Climatic changes in the Norwegian Sea during the last 2.8 Ma

Prior to ODP Leg 104 no continuous paleoclimatic records older than 0.4Ma were available from the Norwegian Sea. Only scattered information on the late Neogene and early Quaternary was provided from the sites drilled by DSDP Leg 38. No continental Plio-Pleistocene records older than the penultimate...

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Published in:Polar Research
Main Authors: Jansen, E., Bleil, U., Henrich, R., Kringstad, L., Slettemark, B.
Format: Article in Journal/Newspaper
Language:English
Published: Norwegian Polar Institute 1987
Subjects:
Online Access:https://polarresearch.net/index.php/polar/article/view/2477
https://doi.org/10.3402/polar.v5i3.6905
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spelling ftjpolarres:oai:journals.openacademia.net:article/2477 2023-05-15T17:46:56+02:00 Climatic changes in the Norwegian Sea during the last 2.8 Ma Jansen, E. Bleil, U. Henrich, R. Kringstad, L. Slettemark, B. 1987-01-12 application/pdf https://polarresearch.net/index.php/polar/article/view/2477 https://doi.org/10.3402/polar.v5i3.6905 eng eng Norwegian Polar Institute https://polarresearch.net/index.php/polar/article/view/2477/5728 https://polarresearch.net/index.php/polar/article/view/2477 doi:10.3402/polar.v5i3.6905 Copyright (c) 2018 Polar Research Polar Research; Vol. 5 No. 3 (1987); 329-332 1751-8369 info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion 1987 ftjpolarres https://doi.org/10.3402/polar.v5i3.6905 2021-11-11T19:12:43Z Prior to ODP Leg 104 no continuous paleoclimatic records older than 0.4Ma were available from the Norwegian Sea. Only scattered information on the late Neogene and early Quaternary was provided from the sites drilled by DSDP Leg 38. No continental Plio-Pleistocene records older than the penultimate glacial (about 0.13 Ma) are known from the Scandinavian Peninsula, which has been the major accumulation area of late Cenozoic ice sheets in Europe. Article in Journal/Newspaper Norwegian Sea Polar Research Polar Research (E-Journal) Norwegian Sea Polar Research 5 3 329 332
institution Open Polar
collection Polar Research (E-Journal)
op_collection_id ftjpolarres
language English
description Prior to ODP Leg 104 no continuous paleoclimatic records older than 0.4Ma were available from the Norwegian Sea. Only scattered information on the late Neogene and early Quaternary was provided from the sites drilled by DSDP Leg 38. No continental Plio-Pleistocene records older than the penultimate glacial (about 0.13 Ma) are known from the Scandinavian Peninsula, which has been the major accumulation area of late Cenozoic ice sheets in Europe.
format Article in Journal/Newspaper
author Jansen, E.
Bleil, U.
Henrich, R.
Kringstad, L.
Slettemark, B.
spellingShingle Jansen, E.
Bleil, U.
Henrich, R.
Kringstad, L.
Slettemark, B.
Climatic changes in the Norwegian Sea during the last 2.8 Ma
author_facet Jansen, E.
Bleil, U.
Henrich, R.
Kringstad, L.
Slettemark, B.
author_sort Jansen, E.
title Climatic changes in the Norwegian Sea during the last 2.8 Ma
title_short Climatic changes in the Norwegian Sea during the last 2.8 Ma
title_full Climatic changes in the Norwegian Sea during the last 2.8 Ma
title_fullStr Climatic changes in the Norwegian Sea during the last 2.8 Ma
title_full_unstemmed Climatic changes in the Norwegian Sea during the last 2.8 Ma
title_sort climatic changes in the norwegian sea during the last 2.8 ma
publisher Norwegian Polar Institute
publishDate 1987
url https://polarresearch.net/index.php/polar/article/view/2477
https://doi.org/10.3402/polar.v5i3.6905
geographic Norwegian Sea
geographic_facet Norwegian Sea
genre Norwegian Sea
Polar Research
genre_facet Norwegian Sea
Polar Research
op_source Polar Research; Vol. 5 No. 3 (1987); 329-332
1751-8369
op_relation https://polarresearch.net/index.php/polar/article/view/2477/5728
https://polarresearch.net/index.php/polar/article/view/2477
doi:10.3402/polar.v5i3.6905
op_rights Copyright (c) 2018 Polar Research
op_doi https://doi.org/10.3402/polar.v5i3.6905
container_title Polar Research
container_volume 5
container_issue 3
container_start_page 329
op_container_end_page 332
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