Articles | Volume 18, issue 8
https://doi.org/10.5194/cp-18-1815-2022
© Author(s) 2022. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/cp-18-1815-2022
© Author(s) 2022. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
10 Aug 2022
Research article |
| 10 Aug 2022
| 10 Aug 2022
Compilation of Southern Ocean sea-ice records covering the last glacial-interglacial cycle (12–130 ka)
Matthew Chadwick
CORRESPONDING AUTHOR
British Antarctic Survey, Cambridge, UK
Xavier Crosta
UMR 5805 EPOC, Université de Bordeaux, CNRS, EPHE, Pessac, France
Oliver Esper
Alfred Wegner Institute, Helmholtz Centre for Polar and Marine
Research, Bremerhaven, Germany
Lena Thöle
Department of Earth Sciences, Utrecht University, Utrecht, the
Netherlands
Karen E. Kohfeld
School of Resource and Environmental Management, Simon Fraser
University, Vancouver, Canada
School of Environmental Science, Simon Fraser University, Vancouver, Canada
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Xavier Crosta, Karen E. Kohfeld, Helen C. Bostock, Matthew Chadwick, Alice Du Vivier, Oliver Esper, Johan Etourneau, Jacob Jones, Amy Leventer, Juliane Müller, Rachael H. Rhodes, Claire S. Allen, Pooja Ghadi, Nele Lamping, Carina B. Lange, Kelly-Anne Lawler, David Lund, Alice Marzocchi, Katrin J. Meissner, Laurie Menviel, Abhilash Nair, Molly Patterson, Jennifer Pike, Joseph G. Prebble, Christina Riesselman, Henrik Sadatzki, Louise C. Sime, Sunil K. Shukla, Lena Thöle, Maria-Elena Vorrath, Wenshen Xiao, and Jiao Yang
Clim. Past, 18, 1729–1756, https://doi.org/10.5194/cp-18-1729-2022, https://doi.org/10.5194/cp-18-1729-2022, 2022
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Despite its importance in the global climate, our knowledge of Antarctic sea-ice changes throughout the last glacial–interglacial cycle is extremely limited. As part of the Cycles of Sea Ice Dynamics in the Earth system (C-SIDE) Working Group, we review marine- and ice-core-based sea-ice proxies to provide insights into their applicability and limitations. By compiling published records, we provide information on Antarctic sea-ice dynamics over the past 130 000 years.
Matthew Chadwick, Claire S. Allen, Louise C. Sime, Xavier Crosta, and Claus-Dieter Hillenbrand
Clim. Past, 18, 129–146, https://doi.org/10.5194/cp-18-129-2022, https://doi.org/10.5194/cp-18-129-2022, 2022
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Algae preserved in marine sediments have allowed us to reconstruct how much winter sea ice was present around Antarctica during a past time period (130 000 years ago) when the climate was warmer than today. The patterns of sea-ice increase and decrease vary between different parts of the Southern Ocean. The Pacific sector has a largely stable sea-ice extent, whereas the amount of sea ice in the Atlantic sector is much more variable with bigger decreases and increases than other regions.
Eleanor Simpson, Debby Ianson, Karen E. Kohfeld, Ana C. Franco, Paul A. Covert, Marty Davelaar, and Yves Perreault
Biogeosciences, 21, 1323–1353, https://doi.org/10.5194/bg-21-1323-2024, https://doi.org/10.5194/bg-21-1323-2024, 2024
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Shellfish aquaculture operates in nearshore areas where data on ocean acidification parameters are limited. We show daily and seasonal variability in pH and saturation states of calcium carbonate at nearshore aquaculture sites in British Columbia, Canada, and determine the contributing drivers of this variability. We find that nearshore locations have greater variability than open waters and that the uptake of carbon by phytoplankton is the major driver of pH and saturation state variability.
Wee Wei Khoo, Juliane Müller, Oliver Esper, Wenshen Xiao, Christian Stepanek, Paul Gierz, Gerrit Lohmann, Walter Geibert, Jens Hefter, and Gesine Mollenhauer
EGUsphere, https://doi.org/10.5194/egusphere-2024-246, https://doi.org/10.5194/egusphere-2024-246, 2024
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Using a multiproxy approach, we analyzed biomarkers and diatom assemblages from a marine sediment core from the Powell Basin, Weddell Sea. The results reveal the first continuous coastal Antarctic sea ice record since the Last Penultimate Glacial. Our findings contribute valuable insights into past glacial-interglacial sea ice response to a changing climate and enhance our understanding of the ocean-sea ice-ice shelf interactions and dynamics.
Isabel A. Dove, Ian W. Bishop, Xavier Crosta, Natascha Riedinger, R. Patrick Kelly, and Rebecca S. Robinson
EGUsphere, https://doi.org/10.5194/egusphere-2023-2564, https://doi.org/10.5194/egusphere-2023-2564, 2023
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The diatom-bound nitrogen isotope proxy is used to study how efficiently diatoms in the Southern Ocean help to remove CO2 from the atmosphere, but may be biased by different diatom species. We examine a specific type of diatom, Chaetoceros resting spores (CRS), commonly preserved in Southern Ocean sediments. We find that CRS record surprisingly low δ15NDB values compared to other diatoms, yet changes in their relative abundance over time does not significantly bias previously published records.
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.
Maria-Elena Vorrath, Juliane Müller, Paola Cárdenas, Thomas Opel, Sebastian Mieruch, Oliver Esper, Lester Lembke-Jene, Johan Etourneau, Andrea Vieth-Hillebrand, Niko Lahajnar, Carina B. Lange, Amy Leventer, Dimitris Evangelinos, Carlota Escutia, and Gesine Mollenhauer
Clim. Past, 19, 1061–1079, https://doi.org/10.5194/cp-19-1061-2023, https://doi.org/10.5194/cp-19-1061-2023, 2023
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Sea ice is important to stabilize the ice sheet in Antarctica. To understand how the global climate and sea ice were related in the past we looked at ancient molecules (IPSO25) from sea-ice algae and other species whose dead cells accumulated on the ocean floor over time. With chemical analyses we could reconstruct the history of sea ice and ocean temperatures of the past 14 000 years. We found out that sea ice became less as the ocean warmed, and more phytoplankton grew towards today's level.
Stephen G. Chastain, Karen E. Kohfeld, Marlow G. Pellatt, Carolina Olid, and Maija Gailis
Biogeosciences, 19, 5751–5777, https://doi.org/10.5194/bg-19-5751-2022, https://doi.org/10.5194/bg-19-5751-2022, 2022
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Salt marshes are thought to be important carbon sinks because of their ability to store carbon in their soils. We provide the first estimates of how much blue carbon is stored in salt marshes on the Pacific coast of Canada. We find that the carbon stored in the marshes is low compared to other marshes around the world, likely because of their young age. Still, the high marshes take up carbon at rates faster than the global average, making them potentially important carbon sinks in the future.
