<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-cave-20446</Entry_ID>
  <Entry_Title>Jeita Cave, Lebanon 20,000 Year Speleothem Stable Isotope Data</Entry_Title>
  <Data_Set_Citation>
    <Dataset_Creator>Cheng, H.; Sinha, A.; Verheyden, S.; Nader, F.H.; Li, X.L.; Zhang, P.Z.; Yin, J.J.; Yi, L.; Peng, Y.B.; Rao, Z.G.; Ning, Y.F.; Edwards, R.L.</Dataset_Creator>
    <Dataset_Title>Jeita Cave, Lebanon 20,000 Year Speleothem Stable Isotope Data</Dataset_Title>
    <Dataset_Release_Date>2016-08-26</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/20446</Online_Resource>
  </Data_Set_Citation>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>H.</First_Name>
    <Last_Name>Cheng</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>A.</First_Name>
    <Last_Name>Sinha</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>S.</First_Name>
    <Last_Name>Verheyden</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>F.H.</First_Name>
    <Last_Name>Nader</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>X.L.</First_Name>
    <Last_Name>Li</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>P.Z.</First_Name>
    <Last_Name>Zhang</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>J.J.</First_Name>
    <Last_Name>Yin</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>L.</First_Name>
    <Last_Name>Yi</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>Y.B.</First_Name>
    <Last_Name>Peng</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>Z.G.</First_Name>
    <Last_Name>Rao</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>Y.F.</First_Name>
    <Last_Name>Ning</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>R.L.</First_Name>
    <Last_Name>Edwards</Last_Name>
  </Personnel>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>speleothems</Term>
    <Detailed_Variable>depth,null,null,millimeter,null,speleothems,null,null,N,distance from top</Detailed_Variable>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>speleothems</Term>
    <Detailed_Variable>age,null,null,calendar year before present,null,speleothems,null,null,N,null</Detailed_Variable>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>speleothems</Term>
    <Detailed_Variable>delta 18O,calcium carbonate,null,per mil VPDB,null,speleothems,raw,isotope ratio mass spectrometry,N,null</Detailed_Variable>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>speleothems</Term>
    <Detailed_Variable>sample identification,null,null,null,null,speleothems,null,null,N,stalagmite ID</Detailed_Variable>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>speleothems</Term>
    <Detailed_Variable>delta 13C,calcium carbonate,null,per mil VPDB,null,speleothems,raw,isotope ratio mass spectrometry,N,null</Detailed_Variable>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>speleothems</Term>
    <Variable_Level_1>carbon isotopes</Variable_Level_1>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>speleothems</Term>
    <Variable_Level_1>oxygen isotopes</Variable_Level_1>
  </Parameters>
  <ISO_Topic_Category>geoscientificInformation</ISO_Topic_Category>
  <Keyword>hydrology</Keyword>
  <Paleo_Temporal_Coverage>
    <Paleo_Start_Date>20367 cal yr BP</Paleo_Start_Date>
    <Paleo_Stop_Date>372 cal yr BP</Paleo_Stop_Date>
  </Paleo_Temporal_Coverage>
  <Data_Set_Progress>Complete</Data_Set_Progress>
  <Spatial_Coverage>
    <Southernmost_Latitude>33.95</Southernmost_Latitude>
    <Northernmost_Latitude>33.95</Northernmost_Latitude>
    <Westernmost_Longitude>35.65</Westernmost_Longitude>
    <Easternmost_Longitude>35.65</Easternmost_Longitude>
    <Minimum_Altitude>100</Minimum_Altitude>
    <Maximum_Altitude>100</Maximum_Altitude>
  </Spatial_Coverage>
  <Location>
    <Location_Category>Continent</Location_Category>
    <Location_Type>Asia</Location_Type>
    <Location_Subregion1>Western Asia</Location_Subregion1>
    <Location_Subregion2>Middle East</Location_Subregion2>
    <Location_Subregion3>Lebanon</Location_Subregion3>
    <Detailed_Location>Jeita Cave&gt;LATITUDE 33.95&gt;LONGITUDE 35.65</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>H. Cheng, A. Sinha, S. Verheyden, F.H. Nader, X.L. Li, P.Z. Zhang, J.J. Yin, L. Yi, Y.B. Peng, Z.G. Rao, Y.F. Ning, R.L. Edwards</Author>
    <Publication_Date>2015</Publication_Date>
    <Title>The climate variability in northern Levant over the past 20,000 years</Title>
    <Series>Geophysical Research Letters</Series>
    <Volume>42</Volume>
    <Issue>20</Issue>
    <Pages>8641-8650</Pages>
    <DOI>10.1002/2015GL065397</DOI>
    <Online_Resource>http://onlinelibrary.wiley.com/doi/10.1002/2015GL065397/full</Online_Resource>
  </Reference>
  <Summary>
    <Abstract>The Levant constitutes an important region for assessing linkages between climate and societal changes throughout the course of human history. However, large uncertainties remain in our understanding of the region&apos;s hydroclimate variability under varying boundary conditions. Here we present a new high-resolution, precisely dated speleothem oxygen-carbon isotope and Sr/Ca records, spanning the last 20 ka from Jeita Cave, northern Levant. Our record reveals a higher (lower) precipitation-evaporation (P-E) balance during the Last Glacial Maximum and Bolling interstadial (Heinrich stadial 1). The early-middle Holocene is characterized by a trend toward higher P-E state, culminating between ~7 and 6 ka. The middle-late Holocene is characterized by two millennial-length drier periods during 5.3-4.2 and 2.8-1.4 ka. On submillennial time scale, the northern Levant climate variability is dominated by 500 year periodicity. Comparisons with the regional proxy records suggest persistent out-of-phase climate variability between the northern and southern Levant on a wide range of timescales. 
          STUDY NOTES: Speleothem stable isotope (d18O and d13C) data from 3 stalagmites collected in Jeita Cave, Lebanon for the past 20,000 years</Abstract>
  </Summary>
  <Related_URL>
    <URL_Content_Type>
      <Type>GET DATA</Type>
    </URL_Content_Type>
    <URL>https://www1.ncdc.noaa.gov/pub/data/paleo/speleothem/asia/lebanon/jeita2015iso.txt</URL>
    <Description>Data File; Jeita Cave Stable Isotope Data</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>2019-05-23</DIF_Creation_Date>
  <Last_DIF_Revision_Date>2019-05-23</Last_DIF_Revision_Date>
</DIF>
