Antarctic Ice Sheet variability across the Eocene-Oligocene boundary climate transition
About 34 million years ago (Ma) Earth’s climate cooled and an ice sheet formed on Antarctica as atmospheric CO2 fell below ~750 ppm. Sedimentary cycles from a drill core in western Ross Sea provide the first direct evidence of orbitally-controlled glacial cycles between 34–31 Ma. Initially, under at...
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Online Access: | https://eprints.soton.ac.uk/393827/ https://eprints.soton.ac.uk/393827/1/Galeotti_et_al_2016_accepted_version_comb.pdf |
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ftsouthampton:oai:eprints.soton.ac.uk:393827 2023-08-27T04:06:12+02:00 Antarctic Ice Sheet variability across the Eocene-Oligocene boundary climate transition Galeotti, S. DeConto, R. Naish, T. Stocchi, P. Florindo, F. Pagani, M. Barrett, P. Bohaty, S.M. Lanci, L. Pollard, D. Sandroni, S. Talarico, F. M. Zachos, J. C. 2016-04-01 text https://eprints.soton.ac.uk/393827/ https://eprints.soton.ac.uk/393827/1/Galeotti_et_al_2016_accepted_version_comb.pdf en English eng https://eprints.soton.ac.uk/393827/1/Galeotti_et_al_2016_accepted_version_comb.pdf Galeotti, S., DeConto, R., Naish, T., Stocchi, P., Florindo, F., Pagani, M., Barrett, P., Bohaty, S.M., Lanci, L., Pollard, D., Sandroni, S., Talarico, F. M. and Zachos, J. C. (2016) Antarctic Ice Sheet variability across the Eocene-Oligocene boundary climate transition. Science, 352 (6281), 76-80. (doi:10.1126/science.aab0669 <http://dx.doi.org/10.1126/science.aab0669>). accepted_manuscript Article PeerReviewed 2016 ftsouthampton https://doi.org/10.1126/science.aab0669 2023-08-03T22:21:42Z About 34 million years ago (Ma) Earth’s climate cooled and an ice sheet formed on Antarctica as atmospheric CO2 fell below ~750 ppm. Sedimentary cycles from a drill core in western Ross Sea provide the first direct evidence of orbitally-controlled glacial cycles between 34–31 Ma. Initially, under atmospheric CO2 levels ? 600 ppm, a smaller Antarctic Ice Sheet, (AIS) restricted to the terrestrial continent, was highly responsive to local insolation forcing. A more stable, continental-scale ice sheet calving at the coastline, did not form until ~32.8 Ma coincident with the first time atmospheric CO2 levels fell below ~600 ppm. Our results provide new insights into the potential of the AIS for threshold behavior, and its sensitivity to atmospheric CO2 concentrations above present day levels. Article in Journal/Newspaper Antarc* Antarctic Antarctica Ice Sheet Ross Sea University of Southampton: e-Prints Soton Antarctic Ross Sea Science 352 6281 76 80 |
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Open Polar |
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University of Southampton: e-Prints Soton |
op_collection_id |
ftsouthampton |
language |
English |
description |
About 34 million years ago (Ma) Earth’s climate cooled and an ice sheet formed on Antarctica as atmospheric CO2 fell below ~750 ppm. Sedimentary cycles from a drill core in western Ross Sea provide the first direct evidence of orbitally-controlled glacial cycles between 34–31 Ma. Initially, under atmospheric CO2 levels ? 600 ppm, a smaller Antarctic Ice Sheet, (AIS) restricted to the terrestrial continent, was highly responsive to local insolation forcing. A more stable, continental-scale ice sheet calving at the coastline, did not form until ~32.8 Ma coincident with the first time atmospheric CO2 levels fell below ~600 ppm. Our results provide new insights into the potential of the AIS for threshold behavior, and its sensitivity to atmospheric CO2 concentrations above present day levels. |
format |
Article in Journal/Newspaper |
author |
Galeotti, S. DeConto, R. Naish, T. Stocchi, P. Florindo, F. Pagani, M. Barrett, P. Bohaty, S.M. Lanci, L. Pollard, D. Sandroni, S. Talarico, F. M. Zachos, J. C. |
spellingShingle |
Galeotti, S. DeConto, R. Naish, T. Stocchi, P. Florindo, F. Pagani, M. Barrett, P. Bohaty, S.M. Lanci, L. Pollard, D. Sandroni, S. Talarico, F. M. Zachos, J. C. Antarctic Ice Sheet variability across the Eocene-Oligocene boundary climate transition |
author_facet |
Galeotti, S. DeConto, R. Naish, T. Stocchi, P. Florindo, F. Pagani, M. Barrett, P. Bohaty, S.M. Lanci, L. Pollard, D. Sandroni, S. Talarico, F. M. Zachos, J. C. |
author_sort |
Galeotti, S. |
title |
Antarctic Ice Sheet variability across the Eocene-Oligocene boundary climate transition |
title_short |
Antarctic Ice Sheet variability across the Eocene-Oligocene boundary climate transition |
title_full |
Antarctic Ice Sheet variability across the Eocene-Oligocene boundary climate transition |
title_fullStr |
Antarctic Ice Sheet variability across the Eocene-Oligocene boundary climate transition |
title_full_unstemmed |
Antarctic Ice Sheet variability across the Eocene-Oligocene boundary climate transition |
title_sort |
antarctic ice sheet variability across the eocene-oligocene boundary climate transition |
publishDate |
2016 |
url |
https://eprints.soton.ac.uk/393827/ https://eprints.soton.ac.uk/393827/1/Galeotti_et_al_2016_accepted_version_comb.pdf |
geographic |
Antarctic Ross Sea |
geographic_facet |
Antarctic Ross Sea |
genre |
Antarc* Antarctic Antarctica Ice Sheet Ross Sea |
genre_facet |
Antarc* Antarctic Antarctica Ice Sheet Ross Sea |
op_relation |
https://eprints.soton.ac.uk/393827/1/Galeotti_et_al_2016_accepted_version_comb.pdf Galeotti, S., DeConto, R., Naish, T., Stocchi, P., Florindo, F., Pagani, M., Barrett, P., Bohaty, S.M., Lanci, L., Pollard, D., Sandroni, S., Talarico, F. M. and Zachos, J. C. (2016) Antarctic Ice Sheet variability across the Eocene-Oligocene boundary climate transition. Science, 352 (6281), 76-80. (doi:10.1126/science.aab0669 <http://dx.doi.org/10.1126/science.aab0669>). |
op_rights |
accepted_manuscript |
op_doi |
https://doi.org/10.1126/science.aab0669 |
container_title |
Science |
container_volume |
352 |
container_issue |
6281 |
container_start_page |
76 |
op_container_end_page |
80 |
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1775346995414695936 |