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Acquiring High to Ultra-High Resolution Geological Records of Past Climate Change by Scientific Drilling

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Figure 2. Comparison of selected high-resolution speleothem, lake, and marine records  for  the  last  deglaciation,  with  the  well-known  Younger  Dryas  cold  event  delineated  by  the  gray  bar  (from  Yancheva  et  al.,  2007)
Figure 4. A one million year comparison of ice core and marine core data to a terrestrial  record of pollen variability from Lake Tenaghi Philippon, Greece
Figure 5. The development of a limited number of well-dated marine ‘reference sections’ for the late  Quaternary would serve as a valuable complement to Greenland and Antarctic ice core records, which  by their nature only record high-latitude processes in
Figure 6. Compilation of potential drilling sites proposed by workshop participants to address the five “petal”

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