Varying sediment sources (Hudson Strait, Cumberland Sound, Baffin Bay) to the NW Labrador Sea slope between and during Heinrich events 0 to 4
Core HU97048-007PC was recovered from the continental Labrador Sea slope at a water depth of 945?m, 250?km seaward from the mouth of Cumberland Sound, and 400?km north of Hudson Strait. Cumberland Sound is a structural trough partly floored by Cretaceous mudstones and Paleozoic carbonates. The recor...
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Online Access: | https://archimer.ifremer.fr/doc/00265/37644/35823.pdf https://doi.org/10.1002/jqs.2535 https://archimer.ifremer.fr/doc/00265/37644/ |
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ftarchimer:oai:archimer.ifremer.fr:37644 2023-05-15T15:34:57+02:00 Varying sediment sources (Hudson Strait, Cumberland Sound, Baffin Bay) to the NW Labrador Sea slope between and during Heinrich events 0 to 4 Andrews, J. T. Barber, D. C. Jennings, A. E. Eberl, D. D. Maclean, B. Kirby, M. E. Stoner, J. S. 2012-07 application/pdf https://archimer.ifremer.fr/doc/00265/37644/35823.pdf https://doi.org/10.1002/jqs.2535 https://archimer.ifremer.fr/doc/00265/37644/ eng eng Wiley-blackwell https://archimer.ifremer.fr/doc/00265/37644/35823.pdf doi:10.1002/jqs.2535 https://archimer.ifremer.fr/doc/00265/37644/ 2012 John Wiley & Sons, Ltd. info:eu-repo/semantics/openAccess restricted use Journal Of Quaternary Science (0267-8179) (Wiley-blackwell), 2012-07 , Vol. 27 , N. 5 , P. 475-484 Baffin Bay detrital carbonate (DC-) events Heinrich events Labrador Sea Laurentide Ice Sheet text Publication info:eu-repo/semantics/article 2012 ftarchimer https://doi.org/10.1002/jqs.2535 2021-09-23T20:26:12Z Core HU97048-007PC was recovered from the continental Labrador Sea slope at a water depth of 945?m, 250?km seaward from the mouth of Cumberland Sound, and 400?km north of Hudson Strait. Cumberland Sound is a structural trough partly floored by Cretaceous mudstones and Paleozoic carbonates. The record extends from similar to 10 to 58?ka. On-board logging revealed a complex series of lithofacies, including buff-colored detrital carbonate-rich sediments [Heinrich (H)-events] frequently bracketed by black facies. We investigate the provenance of these facies using quantitative X-ray diffraction on drill-core samples from Paleozoic and Cretaceous bedrock from the SE Baffin Island Shelf, and on the?<?2-mm sediment fraction in a transect of five cores from Cumberland Sound to the NW Labrador Sea. A sediment unmixing program was used to discriminate between sediment sources, which included dolomite-rich sediments from Baffin Bay, calcite-rich sediments from Hudson Strait and discrete sources from Cumberland Sound. Results indicated that the bulk of the sediment was derived from Cumberland Sound, but Baffin Bay contributed to sediments coeval with H-0 (Younger Dryas), whereas Hudson Strait was the source during H-events 14. Contributions from the Cretaceous outcrops within Cumberland Sound bracket H-events, thus both leading and lagging Hudson Strait-sourced H-events. Article in Journal/Newspaper Baffin Bay Baffin Bay Baffin Island Baffin Cumberland Sound Hudson Strait Ice Sheet Labrador Sea Archimer (Archive Institutionnelle de l'Ifremer - Institut français de recherche pour l'exploitation de la mer) Baffin Bay Baffin Island Buff ENVELOPE(-64.567,-64.567,-64.833,-64.833) Cumberland Sound ENVELOPE(-66.014,-66.014,65.334,65.334) Hudson Hudson Strait ENVELOPE(-70.000,-70.000,62.000,62.000) Journal of Quaternary Science 27 5 475 484 |
institution |
Open Polar |
collection |
Archimer (Archive Institutionnelle de l'Ifremer - Institut français de recherche pour l'exploitation de la mer) |
op_collection_id |
ftarchimer |
language |
English |
topic |
Baffin Bay detrital carbonate (DC-) events Heinrich events Labrador Sea Laurentide Ice Sheet |
spellingShingle |
Baffin Bay detrital carbonate (DC-) events Heinrich events Labrador Sea Laurentide Ice Sheet Andrews, J. T. Barber, D. C. Jennings, A. E. Eberl, D. D. Maclean, B. Kirby, M. E. Stoner, J. S. Varying sediment sources (Hudson Strait, Cumberland Sound, Baffin Bay) to the NW Labrador Sea slope between and during Heinrich events 0 to 4 |
