Articles | Volume 15, issue 10
https://doi.org/10.5194/tc-15-4655-2021
© 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/tc-15-4655-2021
© 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 Oct 2021
Research article |
| 05 Oct 2021
| 05 Oct 2021
Did Holocene climate changes drive West Antarctic grounding line retreat and readvance?
Sarah U. Neuhaus
CORRESPONDING AUTHOR
Earth and Planetary Sciences, University of California Santa Cruz,
Santa Cruz, CA 95064, USA
Slawek M. Tulaczyk
Earth and Planetary Sciences, University of California Santa Cruz,
Santa Cruz, CA 95064, USA
Nathan D. Stansell
Department of Geology and Environmental Geosciences, Northern Illinois University, DeKalb, IL 60115, USA
Jason J. Coenen
Department of Geology and Environmental Geosciences, Northern Illinois University, DeKalb, IL 60115, USA
Reed P. Scherer
Department of Geology and Environmental Geosciences, Northern Illinois University, DeKalb, IL 60115, USA
Jill A. Mikucki
Department of Microbiology, University of Tennessee Knoxville,
Knoxville, TN 37996, USA
Ross D. Powell
Department of Geology and Environmental Geosciences, Northern Illinois University, DeKalb, IL 60115, USA
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Cited
15 citations as recorded by crossref.
- Trace element, rare earth element and trace carbon compounds in Subglacial Lake Whillans, West Antarctica C. Turetta et al. 10.1016/j.scitotenv.2023.164480
- Mechanism for the subglacial formation of cryogenic brines S. Neuhaus & S. Tulaczyk 10.1017/aog.2023.28
- Review article: Existing and potential evidence for Holocene grounding line retreat and readvance in Antarctica J. Johnson et al. 10.5194/tc-16-1543-2022
- Basement Topography and Sediment Thickness Beneath Antarctica's Ross Ice Shelf M. Tankersley et al. 10.1029/2021GL097371
- An ensemble of Antarctic deglacial simulations constrained by geological observations M. Pittard et al. 10.1016/j.quascirev.2022.107800
- 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 Ice Sheet paleo-constraint database B. Lecavalier et al. 10.5194/essd-15-3573-2023
- 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
- Stability of the Antarctic Ice Sheet during the pre-industrial Holocene R. Jones et al. 10.1038/s43017-022-00309-5
- History of Anvers-Hugo Trough, western Antarctic Peninsula shelf, since the Last Glacial Maximum. Part I: Deglacial history based on new sedimentological and chronological data Z. Roseby et al. 10.1016/j.quascirev.2022.107590
- Widespread southern elephant seal occupation of the Victoria land coast implies a warmer-than-present Ross Sea in the mid-to-late Holocene B. Hall et al. 10.1016/j.quascirev.2023.107991
- A decade of in situ cosmogenic 14C in Antarctica K. Nichols 10.1017/aog.2023.13
- Geothermal heat flux is the dominant source of uncertainty in englacial-temperature-based dating of ice rise formation A. Montelli & J. Kingslake 10.5194/tc-17-195-2023
- Constraints on the Timing and Extent of Deglacial Grounding Line Retreat in West Antarctica R. Venturelli et al. 10.1029/2022AV000846
- Breaking All the Rules: The First Recorded Hard Substrate Sessile Benthic Community Far Beneath an Antarctic Ice Shelf H. Griffiths et al. 10.3389/fmars.2021.642040
14 citations as recorded by crossref.
- Trace element, rare earth element and trace carbon compounds in Subglacial Lake Whillans, West Antarctica C. Turetta et al. 10.1016/j.scitotenv.2023.164480
- Mechanism for the subglacial formation of cryogenic brines S. Neuhaus & S. Tulaczyk 10.1017/aog.2023.28
- Review article: Existing and potential evidence for Holocene grounding line retreat and readvance in Antarctica J. Johnson et al. 10.5194/tc-16-1543-2022
- Basement Topography and Sediment Thickness Beneath Antarctica's Ross Ice Shelf M. Tankersley et al. 10.1029/2021GL097371
- An ensemble of Antarctic deglacial simulations constrained by geological observations M. Pittard et al. 10.1016/j.quascirev.2022.107800
- 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 Ice Sheet paleo-constraint database B. Lecavalier et al. 10.5194/essd-15-3573-2023
- 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
- Stability of the Antarctic Ice Sheet during the pre-industrial Holocene R. Jones et al. 10.1038/s43017-022-00309-5
- History of Anvers-Hugo Trough, western Antarctic Peninsula shelf, since the Last Glacial Maximum. Part I: Deglacial history based on new sedimentological and chronological data Z. Roseby et al. 10.1016/j.quascirev.2022.107590
- Widespread southern elephant seal occupation of the Victoria land coast implies a warmer-than-present Ross Sea in the mid-to-late Holocene B. Hall et al. 10.1016/j.quascirev.2023.107991
- A decade of in situ cosmogenic 14C in Antarctica K. Nichols 10.1017/aog.2023.13
- Geothermal heat flux is the dominant source of uncertainty in englacial-temperature-based dating of ice rise formation A. Montelli & J. Kingslake 10.5194/tc-17-195-2023
- Constraints on the Timing and Extent of Deglacial Grounding Line Retreat in West Antarctica R. Venturelli et al. 10.1029/2022AV000846
Latest update: 23 Apr 2024
Short summary
We estimate the timing of post-LGM grounding line retreat and readvance in the Ross Sea sector of Antarctica. Our analyses indicate that the grounding line retreated over our field sites within the past 5000 years (coinciding with a warming climate) and readvanced roughly 1000 years ago (coinciding with a cooling climate). Based on these results, we propose that the Siple Coast grounding line motions in the middle to late Holocene were driven by relatively modest changes in regional climate.
We estimate the timing of post-LGM grounding line retreat and readvance in the Ross Sea sector...
