Pre-Last Glacial Maximum glaciations in the Barents Sea: seismic investigations
The main objective of this PhD thesis is to improve understanding of the evolution of pre-Last Glacial Maximum Barents Sea glaciations through the study of glacial deposits from the continental margin using 3D and 2D seismic reflection data. Paper 1 presents a new chronostratigraphic framework, cove...
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UiT Norges arktiske universitet
2024
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ftunivtroemsoe:oai:munin.uit.no:10037/34515 2024-09-30T14:32:51+00:00 Pre-Last Glacial Maximum glaciations in the Barents Sea: seismic investigations Alexandropoulou, Nikolitsa 2024-09-19 https://hdl.handle.net/10037/34515 eng eng UiT Norges arktiske universitet UiT The Arctic University of Norway Paper 1: Alexandropoulou, N., Winsborrow, M., Andreassen, K., Plaza-Faverola, A., Dessandier, P. A., Mattingsdal, R., Baeten, N. & Knies, J. (2021). A Continuous Seismostratigraphic Framework for the Western Svalbard-Barents Sea Margin over the Last 2.7 Ma: Implications for the Late Cenozoic Glacial History of the Svalbard-Barents Sea Ice Sheet. Frontiers in Earth Science, 9 , 327. Also available in Munin at https://hdl.handle.net/10037/21806 . Paper 2: Alexandropoulou, N., Winsborrow, M., Andreassen, K., Plaza-Faverola, A. & Patton, H. Reconstruction of the southwestern Barents Sea Ice Sheet over the last ~200 ka reveals variations in glacial dynamics during the Late Saalian and Weichselian glaciations. (Manuscript). Paper 3: Alexandropoulou, N., Winsborrow, M. & Andreassen, K. Glacial tectonics, fluid flow and gas hydrates on the Bjørnøyrenna Ice Stream bed, SW Barents Sea. (Manuscript). 978-82-8236-588-8 - trykk 978-82-8236-589-5 - pdf https://hdl.handle.net/10037/34515 embargoedAccess Copyright 2024 The Author(s) DOKTOR-004 Doctoral thesis Doktorgradsavhandling 2024 ftunivtroemsoe 2024-09-11T00:09:06Z The main objective of this PhD thesis is to improve understanding of the evolution of pre-Last Glacial Maximum Barents Sea glaciations through the study of glacial deposits from the continental margin using 3D and 2D seismic reflection data. Paper 1 presents a new chronostratigraphic framework, covering the last ∼2.7 Ma, for the Svalbard-Barents Sea margin, using 2D seismic data to extend available ages from sediment cores along the entire 1000 km long margin. This high-temporal-resolution framework was then used to study the evolution of ice sheets in the Barents Sea since ∼2.7 Ma, allowing comparison along the entire margin in a wider regional perspective. In Paper 2, the chronological framework was then used to, for the first time, differentiate glacigenic sediments deposited on the SW Barents Sea continental margin during the Late Saalian (∼0.2 - 0.13 Ma) and Weichselian (<∼0.123 Ma) glacial periods, providing new insights into the evolution and dynamics of Barents Sea ice sheets during these two most recent glaciations. Finally, in Paper 3, recently acquired 3D seismic data on the outer part of the Bjørnøyrenna (Bear Island Trough) was exploited to investigate the interaction of glacial processes, fluid flow, and gas hydrate systems on the SW Barents Sea margin over successive periods of ice advance and retreat during the Quaternary period. Hovedmålet med denne doktorgradsavhandlingen er å forbedre forståelsen av utviklingen av istider i Barentshavet før siste glasiale maksimum gjennom studier av breavsetninger fra kontinentalmarginen ved å bruke 3D og 2D seismiske refleksjonsdata. Artikkel 1 presenterer et nytt kronostratigrafisk rammeverk som dekker de siste ~2.7 Ma for Svalbard-Barentshavmarginen, basert på 2D seismiske data hvilket utvider tilgjengelige stratigrafiske aldre fra sedimentkjerner langs hele den 1000 km lange marginen. Rammeverket med høy temporal oppløsning ble deretter brukt til å studere utviklingen av isdekker i Barentshavet siden ~2.7 Ma, noe som muliggjorde sammenligning langs ... Doctoral or Postdoctoral Thesis Barents Sea Barentshav* Bear Island Sea ice Svalbard University of Tromsø: Munin Open Research Archive Barents Sea Bear Island ENVELOPE(-67.250,-67.250,-68.151,-68.151) Svalbard |
institution |
Open Polar |
collection |
University of Tromsø: Munin Open Research Archive |
op_collection_id |
ftunivtroemsoe |
language |
English |
topic |
DOKTOR-004 |
spellingShingle |
