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  <dc:title xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:ows="http://www.opengis.net/ows">Wonderkrater, South Africa 20,000 Year Pollen Data</dc:title>
  <dc:creator xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:ows="http://www.opengis.net/ows">Scott, L.</dc:creator>
  <dc:creator xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:ows="http://www.opengis.net/ows">Scott, L.</dc:creator>
  <dc:subject xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:ows="http://www.opengis.net/ows">PAGES 2k Network</dc:subject>
  <dc:subject xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:ows="http://www.opengis.net/ows">PAGES Africa 2k</dc:subject>
  <dc:subject xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:ows="http://www.opengis.net/ows">earth science/paleoclimate/pollen</dc:subject>
  <dc:subject xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:ows="http://www.opengis.net/ows"> (Wonderkrater WkrB3&gt;LATITUDE -24.4333&gt;LONGITUDE 28.75)</dc:subject>
  <dc:description xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:ows="http://www.opengis.net/ows">Pollen spectra from cores of organic spring deposits from 
the Transvaal provide evidence for the climatic evolution 
of the province during the last 35,000 yr B.P. or more. 
The past climatic phases are derived from palynological 
reconstructions of past vegetation types by comparison 
of fossil pollen data with modern surface pollen spectra 
from various localities. Evidence is provided for an early 
moist, cool phase with relatively mesic bushveld and expanded 
montane forest in the central Transvaal, followed by a drier 
period with drier bushveld which probably lasted until 
approximately 25,000 yr B.P. During the next phase, 
which at the latest ended about 11,000 yr B.P., 
the temperatures were probably 5°-6°C cooler than at present. 
At that time bushveld vegetation in the central Transvaal 
was replaced by open grassland with macchia elements. 
Climatic amelioration came and semiarid savanna returned 
to the plains, at first gradually and then developing into 
a warm Kalahari thornveld-type vegetation. After 6000 yr B.P. 
it apparently became slightly wetter and a more broad-leafed 
bushveld developed. About 4000 yr B.P. it again became cooler 
and slightly wetter and the bushveld vegetation on the central 
and northern plains was comparable to present open upland types. 
After 2000 yr B.P. conditions gradually became warner until 
about 1000 yr B.P., when the modern climate of the central 
Transvaal bushveld originated. 
 
          STUDY NOTES: 20,000 year pollen record from a peat deposit surrounding 
the Wonderkrater thermal spring near Naboomspruit, in the 
Transvaal bushveld, South Africa. 

Wonderkrater: 24°26&apos;S, 28°45&apos;E, elevation 1100m.</dc:description>
  <dc:publisher xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:ows="http://www.opengis.net/ows">NCDC-Paleoclimatology</dc:publisher>
  <dc:publisher xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:ows="http://www.opengis.net/ows">https://www.ncdc.noaa.gov/data-access/paleoclimatology-data - Bauer Bruce</dc:publisher>
  <dc:contributor xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:ows="http://www.opengis.net/ows">Investigator : Scott, L.</dc:contributor>
  <dc:date xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:ows="http://www.opengis.net/ows">2012-07-25</dc:date>
  <dc:type xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:ows="http://www.opengis.net/ows">ONLINE Files</dc:type>
  <dc:format xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:ows="http://www.opengis.net/ows">online, ASCII</dc:format>
  <dc:identifier xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:ows="http://www.opengis.net/ows">https://www.ncdc.noaa.gov/paleo/study/13155</dc:identifier>
  <dc:identifier xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:ows="http://www.opengis.net/ows">https://www1.ncdc.noaa.gov/pub/data/paleo/pollen/africa/wonderkrater1982pollen.xls</dc:identifier>
  <dc:identifier xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:ows="http://www.opengis.net/ows">https://www1.ncdc.noaa.gov/pub/data/paleo/pollen/africa/wonderkrater1982pollen.txt</dc:identifier>
  <dc:source xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:ows="http://www.opengis.net/ows">https://www1.ncdc.noaa.gov/pub/data/paleo/pollen/africa/wonderkrater1982pollen.xls</dc:source>
  <dc:source xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:ows="http://www.opengis.net/ows">https://www1.ncdc.noaa.gov/pub/data/paleo/pollen/africa/wonderkrater1982pollen.txt</dc:source>
  <dc:language xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:ows="http://www.opengis.net/ows">English</dc:language>
  <dc:relation xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:ows="http://www.opengis.net/ows">https://www.ncdc.noaa.gov/paleo/study/13155</dc:relation>
  <dc:relation xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:ows="http://www.opengis.net/ows">https://www1.ncdc.noaa.gov/pub/data/paleo/pollen/africa/wonderkrater1982pollen.xls</dc:relation>
  <dc:relation xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:ows="http://www.opengis.net/ows">https://www1.ncdc.noaa.gov/pub/data/paleo/pollen/africa/wonderkrater1982pollen.txt</dc:relation>
  <dc:relation xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:ows="http://www.opengis.net/ows">Scott, L. 1982. 
A Late Quaternary Pollen Record from the Transvaal Bushveld, 
South Africa. 
Quaternary Research, Vol. 17, Issue 3, May 1982, pp. 339-340. 
http://dx.doi.org/10.1016/0033-5894(82)90028-X</dc:relation>
  <dc:coverage xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:ows="http://www.opengis.net/ows">START YEAR: 20035 cal yr BP  * END YEAR: 338 cal yr BP</dc:coverage>
  <ows:WGS84BoundingBox xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:ows="http://www.opengis.net/ows">
   <ows:LowerCorner>28.75  -24.4333</ows:LowerCorner>
   <ows:UpperCorner>28.75  -24.4333</ows:UpperCorner>
  </ows:WGS84BoundingBox>
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