Giant sediment drifts on the continental rise west of the Antarctic Peninsula

1996 ◽  
Vol 16 (2) ◽  
pp. 65-75 ◽  
Author(s):  
Michele Rebesco ◽  
Robert D. Larter ◽  
Angelo Camerlenghi ◽  
Peter F. Barker
Keyword(s):  
Antarctic Peninsula ◽  
Continental Rise ◽  
Sediment Drifts ◽  
The Antarctic

Large sediment drifts on the upper continental rise west of the Antarctic Peninsula

2016 ◽  
Vol 46 (1) ◽  
pp. 401-402 ◽  
Author(s):  
R. D. Larter ◽  
K. A. Hogan ◽  
J. A. Dowdeswell
Keyword(s):  
Antarctic Peninsula ◽  
Continental Rise ◽  
Sediment Drifts ◽  
The Antarctic

The present and past bottom-current flow regime around the sediment drifts on the continental rise west of the Antarctic Peninsula

2008 ◽  
Vol 255 (1-2) ◽  
pp. 55-63 ◽  
Author(s):  
C.-D. Hillenbrand ◽  
A. Camerlenghi ◽  
E.A. Cowan ◽  
F.J. Hernández-Molina ◽  
R.G. Lucchi ◽  
...  
Keyword(s):  
Flow Regime ◽  
Antarctic Peninsula ◽  
Current Flow ◽  
Bottom Current ◽  
Continental Rise ◽  
Sediment Drifts ◽  
The Antarctic

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

2001 ◽  
Vol 56 (3) ◽  
pp. 308-321 ◽  
Author(s):  
Colm Ó Cofaigh ◽  
Julian A. Dowdeswell ◽  
Carol J. Pudsey
Keyword(s):  
Antarctic Peninsula ◽  
Late Quaternary ◽  
Sediment Cores ◽  
Regional Scale ◽  
Ice Sheet ◽  
Glacial Cycles ◽  
Continental Rise ◽  
The North ◽  
Glacial Periods ◽  
The Antarctic

AbstractSediment 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.

The History of Sedimentation on the Continental Rise West of the Antarctic Peninsula

2013 ◽  
pp. 29-49 ◽  
Author(s):  
Michele Rebesco ◽  
Robert D. Larter ◽  
Peter F. Barker ◽  
Angelo Camerlenghi ◽  
Lieve E. Vanneste
Keyword(s):  
Antarctic Peninsula ◽  
Continental Rise ◽  
History Of ◽  
The Antarctic
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