<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-ocean-10551</Entry_ID>
  <Entry_Title>Western Equatorial Pacific ODP806B Late Pliocene Mg/Ca, d18O, and SST</Entry_Title>
  <Data_Set_Citation>
    <Dataset_Creator>Medina-Elizalde, M.; Lea, D.W.</Dataset_Creator>
    <Dataset_Title>Western Equatorial Pacific ODP806B Late Pliocene Mg/Ca, d18O, and SST</Dataset_Title>
    <Dataset_Release_Date>2011-03-18</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/10551</Online_Resource>
  </Data_Set_Citation>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>M.</First_Name>
    <Last_Name>Medina-Elizalde</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>D.W.</First_Name>
    <Last_Name>Lea</Last_Name>
  </Personnel>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>climate reconstructions|paleoceanography</Term>
    <Detailed_Variable>sea surface temperature,magnesium/calcium,null,degree Celsius,null,climate reconstructions|paleoceanography,null,null,N,G. ruber</Detailed_Variable>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>climate reconstructions|paleoceanography</Term>
    <Detailed_Variable>delta 18O,delta 18O|magnesium/calcium|sea water,null,per mil,null,climate reconstructions|paleoceanography,null,null,N,G. ruber</Detailed_Variable>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>paleoceanography</Term>
    <Detailed_Variable>depth,null,null,meter,null,paleoceanography,null,null,N,null</Detailed_Variable>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>paleoceanography</Term>
    <Detailed_Variable>age,null,null,calendar kiloyear before present,null,paleoceanography,null,null,N,null</Detailed_Variable>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>paleoceanography</Term>
    <Detailed_Variable>magnesium/calcium,Globigerinoides ruber,null,dimensionless,null,paleoceanography,null,null,N,null</Detailed_Variable>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>paleoceanography</Term>
    <Detailed_Variable>depth,null,null,meter,null,paleoceanography,corrected,null,N,null</Detailed_Variable>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>paleoceanography</Term>
    <Detailed_Variable>delta 18O,Globigerinoides ruber,null,per mil,null,paleoceanography,null,null,N,null</Detailed_Variable>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>paleocean</Term>
    <Variable_Level_1>geochemistry</Variable_Level_1>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>paleocean</Term>
    <Variable_Level_1>oxygen isotopes</Variable_Level_1>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>paleocean</Term>
    <Variable_Level_1>reconstruction</Variable_Level_1>
  </Parameters>
  <ISO_Topic_Category>geoscientificInformation</ISO_Topic_Category>
  <Keyword>Sea Surface Temperature Reconstruction</Keyword>
  <Keyword>Warm Pool</Keyword>
  <Paleo_Temporal_Coverage>
    <Paleo_Start_Date>3087400 cal yr BP</Paleo_Start_Date>
    <Paleo_Stop_Date>2336900 cal yr BP</Paleo_Stop_Date>
  </Paleo_Temporal_Coverage>
  <Data_Set_Progress>Complete</Data_Set_Progress>
  <Spatial_Coverage>
    <Southernmost_Latitude>.32</Southernmost_Latitude>
    <Northernmost_Latitude>.32</Northernmost_Latitude>
    <Westernmost_Longitude>159.35</Westernmost_Longitude>
    <Easternmost_Longitude>159.35</Easternmost_Longitude>
    <Minimum_Altitude>-2520</Minimum_Altitude>
    <Maximum_Altitude>-2520</Maximum_Altitude>
  </Spatial_Coverage>
  <Location>
    <Location_Category>Ocean</Location_Category>
    <Location_Type>Pacific Ocean</Location_Type>
    <Location_Subregion1>North Pacific Ocean</Location_Subregion1>
    <Detailed_Location>ODP 806B&gt;LATITUDE .32&gt;LONGITUDE 159.35</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>Medina-Elizalde, M. and D.W. Lea. 2010. 
Late Pliocene equatorial Pacific. 
Paleoceanography, 25, PA2208, doi:10.1029/2009PA001780 
</Reference>
  <Summary>
    <Abstract>Late Pliocene foraminiferal Mg/Ca and d18O records from Ocean 
Drilling Program Hole 806B in the western equatorial Pacific (WEP) 
reveal warm pool climate evolution during the onset of Northern 
Hemisphere glaciation, 3.1-2.3 Myr B.P. Mg/Ca data indicate an 
average late Pliocene sea surface temperature (SST) of 27.8°C, 
a small long-term cooling of 0.3°C between 3.1 and 2.3 Ma, 
and a glacial-interglacial (G-I) SST range of 2°C throughout 
this time interval. For comparison, Pleistocene SSTs at this site 
over the last 0.9 Myr average 27.7°C with a G-I range of 3°C. 
Orbital-scale variability in Hole 806B SSTs during the late 
Pliocene occurs predominantly at ~100 ka, in contrast to 
foraminiferal d18O records, which show a dominant 41 kyr period. 
Variability at a 41 kyr period, out of phase with local annual 
insolation changes driven by obliquity, is also observed in the 
new WEP SST record. The WEP SST record suggests that an ~3°C 
equatorial Pacific SST zonal gradient prevailed during the 
late Pliocene, compatible with a weaker Walker circulation. 
Adjustment of Hole 806B SSTs for past changes in seawater Mg/Ca 
suggests that SSTs higher than 30°C prevailed at 3 Myr B.P., 
followed by a progressive cooling of the warm pool through 
the late Pliocene. The characteristics of late Pliocene tropical 
climate evolution suggest that atmospheric greenhouse gas forcing 
played a major role in driving the observed G-I SST changes. 
 
          STUDY NOTES: Planktonic foraminiferal (G. ruber) Mg/Ca and d18O, plus Sea Surface 
Temperature (SST) and d18Oseawater estimates, for the Late Pliocene  
from Western Equatorial Pacific sediment core ODP806B. 

SST estimated from G. ruber Mg/Ca by the method of Lea et al. [2000]. 
d18O seawater record was calculated by removing the temperature 
component in planktonic d18O using the Mg/Ca derived SSTs and the 
paleotemperature equation of Bemis et al., [1998].

</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/medina-elizalde2010/medina-elizalde2010.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/medina-elizalde2010/medina-elizalde2010.xls</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>2019-04-29</DIF_Creation_Date>
  <Last_DIF_Revision_Date>2019-04-29</Last_DIF_Revision_Date>
</DIF>
