Tracing time in the ocean: a brief review of chronological constraints (60-8 kyr) on North Atlantic marine event-based stratigraphies

Well-resolved event-based stratigraphies in marine sediments spanning a significant portion of the last glacial period (60-8 kyr) provide a unique opportunity for time-stratigraphic correlation in the North Atlantic region. Here, we review the current methods available to chronologically constrain t...

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Published in:Quaternary Science Reviews
Main Authors: Austin, William E. N., Hibbert, Fiona D.
Format: Article in Journal/Newspaper
Language:English
Published: 2012
Subjects:
Online Access:https://research-portal.st-andrews.ac.uk/en/researchoutput/tracing-time-in-the-ocean-a-brief-review-of-chronological-constraints-608-kyr-on-north-atlantic-marine-eventbased-stratigraphies(985ed400-3fbe-4072-b190-e695f4acd0df).html
https://doi.org/10.1016/j.quascirev.2012.01.015
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spelling ftunstandrewcris:oai:research-portal.st-andrews.ac.uk:publications/985ed400-3fbe-4072-b190-e695f4acd0df 2024-06-23T07:53:22+00:00 Tracing time in the ocean: a brief review of chronological constraints (60-8 kyr) on North Atlantic marine event-based stratigraphies Austin, William E. N. Hibbert, Fiona D. 2012-03-12 https://research-portal.st-andrews.ac.uk/en/researchoutput/tracing-time-in-the-ocean-a-brief-review-of-chronological-constraints-608-kyr-on-north-atlantic-marine-eventbased-stratigraphies(985ed400-3fbe-4072-b190-e695f4acd0df).html https://doi.org/10.1016/j.quascirev.2012.01.015 eng eng https://research-portal.st-andrews.ac.uk/en/researchoutput/tracing-time-in-the-ocean-a-brief-review-of-chronological-constraints-608-kyr-on-north-atlantic-marine-eventbased-stratigraphies(985ed400-3fbe-4072-b190-e695f4acd0df).html info:eu-repo/semantics/restrictedAccess Austin , W E N & Hibbert , F D 2012 , ' Tracing time in the ocean: a brief review of chronological constraints (60-8 kyr) on North Atlantic marine event-based stratigraphies ' , Quaternary Science Reviews , vol. 36 , pp. 28-37 . https://doi.org/10.1016/j.quascirev.2012.01.015 article 2012 ftunstandrewcris https://doi.org/10.1016/j.quascirev.2012.01.015 2024-06-13T00:35:18Z Well-resolved event-based stratigraphies in marine sediments spanning a significant portion of the last glacial period (60-8 kyr) provide a unique opportunity for time-stratigraphic correlation in the North Atlantic region. Here, we review the current methods available to chronologically constrain these event-based stratigraphies, highlighting, in particular, the value of tephrochronology as an independent tool to validate correlations between records. While the INTIMATE protocols (Lowe et al., 2008; Blockley et al., 2011) are equally applicable to marine and terrestrial records, spatially and temporally variable marine radiocarbon reservoir age effects (MREs) provide a challenge to using marine radiocarbon in the former as an independent chronostratigraphic tool. Despite the inherent uncertainties associated with 'tuning', we conclude that the mid-points of the common abrupt warming transitions associated with the well-defined, millennial-scale climate oscillations (the Dansgaard-Oeschger (D/O) cycles) observed in the oxygen isotopes of the Greenland ice cores and North Atlantic sea surface temperature (SST) records currently provide the most robust correlation tie-points from which to derive age control. In this invited INTIMATE special issue article we propose a new protocol for establishing marine event-based chronostratigraphies in the North Atlantic region and focus on areas of chronological potential in palaeoceanographic research. (C) 2012 Elsevier Ltd. All rights reserved. Article in Journal/Newspaper Greenland Greenland ice cores North Atlantic University of St Andrews: Research Portal Greenland Lowe ENVELOPE(-30.309,-30.309,-80.537,-80.537) Quaternary Science Reviews 36 28 37
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language English
description Well-resolved event-based stratigraphies in marine sediments spanning a significant portion of the last glacial period (60-8 kyr) provide a unique opportunity for time-stratigraphic correlation in the North Atlantic region. Here, we review the current methods available to chronologically constrain these event-based stratigraphies, highlighting, in particular, the value of tephrochronology as an independent tool to validate correlations between records. While the INTIMATE protocols (Lowe et al., 2008; Blockley et al., 2011) are equally applicable to marine and terrestrial records, spatially and temporally variable marine radiocarbon reservoir age effects (MREs) provide a challenge to using marine radiocarbon in the former as an independent chronostratigraphic tool. Despite the inherent uncertainties associated with 'tuning', we conclude that the mid-points of the common abrupt warming transitions associated with the well-defined, millennial-scale climate oscillations (the Dansgaard-Oeschger (D/O) cycles) observed in the oxygen isotopes of the Greenland ice cores and North Atlantic sea surface temperature (SST) records currently provide the most robust correlation tie-points from which to derive age control. In this invited INTIMATE special issue article we propose a new protocol for establishing marine event-based chronostratigraphies in the North Atlantic region and focus on areas of chronological potential in palaeoceanographic research. (C) 2012 Elsevier Ltd. All rights reserved.
format Article in Journal/Newspaper
author Austin, William E. N.
Hibbert, Fiona D.
spellingShingle Austin, William E. N.
Hibbert, Fiona D.
Tracing time in the ocean: a brief review of chronological constraints (60-8 kyr) on North Atlantic marine event-based stratigraphies
author_facet Austin, William E. N.
Hibbert, Fiona D.
author_sort Austin, William E. N.
title Tracing time in the ocean: a brief review of chronological constraints (60-8 kyr) on North Atlantic marine event-based stratigraphies
title_short Tracing time in the ocean: a brief review of chronological constraints (60-8 kyr) on North Atlantic marine event-based stratigraphies
title_full Tracing time in the ocean: a brief review of chronological constraints (60-8 kyr) on North Atlantic marine event-based stratigraphies
title_fullStr Tracing time in the ocean: a brief review of chronological constraints (60-8 kyr) on North Atlantic marine event-based stratigraphies
title_full_unstemmed Tracing time in the ocean: a brief review of chronological constraints (60-8 kyr) on North Atlantic marine event-based stratigraphies
title_sort tracing time in the ocean: a brief review of chronological constraints (60-8 kyr) on north atlantic marine event-based stratigraphies
publishDate 2012
url https://research-portal.st-andrews.ac.uk/en/researchoutput/tracing-time-in-the-ocean-a-brief-review-of-chronological-constraints-608-kyr-on-north-atlantic-marine-eventbased-stratigraphies(985ed400-3fbe-4072-b190-e695f4acd0df).html
https://doi.org/10.1016/j.quascirev.2012.01.015
long_lat ENVELOPE(-30.309,-30.309,-80.537,-80.537)
geographic Greenland
Lowe
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genre Greenland
Greenland ice cores
North Atlantic
genre_facet Greenland
Greenland ice cores
North Atlantic
op_source Austin , W E N & Hibbert , F D 2012 , ' Tracing time in the ocean: a brief review of chronological constraints (60-8 kyr) on North Atlantic marine event-based stratigraphies ' , Quaternary Science Reviews , vol. 36 , pp. 28-37 . https://doi.org/10.1016/j.quascirev.2012.01.015
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