<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-11934</Entry_ID>
  <Entry_Title>Subtropical NW Atlantic ODP1058 Mid-Pleistocene G. ruber d18O Data</Entry_Title>
  <Data_Set_Citation>
    <Dataset_Creator>Weirauch, D.; Billups, K.; Martin, P.A.</Dataset_Creator>
    <Dataset_Title>Subtropical NW Atlantic ODP1058 Mid-Pleistocene G. ruber d18O Data</Dataset_Title>
    <Dataset_Release_Date>2011-09-12</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/11934</Online_Resource>
  </Data_Set_Citation>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>D.</First_Name>
    <Last_Name>Weirauch</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>K.</First_Name>
    <Last_Name>Billups</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>P.A.</First_Name>
    <Last_Name>Martin</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,Globigerinoides ruber white,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>oxygen isotopes</Variable_Level_1>
  </Parameters>
  <ISO_Topic_Category>geoscientificInformation</ISO_Topic_Category>
  <Paleo_Temporal_Coverage>
    <Paleo_Start_Date>1350400 cal yr BP</Paleo_Start_Date>
    <Paleo_Stop_Date>411000 cal yr BP</Paleo_Stop_Date>
  </Paleo_Temporal_Coverage>
  <Data_Set_Progress>Complete</Data_Set_Progress>
  <Spatial_Coverage>
    <Southernmost_Latitude>31.69</Southernmost_Latitude>
    <Northernmost_Latitude>31.69</Northernmost_Latitude>
    <Westernmost_Longitude>-75.43</Westernmost_Longitude>
    <Easternmost_Longitude>-75.43</Easternmost_Longitude>
    <Minimum_Altitude>-2996</Minimum_Altitude>
    <Maximum_Altitude>-2996</Maximum_Altitude>
  </Spatial_Coverage>
  <Location>
    <Location_Category>Ocean</Location_Category>
    <Location_Type>Atlantic Ocean</Location_Type>
    <Location_Subregion1>North Atlantic Ocean</Location_Subregion1>
    <Detailed_Location>ODP 1058&gt;LATITUDE 31.69&gt;LONGITUDE -75.43</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>Weirauch, D., K. Billups, and P. Martin. 2008. 
Evolution of millennial-scale climate variability during 
the mid-Pleistocene. 
Paleoceanography, 23, PA3216, doi:10.1029/2007PA001584. 
</Reference>
  <Summary>
    <Abstract>We use the oxygen isotopic composition of planktonic foraminifera 
Globigerinoides ruber (white) from Ocean Drilling Program Site 1058 
in the subtropical northwestern Atlantic to construct a high-
resolution (~800 year) climate record spanning the mid-Pleistocene 
climate transition (~410 ka to 1350 ka). We investigate whether 
or not millennial-scale instabilities in the proxy record are 
associated with the extent of continental glaciation. G. ruber d18O 
values display high-frequency fluctuations throughout the record, 
but the amplitude about mean glacial and interglacial d18O values 
increases at marine isotope stage (MIS) 22 (880 ka) and is highest 
during MIS 12. These observations support that millennial-scale 
climate instabilities are associated with ice sheet size. 
Time series analysis illustrates that these variations have 
significant concentration of spectral power centered on periods 
of ~10-12 ka and ~5 ka. The timing of these fluctuations agrees 
well, or coincides with, the periodicities of the second and fourth 
harmonics, respectively, of precessional forcing at the equator.
An insolation-based origin of the millennial-scale instabilities 
would be independent of ice volume and explains the presence of 
these fluctuations before the mid-Pleistocene climate transition 
as well as during interglacial intervals (e.g., MIS 37 and 17). 
Because the amplitude of the millennial-scale variations increases 
during the mid-Pleistocene transition, feedback mechanisms 
associated with the growth of large, 100-ka-paced, polar ice sheets 
may be important amplifiers of regional surface water hydrographic 
changes.
 
          STUDY NOTES: The data set summarizes Globigerinoides ruber d18O data from 
Site 1058 spanning Marine Isotope Stages 12-42 (410-1350 Ka). 
Note that G. ruber between 56.30 and 85.13 mcd were published 
by Billups et al. 2006.  
</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/weirauch2008/weirauch2008.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/weirauch2008/weirauch2008.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>2019-05-06</DIF_Creation_Date>
  <Last_DIF_Revision_Date>2019-05-06</Last_DIF_Revision_Date>
</DIF>
