Articles | Volume 11, issue 11
https://doi.org/10.5194/cp-11-1507-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/cp-11-1507-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Research article
| 
12 Nov 2015
Research article |
| 12 Nov 2015
Stratification of surface waters during the last glacial millennial climatic events: a key factor in subsurface and deep-water mass dynamics
UMR 5805, EPOC (Environnements et Paléoenvironnements Océaniques et Continentaux), Université de Bordeaux, 33615 Pessac, France
F. Eynaud
UMR 5805, EPOC (Environnements et Paléoenvironnements Océaniques et Continentaux), Université de Bordeaux, 33615 Pessac, France
M. Sabine
UMR 5805, EPOC (Environnements et Paléoenvironnements Océaniques et Continentaux), Université de Bordeaux, 33615 Pessac, France
S. Zaragosi
UMR 5805, EPOC (Environnements et Paléoenvironnements Océaniques et Continentaux), Université de Bordeaux, 33615 Pessac, France
L. Rossignol
UMR 5805, EPOC (Environnements et Paléoenvironnements Océaniques et Continentaux), Université de Bordeaux, 33615 Pessac, France
B. Malaizé
UMR 5805, EPOC (Environnements et Paléoenvironnements Océaniques et Continentaux), Université de Bordeaux, 33615 Pessac, France
E. Palis
UMR 5805, EPOC (Environnements et Paléoenvironnements Océaniques et Continentaux), Université de Bordeaux, 33615 Pessac, France
now at: UMR 7329, Géoazur, Université de Sophia Antipolis, 06560 Valbonne, France
J. Zumaque
UMR 5805, EPOC (Environnements et Paléoenvironnements Océaniques et Continentaux), Université de Bordeaux, 33615 Pessac, France
now at: UQAM, Université du Québec à Montreal, Montréal, Québec H3C 3P8, Canada
C. Caulle
UMR 5805, EPOC (Environnements et Paléoenvironnements Océaniques et Continentaux), Université de Bordeaux, 33615 Pessac, France
now at: Laboratoire Péagos, Département Dynamiques des écosystèmes côtiers, IFREMER Brest, Technopôle Brest Iroise, 29280 Plouzané, France
A. Penaud
UMR 6538, Domaines Océaniques, IUEM-UBO, 29280 Plouzané, France
E. Michel
UMR 8212, LSCE (Laboratoire des Sciences du Climat et de l'Environnement), CEA/CNRS-INSU/UVSQ, 91198 Gif-sur-Yvette CEDEX, France
K. Charlier
UMR 5805, EPOC (Environnements et Paléoenvironnements Océaniques et Continentaux), Université de Bordeaux, 33615 Pessac, France
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Cited
16 citations as recorded by crossref.
- Imprint of seasonality changes on fluvio-glacial dynamics across Heinrich Stadial 1 (NE Atlantic Ocean) W. Fersi et al. 10.1016/j.gloplacha.2021.103552
- Dinoflagellate fossils: Geological and biological applications A. Penaud et al. 10.1016/j.revmic.2018.09.003
- Western boundary current in relation to Atlantic Subtropical Gyre dynamics during abrupt glacial climate fluctuations D. Nürnberg et al. 10.1016/j.gloplacha.2021.103497
- Changes in the geometry and strength of the Atlantic meridional overturning circulation during the last glacial (20–50 ka) P. Burckel et al. 10.5194/cp-12-2061-2016
- Are Past Sea-Ice Reconstructions Based on Planktonic Foraminifera Realistic? Study of the Last 50 ka as a Test to Validate Reconstructed Paleohydrography Derived from Transfer Functions Applied to Their Fossil Assemblages F. Eynaud et al. 10.3390/geosciences11100409
- Millennial‐Scale Climate Variability and Dinoflagellate‐Cyst‐Based Seasonality Changes Over the Last ~150 kyrs at “Shackleton Site” U1385 M. Datema et al. 10.1029/2018PA003497
- The southern Norwegian Sea during the last 45 ka: hydrographical reorganizations under changing ice‐sheet dynamics M. Wary et al. 10.1002/jqs.2965
- Strong temperature gradients in the ice age North Atlantic Ocean revealed by plankton biogeography L. Jonkers et al. 10.1038/s41561-023-01328-7
- Spatio-temporal dynamics of hydrographic reorganizations and iceberg discharges at the junction between the Northeast Atlantic and Norwegian Sea basins surrounding Heinrich event 4 M. Wary et al. 10.1016/j.epsl.2017.10.042
- An evaluation of benthic foraminiferal U/Ca and U/Mn proxies for deep ocean carbonate chemistry and redox conditions P. Chen et al. 10.1002/2016GC006730
- ForCenS-LGM: a dataset of planktonic foraminifera species assemblage composition for the Last Glacial Maximum L. Jonkers et al. 10.1038/s41597-024-03166-7
- Consistently dated Atlantic sediment cores over the last 40 thousand years C. Waelbroeck et al. 10.1038/s41597-019-0173-8
- Dansgaard-Oeschger and Heinrich event temperature anomalies in the North Atlantic set by sea ice, frontal position and thermocline structure J. Pedro et al. 10.1016/j.quascirev.2022.107599
- Sea ice in the Nordic Seas: Greenland stadial to interstadial changes W. Wong et al. 10.1016/j.quascirev.2024.108916
- High‐Resolution Benthic Mg/Ca Temperature Record of the Intermediate Water in the Denmark Strait Across D‐O Stadial‐Interstadial Cycles E. Sessford et al. 10.1029/2018PA003370
- Consistent fluctuations in intermediate water temperature off the coast of Greenland and Norway during Dansgaard-Oeschger events E. Sessford et al. 10.1016/j.quascirev.2019.105887
14 citations as recorded by crossref.
