Articles | Volume 10, issue 3
https://doi.org/10.5194/tc-10-1003-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/tc-10-1003-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Past ice-sheet behaviour: retreat scenarios and changing controls in the Ross Sea, Antarctica
Anna Ruth W. Halberstadt
CORRESPONDING AUTHOR
Department of Earth Science, Rice University, Houston, Texas 77005,
USA
Lauren M. Simkins
Department of Earth Science, Rice University, Houston, Texas 77005,
USA
Sarah L. Greenwood
Department of Geological Sciences, Stockholm University, 10691
Stockholm, Sweden
John B. Anderson
Department of Earth Science, Rice University, Houston, Texas 77005,
USA
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95 citations as recorded by crossref.
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- Bottom current control on sediment deposition between the Iselin Bank and the Hillary Canyon (Antarctica) since the late Miocene: An integrated seismic-oceanographic approach R. Conte et al. 10.1016/j.dsr.2021.103606
- Late pleistocene paleoceanographic changes in the Ross Sea – Glacial-interglacial variations in paleoproductivity, nutrient utilization, and deep-water formation S. Kim et al. 10.1016/j.quascirev.2020.106356
- Antarctic ice sheet palaeo-thinning rates from vertical transects of cosmogenic exposure ages D. Small et al. 10.1016/j.quascirev.2018.12.024
- The paradox of a long grounding during West Antarctic Ice Sheet retreat in Ross Sea P. Bart et al. 10.1038/s41598-017-01329-8
- A tuff cone erupted under frozen-bed ice (northern Victoria Land, Antarctica): linking glaciovolcanic and cosmogenic nuclide data for ice sheet reconstructions J. Smellie et al. 10.1007/s00445-017-1185-x
- Seismic and geomorphic records of Antarctic Ice Sheet evolution in the Ross Sea and controlling factors in its behaviour J. Anderson et al. 10.1144/SP475.5
- The seafloor geomorphology of the Windmill Islands, Wilkes Land, East Antarctica: Evidence of Law Dome ice margin dynamics C. Carson et al. 10.1016/j.geomorph.2017.04.031
- Glaciovolcanic processes between the Campbell Glacier and Mt. Melbourne Volcano, Antarctica: ICE and FIRE H. Rhee et al. 10.1016/j.palaeo.2024.112611
- Holocene thinning of Darwin and Hatherton glaciers, Antarctica, and implications for grounding-line retreat in the Ross Sea T. Hillebrand et al. 10.5194/tc-15-3329-2021
- Antarctic ice dynamics in warm climates S. Greenwood 10.1038/d41586-017-08285-3
- Mid‐Holocene Grounding Line Retreat and Readvance at Whillans Ice Stream, West Antarctica R. Venturelli et al. 10.1029/2020GL088476
- West Antarctic ice volume variability paced by obliquity until 400,000 years ago C. Ohneiser et al. 10.1038/s41561-022-01088-w
- Subglacial sediment deformation in the Ross Sea, Antarctica D. Robinson et al. 10.1016/j.qsa.2021.100029
- Recent Ostracod Fauna of the Western Ross Sea (Antarctica): A Poorly Known Ingredient of Polar Carbonate Factories G. Salvi et al. 10.3390/min12080937
- Rapid early‐Holocene deglaciation in the Ross Sea, Antarctica P. Spector et al. 10.1002/2017GL074216
- A paleo-perspective on West Antarctic Ice Sheet retreat P. Bart & M. Kratochvil 10.1038/s41598-022-22450-3
- Post-LGM dynamic deglaciation along the Victoria Land coast, Antarctica H. Rhee et al. 10.1016/j.quascirev.2020.106595
- Instability of the Antarctic Ross Sea Embayment as climate warms T. Hughes et al. 10.1002/2016RG000545
- Climate-controlled submarine landslides on the Antarctic continental margin J. Gales et al. 10.1038/s41467-023-38240-y
- Provenance of Ross Sea Drift in McMurdo Sound (Antarctica) and implications for middle-Quaternary to LGM glacial transport: New evidence from petrographic data M. Perotti et al. 10.1016/j.sedgeo.2018.04.009
- Late-glacial grounding line retreat in the northern Ross Sea, Antarctica B. Goehring et al. 10.1130/G45413.1
- Cosmogenic nuclide exposure age scatter records glacial history and processes in McMurdo Sound, Antarctica A. Christ et al. 10.5194/gchron-3-505-2021
- Rapid glaciation and a two-step sea level plunge into the Last Glacial Maximum Y. Yokoyama et al. 10.1038/s41586-018-0335-4
- Spatio-temporal variability of processes across Antarctic ice-bed–ocean interfaces F. Colleoni et al. 10.1038/s41467-018-04583-0
- Sedimentary processes at ice sheet grounding‐zone wedges revealed by outcrops, Washington State (USA) B. Demet et al. 10.1002/esp.4550
- Seafloor geomorphology of western Antarctic Peninsula bays: a signature of ice flow behaviour Y. Munoz & J. Wellner 10.5194/tc-12-205-2018
- On the influence of post-LGM ice shelf loss and grounding zone sedimentation on West Antarctic ice sheet stability A. McGlannan et al. 10.1016/j.margeo.2017.08.005
- Streamlined subglacial bedform sensitivity to bed characteristics across the deglaciated Northern Hemisphere M. McKenzie et al. 10.1002/esp.5382
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Saved (final revised paper)
Latest update: 14 Dec 2024
Short summary
Geomorphic features on the Ross Sea sea floor provide a record of ice-sheet behaviour during the Last Glacial Maximum and subsequent retreat. Based on extensive mapping of these glacial landforms, a large embayment formed in the eastern Ross Sea. This was followed by complex, late-stage retreat in the western Ross Sea where banks stabilised the ice sheet. Physiography and sea floor geology act as regional controls on ice-sheet dynamics across the Ross Sea.
Geomorphic features on the Ross Sea sea floor provide a record of ice-sheet behaviour during the...