A ~240 ka record of Ice Sheet and Ocean interactions on the Snorri Drift, SW of Iceland
Core MD99-2323 was extracted from the Snorri Drift at a water depth of 1062 m, just south of the Denmark Strait, and ~120 km from the Last Glacial Maximum (LGM) margins of the Iceland and East Greenland Ice Sheets. The core chronology (~7.5 to 240 cal ka) is derived from radiocarbon dates, marker te...
Published in: | Global and Planetary Change |
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Main Authors: | , , |
Format: | Article in Journal/Newspaper |
Language: | English |
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Elsevier
2021
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Online Access: | http://eprints.esc.cam.ac.uk/6039/ http://eprints.esc.cam.ac.uk/6039/1/1-s2.0-S0921818121000837-main.pdf http://eprints.esc.cam.ac.uk/6039/2/1-s2.0-S0921818121000837-mmc1.docx https://doi.org/10.1016/j.gloplacha.2021.103498 |
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ftucambridgeesc:oai:eprints.esc.cam.ac.uk:6039 2023-05-15T16:00:41+02:00 A ~240 ka record of Ice Sheet and Ocean interactions on the Snorri Drift, SW of Iceland Andrews, J.T. McCave, I. N. Syvitski, Jaia 2021 text http://eprints.esc.cam.ac.uk/6039/ http://eprints.esc.cam.ac.uk/6039/1/1-s2.0-S0921818121000837-main.pdf http://eprints.esc.cam.ac.uk/6039/2/1-s2.0-S0921818121000837-mmc1.docx https://doi.org/10.1016/j.gloplacha.2021.103498 en eng Elsevier http://eprints.esc.cam.ac.uk/6039/1/1-s2.0-S0921818121000837-main.pdf http://eprints.esc.cam.ac.uk/6039/2/1-s2.0-S0921818121000837-mmc1.docx Andrews, J.T. and McCave, I. N. and Syvitski, Jaia (2021) A ~240 ka record of Ice Sheet and Ocean interactions on the Snorri Drift, SW of Iceland. Global and Planetary Change, 201. p. 103498. ISSN 09218181 DOI https://doi.org/10.1016/j.gloplacha.2021.103498 <https://doi.org/10.1016/j.gloplacha.2021.103498> 01 - Climate Change and Earth-Ocean Atmosphere Systems Article PeerReviewed 2021 ftucambridgeesc https://doi.org/10.1016/j.gloplacha.2021.103498 2022-01-20T23:18:13Z Core MD99-2323 was extracted from the Snorri Drift at a water depth of 1062 m, just south of the Denmark Strait, and ~120 km from the Last Glacial Maximum (LGM) margins of the Iceland and East Greenland Ice Sheets. The core chronology (~7.5 to 240 cal ka) is derived from radiocarbon dates, marker tephra, paleomagnetic excursion, and correlation with North Atlantic δ18O records on Neogloboquadrina pachyderma (δ18ONp). Sedimentation averaged ~7.5 cm/kyr. Records of proxy flow speed, ice rafted debris (IRD) and oxygen isotopes show that many IRD abundance peaks represent winnowing of the fine fraction by faster flows rather than pulses of increased IRD flux. The overall pattern of flow speed does not resemble the classic fast interglacial/slow glacial pattern seen in records of Nordic Sea overflow, rather the current record is suggested to be partly controlled by the production of brine-driven gravity flows from adjacent ice fronts, especially during cold periods. On a smaller scale the usual glacial/slow – interglacial/fast pattern appears to be the case during ~5 kyr oscillations during Marine Isotope Stage (MIS) 6 where periodic low flow speed is matched by high values of planktonic oxygen isotope ratios. Eight peaks in quartz wt% reflect increased contributions from glacial erosion of Precambrian and Caledonian bedrock from E and NE Greenland; peaks in dolomite may reflect glacial-marine transport from the Laurentide Ice Sheet. Cross wavelet analysis of the δ18ONp versus sortable silt and quartz records indicate significant precession and obliquity periodicities, but with little temporal correlations due to leads and lags in responses. Article in Journal/Newspaper Denmark Strait East Greenland Greenland Ice Sheet Iceland Neogloboquadrina pachyderma Nordic Sea North Atlantic University of Cambridge, Department of Earth Sciences: ESC Publications Greenland Global and Planetary Change 201 103498 |
institution |
Open Polar |
collection |
University of Cambridge, Department of Earth Sciences: ESC Publications |
op_collection_id |
