Deep-water sand transfer by hyperpycnal flows, the Eocene of Spitsbergen, Arctic Norway
Flood-generated hyperpycnal flows are dense, sediment-laden, turbulent flows that can form long-lived, bottom-hugging turbidity currents, which undoubtedly transport large volumes of fine-grained sediments into the ocean. However, their ability in transferring sand into deep-water basins is debated....
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Online Access: | https://hdl.handle.net/10037/29230 https://doi.org/10.1111/sed.13105 |
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ftunivtroemsoe:oai:munin.uit.no:10037/29230 2023-06-11T04:07:34+02:00 Deep-water sand transfer by hyperpycnal flows, the Eocene of Spitsbergen, Arctic Norway Grundvåg, Sten-Andreas Helland-Hansen, William Johannessen, Erik P. Eggenhuisen, Joris T. Pohl, Florian Spychala, Yvonne T. 2023-05-11 https://hdl.handle.net/10037/29230 https://doi.org/10.1111/sed.13105 eng eng Wiley Sedimentology Norges forskningsråd: 228107 Grundvåg S.-A., Helland-Hansen W, Johannessen EP, Eggenhuisen JT, Pohl F, Spychala YT. Deep-water sand transfer by hyperpycnal flows, the Eocene of Spitsbergen, Arctic Norway. Sedimentology. 2023 FRIDAID 2147081 doi:10.1111/sed.13105 0037-0746 1365-3091 https://hdl.handle.net/10037/29230 Attribution 4.0 International (CC BY 4.0) Copyright 2023 The Author(s) https://creativecommons.org/licenses/by/4.0 Journal article Tidsskriftartikkel Peer reviewed acceptedVersion 2023 ftunivtroemsoe https://doi.org/10.1111/sed.13105 2023-05-17T23:06:11Z Flood-generated hyperpycnal flows are dense, sediment-laden, turbulent flows that can form long-lived, bottom-hugging turbidity currents, which undoubtedly transport large volumes of fine-grained sediments into the ocean. However, their ability in transferring sand into deep-water basins is debated. This study presents sedimentological evidence of sandy hyperpycnal flow deposits (hyperpycnites) in a series of basin floor lobe complexes associated with a progradational shelf margin in the Eocene of Spitsbergen, Arctic Norway. Four coexisting types of sediment gravity flow deposits are recognized: (i) sandy hyperpycnites deposited by quasi-steady hyperpycnal flows; (ii) turbidites deposited by waning, surge-type turbidity currents; (iii) hybrid event beds deposited by transitional flows; and (iv) mass transport deposits emplaced during rare slope failures. The abundance of thick-bedded massive sandstones, frequent bed amalgamation, the distribution of hyperpycnites across the lobes and the abundance and systematic occurrence of plant-rich hybrid event beds and associated climbing ripple cross-laminated beds in the lobe fringes, suggest that hyperpycnal flow was the most important mechanism driving lobe progradation. Shelf-edge positioned fluvial channels linked to the basin floor lobe complexes via deeply incised, sandstone-filled slope channels, suggest that rivers fed directly onto the slopes where their dense, sand-laden discharges readily generated quasi-steady hyperpycnal flows that regularly reached the basin floor. The composite architecture and complex waxing–waning flow facies configuration of the hyperpycnites is consistent with sustained and concomitant suspension and traction deposition under fluctuating subcritical to supercritical conditions. Similar sandstone beds occur on the clinoform slopes, indicating that the hyperpycnal flows operated likewise on the slope. Plant-rich hybrid event beds indicate transformation of initially turbulent flows by relative enrichment of clay and plant material via ... Article in Journal/Newspaper Arctic Arctic Spitsbergen University of Tromsø: Munin Open Research Archive Arctic Norway Sedimentology |
institution |
Open Polar |
collection |
University of Tromsø: Munin Open Research Archive |
op_collection_id |
ftunivtroemsoe |
language |
English |
description |
