code="1">2011</subfield>
   <subfield code="2">105</subfield>
   <subfield code="o">704</subfield>
  </datafield>
  <datafield tag="856" ind1="4" ind2="0">
   <subfield code="u">https://doi.org/10.1007/s00704-010-0370-z</subfield>
   <subfield code="q">text/html</subfield>
   <subfield code="z">Onlinezugriff via DOI</subfield>
  </datafield>
  <datafield tag="908" ind1=" " ind2=" ">
   <subfield code="D">1</subfield>
   <subfield code="a">research-article</subfield>
   <subfield code="2">jats</subfield>
  </datafield>
  <datafield tag="950" ind1=" " ind2=" ">
   <subfield code="B">NATIONALLICENCE</subfield>
   <subfield code="P">856</subfield>
   <subfield code="E">40</subfield>
   <subfield code="u">https://doi.org/10.1007/s00704-010-0370-z</subfield>
   <subfield code="q">text/html</subfield>
   <subfield code="z">Onlinezugriff via DOI</subfield>
  </datafield>
  <datafield tag="950" ind1=" " ind2=" ">
   <subfield code="B">NATIONALLICENCE</subfield>
   <subfield code="P">700</subfield>
   <subfield code="E">1-</subfield>
   <subfield code="a">Xu</subfield>
   <subfield code="D">Guobao</subfield>
   <subfield code="u">State Key Laboratory of Cryospheric Sciences, Cold and Arid Regions Environmental and Engineering Institute, Chinese Academy of Sciences, Donggang West Road No. 320, 730000, Lanzhou, People's Republic of China</subfield>
   <subfield code="4">aut</subfield>
  </datafield>
  <datafield tag="950" ind1=" " ind2=" ">
   <subfield code="B">NATIONALLICENCE</subfield>
   <subfield code="P">700</subfield>
   <subfield code="E">1-</subfield>
   <subfield code="a">Chen</subfield>
   <subfield code="D">Tuo</subfield>
   <subfield code="u">State Key Laboratory of Cryospheric Sciences, Cold and Arid Regions Environmental and Engineering Institute, Chinese Academy of Sciences, Donggang West Road No. 320, 730000, Lanzhou, People's Republic of China</subfield>
   <subfield code="4">aut</subfield>
  </datafield>
  <datafield tag="950" ind1=" " ind2=" ">
   <subfield code="B">NATIONALLICENCE</subfield>
   <subfield code="P">700</subfield>
   <subfield code="E">1-</subfield>
   <subfield code="a">Liu</subfield>
   <subfield code="D">Xiaohong</subfield>
   <subfield code="u">State Key Laboratory of Cryospheric Sciences, Cold and Arid Regions Environmental and Engineering Institute, Chinese Academy of Sciences, Donggang West Road No. 320, 730000, Lanzhou, People's Republic of China</subfield>
   <subfield code="4">aut</subfield>
  </datafield>
  <datafield tag="950" ind1=" " ind2=" ">
   <subfield code="B">NATIONALLICENCE</subfield>
   <subfield code="P">700</subfield>
   <subfield code="E">1-</subfield>
   <subfield code="a">Jin</subfield>
   <subfield code="D">Liya</subfield>
   <subfield code="u">Center for Arid Environment and Paleoclimate Research (CAEP), Key Laboratory of Western China's Environmental System (Ministry of Education), Lanzhou University, 730000, Lanzhou, People's Republic of China</subfield>
   <subfield code="4">aut</subfield>
  </datafield>
  <datafield tag="950" ind1=" " ind2=" ">
   <subfield code="B">NATIONALLICENCE</subfield>
   <subfield code="P">700</subfield>
   <subfield code="E">1-</subfield>
   <subfield code="a">An</subfield>
   <subfield code="D">Wenling</subfield>
   <subfield code="u">State Key Laboratory of Cryospheric Sciences, Cold and Arid Regions Environmental and Engineering Institute, Chinese Academy of Sciences, Donggang West Road No. 320, 730000, Lanzhou, People's Republic of China</subfield>
   <subfield code="4">aut</subfield>
  </datafield>
  <datafield tag="950" ind1=" " ind2=" ">
   <subfield code="B">NATIONALLICENCE</subfield>
   <subfield code="P">700</subfield>
   <subfield code="E">1-</subfield>
   <subfield code="a">Wang</subfield>
   <subfield code="D">Wenzhi</subfield>
   <subfield code="u">State Key Laboratory of Cryospheric Sciences, Cold and Arid Regions Environmental and Engineering Institute, Chinese Academy of Sciences, Donggang West Road No. 320, 730000, Lanzhou, People's Republic of China</subfield>
   <subfield code="4">aut</subfield>
  </datafield>
  <datafield tag="950" ind1=" " ind2=" ">
   <subfield code="B">NATIONALLICENCE</subfield>
   <subfield code="P">773</subfield>
   <subfield code="E">0-</subfield>
   <subfield code="t">Theoretical and Applied Climatology</subfield>
   <subfield code="d">Springer Vienna</subfield>
   <subfield code="g">105/1-2(2011-08-01), 51-63</subfield>
   <subfield code="x">0177-798X</subfield>
   <subfield code="q">105:1-2&lt;51</subfield>
   <subfield code="1">2011</subfield>
   <subfield code="2">105</subfield>
   <subfield code="o">704</subfield>
  </datafield>
  <datafield tag="900" ind1=" " ind2="7">
   <subfield code="a">Metadata rights reserved</subfield>
   <subfield code="b">Springer special CC-BY-NC licence</subfield>
   <subfield code="2">nationallicence</subfield>
  </datafield>
  <datafield tag="898" ind1=" " ind2=" ">
   <subfield code="a">BK010053</subfield>
   <subfield code="b">XK010053</subfield>
   <subfield code="c">XK010000</subfield>
  </datafield>
  <datafield tag="949" ind1=" " ind2=" ">
   <subfield code="B">NATIONALLICENCE</subfield>
   <subfield code="F">NATIONALLICENCE</subfield>
   <subfield code="b">NL-springer</subfield>
  </datafield>
 </record>
</collection>
