Paleobotanical evidence for near present-day levels of atmospheric CO2 during part of the tertiary

Understanding the Link between the greenhouse gas carbon dioxide (CO2) and Earth's temperature underpins much of paleoclimatology and our predictions of future global warming. Here, we use the inverse relationship between Lea f stomatal indices and the partial pressure of CO2 in modern Ginkgo biloba and Metasequoia glyptostroboides to develop a CO2 reconstruction based on f ossil Ginkgo and Metaseguoia cuticles for the middle Paleocene to early Eoc ene and middle Miocene. Our reconstruction indicates that CO2 remained betw een 300 and 450 parts per million by volume for these intervals with the ex ception of a single high estimate near the Paleocene/Eocene boundary. These results suggest that factors in addition to CO2 are required to explain th ese past intervals of global warmth.