Articles | Volume 9, issue 6
https://doi.org/10.5194/cp-9-2631-2013
© Author(s) 2013. 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-9-2631-2013
© Author(s) 2013. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Research article
| 
25 Nov 2013
Research article |
| 25 Nov 2013
Paleo Agulhas rings enter the subtropical gyre during the penultimate deglaciation
P. Scussolini
Earth and Climate Group, Vrije Universiteit, Amsterdam, the Netherlands
The Bjerknes Centre for Climate Research, Uni Research, Bergen, Norway
E. van Sebille
Climate Change Research Centre & ARC Centre of Excellence for Climate System Science, University of New South Wales, Sydney, Australia
J. V. Durgadoo
GEOMAR Helmholtz Centre for Ocean Research Kiel, Kiel, Germany
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Cited
15 citations as recorded by crossref.
- Globorotalia truncatulinoides as indicator of Subtropical Convergence and thermocline change during the late Quaternary in the Southeast Atlantic E. Bergh & L. Jonk 10.1016/j.palaeo.2024.112274
- Modal shift in North Atlantic seasonality during the last deglaciation G. Brummer et al. 10.5194/cp-16-265-2020
- Late Quaternary responses to glacial-interglacial climate cycles of offshore Benguela region and associated foraminifera in the southeast Atlantic along Namibia and western South Africa E. Bergh 10.1016/j.dsr2.2024.105413
- Saline Indian Ocean waters invaded the South Atlantic thermocline during glacial termination II P. Scussolini et al. 10.1130/G36238.1
- Evolutionary prospection in the Neogene planktic foraminifer Globorotalia menardii and related forms from ODP Hole 925B (Ceara Rise, western tropical Atlantic): evidence for gradual evolution superimposed by long distance dispersal? M. Knappertsbusch 10.1007/s13358-016-0113-6
- Historical Biogeography of Delphininae Dolphins and Related Taxa (Artiodactyla: Delphinidae) K. do Amaral et al. 10.1007/s10914-016-9376-3
- Reconstructing the depth of the permanent thermocline through the morphology and geochemistry of the deep dwelling planktonic foraminifer Globorotalia truncatulinoides W. Feldmeijer et al. 10.1002/2014PA002687
- Oxygen Isotope Variability of Planktonic Foraminifera Provide Clues to Past Upper Ocean Seasonal Variability B. Metcalfe et al. 10.1029/2018PA003475
- Ocean currents generate large footprints in marine palaeoclimate proxies E. van Sebille et al. 10.1038/ncomms7521
- Testing the effect of bioturbation and species abundance upon discrete-depth individual foraminifera analysis B. Lougheed & B. Metcalfe 10.5194/bg-19-1195-2022
- Sedproxy: a forward model for sediment-archived climate proxies A. Dolman & T. Laepple 10.5194/cp-14-1851-2018
- Morphological evolution of menardiform globorotalids at Western Pacific Warm Pool ODP Hole 806C (Ontong-Java Plateau) Evolution morphologique du groupe de Globorotalia menardii au Site ODP 806C (Ontong-Java Plateau, Pacifique tropical occidental) M. Knappertsbusch 10.1016/j.revmic.2022.100608
- Early Eocene Thermal Maximum 3: Biotic Response at Walvis Ridge (SE Atlantic Ocean) E. Thomas et al. 10.1029/2018PA003375
- The INALT family – a set of high-resolution nests for the Agulhas Current system within global NEMO ocean/sea-ice configurations F. Schwarzkopf et al. 10.5194/gmd-12-3329-2019
- Oxygen isotope composition of the final chamber of planktic foraminifera provides evidence of vertical migration and depth-integrated growth H. Pracht et al. 10.5194/bg-16-643-2019
15 citations as recorded by crossref.
- Globorotalia truncatulinoides as indicator of Subtropical Convergence and thermocline change during the late Quaternary in the Southeast Atlantic E. Bergh & L. Jonk 10.1016/j.palaeo.2024.112274
- Modal shift in North Atlantic seasonality during the last deglaciation G. Brummer et al. 10.5194/cp-16-265-2020
- Late Quaternary responses to glacial-interglacial climate cycles of offshore Benguela region and associated foraminifera in the southeast Atlantic along Namibia and western South Africa E. Bergh 10.1016/j.dsr2.2024.105413
- Saline Indian Ocean waters invaded the South Atlantic thermocline during glacial termination II P. Scussolini et al. 10.1130/G36238.1
- Evolutionary prospection in the Neogene planktic foraminifer Globorotalia menardii and related forms from ODP Hole 925B (Ceara Rise, western tropical Atlantic): evidence for gradual evolution superimposed by long distance dispersal? M. Knappertsbusch 10.1007/s13358-016-0113-6
- Historical Biogeography of Delphininae Dolphins and Related Taxa (Artiodactyla: Delphinidae) K. do Amaral et al. 10.1007/s10914-016-9376-3
- Reconstructing the depth of the permanent thermocline through the morphology and geochemistry of the deep dwelling planktonic foraminifer Globorotalia truncatulinoides W. Feldmeijer et al. 10.1002/2014PA002687
- Oxygen Isotope Variability of Planktonic Foraminifera Provide Clues to Past Upper Ocean Seasonal Variability B. Metcalfe et al. 10.1029/2018PA003475
- Ocean currents generate large footprints in marine palaeoclimate proxies E. van Sebille et al. 10.1038/ncomms7521
- Testing the effect of bioturbation and species abundance upon discrete-depth individual foraminifera analysis B. Lougheed & B. Metcalfe 10.5194/bg-19-1195-2022
- Sedproxy: a forward model for sediment-archived climate proxies A. Dolman & T. Laepple 10.5194/cp-14-1851-2018
- Morphological evolution of menardiform globorotalids at Western Pacific Warm Pool ODP Hole 806C (Ontong-Java Plateau) Evolution morphologique du groupe de Globorotalia menardii au Site ODP 806C (Ontong-Java Plateau, Pacifique tropical occidental) M. Knappertsbusch 10.1016/j.revmic.2022.100608
- Early Eocene Thermal Maximum 3: Biotic Response at Walvis Ridge (SE Atlantic Ocean) E. Thomas et al. 10.1029/2018PA003375
- The INALT family – a set of high-resolution nests for the Agulhas Current system within global NEMO ocean/sea-ice configurations F. Schwarzkopf et al. 10.5194/gmd-12-3329-2019
- Oxygen isotope composition of the final chamber of planktic foraminifera provides evidence of vertical migration and depth-integrated growth H. Pracht et al. 10.5194/bg-16-643-2019
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