<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-10513</Entry_ID>
  <Entry_Title>Atlantic Coretop Foraminiferal Mg/Ca and d18O Calibration Data </Entry_Title>
  <Data_Set_Citation>
    <Dataset_Creator>Arbuszewski, J.A.; deMenocal, P.B.; Kaplan, A.; Farmer, E.C.</Dataset_Creator>
    <Dataset_Title>Atlantic Coretop Foraminiferal Mg/Ca and d18O Calibration Data </Dataset_Title>
    <Dataset_Release_Date>2011-01-26</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/10513</Online_Resource>
  </Data_Set_Citation>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>J.A.</First_Name>
    <Last_Name>Arbuszewski</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>P.B.</First_Name>
    <Last_Name>deMenocal</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>A.</First_Name>
    <Last_Name>Kaplan</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>E.C.</First_Name>
    <Last_Name>Farmer</Last_Name>
  </Personnel>
  <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>
  <ISO_Topic_Category>geoscientificInformation</ISO_Topic_Category>
  <Paleo_Temporal_Coverage>
    <Paleo_Start_Date>10 cal yr BP</Paleo_Start_Date>
    <Paleo_Stop_Date>-10 cal yr BP</Paleo_Stop_Date>
  </Paleo_Temporal_Coverage>
  <Data_Set_Progress>Complete</Data_Set_Progress>
  <Spatial_Coverage>
    <Southernmost_Latitude>42.85</Southernmost_Latitude>
    <Northernmost_Latitude>42.85</Northernmost_Latitude>
    <Westernmost_Longitude>-25.15</Westernmost_Longitude>
    <Easternmost_Longitude>-25.15</Easternmost_Longitude>
    <Minimum_Altitude>-3448</Minimum_Altitude>
    <Maximum_Altitude>-3448</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>VM29-178&gt;LATITUDE 42.85&gt;LONGITUDE -25.15</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>Arbuszewski, J., P. deMenocal, A. Kaplan, and E.C. Farmer. 2010. 
On the fidelity of shell-derived d18Oseawater estimates. 
Earth and Planetary Science Letters, Vol. 300, Issues 3-4, 
pp. 185-196, 1 December 2010. 
doi:10.1016/j.epsl.2010.10.035 
</Reference>
  <Summary>
    <Abstract>Paired foraminiferal Magnesium/Calcium ratio and oxygen isotope 
analyses are widely used to estimate surface ocean d18Oseawater, 
a robust proxy for surface salinity.  We assess the fidelity of 
shell-derived d18Oseawater estimates for the surface-dwelling 
foraminifer Globigerinoides ruber (white) using an Atlantic 
meridional coretop transect spanning basin-scale temperature 
and salinity gradients. Shell-derived and observed d18Oseawater 
values are well correlated (r2=0.77), but a large systematic bias 
is observed. Shell Mg/Ca ratios are significantly elevated above 
values expected from observed and isotopic calcification 
temperatures in the saline subtropical gyres of both hemispheres. 
This temperature-independent shell Mg/Ca ratio variability, 
termed &quot;excess Mg/Ca&quot;, is highly correlated with surface salinity 
(r2=0.77), and the observed salinity dependence (27±4%) is much 
higher than indicated by culture studies (6±2%). Our coretop data 
are used to develop new Atlantic Basin temperature and salinity 
calibration equations that are accurate (±1.1°C and ±0.20, 
respectively), precise (r2=0.82 and 0.81, respectively), 
and verifiable using previously published data. These results 
are valid for the relatively high salinities of the subtropical 
Atlantic (35.5-37.3). We discover that inclusion of other published 
data from lower salinity regions (&lt; 35) indicates little or no 
excess Mg/Ca. Taken together, these results point to a strongly 
non-linear, positive salinity effect on shell Mg/Ca ratios that 
significantly affects the accuracy of SST and d18Oseawater 
estimates in high salinity settings (&gt;35). 
 
          STUDY NOTES: Coretop foraminiferal magnesium/calcium ratio and oxygen isotope 
data from a meridional transect of 64 Atlantic samples.  Mg/Ca 
ratio and d18O measured on Globigerinoides ruber (white) are used 
to evaluate shell-derived d18Oseawater estimates across different 
salinity regimes in the Atlantic Ocean.  

</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/arbuszewski2010/arbuszewski2010.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/arbuszewski2010/arbuszewski2010.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>2018-12-11</DIF_Creation_Date>
  <Last_DIF_Revision_Date>2018-12-11</Last_DIF_Revision_Date>
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