Helen Eri Amsler, Lena Mareike Thöle, Ingrid Stimac, Walter Geibert, Minoru Ikehara, Gerhard Kuhn, Oliver Esper, and Samuel Laurent Jaccard
Clim. Past, 18, 1797–1813, https://doi.org/10.5194/cp-18-1797-2022, https://doi.org/10.5194/cp-18-1797-2022, 2022
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We present sedimentary redox-sensitive trace metal records from five sediment cores retrieved from the SW Indian Ocean. These records are indicative of oxygen-depleted conditions during cold periods and enhanced oxygenation during interstadials. Our results thus suggest that deep-ocean oxygenation changes were mainly controlled by ocean ventilation and that a generally more sluggish circulation contributed to sequestering remineralized carbon away from the atmosphere during glacial periods.
Xavier Crosta, Karen E. Kohfeld, Helen C. Bostock, Matthew Chadwick, Alice Du Vivier, Oliver Esper, Johan Etourneau, Jacob Jones, Amy Leventer, Juliane Müller, Rachael H. Rhodes, Claire S. Allen, Pooja Ghadi, Nele Lamping, Carina B. Lange, Kelly-Anne Lawler, David Lund, Alice Marzocchi, Katrin J. Meissner, Laurie Menviel, Abhilash Nair, Molly Patterson, Jennifer Pike, Joseph G. Prebble, Christina Riesselman, Henrik Sadatzki, Louise C. Sime, Sunil K. Shukla, Lena Thöle, Maria-Elena Vorrath, Wenshen Xiao, and Jiao Yang
Clim. Past, 18, 1729–1756, https://doi.org/10.5194/cp-18-1729-2022, https://doi.org/10.5194/cp-18-1729-2022, 2022
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Despite its importance in the global climate, our knowledge of Antarctic sea-ice changes throughout the last glacial–interglacial cycle is extremely limited. As part of the Cycles of Sea Ice Dynamics in the Earth system (C-SIDE) Working Group, we review marine- and ice-core-based sea-ice proxies to provide insights into their applicability and limitations. By compiling published records, we provide information on Antarctic sea-ice dynamics over the past 130 000 years.
Ryan A. Green, Laurie Menviel, Katrin J. Meissner, Xavier Crosta, Deepak Chandan, Gerrit Lohmann, W. Richard Peltier, Xiaoxu Shi, and Jiang Zhu
Clim. Past, 18, 845–862, https://doi.org/10.5194/cp-18-845-2022, https://doi.org/10.5194/cp-18-845-2022, 2022
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Climate models are used to predict future climate changes and as such, it is important to assess their performance in simulating past climate changes. We analyze seasonal sea-ice cover over the Southern Ocean simulated from numerical PMIP3, PMIP4 and LOVECLIM simulations during the Last Glacial Maximum (LGM). Comparing these simulations to proxy data, we provide improved estimates of LGM seasonal sea-ice cover. Our estimate of summer sea-ice extent is 20 %–30 % larger than previous estimates.
Jacob Jones, Karen E. Kohfeld, Helen Bostock, Xavier Crosta, Melanie Liston, Gavin Dunbar, Zanna Chase, Amy Leventer, Harris Anderson, and Geraldine Jacobsen
Clim. Past, 18, 465–483, https://doi.org/10.5194/cp-18-465-2022, https://doi.org/10.5194/cp-18-465-2022, 2022
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We provide new winter sea ice and summer sea surface temperature estimates for marine core TAN1302-96 (59° S, 157° E) in the Southern Ocean. We find that sea ice was not consolidated over the core site until ~65 ka and therefore believe that sea ice may not have been a major contributor to early glacial CO2 drawdown. Sea ice does appear to have coincided with Antarctic Intermediate Water production and subduction, suggesting it may have influenced intermediate ocean circulation changes.
Matthew Chadwick, Claire S. Allen, Louise C. Sime, Xavier Crosta, and Claus-Dieter Hillenbrand
Clim. Past, 18, 129–146, https://doi.org/10.5194/cp-18-129-2022, https://doi.org/10.5194/cp-18-129-2022, 2022
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Algae preserved in marine sediments have allowed us to reconstruct how much winter sea ice was present around Antarctica during a past time period (130 000 years ago) when the climate was warmer than today. The patterns of sea-ice increase and decrease vary between different parts of the Southern Ocean. The Pacific sector has a largely stable sea-ice extent, whereas the amount of sea ice in the Atlantic sector is much more variable with bigger decreases and increases than other regions.
Kelly-Anne Lawler, Giuseppe Cortese, Matthieu Civel-Mazens, Helen Bostock, Xavier Crosta, Amy Leventer, Vikki Lowe, John Rogers, and Leanne K. Armand
Earth Syst. Sci. Data, 13, 5441–5453, https://doi.org/10.5194/essd-13-5441-2021, https://doi.org/10.5194/essd-13-5441-2021, 2021
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Radiolarians found in marine sediments are used to reconstruct past Southern Ocean environments. This requires a comprehensive modern dataset. The Southern Ocean Radiolarian (SO-RAD) dataset includes radiolarian counts from sites in the Southern Ocean. It can be used for palaeoceanographic reconstructions or to study modern species diversity and abundance. We describe the data collection and include recommendations for users unfamiliar with procedures typically used by the radiolarian community.
Kate E. Ashley, Xavier Crosta, Johan Etourneau, Philippine Campagne, Harry Gilchrist, Uthmaan Ibraheem, Sarah E. Greene, Sabine Schmidt, Yvette Eley, Guillaume Massé, and James Bendle
Biogeosciences, 18, 5555–5571, https://doi.org/10.5194/bg-18-5555-2021, https://doi.org/10.5194/bg-18-5555-2021, 2021
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We explore the potential for the use of carbon isotopes of algal fatty acid as a new proxy for past primary productivity in Antarctic coastal zones. Coastal polynyas are hotspots of primary productivity and are known to draw down CO2 from the atmosphere. Reconstructions of past productivity changes could provide a baseline for the role of these areas as sinks for atmospheric CO2.
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.
Kate E. Ashley, Robert McKay, Johan Etourneau, Francisco J. Jimenez-Espejo, Alan Condron, Anna Albot, Xavier Crosta, Christina Riesselman, Osamu Seki, Guillaume Massé, Nicholas R. Golledge, Edward Gasson, Daniel P. Lowry, Nicholas E. Barrand, Katelyn Johnson, Nancy Bertler, Carlota Escutia, Robert Dunbar, and James A. Bendle
Clim. Past, 17, 1–19, https://doi.org/10.5194/cp-17-1-2021, https://doi.org/10.5194/cp-17-1-2021, 2021
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We present a multi-proxy record of Holocene glacial meltwater input, sediment transport, and sea-ice variability off East Antarctica. Our record shows that a rapid Antarctic sea-ice increase during the mid-Holocene (~ 4.5 ka) occurred against a backdrop of increasing glacial meltwater input and gradual climate warming. We suggest that mid-Holocene ice shelf cavity expansion led to cooling of surface waters and sea-ice growth, which slowed basal ice shelf melting.
