Abstract
The Pliocene-Quaternary history of the southwestern Adriatic margin, represented by a complex contourite depositional system, records the palaeoceanography of the basin and the interactions between oceanographic processes and the uneven slope morphology that resulted from tectonic deformation. Three main stages can be recognized: (1) during the Pliocene, a giant sediment drift formed on the southern flank of the slope-transverse Gondola anticline that focused and accelerated the flow of slope-parallel bottom currents; (2) since the early to middle Pleistocene transition, a reorganization of bottom-current pathways led to a sharp change in the sedimentary architecture of the margin that became dominated by the growth of contourite deposits; (3) as of 350 ka, landward-migrating contourites on the outer shelf (less than 120 m water depth) reflect the presence of bottom currents also in shallow waters. This analysis of the sedimentary stacking pattern of the contourite depositional system that developed along the south-western Adriatic margin since the Pliocene enables disentangling the processes that controlled changes in bottom-current activity, demonstrating that bottom-current deposits constitute the bulk of depositional sequences at the Milankovitch timescale.
Original language | English |
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Pages (from-to) | 67-79 |
Number of pages | 13 |
Journal | Geo-Marine Letters |
Volume | 36 |
Issue number | 1 |
Early online date | 29 Sept 2015 |
DOIs | |
Publication status | Published - Feb 2016 |
Bibliographical note
We would like to thank Giovanni Bortoluzzi and Valentina Ferrante for the acquisition and processing of the multichannel seismic lines Adriaseismic 2009. We are grateful to the editors B.W. Flemming and M.T. Delafontaine for their thoughtful comments that improved the readability of the manuscript, and to A. Viana and an anonymous reviewer for their comments on an earlier version of this article. This work was funded by the Flagship Project RITMARE - The Italian Research for the Sea, coordinated by the Italian National Research Council and funded by the Italian Ministry of Education, University and Research as part of the National Research Program 2011–2013. This is ISMAR-CNR contribution number 1875.Keywords
- MEDITERRANEAN OUTFLOW WATER
- SEA GENERAL-CIRCULATION
- NORTH-ATLANTIC OCEAN
- BARI CANYON
- SHELF-EDGE
- CONTINENTAL RISE
- STOREGGA SLIDE
- SLOPE
- VARIABILITY
- DRIFTS