Evolution of the early Antarctic ice ages
Understanding the stability of the early Antarctic ice cap in the geological past is of societal interest because present-day atmospheric CO2 concentrations have reached values comparable to those estimated for the Oligocene and the Early Miocene epochs. Here we analyze a new high-resolution deep-se...
Published in: | Geochemistry, Geophysics, Geosystems |
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Online Access: | https://doi.org/10.1002/2016GC006715 |
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ftzenodo:oai:zenodo.org:466301 2024-09-15T17:44:11+00:00 Evolution of the early Antarctic ice ages Liebrand, Diederik de Bakker, Anouk T. M. Beddow, Helen M. Wilson, Paul A. Bohaty, Steven M. Ruessink, Gerben Pälike, Heiko Batenburg, Sietske J. Hilgen, Frederik J. Hodell, David A. Huck, Claire E. Kroon, Dick Raffi, Isabella Saes, Mischa J. M. van Dijk, Arnold E. Lourens, Lucas J. 2017-03-27 https://doi.org/10.1002/2016GC006715 unknown Zenodo https://zenodo.org/communities/eu https://doi.org/10.1002/2016GC006715 oai:zenodo.org:466301 info:eu-repo/semantics/openAccess Creative Commons Attribution Non Commercial No Derivatives 4.0 International https://creativecommons.org/licenses/by-nc-nd/4.0/legalcode Proceedings of the National Academy of Sciences of the United States of America, (2017-03-27) unipolar icehouse early Antarctic ice sheet Oligocene−Miocene glacial−interglacial cycle geometries bispectral analysis info:eu-repo/semantics/article 2017 ftzenodo https://doi.org/10.1002/2016GC006715 2024-07-26T11:22:32Z Understanding the stability of the early Antarctic ice cap in the geological past is of societal interest because present-day atmospheric CO2 concentrations have reached values comparable to those estimated for the Oligocene and the Early Miocene epochs. Here we analyze a new high-resolution deep-sea oxygen isotope (δ18O) record from the South Atlantic Ocean spanning an interval between 30.1 My and 17.1 My ago. The record displays major oscillations in deep-sea temperature and Antarctic ice volume in response to the ∼110-ky eccentricity modulation of precession. Conservative minimum ice volume estimates show that waxing and waning of at least ∼85 to 110% of the volume of the present East Antarctic Ice Sheet is required to explain many of the ∼110-ky cycles. Antarctic ice sheets were typically largest during repeated glacial cycles of the mid-Oligocene (∼28.0 My to ∼26.3 My ago) and across the Oligocene−Miocene Transition (∼23.0 My ago). However, the high-amplitude glacial−interglacial cycles of the mid-Oligocene are highly symmetrical, indicating a more direct response to eccentricity modulation of precession than their Early Miocene counterparts, which are distinctly asymmetrical—indicative of prolonged ice buildup and delayed, but rapid, glacial terminations. We hypothesize that the long-term transition to a warmer climate state with sawtooth-shaped glacial cycles in the Early Miocene was brought about by subsidence and glacial erosion in West Antarctica during the Late Oligocene and/or a change in the variability of atmospheric CO2 levels on astronomical time scales that is not yet captured in existing proxy reconstructions. The Antarctic ice cap waxed and waned on astronomical time scales throughout the Oligo-Miocene time interval. We quantify geometries of Antarctic ice age cycles, as expressed in a new climate record from the South Atlantic Ocean, to track changing dynamics of the unipolar icehouse climate state. We document numerous ∼110-thousand-year-long oscillations between a near-fully glaciated and ... Article in Journal/Newspaper Antarc* Antarctic Antarctica Ice cap Ice Sheet South Atlantic Ocean West Antarctica Zenodo Geochemistry, Geophysics, Geosystems 18 3 1053 1064 |
institution |
Open Polar |
collection |
Zenodo |
op_collection_id |
ftzenodo |
language |
unknown |
topic |
unipolar icehouse early Antarctic ice sheet Oligocene−Miocene glacial−interglacial cycle geometries bispectral analysis |
spellingShingle |
unipolar icehouse early Antarctic ice sheet Oligocene−Miocene glacial−interglacial cycle geometries bispectral analysis Liebrand, Diederik de Bakker, Anouk T. M. Beddow, Helen M. Wilson, Paul A. Bohaty, Steven M. Ruessink, Gerben Pälike, Heiko Batenburg, Sietske J. Hilgen, Frederik J. Hodell, David A. Huck, Claire E. Kroon, Dick Raffi, Isabella Saes, Mischa J. M. van Dijk, Arnold E. Lourens, Lucas J. Evolution of the early Antarctic ice ages |
