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Please use this identifier to cite or link to this item: http://hdl.handle.net/10261/18739
Title: Miocene to Recent contourite drifts development in the northern Weddell Sea (Antarctica)
Authors: Maldonado, Andrés; Barnolas, Antonio; Bohoyo, Fernando; Escutia, Carlota; Galindo-Zaldívar, Jesús; Hernández-Molina, Francisco J.; Jabaloy, Antonio; Lobo, F. J.; Nelson, C. Hans; Rodríguez-Fernández, José; Somoza, Luis; Vázquez, Juan Tomas
Keywords: Contourite drifts
Antarctic paleoceanography
Weddell Gyre
Issue Date: Feb-2005
Publisher: Elsevier
Citation: Global and Planetary Change 45(1-3): 99-129 (2006)
Abstract: Multichannel and high-resolution seismic profiles complemented with swath bathymetry show a variety of contourite deposits in the northern Weddell Sea resulting from the interaction between bottom currents and the seafloor physiography. Seven types of contourite drifts are identified based on the seismic signature, reflector configuration and geometry of the depositional bodies. Giant elongated–mounded drifts are widespread in the area and associated with major channelized contour currents that flow at the base of large ridges. Thick basement/tectonic drifts result from the seafloor disruptions of the currents caused by the irregularities of the near-surface basement morphology. Sheeted drifts occur under the main core of the Weddell Gyre and also in areas of the abyssal plain away from the main flows. Various types of drifts in-fill depressions or are plastered against steep bathymetric ridges that intersect contour currents. The regional distribution of the drifts is mainly controlled by the physiography of the basin and the confined or unconfined nature of the bottom-current flows. The northern Weddell Sea is a region dominated by contourite processes and thus provides an area to compare contourite drifts with turbidite systems. The giant elongated–mounded drifts have a net asymmetry of the body, in contrast to turbidite channel–levee complexes that develop levees on each side of an axial turbidite channel. The basement/tectonic drifts prograde parallel to the main flow and are plastered following the irregularities of the basement unlike turbidite deposits. Other drifts, in contrast, show internal reflector characteristics similar to turbidite systems, such as the sheeted drifts. In these cases, however, the associations of turbidite and drift deposits are different. The giant elongate-mounded drifts are stacked along the margins and elongate or transverse drift sequences are observed in the basin centre of confined basins. In the unconfined setting, the drifts are normally asymmetric in relation to the marginal channel moats and sheeted drifts develop laterally from the ridges. In turbidite systems of confined or unconfined settings, generally symmetrical proximal channel–levee complexes evolve downstream to sheetlike basin plain sequences. Five main seismic units separated by regional unconformities are recognized above the oceanic basement. The age of the deposits is based on the magnetic anomalies of the oceanic crust and the overlying seismic sequences. The external geometry and acoustic character of the seismic units indicate strong bottom-current processes, except for the basal deposits attributed to the Early Miocene. The development of extensive drifts in the deposits of Unit 4 (not, vert, similarMiddle Miocene) shows the initial influence of the Weddell Sea Bottom Water (WSBW). The opening of the connection of Jane Basin with the Scotia Sea also is marked by a regional unconformity that records a reorganization of bottom flows. The two uppermost Units 1 and 2 (Late Miocene to Recent) indicate intensified bottom currents, which may reflect the increased production of WSBW. The evolution through time of the contourite deposits and the distribution of regional unconformities reflect the ice sheet dynamics that controlled the production of Antarctic Bottom Water (AABW).
Description: 31 pages, 13 figures, 1 table.
Publisher version (URL): http://dx.doi.org/10.1016/j.gloplacha.2004.09.013
URI: http://hdl.handle.net/10261/18739
ISSN: 0169-7722
DOI: 10.1016/j.gloplacha.2004.09.013
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