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Climate of the Past An interactive open-access journal of the European Geosciences Union
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CP | Articles | Volume 14, issue 7
Clim. Past, 14, 991–1014, 2018
https://doi.org/10.5194/cp-14-991-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
Clim. Past, 14, 991–1014, 2018
https://doi.org/10.5194/cp-14-991-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.

Research article 10 Jul 2018

Research article | 10 Jul 2018

Paleoceanography and ice sheet variability offshore Wilkes Land, Antarctica – Part 1: Insights from late Oligocene astronomically paced contourite sedimentation

Ariadna Salabarnada et al.

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Status: closed
Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
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Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision
ED: Reconsider after major revisions (12 Mar 2018) by David Thornalley
AR by Ariadna Salabarnada Roset on behalf of the Authors (23 Apr 2018)  Author's response    Manuscript
ED: Reconsider after major revisions (27 Apr 2018) by David Thornalley
AR by Ariadna Salabarnada Roset on behalf of the Authors (02 May 2018)  Author's response    Manuscript
ED: Referee Nomination & Report Request started (14 May 2018) by David Thornalley
ED: Publish as is (21 Jun 2018) by David Thornalley
Publications Copernicus
Short summary
Here we reconstruct ice sheet and paleoceanographic configurations in the East Antarctic Wilkes Land margin based on a multi-proxy study conducted in late Oligocene (26–25 Ma) sediments from IODP Site U1356. The new obliquity-forced glacial–interglacial sedimentary model shows that, under the high CO2 values of the late Oligocene, ice sheets had mostly retreated to their terrestrial margins and the ocean was very dynamic with shifting positions of the polar fronts and associated water masses.
Here we reconstruct ice sheet and paleoceanographic configurations in the East Antarctic Wilkes...
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