<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-9639</Entry_ID>
  <Entry_Title>Port Blair, Andaman Islands 1975-2006 Coral Stable Isotope Data </Entry_Title>
  <Data_Set_Citation>
    <Dataset_Creator>Rixen, T.; Ramachandran, P.; Lehnhoff, L.; Dasbach, D.; Gaye, B.; Urban, B.; Ramachandran, R.; Ittekkot, V.</Dataset_Creator>
    <Dataset_Title>Port Blair, Andaman Islands 1975-2006 Coral Stable Isotope Data </Dataset_Title>
    <Dataset_Release_Date>2010-10-18</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/9639</Online_Resource>
  </Data_Set_Citation>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>T.</First_Name>
    <Last_Name>Rixen</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>P.</First_Name>
    <Last_Name>Ramachandran</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>L.</First_Name>
    <Last_Name>Lehnhoff</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>D.</First_Name>
    <Last_Name>Dasbach</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>B.</First_Name>
    <Last_Name>Gaye</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>B.</First_Name>
    <Last_Name>Urban</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>R.</First_Name>
    <Last_Name>Ramachandran</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>V.</First_Name>
    <Last_Name>Ittekkot</Last_Name>
  </Personnel>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>corals and sclerosponges</Term>
    <Detailed_Variable>delta 13C,Porites lutea,null,per mil PDB,null,corals and sclerosponges,raw,isotope ratio mass spectrometry,N,null</Detailed_Variable>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>corals and sclerosponges</Term>
    <Detailed_Variable>delta 18O,Porites lutea,null,per mil PDB,null,corals and sclerosponges,raw,isotope ratio mass spectrometry,N,null</Detailed_Variable>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>corals and sclerosponges</Term>
    <Detailed_Variable>age,null,null,year Common Era,null,corals and sclerosponges,null,null,N,null</Detailed_Variable>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>corals and sclerosponges</Term>
    <Detailed_Variable>depth,null,null,millimeter,null,corals and sclerosponges,null,null,N,null</Detailed_Variable>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>corals and sclerosponges</Term>
    <Variable_Level_1>oxygen isotopes</Variable_Level_1>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>corals and sclerosponges</Term>
    <Variable_Level_1>carbon isotopes</Variable_Level_1>
  </Parameters>
  <ISO_Topic_Category>geoscientificInformation</ISO_Topic_Category>
  <Keyword>Monsoon</Keyword>
  <Paleo_Temporal_Coverage>
    <Paleo_Start_Date>1975 AD</Paleo_Start_Date>
    <Paleo_Stop_Date>2006 AD</Paleo_Stop_Date>
  </Paleo_Temporal_Coverage>
  <Paleo_Temporal_Coverage>
    <Paleo_Start_Date>-25 cal yr BP</Paleo_Start_Date>
    <Paleo_Stop_Date>-56 cal yr BP</Paleo_Stop_Date>
  </Paleo_Temporal_Coverage>
  <Data_Set_Progress>Complete</Data_Set_Progress>
  <Spatial_Coverage>
    <Southernmost_Latitude>11.5048</Southernmost_Latitude>
    <Northernmost_Latitude>11.5048</Northernmost_Latitude>
    <Westernmost_Longitude>92.6931</Westernmost_Longitude>
    <Easternmost_Longitude>92.6931</Easternmost_Longitude>
    <Minimum_Altitude>-6</Minimum_Altitude>
    <Maximum_Altitude>-6</Maximum_Altitude>
  </Spatial_Coverage>
  <Location>
    <Location_Category>Ocean</Location_Category>
    <Location_Type>Indian Ocean</Location_Type>
    <Detailed_Location>Port Blair&gt;LATITUDE 11.5048&gt;LONGITUDE 92.6931</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>Rixen, T., P. Ramachandran, L. Lehnhoff, D. Dasbach, B. Gaye, 
B. Urban, R. Ramachandran, and V. Ittekkot.  2010. 
Impact of monsoon-driven surface ocean processes on a coral 
off Port Blair on the Andaman Islands and their link to 
North Atlantic climate variations.  
Global and Planetary Change. 
</Reference>
  <Summary>
    <Abstract>North Atlantic climate variations are reflected in sedimentary records 
from the northern Indian Ocean in which two basins, the Arabian Sea 
and the Bay of Bengal, are strongly affected by the monsoon. Contrary 
to the Bay of Bengal the Arabian Sea plays an important role in the 
global marine nitrogen cycle. In its mid-water oxygen minimum zone (OMZ) 
bioavailable fixed nitrogen is reduced to nitrogen gas (NO3- -&gt; N2), 
whereas oxygen concentrations are slightly above the threshold of 
nitrate reduction in the OMZ of the Bay of Bengal. A coral colony 
(Porites lutea) growing south of Port Blair on the Andaman Islands 
in the Bay of Bengal was studied for its response to changes in the
monsoon system and its link to temperature changes in the North Atlantic 
Ocean, between 1975 and 2006. Its linear extension rates, d13C and d18O 
values measured within the coral skeleton reveal a strong seasonality, 
which seems to be caused by the monsoon-driven reversal of the surface 
ocean circulation. The sampling site appears to be influenced by low 
salinity Bay of Bengal Water during the NE monsoon (boreal winter)
and by the high salinity Arabian Sea Water during the SW monsoon 
in summer. The high salinity Arabian Sea Water circulates along with 
the Summer Monsoon Current (S-MC) from the Arabia Sea into the Bay of 
Bengal. Decreasing d18O and reconstructed salinity values correlate to 
the increasing SSTs in the North Atlantic Ocean indicating a reduced
influence of the S-MC at the sampling site in the course of northern 
hemispheric warming. During such periods oxygen-depletion became 
stronger in the OMZ of the Arabian Sea as indicated by the sedimentary 
records. A reduced propagation of oxygen-depleted high salinity 
Arabian Sea Water into the Bay of Bengal could be a mechanism 
maintaining oxygen concentration above the threshold of nitrate 
reduction in the OMZ of the Bay of Bengal in times of global warming. 
 
          STUDY NOTES: Andaman Islands coral stable isotope data at monthly resolution.  
A Porites lutea colony from a reef south of Port Blair was sampled 
in March 2006, at a water depth of ~6 m. The core has a diameter 
of 6.4 cm and a length of ~37 cm.

The d18O and d13C values were calibrated relative to NBS19 
and are given in per mil deviation from the PDB.
</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/port-blair2010.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/coral/indian_ocean/port-blair2010.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>2018-12-11</DIF_Creation_Date>
  <Last_DIF_Revision_Date>2018-12-11</Last_DIF_Revision_Date>
</DIF>
