Deglaciation and palaeoclimate of the Andfjord‐Vågsfjord area, North Norway
This paper reviews the deglaciation history and palaeoclimate from 22 to 9.5 14 Cka BP in the Andfjord‐Vagsfjord area. Eight main glacial events are recorded: The Egga‐I (>22 14 Cka BP), the Bjerka, the Egga‐II (>14.6 14 Cka BP), the Flesen (14.5 14 Cka BP), the D (13.8–13.2 14 Cka BP), the Sk...
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crwiley:10.1111/j.1502-3885.2002.tb01060.x 2024-09-09T19:32:15+00:00 Deglaciation and palaeoclimate of the Andfjord‐Vågsfjord area, North Norway VORREN, TORE O. PLASSEN, LIV 2002 http://dx.doi.org/10.1111/j.1502-3885.2002.tb01060.x https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fj.1502-3885.2002.tb01060.x https://onlinelibrary.wiley.com/doi/pdf/10.1111/j.1502-3885.2002.tb01060.x en eng Wiley http://onlinelibrary.wiley.com/termsAndConditions#vor Boreas volume 31, issue 2, page 97-125 ISSN 0300-9483 1502-3885 journal-article 2002 crwiley https://doi.org/10.1111/j.1502-3885.2002.tb01060.x 2024-06-18T04:13:56Z This paper reviews the deglaciation history and palaeoclimate from 22 to 9.5 14 Cka BP in the Andfjord‐Vagsfjord area. Eight main glacial events are recorded: The Egga‐I (>22 14 Cka BP), the Bjerka, the Egga‐II (>14.6 14 Cka BP), the Flesen (14.5 14 Cka BP), the D (13.8–13.2 14 Cka BP), the Skarpnes (12.2 14 Cka BP), the Tromsø–Lyngen (10.7–10.3 14 C ka BP) and the Stordal (10.0–9.5 14 Cka BP). Onset of the final deglaciation occurred about 14.6 14 Cka BP. Most of the western part of the Fennoscandian and Barents Sea Ice Sheets receded from the outer continental shelf 15–14 14 Cka BP. The delivery and melting of icebergs at this time to the Norwegian‐Greenland Sea resulted in a low oxygen isotope event recorded in a number of cores in the region. Atlantic water intruded the area 13.2 14 Cka BP, and an atmospheric warming commenced 12.9/12.8 14 Cka BP. A marked glacial recession occurred before the Skarpnes event. During Allerød time, the glaciers retreated to the fjord heads or even farther inland. The Fennoscandian outlet glaciers readvanced (locally more than 40 km), reached their Younger Dryas outer limit after 10.7 14 Cka BP and retreated from this position before about 10.3 14 Cka BP. Article in Journal/Newspaper Barents Sea Fennoscandian Greenland Greenland Sea North Norway Sea ice Tromsø Lyngen Wiley Online Library Barents Sea Greenland Norway Tromsø Egga ENVELOPE(14.802,14.802,68.830,68.830) Skarpnes ENVELOPE(7.816,7.816,63.405,63.405) Boreas 31 2 97 125 |
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Open Polar |
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Wiley Online Library |
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crwiley |
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English |
description |
This paper reviews the deglaciation history and palaeoclimate from 22 to 9.5 14 Cka BP in the Andfjord‐Vagsfjord area. Eight main glacial events are recorded: The Egga‐I (>22 14 Cka BP), the Bjerka, the Egga‐II (>14.6 14 Cka BP), the Flesen (14.5 14 Cka BP), the D (13.8–13.2 14 Cka BP), the Skarpnes (12.2 14 Cka BP), the Tromsø–Lyngen (10.7–10.3 14 C ka BP) and the Stordal (10.0–9.5 14 Cka BP). Onset of the final deglaciation occurred about 14.6 14 Cka BP. Most of the western part of the Fennoscandian and Barents Sea Ice Sheets receded from the outer continental shelf 15–14 14 Cka BP. The delivery and melting of icebergs at this time to the Norwegian‐Greenland Sea resulted in a low oxygen isotope event recorded in a number of cores in the region. Atlantic water intruded the area 13.2 14 Cka BP, and an atmospheric warming commenced 12.9/12.8 14 Cka BP. A marked glacial recession occurred before the Skarpnes event. During Allerød time, the glaciers retreated to the fjord heads or even farther inland. The Fennoscandian outlet glaciers readvanced (locally more than 40 km), reached their Younger Dryas outer limit after 10.7 14 Cka BP and retreated from this position before about 10.3 14 Cka BP. |
format |
Article in Journal/Newspaper |
author |
VORREN, TORE O. PLASSEN, LIV |
spellingShingle |
VORREN, TORE O. PLASSEN, LIV Deglaciation and palaeoclimate of the Andfjord‐Vågsfjord area, North Norway |
author_facet |
VORREN, TORE O. PLASSEN, LIV |
author_sort |
VORREN, TORE O. |
title |
Deglaciation and palaeoclimate of the Andfjord‐Vågsfjord area, North Norway |
title_short |
Deglaciation and palaeoclimate of the Andfjord‐Vågsfjord area, North Norway |
title_full |
Deglaciation and palaeoclimate of the Andfjord‐Vågsfjord area, North Norway |
title_fullStr |
Deglaciation and palaeoclimate of the Andfjord‐Vågsfjord area, North Norway |
title_full_unstemmed |
Deglaciation and palaeoclimate of the Andfjord‐Vågsfjord area, North Norway |
title_sort |
deglaciation and palaeoclimate of the andfjord‐vågsfjord area, north norway |
publisher |
Wiley |
publishDate |
2002 |
url |
http://dx.doi.org/10.1111/j.1502-3885.2002.tb01060.x https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fj.1502-3885.2002.tb01060.x https://onlinelibrary.wiley.com/doi/pdf/10.1111/j.1502-3885.2002.tb01060.x |
long_lat |
ENVELOPE(14.802,14.802,68.830,68.830) ENVELOPE(7.816,7.816,63.405,63.405) |
geographic |
Barents Sea Greenland Norway Tromsø Egga Skarpnes |
geographic_facet |
Barents Sea Greenland Norway Tromsø Egga Skarpnes |
genre |
Barents Sea Fennoscandian Greenland Greenland Sea North Norway Sea ice Tromsø Lyngen |
genre_facet |
Barents Sea Fennoscandian Greenland Greenland Sea North Norway Sea ice Tromsø Lyngen |
op_source |
Boreas volume 31, issue 2, page 97-125 ISSN 0300-9483 1502-3885 |
op_rights |
http://onlinelibrary.wiley.com/termsAndConditions#vor |
op_doi |
https://doi.org/10.1111/j.1502-3885.2002.tb01060.x |
container_title |
Boreas |
container_volume |
31 |
container_issue |
2 |
container_start_page |
97 |
op_container_end_page |
125 |
_version_ |
1809901081943080960 |