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The paleontologists and geochemists in the southern Bighorn Basin are studying the Paleocene-Eocene Thermal Maximum (PETM), a period of rapid climate change 55.8 million years ago. This event saw extreme changes in ecosystems and geochemical cycles, with a more dramatic temperature rise than other global warming episodes. The release of carbon led to massive climate and environmental changes. Scientists see the PETM as a key geological analog for present-day global warming. Western United States sedimentary deposits from this time period are of interest to researchers.