Sedimentology of ODP Leg 104 holes ...

The long-term record of glacial/interglacial cycles indicates three major paleoceanographic regimes in the Norwegian Sea. The period since the first major glaciation over Scandinavia at 2.56 Ma is characterized by high-frequency, low-amplitude oscillations of ice-rafted debris inputs, a lowered sali...

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Main Author: Henrich, Rüdiger
Format: Article in Journal/Newspaper
Language:English
Published: PANGAEA 1989
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.736351
https://doi.pangaea.de/10.1594/PANGAEA.736351
id ftdatacite:10.1594/pangaea.736351
record_format openpolar
spelling ftdatacite:10.1594/pangaea.736351 2024-09-15T18:26:43+00:00 Sedimentology of ODP Leg 104 holes ... Henrich, Rüdiger 1989 application/zip https://dx.doi.org/10.1594/pangaea.736351 https://doi.pangaea.de/10.1594/PANGAEA.736351 en eng PANGAEA https://dx.doi.org/10.2973/odp.proc.sr.104.116.1989 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Drilling/drill rig Leg104 Joides Resolution Ocean Drilling Program ODP article Collection Supplementary Publication Series of Datasets 1989 ftdatacite https://doi.org/10.1594/pangaea.73635110.2973/odp.proc.sr.104.116.1989 2024-08-01T10:53:32Z The long-term record of glacial/interglacial cycles indicates three major paleoceanographic regimes in the Norwegian Sea. The period since the first major glaciation over Scandinavia at 2.56 Ma is characterized by high-frequency, low-amplitude oscillations of ice-rafted debris inputs, a lowered salinity, and decreased carbonate shell production in surface waters as well as overall strong carbonate dissolution at the sea floor. These conditions indicate a more zonal circulation pattern in the Northern Hemisphere and a relative isolation of surface and bottom waters in the Norwegian Sea. The generally temperate glacial climate was only interrupted by episodic weak intrusions of warm Atlantic waters. These intrusions have been detected in considerable magnitude only at Site 644, and thus are restricted to areas much closer to the Norwegian shelf than during earlier periods. The interval from 1.2 to 0.6 Ma is characterized by an increase in carbonate shell production and a better preservation, as well as a ... : Supplement to: Henrich, Rüdiger (1989): Glacial/interglacial cycles in the Norwegian Sea: sedimentology, paleoceanography, and evolution of late Pliocene to Quaternary northern hemisphere climate. In: Eldholm, O; Thiede, J; Taylor, E; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 104, 189-232 ... Article in Journal/Newspaper Norwegian Sea DataCite
institution Open Polar
collection DataCite
op_collection_id ftdatacite
language English
topic Drilling/drill rig
Leg104
Joides Resolution
Ocean Drilling Program ODP
spellingShingle Drilling/drill rig
Leg104
Joides Resolution
Ocean Drilling Program ODP
Henrich, Rüdiger
Sedimentology of ODP Leg 104 holes ...
topic_facet Drilling/drill rig
Leg104
Joides Resolution
Ocean Drilling Program ODP
description The long-term record of glacial/interglacial cycles indicates three major paleoceanographic regimes in the Norwegian Sea. The period since the first major glaciation over Scandinavia at 2.56 Ma is characterized by high-frequency, low-amplitude oscillations of ice-rafted debris inputs, a lowered salinity, and decreased carbonate shell production in surface waters as well as overall strong carbonate dissolution at the sea floor. These conditions indicate a more zonal circulation pattern in the Northern Hemisphere and a relative isolation of surface and bottom waters in the Norwegian Sea. The generally temperate glacial climate was only interrupted by episodic weak intrusions of warm Atlantic waters. These intrusions have been detected in considerable magnitude only at Site 644, and thus are restricted to areas much closer to the Norwegian shelf than during earlier periods. The interval from 1.2 to 0.6 Ma is characterized by an increase in carbonate shell production and a better preservation, as well as a ... : Supplement to: Henrich, Rüdiger (1989): Glacial/interglacial cycles in the Norwegian Sea: sedimentology, paleoceanography, and evolution of late Pliocene to Quaternary northern hemisphere climate. In: Eldholm, O; Thiede, J; Taylor, E; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 104, 189-232 ...
format Article in Journal/Newspaper
author Henrich, Rüdiger
author_facet Henrich, Rüdiger
author_sort Henrich, Rüdiger
title Sedimentology of ODP Leg 104 holes ...
title_short Sedimentology of ODP Leg 104 holes ...
title_full Sedimentology of ODP Leg 104 holes ...
title_fullStr Sedimentology of ODP Leg 104 holes ...
title_full_unstemmed Sedimentology of ODP Leg 104 holes ...
title_sort sedimentology of odp leg 104 holes ...
publisher PANGAEA
publishDate 1989
url https://dx.doi.org/10.1594/pangaea.736351
https://doi.pangaea.de/10.1594/PANGAEA.736351
genre Norwegian Sea
genre_facet Norwegian Sea
op_relation https://dx.doi.org/10.2973/odp.proc.sr.104.116.1989
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.73635110.2973/odp.proc.sr.104.116.1989
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