<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-22643</Entry_ID>
  <Entry_Title>Seychelles Fossil Coral Data from the Last Interglacial</Entry_Title>
  <Data_Set_Citation>
    <Dataset_Creator>Dutton, A.L.; Webster, J.M.; Zwartz, D.; Lambeck, K.; Wohlfarth, B.</Dataset_Creator>
    <Dataset_Title>Seychelles Fossil Coral Data from the Last Interglacial</Dataset_Title>
    <Dataset_Release_Date>2017-09-07</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/22643</Online_Resource>
  </Data_Set_Citation>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>A.L.</First_Name>
    <Last_Name>Dutton</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>J.M.</First_Name>
    <Last_Name>Webster</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>D.</First_Name>
    <Last_Name>Zwartz</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>K.</First_Name>
    <Last_Name>Lambeck</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>B.</First_Name>
    <Last_Name>Wohlfarth</Last_Name>
  </Personnel>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>corals and sclerosponges</Term>
    <Detailed_Variable>notes,null,null,null,null,corals and sclerosponges,null,null,C,taxonomic identification; coral genus species</Detailed_Variable>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>corals and sclerosponges</Term>
    <Detailed_Variable>age,null,null,calendar kiloyear before present,null,corals and sclerosponges,null,null,N,U-Th geochronology</Detailed_Variable>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>corals and sclerosponges</Term>
    <Detailed_Variable>collection elevation,null,null,meter,null,corals and sclerosponges,raw,null,N,elevation measured with respect to mean low water springs</Detailed_Variable>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>corals and sclerosponges</Term>
    <Detailed_Variable>age,null,two standard deviations,calendar kiloyear before present,null,corals and sclerosponges,null,null,N,U-Th geochronology</Detailed_Variable>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>corals and sclerosponges</Term>
    <Detailed_Variable>sample identification,null,null,null,null,corals and sclerosponges,null,null,C,lab sample identification; asterisks represent previously published ages that have been recalculated here using different decay constants for 230Th and 234U</Detailed_Variable>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>corals and sclerosponges</Term>
    <Detailed_Variable>age,null,null,calendar kiloyear before present,null,corals and sclerosponges,averaged,null,N,U-Th geochronology; average ages for a coral are inverse variance-weighted means of data passing the screening criteria</Detailed_Variable>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>corals and sclerosponges</Term>
    <Detailed_Variable>notes,null,null,null,null,corals and sclerosponges,null,null,C,outcrop number</Detailed_Variable>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>corals and sclerosponges</Term>
    <Detailed_Variable>calcite,null,null,weight percent,null,corals and sclerosponges,raw,x-ray diffraction,N,null</Detailed_Variable>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>corals and sclerosponges</Term>
    <Detailed_Variable>notes,null,null,null,null,corals and sclerosponges,null,null,C,growth form of coral</Detailed_Variable>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>corals and sclerosponges</Term>
    <Detailed_Variable>International Geo Sample Number,null,null,null,null,corals and sclerosponges,null,null,C,registered at SESAR</Detailed_Variable>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>corals and sclerosponges</Term>
    <Detailed_Variable>age,null,two standard deviations,calendar kiloyear before present,null,corals and sclerosponges,averaged,null,N,U-Th geochronology; average ages for a coral are inverse variance-weighted means of data passing the screening criteria</Detailed_Variable>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>corals and sclerosponges</Term>
    <Variable_Level_1>physical properties</Variable_Level_1>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>corals and sclerosponges</Term>
    <Variable_Level_1>chemistry</Variable_Level_1>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>corals and sclerosponges</Term>
    <Variable_Level_1>age control</Variable_Level_1>
  </Parameters>
  <ISO_Topic_Category>geoscientificInformation</ISO_Topic_Category>
  <Keyword>Sea Level Reconstruction</Keyword>
  <Paleo_Temporal_Coverage>
    <Paleo_Start_Date>129000 cal yr BP</Paleo_Start_Date>
    <Paleo_Stop_Date>123000 cal yr BP</Paleo_Stop_Date>
  </Paleo_Temporal_Coverage>
  <Data_Set_Progress>Complete</Data_Set_Progress>
  <Spatial_Coverage>
    <Southernmost_Latitude>-4.38</Southernmost_Latitude>
    <Northernmost_Latitude>-4.28</Northernmost_Latitude>
    <Westernmost_Longitude>55.73</Westernmost_Longitude>
    <Easternmost_Longitude>55.84</Easternmost_Longitude>
  </Spatial_Coverage>
  <Location>
    <Location_Category>Ocean</Location_Category>
    <Location_Type>Indian Ocean</Location_Type>
    <Location_Subregion1>Seychelles</Location_Subregion1>
    <Detailed_Location>La Digue and Curieuse Islands&gt;LATITUDE &gt;LONGITUDE </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>Dutton, Andrea, Jody M. Webster, Dan Zwartz, Kurt Lambeck, and Barbara Wohlfarth</Author>
    <Publication_Date>2015</Publication_Date>
    <Title>Tropical tales of polar ice: evidence of Last Interglacial polar ice sheet retreat recorded by fossil reefs of the granitic Seychelles islands</Title>
    <Series>Quaternary Science Reviews</Series>
    <Volume>107</Volume>
    <Pages>182-196</Pages>
    <DOI>10.1016/j.quascirev.2014.10.025</DOI>
    <Online_Resource>http://www.sciencedirect.com/science/article/pii/S0277379114004120</Online_Resource>
  </Reference>
  <Summary>
    <Abstract>In the search for a record of eustatic sea level change on glacial–interglacial timescales, the Seychelles ranks as one of the best places on the planet to study. Owing to its location with respect to the former margins of Northern Hemisphere ice sheets that wax and wane on orbital cycles, the local—or relative—sea level history is predicted to lie within a few meters of the globally averaged eustatic signal during the Last Interglacial period. We have surveyed and dated Last Interglacial fossil corals to ascertain peak sea level and hence infer maximum retreat of polar ice sheets during this time interval. We observe a pattern of gradually rising sea level in the Seychelles between ~129 and 125 thousand years ago (ka), with peak eustatic sea level attained after 125 ka at 7.6 ± 1.7 m higher than present. After accounting for thermal expansion and loss of mountain glaciers, this sea-level budget would require ~5–8 m of polar ice sheet contribution, relative to today&apos;s volume, of which only ~2 m came from the Greenland ice sheet. This result clearly identifies the Antarctic ice sheet as a significant source of melt water, most likely derived from one of the unstable, marine-based sectors in the West and/or East Antarctic ice sheet. Furthermore, the establishment of a +5.9 ± 1.7 m eustatic sea level position by 128.6 ± 0.8 ka would require that partial AIS collapse was coincident with the onset of the sea level highstand. 
          STUDY NOTES: Samples collected ~3.5 - 8 meters above mean low water. Site elevations have a measurement precision of 0.2 m.
      Provided Keywords: sea level, U-Th, MIS 5e, coral, Seychelles</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/dutton2015/dutton2015-seychelles.txt</URL>
    <Description>NOAA Template File; Fossil Coral Data</Description>
  </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>
