<DIF xmlns="http://gcmd.gsfc.nasa.gov/Aboutus/xml/dif/" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xsi:schemaLocation="http://gcmd.gsfc.nasa.gov/Aboutus/xml/dif/ http://gcmd.gsfc.nasa.gov/Aboutus/xml/dif/dif_v9.8.4.xsd">
  <Entry_ID>noaa-loess-21230</Entry_ID>
  <Entry_Title>Chinese Loess Plateau 360KYr Leaf Wax Isotope Data and Temperature Reconstruction</Entry_Title>
  <Data_Set_Citation>
    <Dataset_Creator>Thomas, E.K.; Clemens, S.C.; Sun, Y.; Prell, W.L.; Huang, Y.; Gao, L.; Loomis, S.E.; Chen, G.; Liu, Z.</Dataset_Creator>
    <Dataset_Title>Chinese Loess Plateau 360KYr Leaf Wax Isotope Data and Temperature Reconstruction</Dataset_Title>
    <Dataset_Release_Date>2017-01-04</Dataset_Release_Date>
    <Dataset_Publisher>NCDC-Paleoclimatology</Dataset_Publisher>
    <Data_Presentation_Form>ONLINE Files</Data_Presentation_Form>
    <Dataset_DOI>Pending</Dataset_DOI>
    <Online_Resource>https://www.ncdc.noaa.gov/paleo/study/21230</Online_Resource>
  </Data_Set_Citation>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>E.K.</First_Name>
    <Last_Name>Thomas</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>S.C.</First_Name>
    <Last_Name>Clemens</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>Y.</First_Name>
    <Last_Name>Sun</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>W.L.</First_Name>
    <Last_Name>Prell</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>Y.</First_Name>
    <Last_Name>Huang</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>L.</First_Name>
    <Last_Name>Gao</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>S.E.</First_Name>
    <Last_Name>Loomis</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>G.</First_Name>
    <Last_Name>Chen</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>Z.</First_Name>
    <Last_Name>Liu</Last_Name>
  </Personnel>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>climate reconstructions|loess</Term>
    <Detailed_Variable>temperature,glycerol dialkyl glycerol tetraether index,null,degree Celsius,null,climate reconstructions|loess,null,null,N,null</Detailed_Variable>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>loess</Term>
    <Detailed_Variable>glycerol dialkyl glycerol tetraether,loess,null,percent,null,loess,null,null,N,fraction of 1022 (I)</Detailed_Variable>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>loess</Term>
    <Detailed_Variable>glycerol dialkyl glycerol tetraether,loess,null,percent,null,loess,null,null,N,fraction of 1032 (IIc)</Detailed_Variable>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>climate reconstructions|loess</Term>
    <Detailed_Variable>temperature,glycerol dialkyl glycerol tetraether index,null,degree Celsius,null,climate reconstructions|loess,null,null,N,brGDGT-based temperature from Mangshan (0-128 ka) and Weinan (128-360 ka)</Detailed_Variable>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>loess</Term>
    <Detailed_Variable>number of samples,null,null,count,null,loess,null,null,N,null</Detailed_Variable>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>loess</Term>
    <Detailed_Variable>glycerol dialkyl glycerol tetraether,loess,null,percent,null,loess,null,null,N,fraction of 1018 (Ic)</Detailed_Variable>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>loess</Term>
    <Detailed_Variable>glycerol dialkyl glycerol tetraether,loess,null,percent,null,loess,null,null,N,fraction of 1050 (III)</Detailed_Variable>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>loess</Term>
    <Detailed_Variable>grain size mean,loess,null,micrometer,null,loess,null,null,N,null</Detailed_Variable>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>climate reconstructions|loess</Term>
    <Detailed_Variable>age,null,null,calendar kiloyear before present,null,climate reconstructions|loess,null,null,N,interpolated sample age to 1 kyr time steps</Detailed_Variable>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>climate reconstructions|loess</Term>
    <Detailed_Variable>age,null,null,calendar kiloyear before present,null,climate reconstructions|loess,null,null,N,null</Detailed_Variable>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>loess</Term>
    <Detailed_Variable>age,null,null,calendar kiloyear before present,null,loess,null,null,N,interpolated sample age to 1 kyr time steps</Detailed_Variable>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>loess</Term>
    <Detailed_Variable>age,null,null,calendar kiloyear before present,null,loess,null,null,N,null</Detailed_Variable>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>loess</Term>
    <Detailed_Variable>glycerol dialkyl glycerol tetraether,loess,null,percent,null,loess,null,null,N,fraction of 1046 (IIIc)</Detailed_Variable>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>loess</Term>
