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  <dc:title xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:ows="http://www.opengis.net/ows">Paleo-pCO2 Database Early Paleocene Multiproxy CO2 Data</dc:title>
  <dc:creator xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:ows="http://www.opengis.net/ows">Kowalczyk, J.B.; Royer, D.</dc:creator>
  <dc:creator xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:ows="http://www.opengis.net/ows">Kowalczyk, J.B.</dc:creator>
  <dc:creator xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:ows="http://www.opengis.net/ows">Royer, D.</dc:creator>
  <dc:subject xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:ows="http://www.opengis.net/ows">earth science/paleoclimate/climate forcing</dc:subject>
  <dc:subject xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:ows="http://www.opengis.net/ows"> (Castle Rock CO&gt;LATITUDE 39.38&gt;LONGITUDE -104.85)</dc:subject>
  <dc:description xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:ows="http://www.opengis.net/ows">Proxy estimates of atmospheric CO2 are necessary to reconstruct Earth&apos;s climate history. Confidence in paleo-CO2 estimates can be increased by comparing results from multiple proxies at a single site, but so far this strategy has been implemented only for marine-based techniques. Here we present CO2 estimates for the well-studied early Paleocene Castle Rock site in Colorado using four paleobotanical proxies. Median estimates range from 470 to 813 ppm, demonstrating fair correspondence. The synthesis yields a median of 616 ppm (352-1110 ppm at 95% confidence), considerably higher than previous early Paleocene CO2 estimates (~300 ppm). Ash bed geochronology by the high-precision U-Pb method places the Castle Rock assemblage at 63.844 ± 0.097 Ma (fully propagated 2sigma error). When these results are placed into the broader context of other Cenozoic CO2 estimates from plant-gas-exchange approaches and coeval estimates of global mean surface temperature, a pattern emerges of an Earth system sensitivity around 3C per CO2 doubling during the Paleocene and Eocene, a time with little land ice, then steepening to &gt;7C after the Eocene once land ice was present on Antarctica. 
          STUDY NOTES: Multiproxy paleo-CO2 data from Kowalczyk et al. 2018, contributed to the Paleo-pCO2 Database</dc:description>
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  <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 : Kowalczyk, J.B.</dc:contributor>
  <dc:contributor xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:ows="http://www.opengis.net/ows">Investigator : Royer, D.</dc:contributor>
  <dc:date xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:ows="http://www.opengis.net/ows">2019-02-07</dc:date>
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  <dc:relation xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:ows="http://www.opengis.net/ows">Jennifer B. Kowalczyk, Dana L. Royer, Ian M. Miller, Clive W. Anderson, David J. Beerling, Peter J. Franks, Michaela Grein, Wilfried Konrad, Anita Roth-Nebelsick, Samuel A. Bowring, Kirk R. Johnson, Jahandar Ramezani2018Multiple Proxy Estimates of Atmospheric CO2 From an Early Paleocene RainforestPaleoceanography and Paleoclimatology33121427-143810.1029/2018PA003356https://agupubs.onlinelibrary.wiley.com/doi/full/10.1029/2018PA003356</dc:relation>
  <dc:coverage xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:ows="http://www.opengis.net/ows">START YEAR: 64000000 cal yr BP  * END YEAR: 63600000 cal yr BP</dc:coverage>
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