nerc.ac.uk

Mixed biosiliceous-terrigenous sedimentation under the Antarctic Circumpolar Current, Scotia Sea

Pudsey, Carol J.; Howe, John A.. 2002 Mixed biosiliceous-terrigenous sedimentation under the Antarctic Circumpolar Current, Scotia Sea. In: Stow, D.A.V.; Pudsey, C.J.; Howe, J.A.; Faugères, J.-C.; Viana, A.R., (eds.) Deep-water contourite systems: modern drifts and ancient series, seismic and sedimentary characteristics. London, Geological Society of London, 325-336. (Geological Society Memoir, 22).

Full text not available from this repository. (Request a copy)

Abstract/Summary

Sediment supply to the Scotia Sea is controlled by the east-flowing Antarctic Circumpolar Current (ACC) with some Weddell Gyre influence in the south. Near-bottom flow is unsteady with frequent changes in flow direction and episodic benthic storms. Near the North Scotia Ridge, mounds of sediment up to 1 km thick have accumulated on lower Miocene ocean floor. The basins farther south contain up to 2 km of sediment which is flat-lying or draped rather than mounded. Sediment cores exhibit a biogenic-terrigenous cyclicity related to glacial-interglacial cycles. Grain-size data suggest that ACC flow was stronger during glacials than interglacials.

Item Type: Publication - Book Section
Programmes: BAS Programmes > Other
ISBN: 1862390924
NORA Subject Terms: Marine Sciences
Earth Sciences
Date made live: 14 Mar 2012 11:07 +0 (UTC)
URI: https://nora.nerc.ac.uk/id/eprint/14170

Actions (login required)

View Item View Item

Document Downloads

Downloads for past 30 days

Downloads per month over past year

More statistics for this item...