    <Detailed_Variable>depth,null,null,meter,null,loess,null,null,N,composite depth</Detailed_Variable>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>loess</Term>
    <Detailed_Variable>delta 13C,C28 n-alkanoic acid,null,per mil VPDB,null,loess,null,null,N,from Lantian (0-68 ka) and Weinan (68 to 360 ka)</Detailed_Variable>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>loess</Term>
    <Detailed_Variable>glycerol dialkyl glycerol tetraether,loess,null,percent,null,loess,null,null,N,fraction of 1036 (II)</Detailed_Variable>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>loess</Term>
    <Detailed_Variable>mass magnetic susceptibility,loess,null,cubic meter per kilogram,null,loess,null,null,N,units are 10^-8 m^3 kg^-1</Detailed_Variable>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>climate reconstructions|loess</Term>
    <Detailed_Variable>depth,null,null,meter,null,climate reconstructions|loess,null,null,N,composite depth</Detailed_Variable>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>loess</Term>
    <Detailed_Variable>delta 13C,C28 n-alkanoic acid,one standard deviation,per mil VPDB,null,loess,null,null,N,from Lantian (0-68 ka) and Weinan (68 to 360 ka)</Detailed_Variable>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>loess</Term>
    <Detailed_Variable>sample identification,null,null,null,null,loess,null,null,C,biomarker sample ID</Detailed_Variable>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>climate reconstructions|loess</Term>
    <Detailed_Variable>temperature,glycerol dialkyl glycerol tetraether index,unspecified margin of error,degree Celsius,null,climate reconstructions|loess,null,null,N,calibration error</Detailed_Variable>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>loess</Term>
    <Detailed_Variable>mass magnetic susceptibility,loess,null,cubic meter per kilogram,null,loess,null,null,N,Weinan sediments; units are 10^-8 m^3 kg^-1</Detailed_Variable>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>loess</Term>
    <Detailed_Variable>grain size mean,loess,null,micrometer,null,loess,null,null,N,Weinan sediments</Detailed_Variable>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>loess</Term>
    <Detailed_Variable>glycerol dialkyl glycerol tetraether,loess,null,percent,null,loess,null,null,N,fraction of 1020 (Ib)</Detailed_Variable>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>loess</Term>
    <Detailed_Variable>glycerol dialkyl glycerol tetraether,loess,null,percent,null,loess,null,null,N,fraction of 1034 (IIb)</Detailed_Variable>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>loess</Term>
    <Detailed_Variable>glycerol dialkyl glycerol tetraether,loess,null,percent,null,loess,null,null,N,fraction of 1048 (IIIb)</Detailed_Variable>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>loess</Term>
    <Detailed_Variable>delta 2H,C28 n-alkanoic acid,null,per mil VSMOW,null,loess,null,null,N,from Lantian (0-68 ka) and Weinan (68 to 360 ka)</Detailed_Variable>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>loess</Term>
  </Parameters>
  <ISO_Topic_Category>geoscientificInformation</ISO_Topic_Category>
  <Paleo_Temporal_Coverage>
    <Paleo_Start_Date>443000 cal yr BP</Paleo_Start_Date>
    <Paleo_Stop_Date>6100 cal yr BP</Paleo_Stop_Date>
  </Paleo_Temporal_Coverage>
  <Data_Set_Progress>Complete</Data_Set_Progress>
  <Spatial_Coverage>
    <Southernmost_Latitude>34</Southernmost_Latitude>
    <Northernmost_Latitude>42</Northernmost_Latitude>
    <Westernmost_Longitude>109</Westernmost_Longitude>
    <Easternmost_Longitude>113.5</Easternmost_Longitude>
    <Minimum_Altitude>660</Minimum_Altitude>
    <Maximum_Altitude>660</Maximum_Altitude>
  </Spatial_Coverage>
  <Location>
    <Location_Category>Continent</Location_Category>
    <Location_Type>Asia</Location_Type>
    <Location_Subregion1>Eastern Asia</Location_Subregion1>
    <Location_Subregion2>China</Location_Subregion2>
    <Detailed_Location>Weinan&gt;LATITUDE 34.4274&gt;LONGITUDE 109.5771</Detailed_Location>
  </Location>
  <Location>
    <Location_Category>Continent</Location_Category>
    <Location_Type>Asia</Location_Type>
    <Location_Subregion1>Eastern Asia</Location_Subregion1>
    <Location_Subregion2>China</Location_Subregion2>
    <Detailed_Location>Mangshan&gt;LATITUDE 34.94&gt;LONGITUDE 113.37</Detailed_Location>
  </Location>
  <Location>
    <Location_Category>Continent</Location_Category>
    <Location_Type>Asia</Location_Type>
    <Location_Subregion1>Eastern Asia</Location_Subregion1>
    <Location_Subregion2>China</Location_Subregion2>
    <Detailed_Location>Chinese Loess Plateau&gt;LATITUDE &gt;LONGITUDE </Detailed_Location>