Maria-Elena Vorrath, Juliane Müller, Lorena Rebolledo, Paola Cárdenas, Xiaoxu Shi, Oliver Esper, Thomas Opel, Walter Geibert, Práxedes Muñoz, Christian Haas, Gerhard Kuhn, Carina B. Lange, Gerrit Lohmann, and Gesine Mollenhauer
Clim. Past, 16, 2459–2483, https://doi.org/10.5194/cp-16-2459-2020, https://doi.org/10.5194/cp-16-2459-2020, 2020
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We tested the applicability of the organic biomarker IPSO25 for sea ice reconstructions in the industrial era at the western Antarctic Peninsula. We successfully evaluated our data with satellite sea ice observations. The comparison with marine and ice core records revealed that sea ice interpretations must consider climatic and sea ice dynamics. Sea ice biomarker production is mainly influenced by the Southern Annular Mode, while the El Niño–Southern Oscillation seems to have a minor impact.
Lisa Claire Orme, Xavier Crosta, Arto Miettinen, Dmitry V. Divine, Katrine Husum, Elisabeth Isaksson, Lukas Wacker, Rahul Mohan, Olivier Ther, and Minoru Ikehara
Clim. Past, 16, 1451–1467, https://doi.org/10.5194/cp-16-1451-2020, https://doi.org/10.5194/cp-16-1451-2020, 2020
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A record of past sea temperature in the Indian sector of the Southern Ocean, spanning the last 14 200 years, has been developed by analysis of fossil diatoms in marine sediment. During the late deglaciation the reconstructed temperature changes were highly similar to those over Antarctica, most likely due to a reorganisation of global ocean and atmospheric circulation. During the last 11 600 years temperatures gradually cooled and became increasingly variable.
Maria-Elena Vorrath, Juliane Müller, Oliver Esper, Gesine Mollenhauer, Christian Haas, Enno Schefuß, and Kirsten Fahl
Biogeosciences, 16, 2961–2981, https://doi.org/10.5194/bg-16-2961-2019, https://doi.org/10.5194/bg-16-2961-2019, 2019
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The study highlights new approaches in the investigation of past sea ice in Antarctica to reconstruct the climate conditions in earth's history and reveal its future development under global warming. We examined the distribution of organic remains from different algae at the Western Antarctic Peninsula and compared it to fossil and satellite records. We evaluated IPSO25 – the sea ice proxy for the Southern Ocean with 25 carbon atoms – as a useful tool for sea ice reconstructions in this region.
Stephanie C. Hunter, Diana M. Allen, and Karen E. Kohfeld
Clim. Past Discuss., https://doi.org/10.5194/cp-2019-68, https://doi.org/10.5194/cp-2019-68, 2019
Manuscript not accepted for further review
Stephen G. Chastain, Karen Kohfeld, and Marlow G. Pellatt
Biogeosciences Discuss., https://doi.org/10.5194/bg-2018-166, https://doi.org/10.5194/bg-2018-166, 2018
Revised manuscript not accepted
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We generated estimates of carbon stocks and accumulation rates in soils of salt marshes from Clayoquot Sound on the west coast of Canada. Following established methodologies, we sampled seven sites to generate a regional average estimate and compared it with global marsh carbon data. Our results show the marshes as highly efficient carbon accumulation
hotspots, comparable with those from elsewhere on the NE Pacific coast or similar latitude ranges.
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.
Philippine Campagne, Xavier Crosta, Sabine Schmidt, Marie Noëlle Houssais, Olivier Ther, and Guillaume Massé
Biogeosciences, 13, 4205–4218, https://doi.org/10.5194/bg-13-4205-2016, https://doi.org/10.5194/bg-13-4205-2016, 2016
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Diatoms and biomarkers have been recently used for palaeoclimate reconstructions in the Southern Ocean. Few sediment-based ecological studies have investigated their relationships with environmental conditions. Here, we compare high-resolution sedimentary records with meteorological data to study relationships between our proxies and recent atmospheric and sea surface changes. Our results indicate that coupled wind pattern and sea surface variability act as the proximal forcing at that scale.
S. Albani, N. M. Mahowald, G. Winckler, R. F. Anderson, L. I. Bradtmiller, B. Delmonte, R. François, M. Goman, N. G. Heavens, P. P. Hesse, S. A. Hovan, S. G. Kang, K. E. Kohfeld, H. Lu, V. Maggi, J. A. Mason, P. A. Mayewski, D. McGee, X. Miao, B. L. Otto-Bliesner, A. T. Perry, A. Pourmand, H. M. Roberts, N. Rosenbloom, T. Stevens, and J. Sun
Clim. Past, 11, 869–903, https://doi.org/10.5194/cp-11-869-2015, https://doi.org/10.5194/cp-11-869-2015, 2015
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We propose an innovative framework to organize paleodust records, formalized in a publicly accessible database, and discuss the emerging properties of the global dust cycle during the Holocene by integrating our analysis with simulations performed with the Community Earth System Model. We show how the size distribution of dust is intrinsically related to the dust mass accumulation rates and that only considering a consistent size range allows for a consistent analysis of the global dust cycle.
H. Kuehn, L. Lembke-Jene, R. Gersonde, O. Esper, F. Lamy, H. Arz, G. Kuhn, and R. Tiedemann
Clim. Past, 10, 2215–2236, https://doi.org/10.5194/cp-10-2215-2014, https://doi.org/10.5194/cp-10-2215-2014, 2014
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Annually laminated sediments from the NE Bering Sea reveal a decadal-scale correlation to Greenland ice core records during termination I, suggesting an atmospheric teleconnection. Lamination occurrence is tightly coupled to Bølling-Allerød and Preboreal warm phases. Increases in export production, closely coupled to SST and sea ice changes, are hypothesized to be a main cause of deglacial anoxia, rather than changes in overturning/ventilation rates of mid-depth waters entering the Bering Sea.