ftucambridgeesc |
language |
English |
topic |
01 - Climate Change and Earth-Ocean Atmosphere Systems |
spellingShingle |
01 - Climate Change and Earth-Ocean Atmosphere Systems Andrews, J.T. McCave, I. N. Syvitski, Jaia A ~240 ka record of Ice Sheet and Ocean interactions on the Snorri Drift, SW of Iceland |
topic_facet |
01 - Climate Change and Earth-Ocean Atmosphere Systems |
description |
Core MD99-2323 was extracted from the Snorri Drift at a water depth of 1062 m, just south of the Denmark Strait, and ~120 km from the Last Glacial Maximum (LGM) margins of the Iceland and East Greenland Ice Sheets. The core chronology (~7.5 to 240 cal ka) is derived from radiocarbon dates, marker tephra, paleomagnetic excursion, and correlation with North Atlantic δ18O records on Neogloboquadrina pachyderma (δ18ONp). Sedimentation averaged ~7.5 cm/kyr. Records of proxy flow speed, ice rafted debris (IRD) and oxygen isotopes show that many IRD abundance peaks represent winnowing of the fine fraction by faster flows rather than pulses of increased IRD flux. The overall pattern of flow speed does not resemble the classic fast interglacial/slow glacial pattern seen in records of Nordic Sea overflow, rather the current record is suggested to be partly controlled by the production of brine-driven gravity flows from adjacent ice fronts, especially during cold periods. On a smaller scale the usual glacial/slow – interglacial/fast pattern appears to be the case during ~5 kyr oscillations during Marine Isotope Stage (MIS) 6 where periodic low flow speed is matched by high values of planktonic oxygen isotope ratios. Eight peaks in quartz wt% reflect increased contributions from glacial erosion of Precambrian and Caledonian bedrock from E and NE Greenland; peaks in dolomite may reflect glacial-marine transport from the Laurentide Ice Sheet. Cross wavelet analysis of the δ18ONp versus sortable silt and quartz records indicate significant precession and obliquity periodicities, but with little temporal correlations due to leads and lags in responses. |
format |
Article in Journal/Newspaper |
author |
Andrews, J.T. McCave, I. N. Syvitski, Jaia |
author_facet |
Andrews, J.T. McCave, I. N. Syvitski, Jaia |
author_sort |
Andrews, J.T. |
title |
A ~240 ka record of Ice Sheet and Ocean interactions on the Snorri Drift, SW of Iceland |
title_short |
A ~240 ka record of Ice Sheet and Ocean interactions on the Snorri Drift, SW of Iceland |
title_full |
A ~240 ka record of Ice Sheet and Ocean interactions on the Snorri Drift, SW of Iceland |
title_fullStr |
A ~240 ka record of Ice Sheet and Ocean interactions on the Snorri Drift, SW of Iceland |
title_full_unstemmed |
A ~240 ka record of Ice Sheet and Ocean interactions on the Snorri Drift, SW of Iceland |
title_sort |
~240 ka record of ice sheet and ocean interactions on the snorri drift, sw of iceland |
publisher |
Elsevier |
publishDate |
2021 |
url |
http://eprints.esc.cam.ac.uk/6039/ http://eprints.esc.cam.ac.uk/6039/1/1-s2.0-S0921818121000837-main.pdf http://eprints.esc.cam.ac.uk/6039/2/1-s2.0-S0921818121000837-mmc1.docx https://doi.org/10.1016/j.gloplacha.2021.103498 |
geographic |
Greenland |
geographic_facet |
Greenland |
genre |
Denmark Strait East Greenland Greenland Ice Sheet Iceland Neogloboquadrina pachyderma Nordic Sea North Atlantic |
genre_facet |
Denmark Strait East Greenland Greenland Ice Sheet Iceland Neogloboquadrina pachyderma Nordic Sea North Atlantic |
op_relation |
http://eprints.esc.cam.ac.uk/6039/1/1-s2.0-S0921818121000837-main.pdf http://eprints.esc.cam.ac.uk/6039/2/1-s2.0-S0921818121000837-mmc1.docx Andrews, J.T. and McCave, I. N. and Syvitski, Jaia (2021) A ~240 ka record of Ice Sheet and Ocean interactions on the Snorri Drift, SW of Iceland. Global and Planetary Change, 201. p. 103498. ISSN 09218181 DOI https://doi.org/10.1016/j.gloplacha.2021.103498 <https://doi.org/10.1016/j.gloplacha.2021.103498> |
op_doi |
https://doi.org/10.1016/j.gloplacha.2021.103498 |
container_title |
Global and Planetary Change |
container_volume |
201 |
container_start_page |
103498 |
_version_ |
1766396690540003328 |