<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-10434</Entry_ID>
  <Entry_Title>Laguna de Los Anteojos, Venezuela Younger Dryas Sediment Data</Entry_Title>
  <Data_Set_Citation>
    <Dataset_Creator>Stansell, N.D.; Abbott, M.B.; Rull, V.; Rodbell, D.; Bezada, M.; Montoya, E.</Dataset_Creator>
    <Dataset_Title>Laguna de Los Anteojos, Venezuela Younger Dryas Sediment Data</Dataset_Title>
    <Dataset_Release_Date>2010-04-24</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/10434</Online_Resource>
  </Data_Set_Citation>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>N.D.</First_Name>
    <Last_Name>Stansell</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>M.B.</First_Name>
    <Last_Name>Abbott</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>V.</First_Name>
    <Last_Name>Rull</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>D.</First_Name>
    <Last_Name>Rodbell</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>M.</First_Name>
    <Last_Name>Bezada</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>E.</First_Name>
    <Last_Name>Montoya</Last_Name>
  </Personnel>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>paleolimnology</Term>
    <Detailed_Variable>carbon/nitrogen,sediment,null,dimensionless,null,paleolimnology,null,null,N,null</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>biogenic silica,sediment,null,weight percent,null,paleolimnology,smoothed,spectrophotometry,N,smoothed using lowess 0.01</Detailed_Variable>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>paleolimnology</Term>
    <Detailed_Variable>density,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>volume magnetic susceptibility,sediment,null,dimensionless (SI system),null,paleolimnology,null,magnetic susceptibility measurement with point or surface sensor,N,x10-6 units</Detailed_Variable>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>paleolimnology</Term>
    <Detailed_Variable>titanium,sediment,null,count per second,null,paleolimnology,null,x-ray fluorescence spectroscopy,N,null</Detailed_Variable>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>paleolimnology</Term>
    <Detailed_Variable>biogenic silica,sediment,null,weight percent,null,paleolimnology,null,spectrophotometry,N,null</Detailed_Variable>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>paleolimnology</Term>
    <Detailed_Variable>age,null,null,calendar year before present,null,paleolimnology,null,null,N,null</Detailed_Variable>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>paleolimnology</Term>
    <Detailed_Variable>titanium,sediment,null,count per second,null,paleolimnology,smoothed,x-ray fluorescence spectroscopy,N,smoothed using lowess 0.01</Detailed_Variable>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>paleolimnology</Term>
    <Detailed_Variable>mineral matter,sediment,null,weight percent,null,paleolimnology,null,null,N,calculated as 100% minus organic matter minus Biogenic silica</Detailed_Variable>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>paleolimnology</Term>
    <Detailed_Variable>organic matter,sediment,null,weight percent,null,paleolimnology,null,loss on ignition,N,550 degrees C</Detailed_Variable>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>paleolimnology</Term>
    <Variable_Level_1>magnetic susceptibility</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>
  <Keyword>PAGES 2k Network</Keyword>
  <Keyword>PAGES LOTRED SA2k</Keyword>
  <Keyword>Younger Dryas</Keyword>
  <Keyword>abrupt climate change</Keyword>
  <Paleo_Temporal_Coverage>
    <Paleo_Start_Date>14737 cal yr BP</Paleo_Start_Date>
    <Paleo_Stop_Date>9501 cal yr BP</Paleo_Stop_Date>
  </Paleo_Temporal_Coverage>
  <Data_Set_Progress>Complete</Data_Set_Progress>
  <Spatial_Coverage>
    <Southernmost_Latitude>8.5383</Southernmost_Latitude>
    <Northernmost_Latitude>8.5383</Northernmost_Latitude>
    <Westernmost_Longitude>-71.0737</Westernmost_Longitude>
    <Easternmost_Longitude>-71.0737</Easternmost_Longitude>
    <Minimum_Altitude>3920</Minimum_Altitude>
    <Maximum_Altitude>3920</Maximum_Altitude>
  </Spatial_Coverage>
  <Location>
    <Location_Category>Continent</Location_Category>
    <Location_Type>South America</Location_Type>
    <Location_Subregion1>Venezuela</Location_Subregion1>
    <Detailed_Location>Laguna de Los Anteojos&gt;LATITUDE 8.5383&gt;LONGITUDE -71.0737</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>Stansell, N.D., M.B. Abbott, V. Rull, D.T. Rodbell, M. Bezada, 
and E. Montoya. 2010. 
Abrupt Younger Dryas cooling in the northern tropics recorded 
in lake sediments from the Venezuelan Andes. 
Earth and Planetary Science Letters, Vol. 293, pp. 154-163.  
doi:10.1016/j.epsl.2010.02.040 
</Reference>
  <Summary>
    <Abstract>A radiocarbon dated sediment record from Laguna de Los Anteojos, 
a cirque lake in the Mérida Andes of Venezuela, indicates that 
warmer and wetter atmospheric conditions occurred in the northern 
tropics at the onset of the Bølling (~14,600 cal yr BP), and 
abruptly colder and drier conditions around the time of the
Younger Dryas (YD). Geochemical and clastic sediment analyses 
from Los Anteojos show that glaciers advanced at ~12,850 cal yr BP, 
reached their YD maximum extent at ~12,650 cal yr BP, and then 
retreated until complete deglaciation of the watershed at ~11,750 
cal yr BP. The onset of warmer conditions that ended the coldest 
phase of the YD occurred several hundred years earlier at Los 
Anteojos than in the high latitudes of the Northern Hemisphere. 
During the peak YD glacial advance, glacier equilibrium-line 
altitudes in the region were ~360 to 480 m lower, and temperature 
was ~2.2 to 2.9°C colder than modern.  Independent palynological 
evidence from the Los Anteojos sediment core indicates that the 
northern Andes were more arid and at least 2.3°C colder during 
the YD. The direction and timing of glacial fluctuations in
Venezuela are consistent with observations of marine sediment 
records from the Cariaco Basin that suggest abrupt cooling 
occurred at ~12,850 cal yr BP, followed by a shift to higher 
temperature after ~12,300 cal yr BP. The timing and pattern 
of climatic changes in northern South America are also consistent 
with paleoclimate records from the southern Tropical Andes that 
suggest a southward shift in the position of the Intertropical 
Convergence Zone occurred at the start of the cooling event, 
followed by a return to wetter conditions in northern South 
America during the late stages of the YD. The early warming 
of the tropical atmosphere and invigoration of the hydrologic 
cycle likely contributed to the shift to increased temperature 
in the higher latitudes of the Northern Hemisphere at the end 
of the late glacial stage.

 
          STUDY NOTES: Multiproxy lake sediment data from Laguna de Los Anteojos 
in the Mérida Andes of Venezuela, covering the Younger Dryas 
climate event.  
</Abstract>
  </Summary>
  <Related_URL>
    <URL_Content_Type>
      <Type>GET DATA</Type>
    </URL_Content_Type>
    <URL>https://www1.ncdc.noaa.gov/pub/data/paleo/paleolimnology/southamerica/venezuela/los-anteojos2010.xls</URL>
  </Related_URL>
  <Related_URL>
    <URL_Content_Type>
      <Type>GET DATA</Type>
    </URL_Content_Type>
    <URL>https://www1.ncdc.noaa.gov/pub/data/paleo/paleolimnology/southamerica/venezuela/los-anteojos2010.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>