topic_facet |
Baffin Bay detrital carbonate (DC-) events Heinrich events Labrador Sea Laurentide Ice Sheet |
description |
Core HU97048-007PC was recovered from the continental Labrador Sea slope at a water depth of 945?m, 250?km seaward from the mouth of Cumberland Sound, and 400?km north of Hudson Strait. Cumberland Sound is a structural trough partly floored by Cretaceous mudstones and Paleozoic carbonates. The record extends from similar to 10 to 58?ka. On-board logging revealed a complex series of lithofacies, including buff-colored detrital carbonate-rich sediments [Heinrich (H)-events] frequently bracketed by black facies. We investigate the provenance of these facies using quantitative X-ray diffraction on drill-core samples from Paleozoic and Cretaceous bedrock from the SE Baffin Island Shelf, and on the?<?2-mm sediment fraction in a transect of five cores from Cumberland Sound to the NW Labrador Sea. A sediment unmixing program was used to discriminate between sediment sources, which included dolomite-rich sediments from Baffin Bay, calcite-rich sediments from Hudson Strait and discrete sources from Cumberland Sound. Results indicated that the bulk of the sediment was derived from Cumberland Sound, but Baffin Bay contributed to sediments coeval with H-0 (Younger Dryas), whereas Hudson Strait was the source during H-events 14. Contributions from the Cretaceous outcrops within Cumberland Sound bracket H-events, thus both leading and lagging Hudson Strait-sourced H-events. |
format |
Article in Journal/Newspaper |
author |
Andrews, J. T. Barber, D. C. Jennings, A. E. Eberl, D. D. Maclean, B. Kirby, M. E. Stoner, J. S. |
author_facet |
Andrews, J. T. Barber, D. C. Jennings, A. E. Eberl, D. D. Maclean, B. Kirby, M. E. Stoner, J. S. |
author_sort |
Andrews, J. T. |
title |
Varying sediment sources (Hudson Strait, Cumberland Sound, Baffin Bay) to the NW Labrador Sea slope between and during Heinrich events 0 to 4 |
title_short |
Varying sediment sources (Hudson Strait, Cumberland Sound, Baffin Bay) to the NW Labrador Sea slope between and during Heinrich events 0 to 4 |
title_full |
Varying sediment sources (Hudson Strait, Cumberland Sound, Baffin Bay) to the NW Labrador Sea slope between and during Heinrich events 0 to 4 |
title_fullStr |
Varying sediment sources (Hudson Strait, Cumberland Sound, Baffin Bay) to the NW Labrador Sea slope between and during Heinrich events 0 to 4 |
title_full_unstemmed |
Varying sediment sources (Hudson Strait, Cumberland Sound, Baffin Bay) to the NW Labrador Sea slope between and during Heinrich events 0 to 4 |
title_sort |
varying sediment sources (hudson strait, cumberland sound, baffin bay) to the nw labrador sea slope between and during heinrich events 0 to 4 |
publisher |
Wiley-blackwell |
publishDate |
2012 |
url |
https://archimer.ifremer.fr/doc/00265/37644/35823.pdf https://doi.org/10.1002/jqs.2535 https://archimer.ifremer.fr/doc/00265/37644/ |
long_lat |
ENVELOPE(-64.567,-64.567,-64.833,-64.833) ENVELOPE(-66.014,-66.014,65.334,65.334) ENVELOPE(-70.000,-70.000,62.000,62.000) |
geographic |
Baffin Bay Baffin Island Buff Cumberland Sound Hudson Hudson Strait |
geographic_facet |
Baffin Bay Baffin Island Buff Cumberland Sound Hudson Hudson Strait |
genre |
Baffin Bay Baffin Bay Baffin Island Baffin Cumberland Sound Hudson Strait Ice Sheet Labrador Sea |
genre_facet |
Baffin Bay Baffin Bay Baffin Island Baffin Cumberland Sound Hudson Strait Ice Sheet Labrador Sea |
op_source |
Journal Of Quaternary Science (0267-8179) (Wiley-blackwell), 2012-07 , Vol. 27 , N. 5 , P. 475-484 |
op_relation |
https://archimer.ifremer.fr/doc/00265/37644/35823.pdf doi:10.1002/jqs.2535 https://archimer.ifremer.fr/doc/00265/37644/ |
op_rights |
2012 John Wiley & Sons, Ltd. info:eu-repo/semantics/openAccess restricted use |
op_doi |
https://doi.org/10.1002/jqs.2535 |
container_title |
Journal of Quaternary Science |
container_volume |
27 |
container_issue |
5 |
container_start_page |
475 |
op_container_end_page |
484 |
_version_ |
1766365220733714432 |