<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-recon-12823</Entry_ID>
  <Entry_Title>Sugan Lake, NW China 1000 Year Chironomid Salinity Reconstruction </Entry_Title>
  <Data_Set_Citation>
    <Dataset_Creator>Chen, J.-H.; Chen, F.-H.; Zhang, E.L.; Brooks, S.J.; Zhou, A.F.; Zhang, J.-W.</Dataset_Creator>
    <Dataset_Title>Sugan Lake, NW China 1000 Year Chironomid Salinity Reconstruction </Dataset_Title>
    <Dataset_Release_Date>2012-03-09</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/12823</Online_Resource>
  </Data_Set_Citation>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>J.-H.</First_Name>
    <Last_Name>Chen</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>F.-H.</First_Name>
    <Last_Name>Chen</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>E.L.</First_Name>
    <Last_Name>Zhang</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>S.J.</First_Name>
    <Last_Name>Brooks</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>A.F.</First_Name>
    <Last_Name>Zhou</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>J.-W.</First_Name>
    <Last_Name>Zhang</Last_Name>
  </Personnel>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>climate reconstructions|insect|paleolimnology</Term>
    <Detailed_Variable>depth,null,null,centimeter,null,climate reconstructions|insect|paleolimnology,null,null,N,null</Detailed_Variable>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>climate reconstructions|insect|paleolimnology</Term>
    <Detailed_Variable>salinity,lake water|midge assemblage,null,standard deviation unit,null,climate reconstructions|insect|paleolimnology,null,null,N,null</Detailed_Variable>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>climate reconstructions|insect|paleolimnology</Term>
    <Detailed_Variable>age,null,null,year Common Era,null,climate reconstructions|insect|paleolimnology,null,null,N,varve year</Detailed_Variable>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>reconstructions</Term>
    <Variable_Level_1>lake salinity</Variable_Level_1>
  </Parameters>
  <ISO_Topic_Category>geoscientificInformation</ISO_Topic_Category>
  <Keyword>Other Hydroclimate Reconstruction</Keyword>
  <Keyword>hydrology</Keyword>
  <Paleo_Temporal_Coverage>
    <Paleo_Start_Date>990 AD</Paleo_Start_Date>
    <Paleo_Stop_Date>2002 AD</Paleo_Stop_Date>
  </Paleo_Temporal_Coverage>
  <Paleo_Temporal_Coverage>
    <Paleo_Start_Date>960 cal yr BP</Paleo_Start_Date>
    <Paleo_Stop_Date>-52 cal yr BP</Paleo_Stop_Date>
  </Paleo_Temporal_Coverage>
  <Data_Set_Progress>Complete</Data_Set_Progress>
  <Spatial_Coverage>
    <Southernmost_Latitude>38.8667</Southernmost_Latitude>
    <Northernmost_Latitude>38.8667</Northernmost_Latitude>
    <Westernmost_Longitude>93.8833</Westernmost_Longitude>
    <Easternmost_Longitude>93.8833</Easternmost_Longitude>
    <Minimum_Altitude>2793</Minimum_Altitude>
    <Maximum_Altitude>2793</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>Sugan Lake&gt;LATITUDE 38.8667&gt;LONGITUDE 93.8833</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>Chen, J.H., F.H. Chen, E.L. Zhang, S.J. Brooks, A.F. Zhou, 
and J.W. Zhang. 2009. 
A 1000-year chironomid-based salinity reconstruction from varved 
sediments of Sugan Lake, Qaidam Basin, arid Northwest China, 
and its palaeoclimatic significance. 
Chinese Science Bulletin, Vol.54, No. 20, pp. 3749-3759. 
doi: 10.1007/s11434-009-0201-8 
</Reference>
  <Summary>
    <Abstract>A 1000-year high-resolution (~10 years) chironomid record from varved 
sediments of Sugan Lake, Qaidam Basin on the northern Tibetan Plateau, 
is presented. The chironomid assemblages are mainly composed of the 
relatively high-saline-water taxa Psectrocladius barbimanus-type 
and Orthocladius/ Cricotopus, and the relatively low-saline-water 
taxa Procladius and Psectrocladius sordidellus-type. Variations in 
the chironomid fauna and inferred salinities suggest that over the 
last millennium, the Sugan Lake catchment has alternated between 
contrasting climatic conditions, having a dry climate during the 
period 990-1550 AD, a relatively humid climate during the Little Ice 
Age (LIA) (1550-1840 AD), and a dry climate again from 1840 AD onwards. 
At the decadal to centennial scale, a wet event around 1200-1230 AD, 
interrupting the generally arid period (990-1550 AD), and a dry event 
around 1590-1700 AD, punctuating the generally humid period 
(1550-1840 AD), are clearly documented. Trends in the chironomid-based 
salinity time series indicate a highly unstable climate during the LIA 
when salinity fluctuations were of greater magnitude and higher 
frequency. The effective moisture evolution in the Sugan Lake catchment 
during the last millennium reconstructed by chironomid analysis is in 
broad agreement with previous palaeo-moisture data derived from other 
sites in arid Northwest China (ANC). The LIA, characterized by 
generally humid conditions over the westerly-dominated ANC was 
distinctly different from that in monsoonal China, implying an 
&quot;out-of-phase&quot; relationship between moisture evolution in these 
two regions during the past 1000 years. 
 
          STUDY NOTES: Chironomid-inferred water salinity data from Sugan Lake, Qaidam Basin, 
NW China, for the last millennium. Salinity was estimated using 
a chironomid-salinity transfer function for Tibetan Plateau lakes 
developed by Zhang et al (2007).  The salinity record was standardized 
to have a zero mean and unit standard deviation. Chronology was 
established by varve counting (Zhou et al., 2007, 2009). 
</Abstract>
  </Summary>
  <Related_URL>
    <URL_Content_Type>
      <Type>GET DATA</Type>
    </URL_Content_Type>
    <URL>https://www1.ncdc.noaa.gov/pub/data/paleo/contributions_by_author/chen2009/chen2009.txt</URL>
  </Related_URL>
  <Related_URL>
    <URL_Content_Type>
      <Type>GET DATA</Type>
    </URL_Content_Type>
    <URL>https://www1.ncdc.noaa.gov/pub/data/paleo/contributions_by_author/chen2009/chen2009.xls</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>
