Sedimentology of cores from the continental rise west of the Antarctic Peninsula, supplement to: Pudsey, Carol J (2000): Sedimentation on the continental rise west of the Antarctic Peninsula over the last three glacial cycles. Marine Geology, 167(3-4), 313-338

Carol J Pudsey
The continental rise west of the Antarctic Peninsula includes a number of large sediment mounds interpreted as contourite drifts. Cores from six sediment drifts spanning some 650 km of the margin and 48 of latitude have been dated using chemical and isotopic tracers of palaeoproductivity and diatom biostratigraphy. Interglacial sedimentation rates range from 1.1 to 4.3 cm/ka. Glacial sedimentation rates range from 1.8 to 13.5 cm/ka, and decrease from proximal to distal sites on each...
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