The Younger Dryas cold event - was it synchronous over the North Atlantic region?
Determined independently from annually laminated ice cores and lake sediments, and German pines, the calendar ages of Younger Dryas (YD) boundaries significantly disagree with one another. 14C dates, plotted vs. calendar ages for samples from different sediments, also reveal distinct offsets. The ad...
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ftunivarizonaojs:oai:journals.uair.arizona.edu:article/1647 2023-05-15T15:02:41+02:00 The Younger Dryas cold event - was it synchronous over the North Atlantic region? Goslar, Tomasz Arnold, Maurice Pazdur, Mieczyslaw F 1995-01-01 application/pdf https://journals.uair.arizona.edu/index.php/radiocarbon/article/view/1647 eng eng Radiocarbon https://journals.uair.arizona.edu/index.php/radiocarbon/article/view/1647/1651 https://journals.uair.arizona.edu/index.php/radiocarbon/article/view/1647 Radiocarbon; Vol 37, No 1 (1995); 63-70 0033-8222 climate;Lake Holzmaar;Lake Soppensee;Poland;Lake Gosciaz;lacustrine environment;Arctic region;Greenland;ice cores;planar bedding structures;sedimentary structures;varves;upper Weichselian;Weichselian;Younger Dryas;Atlantic Ocean;North Atlantic;Germany;Central Europe;Pleistocene;upper Pleistocene;time scales;Europe;sediments;Cenozoic;Quaternary;C 14;carbon;dates;isotopes;radioactive isotopes;absolute age info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion Peer-reviewed Article 1995 ftunivarizonaojs 2020-11-14T17:53:01Z Determined independently from annually laminated ice cores and lake sediments, and German pines, the calendar ages of Younger Dryas (YD) boundaries significantly disagree with one another. 14C dates, plotted vs. calendar ages for samples from different sediments, also reveal distinct offsets. The adjustment of varve chronologies to synchronize the boundaries of the YD nearly cancels the discrepancies between 14C data, and supports the synchronism of the YD cold period over the North Atlantic region. However, the exact timing of the event cannot be estimated in this way. Article in Journal/Newspaper Arctic Greenland Greenland ice cores North Atlantic Journals at the University of Arizona Arctic Greenland |
institution |
Open Polar |
collection |
Journals at the University of Arizona |
op_collection_id |
ftunivarizonaojs |
language |
English |
topic |
climate;Lake Holzmaar;Lake Soppensee;Poland;Lake Gosciaz;lacustrine environment;Arctic region;Greenland;ice cores;planar bedding structures;sedimentary structures;varves;upper Weichselian;Weichselian;Younger Dryas;Atlantic Ocean;North Atlantic;Germany;Central Europe;Pleistocene;upper Pleistocene;time scales;Europe;sediments;Cenozoic;Quaternary;C 14;carbon;dates;isotopes;radioactive isotopes;absolute age |
spellingShingle |
climate;Lake Holzmaar;Lake Soppensee;Poland;Lake Gosciaz;lacustrine environment;Arctic region;Greenland;ice cores;planar bedding structures;sedimentary structures;varves;upper Weichselian;Weichselian;Younger Dryas;Atlantic Ocean;North Atlantic;Germany;Central Europe;Pleistocene;upper Pleistocene;time scales;Europe;sediments;Cenozoic;Quaternary;C 14;carbon;dates;isotopes;radioactive isotopes;absolute age Goslar, Tomasz Arnold, Maurice Pazdur, Mieczyslaw F The Younger Dryas cold event - was it synchronous over the North Atlantic region? |
topic_facet |
climate;Lake Holzmaar;Lake Soppensee;Poland;Lake Gosciaz;lacustrine environment;Arctic region;Greenland;ice cores;planar bedding structures;sedimentary structures;varves;upper Weichselian;Weichselian;Younger Dryas;Atlantic Ocean;North Atlantic;Germany;Central Europe;Pleistocene;upper Pleistocene;time scales;Europe;sediments;Cenozoic;Quaternary;C 14;carbon;dates;isotopes;radioactive isotopes;absolute age |
description |
Determined independently from annually laminated ice cores and lake sediments, and German pines, the calendar ages of Younger Dryas (YD) boundaries significantly disagree with one another. 14C dates, plotted vs. calendar ages for samples from different sediments, also reveal distinct offsets. The adjustment of varve chronologies to synchronize the boundaries of the YD nearly cancels the discrepancies between 14C data, and supports the synchronism of the YD cold period over the North Atlantic region. However, the exact timing of the event cannot be estimated in this way. |
format |
Article in Journal/Newspaper |
author |
Goslar, Tomasz Arnold, Maurice Pazdur, Mieczyslaw F |
author_facet |
Goslar, Tomasz Arnold, Maurice Pazdur, Mieczyslaw F |
author_sort |
Goslar, Tomasz |
title |
The Younger Dryas cold event - was it synchronous over the North Atlantic region? |
title_short |
The Younger Dryas cold event - was it synchronous over the North Atlantic region? |
title_full |
The Younger Dryas cold event - was it synchronous over the North Atlantic region? |
title_fullStr |
The Younger Dryas cold event - was it synchronous over the North Atlantic region? |
title_full_unstemmed |
The Younger Dryas cold event - was it synchronous over the North Atlantic region? |
title_sort |
younger dryas cold event - was it synchronous over the north atlantic region? |
publisher |
Radiocarbon |
publishDate |
1995 |
url |
https://journals.uair.arizona.edu/index.php/radiocarbon/article/view/1647 |
geographic |
Arctic Greenland |
geographic_facet |
Arctic Greenland |
genre |
Arctic Greenland Greenland ice cores North Atlantic |
genre_facet |
Arctic Greenland Greenland ice cores North Atlantic |
op_source |
Radiocarbon; Vol 37, No 1 (1995); 63-70 0033-8222 |
op_relation |
https://journals.uair.arizona.edu/index.php/radiocarbon/article/view/1647/1651 https://journals.uair.arizona.edu/index.php/radiocarbon/article/view/1647 |
_version_ |
1766334604081364992 |