J. Etourneau, L. G. Collins, V. Willmott, J.-H. Kim, L. Barbara, A. Leventer, S. Schouten, J. S. Sinninghe Damsté, A. Bianchini, V. Klein, X. Crosta, and G. Massé
Clim. Past, 9, 1431–1446, https://doi.org/10.5194/cp-9-1431-2013, https://doi.org/10.5194/cp-9-1431-2013, 2013
P. Mathiot, H. Goosse, X. Crosta, B. Stenni, M. Braida, H. Renssen, C. J. Van Meerbeeck, V. Masson-Delmotte, A. Mairesse, and S. Dubinkina
Clim. Past, 9, 887–901, https://doi.org/10.5194/cp-9-887-2013, https://doi.org/10.5194/cp-9-887-2013, 2013
Related subject area
Subject: Ice Dynamics | Archive: Marine Archives | Timescale: Pleistocene
Ice-proximal sea-ice reconstruction in Powell Basin, Antarctica since the Last Interglacial
Sea ice and productivity changes over the last glacial cycle in the Adélie Land region, East Antarctica, based on diatom assemblage variability
Reconstructing Antarctic winter sea-ice extent during Marine Isotope Stage 5e
Reconstructing the evolution of ice sheets, sea level, and atmospheric CO2 during the past 3.6 million years
The De Long Trough: a newly discovered glacial trough on the East Siberian continental margin
Sedimentary record from the Canada Basin, Arctic Ocean: implications for late to middle Pleistocene glacial history
A Late Pleistocene sea level stack
Sea level ~400 000 years ago (MIS 11): analogue for present and future sea-level?
Wee Wei Khoo, Juliane Müller, Oliver Esper, Wenshen Xiao, Christian Stepanek, Paul Gierz, Gerrit Lohmann, Walter Geibert, Jens Hefter, and Gesine Mollenhauer
EGUsphere, https://doi.org/10.5194/egusphere-2024-246, https://doi.org/10.5194/egusphere-2024-246, 2024
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Using a multiproxy approach, we analyzed biomarkers and diatom assemblages from a marine sediment core from the Powell Basin, Weddell Sea. The results reveal the first continuous coastal Antarctic sea ice record since the Last Penultimate Glacial. Our findings contribute valuable insights into past glacial-interglacial sea ice response to a changing climate and enhance our understanding of the ocean-sea ice-ice shelf interactions and dynamics.
Lea Pesjak, Andrew McMinn, Zanna Chase, and Helen Bostock
Clim. Past, 19, 419–437, https://doi.org/10.5194/cp-19-419-2023, https://doi.org/10.5194/cp-19-419-2023, 2023
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This study uses diatom assemblages, biogenic silica and Si/Al data over the last 140 kyr from core TAN1302-44 (64°54' S, 144°32' E) to define glacial-to-interglacial paleoenvironments near Antarctica with respect to sea ice duration and ocean circulation. It has found that the sea ice season increased gradually during the last glacial, reaching a maximum before decreasing at the end of MIS 2. Following this, Circumpolar Deep Water increased relative to other times prior to ice sheet retreat.
Matthew Chadwick, Claire S. Allen, Louise C. Sime, Xavier Crosta, and Claus-Dieter Hillenbrand
Clim. Past, 18, 129–146, https://doi.org/10.5194/cp-18-129-2022, https://doi.org/10.5194/cp-18-129-2022, 2022
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Algae preserved in marine sediments have allowed us to reconstruct how much winter sea ice was present around Antarctica during a past time period (130 000 years ago) when the climate was warmer than today. The patterns of sea-ice increase and decrease vary between different parts of the Southern Ocean. The Pacific sector has a largely stable sea-ice extent, whereas the amount of sea ice in the Atlantic sector is much more variable with bigger decreases and increases than other regions.
Constantijn J. Berends, Bas de Boer, and Roderik S. W. van de Wal
Clim. Past, 17, 361–377, https://doi.org/10.5194/cp-17-361-2021, https://doi.org/10.5194/cp-17-361-2021, 2021
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For the past 2.6 million years, the Earth has experienced glacial cycles, where vast ice sheets periodically grew to cover large parts of North America and Eurasia. In the earlier part of this period, this happened every 40 000 years. This value changed 1.2 million years ago to 100 000 years: the Mid-Pleistocene Transition. We investigate this interesting period using an ice-sheet model, studying the interactions between ice sheets and the global climate.
Matt O'Regan, Jan Backman, Natalia Barrientos, Thomas M. Cronin, Laura Gemery, Nina Kirchner, Larry A. Mayer, Johan Nilsson, Riko Noormets, Christof Pearce, Igor Semiletov, Christian Stranne, and Martin Jakobsson
Clim. Past, 13, 1269–1284, https://doi.org/10.5194/cp-13-1269-2017, https://doi.org/10.5194/cp-13-1269-2017, 2017
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Past glacial activity on the East Siberian continental margin is poorly known, partly due to the lack of geomorphological evidence. Here we present geophysical mapping and sediment coring data from the East Siberian shelf and slope revealing the presence of a glacially excavated cross-shelf trough reaching to the continental shelf edge north of the De Long Islands. The data provide direct evidence for extensive glacial activity on the Siberian shelf that predates the Last Glacial Maximum.
Linsen Dong, Yanguang Liu, Xuefa Shi, Leonid Polyak, Yuanhui Huang, Xisheng Fang, Jianxing Liu, Jianjun Zou, Kunshan Wang, Fuqiang Sun, and Xuchen Wang
Clim. Past, 13, 511–531, https://doi.org/10.5194/cp-13-511-2017, https://doi.org/10.5194/cp-13-511-2017, 2017
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In this manuscript, we present the results of our study conducted for a sediment core (ARC4-BN05) collected in the Arctic Ocean. Detailed examination of clay and bulk mineralogy along with grain size, content of Ca and Mn, and planktonic foraminiferal numbers in core ARC4–BN05 provides important new information about sedimentary environments and provenance. Based on these proxies, we try to reveal late to middle Pleistocene glacial history.
Rachel M. Spratt and Lorraine E. Lisiecki
Clim. Past, 12, 1079–1092, https://doi.org/10.5194/cp-12-1079-2016, https://doi.org/10.5194/cp-12-1079-2016, 2016
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This study presents an average of seven Late Pleistocene sea level records, which improves the signal-to-noise ratio for estimates of sea level change during glacial cycles of the past 800 000 years.
D. Q. Bowen
Clim. Past, 6, 19–29, https://doi.org/10.5194/cp-6-19-2010, https://doi.org/10.5194/cp-6-19-2010, 2010
Cited articles
Allen, C. S., Pike, J., and Pudsey, C. J.: Last glacial–interglacial sea-ice cover in the SW Atlantic and its potential role in global deglaciation, Quaternary Sci. Rev., 30, 2446–2458, 2011.
Arrigo, K. R.: Sea ice ecosystems, Annu. Rev. Mar. Sci., 6, 439–467, 2014.
Arrigo, K. R., van Dijken, G. L., and Bushinsky, S.: Primary production in
the Southern Ocean, 1997–2006, J. Geophys. Res., 113, C08004, https://doi.org/10.1029/2007JC004551, 2008.
Bazin, L., Landais, A., Lemieux-Dudon, B., Toyé Mahamadou Kele, H.,
Veres, D., Parrenin, F., Martinerie, P., Ritz, C., Capron, E., Lipenkov, V.,
Loutre, M. F., Raynaud, D., Vinther, B., Svensson, A., Rasmussen, S. O.,
Severi, M., Blunier, T., Leuenberger, M., Fischer, H., Masson-Delmotte, V.,
Chappellaz, J., and Wolff, E.: Carbon dioxide composite data on AICC2012
chronology, PANGAEA, https://doi.org/10.1594/PANGAEA.824893, 2013a.
