<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-25630</Entry_ID>
  <Entry_Title>Deep-sea oxygen depletion and ocean carbon sequestration during the last ice age</Entry_Title>
  <Data_Set_Citation>
    <Dataset_Creator>Anderson, R.F.; Sachs, J.P.; Fleisher, M.Q.; Allen, K.A.; Yu, J.; Koutavas, A.; Jaccard, S.L.</Dataset_Creator>
    <Dataset_Title>Deep-sea oxygen depletion and ocean carbon sequestration during the last ice age</Dataset_Title>
    <Dataset_Release_Date>2018-11-23</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/25630</Online_Resource>
  </Data_Set_Citation>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>R.F.</First_Name>
    <Last_Name>Anderson</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>J.P.</First_Name>
    <Last_Name>Sachs</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>M.Q.</First_Name>
    <Last_Name>Fleisher</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>K.A.</First_Name>
    <Last_Name>Allen</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>J.</First_Name>
    <Last_Name>Yu</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>A.</First_Name>
    <Last_Name>Koutavas</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>S.L.</First_Name>
    <Last_Name>Jaccard</Last_Name>
  </Personnel>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>paleocean</Term>
    <Variable_Level_1>biomarkers</Variable_Level_1>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>paleocean</Term>
    <Variable_Level_1>radiogenic isotope</Variable_Level_1>
  </Parameters>
  <ISO_Topic_Category>geoscientificInformation</ISO_Topic_Category>
  <Paleo_Temporal_Coverage>
    <Paleo_Start_Date>40000 cal yr BP</Paleo_Start_Date>
    <Paleo_Stop_Date>0 cal yr BP</Paleo_Stop_Date>
  </Paleo_Temporal_Coverage>
  <Data_Set_Progress>Complete</Data_Set_Progress>
  <Spatial_Coverage>
    <Southernmost_Latitude>-3.383</Southernmost_Latitude>
    <Northernmost_Latitude>.11</Northernmost_Latitude>
    <Westernmost_Longitude>-139.7157</Westernmost_Longitude>
    <Easternmost_Longitude>-82.0667</Easternmost_Longitude>
    <Minimum_Altitude>-4354</Minimum_Altitude>
    <Maximum_Altitude>-617</Maximum_Altitude>
  </Spatial_Coverage>
  <Location>
    <Location_Category>Ocean</Location_Category>
    <Location_Type>Pacific Ocean</Location_Type>
    <Location_Subregion1>South Pacific Ocean</Location_Subregion1>
    <Detailed_Location>RC11-238&gt;LATITUDE -1.52&gt;LONGITUDE -85.82</Detailed_Location>
  </Location>
  <Location>
    <Location_Category>Ocean</Location_Category>
    <Location_Type>Pacific Ocean</Location_Type>
    <Location_Subregion1>Eastern Pacific Ocean</Location_Subregion1>
    <Detailed_Location>VM19-27&gt;LATITUDE -.4667&gt;LONGITUDE -82.0667</Detailed_Location>
  </Location>
  <Location>
    <Location_Category>Ocean</Location_Category>
    <Location_Type>Pacific Ocean</Location_Type>
    <Location_Subregion1>Central Pacific Ocean</Location_Subregion1>
    <Detailed_Location>TT013-18PC&gt;LATITUDE -1.84&gt;LONGITUDE -139.71</Detailed_Location>
  </Location>
  <Location>
    <Location_Category>Ocean</Location_Category>
    <Location_Type>Pacific Ocean</Location_Type>
    <Location_Subregion1>Eastern Pacific Ocean</Location_Subregion1>
    <Detailed_Location>VM21-30&gt;LATITUDE -1.2167&gt;LONGITUDE -89.6833</Detailed_Location>
  </Location>
  <Location>
    <Location_Category>Ocean</Location_Category>
    <Location_Type>Pacific Ocean</Location_Type>
    <Location_Subregion1>Eastern Pacific Ocean</Location_Subregion1>
    <Detailed_Location>VM19-30&gt;LATITUDE -3.383&gt;LONGITUDE -83.517</Detailed_Location>
  </Location>
  <Location>
    <Location_Category>Ocean</Location_Category>
    <Location_Type>Pacific Ocean</Location_Type>
    <Location_Subregion1>Eastern Pacific Ocean</Location_Subregion1>
    <Detailed_Location>TT013-MC19&gt;LATITUDE -1.868&gt;LONGITUDE -139.7157</Detailed_Location>
  </Location>
  <Location>
    <Location_Category>Ocean</Location_Category>
    <Location_Type>Pacific Ocean</Location_Type>
    <Location_Subregion1>Eastern Pacific Ocean</Location_Subregion1>
