About 34 million years ago, Earth's climate cooled and an ice sheet formed on Antarctica as atmospheric carbon dioxide (CO2) fell below ∼750 parts per million (ppm). Sedimentary cycles from a drill core in the western Ross Sea provide direct evidence of orbitally controlled glacial cycles between 34 million and 31 million years ago. Initially, under atmospheric CO2 levels of >600 ppm, a smaller Antarctic Ice Sheet (AIS), restricted to the terrestrial continent, was highly responsive to local insolation forcing. A more stable, continental-scale ice sheet calving at the coastline did not form until ∼32.8 million years ago, coincident with the earliest time that atmospheric CO2 levels fell below ∼600 ppm. Our results provide insight into the potential of the AIS for threshold behavior and have implications for its sensitivity to atmospheric CO2 concentrations above present-day levels.

Galeotti, S., Deconto, R., Naish, T., Stocchi, P., Florindo, F., Pagani, M., et al. (2016). Antarctic Ice Sheet variability across the Eocene-Oligocene boundary climate transition. SCIENCE, 352(6281), 76-80 [10.1126/science.aab0669].

Antarctic Ice Sheet variability across the Eocene-Oligocene boundary climate transition

Sandroni, Sonia;Talarico, Franco M.;
2016-01-01

Abstract

About 34 million years ago, Earth's climate cooled and an ice sheet formed on Antarctica as atmospheric carbon dioxide (CO2) fell below ∼750 parts per million (ppm). Sedimentary cycles from a drill core in the western Ross Sea provide direct evidence of orbitally controlled glacial cycles between 34 million and 31 million years ago. Initially, under atmospheric CO2 levels of >600 ppm, a smaller Antarctic Ice Sheet (AIS), restricted to the terrestrial continent, was highly responsive to local insolation forcing. A more stable, continental-scale ice sheet calving at the coastline did not form until ∼32.8 million years ago, coincident with the earliest time that atmospheric CO2 levels fell below ∼600 ppm. Our results provide insight into the potential of the AIS for threshold behavior and have implications for its sensitivity to atmospheric CO2 concentrations above present-day levels.
Galeotti, S., Deconto, R., Naish, T., Stocchi, P., Florindo, F., Pagani, M., et al. (2016). Antarctic Ice Sheet variability across the Eocene-Oligocene boundary climate transition. SCIENCE, 352(6281), 76-80 [10.1126/science.aab0669].
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Utilizza questo identificativo per citare o creare un link a questo documento: https://hdl.handle.net/11365/1007376