Articles | Volume 8, issue 6
https://doi.org/10.5194/cp-8-1997-2012
© Author(s) 2012. 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-8-1997-2012
© Author(s) 2012. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
An ocean–ice coupled response during the last glacial: a view from a marine isotopic stage 3 record south of the Faeroe Shetland Gateway
J. Zumaque
EPOC – Environnements et Paléoenvironnements Océaniques, UMR5805, Université Bordeaux I, Talence, France
present address: GEOTOP, Montréal, Canada
F. Eynaud
EPOC – Environnements et Paléoenvironnements Océaniques, UMR5805, Université Bordeaux I, Talence, France
S. Zaragosi
EPOC – Environnements et Paléoenvironnements Océaniques, UMR5805, Université Bordeaux I, Talence, France
F. Marret
School of Environmental Sciences, University of Liverpool, Liverpool, L69 7ZT, UK
K. M. Matsuzaki
EPOC – Environnements et Paléoenvironnements Océaniques, UMR5805, Université Bordeaux I, Talence, France
present address: Institute of Geology and Paleontology, Graduate School of Science, Tohoku University, Aramaki 6-3, Sendai, 980-8578, Japan
C. Kissel
Laboratoire des Sciences du Climat et de l'Environnement (LSCE), CEA/CNRS-INSU/UVSQ – UMR8212, 91191 Gif s/s Yvette, France
D. M. Roche
Laboratoire des Sciences du Climat et de l'Environnement (LSCE), CEA/CNRS-INSU/UVSQ – UMR8212, 91191 Gif s/s Yvette, France
Vrije Universiteit Amsterdam, de Boelelaan 1085, 1081 HV Amsterdam, The Netherlands
B. Malaizé
EPOC – Environnements et Paléoenvironnements Océaniques, UMR5805, Université Bordeaux I, Talence, France
E. Michel
Laboratoire des Sciences du Climat et de l'Environnement (LSCE), CEA/CNRS-INSU/UVSQ – UMR8212, 91191 Gif s/s Yvette, France
I. Billy
EPOC – Environnements et Paléoenvironnements Océaniques, UMR5805, Université Bordeaux I, Talence, France
T. Richter
NIOZ Royal Netherlands Institute for Sea Research, P.O. Box 59, 1790 AB Den Burg (Texel), The Netherlands
E. Palis
EPOC – Environnements et Paléoenvironnements Océaniques, UMR5805, Université Bordeaux I, Talence, France
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Morgan Vervoort, Katleen Wils, Kris Vanneste, Roberto Urrutia, Mario Pino, Catherine Kissel, Marc De Batist, and Maarten Van Daele
Nat. Hazards Earth Syst. Sci., 24, 3401–3421, https://doi.org/10.5194/nhess-24-3401-2024, https://doi.org/10.5194/nhess-24-3401-2024, 2024
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This study identifies a prehistoric earthquake around 4400 years ago near the city of Coyhaique (Aysén Region, Chilean Patagonia) and illustrates the potential seismic hazard in the region. We found deposits in lakes and a fjord that can be related to subaquatic and onshore landslides, all with a similar age, indicating that they were most likely caused by an earthquake. Through modeling we found that this was an earthquake of magnitude 6.3 to 7.0 on a fault near the city of Coyhaique.
Aurélien Quiquet and Didier M. Roche
Clim. Past, 20, 1365–1385, https://doi.org/10.5194/cp-20-1365-2024, https://doi.org/10.5194/cp-20-1365-2024, 2024
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In this work, we use the same experimental protocol to simulate the last two glacial terminations with a coupled ice sheet–climate model. Major differences among the two terminations are that the ice sheets retreat earlier and the Atlantic oceanic circulation is more prone to collapse during the penultimate termination. However, for both terminations the pattern of ice retreat is similar, and this retreat is primarily explained by orbital forcing changes and greenhouse gas concentration changes.
Thi-Khanh-Dieu Hoang, Aurélien Quiquet, Christophe Dumas, Andreas Born, and Didier M. Roche
EGUsphere, https://doi.org/10.5194/egusphere-2024-556, https://doi.org/10.5194/egusphere-2024-556, 2024
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To improve the simulation of surface mass balance (SMB) that influences the advance-retreat of ice sheets, we run a snow model BESSI (BErgen Snow Simulator) with transient climate forcing obtained from an Earth system model iLOVECLIM over Greenland and Antarctica during the Last Interglacial period (130–116 kaBP). Compared to the existing simple SMB scheme of iLOVECLIM, BESSI gives more details about SMB processes with higher physics constraints while maintaining a low computational cost.
Thomas Extier, Thibaut Caley, and Didier M. Roche
Geosci. Model Dev., 17, 2117–2139, https://doi.org/10.5194/gmd-17-2117-2024, https://doi.org/10.5194/gmd-17-2117-2024, 2024
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Stable water isotopes are used to infer changes in the hydrological cycle for different time periods in climatic archive and climate models. We present the implementation of the δ2H and δ17O water isotopes in the coupled climate model iLOVECLIM and calculate the d- and 17O-excess. Results of a simulation under preindustrial conditions show that the model correctly reproduces the water isotope distribution in the atmosphere and ocean in comparison to data and other global circulation models.
Takashi Obase, Laurie Menviel, Ayako Abe-Ouchi, Tristan Vadsaria, Ruza Ivanovic, Brooke Snoll, Sam Sherriff-Tadano, Paul Valdes, Lauren Gregoire, Marie-Luise Kapsch, Uwe Mikolajewicz, Nathaelle Bouttes, Didier Roche, Fanny Lhardy, Chengfei He, Bette Otto-Bliesner, Zhengyu Liu, and Wing-Le Chan
Clim. Past Discuss., https://doi.org/10.5194/cp-2023-86, https://doi.org/10.5194/cp-2023-86, 2023
Revised manuscript under review for CP
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This study analyses transient simulations of the last deglaciation performed by six climate models to understand the processes driving southern high latitude temperature changes. We find that atmospheric CO2 changes and AMOC changes are the primary drivers of the major warming and cooling during the middle stage of the deglaciation. The multi-model analysis highlights the model’s sensitivity of CO2, AMOC to meltwater, and the meltwater history on temperature changes in southern high latitudes.
Lena Mareike Thöle, Peter Dirk Nooteboom, Suning Hou, Rujian Wang, Senyan Nie, Elisabeth Michel, Isabel Sauermilch, Fabienne Marret, Francesca Sangiorgi, and Peter Kristian Bijl
J. Micropalaeontol., 42, 35–56, https://doi.org/10.5194/jm-42-35-2023, https://doi.org/10.5194/jm-42-35-2023, 2023
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Dinoflagellate cysts can be used to infer past oceanographic conditions in the Southern Ocean. This requires knowledge of their present-day ecologic affinities. We add 66 Antarctic-proximal surface sediment samples to the Southern Ocean data and derive oceanographic conditions at those stations. Dinoflagellate cysts are clearly biogeographically separated along latitudinal gradients of temperature, sea ice, nutrients, and salinity, which allows us to reconstruct these parameters for the past.
Nathaelle Bouttes, Fanny Lhardy, Aurélien Quiquet, Didier Paillard, Hugues Goosse, and Didier M. Roche
Clim. Past, 19, 1027–1042, https://doi.org/10.5194/cp-19-1027-2023, https://doi.org/10.5194/cp-19-1027-2023, 2023
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The last deglaciation is a period of large warming from 21 000 to 9000 years ago, concomitant with ice sheet melting. Here, we evaluate the impact of different ice sheet reconstructions and different processes linked to their changes. Changes in bathymetry and coastlines, although not often accounted for, cannot be neglected. Ice sheet melt results in freshwater into the ocean with large effects on ocean circulation, but the timing cannot explain the observed abrupt climate changes.
Claire Waelbroeck, Jerry Tjiputra, Chuncheng Guo, Kerim H. Nisancioglu, Eystein Jansen, Natalia Vázquez Riveiros, Samuel Toucanne, Frédérique Eynaud, Linda Rossignol, Fabien Dewilde, Elodie Marchès, Susana Lebreiro, and Silvia Nave
Clim. Past, 19, 901–913, https://doi.org/10.5194/cp-19-901-2023, https://doi.org/10.5194/cp-19-901-2023, 2023
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The precise geometry and extent of Atlantic circulation changes that accompanied rapid climate changes of the last glacial period are still unknown. Here, we combine carbon isotopic records from 18 Atlantic sediment cores with numerical simulations and decompose the carbon isotopic change across a cold-to-warm transition into remineralization and circulation components. Our results show that the replacement of southern-sourced by northern-sourced water plays a dominant role below ~ 3000 m depth.
Frank Arthur, Didier M. Roche, Ralph Fyfe, Aurélien Quiquet, and Hans Renssen
Clim. Past, 19, 87–106, https://doi.org/10.5194/cp-19-87-2023, https://doi.org/10.5194/cp-19-87-2023, 2023
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This paper simulates transcient Holocene climate in Europe by applying an interactive downscaling to the standard version of the iLOVECLIM model. The results show that downscaling presents a higher spatial variability in better agreement with proxy-based reconstructions as compared to the standard model, particularly in the Alps, the Scandes, and the Mediterranean. Our downscaling scheme is numerically cheap, which can perform kilometric multi-millennial simulations suitable for future studies.
Pepijn Bakker, Hugues Goosse, and Didier M. Roche
Clim. Past, 18, 2523–2544, https://doi.org/10.5194/cp-18-2523-2022, https://doi.org/10.5194/cp-18-2523-2022, 2022
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Natural climate variability plays an important role in the discussion of past and future climate change. Here we study centennial temperature variability and the role of large-scale ocean circulation variability using different climate models, geological reconstructions and temperature observations. Unfortunately, uncertainties in models and geological reconstructions are such that more research is needed before we can describe the characteristics of natural centennial temperature variability.
