Relative sea-level rise around East Antarctica during Oligocene glaciation

During the middle and late Eocene (∼48-34 Myr ago), the Earth's climate cooled and an ice sheet built up on Antarctica. The stepwise expansion of ice on Antarcticainduced crustal deformation and gravitational perturbations around the continent. Close to the ice sheet, sea level rosedespite an o...

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Bibliographic Details
Published in:Nature Geoscience
Main Authors: Stocchi, Paolo, Escutia, Carlota, Houben, Alexander J. P., Vermeersen, Bert L. A., Bijl, Peter K., Brinkhuis, Henk, DeConto, Robert M., Galeotti, Simone, Passchier, Sandra, Pollard, David, Klaus, Adam, Fehr, Annick, Williams, Trevor, Bendle, James A. P., Bohaty, Steven M., Carr, Stephanie A., Dunbar, Robert B., Flores, Jose Abel, Gonzàlez, Jhon J., Hayden, Travis G., Iwai, Masao, Jimenez-Espejo, Francisco J., Katsuki, Kota, Kong, Gee Soo, McKay, Robert M., Nakai, Mutsumi, Olney, Matthew P, Pekar, Stephen F., Pross, Jörg, Riesselman, Christina, Röhl, Ursula
Format: Article in Journal/Newspaper
Language:English
Published: Nature Publishing Group 2013
Subjects:
Climate transition
Ice-sheet
Eustasy
Records
1900 Earth and Planetary Sciences
Antarctic
East Antarctica
The Antarctic
Antarc*
Antarctica
Ice Sheet
Online Access:https://espace.library.uq.edu.au/view/UQ:303118
Description
Summary:During the middle and late Eocene (∼48-34 Myr ago), the Earth's climate cooled and an ice sheet built up on Antarctica. The stepwise expansion of ice on Antarcticainduced crustal deformation and gravitational perturbations around the continent. Close to the ice sheet, sea level rosedespite an overall reduction in the mass of the ocean caused by the transfer of water to the ice sheet. Here we identify the crustal response to ice-sheet growth by forcing a glacial-hydro isostatic adjustment model with an Antarctic ice-sheet model. We find that the shelf areas around East Antarctica first shoaled as upper mantle material upwelled and a peripheral forebulge developed. The inner shelf subsequently subsided as lithosphere flexure extended outwards from the ice-sheet margins. Consequently the coasts experienced a progressive relative sea-level rise. Our analysis of sediment cores from the vicinity of the Antarctic ice sheet are in agreement with the spatial patterns of relative sea-level change indicated by our simulations. Our results are consistent with the suggestion that near-field processes such as local sea-level change influence the equilibrium state obtained by an icesheet grounding line.

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