Middle Eocene to Late Oligocene Antarctic glaciation/deglaciation and Southern Ocean productivity

During the Eocene-Oligocene transition, Earth cooled significantly from a greenhouse to an icehouse climate. Nannofossil assemblages from Southern Ocean sites enable evaluation of paleoceanographic changes and, hence, of the oceanic response to Antarctic

Bibliographic Details
Published in:Paleoceanography
Main Authors: Villa, Giuliana, Fioroni, Chiara, Persico, Davide, Roberts, Andrew, Florindo, Fabio
Format: Article in Journal/Newspaper
Language:unknown
Published: American Geophysical Union
Subjects:
Antarctic
Southern Ocean
Antarc*
Online Access:http://hdl.handle.net/1885/69379
https://doi.org/10.1002/2013PA002518
https://openresearch-repository.anu.edu.au/bitstream/1885/69379/5/U3488905xPUB2006_2014.pdf.jpg
https://openresearch-repository.anu.edu.au/bitstream/1885/69379/7/01_Villa_Middle_Eocene_to_Late_2014.pdf.jpg
Description
Summary:During the Eocene-Oligocene transition, Earth cooled significantly from a greenhouse to an icehouse climate. Nannofossil assemblages from Southern Ocean sites enable evaluation of paleoceanographic changes and, hence, of the oceanic response to Antarctic

Similar Items