Changes in bottom water corrosiveness and carbonate ion concentrations in the sub-Antarctic Atlantic during the last glacial period

The glacial climate system transitioned rapidly between cold (stadial) and warm (interstadial) conditions in the Northern Hemisphere. This variability, referred to as Dansgaard-Oeschger variability, is widely believed to arise from perturbations of the Atlantic Meridional Overturning Circulation. Ev...

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Main Authors: Gottschalk, Julia, Skinner, Luke C, Misra, Sambuddha, Waelbroeck, Claire, Menviel, Laurie, Timmermann, Axel
Format: Other/Unknown Material
Language:English
Published: PANGAEA 2015
Subjects:
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.841244
https://doi.org/10.1594/PANGAEA.841244
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spelling ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.841244 2024-09-15T17:43:16+00:00 Changes in bottom water corrosiveness and carbonate ion concentrations in the sub-Antarctic Atlantic during the last glacial period Gottschalk, Julia Skinner, Luke C Misra, Sambuddha Waelbroeck, Claire Menviel, Laurie Timmermann, Axel LATITUDE: -44.153330 * LONGITUDE: -14.228170 2015 application/zip, 4 datasets https://doi.pangaea.de/10.1594/PANGAEA.841244 https://doi.org/10.1594/PANGAEA.841244 en eng PANGAEA https://doi.pangaea.de/10.1594/PANGAEA.841244 https://doi.org/10.1594/PANGAEA.841244 CC-BY-3.0: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted info:eu-repo/semantics/openAccess Supplement to: Gottschalk, Julia; Skinner, Luke C; Misra, Sambuddha; Waelbroeck, Claire; Menviel, Laurie; Timmermann, Axel (2015): Abrupt changes in the southern extent of North Atlantic Deep Water during Dansgaard–Oeschger events. Nature Geoscience, 8(12), 950-954, https://doi.org/10.1038/ngeo2558 Calypso Square Core System CASQS IMAGES XV - Pachiderme Marion Dufresne (1995) MD07-3076 MD07-3076Q MD159 dataset publication series 2015 ftpangaea https://doi.org/10.1594/PANGAEA.84124410.1038/ngeo2558 2024-07-24T02:31:21Z The glacial climate system transitioned rapidly between cold (stadial) and warm (interstadial) conditions in the Northern Hemisphere. This variability, referred to as Dansgaard-Oeschger variability, is widely believed to arise from perturbations of the Atlantic Meridional Overturning Circulation. Evidence for such changes during the longer Heinrich stadials has been identified, but direct evidence for overturning circulation changes during Dansgaard-Oeschger events has proven elusive. Here we reconstruct bottom water [CO3]2- variability from B/Ca ratios of benthic foraminifera and indicators of sedimentary dissolution, and use these reconstructions to infer the flow of northern-sourced deep water to the deep central sub-Antarctic Atlantic Ocean. We find that nearly every Dansgaard-Oeschger interstadial is accompanied by a rapid incursion of North Atlantic Deep Water into the deep South Atlantic. Based on these results and transient climate model simulations, we conclude that North Atlantic stadial-interstadial climate variability was associated with significant Atlantic overturning circulation changes that were rapidly transmitted across the Atlantic. However, by demonstrating the persistent role of Atlantic overturning circulation changes in past abrupt climate variability, our reconstructions of carbonate chemistry further indicate that the carbon cycle response to abrupt climate change was not a simple function of North Atlantic overturning. Other/Unknown Material Antarc* Antarctic Dansgaard-Oeschger events North Atlantic Deep Water North Atlantic PANGAEA - Data Publisher for Earth & Environmental Science ENVELOPE(-14.228170,-14.228170,-44.153330,-44.153330)
institution Open Polar
collection PANGAEA - Data Publisher for Earth & Environmental Science
op_collection_id ftpangaea
language English
topic Calypso Square Core System
CASQS
IMAGES XV - Pachiderme
Marion Dufresne (1995)
MD07-3076
MD07-3076Q
MD159
spellingShingle Calypso Square Core System
CASQS
IMAGES XV - Pachiderme
Marion Dufresne (1995)
