<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-5431</Entry_ID>
  <Entry_Title>Cruz et al. 2005 Botuvera Cave, Brazil Stalagmite Stable Isotope Data</Entry_Title>
  <Data_Set_Citation>
    <Dataset_Creator>Cruz, J.W.; Burns, S.J.; Karmann, I.; Sharp, W.D.; Vuille, M.; Cardoso, A.O.; Ferrari, J.A.; Silva Dias, P.L.; Viana, O.</Dataset_Creator>
    <Dataset_Title>Cruz et al. 2005 Botuvera Cave, Brazil Stalagmite Stable Isotope Data</Dataset_Title>
    <Dataset_Release_Date>2005-03-01</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/5431</Online_Resource>
  </Data_Set_Citation>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>J.W.</First_Name>
    <Last_Name>Cruz</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>S.J.</First_Name>
    <Last_Name>Burns</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>I.</First_Name>
    <Last_Name>Karmann</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>W.D.</First_Name>
    <Last_Name>Sharp</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>M.</First_Name>
    <Last_Name>Vuille</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>A.O.</First_Name>
    <Last_Name>Cardoso</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>J.A.</First_Name>
    <Last_Name>Ferrari</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>P.L.</First_Name>
    <Last_Name>Silva Dias</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>O.</First_Name>
    <Last_Name>Viana</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,null</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>
    <Detailed_Variable>delta 13C,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>carbon isotopes</Variable_Level_1>
  </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>Dansgaard-Oeschger cycles</Keyword>
  <Keyword>PAGES 2k Network</Keyword>
  <Keyword>PAGES LOTRED SA2k</Keyword>
  <Keyword>millennial resolution</Keyword>
  <Paleo_Temporal_Coverage>
    <Paleo_Start_Date>-114210 AD</Paleo_Start_Date>
    <Paleo_Stop_Date>1950 AD</Paleo_Stop_Date>
  </Paleo_Temporal_Coverage>
  <Paleo_Temporal_Coverage>
    <Paleo_Start_Date>116160 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>-27.22</Southernmost_Latitude>
    <Northernmost_Latitude>-27.22</Northernmost_Latitude>
    <Westernmost_Longitude>-49.16</Westernmost_Longitude>
    <Easternmost_Longitude>-49.16</Easternmost_Longitude>
    <Minimum_Altitude>230</Minimum_Altitude>
    <Maximum_Altitude>230</Maximum_Altitude>
  </Spatial_Coverage>
  <Location>
    <Location_Category>Continent</Location_Category>
    <Location_Type>South America</Location_Type>
    <Location_Subregion1>Brazil</Location_Subregion1>
    <Detailed_Location>Botuverá Cave&gt;LATITUDE -27.22&gt;LONGITUDE -49.16</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>Cruz, F.W., Jr., S.J. Burns, I. Karmann, W.D. Sharp, M. Vuille, A.O. Cardoso, J.A. Ferrari, P.L. Silva Dias, and O. Viana, Jr. 2005. Insolation-driven changes in atmospheric circulation over the past 116,000 years in subtropical Brazil. Nature, 434, No. 7029, 63-66</Reference>
  <Summary>
    <Abstract>During the last glacial period, large millennial-scale temperature
oscillation-the &apos;Dansgaard/Oeschger&apos; cycles-were the primary
climate signal in Northern Hemisphere climate archives
from the high latitudes to the tropics. But whether the
influence of these abrupt climate changes extended to the tropical
and subtropical Southern Hemisphere, where changes in insolation
are thought to be the main direct forcing of climate, has
remained unclear. Here we present a high-resolution oxygen
isotope record of a U/Th-dated stalagmite from subtropical
southern Brazil, covering the past 116,200 years. The oxygen
isotope signature varies with shifts in the source region and
amount of rainfall in the area, and hence records changes in
atmospheric circulation and convective intensity over South
America. We find that these variations in rainfall source and
amount are primarily driven by summer solar radiation, which is
controlled by the Earth&apos;s precessional cycle. The Dansgaard/
Oeschger cycles can be detected in our record and therefore we
confirm that they also affect the tropical hydrological cycle,
but that in southern subtropical Brazil, millennial-scale
climate changes are not as dominant as they are in the Northern
Hemisphere. 
          STUDY NOTES: DESCRIPTION: 
Bt2 stalagmite is a continuous record of paleoclimate changes over 
subtropical Brazil for the last 116,00 years.  The oxygen stable isotope 
(per mil VPDB) data set has a resolution of ~150 years and its age model 
is based on 20 U/Th ages.

</Abstract>
  </Summary>
  <Related_URL>
    <URL_Content_Type>
      <Type>GET DATA</Type>
    </URL_Content_Type>
    <URL>https://www1.ncdc.noaa.gov/pub/data/paleo/speleothem/southamerica/brazil/botuvera2005.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>
