British Ice Sheet dynamics inferred from North Atlantic ice‐rafted debris records spanning the last 175 000 years

Abstract Sediment core MD04‐2822 from the Rockall Trough, northeast Atlantic, provides lithological evidence for the expansion of the British Ice Sheet (BIS) onto the Hebridean margin during both the penultimate (Marine Isotope Stage (MIS) 6/Wolstonian/Saalian) and last glaciation (Devensian/Weichse...

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Published in:Journal of Quaternary Science
Main Authors: Hibbert, Fiona D., Austin, William E. N., Leng, Melanie J., Gatliff, Robert W.
Other Authors: British Geological Survey, University of St Andrews
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 2009
Subjects:
Online Access:http://dx.doi.org/10.1002/jqs.1331
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spelling crwiley:10.1002/jqs.1331 2024-06-23T07:47:13+00:00 British Ice Sheet dynamics inferred from North Atlantic ice‐rafted debris records spanning the last 175 000 years Hibbert, Fiona D. Austin, William E. N. Leng, Melanie J. Gatliff, Robert W. British Geological Survey University of St Andrews 2009 http://dx.doi.org/10.1002/jqs.1331 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fjqs.1331 https://onlinelibrary.wiley.com/doi/pdf/10.1002/jqs.1331 en eng Wiley http://onlinelibrary.wiley.com/termsAndConditions#vor Journal of Quaternary Science volume 25, issue 4, page 461-482 ISSN 0267-8179 1099-1417 journal-article 2009 crwiley https://doi.org/10.1002/jqs.1331 2024-06-04T06:45:40Z Abstract Sediment core MD04‐2822 from the Rockall Trough, northeast Atlantic, provides lithological evidence for the expansion of the British Ice Sheet (BIS) onto the Hebridean margin during both the penultimate (Marine Isotope Stage (MIS) 6/Wolstonian/Saalian) and last glaciation (Devensian/Weichselian). A composite chronology is constructed using: (i) the benthic foraminiferal oxygen isotope record, matched to an orbitally tuned stacked record of global ice volume (SPECMAP); (ii) the synchronisation of the planktonic foraminiferal ( Neogloboquadrina pachyderma (sinistral)) and ITRAX XRF Ca records to the Greenland ice core (NGRIP) back to ca. 123 ka; and (iii) the synchronisation of the same N. pachyderma (sinistral)) and ITRAX XRF Ca records to the atmospheric methane record of the Antarctic ice core (EPICA Dome C) beyond 123 ka. The first offshore evidence for the expansion of the last BIS within MIS 4 is presented, suggesting extensive glaciation of northwestern Britain during the Devensian/Weichselian as early as 70 ka. The proximity of this long sediment core to the glaciated margin of northwestern Scotland makes it ideal to capture the ice‐rafted debris (IRD) signal of the BIS for the last 175 ka, via a continuous flux record of IRD. British Geological Survey © NERC 2009. All rights reserved. Article in Journal/Newspaper Antarc* Antarctic EPICA Greenland Greenland ice core ice core Ice Sheet Neogloboquadrina pachyderma NGRIP North Atlantic Northeast Atlantic Wiley Online Library Antarctic Greenland Rockall Trough ENVELOPE(-15.036,-15.036,53.825,53.825) The Antarctic Journal of Quaternary Science 25 4 461 482
institution Open Polar
collection Wiley Online Library
op_collection_id crwiley
language English
description Abstract Sediment core MD04‐2822 from the Rockall Trough, northeast Atlantic, provides lithological evidence for the expansion of the British Ice Sheet (BIS) onto the Hebridean margin during both the penultimate (Marine Isotope Stage (MIS) 6/Wolstonian/Saalian) and last glaciation (Devensian/Weichselian). A composite chronology is constructed using: (i) the benthic foraminiferal oxygen isotope record, matched to an orbitally tuned stacked record of global ice volume (SPECMAP); (ii) the synchronisation of the planktonic foraminiferal ( Neogloboquadrina pachyderma (sinistral)) and ITRAX XRF Ca records to the Greenland ice core (NGRIP) back to ca. 123 ka; and (iii) the synchronisation of the same N. pachyderma (sinistral)) and ITRAX XRF Ca records to the atmospheric methane record of the Antarctic ice core (EPICA Dome C) beyond 123 ka. The first offshore evidence for the expansion of the last BIS within MIS 4 is presented, suggesting extensive glaciation of northwestern Britain during the Devensian/Weichselian as early as 70 ka. The proximity of this long sediment core to the glaciated margin of northwestern Scotland makes it ideal to capture the ice‐rafted debris (IRD) signal of the BIS for the last 175 ka, via a continuous flux record of IRD. British Geological Survey © NERC 2009. All rights reserved.
author2 British Geological Survey
University of St Andrews
format Article in Journal/Newspaper
author Hibbert, Fiona D.
Austin, William E. N.
Leng, Melanie J.
Gatliff, Robert W.
spellingShingle Hibbert, Fiona D.
Austin, William E. N.
Leng, Melanie J.
Gatliff, Robert W.
British Ice Sheet dynamics inferred from North Atlantic ice‐rafted debris records spanning the last 175 000 years
author_facet Hibbert, Fiona D.
Austin, William E. N.
Leng, Melanie J.
Gatliff, Robert W.
author_sort Hibbert, Fiona D.
title British Ice Sheet dynamics inferred from North Atlantic ice‐rafted debris records spanning the last 175 000 years
title_short British Ice Sheet dynamics inferred from North Atlantic ice‐rafted debris records spanning the last 175 000 years
title_full British Ice Sheet dynamics inferred from North Atlantic ice‐rafted debris records spanning the last 175 000 years
title_fullStr British Ice Sheet dynamics inferred from North Atlantic ice‐rafted debris records spanning the last 175 000 years
title_full_unstemmed British Ice Sheet dynamics inferred from North Atlantic ice‐rafted debris records spanning the last 175 000 years
title_sort british ice sheet dynamics inferred from north atlantic ice‐rafted debris records spanning the last 175 000 years
publisher Wiley
publishDate 2009
url http://dx.doi.org/10.1002/jqs.1331
https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fjqs.1331
https://onlinelibrary.wiley.com/doi/pdf/10.1002/jqs.1331
long_lat ENVELOPE(-15.036,-15.036,53.825,53.825)
geographic Antarctic
Greenland
Rockall Trough
The Antarctic
geographic_facet Antarctic
Greenland
Rockall Trough
The Antarctic
genre Antarc*
Antarctic
EPICA
Greenland
Greenland ice core
ice core
Ice Sheet
Neogloboquadrina pachyderma
NGRIP
North Atlantic
Northeast Atlantic
genre_facet Antarc*
Antarctic
EPICA
Greenland
Greenland ice core
ice core
Ice Sheet
Neogloboquadrina pachyderma
NGRIP
North Atlantic
Northeast Atlantic
op_source Journal of Quaternary Science
volume 25, issue 4, page 461-482
ISSN 0267-8179 1099-1417
op_rights http://onlinelibrary.wiley.com/termsAndConditions#vor
op_doi https://doi.org/10.1002/jqs.1331
container_title Journal of Quaternary Science
container_volume 25
container_issue 4
container_start_page 461
op_container_end_page 482
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