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An Ocean – Ice Coupled Response During the Last Glacial: Zooming on the Marine Isotopic Stage 3 South of the Faeroe Shetland Gateway : Volume 8, Issue 4 (01/08/2012)

By Zumaque, J.

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Book Id: WPLBN0003977686
Format Type: PDF Article :
File Size: Pages 49
Reproduction Date: 2015

Title: An Ocean – Ice Coupled Response During the Last Glacial: Zooming on the Marine Isotopic Stage 3 South of the Faeroe Shetland Gateway : Volume 8, Issue 4 (01/08/2012)  
Author: Zumaque, J.
Volume: Vol. 8, Issue 4
Language: English
Subject: Science, Climate, Past
Collections: Periodicals: Journal and Magazine Collection, Copernicus GmbH
Historic
Publication Date:
2012
Publisher: Copernicus Gmbh, Göttingen, Germany
Member Page: Copernicus Publications

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Marret, F., Zaragosi, S., Eynaud, F., Kissel, C., Billy, I., Zumaque, J.,...Malaizé, B. (2012). An Ocean – Ice Coupled Response During the Last Glacial: Zooming on the Marine Isotopic Stage 3 South of the Faeroe Shetland Gateway : Volume 8, Issue 4 (01/08/2012). Retrieved from http://www.ebooklibrary.org/


Description
Description: Environnements et Paléoenvironnements Océaniques (EPOC), UMR5805, CNRS – Université Bordeaux I, Talence, France. 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) and thus probably recorded their response to the MIS3 pulsed climatic changes.

We conducted a multi-proxy analysis on 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 typify 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.


Summary
An Ocean – ice coupled response during the last glacial: zooming on the marine isotopic stage 3 south of the Faeroe Shetland Gateway

Excerpt
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