Bazin, L., Landais, A., Lemieux-Dudon, B., Toyé Mahamadou Kele, H., Veres, D., Parrenin, F., Martinerie, P., Ritz, C., Capron, E., Lipenkov, V., Loutre, M.-F., Raynaud, D., Vinther, B., Svensson, A., Rasmussen, S. O., Severi, M., Blunier, T., Leuenberger, M., Fischer, H., Masson-Delmotte, V., Chappellaz, J., and Wolff, E.: An optimized multi-proxy, multi-site Antarctic ice and gas orbital chronology (AICC2012): 120–800 ka, Clim. Past, 9, 1715–1731, https://doi.org/10.5194/cp-9-1715-2013, 2013b.
Belt, S. T.: Source-specific biomarkers as proxies for Arctic and Antarctic
sea ice, Org. Geochem., 125, 277–298, 2018.
Benz, V., Esper, O., Gersonde, R., Lamy, F., and Tiedemann, R.: Last Glacial
Maximum sea surface temperature and sea-ice extent in the Pacific sector of
the Southern Ocean, Quaternary Sci. Rev., 146, 216–237, 2016.
Bianchi, C. and Gersonde, R.: The Southern Ocean surface between Marine
Isotope Stages 6 and 5d: Shape and timing of climate changes,
Palaeogeogr. Palaeocl., 187, 151–177, 2002.
Bintanja, R., van Oldenborgh, G. J., Drijfhout, S. S., Wouters, B., and
Katsman, C. A.: Important role for ocean warming and increased ice-shelf
melt in Antarctic sea-ice expansion, Nat. Geosci., 6, 376–379, 2013.
Bouttes, N., Paillard, D., and Roche, D. M.: Impact of brine-induced stratification on the glacial carbon cycle, Clim. Past, 6, 575–589, https://doi.org/10.5194/cp-6-575-2010, 2010.
Capron, E., Govin, A., Stone, E. J., Masson-Delmotte, V., Mulitza, S.,
Otto-Bliesner, B., Rasmussen, T. L., Sime, L. C., Waelbroeck, C., and Wolff,
E. W.: Temporal and spatial structure of multi-millennial temperature
changes at high latitudes during the Last Interglacial, Quaternary Sci. Rev., 103, 116–133, 2014.
Chadwick, M., Allen, C. S., Sime, L. C., and Hillenbrand, C. D.: Analysing
the timing of peak warming and minimum winter sea-ice extent in the Southern
Ocean during MIS 5e, Quaternary Sci. Rev., 229, 106134, https://doi.org/10.1016/j.quascirev.2019.106134, 2020.
Chadwick, M., Sime, L. C., Allen, C. S., Guarino, M.-V., and Oliver, K. I.
C.: Model-data comparison of Antarctic winter sea-ice extent and Southern
Ocean sea-surface temperatures during MIS 5e, Earth Planet. Sci. Lett., in review, 2022a.
Chadwick, M., Crosta, X., Esper, O., and Kohfeld, K. E.: Southern Ocean marine sediment core sea-ice records for the last 150 000 years, PANGAEA [data set], https://doi.org/10.1594/PANGAEA.943275, 2022b.
Collins, L. G., Pike, J., Allen, C. S., and Hodgson, D. A.: High-resolution
reconstruction of southwest Atlantic sea-ice and its role in the carbon
cycle during marine isotope stages 3 and 2, Paleoceanography, 27, PA3217, https://doi.org/10.1029/2011pa002264,
2012.
Collins, L. G., Allen, C. S., Pike, J., Hodgson, D. A., Weckström, K.,
and Massé, G.: Evaluating highly branched isoprenoid (HBI) biomarkers as
a novel Antarctic sea-ice proxy in deep ocean glacial age sediments,
Quaternary Sci. Rev., 79, 87–98, 2013.
Crosta, X., Pichon, J. J., and Burckle, L. H.: Application of modern analog
technique to marine Antarctic diatoms: Reconstruction of maximum sea-ice
extent at the Last Glacial Maximum, Paleoceanography, 13, 284–297, 1998.
Crosta, X., Sturm, A., Armand, L., and Pichon, J.-J.: Late Quaternary sea
ice history in the Indian sector of the Southern Ocean as recorded by diatom
assemblages, Mar. Micropaleontol., 50, 209–223, 2004.
Crosta, X., Kohfeld, K. E., Bostock, H. C., Chadwick, M., Du Vivier, A., Esper, O., Etourneau, J., Jones, J., Leventer, A., Müller, J., Rhodes, R. H., Allen, C. S., Ghadi, P., Lamping, N., Lange, C., Lawler, K.-A., Lund, D., Marzocchi, A., Meissner, K. J., Menviel, L., Nair, A., Patterson, M., Pike, J., Prebble, J. G., Riesselman, C., Sadatzki, H., Sime, L. C., Shukla, S. K., Thöle, L., Vorrath, M.-E., Xiao, W., and Yang, J.: Antarctic sea ice over the past 130,000 years, Part 1: A review of what proxy records tell us, EGUsphere [preprint], https://doi.org/10.5194/egusphere-2022-99, 2022.
De Schepper, S., Ray, J. L., Skaar, K. S., Sadatzki, H., Ijaz, U. Z., Stein,
R., and Larsen, A.: The potential of sedimentary ancient DNA for
reconstructing past sea ice evolution, ISME J., 13, 2566–2577, 2019.
Esper, O. and Gersonde, R.: New tools for the reconstruction of Pleistocene
Antarctic sea ice, Palaeogeog. Palaeocl., 399,
260–283, 2014.
Ferrari, R., Jansen, M. F., Adkins, J. F., Burke, A., Stewart, A. L., and
Thompson, A. F.: Antarctic sea ice control on ocean circulation in present
and glacial climates, P. Natl. Acad. Sci. USA, 111, 8753–8758, 2014.
Ferreira, D., Marshall, J., Bitz, C. M., Solomon, S., and Plumb, A.:
Antarctic Ocean and Sea Ice Response to Ozone Depletion: A Two-Time-Scale
Problem, J. Climate, 28, 1206–1226, 2015.
Ferry, A. J., Crosta, X., Quilty, P. G., Fink, D., Howard, W., and Armand,
L. K.: First records of winter sea ice concentration in the southwest
Pacific sector of the Southern Ocean, Paleoceanography, 30, 1525–1539,
2015a.
Ferry, A. J., Prvan, T., Jersky, B., Crosta, X., and Armand, L. K.:
Statistical modeling of Southern Ocean marine diatom proxy and winter sea
ice data: Model comparison and developments, Prog. Oceanogr., 131,
100–112, 2015b.
