Carcass of a bowhead whale (Balaena mysticetus) found in the lateral moraine of the Jemelianovbreen glacier, eastern Svalbard

An 8 m long carcass of a bowhead whale (Balaena mysticetus) melted out from remnant glacier ice in the lateral moraine of the Jemelianovbreen glacier in August 1996. Folded and sheared sediment bands in the ice suggest that the whale was incorporated during an advance of the glacier. The whale'...

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Published in:Polar Research
Main Authors: Lønne, Ida, Fuglei, Eva
Format: Article in Journal/Newspaper
Language:English
Published: Norwegian Polar Institute 1997
Subjects:
Online Access:https://polarresearch.net/index.php/polar/article/view/2277
https://doi.org/10.3402/polar.v16i1.6621
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spelling ftjpolarres:oai:journals.openacademia.net:article/2277 2023-05-15T15:35:58+02:00 Carcass of a bowhead whale (Balaena mysticetus) found in the lateral moraine of the Jemelianovbreen glacier, eastern Svalbard Lønne, Ida Fuglei, Eva 1997-01-06 application/pdf https://polarresearch.net/index.php/polar/article/view/2277 https://doi.org/10.3402/polar.v16i1.6621 eng eng Norwegian Polar Institute https://polarresearch.net/index.php/polar/article/view/2277/5528 https://polarresearch.net/index.php/polar/article/view/2277 doi:10.3402/polar.v16i1.6621 Copyright (c) 2018 Polar Research Polar Research; Vol. 16 No. 1 (1997); 9-18 1751-8369 info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion 1997 ftjpolarres https://doi.org/10.3402/polar.v16i1.6621 2021-11-11T19:12:21Z An 8 m long carcass of a bowhead whale (Balaena mysticetus) melted out from remnant glacier ice in the lateral moraine of the Jemelianovbreen glacier in August 1996. Folded and sheared sediment bands in the ice suggest that the whale was incorporated during an advance of the glacier. The whale's longitudinal axis was oriented parallel to the direction of the ice-flow, with the thinnest posterior part dipping uFWlow. The posterior section was best preserved with muscles and blubber, although the entire skin surface was strongly decomposed and only a thick fibrous surface was left of the blubber. The abdominal wall was holed, most likely by marine organisms, and partly filled with a compacted mixture of well-sorted gravelly beach sediments and fat. the whale seems to have been incorporated into the glacier together with glaciomarine sediments and carried by the flowing ice to an altitude of ca. 15 m. Jemelianovbreen is a tidewater glacier with two known surge-episodes. The first and most extensive of these occurred ca. 1900 AD and reached ca. 7 km outside the present coast-line. Radiocarbon dating of a fragment of a caudal vertebra yielded 345 ± 40 14C years BP (1535-1660 cal. AD), suggesting that the whale lived some time during the last part of the cold period known as the Little Ice Age. Article in Journal/Newspaper Balaena mysticetus bowhead whale glacier Polar Research Svalbard Tidewater Polar Research (E-Journal) Svalbard Jemelianovbreen ENVELOPE(17.333,17.333,77.367,77.367) Polar Research 16 1 9 18
institution Open Polar
collection Polar Research (E-Journal)
op_collection_id ftjpolarres
language English
description An 8 m long carcass of a bowhead whale (Balaena mysticetus) melted out from remnant glacier ice in the lateral moraine of the Jemelianovbreen glacier in August 1996. Folded and sheared sediment bands in the ice suggest that the whale was incorporated during an advance of the glacier. The whale's longitudinal axis was oriented parallel to the direction of the ice-flow, with the thinnest posterior part dipping uFWlow. The posterior section was best preserved with muscles and blubber, although the entire skin surface was strongly decomposed and only a thick fibrous surface was left of the blubber. The abdominal wall was holed, most likely by marine organisms, and partly filled with a compacted mixture of well-sorted gravelly beach sediments and fat. the whale seems to have been incorporated into the glacier together with glaciomarine sediments and carried by the flowing ice to an altitude of ca. 15 m. Jemelianovbreen is a tidewater glacier with two known surge-episodes. The first and most extensive of these occurred ca. 1900 AD and reached ca. 7 km outside the present coast-line. Radiocarbon dating of a fragment of a caudal vertebra yielded 345 ± 40 14C years BP (1535-1660 cal. AD), suggesting that the whale lived some time during the last part of the cold period known as the Little Ice Age.
format Article in Journal/Newspaper
author Lønne, Ida
Fuglei, Eva
spellingShingle Lønne, Ida
Fuglei, Eva
Carcass of a bowhead whale (Balaena mysticetus) found in the lateral moraine of the Jemelianovbreen glacier, eastern Svalbard
author_facet Lønne, Ida
Fuglei, Eva
author_sort Lønne, Ida
title Carcass of a bowhead whale (Balaena mysticetus) found in the lateral moraine of the Jemelianovbreen glacier, eastern Svalbard
title_short Carcass of a bowhead whale (Balaena mysticetus) found in the lateral moraine of the Jemelianovbreen glacier, eastern Svalbard
title_full Carcass of a bowhead whale (Balaena mysticetus) found in the lateral moraine of the Jemelianovbreen glacier, eastern Svalbard
title_fullStr Carcass of a bowhead whale (Balaena mysticetus) found in the lateral moraine of the Jemelianovbreen glacier, eastern Svalbard
title_full_unstemmed Carcass of a bowhead whale (Balaena mysticetus) found in the lateral moraine of the Jemelianovbreen glacier, eastern Svalbard
title_sort carcass of a bowhead whale (balaena mysticetus) found in the lateral moraine of the jemelianovbreen glacier, eastern svalbard
publisher Norwegian Polar Institute
publishDate 1997
url https://polarresearch.net/index.php/polar/article/view/2277
https://doi.org/10.3402/polar.v16i1.6621
long_lat ENVELOPE(17.333,17.333,77.367,77.367)
geographic Svalbard
Jemelianovbreen
geographic_facet Svalbard
Jemelianovbreen
genre Balaena mysticetus
bowhead whale
glacier
Polar Research
Svalbard
Tidewater
genre_facet Balaena mysticetus
bowhead whale
glacier
Polar Research
Svalbard
Tidewater
op_source Polar Research; Vol. 16 No. 1 (1997); 9-18
1751-8369
op_relation https://polarresearch.net/index.php/polar/article/view/2277/5528
https://polarresearch.net/index.php/polar/article/view/2277
doi:10.3402/polar.v16i1.6621
op_rights Copyright (c) 2018 Polar Research
op_doi https://doi.org/10.3402/polar.v16i1.6621
container_title Polar Research
container_volume 16
container_issue 1
container_start_page 9
op_container_end_page 18
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