Antarctic records of precession-paced insolation-driven warming during early Pleistocene Marine Isotope Stage 31

Precisely dated Antarctic continental margin and Southern Ocean geological records show that the early Pleistocene interglacial Marine Isotope Stage 31 (MIS-31) was characterized by warmer than present surface waters with reduced sea-ice and enhanced high latitude marine carbonate production. Microp...

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Published in:Geophysical Research Letters
Main Authors: Scherer, R, Bohaty, S, Dunbar, Robert B, Esper, O, Flores, J, Gersonde, R, Harnwood, D, Roberts, Andrew, Taviani, M
Format: Article in Journal/Newspaper
Language:unknown
Published: American Geophysical Union
Subjects:
Online Access:http://hdl.handle.net/1885/18971
https://doi.org/10.1029/2007GL032254
https://openresearch-repository.anu.edu.au/bitstream/1885/18971/5/Antarctic_Roberts.pdf.jpg
https://openresearch-repository.anu.edu.au/bitstream/1885/18971/7/01_Scherer_Antarctic_records_of_2008.pdf.jpg
id ftanucanberra:oai:openresearch-repository.anu.edu.au:1885/18971
record_format openpolar
spelling ftanucanberra:oai:openresearch-repository.anu.edu.au:1885/18971 2024-01-14T10:01:12+01:00 Antarctic records of precession-paced insolation-driven warming during early Pleistocene Marine Isotope Stage 31 Scherer, R Bohaty, S Dunbar, Robert B Esper, O Flores, J Gersonde, R Harnwood, D Roberts, Andrew Taviani, M http://hdl.handle.net/1885/18971 https://doi.org/10.1029/2007GL032254 https://openresearch-repository.anu.edu.au/bitstream/1885/18971/5/Antarctic_Roberts.pdf.jpg https://openresearch-repository.anu.edu.au/bitstream/1885/18971/7/01_Scherer_Antarctic_records_of_2008.pdf.jpg unknown American Geophysical Union 0094-8276 http://hdl.handle.net/1885/18971 doi:10.1029/2007GL032254 https://openresearch-repository.anu.edu.au/bitstream/1885/18971/5/Antarctic_Roberts.pdf.jpg https://openresearch-repository.anu.edu.au/bitstream/1885/18971/7/01_Scherer_Antarctic_records_of_2008.pdf.jpg Geophysical Research Letters Keywords: Atmospheric temperature Glacial geology Global warming Oceanography Sea ice Thermal stratification Pleistocene marine isotope Sea surface temperature Water mass stratification Geochronology continental margin ice sheet interglacial marine iso Journal article ftanucanberra https://doi.org/10.1029/2007GL032254 2023-12-15T09:33:34Z Precisely dated Antarctic continental margin and Southern Ocean geological records show that the early Pleistocene interglacial Marine Isotope Stage 31 (MIS-31) was characterized by warmer than present surface waters with reduced sea-ice and enhanced high latitude marine carbonate production. Micropaleontologic, isotopic, and paleomagnetic evidence from drill cores at 77°S (Cape Roberts Project-1) and 53°S (ODP Site 1094) indicate circumantarctic changes in sea surface temperature and water mass stratification that are in phase with high southern latitude insolation changes during MIS-31. These changes imply a significant, though as yet unquantifiable reduction in Antarctic ice volume. This study supports the hypothesis that the interhemispheric antiphased relationship of the precession cycle attenuates a potentially significant Antarctic ice volume signal in the deep sea oxygen isotope record. The implications are that Antarctic marine ice sheets may be more susceptible to warming and high insolation driven retreat than has been widely recognized. Article in Journal/Newspaper Antarc* Antarctic Ice Sheet Sea ice Southern Ocean Australian National University: ANU Digital Collections Antarctic Southern Ocean Cape Roberts ENVELOPE(-70.467,-70.467,-68.950,-68.950) Geophysical Research Letters 35 3
institution Open Polar
collection Australian National University: ANU Digital Collections
op_collection_id ftanucanberra
language unknown
topic Keywords: Atmospheric temperature
Glacial geology
Global warming
Oceanography
Sea ice
Thermal stratification
Pleistocene marine isotope
Sea surface temperature
Water mass stratification