Flood-generated hyperpycnal flows are dense, sediment-laden, turbulent flows that can form long-lived, bottom-hugging turbidity currents, which undoubtedly transport large volumes of fine-grained sediments into the ocean. However, their ability in transferring sand into deep-water basins is debated. This study presents sedimentological evidence of sandy hyperpycnal flow deposits (hyperpycnites) in a series of basin floor lobe complexes associated with a progradational shelf margin in the Eocene of Spitsbergen, Arctic Norway. Four coexisting types of sediment gravity flow deposits are recognized: (i) sandy hyperpycnites deposited by quasi-steady hyperpycnal flows; (ii) turbidites deposited by waning, surge-type turbidity currents; (iii) hybrid event beds deposited by transitional flows; and (iv) mass transport deposits emplaced during rare slope failures. The abundance of thick-bedded massive sandstones, frequent bed amalgamation, the distribution of hyperpycnites across the lobes and the abundance and systematic occurrence of plant-rich hybrid event beds and associated climbing ripple cross-laminated beds in the lobe fringes, suggest that hyperpycnal flow was the most important mechanism driving lobe progradation. Shelf-edge positioned fluvial channels linked to the basin floor lobe complexes via deeply incised, sandstone-filled slope channels, suggest that rivers fed directly onto the slopes where their dense, sand-laden discharges readily generated quasi-steady hyperpycnal flows that regularly reached the basin floor. The composite architecture and complex waxing–waning flow facies configuration of the hyperpycnites is consistent with sustained and concomitant suspension and traction deposition under fluctuating subcritical to supercritical conditions. Similar sandstone beds occur on the clinoform slopes, indicating that the hyperpycnal flows operated likewise on the slope. Plant-rich hybrid event beds indicate transformation of initially turbulent flows by relative enrichment of clay and plant material via ... |
format |
Article in Journal/Newspaper |
author |
Grundvåg, Sten-Andreas Helland-Hansen, William Johannessen, Erik P. Eggenhuisen, Joris T. Pohl, Florian Spychala, Yvonne T. |
spellingShingle |
Grundvåg, Sten-Andreas Helland-Hansen, William Johannessen, Erik P. Eggenhuisen, Joris T. Pohl, Florian Spychala, Yvonne T. Deep-water sand transfer by hyperpycnal flows, the Eocene of Spitsbergen, Arctic Norway |
author_facet |
Grundvåg, Sten-Andreas Helland-Hansen, William Johannessen, Erik P. Eggenhuisen, Joris T. Pohl, Florian Spychala, Yvonne T. |
author_sort |
Grundvåg, Sten-Andreas |
title |
Deep-water sand transfer by hyperpycnal flows, the Eocene of Spitsbergen, Arctic Norway |
title_short |
Deep-water sand transfer by hyperpycnal flows, the Eocene of Spitsbergen, Arctic Norway |
title_full |
Deep-water sand transfer by hyperpycnal flows, the Eocene of Spitsbergen, Arctic Norway |
title_fullStr |
Deep-water sand transfer by hyperpycnal flows, the Eocene of Spitsbergen, Arctic Norway |
title_full_unstemmed |
Deep-water sand transfer by hyperpycnal flows, the Eocene of Spitsbergen, Arctic Norway |
title_sort |
deep-water sand transfer by hyperpycnal flows, the eocene of spitsbergen, arctic norway |
publisher |
Wiley |
publishDate |
2023 |
url |
https://hdl.handle.net/10037/29230 https://doi.org/10.1111/sed.13105 |
geographic |
Arctic Norway |
geographic_facet |
Arctic Norway |
genre |
Arctic Arctic Spitsbergen |
genre_facet |
Arctic Arctic Spitsbergen |
op_relation |
Sedimentology Norges forskningsråd: 228107 Grundvåg S.-A., Helland-Hansen W, Johannessen EP, Eggenhuisen JT, Pohl F, Spychala YT. Deep-water sand transfer by hyperpycnal flows, the Eocene of Spitsbergen, Arctic Norway. Sedimentology. 2023 FRIDAID 2147081 doi:10.1111/sed.13105 0037-0746 1365-3091 https://hdl.handle.net/10037/29230 |
op_rights |
Attribution 4.0 International (CC BY 4.0) Copyright 2023 The Author(s) https://creativecommons.org/licenses/by/4.0 |
op_doi |
https://doi.org/10.1111/sed.13105 |
container_title |
Sedimentology |
_version_ |
1768380756205240320 |