CO2 levels and climate change during Early Eocene hyperthermals
About Dr. Ying Cui
Dr. Cui is currently an Obering Postdoctoral Fellow from the Department of Earth Sciences at Dartmouth College. She obtained a PhD in Geosciences and Biogeochemistry at Penn State. Her research deals with carbon cycles during ancient hyperthermal events, such as the Paleocene-Eocene Thermal Maximum and the end-Permian mass extinction event. Her main research interest is in exploring the links between extinction, carbon emission and hyperthermals. She has published 12 peer-review articles related to this research topic, including Nature Geoscience, Earth and Planetary Science Letters, Geochimica et Cosmochimica Acta and Earth-Science Reviews. She is currently funded by National Science Foundation to study the atmospheric pCO2 and Earth system climate sensitivity during the Cenozoic.
About the Seminar
Early Eocene (56 to 33.9 million years ago) is punctuated by a series of rapid and extreme global warming events, known as the ‘hyperthermals’, triggered by massive release of carbon dioxide. Despite the carbon emission rate might have been ten times smaller than the current emission from burning fossil fuels and cement production, the early Eocene hyperthermals are considered one of the best analogues for CO2 concentration projected into the future. The temperature records are well established from deep sea sediments during these hyperthermals, but the CO2 levels in the atmosphere remain poorly known, partly due to the lack of a reliable CO2 proxy.
Thanks to a newly developed C3 land plant CO2 proxy, we were able to calculate the upper limit of the CO2 levels just before and during five early Eocene hyperthermals (PETM, H1, H2, I1 and I2). This proxy is based on the empirical relationship between carbon isotope fractionation and the ambient CO2 levels: i.e. as CO2 level rises, carbon isotope fractionation also increases. By comparing the carbon isotope excursion recorded in the ocean and on land, we were able to find that CO2 levels just before each of the hyperthermals may have been less than 1000 parts per million, or ppm. CO2 level as high as 2600 ppm might have occurred only briefly during the hyperthermals. This suggests that to maintain the early Eocene ice-free condition and global average surface temperature of ~25 oC, other greenhouse gases, such as methane, water vapor and nitrous oxide must have played more important role.