Glaciology and geological signature of the Last Glacial Maximum Antarctic ice sheet

Dynamical changes in contemporary ice sheets account for significant proportions of their current rates of mass loss, but assessing whether or not these processes are a natural part of ice-sheet evolution requires inference from palaeo-glaciological records. However, a robust mechanism for translati...

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Published in:Quaternary science reviews Vol. 78; pp. 225 - 247
Main Authors: Golledge, Nicholas R., Levy, Richard H., McKay, Robert M., Fogwill, Christopher J., White, Duanne A., Graham, Alastair G.C., Smith, James A., Hillenbrand, Claus-Dieter, Licht, Kathy J., Denton, George H., Ackert, Robert P., Maas, Sanne M., Hall, Brenda L.
Format: Journal Article
Language:English
Published: Elsevier Ltd 15.10.2013
Subjects:
Glacial geology
Ice-sheet modelling
Plio-Pleistocene
Subglacial erosion
PSE, Antarctica, Victoria Land, Arrival Heights, McMurdo Sound
PS, Ross Sea
Glacial geology
Subglacial erosion
Ice-sheet modelling
Plio-Pleistocene
ISSN:0277-3791, 1873-457X
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Abstract Dynamical changes in contemporary ice sheets account for significant proportions of their current rates of mass loss, but assessing whether or not these processes are a natural part of ice-sheet evolution requires inference from palaeo-glaciological records. However, a robust mechanism for translating sparse geological data into meaningful interpretations of past glacier dynamics at the continental scale is lacking, since geological archives can be ambiguous, and often their chronology is only poorly constrained. To address this, we combine the interpretation of high-resolution Antarctic ice sheet model results with continent-wide geological evidence pertinent to the dynamical configuration of the ice sheet during the last, and possibly preceding, glacial maxima. We first focus on the thermal regime of the ice sheet, its pattern and velocity of flow, variability in likely subglacial erosion and sediment transport, and how these characteristics evolve during glacial transitions. We show that rapid basal sliding was restricted to discrete outlets that eroded and advected sediment toward and across the continental shelf primarily during the early stages of advance and retreat of the ice sheet, highlighting the need to consider time-transgressive behaviour in the interpretation of geological archives. Secondly, we present new modelling that attempts to improve the fit of our numerical model to geologically-based reconstructions in the Ross Sea. By accounting for locally-enhanced ablation in McMurdo Sound, our new simulation achieves a much closer fit to empirically-derived flow patterns than previously. Growth of the modelled Last Glacial Maximum ice sheet takes place primarily by marine ice accretion in the major embayments, as a consequence of cooler ocean temperatures and reduced sub-ice-shelf melting, and at its maximal extent represents a grounded ice volume excess above present of approximately 8.3 m sea-level equivalent. This figure thus provides an upper bound on the possible Antarctic contribution to deglacial meltwater pulses. •We describe the glaciology of a modelled LGM Antarctic ice sheet model.•We compare its likely geological signature to inferences from empirical records.•We show that greatest subglacial erosion coincides with climate transitions.•We argue that geological records integrate time-transgressive ice-sheet behaviour.
AbstractList Dynamical changes in contemporary ice sheets account for significant proportions of their current rates of mass loss, but assessing whether or not these processes are a natural part of ice-sheet evolution requires inference from palaeo-glaciological records. However, a robust mechanism for translating sparse geological data into meaningful interpretations of past glacier dynamics at the continental scale is lacking, since geological archives can be ambiguous, and often their chronology is only poorly constrained. To address this, we combine the interpretation of high-resolution Antarctic ice sheet model results with continent-wide geological evidence pertinent to the dynamical configuration of the ice sheet during the last, and possibly preceding, glacial maxima. We first focus on the thermal regime of the ice sheet, its pattern and velocity of flow, variability in likely subglacial erosion and sediment transport, and how these characteristics evolve during glacial transitions. We show that rapid basal sliding was restricted to discrete outlets that eroded and advected sediment toward and across the continental shelf primarily during the early stages of advance and retreat of the ice sheet, highlighting the need to consider time-transgressive behaviour in the interpretation of geological archives. Secondly, we present new modelling that attempts to improve the fit of our numerical model to geologically-based reconstructions in the Ross Sea. By accounting for locally-enhanced ablation in McMurdo Sound, our new simulation achieves a much closer fit to empirically-derived flow patterns than previously. Growth of the modelled Last Glacial Maximum ice sheet takes place primarily by marine ice accretion in the major embayments, as a consequence of cooler ocean temperatures and reduced sub-ice-shelf melting, and at its maximal extent represents a grounded ice volume excess above present of approximately 8.3 m sea-level equivalent. This figure thus provides an upper bound on the possible Antarctic contribution to deglacial meltwater pulses. •We describe the glaciology of a modelled LGM Antarctic ice sheet model.•We compare its likely geological signature to inferences from empirical records.•We show that greatest subglacial erosion coincides with climate transitions.•We argue that geological records integrate time-transgressive ice-sheet behaviour.