Fetterer, F., Knowles, K., Meier, W. N., Savoie, M., and Windnagel, A. K.:
Sea Ice Index, Version 3. NSIDC: National Snow and Ice Data Center, Boulder,
Colorado USA, https://doi.org/10.7265/N5K072F8, 2017.
Fischer, H., Fundel, F., Ruth, U., Twarloh, B., Wegner, A., Udisti, R.,
Becagli, S., Castellano, E., Morganti, A., Severi, M., Wolff, E., Littot,
G., Röthlisberger, R., Mulvaney, R., Hutterli, M. A., Kaufmann, P.,
Federer, U., Lambert, F., Bigler, M., Hansson, M., Jonsell, U., de Angelis,
M., Boutron, C., Siggaard-Andersen, M.-L., Steffensen, J. P., Barbante, C.,
Gaspari, V., Gabrielli, P., and Wagenbach, D.: Reconstruction of millennial
changes in dust emission, transport and regional sea ice coverage using the
deep EPICA ice cores from the Atlantic and Indian Ocean sector of
Antarctica, Earth Planet. Sc. Lett., 260, 340–354, 2007.
Frank, M., Gersonde, R., Rutgers van der Loeff, M., Kuhn, G., and Mangini,
A.: Late Quaternary sediment dating and quantification of lateral sediment
redistribution applying 230Thex: a study from the eastern Atlantic sector of
the Southern Ocean, Geol. Rundsch., 85, 544–566, 1996.
Frontier, S.: Étude de la décroissance des valeurs propres dans une
analyse en composantes principales: comparaison avec le modèle du
bâton brisé, J. Exp. Mar. Biol. Ecol., 25, 67–75, 1976.
Galbraith, E. and de Lavergne, C.: Response of a comprehensive climate model
to a broad range of external forcings: relevance for deep ocean ventilation
and the development of late Cenozoic ice ages, Clim. Dynam., 52,
653–679, 2019.
Gersonde, R. and Zielinski, U.: The reconstruction of late Quaternary
Antarctic sea-ice distribution – the use of diatoms as a proxy for sea-ice,
Palaeogeogr. Palaeocl., 162, 263–286, 2000.
Gersonde, R., Crosta, X., Abelmann, A., and Armand, L.: Sea-surface
temperature and sea ice distribution of the Southern Ocean at the EPILOG
Last Glacial Maximum – a circum-Antarctic view based on siliceous
microfossil records, Quaternary Sci. Rev., 24, 869–896, 2005.
Ghadi, P., Nair, A., Crosta, X., Mohan, R., Manoj, M. C., and Meloth, T.:
Antarctic sea-ice and palaeoproductivity variation over the last
156 000 years in the Indian sector of Southern Ocean, Mar.
Micropaleontol., 160, 101894, https://doi.org/10.1016/j.marmicro.2020.101894, 2020.
Green, R. A., Menviel, L., Meissner, K. J., Crosta, X., Chandan, D., Lohmann, G., Peltier, W. R., Shi, X., and Zhu, J.: Evaluating seasonal sea-ice cover over the Southern Ocean at the Last Glacial Maximum, Clim. Past, 18, 845–862, https://doi.org/10.5194/cp-18-845-2022, 2022.
Hall, A.: The Role of Surface Albedo Feedback in Climate, J.
Climate, 17, 1550–1568, 2004.
Hammer, O., Harper, D. A. T., and Ryan, P. D.: Past: Paleontological
Statistics Software Package for Education and Data Analysis, Palaeontologica
Electronica, 4, 9, http://palaeo-electronica.org/2001_1/past/issue1_01.htm (last access: 3 August 2022), 2001.
Holland, P. R. and Kwok, R.: Wind-driven trends in Antarctic sea-ice drift,
Nat. Geosci., 5, 872–875, 2012.
Holloway, M. D., Sime, L. C., Allen, C. S., Hillenbrand, C.-D., Bunch, P.,
Wolff, E., and Valdes, P. J.: The spatial structure of the 128 ka Antarctic
sea ice minimum, Geophys. Res. Lett., 44, 11129–11139, 2017.
Jones, J., Kohfeld, K. E., Bostock, H., Crosta, X., Liston, M., Dunbar, G., Chase, Z., Leventer, A., Anderson, H., and Jacobsen, G.: Sea ice changes in the southwest Pacific sector of the Southern Ocean during the last 140 000 years, Clim. Past, 18, 465–483, https://doi.org/10.5194/cp-18-465-2022, 2022.
Jouzel, J., Masson-Delmotte, V., Cattani, O., Dreyfus, G., Falourd, S.,
Hoffmann, G., Minster, B., Nouet, J., Barnola, J.-M., Chappellaz, J.,
Fischer, H., Gallet, J. C., Johnsen, S. J., Leuenberger, M., Loulergue, L.,
Luethi, D., Oerter, H., Parrenin, F., Raisbeck, G., Raynaud, D., Schilt, A.,
Schwander, J., Selmo, E., Souchez, R., Spahni, R., Stauffer, B., Steffensen,
J. P., Stenni, B., Stocker, T. F., Tison, J.-L., Werner, M., and Wolff, E.
W.: Orbital and Millennial Antarctic Climate Variability over the Past
800 000 Years, Science, 317, 793–796, 2007.
Kohfeld, K. E. and Chase, Z.: Temporal evolution of mechanisms controlling
ocean carbon uptake during the last glacial cycle, Earth Planet.
Sci. Lett., 472, 206–215, 2017.
Kohfeld, K. E., Bostock, H. C., Crosta, X., Leventer, A., Meissner, K.,
Chadwick, M., Lowe, V., Jaccard, S. L., Skinner, L., Chase, Z., Marzocchi,
A., Thöle, L., Mix, A., Lund, D., Menviel, L., Sime, L. C., Missiaen,
L., Lawler, K.-A., Sikes, E., Eby, M., and Zickfield, K.: Past changes in
Antarctic sea ice, Part 2: Implications for ocean circulation,
biogeochemical cycling, and global climate, in preparation, 2022.
Kwok, R., Pang, S. S., and Kacimi, S.: Sea ice drift in the Southern Ocean:
Regional patterns, variability, and trends, Elem. Sci. Anth., 5, 1–16, 2017.
Lamping, N., Müller, J., Hefter, J., Mollenhauer, G., Haas, C., Shi, X., Vorrath, M.-E., Lohmann, G., and Hillenbrand, C.-D.: Evaluation of lipid biomarkers as proxies for sea ice and ocean temperatures along the Antarctic continental margin, Clim. Past, 17, 2305–2326, https://doi.org/10.5194/cp-17-2305-2021, 2021.
Lecomte, O., Goosse, H., Fichefet, T., de Lavergne, C., Barthelemy, A., and
Zunz, V.: Vertical ocean heat redistribution sustaining sea-ice
concentration trends in the Ross Sea, Nat. Commun., 8, 258, https://doi.org/10.1038/s41467-017-00347-4, 2017.