  </Location>
  <Access_Constraints>None</Access_Constraints>
  <Use_Constraints>Please cite original publication, online resource, dataset and publication DOIs (where available), and date accessed when using downloaded data. If there is no publication information, please cite investigator, title, online resource, and date accessed. The appearance of external links associated with a dataset does not constitute endorsement by the Department of Commerce/National Oceanic and Atmospheric Administration of external Web sites or the information, products or services contained therein. For other than authorized activities, the Department of Commerce/NOAA does not exercise any editorial control over the information you may find at these locations. These links are provided consistent with the stated purpose of this Department of Commerce/NOAA Web site.</Use_Constraints>
  <Data_Set_Language>English</Data_Set_Language>
  <Data_Center>
    <Data_Center_Name>
      <Short_Name>DOC/NOAA/NESDIS/NCEI</Short_Name>
      <Long_Name>National Centers for Environmental Information, NESDIS, NOAA, U.S. Department of Commerce </Long_Name>
    </Data_Center_Name>
    <Data_Center_URL>https://www.ncdc.noaa.gov/data-access/paleoclimatology-data</Data_Center_URL>
    <Personnel>
      <Role>DATA Center Contact</Role>
      <First_Name>Bruce</First_Name>
      <Last_Name>Bauer</Last_Name>
      <Email>bruce.a.bauer@noaa.gov</Email>
      <Email>paleo@noaa.gov</Email>
      <Phone>303-497-6280</Phone>
      <Fax>303-497-6513</Fax>
      <Contact_Address>
        <Address>325 Broadway, E/NE31</Address>
        <City>Boulder</City>
        <Province_or_State>CO</Province_or_State>
        <Postal_Code>80305-3328</Postal_Code>
        <Country>USA</Country>
      </Contact_Address>
    </Personnel>
  </Data_Center>
  <Distribution>
    <Distribution_Media>online</Distribution_Media>
    <Distribution_Format>ASCII</Distribution_Format>
  </Distribution>
  <Reference>
    <Author>Elizabeth K. Thomas, Steven C. Clemens, Youbin Sun, Warren L. Prell, Yongsong Huang, Li Gao, Shannon Loomis, Guangshan Chen, Zhengyu Liu</Author>
    <Publication_Date>2016</Publication_Date>
    <Title>Heterodynes dominate precipitation isotopes in the East Asian monsoon region, reflecting interaction of multiple climate factors</Title>
    <Series>Earth and Planetary Science Letters</Series>
    <Volume>455</Volume>
    <Pages>196-206</Pages>
    <DOI>10.1016/j.epsl.2016.09.044</DOI>
    <Online_Resource>http://www.sciencedirect.com/science/article/pii/S0012821X16305246</Online_Resource>
  </Reference>
  <Reference>
    <Author>Elizabeth K. Thomas, Steven C. Clemens, Youbin Sun, Yongsong Huang, Warren Prell, Guangshan Chen, Zhengyu Liu, Shannon Loomis</Author>
    <Publication_Date>2017</Publication_Date>
    <Title>Midlatitude land surface temperature impacts the timing and structure of glacial maxima</Title>
    <Series>Geophysical Research Letters</Series>
    <DOI>10.1002/2016GL071882</DOI>
    <Online_Resource>http://onlinelibrary.wiley.com/doi/10.1002/2016GL071882/full</Online_Resource>
  </Reference>
  <Summary>
    <Abstract>For the past decade, East Asian monsoon history has been interpreted in the context of an exceptionally well-dated, high-resolution composite record of speleothem oxygen isotopes (d18Ocave) from the Yangtze River Valley. This record is characterized by a unique spectral response, with variance concentrated predominantly within the precession band and an enigmatic lack of variance at the eccentricity and obliquity bands. Here we examine the spectral characteristics of all existing &gt;250-kyr-long terrestrial water isotope records in Asia, including a new water isotope record using leaf wax hydrogen isotope ratios from the Chinese Loess Plateau. There exist profound differences in spectral characteristics among all orbital-scale Asian water isotope records. We demonstrate that these differences result from latitudinal gradients in the influence of the winter and summer monsoons, both of which impact climate and water isotopes throughout East Asia. Water isotope records therefore do not reflect precipitation during a single season or from a single circulation system. Rather, water isotope records in East Asia reflect the complex interplay of oceanic and continental moisture sources, operating at multiple Earth-orbital periods. These non-linear interactions are reflected in water isotope spectra by the presence of heterodynes. Although complex, we submit that water isotope records, when paired with rapidly developing isotope-enabled model simulations, will have the potential to elucidate mechanisms causing seasonal precipitation variability and moisture source variability in East Asia. 