Huan Li, Hans Renssen, and Didier M. Roche
Clim. Past, 18, 2303–2319, https://doi.org/10.5194/cp-18-2303-2022, https://doi.org/10.5194/cp-18-2303-2022, 2022
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In past warm periods, the Sahara region was covered by vegetation. In this paper we study transitions from this
greenstate to the desert state we find today. For this purpose, we have used a global climate model coupled to a vegetation model to perform transient simulations. We analyzed the model results to assess the effect of vegetation shifts on the abruptness of the transition. We find that the vegetation feedback was more efficient during the last interglacial than during the Holocene.
Aurélien Quiquet, Didier M. Roche, Christophe Dumas, Nathaëlle Bouttes, and Fanny Lhardy
Clim. Past, 17, 2179–2199, https://doi.org/10.5194/cp-17-2179-2021, https://doi.org/10.5194/cp-17-2179-2021, 2021
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In this paper we discuss results obtained with a set of coupled ice-sheet–climate model experiments for the last 26 kyrs. The model displays a large sensitivity of the oceanic circulation to the amount of the freshwater flux resulting from ice sheet melting. Ice sheet geometry changes alone are not enough to lead to abrupt climate events, and rapid warming at high latitudes is here only reported during abrupt oceanic circulation recoveries that occurred when accounting for freshwater flux.
Fanny Lhardy, Nathaëlle Bouttes, Didier M. Roche, Xavier Crosta, Claire Waelbroeck, and Didier Paillard
Clim. Past, 17, 1139–1159, https://doi.org/10.5194/cp-17-1139-2021, https://doi.org/10.5194/cp-17-1139-2021, 2021
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Climate models struggle to simulate a LGM ocean circulation in agreement with paleotracer data. Using a set of simulations, we test the impact of boundary conditions and other modelling choices. Model–data comparisons of sea-surface temperatures and sea-ice cover support an overall cold Southern Ocean, with implications on the AMOC strength. Changes in implemented boundary conditions are not sufficient to simulate a shallower AMOC; other mechanisms to better represent convection are required.
Masa Kageyama, Sandy P. Harrison, Marie-L. Kapsch, Marcus Lofverstrom, Juan M. Lora, Uwe Mikolajewicz, Sam Sherriff-Tadano, Tristan Vadsaria, Ayako Abe-Ouchi, Nathaelle Bouttes, Deepak Chandan, Lauren J. Gregoire, Ruza F. Ivanovic, Kenji Izumi, Allegra N. LeGrande, Fanny Lhardy, Gerrit Lohmann, Polina A. Morozova, Rumi Ohgaito, André Paul, W. Richard Peltier, Christopher J. Poulsen, Aurélien Quiquet, Didier M. Roche, Xiaoxu Shi, Jessica E. Tierney, Paul J. Valdes, Evgeny Volodin, and Jiang Zhu
Clim. Past, 17, 1065–1089, https://doi.org/10.5194/cp-17-1065-2021, https://doi.org/10.5194/cp-17-1065-2021, 2021
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The Last Glacial Maximum (LGM; ~21 000 years ago) is a major focus for evaluating how well climate models simulate climate changes as large as those expected in the future. Here, we compare the latest climate model (CMIP6-PMIP4) to the previous one (CMIP5-PMIP3) and to reconstructions. Large-scale climate features (e.g. land–sea contrast, polar amplification) are well captured by all models, while regional changes (e.g. winter extratropical cooling, precipitations) are still poorly represented.
Brett Metcalfe, Bryan C. Lougheed, Claire Waelbroeck, and Didier M. Roche
Clim. Past, 16, 885–910, https://doi.org/10.5194/cp-16-885-2020, https://doi.org/10.5194/cp-16-885-2020, 2020
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Planktonic foraminifera construct a shell that, post mortem, settles to the seafloor, prior to collection by Palaeoclimatologists for use as proxies. Such organisms in life are sensitive to the ambient conditions (e.g. temperature, salinity), which therefore means our proxies maybe skewed toward the ecology of organisms. Using a proxy system model, Foraminifera as Modelled Entities (FAME), we assess the potential of extracting ENSO signal from tropical Pacific planktonic foraminifera.
Lise Missiaen, Nathaelle Bouttes, Didier M. Roche, Jean-Claude Dutay, Aurélien Quiquet, Claire Waelbroeck, Sylvain Pichat, and Jean-Yves Peterschmitt
Clim. Past, 16, 867–883, https://doi.org/10.5194/cp-16-867-2020, https://doi.org/10.5194/cp-16-867-2020, 2020
Eleonora Fossile, Maria Pia Nardelli, Arbia Jouini, Bruno Lansard, Antonio Pusceddu, Davide Moccia, Elisabeth Michel, Olivier Péron, Hélène Howa, and Meryem Mojtahid
Biogeosciences, 17, 1933–1953, https://doi.org/10.5194/bg-17-1933-2020, https://doi.org/10.5194/bg-17-1933-2020, 2020
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This study focuses on benthic foraminiferal distribution in an Arctic fjord characterised by continuous sea ice production during winter and the consequent cascading of salty and corrosive waters (brine) to the seabed. The inner fjord is dominated by calcareous species (C). In the central deep basins, where brines are persistent, calcareous foraminifera are dissolved and agglutinated (A) dominate. The high A/C ratio is suggested as a proxy for brine persistence and sea ice production.
Aurélien Quiquet, Christophe Dumas, Catherine Ritz, Vincent Peyaud, and Didier M. Roche
Geosci. Model Dev., 11, 5003–5025, https://doi.org/10.5194/gmd-11-5003-2018, https://doi.org/10.5194/gmd-11-5003-2018, 2018
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This paper presents the GRISLI (Grenoble ice sheet and land ice) model in its newest revision. We present the recent model improvements from its original version (Ritz et al., 2001), together with a discussion of the model performance in reproducing the present-day Antarctic ice sheet geometry and the grounding line advances and retreats during the last 400 000 years. We show that GRISLI is a computationally cheap model, able to reproduce the large-scale behaviour of ice sheets.
Didier M. Roche, Claire Waelbroeck, Brett Metcalfe, and Thibaut Caley
Geosci. Model Dev., 11, 3587–3603, https://doi.org/10.5194/gmd-11-3587-2018, https://doi.org/10.5194/gmd-11-3587-2018, 2018
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The oxygen-18 signal recorded in fossil planktonic foraminifers has been used for over 50 years in many geoscience applications. However, different planktonic foraminifer species from the same sediment core generally yield distinct oxygen-18 signals, as a consequence of their specific living habitat in the water column and along the year. To explicitly take into account this variability for five common planktonic species, we developed the portable module FAME (Foraminifers As Modeled Entities).
Masa Kageyama, Pascale Braconnot, Sandy P. Harrison, Alan M. Haywood, Johann H. Jungclaus, Bette L. Otto-Bliesner, Jean-Yves Peterschmitt, Ayako Abe-Ouchi, Samuel Albani, Patrick J. Bartlein, Chris Brierley, Michel Crucifix, Aisling Dolan, Laura Fernandez-Donado, Hubertus Fischer, Peter O. Hopcroft, Ruza F. Ivanovic, Fabrice Lambert, Daniel J. Lunt, Natalie M. Mahowald, W. Richard Peltier, Steven J. Phipps, Didier M. Roche, Gavin A. Schmidt, Lev Tarasov, Paul J. Valdes, Qiong Zhang, and Tianjun Zhou
Geosci. Model Dev., 11, 1033–1057, https://doi.org/10.5194/gmd-11-1033-2018, https://doi.org/10.5194/gmd-11-1033-2018, 2018
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The Paleoclimate Modelling Intercomparison Project (PMIP) takes advantage of the existence of past climate states radically different from the recent past to test climate models used for climate projections and to better understand these climates. This paper describes the PMIP contribution to CMIP6 (Coupled Model Intercomparison Project, 6th phase) and possible analyses based on PMIP results, as well as on other CMIP6 projects.
Nathaelle Bouttes, Didier Swingedouw, Didier M. Roche, Maria F. Sanchez-Goni, and Xavier Crosta
Clim. Past, 14, 239–253, https://doi.org/10.5194/cp-14-239-2018, https://doi.org/10.5194/cp-14-239-2018, 2018
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Atmospheric CO2 is key for climate change. CO2 is lower during the oldest warm period of the last million years, the interglacials, than during the most recent ones (since 430 000 years ago). This difference has not been explained yet, but could be due to changes of ocean circulation. We test this hypothesis and the role of vegetation and ice sheets using an intermediate complexity model. We show that only small changes of CO2 can be obtained, underlying missing feedbacks or mechanisms.
Aurélien Quiquet, Didier M. Roche, Christophe Dumas, and Didier Paillard
Geosci. Model Dev., 11, 453–466, https://doi.org/10.5194/gmd-11-453-2018, https://doi.org/10.5194/gmd-11-453-2018, 2018
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Earth system models of intermediate complexity generally have a simplified model physics and a coarse model resolution. In this work we present the inclusion of an online dynamical downscaling of temperature and precipitation in such a model. This downscaling explicitly takes into account sub-grid topography. With this new model functionality we are able to simulate temperature and precipitation on a 40 km grid for the whole Northern Hemisphere from the native model resolution.
Masa Kageyama, Samuel Albani, Pascale Braconnot, Sandy P. Harrison, Peter O. Hopcroft, Ruza F. Ivanovic, Fabrice Lambert, Olivier Marti, W. Richard Peltier, Jean-Yves Peterschmitt, Didier M. Roche, Lev Tarasov, Xu Zhang, Esther C. Brady, Alan M. Haywood, Allegra N. LeGrande, Daniel J. Lunt, Natalie M. Mahowald, Uwe Mikolajewicz, Kerim H. Nisancioglu, Bette L. Otto-Bliesner, Hans Renssen, Robert A. Tomas, Qiong Zhang, Ayako Abe-Ouchi, Patrick J. Bartlein, Jian Cao, Qiang Li, Gerrit Lohmann, Rumi Ohgaito, Xiaoxu Shi, Evgeny Volodin, Kohei Yoshida, Xiao Zhang, and Weipeng Zheng
Geosci. Model Dev., 10, 4035–4055, https://doi.org/10.5194/gmd-10-4035-2017, https://doi.org/10.5194/gmd-10-4035-2017, 2017
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The Last Glacial Maximum (LGM, 21000 years ago) is an interval when global ice volume was at a maximum, eustatic sea level close to a minimum, greenhouse gas concentrations were lower, atmospheric aerosol loadings were higher than today, and vegetation and land-surface characteristics were different from today. This paper describes the implementation of the LGM numerical experiment for the PMIP4-CMIP6 modelling intercomparison projects and the associated sensitivity experiments.