    <Detailed_Location>VM19-28&gt;LATITUDE -2.3667&gt;LONGITUDE -84.65</Detailed_Location>
  </Location>
  <Location>
    <Location_Category>Ocean</Location_Category>
    <Location_Type>Pacific Ocean</Location_Type>
    <Location_Subregion1>Central Pacific Ocean</Location_Subregion1>
    <Detailed_Location>TT013-72PC&gt;LATITUDE .11&gt;LONGITUDE -139.4</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>Anderson R.F., J.P. Sachs, M.Q. Fleisher, K.A. Allen, J. Yu, A. Koutavas, S.L. Jaccard</Author>
    <Publication_Date>2018</Publication_Date>
    <Title>Deep-sea oxygen depletion and ocean carbon sequestration during the last ice age</Title>
    <Series>Global Biogeochemical Cycles</Series>
    <Volume>under review</Volume>
  </Reference>
  <Reference>
    <Author>Anderson, R.F., M.Q. Fleisher, and Y. Lao</Author>
    <Publication_Date>2006</Publication_Date>
    <Title>Glacial-Interglacial variability in the delivery of dust to the central equatorial Pacific Ocean</Title>
    <Series>Earth and Planetary Science Letters</Series>
    <Volume>242</Volume>
    <Pages>406-414</Pages>
    <DOI>10.1016/j.epsl.2005.11.061</DOI>
  </Reference>
  <Reference>
    <Author>Anderson, R.F., M.Q. Fleisher, Y. Lao, and G. Winckler</Author>
    <Publication_Date>2008</Publication_Date>
    <Title>Modern CaCO3 preservation in equatorial Pacific sediments in the context of recent glacial cycles</Title>
    <Series>Marine Chemistry</Series>
    <Volume>111</Volume>
    <Pages>30-46</Pages>
    <DOI>10.1016/j.marchem.2007.11.011</DOI>
  </Reference>
  <Reference>
    <Author>Bradtmiller, L.I., R.F. Anderson, M.Q. Fleisher, and L.H. Burckle</Author>
    <Publication_Date>2007</Publication_Date>
    <Title>Opal burial in the equatorial Atlantic Ocean over the last 30 ka: Implications for glacial-interglacial changes in the ocean silicon cycle</Title>
    <Series>Paleoceanography</Series>
    <DOI>10.1029/2006PA001282</DOI>
  </Reference>
  <Reference>
    <Author>Hayes, C.T., R.F. Anderson, and M.Q. Fleisher</Author>
    <Publication_Date>2011</Publication_Date>
    <Title>Opal accumulation rates in the equatorial Pacific  and mechanisms of deglaciation</Title>
    <Series>Paleoceanography</Series>
    <DOI>10.1029/2010PA002008 </DOI>
  </Reference>
  <Reference>
    <Author>Koutavas, A., and J.P. Sachs</Author>
    <Publication_Date>2008</Publication_Date>
    <Title>Northern timing of deglaciation in the eastern equatorial Pacific from alkenone paleothermometry</Title>
    <Series>Paleoceanography</Series>
    <Volume>23</Volume>
    <Report_Number>PA4205</Report_Number>
    <DOI>10.1029/2008PA001593</DOI>
  </Reference>
  <Reference>Koutavas, A. and J. Lynch-Stieglitz. 2003. Glacial-interglacial dynamics of the eastern equatorial Pacific cold tongue-Intertropical Convergence Zone system reconstructed from oxygen isotope records. Paleoceanography 18(4), 1089.</Reference>
  <Reference>
    <Author>Lyle, M., A.C. Mix, and N.G. Pisias</Author>
    <Publication_Date>2002</Publication_Date>
    <Title>Patterns of CaCO3 deposition in the eastern tropical Pacific Ocean for the last 150 kyr: Evidence for a southeast Pacific depositional spike during marine isotope stage (MIS) 2</Title>
    <Series>Paleoceanography</Series>
    <Volume>17</Volume>
    <DOI>10.1029/2000PA000538</DOI>
  </Reference>
  <Reference>
    <Author>Martinson, D.G., N.G. Pisias, J.D. Hays, J. Imbrie, T.C. Moore, and N.J. Shackleton</Author>
    <Publication_Date>1987</Publication_Date>
    <Title>Age dating and the orbital theory of the ice ages - Development of a high-resolution 0 to 300,000-year chronostratigraphy</Title>
    <Series>Quaternary Research</Series>
    <Volume>27</Volume>
    <Pages>1-29</Pages>
    <DOI>10.1016/0033-5894(87)90046-9</DOI>
  </Reference>
  <Reference>
    <Author>Murray, R.W., C. Knowlton, M. Leinen, A.C. Mix, and C.H. Polsky</Author>
    <Publication_Date>2000</Publication_Date>
    <Title>Export production and carbonate dissolution in the central equatorial Pacific Ocean over the past 1 Ma</Title>
    <Series>Paleoceanography</Series>
    <DOI>10.1029/1999PA000457</DOI>
  </Reference>
  <Reference>
