<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-coral-1890</Entry_ID>
  <Entry_Title>St. Gilles Reef - Oxygen Isotope Data</Entry_Title>
  <Data_Set_Citation>
    <Dataset_Creator>Pfeiffer, M.; Timm, O.; Dullo, W.-C.; Podlech, S.</Dataset_Creator>
    <Dataset_Title>St. Gilles Reef - Oxygen Isotope Data</Dataset_Title>
    <Dataset_Release_Date>2004-11-01</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/1890</Online_Resource>
  </Data_Set_Citation>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>M.</First_Name>
    <Last_Name>Pfeiffer</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>O.</First_Name>
    <Last_Name>Timm</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>W.-C.</First_Name>
    <Last_Name>Dullo</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>S.</First_Name>
    <Last_Name>Podlech</Last_Name>
  </Personnel>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>corals and sclerosponges</Term>
    <Detailed_Variable>age,null,null,null,null,corals and sclerosponges,null,null,N,null</Detailed_Variable>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>corals and sclerosponges</Term>
    <Detailed_Variable>delta 18O,Porites sp.,null,per mil VPDB,null,corals and sclerosponges,interpolated,isotope ratio mass spectrometry,N,null</Detailed_Variable>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>corals and sclerosponges</Term>
    <Variable_Level_1>oxygen isotopes</Variable_Level_1>
  </Parameters>
  <ISO_Topic_Category>geoscientificInformation</ISO_Topic_Category>
  <Keyword>PAGES 2k Network</Keyword>
  <Keyword>PAGES Australasia 2k</Keyword>
  <Paleo_Temporal_Coverage>
    <Paleo_Start_Date>1832 AD</Paleo_Start_Date>
    <Paleo_Stop_Date>1995 AD</Paleo_Stop_Date>
  </Paleo_Temporal_Coverage>
  <Paleo_Temporal_Coverage>
    <Paleo_Start_Date>118 cal yr BP</Paleo_Start_Date>
    <Paleo_Stop_Date>-45 cal yr BP</Paleo_Stop_Date>
  </Paleo_Temporal_Coverage>
  <Data_Set_Progress>Complete</Data_Set_Progress>
  <Spatial_Coverage>
    <Southernmost_Latitude>-21.03</Southernmost_Latitude>
    <Northernmost_Latitude>-21.03</Northernmost_Latitude>
    <Westernmost_Longitude>55.25</Westernmost_Longitude>
    <Easternmost_Longitude>55.25</Easternmost_Longitude>
    <Minimum_Altitude>-12</Minimum_Altitude>
    <Maximum_Altitude>-12</Maximum_Altitude>
  </Spatial_Coverage>
  <Location>
    <Location_Category>Ocean</Location_Category>
    <Location_Type>Indian Ocean</Location_Type>
    <Location_Subregion1>Reunion</Location_Subregion1>
    <Detailed_Location>St. Gilles Reef&gt;LATITUDE -21.03&gt;LONGITUDE 55.25</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>
    <Author>Pfeiffer, M.; Timm, O.; Dullo, W.C.; Podlech, S</Author>
    <Publication_Date>2004</Publication_Date>
    <Title>Oceanic forcing of interannual and multidecadal climate variability in the southwestern Indian Ocean: Evidence from a 160 year coral isotopic record (La Rï¿½union, 55E, 21S)</Title>
    <Series>Paleoceanography</Series>
    <Volume>19</Volume>
    <DOI>10.1029/2003PA000964</DOI>
  </Reference>
  <Summary>
    <Abstract>We have developed a new 163-year bimonthly coral d18O record from  La Rï¿½union (55ï¿½E, 21ï¿½S). Interannual variations in coral d18O are  coherent with the Southern Oscillation Index but not with regional  sea surface temperature (SST). Correlations with the global SST field  suggest more negative seawater d18O (d18Osw) during La Niï¿½a years.  We propose that the signal results from changes in the strength of  the South Equatorial Current and the Indonesian throughflow, which  carry low salinity water. Multidecadal variations in coral d18O are  coherent with regional SST, but the sign is of opposite sense as  expected from the coral d18O-temperature relationship. This requires  multidecadal changes in salinity large enough to overprint the SST  contribution in the coral d18O record. Our results suggest that  multidecadal salinity variations result from modulations in the  transport of the South Equatorial Current, which varies in response  to the surface wind field and/or the Indonesian throughflow.</Abstract>
  </Summary>
  <Related_URL>
    <URL_Content_Type>
      <Type>GET DATA</Type>
    </URL_Content_Type>
    <URL>https://www1.ncdc.noaa.gov/pub/data/paleo/coral/indian_ocean/pfeiffer2004_noaa.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>
