Variable sequence of events during the past seven terminations in two deep-sea cores from the Southern Ocean
The relationships among internally consistent records of summer sea-surface temperature (SSST), winter sea ice (WSI), and diatomaceous stable isotopes were studied across seven terminations over the last 660 ka in sedimentary cores from ODP sites 1093 and 1094. The sequence of events at both sites i...
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crcambridgeupr:10.1016/j.yqres.2011.11.006 2024-09-30T14:43:09+00:00 Variable sequence of events during the past seven terminations in two deep-sea cores from the Southern Ocean Schneider Mor, Aya Yam, Ruth Bianchi, Cristina Kunz-Pirrung, Martina Gersonde, Rainer Shemesh, Aldo 2012 http://dx.doi.org/10.1016/j.yqres.2011.11.006 http://api.elsevier.com/content/article/PII:S0033589411001451?httpAccept=text/xml http://api.elsevier.com/content/article/PII:S0033589411001451?httpAccept=text/plain https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0033589400003963 en eng Cambridge University Press (CUP) https://www.cambridge.org/core/terms Quaternary Research volume 77, issue 2, page 317-325 ISSN 0033-5894 1096-0287 journal-article 2012 crcambridgeupr https://doi.org/10.1016/j.yqres.2011.11.006 2024-09-18T04:03:19Z The relationships among internally consistent records of summer sea-surface temperature (SSST), winter sea ice (WSI), and diatomaceous stable isotopes were studied across seven terminations over the last 660 ka in sedimentary cores from ODP sites 1093 and 1094. The sequence of events at both sites indicates that SSST and WSI changes led the carbon and nitrogen isotopic changes in three Terminations (TI, TII and TVI) and followed them in the other four Terminations (TIII, TIV, TV and TVII). In both TIII and TIV, the leads and lags between the proxies were related to weak glacial mode, while in TV and TVII they were due to the influence of the mid-Pleistocene transition. We show that the sequence of events is not unique and does not follow the same pattern across terminations, implying that the processes that initiated climate change in the Southern Ocean has varied through time. Article in Journal/Newspaper Sea ice Southern Ocean Cambridge University Press Southern Ocean Quaternary Research 77 2 317 325 |
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Open Polar |
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Cambridge University Press |
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crcambridgeupr |
language |
English |
description |
The relationships among internally consistent records of summer sea-surface temperature (SSST), winter sea ice (WSI), and diatomaceous stable isotopes were studied across seven terminations over the last 660 ka in sedimentary cores from ODP sites 1093 and 1094. The sequence of events at both sites indicates that SSST and WSI changes led the carbon and nitrogen isotopic changes in three Terminations (TI, TII and TVI) and followed them in the other four Terminations (TIII, TIV, TV and TVII). In both TIII and TIV, the leads and lags between the proxies were related to weak glacial mode, while in TV and TVII they were due to the influence of the mid-Pleistocene transition. We show that the sequence of events is not unique and does not follow the same pattern across terminations, implying that the processes that initiated climate change in the Southern Ocean has varied through time. |
format |
Article in Journal/Newspaper |
author |
Schneider Mor, Aya Yam, Ruth Bianchi, Cristina Kunz-Pirrung, Martina Gersonde, Rainer Shemesh, Aldo |
spellingShingle |
Schneider Mor, Aya Yam, Ruth Bianchi, Cristina Kunz-Pirrung, Martina Gersonde, Rainer Shemesh, Aldo Variable sequence of events during the past seven terminations in two deep-sea cores from the Southern Ocean |
author_facet |
Schneider Mor, Aya Yam, Ruth Bianchi, Cristina Kunz-Pirrung, Martina Gersonde, Rainer Shemesh, Aldo |
author_sort |
Schneider Mor, Aya |
title |
Variable sequence of events during the past seven terminations in two deep-sea cores from the Southern Ocean |
title_short |
Variable sequence of events during the past seven terminations in two deep-sea cores from the Southern Ocean |
title_full |
Variable sequence of events during the past seven terminations in two deep-sea cores from the Southern Ocean |
title_fullStr |
Variable sequence of events during the past seven terminations in two deep-sea cores from the Southern Ocean |
title_full_unstemmed |
Variable sequence of events during the past seven terminations in two deep-sea cores from the Southern Ocean |
title_sort |
variable sequence of events during the past seven terminations in two deep-sea cores from the southern ocean |
publisher |
Cambridge University Press (CUP) |
publishDate |
2012 |
url |
http://dx.doi.org/10.1016/j.yqres.2011.11.006 http://api.elsevier.com/content/article/PII:S0033589411001451?httpAccept=text/xml http://api.elsevier.com/content/article/PII:S0033589411001451?httpAccept=text/plain https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0033589400003963 |
geographic |
Southern Ocean |
geographic_facet |
Southern Ocean |
genre |
Sea ice Southern Ocean |
genre_facet |
Sea ice Southern Ocean |
op_source |
Quaternary Research volume 77, issue 2, page 317-325 ISSN 0033-5894 1096-0287 |
op_rights |
https://www.cambridge.org/core/terms |
op_doi |
https://doi.org/10.1016/j.yqres.2011.11.006 |
container_title |
Quaternary Research |
container_volume |
77 |
container_issue |
2 |
container_start_page |
317 |
op_container_end_page |
325 |
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1811645075352977408 |