Mélanie Wary, Frédérique Eynaud, Didier Swingedouw, Valérie Masson-Delmotte, Jens Matthiessen, Catherine Kissel, Jena Zumaque, Linda Rossignol, and Jean Jouzel
Clim. Past, 13, 729–739, https://doi.org/10.5194/cp-13-729-2017, https://doi.org/10.5194/cp-13-729-2017, 2017
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The last glacial period was punctuated by abrupt climatic variations, whose cold atmospheric phases have been commonly associated with cold sea-surface temperatures and expansion of sea ice in the North Atlantic and adjacent seas. Here we provide direct evidence of a regional paradoxical see-saw pattern: cold Greenland and North Atlantic phases coincide with warmer sea-surface conditions and shorter seasonal sea-ice cover durations in the Norwegian Sea as compared to warm phases.
Yannick Mary, Frédérique Eynaud, Christophe Colin, Linda Rossignol, Sandra Brocheray, Meryem Mojtahid, Jennifer Garcia, Marion Peral, Hélène Howa, Sébastien Zaragosi, and Michel Cremer
Clim. Past, 13, 201–216, https://doi.org/10.5194/cp-13-201-2017, https://doi.org/10.5194/cp-13-201-2017, 2017
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In the boreal Atlantic, the subpolar and subtropical gyres (SPG and STG respectively) are key elements of the Atlantic Meridional Overturning Circulation (AMOC) cell and contribute to climate modulations over Europe. Here we document the last 10 kyr evolution of sea-surface temperatures over the North Atlantic with a focus on new data obtained from an exceptional sedimentary archive retrieved the southern Bay of Biscay, enabling the study of Holocene archives at (infra)centennial scales.
Pierre Burckel, Claire Waelbroeck, Yiming Luo, Didier M. Roche, Sylvain Pichat, Samuel L. Jaccard, Jeanne Gherardi, Aline Govin, Jörg Lippold, and François Thil
Clim. Past, 12, 2061–2075, https://doi.org/10.5194/cp-12-2061-2016, https://doi.org/10.5194/cp-12-2061-2016, 2016
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In this paper, we compare new and published Atlantic sedimentary Pa/Th data with Pa/Th simulated using stream functions generated under various climatic conditions. We show that during Greenland interstadials of the 20–50 ka period, the Atlantic meridional overturning circulation was very different from that of the Holocene. Moreover, southern-sourced waters dominated the Atlantic during Heinrich stadial 2, a slow northern-sourced water mass flowing above 2500 m in the North Atlantic.
Aurélie Penaud, Frédérique Eynaud, Antje Helga Luise Voelker, and Jean-Louis Turon
Biogeosciences, 13, 5357–5377, https://doi.org/10.5194/bg-13-5357-2016, https://doi.org/10.5194/bg-13-5357-2016, 2016
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This paper presents new analyses conducted at high resolution in the Gulf of Cadiz over the last 50 ky. Palaeohydrological changes in these subtropical latitudes are discussed through dinoflagellate cyst assemblages but also dinocyst transfer function results, implying sea surface temperature and salinity as well as annual productivity reconstructions. This study is thus important for our understanding of past and future productivity regimes, also implying consequences on the biological pump.
William Hardy, Aurélie Penaud, Fabienne Marret, Germain Bayon, Tania Marsset, and Laurence Droz
Biogeosciences, 13, 4823–4841, https://doi.org/10.5194/bg-13-4823-2016, https://doi.org/10.5194/bg-13-4823-2016, 2016
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Our approach is based on a multi-proxy study from a core collected off the Congo River and discusses surface oceanic conditions (upwelling cells, river-induced upwelling), land–sea interactions and terrestrial erosion and in particular enables us to spatially constrain the migration of atmospheric systems. This paper thus presents new data highlighting, with the highest resolution ever reached in this region, the great correlation between phytoplanktonic organisms and monsoonal mechanisms.
Timothé Bolliet, Patrick Brockmann, Valérie Masson-Delmotte, Franck Bassinot, Valérie Daux, Dominique Genty, Amaelle Landais, Marlène Lavrieux, Elisabeth Michel, Pablo Ortega, Camille Risi, Didier M. Roche, Françoise Vimeux, and Claire Waelbroeck
Clim. Past, 12, 1693–1719, https://doi.org/10.5194/cp-12-1693-2016, https://doi.org/10.5194/cp-12-1693-2016, 2016
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This paper presents a new database of past climate proxies which aims to facilitate the distribution of data by using a user-friendly interface. Available data from the last 40 years are often fragmented, with lots of different formats, and online libraries are sometimes nonintuitive. We thus built a new dynamic web portal for data browsing, visualizing, and batch downloading of hundreds of datasets presenting a homogeneous format.
Ruza F. Ivanovic, Lauren J. Gregoire, Masa Kageyama, Didier M. Roche, Paul J. Valdes, Andrea Burke, Rosemarie Drummond, W. Richard Peltier, and Lev Tarasov
Geosci. Model Dev., 9, 2563–2587, https://doi.org/10.5194/gmd-9-2563-2016, https://doi.org/10.5194/gmd-9-2563-2016, 2016
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This manuscript presents the experiment design for the PMIP4 Last Deglaciation Core experiment: a transient simulation of the last deglaciation, 21–9 ka. Specified model boundary conditions include time-varying orbital parameters, greenhouse gases, ice sheets, ice meltwater fluxes and other geographical changes (provided for 26–0 ka). The context of the experiment and the choices for the boundary conditions are explained, along with the future direction of the working group.
Majda Nourelbait, Ali Rhoujjati, Abdelfattah Benkaddour, Matthieu Carré, Frederique Eynaud, Philippe Martinez, and Rachid Cheddadi
Clim. Past, 12, 1029–1042, https://doi.org/10.5194/cp-12-1029-2016, https://doi.org/10.5194/cp-12-1029-2016, 2016
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The present study is related the climate changes and their environmental impacts during the last 6 ky from a fossil record collected in the Middle Atlas, Morocco. We used the reconstruction of three climate variables and geo-chemical elements to evaluate the relationships between all the environmental variables. In summary, this present study confirms the overall climate stability over the last 6 ky and highlights the presence of a short and abrupt climate event at about 5.2 ka cal BP.
Marianne Bügelmayer-Blaschek, Didier M. Roche, Hans Renssen, and Claire Waelbroeck
Clim. Past Discuss., https://doi.org/10.5194/cp-2016-31, https://doi.org/10.5194/cp-2016-31, 2016
Revised manuscript has not been submitted
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Using the global isotope-enabled climate – iceberg model iLOVECLIM we performed three experiments to investigate the mechanisms behind the simulated δ18Ocalcite pattern applying a Heinrich event like iceberg forcing. Our model results display two main patterns in the δ18Ocalcite signal. First, we find regions that display almost no response in δ18Ocalcite and second, regions where the δ18Ocalcite pattern closely follows the δ18Oseawater signal.
M. Wary, F. Eynaud, M. Sabine, S. Zaragosi, L. Rossignol, B. Malaizé, E. Palis, J. Zumaque, C. Caulle, A. Penaud, E. Michel, and K. Charlier
Clim. Past, 11, 1507–1525, https://doi.org/10.5194/cp-11-1507-2015, https://doi.org/10.5194/cp-11-1507-2015, 2015
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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
M. Bügelmayer, D. M. Roche, and H. Renssen
Geosci. Model Dev., 8, 2139–2151, https://doi.org/10.5194/gmd-8-2139-2015, https://doi.org/10.5194/gmd-8-2139-2015, 2015
N. Bouttes, D. M. Roche, V. Mariotti, and L. Bopp
Geosci. Model Dev., 8, 1563–1576, https://doi.org/10.5194/gmd-8-1563-2015, https://doi.org/10.5194/gmd-8-1563-2015, 2015
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We describe the development of a relatively simple climate model to include a model of the carbon cycle in the ocean. The carbon cycle consists of the exchange of carbon between the atmosphere, land vegetation and ocean. In the ocean, carbon exists in organic form, such as plankton which grows and dies, and inorganic forms, such as dissolved CO2. With this we will be able to explore long-standing questions such as why the atmospheric CO2 has changed over time during the last million years.
S. Hoetzel, L. M. Dupont, F. Marret, G. Jung, and G. Wefer
Clim. Past Discuss., https://doi.org/10.5194/cpd-11-1913-2015, https://doi.org/10.5194/cpd-11-1913-2015, 2015
Preprint withdrawn
D. C. Kitover, R. van Balen, D. M. Roche, J. Vandenberghe, and H. Renssen
Geosci. Model Dev., 8, 1445–1460, https://doi.org/10.5194/gmd-8-1445-2015, https://doi.org/10.5194/gmd-8-1445-2015, 2015
M. Bügelmayer, D. M. Roche, and H. Renssen
The Cryosphere, 9, 821–835, https://doi.org/10.5194/tc-9-821-2015, https://doi.org/10.5194/tc-9-821-2015, 2015
K. A. Crichton, D. M. Roche, G. Krinner, and J. Chappellaz
Geosci. Model Dev., 7, 3111–3134, https://doi.org/10.5194/gmd-7-3111-2014, https://doi.org/10.5194/gmd-7-3111-2014, 2014
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Permafrost is ground that remains frozen for two or more consecutive years. An estimated 50% of the global below-ground organic carbon is stored in soils of the permafrost zone. This study presents the development and validation of a simplified permafrost-carbon mechanism for the CLIMBER-2 model. Our model development allows, for the first time, the study of the role of permafrost soils in the global carbon cycle for long timescales and for coupled palaeoclimate Earth system modelling studies.
