Drift bodies in the Prydz Bay Region - a tool to understand the interplay of Antarctic currents and warm and cold periods
The Antarctic Circumpolar Current (ACC) is a massive ocean current and believed to have had a major impact on climate since the late Eocene/early Oligocene. However, its pathway, spatial extent in relation to climate variability and possible regional changes during warm and cold periods are still ha...
Main Authors: | , |
---|---|
Format: | Conference Object |
Language: | unknown |
Published: |
2018
|
Subjects: | |
Online Access: | https://epic.awi.de/id/eprint/48196/ https://hdl.handle.net/10013/epic.90515552-ec45-481e-be3f-ee96dad2d08a |
id |
ftawi:oai:epic.awi.de:48196 |
---|---|
record_format |
openpolar |
spelling |
ftawi:oai:epic.awi.de:48196 2024-09-15T17:38:44+00:00 Drift bodies in the Prydz Bay Region - a tool to understand the interplay of Antarctic currents and warm and cold periods Nielsen, Ricarda Uenzelmann-Neben, Gabriele 2018 https://epic.awi.de/id/eprint/48196/ https://hdl.handle.net/10013/epic.90515552-ec45-481e-be3f-ee96dad2d08a unknown Nielsen, R. orcid:0000-0002-1232-2950 and Uenzelmann-Neben, G. orcid:0000-0002-0115-5923 (2018) Drift bodies in the Prydz Bay Region - a tool to understand the interplay of Antarctic currents and warm and cold periods , AGU Fall meeting, Washington, DC, USA, 10 December 2018 - 15 December 2018 . hdl:10013/epic.90515552-ec45-481e-be3f-ee96dad2d08a EPIC3AGU Fall meeting, Washington, DC, USA, 2018-12-10-2018-12-15 Conference notRev 2018 ftawi 2024-06-24T04:21:00Z The Antarctic Circumpolar Current (ACC) is a massive ocean current and believed to have had a major impact on climate since the late Eocene/early Oligocene. However, its pathway, spatial extent in relation to climate variability and possible regional changes during warm and cold periods are still hardly understood although several models exist. In addition, questions concerning its interactions with and effect on the adjacent Antarctic Slope Current (ASC) and the Antarctic Divergence (AD) are not solved yet. The Prydz Bay/Cooperation Sea area provides a perfect setting to study spatial and temporal changes of the ACC, the ASC and the AD due to the spatial limitations by the southern Kerguelen Plateau in the Northwest. The plateau acts as a northern barrier for the ACC and narrows its path through the Princess Elizabeth Trough. In the south, Prydz Bay has been massively impacted by the advance and retreat of the Amery Ice shelf during warm and cold periods. We have studied the deposition and accumulation history of the Wild drift, the Wilkins drift and the surrounding deep sea in detail by interpreting over 50000 km of multi-channel seismic reflection data in a pseudo 3D-image. Lithology and age information from various ODP Sites were incorporated. We aim to provide a detailed reconstruction model of the prevailing currents, and the interplay of ice sheet dynamics, climate changes and oceanic circulation in the Prydz Bay/Cooperation Sea area during the early Oligocene to the Quaternary. First results suggest onset of a drift formation in the early Oligocene and major changes during warm periods with intensification of currents and ice retreat prior to the Miocene Climatic Optimum. Differences in the seismostratigraphic pattern point towards a shift of the material sources, depending on cold or warm periods and suggest an interplay between down-slope, i.e., ice sheet driven input versus along-slope, i.e., current controlled sediment transport during the Miocene. Conference Object Amery Ice Shelf Antarc* Antarctic Cooperation Sea Ice Sheet Ice Shelf Prydz Bay Alfred Wegener Institute for Polar- and Marine Research (AWI): ePIC (electronic Publication Information Center) |
institution |
Open Polar |
collection |
Alfred Wegener Institute for Polar- and Marine Research (AWI): ePIC (electronic Publication Information Center) |
op_collection_id |
ftawi |
language |
unknown |
description |
