Tracking sediment delivery to central Baffin Bay during the past 40 kyrs: Insights from a multiproxy approach and new age model ...

Reconstructing former ice sheet history and glaciogenic sediment fluxes surrounding Baffin Bay during and since the Last Glacial Maximum (LGM) is a major scientific challenge. Here, a new multi-proxy analysis of sediments from a central Baffin Bay (BB) sediment core reveals two dominant sediment/dis...

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Main Authors: Ownsworth, Emma, Selby, David, Lloyd, Jeremy, Knutz, Paul, Szidat, Sönke, Andrews, John, Ó Cofaigh, Colm
Format: Text
Language:unknown
Published: Elsevier 2023
Subjects:
Online Access:https://dx.doi.org/10.48350/185160
https://boris.unibe.ch/185160/
id ftdatacite:10.48350/185160
record_format openpolar
spelling ftdatacite:10.48350/185160 2024-09-30T14:32:38+00:00 Tracking sediment delivery to central Baffin Bay during the past 40 kyrs: Insights from a multiproxy approach and new age model ... Ownsworth, Emma Selby, David Lloyd, Jeremy Knutz, Paul Szidat, Sönke Andrews, John Ó Cofaigh, Colm 2023 https://dx.doi.org/10.48350/185160 https://boris.unibe.ch/185160/ unknown Elsevier https://dx.doi.org/10.1016/j.quascirev.2023.108082 open access Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 http://purl.org/coar/access_right/c_abf2 570 Life sciences; biology 540 Chemistry Text ScholarlyArticle article-journal journal article 2023 ftdatacite https://doi.org/10.48350/18516010.1016/j.quascirev.2023.108082 2024-09-02T10:17:31Z Reconstructing former ice sheet history and glaciogenic sediment fluxes surrounding Baffin Bay during and since the Last Glacial Maximum (LGM) is a major scientific challenge. Here, a new multi-proxy analysis of sediments from a central Baffin Bay (BB) sediment core reveals two dominant sediment/discharge sources: 1) a detrital carbonate (BBDC; dolomite-rich) source that represents increased discharge from the NE Laurentide Ice Sheet (LIS) and southern Innuitian Ice Sheet (IIS), and 2) a radiogenic, felsic provenance likely from a west Greenland Ice Sheet (GIS) source, although a contribution from the Baffin Island LIS cannot be ruled out. By utilising a new method for radiocarbon calibration in high latitude polar environments we provide updated age constraints on BBDC1 (14.1e13 cal ka BP) and BBDC0 (12.0e10.9 cal ka BP). This coupled with our sediment analysis shows the BBDC layers to be coincident with the Bølling-Allerød (BBDC1) and the recovery from the Younger Dryas (BBDC0). The timing of BBDC1 also ... Text Baffin Bay Baffin Bay Baffin Island Baffin Greenland Ice Sheet DataCite Baffin Bay Baffin Island Greenland
institution Open Polar
collection DataCite
op_collection_id ftdatacite
language unknown
topic 570 Life sciences; biology
540 Chemistry
spellingShingle 570 Life sciences; biology
540 Chemistry
Ownsworth, Emma
Selby, David
Lloyd, Jeremy
Knutz, Paul
Szidat, Sönke
Andrews, John
Ó Cofaigh, Colm
Tracking sediment delivery to central Baffin Bay during the past 40 kyrs: Insights from a multiproxy approach and new age model ...
topic_facet 570 Life sciences; biology
540 Chemistry
description Reconstructing former ice sheet history and glaciogenic sediment fluxes surrounding Baffin Bay during and since the Last Glacial Maximum (LGM) is a major scientific challenge. Here, a new multi-proxy analysis of sediments from a central Baffin Bay (BB) sediment core reveals two dominant sediment/discharge sources: 1) a detrital carbonate (BBDC; dolomite-rich) source that represents increased discharge from the NE Laurentide Ice Sheet (LIS) and southern Innuitian Ice Sheet (IIS), and 2) a radiogenic, felsic provenance likely from a west Greenland Ice Sheet (GIS) source, although a contribution from the Baffin Island LIS cannot be ruled out. By utilising a new method for radiocarbon calibration in high latitude polar environments we provide updated age constraints on BBDC1 (14.1e13 cal ka BP) and BBDC0 (12.0e10.9 cal ka BP). This coupled with our sediment analysis shows the BBDC layers to be coincident with the Bølling-Allerød (BBDC1) and the recovery from the Younger Dryas (BBDC0). The timing of BBDC1 also ...
format Text
author Ownsworth, Emma
Selby, David
Lloyd, Jeremy
Knutz, Paul
Szidat, Sönke
Andrews, John
Ó Cofaigh, Colm
author_facet Ownsworth, Emma
Selby, David
Lloyd, Jeremy
Knutz, Paul
Szidat, Sönke
Andrews, John
Ó Cofaigh, Colm
author_sort Ownsworth, Emma
title Tracking sediment delivery to central Baffin Bay during the past 40 kyrs: Insights from a multiproxy approach and new age model ...
title_short Tracking sediment delivery to central Baffin Bay during the past 40 kyrs: Insights from a multiproxy approach and new age model ...
title_full Tracking sediment delivery to central Baffin Bay during the past 40 kyrs: Insights from a multiproxy approach and new age model ...
title_fullStr Tracking sediment delivery to central Baffin Bay during the past 40 kyrs: Insights from a multiproxy approach and new age model ...
title_full_unstemmed Tracking sediment delivery to central Baffin Bay during the past 40 kyrs: Insights from a multiproxy approach and new age model ...
title_sort tracking sediment delivery to central baffin bay during the past 40 kyrs: insights from a multiproxy approach and new age model ...
publisher Elsevier
publishDate 2023
url https://dx.doi.org/10.48350/185160
https://boris.unibe.ch/185160/
geographic Baffin Bay
Baffin Island
Greenland
geographic_facet Baffin Bay
Baffin Island
Greenland
genre Baffin Bay
Baffin Bay
Baffin Island
Baffin
Greenland
Ice Sheet
genre_facet Baffin Bay
Baffin Bay
Baffin Island
Baffin
Greenland
Ice Sheet
op_relation https://dx.doi.org/10.1016/j.quascirev.2023.108082
op_rights open access
Creative Commons Attribution 4.0 International
https://creativecommons.org/licenses/by/4.0/legalcode
cc-by-4.0
http://purl.org/coar/access_right/c_abf2
op_doi https://doi.org/10.48350/18516010.1016/j.quascirev.2023.108082
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