M. Guillevic, L. Bazin, A. Landais, C. Stowasser, V. Masson-Delmotte, T. Blunier, F. Eynaud, S. Falourd, E. Michel, B. Minster, T. Popp, F. Prié, and B. M. Vinther
Clim. Past, 10, 2115–2133, https://doi.org/10.5194/cp-10-2115-2014, https://doi.org/10.5194/cp-10-2115-2014, 2014
T. Caley, D. M. Roche, C. Waelbroeck, and E. Michel
Clim. Past, 10, 1939–1955, https://doi.org/10.5194/cp-10-1939-2014, https://doi.org/10.5194/cp-10-1939-2014, 2014
D. M. Roche, C. Dumas, M. Bügelmayer, S. Charbit, and C. Ritz
Geosci. Model Dev., 7, 1377–1394, https://doi.org/10.5194/gmd-7-1377-2014, https://doi.org/10.5194/gmd-7-1377-2014, 2014
L. S. Shumilovskikh, D. Fleitmann, N. R. Nowaczyk, H. Behling, F. Marret, A. Wegwerth, and H. W. Arz
Clim. Past, 10, 939–954, https://doi.org/10.5194/cp-10-939-2014, https://doi.org/10.5194/cp-10-939-2014, 2014
P. Beghin, S. Charbit, C. Dumas, M. Kageyama, D. M. Roche, and C. Ritz
Clim. Past, 10, 345–358, https://doi.org/10.5194/cp-10-345-2014, https://doi.org/10.5194/cp-10-345-2014, 2014
G. Milzer, J. Giraudeau, S. Schmidt, F. Eynaud, and J. Faust
Clim. Past, 10, 305–323, https://doi.org/10.5194/cp-10-305-2014, https://doi.org/10.5194/cp-10-305-2014, 2014
T. Caley, S. Zaragosi, J. Bourget, P. Martinez, B. Malaizé, F. Eynaud, L. Rossignol, T. Garlan, and N. Ellouz-Zimmermann
Biogeosciences, 10, 7347–7359, https://doi.org/10.5194/bg-10-7347-2013, https://doi.org/10.5194/bg-10-7347-2013, 2013
D. M. Roche
Geosci. Model Dev., 6, 1481–1491, https://doi.org/10.5194/gmd-6-1481-2013, https://doi.org/10.5194/gmd-6-1481-2013, 2013
D. M. Roche and T. Caley
Geosci. Model Dev., 6, 1493–1504, https://doi.org/10.5194/gmd-6-1493-2013, https://doi.org/10.5194/gmd-6-1493-2013, 2013
T. Caley and D. M. Roche
Geosci. Model Dev., 6, 1505–1516, https://doi.org/10.5194/gmd-6-1505-2013, https://doi.org/10.5194/gmd-6-1505-2013, 2013
C. V. Dylmer, J. Giraudeau, F. Eynaud, K. Husum, and A. De Vernal
Clim. Past, 9, 1505–1518, https://doi.org/10.5194/cp-9-1505-2013, https://doi.org/10.5194/cp-9-1505-2013, 2013
G. Milzer, J. Giraudeau, J. Faust, J. Knies, F. Eynaud, and C. Rühlemann
Biogeosciences, 10, 4433–4448, https://doi.org/10.5194/bg-10-4433-2013, https://doi.org/10.5194/bg-10-4433-2013, 2013
S. Charbit, C. Dumas, M. Kageyama, D. M. Roche, and C. Ritz
The Cryosphere, 7, 681–698, https://doi.org/10.5194/tc-7-681-2013, https://doi.org/10.5194/tc-7-681-2013, 2013
M. Kageyama, U. Merkel, B. Otto-Bliesner, M. Prange, A. Abe-Ouchi, G. Lohmann, R. Ohgaito, D. M. Roche, J. Singarayer, D. Swingedouw, and X Zhang
Clim. Past, 9, 935–953, https://doi.org/10.5194/cp-9-935-2013, https://doi.org/10.5194/cp-9-935-2013, 2013
Related subject area
Subject: Ocean Dynamics | Archive: Marine Archives | Timescale: Millenial/D-O
Leeuwin Current dynamics over the last 60 kyr – relation to Australian ecosystem and Southern Ocean change
Plateaus and jumps in the atmospheric radiocarbon record – potential origin and value as global age markers for glacial-to-deglacial paleoceanography, a synthesis
Millennial-scale variations in sedimentary oxygenation in the western subtropical North Pacific and its links to North Atlantic climate
Relative timing of precipitation and ocean circulation changes in the western equatorial Atlantic over the last 45 kyr
Regional seesaw between the North Atlantic and Nordic Seas during the last glacial abrupt climate events
Changes in the geometry and strength of the Atlantic meridional overturning circulation during the last glacial (20–50 ka)
Stratification of surface waters during the last glacial millennial climatic events: a key factor in subsurface and deep-water mass dynamics
Parallelisms between sea surface temperature changes in the western tropical Atlantic (Guiana Basin) and high latitude climate signals over the last 140 000 years
Thermal evolution of the western South Atlantic and the adjacent continent during Termination 1
Bottom water variability in the subtropical northwestern Pacific from 26 kyr BP to present based on Mg / Ca and stable carbon and oxygen isotopes of benthic foraminifera
Early deglacial Atlantic overturning decline and its role in atmospheric CO2 rise inferred from carbon isotopes (δ13C)
Millennial meridional dynamics of the Indo-Pacific Warm Pool during the last termination
Pulses of enhanced North Pacific Intermediate Water ventilation from the Okhotsk Sea and Bering Sea during the last deglaciation
Persistent millennial-scale link between Greenland climate and northern Pacific Oxygen Minimum Zone under interglacial conditions
Deglacial intermediate water reorganization: new evidence from the Indian Ocean
Water mass evolution of the Greenland Sea since late glacial times
Millennial-scale variability of marine productivity and terrigenous matter supply in the western Bering Sea over the past 180 kyr
Timing and magnitude of equatorial Atlantic surface warming during the last glacial bipolar oscillation
Dirk Nürnberg, Akintunde Kayode, Karl J. F. Meier, and Cyrus Karas
Clim. Past, 18, 2483–2507, https://doi.org/10.5194/cp-18-2483-2022, https://doi.org/10.5194/cp-18-2483-2022, 2022
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The Leeuwin Current to the west of Australia steers the heat exchange between the tropical and the subantarctic ocean areas. Its prominent variability during the last glacial effectively shaped the Australian ecosystem and was closely related to the dynamics of the Antarctic Circumpolar Current. At ~ 43 ka BP, the rapidly weakening Leeuwin Current, the ecological response in Australia, and human interference likely caused the extinction of the exotic Australian megafauna.
Michael Sarnthein, Kevin Küssner, Pieter M. Grootes, Blanca Ausin, Timothy Eglinton, Juan Muglia, Raimund Muscheler, and Gordon Schlolaut
Clim. Past, 16, 2547–2571, https://doi.org/10.5194/cp-16-2547-2020, https://doi.org/10.5194/cp-16-2547-2020, 2020
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The dating technique of 14C plateau tuning uses U/Th-based model ages, refinements of the Lake Suigetsu age scale, and the link of surface ocean carbon to the globally mixed atmosphere as basis of age correlation. Our synthesis employs data of 20 sediment cores from the global ocean and offers a coherent picture of global ocean circulation evolving over glacial-to-deglacial times on semi-millennial scales to be compared with climate records stored in marine sediments, ice cores, and speleothems.
Jianjun Zou, Xuefa Shi, Aimei Zhu, Selvaraj Kandasamy, Xun Gong, Lester Lembke-Jene, Min-Te Chen, Yonghua Wu, Shulan Ge, Yanguang Liu, Xinru Xue, Gerrit Lohmann, and Ralf Tiedemann
Clim. Past, 16, 387–407, https://doi.org/10.5194/cp-16-387-2020, https://doi.org/10.5194/cp-16-387-2020, 2020
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Large-scale reorganization of global ocean circulation has been documented in a variety of marine archives, including the enhanced North Pacific Intermediate Water NPIW. Our data support both the model- and data-based ideas that the enhanced NPIW mainly developed during cold spells, while an expansion of oxygen-poor zones occurred at warming intervals (Bölling-Alleröd).
Claire Waelbroeck, Sylvain Pichat, Evelyn Böhm, Bryan C. Lougheed, Davide Faranda, Mathieu Vrac, Lise Missiaen, Natalia Vazquez Riveiros, Pierre Burckel, Jörg Lippold, Helge W. Arz, Trond Dokken, François Thil, and Arnaud Dapoigny
Clim. Past, 14, 1315–1330, https://doi.org/10.5194/cp-14-1315-2018, https://doi.org/10.5194/cp-14-1315-2018, 2018
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Recording the precise timing and sequence of events is essential for understanding rapid climate changes and improving climate model predictive skills. Here, we precisely assess the relative timing between ocean and atmospheric changes, both recorded in the same deep-sea core over the last 45 kyr. We show that decreased mid-depth water mass transport in the western equatorial Atlantic preceded increased rainfall over the adjacent continent by 120 to 980 yr, depending on the type of climate event.
Mélanie Wary, Frédérique Eynaud, Didier Swingedouw, Valérie Masson-Delmotte, Jens Matthiessen, Catherine Kissel, Jena Zumaque, Linda Rossignol, and Jean Jouzel
Clim. Past, 13, 729–739, https://doi.org/10.5194/cp-13-729-2017, https://doi.org/10.5194/cp-13-729-2017, 2017
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The last glacial period was punctuated by abrupt climatic variations, whose cold atmospheric phases have been commonly associated with cold sea-surface temperatures and expansion of sea ice in the North Atlantic and adjacent seas. Here we provide direct evidence of a regional paradoxical see-saw pattern: cold Greenland and North Atlantic phases coincide with warmer sea-surface conditions and shorter seasonal sea-ice cover durations in the Norwegian Sea as compared to warm phases.