The Antarctic Circumpolar Current (ACC) is a massive ocean current and believed to have had a major impact on climate since the late Eocene/early Oligocene. However, its pathway, spatial extent in relation to climate variability and possible regional changes during warm and cold periods are still hardly understood although several models exist. In addition, questions concerning its interactions with and effect on the adjacent Antarctic Slope Current (ASC) and the Antarctic Divergence (AD) are not solved yet. The Prydz Bay/Cooperation Sea area provides a perfect setting to study spatial and temporal changes of the ACC, the ASC and the AD due to the spatial limitations by the southern Kerguelen Plateau in the Northwest. The plateau acts as a northern barrier for the ACC and narrows its path through the Princess Elizabeth Trough. In the south, Prydz Bay has been massively impacted by the advance and retreat of the Amery Ice shelf during warm and cold periods. We have studied the deposition and accumulation history of the Wild drift, the Wilkins drift and the surrounding deep sea in detail by interpreting over 50000 km of multi-channel seismic reflection data in a pseudo 3D-image. Lithology and age information from various ODP Sites were incorporated. We aim to provide a detailed reconstruction model of the prevailing currents, and the interplay of ice sheet dynamics, climate changes and oceanic circulation in the Prydz Bay/Cooperation Sea area during the early Oligocene to the Quaternary. First results suggest onset of a drift formation in the early Oligocene and major changes during warm periods with intensification of currents and ice retreat prior to the Miocene Climatic Optimum. Differences in the seismostratigraphic pattern point towards a shift of the material sources, depending on cold or warm periods and suggest an interplay between down-slope, i.e., ice sheet driven input versus along-slope, i.e., current controlled sediment transport during the Miocene. |
format |
Conference Object |
author |
Nielsen, Ricarda Uenzelmann-Neben, Gabriele |
spellingShingle |
Nielsen, Ricarda Uenzelmann-Neben, Gabriele Drift bodies in the Prydz Bay Region - a tool to understand the interplay of Antarctic currents and warm and cold periods |
author_facet |
Nielsen, Ricarda Uenzelmann-Neben, Gabriele |
author_sort |
Nielsen, Ricarda |
title |
Drift bodies in the Prydz Bay Region - a tool to understand the interplay of Antarctic currents and warm and cold periods |
title_short |
Drift bodies in the Prydz Bay Region - a tool to understand the interplay of Antarctic currents and warm and cold periods |
title_full |
Drift bodies in the Prydz Bay Region - a tool to understand the interplay of Antarctic currents and warm and cold periods |
title_fullStr |
Drift bodies in the Prydz Bay Region - a tool to understand the interplay of Antarctic currents and warm and cold periods |
title_full_unstemmed |
Drift bodies in the Prydz Bay Region - a tool to understand the interplay of Antarctic currents and warm and cold periods |
title_sort |
drift bodies in the prydz bay region - a tool to understand the interplay of antarctic currents and warm and cold periods |
publishDate |
2018 |
url |
https://epic.awi.de/id/eprint/48196/ https://hdl.handle.net/10013/epic.90515552-ec45-481e-be3f-ee96dad2d08a |
genre |
Amery Ice Shelf Antarc* Antarctic Cooperation Sea Ice Sheet Ice Shelf Prydz Bay |
genre_facet |
Amery Ice Shelf Antarc* Antarctic Cooperation Sea Ice Sheet Ice Shelf Prydz Bay |
op_source |
EPIC3AGU Fall meeting, Washington, DC, USA, 2018-12-10-2018-12-15 |
op_relation |
Nielsen, R. orcid:0000-0002-1232-2950 and Uenzelmann-Neben, G. orcid:0000-0002-0115-5923 (2018) Drift bodies in the Prydz Bay Region - a tool to understand the interplay of Antarctic currents and warm and cold periods , AGU Fall meeting, Washington, DC, USA, 10 December 2018 - 15 December 2018 . hdl:10013/epic.90515552-ec45-481e-be3f-ee96dad2d08a |
_version_ |
1810475016317304832 |