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Late Quaternary Iceberg Rafting along the Antarctic Peninsula Continental Rise and in the Weddell and Scotia Seas

Published online by Cambridge University Press:  20 January 2017

Colm Ó Cofaigh ,
Julian A. Dowdeswell  and
Carol J. Pudsey
Colm Ó Cofaigh
Affiliation:
Bristol Glaciology Centre, School of Geographical Sciences, University of Bristol, Bristol, BS8 1SS, United Kingdom E-mail: Colm.OCofaigh@bristol.ac.uk
Julian A. Dowdeswell
Affiliation:
Bristol Glaciology Centre, School of Geographical Sciences, University of Bristol, Bristol, BS8 1SS, United Kingdom E-mail: Colm.OCofaigh@bristol.ac.uk
Carol J. Pudsey
Affiliation:
British Antarctic Survey, Natural Environment Research Council, Madingley Road, Cambridge, CB3 OET, United Kingdom
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Abstract

Sediment cores from the continental rise west of the Antarctic Peninsula and the northern Weddell and Scotia Seas were investigated for their ice-rafted debris (IRD) content by lithofacies logging and counting of particles >0.2 cm from core x-radiographs. The objective of the study was to determine if there are iceberg-rafted units similar to the Heinrich layers of the North Atlantic that might record periodic, widespread catastrophic collapse of basins within the Antarctic Ice Sheet during the Quaternary. Cores from the Antarctic Peninsula margin contain prominent IRD-rich units, with maximum IRD concentrations in oxygen isotope stages 1, 5, and 7. However, the greater concentration of IRD in interglacial stages is the result of low sedimentation rates and current winnowing, rather than regional-scale episodes of increased iceberg rafting. This is also supported by markedly lower mass accumulation rates (MAR) during interglacial periods versus glacial periods. Furthermore, thinner IRD layers within isotope stages 2–4 and 6 cannot be correlated between individual cores along the margin. This implies that the ice sheet over the Antarctic Peninsula did not undergo widespread catastrophic collapse along its western margin during the late Quaternary (isotope stages 1–7). Sediment cores from the Weddell and Scotia Seas are characterized by low IRD concentrations throughout, and the IRD signal generally appears to be of limited regional significance with few strong peaks that can be correlated between cores. Tentatively, this argues against pervasive, rapid ice-sheet collapse around the Weddell embayment over the last few glacial cycles.

Keywords

Antarctic PeninsulaWeddell and Scotia Seasice-rafted debrisAntarctic Ice SheetQuaternary
Type
Research Article
Information
Quaternary Research , Volume 56 , Issue 3 , November 2001 , pp. 308 - 321
Copyright
University of Washington

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