Pierre Burckel, Claire Waelbroeck, Yiming Luo, Didier M. Roche, Sylvain Pichat, Samuel L. Jaccard, Jeanne Gherardi, Aline Govin, Jörg Lippold, and François Thil
Clim. Past, 12, 2061–2075, https://doi.org/10.5194/cp-12-2061-2016, https://doi.org/10.5194/cp-12-2061-2016, 2016
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In this paper, we compare new and published Atlantic sedimentary Pa/Th data with Pa/Th simulated using stream functions generated under various climatic conditions. We show that during Greenland interstadials of the 20–50 ka period, the Atlantic meridional overturning circulation was very different from that of the Holocene. Moreover, southern-sourced waters dominated the Atlantic during Heinrich stadial 2, a slow northern-sourced water mass flowing above 2500 m in the North Atlantic.
M. Wary, F. Eynaud, M. Sabine, S. Zaragosi, L. Rossignol, B. Malaizé, E. Palis, J. Zumaque, C. Caulle, A. Penaud, E. Michel, and K. Charlier
Clim. Past, 11, 1507–1525, https://doi.org/10.5194/cp-11-1507-2015, https://doi.org/10.5194/cp-11-1507-2015, 2015
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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
O. Rama-Corredor, B. Martrat, J. O. Grimalt, G. E. López-Otalvaro, J. A. Flores, and F. Sierro
Clim. Past, 11, 1297–1311, https://doi.org/10.5194/cp-11-1297-2015, https://doi.org/10.5194/cp-11-1297-2015, 2015
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The alkenone sea surface temperatures in the Guiana Basin show a rapid transmission of the climate variability from arctic to tropical latitudes during the last two interglacials (MIS1 and MIS5e) and warm long interstadials (MIS5d-a). In contrast, the abrupt variability of the glacial interval does follow the North Atlantic climate but is also shaped by precessional changes. This arctic to tropical decoupling occurs when the Atlantic meridional overturning circulation is substantially reduced.
C. M. Chiessi, S. Mulitza, G. Mollenhauer, J. B. Silva, J. Groeneveld, and M. Prange
Clim. Past, 11, 915–929, https://doi.org/10.5194/cp-11-915-2015, https://doi.org/10.5194/cp-11-915-2015, 2015
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Here we show that temperatures in the western South Atlantic increased markedly during the major slowdown event of the Atlantic meridional overturning circulation (AMOC) of the last deglaciation. Over the adjacent continent, however, temperatures followed the rise in atmospheric carbon dioxide, lagging changes in oceanic temperature. Our records corroborate the notion that the long duration of the major slowdown event of the AMOC was fundamental in driving the Earth out of the last glacial.
Y. Kubota, K. Kimoto, T. Itaki, Y. Yokoyama, Y. Miyairi, and H. Matsuzaki
Clim. Past, 11, 803–824, https://doi.org/10.5194/cp-11-803-2015, https://doi.org/10.5194/cp-11-803-2015, 2015
A. Schmittner and D. C. Lund
Clim. Past, 11, 135–152, https://doi.org/10.5194/cp-11-135-2015, https://doi.org/10.5194/cp-11-135-2015, 2015
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Model simulations of carbon isotope changes as a result of a reduction in the Atlantic Meridional Overturning Circulation (AMOC) agree well with sediment data from the early last deglaciation, supporting the idea that the AMOC was substantially reduced during that time period of global warming. We hypothesize, and present supporting evidence, that changes in the AMOC may have caused the coeval rise in atmospheric CO2, owing to a reduction in the efficiency of the ocean's biological pump.
L. Lo, C.-C. Shen, K.-Y. Wei, G. S. Burr, H.-S. Mii, M.-T. Chen, S.-Y. Lee, and M.-C. Tsai
Clim. Past, 10, 2253–2261, https://doi.org/10.5194/cp-10-2253-2014, https://doi.org/10.5194/cp-10-2253-2014, 2014
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1. We have reconstructed new meridional thermal and precipitation stacked records in the Indo-Pacific Warm Pool (IPWP) during the last termination.
2. Meridional thermal gradient variations in the IPWP show tight links to the Northern Hemisphere millennial timescales event.
3. Anomalous warming in the south IPWP region could induce the southward shifting of the Intertropical Convergence Zone (ITCZ) in the IPWP during the Heinrich 1 and Younger Dryas events.
L. Max, L. Lembke-Jene, J.-R. Riethdorf, R. Tiedemann, D. Nürnberg, H. Kühn, and A. Mackensen
Clim. Past, 10, 591–605, https://doi.org/10.5194/cp-10-591-2014, https://doi.org/10.5194/cp-10-591-2014, 2014
O. Cartapanis, K. Tachikawa, O. E. Romero, and E. Bard
Clim. Past, 10, 405–418, https://doi.org/10.5194/cp-10-405-2014, https://doi.org/10.5194/cp-10-405-2014, 2014
S. Romahn, A. Mackensen, J. Groeneveld, and J. Pätzold
Clim. Past, 10, 293–303, https://doi.org/10.5194/cp-10-293-2014, https://doi.org/10.5194/cp-10-293-2014, 2014
M. M. Telesiński, R. F. Spielhagen, and H. A. Bauch
Clim. Past, 10, 123–136, https://doi.org/10.5194/cp-10-123-2014, https://doi.org/10.5194/cp-10-123-2014, 2014
J.-R. Riethdorf, D. Nürnberg, L. Max, R. Tiedemann, S. A. Gorbarenko, and M. I. Malakhov
Clim. Past, 9, 1345–1373, https://doi.org/10.5194/cp-9-1345-2013, https://doi.org/10.5194/cp-9-1345-2013, 2013
S. Weldeab
Clim. Past, 8, 1705–1716, https://doi.org/10.5194/cp-8-1705-2012, https://doi.org/10.5194/cp-8-1705-2012, 2012
Cited articles
Alley, R. B., Clark, P. U., Keigwin, L. D., and Webb, R. S.: Making sense of millennial-scale climate change, in: Mechanisms of global climate change at millennial time scales, edited by: Clark, P. U., Webb, R. S., and Keigwin, L. D., Geophys. Monogr., 385–394, 1999.
Alvarez-Solas, J., Charbit, S., Ritz, C., Paillard, D., Ramstein, G., and Dumas, C.: Links between ocean temperature and iceberg discharge during Heinrich events, Nat. Geosci., 3, 122–126, 2010.
Auffret, G. A., Boelaert, A., Vergnaud-Grazzini, C., Müller, C., and Kerbrat, R.: Identification of Heinrich layers in core ks 01 north-eastern Atlantic (46° N, 17° W), implications for their origin, Mar. Geol., 131, 5–20, 1996.
Austin, W. E. N. and Hibbert, F. D.: Tracing time in the ocean: A brief review of chronological constraints (60–8 kyr) on north atlantic marine event-based stratigraphies, Quaternary Sci. Rev., 36, 28–37, 2012.
Ballini, M., Kissel, C., Colin, C., and Richter, T.: Deep-water mass source and dynamic associated with rapid climatic variations during the last glacial stage in the north Atlantic: a multi-proxy investigation of the detrital fraction of deep-sea sediments, Geochem. Geophy. Geosy., 7, Q02N01, https://doi.org/10.1029/2005GC001070, 2006.
Bard, E.: Geochemical and geophysical implications of the radiocarbon calibration, Geochim. Cosmochim. Acta, 62, 2025–2038, 1998.
Bard, E., Arnold, M., Hamelin, B., Tisnerat-Laborde, N., and Cabioch, G.: Radiocarbon calibration by means of mass spectrometric 230Th/234U and 14C ages of corals. An updated data base including samples from Barbados, Mururoa and Tahiti, Radiocarbon, 40, 1085–1092, 1998.
Berger, A.: Les causes astronomiques des grandes variations du climat au Quaternaire, C. R. Palevol., 5, 21–26, 2006.
Bett, B. J.: UK atlantic margin environmental survey: introduction and overview of bathyal benthic ecology, Cont. Shelf Res., 21, 917–956, 2001.
Bogus, K. A., Zonneveld, K. A. F., Fischer, D., Kasten, S., Bohrmann, G., and Versteegh, G. J. M.: The effect of meter-scale lateral oxygen gradients at the sediment-water interface on selected organic matter based alteration, productivity and temperature proxies, Biogeosciences, 9, 1553–1570, https://doi.org/10.5194/bg-9-1553-2012, 2012.
Boldreel, L. O., Andersen, M. S., and Kuijpers, A.: Neogene seismic facies and deep-water gateways in the faeroe bank area, ne atlantic, Mar. Geol., 152, 129–140, 1998.
Bond, G. and Lotti, R.: Iceberg discharges into the north Atlantic on millennial time scales during the last glaciation, Science, 267, 1005–1010, 1995.
Bond, G., Heinrich, H., Broecker, W., Labeyrie, L., McManus, J., Andrews, J., Huon, S., Jantschik, R., Clasen, S., Simet, C., Tedesco, C., Klas, M., Bonani, G., and Ivy, S.: Evidence for massive discharges of icebergs into the north Atlantic ocean during the last glacial period, Nature, 360, 246–249, 1992.
Bond, G., Broecker, W., Johnsen, S., McManus, J., Labeyrie, L., Jouzel, J., and Bonani, G.: Correlations between climate records from North Atlantic sediments and Greenland ice, Nature, 365, 143–147, 1993.
Boulay, S.: Variabilité climatique rapide en atlantique nord - un potentiel de réponses: La carotte MD99-2281 (sud des îles faeroes), MASTER Université Paris-Sud, Orsay, 2000.
Bourillet, J.-F., Reynaud, J. Y., Baltzer, A., and Zaragosi, S.: The "fleuve manche": The sub-marine sedimentary features from the outer shelf to the deep-sea fans, J. Quaternay Sci., 18, 261–282, 2003.
Brachfeld, S., Kissel, C., Laj, C., and Mazaud, A.: Behavior of u-channels during acquisition and demagnetization of remanence: Implications for paleomagnetic and rock-magnetic measurements, Phys. Earth Planet. Int., 145, 1–8, 2004.
