Active North Atlantic deepwater formation during Heinrich Stadial 1 ...
Deepwater circulation significantly changed during the last deglaciation from a shallow to a deep-reaching overturning cell. This change went along with a drawdown of isotopically light waters into the abyss and a deep ocean warming that changed deep ocean stratification from a salinity-to a tempera...
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Online Access: | https://dx.doi.org/10.3929/ethz-b-000505317 http://hdl.handle.net/20.500.11850/505317 |
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ftdatacite:10.3929/ethz-b-000505317 2024-09-30T14:37:23+00:00 Active North Atlantic deepwater formation during Heinrich Stadial 1 ... Repschläger, Janne Zhao, Ning Rand, Devin Lisiecki, Lorraine Muglia, Juan Mulitza, Stefan Schmittner, Andreas Cartapanis, Olivier Bauch, Henning A. Schiebel, Ralf Haug, Gerald H. 2021 application/pdf https://dx.doi.org/10.3929/ethz-b-000505317 http://hdl.handle.net/20.500.11850/505317 en eng ETH Zurich info:eu-repo/semantics/openAccess Creative Commons Attribution Non Commercial No Derivatives 4.0 International https://creativecommons.org/licenses/by-nc-nd/4.0/legalcode cc-by-nc-nd-4.0 Quaternary Paleoceanography North Atlantic Data compilation stable isotopes Text Journal Article ScholarlyArticle article-journal 2021 ftdatacite https://doi.org/10.3929/ethz-b-000505317 2024-09-02T07:54:09Z Deepwater circulation significantly changed during the last deglaciation from a shallow to a deep-reaching overturning cell. This change went along with a drawdown of isotopically light waters into the abyss and a deep ocean warming that changed deep ocean stratification from a salinity-to a temperature-controlled mode. Yet, the exact mechanisms causing these changes are still unknown. Furthermore, the long-standing idea of a complete shutdown of North Atlantic deepwater formation during Heinrich Stadial 1 (HS1) (17.5–14.6 kyr BP) remains prevalent. Here, we present a new compilation of benthic δ13C and δ18O data from the North Atlantic at high temporal resolution with consistent age models, established as part of the international PAGES working group OC3, to investigate deepwater properties in the North Atlantic. The extensive compilation, which includes 105 sediment cores, reveals different water masses during HS1. A water mass with heavy δ13C and δ18O signature occupies the Iceland Basin, whereas between ... : Quaternary Science Reviews, 270 ... Text Iceland North Atlantic DataCite |
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ftdatacite |
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English |
topic |
Quaternary Paleoceanography North Atlantic Data compilation stable isotopes |
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Quaternary Paleoceanography North Atlantic Data compilation stable isotopes Repschläger, Janne Zhao, Ning Rand, Devin Lisiecki, Lorraine Muglia, Juan Mulitza, Stefan Schmittner, Andreas Cartapanis, Olivier Bauch, Henning A. Schiebel, Ralf Haug, Gerald H. Active North Atlantic deepwater formation during Heinrich Stadial 1 ... |
topic_facet |
Quaternary Paleoceanography North Atlantic Data compilation stable isotopes |
description |
Deepwater circulation significantly changed during the last deglaciation from a shallow to a deep-reaching overturning cell. This change went along with a drawdown of isotopically light waters into the abyss and a deep ocean warming that changed deep ocean stratification from a salinity-to a temperature-controlled mode. Yet, the exact mechanisms causing these changes are still unknown. Furthermore, the long-standing idea of a complete shutdown of North Atlantic deepwater formation during Heinrich Stadial 1 (HS1) (17.5–14.6 kyr BP) remains prevalent. Here, we present a new compilation of benthic δ13C and δ18O data from the North Atlantic at high temporal resolution with consistent age models, established as part of the international PAGES working group OC3, to investigate deepwater properties in the North Atlantic. The extensive compilation, which includes 105 sediment cores, reveals different water masses during HS1. A water mass with heavy δ13C and δ18O signature occupies the Iceland Basin, whereas between ... : Quaternary Science Reviews, 270 ... |
format |
Text |
author |
Repschläger, Janne Zhao, Ning Rand, Devin Lisiecki, Lorraine Muglia, Juan Mulitza, Stefan Schmittner, Andreas Cartapanis, Olivier Bauch, Henning A. Schiebel, Ralf Haug, Gerald H. |
author_facet |
Repschläger, Janne Zhao, Ning Rand, Devin Lisiecki, Lorraine Muglia, Juan Mulitza, Stefan Schmittner, Andreas Cartapanis, Olivier Bauch, Henning A. Schiebel, Ralf Haug, Gerald H. |
author_sort |
Repschläger, Janne |
title |
Active North Atlantic deepwater formation during Heinrich Stadial 1 ... |
title_short |
Active North Atlantic deepwater formation during Heinrich Stadial 1 ... |
title_full |
Active North Atlantic deepwater formation during Heinrich Stadial 1 ... |
title_fullStr |
Active North Atlantic deepwater formation during Heinrich Stadial 1 ... |
title_full_unstemmed |
Active North Atlantic deepwater formation during Heinrich Stadial 1 ... |
title_sort |
active north atlantic deepwater formation during heinrich stadial 1 ... |
publisher |
ETH Zurich |
publishDate |
2021 |
url |
https://dx.doi.org/10.3929/ethz-b-000505317 http://hdl.handle.net/20.500.11850/505317 |
genre |
Iceland North Atlantic |
genre_facet |
Iceland North Atlantic |
op_rights |
info:eu-repo/semantics/openAccess Creative Commons Attribution Non Commercial No Derivatives 4.0 International https://creativecommons.org/licenses/by-nc-nd/4.0/legalcode cc-by-nc-nd-4.0 |
op_doi |
https://doi.org/10.3929/ethz-b-000505317 |
_version_ |
1811640238424981504 |