Age models of ODP sites from the Barents Sea-Svalbard region ...

Based on a revised chronostratigraphy, and compilation of borehole data from the Barents Sea continental margin, a coherent glaciation model is proposed for the Barents Sea ice sheet over the past 3.5 million years (Ma). Three phases of ice growth are suggested: (1) The initial build-up phase, cover...

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Main Authors: Knies, Jochen, Matthiessen, Jens, Vogt, Christoph, Laberg, Jan Sverre, Hjelstuen, Berit O, Smelror, Morten, Larsen, Eiliv, Andreassen, Karin, Eidvin, Tor, Vorren, Tore O
Format: Article in Journal/Newspaper
Language:English
Published: PANGAEA 2009
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.817589
https://doi.pangaea.de/10.1594/PANGAEA.817589
id ftdatacite:10.1594/pangaea.817589
record_format openpolar
spelling ftdatacite:10.1594/pangaea.817589 2024-09-15T17:57:39+00:00 Age models of ODP sites from the Barents Sea-Svalbard region ... Knies, Jochen Matthiessen, Jens Vogt, Christoph Laberg, Jan Sverre Hjelstuen, Berit O Smelror, Morten Larsen, Eiliv Andreassen, Karin Eidvin, Tor Vorren, Tore O 2009 application/zip https://dx.doi.org/10.1594/pangaea.817589 https://doi.pangaea.de/10.1594/PANGAEA.817589 en eng PANGAEA https://dx.doi.org/10.1016/j.quascirev.2008.12.002 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Ocean Drilling Program ODP article Collection Supplementary Publication Series of Datasets 2009 ftdatacite https://doi.org/10.1594/pangaea.81758910.1016/j.quascirev.2008.12.002 2024-08-01T10:53:02Z Based on a revised chronostratigraphy, and compilation of borehole data from the Barents Sea continental margin, a coherent glaciation model is proposed for the Barents Sea ice sheet over the past 3.5 million years (Ma). Three phases of ice growth are suggested: (1) The initial build-up phase, covering mountainous regions and reaching the coastline/shelf edge in the northern Barents Sea during short-term glacial intensification, is concomitant with the onset of the Northern Hemisphere Glaciation (3.6-2.4 Ma). (2) A transitional growth phase (2.4-1.0 Ma), during which the ice sheet expanded towards the southern Barents Sea and reached the northwestern Kara Sea. This is inferred from step-wise decrease of Siberian river-supplied smectite-rich sediments, likely caused by ice sheet blockade and possibly reduced sea ice formation in the Kara Sea as well as glacigenic wedge growth along the northwestern Barents Sea margin hampering entrainment and transport of sea ice sediments to the Arctic-Atlantic gateway. (3) ... : Supplement to: Knies, Jochen; Matthiessen, Jens; Vogt, Christoph; Laberg, Jan Sverre; Hjelstuen, Berit O; Smelror, Morten; Larsen, Eiliv; Andreassen, Karin; Eidvin, Tor; Vorren, Tore O (2009): The Plio-Pleistocene glaciation of the Barents Sea–Svalbard region: a new model based on revised chronostratigraphy. Quaternary Science Reviews, 28(9-10), 812-829 ... Article in Journal/Newspaper Barents Sea Ice Sheet Kara Sea Sea ice Svalbard DataCite
institution Open Polar
collection DataCite
op_collection_id ftdatacite
language English
topic Ocean Drilling Program ODP
spellingShingle Ocean Drilling Program ODP
Knies, Jochen
Matthiessen, Jens
Vogt, Christoph
Laberg, Jan Sverre
Hjelstuen, Berit O
Smelror, Morten
Larsen, Eiliv
Andreassen, Karin
Eidvin, Tor
Vorren, Tore O
Age models of ODP sites from the Barents Sea-Svalbard region ...
topic_facet Ocean Drilling Program ODP
description Based on a revised chronostratigraphy, and compilation of borehole data from the Barents Sea continental margin, a coherent glaciation model is proposed for the Barents Sea ice sheet over the past 3.5 million years (Ma). Three phases of ice growth are suggested: (1) The initial build-up phase, covering mountainous regions and reaching the coastline/shelf edge in the northern Barents Sea during short-term glacial intensification, is concomitant with the onset of the Northern Hemisphere Glaciation (3.6-2.4 Ma). (2) A transitional growth phase (2.4-1.0 Ma), during which the ice sheet expanded towards the southern Barents Sea and reached the northwestern Kara Sea. This is inferred from step-wise decrease of Siberian river-supplied smectite-rich sediments, likely caused by ice sheet blockade and possibly reduced sea ice formation in the Kara Sea as well as glacigenic wedge growth along the northwestern Barents Sea margin hampering entrainment and transport of sea ice sediments to the Arctic-Atlantic gateway. (3) ... : Supplement to: Knies, Jochen; Matthiessen, Jens; Vogt, Christoph; Laberg, Jan Sverre; Hjelstuen, Berit O; Smelror, Morten; Larsen, Eiliv; Andreassen, Karin; Eidvin, Tor; Vorren, Tore O (2009): The Plio-Pleistocene glaciation of the Barents Sea–Svalbard region: a new model based on revised chronostratigraphy. Quaternary Science Reviews, 28(9-10), 812-829 ...
format Article in Journal/Newspaper
author Knies, Jochen
Matthiessen, Jens
Vogt, Christoph
Laberg, Jan Sverre
Hjelstuen, Berit O
Smelror, Morten
Larsen, Eiliv
Andreassen, Karin
Eidvin, Tor
Vorren, Tore O
author_facet Knies, Jochen
Matthiessen, Jens
Vogt, Christoph
Laberg, Jan Sverre
Hjelstuen, Berit O
Smelror, Morten
Larsen, Eiliv
Andreassen, Karin
Eidvin, Tor
Vorren, Tore O
author_sort Knies, Jochen
title Age models of ODP sites from the Barents Sea-Svalbard region ...
title_short Age models of ODP sites from the Barents Sea-Svalbard region ...
title_full Age models of ODP sites from the Barents Sea-Svalbard region ...
title_fullStr Age models of ODP sites from the Barents Sea-Svalbard region ...
title_full_unstemmed Age models of ODP sites from the Barents Sea-Svalbard region ...
title_sort age models of odp sites from the barents sea-svalbard region ...
publisher PANGAEA
publishDate 2009
url https://dx.doi.org/10.1594/pangaea.817589
https://doi.pangaea.de/10.1594/PANGAEA.817589
genre Barents Sea
Ice Sheet
Kara Sea
Sea ice
Svalbard
genre_facet Barents Sea
Ice Sheet
Kara Sea
Sea ice
Svalbard
op_relation https://dx.doi.org/10.1016/j.quascirev.2008.12.002
op_rights Creative Commons Attribution 3.0 Unported
https://creativecommons.org/licenses/by/3.0/legalcode
cc-by-3.0
op_doi https://doi.org/10.1594/pangaea.81758910.1016/j.quascirev.2008.12.002
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