<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-15089</Entry_ID>
  <Entry_Title>Line Islands Coral P/Ca Reconstructions from 1981-2002</Entry_Title>
  <Data_Set_Citation>
    <Dataset_Creator>LaVigne, M.; Nurhati, I.S.; Cobb, K.M.; McGregor, H.V.; Sinclair, D.J.; Sherrell, R.M.</Dataset_Creator>
    <Dataset_Title>Line Islands Coral P/Ca Reconstructions from 1981-2002</Dataset_Title>
    <Dataset_Release_Date>2013-09-25</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/15089</Online_Resource>
  </Data_Set_Citation>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>M.</First_Name>
    <Last_Name>LaVigne</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>I.S.</First_Name>
    <Last_Name>Nurhati</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>K.M.</First_Name>
    <Last_Name>Cobb</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>H.V.</First_Name>
    <Last_Name>McGregor</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>D.J.</First_Name>
    <Last_Name>Sinclair</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>R.M.</First_Name>
    <Last_Name>Sherrell</Last_Name>
  </Personnel>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>corals and sclerosponges</Term>
    <Detailed_Variable>phosphorus/calcium,Porites sp.,null,micromole per mole,null,corals and sclerosponges,smoothed,inductively-coupled plasma mass spectrometry|laser ablation,N,smoothed using 3 month running mean</Detailed_Variable>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>corals and sclerosponges</Term>
    <Detailed_Variable>age,null,null,year Common Era,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>phosphorus/calcium,Porites lutea,null,micromole per mole,null,corals and sclerosponges,raw,inductively-coupled plasma mass spectrometry|laser ablation,N,null</Detailed_Variable>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>corals and sclerosponges</Term>
    <Detailed_Variable>phosphorus/calcium,Porites lutea,null,micromole per mole,null,corals and sclerosponges,smoothed,inductively-coupled plasma mass spectrometry|laser ablation,N,smoothed using 3 month running mean</Detailed_Variable>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>corals and sclerosponges</Term>
    <Variable_Level_1>chemistry</Variable_Level_1>
  </Parameters>
  <ISO_Topic_Category>geoscientificInformation</ISO_Topic_Category>
  <Keyword>ENSO</Keyword>
  <Keyword>Other Reconstruction</Keyword>
  <Paleo_Temporal_Coverage>
    <Paleo_Start_Date>1981 AD</Paleo_Start_Date>
    <Paleo_Stop_Date>2002 AD</Paleo_Stop_Date>
  </Paleo_Temporal_Coverage>
  <Paleo_Temporal_Coverage>
    <Paleo_Start_Date>-31 cal yr BP</Paleo_Start_Date>
    <Paleo_Stop_Date>-52 cal yr BP</Paleo_Stop_Date>
  </Paleo_Temporal_Coverage>
  <Data_Set_Progress>Complete</Data_Set_Progress>
  <Spatial_Coverage>
    <Southernmost_Latitude>1.855333</Southernmost_Latitude>
    <Northernmost_Latitude>3.86667</Northernmost_Latitude>
    <Westernmost_Longitude>-159.36667</Westernmost_Longitude>
    <Easternmost_Longitude>-157.4</Easternmost_Longitude>
    <Minimum_Altitude>-11</Minimum_Altitude>
    <Maximum_Altitude>0</Maximum_Altitude>
  </Spatial_Coverage>
  <Location>
    <Location_Category>Ocean</Location_Category>
    <Location_Type>Pacific Ocean</Location_Type>
    <Location_Subregion1>Central Pacific Ocean</Location_Subregion1>
    <Location_Subregion2>Kiribati</Location_Subregion2>
    <Detailed_Location>Fanning Island West&gt;LATITUDE 3.86667&gt;LONGITUDE -159.36667</Detailed_Location>
  </Location>
  <Location>
    <Location_Category>Ocean</Location_Category>
    <Location_Type>Pacific Ocean</Location_Type>
    <Location_Subregion1>Central Pacific Ocean</Location_Subregion1>
    <Location_Subregion2>Kiribati</Location_Subregion2>
    <Detailed_Location>Christmas Island Coral 2&gt;LATITUDE 1.883333&gt;LONGITUDE -157.4</Detailed_Location>
  </Location>
  <Location>
    <Location_Category>Ocean</Location_Category>
    <Location_Type>Pacific Ocean</Location_Type>
    <Location_Subregion1>Central Pacific Ocean</Location_Subregion1>
    <Location_Subregion2>Kiribati</Location_Subregion2>
    <Detailed_Location>Christmas Island Coral 1&gt;LATITUDE 1.855333&gt;LONGITUDE -157.500133</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>LaVigne, M., I.S. Nurhati, K.M. Cobb, H.V. McGregor, D. Sinclair, and R.M. Sherrell</Author>
    <Publication_Date>2013</Publication_Date>
    <Title>Systematic ENSO-driven nutrient variability recorded by central equatorial Pacific corals</Title>
    <Series>Geophysical Research Letters</Series>
    <Volume>40</Volume>
    <Issue>15</Issue>
    <Pages>3956-3961</Pages>
    <DOI>10.1002/grl.50765</DOI>
  </Reference>
  <Summary>
    <Abstract>Variations in ocean productivity are driven largely by nutrient supply to the photic zone, but temporal records of nutrient variability are sparse. Here we show scleractinian coral P/Ca proxy records of variations in phosphate concentrations during El Niño Southern Oscillation (ENSO) cycles in the central equatorial Pacific. Covarying P/Ca records in Porites corals from Christmas and Fanning Islands show a regional ~40% decrease during the upwelling relaxation of the 1997-1998 El Niño, consistent with less frequent nutrient measurements from this area. Similar ~35-45% skeletal P/Ca decreases occur during the 1982–1983 and 1986-1987 El Niño events, which predate satellite color and regional nutrient measurements. After each El Niño event, nutrient increases lag temperature recovery by 4-12months, likely reflecting uptake by massive phytoplankton blooms that followed resumption of upwelling. The results support the utility of coral P/Ca to probe the mechanisms linking ENSO, equatorial upwelling, and carbon cycling in the past. 
          STUDY NOTES: This dataset contains skeletal P/Ca data from 3 Line Island coral records through 3 El Nino events (Fanning and Christmas Islands).  This dataset includes all P/Ca data published in LaVigne et al., 2013.  Details on chronologies and methodology can be found in the original publication.</Abstract>
  </Summary>
  <Related_URL>
    <URL_Content_Type>
      <Type>GET DATA</Type>
    </URL_Content_Type>
    <URL>https://www1.ncdc.noaa.gov/pub/data/paleo/contributions_by_author/lavigne2013/lavigne2013-fanning.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/contributions_by_author/lavigne2013/lavigne2013-christmas1.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/contributions_by_author/lavigne2013/lavigne2013-christmas2.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>
