Articles | Volume 17, issue 1
https://doi.org/10.5194/cp-17-1-2021
© Author(s) 2021. 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-17-1-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
05 Jan 2021
Research article |
| 05 Jan 2021
| 05 Jan 2021
Mid-Holocene Antarctic sea-ice increase driven by marine ice sheet retreat
Kate E. Ashley
School of Geography, Earth and Environmental Sciences, University of Birmingham, Edgbaston, Birmingham, B15 2TT, UK
Robert McKay
Antarctic Research Centre, Victoria University of Wellington,
Wellington 6140, New Zealand
Johan Etourneau
EPHE/PSL Research University, 4-14 rue Ferrus, 75014 Paris, France
UMR 5805 EPOC, Université de Bordeaux, CNRS, EPHE, 33615 Pessac, France
Francisco J. Jimenez-Espejo
EPHE/PSL Research University, 4-14 rue Ferrus, 75014 Paris, France
Department of Biogeochemistry, Japan Agency for Marine-Earth Science and Technology (JAMSTEC), Yokosuka 237-0061, Japan
Alan Condron
Department of Geology and Geophysics, Woods Hole Oceanographic
Institution, Woods Hole, MA 02543, USA
Anna Albot
Antarctic Research Centre, Victoria University of Wellington,
Wellington 6140, New Zealand
Xavier Crosta
UMR 5805 EPOC, Université de Bordeaux, CNRS, EPHE, 33615 Pessac, France
Christina Riesselman
Department of Geology, University of Otago, Dunedin 9016, New Zealand
Department of Marine Science, University of Otago, Dunedin 9016, New Zealand
Osamu Seki
Institite of Low Temperature Science, Hokkaido University, Sapporo 060-0819,
Hokkaido, Japan
Guillaume Massé
TAKUVIK, UMI 3376 UL/CNRS, Université Laval, 1045 avenue de la
Médecine, Quebec City, Quebec, G1V 0A6, Canada
Nicholas R. Golledge
Antarctic Research Centre, Victoria University of Wellington,
Wellington 6140, New Zealand
GNS Science, Avalon, Lower Hutt 5011, New Zealand
Edward Gasson
School of Geographical Sciences, University of Bristol, Bristol, BS8 1RL, UK
Daniel P. Lowry
Antarctic Research Centre, Victoria University of Wellington,
Wellington 6140, New Zealand
GNS Science, Avalon, Lower Hutt 5011, New Zealand
Nicholas E. Barrand
School of Geography, Earth and Environmental Sciences, University of Birmingham, Edgbaston, Birmingham, B15 2TT, UK
Katelyn Johnson
Antarctic Research Centre, Victoria University of Wellington,
Wellington 6140, New Zealand
GNS Science, Avalon, Lower Hutt 5011, New Zealand
Nancy Bertler
Antarctic Research Centre, Victoria University of Wellington,
Wellington 6140, New Zealand
GNS Science, Avalon, Lower Hutt 5011, New Zealand
Carlota Escutia
EPHE/PSL Research University, 4-14 rue Ferrus, 75014 Paris, France
Robert Dunbar
Department of Environmental Earth Systems Science, Stanford
University, Stanford, A 94305, California, USA
School of Geography, Earth and Environmental Sciences, University of Birmingham, Edgbaston, Birmingham, B15 2TT, UK
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Cited
15 citations as recorded by crossref.
