<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-10749</Entry_ID>
  <Entry_Title>Bison Lake, Colorado Holocene Calcite Oxygen Isotope Data</Entry_Title>
  <Data_Set_Citation>
    <Dataset_Creator>Anderson, L.</Dataset_Creator>
    <Dataset_Title>Bison Lake, Colorado Holocene Calcite Oxygen Isotope Data</Dataset_Title>
    <Dataset_Release_Date>2011-04-06</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/10749</Online_Resource>
  </Data_Set_Citation>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>L.</First_Name>
    <Last_Name>Anderson</Last_Name>
  </Personnel>
  <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>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>delta 18O,carbonate,null,per mil VPDB,null,paleolimnology,null,isotope ratio mass spectrometry,N,null</Detailed_Variable>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>paleolimnology</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>10201 cal yr BP</Paleo_Start_Date>
    <Paleo_Stop_Date>-58 cal yr BP</Paleo_Stop_Date>
  </Paleo_Temporal_Coverage>
  <Data_Set_Progress>Complete</Data_Set_Progress>
  <Spatial_Coverage>
    <Southernmost_Latitude>39.7653</Southernmost_Latitude>
    <Northernmost_Latitude>39.7653</Northernmost_Latitude>
    <Westernmost_Longitude>-107.3464</Westernmost_Longitude>
    <Easternmost_Longitude>-107.3464</Easternmost_Longitude>
    <Minimum_Altitude>3255</Minimum_Altitude>
    <Maximum_Altitude>3255</Maximum_Altitude>
  </Spatial_Coverage>
  <Location>
    <Location_Category>Continent</Location_Category>
    <Location_Type>North America</Location_Type>
    <Location_Subregion1>United States Of America</Location_Subregion1>
    <Location_Subregion2>Colorado</Location_Subregion2>
    <Detailed_Location>Bison Lake&gt;LATITUDE 39.7653&gt;LONGITUDE -107.3464</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>Anderson, L. 2011. 
Holocene record of precipitation seasonality from lake calcite 
d18O in the central Rocky Mountains, United States. 
Geology, Vol. 39, pp. 211-214, March 2011, doi:10.1130/G31575.1 
</Reference>
  <Summary>
    <Abstract>A context for recent hydroclimatic extremes and variability 
is provided by a ~10 k.y. sediment carbonate oxygen isotope 
(d18O) record at 5-100 yr resolution from Bison Lake, 3255m 
above sea level, in northwestern Colorado (United States). 
Winter precipitation is the primary water source for the alpine 
headwater lake in the Upper Colorado River Basin and lake water 
d18O measurements reflect seasonal variations in precipitation 
d18O. Holocene lake water d18O variations are inferred from 
endogenic sedimentary calcite d18O based on comparisons with 
historic watershed discharge records and tree-ring reconstructions. 
Drought periods (i.e., drier winters and/or a more rain-dominated 
seasonal precipitation balance) generally correspond with higher 
calcite d18O values, and vice-versa. Early to middle Holocene 
d18O values are higher, implying a rain-dominated seasonal 
precipitation balance. Lower, more variable d18O values after 
ca. 3500 yr ago indicate a snow-dominated but more seasonally 
variable precipitation balance. The middle to late Holocene 
d18O record corresponds with records of El Niño Southern 
Oscillation intensification that supports a teleconnection 
between Rocky Mountain climate and North Pacific sea-surface 
temperatures at decade to century time scales. 
 
          STUDY NOTES: Calcite oxygen isotope (d18O) data for the Holocene from
Bison Lake, northwest Colorado, USA.  

Calcite-d18O ratios of bulk sediment 32um size fraction 
from continuous intervals of 0.25 cm from 0 to 5 cm depth, 
at 1.0 cm intervals from 5 to 69 cm depth and at spaced 
intervals of 2.0 cm from 69 to 300 cm depth. 
</Abstract>
  </Summary>
  <Related_URL>
    <URL_Content_Type>
      <Type>GET DATA</Type>
    </URL_Content_Type>
    <URL>https://www1.ncdc.noaa.gov/pub/data/paleo/paleolimnology/northamerica/usa/colorado/bison2011.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/northamerica/usa/colorado/bison2011.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>
