New insights into marine-based paleo-ice sheet dynamics and glaciomarine depositional environment in an interfan area between ice stream-derived Trough Mouth Fans, off West Svalbard
New insights into marine-based paleo-ice sheet dynamics and glaciomarine depositional environment in an interfan area between ice stream-derived Trough Mouth Fans, off West Svalbard
Understanding the dynamic history of the marine-based paleo-Svalbard Ice Sheet provides critical insights into past climate change and the interactions between the ocean system and the cryosphere. High-resolution seismic imaging is needed to decipher the glacial history of the western Svalbard continental margin, which has experienced multiple glaciations throughout the Quaternary period. Glaciomarine sediments preserved on the continental margin provide a detailed record of these events. We integrate high-resolution airgun seismic (vertical resolution 5 m), and deep-towed transducer seismic data (vertical and horizontal resolutions 1 and 3 m, respectively) along with age constraints derived from a piston core to determine the seismic stratigraphic framework, depositional architecture, and sedimentation processes of the interfan area between the Kongsfjorden and Isfjorden Trough Mouth Fans (TMFs). Age constraints from seafloor drilling indicate that the build-up of the Kongsfjorden TMF began around 1.2 million years ago. Our data analysis reveals four distinct shelf-edge glaciations during the Weichselian period, dated at 120–110 ka, ~90 ka, 61–54 ka, and ~24 ka. These glacial units on the upper continental slope contain debris materials transported by slow-moving ice sheets. During maximum glacial expansion, iceberg calving created V-shaped indentations, and glaciogenic debris flows carved erosional troughs. Seismic interpretation and debris flow modeling aided in understanding the development of lensoid debris morphology, stacking patterns, and the evolution of debris lobes resulting from local variations in bottom topography. This study underscores the value of using multiple high-resolution seismic data sources to enhance our understanding of the glacial history and depositional processes in the interfan region.
Trivedi, Akash
15ec9e24-3495-4623-a442-e5758dffd9e6
Sarkar, Sudipta
53e08952-8fd6-4c90-bb39-15f71baa494d
Ker, Stephan
3daed197-4ba3-4ed2-b7d4-ff267c2350c1
Minshull, Tim A.
bf413fb5-849e-4389-acd7-0cb0d644e6b8
Hafildason, Haflidi
e92b0aa2-a41f-4402-bf76-637c423fc146
18 March 2025
Trivedi, Akash
15ec9e24-3495-4623-a442-e5758dffd9e6
Sarkar, Sudipta
53e08952-8fd6-4c90-bb39-15f71baa494d
Ker, Stephan
3daed197-4ba3-4ed2-b7d4-ff267c2350c1
Minshull, Tim A.
bf413fb5-849e-4389-acd7-0cb0d644e6b8
Hafildason, Haflidi
e92b0aa2-a41f-4402-bf76-637c423fc146
Trivedi, Akash, Sarkar, Sudipta, Ker, Stephan, Minshull, Tim A. and Hafildason, Haflidi
(2025)
New insights into marine-based paleo-ice sheet dynamics and glaciomarine depositional environment in an interfan area between ice stream-derived Trough Mouth Fans, off West Svalbard.
Quaternary Science Reviews, 356.
(doi:10.1016/j.quascirev.2025.109281).
Abstract
Understanding the dynamic history of the marine-based paleo-Svalbard Ice Sheet provides critical insights into past climate change and the interactions between the ocean system and the cryosphere. High-resolution seismic imaging is needed to decipher the glacial history of the western Svalbard continental margin, which has experienced multiple glaciations throughout the Quaternary period. Glaciomarine sediments preserved on the continental margin provide a detailed record of these events. We integrate high-resolution airgun seismic (vertical resolution 5 m), and deep-towed transducer seismic data (vertical and horizontal resolutions 1 and 3 m, respectively) along with age constraints derived from a piston core to determine the seismic stratigraphic framework, depositional architecture, and sedimentation processes of the interfan area between the Kongsfjorden and Isfjorden Trough Mouth Fans (TMFs). Age constraints from seafloor drilling indicate that the build-up of the Kongsfjorden TMF began around 1.2 million years ago. Our data analysis reveals four distinct shelf-edge glaciations during the Weichselian period, dated at 120–110 ka, ~90 ka, 61–54 ka, and ~24 ka. These glacial units on the upper continental slope contain debris materials transported by slow-moving ice sheets. During maximum glacial expansion, iceberg calving created V-shaped indentations, and glaciogenic debris flows carved erosional troughs. Seismic interpretation and debris flow modeling aided in understanding the development of lensoid debris morphology, stacking patterns, and the evolution of debris lobes resulting from local variations in bottom topography. This study underscores the value of using multiple high-resolution seismic data sources to enhance our understanding of the glacial history and depositional processes in the interfan region.
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Accepted/In Press date: 24 February 2025
e-pub ahead of print date: 18 March 2025
Published date: 18 March 2025
Identifiers
Local EPrints ID: 499857
URI: http://eprints.soton.ac.uk/id/eprint/499857
ISSN: 0277-3791
PURE UUID: cda5a3e3-60f4-4ece-baab-fd9c968d81d2
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Date deposited: 08 Apr 2025 16:30
Last modified: 09 Apr 2025 01:37
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Contributors
Author:
Akash Trivedi
Author:
Sudipta Sarkar
Author:
Stephan Ker
Author:
Haflidi Hafildason
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