Were last glacial climate events simultaneous between Greenland and France? A quantitative comparison using non‐tuned chronologies

Abstract Several large abrupt climate fluctuations during the last glacial have been recorded in Greenland ice cores and archives from other regions. Often these Dansgaard–Oeschger events are assumed to have been synchronous over wide areas, and then used as tie‐points to link chronologies between t...

Full description

Bibliographic Details
Published in:Journal of Quaternary Science
Main Authors: Blaauw, Maarten, Wohlfarth, Barbara, Christen, J. Andrés, Ampel, Linda, Veres, Daniel, Hughen, Konrad A., Preusser, Frank, Svensson, Anders
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 2009
Subjects:
Online Access:http://dx.doi.org/10.1002/jqs.1330
https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fjqs.1330
https://onlinelibrary.wiley.com/doi/pdf/10.1002/jqs.1330
id crwiley:10.1002/jqs.1330
record_format openpolar
spelling crwiley:10.1002/jqs.1330 2024-10-13T14:06:48+00:00 Were last glacial climate events simultaneous between Greenland and France? A quantitative comparison using non‐tuned chronologies Blaauw, Maarten Wohlfarth, Barbara Christen, J. Andrés Ampel, Linda Veres, Daniel Hughen, Konrad A. Preusser, Frank Svensson, Anders 2009 http://dx.doi.org/10.1002/jqs.1330 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fjqs.1330 https://onlinelibrary.wiley.com/doi/pdf/10.1002/jqs.1330 en eng Wiley http://onlinelibrary.wiley.com/termsAndConditions#vor Journal of Quaternary Science volume 25, issue 3, page 387-394 ISSN 0267-8179 1099-1417 journal-article 2009 crwiley https://doi.org/10.1002/jqs.1330 2024-09-17T04:51:30Z Abstract Several large abrupt climate fluctuations during the last glacial have been recorded in Greenland ice cores and archives from other regions. Often these Dansgaard–Oeschger events are assumed to have been synchronous over wide areas, and then used as tie‐points to link chronologies between the proxy archives. However, it has not yet been tested independently whether or not these events were indeed synchronous over large areas. Here, we compare Dansgaard–Oeschger‐type events in a well‐dated record from southeastern France with those in Greenland ice cores. Instead of assuming simultaneous climate events between both archives, we keep their age models independent. Even these well‐dated archives possess large chronological uncertainties that prevent us from inferring synchronous climate events at decadal to multi‐centennial time scales. If possible, comparisons between proxy archives should be based on independent, non‐tuned time‐scales. Copyright © 2009 John Wiley & Sons, Ltd. Article in Journal/Newspaper Dansgaard-Oeschger events Greenland Greenland ice cores Wiley Online Library Greenland Journal of Quaternary Science 25 3 387 394
institution Open Polar
collection Wiley Online Library
op_collection_id crwiley
language English
description Abstract Several large abrupt climate fluctuations during the last glacial have been recorded in Greenland ice cores and archives from other regions. Often these Dansgaard–Oeschger events are assumed to have been synchronous over wide areas, and then used as tie‐points to link chronologies between the proxy archives. However, it has not yet been tested independently whether or not these events were indeed synchronous over large areas. Here, we compare Dansgaard–Oeschger‐type events in a well‐dated record from southeastern France with those in Greenland ice cores. Instead of assuming simultaneous climate events between both archives, we keep their age models independent. Even these well‐dated archives possess large chronological uncertainties that prevent us from inferring synchronous climate events at decadal to multi‐centennial time scales. If possible, comparisons between proxy archives should be based on independent, non‐tuned time‐scales. Copyright © 2009 John Wiley & Sons, Ltd.
format Article in Journal/Newspaper
author Blaauw, Maarten
Wohlfarth, Barbara
Christen, J. Andrés
Ampel, Linda
Veres, Daniel
Hughen, Konrad A.
Preusser, Frank
Svensson, Anders
spellingShingle Blaauw, Maarten
Wohlfarth, Barbara
Christen, J. Andrés
Ampel, Linda
Veres, Daniel
Hughen, Konrad A.
Preusser, Frank
Svensson, Anders
Were last glacial climate events simultaneous between Greenland and France? A quantitative comparison using non‐tuned chronologies
author_facet Blaauw, Maarten
Wohlfarth, Barbara
Christen, J. Andrés
Ampel, Linda
Veres, Daniel
Hughen, Konrad A.
Preusser, Frank
Svensson, Anders
author_sort Blaauw, Maarten
title Were last glacial climate events simultaneous between Greenland and France? A quantitative comparison using non‐tuned chronologies
title_short Were last glacial climate events simultaneous between Greenland and France? A quantitative comparison using non‐tuned chronologies
title_full Were last glacial climate events simultaneous between Greenland and France? A quantitative comparison using non‐tuned chronologies
title_fullStr Were last glacial climate events simultaneous between Greenland and France? A quantitative comparison using non‐tuned chronologies
title_full_unstemmed Were last glacial climate events simultaneous between Greenland and France? A quantitative comparison using non‐tuned chronologies
title_sort were last glacial climate events simultaneous between greenland and france? a quantitative comparison using non‐tuned chronologies
publisher Wiley
publishDate 2009
url http://dx.doi.org/10.1002/jqs.1330
https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fjqs.1330
https://onlinelibrary.wiley.com/doi/pdf/10.1002/jqs.1330
geographic Greenland
geographic_facet Greenland
genre Dansgaard-Oeschger events
Greenland
Greenland ice cores
genre_facet Dansgaard-Oeschger events
Greenland
Greenland ice cores
op_source Journal of Quaternary Science
volume 25, issue 3, page 387-394
ISSN 0267-8179 1099-1417
op_rights http://onlinelibrary.wiley.com/termsAndConditions#vor
op_doi https://doi.org/10.1002/jqs.1330
container_title Journal of Quaternary Science
container_volume 25
container_issue 3
container_start_page 387
op_container_end_page 394
_version_ 1812813021180854272