Paleoceanographic and climatic teleconnections between the subarctic and subtropical North Atlantic during the last interglacial (MIS 5e)
The last interglacial, MIS (Marine Isotope Stage) 5e, lasting from about ~129 to 116 ka, holds important implications for the projected global warming, as this geological interval is believed to have been significantly warmer-than-preindustrial. This thesis refines the current understanding of the M...
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ftoceanrep:oai:oceanrep.geomar.de:44461 2023-05-15T16:03:53+02:00 Paleoceanographic and climatic teleconnections between the subarctic and subtropical North Atlantic during the last interglacial (MIS 5e) Zhuravleva, Anastasia 2018 text https://oceanrep.geomar.de/id/eprint/44461/ https://oceanrep.geomar.de/id/eprint/44461/1/Zhuravleva_2017_Dissertation.pdf https://macau.uni-kiel.de/receive/dissertation_diss_00023531 en eng https://oceanrep.geomar.de/id/eprint/44461/1/Zhuravleva_2017_Dissertation.pdf Zhuravleva, A. (2018) Paleoceanographic and climatic teleconnections between the subarctic and subtropical North Atlantic during the last interglacial (MIS 5e). Open Access (PhD/ Doctoral thesis), Christian-Albrechts-Universität Kiel, Kiel, Germany, III, 134 pp. info:eu-repo/semantics/openAccess Thesis NonPeerReviewed 2018 ftoceanrep 2023-04-07T15:41:35Z The last interglacial, MIS (Marine Isotope Stage) 5e, lasting from about ~129 to 116 ka, holds important implications for the projected global warming, as this geological interval is believed to have been significantly warmer-than-preindustrial. This thesis refines the current understanding of the MIS 5e paleoceanography in the subarctic and subtropical North Atlantic, providing new insights into ice-sheets dynamics and cross-latitudinal climatic teleconnections. For this purpose, a multi-proxy dataset comprising stable isotope compositions, foraminiferal assemblages and lithic as well as X-ray fluorescence data was produced using marine sediments from the Nordic Seas and the Bahama region. Several lines of evidence from the Nordic Seas suggest a strong sea surface freshening that persisted in the region until mid-MIS 5e (~125 ka). Comparison of published data from the Labrador Sea with the new records from the East Greenland margin provides evidence for a millennial-scale sea surface cooling and reduction in vertical water convection during early MIS 5e (at ~126.5 ka), which appears to follow a meltwater discharge event attributed to the Greenland deglaciation. A multiproxy dataset from the Bahama region further reveals a comparable cooling event as found in the high northern latitudes during early MIS 5e. The cooling was associated with a sudden southward displacement of the Intertropical Convergence Zone, in relation to a temporary reduction in deep-water formation. These observations lead to the inference that the persistent high-latitude freshening and unstable deep-water overturning during early MIS 5e accounted for a particularly sensitive climatic regime, resulting in the abrupt cold-warm switches which could be traced across various oceanic basins. Thesis East Greenland Greenland Labrador Sea Nordic Seas North Atlantic Subarctic OceanRep (GEOMAR Helmholtz Centre für Ocean Research Kiel) Greenland |
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Open Polar |
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OceanRep (GEOMAR Helmholtz Centre für Ocean Research Kiel) |
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ftoceanrep |
language |
English |
description |
The last interglacial, MIS (Marine Isotope Stage) 5e, lasting from about ~129 to 116 ka, holds important implications for the projected global warming, as this geological interval is believed to have been significantly warmer-than-preindustrial. This thesis refines the current understanding of the MIS 5e paleoceanography in the subarctic and subtropical North Atlantic, providing new insights into ice-sheets dynamics and cross-latitudinal climatic teleconnections. For this purpose, a multi-proxy dataset comprising stable isotope compositions, foraminiferal assemblages and lithic as well as X-ray fluorescence data was produced using marine sediments from the Nordic Seas and the Bahama region. Several lines of evidence from the Nordic Seas suggest a strong sea surface freshening that persisted in the region until mid-MIS 5e (~125 ka). Comparison of published data from the Labrador Sea with the new records from the East Greenland margin provides evidence for a millennial-scale sea surface cooling and reduction in vertical water convection during early MIS 5e (at ~126.5 ka), which appears to follow a meltwater discharge event attributed to the Greenland deglaciation. A multiproxy dataset from the Bahama region further reveals a comparable cooling event as found in the high northern latitudes during early MIS 5e. The cooling was associated with a sudden southward displacement of the Intertropical Convergence Zone, in relation to a temporary reduction in deep-water formation. These observations lead to the inference that the persistent high-latitude freshening and unstable deep-water overturning during early MIS 5e accounted for a particularly sensitive climatic regime, resulting in the abrupt cold-warm switches which could be traced across various oceanic basins. |
format |
Thesis |
author |
Zhuravleva, Anastasia |
spellingShingle |
Zhuravleva, Anastasia Paleoceanographic and climatic teleconnections between the subarctic and subtropical North Atlantic during the last interglacial (MIS 5e) |
author_facet |
Zhuravleva, Anastasia |
author_sort |
Zhuravleva, Anastasia |
title |
Paleoceanographic and climatic teleconnections between the subarctic and subtropical North Atlantic during the last interglacial (MIS 5e) |
title_short |
Paleoceanographic and climatic teleconnections between the subarctic and subtropical North Atlantic during the last interglacial (MIS 5e) |
title_full |
Paleoceanographic and climatic teleconnections between the subarctic and subtropical North Atlantic during the last interglacial (MIS 5e) |
title_fullStr |
Paleoceanographic and climatic teleconnections between the subarctic and subtropical North Atlantic during the last interglacial (MIS 5e) |
title_full_unstemmed |
Paleoceanographic and climatic teleconnections between the subarctic and subtropical North Atlantic during the last interglacial (MIS 5e) |
title_sort |
paleoceanographic and climatic teleconnections between the subarctic and subtropical north atlantic during the last interglacial (mis 5e) |
publishDate |
2018 |
url |
https://oceanrep.geomar.de/id/eprint/44461/ https://oceanrep.geomar.de/id/eprint/44461/1/Zhuravleva_2017_Dissertation.pdf https://macau.uni-kiel.de/receive/dissertation_diss_00023531 |
geographic |
Greenland |
geographic_facet |
Greenland |
genre |
East Greenland Greenland Labrador Sea Nordic Seas North Atlantic Subarctic |
genre_facet |
East Greenland Greenland Labrador Sea Nordic Seas North Atlantic Subarctic |
op_relation |
https://oceanrep.geomar.de/id/eprint/44461/1/Zhuravleva_2017_Dissertation.pdf Zhuravleva, A. (2018) Paleoceanographic and climatic teleconnections between the subarctic and subtropical North Atlantic during the last interglacial (MIS 5e). Open Access (PhD/ Doctoral thesis), Christian-Albrechts-Universität Kiel, Kiel, Germany, III, 134 pp. |
op_rights |
info:eu-repo/semantics/openAccess |
_version_ |
1766399580649291776 |