Leventer, A.: The fate of Antarctic “sea ice diatoms” and their use as
paleoenvironmental indicators, in: Antarctic Sea-ice, Biological Processes,
Interactions and Variability, edited by: Lizotte, M. P. and Arrigo, K. R.,
Antarctic Research Series, American Geophysical Union, Washington D.C., USA, 73, 121–137, https://agupubs.onlinelibrary.wiley.com/doi/epdf/10.1029/AR073p0121?saml_referrer (last access: 8 August 2022),
1998.
Lisiecki, L. E. and Raymo, M. E.: A Pliocene-Pleistocene stack of 57
globally distributed benthic δ18O records, Paleoceanography, 20,
PA1003, https://doi.org/10.1029/2004pa001071, 2005.
Maksym, T.: Arctic and Antarctic Sea Ice Change: Contrasts, Commonalities,
and Causes, Annu. Rev. Mar. Sci., 11, 187–213, 2019.
Manoj, M. C. and Thamban, M.: Shifting frontal regimes and its influence on
bioproductivity variations during the Late Quaternary in the Indian sector
of Southern Ocean, Deep-Sea Res. Pt. II, 118, 261–274, 2015.
Martínez-Garcia, A., Rosell-Melé, A., Geibert, W., Gersonde, R.,
Masqué, P., Gaspari, V., and Barbante, C.: Links between iron supply,
marine productivity, sea surface temperature, and CO2 over the last 1.1 Ma, Paleoceanography, 24, PA1207, https://doi.org/10.1029/2008pa001657, 2009.
Massom, R. A., Scambos, T. A., Bennetts, L. G., Reid, P., Squire, V. A., and
Stammerjohn, S. E.: Antarctic ice shelf disintegration triggered by sea ice
loss and ocean swell, Nature, 558, 383–389, 2018.
Nair, A., Mohan, R., Crosta, X., Manoj, M. C., Thamban, M., and Marieu, V.:
Southern Ocean sea ice and frontal changes during the Late Quaternary and
their linkages to Asian summer monsoon, Quaternary Sci. Rev., 213,
93–104, 2019.
Osman, M. B., Tierney, J. E., Zhu, J., Tardif, R., Hakim, G. J., King, J.,
and Poulsen, C. J.: Globally resolved surface temperatures since the Last
Glacial Maximum, Nature, 599, 239–244, 2021.
Otto-Bliesner, B. L., Brady, E. C., Zhao, A., Brierley, C. M., Axford, Y., Capron, E., Govin, A., Hoffman, J. S., Isaacs, E., Kageyama, M., Scussolini, P., Tzedakis, P. C., Williams, C. J. R., Wolff, E., Abe-Ouchi, A., Braconnot, P., Ramos Buarque, S., Cao, J., de Vernal, A., Guarino, M. V., Guo, C., LeGrande, A. N., Lohmann, G., Meissner, K. J., Menviel, L., Morozova, P. A., Nisancioglu, K. H., O'ishi, R., Salas y Mélia, D., Shi, X., Sicard, M., Sime, L., Stepanek, C., Tomas, R., Volodin, E., Yeung, N. K. H., Zhang, Q., Zhang, Z., and Zheng, W.: Large-scale features of Last Interglacial climate: results from evaluating the lig127k simulations for the Coupled Model Intercomparison Project (CMIP6)–Paleoclimate Modeling Intercomparison Project (PMIP4), Clim. Past, 17, 63–94, https://doi.org/10.5194/cp-17-63-2021, 2021.
Parkinson, C. L.: A 40-y record reveals gradual Antarctic sea ice increases
followed by decreases at rates far exceeding the rates seen in the Arctic,
P. Natl. Acad. Sci. USA, 116, 14414–14423, 2019.
Parrenin, F., Barnola, J.-M., Beer, J., Blunier, T., Castellano, E., Chappellaz, J., Dreyfus, G., Fischer, H., Fujita, S., Jouzel, J., Kawamura, K., Lemieux-Dudon, B., Loulergue, L., Masson-Delmotte, V., Narcisi, B., Petit, J.-R., Raisbeck, G., Raynaud, D., Ruth, U., Schwander, J., Severi, M., Spahni, R., Steffensen, J. P., Svensson, A., Udisti, R., Waelbroeck, C., and Wolff, E.: The EDC3 chronology for the EPICA Dome C ice core, Clim. Past, 3, 485–497, https://doi.org/10.5194/cp-3-485-2007, 2007.
Peacock, S., Lane, E., and Restrepo, J. M.: A possible sequence of events
for the generalized glacial-interglacial cycle, Global Biogeochem.
Cy., 20, GB2010, https://doi.org/10.1029/2005gb002448, 2006.
Rintoul, S. R.: The global influence of localized dynamics in the Southern
Ocean, Nature, 558, 209–218, 2018.
Rosenblum, E. and Eisenman, I.: Sea Ice Trends in Climate Models Only
Accurate in Runs with Biased Global Warming, J. Climate, 30,
6265–6278, 2017.
Röthlisberger, R., Crosta, X., Abram, N. J., Armand, L., and Wolff, E.
W.: Potential and limitations of marine and ice core sea ice proxies: an
example from the Indian Ocean sector, Quaternary Sci. Rev., 29,
296–302, 2010.
Rysgaard, S., Bendtsen, J., Delille, B., Dieckmann, G. S., Glud, R. N.,
Kennedy, H., Mortensen, J., Papadimitriou, S., Thomas, D. N., and Tison,
J.-L.: Sea ice contribution to the air–sea CO2 exchange in the Arctic
and Southern Oceans, Tellus B, 63, 823–830, 2011.
Schneider Mor, A., Yam, R., Bianchi, C., Kunz-Pirrung, M., Gersonde, R., and
Shemesh, A.: Variable sequence of events during the past seven terminations
in two deep-sea cores from the Southern Ocean, Quaternary Res., 77,
317–325, 2012.
Shaw, T. J., Raiswell, R., Hexel, C. R., Vu, H. P., Moore, W. S., Dudgeon,
R., and Smith, K. L.: Input, composition, and potential impact of
terrigenous material from free-drifting icebergs in the Weddell Sea, Deep
Sea Res. Pt. II, 58, 1376–1383, 2011.
Shemesh, A., Hodell, D., Crosta, X., Kanfoush, S., Charles, C., and
Guilderson, T.: Sequence of events during the last deglaciation in Southern
Ocean sediments and Antarctic ice cores, Paleoceanography, 17, 8-1–8-7,
2002.
Studer, A. S., Sigman, D. M., Martínez-García, A., Benz, V.,
Winckler, G., Kuhn, G., Esper, O., Lamy, F., Jaccard, S. L., Wacker, L.,
Oleynik, S., Gersonde, R., and Haug, G. H.: Antarctic Zone nutrient
conditions during the last two glacial cycles, Paleoceanography, 30,
845–862, 2015.
