An ocean–ice coupled response during the last glacial: a view from a marine isotopic stage 3 record south of the Faeroe Shetland Gateway
The rapid climatic variability characterising the Marine Isotopic Stage (MIS) 3 (~60–30 cal ka BP) provides key issues to understand the atmosphere–ocean–cryosphere dynamics. Here we investigate the response of sea-surface paleoenvironments to the MIS3 climatic variability through the study of a hig...
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2012
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ftvuamstcris:oai:research.vu.nl:publications/d63a0910-3827-47f4-a4d6-b703f7227639 2023-05-15T16:12:58+02:00 An ocean–ice coupled response during the last glacial: a view from a marine isotopic stage 3 record south of the Faeroe Shetland Gateway Zumaque, J. Eynaud, F. Zaragosi, S. Marret, F. Matsuzaki, K.M. Kissel, C. Roche, D.M.V.A.P. Malaizé, B. Michel, E. Billy, I. Richter, T. Palis, E. 2012 application/pdf https://research.vu.nl/en/publications/d63a0910-3827-47f4-a4d6-b703f7227639 https://doi.org/10.5194/cp-8-1997-2012 https://research.vu.nl/ws/files/658841/298498.pdf http://www.clim-past.net/8/1997/2012/cp-8-1997-2012.html eng eng info:eu-repo/semantics/openAccess Zumaque , J , Eynaud , F , Zaragosi , S , Marret , F , Matsuzaki , K M , Kissel , C , Roche , D M V A P , Malaizé , B , Michel , E , Billy , I , Richter , T & Palis , E 2012 , ' An ocean–ice coupled response during the last glacial: a view from a marine isotopic stage 3 record south of the Faeroe Shetland Gateway ' , Climate of the Past , vol. 8 , no. 6 , pp. 1997-2017 . https://doi.org/10.5194/cp-8-1997-2012 article 2012 ftvuamstcris https://doi.org/10.5194/cp-8-1997-2012 2021-12-29T07:45:40Z The rapid climatic variability characterising the Marine Isotopic Stage (MIS) 3 (~60–30 cal ka BP) provides key issues to understand the atmosphere–ocean–cryosphere dynamics. Here we investigate the response of sea-surface paleoenvironments to the MIS3 climatic variability through the study of a high resolution oceanic sedimentological archive (core MD99-2281, 60°21' N; 09°27' W; 1197 m water depth), retrieved during the MD114-IMAGES (International Marine Global Change Study) cruise from the southern part of the Faeroe Bank. This sector was under the proximal influence of European ice sheets (Fennoscandian Ice Sheet to the East, British Irish Ice Sheet to the South) during the last glacial and thus probably responded to the MIS3 pulsed climatic changes. We conducted a multi-proxy analysis of core MD99-2281, including magnetic properties, x-ray fluorescence measurements, characterisation of the coarse (>150 μm) lithic fraction (grain concentration) and the analysis of selected biogenic proxies (assemblages and stable isotope ratio of calcareous planktonic foraminifera, dinoflagellate cyst – e.g. dinocyst – assemblages). Results presented here are focussed on the dinocyst response, this proxy providing the reconstruction of past sea-surface hydrological conditions, qualitatively as well as quantitatively (e.g. transfer function sensu lato). Our study documents a very coherent and sensitive oceanic response to the MIS3 rapid climatic variability: strong fluctuations, matching those of stadial/interstadial climatic oscillations as depicted by Greenland ice cores, are recorded in the MD99-2281 archive. Proxies of terrigeneous and detritical material suggest increases in continental advection during Greenland Stadials (including Heinrich events), the latter corresponding also to southward migrations of polar waters. At the opposite, milder sea-surface conditions seem to develop during Greenland Interstadials. After 30 ka, reconstructed paleohydrological conditions evidence strong shifts in SST: this increasing variability seems consistent with the hypothesised coalescence of the British and Fennoscandian ice sheets at that time, which could have directly influenced sea-surface environments in the vicinity of core MD99-2281. Article in Journal/Newspaper Fennoscandian Greenland Greenland ice cores Ice Sheet Planktonic foraminifera Vrije Universiteit Amsterdam (VU): Research Portal Greenland Climate of the Past 8 6 1997 2017 |
institution |
Open Polar |
collection |
Vrije Universiteit Amsterdam (VU): Research Portal |
op_collection_id |
ftvuamstcris |
language |
English |
description |