Bradwell, T., Stoker, M., and Larter, R.: Geomorphological signature and flow dynamics of the minch palaeo-ice stream, northwest Scotland, J. Quaternary Sci., 22, 609–617, 2007.
Bradwell, T., Stoker, M., Golledge, N. R., Wilson, C. K., Merritt, J. W., Long, D., Everest, J. D., Hestvik, O. B., Stevenson, A. G., Hubbard, A. L., Finlayson, A. G., and Mathers, H. E.: The northern sector of the last British ice sheet: Maximum extent and demise, Earth-Sci. Rev., 88, 207–226, 2008.
Broecker, W. S.: Thermohaline circulation, the Achilles heel of our climate system: Will man-made co2 upset the current balance?, Science, 278, 1582–1588, 1997.
Broecker, W. S.: Does the trigger for abrupt climate change reside in the ocean or in the atmosphere?, Science, 300, 1519–1522, 2003.
Bromwich, D. H., Chen, Q.-S., Li, Y., and Cullather, R. I.: Precipitation over Greenland and its relation to the north Atlantic oscillation, J. Geophys. Res., 104, 22103–22115, 1999.
Chiverrell, R. C. and Thomas, G. S. P.: Extent and timing of the last glacial maximum (LGM) in Britain and Ireland: A review, J. Quaternary Sci., 25, 535–549, 2010.
Clark, P. U., Pisias, N. G., Stocker, T. F., and Weaver, A. J.: The role of the thermohaline circulation in abrupt climate change, Nature, 415, 863–869, 2002.
Cortijo, E., Labeyrie, L., Vidal, L., Vautravers, M., Chapman, M., Duplessy, J. C., Elliot, M., Arnold, M., Turon, J. L., and Auffret, G. A.: Changes in sea surface hydrology associated with Heinrich event 4 in the north Atlantic ocean between 40° and 60° N, Earth Planet. Sc. Lett., 146, 29-45, 1997.
Dansgaard, W., Johnsen, S. J., Clausen, H. B., Dahl-Jengen, D., Gundestrup, N. S., Hammer, C. U., Hvidberg, C. S., Steffensen, J. P., Sveinbjörnsdottir, A. E., Jouzel, J., and Bond, G.: Evidence for general instability of past climate from 250-kyr ice-core record, Nature, 364, 218–220, 1993.
De Leeuw, J. W., Versteegh, G. J. M., and Van Bergen, P. F.: Biomacromolecules of algae and plants and their fossil analogues, Plant Ecol., 182, 209–233, 2006.
de Vernal, A.: Dino8 workshop: Quantitative treatments for paleoceanographical reconstructions based on dinocyst assemblages, Dino8 conference, Montréal, 2008.
de Vernal, A. and Marret, F.: Chapter nine : Organic-walled dinoflagellate cysts: tracers of sea-surface conditions, in: Developments in marine geology, edited by: Hillaire-Marcel, C. and de Vernal, A., Elsevier, 371–408, 2007.
de Vernal, A. and Rochon, A.: Dinocysts as tracers of sea-surface conditions and sea-ice cover in polar and subpolar environments, IOP Conference Series: Earth and Environmental Science, 2011.
de Vernal, A., Henry, M., and Bilodeau, G.: Techniques de préparation et d'analyse en micropaléontologie, Les cahiers du GEOTOP, 3, 1–29, 1996.
de Vernal, A., Hillaire-Marcel, C., Turon, J. L., and Matthiessen, J.: Reconstruction of sea-surface temperature, salinity, and sea-ice cover in the northern north Atlantic during the last glacial maximum based on dinocyst assemblages, Can. J. Earth Sci., 37, 725–750, 2000.
de Vernal, A., Henry, M., Matthiessen, J., Mudie, P. J., Rochon, A., Boessenkool, K. P., Eynaud, F., Grãsfjeld, K., Guiot, J., Hamel, D., Harland, R., Head, M. J., Kunz-Pirrung, M., Levac, E., Loucheur, V., Peyron, O., Pospelova, V., Radi, T., Turon, J. L., and Voronina, E.: Dinoflagellate cyst assemblages in surface sediments of the Laptev sea region (Arctic Ocean) and their relationship to hydrographic conditions, J. Quaternary Sci., 16, 637–649, 2001.
de Vernal, A., Eynaud, F., Henry, M., Hillaire-Marcel, C., Londeix, L., Mangin, S., Matthiessen, J., Marret, F., Radi, T., Rochon, A., Solignac, S., and Turon, J. L.: Reconstruction of sea-surface conditions at middle to high latitudes of the northern hemisphere during the last glacial maximum (LGM) based on dinoflagellate cyst assemblages, Quaternary Sci. Rev., 24, 897–924, 2005.
de Vernal, A., Rosell-Melé, A., Kucera, M., Hillaire-Marcel, C., Eynaud, F., Weinelt, M., Dokken, T., and Kageyama, M.: Comparing proxies for the reconstruction of LGM sea-surface conditions in the northern north Atlantic, Quaternary Sci. Rev., 25, 2820–2834, 2006.
Dickson, R. R., Meincke, J., Malmberg, S.-A., and Lee, A. J.: The "Great salinity anomaly" in the northern north Atlantic 1968–1982, Prog. Oceanogr., 20, 103–151, 1988.
Ehlers, J. and Gibbard, P.: Quaternary glaciations - extent and chronology part I: Europe, in: Developments in quaternary science, no. 2, Publisher Elsevier, Amsterdam, p. 488, 2004.
Elliot, M., Labeyrie, L., Dokken, T., and Manthe, S.: Coherent patterns of ice-rafted debris deposits in the Nordic regions during the last glacial (10–60 ka), Earth Planet. Sc. Lett., 194, 151–163, 2001.
Ericson, D. B.: Coiling direction of Globigerina pachyderma as a climatic index, Science, 130, 219–220, 1959.
Evitt, W. R.: Sporopollenin dinoflagellate cysts: their morphology and interpretation, AASP Foundation – American Association of Stratigraphic Palynologists, Dallas, 1985.
Eynaud, F.: Kystes de dinoflagellés et evolution paléoclimatique et paléohydrologique de l'atlantique nord au cours du dernier cycle climatique du quaternaire, Université de Bordeaux I, 291 pp., 1999.
Eynaud, F., Turon, J. L., Matthiessen, J., Kissel, C., Peypouquet, J. P., De Vernal, A., and Henry, M.: Norwegian sea-surface palaeoenvironments of marine oxygen-isotope state 3: the paradoxical response of dinoflagellate cysts, J. Quaternary Sci., 17, 349–359, 2002.
Eynaud, F., Zaragosi, S., Scourse, J. D., Mojtahid, M., Bourillet, J. F., Hall, I. R., Penaud, A., Locascio, M., and Reijonen, A.: Deglacial laminated facies on the NW European continental margin: The hydrographic significance of British-Irish Ice Sheet deglaciation and Fleuve Manche paleoriver discharges, Geochem. Geophy. Geosy., 8, Q06019, https://doi.org/10.1029/2006GC001496, 2007.
Eynaud, F., De Abreu, L., Voelker, A., Schönfeld, J., Salgueiro, E., Turon, J. L., Penaud, A., Toucanne, S., Naughton, F., Sanchez Goni, M. F., Malaizé, B., and Cacho, I.: Position of the polar front along the western Iberian margin during key cold episodes of the last 45 ka, Geochem. Geophy. Geosy., 10, Q07U05, https://doi.org/10.1029/2009GC002398, 2009.
Eynaud, F., Malaizé, B., Zaragosi, S., de Vernal, A., Scourse, J., Pujol, C., Cortijo, E., Grousset, F. E., Penaud, A., Toucanne, S., Turon, J. L., and Auffret, G.: New constraints on European glacial freshwater releases to the North Atlantic Ocean, Geophys. Res. Lett., 39, L15601, https://doi.org/10.1029/2012GL052100, 2012.
Fogelqvist, E., Blindheim, J., Tanhua, T., Østerhus, S., Buch, E., and Rey, F.: Greenland-Scotland overflow studied by hydro-chemical multivariate analysis, Deep-Sea Res. Pt. I, 50, 73–102, 2003.
Grosswald, M. G. and Hughes, T. J.: The russian component of an arctic ice sheet during the last glacial maximum, Quaternary Sci. Rev., 21, 121–146, 2002.
Grousset, F., Pujol, C., Labeyrie, L., Auffret, G. A., and Boelaert, A.: Were the North Atlantic Heinrich events triggered by the behavior of the European ice sheet?, Geology, 28, 123–126, 2000.
Grousset, F. E., Cortijo, E., Huon, S., Hervé, L., Richter, T., Burdloff, D., Duprat, J., and Weber, O.: Zooming in on Heinrich layers, Paleoceanography, 16, 240–259, 2001.
Grützner, J. and Higgins, S. M.: Threshold behavior of millennial scale variability in deep water hydrography inferred froma 1.1 Ma long record of sediment provenance at the southern Gardar Drift, Paleoceanography, 25, PA4204, https://doi.org/10.1029/2009PA001873, 2010.
Guiot, J. and de Vernal, A.: Chapter thirteen transfer functions: Methods for quantitative paleoceanography based on microfossils, in: Developments in marine geology, edited by: Hillaire-Marcel, C. and de Vernal, A., Elsevier, Amsterdam, 523–563, 2007.
Guiot, J. and de Vernal, A.: Is spatial autocorrelation introducing biases in the apparent accuracy of paleoclimatic reconstructions?, Quaternary Sci. Rev., 30, 1965–1972, 2011a.
Guiot, J. and de Vernal, A.: QSR correspondence "Is spatial autocorrelation introducing biases in the apparent accuracy of palaeoclimatic reconstructions?" Reply to Telford and Birks, Quaternary Sci. Rev., 30, 3214–3216, 2011b.
Hall, I. R., E. Colmenero-Hidalgo, R. Zahn, V. L. Peck, and S. R. Hemming: Centennial- to millennial-scale ice-ocean interactions in the subpolar northeast Atlantic 18–41 kyr ago, Paleoceanography, 26, PA2224, https://doi.org/10.1029/2010PA002084, 2011.
