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 Antarctica induced crustal deformation and gravitational perturbations around the continent. Close to the ice sheet, sea level rose despite a...
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fttno:oai:tudelft.nl:uuid:5cef1b23-bae6-4442-9b35-eee9757cd7af 2023-05-15T13:51:55+02:00 Relative sea-level rise around East Antarctica during Oligocene glaciation: Stocchi, P. Escutia, C. Houben, A.J.P. Vermeersen, B.L.A. Bijl, P.K. Brinkhuis, H. Deconto, R.M. Galeotti, S. Passchier, S. Pollard, D. 2013-01-01 http://resolver.tudelft.nl/uuid:5cef1b23-bae6-4442-9b35-eee9757cd7af en eng uuid:5cef1b23-bae6-4442-9b35-eee9757cd7af 472370 http://resolver.tudelft.nl/uuid:5cef1b23-bae6-4442-9b35-eee9757cd7af Nature Geoscience, 5, 6, 380-384 Geosciences Geological Survey Netherlands Energy / Geological Survey Netherlands Earth & Environment PG - Petroleum Geosciences EELS - Earth Environmental and Life Sciences article 2013 fttno 2022-04-10T16:03:26Z 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 Antarctica induced crustal deformation and gravitational perturbations around the continent. Close to the ice sheet, sea level rose despite 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 ice-sheet grounding line. Article in Journal/Newspaper Antarc* Antarctic Antarctica East Antarctica Ice Sheet TU Delft: Institutional Repository (Delft University of Technology) Antarctic East Antarctica The Antarctic |
institution |
Open Polar |
collection |
TU Delft: Institutional Repository (Delft University of Technology) |
op_collection_id |
fttno |
language |
English |
topic |
Geosciences Geological Survey Netherlands Energy / Geological Survey Netherlands Earth & Environment PG - Petroleum Geosciences EELS - Earth Environmental and Life Sciences |
spellingShingle |
Geosciences Geological Survey Netherlands Energy / Geological Survey Netherlands Earth & Environment PG - Petroleum Geosciences EELS - Earth Environmental and Life Sciences Stocchi, P. Escutia, C. Houben, A.J.P. Vermeersen, B.L.A. Bijl, P.K. Brinkhuis, H. Deconto, R.M. Galeotti, S. Passchier, S. Pollard, D. Relative sea-level rise around East Antarctica during Oligocene glaciation: |
topic_facet |
Geosciences Geological Survey Netherlands Energy / Geological Survey Netherlands Earth & Environment PG - Petroleum Geosciences EELS - Earth Environmental and Life Sciences |
description |
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 Antarctica induced crustal deformation and gravitational perturbations around the continent. Close to the ice sheet, sea level rose despite 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 ice-sheet grounding line. |
format |
Article in Journal/Newspaper |
author |
Stocchi, P. Escutia, C. Houben, A.J.P. Vermeersen, B.L.A. Bijl, P.K. Brinkhuis, H. Deconto, R.M. Galeotti, S. Passchier, S. Pollard, D. |
author_facet |
Stocchi, P. Escutia, C. Houben, A.J.P. Vermeersen, B.L.A. Bijl, P.K. Brinkhuis, H. Deconto, R.M. Galeotti, S. Passchier, S. Pollard, D. |
author_sort |
Stocchi, P. |
title |
Relative sea-level rise around East Antarctica during Oligocene glaciation: |
title_short |
Relative sea-level rise around East Antarctica during Oligocene glaciation: |
title_full |
Relative sea-level rise around East Antarctica during Oligocene glaciation: |
title_fullStr |
Relative sea-level rise around East Antarctica during Oligocene glaciation: |
title_full_unstemmed |
Relative sea-level rise around East Antarctica during Oligocene glaciation: |
title_sort |
relative sea-level rise around east antarctica during oligocene glaciation: |
publishDate |
2013 |
url |
http://resolver.tudelft.nl/uuid:5cef1b23-bae6-4442-9b35-eee9757cd7af |
geographic |
Antarctic East Antarctica The Antarctic |
geographic_facet |
Antarctic East Antarctica The Antarctic |
genre |
Antarc* Antarctic Antarctica East Antarctica Ice Sheet |
genre_facet |
Antarc* Antarctic Antarctica East Antarctica Ice Sheet |
op_source |
Nature Geoscience, 5, 6, 380-384 |
op_relation |
uuid:5cef1b23-bae6-4442-9b35-eee9757cd7af 472370 http://resolver.tudelft.nl/uuid:5cef1b23-bae6-4442-9b35-eee9757cd7af |
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1766255954643386368 |