<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-13134</Entry_ID>
  <Entry_Title>Southeast Atlantic ODP1262 Upper Paleocene/Lower Eocene Isotope Data</Entry_Title>
  <Data_Set_Citation>
    <Dataset_Creator>Zachos, J.C.; McCarren, H.; Murphy, B.; Röhl, U.; Westerhold, T.</Dataset_Creator>
    <Dataset_Title>Southeast Atlantic ODP1262 Upper Paleocene/Lower Eocene Isotope Data</Dataset_Title>
    <Dataset_Release_Date>2012-07-10</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/13134</Online_Resource>
  </Data_Set_Citation>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>J.C.</First_Name>
    <Last_Name>Zachos</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>H.</First_Name>
    <Last_Name>McCarren</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>B.</First_Name>
    <Last_Name>Murphy</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>U.</First_Name>
    <Last_Name>Röhl</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>T.</First_Name>
    <Last_Name>Westerhold</Last_Name>
  </Personnel>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>paleoceanography</Term>
    <Detailed_Variable>depth,null,null,meter,null,paleoceanography,composited,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>delta 18O,carbonate,null,per mil,null,paleoceanography,null,null,N,bulk sediment</Detailed_Variable>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>paleoceanography</Term>
    <Detailed_Variable>delta 13C,carbonate,null,per mil,null,paleoceanography,null,null,N,bulk sediment</Detailed_Variable>
  </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>carbon isotopes</Variable_Level_1>
  </Parameters>
  <ISO_Topic_Category>geoscientificInformation</ISO_Topic_Category>
  <Keyword>carbon cycle</Keyword>
  <Paleo_Temporal_Coverage>
    <Paleo_Start_Date>56600000 cal yr BP</Paleo_Start_Date>
    <Paleo_Stop_Date>52100000 cal yr BP</Paleo_Stop_Date>
  </Paleo_Temporal_Coverage>
  <Data_Set_Progress>Complete</Data_Set_Progress>
  <Spatial_Coverage>
    <Southernmost_Latitude>-27.186</Southernmost_Latitude>
    <Northernmost_Latitude>-27.186</Northernmost_Latitude>
    <Westernmost_Longitude>1.577</Westernmost_Longitude>
    <Easternmost_Longitude>1.577</Easternmost_Longitude>
    <Minimum_Altitude>-4755</Minimum_Altitude>
    <Maximum_Altitude>-4755</Maximum_Altitude>
  </Spatial_Coverage>
  <Location>
    <Location_Category>Ocean</Location_Category>
    <Location_Type>Atlantic Ocean</Location_Type>
    <Location_Subregion1>South Atlantic Ocean</Location_Subregion1>
    <Detailed_Location>ODP 1262&gt;LATITUDE -27.186&gt;LONGITUDE 1.577</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>Zachos, J.C., H. McCarren, B. Murphy, U. Röhl, and T. Westerhold. 2010. 
Tempo and Scale of Late Paleocene and Early Eocene Carbon Isotope 
Cycles: Implications for the Origin of Hyperthermals. 
Earth Planet. Sci. Lett., Vol. 299, pp. 242-249. 
doi:10.1016/j.epsl.2010.09.004 </Reference>
  <Summary>
    <Abstract>The upper Paleocene and lower Eocene are marked by several prominent 
(&gt;1‰) carbon isotope (d13C) excursions (CIE) that coincide with 
transient global warmings, or thermal maxima, including the 
Paleocene-Eocene Thermal Maximum (PETM). The CIE, which are recorded 
mainly in marine sedimentary sequences, have also been identified 
in continental sequences, occurred episodically, and yet appear 
to be paced or triggered by orbital forcing. To constrain the timing 
and scale of the CIE relative to long-term baseline variability, 
we have constructed a 4.52 million year (myr) long, high-resolution 
(~3 kyr) bulk sediment carbon isotope record spanning the lower 
Eocene to upper Paleocene (C25r-C24n) from a pelagic sediment section 
recovered at ODP Site 1262 in the southeast Atlantic. This section, 
which was orbitally-tuned utilizing high-resolution core log physical 
property and geochemical records, is the most stratigraphically 
complete upper Paleocene to lower Eocene sequence recovered to date. 
Time-series analysis of the carbon isotope record along with a high-
resolution Fe intensity record obtained by XRF core scanner reveal 
cyclicity with variance concentrated primarily in the precession 
(21 kyr) and eccentricity bands (100 and 400-kyr) throughout the 
upper Paleocene-lower Eocene. In general, minima in d13C correspond 
with peaks in Fe (i.e., carbonate dissolution), both of which appear 
to be in phase with maxima in eccentricity. This covariance is 
consistent with excess oceanic uptake of isotopically depleted 
carbon resulting in lower carbonate saturation during periods 
of high eccentricity. This relationship includes all late Paleocene 
and early Eocene CIE confirming pacing by orbital forcing. The lone 
exception is the PETM, which appears to be out of phase with the 
400-kyr cycle, though possibly in phase with the 100-kyr cycle, 
reinforcing the notion that a mechanism other than orbital forcing 
and/or an additional source of carbon is required to account for 
the occurrence and unusual scale of this event. 
 
          STUDY NOTES: Bulk sediment carbon and oxygen isotope record for 
the composite sections from Ocean Drilling Program 
Holes 1262A, B, and C. 

ODP Site 1262: 27°11.160&apos;S, 1°34.620&apos;E, 4755m water depth 
</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/zachos2010/zachos2010.xls</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/zachos2010/zachos2010.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>2019-02-12</DIF_Creation_Date>
  <Last_DIF_Revision_Date>2019-02-12</Last_DIF_Revision_Date>
</DIF>