Harland, R.: Distribution maps of recent dinoflagellate cysts in bottom sediments from the north Atlantic Ocean and adjacent seas, Palaeontology, 26, 321–387, 1983.
Heinrich, H.: Origin and consequences of cyclic ice rafting in the northeast Atlantic Ocean during the past 130,000 years, Quaternary Res., 29, 142–152, 1988.
Hemming, S. R.: Heinrich events: massive late Pleistocene detritus layers of the north Atlantic and their global climate imprint, Rev. Geophys., 42, 1001–1043, 2004.
Hibbert, F. D., Austin, W. E. N., Leng, M. J., and Gatliff, R. W.: British ice sheet dynamics inferred from north Atlantic ice-rafted debris records spanning the last 175 000 years, J. Quaternary Sci., 25, 461–482, 2010.
Hodell, D. A., Channell, J. E. T., Curtis, J. H., Romero, O. E., and Röhl, U.: Onset of "Hudson Strait" Heinrich events in the eastern North Atlantic at the end of the middle Pleistocene transition ( 640 ka)?, Paleoceanography, 23, PA4218, https://doi.org/10.1029/2008PA001591, 2008.
Holliday, N. P., Pollard, R. T., Read, J. F., and Leach, H.: Water mass properties and fluxes in the Rockall trough, 1975–1998, Deep-Sea Res. Pt. I, 47, 1303–1332, 2000.
Howe, J. A., Stoker, M. S., Masson, D. G., Pudsey, C. J., Morris, P., Larter, R. D., and Bulat, J.: Seabed morphology and the bottom-current pathways around rosemary bank seamount, northern Rockall trough, north Atlantic, Mar. Petrol. Geol., 23, 165–181, 2006.
Hulbe, C. L., MacAyeal, D. R., Denton, G. H., Kleman, J., and Lowell, T. V.: Catastrophic ice shelf breakup as the source of Heinrich event icebergs, Paleoceanography, 19, 711–717, 2004.
Imbrie, J., Berger, A., Boyle, E. A., Clemens, S. C., Duffy, A., Howard, W. R., Kukla, G., Kutzbach, J., Martinson, D. G., McIntyre, A., Mix, A. C., Molfino, B., Morley, J. J., Peterson, L. C., Pisias, N. G., Prell, W. L., Raymo, M. E., Shackleton, N. J., and Toggweiler, J. R.: On the structure and origin of major glaciation cycles: 2. The 100,000 year cycle, Paleoceanography, 8, 699–735, 1993.
Jonkers, L., Moros, M., Prins, M. A., Dokken, T., Andersson Dahl, C., Dijkstra, N., Perner, K., and Brummer, G.-J. A.: A reconstruction of sea surface warming in the northern north Atlantic during MIS3 ice-rafting events, Quaternary Sci. Rev., 29, 1791–1800, 2010a.
Jonkers, L., Brummer, G. J. A., and De Jong, M. F.: Seasonal stratification, shell flux, and oxygen isotope dynamics of left coiling N. pachyderma and T. quinqueloba in the western subpolar north Atlantic, Paleoceanography, 25, PA2204, https://doi.org/10.1029/2009PA001849, 2010b.
Kiefer, T., Lorenz, S., Schulz, M., Lohmann, G., Sarnthein, M., and Elderfield, H.: Response of precipitation over Greenland and the adjacent ocean to the north pacific warm spells during Dansgaard-Oeschger stadials, Terra Nova, 14, 295–300, 2002.
Kissel, C., Laj, C., Labeyrie, L., Dokken, T., Voelker, A., and Blamart, D.: Rapid climatic variations during marine isotopic stage 3: Magnetic analysis of sediments from Nordic seas and north Atlantic, Earth Planet. Sc. Lett., 171, 489–502, 1999a.
Kissel, C., Laj, C., Labeyrie, L., Dokken, T., Voelker, A., and Blamart, D.: Magnetic signature of rapid climatic variations in North Atlantic sediments, in: Reconstructing Ocean History: A Window Into the Future, edited by: Abrantes, F. and Mix, A., Springer, New York, 419–437, 1999b.
Knutz, P. C., Austin, W. E. N., and Jones, E. J. W.: Millennial-scale depositional cycles related to British ice sheet variability and north Atlantic paleocirculation since 45 kyr B.P., Barra fan, U.K. Margin, Paleoceanography, 16, 53–64, 2001.
Kucera, M.: Chapter six: planktonic foraminifera as tracers of past oceanic environments, in: Developments in Marine Geology, Elsevier, Amsterdam, 213–262, 2007.
Kucera, M., Rosell-Melé, A., Schneider, R., Waelbroeck, C., and Weinelt, M.: Multiproxy approach for the reconstruction of the glacial ocean surface (MARGO), Quaternary Sci. Rev., 24, 813–819, 2005.
Kuijpers, A., Andersen, M. S., Kenyon, N. H., Kunzendorf, H., and van Weering, T. C. E.: Quaternary sedimentation and Norwegian sea overflow pathways around bill bailey bank, northeastern Atlantic, Mar. Geol., 152, 101–127, 1998.
Kuijpers, A., Hansen, B., Huhnerbach, V., Larsen, B., Nielsen, T., and Werner, F.: Norwegian sea overflow through the Faroe-Shetland gateway as documented by its bedforms, Mar. Geol., 188, 147–164, 2002.
Labeyrie, L., Cortijo, E., and Jansen, E.: Rapport scientifique de la mission INTERPOLE MD99-114/812 IMAGES V, Brest, 1999.
Laj, C., Kissel, C., Mazaud, A., Channell, J. E. T., and Beer, J.: North Atlantic Paleointensity Stack since 75 ka (NAPIS-75) and the duration of the Laschamp event, Philos. T. Roy. Soc. Lond., 358, 1009–1025, 2000.
Lang, C., Leuenberger, M., Schwander, J., and Johnsen, S.: 16 °C rapid temperature variation in central Greenland 70,000 years ago, Science, 1286, 934–937, 1999.
Larsen, K. M. H., Hansen, B., and Svendsen, H.: Faroe shelf water, Cont. Shelf Res., 28, 1754–1768, 2008.
Larsen, K. M. H., Hansen, B., and Svendsen, H.: The Faroe shelf front: Properties and exchange, J. Mar. Syst., 78, 9–17, 2009.
Lericolais, G., Auffret, J.-P., and Bourillet, J.-F.: The Quaternary Channel River: seismic stratigraphy of its palaeo-valleys and deeps, J. Quaternary Sci., 18, 245–260, 2003.
Marret, F. and Zonneveld, K. A. F.: Atlas of modern organic-walled dinoflagellate cyst distribution, Rev. Palaeobot. Palynol., 125, 1–200, 2003.
Martinson, D. G., Pisias, N. G., Hays, J. D., Imbrie, J., Moore Jr., T. C., and Shackleton, N. J.: Age dating and the orbital theory of the ice ages: Development of a high-resolution 0 to 300,000-year chronostratigraphy, Quaternary Res., 27, 1–29, 1987.
Masson, D. G., Howe, J. A., and Stoker, M. S.: Bottom-current sediment waves, sediment drifts and contourites in the northern Rockall trough, Mar. Geol., 192, 215–237, 2002.
Matthiessen, J., Kunz-Pirrung, M., and Mudie, P. J.: Freshwater chlorophycean algae in recent marine sediments of the Beaufort, Laptev and Kara seas (Arctic ocean) as indicators of river runoff, Int. J. Earth Sci., 89, 470–485, 2000.
Ménot, G., Bard, E., Rostek, F., Weijers, J. W. H., Hopmans, E. C., Schouten, S., and Sinninghe-Damsté, J. S.: Early reactivation of European rivers during the last deglaciation, Science, 313, 1623–1625, 2006.
Mertens, K. N., Verhoeven, K., Verleye, T., Louwye, S., Amorim, A., Ribeiro, S., Deaf, A. S., Harding, I., De Schepper, S., Kodrans-Nsiah, M., de Vernal, A., Radi, T., Dybkjaer, K., Poulsen, N. E., Feist-burkhardt, S., Chitolie, J., González Arango, C., Heilmann-Clausen, C., Londeix, L., Turon, J.-L., Marret, F., Matthiessen, J., McCarthy, F. M. G., Prasad, V., Pospelova, V., Kyffin Hughes, J. E., Riding, J. B., Rochon, A., Sangiorgi, F., Welters, N., Sinclair, N., Thun, C., Soliman, A., Van Nieuwenhove, N., Vink, A., and Young, M.: Determining the absolute abundance of dinoflagellate cysts in recent marine sediments: The Lycopodium marker-grain method put to the test, Rev. Palaeobot. Palynol., 157, 238–252, 2009.
Mix, A. E., Bard, E., and Schneider, R.: Environmental processes of the ice age: Land, ocean, glacier (EPILOG), Quaternary Sci. Rev., 20, 627–657, 2001.
Mojtahid, M., Eynaud, F., Zaragosi, S., Scourse, J., Bourillet, J. F., and Garlan, T.: Palaeoclimatology and palaeohydrography of the glacial stages on Celtic and Armorican margins over the last 360 000 yrs, Mar. Geol., 224, 57–82, 2005.
New, A. L. and Smythe-Wright, D.: Aspects of the circulation in the Rockall trough, Cont. Shelf Res., 21, 777–810, 2001.
Penaud, A.: Interactions climatiques et hydrologiques du système Méditerranée/Atlantique au Quaternaire, PhD thesis, Bordeaux, 2009.
Penaud, A., Eynaud, F., Turon, J. L., Zaragosi, S., Malaizé, B., Toucanne, S., and Bourillet, J. F.: What forced the collapse of European ice sheets during the last two glacial periods (150 ka B.P. and 18 ka cal B.P.)? Palynological evidence, Palaeogeogr. Palaeocl., 281, 66–78, 2009.
