Antarctic environmental change and ice sheet evolution through the Miocene to Pliocene – a perspective from the Ross Sea and George V to Wilkes Land Coasts

The Miocene to Pliocene (Neogene) occurred between 23.04 and 2.58 million years ago and includes intervals of peak global warmth where Earth’s average surface temperature was up to 8℃ warmer than present. Major cooling steps also occurred, across which Antarctica’s ice sheets advanced to the contine...

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Bibliographic Details
Main Authors: Levy, Richard H., Dolan, Aisling M., Escutia, Carlota, Gasson, Edward G.W., McKay, Robert M., Naish, Tim, Patterson, Molly O., Perez, Lara F., Shevenell, Amelia E., Flierdt, Tina van de, Dickinson, Warren, Kowalewski, Douglas E., Meyers, Stephen R., Ohneiser, Christian, Sangiorgi, Francesca, Williams, Trevor, Chorley, Hannah K., Santis, Laura De, Florindo, Fabio, Golledge, Nicholas R., Grant, Georgia R., Halberstadt, Anna Ruth W., Harwood, David M., Lewis, Adam R., Powell, Ross, Verret, Marjolaine
Other Authors: Siegert, Martin, De Santis, Laura
Format: Book Part
Language:unknown
Published: Elsevier 2021
Subjects:
Online Access:http://nora.nerc.ac.uk/id/eprint/531569/
https://doi.org/10.1016/B978-0-12-819109-5.00014-1