Dynamical changes in contemporary ice sheets account for significant proportions of their current rates of mass loss, but assessing whether or not these processes are a natural part of ice-sheet evolution requires inference from palaeo-glaciological records. However, a robust mechanism for translating sparse geological data into meaningful interpretations of past glacier dynamics at the continental scale is lacking, since geological archives can be ambiguous, and often their chronology is only poorly constrained. To address this, we combine the interpretation of high-resolution Antarctic ice sheet model results with continent-wide geological evidence pertinent to the dynamical configuration of the ice sheet during the last, and possibly preceding, glacial maxima. We first focus on the thermal regime of the ice sheet, its pattern and velocity of flow, variability in likely subglacial erosion and sediment transport, and how these characteristics evolve during glacial transitions. We show that rapid basal sliding was restricted to discrete outlets that eroded and advected sediment toward and across the continental shelf primarily during the early stages of advance and retreat of the ice sheet, highlighting the need to consider time-transgressive behaviour in the interpretation of geological archives. Secondly, we present new modelling that attempts to improve the fit of our numerical model to geologically-based reconstructions in the Ross Sea. By accounting for locally-enhanced ablation in McMurdo Sound, our new simulation achieves a much closer fit to empirically-derived flow patterns than previously. Growth of the modelled Last Glacial Maximum ice sheet takes place primarily by marine ice accretion in the major embayments, as a consequence of cooler ocean temperatures and reduced sub-ice-shelf melting, and at its maximal extent represents a grounded ice volume excess above present of approximately 8.3 m sea-level equivalent. This figure thus provides an upper bound on the possible Antarctic contribution to deglacial meltwater pulses.
Author Licht, Kathy J.
Maas, Sanne M.
Hall, Brenda L.
Levy, Richard H.
McKay, Robert M.
Graham, Alastair G.C.
Ackert, Robert P.
Denton, George H.
Golledge, Nicholas R.
Smith, James A.
Fogwill, Christopher J.
Hillenbrand, Claus-Dieter
White, Duanne A.
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  surname: Golledge
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  givenname: Richard H.
  surname: Levy
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  organization: Antarctic Research Centre, Victoria University of Wellington, Wellington 6140, New Zealand
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  organization: British Antarctic Survey, High Cross, Madingley Road, Cambridge CB3 0ET, UK
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  surname: Hillenbrand
  fullname: Hillenbrand, Claus-Dieter
  organization: British Antarctic Survey, High Cross, Madingley Road, Cambridge CB3 0ET, UK
– sequence: 9
  givenname: Kathy J.
  surname: Licht
  fullname: Licht, Kathy J.
  organization: Indiana University–Purdue University Indianapolis, Dept. of Earth Sciences, Indianapolis, IN 46202, USA
– sequence: 10
  givenname: George H.
  surname: Denton
  fullname: Denton, George H.
  organization: School of Earth and Climate Sciences & The Climate Change Institute, Bryand Global Sciences Center, University of Maine, Orono, ME 04469, USA
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  givenname: Robert P.
  surname: Ackert
  fullname: Ackert, Robert P.
  organization: Department of Earth and Planetary Science, Harvard University, Cambridge, MA 02138, USA
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  givenname: Sanne M.
  surname: Maas
  fullname: Maas, Sanne M.
  organization: Antarctic Research Centre, Victoria University of Wellington, Wellington 6140, New Zealand
– sequence: 13
  givenname: Brenda L.
  surname: Hall
  fullname: Hall, Brenda L.
  organization: School of Earth and Climate Sciences & The Climate Change Institute, Bryand Global Sciences Center, University of Maine, Orono, ME 04469, USA
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Snippet Dynamical changes in contemporary ice sheets account for significant proportions of their current rates of mass loss, but assessing whether or not these...
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SubjectTerms Glacial geology
Ice-sheet modelling
Plio-Pleistocene
Subglacial erosion
Title Glaciology and geological signature of the Last Glacial Maximum Antarctic ice sheet
URI https://dx.doi.org/10.1016/j.quascirev.2013.08.011
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