Platov, G. A.: Numerical modeling of the arctic ocean deepwater formation: Part II. Results of regional and global experiments, Izvestiya, Atmos. Ocean. Phys., 47, 377–392, 2011.
Rahmstorf, S.: Ocean circulation and climate during the past 120,000 years, Nature, 419, 207–214, 2002.
Rasmussen, S. O., Seierstad, I. K., Andersen, K. K., Bigler, M., Dahl-Jansen, D., and Johnsen, S. J.: Synchronization of the NGRIP, GRIP, and GISP2 ice cores across MIS 2 and palaeoclimatic implications, Quaternary Sci. Rev., 27, 18–28, 2008.
Rasmussen, T. L. and Thomsen, E.: The role of the north Atlantic drift in the millennial timescale glacial climate fluctuations, Palaeogeogr. Palaeocl., 210, 101–116, 2004.
Rasmussen, T. L. and Thomsen, E.: Warm Atlantic water inflow to the Nordic seas 34–10 ka calibrated ka BP, Paleoceanography, 23, PA1201, https://doi.org/10.1029/2007PA001453, 2008.
Rasmussen, T. L., Vanweering, T. C. E., and Labeyrie, L.: High resolution stratigraphy of the Faeroe-Shetland channel and its relation to north Atlantic paleoceanography: The last 87 kyr, Mar. Geol., 131, 75–88, 1996a.
Rasmussen, T. L., Thomsen, E., Vanweering, T. C. E., and Labeyrie, L.: Rapid changes in surface and deep water conditions at the Faeroe margin during the last 58,000 years, Paleoceanography, 11, 757–771, 1996b.
Rasmussen, T. L., Van weering, T. C. E., and Labeyrie, L.: Climatic instability, ice sheets and ocean dynamics at high northern latitudes during the last glacial period (58–10 ka BP), Quaternary Sci. Rev., 16, 71–80, 1997.
Rasmussen, T. L., Thomsen, E., Troelstra, S. R., Kuijpers, A., and Prins, M. A.: Millennial-scale glacial variability versus Holocene stability: Changes in planktic and benthic foraminifera faunas and ocean circulation in the north Atlantic during the last 60000 years, Mar. Micropaleontol., 47, 143–176, 2002a.
Rasmussen, T. L., Bäckström, D., Heinemeier, J., Klitgaard-Kristensen, D., Knutz, P. C., Kuijpers, A., Lassen, S., Thomsen, E., Troelstra, S. R., and van Weering, T. C. E.: The faroe- shetland gateway: Late quaternary water mass exchange between the nordic seas and the northeastern atlantic, Mar. Geol., 188, 165–192, 2002b.
Richter, T. O., Van Der Gaast, S., Koster, B., Vaars, A., Gieles, R., de Stigter, H. C., de Haas, H., and Van Weering, T. C. E.: The AVAATECH XRF core scanner: Technical description and applications to NE Atlantic sediments, in: New techniques in sediment core analysis, edited by: Rothwell, R. G., Geological Society Special Publications, London, 39–50, 2006.
Roche, D. M., Wiersma, A. P., and Renssen, H.: A systematic study of the impact of freshwater pulses with respect to different geographical locations, Clim. Dynam., 34, 997–1013, 2010.
Rochon, A., de Vernal, A., Turon, J.-L., Matthiessen, J., and Head, M. J.: Recent dinoflagellate cysts of the north Atlantic ocean and adjacent seas in relation to sea-surface parameters, edited by: Ser, A. C., AASP – American Association of Stratigraphic Palynologists, Contrib. Ser., Dallas, 1–152, 1999a.
Rochon, A., de Vernal, A., Turon, J.-L., Matthiessen, J., and Head, M. J.: Distribution of dinoflagellate cysts in surface sediments from the north Atlantic ocean and adjacent basins and quantitative reconstruction of sea-surface parameters, AASP special pub., p. 146, 1999b.
Rochon, A., Eynaud, F., and de Vernal, A.: Dinocysts as tracers of hydrographical conditions and productivity along the ocean margins: Introduction, Mar. Micropaleontol., 68, 1-5, 2008.
Rohling, E. J., Grant, K., Bolshaw, M., Roberts, A. P., Siddall, M., Hemleben, C., and Kucera, M.: Antarctic temperature and global sea level closely coupled over the past five glacial cycles, Nat. Geosci., 2.7, 500–504, 2009.
Ruddiman, W. F.: Late Quaternary deposition of ice-rafted sand in the subpolar North Atlantic (lat 40° to 65° N), GSA Bulletin, 88, 1813–1827, 1977.
Sánchez Goñi, M. F. and Harrison, S. P.: Global patterns of vegetation response to millennial-scale variability and rapid climate change during the last glacial period, Quaternary Sci. Rev., 29, 2957–2980, 2010.
Sánchez-Goñi, M. F., Landais, A., Fletcher, W. J., Naughton, F., Desprat, S., and Duprat, J.: Contrasting impacts of dansgaard-oeschger events over a western european latitudinal transect modulated by orbital parameters, Quaternary Sci. Rev., 27, 1136–1151, 2008.
Schulz, M.: On the 1470-year pacing of Dansgaard-Oeschger warm events, Paleoceanography, 17, 1014, https://doi.org/10.1029/2000PA000571, 2002.
Scourse, J. D., Hall, I. R., McCave, I. N., Young, J. R., and Sugdon, C.: The origin of Heinrich layers: Evidence from h2 for European precursor events, Earth Planet. Sc. Lett., 182, 187–195, 2000.
Scourse, J. D., Haapaniemi, A. L., Colmenero-Hidalgo, E., Peck, V. L., Hall, I. R., Austin, W. E. N., Knutz, P. C., and Zahn, R.: Growth, dynamics and deglaciation of the last British-Irish ice sheet: The deep-sea ice rafted detritus record, Quaternary Sci. Rev., 28, 3066–3084, 2009.
Severinghaus, J. P. and Brook, E. J.: Abrupt climate change at the end of the last glacial period inferred from trapped air in polar ice, Science, 286, 930–934, 1999.
Siddall, M. et al.: Red Sea Sea Level Reconstruction, IGBP PAGES/World Data Center for Paleoclimatology Data Contribution Series # 2006-063, NOAA/NCDC Paleoclimatology Program, Boulder CO, USA. 2006.
Snoeckx, H., Grousset, F. E., Revel, M., and Boelaert, A.: European contribution of ice-rafted sand to Heinrich layers H3 and H4, Mar. Geol., 158, 197–208, 1999.
Stoner, J. S., Channell, J. E. T., Hillaire-Marcel, C., and Kissel, C.: Geomagnetic paleointensity and environmental record from Labrador sea core MD95-2024: Global marine sediment and ice core chronostratigraphy for the last 110 kyr, Earth Planet. Sc. Lett., 183, 161–177, 2000.
Svensson, A., Andersen, K. K., Bigler, M., Clausen, H. B., Dahl-Jensen, D., Davies, S. M., Johnsen, S. J., Muscheler, R., Parrenin, F., Rasmussen, S. O., Röthlisberger, R., Seierstad, I., Steffensen, J. P., and Vinther, B. M.: A 60 000 year Greenland stratigraphic ice core chronology, Clim. Past, 4, 47–57, https://doi.org/10.5194/cp-4-47-2008, 2008.
Toucanne, S., Zaragosi, S., Bourillet, J. F., Marieu, V., Cremer, M., Kageyama, M., Van Vliet-Lanoé, B., Eynaud, F., Turon, J. L., and Gibbard, P. L.: The first estimation of fleuve manche palaeoriver discharge during the last deglaciation: Evidence for Fennoscandian ice sheet meltwater flow in the English channel ca 20–18 ka ago, Earth Planet. Sc. Lett., 290, 459–473, 2010.
Van Kreveld, S., Sarnthein, M., Erlenkeuser, H., Grootes, P., Jung, S., Nadeau, M. J., Pflaumann, U., and Voelker, A.: Potential links between surging ice sheets, circulation changes, and the Dansgaard-Oeschger cycles in the Irmiger Sea, 60–80 kyr, Paleoceanography, 15, 425–442, 2000.
Versteegh, G. J. M., Blokker, P. K. B., Harding, I., Lewis, J., Oltmanns, S., Rochon, A., and Zonneveld, K. A. F.: Infra red spectroscopy, flash pyrolysis, thermally assisted hydrolysis and methylation (THM) in the presence of tetramethylammonium hydroxide (TMAH) of cultured and sediment-derived Lingulodinium polyedrum (Dinoflagellata) cyst walls, Org. Geochem., 43, 92–102, 2012.
Voelker, A. H. L.: Global distribution of centennial-scale records for marine isotope stage (MIS) 3: a database, Quaternary Sci. Rev., 21, 1185–1212, 2002.
Wagner, G., Beer, J., Laj, C., Kissel, C., Mazarik, J., Muscheler, R., and Synal, H.-A.: Chlorine-36 evidence for the mono lake event in the summit grip ice core, Earth Planet. Sc. Lett., 181, 1–6, 2000.
WOA – World Ocean Atlas: general information available at: http://www.nodc.noaa.gov/OC5/, sampling tool: http://www.geo.uni-bremen.de/geomod/staff/csn/woasample.html (last access: 31 July 2012), 1998.
Wolff, E. W., Chappellaz, J., Blunier, T., Rasmussen, S. O., and Svensson, A.: Millennial-scale variability during the last glacial: The ice core record, Quaternary Sci. Rev., 29, 2828–2838, 2010.
Zaragosi, S., Eynaud, F., Pujol, C., Auffret, G. A., Turon, J. L., and Garlan, T.: Initiation of the European deglaciation as recorded in the north-western Bay of Biscay slope environments (Meriadzek terrace and Trevelyan escarpment): A multi-proxy approach, Earth Planet. Sc. Lett., 188, 493–507, 2001.
Zonneveld, K. A. F., Bockelmann, F., and Holzwarth, U.: Selective preservation of organic-walled dinoflagellate cysts as a tool to quantify past net primary production and bottom water oxygen concentrations, Mar. Geol., 237, 109–126, 2007.