- Holocene Sea Ice Evolution and Dynamics in Transient Climate Simulations 旭. 张 10.12677/CCRL.2022.111008
- Holocene Palaeoenvironmental and Palaeoproductivity Changes in the Western Amundsen Sea Embayment of Antarctica M. Kim et al. 10.1029/2023JC019797
- Variety and Distribution of Diatom-Based Sea Ice Proxies in Antarctic Marine Sediments of the Past 2000 Years C. Allen & Z. Weich 10.3390/geosciences12080282
- Temporal variations of surface mass balance over the last 5000 years around Dome Fuji, Dronning Maud Land, East Antarctica I. Oyabu et al. 10.5194/cp-19-293-2023
- Diatom based reconstruction of climate evolution through the Last Glacial Maximum to Holocene in the Cosmonaut Sea, East Antarctica Q. Li et al. 10.1016/j.dsr2.2021.104960
- Holocene paleoceanographic variability in Robertson Bay, Ross Sea, Antarctica: A marine record of ocean, ice sheet, and climate connectivity O. Truax et al. 10.1016/j.quascirev.2024.108635
- Biomarker proxies for reconstructing Quaternary climate and environmental change E. McClymont et al. 10.1002/jqs.3559
- Beryllium isotope variations recorded in the Adélie Basin, East Antarctica reflect Holocene changes in ice dynamics, productivity, and scavenging efficiency B. Behrens et al. 10.1016/j.qsa.2022.100054
- Stability of the Antarctic Ice Sheet during the pre-industrial Holocene R. Jones et al. 10.1038/s43017-022-00309-5
- Exploring the use of compound-specific carbon isotopes as a palaeoproductivity proxy off the coast of Adélie Land, East Antarctica K. Ashley et al. 10.5194/bg-18-5555-2021
- Sensitivity of Holocene East Antarctic productivity to subdecadal variability set by sea ice K. Johnson et al. 10.1038/s41561-021-00816-y
- Antarctic sea ice over the past 130 000 years – Part 1: a review of what proxy records tell us X. Crosta et al. 10.5194/cp-18-1729-2022
- Evaluation of geomagnetic relative palaeointensity as a chronostratigraphic tool in the Southern Ocean: Refined Plio-/Pleistocene chronology of IODP Site U1533 (Amundsen Sea, West Antarctica) B. Hopkins et al. 10.1016/j.quascirev.2023.108460
- ADVANCING ANTARCTIC SEDIMENT CHRONOLOGY THROUGH COMBINED RAMPED PYROLYSIS OXIDATION AND PYROLYSIS-GC-MS C. Ginnane et al. 10.1017/RDC.2023.116
- Multi-decadal trends in Antarctic sea-ice extent driven by ENSO–SAM over the last 2,000 years X. Crosta et al. 10.1038/s41561-021-00697-1
15 citations as recorded by crossref.
- Holocene Sea Ice Evolution and Dynamics in Transient Climate Simulations 旭. 张 10.12677/CCRL.2022.111008
- Holocene Palaeoenvironmental and Palaeoproductivity Changes in the Western Amundsen Sea Embayment of Antarctica M. Kim et al. 10.1029/2023JC019797
- Variety and Distribution of Diatom-Based Sea Ice Proxies in Antarctic Marine Sediments of the Past 2000 Years C. Allen & Z. Weich 10.3390/geosciences12080282
- Temporal variations of surface mass balance over the last 5000 years around Dome Fuji, Dronning Maud Land, East Antarctica I. Oyabu et al. 10.5194/cp-19-293-2023
- Diatom based reconstruction of climate evolution through the Last Glacial Maximum to Holocene in the Cosmonaut Sea, East Antarctica Q. Li et al. 10.1016/j.dsr2.2021.104960
- Holocene paleoceanographic variability in Robertson Bay, Ross Sea, Antarctica: A marine record of ocean, ice sheet, and climate connectivity O. Truax et al. 10.1016/j.quascirev.2024.108635
- Biomarker proxies for reconstructing Quaternary climate and environmental change E. McClymont et al. 10.1002/jqs.3559
- Beryllium isotope variations recorded in the Adélie Basin, East Antarctica reflect Holocene changes in ice dynamics, productivity, and scavenging efficiency B. Behrens et al. 10.1016/j.qsa.2022.100054
- Stability of the Antarctic Ice Sheet during the pre-industrial Holocene R. Jones et al. 10.1038/s43017-022-00309-5
- Exploring the use of compound-specific carbon isotopes as a palaeoproductivity proxy off the coast of Adélie Land, East Antarctica K. Ashley et al. 10.5194/bg-18-5555-2021
- Sensitivity of Holocene East Antarctic productivity to subdecadal variability set by sea ice K. Johnson et al. 10.1038/s41561-021-00816-y
- Antarctic sea ice over the past 130 000 years – Part 1: a review of what proxy records tell us X. Crosta et al. 10.5194/cp-18-1729-2022
- Evaluation of geomagnetic relative palaeointensity as a chronostratigraphic tool in the Southern Ocean: Refined Plio-/Pleistocene chronology of IODP Site U1533 (Amundsen Sea, West Antarctica) B. Hopkins et al. 10.1016/j.quascirev.2023.108460
- ADVANCING ANTARCTIC SEDIMENT CHRONOLOGY THROUGH COMBINED RAMPED PYROLYSIS OXIDATION AND PYROLYSIS-GC-MS C. Ginnane et al. 10.1017/RDC.2023.116
- Multi-decadal trends in Antarctic sea-ice extent driven by ENSO–SAM over the last 2,000 years X. Crosta et al. 10.1038/s41561-021-00697-1
Discussed (final revised paper)
Latest update: 13 Dec 2024
Short summary
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.
We present a multi-proxy record of Holocene glacial meltwater input, sediment transport, and...
