<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-lake-12910</Entry_ID>
  <Entry_Title>Verlorenvlei, South Africa 1400 Year Diatom Abundance Data</Entry_Title>
  <Data_Set_Citation>
    <Dataset_Creator>Stager, J.C.; Mayewski, P.A.; White, J.; Chase, B.M.; Neumann, F.H.; Meadows, M.E.; King, C.D.; Dixon, D.A.</Dataset_Creator>
    <Dataset_Title>Verlorenvlei, South Africa 1400 Year Diatom Abundance Data</Dataset_Title>
    <Dataset_Release_Date>2012-05-15</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/12910</Online_Resource>
  </Data_Set_Citation>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>J.C.</First_Name>
    <Last_Name>Stager</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>P.A.</First_Name>
    <Last_Name>Mayewski</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>J.</First_Name>
    <Last_Name>White</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>B.M.</First_Name>
    <Last_Name>Chase</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>F.H.</First_Name>
    <Last_Name>Neumann</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>M.E.</First_Name>
    <Last_Name>Meadows</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>C.D.</First_Name>
    <Last_Name>King</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>D.A.</First_Name>
    <Last_Name>Dixon</Last_Name>
  </Personnel>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>paleolimnology</Term>
    <Detailed_Variable>depth,null,null,centimeter,null,paleolimnology,null,null,N,null</Detailed_Variable>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>paleolimnology</Term>
    <Detailed_Variable>age,null,null,year Common Era,null,paleolimnology,null,null,N,null</Detailed_Variable>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>paleolimnology</Term>
    <Detailed_Variable>total epiphytic diatoms,null,null,percent,null,paleolimnology,null,null,N,null</Detailed_Variable>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>paleolimnology</Term>
    <Detailed_Variable>diatom tolerance-based index,null,null,percent,null,paleolimnology,null,null,N,diluted water taxa</Detailed_Variable>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>paleolimnology</Term>
    <Detailed_Variable>diatom tolerance-based index,null,null,percent,null,paleolimnology,null,null,N,brackish water taxa</Detailed_Variable>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>paleolimnology</Term>
    <Detailed_Variable>age,null,null,calendar year before present,null,paleolimnology,null,null,N,null</Detailed_Variable>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>paleolimnology</Term>
    <Variable_Level_1>population abundance</Variable_Level_1>
  </Parameters>
  <ISO_Topic_Category>geoscientificInformation</ISO_Topic_Category>
  <Keyword>westerlies</Keyword>
  <Paleo_Temporal_Coverage>
    <Paleo_Start_Date>1400 cal yr BP</Paleo_Start_Date>
    <Paleo_Stop_Date>-59 cal yr BP</Paleo_Stop_Date>
  </Paleo_Temporal_Coverage>
  <Data_Set_Progress>Complete</Data_Set_Progress>
  <Spatial_Coverage>
    <Southernmost_Latitude>-32.36</Southernmost_Latitude>
    <Northernmost_Latitude>-32.36</Northernmost_Latitude>
    <Westernmost_Longitude>18.44</Westernmost_Longitude>
    <Easternmost_Longitude>18.44</Easternmost_Longitude>
    <Minimum_Altitude>1</Minimum_Altitude>
    <Maximum_Altitude>1</Maximum_Altitude>
  </Spatial_Coverage>
  <Location>
    <Location_Category>Continent</Location_Category>
    <Location_Type>Africa</Location_Type>
    <Location_Subregion1>Southern Africa</Location_Subregion1>
    <Location_Subregion2>South Africa</Location_Subregion2>
    <Detailed_Location>Verlorenvlei&gt;LATITUDE -32.36&gt;LONGITUDE 18.44</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>Stager, J.C., P.A. Mayewski, J. White, B.M. Chase, F.H. Neumann, 
M.E. Meadows, C.D. King, and D.A. Dixon. 2012. 
Precipitation variability in the winter rainfall zone of South 
Africa during the last 1400 yr linked to the austral westerlies. 
Climate of the Past, Vol. 8, pp. 877-887. 
www.clim-past.net/8/877/2012/
doi:10.5194/cp-8-877-2012 </Reference>
  <Summary>
    <Abstract>The austral westerlies strongly influence precipitation and ocean 
circulation in the southern temperate zone, with important 
consequences for cultures and ecosystems. Global climate models 
anticipate poleward retreat of the austral westerlies with future 
warming, but the available paleoclimate records that might test 
these models have been limited to South America and New Zealand, 
are not fully consistent with each other and may be complicated 
by influences from other climatic factors. Here we present the 
first high-resolution diatom and sedimentological records from 
the winter rainfall region of South Africa, representing 
precipitation in the equatorward margin of the westerly wind belt 
during the last 1400 yr. Inferred rainfall was relatively high 
~1400-1200 cal yr BP, decreased until ~950 cal yr BP, and rose 
notably through the Little Ice Age with pulses centred on ~600, 
530, 470, 330, 200, 90, and 20 cal yr BP. Synchronous fluctuations 
in Antarctic ice core chemistry strongly suggest that these 
variations were linked to changes in the westerlies. Equatorward 
drift of the westerlies during the wet periods may have influenced 
Atlantic meridional overturning circulation by restricting marine 
flow around the tip of Africa. Apparent inconsistencies among some 
aspects of records from South America, New Zealand and South Africa 
warn against the simplistic application of single records to the 
Southern Hemisphere as a whole. Nonetheless, these findings in 
general do support model projections of increasing aridity in 
the austral winter rainfall zones with future warming.  
          STUDY NOTES: Diatom time series from Verlorenvlei, South Africa for the past 
1400 years.  Diatom data grouped as follows: 

dilute-water taxa = mostly Aulacoseira granulata + Nitzschia lacuum 
+ Synedra delicatissima (sensu Partrick &amp; Reimer) 
Brackish taxa  = Cyclotella meneghiniana + Thalassiosira 
Epiphytic taxa  = Cocconeis + Epithemia 

Higher &quot;% dilute&quot; interpreted as indicating more winter rains, 
with austral westerlies shifted equatorward. 

Core VV09, Verlorenvlei, South Africa: 
32.36°S, 18.44°&apos;E, ~1m elevation, 4m water depth. 
</Abstract>
  </Summary>
  <Related_URL>
    <URL_Content_Type>
      <Type>GET DATA</Type>
    </URL_Content_Type>
    <URL>https://www1.ncdc.noaa.gov/pub/data/paleo/paleolimnology/africa/verlorenvlei2012.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/paleolimnology/africa/verlorenvlei2012.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>
</DIF>