    <Author>Shackleton, N.J., M.A. Hall, J. Line, and C. Shuxi</Author>
    <Publication_Date>1983</Publication_Date>
    <Title>Carbon isotope data In core V19-30 confirm reduced carbon-dioxide concentration In the ice-age atmosphere</Title>
    <Series>Nature</Series>
    <Volume>306</Volume>
    <Pages>319-322</Pages>
    <DOI>10.1038/306319a0</DOI>
  </Reference>
  <Reference>
    <Author>Winckler, G., R.F. Anderson, S.L. Jaccard, and F. Marcantonio</Author>
    <Publication_Date>2016</Publication_Date>
    <Title>Ocean dynamics, not dust, have controlled equatorial Pacific productivity over the past 500,000 years</Title>
    <Series>Proceedings of the National Academy of Sciences</Series>
    <Volume>113</Volume>
    <Issue>22</Issue>
    <Pages>6119-6124</Pages>
    <DOI>10.1073/pnas.1600616113</DOI>
  </Reference>
  <Summary>
    <Abstract>A possible imprint on equatorial Pacific sediments of a deglacial 
reinvigoration of the Southern Ocean overturning is increased 
opal accumulation rate. This would arise from the transmission 
of silica-rich deep water to the equatorial thermocline via 
Subantarctic Mode Water and an associated increase in diatom 
productivity. In search of this imprint, sediment cores from 
the central (TT013-PC72) and eastern (V19-30) equatorial Pacific 
have been analyzed for 230Th-normalized opal accumulation rates 
over the past five and three glacial terminations, respectively. 
Equatorial opal accumulation rates sustained relatively low values 
over much of the records and were punctuated by large increases 
centered on some terminations, but not all.  Furthermore, two 
periods of increased opal flux were observed that do not coincide 
with terminations.  Sources other than the Southern Ocean may need 
to be considered in the silica budget of the equatorial Pacific, 
but the d13C of Neogloboquadrina dutertrei can be used to support 
the presence of a deepwater nutrient signal in each case. 
Although a common deglacial mechanism, or a common imprint thereof, 
for each of the late Pleistocene glaciations remains elusive, 
the combination of opal flux and d13C of N. dutertrei provides 
a diagnostic for past injection of deepwater nutrients into 
the Equatorial Undercurrent. 
          STUDY NOTES: Combination of data from previous publications and new data
      Provided Keywords: Pacific Ocean, deglacial, last ice age</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/anderson2019/anderson2018-vm19-30.txt</URL>
    <Description>NOAA Template File; VM19-30 Biomarker and Radiogenic Isotope Data</Description>
  </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/anderson2019/anderson2018-vm21-30.txt</URL>
    <Description>NOAA Template File; VM21-30 Biomarker and Radiogenic Isotope Data</Description>
  </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/anderson2019/anderson2018-pc72.txt</URL>
    <Description>NOAA Template File; TT013-PC72 Biomarker and Radiogenic Isotope Data</Description>
  </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/anderson2019/anderson2018-mc19.txt</URL>
    <Description>NOAA Template File; TT013-MC19 Biomarker and Radiogenic Isotope Data</Description>
  </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/anderson2019/anderson2018-rc11-238.txt</URL>
    <Description>NOAA Template File; RC11-238 Biomarker and Radiogenic Isotope Data</Description>
  </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/anderson2019/anderson2018-vm19-28.txt</URL>
    <Description>NOAA Template File; VM19-28 Biomarker and Radiogenic Isotope Data</Description>
  </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/anderson2019/anderson2018-pc18.txt</URL>
    <Description>NOAA Template File; TT013-PC18 Biomarker and Radiogenic Isotope Data</Description>
  </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/anderson2019/anderson2018-vm19-27.txt</URL>
    <Description>NOAA Template File; VM19-27 Biomarker and Radiogenic Isotope 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>2019-07-03</DIF_Creation_Date>
  <Last_DIF_Revision_Date>2019-07-03</Last_DIF_Revision_Date>
</DIF>