Geochronology
continental margin
ice sheet
interglacial
marine iso
spellingShingle Keywords: Atmospheric temperature
Glacial geology
Global warming
Oceanography
Sea ice
Thermal stratification
Pleistocene marine isotope
Sea surface temperature
Water mass stratification
Geochronology
continental margin
ice sheet
interglacial
marine iso
Scherer, R
Bohaty, S
Dunbar, Robert B
Esper, O
Flores, J
Gersonde, R
Harnwood, D
Roberts, Andrew
Taviani, M
Antarctic records of precession-paced insolation-driven warming during early Pleistocene Marine Isotope Stage 31
topic_facet Keywords: Atmospheric temperature
Glacial geology
Global warming
Oceanography
Sea ice
Thermal stratification
Pleistocene marine isotope
Sea surface temperature
Water mass stratification
Geochronology
continental margin
ice sheet
interglacial
marine iso
description Precisely dated Antarctic continental margin and Southern Ocean geological records show that the early Pleistocene interglacial Marine Isotope Stage 31 (MIS-31) was characterized by warmer than present surface waters with reduced sea-ice and enhanced high latitude marine carbonate production. Micropaleontologic, isotopic, and paleomagnetic evidence from drill cores at 77°S (Cape Roberts Project-1) and 53°S (ODP Site 1094) indicate circumantarctic changes in sea surface temperature and water mass stratification that are in phase with high southern latitude insolation changes during MIS-31. These changes imply a significant, though as yet unquantifiable reduction in Antarctic ice volume. This study supports the hypothesis that the interhemispheric antiphased relationship of the precession cycle attenuates a potentially significant Antarctic ice volume signal in the deep sea oxygen isotope record. The implications are that Antarctic marine ice sheets may be more susceptible to warming and high insolation driven retreat than has been widely recognized.
format Article in Journal/Newspaper
author Scherer, R
Bohaty, S
Dunbar, Robert B
Esper, O
Flores, J
Gersonde, R
Harnwood, D
Roberts, Andrew
Taviani, M
author_facet Scherer, R
Bohaty, S
Dunbar, Robert B
Esper, O
Flores, J
Gersonde, R
Harnwood, D
Roberts, Andrew
Taviani, M
author_sort Scherer, R
title Antarctic records of precession-paced insolation-driven warming during early Pleistocene Marine Isotope Stage 31
title_short Antarctic records of precession-paced insolation-driven warming during early Pleistocene Marine Isotope Stage 31
title_full Antarctic records of precession-paced insolation-driven warming during early Pleistocene Marine Isotope Stage 31
title_fullStr Antarctic records of precession-paced insolation-driven warming during early Pleistocene Marine Isotope Stage 31
title_full_unstemmed Antarctic records of precession-paced insolation-driven warming during early Pleistocene Marine Isotope Stage 31
title_sort antarctic records of precession-paced insolation-driven warming during early pleistocene marine isotope stage 31
publisher American Geophysical Union
url http://hdl.handle.net/1885/18971
https://doi.org/10.1029/2007GL032254
https://openresearch-repository.anu.edu.au/bitstream/1885/18971/5/Antarctic_Roberts.pdf.jpg
https://openresearch-repository.anu.edu.au/bitstream/1885/18971/7/01_Scherer_Antarctic_records_of_2008.pdf.jpg
long_lat ENVELOPE(-70.467,-70.467,-68.950,-68.950)
geographic Antarctic
Southern Ocean
Cape Roberts
geographic_facet Antarctic
Southern Ocean
Cape Roberts
genre Antarc*
Antarctic
Ice Sheet
Sea ice
Southern Ocean
genre_facet Antarc*
Antarctic
Ice Sheet
Sea ice
Southern Ocean
op_source Geophysical Research Letters
op_relation 0094-8276
http://hdl.handle.net/1885/18971
doi:10.1029/2007GL032254
https://openresearch-repository.anu.edu.au/bitstream/1885/18971/5/Antarctic_Roberts.pdf.jpg
https://openresearch-repository.anu.edu.au/bitstream/1885/18971/7/01_Scherer_Antarctic_records_of_2008.pdf.jpg
op_doi https://doi.org/10.1029/2007GL032254
container_title Geophysical Research Letters
container_volume 35
container_issue 3
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