The rapid climatic variability characterising the Marine Isotopic Stage (MIS) 3 (~60–30 cal ka BP) provides key issues to understand the atmosphere–ocean–cryosphere dynamics. Here we investigate the response of sea-surface paleoenvironments to the MIS3 climatic variability through the study of a high resolution oceanic sedimentological archive (core MD99-2281, 60°21' N; 09°27' W; 1197 m water depth), retrieved during the MD114-IMAGES (International Marine Global Change Study) cruise from the southern part of the Faeroe Bank. This sector was under the proximal influence of European ice sheets (Fennoscandian Ice Sheet to the East, British Irish Ice Sheet to the South) during the last glacial and thus probably responded to the MIS3 pulsed climatic changes. We conducted a multi-proxy analysis of core MD99-2281, including magnetic properties, x-ray fluorescence measurements, characterisation of the coarse (>150 μm) lithic fraction (grain concentration) and the analysis of selected biogenic proxies (assemblages and stable isotope ratio of calcareous planktonic foraminifera, dinoflagellate cyst – e.g. dinocyst – assemblages). Results presented here are focussed on the dinocyst response, this proxy providing the reconstruction of past sea-surface hydrological conditions, qualitatively as well as quantitatively (e.g. transfer function sensu lato). Our study documents a very coherent and sensitive oceanic response to the MIS3 rapid climatic variability: strong fluctuations, matching those of stadial/interstadial climatic oscillations as depicted by Greenland ice cores, are recorded in the MD99-2281 archive. Proxies of terrigeneous and detritical material suggest increases in continental advection during Greenland Stadials (including Heinrich events), the latter corresponding also to southward migrations of polar waters. At the opposite, milder sea-surface conditions seem to develop during Greenland Interstadials. After 30 ka, reconstructed paleohydrological conditions evidence strong shifts in SST: this increasing variability seems consistent with the hypothesised coalescence of the British and Fennoscandian ice sheets at that time, which could have directly influenced sea-surface environments in the vicinity of core MD99-2281. |
format |
Article in Journal/Newspaper |
author |
Zumaque, J. Eynaud, F. Zaragosi, S. Marret, F. Matsuzaki, K.M. Kissel, C. Roche, D.M.V.A.P. Malaizé, B. Michel, E. Billy, I. Richter, T. Palis, E. |
spellingShingle |
Zumaque, J. Eynaud, F. Zaragosi, S. Marret, F. Matsuzaki, K.M. Kissel, C. Roche, D.M.V.A.P. Malaizé, B. Michel, E. Billy, I. Richter, T. Palis, E. An ocean–ice coupled response during the last glacial: a view from a marine isotopic stage 3 record south of the Faeroe Shetland Gateway |
author_facet |
Zumaque, J. Eynaud, F. Zaragosi, S. Marret, F. Matsuzaki, K.M. Kissel, C. Roche, D.M.V.A.P. Malaizé, B. Michel, E. Billy, I. Richter, T. Palis, E. |
author_sort |
Zumaque, J. |
title |
An ocean–ice coupled response during the last glacial: a view from a marine isotopic stage 3 record south of the Faeroe Shetland Gateway |
title_short |
An ocean–ice coupled response during the last glacial: a view from a marine isotopic stage 3 record south of the Faeroe Shetland Gateway |
title_full |
An ocean–ice coupled response during the last glacial: a view from a marine isotopic stage 3 record south of the Faeroe Shetland Gateway |
title_fullStr |
An ocean–ice coupled response during the last glacial: a view from a marine isotopic stage 3 record south of the Faeroe Shetland Gateway |
title_full_unstemmed |
An ocean–ice coupled response during the last glacial: a view from a marine isotopic stage 3 record south of the Faeroe Shetland Gateway |
title_sort |
ocean–ice coupled response during the last glacial: a view from a marine isotopic stage 3 record south of the faeroe shetland gateway |
publishDate |
2012 |
url |
https://research.vu.nl/en/publications/d63a0910-3827-47f4-a4d6-b703f7227639 https://doi.org/10.5194/cp-8-1997-2012 https://research.vu.nl/ws/files/658841/298498.pdf http://www.clim-past.net/8/1997/2012/cp-8-1997-2012.html |
geographic |
Greenland |
geographic_facet |
Greenland |
genre |
Fennoscandian Greenland Greenland ice cores Ice Sheet Planktonic foraminifera |
genre_facet |
Fennoscandian Greenland Greenland ice cores Ice Sheet Planktonic foraminifera |
op_source |
Zumaque , J , Eynaud , F , Zaragosi , S , Marret , F , Matsuzaki , K M , Kissel , C , Roche , D M V A P , Malaizé , B , Michel , E , Billy , I , Richter , T & Palis , E 2012 , ' An ocean–ice coupled response during the last glacial: a view from a marine isotopic stage 3 record south of the Faeroe Shetland Gateway ' , Climate of the Past , vol. 8 , no. 6 , pp. 1997-2017 . https://doi.org/10.5194/cp-8-1997-2012 |
op_rights |
info:eu-repo/semantics/openAccess |
op_doi |
https://doi.org/10.5194/cp-8-1997-2012 |
container_title |
Climate of the Past |
container_volume |
8 |
container_issue |
6 |
container_start_page |
1997 |
op_container_end_page |
2017 |
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1765998568136507392 |