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Anema, J. (author)As a result of the injection of massive amounts of carbon, the Paleocene-Eocene boundary is characterized by an abrupt rise in global temperature. The Paleocene-Eocene Thermal Maximum (PETM) is coincided with a drastic change in sediments and a negative Carbon Isotope Excursion (CIE). Given the recent issues of global warming, with a changing...report 2017