Stuut, J.-B. W., Crosta, X., van der Borg, K., and Schneider, R.:
Relationship between Antarctic sea ice and southwest African climate during
the late Quaternary, Geology, 32, 909–912, 2004.
Thomas, E. R., Allen, C. S., Etourneau, J., King, A. C. F., Severi, M.,
Winton, V. H. L., Mueller, J., Crosta, X., and Peck, V. L.: Antarctic Sea
Ice Proxies from Marine and Ice Core Archives Suitable for Reconstructing
Sea Ice over the Past 2000 Years, Geosciences, 9, 506, https://doi.org/10.3390/geosciences9120506, 2019.
Trathan, P. N., Brandon, M. A., Murphy, E. J., and Thorpe, S. E.: Transport
and structure within the Antarctic Circumpolar Current to the north of South
Georgia, Geophys. Res. Lett., 27, 1727–1730, 2000.
Turner, J., Hosking, J. S., Marshall, G. J., Phillips, T., and Bracegirdle,
T. J.: Antarctic sea ice increase consistent with intrinsic variability of
the Amundsen Sea Low, Clim. Dynam., 46, 2391–2402, 2016.
Veres, D., Bazin, L., Landais, A., Toyé Mahamadou Kele, H., Lemieux-Dudon, B., Parrenin, F., Martinerie, P., Blayo, E., Blunier, T., Capron, E., Chappellaz, J., Rasmussen, S. O., Severi, M., Svensson, A., Vinther, B., and Wolff, E. W.: The Antarctic ice core chronology (AICC2012): an optimized multi-parameter and multi-site dating approach for the last 120 thousand years, Clim. Past, 9, 1733–1748, https://doi.org/10.5194/cp-9-1733-2013, 2013.
Vernet, M., Geibert, W., Hoppema, M., Brown, P. J., Haas, C., Hellmer, H.
H., Jokat, W., Jullion, L., Mazloff, M., Bakker, D. C. E., Brearley, J. A.,
Croot, P., Hattermann, T., Hauck, J., Hillenbrand, C. D., Hoppe, C. J. M.,
Huhn, O., Koch, B. P., Lechtenfeld, O. J., Meredith, M. P., Naveira
Garabato, A. C., Nöthig, E. M., Peeken, I., Rutgers van der Loeff, M.
M., Schmidtko, S., Schröder, M., Strass, V. H., Torres-Valdés, S.,
and Verdy, A.: The Weddell Gyre, Southern Ocean: Present Knowledge and
Future Challenges, Rev. Geophys., 57, 623–708, 2019.
Vorrath, M.-E., Müller, J., Esper, O., Mollenhauer, G., Haas, C., Schefuß, E., and Fahl, K.: Highly branched isoprenoids for Southern Ocean sea ice reconstructions: a pilot study from the Western Antarctic Peninsula, Biogeosciences, 16, 2961–2981, https://doi.org/10.5194/bg-16-2961-2019, 2019.
Warnock, J. P., Scherer, R. P., and Konfirst, M. A.: A record of Pleistocene
diatom preservation from the Amundsen Sea, West Antarctica with possible
implications on silica leakage, Mar. Micropaleontol., 117, 40–46, 2015.
Weber, M. E., Clark, P. U., Kuhn, G., Timmermann, A., Sprenk, D., Gladstone,
R., Zhang, X., Lohmann, G., Menviel, L., Chikamoto, M. O., Friedrich, T.,
and Ohlwein, C.: Millennial-scale variability in Antarctic ice-sheet
discharge during the last deglaciation, Nature, 510, 134–138, 2014.
Wolff, E. W., Fischer, H., Fundel, F., Ruth, U., Twarloh, B., Littot, G. C.,
Mulvaney, R., Rothlisberger, R., de Angelis, M., Boutron, C. F., Hansson,
M., Jonsell, U., Hutterli, M. A., Lambert, F., Kaufmann, P., Stauffer, B.,
Stocker, T. F., Steffensen, J. P., Bigler, M., Siggaard-Andersen, M. L.,
Udisti, R., Becagli, S., Castellano, E., Severi, M., Wagenbach, D.,
Barbante, C., Gabrielli, P., and Gaspari, V.: Southern Ocean sea-ice extent,
productivity and iron flux over the past eight glacial cycles, Nature, 440,
491–496, 2006.
Wolff, E. W., Barbante, C., Becagli, S., Bigler, M., Boutron, C. F.,
Castellano, E., de Angelis, M., Federer, U., Fischer, H., Fundel, F.,
Hansson, M., Hutterli, M., Jonsell, U., Karlin, T., Kaufmann, P., Lambert,
F., Littot, G. C., Mulvaney, R., Röthlisberger, R., Ruth, U., Severi,
M., Siggaard-Andersen, M. L., Sime, L. C., Steffensen, J. P., Stocker, T.
F., Traversi, R., Twarloh, B., Udisti, R., Wagenbach, D., and Wegner, A.:
Changes in environment over the last 800 000 years from chemical analysis of
the EPICA Dome C ice core, Quaternary Sci. Rev., 29, 285–295, 2010.
Wu, S., Lembke-Jene, L., Lamy, F., Arz, H. W., Nowaczyk, N., Xiao, W.,
Zhang, X., Hass, H. C., Titschack, J., Zheng, X., Liu, J., Dumm, L.,
Diekmann, B., Nurnberg, D., Tiedemann, R., and Kuhn, G.: Orbital- and
millennial-scale Antarctic Circumpolar Current variability in Drake Passage
over the past 140 000 years, Nat. Commun., 12, 3948, https://doi.org/10.1038/s41467-021-24264-9, 2021.
Xiao, W.: Late Quaternary climate variability in Southern Ocean Atlantic
Sector, PhD, Fachbereich Geowissenschaften, Der Universitat Bremen, https://archimer.ifremer.fr/doc/00493/60451/ (last access: 6 December 2021), 2011.
Xiao, W., Esper, O., and Gersonde, R.: Last Glacial – Holocene climate
variability in the Atlantic sector of the Southern Ocean, Quaternary Sci. Rev., 135, 115–137, 2016a.
Xiao, W., Frederichs, T., Gersonde, R., Kuhn, G., Esper, O., and Zhang, X.:
Constraining the dating of late Quaternary marine sediment records from the
Scotia Sea (Southern Ocean), Quat. Geochronol., 31, 97–118, 2016b.
Short summary
Algae preserved in seafloor sediments have allowed us to reconstruct how Antarctic sea ice has varied between cold and warm time periods in the last 130 000 years. The patterns and timings of sea-ice increase and decrease vary between different parts of the Southern Ocean. Sea ice is most sensitive to changing climate at the external edges of Southern Ocean gyres (large areas of rotating ocean currents).
Algae preserved in seafloor sediments have allowed us to reconstruct how Antarctic sea ice has...
