Contamination of 8.2 ka cold climate records by the Storegga tsunami in the Nordic Seas
The 8200-year BP cooling event is reconstructed in part from sediments in the Norwegian and North Seas. Here we show that these sediments have been reworked by the Storegga tsunami – dated to the coldest decades of the 8.2 ka event. We simulate the maximum tsunami flow velocity to be 2–5 m/s on the...
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Online Access: | https://hdl.handle.net/10037/33373 https://doi.org/10.1038/s41467-024-47347-9 |
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ftunivtroemsoe:oai:munin.uit.no:10037/33373 2024-05-12T08:07:21+00:00 Contamination of 8.2 ka cold climate records by the Storegga tsunami in the Nordic Seas Bondevik, Stein Risebrobakken, Bjørg Gibbons, Steven J. Rasmussen, Tine Lander Løvholt, Finn 2024-04-04 https://hdl.handle.net/10037/33373 https://doi.org/10.1038/s41467-024-47347-9 eng eng Springer Nature Nature Communications Bondevik S, Risebrobakken B, Gibbons SJ, Rasmussen TLR, Løvholt F. Contamination of 8.2 ka cold climate records by the Storegga tsunami in the Nordic Seas. Nature Communications. 2024;15 FRIDAID 2259796 doi:10.1038/s41467-024-47347-9 2041-1723 https://hdl.handle.net/10037/33373 Attribution 4.0 International (CC BY 4.0) openAccess Copyright 2024 The Author(s) https://creativecommons.org/licenses/by/4.0 Journal article Tidsskriftartikkel Peer reviewed publishedVersion 2024 ftunivtroemsoe https://doi.org/10.1038/s41467-024-47347-9 2024-04-17T14:00:51Z The 8200-year BP cooling event is reconstructed in part from sediments in the Norwegian and North Seas. Here we show that these sediments have been reworked by the Storegga tsunami – dated to the coldest decades of the 8.2 ka event. We simulate the maximum tsunami flow velocity to be 2–5 m/s on the shelf offshore western Norway and in the shallower North Sea, and up to about 1 m/s down to a water depth of 1000 m. We re-investigate sediment core MD95-2011 and found the cold-water foraminifera in the 8.2 ka layer to be re-deposited and 11,000 years of age. Oxygen isotopes of the recycled foraminifera might have led to an interpretation of a too large and dramatic climate cooling. Our simulations imply that large parts of the sea floor in the Norwegian and North Seas probably were reworked by currents during the Storegga tsunami. Article in Journal/Newspaper Nordic Seas University of Tromsø: Munin Open Research Archive Norway Storegga ENVELOPE(18.251,18.251,68.645,68.645) Nature Communications 15 1 |
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Open Polar |
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University of Tromsø: Munin Open Research Archive |
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ftunivtroemsoe |
language |
English |
description |
The 8200-year BP cooling event is reconstructed in part from sediments in the Norwegian and North Seas. Here we show that these sediments have been reworked by the Storegga tsunami – dated to the coldest decades of the 8.2 ka event. We simulate the maximum tsunami flow velocity to be 2–5 m/s on the shelf offshore western Norway and in the shallower North Sea, and up to about 1 m/s down to a water depth of 1000 m. We re-investigate sediment core MD95-2011 and found the cold-water foraminifera in the 8.2 ka layer to be re-deposited and 11,000 years of age. Oxygen isotopes of the recycled foraminifera might have led to an interpretation of a too large and dramatic climate cooling. Our simulations imply that large parts of the sea floor in the Norwegian and North Seas probably were reworked by currents during the Storegga tsunami. |
format |
Article in Journal/Newspaper |
author |
Bondevik, Stein Risebrobakken, Bjørg Gibbons, Steven J. Rasmussen, Tine Lander Løvholt, Finn |
spellingShingle |
Bondevik, Stein Risebrobakken, Bjørg Gibbons, Steven J. Rasmussen, Tine Lander Løvholt, Finn Contamination of 8.2 ka cold climate records by the Storegga tsunami in the Nordic Seas |
author_facet |
Bondevik, Stein Risebrobakken, Bjørg Gibbons, Steven J. Rasmussen, Tine Lander Løvholt, Finn |
author_sort |
Bondevik, Stein |
title |
Contamination of 8.2 ka cold climate records by the Storegga tsunami in the Nordic Seas |
title_short |
Contamination of 8.2 ka cold climate records by the Storegga tsunami in the Nordic Seas |
title_full |
Contamination of 8.2 ka cold climate records by the Storegga tsunami in the Nordic Seas |
title_fullStr |
Contamination of 8.2 ka cold climate records by the Storegga tsunami in the Nordic Seas |
title_full_unstemmed |
Contamination of 8.2 ka cold climate records by the Storegga tsunami in the Nordic Seas |
title_sort |
contamination of 8.2 ka cold climate records by the storegga tsunami in the nordic seas |
publisher |
Springer Nature |
publishDate |
2024 |
url |
https://hdl.handle.net/10037/33373 https://doi.org/10.1038/s41467-024-47347-9 |
long_lat |
ENVELOPE(18.251,18.251,68.645,68.645) |
geographic |
Norway Storegga |
geographic_facet |
Norway Storegga |
genre |
Nordic Seas |
genre_facet |
Nordic Seas |
op_relation |
Nature Communications Bondevik S, Risebrobakken B, Gibbons SJ, Rasmussen TLR, Løvholt F. Contamination of 8.2 ka cold climate records by the Storegga tsunami in the Nordic Seas. Nature Communications. 2024;15 FRIDAID 2259796 doi:10.1038/s41467-024-47347-9 2041-1723 https://hdl.handle.net/10037/33373 |
op_rights |
Attribution 4.0 International (CC BY 4.0) openAccess Copyright 2024 The Author(s) https://creativecommons.org/licenses/by/4.0 |
op_doi |
https://doi.org/10.1038/s41467-024-47347-9 |
container_title |
Nature Communications |
container_volume |
15 |
container_issue |
1 |
_version_ |
1798850016367869952 |