DOKTOR-004 Alexandropoulou, Nikolitsa Pre-Last Glacial Maximum glaciations in the Barents Sea: seismic investigations |
topic_facet |
DOKTOR-004 |
description |
The main objective of this PhD thesis is to improve understanding of the evolution of pre-Last Glacial Maximum Barents Sea glaciations through the study of glacial deposits from the continental margin using 3D and 2D seismic reflection data. Paper 1 presents a new chronostratigraphic framework, covering the last ∼2.7 Ma, for the Svalbard-Barents Sea margin, using 2D seismic data to extend available ages from sediment cores along the entire 1000 km long margin. This high-temporal-resolution framework was then used to study the evolution of ice sheets in the Barents Sea since ∼2.7 Ma, allowing comparison along the entire margin in a wider regional perspective. In Paper 2, the chronological framework was then used to, for the first time, differentiate glacigenic sediments deposited on the SW Barents Sea continental margin during the Late Saalian (∼0.2 - 0.13 Ma) and Weichselian (<∼0.123 Ma) glacial periods, providing new insights into the evolution and dynamics of Barents Sea ice sheets during these two most recent glaciations. Finally, in Paper 3, recently acquired 3D seismic data on the outer part of the Bjørnøyrenna (Bear Island Trough) was exploited to investigate the interaction of glacial processes, fluid flow, and gas hydrate systems on the SW Barents Sea margin over successive periods of ice advance and retreat during the Quaternary period. Hovedmålet med denne doktorgradsavhandlingen er å forbedre forståelsen av utviklingen av istider i Barentshavet før siste glasiale maksimum gjennom studier av breavsetninger fra kontinentalmarginen ved å bruke 3D og 2D seismiske refleksjonsdata. Artikkel 1 presenterer et nytt kronostratigrafisk rammeverk som dekker de siste ~2.7 Ma for Svalbard-Barentshavmarginen, basert på 2D seismiske data hvilket utvider tilgjengelige stratigrafiske aldre fra sedimentkjerner langs hele den 1000 km lange marginen. Rammeverket med høy temporal oppløsning ble deretter brukt til å studere utviklingen av isdekker i Barentshavet siden ~2.7 Ma, noe som muliggjorde sammenligning langs ... |
format |
Doctoral or Postdoctoral Thesis |
author |
Alexandropoulou, Nikolitsa |
author_facet |
Alexandropoulou, Nikolitsa |
author_sort |
Alexandropoulou, Nikolitsa |
title |
Pre-Last Glacial Maximum glaciations in the Barents Sea: seismic investigations |
title_short |
Pre-Last Glacial Maximum glaciations in the Barents Sea: seismic investigations |
title_full |
Pre-Last Glacial Maximum glaciations in the Barents Sea: seismic investigations |
title_fullStr |
Pre-Last Glacial Maximum glaciations in the Barents Sea: seismic investigations |
title_full_unstemmed |
Pre-Last Glacial Maximum glaciations in the Barents Sea: seismic investigations |
title_sort |
pre-last glacial maximum glaciations in the barents sea: seismic investigations |
publisher |
UiT Norges arktiske universitet |
publishDate |
2024 |
url |
https://hdl.handle.net/10037/34515 |
long_lat |
ENVELOPE(-67.250,-67.250,-68.151,-68.151) |
geographic |
Barents Sea Bear Island Svalbard |
geographic_facet |
Barents Sea Bear Island Svalbard |
genre |
Barents Sea Barentshav* Bear Island Sea ice Svalbard |
genre_facet |
Barents Sea Barentshav* Bear Island Sea ice Svalbard |
op_relation |
Paper 1: Alexandropoulou, N., Winsborrow, M., Andreassen, K., Plaza-Faverola, A., Dessandier, P. A., Mattingsdal, R., Baeten, N. & Knies, J. (2021). A Continuous Seismostratigraphic Framework for the Western Svalbard-Barents Sea Margin over the Last 2.7 Ma: Implications for the Late Cenozoic Glacial History of the Svalbard-Barents Sea Ice Sheet. Frontiers in Earth Science, 9 , 327. Also available in Munin at https://hdl.handle.net/10037/21806 . Paper 2: Alexandropoulou, N., Winsborrow, M., Andreassen, K., Plaza-Faverola, A. & Patton, H. Reconstruction of the southwestern Barents Sea Ice Sheet over the last ~200 ka reveals variations in glacial dynamics during the Late Saalian and Weichselian glaciations. (Manuscript). Paper 3: Alexandropoulou, N., Winsborrow, M. & Andreassen, K. Glacial tectonics, fluid flow and gas hydrates on the Bjørnøyrenna Ice Stream bed, SW Barents Sea. (Manuscript). 978-82-8236-588-8 - trykk 978-82-8236-589-5 - pdf https://hdl.handle.net/10037/34515 |
op_rights |
embargoedAccess Copyright 2024 The Author(s) |
_version_ |
1811636928942964736 |