<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-lake-5496</Entry_ID>
  <Entry_Title>Lake Telmen, Mongolia 7,000 Year Sediment Data</Entry_Title>
  <Data_Set_Citation>
    <Dataset_Creator>Peck, J.A.; Khosbayar, P.</Dataset_Creator>
    <Dataset_Title>Lake Telmen, Mongolia 7,000 Year Sediment Data</Dataset_Title>
    <Dataset_Release_Date>2003-01-01</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/5496</Online_Resource>
  </Data_Set_Citation>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>J.A.</First_Name>
    <Last_Name>Peck</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>P.</First_Name>
    <Last_Name>Khosbayar</Last_Name>
  </Personnel>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>paleolimnology</Term>
    <Detailed_Variable>density,wet sediment,null,gram per cubic centimeter,null,paleolimnology,null,null,N,null</Detailed_Variable>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>paleolimnology</Term>
    <Detailed_Variable>water content,sediment,null,percent,null,paleolimnology,raw,null,N,null</Detailed_Variable>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>paleolimnology</Term>
    <Detailed_Variable>identified diatom,null,null,percent,null,paleolimnology,null,null,N,Anomoeoneis sphaerophora</Detailed_Variable>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>paleolimnology</Term>
    <Detailed_Variable>depth,null,null,centimeter,null,paleolimnology,null,null,N,null</Detailed_Variable>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>paleolimnology</Term>
    <Detailed_Variable>calcium carbonate,sediment,null,weight percent,null,paleolimnology,null,carbon coulometry,N,null</Detailed_Variable>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>paleolimnology</Term>
    <Detailed_Variable>identified diatom,null,null,percent,null,paleolimnology,null,null,N,Cyclotella caspia</Detailed_Variable>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>paleolimnology</Term>
    <Detailed_Variable>mass magnetic susceptibility,sediment,null,cubic meter per kilogram,null,paleolimnology,null,null,N,x10-6 units</Detailed_Variable>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>paleolimnology</Term>
    <Detailed_Variable>density,organic matter,null,gram per cubic centimeter,null,paleolimnology,null,null,N,null</Detailed_Variable>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>paleolimnology</Term>
    <Detailed_Variable>density,dry sediment,null,gram per cubic centimeter,null,paleolimnology,null,null,N,null</Detailed_Variable>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>paleolimnology</Term>
    <Detailed_Variable>organic matter,sediment,null,percent,null,paleolimnology,null,loss on ignition,N,null</Detailed_Variable>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>paleolimnology</Term>
    <Variable_Level_1>population abundance</Variable_Level_1>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>paleolimnology</Term>
    <Variable_Level_1>physical properties</Variable_Level_1>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>paleolimnology</Term>
    <Variable_Level_1>geochemistry</Variable_Level_1>
  </Parameters>
  <ISO_Topic_Category>geoscientificInformation</ISO_Topic_Category>
  <Paleo_Temporal_Coverage>
    <Paleo_Start_Date>7110 cal yr BP</Paleo_Start_Date>
    <Paleo_Stop_Date>0 cal yr BP</Paleo_Stop_Date>
  </Paleo_Temporal_Coverage>
  <Data_Set_Progress>Complete</Data_Set_Progress>
  <Spatial_Coverage>
    <Southernmost_Latitude>48.8129</Southernmost_Latitude>
    <Northernmost_Latitude>48.8332</Northernmost_Latitude>
    <Westernmost_Longitude>97.2367</Westernmost_Longitude>
    <Easternmost_Longitude>97.3888</Easternmost_Longitude>
    <Minimum_Altitude>1789</Minimum_Altitude>
    <Maximum_Altitude>1789</Maximum_Altitude>
  </Spatial_Coverage>
  <Location>
    <Location_Category>Continent</Location_Category>
    <Location_Type>Asia</Location_Type>
    <Location_Subregion1>Eastern Asia</Location_Subregion1>
    <Location_Subregion2>Mongolia</Location_Subregion2>
    <Detailed_Location>Lake Telmen, core TN99C4&gt;LATITUDE 48.8332&gt;LONGITUDE 97.3888</Detailed_Location>
  </Location>
  <Location>
    <Location_Category>Continent</Location_Category>
    <Location_Type>Asia</Location_Type>
    <Location_Subregion1>Eastern Asia</Location_Subregion1>
    <Location_Subregion2>Mongolia</Location_Subregion2>
    <Detailed_Location>Lake Telmen, core TN98C2&gt;LATITUDE 48.8129&gt;LONGITUDE 97.2367</Detailed_Location>
  </Location>
  <Location>
    <Location_Category>Continent</Location_Category>
    <Location_Type>Asia</Location_Type>
    <Location_Subregion1>Eastern Asia</Location_Subregion1>
    <Location_Subregion2>Mongolia</Location_Subregion2>
    <Detailed_Location>Lake Telmen, core TN99C1&gt;LATITUDE 48.8332&gt;LONGITUDE 97.3888</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>Peck, J.A., P. Khosbayar. 2002. Mid to Late Holocene climate change in northcentral Mongolia as recorded in the sediments of Lake Telmen. Palaeogeography, Palaeoclimatology, Palaeoecology Vol. 182, pp. 135-153</Reference>
  <Summary>
    <Abstract>A record of climatic change has been reconstructed for the past 7110 calibrated  calendar (cal) years for Lake Telmen, Mongolia, based upon sedimentologic and  geomorphic evidence from the lake-watershed system. Lake Telmen is a saline  (presently 4 g l-1) closed-basin lake and is therefore sensitive to changes in  effective moisture balance. Between 7110 and 6260 cal yr ago, conditions in the  Lake Telmen region were hyperarid and a small saline (approximately 20 g l-1)  lake was present. Increased effective moisture balance but still arid conditions  prevailed between 6260 and 4390 cal yr ago. Since 4390 cal yr ago, generally  more humid conditions prevailed in the Lake Telmen region. As the lake deepened,  a hypoxic hypolimnion became established below a well-developed summer thermocline  resulting in varved sediment accumulation since 4390 cal yr ago. Between about  2710 and 1260 cal yr ago, a greater than present-day effective moisture balance  is recorded by a series of four lake highstand terraces. Sedimentologic profiles  from lacustrine cores suggest an increase in effective moisture during the past  approximately 680 cal yr. 
          STUDY NOTES: Data from cores TN98C2, TN99C1 and TN99C4 from Lake Telmen, Mongolia. Data include sedimentary physical property values for core TN98C2, plus wet bulk density values, loss-on-ignition,  pollen and diatom values, carbonate content, and radiocarbon dates for cores TN99C1 and TN99C4.</Abstract>
  </Summary>
  <Related_URL>
    <URL_Content_Type>
      <Type>GET DATA</Type>
    </URL_Content_Type>
    <URL>https://www1.ncdc.noaa.gov/pub/data/paleo/paleolimnology/asia/telmen.txt</URL>
  </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>