          STUDY NOTES: Leaf wax isotope (d13C and d2H) and physical properties (grain size, magnetic susceptibility) data from Weinan and Lantian, Chinese Loess Plateau, plus leaf wax-based temperature reconstruction for the past 360,000 years.</Abstract>
  </Summary>
  <Related_URL>
    <URL_Content_Type>
      <Type>GET DATA</Type>
    </URL_Content_Type>
    <URL>https://www1.ncdc.noaa.gov/pub/data/paleo/loess/china/thomas2016weinan-gs-ms.txt</URL>
    <Description>Formatted Text File ; Weinan Grain Size and Magnetic Susceptibility</Description>
  </Related_URL>
  <Related_URL>
    <URL_Content_Type>
      <Type>GET DATA</Type>
    </URL_Content_Type>
    <URL>https://www1.ncdc.noaa.gov/pub/data/paleo/loess/china/thomas2016mangshan-temp.txt</URL>
    <Description>Formatted Text File ; Mangshan Leaf Wax Data and Temperature Reconstruction</Description>
  </Related_URL>
  <Related_URL>
    <URL_Content_Type>
      <Type>GET DATA</Type>
    </URL_Content_Type>
    <URL>https://www1.ncdc.noaa.gov/pub/data/paleo/loess/china/thomas2016clp13c.txt</URL>
    <Description>Formatted Text File ; Chinese Loess Plateau Leaf Wax d13C</Description>
  </Related_URL>
  <Related_URL>
    <URL_Content_Type>
      <Type>GET DATA</Type>
    </URL_Content_Type>
    <URL>https://www1.ncdc.noaa.gov/pub/data/paleo/loess/china/thomas2016clp1ka.txt</URL>
    <Description>Formatted Text File ; Chinese Loess Plateau All Data 1ka Interpolated</Description>
  </Related_URL>
  <Related_URL>
    <URL_Content_Type>
      <Type>GET DATA</Type>
    </URL_Content_Type>
    <URL>https://www1.ncdc.noaa.gov/pub/data/paleo/loess/china/thomas2016clp2h.txt</URL>
    <Description>Formatted Text File ; Chinese Loess Plateau Leaf Wax d2H</Description>
  </Related_URL>
  <Related_URL>
    <URL_Content_Type>
      <Type>GET DATA</Type>
    </URL_Content_Type>
    <URL>https://www1.ncdc.noaa.gov/pub/data/paleo/loess/china/thomas2016weinan-temp.txt</URL>
    <Description>Formatted Text File ; Weinan Leaf Wax Data and Temperature Reconstruction</Description>
  </Related_URL>
  <IDN_Node>
    <Short_Name>USA/NOAA</Short_Name>
  </IDN_Node>
  <Metadata_Name>DIF</Metadata_Name>
  <Metadata_Version>Version 9.8.4</Metadata_Version>
  <DIF_Creation_Date>2018-12-11</DIF_Creation_Date>
  <Last_DIF_Revision_Date>2018-12-11</Last_DIF_Revision_Date>
</DIF>
