High resolution, multi-proxy analysis of the Younger Dryas Stadial section of Lake Suigetsu sediments
The Younger Dryas Stadial (YDS) was an episode of northern hemispheric cooling which occurred within the Last Glacial Interglacial Transition (LGIT). A major driver for the YDS climate was a weakening of the Atlantic Meridional Overturning Circulation (AMOC). It has been inferred that the AMOC began...
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ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.874228 2024-09-15T18:22:24+00:00 High resolution, multi-proxy analysis of the Younger Dryas Stadial section of Lake Suigetsu sediments Schlolaut, Gordon Brauer, Achim Nakagawa, Takeshi Lamb, Henry F Tyler, Jonathan James Staff, Richard A Marshall, Michael H Ramsey, Christopher Bronk Bryant, Charlotte L Tarasov, Pavel E LATITUDE: 35.583330 * LONGITUDE: 135.883330 2017 application/zip, 3 datasets https://doi.pangaea.de/10.1594/PANGAEA.874228 https://doi.org/10.1594/PANGAEA.874228 en eng PANGAEA https://doi.pangaea.de/10.1594/PANGAEA.874228 https://doi.org/10.1594/PANGAEA.874228 CC-BY-3.0: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted info:eu-repo/semantics/openAccess Supplement to: Schlolaut, Gordon; Brauer, Achim; Nakagawa, Takeshi; Lamb, Henry F; Tyler, Jonathan James; Staff, Richard A; Marshall, Michael H; Ramsey, Christopher Bronk; Bryant, Charlotte L; Tarasov, Pavel E (2017): Evidence for a bi-partition of the Younger Dryas Stadial in East Asia associated with inversed climate characteristics compared to Europe. Scientific Reports, 7, 44983, https://doi.org/10.1038/srep44983 Lake Suigetsu Honshu Japan PC-hp Piston corer hydro-pressure thin-walled SG06 dataset publication series 2017 ftpangaea https://doi.org/10.1594/PANGAEA.87422810.1038/srep44983 2024-07-24T02:31:21Z The Younger Dryas Stadial (YDS) was an episode of northern hemispheric cooling which occurred within the Last Glacial Interglacial Transition (LGIT). A major driver for the YDS climate was a weakening of the Atlantic Meridional Overturning Circulation (AMOC). It has been inferred that the AMOC began to strengthen mid-YDS, producing a bipartite structure of the YDS in records from continental Europe. These records imply that the polar front and westerlies shifted northward, producing a warmer second phase of the YDS in Europe. Here we present multi-proxy data from the sediments of Lake Suigetsu (Japan), as evidence that a related bi-partition of the YDS also occurred in East Asia. Besides showing for the first time that the bi-partition was not limited to the North Atlantic/European region, the data also imply a climatic dipole between Europe and East Asia since the cold-warm characteristics are reversed at Lake Suigetsu. We suggest that changes in eastward moisture transport from the North Atlantic are the primary mechanism by which the teleconnection can be explained. Other/Unknown Material North Atlantic PANGAEA - Data Publisher for Earth & Environmental Science ENVELOPE(135.883330,135.883330,35.583330,35.583330) |
institution |
Open Polar |
collection |
PANGAEA - Data Publisher for Earth & Environmental Science |
op_collection_id |
ftpangaea |
language |
English |
topic |
Lake Suigetsu Honshu Japan PC-hp Piston corer hydro-pressure thin-walled SG06 |
spellingShingle |
Lake Suigetsu Honshu Japan PC-hp Piston corer hydro-pressure thin-walled SG06 Schlolaut, Gordon Brauer, Achim Nakagawa, Takeshi Lamb, Henry F Tyler, Jonathan James Staff, Richard A Marshall, Michael H Ramsey, Christopher Bronk Bryant, Charlotte L Tarasov, Pavel E High resolution, multi-proxy analysis of the Younger Dryas Stadial section of Lake Suigetsu sediments |
topic_facet |
Lake Suigetsu Honshu Japan PC-hp Piston corer hydro-pressure thin-walled SG06 |
description |
The Younger Dryas Stadial (YDS) was an episode of northern hemispheric cooling which occurred within the Last Glacial Interglacial Transition (LGIT). A major driver for the YDS climate was a weakening of the Atlantic Meridional Overturning Circulation (AMOC). It has been inferred that the AMOC began to strengthen mid-YDS, producing a bipartite structure of the YDS in records from continental Europe. These records imply that the polar front and westerlies shifted northward, producing a warmer second phase of the YDS in Europe. Here we present multi-proxy data from the sediments of Lake Suigetsu (Japan), as evidence that a related bi-partition of the YDS also occurred in East Asia. Besides showing for the first time that the bi-partition was not limited to the North Atlantic/European region, the data also imply a climatic dipole between Europe and East Asia since the cold-warm characteristics are reversed at Lake Suigetsu. We suggest that changes in eastward moisture transport from the North Atlantic are the primary mechanism by which the teleconnection can be explained. |
format |
Other/Unknown Material |
author |
Schlolaut, Gordon Brauer, Achim Nakagawa, Takeshi Lamb, Henry F Tyler, Jonathan James Staff, Richard A Marshall, Michael H Ramsey, Christopher Bronk Bryant, Charlotte L Tarasov, Pavel E |
author_facet |
Schlolaut, Gordon Brauer, Achim Nakagawa, Takeshi Lamb, Henry F Tyler, Jonathan James Staff, Richard A Marshall, Michael H Ramsey, Christopher Bronk Bryant, Charlotte L Tarasov, Pavel E |
author_sort |
Schlolaut, Gordon |
title |
High resolution, multi-proxy analysis of the Younger Dryas Stadial section of Lake Suigetsu sediments |
title_short |
High resolution, multi-proxy analysis of the Younger Dryas Stadial section of Lake Suigetsu sediments |
title_full |
High resolution, multi-proxy analysis of the Younger Dryas Stadial section of Lake Suigetsu sediments |
title_fullStr |
High resolution, multi-proxy analysis of the Younger Dryas Stadial section of Lake Suigetsu sediments |
title_full_unstemmed |
High resolution, multi-proxy analysis of the Younger Dryas Stadial section of Lake Suigetsu sediments |
title_sort |
high resolution, multi-proxy analysis of the younger dryas stadial section of lake suigetsu sediments |
publisher |
PANGAEA |
publishDate |
2017 |
url |
https://doi.pangaea.de/10.1594/PANGAEA.874228 https://doi.org/10.1594/PANGAEA.874228 |
op_coverage |
LATITUDE: 35.583330 * LONGITUDE: 135.883330 |
long_lat |
ENVELOPE(135.883330,135.883330,35.583330,35.583330) |
genre |
North Atlantic |
genre_facet |
North Atlantic |
op_source |
Supplement to: Schlolaut, Gordon; Brauer, Achim; Nakagawa, Takeshi; Lamb, Henry F; Tyler, Jonathan James; Staff, Richard A; Marshall, Michael H; Ramsey, Christopher Bronk; Bryant, Charlotte L; Tarasov, Pavel E (2017): Evidence for a bi-partition of the Younger Dryas Stadial in East Asia associated with inversed climate characteristics compared to Europe. Scientific Reports, 7, 44983, https://doi.org/10.1038/srep44983 |
op_relation |
https://doi.pangaea.de/10.1594/PANGAEA.874228 https://doi.org/10.1594/PANGAEA.874228 |
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.87422810.1038/srep44983 |
_version_ |
1810462190584463360 |