<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-9739</Entry_ID>
  <Entry_Title>Pink Panther Cave 12KYr Stalagmite Oxygen Isotope Data</Entry_Title>
  <Data_Set_Citation>
    <Dataset_Creator>Asmerom, Y.; Polyak, V.J.; Burns, S.J.</Dataset_Creator>
    <Dataset_Title>Pink Panther Cave 12KYr Stalagmite Oxygen Isotope Data</Dataset_Title>
    <Dataset_Release_Date>2010-10-08</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/9739</Online_Resource>
  </Data_Set_Citation>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>Y.</First_Name>
    <Last_Name>Asmerom</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>V.J.</First_Name>
    <Last_Name>Polyak</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>S.J.</First_Name>
    <Last_Name>Burns</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,null</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,present defined as 2003 CE</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>
    <Variable_Level_1>oxygen isotopes</Variable_Level_1>
  </Parameters>
  <ISO_Topic_Category>geoscientificInformation</ISO_Topic_Category>
  <Keyword>Pacific Decadal Oscillation</Keyword>
  <Keyword>hydrology</Keyword>
  <Paleo_Temporal_Coverage>
    <Paleo_Start_Date>12087 cal yr BP</Paleo_Start_Date>
    <Paleo_Stop_Date>-15 cal yr BP</Paleo_Stop_Date>
  </Paleo_Temporal_Coverage>
  <Data_Set_Progress>Complete</Data_Set_Progress>
  <Spatial_Coverage>
    <Southernmost_Latitude>32.083</Southernmost_Latitude>
    <Northernmost_Latitude>32.083</Northernmost_Latitude>
    <Westernmost_Longitude>-105.1667</Westernmost_Longitude>
    <Easternmost_Longitude>-105.1667</Easternmost_Longitude>
  </Spatial_Coverage>
  <Location>
    <Location_Category>Continent</Location_Category>
    <Location_Type>North America</Location_Type>
    <Location_Subregion1>United States Of America</Location_Subregion1>
    <Location_Subregion2>New Mexico</Location_Subregion2>
    <Detailed_Location>Pink Panther Cave&gt;LATITUDE 32.083&gt;LONGITUDE -105.1667</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>Asmerom, Y., V. Polyak, S. Burns, and J. Rassmussen. 2007. 
Solar forcing of Holocene climate: New insights from 
a speleothem record, southwestern United States. 
Geology, vol. 35, no. 1, pp. 1-4, January 2007. 
doi: 10.1130/G22865A.1</Reference>
  <Summary>
    <Abstract>Holocene climate change has likely had a profound influence 
on ecosystems and culture. A link between solar forcing and 
Holocene climate, such as the Asian monsoon, has been shown 
for some regions, although no mechanism for this relationship 
has been suggested. Here we present the first high-resolution 
complete Holocene climate record for the North American monsoon 
region of the southwestern United States (southwest) in order 
to address the nature and causes of Holocene climate change. 
We show that periods of increased solar radiation correlate 
with decreased rainfall, the opposite to that observed in the 
Asian monsoon, and suggest that a solar link to Holocene 
climate is through changes in the Walker circulation and the 
Pacific Decadal Oscillation and El Niño-Southern Oscillation 
systems of the tropical Pacific Ocean. Given the link between 
increased warming and aridity in the southwest, additional 
warming due to greenhouse forcing could potentially lead to 
persistent hyperarid conditions, similar to those seen in 
our record during periods of high solar activity. 
 
          STUDY NOTES: High-resolution (average time step 17 years) Holocene 
stalagmite oxygen isotope data from Pink Panther Cave 
in the Guadalupe Mountains, New Mexico.  

Oxygen stable isotope ratios were measured at 200 um 
intervals from sample PP1, a 14-cm-long stalagmite, 
for a total of 681 samples, an average time resolution 
of 17 yr over the entire period.
</Abstract>
  </Summary>
  <Related_URL>
    <URL_Content_Type>
      <Type>GET DATA</Type>
    </URL_Content_Type>
    <URL>https://www1.ncdc.noaa.gov/pub/data/paleo/speleothem/northamerica/usa/newmexico/pink-panther2007.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/speleothem/northamerica/usa/newmexico/pink-panther2007.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/syntrace/speleothem/cave-pink-panther-pp-1.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>
