Geochemical and isotopic tracers of Arctic sea ice sources and export with special attention to the Younger Dryas interval

Radiogenic isotopes (Sr, Nd) in Ice Rafted Debris (IRD) sediments from the Lomonosov Ridge and Fram Strait Arctic areas are used to document changes in Arctic sea-ice sources and trajectories since the Last Glacial Maximum (LGM). The two records provide evidence for enhanced sea-ice production in th...

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Published in:Quaternary Science Reviews
Main Authors: Maccali, Jenny, Not, Christelle, Poirier, André, Hillaire-Marcel, Claude
Format: Article in Journal/Newspaper
Language:English
Published: 2013
Subjects:
Online Access:https://doi.org/10.1016/j.quascirev.2013.05.001
http://hdl.handle.net/10722/210089
id ftunivhongkonghu:oai:hub.hku.hk:10722/210089
record_format openpolar
spelling ftunivhongkonghu:oai:hub.hku.hk:10722/210089 2023-05-15T14:40:07+02:00 Geochemical and isotopic tracers of Arctic sea ice sources and export with special attention to the Younger Dryas interval Maccali, Jenny Not, Christelle Poirier, André Hillaire-Marcel, Claude 2013 https://doi.org/10.1016/j.quascirev.2013.05.001 http://hdl.handle.net/10722/210089 eng eng Quaternary Science Reviews Quaternary Science Reviews, 2013, v. 79, p. 184-190 doi:10.1016/j.quascirev.2013.05.001 190 0277-3791 eid_2-s2.0-84885950691 184 http://hdl.handle.net/10722/210089 79 Meltwater Sea-ice Younger Dryas Isotopes Arctic Article 2013 ftunivhongkonghu https://doi.org/10.1016/j.quascirev.2013.05.001 2023-01-14T16:06:40Z Radiogenic isotopes (Sr, Nd) in Ice Rafted Debris (IRD) sediments from the Lomonosov Ridge and Fram Strait Arctic areas are used to document changes in Arctic sea-ice sources and trajectories since the Last Glacial Maximum (LGM). The two records provide evidence for enhanced sea-ice production in the Beaufort Sea and its subsequent export through Fram Strait during the Younger Dryas (YD) interval. This pattern, exclusive to the YD, followed an LGM-Bølling-Allerød interval, when multiyear and/or reduced sea-ice mobility resulted in sedimentary hiatuses in the Central Arctic. Meanwhile, IRD from Svalbard-Barents ice-sheet margin source were still deposited in the Fram Strait area. The "isotopic excursion" of the YD points to enhanced sea-ice production in the Beaufort Sea, which we link to the Lake Agassiz (?)/Laurentide ice sheet drainage event through the Mackenzie route. Following this event, the Holocene depicts a 5-fold reduction in IRD rates with a shift towards prominent sea-ice production along Russian shelves. From a methodological viewpoint, we demonstrate that radiogenic isotopes must be used in a multi-proxy approach to better constrain IRD and sea-ice sources and routes. From a paleoceanographic perspective, we conclude that an Arctic freshwater/sea-ice export route should now be seen as the most likely mechanism for an AMOC reduction during the YD in accordance with more recent improved model experiment. © 2013 Elsevier Ltd. Link_to_subscribed_fulltext Article in Journal/Newspaper Arctic Beaufort Sea Fram Strait Ice Sheet Lomonosov Ridge Sea ice Svalbard University of Hong Kong: HKU Scholars Hub Arctic Svalbard Quaternary Science Reviews 79 184 190
institution Open Polar
collection University of Hong Kong: HKU Scholars Hub
op_collection_id ftunivhongkonghu
language English
topic Meltwater
Sea-ice
Younger Dryas
Isotopes
Arctic
spellingShingle Meltwater
Sea-ice
Younger Dryas
Isotopes
Arctic
Maccali, Jenny
Not, Christelle
Poirier, André
Hillaire-Marcel, Claude
Geochemical and isotopic tracers of Arctic sea ice sources and export with special attention to the Younger Dryas interval
topic_facet Meltwater
Sea-ice
Younger Dryas
Isotopes
Arctic
description Radiogenic isotopes (Sr, Nd) in Ice Rafted Debris (IRD) sediments from the Lomonosov Ridge and Fram Strait Arctic areas are used to document changes in Arctic sea-ice sources and trajectories since the Last Glacial Maximum (LGM). The two records provide evidence for enhanced sea-ice production in the Beaufort Sea and its subsequent export through Fram Strait during the Younger Dryas (YD) interval. This pattern, exclusive to the YD, followed an LGM-Bølling-Allerød interval, when multiyear and/or reduced sea-ice mobility resulted in sedimentary hiatuses in the Central Arctic. Meanwhile, IRD from Svalbard-Barents ice-sheet margin source were still deposited in the Fram Strait area. The "isotopic excursion" of the YD points to enhanced sea-ice production in the Beaufort Sea, which we link to the Lake Agassiz (?)/Laurentide ice sheet drainage event through the Mackenzie route. Following this event, the Holocene depicts a 5-fold reduction in IRD rates with a shift towards prominent sea-ice production along Russian shelves. From a methodological viewpoint, we demonstrate that radiogenic isotopes must be used in a multi-proxy approach to better constrain IRD and sea-ice sources and routes. From a paleoceanographic perspective, we conclude that an Arctic freshwater/sea-ice export route should now be seen as the most likely mechanism for an AMOC reduction during the YD in accordance with more recent improved model experiment. © 2013 Elsevier Ltd. Link_to_subscribed_fulltext
format Article in Journal/Newspaper
author Maccali, Jenny
Not, Christelle
Poirier, André
Hillaire-Marcel, Claude
author_facet Maccali, Jenny
Not, Christelle
Poirier, André
Hillaire-Marcel, Claude
author_sort Maccali, Jenny
title Geochemical and isotopic tracers of Arctic sea ice sources and export with special attention to the Younger Dryas interval
title_short Geochemical and isotopic tracers of Arctic sea ice sources and export with special attention to the Younger Dryas interval
title_full Geochemical and isotopic tracers of Arctic sea ice sources and export with special attention to the Younger Dryas interval
title_fullStr Geochemical and isotopic tracers of Arctic sea ice sources and export with special attention to the Younger Dryas interval
title_full_unstemmed Geochemical and isotopic tracers of Arctic sea ice sources and export with special attention to the Younger Dryas interval
title_sort geochemical and isotopic tracers of arctic sea ice sources and export with special attention to the younger dryas interval
publishDate 2013
url https://doi.org/10.1016/j.quascirev.2013.05.001
http://hdl.handle.net/10722/210089
geographic Arctic
Svalbard
geographic_facet Arctic
Svalbard
genre Arctic
Beaufort Sea
Fram Strait
Ice Sheet
Lomonosov Ridge
Sea ice
Svalbard
genre_facet Arctic
Beaufort Sea
Fram Strait
Ice Sheet
Lomonosov Ridge
Sea ice
Svalbard
op_relation Quaternary Science Reviews
Quaternary Science Reviews, 2013, v. 79, p. 184-190
doi:10.1016/j.quascirev.2013.05.001
190
0277-3791
eid_2-s2.0-84885950691
184
http://hdl.handle.net/10722/210089
79
op_doi https://doi.org/10.1016/j.quascirev.2013.05.001
container_title Quaternary Science Reviews
container_volume 79
container_start_page 184
op_container_end_page 190
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