<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-8404</Entry_ID>
  <Entry_Title>Wang et al. 2004 NE Brazil Speleothem/Travertine Growth Phases</Entry_Title>
  <Data_Set_Citation>
    <Dataset_Creator>Wang, X.; Auler, A.S.; Edwards, R.L.; Cheng, H.; Cristalli, P.S.; Smart, P.L.; Richards, D.A.; Shen, C.-C.</Dataset_Creator>
    <Dataset_Title>Wang et al. 2004 NE Brazil Speleothem/Travertine Growth Phases</Dataset_Title>
    <Dataset_Release_Date>2004-12-09</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/8404</Online_Resource>
  </Data_Set_Citation>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>X.</First_Name>
    <Last_Name>Wang</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>A.S.</First_Name>
    <Last_Name>Auler</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>R.L.</First_Name>
    <Last_Name>Edwards</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>H.</First_Name>
    <Last_Name>Cheng</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>P.S.</First_Name>
    <Last_Name>Cristalli</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>P.L.</First_Name>
    <Last_Name>Smart</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>D.A.</First_Name>
    <Last_Name>Richards</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>C.-C.</First_Name>
    <Last_Name>Shen</Last_Name>
  </Personnel>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>speleothems</Term>
    <Variable_Level_1>age control</Variable_Level_1>
  </Parameters>
  <ISO_Topic_Category>geoscientificInformation</ISO_Topic_Category>
  <Keyword>PAGES 2k Network</Keyword>
  <Keyword>PAGES LOTRED SA2k</Keyword>
  <Paleo_Temporal_Coverage>
    <Paleo_Start_Date>132500 cal yr BP</Paleo_Start_Date>
    <Paleo_Stop_Date>12800 cal yr BP</Paleo_Stop_Date>
  </Paleo_Temporal_Coverage>
  <Data_Set_Progress>Complete</Data_Set_Progress>
  <Spatial_Coverage>
    <Southernmost_Latitude>-10.1666</Southernmost_Latitude>
    <Northernmost_Latitude>-10.1666</Northernmost_Latitude>
    <Westernmost_Longitude>-40.833</Westernmost_Longitude>
    <Easternmost_Longitude>-40.833</Easternmost_Longitude>
    <Minimum_Altitude>500</Minimum_Altitude>
    <Maximum_Altitude>500</Maximum_Altitude>
  </Spatial_Coverage>
  <Location>
    <Location_Category>Continent</Location_Category>
    <Location_Type>South America</Location_Type>
    <Location_Subregion1>Brazil</Location_Subregion1>
    <Detailed_Location>Lapa dos Brejoes&gt;LATITUDE -10.1666&gt;LONGITUDE -40.833</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>Wang, X., A.S. Auler, R.L. Edwards, H. Cheng, P.S. Cristalli, P.L. Smart, D.A. Richards, and C.-C. Shen. 2004. Wet periods in northeastern Brazil over the past 210 kyr linked to distant climate anomalies. Nature, 432, 740-743. doi:10.1038/nature03067</Reference>
  <Summary>
    <Abstract>The tropics are the main source of the atmosphere&apos;s sensible 
and latent heat, and water vapour, and are therefore important 
for reconstructions of past climate. But long, accurately dated
records of southern tropical palaeoclimate, which would allow
the establishment of climatic connections to distant regions, 
have not been available. Here we present a 210,000-year (210-kyr)
record of wet periods in tropical northeastern Brazil - a region
that is currently semi-arid. The record is obtained from speleothems
and travertine deposits that are accurately dated using the U/Th 
method. We find wet periods that are synchronous with periods of 
weak East Asian summer monsoons, cold periods in Greenland, 
Heinrich events in the North Atlantic and periods of decreased 
river runoff to the Cariaco basin.  We infer that the wet periods 
may be explained with a southward displacement of the Intertropical 
Convergence Zone. This widespread synchroneity of climate anomalies 
suggests a relatively rapid global reorganization of the ocean-
atmosphere system.  We conclude that the wet periods probably 
affected rainforest distribution, as plant fossils show that 
forest expansion occurred during these intermittent wet intervals, 
and opened a forest corridor between the Amazonian and Atlantic 
rainforests.</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/northeast-brazil2004.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>2019-04-01</DIF_Creation_Date>
  <Last_DIF_Revision_Date>2019-04-01</Last_DIF_Revision_Date>
</DIF>
