<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-13286</Entry_ID>
  <Entry_Title>Bohai Sea 135KYr Relative Sea Level Reconstruction </Entry_Title>
  <Data_Set_Citation>
    <Dataset_Creator>Yi, L.; Yu, H.; Ortiz, J.D. ; Xu, X.; Qiang, X.K.; Huang, H.; Shi, X.; Deng, C.</Dataset_Creator>
    <Dataset_Title>Bohai Sea 135KYr Relative Sea Level Reconstruction </Dataset_Title>
    <Dataset_Release_Date>2012-09-20</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/13286</Online_Resource>
  </Data_Set_Citation>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>L.</First_Name>
    <Last_Name>Yi</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>H.</First_Name>
    <Last_Name>Yu</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>J.D. </First_Name>
    <Last_Name>Ortiz</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>X.</First_Name>
    <Last_Name>Xu</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>X.K.</First_Name>
    <Last_Name>Qiang</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>H.</First_Name>
    <Last_Name>Huang</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>X.</First_Name>
    <Last_Name>Shi</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>C.</First_Name>
    <Last_Name>Deng</Last_Name>
  </Personnel>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>paleocean</Term>
    <Variable_Level_1>physical properties</Variable_Level_1>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>paleocean</Term>
    <Variable_Level_1>reconstruction</Variable_Level_1>
  </Parameters>
  <ISO_Topic_Category>geoscientificInformation</ISO_Topic_Category>
  <Keyword>Sea Level Reconstruction</Keyword>
  <Keyword>sea level</Keyword>
  <Paleo_Temporal_Coverage>
    <Paleo_Start_Date>135600 cal yr BP</Paleo_Start_Date>
    <Paleo_Stop_Date>1900 cal yr BP</Paleo_Stop_Date>
  </Paleo_Temporal_Coverage>
  <Data_Set_Progress>Complete</Data_Set_Progress>
  <Spatial_Coverage>
    <Southernmost_Latitude>37.15</Southernmost_Latitude>
    <Northernmost_Latitude>37.15</Northernmost_Latitude>
    <Westernmost_Longitude>118.9667</Westernmost_Longitude>
    <Easternmost_Longitude>118.9667</Easternmost_Longitude>
    <Minimum_Altitude>6</Minimum_Altitude>
    <Maximum_Altitude>6</Maximum_Altitude>
  </Spatial_Coverage>
  <Location>
    <Location_Category>Continent</Location_Category>
    <Location_Type>Asia</Location_Type>
    <Location_Subregion1>Eastern Asia</Location_Subregion1>
    <Location_Subregion2>China</Location_Subregion2>
    <Detailed_Location>LZ908&gt;LATITUDE 37.15&gt;LONGITUDE 118.9667</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>Yi, L., H. Yu, J.D. Ortiz, X. Xu, X. Qiang, H. Huang, X. Shi, and C. Deng</Author>
    <Publication_Date>2012</Publication_Date>
    <Title>A reconstruction of late Pleistocene relative sea level in the  south Bohai Sea, China, based on sediment grain-size analysis</Title>
    <Series>Sedimentary Geology</Series>
    <Volume>281</Volume>
    <Pages>88-100</Pages>
    <DOI>10.1016/j.sedgeo.2012.08.007</DOI>
  </Reference>
  <Summary>
    <Abstract>Future anthropogenic sea-level rise and its impact on coastal regions 
is an important issue facing human civilizations. Due to the short 
nature of the instrumental record of sea-level change, development 
of proxies for sea-level change prior to the advent of instrumental 
records is essential to reconstruct long-term background sea-level 
changes on local, regional and global scales. Here, we employ numerical 
methods to partition sediment grain size using a combined database 
of marine surface and core samples, and to quantitatively reconstruct 
sea-level variation since the late Pleistocene in the south Bohai Sea, 
China. Our sea-level reconstruction indicates that relative sea-level 
changes in the southern Bohai Sea track global sea-level variation 
for the duration of the record. The results also indicate substantial 
regression from 70 to 30 cal kyr BP, and potentially subarial exposure 
from 38 to 20 cal kyr BP. Our results document the feasibility of 
reconstructing relative sea-level change by numerical partitioning 
of sediment grain size data, demonstrating the potential for future 
applications.  
          STUDY NOTES: Relative sea level (RSL) reconstruction for the south Bohai Sea, 
China over the last 135Kyr, based on sediment grain size data 
from coastal core LZ908 and Bohai Sea surface sediment samples.

Core LZ908: 37°09&apos;N, 118°58&apos;E, 6 m a.s.l.</Abstract>
  </Summary>
  <Related_URL>
    <URL_Content_Type>
      <Type>GET DATA</Type>
    </URL_Content_Type>
    <URL>https://www1.ncdc.noaa.gov/pub/data/paleo/paleocean/relative_sea_level/bohai2012rsl.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/paleocean/relative_sea_level/bohai2012rsl.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>2019-04-25</DIF_Creation_Date>
  <Last_DIF_Revision_Date>2019-04-25</Last_DIF_Revision_Date>
</DIF>
