Articles | Volume 13, issue 11
https://doi.org/10.5194/tc-13-2935-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/tc-13-2935-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| Highlight paper
| 
08 Nov 2019
Research article | Highlight paper |
| 08 Nov 2019
| 08 Nov 2019
New Last Glacial Maximum ice thickness constraints for the Weddell Sea Embayment, Antarctica
Department of Earth and Environmental Sciences, Tulane University,
New Orleans, LA 70118, USA
Brent M. Goehring
Department of Earth and Environmental Sciences, Tulane University,
New Orleans, LA 70118, USA
Greg Balco
Berkeley Geochronology Center, 2455 Ridge Road, Berkeley, CA 94709, USA
Joanne S. Johnson
British Antarctic Survey, Natural Environment Research Council, High Cross, Madingley Road, Cambridge, CB3 0ET, UK
Andrew S. Hein
School of GeoSciences, University of Edinburgh, Drummund Street,
Edinburgh, EH8 9XP, UK
Claire Todd
Department of Geosciences, Pacific Lutheran University, Tacoma, WA 98447, USA
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- High mid-Holocene accumulation rates over West Antarctica inferred from a pervasive ice-penetrating radar reflector J. Bodart et al. 10.5194/tc-17-1497-2023
- Antarctic upper mantle rheology E. Ivins et al. 10.1144/M56-2020-19
- Past ice sheet–seabed interactions in the northeastern Weddell Sea embayment, Antarctica J. Arndt et al. 10.5194/tc-14-2115-2020
- Blue-ice moraines formation in the Heritage Range, West Antarctica: Implications for ice sheet history and climate reconstruction J. Woodward et al. 10.1016/j.qsa.2022.100051
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- Technical note: A prototype transparent-middle-layer data management and analysis infrastructure for cosmogenic-nuclide exposure dating G. Balco 10.5194/gchron-2-169-2020
- Reversible ice sheet thinning in the Amundsen Sea Embayment during the Late Holocene G. Balco et al. 10.5194/tc-17-1787-2023
- Mid-Holocene thinning of David Glacier, Antarctica: chronology and controls J. Stutz et al. 10.5194/tc-15-5447-2021
- A decade of in situ cosmogenic 14C in Antarctica K. Nichols 10.1017/aog.2023.13
- Ice surface changes during recent glacial cycles along the Jutulstraumen and Penck Trough ice streams in western Dronning Maud Land, East Antarctica J. Andersen et al. 10.1016/j.quascirev.2020.106636
- Stability of the Antarctic Ice Sheet during the pre-industrial Holocene R. Jones et al. 10.1038/s43017-022-00309-5
- Major Ice Sheet Change in the Weddell Sea Sector of West Antarctica Over the Last 5,000 Years M. Siegert et al. 10.1029/2019RG000651
21 citations as recorded by crossref.
- New cosmogenic nuclide constraints on Late Glacial and Holocene glacier fluctuations in the sub-Antarctic Indian Ocean (Kerguelen Islands, 49°S) J. Charton et al. 10.1016/j.quascirev.2022.107461
- Regional sea-level highstand triggered Holocene ice sheet thinning across coastal Dronning Maud Land, East Antarctica Y. Suganuma et al. 10.1038/s43247-022-00599-z
- A topographic hinge-zone divides coastal and inland ice dynamic regimes in East Antarctica J. Andersen et al. 10.1038/s43247-022-00673-6
- Antarctic Ice Sheet paleo-constraint database B. Lecavalier et al. 10.5194/essd-15-3573-2023
- Comparing Glacial‐Geological Evidence and Model Simulations of Ice Sheet Change since the Last Glacial Period in the Amundsen Sea Sector of Antarctica J. Johnson et al. 10.1029/2020JF005827
- A history-matching analysis of the Antarctic Ice Sheet since the Last Interglacial – Part 1: Ice sheet evolution B. Lecavalier & L. Tarasov 10.5194/tc-19-919-2025
- Abrupt Holocene ice loss due to thinning and ungrounding in the Weddell Sea Embayment M. Grieman et al. 10.1038/s41561-024-01375-8
- Cosmogenic-nuclide data from Antarctic nunataks can constrain past ice sheet instabilities A. Halberstadt et al. 10.5194/tc-17-1623-2023
- Can we use springtails to improve our understanding of Antarctic Ice Sheet history? — A case study from Dronning Maud Land E. Cooper et al. 10.1016/j.quascirev.2025.109297
- Location, location, location: survival of Antarctic biota requires the best real estate M. Stevens & A. Mackintosh 10.1098/rsbl.2022.0590
- High mid-Holocene accumulation rates over West Antarctica inferred from a pervasive ice-penetrating radar reflector J. Bodart et al. 10.5194/tc-17-1497-2023
- Antarctic upper mantle rheology E. Ivins et al. 10.1144/M56-2020-19
- Past ice sheet–seabed interactions in the northeastern Weddell Sea embayment, Antarctica J. Arndt et al. 10.5194/tc-14-2115-2020
- Blue-ice moraines formation in the Heritage Range, West Antarctica: Implications for ice sheet history and climate reconstruction J. Woodward et al. 10.1016/j.qsa.2022.100051
- Cosmogenic nuclide exposure age scatter records glacial history and processes in McMurdo Sound, Antarctica A. Christ et al. 10.5194/gchron-3-505-2021
- Technical note: A prototype transparent-middle-layer data management and analysis infrastructure for cosmogenic-nuclide exposure dating G. Balco 10.5194/gchron-2-169-2020
- Reversible ice sheet thinning in the Amundsen Sea Embayment during the Late Holocene G. Balco et al. 10.5194/tc-17-1787-2023
- Mid-Holocene thinning of David Glacier, Antarctica: chronology and controls J. Stutz et al. 10.5194/tc-15-5447-2021
- A decade of in situ cosmogenic 14C in Antarctica K. Nichols 10.1017/aog.2023.13
- Ice surface changes during recent glacial cycles along the Jutulstraumen and Penck Trough ice streams in western Dronning Maud Land, East Antarctica J. Andersen et al. 10.1016/j.quascirev.2020.106636
- Stability of the Antarctic Ice Sheet during the pre-industrial Holocene R. Jones et al. 10.1038/s43017-022-00309-5
1 citations as recorded by crossref.
Latest update: 03 May 2025
Short summary
We studied the history of ice masses at three locations in the Weddell Sea Embayment, Antarctica. We measured rare isotopes in material sourced from mountains overlooking the Slessor Glacier, Foundation Ice Stream, and smaller glaciers on the Lassiter Coast. We show that ice masses were between 385 and 800 m thicker during the last glacial cycle than they are at present. The ice masses were both hundreds of metres thicker and remained thicker closer to the present than was previously thought.
We studied the history of ice masses at three locations in the Weddell Sea Embayment,...