topic_facet |
unipolar icehouse early Antarctic ice sheet Oligocene−Miocene glacial−interglacial cycle geometries bispectral analysis |
description |
Understanding the stability of the early Antarctic ice cap in the geological past is of societal interest because present-day atmospheric CO2 concentrations have reached values comparable to those estimated for the Oligocene and the Early Miocene epochs. Here we analyze a new high-resolution deep-sea oxygen isotope (δ18O) record from the South Atlantic Ocean spanning an interval between 30.1 My and 17.1 My ago. The record displays major oscillations in deep-sea temperature and Antarctic ice volume in response to the ∼110-ky eccentricity modulation of precession. Conservative minimum ice volume estimates show that waxing and waning of at least ∼85 to 110% of the volume of the present East Antarctic Ice Sheet is required to explain many of the ∼110-ky cycles. Antarctic ice sheets were typically largest during repeated glacial cycles of the mid-Oligocene (∼28.0 My to ∼26.3 My ago) and across the Oligocene−Miocene Transition (∼23.0 My ago). However, the high-amplitude glacial−interglacial cycles of the mid-Oligocene are highly symmetrical, indicating a more direct response to eccentricity modulation of precession than their Early Miocene counterparts, which are distinctly asymmetrical—indicative of prolonged ice buildup and delayed, but rapid, glacial terminations. We hypothesize that the long-term transition to a warmer climate state with sawtooth-shaped glacial cycles in the Early Miocene was brought about by subsidence and glacial erosion in West Antarctica during the Late Oligocene and/or a change in the variability of atmospheric CO2 levels on astronomical time scales that is not yet captured in existing proxy reconstructions. The Antarctic ice cap waxed and waned on astronomical time scales throughout the Oligo-Miocene time interval. We quantify geometries of Antarctic ice age cycles, as expressed in a new climate record from the South Atlantic Ocean, to track changing dynamics of the unipolar icehouse climate state. We document numerous ∼110-thousand-year-long oscillations between a near-fully glaciated and ... |
format |
Article in Journal/Newspaper |
author |
Liebrand, Diederik de Bakker, Anouk T. M. Beddow, Helen M. Wilson, Paul A. Bohaty, Steven M. Ruessink, Gerben Pälike, Heiko Batenburg, Sietske J. Hilgen, Frederik J. Hodell, David A. Huck, Claire E. Kroon, Dick Raffi, Isabella Saes, Mischa J. M. van Dijk, Arnold E. Lourens, Lucas J. |
author_facet |
Liebrand, Diederik de Bakker, Anouk T. M. Beddow, Helen M. Wilson, Paul A. Bohaty, Steven M. Ruessink, Gerben Pälike, Heiko Batenburg, Sietske J. Hilgen, Frederik J. Hodell, David A. Huck, Claire E. Kroon, Dick Raffi, Isabella Saes, Mischa J. M. van Dijk, Arnold E. Lourens, Lucas J. |
author_sort |
Liebrand, Diederik |
title |
Evolution of the early Antarctic ice ages |
title_short |
Evolution of the early Antarctic ice ages |
title_full |
Evolution of the early Antarctic ice ages |
title_fullStr |
Evolution of the early Antarctic ice ages |
title_full_unstemmed |
Evolution of the early Antarctic ice ages |
title_sort |
evolution of the early antarctic ice ages |
publisher |
Zenodo |
publishDate |
2017 |
url |
https://doi.org/10.1002/2016GC006715 |
genre |
Antarc* Antarctic Antarctica Ice cap Ice Sheet South Atlantic Ocean West Antarctica |
genre_facet |
Antarc* Antarctic Antarctica Ice cap Ice Sheet South Atlantic Ocean West Antarctica |
op_source |
Proceedings of the National Academy of Sciences of the United States of America, (2017-03-27) |
op_relation |
https://zenodo.org/communities/eu https://doi.org/10.1002/2016GC006715 oai:zenodo.org:466301 |
op_rights |
info:eu-repo/semantics/openAccess Creative Commons Attribution Non Commercial No Derivatives 4.0 International https://creativecommons.org/licenses/by-nc-nd/4.0/legalcode |
op_doi |
https://doi.org/10.1002/2016GC006715 |
container_title |
Geochemistry, Geophysics, Geosystems |
container_volume |
18 |
container_issue |
3 |
container_start_page |
1053 |
op_container_end_page |
1064 |
_version_ |
1810491579568226304 |