MD07-3076
MD07-3076Q
MD159
Gottschalk, Julia
Skinner, Luke C
Misra, Sambuddha
Waelbroeck, Claire
Menviel, Laurie
Timmermann, Axel
Changes in bottom water corrosiveness and carbonate ion concentrations in the sub-Antarctic Atlantic during the last glacial period
topic_facet Calypso Square Core System
CASQS
IMAGES XV - Pachiderme
Marion Dufresne (1995)
MD07-3076
MD07-3076Q
MD159
description The glacial climate system transitioned rapidly between cold (stadial) and warm (interstadial) conditions in the Northern Hemisphere. This variability, referred to as Dansgaard-Oeschger variability, is widely believed to arise from perturbations of the Atlantic Meridional Overturning Circulation. Evidence for such changes during the longer Heinrich stadials has been identified, but direct evidence for overturning circulation changes during Dansgaard-Oeschger events has proven elusive. Here we reconstruct bottom water [CO3]2- variability from B/Ca ratios of benthic foraminifera and indicators of sedimentary dissolution, and use these reconstructions to infer the flow of northern-sourced deep water to the deep central sub-Antarctic Atlantic Ocean. We find that nearly every Dansgaard-Oeschger interstadial is accompanied by a rapid incursion of North Atlantic Deep Water into the deep South Atlantic. Based on these results and transient climate model simulations, we conclude that North Atlantic stadial-interstadial climate variability was associated with significant Atlantic overturning circulation changes that were rapidly transmitted across the Atlantic. However, by demonstrating the persistent role of Atlantic overturning circulation changes in past abrupt climate variability, our reconstructions of carbonate chemistry further indicate that the carbon cycle response to abrupt climate change was not a simple function of North Atlantic overturning.
format Other/Unknown Material
author Gottschalk, Julia
Skinner, Luke C
Misra, Sambuddha
Waelbroeck, Claire
Menviel, Laurie
Timmermann, Axel
author_facet Gottschalk, Julia
Skinner, Luke C
Misra, Sambuddha
Waelbroeck, Claire
Menviel, Laurie
Timmermann, Axel
author_sort Gottschalk, Julia
title Changes in bottom water corrosiveness and carbonate ion concentrations in the sub-Antarctic Atlantic during the last glacial period
title_short Changes in bottom water corrosiveness and carbonate ion concentrations in the sub-Antarctic Atlantic during the last glacial period
title_full Changes in bottom water corrosiveness and carbonate ion concentrations in the sub-Antarctic Atlantic during the last glacial period
title_fullStr Changes in bottom water corrosiveness and carbonate ion concentrations in the sub-Antarctic Atlantic during the last glacial period
title_full_unstemmed Changes in bottom water corrosiveness and carbonate ion concentrations in the sub-Antarctic Atlantic during the last glacial period
title_sort changes in bottom water corrosiveness and carbonate ion concentrations in the sub-antarctic atlantic during the last glacial period
publisher PANGAEA
publishDate 2015
url https://doi.pangaea.de/10.1594/PANGAEA.841244
https://doi.org/10.1594/PANGAEA.841244
op_coverage LATITUDE: -44.153330 * LONGITUDE: -14.228170
long_lat ENVELOPE(-14.228170,-14.228170,-44.153330,-44.153330)
genre Antarc*
Antarctic
Dansgaard-Oeschger events
North Atlantic Deep Water
North Atlantic
genre_facet Antarc*
Antarctic
Dansgaard-Oeschger events
North Atlantic Deep Water
North Atlantic
op_source Supplement to: Gottschalk, Julia; Skinner, Luke C; Misra, Sambuddha; Waelbroeck, Claire; Menviel, Laurie; Timmermann, Axel (2015): Abrupt changes in the southern extent of North Atlantic Deep Water during Dansgaard–Oeschger events. Nature Geoscience, 8(12), 950-954, https://doi.org/10.1038/ngeo2558
op_relation https://doi.pangaea.de/10.1594/PANGAEA.841244
https://doi.org/10.1594/PANGAEA.841244
op_rights CC-BY-3.0: Creative Commons Attribution 3.0 Unported
Access constraints: unrestricted
info:eu-repo/semantics/openAccess
op_doi https://doi.org/10.1594/PANGAEA.84124410.1038/ngeo2558
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