General Project Info Project-id Project-title Project-acronym Project-reference Associated-programme Project-centre name Begin-date End-date Ongoing Location Geographical coverage Area-type Sea-area Descriptions Summary Reference Keywords Data theme Project-website Centre-Information Project centre Role-of-research-centre Other-partners-andcountries Contact Contact post address Contact phone Contact fax 49-001-015 SEdiment Drifts of the ANtarctic Offshore SEDANO SEDANO I, SEDANO II Italian Research Programme in Antartica, Programma Nazionale Ricerche in Antartide OGS, Istituto Nazionale di Oceanografia e di Geofisica Sperimentale, Trieste 01/06/1994 31/05/1998 No Antartic Peninsula Pacific Margin (67-65S, 82-70W) Coastal and Offshore SOUTHERN OCEAN REGION, Southern Ocean (localised) SEDANO Project aim to understand the origin of the glacial depositional systems found offshore the Pacific margin of the Antarctic Peninsula. Four main glacial depositional systems have been identified. Geophysical surveys were carried out during these two projects The cores collected in this area characterise the sediment drifts as composed by fine-grained, poorly-sorted sediments, sourced from turbidity currents generated on the continental slope. To elucidate the role of dispersal and redistribution of sediments by bottom currents, three one-year long bottom current records in the area of the mound 7 were collected as well as nine CTD measurements collected in the same area . It is worthwhile noting the importance of this data set, constituting the first current measurements available in the Pacific margin of the Antarctic Peninsula. The aim of this work threefold: to infer which are the major large scale processes that govern bottom current regime, to understand the Bottom Boundary Layer (BBL) dynamics, and to assess the potential for resuspension induced by the measured currents. Camerlenghi, A., Crise, A., Pudsey, C.J., Accerboni, E., Laterza, R. and Rebesco, M. 1997. Ten-month observation of the bottom current regime across a sediment drift of the Pacific margin of the Antarctic Peninsula. Antarctic Science, 9, 426–433. Pudsey, C.J. and Camerlenghi, A. 1998. Glacial–interglacial deposition on a sediment drift on the Pacific margin of the Antarctic Peninsula. Antarctic Science, 10, 1–23. Giorgetti A., A. Crise, R. Laterza, L. Perini, M. Rabesco and A. Camerlenghi, 2003, Water masses and bottom boundary layer dynamics above a sediment drifts of the Antarctic Peninsula Pacific Margin, Antarctic Science, 15 (4), 537-546. Monitoring, bottom-current, sedimentation, multichannel seismic reflection profiles, sediment cores PHYSICAL OCEANOGRAPHY, GEOLOGY - GEOPHYSICS – SEDIMENTATION, SEAFLOOR SAMPLES (eg core,dredge,grab) http://doga.ogs.trieste.it/ OGS, Istituto Nazionale di Oceanografia e di Geofisica Sperimentale, Trieste Workpackage coordinator British Antarctic Survey (GB), Istituto di Geologia Marina di Bologna (Italy), University of Trieste (Italy), ETH Zurich (CH), Geomare Sud (Italy) Dr. Alessandro Crise (OGS, Italy) OGS, Istituto Nazionale di Oceanografia e di Geofisica Sperimentale, Trieste, Borgo Grotta Gigante 42/c, 34010 Sgonico (Trieste), Italy +39 040 2140205 +39-040-2140266 Contact email Administration Completed by Currency date Revision-date Collating-centre Modify-date acrise@ogs.trieste.it A. Giorgetti, OGS, Italy (agiorgetti@ogs.trieste.it) 10/05/2005 10/05/2005 OGS, Trieste, Italy 10/05/2005