The influence of deep ocean currents in shaping the Argentine continental slope during the Neogene
A complex history of sediment deposition at the Argentine continental margin during the Plio-Pleistocene is indicated by the presence of a canyon system, submarine channels and sediment drifts. We use a dense grid of seismic reflection profiles together with bathymetric data to identify sedimentary...
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ftawi:oai:epic.awi.de:32250 2024-09-15T17:46:40+00:00 The influence of deep ocean currents in shaping the Argentine continental slope during the Neogene Gruetzner, Jens Uenzelmann-Neben, Gabriele Franke, Dieter 2013 https://epic.awi.de/id/eprint/32250/ https://hdl.handle.net/10013/epic.40983 unknown Gruetzner, J. orcid:0000-0001-5445-2393 , Uenzelmann-Neben, G. orcid:0000-0002-0115-5923 and Franke, D. (2013) The influence of deep ocean currents in shaping the Argentine continental slope during the Neogene , 73. Jahrestagung der Deutschen Geophysikalischen Gesellschaft (DGG), Leipzig, 4 March 2013 - 7 March 2013 . hdl:10013/epic.40983 EPIC373. Jahrestagung der Deutschen Geophysikalischen Gesellschaft (DGG), Leipzig, 2013-03-04-2013-03-07 Conference notRev 2013 ftawi 2024-06-24T04:06:16Z A complex history of sediment deposition at the Argentine continental margin during the Plio-Pleistocene is indicated by the presence of a canyon system, submarine channels and sediment drifts. We use a dense grid of seismic reflection profiles together with bathymetric data to identify sedimentary units, map depocenter geometries, separate along-slope from down-slope processes and relate depositional stages to past changes in climate, oceanography and tectonics. The topmost seismic unit in the working area (40 to 48°S) exhibits a variety of co-occurring seismic and morphological features that are diagnostic for both down-slope and along-slope sediment redistribution. In general, current controlled sedimentation is more obvious south of 45°S (“terraces sector”) while in the northern part (“canyons sector”) of the working area contouritic features are reshaped by cross-slope erosion through canyons. Within the canyons sector a slope plastered drift occurs in ~3000 m water depth seaward of the 3000 m isobath. The drift has a thickness of ~400 - 600 m and a width of ~10 - 20 km and can be traced for ~100 km within the working area. The feature likely is a northward extension of a current derived unit identified in the terraces sector and indicates that during the Plio-Pleistocene strong current controlled sedimentation occurred close to the interface between Lower Circumpolar Deep Water (LCDW) and Antarctic Bottom Water (AABW). Erosion via slope cutting canyons is most extensive in ~3000 m water depth at the central Argentine margin (43.5°S, 57.5°W) where multiple branches of the Ameghino canyon system join. None of the canyons in the working area cut into reflectors AR5/AR6 (~14 – 17 Ma), and only the main branches of the Ameghino canyon cut into reflector AR7 (~6 Ma) on the upper slope. Together with the fact that no buried canyons are observed this suggests that canyon development most likely occurred during the late Neogene possibly due to the buildup of slope instabilities caused by vigorous bottom current ... Conference Object Antarc* Antarctic Alfred Wegener Institute for Polar- and Marine Research (AWI): ePIC (electronic Publication Information Center) |
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Alfred Wegener Institute for Polar- and Marine Research (AWI): ePIC (electronic Publication Information Center) |
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ftawi |
language |
unknown |
description |
A complex history of sediment deposition at the Argentine continental margin during the Plio-Pleistocene is indicated by the presence of a canyon system, submarine channels and sediment drifts. We use a dense grid of seismic reflection profiles together with bathymetric data to identify sedimentary units, map depocenter geometries, separate along-slope from down-slope processes and relate depositional stages to past changes in climate, oceanography and tectonics. The topmost seismic unit in the working area (40 to 48°S) exhibits a variety of co-occurring seismic and morphological features that are diagnostic for both down-slope and along-slope sediment redistribution. In general, current controlled sedimentation is more obvious south of 45°S (“terraces sector”) while in the northern part (“canyons sector”) of the working area contouritic features are reshaped by cross-slope erosion through canyons. Within the canyons sector a slope plastered drift occurs in ~3000 m water depth seaward of the 3000 m isobath. The drift has a thickness of ~400 - 600 m and a width of ~10 - 20 km and can be traced for ~100 km within the working area. The feature likely is a northward extension of a current derived unit identified in the terraces sector and indicates that during the Plio-Pleistocene strong current controlled sedimentation occurred close to the interface between Lower Circumpolar Deep Water (LCDW) and Antarctic Bottom Water (AABW). Erosion via slope cutting canyons is most extensive in ~3000 m water depth at the central Argentine margin (43.5°S, 57.5°W) where multiple branches of the Ameghino canyon system join. None of the canyons in the working area cut into reflectors AR5/AR6 (~14 – 17 Ma), and only the main branches of the Ameghino canyon cut into reflector AR7 (~6 Ma) on the upper slope. Together with the fact that no buried canyons are observed this suggests that canyon development most likely occurred during the late Neogene possibly due to the buildup of slope instabilities caused by vigorous bottom current ... |
format |
Conference Object |
author |
Gruetzner, Jens Uenzelmann-Neben, Gabriele Franke, Dieter |
spellingShingle |
Gruetzner, Jens Uenzelmann-Neben, Gabriele Franke, Dieter The influence of deep ocean currents in shaping the Argentine continental slope during the Neogene |
author_facet |
Gruetzner, Jens Uenzelmann-Neben, Gabriele Franke, Dieter |
author_sort |
Gruetzner, Jens |
title |
The influence of deep ocean currents in shaping the Argentine continental slope during the Neogene |
title_short |
The influence of deep ocean currents in shaping the Argentine continental slope during the Neogene |
title_full |
The influence of deep ocean currents in shaping the Argentine continental slope during the Neogene |
title_fullStr |
The influence of deep ocean currents in shaping the Argentine continental slope during the Neogene |
title_full_unstemmed |
The influence of deep ocean currents in shaping the Argentine continental slope during the Neogene |
title_sort |
influence of deep ocean currents in shaping the argentine continental slope during the neogene |
publishDate |
2013 |
url |
https://epic.awi.de/id/eprint/32250/ https://hdl.handle.net/10013/epic.40983 |
genre |
Antarc* Antarctic |
genre_facet |
Antarc* Antarctic |
op_source |
EPIC373. Jahrestagung der Deutschen Geophysikalischen Gesellschaft (DGG), Leipzig, 2013-03-04-2013-03-07 |
op_relation |
Gruetzner, J. orcid:0000-0001-5445-2393 , Uenzelmann-Neben, G. orcid:0000-0002-0115-5923 and Franke, D. (2013) The influence of deep ocean currents in shaping the Argentine continental slope during the Neogene , 73. Jahrestagung der Deutschen Geophysikalischen Gesellschaft (DGG), Leipzig, 4 March 2013 - 7 March 2013 . hdl:10013/epic.40983 |
_version_ |
1810494984017674240 |