- Imprint of seasonality changes on fluvio-glacial dynamics across Heinrich Stadial 1 (NE Atlantic Ocean) W. Fersi et al. 10.1016/j.gloplacha.2021.103552
- Dinoflagellate fossils: Geological and biological applications A. Penaud et al. 10.1016/j.revmic.2018.09.003
- Western boundary current in relation to Atlantic Subtropical Gyre dynamics during abrupt glacial climate fluctuations D. Nürnberg et al. 10.1016/j.gloplacha.2021.103497
- Changes in the geometry and strength of the Atlantic meridional overturning circulation during the last glacial (20–50 ka) P. Burckel et al. 10.5194/cp-12-2061-2016
- Are Past Sea-Ice Reconstructions Based on Planktonic Foraminifera Realistic? Study of the Last 50 ka as a Test to Validate Reconstructed Paleohydrography Derived from Transfer Functions Applied to Their Fossil Assemblages F. Eynaud et al. 10.3390/geosciences11100409
- Millennial‐Scale Climate Variability and Dinoflagellate‐Cyst‐Based Seasonality Changes Over the Last ~150 kyrs at “Shackleton Site” U1385 M. Datema et al. 10.1029/2018PA003497
- The southern Norwegian Sea during the last 45 ka: hydrographical reorganizations under changing ice‐sheet dynamics M. Wary et al. 10.1002/jqs.2965
- Strong temperature gradients in the ice age North Atlantic Ocean revealed by plankton biogeography L. Jonkers et al. 10.1038/s41561-023-01328-7
- Spatio-temporal dynamics of hydrographic reorganizations and iceberg discharges at the junction between the Northeast Atlantic and Norwegian Sea basins surrounding Heinrich event 4 M. Wary et al. 10.1016/j.epsl.2017.10.042
- An evaluation of benthic foraminiferal U/Ca and U/Mn proxies for deep ocean carbonate chemistry and redox conditions P. Chen et al. 10.1002/2016GC006730
- ForCenS-LGM: a dataset of planktonic foraminifera species assemblage composition for the Last Glacial Maximum L. Jonkers et al. 10.1038/s41597-024-03166-7
- Consistently dated Atlantic sediment cores over the last 40 thousand years C. Waelbroeck et al. 10.1038/s41597-019-0173-8
- Dansgaard-Oeschger and Heinrich event temperature anomalies in the North Atlantic set by sea ice, frontal position and thermocline structure J. Pedro et al. 10.1016/j.quascirev.2022.107599
- Sea ice in the Nordic Seas: Greenland stadial to interstadial changes W. Wong et al. 10.1016/j.quascirev.2024.108916
2 citations as recorded by crossref.
- High‐Resolution Benthic Mg/Ca Temperature Record of the Intermediate Water in the Denmark Strait Across D‐O Stadial‐Interstadial Cycles E. Sessford et al. 10.1029/2018PA003370
- Consistent fluctuations in intermediate water temperature off the coast of Greenland and Norway during Dansgaard-Oeschger events E. Sessford et al. 10.1016/j.quascirev.2019.105887
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Latest update: 18 Nov 2024
Short summary
This study reports the hydrological variations recorded at different depths of the water column SW of the Faeroe Is. during the last glacial abrupt climatic events (Heinrich events and Dansgaard-Oeschger cycles). Our combined multiproxy and high-resolution approach allows us to evidence that 1) Greenland and Heinrich stadials were characterized by strong stratification of surface waters, 2) this surface stratification seems to have played a key role in the dynamics of the underlying water masses
This study reports the hydrological variations recorded at different depths of the water column...
